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
41291|30 Foot seam|44244|6|Mentioned|p325 Tb. 10|||Informal alternative name for Weismantel seam.||||||
38992|500 Acre Granodiorite|23866|5|Briefly described|p121 Fig. 1|||See also Five Hundred Acre Granodiorite.  Geological Province: Murrumbidgee Batholith.  See also p123 Fig. 3.||||||07-MAR-05
30639|Aaron's Pass Granite|24126|5|Briefly described|p4|||||||||
30639|Aaron's Pass Granite|43316|14|Not recorded|p15|||||||||
38225|Abbay Green Coal|23717|5|Briefly described|p118 Fig. 2|||Misspelt - see Abbey Green Coal.||||||
69590|Abercrombie Province Volcanics|61155|5|Briefly described|p19|Middle Miocene|Middle Eocene|In the Bathurst-Goulburn region. ||||||
68164|Aberdare conglomerate|60281|6|Mentioned|p27|||Informal name. Geological Province: Clarence-Moreton Basin.||||||
83045|Abroi granodiorites|73202|6|Mentioned|p637|Asselian|Kasimovian|New England Orogen, southern. Zircon U-Pb crystallisation age from Collins et al., (1993). [Misspelling of Abroi Granodiorite?]|302 +/- 4 Ma U-Pb zircon|Hillgrove Plutonic Supersuite||||
24643|Acacia Downs quartzite|33734|6|Mentioned|p494|||Refers Webby (1970).||||||
70246|Acheron Ledge Siltstone""|60902|6|Mentioned|p873|||Of Ralser (1981).  Possibly a correlative of the argillaceous part of Bogolo Formation.||||||
31122|Acton Limestone|43481|6|Mentioned|12,13|||Member of Canberra Formation.||||||07-MAY-07
24644|Acton Limestone Member""|33328|6|Mentioned|p12|||||||||
24644|Acton Limestone Member""|40328|6|Mentioned|p57|||||||||
24644|Acton Limestone Member""|41356|6|Mentioned|p5|||||||||
24644|Acton Limestone Member""|42820|6|Mentioned|p15|||refers to Opik (1954,1958)||||||
31040|Acton limestone|44970|14|Not recorded|p24|||||||||
31040|Acton limestone|73211|6|Mentioned|p909|||||Canberra Formation||||
70247|Adaminaby Group""|60902|6|Mentioned|p873|Early Ordovician|Early Ordovician|Informal - see Adaminaby Group.||||||11-APR-06
34570|Adaminaby beds""|22815|6|Mentioned|p18|Ordovician|Ordovician|proposal of upgrading and redefinition of this unit .||||||
34570|Adaminaby beds""|23170|6|Mentioned|p29|||now part of the Adaminably Group.||||||
38443|Adaminaby group|23309|5|Briefly described|p5 Fig. 1.3|Ordovician|Ordovician|Misspelt-see Adaminaby Group.||||||
38443|Adaminaby group|24133|5|Briefly described|p20 Fig. 8|||Informal name - see Adaminaby Group.  Geological Province: Lachlan Fold Belt.||||||
38443|Adaminaby group|24551|6|Mentioned|p96 Fig.4.1|||Informal - see Adaminaby Group||||||
38443|Adaminaby group|60541|6|Mentioned|p16|||Informal name.||||||
38443|Adaminaby group|60542|6|Mentioned|p17|Early Silurian|Early Silurian|Informal name. ||||||
38443|Adaminaby group|61160|6|Mentioned|p44|||Informal - see Adaminaby Group.||||||
34203|Adelaidean sequence|22671|6|Mentioned|p832||Neoproterozoic|||||||
34203|Adelaidean sequence|22772|5|Briefly described|p62-63,Table13.1,71|Neoproterozoic III|Cryogenian|||||||
34203|Adelaidean sequence|22858|6|Mentioned|Fig14.8p96|||||||||
34203|Adelaidean sequence|22933|6|Mentioned|Table11.1p5,10|Neoproterozoic III|Cryogenian|||||||
31840|Adelargo Member|23392|6|Mentioned|p6|||parent: Illunie Volcanics||||||
31840|Adelargo Member|24417|4|Described|p124|Middle Devonian|Middle Devonian|Of Warrumba Volcanics.  Formerly "Adelargo Volcanics".||||||
31840|Adelargo Member|60009|5|Briefly described|Map Legend|Givetian|Givetian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||13-JUL-04
38941|Adelargo Volcanics""|24417|6|Mentioned|p119|||Now included in the Warrumba Volcanics as the Adelargo Member.||||||
24648|Adelong Gabbro|42726|5|Briefly described|map legend|||453. Variation on Adelong Norite, Adelong Granite?||||||
31043|Ainslie Orogenic Phase|44970|14|Not recorded|p56||Early Devonian|||||||
31042|Ainslie bedded tuffs|44970|14|Not recorded|p56||Early Devonian|||||||
31041|Ainslie dacites|44970|14|Not recorded|p33,44|||||||||
31044|Ainslie rhyolites|44970|14|Not recorded|p64||Early Devonian|||||||
69593|Airly Province Volcanics|61155|5|Briefly described|p19|Early Oligocene|Middle Eocene|Overlies the Neriga Province Volcanics.  In the Bathurst-Goulburn region. ||||||
37944|Aldas Tank Formation|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
29199|Alders Tank Formation|6823|6|Mentioned|p205|||||Thackaringa Group||||
29199|Alders Tank Formation|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
29199|Alders Tank Formation|22575|6|Mentioned|p179 Fig.2|||Of the Thackaringa Group.||||||11-JUN-08
29199|Alders Tank Formation|22771|6|Mentioned|Table12.2p45|||||||||
29199|Alders Tank Formation|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackeringa Group. Max. thickness: 200m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
29199|Alders Tank Formation|22965|6|Mentioned|Fig 1||Statherian|Part of the Thackaringa Group.||||||
29199|Alders Tank Formation|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
29199|Alders Tank Formation|22967|6|Mentioned|p39||Statherian|||||||
29199|Alders Tank Formation|23025|6|Mentioned|Fig1p75|||||||||
29199|Alders Tank Formation|23160|6|Mentioned|fig1|||||||||
29199|Alders Tank Formation|23248|5|Briefly described|Fig2p169|||||||||
29199|Alders Tank Formation|38969|4|Described|p206|||||||||
29199|Alders Tank Formation|39662|2|Defined|p417|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29199|Alders Tank Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29199|Alders Tank Formation|39849|6|Mentioned|Table 2|||||||||
29199|Alders Tank Formation|40290|6|Mentioned|Fig.2|||||||||
29199|Alders Tank Formation|40822|6|Mentioned|Fig.2|||||||||
29199|Alders Tank Formation|41093|6|Mentioned|p252|||||||||
29199|Alders Tank Formation|41145|6|Mentioned|Fig.4|||||||||
29199|Alders Tank Formation|41630|6|Mentioned|Fig.1.3|||||||||
29199|Alders Tank Formation|41633|6|Mentioned|Fig.2.14|||||||||
29199|Alders Tank Formation|42261|6|Mentioned|Fig 1 P530|||||||||
29199|Alders Tank Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
29199|Alders Tank Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
29199|Alders Tank Formation|42537|6|Mentioned|p8|||||||||
29199|Alders Tank Formation|43052|6|Mentioned|Fig.4.22|||||||||
29199|Alders Tank Formation|43086|6|Mentioned|Fig.3|||||||||
29199|Alders Tank Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
29199|Alders Tank Formation|43572|6|Mentioned|Fig.3.2 p6|||||||||
29199|Alders Tank Formation|46598|4|Described|p303|||||||||
29199|Alders Tank 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 Cues Formation. Underlain by Lady Brassey Formation and Alma Gneiss.||||||31-MAY-07
29199|Alders Tank Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
29199|Alders Tank Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group. Geological Province: Broken Hill Domain.||||||11-JUN-08
29199|Alders Tank Formation|61606|5|Briefly described|p4 Fig.2|||Of the Thackaringa Group.||||||18-MAY-06
29199|Alders Tank Formation|61735|5|Briefly described|p636 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Presented as Alders Tank only in Fig. 2.||||||30-JUN-09
29199|Alders Tank Formation|62536|5|Briefly described|p636|||Broken Hill area.||Thackaringa Group.||Hosts Alma Gneiss.||
29199|Alders Tank Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
29199|Alders Tank Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group||||15-DEC-21
29199|Alders Tank Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
29199|Alders Tank Formation|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological Province: Broken Hill Block-Euriowie Block.||||||07-SEP-15
29199|Alders Tank Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province||Thackaringa Group||||
29199|Alders Tank Formation|64097|5|Briefly described|p306, p320|||Of the Thackaringa Group. Recommendation is for name to be discontinued and rocks to be incorporated into Cues Formation.||||||07-FEB-11
29199|Alders Tank Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Geological province: Broken Hill Domain.||||||07-FEB-11
29199|Alders Tank Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Geological province: Broken Hill Domain.||||||07-FEB-11
29199|Alders Tank Formation|66302|5|Briefly described|p36 Fig.9, p39|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Appears as Alders Creek Formation on p39.||Thackaringa Group||Overlies the Lady Brassey Formation. Overlain by the Cues Formation.||
29199|Alders Tank Formation|70014|5|Briefly described|Map legend|||The composite gneisses range from quartzo-feldspathic and psammopelitic in the SW, to psammitic/psammopelitic elsewhere. In the Broken Hill Synform the composite gneiss is quartzo-feldspathic and very cordierite-rich near the base.||Unit in Thackaringa Group.||Overlies Lady Brassey Formation. Is overlain by Cues Formation.|Consists largely of composite gneisses, with little or no basic gneiss, local minor plagioclase-quartz rocks and minor granular quartz-iron oxide/iron sulfide "lode" rocks.|
29199|Alders Tank Formation|70405|6|Mentioned|p9 table 1|Paleoproterozoic|Paleoproterozoic||1700 Ma|Thackaringa Group||||
29199|Alders Tank Formation|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|<1705 Ma|Thackaringa Group||Underlies Cues Formation. Overlies Lady Brassey Formation and Alma Gneiss of Silver City Suite.||
29199|Alders Tank Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Thackaringa Group.||||
29199|Alders Tank Formation|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Thackaringa Group||Overlies Lady Brassey Formation, underlies Cues Formation||
30966|Allandale Formation Basalt Member|43440|14|Not recorded|p74|||||||||
30754|Allandale Stage|43344|14|Not recorded|p84||Permian|Now called Allandale Formation||||||
30754|Allandale Stage|43440|14|Not recorded|p91|||Ref. to David 1950. See also Lexicon||||||
30754|Allandale Stage|43477|14|Not recorded|pg not known|||||||||
30754|Allandale Stage|44855|14|Not recorded|p25|Permian|Carboniferous|||||||
34079|Allandale-Lochinvar Formation|22612|6|Mentioned|424|||Geological province: Sydney Basin. Max. thickness: 900 m.||||||23-JUL-08
73836|Allans Creek Sandstone|24471|4|Described|p31 Fig.3|Late Permian|Late Permian|Overlies Bargo Claystone. Overlain by Kembla Sandstone. Contains American Coal Member. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Adamstown Formation. Geological Province: Sydney Basin.||||||07-FEB-11
70447|Allawa Member|62095|6|Mentioned|p260 Tb. 1|Late Carboniferous|Late Carboniferous|Abbreviated form of Allawa Ignimbrite Member.  Age: 311.5+/-2.9Ma.||||||
69436|Allawa Tuff Member|62095|6|Mentioned|p276 Appdx.|Late Carboniferous|Late Carboniferous|Of Kelk (1986). Superseded by Allawa Ignimbrite Member.||||||22-MAY-06
69436|Allawa Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
69436|Allawa Tuff Member|68005|6|Mentioned|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
32827|Allendale Beds|48831|14|Not recorded|p.8|||||||||
35213|Allendale Formation|22969|4|Described|p 16,18, Fig 2.2||Early Permian|Of the Dalwood Group. Age is Sakmarian, ~289 Ma.||||||23-JUL-08
35213|Allendale Formation|67663|6|Mentioned|p518, p519 Fig. 1|Permian|Permian|Early Permian.||Of the Dalwood Group.||||
29736|Alley Formation|43032|5|Briefly described|Table 1,p8|||Rayner 1969||||||
34442|Alloway Bank Conglomerate|22750|6|Mentioned|p 228|||Of Drik Drik Formation.||||||
70669|Alloway Bank Conglomerate Member""|50094|5|Briefly described|p316|Emsian|Emsian|Basal part of Drik Drik Formation.||||||
30919|Allston Limestone Member|43417|14|Not recorded|Map Legend||Givetian|||||||
69945|Alma Formation|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: 1704+/-3Ma (Page et al 2000a,b). Geological Province: Broken Hill-Olary region.||||||07-NOV-08
69945|Alma Formation|72037|5|Briefly described|p862|||Geological province: New England Orogen, Gympie Terrane. Nomenclature of Arnold (1996). Depositional environment: deepwater marine. LA-ICP-MS peak detrital zircon U-Th-Pb ages include 302, 345, 384, 427 and 505 Ma.||Unit of Rammutt Formation|||Pale green, massive or laminated mudstone and siltstone interbedded with fine-grained tuffaceous rocks and hyaloclastites,|
24654|Alma Gneiss|6823|5|Briefly described|p203, 205-208, 210-211, 213-215,|Palaeoproterozoic|Palaeoproterozoic|Previously interpreted as volcanic in origin, interpreted now as highly deformed granites. A metamorphic age of 1670 +/- 100 Ma (Rb-Sr whole rock) has been derived from Pidgeon (1967). An additional Metamorphic age of 1594 +/- 15 Ma is derived from this study. Numerous additional SHRIMP ages are provided on p8(210) table 3. Zircons, zircon morphology and analytical results are discussed in detail. See also p220, 222-223, 232-234, 236.|1691 +/- 11 Ma (U-Pb zircon) crystallisation|Base of Thackaringa Group?|||Megacrystic gneiss.|26-MAR-22
24654|Alma Gneiss|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Thakaringa Group (Willyama Supergroup).||||||11-SEP-07
24654|Alma Gneiss|22575|6|Mentioned|p179 Fig.2|||of the Thackaringa Group||||||
24654|Alma Gneiss|22771|6|Mentioned|Table12.2p45,45|||||||||
24654|Alma Gneiss|22788|6|Mentioned|p48|||||||||
24654|Alma Gneiss|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackeringa Group. Supersedes Alma augen gneiss. Lady Brassey Formation is lateral equivalent. Max. thickness: 1000m. Geological Province: Willyama Fold belt.||||||07-NOV-08
24654|Alma Gneiss|22965|5|Briefly described|p13,14,Fig1||Statherian|||||||
24654|Alma Gneiss|22966|6|Mentioned|p3 Fig 1||Proterozoic|Early rift stage of development.||||||
24654|Alma Gneiss|22967|6|Mentioned|p39||Statherian|||||||
24654|Alma Gneiss|23025|6|Mentioned|Fig1p75|||||||||
24654|Alma Gneiss|23160|6|Mentioned|fig1|||||||||
24654|Alma Gneiss|23248|5|Briefly described|Fig2p169|||||||||
24654|Alma Gneiss|24197|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. Age: 1691+/-12Ma. Geological province: Broken Hill Inlier.||||||07-FEB-11
24654|Alma Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|Of the Thackaringa Group.||||||11-SEP-07
24654|Alma Gneiss|38969|4|Described|p206|||||||||
24654|Alma Gneiss|39662|2|Defined|p415|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24654|Alma Gneiss|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24654|Alma Gneiss|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24654|Alma Gneiss|39849|6|Mentioned|Table 2|||||||||
24654|Alma Gneiss|40290|6|Mentioned|p1|||||||||
24654|Alma Gneiss|40822|6|Mentioned|Fig.2|||||||||
24654|Alma Gneiss|41093|6|Mentioned|p252|||||||||
24654|Alma Gneiss|41145|6|Mentioned|Fig.4|||||||||
24654|Alma Gneiss|41633|6|Mentioned|Fig.2.2|||||||||
24654|Alma Gneiss|42261|6|Mentioned|Fig 1 P530|||||||||
24654|Alma Gneiss|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24654|Alma Gneiss|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24654|Alma Gneiss|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24654|Alma Gneiss|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24654|Alma Gneiss|42537|4|Described|p10|||||||||
24654|Alma Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
24654|Alma Gneiss|42897|5|Briefly described|Fig.3, P321|||||||||
24654|Alma Gneiss|43052|5|Briefly described|p95|||||||||
24654|Alma Gneiss|43086|6|Mentioned|Fig.3|||||||||
24654|Alma Gneiss|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Thackaringa Group.||||||07-NOV-08
24654|Alma Gneiss|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the of Thackaringa Group.||||||07-NOV-08
24654|Alma Gneiss|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of  Lady Brassey Formation.||||||07-NOV-08
24654|Alma Gneiss|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Thackaringa Group.||||||07-NOV-08
24654|Alma Gneiss|43485|6|Mentioned|2|||||||||
24654|Alma Gneiss|43572|6|Mentioned|Fig.3.2 p6|||||||||
24654|Alma Gneiss|46595|14|Not recorded|p.288,294,296-319|||On many pages. p.296,297,304,305,309-311,319. 1670 +/- 100 m.y. Age determinations. (H54-15,T54-3).||||||
24654|Alma Gneiss|46598|6|Mentioned|p303|||||||||
24654|Alma Gneiss|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 Kyong Formation; underlain by Thorndale Composite Gneiss.||||||31-MAY-07
24654|Alma Gneiss|50606|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. Geological Province: Broken Hill Block.  Age: 1670 +/- 100Ma (U-Pb)||||||07-NOV-08
24654|Alma Gneiss|50619|5|Briefly described|p178 Fig. 3||Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
24654|Alma Gneiss|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|S-type. Intrudes the Thackaringa Group.  Age: 1704+/-3Ma.  Geological Province: Broken Hill Domain.||||||03-MAR-05
24654|Alma Gneiss|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: 1704+/-4Ma||||||07-NOV-08
24654|Alma Gneiss|61735|5|Briefly described|p634, p636, p642|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Magmatic age: 1704+/-3Ma. Metamorphic age 1610+/-9Ma. U/Pb SHRIMP. Felsic gneiss unit of the Broken Hill Domain. See also p636 Fig. 2.||||||04-JUN-15
24654|Alma Gneiss|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1704+/-3Ma. Geological province: Olary Domain.||||||
24654|Alma Gneiss|62373|6|Mentioned|p503, p504 Fig.3|||S-type.||||||09-JUN-06
24654|Alma Gneiss|62473|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Age: 1704+/-3Ma (for igneous crystallisation).||||||17-JUN-09
24654|Alma Gneiss|62535|5|Briefly described|p666, p672|Statherian|Statherian|Broken Hill Domain.|1704 +/- 3 Ma.|||||
24654|Alma Gneiss|62536|5|Briefly described|p633-634, 636, 639-643|||Broken Hill area. Earlier dating had this unit at 1691 +/- 12 Ma (protoliths: Nutman and Ehlers, 1998). Metamorphosed at 1610 +/- 9 Ma.|1704 +/- 3 Ma.|Thackaringa Group.||Intrudes Thackaringa Group. Hosted by Cues Formation and Alders Tank Formation.|A major felsic gneiss body.|
24654|Alma Gneiss|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1704 +/- 3 Ma.|||Intrudes Thackaringa Group.||
24654|Alma Gneiss|62728|5|Briefly described|p26|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. A gneissic body correlating with Mutooroo Gneiss. S-type and per-aluminous. Age: 1704+/-3Ma (u-Pb, Page et al 2000).||||||07-FEB-11
24654|Alma Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Silver City Suite||||15-DEC-21
24654|Alma Gneiss|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: 1705+/-5Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
24654|Alma Gneiss|63102|5|Briefly described|p10,13,28,40|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. S-type felsic magmatism. |1704+\-3 Ma|||||
24654|Alma Gneiss|63186|5|Briefly described|p70, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1596+/-22 Ma (monazite mean). Geological Province: Curnamona Province.||||||07-NOV-08
24654|Alma Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzofeldspathic orthogneiss, with abundant megacrysts. Geological Province: Broken Hill Domain. Gneiss at Amaroo Hill in the Olary Domain - age: ~1700Ma.||||||07-NOV-08
24654|Alma Gneiss|63519|5|Briefly described|p8, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Age: 1704+/-3Ma. Geological Province: Broken Hill Block-Euriowie Block. Quartzo-feldspathic gneiss.||||||07-NOV-08
24654|Alma Gneiss|63866|4|Described|p36-p38|Statherian|Statherian|Redan Subdomain of the Broken Hill Domain, Curnamona Province. |1704 +/- 3 Ma (Page et al., 2005 Ma)|Silver City Suite||Intrudes the Cues Formation.|S-type granitic gneiss.|
24654|Alma Gneiss|64097|5|Briefly described|p302, p323|Paleoproterozoic|Paleoproterozoic|Superseded by Alma Granite Gneiss. Age: 1704+/-3Ma. Together with Rasp Ridge Gneiss, was formerly part of Thackaringa Group as defined by Stevens et al (1983) and Willis et al (1983).||||||07-FEB-11
24654|Alma Gneiss|64316|5|Briefly described|p531, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca.1704-1685Ma. Geological Province: Broken Hill Block.  See also p532.||||||07-FEB-11
24654|Alma Gneiss|64726|6|Mentioned|p83 Fig.2.|||||||||
24654|Alma Gneiss|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Probably should be Alma Granite Gneiss? Of Silver City Suite. Age: 1704+/-3Ma. Geological province: Broken Hill Domain. S-type.||||||07-FEB-11
24654|Alma Gneiss|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Intrudes Thackaringa Group.||
24654|Alma Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1704+/-3Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
24654|Alma Gneiss|65681|4|Described|pp733-747.|Paleoproterozoic|Paleoproterozoic|Crops out as massive rounded bodies. K-feldspar megacrysts to 45 mm aligned parallel to S1 implies intrusion (ie igneous origin) during D1. Has rapakivi structure.|1691 +/- 12 Ma (Nutman & Ehlers, 1998).|Unit in Willyama Supergroup.||Intrudes Feral gneiss.|Orange coloured; dark foliation anastomosing around abundant, near-euhedral K-feldspar megacrysts that are commonly aligned parallel to lenticular tectonic foliation.|14-MAY-13
24654|Alma Gneiss|66302|5|Briefly described|p36 Fig.9, p40, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. S-type geochemistry.|1704 +/- 3 Ma (Page et al, 2005)|Silver City Suite||Intrudes the Lady Brassey Formation and the Cues Formation.||
24654|Alma Gneiss|66857|5|Briefly described|p971.|Paleoproterozoic|Paleoproterozoic|Deformed granitoids, not sedimentary rocks or felsic volcaniclastics.||Unit in Willyama Supergroup.|||Quartzo-feldspathic gneiss.|
24654|Alma Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Broken Hill Domain, Curnamona Province.|1704 +/- 3 Ma.|||||
24654|Alma Gneiss|68126|6|Mentioned|p6|||Broken Hill Domain, Curnamona Province.||||||
24654|Alma Gneiss|70014|5|Briefly described|Map legend|||Variants include rare megacryst-poor gneisses. The Formation also includes interlayered basic gneisses, leucocratic quartzo-feldspathic phases, and thin beds or bodies of leucocratic sodic plagioclase-quartz rocks. The quartzo-feldspathic gneisses of the Formation are interpreted as conformable rhyodacitic to dacitic metavolcanics.||Unit in Thackaringa Group.||Overlies Thorndale Composite Gneiss. Is overlain by Kyong Formation.|Mainly medium- to coarse-grained quartz-feldspar-biotite +/- garnet gneiss with abundant to sporadic megacrysts of K-feldspar and plagioclase, or of aggregates of quartz + feldspar. Megacrysts are prismatic to augen shaped.|
24654|Alma Gneiss|70657|4|Described|p12, p13 Fig.6, p15, p33, p46|Statherian|Statherian|Curnamona Province: Broken Hill Domain.|1704 +/- 3 Ma (Page et al., 2003).|Silver City Suite||Intrudes Lady Brassey Formation (Thackaringa Group). Underlies Alders Tank Formation. Overlies Thorndale Composite Gneiss.|Intrusive S-type felsic rocks (granite sills), metamorphosed to gneiss.|
24654|Alma Gneiss|70658|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1704 +/- 3 Ma.|Silver City Suite.||||
24654|Alma Gneiss|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Curnamona Province.|1704 +/- 3 Ma.|||||
24654|Alma Gneiss|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain.|||||Includes gneiss.|
24654|Alma Gneiss|72461|6|Mentioned|p6||||1704 +/- 3 Ma|||||
24654|Alma Gneiss|73021|6|Mentioned|p230|||Broken Hill mine area. Underwent peak metamorphic temperatures of 706-726 degrees C.||||||
24654|Alma Gneiss|73524|6|Mentioned|p5 Fig.3|||||Silver City Suite||||
24654|Alma Gneiss|73575|6|Mentioned|p826|||Stratabound. Shown as an intrusive sill, emplaced before initial deformation.||||||
74655|Alum Mountain basalts|24040|5|Briefly described|p477, p486|Early Permian|Early Permian|Informal - see Alum Mountain Volcanics.  Age: ca.280Ma. Also referred to as the informal Alum Mountain volcanics.||||||21-AUG-08
37387|Alum Mountain volcanics|24040|6|Mentioned|p468 Fig. 1|||Informal name - see Alum Mountain Volcanics. Geological Province: Manning Basin||||||
80482|Amaroo Subsuite|63866|5|Briefly described|p41|||Olary Domain, Curnamona Province. [Misspelling of the Ameroo Subsuite].||Basso Suite||||
36123|Amboyne granite|23309|6|Mentioned|p338|||||||||
36123|Amboyne granite|23454|5|Briefly described|p28|Llandovery|Llandovery|427+/-3Ma||||||
68025|Ambrose Dacite Ignimbrite Member|50613|6|Mentioned|p230|||Of Geeves (thesis, unpubl., 1995) - synonymous with Tranquille Dacite Member.||||||24-FEB-05
34010|American Creek Coal|22578|6|Mentioned|Fig.10 p400|||||||||
34010|American Creek Coal|24471|4|Described|p29 Fig.2, p33|Late Permian|Late Permian|Overlies Appin Formation. Overlain by Wongawilli Coal. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Australasian Coal. Geological Province: Sydney Basin.||||||07-FEB-11
70046|American Creek coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
37958|Ameroo Hill Granite|24307|6|Mentioned|p977|||||||||
33511|Amphitheater Formation|44770|14|Not recorded|p115|||||||||
82814|Amphitheatre Formation, lower|72958|6|Mentioned|p37|||Gilligan and Byrnes (1994).||||||
24657|Amphitheatre Group, Upper|22857|6|Mentioned|p171 photo 4|||Informal - see Amphitheatre Group. Of the Cobar Supergroup. Geological Province: Cobar Basin.||||||
24657|Amphitheatre Group, Upper|23096|6|Mentioned|p601 (Fig 1)|||||||||21-JAN-05
24657|Amphitheatre Group, Upper|23734|5|Briefly described|p12 Fig. 1|||Informal name - see Amphitheatre Group.  Mudstone and sandstone.||||||
24657|Amphitheatre Group, Upper|41395|6|Mentioned|Map legend|Pragian|Lochkovian|||||||21-JAN-05
24657|Amphitheatre Group, Upper|41528|3|Fully described|p94|||||||||21-JAN-05
24657|Amphitheatre Group, Upper|41529|6|Mentioned|Map legend|Early Devonian||||||||21-JAN-05
24657|Amphitheatre Group, Upper|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
24657|Amphitheatre Group, Upper|41821|3|Fully described|p40|Pragian|Lochkovian|||||||01-SEP-20
24657|Amphitheatre Group, Upper|42144|5|Briefly described|Fig.3 P604|||||||||
24657|Amphitheatre Group, Upper|42521|5|Briefly described|Fig.3A P16|||Actually shown as Upper Amphitheatre Group.||||||
24657|Amphitheatre Group, Upper|43089|5|Briefly described|Map Legend|||of Amphitheatre Group||||||21-JAN-05
24657|Amphitheatre Group, Upper|43774|1|Redefined|p77-94||Devonian|||||||21-JAN-05
24657|Amphitheatre Group, Upper|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal subdivision of the Amphitheatre Group.  Geological Province: Cobar Basin.||||||
24657|Amphitheatre Group, Upper|61905|5|Briefly described|p135 Fig. 1|||Informal - see Amphitheatre Group. Geological Province: Cobar Basin.||||||
24657|Amphitheatre Group, Upper|65469|6|Mentioned|p52, p55 fig 3-19, p62, p67|||Lachlan Orogen. See also references for the Amphitheatre Group and Amphitheatre Group, Lower. See also  p81, p133, p136, p139, p332, p342, p352, App A-VI 3, App A-VI 5.||||||
24657|Amphitheatre Group, Upper|68823|6|Mentioned|p378 Fig.4|Pragian|Lochkovian|||||||
24657|Amphitheatre Group, Upper|71285|6|Mentioned|p538, p552 Fig.9|Early Devonian|Late Silurian|Cobar region.||||||
24657|Amphitheatre Group, Upper|72958|6|Mentioned|p21|||Edgecome and Soininen (2019).||Amphitheatre Group||||
24657|Amphitheatre Group, Upper|73143|6|Mentioned|p2|||||Amphitheatre Group||||
24657|Amphitheatre Group, Upper|73174|5|Briefly described|p1037, p1040-1042, p1045|Emsian|Lochkovian|Cobar Basin. Represents sag phase of sedimentation. Variable thickness of 6-8 km. See also upper Amphitheatre Group p1037.|427 +/- 29 Ma U-Pb LA-ICP-MS MDA|Amphitheatre Group, Cobar Supergroup||Equivalent to Winduck Group.|Thin- to medium bedded turbidite sequence of sandstone, siltstone and mudstone. Sandstones are typically quartz-rich with well-developed Bouma divisions.|24-NOV-22
79983|Amphitheatre Stage|70037|5|Briefly described|p310|||Andrews (1913). Subsequently the Amphitheatre Group (Rayner, 1962).|||||Shale, sandstone and thin limestone beds containing shallow-marine fossils.|
30883|Anderson's Flat Beds|43400|14|Not recorded|map opp.p.188||Early Permian|||||||
30883|Anderson's Flat Beds|43401|2|Defined|p209||Early Permian|||||||
26345|Anembo Adamellite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Jerangle Igneous Complex. Hornblende-biotite granodiorite with xenoliths. GSNSW map code: gja.||||||
39935|Angullong Tuff Formation|24268|4|Described|p1535|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
28328|Angullong Tuff shales and volcanics|35258|6|Mentioned|Fig.3|||||||||
34261|Angullong Tuff""|22679|6|Mentioned|p 17|||||||||
40716|Angullong formation|23309|6|Mentioned|p390|||||||||
37953|Antro granite|24307|5|Briefly described|p970|Paleoproterozoic|Paleoproterozoic|Informal name||||||07-NOV-08
34505|Apollyon Suite|22771|6|Mentioned|Table12.2p45|||||||||
34505|Apollyon Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Now part of the Paragon Group (Willyama Supergroup). Referred to as Suite 6 by Stevens, Stroud et al (1979, 1980).||||||
77270|Apple Tree Flat Sub-group|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in lower part of Wollombi Coal Measures.|Includes Abbey Green Coal and Charlton Formation.|Overlies Watts Sandstone. Is overlain by Horseshoe Creek Sub-group.||
83959|Apple Tree Granite|71628|6|Mentioned|p10: 1|||Included in the Boxwell Suite by Blevin (unpublished).||||||
40550|Appleogue Dacite|24605|2|Defined|p950 App.1, p939|Namurian|Namurian|Dark-grey to black, hornblende dacite containing plagioclase, hornblende, altered biotite, and opaque minerals.  Referred to throughout text as Appleogue Dacite Member.  Synonymous. Overlies Peri Rhyolite member.   Max. thickness: 35m at type section.||||||14-JUL-04
40550|Appleogue Dacite|61214|5|Briefly described|p172 Fig. 2|Namurian|Namurian|Member of the Clifden Formation. Presented in text as Appleogue Dacite only - not named as a member. Geological Province: Boomi Block.||||||17-JAN-06
40550|Appleogue Dacite|68003|5|Briefly described|p137.|Carboniferous|Carboniferous|Tamworth Belt (North), New England Fold Belt.||Unit in Clifden Formation.|||Grey to black, ignimbritic, hornblende dacite to resedimented, volcanolithic sandstone.|
40550|Appleogue Dacite|68005|5|Briefly described|p144.|Carboniferous|Carboniferous|||Unit in Clifden Formation.|||Grey to black, ignimbritic hornblende dacite to resedimented volcanilithic sandstone.|
34190|Ardlethan Granite""|22638|6|Mentioned|p50|||Superseded by Wantabadgery Granite and Junee Reefs Granite [in some places].||||||19-JAN-17
28332|Ardlethan Sandstone|34109|5|Briefly described|p175|||Upper Devonian. See also Fig 3.21||||||
28332|Ardlethan Sandstone|43509|14|Not recorded|p113||Late Devonian|Unit of Cocoparra Group.||||||04-AUG-08
28332|Ardlethan Sandstone|43511|14|Not recorded|p131-2,134,139,140-4||Late Devonian|Overlies Barrat Conglomerate.||||||04-AUG-08
42326|Ardwest group|24271|6|Mentioned|p1634|||Geological Province: Lachlan Fold Belt.||||||
77271|Arkaroola Formation|68004|6|Mentioned|p27.|Permian|Permian|Mis-spelling of Arkarula Formation (p23 Table 1, p44 Table 3), presumably by confusion with the Flinders Ranges location in South Australia. Deposition of beach, lagoonal, near-shore and deeper shelf sediments in the Gunnedah Basin.||||||
77271|Arkaroola Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Pamboola Formation. Is overlain by Brigalow Formation.||
33383|Arranmor Ignimbrite|23859|5|Briefly described|p931 Fig 3|||See Arranmor Ignimbrite Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
33383|Arranmor Ignimbrite|61793|4|Described|p341, p342 Fig. 1(b), p343 Tb. 1, p347|Late Permian|Late Permian|Of Emmaville Volcanics. Thickness: 150m. Geological Province: New England Fold Belt. Densely welded light grey ignimbrite with well deveolped foliation of platy, dark brown relic pumice lenticles.||||||07-FEB-11
33383|Arranmor Ignimbrite|70210|5|Briefly described|p2, p24, p28-29, p38, p40-41|Permian|Permian|New England district. Described as a "representative" of the Emmaville Volcanics, but nowhere is it presented as a Member of that formation. Also 257.5 +/- 1.7 Ma. Issues in the calculation of preferred age are discussed.|256.4 +/- 1.6 Ma (preferred).|||||
33383|Arranmor Ignimbrite|71628|5|Briefly described|p14: 7|||||Wandsworth Volcanic Group.||Is intruded by Kingsgate Syenogranite.||
24669|Arrowfield coal seam|40805|6|Mentioned|p133|||||||||
32253|Arsenic Ridge Quartz monzodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh26. Misspelling of Arsenic Ridge Quartz Monzodiorite.||||||
41307|Arsenic Ridge Quartz-monzodiorite|60078|6|Mentioned|Map Legend|Devonian|Late Silurian|||||||
31192|Artesian Series|43491|4|Described|pVIII/17|Jurassic|Triassic|||||||
31192|Artesian Series|44861|4|Described|p234,266||Late Jurassic|||||||
80082|Arthursleigh Supersuite|71069|6|Mentioned|p43|Early Devonian|Early Devonian|Mentioned as 'plutons of the Candello [missp. of Candelo] and Arthursleigh supersuites'.||||Intrudes the Bungonia and Bindook Groups.||22-SEP-17
32815|Artie's Sandstone Member|48830|14|Not recorded|p.8|||||||||
26355|Arties seam|37087|4|Described|p200|||||||||
26355|Arties seam|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26355|Arties seam|41604|6|Mentioned|p5|||||||||
26355|Arties seam|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup).||||||
73748|Ashburnia Formation|63293|6|Mentioned|p475, p449 Fig. 2|Llandovery|Llandovery|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73748|Ashburnia Formation|70684|6|Mentioned|p9 Fig.4(g)|Early Silurian|Early Silurian|||||||
79839|Ashfield Formation|60726|5|Briefly described|p2, p3 Fig.2, p8, throughout text.|||See aso reference to Ashfield Shale. Formerly known as the Wianamatta Shales. 40-60m thick. Contains a diverse fauna (listed). Extensively quarried for house bricks.||||||
37002|Ashford Caves Limestone|44450|5|Briefly described|p12 Table 1|Visean|Visean|||||||
28337|Ashford Coalmeasures|31577|6|Mentioned|p86|||Stratigraphy||||||
33602|Ashford Formation|48600|14|Not recorded|p7-8,10-11,18|||Formation of Bowen Group. Late Permian? See also Lexicon.||||||
79450|Ashford beds|70373|6|Mentioned|p789, p791|Early Permian|Permian|||||||
35051|Ashford group|23050|4|Described|p77|||||||||
77366|Attunga Creek Granite|68006|5|Briefly described|p143, p144, p146.|||Associated with W-Mo vein mineralisation. The Kensington Cu-Au skarn deposit is 3 km NW of this unit. Probably the same unit as Attunga Creek Monzogranite (p143, p146).||Unit in Moonbi Supersuite.||||
36468|Attunga Creek Suite|23549|5|Briefly described|p520|||Of Moonbi Supersuite. Geological Province: New England Batholith.  See also the informal Attunga suite.||||||05-APR-05
36468|Attunga Creek Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
36468|Attunga Creek Suite|71628|5|Briefly described|p7: 6|||||Moonbi Supersuite.|Attunga Creek Monzogranite.|||
80784|Attunga Creek volcanics|69639|6|Mentioned|p2, 211, 212|||Informal name of Chisolm et al., 2014.|255.8+/-1.4 Ma|Of Wandsworth Volcanics Group.||||01-MAR-19
81789|Attunga Creek volcanics''|69323|4|Described|p1,3,13,20-27,70|Lopingian|Lopingian|Geological province: New England Orogen. Represent the southwestern-most occurrence of the WVG (Vickery et al., 2010). SHRIMP U-Pb zircon geochronology of GA 2120076 (hornfelsed crystal-rich dacite hosting granite fragments) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 255.8+\-1.5 Ma. This SHRIMP age is consistent with the Moonbi Supersuite granites, and can be inferred that the 'Attunga Creek volcanics' and Attunga Creek Monzogranite are co-magmatic, and subsidence onto a still-cooling pluton resulte in local contact metamorphism of this unit. Sample details, SHRIMP analyses, zircon characteristics and geochronology results are discussed.|255.8+\-1.5 Ma (SHRIMP U-Pb; this study)|Unit of Wandsworth Volcanic Group.||Intruded and metamorphosed by Attunga Creek Monzogranite.|Hornfelsed crystal-rich dacite hosting fragments of mica-rich granite.|03-DEC-19
68006|Attunga suite|23549|6|Mentioned|p516 Fig. 1|||Informal name.||||||
31061|Australasian Beds|43477|14|Not recorded|p55||Late Permian|Occurs in Newcastle Coal Measures||||||
70044|Australasian coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam in the Adamstown Formation (Newcastle Coal Measures).||||||
70044|Australasian coal seam|68711|5|Briefly described|p118, p116 Tbl 6|||Informal unit.||Within Adamstown Formation||||
39828|Australasian seam, lower|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Adamstown Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
39827|Australasian seam, upper|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Adamstown Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
77663|Avenell Basic Igneous Complex|67806|6|Mentioned|pp111-112|||Located at Adelong NSW. I-type. Gold, located in shear systems in this unit, appears to post-date the intrusion by a significant time margin.||||||24-MAY-17
41297|Avon Coal Measures""|44244|6|Mentioned|p167|||Informal - see Avon Coal Measures (superseded by Gloucester Coal Measures).   Max. thickness: 580m.||||||13-JUL-04
40753|Avon Seam|42182|5|Briefly described|p301-302|Permian|Permian|Parent: Gloucester Coal Measures.  Geological Province: Gloucester Basin||||||
41298|Avon Subgroup, lower|44244|6|Mentioned|p174|||Not intended as a formal name - see Avon Subgroup.||||||
38310|Avon seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
38310|Avon seam|44244|5|Briefly described|p325 Tb. 10, p327|Late Permian|Late Permian|Of the Waukivory Formation (Gloucester Coal Measures).||||||
69371|Ayr Conglomerate member|50099|5|Briefly described|p10|||Informal - see Ayr Conglomerate Member.||||||26-JUN-05
24677|Ayrdale Sandstone|40331|4|Described|p9|||||||||
30927|Babbinboon Conglomerate Member|43417|14|Not recorded|Map Legend|||Nth equivalent of Ayr Conglomerate||||||
35427|Back Creek Formation""|23170|6|Mentioned|p53|||||||||
39278|Back Creek Group, Lower|24241|5|Briefly described|p19 Fig.4|Late Permian|Early Permian|Informal name - see Back Creek Group.||||||
39277|Back Creek Group, Upper|24241|5|Briefly described|p19 Fig.4|Late Permian|Late Permian|Informal name - see Back Creek Group.||||||
39277|Back Creek Group, Upper|24616|6|Mentioned|p35|||Informal name.  Geological Province: Bowen Basin.||||||
73039|Back Creek Group, upper|61377|6|Mentioned|p150, p157|||Informal - see Back Creek Group.||||||07-FEB-11
31322|Back Creek Limestone|43538|14|Not recorded|p2,14,20,26-7,36||Visean|Visean, near middle of Caroda Formation.||||||
28339|Back Creek Member""|40328|6|Mentioned|p164|||of Roy (1961). Equivalent to the Kildrummie Formation.||||||
38983|Back Creek Rhyodacite|23861|5|Briefly described|p4 Fig. 2|Namurian|Namurian|Geological Province: New England Orogen.||||||
40551|Back Creek Rhyodacite Tuff""|24605|6|Mentioned|p941, p950 App.1|||Informal name.||||||
70449|Back Creek Tuff Member|62095|6|Mentioned|p275 Appdx.|||Of Kelk (1986). Superseded by Kankool Ignimbrite Member.||||||
70449|Back Creek Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
70449|Back Creek Tuff Member|68005|6|Mentioned|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
76030|Baconian Swamp Granite Suite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. |||Includes Darcoola, Glenhope, Maude, Toopuntul, Ngangay, Oolambeyan and Baconian Swamp granites.||Interpreted S-type granites.|
33997|Badgery's Breccia|22591|6|Mentioned|p 64|||||||||
72791|Badgerys Sub-Group|62740|5|Briefly described|p371|Eocene|Eocene|Of the Koringaroo Group (spelling?). Sedimentary units, many of which have been silicified and occur as two distinct levels of silcretes in the region; fine;grained and massive, existing as a discontinuous sheet. Age is preneted as 'pre-Middle Eocene'.||||||15-JAN-08
30470|Badja Suite|22815|5|Briefly described|p80|||One member, Badja Granodiorite.||||||
30470|Badja Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
30470|Badja Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||19-AUG-08
30470|Badja Suite|44093|5|Briefly described|p222 App. 2|Early Devonian|Early Devonian|||||||
30470|Badja Suite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
73103|Bakers Creek Diorite Complex|62757|5|Briefly described|p14|||Granitoid of Hillgrove Supersuite. Age: ~300Ma.||||||07-FEB-11
73103|Bakers Creek Diorite Complex|71628|6|Mentioned|p2: 8|||Ashley and Craw (2004), after the Bakers Creek Diorite of Binns et al. (1967). Now the Bakers Creek Complex.||||||
37376|Bakers Creek suite|24040|6|Mentioned|p470 Fig.2|||Informal - see Bakers Creek Suite.||||||
37447|Bald Hill Creek Conglomerate|23214|6|Mentioned|p241|||Now included in Slowmans Creek Conglomerate.||||||
77155|Bald Hill Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Buff brown coloured, andesitic, highly welded vitric tuff, containing celadonite.|
77155|Bald Hill Tuff Member|68005|5|Briefly described|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.|||Buff brown coloured, andesitic, highly welded vitric tuff containing celadonite.|
40231|Bald Knobs basalt|38799|6|Mentioned|p143|||Geological Province: New England Fold Belt||||||
31037|Bald Mountain Creek Portal Beds|44970|14|Not recorded|p87|||||||||
28341|Baldwin Formation""|43451|14|Not recorded|Map Legend|||||||||
28341|Baldwin Formation""|48924|6|Mentioned|p18||Late Devonian|U.Dev.||||||
30899|Baldwin Series|43399|14|Not recorded|p190,194|||See also Lexicon||||||
30900|Baldwin Stage|43399|14|Not recorded|p190||Late Devonian|Ref.to Brown(in David 1950,p251(Geology of Comm. of Aust)||||||
30913|Baldwin laminites|43409|14|Not recorded|Map Legend|||More indurated than Mandowa Mudstone||||||
29998|Balgowni Coal|43028|6|Mentioned|Fig.7,p618|||of Illawarra Coal Measures. Misspelling of Balgownie Coal.||||||
70045|Balgownie coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
32977|Balickera bentonites|44265|14|Not recorded|p121|||||||||
27282|Ballallaba Adamellite|22857|6|Mentioned|p215|||Geological Province: Lambie Basin.||||||
27282|Ballallaba Adamellite|22859|6|Mentioned|p215|||||||||
27282|Ballallaba Adamellite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27282|Ballallaba Adamellite|40276|2|Defined|p10|Early Devonian|Early Devonian|||||||
27282|Ballallaba Adamellite|42497|5|Briefly described|Map legend|Zlichovian|Pragian|||||||
27282|Ballallaba Adamellite|60308|6|Mentioned|p39|||Intruded by mafic dyke swarms in the Middle Devonian (385-395 Ma)||||||
77695|Ballallaba Dyke Swarm|60308|6|Mentioned|p38|Givetian|Givetian|Informal name. [Invalid name for dolerite dykes intruding the Ballallaba Adamellite and other units.]"Important stratigraphic unit with contentious age". Preferred age quoted.|388 Ma|||||28-MAY-13
72770|Ballallabra Adamellite|61818|5|Briefly described|p85|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||25-JAN-07
28343|Ballast Chert|730|6|Mentioned|p15, p16.|||Synonymous with Ballast Beds. Well-bedded radiolarian cherts, now included in Girilambone Group.||||||11-NOV-14
28343|Ballast Chert|29621|4|Described|Table 1|||||||||
28343|Ballast Chert|29948|6|Mentioned|p27|||||||||
28343|Ballast Chert|29984|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28343|Ballast Chert|29987|6|Mentioned|p11|||||||||
28343|Ballast Chert|34057|6|Mentioned|Map legend|Silurian|Silurian|||||||
28343|Ballast Chert|34400|6|Mentioned|p6|||Ordovician||||||
28343|Ballast Chert|34404|6|Mentioned|p99|||||||||
28343|Ballast Chert|34449|6|Mentioned|p128|||||||||
28343|Ballast Chert|34469|6|Mentioned|p109|||Table. Ordovician? See also P114||||||
28343|Ballast Chert|35163|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
28343|Ballast Chert|35287|6|Mentioned|Table 1|||||||||
28343|Ballast Chert|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
28343|Ballast Chert|38065|6|Mentioned|p44|||||||||
28343|Ballast Chert|39618|6|Mentioned|Table 1|||||||||
28343|Ballast Chert|41528|6|Mentioned|Fig.3|||||||||
28343|Ballast Chert|42172|4|Described|Fig.1 P162|||See also Fig 5||||||
28343|Ballast Chert|42467|5|Briefly described|Map Legend|||||||||
28343|Ballast Chert|43383|14|Not recorded|p10||Ordovician|||||||
28343|Ballast Chert|43387|4|Described|Map Legend|||Ordovician? Silurian?||||||
28343|Ballast Chert|43389|14|Not recorded|Map Legend||Silurian|||||||
28343|Ballast Chert|43398|14|Not recorded|Map Legend||Silurian|||||||
28343|Ballast Chert|46032|14|Not recorded|p.413|||(H-14/Cobar).||||||
28343|Ballast Chert|67322|6|Mentioned|p19|Darriwilian|Darriwilian|Replaced by the Ballast Formation.||||||
28343|Ballast Chert|72080|4|Described|p2, p4-p5, p7|Silurian|Ordovician|Rocks in the Harts tank area were originally assigned by Brunker (1969) to this unit. Equivalent to the Ballast Formation.|||||Terrigenous turbidites with minor mafic volcanics and common thick chert horizons.|07-JAN-22
28343|Ballast Chert|72296|5|Briefly described|p6|||See p6 for the complicated evolution of this unit's name and relationships with the Girilambone Group.||||||
29997|Ballast Cherts""|43032|6|Mentioned|p19|||Refers to Russell & Lewis (1965).||||||20-OCT-08
29997|Ballast Cherts""|70941|6|Mentioned|p89|||Of Brunker 1971?||||||
33965|Ballast beds""|22555|5|Briefly described|p371|||||||||
36367|Ballengarra Member|22736|6|Mentioned|p619|||part of Cooperabung Formation||||||
24686|Ballerang Conglomerate|37987|6|Mentioned|Fig.4|||Misspelling of Balarang?||||||
70126|Ballimore Formation""|43494|5|Briefly described|p12-13|Triassic|Triassic|Drill holes showed this to be divided into a lower Napperby (more sandy) and upper Purlawaugh Formations (coal-bearing), with intervening Garrawilla Volcanics (MIRRIE DDH1)||||||
39391|Ballimore Sandstone|24126|5|Briefly described|p5|Jurassic|Triassic|||||||
32435|Ballimore Series|44171|14|Not recorded|p197|||See also lexicon. Equivalent to Walloon Coal Measures.||||||
42333|Ballingoole Limestone, upper|13139|5|Briefly described|p7|Ordovician|Ordovician|Informal - see Ballingoole Limestone (Bowan Park Limestone Subgroup).  ||||||
31560|Ballyhooley Suite|42726|5|Briefly described|map legend||Silurian|||||||
31560|Ballyhooley Suite|44093|5|Briefly described|p202 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||28-FEB-05
72764|Ballyhooley granite|61910|5|Briefly described|p152|||Informal - see Ballyhooley Granite. Intrudes Hawkins Volcanics. Geological Province: Lachlan Fold Belt.||||||
35912|Balmoral Coal|23350|5|Briefly described|265, 266|Permian|Permian|Abbreviation of Balmoral Coal Member?  Used interchangeably in text.  of the Skeletar Formation.||||||15-JUL-04
40242|Banalasta Suite""|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
27105|Banar Formation|22857|4|Described|p446 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Part of Ootha Formation. Finely laminated tuffaceous quartz greywackes; contains brachiopods, nautiloids. Max. thickness: ~4km. ||||||
27105|Banar Formation|24417|5|Briefly described|p13|Silurian|Silurian|Of Kemezys (1976).  Superseded by Girilambone Group.||||||
27105|Banar Formation|35503|2|Defined|p206|Silurian|Silurian|New name refs Kemezys (1976)Prob. Silurian||||||
27105|Banar Formation|40328|5|Briefly described|p37|||||||||
31558|Bangadilly Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31558|Bangadilly Suite|44093|5|Briefly described|p219 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||28-FEB-05
31558|Bangadilly Suite|70661|6|Mentioned|p77|||||||||
33601|Bangheet mudstone|48600|14|Not recorded|p4|||||||||
31204|Bango Formation|43479|14|Not recorded|p103||Llandoverian|||||||
24691|Bango Series""|35070|6|Mentioned|p77|||||||||
24691|Bango Series""|35386|6|Mentioned|p14|||Refers Brown(1941) now included in Hawkins Volcanics||||||
30755|Bango beds|43344|5|Briefly described|p122||Silurian|||||||
30755|Bango beds|44861|14|Not recorded|p219,220||Silurian|||||||
31460|Bangrove Limestone Member|43576|6|Mentioned|p350|||Misspelling of Bandon Grove Limestone Member.||||||
82345|Bannaweera Suite|71628|5|Briefly described|p19:10||||||Bannaweera Gabbro.|||
24174|Bannister Basalt|39848|2|Defined|p115|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
24174|Bannister Basalt|40293|6|Mentioned|p459|||||||||
24174|Bannister Basalt|40742|5|Briefly described|p300|||||||||
24174|Bannister Basalt|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|In the Bathurst-Goulburn region. ||||||
24174|Bannister Basalt|68592|6|Mentioned|p1814|Cenozoic|Cenozoic|Bishop (1984). Obsolete: this unit is included in the Wheeo Basalt.||||||
41296|Bansby Beds|60007|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|Included in unnamed Ordovician sequence in map legend.||||||
80474|Barallier Formation|70210|5|Briefly described|p2, p31-32, p35-36, p38, p40-41|Lochkovian|Lochkovian|Yass-Goulburn district. A similar, weighted mean age of 414.5 +/- 3.2 Ma is also given.|414.4 +/- 2.9 Ma.||||Ignimbrite.|
80264|Barallier Ignimbrite|71040|5|Briefly described|p8 Fig.5|||Canberra Zone.|414 +/- 3 Ma; U-Pb zircon.|||||
31924|Bardool Conglomerate basalt|43881|14|Not recorded|p49-50,59,62||Triassic|Basalt unit with in the Bardool Conglomerate||||||
72972|Bargo Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin. See also Bargo Sandstone stated to be Triassic in age?||||||
39267|Barmedman granite|24233|6|Mentioned|p257 Fig.5, p259|||Informal name.||||||
31203|Barnaby Hills Shale Member|43479|14|Not recorded|p116||Ludlovian|||||||
83042|Barnard Beds|73202|6|Mentioned|p628-629, p633|Early Permian|Early Permian|Of Allan & Leitch, 1990. New England Orogen, southern. Early Permian diamictites and mass-flow deposits regionally grouped together as the Manning Group (Mayer, 1972) or Barnard Beds (Allan and Leitch, 1990). All early Permian sedimentary rocks in the southern New England Orogen originally referred to as the Barnard Beds (Allan, 1987; Allan and Leitch, 1990; Heugh, 1971; Leitch, 1988).|||||Includes diamictites and mass-flow deposits.|
40552|Barney Springs Andesite|24605|6|Mentioned|p948 App.1|||Superseded by Barneys Springs Andesite Member.||||||
40552|Barney Springs Andesite|61214|5|Briefly described|p172 Fig. 2|Visean|Visean|Of the Caroda Formation. See also Barney Springs Andesite Member (misspelt), Barneys Springs Andesite Member and Barneys Springs Andesite - names used interchangeably. Presented only as Barney Springs Andesite in Fig. 2. Geological Province: Boomi Block.||||||
40552|Barney Springs Andesite|65382|5|Briefly described|p714|Visean|Visean|[Member] of Caroda Formation. Age of 338.6 +/- 3.5 Ma given from Fielding et al., 2008.||||||
40553|Barney Springs Andesite Member|24605|5|Briefly described|p931, p937 Tb.1|Visean|Visean|Probably misspelt - see Barneys Springs Andesite Member. Of the Caroda Formation. Geological Province: New England Orogen.||||||
40553|Barney Springs Andesite Member|61214|5|Briefly described|p175 Tables 3 and 4.|Visean|Visean|||||||
38979|Barneys Springs Andesite|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Of Caroda Formation.  Geological Province: New England Orogen.||||||
38979|Barneys Springs Andesite|61214|5|Briefly described|p173, p174|Visean|Visean|Of the Caroda Formation. See also Barneys Springs Andesite Member, Barney Springs Andesite Member (misspelt) and Barney Springs Andesite (misspelt) - names used interchangeably.||||||
38979|Barneys Springs Andesite|61767|6|Mentioned|p78|Visean|Visean|Geological Province: Tamworth Belt.||||||
37927|Barneys Springs Andesite Member|24605|5|Briefly described|p936 Fig. 5, p948 App.1|Visean|Visean|Of the Caroda Formation. Thickness at type section: 300m. Age: ~342 Ma. Geological Province: New England Orogen.||||||
37927|Barneys Springs Andesite Member|50613|5|Briefly described|p208 Fig. 3, p210 Fig. 4|Visean|Visean|Of the Caroda Formation.||||||
37927|Barneys Springs Andesite Member|61214|5|Briefly described|p173 Tab. 1, p172 Fig. 3, p174|Visean|Visean|Of the Caroda Formation - present only in the upper part, near the southern closure of the Rocky Creek Syncline. See Barneys Springs Andesite, Barney Springs Andesite (misspelt) and Barney Springs Andesite Member (misspelt) - names used interchangeably.||||||
37927|Barneys Springs Andesite Member|65902|5|Briefly described|p203-4|Visean|Visean|Of Caroda Formation. Dated at 342 Ma by Roberts et al. (2003). Volcanics.||||||09-MAR-12
37927|Barneys Springs Andesite Member|68003|5|Briefly described|p138.|Carboniferous|Carboniferous|Tamworth Belt (North), New England Fold Belt.||Unit in Caroda Formation.|||Porphyritic andesite.|
37927|Barneys Springs Andesite Member|68005|5|Briefly described|p146.|Carboniferous|Carboniferous|||Unit in Caroda Formation.|||Porphyritic andesite.|
35094|Barnsley Member|23055|6|Mentioned|p15|||||||||
70452|Barongarook Member|62095|5|Briefly described|p259 Fig. 10|Permian|Permian|Abbreviated form of Barongarook Ignimbrite Member of the Woodton Formation.||||||
81715|Baronia Granite|71965|6|Mentioned|p910|||Geological province: Thomson Orogen. Concealed S-type granite occurring immediate north of the Mount Oxley Fault.||||||
78508|Baroona granite|68823|6|Mentioned|p376 Fig.3|||||||||08-NOV-13
35624|Baroorangee Creek Subgroup|63789|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Ponto Group. Mica schist and greenschist, minor dolerite and very minor calcite-quartz schist, hematite-quartz gneiss, magnetite-chlorite schist. Possible higher grade equlivalent of Pronto Group.||||||
35624|Baroorangee Creek Subgroup|63793|5|Briefly described|p34, 35, 36.|||Commonly multiply deformed.Colloquially referred to simply as the "high grade Ponto Beds".||Unit in Ponto Group.|||Two main groupings: low amphibolite facies mica schists and metasandstones derived from a sedimentary precursor, and basic rocks containing blue-green amphiboles, derived from a mafic volcanic precursor.|19-JAN-15
35624|Baroorangee Creek Subgroup|64169|5|Briefly described|p19, p20 Fig. 9|||Of the Ponto Group. Overlain by Palgamurtie Subgroup. Includes polydeformed slates and mica schists, with rare interbedded metabasalts - rocks which are atypical of the remainder of the Ponto Group. reach amphibolite grade east of Mount Wright Fault.||||||15-MAY-08
35624|Baroorangee Creek Subgroup|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of Ponto Group. Mica schist and greenschist (very deformed tholeiitic metabasalt), minor dolerite and very minor calcite-quartz schist, hematite-quartz gneiss, magnetite-chlorite schist; unfossiliferous, undated.||||||26-NOV-08
35624|Baroorangee Creek Subgroup|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Mica schist and greenschist, minor dolerite and very minor calcite-quartz schist, hematite-quartz gneiss, magnetite-chlorite schist. Possibly part of Ponto beds, but unfossiliferous and undated.||||||
35624|Baroorangee Creek Subgroup|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Mica schist and greenschist, minor dolerite and very minor calcite-quartz schist, heamatite-quartz gneiss, magnetite-chlorite schist.||||||
35624|Baroorangee Creek Subgroup|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Mica schist and greenschist (very deformed tholeiitic metabasalt), minor dolerite and very minor calcite-quartz schist, hematite-quartz gneiss, magnetite-chlorite schist. Possibly part of Ponto Group?||||||
35624|Baroorangee Creek Subgroup|64686|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Mica schist and other minor metasediments.||||||
35624|Baroorangee Creek Subgroup|66623|6|Mentioned|p81.|||Name replaced by Baroorangee Creek Formation.||Unit in Ponto Group.||||
35624|Baroorangee Creek Subgroup|66929|5|Briefly described|Map legend|||Magnetic pattern unlike remainder of Ponto Group. Corresponds with a gravity high.||Unit in Ponto Group.|||Very deformed tholeiitic basalt: mica schist and greenschist; minor dolerite; very minor calcite-quartz schist, hematite-quartz gneiss, magnetite-chlorite schist; unfossiliferous.|
35624|Baroorangee Creek Subgroup|67322|6|Mentioned|p39|||Obsolete. Briefly described by Buckley (2001) and in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map (Stevens et al. 2002) - now Baroorangee Creek Formation. ||Ponto Group.||||21-FEB-18
76137|Baroorangee Creek Ultramafic|63793|6|Mentioned|p51, p63.|||Not a formal name. Locally sheared and replaced by opaline silica. No precious opal is apparent; recent assays uncovered no anomalous Pt or Pd.||||||
69952|Baroorangee Creek ultramafic|22671|5|Briefly described|p839|||An upper greenschist facies, metamorphosed serpentinised ultramafic of probable Iherzolitic composition; contains blocks of foliated to massive greenschist and amphibolite.  This is a fault slice of the Mount Wright Fault.||||||18-JAN-06
40785|Baroorangee Subgroup|50129|5|Briefly described|p17 Fig.2|Cambrian|Cambrian|Overlain by the Snake Cave Sandstone in the Wonominta Block. Geological Province: Darling Basin.||||||
27326|Barra Beds|30910|6|Mentioned|Map legend|Permian|Permian|||||||
27326|Barra Beds|31882|6|Mentioned|Table 1|||||||||
27326|Barra Beds|32944|6|Mentioned|p702|||See also P710. U.Perm.||||||
27326|Barra Beds|33676|6|Mentioned|Map legend|Permian|Permian|||||||
27326|Barra Beds|34043|6|Mentioned|p452|||Perm. Correlated with Maitland Gp.||||||
27326|Barra Beds|37082|6|Mentioned|p161|||||||||
27326|Barra Beds|37094|5|Briefly described|p238|||||||||
27326|Barra Beds|39288|6|Mentioned|p64|||||||||
27326|Barra Beds|43405|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27326|Barra Beds|43410|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27326|Barra Beds|43429|14|Not recorded|Map Legend|||Description given see Strat form.||||||
24695|Barra Group|29870|6|Mentioned|Table 1|||||||||
24695|Barra Group|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24695|Barra Group|32671|6|Mentioned|Map legend|Permian|Permian|||||||
24695|Barra Group|34043|6|Mentioned|Fig.5.9|||||||||
24695|Barra Group|34292|6|Mentioned|Table 1|||Permian||||||
24695|Barra Group|39288|6|Mentioned|Fig. 3.3|||||||||
24695|Barra Group|43429|14|Not recorded|Map Legend|||Renamed as Barra Beds(q.v.) See also Lexicon||||||
28348|Barraba Mudstone|34287|6|Mentioned|p98|||||||||
28348|Barraba Mudstone|34555|6|Mentioned|Table 4.2|||||||||
28348|Barraba Mudstone|37987|6|Mentioned|p214|||||||||
28348|Barraba Mudstone|43384|14|Not recorded|Map Legend||Late Devonian|||||||
28348|Barraba Mudstone|43385|14|Not recorded|p174,175||Late Devonian|||||||
28348|Barraba Mudstone|43397|14|Not recorded|p210,212,213,map||Late Devonian|||||||
28348|Barraba Mudstone|43399|4|Described|p189,190,192,195,197||Late Devonian|||||||
28348|Barraba Mudstone|43400|14|Not recorded|p175||Late Devonian|||||||
28348|Barraba Mudstone|43479|14|Not recorded|p216||Devonian|||||||
28348|Barraba Mudstone|44565|14|Not recorded|p234|||See also Lexicon.||||||
28348|Barraba Mudstone|44743|14|Not recorded|p40|||Former name for Parry Mudstone.||||||
28348|Barraba Mudstone|44861|14|Not recorded|p244|||||||||
28348|Barraba Mudstone|48600|14|Not recorded|Plate 3|||||||||
30986|Barraba Mudstone""|43447|14|Not recorded|p4,5|||||||||
30986|Barraba Mudstone""|43451|14|Not recorded|Map Legend|||||||||
31029|Barrack Creek Adamellite""|43472|14|Not recorded|p422|||Pre-dates "Queanbeyan Granite"||||||
29569|Barrajin Group|22679|6|Mentioned|p 13|||||||||
29569|Barrajin Group|22857|4|Described|p129, p424 App.1, Tb.A1.5|Eastonian|Eastonian|Contains corals, brachiopods, gastropods.||||||07-SEP-09
29569|Barrajin Group|23213|6|Mentioned|p19|||Includes the Reedy Creek Limestone after revision of Bathurst 1:250 000 geological map.||||||
29569|Barrajin Group|23214|3|Fully described|p33|Late Ordovician|Late Ordovician|||||||
29569|Barrajin Group|23245|6|Mentioned|p129|||||||||
29569|Barrajin Group|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes; Cliefden Caves Limestone Subgroup, Canomodine Limestone, Regans Creek Limestone.||||||17-JUL-08
29569|Barrajin Group|43782|5|Briefly described|Map Legend|Eastonian|Gisbornian|||||||
29569|Barrajin Group|44093|5|Briefly described|p201 App. 1|Early Silurian|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
29569|Barrajin Group|63277|6|Mentioned|p139|Eastonian|Eastonian|Consists of limestones.||||||
29569|Barrajin Group|63287|4|Described|p316, p317 Fig. 2, p333-334, p343|Eastonian|Eastonian|Includes; Canomodine Lst, Cargo Lst, Regans Creek Lst, Bowan Park Lst, Cliefden Caves Lst, Reedy Creek Lst. Consists of thick limestone units. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29569|Barrajin Group|63290|5|Briefly described|p400 Fig. 5(b)|Ordovician|Ordovician|Geological Province: Molong Volcanic Belt. Consists of limestone.||||||
29569|Barrajin Group|64826|5|Briefly described|p1040 Tb. 1|Eastonian|Eastonian|Contains the Cliefden Caves Limestone and Bowan Park Limestone Subgroup.||||||04-MAR-09
29569|Barrajin Group|67322|6|Mentioned|p22, p39|Late Ordovician|Middle Ordovician|Obsolete. Of Morgan, in Pogson and Watkins (1998): now subsumed within the Cabonne Group as a result of reassessment of stratigraphic relationships on the Dubbo 1:250 000 sheet (Meakin and Morgan 1999) and Goulburn 1:250 000 sheet (Thomas et al. in press).||||||
29569|Barrajin Group|68592|5|Briefly described|p370, p378|Late Ordovician|Late Ordovician|Interpreted as disconformably overlying the Kenilworth Group and interfingering with, and being overlain by, Cabonne Group. Pogson et al. (2012) here recommend discontinuation of both Kenilworth and Barrajin Groups in favour of Cabonne Group.||||Disconformably or unconformably overlaid Kenilworth Group and overlain by Cabonne Group.|Included carbonates.|
35416|Barrajin Group""|23170|6|Mentioned|p31|||||||||
28350|Barrandella"" Shale|33116|5|Briefly described|Fig.11|||Correlation||||||
28350|Barrandella"" Shale|35386|6|Mentioned|p30|||Refers to Etheridge(1904). Actually spelt (italics)"Barrandella"(end italics) Shale".||||||
28350|Barrandella"" Shale|37727|6|Mentioned|p85|||||||||
28350|Barrandella"" Shale|44970|14|Not recorded|p43,89|||Correlated with Red Hill Group||||||
27327|Barrett Seam|29942|4|Described|Fig.2|||||||||
27327|Barrett Seam|31124|6|Mentioned|Fig. 2|||Stratigraphic column||||||
27327|Barrett Seam|31125|6|Mentioned|Fig. 1|||Geological map.||||||
27327|Barrett Seam|34466|5|Briefly described|p353|||Vane Formation||||||
27327|Barrett Seam|35823|6|Mentioned|p31|||||||||
27327|Barrett Seam|36604|6|Mentioned|p28|||||||||
27327|Barrett Seam|39346|6|Mentioned|Map legend|Permian|Permian|||||||
27327|Barrett Seam|42182|6|Mentioned|p299|||||||||
27327|Barrett Seam|42648|5|Briefly described|p36|||||||||
41299|Barrett seam, Lower|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Refers to the lower section of the informally named Barrett seam.||||||
41300|Barrett seam, Upper|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Refers to the upper section of the informally named Barrett seam.||||||
32814|Barrett's Sandstone Member|48830|14|Not recorded|p.8,12,15||Late Permian|Upper Permian.||||||
79196|Barrier Member|68592|6|Mentioned|p673|||Wohlt (1996), for two lensoid rhyolitic units within the basalt-dominated Barrier Volcanics of Green (1980). Now an unnamed part of Box Ridge Volcanics.||||||
34278|Barrier Volcanics|22679|6|Mentioned|p 31|||Informal subdivision  of  Green (1980) now included in Box Ridge Volcanics.||||||
34278|Barrier Volcanics|68592|5|Briefly described|p673|||Green (1980). Now the upper part of Box Ridge Volcanics. Two lensoid rhyolitic units within this package were called the Barrier Member by Wohlt (1996).||||Overlay Crawford Formation.|Basalts.|
37416|Barrier Volcanics""|23214|6|Mentioned|p147|||Informal sub-unit of Box Ridge Volcanics.||||||
73703|Barrijin Group|63286|6|Mentioned|p294 Fig. 1|||Consists of wackestone, packstone, limestone, sandstone and mudstone.||||||07-FEB-11
42313|Barrington Granite|24266|5|Briefly described|p1492|Permian|Permian|Age: ~270 Ma. Geological Province: Lachlan Fold Belt.||||||09-MAR-05
82348|Barrington River Supersuite|71628|6|Mentioned|p6: 2|||A mysterious unit mentioned by the author in a bewildering paragraph that attempts to justify having the same constituents in the Barrington Tops Complex and the Barrington Tops Supersuite.||||||
82350|Barrington Tops Complex|71628|4|Described|p1: 6; p6: 1-10, 13, 15-16, 18-25; p9-2|||New name, for a coherent spatio-temporal magmatic collection of rocks located at Barrington Tops, which spanned perhaps more than 10 Ma. Located 40 km W of Gloucester. Distinguished from Clarence River Supersuite by duration of emplacement, spatial separation, and geochemistry. Has the same constituents as Barrington Tops Supersuite [??!] but the author claims that this ""facilitates alteration to the Barrington River Supersuite"" [a unit name which does not appear again in the 1,153 pages of this study, although the Barrington River Complex appears on p6-6, presumably a mis-spelling of Barrington Tops Complex]. History of age determinations discussed. Geochemistry described. Associated with extensive Au mineralisation. Appears as Barrington Top Complex on p6-19.|c.277 Ma to c.267 Ma.|Barrington Tops Supersuite.|Omadale Brook, Gummi Plain, Barrington River, Gloucester Tops Granodiorites.||Quartz diorite dykes and stocks, clinopyroxene-orthopyroxene granodiorite and hornblende-biotite-granodiorite plutons (dominant), with later-stage aplitic, granodioritic and hornblende-phyric dykes. I-type.|
24698|Barrington Tops Granite|29990|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24698|Barrington Tops Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24698|Barrington Tops Granite|31694|6|Mentioned|p341|||||||||
24698|Barrington Tops Granite|33004|6|Mentioned|p112|||See also P200.||||||
24698|Barrington Tops Granite|36391|6|Mentioned|p31|||Also P38||||||
24698|Barrington Tops Granite|71628|6|Mentioned|p6: 3|||Brunker and Offenberg (1970).||||||
27328|Barrington Tops Granodiorite|22610|5|Briefly described|Fig 5||Late Permian|Depositional ages 265+/- 2Ma  and 269+/- 2Ma||||||
27328|Barrington Tops Granodiorite|22612|6|Mentioned|425|Late Permian|Early Permian|||||||
27328|Barrington Tops Granodiorite|22857|6|Mentioned|p257|Late Permian|Late Permian|Age: 265Ma.||||||
27328|Barrington Tops Granodiorite|22864|6|Mentioned|p257,263,266||Late Permian|Max Age: 265 Ma.||||||
27328|Barrington Tops Granodiorite|23462|5|Briefly described|p222|Permian|Permian|||||||
27328|Barrington Tops Granodiorite|24040|5|Briefly described|p471|Early Permian|Early Permian|I-type granite.  Age: ca. 289Ma.||||||21-AUG-08
27328|Barrington Tops Granodiorite|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27328|Barrington Tops Granodiorite|38837|6|Mentioned|p234|||||||||
27328|Barrington Tops Granodiorite|38842|6|Mentioned|p286|||||||||
27328|Barrington Tops Granodiorite|39874|6|Mentioned|p374|||||||||
27328|Barrington Tops Granodiorite|40508|6|Mentioned|p62|||||||||
27328|Barrington Tops Granodiorite|40762|6|Mentioned|p298|||||||||
27328|Barrington Tops Granodiorite|40848|6|Mentioned|p1314|||||||||
27328|Barrington Tops Granodiorite|40883|6|Mentioned|p8|||||||||
27328|Barrington Tops Granodiorite|41347|6|Mentioned|p361|||||||||
27328|Barrington Tops Granodiorite|41348|5|Briefly described|Map legend|Early Paleozoic||Granodiorite, minor adamellite, microgranite.||||||07-NOV-08
27328|Barrington Tops Granodiorite|42780|6|Mentioned|p418, Fig.1 p410|||||||||
27328|Barrington Tops Granodiorite|43017|5|Briefly described|Fig.1,p372|||||||||
27328|Barrington Tops Granodiorite|43755|6|Mentioned|p551|||Age: 265-269 Ma||||||
27328|Barrington Tops Granodiorite|44093|5|Briefly described|p227 App. 1|Early Permian|Early Permian|Age: 269-265Ma. See also p288 Appendix 1. Geological Province: New England Fold Belt.||||||28-FEB-05
27328|Barrington Tops Granodiorite|44244|4|Described|p124, p252|Early Permian|Early Permian|Age: 265+/-2Ma, 269+/-2Ma, 262Ma.  Geological Province: New England Fold Belt.||||||10-MAY-13
27328|Barrington Tops Granodiorite|50099|4|Described|p5-6, p13|Late Permian|Permian|Within the eastern Gresford Block. Geological Province: Tamworth Belt of the New England Orogen.||||||
27328|Barrington Tops Granodiorite|50132|5|Briefly described|p243|Guadalupian|Guadalupian||K-Ar hornblende emplacement age 269-265 Ma.|||||27-MAR-12
27328|Barrington Tops Granodiorite|50147|5|Briefly described|Map legend|Early Permian|Early Permian|Grey hypersthene-augite granodiorite and minor microgranite.  Geological Province: Gresford Block.||||||
27328|Barrington Tops Granodiorite|50268|5|Briefly described|Map Legend|Late Permian|Early Permian|Geological Province: Rouchel and Gresford Blocks.||||||
27328|Barrington Tops Granodiorite|61770|6|Mentioned|p106, p112, p109 Fig. 2||Early Permian|Age of intrusion: 280-269Ma.||||||25-SEP-08
27328|Barrington Tops Granodiorite|62095|5|Briefly described|p250, p269|Early Permian|Early Permian|I-type.||||||
27328|Barrington Tops Granodiorite|68005|5|Briefly described|p63.|||Previous dating using whole rock Rb-Sr (Hensel et al. 1982) gave ages of 273-264 Ma.|281 - 273 Ma (SHRIMP: Kimborough et al. 1993).|Unit in Nundle Suite.||||
27328|Barrington Tops Granodiorite|68111|5|Briefly described|p968 Tb.1, p970 Fig.2, p976|Wordian|Roadian|U-Pb SHRIMP geochronology by Cawood et al. (2011). Mis-spelt as Barrington Top in Fig.2.|267.2 +/- 1.4 Ma|Of the Clarence River Supersuite.||||16-OCT-14
27328|Barrington Tops Granodiorite|68822|5|Briefly described|p338|Wordian|Wordian||ca. 267 Ma|||||
27328|Barrington Tops Granodiorite|69601|5|Briefly described|p403, p408, p410|||New England Orogen. Comprises three main plutons. Geochronology discussed in detail. Cooling rate calculated at 21 degrees C/Ma. No inherited zircons, and very primitive isotopic signature, suggests it formed above oceanic crust.|281 Ma (207Pb/206Pb crystallisation age).|Nundle Suite.|||Mainly hornblende-biotite granodiorites with some tonalitic variants. Two of the main plutons have augite and hypersthene instead of biotite and hornblende. Essentially unstressed I-type granites.|
27328|Barrington Tops Granodiorite|69639|6|Mentioned|p223|Wordian|Wordian||267 +/- 2 Ma |Clarence River Supersuite||||
27328|Barrington Tops Granodiorite|69930|6|Mentioned|p260|Permian|Permian|Tamworth Belt.||||||
27328|Barrington Tops Granodiorite|70125|5|Briefly described|p398 Fig.12|||Southern New England Orogen. Zircon age probability density plot.|267 Ma (U-Pb zircon: Cawood et al., 2011).|||||
27328|Barrington Tops Granodiorite|70217|4|Described|v, p1 tbl 1.1, p11-p26, p72, p73, p87|Wordian|Artinskian|New England Orogen. Primitive I-type geochemistry. SHRIMP ages derived from this volume. Other SHRIMP ages are also given ranging from 272.5 +/- 1.6 Ma to 267.8 +/- 1.4 Ma; these ages fall within the 281-258 Ma age range previously determined for this unit. Other ages include: c. 258 Ma (K-Ar, Cooper et al, 1963), c. 265 (Sm-Nd (Hensel et al, 1985), 265 +/- 2 Ma, 269 +/- 2 ma (K-Ar, Roberts et al, 1991), 265 +/- 8 Ma (U-Pb, Collins et al, 1993), c. 281 Ma (ID-TIMS Pb-Pb, Kimbrough et al, 1993), c. 269 Ma (LA-ICPMS, Phillips et al, 2011) and 267.2 +/- 1.4 Ma (SHRIMP U-Pb, Cawood et al, 2011).  It should be noted however that this unit is interpeted to be the product of three distinct intrusive episodes over a period of 10 million years.   Petrography, zircon morphology and SHRIMP results discussed in detail. |277.1 +/- 1.9 to 267.8 +/- 1.4 Ma (SHRIMP U-Pb)|Nundle Suite||Intrudes the Parry and Manning Groups.|Tonalite consisting of 50 percent plagioclase, 30-35 percent quartz and 15% ferromagnesian minerals with very minor alkali feldspar.|
27328|Barrington Tops Granodiorite|70876|5|Briefly described|p2, p77-p78|Permian|Permian|New England Orogen. Additional ages are provided and are as follows: c. 258 Ma (K-Ar biotite, Cooper et al, 1963), c. 265 Ma (Sm-Nd whole rock, Hensel et al, 1985), 265 +/- 2 Ma (K-Ar biotite, Roberts et al, 1991), 265 +/- 8 Ma (U-Pb, Collins et al, 1993), c. 281 Ma (ID-TIMS Pb-Pb zircon, Kimbrough et al, 1993), c. 269 Ma (LA-ICP-MS U-Pb zircon, Phillips et al, 2011), 267.2 +/- 1.4 Ma (SHRIMP U-Pb zircon, Cawood et al, 2011) and 267.8 +/- 1.4 Ma, 272.5 +/- 1.6 Ma, 277.1 +/- 1.9 Ma (SHRIMP U-Pb, Waltenberg et al, 2015).|>270 Ma (Waltenberg et al., 2015)|Clarence River Supersuite||||
27328|Barrington Tops Granodiorite|71628|5|Briefly described|p6: 1, 3-5, 18; p9:1; p18:8|||Gilligan and Brownlow (1981). These authors also referred to this intrusion as Barrington Granodiorite. Was tentatively included in the Clarence River Plutonic Suite of Shaw and Flood (1981). Bryant et al. (2003), after unpublished work by Chappell and Bryant (1994), replaced Barrington Tops Granodiorite with Gummi Plain, Omadale Brook and Barrington River Granodiorites. Subsequently the Barrington Tops Complex (redefined in this study).|262 Ma (Rb-Sr: Roberts et al., 1991).|||||
27328|Barrington Tops Granodiorite|72313|6|Mentioned|p459 Table 2|||New England Orogen. I-type.  Hf isotope data included.|269 Ma|||||
27328|Barrington Tops Granodiorite|73197|6|Mentioned|p475 Fig.6|Lopingian|Guadalupian|New England Orogen, southern. Referred to as Barrington Tops plutons on p477, p478, 484? [Barrington Tops plutons have U-Pb ages between 277 and 266 Ma]|||||Granitic intrusive.|
69372|Barrington Tops quartz diorites|50099|6|Mentioned|p17|||Informal reference to rocks of the Barrington Tops Granodiorite.||||||
37383|Barrington Tops suite|24040|6|Mentioned|p486|||Informal - see Barrinton Tops Granodiorite.||||||
78370|Barrona granite|68823|6|Mentioned|p394|||Informal name on Wanaaring 1:100k map sheet area. Mis-spelt as Baroona granite in Fig.3.||||||22-JUL-15
78370|Barrona granite|69002|5|Briefly described|p9|Eifelian|Eifelian|Informal name. Peanut shaped on the Wanaaring 1:100k map sheet. Recalculated K-Ar age.|c. 389 Ma, K-Ar (Richards and McDougall 1986)|Of the Utah Lake plutonic complex.|||Shows magnetic contrast in the aureole with both granite and schist intersected in water bores|
78370|Barrona granite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen.?Low-magnetic intensity||||||
78370|Barrona granite|69043|5|Briefly described|p11, p93|||Thomson Orogen. K-Ar age by Richards and McDougall in Jones (1986).|c.389 Ma.|||||
76146|Barrongie Creek Ultramafic|66623|6|Mentioned|p226.|||Named by Buckley (2002); superseded and redefined in this study as Cliffs Tank Complex.||||||
76138|Barroorangee Creek Subgroup|63793|6|Mentioned|p36|||Misspelling of Baroorangee (used p34, 35)||||||19-JAN-15
24699|Barrow Range Sandstone|34449|6|Mentioned|Table 2-1|||||||||
24699|Barrow Range Sandstone|41528|6|Mentioned|Fig.3|||||||||
24699|Barrow Range Sandstone|42566|6|Mentioned|Fig.3 P6|||||||||
27704|Barry Granite|23214|5|Briefly described|p172|||Renamed Barry Granodiorite. Formerly included Sunset Hills Granodiorite.||||||
27704|Barry Granite|24268|6|Mentioned|p1536 Fig.2|||Geological Province: Lachlan Fold Belt||||||
27704|Barry Granite|29903|6|Mentioned|p194|||||||||
27704|Barry Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
27704|Barry Granite|33006|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
27704|Barry Granite|33282|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27704|Barry Granite|33285|6|Mentioned|p18|||Middle Dev.||||||
27704|Barry Granite|34255|6|Mentioned|p202|||Early - Mid Devonian||||||
27704|Barry Granite|34544|5|Briefly described|p193|||||||||
27704|Barry Granite|35257|6|Mentioned|p102|||||||||
27704|Barry Granite|40328|4|Described|p202|||||||||
27704|Barry Granite|42384|6|Mentioned|p10|||||||||
27704|Barry Granite|42726|5|Briefly described|map legend|Silurian||Wyangala Batholith. NOT variation on Barry Mountains Granite, Wagga Batholith, Vic.||||||
27704|Barry Granite|43515|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
27704|Barry Granite|43516|14|Not recorded|Map Legend||Middle Devonian|(U.M.Dev.)||||||
27704|Barry Granite|49794|5|Briefly described|p9|||||||||
27704|Barry Granite|73431|6|Mentioned|p363 Fig.1, p372, p373 Fig.8, p374|Devonian|Silurian|Lachlan Orogen. I-type granite.|||||Granite.|
34300|Barry Granite""|22679|6|Mentioned|p 47|||||||||
42217|Basal Wilton Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Woonona Coal Measure. Informal description of lowermost part of Wilton Formation.||||||30-NOV-04
82720|Basket Swamp Leucomonzogranite Phase|71628|5|Briefly described|p15: 35, 52, 60-63, 65, 115|||New unit, after a local watercourse; distinguished geochemically. This subunit does not ""technically"" qualify as a Phase according to stratigraphic naming conventions. Formerly part of Stanthorpe Monzogranite. Occurs between 3 to 7 km SSE of Boonoo Boonoo locality. Limited geochemistry described; it is geochemically assigned to the Surface Hill Suite. Is associated with Au- and Ag-rich polymetallic mineralisation (described).||Mount Lindesay Monzogranite.||Likely abuts (currently undefined) Jenners Monzogranite, and other ""Phases"" of Mount Lindesay Monzogranite.|Leucogranite. I-type.|
83080|Bathurst granites|73299|6|Mentioned|p1094 Fig.2, p1095, p1107 Fig.12|Serpukhovian|Visean|U-Pb zircon ages include 331 +/- 2 Ma (Jeon and Williams, 2018). Locations in text include p1102 Fig.8-9. See also Bathurst Granite.|ca 330 Ma, 328 +/- 2 Ma, 332 +/- 2 Ma U-Pb zircon||||Granite.|
37380|Bathurst group|24040|6|Mentioned|p482|||Informal.||||||
34765|Bathurst-type granites|22857|5|Briefly described|p218, p223, p238-239|Devonian|Devonian|Of Vallance (1969a).Informal name for post-kinematic magmatism in the Lachlan Fold Belt after the Kanimblan Orogeny. Term used extensively throughout. ||||||
34765|Bathurst-type granites|22933|4|Described|Table11.1p5, p238-9|Early Permian|Early Carboniferous|Of Vallance (1969b).  See also p218 and p231-2.||||||20-JUL-04
23366|Batlow Amphibolite|39331|6|Mentioned|p30|||See also P33||||||
77696|Batlow Gabbro|60308|6|Mentioned|p38|Llandovery|Llandovery|"Important stratigraphic unit with contentious age". Preferred age quoted.|433 Ma|||||28-MAY-13
33957|Batobolar Granite|22529|6|Mentioned|4 fig 2|Middle Carboniferous|Middle Carboniferous|||||||
68155|Bawley Microgranite|60281|6|Mentioned|p61|||See also Bawley Gabbro - one may supersede the other?||||||17-MAR-05
32816|Bayswater Siltstone""|48830|14|Not recorded|p.9,10|||Reference to Reynolds, 1956.||||||
28355|Bayswater complex|40332|6|Mentioned|p24|||||||||
31064|Bayswater shales|43477|14|Not recorded|page not known|||||||||
35758|Beacons Hill Chert|50230|5|Briefly described|Map legend|Gisbornian|Darriwilian|Of the Adaminaby Group (top).  Thin-bedded to laminated radiolarian and conodont-bearing chert, variably cherty siltstone and mudstone, minor graded fine-grained quartzose sandstone.||||||
35758|Beacons Hill Chert|50231|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Adaminaby Group.||||||
35758|Beacons Hill Chert|50233|5|Briefly described|Map Lagend|Gisbornian|Darriwilian|Of the Adaminaby Group.||||||
35758|Beacons Hill Chert|67322|5|Briefly described|p39|Middle Ordovician|Middle Ordovician|Shown on provisional 1st editions of Crookwell, Boorowa and Yass 1:100 000 geological maps; this unit is now regarded as an equivalent of the Nattery Chert Member of the Abercrombie Formation, and is therefore redundant. Age based on that of the Nattery Chert Member.||||Equivalent to the Nattery Chert Member.||21-FEB-18
35758|Beacons Hill Chert|68592|6|Mentioned|p313|||Obsolete. Occurs on the provisional Boorowa and Gunning 1:100 000 sheets. Replaced by Nattery Chert Member (Abercrombie Formation).||||||
38944|Beargamil Sub-Group""|23217|5|Briefly described|p3|||Informal name - see Beargamil Sub-group.  Of Connolly (1965a).  Includes Clagger Sandstone.||||||08-MAR-06
38944|Beargamil Sub-Group""|24417|6|Mentioned|p127|||Of Hervey Group.||||||
42303|Beargamil Subgroup""|22857|5|Briefly described|p213|Devonian|Devonian|One of three former subdivisions (Connolly, 1965a) of the Hervey Group; not applied in recent mapping. Geological Province: Hervey Basin.||||||
39379|Beargamil subgroup|24125|5|Briefly described|p46|||Informal.  Of the Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
42418|Beaumah limburgite|24015|5|Briefly described|p10|Ordovician|Ordovician|Informal. Derived from shoshonitic arc magmas. Of Blayney Volcanics. Geochemistry described here.||||||
29723|Bee Conglomerate Formation""|43032|6|Mentioned|p47|||refers to Rayner (1969).||||||
42321|Beechworth granites|24270|6|Mentioned|p1608|||Geological Province: Lachlan Fold Belt.||||||09-MAR-05
38324|Beenleigh Association""|23812|5|Briefly described|p10|Early Carboniferous|Late Devonian|Former informal name (Korsh, 1977) for sedimentary rocks forming part of the 'Aaiwan terrane' of Flood and Aitchison (1988).||||||
78141|Bega Suite|68255|6|Mentioned|p1063|||||||||
26379|Begonia Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Begonia Adamellite.||||||
80301|Belah Formation""|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|Geophysical signature: low magnetic intensity and only slight contrast with adjacent sedimentary rocks in aeromagnetic data. Low radioelement values.||Winduck Group.|||Thickly bedded argillaceous and quartzose sandstone, and siltstone.|
35632|Belah beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group). Metasediments, including magnetic pelitic phyllite; significant cherty tuffs with or without dolerite.||||||26-NOV-08
35632|Belah beds|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Palgamurtie Subgroup. Metasediments, including magnetic pelitic phyllite; significant cherty tuffs with or without dolerite.||||||
35632|Belah beds|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Palgamurtie Subgroup. Metasediments, including magnetic pelitic phyllite; significant cherty tuffs with or without dolerite.||||||
35632|Belah beds|66623|6|Mentioned|p93.|||Included with Yandenberry beds (Stevens et al. 2000) in this study's definition of the Yandenberry Formation.||||||
35632|Belah beds|66929|5|Briefly described|Map legend|||||Unit in Palgamurtie Subgroup.|||Metasediments, including magnetic pelitic phyllite; significant cherty tuffs with or without dolerite.|
35632|Belah beds|67322|6|Mentioned|p39|Permian|Cambrian|Part of the Palgamurtie Subgroup (obsolete) in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map (Stevens et al. 2002). Occurs in the Kayrunnera-Koonenberry region. ||Of the Ponto Group.||||
70007|Belbora formation|61766|6|Mentioned|p68|||Informal - see Belbora Formation. Geological Province: Tamworth Belt.||||||
30868|Belford Beds|43366|14|Not recorded|Map Legend||Late Devonian|Unit of Mulga Downs Group||||||22-DEC-09
81802|Belimebung Igneous Complex|72495|6|Mentioned|p225, 240|||See also Belimebung Volcanics p218, 225, 236, 241. Named from the Cootamundra 1:250k map sheet area by Warren et al. 1995.||||||26-MAR-20
79444|Belimebung volcanic rocks|70178|6|Mentioned|p4 fig. 2|Ordovician|Ordovician|Macquarie Arc.||||||
31255|Bell Limestone""|43512|14|Not recorded|p100,101,104||Early Silurian|(M.Sil)||||||
31271|Bell's Creek Volcanics|24278|5|Briefly described|p1764|Silurian|Ordovician|Minimum age is Middle Silurian.||||||24-JUL-06
31271|Bell's Creek Volcanics|43517|2|Defined|p112,116-7,p122-159||Wenlockian|C.on Tanwarra Shale. Type section 2miles SW of Sofala. Map Plate XII||||||
24176|Bellbridge Gneiss|37871|4|Described|p7|||||||||
24176|Bellbridge Gneiss|38367|6|Mentioned|Fig.27|||||||||
24176|Bellbridge Gneiss|39858|6|Mentioned|Map legend|Silurian|Silurian|Silurian - Ordovician||||||
24176|Bellbridge Gneiss|68115|5|Briefly described|p7.|||Omeo Zone. Shown under this name on the Hume 1:50 000 geological map (O'Shea, 1979). Later mapping showed it to be granite, hence its renaming as Bellbridge Granite. G174.||||||07-DEC-21
39416|Bellingen Slates|24127|5|Briefly described|p4|Permian|Permian|||||||
39430|Bellinger Slates|24129|5|Briefly described|p4|||Probably misspelt.||||||
26382|Belowra Granite|42726|5|Briefly described|map legend|Early Devonian||116.  Of the Belowra Suite (Candelo Supersuite).  Not intended as a formal name.||||||09-FEB-05
72275|Belubula formation|62349|6|Mentioned|p73|||Informal name. Geological Province: Lachlan Fold Belt.||||||
34105|Belulula Limestone|22503|6|Mentioned|Fig.4 p646|||Misspelling of Belubula Limestone||||||07-MAR-16
24710|Bemboka Granite|42726|5|Briefly described|map legend|Early Devonian||129.  Of the Bemboka Suite.||||||07-FEB-05
24710|Bemboka Granite|45087|5|Briefly described|p35|||chem. analyses.||||||
73961|Ben Boyd Formation""|63605|5|Briefly described|p994, p100|Famennian|Famennian|Undefined fourth unit of Lewis et al (1994) within Merrimbula Group - the upper point bar sequence of Worange Point Formation - rocks now part of this unit. Dominated by thick packets of mudstone and thinner, regularly bedded sandstones; fish fauna.||||||07-FEB-11
26383|Ben Bullen Gabbro|42726|5|Briefly described|map legend|Carboniferous||11. Variation on the informal Ben Bullen complex?||||||
24711|Ben Bullen complex|34544|6|Mentioned|p192|||||||||
74652|Ben Bullen gabbros|24040|6|Mentioned|p469, p481 Fig. 5|||Informal name. High-K calc-alkaline rocks.||||||21-AUG-08
30886|Benama Greywacke Member|43399|2|Defined|p196,197,203,205||Tournaisian|Member of Goonoo Goonoo Mudstone (Parry Gp)||||||
30886|Benama Greywacke Member|43400|14|Not recorded|map opp.p.188|Early Carboniferous|Late Devonian|||||||
30886|Benama Greywacke Member|43406|14|Not recorded|p42||Early Carboniferous|||||||
35681|Bendee beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup. Sandy phyllite containing magnetic pelitic phyllite, and altered basalt, with or without dolerite; minor quartz-magnetite rock.||||||26-NOV-08
35681|Bendee beds|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Overlian by Weinteriga Creek beds. Sandy phyllite containing magnetic pelitic phyllite, and altered basalt, with or without dolerite; minor quartz-magnetite rock.||||||01-DEC-08
35681|Bendee beds|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Sandy phyllite containing magnetic pelitic phyllite, and altered basalt, with or without dolerite; altered minor quartz-magnetite rock.||||||
35681|Bendee beds|66623|6|Mentioned|p85. |||Incorporated  with Grasmere beds (Buckley 2000) into Grasmere Formation (this study).||Unit in Palgamurtie Subgroup.||||
35681|Bendee beds|66929|5|Briefly described|Map legend|||||Unit in Palgamurtie Subgroup.||Is overlain by Weinteriga Creek beds.|Sandy phyllite containing magnetic pelitic phyllite, and altered basalt, with or without dolerite; minor quartz-magnetite rock.|
35681|Bendee beds|67322|6|Mentioned|p39|Cambrian|Cambrian|Part of the Palgamurtie Subgroup (obsolete) in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map - now assigned to the Grasmere Formation (Greenfield et al. 2010). Age is assumed to be similar to the parent Grasmere Formation. Occurs in the Kayrunnera-Koonenberry region.||||||
26384|Bendemeer Adamellite|721|5|Briefly described|Map legend|Early Triassic|Early Triassic|Of the Moonbi Plutonic Suite.  Approximately  equigranular coarse-grained, hornblende-biotite monzogranite and minor monzonite.||||||
26384|Bendemeer Adamellite|24519|5|Briefly described|p89, p90|Permian|Permian|Of the New England Batholith. I-type pluton. Thickness: 2-4km (modelled using gravity data).||||||
26384|Bendemeer Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
26384|Bendemeer Adamellite|30787|6|Mentioned|p49|||Differentiation index||||||
26384|Bendemeer Adamellite|30789|6|Mentioned|Fig.1B|||Petrology & Geochemistry||||||
26384|Bendemeer Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26384|Bendemeer Adamellite|31140|6|Mentioned|p55|||||||||
26384|Bendemeer Adamellite|33781|6|Mentioned|Table 1|||||||||
26384|Bendemeer Adamellite|34093|4|Described|p282|||U.Perm.||||||
26384|Bendemeer Adamellite|35192|6|Mentioned|Fig.1|||||||||
26384|Bendemeer Adamellite|35257|6|Mentioned|Fig.17|||||||||
26384|Bendemeer Adamellite|38842|6|Mentioned|p286|||||||||
26384|Bendemeer Adamellite|38905|6|Mentioned|p305|||||||||
26384|Bendemeer Adamellite|43091|5|Briefly described|Map legend|||of Moonbi Platonic Suite||||||
26384|Bendemeer Adamellite|45087|5|Briefly described|p22|||See also P39. Chemical analyses||||||
26384|Bendemeer Adamellite|71628|6|Mentioned|p7:10|||Chappell (1959). This appears to apply to rocks of the Bundarra Supersuite. The currently-defined Bendemeer intrusion was mapped and described by Chappell (1966), also named Bendemeer Adamellite, but the name was first published by Binns et al. (1967). Subsequently the Bendemeer Monzogranite (first published by Brown, 2003 after Chappell and Bryant, 1994).||||||
40233|Bendemeer Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
40233|Bendemeer Suite|61773|5|Briefly described|p139|||Of the Bendemeer Supersuite.||||||25-JAN-06
40233|Bendemeer Suite|71628|5|Briefly described|p7: 11, 28, 33|||Chappell (1978). Later modified to the Moonbi Suite (Chappell et al., 1987).|||Bendemeer, Moonbi Monzogranites.|||
40243|Bendemeer Suite""|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
69992|Bendemeer suite granitoids|61773|6|Mentioned|p138|||Informal name - probably refers to granites of the Bendemeer Suite.||||||19-DEC-07
38444|Bendoc group|23309|5|Briefly described|p5 Fig. 1.3, 59-61 Tb2.19|Ordovician|Ordovician|||||||
38444|Bendoc group|24133|6|Mentioned|p21|Ordovician|Ordovician|Misspelt - see Bendoc Group.  Geological Province: Lachlan Fold Belt.||||||
38444|Bendoc group|24551|6|Mentioned|p96 Fig.4.1|||Informal - see Bendoc Group||||||
38444|Bendoc group|60541|6|Mentioned|p13|||Informal - see Bendoc Group.||||||
38444|Bendoc group|60542|6|Mentioned|p17|Early Silurian|Early Silurian|Informal - see Bendoc Group. ||||||
38444|Bendoc group|61160|6|Mentioned|p44|||Informal - See Bendoc Group. ||||||
38444|Bendoc group|61161|6|Mentioned|p78|||Informal - see Bendoc Group.||||||
32265|Bendoura Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb6. Misspelling of Bendora Granodiorite.||||||
32265|Bendoura Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
30033|Benelabri Mudstone Member|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Clare Sandstone. New, formal name for the 'organic-rich mudstone unit' in Clare Sandstone Member (now Clare Sandstone). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
80142|Benelebri Formation|70791|5|Briefly described|p277 Fig 2|Lopingian|Lopingian|Gunnedah Basin.||Coogal Subgroup.||||28-SEP-17
35269|Bennetts Green Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
75858|Benny's Top limestone|44447|6|Mentioned|p133 Fig.2|Early Devonian|Early Devonian|Also named Bennys Tops limestones"" (p132) and Benny's Tops limestone (p137). Member of Glen Ward Beds.||||||
75855|Benny's Tops limestone|44447|6|Mentioned|p137|Early Devonian|Early Devonian|Also named Bennys Tops limestone"" (p132) and Benny's Top limestone (p133 Fig.2). Member of Glen Ward Beds.||||||
75857|Bennys Tops limestones""|44447|5|Briefly described|p132|Early Devonian|Early Devonian|Also named Benny's Tops limestone (p137) and Benny's Top limestone (p133 Fig.2). Member of Glen Ward Beds.||||||
27706|Berkley Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
27706|Berkley Latite Member|22488|5|Briefly described|p840-1|||||||||
27706|Berkley Latite Member|38690|4|Described|p295|||Misspelling of Berkeley?||||||
27706|Berkley Latite Member|40270|6|Mentioned|Table 1|||||||||
27706|Berkley Latite Member|67500|5|Briefly described|p12 Tb.1|||[Mis-spelling of Berkeley]. Between 24-35m thick.||Of the Pheasants Nest Formation and Gerringong volcanic facies.|||Two coarsely porphyritic flows.|02-MAY-12
28363|Bermagui beds""|35289|6|Mentioned|p38|||||||||
31065|Berry shale|43477|14|Not recorded|p19|||||||||
31496|Bethanga Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Cooma Supersuite.  Includes the Bethanga and House Creek Granites (informal names).||||||09-FEB-05
26389|Bethungra Granite|23454|5|Briefly described|p27 Fig.1|Silurian|Ordovician|~420Ma||||||
26389|Bethungra Granite|35185|6|Mentioned|p231|||||||||
26389|Bethungra Granite|42726|5|Briefly described|map legend|Silurian||533.||||||
31553|Bethungra Suite|42726|5|Briefly described|map legend||Silurian|||||||
31553|Bethungra Suite|44093|5|Briefly described|p182 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
72895|Beugamel Sandstone, upper|62569|6|Mentioned|p607|||Informal - see Beugamel Sandstone. ||||||
26293|Bevendale Basalt|39848|2|Defined|p113|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
26293|Bevendale Basalt|40240|5|Briefly described|p107|||||||||
26293|Bevendale Basalt|40293|6|Mentioned|p459|||||||||
26293|Bevendale Basalt|40742|5|Briefly described|p298|||||||||
26293|Bevendale Basalt|41110|5|Briefly described|p223|||||||||
26293|Bevendale Basalt|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|In the Bathurst-Goulburn region. ||||||
26293|Bevendale Basalt|68592|6|Mentioned|p1814|Cenozoic|Cenozoic|Bishop (1984). Obsolete: this unit is included in the Wheeo Basalt.||||||
32630|Beverley Group|23911|6|Mentioned|p88 Fig. 2|||Geological Province: Whitsunday Volcanic Province.||||||
32630|Beverley Group|46568|14|Not recorded|p.423||Ordovician|(I55-16/Michelago).||||||
29489|Beverly Beds""|42820|6|Mentioned|p7|||Refers Glasson, 1957. Part of Pittman Formation?||||||
40588|Bexley Rhyodacite Tuff|24605|6|Mentioned|p950 App.1|||Superseded by the Bexley Rhyolite.||||||
37316|Bexley Rhyolite|23861|5|Briefly described|p4 Fig. 2|Namurian|Namurian|Geological Province: New England Orogen.||||||
37316|Bexley Rhyolite|24010|6|Mentioned|p380 Fig. 6|||||||||
37316|Bexley Rhyolite|24605|2|Defined|p950 App.1|Namurian|Visean|Of the Clifden Formation. Maximum Thickness: 2m. Age: 327.2 +/- 2.9 Ma. Geological Province: New England Orogen. Referred throughout text as Bexley Rhyolite Member.||||||
31235|Biddabirra beds|43491|14|Not recorded|pV/14||Middle Devonian|Ref. to Andrews 1911, and Mulholland 1940||||||
31193|Biddabirra sandstones|43491|14|Not recorded|pV/14||Middle Devonian|May also be Lower Devonian or earlier||||||
24718|Biddabirrah Beds|29621|6|Mentioned|Table 1|||||||||
24718|Biddabirrah Beds|39618|6|Mentioned|Table 1|||Refers Andrew 1913.||||||
28366|Big Ben seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a coal seam within the Four Mile Creek Formation (Tomago Coal Measures).||||||
28366|Big Ben seam|36545|6|Mentioned|p12|||||||||
28366|Big Ben seam|37084|4|Described|p178|||||||||
28366|Big Ben seam|39308|6|Mentioned|Fig. 23.4|||||||||
37379|Big Bull Gabbro|24040|6|Mentioned|p477|||||||||
37379|Big Bull Gabbro|71628|5|Briefly described|p2: 46-47, 49-51, 53|||Named but unpublished by Paul (1984), after Big Bull Creek. The largest unit in the parent Complex. Geochemistry described. Has strong compositional similarities with Barney House Gabbro.||Sheep Station Creek Complex.||Intrudes Moombil Sandstone and Brooklana beds. Is intruded by (and includes masses of) Marengo Plain Monzogranite, Collett Monzogranite, and (veins of) Gumtree Monzogranite.|Massive, black, medium-grained olivine gabbro, quartz gabbro, and pegmatite gabbro.|
82725|Big Bull Granite Complex|71628|6|Mentioned|p17: 47|||Endurance Mining Corporation N.L. (1972). Now part of Billys Creek Granodiorite.||||||
82357|Big Hill Creek Suite|71628|6|Mentioned|p17:90||||||Big Hill Creek Granite.|||
37221|Big Shell Unit"|23214|6|Mentioned|p41|||See Fossil Hill Limestone.||||||
34929|Big Sink unit|22952|6|Mentioned|p178-9,Table1p179||Early Pliocene|||||||
37424|Bigga Adamellite|23214|6|Mentioned|p167|||Replaced by Bigga Granite.||||||
37424|Bigga Adamellite|68592|6|Mentioned|p1272|||Gibson (1973); formerly Bigga Granite of Hasan (1957, 1959). Close (1978) continued Gibson's terminology in his mapping, which extended the pluton to the N. The name reverted to Bigga Granite to meet standard nomenclature (Pogson and Watkins, 1998).||||||
79191|Bigga House Basic Igneous Complex|68592|6|Mentioned|p1497|||Of Hasan (1957, 1959); changed to Bigga Mafic Complex following further mapping by Yacopetti (1987). Chappell et al. (1991) changed the name to Goonoonglah Gabbro (after Goonoonglah Creek) to avoid confusion with adjacent Bigga Granite; here renamed Goonoonglah Monzodiorite after more recent petrography. ||||||
79192|Bigga Mafic Complex|68592|6|Mentioned|p1497|||Originally named the Bigga House Basic Igneous Complex (Hasan, 1957, 1959); changed to Bigga Mafic Complex following further mapping by Yacopetti (1987). Chappell et al. (1991) changed the name to Goonoonglah Gabbro (after Goonoonglah Creek) to avoid confusion with adjacent Bigga Granite; here renamed Goonoonglah Monzodiorite after more recent petrography. ||||||
27338|Bijerkerno Beds|22771|6|Mentioned|Fig12.2p45|||||||||
27338|Bijerkerno Beds|22857|5|Briefly described|p45 Tb. 12.2|||Of Tuckwell (1974). Superseded by Bijerkerno Metasediments, Dalnit Bore Metasediments and part of Cartwrights Creek Metasediments of the Paragon Group (Willyama Supergroup). Geological Province: Willyama Fold Belt.||||||
27338|Bijerkerno Beds|29921|6|Mentioned|p64|||||||||
27338|Bijerkerno Beds|30908|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Lower - Middle Proterozoic||||||07-NOV-08
27338|Bijerkerno Beds|33004|6|Mentioned|p126|||||||||
27338|Bijerkerno Beds|34469|6|Mentioned|p110|||Proterozoic. See also P109||||||
27338|Bijerkerno Beds|34896|6|Mentioned|Fig.2|||Also P299||||||
27338|Bijerkerno Beds|36756|6|Mentioned|p112|||||||||
27338|Bijerkerno Beds|36762|6|Mentioned|p20|||||||||
27338|Bijerkerno Beds|37461|4|Described|p319|||||||||
27338|Bijerkerno Beds|38969|6|Mentioned|p198|||||||||
27338|Bijerkerno Beds|39214|5|Briefly described|p7|||||||||
27338|Bijerkerno Beds|39639|6|Mentioned|Fig.3|||||||||
27338|Bijerkerno Beds|39652|6|Mentioned|p47|||||||||
27338|Bijerkerno Beds|39662|6|Mentioned|Table 1|||Refers Tuckwell (1978)||||||
27338|Bijerkerno Beds|39885|6|Mentioned|p430|||||||||
27338|Bijerkerno Beds|43501|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|(Provisional Edition)||||||07-NOV-08
27338|Bijerkerno Beds|43502|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|(Provisional Edition)||||||07-NOV-08
34184|Bijerkerno Metasediment|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30676|Bilgola Sandstone|43338|14|Not recorded|p117||Triassic|||||||
30676|Bilgola Sandstone|43344|5|Briefly described|p34,35||Triassic|Unit of Narrabeen Group||||||
34245|Billabong Creek Granite|22685|6|Mentioned|p728|Silurian|Silurian|Age is Middle Silurian.||||||17-JAN-06
38851|Billabong Creek Limestone Member""|24417|5|Briefly described|p19|||Raised to formation status - see Billabong Creek Limestone .||||||
38856|Billabong Creek Limestone member""|24417|6|Mentioned|p23|||Superseded by Billabong Creek Limestone.||||||
31252|Billabong Creek limestone|43518|14|Not recorded|p106|||Rich fauna. Fauna similar to Cliefden Caves and Bowan Park Limestones||||||
73657|Billabong Limestone|63291|6|Mentioned|p419 Fig. 2|||Name not current, probably referring to Billabong Creek Limestone Member.||||||
81936|Billy Creek Formation (NSW)|70096|5|Briefly described|p221|Artinskian|Artinskian|Of northern Sydney Basin. SHRIMP U-Pb ages of 285.4+\-2.2Ma and 285.8+\-3.0Ma (Claoue-Long and Korsch, 2003). See also supplementary files in appendix for additional stratigraphic and locality information. [See also Billy Brook Formation].||||Underlain by Cranky Corner Sandstone.||12-JUN-20
41599|Bilpa conglomerate|50618|6|Mentioned|p249-251|||Informal-see Bilpa Conglomerate.||||||
41599|Bilpa conglomerate|66623|6|Mentioned|p139.|||Informally named Bilpa conglomerate by Pahl and Sikorska (2004). Formerly part of Torrowangee Series (Mawson 1912), Mootwingee Series (Andrews 1922), Scopes Range beds (Rose and Brunker 1968).||||||
30093|Bimba Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
30093|Bimba Suite|22960|5|Briefly described|p92||Paleoproterozoic|||||||07-NOV-08
30093|Bimba Suite|23223|5|Briefly described|p39|||Described as 'Bimba suite - Ettlewood Calcsilicate Member (BS-ECM)' - meaning equivalence. of Allendale Metasediments, Broken Hill Group. Broken Hill Domain.||||||
30093|Bimba Suite|23248|5|Briefly described|Fig2p169|||||||||
30093|Bimba Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
30093|Bimba Suite|43086|4|Described|p4|||||||||
30093|Bimba Suite|63102|6|Mentioned|p13, p23|||Geological province: Olary Domain, Curnamona Province. Superseded; Used by Clarke et al (1986) to stratigraphically link Olary Domain stratigraphy to the 'suite' terminology used at the time as the Broken Hill mine sequence.||||||22-OCT-19
30093|Bimba Suite|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Block.||||||07-NOV-08
30093|Bimba Suite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Olary Domain. Informal name.||Unit in Willyama Supergroup.||Overlies Calcsilicate Suite. Is overlain by Pelite Suite.||
30093|Bimba Suite|70657|6|Mentioned|p34|||One of a number of name variations including Bimba Formation, horizon, and Sulphide Member. This name was used by Clarke et al. (1986) to tie the Olary Domain stratigraphy to the suites in the Broken Hill Domain. Subsequently, the name Bimba Formation has become entrenched, and is used in this study; see references (p5, p10 Fig.4, p12, p13 Fig.6, p14-16, p20-21, p24, p28-30, p32-39, p41, p43-44, p58, p60, p63-68, p73-75, p77).||||||
26392|Bimberi Granite|42726|5|Briefly described|map legend|Silurian||Variation on Bimberi Leucogranite.||||||
37955|Bimbowrie Granite|24307|5|Briefly described|p971|Mesoproterozoic|Mesoproterozoic|||||||
37955|Bimbowrie Granite|62514|5|Briefly described|p747 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Bimbowrie Suite. Age: c.1580Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
37955|Bimbowrie Granite|69650|6|Mentioned|p15|||Originally Bimbowrie Granites (Benton, 1994); subsequently Bimbowrie Suite (Conor, 2004).||||||
70460|Bindawalla Tuff Member|62095|6|Mentioned|p274 Appdx.|||Of Cherry (1987). Superseded by Bindawalla Ignimbrite Member.||||||31-JAN-08
27708|Bindook Porphyry Complex|22580|6|Mentioned|p95||Early Devonian|||||||
27708|Bindook Porphyry Complex|22768|5|Briefly described|p179|Middle Devonian|Early Devonian|||||||
27708|Bindook Porphyry Complex|22857|4|Described|p157, p179, p480 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Includes the Kowmung Volcaniclastics. Possible correlative of Tangerang Volcanics Max. thickness: >600m. Geological Province: Bindook Rise and Murruin Basin.||||||
27708|Bindook Porphyry Complex|29902|6|Mentioned|p6|||||||||
27708|Bindook Porphyry Complex|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
27708|Bindook Porphyry Complex|30734|6|Mentioned|p5|||||||||
27708|Bindook Porphyry Complex|31161|5|Briefly described|PA8|||||||||
27708|Bindook Porphyry Complex|31993|6|Mentioned|p680|||||||||
27708|Bindook Porphyry Complex|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
27708|Bindook Porphyry Complex|32672|6|Mentioned|p673|||||||||
27708|Bindook Porphyry Complex|32999|3|Fully described|p35|||See also P6. Heavily dissected||||||
27708|Bindook Porphyry Complex|33004|6|Mentioned|p77|||See also P195.||||||
27708|Bindook Porphyry Complex|34481|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early - Middle DevonianE - M||||||
27708|Bindook Porphyry Complex|34692|6|Mentioned|p185|||||||||
27708|Bindook Porphyry Complex|35246|6|Mentioned|p169|||On a table.||||||
27708|Bindook Porphyry Complex|35655|6|Mentioned|Fig.1|||Regional structural setting.||||||
27708|Bindook Porphyry Complex|36390|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27708|Bindook Porphyry Complex|36391|6|Mentioned|p98|||Also P99,100,102-108,110.||||||
27708|Bindook Porphyry Complex|37490|5|Briefly described|Fig.1|||||||||
27708|Bindook Porphyry Complex|39663|6|Mentioned|Table 1|||||||||
27708|Bindook Porphyry Complex|40328|6|Mentioned|p162|||See also P163 and P189||||||
27708|Bindook Porphyry Complex|40821|6|Mentioned|p46|||||||||
27708|Bindook Porphyry Complex|44093|5|Briefly described|p216 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
27708|Bindook Porphyry Complex|61892|6|Mentioned|p201 Fig.1|Middle Devonian|Early Devonian|||||||
27708|Bindook Porphyry Complex|63633|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|||||||
27708|Bindook Porphyry Complex|68592|5|Briefly described|p892, p1060|||Scheibner (1973) for rocks now included in the Bindook Group. He recognised that the rock types around Mares Forest differed from those in the remainder of the complex: see Mares Forest Volcanics. Subsequently named Bindook Complex (Fergusson, 1980); Bindook Volcanic Complex (Simpson, 1986); these terms are obsolete.|||||Quartz porphyry, quartz-hypersthene porphyry, felsite, granite and 'intrusive' dacitic tuff.|
35040|Bingara Gold Group|23050|4|Described|p59|||Formal name NOT intended.||||||
82726|Bingara Plutonic Suite|71628|6|Mentioned|p1: 4; p4: 10, 17, 24, 29, 33, 36,38,41|||See also p4: 47, 52, 55, 58. Flood (1971). The long belt of granites extending from Bendemeer to north of the QLD/NSW border. Replaced by Bundarra Plutonic Suite (Flood and Shaw,1975, 1977).||||||
34088|Bingie Bingie gabbroic diorites|22606|6|Mentioned|P827|||||||||
34461|Bingie Complex|22779|5|Briefly described|p 172|||||||||
68026|Birken Head Volcanic member|50613|6|Mentioned|p211|||Informal - see Birken Head Volcanic Member.||||||
26395|Birkenburn Beds|23048|5|Briefly described|p6 fig5,9||Late Ordovician|||||||
26395|Birkenburn Beds|24116|5|Briefly described|p3|Ordovician|Ordovician|||||||
26395|Birkenburn Beds|24128|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
26395|Birkenburn Beds|30730|6|Mentioned|p10|||Geological map||||||
26395|Birkenburn Beds|30735|3|Fully described|p10|||||||||
26395|Birkenburn Beds|30736|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
26395|Birkenburn Beds|30738|6|Mentioned|p2|||Graptolite faunas. Correlation||||||
26395|Birkenburn Beds|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
26395|Birkenburn Beds|35503|6|Mentioned|p201|||Defined in Felton and Huleatt (1977)||||||
26395|Birkenburn Beds|36413|6|Mentioned|Table 3|||||||||
26395|Birkenburn Beds|40136|5|Briefly described|p17|||||||||
26395|Birkenburn Beds|40328|6|Mentioned|p184|||||||||
26395|Birkenburn Beds|68592|5|Briefly described|p298|Ordovician|Ordovician|Felton and Huleatt (1977). Braidwood area.||||Equivalent to Abercrombie Formation.|Sandstone-rich.|
26395|Birkenburn Beds|71069|6|Mentioned|p58, p71, p169|||Obsolete name, rocks in this unit are now assigned either to the Abercrombie Formation, Covan Creek Formation or the Bendoc Group. ||||||
82364|Bitter Vine Suite|71628|6|Mentioned|p17:18|||||Carrai Supersuite.||||
83862|Bittles Tank Formation|67107|6|Mentioned|p701|Cambrian|Cambrian|||Ponto Group.|||Mafic dykes and flows of fundamentally tholeiitic composition.|
76141|Bittles Tank Suite|66623|6|Mentioned|p80 Fig. 21. |||This name appears twice in the diagram; it should be Bittles Tank Volcanics.||||||
39808|Black Bog Shale, Lower|24248|6|Mentioned|p61|||Informal - see Black Bog Shale.||||||
39812|Black Bog Shale, Upper|24248|6|Mentioned|p67|||Informal - see Black Bog Shale.||||||
39805|Black Bog Shale, lower|24248|6|Mentioned|p54, p65 Fig.9|||Informal - see Black Bog Shale.||||||
39806|Black Bog Shale, upper|24248|6|Mentioned|p52|||Informal - see Black Bog Shale.||||||
39804|Black Bog shale|24248|6|Mentioned|p63, p64|||Informal - see Black Bog Shale.||||||
83688|Black Hill complex|73430|5|Briefly described|p498|||Also referred to as Black Hill intrusion p498, p507 Fig.7, although said to include sub-alkaline gabbros under this name.|||||Includes gabbros, norites, monzogabbros and dolerites.|
38192|Black Jack Group, Lower|61313|6|Mentioned|p105|||Informal name - see Black Jack Group. Shallow marine facies.||||||
39793|Black Jack Group, lower|24159|6|Mentioned|p149|||Informal - see Black Jack Group.||||||
39793|Black Jack Group, lower|61313|6|Mentioned|p103|||Informal name - see Black Jack Group. Channel Facies.||||||
70648|Black Jack Group, upper|61313|5|Briefly described|p97|||Informal - see Black Jack Group. Lacustrine facies that acts as a seal for the basal Black Jack Group 'western bed load' reservoir sandstones. This facies consists of thick and regionally extensive shales and coals (Hoskissons Coal)||||||16-JUN-06
82727|Black Mountain Leucogranite|71628|6|Mentioned|p14:3|||Mikulski (1973). Now part of Glen Garry Microleucosyenogranite.||||||
24728|Black Range Group volcanics|40328|6|Mentioned|p92|||||||||
31045|Black Range rhyolites|44970|14|Not recorded|p55|||||||||
24187|Black Ridge Tuff|39656|4|Described|M14|||||||||
24187|Black Ridge Tuff|39663|6|Mentioned|Table 1|||See also Table 4||||||
24187|Black Ridge Tuff|46524|5|Briefly described|p99|||||||||
29504|Black Rock Sandstone (NSW)|32151|6|Mentioned|p209|||U.Devonian||||||
29504|Black Rock Sandstone (NSW)|43344|14|Not recorded|p158||Late Devonian|||||||
29504|Black Rock Sandstone (NSW)|43384|14|Not recorded|Map Legend||Late Devonian|||||||
29504|Black Rock Sandstone (NSW)|43385|14|Not recorded|p173,174||Late Devonian|Ref. to Stevens & Packham 1952||||||
29504|Black Rock Sandstone (NSW)|71419|6|Mentioned|p8|Devonian|Devonian|Of Stevens and Packham (1953).||||||02-FEB-18
31036|Black Rock Sub Group|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
31036|Black Rock Sub Group|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Unit of Catombal Group||||||
31036|Black Rock Sub Group|43516|14|Not recorded|Map Legend||Late Devonian|||||||
29785|Black Rock Sub-group|43039|5|Briefly described|p10|||Misspelling of Black Rock Subgroup||||||
73712|Black Rock Supergroup|63287|6|Mentioned|p321 Fig. 4|||Consists of sandstone, shale and conglomerate.||||||07-FEB-11
39394|Black Rock subgroup|24126|6|Mentioned|p135|||Of  the Catombal Group.||||||
32653|Black Spring Formation|46547|14|Not recorded|Not recorded|||||||||
30804|Black Springs Formation|43384|14|Not recorded|Map Legend||Silurian|||||||
35160|Blackbutt Formation|23055|6|Mentioned|Fig13 p25|||||||||17-APR-14
24730|Blackfellows Gully Leucoadamellite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Biotite-(hornblende) leucomonzonite; includes porphyritic, flow-banded, and coarse equigranular variants.||||||21-DEC-04
24730|Blackfellows Gully Leucoadamellite|23720|5|Briefly described|Map Legend|||Of Uralla Plutonic Suite.  Biotite leucogranite.||||||15-DEC-04
24730|Blackfellows Gully Leucoadamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
24730|Blackfellows Gully Leucoadamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24730|Blackfellows Gully Leucoadamellite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24730|Blackfellows Gully Leucoadamellite|38288|6|Mentioned|Fig.12|||||||||
24730|Blackfellows Gully Leucoadamellite|38842|6|Mentioned|p286|||||||||
24730|Blackfellows Gully Leucoadamellite|43091|5|Briefly described|Map legend|||||||||
41555|Blackjack Group|60267|6|Mentioned|p15|||Of the Gunnedah region.||||||
41555|Blackjack Group|68004|6|Mentioned|p139, pp166-167.|||Kaolin prospectivity is discussed. See also references to Black Jack Formation (p168, p169) and Black Jack Group (p23 Table 1, p84, p142, p172, p179).||||||
31212|Blackman's Flat conglomerate|43477|14|Not recorded|p25,58|||||||||
77153|Blackmans Flat Formation|68003|6|Mentioned|p41.|Late Permian|Late Permian|Referred to as "Marrangaroo and Blackmans Flat Formations" (sic). Alluvial deposits sourced from Lachlan Fold Belt.||||||
77153|Blackmans Flat Formation|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield. Persistent unit along western margin of the Basin. Wedges out in the Ulan area.||Unit in Cullen Bullen Subgroup.||Overlies Lithgow Coal. Is overlain by Lidsdale Coal and Ulan Coal.|Coarse-grained, pebble-bearing, quartzose sandstone.|
29460|Blanchetown Formation|42966|5|Briefly described|p406|||Superseded by Blanchetown Clay||||||
34247|Bland Granite""|22638|6|Mentioned|p55|||Previously and presently mapped as Kikoira Granite.||||||24-AUG-04
34247|Bland Granite""|61964|5|Briefly described|p37, p43|||Part of Ungarie Granite on COOTAMUNDRA renamed "Bland Granite" in "Ungarie Suite" by Chappell et al (1991). Now superseded by Ungarie and Yalgogrin Granites (Koetong Suite). Unconformable below Tullibigeal Leucitite. Intrudes Clements Fm (Wagga Group)||||||
70461|Blandford Rhyodacite|62095|5|Briefly described|p259 Fig. 10|Permian|Permian|Abbreviated version of Blandford Rhyodacite Member of the Woodton Formation.||||||
31554|Blanket Flat Suite|42726|5|Briefly described|map legend||Silurian|||||||
31257|Blathery Creek Member|43512|2|Defined|p88,89||Late Devonian|Member of the Curra Creek Conglomerate, maximum recorded thickness 500 ft, massive red conglomerate||||||
35490|Blathery Creek Volcanics""|23170|6|Mentioned|p26|||now Fairbridge Volcanics.||||||
35490|Blathery Creek Volcanics""|23213|6|Mentioned|p13|||of Kemezys (1959) and others. Now Fairbridge Volcanics at Bakers Swamp.||||||
70350|Blaxland Fossil Wood Conglomerate|60993|5|Briefly described|p6 Fig. 2|||Of the Marburg Formation (McElroy 1963). Superseded by Koukandowie Formation.||||||
26400|Blaxland Fossil Wood Conglomerate Member|29988|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26400|Blaxland Fossil Wood Conglomerate Member|33476|4|Described|p104|||Mention P99||||||
26400|Blaxland Fossil Wood Conglomerate Member|33766|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26400|Blaxland Fossil Wood Conglomerate Member|34340|3|Fully described|p468|||||||||
26400|Blaxland Fossil Wood Conglomerate Member|42248|4|Described|p406|||||||||
26400|Blaxland Fossil Wood Conglomerate Member|43383|14|Not recorded|p24|||||||||
26400|Blaxland Fossil Wood Conglomerate Member|43468|14|Not recorded|Map Legend|Jurassic|Triassic|Provisional Edition||||||
26400|Blaxland Fossil Wood Conglomerate Member|43881|14|Not recorded|p6-7,11,33,37-8,70,9|||||||||
26400|Blaxland Fossil Wood Conglomerate Member|44450|5|Briefly described|p27|||Of Marburg Formation. Geological Province: Clarence-Moreton Basin.||||||
26400|Blaxland Fossil Wood Conglomerate Member|60995|5|Briefly described|p55 Fig. 6, p64|||See also "Blaxland Fossil Wood Conglomerate Member". Equivalent to Gatton Sandstone in NSW.||||||
26400|Blaxland Fossil Wood Conglomerate Member|60997|5|Briefly described|p140 Fig. 2|||See also "Blaxland Fossil Wood Conglomerate Member".  Replaced by Gatton Sandstone.||||||
39417|Blaxland Fossil Wood Member|24127|5|Briefly described|p5|Jurassic|Triassic|Of the Bundamba Group.||||||
24733|Blayney Andesite|23214|6|Mentioned|p61|||Renamed Blayney Volcanics.||||||
24733|Blayney Andesite|39325|6|Mentioned|p433|||||||||
24733|Blayney Andesite|39663|6|Mentioned|Table 4|||||||||
24733|Blayney Andesite|40328|6|Mentioned|p172|||||||||
24733|Blayney Andesite|43767|6|Mentioned|p894|||||||||
34263|Blayney Andesite""|22679|6|Mentioned|p 21|||replaced by Blayney Volcanics||||||
73672|Blayney Volcanics, lower|63278|6|Mentioned|p145 Fig. 1, p147 Fig. 2b|Late Ordovician|Middle Ordovician|Informal name. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
73672|Blayney Volcanics, lower|63283|5|Briefly described|p191 Tb. 2, p195 Fig. 2|Late Ordovician|Early Ordovician|Informal name: see Blayney Volcanics. Age: 460Ma (basalt). Geological Province: Junee-Narromine Volcanic Belt and Molong Volcanic Belt.||||||07-FEB-11
73672|Blayney Volcanics, lower|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group||||
73672|Blayney Volcanics, lower|73154|5|Briefly described|p77 Fig.3|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Molong Volcanic Belt.|||Byng Volcanics|Overlies Coombing Formation, underlies upper Blayney Volcanics.|Intermediate-mafic lava.|
73673|Blayney Volcanics, upper|63278|6|Mentioned|p145 Fig. 1, p147 Fig. 2b|Late Ordovician|Late Ordovician|Informal name. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
73673|Blayney Volcanics, upper|63283|5|Briefly described|p191 Tb. 2, p208|Late Ordovician|Early Ordovician|Informal name: see Blayney Volcanics. Age: 455Ma (basalt). Geological Province: Junee-Narromine Volcanic Belt and Molong Volcanic Belt.||||||07-FEB-11
73673|Blayney Volcanics, upper|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Shown as Blayney Volcanics (upper).|c. 449-443 Ma|Cabonne Group|Cowriga Limestone Member|||
73673|Blayney Volcanics, upper|73154|5|Briefly described|p77 Fig.3|Bolindian|Gisbornian|Macquarie Arc, Phase 4. Molong Volcanic Belt.||||Overlies lower Blayney Volcanics, underlies Millthorpe Volcanics.|Intermediate-mafic lava.|
73723|Blayney volcanics|63290|6|Mentioned|p391|||Informal: see Blayney Volcanics. Geological Province: Molong Volcanic Belt.||||||
39229|Bloomfield Limestone Member, Lower|23898|6|Mentioned|p274|||Informal name - see Bloomfield Limestone Member.||||||
39229|Bloomfield Limestone Member, Lower|24250|6|Mentioned|p112|||||||||
39817|Bloomfield Limestone Member, middle - upper|24250|6|Mentioned|p112, 114, 117, 120, 123|||||||||
39818|Bloomfield Limestone Member, upper|24250|6|Mentioned|p112|||||||||
31067|Blow Hole latite|43477|4|Described|p19,41|||Included in Broughton tuff. (Part of Gerringong Volcanics)||||||
24735|Blowhole Latite|34292|6|Mentioned|Table 2|||Permian. Gerringong Volc.||||||
24735|Blowhole Latite|36042|6|Mentioned|Fig.16|||||||||
24735|Blowhole Latite|39287|6|Mentioned|Fig. 2.12|||||||||
24735|Blowhole Latite|39289|6|Mentioned|p78|||||||||
24735|Blowhole Latite|43345|14|Not recorded|p3 Table 1||Permian|||||||
24735|Blowhole Latite|43349|14|Not recorded|Map|||||||||
24735|Blowhole Latite|43491|14|Not recorded|pVII/51||Permian|Of Gerringong Volcanics.||||||
24735|Blowhole Latite|45003|14|Not recorded|p186|||||||||
24735|Blowhole Latite|45090|6|Mentioned|p171|||Refers Hanlon et al.(1953)||||||
41052|Blue Knobby Monzogranite|24366|5|Briefly described|p8 Fig. 6|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41052|Blue Knobby Monzogranite|69639|6|Mentioned|p217|Asselian|Asselian||296 +/- 3.3 Ma (SHRIMP U-Pb)|Hillgrove Supersuite||||
41052|Blue Knobby Monzogranite|71628|6|Mentioned|p3: 4, 22|||Originally the Blue Knobby Adamellite of Binns et al. (1967). Subsequently Blue Knobby Monzogranite (Brown, 2003). The spelling is changed here to Blue Nobby Monzogranite because the local homestead, mountain and road appear thus in the Australian Gazetteer. Included in the Hillgrove Supersuite by Landenberger et al. (2010).||||||
41052|Blue Knobby Monzogranite|71703|5|Briefly described|p203, p193 Fig. 1|Cisuralian|Cisuralian|~296 Ma; Rosenbaum et al., 2012.[Probably location 1053 age 296.0+/-3.3 Ma]||Of Hillgrove Supersuite.||Spatially associated with Bakers Creek Suite.||
24736|Blue Mountain basalt|40591|4|Described|p330|||||||||
82815|Blue Mountain limestone''|72958|6|Mentioned|p19, p25|||[Written as 'Blue Mountain limestone']. Brewer (1993). From the Mount Hope Trough?||||||
78589|Blue Mountains Basalts|65195|6|Mentioned|p4|||Erupted onto low (<200 m) relief, W of Lapstone Structural Complex.||||||
82368|Blue Nobby Suite|71628|6|Mentioned|p3: 23|||||Hillgrove Supersuite.|Blue Nobby Monzogranite|||
35630|Blue Rock Formation|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of Noonthorangee Subgroup (Ponto Group). Phyllite with minor arenite, and thin, laminated, siliceous tuff horizons; distinctive on TM image (northern area).||||||26-NOV-08
35630|Blue Rock Formation|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Noothorangee Subgroup. Phyllite with minor arenite, and thin, laminated, siliceous tuff horizons; distinctive on TM image (in northern area). In southern area is intensely deformed phyllite.||||||
35630|Blue Rock Formation|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Noonthorange Subgroup. Phyllite with minor arenite, and thin, laminated, siliceous tuff horizons; distinctive on TM image.||||||01-DEC-08
35630|Blue Rock Formation|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Noonthorangee Subgroup. Phyllite with minor arenite, and thin, laminated, siliceous tuff horizons; distinctive on TM image.||||||27-NOV-08
35630|Blue Rock Formation|66623|6|Mentioned|p89.|||The parent (Noonthorangee Subgroup) is redefined and renamed Noonthorangee Formation in this study.||Unit in Noonthorangee Subgroup.||||
35630|Blue Rock Formation|66929|5|Briefly described|Map legend|||Distinctive on TM image.||Unit in Noonthorangee Subgroup.|||Phyllite with minor arenite and thin, laminated, siliceous tuff horizons.|
35630|Blue Rock Formation|66933|5|Briefly described|Map legend|||Distinctive on TM image.||Unit in Noonthorangee Subgroup.|||Phyllite; minor arenite and thin laminated siliceous tuff horizons.|
35630|Blue Rock Formation|67322|6|Mentioned|p39|Cambrian|Cambrian|Previously part of the Noonthorangee Subgroup (obsolete) - now included in Noonthorangee Formation (Greenfield et al 2010).||||||
74923|Blue Rock Well Basalt|64671|5|Briefly described|Map legend|||Within the Ponto Group. Porphyritic metabasalt; olive green to green-grey, medium to locally coarse-grained, massive to locally strongly foliated feldspar phyric metabasalt as flows, plugs, sills. Porphyritic feldspar crystals locally exceed 1cm.||||||26-NOV-08
74923|Blue Rock Well Basalt|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Noothorangee Subgroup. Porphyritic metabasalt; olive green to green grey, medium to locally coarse grained, massive to locally strongly foliated feldspar phyric metabasalt occuring as flows, plugs or sills.||||||
74923|Blue Rock Well Basalt|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Noonthorange Subgroup. Porphyritic metabasalt; olive green to green grey, medium to locally coarse grained, massive to locally strongly foliated feldspar phyric metabasalt occuring as flows, plugs or sills.||||||01-DEC-08
74923|Blue Rock Well Basalt|66623|6|Mentioned|p89, 95|||The parent (Noonthorangee Subgroup) is redefined and renamed Noonthorangee Formation in this study. The volcanic and intrusive elements now included in Bittles Tank Volcanics.||Unit in Noonthorangee Subgroup.||||24-SEP-13
74923|Blue Rock Well Basalt|66929|5|Briefly described|Map legend|||||Unit in Noonthorangee Subgroup.|||Porphyritic metabasalt; olive green to green grey, medium- to locally coarse-grained, massive to foliated feldspar-phyric metabasalt flows, plugs or sills; phenocrysts locally exceed 1 cm.|
74923|Blue Rock Well Basalt|67322|6|Mentioned|p39|Cambrian|Cambrian|Previously part of the Noonthorangee Subgroup (obsolete) - now included in Noonthorangee Formation (Greenfield et al 2010). Age is assumed to be similar to the parent Grasmere Formation. Occurs in the Kayrunnera-Koonenberry region.||||||
76144|Blue Rock Well Phyllite|66623|6|Mentioned|p89.|||Said (Greenfield et al. 2010) to be a unit in Noonthorangee Subgroup (after Stevens et al. 2000; 2002; Mills 2003) which is replaced by Noonthorangee Formation in this study.||Unit in Noonthorangee Subgroup.||||
76144|Blue Rock Well Phyllite|67322|6|Mentioned|p39|Cambrian|Cambrian|Previously part of the Noonthorangee Subgroup (obsolete) - now included in Noonthorangee Formation (Greenfield et al 2010). Occurs in the Kayrunnera-Koonenberry region.||||||
76145|Blue Rock Well Sandstone|66623|6|Mentioned|p89.|||Said (Greenfield et al. 2010) to be a unit in Noonthorangee Subgroup (after Stevens et al. 2000; 2002; Mills 2003) which is replaced by Noonthorangee Formation in this study.||Unit in Noonthorangee Subgroup.||||
76145|Blue Rock Well Sandstone|67322|6|Mentioned|p39|Cambrian|Cambrian|Previously part of the Noonthorangee Subgroup (obsolete) - now included in Noonthorangee Formation (Greenfield et al 2010). Age is assumed to be similar to the parent Grasmere Formation. Occurs in the Kayrunnera-Koonenberry region.||||||
26406|Blue Waterhole Beds|24266|6|Mentioned|p1486|||Geological Province: Lachlan Fold Belt.||||||09-MAR-05
26406|Blue Waterhole Beds|29456|5|Briefly described|p423|||||||||
26406|Blue Waterhole Beds|31019|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
26406|Blue Waterhole Beds|32820|6|Mentioned|Table 1|||Refers Owen et al. (in press)||||||
26406|Blue Waterhole Beds|33325|6|Mentioned|Table 3|||||||||
26406|Blue Waterhole Beds|34405|5|Briefly described|p117|||Table 3.4||||||
26406|Blue Waterhole Beds|34692|5|Briefly described|p186|||||||||
26406|Blue Waterhole Beds|36050|6|Mentioned|p399|||||||||
26406|Blue Waterhole Beds|36413|6|Mentioned|Table 3|||||||||
26406|Blue Waterhole Beds|37727|4|Described|p39|||||||||
26406|Blue Waterhole Beds|40328|3|Fully described|p62|||||||||
26406|Blue Waterhole Beds|40424|6|Mentioned|p83|||||||||
26406|Blue Waterhole Beds|45147|6|Mentioned|M77|||||||||
35215|Blueys Beach Formation|23157|5|Briefly described|p110 fig2,7,8|Carboniferous|Carboniferous|||||||
35215|Blueys Beach Formation|65380|6|Mentioned|p670|||Of Skilbeck and Cawood (1994) as a lateral equivalent of Yagon Siltstone.||||||
31236|Blythesdale Series|43491|14|Not recorded|pX/18,19||Cretaceous|||||||
31236|Blythesdale Series|44432|4|Described|p55,60,64,88|Cretaceous|Late Jurassic|See also Lexicon.||||||
31236|Blythesdale Series|44861|14|Not recorded|p234,266||Early Cretaceous|||||||
31236|Blythesdale Series|45009|14|Not recorded|p64|||Replaced "Blythesdale Braystone" by Whitehouse 1940. See also Lexicon.||||||
24739|Blythesdale beds|34254|6|Mentioned|PP494|||||||||
24739|Blythesdale beds|44861|14|Not recorded|p235||Early Cretaceous|Overlain by Roma and Tambo Series.||||||
40930|Boambolo Member|50230|4|Described|Map legend|Wenlock|Wenlock|Of the Yass Formation.  Interbeds with and partly overlies the Copplestone Member within the Yass Formation.  Massive shale, interbedded sandstone; sparsely fossiliferous.||||||
73720|Bocobidgle Formation|63290|6|Mentioned|p393 Tb. 1|Wenlock|Wenlock|Of Forbes Group. Contains pebbles and cobbles from the Goonumbla Volcanics. Shallow-water depositional environment and contains igneous clasts of porphyritic volcanics and monzonite in a calcareous sandy matrix.||||||
26408|Bodalla Adamellite|22779|5|Briefly described|Table 1|||Tuross Tonalite||||||
26408|Bodalla Adamellite|22815|4|Described|p90|Late Devonian|Middle Devonian|Age: 365+/-11 Ma.||||||
26408|Bodalla Adamellite|32127|6|Mentioned|p271|||Dated 365 +/- 11m.y.||||||
26408|Bodalla Adamellite|32129|6|Mentioned|p6|||Refers Thomson (1974)||||||
26408|Bodalla Adamellite|32673|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early to Middle DevonianE - M||||||
26408|Bodalla Adamellite|33480|6|Mentioned|p243|||Age dating||||||
26408|Bodalla Adamellite|35248|6|Mentioned|p236|||||||||
26408|Bodalla Adamellite|35289|4|Described|p19|||||||||
26408|Bodalla Adamellite|36411|6|Mentioned|p268|||Refers Chalker & Bembrick 1977 for definition.||||||
26408|Bodalla Adamellite|39627|6|Mentioned|Appendix|||||||||
26408|Bodalla Adamellite|40328|4|Described|p202|||||||||
26408|Bodalla Adamellite|40646|6|Mentioned|p22|||||||||
26408|Bodalla Adamellite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Moruya Suite.||||||
26408|Bodalla Adamellite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moruya Igneous Complex. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
38456|Boebuck granite|24133|6|Mentioned|p53|||Informal name.||||||
25797|Bog Hole Adamellite|22815|4|Described|p52|Early Devonian|Late Silurian|||||||
25797|Bog Hole Adamellite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25797|Bog Hole Adamellite|35109|2|Defined|p67|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25797|Bog Hole Adamellite|35263|6|Mentioned|p222|||||||||
25797|Bog Hole Adamellite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
25797|Bog Hole Adamellite|40328|6|Mentioned|p205|||||||||
25797|Bog Hole Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian.||||||
25797|Bog Hole Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab9.||||||
25797|Bog Hole Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
29279|Bog Hole Granite|42726|5|Briefly described|map legend|Silurian||388. Variation on Bog Hole Adamellite.||||||
38925|Bogalong Granite""|24417|6|Mentioned|p99|||Superseded by Bogalong Suite.||||||
38937|Bogalong Granodiorite""|24417|6|Mentioned|p112|||Superseded by Grenfell Granite.  Originally described, along with "Warraderry Porphyry", to subdivide Grenfell Granite - but now abandoned.||||||
28240|Bogan Gate Sandstone|22638|6|Mentioned|Fig4,p71|||||||||
28240|Bogan Gate Sandstone|22831|5|Briefly described|p 75|Mesozoic|Late Silurian|||||||
28240|Bogan Gate Sandstone|23392|6|Mentioned|p3|||Superseded by Peaks Sandstone and Hunter Formation of Conolly 1965.||||||
28240|Bogan Gate Sandstone|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28240|Bogan Gate Sandstone|30071|6|Mentioned|p371|||||||||
28240|Bogan Gate Sandstone|33121|4|Described|p77|||Refers Conolly (1965). ?Middle-Late Dev. See also P73||||||
28240|Bogan Gate Sandstone|33732|5|Briefly described|p114|||||||||
28240|Bogan Gate Sandstone|35070|6|Mentioned|Fig.6|||||||||
28240|Bogan Gate Sandstone|42714|4|Described|p24|||Name to be dropped/suppressed||||||
28240|Bogan Gate Sandstone|43441|5|Briefly described|32|Mesozoic|Late Silurian|Of Connelly, 1965: Name dropped||||||08-JAN-10
28240|Bogan Gate Sandstone|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Beargamil Sub-Group. In Tullamore Syncline||||||
28240|Bogan Gate Sandstone|43507|2|Defined|p126,128,135,165||Late Devonian|Basal formation of Beargamil Subgroup (Hervey Group)||||||
28240|Bogan Gate Sandstone|43510|2|Defined|p41,45,70-1|||||||||
77672|Bogan Gate Sandstone Group""|68297|6|Mentioned|p181|Ludlow|Ludlow|Replaced by Cookeys Plains Formation (Pickett 1992)||||||
38940|Bogan Gate Sandstone""|23392|6|Mentioned|p3|||Superseded by Peaks Sandstone and Hunter Formation. Of Conolly 1965.||||||11-FEB-16
38940|Bogan Gate Sandstone""|24417|6|Mentioned|p126|||Superseded by Peaks Formation.||||||
38940|Bogan Gate Sandstone""|62569|5|Briefly described|p607 Fig. 2|Late Devonian|Late Devonian|Within the Hervey Group of Conolly (1965, 1969). Now superseded and incorporated into Sherwin's (1996, 1997) Hervey Group - as ?Clagger Sandstone?||||||
24741|Bogandillon Chert Member|22857|5|Briefly described|p446 App.1, Tb.A1.6|Silurian|Silurian|Of the Weelah Formation. Max. thickness: ~500m.||||||
24741|Bogandillon Chert Member|24417|6|Mentioned|p64|||Of Kemezy (1976).  Of the Weelah Formation?  Name to be retained in case of further definition of the unit.||||||
24741|Bogandillon Chert Member|35503|2|Defined|p208|Silurian|Silurian|New name refs Kemezys (1976). Part of Weelah Formation. Prob. Silurian||||||
24741|Bogandillon Chert Member|40328|6|Mentioned|p45|||||||||
38913|Bogandillon Member""|24417|6|Mentioned|p64|||See also Bogandillon Chert Member.||||||
81733|Bogandyera Suite|69801|6|Mentioned|p104|||Central Lachlan Orogen. Supersedes the Mannus Creek Suite.|||Includes the Bogandyera Granite.|||
41338|Bogang Granite|60086|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite granite.||||||07-NOV-08
74653|Boggabri-Gunnedah Volcanics|24040|6|Mentioned|p468 Fig. 1|||Compound term for informal  grouping of the Boggabri Volcanics with the Gunnedah Volcanics, situated at the eastern margin of the Surat Basin.||||||21-AUG-08
27111|Boggy Plain Adamellite|33959|6|Mentioned|p233|||Age.||||||
27111|Boggy Plain Adamellite|36443|5|Briefly described|map legend|Pragian|Lochkovian|Of Boggy Plain I-type Suite. Intrusives. BMR map code Dba: adamellite; Dbg: granodiorite, minor quartz gabbro; Dbd: gabbro, quartz gabbro, minor granodiorite.||||||
27111|Boggy Plain Adamellite|40328|4|Described|p202|||||||||
27111|Boggy Plain Adamellite|45147|2|Defined|M258|Early Devonian|Early Devonian|Probably Early Devonian.||||||
77697|Boggy Plains Suite|60308|6|Mentioned|p38||||||Coolamine Complex, Cuga Burga Volcanics, Yoeval Complex.|||
80245|Bogolong Suite|67847|5|Briefly described|p22|Lochkovian|Lochkovian|Age derived from L.Black pers.comm. (cited in Raymond and Wallace 2000a)|415.6 +/- 5.1 Ma (SHRIMP U-Pb)|||Intrudes the Kirribilli Formation.||
39383|Bogolong granodiorite|24125|5|Briefly described|p87|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
68703|Bogong Suites|44093|5|Briefly described|p183 App. 1|Early Devonian|Early Devonian|Informal name see Bogong Suite p184 Appendix 1. Of the Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||25-JAN-06
79194|Bogungra Microtonalite|68592|5|Briefly described|p1079, p1109|||Originally distinguished as a pluton of undifferentiated Marulan Batholith by Hall (1981). Defined by Jones, Hall et al. (1986). Here (Thomas and Pogson, 2012) redefined as the Bogungra Dacite Member of the Tangerang Formation on the basis of textural and compositional similarities with the Carne Dacite Member.|||||A high-level dacitic intrusion.|
31559|Bogungra Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31559|Bogungra Suite|44093|5|Briefly described|p219 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31559|Bogungra Suite|70661|6|Mentioned|p77|||||||||
28385|Bolivia Range Adamellite|34489|6|Mentioned|Fig.4.9|||||||||
28385|Bolivia Range Adamellite|34589|6|Mentioned|p275|||238 my||||||
28385|Bolivia Range Adamellite|71628|6|Mentioned|p15:8|||Shaw (1969). Later the Bolivia Range Leucoadamellite (Brunker and Chesnut, 1976), and now Bolivia Range Leucomonzogranite (Henley et al., 2001 after unpublished work by Barnes, 1987).||||||
32510|Bolivia mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
32266|Boloka Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb18. Misspelling of Boloko Granodiorite.||||||
32266|Boloka Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
31224|Bolten Formation|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Beargamil Sub-Group. Manildra-Gooloogong Region.||||||25-JUN-08
31224|Bolten Formation|43510|14|Not recorded|p52|||Listed as part of the Beargamil Subgroup in map legend Manildra-Gooloogong area||||||
38947|Bolten Formation""|23217|6|Mentioned|p3|||(Conolly, 1965a). Informal - see Bolten Formation. Superseded by Boulton Formation.  Misspelt as "Bolton Formation" on the 1972 FORBES 1:250 000 sheet; also confused with "Bolton beds" (Silurian) in the Tantangara region of NSW.||||||08-MAR-06
38947|Bolten Formation""|24417|5|Briefly described|p129|||Name replaced by "Boulton Formation" to avoid confusion with "Boltons beds".||||||
31050|Bolton Greywacke|43491|4|Described|pIII/14||Ordovician|||||||
31050|Bolton Greywacke|44970|14|Not recorded|p12,85|||May be correlated with Black Mountain Sandstone||||||
38945|Boltons beds""|24417|5|Briefly described|p129|||Not related to "Bolten Formation" or Boulton Formation.||||||
30756|Bolwarra Conglomerate|22610|6|Mentioned|Fig 5|||||||||
30756|Bolwarra Conglomerate|43344|14|Not recorded|p88|||See also Lexicon. Ref.to David||||||
30756|Bolwarra Conglomerate|43477|4|Described|p43||Permian|Basal member of Muree formation||||||
30756|Bolwarra Conglomerate|43491|14|Not recorded|pVII/48||Permian|||||||
34579|Bombala Beds""|22815|6|Mentioned|p28|Ordovician|Ordovician|||||||
34579|Bombala Beds""|23329|6|Mentioned|1044|||||||||
34579|Bombala Beds""|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Monaro Slope and Basin. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
34579|Bombala Beds""|60988|5|Briefly described|p144 Fig.1, p146|Late Ordovician|Late Ordovician|Apparently replaced by Adaminaby Group.|||||Turbiditic sandstones and shales.|
75775|Bombala Intrusion|65779|6|Mentioned|p288 Fig. 1, p290 Fig. 2|||Informal name.||||||
30729|Bondi sandstone|43358|14|Not recorded|p50||Triassic|(Hawkesbury Sandstone)||||||
29424|Bondo Dolerite|23017|6|Mentioned|p310|||||||||
29424|Bondo Dolerite|42960|6|Mentioned|p69|||Variation on Bondo Dolerite Member||||||
29424|Bondo Dolerite|43679|6|Mentioned|p310|||||||||
29424|Bondo Dolerite|50126|5|Briefly described|p76, p83 App.2|Middle Eocene|Middle Eocene|Of the Monaro Volcanics. Age: 48.9 +/- 0.4 Ma (Roach 1996)||||||
29423|Bondo Dolerite Member|22815|2|Defined|p112|Early Eocene|Early Eocene|||||||
29423|Bondo Dolerite Member|42960|5|Briefly described|p69|||To be used on Bega 1:250 000 sheet.||||||
29423|Bondo Dolerite Member|42961|5|Briefly described|p72|||||||||
29423|Bondo Dolerite Member|43126|3|Fully described|p12|||||||||
29423|Bondo Dolerite Member|43233|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
29423|Bondo Dolerite Member|43577|6|Mentioned|p384|||||||||
26413|Bondonga Beds|29988|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26413|Bondonga Beds|38914|6|Mentioned|p328|||||||||
24745|Bong Bong Flow|36220|6|Mentioned|p97|||||||||
70381|Bong Bong basalt|60997|5|Briefly described|p139 Fig. 1|Early Jurassic|Early Jurassic|Informal name. Geological Province: Sydney Basin.||||||
30955|Bonningnot Formation|43432|14|Not recorded|p207||Carboniferous|Misspelling of Bonnington Formation. Marine.||||||
26414|Bonnington Formation|32324|6|Mentioned|Table 8.1|||||||||
26414|Bonnington Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26414|Bonnington Formation|32866|6|Mentioned|p16|||Fossil content||||||
26414|Bonnington Formation|33728|6|Mentioned|p50|||||||||
26414|Bonnington Formation|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26414|Bonnington Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
26414|Bonnington Formation|34077|5|Briefly described|p252|||||||||
26414|Bonnington Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
26414|Bonnington Formation|34086|6|Mentioned|p262|||||||||
26414|Bonnington Formation|34238|6|Mentioned|Table 1|||||||||
26414|Bonnington Formation|39302|5|Briefly described|p342|||||||||
26414|Bonnington Formation|39979|6|Mentioned|p39|||||||||
26414|Bonnington Formation|41826|6|Mentioned|p344|||||||||
26414|Bonnington Formation|43447|14|Not recorded|p12,Table 1||Carboniferous|||||||
26414|Bonnington Formation|43451|14|Not recorded|Map Legend|||||||||
26414|Bonnington Formation|44797|14|Not recorded|p174|||||||||
26414|Bonnington Formation|44833|14|Not recorded|p108-121||Early Carboniferous|Faunal zones.||||||
26414|Bonnington Formation|45097|6|Mentioned|p15|||Orthotetes australis zone||||||
41301|Bonnington Formation""|44244|6|Mentioned|p59|||Superseded by Bonnington Siltstone.||||||
39360|Bonnington siltstone|24121|6|Mentioned|p4|||Misspelt - see Bonnington Siltstone.||||||25-AUG-22
37162|Boogeldie Formation|23522|5|Briefly described|p248 Fig 4|Middle Devonian|Early Devonian|||||||
37162|Boogeldie Formation|65214|6|Mentioned|p277|Devonian|Devonian|Mawson and Talent, 2000. NSW, Mudgee. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
31210|Boogie Sandstone|43499|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
74753|Boohlabone Granite|61964|6|Mentioned|p80|||Misspelling of Boolahbone Granite. A-type.||||||
74533|Boohlahbone Granite|63891|6|Mentioned|p241|||Misspelt. See Boolahbone Granite.||||||
74533|Boohlahbone Granite|71206|6|Mentioned|p372-373|||Mentioned in a list of A-type granites. Mis-spelling of Boolahbone. Mention is made of a Boohlahbone Suite, attributed to Barron et al. (1982), but no such Unit occurs anywhere in that article. This, and with no other constituents suggested to comprise a Suite, as well as the persistent mis-spelling, militate against inclusion in the Database.|||||Shallow-level, A-type granite.|
26415|Bookookoorara Porphyritic Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26415|Bookookoorara Porphyritic Adamellite|71628|6|Mentioned|p11:4|||Pogson and Hitchins (1973). Later the Bookookoorara Monzogranite (Brown et al., 2001).||||||
82728|Bookookoorara Suite|71628|5|Briefly described|p11:5|||||Bungulla Supersuite.|Bookookoorara Monzogranite.|||
76068|Bookpornong Formation|66286|6|Mentioned|p180 Fig.2.|||[Misspelling of Bookpurnong]||||||08-AUG-11
34518|Bookpurnong Beds""|22799|6|Mentioned|p34|||||||||
34519|Bookpurnong Formation""|22799|6|Mentioned|p34|||||||||
41339|Boomerang Creek Granite Gneiss|60086|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Maragle Bathylith (Batholith?).||||||07-NOV-08
69979|Boomi Creek mafic granulite|61794|6|Mentioned|p360|||Informal name.||||||
69978|Boomi Creek ultramafic granulite|61794|6|Mentioned|p360|||Informal name.||||||
37302|Boomi Rhyolite|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Of Caroda Formation.  Geological Province: New England Orogen.||||||10-MAR-05
37302|Boomi Rhyolite|24010|5|Briefly described|p381|||||||||
37302|Boomi Rhyolite|24348|5|Briefly described|p134|Carboniferous|Carboniferous|||||||
37302|Boomi Rhyolite|24603|6|Mentioned|p895 Fig. 16|||||||||
37302|Boomi Rhyolite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of the Clifden Formation, not Caroda Formation as previously identified.||||||30-JUN-05
31220|Boona beds|43510|14|Not recorded|p73||Late Devonian|Now named Boona Sandstone||||||
79445|Boonabah volcanic rocks|70178|6|Mentioned|p4 fig. 2|Ordovician|Ordovician|Macquarie Arc.||||||
27114|Boonanghi Beds|24124|5|Briefly described|p3|Carboniferous|Devonian|||||||
27114|Boonanghi Beds|29990|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27114|Boonanghi Beds|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27114|Boonanghi Beds|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27114|Boonanghi Beds|34293|2|Defined|p42|Carboniferous|Carboniferous|||||||
27114|Boonanghi Beds|34294|6|Mentioned|p912|||||||||
27114|Boonanghi Beds|36528|6|Mentioned|p179|||||||||
27114|Boonanghi Beds|36961|6|Mentioned|Fig.5|||||||||
27114|Boonanghi Beds|38803|5|Briefly described|p109|||||||||
27114|Boonanghi Beds|43385|14|Not recorded|p167||Carboniferous|= Boonanghi Series||||||
27114|Boonanghi Beds|45097|6|Mentioned|p27|||Fragmentary fossils. Not possible to zone.||||||
27114|Boonanghi Beds|47056|6|Mentioned|Fig.2 P523|||||||||
27114|Boonanghi Beds|47059|5|Briefly described|p145|||Probably intended Boonanghi beds.||||||
27114|Boonanghi Beds|61771|5|Briefly described|p116|||Probably an informal name. Exposed in the Parrabel Beds. Geological Province: Northern Hastings Terrane.||||||
27114|Boonanghi Beds|63832|6|Mentioned|p131 fig 2|Visean|Tournaisian|Northern Hastings block, Southern New England Fold Belt.||||||
27114|Boonanghi Beds|64631|6|Mentioned|p44 Fig.2.|Visean|Tournaisian|Southern New England Fold Belt: northern Hastings Block. Some biostratigraphic age control ~ mid-Formation. ||||||
30830|Boonanghi Series|43385|14|Not recorded|p167,177||Early Carboniferous|||||||
30829|Boonanghi group|43385|14|Not recorded|p167||Early Carboniferous|=Boonanghi Series||||||
24750|Boonderoo Limestone Member|23214|6|Mentioned|p45|||Replaced by Belubula Limestone||||||
24750|Boonderoo Limestone Member|38219|5|Briefly described|p300|||||||||
24750|Boonderoo Limestone Member|40127|6|Mentioned|p9|||||||||
24750|Boonderoo Limestone Member|40136|5|Briefly described|p18|||||||||
68027|Boorabil Ignimbrite|50613|6|Mentioned|p211|||Probably misspelt (or an informal abbreviation?) - see Boorabil Ignimbrite Member.||||||22-FEB-05
36967|Booralong Adamellite|23720|5|Briefly described|Map Legend|||Of Uralla Plutonic Suite.  Porphyritic hornblende-biotite monzogranite.||||||15-DEC-04
36967|Booralong Adamellite|68111|5|Briefly described|p968 Tb.1|Olenekian|Olenekian||ca. 250 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
36967|Booralong Adamellite|71628|6|Mentioned|p8:18|||Gilligan et al. (1992), who renamed the previous Booralong Granodiorite to better reflect the composition of the unit. The revised lithology nomenclature, Booralong Monzogranite, is currently Reserved in the ASUD; it occurs also in unpublished work of Chappell and Bryant (1994).||||||
77033|Booralong Monzogranite|71628|6|Mentioned|p8:18|||Previously Booralong Adamellite of Gilligan et al. (1992), who renamed the earlier Booralong Granodiorite to better reflect the composition of the unit. The revised lithology nomenclature, Booralong Monzogranite, is currently Reserved in the ASUD; it occurs also in unpublished work of Chappell and Bryant (1994).||||||
35217|Booraloo Subgroup|22969|4|Described|Fig 4.1a||Late Permian|||||||
79103|Boorooban granite|69635|5|Briefly described|p182-187|Early Devonian|Early Devonian|Informal name. Western Lachlan Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age. Sample from petroleum borehole Hay-1, drilled in 1970. This unit does not crop out.|409.4+/-5.1 Ma||||Porphyritic granodiorite, consisting of ~35% quartz, ~30% plagioclase, ~10% biotite, ~10% hornblende and ~15% orthoclase phenocrysts. I-type.|
81734|Boorooban granite''|69801|6|Mentioned|p2, p137|Devonian|Devonian|Central Lachlan Orogen. Intersected in a drillhole midway between Hay and Denilquin 220km to the northwest of the Jindera Granite.|409.4 +/- 5.1 Ma (SHRIMP)|||||
76038|Booroorban Granodiorite Suite|66934|6|Mentioned|Map legend|Early Devonian|Late Silurian|Informal name. |||Includes Eurolie and Booroorban granodiorites.|||
76039|Booroorban granodiorite|66934|5|Briefly described|Map legend|Early Devonian|Late Silurian|Informal name. Magnetic susceptibility and gravity readings are given. Relatively non-magnetic source rock.||Unit in Booroorban Granodiorite Suite.|||Coarse-grained porphyritic granodiorite consisting of 35% quartz, 30% plagioclase, 15% orthoclase phenocrysts, 10% biotite and 10% hornblende.|
41551|Boorowa basalt|50616|6|Mentioned|p286 Fig. 9||Miocene|Informal name.||||||
37164|Booth Limestone|23522|5|Briefly described|p249 Fig 5|Pragian|Pragian|||||||
37164|Booth Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cobar. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
74754|Boothumble beds|61964|6|Mentioned|p30, p67, p68|Devonian|Devinian|Of Brunker (1973). Previously contained Marobee Conglomerate. Superseded by Boothumble Formation. Also written as "Boothumble beds".||||||
74618|Boothumble beds""|61964|6|Mentioned|p67, p68|||One of former names for Preston Formation rocks, mapped originally as Ural Volcanics.Informal name.Superseded by Preston Fm. Divided into upper + lower Boothumble beds (Maniw 1983a - p68) to describe  Preston Fm + Ural Volcanics equivalents||||||
29738|Boppy Sandstone|43032|5|Briefly described|Table 1,p8|||Rayner 1969||||||
28390|Borenore Limestone Member|33116|6|Mentioned|p210|||Refers Walker (1959)||||||
28390|Borenore Limestone Member|33117|6|Mentioned|p92|||||||||
28390|Borenore Limestone Member|34405|4|Described|p110|||||||||
27721|Borenore Limestone member|40620|4|Described|p76|||||||||
31006|Boriag Group|43461|14|Not recorded|Table p621||Devonian|||||||
39425|Boro granite|24128|6|Mentioned|p82|||Informal name - see Boro Granite.  Geological Province: Lachlan Fold Belt.||||||
80167|Botany Sand Beds|68811|5|Briefly described|p56-p58, p126 tbl 13, p165 tbl 27|Quaternary|Quaternary|Sediments are sourced from either tidal swamp or aeolian dune environments. The Beds can be subdivided into four stratigraphic units: a basal fluvial sand with minor gravel that grades into marine sand with estuarine shells and peaty marine muds. The second unit is composed of clay, clayey quartz sands and minor peat beds. The third unit consists of clean, well-sorted, medium-grained sands that is overlain by the fourth unit of clean, fine to medium grained sands with silt and clay. ||||Overlies the Hawkesbury Sandstone.|Unconsolidated sands, silts, clay and peat.|
24755|Botumburra Granodiorite|40258|6|Mentioned|Fig.1|||||||||
24755|Botumburra Granodiorite|42659|6|Mentioned|p119|||||||||
24755|Botumburra Granodiorite|71628|6|Mentioned|p17:14|||Asthana and Leitch (1985). Currently Botumburra Range Monzogranite (Chappell and Bryant, 1994). The author prefers an earlier version, Botumburra Range Granodiorite of Leitch et al.(1982)(reasons given).||||||
73825|Botumburra Range Monzogranite|70876|5|Briefly described|p80-p81|Upper Triassic|Upper Triassic||228-227 Ma (Rb-Sr age)|Herries Supersuite||||
73825|Botumburra Range Monzogranite|72528|4|Described|p2, p4 Tb.1.2, p102-107, p110, p127.|Ladinian|Ladinian|Magmatic crystallisation age determined. Previous K-Ar and Rb-Sr dating discussed. This is a relatively young age for a southern New England Orogen granite. Shown as part of the New England Orogen. May be related to the Purkiss prospect silver occurrence.|232.7+/-1.0 Ma 238U/206Pb (207Pb-corrected)|Botumburra Suite, Carrai Supersuite||Intrudes Nambucca beds|Includes grey, fine to medium-grained, porphyritic biotite-hornblende granodiorite, with plagioclase phenocrysts <1cm in length. Percentage mineral composition plagioclase (50), quartz (20), alkali feldspar (15), hornblende (8), and biotite (7).|
83960|Botumburra Range Suite|71628|5|Briefly described|p17: 15|||||Carrai Supersuite.|Botumburra Range Granodiorite.|||
73826|Botumburra Suite|72528|5|Briefly described|p102.|Ladinian|Ladinian||232.7+/-1.0 Ma|Carrai Supersuite|Includes Botumburra Range Monzogranite||Includes granodiorite.|
35109|Boughton Member|23055|6|Mentioned|p26|||of Bunya Bunya Formation, Newcastle Coal Measures.||||||
79195|Boulder Conglomerate Member|68592|6|Mentioned|p884-5|||Superseded. The 'Boulder Conglomerate Member' and overlying 'Lenticle Tuff' unit of Cas et al. (1981) is now included in the Murruin Formation (Bindook Group) with the upper part considered as a possible reworked equivalent of the Barrallier Ignimbrite.||||Is overlain by Lenticle Tuff Member.||
30943|Boundary Creek Intrusives|43429|14|Not recorded|Map Legend|||Manilla River Intrusives are similar||||||
30943|Boundary Creek Intrusives|43435|14|Not recorded|Map Legend||Tertiary|Name is invalid||||||
35431|Bournewood Formation""|23170|6|Mentioned|p55|||||||||
73711|Bowan Park Limestone Sub-group|63287|5|Briefly described|p320, p347-349|Eastonian|Gisbornian|Of the Barrajin Group. Includes: Daylesford Limestone. Underlain by Cargo Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73714|Bowan Park Subgroup|63287|6|Mentioned|p333|Eastonian|Gisbornian|Not a current name, referres to Bowan Park Limestone Subgroup. Age: 453Ma (palaeontological data).||||||07-FEB-11
73714|Bowan Park Subgroup|63293|5|Briefly described|p470, p469 Fig. 2|Eastonian|Eastonian|Includes; Daylesford Limestone. Overlain by Malachis Hill Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73714|Bowan Park Subgroup|70684|5|Briefly described|p34-35, p39-42|Late Ordovician|Late Ordovician|Mapped and subdivided by Semeniuk (1970, 1972). An Eastonian limestone sequence. Used, as often as not, as an equivalent name to Bowan Park Limestone Subgroup (see references p34, p39-42, p75).||||Overlies Malachis Hill Formation and Cargo Volcanics.|Limestone.|
73714|Bowan Park Subgroup|70754|5|Briefly described|p448, p450-451|Late Ordovician|Late Ordovician|Outer shelf-edge deposits. Fossiliferous olistoliths occur in Barnby Hills Shale.|||Ballingoole, Daylesford Limestones.|Overlies ?unconformably Cargo Volcanics. Is overlain conformably by Malachis Hill Formation.||
73714|Bowan Park Subgroup|73299|6|Mentioned|p1104 Fig.10|Late Ordovician|Late Ordovician|Molong High.||||Overlies the Fairbridge Volcanics, underlies the Malachis Hill Limestone.|Limestone.|
38198|Bowen Park Group|23736|5|Briefly described|p19|||||||||
41709|Bowens Road Lower coal seam|44244|5|Briefly described|p181, p182 Fig. 37|Late Permian|Late Permian|Informal name.  Of the Wenham Formation.  Lower section of the Bowens Road coal seam.  Geological Province: Myall Block.||||||
70098|Bowens Road Lower seam|22857|5|Briefly described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for seam at base of the Wenham Formation (Craven Subgroup, Gloucester Coal Measures). Geological Province: Sydney Basin.||||||
41708|Bowens Road coal seam|22857|5|Briefly described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for seam at top of the Wenham Formation (Craven Subgroup, Gloucester Coal Measures). Geological Province: Sydney Basin.||||||
41708|Bowens Road coal seam|44244|5|Briefly described|p182 Fig. 37, p183|Late Permian|Late Permian|Informal.  Of the Wenham Formation.  Has a lower section known as the Bowen Road Lower coal seam.  Overlain everywhere by Wards River Conglomerate.||||||30-AUG-04
31189|Bowling Alley Group|43491|14|Not recorded|pV/13|Middle Devonian|Early Devonian|=Tamworth Group. Ref.to Benson 1915||||||
30885|Bowling Alley Series|43399|14|Not recorded|p190|||||||||
30885|Bowling Alley Series|43400|14|Not recorded|p176|Middle Devonian|Early Devonian|=Tamworth Group. Ref. to Benson 1912||||||
70099|Bowman beds""|22857|6|Mentioned|p500 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Included in the Bundook beds.||||||
72753|Bowning Group Volcanics""|63025|5|Briefly described|p1052 Fig. 1, p1053|Pragian|Lochkovian|Informal unit of the Black Range Group (Luck, 1973). Geological Province: Eastern Lachlan Orogen.||||||
24758|Bowning Group""|35386|6|Mentioned|p42|||Refers Link(1970,1971)||||||
32925|Bowning granites|48878|14|Not recorded|p.20|||Age of pre-Bowning granites.||||||
34274|Box Ridge Member|22679|6|Mentioned|p 30|||||||||
34274|Box Ridge Member|23214|6|Mentioned|p146|||Replaced by Box Ridge Volcanics.||||||
78524|Boxwell Granite|68111|5|Briefly described|p968 Tb.1|Wuchiapingian|Wuchiapingian||256.6 +/- 1.7 Ma, U-Pb SHRIMP (Cross et al. 2010)|||||
69163|Boyd Volcanic complex|60423|6|Mentioned|p381|Late Devonian|Late Devonian|||||||
40698|Boyd volcanics|23309|6|Mentioned|p390|||||||||
35828|Bradleys Creek Complex|23321|5|Briefly described|p430 Fig.2|||||||||07-FEB-07
36140|Bradleys Creek complex|23464|6|Mentioned|p249|||||||||
35170|Bradman Member|23055|6|Mentioned|Fig23p37|||||||||
77698|Braidwood Dykes|60308|6|Mentioned|p38|Givetian|Eifelian|[Invalid name for dykes intruding the Braidwood Granodiorite] "Important stratigraphic unit with contentious age". Preferred age quoted.|390 Ma|||||28-MAY-13
74773|Branch Creek Formation (NSW)|60290|6|Mentioned|p15|Permian|Permian|Proposed by Slee (1968) that Dalwood Group should be subdivided into Billy Brook Formation, Cranky Corner Sandstone, Branch Creek and Tamby Creek Formations. All but Branch Creek Fm. were retained. Geol. Prov: Cranky Corner Basin.||||||07-FEB-11
31237|Brandon Conglomerate|43491|14|Not recorded|pVII/42-3||Early Permian|||||||
40797|Brandon Grove Limestone Member|50147|5|Briefly described|Map legend|Visean|Visean|Misspelt - see Bandon Grove Limestone Member of Flagstaff Formation.  Geological Province: Gresford Block||||||
24761|Brandy Springs Beds|31694|6|Mentioned|p343|||||||||
80246|Brangan Chert|67847|6|Mentioned|p21-p22|Late Ordovician|Middle Ordovician|||||Conformably overlain by the Kirribilli Formation.||
31063|Branxton Beds|43477|14|Not recorded|Pl.3||Permian|||||||
31063|Branxton Beds|44489|14|Not recorded|p70|||See also Lexicon.||||||
31063|Branxton Beds|48830|14|Not recorded|p.6|||||||||
68156|Branxton Formation, Middle|60281|6|Mentioned|p9|||Informal - see Branxton Formation.||||||
68157|Branxton Formation, middle|60281|6|Mentioned|p14|||See also Branxton Formation, Middle.||||||
41306|Branxton Fromation|23350|6|Mentioned|261 Fig 2|||Misspelt - see Branxton Formation.  Contains Jasdec Park Sandstone Member.||||||
31062|Branxton Group|43477|14|Not recorded|p42|||||||||
31190|Branxton Mudstone|43491|14|Not recorded|pVII/44||Permian|||||||
30757|Branxton Stage|43344|14|Not recorded|p84|||Now included in Branxton Formation||||||
30757|Branxton Stage|43440|14|Not recorded|p90|||Ref.to David 1950||||||
30757|Branxton Stage|43477|14|Not recorded|p15,Pl.3|||Ref.to David||||||
30757|Branxton Stage|43491|4|Described|pVII/48||Permian|||||||
30757|Branxton Stage|44383|14|Not recorded|p256||Artinskian|Fossil. See also Lexicon.||||||
30757|Branxton Stage|44855|14|Not recorded|p25||Late Permian|Glacio.-marine||||||
30757|Branxton Stage|44861|14|Not recorded|p246|||||||||
41305|Branxton Sub Group|23350|6|Mentioned|261 Fig 2|||Superseded by Branxton Formation.||||||
31213|Branxton Sub-group|43477|4|Described|p18,23,41-45|||Part of Maitland Group||||||
30758|Breakwater Conglomerate""|43344|14|Not recorded|p106||Permian|Kempsey area||||||
26423|Bredbo River Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Bredbo River Adamellite. Not variation on Bredbo Group.||||||
77274|Breeza Seam|43194|5|Briefly described|p115, p133 App. 1|Late Permian|Late Permian|Informal name? Within Benelabri Mudstone Member (Clare Sandstone, Coogal Subgroup, Black Jack Group)||||||
77274|Breeza Seam|68004|5|Briefly described|p152, p170.|||Southern Mullaley Sub-basin, Gunnedah Basin. Widely developed; 1.5 to 4.8 m thick. Numerous stone bands make the ash content high to very high; hence the unit has limited underground development potential.|||||Contains banded dull coal and several tuff layers to 0.35 m thick.|
70100|Breeza coal seam|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name? At top of Clare Sandstone (Coogal Subgroup, Black Jack Group). ||||||
77172|Breeza member|68003|5|Briefly described|p75 Fig.3-r.|Pliocene|Miocene|Mooki Valley, Liverpool Plains.||||Overlies Quipolly gravels. Is overlain by Curlewis member.|Sand, silt and gravel.|
74159|Brewery Well Granite|63519|5|Briefly described|p6 Fig. 2, p12|Mesoproterozoic|Mesoproterozoic|Age: 1580+/-5Ma. Geological Province: Broken Hill Block-Euriowie Block. Undeformed granite.||||||20-FEB-08
83491|Brindalbert Gabbro|73264|6|Mentioned|p1384 Fig.7|||From Maher et al., (1997).||||||
83560|Bringelli Shale|73304|6|Mentioned|p76|||[Probably misspelt from Bringelly Shale]. Sydney Basin.||||||
30759|Bringelly Shale formation|43344|14|Not recorded|p56,57||Triassic|||||||
41382|Broad Gully Formation""|44244|5|Briefly described|p167|Late Permian|Late Permian|Informal name - see Broad Gully Formation.  Superseded by "Stratford Coal Measures" (Bewley, 1971) and "Upper Craven Coal Measures" (George, 1971, 1975).||||||
82729|Broadwater Monzogranite Phase|71628|5|Briefly described|p15: 35, 98, 102-104, 115|||This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.||Severn River Monzogranite.|||Pink, medium- to fine-grained, slightly to moderately porphyritic biotite-(hornblende) monzogranite to ?syenogranite.|
41552|Brocklehurst basalts|50616|6|Mentioned|p286 Fig. 9||Miocene|Informal name.||||||
37322|Brodribb Volcanics|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
29514|Brogans Creek Limestone|43641|5|Briefly described|Map Legend||Devonian|||||||
77152|Brogans Ignimbrite|68003|5|Briefly described|p133.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Beige, unwelded, rhyolitic ignimbrite, pumiceous in parts.|
77152|Brogans Ignimbrite|68005|5|Briefly described|p139.|Stephanian|Namurian|Probably missing the rank 'Member' in the Table.||Unit in Currabubula Formation.|||Beige, unwelded rhyolitic ignimbrite, pumiceous in part.|
70468|Brogans Rhyodacite|62095|5|Briefly described|p259 Fig. 10, p260 Tb. 1|Early Permian|Early Permian|Abbreviated form of Brogans Rhyodacite Member. Age: 290.6+/-2.8Ma.||||||
70468|Brogans Rhyodacite|70096|6|Mentioned|p222|||Geological province: New England Orogen. Of Gunnedah Basin. SHRIMP U-Pb ages from volcanic samples indicate a Sakmarian age.||||||
30922|Brogans Tuff Member|43417|14|Not recorded|Map Legend||Late Carboniferous|||||||
30922|Brogans Tuff Member|62095|6|Mentioned|p279 Appdx.|||Of Manser (1968). Superseded by Brogans Rhyodacite Member.||||||
34509|Broken Hill Suite|22771|6|Mentioned|Table12.2p45|||||||||
34509|Broken Hill Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Incorporated Parnell Beds and top of "Yancoe Complex" (of Cordwell and Williams, 1962). Superseded by the Broken Hill Group (Willyama Supergroup). Referred to as Suite 4 by Stevens, Stroud et al (1979, 1980). ||||||
69470|Broken Hill gabbro|61154|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Informal name. Age: ~820Ma. Part of extensive mafic magmatism together with the Gairdner Dyke Swarm. Geological Province: South Australian Craton.||||||
34568|Broken formation|22815|6|Mentioned|p16|Paleozoic|Paleozoic|Informal subdivision applied to the block-in-matrix features in the Bogolo Formation.||||||07-NOV-08
80005|Bronxholme Formation|70684|6|Mentioned|p54 Fig.27|Ordovician|Ordovician|Adaminaby Superterrane.||||||
80005|Bronxholme Formation|72495|6|Mentioned|p218|Ordovician|Ordovician|Adaminaby Superterrane.|||||Turbidite.|
25813|Brooklana Beds|24127|5|Briefly described|p4|||||||||
25813|Brooklana Beds|24129|5|Briefly described|p4|Carboniferous|Carboniferous|||||||
25813|Brooklana Beds|31695|4|Described|p254|||Mention Fig. 1, petrology||||||
25813|Brooklana Beds|31802|5|Briefly described|p137|||U.Palaeozoic||||||
25813|Brooklana Beds|35171|6|Mentioned|p93|||||||||
25813|Brooklana Beds|35173|6|Mentioned|p102|||||||||
25813|Brooklana Beds|35264|2|Defined|p15|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
25813|Brooklana Beds|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition.||||||
25813|Brooklana Beds|36528|6|Mentioned|p175|||||||||
25813|Brooklana Beds|36961|6|Mentioned|Fig.5|||||||||
25813|Brooklana Beds|37438|6|Mentioned|p17|||||||||
25813|Brooklana Beds|37489|6|Mentioned|Fig.2|||||||||
25813|Brooklana Beds|37808|6|Mentioned|p25|||||||||
25813|Brooklana Beds|38822|6|Mentioned|p195|||Geological Province: New England Fold Belt||||||
25813|Brooklana Beds|69639|6|Mentioned|p123, p223|Permian|Devonian|||||Intruded by the Chaelundi Complex.||
25813|Brooklana Beds|71628|5|Briefly described|p17:51|||Is associated with As-Au mineralisation (prospect named).||||Is intruded by Billys Creek Granodiorite.||
79443|Brooklyn Conglomerate|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dktb. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot. [Should this be Brooklyn Conglomerate Member?] ||Tangerang Formation||Erosional at base. Overlain by unnamed member near base of Tangerang Formation.|Massive-diffusely bedded, cobble-boulder conglomerate (with clasts of quartz arenite, siltstone and mudstone), interbedded with graded and cross bedded, pebbly and coarse-grained sandstone.|
79443|Brooklyn Conglomerate|70542|5|Briefly described|Map Legend|Devonian|Devonian|[Should this be Brooklyn Conglomerate Member?]||Tangerang Formation|||Massive-diffusely bedded, cobble-boulder conglomerate (with clasts of quartz arenite, siltstone and mudstone), interbedded with graded and cross bedded, pebbly and coarse-grained sandstone.|
35273|Brooklyn Formation|23171|6|Mentioned|p45 Fig. 1|||||||||12-MAY-04
83661|Brooman basalt|73581|5|Briefly described|p22|Oligocene|Oligocene|South Coast Volcanic Province. Outcrops 25 km north of Batemans Bay. Up to 22 m thick.|27.4 Ma and 28.0 Ma K-Ar||||Basalt lavas with olivine and augite phenocrysts in a plagioclase-rich groundmass.|
31071|Broughton tuff|43477|14|Not recorded|p19,41|||Inc.Jamberoo tf mbr,Bumbo lat,Kiama tf mbr,Blow Hole lat,Westley Park tf mbr.Part of Gerringong Volc||||||
70101|Brown seam|22857|6|Mentioned|p520 App.1 Tb.A1.9|Early Permian|Early Permian|Informal reference to coal seam within the Maules Creek Formation (Bellata Group). ||||||
70101|Brown seam|43194|5|Briefly described|p133 App. 1|Early Permian|Early Permian|Informal name? Within Maules Creek Formation (Bellata Group)||||||
83253|Browns Creek dykes|73431|5|Briefly described|p364, p372, p373 Fig.8, p374 Fig.9|||Same rocks as the Mine Dyke Group. See p372.||Browns Creek Intrusive Complex||Intrudes Cowriga Limestone Member.||
82730|Bruisers Creek Granodiorite Phase|71628|4|Described|p11: 20-23|||New name, after a local creek, for the SE lobe of the parent body. Occurs at Newton Boyd, ~45 km due E of Glen Innes. Crops out as whalebacks, tors and rock platforms. Petrology and mineralogy described in some detail. Associated with Mo and Pb-Cu-Ag-Zn mineralisation; prospects named.||Mount Mitchell Monzogranite.||Intrudes Sara beds and Brooklana Beds (Coffs Harbour Association); also faulted against the latter. Abuts Wandsworth Volcanic Group. Is faulted against Newton Boyd Granodiorite.|Light grey to light pink, texturally heterogeneous, medium- to coarse-grained, equigranular to porphyritic, biotite-hornblende granodiorite and monzogranite, minor monzodiorite; leucocratic veins. Abundant xenoliths (mostly mudstone or siltstone).|
34306|Brungle Metabasalts|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol province Lachlan Fold Belt.||||||
27350|Brushy Hill Limestone|31519|6|Mentioned|p912|||||||||
27350|Brushy Hill Limestone|32529|4|Described|p198|||Refers Osborne (1950)||||||
27350|Brushy Hill Limestone|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27350|Brushy Hill Limestone|32866|6|Mentioned|p8|||Fossil content||||||
27350|Brushy Hill Limestone|32869|5|Briefly described|p166|||Depositional environment. Refers Osborne (1928)||||||
27350|Brushy Hill Limestone|38215|6|Mentioned|p275|||||||||
27350|Brushy Hill Limestone|39214|6|Mentioned|p32|||||||||
27350|Brushy Hill Limestone|41279|6|Mentioned|Fig.2|||||||||
27350|Brushy Hill Limestone|45088|4|Described|p21|||See also P20, P61 and Plate 2||||||
27350|Brushy Hill Limestone|45097|5|Briefly described|p14|||Conodonts. Brachiopods P24.||||||
27350|Brushy Hill Limestone|46803|6|Mentioned|Fig. 3|||||||||
27350|Brushy Hill Limestone|63832|6|Mentioned|p131 fig 2|Tournaisian|Tournaisian|Rouchel block, Southern New England Fold Belt.||||||
27350|Brushy Hill Limestone|64631|6|Mentioned|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, Rouchel Block.||||||
25815|Bruxner Adamellite|33476|2|Defined|p94|Triassic|Triassic|Mention p22.||||||15-NOV-07
25815|Bruxner Adamellite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
25815|Bruxner Adamellite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
25815|Bruxner Adamellite|40773|6|Mentioned|p458|||||||||
25815|Bruxner Adamellite|42378|6|Mentioned|Table 1 P11|||||||||
25815|Bruxner Adamellite|43008|5|Briefly described|map legend|||||||||
25815|Bruxner Adamellite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
25815|Bruxner Adamellite|71628|6|Mentioned|p9: 1-2, 4|||Thomson (1973, 1976). Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). Appeared as Bruxner Park Adamellite in Barnes et al. (1995). The lithology is not included in the list of constituents of the Suite on p9-1.||||||
39023|Bruxner Monzogranite|23799|5|Briefly described|p117|||Of the Bruxner Suite (in Clarence River Supersuite).||||||
39023|Bruxner Monzogranite|68008|6|Mentioned|p333|||Geochemistry mentioned.||||||
39023|Bruxner Monzogranite|70876|4|Described|p2-p3, p36-p41, p78-80, p94|Permian|Permian|New England Orogen. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|256.0 +/- 1.4 Ma (SHRIMP U-Pb)|Bruxner Suite|||Medium-grained, coherent, inequigranular orange-pink rock.|
39023|Bruxner Monzogranite|71628|6|Mentioned|p9:4|||Cranfield et al. (2001). Originally Bruxner Adamellite (Thomson; 1973, 1976). Now the Bruxner Granodiorite; new name, this study.||||||
39021|Bruxner Suite|23799|5|Briefly described|p117, p115 Fig. 10|||Of Clarence River Supersuite.||||||
39021|Bruxner Suite|69639|6|Mentioned|p170, p223|||Formerly included the Koreelan Creek Granodiorite.||Clarence River Supersuite||||
39021|Bruxner Suite|70876|5|Briefly described|p36, p80|||New England Orogen.||Clarence River Supersuite|Includes the Bruxner Monzogranite.|||
39021|Bruxner Suite|71628|5|Briefly described|p9:5|||||Clarence River Supersuite.|Bruxner Granodiorite.|||
39022|Bruxner suite|23799|6|Mentioned|p117|||Informal - see Bruxner Suite.||||||
36982|Buaraba granodiorite|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Informal name.||||||
36982|Buaraba granodiorite|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Informal name.  Granodiorite, leucogranodiorite, tonalite, quartz diorite.||||||
38470|Buchan group|23309|5|Briefly described|p5 Fig. 1.3|||Informal-see Buchan Group.||||||
38470|Buchan group|24133|5|Briefly described|p20 Fig. 8|Early Devonian|Silurian|Informal.  Geological Province: Lachlan Fold Belt.||||||
38470|Buchan group|24551|6|Mentioned|p38 Fig. 2.41|Lower Devonian|Lower Devonian|||||||
39356|Buchargingah Muscovite Granite|24119|5|Briefly described|p47|Silurian|Silurian|||||||
79442|Buchargingah granite|69371|6|Mentioned|p9, p14, p18-19|Silurian|Silurian|||||||
69373|Bucketts rhyolites""|50099|5|Briefly described|p13|Early Permian|Early Permian|Informal name for banded-rhyolites of the Alum Mountain Volcanics. Previously termed the "Gloucester Rhyolites". Unconformably overlies the Johnsons Creek Conglomerate; disconformably overlain by Dewrang Group. Geological Province: West Myall Block.||||||
35433|Buckinbah Volcanics""|23170|6|Mentioned|p55|||||||||
39399|Buckinbar Volcanics|24126|6|Mentioned|p141|||||||||
81879|Buckley's Lake Monzogranite|72571|5|Briefly described|p90-91, p96-99, p101|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail. I-type.|||||Felsic biotite granite with titanite, allanite and magnetite.|
81880|Buckley's Lake Suite|72571|6|Mentioned|p90|||Of the Tasmanides of eastern Australia.||||||
24776|Buckleys Vale Adamellite|41905|6|Mentioned|p37|||||||||
29727|Buckwaroon Beds""|43032|6|Mentioned|p64|||Refers to Andrews (1913)||||||
34258|Buddigower Granite""|22638|6|Mentioned|p55|||Superseded by Buddigower Granite||||||07-MAR-16
31245|Budgebegambil Tuff""|43510|14|Not recorded|p48|||In legend of map showing Hervey Syncline||||||
27726|Budgery Sandstone""|34404|4|Described|p99|||||||||
36360|Budgong Sandstone""|23544|5|Briefly described|p359|||In the Broughton Formation||||||
73670|Budhang Chert|63278|6|Mentioned|p156|Early Ordovician|Early Ordovician|Previously a member of the Triangle Formation by Murray and Stewart (2001). Contains conodont fauna indicating an age range of late Lancefieldian to early Bendigonian.||||||07-FEB-11
73670|Budhang Chert|63283|6|Mentioned|p195 Fig. 2, p205|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Geological Province: Rockley-Gulgong Volcanic Belt.||||||07-FEB-11
73670|Budhang Chert|63289|6|Mentioned|p371|Lancefieldian|Bendigonian|Geological Province: Rockley - Gulgong Volcanic Belt. Contains chert.||||||07-FEB-11
73670|Budhang Chert|67322|5|Briefly described|p17|Early Ordovician|Early Ordovician|Albury-Bega Terrane. Murray and Stewart (2001). Oldest unit in the Oberon-Rockley region due to the presence of late Lancefieldian to early Bendigonian conodont assemblages. Originally a member of the Triangle Formation, but was subsequently tentatively reassigned to the Adaminaby Group (Percival and Glen 2007). Occurs in the Oberon-Rockley region.||Of the Adaminaby Group||||
73670|Budhang Chert|67847|5|Briefly described|p27||||||||Imbricated cherts.|
73670|Budhang Chert|68466|5|Briefly described|p65, 67|Early Ordovician|Early Ordovician|Oberon district. Similar in age to the Mummel Chert Member (Floian). Is the thickest Early Ordovician chert in the Lachlan Orogen.|||||Grey-black.|
73670|Budhang Chert|68592|6|Mentioned|p307|Early Ordovician|Early Ordovician|Oberon area. Contains abundant Paracordylodus gracilis conodonts.||||||
73670|Budhang Chert|69668|6|Mentioned|p931|Floian|Floian|Oberon district. Similar early Floian age to Mummel Chert Member. Contains Paracordylodus gracilis conodonts, amongst others.||||||
73670|Budhang Chert|71700|6|Mentioned|CD|Early Ordovician|Early Ordovician|||||||
28409|Budjong Sandstone Member|34334|6|Mentioned|p366|||Misspelling of Budgong?||||||
26431|Buggary Granite|42726|5|Briefly described|map legend|Early Devonian||407. Variation on Buggary Granodiorite.||||||
83478|Buggs Creek Ignimbrite|73487|6|Mentioned|p565, p574 Fig.8, p583-584|||||||||
34295|Bugs Ridge Adamellite""|22679|6|Mentioned|p 44|||||||||
68003|Bukalong Adamellite""|22815|6|Mentioned|p84|||Informal - see Bukalong Granite. Of Beams (1980 unpubl.).||||||
29683|Buladelah Formation|43017|5|Briefly described|Fig.1,p372|||Misspelling of Bulahdelah Formation||||||
73724|Bulbodney Complex|63290|6|Mentioned|p391|Llandovery|Bolindian|Age: 448+/-4Ma (SHRIMP).||||||
36205|Bulbodney Creek Complex|23088|6|Mentioned|p652|||||||||
34617|Bulbodney Creek Complex""|22831|6|Mentioned|p 19|||Replaced by Bulbodney Creek Intrusive Complex||||||
38959|Bulbodney Creek Ultramafic Intrusive Complex|24417|6|Mentioned|p39|||||||||
35362|Bulga Ignimbrite Member|23185|6|Mentioned|p162||Frasnian|||||||
30805|Bull's Camp Rhyolite|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
30805|Bull's Camp Rhyolite|43385|14|Not recorded|p173,174||Early Devonian|Ref. to Stevens & Packham 1952||||||
30805|Bull's Camp Rhyolite|43525|14|Not recorded|map p124,126,Tb p127|||||||||
30806|Bull's Camp Volcanics|43344|14|Not recorded|p139|Early Devonian|Late Silurian|||||||
30806|Bull's Camp Volcanics|43517|14|Not recorded|p151,diag.p153||Gedinnian|||||||
69717|Bulla granite|24222|5|Briefly described|p2|||Informal name. Geological Province: Lachlan Fold Belt.||||||24-JAN-06
68004|Bullamanang Porphyry|22815|6|Mentioned|p39 Fig. 16|||Misspelt - see Bullnamang Porphyry (p40).||||||
24781|Bullanamang Granite|42726|5|Briefly described|map legend|Early Devonian||145. Variation on Bullanamang Porphyry? Part of Bega Batholith.||||||
82731|Bulldog Diggings Monzogranite Phase|71628|5|Briefly described|p11: 3, 27-29, 31, 34-35|||New unit, after Bultitude (Chappell, unpublished data). Named after the locality of that name, ~40 km E of Tenterfield, Timbarra Tableland. Geochemistry very briefly described.||Rocky River Monzogranite.||Possibly abuts Long Creek Quartz Monzonite Phase. Also said to be 'entirely enclosed within… Ewingar Monzogranite Phase'.|Leucocratic hornblende-biotite monzogranite.|
78304|Bulldog Shale Formation|68821|6|Mentioned|p301 Fig.5|||Misspelt Bulldog Shale in figure||||||
79337|Bullenbalong Group|70297|6|Mentioned|map legend|Ludlow|Wenlock|Misspelt in Time-Space plot. See Bullenbalong Supersuite in legend.||||||
68676|Bullenbalong granites|23549|6|Mentioned|p522|||Informal name. Important to recognise that these "B. granites are part of the same supersuite as the Hawkins Volcanics" in order to understand the crystallisatiuon histroy of these granites.||||||
68676|Bullenbalong granites|24099|6|Mentioned|p47|||Informal name - refers to granites of the Bullenbalong Suite.  Geological Province: Lachlan Fold Belt.||||||18-APR-05
69718|Bullenbalong supersuite|24222|6|Mentioned|p4|||Informal - see Bullenbalong Supersuite; see also Bullenbalong Suite. Geological Province: Lachlan Fold Belt.||||||
81249|Bullenbung granite|72083|5|Briefly described|p7-8, p15|||Chappell et al. (1991). Mount Arthur area: south side of Murrumbidgee River. May be part of the Collingullie Granite.||||||
24782|Bulli Coal Meeasures""|30006|6|Mentioned|p6|||||||||
70096|Bulli coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
24783|Bulli seam|33129|6|Mentioned|p328|||||||||
24783|Bulli seam|33869|6|Mentioned|p66|||||||||
24783|Bulli seam|35635|6|Mentioned|p139|||||||||
24783|Bulli seam|36545|6|Mentioned|Fig.6|||||||||
24783|Bulli seam|36594|6|Mentioned|p2|||||||||
24783|Bulli seam|37087|6|Mentioned|p203|||||||||
24783|Bulli seam|37088|4|Described|p205|||||||||
24783|Bulli seam|37089|4|Described|p211|||||||||
24783|Bulli seam|37091|6|Mentioned|p226|||||||||
24783|Bulli seam|37834|6|Mentioned|p50|||||||||
24783|Bulli seam|37835|6|Mentioned|p22|||||||||
24783|Bulli seam|39293|6|Mentioned|Fig. 8.4|||||||||
24783|Bulli seam|39576|6|Mentioned|p15|||||||||
24783|Bulli seam|40017|6|Mentioned|p48|||||||||
24783|Bulli seam|40166|6|Mentioned|p348|||||||||
24783|Bulli seam|40279|6|Mentioned|p16|||||||||
24783|Bulli seam|40335|6|Mentioned|p98|||||||||
24783|Bulli seam|40548|6|Mentioned|p186|||||||||
69997|Bulliac beds|61766|5|Briefly described|p67|||Informal status (Mayer 1972). Included along with Ghanghat Spilite and Belbora beds within an undifferentiated unit termed Bundook beds. Geological Province: Tamworth Belt.||||||
70006|Bulliac formation|61766|6|Mentioned|p68|||Informal - see Bulliac Formation. Geological Province: Tamworth Belt.||||||
32927|Bullongong Member|48878|14|Not recorded|p.6|||= Bullongong Shale Member.||||||
36403|Bulls Pit Limestone Member|50234|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Longreach Volcanics (Mount Fairy Group).  White to cream bedded fossiliferous marble.||||||13-MAY-04
38934|Bumbaldry Granite""|24417|6|Mentioned|p101|||||||||
37111|Bumberry Formation""|23392|6|Mentioned|p15|||||||||
37111|Bumberry Formation""|24417|6|Mentioned|p145|||Informal - see Bumberry Formation.||||||
38935|Bumberry Granite""|24417|6|Mentioned|p108|||Superseded by Bindogandri Granite.||||||
32951|Bumbo Basalt|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama). Part of Upper Marine Series.||||||
27728|Bumbo Latite Member|22488|4|Described|p840-1|||||||||
27728|Bumbo 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.||||||
27728|Bumbo Latite Member|23442|4|Described|p168|||of Broughton Formation||||||
27728|Bumbo Latite Member|23544|4|Described|Table 1 p360.|||also see Fig 2 p358. Of the Gerringong Volcanics in the Broughton Formation, Sydney Basin||||||
27728|Bumbo Latite Member|29900|6|Mentioned|p175|||||||||
27728|Bumbo Latite Member|29901|4|Described|Table 1|||||||||
27728|Bumbo Latite Member|31128|6|Mentioned|Table 1|||||||||
27728|Bumbo Latite Member|32938|6|Mentioned|p67|||Geology||||||
27728|Bumbo Latite Member|36220|4|Described|p37|||See also Table 1.||||||
27728|Bumbo Latite Member|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27728|Bumbo Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27728|Bumbo Latite Member|38690|4|Described|p291|||Formerly Bumbo Latite||||||
27728|Bumbo Latite Member|39308|6|Mentioned|p517|||||||||
27728|Bumbo Latite Member|40270|6|Mentioned|Table 1|||||||||
27728|Bumbo Latite Member|40519|6|Mentioned|Fig.2|||||||||
27728|Bumbo Latite Member|41832|5|Briefly described|p671|||||||||
27728|Bumbo Latite Member|42787|5|Briefly described|p135|||||||||
27728|Bumbo Latite Member|45090|6|Mentioned|p171|||Refers Hanlon et al. (1953)||||||
27728|Bumbo Latite Member|67500|5|Briefly described|p12 Tb.1, p16|Late Permian|Late Permian|Between 9-150m thick.||Of the Broughton Formation and Gerringong volcanic facies.|||Three coarsely porphyritic columnar jointed flows, with breccia pipes; large phenocrysts of labradorite and small phenocrysts of augite.|01-MAY-12
27728|Bumbo Latite Member|71115|5|Briefly described|p178-180, 182-185, 187-188, 191-192|Permian|Permian|Southern Sydney Basin. Sub-aqueous eruptions; northerly flow direction. Columnar jointing. Paleomagnetic results tabulated, discussed. See also p194-195.|265.05 +/- 0.35 Ma.|Gerringong Volcanics (Broughton Formation).||Overlies Kiama Sandstone. Is overlain by Jamberoo Sandstone.|Porphyritic basaltic andesite with a mid-grey to black aphanitic groundmass and phenocrysts of plagioclase and minor pyroxene.|
27728|Bumbo Latite Member|71542|6|Mentioned|p25, 26|Late Permian|Late Permian|Of southern Sydney Basin.  See also Bumbo flow p31.||Unit of Gerringong Volcanics.||Within Broughton Formation.||20-OCT-21
27728|Bumbo Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.||Overlies Kiama Sandstone. Is overlain by Jamberoo Sandstone.|Shoshonitic basaltic andesite; porphyritic, holocrystalline, dark grey to black.|
31072|Bumbo latite|43477|14|Not recorded|p19,41|||Part of Broughton tuff||||||
24786|Bumbolee Creek Beds|29450|6|Mentioned|p53|||||||||
24786|Bumbolee Creek Beds|29454|4|Described|p11|||Pre-M.Silurian||||||
24786|Bumbolee Creek Beds|29648|6|Mentioned|p15|||||||||
24786|Bumbolee Creek Beds|31161|5|Briefly described|PA6|||||||||
24786|Bumbolee Creek Beds|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
24786|Bumbolee Creek Beds|32672|6|Mentioned|p672|||||||||
24786|Bumbolee Creek Beds|35185|6|Mentioned|p232|||||||||
24786|Bumbolee Creek Beds|36534|6|Mentioned|p225|||||||||
24786|Bumbolee Creek Beds|37727|6|Mentioned|p39|||See also Fig.1.||||||
24786|Bumbolee Creek Beds|39331|4|Described|p36|||See also P34||||||
24786|Bumbolee Creek Beds|40328|5|Briefly described|p37|||||||||
24786|Bumbolee Creek Beds|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
24786|Bumbolee Creek Beds|40498|6|Mentioned|p364|||||||||
68028|Bunaleer Dacite|50613|6|Mentioned|p211|||Probably misspelt (or an informal abbreviation?) - see Bunaleer Dacite Member.||||||
68028|Bunaleer Dacite|68005|5|Briefly described|p137.|Stephanian|Namurian|Forms a dome 4 km by 1.5 km.|316.3 +/- 2.7 Ma.|Unit in Willuri Formation.|||Grey, strongly flow foliated, dacite; dome-like structure with interbedded glass, pyroclastics and conglomerate at flanks; related flow remnants south of dome.|
38930|Bundaburrah Granite""|24417|6|Mentioned|p106|||Superseded by Bundaburrah Granodiorite.||||||
39386|Bundaburrah granodiorite|24125|5|Briefly described|p87|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
80265|Bundahburrah Granodiorite|71040|6|Mentioned|p16|Devonian|Devonian|Currowong Syncline.||||||
41347|Bundamba Group Quartz|60079|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|Informal name for Bundamba Group.||||||
70660|Bundamba Group, Lower|61310|6|Mentioned|p28 Fig.C10|||Informal - see bundamba Group.||||||
70661|Bundamba Sandstone, Mid""|61310|5|Briefly described|p21, p24|||Informal name for the sandstone part of the Pillar Valley Formation also known as the "Middle Bundamba Unit". See also p31, p32, p G4036.||||||
70662|Bundamba Unit, Lower""|61310|5|Briefly described|p21, Tabl C1 (p22-23)|||Informal name previously used for Laytons Range Conglomerate and Raceview Formation. Geological Province: Clarence-Moreton Basin. See also p31.||||||
70663|Bundamba Unit, Middle""|61310|5|Briefly described|p21, Table c1 (p22-23)|Early Jurassic|Early Jurassic|Informal name previously used for Pillar Valley Formation.  Also referred to as the "Middle Unit". Conformably overlies Raceview Formation; conformably overlain by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin||||||
70664|Bundamba Unit, Upper""|61310|5|Briefly described|p20, Table C1 (p22-23)|||Informal name previously used for Ripley Road Sandstone. Underlies the base of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
31922|Bundamba sandstones|43881|14|Not recorded|p73-74,77|||See also Lexicon.||||||
31922|Bundamba sandstones|44068|14|Not recorded|p14,17|||||||||
31922|Bundamba sandstones|44555|14|Not recorded|p223|||||||||
31922|Bundamba sandstones|44673|14|Not recorded|p28|||Porus basal unit of Bundamba||||||
31922|Bundamba sandstones|44825|14|Not recorded|p52|||||||||
70363|Bundamba sequence|60995|6|Mentioned|p63|||Informal reference to the sequence of rocks which should include Gatton Sandstone (Cameron 1907). ||||||
83064|Bundandah Granite|73197|6|Mentioned|p465 Fig.4|Carboniferous|||||||Intrusives.|
77276|Bundarra Granite|67818|5|Briefly described|p130|Artinskian|Artinskian|Whole rock Rb-Sr age.|286+/-13 Ma|||||
77276|Bundarra Granite|67908|5|Briefly described|p281|Permian.|Permian.|Texas Orocline, New England Orogen. Occupies the western limb of the Orocline.|290 Ma.||||S-type granitoid.|
77276|Bundarra Granite|68004|6|Mentioned|p128.|Late Carboniferous|Late Carboniferous|Mineral potential and level of certainty are discussed.||||||
77276|Bundarra Granite|68006|5|Briefly described|p108, p122.|||Copeton area. A NE-trending lineament passes through the junction of this unit and the Gilgai Granite and may be prospective for diamonds.||||||
40257|Bundarra Granitoid Suite|38905|6|Mentioned|p302 Fig.1|||Geological Province: New England Fold Belt||||||
40244|Bundarra Plutonic Suite""|38842|5|Briefly described|p287|||Geological Province: New England Fold Belt. Age: 285 +/- 15Ma||||||
83043|Bundarra Plutonic Supersuite|73202|5|Briefly described|p625-626, p630, p634, p636-638, p640|Early Permian|Early Permian|New England Orogen, southern. S-type granites. Formed from melting of the Carboniferous accretionary wedge. Geochemically and lithologically very similar to Hillgrove Plutonic Supersuite. Whole rock Rb-Sr age of 286 +/- 13 Ma from Flood and Shaw (1977), 285 +/- 4 Ma magmatic zircon age (SHRIMP) shown on p639 Fig.10.|ca 285 Ma, 292-285 Ma||||Characterised by non-foliated monzogranites containing muscovite, cordierite and minor garnet, largely homogeneous.|
69991|Bundarra Plutonic suite|61773|6|Mentioned|p139|||Informal name.||||||
39784|Bundarra Suite""|35020|6|Mentioned|p346 Fig. 8, p349|Early Permian|Late Carboniferous|||||||
68805|Bundarra granites|24513|6|Mentioned|p9|||Informal reference to granites within the Bundarra Supersuite.||||||
37384|Bundarra suite|23763|6|Mentioned|p543|||Informal.  Geological Province: New England Fold Belt.||||||
37384|Bundarra suite|24040|6|Mentioned|p486|||Informal - see Bundarra Suite.||||||
68806|Bundarra supersuite|24513|6|Mentioned|p9, p10 Fig. 1|||Informal. See Bundarra Supersuite.||||||
69876|Bundong Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains the Bundong Granite.||||||
24790|Bundook Beds|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
24790|Bundook Beds|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
24790|Bundook Beds|32672|6|Mentioned|p673|||||||||
24790|Bundook Beds|36390|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24790|Bundook Beds|40883|6|Mentioned|p5|||||||||
41387|Bundook Beds""|44244|6|Mentioned|p191|||Of Pogson (1972).  Superseded by Bundook beds.||||||
79560|Bundycoota Formation|67870|5|Briefly described|p62|Devonian|Devonian|Darling Basin. Appears only as Bundycoota (braided).||Mulga Downs Group.||Unconformably overlies Bulgoo Formation.||
34006|Bungaba Coal|22578|6|Mentioned|p398|||||||||
70097|Bungaba seam|22857|5|Briefly described|p526 App.1 Tb.A1.9|Late Permian|Late Permian|Included in both the State Mine Creek and Denman Formations (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
41553|Bunglegumbie unit|50616|4|Described|p280, p282|Quaternary|Quaternary|Informally named surface sandy clays and clay in the floodplain area upstream of Dubbo. Unconformably overlies: Mickety Mulga unit.  Forms part of the surface infilling of the Macquarie River valley.||||||
77774|Bungulla Granite|67818|5|Briefly described|p131, Fig. 2|Middle Triassic|Middle Triassic|Northern New England region. Rb/Sr biotite age (Shaw, 1994), U/Pb zircon SHRIMP age (Hughes, 1993).|~244.4 Ma Rb/Sr, ~247 Ma U/Pb |||||
77774|Bungulla Granite|71628|6|Mentioned|p11:8|||Flood et al. (1977). See Bungulla Monzogranite.||||||
67898|Bungulla Porphyritic Monzogranite|71628|6|Mentioned|p11: 8|||Henley et al. (2001). See Bungulla Monzogranite.||||||
82732|Bungulla Porphyritic-Adamellite|71628|6|Mentioned|p11: 8|||Robertson (1974) after Shaw (1964, unpublished). See Bungulla Monzogranite.||||||
38339|Bungulla monzogranite|23763|5|Briefly described|p543 Fig. 1|Early Triassic|Late Permian|Of the Moonbi Supersuite.   Geological Province: New England Fold Belt.||||||22-NOV-07
38339|Bungulla monzogranite|71628|6|Mentioned|p11: 8|||Mustard (2001). Informal name; see Bungulla Monzogranite.||||||
83408|Bunjeroop pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G656.|||||Magnetic response to 120 nT and shows distinct layering;  gravity response to 20 micrometres/second/second, lower to southeast.|
24792|Bunnyong Sandstone|34040|5|Briefly described|p386|||||||||
24792|Bunnyong Sandstone|34205|6|Mentioned|Table 2|||Refers McElroy & Ralph (1961)||||||
24792|Bunnyong Sandstone|37093|5|Briefly described|p233|||||||||
24792|Bunnyong Sandstone|39232|6|Mentioned|Table 1|||||||||
24792|Bunnyong Sandstone|43317|5|Briefly described|Table 1 p8|||||||||
24792|Bunnyong Sandstone|43318|14|Not recorded|opp p6||Permian|||||||
24792|Bunnyong Sandstone|43320|14|Not recorded|Table 1||Permian|Part of Illawarra Coal Measure||||||
24792|Bunnyong Sandstone|43477|14|Not recorded|p16,25,58|||Lithgow Coal Measure||||||
24792|Bunnyong Sandstone|45090|6|Mentioned|p188|||Refers Raynor (1955)||||||
35108|Bunya Bunya Formation|23055|6|Mentioned|Fig13 p25,26|||||||||17-APR-14
24793|Bunyan Leucogranite|34544|6|Mentioned|p186|||||||||
24793|Bunyan Leucogranite|40328|4|Described|p203|||||||||
24793|Bunyan Leucogranite|45003|14|Not recorded|p14,18|||||||||
38459|Burbibyong granite|24133|6|Mentioned|p57|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
24794|Burburba Formation|22857|5|Briefly described|p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Of the Fernleigh Group. Tuffaceous sediments. Max. thickness: 1.2km. Geological Province: Bindook Rise.||||||
24794|Burburba Formation|30735|2|Defined|p45|Devonian|Devonian|||||||
24794|Burburba Formation|30736|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
24794|Burburba Formation|39568|5|Briefly described|p78|||Name should be suppressed on basis that Tangerang Formation has priority||||||
24794|Burburba Formation|68592|5|Briefly described|p1096|||Felton and Huleatt (1977). Thought to overlie Windellama Limestone "probably conformably".|||||Interbedded sandstones and siltstones.|
34020|Burdekin Basalt Member|22601|6|Mentioned|407|||Underlying unit Sams Road Rhyolite Member. Member of Alum Mountain Volcanics.||||||
37418|Burgoon Subgroup|23214|6|Mentioned|p150|||Now included in the Goonigal Group.||||||
39408|Burgoon formation|24126|6|Mentioned|p207|||Informal.||||||
31238|Burindi Beds|43491|14|Not recorded|pVI/4||Tournaisian|||||||
30949|Burindi Formation""|43432|14|Not recorded|p199||Early Carboniferous|See also "Burindi Group"||||||
30950|Burindi Group""|43432|14|Not recorded|p199||Early Carboniferous|||||||
30831|Burindi Mudstone|43385|14|Not recorded|p176||Early Carboniferous|||||||
30831|Burindi Mudstone|43399|14|Not recorded|p192||Early Carboniferous|||||||
35259|Burkes Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
37400|Burley Limestone|23214|5|Briefly described|p120|||Now included as part of the Ghost Hill Formation.||||||
70470|Burnewang Ignimbrite|62095|6|Mentioned|p260 Tb. 1|Early Carboniferous|Early Carboniferous|Variation/abbreviation of Burnewang Ignimbrite Member. See also Burnewang Member.  Age: 342.4+/-3.3Ma, 343.0+/-3.0Ma, 348.9+/-2.9Ma. See also p273 Appendix.||||||31-JAN-08
70471|Burnewang Member|62095|5|Briefly described|p259 Fig. 10|Early Carboniferous|Early Carboniferous|Abbreviated form of Burnewang Ignimbrite Member. See also Burnewang Ignimbrite.||||||31-JAN-08
73706|Burnt Yards Basalt|63286|6|Mentioned|p304, p295, p302, p310|Llandovery|Llandovery|Consists of basaltic andesite to basaltic trachyandesite and is high-K calc-alkaline suite.||||||07-FEB-11
37226|Burnt Yards basalt member""|23214|6|Mentioned|p64|||Of Forest Reefs Volcanics.||||||
80052|Burra Burra Formation|70661|6|Mentioned|p7|Ordovician|Ordovician|Local unit name of Erickson, 1986 (BSc Hons), in Moss Vale area. Now included in the Adaminaby Group.||||||21-SEP-17
35524|Burra-Moko Sandstone|23218|6|Mentioned|p28|||||||||
37435|Burraga Beds""|23214|6|Mentioned|p196|||Informal. Superseded by Crudine Group.||||||
31070|Burragorang claystone|43477|14|Not recorded|p17,26,27,58,59|||Wollondilly Coal Measures||||||
35435|Burragundy Formation""|23170|6|Mentioned|p55|||||||||
35435|Burragundy Formation""|43494|6|Mentioned|p19|||Of Pickett (1982).  Informal - see Burragundy Formation.||||||
72973|Burralow Subgroup|61315|5|Briefly described|Table SY2|Middle Triassic|Early Triassic|Of the Narrabeen Group. Geological Province: Sydney Basin||||||
73747|Burranah Volcanics|63293|6|Mentioned|p474|||Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
73747|Burranah Volcanics|67847|6|Mentioned|p74|Ordovician|Ordovician|Rockley-Gulgon Volcanic Belt. Hosts structurally controlled gold. ||||||
27263|Burrandong Creek Conglomerate Member|40891|2|Defined|p10|Early Silurian|Late Ordovician|Late Ordovician to Early Silurian. Superseded by Burrandong Creek Member RDEF GOLD1608 p45.||||||
28418|Burrawong Limestone""|40328|6|Mentioned|p85|||||||||
39398|Burrawong limestone|24126|6|Mentioned|p141|||||||||
39371|Burrendong Creek Member|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27125|Burrinjuck Adamellite|29452|6|Mentioned|p219|||||||||
27125|Burrinjuck Adamellite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
27125|Burrinjuck Adamellite|30734|6|Mentioned|p54|||||||||
27125|Burrinjuck Adamellite|31015|6|Mentioned|p12|||||||||
27125|Burrinjuck Adamellite|31019|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27125|Burrinjuck Adamellite|35070|6|Mentioned|p84|||||||||
27125|Burrinjuck Adamellite|35257|6|Mentioned|p146|||||||||
27125|Burrinjuck Adamellite|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27125|Burrinjuck Adamellite|35386|3|Fully described|p60|||Early Devonian.||||||
27125|Burrinjuck Adamellite|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
27125|Burrinjuck Adamellite|36441|5|Briefly described|map legend|Pragian|Lochkovian|Intrusive. Boggy Plain I-type Suite. Adamellite, granite, aplite. Intrudes Couragago Grnodiorite. BMR map code: Dgb.||||||
27125|Burrinjuck Adamellite|38905|6|Mentioned|p305|||||||||
27125|Burrinjuck Adamellite|40328|4|Described|p204|||||||||
27125|Burrinjuck Adamellite|40882|6|Mentioned|p27|||||||||
27125|Burrinjuck Adamellite|42313|6|Mentioned|p164|||||||||
27125|Burrinjuck Adamellite|42497|5|Briefly described|Map legend|Lochkovian|Pridolian|||||||
27125|Burrinjuck Adamellite|45147|2|Defined|M283|Early Devonian|Early Devonian|See also M233||||||
24798|Burrinjuck Granite Complex""|22638|6|Mentioned|p57|||Superseded by Young Granodiorite||||||24-AUG-04
24798|Burrinjuck Granite Complex""|42313|6|Mentioned|p135|||Used 1966. Replaced by Young Granodiorite.||||||
31483|Burrinjuck Suite|42726|5|Briefly described|map legend||Silurian|Of the Boggy Plain Supersuite.  Contains the Burrinjuck Granite (informal name).||||||08-FEB-05
31483|Burrinjuck Suite|44093|5|Briefly described|p187 App. 1|Middle Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||01-MAR-05
31483|Burrinjuck Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains the Burrinjuck Granite.||||||
31483|Burrinjuck Suite|68592|3|Fully described|p1397-8, p1405-12|Early Devonian|Early Devonian|Chappell et al. (1991), named after Burrinjuck Dam. Consists of a single [!] N-S elongate pluton (Burrinjuck Granite) which is therefore the type pluton. Geochemistry described.|415 +/- 8 Ma.|Unit in Boggy Plain Supersuite.|Includes Burrinjuck Granite.||Granite with minor, marginal, aplite. I-type.|
31483|Burrinjuck Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Yass 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Burrinjuck Granite.|||
31483|Burrinjuck Suite|70540|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Burrinjuck Granite.|||
76063|Burrowang Limestone|66197|5|Briefly described|p632, p633 Fig.4c|Ludlow|Ludlow|Cowra Trough-Molong High. Deep marine redeposited limestone. Underlies the Burgoon Formation, overlies the Cary Formation [misspelling of Burrawong Limestone].||||||13-MAR-12
39395|Burrundulla Formation|24126|6|Mentioned|p138|||||||||
34287|Burrunjuck Adamellite|22691|6|Mentioned|P315, Fig2||Silurian|||||||
28420|Busches Formation""|32619|6|Mentioned|p461|||||||||
24801|Bushman Andesite|29907|2|Defined|Appendix 1|Late Ordovician|Late Ordovician|||||||
24801|Bushman Andesite|29910|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
24801|Bushman Andesite|36411|6|Mentioned|p268|||Refers Bowman 1977.||||||
24801|Bushman Andesite|39656|4|Described|Fig.1|||||||||
24801|Bushman Andesite|40136|6|Mentioned|p26|||||||||
29305|Bushman Andesite""|40891|6|Mentioned|p9|||||||||
32503|Bushman Volcanics|63278|6|Mentioned|p145 Fig. 1, p151|Silurian|Silurian|||||||07-FEB-11
32503|Bushman Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
32503|Bushman Volcanics|63283|5|Briefly described|p185 Tb. 1, p192-193, p196 Fig. 4|Early Silurian|Early Silurian|Structurally and conformably interfinger with Cotton Formation. Geological Province: Junee-Narromine Volcanic Belt. Consists of andesite lavas and lava breccias. See p192-193.||||||07-FEB-11
32503|Bushman Volcanics|70684|6|Mentioned|p3|||Probably Silurian.||||||
38858|Bushmans Volcanics""|24417|5|Briefly described|p27|||Now re-included in Nash Hill Volcanics.||||||
34280|Bushranger Andesite|22679|5|Briefly described|p 34|Devonian|Devonian|||||||
34279|Bushranger Ignimbrite""|22679|6|Mentioned|p 33|||||||||
31281|Bushy Park Rhyolite|43474|14|Not recorded|no card|||(no card)||||||
31281|Bushy Park Rhyolite|43476|14|Not recorded|Map Legend|||(Provisional Edition)||||||
34301|Butlers Granite""|22679|6|Mentioned|p 49|||Invalid name of Taylor (1983). Now called Kempfield Granodiorite.||||||08-MAR-16
35098|Buttaba Tuff|23055|6|Mentioned|p24|||||||||
34007|Buttai Coal|22578|6|Mentioned|p398, Fig.9 p399|||||||||
29237|Buttai Seam Lower|42182|6|Mentioned|p297|||||||||
31135|Buttai beds|43491|14|Not recorded|pVII/52||Permian|||||||
31073|Buttai conglomerate|43477|14|Not recorded|p12,21|||Newcastle Coal Measures. Is not equivalent to Buttai Beds||||||
39369|Byabarra beds|24124|5|Briefly described|p62|||||||||
26444|Byabbara Beds|29990|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26444|Byabbara Beds|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26444|Byabbara Beds|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26444|Byabbara Beds|32672|6|Mentioned|p674|||||||||
26444|Byabbara Beds|38803|6|Mentioned|p105|||||||||
26444|Byabbara Beds|39214|4|Described|p43|||||||||
26444|Byabbara Beds|41347|5|Briefly described|p414|||||||||
70094|Byabbara beds""|22857|6|Mentioned|p502 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Included in the Boonanghi beds. Geological Province: Tamworth Forearc Basin.||||||
74619|Byawatha Member|61964|6|Mentioned|p115|||Abbreviated version of Byawatha Conglomerate Member?  Of the Rankin Formation. ||||||
32654|Byng Rhyolite|46547|14|Not recorded|Not recorded|||||||||
40786|Bynguano Formation|50129|6|Mentioned|p28|||Probably misspelt - see Bynguano Quartzite.||||||
40786|Bynguano Formation|60287|5|Briefly described|p384|Ordovician|Cambrian|Thickness: 30 m.||||||
40786|Bynguano Formation|64685|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Equivalents of Bynguano Formation. Quartzite and quartz sandstone.||||||
40786|Bynguano Formation|66623|6|Mentioned|p148.|||Named Bynguano Quartzite and described by Warris (1967), elaborated by Pogson and Scheibner (1976), renamed the Bynguano Formation by Droser et al. (1994). Subsequently renamed Bynguano Quartzite again in this study.||||||
40786|Bynguano Formation|67322|6|Mentioned|p9|||Originally the Bynguano Quartzite of 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.||||||
28422|Byong Volcanics""|33326|6|Mentioned|p443|||Fauna.||||||
28422|Byong Volcanics""|35070|6|Mentioned|p115|||||||||
28422|Byong Volcanics""|46522|6|Mentioned|p66|||See also P68||||||
28423|C.S.A. Group|29621|6|Mentioned|Table 1|||||||||
28423|C.S.A. Group|35287|6|Mentioned|Table 1|||||||||
28423|C.S.A. Group|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
28423|C.S.A. Group|39618|6|Mentioned|Table 1|||||||||
28423|C.S.A. Group|43385|14|Not recorded|p172||Silurian|||||||
28224|C.S.A. Siltstone Member|29621|4|Described|p10|||||||||
28224|C.S.A. Siltstone Member|33123|6|Mentioned|p4|||Occurrence of some chondrites-type burrows||||||
28224|C.S.A. Siltstone Member|35185|6|Mentioned|p226|||||||||
28224|C.S.A. Siltstone Member|35287|6|Mentioned|p6|||||||||
28224|C.S.A. Siltstone Member|35383|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28224|C.S.A. Siltstone Member|35385|3|Fully described|p27|||||||||
28224|C.S.A. Siltstone Member|38367|6|Mentioned|p26|||||||||
28224|C.S.A. Siltstone Member|39618|6|Mentioned|p15|||See also Table 1||||||
28224|C.S.A. Siltstone Member|41528|6|Mentioned|p75|||||||||
32603|C.S.A. Siltstone formation|46032|14|Not recorded|p.412||Silurian|||||||
32604|C.S.A. Siltstones|46032|14|Not recorded|p.411-414||Silurian|Mineralised.||||||
24804|Cabawin Formation|22757|6|Mentioned|Table3,p9|Early Triassic|Early Triassic|Bowen Basin||||||
24804|Cabawin Formation|29385|6|Mentioned|p82|||||||||
24804|Cabawin Formation|29721|6|Mentioned|p75|||||||||
24804|Cabawin Formation|30692|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
24804|Cabawin Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
24804|Cabawin Formation|34133|6|Mentioned|p1|||See also PP28,29.||||||
24804|Cabawin Formation|36914|6|Mentioned|p90|||||||||
24804|Cabawin Formation|39212|6|Mentioned|p15|||||||||
24804|Cabawin Formation|39491|4|Described|p18|||||||||
24804|Cabawin Formation|39494|6|Mentioned|Fig.5|||||||||
24804|Cabawin Formation|39815|6|Mentioned|p445|||||||||
24804|Cabawin Formation|40030|6|Mentioned|Fig.5|||||||||
24804|Cabawin Formation|40245|6|Mentioned|Table 2|||||||||
24804|Cabawin Formation|40249|6|Mentioned|p41|||||||||
24804|Cabawin Formation|40544|6|Mentioned|Fig.6|||||||||
24804|Cabawin Formation|41188|6|Mentioned|Fig.3|||||||||
24804|Cabawin Formation|41247|6|Mentioned|p127|||See also Fig.7||||||
24804|Cabawin Formation|41535|6|Mentioned|Fig.2|||||||||
24804|Cabawin Formation|42634|5|Briefly described|Table 2 P10|||||||||
24804|Cabawin Formation|43000|6|Mentioned|p108|||||||||
24804|Cabawin Formation|43883|14|Not recorded|p18 Fig.4-3,19|||||||||
24804|Cabawin Formation|43913|14|Not recorded|p43|||||||||
24804|Cabawin Formation|43919|14|Not recorded|p28-29,36-37,39|||||||||
24804|Cabawin Formation|44091|14|Not recorded|p53||Triassic|||||||
24804|Cabawin Formation|44115|14|Not recorded|p17,22-24|||||||||
24804|Cabawin Formation|44163|4|Described|p10-13,16-18,Pl.1,4||Early Triassic|||||||
24804|Cabawin Formation|44164|4|Described|p1,13,16-7,20,26-7,|||p30,Fig.4,Pl.1||||||
24804|Cabawin Formation|44165|4|Described|p1,2,8,11,13,15-18,|||Pl.1,Fig.3. Gas.||||||
24804|Cabawin Formation|44166|14|Not recorded|p1,9,10,Pl.2|||||||||
24804|Cabawin Formation|44169|14|Not recorded|p6|||Mapped by Mack 1962. Here mapped as Rewan Formation, Clematis Sandstone, Moolayember Formation. Not known which part is equivalent to Cabawin Formation.||||||
24804|Cabawin Formation|44170|14|Not recorded|p14,17|||||||||
24804|Cabawin Formation|44545|14|Not recorded|p8|||||||||
24804|Cabawin Formation|44567|14|Not recorded|p11,14,15,Pl.2|||||||||
24804|Cabawin Formation|44568|14|Not recorded|p1,4-7,Pls.1,3|||||||||
24804|Cabawin Formation|44585|14|Not recorded|p45-Fig.2|||||||||
24804|Cabawin Formation|44605|14|Not recorded|p38|||||||||
24804|Cabawin Formation|44607|14|Not recorded|p38|||||||||
24804|Cabawin Formation|44610|14|Not recorded|p47,49,Fig.7|||||||||
24804|Cabawin Formation|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
24804|Cabawin Formation|44627|14|Not recorded|p139-141||Triassic|||||||
24804|Cabawin Formation|44840|14|Not recorded|p34|||Central Surat Basin.||||||
24804|Cabawin Formation|44852|14|Not recorded|p78||Triassic|||||||
24804|Cabawin Formation|44853|14|Not recorded|p78||Triassic|||||||
24804|Cabawin Formation|45110|3|Fully described|p77|||See also p24 and Table 13.||||||16-NOV-15
24804|Cabawin Formation|48600|2|Defined|p7-23||Triassic|Topmost formation of Bowen Group.||||||
24804|Cabawin Formation|48919|6|Mentioned|p29|||||||||
24804|Cabawin Formation|64856|4|Described|p68-69, p71, p78|Early Triassic|Late Permian|Obsolete name? of Union Oil Development Corporation (1961). Described by Mack (1963). Conglomerate, conglomeratic sandstone and mudstone. Originally described from Cabawin 1 well. These rocks included in Rewan Group in this report. Said to be Scythian age.| | ||||28-NOV-17
24804|Cabawin Formation|64857|5|Briefly described|p126|||Conglomeratic unit. Alluvial fan. Sequence G.||||||
24804|Cabawin Formation|65115|6|Mentioned|p420|||Part of Supersequence G. Conglomerate and pebbly sandstone?||||||
24804|Cabawin Formation|66615|6|Mentioned|p2|||Older company nomenclature; replaced by Rewan Formation.||||||
24804|Cabawin Formation|67402|6|Mentioned|p209|||||||Overlies the Camboon Andesite. Overlain by the Cynthia beds.||
24804|Cabawin Formation|67669|5|Briefly described|p11|Middle Triassic|Early Triassic|Of Bowen Basin.||Unit of Mimosa and Rewan groups.||Overlain by Wandoan Sandstone. Underlain by Kianga Formation. Equivalent to Clematis Formation and Rewan Formation.||
24804|Cabawin Formation|68679|5|Briefly described|p397|||Hoyling and Stewart (1964). The lithology description includes the Esk beds. Apparently reassigned to the Cynthia beds.|||||Coarse volcaniclastic conglomerate overlain by feldspathic sandstone (commonly carbonaceous), shale, siltstone and rare tuff.|
36121|Cabbannah Group|23454|5|Briefly described|p28|Silurian|Silurian|||||||
82819|Cabone Group|71600|6|Mentioned|p23 Fig 1|Ordovician|Ordovician|Geological province: Lachlan Fold Belt.|||Includes Oakdale Formation.|||
83663|Cabramurra basalt|73581|6|Mentioned|p25|||Snowy Mountains Volcanic Province. Previously named Kiandra basalt.||||||
39944|Cadia Complex|24263|5|Briefly described|p1397||Late Ordovician|Geological Province: Lachlan Fold Belt||||||
73745|Cadia Far East Monzonite|63293|6|Mentioned|p471|||Age: 437.1+/-3.5Ma (Squire and Crawford 2007).||||||07-FEB-11
39647|Cadia Hill Monzodiorite|24398|6|Mentioned|p268|Ordovician|Ordovician|[Mentioned in acknowledgements only].  Geological Province: Lachlan Fold Belt.||||||
37228|Cadia Hill Monzonite intrusive suite|23214|5|Briefly described|p86|||Informal name.||||||
83284|Cadia Igneous Complex|73154|5|Briefly described|p79, p84|||||||Intrudes Forest Reefs Volcanics|Strongly zoned from cumulate gabbroic and monzodiorite to quartz monzonites and very minor syenogranitic aplite and pegmatite veins.|
67990|Cadia Intrusive Complex|24518|6|Mentioned|p68|||||||||
67990|Cadia Intrusive Complex|60443|5|Briefly described|p761|Early Silurian|Late Ordovician|Shoshonitic intrusions ranging from diorite to aplite, including monzonite and quartz monzonite. Geological Province: Lachlan Fold Belt.||||||
67990|Cadia Intrusive Complex|62478|5|Briefly described|p88-89|Ordovician|Ordovician|Gabbroic to monzodioritic, quartz monzonites, syenogranitic aplite and pegmatites. Age inferred from text.||||||
67990|Cadia Intrusive Complex|63278|5|Briefly described|p156|Early Silurian|Late Ordovician|Age: 439+/-6Ma (U/Pb SHRIMP). Consists of monzonite to monzodiorite bodies. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
67990|Cadia Intrusive Complex|63286|6|Mentioned|p300-301|Late Ordovician|Middle Ordovician|Age: 445+/-6Ma (L.P. Black pers. Comm), 456+/-10Ma (Perkins et al. 1992). Age of crystallisation is 437.1+/-3.5Ma.||||||07-FEB-11
67990|Cadia Intrusive Complex|63293|6|Mentioned|p475|||||||||07-FEB-11
67990|Cadia Intrusive Complex|67106|6|Mentioned|p673, 676, 681|||Molong Volcanic Belt.||||||
67990|Cadia Intrusive Complex|67107|6|Mentioned|p689-690, 698-701|||Located 20km S of Orange. Spatially associated with numerous major Au-Cu deposits. Likely the single source of Cu and Pb ores in the Cadia deposits. The most evolved suite studied in this article. Earlier radiometric dating doubtful due to inherited zircons.||||Intrudes Weemalla Formation and Forest Reefs Volcanics.|Compositions range from diorite to quartz syenite. High-K calc-alkaline to shoshonitic chemistry.|
67990|Cadia Intrusive Complex|67821|6|Mentioned|p157|Early Silurian|Ordovician|||||||08-FEB-18
67990|Cadia Intrusive Complex|70297|6|Mentioned|on side 2 of map sheet|||Shown as "Cadia Intrusive Complex". Hosts world class Cadia porphyry Au-Cu system.|c. 440-437 Ma|||||
67990|Cadia Intrusive Complex|73154|5|Briefly described|p78 Tb.1|Llandovery|Late Ordovician|Molong structural belt. 441.4+/-2.9 Ma age from Cadia monzonite sample p89 Tb.2, shown as from Cadia Intrusive Complex p78 Tb.1, referred to as Cadia monzonite p83-84, p89 Tb.2, p90, p92 Fig.8.|441.4+/-2.9 Ma zircon U-Pb||||Includes monzonite.|
39648|Cadia Monzonite|24398|5|Briefly described|p267, p259 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
39648|Cadia Monzonite|63286|6|Mentioned|p304|Ordovician|Ordovician|Renamed as the Cadia Intrusive Complex.||||||07-FEB-11
39648|Cadia Monzonite|63293|5|Briefly described|p471|||Intrudes Forest Reefs Volcanics. Age: 439+/-6Ma (OZCHRON).||||||07-FEB-11
73746|Cadia Quarry monzonite|63293|6|Mentioned|p471|||Informal. Age: 438+/-2.7Ma (Foster et al. 2004).||||||07-FEB-11
24805|Cadia monzodiorite complex|35374|6|Mentioned|p68|||||||||
73656|Cadia monzonite|63292|6|Mentioned|p458 Fig. 9|||Informal name; mis-spelt.||||||15-FEB-16
73656|Cadia monzonite|73154|6|Mentioned|p83-84, p89 Tb.2, p90, p92 Fig.8|Llandovery|Late Ordovician|Cadia monzonites on p84.|441.4+/-2.9 Ma zircon U-Pb|||||
37461|Cadiangullong pophyry|23214|6|Mentioned|p v (index)|||Misspelt - see Cadiangullong Porphyry.||||||
39368|Cairncross Adamellites|24124|5|Briefly described|p3|||||||||
34366|Cairncross Granite|22736|6|Mentioned|p623|||misspelled reference to Caincross Adamellite||||||
34366|Cairncross Granite|71628|6|Mentioned|p17:55|||Roberts et al. (1995). Previously the Cairncross Adamellite. Now Cairncross Monzogranite.||||||
82733|Cairncross Suite|71628|5|Briefly described|p17:56|||||Glen Esk Supersuite.|Cairncross Monzogranite.|||
39381|Calaire Sandstone|24125|5|Briefly described|p61|Silurian|Ordovician|Geological Province: Lachlan Fold Belt.||||||
35954|Calavil Formation|23365|5|Briefly described|8|Tertiary|Tertiary|||||||
33991|Calc-silicate Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
33991|Calc-silicate Suite|23869|5|Briefly described|p13|||Not a formal name.||||||
33991|Calc-silicate Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
33991|Calc-silicate Suite|24592|5|Briefly described|p635|||Overlain by the Pelite Suite. Overlies the Quartzo-feldspathic Suite. Of the Willyama Supergroup. Geological Province: Curnamona Province. Interbedded calc-silcate & albitic siltstone. A magnetic susceptibility division of the Willyama Supergroup.||||||
35212|Caley Subgroup|22969|5|Briefly described|Fig 2.2||Early Triassic|Narrabeen Group||||||
35212|Caley Subgroup|60281|5|Briefly described|Fig. 7 Appendix 1|Early Triassic|Early Triassic|Of the Narrabeen Group.  Age: ~250Ma.  Geological Province: Sydney Basin.||||||
35212|Caley Subgroup|69297|6|Mentioned|p501|Olenekian|Induan|Sydney Basin. ||Narrabeen Group||Overlies the Illawarra Coal Measures. Overlain by the Grose Subgroup.||
77040|Callaghan Creek Tonalite|71628|6|Mentioned|p7: 15|||Originally Back Creek Complex of Binns et al. (1967) after Flood (1964). Later referred to as Back Creek Tonalite (Flood, 1971). Both names invalid as Back Creek Group had priority. Consequently renamed as Callaghan Creek Tonalite (DMR NAND04 Nandewar Geology Integration and Upgrade project), and again renamed in this study as Callaghans Creek Quartz Monzodiorite to more accurately reflect the geographic feature's name and the composition of the intrusion.||||||
82374|Callaghans Creek Suite|71628|5|Briefly described|p7: 16|||||Moonbi Supersuite.|Callaghans Creek Quartz Monzodiorite.|||
37775|Calliope Volcanics|24168|5|Briefly described|p643 Tb 1|Late Devonian|Late Devonian|||||||
40285|Callivil Formation|24574|6|Mentioned|p705|||Geological Province: Murray Basin||||||
38950|Caloma Sandstone""|24417|6|Mentioned|p136|||||||||
68029|Calpe Ignimbrite Member|50613|2|Defined|p227 App. 1|Late Carboniferous|Late Carboniferous|Of  Willuri Fm. Volcanic member of the Kaputar package (informal grouping of stratigraphically recognisable distinctive, mappable units). Max.thickness: 40m. Geol.Prov: New England Orogen. See also name variation - The Calpe Ignimbrite Member.||||||22-FEB-05
24207|Cambalong Complex|23321|5|Briefly described|p430 Fig.2|||||||||07-FEB-07
24207|Cambalong Complex|41563|6|Mentioned|p508|||||||||
24207|Cambalong Complex|43233|5|Briefly described|Map Legend|Ordovician||||||||
24207|Cambalong Complex|43577|6|Mentioned|p381|||||||||
24207|Cambalong Complex|60988|6|Mentioned|p147|||One of five fault-bounded metamorphic Complexes in the Eastern Metamorphic Belt of the SE Lachlan Fold Belt. Occurs 6km to the E of Quidong Basin. See reference to Cambalong Metamorphic Complex (p144 Fig.1).||||||
24207|Cambalong Complex|65779|4|Described|p287-291, Fig. 1, Fig. 2|Silurian|Late Ordovician|Elongate, N-S trending area of regional metamorphism (probable Silurian), 7km wide, >25 km long. Developed in Bombala Beds. Lower grade schists and phyllites on either side of central belt of schists and gneisses. Some basalt and sediment cover.||||||
30864|Cambewarra flow|43346|14|Not recorded|p2|||||||||
31069|Cambewarra latite|43477|14|Not recorded|p19,41||Permian|Included in Gerringong Volcanics||||||
26450|Camboon Granite|42726|5|Briefly described|map legend|Carboniferous||4. Not a variation on Camboon Andesite, NSW & Qld.||||||
74657|Cambroon basalt|24040|5|Briefly described|p486|Early Permian|Early Permian|Probably not intended as a formal name.  In the New England Fold Belt.  Associated with Cedarton basalt.||||||21-AUG-08
70095|Camden Head Claystone Member|22857|4|Described|p538 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Camden Haven Group (at Grants Head). Red-brown claystone and siltstone, less grey plant-bearing siltstone, sandstone and conglomerate. Geological Province: Lorne Basin.||||||
26451|Camden Sub-group|31725|6|Mentioned|p12|||||||||
26451|Camden Sub-group|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
26451|Camden Sub-group|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
26451|Camden Sub-group|43318|14|Not recorded|opp p6||Late Triassic|||||||
26451|Camden Sub-group|43319|14|Not recorded|Map Legend|||||||||
26451|Camden Sub-group|43320|14|Not recorded|Table 1 p14||Late Triassic|||||||
30643|Camden Subgroup|43317|4|Described|Table 1 p14|||||||||
24810|Camden sub-Group|32187|6|Mentioned|p6|||||||||
26452|Camels Humps Quartzite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
26452|Camels Humps Quartzite|22857|4|Described|Tb 13.1 (insert p70), p400 App.1 Tb A1.3|Marinoan|Marinoan|Of the Farnell Group. Well-bedded, silicified quartzite, minor shale. Age: ~580Ma. Max. thickness: 332m. Geological Province: Adelaide Fold Belt. ||||||
26452|Camels Humps Quartzite|30261|6|Mentioned|Table 1|||||||||
26452|Camels Humps Quartzite|34563|4|Described|p66|||||||||
26452|Camels Humps Quartzite|34812|3|Fully described|p104|||||||||
26452|Camels Humps Quartzite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26452|Camels Humps Quartzite|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26452|Camels Humps Quartzite|39214|5|Briefly described|p9|||||||||
30807|Campbell's Group|43384|14|Not recorded|Map Legend||Silurian|||||||
30807|Campbell's Group|43385|14|Not recorded|p171,172||Early Silurian|Ref. to Stanton 1955||||||
30807|Campbell's Group|43469|4|Described|p131-33,135,142-44||Early Silurian|May be Upper Ordovician||||||
24812|Campbells Hill Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
24812|Campbells Hill Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24812|Campbells Hill Adamellite|35257|6|Mentioned|Fig.17|||||||||
24812|Campbells Hill Adamellite|43091|5|Briefly described|Map Legend|||||||||
24812|Campbells Hill Adamellite|71628|6|Mentioned|p7: 37, 40, 49-50|||Chesnut et al. (1973) after unpublished work by Flood (1971). Subsequently renamed Campbells Hill Monzogranite by Brown (2003) after unpublished work by Chappell and Bryant (1994). In this study it becomes Campbells Hill Monzogranite Phase (of Walcha Road Monzogranite).||||||
41053|Campbells Hill Monzogranite|24366|6|Mentioned|p21 Fig. 12|||||||||
41053|Campbells Hill Monzogranite|68005|5|Briefly described|p67, p133.|Permian|Permian|Listed on p.134 as a unit in Moonbi Supersuite.||Unit in Southern Moonbi Supersuite.|||Approximately equigranular biotite leucomonzogranite and monzogranite.|
41053|Campbells Hill Monzogranite|71628|6|Mentioned|p7: 37, 49|||Originally Campbells Hill Adamellite of Chesnut et al. (1973) after unpublished work by Flood (1971). Subsequently renamed Campbells Hill Monzogranite by Brown (2003) after unpublished work by Chappell and Bryant (1994). In this study it becomes Campbells Hill Monzogranite Phase (of Walcha Road Monzogranite).||||||
31984|Campbells/Kildrummie Group|22679|6|Mentioned|p 27|||||||||
31984|Campbells/Kildrummie Group|42712|4|Described|5,8,19|Devonian|Silurian|Name invalidly made up of 2 of the component formations, the Campbells & Kildrummie Fms.  Unconformable on Rockley Volcanics.||||||
26454|Campfire Adamellites|30911|6|Mentioned|Map legend|Permian|Permian|||||||
82734|Campfire Suite|71628|6|Mentioned|p3: 26||||||Campfire Monzogranite.|||
82378|Campground Granodiorite|71628|5|Briefly described|p2: 46-48, 52-53, 55, 58-59|||Named but unpublished by Paul (1984). A small (1.0 km2), irregularly-shaped unit at the SE of the parent Complex. Geochemistry described; contrasted with Dundurrabin Granodiorite.||Sheep Station Creek Complex.||Intrudes Moombil Siltstone. Is intruded by Collett Monzogranite.|A contaminated I-type granite: medium- to fine-grained amphibole-biotite granodiorite.|
79255|Canah Creek Tuff|64631|6|Mentioned|p51.|Bashkirian|Bashkirian|Lower in succession than Taggarts Mountain Ignimbrite (316.1 Ma). See also discussion p54.||Unit in Currabubula Formation||||
27359|Canangle Sub Group|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27359|Canangle Sub Group|32865|6|Mentioned|p483|||Late Dev. - early Carb.||||||
27359|Canangle Sub Group|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27359|Canangle Sub Group|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
27359|Canangle Sub Group|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Unit of Catombal Group||||||
27359|Canangle Sub Group|43516|14|Not recorded|Map Legend||Late Devonian|||||||
39444|Canangle sub-group|24126|6|Mentioned|p198|||See Canangle Subgroup.||||||
39393|Canangle subgroup|24126|6|Mentioned|p135|||Informal name.  Of the Catombal Group.||||||
70420|Canaway silcrete profile|61007|5|Briefly described|p296|Late Oligocene|Eocene|Formed by the truncation and re-weathering of the Morney silcrete profile. See also Canoway profile - names used interchangeably. In the Clarence-moreton Basin area.||||||
28430|Canbelego Series|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
28430|Canbelego Series|39618|6|Mentioned|Table 2|||||||||
31046|Canberra Beds|44970|14|Not recorded|p24,32|||See also Lexicon||||||26-JUN-09
31047|Canberra Series|44970|14|Not recorded|p24|||See also Lexicon||||||
39419|Canberra formation|23309|6|Mentioned|p390|||||||||
39419|Canberra formation|24128|5|Briefly described|p3|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
79137|Candello Suite|69270|5|Briefly described|p16, p20, p23, p30, p34|Early Devonian|Early Devonian|The new age for Anembo Granodiorite (412.7+/-1.9 Ma, n = 24, magmatic crystallisation age) also confirms that all plutons assigned by Chappell et al. (1991) to Glenbog and Candello Suites have indistinguishable Early Devonian ages (to the extent of available U-Pb zircon data).||||||
79137|Candello Suite|71069|6|Mentioned|p135|Early Devonian|Early Devonian|See also Candelo Suite p43, 195 and ref to  'plutons of the Candello and Arthursleigh supersuites' p43.||||Intrudes the Mount Fairy Group.||22-SEP-17
24814|Candelo Granite|42726|5|Briefly described|map legend|Early Devonian||118.  Of the Candelo Suite (Candelo Supersuite).  Not intended as a formal name. Reserved as Candelo Tonalite.||||||09-FEB-05
35268|Cane Point Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
80473|Canella beds|70210|5|Briefly described|p1, p24, p27-p28, p40-41|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district. Age is derived from a tuff in this unit. Occasionally (eg p38) presented as Canella Beds. Also 508.2 +/- 3.3 Ma, and a weighted mean age of 509.4 +/- 7.5 Ma are also given.|508.3 +/- 2.2 Ma (preferred).|Ponto Group.|||Includes tuff.|11-APR-18
70092|Cann River beds|22857|6|Mentioned|p213|Late Devonian|Late Devonian|||||||
73610|Cannela beds|63489|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Very deformed phyllite. minor sandstone, silicic tuff.||||||10-SEP-07
73610|Cannela beds|66623|6|Mentioned|p88.|||Term used by Mills (2003) for rocks previously part of Wonominta beds (Warris 1967). Redefined as Cannela Formation in this study.||||||
73610|Cannela beds|66933|5|Briefly described|Map legend|Cambrian|Cambrian|Milparinka Zone, Delamerian Fold Belt.|||||Phyllite, cleaved metasandstone, turbiditic metasandstone and abundant very fine rhyolitic tuffs of cherty appearance.|
82735|Cannon Creek Monzogranite Phase|71628|5|Briefly described|p15: 35, 99, 102-104, 115|||This subunit does not ""technically"" qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.",,||Severn River Monzogranite.||Abuts Ruby Creek Leucogranite, Amiens and Donnellys Castle Leucomonzogranites.|Contains scattered lenses, pipes or pods of vuggy pegmatite up to 40 cm across.|
24815|Canobolas trachyte|40586|6|Mentioned|p388|||||||||
34606|Cappanana Beds""|22815|6|Mentioned|p38|||Changed to Cappanana Formation.||||||
27362|Cappanana Group|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
24819|Cappanana beds|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24819|Cappanana beds|37728|4|Described|Table 2|||||||||
70008|Captain Rocks formation|61766|6|Mentioned|p68|Late Devonian|Middle Devonian|Informal name. Volcaniclastic sediments and minor basalt flows.||||||
32636|Captain's Flat Group|46568|14|Not recorded|p.423,424||Silurian|(I55-16/Michelago). Middle-Upper Silurian.||||||
80083|Captains Flat Group|71069|6|Mentioned|p100|||Of Glasson & Paine (1965). Junior synonym of the Hoskinstown Group.||||||22-SEP-17
34297|Carcoar Granite""|22679|6|Mentioned|p 46|||||||||
34302|Carcoar Suite|22679|6|Mentioned|p 50|||||||||
34302|Carcoar Suite|23214|6|Mentioned|p171|||Mafic I-type composition.||||||
36124|Carcoar granite|23454|5|Briefly described|p32|Silurian|Ordovician|425+/-4.7Ma||||||
30993|Cardiff Subgroup|43448|14|Not recorded|p224,226,235|||Incl. Kotara, Highfields, Kahibah and Tickhole Formations||||||
39403|Carey Beds|24126|5|Briefly described|p158|||||||||
74620|Cargelligo beds|61964|6|Mentioned|p64, p68|||Superseded "Cargelligo Group" in 1970s and 1980s usage in describing an Ordovician-Silurian turbiditic sequence of sericitic quartz sandstone and siltstone. Written as "Cargelligo beds". See also p232.||||||27-OCT-08
74200|Cargelligo magnesite""|61964|3|Fully described|p196|||Not intended as a formal name. Hosted by deeply weathered turbiditic metaseds. of Wagga Group and overlying residuum. V.pure white to near-white, v.fine-gr.to mostly microcrystalline, massive to nodular, hard to compact, carbonate. ||||||
74200|Cargelligo magnesite""|62405|5|Briefly described|Map legend|Cenozoic|Cenozoic|Residual and replacement magnesite-rich pedogenic carbonate and in situ bedrock fragments locally capped by colluvial pedogenic magnesitic carbonate.||||||03-NOV-15
74200|Cargelligo magnesite""|69164|5|Briefly described|Map legend|Quaternary|Quaternary||||||Residual and replacement magnesite-rich regolithic carbonate and in-situ bedrock fragments within saprolitic bedrock, locally capped by mobile pedogenic magnesite-rich carbonate in soil profile.|
35418|Cargo Andesite""|23170|6|Mentioned|p37|||||||||
35418|Cargo Andesite""|23213|6|Mentioned|p16|||Outcrop of Wahringa Limestone Member initially plotted as occurring in the Cargo Andesite, now Fairbridge Volcanics.||||||
35418|Cargo Andesite""|63278|6|Mentioned|p153|||Superseded into Fairbridges Volcanics.||||||07-FEB-11
37469|Cargo Intrusive Complex|23214|5|Briefly described|p344|Late Ordovician|Late Ordovician|Intrudes Fairbridge Volcanics.|||||Dacitic intrusives.|05-APR-20
37469|Cargo Intrusive Complex|24398|6|Mentioned|p259 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
37469|Cargo Intrusive Complex|73154|5|Briefly described|p78 Tb.1|Darriwilian|Floian|Molong structural belt. Syn-mineralisation age of 471.4+/-2.7 Ma from Cargo dacitic porphyry, post-mineralisation age of 466.3+/-3.4 Ma from Cargo monzodiorite, zircon U-Pb dating. Porphyry and monzodiorite samples shown as from the Cargo Intrusive Complex, samples also referred to in text as Cargo monzonite p92, Cargo monzonite porphyries p80, Cargo dacitic porphyries p91, Cargo intrusives p92.|471.4+/-2.7 Ma, 466.3+/-3.4 Ma zircon U-Pb||||Includes quartz monzonite porphyry, monzonite.|
35489|Cargo Volcanics""|23213|5|Briefly described|p13|||of Stevens 1950, now included in Fairbridge Volcanics.||||||
37463|Cargo dacite complex""|23214|5|Briefly described|p83|Ordovician|Ordovician|See also page 85. Informal name.||||||
37463|Cargo dacite complex""|24398|6|Mentioned|p262|Ordovician|Ordovician|Informal name.  Geological Province: Lachlan Fold Belt.||||||
37463|Cargo dacite complex""|63287|6|Mentioned|p332|||Informal and superseded name by Paffard, 1992. Apparently now included in the Cargo Volcanics.||||||05-APR-20
73713|Cargo intrusive complex""|63287|6|Mentioned|p332|||Informal and superseded name by Paffard, 1992. Apparently now included in the Cargo Volcanics.||||||05-APR-20
83287|Cargo porphyries|73154|5|Briefly described|p79, p92|Katian|Early Ordovician|Age estimated by Simpson et al., (2007) based on dating of detrital zircon in overlying sediments assumed to be derived from the dacite or monzonite phase of the Cargo porphyries. Sample LON 4 dated herein gave an age of 470.0+/-3.2 Ma using U-Pb zircon SHRIMP.|453.0+/-4.1 Ma||||Porphyries with dacite and monzonite phases.|
39401|Carinya shale|24126|6|Mentioned|p141|||||||||
79338|Carnangle Subgroup|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|[Misspelling of Canangle Subgroup.]||Catombal Group||||
34031|Carnot gneiss|22603|5|Briefly described|p96||Archean|2600 Ma||||||07-NOV-08
34031|Carnot gneiss|69876|6|Mentioned|p313, p315|Archean|Archean|87Sr/86Sr ratios discussed.||||||
81174|Caro Schist|72296|5|Briefly described|p9|||Smith (1973). Girilambone mine area. See p9 for the evolving use of this name. |||Pink Quartzite Member.|Overlain conformably by Tritton Formation. Equivalent to Wilga Downs Metamorphics.|Metasedimentary rocks.|
69994|Caroda Formation, upper|61767|6|Mentioned|p74|||Informal - see Caroda Formation.||||||
77255|Caroona Seam|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Informal name? Within Benelabri Mudstone Member (Clare Sandstone, Coogal Subgroup, Black Jack Group)||||||
77255|Caroona Seam|68004|5|Briefly described|p150, p152.|||Mullaley Sub-basin, Gunnedah Basin. In the Caroona area, this unit converges with the Hoskissons Seam to form a seam up to 15 m thick, with a consistent 3 to 4.5 m dull to bright banded working section across the area. Described in some detail.||||||
70093|Caroona seam|22857|6|Mentioned|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for coal seam in the Benelabri Formation (Black Jack Group).||||||
42327|Carpathia group|24271|6|Mentioned|p1634|||Geological Province: Lachlan Fold Belt.||||||07-DEC-04
42328|Carpathia-Blackreef group|24271|6|Mentioned|p1635|||Geological Province: Lachlan Fold Belt.||||||
28439|Carrai Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28439|Carrai Adamellite|35257|6|Mentioned|p82|||||||||
28439|Carrai Adamellite|40245|6|Mentioned|Fig.2|||||||||
28439|Carrai Adamellite|71628|6|Mentioned|p17:19|||Pogson and Hitchins (1973), after unpublished work by Atkinson et al. (1969). Appeared as a mis-spelling (Corrai Adamellite) in Leitch et al. (1971). Now the Carrai Granodiorite.||||||
73981|Carrai Suite|69639|6|Mentioned|p118|||||Round Mountain Supersuite|Includes the Carrai Granodiorite.|||
73981|Carrai Suite|71628|6|Mentioned|p17:21|||||Carrai Supersuite.||||
38227|Carramere Coal|23717|5|Briefly described|p118 Fig.2|Permian|Permian|||||||
68030|Carramundra bed b|50613|6|Mentioned|p207 Tb. 1|||Informally named ignimbrite within the Carramundra Member (one of three beds - a, b and c) separated by volcanolithic sandstone and conglomerate.  See also p228 Appendix 1.||||||
40436|Carrawandool Volcanics|24580|5|Briefly described|p828|Emsian|Emsian|Age: 403.2 +/- 2.1 Ma. Geological Province: Eastern Lachlan Fold Belt.||||||
82736|Carrolls Creek Monzogranite Phase|71628|4|Described|p11: 4; 15: 35, 52, 55, 60, 62-65, 68|Middle Triassic|Early Triassic|See also p15: 71, 82, 115. New unit, after a local watercourse; differentiated geochemically. This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Previously part of Stanthorpe Monzogranite. Crops out along Mount Lindesay Highway, N and S of Carrolls Creek; extent unknown. Geochemistry described. Is geochemically assigned to Carrolls Creek Suite.||Mount Lindesay Monzogranite.||Likely abuts Jenners Monzogranite and other 'Phases' of the parent unit.|High-K granite. A-type to borderline I-A type.|
82737|Carrolls Creek Suite|71628|6|Mentioned|p15: 35|Middle Triassic|Early Triassic|The Carrolls Creek Monzogranite Phase (of Mount Lindesay Monzogranite) is geochemically assigned to this Suite.||||||
41388|Carsonville Formation""|44244|6|Mentioned|p131|||Informal name.  Of Peou and Engel (1979).  Superseded by Conger Formation.||||||
76808|Cartwrights Creek Formation|64742|6|Mentioned|pp329-330.|||Mis-named for Cartwrights Creek Metasediments (see p321 Fig.3).||||||29-MAR-12
76808|Cartwrights Creek Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Curnamona Province. [Unclear whether this unit is referred to as the Cartwrights Creek Metasediments (current) or Cartwrigths Creek Formation (misspelling)]|ca 1650 Ma|||Overlies the Sundwon Group.|Siltstone, carbonaceous shale and dolomite.|
27736|Carwell Creek Beds|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
27736|Carwell Creek Beds|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||29-SEP-04
27736|Carwell Creek Beds|32046|6|Mentioned|p277|||||||||
27736|Carwell Creek Beds|32485|6|Mentioned|Map legend|Devonian|Silurian|||||||
27736|Carwell Creek Beds|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
27736|Carwell Creek Beds|34059|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Silurian - L.Devonian||||||
27736|Carwell Creek Beds|36285|4|Described|p57|||See also Fig.2.& 3.||||||
27736|Carwell Creek Beds|37727|5|Briefly described|p44|||||||||
27736|Carwell Creek Beds|40328|5|Briefly described|p136|||||||||
27736|Carwell Creek Beds|42379|6|Mentioned|p208, Fig.2 p202|||Superseded ? herein by Carwell Creek Formation.||||||
27736|Carwell Creek Beds|43476|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
29787|Carwell Creek beds|23214|6|Mentioned|p205|||Replaced by Carwell Creek Formation.||||||
29787|Carwell Creek beds|43043|4|Described|p95|||see also Fig.2 p93||||||
70472|Castle Mountain Tuff Member|62095|6|Mentioned|p274 Appdx.|||Of Cherry (1987). Superseded by White Rocks Tuff Member of Dawson (1988) and Davies (1988) and now White Rocks Ignimbrite Member.||||||25-MAY-06
70472|Castle Mountain Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
70472|Castle Mountain Tuff Member|68005|6|Mentioned|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
28443|Cataract River Formation|29440|6|Mentioned|p38|||||||||
28443|Cataract River Formation|32944|6|Mentioned|p709|||Permian||||||
28443|Cataract River Formation|32945|6|Mentioned|p90|||||||||
28443|Cataract River Formation|33436|2|Defined|Fig.1|Permian|Permian|||||||
28443|Cataract River Formation|33476|6|Mentioned|Table 1|||||||||
28443|Cataract River Formation|33702|6|Mentioned|p223|||Trilobites.||||||
28443|Cataract River Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
28443|Cataract River Formation|34340|6|Mentioned|Table 6.1|||Permian||||||
28443|Cataract River Formation|34350|6|Mentioned|p17|||Permian||||||
28443|Cataract River Formation|34556|4|Described|p268|||||||||
28443|Cataract River Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
28443|Cataract River Formation|43318|14|Not recorded|p6-7,9|||||||||
28443|Cataract River Formation|43385|14|Not recorded|p179,180||Kungurian|||||||
28443|Cataract River Formation|43881|14|Not recorded|p6-7,9|||||||||
28443|Cataract River Formation|48940|6|Mentioned|p46|||Refers Voisey (1957)||||||
33672|Cathcart Adamellite|22815|4|Described|p85|||||||||
33672|Cathcart Adamellite|23329|6|Mentioned|1043|||||||||
33672|Cathcart Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Cathcart Suite.||||||
31258|Catombal Formation""|43512|14|Not recorded|p76|||Nomenclature change to Group and sub-division to two Sub-Groups (as suggested by Joplin 1952)||||||
35442|Catombal Park Formation""|6969|5|Briefly described|p12|Middle Silurian|Middle Silurian|Replaced by Bell River Member of the Dripstone Formation.  Geological Province: Lachlan Fold Belt.||||||
35442|Catombal Park Formation""|23170|6|Mentioned|p81|||Renamed the Bell River Member.||||||
35442|Catombal Park Formation""|23225|6|Mentioned|p12|||Superceded by Bell River Member. of Lachlan Fold Belt.||||||
28445|Cavan Bluff "Stage"|33325|5|Briefly described|Table 4|||||||||
68818|Cavan Formation, upper|50077|6|Mentioned|p9|||Informal - see Cavan Formation.  Found at Taemas.||||||
30746|Cayley Formation|23218|6|Mentioned|p28|||||||||
30746|Cayley Formation|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
74658|Cedarton basalt|24040|5|Briefly described|p484|Early Permian|Early Permian|Not intended as a formal name. In the New England Fold Belt. Associated with the Cambroon basalt.||||||21-AUG-08
41272|Cemetery Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Medium grained muscovite granite.  Intrudes: Kirribilli Formation.||||||05-JUL-04
69587|Central Province Volcanics|61155|5|Briefly described|p19|Early Miocene|Early Oligocene|In the Inverell area.||||||
69587|Central Province Volcanics|70036|5|Briefly described|Map legend|||Included in a mapped unit of Tertiary volcanic rocks: trachyte, basalt, nephelinite, syenite, rhyolite, monzonite and tuff. Appears as Central Province.||||||
26472|Chaelundi Adamellite|29988|6|Mentioned|Map legend|Permian|Permian|||||||
26472|Chaelundi Adamellite|71628|5|Briefly described|p2: 46-47; p17:90|||Brunker and Chesnut (1976), after work by Binns et al. (1967) and (unpublished) Paul (1984). Geochemically distinct from Chaelundi Complex, and the rocks are herein assigned to the Gumtree Monzogranite.||Sheep Station Creek Complex.||||
41353|Chaelundi Granite|60079|5|Briefly described|Map Legend|Permian|Permian|Leucocratic biotite granite.||||||
41353|Chaelundi Granite|71628|6|Mentioned|p17:90|||Babaahmadi and Rosenbaum (2013). Now Chaelundi Complex.||||||
78525|Chaelundi Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Carnian|Ladinian|Mis-spelt in Table 1 as Leucomonnzogranite. Also dated at 235-232 Ma (Rb-Sr biotite; Shaw 1994).|233 +/- 3 Ma; U-Pb zircon (Phillips et al. 2011).|||||
33678|Chakola Formation|22815|3|Fully described|p23, fig10|Early Ordovician|Early Ordovician|Upper Adaminaby Group||||||
33678|Chakola Formation|22857|4|Described|p422 App. 1, Tb. A1.5|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Typical turbidite sequence; contains graptolites, conodonts, radiolaria. Max. thickness: 400m. Geological Province: Monaro Forearc Basin. ||||||
33678|Chakola Formation|24037|6|Mentioned|p424|||Geological Province: Lachlan Fold Belt||||||
33678|Chakola Formation|43233|6|Mentioned|Map Legend||Darriwilian|of Adaminaby Group.||||||
33678|Chakola Formation|67322|4|Described|p15, p20 Fig.5|Sandbian|Darriwilian|Glen (1994). Here left ungrouped. Approximately 300-400m thick. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Cooma-Monaro region.|||Glen Fergus Member|Overlies the Numeralla Chert (Adaminaby Group) conformably. Overlain conformably by the Sunlight Creek Formation (Bendoc Group).|A thin succession of interbedded sandstone, siltstone and slate.|21-FEB-18
33678|Chakola Formation|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.|||Glen Fergus Member.|||
33678|Chakola Formation|68592|5|Briefly described|p272, p282|||Cooma area.||Unit in Adaminaby Group.|Includes Glen Fergus Member.|Overlies Numeralla Chert.||
33678|Chakola Formation|69541|5|Briefly described|p652|Late Ordovician|Late Ordovician|Cooma area. Age is early Gisbornian.||Topmost unit in Adaminaby Group.||||
33678|Chakola Formation|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Cooma-Bega area, Albury-Bega terrane.||||Overlies Numeralla Chert. Is overlain by Warbisco Shale.||
33678|Chakola Formation|70601|5|Briefly described|p27, p43|Gisbornian|Gisbornian|Albury-Bega Basin: Inland Zone. Shown as part of Bendoc Group on p43.||Adaminaby Group.||Overlies Numeralla Chert, Adaminaby Group. Underlies Warbisco Shale transitionally.|Thin cross-laminated quartzitic silt.|
33678|Chakola Formation|71069|6|Mentioned|p52, p58, p78, p79, p84|||||Adaminaby Group|Includes the Glen Fergus Member|Overlies the Numeralla Chert.||
33678|Chakola Formation|71700|6|Mentioned|CD|||||Adaminaby Group||||
33678|Chakola Formation|73140|6|Mentioned|p495 Fig.3|||Proposed to be superseded and replaced by the Abercrombie Formation.||||||
34601|Chakola Group""|22815|6|Mentioned|p37|||Proposed name to group the Cappanana Formation and Colinton Volcanics.||||||
30649|Chalybeate Spring Deposits|43346|2|Defined|p4|||||||||19-JAN-10
31250|Chambers Creek Granite|43517|14|Not recorded|map plate XII|||Possibly a mistake - Should be Bruinbun Granite?||||||
41391|Champion Suite|50606|5|Briefly described|p1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Mundi Mundi Suite. Geological Province: Broken Hill Block.||||||07-NOV-08
41389|Champion granite|50606|5|Briefly described|p5.16|||Geological Province: Broken Hill Block.||||||
38226|Charton Formation|23717|5|Briefly described|p118 Fig. 2|||Misspelt - see Charlton Formation.||||||
73678|Cheesemans Creek Formation, lower|63278|6|Mentioned|p145 Fig. 1, p146 Fig. 2a, |Late Ordovician|Late Ordovician|Informal name. Geological Province: Molong Volcanic Belt, Lachlan Fold Belt.||||||07-FEB-11
73679|Cheesemans Creek Formation, upper|63278|6|Mentioned|p145 Fig. 1|||Consists of breccias. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
73715|Cheesemans Creek Volcanics|63287|6|Mentioned|p335|||Non current name.||||||07-FEB-11
28192|Cheitmore Limestone|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Limestone. BMR map symbol: Suh.||||||
28192|Cheitmore Limestone|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
28192|Cheitmore Limestone|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
28192|Cheitmore Limestone|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
28192|Cheitmore Limestone|33325|6|Mentioned|p14|||||||||
28192|Cheitmore Limestone|37727|5|Briefly described|p45|||||||||
28192|Cheitmore Limestone|38549|6|Mentioned|p1|||||||||
28192|Cheitmore Limestone|40328|6|Mentioned|p185|||||||||
37417|Chesleigh Formation undifferentiated|23214|5|Briefly described|p150|||Informal Name.||||||
40895|Chesleigh Formation, upper|50124|6|Mentioned|p126|||Informal name. The felsic volcaniclastic rocks of the upper Chesleigh Formation are now included in the Piambong Formation (Colquhoun et al. 1999b)||||||
27366|Chesney Greywacke|29621|6|Mentioned|p5|||||||||
27366|Chesney Greywacke|29680|6|Mentioned|Fig.1|||||||||
27366|Chesney Greywacke|29947|4|Described|p685|||||||||
27366|Chesney Greywacke|29948|5|Briefly described|p27|||Mention Fig.12||||||
27366|Chesney Greywacke|31592|6|Mentioned|Fig. 1|||L.-U.Silurian. Pt of Cobar Gp.||||||
27366|Chesney Greywacke|33004|6|Mentioned|Plate 18|||Shown photo 18||||||
27366|Chesney Greywacke|33342|6|Mentioned|p172|||?Early Sil.||||||
27366|Chesney Greywacke|34057|6|Mentioned|Map legend|Silurian|Silurian|||||||
27366|Chesney Greywacke|34405|5|Briefly described|p126|||||||||
27366|Chesney Greywacke|34469|6|Mentioned|p108|||Ordovician? See also P114||||||
27366|Chesney Greywacke|35287|6|Mentioned|Table 1|||||||||
27366|Chesney Greywacke|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
27366|Chesney Greywacke|37727|6|Mentioned|p47|||||||||
27366|Chesney Greywacke|39618|6|Mentioned|Table 1|||||||||
27366|Chesney Greywacke|41090|6|Mentioned|p89|||||||||
27366|Chesney Greywacke|42467|5|Briefly described|Map Legend|||||||||
27366|Chesney Greywacke|43398|14|Not recorded|Map Legend||Silurian|Part of Cobar Group||||||
27366|Chesney Greywacke|46032|14|Not recorded|p.411,413-414||Silurian|Unit of Cobar Group.||||||
27366|Chesney Greywacke|46900|6|Mentioned|p17|||Contacts discussed, also P20||||||
27366|Chesney Greywacke|61907|5|Briefly described|p143 Fig. 1|||Of the Cobar Group.||||||
32602|Chesney Greywacke Formation|46032|14|Not recorded|p.412|||||||||
29722|Chesney Greywacke Formation""|43032|6|Mentioned|p31|||refers to Rayner (1969).Superseded by Chesney Formation||||||
82386|Cheviot Hills Suite|71628|6|Mentioned|p19:23||||||Cheviot Hills Granite.|||
81111|Cheyenne complex|71703|5|Briefly described|p203,  p193 Fig. 1|Kungurian|Kungurian|~280 Ma, Rosenbaum et al., 2012.[probably location 1047, age 280.0 +/-2.8 Ma]||Of Hillgrove Supersuite.||||
41390|Chichester Formation, lower|44244|6|Mentioned|p111|||Informal reference to lowermost unit of the Chichester Formation.||||||
70477|Chilcotts Creek Tuff Member|62095|6|Mentioned|p276 Appdx.|||Of Kelk (1986). Superseded by Chilcotts Creek Ignimbrite Member.||||||31-JAN-08
70477|Chilcotts Creek Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
70477|Chilcotts Creek Tuff Member|68005|6|Mentioned|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
37413|Chimney Limestone - Mudstone Member|23214|6|Mentioned|p145|Late Silurian|Late Silurian|Of Hollanders Formation.  Now designated undifferentiated Hollanders Formation.||||||
31282|Chinamans Creek Formation|43474|14|Not recorded|no card|||(no card)||||||
31282|Chinamans Creek Formation|43476|14|Not recorded|Map Legend|||(Provisional Edition)||||||
79187|Chowdilla Quartz Monzonite|68592|6|Mentioned|p1417|||MacDonald (1979); a mis-spelling of the property name Childowla. Here renamed Childowla Quartz Monzonite.|||||A small body of monzonite.|
31277|Cinaltra Group|43501|14|Not recorded|Map Legend|||(Provisional Edition) (no card)||||||
36197|Clagger Formation|23392|6|Mentioned|p7|||Misspelling of Clagger Sandstone.||||||
79188|Clare Vale Beds|68592|6|Mentioned|p169|||Former name for Wet Lagoon Volcanics.||||||
40258|Clarence River Granitoid Suite|38905|6|Mentioned|p302 Fig.1|||Geological Province: New England Fold Belt||||||
36968|Clarence River Plutonic Suite|23720|5|Briefly described|Map Legend|||Includes the Linden Hill Adamellite.  Equates with the Nundle Plutonic Suite.  Low-K granitoids.||||||15-DEC-04
36968|Clarence River Plutonic Suite|23811|5|Briefly described|Map Legend|Triassic|Permian|Includes: Dumbudgery Creek, Towgon Grange and Kaloe Granodiorites.||||||20-DEC-04
36968|Clarence River Plutonic Suite|23812|4|Described|p18, p63|Late Permian|Early Permian|Comprised of Dumbudgery Creek, Towgon Grange and Kaloe Granodiorites.||||||
36968|Clarence River Plutonic Suite|38837|5|Briefly described|p234|Early Permian|Early Permian|Geological Province: New England Fold Belt||||||
36968|Clarence River Plutonic Suite|44244|5|Briefly described|p291|Triassic|Triassic|Of the New England Batholith.||||||
36968|Clarence River Plutonic Suite|44450|6|Mentioned|p17|||Geological Province: New England Fold Belt.||||||
36968|Clarence River Plutonic Suite|61772|6|Mentioned|p133||Late Triassic|||||||
36968|Clarence River Plutonic Suite|68003|6|Mentioned|p131.|Permian|Permian|[Superseded name]. See also Clarence River Suite (p29, p31).||||||
36968|Clarence River Plutonic Suite|68679|5|Briefly described|p454, p464|Permian|Permian|Shaw and Flood (1981). One of their five subdivisions of the granitoids of the New England Batholith. Subsequently the Clarence River Supersuite (Bryant et al., 1997). I-type.||||||
36968|Clarence River Plutonic Suite|70036|5|Briefly described|Map legend|Permian|Permian|New England Fold Belt.|||||Includes granodiorite.|
36968|Clarence River Plutonic Suite|71628|5|Briefly described|p1:5; p2:46, 52, 54; p6: 1, 6; p9: 1,5|Triassic||See also p9: 12, 32, 36; p10: 1, 5; p18: 1, 14; p19-91. Shaw and Flood (1981). Southern New England Orogen. Interpreted to have formed from partial melting of a LILE-poor (gabbro) source region. Subsequently the Clarence River Supersuite.|||Dumbudgery Creek, Jenny Lind, Kaloe, Koreelan Creek, Towgon Grange and (tentatively) Barrington Tops Granodiorites; Bruxner Adamellite.||A series of isotopically primitive, LILE-poor, K-poor granodiorites and tonalites.|
40245|Clarence River Plutonic Suite""|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
83049|Clarence River Plutonic Supersuite|73202|6|Mentioned|p636|Late Permian|Late Permian|New England Orogen, southern. I-type group. See also misspelt Clarance River Suite p639 Fig.10.|||||Predominantly tonalite, granodiorite and diorite.|
29561|Clarence River Suite|22580|5|Briefly described|p99|||||||||
29561|Clarence River Suite|22857|6|Mentioned|p204 Fig. 17.2|||Plutonic suite within the New England Batholith. See also p243 Fig. 18.4.||||||
29561|Clarence River Suite|22859|6|Mentioned|Fig17.2p204|||||||||
29561|Clarence River Suite|22863|6|Mentioned|Fig18.4p243|||||||||
29561|Clarence River Suite|38839|6|Mentioned|p244|||Geological Province: New England Fold Belt||||||
29561|Clarence River Suite|38905|6|Mentioned|p307|||Geological Province: New England Fold Belt||||||
29561|Clarence River Suite|42984|5|Briefly described|p365|||||||||
29561|Clarence River Suite|60079|5|Briefly described|Map Legend|Late Permian|Permian|||||||
29561|Clarence River Suite|60422|5|Briefly described|p386|||Of the New England Batholith. Also classified as Supersuites (Chappell and Bryant).||||||
29561|Clarence River Suite|64098|5|Briefly described|p335|||Includes Kaloe Granodiorite.||||||
29561|Clarence River Suite|68003|5|Briefly described|p29, p31, p131.|Early Triassic|Late Permian|New England Fold Belt. I-type granitoids. Called Clarence River Plutonic Suite [superseded name] on p131.|||Includes the Boxwell Creek Granodiorite.|||
29561|Clarence River Suite|68004|5|Briefly described|p23 Table 1. |Early Triassic|Late Permian|Central Block, New England Fold Belt.|||||Granites.|
29561|Clarence River Suite|68822|6|Mentioned|p328 Fig.8, p329 Fig.8, p348|||New England Orogen. 'Cordilleran-like'.|ca. 250 Ma|||||
29561|Clarence River Suite|71280|5|Briefly described|p410|Early Triassic|Permian||||||I-type plutonic rocks.|
29561|Clarence River Suite|71628|6|Mentioned|p6:16; p9:12; p19:91|||||||||
29561|Clarence River Suite|73264|6|Mentioned|p1399|||||||||
38334|Clarence River suite|23763|6|Mentioned|p543|||Informal.  Geological Province: New England Fold Belt.||||||
31187|Clarence Series|43491|14|Not recorded|pVIII/16,17||Triassic|Ref.to Sussmilch 1922. Freshwater beds. Compared with Sydney Basin||||||
38993|Clear Range Tonalite|23866|5|Briefly described|p123 Fig. 3|||Part of the Clear Range Granodiorite which grades into a tonalitic variety southwards where it is intersheeted with Murrumbucca Tonalite and Cooma Granodiorite.  Geological Province: Murrumbidgee Batholith.||||||17-AUG-04
39429|Clear Range adamellite|24128|5|Briefly described|p167|||Geological Province: Lachlan Fold Belt.||||||
68102|Clear Range granite|23866|6|Mentioned|p120|||Informal name.  Geological Province: Lachlan Fold Belt.||||||07-MAR-05
39423|Clear Range granodiorite|24128|6|Mentioned|p59|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
68841|Clear Range suite|24517|6|Mentioned|p49|||Informal name. S-type granite. Geological Province: Lachlan Fold Belt.||||||
73040|Clemantis Group|61377|5|Briefly described|p149 Fig. SU8|||Misspelling of Clematis? Geological Province: Gunnedah Basin.||||||07-FEB-11
39794|Clematis Group, upper|24159|6|Mentioned|p148|||Informal - see Clematis Group.||||||
32694|Clements Formation|24215|5|Briefly described|p805|||Of the Wagga Group. Geological Province:  Lachlan Fold Belt.||||||14-OCT-08
32694|Clements Formation|24417|3|Fully described|p9|Darriwilian|Darriwilian|Of the Wagga Group. Intruded by Ungarie Granite.||||||09-JAN-08
32694|Clements Formation|44936|5|Briefly described|Map Legend||Ordovician|||||||
32694|Clements Formation|50385|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Wagga Group. Interbeddded sandstone, siltstone, chert and shale (often phyllitic).||||||11-JUN-04
32694|Clements Formation|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of the Wagga Group.||||||13-JUL-04
32694|Clements Formation|61964|3|Fully described|p14 Fig. 4, p20-21|Gisbornian|Chewtonian|Dominated by thin-thick bedded qtz sst turbidites+siltst.DEF expanded to incl.former Humbug Sst.Unconform. below Gurragong Volcs in S, and Cocoparra Gp. in W. Partly equiv.to Pinnak Sst, the only constituent differentiated in Adaminaby Gp. in VIC. ||||||
32694|Clements Formation|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Wagga Group. Contains the Doongala Chert Member and the Milby Chert Member. Thin to medium bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.||||||10-APR-08
32694|Clements Formation|63019|5|Briefly described|p921 Fig.2|Ordovician|Ordovician|||||||
32694|Clements Formation|63891|5|Briefly described|p237|||Of Wagga Group. Faulted contact with Boothumble Formation. Poorly exposed and strongly deformed, craton-derived, quartz-rich turbidites.||||||
32694|Clements Formation|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Wagga Group. Contains Milby Chert Member - thin-to med.-bedded, qtz-rich sandstone interbedded with slate, shale+ phyllite.Unnamed members are of:  fine-g. quartzite; quartzose sandstone interbedded with mudstone; chert; pebble granule conglomerate||||||23-SEP-08
32694|Clements Formation|65469|5|Briefly described|p16, p18|Late Ordovician|Middle Orodovician|Lachlan Orogen.||Wagga Group|Includes the Milby Chert Member and the Doongala Chert Member.|Overlain by the Currawalla Shale.||
32694|Clements Formation|67322|4|Described|p18-19, p39; Fig.5|Darriwilian|Early Ordovician|Duggan and Scott (in Lyons et al. 2000). A 10-25m thick lens of clast-supported conglomerate represents channel fill facies. Darriwilian graptolites from outcrops at The Meadows Tank and at Illewong, previously assigned to the Tallebung Group, are now inferred to belong to the Clements Formation (by Colquhoun, Hendrickx and Meakin, in Colquhoun et al. 2005, p31). Occurs in the Cargelligo region. Includes the former Humbug Sandstone.||Of the Wagga Group|Milby Chert Member, Doongala Chert Member|Is ?conformably overlain by Currawalla Shale (Bendoc Group).|Turbiditic, with alternating beds of quartz-rich sandstone grading to siltstone and slate. Sandstones are very fine to medium grained, mature to supermature with minor feldspar (up to 2%); local conglomerate lens and outcrops of massive quartzite.|21-FEB-18
32694|Clements Formation|68466|5|Briefly described|p65-66|Middle Ordovician|Early Ordovician|Lake Cargelligo region, Albury-Bega Terrane.|||Milby, Doongala, Chert Members.||Turbiditic; beds of quartz-rich sandstone grading to siltstone and slate. Two discontinuous chert horizons, both relatively poorly exposed, forming lenticular bodies which pass into the turbiditic sandstone, mudstone and shale succession.|
32694|Clements Formation|68592|5|Briefly described|p307|||Central Lachlan Orogen.||Unit in Wagga Group.|Includes Milby Chert Member.|||
32694|Clements Formation|69160|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Wagga Group.|Includes Doongala Chert Member.|Is unconformably overlain by Gurragong Volcanics. Is intruded by Yalgogrin and Eura Bonny Granites.|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|69161|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Wagga Group.||Is intruded by Erigolia Granite.|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|69162|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Wagga Group.||Is overlain unconformably by Bootheragandra Group.|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|69163|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Wagga Group.||Is overlain unconformably by Bootheragandra Group.|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|69164|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Wagga Group.||Is overlain unconformably by Walters Range Group. Is faulted against Crossleys Tank Formation and Preston Formation (Rast Group).|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|69540|6|Mentioned|p640|Late Ordovician|Early Ordovician|Cargelligo 1:250 000 sheet area. Age ranges into early Gisbornian.||Unit in Wagga Group.||||
32694|Clements Formation|69668|5|Briefly described|p929 Fig.2, p931|Middle Ordovician|Early Ordovician|Cargelligo area, Albury-Bega terrane.||Unit in Wagga Group.|Includes Milby and Doongala, Chert Members.|Is overlain by Currawalla Shale.|Turbiditic quartz-rich sandstone grading to siltstone and slate; two discontinuous chert horizons.|
32694|Clements Formation|71693|5|Briefly described|Map legend.|Ordovician|Ordovician|This unit is mapped separately (with the symbol Owac), as well as in combination with the Bendoc Group (with the symbol Owac_Obe) where these two units are fault-imbricated.||Wagga Group.||Is overlain by Bendoc Group. Lateral equivalent of Girilambone Group.|Thin- to medium-bedded, quartz-rich sandstone interbedded with slate, shale and phyllite.|
32694|Clements Formation|71700|6|Mentioned|CD||||||Includes the Milby Chert Member.|Equivalent to the Wagga Group.||18-OCT-22
32694|Clements Formation|72296|5|Briefly described|p6, p9|||||Wagga Group.||Lower part is equivalent to Narrama Formation; part-equivalent to the Pinnak Sandstone.||
32694|Clements Formation|72908|6|Mentioned|p8 Tb.1, p11|||Hosts the Tallebung deposit.||Wagga Group|||Sedimentary units.|
32694|Clements Formation|73140|5|Briefly described|p495|||Proposed to be incorporated into, and superseded by the Abercrombie Formation.||Wagga Group||||18-OCT-22
68832|Cliefden Caves Limestone Group, lower|50098|6|Mentioned|p4||Late Ordovician|Informal name. Includes the Fossil Hill Limestone.||||||04-MAY-05
73695|Cliefden Caves Limestone Sub-group|63286|6|Mentioned|p308 Fig. 9|Bolindian|Eastonian|Uncomformably overlain by Malongulli Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
40463|Clifden Formation, Upper|24603|6|Mentioned|p895 Fig. 16|||Informal - see Clifden Formation.||||||
40554|Clifden Formation, upper|24605|6|Mentioned|p946|||Informal - see Clifden Formation.||||||
76147|Cliffs Tank Ultramafic body|66623|6|Mentioned|p81.|||Not a formal name. Mapped separately on Koonenberry area maps. Intrudes Baroorangee Creek Formation.||||||
77256|Clift Seam|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Informal name? Within Wallala Formation (Nea Subgroup, Black Jack Group)||||||
77256|Clift Seam|68004|5|Briefly described|pp152-153.|||Southern Mullaley Sub-basin, Gunnedah Basin. Widely developed; 3 to 4.5 m thick at depths of c.150 to 400 m. Suitable for underground extraction; low to medium ash soft coking coal.|||||Predominantly dull banded coal with sparse very thin tuffaceous or carbonaceous claystone bands.|
30218|Clifton Grove Formation|23214|6|Mentioned|p133|||Renamed Anson Formation.||||||
30218|Clifton Grove Formation|43127|5|Briefly described|p4,Fig.2,Fig.3|||Ludlow age fossils.||||||
37328|Clifton Grove limburgite|23214|5|Briefly described|p101|||Formal name not intended.||||||
37328|Clifton Grove limburgite|24015|5|Briefly described|p10|Ordovician|Ordovician|Informal. Geochemistry described. Derived from ultramafic shoshonitc arc magmas.||||||
37329|Clifton Grove ultramafics|23214|5|Briefly described|p102|Early Silurian|Late Ordovician|Formal name not intended.||||||
28457|Clive Adamellite|22443|6|Mentioned|p863||Triassic|||||||
28457|Clive Adamellite|29988|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
28457|Clive Adamellite|30787|6|Mentioned|Table 3|||||||||
28457|Clive Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28457|Clive Adamellite|34489|3|Fully described|p290|||||||||
28457|Clive Adamellite|38824|6|Mentioned|p218|||||||||
28457|Clive Adamellite|40509|6|Mentioned|p53|||||||||
28457|Clive Adamellite|45087|5|Briefly described|p12|||Chem. analyses.||||||
28457|Clive Adamellite|50015|6|Mentioned|p351|||Geological Province: New England Fold Belt||||||
28457|Clive Adamellite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Leucogranite.||||||
28457|Clive Adamellite|71628|6|Mentioned|p15:25|||Shaw (1964). Subsequently Clive Monzogranite (Henley et al., 2001) after unpublished work by Barnes (1987). Now Clive Leucomonzogranite (this study).||||||
38274|Clive Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse-grained, equigranular, pale buff to white bitotie monzogranite. Of the I-type granitoids.||||||20-DEC-04
38274|Clive Monzogranite|23812|5|Briefly described|p20 Tb. 2|Triassic|Triassic|||||||
38274|Clive Monzogranite|68005|5|Briefly described|p67, p133.|Permian|Permian|Listed on p.133 as a unit in Moonbi Supersuite.||Unit in Northern Moonbi Supersuite.|||Coarse-grained, equigranular, pale buff to white biotite leucogranite.|
38274|Clive Monzogranite|70217|4|Described|vi, p1 tbl 1.1, p60-p66, p76, p87|Wuchiapingian|Wuchiapingian|New England Orogen. Previously assigned to Moonbi Supersuite by Dawson (2004) but has since been reassigned to the Stanthorpe Supersuite. Petrography, zircon morphology and SHRIMP results discussed in detail. |254.6 +/- 1.4 Ma (SHRIMP U-Pb)|Stanthorpe Supersuite||Intrudes the Wandsworth Volcanics.|Mildly porphyritic to seriate alkali feldspar granite containg 45 percent quartz, 45 percent alkali feldspar, 5 percent biotite and minor plagioclase.|
38274|Clive Monzogranite|71628|6|Mentioned|p15: 25|||Of Barnes (1987). Replaced here by Clive Leucomonzogranite.||||||
38274|Clive Monzogranite|72078|6|Mentioned|p4|Permian|Permian|Geological province: New England Orogen. U-Pb SHRIMP date for zircon is derived from Cross and Blevin 2013.  Features minor scattered Sn-W mineralisation.|252.17-247.2 Ma (SHRIMP U-Pb)|||||14-JAN-20
82389|Clive Suite|71628|5|Briefly described|p15: 26|Middle Triassic|Late Permian|||Stanthorpe Supersuite.|Clive Leucomonzogranite.|||
72896|Cloghnan Shale""|62569|5|Briefly described|p607 Fig. 2|Late Devonian|Late Devonian|Within the Hervey Group of Conolly (1965, 1969).||||||
30991|Clonally Ignimbrite Member|43441|6|Mentioned|29||Early Devonian|?of Connemarra Formation?||||||08-JAN-10
31918|Clougher's Creek Formation|43881|2|Defined|p6-7,160, Map 12|||||||||
80266|Cloughlan Shale|71040|5|Briefly described|p16|Late Devonian|Late Devonian|Adjacent to Currowong Syncline.||Hervey Group.||||06-NOV-17
37414|Clover Hills Siltstone Member|23214|6|Mentioned|p145|Late Silurian|Late Silurian|Of Hollanders Formation.||||||
41620|Cloverdale coal seam|44244|5|Briefly described|p182 Fig. 37, p186|Late Permian|Late Permian|Of the Jilleon Formation.||||||
38305|Cloverdale seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Probably misspelt.   Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
38305|Cloverdale seam|44244|6|Mentioned|p327|||Within the Stroud-Gloucester Syncline.||||||
30651|Coal Measure Tuffs|43346|14|Not recorded|p2|||||||||
30832|Coalcliff Greywacke|43385|14|Not recorded|p182 Table||Early Triassic|||||||
70090|Coastal granitoids|22857|6|Mentioned|p262, p285|Early Triassic|Late Permian|Informal name for part of the New England Batholith.||||||
29508|Coates Creek Member|22857|5|Briefly described|p490 App.1 Tb.A1.7|Middle Devonian|Middle Devonian|Of the Dulladerry Volcanics. Geological Province: Dulladerry Rift.||||||
29508|Coates Creek Member|23214|3|Fully described|p223|Middle Devonian|Middle Devonian|Of Dulladerry Volcanics. Maroon, flow banded rheomorphic ignimbrite. Overlying unit: Hervey Group.||||||
29508|Coates Creek Member|43640|5|Briefly described|Map Legend||Devonian|||||||
29508|Coates Creek Member|43782|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
30760|Cobar Beds""|43344|14|Not recorded|p176|Early Devonian||||||||
29735|Cobar Slate Formation|43032|5|Briefly described|Table 1,p8|||Rayner 1969||||||
24853|Cobar Sub-group|37668|6|Mentioned|p101|||||||||
24854|Cobar formation|31618|6|Mentioned|p104|||||||||
34630|Cobargo Quartz Monzonite""|22815|6|Mentioned|p68|||Now obsolete. Superseded by Cobargo Granodiorite.||||||08-MAR-16
38446|Cobbannah group|23309|6|Mentioned|p211|||||||||
38446|Cobbannah group|24133|5|Briefly described|p21|||Misspelt - see Cobbannah Group.  Geological Province: Lachlan Fold Belt.||||||
38446|Cobbannah group|61161|6|Mentioned|p78|||Informal - see Cobannah Group.||||||
38446|Cobbannah group|61163|6|Mentioned|p27|||Informal name - see Cobbannah Group.||||||
79846|Cobbler's Creek Limestone|61892|6|Mentioned|p216|Wenlock|Llandovery|Contains Acrotretella brachiopods, contrasted with those around the world.||||||
73752|Coco Range Formation|63632|6|Mentioned|p658|||Geological Province: western Darling Basin. Alluvial fan deposits.||||||16-OCT-07
73752|Coco Range Formation|67562|5|Briefly described|p96-97, p100-103, p111|Givetian|Emsian|West of the Nundooka Creek Fault (Part of the Tasman Line). Overlies Neoproterozoic strata. Contains 5 units and members. > 1320m thick (top faulted out).|||||Lower and central parts are sublitharenite-rich.|23-JAN-17
70643|Coco range beds|61311|6|Mentioned|p51|||Geological Province: Darling Basin.||||||
31005|Cocopara Group|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
31005|Cocopara Group|71040|6|Mentioned|p14||Eifelian|Cocoparra Syncline. Mildly deformed during Tabberabberan Orogeny.||||||
80754|Cocoparra Group, upper|71889|5|Briefly described|p47, 48, p54|||Narrandera area. Includes fish fossils.||Cocoparra Group||Equivalent to the Jimberoo Formation and Rankin Formation in te Rankin Springs area..||28-FEB-19
80754|Cocoparra Group, upper|72083|5|Briefly described|p7, p39-40, p46, p49-50, p52 Photo.24|||An informal name for the undivided part of the Group above the Narrandera Sandstone. Occasionally presented as Upper Cocoparra Group [intended formalisation is highly doubtful]. A poorly exposed sequence comprising a recessive unit and an overlying resistive unit, occupying the centre of a basin structure N of Narrandera and W of Lake Coolah.||||Overlies Narrandera Sandstone.|Basal intercalated muddy siltstone and mostly medium-grained, grey to pale cream sandstone; mostly medium- to coarse-grained quartz sandstone to granule conglomerate and minor shale.|
68059|Cocoparra group|44093|5|Briefly described|p167 App. 1|Early Carboniferous|Early Devonian|Informal name. Clastic sediments. Geological Province: Lachlan Fold Belt.||||||02-MAR-05
83474|Cocoparra group''|73457|6|Mentioned|p2 Fig. 1 caption|||Mentioned as being the ex-'Cocoparra group', now included in Mulga Downs Group.||||||01-SEP-22
75941|Coepolly Conglomerate Member|65902|5|Briefly described|p200 Fig.5, p203 Fig.7|Serpukhovian|Serpukhovian|Misspelling. See Coeypolly Conglomerate Member, of Currabubula Formation p202, 204.||||||21-NOV-16
37441|Coffee Hill Member|23214|6|Mentioned|p235|||Of Davis (1968). Now included in Macquarie Park Sandstone. Basal marine mudstone and sandstone of the Macquarie Park Sandstone.||||||22-JAN-13
37441|Coffee Hill Member|24247|5|Briefly described|p42|Famennian|Famennian|Parent: Columbine Sandstone||||||
37441|Coffee Hill Member|68297|5|Briefly described|p194|Famennian|Famennian|Of Turner 1991, Kemp 1991. Includes lungfish, conodonts and brachiopods of the triangularis zone.||||||
37441|Coffee Hill Member|68592|6|Mentioned|p1737-8|Late Devonian|Late Devonian|Obsolete.||Unit in Columbine Sandstone.||||
37442|Coffee Hill Member""|23214|6|Mentioned|p236|||Now included in Macquarie Park Sandstone.||||||
28145|Coffs Harbour Beds|24237|5|Briefly described|p6|||Geological Province: Clarence-Moreton Basin.||||||
28145|Coffs Harbour Beds|29869|6|Mentioned|p38|||||||||
28145|Coffs Harbour Beds|30784|6|Mentioned|p70|||Refers McElroy (1963,1969),Voisey (1969)||||||
28145|Coffs Harbour Beds|31692|2|Defined|p65|Late Paleozoic|Late Paleozoic|Prob.Upper Palaeozoic||||||07-NOV-08
28145|Coffs Harbour Beds|31693|6|Mentioned|p98|||||||||
28145|Coffs Harbour Beds|34551|6|Mentioned|p229|||||||||
28145|Coffs Harbour Beds|35264|6|Mentioned|p15|||||||||
28145|Coffs Harbour Beds|35757|6|Mentioned|Fig.7|||||||||
28145|Coffs Harbour Beds|37808|6|Mentioned|p25|||||||||
28145|Coffs Harbour Beds|38755|6|Mentioned|Fig.1|||||||||
38327|Coffs Harbour Sequence""|23812|6|Mentioned|p10|||Informal name of Fergusson, 1982.||||||
37195|Coffs Harbour beds""|23812|6|Mentioned|p10|||Informal name of Korsch, 1977.||||||
37195|Coffs Harbour beds""|44450|6|Mentioned|p14|||||||||
70481|Cohens Gully Member|62095|5|Briefly described|p256 Fig. 7|||Abbreviated version of Cohens Gully Ignimbrite Member. Of the Currabubula Formation. Geological Province: Werrie block/Tamworth Belt.||||||
27744|Colemans Creek Sandstone|33334|6|Mentioned|Table 3|||Perm.||||||
27744|Colemans Creek Sandstone|34585|4|Described|p380|||Permian||||||
27744|Colemans Creek Sandstone|34605|6|Mentioned|Fig.5.28|||||||||
27744|Colemans Creek Sandstone|37087|6|Mentioned|p198|||||||||
28462|Coleraine Mudstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
28462|Coleraine Mudstone|38837|6|Mentioned|p233|||||||||
69663|Colia Basalts|61155|5|Briefly described|p19|Late Oligocene|Late Oligocene|Part of the Moruya Province Volcanics.  In Southeastern NSW.||||||
39428|Colinton volcanics|23309|6|Mentioned|p390|||||||||
39428|Colinton volcanics|24128|5|Briefly described|p132|Silurian|Silurian|Informal - see Colinton Volcanics.  Geological Province: Lachlan Fold Belt.||||||
82380|Collett Monzogranite|71628|5|Briefly described|p2: 47-50, 52, 54-56|||Named here after unpublished Collett Adamellite of Paul (1984). Has generally poor exposure; crops out over ~7 km2. Geochemistry described. Probably the result of mixing of mantle-derived and sedimentary-derived magmas. Assigned to Clarence River Plutonic Suite by Gilligan et al. (1972) but reassigned here to the Bakers Creek Supersuite.||Sheep Station Creek Complex.||Intrudes Moombil Siltstone, Campground Granodiorite and Big Bull Gabbro. Is intruded by Gumtree Monzogranite.|Light grey, weakly porphyritic, medium- to fine-grained, biotite(+/- hornblende) monzogranite. I-type.|
81251|Collingullie granite|72083|5|Briefly described|p7, p17, p39|||Here includes the (obsolete) Galore granite. See also Collingullie Granite (p7-8, p13-16, p41, p58 Fig.9).|||||Features spherical, up to 3cm diameter, fine-grained tourmaline bodies /(?)alteration masses.|
34270|Colo Creek Formation""|22679|6|Mentioned|p 29|||Name dropped.||||||
69664|Comboyne Province Volcanics|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Includes the Comboyne Basalt. Age: 16-14.5Ma.  In the Kempsey area.||||||
40699|Comerong volcanics|23309|6|Mentioned|p390|||||||||
26488|Comiala Formation|34059|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
74532|Comiala beds|61772|6|Mentioned|p128 Fig. 1|Carboniferous||In New England Orogen.||||||
74532|Comiala beds|61791|6|Mentioned|p326 Fig. 2|Permian|Carboniferous|||||||
80084|Commerong Volcanics|71069|6|Mentioned|p61|||||||||
35565|Composite Gneiss|23248|6|Mentioned|p174|||||||||
35565|Composite Gneiss|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
74930|Compton Downs granite|64681|6|Mentioned|p2|Late Silurian|Late Silurian|Informal name. Age: 416.4+/-2.5Ma.||||||15-DEC-08
68848|Condobolin Road Intrusive Complex|24518|5|Briefly described|p66|Early Ordovician|Early Ordovician|Porphyries. High-K calc-alkaline geochemistry. Age: ~484Ma.||||||
68848|Condobolin Road Intrusive Complex|63293|6|Mentioned|p467|Early Ordovician|Early Ordovician|Age: 481+/-4Ma (revised age). Has high-K calc-alkaline affinities.||||||07-FEB-11
83928|Condobolin Road monzodiorite|70278|6|Mentioned|p1627|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.|484.3 +/- 2.9 Ma (SHRIMP; Butera et al., 2001).|||||
27746|Condor Granodiorite|36441|5|Briefly described|map legend|Pridolian|Pridolian|Intrusive. Granodiorite, tonalite. BMR map code: Scg.||||||
27746|Condor Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh2||||||
27746|Condor Granodiorite|45147|3|Fully described|M254|Late Silurian|Late Silurian|Probably Late Silurian in age. Named after Condor Creek, which flows across its outcrop. Originally described as hornblende microgranite, but now known to be granodiorite, with tonalite near the edge, suggesting a zoned pluton. Mineralogy discussed.||||Apparently older than the Mountain Creek Volcanics, and is probably related to chemically similar Jindabyne Suite I-type granitoids farther south.||23-DEC-21
27746|Condor Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
28173|Congi Creek Adamellite|721|5|Briefly described|Map legend|Early Triassic|Early Triassic|Of the Moonbi Plutonic Suite.  Approximately  equigranular fine to medium-grained biotite monzogranite.||||||
28173|Congi Creek Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
28173|Congi Creek Adamellite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
28173|Congi Creek Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28173|Congi Creek Adamellite|35257|6|Mentioned|Fig.17|||||||||
28173|Congi Creek Adamellite|43091|5|Briefly described|Map legend|||of Moonbi Platonic Suite||||||
28173|Congi Creek Adamellite|71628|6|Mentioned|p7: 37, 40, 46|||Flinter et al. (1972) after work by Flood (1971) and others. Subsequently the Congi Creek Monzogranite (Brown, 2003 after unpublished work by Chappell and Bryant, 1994). In this study it becomes Congi Creek Monzogranite Phase (of Walcha Road Monzogranite).||||||
41054|Congi Creek Monzogranite|24366|6|Mentioned|p21 Fig. 12|||||||||
41054|Congi Creek Monzogranite|68005|5|Briefly described|p67, p133.|Permian|Permian|Listed on p.133 as a unit in Moonbi Supersuite.||Unit in Southern Moonbi Supersuite.|||Approximately equigranular fine- to medium-grained biotite monzogranite.|
41054|Congi Creek Monzogranite|69639|4|Described|p2, p6, p8, p10, p199|Lopingian|Lopingian|New England Orogen. Probably a felsic equivalent of the Walcha Road Monzogranite. See also p204-p209, p217-p218, p238.|250.6 +/- 1.7 Ma|Moonbi Supersuite|||Massive, medium-grained, equigranular biotite granite of probable I-type affinity.|
41054|Congi Creek Monzogranite|71628|6|Mentioned|p7: 37-38, 43-44, 46|||Brown (2003) after unpublished work by Chappell and Bryant (1994). Originally Congi Creek Adamellite of Flinter et al. (1972) after work by Flood (1971) and others. In this study it becomes Congi Creek Monzogranite Phase (of Walcha Road Monzogranite).||||||
30866|Conjola Beds|43346|14|Not recorded|p2|||||||||
30866|Conjola Beds|43491|14|Not recorded|page not known||Permian|||||||
30866|Conjola Beds|44282|14|Not recorded|p.17,18;Pl.3|||(I56-9/Kiama).||||||
30865|Conjola Beds""|43346|14|Not recorded|p2|||||||||
27374|Conjola Formation|22591|5|Briefly described|Fig 1||Early Permian|||||||
27374|Conjola Formation|23013|6|Mentioned|p326|||||||||
27374|Conjola Formation|29728|6|Mentioned|p394|||||||||
27374|Conjola Formation|29752|6|Mentioned|p25|||||||||
27374|Conjola Formation|29992|6|Mentioned|Map legend|Permian|Permian|||||||
27374|Conjola Formation|29994|6|Mentioned|Map legend|Permian|Permian|||||||
27374|Conjola Formation|30341|6|Mentioned|p134|||Permian age||||||
27374|Conjola Formation|30450|6|Mentioned|Table 1|||Sydney Basin. Permian||||||
27374|Conjola Formation|31062|6|Mentioned|p478|||Permian. On Table||||||
27374|Conjola Formation|31081|6|Mentioned|p51|||See also P65 & Fig. 2||||||
27374|Conjola Formation|31277|6|Mentioned|p3|||||||||
27374|Conjola Formation|32073|6|Mentioned|p21|||||||||
27374|Conjola Formation|32128|6|Mentioned|p25|||||||||
27374|Conjola Formation|32943|6|Mentioned|p86|||See also PP87,97,98,105 & Fig.2||||||
27374|Conjola Formation|32945|6|Mentioned|p84|||Permian||||||
27374|Conjola Formation|33420|6|Mentioned|Fig.2|||||||||
27374|Conjola Formation|34039|6|Mentioned|p355|||||||||
27374|Conjola Formation|34059|6|Mentioned|Map legend|Permian|Permian|||||||
27374|Conjola Formation|34084|6|Mentioned|p368|||Permian||||||
27374|Conjola Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian - Artinskian||||||
27374|Conjola Formation|34211|6|Mentioned|p32|||Permian||||||
27374|Conjola Formation|34215|6|Mentioned|p42|||||||||
27374|Conjola Formation|34292|6|Mentioned|p29|||Permian||||||
27374|Conjola Formation|34333|6|Mentioned|p356|||||||||
27374|Conjola Formation|34334|3|Fully described|p360|||Fossil lists P361||||||
27374|Conjola Formation|34426|6|Mentioned|p9|||Palaeontology||||||
27374|Conjola Formation|34445|6|Mentioned|p319|||Faunal correlation||||||
27374|Conjola Formation|34451|4|Described|p197|||Permian||||||
27374|Conjola Formation|34475|6|Mentioned|p263|||Permian||||||
27374|Conjola Formation|34568|6|Mentioned|p218|||Fauna||||||
27374|Conjola Formation|34692|5|Briefly described|p185|||||||||
27374|Conjola Formation|35530|6|Mentioned|p8|||Location of Bivalvia fossils.||||||
27374|Conjola Formation|36220|6|Mentioned|Table 1|||||||||
27374|Conjola Formation|39078|6|Mentioned|p117|||||||||
27374|Conjola Formation|39267|6|Mentioned|p237|||||||||
27374|Conjola Formation|41315|6|Mentioned|p149|||||||||
27374|Conjola Formation|43349|14|Not recorded|Map|||||||||
27374|Conjola Formation|43383|14|Not recorded|Fig.3,p20,Fig.5||Permian|||||||
27374|Conjola Formation|43460|14|Not recorded|p96|||||||||
27374|Conjola Formation|43474|14|Not recorded|fig.1,p43,49,50,57,||Sakmarian|p71,72,88,100,104||||||
27374|Conjola Formation|43475|14|Not recorded|p552,553||Permian|||||||
27374|Conjola Formation|43479|14|Not recorded|p188,189,218||Artinskian|||||||
27374|Conjola Formation|43676|6|Mentioned|p326|||||||||
27374|Conjola Formation|43981|2|Defined|p3,20||Permian|||||||
27374|Conjola Formation|45006|14|Not recorded|Tb.1,p6,32,40,42-3,|||p94-5,116,118,126,128,130,142.||||||
27374|Conjola Formation|45031|14|Not recorded|p35,49,52,54,63-4,67|||||||||
27374|Conjola Formation|45090|6|Mentioned|p147|||Refers Gostin(1968)||||||
27374|Conjola Formation|48926|6|Mentioned|p39|||P39 et seq.||||||
29811|Conjola Group|43050|5|Briefly described|p16|||Mispelling of Conjola Subgroup?||||||
79633|Conlea Porphyry|70821|5|Briefly described|p9-10, p13 Tb.2.1|Early Devonian|Early Devonian||398.0 +/- 2.8 Ma (Fraser et al., 2014).||||Intermediate porphyry.|01-DEC-16
83625|Consols Amphibolites|73575|6|Mentioned|p826, p830 Fig.4|||Interpreted to be a single unit with the Town Amphibolites. Shown as Consols Amphibolite in Fig. 4.||||||
24865|Coodravale Granite|42726|5|Briefly described|map legend|Silurian||433. Variation on Coodravale Granodiorite.||||||
31701|Cookamidgera Formation|22857|5|Briefly described|p488 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Formerly "Cookamidgera Subgroup". Fine-grained red arenite, siltstone and shale; minor red-purple conglomerate. Max. thickness: 600m. Geological Province: Hervey Basin.||||||
31701|Cookamidgera Formation|23214|3|Fully described|p231|Late Devonian|Late Devonian|Of Hervey Group. Previously Cookamidgera Subgroup and now includes the Eurow Member (formerly Eurow Formation).||||||
31701|Cookamidgera Formation|23217|6|Mentioned| p17|||See also "Cookamidgera Formation". Replaced Cookamidgera Sub-group.  Now (in part) superseded by Wingara Formation.||||||17-JUL-08
31701|Cookamidgera Formation|24417|6|Mentioned|p141|||The Wingara Formation was mapped within this unit by Pogson and Watkins (1998).  Wingara Formation now a formation in its own right.||||||09-OCT-08
31701|Cookamidgera Formation|43640|5|Briefly described|Map Legend|Devonian|Devonian|Of Hervey Group.||||||09-OCT-08
31701|Cookamidgera Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Hervey Group. Includes Eurow Member. Consists of Fine-grained red sandstone, siltstone and shale; minor red-purple conglomerate.||||||17-JUL-08
31701|Cookamidgera Formation|43782|5|Briefly described|Map Legend|Famennian|Famennian|Of Hervey Group.||||||17-JUL-08
31701|Cookamidgera Formation|68592|6|Mentioned|p1721|||In the Bathurst 1:250 000 map area.||||Correlated with Koorawatha Formation.||
37114|Cookamidgera Formation""|23392|6|Mentioned|p24|||Of Pogson & Watkins (1998). Superseded by Eurow Formation.||||||
37114|Cookamidgera Formation""|24417|6|Mentioned|p140|||Of Pogson and Watkins (1998).  Informal name.  Proposed that it should contain a lower "Eurow Member'.  However, Eurow Formation is retained (Young, 1999b).||||||13-OCT-04
37116|Cookamidgera Sub-Group""|23217|5|Briefly described|p1, p16|||Informal - see Cookamidgera Sub-group.||||||08-MAR-06
37116|Cookamidgera Sub-Group""|23392|6|Mentioned|p24|||||||||
37116|Cookamidgera Sub-Group""|24417|6|Mentioned|p141|||Of Connolly (1965a).  'Undifferentiated upper Cookamidgera Sub-Group' was the term used by O'Connolly (1965a) for the Wingara Formation.  Superseded by Cookamidgera Subgroup.||||||13-OCT-04
27376|Cookamidgera Sub-group|23217|6|Mentioned|p13, p16|||Later replaced by Cookamidgera Formation.||||||08-MAR-06
27376|Cookamidgera Sub-group|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
70086|Cookamidgera Subgroup""|22857|5|Briefly described|p213|Devonian|Devonian|One of three former subdivisions ( Connolly, 1965a) of the Hervey Group; superseded by Cookamidgera Formation. Geological Province: Hervey Basin.||||||
39377|Cookamidgera subgroup|24125|5|Briefly described|p46|||Informal.  Of the Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
28467|Cookbundoon Sandstone|22857|4|Described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Lambie Group. White quartzite, quartzite arenite, pebbly arenite, conglomerate, mudstone; contains 'Lepidodendron' fossils. Max. thickness: 200m. Geological Province: Lambie Basin.||||||
28467|Cookbundoon Sandstone|22859|6|Mentioned|p217|||||||||
28467|Cookbundoon Sandstone|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
28467|Cookbundoon Sandstone|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
28467|Cookbundoon Sandstone|32865|6|Mentioned|p483|||||||||
28467|Cookbundoon Sandstone|32999|3|Fully described|p42|||See also P39. Refers Brunker et al. (1970)||||||
28467|Cookbundoon Sandstone|34481|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28467|Cookbundoon Sandstone|35655|6|Mentioned|p209|||Stratigraphy||||||
28467|Cookbundoon Sandstone|63633|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Lambie Group. White quartzite, quartzitic sandstone, pebbly sandstone, red siltstone, sandstone.||||||
30761|Cookman Formation beds|43344|14|Not recorded|p152|||||||||
34176|Coolac Ophiolite Suite""|22638|6|Mentioned|pviii|||Contains the North Mooney Complex||||||
79642|Coolac ophiolite suite|69043|6|Mentioned|p63||||||||Metamorphosed basalts, dolerites and supracrustal rocks.|
77258|Coolah seam""|68004|5|Briefly described|p61, p157, p220.|Late Permian|Late Permian|Western Coalfield. Correlated with Irondale Coal. Average thickness of 1.7 m and raw coal ash of 20%. May prove a mineable resource.|||||Dull coal with minor bright layers.|
77699|Coolamine Complex|60308|6|Mentioned|p38|||||Boggy Plains Suite||||
36358|Coolangatta Latite Member""|23544|5|Briefly described|p357|||Informal||||||
28132|Coolangubra Granite|42726|5|Briefly described|map legend|Early Devonian||132.  Of the Coolangubra Suite (Bemboka Supersuite).||||||07-FEB-05
28469|Coolringden Beds|30332|6|Mentioned|p126|||Refers Vallance in Packham(1969)||||||
34466|Cooma "granite"|22719|6|Mentioned|p493|||||||||
34581|Cooma Complex""|22815|6|Mentioned|p30|||Superseded by Cooma Metamorphic Complex||||||23-AUG-04
34581|Cooma Complex""|46574|5|Briefly described|Map Legend|Early Silurian|Early Silurian|Includes: Cooma Gneiss. Structural term. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
34662|Cooma Granite""|22815|6|Mentioned|p63|||Superseded by Cooma Granodiorite.||||||
36138|Cooma complex|23464|6|Mentioned|p249|||||||||
28470|Cooma granodiorite|42154|6|Mentioned|p343|||||||||
28470|Cooma granodiorite|70890|5|Briefly described|p326|||Geological province: Lachlan Fold  Belt. Derived from in-situ melting of exposed Ordovician turbidites (cf. Joplin 1962; Pidgeon and Compston 1965; White et al. 1974). Geochemically similar yo Yabba adamellite.||||||
68840|Cooma suite|24517|6|Mentioned|p49|||Informal name. Heterogenous diatexitic granite core of the Cooma Metamorphic Complex. Geological Province: Lachlan Fold Belt.||||||25-MAY-05
34465|Cooma supersuite""|22719|6|Mentioned|p490|||||||||
80785|Coombadja Volcanic Cauldron Complex|69639|6|Mentioned|p57, 219|||Intruded by Moonta Gully Monzogranite (magmatic crystallisation age 253.6 +/-1.6 Ma U-Pb SHRIMP).||||||06-MAR-19
38340|Coombadja Volcanic Complex|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Parent: Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||
38340|Coombadja Volcanic Complex|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
36823|Coombadjha Complex|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
36823|Coombadjha Complex|71628|5|Briefly described|p17:4; p19:72|||Named by McPhie (1984, unpublished).|||Moonta Gully Monzogranite, Pheasant Creek Volcanics, Dundee Rhyodacite.|Is intruded by Dundahra Creek Leucosyenogranite.||
23506|Coombadjha Volcanic Complex|22857|4|Described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Part of Wandsworth Volcanic Group. Volcaniclastics, felsic porphyry, welded ignimbrite. Includes Dundee Rhyolite (part), Babepercy Volcanics, Pi Pi Ignimbrite, Hianana and Pheasant Creek Volcanics. Max. thickness: >1500m. Geol. Prov: New England Fold Belt||||||
23506|Coombadjha Volcanic Complex|23443|4|Described|p418|Late Permian|Late Permian|||||||
23506|Coombadjha Volcanic Complex|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Pheasant Creek, Hianana and Babepercy  Volcanics, and Pi Pi Ignimbrite and the Coombadjha mass of the Dundee Rhyodacite.||||||20-DEC-04
23506|Coombadjha Volcanic Complex|23812|5|Briefly described|p25|Late Permian|Late Permian|Of Wandsworth Volcanic Group.||||||
23506|Coombadjha Volcanic Complex|23859|6|Mentioned|p929|||Geological Province: New England Fold Belt.||||||
23506|Coombadjha Volcanic Complex|38755|6|Mentioned|Fig.1|||||||||
23506|Coombadjha Volcanic Complex|39238|5|Briefly described|p123|||||||||
23506|Coombadjha Volcanic Complex|39673|6|Mentioned|Fig.14|||||||||
23506|Coombadjha Volcanic Complex|40514|6|Mentioned|p7|||||||||
23506|Coombadjha Volcanic Complex|41041|3|Fully described|p258|||||||||
23506|Coombadjha Volcanic Complex|41998|6|Mentioned|p481|||||||||
23506|Coombadjha Volcanic Complex|42378|5|Briefly described|Table 1 P6, Fig.1 P5|||||||||
23506|Coombadjha Volcanic Complex|43017|6|Mentioned|p378|||||||||
23506|Coombadjha Volcanic Complex|43161|5|Briefly described|32|||||||||
23506|Coombadjha Volcanic Complex|43705|6|Mentioned|p19||Triassic|||||||
23506|Coombadjha Volcanic Complex|60079|5|Briefly described|Map Legend|Late Permian|Permian|||||||
23506|Coombadjha Volcanic Complex|61793|5|Briefly described|p341, p347|||Geological Province: New England Fold Belt.||||||07-FEB-11
23506|Coombadjha Volcanic Complex|63748|6|Mentioned|p20|||In NSW. May be represent equivalent to the large bodies of Dundee Rhyodacite in Queensland.||||||07-FEB-11
23506|Coombadjha Volcanic Complex|71628|5|Briefly described|p15:5; p19: 128-129|||Is interpreted to have a three-stage formation: accumulation of a thick pile of volcanics, eruption of voluminous ignimbrite with associated cauldron collapse, and emplacement of monzogranite.|||Pheasants Creek and Hianana Volcanics, ?Dundee Rhyodacite, Pi Pi Ignimbrite and Moonta Gully Monzogranite.|Is almost totally surrounded by Moonta Gully Monzogranite.||
23506|Coombadjha Volcanic Complex|73215|6|Mentioned|p1003|||Southern New England Orogen. Caldera collapse structures have been recognised in this rock assemblage; the authors suggest a similar tectonic setting for the Talmo Formation.||||||
35420|Coomber Beds""|23170|6|Mentioned|p44|||||||||
80461|Coonabidgal Formation|70718|5|Briefly described|p23|||Misspelling of Coonambidgal Formation - see p25. Deposited in fluvial, fluvio-lacustrine, channel and flood plain environments of existing rivers.|||||Unconsolidated grey-brown micaceous silty clay, silt, polymictic sand and gravel.|30-MAY-19
34525|Coonambidgal Formation""|22799|6|Mentioned|p58|||||||||
25860|Coondella Creek Adamellite|22857|6|Mentioned|p215|||Geological Province: Lambie Basin.||||||
25860|Coondella Creek Adamellite|22859|6|Mentioned|p215|||||||||
25860|Coondella Creek Adamellite|39028|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian to Givetian.||||||21-MAY-08
25860|Coondella Creek Adamellite|40276|2|Defined|p22|Late Devonian|Middle Devonian|Middle to Late Devonian.||||||21-MAY-08
35866|Cooningan Formation|23336|6|Mentioned|3|||Probable misspelling of Coonigan Formation.||||||
26260|Cooperabung Formation|22736|5|Briefly described|p619,22,23|Namurian|Visean|author recomends this name no longer be used,  replaced with... in its lower section by the Hyndmans Creek Formation and in its upper section by the Mingaletta Formation.||||||
26260|Cooperabung Formation|24124|5|Briefly described|p3|||||||||
26260|Cooperabung Formation|38803|2|Defined|p105|Middle Carboniferous|Middle Carboniferous|||||||
26260|Cooperabung Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Hastings Block.||||||16-DEC-04
70087|Cooperabung Formation""|22857|6|Mentioned|p514 App.1 Tb.A1.8|Namurian|Namurian|Informal name. ||||||
79190|Coopers Creek Dacite|68592|6|Mentioned|p660|||Gould (1974); Farrell (1986). Now Wet Lagoon Volcanics (Thomas, 2012).||||||
26492|Coopers Creek Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group||||||
26492|Coopers Creek Formation|23710|6|Mentioned|p74|||||||||
26492|Coopers Creek Formation|24098|5|Briefly described|p27 Fig. 2|Early Devonian|Early Devonian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
26492|Coopers Creek Formation|30245|6|Mentioned|p79|||||||||
26492|Coopers Creek Formation|30246|6|Mentioned|p192|||Refers Philip(1962) Strusz(1972)||||||
26492|Coopers Creek Formation|30597|6|Mentioned|p29|||Early Siegenian. See also P31.||||||
26492|Coopers Creek Formation|30930|6|Mentioned|Map legend|Early Devonian|Early Devonian|Walhalla Group||||||
26492|Coopers Creek Formation|31331|6|Mentioned|p182|||||||||
26492|Coopers Creek Formation|31503|6|Mentioned|p2|||||||||
26492|Coopers Creek Formation|32984|6|Mentioned|p343|||Fossil content||||||
26492|Coopers Creek Formation|32985|6|Mentioned|Fig.2|||Correlation chart.||||||
26492|Coopers Creek Formation|33238|5|Briefly described|p642|||||||||
26492|Coopers Creek Formation|33326|6|Mentioned|p431|||Fauna||||||
26492|Coopers Creek Formation|33393|6|Mentioned|p163|||||||||
26492|Coopers Creek Formation|33434|6|Mentioned|p66|||||||||
26492|Coopers Creek Formation|33732|4|Described|Table III|||Dev. Correlation chart.||||||
26492|Coopers Creek Formation|34153|6|Mentioned|p48|||Lower Devonian.||||||
26492|Coopers Creek Formation|34250|6|Mentioned|p3|||Siegenian||||||
26492|Coopers Creek Formation|34403|6|Mentioned|p149|||||||||
26492|Coopers Creek Formation|34478|6|Mentioned|p483|||||||||
26492|Coopers Creek Formation|34954|6|Mentioned|Fig.34|||||||||
26492|Coopers Creek Formation|35193|6|Mentioned|p20|||||||||
26492|Coopers Creek Formation|35274|6|Mentioned|p420|||||||||
26492|Coopers Creek Formation|35283|3|Fully described|p53|||||||||
26492|Coopers Creek Formation|37727|5|Briefly described|p65|||||||||
26492|Coopers Creek Formation|42015|6|Mentioned|p316|||||||||
26492|Coopers Creek Formation|42418|5|Briefly described|p235|||Superseded in part? by Wurutwun Formation||||||
26492|Coopers Creek Formation|42635|5|Briefly described|p27|||||||||
26492|Coopers Creek Formation|43525|14|Not recorded|p130,Tb p131,132||Siegenian|||||||
26492|Coopers Creek Formation|43526|14|Not recorded|p583||Gedinnian|Fossils||||||
26492|Coopers Creek Formation|43527|14|Not recorded|p543,544,549|||||||||
26492|Coopers Creek Formation|43529|14|Not recorded|p233||Siegenian|||||||
26492|Coopers Creek Formation|43530|14|Not recorded|p1025,1026||Siegenian|L.Siegenian||||||
26492|Coopers Creek Formation|43531|14|Not recorded|p795-7||Siegenian|Correlated with Lilydale Limestone||||||
26492|Coopers Creek Formation|43532|14|Not recorded|p201,210,215-6,220||Devonian|Revision of Devonian Mictophyllum||||||
26492|Coopers Creek Formation|43533|14|Not recorded|p116-7,119,123,130|||Late Gedinnian or Siegenian.Tyers R. L.Dev corals||||||
26492|Coopers Creek Formation|43537|14|Not recorded|p3,9,22-3,28-9|||Late Gedinnian or Siegenian. Cooper's Creek ?. Devonian tetracorals||||||
26492|Coopers Creek Formation|45039|6|Mentioned|p5|||||||||
26492|Coopers Creek Formation|45075|6|Mentioned|p29|||Devonian||||||
26492|Coopers Creek Formation|61181|6|Mentioned|p126|Early Devonian|Early Devonian|Contains a number of limestone lenses - grey to dark grey with varying purity from pure to impure and silty; fine- to coarse-grained and consists essentially of comminuted bioclastic debris. See also p129 Tb. 32.||||||
26492|Coopers Creek Formation|64616|5|Briefly described|p92, p254|||Of Philip (1962). Superseded: replaced by Coopers Creek Limestone (see p99, p164, p294, p304, p385 Tb.1, p386) and the 'basal grits and conglomerates' in Coopers Creek are now included in the Boola Formation. Hosts the Boola limestone quarry, worked for lime production.||||||
26492|Coopers Creek Formation|68297|5|Briefly described|p191|Pragian|Pragian|Of Philip (1965), Turner (1991). Misspelling of Coopers Creek Limestone? See also Coopers Creek Beds. Both p189. Includes Pragian vertebrate fossil fauna.||||||
70088|Cooreen Creek Coal Member|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Loughmore Formation (Coorabin Coal Measures). Carbonaceous sandstone and mudstone. Max. thickness: 7m. Geological Province: Ovens Graben.||||||
26494|Cootawundy Beds|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
26494|Cootawundy Beds|32677|6|Mentioned|P5||Early Devonian|||||||
26494|Cootawundy Beds|33004|6|Mentioned|p157|||See also P196||||||
26494|Cootawundy Beds|35235|6|Mentioned|p209|||||||||
26494|Cootawundy Beds|36534|6|Mentioned|p227|||||||||
26494|Cootawundy Beds|38692|6|Mentioned|p129|||Also known as Mount Daubney Beds.||||||
26494|Cootawundy Beds|42298|6|Mentioned|p29 (p101a)|||Used 1978. Replaced by Mount Daubeny Formation 1990||||||
70146|Cootawundy Tank rippled pale red muddy siltstone|23336|6|Mentioned|p13|||Informal name.  Invariably mica-rich - mica being derived from the Ponto beds.||||||
70089|Cootawundy beds""|22857|6|Mentioned|p166|||Superseded by Mount Daubeny Formation.||||||
31568|Cootralantra Suite|42726|5|Briefly described|map legend||Silurian|||||||
31568|Cootralantra Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
31568|Cootralantra Suite|72571|6|Mentioned|p90|||Of the Tasmanides of eastern Australia.||||||
30884|Cope's Creek Keratophyre|43400|2|Defined|p178,179,183,184,map||Gedinnian|Formation of Tamworth Group (L.Dev)||||||
30884|Cope's Creek Keratophyre|43406|14|Not recorded|p42|||||||||
30821|Cope's Creek Tuff|43383|14|Not recorded|p23||Triassic|||||||
30821|Cope's Creek Tuff|43881|14|Not recorded|p6-7,10,20-2.49-51,||Triassic|Formation within Nymboida Coal Measures.p57-8,63,70,79-80,167, Map 12||||||
34444|Copes Creek Keratophyre""|22750|6|Mentioned|p 228|||||||||
23509|Copeton Adamellite|38842|6|Mentioned|p286|||||||||
23509|Copeton Adamellite|71628|6|Mentioned|p4:3|||||||||
35055|Copeton Group|23050|5|Briefly described|p76|||||||||
35055|Copeton Group|68004|5|Briefly described|p125, p201.|||New England Fold Belt. Alluvial tin occurs in deep leads: two main levels of intrabasaltic alluvials containing cassiterite and diamonds have been worked.||||||
82397|Copeton Leucoadamellite|71628|6|Mentioned|p4:16|||Flinter (1982). Now the Copeton Monzogranite.||||||
82399|Copeton Supersuite|71628|6|Mentioned|p4: 2, 10, 18, 24, 29, 33, 36, 38, 41|||See also p4: 47, 52, 55, 58. Bryant et al. (1997). Subsequently replaced by Bundarra Supersuite (Bryant et al., 1997).||||||
40246|Copeton group|38842|5|Briefly described|p286|Permian|Permian|Geological Province: New England Fold Belt. Age: 285 +/- 15Ma||||||
68776|Copi Dam Arenite|60648|6|Mentioned|p46, p50|Eifelian|Emsian|See also Copi Dam Member, Copi Dam Arenite Member and Copi Dam Pebbly Arenite Member.||||||
68777|Copi Dam Member|60648|5|Briefly described|p42 Fig. 2, p52|Eifelian|Emsian|Of the Coco Range Sandstone.  See also Copi Dam Arenite, Copi Dam Arenite Member, and Copi Dam Pebbly Arenite Member. Geological Province: Darling Basin.||||||28-APR-05
68777|Copi Dam Member|67562|6|Mentioned|p101|||See also Copi Dam Arenite Member, p103||||||01-OCT-15
68778|Copi Dam Pebbly Arenite|60648|5|Briefly described|p44|Eifelian|Emsian|Of the Coco Range Sandstone. See also Copi Dam Arenite, Copi Dam Arenite Member, and Copi Dam Member. Coarse-grained pebbly arenite.  Max. thickness: 38m. Gological Province: Darling Basin.||||||26-APR-05
70156|Copi Tank Arenite|23336|5|Briefly described|p27, p28|||Informal - see Copi Tank Arenite Member.  Of the Copi Range Sandstone. Coarse-grained and pebbly.  Max. thickness: 15m.||||||
35873|Copi Tank Member|23336|5|Briefly described|p15, p17 Fig. 12|||Of Coco Range Sandstone. Max. thickness: ~38m.||||||21-MAR-06
70152|Copi Tank arenite member|23336|6|Mentioned|p16|||Informal reference to Copi Tank Member (of the Coco Range Sandstone). Coarse-grained, pebbly.||||||
32928|Copper Creek Slates|48873|14|Not recorded|p.11|||(I55-16/Michelago).||||||
32924|Copper Creek siltstone|48878|14|Not recorded|p.44|||(I55-16).||||||
73683|Copper Hill Complex|63283|6|Mentioned|p206|||In the Molong area. Copper Hill Suite is part of this, but refers to the widespread magmatic suite.||||||21-FEB-23
73683|Copper Hill Complex|63287|6|Mentioned|p342, p343|||Intrusive dacites.||||||07-FEB-11
73683|Copper Hill Complex|63293|5|Briefly described|p470|||Age: 450 to 446Ma (Crawford et al. 2007a, b; Percival and Glen 2007). Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73683|Copper Hill Complex|70684|5|Briefly described|p27, p30|||Hosts the Copper Hill Cu-Au deposit. Partly concentric alteration zonation described and illustrated in some detail. The dacite was K-Ar hornblende dated at 446 +/- 6 Ma (Chivas in Perkins et al., 1995). Other similar ages given.|447 +/- 5 Ma (hornblende: Chivas in Scott, 1978).|||Intrudes Fairbridge Volcanics and Reedy Creek Limestone.|Quartz diorite and younger dacite; they have medium K calc-alkaline affinities. Locally well-mineralised.|
73694|Copper Hill Dacite|63286|6|Mentioned|p308 Fig. 9|Bolindian|Bolindian|Geological Province: Molong Volcanic Belt. Consists of medium-K calc-alkaline dacitic intrusion.||||||07-FEB-11
37468|Copper Hill Intrusive Complex|23214|5|Briefly described|p344|Ordovician|Ordovician|Age: 477Ma.||||||
37468|Copper Hill Intrusive Complex|24398|6|Mentioned|p259 Fig. 2|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37468|Copper Hill Intrusive Complex|62478|5|Briefly described|p88|Ordovician|Ordovician|Age inferred from text. Includes Fairbridge Volcanics? Ages: 455.4 +/- 1.0Ma, 449.1 +/- 1.5Ma. Includes two intrusive phases.||||||12-FEB-16
37468|Copper Hill Intrusive Complex|67107|5|Briefly described|p694, 700|||Hosts the Copper Hill Cu-Au porphyry and skarn deposits.|450 +/- 6 Ma (SHRIMP: Perkins et al., 1995).|||Intrudes Fairbridge Volcanics.|Mainly dacites and tonalites with calc-alkaline to high-K calc-alkaline affinity.|
37468|Copper Hill Intrusive Complex|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 3 intrusion. Hosts large Copper Hill porphyry Cu-Au deposit. Shown as Copper Hill Intrusive Complex"".|c. 450 Ma||||Medium-K calc-alkaline tonalite and dacite. Hosts Cu-Au porphyry-style mineralisation as stockworks and sheeted veins.|
37468|Copper Hill Intrusive Complex|73154|5|Briefly described|p78, p94|Sandbian|Darriwilian|Macquarie Arc, Molong structural belt. Medium-K magmatism, nominally Phase 3. 458.2+/-2.4 Ma zircon U-Pb age from Copper Hill tonalite sample, subsequently referred to as Copper Hill tonalite p84, p89 Tb.2, p92. Predates Eastonian carbonate deposition and inferred uplift in western Molong belt. Appears as Copper Hill intrusive complex p78, p94.|458.2+/-2.4 Ma zircon U-Pb||||Includes tonalite, andesite porphyry.|
37468|Copper Hill Intrusive Complex|73287|6|Mentioned|p678|||Macquarie Arc.||||||
68846|Copper Hill suite|24518|5|Briefly described|p67|Late Ordovician|Late Ordovician|Informal. See Copper Hill Suite. Age: ~450-445Ma.||||||04-MAY-05
68846|Copper Hill suite|73154|4|Described|p75, p84, p92|Llandovery|Late Ordovician|Macquarie Arc, Phase 3. Widespread but volumetrically minor, relatively silicic, medium-K. 458 Ma age from Copper Hill Intrusive Complex discussed in text in relation to age of the Copper Hill suite. 441-445 Ma age with ca. 467-571 Ma zircon inheritance interpreted by Crawford et al., (2007a, 2007b). See also Copper Hill Suite p92.|ca. 458 Ma, 441-445 Ma|Narromine Igneous Complex|||Dominantly dacitic, distinguished by prominent modal quartz, hornblende phenocrysts and a medium-K, calc-alkaline affinity.|
34549|Copper Mine Range beds|22772|5|Briefly described|Table13.1|Middle Cambrian|Early Cambrian|||||||
34549|Copper Mine Range beds|22857|5|Briefly described|Tb 13.1 (insert p70), p81, p91 Fig 14.7B|Cambrian|Early Cambrian|A lithological variant of the Teltawongee beds. Range is Rg. in text of Tb.. Geological Province: Kanmantoo Fold Belt. See also p75.||||||11-SEP-07
34549|Copper Mine Range beds|22858|5|Briefly described|p75,81,Fig14.7bp90-1||Early Cambrian|A lithological variant within the Teltawongee beds (Mills 1992).||||||
34549|Copper Mine Range beds|23245|5|Briefly described|p120|Middle Cambrian|Cambrian|||||||
34549|Copper Mine Range beds|44093|6|Mentioned|p47, p109|||Now considered to be a lithological variant within the Teltawongee beds. Unconformably underlies Cupala Creek Formation and Kandie Tank Limestone. See also p148 Appendix 1.||||||01-APR-05
34549|Copper Mine Range beds|50618|5|Briefly described|p249|Middle Cambrian|Early Cambrian|Represents the basal unit of the Cupala Creek Formation. Maximum Thickness: 90m.||||||
34549|Copper Mine Range beds|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Phyllite and sandstone.  May be equivalent to Teltawongee beds?||||||10-SEP-07
34549|Copper Mine Range beds|63790|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Red, purple and green phyllites, slates, siltstones, fine-grained laminated and micro-corss-bedded sandstones.||||||
34549|Copper Mine Range beds|63793|5|Briefly described|p22.|Middle Cambrian|Early Cambrian|Eastern edge of Coturaundee Range. Contains sponge spicule beds, trace fossils, and rare sponges and brachiopods.||Unit in Teltawongee beds.|||Extensive fault-bounded wedge of slates and siltstones, with rarer sandstones and dolomites.|
34549|Copper Mine Range beds|64671|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|May be equiv. to or conformably overlies Teltawongee beds; unconformably overlain by Kandie Tank Limestone. Red, purple and green phyllites, slates, siltstones, fine-grained laminated and micro-cross-bedded sandstones.||||||01-DEC-08
34549|Copper Mine Range beds|64680|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group.||||||
34549|Copper Mine Range beds|64683|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Red, purple and green phyllites, slates, siltstones, fine-grained laminated and micro-cross-bedded sandstones. Rare vertical and horizontal worm burrows, sponge spicule brds, sponges and brachiopods.||||||
34549|Copper Mine Range beds|64684|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Unconformably overlain by Kandie Tank Limestone, Cupala Creek Formation and Kayrunnera Group. Conformably overlie western Kara beds, faulted against Ponto Group. May be equlivalent to, or conformably overlie Teltawongee beds.||||||01-DEC-08
34549|Copper Mine Range beds|64686|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group.||||||
34549|Copper Mine Range beds|65381|6|Mentioned|p689 Fig. 2|Middle Cambrian|Early Cambrian|||||||
34549|Copper Mine Range beds|66623|6|Mentioned|p43.|||Recognised by Pogson and Scheibner (1971). Considered by Mills (1992) to be a distinctive variant of Teltawongee beds (now Group). Called Copper Mine Range beds by Scheibner & Basden (1998). Now Copper Mine Range Formation (this study).||||||
34549|Copper Mine Range beds|66929|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian||||||Red, purple and green phyllites, slates, siltstones, fine-grained laminated and micro-cross-bedded sandstones; rare worm burrows; sponge spicule beds, sponges and brachiopods.|
34549|Copper Mine Range beds|66933|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian||||||Red, purple and green phyllites, slates, siltstones, fine-grained laminated and micro-cross-bedded sandstones; rare vertical and horizontal worm burrows, sponge spicule beds, sponges and brachiopods.|
24876|Copperhannia Formation|34692|6|Mentioned|p185|||||||||
24876|Copperhannia Formation|68592|6|Mentioned|p1211|||Langley (1976), after unpublished work by Hobbs (1964). Discussed by Bradley (in Pickett, 1982) as a gradation between Box Ridge Formation and Kildrummie Formation. Now Copperhannia Member (of Cunningham Formation).||||||
25862|Coramba Beds|24127|5|Briefly described|p4|||||||||
25862|Coramba Beds|24129|5|Briefly described|p4|Carboniferous|Carboniferous|||||||
25862|Coramba Beds|29988|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25862|Coramba Beds|30911|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
25862|Coramba Beds|31695|4|Described|p255|||Mention Fig. 1, petrology||||||
25862|Coramba Beds|31802|4|Described|p137|||Refers Korsch (1972)||||||
25862|Coramba Beds|31806|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
25862|Coramba Beds|31993|6|Mentioned|p682|||||||||
25862|Coramba Beds|32671|6|Mentioned|Map legend|Carboniferous|Devonian|Dev.-Carb.||||||
25862|Coramba Beds|35171|6|Mentioned|p92|||||||||
25862|Coramba Beds|35257|6|Mentioned|Fig.18|||||||||
25862|Coramba Beds|35264|2|Defined|p16|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
25862|Coramba Beds|35757|6|Mentioned|p28|||Discussion re deformation.||||||
25862|Coramba Beds|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition.||||||
25862|Coramba Beds|36528|6|Mentioned|p182|||||||||
25862|Coramba Beds|36961|6|Mentioned|Fig.5|||||||||
25862|Coramba Beds|37438|6|Mentioned|p17|||||||||
25862|Coramba Beds|37808|6|Mentioned|p25|||||||||
25862|Coramba Beds|38806|5|Briefly described|p72|||||||||
25862|Coramba Beds|41550|5|Briefly described|p491|||||||||
25862|Coramba Beds|71628|5|Briefly described|p17:93|||||Coffs Harbour Association.||Is intruded by Emerald Beach Monzogranite.||
70588|Cordillo Surface""|61824|5|Briefly described|p128|Oligocene|Oligocene|This is the Silcrete of Wopfner (1974).  However, this age is disputed as "silcrete in the area clearly occurs at various levels within the Mesozoic sediment".||||||
70588|Cordillo Surface""|61825|5|Briefly described|p138|Oligocene|Late Eocene|See also "Cordillo Silcrete". Both of Wopfner and Twidale (1967) and Alley (1998). Geological Province:  Lake Eyre Basin.||||||05-JUN-06
68779|Corona chert|60648|6|Mentioned|p46|||Informal name.||||||
80445|Corrong metasediments|70718|5|Briefly described|p58, p82, p94, p117|Silurian|Ordovician|Informal name, interpreted entirely from geophysics. Aeromag. character: Only visible in tilt-filtered TMI RTP imagery. They appear as approximately parallel linearments 5-12 km long on a northeast-southwest trend. The anomalies are approximately 1 km wide and have a peak phase angle of approximately 12¿40 degrees.|||||Interpreted as turbiditic metasediments.|30-MAY-19
83052|Costal leucomonzogranites|73202|6|Mentioned|p639 Fig.10|Late Triassic|Late Triassic|New England Orogen, southern. Felsic I-type granitoids.|ca 233 Ma SHRIMP zircon|||||
81611|Cotambal Group|72263|6|Mentioned|p517|Late Devonian|Late Devonian|Geological province: Lachlan Orogen.||||Unconformable fault contact with Fairbridge Volcanics.||03-SEP-19
38861|Cotton Beds""|24417|6|Mentioned|p35|||Superseded by Cotton Formation.  Also previously known as "Cotton Series".||||||
81803|Cotton Group|72495|6|Mentioned|p230||| Exhibits low magnetisation and low Bouger gravity values.  [probable misspelling of Cotton Formation - used in Fig 9, also p230, and many other pages]|||||Siltstone.|02-MAR-20
39420|Covan Creek formation|24128|5|Briefly described|p29|||Informal name.||||||
24883|Cow Flat Volcanics""|33742|6|Mentioned|p116|||Refers Binns (1958) etc||||||
24883|Cow Flat Volcanics""|42413|5|Briefly described|p50|||Superseded by Vale Creek Formation 1987.||||||
37406|Cow Quarries limestone|23214|6|Mentioned|p140|||Binns (1958) replaced by Jericho Limestone and subsequently renamed Alton Limestone Member of Bells Creek Volcanics.||||||
35225|Cowal Conglomerate Unit|22797|6|Mentioned|Fig3, P839|||Informal unit of Miles (1993).||||||
35225|Cowal Conglomerate Unit|63283|6|Mentioned|p194 Fig. 2|Early Ordovician|Early Ordovician|Of the Cowal Igneous Complex. Geological Province: Junee-Narromine Volcanic Belt.||||||07-FEB-11
35225|Cowal Conglomerate Unit|63293|6|Mentioned|p468 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Golden Lava Unit. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35225|Cowal Conglomerate Unit|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
35225|Cowal Conglomerate Unit|70684|6|Mentioned|p74|Early Ordovician|Early Ordovician|Junee-Narromine Volcanic Belt||Cowal Igneous Complex.||||
37285|Cowal Igneous Complex|24007|4|Described|p329|||Same as "Lake Cowal Volcanic Complex" of Raymond et al. (2000b).||||||
37285|Cowal Igneous Complex|24518|6|Mentioned|p66|||Mainly medium-K rocks.||||||
37285|Cowal Igneous Complex|63277|6|Mentioned|p138|Early Ordovician|Early Ordovician|From the Maquarie Arc. Consists dominantly of dacitic porphyries, dorites and granodiorites. Geological Province: Lachlan Fold Belt.||||||
37285|Cowal Igneous Complex|63278|5|Briefly described|, p148, p145 Fig. 1, p146 Fig. 2a|Odrovician|Early Ordovician|Includes; Great Flood unit, Golden Lava unit Cowal Conglomerate unit. Geological Province: Junee-Narromine Volcanic Belt, LFB. Informal named units of this complex. Muddy Lake Diorite intrudes the Complex.||||||07-FEB-11
37285|Cowal Igneous Complex|63279|6|Mentioned|p167|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt. South part of the province.||||||
37285|Cowal Igneous Complex|63283|5|Briefly described|p185, p188, p194 Fig. 2, p191 Tb. 2|Late Ordovician|Early Ordovician|Age: 475-450Ma (Sm/ Nd Phase 1 andesite lava and Phase 2 intrusives). Geological Province: Junee-Narromine Volcanic Belt. See p193.||||||26-MAR-20
37285|Cowal Igneous Complex|63284|5|Briefly described|p255-264, p245 Fig. 2|||Includes; Golden Lava. Geological Province: Junee - Narromine Volcanic Belt. Consists of a sequence of trachytic lavas and volcaniclastics (Miles and Brooker, 1998).  Intruded by Muddy Lake Gabbro 466-456Ma (U-Pb zircon). See p255-264 for more information.||||||24-AUG-12
37285|Cowal Igneous Complex|63287|6|Mentioned|p343|||||||||07-FEB-11
37285|Cowal Igneous Complex|63292|6|Mentioned|p450|||Geological Province: Junee - Narromine Volcanic Belt.||||||
37285|Cowal Igneous Complex|63293|5|Briefly described|p467, p468 Fig. 2, p471|Late Ordovician|Early Ordovician|Underlain by Great Flood Unit at Cowal locality. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
37285|Cowal Igneous Complex|64963|5|Briefly described|p182 Fig. 2, p184|||Age: Intruded by Muddy Lake Gabbro 466-456Ma (U-Pb zircon, Crawford et al 2007c).||||||24-AUG-12
37285|Cowal Igneous Complex|67106|6|Mentioned|p673, 676-677, 679|Late Ordovician|Early Ordovician|Junee-Narromine Volcanic Belt. The authors suggest this requires redating.|450.9 +/- 4.5 Ma (SHRIMP: Crawford et al., 2007).|||||
37285|Cowal Igneous Complex|67107|5|Briefly described|p695, 700-701|Ordovician|Ordovician|Cowal district. Several Au deposits. Hosts various Ordovician mineralised monzogabbro to monzonite and granodiorite intrusions. The oldest and most primitive intrusive suite studied in this article.||||Is intruded by Muddy Lake Gabbro.|Volcanic-dominated rocks including diorite, trachyandesite lavas and volcaniclastic sedimentary rocks.|
37285|Cowal Igneous Complex|67322|5|Briefly described|p20-21|Darriwilian|Tremadocian|Junee-Narromine Volcanic Belt, Macquarie Arc. Comparable history to Narromine Igneous Complex (q.v.). Abuts the southernmost extent of Girilambone Group rocks. Occurs in the Condobolin - West Wyalong region. Described in detail by Crawford, Cooke and Fanning (2007).||||||21-FEB-18
37285|Cowal Igneous Complex|67847|5|Briefly described|p56|Middle Ordovician|Early Ordovician|Hosts the Cowal gold mine. Age given is Ar-Ar from a granodiorite within this unit. Geochemically similar to the Nelungaloo Volcanics (Wilson et al., 2007b) and on that basis has a suggested early Ordovician age.|465.7 +/- 5 Ma (Miles and Brooker, 1998)|||||26-MAR-20
37285|Cowal Igneous Complex|70178|4|Described|p2, p3 fig. 1, p4 fig. 2, p5, p8|Ordovician|Ordovician|Macquarie Arc. Previously termed Lake Cowal Volcanic Complex. Includes six unnamed members. Gold mineralisation is either structurally controlled or porphyritic.|466 Ma - 439 Ma?|||Includes Muddy Lake Diorite.|Characterised by volcaniclastic sedimentary (hyaloclastite breccia, sandstone, mudstone) successions that have been intruded by monzodiorite, monzonite, granodiorite and diorite stocks and dykes; trachyandesite.|17-JAN-17
37285|Cowal Igneous Complex|70684|5|Briefly described|p3, p54, p74|||Junee-Narromine Volcanic Belt.|||Cowal Conglomerate Unit, Golden Lava Unit, Great Flood Unit.|||
37285|Cowal Igneous Complex|72495|5|Briefly described|p218-219, 225-226, 228, p234-236|Darriwilian||Best defined by geophysics with some exploration drillhole data. Lies between the Booberoi Shear Zone and the Marsden Thrust. Lithology derived from minesite stratigraphy of Miles and Brooker (1998). Minimum age is constrained from a K-Ar date of 456 +/- 5 Ma from the intruding Muddy Lake Diorite and from an Ar-Ar date of 465.7 +/- 1 Ma derived from an unnamed intruding granodiorite (Perkins, 1993).||||Intruded by the Muddy Lake Diorite.|Basal conglomerate overlain by trachyandesitic lavas and breccieas which is subsequently overlain by redeposited pyroclastics.|26-MAR-20
83272|Cowal Intrusive Complex|73154|6|Mentioned|p75|Late Ordovician|Late Ordovician|Zircon U-Pb data interpreted to show 475-460 Ma inheritance in a 445 Ma magma (Crawford et al., 2007a, 2007b).|~445 Ma||||Includes granodiorite.|
25863|Cowal Member|22857|5|Briefly described|p446 App.1, Tb.A1.6|Silurian|Silurian|Of the Ina Volcanics. Massive coarse rhyolitic tuff porphyry. Max. thickness: ~1km. ||||||
25863|Cowal Member|35503|2|Defined|p206|Silurian|Silurian|New name refs Kemezys (1976). Part of Ina Volcanics. Prob. Silurian||||||26-MAY-08
25863|Cowal Member|40328|6|Mentioned|p41|||||||||
38911|Cowal Member""|24417|5|Briefly described|p49|||Formerly a member of Ina Volcanics (Kemezy, 1976). Name discontinued as a seperate unit and now included as part of Ina Volcanics.||||||
38957|Cowal conglomerate unit""|24417|6|Mentioned|p182|||||||||
68851|Cowal intrusives|24518|6|Mentioned|p67|||Informal name - refers to rocks of the Cowal Igneous Complex.||||||
34144|Cowangarra Formation|22616|6|Mentioned|Fig.1 p670|Devonian|Devonian|||||||
34144|Cowangarra Formation|44093|5|Briefly described|p67 Fig. 6.6|Devonian|Devonian|Misspelt. In the South Hastings Block. See also Cowangara Formation. Geological Province: New England Fold Belt.||||||
24885|Cowra Formation|24125|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
24885|Cowra Formation|29591|5|Briefly described|p48|||||||||
24885|Cowra Formation|31589|6|Mentioned|p181|||||||||
24885|Cowra Formation|32020|4|Described|p36|||Pleistocene. Refers Williamson (1964)||||||
24885|Cowra Formation|32021|6|Mentioned|p42|||||||||
24885|Cowra Formation|34600|4|Described|p547|||Invalid||||||
24885|Cowra Formation|34813|6|Mentioned|p63|||||||||
24885|Cowra Formation|35187|6|Mentioned|Table1|||||||||
24885|Cowra Formation|41136|5|Briefly described|p215|||||||||
24885|Cowra Formation|43578|6|Mentioned|p337|Pleistocene|Pliocene|||||||
24885|Cowra Formation|43780|6|Mentioned|p6|Pleistocene|Pliocene|||||||
24885|Cowra Formation|45168|6|Mentioned|p19|||||||||
24885|Cowra Formation|50616|5|Briefly described|p287|Pleistocene|Pleistocene|Contains two members: an upper silty clay unit forming the modern floodplain and terraces in the Cowra area; and lower sand and gravel unit (similar to Bunglegumbie unit) disconformably overlying the Lachlan Formation. Of the Lachlan River area.||||||
24885|Cowra Formation|61155|5|Briefly described|p19|Pleistocene|Late Pliocene|Overlies the Lachlan Formation. Thickness: 30m. Geological Province: Lachlan Valley. ||||||
37458|Cowra Formation""|23214|4|Described|p280|Pleistocene|Pleistocene|Williamson (1969). Informal.||||||
37458|Cowra Formation""|24106|6|Mentioned|p184|||||||||
37458|Cowra Formation""|24417|5|Briefly described|p198|Pleistocene|Pleistocene|Of Williamson (1964, 1969).  Technically invalid name due to prior use of Cowra Granodiorite.||||||
68264|Cowra formation|24551|6|Mentioned|p425|||||||||
68264|Cowra formation|62349|6|Mentioned|p73|||Informal name. Geological Province: Lachlan Fold Belt.||||||03-JUL-06
39807|Cowridge Siltstone, lower|24248|6|Mentioned|p72|||Informal - see Cowridge Siltstone.||||||
24231|Cowriga Limestone|23214|6|Mentioned|p62|||Superseded by Cowriga Limestone Member.||||||
24231|Cowriga Limestone|24265|6|Mentioned|p1451|||Geological Province: Lachlan Fold Belt||||||
24231|Cowriga Limestone|24268|6|Mentioned|p1536 Fig.2|||Geological Province: Lachlan Fold Belt||||||
24231|Cowriga Limestone|39325|6|Mentioned|p433|||||||||
24231|Cowriga Limestone|39663|6|Mentioned|Table 1|||See also Table 4||||||
24231|Cowriga Limestone|49794|5|Briefly described|p8|||Used 1977||||||
30743|Cox Creek Basalt|43362|14|Not recorded|Map Legend||Tertiary|(Provisional first edition)||||||
34686|Cox Subgroup|22859|6|Mentioned|p216|||Of Connolly 1962, 1969a, b. Superseded by Gibbons Creek Sandstone.||||||
70084|Cox Subgroup""|22857|6|Mentioned|p216|||Of Conolly (1962, 1969a,b). Superseded by Gibbons Creek Sandstone (Lambie Group).||||||
37444|Coxs Formation|23214|6|Mentioned|p240|||Now included in Gibbons Creek Sandstone.||||||
38463|Coynallan Suite|24133|6|Mentioned|p73|||Geological Province: Lachlan Fold Belt.||||||
23517|Crack Hardy Point Quartz Monzodiorite|40882|6|Mentioned|p26|||||||||
23517|Crack Hardy Point Quartz Monzodiorite|49705|5|Briefly described|p20|||||||||
74656|Cranky Corner Suite|24040|6|Mentioned|p477|||Probably not intended as a formal name? and refers to the basalts at Cranky Corner.||||||
37388|Cranky Corner basalt|24040|6|Mentioned|p468 Fig. 1|||Informal name. Geological Province: Cranky Corner Basin in the Tamworth Belt.  Also referred to as the Cranky Corner series (p471) and as Cranky Corner basalts (p475).||||||21-AUG-08
80146|Cranliegh Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin. [Mis-spelling of Cranleigh.]||Maules Creek Formation.||||
41393|Craven Coal Measures""|44244|5|Briefly described|p167|Late Permian|Late Permian|Superseded by "Stratford Coal Measures" (Bewley, 1971), then "Lower Craven Coal Measures" (George, 1971, 1975); returned to "Stratford C.M." (Crapp, 1973).||||||27-JUL-04
41394|Craven Coal Measures, Lower|44244|5|Briefly described|p168 Tb. 2|Late Permian|Late Permian|Superseded by Craven Subgroup (Gloucester Coal Measures).  Replaced Stratford Coal Measures, and Craven Coal Measures before that.||||||27-JUL-04
41398|Craven Coal Measures, Lower""|44244|6|Mentioned|p167|Late Permian|Late Permian|Of George (1971, 1975) - to replace the "Craven Coal Measures".  Then recombined with "Upper Craven Coal Measures" by Crapp (1973) to form the "Stratford Coal Measures".||||||27-JUL-04
41399|Craven Coal Measures, Upper|44244|5|Briefly described|p168 Tb. 2|Late Permian|Late Permian|Superseded by Craven Subgroup.  Replaced Stratford Coal Measures, and Broad Gully Formation before that.||||||
41400|Craven Coal Measures, Upper""|44244|6|Mentioned|p167|Late Permian|Late Permian|Of George (1971, 1975).  Replaced Broad Gully Formation (Louhgan, 1955).  Recombined with "Lower Craven C.M." back to "Stratford Coal Measures" (Crapp, 1973).||||||
41401|Craven Subgroup, upper|44244|6|Mentioned|p174|Permian|Permian|Not intended as a formal name - see Craven Subgroup.  Geological province: Myall Block.||||||27-JUL-04
38453|Cravensville Formation""|24133|6|Mentioned|p36|||Informal - see Cravensville Formation.  Geological Province: Lachlan Fold Belt.||||||
38453|Cravensville Formation""|60503|6|Mentioned|p114|||Informal - see Cravensville Formation. ||||||
34276|Crawford Formation""|22679|6|Mentioned|p 31|||||||||
34276|Crawford Formation""|23214|5|Briefly described|p147|||Informal sub-unit of Box Ridge Volcanics.||||||
34276|Crawford Formation""|44244|6|Mentioned|p206|||Of Engel (1962).  Synonymous with Booti Booti Sandstone (part) and Muirs Creek Conglomerate (part).||||||26-MAR-18
24889|Cremorne Seam|42182|6|Mentioned|p300|||||||||
78882|Crinoid Limestone Member|65214|6|Mentioned|p272|Early Devonian|Early Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||Taemas Limestone, Murrumbidgee Group.||||19-MAY-14
37956|Crokers Well Suite|24307|5|Briefly described|p971|Mesoproterozoic|Mesoproterozoic|||||||
77430|Croppies Gunyah Rhyolite Member|66300|5|Briefly described|p36,41,45-50.|Early Devonian|Early Devonian||414.0 +/- 2.5 Ma.|Said in this study to be a unit in Long Flat Volcanics.||Is overlain by Manar Ignimbrite. Possible lateral equivalent to Kadoona Dacite Member or Toggannoggra Rhyolite Member.|Weakly-foliated, densely-welded rhyolitic ignimbrite.|29-OCT-13
69856|Crowl Formation|61213|5|Briefly described|p319 Fig. 3, p322|Emsian|Lochkovian|Overlies the Bundycoola Formation. Frasnian age also mentioned in text. Geological Province: Darling Basin. ||||||
69856|Crowl Formation|64964|3|Fully described|p160, p163, p172|||Marker unit of Mulga Downs Gp. Thickness: >2.8km. Comprises fine-grained, planar-bedded sandstone with minor ~50cm-thick cross-beds, with a coarse-grained, pebbly sandstone above; with abundance of vein quartz clasts - form white line in air photographs.||||||08-APR-09
69856|Crowl Formation|67562|5|Briefly described|p97 Fig.4, p102 Fig.8, p106, p108, p111|Frasnian|Givetian|> 2.3 km thick. Mid Givetian-Late Frasnian age. Deposition was on distal braidplains. Includes a pebbly sandstone marker bed.||||Overlies Mount Jack Beds.|Includes sandstones.|23-JAN-17
31208|Cudal Shale|23214|6|Mentioned|p113|||Replaced by Cudal Group.||||||
31208|Cudal Shale|43479|14|Not recorded|p105,116|Late Silurian|Early Silurian|||||||
35419|Cudgegong Volcanics""|23170|6|Mentioned|p40|||Superseded by the Sofala Volcanics.||||||
30808|Culcairn Porphyry|43384|14|Not recorded|Map Legend||Devonian|||||||
33408|Culela Member|23392|2|Defined|p20||Famennian|Contains the Culela fish fauna. Correlation with Eurow Formation (Parkes 1:100 000). Of the Weddin Formation. Geological Province: Lachlan Fold Belt. Max Thickness: 113m||||||
33408|Culela Member|24417|3|Fully described|p148|Late Devonian|Late Devonian|Of Weddin Sandstone.  Max. thickness: 113m.||||||
33408|Culela Member|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Weddin Sandstone (Hervey Group).||||||13-JUL-04
73992|Cullendore Granite|69639|4|Described|p2, p6, p8, p192-p197, p222, p239|Triassic|Triassic|New England Orogen. Spatially related to the Stanthorpe Granite. Previously regarded as a member of the Stanthorpe Supersuite despite being geographically seperated from the main body, is less magnetised and displays subtle compositional differences relative to the Stanthorpe Supersuite. Sampling locality, petrography and geochronology are discussed. In contact with the Undercliffe Falls Monzogranite although relationship between these two units is unclear.|246.9 +/- 1.4 Ma (SHRIMP U-PB)|||Intrudes the Maryland Granite, Razorback Creek Mudstone. Overlain by the Marburg Subgroup.|Medium- to fine-grained porphyritic pale pink-grey granite.|
73992|Cullendore Granite|70217|5|Briefly described|p74 tbl 14.1|Anisian|Olenekian|New England Orogen.|246.9 +/- 1.4 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
25867|Cullens Creek Granite|33476|2|Defined|p95|Triassic|Permian|Permian - Triassic||||||
25867|Cullens Creek Granite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
25867|Cullens Creek Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
25867|Cullens Creek Granite|42378|6|Mentioned|Table 1 P11|||||||||
25867|Cullens Creek Granite|43008|5|Briefly described|map legend|||||||||
25867|Cullens Creek Granite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
25867|Cullens Creek Granite|71628|6|Mentioned|p19: 23, 173-174|||Thomson (1973). That account was comprehensively modified by subsequent workers. Now Cullens Creek Granodiorite.||||||
25867|Cullens Creek Granite|72528|5|Briefly described|p2, p3-4,  p90-95, p110, p127.|Middle Triassic|Middle Triassic|Magmatic crystallisation age determined. Dates indistinguishable from Koreelan Creek Granodiorite and temporal associations with Cullens Creek and Koreelan Creek plutons is shown. This is a small intrusive complex located c. 24 km southwest of Urbenville. Shown as part of the New England Orogen.|246.7+/-1.5 Ma U-Pb SHRIMP|Cullens Creek Suite||Intrudes Emu Creek Formation. Unconformably overlain by Koreelah Conglomerate Member. Cut by epithermal-like polymetallic veins.|Dated sample is a medium-grained, massive, pale grey-pink granite/granodiorite.|01-FEB-21
73890|Cullens Creek Suite|71628|5|Briefly described|p19:24|||No longer included in Clarence River Supersuite.|||Cullens Creek Granodiorite.|||
73890|Cullens Creek Suite|72528|5|Briefly described|p90.|Middle Triassic|Middle Triassic|Quoted age from Cullens Creek Granite.|246.7+/-1.5 Ma|Clarence River Supersuite|Includes Cullens Creek Granite|||
34249|Cumberland Rhyolite""|22638|6|Mentioned|p64|||Boraig Group. Correlates with Cowcumbala Rhyolite.||||||
27384|Cumberland Sub-Group|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
27384|Cumberland Sub-Group|29751|6|Mentioned|p10|||||||||
27384|Cumberland Sub-Group|29900|6|Mentioned|Table 1|||||||||
27384|Cumberland Sub-Group|29901|6|Mentioned|p169|||||||||
27384|Cumberland Sub-Group|30006|6|Mentioned|p7|||||||||
27384|Cumberland Sub-Group|31062|6|Mentioned|p478|||Triassic. On Table||||||
27384|Cumberland Sub-Group|31128|6|Mentioned|Table 1|||||||||
27384|Cumberland Sub-Group|31879|5|Briefly described|p294|||Permian||||||
27384|Cumberland Sub-Group|31887|6|Mentioned|p5|||||||||
27384|Cumberland Sub-Group|32618|6|Mentioned|Table 1|||Perm. Strat. table||||||
27384|Cumberland Sub-Group|32938|6|Mentioned|Fig.2|||||||||
27384|Cumberland Sub-Group|33334|6|Mentioned|Table 3|||Perm.||||||
27384|Cumberland Sub-Group|33869|6|Mentioned|Fig.2|||||||||
27384|Cumberland Sub-Group|34038|5|Briefly described|p435|||||||||
27384|Cumberland Sub-Group|34060|6|Mentioned|p24|||Permian. Table||||||
27384|Cumberland Sub-Group|34205|6|Mentioned|p15|||||||||
27384|Cumberland Sub-Group|34335|6|Mentioned|p369|||Permian||||||
27384|Cumberland Sub-Group|34399|6|Mentioned|p312|||||||||
27384|Cumberland Sub-Group|34569|6|Mentioned|p8|||Correlates with Tomago Coal Measures. See P9,Fig.2. Permian||||||
27384|Cumberland Sub-Group|34605|4|Described|p372|||Stratigraphic units||||||
27384|Cumberland Sub-Group|36042|6|Mentioned|p20|||||||||
27384|Cumberland Sub-Group|36220|4|Described|p38|||See also Table 10.||||||
27384|Cumberland Sub-Group|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27384|Cumberland Sub-Group|37089|5|Briefly described|p208|||||||||
27384|Cumberland Sub-Group|37090|6|Mentioned|p219|||||||||
27384|Cumberland Sub-Group|39307|6|Mentioned|Table 22.1|||||||||
27384|Cumberland Sub-Group|39308|5|Briefly described|p514|||||||||
27384|Cumberland Sub-Group|39309|4|Described|p121|||See also Table 7.2||||||
27384|Cumberland Sub-Group|42182|5|Briefly described|p300|||||||||
27384|Cumberland Sub-Group|43320|14|Not recorded|p9,10,28,29,31|||Lower part of Illawarra Coal Measure||||||
27384|Cumberland Sub-Group|43383|14|Not recorded|p20,Fig.5||Permian|||||||
27384|Cumberland Sub-Group|45090|6|Mentioned|p28|||Relationship of rock units||||||
33793|Cumberoona Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Strongly foliated porphyritic hornblende-biotite metamict allanite soda-diorite.||||||13-MAY-04
38928|Cumbijowa Adamellite""|24417|6|Mentioned|p105|||Superseded by Cumbijowa Granite.||||||
35079|Cumborah Formation|23053|6|Mentioned|Fig10p17|Late Miocene|Middle Miocene|Misspelling of Cumborah Gravel of Taylor (1976)? used in the Walgett-Cumborah region.  Gravels shown on the Nyngan & Walgett 1:250 000 sheets asTg have been correlated with this unit.||||||
24234|Cumnock Limestone|40328|6|Mentioned|Fig.12(B3)|||||||||
23526|Cunglebung Creek Beds|38755|6|Mentioned|Fig.1|||||||||
72318|Cunningham Formation, lower|24278|6|Mentioned|p1765|||Informal - see Cunningham Formation.||||||
30809|Cunningham Group|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
30809|Cunningham Group|43523|14|Not recorded|map p427|||||||||
24895|Cunningham formation|30099|6|Mentioned|p396|||||||||
76049|Cunninyuek Granite Suite|66934|6|Mentioned|Map legend|Late Devonian|Late Devonian|Informal name. |||Includes Baldon granite.|||
41600|Cupala Creek Formation Conglomerate|50618|5|Briefly described|p249 Fig. 3|Late Cambrian|Late Cambrian|Informal reference to conglomerate of the Cupala Creek Formation?||||||
41601|Cupala Creek Formation conglomerate|50618|5|Briefly described|p251, 255|||Informal-see Cupala Creek Formation.||||||
78267|Cupala Creek Sill|67562|6|Mentioned|p105 Fig.11|||||||||
76149|Curalle silcrete|66623|5|Briefly described|p269, p277.|||Equivalent to Cordillo Silcrete in SA and the top of the Canaway profile in Qld.||Surficial part of the informal Canaway profile of surface weathering with silcrete cap.||||
70085|Curdimurka Subgroup, lower|22857|6|Mentioned|p65|||Informal - see Curdimurka Group.||||||
82818|Curga Burga Volcanics|71600|5|Briefly described|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.||Unit of Gregra Group.|||Latitic, crystal-lithic sandstone, breccia, siltstone, tuff; latite and lesser andesite, basalt; minor allochthonous limestone, quartzose sandstone|
77171|Curlewis member|68003|5|Briefly described|p75 Fig.3-r.|Recent|Pliocene|Mooki Valley, Liverpool Plains.||||Overlies Breeza member.|Clay, sand and gravel.|
70619|Curnamona metabasites|62373|5|Briefly described|p511|||Informal term for a suite metabasites in the southern Curnamona Province, with informal group names such as Mingary, Mundi, Outalpa, Plumbago, Waukaloo and Weekeroo which are informal nomenclature.||||||
41248|Curra Curra Conglomerate|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Canangle Subgroup. Red-purple conglomerate with minor sandstone and siltstone.||||||
41199|Curra Granite|50554|6|Mentioned|Map legend|Silurian|Silurian|Misspelt - intended as Currah Granite.   Shown in Solid Geology and Structure map/legend.||||||21-JUN-04
31406|Curra Keith Ignimbrite Tongue|44244|6|Mentioned|p304|||||||||
27137|Curra Keith Tongue|22857|5|Briefly described|p508 App.1 Tb.A1.8|Carboniferous|Carboniferous|Of the Isismurra Formation. Ignimbrite at top of Native Dog Member. Max. thickness: 95m. Geological Province: Tamworth Forearc Basin.||||||
27137|Curra Keith Tongue|24603|6|Mentioned|p897 Fig. 17|||In the Ruochel Block.  Geological Province: Tamworth Belt.||||||
27137|Curra Keith Tongue|32529|3|Fully described|p199|||||||||
27137|Curra Keith Tongue|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27137|Curra Keith Tongue|32869|6|Mentioned|p168|||Pt. of Isismurra Formation||||||
27137|Curra Keith Tongue|44244|5|Briefly described|p35|||Max. thickness: 70m.  Geological Province: Rouchel Block.||||||16-AUG-04
27137|Curra Keith Tongue|45088|2|Defined|p50|Early Carboniferous|Early Carboniferous|||||||
27137|Curra Keith Tongue|50099|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Consists of two distinct buff to pale purple ignimbrites, 70 and 20m thick, separated by a sequence of sandstone, shale and conglomerate. Continuous with lowermost part of Native Dog Member.||||||
27137|Curra Keith Tongue|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Of the Isismurra Formation.  Overlies: Ayr Conglomerate Member.||||||
27137|Curra Keith Tongue|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Age: 342 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Rouchel Block||||||
27137|Curra Keith Tongue|62095|5|Briefly described|p280 Appdx., p260 Tb. 1|Early Carboniferous|Early Carboniferous|Of Isismurra Formation. Overlies Ayr Conglomerate Member; overlain by a thin succession of sedimentary rocks and Oakfields Tongue.  Age: 349.5+/-1.8Ma (at Tournaisian-Visean boundary). Geol. Prov: Rouchel block/Tamworth Belt. See also Plate 1, p258.||||||25-MAY-06
27137|Curra Keith Tongue|65107|5|Briefly described|p275, 276 Fig 4, 282, Fig 11 p286-7|Visean|Visean|Rouchel Block. Of Isismurra Formation. Age: 342.1+/-3.2 Ma from SHRIMP U-Pb zircons||||||24-NOV-09
27137|Curra Keith Tongue|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Isismurra Formation||||
27137|Curra Keith Tongue|73487|6|Mentioned|p566|Visean|Visean|Rouchel Block. Orthotetes australia zone.||||||
40464|Curra Keith Tonque|24603|6|Mentioned|p898|||Misspelt - see Curra Keith Tongue.  Age: 342+/-3.2Ma (Roberts et al, 1995a).  Geological Province: Tamworth Belt.||||||
41110|Curra Sandstone|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.||||||
28490|Currabubula Tillite|42713|5|Briefly described|Fig. P18|||Variation on Currabubula Formation||||||
30824|Curragong Volcanic Complex|22508|5|Briefly described|p3||Early Devonian|Cobar Supergroup, Lachlan Fold Belt. Overlies Weethalle granite||||||
30824|Curragong Volcanic Complex|22768|5|Briefly described|Fig16.7p167|Early Devonian|Late Silurian|||||||
30824|Curragong Volcanic Complex|22857|5|Briefly described|p448 App.1, Tb.A1.6|Devonian|Devonian|Aphanitic and quartz-feldspar phyric voclanics, tuff, agglomerate, basal feldspathic arenite. Geological Province: Darling Basin. See also p167 Fig. 16.7||||||
39815|Currajong Limestone Member, lower|24250|6|Mentioned|p114|||Informal - see Currajong Limestone Member||||||
39816|Currajong Limestone Member, upper|24250|6|Mentioned|p120|||Informal - see Currajong Limestone Member||||||
38857|Currajong Park Beds""|24417|5|Briefly described|p24|||Informal subdivision of Gunningbland Formation.||||||
25869|Currango Beds|30332|2|Defined|p120|Late Silurian|Late Silurian|Prob.Upper Silurian||||||
25869|Currango Beds|32672|6|Mentioned|p672|||||||||
25869|Currango Beds|45147|6|Mentioned|M78|||||||||
30098|Currawalla Formation|22857|4|Described|p412 App. 1 Tb. A1.4.|Late Ordovician|Early Ordovician|Of the Tallebung Group. Thinly bedded laminated carbonaceous mudstone and siltstone. Geological Province: Wagga Marginal Basin.||||||
30098|Currawalla Formation|43089|5|Briefly described|Map Legend|||Of Tallebung Group.||||||26-MAR-08
30098|Currawalla Formation|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Massive or laminated black shale to siliceous mudstone, minor thin interbeds of fine sandstone.||||||10-APR-08
30098|Currawalla Formation|70950|6|Mentioned|p1029|||Geological province: Central Lachlan Orogen. Formerly of Tallebung Group (of Trigg 1987; see Colquhoun, Hendrickx and Meakin 2005a). ||Unit of Bendoc Group.||||
74756|Currawalla Shale""|61964|6|Mentioned|p30|||Of MacRae and Pogson (1990) unpubl. Informal name suggested for the thin-bedded sequence (of Trigg 1987) within the former Tallebung Group.Now adopted formally for a unit of the Bendoc Group. ||||||
24897|Currawang Volcanics""|32483|6|Mentioned|p24|||Refers Graylin (1966,unpubl.)||||||
80756|Currawinya granite|71860|5|Briefly described|p7|||Informal name. Age is a SHRIMP U-Pb date.|381.5 +/- 2.4 Ma (Bultitude et al, 2012)||||Monzogranite.|
32252|Currawong Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh21. Misspelling of Currowong Granodiorite.||||||
32252|Currawong Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
81171|Currawynnia Formation|72296|5|Briefly described|p9|||Longman and Meares (1971). Correleted with Tritton Formation. Evidently now included in Narrama Formation.||||Said to unconformably overlie Wilga Downs Metamorphics. Equivalent to the Tritton Formation.||20-JUN-19
70009|Curricabark formation|61766|6|Mentioned|p68|Late Devonian|Middle Devonian|Informal name. Volcaniclastic sediments and minor basalt flows.||||||
24898|Currububula Formation|35803|6|Mentioned|p321|||Misspelling of Currabubula Formation?||||||
73674|Currumburrama Igneous Complex|63278|5|Briefly described|p145 Fig. 1, p149|||Includes; Jinerangle Formation. Geological Province: Junee-Narromine Volcanic Belt, LFB. Consists of andesitic lavas and volcaniclastics intruded by monzodiorites, diorites, monzonites and granites, near the southeastern edge of the complex.||||||07-FEB-11
73674|Currumburrama Igneous Complex|70178|6|Mentioned|p4 fig. 2|Ordovician|Ordovician|Macquarie Arc.||||||
73674|Currumburrama Igneous Complex|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
73674|Currumburrama Igneous Complex|72495|5|Briefly described|p217-219,225-26,228,233-34,235, 240-41|Late Ordovician|Late Ordovician|Approximately 44 x 16km^2. Occurs to the east of the Tullamore Syncline. Coincides with individual highs to the south of the Canonbar Igneous Complex in the Junee-Narromine volcanic belt. Best defined by geophysics with some exploration drillhole data. |||Includes the Jingerangle Formation.||Basalt to andesitic lavas and volcaniclastic rocks intruded by monzonite to monzodiorites.|26-MAR-20
79847|Currumburrama volcanics|61893|5|Briefly described|p237, p249|||Caragabal-Quandialla district. Only recognised by its distinctive geophysical response. Associated with Jingerangle Formation.||||||22-MAY-17
30222|Curruwong Basalt|43128|5|Briefly described|Fig.6,p476||Silurian|Misspelling of Currawong Basalt?||||||
28492|Cusack Creek member|35526|6|Mentioned|p90|||||||||
34829|Cusin Creek granite|22962|6|Mentioned|p73,76||Statherian|Misspelling of Cusin Creek Granite.||||||10-SEP-19
76810|Cusins Creek Pluton|64743|6|Mentioned|p344 Fig.5. |||Intruded the Broken Hill Block during the Olarian Orogeny.|1596 +/- 3 Ma.|||||
82893|Cuttaburra Sandstone|73177|6|Mentioned|1114 Fig.16|||[probably sample description rather than unit name]||Warratta Group.||||
82871|Cuttaburra granite|72951|5|Briefly described|p1013, p1020, p1025|Ludlow|Wenlock|Thomson Orogen, southeast. I-type granodiorite. Granodiorite named 'Cuttaburra granite' with SHRIMP U-Pb zircon isotope analyses from Chisholm et al. (2014). Interpreted to intrude the Warratta Group. eHf = -6.8 +/- 1.6, and d18O = 7.33 +/- 0.16. See also p1024, 1025,1029. Discussed as 'granite, Cuttaburra' p1013, 1020, 1025.|428.3 +/- 2.8 Ma|||Interpreted to intrude Warrata Group.|Granodiorite. Felsic biotite granite.|
79646|Cuttaburra granite""|69511|5|Briefly described|p2, p34-39, p44, p48|Late Silurian|Late Silurian|Cuttaburra (Louth) region, Thomson Orogen. The sample dated is from the CUT A (drillhole 01) at 597m depth by Thomson Resources. Geochemical classification (S- or I-type) is uncertain. This age is indistinguishable from several S-type Koetong Supersuite plutons to the south, and is similar to the S-type Thule Granite in the Nymagee region.|428.3 +/- 2.8 Ma.||||Medium-grained, porphyritic granodiorite; crystals of feldspar, quartz and biotite up to 4.5mm long occur in a coarsely recrystallised groundmass.|
82471|Cuttaburra granites|72914|6|Mentioned|p16|||[Unsure whether this refers to an informal unit name or more generally to granites from the Cuttaburra borehole area]. Plots in the Cu-Mo mineralisation field based on the classification scheme of Blevin et al. (1996) and Blevin (2004).||||||
69958|Cymbric Vale Rhyolites|22671|6|Mentioned|p844 Fig. 3a and 3b|||This is most likely an informal reference to rhyolites within the Cymbric Vale Formation.  See also Cymbric Vale rhyolites.||||||18-JAN-06
69962|Cymbric Vale rhyolites|22671|6|Mentioned|p845|||See also Cymbric Vale Rhyolites - both informal names - see Cymbric Vale Formation.||||||
31370|Cymbric Vale tuff|43560|6|Mentioned|p235|||Informal name. Variation on Cymbric Vale Formation?||||||
31370|Cymbric Vale tuff|64829|6|Mentioned|p1084|Cambrian|Cambrian|Informal name for rocks dated at 517.8+/-21Ma (SHRIMP) in NSW.||||||07-FEB-11
24899|Cypress Hill Volcanics|23214|5|Briefly described|p70|||||||||
24899|Cypress Hill Volcanics|32154|6|Mentioned|p181|||Stratigraphy. Refers Vandyke (1970 unpubl.)||||||
24899|Cypress Hill Volcanics|33611|3|Fully described|p125|||||||||
24899|Cypress Hill Volcanics|39663|6|Mentioned|Table 1|||See also Table 4||||||
24899|Cypress Hill Volcanics|40136|5|Briefly described|p22|||||||||
24899|Cypress Hill Volcanics|40328|6|Mentioned|p160|||||||||
35423|Cypress Hill Volcanics""|23170|6|Mentioned|p48|||Name abandoned when Oakdale Group reduced to Oakdale Formation.||||||
83935|D'Aguilar metamorphic complex|70329|6|Mentioned|p3 Fig.3|Early Permian|Early Permian|New England Orogen.||||||
25871|Dairymans Beds|30332|2|Defined|p119|Ordovician|Ordovician|L.or M.Ordovician. Refs Bein 68 unpub. Part of Kiandra Beds?||||||
25871|Dairymans Beds|40136|6|Mentioned|p41|||Correlative of Temperance Formation.||||||
42035|Dalgety Adamellite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Berridale Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
26511|Dalgety Granite|42726|5|Briefly described|map legend|Silurian||299.  Of the Dalgety Suite (Dalgety Supersuite).  Formal name not intended. Variation on Dalgety Granodiorite.||||||09-FEB-05
68782|Dalwood Group, Lower|60281|6|Mentioned|p54|Early Permian|Early Permian|Informal - see the Dalwood Group. Term applied to the combined Lochivar and Allandale Formations. Combined thickness is 1090m. Geological Province: Sydney Basin.||||||
68170|Dalwood Group, Upper|60281|6|Mentioned|p56|Early Permian|Early Permian|Informal - see Dalwood Group. Refers to the Rutherford and Farley Formations together.  Geological Province: Sydney Basin.||||||22-MAR-05
41593|Dalwood Group, lower|44244|6|Mentioned|p274|Early Permian|Early Permian|Informal - see Dalwood Group.||||||
41594|Dalwood Group, upper|44244|6|Mentioned|p299|Early Permian|Early Permian|Informal - see Dalwood Group.||||||16-AUG-04
69462|Dalwood group|61201|6|Mentioned|p6|||Informal name.||||||
24901|Dalwood volcanics|39288|6|Mentioned|Fig.3.4|||||||||
26512|Danswell Creek Granite|23550|4|Described|p504|||See also Fig 1 p502 and p509. Wangrah Suite. Lachlan Fold Belt.||||||
26512|Danswell Creek Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Danswell Creek Granodiorite.||||||
26512|Danswell Creek Granite|71206|6|Mentioned|p373, 377|||Lachlan Fold Belt.||Wangrah Suite.|||Aluminous A-type granite.|
42208|Danswell Creek granite|24456|6|Mentioned|p328, 329 Tb.1|||Informal name.||||||26-NOV-04
32952|Dapto Flow|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
81859|Daraboolgie Volcanics|72495|6|Mentioned|p225|Ordovician|Ordovician|Included in the Parkes Volcanics. Age inferred. [Misspelling of Daroobalgie Volcanics]||||||
41198|Darbeys Ridge Conglomerate|50554|5|Briefly described|Map legend|Devonian|Devonian|Of the Yarra Yarra Creek Group.||||||
38920|Darby Conglomerate Member""|24417|5|Briefly described|p78|||Of "Weelah Formation".  Superseded by Darbys Ridge Conglomerate and now included in Yarra Yarra Creek Group.||||||
32245|Dargals Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah6||||||
32245|Dargals Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
26513|Darghals Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
26513|Darghals Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
24904|Darkes Forest Sandstone Member|29900|6|Mentioned|p169|||||||||
24904|Darkes Forest Sandstone Member|30006|6|Mentioned|p13|||||||||
24904|Darkes Forest Sandstone Member|32849|6|Mentioned|Table 1|||Permian||||||
24904|Darkes Forest Sandstone Member|34569|6|Mentioned|Fig.2|||Appin Formation||||||
24904|Darkes Forest Sandstone Member|36220|6|Mentioned|p49|||||||||
24904|Darkes Forest Sandstone Member|37089|6|Mentioned|p208|||||||||
24904|Darkes Forest Sandstone Member|39661|6|Mentioned|p447|||Replaces Lacys Creek Sandstone||||||
34513|Darling Suite|22771|6|Mentioned|Table12.2p45|||||||||
34513|Darling Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Superseded by Clevedale Migmatite and Ednas Gneiss of the Willyama Supergroup (Stevens, 1995). Referred to as Suite 1 by Stevens, Stroud et al (1979, 1980). ||||||
38859|Daroobalgie Volcanics""|24417|6|Mentioned|p26|||Now included in Parkes Volcanics.||||||
30822|Darrawillian Stage|43383|14|Not recorded|p10||Ordovician|||||||
40555|Darthula Rhyodacite Tuff Member|24605|6|Mentioned|p953 App.1|||Superseded by Darthula Rhyodacite Member.||||||
38987|Darthula Rhyolite|23861|6|Mentioned|p6 Tb. 1|||See also Darthula Rhyodacite.||||||
69858|Darthula Ryhodacite Member|61214|6|Mentioned|p174 Tb. 1|||Misspelt - see Darthula Rhyodacite Member.||||||
69998|Darts Creek mudstone|61766|5|Briefly described|p67|||Informal status (Roberts et al 1991) - authors upgraded it to formation level. Dee Darts Creek Formation.||||||
24906|Daubney beds|40595|6|Mentioned|Fig.7|||||||||
31244|David moraine|43491|14|Not recorded|pXII/62|||Quote of W.R.Browne 1952. Quaternary||||||
82896|Davys Creek Limestone Member|73210|6|Mentioned|p903|||See also Davys Plains Limestone Member (p893).||||||
24908|Daylesford Formation|33061|3|Fully described|p18|||See also PP,19,20. Ord.||||||
24908|Daylesford Formation|33062|5|Briefly described|p939|||||||||
24908|Daylesford Formation|33066|6|Mentioned|p235|||Ord. Fauna.||||||
24908|Daylesford Formation|33735|6|Mentioned|Fig.3|||||||||
39300|De Drack formation|24318|5|Briefly described|p19|Early Silurian|Early Silurian|||||||
36198|Debris Flow""|23392|6|Mentioned|p7|||Informal subdivision of Jones (1984) BSc Hons, of the Mogongong Conglomerate Member.||||||
25876|Delegate Adamellite|22815|4|Described|p59|Silurian|Silurian|Rb/Sr Age; 415.5 +/-0.9 Ma.||||||
25876|Delegate Adamellite|33852|6|Mentioned|Fig.2|||Date on Table 1.||||||
25876|Delegate Adamellite|38327|6|Mentioned|Table 4|||||||||
25876|Delegate Adamellite|38500|4|Described|p89|||||||||
25876|Delegate Adamellite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
25876|Delegate Adamellite|40328|4|Described|p205|||||||||
25876|Delegate Adamellite|41905|2|Defined|p67|Silurian||||||||
25876|Delegate Adamellite|41933|5|Briefly described|Map legend|Late Silurian||||||||
25876|Delegate Adamellite|42627|5|Briefly described|Map legend|Wenlock||||||||
25876|Delegate Adamellite|42647|3|Fully described|p42|||||||||
25876|Delegate Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||of Delegate Suite.||||||
25876|Delegate Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah10||||||
25876|Delegate Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
25876|Delegate Adamellite|60988|6|Mentioned|p144 Fig.1|||||||||
34657|Delegate breccia pipes|22815|3|Fully described|p105|Jurassic|Jurassic|||||||
34657|Delegate breccia pipes|61819|5|Briefly described|p91|Middle Jurassic|Middle Jurassic|Informal name for intrusive rocks.||||||
69976|Delegate suite|61794|6|Mentioned|p360|||Informal name.||||||
32511|Demon Creek mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
68171|Dempsey Formation, upper|60281|6|Mentioned|p65|||Informal - see Dempsey Formation.||||||22-MAR-05
76064|Deriwong Group|66197|5|Briefly described|p635 Fig.5a|Lochkovian|Pridoli|[misspelling of Derriwong]||||||13-MAR-12
74757|Derrida Granite""|61964|5|Briefly described|p37, p47|||On NYMAGEE sheet - previously mapped separately but is probably related to Ungarie Granite (thus a member of Koetong Suite). Informal name; now referred to as Derrida Phase (of Ungarie Granite) - equigranular, fine- to med,-gr.cordierite-biotite granite||||||
24915|Derringullon Formation|29989|6|Mentioned|Map legend|Late Silurian|Late Silurian|Misspelling of Derringullen Formation. Comment added 1993.||||||
35271|Dewey Point Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
41596|Dewrang Formation""|44244|6|Mentioned|p169, p167|||||||||
37437|Diamond Creek Limestone|23214|6|Mentioned|p203|||Superseded by Jesse Limestone (subsequently Jesse Limestone Member).||||||
32264|Dicky Cooper Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab22.||||||
32264|Dicky Cooper Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
27042|Dicky Cooper Granite|42726|5|Briefly described|map legend|Silurian||360.  Of the Bullenbalong Suite (Bullenbalong Supersuite).  Formal name not intended. Reservation lapsed 5-DEC-89.||||||08-FEB-05
35270|Diega Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
70650|Digby "Quartz Sand"|61313|6|Mentioned|p100|Early Triassic|Late Permian|Informal name for deposits at the Late Permian-Early Triassic transition zone at the top of the Black Jack Group; also referred to as the "Quartz Sand" of the Digby Formation and Digby Formation "Quartz Sand".||||||14-FEB-07
26519|Digby Conglomerate|32482|6|Mentioned|Map legend|Triassic|Triassic|||||||
26519|Digby Conglomerate|37856|6|Mentioned|Table I|||||||||
26519|Digby Conglomerate|38089|6|Mentioned|p9|||||||||
26519|Digby Conglomerate|39666|6|Mentioned|p86|||||||||
26519|Digby Conglomerate|43194|5|Briefly described|p96 Tb 8.1, p116|Early Triassic|Early Triassic|Replaced by Digby Formation||||||
26519|Digby Conglomerate|43407|14|Not recorded|Map Legend||Triassic|(Provisional Edition) Part of Narrabeen Group.||||||14-FEB-07
26519|Digby Conglomerate|43410|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
26519|Digby Conglomerate|65118|6|Mentioned|Fig 13 p495|||Conglomerate. See also Digby Formation p479, 491.||||||
26519|Digby Conglomerate|66090|6|Mentioned|p23.|Triassic|Triassic|Gunnedah Basin. Its chert and jasper clasts are typical of New England Orogen provenance; similar to Laurieton Conglomerate (Lorne Basin) and Munmorah Conglomerate (Sydney Basin).||||||
70649|Digby Formation "Quartz Sand"|61313|6|Mentioned|p106|||Informal. Same unit as the Digby "Quartz Sand".||||||
70651|Digby Formation, Upper|61313|5|Briefly described|p105|||Also known as "Quartz Sand" of the Digby Formation, or Digby Formation "Quartz Sand" or Digby "Quartz Sand". Laterally equivalent to Wollar Sandstone. Displays excellent reservoir characteristics. Max. thickness: 25m.||||||
73041|Digby Formation, lower|61377|6|Mentioned|p150|||Informal - see Digby Formation.||||||07-FEB-11
83575|Digby Sandstone Formation|73304|6|Mentioned|p71|||[Possibly a variation of Digby Formation]. Gunnedah Basin. [Basal?] boundary marks a major extinction of peat-producing plants.||||||
78538|Digby Series|43194|5|Briefly described|p96 Tb 8.1, p116|Early Triassic|Early Triassic|Of Kenny (1928, 1964). Superseded name for the Digby Formation in the Coonabarabran-Gunnedah region of the Gunnedah Basin.||||||27-NOV-13
39407|Dilga formation|24126|6|Mentioned|p207|||||||||
41556|Dilly hills trachytes|60267|6|Mentioned|p24|||Informal name - refers to the trachyte of the Warrumbungle Volcanics in the Dilly hills. See also Dilly trachyte,  "Dilly trachyte" and Dilly trachytes.||||||11-AUG-04
41557|Dilly trachyte|60267|4|Described|p24|Middle Miocene|Middle Miocene|Informal name for trachytes of the Warrumbungle Volcanics in the three main Dilly hills (Dill Dolly, Dill Dilly and Dill Killy). See also Dilly Hill trachytes, "Dilly trachyte" and Dilly trachytes.  Age: 15.8+/-0.2Ma.  See also p16, p21.||||||11-AUG-04
41558|Dilly trachyte""|60267|6|Mentioned|p16|||Informal reference to the rocks of the summits of the Dilly hills - trachytes of the Warrumbungle Volcanics.  See also Dilly hill trachytes, Dilly trachytes and Dilly trachyte.||||||
41559|Dilly trachytes|60267|6|Mentioned|p24|||Informal - see Dilly trachyte, also an informal name for the trachytes of the Warrumbungle Volcanics.  See also "Dilly trachyte" and Dilly hill trachytes.||||||
82738|Dinner Creek Microgranite Phase|71628|4|Described|p15: 48, 94-95, 106-107, 110-112, 114|||New name (this study) after work by Mustard (2004). Main component of the parent unit. Timbarra Plateau. Geochemistry described in great detail.|249.5 +/- 2.7 Ma (SHRIMP: Mustard, 2004).|Surface Hill Leucomonzogranite.||Abuts (intrudes) Sandy Creek Monzogranite.|Strongly porphyritic (K-feldspar phenocrysts to 5.5 mm) biotite microgranite.|
83260|Dirk Dirk Formation|73440|6|Mentioned|p132|||[Probably a misspelling of Drik-Drik Formation].||||||
34257|Dirnaseer basic intrusion""|22638|6|Mentioned|p79|||Superseded by Dirnaseer Gabbro||||||08-MAR-16
28311|Divide Basalt|39848|2|Defined|p115|early Miocene|early Oligocene|Late Oligocene to Early Miocene||||||
28311|Divide Basalt|40240|6|Mentioned|Fig.1|||||||||
28311|Divide Basalt|40293|6|Mentioned|Fig.4|||||||||
28311|Divide Basalt|40742|6|Mentioned|Fig.2|||||||||
28311|Divide Basalt|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|In the Bathurst-Goulburn region. ||||||
28311|Divide Basalt|68592|6|Mentioned|p1814|Cenozoic|Cenozoic|Bishop (1984). Obsolete: this unit is included in the Wheeo Basalt.||||||
41035|Dobroyde Volcanics|50191|6|Mentioned|p30 Table 1|Early Silurian|Late Ordovician|See also Dobroyde volcanics.||||||02-AUG-04
41035|Dobroyde Volcanics|63278|6|Mentioned|p149|||Now incoporated into the Temora Volcanics.||||||07-FEB-11
41035|Dobroyde Volcanics|72495|6|Mentioned|p227|||Of Wyborn (1996), included by the authors in the Temora Volcanics. Originally removed from the Junawarra Volcanics of Warren et al 1995 due to different geochemical affinities.||Temora Volcanics||||
41032|Dobroyde volcanics|50191|6|Mentioned|p5, 11|Silurian|Ordovician|Informal - see Dobroyde Volcanics.||||||02-AUG-04
41032|Dobroyde volcanics|72082|5|Briefly described|p32|||In the Dobroyde property, 14km NE of Junee. Included in the Junawarra Volcanics by Warren et al. (1995), but considered a geochemically distinct unit by Wyborn (1996) who gave the rocks this informal name. To be the subject of a fuller description in a future report. Ages are of an andesite and a felsic dyke respectively.|432 Ma and 428 Ma (SHRIMP: Geoscience Australia).|||||
41036|Dobroyde volcanics""|50191|6|Mentioned|p11|||Informal - see Dobroyde Volcanics.||||||02-AUG-04
28507|Dodger Granite|42726|5|Briefly described|map legend|Early Devonian||395.  Of the Boggy Plain Suite.  Formal name not intended. Variation on Dodger Diorite||||||08-FEB-05
70082|Donaldsons seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to coal seam within the Four Mile Creek Formation (Tomago Coal Measures).||||||
70645|Doncaster Member mudstone|61312|6|Mentioned|p74|||Informal - see Doncaster Member.||||||
77700|Donovan Complex|60308|6|Mentioned|p39|||Abbreviation of Donovan Basin Complex.||||Correlated with Comerong volcanics.||29-MAY-13
77701|Donovan Mafic Complex|60308|6|Mentioned|p39|||See also  Donovan Basic Complex p38||||||
77246|Doona Seam|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Informal name? Within Trinkey Formation (Nea Subgroup, Black Jack Group)||||||
77246|Doona Seam|68004|6|Mentioned|p153.|Late Permian|Late Permian|Southern Mullaley Sub-basin, Gunnedah Basin. Thickness to 2.5 m; interbanded stony coal and tuff units make this a very high ash coal with limited to no development potential.||Unit in Black Jack Group.|||Interbanded stony coal and tuff.|
79446|Dooralong Formation|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Clifton Subgroup, Narrabeen Group.|||Medium-grained quartz-lithic sandstone, siltstone, claystone, laminate, coal.|13-JUL-16
78381|Doradilla sandstone|69002|6|Mentioned|p16|||||||||
82411|Dormans Flat Suite|71628|5|Briefly described|p12: 6|||New name. Assignation is tentative.||Sailor Jack Supersuite.|Dormans Flat Monzogranite.|||
30762|Dorroughby Tuff|22582|6|Mentioned|Fig2,p70|||||||||
30762|Dorroughby Tuff|43344|14|Not recorded|p101,102|||||||||
30762|Dorroughby Tuff|43881|14|Not recorded|p6-7,56,132||Tertiary|This name now superseded by Dorroughby Tuff Member. See also Lexicon.||||||
69666|Doughboy Province Volcanics|61155|5|Briefly described|p19|Middle Eocene|Middle Eocene|Overlies Walcha Province Volcanics.  In the Kempsey area.||||||
31283|Doughboy Shale|43474|14|Not recorded|no card|||(no card)||||||
31283|Doughboy Shale|43476|14|Not recorded|Map Legend|||(Provisional Edition)||||||
35428|Doughboy Shale""|23170|6|Mentioned|p53|||||||||
31209|Douro Formation|43479|14|Not recorded|p103|||||||||
70083|Douro Group""|22857|6|Mentioned|p454 App.1, Tb.A1.6|Silurian|Silurian|Of Basden, Adrian et al, 1975, 1978), and part of "Douro Group" of Cramsie, Pogson and Baker (1975,1978) - now included in the Goobarragandra Volcanics. Geological Province: Canberra-Yass Shelf. ||||||
77247|Doyles Creek Sub-group|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Wollombi Coal Measures.|Includes Pinegrove and Waterfall Gully Formations.|Overlies Horseshoe Creek Sub-group. Is overlain by Glen Gallic Sub-group.||
26526|Drik Drik Formation|22750|4|Described|p 228|||Tamworth Group||||||
26526|Drik Drik Formation|23185|6|Mentioned|Fig5p161|Emsian|Pragian|||||||
26526|Drik Drik Formation|23522|5|Briefly described|p249 Fig 5|Emsian|Emsian|||||||
26526|Drik Drik Formation|31999|5|Briefly described|p150|||Table 1||||||
26526|Drik Drik Formation|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
26526|Drik Drik Formation|34397|5|Briefly described|p230|||Ordovician||||||
26526|Drik Drik Formation|34554|4|Described|p231|||See also P232||||||
26526|Drik Drik Formation|36961|6|Mentioned|Fig.3|||||||||
26526|Drik Drik Formation|37727|6|Mentioned|p81|||||||||
26526|Drik Drik Formation|39214|6|Mentioned|p33|||||||||
26526|Drik Drik Formation|39331|6|Mentioned|Table 10-1|||||||||
26526|Drik Drik Formation|40136|6|Mentioned|p41|||See also P46||||||
26526|Drik Drik Formation|43407|14|Not recorded|Map Legend|||(Provisional Edition) Part of Tamworth Group||||||
26526|Drik Drik Formation|43419|14|Not recorded|p112|||Includes Nemingha Limestone. (Crook,1961) Now regarded as part of Trelawney Beds.||||||
26526|Drik Drik Formation|43428|14|Not recorded|p137,142|||||||||
26526|Drik Drik Formation|43479|14|Not recorded|p151||Early Devonian|||||||
26526|Drik Drik Formation|43525|14|Not recorded|Table p132||Emsian|||||||
26526|Drik Drik Formation|47056|6|Mentioned|Fig.2 P523|||||||||
26526|Drik Drik Formation|50094|5|Briefly described|p315, p316 Fig.1, p317 Fig.2|Emsian|Emsian|Unconformably overlies Haedon Formation. Basal unit of Tamworth Group.||||||
26526|Drik Drik Formation|61392|5|Briefly described|p165 Fig. 2|Emsian|Emsian|In the Gamilaroi terrane.||||||07-FEB-11
26526|Drik Drik Formation|63119|5|Briefly described|p214|||Of the Tablelands Complex. Contains osteoliths of Eastonian age. Geological Province: Tamworth Belt.||||||13-MAR-07
26526|Drik Drik Formation|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Nundle. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26526|Drik Drik Formation|67322|5|Briefly described|p27, p39|Early Devonian|Early Devonian|Contains allochthonous limestone blocks associated with the 'Trelawney beds'. Depositional age of Early Devonian. Occurs in the Tamworth-Neminha region.  ||||Unconformably overlies the Haedon Formation.|Basal red sandstone marks the unconformity boundary; also conglomerates containing Ordovician limestone clasts.|21-FEB-18
26526|Drik Drik Formation|68822|5|Briefly described|p332|Lower Devonian|Lower Devonian|||||Unconformably underlain by the Haedon Formation.||
26526|Drik Drik Formation|71091|6|Mentioned|p147|Early Devonian|Early Devonian|||||||
26526|Drik Drik Formation|73492|5|Briefly described|p704|Early Devonian|Early Devonian||||Trelawney beds''|||
40229|Drik-Drik Formation, upper|38686|6|Mentioned|p57|||Geological Province: New England Fold Belt||||||
39319|Drildool Beds|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
39319|Drildool Beds|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment.||||Overlies Keelindi Beds. Is overlain by Wallumbilla Formation.||
35441|Dripstone Group""|23170|6|Mentioned|p80|||Superseded by Dripstone Formation.||||||
23561|Drogheda Dolerite|42712|4|Described|8; Table 1 p14.|Early Devonian|Late Silurian|||||||
24930|Dromedary Complex|36042|6|Mentioned|p44|||||||||
24930|Dromedary Complex|40266|6|Mentioned|p16|||||||||
24930|Dromedary Complex|41561|6|Mentioned|p541|||||||||
36136|Dromedary Igneous complex|23464|6|Mentioned|p245|||||||||
36137|Dromedary monzonite complex|23464|6|Mentioned|p249|Cretaceous|Cretaceous|||||||
82417|Dry Creek Suite|71628|5|Briefly described|p10: 9|Late Permian|Late Permian|||Boxwell Supersuite.|Dry Creek Granodiorite.|||
30763|Dryamberin Beds|43344|14|Not recorded|p95|||misspelling of Dyamberin Beds||||||
69668|Dubbo Province Volcanics|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Overlies rocks associated with the Warrumbungle Volcano. In the Liverpool Range area.||||||
69668|Dubbo Province Volcanics|70036|5|Briefly described|Map legend|||Included in a mapped unit of Tertiary volcanic rocks: trachyte, basalt, nephelinite, syenite, rhyolite, monzonite and tuff. Appears as Dubbo Province.||||||
30810|Dubbo Sandstone|43384|14|Not recorded|Map Legend|Jurassic|Triassic|||||||
69851|Dubbo basalts|61210|6|Mentioned|p257|||Informal name.||||||
34250|Dudaumon Granite""|22638|6|Mentioned|p68|||Superseded by Gundibindyal Granite||||||24-AUG-04
79840|Dudley Coal Seam|60726|5|Briefly described|p3.|Late Permian|Late Permian|||Basal Newcastle Coal Measures.||||
70043|Dudley coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
70043|Dudley coal seam|68711|5|Briefly described|p119, p116 Tbl 6|||Informal unit.||Within Lambton Formation||||
27762|Dudley seam|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Of the Lambton Formation.   Geological Province: Sydney Basin||||||
27762|Dudley seam|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Lambton Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
27762|Dudley seam|37083|3|Fully described|p172|||||||||
27762|Dudley seam|39609|6|Mentioned|p6|||||||||
27762|Dudley seam|40166|6|Mentioned|p361|||||||||
27762|Dudley seam|62033|5|Briefly described|p25 (Table)|||Of the Lambton Formation (Newcastle Coal Measures). Overlies Yard seam; overlain by Nobbys seam. Geological Province: Sydney Basin. Informal name.||||||04-FEB-08
28516|Dudley-Yard seam|39609|6|Mentioned|p1|||||||||
31251|Duladerry Rhyolite|43517|14|Not recorded|p151|||||||||
34636|Duladerry Rhyolite""|22831|6|Mentioned|p 67|||||||||
38939|Dulladerry Rhyolite""|24417|6|Mentioned|p114|||Superseded by Dulladerry Volcanics.||||||
81804|Dulladerry Volcanics''|72495|6|Mentioned|p229|||||||||
39382|Dulladerry rhyolite|24125|5|Briefly described|p79|||Geological Province: Lachlan Fold Belt.||||||
39388|Dulladerry volcanics|24126|6|Mentioned|p2|||Misspelt- see Dulladerry Volcanics.||||||
77248|Dumboy Gragin Granite|68004|6|Mentioned|p125, p128, p198, p200.|Early Triassic|Late Permian|New England Fold Belt. Tin vein and tin greisen occurrences, potential and level of certainty are discussed.||||||
77248|Dumboy Gragin Granite|70036|5|Briefly described|Map legend|Triassic|Triassic|New England Fold Belt.|||||Porphyritic granite.|
73938|Dumboy-Gragin Suite|71628|6|Mentioned|p19: 28|||||||||
82739|Dumboy-Gragin granite|71628|6|Mentioned|p19: 27|||Carne (1911). Now Dumboy-Gragin Leucosyenogranite.||||||
27393|Dumbudgery Creek Granodiorite|22580|5|Briefly described|p99|Late Permian|Late Permian|||||||
27393|Dumbudgery Creek Granodiorite|23799|6|Mentioned|p117|||Includes a high-K group of the Bruxner Suite (geochemical suite of Clarence River Supersuite as defined by Shaw and Flood, 1981, and Bryant  and others, 1997).||||||
27393|Dumbudgery Creek Granodiorite|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Clarence River Plutonic Suite.  Medium- to coarse-grained, hornblende-rich granodiorite; tonalite and leucotonalitic phases, some with intermediate to basic encalves; includes porphyritic gabbroic rock and diorite phases.||||||20-DEC-04
27393|Dumbudgery Creek Granodiorite|23812|4|Described|p21 Tb.2, p63|Late Permian|Late Permian|Of Clarence River Plutonic Suite. Intrudes the Drake Volcanics.||||||
27393|Dumbudgery Creek Granodiorite|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27393|Dumbudgery Creek Granodiorite|33476|6|Mentioned|p13|||||||||
27393|Dumbudgery Creek Granodiorite|42378|6|Mentioned|Table 1 P11|||||||||
27393|Dumbudgery Creek Granodiorite|42866|5|Briefly described|Table 2, P12|||||||||
27393|Dumbudgery Creek Granodiorite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Granodiorite and tonalite. Of the Clarence River Suite.||||||
27393|Dumbudgery Creek Granodiorite|61772|6|Mentioned|p132|||Age: 249-257Ma.||||||24-SEP-08
27393|Dumbudgery Creek Granodiorite|61795|6|Mentioned|p368|Early Triassic|Late Permian|Geological Province: New England Fold Belt. I-type granites.||||||17-NOV-08
27393|Dumbudgery Creek Granodiorite|68008|6|Mentioned|p333|||Geochemistry mentioned.||||||
27393|Dumbudgery Creek Granodiorite|68111|5|Briefly described|p968 Tb.1|Induan|Wuchiapingian|Ar-Ar dating of hornblende by Bryant et al. (1997b).|ca. 259 - 252 Ma|Of the Clarence River Supersuite.||||
27393|Dumbudgery Creek Granodiorite|68679|5|Briefly described|p465|||Geochemical plots; similar to Boxwell Granodiorite.||Clarence River Supersuite.||||
27393|Dumbudgery Creek Granodiorite|70217|5|Briefly described|p72, p73 tbl 14.1|Triassic|Permian|New England Orogen. Ages are similar to the Mount Ephraim Granodiorite. Additional ages include Rb-Sr dates of c. 249 and c. 250 Ma from Shaw and Flood (1993) and Ar/Ar ages of 253.6 +/- 1.0 and 256.9 +/- 1.8 Ma from Bryant et al 1997a.|c. 257-253 Ma|Clarence River Supersuite||||
27393|Dumbudgery Creek Granodiorite|70876|4|Described|p2-p3, p47-p52, p78-p79, p94|Permian|Permian|New England Orogen. Additional ages are provided as follows: c. 250-249 Ma (Rb-Sr, Shaw and Flood, 1993), 253.6 +/- 1 Ma and 256.9 +/- 1.8 Ma (Ar-Ar, Bryant et al, 1997). Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|255.0 +/- 1 Ma (SHRIMP U-Pb)|Dumbudgery Creek Suite|||Medium-grained, equigranular granodiorite with plagiolcase, alkali feldspar, quartz and ferromagesian minerals.|
27393|Dumbudgery Creek Granodiorite|71628|6|Mentioned|p9: 1-2, 10, 12, 14, 19-20, 27|||Brunker and Chesnut (1974), after a local watercourse. Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). Was mis-spelled as Dumbadgery Creek Granodiorite in Korsch and Harrington (1981). The lithology is not included in the list of constituents of the Suite on p9-1. Comprises a series of disparate rocks, hence renamed Mount Carnham Granodiorite in the Dumbudgery Creek Complex (this study).||||||
73891|Dumbudgery Creek Suite|70876|5|Briefly described|p47|||New England Orogen.||Clarence River Supersuite|Includes the Dumbudgery Creek Granodiorite.|||
38328|Dummy Creek Association""|23812|5|Briefly described|p25|Early Triassic|Late Permian|Informal name of Korsch, 1977.||||||
39094|Duncan Suite|23799|6|Mentioned|p115 Fig. 10|||Abbreviation of Duncans Creek Suite?  Of the Clarence River Supersuite.||||||
39093|Duncan's Creek Trondhjemite|23799|5|Briefly described|p117|||Probably misspelt?  Of Duncans Creek Suite.||||||
39093|Duncan's Creek Trondhjemite|71628|6|Mentioned|p18:3|||Gilligan and Brown (1981) after unpublished work by Bultitude (1965). See Duncans Creek Trondhjemite.||||||
39093|Duncan's Creek Trondhjemite|72313|6|Mentioned|p459 Table 2|||New England Orogen. I-type.  Hf isotope data included.|252 - 249 Ma|||||
38329|Dundee "Adamellite Porphyrite"|23812|5|Briefly described|p26 Tb.3|||Part of the Dundee Rhyodactie, now included in the Dundee mass.||||||
38329|Dundee "Adamellite Porphyrite"|60079|5|Briefly described|Map Legend|Late Permian|Permian|Superseded by Dundee Rhyodacite.||||||
40265|Dundee Adamellite|50015|6|Mentioned|p351|||Geological Province: New England Fold Belt||||||
38286|Dundee Adamellite Porphyrite""|23811|5|Briefly described|Map Legend description|Late Permian|Late Permian|Also called "Blue Granite" - informal former name for Dundee mass of Dundee Rhyodacite.||||||20-DEC-04
28519|Dundee Ignimbbrite|41998|5|Briefly described|p481|||||||||
74856|Dundee Rhyodacite Ignimbrite|61793|4|Described|p341, p342 Fig. 1(b), p344, p347|||Inferred to overlie Emmaville Volcanics. Comformably underlain by Yarramundi Andesite.||||||07-FEB-11
40240|Dundee Rhyodacite Suite|38824|6|Mentioned|p215|Late Permian|Late Permian|Geological Province: New England Fold Belt||||||
32512|Dundee mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
81112|Dundurabbin Granodiorite|71628|6|Mentioned|p3:27|||Kemp et al. (2009); mis-spelling of Dundurrabin Granodiorite.||||||
81112|Dundurabbin Granodiorite|71703|6|Mentioned|p204|||||Of Hillgrove Supersuite.||||
81112|Dundurabbin Granodiorite|72313|6|Mentioned|p459 Table 2|||New England Orogen. S-type.  Hf isotope data included.|290 Ma|||||
73512|Dungarvan diorite|63284|6|Mentioned|p266, p268|Late Ordovician|Late Ordovician|Informal name. Intrusive is compositionally shoshonitic, with strong similarities to the Goonumbla and Wombin Volcanics - Northparkes Igneous Complex suites.||||||
83053|Dungowan Adamellite|73202|6|Mentioned|p630-631, p636|||Southwest corner of the Echo Hills Formation basin. Related to the Bundarra Plutonic Supersuite by Blair (1983) based on geochemical affinity and minor quartz and feldspar intercrystal deformation. Shown as Dungowan Adamallite p636.|||||Granitic rock.|
42209|Dunskeig granite|24456|6|Mentioned|p329 Tb.1|||Informal name.||||||26-NOV-04
24939|Duoro "Series"|30332|6|Mentioned|p127|||Misspelling of Douro?||||||
31907|Duro Porphyry|43870|14|Not recorded|p300,325||Silurian|Palaeomagnetic readings. Middle Silurian||||||
28115|Duronal Granite|42726|5|Briefly described|map legend|Carboniferous||17. Of the Bathurst Suite (Bathurst Supersuite).  Formal name not intended.||||||07-FEB-05
31851|Durras Latite|45003|6|Mentioned|p186|||||||||
25889|Dyamberin Beds|31694|6|Mentioned|p345|||||||||
25889|Dyamberin Beds|32944|6|Mentioned|p709|||||||||
25889|Dyamberin Beds|34556|6|Mentioned|p269|||Permian||||||
25889|Dyamberin Beds|34589|6|Mentioned|p277|||Permian unmetamorphosed||||||
25889|Dyamberin Beds|35145|6|Mentioned|p83|||||||||
25889|Dyamberin Beds|35264|2|Defined|p14|Permian|Permian|||||||
25889|Dyamberin Beds|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition.||||||
25889|Dyamberin Beds|36948|6|Mentioned|Fig.1|||||||||
25889|Dyamberin Beds|39214|6|Mentioned|p40|||||||||
25889|Dyamberin Beds|40246|6|Mentioned|Fig.1|||||||||
25889|Dyamberin Beds|71280|5|Briefly described|p403 Fig.2, p412|||Coffs Harbour Block. Occurs to the E of the Wongwibinda Fault. Similar intermediate-volcanic provenance to Girrakool Beds, but this unit is more proximal.||||||
74863|Dyambrian Beds|61805|6|Mentioned|p439 Fig. 2|||Misspelt - see Dyamberin beds. Geological Province: New England Orogen.||||||27-NOV-08
76028|Dynamite Creek Granodiorite|66927|5|Briefly described|Map legend|Silurian|Silurian|Low to moderate magnetic zones.  Intrusive boundaries contrast strongly with magnetised aureole zones.|||Unit in Tibooburra Suite.||Hornblende granodiorite.|
31288|Eadvale Volcanics|43525|14|Not recorded|map p124,Table p127|||||||||
73705|Eagle Hawk Basalt|63286|5|Briefly described|p295, p298, p304, p307|Gisbornian|Darriwilian|Intrudes Coombing Formation and Blayney Volcanics. Basalt Sills that comprise abundant clinopyroxene, subordinate or no plagioclase, and rare altered olivine phenocrysts.Is also amoung the least-evolved rocks in the Cadia-Neville region.||||||07-FEB-11
73689|Eaglehawk Basalt|63283|6|Mentioned|p202|||Of Wyborn and Henderson (1996).  Composition shows this is a synonym of the upper Blayney Volcanics.||||||04-NOV-14
41055|East Lake Monzogranite|24366|5|Briefly described|p8 Fig. 6|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41055|East Lake Monzogranite|71628|6|Mentioned|p3:33|||Brown (2003). Originally the Hillview Adamellite (Binns et al., 1967). Subsequently Eastlake Adamellite (Landenberger, 1986) then East Lake Monzogranite (Brown, 2003). Here spelled Eastlake Monzogranite after the homestead of that name.||||||
39622|Eastern Schist|24087|6|Mentioned|p330 Fig. 4|||Geological Province: Lachlan Fold Belt.||||||
39622|Eastern Schist|50546|5|Briefly described|p1232 Fig.1c, p1234 Fig.2a|||Geological Province: Lachlan Fold Belt.||||||30-NOV-04
39622|Eastern Schist|62747|5|Briefly described|p737|||Comprises laminated (10-100m) quartz-rich sandstone and mudstone. Overlain by the Albion Formation.||||||
39622|Eastern Schist|62749|6|Mentioned|p722 Fig. 1a, b|||||||||
39622|Eastern Schist|62751|6|Mentioned|p760 Fig. 1b|||||||||
39622|Eastern Schist|62752|6|Mentioned|p760 Fig. 1b|||||||||
39622|Eastern Schist|62753|6|Mentioned|p802 Fig. 2|||||||||
39622|Eastern Schist|64597|6|Mentioned|p760 Fig.1. |||||||||
35920|Eastern View Coal Measures Group|23357|6|Mentioned|55 Fig.6|||||||||
82431|Eastlake Suite|71628|5|Briefly described|p3:33|||||Hillgrove Supersuite.|Eastlake Monzogranite.|||
38986|Eastons Aem Rhyolite|23861|6|Mentioned|p6 Tb. 1, p20 Tb. 2|||Misspelt - see Eastons Arm Rhyolite.  Geological Province: New England Orogen.||||||
37300|Eastons Arm Rhyolite|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Of Clifden Formation.  Underlain by Wanganui Andesite.  Geological Province: New England Orogen.  See also p5, p12.||||||
37300|Eastons Arm Rhyolite|24010|6|Mentioned|p381|||||||||
37300|Eastons Arm Rhyolite|24603|5|Briefly described|p868 Fig. 3|Namurian|Namurian|Of the Clifden Formation.  Age: 318.0 +/- 3.4Ma.  Geological Province: Tamworth Belt.||||||
69859|Eastons Arm Rhyolite Member""|61214|5|Briefly described|p170, p172 Fig. 2|Namurian|Namurian|Informal name for part of the Clifden Formation - junior synonym of Peri Rhyolite Member; there is significant overlap between these units eg. trace element similarities. Age: 317.8+/-2.8Ma.||||||
42207|Eastwood granite|24456|6|Mentioned|p329 Tb.1|||Informal name.||||||26-NOV-04
69670|Ebor-Dorrigo Province Volcanics|61155|5|Briefly described|p19|Early Miocene|Early Miocene|Age: 19.5-18Ma.  In the Kempsey area.||||||
74857|Echo Sandstones|61793|4|Described|p343 Tb. 1|Late Permian|Late Permian|Of Emmaville Volcanics. Thickness: ~625m. Geological Province: New England Fold Belt. Consists of 3 volcaniclastic facies; coarse sandstones, coarse angular breccia and conglomerates, all interbedded.||||||07-FEB-11
74858|Echo Volcaniclastics|61793|5|Briefly described|p341, p342 Fig. 1(b), p344, p347|Late Permian|Late Permian|Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||07-FEB-11
29448|Echuca Formation""|42966|6|Mentioned|Table 29 p183|||Synonym of Torumbarry Clay.||||||
31240|Eden Stage|43491|14|Not recorded|pV/15||Late Devonian|||||||
31138|Eden rhyolites|43491|14|Not recorded|pV/15||Late Devonian|||||||
28526|Edol Sandstone""|22831|6|Mentioned|p 43|||||||||
28526|Edol Sandstone""|36066|6|Mentioned|p9|||Refers Brunker 1972. This is a misspelling of Edols.||||||
39372|Edol sandstone|24125|5|Briefly described|p3|||Informal - see Edol Sandstone.  Geological Province: Lachlan Fold Belt.||||||
38915|Edols Sandstone""|24417|6|Mentioned|p67|||Superseded by Edols Conglomerate.||||||
29422|Eight Mile Basalts|42960|6|Mentioned|p70|||Old name, used 1957, Cabramurra area.||||||
68169|Elderslie Formation, lower|60281|5|Briefly described|p58|Late Permian|Early Permian|Informal name.||||||
32655|Eldorado Formation|46547|14|Not recorded|Not recorded|||||||||
35024|Ellendale Granite|23048|6|Mentioned|p7||Devonian|Mentioned in text.||||||21-OCT-08
35024|Ellendale Granite|24128|5|Briefly described|p125|||Geological Province: Lachlan Fold Belt.||||||
39424|Ellendale Granites|24128|5|Briefly described|p82|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
32663|Elliot's Shale Member|46568|14|Not recorded|p.426,428|||Lens in Kohinoor Volcanics (I55-16/Michelago).||||||
32632|Elliot's shale|46568|14|Not recorded|p.426,428|||(I55-16/Michelago).||||||
34133|Elmsdale Formation|22639|5|Briefly described|p267 Fig.2|Early Devonian|Early Devonian|||||||
70483|Elmswood Ignimbrite|62095|6|Mentioned|p260 Tb. 1|Early Carboniferous|Early Carboniferous|Abbreviated version of Elmswood Ignimbrite Member; see also the abbreviated Elmswood Member. Age: 326.4+/-2.6Ma.||||||25-MAY-06
70484|Elmswood Member|62095|5|Briefly described|p259 Fig. 10|Namurian|Namurian|Abbreviated version of Elmswood Ignimbrite Member.  Age:326.4+/-2.9Ma.||||||
29726|Elouera Beds""|43032|6|Mentioned|p64|||Refers to Andrews (1913)||||||
73956|Elsmore Suite|71628|6|Mentioned|p19:33||||||Elsmore Leucomonzogranite.|||
83246|Elura limestone""|73143|6|Mentioned|p1|||Informal stratigraphic name to describe a prominent subsurface reef limestone in drillcore beneath the Endeavor Zn-Pb-Ag massive sulfide deposit. Formal definition as Elura Limestone Member of the Brookong Formation.||||||
27147|Emerald Beach Adamellite|23720|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium-grained biotite monzogranite.||||||16-DEC-04
27147|Emerald Beach Adamellite|24129|5|Briefly described|p4|Middle Triassic|Middle Triassic|||||||
27147|Emerald Beach Adamellite|31695|6|Mentioned|Fig. 1|||Variation of Emerald?||||||
27147|Emerald Beach Adamellite|35264|2|Defined|p16|Late Paleozoic|Late Paleozoic|Late Palaeozoic? to Early Mesozoic?Prob.Late Palaeozoic||||||07-NOV-08
27147|Emerald Beach Adamellite|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition.||||||
27147|Emerald Beach Adamellite|44450|5|Briefly described|p36|Late Triassic|Early Permian|Geological Province: New England Fold Belt.||||||
27147|Emerald Beach Adamellite|71628|6|Mentioned|p17:92|||Korsch (1978). Now Emerald Beach Monzogranite.||||||
74016|Emerald Beach Suite|71628|5|Briefly described|p17_93|||Coastal Granite Association.|||Emerald Beach Monzogranite.|||
40262|Emmaville formation|38915|6|Mentioned|p343|||Geological Province: New England Fold Belt||||||
24952|Emmaville volcanics""|38842|6|Mentioned|p291|||||||||
25896|Emu Creek Beds|31676|6|Mentioned|p7|||||||||
25896|Emu Creek Beds|31694|6|Mentioned|p348|||||||||
25896|Emu Creek Beds|32086|2|Defined|p326|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian. See P325||||||
25896|Emu Creek Beds|33436|6|Mentioned|p233|||Carb.||||||
25896|Emu Creek Beds|33476|6|Mentioned|Table 1|||||||||
25896|Emu Creek Beds|34340|6|Mentioned|Table 6.1|||Carboniferous||||||
25896|Emu Creek Beds|36528|6|Mentioned|p182|||||||||
25896|Emu Creek Beds|36936|6|Mentioned|p208|||||||||
25896|Emu Creek Beds|36961|6|Mentioned|Fig.5|||||||||
25896|Emu Creek Beds|38806|6|Mentioned|p74|||||||||
25896|Emu Creek Beds|39279|4|Described|p367|||||||||
25896|Emu Creek Beds|40505|5|Briefly described|p81|||||||||
25896|Emu Creek Beds|43383|14|Not recorded|p19||Late Carboniferous|||||||
25896|Emu Creek Beds|43881|14|Not recorded|p8-9||Late Carboniferous|||||||
25896|Emu Creek Beds|69793|6|Mentioned|p1114 Fig.5|||Of McCarthy et al., (1974). Originally part of the Pretty Gully Series (Andrews, 1908); later Emu Creek Series (Voisey, 1936), Emu Creek Formation (Olgers et al., 1974) and, after this unit name, Emu Creek Formation again (Thomson, 1976). Redefined here (Hoy et al., 2014).||||||
37227|Emu Hollow Dacite""|23214|5|Briefly described|p83|Late Ordovician|Late Ordovician|Informal name. Age: 450+/-9Ma||||||
40787|Emu Plain basalt|50126|6|Mentioned|p71|Early Miocene|Early Miocene|||||||
37774|Enano Group volcanics|24168|5|Briefly described|p643|Silurian|Silurian|Informal name||||||
24954|Endrick River Basalt|32129|5|Briefly described|p7|||Includes type locality. Refers Raine (1967 unpubl.)||||||
24954|Endrick River Basalt|68592|6|Mentioned|p1802|||McIlveen (1975); one of the basalts at Sassafras (Young and McDougall, 1985).||||Is correlated with the Reevesdale Basalt.||
24954|Endrick River Basalt|73581|5|Briefly described|p23|Eocene|Eocene|Southern Highlands Volcanic Province. List of K-Ar ages provided from Wellman and McDougall (1974b). See also Endrick River basalt p22.|49.8 Ma-41.9 Ma K-Ar||||Low-K tholeiite to alkali basalt. High-Ti mineralogy and mantle xenoliths.|
73914|Enmore Suite|71628|5|Briefly described|p3:36|||||Hillgrove Supersuite.|Enmore Monzogranite.|||
34511|Erehwon Suite|22771|6|Mentioned|Table12.2p45|||||||||
34511|Erehwon Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Superseded by Thorndale Composite Gneiss and Mulculca Formation of the Willyama Supergroup (Stevens, 1995). Referred to as Suite 2 by Stevens, Stroud et al (1979, 1980). ||||||
37313|Ermelo Dacite|24010|6|Mentioned|p394 Fig. 11|||||||||
37313|Ermelo Dacite|24603|5|Briefly described|p868 Fig. 3|Namurian|Namurian|Dacite is Dt in text of figure.  Geological Province: Tamworth Belt.||||||
38469|Errinundra group|23309|5|Briefly described|p5 Fig. 1.3|||Informal-See Errinundra Group.||||||
38469|Errinundra group|24133|5|Briefly described|p20 Fig. 8|Early Devonian|Silurian|Informal.  Geological Province: Lachlan Fold Belt.||||||
38469|Errinundra group|24551|5|Briefly described|p118 Fig. 5.1|Devonian|Devonian|Informal - see Errinundra Group.||||||
73701|Errowan Intrusive Complex|63286|6|Mentioned|p304|Ordovician|Ordovician|||||||07-FEB-11
34288|Errowan Syenite""|22679|6|Mentioned|p 37|||||||||
68032|Escott Zeolitite|50613|6|Mentioned|p207 Tb. 1|||Probably informal, or an abbreviation - see Escott Zeolitite Member.||||||22-FEB-05
35229|Eskersley Formation|22969|5|Briefly described|Appendix 1 p 22|||Maybe misspelt? Eckersley?||||||
35261|Estelville Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
32263|Etheridge Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab21.||||||
32263|Etheridge Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
83063|Ettlewood CS|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Broken Hill block-Euriowie block.|1693 +/- 4 Ma|Allendale Metasediments||||
29886|Ettlewood Calcsilicate Member|23223|5|Briefly described|p39|||Described as 'Bimba suite - Ettlewood Calcsilicate Member (BS-ECM)' - meaning equivalence. of Allendale Metasediments, Broken Hill Group.||||||
29886|Ettlewood Calcsilicate Member|23347|5|Briefly described|p52|||Of the Broken Hill Group. Geological province: Broken Hill Domain.||||||24-MAR-09
29886|Ettlewood Calcsilicate Member|43052|6|Mentioned|p86, Fig. 4.22|||of Allendale Metasediments, Broken Hill Group||||||
29886|Ettlewood Calcsilicate Member|43086|6|Mentioned|p3|||of Broken Hill Group. Same as Ettlewood Calc-Silicate Member.||||||
29886|Ettlewood Calcsilicate Member|64742|6|Mentioned|p320.|||Formal version has Calc-Silicate (see pp320-321, p323).||||||29-MAR-12
77692|Ettrema Limestone member|68298|5|Briefly described|p215, 216||Frasnian|Age: late Frasnian based on conodonts of the upper gigas Zone (Pickett, 1972). Oldest reliable age for Late Devonian marine transgression.||||||
72897|Euchabil Gap Formation, middle|62569|5|Briefly described|p607|||Originally interpreted by Conolly (1965) and now represented by Cloghnan Shale of the Hervey Group. ||||||
38924|Eugowra Granite""|24417|6|Mentioned|p95|||Has been used by authors to describe Eugowra Suite.||||||
40438|Eugowra Suite Granites|24580|6|Mentioned|p828 Fig.1|||Informal - see Eugowra Suite. Geological Province: Eastern Lachlan Fold Belt.||||||
40439|Eugowra Suite granites|24580|6|Mentioned|p828|Eifelian|Emsian|Informal - see Eugowra Suite. Geological Province: Eastern Lachlan Fold Belt.||||||
73658|Eugowra granite|63291|6|Mentioned|p419 Fig. 2|||Informal name.||||||
73658|Eugowra granite|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
40437|Eugowra granites|24580|6|Mentioned|p828|||Informal - see Eugowra Granite. Geological Province: Eastern Lachlan Fold Belt.||||||
82740|Eukey Monzogranite Phase|71628|5|Briefly described|p15: 35, 102-104, 115|||This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.||Severn River Monzogranite.||Abuts Mount Norman Leucomonzogranite and Ruby Creek Leucogranite.||
78539|Eulah Sandstone|43194|5|Briefly described|p96 Tb. 8.1, p121|Triassic|Triassic|Of Martignoni (1986). Obsolete name . Equivalent to the upper part of the Napperby Formation, Gunnedah Basin.||||||27-NOV-13
68103|Eulo Ridge Granite|44093|5|Briefly described|p70|Late Devonian|Late Devonian|In Eromanga Basin. Age: 386Ma.||||||
68103|Eulo Ridge Granite|67874|6|Mentioned|p50|||Mentioned in analytical session metadata.||||||
68103|Eulo Ridge Granite|68731|5|Briefly described|p166|||Several small areas (< 5 km2) of granite mapped in southwestern Queensland between Eulo and Hungerford, forming part of the Eulo Ridge, were collectively referred to as Eulo Ridge Granite by Scheibner and Basden (1996, p.70). Textural and compositional variations indicate several discrete plutons, confirmed by isotopic dating. Identified separately as Currawinya Granite, Eulo Granite, Hungerford Granite and Granite Springs Granite. See also Eulo Granite.||||||03-JUL-14
68103|Eulo Ridge Granite|68823|6|Mentioned|p378 Fig.4|Givetian|Givetian|See also Eulo Granite (p393). Geochronology by Bultitude and Cross (2012).|ca 385 Ma|||||
68103|Eulo Ridge Granite|69541|5|Briefly described|p645 Fig.1(b)|Middle Devonian|Middle Devonian|Thomson Orogen.|385 Ma.|||||
68103|Eulo Ridge Granite|69952|6|Mentioned|p15|||Scheibner and Basden (1996). Name used to refer to several small areas of granite forming part of the Eulo Ridge between Eulo and Hungerford. Superseded by Eulo Granite and Granite Springs Granite (and probably others).||||||
68103|Eulo Ridge Granite|73179|6|Mentioned|p1133, p1134 Fig.1, p1152|Frasnian|Eifelian|Thomson Orogen, southern. Geochron from Cross et al. (2015).|385 +/- 2.5 Ma|||||20-SEP-22
78562|Eulo Ridge Granites|68731|6|Mentioned|p213 Fig 3.118|||See also Eulo Ridge Granite. See also p166 - Granites of the Eulo Ridge.||||||17-DEC-13
37309|Eulowrie Pyroclastics|24010|5|Briefly described|p381|Westphalian|Westphalian|Age:310.6+/-4Ma (SHRIMP U/Pb)||||||
37309|Eulowrie Pyroclastics|24603|5|Briefly described|p868 Fig. 3 (caption)|Stephanian|Westphalian|Of the Lark Hill Formation.  Age: 310.6+/-4.0Ma.  Geological Province: Tamworth Belt.||||||
37309|Eulowrie Pyroclastics|24605|5|Briefly described|p933 Fig.2|Carboniferous|Carboniferous|Geological Province: New England Orogen.||||||
37309|Eulowrie Pyroclastics|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|||||||
37309|Eulowrie Pyroclastics|61214|5|Briefly described|p171 Fig. 1|Westphalian|Westphalian|Of Lark Hill Formation. Geological Province: Boomi Block and Darthula Block. See also p172 Fig. 2. Presented as only Eulowrie in text of figure.||||||
23583|Euranbene Adamellite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
23583|Euranbene Adamellite|40276|2|Defined|p16|Early Devonian|Early Devonian|||||||
79186|Eurimbla Conglomerate|68592|6|Mentioned|p409|||Of Bartolo (1994) and O'Sullivan (1993). Formerly part of Kenyu Formation of Stevens (1955) and Gibbons (1960). Here renamed Eurimbla Formation to include associated sandstone and siltstone which had been assigned as equivalents of Adaminaby Group, Kenyu Formation or Hawkins Volcanics.||||||
24964|Euriowie Group|41630|6|Mentioned|p13|||Mineral deposit category of Andrews (1922).||||||
26540|Euriowie Sub-Group|30261|4|Described|Table 1|||Sturtian - Marinoan age||||||
26540|Euriowie Sub-Group|33004|6|Mentioned|p136|||||||||
26540|Euriowie Sub-Group|34812|4|Described|p78|||||||||
26540|Euriowie Sub-Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26540|Euriowie Sub-Group|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26540|Euriowie Sub-Group|37931|6|Mentioned|p531|||||||||
26540|Euriowie Sub-Group|39214|6|Mentioned|p5|||See P7||||||
26540|Euriowie Sub-Group|46889|6|Mentioned|p275|||||||||
76040|Eurolie granodiorite|66934|5|Briefly described|Map legend|Early Devonian|Late Silurian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Booroorban Granodiorite Suite.|||Interpreted granodiorite similar to Booroorban granodiorite.|
41554|Eurombedah unit|50616|4|Described|p280-281|Late Miocene|Late Miocene|Informally named clays and sand near Narromine, distinctive stratigraphic unit not yet formally designated as a formation. Conformably underlies the basal Mickety Mulga unit.||||||
37112|Eurow Formation""|23214|6|Mentioned|p231|||Superseded by Eurow Member.||||||
37112|Eurow Formation""|23392|6|Mentioned|p15|||||||||
31702|Eurow Member|23214|4|Described|p231|Late Devonian|Late Devonian|Lower part of Cookamidgera Formation. Previously Eurow Formation. Sequence of friable siltstone and shale.||||||
31702|Eurow Member|23217|6|Mentioned|p17|||See also "Eurow Member".||||||07-MAR-06
31702|Eurow Member|43640|5|Briefly described|Map Legend|Devonian|Devonian|of Cookamidgera Formation||||||
31702|Eurow Member|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Cookamidgera Formation, Hervey Group. Consists of friable red siltstone and shale.||||||17-JUL-08
31702|Eurow Member|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Cookamidgera Formation, Hervey Group.||||||
37115|Eurow Member""|23217|6|Mentioned|p16|||Proposal by Pgson and Watkins (1998) as lower part of a "Cookamidgera Formation".  See Eurow Formation.||||||07-MAR-06
37115|Eurow Member""|23392|6|Mentioned|p24|||Of Pogson & Watkins (1998). Superseded by Eurow Formation. Of Cookamidgera Formation.||||||
37115|Eurow Member""|24417|5|Briefly described|p140|||Of "Cookamidgera Formation".  Retained as Eurow Formation of Hervey Group.||||||
25902|Eusdale Adamellite|23214|6|Mentioned|p253|||Superseded by Eusdale Granite.||||||
25902|Eusdale Adamellite|30709|6|Mentioned|p26|||||||||
25902|Eusdale Adamellite|35503|2|Defined|p204|Carboniferous|Carboniferous|New name refs Facer (1977)||||||
30811|Evan's Head Coal Measures|43384|14|Not recorded|Map Legend||Triassic|||||||
30811|Evan's Head Coal Measures|43881|2|Defined|p6-7,10,28-9,80,106||Triassic|||||||
73408|Evelyn Creek Suite|66920|5|Briefly described|Map legend|Cambrian|Cambrian||||||Dark brown to green aphanitic metadolerite, variably folded.|
73408|Evelyn Creek Suite|66922|5|Briefly described|Map legend|Ordovician|Cambrian|The two sub-units are mapped separately. Both are foliated and folded.|||||Dark grey, medium-grained alkaline monzodiorite sills and dykes; dark brown to green, aphanitic alkaline mafic (basalt to trachybasalt) sills or flows with amygdales and possible vesicles, regionally metamorphosed to greenschist facies.|
76150|Evelyn Creek volcanics|66623|2|Defined|pp51-55.|Late Cambrian|Middle Cambrian|First defined in this publication as informal unit. Formerly part of Torrowangee Series (Mawson 1912). May be related to Williams Peak Granite on bases of age, geochemistry and setting. Possible geochemical affinity with Tibooburra Suite. Mostly altered to an assemblage of chlorite, sericite, carbonate, epidote and rare biotite. Individual bodies range from a few metres to 100 m thick.||||Intrudes Depot Glen and Easter Monday Formations.|Medium-grained, dark grey, monzodiorite sills and dykes; brown to green aphanitic metabasalt, interlayered with Easter Monday Formation; brown to green, aphanitic, basalt to trachybasalt sills or flows with amygdales and vesicles. Strongly foliated.|
76150|Evelyn Creek volcanics|67209|5|Briefly described|Map legend.|Ordovician|Cambrian||||||Dark brown to green aphanitic metadolerite, variably folded.|03-OCT-13
76150|Evelyn Creek volcanics|67322|5|Briefly described|p13|Late Cambrian|Drumian|Informally named by Greenfield, in Greenfield et al. (2010). An ungrouped unit. Age is based on magmatism coeval with the deposition of the Depot Glen Formation (Teltawongee Group), followed by intrusion into this unit, and finally extrusion coeval with the Easter Monday Formation (Late Cambrian). Restricted to flows, sills, and dykes. Occurs in the Tibooburra and Mount Poole Inliers.|||||Mafic igneous rocks of alkaline affinity.|
76150|Evelyn Creek volcanics|72522|6|Mentioned|p125.|||Identified by Greenfield et al. (2010).||||||
76150|Evelyn Creek volcanics|72951|6|Mentioned|p1012|||||||Intrudes the Warrata Group.|Magmatic rocks.|
70404|Evergreen Formation""|60998|6|Mentioned|p145|||Informal - see Evergreen Formation. ||||||
82741|Ewingar Monzogranite Phase|71628|5|Briefly described|p11: 3, 27, 29-35|||New name, after Mustard (2004). Named after the locality of that name, 40 km E of Tenterfield, Timbarra Tableland. Outcrop area is ~150 km2. Geochemistry briefly described.||Rocky River Monzogranite.||Intrudes Drake Volcanics. Abuts the other Phases of the parent unit.|Medium- to very coarse-grained, porphyritic, pink K-feldspar-megacrystic (average 17mm) biotite-hornblende monzogranite.|
39630|Extended Basalt|24087|6|Mentioned|p336 Fig. 8|||See also Extended basalt.   Geological Province: Lachlan Fold Belt.||||||
39630|Extended Basalt|61410|6|Mentioned|p29, |||||||||
38228|Eyriebower Coal|23717|5|Briefly described|p118 Fig.2|Permian|Permian|Geological Province: Sydney Basin||||||
73704|Fairbridge Formation|63286|5|Briefly described|p294 Fig. 1|Ordovician|Ordovician|Consists of basalt lava, volcanic sandstone, mudstone and conglomerate, also has mudium-K and high-K calc-alkaline affinities (Crawford et al. 2007).||||||07-FEB-11
73704|Fairbridge Formation|67106|6|Mentioned|p674|||||||||
73675|Fairbridge Volcanics, lower|63278|6|Mentioned|p145 Fig. 1, p146 Fig. 2a|Middle Ordovician|Middle Ordovician|Informal name. Geological Province: Molong Volcanic Belt, Lachlan Fold Belt.||||||07-FEB-11
73676|Fairbridge Volcanics, middle|63278|6|Mentioned|p145 Fig. 1, p146 Fig. 2a|Late Ordovician|Middle Ordovician|Informal name. Geological Province: Molong Volcanic Belt, Lachlan Fold Belt.||||||07-FEB-11
73677|Fairbridge Volcanics, upper|63278|6|Mentioned|p145 Fig. 1, p146 Fig. 2a, p152, p160|Late Ordovician|Middle Ordovician|Informal name. Geological Province: Molong Volcanic Belt, Lachlan Fold Belt.||||||07-FEB-11
38960|Fairholme igneous complex""|24417|6|Mentioned|p194|||Informal name.||||||
31275|Fairview Sandstone|43500|14|Not recorded|Map Legend|||(Provisional Edition) (no card)||||||
31080|Fal Brook conglomerates|43477|14|Not recorded|p47||Late Permian|Ref.to Raggatt 1938.(unpubl.thesis) Included in Rix's Creek formation.(Newcastle Coal Measures)||||||
24973|Far Away Hills Quartzite|22730|5|Briefly described|p559||Proterozoic|||||||
24973|Far Away Hills Quartzite|29991|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
24973|Far Away Hills Quartzite|38632|6|Mentioned|p20|||||||||
24973|Far Away Hills Quartzite|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group||||||
24973|Far Away Hills Quartzite|43502|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group. Marinoan div. of U.Proterozoic||||||
24973|Far Away Hills Quartzite|67562|6|Mentioned|p103 Fig.9|Precambrian|Precambrian|||||||
31075|Farley Beds|44489|14|Not recorded|p70|||See also Lexicon.||||||
31075|Farley Beds|48831|14|Not recorded|p.7|||||||||
31191|Farley Sandstone|43491|14|Not recorded|pVII/44||Permian|(Lower Marine Series)||||||
30753|Farley Stage|43344|14|Not recorded|p84||Permian|||||||
30753|Farley Stage|43382|14|Not recorded|p74|||||||||
30753|Farley Stage|43440|14|Not recorded|p91|||Ref to David 1950||||||
30753|Farley Stage|43477|14|Not recorded|p15,17,Pl.3|||Ref. to David||||||
30753|Farley Stage|44063|14|Not recorded|p281|||||||||
30753|Farley Stage|44861|14|Not recorded|p228,245||Early Permian|||||||
30753|Farley Stage|48600|14|Not recorded|p30|||Includes fossil Cancrinella farleyensis. See also Lexicon.||||||
31076|Farley beds|43477|14|Not recorded|p29|||||||||
31076|Farley beds|43491|14|Not recorded|pVII/45||Permian|||||||
81438|Farmborough Claystone|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Sydney Basin. CA-TIMS age of 254.1 Ma (Metcalfe etal., 2015), corresponding to D. parvihola zone (Wuchiangpingian).||Unit of Illawarra Coal Measures.||||
81438|Farmborough Claystone|73304|5|Briefly described|p65-66, p70, p74|Changhsingian|Wuchiapingian|[Probably an abbreviation of Farmborough Claystone Member].
Dates on both this unit, and from tuff 1m above (253.59+/-0.05 Ma) in Wongawilli Coal.|254.10 +/- 0.32 Ma U-Pb CA-TIMS.|Illawarra Coal Measures||||
81438|Farmborough Claystone|73421|6|Mentioned|p16|Changhsingian|Wuchiapingian|Sydney Basin, southern. Age from Metcalfe et al., (2015).|254.10+/-0.32 Ma|Illawarra Coal Measures||||
37957|Farmcote gneiss|24307|6|Mentioned|p973|Paleoproterozoic|Paleoproterozoic|Informal name - see Farmcote Gneiss.   Age: 1704+/-3Ma||||||07-NOV-08
34180|Farmcote gneiss""|22641|4|Described|p688, p692|||Possibly Archaean?||||||23-JUN-08
34180|Farmcote gneiss""|64097|6|Mentioned|p309, p328 Appdx., p309|||Informal reference to all or part of Farmcote Gneiss rocks before it was formally defined.||||||07-FEB-11
31919|Farquhar's Creek Seam|43881|14|Not recorded|p6-7,27|||Basal unit of Basin Creek Formation (q.v.)||||||
70665|Farquhars Coal Seam|61310|5|Briefly described|p34|||Within the Basin Creek Formation (Nymboida Coal Measures).  Has the only coal to be mined from the Nymboida Coal Measures. Seam Thickness: 1.8m. Geological Province: Clarence-Moreton Basin.||||||
81439|Fassifern Lower Seam|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS age of 253.38 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||||||
81439|Fassifern Lower Seam|73304|5|Briefly described|p65, p70, p75|Changhsingian|Changhsingian|[Written as Fassifern Lower Seam and ""Fassifern Lower Seam"" and lower Fassifern Seam p67].",,|253.38 +/- 0.31 Ma U-Pb CA-TIMS.|||||
30971|Fassifern Sandstone|43440|14|Not recorded|p49|||Unit of Newcastle Coal Measures||||||
30971|Fassifern Sandstone|43477|14|Not recorded|p21,50,56|||||||||
74609|Featureless Sandplain|61964|6|Mentioned|p154|||See also "The Featureless Sandplain" and "Featureless sandplain"||||||
74608|Featureless Sandplain, The""|61964|6|Mentioned|p14 Fig. 4, p153 Fig. 42|||Referred to as a unit in text. See also "Featureless Sandplain" and "Featureless sandplain". ||||||
74610|Featureless sandplain""|61964|3|Fully described|p163-168|Late Pleistocene|Middle Pleistocene|Of Cameron (1996b) after Brown and Stephenson (1991b) who originally named unit "Unnamed Quaternary Aeolian Sand Plain Unit" - name explained in text. Precursor of Woorinen Fm. Lith. incl. Overlies Shepparton Fm or Calivil Fm; underlies Woorinen Fm ||||||
24976|Fencers Creek Conglomerate|35070|6|Mentioned|p3|||||||||
24976|Fencers Creek Conglomerate|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
24976|Fencers Creek Conglomerate|35608|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24976|Fencers Creek Conglomerate|35609|6|Mentioned|p6|||||||||
24976|Fencers Creek Conglomerate|36411|6|Mentioned|p268|||Refers Basden et al 1978 for definition.||||||
83489|Fences Creek Conglomerate|73483|6|Mentioned|p408|||||Blowering Formation||||
83487|Fences Creek beds|73483|6|Mentioned|p408-409|||||Blowering Formation||||
30967|Fennel Bay Chert|43440|14|Not recorded|p49|||Unit of Newcastle Coal Measures||||||
30967|Fennel Bay Chert|43477|14|Not recorded|p56|||Fennel Bay cherts - p21||||||
37176|Fermor Volcanics|23522|5|Briefly described|p253|Devonian|Devonian|||||||
28550|Fern Valley Coal Formation|37083|6|Mentioned|p164|||||||||
31225|Fern Valley Conglomerate|43477|14|Not recorded|p21,53||Late Permian|Unit of Newcastle Coal Measures||||||
35121|Fern Valley coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for seam within the Adamstown Formation (Newcastle Coal Measures.). Geological Province: Sydney Basin.||||||
35121|Fern Valley coal seam|23055|6|Mentioned|p34|||||||||
35121|Fern Valley coal seam|68711|5|Briefly described|p118, p116 Tbl 3|||Informal unit.||Within Adamstown Formation||||
73686|Ferndale Monzonite|63283|6|Mentioned|p191 Tb. 2|Late Ordovician|Middle Ordovician|Age: 445Ma. Geological Province: Molong Volcanic Belt.||||||04-NOV-14
26548|Fernleigh Group|22857|5|Briefly described|p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Geological Province: Bindook Rise.||||||
26548|Fernleigh Group|30735|4|Described|p42|||||||||
26548|Fernleigh Group|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26548|Fernleigh Group|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
26548|Fernleigh Group|39568|6|Mentioned|p78|||Name proposed to be abandoned.||||||
26548|Fernleigh Group|68592|6|Mentioned|p1093|||Jones, Carr et al. (1984) demonstrated that this unit was a junior synonym of the Tangerang Formation; they also reduced the Windellama Limestone constituent to Member status within that Formation.||||||
34289|Fernside Diorite""|22679|6|Mentioned|p 40|||||||||
27405|Fiery Range Porphyry|39800|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Late Middle Devonian.||||||
27405|Fiery Range Porphyry|45147|6|Mentioned|M127|||||||||
82744|Fife Suite|71628|6|Mentioned|p17:95||||||Fife Monzogranite.|||
39941|Fifield Complex|24263|5|Briefly described|p1387||Late Ordovician|||||||
39941|Fifield Complex|24267|5|Briefly described|p1508 Fig.1||Ordovician|Geological Province: Parkes-Narromine Belt||||||
39941|Fifield Complex|67107|6|Mentioned|p700|||||||Intrudes Girilambone Group.|Alaskan-type intrusions. Appears as Fifield complex.|
39941|Fifield Complex|73154|5|Briefly described|p79|||Associated with minor PGE mineralisation. See also Fifield Complexes, Fifield complexes.|||Hylea Intrusion/Hylea Intrusive Complex||Ultramafic to mafic 'Alaskan-style' complex.|
73574|Fifield Complexes|63288|6|Mentioned|p354 Fig. 1, p358|Early Silurian|Early Silurian|Belived to be compositionally similar to the Nash Hill Volcanics (Crawford et al. 2007).||||||
73574|Fifield Complexes|70684|6|Mentioned|p9 Fig.4(f)|Early Silurian|Early Silurian|||||||
73574|Fifield Complexes|73154|5|Briefly described|p75, p77 Fig.3|Llandovery|Late Ordovician|Junee-Narromine Belt. Emplaced into deformed Ordovician metaturbidites, hosts minor PGE mineralisation. See also Fifield Complex p79, Fifield complexes p84.|443 Ma, 448 Ma||||Alaskan-type ultramafic to mafic intrusions.|
80006|Fifield Igneous Complex|70684|6|Mentioned|p54 Fig.27|||||||||
80006|Fifield Igneous Complex|72495|6|Mentioned|p217-218|||Coincides with the western gravity high in the Junee-Narromine volcanic belt.||||||
73684|Fifield complexes|63283|6|Mentioned|p206-208, p210|||Parental magmas are Nash Hill Volcanics. Consists of rare intrusive plugs. See p206-207 for more infotmation.||||||07-FEB-11
73684|Fifield complexes|73154|5|Briefly described|p84|Llandovery|Late Ordovician|See also Fifield Complexes and Fifield Complex.|443+/-2 Ma zircon Pb/U||Honeybugle Complex||Includes monzonite.|
83562|Fig Tree Coal|73304|6|Mentioned|p74|||[Probably misspelt from Figtree Coal Member]. Sydney Basin, southern.||Illawarra Coal Measures||||
70080|Figtree coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Pheasants Nest Formation (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
26552|Figurehead Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Figurehead Adamellite.||||||
77249|Finch Clay|68004|5|Briefly described|p205.|||An impermeable bed within a sandstone unit: suggested as an assessment criterion for precious opal formation.||Unit in Wallangulla Sandstone Member.||||
82872|Finch Clay Facies|73203|6|Mentioned|p648|Cretaceous|Cretaceous|[Variation of informal published name? See Finch clay facies]. Hosts opal at Lightning Ridge. Similar trace element concentrations as Wallangulla Sandstone.||Griman Creek Formation|||Highly weathered.|
70149|Fine Arenite, Central|23336|5|Briefly described|p15, p17 Fig. 12, p27|||Part of the classification of Neef et al (1995) of Coco Range Sandstone into Lower, Central and Upper Fine Arenite, a sequence which includes also The Valley Tank Member and Copi Tank Member. Max. thickness: ~240m.||||||21-MAR-06
70150|Fine Arenite, Lower|23336|5|Briefly described|p15, p17 Fig. 12, p27|||Part of the classification of Neef et al (1995) of Coco Range Sandstone into Lower, Central and Upper Fine Arenite, a sequence which includes also The Valley Tank Member and Copi Tank Member. Max. thickness: ~300m.||||||21-MAR-06
79159|Fine Arenite, Upper|23336|5|Briefly described|p15, p17 Fig. 12, p26-27, p28|||Part of the classification of Neef et al (1995) of Coco Range Sandstone into Lower, Central and Upper Fine Arenite, a sequence which includes also The Valley Tank Member and Copi Tank Member. Max. thickness: >500m.||||||
72330|Fish Bed Chert""|62578|5|Briefly described|p44|Jurassic|Jurassic|Of Dulhunty and Eadie (1969) when referring to their Talbragar Fossil Fish Bed. "A hard, fine limonitic cherty shale" (Dulhunty and Eadie (1969).||||||26-JUL-06
39820|Fish Hill Limestone Member|24250|5|Briefly described|p123|Eifelian|Eifelian|Parent: Broken River Group||||||
30870|Fitzroy beds|43385|14|Not recorded|p171||Silurian|||||||
30870|Fitzroy beds|44645|14|Not recorded|p23||Silurian|||||||
37194|Five Day Creek Phyllite""|44450|6|Mentioned|p87|||Geological Province: New Enlgand Fold Belt||||||
39357|Five Days phyllites|24120|5|Briefly described|p6|Permian|Permian|||||||
24982|Five Islands Basaltic Andesite|40270|6|Mentioned|Table 2|||||||||
82743|Five Mile Creek Syenogranite Phase|71628|4|Described|p16: 5,9, 11-18, 20, 22, 31; p19: 97,163|||New name (this study); previously Five Mile Creek Syenogranite of Sivell and Passmore (1999) after unpublished work by Passmore (1998). Originally part of Stanthorpe Monzogranite. Named after a local watercourse. Occurs ~10 km NNW of Liston, 8 km ESE of Maryland. Commonly crops out as clusters of (sub)-rounded boulders on gently rolling hills. Geochemistry described in some detail; is assigned geochemically to the Five Mile Creek Suite.|242.2 Ma (Rb-Sr; Shaw, 1994).|Cullendore Syenogranite.||Intrudes Undercliffe Falls Monzogranite. Is intruded by Mossvale Alkali Feldspar Granite Phase and Herding Yard Creek Intrusives. Abuts The Ridge Monzogranite.|Medium-grained, seriate to mildly porphyritic, biotite-hornblende syenogranite. A-type(?).|
41609|Flagstaff Formation, lower|44244|6|Mentioned|p79|Visean|Visean|Informal - see Flagstaff Formation.||||||
41610|Flagstaff Formation, upper|44244|6|Mentioned|p79, p263|||Informal - see Flagstaff Formation.||||||
41611|Flagstaff Sandstone""|44244|6|Mentioned|p63|||Informal name.  Superseded by Flagstaff Formation.||||||18-AUG-04
80150|Flemming Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
80248|Flint Hills Chert|67847|6|Mentioned|p25|Late Ordovician|Middle Ordovician|||||||
36199|Fluviatile Conglomerate""|23392|6|Mentioned|p7|||Informal subdivision of Jones (1984) BSc Hons, of the Mogongong Conglomerate Member.||||||
81992|Folley Point Limestone Member|71656|6|Mentioned|p13 Fig.2, p31|Pridoli|Pridoli|[misspelling of Folly Point?]. Shown In Fig.2 as Pridoli age.||Frome Hill Formation, Bungonia Group||Overlain by Efflux Siltstone Member.|Fossiliferous limestone.|
37293|Folly Basalt|24009|5|Briefly described|p368|Middle Devonian|Middle Devonian|Referred to as Folly Volcanics by Stratford and Aitchson (1997).||||||
37293|Folly Basalt|63774|6|Mentioned|p1083|Middle Devonian|Middle Devonian|||||||
37293|Folly Basalt|68008|6|Mentioned|p19|||Nundle area, NSW. Similar geochemistry to Calliope  beds, Yarrol Province.||||||
23597|Folly Point Limestone|22842|6|Mentioned|p26|||Superseded by Folly Point Limestone Member||||||
23597|Folly Point Limestone|40698|6|Mentioned|p53|||Are actually Lookdown Limestone||||||
70005|Folly Spilite|61766|5|Briefly described|p68|Middle Devonian|Middle Devonian|Correlated with Ghanghat Basalt. In the Nundle district south of Tamworth. Overlain by the Yarramie Formation.||||||27-JAN-06
34393|Folly Spilite""|22736|6|Mentioned|p630|Frasnian|Emsian|||||||
77358|Folly Spillite|68005|5|Briefly described|p49 Fig.3-M, p150, p170.|Givetian|Eifelian|Tamworth Belt. [Mis-spelling of Spilite].||Unit in Tamworth Group.|||Massive basalts with subordinate intercalated basaltic pillow lavas, albite dolerite, siliceous argillite, sandstone and rare basaltic breccias.|
83488|Fontenoy Serpentinite''|73483|6|Mentioned|p408|||Northern part of Wambidgee Serpentinite Belt, in the Fontenoy area. Termed 'Fontenoy Serpentinite' by Cooper, (1985). Faulted against the Young Granodiorite and the Jindalee Group.||||Faulted against Young Granodiorite||
31821|Footwall Gneiss|45003|14|Not recorded|p331,333-4,337|||||||||
31821|Footwall Gneiss|73575|6|Mentioned|p826|||Of Webster (2006), shown with the Hangingwall Gneiss in this study as a single unit (Rasp Ridge Granite Gneiss).||||||
82746|Forbes River Porphyrite|71628|5|Briefly described|p17: 2, 97-98|||New name (this study), after a local watercourse. Occurs ~10 km NNW of Birdwood and ~40 km WNW of Wauchope. Extent unknown; occurs in highly rugged, inaccessible country. Geochemically unaffiliated, but part of the Coastal Granite Association.||Forbes River Suite.||Intrudes Birdwood and Rollans Road Formations, and Werrikimbe Volcanics.|Quartz-feldspar porphyrite, microgranite porphyrite, monzogranite porphyrite, and associated quartz porphyry dykes.|
82747|Forbes River Suite|71628|5|Briefly described|p17:97|||Coastal Granite Association.|||Forbes River Porphyrite.|||
35380|Forest Reef Volcanics|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
35380|Forest Reef Volcanics|23202|6|Mentioned|Fig.1||Ordovician|of Cabonne Group||||||
35380|Forest Reef Volcanics|24398|5|Briefly described|p259 Fig. 2|Bolindian|Eastonian|||||||
35380|Forest Reef Volcanics|63292|6|Mentioned|p451|||Informal; misspelt. Probably Forest Reefs Volcanics. Ridgeway and Cadia East (underground) ore spreads out into this unit.||||||
34260|Forest Reefs Beds""|22679|6|Mentioned|p 17|||replaced by Angullong Tuff||||||
75067|Fort Cooper Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
70405|Fossil Wood Member""|60999|6|Mentioned|p175 Tb. 3|||||||||
82745|Four Bull Suite|71628|6|Mentioned|p19:37||||||Four Bull Granodiorite.|||
30970|Four Mile Creek Sub-Group|43440|14|Not recorded|p35,fig.4-3||Permian|Unit of Tomago Coal Measures||||||
31241|Four-mile Creek beds|43491|14|Not recorded|pVII/52||Permian|||||||
39666|Fox Tor Diorite|62534|6|Mentioned|p22|Triassic|Triassic|Age: 240Ma.||||||07-FEB-11
39666|Fox Tor Diorite|62757|2|Defined|p6, p3 Fig. 1, p5 Fig. 2|Middle Triassic|Middle Triassic|Intrusive into Bundarra Supersuite. Age:239.7+/-6.7Ma (K-Ar). Composed essentially of single rock type - two pyroxene-hornblende-biotite-quartz diorite. Grey, mesocratic, relatively equigranular and medium-grained. I-type within an S-type supersuite||||||07-FEB-11
39666|Fox Tor Diorite|68005|5|Briefly described|p70, p136, p170.|Early Triassic|Permian|Informal name: Brown (2003). A small, highly conspicuous body. Produces an intense magnetic high, indicating a plug-like structure. Written as Foxtor Diorite on p.136 and p170.|239.7 +/- 6.7 Ma (K-Ar).|Unit in Moonbi Supersuite.||Intrudes the Pringles Monzogranite.||
39666|Fox Tor Diorite|71628|6|Mentioned|p19:39|||Stonestreet et al. (2006). Originally the informal 'Fox Tor diorite' of Brown (2003). Now Fox Tor Quartz Diorite.||||||
82449|Fox Tor Suite|71628|6|Mentioned|p19:40||||||Fox Tor Quartz Diorite.|||
41057|Fox Tor diorite""|24366|5|Briefly described|p11, 17 Fig. 3|Early Permian|Early Permian|Of the Bundarra Plutonic Suite.  Informal Name.||||||
41057|Fox Tor diorite""|71628|6|Mentioned|p19: 39|||Informal name by Brown (2003); formalised by Stonestreet et al. (2006). Now Fox Tor Quartz Diorite.||||||
24990|Foxlow Beds|23048|5|Briefly described|p2||Late Ordovician|||||||03-OCT-07
24990|Foxlow Beds|23550|4|Described|Fig 1 p502.|||(Probably misspelt) - should be 'beds'||||||
24990|Foxlow Beds|24128|5|Briefly described|p3|Ordovician|Ordovician|See also Pittman Formation.  Geological Province: Lachlan Fold Belt.||||||
24990|Foxlow Beds|29992|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
24990|Foxlow Beds|29994|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
24990|Foxlow Beds|30332|6|Mentioned|p126|||Refers Strusz(1971)||||||
24990|Foxlow Beds|30433|5|Briefly described|Fig.2|||||||||
24990|Foxlow Beds|32820|5|Briefly described|p2|||||||||
24990|Foxlow Beds|36413|2|Defined|p26-27|Ordovician|Ordovician|||||||09-JUN-09
24990|Foxlow Beds|36414|5|Briefly described|map legend|Llandoverian|Late Ordovician|Greywacke, shale, slate, black carbonaceous pyritic slate, and minor chert. Includes unnamed units: slate (-Ofc); schist (-Ofk); sandstone (-Ofs). Unconformably underlies Cappanana Formation and Copper Creek Shale. GSNSW map code: -Of (theta symbol + f).||||||
24990|Foxlow Beds|37251|5|Briefly described|p240|||||||||
24990|Foxlow Beds|37727|6|Mentioned|Fig.1|||||||||
24990|Foxlow Beds|39331|6|Mentioned|p45|||See also P52||||||
24990|Foxlow Beds|39627|6|Mentioned|p268|||||||||
24990|Foxlow Beds|40136|5|Briefly described|p25|||||||||
24990|Foxlow Beds|40328|6|Mentioned|p60|||||||||
24990|Foxlow Beds|40646|6|Mentioned|p39|||||||||
24990|Foxlow Beds|42497|5|Briefly described|Map Legend|Bolindian|Gisbornian|||||||
24990|Foxlow Beds|48878|2|Defined|Fig.3,p.7,p.4-6||Ordovician|On many pages. p.1,7,18,19,25,36. Contains Bullongong Shale Member in upper part. Ord. (I55-16).||||||
24990|Foxlow Beds|61895|6|Mentioned|p133, p134 Fig.1|Ordovician|Ordovician|Graptoloid fauna of Eastonian age.|||||Includes graptolite-bearing black shales near the top, weathering to whitish, soft mudstone with haematite staining.|24-SEP-14
34011|Foxlow Formation|22577|6|Mentioned|p120||Ordovician|replaced by Adaminaby Group||||||
34572|Foxlow beds""|22815|5|Briefly described|p18|Ordovician|Ordovician|Superseded by Adaminaby Group.||||||08-MAR-16
83496|FoyBrook Andesite|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, forearc basin. Zircon probability plot from Roberts et al., (1995a). Also shown as Foybrook Andesite p1396 Fig.18.||||||
83480|Foybrook Andesite (Member)|73487|6|Mentioned|p566 Fig. 2|Tournaisian|Tournaisian|Rouchel Block. Age uncertain form diagram. May be Famennian.||||||01-SEP-22
32241|Free Damper Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah3||||||
32241|Free Damper Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
34281|Freeman Marble""|22679|6|Mentioned|p 35|||||||||
81252|French Park granite|72083|5|Briefly described|p15|||Informal name by Chappell et al. (1991). Mount Arthur area. May be part of the Collingullie Granite.||||||
34183|Freyers Metasediment|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26563|Frogs Hollow Granite|42726|5|Briefly described|map legend|Early Devonian||150. Reserved as Frogs Hollow Granodiorite.||||||29-AUG-12
37142|Fryers Formation|23565|5|Briefly described|p195|||Of Broken Hill Group||||||
79155|Funeral Creek Formation|69961|5|Briefly described|Map legend|Ordovician||||Unit in Kayrunnera Group.|||Single allochthonous block (20-30m thick) of brecciated, intraclast, conodont-bearing limestone (carbonate clasts are tabular and cm-scale; at contact between conglomerate and sandstone-siltstone units of Wheeney Creek Formation).|09-SEP-15
69160|Gabbo Suite|60423|6|Mentioned|p377 Fig. 5|||A Type suite. Geological Province: Lachlan Fold Belt.||||||
74617|Gabo Island granites|61964|6|Mentioned|p81|||Informal name. Geological Province: Lachlan Orogen.||||||
69721|Gabo suite|24222|6|Mentioned|p22|||Informal - see Gabo Suite.  Geological Province: Lachlan Fold Belt.||||||12-SEP-05
41309|Gadden Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
78507|Galambo granite|68823|6|Mentioned|p400|||||||||15-NOV-13
79860|Galore Hill Formation|71889|5|Briefly described|p65|||A small isolated sequence included in the Cocoparra Group by Trigg (2017). A brief petrographic description is provided.|||||Basal conglomerate and overlying sandstone.|
79860|Galore Hill Formation|72083|3|Fully described|p7, p41, p52-57|||New name, after Galore Hill which is capped by this Formation; a subdivision of previously undifferentiated Cocoparra Group. Comprises two separate bodies with a total area of c.3 km2. About 55km SE of Narrandera. The type section is the sequence along the road from GR 480040 6115145 up to GR 480730 6115020 (Narrandera 1:100k sheet). Is lithologically similar to Narrandera Sandstone; differences mentioned. Unfossiliferous.||Cocoparra Group.||Overlies Wagga Group unconformably and Billenbah Granite disconformably.|Thin, irregularly developed basal conglomerate, typically matrix-supported pebble to cobble conglomerate, <5m thick but up to 15m locally; fining upward into medium-grained quartz-rich sandstone and siltstone.|
79860|Galore Hill Formation|73457|4|Described|ii, p1, p3-6, p14|Late Devonian|Middle Devonian|Sedimentary sequence that caps Galore Hill, northeast of Lockhart. Total extent of only ca 3 square kilometres, estimated preserved thickness of 40m. Structure interpreted as an open syncline plunging shallowly to the southwest. Tentatively included in Mulga Downs Group by Trigg (2017) based on similarity with the Melbergen Sandstone. Basement lithologies are present as clasts in the basal conglomerate, could have been deposited in an alluvial fan with a lower energy and more distal depositional environment in the overlying quartz sandstone, non-marine. More details are given in Trigg (2017, 2018b), full definition in Trigg (2021).|391.3+/-4.4 Ma MDA detrital zircon (Huang, 2019)|Mulga Downs Group||Nonconformably overlies Gillenbah Granite in western part, unconformably overlies Adaminaby Group in eastern part|Basal polymictic conglomerate that rapidly fines up into quartz-rich sandstone forming the bulk of the unit. Thin beds of red siltstone are intercalated with the conglomerate and pebbly sandstone locally. Local sedimentary breccia at base.|
31546|Galore Suite|42726|5|Briefly described|map legend||Silurian|||||||
31546|Galore Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||08-MAR-05
81253|Galore granite|72083|5|Briefly described|p7, p13, p17, p41|||Informal name by Chappell et al. (1991) for granite outcrops immediately to the S of the Murrumbidgee River, in the study area. Obsolete: here included in the Collingullie granite. See also references to the Galore Granite (p7).|c.417 Ma (Bodorkos et al., in prep.)||||Sub-cropping equigranular, medium-grained granite.|
38936|Ganantagai Granite""|24417|6|Mentioned|p111|||Replaced by Ganantagi Granite.||||||
39387|Ganantagi granite|24125|5|Briefly described|p151|||Informal name.   Geological Province: Lachlan Fold Belt.||||||
82748|Gandar Granodiorite|71628|5|Briefly described|p3: 27|||Rosenbaum et al. (2012). The author here includes this unit in the Dundurrabin Granodiorite.|290.9 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|||||
34193|Ganmain Granodiorite""|22638|6|Mentioned|p52|||Superseded by Ganmain Granite||||||
34628|Gap Granodiorite|22815|6|Mentioned|p62|||Now obsolete. Replaced with Dramore Granodiorite||||||
73915|Gara Suite|71628|5|Briefly described|p3:40|||||Hillgrove Supersuite.|Gara Monzogranite.|||
27412|Garibaldi Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
27412|Garibaldi Adamellite|41348|5|Briefly described|Map legend|Early Paleozoic||Gabbro, diorite, granodiorite, adamellite.||||||07-NOV-08
27412|Garibaldi Adamellite|71628|5|Briefly described|p2:4; p3:43|||Binns et al. (1967).||Hillgrove Plutonic Suite.||||
74038|Garibaldi Suite|71628|5|Briefly described|p3:44|||||Hillgrove Supersuite.|Garibaldi Monzogranite.|||
25919|Garie Member|30006|6|Mentioned|p64|||||||||
25919|Garie Member|30007|6|Mentioned|p61|||||||||
25919|Garie Member|31297|6|Mentioned|p4|||See also P6||||||
25919|Garie Member|31613|6|Mentioned|p348|||||||||
25919|Garie Member|31878|3|Fully described|p823|||Refers previous literature. Mineralogy P824.||||||
25919|Garie Member|31880|6|Mentioned|p18|||||||||
25919|Garie Member|31884|6|Mentioned|Table 1|||Triassic||||||
25919|Garie Member|31886|6|Mentioned|p394|||||||||
25919|Garie Member|34303|2|Defined|p14|Triassic|Triassic|||||||
25919|Garie Member|36220|6|Mentioned|p65|||||||||
25919|Garie Member|45090|5|Briefly described|p200|||||||||
31584|Garland Suite|42726|5|Briefly described|map legend||Silurian|||||||
31584|Garland Suite|44093|5|Briefly described|p201  App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
28565|Garoo member|41238|6|Mentioned|Table 1|||||||||
31260|Garra Bed limestones|43512|14|Not recorded|p77|Middle Devonian|Early Devonian|||||||
31259|Garra Bed shales|43512|14|Not recorded|p77|Middle Devonian|Early Devonian|Green and buff shales and siltstones||||||
31173|Garra Group|43491|4|Described|pV/13|Middle Devonian|Early Devonian|||||||
77674|Garra Limestone Formation|68297|5|Briefly described|p190|Lochkovian|Lochkovian|Includes Lochkovian vertebrate fossil fauna. See also Garra Limestone p191||||||
37431|Garra Series|23214|6|Mentioned|p179|||Superseded by Garra Formation.||||||
77359|Garrambeel Sandstone Member|68005|5|Briefly described|p146.|Carboniferous|Carboniferous|||Unit in Caroda Formation.|||Sandstone, conglomerate.|
31975|Garrawilla Basalt|43881|14|Not recorded|p53|Jurassic|Triassic|Coonabarabran area.||||||
24998|Garrawilla Lava|29591|6|Mentioned|p75|||||||||
24998|Garrawilla Lava|29698|6|Mentioned|p64|||||||||
24998|Garrawilla Lava|30785|6|Mentioned|p399|||||||||
24998|Garrawilla Lava|34016|6|Mentioned|p537|||Early Mesozoic||||||
24998|Garrawilla Lava|34254|6|Mentioned|p488|||Late Triassic - Early Jurassic||||||
24998|Garrawilla Lava|34394|6|Mentioned|Fig.43|||Refers Dulhunty (1967).||||||
24998|Garrawilla Lava|36961|6|Mentioned|Table 1|||||||||
24998|Garrawilla Lava|38064|5|Briefly described|42|||||||||
24998|Garrawilla Lava|40245|6|Mentioned|p187|||Mention P198||||||
24998|Garrawilla Lava|64570|6|Mentioned|p861|||||||||
30812|Garrawilla Lavas|23053|6|Mentioned|p24|||(Dulhunty 1967).||||||
30812|Garrawilla Lavas|30610|6|Mentioned|p320|||Refers Kenny (1928,1963)||||||
30812|Garrawilla Lavas|43384|14|Not recorded|Map Legend||Jurassic|||||||
30812|Garrawilla Lavas|43394|14|Not recorded|p105-108|||||||||
30812|Garrawilla Lavas|43408|14|Not recorded|Map Legend|||Alkali olivine basalt in Curlewis area not now included in Jurassic Garrawilla Lavas||||||
30812|Garrawilla Lavas|43534|14|Not recorded|p393|||||||||
30812|Garrawilla Lavas|43535|14|Not recorded|p133-4,136-7|Early Jurassic|Late Triassic|Overlies Napperby Beds. Overlain by Purlawaugh Beds and Pilliga Sandstone. 181 m.y.(L.Tri.or E.Jur)||||||
30812|Garrawilla Lavas|43881|14|Not recorded|p80|Early Jurassic|Late Triassic|See also Lexicon. Ref. to David 1950||||||
31307|Garrawilla Series|43554|14|Not recorded|p29|||||||||
31307|Garrawilla Series|43555|14|Not recorded|p150|||||||||
31307|Garrawilla Series|43557|14|Not recorded|p88|||||||||
31150|Garwilla Volcanics|43161|6|Mentioned|23-26||Jurassic|||||||
35272|Gateshead Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
70666|Gatton Formation|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Late Triassic|Includes the Koreelah Conglomerate and Calamia Members. Max. thicknesss: 600m||||||
70666|Gatton Formation|73570|6|Mentioned|p912 Fig.2|||See also Gatton Sandstone.||||||
70351|Gatton Sandstone "Member"|60993|6|Mentioned|p18|||Informal version of Gatton Sandstone Member - now upgraded to formation status as Gatton Sandstone.||||||
80663|Geary's Gap Gravels|71408|5|Briefly described|p1029-p1030|Pliocene|Pliocene|Originally described by Taylor (1907) who concluded they were fluvial gravels. Up to 8m of gravel was reportedly intersected in abandoned gold mining shafts. Referred to as Geary's Gap gravels in text on pp1029, 1030. Macphail et al. (2015) reported an age of ca 4 Ma for similar, possibly correlative gravels occurring at a depth of 165 m below the current bed of Lake George.||||||31-OCT-18
39445|Gearys Gap formation|24128|5|Briefly described|p89|||Informal.  Geological Province: Lachlan Fold Belt.||||||
41329|Geehi Metamorphics|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Pre-Cratonic Province. Slate, sandstone, schist, granulite.||||||09-NOV-04
41329|Geehi Metamorphics|60085|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
31246|Geehi Schists|43491|14|Not recorded|pIII/14||Ordovician|Ref.to Ball, Dallwitz and Noakes 1948||||||
70144|Geneffe Shale""|43494|6|Mentioned|p22|||Of Maggs (1963).  Informal name.||||||
73963|Genoa River beds""|63605|5|Briefly described|p991, p1003|Late Devonian|Late Devonian|Of Clarke (1860). Informal name - see Genoa River beds.||||||07-FEB-11
38452|Gentle Annie porphyry|24133|6|Mentioned|p27|||Geological Province: Lachlan Fold Belt.||||||
31976|George's Knob Conglomerate Member|43881|2|Defined|p6-7,10,26-7||Triassic|Upper Member of Basin Creek Formtion.||||||
79900|Georges Bore Granite|63866|5|Briefly described|p38|Statherian|Statherian|[Replaces the Oakdale Granite Gneiss].|1695 +/-4 Ma|Silver City Suite||Intrudes the Thackaringa Group and/or the Broken Hill Group.||
79900|Georges Bore Granite|66302|6|Mentioned|p41|||Shown as Oakdale Granite Gneiss (Georges Bore Granite) dated at 1695+/- 4 Ma.||Silver City Suite||||07-JUL-17
82749|Georges Mountain Volcanics|71628|5|Briefly described|p8: 40|||[Appears to be shown as an alternative informal name of Muir (1990) for the Wandsworth Volcanic Group]||Wandsworth Volcanic Group.||May be intruded by The Basin Monzogranite (no contacts observed).||
78430|Gerra Clay|65194|6|Mentioned|p26|||aquiclude||||||
36359|Gerringong Volcanic Complex|23544|5|Briefly described|p358|||Informal variation on Gerringing Volcanics||||||
36359|Gerringong Volcanic Complex|73494|4|Described|p542-543, 554-555|Permian|Permian|Southern Sydney Basin. Late Permian. Comprises Gerringong Volcanics and three intercalated sandstone units. Extends offshore at least 200km to the NE. Lava flow thicknesses diminish to the west.|265.05 +/- 0.35 Ma (Belica et al., 2017).||Berkeley, Minnamurra, Calderwood, Five Islands, Cambewarra, Saddleback, Dapto, Bumbo, Blow Hole, Coolangatta, Latite Members; Koo-Lee Tuff Member; Jamberoo, Kiama, Westley Park Sandstones.||A collection of flows and sills; shoshonitic; K-rich; varies from basaltic andesite to basalt and andesite. Most units are porphyritic with a holocrystalline groundmass. Locally vesicular or amygdaloidal.|
70078|Gerringong volcanic facies|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Early Permian|Informal name. Formed by the five latite members of the Broughton Formation and 4 latite members of the Pheasants Nest Formation (Illawarra C.M.). Geological Province: Sydney Basin.||||||
70078|Gerringong volcanic facies|67500|5|Briefly described|p12, p12 Tb.1, p18,19|||||||Includes the four Latite Members of the Pheasants Nest Formation (of the Illawarra Coal Measures) and all of the Broughton Formation (of the Upper Shoalhaven Group).||01-MAY-12
78378|Getty gabbro|69002|6|Mentioned|p12, 14|||May be Neoproterozoic, if  ~580 and ~600 Ma zircons not inherited.||||||
78378|Getty gabbro|69541|5|Briefly described|p645 Fig.1(b)|Neoproterozoic|Neoproterozoic|Zircon peak age.|594 Ma.|||||
69996|Ghanghat Spilite|61766|5|Briefly described|p67|||Informal status (Mayer 1972). Included along with Bulliac beds and Belbora beds within an undifferentiated unit termed Bundook beds. Geological Province: Tamworth Belt.||||||27-JAN-06
23613|Giants Den Leucoadamellite|38842|6|Mentioned|p286|||||||||
40247|Giants Den group|38842|5|Briefly described|p286|Permian|Permian|Informal name. Geological Province: New England Fold Belt. Age: 270 +/- 10Ma||||||14-JAN-08
25003|Gibraltar Adamellite|42727|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Bega Batholith. Adamellite; I-type. Intrudes Birkenburn beds. BMR map symbol: Dgi. Geol. Prov: Rocky Pic Block.||||||
25003|Gibraltar Adamellite|42820|2|Defined|p72|Early Devonian||3 km East of Bungendore.||||||
25003|Gibraltar Adamellite|71700|5|Briefly described|CD|||||||This unit is (probably) equivalent to the Ellenden Granite.||
31908|Gibraltar Microsyenite|43870|14|Not recorded|p276,308||Early Jurassic|Intrudes Middle or Late Triassic. Based on age determinations.||||||
73665|Gidyen Volcanics|63278|6|Mentioned|p147 Fig. 2b|Late Ordovician|Middle Ordovician|Geological Province: Rockley Volcanic Belt, LFB.||||||07-FEB-11
73665|Gidyen Volcanics|63283|6|Mentioned|p195 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||07-FEB-11
73665|Gidyen Volcanics|63290|5|Briefly described|p396 Fig. 3|Darriwilian|Middle Ordovician|Overlain by Mozart Chert. Geological Province: Rockley - Gulgong Volcanic Belt.||||||
73665|Gidyen Volcanics|63293|6|Mentioned|p469 Fig. 2|Darriwilian|Darriwilian|Overlain by Mozart Chert. Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
73665|Gidyen Volcanics|67847|5|Briefly described|p28|Early Ordovician|Early Ordovician||||||Volcaniclastic and mafic volcanic sequence.|
73665|Gidyen Volcanics|68592|6|Mentioned|p371|||Rockley-Gulgong Volcanic Belt.||Unit in Cabonne Group.||||
73665|Gidyen Volcanics|70684|6|Mentioned|p75|Middle Ordovician|Middle Ordovician|Oberon district, Rockley-Gulgong Volcanic Belt.||||||
35071|Gilgai Complex|23053|6|Mentioned|p20|||||||||
73957|Gilgai Suite|71628|6|Mentioned|p19: 44||||||Gilgai Leucogranite.|||
82454|Gilgai Supersuite|71628|6|Mentioned|p19: 42|||||||||
25007|Gillan Creek Seam|34605|6|Mentioned|Fig.5.28|||||||||
31081|Gillan's Creek Sandstone|43477|14|Not recorded|p58||Late Permian|Unit of Wollondilly Coal Measures||||||
37377|Gilmore Andesite|24040|6|Mentioned|p473|||Also informally written as Gilmore andesite.||||||21-AUG-08
26573|Gilmore Hill Granite|22638|6|Mentioned|p75|||Superseded by Thurungly Granite||||||24-AUG-04
26573|Gilmore Hill Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
26573|Gilmore Hill Granite|60423|6|Mentioned|p379|||Of the Gilmore Hill Suite. Geological Province: Lachlan Fold Belt.||||||
82810|Gilmore Hill granite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. I/A-type.  Hf isotope data included.|375 Ma|||||
41612|Gilmore Volcanics""|44244|6|Mentioned|p87|||Superseded by Gilmore Volcanic Group.||||||
41710|Gilmore-Nerong volcanics|44244|6|Mentioned|p293|||Informal grouping of the rocks of the Gilmore Volcanic Group and the Nerong Volcanics.||||||
30921|Gilwhite Limestone Member|23185|6|Mentioned|p160|||||||||
30921|Gilwhite Limestone Member|43417|14|Not recorded|Map Legend|||Part of Lilberne Beds||||||
26574|Ginini Granite|42726|5|Briefly described|map legend|Silurian||286. Variation on Ginini Leucoadamellite.||||||
32260|Ginini Leuco-adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab3. Misspelling of Ginini Leucoadamellite.||||||
27157|Ginini Leucoadamellite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Gingera Batholith. Intrusive. Leucoadamellite, aplite. S-type. BMR map code: Sgg.||||||
27157|Ginini Leucoadamellite|39660|6|Mentioned|p449|||||||||
27157|Ginini Leucoadamellite|45147|2|Defined|M220|Late Silurian|Late Silurian|Prob.Late Silurian||||||
27157|Ginini Leucoadamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
74172|Ginnagulla Volcanics""|61769|5|Briefly described|p96 Fig. 2, p101-102||Tertiary|Informally named. Used to constrain the Kelvin Thrust. Consists of fresh and altered basalts, basaltic andesites, andesites, fine grained epiclastic breccia with interbedded coarse arenite containing Late Devonian brachiopods. See p101-102.||||||06-AUG-20
28244|Ginnini Leucoadamellite|36441|5|Briefly described|map legend|Pridolian|Pridolian|Of Gingera Batholith. Intrusive. S-type. Leucoadamellite, aplite. BMR map code: Sgg.||||||
25009|Giralambone Beds|30683|6|Mentioned|Table 1|||Misspelling of Girilambone?||||||
25009|Giralambone Beds|43389|14|Not recorded|Map Legend|||||||||
82456|Girard Creek Suite|71628|6|Mentioned|p19:52||||||Girard Creek Diorite.|||
25010|Girilambone beds|22671|6|Mentioned|p833|||||||||17-JAN-06
25010|Girilambone beds|24267|5|Briefly described|p1515|Early Ordovician|Early Ordovician|Geological Province: Parkes-Narromine Belt||||||
25010|Girilambone beds|32954|6|Mentioned|p172|||||||||
25010|Girilambone beds|36534|6|Mentioned|p222|||||||||
25010|Girilambone beds|42614|6|Mentioned|p8|||||||||
25010|Girilambone beds|43213|5|Briefly described|p63|||Written as Girilambone beds (or Group). Originally defined by Brunker (1969). Has undergone at least three episodes of cleavage-forming deformation.|||||A sequence of flysch-like sediments, thinly-bedded chert, quartzite, magnetite quartzite and greenstones (dismembered ophiolite, including serpentinite).|
25010|Girilambone beds|45147|6|Mentioned|M8|||||||||
33966|Girilambone beds""|22555|5|Briefly described|p371|||||||||
81843|Girrabool Beds|70125|5|Briefly described|p398 Fig.12|||[Mis-spelling of Girrakool beds]. The main component of the Tablelands Complex, Southern New England Orogen. Zircon age probability density plot.|||||Turbidites.|
25011|Girrakool Beds|35264|2|Defined|p13|Permian|Permian|||||||
25011|Girrakool Beds|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition of modified name.||||||
25011|Girrakool Beds|36948|6|Mentioned|p51|||||||||
25011|Girrakool Beds|36961|6|Mentioned|Fig.5|||||||||
25011|Girrakool Beds|39214|4|Described|p39|||Formerly Lyndhurst Beds. See P40||||||
25011|Girrakool Beds|39627|6|Mentioned|p268|||||||||
25011|Girrakool Beds|39747|6|Mentioned|p195|||||||||
25011|Girrakool Beds|61797|6|Mentioned|p394 Fig. 1(b)|Carboniferous|Carboniferous|||||||
25011|Girrakool Beds|61805|6|Mentioned|p437, p439 Fig. 2|||Informal, see Girrakool beds. Geological Province: New England Orogen. ||||||
25011|Girrakool Beds|71280|4|Described|p401-406, p410-414|Carboniferous|Carboniferous|Korsch (1978); originally the Lyndhurst Beds of Binns (1966). Tablelands Complex, southern New England Orogen. The major unit in, and likely protolith to, the Wongwibinda Metamorphic Complex. Shows gradational increase in metamorphic grade from west to east. Contains the Permian biostratigraphic marker, the lamellibranch Myonia. Dips steeply to the NW. Zircon dating detailed.|309 +/- 4 Ma (maximum depositional age).|Coffs Harbour Association, Wongwibinda Metamorphic Complex.||Is intruded by Hillgrove Plutonic Suite.|A thick, monotonous sequence of medium- to fine-grained turbidites (psammites and pelites) with minor chert lenses, and rare basalt and calcareous nodules.|10-JAN-19
25011|Girrakool Beds|71703|4|Described|p191-192, 196, 197, 198, 202, 203-205||Late Carboniferous|[Misspelling of Girrakool beds] Dated by detrital zircons p192. Includes deep marine turbidites.|Maximum deposition age of 309 +/- 5 Ma.|||Intruded by S-type plutons of the Hillgrove Supersuite, and pegmatites.|Medium grained turbidites, with intercalated lenses and layers of calcsilicate. Migmatites present as high grade metamorphic rocks.|16-MAY-19
73669|Gleesons Member|63278|5|Briefly described|p154|||Of the Fossil Hill Limestone. Is the basal unit of Fossil Hill Limestone, and is mostly mudstones. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
73687|Glen Ayr syenite|63283|6|Mentioned|p191 Tb. 2|Late Ordovician|Middle Ordovician|Informal name. Age: 445Ma. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73710|Glen Ayre Syenite|63286|6|Mentioned|p300, p304|Late Ordovician|Middle Ordovician|Age: 441+/-10Ma (U-Pb SHRIMP: Pogson and Watkins 1998).||||||07-FEB-11
83495|Glen Creek Sandstone|73264|6|Mentioned|p1394 Fig.16|Early Devonian|Early Devonian|||||||
83495|Glen Creek Sandstone|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
82751|Glen Eden Suite|71628|6|Mentioned|p15: 29|||||Stanthorpe Supersuite.||||
38330|Glen Eden granite""|23812|6|Mentioned|p121|||Formal name not intended.||||||
76041|Glen Emu Granite Suite|66934|6|Mentioned|Map legend|Devonian|Silurian|Informal name. Based on TMI anomaly.|||Includes Rata granite.|||04-OCT-13
26576|Glen Esk Adamellite|38916|6|Mentioned|p348|||Misspelling of Glenesk?||||||
26576|Glen Esk Adamellite|41347|6|Mentioned|p376|||||||||
26576|Glen Esk Adamellite|41348|5|Briefly described|Map legend|Early Paleozoic||Adamellite, leucoadamellite.  Granitoid of the Gundle Belt.||||||07-NOV-08
26576|Glen Esk Adamellite|44450|5|Briefly described|p105 Fig 30|||Geological Province: New England Fold Belt.||||||
26576|Glen Esk Adamellite|69188|5|Briefly described|p1-2, p4, p12-16, p79|Late Triassic|Late Triassic|One of the "coastal granitoids" east of the central axis granites of the New England batholith. Informally named the Gundle Tin Granitoids. Deeply weathered and poorly exposed.|221.2 +/- 1.5 Ma (magmatic age)||||Coarse-grained monzogranite and porphyritic monzogranite, granodiorite with microgranular enclaves with quenched and scalloped margins. I-type.|16-APR-20
26576|Glen Esk Adamellite|69323|6|Mentioned|p71|Triassic|Triassic|Geological province: New England Orogen.|221.2+\-1.5 Ma (SHRIMP)|||||
25012|Glen Esk Granite|40762|6|Mentioned|p297|||Misspelling of Glenesk?||||||
25012|Glen Esk Granite|71628|6|Mentioned|p17: 57, 88|||Gilligan and Brownlow (1981). Initially Glen Esk Adamellite (Leitch et al., 1982); now Glen Esk Monzogranite.||||||
33679|Glen Fergus Member|22624|6|Mentioned|p678|||||||||
33679|Glen Fergus Member|22815|4|Described|p23, fig10|Early Ordovician|Early Ordovician|||||||
33679|Glen Fergus Member|22857|4|Described|p422 App. 1, Tb. A1.5|Early Ordovician|Early Ordovician|Of the Chakola Formation. Mudstone/slates interbedded with arenites. Max. thickness: 100m. ||||||
33679|Glen Fergus Member|22878|6|Mentioned|p34|||||||||
33679|Glen Fergus Member|24037|5|Briefly described|p424|||Of Adaminaby Group. Geological Province: Lachlan Fold Belt||||||
33679|Glen Fergus Member|43233|6|Mentioned|Map Legend||Darriwilian|Of Chakola Formation.||||||
33679|Glen Fergus Member|67322|5|Briefly described|p15; Fig.5|Sandbian|Sandbian|Approximately 50-100m thick (Glen 1994; Glen and Lewis 1994). Age is determined from Fig.5 (Strat. column). Occurs in the Cooma-Monaro region.||Of the Chakola Formation|||Very thinly bedded mudstones and slates interbedded with thin sandstones containing broad, low amplitude cross laminations. Sandstones within this sequence contain large quartzite lenses. Micaceous and feldspathic sandstones are also conspicuous.|19-OCT-22
33679|Glen Fergus Member|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|||Chakola Formation.||||
33679|Glen Fergus Member|68592|6|Mentioned|p272|||||Unit in Chakola Formation.||||
33679|Glen Fergus Member|71069|6|Mentioned|p78, p79, p84|||||Chakola Formation||Equivalent to the Bumballa Formation. Conformably overlain by the Warbisco Shale.||
33679|Glen Fergus Member|73140|6|Mentioned|p495 Fig.6|||Proposed to be superseded and replaced by Bumballa Formation [misspelt as Bumbulla] in the Bendoc Group.||||||19-OCT-22
77250|Glen Gallic Sub-group|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Topmost unit in Wollombi Coal Measures.|Includes Dights Creek Coal, Redmanvale Creek Formation and Greigs Creek Coal.|Overlies Doyles Creek Sub-group. Is overlain by Narrabeen Group.||
41349|Glen Garry Microleuco granite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Leucogranite, microleucogranite.||||||
38275|Glen Garry Microleucogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Fine- to medium-grained leucogranite and microleucogranite.  An I-type granitoid.||||||20-DEC-04
38275|Glen Garry Microleucogranite|23812|5|Briefly described|p20 Tb.2|Early Triassic|Late Permian|||||||
38275|Glen Garry Microleucogranite|71628|6|Mentioned|p14:3|||Willis (1987). Now Glen Garry Microleucosyenogranite.||||||
74018|Glen Garry Suite|71628|5|Briefly described|p14:4|||||Kingsgate Supersuite.|Glen Garry Microleucosyenogranite.|||
40558|Glen Idle Andesite Tuff|24605|6|Mentioned|p949 App.1|||Superseded by Glen Idle Rhyolite.||||||
37305|Glen Idle Rhyolite|24010|6|Mentioned|p381|||||||||
37305|Glen Idle Rhyolite|24605|2|Defined|p949 App.1|Namurian|Namurian|Of the Clifden Formation. Thickness at type section: 7m. Geological Province: New England Orogen. Referred throughout text as Glen Idle Rhyolite Member.||||||
37305|Glen Idle Rhyolite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of Clifden Formation.||||||30-JUN-05
37457|Glen Logan Formation|23214|5|Briefly described|p279|Pliocene||Underlying unit: Lachlan Formation.||||||
37165|Glen Ward Beds|23522|5|Briefly described|p249 Fig. 5|Middle Devonian|Pragian|||||||
37165|Glen Ward Beds|44447|5|Briefly described|p131-132, p133 Fig.2, p135|Early Devonian|Early Devonian|Overlie Pitch Creek Volcanics. c.5000m thick, comprising conglomeratic sandstones, limestones, turbidite sequence and basaltic extrusives.||||||
37165|Glen Ward Beds|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Pigna. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
30999|Glen William Beds|43451|14|Not recorded|Map Legend||Carboniferous|See also Lexicon. Included with Wooton Beds||||||
30920|Glenalvon Formation|43417|14|Not recorded|Map Legend||Triassic|||||||
78376|Glenariff granite|69002|5|Briefly described|p12|Pridoli|Ludfordian||422 +/- 2.4 Ma, U-Pb SHRIMP||||S-type granite.|
78376|Glenariff granite|69043|5|Briefly described|p3, p91|Silurian|Silurian|Thomson Orogen. This age is indistinguishable from the Brewarrina granite (420.9 +/- 2.3 Ma). Other granitic units' ages given for comparison.|422.7 +/- 2.4 Ma (Black, 2007).||||I-type.|19-JAN-17
26578|Glenbog Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Glenbog Granodiorite.||||||
82752|Glenbrae Monzogranite Phase|71628|5|Briefly described|p15: 35, 82, 100-104, 115|||This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Geochemistry briefly described.||Severn River Monzogranite.||||
83048|Glenburnie Leuco-adamellite|73202|6|Mentioned|p637|Cisuralian|Cisuralian|Anaiwan terrane (also spelt Anawian), western. I-type plutonism.|ca 295 Ma|||||
27418|Glenburnie Leucoadamellite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|One of the "leucoadamellites" of the region.  A granitoid of fine to coarse-grained, porphyritic to equigranular biotite-(hornblende)  monzogranite.||||||20-JAN-05
27418|Glenburnie Leucoadamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
27418|Glenburnie Leucoadamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
27418|Glenburnie Leucoadamellite|43091|5|Briefly described|Map legend|||Granitoids||||||
27418|Glenburnie Leucoadamellite|69323|6|Mentioned|p35|||Geological province: New England Orogen. Superseded, see Glenburnie Leuzomonzogranite.||||||
27418|Glenburnie Leucoadamellite|71628|6|Mentioned|p19:54|||Binns et al. (1967), after work by Flood. Now Glenburnie Leucomonzogranite.||||||
27418|Glenburnie Leucoadamellite|72313|6|Mentioned|p459 Table 2|||New England Orogen. I-type.  Hf isotope data included.|295 Ma|||||
74019|Glenburnie Suite|71628|6|Mentioned|p19:55||||||Glenburnie Leucomonzogranite.|||
82812|Glencair Adamellite|72313|6|Mentioned|p459 Table 2|||New England Orogen. S-type.  Hf isotope data included.|288 Ma|||||
35361|Glencairn Limestone|23185|6|Mentioned|Fig1p156,162||Lochkovian|||||||
35361|Glencairn Limestone|23522|5|Briefly described|p249 Fig 5|Pragian|Lochkovian|||||||
35361|Glencairn Limestone|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Tamworth. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
41060|Glenclair Monzogranite|24366|5|Briefly described|p12 Fig. 10|Early Permian|Early Permian|Of the Bundarra Plutonic Suite.||||||
41060|Glenclair Monzogranite|68005|5|Briefly described|p62, p136.|Early Permian|Late Carboniferous|Boundaries have been refined using radiometric imagery.||Unit in Glenclair Suite.|||Porphyritic biotite granite.|
41060|Glenclair Monzogranite|71628|6|Mentioned|p4:28|||Brown (2003). Named after a local homestead. Now the Glenclair Syenogranite.||||||
39936|Glendale Monzodiorite|24268|5|Briefly described|p1537 Fig.3|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt||||||
28577|Glendale Monzonite|24268|5|Briefly described|p1541|Late Ordovician|Late Ordovician|Age: ~440Ma. Geological Province: Lachlan Fold Belt||||||
28577|Glendale Monzonite|42802|5|Briefly described|p100|||Reserved as Glendale by J.Pemberton.||||||
30987|Glendon Limestone Member|43447|14|Not recorded|p20|||Maitland Group. Part of Mulbring Siltstone||||||
70079|Glenelg Metamorphics""|22857|5|Briefly described|p94|||Informal - see Glenelg River Complex. Of VandenBurg (1978).||||||
39415|Gleniffer Adamellite|24127|5|Briefly described|p4|Permian|Permian|||||||
39415|Gleniffer Adamellite|71628|6|Mentioned|p3:46|||Originally Glenifer Adamellite of Leitch et al. (1971). Spelling corrected to Gleniffer Adamellite (after the locality) in Milford (1996); changed again to Gleniffer Monzogranite in Chisholm et al. (2014).||||||
82753|Gleniffer Suite|71628|5|Briefly described|p3:47|||||Hillgrove Supersuite.|Gleniffer Monzogranite.|||
38199|Glenn Gallic Subgroup|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures.   Geological Province: Sydney Basin||||||
73883|Glenncairn Limestone|50095|6|Mentioned|p123, p134 Tb.4|||Contains Pedavis pesavis and Kimognathus alexeii(conodont).||||||14-JAN-08
35161|Glenrock Lagoon Formation|23055|6|Mentioned|Fig13p25|||||||||
34003|Glenrock leucogabbro|22571|6|Mentioned|Table2,p17|Devonian|Silurian|New England Orogen. Gamilaroi terrane||||||
34002|Glenrock tonalite|22571|6|Mentioned|p18||Silurian|New England Orogen. Also p16.||||||
35407|Glenroe Granite|23043|6|Mentioned|Map Diagram|Emsian|Lochkovian|Misspelt. Should be Glenrowe Granite as referred to in Legend.||||||
42111|Glenroy Granite|60548|5|Briefly described|map legend|Devonian|Devonian|Granite.||||||
38926|Glenroy Granite""|24417|5|Briefly described|p100|||Duggan et al (1999) used the name to describe Milroy Granite, however, the name was already reserved.||||||
38309|Glenview seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Probably misspelt - see Glenview Seam.   Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
38309|Glenview seam|44244|6|Mentioned|p327|||Within the Stroud-Gloucester Syncline.||||||
41613|Gloucester Rhyolites""|44244|6|Mentioned|p164|||Term used by Sussmilch (1922) for volcanics in the northern part of the Stroud-Gloucester Syncline - never formalised.  Suoperseded by Alum Mountain Volcanics.||||||
41613|Gloucester Rhyolites""|50099|6|Mentioned|p13|||Informal name of Sussmilch (1922)). Of the Alum Mountain Volcanics.||||||
31228|Gloucester Volcanics|43479|14|Not recorded|p162||Carboniferous|||||||
69977|Gloucester suite|61794|6|Mentioned|p360|||Informal name.||||||
37386|Gloucester volcanics|24040|6|Mentioned|p468 Fig. 1|||Informal name. Geological Province: Manning Basin||||||
30764|Gnalta Beds|22580|5|Briefly described|p87|Cambrian|Cambrian|||||||
30764|Gnalta Beds|43344|14|Not recorded|p2,3,||Cambrian|Gnalta||||||
30764|Gnalta Beds|43384|14|Not recorded|Map Legend||Cambrian|||||||
31175|Gnalta formation|43491|14|Not recorded|pV/16||Devonian|||||||
73402|Gnaltaknoka Member|66623|6|Mentioned|p183 Fig.41.|||Mis-spelling of Gnaltaknoko.||||||
73402|Gnaltaknoka Member|70651|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Daubeny Formation|||Conglomerate with horizons of andesitic volcanic beds and, near the base, rafts and boulders of bedded pale red quartz sandstone, minor siltstone and pale brown quartzite.|
31274|Gobondry Granite|43500|14|Not recorded|Map Legend|||(Provisional Edition) (not on card)||||||
31274|Gobondry Granite|70684|6|Mentioned|p54 Fig.27|||||||||
31274|Gobondry Granite|72495|6|Mentioned|p218,233|||||||Faulted against the Raggatt Volcanics.||
31583|Gocup Suite|42726|5|Briefly described|map legend||Silurian|||||||
31583|Gocup Suite|44093|5|Briefly described|p183 App. 1|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||08-APR-05
79105|Goiters Tank metamudstone|69635|5|Briefly described|p84-87|||Informal name for part of Ballast Formation. North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age.|507+/-13 Ma||||Weathered quartz-mica metamudstone sampled.|15-JUL-15
79202|Goker Volcaniclastics|68592|5|Briefly described|p754, p885|||Of Whalan (1986). An unnamed lithological subdivision in Cobra Formation (a porphyritic, flow-banded rhyolite body) was mapped by Whalan (1986) as a dacitic 'plug' with breccia at the margins, and was presented as a possible source for the younger Kowmung Formation (his Goker Volcaniclastics).||||||
73508|Golden Lava|63283|5|Briefly described|p191 Tb. 2, p194 Fig. 2|Early Ordovician|Early Ordovician|Of the Cowal Igneous Complex. Age: 475Ma (trachyte lava and trachyte dyke). Geological Province: Junee-Narromine Volcanic Belt. Consists of trachyte lava and dykes.||||||07-FEB-11
73508|Golden Lava|63284|5|Briefly described|p247, p256|||Informal name. Named from Cowal mine, found at E42. Consists of trachyandesites-trachytes.||||||
35224|Golden Lava Unit|22797|6|Mentioned|Fig3, P839|||Informal name of Miles (1993).||||||
35224|Golden Lava Unit|63293|6|Mentioned|p468 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Great Flood Unit, underlain by Cowal Conglomerate Unit. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35224|Golden Lava Unit|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
35224|Golden Lava Unit|70684|5|Briefly described|p74|Early Ordovician|Early Ordovician|Junee-Narromine Volcanic Belt||Cowal Igneous Complex.||||
38956|Golden Lava unit""|24417|6|Mentioned|p182|||Informal name referring to unit hosting the Endevour 42 gold deposit.||||||
25019|Gongolgin Granite|34449|6|Mentioned|Table 2-1|||||||||
34182|Goobarragandra porphyry""|22638|6|Mentioned|p32|||Superseded by Goobarragandra Volcanics||||||24-AUG-04
41337|Gooborragandra Porphyry|60086|5|Briefly described|Map legend|||Quartz, feldspar porphyry and basic lavas, wacke, siltstone, quartzite, breccia.||||||
25020|Goodradigbee Group|39800|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
25020|Goodradigbee Group|68592|6|Mentioned|p980|||Of Joplin et al. (1953), referring to limestone in the Goodradigbee River valley N and S of Wee Jasper. Called Goodradigbee Limestone by Best et al. (1964). The rocks were divided into 3 units by Brown (1964); these were shown (by Young,1969 and Pedder et al., 1970) to be equivalent to the 3 stages of the Murrumbidgee Series of Browne (1959), and have thus fallen into disuse.||||||
28218|Goodradigbee Limestone|12185|5|Briefly described|map legend|Devonian|Devonian|Limestone, shale. BMR map symbol: Dmg.||||||
28218|Goodradigbee Limestone|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
28218|Goodradigbee Limestone|32483|6|Mentioned|p31|||Refers Best et al. (1964). Now Murrumbidgee Gp.||||||
28218|Goodradigbee Limestone|68592|6|Mentioned|p980|||Of Best et al. (1964); formerly Goodradigbee Group of Joplin et al. (1953), referring to limestones in the Goodradigbee River valley N and S of Wee Jasper. Brown (1964) divided the sequence into 3 units; these were later shown (by Young, 1969 and Pedder et al., 1970) to be equivalent to the 3 stages of the Murrumbidgee Series of Browne (1959), and have thus fallen into disuse.||||||
79203|Goodradigbee Limestone, Lower|68592|6|Mentioned|p980|||Of Brown (1964), who divided the sequence of limestones in the Goodradigbee River valley into 3 units. These were shown to be equivalent to the three subdivisions of the Murrumbidgee Series of Browne (1959), and have fallen into disuse.||||||
79204|Goodradigbee Limestone, Upper|68592|6|Mentioned|p980|||Of Brown (1964), who divided the sequence of limestones in the Goodradigbee River valley into 3 units. These were shown to be equivalent to the three subdivisions of the Murrumbidgee Series of Browne (1959), and have fallen into disuse.||||||
39397|Googoodery rhyolite|24126|6|Mentioned|p141|||Informal name.||||||
31977|Goolang Siltstone|43881|14|Not recorded|p133||Triassic|See Goolang Siltstone Member. Member of Bardool Conglomerate.||||||
73707|Gooleys Basalt|63286|5|Briefly described|p295, 298, p304|Llandovery|Llandovery|Coarsely phorphyritic basaltic intrusions, also have lower clinopyroxene and higher plagioclase phenocrysts abundances.||||||04-NOV-14
36200|Gooloogong Beds""|23392|6|Mentioned|p13|||Of Colwell (1974) BSc Hons. Superseded by Gooloogong Member.||||||
36200|Gooloogong Beds""|24417|6|Mentioned|p126|||Superseded by Gooloogong Member of the Hunter Formation.||||||
40221|Goonbri formation|24313|6|Mentioned|p22|Early Permian|Early Permian|||||||30-NOV-04
70485|Goonoo Formation|62095|6|Mentioned|Plate 1|Carboniferous|Carboniferous|Probably misspelt - see Goonoo Goonoo Formation. Geological Province: Werrie block/Tamworth Belt.||||||20-APR-08
70485|Goonoo Formation|70777|6|Mentioned|p8|Carboniferous|Carboniferous|Werrie Block, New England Orogen.||||||
28582|Goonoo Goonoo conglomerate|41238|6|Mentioned|p88|||||||||
40940|Goonooglah Monzodiorite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith.  Probably misspelt?  See also Goonoonglah Monzodiorite.||||||13-MAY-04
78680|Goonoogoonoo Mudstone|50168|6|Mentioned|p158 Fig.3|||Gamilaroi Terrane. Presented as Goonoogoonoo Mdst.||||||
69892|Goonoonglah Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Goonoonglah Monzodiorite.||||||24-JUN-08
69892|Goonoonglah Suite|68592|2|Defined|p1482-9, p1491-1507|Early Devonian|Early Devonian|New name, after Blevin (2011); after Goonoonglah Creek. Consists of one [!] unit, the Goonoonglah Monzodiorite. Geochemistry described in considerable detail. The minor gabbro and dolerite have very similar geochemical characteristics to Box Ridge Volcanics.|413 +/- 5 Ma (SHRIMP U-Pb zircon: Wilde, 2001).|Unit in Keverstone Supersuite.|Includes Goonoonglah Monzodiorite.|Is intruded by Bigga and Yewrangara Granites.|A-type. Grey to dark-grey, medium-grained, massive, often porphyritic, quartz syenite, quartz monzonite and quartz monzodiorite; minor quartz diorite; black, massive gabbro. Some phases intrude others. All phases fractionated from a common magma.|
69892|Goonoonglah Suite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Goonoonglah Monzodiorite.|||
69892|Goonoonglah Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Goonoonglah Monzodiorite|||
39950|Goonumbla Complex|24267|6|Mentioned|p1507, p1508 Fig.1|||Not intended as a formal name. Geological Province: Parkes-Narromine Belt||||||
39950|Goonumbla Complex|24593|5|Briefly described|p629|Late Ordovician|Late Ordovician|Shoshonitic unit.  Age: 439Ma.  Geological Province: Lachlan Orogen.||||||
39265|Goonumbla Volcanic Complex|24230|5|Briefly described|p171|||Unit referred to as GVC throughout text.||||||
39265|Goonumbla Volcanic Complex|24263|5|Briefly described|p1387|Late Ordovician|Late Ordovician|Age: ~440Ma. Geological Province: Parkes-Narromine Belt||||||
39265|Goonumbla Volcanic Complex|24265|5|Briefly described|p1444|Early Silurian|Late Ordovician|Geological Province: Lachlan Fold Belt||||||
39265|Goonumbla Volcanic Complex|24267|4|Described|p1506, p1509 Fig.2||Late Ordovician|Contains the Wombin, Goonumbla and Nelungaloo Volcanics. Geological Province: Parkes-Narromine Belt||||||
39265|Goonumbla Volcanic Complex|62478|5|Briefly described|p88-89|Early Silurian|Early Ordovician|||||||
39265|Goonumbla Volcanic Complex|67107|5|Briefly described|p693, 701|Late Ordovician|Late Ordovician|Located c.20km NW of Parkes. Hosts the porphyry-style Cu-Au mineralisation in the area, which occurred between 444.2 +/- 4.7 Ma and 436.7 +/- 3.3 Ma (intrusions).||||Intrudes Goonumbla and Wombin Volcanics.||
39265|Goonumbla Volcanic Complex|67805|5|Briefly described|p73|Ordovician|Ordovician|||||||
39265|Goonumbla Volcanic Complex|67821|6|Mentioned|p150, p170|Ordovician||Hosts the Northparkes Cu-Au porphyry system.|||Nelungaloo Volcanics.|||08-FEB-18
39265|Goonumbla Volcanic Complex|70278|6|Mentioned|p1607, 1609, 1612, 1618, 1627|Ordovician|Ordovician|Junee-Narromine volcanic belt, Central-west NSW. Hosts the Endeavour Cu-Au porphyry deposits.|||Nelungaloo, Goonumbla, Wombin Volcanics.|||
39265|Goonumbla Volcanic Complex|73287|5|Briefly described|p660-661, p662 Tb.3, p665 Fig.2|||Macquarie Arc, Junee-Narromine Belt. Hosts the Northparkes porphyry deposits and the Two-Thirty Prospect. Location in text includes p667 Fig.4.|||Nelungaloo Volcanics, Goonumbla Volcanics, Wombin Volcanics.||Includes pebbly volcanic sandstone, trachyte lava, latite lava, poorly fossiliferous limestone, volcanic siltstone and conglomerate, monzonite, aplite (micro-syenite?).|
72280|Goonumbla Volcanic Complex Intrusives|62478|4|Described|p89|Early Silurian|Ordovician|Of the Goonumbla Volcanic Complex. Various Monzodiorite to monzonitic intrusions. Intrudes Neelungaloo, Goonumbla and Wombin Volcanics. Ages: 482, 450 and 440Ma||||||
33690|Goonumbla Volcanic Group|22434|5|Briefly described|12||Ordovician|See also Goonumbla Volcanics p11 fig 15||||||
35237|Goonumbla porphyry|22797|6|Mentioned|P846|||||||||
28583|Goonumbla volcanic complex|22659|4|Described|p 280|Late Ordovician|Late Ordovician|||||||
28583|Goonumbla volcanic complex|39663|6|Mentioned|Table 4|||||||||
39951|Goonumbla volcanics|24267|6|Mentioned|p1515|||Not intended as a formal name. Geological Province: Parkes-Narromine Belt||||||
81805|Goonumbla volcanics, lower|72495|6|Mentioned|p227|||||||||
81806|Goonumbla volcanics, upper|72495|6|Mentioned|p227|||||||||
23632|Gordies Spur Gabbro|45147|6|Mentioned|M48|||||||||
26590|Gosford Sub-Group|24079|5|Briefly described|p433 Fig. 6|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
26590|Gosford Sub-Group|24083|5|Briefly described|p457|||Of the Narrabeen Group.   Geological Province: Sydney Basin.||||||
26590|Gosford Sub-Group|29361|6|Mentioned|p3|||On table.||||||
26590|Gosford Sub-Group|29901|4|Described|Table 1|||||||||
26590|Gosford Sub-Group|30007|6|Mentioned|p61|||||||||
26590|Gosford Sub-Group|30132|6|Mentioned|Table 1|||||||||
26590|Gosford Sub-Group|31297|6|Mentioned|p4|||See also Fig. 3||||||
26590|Gosford Sub-Group|32719|6|Mentioned|p209|||Section||||||
26590|Gosford Sub-Group|33685|6|Mentioned|p394|||||||||
26590|Gosford Sub-Group|33867|4|Described|p6|||See also P3.||||||
26590|Gosford Sub-Group|35062|6|Mentioned|p279|||||||||
26590|Gosford Sub-Group|35416|6|Mentioned|Fig.2|||Stratigraphy and palynological framework shown||||||
26590|Gosford Sub-Group|36042|6|Mentioned|Table 1|||||||||
26590|Gosford Sub-Group|36220|4|Described|p71|||See also Table 20.||||||
26590|Gosford Sub-Group|36221|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
26590|Gosford Sub-Group|36222|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
26590|Gosford Sub-Group|36223|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic.||||||
26590|Gosford Sub-Group|39287|6|Mentioned|Fig. 2.5|||||||||
26590|Gosford Sub-Group|39294|6|Mentioned|p163|||||||||
26590|Gosford Sub-Group|39308|5|Briefly described|p454|||||||||
26590|Gosford Sub-Group|60281|5|Briefly described|Fig. 15 Appendix 1|||Superseded by Gosford Subgroup.  Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
31176|Gosford beds|43491|14|Not recorded|page not known||Triassic|Correlated with upper Narrabeen Group||||||
33219|Gosford formation|44546|14|Not recorded|p26|||||||||
30730|Gosford sandstone|43358|14|Not recorded|p51,58,59||Triassic|(Hawkesbury Sandstone)||||||
31039|Gosforth shale member|43474|14|Not recorded|p7||Sakmarian|of Lochinvar Fm||||||
82754|Gosling Swamp Leucomonzogranite Phase|71628|4|Described|p12:11; p15: 34-35, 52, 60-61, 63-67,77|||See also p15: 82, 91, 115. New unit, after a local creek; differentiated geochemically. This subunit does not ""technically"" qualify as a Phase according to stratigraphic naming conventions. Previously part of Stanthorpe Monzogranite. Location of various outcrops given; occurs c.15 x 13 km. Geochemistry and mineralogy described in some detail. Is geochemically assigned to the Gosling Swamp Suite. Is spatially associated with Mo-dominant and Sn mineralisation (occurrences listed). RELATED UNITS (continued): Also abuts Sailor Jack Supersuite,  Mount Norman Leucomonzogranite, Ruby Creek Leucogranite.|248.7 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Mount Lindesay Monzogranite.||Likely intrudes Wallangarra Volcanics and Dundee Rhyodacite. Abuts Bungulla, Severn River, The Ram Swamp, ?Boonoo Monzogranite and ?Jenners Monzogranites. See COMMENTS for more.|Pale pink to pale brown, buff, pale greyish-brown, or reddish brown, uneven grained to moderately porphyritic, leucocratic biotite monzogranite. I-type.|
82755|Gosling Swamp Suite|71628|5|Briefly described|p15: 35, 65|||The Gosling Swamp Monzogranite Phase (of Mount Lindesay Monzogranite) is geochemically assigned to this Suite.||Stanthorpe Supersuite.||||
73717|Gospal Oak Shale|63287|5|Briefly described|p317 Fig. 2|Wenlock|Wenlock|Of the Cudal Group. Overlain by Canowindra Volcanics, underlain by Liscombe Pools Limestone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29568|Gospel Oak Formation|63288|6|Mentioned|p359|||Overlain by Avoca Valley Shale.||||||
29568|Gospel Oak Formation|63290|6|Mentioned|p395|Wenlock|Llandovery|Contains abundant quartz detritus.||||||
73916|Gostwyck Suite|71628|5|Briefly described|p3:49|||||Hillgrove Supersuite.|Gostwyck Monzogranite.|||
25024|Gourock Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Gourock Granodiorite.||||||
25024|Gourock Granite|42820|5|Briefly described|p72|||||||||
23634|Governors Chair Volcanics|39969|6|Mentioned|p9|||||||||
23634|Governors Chair Volcanics|40542|6|Mentioned|p98|||||||||
23634|Governors Chair Volcanics|40587|6|Mentioned|p361|||||||||
23634|Governors Chair Volcanics|42485|5|Briefly described|p264|||||||||
23634|Governors Chair Volcanics|69599|5|Briefly described|p630 Fig.8.31, p639|||Main Range volcano. Total alkalis v. SiO2 plot and discussion. Abbreviated to Governors Chair in Fig.8.31. Several ages for the collective Main Range lavas given.|Between ~26 Ma and ~20 Ma.||||Mildly alkaline basalt, through hawaiite, mugearite, benmoreite, metaluminous trachyte and peralkaline trachyte, to peralkaline rhyolite; mafic lavas low in the succession and silicic lavas above (typical fractional crystallisation).|
23634|Governors Chair Volcanics|73450|5|Briefly described|p90, p92-93|||Of Ewart and Grenfell (1985). Southern Main Range [possibly a constituent of the Main Range Volcanics]. The authors (Purdy and Bultitude, 2022) indicate the name is not in current use nor is it formally defined [?].|||Wild Cattle, Steamers, Swanfels, Guymer and Spicers Gap Trachyte Members|Equivalent to Meringandan Volcanics. Conformably overlain by Superbus Basalt.|Includes mildly alkaline basalt through to peralkaline rhyolite.|
23634|Governors Chair Volcanics|73581|5|Briefly described|p7|||Southern part of the Main Range Volcano. Bimodal in character. Separated from Superbus Basalt by the Streamers Trachyte and Wild Cattle Trachyandesite, the boundary is considered indistinguishable where the felsic units are absent.||||Underlies Superbus Basalt|Contains basal alkaline basalt lavas, overlain by trachyandesite, benmoreite and peralkaline rhyolite lavas.|
73105|Gowan Brae monzogranite""|62757|6|Mentioned|p13 Fig. 5|||Granitoid of the Moonbi Supersuite. Informal - see Gowan Brae monzogranite.||||||07-FEB-11
31917|Grafton Beds|43881|14|Not recorded|p45|Cretaceous|Late Jurassic|Now known as Grafton Formation. See also Lexicon.||||||
31946|Grafton Stage|43881|14|Not recorded|p45|Cretaceous|Late Jurassic|Name replaced by Grafton Formation||||||
41614|Grahamstown Lake Formation""|44244|6|Mentioned|p102|||Junior synonym of Seaham Formation.||||||
82468|Graman Suite|71628|5|Briefly described|p4: 34|||||Bundarra Supersuite.|Graman Monzogranite.|||
37421|Grants Corner Tonalite|23214|6|Mentioned|p158|||Replaced by Grants Corner Granodiorite.||||||
31223|Graptolite Bed|43857|6|Mentioned|p324|||||||||
35626|Grasmere beds|63793|5|Briefly described|p61.|||||Unit in Ponto Group.|||Metasedimentary phyllite, chloritic schist, interlayered tuff, quartz-magnetite rock, magnetite, altered basalt.|
35626|Grasmere beds|64169|5|Briefly described|p19, p20 Fig. 9|||Uppermost unit of Palgamurtie Subgroup (Ponto Group). Overlie Weinteriga beds. In Koonenberry  Belt. Incl: Grasmere sulphide lodes and gossan, minor altered mafic rocks, cherty tuff horizons and quartz-magnetite rocks.||||||20-MAY-08
35626|Grasmere beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group).  Magnetic and non-magnetic phyllite containing altered chloritic and epidote-rich mafic rocks, minor porphyritic basalt, thin cherty tuffs, thin quartz-magnetite rocks, and the Grasmere sulphide lodes.||||||26-NOV-08
35626|Grasmere beds|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Underlain by Weinteriga Creek beds. Magnetic and non-magnetic phyllite containing altered chloritic and epidote-rich mafic rocks, minor porphyritic basalt, thin cherty tuffs, thin quartz-magnetite rocks.||||||01-DEC-08
35626|Grasmere beds|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Magnetic part of Ponto beds consisting of magnetic and non-magnetic phyllite containing altered chloritic and epidote-rich mafic rocks, minor porphyritic basalt, thin cherty tuffs, thin quartz-magnetite rocks.||||||08-DEC-08
35626|Grasmere beds|66623|6|Mentioned|p85. |||Portion of former Wonnaminta beds (Warris 1967). Redefined (this study) as Grasmere Formation to include the Bendee beds (Stevens et al. 2000).||Unit in Palgamurtie Subgroup.||||
35626|Grasmere beds|66929|5|Briefly described|Map legend|||||Unit in Palgamurtie Subgroup.||Overlies Weinteriga Creek beds.|Magnetic and non-magnetic phyllite containing altered chloritic and epidote-rich mafic rocks; minor porphyritic basalt, thin cherty tuffs, thin quartz-magnetite rocks, and sulphide lodes.|
32262|Grass Flat Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab7.||||||
32262|Grass Flat Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
80728|Grasstree Suite (NSW)|71628|5|Briefly described|p19: 73, 96|||[Invalid. This name exists for a unit in the Charters Towers Province (QLD).]|||Malara Quartz Monzodiorite.|||
72758|Great Cbar Slate|61905|5|Briefly described|p135 Fig. 1|||Misspelt - should be Cobar. Geological Province: Cobar Basin.||||||
32605|Great Cobar Slate formation|46032|14|Not recorded|p.412||Silurian|||||||
35223|Great Flood Unit|22797|6|Mentioned|Fig3, P839|||Informal unit of Miles (1993).||||||
35223|Great Flood Unit|63283|6|Mentioned|p194 Fig. 2|Early Ordovician|Early Ordovician|Of the Cowal Igneous Complex. Geological Province: Junee-Narromine Volcanic Belt.||||||07-FEB-11
35223|Great Flood Unit|63293|6|Mentioned|p468 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Cowal Igneous Complex, underlain by Golden Lava Unit. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35223|Great Flood Unit|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
35223|Great Flood Unit|70684|6|Mentioned|p74|Early Ordovician|Early Ordovician|Junee-Narromine Volcanic Belt||Cowal Igneous Complex.||||
38955|Great Flood unit""|24417|6|Mentioned|p182|||Informal name referring to unit hosting the Endeavour 42 gold deposit.||||||
70076|Great Northern coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Moon Island Beach Formation (Newcastle Coal Measures)||||||
70076|Great Northern coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Moon Island Beach Formation||||
27788|Great Northern seam|23717|5|Briefly described|p117 Tb. 1|Permian|Permian|||||||
27788|Great Northern seam|24157|4|Described|p188 Tb.1|Permian|Permian|Of the Moon Island Beach Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||14-MAR-07
27788|Great Northern seam|24479|5|Briefly described|p41|||Of Newcastle Coal Measures. Equivalent to parts of the Wollombi Coal Measures.||||||
27788|Great Northern seam|36330|6|Mentioned|p94|||||||||
27788|Great Northern seam|36545|6|Mentioned|p10|||||||||
27788|Great Northern seam|37083|3|Fully described|p167|||||||||
27788|Great Northern seam|39576|6|Mentioned|p14|||||||||
27788|Great Northern seam|39609|6|Mentioned|p1|||||||||
27788|Great Northern seam|39666|6|Mentioned|p89|||||||||
27788|Great Northern seam|40166|6|Mentioned|p352|||||||||
27788|Great Northern seam|40697|6|Mentioned|p22|||||||||
27788|Great Northern seam|41463|6|Mentioned|p38|||||||||
27788|Great Northern seam|62033|5|Briefly described|p24, p25 (Table)|||Of Moon Island Beach Formation (Newcastle Coal Measures). Overlies the Awaba Tuff (Newcastle Coal Measures). Geological Province: Sydney Basin.||||||14-MAR-07
27788|Great Northern seam|67786|5|Briefly described|p94-96, 99, 102, 105, 108|Permian|Permian|Catherine Hill Bay, Sydney Basin. Late Permian. A major economic coal seam. Lithologic column sections. Proximate analysis, maceral analysis, mineralogy, major element tables.||Moon Island Beach Subgroup.||Overlies Awaba Tuff. Is overlain by Teralba Conglomerate.|Coal seams; relatively rich in inertinite; high volatile A bituminous in rank; low ash yields; low in total sulfur. Claystone bands. Interbedded with alluvial channel deposits.|
31945|Green Scrub Flow|43880|14|Not recorded|p58-60||Tertiary|||||||
73719|Greenslope Granite|63289|5|Briefly described|p368 Fig. 5c, p371|Silurian|Silurian|Age: 425+/-11Ma (microprobe monzanite U-Th-Pb: Meffre 2003). Silurian granite.||||||07-FEB-11
68125|Grega Group|44093|5|Briefly described|p201 App. 1|Early Devonian|Silurian| Geological Province: Lachlan Fold Belt.||||||
68125|Grega Group|64826|5|Briefly described|p1040 Tb. 1|Early Gedinnian|Early Gedinnian|||||||
68125|Grega Group|70297|4|Described|map legend|Emsian|Lochkovian|Indexing error: appears correctly as Gregra Group on the map legend. Largely deposited in shallow water. Final fill of the Cowra Trough.|||Bulls Camp Volcanics, Cuga Burga Volcanics, Berkley Formation, Garra Formation, Maradana Shale|Conformably overlies Goonigal Group.|Fossiliferous limestone, calcareous sandstone and shale, siltstone and breccia; latitic to rhyolitic and andesitic volcanic and volcaniclastic rocks; laminated shale, siltstone, fine-grained feldspathic sandstone.|18-MAY-16
34653|Greig Creek Conglomerate""|22815|6|Mentioned|p102|||Renamed Curmulee Conglomerate.||||||
72982|Greig's Creek seam|62033|6|Mentioned|p24|||In Hunter Valley Coalfield. Included within Wollombi Coal Measures before replacement of this nomenclature with Newcastle Coal Measures. Unclear if this name has been retained?||||||14-MAR-07
31471|Grenfell Suite|22768|6|Mentioned|p178|||||||||
31471|Grenfell Suite|22857|5|Briefly described|p178|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. ||||||
31471|Grenfell Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Grenfell Granite - formal name not intended.||||||08-FEB-05
31471|Grenfell Suite|44093|5|Briefly described|p181 App. 1|Early Devonian|Late Silurian| Geological Province: Lachlan Fold Belt.||||||
39374|Grenfell granite|24125|5|Briefly described|p3|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
41615|Greta Coal Measures, lower|44244|6|Mentioned|p292|||||||||
31077|Greta Conglomerate|43477|14|Not recorded|p32-36|||Part of Greta Coal Measures||||||
70077|Greta coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Early Permian|Informal reference to a seam within the Greta Coal Measures.||||||
31079|Greta formation|43477|4|Described|p39|||Greta Coal Measures. Includes Greta Conglomerate||||||
25031|Grey Mare Granite|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
25031|Grey Mare Granite|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
25031|Grey Mare Granite|40328|4|Described|p206|||||||||
25031|Grey Mare Granite|42726|5|Briefly described|map legend|Silurian||||||||
25031|Grey Mare Granite|60085|5|Briefly described|Map legend|Silurian|Silurian|||||||
83665|Griffith analcimite|73581|6|Mentioned|p26 Fig.7|||Distinguished from the Cargelligo Volcanic Province by its well constrained age and composition.||||||
78340|Griman Creek Formation, Lower|68734|5|Briefly described|p218 Fig.2|Albian|Albian|Surat Basin. Paralic. The rank of Member, though implied in Fig.2, is omitted.||Of the Griman Creek Formation.||||16-JAN-17
31630|Grong Grong Suite|42726|5|Briefly described|map legend||Silurian|||||||
31630|Grong Grong Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone.  Geological Province: Lachlan Fold Belt.||||||
31630|Grong Grong Suite|69801|6|Mentioned|p32|||Central Lachlan Orogen. Previously a suite of Chappell et al (1991) before being replaced by the Koetong Suite of Chappell et al  (1999).||Koetong Supersuite||||
30872|Grose Formation|43395|14|Not recorded|p73|||=Grose Sandstone||||||
25719|Grose Sandstone|24117|5|Briefly described|p100|||Of Narrabeen Group. Geological Basin: Sydney Basin.||||||
25719|Grose Sandstone|24123|5|Briefly described|p3|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
25719|Grose Sandstone|29749|6|Mentioned|p11|||||||||
25719|Grose Sandstone|31297|6|Mentioned|p6|||||||||
25719|Grose Sandstone|31373|6|Mentioned|Table 1|||||||||
25719|Grose Sandstone|31426|5|Briefly described|Fig.1|||||||||
25719|Grose Sandstone|31740|6|Mentioned|p13|||||||||
25719|Grose Sandstone|31884|6|Mentioned|Table 1|||Triassic||||||
25719|Grose Sandstone|33682|6|Mentioned|p22|||||||||
25719|Grose Sandstone|33683|4|Described|Table 1|||Narrabeen Gp.||||||
25719|Grose Sandstone|33685|6|Mentioned|Table 2|||||||||
25719|Grose Sandstone|34107|5|Briefly described|p217|||?equivalent Collaroy Claystone & Tuggerah Formation||||||
25719|Grose Sandstone|34121|4|Described|p398|||Type section described.||||||
25719|Grose Sandstone|34205|1|Redefined|p24|Triassic|Triassic|3 members.||||||
25719|Grose Sandstone|34209|6|Mentioned|Table 1|||See also PP137,140 etc. Triassic.||||||
25719|Grose Sandstone|34236|6|Mentioned|p17|||||||||
25719|Grose Sandstone|34240|4|Described|p395|||Triassic||||||
25719|Grose Sandstone|34241|6|Mentioned|p404|||||||||
25719|Grose Sandstone|34336|6|Mentioned|Table 5.15|||||||||
25719|Grose Sandstone|34884|6|Mentioned|p57|||||||||
25719|Grose Sandstone|34944|6|Mentioned|p361|||||||||
25719|Grose Sandstone|36058|6|Mentioned|p4|||||||||
25719|Grose Sandstone|37093|5|Briefly described|p231|||||||||
25719|Grose Sandstone|37492|6|Mentioned|Fig.2|||||||||
25719|Grose Sandstone|43146|6|Mentioned|Fig.2 p41|||of Narrabeen Group.||||||
25719|Grose Sandstone|43317|4|Described|Table 1 p11|||||||||
25719|Grose Sandstone|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
25719|Grose Sandstone|43320|14|Not recorded|Table 1 p11,16,19,20||Triassic|Part of Narrabeen Group||||||
25719|Grose Sandstone|43344|14|Not recorded|p21,53,77|Early Triassic||Unit of Narrabeen Group||||||
25719|Grose Sandstone|43352|14|Not recorded|p 209-223||Triassic|||||||
25719|Grose Sandstone|43359|14|Not recorded|Map Legend||Triassic|Provisional first edition||||||
25719|Grose Sandstone|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Narrabeen Group||||||
25719|Grose Sandstone|43361|14|Not recorded|Map Legend||Triassic|(Provisional first edition) Part of Narrabeen Formation||||||
25719|Grose Sandstone|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Narrabeen Group||||||
25719|Grose Sandstone|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
25719|Grose Sandstone|43383|14|Not recorded|p22|||||||||
25719|Grose Sandstone|43385|14|Not recorded|p182, Table||Early Triassic|||||||
25719|Grose Sandstone|43395|2|Defined|p61,62,64,65-67,||Early Triassic|69-74,76-79||||||
25719|Grose Sandstone|45090|6|Mentioned|p202|||Refers Goldbery (1966)||||||
25719|Grose Sandstone|68004|6|Mentioned|p137, p210.|||At Lithgow, high quality kaolin occurs as clay cement within this friable sandstone.||||||
35483|Grosses Plains Tonalite|22719|6|Mentioned|p485|||||||||
76054|Gubberamunda Siltstone|65119|6|Mentioned|p512 Fig.6|||See Gubberamunda Sandstone p504 etc.||||||07-MAR-12
72977|Gubberamundra Sandstone|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Late Jurassic|Quartz sandstone, minor siltstone and mudstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
40263|Gulf Siltstone-Argillite|38915|6|Mentioned|p338|||Geological Province: New England Fold Belt||||||
82479|Gulf Station Suite|71628|6|Mentioned|p19:74||||||Gulf Station Leucosyenogranite.|||
34347|Gulgamree beds|22728|5|Briefly described|p599 table1||Devonian|||||||
35421|Gulgamree beds""|23170|6|Mentioned|p44|||Superseded by Coomber Formation.||||||
39396|Gulgomree Beds|24126|6|Mentioned|p138|||||||||
32526|Gulgong Plutonic Suite|23043|5|Briefly described|Map Legend|Late Carboniferous|Tournaisian|||||||
32526|Gulgong Plutonic Suite|23170|4|Described|p268|Carboniferous|Carboniferous|of Lachlan Fold Belt.||||||
32526|Gulgong Plutonic Suite|60267|5|Briefly described|p14|Carboniferous|Carboniferous|Geological Province: Lachlan Fold Belt.||||||
32526|Gulgong Plutonic Suite|66191|6|Mentioned|p484 Fig.1|||Gunnedah Basin||||||
32526|Gulgong Plutonic Suite|68003|5|Briefly described|p17, p24 Fig.3-e, pp140-141.|Visean|Famennian|Lachlan Fold Belt. Post-tectonic granites.|||Includes Old Leake, Leadville, Ulan, Quartz Monzonites; Gulgong Granite; and Worobil and Goat Mountain Alkali Granites.||Granite, quartz monzonite, aplite, quartz-feldspar porphyritic rhyolite.|
32526|Gulgong Plutonic Suite|70036|5|Briefly described|Map legend|Carboniferous|Carboniferous|Lachlan Fold Belt. Included in a mapped unit of Carboniferous intrusive rocks: quartz monzonite and granodiorite.||||||
35074|Gulgong deep leads""|23043|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
35074|Gulgong deep leads""|23170|4|Described|p348|Miocene|Miocene|||||||
39390|Gulgong granite|24126|6|Mentioned|p4|||Informal - see Gulgong Granite.||||||
39390|Gulgong granite|67669|6|Mentioned|p14|||Of Bowen Basin. Density range 2.51-2.62 t/m3; mean 2.59 t/m3.||||||
83081|Gulgong granites|73299|6|Mentioned|p1094 Fig.2, p1107|Carboniferous|Carboniferous|U-Pb zircon ages of 358 +/- 5 Ma, 314 +/- 8 Ma, 325 +/- 5 Ma, 323 +/- 7 Ma (Meakin and Morgan, 1999) and 328 +/- 4 Ma (Jeon and Williams, 2018). See also Gulgong Granite.|358 +/- 5 Ma, 314 +/- 8 Ma U-Pb zircon||||Granite.|
28590|Gulgong gravels|32047|6|Mentioned|p11|||||||||
35631|Gum Creek Basalt|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of Noonthorangee Subgroup (Ponto Group). Pale to dark green-grey, foliated, dominantly fine-grained tholeiitic metabasalts, feldspar phyric metabasalts, vesicular metabasalts; some pillow textures. Flows, sills and plugs. Weakly magnetic.||||||26-NOV-08
35631|Gum Creek Basalt|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Noothorangee Subgroup. Pale to dark green-grey, foliated, dominantly fine-grained tholeiitic metabasalts, feldspar phyric metabasalts, vesicular metabasalts; some pillow textures. Flows, sills and plugs.||||||
35631|Gum Creek Basalt|66623|6|Mentioned|p89, 95.|||The parent (Noonthorangee Subgroup) is redefined and renamed Noonthorangee Formation in this study,  but the extrusive and intrusive parts have been included in the Bittles Tank Volcanics.||Unit in Noonthorangee Subgroup.||||27-SEP-13
35631|Gum Creek Basalt|66929|5|Briefly described|Map legend|||Weakly magnetic.||Unit in Noonthorangee Subgroup.|||Pale to dark green-grey, foliated, dominantly fine-grained tholeiitic metabasalts, feldspar phyric metabasalts, vesicular metabasalts; some pillow textures. Flows, sills and plugs..|31-JAN-12
35631|Gum Creek Basalt|67322|6|Mentioned|p39|Cambrian|Cambrian|Part of the Noonthorangee Subgroup (obsolete) in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map (Stevens et al. 2002) - now included in the Noonthorangee Formation (Greenfield et al. 2010). Age is assumed to be similar to the parent Noonthorangee Formation. Occurs in the Kayrunnera-Koonenberry region.||||||
78268|Gum Creek Beds|67562|5|Briefly described|p107 Fig.12, p109, p113|Fammenian|Fammenian|Small subhorizontal deposit a few tens of metres thick.||||Unconformably underlain by the Menamurtee Sandstone.|Comprises medium-grained sandstone.|23-JAN-17
38165|Gum Creek beds|24345|5|Briefly described|p85|Givetian|Givetian|Overlies Menamurtee Sandstone.  Geological Province: Moona Vale Trough.||||||
38165|Gum Creek beds|66623|6|Mentioned|p222.|||Named by Neef and Larsen (2003). Subsequently redefined (this study) as a basal member in Ravendale Formation.||||||28-JUL-13
70597|Gum Vale Formation|61823|5|Briefly described|p118, p121|Albian|Neocomian|Part of a marine transgressive sequence.  Geological Province: Eromanga Basin.||||||
70597|Gum Vale Formation|66623|6|Mentioned|p247.|||Name changed to Gum Vale beds. Partly equivalent to Namur Sandstone.|||Included Warratta Sandstone Member.|||
70597|Gum Vale Formation|69001|6|Mentioned|p16|||Locally defined by McMinn (1981b) and/or Morton (1982) as a mixture of the Algebuckina Sandstone and Cadna-owie Formation. Previously incorrectly correlated with the Eyre Formation.||||||
31477|Gumble Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Gumble Granite (informal name).||||||08-FEB-05
31477|Gumble Suite|44093|5|Briefly described|p194 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
73892|Gummi Plain Suite|71628|5|Briefly described|p6:19|||||Barrington Tops Supersuite.|Gummi Plain Granodiorite.|||
82382|Gumtree Monzogranite|71628|5|Briefly described|p2: 46-49, 54, 56-57|||Named here, incorporating the unpublished Gumtree Adamellite and Chaelundi Adamellite of Paul (1984). Comprises two intrusions. Geochemistry briefly described. Highly felsic. Geochemically and temporally distinct from the Chaelundi Complex to the NW.||Sheep Station Creek Complex.||Intrudes Brooklana beds, Collett Monzogranite.|Creamy-grey, equigranular, medium-grained biotite monzogranite.|
30823|Gumvale Beds|43383|14|Not recorded|p25,26|Early Cretaceous|Jurassic|||||||
30823|Gumvale Beds|43390|14|Not recorded|p15,16||Jurassic|||||||
70486|Gun Barrel Tuff Member|62095|6|Mentioned|p274 Appdx.|||Of Cherry (1987). Synonymous with Ignimbrite Z of McPhie (1983). Remains an unnamed ignimbrite in this study.||||||31-JAN-08
70486|Gun Barrel Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
70486|Gun Barrel Tuff Member|68005|6|Mentioned|p140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
28591|Gundangaree Formation|33334|6|Mentioned|Table 3|||Perm.||||||
28591|Gundangaree Formation|42657|5|Briefly described|p77|||||||||
25035|Gundangaroo Seam|42182|6|Mentioned|p300|||||||||
77264|Gundangaroo seam""|68004|5|Briefly described|p220.|||Intersected by one NSW Department of Mineral Resources drillhole in 1993: raw ash content of <10%. If the seam is found to have sufficient extent, it could be sold on the export thermal market.||||||
76022|Gundara Quartzite|66918|5|Briefly described|Map legend|||Formal name is Gundara Quartzite Member.||Unit in Rowena Formation.|||Buff to white, planar and cross-bedded quartzite, includes angular quartz-vein conglomerate, distinctive quartz pebble bands and trace fossils.|
76022|Gundara Quartzite|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||[Member of?] Rowena Formation|||Buff to white, planar- and cross-bedded quartzite, includes angular quartz-vein conglomerate, distinctive quartz pebble bands and trace fossils.|
31755|Gundary Formation|22857|6|Mentioned|ERRATA sheet for p179, p480|Early Silurian|Early Silurian|Age is Wenlockian based on K/Ar dating.||||||
31755|Gundary Formation|43834|3|Fully described|p26||Wenlock|Formerly Gundary beds. Informally subdivided.||||||
31755|Gundary Formation|50234|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Mount Fairy Group. Overlies: Boxers Creek Formation.||||||25-FEB-08
31755|Gundary Formation|61762|6|Mentioned|p19 Fig. 2(a)||Early Silurian|||||||
31755|Gundary Formation|67820|6|Mentioned|p136 Fig.3|Devonian|Silurian|||Mount Fairy Group.||||
31755|Gundary Formation|68592|6|Mentioned|p835, p851, p869, p1060, p1162|||Of Jones et al. (1995). Here renamed Gundary Volcanics to reflect the large volume of primary volcanic rocks and was redefined due to the recognition of a regional depositional break and accompanying conglomerate unit (Bullamalita Conglomerate, Bindook Group). It is equivalent to the lower part of the Gundary Formation of Jones et al. (1995). See also Gundary Beds.||||||
31758|Gundary beds|22768|6|Mentioned|p179|||||||||
31758|Gundary beds|22857|4|Described|p179, p480 App.1 Tb.A1.6|Early Devonian|Early Devonian|Superseded by Gundary Formation - see ERRATA insert. Geological Province: Captains Flat-Goulburn Trough.||||||
31758|Gundary beds|43834|6|Mentioned|p26|||Superseded by Gundary Formation.||||||
31758|Gundary beds|44093|5|Briefly described|p218 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
70073|Gundary beds""|22857|6|Mentioned|p179, p480|||Superseded by Gundary Formation - see ERRATA insert.||||||
31579|Gundibindya Suite|42726|5|Briefly described|map legend||Silurian|||||||
31579|Gundibindya Suite|44093|5|Briefly described|p182 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
81828|Gundle Tin Granitoids|69188|5|Briefly described|p12|||An informal name for Glen Esk Adamellite. It occurs in the text also as the more obviously informal Gundle tin granitoids (p12) and "Gundle tin granites" (p12, p22, p27, p32).|||||Monzogranite.|
38331|Gundle granitoid|23812|6|Mentioned|p17 Fig.5|||Informal name.||||||
70074|Gundle granitoids|22857|6|Mentioned|p204 Fig. 17.2, p285|Late Triassic|Late Devonian|Informal name for rocks within the New England Batholith. See also p243 Fig. 18.4.||||||
25938|Gungarlin Adamellite|22815|4|Described|p44|Silurian|Silurian|||||||
25938|Gungarlin Adamellite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25938|Gungarlin Adamellite|35109|2|Defined|p64|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25938|Gungarlin Adamellite|35263|6|Mentioned|Table.3|||||||||
25938|Gungarlin Adamellite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
25938|Gungarlin Adamellite|40328|4|Described|p207|||||||||
25938|Gungarlin Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
25938|Gungarlin Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab8.||||||
25938|Gungarlin Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
77360|Gunnan Ignimbrite|68005|5|Briefly described|p137.|Stephanian|Namurian|||Unit in Willuri Formation.|||Brown-grey, coarse, crystal-rich, slightly welded to unwelded, rhyolitic ignimbrite.|
73664|Gunnars Dam Beds|63283|6|Mentioned|p194 Fig. 2|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt. Consists of shale and siltstone.||||||07-FEB-11
73664|Gunnars Dam Beds|63290|6|Mentioned|p397 Fig. 3(b)|Gisbornian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||
73664|Gunnars Dam Beds|63293|6|Mentioned|p468 Fig. 2|Gisbornian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73664|Gunnars Dam Beds|70684|6|Mentioned|p74|||||||||
73575|Gunnars Dam beds|63278|6|Mentioned|p153, p146 Fig2a|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt. Consists of shales, siltstone, with graptolites.||||||07-FEB-11
73575|Gunnars Dam beds|63288|6|Mentioned|p361|||Geological Province: Molong Volcanic Belt.||||||
73575|Gunnars Dam beds|67322|5|Briefly described|Fig.5; p25|Late Ordovician|Late Ordovician|Informally named by Percival and Glen (2007); reinterpreted as allochthonous blocks of spiculitic and graptolitic siltstone emplaced within the Lower Silurian Kabadah Formation.||||Emplaced within the Kabadah Formation.|Spiculitic and graptolitic siltstone.|22-FEB-18
73575|Gunnars Dam beds|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
26598|Gunnary Granite|42726|5|Briefly described|map legend|Silurian||||||||
26598|Gunnary Granite|68592|6|Mentioned|p1260|||Chappell et al. (1991). Renamed Licking Gully Granite. The parent Wyangala Suite has been renamed Hovells Suite, incorporating several new units on geochemical grounds.||||||
30914|Gunnedah Lavas|43408|14|Not recorded|Map Legend|||Werrie Basalts not now 'regarded as part of the 'Gunnedah Lavas'".||||||
25037|Gunnee Beds""|36570|6|Mentioned|p15|||||||||
80249|Gunners Dam Formation|67847|5|Briefly described|p32-p33|||Reference to  an informal redefinition of the inferred late Ordovician part of the Kabadah Formation. (Percival and Glenn, 2007)||||||06-OCT-17
30912|Gunnible Beds|43409|14|Not recorded|Map Legend|||Vickery Beds are equiv.? Correct name for unit is Gunnible Formation (q.v.)||||||
39013|Gunningbland Shale Member""|24417|5|Briefly described|p19|||Raised to formation status - see Gunningbland Formation.||||||
26599|Gunnungrah Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Gunningrah Tonalite.||||||
82486|Gunny Bag Suite|71628|6|Mentioned|p17:98||||||Gunny Bag Granite.|||
79205|Gurnang Granite|68592|6|Mentioned|p1771|||Of Sylvester (1966); named after a state forest 12 km W of the pluton. Later (Scheibner, 1973) renamed Abercorn Granite after the local Parish.||||||
82488|Guy Fawkes Suite|71628|5|Briefly described|p17:28|||||Carrai Supersuite.|Guy Fawkes Granodiorite.|||
38466|Guys Forest granodiorite|24133|6|Mentioned|p93|||Informal - see Guys Forest Granodiorite.  Geological Province: Lachlan Fold Belt.||||||
28270|Gwydir River Adamellite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Coarse, porphyritic monzogranite to granodiorite.||||||21-DEC-04
28270|Gwydir River Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
28270|Gwydir River Adamellite|30787|6|Mentioned|p49|||Differentiation index||||||
28270|Gwydir River Adamellite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
28270|Gwydir River Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28270|Gwydir River Adamellite|35257|6|Mentioned|Fig.15|||||||||
28270|Gwydir River Adamellite|38288|6|Mentioned|p76|||||||||
28270|Gwydir River Adamellite|41603|6|Mentioned|p18|||||||||
28270|Gwydir River Adamellite|42378|6|Mentioned|Table 1 P9|||||||||
28270|Gwydir River Adamellite|43091|5|Briefly described|Map legend|||||||||
28270|Gwydir River Adamellite|69323|5|Briefly described|p6,41,71|Lopingian|Lopingian|Geological province: New England Orogen.|252.3+\-1.5 Ma (SHRIMP; Cross and Blevin, 2010)|Unit of Uralla Supersuite.||Truncates Regional Felsic Dyke Swarm and Yarrowyck Granodiorite.||
28270|Gwydir River Adamellite|70217|6|Mentioned|p43|||New England Orogen. Obsolete name, now referred to as the Gwydir River Monzogranite. ||||||
28270|Gwydir River Adamellite|71628|6|Mentioned|p8:27|||Name updated to Gwydir River Monzogranite by Brown (2003) after unpublished work by Chappell and Bryant (1994).||||||
80400|Gyaran Volcanics|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
37389|Gyarran Basalt|24040|6|Mentioned|p468 Fig. 1|||Geological Province: Sydney Basin||||||
37394|Haematitic Limestone Member""|23214|5|Briefly described|p106|Llandovery|Llandovery|Informal name. Local horizon of Bagdad Formation overlying Bridge Creek Limestone Member.||||||24-AUG-12
23641|Half Moon Peak Adamellite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Gingera Batholith. Intrusive. Adamellite, granodiorite, aplite. S-type. BMR map code: Sgh.||||||
23641|Half Moon Peak Adamellite|39660|6|Mentioned|p449|||||||||
23641|Half Moon Peak Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab5.||||||
23641|Half Moon Peak Adamellite|45147|2|Defined|M218|Late Silurian|Late Silurian|Probably Late Silurian.||||||
23641|Half Moon Peak Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
76845|Half-Tide Volcanic Member|66855|6|Mentioned|p955.|||Of Scott (1982), now included in Chillingham Volcanics.||||||11-MAY-12
31321|Hall's Creek Limestone|43538|14|Not recorded|p2,6,15,27,36||Visean|||||||
83047|Halls Creek Volcanics|73202|6|Mentioned|p637|Sakmarian|Asselian|I-type. The 295.7 +/- 2.2 Ma zircon age is from a recalculation by McKibbin et al., (2017) [Misspelling of Halls Peak Volcanics?]|295.7 +/- 2.2 Ma U-Pb zircon|||||
38200|Hambledon Hill Sand Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Pinegrove Formation.   Geological Province: Sydney Basin||||||
77265|Hambledon Hill Sandstone Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield. The rank 'Member' is missing in table 5.||Top unit in Pinegrove Formation.||Overlies Wylies Flat Coal Member. Is overlain by Waterfall Gully Formation.||
40951|Hanaminno Limestone|50231|5|Briefly described|Map Legend|Silurian|Silurian|||||||
40951|Hanaminno Limestone|64238|5|Briefly described|Map legend|Silurian|Silurian|Cream to white massive, fossiliferous, recrystallised limestone.||||||
40951|Hanaminno Limestone|68592|3|Fully described|p408-26, p1866-7|Llandovery|Llandovery|New name, after Hanaminno homestead. Single outcrop (and thus type locality) 15m long, 11km NE of Boorowa (location specified). Fossils described. Conodont alteration from contact metamorphism (350-550 degrees C) by Licking Gully Granite. May have overlain Eurimbla Formation.||||All contacts concealed. Same age as Liscombe Pools Limestone and Jerrara Formation.|Cream to white, massive, fossiliferous, recrystallised limestone; finer structures of the fossils have been destroyed.|23-SEP-16
40951|Hanaminno Limestone|70192|5|Briefly described|Map Legend|Llandovery|Llandovery|Sxh. Ungrouped Silurian formation. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||||Cream to white, massive, fossiliferous recrystallised limestone.|
40951|Hanaminno Limestone|70545|5|Briefly described|Map Legend|Silurian|Silurian||||||Cream to white, massive, fossiliferous recrystallised limestone.|
40951|Hanaminno Limestone|71656|5|Briefly described|p21|Wenlock|Wenlock|Unit of limited extent in the Boorowa 1:100k mapsheet area. Name recommended to be abandoned. Unit originally thought to be late Llandovery on the basis of a single conodont element. Identification has been revised and now considered Wenlock, removing the need to distinguish this limestone from the rest of the Hawkins Volcanics.||||||
32650|Hanging Wall Basin Gneiss|46595|14|Not recorded|p.288,292,304-318|||On many pages. 1750 m.y. Age determinations.||||||
31828|Hanging Wall Gneiss|23461|6|Mentioned|p202|||||||||
31828|Hanging Wall Gneiss|45003|14|Not recorded|p327|||||||||
31828|Hanging Wall Gneiss|46601|14|Not recorded|p.320,323|||Fig.7.||||||
83622|Hangingwall Gneiss|73575|6|Mentioned|p826|||Of Webster (2006), shown with the Footwall Gneiss in this study as a single unit (Rasp Ridge Granite Gneiss).||||||
25941|Happy Jacks Adamellite|22815|4|Described|p44|Silurian|Silurian|Originally named Happy Jacks Granite.||||||
25941|Happy Jacks Adamellite|35109|2|Defined|p66|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25941|Happy Jacks Adamellite|35263|6|Mentioned|Table 3|||||||||
25941|Happy Jacks Adamellite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
25941|Happy Jacks Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
25941|Happy Jacks Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab23.||||||
25941|Happy Jacks Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
25941|Happy Jacks Adamellite|63289|6|Mentioned|p366|Late Silurian|Late Silurian|Geological Province: Kiandra Volcanic Belt.||||||07-FEB-11
27427|Happy Jacks Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
27427|Happy Jacks Granite|34404|6|Mentioned|p92|||||||||
27427|Happy Jacks Granite|42726|5|Briefly described|map legend|Silurian||358.  Of the Bullenbalong Suite (Bullenbalong Supersuite).  Formal name not intended.||||||08-FEB-05
27427|Happy Jacks Granite|43344|14|Not recorded|p124|||||||||
27427|Happy Jacks Granite|45087|5|Briefly described|p42|||Chemical analyses||||||
27427|Happy Jacks Granite|45147|6|Mentioned|M5|||See also M226||||||
27427|Happy Jacks Granite|46574|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kosciusko Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
27427|Happy Jacks Granite|60007|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Kosciusko  Batholith.  Biotite granite and leucocratic granite.||||||
27427|Happy Jacks Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
82494|Harnham Grove Porphyrite|71628|6|Mentioned|p8: 65, 67|||Binns et al. (1967). Included in Terrible Vale Porphyritic Microtonalite of Flood (1971 unpublished). Later referred to as Harnham Grove Porphyritic Microtonalite by Chesnut et al. (1973) and others.||||||
82493|Harnham Grove Porphyritic Microgranodiorite|71628|6|Mentioned|p3: 4|||Tentatively included in the Hillgrove Supersuite by Landenberger et al. (2010).||||||
28176|Harnham Grove Porphyritic Microtonalite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Massive, coarse-grained granodiorite, pyrozene monzogranite, diorite and microtonalite.||||||21-DEC-04
28176|Harnham Grove Porphyritic Microtonalite|24366|6|Mentioned|p18 Fig. 11|||||||||
28176|Harnham Grove Porphyritic Microtonalite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
28176|Harnham Grove Porphyritic Microtonalite|30787|6|Mentioned|p46|||||||||
28176|Harnham Grove Porphyritic Microtonalite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28176|Harnham Grove Porphyritic Microtonalite|43091|5|Briefly described|Map legend|||||||||
28176|Harnham Grove Porphyritic Microtonalite|71628|6|Mentioned|p8:64|||Chesnut et al. (1973). Originally Harnham Grove Porphyrite (Binns et al., 1967), then included in Terrible Vale Porphyritic Microtonalite (Flood, 1971 unpublished), and later named Harnham Grove Porphyritic Tonalite (Chesnut et al., 1973). In this work it is included in Terrible Vale Porphyritic Microgranodiorite (new name).||||||
28176|Harnham Grove Porphyritic Microtonalite|73202|6|Mentioned|p637|Sakmarian|Asselian|New England Orogen, southern. Zircon U-Pb crystallisation age from Black (2007). Misspelt as Harnham Grove Porphyriritc Microtonalite.|295 +/- 2 Ma U-Pb zircon|Hillgrove Plutonic Supersuite||||
31177|Harpers Hill Beds|43491|4|Described|pVII/45||Permian|||||||
32665|Harrison's Peak Granite|46568|14|Not recorded|p.423,425||Silurian|(I55-16/Michelago).||||||
80272|Harts Tank Beds|65469|6|Mentioned|p15, p17, |Late Silurian|Early Silurian|Lachlan Orogen. [Probable misspelling]. See also references for the Harts Tank beds. ||||||
25046|Harvey Group|33722|6|Mentioned|p229|||Misspelling of Hervey||||||
25046|Harvey Group|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
25046|Harvey Group|61894|6|Mentioned|p179 Fig.3|||||||||
25047|Hatchery Creek Conglomerate|12185|5|Briefly described|map legend|Middle Devonian|Middle Devonian|Mainly conglomerate, grit, shale, sandstone, and minor limestone. BMR map symbol: Dmh.||||||
25047|Hatchery Creek Conglomerate|22857|4|Described|p492 App.1 Tb.A1.7|Late Devonian|Middle Devonian|Conglomerate, arenite and shale, fining upward cycles. Max. thickness: 2900m. Geological Province: Hervey Basin. ||||||
25047|Hatchery Creek Conglomerate|23309|6|Mentioned|p390|||||||||
25047|Hatchery Creek Conglomerate|24005|5|Briefly described|p293|Middle Devonian|Middle Devonian|Geological Province: Lachlan Fold Belt||||||
25047|Hatchery Creek Conglomerate|24250|5|Briefly described|p107, p109 Fig.5|Early Devonian|Early Devonian|Underlying Unit: Taemas Limestone (disconformably) -  within the Goodradigbee Valley||||||
25047|Hatchery Creek Conglomerate|24580|5|Briefly described|p827|Devonian|Devonian|Contains fish fauna dated at late Emsian to middle Eifelian. Maximum Thickness: 2900m. Geological Province: Eastern Lachlan Fold Belt.||||||
25047|Hatchery Creek Conglomerate|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25047|Hatchery Creek Conglomerate|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25047|Hatchery Creek Conglomerate|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
25047|Hatchery Creek Conglomerate|29994|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25047|Hatchery Creek Conglomerate|30329|6|Mentioned|p30|||On Table P30.||||||
25047|Hatchery Creek Conglomerate|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25047|Hatchery Creek Conglomerate|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
25047|Hatchery Creek Conglomerate|31161|5|Briefly described|PA8|||||||||
25047|Hatchery Creek Conglomerate|32483|4|Described|p33|||Lower Devonian. Strat. table p4.||||||17-JUN-08
25047|Hatchery Creek Conglomerate|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25047|Hatchery Creek Conglomerate|33732|5|Briefly described|p112|||||||||
25047|Hatchery Creek Conglomerate|33959|6|Mentioned|p234|||||||||
25047|Hatchery Creek Conglomerate|34403|4|Described|p143|||||||||
25047|Hatchery Creek Conglomerate|34405|6|Mentioned|Fig.3.9|||||||||
25047|Hatchery Creek Conglomerate|35384|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25047|Hatchery Creek Conglomerate|35386|4|Described|p56|||||||||
25047|Hatchery Creek Conglomerate|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
25047|Hatchery Creek Conglomerate|36441|5|Briefly described|map legend|Middle Devonian|Middle Devonian|Conglomerate, sandstone and siltstone. Overlies Taemas Limestone. BMR map code: Dmh.||||||
25047|Hatchery Creek Conglomerate|36534|6|Mentioned|p225|||||||||
25047|Hatchery Creek Conglomerate|38193|6|Mentioned|p59|||||||||
25047|Hatchery Creek Conglomerate|38593|4|Described|p86|||||||||
25047|Hatchery Creek Conglomerate|39331|6|Mentioned|Fig.0-3|||||||||
25047|Hatchery Creek Conglomerate|39800|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
25047|Hatchery Creek Conglomerate|39978|6|Mentioned|p75|||||||||
25047|Hatchery Creek Conglomerate|41276|6|Mentioned|p67|||||||||
25047|Hatchery Creek Conglomerate|42015|6|Mentioned|p318|||||||||
25047|Hatchery Creek Conglomerate|42482|6|Mentioned|p103|||||||||
25047|Hatchery Creek Conglomerate|42497|5|Briefly described|Map Legend|Givetian|Eifelian|||||||
25047|Hatchery Creek Conglomerate|42577|5|Briefly described|p25|||||||||
25047|Hatchery Creek Conglomerate|42820|5|Briefly described|p95|||||||||
25047|Hatchery Creek Conglomerate|43430|14|Not recorded|p145|||||||||
25047|Hatchery Creek Conglomerate|43461|14|Not recorded|table p621||Ludlovian|||||||
25047|Hatchery Creek Conglomerate|44093|5|Briefly described|p196 App. 1|Middle Devonian|Middle Devonian|Geological Province: Lachlan Fold Belt.||||||
25047|Hatchery Creek Conglomerate|45147|2|Defined|M314|Middle Devonian|Middle Devonian|Eifelian ? p4.||||||17-JUN-08
25047|Hatchery Creek Conglomerate|46973|6|Mentioned|p51|||||||||
25047|Hatchery Creek Conglomerate|47050|6|Mentioned|p248|||||||||
25047|Hatchery Creek Conglomerate|50230|5|Briefly described|Map legend|Eifelian|Eifelian|Purple quartz-rich pebble conglomerate, quartz sandstone, minor siltstone.||||||
25047|Hatchery Creek Conglomerate|64238|5|Briefly described|Map legend|Devonian|Devonian|Purple, quartz-rich pebble conglomerate, quartz sandstone, and minor siltstone.||||||
25047|Hatchery Creek Conglomerate|68297|5|Briefly described|p192, 193|Givetian|Eifelian|See also Hatchery Creek Conglomerate Group p183. Includes Emsian, and Eifelian? vertebrate fossil faunas, but may be as young as Givetian.||||||
25047|Hatchery Creek Conglomerate|68298|5|Briefly described|p223|Eifelian|Emsian|Non-marine fauna. Biostratigraphic significance with Aztec fauna of Antarctica (Young and Gorter, 1981). Older age limit of late Emsian provided by conodonts in upper part of underlying unit. See also Hatchery Creek Formation. ||||Overlies Taemas Limestone.||
25047|Hatchery Creek Conglomerate|68592|5|Briefly described|p987-8, p1193, p1197, p1199, p1202|Eifelian|Emsian|Of Joplin et al. (1953). Subsequent work divided this unit into two Formations and elevated it to Group status (Hunt and Young, 2010). Type section described.|||||A thick sequence of Devonian clastic rocks overlying limestones.|
77675|Hatchery Creek Conglomerate Group|68297|6|Mentioned|p183|Middle Devonian|Middle Devonian|Of Young and Gorter (1981). Includes vertebrate fossils.See also Hatchery Creek Conglomerate p192.||||||
28598|Hatcherys Creek Conglomerate|33325|5|Briefly described|Table 4|||Age uncertain P16. Misspelling of Hatchery Creek [CB 12OCT94]||||||
30887|Hawk's Nest Beds|43400|2|Defined|p178,184,185||Early Devonian|||||||
30887|Hawk's Nest Beds|43406|14|Not recorded|p42,45,48-50|||Part of Tamworth Group, but strat. position unknown||||||
26607|Hawkes Creek Beds|22831|6|Mentioned|p 31|||||||||
26607|Hawkes Creek Beds|29986|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
26607|Hawkes Creek Beds|40136|6|Mentioned|p15|||||||||
26607|Hawkes Creek Beds|40328|6|Mentioned|p213|||||||||
26607|Hawkes Creek Beds|43500|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) (M.Ord)||||||
26607|Hawkes Creek Beds|46522|6|Mentioned|p50|||||||||
26607|Hawkes Creek Beds|48958|6|Mentioned|p8|||||||||
34626|Hawkes Creek Beds""|22831|6|Mentioned|p 31|||||||||
31178|Hawkesbury Beds|43491|14|Not recorded|pVIII/11a||Triassic|||||||
37382|Hawkesbury Sandstone unit|24040|6|Mentioned|p484|||Informal - see Hawkesbury Sandstone. Geological Province: Sydney Basin.||||||
31194|Hawkesbury Stage|43477|14|Not recorded|p16|||||||||
31194|Hawkesbury Stage|43491|14|Not recorded|pVIII/11a||Triassic|||||||
31194|Hawkesbury Stage|44861|14|Not recorded|p231|||||||||
31179|Hawkesbury sandstone formation|43491|14|Not recorded|pVIII/11a||Triassic|||||||
83493|Hawkesview Adamellite|73264|6|Mentioned|p1392, p1393 Fig.15|Devonian|Silurian|Lachlan Orogen, eastern. I-type. Also spelt (more correctly) as Hawksview Adamellite p1393 Fig.15.||||||01-SEP-22
81844|Hawkins Dacite|70125|5|Briefly described|p391, p394|Early Silurian|Early Silurian|~45 km N of Canberra. Probability density plot (PDP) of U-Pb ages of detrital zircons is compared with that of other units. PDP peaks indicate the Adaminaby Beds contributed zircons at source, as wall rock, or both.|430 Ma.|||||
81844|Hawkins Dacite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. S-type. Hf and O18 isotope data included.|430 Ma|||||
31229|Hawkins Formation|43479|14|Not recorded|p103|||||||||
30519|Hawkins Suite Volcanics|43202|5|Briefly described|Table 2 p20|||Informal use intended?||||||
25048|Hawkins Tuff|37727|6|Mentioned|p29|||||||||
30765|Hawkins beds|43344|14|Not recorded|p122,123|Early Silurian||||||||
30766|Hawkins prophyry|43344|14|Not recorded|p122|||Yass||||||
35030|Hawkins suite|23048|6|Mentioned|p13|||Informal name.||||||
40727|Hawkins volcanics|23309|6|Mentioned|p390|||||||||
70075|Hawkins/Laidlaw Volcanics|22857|6|Mentioned|p176|||Informal compound term - see Hawkins Volcanics and Laidlaw Volcanics.||||||
27428|Hawks Nest Beds|30911|6|Mentioned|Map legend|Silurian|Silurian|||||||
27428|Hawks Nest Beds|32482|6|Mentioned|Map legend|Devonian|Silurian|Ord.-Dev.||||||
27428|Hawks Nest Beds|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
27428|Hawks Nest Beds|32672|6|Mentioned|p673|||||||||
27428|Hawks Nest Beds|34554|6|Mentioned|p233|||Precise stratigraphic position unknown.||||||
27428|Hawks Nest Beds|37727|5|Briefly described|p62|||||||||
27428|Hawks Nest Beds|40328|3|Fully described|p196|||||||||
27428|Hawks Nest Beds|42849|6|Mentioned|p542|||||||||
27428|Hawks Nest Beds|43407|14|Not recorded|Map Legend|Devonian|Ordovician|(Provisional Edition)||||||
83561|Hawksbury Sandstone|73304|6|Mentioned|p61, p73, p76, p78-79|||[Probably misspelt from Hawkesbury Sandstone]. Base is equivalent to the Olenekian-Anisian boundary. Shown as Hawksbury Sandstone Formation p66.||||||
40560|Hazelvale Dacite Tuff|24605|6|Mentioned|p952 App.1|||Superseded by Hazelvale Rhyodacite Member.||||||
38984|Hazelvale Rhyodacite|23861|5|Briefly described|p4 Fig. 2, p17|Westphalian|Westphalian|Of Rocky Creek Conglomerate.  Geological Province: New England Orogen.||||||
38984|Hazelvale Rhyodacite|24605|6|Mentioned|p952 App.1|||Superseded by Hazelvale Rhyodacite Member.||||||
37307|Hazelvale Rhyolite|24010|6|Mentioned|p381|||||||||
36111|Heathcote tholeiite|23439|5|Briefly described|p131|||||||||
36111|Heathcote tholeiite|66575|6|Mentioned|p960,|Cambrian|Cambrian|Informal name.||||||
29286|Hebden seam|37087|4|Described|p199|||||||||
29286|Hebden seam|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
29286|Hebden seam|41604|6|Mentioned|p5|||||||||
29286|Hebden seam|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup, Wittingham Coal Measures).  Age: <260Ma.||||||
68173|Heffer Creek Sandstone Member|60281|6|Mentioned|p22|||Misspelt - see Heifer Creek Sandstone Member.  Of the Koukandowie Formation.||||||27-APR-05
70667|Heifer Creek Sandstone""|61310|5|Briefly described|Table C1 (p22-23)|||Informal name. Part of the Koukandowie Sandstone. Interbedded sandstone, siltstone, claystone, coal. Max. thickness: 400m. Geological Province: Clarence-Moreton Basin.  See also p24||||||
80634|Helidon Formation|71805|5|Briefly described|p75, 77|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. This unit is a time equivalent to the Precipice Sandstone, Poolowanna Formation and the Ripley Road Formation.||||||15-MAY-19
70352|Helidon Series|60993|6|Mentioned|p9|||Part of the Series sequence devised by Dunstan (1915) to describe the stratigraphy between the Walloon Series above and Ipswich Series below.||||||
26610|Hell Hole Beds|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26610|Hell Hole Beds|34692|6|Mentioned|p186|||||||||
26610|Hell Hole Beds|36390|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26610|Hell Hole Beds|40136|6|Mentioned|p15|||||||||
26610|Hell Hole Beds|70661|6|Mentioned|p7|||Named after Hell Hole Creek. Is an informal name and is included within undifferentiated Adaminaby Group.||||||
24308|Hell Hole Creek Adamellite|36443|5|Briefly described|map legend|Pragian|Lochkovian|Of Boggy Plain I-type Suite. Intrusive. Adamellite, minor granodiorite. BMR map code: Dhh.||||||
24308|Hell Hole Creek Adamellite|39660|6|Mentioned|p449|||||||||
24308|Hell Hole Creek Adamellite|40328|4|Described|p207|||||||||
24308|Hell Hole Creek Adamellite|40882|6|Mentioned|p25|||||||||
24308|Hell Hole Creek Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah11||||||
24308|Hell Hole Creek Adamellite|45147|2|Defined|M289|Early Devonian|Early Devonian|||||||
24308|Hell Hole Creek Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
40561|Hell Hole Creek Pyroclastics|24605|6|Mentioned|p953 App.1|||Superseded by Eulowrie Pyroclastic Member.||||||
77099|Hell Hole Monzogranite|71628|5|Briefly described|p8: 4, 85-87|||Reserved by Blevin and retained in this study. Originally Hell Hole Granodiorite (Wood, 1982). A small, bulbous, irregularly-shaped body 500m N of Tent Hill. Very limited geochemistry briefly described. Is associated with post-intrusion Sn, As mineralisation.||Wards Mistake Suite.||Intrudes Emmaville Volcanics and Gulf Siltstone-Argillite Formation.|Light grey-white, fine- to medium-grained, porphyritic biotite-hornblende monzogranite.|
77361|Hell Hole Pyroclastic Member|68005|5|Briefly described|p57, p142.|Late Carboniferous|Late Carboniferous|Felsic volcanics associated with fluvioglacial sequences in the Rocky Creek Block, Tamworth Belt.||Unit in Lark Hill Formation.|||Vitric tuff.|
73917|Henry River Suite|71628|5|Briefly described|p3:53|||||Hillgrove Supersuite.|Henry River Monzogranite.|||
81612|Hensleigh Formation|72263|4|Described|p515-518,522-523|Early Ordovician|Early Ordovician|Geological province: Lachlan Orogen. [Informal usage: Formal name is Hensleigh Siltstone.]Thickness: 310m (Bakers Swamp Creek) to 2km (SW of Wahringa homestead) (Morgan and Scott in Meakin et al., 1999, Percival et al., 1999, Glen et al., 2007b). Contains early to middle-late Bendigonian (476-472 Ma) conodonts and graptolites.||||Overlain unconformably by Cabonne Group. Underlain conformably by Mitchell Formation.|Laminated graptolitic siltstone, with minor volcaniclastic sandstone and allochthonous limestone.|
72962|Hensleigh Siltstone, lower|63121|6|Mentioned|p239|Early Ordovician|Early Ordovician|Contains allochthonous limestone with  brachiopods fragments of mid-Bendigonian age.||||||
39649|Hensley Siltstone|24398|5|Briefly described|p259 Fig. 2|Bendigonian|Bendigonian|Misspelt - see Hensleigh Siltstone.  Geological Province: Lachlan Fold Belt.||||||
82526|Herding Yard Creek Intrusives|71628|5|Briefly described|p11: 39; p15: 34, 53, 81; p16: 12,14,16|||See also p16: 20; p19: 83. Sivell and Passmore (1999), Passmore (1998). Appears in various forms including Herding Yard Creek intrusives/Intrusive.It remains unclear if all of the fine-grained felsic dykes derive from the Ruby Creek Leucogranite (e.g., Herding Yard Creek Intrusives of Passmore, 1998 and Sivell & Passmore, 1999a, b).||||Intrudes Cullendore Syenogranite; Undercliffe Falls and Jenners Monzogranites; Karonstadt and Stanthorpe Complexes.|Fine-grained mafic and felsic dykes.|
39376|Hervey group|24125|5|Briefly described|p3|Late Devonian|Late Devonian|Informal - see Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
30969|Hexham Sub-Group|43440|14|Not recorded|p35,fig.4-3|||Unit of Tomago Coal Measures||||||
31089|Higgin's Creek sandstone|43477|14|Not recorded|p26,27,58||Late Permian|Correlated with Marrangaroo conglomerate. Part of Wollondilly Coal Measures||||||
40562|High Valley Tuff""|24605|6|Mentioned|p937, p948 App.1|||Informal name for unnamed ignimbrite.||||||
25948|Highbury Volcanics|22857|5|Briefly described|p262|Early Permian|Early Permian|Geological Province: Gympie Terrane.||||||
25948|Highbury Volcanics|22864|6|Mentioned|p262||Early Permian|||||||
25948|Highbury Volcanics|23251|5|Briefly described|Table 1 p16, p19|||By Runnegar and Ferguson. Contains varying composition including Alma unit, Tozer Volcanics, Hall Clastics and Highbury Ankaramite. Of Gympie Group. Geol. Prov: Kin Kin Subprovince, Gympie Province. See also p35.||||||21-JUN-06
25948|Highbury Volcanics|23542|4|Described|p378|||Also see Table 1 p379 + p384. In the Gympie Group.||||||12-NOV-08
25948|Highbury Volcanics|23608|5|Briefly described|p53|Carboniferous|Devonian|Intruded by Woolooga Granodiorite.||||||
25948|Highbury Volcanics|23799|6|Mentioned|p31|||May be a correlative of Pinecliff Formation.  Geological Province: Gympie Province.||||||
25948|Highbury Volcanics|24040|5|Briefly described|p486|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
25948|Highbury Volcanics|24078|5|Briefly described|p425 Tb. 1|Early Permian|Early Permian|Amygdaloidal andesite with some andesitic agglomerate and pillow lavas.  Max. thickness: 3660m. Geological Province: Gympie Basin.||||||12-NOV-08
25948|Highbury Volcanics|30334|6|Mentioned|Table 111|||||||||
25948|Highbury Volcanics|30450|6|Mentioned|Table 1|||Permian age. Maryborough Basin.||||||12-NOV-08
25948|Highbury Volcanics|31703|6|Mentioned|Table|||P4||||||
25948|Highbury Volcanics|34475|2|Defined|p250|Early Permian|Early Permian|See pp247,249||||||29-MAY-15
25948|Highbury Volcanics|35101|5|Briefly described|p31|||||||||
25948|Highbury Volcanics|38805|6|Mentioned|p82|||||||||
25948|Highbury Volcanics|39252|6|Mentioned|Fig.13|||||||||
25948|Highbury Volcanics|39284|5|Briefly described|p431|||||||||
25948|Highbury Volcanics|39445|5|Briefly described|Table 8|||||||||
25948|Highbury Volcanics|41157|5|Briefly described|p81|||||||||
25948|Highbury Volcanics|41790|5|Briefly described|p469|||||||||
25948|Highbury Volcanics|42450|6|Mentioned|p403|||||||||
25948|Highbury Volcanics|42751|4|Described|p24|||Of Gympie Group.||||||24-SEP-08
25948|Highbury Volcanics|43006|4|Described|Table 1,p239|||||||||
25948|Highbury Volcanics|43017|6|Mentioned|p379|||Of Gympie Group.||||||12-NOV-08
25948|Highbury Volcanics|43018|6|Mentioned|p388|||||||||
25948|Highbury Volcanics|43100|4|Described|p18|||Of Gympie Group.||||||12-NOV-08
25948|Highbury Volcanics|44786|14|Not recorded|p193-202||Early Permian|||||||
25948|Highbury Volcanics|44923|5|Briefly described|Map Legend||Permian|||||||
25948|Highbury Volcanics|44928|5|Briefly described|Map Legend||Permian|||||||
25948|Highbury Volcanics|50320|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Gympie Province.||||||12-NOV-08
25948|Highbury Volcanics|61772|6|Mentioned|p128 Fig. 1||Carboniferous|In text, Volcanics is V.. In New England Orogen.||||||
25948|Highbury Volcanics|61780|5|Briefly described|p256, p257, p258||Early Permian|Of Gympie Group. Defined by Cranfield and Scott (1993).||||||
25948|Highbury Volcanics|61791|6|Mentioned|p326 Fig. 2|Permian|Carboniferous|In fig. 2 Volcanics is V.||||||
25948|Highbury Volcanics|65114|5|Briefly described|p383 Tb.1, p397|Early Permian||Tectonic unit: Gympie Province; in the Gympie Block||||||
25948|Highbury Volcanics|65118|5|Briefly described|p496|Early Permian|Early Permian|Gympie Province. Island arc tholeiites.||||||
25948|Highbury Volcanics|68679|5|Briefly described|p326, p369-370, p470|Permian|Mississippian|Runnegar and Ferguson (1969). Southern Gympie Province. Geochemical studies suggest a volcanic arc or backarc basin origin (primitive island-arc tholeiites). The LITHOLOGY entry includes the Alma unit.|||Alma unit.|Correlated with Mant Basalt.|Amygdaloidal pyroxene-phyric basalts with lava flows, pillow structures and tuff breccias and with minor interbedded conglomerate, sandstone and siltstone, hyaloclastites, dacitic epiclastics, shale, sandstone in Gympie area only.|
25948|Highbury Volcanics|70913|5|Briefly described|p1, p7, p9, p10-11, p12 fig 4|Permian|Permian|Gympie Province. Replaced in part by Highbury Basalt, see p58. Shown as Highbury volcanics p8, also Highbury Formation p9. Note the "andesites" within this unit have been reinterpreted as basalts, and the distribution modified, hence the name change.||Gympie Group|||Amygdaloidal andesite with andesitic agglomerate and pillow lava.|18-SEP-17
25948|Highbury Volcanics|72037|4|Described|p859,861-862,866,868-871|Early Permian|Early Permian|Geological province: New England Orogen, Gympie Terrane. Basal unit of the Gympie Terrane. Depositional age is poorly constrained, but interpreted to be Early Permian, based on its stratigraphic position below Rammutt Formation (Runnegar and Ferguson 1969). Previous theories on the origin of the Highbury Volcanics include an intraoceanic island arc (Mariana-type; Xiao et al., 2010) or marginal island arc (Japan-type of Xiao et al., 2010; Sivell and McCulloch, 2001). Present geological, geochemical, and geochronological data from Gympie Terrane suggest an interpretion of an extensional continental arc in the earliest Permian, evolving to be more felsic, as represented by andesites of the Rammutt Formation.||||Overlain disconformably to unconformably by Rammutt Formation.|Basaltic tuff breccias, agglomerate, and mafic volcanic lavas (submarine).|
25948|Highbury Volcanics|73197|5|Briefly described|p472, p478|||New England Orogen, northern. Basal unit in the Gympie Group. Represents early submarine volcanism in an island arc, formed over oceanic crust with a gradual change from deep water to shallow water environment. Proposed to be contemporaneous with New England Orogen rift volcanism (Li et al., 2015).||Gympie Volcanics||Underlies the Rammutt Formation.|Sequence of basalt and associated sedimentary rocks, includes horizons of deep marine muds gradually changing to shallow water pyroclastic deposits.|
40223|Highbury volcanics|38681|5|Briefly described|p35|Early Permian|Early Permian|Geological Province: New England Fold Belt||||||
77169|Highlands Creek Tuff Member|68003|5|Briefly described|p135.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
77169|Highlands Creek Tuff Member|68005|6|Mentioned|p141.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
29564|Highlands Igneous Complex|42984|6|Mentioned|p371|||Variation on Highlands Complex?||||||
29564|Highlands Igneous Complex|71628|6|Mentioned|p13:2|||Now the Highlands Complex, after unpublished work by Kilpatrick (1986).||||||
70487|Highlands Tuff Member|62095|6|Mentioned|p276 Appdx.|||Of Kelk (1986). Superseded by Rockford Ignimbrite Member.||||||29-MAY-06
41271|Hill Sixty Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Leucocratic, perthitic biotite ilmenite Ti-magnetite granite.||||||05-JUL-04
38933|Hill Sixty Granite""|24417|6|Mentioned|p100|||Name abandoned - still included as part of the Mortray Hill Granite Complex.||||||
82757|Hillgrove Blue Granite|71628|6|Mentioned|p1: 4; p3: 56|||Andrews (1905). Later Hillgrove Adamellite (Binns et al., 1967).||||||
31230|Hillgrove Granite|43479|14|Not recorded|p178||Early Carboniferous|||||||
31230|Hillgrove Granite|67818|5|Briefly described|p130|Artinskian|Artinskian|Whole rock Rb-Sr age.|289+/-25 Ma|||||
31230|Hillgrove Granite|71628|6|Mentioned|p3: 56|||Brown et al. (1968). Subsequently Hillgrove Monzogranite (Ashley et al., 2007).||||||
31230|Hillgrove Granite|73264|6|Mentioned|p1398 Fig.20|Permian|Permian|New England Orogen.||Hillgrove Supersuite||||
37373|Hillgrove Granite Suite|24040|5|Briefly described|p468 Fig. 1, p469, p470 Fig. 2|Late Carboniferous|Late Carboniferous|See also Hillgrove Suite. S-type granite. Age: ca.300Ma.||||||21-AUG-08
40259|Hillgrove Granitoid Suite|38905|6|Mentioned|p302 Fig.1|||Geological Province: New England Fold Belt||||||
40248|Hillgrove Plutonic Suite""|38842|5|Briefly described|p287|Permian|Permian|Geological Province: New England Fold Belt. Age: 285 +/- 15Ma||||||
83044|Hillgrove Plutonic Supersuite|73202|5|Briefly described|p625-626, p628, p634, p636-638, p640|Early Permian|Late Carboniferous|New England Orogen, southern. S-type granites. Formed from melting of the Carboniferous accretionary wedge, includes zircon inheritance. Geochemically and lithologically very similar to Bundarra Plutonic Supersuite. Mingling occurs with the Bakers Creek Suite. Rb-Sr ages of ca 260 Ma for biotite formed at lower amphibolite facies in solid-state deformation (Landenberger, 1995). Described as early Permian in text but includes crystallisation ages in the late Carboniferous (Collins et al., 1993; Kent, 1994; Cawood et al., 2011). Suggested to be comagmatic with the Ramleh Volcanics.|ca 300 Ma, 296-288 Ma, 302 Ma, 305 Ma||Abroi granodiorites, Tia granodiorites, Rockvale Monzogranite, Harnham Grove Porphyritic Microtonalite||Granites, homogeneous, has experienced solid-state deformation.|
69990|Hillgrove Plutonic suite|61773|6|Mentioned|p139|||Informal name.||||||
69988|Hillgrove Suite granitoids|61773|6|Mentioned|p139|||Informal reference to granitoid rocks of the Hillgrove Plutonic Suite.||||||
69988|Hillgrove Suite granitoids|62095|5|Briefly described|p268|Late Carboniferous|Late Carboniferous|Informal - see Hillgrove Suite. Intruded Tablelands Complex at 320Ma.||||||
35365|Hillgrove plutonic suite|23186|6|Mentioned|p485|||||||||
37375|Hillgrove suite|23763|6|Mentioned|p543|||Informal.  Geological Province: New England Fold Belt.||||||
37375|Hillgrove suite|24040|6|Mentioned|p470 Fig.2|||Informal - see Hillgrove Suite.||||||
37375|Hillgrove suite|24521|6|Mentioned|p102|||Geological Province: New England Orogen.||||||
37375|Hillgrove suite|38681|6|Mentioned|p36|||Geological Province: New England Fold Belt||||||
68807|Hillgrove supersuite|24513|6|Mentioned|p9, p10 Fig.1|||Informal. See Hillgrove Supersuite.||||||
77278|Hillsdale Claystone Member|68004|5|Briefly described|p51 Table 5, p53.|Late Permian|Late Permian|Upper Hunter Coalfield. The rank 'Member' is missing in table 5.||Unit in Lucernia Coal.||Overlies Carramere Coal Member. Is overlain by Rombo Coal Member.||
38230|Hillsdale Coal|23717|5|Briefly described|p118 Fig.2|Permian|Permian|Parent: Dights Creek Coal.   Geological Province: Sydney Basin||||||
28607|Hillton Seam|42182|6|Mentioned|p298|||||||||
83572|Hilltop coal seam|73304|6|Mentioned|p66|||[Possibly a variation of Hilltop Coal Member].||||||
27799|Hilltop sandstone|40331|4|Described|p12|||||||||
82440|Hillview Adamellite|71628|6|Mentioned|p3:32|||Binns et al. (1967). Now the Eastlake Monzogranite.||||||
82438|Hillview Gabbro|71628|5|Briefly described|p2: 62-68, 71|||New name, after a nearby homestead. A sigmoidal-shaped body in the SE corner of the Complex. Occurs ~25 km SE of Uralla. Forms rounded boulders on rounded hills and swampy basins. No radiometric age. Geochemistry described.||Woodburn Complex.||Almost completely enclosed by Shallow Lagoon Monzogranite. Abuts The Knobs Tonalite.|Compositionally and texturally zoned, medium- to coarse-grained, leucocratic olivine gabbro and clinopyroxene-orthopyroxene leucogabbro; chilled marginal phase.|
82441|Hillview Granite|71628|6|Mentioned|p17: 30|||Daigle (1993, unpublished). Now Kindee Creek Tonalite.||||||
72799|Hoares Gneiss|23313|6|Mentioned|p319|||Mentioned only as Hoares Gneiss-style mineralisation in the Broken Hill district.||||||07-FEB-07
38231|Hobden Gully Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Dights Creek Coal.||||||
77266|Hobden Gully Member|68004|5|Briefly described|p51 Table 5, p53.|Late Permian|Late Permian|Upper Hunter Coalfield.||Basal unit in Dights Creek Coal.||Overlies Waterfall Gully Formation. Is overlain by Naleen Tuff Member.||
70071|Homeville coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Early Permian|Informal reference to a seam within the Greta Coal Measures.||||||
31088|Homeville formation|43477|4|Described|p39|||||||||
25064|Honeyman Rodingite|39331|6|Mentioned|Table 8-1|||||||||
25950|Honeysuckle Beds|23309|5|Briefly described|p383|Wenlock|Silurian|||||||
25950|Honeysuckle Beds|29450|6|Mentioned|p53|||||||||
25950|Honeysuckle Beds|29453|6|Mentioned|p26|||||||||
25950|Honeysuckle Beds|29454|4|Described|p11|||||||||
25950|Honeysuckle Beds|29648|6|Mentioned|p15|||||||||
25950|Honeysuckle Beds|29682|4|Described|p12|||||||||
25950|Honeysuckle Beds|30172|6|Mentioned|p43|||||||||
25950|Honeysuckle Beds|30334|6|Mentioned|p121|||||||||
25950|Honeysuckle Beds|31279|6|Mentioned|p215|||||||||
25950|Honeysuckle Beds|31448|6|Mentioned|p20|||||||||
25950|Honeysuckle Beds|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25950|Honeysuckle Beds|33001|6|Mentioned|p64|||||||||
25950|Honeysuckle Beds|33002|6|Mentioned|p410|||Section||||||
25950|Honeysuckle Beds|33004|6|Mentioned|p175|||||||||
25950|Honeysuckle Beds|33959|6|Mentioned|p235|||||||||
25950|Honeysuckle Beds|35070|2|Defined|p36|Early Silurian|Early Silurian|Probably Early Silurian. Superseded by Honeysuckle Metabasic Igneous Complex.||||||25-NOV-08
25950|Honeysuckle Beds|35185|6|Mentioned|p230|||||||||
25950|Honeysuckle Beds|35194|4|Described|Table 1|||See also p66.||||||05-DEC-07
25950|Honeysuckle Beds|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25950|Honeysuckle Beds|35522|5|Briefly described|p45|||||||||
25950|Honeysuckle Beds|35608|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25950|Honeysuckle Beds|35609|4|Described|p5|||||||||
25950|Honeysuckle Beds|35946|6|Mentioned|p27|||||||||
25950|Honeysuckle Beds|36051|5|Briefly described|p411|||||||||
25950|Honeysuckle Beds|36411|6|Mentioned|p269|||Refers Basden et al 1978 for definition.||||||
25950|Honeysuckle Beds|37727|4|Described|p63|||||||||
25950|Honeysuckle Beds|39319|6|Mentioned|p357|||||||||
25950|Honeysuckle Beds|39331|5|Briefly described|p33|||L.Sil.? See P34. Chem.anal. Fig.4-3,4-8||||||
25950|Honeysuckle Beds|40328|4|Described|p40|||||||||
25950|Honeysuckle Beds|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
25950|Honeysuckle Beds|40498|6|Mentioned|p378|||||||||
25950|Honeysuckle Beds|41798|5|Briefly described|Fig.2|||||||||
25950|Honeysuckle Beds|42145|4|Described|Table 1 P624|||||||||
25950|Honeysuckle Beds|42497|5|Briefly described|Map Legend|Llandoverian|Bolindian|||||||
25950|Honeysuckle Beds|42828|4|Described|p130|||||||||
25950|Honeysuckle Beds|45147|6|Mentioned|M128|||||||||
26619|Honeysuckle Creek Leucoadamellite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Fine to medium-grained, equigranular to porphyritic, biotite leucogranite and leucomonzogranite.||||||21-DEC-04
26619|Honeysuckle Creek Leucoadamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
26619|Honeysuckle Creek Leucoadamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26619|Honeysuckle Creek Leucoadamellite|38842|6|Mentioned|p286|||||||||
26619|Honeysuckle Creek Leucoadamellite|42378|6|Mentioned|Table 1 P11|||||||||
26619|Honeysuckle Creek Leucoadamellite|43091|5|Briefly described|Map legend|||||||||
26619|Honeysuckle Creek Leucoadamellite|71628|6|Mentioned|p19:76|||Binns et al. (1976), after unpublished work by Ransley (1970). Now Honeysuckle Creek Leucosyenogranite.||||||
41063|Honeysuckle Creek Leucogranite|24366|6|Mentioned|p10|||||||||
41063|Honeysuckle Creek Leucogranite|71628|6|Mentioned|p19:76|||Brown (2003) after unpublished work by Chappell and Bryant (1994). Now Honeysuckle Creek Leucosyenogranite.||||||
41064|Honeysuckle Creek Leucomonzogranite|24366|6|Mentioned|p9 Fig. 7|||||||||
41064|Honeysuckle Creek Leucomonzogranite|71628|6|Mentioned|p19:76|||Brown (2003) after unpublished work by Chappell and Bryant (1994). Now Honeysuckle Creek Leucosyenogranite.||||||
34186|Honeysuckle Metabasic Igneous Complex""|22857|6|Mentioned|p174|||Of Basden (1990a,b). Replaced by Honeysuckle beds.||||||
34187|Honeysuckle beds""|22638|6|Mentioned|p39|||Superseded by Honeysuckle beds||||||24-AUG-04
70646|Hooray Sandstone, Lower""|61312|6|Mentioned|p71|||Replaced by Hooray Sandstone. Essentially a fluviatile sandstone sequence. Geological Province: Eromanga Basin.||||||
70646|Hooray Sandstone, Lower""|70821|6|Mentioned|p31|||In western QLD and SA, this unit has been subdivided into the Namur Sandstone and the overlying Murta Formation.||||||
70647|Hooray Sandstone, Upper""|61312|6|Mentioned|p71|||Replaced by Cadna-owie Formation. Geological Province: Eromanga Basin.||||||
70647|Hooray Sandstone, Upper""|70821|6|Mentioned|p31|||Now the Cadna-owie Formation.||||||
68980|Hornsby breccia""|60299|6|Mentioned|p223|||||||||
37999|Horses Gneiss Formation|24307|5|Briefly described|p966|Proterozoic|Proterozoic|Misspellling of Hores Gneiss.||||||22-APR-08
77267|Horseshoe Creek Sub-group|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Wollombi Coal Measures.|Includes Clifford Formation, Alcheringa Coal, Strathmore Formation and Lucernia Coal.|Overlies Apple Tree Flat Sub-group. Is overlain by Doyles Creek Sub-group.||
38202|Horshoe Creek Subgroup|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures.   Geological Province: Sydney Basin||||||
25951|Hoskins Formation|22857|4|Described|p418 App. 1 Tb. A1.5|Ordovician|Cambrian|Chert, cherty siltstone with interbedded manganiferous (pyrolusite) horizons.||||||24-FEB-06
25951|Hoskins Formation|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
25951|Hoskins Formation|24215|6|Mentioned|p802|||Superseded by Hoskins Chert. Geological Province:  Lachlan Fold Belt||||||
25951|Hoskins Formation|29907|2|Defined|Appendix 1|Late Ordovician|Late Ordovician|Prob.Late Ordovician||||||
25951|Hoskins Formation|29910|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
25951|Hoskins Formation|35185|6|Mentioned|p237|||||||||
25951|Hoskins Formation|36411|6|Mentioned|p269|||Refers Bowman 1977.||||||
25951|Hoskins Formation|36534|6|Mentioned|p223|||||||||
25951|Hoskins Formation|40136|6|Mentioned|p15|||||||||
25951|Hoskins Formation|40365|6|Mentioned|p270|||||||||
25951|Hoskins Formation|40762|6|Mentioned|Fig.18|||||||||
25951|Hoskins Formation|40772|4|Described|p443|||||||||
25951|Hoskins Formation|40891|3|Fully described|p11|||||||||
25951|Hoskins Formation|41897|5|Briefly described|p86|||||||||
25951|Hoskins Formation|42262|6|Mentioned|Fig. 2 P1810|||||||||
25951|Hoskins Formation|42489|5|Briefly described|Map legend|Llandovery|Darriwilian|||||||
25951|Hoskins Formation|43263|6|Mentioned|Map Legend||Ordovician|||||||
25951|Hoskins Formation|44093|5|Briefly described|p180 App. 1|Early Silurian|Ordovician|Geological Province: Lachlan Fold Belt.||||||
25951|Hoskins Formation|46522|2|Defined|p52|Late Ordovician||||||||
25951|Hoskins Formation|46524|6|Mentioned|p121|||||||||
25951|Hoskins Formation|46525|6|Mentioned|Fig.1 P143|||||||||
25951|Hoskins Formation|46528|5|Briefly described|Map legend|Ordovician||||||||
25951|Hoskins Formation|63291|6|Mentioned|p419 Fig. 2|||||||||
25951|Hoskins Formation|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
38844|Hoskins Formation""|24417|6|Mentioned|p7|||Superseded by Hoskins Chert.  Formerly included Bragan Volcanics.||||||
39421|Hoskinstown group|23309|6|Mentioned|p390|||||||||
39421|Hoskinstown group|24128|5|Briefly described|p32|||Informal name.||||||
79106|Hoskintown Group|69635|6|Mentioned|p12, 14, 19, 25|||[Misspelling of Hoskinstown] See also Hoskinstown Group p11, 32, 38.  Some fossil control available.||||||
28610|Hoskissons Coal Member|24159|5|Briefly described|p149|Late Permian|Late Permian|Parent: Black Jack Group. Geological Province: Gunnedah Basin.||||||
28610|Hoskissons Coal Member|37094|4|Described|p243|||||||||
28610|Hoskissons Coal Member|38614|4|Described|p9|||||||||
28610|Hoskissons Coal Member|39666|6|Mentioned|p84|||||||||
28610|Hoskissons Coal Member|39693|6|Mentioned|p17|||||||||
28610|Hoskissons Coal Member|39913|5|Briefly described|p6|||||||||
28610|Hoskissons Coal Member|40060|6|Mentioned|p63|||||||||
28610|Hoskissons Coal Member|40198|6|Mentioned|p31|||||||||
28610|Hoskissons Coal Member|40321|6|Mentioned|p19|||||||||
28610|Hoskissons Coal Member|40680|4|Described|p23|||||||||
28610|Hoskissons Coal Member|40767|6|Mentioned|Fig.10|||||||||
28610|Hoskissons Coal Member|40952|4|Described|p9|||||||||
28610|Hoskissons Coal Member|41229|5|Briefly described|p1|||See also Fig.9||||||
28610|Hoskissons Coal Member|41290|6|Mentioned|Fig.5|||||||||
28610|Hoskissons Coal Member|41990|5|Briefly described|p8|||||||||
28610|Hoskissons Coal Member|42679|6|Mentioned|Fig.3 P3|||||||||
28610|Hoskissons Coal Member|43194|3|Fully described|p98 Tb. 8.2, p108-113, p127, p133 App. 1|Late Permian|Late Permian|See also references on p95, p97, p105-106, p129 Tb.8.3, p130. Of Black Jack Formation in this article. Has been elevated to Formation status, of Coogal Subgroup, Black Jack Group. Overlies Arkarula Sandstone Member; interfingers with and underlies Clare Sandstone Member. Age Lower to Upper Stage 5.||||||
70652|Hoskissons coal|61313|6|Mentioned|p105|||Informal - see Hoskissons Coal.||||||25-NOV-08
25067|Hoskissons seam|37094|4|Described|p243|||||||||
25067|Hoskissons seam|38614|6|Mentioned|p1|||||||||
25067|Hoskissons seam|38958|5|Briefly described|p494|||||||||
25067|Hoskissons seam|39913|4|Described|p13|||||||||
25067|Hoskissons seam|40060|4|Described|p63|||||||||
25067|Hoskissons seam|40330|6|Mentioned|p59|||||||||
25067|Hoskissons seam|40680|6|Mentioned|p25|||||||||
25067|Hoskissons seam|40952|4|Described|p10|||||||||
25067|Hoskissons seam|41990|6|Mentioned|Fig.4 P16|||||||||
26621|Hospital Hill Porphyry|29992|6|Mentioned|Map legend|Carboniferous|Carboniferous|Post-Devonian. Prob. Carboniferous||||||
26621|Hospital Hill Porphyry|29994|6|Mentioned|Map legend|Carboniferous|Carboniferous|Post-Devonian. Prob. Carboniferous||||||
34648|Hospital Porphyry""|22815|5|Briefly described|p94|||Probably obsolete. Now part of Boyd Volcanic Complex.||||||
81420|Hovell Suite|70727|5|Briefly described|p171|||Geological province: Hill End Zone, Eastern Lachlan Orogen. Comprises ten plutons, including the Wyangala Granite.||Unit of Wyangala Supersuite.||||
82758|Howell Granite|71628|6|Mentioned|p19: 42|||Andrews et al. (1907). Renamed Howell Leucoadamellite by Flinter (1982), then Gilgai Granite by Korsch (1977) after work by Juniper (1974). Now Gilgai Leucogranite (this study).||||||
23656|Howell Leucoadamellite|38842|6|Mentioned|p286|||||||||
23656|Howell Leucoadamellite|38905|6|Mentioned|p303|||||||||
23656|Howell Leucoadamellite|41347|6|Mentioned|p376|||||||||
23656|Howell Leucoadamellite|71628|6|Mentioned|p19: 33, 42, 44|||Flinter (1981). Later renamed Gilgai Granite (Korsch, 1977 after work by Juniper, 1974); now Gilgai Leucogranite. Originally Howell Granite (Andrews et al., 1907).||||||
77268|Howes Hill Seam|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Informal name? Within Clare Sandstone (Coogal Subgroup, Black Jack Group)||||||
77268|Howes Hill Seam|68004|5|Briefly described|p152.|||South Mullaley Sub-basin, Gunnedah Basin. Thickness 2.5 m; amenable to underground mining. Suitable for domestic electricity generation; washing may raise it to export quality.|||||Predominantly high-ash coal.|
70072|Howes Hill seam|22857|6|Mentioned|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for coal seam in the Benelabri Formation (Black Jack Group). ||||||
33403|Humbug Formation|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of the Wagga Group.||||||13-JUL-04
32693|Humbug Sandstone|24417|3|Fully described|p12|Ordovician|Ordovician|Of Wagga Group.  Intruded by Ungarie Granite, Charcoal Tank Granite and Cookaburragong Granodiorite.  Probably Darriwilian in age.||||||
32693|Humbug Sandstone|44936|5|Briefly described|Map Legend||Ordovician|||||||
32693|Humbug Sandstone|50385|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Wagga Group. Quartzose sandstone and minor siltstone, locally metamorphosed||||||11-JUN-04
32693|Humbug Sandstone|61964|5|Briefly described|p19, p21|Ordovician|Ordovician|Replaced by Clements Formation (Wagga Group).Originally of Duggan and Scott (2000a) - and equivalent to Sequence 3 of Warren et al (1995).Nomenclatural details included. Also written as "Humbug Sandstone".||||||
32693|Humbug Sandstone|67322|5|Briefly described|p39|||(Duggan and Scott, in Lyons et al. 2000): this name for thick-bedded sandstone and quartzite facies within the Wagga Group on the Forbes 1:250 000 sheet has now been suppressed in favour of an expanded definition of the Clements Formation (Hendrickx and Colquhoun, in Colquhoun et al. 2005).||||||22-FEB-18
25069|Hume Group|33732|5|Briefly described|p112|||||||||
25069|Hume Group|37727|6|Mentioned|p64|||||||||
25069|Hume Group|48926|6|Mentioned|p35|||P35 et seq.||||||
31590|Hume Park Suite|42726|5|Briefly described|map legend||Silurian|||||||
31590|Hume Park Suite|44093|5|Briefly described|p196 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
31590|Hume Park Suite|68592|6|Mentioned|p1242|||Chappell et al. (1991), including Hume Park Granite which was originally mapped by Browne (1959). Subsequently reassigned to the Young Suite of the Bullenbalong Supersuite by Blevin (2011).||||||
30767|Hume Series andesite|43344|14|Not recorded|p117|||On Map Legend||||||
30768|Hume Series conglomerate|43344|14|Not recorded|p117|||On Map Legend||||||
30769|Hume Series shales|43344|14|Not recorded|p117|||On Map Legend||||||
31139|Hume beds|43491|14|Not recorded|pIV/8||Late Silurian|||||||
76157|Hummocks Formation|66623|6|Mentioned|p125 Photograph 28.|||Typo for Hummock.||||||
30988|Hunter River Coal Measures|43447|14|Not recorded|p3|||||||||
37440|Hunter Sandstone|23214|6|Mentioned|p227|||Superseded by Hunter Formation.||||||
38946|Hunter Siltstone""|24417|6|Mentioned|p132|||Superseded by Hunter Formation.||||||
33975|Huntley Claystone|22578|6|Mentioned|p401|||of Bargo Claystone||||||
33975|Huntley Claystone|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Sydney Basin. CA-TIMS age of 254.86 Ma (Metcalfe et al., 2015), corresponding to D. parvihola zone (Wuchiangpingian).||Unit of Illawarra Coal Measures.||||
33975|Huntley Claystone|73304|5|Briefly described|p70, p74, p78|Wuchiapingian|Wuchiapingian|Sydney Basin, southern.|254.86 +/- 0.30 Ma U-Pb CA-TIMS.|||||
33975|Huntley Claystone|73421|6|Mentioned|p16|Wuchiapingian|Wuchiapingian|Sydney Basin, southern. Age of 254.86+/-0.30 Ma from Metcalfe et al., (2015), same age is also shown with the Bargo Claystone.|254.86+/-0.30 Ma|Illawarra Coal Measures||||
26624|Hurlstone Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Hurlstone Adamellite.||||||
40728|Hyandra Volcanics|23309|6|Mentioned|p390|||||||||
26625|Hyde Creek Granite|42726|5|Briefly described|map legend|Early Devonian||131. Of the Hyde Creek Suite.  Reserved as Hyde Creek Granodiorite.  Bega Batholith.||||||08-FEB-05
30888|Hyde's Creek Complex|43400|14|Not recorded|p183||Middle Devonian|Near base of Yarrimie Formation. See also Lexicon||||||
34618|Hylea Intrusive Complex""|22831|6|Mentioned|p 19|||Informal name - see Hylea Intrusive Complex.||||||21-JUL-04
72974|Illawarra Coal Measures, upper|61315|6|Mentioned|p183|||Informal - see Illarawarra Coal Measures. ||||||
28614|Illawarra"" Coal Measures|34335|6|Mentioned|p369|||Permian. Sydney Sub-Group||||||
38910|Illunie Rhyolite""|24417|6|Mentioned|p44|||Superseded by Illunie Volcanics and parts now included in Warrangong Volcanics.||||||
73605|Illwarra coal measures|63461|6|Mentioned|p862 Fig. 1c|||Misspelt and informal - see Illawarra Coal Measures.||||||
41304|Ingebryah Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
70488|Inglewood Formation|62095|6|Mentioned|p278 Appdx.|||Of Kelk (1986), Cherry (1987) and Davies (1988). Superseded Inglewood Mudstone and is now itself superseded by Woodton Formation.||||||
70489|Inglewood Mudstone|62095|6|Mentioned|p278 Appdx.|||of Lowe (1971) and Warner (1972). Together with Kankool Formation this was formerly superseded by Inglewood Formation and is now itself superseded by Woodton Formation.||||||
77170|Inglewood member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Laminated to massive, multicoloured, silty mudstone; fine- to medium-grained, beige, lithic sandstone (some with rip-up clasts); diamictite and conglomerate.|
25078|Inlet Quartz Monzonite|23549|6|Mentioned|p520|||Referred to as a suite in the context of discussing the Moonbi Supersuite, of which it is part. Mafic pluton.  Adjacent to the Moonbi pluton.||||||05-APR-05
25078|Inlet Quartz Monzonite|35192|6|Mentioned|Fig.1|||||||||
25078|Inlet Quartz Monzonite|39564|6|Mentioned|p12|||||||||
36467|Inlet Suite|23549|5|Briefly described|p520|||Of Moonbi Supersuite. Geological Province: New England Batholith.  See also the informal Inlet suite and misspelt Inlets suite.||||||05-APR-05
36467|Inlet Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
36467|Inlet Suite|69541|5|Briefly described|p646|||New England Batholith.||Unit in Moonbi Supersuite.|Includes Inlet Monzonite.|||
36467|Inlet Suite|71628|5|Briefly described|p7:20|||||Moonbi Supersuite.|Inlet Monzogranite.|||
68008|Inlet suite|23549|5|Briefly described|p519|||Of the Moonbi Supersuite. Geological Province: New England Batholith.||||||05-APR-05
68007|Inlets suite|23549|6|Mentioned|p516 Fig.1|||Misspelt and informal - see Inlet Suite.  See also the informal Inlet suite.||||||16-FEB-05
33598|Intake Formation|48600|2|Defined|p14,17-18|||Plant fossils. Formation of Great Artesian Group. Name is invalid.||||||
25080|Irondale Seam""|39232|6|Mentioned|p105|||||||||
29652|Isaac's Formation|43014|6|Mentioned|p250|||Misspelling/variation on Isaacs Formation.||||||
41619|Isaacs Formation ""|44244|6|Mentioned|p155|||Of Campbell (1961).  Replaced by McInnes Formation and/or the overlying Johnsons Creek Conglomerate.||||||
25081|Isabella granite|32347|6|Mentioned|p182|||||||||
70491|Isismede Ignimbrite|62095|6|Mentioned|p260 Tb. 1|Early Carboniferous|Early Carboniferous|Variation/abbreviation of Isismede Ignimbrite Member. Ages: 3517+/-3.2Ma, 352.4+/-3.0Ma, 355.5+/-2.0Ma. See also Isismede Member (Caldwell 1985).||||||29-MAY-06
70492|Isismede Member|62095|5|Briefly described|p259 Fig. 10|Early Carboniferous|Early Carboniferous|Of Caldwell (1985). Superseded by Isismede Ignimbrite Member. Age: 352Ma. See also p272 Appdx.||||||31-JAN-08
40465|Isismurra Formation, upper|24603|6|Mentioned|p898|||Informal - see Isismurra Formation.  Geological Province: Tamworth Belt.||||||
32247|Island Bend Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah13||||||
32247|Island Bend Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
25082|Island Bend Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25082|Island Bend Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
25082|Island Bend Granite|34544|6|Mentioned|p187|||||||||
25082|Island Bend Granite|40328|4|Described|p207|||||||||
25082|Island Bend Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
25082|Island Bend Granite|45087|6|Mentioned|p30|||Chemical analyses||||||
25082|Island Bend Granite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Kosciusko Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
25082|Island Bend Granite|60007|6|Mentioned|Map legend|Early Devonian|Early Devonian|Included in the Jindabyne Granite in map legend.||||||
25082|Island Bend Granite|60085|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|||||||
38853|J-K beds""|24070|5|Briefly described|p303|Cretaceous|Jurassic|Informal name. Geological Province: Coonamble Embayment.||||||
82641|Jacks Creek Monzogranite Phase|71628|5|Briefly described|p16: 29-32; p19:91|||New name (this study), after unpublished work by Fogarty (2000). Has previously been regarded as part of Rivertree Syenogranite, and despite geochemical differences remains as such pending further investigation. Occurs as two small outcrops (measured in hundred of metres), 20 km E of Liston. The limited geochemistry is described; is geochemically assigned (tentatively) to the Five Mile Creek Suite.||Rivertree Syenogranite.||Abuts Rivertree Syenogranite and Koreelah Creek Granodiorite (probably intrudes the latter).|Porphyritic, rapakivi, biotite-(hornblende) monzogranite.|
31478|Jackson Suite|42726|5|Briefly described|map legend||Silurian|Of the Boggy  Plain Supersuite.  Contains the Jackson Granite.||||||08-FEB-05
25960|Jacqua Formation|22857|5|Briefly described|p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Of the Fernleigh Group. Thinly bedded siltstone and sandstone. Max. thickness: 220m. Geological Province: Bindook Rise. ||||||
25960|Jacqua Formation|30735|2|Defined|p42|Early Devonian|Early Devonian|||||||
25960|Jacqua Formation|30736|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
25960|Jacqua Formation|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
25960|Jacqua Formation|39568|5|Briefly described|p77|||Name proposed to be abandoned. Nominated type section .||||||
25960|Jacqua Formation|68592|5|Briefly described|p1096|||Felton and Huleatt (1977). Base contains a poorly-preserved fauna of probable Siluro-Devonian age.||||Overlain conformably by Windellama Limestone.|Well-bedded fine sandstones and silty shales.|
27804|Jamberoo Sandstone|22969|6|Mentioned|Fig 5.5|||||||||
27804|Jamberoo Sandstone|29900|6|Mentioned|p166|||||||||
27804|Jamberoo Sandstone|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
27804|Jamberoo Sandstone|34434|4|Described|Table 5.8|||||||||
27804|Jamberoo Sandstone|36042|6|Mentioned|p20|||See also Fig.16.||||||
27804|Jamberoo Sandstone|36220|6|Mentioned|p18|||||||||
27804|Jamberoo Sandstone|38656|6|Mentioned|Fig.1.5.14|||p281.||||||04-DEC-08
27804|Jamberoo Sandstone|38690|6|Mentioned|p291|||Renamed Jamberoo Sandstone Member.||||||
27804|Jamberoo Sandstone|39287|6|Mentioned|p32|||||||||
27804|Jamberoo Sandstone|39289|4|Described|p79|||See also p78.||||||04-DEC-08
30668|Jamberoo Tuff|43344|14|Not recorded|p77|||||||||
30668|Jamberoo Tuff|43349|14|Not recorded|Map|||||||||
30668|Jamberoo Tuff|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
30668|Jamberoo Tuff|45018|14|Not recorded|p40|||||||||
31082|Jamberoo tuff|43477|14|Not recorded|p41,59|||||||||
31083|Jamberoo tuff member|43477|14|Not recorded|p19||Permian|Part of Broughton tuff. Gerringong Volcanics||||||
80462|Jawbone Creek granodiorite suite|70718|5|Briefly described|p60-p62, p64, p71, p94, p120|||Informal name, interpreted mostly from geophysics. Wanganella granodiorite intersected in Bundy No.1 drillhole. Strongly magnetically zoned, indicating multiple injections of magma with a TMI peak amplitude of approximately 200nT. Most constituent granodiorites have associated Bouger gravity lows. Magnetic signatures suggest suite is I-type.|||Includes the Windouran Swamp granodiorite, Wanganella granodiorite, Niemur granodiorite, Jawbone Creek granodiorite, Billabong Creek granodiorite, Werai granodiorite.|||03-APR-18
76026|Jeffereys Flat Formation|66927|6|Mentioned|Map legend|Cambrian|Cambrian|[Mis-spelling of Jeffreys Flat Formation].||||||24-SEP-13
76025|Jefferys Flat Formation|66922|5|Briefly described|Map legend|Cambrian|Cambrian|Mis-spelling of Jeffreys Flat Formation.||Unit in Warratta Group.|||Variably cleaved phyllite and slate; originally siltstone with minor sandstone beds; local minor limestone and conglomerate.|
22022|Jeffreys Flat beds|44093|5|Briefly described|p147 App. 1|Early Paleozoic|Early Paleozoic|Geological Province: Kanmantoo Fold Belt.||||||07-NOV-08
22022|Jeffreys Flat beds|63489|5|Briefly described|Map legend|Ordovician|Late Cambrian|Deformed slate, sandstone, very minor diamictite, carbonate.||||||10-SEP-07
22022|Jeffreys Flat beds|66623|6|Mentioned|p99, p105.|||Named by Scheibner and Basden (1996); redefined as Jeffreys Flat Formation (Greenfield 2010).||||||
22022|Jeffreys Flat beds|66933|5|Briefly described|Map legend|||New Bendigo Zone, Delamerian Fold Belt.|||||Phyllite, lesser metasandstone; very minor granule conglomerate, diamictite, limestone.|
22022|Jeffreys Flat beds|70210|5|Briefly described|p1, p12, p18, p22, p26, p38, p40-41|Silurian|Middle Cambrian|Koonenberry-Tibooburra district. Ages of a tuff cobble and a foliated tuff respectively.|510.4 +/- 3.0 Ma; 423.3 +/- 2.1 Ma.||||Diamictite containing a tuff cobble, and foliated tuff.|
38454|Jemba volcanics|24133|6|Mentioned|p41|||Replaced by Jemba Ignimbrite.  Geological Province: Lachlan Fold Belt.||||||
23665|Jemidee granodiorite|36600|6|Mentioned|Table 1|||||||||
25087|Jenny Lind Granite|33476|2|Defined|p95|Early Triassic|Early Triassic|Mention p22.||||||19-NOV-07
25087|Jenny Lind Granite|33766|6|Mentioned|Map legend|Early Triassic|Permian|Permian - Early Triassic||||||
25087|Jenny Lind Granite|35257|6|Mentioned|p76|||See also Fig.7.||||||
25087|Jenny Lind Granite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
25087|Jenny Lind Granite|43008|5|Briefly described|map legend|||||||||
25087|Jenny Lind Granite|68111|5|Briefly described|p968 Tb.1|Olenekian|Olenekian|Ar-Ar (hornblende) geochronology by Bryant et al. (1997).|ca. 249.7 Ma|Of the Clarence River Supersuite.||||21-OCT-14
25087|Jenny Lind Granite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
25087|Jenny Lind Granite|70876|4|Described|p2-p3, p42-p46, p78-p79, p94|Permian|Permian|New England Orogen. An additional date of c. 249.7  Ma is derived from Ar-Ar dating by Bryant et al, 1997. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|255.3 +/- 1.2 Ma (SHRIMP U-Pb)|Jenny Lind Suite|||Medium-grained, equigranular, plagioclase-dominated tonalite.|
25087|Jenny Lind Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|255+/-1.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
25087|Jenny Lind Granite|71628|6|Mentioned|p9:31|||Thomson (1976). Later the Jenny Lind Granodiorite (Bryant et al., 1997) and subsequently Jenny Lind Tonalite (Blevin).||||||
39536|Jenny Lind Granodiorite|23799|5|Briefly described|p117|||Of the Towgon Suite (Clarence River Supersuite - as defined by Shaw and Flood, 1981 and Bryant et al, 1997).||||||
39536|Jenny Lind Granodiorite|68008|6|Mentioned|p333|||Geochemistry mentioned.||||||
39536|Jenny Lind Granodiorite|70217|5|Briefly described|p73 tbl 14.1|Induan|Induan|New England Orogen.|c. 249.7 Ma (Ar/Ar Bryant et al. 1997a)|Clarence River Supersuite||||
39536|Jenny Lind Granodiorite|71628|6|Mentioned|p9: 1-2, 4, 32|||Bryant et al. (1997). Originally Jenny Lind Granite of Thomson (1976). The name Jenny Lind Tonalite was reserved in ASUD by Blevin and is used in this study. Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). The lithology is not included in the list of constituents of the Suite on p9: 1-2. Is excluded from Clarence River Supersuite in this study.||||||
73893|Jenny Lind Suite|70876|5|Briefly described|p42|||New England Orogen.||Clarence River Supersuite|Includes the Jenny Lind Granite.|||
73893|Jenny Lind Suite|71628|5|Briefly described|p9:32|||||Clarence River Supersuite.|Jenny Lind Tonalite.|||
30665|Jenolan Beds""|43320|14|Not recorded|p6|||||||||
70582|Jenolan beds""|62368|5|Briefly described|p379, p391 Fig.10|Early Devonian|Early Devonian|Informal name. Silicic volcaniclastics of Allan (1986). Overlies the Jenolan Caves Limestone. Likely to be of similar age to Bindook Volcanic Complex. See also informal Jenolan volcanics.||||||
70584|Jenolan volcanics|62368|6|Mentioned|p401|||Informal name. Weathered and contains illite. Refer to the "Jenolan beds".||||||
30923|Jepson Limestone Member|43417|14|Not recorded|Map Legend||Eifelian|Part of Timor Limestone||||||
35829|Jerangle Complex|23321|5|Briefly described|p430 Fig.2|||||||||07-FEB-07
28117|Jerangle Granite|39800|6|Mentioned|Map legend|Carboniferous|Late Devonian|Late Devonian or Carboniferous||||||
28117|Jerangle Granite|45087|5|Briefly described|p35|||Chemical analyses||||||
36139|Jerangle complex|23464|6|Mentioned|p249|||||||||
69939|Jerangle metamorphic complex|60412|6|Mentioned|p233|||Lachlan Fold Belt.||||||
69939|Jerangle metamorphic complex|60904|6|Mentioned|p794|||Informal - see Jerangle Metamorphic Complex.||||||
37407|Jericho Limestone|23214|6|Mentioned|p140|||Formerly Cow Quarries limestone. Now replaced by Alton Limestone Member of Bells Creek Volcanics.||||||
30813|Jerrara "Series"|43384|14|Not recorded|Map Legend||Silurian|||||||
25088|Jerrawa Beds|30069|5|Briefly described|p3|||||||||
25088|Jerrawa Beds|30332|4|Described|p122|||Ordovician age||||||
25088|Jerrawa Beds|32483|6|Mentioned|p9|||Refers Mann (1921)||||||
25088|Jerrawa Beds|32820|4|Described|p3|||||||||
25088|Jerrawa Beds|33125|6|Mentioned|p15|||Correlation chart||||||
25088|Jerrawa Beds|35384|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
25088|Jerrawa Beds|35386|3|Fully described|p8|Ordovician|Ordovician|Graptolite fauna from several localities indicates Late Eastonian age.||||||
25088|Jerrawa Beds|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
25088|Jerrawa Beds|36413|6|Mentioned|p26|||See also Table 3.||||||
25088|Jerrawa Beds|37727|6|Mentioned|Fig.1|||||||||
25088|Jerrawa Beds|38151|6|Mentioned|Table 1|||||||||
25088|Jerrawa Beds|39331|5|Briefly described|p49|||||||||
25088|Jerrawa Beds|40136|5|Briefly described|p28|||||||||
25088|Jerrawa Beds|40328|6|Mentioned|p159|||||||||
25088|Jerrawa Beds|43857|6|Mentioned|p317|||Same as Jerrawa Shales, Jerrawa Series, p315?||||||
25088|Jerrawa Beds|68592|6|Mentioned|p282|||Brown (1940). Subsequently included in Abercrombie Formation.||||||
25088|Jerrawa Beds|71069|6|Mentioned|p58|||Obsolete name, replaced by the Abercrombie Formation. Incorporates rocks which were previously assigned to the Bendoc, Margules and Douro Groups. ||||||
68981|Jerrys Plain Subgroup|60299|5|Briefly described|p208|||Of Wittingham Coal Measures. Geological Province: Sydney Basin||||||
68981|Jerrys Plain Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
23666|Jerula Formation|22520|6|Mentioned|p18|||of the Yarra Yarra Creek Group||||||
23666|Jerula Formation|22831|6|Mentioned|p 57|||||||||
23666|Jerula Formation|42449|2|Defined|p24|||Reserved March 1991, J. Pickett.||||||
23666|Jerula Formation|68297|5|Briefly described|p189, 191|Pragian|Lochkovian|NSW.  Includes a range of acanthodian scales and platelets.||||||
27806|Jervis Bay Sandstone""|34334|4|Described|p362|||||||||
27806|Jervis Bay Sandstone""|39664|6|Mentioned|p131|||||||||
30751|Jervis Bay formation|43377|14|Not recorded|p143|||Formation of Shoalhaven Group||||||
25089|Jesse Limestone|5178|6|Mentioned|p106 Fig.1, p108-109, p114|||Of Limekilns Group. Contains calcarenites and limestone conglomerates with pebble to boulder sized clasts of carbonate and chert common.||||||
25089|Jesse Limestone|22520|6|Mentioned|p18|Emsian|Emsian|||||||
25089|Jesse Limestone|22590|6|Mentioned|Fig3 P754||Emsian|||||||
25089|Jesse Limestone|23214|6|Mentioned|p203|||Superseded by Jesse Limestone Member of Limekilns Formation. Formerly Diamond Creek Limestone.||||||
25089|Jesse Limestone|23522|5|Briefly described|p248 Fig 4|Emsian|Emsian|||||||
25089|Jesse Limestone|24019|6|Mentioned|p354, p356|Emsian|Emsian|||||||
25089|Jesse Limestone|31331|6|Mentioned|p181|||See also P182||||||
25089|Jesse Limestone|31502|6|Mentioned|p95|||Devonian||||||
25089|Jesse Limestone|32619|6|Mentioned|p460|||Fauna||||||
25089|Jesse Limestone|33326|6|Mentioned|p436|||Fauna.||||||
25089|Jesse Limestone|33732|5|Briefly described|p117|||||||||
25089|Jesse Limestone|34403|4|Described|p131|||Fauna early mid Devonian.||||||
25089|Jesse Limestone|34405|6|Mentioned|Fig.3.9|||||||||
25089|Jesse Limestone|35491|6|Mentioned|p135|||||||||
25089|Jesse Limestone|39214|5|Briefly described|p23|||||||||
25089|Jesse Limestone|40131|6|Mentioned|Fig.4|||||||||
25089|Jesse Limestone|41000|6|Mentioned|p279|||||||||
25089|Jesse Limestone|41207|5|Briefly described|p94|||||||||
25089|Jesse Limestone|42033|6|Mentioned|p654|||||||||
25089|Jesse Limestone|42051|6|Mentioned|p139|||||||||
25089|Jesse Limestone|43461|14|Not recorded|table p621,p622||Emsian|||||||
25089|Jesse Limestone|43517|14|Not recorded|p139-40,153,155,161||Early Devonian|map plate XII||||||
25089|Jesse Limestone|43519|14|Not recorded|p118,Tb p119,120|||||||||
25089|Jesse Limestone|62735|6|Mentioned|p987|Emsian|Emsian|Contains scutellum fossils.  In New South Wales.||||||
25089|Jesse Limestone|64296|5|Briefly described|p84|Late Emsian|Late Emsian|Overlies Limekilns Formation. Has a 'serotinus' conodont fauna as well as rich coral.||||||28-AUG-08
25089|Jesse Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Limekilns. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25089|Jesse Limestone|68297|5|Briefly described|p186, 192|Emsian|Pragian|Includes Emsian vertebrate fossil fauna.||||||
25089|Jesse Limestone|71600|6|Mentioned|p34|Early Devonian|Early Devonian|Of Wright and Flory, 1981. Limekilns, NSW.||||||
25089|Jesse Limestone|71924|6|Mentioned|p1, 2, 3||Emsian|Limekilns district. Includes Polygnathus serotinus near base. Has fauna different to Cunningham Formation. But fauna similar to Suchers Creek Limestone||Of 'Limekilns Group'.||Underlain by Rosedale Shale.||
26640|Jillamatong Granite|42726|5|Briefly described|map legend|Silurian||368.  Of the Bullenbalong Suite (Bullenbalong Supersuite).  Formal name not intended. Variation on Jillamatong Granodiorite.||||||08-FEB-05
22034|Jillicambra Adamellite|22815|4|Described|p85|||||||||
22034|Jillicambra Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
26641|Jimberoo Member|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Womboyne Formation (Cocoparra Group). Arenite and siltstone.||||||
26641|Jimberoo Member|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26641|Jimberoo Member|34109|5|Briefly described|p174|||||||||
26641|Jimberoo Member|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26641|Jimberoo Member|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26641|Jimberoo Member|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. (Proposed as JIMBAROO) Upper Devonian. Top of the Womboyne Formation. Overlies the Melbergen Sandstone Member; underlies the Mailman Gap Conglomerate Member of the Rankin Formation.||||||25-MAR-08
26641|Jimberoo Member|61964|5|Briefly described|p14 Fig. 4, p114|Frasnian|Frasnian|Of the Cocoparra Group. Superseded "Stitts Member". Written as "Jimberoo Member". Upgraded to Jimberoo Formation. See also p117 Fig. 35.||||||14-OCT-08
25090|Jincumbilly Granite|42726|5|Briefly described|map legend|Silurian||Variation on Jincumbilly Adamellite.||||||
34611|Jindabyne Granite""|22815|6|Mentioned|p49|||Superseded by Jindabyne Tonalite.||||||
24320|Jinden Adamellite|22815|4|Described|p72||Early Devonian|K/Ar Age: 406+/-6 Ma, Rb/Sr Age: 402+/-6 Ma.||||||
24320|Jinden Adamellite|22857|6|Mentioned|p215|||Geological Province: Lambie Basin.||||||
24320|Jinden Adamellite|22859|6|Mentioned|p215|||||||||
24320|Jinden Adamellite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24320|Jinden Adamellite|40276|2|Defined|p9|Early Devonian|Early Devonian|||||||
24320|Jinden Adamellite|42497|5|Briefly described|Map Legend|Zlichovian|Lochkovian|||||||
24320|Jinden Adamellite|42820|5|Briefly described|p77|||||||||
24320|Jinden Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Jinden Suite.||||||
24320|Jinden Adamellite|61818|5|Briefly described|p85|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
24320|Jinden Adamellite|71700|6|Mentioned|CD|||||Jinden Suite||||
22036|Jingo Creek Adamellite|22815|4|Described|p81,82|||||||||
22036|Jingo Creek Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Jingo Creek Suite.||||||
23671|Jo Doth Tuff|40872|6|Mentioned|Fig.2|||||||||
79254|Johnson's Creek Conglomerate|64631|5|Briefly described|p47.|Serpukhovian|Serpukhovian|Myall Block, southern New England Fold Belt. See also Johnsons Cr. p44. Biostratigraphic age control for base and top and radiometric age control within unit.|||||Diamictites and rhythmically laminated mudrocks, interbedded with other facies such as thick fluvial conglomerates.|
29653|Johnson's Peak Conglomerate|43014|6|Mentioned|p250|||Misspelling of Johnsons Creek Conglomerate?||||||
36334|Joppa Formation|50234|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Mount Fairy Group.  Interbedded with Sooley Volcanics, Woodlawn Volcanics, De Drack Formation.||||||11-MAY-04
36334|Joppa Formation|67820|6|Mentioned|p136 Fig.3|Late Silurian|Late Silurian|||Mount Fairy Group.||||
70069|Jounama Creek Limestone, Lower|22857|5|Briefly described|p454 App.1, Tb.A1.6|Silurian|Silurian|Informal name. Massive limestone. Max. thickness:>500m. Geological Province: Tumut Trough.||||||
73696|Junction Reefs Limestone|63286|6|Mentioned|p308 Fig. 9|Bolindian|Bolindian|Of the Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
35429|Kabadah Beds""|23170|6|Mentioned|p55|||||||||
35429|Kabadah Beds""|43494|6|Mentioned|p17|Early Silurian|Ordovician|Informal - see Kabadah Beds.  Superseded by Kabadah Formation.||||||
38943|Kadina Formation""|23217|5|Briefly described|p3|||(Conolly, 1965a).  Informal - see Kadina Formation.||||||08-MAR-06
38943|Kadina Formation""|24417|5|Briefly described|p127|||Of "Beargamil Sub-Group".  Superseded by Boulton Formation.||||||
26646|Kadoona Dacite|22606|6|Mentioned|P828|||||||||
26646|Kadoona Dacite|22719|6|Mentioned|p486|||||||||
26646|Kadoona Dacite|22778|6|Mentioned|p 163|||||||||
26646|Kadoona Dacite|24222|5|Briefly described|p9|||Chemistry of samples reported. I-type.  Geological Province: Lachlan Fold Belt.||||||21-OCT-08
26646|Kadoona Dacite|40738|4|Described|p622|||||||||
26646|Kadoona Dacite|41133|4|Described|p1116|||||||||
26646|Kadoona Dacite|42497|5|Briefly described|Map Legend|Pridolian|Ludlovian|||||||
26646|Kadoona Dacite|61818|5|Briefly described|p85|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
26646|Kadoona Dacite|64312|6|Mentioned|p433|||||||||
26646|Kadoona Dacite|69876|5|Briefly described|p314|||Lachlan Fold Belt. Sourced from partial crustal melting at ~25 km depth.|||||I-type dacite.|
82809|Kadoona dacite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. I-type. Hf and O18 isotope data included.|414 Ma|||||
38923|Kadungle rhyolites|24417|6|Mentioned|p90|||Not intended as a formal name - see Kadungle Volcanics.||||||
28630|Kahiba Formation|22578|6|Mentioned|p401|||||||||
28630|Kahiba Formation|37083|6|Mentioned|p164|||||||||
25691|Kain Porphyry|22857|5|Briefly described|p480 App.1 Tb.A1.6|Silurian|Silurian|Dacitic and rhyodacitic porphyry - mainly intrudes Toggannoggra Rhyolite Member.||||||24-OCT-13
25691|Kain Porphyry|39028|6|Mentioned|Map legend|Pridolian|Pridolian|||||||
25691|Kain Porphyry|40276|2|Defined|p8|Late Silurian|Late Silurian|Of the Long Flat Volcanics?||||||23-AUG-12
25691|Kain Porphyry|42497|5|Briefly described|Map Legend|Pridolian|Ludlovian|||||||
25691|Kain Porphyry|61818|5|Briefly described|p85|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
29444|Kalimnan Series""|42966|6|Mentioned|p152|||superseded by Bookpurnong beds.||||||
28222|Kalkite Adamellite|22815|4|Described|p45|Silurian|Silurian|Rb/Sr age: 410+/-5.4 Ma.||||||24-AUG-12
28222|Kalkite Adamellite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28222|Kalkite Adamellite|35109|2|Defined|p61|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
28222|Kalkite Adamellite|35263|6|Mentioned|Table 3|||||||||
28222|Kalkite Adamellite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
28222|Kalkite Adamellite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
28222|Kalkite Adamellite|40328|4|Described|p207|||||||||
28222|Kalkite Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
28222|Kalkite Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab11.||||||
28222|Kalkite Adamellite|49705|6|Mentioned|p38|||||||||
28222|Kalkite Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||15-JUL-04
26648|Kalkite Granite|42726|5|Briefly described|map legend|Silurian||365.  Of the Bullenbalong Suite (Bullenbalong Supersuite).  Formal name not intended. Variation on Kalkite Granodiorite, Adamellite.||||||08-FEB-05
34679|Kalnura Marine Tongue|22864|6|Mentioned|p264||Late Permian|Max Age: 256 Ma.||||||
82759|Kaloe Granite|71628|6|Mentioned|p18: 13|||Cawood et al. (2011). Now the Kaloe Tonalite.||||||
22059|Kaloe Granodiorite|23799|5|Briefly described|p117|||Of the Duncans Creek Suite (Clarence River Supersuite).||||||
22059|Kaloe Granodiorite|23811|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Clarence River Plutonic Suite.  Medium-grained, equigranular, hornblende-rich granodiorite with a platy deformation foliation; abundant mafic dykes in places.||||||20-DEC-04
22059|Kaloe Granodiorite|23812|4|Described|p21 Tb.2, p33|Early Permian|Early Permian|Of Clarence River Plutonic Suite.  Age: 293Ma (Ar/Ar).||||||
22059|Kaloe Granodiorite|60079|5|Briefly described|Map Legend|Permian|Permian|Of the Clarence River Suite.||||||20-JUL-04
22059|Kaloe Granodiorite|61770|6|Mentioned|p108, p109|||Age: 293.1+/-1.8Ma (Ar-Ar, Byrant etal. 1997). I-Type. Intrudes the Willowie Creeks beds.||||||
22059|Kaloe Granodiorite|61772|6|Mentioned|p131||Carboniferous|Age: ca. 293Ma (Bryant et al, 1997).||||||
22059|Kaloe Granodiorite|64098|5|Briefly described|p335, p332 Fig. 1|Early Permian|Early Permian|Of Clarence River Suite. Age: 291 Ma Ar40/Ar39 hornblende.||||||
22059|Kaloe Granodiorite|65114|5|Briefly described|p396|Sakmarian||I-type; 40Ar/39Ar age on a hornblende separate of 293.1 +/- 1.8 Ma||||||
22059|Kaloe Granodiorite|68008|6|Mentioned|p333|||Geochemistry mentioned. Similar composition to Kaloe Granodiorite.||||||
22059|Kaloe Granodiorite|68679|5|Briefly described|p465 Fig.5.142|||Geochemistry briefly described; geochemical plots.||Clarence River Supersuite.|||The high-silica part of this unit is a TTG Group granitoid.|
22059|Kaloe Granodiorite|68901|6|Mentioned|p6|Permian|Early Permian|New England Region. SHRIMP age derived from Cawood et al, 2011.|291.9 +/- 2 Ma (SHRIMP U-Pb)||||I type granodiorite.|15-NOV-18
22059|Kaloe Granodiorite|70217|5|Briefly described|p72, p73|Early Permian|Early Permian|New England Orogen. Ages given are Ar/Ar from Bryant et al (1997a) and SHRIMP U-Pb from Cawood et al (2011) respectively.|293.1 +/- 1.8 Ma to 291.9 +/- 2 Ma|Clarence River Supersuite||||
22059|Kaloe Granodiorite|71628|6|Mentioned|p9: 1-2; p18:13|||Barnes (1987). Previously Hanging Rock Adamellite. Now Kaloe Tonalite. Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). The lithology is not included in the list of constituents of the Suite on p9-1.||||||
22059|Kaloe Granodiorite|73197|6|Mentioned|p471|Guadalupian|Late Carboniferous|New England Orogen, southern. Geosynchronous with rifting, intrudes accretionary wedge.||||||
73894|Kaloe Suite|71628|6|Mentioned|p18: 14||||||Kaloe Tonalite.|||
31986|Kanagra Granite|42712|6|Mentioned|Fig3 p9|Carboniferous|Early Carboniferous|Misspelling of Kanangra? Replaced by Tuglow Granite?||||||
30640|Kandos "Series"|43316|14|Not recorded|p12|Middle Devonian|Middle Devonian|||||||
30640|Kandos "Series"|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|See also Lexicon||||||
30038|Kandos Series|23214|6|Mentioned|p205|||Superseded by Kandos Group.||||||
30038|Kandos Series|43188|6|Mentioned|p205|||of Sussmilch (1934).Superseded by Kandos Group.||||||
40724|Kandos group|23309|6|Mentioned|p390|||||||||
42316|Kangaloohah Volcanics|24266|5|Briefly described|p1480|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
70354|Kangaroo "Series"|60993|6|Mentioned|p35|||Of Lloyd and Whiting (1940), and others. Superseded by Kangaroo Creek Sandstone. ||||||
25103|Kangaroo Basanite|36220|5|Briefly described|p97|||||||||
70353|Kangaroo Creek "Stage"|60993|6|Mentioned|p35|||Of Lloyd and Whiting (1940), and others. Superseded by Kangaroo Creek Sandstone. ||||||
31973|Kangaroo Creek Series|43881|14|Not recorded|p44|Cretaceous|Late Jurassic|Now known as Kangaroo Creek Sandstone.||||||
31974|Kangaroo Creek Stage|43881|14|Not recorded|p44|Cretaceous|Late Jurassic|See also Lexicon. Rocks now called Kangaroo Creek Sandstone.||||||
26652|Kangaroo Mount Basanite|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic. Variation of Kangaroo Basanite?||||||
28633|Kangaroo Mountain Basalt|34434|6|Mentioned|Fig.5.25|||||||||
70418|Kangaroo Sandstone|61005|6|Mentioned|p254 Tb. 4|||Misspelt - should be Kangaroo Creek Sandstone.||||||
22063|Kangaroobie Formation|23214|5|Briefly described|p70|||Now included in the Oakdale Formation.||||||
22063|Kangaroobie Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
42314|Kangiara group|24266|5|Briefly described|p1481|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
69704|Kangorong Sand|61155|5|Briefly described|p18|Middle Eocene|Middle Eocene|Overlain by Lacepede Formation. Thickness: 30m. Geological Province: Otway Basin (Gambier Embayment). ||||||
70495|Kankool Member|62095|6|Mentioned|p260 Tb. 1|Late Carboniferous|Late Carboniferous|Abbreviated version of Kankool Ignimbrite Member.  Age: 308.9+/-2.8Ma.||||||
68138|Kanmantoo Complex""|44093|6|Mentioned|p89|||Superseded by Kanmantoo Group. Geological Province: Kanmantoo Trough.||||||14-MAR-05
69940|Kanmantoo turbidite fans|60904|6|Mentioned|p806 Fig. 25b|||Informal term for turbidites of the Kanmantoo Group. ||||||
35978|Kara Beds|23380|5|Briefly described|p105||Late Precambrian|of Wonaminta Block. Preferred name is Kara beds.||||||
35978|Kara Beds|23469|6|Mentioned|Fig 6 p 321|||||||||
35978|Kara Beds|23932|5|Briefly described|p665 Table 1|Neoproterozoic|Neoproterozoic|Age: 586 Ma.||||||
35978|Kara Beds|62787|5|Briefly described|p77|Cambrian|Neoproterozoic|Of Mills (1992). Unconformably overlain by Mutawintji Group. Metasediments.||||||07-FEB-11
35978|Kara Beds|64685|5|Briefly described|Map Legend|Middle Cambrian|Proterozoic|Strongly weathered slaty and metabasaltic units. Rarely exposed but believed to underlie much of northwestern part of map sheet. Some units with strong magnetic signature.||||||20-MAY-13
33999|Karignon Conglomerate|22578|6|Mentioned|p402|||of Newcastle Coal Measures||||||
33999|Karignon Conglomerate|23055|6|Mentioned|Fig9 p17|||||||||16-APR-14
74789|Karonstadt Hybrid suite|61790|6|Mentioned|p318, p321|||One of a group of hybrid monzogranite suites. ?Accidently written as Karonstadt Hybrid Monzogranite on p321.||||||18-SEP-09
82514|Karonstadt Hybrids|71628|6|Mentioned|p19: 80|||Passmore (1988, unpublished). This text states ""The name Karonstadt Hybrids is currently included within Geoscience Australia's ASUD but is considered invalid"". [In fact the ASUD lists Karonstadt Hybrid suite (sic) as informal.] See Karonstadt Complex.||||||
69866|Karoopa Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains the Karoopa Granite.||||||09-SEP-08
69866|Karoopa Suite|68592|2|Defined|p1397-8, p1459-65|Early Devonian|Early Devonian|New unit and name, after Karoopa Lane and nearby Karoopa property. Contains one [!] pluton, the Karoopa Granite. Assigned to Boggy Plain Supersuite on the basis of chemistry and inferred age.||Unit in Boggy Plain Supersuite.|Includes Karoopa Granite.|Intrudes Young Granodiorite. Is overlain unconformably by Hervey Group (inferred).|Predominantly biotite granite; minor biotite tonalite phase and a few late-stage porphyritic rhyolite dykes. Rare miarolitic cavities and originally glassy groundmass indicate high level intrusion. I-type.|
69866|Karoopa Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Karoopa Granite|||
69866|Karoopa Suite|70545|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Karoopa Granite|||
70497|Karralee Member|62095|6|Mentioned|p257 Fig. 8|||Abbreviated version of Karralee Ignimbrite Member.||||||
38909|Kars intrusive complex""|24417|6|Mentioned|p39|||Informal name replaced by Kars Ultramafic Intrusive Complex.||||||
41197|Kars ultramafic intrusive complex|50554|5|Briefly described|Map legend|Ordovician|Ordovician|Informal name.  Intermediate to mafic volcanics and instrusives.||||||24-JUN-04
76159|Kayrunnera Gabbro|66623|6|Mentioned|pp95-97. |||Informal name for outcropping rock now included in Bittles Tank Volcanics.||||||
76158|Kayrunnera beds|66623|6|Mentioned|p115|||Name first used by Brunker et al. (1971) on Koonenberry 1:500 000 sheet. Subsequently defined as a Group by Webby et al. (1988).||||||
32664|Keating's Shale Member|46568|14|Not recorded|p.428|||Lens in Kohinoor Volcanics. (I55-16/Michelago).||||||
32634|Keating's shale|46568|14|Not recorded|p.426|||(I55-16/Michelago).||||||
75065|Kedumba Creek Sandstone''|61609|6|Mentioned|p239, p241|Permian|Permian|Informal name of Benedek (1965). Missnamed when drilling. Equivalent unit to Snapper Point Formation.||||||07-FEB-11
30662|Kedumba breccia|43341|14|Not recorded|p230|||||||||
35072|Keelindi Beds|23053|6|Mentioned|p26|||(Hawke and Cramsie 1984). Presently 'Keelindi beds'||||||
35072|Keelindi Beds|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment.||||Overlies Pilliga Sandstone. Is overlain by Drildool Beds.||
30901|Keepit Beds|43399|14|Not recorded|p194|||Ref.to Williams 1954(unpubl.)No other data||||||
28639|Keewong-Micaligo Porphyry Complex""|36413|6|Mentioned|p45|||||||||
26656|Keginni Sandstone|29987|5|Briefly described|p24|||||||||
26656|Keginni Sandstone|34057|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26656|Keginni Sandstone|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26656|Keginni Sandstone|35925|6|Mentioned|p9|||Refers Bryan 1968.||||||
26656|Keginni Sandstone|43380|14|Not recorded|Map Legend||Late Devonian|Unit of Mulga Downs Group||||||
26656|Keginni Sandstone|43381|14|Not recorded|Map Legend||Late Devonian|Mulga Downs Group||||||
26656|Keginni Sandstone|43389|14|Not recorded|Map Legend||Late Devonian|||||||
26656|Keginni Sandstone|43398|14|Not recorded|Map Legend||Late Devonian|Part of Mulga Downs Group||||||
69857|Keginni Sandstone Member|61213|5|Briefly described|p319 Fig. 3|Givetian|Givetian|Diagrammatically shown as near base of Crowl Formation.||||||
26658|Kellys Plain Porphyry|12185|5|Briefly described|map legend|Devonian|Devonian|Quartz-feldspar porphyry, dacite, ignimbrite(?) rhyolite. BMR map symbol: Dk.||||||
26658|Kellys Plain Porphyry|30332|6|Mentioned|Table 1|||||||||
26658|Kellys Plain Porphyry|31015|6|Mentioned|p252|||||||||
26658|Kellys Plain Porphyry|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
26658|Kellys Plain Porphyry|34403|5|Briefly described|p146|||||||||
26658|Kellys Plain Porphyry|45147|6|Mentioned|M165|||||||||
30924|Kelso Greywacke Member|43417|14|Not recorded|Map Legend||Early Carboniferous|Part of Glenlawn Mudstone||||||
30679|Kembla Greywacke|43345|14|Not recorded|p6||Permian|||||||
23692|Kempfield Granite|22679|6|Mentioned|p 7|||||||||
23692|Kempfield Granite|42726|5|Briefly described|map legend|Silurian||||||||
29516|Kenilworth Group|22679|4|Described|p 9|Ordovician|Ordovician|||||||
29516|Kenilworth Group|22704|6|Mentioned|Fig1(b),p51|||Also p59||||||
29516|Kenilworth Group|22857|5|Briefly described|p129, p422 App. 1, Tb. A1.5|Ordovician|Ordovician|Includes Fairbridge Volcanics, Wahringa Limestone Member and Kenyu Formation. Geol. Prov: Molong Volcanic Arc.  See also p424 App.1 Tb.A1.5.||||||
29516|Kenilworth Group|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
29516|Kenilworth Group|23170|6|Mentioned|p31,34|Ordovician|Ordovician|Age: Middle Ordovician.||||||
29516|Kenilworth Group|23202|6|Mentioned|Fig.1|||||||||
29516|Kenilworth Group|23213|6|Mentioned|p13|||Pogson and Watkins 1998 put Fairbridge Volcanics into this group. This article moves Fairbridge Volcanics to Cabonne Group, based on fossil evidence.||||||
29516|Kenilworth Group|23214|2|Defined|p22|Ordovician|Ordovician|Age determined by palaeontological evidence. Includes Walli Volcanics, Triangle Formation, Kenyu Formation, Coombing Formation and Fairbridge Volcanics. Geological Province: Lachlan Fold Belt.||||||04-MAR-09
29516|Kenilworth Group|23245|6|Mentioned|p129|||||||||
29516|Kenilworth Group|24233|5|Briefly described|p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
29516|Kenilworth Group|24417|5|Briefly described|p164|Ordovician|Ordovician|||||||
29516|Kenilworth Group|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes; Fairbridge Volcanics, Kenyu Formation, Cooming Formation and Walli Volcanics.||||||17-JUL-08
29516|Kenilworth Group|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes Coombing Formation and Triangle Formation.||||||
29516|Kenilworth Group|43782|5|Briefly described|Map Legend|Darriwilian|Yapeenian|||||||
29516|Kenilworth Group|44093|5|Briefly described|p201 App. 1|Early Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt.||||||
29516|Kenilworth Group|63287|4|Described|p316, p316 Fig. 1, p317 Fig. 2|Late Ordovician|Middle Ordovician|Includes: Cargo Volcanics, Walli Volcanics, Fairbridge Volcanics. Geological Province: Molong Volcanic Belt. Consists of volcanic/volcaniclastic successions.||||||07-FEB-11
29516|Kenilworth Group|63290|5|Briefly described|p400 Fig. 5(b)|Ordovician|Ordovician|Geological Province: Molong Volcanic Belt. Consists of volcanics and volcaniclastics.||||||
29516|Kenilworth Group|64826|5|Briefly described|p1040 Tb. 1|Ordovician|Ordovician|Contains Fairbridge Volcanics and Cooming and Triangle Formations.||||||04-MAR-09
29516|Kenilworth Group|67322|5|Briefly described|p22, p39|Sandbian|Darriwilian|Obsolete. Of Pogson, in Pogson and Watkins (1998): now subsumed within the Cabonne Group as a result of reassessment of stratigraphic relationships on the Dubbo 1:250 000 sheet (Meakin and Morgan 1999) and Goulburn 1:250 000 sheet (Thomas et al. in press).|||||Mostly volcanic and volcaniclastic units.|22-FEB-18
29516|Kenilworth Group|68310|6|Mentioned|p237|||Cowra-Canowindra region.||||||
29516|Kenilworth Group|68592|6|Mentioned|p378|Middle Ordovician|Middle Ordovician|Bathurst 1:250 000 sheet (Pogson and Watkins, 1998). Included Kenyu Formation, Walli and Fairbridge Volcanics and was overlain by Barrajin Group. Pogson et al.(2012) here recommend discontinuation of Kenilworth and Barrajin Groups, and place Kenyu Formation in the Cabonne Group.||||||
25969|Kenmure Group|35287|6|Mentioned|p6|||||||||
25969|Kenmure Group|39618|2|Defined|p91|Early Devonian|Early Devonian|||||||
25969|Kenmure Group|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25969|Kenmure Group|41528|6|Mentioned|p49|||See also P75||||||
25969|Kenmure Group|42566|6|Mentioned|Fig.3 P6|||||||||
25969|Kenmure Group|46900|6|Mentioned|p16|||||||||
31360|Kennedy Group (NSW)|41630|6|Mentioned|p13|||Mineral deposit category of Andrews (1922), Broken Hill area.||||||
29223|Kennedy Range Adamellite|36443|5|Briefly described|map legend|Pridolian|Pridolian|Of Coodravale I-type Suite. Of Young Batholith. Intrusive. Adamellite, granite, aplite. I-type. BMR map code: Syk.||||||
29223|Kennedy Range Adamellite|39660|6|Mentioned|p450|||||||||
29223|Kennedy Range Adamellite|40328|4|Described|p207|||||||||
29223|Kennedy Range Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah1||||||
29223|Kennedy Range Adamellite|45147|2|Defined|M244|Late Silurian|Late Silurian|Prob.Late Silurian||||||
29223|Kennedy Range Adamellite|60078|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
26660|Kentucky Diorite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Diorite and minor biotite gabbro.||||||21-DEC-04
26660|Kentucky Diorite|24366|6|Mentioned|p10 Fig. 8|||||||||
26660|Kentucky Diorite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
26660|Kentucky Diorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26660|Kentucky Diorite|41990|6|Mentioned|p10|||||||||
26660|Kentucky Diorite|43091|5|Briefly described|Map legend|||||||||
26660|Kentucky Diorite|62757|6|Mentioned|p13 Fig. 5, p16 Fig.6|||Granitoid of the Uralla Supersuite.||||||07-FEB-11
26660|Kentucky Diorite|68111|5|Briefly described|p968 Tb.1|Anisian|Induan||252 - 245 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
26660|Kentucky Diorite|71628|5|Briefly described|p8: 49, 66|||Binns et al. (1967). Originally Kentucky Ponds Diorite (Flood, 1971 unpublished). Now included in the herein-redefined Kentucky Quartz Diorite.|||||Mafic diorite.|
25116|Kentucky Ponds diorite|31140|6|Mentioned|Fig. 1|||Refers Flood (1971, unpubl.)||||||
30925|Kewell Creek Tuff Member|43417|14|Not recorded|Map Legend||Early Carboniferous|||||||
30925|Kewell Creek Tuff Member|62095|6|Mentioned|p282 Appdx.|||Formerly of Manser's (1967, 1968) Rossmore Formation. Superseded by Kewell Creek Volcanic Member.||||||31-JAN-08
67878|Kewell Creek Volcanics|68003|5|Briefly described|p136.|Carboniferous|Carboniferous|Tamworth Belt (South), New England Fold Belt.||Unit in Seaham Formation.|||Rhyolitic ignimbrites, flows, agglomerate and resedimented rhyolitic siltstone, sandstone and conglomerate.|
25118|Khancoban granite|34221|6|Mentioned|p11|||||||||
25118|Khancoban granite|34222|6|Mentioned|Table 1|||See also PP149,152 etc||||||
37006|Khantoun Tonalite|44450|6|Mentioned|p98|||Geological Province: New England Fold Belt.||||||
28269|Khatown Tonalite|30911|6|Mentioned|Map legend|Permian|Permian|Misspelling of Khartoun Tonalite? Comment added 1993.||||||
74783|Kia-Ora Syenogranite|61789|4|Described|p304, p311-312|Early Triassic|Early Triassic|Small stocks intrude Undercliffe Falls Adamellite. Medium-grained, mildly porphyritic syenogranite. See p311-312 for detailed information.||||||
74783|Kia-Ora Syenogranite|71628|5|Briefly described|p16: 8|||Sivell and Passmore (1999) after unpublished work by Passmore (1998). Previously part of Undercliffe Falls Monzogranite. Renamed (this study) as a ""Phase"" of Cullendore Syenogranite.",,|||||Medium-grained, mildly porphyritic syenogranite.|
74784|Kia-ora Syenogranite|61790|6|Mentioned|p318, p320, p321|||Variation on Kia-Ora Syenogranite & possibly Kiaora Adamellite.||||||
31084|Kiama tuff|43477|14|Not recorded|p41|||||||||
31085|Kiama tuff member|43477|14|Not recorded|p19||Permian|Part of Broughton tuff. (Gerringong Volcanics)||||||
25120|Kiandra Beds""|45147|6|Mentioned|M20|||||||||
31049|Kiandra andesites|44970|14|Not recorded|p82||Early Ordovician|(Middle Ordovician)||||||
22092|Kianga Basalt|22815|2|Defined|p15|Late Cambrian|Middle Cambrian|new name.||||||
22092|Kianga Basalt|22857|4|Described|p135, p432 App. 1 Tb. A1.5.|Late Cambrian|Middle Cambrian|Of the Wagonga Group. Massive igneous rocks, pyroclastics with pillow lavas, volcanic breccia; limestone blocks. Overlies Narooma Chert. Max. thickness: 500m.||||||
22092|Kianga Basalt|23245|6|Mentioned|p135|||||||||
22092|Kianga Basalt|43233|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|of Wagonga Group.||||||
22092|Kianga Basalt|44093|5|Briefly described|p225 App. 1|Ordovician|Cambrian|Of the Wagonga Group. Geological Province: Lachlan Fold Belt.||||||
22092|Kianga Basalt|60902|5|Briefly described|p860, p865-866|||Mapped by Wilson (1968) as a coherent unit at base of Wagonga Fm. and under Narooma Chert and over Bogolo Fm. Now concluded not to be coherent but represents basalt-rich parts of Bogolo Fm lying above Narooma Chert - with major implications.........||||||29-NOV-13
22092|Kianga Basalt|67322|6|Mentioned|p26, p39|Late Cambrian||Glen (1994). Previously interpreted to underlie the Narooma Chert. Now obsolete, reinterpreted as blocks of basalt within the Bogolo Formation overlying the Narooma Chert (Glen et al. 2004).||||||22-FEB-18
22092|Kianga Basalt|70026|5|Briefly described|p40|||Geological province: Lachlan Orogen. No longer current? Glen et al., 2004 suggests that Kianga Basalt is "no longer considered to exist as a mappable unit".||Unit of Wagonga Group.|||Altered basalt.|
22092|Kianga Basalt|70601|5|Briefly described|p45, p47|||Referred to basalts at Batemans Bay and Narooma with oceanic island basalt affinities. Superseded; now included in the Wagonga Group.|||||OIB basalt.|
28644|Kiaora Adamellite""|30787|6|Mentioned|p49|||Differentiation index||||||
82524|Kiaora Leucoadamellite|71628|6|Mentioned|p4: 7, 24, 29, 38, 41, 47, 52, 55, 58|||Binns et al. (1967). Subsequently Kiaora Adamellite.  Now included in Banalasta Monzogranite.||||||
31531|Kikoira Suite|42726|5|Briefly described|map legend||Silurian|||||||
31531|Kikoira Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
31531|Kikoira Suite|44192|5|Briefly described|Map Legend|||||||||
31531|Kikoira Suite|61964|5|Briefly described|p37|||Felsic suite of Chappell et al (1991) and contained Kikoira Granite. Now superseded by Koetong Suite which incorporates the former "Ungarie Suite" and "Kikoira Suite". Written informally as "Kikoira Suite".||||||20-OCT-08
35254|Kilaben Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
73923|Kilburnie Suite|71628|5|Briefly described|p3: 61, 64|||||Hillgrove Supersuite.|Ingleba Leucomonzogranite, Kilburnie Monzogranite.|||
80250|Kildrummie Limestone|67847|6|Mentioned|p29|Pridoli|Ludlow|Age constrained on the basis of coral fossil assemblage (De Deckker, 1976). Alternative age of Wenlock-Ludlow derived from conodont fossil assemblage (Simpson, 1995)||||Equivalent to the Alton Limestone Member.||
31709|Kildrummie Limestone Member|22857|4|Described|p472 App.1 Tb.A1.6|Pridoli|Ludlovian|Of Campbells Formation (Mumbil Group). Fossiliferous limestone, feldspathic arenite, minor conglomerate, slate. Max. thickness: 300m. Geological Province: Hill End Trough and Capertee Rise.||||||
31709|Kildrummie Limestone Member|23214|4|Described|p144|Ludlow|Ludlow|Of Campbells Formation.  Formerly named Kildrummie Formation and Kildrummie Group.||||||
31709|Kildrummie Limestone Member|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Campbells Formation (Mumbil Group).||||||11-JUN-08
32520|Kildrummie Member|43639|5|Briefly described|Map Legend|Silurian|Silurian|Of Campbells Formation.||||||11-JUN-08
32520|Kildrummie Member|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Of the Mumbil Group. See also p215 Appendix 1. Geological Province: Lachlan Fold Belt.||||||
27448|Killimicat Adamellites|29994|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
30926|Kiloran Conglomerate Member|43417|14|Not recorded|Map Legend||Late Carboniferous|||||||
28312|Kimberley Park Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28312|Kimberley Park Adamellite|41348|5|Briefly described|Map legend|Early Paleozoic||Of the Hillgrove Plutonic Suite.||||||07-NOV-08
28312|Kimberley Park Adamellite|71628|6|Mentioned|p3:67|||Binns et al. (1967).||||||
68141|Kimbriki Limestone|44093|5|Briefly described|p67 Fig. 6.6|Permian|Permian|Geological Province: New England Fold Belt.||||||
25123|Kimo Gabbro|42726|5|Briefly described|map legend|||Variation on Kimo Diorite.||||||
34824|Kin Gunnia Calc-Silicate Member|22960|5|Briefly described|p91||Paleoproterozoic|Misspelling of the King Gunnia Calc-Silicate Member.||||||10-SEP-19
70500|Kindalyn Member|62095|5|Briefly described|p251|||Of the Merlewood Formation. Geological Province: Werrie block/Tamworth Belt.||||||
70500|Kindalyn Member|65902|6|Mentioned|p195 Fig.2 |Visean|Visean|Of Merlewood Formation. Misspelling of Kyndalyn Member. See p200. See also Kyndallyn Member Fig. 7.||||||
82760|Kindee Creek Suite|71628|5|Briefly described|p17:31|||||Carrai Supersuite.|Kindee Creek Tonalite.|||
80786|Kindee Creek tonalite|69639|6|Mentioned|p3, p8, p223-p224|Triassic|Triassic|New England Orogen.|227.3 +/- 1.3 Ma (Chisholm et al., 2014)|||||
81790|Kindee Creek tonalite''|69323|4|Described|p3,55-60,71, 76|Triassic|Triassic|Geological province: New England Orogen. Centred on a large diffuse porphyry-like polymetallic system, and is also centred on the Hillview thermal high, identified by biotite isograd conditions (Daigle, 1993). Previously assumed to be Triassic in age (Daigle, 1993; Roberts et al., 1995). SHRIMP U-Pb zircon geochronology of GA 2121505 (porphyritic tonalite) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 227.3+\-1.3 Ma. This age indicate that this tonalite was part of a flush of c. 230 Ma plutonic magmatism in the New England Orogen with Yarrahappini Adamellite and Valla Granite.|227.3+\-1.3 Ma (SHRIMP U-Pb; this study)|||Intrudes into Nevann Siltstone. Broadly coeval (and comagmatic?) with Yarrahappini Adamellite and Valla Granite.|Undifferentiated porphyry, leuocogranite and granodiorite.|03-DEC-19
33994|King Gunnia Calc-Silicates|22575|6|Mentioned|p179 Fig.2|||of the Paragon Group, Broken Hill Block||||||
35566|King Gunnia Calc-silicate Member|22857|5|Briefly described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group). Max. thickness: 50m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
35566|King Gunnia Calc-silicate Member|23248|5|Briefly described|Fig2p169|||||||||
35566|King Gunnia Calc-silicate Member|60485|5|Briefly described|p28 Fig. 2|||Of the Cartwrights Creek Metasediments (Paragon Group).  Geological Province: Broken Hill Domain.||||||03-MAR-05
35566|King Gunnia Calc-silicate Member|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Paragon Group.||||
35566|King Gunnia Calc-silicate Member|63102|5|Briefly described|p13,59|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Paragon Group.||||
35566|King Gunnia Calc-silicate Member|70405|6|Mentioned|P30|||||||||
29949|King Gunnia Calcsilicate Member|23223|5|Briefly described|p46|||of Cartwright Creek Metasediments.||||||
29949|King Gunnia Calcsilicate Member|43052|6|Mentioned|Fig.4.22|||Misspelling of King Gunnia Calc-Silicate Member.||||||
82763|Kings Plain Granite|71628|6|Mentioned|p10: 1|||Included in the Boxwell Suite by Blevin (unpublished). Renamed the Kings Plains Granodiorite in this study.||||||
82762|Kings Plains Suite|71628|5|Briefly described|p10:11|Late Permian|Late Permian|||Boxwell Supersuite.|Kings Plains Granodiorite.|||
41621|Kingsfield Beds""|44244|6|Mentioned|p21|||Superseded by Kingsfield Formation.||||||
77150|Kingsfield beds|68003|5|Briefly described|p32 Fig.3-h. |Tournaisian|Famennian|Tamworth Belt (South); New England Fold Belt.||||Is overlain by Dangarfield Formation.||
37189|Kingsgate Leucogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Very coarse-grained, leucocratic, equigranular pinkish-green biotite granite.  An I-type granitoid.||||||20-DEC-04
37189|Kingsgate Leucogranite|23812|4|Described|p14, p24, p105|Late Permian|Late Permian|Age: 246-243Ma (Rb-Sr).||||||
37189|Kingsgate Leucogranite|23859|6|Mentioned|p933|||Geological Province: New England Fold Belt.||||||
37189|Kingsgate Leucogranite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Biotite granite.||||||
37189|Kingsgate Leucogranite|61793|5|Briefly described|p341|||Intrudes Emmaville Volcanics in the south. Geological Province: New England Fold Belt.||||||07-FEB-11
37189|Kingsgate Leucogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||246 - 243 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
37189|Kingsgate Leucogranite|69639|4|Described|p1, p5, p8-p9, p15-p19|Lopingian|Lopingian|New England Orogen. Molybdenum-bismuth mineralisation is noted. Mistakenly referred to as the Kingsgate Monzogranite on p10. Petrographically similar to the Dhandara Creek Leucogranite. Sample locality, petrography, and geochronology is described. See also p26, p94, p217-p218, p221.|254.4 +/- 1.4 Ma (SHRIMP)|Oban Suite||Intrudes the Mount Mitchell Monzogranite, the Wandsworth Volcanic Group and the Wards Mistake Monzogranite.|Coarse-grained, massive, alkali feldspar-rich granite.|
37189|Kingsgate Leucogranite|71628|6|Mentioned|p14: 7; p15:12|||Weber et al. (1978). Renamed in this study the Kingsgate Syenogranite based on modal analyses, although the northernmost body as described by Henley et al. (2001) is excluded and herein named the Deepwater Syenogranite.||||||
69451|Kingsmill's Peak Andesite|68003|5|Briefly described|p135.|Carboniferous|Carboniferous|Tamworth Belt south, New England Fold Belt.|||||Pyroxene andesite.|
69451|Kingsmill's Peak Andesite|68005|5|Briefly described|p56, p142.|Carboniferous|Carboniferous|Also spelt as Kingsmill's Peek Andesite on p.142. [Both wrong; formal name is Kingsmill Peak Andesite Member].||Unit in Merlewood Formation.|||Pyroxene andesite.|
77151|Kingsmills Peak andesite|68003|5|Briefly described|p135.|Carboniferous|Carboniferous|New England Fold Belt.|||||Intrusive, porphyritic pyroxene andesite. Contains rafted Coepolly Conglomerate lenses.|
24612|Kirribilli beds|22857|4|Described|p418 App.1 Tb. A1.5|Early Silurian|Late Ordovician|Shale, slate and sandstone; abundant quartz veins.||||||
24612|Kirribilli beds|40891|2|Defined|p13|||No internal evidence for age||||||
24612|Kirribilli beds|42489|5|Briefly described|Map legend|Llandovery|Darriwilian|||||||
24612|Kirribilli beds|43263|6|Mentioned|Map Legend||Ordovician|||||||
24612|Kirribilli beds|46522|2|Defined|p53|||No internal evidence for age||||||
24612|Kirribilli beds|46524|6|Mentioned|p121|||||||||
24612|Kirribilli beds|46525|6|Mentioned|Fig.1 P143|||||||||
24612|Kirribilli beds|46528|5|Briefly described|Map legend|Late Ordovician?|Early Silurian?|||||||
70620|Koeris metabasalts|62373|6|Mentioned|p510 Fig.5, p516|||Not intended as a formal name - related to the suite of metabasite groups in the Curnamona Province.||||||
69719|Koetong supersuite|24222|6|Mentioned|p4|||Informal - see Koetong Supersuite.   Geological Province: Lachlan Fold Belt.||||||
76065|Kohinoor Formation|66197|5|Briefly described|p631 Fig.3c|||Canberra-Yass and Ngunawal Basins. Shallow marine clastics. In the Hoskinstown Group. Underlies the Carwoola or Captains Flat Formations; overlies the Copper Creek Shale.||||||13-MAR-12
32631|Kohinoor Volcanics Formation|46568|2|Defined|p.424,425||Silurian|(I55-16/Michelago).||||||
31596|Koo-rilla Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31596|Koo-rilla Suite|68592|6|Mentioned|p1611|Devonian|Devonian|Included in the Marulan Batholith by Chappell et al. (1991).||||||
31596|Koo-rilla Suite|70661|6|Mentioned|p77,p87|||Discontinued suite. ||||||
73931|Kookabookra Suite|71628|5|Briefly described|p3: 72|||||Hillgrove Supersuite.|Kookabookra Monzogranite.|||
24340|Koolambah Adamellite|36413|2|Defined|p95|Devonian|Devonian|||||||
24340|Koolambah Adamellite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Michelago Igneous Complex. Hornblende-biotite adamellite. GSNSW map code: gck.||||||
24340|Koolambah Adamellite|39626|6|Mentioned|p275|||||||||
24340|Koolambah Adamellite|40328|4|Described|p208|||||||||
39355|Koolanook Sandstone|24118|5|Briefly described|p3|||||||||
78269|Koonaburra Creek Quartzite Member|67562|6|Mentioned|p98 Fig.5, p99|||~ 75m thick. Deposited by SW-flowing streams from E of the Koonenberry Fault.||Basal unit of Mount Daubeny Formation.||||23-JAN-17
70154|Koonburra Quartzite|23336|6|Mentioned|p23|||Abbreviation of the full name Koonburra Creek Quartzite Member, used in Excursion schedule details.||||||
70154|Koonburra Quartzite|66623|6|Mentioned|p185.|||Named by Neef et al. (1996). Formerly the Koonburra Creek Quartzite (Neef and Bottrill (1991); formally named the Koonburra Creek Quartzite Member in this study.||||||
70155|Koonburra Quartzite Member|23336|5|Briefly described|p23-24|||Abbreviation of the full name Koonburra Creek Quartzite Member used in Excursion schedule details.  Unconformable on Ponto Beds.||||||
35625|Koonenberry beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group). Strongly magnetic package: basalt, dolerite, magnetic and non-magnetic phyllite, thin, fine-grained quartz-magnetite horizons.||||||26-NOV-08
35625|Koonenberry beds|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Palgamurtie Subgroup. Strongly magnetic package within Ponto Group; basalt, dolerite, magnetic and non-magnetic phyllite, thin, fine-grained quartz-magnetite horizons.||||||
35625|Koonenberry beds|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Palgamurtie Subgroup. Strongly magnetic package within Ponto beds; basalt, dolerite, magnetic and non-magnetic phyllite, thin, fine-grained quartz-magnetite horizons.||||||
35625|Koonenberry beds|66623|6|Mentioned|p92.|||Named by Stevens et al. (2000). Formerly part of Wonominta beds (Warris 1967). Subsequently redefined as Koonenberry Formation (this study).||||||
35625|Koonenberry beds|66929|5|Briefly described|Map legend|||Strongly magnetic package within Ponto Group.||Unit in Palgamurtie Subgroup.|||Basalt, dolerite, magnetic and non-magnetic phyllite; thin, fine-grained quartz-magnetite horizons.|
35625|Koonenberry beds|66933|5|Briefly described|Map legend|||Strongly magnetic package.||Unit in Palgamurtie Subgroup.|||Basalt, dolerite, magnetic and non-magnetic phyllite, thin fine-grained quartz-magnetite horizons.|
28653|Koorainghat Beds|29990|6|Mentioned|Map legend|Devonian|Devonian|||||||11-JAN-10
28653|Koorainghat Beds|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28653|Koorainghat Beds|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28653|Koorainghat Beds|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
37303|Koorigal Dacite|24010|6|Mentioned|p381|||||||||
69995|Kooringal Andesite|61767|6|Mentioned|p78|||Geological Province: Tamworth Belt.||||||
38981|Kooringal Dacite|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Of Caroda Formation.  Geological Province: New England Orogen.||||||
38981|Kooringal Dacite|24603|6|Mentioned|p895 Fig. 16|||Geological Province: Tamworth Belt.||||||
35257|Kooroora Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
26669|Kopje Beds|32088|6|Mentioned|p2|||||||||
26669|Kopje Beds|34057|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
26669|Kopje Beds|42467|5|Briefly described|Map Legend|||||||||
26669|Kopje Beds|43387|14|Not recorded|Map Legend|||||||||
26669|Kopje Beds|43398|14|Not recorded|Map Legend|Early Devonian|Late Silurian|Lower part of Barrow Range Beds (Siluro-Dev  - L.Dev)||||||
27452|Kopyje Beds|29987|6|Mentioned|p19|||||||||
27452|Kopyje Beds|31161|5|Briefly described|PA3|||||||||
27452|Kopyje Beds|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
27452|Kopyje Beds|33004|6|Mentioned|p171|||||||||
27452|Kopyje Beds|33121|6|Mentioned|p90|||Correlated with lower Amphitheatre Beds||||||
27452|Kopyje Beds|37727|5|Briefly described|p67|||||||||
27452|Kopyje Beds|39618|6|Mentioned|Table 2|||||||||
27452|Kopyje Beds|42566|6|Mentioned|Fig.3 P6|||||||||
27452|Kopyje Beds|67416|6|Mentioned|p83|Devonian|Silurian|Brunker (1969, in Pogson, 1991). Upgraded to Kopyje Group by Pogson and Felton (1978, in Pogson, 1991).||||||
27452|Kopyje Beds|70941|6|Mentioned|p79, p85|||Replaced by the Baledmund Formation.||||||
38336|Koreelah Conglomerate|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Gatton Sandstone.  Maximum thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
38336|Koreelah Conglomerate|60281|5|Briefly described|Fig.18 Appendix 1|Early Jurassic|Early Jurassic|Of the Gatton Sandstone. Pebble-cobble conglomerate, sandstone.  Max. thickness: 50m.  Geological Province: Clarence-Moreton Basin.||||||
38336|Koreelah Conglomerate|69297|5|Briefly described|p487 fig 5.38|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Up to 250m thick.||Gatton Sandstone||Overlies the Calamia Member.|Pebble-cobble conglomerate and sandstone.|
38336|Koreelah Conglomerate|69594|5|Briefly described|p544|||Clarence-Moreton Basin (QLD only). Mainly Texas Subprovince. Exposed in a SE-NW line just west of Warwick. Derived from local basement. Appears as Koreelah Conglomerate; [the rank of Member is conspicuous by its absence].||Gatton Sandstone.|||Pebble and cobble conglomerate with fossil wood often abundant.|
82764|Koreelah Creek Suite|71628|6|Mentioned|p19:91||||||Koreelah Creek Granodiorite.|||
25132|Koreelan Creek Granodiorite|23799|5|Briefly described|p117|||Of Bruxner Suite (Clarence River Supersuite).||||||
25132|Koreelan Creek Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
25132|Koreelan Creek Granodiorite|33476|6|Mentioned|p22|||||||||
25132|Koreelan Creek Granodiorite|33480|6|Mentioned|p240|||Refers age dating||||||
25132|Koreelan Creek Granodiorite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
25132|Koreelan Creek Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
25132|Koreelan Creek Granodiorite|39627|6|Mentioned|Appendix|||||||||
25132|Koreelan Creek Granodiorite|40508|6|Mentioned|p63|||||||||
25132|Koreelan Creek Granodiorite|43008|5|Briefly described|map legend|||||||||
25132|Koreelan Creek Granodiorite|68008|6|Mentioned|p333|||Geochemistry mentioned.||||||
25132|Koreelan Creek Granodiorite|68111|5|Briefly described|p968 Tb.1|Olenekian|Induan|Ar-Ar (hornblende) geochronology by Bryant et al. 1997).|250.5 +/- 1.4 Ma|||||21-OCT-14
25132|Koreelan Creek Granodiorite|69639|4|Described|p2, p6, p8, p169-p174, p176, p223, p239|Anisian|Anisian|New England Orogen. Previously believed to be intruded by the Rivertree Granite, but the new magmatic crystallisation age does not support such a relationship. Sample locality, petrography, and geochronology is described. Formerly of the Bruxner Suite (Clarence River Supersuite) . Mistakenly referred to as the Koreelan Creek Granite on p176.|246.3 +/- 1.4 Ma (SHRIMP, magmatic crys.)|Koreelan Creek Suite||Intruded by the Main Camp Creek Gabbro and the Rivertree Granite. Intrudes the Emu Creek Formation and the Razorback Creek Mudstone. Faulted against the Stanthorpe Granite.|Massive, relatively equigranular, medium-grained, hornblende-biotite granodiorite.|
25132|Koreelan Creek Granodiorite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
25132|Koreelan Creek Granodiorite|70217|5|Briefly described|p73 tbl 14.1|Olenekian|Induan|New England Orogen. A SHRIMP U-Pb age of 246.3 +/- 1.4 Ma from Chisholm et al (2014b) is also given. |250.5 +/- 1.4 Ma (Ar/Ar Bryant et al. 1997a)|Clarence River Supersuite||||
25132|Koreelan Creek Granodiorite|70876|5|Briefly described|p78-p80|Triassic|Early Triassic|SHRIMP date is derived from Chisholm et al, 2014c. Formerly part of the Bruxner Suite, dating by Chisholm et al (2014c) and the new date for the Bruxner Monzogranite (this volume) supports removal of this unit from the Bruxner suite.|246.3 +/- 1.4 Ma (SHRIMP U-Pb zircon)|||||
25132|Koreelan Creek Granodiorite|71628|5|Briefly described|p9: 1; p16: 26, 30; p19: 89|||Flinter et al. (1972). Renamed Koreelah Creek Granodiorite (Brown et al., 2001) in this study to reflect the correct spelling of the watercourse. Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). The lithology is not included in the list of constituents of the Suite on p9-1.||Koreelan Creek Suite.||Is intruded by Rivertree Syenogranite.||
25132|Koreelan Creek Granodiorite|72528|5|Briefly described|p2, p110.|Middle Triassic|Middle Triassic|Also mentioned as Koreelan Creek pluton p90. Indistinguishable from Cullens Creek Granite. Not related to Koreelah Conglomerate Member.|246.3+/-1.4 Ma|||Cut by epithermal-like polymetallic veins.|Includes granodiorite.|
26670|Koreelan Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
42042|Kosciusko Metamorphics""|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Monaro Slope and Basin. Geological Province: Lachlan Pre-Cratonic Province.  Leucocratic gneiss and phyllite.||||||09-NOV-04
70355|Koukandowie Sandstone "Member"|60993|6|Mentioned|p18|||Informal version of McElroy's Koukandowie Sandstone Member (1963) as part of his Marburg "Formation". Now superseded by Koukandowie Formation (Marburg Subgroup). ||||||
27177|Kowmung Volcaniclastics|22678|3|Fully described|Fig1p712,723,725|Middle Devonian|Early Devonian|Described and formally defined by Powell and Fergusson (1979) and Cas et al. (1981).||||||
27177|Kowmung Volcaniclastics|22768|5|Briefly described|p179|Middle Devonian|Early Devonian|||||||
27177|Kowmung Volcaniclastics|22857|4|Described|p179, p478 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Part of the Bindook Porphyry Complex. Disconformably overlies the Taralga Group. Max. thickness: 825m. Geological Province: Murruin Basin.||||||
27177|Kowmung Volcaniclastics|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
27177|Kowmung Volcaniclastics|35759|2|Defined|p42|Middle Devonian|Early Devonian|Lower to Middle? Devonian||||||
27177|Kowmung Volcaniclastics|37490|4|Described|p271|||||||||
27177|Kowmung Volcaniclastics|39568|5|Briefly described|p87|||||||||
27177|Kowmung Volcaniclastics|39626|6|Mentioned|p275|||||||||
27177|Kowmung Volcaniclastics|41413|6|Mentioned|p333|||||||||
27177|Kowmung Volcaniclastics|42712|4|Described|8; Table 1 p14.|Early Devonian|Late Silurian|Within Crudine Group. Unconformable between Hollanders Fm below and Lambie Group above.||||||
27177|Kowmung Volcaniclastics|42820|6|Mentioned|p15|||||||||
27177|Kowmung Volcaniclastics|68592|4|Described|p725, p742, p884-91, p1147|||Superseded. Of Powell and Fergusson (1979) and Cas et al. (1981). Now redefined as Kowmung Formation overlain by Murruin Formation. The interval of Kowmung Volcaniclastics (Powell and Fergusson 1979) with (in ascending order) informal members of 'Quartzo-Feldspathic Sandstone Member', 'Silicic Breccia Member', 'Boulder Conglomerate Member' and 'Lenticle Tuff Member' (Cas et al. 1981). See Kowmung Formation.||||Is conformably overlain by Murruin Formation.|Thick sequence of massive, very thick-bedded, medium to coarse-grained, quartzofeldspathic sandstone interbedded with siltstone and mudstone; minor rhyolite and rhyolite breccia occur.|
31985|Kowmung Volcanoclastics|42712|6|Mentioned|8|Early Devonian|Late Silurian|Misspelling of Kowmung Volcaniclasts||||||
38476|Kuark metamorphic complex|24133|5|Briefly described|p20 Fig. 8|Silurian|Silurian|Informal.  Geological Province: Lachlan Fold Belt.||||||
38476|Kuark metamorphic complex|60412|6|Mentioned|p233|||Lachlan Fold Belt.||||||
38476|Kuark metamorphic complex|60904|6|Mentioned|p794|||Informal - see Kuark Metamorphic Complex.||||||
30834|Kullatine Beds|43385|14|Not recorded|p167||Carboniferous|||||||
40222|Kullatine Formation, upper|38685|6|Mentioned|p27|||Geological Province: New England Fold Belt||||||
31242|Kullatine Group|43491|14|Not recorded|pVI/10|||||||||
30835|Kullatine group|43385|14|Not recorded|p167||Carboniferous|||||||
25136|Kumbarilla Beds|22757|5|Briefly described|p6|||Also Table6,p11. Surat Basin.||||||
25136|Kumbarilla Beds|23843|5|Briefly described|p456 Table 1|Cretaceous|Jurassic|Geological Province: Moreton Basin.  Maximum thickness: 760m.||||||
25136|Kumbarilla Beds|30692|6|Mentioned|Map legend|Early Cretaceous|Middle Jurassic|Lower Cretaceous to Middle Jurassic||||||
25136|Kumbarilla Beds|30696|4|Described|Table 4|||Jurassic to Lower Cretaceous||||||
25136|Kumbarilla Beds|30698|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Lower Cretaceous||||||
25136|Kumbarilla Beds|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
25136|Kumbarilla Beds|30702|2|Defined|p48|Early Cretaceous|Middle Jurassic|Middle Jurassic-Lower Cretaceous||||||
25136|Kumbarilla Beds|30911|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
25136|Kumbarilla Beds|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
25136|Kumbarilla Beds|31086|6|Mentioned|p37|||Faunas P37.||||||
25136|Kumbarilla Beds|31208|6|Mentioned|Table 1|||||||||
25136|Kumbarilla Beds|32193|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jur.-L.Cret.||||||
25136|Kumbarilla Beds|32276|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Middle Jurassic - Lower Cretaceous||||||
25136|Kumbarilla Beds|32671|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
25136|Kumbarilla Beds|32797|4|Described|Table 4|||Jur.-L.Cret.||||||
25136|Kumbarilla Beds|33091|5|Briefly described|p6|||Refers Exon & Vine (1970)||||||
25136|Kumbarilla Beds|33367|6|Mentioned|p23|||Refers Exon & Vine (1970).||||||
25136|Kumbarilla Beds|33371|6|Mentioned|p58|||Includes Springbok Sst.||||||
25136|Kumbarilla Beds|35937|6|Mentioned|Fig.5|||||||||
25136|Kumbarilla Beds|36570|6|Mentioned|p46|||||||||
25136|Kumbarilla Beds|37117|6|Mentioned|p312|||||||||
25136|Kumbarilla Beds|37122|5|Briefly described|Table 1|||||||||
25136|Kumbarilla Beds|37252|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
25136|Kumbarilla Beds|37992|6|Mentioned|p166|||||||||
25136|Kumbarilla Beds|37994|5|Briefly described|p146|||||||||
25136|Kumbarilla Beds|39445|5|Briefly described|Table 10|||||||||
25136|Kumbarilla Beds|43000|5|Briefly described|Fig.5,p112|||||||||
25136|Kumbarilla Beds|45110|4|Described|p110|||See also P105.||||||
25136|Kumbarilla Beds|60281|6|Mentioned|p27|||Probably replaced by Kumbarilla beds?||||||
25136|Kumbarilla Beds|73200|5|Briefly described|p532 Fig.1, Fig.2, p533, p540-542|Jurassic|Jurassic|Generic term for intensely weathered and indistinguishable Jurassic Springbook Sandstone and Westbourne Formation (Scott et al., 2007). Exposed along the western banks of the Condamine River valley.||||Overlies the Walloon Coal Measures. Underlies the Condamine Alluvium.|Intensely weathered sedimentary rocks including sandstones.|
30917|Kurnell Sand|43416|14|Not recorded|p8,12|||See also Kurnell Sands on p9||||||
81791|Kurrajong Park Leucogranite|69323|5|Briefly described|p27-28,71|||Geological province: New England Orogen.||||Intrudes into, and hornfelses the 'Kurrajong Park volcanics'.||
82765|Kurrajong Park Volcanics|71628|5|Briefly described|p19: 77|||||Wandsworth Volcanic Group.||Is possibly intruded by Honeysuckle Creek Leucosyenogranite.||
81792|Kurrajong Park volcanics''|69323|5|Briefly described|p1,3,13,21,27-28,32, 71|Lopingian|Lopingian|Geological province: New England Orogen. SHRIMP U-Pb zircon geochronology of GA 2120076 (dacitic ignimbrite) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 256.3+\-1.5 Ma.|256.3+\-1.5 Ma (SHRIMP U-Pb; this study)|Unit of Wandsworth Volcanic Group.||Intruded and hornfelsed by Kurrajong Park Leucogranite.||03-DEC-19
30836|Kuttung Beds|43385|14|Not recorded|p176|||||||||
30836|Kuttung Beds|43400|14|Not recorded|map opp.p.188||Early Carboniferous|L-M Carboniferous||||||
30836|Kuttung Beds|43874|14|Not recorded|p204|||(H/56-13) no age given||||||
28659|Kuttung Group""|36961|6|Mentioned|Table 1|||||||||
28659|Kuttung Group""|40245|6|Mentioned|Table 2|||||||||
28659|Kuttung Group""|40246|6|Mentioned|Table 1|||||||||
28659|Kuttung Group""|43432|14|Not recorded|p199|||mostly U.Carb||||||
28659|Kuttung Group""|45090|6|Mentioned|p25|||Stratigraphic table||||||
30963|Kuttung beds|43440|14|Not recorded|p40|||||||||
30963|Kuttung beds|44861|14|Not recorded|p190||Late Carboniferous|||||||
31944|Kuttung glacial beds|43872|14|Not recorded|p18|||Zeolitized tuffs.||||||
31216|Kuttung group|43491|14|Not recorded|pVI/2-4||Carboniferous|||||||
31180|Kuttung shales|43491|14|Not recorded|pVII/42||Carboniferous|||||||
31180|Kuttung shales|44861|14|Not recorded|p227||Carboniferous|||||||
32991|Kuttung tillites|44040|14|Not recorded|p27|||||||||
33522|Kuttung volcanics|44834|14|Not recorded|p470|||||||||
33522|Kuttung volcanics|48600|14|Not recorded|p19|||||||||
25140|Kuttung"" Volcanics|34130|6|Mentioned|p178|||||||||
34638|Kybeyan Complex""|22815|6|Mentioned|p79|||Osolete. Renamed Myocum Adamellite.||||||
34640|Kydra Complex""|22815|6|Mentioned|p80|||Probably obsolete. Unit now split up.||||||
27816|Kyeamba Adamellite|23721|5|Briefly described|Map Legend|Silurian|Silurian|||||||
27816|Kyeamba Adamellite|24119|5|Briefly described|p26|Silurian|Silurian|||||||
27816|Kyeamba Adamellite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27816|Kyeamba Adamellite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
27816|Kyeamba Adamellite|40328|4|Described|p208|||||||||
27816|Kyeamba Adamellite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27816|Kyeamba Adamellite|40498|6|Mentioned|Table 5|||||||||
27816|Kyeamba Adamellite|60086|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
68142|Kyemba Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
37385|Kywong volcanics|24040|6|Mentioned|p468 Fig. 1|||Informal name. Geological Province: Manning Basin||||||
74654|Kywong-Gloucester volcanics|24040|6|Mentioned|p468 Fig. 1|||Compound term for informal grouping of the Kywong Volcanics and Gloucester Volcanics in the manning Basin.||||||18-SEP-08
31214|Lacey's Creek sandstone|43477|14|Not recorded|p27,58||Permian|Part of Wollondilly Coal Measures||||||
74614|Lachlan Alluvial Fan|61964|5|Briefly described|p17|||Fluvial deposits from the Lachlan River Valley forming part of the eastern margin of the Murray Basin - formed from radial palaeochannels and modern channels. ||||||
70621|Lady Louise Suite metabasites|62373|6|Mentioned|p511|||Informal - see Lady Louise Suite.||||||
32269|Lady Northcott's Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb31. Should be spelt Lady Northcotts Granodiorite.||||||
70065|Laidlaw Formation""|22857|5|Briefly described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Formerly of Silverdale Formation (Hattons Cornet Group) (Cramsie, Pogson and Baker (1975, 1978). Name now invalid - see Laidlaw Volcanics. Max. thickness: 127.3m. Geological Province: Canberra-Yass Shelf. ||||||
79208|Laidlaw Porphyry|68592|6|Mentioned|p514|||Mann (1921), for intrusive acid porphyries outcropping around the Laidlaw Trigonometrical Station, 1 km W of Yass. Subsequently Laidlaw Series (Brown, 1940), Laidlaw Formation (Link, 1970), Laidlaw Volcanics (Owen and Wyborn, 1979).||||||
28662|Laidlaw Suite|22768|5|Briefly described|p176|||||||||
28662|Laidlaw Suite|22857|6|Mentioned|p176|||Includes the Deakin and Laidlaw Volcanics.||||||
28662|Laidlaw Suite|24128|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
28662|Laidlaw Suite|41563|6|Mentioned|p512|||||||||
28662|Laidlaw Suite|43158|4|Described|Fig1p2; p3||Late Silurian|Age restricted to short interval in early Ludlovian - control point on geological time scale||||||
28662|Laidlaw Suite|43159|4|Described|Fig2,p4,p6,p9.||Late Silurian|||||||
30770|Laidlaw beds|43344|14|Not recorded|p118|||||||||
30771|Laidlaw tuff|43344|14|Not recorded|p120|||||||||
40726|Laidlaw volcanics|23309|6|Mentioned|p390|||||||||
40370|Laidlaw-Douro Volcanics|24334|5|Briefly described|p49 Tb.1|Pridolian|Llandovery|Age: 410 - 428 Ma.||||||
35031|Laidlow suite|23048|6|Mentioned|p13|||Informal name.||||||
26680|Lake Bathurst Limestone|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
26680|Lake Bathurst Limestone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
39942|Lake Cowal Complex|24263|6|Mentioned|p1387|||||||||
39942|Lake Cowal Complex|24267|6|Mentioned|p1508 Fig.1|||Geological Province: Parkes-Narromine Belt||||||
37288|Lake Cowal Volcanic Complex""|24007|6|Mentioned|p329|||||||||
33987|Lake Cowal Volcanics|22434|6|Mentioned|12|Ordovician|Ordovician|Of Clarke (1990). Geol province Lachlan Fold Belt||||||
33987|Lake Cowal Volcanics|24265|5|Briefly described|p1446||Ashgill|Age: ~440Ma. Geological Province: Lachlan Fold Belt||||||
33987|Lake Cowal Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
38849|Lake Cowal Volcanics""|24417|6|Mentioned|p17|||Of Miles (1993).  Superseded and formalised by Lake Cowal Volcanic Complex.||||||
38850|Lake Cowal volcanic complex""|24417|6|Mentioned|p17|||Of Miles and Brooker (1998).  Now superseded and formalised by Lake Cowal Volcanic Complex.||||||
74615|Lake Cudgelligo Leucite Basalt|61964|6|Mentioned|p145|||Of Stonier (1894). This, together with Scott's "Weja Hill Leucitite" (2000b) an outlier of the main body, are now renamed Tullibigeal Leucitite. Written as "Lake Cudgelligo Leucite Basalt". ||||||
70066|Lake Frome Group, lower|22857|6|Mentioned|p92|||Informal - see Lake Frome Group.||||||
31272|Lambian Stage|43512|14|Not recorded|p75|||(or Upper Devonian)||||||
31248|Lambie Beds|45015|6|Mentioned|p59|Devonian|Devonian|Unit in NSW.  Probably same age as Willaraddie Formation, W.A.||||||01-JUN-06
30641|Lambie Sandstone|43316|14|Not recorded|p12||Late Devonian|||||||
30653|Lambie Stage|43346|14|Not recorded|p1|||||||||
30653|Lambie Stage|43491|14|Not recorded|pV/15||Late Devonian|||||||
31249|Lambie beds|43491|14|Not recorded|pV/15||Late Devonian|||||||
32897|Lambie series|44081|14|Not recorded|p116|||||||||
74170|Lambs Valley Ignimbrite|61768|6|Mentioned|p83 Fig. 2|||Of Mowbray Formation.||||||06-AUG-08
25150|Lambton Sub-Group|23055|6|Mentioned|Fig11p23|||||||||
25150|Lambton Sub-Group|29922|6|Mentioned|Appendix 4|||||||||
25150|Lambton Sub-Group|29926|6|Mentioned|Fig.3|||||||||
25150|Lambton Sub-Group|29942|4|Described|Fig.2|||||||||
25150|Lambton Sub-Group|33867|6|Mentioned|p11|||||||||
25150|Lambton Sub-Group|34271|6|Mentioned|p12|||||||||
25150|Lambton Sub-Group|34351|3|Fully described|p3411|||See also pp342-343.||||||09-DEC-08
25150|Lambton Sub-Group|34448|5|Briefly described|p433|||Permian||||||
25150|Lambton Sub-Group|35319|6|Mentioned|Table 1|||||||||
25150|Lambton Sub-Group|36933|6|Mentioned|p49|||||||||
25150|Lambton Sub-Group|38656|6|Mentioned|Fig.1.3.11|||P150||||||
25150|Lambton Sub-Group|39292|6|Mentioned|Fig. 6.2|||See also Fig. 6.6||||||
25150|Lambton Sub-Group|39308|6|Mentioned|p467|||||||||
25150|Lambton Sub-Group|41479|6|Mentioned|Fig.2|||||||||
25150|Lambton Sub-Group|42182|6|Mentioned|p298|||||||||
25150|Lambton Sub-Group|43440|14|Not recorded|p34,fig4-3|||||||||
25150|Lambton Sub-Group|43447|4|Described|Table 1,p24,diag.p26|||Of the Newcastle Coal Measures.||||||09-DEC-08
25150|Lambton Sub-Group|45090|6|Mentioned|p220|||U. Tatarian||||||
28665|Lana Formation|22529|6|Mentioned|1|||Junior synonym of Turondale Formation||||||
28665|Lana Formation|24126|6|Mentioned|p228, p234|||Geological Province: Hill End Trough.||||||
28665|Lana Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
28665|Lana Formation|32046|6|Mentioned|p51|||||||||
28665|Lana Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
28665|Lana Formation|40328|3|Fully described|p174|||||||||
28665|Lana Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
28665|Lana Formation|43494|6|Mentioned|p26||Devonian|First mapped by Dickson (1962).  Superseded by Turondale Formation.  Name no longer used?||||||16-MAR-06
29436|Lane's Shaft Coal Member|42966|4|Described|p64|||Misspelling of Lanes Shaft Coal Member. Part of Coorabin Coal Measures.||||||
25152|Lanes Shaft Seam|42182|6|Mentioned|p302|||||||||
69818|Langari Hill Volcanic Suite|63347|2|Defined|p5 Fig. 2, p31|Middle Miocene|Middle Miocene|Includes the Langari Hill Volcanics. Age: 14Ma (K-Ar). Tholeiitic basalt with minor volcaniclastic rocks. See also p7, p14, p19, p22.||||||
41560|Lapstone Structural Complex|50616|6|Mentioned|p273|||A structural term in this context.||||||
25156|Laurel Group|41630|6|Mentioned|p12|||Mineral deposit category of Andrews (1922).||||||
38342|Laurieton granitoid|23812|6|Mentioned|p17 Fig.5|||||||||
70067|Laurieton granitoids|22857|6|Mentioned|p204 Fig. 17.2, p262|Early Triassic|Late Permian|Informal name for rocks within the New England Batholith. See also p243 Fig. 18.4.||||||
30678|Lawrence Greywacke|43345|14|Not recorded|p3 Table 1||Permian|||||||
33936|Lawson Creek Shale|22472|6|Mentioned|p47 Fig.6(e)|||of the Mt. Knowles Group||||||
70343|Laytons Range Conglomerate""|60993|6|Mentioned|p6 Fig. 2|||Informal - see Laytons Range Conglomerate. ||||||
68175|Laytons Range conglomerate|60281|6|Mentioned|p27|||Informal - see Laytons Range Conglomerate.||||||
32259|Leaning Rock Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|glw8||||||
32259|Leaning Rock Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
42275|Leard formation|24313|6|Mentioned|p22|Early Permian|Early Permian|||||||30-NOV-04
25161|Legume Sandstone""|33476|6|Mentioned|p100|||Refers Brunker||||||
27462|Lemington seam|37087|4|Described|p200|||||||||
27462|Lemington seam|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27462|Lemington seam|41604|6|Mentioned|Table 1|||||||||
27462|Lemington seam|44244|6|Mentioned|p240 Fig 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup,  Wittingham Coal Measures).||||||
77269|Lennox seam""|68004|5|Briefly described|p61.|Late Permian|Late Permian|Western Coalfield. Apparently also known as the "Goulburn seam".||Unit in State Mine Creek Formation.||||
79209|Lenticle Tuff Member|68592|6|Mentioned|p884, p1148|||Superseded. The 'Boulder Conglomerate Member' and overlying 'Lenticle Tuff' unit of Cas et al. (1981) are now included in the Murruin Formation (Bindook Group) with the upper part considered as a possible reworked equivalent of the Barrallier Ignimbrite.||||Overlies Boulder Conglomerate Member.||11-SEP-15
68005|Lenticle Tuff""|22815|6|Mentioned|p92|||||||||
83061|Lepidodendron Beds|73181|6|Mentioned|p60|||Of Andrews (1901). Walkom's (1928) Yalwal [palaeobotanic] type locality. [Name use appears casual/informal].||||||
73047|Leucitite Suite|63185|5|Briefly described|p1, p2 Fig. 2|Miocene|Miocene|Not a valid name. Of Johnson (1989). Also known as Condobolin Province (Wellman and McDougall 1974).  North-south trending linear leucitite belt, occurrencing over 90km wide/640km in Lake Cargelligo, Bygalorie, Griffith and Cosgrove area. Age: 15.7+/-0.2||||||12-APR-07
35039|Leucoadamellite Suite|23050|5|Briefly described|p16|||Informal name.||||||
70068|Levy Graywacke Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Of the Yarrimie Formation (Tamworth Group). Possibly misspelt? (graywacke instead of greywacke?). Max. thickness: >270m. ||||||
34179|Lf leucocratic gneiss""|22641|5|Briefly described|p688|Paleoproterozoic|Paleoproterozoic|Age of unit 1650 Ma||||||07-NOV-08
74675|Lf leucocratic gneisses""|64316|5|Briefly described|p533 Fig. 1, p535|||GIVE THIS 'GROUP' STATUS. Name assigned by Geological Survey of NSW for a grouping of felsic gneisses. Example of one of these is the Purnamoota Road Gneiss.||||||07-FEB-11
22191|Lickhole Volcanics|22628|6|Mentioned|fig1p108|||||||||
22191|Lickhole Volcanics|22832|5|Briefly described|p635|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|23309|5|Briefly described|p25 Table 2.1, p28 Tb 2.4|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|23860|5|Briefly described|p947|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|24002|5|Briefly described|p233|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|24004|5|Briefly described|p275 Fig.2|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|24037|6|Mentioned|p425 Fig.2|Cambrian||Geological Province: Lachlan Fold Belt.||||||
22191|Lickhole Volcanics|24098|5|Briefly described|p27 Fig. 2|Late Cambrian|Early Cambrian|Geological Province: Lachlan Fold Belt.||||||19-APR-05
22191|Lickhole Volcanics|24164|6|Mentioned|p15 Fig.8|Cambrian|Neoproterozoic|Ages estimated from figure.|||||Mafic|
22191|Lickhole Volcanics|24576|6|Mentioned|p737|||Geological Province: Lachlan Fold Belt||||||
22191|Lickhole Volcanics|61187|5|Briefly described|p5 Fig.3. |Early Cambrian|Early Cambrian|Tabberabbera Zone, Benambra Terrane. Correlated with Mount Stavely Volcanics (Glenelg Zone), Heathcote Volcanics (Bendigo Zone), Licola and Jamieson Volcanics (Melbourne Zone). Age interpreted from Fig.3.|c.560-c.525 Ma.|||||
22191|Lickhole Volcanics|64616|6|Mentioned|p313 Fig.2|||||||||
22191|Lickhole Volcanics|66196|5|Briefly described|p616|Early Cambrian||||||||
22191|Lickhole Volcanics|68592|6|Mentioned|p279|Cambrian|Cambrian|||||Is overlain by Howqua Chert.||
22191|Lickhole Volcanics|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Tabberabbera Zone, Lachlan Orogen.||||Is overlain by Howqua Chert.||
22191|Lickhole Volcanics|70601|5|Briefly described|p44-45, p47|Early Cambrian|Early Cambrian|Tholeiites from Lickhole Volcanics and Dookie Igneous Complex are correlated.|||Eagles Peak Basalt.|Lower part correlated with Dookie Igneous Complex and lower part of Heathcote Volcanics.|Andesite, boninite and tholeiite volcanics.|
22191|Lickhole Volcanics|70661|6|Mentioned|p14|Cambrian|Cambrian|||||Overlain by Howqua Chert||
22191|Lickhole Volcanics|71069|6|Mentioned|p52|Cambrian|Cambrian|||||Overlain by the Howqua Chert.||
22191|Lickhole Volcanics|71700|6|Mentioned|CD|Cambrian|Cambrian|||||||
22191|Lickhole Volcanics|73059|6|Mentioned|p1053 Fig.2, 1059|Cambrian|Cambrian|||||Is overlain by Howqua Chert.||
72763|Licking Gully granite|61910|5|Briefly described|p152|||Informal - see Licking Gully Granite. Intrudes Hawkins Volcanics.||||||
37405|Licking Hole Limestone Member|23214|6|Mentioned|p133|Silurian||Renamed Anson Formation.||||||06-FEB-09
70103|Liddell Middle Seam|61529|5|Briefly described|p860 Fig. 6d|||Within the Foybrook Formation (Wittingham Coal Measures). Geological Province: Sydney Basin.||||||
68143|Liddell Middle seam|44093|6|Mentioned|p64 Photo 3|||Geological Province: Sydney Basin.||||||
32819|Liddell Sandstone Member|48830|14|Not recorded|p.8,12|||||||||
31087|Liddell sandstone|43477|14|Not recorded|p49||Permian|||||||
26688|Liddell seam|23060|6|Mentioned|5|||Geol province Sydney Basin||||||
26688|Liddell seam|37087|4|Described|p199|||||||||
26688|Liddell seam|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26688|Liddell seam|41604|6|Mentioned|p5|||||||||
26688|Liddell seam|44244|6|Mentioned|p319|||||||||
41625|Liddell seam, Lower|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup, Wittingham Coal Measures).||||||
41626|Liddell seam, Middle|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup, Wittingham Coal Measures).||||||
41628|Liddell seam, Upper|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup, Wittingham Coal Measures).||||||
25165|Lidsdale Seam|34040|6|Mentioned|p385|||||||||
25165|Lidsdale Seam|34605|6|Mentioned|Fig.5.27|||||||||
25165|Lidsdale Seam|37339|6|Mentioned|p14|||||||||
25165|Lidsdale Seam|39232|6|Mentioned|Table 1|||||||||
25165|Lidsdale Seam|42182|6|Mentioned|p300|||||||||
25165|Lidsdale Seam|42648|5|Briefly described|p38|||||||||
25165|Lidsdale Seam|45090|6|Mentioned|p220|||U. Tatarian||||||
30918|Lilberne Beds|23185|6|Mentioned|Fig4p160||Middle Devonian|||||||
30918|Lilberne Beds|43417|4|Described|Map Legend||Middle Devonian|Formerly Tamworth Series, Tamworth Group.||||||
40241|Limbri Group|50014|6|Mentioned|p250|||Geological Province: New England Fold Belt||||||
41065|Limbri Leucomonzogranite|24366|5|Briefly described|p16 Fig. 3|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41065|Limbri Leucomonzogranite|68005|5|Briefly described|pp67-68, p133.|Permian|Permian|Listed on p.133 as a unit in Moonbi Supersuite. Uniform, very high K, Th and U radiometric responses.||Unit in Southern Moonbi Supersuite.|||Medium- to coarse-grained biotite(-muscovite) leucomonzogranite with prominent pink K-feldspar crystals, and minor titanite and magnetite grains.|
41065|Limbri Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 245 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
41065|Limbri Leucomonzogranite|71628|4|Described|p7: 1, 24-27|||Brown (2003) after Chappell and Bryant (1994). Previously the Limbri Leucoadamellite of Binns et al. (1967). Named after the locality of Limbri. Located 26 km NE of Tamworth. Forms a N-trending body ~3 km x 1 to 2 km, centred on Big Billy Mountain. Forms poorly-accessed pavements and tors. Variants with muscovite and garnet are atypical of I-type granites; assignation is uncertain. Limited geochemistry description.|245.4 Ma (Rb-Sr biotite: Shaw and Flood, 1993).|Limbri Suite.||Intrudes 'Sandon Association'.|Medium-grained, inequigranular to equigranular, biotite monzogranite.|
73974|Limbri Suite|71628|6|Mentioned|p7: 26|||||Moonbi Supersuite.||||
72793|Limekiln Creek Siltstone|62740|5|Briefly described|p371|Middle Eocene|Middle Eocene|Of the Nerriga Sub-Group. Lacustrine deposits caused by basalt blockages of Limekiln Creek to form Lake Bungonia.||||||06-FEB-07
27465|Limekiln Group|34059|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27465|Limekiln Group|36413|6|Mentioned|p98|||Misspelling of Limekilns?||||||
37439|Limekilns Creek Shale""|23214|6|Mentioned|p204|||Superseded by Limekilns Formation.||||||
37438|Limekilns Group""|23214|6|Mentioned|p203|||Superseded by Limekilns Formation.||||||
37438|Limekilns Group""|71924|6|Mentioned|p2||Emsian|||||||
37397|Limestone A""|23214|3|Fully described|p111|Wenlock|Llandovery|Informal name for basal unit of Boree Creek Formation. Red coloured thinly bedded limestone / extremely fossiliferous.||||||
37399|Limestone B""|23214|3|Fully described|p111|Wenlock|Llandovery|Informal top unit of Boree Creek Formation. Consists of thin to moderately thick bedded, marly, partly dolomitic limestone.||||||
32188|Lindemans Siltstone|22500|5|Briefly described|p 7  Fig 10|||||||||
35867|Lingula Beds|23336|5|Briefly described|p5|||Of Rade, 1963.||||||21-MAR-06
39404|Links Andesite|24126|6|Mentioned|p185|||||||||
30217|Links Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
35379|Links Volcanics|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
35379|Links Volcanics|23202|6|Mentioned|Fig.1||Ordovician|of Cabonne Group||||||
25168|Lintiss Vale Beds""|34812|6|Mentioned|p15|||Subdivision of Torrowangee Group||||||
25168|Lintiss Vale Beds""|41429|6|Mentioned|p246|||||||||
82547|Linton monzogranite|71628|6|Mentioned|p4:35|||Informal name by Jeon et al. (2012); formalised in this study.||||||
35251|Lisarow Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
39431|Lismore Basalts|24299|5|Briefly described|p178|Tertiary|Tertiary|||||||
39313|Little Broken Hill gabbro|24401|5|Briefly described|p100|Neoproterozoic|Neoproterozoic|Age: 827+/-9Ma. Informal name.||||||
39313|Little Broken Hill gabbro|62664|5|Briefly described|p137, p140, pp150-153.|Neoproterozoic|Neoproterozoic|Written with lower-case g throughout the article. Mafic intrusive suite in eastern Willyama Inlier. Includes gabbro plutons and northwest-trending dykes, interpreted as a magma chamber feeding structurally higher dykes.|827 +/- 9 Ma.(Wingate et al. 1998)||||Includes minor uralitic gabbro plutons.|
39313|Little Broken Hill gabbro|74367|5|Briefly described|p18|Tonian|Tonian|Of Wingate et al. (1998). Shown in quotation marks, implying the name is no longer current.|827+/-9 Ma (Wingate et al., 1998)|Gairdner Dyke Swarm||||
22202|Little Forest Adamellite|23214|6|Mentioned|p166|||Replaced by Little Forest Granite.||||||
34294|Little Forest Adamellite""|22679|6|Mentioned|p 43|||||||||
80302|Little Mountain Formation""|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Mapped in the same unit as Meryula Formation and conglomerates of Brookong Formation and Drysdale Conglomerate Member extending from the Cobar 1:100 000 map sheet area.||Kopyje Group.||||
35265|Little Pelican Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
25996|Little Popong Adamellite|22815|4|Described|p56|Silurian|Silurian|||||||
25996|Little Popong Adamellite|41905|2|Defined|p53|Silurian||Reserved as Little Popong||||||
25996|Little Popong Adamellite|41933|5|Briefly described|Map legend|Late Silurian||||||||
25996|Little Popong Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||of Dalgety Suite.||||||
25996|Little Popong Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab17.||||||
25996|Little Popong Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
31602|Little Redbank Suite|42726|5|Briefly described|map legend||Silurian|||||||
79210|Little Redbank Tonalite|68592|6|Mentioned|p1334|||Yacopetti (1987), after Little Redbank Gully, a tributary of Memunday Creek. Subsequently Little Redbank Granite (Chappell et al., 1991). Their definitions included rocks now assigned to Little Redbank Granodiorite, Willdamar Tonalite and Mulgowrie Granodiorite.||||||
30928|Liverpool Range Basalts|43417|4|Described|Map Legend||Tertiary|||||||
35077|Liverpool Range basalts|23043|6|Mentioned|Map Diagram|Tertiary|Tertiary|||||||
31330|Liverpool Range lavas|43534|14|Not recorded|p394||Miocene|(U.Miocene)||||||
26694|Liverpool Sub-Group|29901|4|Described|Table 1|||||||||
26694|Liverpool Sub-Group|30286|6|Mentioned|p1099|||Stratigraphic Table||||||
26694|Liverpool Sub-Group|32187|5|Briefly described|p6|||||||||
26694|Liverpool Sub-Group|34243|6|Mentioned|p423|||||||||
26694|Liverpool Sub-Group|34305|3|Fully described|p418|||Triassic||||||
26694|Liverpool Sub-Group|35690|6|Mentioned|p13|||Suggest be abandoned.||||||
26694|Liverpool Sub-Group|36220|6|Mentioned|p91|||||||||
26694|Liverpool Sub-Group|36222|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
26694|Liverpool Sub-Group|39293|6|Mentioned|Fig. 8.3|||||||||
26694|Liverpool Sub-Group|39298|6|Mentioned|Fig. 13.2|||||||||
26694|Liverpool Sub-Group|42896|5|Briefly described|Fig.8|||refers to Lovering (1954)||||||
26694|Liverpool Sub-Group|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
26694|Liverpool Sub-Group|43319|14|Not recorded|Map Legend|||||||||
26694|Liverpool Sub-Group|43349|14|Not recorded|Map|||||||||
26694|Liverpool Sub-Group|43365|14|Not recorded|p169-210||Triassic|||||||
26694|Liverpool Sub-Group|43383|14|Not recorded|p23,13||Late Triassic|Inc Mittagong Fm,  Ashfield Shale, Minchinbury Ss, Bringelly Shale, Liverpool Sub-Group Table 1||||||
26694|Liverpool Sub-Group|43385|14|Not recorded|p182, Table||Late Triassic|||||||
26694|Liverpool Sub-Group|45090|6|Mentioned|p79|||Wianamatta Gp.||||||
28685|Liverpool Sub-Group""|39298|6|Mentioned|p257|||||||||
40466|Liverpool Volcanics|24603|5|Briefly described|p869 Fig. 4a|Tertiary|Tertiary|See also 886 Fig. 11.  Geological Province: Tamworth Belt.||||||
26695|Llanelly Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Llanelly. Reservation lapsed 1984.||||||
82766|Llangothlin Group|71628|6|Mentioned|p8: 1, 6, 9, 13, 16|||Bryant et al. (2002) included this unit in the Uralla Supersuite.||||||
30814|Lob's Hole Beds|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
28687|Lobbs Hole Adamellite|40498|6|Mentioned|p368|||Misspelling of Lobs Hole Adamellite? Comment added 1993.||||||
26696|Lobs Hole Granite|42726|5|Briefly described|map legend|Early Devonian||442. Variation on Lobs Hole Adamellite.||||||
25172|Lochiel Formation|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25172|Lochiel Formation|29994|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25172|Lochiel Formation|30662|6|Mentioned|p188|||Palaeomagnetism.||||||
25172|Lochiel Formation|30663|6|Mentioned|p27|||||||||
25172|Lochiel Formation|30938|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
25172|Lochiel Formation|31918|4|Described|p39|||Palaeomagnetic results Table 3, Fig.4.||||||
25172|Lochiel Formation|32127|4|Described|p249|||Refers Hall (1960)||||||
25172|Lochiel Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25172|Lochiel Formation|32672|6|Mentioned|p673|||||||||
25172|Lochiel Formation|32865|4|Described|p484|||||||||
25172|Lochiel Formation|33004|6|Mentioned|p78|||||||||
25172|Lochiel Formation|33268|4|Described|p268|||||||||
25172|Lochiel Formation|33269|6|Mentioned|p40|||Refers geology||||||
25172|Lochiel Formation|33325|5|Briefly described|Table 5|||U.Dev.||||||
25172|Lochiel Formation|33732|5|Briefly described|p113|||Table III||||||
25172|Lochiel Formation|33871|6|Mentioned|Fig.4|||||||||
25172|Lochiel Formation|33875|6|Mentioned|p32|||Uraninite deposits.||||||
25172|Lochiel Formation|34109|4|Described|p156|||||||||
25172|Lochiel Formation|34403|6|Mentioned|p129|||||||||
25172|Lochiel Formation|34405|6|Mentioned|Fig.3.9|||||||||
25172|Lochiel Formation|34406|6|Mentioned|p224|||||||||
25172|Lochiel Formation|34519|5|Briefly described|p45|||||||||
25172|Lochiel Formation|35277|6|Mentioned|p121|||||||||
25172|Lochiel Formation|35526|6|Mentioned|Table 1|||Stratigraphic nomenclature.||||||
25172|Lochiel Formation|39665|6|Mentioned|p1|||||||||
25172|Lochiel Formation|42050|6|Mentioned|Fig.3 P229|||||||||
25172|Lochiel Formation|42827|6|Mentioned|p191|||||||||
25172|Lochiel Formation|43461|14|Not recorded|table p62|Early Carboniferous|Late Devonian|||||||
25172|Lochiel Formation|43479|14|Not recorded|p150||Late Devonian|||||||
25172|Lochiel Formation|43507|14|Not recorded|p125|||||||||
25172|Lochiel Formation|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Includes: Cusack Creek Conglomerate Member. Of the Budawang Rift. Geological Province: Lambian Transitional Province.  Basalt interbedded with mudstone and conglomerate.||||||
25172|Lochiel Formation|46579|2|Defined|p.108||Late Devonian|Name replaces 'Yalwal Stage'. U. Devonian. (J55-4/Pambula; J55-8/Eden).||||||
25172|Lochiel Formation|60007|5|Briefly described|Map legend|Late Devonian|Late Devonian|Epidotised amygdaloidal basalt, dolerite, rhyolite, felsite, red shale, sandstone arkose.  Overlain by Merrimbula Formation; overlies Eden Rhyolite.||||||12-JUL-04
25172|Lochiel Formation|70351|5|Briefly described|p55|Late Devonian|Late Devonian|||Unit of Boyd Volcanic Complex.||Underlain by Eden Rhyolite||
31184|Lochinvar Beds|43491|14|Not recorded|pVII/43||Permian|See also Lexicon||||||
31183|Lochinvar Glacial Beds|43491|14|Not recorded|pVII/42||Permian|||||||
31182|Lochinvar Glacials|43491|14|Not recorded|pVII/44||Permian|||||||
31181|Lochinvar Group|43491|14|Not recorded|pVII/44||Permian|||||||
30773|Lochinvar Stage|43344|14|Not recorded|p84|||Now called Lochinvar Formation||||||
30773|Lochinvar Stage|43440|14|Not recorded|p91|||Ref. to David 1950. See also Lexicon||||||
30773|Lochinvar Stage|43477|14|Not recorded|p15,Pl.3|||Ref.to David||||||
30773|Lochinvar Stage|44855|14|Not recorded|p25|Permian|Carboniferous|Scattered glacial erratics.||||||
30773|Lochinvar Stage|44861|14|Not recorded|p228,245||Early Permian|||||||
34077|Lochinvar glacial stage|22612|6|Mentioned|423, 424 table 1|Early Permian|Early Permian|Geol province Sydney Basin. Max thickness ?50 m||||||
31091|Lochinvar shales|43477|14|Not recorded|Pl.3|||See also Lexicon||||||
25998|Lockhart Basic Intrusive Complex|42727|5|Briefly described|map legend||Late Silurian|Amphibolite and gabbro. Intrudes Birkenburn beds. Intruded by Rossi Granodiorite. BMR map symbol: Sa. Geol. Prov: Rocky Pic Block.||||||
25998|Lockhart Basic Intrusive Complex|42820|2|Defined|p76|Late Silurian||||||||
25998|Lockhart Basic Intrusive Complex|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
25998|Lockhart Basic Intrusive Complex|68115|6|Mentioned|p7.|||||||||
25998|Lockhart Basic Intrusive Complex|71069|6|Mentioned|p178, p179|||Obsolete name, replaced by the Lockhart Igneous Complex. ||||||
26697|Lockyersleigh adamellite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
26697|Lockyersleigh adamellite|32516|4|Described|p292|||||||||
26697|Lockyersleigh adamellite|36602|6|Mentioned|p114|||||||||
28691|London Bridge Limestone""|36413|6|Mentioned|p33|||||||||
28691|London Bridge Limestone""|42820|6|Mentioned|p39|||refers to Veevers (1953)||||||
82767|Long Creek Quartz Monzonite Phase|71628|5|Briefly described|p11: 2-3, 27, 29-31|||New name, after Mustard (2004). Named after a local watercourse. Crops out over 14 km2 on the NE margin of Timbarra Plateau. Geochemistry briefly described.||Rocky River Monzogranite.||Intrudes Drake Volcanics and Gilgurry Mudstone. Abuts Ewingar and ?Bulldog Diggings, Monzogranite Phases.|Medium- to coarse-grained, strongly porphyritic (pink K-feldspar megacrysts averaging 11mm) leucocratic quartz monzonite to monzogranite.|
24362|Long Hill Diorite|23214|5|Briefly described|p171|||Obsolete. Previously included in the Carcoar Granite (now Carcoar Granodiorite).||||||
24362|Long Hill Diorite|24265|5|Briefly described|p1451||Silurian|Geological Province: Lachlan Fold Belt||||||
24362|Long Hill Diorite|24266|5|Briefly described|p1476|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
24362|Long Hill Diorite|39325|6|Mentioned|p433|||||||||
24362|Long Hill Diorite|49794|6|Mentioned|p9|||||||||
24362|Long Hill Diorite|73431|5|Briefly described|p363 Fig.1, p364, p367 Tb.1|Devonian|Silurian|Comprises the more mafic phase of the Browns Creek Intrusive Complex near Browns Creek, in the north-western part of the intrusion. Appears as 'Long Hill Diorite' p364. Previous age of 418.9 +/- 2.8 Ma Ar/Ar hornblende (Perkins et al., 1995b).|418.9+/-2.8 Ma Ar/Ar hornblende|Browns Creek Intrusive Complex||||
37427|Long Hill Diorite""|23214|6|Mentioned|p171|||Informal name.||||||
42315|Long Hill Granodiorite|24266|5|Briefly described|p1476|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
25176|Longford Creek Member|29942|3|Fully described|p15|||||||||
34298|Longhill Diorite""|22679|6|Mentioned|p 46|||||||||
40933|Lookdown Limestone Member|50234|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Cardinal View Formation (Bungonia Group).||||||
40933|Lookdown Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Cardinal View Formation (Bungonia Group).  Fossiliferous limestone (dominantly biomicrudite and biomicrite) with small lenses of primary dolomite, spiculite and quartz rich anhydrite; coarsely recrystallised in places.||||||03-JUN-08
40933|Lookdown Limestone Member|68592|5|Briefly described|p110, p898, p900, p902, p904-7, p909-13|Ludlow|Ludlow|See also p1891-2. The Frome Hill Fault repeats this unit and is marked by a narrow crush zone and strongly recrystallised limestone. Fossil fauna described.||Unit in Cardinal View Formation.||Unconformably overlies Adaminaby Group. Near equivalent to Kingsdale Limestone Member (De Drack Formation).|Fossiliferous, biostromal limestone; basal intraclast conglomerate; small lenses of primary dolomite.|
40933|Lookdown Limestone Member|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sbcl[2 asterisks]. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Cardinal View Formation|||Fossiliferous, biostromal limestone, dominantly biomicrudite and biomicrite with small lenses of primary dolomite, spiculite and anhydrite.|
40933|Lookdown Limestone Member|70542|5|Briefly described|Map Legend|Silurian|Silurian|||Cardinal View Formation|||Fossiliferous, biostromal limestone, dominantly biomicrudite and biomicrite with small lenses of primary dolomite, spiculite and anhydrite.|
40933|Lookdown Limestone Member|71656|5|Briefly described|p13 Fig.2, p31|Ludlow|Ludlow|Gastropods, graptolites and rugose corals included in diverse fauna.||Cardinal View Formation|||Fossiliferous limestone.|
33673|Loomat Granodiorite|22815|4|Described|p75|||||||||
33673|Loomat Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian||of Coolangubra Suite.||||||
35430|Loombah Formation""|23170|6|Mentioned|p55|||||||||
31312|Loomberah Member|43529|14|Not recorded|p236||Eifelian|||||||
77357|Loombrah Limestone|68005|6|Mentioned|p52.|||This name is used in the Loombrah [correct geographic name is Loomberah] and Timor region for a unit which, in the Attunga region, is called the Sulcor Limestone.||Unit in Yarrimie Formation.||||
81716|Louth volcanics''|71965|6|Mentioned|p903|||Geological province: Thomson Orogen. Different from Louth Volcanics. "Louth volcanics" was previously informally used to describe all rocks occurring in the vicinity of Louth (excluding cherts). Recent geochemistry, geochroonology and petrography work has helped discriminate units.||||||
68124|Lovett Formation|24266|6|Mentioned|p1480|||Geological Province: Lachlan Fold Belt.||||||09-MAR-05
39266|Lowell-Guilbert porphyry|24230|6|Mentioned|p174|||Informal name.||||||
32457|Lower "Blythesdale Group"|34254|14|Not recorded|p.481-497.||Late Jurassic|||||||
30908|Lower Blythesdale Sub-Group|43404|14|Not recorded|Table p11,20||Jurassic|||||||
30838|Lower Burindi Group|43385|14|Not recorded|p176,177||Tournaisian|||||||
30838|Lower Burindi Group|43399|4|Described|p189-90,192-3,196-7||Early Carboniferous|||||||
30838|Lower Burindi Group|43876|14|Not recorded|p587||Late Carboniferous|Spelt 'group' on reference card.||||||
30838|Lower Burindi Group|44874|14|Not recorded|p104|||Refers to Cvancara A.M. 1958: J.Palaeontology, 32,846-888.||||||
30838|Lower Burindi Group|48600|14|Not recorded|Plate 3|||||||||
30837|Lower Burindi Mudstone|43385|14|Not recorded|p176||Tournaisian|||||||
30772|Lower Chesleigh Formation|23214|5|Briefly described|p150|||Informal Name. See Chesleigh Formation.||||||
30772|Lower Chesleigh Formation|43344|14|Not recorded|p153|||||||||
31185|Lower Clarence Beds|43491|14|Not recorded|pVIII/16||Triassic|||||||
31186|Lower Clarence Series|43491|14|Not recorded|pVIII/16||Triassic|||||||
31186|Lower Clarence Series|43881|14|Not recorded|pxii|||Ref to David 1950. See also Lexicon||||||
32541|Lower Coal Measures""|33334|6|Mentioned|p2.||Permian|||||||
31972|Lower Drake Series|43881|14|Not recorded|p6-7,9||Permian|Now named Cheviot Hills Group.||||||
35144|Lower Fern Valley Coal|23055|6|Mentioned|Fig4p11|||||||||
34503|Lower Knight Beds""|22799|6|Mentioned|p25|||||||||
34501|Lower Knight Group""|22799|6|Mentioned|p25|||||||||
30839|Lower Kuttung Group|43385|14|Not recorded|p176,177||Visean|||||||
30839|Lower Kuttung Group|43418|14|Not recorded|Map Legend|||||||||
30839|Lower Kuttung Group|43876|14|Not recorded|p587||Late Carboniferous|Spelt 'group' on reference card.||||||
30839|Lower Kuttung Group|48600|14|Not recorded|Plate 3|||||||||
31910|Lower Kuttung Lavas|43870|14|Not recorded|p158,304,330||Late Carboniferous|Age Visean (David 1950).Now regarded as Late Carb. since 2 toscanites gave age of 288 Ma and 307 Ma.||||||
30983|Lower Kuttung Volcanics|43446|14|Not recorded|p6048||Visean|||||||
30982|Lower Kuttung andesites|43446|14|Not recorded|p6040||Visean|||||||
25181|Lower Kuttung lavas|37818|6|Mentioned|p82|||||||||
25181|Lower Kuttung lavas|43439|14|Not recorded|p409||Early Carboniferous|||||||
28697|Lower Marine basalt|32106|6|Mentioned|p305|||Palaeomagnetic data||||||
70636|Lower Marine series|45015|6|Mentioned|p8|Early Permian|Early Permian|Of Raggatt and Fletcher (1937). Informal name for unit in NSW.||||||
25182|Lower Merrygoen Beds""|41264|6|Mentioned|Table 1|||||||||
31324|Lower Murrindal beds""|43533|14|Not recorded|p113,120|||Ref.to Teichert and Talent 1958||||||
37948|Lower Pelitic Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
78866|Lower Pilot coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Boolaroo Formation||||
38216|Lower Pilot seam|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Boolaroo Formation.   Geological Province: Sydney Basin||||||
38216|Lower Pilot seam|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Boolaroo Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
38216|Lower Pilot seam|62033|5|Briefly described|p25 (Table)|||Of the Boolaroo Formation (Newcastle Coal Measures). Overlies Hartley Hill seam; overlain by Mount Hutton tuff. Geological Province: Sydney Basin. Informal name.||||||14-MAR-07
34504|Lower Renmark Beds""|22799|6|Mentioned|p25|||||||||
34733|Lower Renmark Group|22893|6|Mentioned|p25 fig9|Tertiary|Tertiary|||||||
35870|Lower Snake Cave Sandstone|23336|5|Briefly described|p15|||Informal - see Snake Cave Sandstone.||||||21-MAR-06
37294|Lower Tamworth Group|24009|5|Briefly described|p368 Fig.1|Middle Devonian|Early Devonian|Informal name - see Tamworth Group.||||||
31221|Lower Trilobite Bed|43857|6|Mentioned|p322|||of Mitchell (1886 etc). Later informally called Hume Shales.||||||
31221|Lower Trilobite Bed|68592|6|Mentioned|p587, 1881|||Former name for Yarwood Siltstone Member.||||||12-JAN-17
35356|Lower Yarrimie Limestone|23185|6|Mentioned|p157|||||||||
73524|Loxton Sands""|10010|6|Mentioned|p17|||Term used for separate Pliocene sand units in some parts of Murray Basin - but not always distinct from "Parilla Sands" - hence the collective term Loxton-Parilla Sands.  ||||||
73524|Loxton Sands""|73228|6|Mentioned|p58|||[Written as 'Loxton Sands'; variation of Loxton Sands, which is superseded by Loxton Sand].||||||
33864|Loxton-Parilla Sands|10010|5|Briefly described|p17|Pliocene|Late Miocene|Combined term of Brown and Stephenson (1991). Conformable on Bookpurnong beds or disconformable on Renmark Group or Geera Clay; disconformable below Blanchetown Clay.  Average thickness: 30m.Geol.Prov: Murray Basin.Very fine to coarse, gravelly in places.||||||13-AUG-07
33864|Loxton-Parilla Sands|22531|4|Described|p20|Pliocene|Late Miocene|||||||
33864|Loxton-Parilla Sands|22799|3|Fully described|p35|||||||||
33864|Loxton-Parilla Sands|22835|6|Mentioned|P14||Pliocene|||||||
33864|Loxton-Parilla Sands|22857|5|Briefly described|p353 Fig. 24.9|Pliocene|Pliocene|See also Loxton-Parilla Sand. ||||||
33864|Loxton-Parilla Sands|23884|6|Mentioned|p153|||Geological Province: Murray Basin.||||||28-APR-05
33864|Loxton-Parilla Sands|23921|4|Described|p1109, p1114|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
33864|Loxton-Parilla Sands|24103|5|Briefly described|p139 Fig.3|Pliocene|Pliocene|Geological Province: Murray Basin. Age: 6.6-3.5 Ma.||||||
33864|Loxton-Parilla Sands|24439|6|Mentioned|p39 Fig. 21|||||||||06-APR-05
33864|Loxton-Parilla Sands|24440|5|Briefly described|Map legend|||Shallow marine sands.||||||
33864|Loxton-Parilla Sands|60421|5|Briefly described|p407, 408 Fig. 1, 415, 418 Fig. 5|Pliocene|Late Miocene|Geological Province: Murray Basin. Forms strandlines. Overlies: Glenelg River Metamorphic Complex.||||||
33864|Loxton-Parilla Sands|61155|5|Briefly described|p5, p18|Early Pliocene|Late Miocene|Strand plain and fluvial sand deposits. Overlie Bookpurnong beds; overlain by Blanchetown Clay, and by Norwest Bend Formation in the west. Age: ~6.0-2.5Ma. Max. thickness: 150m. Geological Province: Murray Basin.||||||
33864|Loxton-Parilla Sands|61207|5|Briefly described|p281|Pliocene|Late Miocene|See also Loxton-Parilla Sand.  This is a shoreface, beach and possibly alluvial succession of sands and some gravels (Firman 1966; Roy et al 2000). Overlain by Blanchetown Clay.||||||
33864|Loxton-Parilla Sands|61624|6|Mentioned|p471|||Geological Province: Murray Basin.||||||07-APR-09
33864|Loxton-Parilla Sands|63887|5|Briefly described|p20, p21, p22, p21 Fig. 1, p23 Fig. 2|Pleistocene|Late Miocene|Prograding beach strandplains and barrier islands.||||||
33864|Loxton-Parilla Sands|63893|5|Briefly described|p191, p185, p184, p188 Fig. 3|Late Pliocene|Late Miocene|Series of shallow-marine beach, estaurine and fluvial sands. Thick strata, often almost pure quartz. Intermittent heavy minerals. Age: Victorian sequences 3.5 Ma mid-Pliocence. With Blanchetown Clay underlie Shepparton Formation. Geol Prov: Murray Basin.||||||
33864|Loxton-Parilla Sands|64961|5|Briefly described|p269 Fig. 9|Late Pliocene|Late Miocene|See also the misspelt Loxton-Parilla Sand.||||||08-APR-09
33864|Loxton-Parilla Sands|64966|5|Briefly described|pp140|Late Miocene|Early Eocene|Geological province: Murray Basin. An extensive system of arcuate strandlines indicating marine transgression.||||||07-FEB-11
33864|Loxton-Parilla Sands|65552|5|Briefly described|p2; p4-17; p22,25,26,27 App.1,4,5,6|Late Pliocene|Early Pliocene|Loxton Sands and Parilla Sand, undifferentiated in central Murray Basin. Hosts silica, heavy sands, bentonite. Contains Wandella Sandstone, Kerang Sand, Tragowel Members. Underlies Blanchetown Clay; overlies Murray Group, Bookpurnong beds, Olney Formation||||||
33864|Loxton-Parilla Sands|65715|5|Briefly described|p15 Tb.8|||Superseded name for Loxton Sand in Victoria.||||||
33864|Loxton-Parilla Sands|65904|5|Briefly described|p244||Pliocene|20-60m thick, widely distributed across Murray Basin. Mainly marine sand sequence; some beach, deltaic, non-marine sediments. 3 marine facies units: fine grained micaceous sediment, coarse sands and occasional gravel, upwards fining beach sand unit. Contains economic heavy-mineral sands.||||||29-APR-11
33864|Loxton-Parilla Sands|66002|6|Mentioned|p13 Tb.9|||Widely used but invalidly named unit equivalent to Loxton Sand in Victoria. ||||||
33864|Loxton-Parilla Sands|66287|3|Fully described|p24,26,27,31-42, Fig 2,4-5,7-14,17|Early Pliocene|Late Miocene|Progradational strandplain in Murray Basin; over 600 individual ridges. Previous age range ~6 Ma - 2.4 Ma, based on sea level curves, palaeomag and age of overlying Blanchetown Clay. This study's age is from Sr/Sr ratios.|Deposited between 7.2 and 4.5 Ma.|||Overlies and interfingers with Bookpurnong Beds.|Marine, estuarine + minor fluvial depositional environments. Heavy mineral deposits associated.|25-FEB-13
33864|Loxton-Parilla Sands|66934|5|Briefly described|Map legend|Pliocene|Pliocene|Near-surface magnetically-susceptible heavy mineral sands that formed along Murrayian Gulf shoreline in arcs 0.4-1 km wide and tens of kilometres long.||Unit in Wunghnu Group.|||Loosely consolidated cross-bedded micaceous sand, grit and silty sand.|
33864|Loxton-Parilla Sands|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Murray Basin.||||||
33864|Loxton-Parilla Sands|67179|5|Briefly described|p581|Pliocene|Miocene|Informal, superseded by revised Loxton Sand. Compound name was used because marine strata (Loxton Sand) and dune and fluvial strata (Parilla Sands) are often not possible to map separately.||||||
33864|Loxton-Parilla Sands|68140|5|Briefly described|p1699, p1701-1704, p1707, p1708|||See also Loxton-Parilla Formation. Groundwater in this unit is susceptible to contamination from human activities on the surface.||||Overlain by the Shepparton Formation. Underlain by the Murray Group.|Comprises a sequence of marine sands and silts.|09-FEB-18
33864|Loxton-Parilla Sands|69572|6|Mentioned|p1190-1191|Pleistocene|Miocene|Contains fossil koala of Phascolarctos yorkensis.||||||
33864|Loxton-Parilla Sands|70718|5|Briefly described|p90, 104|||Murray Basin. Obsolete name, see the Loxton Sand which has replaced it.||||||30-MAY-19
33864|Loxton-Parilla Sands|72445|5|Briefly described|App.6 p1 Tb.1, p5, p7; App.7 p7.|Pliocene|Late Miocene|Spelt as 'Loxton-Parilla Sand' in App.6 p1 Tb.1. App 6 suggests in Stavely 11, 14 samples, but well log indicates Bookpurnong Formation at these depths. Described App 7 as fluvio-lacustrine, App.6 as shallow marine.|< 5.72 Ma||Probably includes Wandella Sandstone Member.|Shown as overlying Bookpurnong beds and partially and unconformably underlying Blanchetown Clay and partially equivalent to Parilla Sand and Loxton Sands.|Includes sand.|
33864|Loxton-Parilla Sands|73118|5|Briefly described|p12, 17, 21, 24, 30, 34, 37, 45, 48, 53|Pliocene|Miocene|See also p58, 61, 64, 81. Forms blanket of sand beneath almost the entire SW Murray Basin. 100m thick; mainly <60m. CRA Exploration found (between 1980-1992) several world-class mineral sand accumulations along the southern margin region of the Murray Basin. Drill core summary logs. Strand-plain (shallow-marine, beach and estuarine) deposits flanked/overlain by fluvial and fluvio-lacustrine deposits.||||Overlies Grampians Group, Duddo Limestone, Geera Clay, Bookpurnong Beds, Winnambool Formation and Olney Formation. Is overlain by Woorinen and Shepparton Formations, Molineaux-Lowan Sands.|Unconsolidated to weakly cemented,yellow-brown fine to coarse well-sorted quartz sand, sandstone, with minor clay, silt, pebbly conglomerate.|
83137|Loxton-Parilla Sands''|73228|4|Described|p58-59|||Name has been widely used to describe the Pliocene strandline sands of the Murray Basin and was invoked to address difficulties encountered in stratigraphic correlation across state boundaries, particularly between the 'Loxton Sands' of Ludbrook (1957), the 'Parilla Sand' of Firman (1966), and the 'Diapur Sandstone' of Lawrence and Goldberry (1973). Defined as a 'single composite sand sheet' deposited in a complex array of strandplain environments varying from shallow to marginal marine, estuarine and fluvial (Brown and Stephenson, 1991). Fossil poor but contains calcareous, often fossiliferous, facies in the western and southwestern Murray Basin. Well-laminated horizons often exhibit cross-bedding, particularly within the quartz-gravel units. Thickness typically ranges from 20 to 60 m and is up to 150 m in places. Contains large concentrations of heavy minerals (mainly rutile, zircon and ilmenite; Roy et al. 2000).||||Disconformably overlain by upper Norwest Bend Formation.|Fine to coarse, well-sorted quartz sand and sandstone, yellow-brown in colour, with minor silt, clay and pebble conglomerates, locally containing micaceous quartz sands and/or gravel facies and large concentrations of heavy minerals.|
32656|Lucknow Formation|46547|14|Not recorded|Not recorded|||||||||
33740|Lucy Hill Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Massive, leucocratic, perthitic, biotite muscovite magnetite granite.||||||05-JUL-04
38931|Lucy Hill Granite""|24417|6|Mentioned|p100|||Name abandoned - still included as part of the Mortray Hill Granite Complex.||||||
38448|Lucyvale granite|24133|6|Mentioned|p22|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
25184|Lue Beds|24126|6|Mentioned|p42|||||||||
25184|Lue Beds|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25184|Lue Beds|30329|6|Mentioned|p30|||On table P30||||||
25184|Lue Beds|31161|5|Briefly described|PA3|||||||||
25184|Lue Beds|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
25184|Lue Beds|32046|6|Mentioned|p97|||See also P159,169||||||
25184|Lue Beds|32047|6|Mentioned|p7|||||||||
25184|Lue Beds|32485|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25184|Lue Beds|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
25184|Lue Beds|34059|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25184|Lue Beds|34130|6|Mentioned|p178|||Ordovician?||||||
25184|Lue Beds|35257|6|Mentioned|p132|||||||||
25184|Lue Beds|36534|6|Mentioned|p225|||||||||
25184|Lue Beds|37727|5|Briefly described|p69|||See also P21.||||||
25184|Lue Beds|39331|6|Mentioned|Fig.0-3|||||||||
25184|Lue Beds|39663|6|Mentioned|Table 1|||||||||
25184|Lue Beds|40136|6|Mentioned|p15|||||||||
25184|Lue Beds|40328|5|Briefly described|p138|||||||||
25184|Lue Beds|42657|5|Briefly described|p73|||||||||
25184|Lue Beds|43188|5|Briefly described|Fig.4 p202||Late Ordovician|Misspelling of Lue beds.||||||
25184|Lue Beds|43476|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
35347|Lue Beds""|23170|6|Mentioned|p29|||Divided into Adaminaby Group and Coomber Formation.||||||
35347|Lue Beds""|23181|6|Mentioned|Fig.2, p3|||Now Adaminably Group.||||||
30022|Lue beds|5258|5|Briefly described|164|Darriwilian|Darriwilian|Age based on conodonts. Location in Bara Creek given. Strongly deformed, dominantly quartz-rich turbidite succession||||||22-JAN-10
30022|Lue beds|22529|5|Briefly described|2|Ordovician|Ordovician|||||||
30022|Lue beds|22545|6|Mentioned|p498,499|||||||||
30022|Lue beds|43188|4|Described|p199,Table 1 p200||Darriwilian|Age based on conodonts. Capertee High.||||||
35348|Lue beds""|23181|6|Mentioned|p1|||Now Adaminaby Group. Underlie Gudgegong Volcanics? Include chert containing conodonts implying a late Darriwilian age (Latest Middle Ordovician).||||||
29224|Lumley Adamellite|40132|2|Defined|p238|Early Devonian|Early Devonian|||||||
73882|Lynore Limestone|50095|5|Briefly described|p121|Devonian|Silurian|Contains Belodella Anomalis (conodont). NSW.||||||30-JAN-08
73882|Lynore Limestone|61892|6|Mentioned|p216|Pridoli|Pridoli|Contains Acrotretella brachiopods, contrasted with those around the world.||||||
68914|Lynore Limestone""|60332|6|Mentioned|p952|||Informal. Contains Belodella anomalis (conodont).||||||
70406|Ma-Ma Creek Member|60999|5|Briefly described|p169 Fig. 3|||Misspelt- see Ma Ma Creek Member. See also p172 Fig. 6.||||||
78270|MacCullochs Range Beds|67562|5|Briefly described|p92, p96-97, p99-100, p115|Emsian|Wenlock|Darling Basin. Coeval with the Mount Daubeny Formation, and similarly poly-deformed. Cut by five ENE-trending, high-angle faults parallel to the Darling Fault. Sandstone at the base of this unit contains clay clasts consistent with flood plain deposition. Sporadic brachiopods and gastropods indicate minor marine transgressions.|||||Fine-grained, grey-brown sublitharenites and feldspathic arenites.|23-JAN-17
82566|MacDonald River Suite|71628|5|Briefly described|p4:38|||||Bundarra Supersuite.|MacDonald River Monzogranite.|||
80191|MacKenzie Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Induan|Changhsingian|New England Orogen.|251.7 +/- 2.1 Ma (SHRIMP, Black, 2007)|Stanthorpe Supersuite||||04-OCT-17
31971|MacPherson Range volcanics|43881|14|Not recorded|p62||Tertiary|See MacPherson Volcanics. (probably Eocene-Oligocene)||||||
73751|Maccullochs Range Beds|63632|5|Briefly described|p652 Fig. 4|Early Devonian|Early Devonian|Misspelt - should be Maccullochs Range beds.||||||16-OCT-07
34751|Macleay Formation|22892|6|Mentioned|p41|||Present floodplain of the Macleay River valley.||||||
31188|Macleay beds|43491|14|Not recorded|pVII/45|||Equivalent of Lower Marine Series Permian in Sydney Basin||||||
33597|Macleay series|48600|14|Not recorded|p30|||Cancrinella farleyensis found.||||||
31261|Macquarie Sandstone|43512|14|Not recorded|p97||Late Devonian|(?Macquarie Park Sandstone)||||||
78193|Macquarie Volcanics|68822|5|Briefly described|p320 Fig.3|Ordovician|Ordovician|Eastern Subprovince, Lachlan Orogen.|Early to Late Ordovician|||||
78193|Macquarie Volcanics|70601|5|Briefly described|p38 Fig.9, p56|||A postulated arc on the outer edge of the Gondwana margin; its role in the Benambran Orogeny discussed. The hypothesis has been abandoned. Contrasted with Wagonga Group in a N-MORB normalised Nb/La plot.|||||Basalt.|
41629|Macqueen Formation""|44244|6|Mentioned|p23|||Informal term for basal portion of the Dangarfield Formation, now reduced to member status as Macqueen Member.  On MUSWELLBROOK 1:100 000 sheet only.||||||23-AUG-04
76163|Macs Tank Serpentinite|66623|6|Mentioned|p227|||Name superseded by Macs Tank Ultramafic.||||||
74924|Macs Tank Ultramafic Complex|64679|5|Briefly described|Map legend|||Age not known.||||||
74924|Macs Tank Ultramafic Complex|66623|6|Mentioned|p228.|||Name superseded by Macs Tank Ultramafic.||||||
69951|Macs Tank ultramafic|22671|5|Briefly described|p839|||In the Conns Creek (Nundora), Mount Wright and Mount Arrowsmith areas. An upper greenschist facies, metamorphosed serpentinised ultramafic of probable Iherzolitic composition.  May intrude the Ponto beds, or may be thrust over them.||||||18-JAN-06
26005|Maffra Adamellite|22815|4|Described|p59|Silurian|Silurian|Age: 412-413 Ma.||||||
26005|Maffra Adamellite|23454|6|Mentioned|p27 Fig.1|||||||||
26005|Maffra Adamellite|33779|4|Described|p168|||Map||||||
26005|Maffra Adamellite|33852|6|Mentioned|p499|||Date given.||||||
26005|Maffra Adamellite|38327|6|Mentioned|Table 4|||||||||
26005|Maffra Adamellite|38500|4|Described|p85|||||||||
26005|Maffra Adamellite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
26005|Maffra Adamellite|40328|4|Described|p208|||||||||
26005|Maffra Adamellite|41905|2|Defined|p69|Silurian||||||||
26005|Maffra Adamellite|41933|5|Briefly described|Map legend|Late Silurian||||||||
26005|Maffra Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||of Delegate Suite.||||||
26005|Maffra Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|glp1||||||
26005|Maffra Adamellite|60078|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
37837|Magdala basalt|24100|6|Mentioned|p99|||Informal - see Magdala Basalt. Geological Province: Lachlan Fold Belt.||||||
37837|Magdala basalt|24221|6|Mentioned|p895|||Informal name.||||||
37837|Magdala basalt|62741|6|Mentioned|p683 Fig. 5b|||Informal name.||||||
37837|Magdala basalt|62747|6|Mentioned|p735|||Informal - see Magdala Basalt.||||||31-OCT-06
37837|Magdala basalt|73430|6|Mentioned|p498-499, p506, p508, p516 Fig.19|||Magdala basalt described from the Stawell Mine (Squire et al., 2006) are relatively Ti-rich tholeiites, and significantly different to the boninite-like Magdala basalts that outcrop directly east of the Mt Stavely outcrops and Moyston Fault. See also Magda Basalt p517. [Also appears as Magdala basalts p498, p508, p510 Fig.10].|||||Tholeiites, and boninite-like basalts.|
39621|Magdala volcanogenic rocks|24087|4|Described|p329|||Informal name.   Geological Province: Lachlan Fold Belt.||||||
39619|Magdala volcanogenic rocks""|24087|5|Briefly described|p329|||Informal name.   Geological Province: Lachlan Fold Belt.||||||
39619|Magdala volcanogenic rocks""|50546|6|Mentioned|p1235|||Geological Province: Lachlan Fold Belt.||||||
33386|Magistrate Volcanics|23859|5|Briefly described|p931 Fig 3|||See Magistrate Volcanic Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
33386|Magistrate Volcanics|61793|4|Described|p341, p342 Fig. 1(b), p343 Tb. 1, p347|Late Permian|Late Permian|Of Emmaville Volcanics. Overlain unconformably by Four Mile Mudstones. Thickness: 450m. Geological Province: New England Fold Belt. Mainly ignimbrite with subordinate air-fall tuff beds.||||||07-FEB-11
33386|Magistrate Volcanics|70210|5|Briefly described|p2, p25-26, p29-30, p38, p40-41|Permian|Permian|New England district. Described as a "representative" of the Emmaville Volcanics, but nowhere is it presented as a Member of that formation. Also 250.7 +/- 3.9 Ma.|252.5 +/- 1.7 Ma (preferred age).|||||
26717|Mailman Gap Conglomerate Member|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Rankin Formation (Cocoparra Group). Pebbly arenite with thin conglomerate bands, arenite and lithic arenite.||||||
26717|Mailman Gap Conglomerate Member|22887|3|Fully described|p28, Fig.4 p11|Middle Devonian|Early Devonian|||||||
26717|Mailman Gap Conglomerate Member|23252|5|Briefly described|Map Legend||Middle Devonian|of Cocoparra Group.||||||
26717|Mailman Gap Conglomerate Member|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26717|Mailman Gap Conglomerate Member|34109|6|Mentioned|Fig.3.21|||||||||
26717|Mailman Gap Conglomerate Member|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26717|Mailman Gap Conglomerate Member|43511|14|Not recorded|p131,134,136,147|||Basal member of Rankin Formation||||||
26717|Mailman Gap Conglomerate Member|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. Bottom of the Rankin Formation, member of hte Cocoparra Group, Upper Devonian in age, O/lies the Jimberoo Member, U/lies undifferentiated Rankin Formation.||||||
26717|Mailman Gap Conglomerate Member|61964|5|Briefly described|p114, p126|Late Devonian|Late Devonian|Of Conolly (1962). Superseded by Mailman Gap Member (Rankin Formation, Cocoparra Group). Characterised by outcrops of cobble orthoconglomerates. Written as "Mailman Gap Conglomerate Member".||||||
80787|Main Camp Creek Gabbro|69639|6|Mentioned|p170, p176, p182|||Equivalent mafic diorite to gabbroic intrusions to this unit are cut [ intruded?] by the Rivertree Granite. [Said to be] Called Main Camp Creek Road Gabbro (Thomson, 1976) p182 [but Thomson used Main Camp Syenite].|||||Mafic diorite to gabbroic intrusions.|06-MAR-19
41631|Main Glacial Beds""|44244|6|Mentioned|p102|||Of the "Kuttung Series" of Osborne (1922) - name now abandoned.  Replaced by Seaham Formation.||||||
34593|Main Gully limestone|22842|5|Briefly described|p29|||Informal name for limestone unit within Cardinal View Shale.||||||
34593|Main Gully limestone|70661|6|Mentioned|p39|||||Cardinal View Formation||||
25194|Main Sandstone""|35065|6|Mentioned|p44|||||||||
83574|Main Seam|73304|6|Mentioned|p71|||Of the Wallabella Coal Member[?].||||||
83479|Main Volcanics|73487|6|Mentioned|p566 Fig. 2|Tournasian|Tournaisian|Probably not a unit of this age, but part of the map key.||||||01-SEP-22
30994|Maitland beds|43448|14|Not recorded|p223|||= Maitland Group||||||
70520|Majuba Supersuite""|62367|5|Briefly described|p8|Silurian|Silurian|Group of felsic I-type volcanic rocks and related I-type intrusions. Includes the Mineral Hill Volcanics. Age: 428-418Ma (Morrison et al 2004).||||||23-SEP-19
79849|Majuba supersuite|67416|5|Briefly described|p85, p91|||Blevin and Jones (2004). An informal term applied to volcanics in the Canbelego-Mineral Hill Volcanic Belt. Mainly shallow-marine felsic pyroclastics with lesser lavas. Appears in various guises including Majuba Supersuite and "Majuba supersuite". Includes Mineral Hill, Majuba, Florida, Babinda and Canbelego Volcanics and the Mount Walton Porphyry, Wilmatha and Yellow Mountain Granites.|||||I-type. Felsic and rhyolitic pyroclastics with minor rhyodacite, dacite and rare andesites. Intercalated and gradational to sandstones, conglomerates and limestones.|21-JUN-17
31232|Majurgong Beds|43479|14|Not recorded|p125||Devonian|||||||
30774|Majurgong Quartzite|43344|14|Not recorded|p117|||||||||
82768|Malachi Monzogranite Phase|71628|5|Briefly described|p15: 35, 100-104, 115|||This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.||Severn River Monzogranite.|||Pale pinkish grey to pale greenish grey, medium-grained monzogranite with minor biotite, hornblende and titanite.|
30775|Malachi's Hill Formation|43344|14|Not recorded|p139,160-162||Late Ordovician|||||||
30775|Malachi's Hill Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
30775|Malachi's Hill Formation|43385|14|Not recorded|p169||Ashgillian|Ref.to Stevens 1957 (U.Ord)||||||
30775|Malachi's Hill Formation|43515|14|Not recorded|Map Legend||Late Ordovician|(Provisional Edition)||||||
31262|Malachi's Hill Formation""|43512|14|Not recorded|p102-104||Late Devonian|Mapped only||||||
35426|Malachis Hill Formation""|23170|6|Mentioned|p48|||||||||
40717|Malachis Hill formation|23309|6|Mentioned|p390|||||||||
35759|Malay Creek Formation|50232|4|Described|Malay|Eastonian|Gisbornian|Of the Bendoc Group.  Overlain by and interfingered with Warbisco Shale.||||||
35759|Malay Creek Formation|67322|5|Briefly described|p39|Sandbian|Sandbian|Shown on provisional 1st edition of Gunning 1:100 000 geological map (Thomas et al. 2001), this unit occupies an identical stratigraphic position to the Sunlight Creek Formation, hence is redundant. Age is assumed to be similar to the Sunlight Creek Formation.|||||Interbedded sandstone and black shale.|22-FEB-18
35759|Malay Creek Formation|68592|6|Mentioned|p328|Ordovician|Ordovician|Appeared as 'Malay Creek Formation' on the provisional Gunning 1:100 000 map sheet (Thomas et al. 2001, unpublished). Included here in Bumballa  Formation.||Bendoc Group.||||01-APR-16
28715|Mallee Tank Group""|35385|6|Mentioned|p11|||Refers Joklik(1950)||||||
28715|Mallee Tank Group""|39618|6|Mentioned|p70|||||||||
28715|Mallee Tank Group""|41528|6|Mentioned|p39|||See also P94||||||
28715|Mallee Tank Group""|41821|6|Mentioned|p34|||Now recognized as Amphitheatre Group in the Lachlan Downs sheet area||||||
28715|Mallee Tank Group""|42566|6|Mentioned|p47|||Superseded by Kopyje Group||||||
31276|Malongulli Tuff|43479|14|Not recorded|no card|||(no card)||||||
39934|Malongulli Tuff Formation|24268|4|Described|p1535|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
29684|Mammy Johnson Formation|43017|5|Briefly described|Fig.1,p372|||Misspelling of Mammy Johnsons Formation.||||||
81807|Mana Conglomerate|72495|6|Mentioned|p228|Devonian|Silurian|||||||
27476|Manar Porphyry|34405|6|Mentioned|p105|||||||||
27476|Manar Porphyry|39800|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27476|Manar Porphyry|43384|14|Not recorded|Map Legend||Devonian|See also Lexicon||||||
27476|Manar Porphyry|43385|14|Not recorded|p174||Late Devonian|||||||
37401|Mandagery Cherts|23214|5|Briefly described|p123|||Maggs (1963).||||||
37109|Mandagery Formation""|23392|6|Mentioned|p15|||||||||
36201|Mandagery Sandstone""|23392|6|Mentioned|p15|||Of Conolly 1965.  Superseded by Weddin Formation in Grenfell area.||||||
36201|Mandagery Sandstone""|24417|6|Mentioned|p128|||Superseded by Mandagery Formation.||||||
72898|Mandagery"" Formation|62569|5|Briefly described|p606 Fig. 1E|Late Devonian|Late Devonian|Of the Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
31605|Mandari Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31605|Mandari Suite|44093|5|Briefly described|p219 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||15-MAR-05
31605|Mandari Suite|68592|6|Mentioned|p1611|Devonian|Devonian|Included in the Marulan Batholith by Chappell et al. (1991).||||||
31605|Mandari Suite|70661|6|Mentioned|p77|||||||||
23758|Mandari granodiorite|36600|6|Mentioned|Table 1|||||||||
34008|Mandowa Formation|22572|5|Briefly described|p108||Devonian|Mandowa-Mostyn Vale-Tulcumba corremlates||||||
34008|Mandowa Formation|22736|6|Mentioned|p628 Fig7||Famennian|||||||
34008|Mandowa Formation|65214|6|Mentioned|p280|Devonian|Devonian|NSW, Tamworth. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
31279|Mandurama claystone|43491|14|Not recorded|no card|||(no card)||||||
35415|Manildra Formation""|23170|6|Mentioned|p31|||||||||
26719|Manildra Granite|42726|5|Briefly described|map legend|Early Devonian||414. Of the Manildra Suite (Boggy Plain Supersuite).  Not intended as a formal name.  NOT Variation on Manildra Formation etc.||||||08-FEB-05
25201|Manildra Group""|40328|6|Mentioned|p71|||See also P124||||||
31469|Manildra Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Manildra Granite (informal name).||||||08-FEB-05
30945|Manilla River Intrusives|43429|14|Not recorded|Map Legend|||Description given see Strat form.||||||
28719|Mannering Park Tuff|23055|6|Mentioned|Fig4p11|||||||||
28719|Mannering Park Tuff|33867|6|Mentioned|Fig.4|||||||||
28719|Mannering Park Tuff|41463|6|Mentioned|p38|||||||||
28719|Mannering Park Tuff|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Moon Island Beach Subgroup.||Overlies Teralba Conglomerate. Is overlain by Wallarah seam.||
28719|Mannering Park Tuff|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS age of 252.7 Ma (Metcalfe etal., 2015). Corresponding to APP% zone (Lopingian).||Unit of Moon Island Beach Formation.||||
28719|Mannering Park Tuff|73304|5|Briefly described|p65-66, p69, p75|Changhsingian|Changhsingian|[Possibly abbreviated from Mannering Park Tuff Member].|252.70 +/- 0.30 Ma U-Pb CA-TIMS.|Moon Island Beach Formation[?], Newcastle Coal Measures||Underlain by Wallarah Coal.||
25204|Maradena Shale|33732|6|Mentioned|Table II|||Misspelling of Maradana.||||||
37229|Maragulla Syenite|23214|6|Mentioned|p88|||Misspelt. See Marangulla Syenite.||||||
33674|Maramingo Adamellite|22815|4|Described|p88|||||||||
33674|Maramingo Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unassigned pluton, Bega Batholith.||||||
70344|Marburg "Formation"|60993|6|Mentioned|p4, p18, p28|||Informal version of McElroy's Marburg Formation (1963) now redefined as Marburg Subgroup. Geological Province: Clarence-Moreton Basin.||||||
70344|Marburg "Formation"|60997|5|Briefly described|p138|||Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
70345|Marburg Formation, Lower|60993|5|Briefly described|p6 Fig. 2|||Of Etheridge et al (1985) but name is informal. Unit now divided into Gatton Sandstone and two members within the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
70346|Marburg Formation, Upper|60993|5|Briefly described|p6 Fig. 2|||Of Etheridge et al (1985) but name is informal. Unit now divided into Koukandowie Formation and two members within the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
70364|Marburg Formation, upper|60995|6|Mentioned|p67|||Informal term used by Cameron (1970) - see Marburg Formation. ||||||
70365|Marburg Formation, upper""|60995|6|Mentioned|p66|||Informal - see the former Marburg Formation. ||||||
28721|Marburg Sandstone|22601|6|Mentioned|405|Jurassic|Jurassic|||||||
28721|Marburg Sandstone|22757|6|Mentioned|p6||Early Jurassic|Also Table5,p10. 400 m. Ipswich-Moreton Basin||||||
28721|Marburg Sandstone|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
28721|Marburg Sandstone|29385|6|Mentioned|p80|||Part of Bundamba Group, see also P82. Jurassic.||||||
28721|Marburg Sandstone|30058|6|Mentioned|p4|||See also P5||||||
28721|Marburg Sandstone|30302|6|Mentioned|p415|||Refers to McTaggart(1963)||||||
28721|Marburg Sandstone|30455|6|Mentioned|p7|||Jurassic age. See also P17,21||||||
28721|Marburg Sandstone|30458|6|Mentioned|p3|||Jurassic age||||||
28721|Marburg Sandstone|30460|6|Mentioned|p15|||Jurassic age. See also P22||||||
28721|Marburg Sandstone|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
28721|Marburg Sandstone|30698|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
28721|Marburg Sandstone|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||11-JAN-10
28721|Marburg Sandstone|30702|6|Mentioned|Fig.1|||Stratigraphic table||||||
28721|Marburg Sandstone|31248|6|Mentioned|p61|||Refers de Jersey (1963)||||||
28721|Marburg Sandstone|31603|6|Mentioned|Fig. 1|||||||||
28721|Marburg Sandstone|32276|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
28721|Marburg Sandstone|32492|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
28721|Marburg Sandstone|32797|4|Described|Table 4|||Lower Jurassic||||||
28721|Marburg Sandstone|32880|6|Mentioned|p2|||Dev.||||||
28721|Marburg Sandstone|33091|5|Briefly described|p10|||Strat.||||||
28721|Marburg Sandstone|33476|6|Mentioned|Table 6|||Refers Olgers et al. 1972 unpublished||||||
28721|Marburg Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
28721|Marburg Sandstone|34172|6|Mentioned|p51|||Jurassic.||||||
28721|Marburg Sandstone|34287|6|Mentioned|p171|||See also P177. Jurassic||||||
28721|Marburg Sandstone|34452|6|Mentioned|p7|||See also PP13,17||||||
28721|Marburg Sandstone|34998|6|Mentioned|p347|||||||||
28721|Marburg Sandstone|35053|5|Briefly described|p36|||||||||
28721|Marburg Sandstone|35574|6|Mentioned|Table 1|||||||||
28721|Marburg Sandstone|36570|6|Mentioned|p26|||||||||
28721|Marburg Sandstone|37995|6|Mentioned|p62|||||||||
28721|Marburg Sandstone|38373|6|Mentioned|p617|||||||||
28721|Marburg Sandstone|40896|6|Mentioned|p17|||||||||
28721|Marburg Sandstone|40920|6|Mentioned|Fig.2|||||||||
28721|Marburg Sandstone|43907|14|Not recorded|p13|Late Jurassic|Early Jurassic|||||||
28721|Marburg Sandstone|43908|14|Not recorded|p6|||||||||
28721|Marburg Sandstone|43910|14|Not recorded|p1,4,7,19,20|||||||||
28721|Marburg Sandstone|43923|6|Mentioned|p5||Jurassic|||||||
28721|Marburg Sandstone|43924|14|Not recorded|p2,3|||||||||
28721|Marburg Sandstone|43993|14|Not recorded|p95|||Ref. to Swindon 1956,1960.||||||
28721|Marburg Sandstone|43995|14|Not recorded|Tb.p9,Tb.p10,20,56,|||Fig.13||||||
28721|Marburg Sandstone|43996|14|Not recorded|p89|||||||||
28721|Marburg Sandstone|44029|14|Not recorded|p153-154,157,168,|Middle Jurassic|Early Jurassic|Plant fossils.||||||
28721|Marburg Sandstone|44077|14|Not recorded|p298|||||||||
28721|Marburg Sandstone|44084|14|Not recorded|p30,32|Middle Jurassic|Early Jurassic|Ipswich-Moreton Basin.||||||
28721|Marburg Sandstone|44091|14|Not recorded|p56,57,58||Jurassic|||||||
28721|Marburg Sandstone|44098|14|Not recorded|p98|||||||||
28721|Marburg Sandstone|44554|2|Defined|p289-295|||Overlain by Walloon Coal Measures. Fossils rare except Cladophlebis australis and Taeniopteris spatulata, Unio,Unionella?||||||
28721|Marburg Sandstone|44727|14|Not recorded|p303-304|||||||||
28721|Marburg Sandstone|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
28721|Marburg Sandstone|44774|4|Described|p30|||Overlies or is possibly part of Bundamba Group; lower limit not clearly delineated from Ripley Road Sandstone.||||||
28721|Marburg Sandstone|44775|14|Not recorded|p9|||||||||
28721|Marburg Sandstone|44814|14|Not recorded|p485||Early Jurassic|||||||
28721|Marburg Sandstone|44913|14|Not recorded|p53,Fig.1,57,Fig.3|||||||||
28721|Marburg Sandstone|45110|3|Fully described|p83|||See also Fig.5.||||||
28721|Marburg Sandstone|48917|3|Fully described|17|||||||||
28721|Marburg Sandstone|48928|6|Mentioned|p7|||||||||
28721|Marburg Sandstone|48940|6|Mentioned|p24|||O'lies Risdon Stud Fm.||||||
28721|Marburg Sandstone|61392|5|Briefly described|p164 Fig. 1|Early Jurassic|Early Jurassic|||||||07-FEB-11
28721|Marburg Sandstone|68576|6|Mentioned|Q_4: p4|||||||||
28721|Marburg Sandstone|72298|6|Mentioned|p798|||Condamine Valley Sub-basin.||||||
28721|Marburg Sandstone|72921|5|Briefly described|p17, p19.|Middle Jurassic||Described as being part of the Clarence-Moreton Basin, but depositional interpretations are unclear (Exon, 1976). Grades into the Hutton Sandstone on the Kumbarilla Ridge.||||Upper part grades into the Hutton Sandstone on the Kumbarilla Ridge.||
28721|Marburg Sandstone|73113|6|Mentioned|p23|||Surat Basin.||||||
28721|Marburg Sandstone|73200|5|Briefly described|p532 Fig.2, p533, p541 Fig.13, p542|Jurassic|Jurassic|Exposed on the northeast and southeast rim of the Condamine Valley. [Informal unit name?]||||Underlies the Walloon Coal Measures.|Interbedded mudstone and sandstone.|
70419|Marburg Sub-group|61006|6|Mentioned|p279|||Informal version of the name - see Marburg Subgroup.||||||07-APR-14
70407|Marburg Subgroup, upper|60999|6|Mentioned|p164|||Informal - see Marburg Subgroup.||||||
70366|Marburg sequence|60995|6|Mentioned|p53|||Informal reference to parts, or all of, the sandstone overlying the Woogaroo Subgroup (Wells et al 199a). ||||||
70347|Marburgh "Stage"|60993|6|Mentioned|p17|||Name first used by Reid (1921) and superseded by "Marburg Formation" (Whitehouse 1955). ||||||
83961|Marengo Plain Monzogranite|71628|5|Briefly described|p2: 47-49, 57-59|||Named after unpublished Marengo Adamellite of Paul (1984). A Victorian pluton called the Marengo Granodiorite has precedence, so Paul's unit is renamed the Marengo Plain Monzogranite, after a local geographical feature. Has five small sub-circular outcrops, four of which are 'hosted' by the Big Bull Gabbro. Geochemistry described. Has similarities with Dundurrabin and Campground Granodiorites.||Sheep Station Creek Complex.||Intrudes Big Bull Gabbro.|A hybrid, contaminated I-type granite. Grey, heterogeneous, equigranular to porphyritic, biotite(+/- amphibole) monzogranite; locally contains abundant enclaves and mafic clots.|
77880|Marker Bed Unit|65759|5|Briefly described|p131|||Northern Barrier Ranges, Darling Basin. In Nundooka Sandstone. Braided fluvial lithofacies, predominantly medium to coarse pebbly sandstone, often with a basal lag of quartz pebbles and granules and shale or siltstone intraclasts.||||||
35267|Marmong Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
30731|Maroubra sandstone|43358|14|Not recorded|p57||Triassic|||||||
77166|Marrangaroo Formation|68003|6|Mentioned|p41.|Late Permian|Late Permian|Western Sydney Basin. A braided fluvial wedge. See also Marrangaroo Conglomerate p38.||||||11-SEP-12
77166|Marrangaroo Formation|68004|5|Briefly described|p59, p60 Table 6.|Late Permian|Late Permian|Western Coalfield. Forms characteristic benches several metres high.||Basal unit in Cullen Bullen Subgroup.||Overlies Gundangaroo Formation. Is overlain by Lithgow Coal.|Upward-fining units of quartz-lithic to quartzose pebbly sandstone.|
35762|Marrawarra Rhyolite|23859|5|Briefly described|p931 Fig 3|||See Marrawarra Rhyolite Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
30951|Martin's Creek Andesite|43432|14|Not recorded|p206|||Kuttung facies||||||
30951|Martin's Creek Andesite|43446|14|Not recorded|p6048||Visean|||||||
30964|Martin's Creek Andesite Member|43440|14|Not recorded|p37,fig4-3|||||||||
30842|Martin's Creek Beds|43385|14|Not recorded|p177||Visean|||||||
30842|Martin's Creek Beds|44254|14|Not recorded|p78||Early Carboniferous|See also Lexicon. Now part of Gilmore Volcanic Group.||||||
30968|Martin's Creek Hornblende Andesite|43440|14|Not recorded|p66|||||||||
27481|Martins Creek Andesite|31228|6|Mentioned|p78|||Refers Roberts (1961)||||||
27481|Martins Creek Andesite|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27481|Martins Creek Andesite|32869|6|Mentioned|p171|||||||||
27481|Martins Creek Andesite|39308|6|Mentioned|p490|||||||||
27481|Martins Creek Andesite|42547|6|Mentioned|p120|||Permian.||||||
27481|Martins Creek Andesite|45097|6|Mentioned|p18|||Refers Evorndent & Richards (1962). Correlation chart||||||
41632|Martins Creek Ignimbrite Member""|44244|6|Mentioned|p37|||Informal - see Martins Creek Ignimbrite Member.||||||
70501|Martins Creek Member|62095|5|Briefly described|p266|||Abbreviated version of Martins Creek Ignimbrite Member.||||||
31140|Martins Creek beds|43491|14|Not recorded|pVI/5||Carboniferous|||||||
36109|Marulan Suite|23439|5|Briefly described|p124 fig.1|||||||||
36109|Marulan Suite|23549|4|Described|p524|||Compositionally distinct from the Boggy Plain Supersuite, most mafic rocks being less potassic and they are dioritic rather than monzodioritic. Geological Province: Lachlan Fold Belt, at eastern margin.||||||05-APR-05
36109|Marulan Suite|24514|6|Mentioned|p32|||High temperature granites. Geological Province: Lachlan Fold Belt.||||||25-MAY-05
36109|Marulan Suite|68592|6|Mentioned|p1611|||Fourteen plutons of the Arthursleigh Suite were incorrectly referred to as this unit by White et al. (2001).||||||
82572|Maryland River Suite|71628|6|Mentioned|p19:101||||||Maryland River Quartz Monzodiorite.|||
82573|Maryland River complex|71628|6|Mentioned|p16: 1, 3, 8|||Donchak et al. (2007); refers to that part of the Stanthorpe Monzogranite to the NE of the Undercliffe Falls Monzogranite. Now (this study) referred to as Cullendore Syenogranite.||||||
73906|Maryland Suite|63748|5|Briefly described|p34|Late Permian|Permian|Of the Herries Supersuite.||||||07-FEB-11
73906|Maryland Suite|69639|6|Mentioned|p151|||||Herries Supersuite|Includes the Maryland Granite.|||
73906|Maryland Suite|71628|5|Briefly described|p19: 98, 101|||Previously assigned to the Herries Supersuite (Donchak et al., 2007). In this study the Maryland Granodiorite is not assigned to a Supersuite.|||Maryland Granodiorite.|||
28729|Marys Hill Beds|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Of Cooleman Group. Chert, with interbedded limestone, sandstone, shale. BMR map symbol: Sua.||||||
28729|Marys Hill Beds|33325|5|Briefly described|Table 2|||||||||
28729|Marys Hill Beds|37727|6|Mentioned|p70|||Junior synonym for Blue Waterhole Beds.||||||
28729|Marys Hill Beds|45147|6|Mentioned|M77|||See also M102||||||
82769|Mascotte granodiorite|71628|6|Mentioned|p10:4|||Informal name by Shaw (1981) and subsequently used by several workers. Renamed Boxwell Granodiorite (Stroud, 1992) because of priority issues.||||||
30776|Masson Moraine|43344|14|Not recorded|p126|||Quaternary, terminal moraine. Invalid stratigraphic name.||||||02-NOV-06
68982|Mathews Gap Dacitic Tuff Member|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Age: 309 Ma (U-Pb zircon, Roberts et al., 1995).||||||
23771|Matong Granite|42726|5|Briefly described|map legend|Silurian||301.  Of the Dalgety Suite (Dalgety Supersuite).  Formal name not intended. Variation on Matong Granodiorite.||||||09-FEB-05
75527|Matthews Gap Dacite Tuff Member|65107|5|Briefly described|p276, 285, Fig 4 p279, Fig 11 p286-7|Middle Pennsylvianian|Middle Pennsylvianian|Age: 309+/-3 Ma, noted as conventional U-Pb date. Occurs in the Pokolbin Hills, south of the Hunter Thrust. Provides segments that agree with east to west pole path (for the Gresford Block) for the New England Orogen.||||||24-NOV-09
34104|Matthews Gap Dacitic Tuff|22610|5|Briefly described|Fig 5||Westphalian|Age 309 +/- 3Ma||||||
80018|Mauburg Subgroup|69297|5|Briefly described|p487 fig 5.38|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. More than 1000m thick. ||Bundamba Group|Includes the Gatton Sandstone and the Koukandowie Formation.|||
42276|Maules Creek formation|24313|6|Mentioned|p22|Permian|Permian|Middle Permian.||||||30-NOV-04
42226|McCarty's limestone lens|50088|6|Mentioned|p467|||Informal name. Conodonts present.||||||24-FEB-05
23779|McKeahnie Adamellite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Gingera Batholith. Intrusive. Adamellite. S-type. BMR map code: Sgk.||||||
23779|McKeahnie Adamellite|39660|6|Mentioned|p450|||||||||
23779|McKeahnie Adamellite|45147|2|Defined|M216|Late Silurian|Late Silurian|Probably Late Silurian.||||||
32261|McKeanhie Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab4. Misspelling of McKeahnie Adamellite.||||||
32261|McKeanhie Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
25221|McLaughlans Flat Granite|42726|5|Briefly described|map legend|Silurian||290.Variation/misspelling of McLaughlins Flat Granodiorite?||||||
82770|McLeods Creek Monzogranite Phase|71628|5|Briefly described|p11: 3, 26-27, 30, 32-34|||New name, after Mustard (2004). Named after a local watercourse. Outcrop area is ~168 km2 about 40 km E of Tenterfield, on the Timbarra Tableland. Geochemistry briefly described.||Rocky River Monzogranite.||Abuts Ewingar Monzogranite Phase gradationally and Sandy Creek Monzogranite.|Medium- to very coarse-grained, porphyritic, pink K-feldspar megacrystic (up to 60mm, average 25mm), hornblende-biotite-quartz poor, plagioclase-rich monzogranite to granodiorite; enclaves locally abundant. Contains abundant ferromagnesian minerals.|
29732|Meadows Formation|43032|6|Mentioned|p154|||Misspelling of Meadows Tank Formation?||||||
29732|Meadows Formation|43500|14|Not recorded|Map Legend|||(Provisional Edition) (no card)||||||
30748|Meadows Sandstone""|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
27485|Meadows Tank Conglomerate|29987|4|Described|p23|||||||||
27485|Meadows Tank Conglomerate|32619|6|Mentioned|p459|||||||||
27485|Meadows Tank Conglomerate|34057|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27485|Meadows Tank Conglomerate|34449|6|Mentioned|p128|||||||||
27485|Meadows Tank Conglomerate|34469|6|Mentioned|p107|||Table. Upper Devonian||||||
27485|Meadows Tank Conglomerate|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27485|Meadows Tank Conglomerate|35925|6|Mentioned|p5|||Refers Bryan 1968||||||
27485|Meadows Tank Conglomerate|41821|6|Mentioned|p55|||Modified to Meadows Tank Sandstone 1979 and to Meadows Tank Formation 1987||||||
27485|Meadows Tank Conglomerate|42467|5|Briefly described|Map Legend|||||||||
27485|Meadows Tank Conglomerate|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
27485|Meadows Tank Conglomerate|43380|14|Not recorded|Map Legend|||Unit of Mulga Downs Group||||||
27485|Meadows Tank Conglomerate|43381|14|Not recorded|Map Legend||Late Devonian|Mulga Downs Group||||||
27485|Meadows Tank Conglomerate|43389|14|Not recorded|Map Legend||Late Devonian|||||||
27485|Meadows Tank Conglomerate|43398|14|Not recorded|Map Legend||Late Devonian|Part of Mulga Downs Group||||||
27485|Meadows Tank Conglomerate|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
30739|Megalong Formation|43360|14|Not recorded|Map Legend|||(Provisional first edition)||||||
26732|Melbergen Sandstone Member|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Womboyne Formation (Cocoparra Group). Orthoquartzite, quartz arenite.||||||10-MAR-06
26732|Melbergen Sandstone Member|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26732|Melbergen Sandstone Member|34109|4|Described|Table 3.12|||||||||
26732|Melbergen Sandstone Member|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26732|Melbergen Sandstone Member|43511|14|Not recorded|p131-2,134,141-4,147||Late Devonian|Overlain by Stitts Member.  p148.||||||25-MAR-08
26732|Melbergen Sandstone Member|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. part of the Womboyne Formation, O/lies the Confreys Shale Member, U/lies the Jimberoo Member. Upper Devonian.||||||
26732|Melbergen Sandstone Member|61964|5|Briefly described|p114|||Of Conolly (1962)  - middle subunit in Mountain Creek Formation of the Cocoparra Group (written as "Melbergen Sandstone Member"). Overlain by Stitts Member and underlain by "Confreys Shale Member". Later, the formation was renamed "Womboyne Formation"||||||14-OCT-08
80158|Melville Chert""|70601|5|Briefly described|p43-45, p47-52|Warendan|Middle Cambrian|Informal term for chert at Melville Point, basal in the Albury-Bega basin succession, to avoid confusion with Narooma Chert in the Narooma Terrane. The (informal) name "Melville Formation" confusingly appears on p52 and probably refers to this unit. Also appears without inverted commas on p49 and p52. Overlain by Adaminaby Group.||||Underlies Adaminaby Group. Conformably overlies "Tomakin Basalt". The upper part is correlated with the upper part of Howqua Chert.|500 m-wide band of black siliceous mudstone with minor chert; mafic lithic sandstone.|
77167|Melville Coal Seam|68003|6|Mentioned|p44 Photo.3-g.|||West of Gunnedah.||||||
76164|Menamurtee Dome Sequence|66623|6|Mentioned|p210, 209|||Neef et al. (1996). Not a formal name; see Menamurtee Sandstone.||||||
70145|Menamurtee Dome sequence|23336|3|Fully described|p5, p7 Fig. 4|||Also referred to as Memamurtee Dome Sequence. Of Mulga Downs Group. Unfossiliferous fine- to coarse-grained sublitharenite and quartzarenite, with common thin gravel lags composed of white vein quartz and grey quartzite pebbles.). Max. thickness: 700m.||||||21-MAR-06
41308|Merimbaga Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
42043|Meringi Gap Conglomerate Member|61964|5|Briefly described|p14 Fig. 4, p117 Fig. 35|Frasnian|Frasnian|Misspelt? - place name is Merungi. Of the Naradhan Sandstone (Cocoparra Group).||||||23-OCT-08
40467|Merlewood andesites|24603|6|Mentioned|p883|||Informal - see Merlewood Formation.||||||
38845|Merrere Conglomerate Member|22857|4|Described|p414 App. 1 Tb. A1.5|Gisbornian|Darriwillian|Of the Ballast Formation. Sandstone, pebbly sandstone, polymictic to oligomictic conglomerate, rare cobbles and boulders in conglomerate, siltstone. Geological Province: Canbelego Block. ||||||
38845|Merrere Conglomerate Member|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
38845|Merrere Conglomerate Member|67322|5|Briefly described|p39|Silurian|Silurian|Formalised by Scheibner and Basden (1998) as a Member of the Ballast Formation, this unit is now regarded as a basal conglomerate of the Cobar Supergroup (Glen et al. 2010).||||||22-FEB-18
38845|Merrere Conglomerate Member|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|Stated as "previously within the Ballast Formation". The location of this unit in the map legend implies that it is a unit within the Meryula Formation, but certainly within the Kopyje Group; it is mapped in the same unit as Meryula Formation, "Little Mountain Formation", and conglomerates of Brookong Formation and Drysdale Conglomerate Member extending from the Cobar 1:100 000 map sheet area.||Kopyje Group.||||
26735|Merriangaah Formation|22968|6|Mentioned|P108|||Parent is Yalmy Group||||||
26735|Merriangaah Formation|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
27833|Merricumbene Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Leucocratic hornblende granodiorite. BMR map symbol: gz.||||||
27833|Merricumbene Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27833|Merricumbene Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
27833|Merricumbene Granite|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
27833|Merricumbene Granite|33325|6|Mentioned|p19|||||||||
27833|Merricumbene Granite|40276|6|Mentioned|p14|||||||||
27833|Merricumbene Granite|40328|4|Described|p208|||||||||
27833|Merricumbene Granite|42726|5|Briefly described|map legend|Early Devonian||96.  Of the Merricumbene Suite (Cobargo Supersuite).  Formal name not intended.||||||09-FEB-05
79206|Merrigan Black Shale|68592|6|Mentioned|p338|||Felton and Huleatt (1975). Canberra 1:250 000 map sheet area.||||Probably equivalent to Warbisco Shale.||
35486|Merriganowry Beds|23217|6|Mentioned|p6|||Included in the top of the Dulladerry Volcanics beneath the Hervey Group by Pogson and Watkins (1998).||||||08-MAR-06
36196|Merriganowry Member|23392|6|Mentioned|p7||Givetian|Of Dulladerry Volcanics. Possible correlation with basal part of Peaks Formation.||||||
38549|Merrions Formation, lower|24394|6|Mentioned|p174, p178|||Not intended as a formal name - see Merrions Formation.||||||
38552|Merrions Formation, middle|24394|6|Mentioned|p174|||Not intended as a formal name - see Merrions Formation.||||||
38553|Merrions Formation, upper|24394|6|Mentioned|p178|||Not intended as a formal name - see Merrions Formation.||||||
27834|Merrions Tuff|22472|6|Mentioned|p35|Devonian|Devonian|current name Merrions Formation||||||
27834|Merrions Tuff|22590|6|Mentioned|Fig3 P754||Pragian|||||||
27834|Merrions Tuff|23039|6|Mentioned|p166,7|Devonian|Silurian|||||||
27834|Merrions Tuff|23214|6|Mentioned|p186|||Superseded by Merrions Formation.||||||
27834|Merrions Tuff|24278|6|Mentioned|p1765 Fig. 1|||See also Merrions tuff.||||||
27834|Merrions Tuff|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
27834|Merrions Tuff|30099|4|Described|p381|||||||||
27834|Merrions Tuff|30100|6|Mentioned|p205|||Dates on P205||||||
27834|Merrions Tuff|31161|5|Briefly described|PA4|||||||||
27834|Merrions Tuff|31706|6|Mentioned|p645|||Devonian correlation chart||||||
27834|Merrions Tuff|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
27834|Merrions Tuff|32046|6|Mentioned|p140|||See also P254,255,265||||||
27834|Merrions Tuff|32047|6|Mentioned|p18|||Refers gold mineralization||||||
27834|Merrions Tuff|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
27834|Merrions Tuff|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
27834|Merrions Tuff|32672|6|Mentioned|p673|||||||||
27834|Merrions Tuff|33006|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27834|Merrions Tuff|33282|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27834|Merrions Tuff|33285|6|Mentioned|p22|||Early Dev.||||||
27834|Merrions Tuff|33326|6|Mentioned|p444|||Fauna.||||||
27834|Merrions Tuff|33732|5|Briefly described|p116|||Table II||||||
27834|Merrions Tuff|34059|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27834|Merrions Tuff|34403|4|Described|p131|||See also P136||||||
27834|Merrions Tuff|34404|6|Mentioned|Fig.3.4b|||||||||
27834|Merrions Tuff|34405|6|Mentioned|Fig.3.9|||||||||
27834|Merrions Tuff|34406|6|Mentioned|p223|||||||||
27834|Merrions Tuff|35072|6|Mentioned|p363|||||||||
27834|Merrions Tuff|35185|6|Mentioned|p245|||||||||
27834|Merrions Tuff|37490|6|Mentioned|p279|||||||||
27834|Merrions Tuff|37746|6|Mentioned|Notes|||||||||
27834|Merrions Tuff|37748|6|Mentioned|Map legend|Early Devonian|Silurian|Middle and Early Devonian and Silurian.||||||
27834|Merrions Tuff|37806|6|Mentioned|p46|||||||||
27834|Merrions Tuff|38216|5|Briefly described|p253|||||||||
27834|Merrions Tuff|39214|6|Mentioned|p23|||||||||
27834|Merrions Tuff|39331|6|Mentioned|p71|||||||||
27834|Merrions Tuff|40328|6|Mentioned|Plate 4|||||||||
27834|Merrions Tuff|41207|5|Briefly described|Table 1|||||||||
27834|Merrions Tuff|41799|4|Described|p471|||||||||
27834|Merrions Tuff|42051|6|Mentioned|p137|||||||||
27834|Merrions Tuff|42380|4|Described|p365|||||||||
27834|Merrions Tuff|42726|5|Briefly described|map legend|Early Devonian||||||||
27834|Merrions Tuff|42820|5|Briefly described|p15|||||||||
27834|Merrions Tuff|43127|5|Briefly described|p4,Fig.2,Fig.3||Early Devonian|||||||
27834|Merrions Tuff|43263|6|Mentioned|Map Legend||Early Devonian|||||||
27834|Merrions Tuff|43344|14|Not recorded|p139,148,150,153,154|Early Devonian||||||||
27834|Merrions Tuff|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
27834|Merrions Tuff|43461|14|Not recorded|Table p621,622||Siegenian|||||||
27834|Merrions Tuff|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
27834|Merrions Tuff|43494|6|Mentioned|p27|Devonian|Devonian|Superseded by Merrions Formation.||||||16-MAR-06
27834|Merrions Tuff|43515|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
27834|Merrions Tuff|43516|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
27834|Merrions Tuff|43517|14|Not recorded|p111-2,123-163,|||Overlies Waterbeach Formation. Map plates XII||||||
27834|Merrions Tuff|43519|14|Not recorded|Table p119|||||||||
27834|Merrions Tuff|43525|14|Not recorded|map p124,Tb p126-7||Siegenian|||||||
27834|Merrions Tuff|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Of the Crudine Group. See also p213 Appendix 1. Geological Province: Lachlan Fold Belt.||||||
27834|Merrions Tuff|63519|6|Mentioned|p22|Silurian|Silurian|In Hill End Trough.||||||11-JUN-08
27834|Merrions Tuff|64296|5|Briefly described|p84 Tb. 1|||||||||
27834|Merrions Tuff|68592|6|Mentioned|p1147|||Later renamed Merrions Formation (see references p1038, p1059).||||||
27834|Merrions Tuff|71924|6|Mentioned|p2, 3|||Hill End Trough? Includes sparse fossil fauna. May correlate with basal part of Mullamuddy Formation.||||||
25230|Merrions Tuff Formation|39331|6|Mentioned|Fig.7-1|||||||||
37434|Merrions Tuff""|23214|6|Mentioned|p193|||Superseded by Merrions Formation.||||||
38253|Merrions formation|23738|6|Mentioned|p252|||Informal name - see Merrions Formation.||||||
69186|Merrions tuff|24278|5|Briefly described|p1765|||Informal - see Merrions Tuff. Overlies Crudine Group.||||||
26736|Merton Hornfels|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
26736|Merton Hornfels|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
26736|Merton Hornfels|40328|4|Described|p128|||||||||
26736|Merton Hornfels|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
23789|Merumbadgee Granite|42726|5|Briefly described|map legend|Silurian||304.  Of the Dalgety Suite (Dalgety Supersuite).  Formal name not intended. Variation on Merumbadgee Adamellite.||||||09-FEB-05
24379|Micaligo Adamellite|36413|2|Defined|p94|Devonian|Devonian|||||||
24379|Micaligo Adamellite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Michelago Igneous Complex. Biotite-hornblende adamellite. GSNSW map code: gcc.||||||
24379|Micaligo Adamellite|39626|6|Mentioned|p276|||||||||
24379|Micaligo Adamellite|40328|4|Described|p209|||||||||
26737|Micaligo Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Micaligo Adamellite.||||||
28749|Micalong Basic Igneous Complex|42820|5|Briefly described|p76|||||||||
78491|Micalong Swamp Basic Igneous Suite|66768|6|Mentioned|p209|||Said to be of Collins and Hobbs (2001). [Listed as 'Complex' in ASUD.] Sourced from subduction-related mafic melts in the Silurian.||||||07-NOV-13
37283|Micalong Swamp Complex|24005|6|Mentioned|p293|||||||||
37283|Micalong Swamp Complex|73483|6|Mentioned|p407 Fig.1|||||||||
36125|Micalong Swamp Igneous Complex|23454|5|Briefly described|p33|Silurian|Silurian|ca. 430Ma||||||
25234|Michelago tuff|40328|6|Mentioned|p62|||||||||
41561|Mickety Mulga unit|50616|4|Described|p280-281|Pliocene|Late Miocene|Informally named gravel, sand and clay in the Gobolion area - distinctive stratigraphic unit not yet formally designated as a formation. Conformably overlies the Eurombedah unit; unconformably underlies the Bunglegumbie unit.||||||
78520|Middle Brother Diorite|68111|6|Mentioned|p970 Fig.2|Triassic|Triassic|Late Triassic ? age.||||||
78520|Middle Brother Diorite|71628|6|Mentioned|p17:80|||Li et al. (2012). Now the Middle Brother Granodiorite.||||||
81829|Middle Brother Monzodiorite|69188|5|Briefly described|p1-2, p4, p7, p11|Late Triassic|Late Triassic|One of the "coastal granitoids" east of the central axis granites of the New England batholith. See also references to Middle Brother monzodiorite (p7-10, p79).|212.5 +/- 1.6 Ma (magmatic age)|||||16-APR-20
81829|Middle Brother Monzodiorite|73570|5|Briefly described|p911, p918|Late Triassic|Late Triassic|Intrudes the Lorne Basin.|212.5+/-1.6 Ma SHRIMP U-Pb zircon||||A-type granites.|
80788|Middle Brother Monzogranite|69639|5|Briefly described|p223|Norian|Norian||212.3 +/- 1.7 Ma (Cross and Blevin, 2013)|||||06-MAR-19
80913|Middle Brother monzodiorite|69188|5|Briefly described|p7-10, p79|Late Triassic|Late Triassic|An informal name for a sample of the Middle Brother intrusion of The Brothers Granitoids. Previously (McDougall and Wellman, 1976) dated at 205 +/- 3 Ma. See also references to Middle Brother Monzodiorite (p1-2, p4, p7, p11).|212.5 +/- 1.6 Ma (magmatic age)||||Grey-white, fine- to medium-grained, mildly to sparsely porphyritic, two pyroxene monzodiorite. I-type.|16-APR-20
80913|Middle Brother monzodiorite|71628|6|Mentioned|p17:80|||Cross and Blevin (2013). Now Middle Brother Granodiorite.||||||
35159|Middle Camp Formation|23055|6|Mentioned|Fig13 p25|||||||||17-APR-14
31278|Middle Clarence Beds|43491|14|Not recorded|no card|||(no card)||||||
30732|Middle Hawkesbury Sandstone|43358|14|Not recorded|p48||Triassic|||||||
30930|Middle Luton Formation|43417|14|Not recorded|Map Legend|||||||||
34734|Middle Renmark Group|22893|6|Mentioned|p25|Tertiary|Tertiary|||||||
37950|Middle Schist|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
32537|Middle Trilobite Bed""|33117|6|Mentioned|p.83-99.|||Ludlow-Downton.||||||13-JAN-17
32537|Middle Trilobite Bed""|61120|6|Mentioned|p11.|||At Bowning, NSW. Not a formal name. Etheridge and Mitchell (1896) stated Paciphacops latigenalis came from this unit.||||||
32537|Middle Trilobite Bed""|68592|5|Briefly described|p429, 590, 594, 1883|||Of Mitchell (1888). Former name for Rainbow Hill Member. Shown as Middle trilobite bed in fig 89 p429.||||||13-JAN-17
80255|Mile Road Beds|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
70357|Mill Creek "Siltstone"|60995|5|Briefly described|p53 Fig. 4|||Of Ellice-Flint (1973) as part of his "Pillar Valley Subgroup". Replaced later by Wooli Road Formation (Morrison 1984). Now incorporated into Ripley Road Sandstone / Raceview Formation units.||||||
26739|Mill Creek Siltstone Member|29988|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
70358|Mill Creek Siltstone""|60995|6|Mentioned|p55, p56 Fig. 7|||Referred to as Raceview Formation equivalents. Of McElroy (1963). ||||||
81359|Millfield Farm member""|70096|5|Briefly described|p220-221;Supp1-3|Cisuralian|Cisuralian|Of northern Sydney Basin. Thickness: 5m. Informal name used in this study. See also supplementary files in appendix for additional stratigraphic and locality information.||Unit of Dalwood Group.||Overlain by Farley Formation.|Fossiliferous lithic-feldspathic pyroclastic sandstone .|08-AUG-19
34266|Millimbri Formation|22679|6|Mentioned|p 21|||||||||
29210|Millsville Beds|40106|6|Mentioned|p593|||||||||
35439|Millsville beds""|23170|6|Mentioned|p71|||Superseded by Millsville Formation.||||||
73690|Millthorpe Group|63283|6|Mentioned|p186 Tb. 1, p191 Tb. 2, p195 Fig. 2|Late Ordovician|Late Ordovician|Age: 445Ma ( evolved basalt). Geological Province: Molong Volcanic Belt.||||||07-FEB-11
76165|Milparinka Group|66623|6|Mentioned|p99, 105 |||A division (Andrews 1922) of Torrowangee Series.||Unit in Torrowangee Series.||||
26031|Milpose Volcanics|22466|6|Mentioned|P9||Early Devonian|||||||
26031|Milpose Volcanics|22831|6|Mentioned|p 42|||||||||
26031|Milpose Volcanics|23522|5|Briefly described|p253|Devonian|Devonian|||||||
26031|Milpose Volcanics|24267|4|Described|p1508||Early Devonian|Overlying Unit: Hervey Group. Underlying Unit: Forbes Group. Geological Province: Parkes-Narromine Belt||||||
26031|Milpose Volcanics|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|Prob.Early Devonian||||||
26031|Milpose Volcanics|29910|6|Mentioned|Map legend|Devonian|Devonian|||||||
26031|Milpose Volcanics|35244|6|Mentioned|p36|||||||||
26031|Milpose Volcanics|36066|6|Mentioned|p6|||||||||
26031|Milpose Volcanics|36283|6|Mentioned|p109|||||||||
26031|Milpose Volcanics|36411|6|Mentioned|p269|||Refers Bowman 1977.||||||
26031|Milpose Volcanics|38230|5|Briefly described|p474|||Palaeontology||||||
26031|Milpose Volcanics|39663|6|Mentioned|Table 1|||||||||
26031|Milpose Volcanics|40328|3|Fully described|p41|||||||||
26031|Milpose Volcanics|40365|6|Mentioned|p241|||||||||
26031|Milpose Volcanics|40891|3|Fully described|p20|||||||||
26031|Milpose Volcanics|42262|6|Mentioned|Fig. 2 P1810|||||||||
26031|Milpose Volcanics|42449|6|Mentioned|p11|||||||||
26031|Milpose Volcanics|42456|6|Mentioned|p4|||in Derriwong Group||||||
26031|Milpose Volcanics|42489|5|Briefly described|Map legend|Lochkovian||||||||
26031|Milpose Volcanics|42714|5|Briefly described|Fig.1 P25|Late Silurian||||||||
26031|Milpose Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
26031|Milpose Volcanics|43441|6|Mentioned|26|Early Devonian|Late Silurian|||||||08-JAN-10
26031|Milpose Volcanics|46522|3|Fully described|p66|||||||||
26031|Milpose Volcanics|46524|5|Briefly described|p104|||See also Appendix 1 P129||||||
26031|Milpose Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
26031|Milpose Volcanics|46528|5|Briefly described|Map legend|Early Devonian||||||||
26031|Milpose Volcanics|63291|6|Mentioned|p419 Fig. 2|||||||||
26031|Milpose Volcanics|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
79207|Milthorpe Volcanics|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
36361|Milton Complex|23544|5|Briefly described|p372|||Age: 245+/-6Ma K-Ar whole rock (Facer and Carr, 1979). In the Sydney Basin||||||13-JUN-13
36361|Milton Complex|67663|6|Mentioned|p519 Fig.1|||See reference to Milton Monzonite (p518, p524 Fig.4, p535).||||||
36361|Milton Complex|73197|6|Mentioned|p475 Fig.6, p478|Lopingian|Guadalupian|Attributed to the Currarong Arc.|||||Mafic intrusives.|
36361|Milton Complex|73421|4|Described|p1, p2 Fig.1, p5, p7, p10-11, p15-17|Roadian|Kungurian|Sydney Basin, southern. Exposed in the vicinity of Milton, contacts are poorly exposed. Consists of a central core with monzonitic laccolithic sills and dykes emplaced into surrounding strata. Based on previous studies, possibly contemporaneous with deposition of the Wandrawandian Siltstone. Mineralogy indicates an oxidised, hydrous melt, emplaced at a high crustal level. Location in text includes p12 Fig.7, p14 Fig.12. Milton monzo-diorite used p14 Tb.2.|275.5+/-4.3 Ma U-Pb zircon|||Intrudes Snapper Point Formation, and interpretedly the Wandrawandian Siltstone|Mafic monzonitic intrusion, porphyritic to equigranular. Dominant lithology is medium- to coarse-grained monzo-diorite, weakly plagioclase-phyric. Contains spidery/diffuse felsic segregations in places, and rare felsic veins of monzonite.|
22336|Milton Grove beds|44188|5|Briefly described|Map Legend|Late Devonian|Early Devonian|Of the Mulga Downs Group. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Medium- to fine-grained, red-brown quartz arenite to litharenite forming resistant beds.||||||15-MAY-08
31013|Milton Monzanite|43465|14|Not recorded|Map Legend||Mesozoic|||||||
31013|Milton Monzanite|43981|4|Described|p7,29|||||||||
68983|Milton monzonite""|60299|6|Mentioned|p224|||||||||
83564|Minamurra Latite|73304|6|Mentioned|p74|||[Probably misspelt from Minnamurra Latite, which was superseded by Minnamurra Latite Member]. Sydney Basin, southern.||Illawarra Coal Measures||||
33947|Minamurra Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
33947|Minamurra Latite Member|67500|5|Briefly described|p12 Tb.1|||[Typo for Minnamurra]. Up to 37m thick.||Of the Pheasants Nest Formation and Gerringong volcanic facies.|||Glomeroporphyritic flow with phenocrysts of labradorite.|01-MAY-12
83254|Mine Dyke Group|73431|5|Briefly described|p363 Fig.1, p367 Tb.1, p372|Silurian|Silurian|Previous U/Pb SHRIMP zircon ages of 436.2+/-5.2 and 437.1+/-5.9 Ma from Kovacs (2000). Misspelt as Ming Dyke Group p364?|436.2+/-5.2 and 437.1+/-5.9 Ma zircon U/Pb SHRIMP|||Equivalent to Browns Creek dykes?||
42329|Mine granite|24271|5|Briefly described|p1620|Late Silurian|Late Silurian|Geological Province: Wagga tin belt. Age: 417+/-2.5 Ma. Of the Koetong Supersuite.||||||07-DEC-04
39620|Mine schist|24087|5|Briefly described|p329|||Informal name.   Geological Province: Lachlan Fold Belt.||||||
39620|Mine schist|24196|6|Mentioned|p69 Fig.10|||Informal name for schist located in the East Agnew-Mount Clifford sub-domain, Yilgarn Craton in Western Australia.||||||
34616|Minemoorong Intrusive Complex|22831|4|Described|p23||Ordovician|||||||01-NOV-13
28754|Mineral Hills Volcanics|42726|5|Briefly described|map legend|Silurian||Misspelling of Mineral Hill Volcanics.||||||
32240|Mingary Volcanics|44092|5|Briefly described|map legend|Early Devonian|Early Devonian|Dlv1. Misspelling of Minjary Volcanics.||||||
32240|Mingary Volcanics|60078|6|Mentioned|Map Legend|Early Devonian|Early Devonian|||||||
70622|Mingary group|62373|5|Briefly described|p511|||Informal group in the metabasite suite of the Curnamona Province - Lady Louise Suite, Broken Hill Domain.||||||
28227|Mingelo Dacite|22831|6|Mentioned|p 26|||||||||
28227|Mingelo Dacite|40365|2|Defined|p327|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
28755|Mingelo Dacite""|46522|5|Briefly described|p38|||Renamed as Mingelo Volcanics||||||
30833|Minnamurra Dolerite|43344|14|Not recorded|p77|||||||||
27488|Minnamurra Falls Tinguaite|36220|4|Described|p97|||||||||
27488|Minnamurra Falls Tinguaite|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic||||||
27488|Minnamurra Falls Tinguaite|37253|6|Mentioned|Table 1|||||||||
30929|Minto Limestone Member|43417|14|Not recorded|Map Legend|||Equivalent of Lilberne Beds||||||
30654|Minumurra Falls Tinguaite|43346|14|Not recorded|p4 Map||Eocene|||||||
30654|Minumurra Falls Tinguaite|43349|14|Not recorded|Map|||||||||
31092|Minumurra latite|43477|14|Not recorded|p24|||(Illawarra Coal Measures)||||||
30777|Minyon Falls Rhyolite|22582|6|Mentioned|p73|||||||||
30777|Minyon Falls Rhyolite|43344|14|Not recorded|unknown|||No reference recorded on card||||||
30777|Minyon Falls Rhyolite|43881|14|Not recorded|p56||Tertiary|Now known as Minyon Falls Rhyolite Member.||||||
41067|Mirani Monzogranite""|24366|6|Mentioned|p8 Fig. 6|||||||||
82575|Mirani Suite|71628|5|Briefly described|p3:75|||||Hillgrove Supersuite.|Mirani Monzogranite.|||
41068|Mirani monzogranite""|24366|5|Briefly described|p11 Photo. 1|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41068|Mirani monzogranite""|71628|6|Mentioned|p3:75|||Brown (2003). Formalised in this study.||||||
41649|Mirannie Felsite""|44244|6|Mentioned|p109|||Superseded by Mirannie Volcanic Member.||||||
74171|Mirannie Ignimbrite|61768|6|Mentioned|p83 Fig. 2|||Of Seaham Formation.||||||13-MAY-08
40468|Mirannie Ignimbrite Member|24603|5|Briefly described|p897 Fig. 17|Carboniferous|Carboniferous|Of the Seaham Formation.  Age: 321.3+/-4.4Ma (Roberts et al, 1995b).  Geological Province: Tamworth Belt.  In the Gresford Block.||||||
40468|Mirannie Ignimbrite Member|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|of the Seaham Formation. Geological Province: Rouchel Block/Tamworth Belt.||||||
40468|Mirannie Ignimbrite Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Seaham Formation||||
80401|Mirool porphyry|70777|6|Mentioned|p24|||Informal name of Chappell (1999), for outcrops in the Beckom Rest Area. SHRIMP analysis shows that this sample is part of the Wallaroobie Volcanics.||||||07-FEB-18
68984|Mirranie Volcanic Member|60299|5|Briefly described|p208|Carboniferous|Carboniferous|Of Seaham Formation. Age: 321 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Gresford Block.||||||
35493|Mitchell Breccia""|23170|6|Mentioned|p23|||Now the Mitchell Formation.||||||
35493|Mitchell Breccia""|23213|6|Mentioned|p10|||of Wolf et al(1968). now Mitchell Formation.||||||
38190|Mitchell Cave Beds|23555|5|Briefly described|p6, p7 Tb. 1|Pleistocene|Pleistocene|||||||
35492|Mitchell Grit""|23170|6|Mentioned|p23|||Now the Mitchell Formation.||||||
35492|Mitchell Grit""|23213|6|Mentioned|p10|||of Kenmezys (1959). now Mitchell Formation.||||||
30780|Mittagong Formation""|43344|14|Not recorded|p22,61,64||Triassic|Basal unit of Wianamatta Group||||||
34580|Mittagong Gneiss""|22815|6|Mentioned|p30|||Name has been superseeded||||||
82578|Moggs Swamp Suite|71628|6|Mentioned|p19:105||||||Moggs Swamp Complex.|||
76166|Mokely Creek Sandstone member|66623|6|Mentioned|p254.|||Morton (1982). Informal name. Equivalent to Wyandra Sandstone Member of Cadna-owie Formation.||||||
73958|Mole Suite|69639|6|Mentioned|p38|||New England Orogen.||Mole Supersuite||||
73958|Mole Suite|70217|6|Mentioned|p55|||New England Orogen.||Mole Supersuite|Includes the Dumboy-Gragin Granite, Mole Granite, Elsmore Granite and the Gilgai Granite.|||
73958|Mole Suite|71628|5|Briefly described|p19:113|||Waltenberg et al. (2015) included the Mole Syenogranite (now Mole Leucogranite) within the Mole Supersuite. This study regards the Mole Leucogranite as distinctive, and does not assign its Suite to a Supersuite.|||Mole Leucogranite.|||
73955|Mole Supersuite|68111|5|Briefly described|p968 Tb.1||||||Includes Mole Granite and Dumboy-Gragin Granite.|||
73955|Mole Supersuite|69639|5|Briefly described|p1-p2, p38, p221|||New England Orogen.|||Includes the Mole Suite, Elsmore Granite and the Gilgai Granite.|||
73955|Mole Supersuite|70217|5|Briefly described|v, p55, p74 tbl 14.1, p75|||New England Orogen. Hosts tin mineralisation of predominantly early Triassic age. |||Includes the Mole Suite, Elsmore Granite and the Gilgai Granite.|||
73955|Mole Supersuite|71628|6|Mentioned|p19:113|||Waltenberg et al. (2015) included the Mole Syenogranite (now Mole Leucogranite) within this unit. This study regards the Mole Leucogranite as distinctive, and does not assign its Suite to a Supersuite.||||||
82772|Mole Syenogranite|71628|5|Briefly described|p19:113|||Waltenberg et al. (2015) included the Mole Syenogranite (now Mole Leucogranite) within the Mole Suite and Supersuite. This study regards the Mole Leucogranite as distinctive, and does not assign its Suite to a Supersuite.||Mole Suite.||||
40249|Mole group|38842|6|Mentioned|p290|||Geological Province: New England Fold Belt. Age: 225 +/- 10Ma||||||
40249|Mole group|71628|6|Mentioned|p15:83|||Flinter (unpublished, 1981). Now Ruby Creek Leucogranite.||||||
34523|Molineaux Sands""|22799|6|Mentioned|p46|||||||||
37402|Molong Beds|23214|5|Briefly described|p123|||||||||
39801|Molong limestone|24247|6|Mentioned|p45|Silurian|Silurian|||||||
31051|Molonglo Hornfels|44970|14|Not recorded|p78 (table 4)|||||||||
35424|Mona Vale Siltstone""|23170|6|Mentioned|p48|||Of Vandyke & Byrnes (1976).||||||
40788|Monarco Volcanics|50126|6|Mentioned|p83 App.2|||Misspelt - see Monaro Volcanics.||||||
25251|Monaro Alkaline Volcanics|31644|4|Described|p93|||?Primary magmas. See also P94-108||||||
30215|Monaro Basalts""|43126|6|Mentioned|p1|||Now Monaro Volcanics.||||||
69643|Monaro Province Volcanics|61155|5|Briefly described|p19|Early Oligocene|Early Eocene|Includes Tomboye Basalt. In Southeastern NSW.||||||
30214|Monaro alkaline volcanics""|22815|6|Mentioned|p108|||Renamed Monaro Volcanics.||||||
30214|Monaro alkaline volcanics""|43126|6|Mentioned|p1|||Of Kesson 1973. Now Monaro Volcanics.||||||
75046|Monaro paleosols|64837|5|Briefly described|p563|||Informal name.  Associated with the Early Eocene Monaro Volcanics.||||||21-APR-09
42211|Monga A-type granite|24456|6|Mentioned|p327|||Informal name.||||||26-NOV-04
35491|Monga beds""|23213|5|Briefly described|Fig.10 p24|||Contains Darriwilian fossils. of Monaro Trough.||||||
24383|Mongamula Adamellite|22857|6|Mentioned|p215|||Geological Province: Lambie Basin.||||||
24383|Mongamula Adamellite|22859|6|Mentioned|p215|||||||||
24383|Mongamula Adamellite|39028|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian to Givetian||||||
24383|Mongamula Adamellite|40276|2|Defined|p22|Late Devonian|Middle Devonian|Middle to Late Devonian||||||
24383|Mongamula Adamellite|42497|5|Briefly described|Map Legend|Givetian|Givetian|||||||
35413|Monivae Formation ""|23170|6|Mentioned|p29|||of Lue Beds.||||||
38248|Monkey Place Creek Tuff|23717|6|Mentioned|p133|||||||||
39824|Monkey Place Tuff Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Charlton Formation. Geological Province: Sydney Basin||||||
39824|Monkey Place Tuff Member|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. The rank 'Member' is missing in Table 5.||Basal unit in Charlton Formation.||Overlies Abbey Green Coal.|Biotite-rich tuffaceous claystone.|
28765|Montrose Seam|29926|6|Mentioned|Fig.3|||||||||
28765|Montrose Seam|29942|5|Briefly described|Fig.2|||||||||
28765|Montrose Seam|36933|6|Mentioned|p50|||||||||
28765|Montrose Seam|38656|6|Mentioned|Fig.1.3.11|||P150||||||
28765|Montrose Seam|39292|6|Mentioned|Fig. 6.2|||||||||
28765|Montrose Seam|41479|6|Mentioned|p93|||See also Fig.2||||||
28765|Montrose Seam|42182|6|Mentioned|p298|||||||||
28765|Montrose Seam|45090|6|Mentioned|p221|||U.Tatarian||||||
78865|Montrose coal seam|68711|5|Briefly described|p118, p116 Tbl 5|||Informal unit.||Within Adamstown Formation||||
70623|Montstephen Metabasalts|62373|5|Briefly described|p502, p503|Statherian|Statherian|Subvolcanic mafic magmatic event. Pillow lavas and amygdaloidal basalts. Intercalated with the Ethiudna Subgroup rocks. Age: 1715-1700Ma.||||||
70623|Montstephen Metabasalts|64316|5|Briefly described|p534|Paleoproterozoic|Paleoproterozoic|Age: 1710-1699Ma. Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
83275|Monza Gabbro|73154|6|Mentioned|p73, p91-93|Miaolingian|Miaolingian|Zircon ages from samples MZ0807 and MZ0810, shown as from Monza Intrusive Complex p78 Tb.1. Juvenile Hf isotope signature. See also Monza gabbro.|503 Ma|||||
83273|Monza Intrusive Complex|73154|5|Briefly described|p77, p78 Tb.1|Wenlock|Miaolingian|Junee-Narromine volcanic belt, buried. Monza intrusive complex on p94. Zircon U-Pb ages of 503.2+/-3.2 Ma and 503.4+/- 3.7 Ma from Monza gabbro samples MZ0807 and MZ0810 interpreted as crystallisation age, samples are shown as being from the Monza Intrusive Complex on p78 Tb.1 and referred to as Monza Gabbro, Monza gabbro and Monza metagabbro in text. 432.1 +/-3.4 Ma age from Monza monzodiorite sample. See also Monza igneous complex p73.|503.4+/- 3.7 Ma, 432.1+/-3.4 zircon U-Pb SHRIMP||||Includes grey quartz monzodiorite to diorite, and coarse-grained gabbro, modified by low-grade metamorphism and hydrothermal alteration.|
41562|Mookerawa basalts|50616|6|Mentioned|p286 Fig. 9||Miocene|Informal name.||||||
70063|Moolarben seam|22857|5|Briefly described|p526 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name for seam in the State Mine Creek Formation (Illawarra Coal Measures). Geological Province: Sydney Basin. See also p528 App.1 TB.A1.9.||||||
39797|Moolayember Formation, lower|24159|6|Mentioned|p148|||Informal - see Moolayember Formation.||||||
76055|Moolyember Formation|65119|5|Briefly described|p503 Fig 2|Middle Triassic|Middle Triassic|Misspelling of Moolayember Formation. Bowen Basin.||||||07-MAR-12
30977|Moon Island Sub-Group|23055|6|Mentioned|Fig11p23|||||||||
30977|Moon Island Sub-Group|43440|14|Not recorded|p34,fig.4-3||Permian|Unit of Newcastle Coal Measures||||||
35216|Moon Island Subgroup|22969|4|Described|Fig 4.1a||Late Permian|||||||
25257|Moona Plains Complex|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Granodiorite, leucogranite, trondhjemite, diorite, gabbro.||||||15-DEC-04
25257|Moona Plains Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
25257|Moona Plains Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25257|Moona Plains Complex|41348|5|Briefly described|Map legend|Early Paleozoic||Granodiorite, leucoadamellite, trondhjemite, diorite, gabbro.||||||07-NOV-08
25257|Moona Plains Complex|71628|4|Described|p2: 3-4, 36-41, 62; p3: 3, 10, 19, 68-69|||Binns et al. (1967). Named after a local homestead. Crops out as numerous small bodies (many too small to appear on maps), ~30 km E of Walcha. Assigned to Bakers Creek Suite by Landenberger (1996) and to Bakers Creek Supersuite by Landenberger et al. (2010). Geochemistry detailed.|289.0 +/- 2.9 Ma (Rosenbaum et al., 2012).|Bakers Creek Supersuite.||Intrudes Agnes Greywacke. Is 'spatially associated' with Kimberley Park Monzogranite.|Mafic igneous complex comprising olivine gabbro, gabbro, diorite, quartz diorite, tonalite, monzogranite and granophyre.|
35868|Moona Vale Conglomerate|23336|4|Described|p10|||||||||21-MAR-06
35868|Moona Vale Conglomerate|67562|6|Mentioned|p105 Fig.11, p113 Fig.16|||See also Moona Vale Conglomerate Member.||||||
35868|Moona Vale Conglomerate|70651|5|Briefly described|Map Legend|Devonian|Devonian|[map symbol suggests this is probably a member of Menamurtee Sandstone, but may be a partial equivalent?]||Menamurtee Sandstone|||Massive, clast-supported conglomerate with rounded to angular clasts to 1.5m diameter, coarse sandstone matrix and rare sandstone lenses.|
70148|Moona Vale Conglomerate Sequence|23336|3|Fully described|p7 Fig. 4, p10|||Also referred to as the Moona Vale Conglomerate sequence. Of the Mulga Downs Group. Basal unit of the group - poorly sorted granule to boulder conglomerate. Max. thickness: up to 250m.||||||21-MAR-06
26749|Moonbah Granite|42726|5|Briefly described|map legend|Silurian||405. Variation on Moonbah Tonalite.||||||
27492|Moonbi Adamellite|22572|6|Mentioned|p108|Permian||||||||
27492|Moonbi Adamellite|22857|6|Mentioned|p242, p264|Late Permian|Late Permian|Age: 248Ma. ||||||
27492|Moonbi Adamellite|22864|6|Mentioned|p264|||||||||
27492|Moonbi Adamellite|24519|5|Briefly described|p89, p90 Fig. 1|Permian|Permian|Of the New England Batholith. I-type pluton. Thickness: average 2-6km (modelled using gravity data).||||||
27492|Moonbi Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
27492|Moonbi Adamellite|30787|6|Mentioned|p49|||Differentiation index||||||
27492|Moonbi Adamellite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
27492|Moonbi Adamellite|31732|6|Mentioned|p16|||Refers dates||||||
27492|Moonbi Adamellite|32482|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
27492|Moonbi Adamellite|34093|4|Described|p278|||||||||
27492|Moonbi Adamellite|34589|6|Mentioned|p272|||||||||
27492|Moonbi Adamellite|34590|6|Mentioned|p300|||||||||
27492|Moonbi Adamellite|34888|6|Mentioned|Fig. 1|||||||||
27492|Moonbi Adamellite|35192|6|Mentioned|Fig.1|||||||||
27492|Moonbi Adamellite|35198|6|Mentioned|p84|||||||||
27492|Moonbi Adamellite|38685|5|Briefly described|p29|Early Permian|Early Permian|Geological Province: New England Fold Belt||||||
27492|Moonbi Adamellite|38842|6|Mentioned|p286|||||||||
27492|Moonbi Adamellite|38905|6|Mentioned|p304|||||||||
27492|Moonbi Adamellite|39214|5|Briefly described|p37|||||||||
27492|Moonbi Adamellite|39240|6|Mentioned|Fig.2|||||||||
27492|Moonbi Adamellite|39441|6|Mentioned|p34|||||||||
27492|Moonbi Adamellite|40816|4|Described|p115|||||||||
27492|Moonbi Adamellite|40883|6|Mentioned|p14|||||||||
27492|Moonbi Adamellite|41237|6|Mentioned|p78|||||||||
27492|Moonbi Adamellite|41347|5|Briefly described|p378|||||||||
27492|Moonbi Adamellite|41348|5|Briefly described|Map legend|Early Paleozoic||Of the Moonbi Plutonic Suite.||||||07-NOV-08
27492|Moonbi Adamellite|41603|6|Mentioned|p18|||||||||
27492|Moonbi Adamellite|43091|5|Briefly described|Map Legend|||||||||
27492|Moonbi Adamellite|43407|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27492|Moonbi Adamellite|43418|14|Not recorded|Map Legend|||||||||
27492|Moonbi Adamellite|45087|5|Briefly described|p43|||Chemical analyses||||||
27492|Moonbi Adamellite|50014|6|Mentioned|p253|||Geological Province: New England Fold Belt||||||
27492|Moonbi Adamellite|61773|5|Briefly described|p138|||Intrudes into the Tamworth Belt.||||||
27492|Moonbi Adamellite|63774|6|Mentioned|p1078, p1081|||||||||17-MAR-09
27492|Moonbi Adamellite|71628|6|Mentioned|p7: 30-31|||White (1964), after unpublished work by Chappell (1959, 1966). Now Moonbi Monzogranite.||||||
27492|Moonbi Adamellite|73440|6|Mentioned|p128|Early Triassic|Early Triassic|Cross-cuts the Peel Fault north of Tamworth.|240-245 Ma|||||
82774|Moonbi Granite Group|71628|6|Mentioned|p1: 8; p11: 1; p15:1|||Blevin and Chappell (1996), who differentiated this grouping from the Stanthorpe Granite Group, both within the Moonbi Supersuite. Southern portion of southern New England Orogen.||||||
40260|Moonbi Granitoid Suite|38905|6|Mentioned|p302 Fig.1|||Geological Province: New England Fold Belt||||||
40251|Moonbi Plutonic Suite""|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
82773|Moonbi granite|71628|6|Mentioned|p7:10, 18|||Benson (1913, 1915). Some of these rocks are now the Bendemeer Monzogranite.||||||
68808|Moonbi granites|24513|6|Mentioned|p10|||Informal reference to granites within the Moonbi Supersuite.||||||
40234|Moonbi granitoids|38822|6|Mentioned|p196|||Geological Province: New England Fold Belt||||||
40250|Moonbi group|38842|5|Briefly described|p286|Early Triassic|Late Permian|Geological Province: New England Fold Belt. Age: 245 +/- 5Ma||||||
38332|Moonbi suite|23549|6|Mentioned|p516 Fog. 1|||Informal - see Moonbi Suite.||||||
38332|Moonbi suite|23763|6|Mentioned|p543|||Superseded by Moonbi Suite.||||||
69974|Moonbie Adamellite|61801|5|Briefly described|p403 Fig.1|||Name misspelt.||||||
30023|Moonbucca Formation|22529|6|Mentioned|6|Silurian|Silurian|Local name||||||
30023|Moonbucca Formation|43188|4|Described|p199,Table 1 p200|Ludlovian|Wenlockian|Contains late Wenlockian to Ludlovian fauna. Representative section location given in Table.||||||
35436|Moonbucca Formation""|23170|6|Mentioned|p63|||Demonstrated to be same unit as Dungaree Volcanics, which have name priority.||||||
74022|Moonta Gully Suite|69639|5|Briefly described|p56, p219|||New England Orogen.|||Includes the Moonta Gully Monzogranite.|||
74022|Moonta Gully Suite|71628|5|Briefly described|p19:128|||||Dundee Supersuite.|Moonta Gully Monzogranite.|||
25262|Moore Creek Member|23185|6|Mentioned|p170|||||||||
25262|Moore Creek Member|39331|6|Mentioned|p110|||||||||
25262|Moore Creek Member|43091|5|Briefly described|Map legend|||of Tamworth Group||||||
30895|Moore Creek Stage|43396|14|Not recorded|p165-176|||||||||
30895|Moore Creek Stage|43400|14|Not recorded|p171,176,177,179||Givetian|=Nundle Series. Ref. to Brown 1947 (M.Devn)||||||
34742|Moorealla Formation|22893|6|Mentioned|fig4 p9|Early Cretaceous|Early Cretaceous|||||||10-SEP-19
25264|Mootwingee Beds""|32918|6|Mentioned|p12|||||||||
30785|Mootwingee Sandstone|43344|14|Not recorded|p2||Ordovician|||||||
30785|Mootwingee Sandstone|43491|14|Not recorded|pV/16|||Littoral facies suggests Upper Devonian but may be earlier||||||
30749|Mootwingee Stage|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
30749|Mootwingee Stage|43368|14|Not recorded|Map Legend|||||||||
30749|Mootwingee Stage|43390|14|Not recorded|p13,14|||||||||
30749|Mootwingee Stage|66623|6|Mentioned|p216.|||Kenny (1934); formerly Mootwingee Series (Andrews 1922). Subsequently redefined by various authors including this study; see Wana Karnu Group and Ravendale Formation.||||||
73843|Morgans Creek Monzogranite|69639|4|Described|p2, p6, p8, p181-p186, p239|Triassic|Triassic|New England Orogen. Sample locality, petrography, and geochronology is described. Also intrudes equivalents of the Main Camp Creek Gabbro.|240.8 +/- 1.3 Ma  (SHRIMP U-Pb, magmatic.)|Stanthorpe Suite||Intrudes the Drake Volcanics. Faulted against the Razorback Creek Mudstone.|Massive, undeformed, coarse-grained leucocratic granite (syenogranite).|
73843|Morgans Creek Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Anisian|Anisian|New England Orogen.|240.8 +/- 1.3 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
82582|Morgans Creek Suite|71628|6|Mentioned|p19:131||||||Morgans Creek Leucomonzogranite.|||
35258|Morisset Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
70421|Morney silcrete profile|61007|5|Briefly described|p296|Paleocene|Late Cretaceous|In the Clarence-Moreton Basin area.||||||
82584|Mornington Tonalite|71628|6|Mentioned|p2: 42|||Of Hensel (1982). Now Mornington Complex.||||||
82584|Mornington Tonalite|71629|6|Mentioned|p2: 42|||Of Hensel (1982). Now Mornington Complex.||||||
34526|Morolana Supergroup|22772|5|Briefly described|Table 13.1|Middle Cambrian|Early Cambrian|||||||
34526|Morolana Supergroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Middle Cambrian|Early Cambrian|Age: ~545-498Ma.||||||
28777|Morrawong Creek Formation|41796|6|Mentioned|Fig.3.4|||Misspelling of Murrawong Creek Formation||||||
38927|Mortray Hill Granite""|24417|6|Mentioned|p100|||Name discontinued - still included as part of the Mortray Hill Granite Complex.||||||
27496|Moruya Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27496|Moruya Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
27496|Moruya Granite|30600|4|Described|p159|||Magnetic fabric discussed. See also P160-164||||||
27496|Moruya Granite|33325|6|Mentioned|p19|||See also P20. Sil.-Dev.||||||
27496|Moruya Granite|34404|6|Mentioned|p88|||||||||
27496|Moruya Granite|42726|5|Briefly described|map legend|Silurian||||||||
27496|Moruya Granite|43344|14|Not recorded|p31,32|||Building stone||||||
27496|Moruya Granite|45087|5|Briefly described|p48|||Chemical analyses||||||
27496|Moruya Granite|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|||||||
27496|Moruya Granite|70601|5|Briefly described|p23,p25-26, p46, p55, p57-58|Middle Devonian|Early Devonian|The most primitive of the Lachlan Orogen granites. Includes Tuross Pluton.|U Pb zircon 396.2+/-1.4Ma Tuross pluton||||Granitic rocks.|
27496|Moruya Granite|72571|6|Mentioned|p99|||||||||
34644|Moruya Granite""|22815|6|Mentioned|p89|||Superseded by Moruya Suite.||||||
34646|Moruya Igneous Complex""|22815|6|Mentioned|p89|||Superseded by Moruya Suite.||||||
69646|Moruya Province Volcanics|61155|5|Briefly described|p19|Late Oligocene|Late Oligocene|Includes the Colia Basalts. Overlie the Bergalia Formation; overlain by Meringo Creek Formation. In Southeastern NSW.||||||
42322|Moruya granite|24270|5|Briefly described|p1607|Carboniferous|Carboniferous|Geological Province: Lachlan Fold Belt.||||||
83524|Mosman Swamp Andesite|24121|5|Briefly described|p4, p151|||Of Gilmore Volcanic Group.||||||25-AUG-22
76014|Mosman Swamp Andesites|50132|6|Mentioned|p246 Fig. 4|Late Carboniferous|Late Carboniferous|New England Fold Belt, Raymond Terrace area||||||
32976|Mosman's Swamp Andesites|44254|2|Defined|p76,77,79,80||Early Carboniferous|Unit of Gilmore Volcanic Group.||||||
70375|Moss Vale tholeiitic dolerite|60997|5|Briefly described|p139 Fig. 1|Early Jurassic|Early Jurassic|Informal name. Geological Province: Sydney Basin.||||||
74780|Mossvale Alkali Feldspar Granite|61789|5|Briefly described|p303|Triassic||Previously mapped as Stanthorpe Adamellite.  Medium-grained seriate, biotite-bearing alkali feldspar granite. See also Mossvale Granite p311.||||||27-OCT-08
74780|Mossvale Alkali Feldspar Granite|71628|6|Mentioned|p16: 16|||Sivell and Passmore (1999) after Mossvale Granite of Passmore (1998, unpublished). Now (this study) Mossvale Alkali Feldspar Granite Phase of Cullendore Syenogranite.||||||
82775|Mossvale Alkali Feldspar Granite Phase|71628|4|Described|p11: 39; p16: 12, 16-18, 20|||New name (this study); previously Mossvale Alkali Feldspar Granite of Sivell and Passmore (1999), which replaced the Mossvale Granite of Passmore (1998, unpublished). Originally part of Stanthorpe Monzogranite. Named after a local property. Crops out as gentle hills with intermittent rocky knolls, ~15 km NE of Stanthorpe and 7km ESE of Maryland. Geochemistry described; is geochemically assigned to the Five Mile Creek Suite.||Cullendore Syenogranite.||Intrudes Undercliffe Falls Monzogranite and Five Mile Creek Syenogranite Phase. Is intruded by Herding Yard Creek Intrusives.|Pink, medium-grained, seriate, alkali-feldspar granite. Contains xenoliths of Undercliffe Falls Monzogranite.|
22392|Mossvale Granite|61789|4|Described|p304, p311|||Refers to Mossvale Alkali Feldspar Granite (p303). Not clear which is meant to be formal name.||||||
22392|Mossvale Granite|61790|6|Mentioned|p315, p318, p320, p321|||Alkali feldspar granite.||||||18-SEP-09
22392|Mossvale Granite|71628|5|Briefly described|p16: 8, 16|||Passmore (1988 unpublished). Now (this study) Mossvale Alkali Feldspar Granite Phase of Cullendore Syenogranite.|||||Medium-grained, seriate, biotite-bearing alkali-feldspar granite.|
83307|Mother Shipton monzodiorite|73082|5|Briefly described|p10|||Temora area. A stock with two lobes, each 8km x 1km. Believed to be the source of alluvial gold in the Deep or Frontage lead.||||||
30782|Mount Ainslie volcanics|43344|14|Not recorded|p185|||=Ainslie Volcanics||||||
38457|Mount Alfred granite|24133|6|Mentioned|p57|||Informal - see Mount Alfred Granite.  Geological Province: Lachlan Fold Belt.||||||
41278|Mount Alma Conglomerate Member|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Knobby Formation.||||||
40567|Mount Amore Pyroclastic Member|24605|6|Mentioned|p951 App.1|||Superseded by the Plagyan Ignimbrite Member. Informal name for dacitic ignimbrite from the Boomi Creek region.||||||
40567|Mount Amore Pyroclastic Member|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|||||||
69953|Mount Arrowsmith intrusives|22671|5|Briefly described|p840 Tb. 2|||Informal name. Mount is Mt in text.||||||18-JAN-06
69954|Mount Arrowsmith lavas|22671|5|Briefly described|p840 Tb. 2|||Informal name. Mount is Mt in text.||||||18-JAN-06
25271|Mount Arthur coal seam|40805|5|Briefly described|p138|||||||||
28784|Mount Arthur seam|37087|4|Described|p202|||||||||
28784|Mount Arthur seam|40805|5|Briefly described|p143|||Mention P133||||||
28784|Mount Arthur seam|41010|6|Mentioned|Fig.3|||||||||
28784|Mount Arthur seam|42078|6|Mentioned|Table 1 P5|||||||||
28784|Mount Arthur seam|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Burnamwood Formation (Jerrys Plains Subgroup).||||||
79049|Mount Barney Volcanics|69793|6|Mentioned|p1113 Fig.3|Cenozoic|Cenozoic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
70412|Mount Barney igneous complex|61002|6|Mentioned|p202|||Informal - see Mount Barney Igneous Complex. ||||||
29739|Mount Boppy Conglomerate|43032|5|Briefly described|Table 1.|||Actually spelt Mt Boppy Conglomerate||||||
29739|Mount Boppy Conglomerate|73174|5|Briefly described|p1037, p1042, p1045|Lochkovian|Lochkovian|Kopyje Shelf. [Written as Mt Boppy Conglomerate. See also Mount Boppy Conglomerate Member.]||Kopyje Group, Cobar Supergroup||Underlain by Girilambone Beds [Group]. Equivalent to Florida Volcanics.||24-NOV-22
29734|Mount Boppy Series|43032|5|Briefly described|Table 1.|||Actually spelt Mt Boppy Series. Refers to Andrews (1915).||||||
28787|Mount Boppy complex|37345|6|Mentioned|p286|||||||||
77261|Mount Brace seam|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Charbon Subgroup.||||
76160|Mount Browne Series|66623|6|Mentioned|p99, 105 |||A division (Andrews 1922) of Torrowangee Series.||Unit in Torrowangee Series.||||
82587|Mount Bullaganang Suite|71628|5|Briefly described|p5:5|||||Mount Bullaganang Supersuite.|Mount Bullaganang Leucosyenogranite.|||
82776|Mount Cairncross Porphyry|71628|6|Mentioned|p17: 55|||Gilligan and Brownlow (1981). Now Cairncross Monzogranite.||||||
37462|Mount Canobolas Tertiary volcanics|23214|6|Mentioned|p70|||Formal name not intended.||||||
31289|Mount Canobolas Volcanic Complex|43525|14|Not recorded|map p124,p130|||||||||
31289|Mount Canobolas Volcanic Complex|60443|5|Briefly described|p772|Miocene|Miocene|Alkaline.||||||
82420|Mount Carnham Granodiorite|71628|4|Described|p9: 3-4, 12, 16-17, 19-22, 24, 26-27,31|||See also p10-7. New name and definition. Previously Dumbudgery Creek Granodiorite. Named after a prominent local hill. Occurs ~5km W of Baryulgil. Outcrop is excellent in hilly terrain; poor in flatter areas. Geochemistry described.|255.0 +/- 1.0 Ma (SHRIMP: Waltenberg et al. 2016)|Mount Carnham Suite.||Intrudes Silverwood Group, Gordonbrook Serpentinite and Drake Volcanics. Abuts Yugilbar Gabbro.|Pink-grey or pink, medium-grained, equigranular, biotite-hornblende granodiorite with minor tonalite and monzogranite. Cut by aplite dykes. Locally strongly altered. I-type.|
82421|Mount Carnham Suite|71628|5|Briefly described|p9: 20|||||Clarence River Supersuite.|Mount Carnham Granodiorite.|||
25273|Mount Carrington rhyolite|33106|6|Mentioned|PB10|||||||||
37282|Mount Creek Volcanics|24005|5|Briefly described|p292 Fig.1|Early Devonian|Early Devonian|Of Black Range Group. Geological Province: Lachlan Fold Belt.  Probably should be Mountain Creek Volcanics.||||||
28792|Mount Daubeny Beds|42298|6|Mentioned|p29 (p101a)|||Used 1967. Name replaced by Mount Daubeny Formation 1990.||||||
76161|Mount Daubeny beds|66623|6|Mentioned|p178.|||Named by Warris (1967); formerly part of Wertago-Cootawundy Series (Kenny 1934); subsequently Cootawundy beds (Scheibner 1978); defined as Mount Daubeny Formation by Neef et al. (1989).||||||
24394|Mount Daubney Beds|38692|6|Mentioned|p129|||Also known as Cootawundy Beds. Misspelling of Mount Daubeny Beds? Comment added 1993.||||||
76162|Mount Daubney Formation|66623|6|Mentioned|p186, pp190-191.|||Typo for Daubeny.||||||
70064|Mount Daubney Formation""|22857|6|Mentioned|p436 App.1 Tb.A1.6|||Misspelt - see Mount Daubeny Formation||||||
37166|Mount Dick Beds|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|Of Capella Creek Group. Mount is Mt. in text.||||||
37166|Mount Dick Beds|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Mount Morgan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27501|Mount Dijou Volcanics|730|5|Briefly described|p15, p17, p21, p36-38, p62-63.|Ordovician|Cambrian|Steeply dipping, sheared  basalt and basaltic andesite, pillow lavas, hyaloclastic and pyroclastic breccias, generally regarded as interfingering with Girilambone Group sediments. Contains gold - silver deposits in fault and shear zones, and quartz veins.||||||11-NOV-14
27501|Mount Dijou Volcanics|22857|5|Briefly described|p126, p132|Ordovician|Ordovician|Interfingers with Ballast Formation. See also p414 App. 1 Tb. A1.5.||||||
27501|Mount Dijou Volcanics|23245|5|Briefly described|p126,132-3||Ordovician|||||||
27501|Mount Dijou Volcanics|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
27501|Mount Dijou Volcanics|29984|6|Mentioned|Map legend|Silurian|Ordovician|Silurian - Ordovician||||||
27501|Mount Dijou Volcanics|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
27501|Mount Dijou Volcanics|32917|6|Mentioned|p125|||Detailed mapping||||||
27501|Mount Dijou Volcanics|33002|6|Mentioned|p416|||Tectonic history||||||
27501|Mount Dijou Volcanics|33004|6|Mentioned|p75|||||||||
27501|Mount Dijou Volcanics|34449|6|Mentioned|p128|||||||||
27501|Mount Dijou Volcanics|34469|6|Mentioned|p109|||Ordovician||||||
27501|Mount Dijou Volcanics|35118|6|Mentioned|Fig.5|||||||||
27501|Mount Dijou Volcanics|35185|6|Mentioned|p227|||||||||
27501|Mount Dijou Volcanics|36512|5|Briefly described|p20|||||||||
27501|Mount Dijou Volcanics|36534|6|Mentioned|p222|||||||||
27501|Mount Dijou Volcanics|39214|5|Briefly described|p11|||||||||
27501|Mount Dijou Volcanics|40136|5|Briefly described|p32|||||||||
27501|Mount Dijou Volcanics|42467|5|Briefly described|Map Legend|||||||||
27501|Mount Dijou Volcanics|43090|5|Briefly described|Map legend|Ordovician|Cambrian|of Girilambone Group||||||
27501|Mount Dijou Volcanics|43387|4|Described|Map Legend|||Ordovician? Silurian?||||||
27501|Mount Dijou Volcanics|43388|14|Not recorded|Map Legend|Silurian|Ordovician|(on reserve card as Late Silurian-Middle Devonian)||||||
27501|Mount Dijou Volcanics|44093|5|Briefly described|p174 App. 1|Ordovician|Ordovician|Mount is Mt in text of Table. Geological Province: Lachlan Fold Belt.||||||
27501|Mount Dijou Volcanics|46524|6|Mentioned|p119|||||||||
26757|Mount Dromedary Complex|22594|5|Briefly described|p145,6,8||Cretaceous|spelled Mt in text||||||
26757|Mount Dromedary Complex|30661|6|Mentioned|Table 1|||||||||
26757|Mount Dromedary Complex|32673|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
26757|Mount Dromedary Complex|35289|6|Mentioned|p21|||Should have been Mount Dromedary Igneous Complex.||||||
26757|Mount Dromedary Complex|40178|6|Mentioned|p6|||||||||
26757|Mount Dromedary Complex|40811|4|Described|p324|||||||||
26757|Mount Dromedary Complex|42855|5|Briefly described|p620|||actually spelt Mt Dromedary Complex||||||
26757|Mount Dromedary Complex|43715|6|Mentioned|p28|||||||||
26757|Mount Dromedary Complex|45090|6|Mentioned|p89|||Cret. igneous rocks||||||
32025|Mount Dromedary intrusive complex|43870|14|Not recorded|p27,28|||Palaeomagnetic readings.||||||
32025|Mount Dromedary intrusive complex|44798|4|Described|p2299,2300|||late Early Carboniferous-Cenomanian||||||
28793|Mount Dromedary intrusive complex""|22815|6|Mentioned|p106|||Superseded. Renamed Mount Dromedary Igneous Complex||||||
28793|Mount Dromedary intrusive complex""|35289|6|Mentioned|p21|||||||||
25275|Mount Dromedary monzonite""|22815|6|Mentioned|p106|||Superseded. Renamed Mount Dromedary Igneous Complex||||||
25275|Mount Dromedary monzonite""|35289|6|Mentioned|p21|||||||||
31206|Mount Dromedary shoshonitic complex|43479|14|Not recorded|p290||Early Cretaceous|||||||
35274|Mount Drysdale Conglomerate Member|23171|6|Mentioned|p15|||||||||
35274|Mount Drysdale Conglomerate Member|23173|6|Mentioned|Map Legend|||||||||
82777|Mount Duval Group|71628|6|Mentioned|p8: 1, 19, 21, 23, 26, 29, 41, 45|||Bryant et al. (2002) included this unit in the Uralla Supersuite. Appears as Mt Duval Group (Bryant et al., 2002) on p8: 19, 21, 23, 26, 29, 41.||||||
70422|Mount Duval granite|61007|6|Mentioned|p295|Permian|Permian|Informal name. Intruded its own genetically associated volcanics. ||||||
27502|Mount Ephraim Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
27502|Mount Ephraim Granite|40328|6|Mentioned|p196|||||||||
27502|Mount Ephraim Granite|41347|5|Briefly described|p385|||||||||
27502|Mount Ephraim Granite|41348|5|Briefly described|Map legend|Early Paleozoic||Trondhjemite, granodiorite.||||||07-NOV-08
27502|Mount Ephraim Granite|42866|5|Briefly described|Table 2, p12|||||||||31-JAN-08
27502|Mount Ephraim Granite|43400|14|Not recorded|map opp.p.188|||||||||
27502|Mount Ephraim Granite|43401|4|Described|p209,210,211||Late Permian|||||||
27502|Mount Ephraim Granite|43407|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27502|Mount Ephraim Granite|69601|5|Briefly described|p403, p408|||New England Orogen. Included in Nundle Suite by Hensel et al. (1985) on basis of petrologic characteristics and Sr isotopic compositions. Geochronology discussed in detail.|273 Ma (crystallisation age).|Nundle Suite.|||Mainly hornblende-biotite granodiorites with some tonalitic variants. Essentially unstressed I-type granites.|
27502|Mount Ephraim Granite|71628|6|Mentioned|p18:20|||Crook (1961).  Also shown as Mt Ephraim Granite of Kimbrough et al. (1993). Now Mount Ephraim Granodiorite.||||||
73896|Mount Ephraim Suite|70217|5|Briefly described|p27|||New England Orogen. ||Clarence River Supersuite|Includes the Mount Ephraim Granodiorite.|||
40720|Mount Fairy group|23309|6|Mentioned|p390|||||||||
36978|Mount Flakney Adamellite|23721|5|Briefly described|Map Legend|Silurian|Silurian|||||||
36978|Mount Flakney Adamellite|24119|5|Briefly described|p32|Silurian|Silurian|||||||
31054|Mount Franklin Formation""|44970|14|Not recorded|p22||Ordovician|||||||
40441|Mount Frome Group|24580|5|Briefly described|p829|Late Devonian|Late Devonian|Unconformably overlies the Boolgledie Formation. Mount is Mt. in text. Geological Province: Eastern Lachlan Fold Belt.||||||21-JAN-13
34595|Mount Frome Series|22842|6|Mentioned|p29|||Replaced by Frome Hill Formation.||||||
70376|Mount Gib microsyneite|60997|5|Briefly described|p139 Fig. 1|Middle Jurassic|Middle Jurassic|Informal name. Geological Province: Sydney Basin. Mount is Mt in text of figure.||||||
70377|Mount Gib tholeiitic dolerite|60997|5|Briefly described|p139 Fig. 1|Early Jurassic|Early Jurassic|Informal name. Geological Province: Sydney Basin. Mount is Mt in text of figure.||||||
77432|Mount Gibraltar microsyenite""|66300|5|Briefly described|pp87-91.|||An informal name. One of several plutonic to subvolcanic alkaline bodies intruding southern Sydney Basin. This age is interpreted as entirely inherited zircons from Carboniferous granites possibly present in significant volumes beneath Sydney Basin.|(Inherited, not crystallisation) 325.4 +/- 4.1 Ma.|||Intrudes Wianamatta Group.|Massive, fine- to medium-grained aegirine-bearing microsyenite.|
37315|Mount Hook Rhyolite|23861|5|Briefly described|p4 Fig. 2, p5, p17|Westphalian|Westphalian|Of Rocky Creek Conglomerate.  Geological Province: New England Orogen.||||||
37315|Mount Hook Rhyolite|24010|6|Mentioned|p380 Fig. 6|||||||||
80933|Mount Hope Granite|70751|6|Mentioned|p5|Late Silurian|Late Silurian|Also mention of possible granite, at depth, to the east of Mount Hope, p25. Clearly intended as an informal name.||||||16-MAR-19
28799|Mount Hope Volcanics""|41126|6|Mentioned|p24|||||||||
28799|Mount Hope Volcanics""|41528|6|Mentioned|p98|||||||||
37445|Mount Horrible Conglomerate|23214|6|Mentioned|p241|||Now included in Slowmans Creek Conglomerate.||||||
37448|Mount Horrible Conglomerate""|23214|6|Mentioned|p242|||Informal. Now included in Slowmans Creek Conglomerate.||||||
38235|Mount Hutton Coal|23717|5|Briefly described|p118  Fig. 2|Permian|Permian|Mount is Mt. in text.   Parent: Boolaroo Formation.   Geological Province: Sydney Basin||||||
38214|Mount Hutton Tuff|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Boolaroo Formation.   Geological Province: Sydney Basin||||||
38214|Mount Hutton Tuff|24471|5|Briefly described|p32 Fig.4|Late Permian|Late Permian|Of Newcastle Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
38214|Mount Hutton Tuff|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|||Unit in Boolaroo Formation.||||
38214|Mount Hutton Tuff|73304|6|Mentioned|p75|||[Written as Mt Hutton Tuff].||Boolaroo Formation, Newcastle Coal Measures||||
39826|Mount Hutton Tuff member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Boolaroo Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
38245|Mount Hutton group|23717|6|Mentioned|p133|||Mount is Mt. in text.   Not intended as a formal name in discourse on tuffs - see Mount Hutton Tuff.||||||
78271|Mount Jack Beds|67562|5|Briefly described|p97-98, p102 Fig.8, p106, p108, p110|Givetian|Emsian|Mount is spelt as Mt in text. Deposition was on distal braidplains. Contains Skolithos strata in the Paroo National Park and at Momba Station. Invertebrate-formed tracks are very rare, and plant fossils, the Baragwanathia Flora, have been discovered at one locality. ~ 3km thick.||||Is overlain by Crowl Formation.|Includes sandstones, and an 18km-long marker bed referred to as the fish fragment horizon.|23-JAN-17
75116|Mount Jack beds|64964|3|Fully described|p159, p163 Fig. 4, p166, p172|Givetian|Eifelian|Of Mulga Downs Group. Max.thickness: 3.4km. Fluvial thick-bedded sequences alternating with thinner-bedded fluvial strata, both commonly 100s of metres thick. See also p164 Fig. 5 for detailed geology within Paroo N.P. Mostly appears as Mt Jack in text||||||
25283|Mount Jellore igneous complex""|32187|6|Mentioned|p8|||||||||
28802|Mount Johnstone Beds|31228|6|Mentioned|p83|||Refers Sussmitch & David (1920)||||||
28802|Mount Johnstone Beds|43385|14|Not recorded|p177||Visean|||||||
68176|Mount Johnstone Conglomerates|60281|6|Mentioned|p53 App. 1|||Possibly should be Mount Johnstone Conglomerate? Mount is Mt in text.||||||
31141|Mount Johnstone beds|43491|14|Not recorded|pVI/5||Carboniferous|||||||
26763|Mount Jonblee Leucoadamellites|30911|6|Mentioned|Map legend|Permian|Permian|||||||
77677|Mount Knowles limestone member|68297|5|Briefly described|p192|Emsian|Emsian|Informal unit [since 1997]. Includes Emsian vertebrate fossil and conodont fauna.||Of Boogledie Formation||||
82593|Mount Marley Monzogranite|71628|5|Briefly described|p15: 35, 72-74, 97, 115|||New name, after a local topographic feature, on the northern outskirts of Stanthorpe, formed by this small (<0.5 km2) unit. Limited geochemistry described; is geochemically assigned to the Severn River Suite.||Stanthorpe Complex.||Is entirely enclosed within Severn River Monzogranite. Is intruded by Ruby Creek Leucogranite dykes.|Pale grey to pale pink, fine-grained, moderately porphyritic biotite monzogranite containing numerous plagioclase phenocrysts. I-type.|
37143|Mount McRae Shale Formation|23612|5|Briefly described|p840|Proterozoic|Archean|Age: ~2600-2480 Ma.||||||07-NOV-08
37143|Mount McRae Shale Formation|24231|5|Briefly described|p186|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||17-MAR-05
37143|Mount McRae Shale Formation|73574|6|Mentioned|p769|||Hamersley Province.||||||
37423|Mount Misery Adamellite|23214|6|Mentioned|p163|||Replaced by Mount Misery Granite.||||||
34291|Mount Misery Adamellite""|22679|6|Mentioned|p 41|||||||||
70378|Mount Misery trachyte|60997|5|Briefly described|p139 Fig. 1|Middle Jurassic|Middle Jurassic|Informal name. Geological Province: Sydney Basin. Mount is Mt in text of figure.||||||
70378|Mount Misery trachyte|68204|6|Mentioned|p47|||Sydney Basin; Mittagong-Bowral area.|175 +/- 10 Ma (K-Ar; McDougall and Wellman, 1976).|||||
25290|Mount Nullum Complex|40896|6|Mentioned|p11|||||||||
25290|Mount Nullum Complex|43161|5|Briefly described|14||Tertiary|||||||
83286|Mount Olive diorite|73154|5|Briefly described|p79|Llandovery|Middle Ordovician|Scatter of zircon Pb/U SHRIMP ages from ca. 469-435 Ma (Squire and Crawford, 2007). See also Mount Olive Diorite p84.|ca. 469-435 Ma Pb/U zircon SHRIMP|||Intrudes Forest Reefs Volcanics||
79469|Mount Oxley Granite|70602|6|Mentioned|p67 Fig 3,72|Early Devonian|Silurian|[Invalid name. See Mount Oxley Formation in same area] Age inferred from  map symbol. Aeromagnetic map data given. Grouped with Galambo Granite, Glenariff Granite Knightvale Granite and 3 informal units: Rosses Tank Unit, Brevelon Unit, Mulgawarrina Unit.||||||
26769|Mount Pleasant Andesite|22679|6|Mentioned|p 15|||||||||
26769|Mount Pleasant Andesite|23214|6|Mentioned|p53|||Replaced by Mount Pleasant Basalt Member.||||||
26769|Mount Pleasant Andesite|24265|5|Briefly described|p1444|Early Silurian|Early Ordovician|||||||
26769|Mount Pleasant Andesite|32151|6|Mentioned|p198|||Refers Smith (1966)||||||
26769|Mount Pleasant Andesite|33006|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26769|Mount Pleasant Andesite|33282|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26769|Mount Pleasant Andesite|34404|6|Mentioned|Fig.3.3b|||||||||
26769|Mount Pleasant Andesite|34498|6|Mentioned|p150|||See also P155. Lower Ordovician||||||
26769|Mount Pleasant Andesite|35118|6|Mentioned|Fig.5|||||||||
26769|Mount Pleasant Andesite|40136|5|Briefly described|p33|||||||||
26769|Mount Pleasant Andesite|42802|5|Briefly described|p100|||||||||
26769|Mount Pleasant Andesite|43515|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition)||||||
26769|Mount Pleasant Andesite|43548|2|Defined|p239-43,250,252,260||Early Ordovician|No fossils. Equivalent to Walli Andesite. Ref.to Bruce&Langley (unpubl) 1949. (M.Ord)||||||
26769|Mount Pleasant Andesite|60417|5|Briefly described|p155 Fig.2|Late Ordovician|Middle Ordovician|Overlain by Malongulli Formation. Probably obsolete.||||||
80256|Mount Pleasant Limestone|70939|6|Mentioned|p826|Permian|Permian|Northern Hastings Block.||||||
28808|Mount Pleasant Porphyry""|42820|6|Mentioned|p22|||refers to Strusz (1971)||||||
30840|Mount Pleasant Rhyolite|43385|14|Not recorded|p172||Wenlock|||||||
30840|Mount Pleasant Rhyolite|44852|14|Not recorded|p60||Silurian|||||||
30840|Mount Pleasant Rhyolite|44970|14|Not recorded|p32,map|||=Mount Pleasant Porphyry. See also Lexicon||||||
22441|Mount Poole Adamellite|22815|5|Briefly described|p71|||||||||
22441|Mount Poole Adamellite|22878|6|Mentioned|p136|||||||||10-SEP-19
22441|Mount Poole Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Wallagaraugh Suite.||||||
28810|Mount Robe Basin Group|41630|6|Mentioned|p12|||See also P.49||||||
69615|Mount Royal Basalt|61155|5|Briefly described|p19|Early Eocene|Early Eocene|Age: 54.5-53.5Ma. In the Liverpool Range area.||||||
82129|Mount Royal Granite|72528|5|Briefly described|p1, p3 Tb.1.1, p49-56, p109.|Ludlow|Llandovery|Dated sample is from drillcore. Recorded as Jindera Granite in company reports. Informally named Hickory Hill. Previous dating of Mount Royal Granite, 9km to SW of present sample gave age of c. 429 Ma. Part of a period of intrusive activity that took place between c. 430 Ma and c. 400 Ma. Shown as part of the Central Lachlan orogen.|430.5+/-3.4 Ma U238/Pb206 (Pb207-corrected)|Jindera Suite|||Dated sample described as medium grained, graphic leucogranite with a moderately developed fabric. Leucocratic, fine to medium-grained (0.5-2 mm), equigranular, two-mica granite. S-type.|01-FEB-21
37443|Mount Scholfield Formation|23214|6|Mentioned|p240|||Now included in Gibbons Creek Sandstone.||||||
30906|Mount Sheba Series""|43401|14|Not recorded|p211||Tertiary|See also Lexicon. Ref.to Benson 1913. =Liverpool Range Beds||||||
37836|Mount Stavelly Volcanic Complex|24221|5|Briefly described|p894 Fig.3|Cambrian|Cambrian|Probably misspelt.||||||05-JAN-18
39632|Mount Stavelly volcanics|24087|6|Mentioned|p327 Fig.2|||Informal name.   Geological Province: Lachlan Fold Belt.||||||
37430|Mount Stromlo Granite complex|23214|6|Mentioned|p174|||||||||
37466|Mount Stromlo complex|23214|6|Mentioned|p258|||Formal name not intended.||||||
37452|Mount Stromlo granite|23214|6|Mentioned|p258|||Probably misspelt - see Mount Stromlo Granite.||||||
41565|Mount Terrabile hawaiite|60267|6|Mentioned|p27|||Informal reference to the hawaiite of the Warrumbungle Volcanics.||||||
83068|Mount Terrible Complex|73197|6|Mentioned|p472 Tb.2|Sakmarian|Moscovian|Written as Mt Terrible Complex. Thought to be source of Werrie Basalt, heavy mineral, Rb-Sr age from Shaw et al. (1989).|300.0 +/- 8 Ma, 292 +/- 10 Ma Rb-Sr age|||||
38451|Mount Unicorn porphyry|24133|6|Mentioned|p27|||Geological Province: Lachlan Fold Belt.||||||
82778|Mount View Suite|71628|6|Mentioned|p19: 134||||||Mount View Range Granodiorite.|||
80934|Mount Walton porphyry|70751|6|Mentioned|p12|Early Devonian|Late Silurian|||||||16-MAR-19
80934|Mount Walton porphyry|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Intrudes[?] Baledmund Formation.||
70668|Mount Warning central complex|61310|6|Mentioned|p22|Tertiary|Tertiary|A structural term for a variety of intrusives. Mount is Mt in text.||||||
70668|Mount Warning central complex|73581|5|Briefly described|p6, p7|||Intrusive plugs and paleo-magma chambers of the Tweed Volcano. A series of late-stage dykes and sills of icelandite and peralkaline rhyolite ring the central complex.|||||Gabbro, syenite, trachyandesite, laminated gabbro, monzonite.|
70411|Mount Warning igneous intrusive complex|61001|6|Mentioned|p193|||||||||
25299|Mount Woowoolahra granite|46889|6|Mentioned|p277|||||||||
69950|Mount Wright Volcanics""|22671|6|Mentioned|p838|||Of Zhou and Whitford (1994) for basic-intermediate volcanics intercalated between two sequences of undated, deformed metasediments. Referred to as Mt.Arrowsmith Volcanics by Crook (1988); inc. in Kara beds by Mills (1992). Authors favour Mt Arrowsmith Vol||||||
69959|Mount Wright alkali rhyolite|22671|6|Mentioned|p845|||An informal reference to rhyolite within the Mount Wright Volcanics.||||||
69960|Mount Wright calc-alkaline basalts|22671|6|Mentioned|p845|||Informal reference to basalts within the Mount Wright Volcanics.||||||
69961|Mount Wright calc-alkaline suite|22671|6|Mentioned|p845|||Informal name. Refers to the calc-alkaline basalts within the Mount Wright Volcanics.||||||
69956|Mount Wright lavas|22671|5|Briefly described|p840 Tb. 2, p843 Tb. 3|||Informal name. Mount is Mt in text.||||||18-JAN-06
82781|Mount Yarrahappini granite|71628|6|Mentioned|p17: 42|||Of Andrews (1916) after notes from Carne.||||||
37318|Mount Yarrahappinni granitoid|24011|5|Briefly described|p411|Triassic|Triassic|Age:224-223Ma||||||
37318|Mount Yarrahappinni granitoid|71628|6|Mentioned|p17: 42|||Of Johnston et al. (2002) as Mt Yarrahappinni granitoid. Previously Yarrahapinni Adamellite. Now Yarrahapinni Monzogranite.||||||
74758|Mountain Creek Formation""|61964|6|Mentioned|p114|||Of the Cocoparra Group of Conolly (1962), but now superseded by "Womboyne Formation". Contained "Stitts Member" and Melbergen Sandstone Member" and "Confreys Shale Member". ||||||
37177|Mountain Dam Limestone Member|23522|5|Briefly described|p253|Middle Devonian|Early Devonian|Of Boothumble Beds.||||||
82780|Mountain Home Suite|71628|6|Mentioned|p19: 136||||||Mountain Home Granite.|||
37420|Moura Beds|23214|6|Mentioned|p155|||Now formalised and renamed Moura Formation.||||||
38912|Moura Beds""|24417|6|Mentioned|p58|||Superseded by Moura Formation.||||||
37821|Mozart Chert Member|24215|5|Briefly described|p804|||Parent:  Triangle Formation.   Geological Province:  Lachlan Fold Belt||||||
37821|Mozart Chert Member|63286|6|Mentioned|p308 Fig. 9|Gisbornian|Darriwilian|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
37821|Mozart Chert Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|||Adaminaby Group||||
33990|Mt Warning Complex|22586|6|Mentioned|400|||||||||
78272|Mucka Bunnya Beds|67562|6|Mentioned|p97 Fig.4|Givetian|Emsian|Misspelling of Muckabunnya Beds.||||||
78274|Muckabunnya Beds|67562|5|Briefly described|p104-107, p110 Fig.14, p113|Eifelian|Emsian|Units 2 and 3 of the Muckabunnya Beds in the Copper Mine Range continue to be called the Muckabunnya Beds at Moona Vale but strata coeval with units 4-8 of the Copper Mine Range sequence were renamed as the Menamurtee Sandstone (Neef and Larsen 2003).||||Unconformably overlies Mount Daubeny Formation. Is overlain by the Moona Vale Conglomerate Member (Menamurtee Sandstone).|Almost unfossiliferous, quartz arenite-rich fluvial units; local aeolian and lacustrine deposits.|23-JAN-17
38164|Muckabunnya beds|24345|4|Described|p82, 83, 84 Fig. 2.|Emsian|Emsian|Geological Province: Moona Vale Trough.||||||
38164|Muckabunnya beds|66623|6|Mentioned|p194.|||Thick sandstones of the Coturaundee Range area, interpreted (Neef & Larsen 2003)as lateral equivalents of Wana Karnu Group. Formally named Muckabunnya Formation of the Wana Karnu Group in this study.||||||
78273|Muckabunya Beds|67562|6|Mentioned|p102 Fig.8|||Misspelling of Muckabunnya Beds.||||||
73510|Muddy Lake Gabbro|63283|6|Mentioned|p193|||||||||07-FEB-11
73510|Muddy Lake Gabbro|63284|5|Briefly described|p256, p259|Middle Ordovician|Middle Ordovician|Intrudes Golden Lava. Age: 465-456Ma. Geological Province: Junee - Narromine Volcanic Belt. Dioritic intrusion.||||||24-AUG-12
73510|Muddy Lake Gabbro|67107|5|Briefly described|p695|Ordovician|Ordovician|Cowal district. Associated with much of the Au mineralisation at the Cowal Mine. Minimum age of the deposit is 447 +/- 7.0 Ma (dyke).|456 +/- 5.0 Ma (K-Ar hornblende; Perkins, 1993).|||Intrudes Cowal Igneous Complex.||
35236|Muddy Lake diorite|22797|5|Briefly described|Fig5, P841||Caradoc|K-Ar age of unit is 456+/-5 Ma||||||
38958|Muddy Lake diorite""|24417|5|Briefly described|p182|Late Ordovician|Late Ordovician|Age: 456+/-5Ma (K-Ar).||||||
77662|Mudgincoble Chert|67805|6|Mentioned|p73|Ordovician|Ordovician|Age is described as "probable Ordovician". [misspelling of Mugincoble Chert]||||||03-OCT-14
28824|Mugga Porphyry""|35326|6|Mentioned|p485|||||||||
31053|Mugga Series|44970|14|Not recorded|p49|||||||||
80267|Mugincobble Chert|71040|6|Mentioned|p17-18|Middle Ordovician|Middle Ordovician|Forbes area.||||||
38862|Mugincoble Chert beds|24417|6|Mentioned|p37|||Not intended as a formal name - see Mugincoble Chert.||||||
38195|Mugincoble Formation|23736|5|Briefly described|p11|||||||||
31196|Mulbring Beds|43477|14|Not recorded|p44,45,46,12|||||||||
31196|Mulbring Beds|48830|2|Defined|p9|||See also p5-6,7-11,15,18,21, Pl.2.||||||
31195|Mulbring Shale|43477|14|Not recorded|p12,13,43|||||||||
31195|Mulbring Shale|43491|14|Not recorded|pVII/44||Permian|||||||
31195|Mulbring Shale|44489|14|Not recorded|p71|||||||||
30965|Mulbring Siltstone beds|43440|14|Not recorded|p83|||||||||
31215|Mulbring Sub-group|43477|4|Described|p18,19,22,23,41,44||Permian|||||||
70644|Mulga Down Group|61311|5|Briefly described|p42|Early Carboniferous|Middle Devonian|Misspelt - see Mulga Downs Group. Geological Province: Darling Basin.||||||
33925|Mulga Downs Group""|22518|5|Briefly described|Table 1|Late Devonian|Early Permian|Darling Basin||||||
77881|Mulga Downs Stage|65759|6|Mentioned|p113|||Of Mulholland (1940); redefined as Mulga Downs Group  by Rayner (1962, cited in Conolly et al. 1969) and subsequently.||||||
31217|Mulga Downs formation|43491|14|Not recorded|pV/15||Late Devonian|||||||
25304|Mulgoa Laminite|35690|6|Mentioned|p13|||||||||
34649|Mulgunnia Formation""|22679|6|Mentioned|p 32|||Now undifferentiated Crudine Group?||||||
81169|Mullagallah Quartz Diorite|72296|6|Mentioned|p6|Devonian|Devonian|||||Intrudes the Girilambone Group (presumably: no contacts observed).||
30784|Mullion's Range Volcanics|43344|14|Not recorded|p162||Silurian|Orange-Molong||||||
40722|Mulwary group|23309|6|Mentioned|p390|||||||||
73573|Mumbidgil Formation|63288|6|Mentioned|p353|||||||||
25307|Mumbil Formation|23214|5|Briefly described|p124|||Superseded by Mumbil Group.||||||
25307|Mumbil Formation|24126|6|Mentioned|p148|||||||||
25307|Mumbil Formation|29362|6|Mentioned|Table 1|||Silurian.||||||
25307|Mumbil Formation|29906|6|Mentioned|p12|||||||||
25307|Mumbil Formation|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
25307|Mumbil Formation|31161|5|Briefly described|PA3|||||||||
25307|Mumbil Formation|31852|6|Mentioned|p719|||Gedinnian. See also Fig.4||||||
25307|Mumbil Formation|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
25307|Mumbil Formation|32046|6|Mentioned|p128|||See also P135,137||||||
25307|Mumbil Formation|32047|6|Mentioned|p7|||Refers mineralization||||||
25307|Mumbil Formation|32154|6|Mentioned|p181|||Refers Strusz (1960)||||||
25307|Mumbil Formation|32485|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25307|Mumbil Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
25307|Mumbil Formation|32672|6|Mentioned|p672|||||||||
25307|Mumbil Formation|33006|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25307|Mumbil Formation|33282|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25307|Mumbil Formation|33611|6|Mentioned|p129|||Refers Strusz. Now Mumbil Gp.||||||
25307|Mumbil Formation|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
25307|Mumbil Formation|34403|6|Mentioned|p140|||||||||
25307|Mumbil Formation|34404|6|Mentioned|Fig.3.4b|||||||||
25307|Mumbil Formation|34405|5|Briefly described|p110|||Fig.3.9||||||
25307|Mumbil Formation|34567|6|Mentioned|p160|||See Fig.1||||||
25307|Mumbil Formation|37013|6|Mentioned|p31|||||||||
25307|Mumbil Formation|37488|6|Mentioned|p251|||||||||
25307|Mumbil Formation|37727|4|Described|p75|||||||||
25307|Mumbil Formation|39214|5|Briefly described|p21|||||||||
25307|Mumbil Formation|39663|6|Mentioned|Table 4|||||||||
25307|Mumbil Formation|39683|6|Mentioned|p314|||||||||
25307|Mumbil Formation|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
25307|Mumbil Formation|43384|14|Not recorded|Map Legend||Silurian|||||||
25307|Mumbil Formation|43461|14|Not recorded|Table p621|||||||||
25307|Mumbil Formation|43476|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
25307|Mumbil Formation|43479|14|Not recorded|page not known|||||||||
25307|Mumbil Formation|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
25307|Mumbil Formation|43516|14|Not recorded|Map Legend||Late Silurian|||||||
25307|Mumbil Formation|43517|14|Not recorded|p150-159,Map Pl.XII|Ludlow|Late Wenlockian|Approx.equal to Chesleigh Formation||||||
25307|Mumbil Formation|43525|14|Not recorded|Tb p126-7,Tb p132||Ludlovian|||||||
25307|Mumbil Formation|43528|2|Defined|p131||Silurian|||||||
25307|Mumbil Formation|60987|6|Mentioned|p153|||Strusz (1960). |||Barnby Hills Shale Member.|||
69722|Mumbulla suite|24222|6|Mentioned|p22|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
39392|Mumil formation|24126|6|Mentioned|p122|||Informal name.||||||
25308|Munderoo Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Munderoo Granodiorite.||||||
69909|Mundi Mundi Granites|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic||Age: ~1600Ma. Geological Province: Broken Hill.||||||
69909|Mundi Mundi Granites|61825|6|Mentioned|p130|Mesoproterozoic|Mesoproterozoic|Intrudes the Willyama Supergroup.||||||09-JUN-06
69909|Mundi Mundi Granites|64725|6|Mentioned|p58 Fig.2. |||||||||
69909|Mundi Mundi Granites|67540|6|Mentioned|p27|||Of Page, Conor and Jagodzinski (in prep.). Informal name for some of the granites in the NSW portion of the Curnamona Province  considered to be part of the Ninnerie Supersuite.|||||Quartz-K-feldspar-biotite-muscovite granite.|04-FEB-16
69909|Mundi Mundi Granites|67621|6|Mentioned|p224|||Curnamona Province.||||||
69909|Mundi Mundi Granites|73165|6|Mentioned|p637, Fig. 12|||Curnamona Province.||||||
40286|Mundi Mundi Granites""|24574|5|Briefly described|p692|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by Adelaidean metasediments. Geological Province: Broken Hill Domain||||||
40286|Mundi Mundi Granites""|69650|5|Briefly described|p1|||Mentioned as one of four granite types, yet to be defined [as at 2010], considered to belong to the Ninnerie Supersuite. Broken Hill and/or Mulyungarie Domains.|||||Quartz-K-feldspar-biotite-muscovite granite.|
34205|Mundi Mundi granites|22671|6|Mentioned|Fig1p835||Calymmian|Max Age: 1490 Ma.  mentioned only in the context of 'Mundi Mundi type granites'.||||||17-JAN-06
34205|Mundi Mundi granites|61735|6|Mentioned|p654|Mesoproterozoic|Mesoproterozoic|Informal name.  Felsic magmatism at 1600 to 1580Ma.||||||30-JUN-09
34205|Mundi Mundi granites|62536|5|Briefly described|p654, 656-657||||1591 +/- 5 Ma.||||Massive, medium-grained, mildly porphyritic biotite-muscovite granite.|
34205|Mundi Mundi granites|64741|6|Mentioned|p313|||Informal name for suite of granite similar in age and composition to Bimbowrie Suite.||||||07-FEB-11
70333|Mundi Mundi sediments|62096|6|Mentioned|p294|||Informal reference to sediments in the area of Mundi Mundi.||||||
68694|Mundi Mundi type granite|44093|6|Mentioned|p40 (photo), p139 App. 1|Mesoproterozoic|Mesoproterozoic|Informal name. Geological Province: Adelaide Fold Belt.||||||25-JAN-06
68694|Mundi Mundi type granite|63519|5|Briefly described|p7, p12, p16|Mesoproterozoic|Mesoproterozoic|Informal name. Age: 1591+/-5Ma. A dyke of this granite cuts across Hores Gneiss at Hores mine - consisting of quartz, microcline, albite, muscovite and biotite. No association of minerlisation with these granites.||||||
34493|Mundi Mundi type granites|22771|6|Mentioned|p36-37,50||Calymmian|||||||
34493|Mundi Mundi type granites|44093|5|Briefly described|p5 Tab. 1.1|Mesoproterozoic|Mesoproterozoic|Informal name. Age: 1600-1000Ma. Post-kinematic ?transitional tectonic.||||||25-JAN-06
34763|Mundi Mundi-type granites|22933|6|Mentioned|Table11.1p5||Mesoproterozoic|||||||
26783|Mundoonan Sandstone|31161|5|Briefly described|PA6|||||||||
26783|Mundoonan Sandstone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
26783|Mundoonan Sandstone|32672|6|Mentioned|p672|||||||||
26783|Mundoonan Sandstone|37727|4|Described|p75|||See also P29.||||||
26783|Mundoonan Sandstone|37752|6|Mentioned|Fig.2|||Misspelling?||||||
26783|Mundoonan Sandstone|42820|6|Mentioned|p11|||||||||
26783|Mundoonan Sandstone|43385|14|Not recorded|p172||Early Silurian|||||||
30786|Mundoonan Series|43344|14|Not recorded|p113,123||Late Ordovician|||||||
83494|Mundoonen Formation|73264|6|Mentioned|p1392 Fig.14|||See also Mundoonen Sandstone.||||||
37161|Mungallala Formation|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
37161|Mungallala Formation|50095|5|Briefly described|p108 Fig.1|Early Devonian|Early Devonian|See also Mungallala Limestone and ?Mungallala Member.||||||11-FEB-08
37161|Mungallala Formation|60332|5|Briefly described|p938|Early Devonian|Early Devonian|Shale and conglomerate.||||||31-JAN-08
37161|Mungallala Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Wellington. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
73881|Mungallala Limestone|50095|4|Described|p114|||Of Garra Limestone. Has been placed in Cuga Burga Volcanics previously. See also Mungallala Member and Mungallala Formation.||||||11-FEB-08
73880|Mungallala Member|50095|4|Described|p109 Fig.2|Early Devonian|Early Devonian|Siltstone, shale and conglomerate. See also Mungallala Limestone and Formation. ||||||
73880|Mungallala Member|60987|5|Briefly described|p154 Fig.1|Early Devonian|Early Devonian||||||Shale and conglomerate.|
39361|Munmorah Conglomerate Formation|24121|5|Briefly described|p103, p227, p231|Permian|Permian|Of Narrabeen Group.||||||25-AUG-22
31306|Munmurra Sandstone|43554|14|Not recorded|p29|||||||||
31306|Munmurra Sandstone|43556|14|Not recorded|p350|||||||||
73932|Murder Dog Suite|69639|6|Mentioned|p145|||||Hillgrove Supersuite|Includes the Murder Dog Monzogranite.|||
73932|Murder Dog Suite|71628|5|Briefly described|p3:77|||||Hillgrove Supersuite.|Murder Dog Monzogranite.|||
25311|Muree Stage|34345|6|Mentioned|p331|||||||||
25311|Muree Stage|43440|14|Not recorded|p90|||Ref.to David 1950||||||
25311|Muree Stage|43477|14|Not recorded|p15,Pl.3|||Ref.to David||||||
25311|Muree Stage|43491|4|Described|pVII/48||Permian|||||||
25311|Muree Stage|44855|14|Not recorded|p25||Late Permian|Glacio-Marine.||||||
31035|Muree sandstone""|43474|14|Not recorded|p67|||Ref.to de Koninck 1876-7||||||
34619|Murga Complex""|22831|6|Mentioned|p 23|||||||||
24410|Murga Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
24410|Murga Intrusive Complex|22831|4|Described|p 23||Late Ordovician|||||||
24410|Murga Intrusive Complex|40365|2|Defined|p328|Early Devonian|Early Devonian|||||||
24410|Murga Intrusive Complex|40682|5|Briefly described|p2|||||||||
24410|Murga Intrusive Complex|41871|6|Mentioned|Fig.1|||||||||
24410|Murga Intrusive Complex|42077|6|Mentioned|p27|||||||||
24410|Murga Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
24410|Murga Intrusive Complex|43441|5|Briefly described|12, 21|||?Late Ordovician||||||08-JAN-10
24410|Murga Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||08-JAN-10
34620|Murga Intrusive Complex""|22831|6|Mentioned|p 23|||||||||
32860|Murramarang Flow|43981|14|Not recorded|not on card|||||||||
70248|Murramurrang Melange""|60902|6|Mentioned|p873|||Contains abundant fragments of quartz-rich sandstone.||||||
34401|Murrawang Creek Formation|22736|6|Mentioned|p628 Fig7||Cambrian|Misspelling of Murrawong Creek Formation.||||||08-MAR-16
38449|Murray Gates leucogranite|24133|6|Mentioned|p74|||Geological Province: Lachlan Fold Belt.||||||
34739|Murray Group calcarenites|22893|6|Mentioned|p27|||||||||
34550|Murray Group carbonates|22773|5|Briefly described|p351|||||||||
34551|Murray Group limestones|22773|6|Mentioned|p351|||||||||
34551|Murray Group limestones|50154|6|Mentioned|p140|||Informally referring to the limestones of the Murray Group||||||
40721|Murrays Flats group|23309|6|Mentioned|p390|||||||||
83252|Murree Sandstone|73421|6|Mentioned|p18|||Sydney Basin, northern. Previously correlated with Nowra Sandstone based on sedimentary facies and marine faunas.||||||
34590|Murrulula Formation""|22815|6|Mentioned|p32|||Similar to the rocks of the Jerangle Metamorphic Complex.||||||
76066|Murrumbateman Formation|66197|6|Mentioned|p629|||Deep marine quartz and lithic turbidites.||||||14-MAR-12
28836|Murrumbidgee "Series"|12185|5|Briefly described|map legend|Middle Devonian|Middle Devonian|Includes Taemas "Stage", Majurgong "Stage" and Cavan Bluff Limestone.||||||
28836|Murrumbidgee "Series"|33325|5|Briefly described|Table 4|||||||||
28836|Murrumbidgee "Series"|34403|4|Described|p141|||See also P149||||||
28836|Murrumbidgee "Series"|34405|6|Mentioned|Fig.3.9|||||||||
28836|Murrumbidgee "Series"|34406|6|Mentioned|p223|||||||||
28836|Murrumbidgee "Series"|43344|14|Not recorded|p120|||||||||
28836|Murrumbidgee "Series"|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
28836|Murrumbidgee "Series"|43461|14|Not recorded|Table p621|||||||||
28836|Murrumbidgee "Series"|43479|14|Not recorded|p125,126,151|Middle Devonian|Early Devonian|||||||
31243|Murrumbidgee Group""|43491|14|Not recorded|pV/12||Middle Devonian|Sussmilch includes (1914) Black Range and Taemas Group in his "Murrumbidgee Group"||||||
28837|Murrumbidgee Series|30125|6|Mentioned|p3|||Refers to David(1932),Browne(1959).||||||
28837|Murrumbidgee Series|36138|6|Mentioned|Table 1|||||||||
28837|Murrumbidgee Series|43558|14|Not recorded|p3|||||||||
28837|Murrumbidgee Series|43857|14|Not recorded|p336||Middle Devonian|||||||
28837|Murrumbidgee Series|43870|14|Not recorded|p301,326||Middle Devonian|Ref. to Green 1961 Palaeomagnetic readings||||||
28837|Murrumbidgee Series|45147|6|Mentioned|M310|||||||||
28837|Murrumbidgee Series|63025|5|Briefly described|p1052 Fig. 1, p1053|Pragian|Pragian|Of Green (1961). Name now obsolete - replaced by Majurgong Formation. Redbeds. Geological Province: Eastern Lachlan Orogen.||||||23-JAN-07
28837|Murrumbidgee Series|68592|5|Briefly described|p980|||Of David (1932); further described by Browne (1959). Formerly Murrumbidgee Beds of Jenkins (1878). Later renamed Murrumbidgee Group by Pedder et al. (1970).|||Included Cavan, Majurgong and Taemas Stages.|||
31311|Murrumbidgee limestone|43529|14|Not recorded|p235||Siegenian|(late Sieg.) Ref.to Brown 1959||||||
38991|Murrumbucca Tonalite|23866|4|Described|p120, p121 Fig. 1|||See also p122 Fig. 2.  Geological Province: Murrumbidgee Batholith.||||||
38994|Murrumbucca granite|23866|6|Mentioned|p120|||Informal name - see Murrumbucca Tonalite.  Geological Province: Lachlan Fold Belt.||||||
69019|Murrumbucka suite|24517|6|Mentioned|p49|||Informal name. Migmatitic metasedimentary and gabbroic rocks. Part of the Murrumbidgee Batholith. Geological Province: Lachlan Fold Belt.||||||25-MAY-05
70504|Murrurundi Ignimbrite Member, lower|62095|6|Mentioned|p257|||Informal - see Murrurundi Ignimbrite Member. Characterised by rare occurrences of biotite and a groundmass containing abundant vesicles; frequently dark red in colour.||||||
70505|Murrurundi Member|62095|5|Briefly described|p256 Fig. 7|||Abbreviation of Murrurundi Ignimbrite Member.  Of the Currabubula Formation. Geological Province: Werrie block/Tamworth Belt.||||||
77353|Murula beds|68005|5|Briefly described|pp132-133.|Permian|Permian|South Werrie Basin and Hunter Coalfield.||Unit in Singleton Supergroup.|||Coal seams, claystone, siltstone, sandstone, conglomerate.|
26790|Musical Granite|42726|5|Briefly described|map legend|Silurian||Reserved as Musical Tonalite.||||||
80153|Musswellbrook Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area. [Mis-spelling of Muswellbrook.]||Rowan Formation. ||||
26791|Muswellbrook Coal Measures|31649|6|Mentioned|p59|||||||||
26791|Muswellbrook Coal Measures|33334|6|Mentioned|p4|||See also PP5 & 6. Perm.||||||
26791|Muswellbrook Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
26791|Muswellbrook Coal Measures|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
26791|Muswellbrook Coal Measures|34292|6|Mentioned|p24|||See also P25 & Table 1. Permian||||||
26791|Muswellbrook Coal Measures|36042|6|Mentioned|Fig.12|||||||||
26791|Muswellbrook Coal Measures|37065|6|Mentioned|p31|||||||||
26791|Muswellbrook Coal Measures|37081|6|Mentioned|p156|||||||||
26791|Muswellbrook Coal Measures|43384|14|Not recorded|Map Legend||Early Permian|||||||
25316|Myall Camp Member|32286|6|Mentioned|p50|||||||||
30992|Myall Formation|43447|14|Not recorded|p14||Permian|||||||
27855|Myalla Road Syenite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27855|Myalla Road Syenite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
27855|Myalla Road Syenite|32104|6|Mentioned|p5|||Refers dates||||||
27855|Myalla Road Syenite|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27855|Myalla Road Syenite|38327|6|Mentioned|p558|||||||||
27855|Myalla Road Syenite|39666|6|Mentioned|p105|||||||||
27855|Myalla Road Syenite|40178|5|Briefly described|p6|||||||||
27855|Myalla Road Syenite|40328|4|Described|p209|||||||||
27855|Myalla Road Syenite|43577|6|Mentioned|p381||Jurassic|||||||
27855|Myalla Road Syenite|43715|6|Mentioned|p28|||||||||
27855|Myalla Road Syenite|46574|5|Briefly described|Map Legend|Jurassic|Jurassic|Intrusive explosion breccia. Central quartz monzonite. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
27855|Myalla Road Syenite|60007|5|Briefly described|Map legend|Middle Devonian|Early Devonian|||||||
27855|Myalla Road Syenite|61819|5|Briefly described|p90|Middle Jurassic|Middle Jurassic|Intrusive complex.||||||
41279|Myamely Sandstone|9548|5|Briefly described|Map Legend|Zlichovian|Pragian|Of the Yarra Yarra Creek Group.  Underlies: Daalboro Sandstone.  Overlies: Gwando Siltstone.||||||
67909|Myanbah Leucomonzogranite|71628|6|Mentioned|p8:98|||DMR NAND04 Nandewar Geology Integration and Upgrade project, after unpublished work by Chappell and Bryant (1994). Originally Myanbah Leucoadamellite (Binns et al., 1967 after unpublished work by Ransley, 1970). Renamed Myanbah Leucosyenogranite in this study better to reflect its composition.||||||
74011|Myanbah Suite|71628|6|Mentioned|p8-100|||||Uralla Supersuite.||||
22493|Myocum Adamellite|22815|4|Described|p79|||||||||
22493|Myocum Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Myocum Suite.||||||
34639|Myocum Complex""|22815|6|Mentioned|p79|||Osolete. Renamed Myocum Adamellite.||||||
35434|Myrangle Formation""|23170|6|Mentioned|p55|||||||||
69149|Nacka Nacka Complex|60423|5|Briefly described|p371 Fig. 2|Cambrian|Cambrian|Geological Province: Lachlan Fold Belt.||||||
69149|Nacka Nacka Complex|63290|6|Mentioned|p407|Early Silurian|Ordovician|Age: 465+/-6Ma (K-Ar) and 467+/-6Ma (Basden 1990) and 438+/-3Ma (S. Meffre and R.A. Glen unpubl. Data). In Tumut region.||||||
69149|Nacka Nacka Complex|68822|6|Mentioned|p335|Darriwilian|Darriwilian|Weighted minimum LA-ICPMS zircon age of 438 +/- 3 Ma determined from a hornblende quartz diorite that intrudes the middle of the complex.|466 Ma (K-Ar, Basden 1990), > 438 +/- 3 Ma|||||
69149|Nacka Nacka Complex|72495|5|Briefly described|p234|Ordovician|Ordovician|Locally outcrop along the western side of the Gilmore Fault Zone and Tullamore Fault.|||||Tholeiitic MORB-like rocks.|
33985|Nacka Nacka Volcanics|22434|6|Mentioned|11 fig 15|||Geol province Lachlan Fold Belt||||||
72794|Nadgigomar Sub-Group|62740|5|Briefly described|p364|Oligocene|Oligocene|Of the Koringaroo Group. Predominantly lacustrine. Age is Middle Oligocene.||||||06-FEB-07
22499|Nagha Adamellite|22815|4|Described|p95|Late Devonian|Late Devonian|||||||
22499|Nagha Adamellite|23309|6|Mentioned|p440 Appendix 1|||Superseded by Nagha Granite.||||||
22499|Nagha Adamellite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Gabo Suite.||||||
22500|Naghi Adamellite|22815|4|Described|p95|Late Devonian|Late Devonian|||||||
22500|Naghi Adamellite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Gabo Suite.||||||
22500|Naghi Adamellite|68115|6|Mentioned|p6.|||A pluton that straddles the NSW-Victoria border. Renamed Naghi Granite in Victoria to accord with GSV naming practice.||||||
39830|Naleen Tuff|24157|5|Briefly described|p205 Fig.15|Permian|Permian|Abbreviation of Naleen Tuff Member - misspelt - see also Nalleen Tuff Member. Parent: Dights Creek Coal (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
39823|Naleen Tuff Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Dights Creek Coal. Geological Province: Sydney Basin||||||
39823|Naleen Tuff Member|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Given as Naleeen Tuff in Table 5.||Middle unit in Dights Creek Coal.||Overlies Hobden Gully Member. Is overlain by Hillsdale Coal Member.||
30909|Nallawa Complex|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30909|Nallawa Complex|23170|3|Fully described|p212|||of Yeoval Batholith.||||||
30909|Nallawa Complex|24519|6|Mentioned|p90|||Of the Yeoval Batholith, western side.||||||
30909|Nallawa Complex|68003|5|Briefly described|p24 Fig.3-e, p142. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Part of the Yeoval Batholith.|||||Pink fine- to medium-grained two feldspar-biotite granite, ferrohastingsite and magnetite hypersolvus granite; diorite phase: hornblende diorite, quartz monzodiorite, hornblende granodiorite, quartz diorite, tonalite.|
38242|Nalleen Tuff|23717|6|Mentioned|p128 Fig. 9|||||||||
38242|Nalleen Tuff|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. See Awaba Tuff.||Unit of Newcastle Coal Measures.||||
38242|Nalleen Tuff|73304|6|Mentioned|p65|||Superseded; see Awaba Tuff.||||||
38249|Nallen Tuff|23717|6|Mentioned|p133|||Misspelt - see Nalleen Tuff and Nalleen Tuff Member.||||||
82782|Nambucca Association|71628|6|Mentioned|p17: 1|||||||||
26796|Nambucca Beds|24120|5|Briefly described|p6|Permian|Permian|||||||
26796|Nambucca Beds|24127|5|Briefly described|p5|||||||||
26796|Nambucca Beds|24129|5|Briefly described|p4|||||||||
26796|Nambucca Beds|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26796|Nambucca Beds|31676|6|Mentioned|p7|||||||||
26796|Nambucca Beds|31993|6|Mentioned|p682|||||||||
26796|Nambucca Beds|32671|6|Mentioned|Map legend|Permian|Permian|||||||
26796|Nambucca Beds|32672|6|Mentioned|p675|||||||||
26796|Nambucca Beds|33000|6|Mentioned|p5|||||||||
26796|Nambucca Beds|33001|6|Mentioned|p63|||||||||
26796|Nambucca Beds|33002|6|Mentioned|p421|||Tectonic history also on P422||||||
26796|Nambucca Beds|33004|6|Mentioned|p74|||See also P210||||||
26796|Nambucca Beds|34589|6|Mentioned|p276|||||||||
26796|Nambucca Beds|35020|6|Mentioned|p347, p353|||||||||
26796|Nambucca Beds|35194|4|Described|Table 1|||See also P70.||||||
26796|Nambucca Beds|35927|6|Mentioned|p8|||||||||
26796|Nambucca Beds|36042|6|Mentioned|p40|||See also Plate 1.||||||
26796|Nambucca Beds|38065|6|Mentioned|p45|||||||||
26796|Nambucca Beds|38228|6|Mentioned|p432|||||||||
26796|Nambucca Beds|38288|6|Mentioned|Fig.3|||||||||
26796|Nambucca Beds|38793|6|Mentioned|p192|||||||||
26796|Nambucca Beds|39214|6|Mentioned|p41|||||||||
26796|Nambucca Beds|39287|6|Mentioned|p13|||See also P52||||||
26796|Nambucca Beds|43344|14|Not recorded|p167||Paleozoic|||||||07-NOV-08
26796|Nambucca Beds|43375|14|Not recorded|p3||Ordovician|Phyllite and Slate||||||
26796|Nambucca Beds|43384|14|Not recorded|Map Legend||Ordovician|||||||
26796|Nambucca Beds|43385|14|Not recorded|p170||Ordovician|=Bunya Phylites||||||
26796|Nambucca Beds|43479|14|Not recorded|p82||Ordovician|||||||
26796|Nambucca Beds|43852|14|Not recorded|p196|||||||||
26796|Nambucca Beds|48940|5|Briefly described|p7|||Refers Voisey (1934)||||||
26796|Nambucca Beds|69639|6|Mentioned|p100|Early Permian|Late Carboniferous|||||Intruded by the Gleniffer Monzogranite.||
26796|Nambucca Beds|71628|5|Briefly described|p3:46|Permian|Late Carboniferous|Nambucca Block.|||Bellingen Slate|||
34080|Nambucca Block|22612|6|Mentioned|425|||||||||
30841|Nambucca Series|43385|14|Not recorded|p170||Ordovician|||||||
30841|Nambucca Series|44861|14|Not recorded|p217,248|||Ordovician? Age uncertain. No fossils.||||||
80449|Nambucurra granite|70718|5|Briefly described|p66|Silurian|Silurian|Age provided is a K-Ar biotite age interpreted as the age of emplacement. Only shown by place name. Ending inferred.|415.3 +/- 8.2 (Zwingmann et al., 2001)|||||03-APR-18
28845|Namungo Adamellite|22815|4|Described|p60|Silurian|Silurian|Rb/Sr Ages: 410.4+/-1.5 Ma, 412Ma.||||||
28845|Namungo Adamellite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
28845|Namungo Adamellite|33852|6|Mentioned|p502|||Date given.||||||
28845|Namungo Adamellite|35109|2|Defined|p51|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
28845|Namungo Adamellite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
28845|Namungo Adamellite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
28845|Namungo Adamellite|40328|4|Described|p209|||||||||
28845|Namungo Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||||||||
25322|Namungo Granite|42726|5|Briefly described|nap legend|Silurian||Variation on Namungo Adamellite.||||||
34019|Namurian Booral Formation|22601|6|Mentioned|407|Namurian||||||||
34019|Namurian Booral Formation|61768|6|Mentioned|p82|||Roberts et al. 1995.||||||13-MAY-08
30956|Nandewar Complex|43435|2|Defined|Map Legend||Tertiary|||||||
28847|Nandewar Formation|40200|6|Mentioned|p2|||||||||
30942|Nandewar Igneous Complex|43194|6|Mentioned|p131|Triassic|Triassic|||||||
30942|Nandewar Igneous Complex|43429|14|Not recorded|Map Legend||Tertiary|||||||
30942|Nandewar Igneous Complex|43434|14|Not recorded|Map Legend|||||||||
30942|Nandewar Igneous Complex|43435|14|Not recorded|Map Legend||Tertiary|||||||
30944|Nandewar alkali ingeous complex|43429|14|Not recorded|Map Legend|||Description given see Strat form.||||||
30944|Nandewar alkali ingeous complex|43435|14|Not recorded|Map Legend||Tertiary|||||||
25324|Nandewar volcanics|24042|6|Mentioned|p511|||Informal||||||
25324|Nandewar volcanics|40142|6|Mentioned|p1002|||||||||
25324|Nandewar volcanics|40563|6|Mentioned|p241|||||||||
39803|Nandillian limestone|24247|6|Mentioned|p45|Silurian|Silurian|||||||
33883|Nandillyan Limestone""|22486|6|Mentioned|p 3|||||||||
70062|Nangar Subgroup""|22857|5|Briefly described|p213|Devonian|Devonian|One of three former subdivisions (Connolly, 1965a) of the Hervey Group; not applied in recent mapping. Geological Province: Hervey Basin.||||||
39378|Nangar subgroup|24125|5|Briefly described|p46|||Informal. Of the Hervey Group. Geological Province: Lachlan Fold Belt.||||||08-MAY-07
70011|Nangarah Formation|61764|6|Mentioned|p45, p46|||Basalt, chert, argillite.||||||
35417|Nanima Formation""|23170|6|Mentioned|p34|||Of Joplin and others (1952).||||||
39798|Napperby Formation, Lower|24159|6|Mentioned|p163 App. A|||Informal name - see Napperby Formation.||||||
39799|Napperby Formation, Upper|24159|6|Mentioned|p163 App. A|||Informal name - see Napperby Formation.||||||
73042|Napperby Formation, upper|61377|6|Mentioned|p150|||Informal - see Napperby Formation.||||||07-FEB-11
78537|Napperby Series|43194|5|Briefly described|p96 Tb 8.1, p121|Middle Triassic|Early Triassic|Of Kenny (1928, 1964). Superseded name for the Napperby Formation in the Coonabarabran-Gunnedah region of the Gunnedah Basin.||||||27-NOV-13
70249|Narooma Chert, upper|60902|6|Mentioned|p866, p872, p873|||Of Wagonga Group.  Divided into lower and upper cherts, the latter interbedded with shales bearing Eastonian graptolites. Conformably overlain by Bogolo Formation (and former Kianga Basalt).  Geological Province: Narooma Terrane. See also p861 Fig. 2a.||||||
38033|Narooma Complex|24310|5|Briefly described|p1043|||||||||
38033|Narooma Complex|67849|6|Mentioned|p22 Fig.1.|||||Unit in Narooma Accretionary Complex?||||02-OCT-15
70250|Narooma Group|60902|5|Briefly described|p860|||Wilson (1968) interpreted this group's stratigraphy  to comprise basal Bogolo Fm. passing up into Wagonga Fm. Glen (1993, 1994a) showed Bogolo Fm to overlie Wagonga Fm which comprised basal Kianga Basalt and Narooma Chert above. All now REDEFINED.||||||11-APR-06
38031|Narooma accretionary complex|24310|5|Briefly described|p1043|||Informal name.||||||17-JAN-07
38031|Narooma accretionary complex|60904|5|Briefly described|p790 Fig. 16|||Informal - see Narooma Accretionary Complex. Of the Lachlan Orogen. Age: ~445Ma. See also p802 Fig. 23. ||||||
38031|Narooma accretionary complex|61731|6|Mentioned|p1038|||Informal term.||||||
38031|Narooma accretionary complex|68309|5|Briefly described|p224-225, 232-233|||SE Lachlan Orogen. At Narooma, has the structure of a stack of imbricate thrust slices. The basalts were derived from a deep, enriched, asthenospheric, HIMU-type source that underwent varying degrees of partial melting produced by a plume. See also reference to Narooma Accretionary Complex (p225).|||||Minor alkaline basalts with ocean-island-basalt character.|
31909|Narrabeen Chocolate Shales|43870|14|Not recorded|p241||Early Triassic|Red beds.||||||
39354|Narrabeen Group Sandstone|24117|5|Briefly described|p32|||Informal name. Geological Basin: Sydney Basin.||||||
70104|Narrabeen Group sandstones|61529|6|Mentioned|p872|||Informal reference to sandstones within the Narrabeen Group.||||||
38239|Narrabeen Group, Lower|23717|6|Mentioned|p122|||Informal name - see Narrabeen Group.    Geological Province: Sydney Basin||||||
38239|Narrabeen Group, Lower|67560|5|Briefly described|p270 Tb.4, p271, p272|Triassic|Triassic|See Narrabeen Group (p258-272). Fluviodeltaic, continual variation, cyclic deposition, kindred lithologies; changing salinity imprints.|||Includes Bulgo Sandstone, Stanwell Park Claystone, Scarborough Sandstone, Wombarra Shale, Coalcliff Sandstone.|Underlain by the Illawarra Coal Measures. Overlain by the Bald Hill Claystone.||
68184|Narrabeen Group, Upper|60281|6|Mentioned|p63|||Informal - see Narrabeen Group.||||||
72975|Narrabeen Group, lower|61315|6|Mentioned|p183|||Informal - see Narrabeen Group. ||||||
40232|Narrabeen Group, upper|38820|6|Mentioned|p182|||Geological Province: New England Fold Belt||||||
39412|Narrabeen Sandstone Group|24126|6|Mentioned|p278|||||||||
37381|Narrabeen Sandstone unit|24040|6|Mentioned|p484|||Informal - see Narrabeen Sandstone. Geological Province: Sydney Basin.||||||
31218|Narrabeen Series""|43491|14|Not recorded|pVIII/8a,9,10||Triassic|||||||
30979|Narrabeen series|43443|14|Not recorded|p2283||Early Triassic|Palaeomagnetism||||||
32382|Narrabeen shales|43905|14|Not recorded|p87||Triassic|Flora||||||
69150|Narraburra Complex|60423|5|Briefly described|p370|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||09-JUN-05
69150|Narraburra Complex|64329|5|Briefly described|p15, p20|||Alkaline igneous complex containing three suites of alkaline granite - Barmedman and Gilmore Hill Suites (Itype) and Narraburra Suite (Atype)|358 +/- 9 to 365 +/- 4, Rb-Sr whole rock||Barmedman Suite, Gilmore Hill Suite, Narraburra Suite||arfvedsonite and aegerine-arfvedsonite granite|30-APR-10
69150|Narraburra Complex|72084|6|Mentioned|p2|Late Devonian|Late Devonian|Post-tectonic intrusions. See also references to the Narraburra Suite (p54, p55 Fig.57, p56).||||||
69151|Narraburra Complex""|60423|5|Briefly described|p370|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
82811|Narraburra granite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. A-type. Hf and O18 isotope data included.|375 Ma|||||
28853|Narragal Limestone Member|23214|5|Briefly described|p124|||Previously included in the Mumbil Formation, since been given formation status. See Narragal Limestone.||||||
28853|Narragal Limestone Member|31852|6|Mentioned|p718|||Ludlovian. See also Fig.4||||||
28853|Narragal Limestone Member|34405|5|Briefly described|p110|||||||||
28853|Narragal Limestone Member|37727|6|Mentioned|p75|||||||||
28853|Narragal Limestone Member|43479|14|Not recorded|p116|Wenlockian|Llandoverian|||||||
28853|Narragal Limestone Member|43528|14|Not recorded|p128-9,131-2,134-5|Wenlockian|Llandoverian|||||||
31273|Narragal Limestone""|43528|14|Not recorded|p131,134|||Ref. to Carne and Jones 1919. See also Lexicon||||||
39802|Narragal limestone|24247|6|Mentioned|p45|Silurian|Silurian|||||||
68150|Narrambeen Group|60281|5|Briefly described|p63|Early Triassic|Early Triassic|Miispelt - see Narrabeen Group.||||||
39952|Narromine Complex|24267|6|Mentioned|p1508 Fig.1|||Geological Province: Parkes-Narromine Belt||||||
39952|Narromine Complex|73154|6|Mentioned|p77|Llandovery|Llandovery|Contains a Copper Hill-type intrusion with zircon age populations of ~467 Ma and ~441 Ma interpreted by Crawford et al. (2007b) as inherited cores and melt-precipitated rims (emplacement age) respectively.|~441 Ma|||||
29435|Narrow Plains Formation|42966|4|Described|p64|||Misspelling of Narrow Plain Formation? Part of Coorabin Coal Measures.||||||
38450|Narrowleaf leucogranite|24133|6|Mentioned|p74|||Geological Province: Lachlan Fold Belt.||||||
26801|Narwonah Volcanics|42726|5|Briefly described|map legend|Early Devonian||Variation on Narwonah Rhyolite.||||||
41655|Native Dog Ignimbrite Member, lower|44244|6|Mentioned|p304|||Informal name.  Geological Province: Rouchel Block.||||||25-AUG-04
36333|Nattery Chert|50232|5|Briefly described|Map strat. chart|Gisbornian|Darriwilian|Of the Adaminaby Group.||||||13-MAY-04
36333|Nattery Chert|50234|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Adaminaby Group.  Thin-bedded to lamintaed radiolarian and conodont-bearing chert, variably cherty siltstone and mudstone, minor graded and cross-laminated fine-grained quartzose sandstone.||||||13-MAY-04
82783|Navies Creek Member|71628|5|Briefly described|p19: 131|||||Drake Volcanics.||Is intruded by Morgans Creek Leucomonzogranite.||
72279|Neelungaloo Volcanics|62478|4|Described|p89|Late Ordovician|Early Ordovician|Basal unit of the Goonumbla Volcanic Complex. Andesite, conglomerate, sandstone, chert. Underlies Goonumbla Volcanics.||||||
30852|Neerkol Series|43385|14|Not recorded|p178||Late Carboniferous|||||||
30852|Neerkol Series|44432|14|Not recorded|p34,36||Carboniferous|(Muscovian-Uralian)||||||
26803|Nelligen Granite|42726|5|Briefly described|map legend|Silurian||Variation on Nelligen Granodiorite.||||||
82784|Nelson Creek Leucomonzogranite Phase|71628|5|Briefly described|p15: 48, 95, 106-107, 109-112, 114|||New name (this study) after work by Mustard (2004). Timbarra Plateau. Geochemistry described in great detail.|248.8 +/- 2.4 Ma (SHRIMP: Mustard, 2004).|Surface Hill Leucomonzogranite.|||Medium- to coarse-grained, inequigranular to weakly porphyritic (K-feldspar phenocrysts to 15 mm), ""syenogranite"" (probably leucomonzogranite to leucosyenogranite: discussed). Rare enclaves. Amphibole and megacrysts absent.|
73509|Nelungaloo Intrusives|63284|6|Mentioned|p249|Early Ordovician|Early Ordovician|Age: 481+/-3Ma. (Butera et al. 2001; Simpson et al. 2005).||||||
77362|Neminga Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|[Correct spelling of the location is Nemingha].||Unit in Tamworth Group.||||
34445|Neminga Limestone Member""|22750|6|Mentioned|p 228|||||||||
75860|Nemingah Limestone|5254|6|Mentioned|p121||Early Devonian|Of Tamworth Group.||||||
75860|Nemingah Limestone|73440|6|Mentioned|p132|||||||||
75859|Nemingah Limestone""|44447|6|Mentioned|p131|Early Devonian|Early Devonian|A suite of small, lenticular conglomeratic (?allochthonous) limestone bodies of Manilla-Tamworth region. Age: mid-Early Devonian||||||
31160|Nemingha Formation|43491|14|Not recorded|pV/13||Early Devonian|||||||
26804|Nemingha Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
26804|Nemingha Limestone Member|31999|6|Mentioned|p150|||Table 1||||||
26804|Nemingha Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
26804|Nemingha Limestone Member|34554|6|Mentioned|p234|||||||||
26804|Nemingha Limestone Member|34692|5|Briefly described|p188|||||||||
26804|Nemingha Limestone Member|39331|6|Mentioned|Table 10-1|||||||||
26804|Nemingha Limestone Member|43400|2|Defined|p178,179,183,184,map|||||||||
26804|Nemingha Limestone Member|43428|14|Not recorded|p137||Gedinnian|Part of Drik Drik Formation (L.Gedinnian).List of fauna||||||
26804|Nemingha Limestone Member|68005|5|Briefly described|p53 Photo.3-M.|||Note that the text on p.50 states that the Northcotte Formation "hosts the Nemingha Limestone (Photograph 3-M)"; but at that reference the caption names "the Nemingha Limestone Member of the Wogarda Argillite".||Unit in Wogarda Argillite.|||Fossiliferous limestone.|
34443|Nemingha Limestone""|22750|6|Mentioned|p 228|||||||||
30843|Nemingha Red Breccia|22750|6|Mentioned|p 228|||||||||
30843|Nemingha Red Breccia|43385|14|Not recorded|p175|||||||||
30843|Nemingha Red Breccia|43400|14|Not recorded|p177,182,183||Early Devonian|=Drik-Drik Formation (Coblenzian)||||||
30896|Nemingha Stage|43396|14|Not recorded|p165-176|||||||||
30896|Nemingha Stage|43400|14|Not recorded|p177,179|Middle Devonian|Early Devonian|Includes M.Devn Silver Gully Agglomerate||||||
31969|Neranleigh 'Series'|43881|14|Not recorded|p8||Paleozoic|See also Lexicon. NSW equivalents of Brisbane Metamorphics may be restricted to this 'series'. Ref.to Denmead 1927.||||||07-NOV-08
25337|Nerri Basalt|37094|5|Briefly described|p239|||||||||
72796|Nerriga Sub-Group|62740|5|Briefly described|p364, p371|Middle Eocene|Middle Eocene|Of the Korinagaroo Group. Includes Titringo Creek and Limekiln Creek Siltstones. Lacustrine deposits.||||||15-JAN-08
23870|Neville Granite|22503|5|Briefly described|Fig.7 p650, p651|Early Devonian|Silurian|||||||
23870|Neville Granite|22679|6|Mentioned|p 48|||Informal and invalid name. Replaced by Sunset Hills Granite||||||08-MAR-16
23870|Neville Granite|23214|5|Briefly described|p171|||Originally included Rocky Bridge Granodiorite. Renamed Sunset Hills Granite.||||||
23870|Neville Granite|42726|5|Briefly described|map legend|Silurian||Note: Neville Granodiorite, WA published 1992.||||||
35381|Neville Granodiorite (NSW)|23100|5|Briefly described|p575 (Fig 1)||Silurian|||||||
35381|Neville Granodiorite (NSW)|23202|6|Mentioned|Fig.1||Silurian|||||||
30941|New Albany Shale|43428|14|Not recorded|p141|||||||||
34013|New England Batholith|22601|6|Mentioned|419|||||||||
34013|New England Batholith|44244|6|Mentioned|p291|||Same as New England Super-Suite of Hensel et al (1985).  Not a formal name.||||||
40252|New England Bathylith Plutonic Suite|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
25338|New England Granite|29591|6|Mentioned|p113|||||||||
25338|New England Granite|33091|6|Mentioned|p7|||Structure||||||
25338|New England Granite|33476|6|Mentioned|p67|||||||||
25338|New England Granite|34340|6|Mentioned|p477|||Rutile in Mesozoic sediments.||||||
25338|New England Granite|36045|6|Mentioned|Fig.7|||||||||
25338|New England Granite|38913|6|Mentioned|p321|||||||||
25338|New England Granite|43344|14|Not recorded|p10,38||Late Permian|||||||
25338|New England Granite|43852|14|Not recorded|p196|||(New England Granite Bathylith)||||||
25338|New England Granite|44565|14|Not recorded|p234|||||||||
25338|New England Granite|44671|14|Not recorded|p245|||||||||
40235|New England Granitoid Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt. Age: 232-235Ma||||||
40236|New England Plutonic Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
40236|New England Plutonic Suite|71628|6|Mentioned|p1:5; p3: 2, 40; p7: 1, 6, 11, 15, 20|||See also p7: 28, 32, 41; p8: 58, 73, 77; p13: 1, 5; p17-48; p19: 2, 152. Hensel et al. (1985) referred to as the New England Super-suite.||||||
29563|New England Super Suite|42984|6|Mentioned|p365|||New England Supersuite probably intended. Name invalid anyway if New England Granite still in use.||||||
40238|New England Super-Suite|38822|6|Mentioned|p193|||Formerly known as the New England Suite. Geological Province: New England Fold Belt||||||
40238|New England Super-Suite|44244|6|Mentioned|p291|Triassic|Permian|Age: 250+/-2Ma.  Same as New England Batholith of Korsch (1977).||||||16-SEP-04
82785|New England Super-suite|71628|6|Mentioned|p1: 5; p3: 40; p7: 1, 6, 11, 15, 20, 28|||See also p7: 32, 41; p8: 1, 5, 9, 51, 62, 67, 104; p13: 1, 5; p19: 55. Hensel et al. (1985) after the New England Plutonic Suite of Hensel et al. (1982). Appears also as New England Super-Suite.||||||
38353|New England Super-suite""|23812|5|Briefly described|p24|Early Triassic|Late Permian|Informal name of Hansel et al, 1985.||||||
32623|New England granite|46159|14|Not recorded|p.404|||||||||
30817|Newbridge Formation|43384|14|Not recorded|Map Legend||Silurian|||||||
28862|Newcastle (Upper) Coal Measures|41911|6|Mentioned|p146|||||||||
32464|Newcastle Coal|34270|6|Mentioned|p.254?|||Added to card in pencil.||||||
30995|Newcastle Group|43448|14|Not recorded|p228,230,231|||||||||
30788|Newcastle Stage|43344|14|Not recorded|p84|||Now called Newcastle Coal Measures||||||
30788|Newcastle Stage|43440|14|Not recorded|p90|||Ref. to David 1950||||||
30788|Newcastle Stage|43477|14|Not recorded|p15,16,23,Pl.3|||Ref.to David||||||
30788|Newcastle Stage|43552|14|Not recorded|p99|||||||||
30788|Newcastle Stage|43909|14|Not recorded|p18|||||||||
30788|Newcastle Stage|44855|14|Not recorded|p25||Late Permian|||||||
29790|Newport Formation"" (NSW)|33683|6|Mentioned|p77|||||||||
31263|Newrea Formation""|43512|14|Not recorded|p100-1,104|Middle Devonian|Early Devonian|Mapped only||||||
35052|Newstead-Elsmore group|23050|4|Described|p77|||||||||
73907|Newton Boyd Suite|71628|6|Mentioned|p19:138||||||Newton Boyd Granodiorite.|||
30415|Nile Sub Group|43146|6|Mentioned|Fig.2 p41|||Misspelling of Nile Subgroup.||||||
22554|Nimmitabel Adamellite|22815|4|Described|p78|||||||||
22554|Nimmitabel Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
22554|Nimmitabel Adamellite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
31172|Nine Mile Shale|43491|4|Described|pIII/14||Ordovician|||||||
28867|Nine Mile Shale""|45147|6|Mentioned|M32|||||||||
41355|Nioka Dacite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Equivalent to the Tent Hill Volcanics.||||||
30972|Nobby's Cherts|43440|14|Not recorded|p49,54|||Unit of Newcastle Coal Measures||||||
30972|Nobby's Cherts|43477|14|Not recorded|p22,53|||||||||
30789|Nobby's Tuff|43344|14|Not recorded|p21,79,80,85||Late Permian|||||||
30996|Nobby's Tuff Member|43447|14|Not recorded|diag.p26|||Part of Lambton Sub-Group||||||
30996|Nobby's Tuff Member|43448|14|Not recorded|p226||Permian|(Lambton Subgroup?) Newcastle Coal Measures||||||
78868|Nobbys Chert|68711|5|Briefly described|p119|||Of David (1907). Superseded by Nobbys Tuff Member, Nobbys Tuff.||||||
34009|Nobbys-Dudley-Yard Coal|22578|6|Mentioned|Fig.9 p399|||||||||
36916|Noltenius formation|23714|5|Briefly described|p10|||Of Finniss River Group.||||||
35622|Noonthorangee Subgroup|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Ponto Group. Largely non-magnetic unit; phyllite, minor arenite, fine-grained, laminated siliceous tuff and weakly magnetic tholeiitic metabasalt.||||||26-NOV-08
35622|Noonthorangee Subgroup|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Includes Blue Rock Formation, Gum Creek and Blue Rock Well Basalts. Largely non-magnetic: phyllite, minor arenite, fine-grained, laminated siliceous tuff and weakly-magnetic tholetiitie metabasalt.||||||
35622|Noonthorangee Subgroup|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Largely non-magnetic: phyllite, minor arenite, fine-grained, laminated siliceous tuff and weakly-magnetic tholeiitic metabasalt.||||||27-NOV-08
35622|Noonthorangee Subgroup|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Blue Rock Formation, Tekum Creek Basalt and Blue Rock Well Basalt.||||||01-DEC-08
35622|Noonthorangee Subgroup|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes Blue Rock Formation.||||||27-NOV-08
35622|Noonthorangee Subgroup|66623|6|Mentioned|p89.|||Former (Buckley 2000) name of Noonthorangee Formation, redefined in this study. Previously, portion of Wonominta beds (Warris 1967).||Unit in Ponto Group.|Said to include Blue Rock Well Basalt, Phyllite and Sandstone; Blue Rock Formation; Gum Creek Basalt.|||
35622|Noonthorangee Subgroup|66929|5|Briefly described|Map legend|||||Unit in Ponto Group.|Includes Blue Rock Well, Tekum Creek and Gum Creek Basalts, and Blue Rock Formation.|||
35622|Noonthorangee Subgroup|66933|5|Briefly described|Map legend|||Largely non-magnetic.||Unit in Ponto Group.|Includes Blue Rock Formation.||Phyllite; minor arenite, fine-grained laminated siliceous tuff and weakly magnetised tholeiitic metabasalt.|
35622|Noonthorangee Subgroup|67322|6|Mentioned|p39|Cambrian|Cambrian|Obsolete: now the Noonthorangee Formation (Greenfield et al 2010).  Age is assumed to be similar to the Noonthorangee Formation. Occurs in the Kayrunnera-Koonenberry region.||||||22-FEB-18
76143|Noonthorangie Formation|66623|6|Mentioned|p80 Fig. 21. |||Mis-spelling of Noonthorangee.||||||
76027|Noothorangee Formation|66927|5|Briefly described|Map legend|Cambrian||[Mis-spelling of Noonthorangee Formation]. Formerly Noonthorangee Subgroup. Irregularly shaped area west of The Gorge Inlier where regional high magnetic intensity trends are reduced in amplitude.||||Is overlain by Ponto Formation?|Possibly altered phyllite.|24-SEP-13
76136|Noothorangee Subgroup|63793|6|Mentioned|p36. |||[misspelling of Noonthorangee]|||||Includes basalts.|
76167|Nootumbulla Formation|66623|6|Mentioned|p136.|||Misnomer for Nootumbulla Sandstone.||||||
30750|Nootwingee Stage|43369|14|Not recorded|Map Legend|||Misspelling of Mootwingee Stage||||||
31292|Norah Creek Limestone|43513|14|Not recorded|p90||Late Devonian|||||||
37141|Normanville Groups|23564|6|Mentioned|p1444|||||||||
73688|North Parkes Igneous Complex|63283|6|Mentioned|p194 Fig. 2|Early Silurian|Middle Ordovician|Includes; Nash Hill Volcanics, Parkes Volcanics. Geologiacl Province: Junee-Narromine Volcanic Belt.||||||07-FEB-11
73688|North Parkes Igneous Complex|73154|6|Mentioned|p77 Fig.3|Late Ordovician|Middle Ordovician|Junee-Narromine Belt.||||||
77354|Northcotte Limestone Member|68005|6|Mentioned|p151.|Devonian|Devonian|||Unit in Northcotte Formation.||||
77331|Northern Moonbi Supersuite|68005|6|Mentioned|p67.|||Of Bryant (2001) who subdivided the Moonbi Supersuite into two Supersuites.|||Includes Clive Monzogranite.|||
77331|Northern Moonbi Supersuite|71628|6|Mentioned|p9:1; p11: 1, 5, 11, 17, 40; p14: 1, 4,|||See also p14: 13, 17, 23, 29, 32; p15: 1, 6, 9, 16, 20, 23, 26, 34, 46-47, 53, 73, 77, 83, 98, 107; p16:26; p17-5; p18:10; p19: 37, 91, 98, 131, 138. Bryant et al. (2002). Apparently referred to a grouping including Stanthorpe and Bungulla Supersuites, and others. Is occasionally presented in the text as northern, (northern) or (Northern) Moonbi Supersuite.||||||
38197|Northparkes Group|23736|6|Mentioned|p12|||||||||
38197|Northparkes Group|24417|6|Mentioned|p19|||Should be Northparkes Volcanic Group.||||||
38197|Northparkes Group|63278|4|Described|p146 Fig. 2a, p150|Early Silurian|Middle Ordovician|Includes; Parkes Vols, Nash Hill Vols, Goonumlba Vols, Wombin Vols, Raggatt Vols. Name is a modification of the Northparkes Vols Gp + excludes rocks east of Parkes Thrust. Geol Prov: Molong Volcanic Belt, LFB.||||||07-FEB-11
38197|Northparkes Group|63289|6|Mentioned|p374|||Overlain (or interfingered with) Cotton Formation.||||||07-FEB-11
38197|Northparkes Group|63290|5|Briefly described|p397 Fig. 3(b)|Llandovery|Darriwilian|Includes; Parkes Volcanics, Nash Hill Volcanics. Geological Province: Junee - Narromine Volcanic Belt.||||||
38197|Northparkes Group|63291|4|Described|p421|Middle Ordovician|Middle Ordovician|Includes; Goonumbla + Wombin Vols. Geol P: Junee-Narromine Vol Belt. Lavas, volcaniclastics, shallow-water carbonates, deeper-wter clastic rocks. Name is modification on Northparkes Vol Gp proposed by Percival (2000). Defined by Percival and Glen (2007).||||||28-SEP-07
38197|Northparkes Group|64826|5|Briefly described|p1040 Tb. 1|Ordovician|Ordovician|Contains Gunningbland Formation, Goonumbla Volcanics and Billabong Creek Limestone. ||||||
38197|Northparkes Group|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
38197|Northparkes Group|67322|4|Described|p20 Fig.5, p22|Bolindian|Katian|Macquarie Arc. (Originally Northparkes Volcanic Group of Percival, in Lyons et al. 2000). Established to include the Goonumbla Volcanics and correlative volcanic and sedimentary units. Fossiliferous limestones contain Eastonian corals and conodonts. Occurs in the Junee-Narromine region.|||Goonumbla Volcanics, Raggatt Volcanics, Wombin Volcanics.|Now a correlative with the redefined Cabonne Group.|Andesitic to trachyandesitic lavas, tuffs, volcaniclastic breccias and sparse fossiliferous limestones; fossiliferous arkose.|22-FEB-18
38197|Northparkes Group|68592|6|Mentioned|p377|||Junee-Narromine Volcanic Belt of the Macquarie Arc. Thought to be approximately equivalent to Cabonne Group.||||||
38197|Northparkes Group|70684|5|Briefly described|p54 Fig.27, p55, p61, p74-75|Late Ordovician|Middle Ordovician|Junee-Narromine Volcanic Belt.|||Raggatt, Wombin, Goonumbla Volcanics; Billabong Creek Limestone; Gunningbland Formation.||An association of mafic to intermediate lavas, shallow-water carbonates and volcaniclastic deposits, including deeper-water rocks.|
38197|Northparkes Group|72495|5|Briefly described|p217-220,222,225, 228,231,235,240,241|Late Ordovician|Late Ordovician|Occurs north and south of a prominent gravity low coincident with the Wombin Volcanics. Constituent units often are poorly outcropping. Hosts the Endeavour Cu deposits at Goonumbla. These deposits occur in vertical magnetite rich porphyries of the Wombin Volcanics. Percival (2000) introduced the name Northparkes Volcanic Group, this name is replaced by the Authors with just the Northparkes Group. Intersected by the Parkes Thrust fault.|||Includes the Goonumbla Volcanics, Wombin Volcanics and the Raggatt Volcanics.||Basal volcaniclastic sediments and limestone overlain by limestones interbedded with a thin volcanic interval that is overlain by siltstone.|05-APR-20
73511|Northparkes Igneous Complex|63283|6|Mentioned|p186 Tb. 1|Early Silurian|Late Ordovician|Age:437Ma (Zero porphyry, trachyte).||||||07-FEB-11
73511|Northparkes Igneous Complex|63284|6|Mentioned|p266|||||||||
73511|Northparkes Igneous Complex|63293|6|Mentioned|p468 Fig. 2|Llandovery|Darriwilian|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
73716|Northparkes Intrusive Complex|63287|6|Mentioned|p342|||Shoshonitic rocks.||||||07-FEB-11
83258|Northparkes intrusive complex|73287|5|Briefly described|p662, p666, p670, p677-678|Late Ordovician|Late Ordovician|Macquarie Arc, Northparkes district. Contains vein-hosted molybdenite. Misspelt as Northparkes igneous complex, top of p677.|437.6 Ma, 439.0 Ma mineralisation ages||||Contains at least eight intrusive phases of monzonitic porphyries, only subtle variations in mineralogy and texture.|
73655|Northparkes monzonite|63292|6|Mentioned|p458 Fig. 9|||Informal name.||||||
29728|Norwood Siltstone""|43032|6|Mentioned|p66|||Refers to Robertson (1974)||||||
74173|Noumea Formation|61769|6|Mentioned|p96||Late Devonian|||||||
30655|Nowra "Grits"|43346|14|Not recorded|p2|||||||||
30656|Nowra Grits|43477|14|Not recorded|p18,19|||Ref.to David||||||
30656|Nowra Grits|44861|14|Not recorded|Fig.159,p226,229,||Permian|Unit of Shoalhaven Group. Equivalent to Wandra Wandrian Sandstones.||||||
68194|Nowra Sandstone, lower|60281|6|Mentioned|p59|||Informal - see Nowra Sandstone.  Passes laterally into Wandrawandian Siltstone.||||||
68192|Nowra Sandstone, upper|60281|6|Mentioned|p59|||Informal - see Nowra Sandstone.||||||22-MAR-05
25352|Nowra beds|36148|6|Mentioned|p274|||||||||
25353|Nubrigyn Formation""|33061|6|Mentioned|p28|||Marylebone Dol. possible source of fragments||||||
25353|Nubrigyn Formation""|43517|14|Not recorded|p150-163,Map Pl XII||Early Devonian|||||||
31234|Nubrigyn Limestone|43479|14|Not recorded|p151|Middle Devonian|Early Devonian|||||||
31234|Nubrigyn Limestone|43517|14|Not recorded|p150,152|||||||||
31234|Nubrigyn Limestone|43537|14|Not recorded|p17|||Molong-Wellington area Devonian tetracorals||||||
39402|Nubrygyn Formation|24126|6|Mentioned|p145|||||||||
29455|Nulla Sand Member|42966|6|Mentioned|p239|||Variation/misspelling of Nulla Nulla Sand Member.||||||
68677|Nullawa Suite|23549|5|Briefly described|p523|||Misspelt - should be Nallawa Suite. The Nallawa Suite is a major member of the Boggy Plain Supersuite.  It is part of the Yeovil Batholith.||||||
80008|Nullawonga Latite|70684|6|Mentioned|p3, p33|||||||||
73702|Nullawonga Trachyandesite|63286|6|Mentioned|p304|||||||||07-FEB-11
37225|Nullawonga latite member""|23214|6|Mentioned|p64|||Of Forest Reefs Volcanics.||||||
35440|Nulling Formation""|23170|6|Mentioned|p75|||Superseded by Nulling Member.||||||
32461|Numeralla Chert|22577|6|Mentioned|p120||Darriwilian|||||||
32461|Numeralla Chert|22815|2|Defined|p21, fig10|Early Ordovician|Early Ordovician|Age: Darriwilian. Top of Adaminaby Group.||||||
32461|Numeralla Chert|22857|4|Described|p422 App. 1, Tb. A1.5|Darriwillian|Darriwillian|Of the Adaminaby Group. Contains one or more mappable chert bands 20-100m thick, each separated by turbidites.||||||
32461|Numeralla Chert|23171|6|Mentioned|p11||Darriwilian|||||||
32461|Numeralla Chert|24037|4|Described|p425|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt||||||
32461|Numeralla Chert|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
32461|Numeralla Chert|43233|5|Briefly described|Map Legend|Darriwilian|Darriwilian|Of the Adaminaby Group.||||||17-JAN-07
32461|Numeralla Chert|60902|5|Briefly described|p870|Darriwilian|Darriwilian|Of the Adaminaby Group. Turbidites.||||||11-APR-06
32461|Numeralla Chert|60904|5|Briefly described|p782|Middle Ordovician|Middle Ordovician|Within the Adaminaby Group. ||||||
32461|Numeralla Chert|61413|6|Mentioned|p82 Fig.103.|||||Unit in Adaminaby Group.||||
32461|Numeralla Chert|66196|5|Briefly described|p622|Darriwilian||Strongly bioturbated.||||||
32461|Numeralla Chert|67322|4|Described|p15, p17, p28; Fig.5|Sandbian|Darriwilian|Chert beds contain recrystallised radiolarian tests that were originally ascribed a Darriwilian-Gisbornian age but are now known to be late Darriwilian. Occurs in the Cooma-Mallacoota region.||Of the Adaminaby Group.||Overlies the turbiditic parts of the Adaminaby Group. Equivalent to the Nattery Chert Member and Mozart Chert. Is overlain conformably by Chakola Formation.|Chert dominated units up to 100 m thick that consist of beds of parallel-sided ribbon chert, interbedded with cleaved slate and siltstone and rare sandstone beds.|22-FEB-18
32461|Numeralla Chert|67847|6|Mentioned|p22|||||||||
32461|Numeralla Chert|68466|5|Briefly described|p65-67, 70|Middle Ordovician|Middle Ordovician|Albury-Bega Terrane. A prominent and widespread unit.||Adaminaby Group.||Contemporaneous with the Abercrombie Formation. Correlates with Doongala Chert Member.|Comprises individual beds of parallel-sided ribbon chert up to 50cm thick, interbedded with cleaved slate and siltstone, and rare sandstone beds.|
32461|Numeralla Chert|68592|5|Briefly described|p272, p282, p299, p311, p318|||Cooma area.||Unit in Adaminaby Group.||Equivalent to Nattery Chert Member. Is overlain by Chakola Formation.||
32461|Numeralla Chert|68822|6|Mentioned|p335|Eastonian|Late Cambrian|||||||
32461|Numeralla Chert|69668|5|Briefly described|p929 Fig.2, p931|Middle Ordovician|Middle Ordovician|Cooma-Bega area, Albury-Bega terrane. Prominent and widespread upper chert horizon; over 50m thick.||Unit in Adaminaby Group.||Is overlain by Chakola Formation. Contemporaneous with Abercrombie Formation.|Individual beds of parallel-sided ribbon chert up to 50cm thick, interbedded with cleaved slate and siltstone, and rare sandstone beds.|
32461|Numeralla Chert|70601|5|Briefly described|p43, p49-51, p53|Gisbornian|Darriwilian|Albury-Bega Basin: Inland Zone.||Topmost Adaminaby Group.||Overlies Adaminaby Group. Underlies Bendoc Group, Bogolo Formation, Narooma Chert.||
32461|Numeralla Chert|71069|6|Mentioned|p52, p58, p68, p79|||Original name for the Nattery Chert Member, in the map sheet this name has been replaced by the Nattery Chert Member but in the Cooma area remains current.||Adaminaby Group||Overlain by the Chakola Formation. Equivalent to the Nattery Chert Member.||
32461|Numeralla Chert|71700|5|Briefly described|p8, CD|||Cooma Region.||Adaminaby Group||Equivalent to the Nattery Chert Member.||
30903|Nundle (Barraba) Series|43399|14|Not recorded|p196||Late Devonian|||||||
36969|Nundle Plutonic Suite|23720|5|Briefly described|Map Legend|||Equates with the Clarence River Plutonic Suite.||||||15-DEC-04
36969|Nundle Plutonic Suite|44450|6|Mentioned|p10|||New England Fold Belt.||||||
36969|Nundle Plutonic Suite|71628|6|Mentioned|p3-2; p17-48; p18: 7-8; p19-152|||||||||
30902|Nundle-Barraba Series|43399|14|Not recorded|190||Late Devonian|Ref. to Benson 1913?||||||
77783|Nundooka Sandstone""|66499|5|Briefly described|p66|||[Informal or obsolete name?] Investigation of fish fauna suggests Middle Devonian age likely rather than Famennian age assigned by Neef et al (1995)||||||
69955|Nundora lavas|22671|5|Briefly described|p840 Tb. 2|||Informal name.||||||
73718|Nungar Group|63289|5|Briefly described|p364|Ordovician|Ordovician|Geological Province: Kiandra Volcanic Belt. Consists of quartz-rich sequences.||||||07-FEB-11
36122|Nunniong granite|23309|6|Mentioned|p338|||||||||
36122|Nunniong granite|23454|5|Briefly described|p28|Silurian|Ordovician|430+/-13Ma||||||
74353|Nuntherangie Subgroup|64169|5|Briefly described|p19, p20 Fig. 9|||Subdivison of the Ponto Group erected by author. Top unit. Overlies Palgamurtie Subgroup. Primary rock types are feldspar-phyric; vesicular and pillow-tectured tholeiitic basalt; immature sandstones.||||||20-MAY-08
76168|Nuntherungie Dolerite|66623|6|Mentioned|p95.|||Informal name for a unit now incorporated into Bittles Tank Volcanics.||||||
31619|Nymagee Suite|42726|5|Briefly described|map legend||Silurian|||||||
31619|Nymagee Suite|44093|5|Briefly described|p174 App. 1|Ordovician|Ordovician|Synkinematic to late kinematic granite. Geological Province: Lachlan Fold Belt.||||||
82816|Nymagee felsic dykes|70751|6|Mentioned|p6, p9 Tbl 2, p11, p12 Fig. 4, p38|Lochkovian|Lochkovian|Nymagee felsic dyke swarm. I-type.||||||
82816|Nymagee felsic dykes|72958|6|Mentioned|p6, p11, p57, p61|Lochkovian|Lochkovian|Cobar Basin. Nymagee area. [Informal name] Nymagee felsic dyke swarm, dated at 415.0 +/- 3.2 Ma, intrudes the Mouramba Group.|415.0+/-3.2 Ma SHRIMP U-Pb|||Equivalent to Tarran Volcanics.||
33875|Nyngan Intrusive Complex|22519|4|Described|p8|Silurian|Silurian|||||||
33875|Nyngan Intrusive Complex|72495|5|Briefly described|p226, 239|Silurian|Silurian|||||Thrust over the Hervey Group. Intrudes Canonbar Complex.||30-MAR-20
38948|Nyrang Formation""|23217|6|Mentioned|p9|||(Conolly, 1965a). Informal name. Superseded by 'Mount Cole Formation'.||||||08-MAR-06
38948|Nyrang Formation""|24417|5|Briefly described|p135|||Of Connolly (1965a) - refers to the now Mount Cole Formation.  Name preoccupied by "Nyrang Sandstone Member" of Wallace Shale.||||||
38949|Nyrang Sandstone Member""|23217|6|Mentioned|p9|||(Pickett, 1982).  Member of Wallace Shale in Cheesemans Creek district.  No relationship to "Nyrang Formation" once used for Mount Cole Formation.||||||08-MAR-06
38949|Nyrang Sandstone Member""|24417|6|Mentioned|p135|||Of Wallace Shale.  Not related to the "Nyrang Formation".||||||
25359|O'Briens Creek Sandstone|24248|5|Briefly described|p50 Fig.1|Wenlock|Wenlock|Parent: Yass Formation. Geological Province: Yass Syncline.||||||
25359|O'Briens Creek Sandstone|30069|6|Mentioned|p5|||||||||
25359|O'Briens Creek Sandstone|31852|6|Mentioned|p711|||See also Figs. 1,2,4,5.||||||
25359|O'Briens Creek Sandstone|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature||||||
25359|O'Briens Creek Sandstone|33116|6|Mentioned|Fig.11|||Correlation||||||
25359|O'Briens Creek Sandstone|33325|5|Briefly described|Table 2|||See also Table 3.||||||
25359|O'Briens Creek Sandstone|35386|3|Fully described|p16|||||||||
25359|O'Briens Creek Sandstone|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
25359|O'Briens Creek Sandstone|38691|5|Briefly described|Fig.1|||||||||
25359|O'Briens Creek Sandstone|39331|6|Mentioned|Fig.5-5|||||||||
25359|O'Briens Creek Sandstone|39975|6|Mentioned|p144|||||||||
25359|O'Briens Creek Sandstone|40328|3|Fully described|p97|||||||||
25359|O'Briens Creek Sandstone|40689|6|Mentioned|Fig.4|||||||||
25359|O'Briens Creek Sandstone|42820|6|Mentioned|p29|||of Yass Formation||||||
25359|O'Briens Creek Sandstone|45075|5|Briefly described|p5|||Fauna||||||
25359|O'Briens Creek Sandstone|45147|6|Mentioned|M123|||See also M154||||||
25359|O'Briens Creek Sandstone|68592|5|Briefly described|p429-430 Fig.89, p497, p503, p509|||Link (1970, 1971); Link and Druce (1972), a Formation in their Yass Group. Subsequently, Owen and Wyborn (1979) reduced it to Member status in their similarly-downgraded Yass Formation.||Unit in Yass Group.||Was overlain by Cliftonwood Limestone.||
31052|O'Connor fanglomerates|44970|14|Not recorded|p66|||||||||
28884|O'Hares Beds""|45147|6|Mentioned|M10|||||||||
27526|O'briens Creek Sandstone|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|Misspelling of O'Briens?||||||
39650|Oakdale Formation""|24398|5|Briefly described|p259 Fig. 2|Bolindian|Bolindian|See also p261.  Name used interchangeably with Oakdale Formation in this study.||||||
75481|Oakdale Granite Gneiss|63866|5|Briefly described|p38|||[Replaced by the Georges Bore Granite].||Silver City Suite||Intrudes the Thackaringa Group and/or the Broken Hill Group.||
75481|Oakdale Granite Gneiss|66302|6|Mentioned|p41|Statherian|Statherian|Shown as Oakdale Granite Gneiss (Georges Bore Granite).|1695 +/- 4 Ma |Silver City Suite||||07-JUL-17
75481|Oakdale Granite Gneiss|72461|6|Mentioned|p16 fig 9||||1695 +/- 4 Ma|||||
35425|Oakdale Group""|23170|6|Mentioned|p48|||||||||
26088|Oakfields Tongue|22857|5|Briefly described|p508 App.1 Tb.A1.8|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Ignimbrite at bottom of Native Dog Member. Max. thickness: 30m. Geological Province: Tamworth Forearc Basin.||||||
26088|Oakfields Tongue|32529|3|Fully described|p199|||||||||
26088|Oakfields Tongue|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26088|Oakfields Tongue|32869|5|Briefly described|p168|||Ages. Isismurra Fm.||||||
26088|Oakfields Tongue|44244|5|Briefly described|p35-37, p349|Carboniferous|Carboniferous|Max. thickness: 30m.  Geological Province: Rouchel Block.||||||
26088|Oakfields Tongue|45088|2|Defined|p50|Early Carboniferous|Early Carboniferous|See also Plate 2||||||
26088|Oakfields Tongue|50099|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Max. thickness: >30m. Geological Province: Tamworth Belt/New England Orogen.||||||
26088|Oakfields Tongue|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Of the Isismurra Formation.  Interbedded with the Wolooma Formation.||||||
26088|Oakfields Tongue|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|Of Isismurra Formation. Geological Province: Rouchel Block/Tamworth Belt.||||||
26088|Oakfields Tongue|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Isismurra Formation||||
41350|Oban River Leucogranite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Biotite granite.||||||
41350|Oban River Leucogranite|71628|6|Mentioned|p14: 15, 32|||Barnes and Willis (1989); previously Oban River Leucoadamellite of Binns et al. (1967). Now Oban River Leucomonzogranite.||||||
73781|Oban Suite|69639|5|Briefly described|p15, p94, p133|||New England Orogen.||Moonbi Supersuite|Includes the Kingsgate Leucogranite, Red Range Microleucogranite, Yellow Gap Micromonzogranite and Oban River Leucomonzogranite.|Intruded by the Llangothlin Monzogranite.||
37467|Oberon Granite complex|23214|6|Mentioned|p259|||Informal.||||||
32246|Ogilvies Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah7||||||
32246|Ogilvies Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
23884|Old Timberlight Conglomerate|42567|5|Briefly described|p136|||Reserved J.Nott Aug 1990.||||||
23884|Old Timberlight Conglomerate|62740|4|Described|p365|Oligocene|Oligocene|Of Nadgigomar Sub-Group (Koringaroo Group). Composed of well-sorted silts which form brown to purple-brown laminations. Underlies Spa Creek Siltstone; overlies Sewells Point Siltstone. Thickness: up to 2m.||||||
70359|Olive Gap Formation""|60995|5|Briefly described|p53 Fig. 4, p62|||Of Scott (1982). Informal name for unit at base of the then Marburg Formation. Now incorporated into Ripley Road Sandstone. ||||||
34506|Olney Formation""|22799|6|Mentioned|p28|||Of Lawrence (1975).||||||
39427|Ondyong Point formation|24128|5|Briefly described|p89|||Informal.  Geological Province: Lachlan Fold Belt.||||||
78303|Ooddanatta Formation|68821|5|Briefly described|p296|Cretaceous|Cretaceous|Misspelt Oodnadatta Formation. Lower Cretaceous age.||||Unconformably overlain by the Eyre Formation.||
78302|Ooddnadatta Formation|68821|6|Mentioned|p292 Fig.1|||Misspelt Oodnadatta Formation.||Of the Rolling Downs Group.||||
37816|Oolloo Formation|44113|5|Briefly described|p240|Early Ordovician|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 397m.||||||
76169|Oornoo Sandstone|66623|6|Mentioned|p262.|||Informal name of Morton (1982) cited by Brown (this study). Correlates with Coreena Member, Rolling Downs Group.||||||
70060|Oornoo beds|22857|6|Mentioned|p544 App.1 Tb.A1.12|Early Cretaceous|Early Cretaceous|In Tibooburra area these beds include Coreena Member. ||||||
25367|Ootha "Series"|29987|6|Mentioned|p18|||||||||
25367|Ootha "Series"|34405|6|Mentioned|p125|||Refers Raggatt (1937)||||||
25367|Ootha "Series"|42449|6|Mentioned|p9|||Used by Raggott 1936, 1937. Published Mulholland 1940.||||||
34625|Ootha Beds""|22831|6|Mentioned|p 28|||||||||
30990|Ootha Formation|22519|6|Mentioned|p3|||||||||
30990|Ootha Formation|22768|4|Described|p170-71|Pridoli|Late Wenlockian|||||||
30990|Ootha Formation|22831|3|Fully described|p 41|Early Devonian|Late Silurian|||||||
30990|Ootha Formation|22857|4|Described|p170-171, p450 App.1, Tb.A1.6|Pridoli|Wenlockian|Supersedes "Ootha beds". Unconformably overlain by the Derriwong Group. Shallow water sediments and felsic volcanics. Max. thickness: >300m. Geological Province: Bogan Gate Terrace.||||||
30990|Ootha Formation|23099|5|Briefly described|p582 (Fig 2)|Devonian|Silurian|of Derriwong Group||||||
30990|Ootha Formation|43441|5|Briefly described|21,27|Early Devonian|Late Silurian|||||||08-JAN-10
30990|Ootha Formation|44093|5|Briefly described|p178 App. 1|Early Devonian|Silurian|In the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
30990|Ootha Formation|44160|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||
38919|Ootha Formation""|24417|6|Mentioned|p61|||Superseded by Ootha Group.||||||
33402|Ootha Subgroup|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Derriwong Group.  Includes the Mulguthrie Formation and Yarnel Volcanics.||||||21-JUN-04
70061|Ootha beds""|22857|6|Mentioned|p171|||Superseded by Ootha Formation.||||||
40730|Ootha formation|23309|6|Mentioned|p390|||||||||
39279|Oralla Formation|24243|5|Briefly described|p3 Fig.2|Early Cretaceous|Early Cretaceous|Of Blythesdale Group.||||||
69637|Orange Province Volcanics|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Age: 13-10.5Ma.  In the Bathurst-Goulburn region. ||||||
39405|Orange Shale Beds|24126|6|Mentioned|p185|||||||||
32657|Orange Tuff Formation|46547|14|Not recorded|Not recorded|||||||||
80047|Ottawa Creek Formation|70661|6|Mentioned|p141|||Of Fisher (1972) BSc Hons (unpub.).Discontinued. Name for upper parts of the Tallong Conglomerate and lower parts of the Snapper Point Formation.||||||22-SEP-17
40264|Ottery Adamellite Porphyrite|38915|6|Mentioned|p343|||Geological Province: New England Fold Belt||||||
77355|Ourinperee Ignimbrite|68005|5|Briefly described|p137.|Stephanian|Namurian|[Mis-spelling of Ourimperee].||Unit in Willuri Formation.|||Beige, purple to red, unwelded to slightly welded rhyolitic ignimbrite; underlain by pyroxene andesite at 'Ourimperee'.|
81717|Oxley volcanics|71965|6|Mentioned|p903,913||Early Devonian|Geological province: Thomson Orogen. Nomenclature of Hack et al. (2018) to describe interbedded volcanics intersected in drill holes DDH T11, T14A, DDH T14B, and provided a depositional age of 411+\-2.5 Ma, based on possible correlations with Cobar Supergroup.||||||25-AUG-21
76170|Packsaddle Series|66623|6|Mentioned|p31.|||Name coined by Andrews (1922) for some rocks east of Broken Hill, including units now of Teltawongee Group. Not a recognised formal name.||||||
30733|Paddington sandstone|43358|14|Not recorded|p59,60||Triassic|Ref.to Photo.(Hawkesbury Sandstone)||||||
74355|Paddys Creek beds|64169|5|Briefly described|p19, p20 Fig. 9|||Of the Palgamurtie Subgroup (Ponto Group). Overlain by Weinteriga Creek beds. Similar lithology to Grasmere beds and may prove to be a thrust repeat of those beds.||||||20-MAY-08
74355|Paddys Creek beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group). The Weinteriga Creek beds occur between Paddys Creek beds and Grasmere beds - upper and lower relationships are unclear.||||||26-NOV-08
74355|Paddys Creek beds|67322|6|Mentioned|p39|Permian|Cambrian|Obsolete: Part of the Palgamurtie Subgroup (obsolete) in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map (Stevens et al. 2002); probably a thrust repeat of what is now the Grasmere Formation, as discussed by Buckley (2001). Age is based on the age of the Palgamurtie Subgroup (obsolete).||||||
26828|Padua Granite|42726|5|Briefly described|map legend|Silurian||||||||
30934|Pages Gorge Tuff Member|43417|4|Described|Map Legend||Late Carboniferous|||||||
26094|Palerang Beds|40276|2|Defined|p9|Late Silurian|Late Silurian|||||||
25376|Palerang beds|22768|6|Mentioned|p176|||||||||
25376|Palerang beds|22857|5|Briefly described|p176, p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Arenite, siltstone. Max. thickness: 900m. Geological Province: Captains Flat-Goulburn Trough. ||||||
25376|Palerang beds|39028|6|Mentioned|Map legend|Lochkovian|Pridolian|Pridolian to Lochkovian||||||
25376|Palerang beds|40276|6|Mentioned|p9|||Mention P33||||||
25376|Palerang beds|42820|6|Mentioned|p52|||||||||
35623|Palgamurtie Subgroup|63793|6|Mentioned|p36. ||||||||Includes phyllites and cherts (?air-fall tuffs).|
35623|Palgamurtie Subgroup|64169|5|Briefly described|p19, p20 Fig. 9|||Of the Ponto Group erected by author. Comprises Grasmere beds, Weinteriga Creek beds and Paddys Creek beds. Overlain by Nuntherangie Subgroup.||||||15-MAY-08
35623|Palgamurtie Subgroup|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Magnetic part of Ponto Group. Includes Bendee, Paddy Creek, Weinteriga Creek, Grassmere beds in southern area; Belah, Yandenberry, Koonenberry beds in northern area. Phyllite with fine-gr. magnetite, magnetite-bearing basalt, dolerite +altered mafic rocks||||||26-NOV-08
35623|Palgamurtie Subgroup|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Includes Grasmere, Weinteriga Creek, and Bendee beds. Magnetic part of Ponto Group; characterised by phyllite containing fine-grained magnetite, magnetite-bearing basalt, dolerite and altered mafic rocks, and thin quartz-magnetite units.||||||
35623|Palgamurtie Subgroup|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Includes Grasmere beds, Weinteriga Creek beds and Bendee beds.||||||
35623|Palgamurtie Subgroup|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Ponto Group. Includes Koonenberry beds, Yandenberry beds and Belah beds. Characterised by phyllite containing fine-grained magnetite, magnetite-bearing basalt, dolerite and altered mafic rocks, and thin quartz-magnetite units.||||||01-DEC-08
35623|Palgamurtie Subgroup|64686|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Ponto Group. Magnetic part of Ponto Group; characterised by phyllite containing fine-grained magnetite, magnetite-bearing basalt, dolerite and altered mafic rocks, and thin quartz-magnetite units.||||||
35623|Palgamurtie Subgroup|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes Koonenberry beds, Yandenberry beds and Belah beds.||||||27-NOV-08
35623|Palgamurtie Subgroup|66623|6|Mentioned|pp84-85.|||||Unit in Ponto Group.|Included Weinteriga Creek, Bendee and Grasmere beds.|||
35623|Palgamurtie Subgroup|66929|5|Briefly described|Map legend|||Magnetic part of Ponto Group.||Unit in Ponto Group.|Includes Bendee, Weinteriga Creek, Grasmere, Belah, Yandenberry and Koonenberry beds.||Phyllite containing fine-grained magnetite, magnetite-bearing basalt, dolerite and altered mafic rocks, and thin quartz-magnetite units; abundant psammitic and non-magnetic pelitic phyllite; minor laminated siliceous tuff.|
35623|Palgamurtie Subgroup|66933|6|Mentioned|Map legend|||||Unit in Ponto Group.|Includes Koonenberry beds.|||
35623|Palgamurtie Subgroup|67322|6|Mentioned|p39|Permian|Cambrian|Obsolete: in the legend to the 2nd edn Koonenberry 1:250 000 pre-Permian interpretation map (Stevens et al. 2002). Kayrunnera-Koonenberry region.||Of the Ponto Group.||||22-FEB-18
37433|Paling Yard Tuff|23214|6|Mentioned|p193|||Now included in Merrions Formation.||||||
28903|Paling Yards Tuff|30099|6|Mentioned|Fig.2|||Variation of Paling Yard?||||||
73525|Parilla Formation|10010|5|Briefly described|p17|||Term used for separate Pliocene sand units in some parts of Murray Basin. Overlies Loxton Sands in the Wemen area, but in other areas the distinction is not always apparent hence the combined term Loxton-Parilla Sands is preferred.||||||
73525|Parilla Formation|63777|6|Mentioned|p1104 Fig. 1|||Geological Province: Murray Basin.||||||
73525|Parilla Formation|64823|5|Briefly described|p1011, p1012 Fig. 2b|||Probably should be Parilla Sands.||||||03-FEB-09
73525|Parilla Formation|68140|6|Mentioned|p1700|Neogene|Paleogene|||||||
73526|Parilla Formation""|10010|6|Mentioned|p17|||Informal name - see Parilla Formation. But Loxton-Parilla Sands is preferred term due to lack of distinction between the two sands. Geological Province: Murray Basin.||||||13-AUG-07
28910|Parlour Mountain Leucoadamellite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Massive, equigranular, medium to coarse-grained biotite granite; physical characteristics and associated mineralisation suggest this is probably a "Leucoadamellite".||||||21-DEC-04
28910|Parlour Mountain Leucoadamellite|23790|5|Briefly described|p6 Fig. 5|||||||||
28910|Parlour Mountain Leucoadamellite|38842|6|Mentioned|p286|||||||||
28910|Parlour Mountain Leucoadamellite|42378|6|Mentioned|Table 1 P9|||||||||
28910|Parlour Mountain Leucoadamellite|43091|5|Briefly described|Map legend|||Granitoids.||||||19-FEB-08
28910|Parlour Mountain Leucoadamellite|69323|6|Mentioned|p48|Lopingian|Lopingian|Geological province: New England Orogen. Superseded, see Parlour Mountain Leuzomonzogranite.|254.7+\-1.6 Ma (SHRIMP; Cross and Blevin, 2010)|||||03-DEC-19
28910|Parlour Mountain Leucoadamellite|71628|6|Mentioned|p19: 141-145|||Flinter (1982), after unpublished work by Jones (1976) and Cuddy (1978) who had referred to the unit as Parlour Mountain Granite. Now Parlour Mountain Leucomonzogranite.||||||
25381|Parlour Mountain volcanic complex|42378|5|Briefly described|Table 1 P8|||Informal name.||||||10-DEC-07
35222|Parnel Formation|23160|6|Mentioned|fig1|||Probably Misspelt.||||||
34502|Parnell Beds|22771|6|Mentioned|Table12.2p45|||||||||
34502|Parnell Beds|22857|5|Briefly described|p45 Tb. 12.2|||Now part of the Broken Hill Group.||||||
79136|Parnell Metadolerites|70000|5|Briefly described|p36|||Of Purnamoota Subgroup or intruding Purnamoota Subgroup?|||||Basic gneiss from syn-depositional, high-Fe tholeiitic dykes and sills; locally very abundant.|10-JUN-15
79136|Parnell Metadolerites|73243|6|Mentioned|p52 Fig.1|||[Also mentions Parnell sills of Stevens et al., (2008) on p68]|||||Sills.|
79136|Parnell Metadolerites|73308|6|Mentioned|p607 Fig.1|||||||||
34507|Parnell Suite|22771|6|Mentioned|Table12.2p45|||||||||
34507|Parnell Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Now part of the Sundown Group (Willyama Supergroup). Referred to as Suite 5 by Stevens, Stroud et al (1979,1980).||||||
83475|Parnell metadolerites|73482|6|Mentioned|p422 Fig.3|||Sills.||Lady Louise Suite||||
72978|Paronga Claystone|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
27218|Parrabel Beds|24120|5|Briefly described|p6|Permian|Permian|||||||
27218|Parrabel Beds|34293|2|Defined|p49|Permian|Permian|Map P43||||||
27218|Parrabel Beds|40590|6|Mentioned|p334|||||||||
27218|Parrabel Beds|47056|6|Mentioned|Fig.2 P523|||||||||
27218|Parrabel Beds|47059|4|Described|p152|||Misspelling of Parrabel beds||||||
27218|Parrabel Beds|61771|5|Briefly described|p116|||Geological Province: Northern Hastings Terrane. See also Parrabel beds.||||||
40228|Parry Group, lower|38686|6|Mentioned|p56|||Geological Province: New England Fold Belt||||||
41656|Paterson Rhyolite""|44244|6|Mentioned|p99|||Of Sussmilch and David (1920).  Superseded by Paterson Volcanics.||||||25-AUG-04
41657|Paterson Toscanite""|44244|6|Mentioned|p99|||of Engel et al (in Packham 1969).  Superseded by Paterson Volcanics.||||||25-AUG-04
28913|Paterson toscanite|30312|6|Mentioned|p60|||See also p64.Middle - Upper Carboniferous||||||19-JUL-21
28913|Paterson toscanite|32106|6|Mentioned|p305|||Palaeomagnetic data [wrong State? should be NT? CEBFeb95]||||||
28913|Paterson toscanite|43479|14|Not recorded|p173(fig)|||||||||
32398|Peachvale Formation|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hyandra Creek Group.   Rhyolite breccia, rhyolite, minor spilite.||||||
41274|Peak Formation|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group. Includes: Mogongong Conglomerate Member.  Red shale, mudstone, siltstone, minor sandstone. Overlies: Warrumba Volcanics.||||||05-JUL-04
80273|Peak Rhyolite""|71285|6|Mentioned|p550|Early Devonian|Late Silurian|Cobar region. Mentioned as a possible source of (minor) sulfur contribution at the New Cobar mineral deposit.||||||
81735|Peak rhyolite''|69043|5|Briefly described|p3, 5, 6, 79-85|||Previous magmatic crystallisation age: 423.2+/-3.5 Ma U-Pb SHRIMP (Black, 2007). Current sample: 418.3+/-3 Ma U-Pb SHRIMP.||||Interbedded with Chesney Formation.|flow foliated rhyolite.|25-NOV-19
81735|Peak rhyolite''|69801|6|Mentioned|p1, p135|Silurian|Silurian|Cobar Basin.|418.7 +/- 3 Ma (Bodorkos et al., 2013)|||||
81735|Peak rhyolite''|73578|6|Mentioned|p1, p25, p28|Lochkovian|Gorstian|Age of 423.2 +/- 3.5 Ma reported by Black (2007). Age of 418.3 +/- 3.0 Ma reported by Bodorkos et al. (2013).|423.2 +/- 3.5 Ma, 418.3 +/- 3.0 Ma|||||
72899|Peakes Formation|62569|6|Mentioned|p612|||Of the Hervey Group. Forms a sandstone ridge. ||||||
27875|Peaks Sandstone|23214|6|Mentioned|p227|||Superseded by Peaks Formation.||||||
27875|Peaks Sandstone|23392|6|Mentioned|p3|||Superseded by Peaks Formation of Conolly 1965.||||||
27875|Peaks Sandstone|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27875|Peaks Sandstone|29989|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27875|Peaks Sandstone|30731|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27875|Peaks Sandstone|32483|4|Described|p37|||U.Dev. Strat. table 1||||||
27875|Peaks Sandstone|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27875|Peaks Sandstone|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27875|Peaks Sandstone|43499|14|Not recorded|Map Legend|||(Provisional Edition) Goologong-Grenfell Region. Part of Beargamil Sandstone||||||
27875|Peaks Sandstone|43507|2|Defined|p126,128,134-5,138-9||Late Devonian|Defined as Formation of Beargamil Subgoup(Hervey Group)Inc.Mogongong Conglomerate Member. p165||||||
27875|Peaks Sandstone|43508|14|Not recorded|p130,131|||Petrographic analyses. Derived from volcanics, sediments and granite||||||
27875|Peaks Sandstone|43510|2|Defined|p41-2,58,60-1|||||||||
27875|Peaks Sandstone|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
27875|Peaks Sandstone|43516|14|Not recorded|Map Legend||Late Devonian|Part of Beargamil Sub Group||||||
27875|Peaks Sandstone|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Hervey Group. Consists of red shale, mudstone and siltstone; white to pink-red-brown sandstone.||||||17-JUL-08
38942|Peaks Sandstone""|24417|6|Mentioned|p126|||Superseded by Peaks Formation.||||||
35253|Pearl Beach Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
30981|Peat's Ridge basalt|43446|14|Not recorded|p6044|||Ref. to Manwaring 1963||||||
39358|Pee Dee Beds|24120|5|Briefly described|p6|Permian|Permian|||||||
30898|Peel Valley Alluvials|43400|14|Not recorded|map opp.p.188||Quaternary|||||||
30898|Peel Valley Alluvials|43401|2|Defined|p209,212||Neogene|Late Neogene, probably post Pleistocene||||||
35028|Peelwood Shale""|23048|6|Mentioned|p9 fig14|||||||||
35028|Peelwood Shale""|50124|6|Mentioned|p130|||Informal name. Geological Province: eastern Lachlan Fold Belt.||||||
70058|Pelton coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Early Permian|Informal reference to a seam within the Greta Coal Measures.||||||
79470|Pendiana Tank Granite|70602|6|Mentioned|p67 Fig 3|Early Devonian|Silurian|Age inferred from Byrock Granite.||Westella Suite||||
32242|Pennyweight Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah4||||||
32242|Pennyweight Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
23897|Pennyweight Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
77356|Penryn Rhyolite|68005|5|Briefly described|p57, p137, p143.|Late Carboniferous|Late Carboniferous|Associated with 3 ignimbrite members of the Willuri Formation. Shown [wrongly] as a unit in Rocky Creek Conglomerate on p143.||Unit in Willuri Formation.|||Beige-orange rhyolite lava, glass and welded rhyolitic ignimbrite. Also felsic volcanic breccia and grey to green andesitic ignimbrite; moderately welded, purple rhyolitic ignimbrite; crystal-rich, grey, beige or red, unwelded rhyolitic ignimbrite.|
37314|Peri Rhyodacite|24010|6|Mentioned|p380 Fig. 6|||||||||
37314|Peri Rhyodacite|65107|6|Mentioned|Fig 4 p279|Late Palezoic|Late Palezoic|Rocky Creek Block. This unit helped constrain the Late Paleozoic pole path for the New England orogen. See also variation Peri Rhyolite.||||||
37299|Peri Rhyolite|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Of Clifden Formation.  Geological Province: New England Orogen.  See also p5, p12.||||||
37299|Peri Rhyolite|24010|6|Mentioned|p381|||||||||
37299|Peri Rhyolite|24348|5|Briefly described|p133 Fig.3, p134|Carboniferous|Carboniferous|||||||
37299|Peri Rhyolite|24603|5|Briefly described|p868 Fig. 3|Namurian|Namurian|Of the Clifden Formation.  Age: 318.0+/-3.4Ma.  See also p897 Fig. 17.  Geological Province: Tamworth Belt.||||||
37299|Peri Rhyolite|24605|2|Defined|p939, p949 App. 1|Namurian|Namurian|Of the Clifden Formation. Maximum thickness: 30m. Age: 318 +/- 3.4 Ma and 317.8 +/- 2.8 Ma. Geological Province: New England Orogen. Referred throughout text as Peri Rhyolite Member.||||||
37299|Peri Rhyolite|50613|5|Briefly described|p219 Fig. 9|||Probably should be Peri Rhyolite Member? Of the Clifden Formation.  Age: ~325Ma.  Geological Province: Rocky Creek Syncline.||||||22-FEB-05
37299|Peri Rhyolite|60299|5|Briefly described|p212 Fig.2c|||Of Clifden Formation . Geological Province: Rocky Creek Block.||||||
37299|Peri Rhyolite|61767|6|Mentioned|p74, p76|||Geological Province: Tamworth Belt.||||||
37299|Peri Rhyolite|65107|6|Mentioned|Fig 11 p286-7|||Rocky Creek Block. See also Peri Rhyodacite||||||
37299|Peri Rhyolite|73487|6|Mentioned|p578|Bashkirian|Bashkirian|Rocky Creek Block.|ca 318 Ma (Opdyke et al., 2000)|||||
40570|Peri Rhyolite Member|24605|3|Fully described|p931, p937, p939|Namurian|Namurian|Of the Clifden Formation. Geological Province: New England Orogen. Age: 317+/- 2.8 Ma. Overlies the Spion Kop Conglomerate and Glen Idle Rhyolite Member. Overlain by the Appleogue Dacite Member. Defined as Peri Rhyolite.||||||
40570|Peri Rhyolite Member|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Of the Clifden Formation. Senior synonym of the informal "Eastons Arm Rhyolite Member"; there is significant overlap between these units eg. trace element similarities. Age: 318.0+/-3.4Ma. Geological Province: Boomi Block. See also p172 Fig. 2. ||||||
40570|Peri Rhyolite Member|65382|5|Briefly described|p714|Bashkirian|Bashkirian|Of Clifden Formation. Age of 317.8 +/- 2.8 given.||||||
30947|Peri Rhyolite Tuff|43429|14|Not recorded|Map Legend|||Description given see Strat form.||||||
30947|Peri Rhyolite Tuff|43435|14|Not recorded|Map Legend||Carboniferous|||||||
77157|Peri Tuff|68003|5|Briefly described|p32 Fig.3-h. |Namurian|Namurian|Tamworth Belt (North), New England Fold Belt. See also reference to Peri Rhyodacite Tuff (p137).||||Overlies Clifden Formation. Is overlain by Rocky Creek Conglomerate.||
77157|Peri Tuff|68005|5|Briefly described|p49 Fig.3-M, p170.|Westphalian|Westphalian|Rocky Creek Block, Tamworth Belt.||||Locally overlies Clifden Formation. Is overlain by Rocky Creek Conglomerate.||
31679|Perico Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
22642|Pericoe Adamellite|22815|4|Described|p70|||||||||
22642|Pericoe Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Pericoe Suite.||||||
25390|Pericoe Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Pericoe Adamellite.||||||
23900|Petroi Leucoadamellite|38842|6|Mentioned|p286|||||||||
23900|Petroi Leucoadamellite|71628|6|Mentioned|p17:18|||Flinders (1981 unpublished). Invalid name; Petroi Metabasalt has precedence. Now Bitter Vine Leucomonzogranite Phase (of Botumburra Range Granodiorite).||||||
70147|Peveril Peak Sequence|23336|3|Fully described|p7 Fig. 4, p10|||Also referred to as Peveril Peak sequence. Of the Mulga Downs Group. Composed of moderately- to well-sorted, fine- to medium-grained quartzarenite and pebble quartzarenite. Unconformably overlies Ponto Beds to the west. Max. thickness: 300m.||||||21-MAR-06
39811|Phacops Bed""|24248|6|Mentioned|p52|||Of Jenkins (1879). Superseded by Rainbow Hill Member (Rosebank Shale).||||||
23901|Pheasant Creek Volcanics|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Part of the Coombadhja Volcanic Complex within the Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
23901|Pheasant Creek Volcanics|23443|5|Briefly described|p418|||||||||
23901|Pheasant Creek Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Coombadjha Volcanic Complex.  Predominantly ignombrite with lesser breccia, crystal tuff and silicic lava: with parts which are strongly foliated, lithic-rich, brecciated or comprised of microbreccia, lava and lava breccia.||||||20-DEC-04
23901|Pheasant Creek Volcanics|23812|5|Briefly described|p29 Tb.3|Late Permian|Early Permian|Of Coombadjha Volcanic Complex.  Maximum thickness: 1500m.||||||
23901|Pheasant Creek Volcanics|23859|5|Briefly described|p937|||Of Coombadjha Volcanic Complex. Geological Province: New England Fold Belt.||||||
23901|Pheasant Creek Volcanics|41041|3|Fully described|p258|||||||||
23901|Pheasant Creek Volcanics|42378|5|Briefly described|Table 1 P6|||Coombadjha Volcanic Complex.||||||
23901|Pheasant Creek Volcanics|71628|5|Briefly described|p17:5; p19: 72, 128|||See also references to Pheasants Creek Volcanics.||Coombadjha Volcanic Complex.||Is intruded by Dundahra Creek Leucosyenogranite and Grasstree Quartz Monzodiorite. Is bounded by Moonta Gully Monzogranite.||
38465|Pheasants Creek Granodiorite|24133|6|Mentioned|p54 Fig. 27|||Geological Province: Lachlan Fold Belt.||||||
41354|Pheasants Creek Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Coombadjha Volcanic Complex.||||||
41354|Pheasants Creek Volcanics|71628|5|Briefly described|p15:5; p17:4|||||Coombadjha Volcanic Complex.||Is intruded by Billyrimba Leucomonzogranite and Dandahra Creek Leucosyenogranite.||
38189|Phosphate Mine Beds|23555|5|Briefly described|p4, p7 Tb. 1|Early Pliocene|Early Pliocene|||||||
75940|Piallaway Ignimbrite Member|65902|5|Briefly described|p195 Fig.2|||Misspelling. See also Piallaway Trig Member Fig.6, Fig.7. [Both are abbreviations of Piallaway Trig Ignimbrite Member] Of Currabubula Formation. Piallaway Trig Member dated at 306+/-4.2 Ma.||||||09-MAR-12
22648|Piallaway Trig Ignimbrite|65107|5|Briefly described|p285|Kasimovian|Kasimovian|Of the Werrie Basin, age: 306+/-4.2 Ma SHRIMP U-Pb Zircon. Constrains pole path apex in the Bowen-Gunnedah-Sydney basin system.||||||
75938|Piallaway Trig Member|65902|5|Briefly described|p202 Fig. 6, 203 Fig. 7|Kasimovian|Muscovian|Of  Currabubula Formation. Dated at 306 +/- 4.2 Ma. See also Piallaway Ignimbrite Member. [Both are abbreviations of Piallaway Trig Ignimbrite Member]||||||09-MAR-12
76171|Picnic Creek Basalt|66623|5|Briefly described|p18.|||See also p13, p26. Accidental capitalisation of basalt at Picnic Creek, that now seems to be included in Mount Arrowsmith Volcanics.||Unit in Farnell Group.||Overlies Sturts Meadows Siltstone. Is overlain by Faraway Hills Quartzite.|Fine-grained, dark-grey basalt.|23-FEB-12
27879|Piercefield seams|37087|4|Described|p202|||||||||
31207|Pigeon House Siltstone|43479|14|Not recorded|p189,218||Artinskian|||||||
30825|Pigeonhouse Creek Siltstone|43383|14|Not recorded|p20|||||||||
26842|Pikes Gully Seam|29941|6|Mentioned|p14|||||||||
26842|Pikes Gully Seam|29942|4|Described|Fig.2|||||||||
26842|Pikes Gully Seam|34466|5|Briefly described|p353|||||||||
26842|Pikes Gully Seam|35823|6|Mentioned|p29|||||||||
26842|Pikes Gully Seam|39346|6|Mentioned|Map legend|Permian|Permian|||||||
26842|Pikes Gully Seam|42182|6|Mentioned|p299|||||||||
26842|Pikes Gully Seam|42648|5|Briefly described|p37|||||||||
26842|Pikes Gully Seam|45090|6|Mentioned|p222|||L. Tatarian||||||
28924|Pikes Gully seam|37087|4|Described|p200|||||||||
28924|Pikes Gully seam|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
28924|Pikes Gully seam|41604|6|Mentioned|p5|||||||||
28924|Pikes Gully seam|44244|5|Briefly described|p240 Fig. 45|Late Permian|Late Permian|Of the Foybrook Formation (Vane Subgroup).||||||
30867|Piles Creek sandstone|43358|14|Not recorded|p51-53,55,58-60||Triassic|(Hawkesbury Sandstone)||||||
30818|Pillaga Beds|43384|14|Not recorded|Map Legend||Jurassic|||||||
39280|Pillaga Sandstone|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
70360|Pillar Valley Subgroup""|60995|5|Briefly described|p53 Fig. 4|||Of Ellice-Flint (1973) and Morrison (1984). Replaced (or part of?) "Tabulam Group". ||||||
80475|Pilleul Andesite|70210|5|Briefly described|p2, p39|Ludlow|Ludlow|Yass-Goulburn district.|420.2 +/- 3.1 Ma.|||||21-JAN-21
80475|Pilleul Andesite|70296|6|Mentioned|p1, p11-12, p24|Ludlow|Ludlow|Goulburn-Yass district.|420.2 +/- 3.1 Ma (SHRIMP U-Pb)|||||21-JAN-21
83568|Pilot A Seam, Upper|73304|6|Mentioned|p75|||[Written as Upper Pilot A Seam].||||||
83570|Pilot A interbeds,Upper|73304|6|Mentioned|p67, p70|||[Written as Upper Pilot A Interbeds and Upper Pilot A interbeds].||||||
83569|Pilot B Seam, Upper|73304|6|Mentioned|p75|||[Written as Upper Pilot B Seam].||||||
81440|Pilot Coal A Interbeds, Upper|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS age of 253.55 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||||||
70059|Pilot coal seam, Lower|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam in the Boolaroo Formation (Newcastle Coal Measures).||||||
70057|Pilot coal seam, Upper|22857|6|Mentioned|p522 App.1 Tb.A1.10|Late Permian|Late Permian|Informal reference to a seam in the Boolaroo Formation (Newcastle Coal Measures).||||||
34692|Pimpira Member|12066|5|Briefly described|p13|Cambrian|Cambrian|Of Wydjah Formation.||||||
34692|Pimpira Member|22857|6|Mentioned|p404 App. 1 Tb. A1.4|||Of the Wydjah Formation. Geological Province: Bancannia Block in the Adelaide Fold Belt||||||
34692|Pimpira Member|22858|6|Mentioned|p99|||||||||
34692|Pimpira Member|62787|4|Described|p77, p76 Fig. 1, p79, p80, p81|Middle Cambrian|Early Cambrian|Of Warris (1967). Of Wydjah Formation (Of Gnalta Group). Thickness: 64m. Interbedded dolostones, phyllitic siltstones and shales.||||||07-FEB-11
34692|Pimpira Member|66623|3|Fully described|pp56-57, pp69-72. |Early Cambrian|Early Cambrian|Included in Gnalta Group by Brock and Percival (2006) based on palaeontological studies. Ordian - early Templetonian. Broadly contemporaneous with Coonigan Formation. About 74 m thick. Contains small shelly fossils.||Unit in Wydjah Formation.|||Prominent yellow-cream dolostone - syn-sedimentary limestone micro-breccia, massive-bedding to parallel laminations, shelly fauna; sporadic recessive interbeds of blue-grey phyllitic shale and siltstone.|
34692|Pimpira Member|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Wydjah Formation.|||Boldly outcropping impure dolomite interbedded with recessive blue-grey shale and siltstone.|
34692|Pimpira Member|67322|4|Described|p9-10|Stage 5|Stage 5|74m thick (including 8-9m total thickness of dolostones). Ordian to early Templetonian, or Toyonian, age from Pelagiella madianensis fossils. Occurs in the Mount Arrowsmith region.||Of the Wydjah Formation|||Consists of four to five prominent dolostone beds (and numerous thin and intermittent dolostones) separated by recessive phyllitic siltstones and shales. Contains several beds of granule conglomerate each up to 0.5m thick.|22-FEB-18
40587|Pine Cliffs Rhyodacite Tuff|24605|6|Mentioned|p950 App.1|||Superseded by Pine Cliffs Rhyolite Member.||||||
37311|Pine Cliffs Rhyolite|23861|5|Briefly described|p4 Fig. 2|Namurian|Namurian|Geological Province: New England Orogen.||||||
37311|Pine Cliffs Rhyolite|24010|6|Mentioned|p390|||||||||
37311|Pine Cliffs Rhyolite|24605|2|Defined|p950 App.1|Namurian|Namurian|Of the Clifden Formation. Thickness at type locality: 25m. Geological Province: New England Orogen. Referred throughout text as Cliffs Rhyolite Member.||||||
37311|Pine Cliffs Rhyolite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of Clifden Formation||||||
31624|Pine Mountain Suite|42726|5|Briefly described|map legend||Silurian|||||||
34275|Pine Ridge Volcanics|22679|6|Mentioned|p 30|||||||||
34275|Pine Ridge Volcanics|23214|6|Mentioned|p146|||Now included in Box Ridge Volcanics.||||||
34275|Pine Ridge Volcanics|68592|5|Briefly described|p673|||Green (1980). Now the lower part of Box Ridge Volcanics.||||Was overlain by Crawford Formation.|Basaltic volcanic rocks and lithic sandstone.|
68034|Piney Range bed a|50613|6|Mentioned|p207 Tb. 1|||Informally named purple ignimbrite in the Piney Range Member (one of three beds - a, b and c).  Overlain by Mount Byar Ignimbrite Member.||||||
35308|Pink Quartzite Member|23173|6|Mentioned|Map Legend|||||||||
35308|Pink Quartzite Member|72296|5|Briefly described|p9, p16, p20|||Smith (1973). Now the Birrimba Member. Girilambone mine area. See p9 for the evolving use of this name. ||Caro Schist.|||Lenses of mineralised chert and quartzite.|
38855|Pinnabar Adamellite|24133|6|Mentioned|p68|||Of Wyborn et al (1987).  Superseded by Boebuck Granodiorite.  Geological Province: Lachlan Fold Belt.||||||
28928|Pinnacles aplite""|33472|5|Briefly described|p470|||||||||
26844|Pintapah Sub-Group|30261|4|Described|Table 1|||Willouran age||||||
26844|Pintapah Sub-Group|33004|6|Mentioned|p134|||||||||
26844|Pintapah Sub-Group|34812|6|Mentioned|Table 1|||||||||
26844|Pintapah Sub-Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26844|Pintapah Sub-Group|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
26844|Pintapah Sub-Group|37931|6|Mentioned|Fig.2|||||||||
26844|Pintapah Sub-Group|39214|6|Mentioned|p5|||See also Table 1||||||
26844|Pintapah Sub-Group|39652|6|Mentioned|p53|||||||||
31123|Pipe Clay Creek Formation|43479|14|Not recorded|p151||Early Devonian|||||||
37113|Pipe Formation""|23217|5|Briefly described|p1, p6, p9|||Informal - see Pipe Formation.  Superseded by Mount Cole Formation.||||||08-MAR-06
37113|Pipe Formation""|23392|6|Mentioned|p21|||||||||
37113|Pipe Formation""|24417|6|Mentioned|p135|||Superseded by Mount Cole Formation.||||||
30939|Pipe-clay Creek Formation|43428|14|Not recorded|p142|||||||||
39422|Pittman formation|24128|5|Briefly described|p48|||Informal - see Pittman Formation.  Geological Province: Lachlan Fold Belt.||||||
37306|Plagyan Ignimbrite|23861|5|Briefly described|p3, p4 Fig. 2|Westphalian|Westphalian|Of Rocky Creek Conglomerate.  Geological Province: New England Orogen.  See also p5, p12.||||||
37306|Plagyan Ignimbrite|24010|6|Mentioned|p381|||||||||
37306|Plagyan Ignimbrite|50613|6|Mentioned|p217|||Abbreviation (or misspelling?) of Plagyan Ignimbrite Member.||||||11-SEP-12
37306|Plagyan Ignimbrite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of the Rocky Creek Conglomerate||||||
37306|Plagyan Ignimbrite|68005|5|Briefly described|p137.|Stephanian|Namurian|See also reference to Plagyan Rhyodacite (p49 Fig.3-M).||Unit in Willuri Formation.|||Interbedded coarse grey or purple rhyolitic ignimbrite and interbedded grey hornblende-rich dacitic to andesitic ignimbrite.|
31001|Plagyan Rhyodacite|43434|14|Not recorded|Map Legend||Carboniferous|||||||
31001|Plagyan Rhyodacite|68003|5|Briefly described|p32 Fig.3-h. |Namurian|Namurian|Tamworth Belt (West), New England Fold Belt.||Unit in Willuri Formation.||||
31001|Plagyan Rhyodacite|68005|6|Mentioned|p49 Fig.3-M, p170.|Westphalian|Namurian|Tamworth Belt. See also reference to Plagyan Ignimbrite (p.137).||Unit in Willuri Formation.||||
40581|Plagyan Rhyodacite Tuff|24605|6|Mentioned|p951 App.1|||Superseded by Plagyan Ignimbrite Member.||||||
77158|Plagyan Rhyodacitic Tuff Member|68003|5|Briefly described|p136.|Carboniferous|Carboniferous|Tamworth Belt (North), New England Fold Belt.||Unit in Rocky Creek Conglomerate.|||Multiple beds of rhyolitic to andesitic crystal and vitric tuff.|
77158|Plagyan Rhyodacitic Tuff Member|68005|5|Briefly described|p143.|Carboniferous|Carboniferous|Shown as a unit in Rocky Creek Conglomerate. See also reference to Plagyan Rhyodacite (p49 Fig.3-M).|||||Multiple beds of rhyolitic to andesitic crystal and vitric tuff.|
69862|Plagyani Ignimbrite Member|61214|6|Mentioned|p179 Tb. 10|||Misspelt - see Plagyan Ignimbrite Member.||||||
82786|Plateau Microgranite Phase|71628|5|Briefly described|p15: 106-107, 109-112, 114|||New name (this study) after work by Mustard (2004). Geochemistry described in great detail.|247.27 +/- 1.2 Ma (Ar40-Ar39: Mustard, 2001).|Surface Hill Leucomonzogranite.|||Very fine-grained, equigranular biotite microgranite;  texture varies with layered, graphic, granophyric, pegmatitic, miarolitic and crenulated variants. Lacks K-feldspar megacrysts and phenocrysts, and enclaves.|
40469|Playgan Ignimbrite|24603|5|Briefly described|p868|||Of the Rocky Creek Conglomerate. Geological Province: Tamworth Belt.||||||
30915|Playgan Rhyolite|43409|14|Not recorded|Map Legend|||"a distinctive pink coarse pyroclastic in Currabuula Fm nr Gunnedah may represent Playgan Rhyolite||||||
30915|Playgan Rhyolite|43429|14|Not recorded|Map Legend|||Ash flow tuff||||||
30915|Playgan Rhyolite|43435|2|Defined|Map Legend||Carboniferous|||||||
30946|Playgan Rhyolite Member|43429|14|Not recorded|Map Legend||Carboniferous|Description given see Strat form.||||||
30957|Playgan Rhyolite Tuff|43435|14|Not recorded|Map Legend|||||||||
82130|Pleasant Hills Granite|72528|5|Briefly described|p108.|Early Devonian|Early Devonian||412.6+/-2.2 Ma|Arthursleigh Suite||||
29635|Plumbago Creek Mudstone|43008|5|Briefly described|map legend|Permian|Permian|New England Fold Belt, east of Drake.||||||
70055|Plumbago Creek beds""|22857|6|Mentioned|p514 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Informal name.||||||
28930|Pocket Beds|29456|5|Briefly described|p423|||||||||
28930|Pocket Beds|31019|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28930|Pocket Beds|32820|6|Mentioned|Table 1|||Refers Owen et al. (in press)||||||
28930|Pocket Beds|33325|5|Briefly described|Table 3|||||||||
28930|Pocket Beds|34405|4|Described|p119|||Table 3.4||||||
28930|Pocket Beds|34692|5|Briefly described|p186|||||||||
28930|Pocket Beds|36413|6|Mentioned|Table 3|||||||||
28930|Pocket Beds|37727|4|Described|p82|||||||||
28930|Pocket Beds|40328|3|Fully described|p69|||||||||
28930|Pocket Beds|45147|6|Mentioned|M77|||||||||
70056|Pokolbin Hills Volcanics""|22857|6|Mentioned|p508 App.1 Tb.A1.8|Westphalian|Westphalian|Informal name. Equivalent to Seaham Formation at Lochinvar.||||||
83261|Pola Fogal Hornblendite|73440|6|Mentioned|p141-142|Devonian|Silurian|U-Pb zircon ages of 436-411 Ma provided by Aitchison and Ireland (1995) and Kimbrough et al. (1993). [See Pola Fogal Complex].|436-411 Ma||||Intrusive rocks.|
79982|Pola Fogal Hornblendite-Tonalite Suite|69601|5|Briefly described|p403, p405-406, p409|||Cross (1983). New England Orogen. This name is used interchangeably with Pola Fogal Suite (see references p403, p405, p407-410). Spatially associated with the Pigna Barney Ophiolitic Complex. Blocks of this unit occur in the Pigna Barney Ophiolitic Complex. Also occurs in close association with Pitch Creek Volcanics. Discordant Pb/U and Pb/Pb results discussed.||||Faulted against Pitch Creek Volcanics.|Silicic intrusives.|
78681|Pola Fogal Suite|50168|5|Briefly described|p160|Early Silurian|Early Silurian||436 +/- 9 Ma (Kimbrough et al., 1993).|||Intrudes the Pitch Creek Volcanics.||06-FEB-18
78681|Pola Fogal Suite|69601|5|Briefly described|p403, p405, p407-410|||New England Orogen. This name is used interchangeably with Pola Fogal Hornblendite-Tonalite Suite (see references p403, p405-406, p409). Spatially associated with the Pigna Barney Ophiolitic Complex; geochronological results suggest a related geological history with that unit. Probable island-arc source. Discordant ages discussed. Serpentine appears to have been emplaced along faults in some members of this unit. Mineralogy variations described. Discordant Pb/U and Pb/Pb results discussed.|436 +/- 9 Ma (minimum emplacement age).||||Silicic intrusives.|
26850|Pollwombra Granite|42726|5|Briefly described|map legend|Silurian||Variation on Pollwombra Granodiorite, Adamellite.||||||
24462|Pomeroy Basalt|39848|2|Defined|p116|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
24462|Pomeroy Basalt|40293|6|Mentioned|p459|||||||||
24462|Pomeroy Basalt|40742|5|Briefly described|p300|||||||||
24462|Pomeroy Basalt|50234|5|Briefly described|Map Legend|Oligocene|Oligocene|Alkali basalt containing porphyritic olivine, Ti-augite, flow-banding, vesicles, xenocrysts and miarolitic cavities.||||||14-NOV-13
24462|Pomeroy Basalt|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|In the Bathurst-Goulburn region. ||||||
24462|Pomeroy Basalt|68592|6|Mentioned|p1814|Cenozoic|Cenozoic|Bishop (1984). Obsolete: this unit is included in the Wheeo Basalt.||||||
32818|Pond's Creek Formation|48830|2|Defined|p9-10||Permian|Conf.o/lies Tomago Coal Measures. Uppermost part of Mulbring Beds. See also p5,7-12,15,18,21, Pl.1,2.||||||
35869|Ponto Beds|23336|6|Mentioned|p5, p10|Mesoproterozoic|Mesoproterozoic|Overlain by Mount Daubeny Formation.||||||21-MAR-06
35869|Ponto Beds|23380|5|Briefly described|p105-107||Proterozoic|of Wonaminta Block. Age: Middle Proterozoic. Preferred name Ponto beds.||||||
35869|Ponto Beds|23469|6|Mentioned|Fig 8 p 322|||||||||
35869|Ponto Beds|23889|6|Mentioned|p35 Fig. 30|Ordovician|Cambrian|||||||
35869|Ponto Beds|50618|5|Briefly described|p249 Fig. 2|Middle Cambrian|Early Cambrian|See also Ponto beds.||||||
35869|Ponto Beds|64685|5|Briefly described|Map Legend|Middle Cambrian|Proterozoic|Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites. Some well-cleaved metabasalts, trachyandesites and laminated dacitic tuffs.||||||
22678|Ponto Formation|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Numerous narrow trends of moderate magnetic intensity occur within linear zones; hinge zones and splaying of trends are interpreted as tight, plunging folds within the unit.||||Overlies Noonthorangee Formation.|Phyllite, quartzo-feldspathic sandstone, tholeiitic metabasalt; minor siliceous tuff bands.|
38001|Poolda Hill granite|24307|5|Briefly described|p970|Paleoproterozoic|Paleoproterozoic|Informal name||||||07-NOV-08
34740|Pooncarie Sandstone""|22893|6|Mentioned|p29|||Abandoned name.||||||
78893|Poplins Member|72296|6|Mentioned|p20|||Trigg (in Gilmore et al., 2012, pp32-36), in describing rocks now considered to be Budgery Sandstone Member which has priority.||||||18-JUN-19
70479|Porphyry Boulder Horizon|62095|6|Mentioned|p255|||Informal name of Carey (1937) for the basal conglomerate of the Currabubula Formation in the northern Werrie Block.  Renamed as Coeypolly Conglomerate Member by Voisey and Williams (1964).||||||
78760|Port Macquarie Serpentinite Melange|62058|6|Mentioned|p14 fig 5, map sheets|||||||||12-MAR-14
38929|Porters Mount Tonalite""|24417|6|Mentioned|p105|||Superseded by Porters Mount Quartz Diorite.||||||
26852|Pot Hole Granite|42726|5|Briefly described|map legend|Silurian||Variation on Pot Hole Adamellite.||||||
41392|Potosi Supersuite|24197|4|Described|p17, p62|Proterozoic|Proterozoic|Example of the Forsayth Association. Comprises the intrusive Alma and Rasp Ridge Gneisses, and the 'Potosi-type' gneisses of Hores Gneiss and Parnell Formation. Strongly peraluminous. Geological province: Broken Hill Inlier.||||||07-FEB-11
41392|Potosi Supersuite|50606|5|Briefly described|p1.1, 1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block. Age: 1690Ma.||||||07-NOV-08
41392|Potosi Supersuite|62728|5|Briefly described|p26|||Of Wyborn et al (1998). Includes the Silver City Suite. Contains rocks now considered to be metamorphosed granites commonly containing abundant K-feldspar megacrysts. Geological Province: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
41392|Potosi Supersuite|64097|5|Briefly described|p328 Appdx., p323|||Includes Barrier and Silver City Suites. This also includes volcanic and intrusive rocks in Olary Domain in South Australia.||||||07-FEB-11
30644|Pott's Hill Sandstone|43317|5|Briefly described|Table 1 p14|||||||||
30644|Pott's Hill Sandstone|43319|14|Not recorded|Map Legend|||||||||
30644|Pott's Hill Sandstone|43320|14|Not recorded|Table 1 p14||Late Triassic|Part of Camden Subgroup||||||
30644|Pott's Hill Sandstone|43385|14|Not recorded|p182||Triassic|||||||
40582|Pound Creek Andesite Tuff Member|24605|6|Mentioned|p952 App.1|||Superseded by Mount Hook Rhyolite Member.||||||
37312|Pound Creek andesite tuff|24010|6|Mentioned|p390|||Informal name.||||||
37312|Pound Creek andesite tuff|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of the Rocky Creek Conglomerate.||||||
34612|Prendergast Tonalite|22815|4|Described|p51|Early Devonian|Late Silurian|||||||
41570|Preston Beds""|60303|6|Mentioned|p14 Appendix|||Informal name - probably superseded by the Preston Formation?  Referred to as the basal and middle "Preston Beds".||||||
33858|Preston beds|22508|5|Briefly described|p7||Early Devonian| Lachlan Fold Belt. Of Electrolytic Zinc Co. (1977)||||||
33858|Preston beds|61964|5|Briefly described|p67, p71, 232|Early Devonian|Early Devonian|One of former informal names for Preston Formation rocks, mapped originally as Ural Volcanics. Superseded by Preston Formation. Subdivided into upper, middle and lower "Preston beds" (Maniw 1980, 1983a) and others.||||||23-OCT-08
26855|Pretty Point Granite|42726|5|Briefly described|map legend|Early Devonian||127.  Of the Wologorong Suite (Bemboka Supersuite).  Formal name not intneded.  Reserved as Pretty Point Tonalite.||||||08-FEB-05
82602|Primley Suite|71628|5|Briefly described|p8: 102|||||Uralla Supersuite.|Primley Monzogranite.|||
25416|Prince of Wales Monzodiorite|24265|5|Briefly described|p1445|Wenlock|Caradoc|Age: 449 +/- 10Ma (K-Ar) and 428.6 +/- 7.6Ma (U-Pb). Geological Province: Lachlan Fold Belt||||||
25416|Prince of Wales Monzodiorite|24267|6|Mentioned|p1511|||Geological Province: Parkes-Narromine Belt||||||
25416|Prince of Wales Monzodiorite|24268|5|Briefly described|p1535, p1536 Fig.2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt||||||
25416|Prince of Wales Monzodiorite|24398|5|Briefly described|p259 Fig. 2|Late Ordovician|Late Ordovician|Superseded by Tettenhall Monzodiorite.  Geological Province: Lachlan Fold Belt.||||||
25416|Prince of Wales Monzodiorite|49794|6|Mentioned|p10|||late Ordovician. cf Prince of Wales Granodiorite, WA.||||||
34282|Princes of Wales Diorite""|22679|6|Mentioned|p 36|||||||||
77363|Pringles Monzonite|68006|6|Mentioned|p140.|||Hosts the Giants Den tin deposit.||Unit in Bundarra Supersuite.||||
77363|Pringles Monzonite|69188|6|Mentioned|p55|||Superseded: see Pringles Monzogranite (p2, p4, p55-59, p79). Appears under this name on the 1:250K Manilla-Narrabri Metallogenic map and 1:1M scale digital geology.||||||
82630|Pringles Suite|71628|5|Briefly described|p4: 48, 52, 55|||||Bundarra Supersuite.|Pringles Monzogranite.|||
28942|Prison Farm Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Prison Farm Granodiorite.||||||
70379|Prospect Hill dolerite|60997|5|Briefly described|p139 Fig. 1|Middle Jurassic|Middle Jurassic|Informal name. Geological Province: Sydney Basin.||||||
31848|Protogine Granite|45003|6|Mentioned|p19|||Not valid strat name||||||
29254|Prudhoe Shale|31296|6|Mentioned|Fig. 2|||||||||
29254|Prudhoe Shale|32187|6|Mentioned|p6|||Camden Sub-Group||||||
29254|Prudhoe Shale|34305|2|Defined|p422|Triassic|Triassic|||||||
29254|Prudhoe Shale|35690|6|Mentioned|p18|||Now abandoned.||||||
29254|Prudhoe Shale|39298|6|Mentioned|Fig. 13.2|||||||||
29254|Prudhoe Shale|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
29254|Prudhoe Shale|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
29254|Prudhoe Shale|42896|5|Briefly described|Fig.8|||refers to Lovering (1954)||||||
29254|Prudhoe Shale|43317|5|Briefly described|Table 1 p14|||||||||
29254|Prudhoe Shale|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
29254|Prudhoe Shale|43319|14|Not recorded|Map Legend|||||||||
29254|Prudhoe Shale|43320|14|Not recorded|Table 1 p14||Late Triassic|Part of Camden Subgroup||||||
29254|Prudhoe Shale|43344|14|Not recorded|p22,59,61|||Unit of Wianamatta Group||||||
29254|Prudhoe Shale|43365|14|Not recorded|p169-210||Triassic|||||||
29254|Prudhoe Shale|43383|14|Not recorded|p23|||Camden Sub-Group||||||
29254|Prudhoe Shale|43385|14|Not recorded|p182||Triassic|||||||
29254|Prudhoe Shale|45090|6|Mentioned|p79|||Wianamatta Gp.||||||
35256|Pulbah Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
38922|Pullabooka beds""|24417|6|Mentioned|p80|||Superseded by Pullabooka Formation.||||||
27224|Pulpit Rock Dacite Member|37986|2|Defined|p310, 312, 313|Late Silurian|Late Silurian|||||||14-APR-22
27224|Pulpit Rock Dacite Member|68592|6|Mentioned|p1141|||Hutton (1981), who defined two subtly different variants of dacitic ignimbrite (the other being Rileys Ridge Rhyodacite Member).||Unit in Bindook Complex.||||
23923|Pulpit Rock member|36600|6|Mentioned|Table 2|||||||||
33995|Pumamoota Subgroup|22575|5|Briefly described|p179 Fig.2|||of Broken Hill Group, Broken Hill Block||||||
82629|Purgatory Suite|71628|5|Briefly described|p19:147|||New name (this study).|||Purgatory Monzogranite.|||
27884|Purlawaugh Beds|23053|6|Mentioned|p25|||(Kenny 1928, 1964).||||||
27884|Purlawaugh Beds|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
27884|Purlawaugh Beds|29698|4|Described|p65|||||||||
27884|Purlawaugh Beds|29699|6|Mentioned|p133|||||||||
27884|Purlawaugh Beds|29909|6|Mentioned|p137|||||||||
27884|Purlawaugh Beds|30608|5|Briefly described|p116|||Lithology||||||
27884|Purlawaugh Beds|30610|6|Mentioned|p320|||Refers Kenny (1928,1963). Replaced by Purlawaugh Formation||||||
27884|Purlawaugh Beds|30910|6|Mentioned|Map legend|Triassic|Triassic|||||||
27884|Purlawaugh Beds|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27884|Purlawaugh Beds|32482|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27884|Purlawaugh Beds|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27884|Purlawaugh Beds|33676|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
27884|Purlawaugh Beds|33709|6|Mentioned|p100|||Jurassic.||||||
27884|Purlawaugh Beds|34254|6|Mentioned|p489|||||||||
27884|Purlawaugh Beds|34394|6|Mentioned|Fig.43|||Refers Dulhunty (1967).||||||
27884|Purlawaugh Beds|40869|6|Mentioned|Fig.2|||||||||
27884|Purlawaugh Beds|43354|5|Briefly described|p105-108,p107||Jurassic|||||||
27884|Purlawaugh Beds|43355|14|Not recorded|Map Legend||Jurassic|Provisional Edition, includes Comiala Shale||||||
27884|Purlawaugh Beds|43356|14|Not recorded|Map Legend||Jurassic|||||||
27884|Purlawaugh Beds|43383|14|Not recorded|p25||Jurassic|||||||
27884|Purlawaugh Beds|43394|14|Not recorded|p105-108||Jurassic|||||||
27884|Purlawaugh Beds|43404|14|Not recorded|Table p11,12|||||||||
27884|Purlawaugh Beds|43405|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27884|Purlawaugh Beds|43407|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27884|Purlawaugh Beds|43410|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27884|Purlawaugh Beds|43534|14|Not recorded|p393,394|||||||||
27884|Purlawaugh Beds|43535|14|Not recorded|p133-136||Jurassic|||||||
27884|Purlawaugh Beds|43554|14|Not recorded|p29|||||||||
27884|Purlawaugh Beds|44028|14|Not recorded|p514|||See Strat Table.||||||
41566|Purlawaugh Formation clayrocks|60267|5|Briefly described|p26|||Informal reference to the claystone of the Purlawaugh Formation.||||||
30871|Purlawaugh Sediments|43393|14|Not recorded|p180,181 map||Jurassic|||||||
39800|Purlawaugh shales, upper|24159|6|Mentioned|p152|||Geological Province: Surat Basin. Informal - see Purlawaugh Formation.||||||
25421|Purlewaugh Shale|34134|6|Mentioned|Cor.Chart|||Lower - Middle Jurassic. Misspelling of Purlawaugh.||||||
80481|Purnamoota Leucogneiss|63866|5|Briefly described|p38|Calymmian|Calymmian||1597 +/- 5 Ma (Page et al., 2005a)|||||
82028|Purnamoota Road leucocratic gneiss|72454|5|Briefly described|p7, p20, p21 Tb.3|Calymmian|Calymmian|Part of the Broken Hill Domain. Varied dates given using U-Pb geochronology on both monazite and zircon. Monazite age: 1586+/-9 U-Pb.|1597+/-3 Ma||||Weakly foliated, coarse grained, quartzofeldspathic granitic gneiss.|
80365|Purnamoota Road leucogneiss|70657|5|Briefly described|p13 Fig.6|||Curnamona Province, Broken Hill Domain. Cusin Creek Granite and Purnamoota Road leucogneiss shown grouped together in Fig.6. Associated with Willyama Supergroup.||||May be equivalent to Cusin Creek Granite.|Leucogneiss.|
80365|Purnamoota Road leucogneiss|73482|5|Briefly described|p430, p431 Fig.9, p436|Calymmian|Calymmian|See also Purnamoota Road gneiss.|1597+/-3 Ma|||||
27543|Purnamoota Sub-Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27543|Purnamoota Sub-Group|41633|6|Mentioned|p121|||||||||
27543|Purnamoota Sub-Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|of Broken Hill Group.||||||07-NOV-08
28945|Purnamoota Super Group|41145|6|Mentioned|Fig.4|||||||||
83163|Purnamoota gneiss|6823|5|Briefly described|p211|||Of Browne (1922) and Chenhall (1973). Previously considered to be old name for the Hores Gneiss, along the Purnamoota Road. This location now considered to be part of Potosi Gneiss.||||||
83419|Purnamoota leucogneiss|62536|5|Briefly described|p639, 641, 655-657|||Broken Hill area. Igneous crystallisation age. Also presented as Purnamoota road leucogneiss.|1597 +/- 3 Ma. U-Pb SHRIMP|||Intrudes Hores Gneiss.|Has strong gneissosity and parallel biotite schistosity.|06-JUL-22
25423|Pyes Creek Leucoadamellite|29988|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25423|Pyes Creek Leucoadamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
25423|Pyes Creek Leucoadamellite|35257|6|Mentioned|p34|||||||||
25423|Pyes Creek Leucoadamellite|38842|6|Mentioned|p286|||||||||
25423|Pyes Creek Leucoadamellite|42378|6|Mentioned|Table 1 P9|||||||||
25423|Pyes Creek Leucoadamellite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Leucogranite.||||||
30905|Pyramid Hill Tuff|43399|14|Not recorded|p190||Tournaisian|See also Lexicon||||||
29211|Quaama granodiorite|40207|6|Mentioned|p902|||||||||
79832|Quarry Formation|13996|6|Mentioned|p129|Silurian|Silurian|Midwestern NSW. Most likely meant to refer to Quarry Creek Limestone (p136). Contains Wenlock conodonts.||||||
82632|Quartz Pot Creek Suite|71628|5|Briefly described|p12:11|||New name.||Sailor Jack Supersuite.|Quartz Pot Creek Monzogranite.|||
37951|Quartz feldspathic Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
79215|Quartzo-Feldspathic Sandstone Member|68592|6|Mentioned|p884|||Superseded. Of Cas et al. (1981). See Kowmung Formation.||||Is overlain by Silicic Breccia Member.||
40452|Quartzo-feldspathic Suite|24592|5|Briefly described|p635|||Informal name. Of the Willyama Supergroup. Overlain by the Calc-silicate Suite. Quartz albite +/- magnetic albitic siltstone/shale + magnetic and iron formation that is between this unit and the overlying Calc-silicate Suite.||||||
40452|Quartzo-feldspathic Suite|66857|5|Briefly described|pp971-972, p976.|Paleoproterozoic|Paleoproterozoic|Informal name for rocks in the Olary Domain, including widespread leucocratic quartzo-feldspathic gneisses formed from granitoids and co-magmatic felsic (rhyolitic) volcanics and epiclastic sediments. |c.1700 Ma (Ashley et al. 1997).|Unit in Willyama Supergroup.||||
36204|Queen Bee Conglomerate Member|23095|5|Briefly described|p610 (table 1)|Early Devonian|Early Devonian|Of Chesney Formation, Nurri Group.||||||
40723|Queens Pinch group|23309|6|Mentioned|p390|||||||||
36337|Quialigo Formation|50234|5|Briefly described|Map Legend|Emsian|Lochkovian|Of the Bindook Volcanic Complex.  Overlies: Bullamalita Conglomerate.||||||
36337|Quialigo Formation|70210|5|Briefly described|p2, p31, p35, p38, p40-41|Lochkovian|Lochkovian|Yass-Goulburn district. Appears on p2 as Quilago Formation. A similar age of 414.9 +/- 3.2 Ma is also given.|414.4 +/- 2.9 Ma.||||Rhyolite.|
41294|Quidong Beds|60007|5|Briefly described|Map legend|Late Silurian|Late Silurian|Limestone, marl, shale, sandstone, quartzite.||||||12-JUL-04
82330|Quidong Limestone Member|62070|5|Briefly described|p37, p38|Ludlow|Wenlock|Abundantly fossiliferous. Dated as close to the Wenlock/Ludlow boundary.||[said to be] Of the Cappanana Formation.||||
73722|Quidong limestone|63290|6|Mentioned|p403|Wenlock|Wenlock|Informal name: see Quidong Limestone (Quidong Orogeny: Crook et al. 1973; Rickards et al. 2004).||||||
24466|Quigleys Hill Tuff|23214|6|Mentioned|p61|||Now included in Blayney Volcanics.||||||
24466|Quigleys Hill Tuff|39663|6|Mentioned|Table 4|||||||||
24466|Quigleys Hill Tuff|49790|5|Briefly described|p14|||||||||
24466|Quigleys Hill Tuff|49794|5|Briefly described|p14|||||||||
34267|Quigleys Hill Tuff""|22679|6|Mentioned|p 21|||Now included in the Blayney Volcanics.||||||
77149|Quipolly gravels|68003|5|Briefly described|p75 Fig.3-r.|Late Miocene|Late Miocene|Mooki Valley, Liverpool Plains.||||Is overlain by Breeza member.|Gravel.|
79156|Quondong volcanics""|70013|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|An informal name [probably invalid: Quondong Limestone, also in NSW, has precedence]. In the northern extent of the Kanbara (geophysical basement) Zone. Tentatively correlated with Mount Arrowsmith Volcanics. Minimum age is given as ?Early Cambrian.||||||
82636|Racehorse Suite|71628|6|Mentioned|p19:148||||||Racehorse Porphyry.|||
68196|Raceview Formartion|60281|6|Mentioned|p30|||Misspelt - see Raceview Formation.||||||22-MAR-05
70382|Raceview sandstone|60996|6|Mentioned|p85 Fig. 21|||Informal - see Raceview Formation. Geological Province: Clarence-Moreton Basin.||||||
41658|Raglan Limestone ""|44244|6|Mentioned|p57|||Informal name of Jenkins (1974) for lower limestone in Ararat Formation.||||||
25428|Railway Slate|40136|6|Mentioned|p25|||||||||
32629|Railway Slates|46568|4|Described|p.423||Late Ordovician|Upper Ordovician. Unit of Beverley Group. "Railway Slate Member" - Defn on Tech. File I/55-16.||||||
41039|Rain Hill Quartz Monzonite""|50191|5|Briefly described|p29|Early Silurian|Late Ordovician|Age: 434.9 +/- 2.3Ma.  Intrudes: Gidginbung Volcanics.||||||25-MAY-04
79841|Rainbow Hill Marl|60987|5|Briefly described|p158|Ludlow|Ludlow|Yass district. Shallow-water strata.||||||
78649|Ralpin Valley Sandstone Member|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Long Flat Volcanics.|||Green, grey to purple, thick- to very thick-bedded, very coarse-grained, poorly sorted volcaniclastic sandstone to granule conglomerate, with rare interbedded grey, buff to green siltstone and grey to pink cobble conglomerate.|07-SEP-15
38784|Ramparts Creek Sandstone Member|50129|4|Described|p23|Givetian|Givetian|Of the Waverly Creek Formation. Conformably overlies the Rocky Tank Conglomerate Member. Thickness at Type Section: ~60m. Geological Province: Bancannia Trough, Darling Basin.||||||
38784|Ramparts Creek Sandstone Member|65759|5|Briefly described|p136|Givetian|Givetian|In South Mootwingee area. Lacustrine complex deposits.||||||
38784|Ramparts Creek Sandstone Member|66623|6|Mentioned|p216.|||A unit in the Waverly Creek Formation described by Neef (2004a); not recognised in this redefinition of the Ravendale Formation.||Unit in Waverly Creek Formation.||Overlies Rocky Tank Conglomerate Member.||
38784|Ramparts Creek Sandstone Member|67562|5|Briefly described|p102|Frasnian|Frasnian|~ 60m thick. Late Frasnian age.||Of the Waverly Creek Formation.||Conformably overlain by the Ravendale Formation. Conformably underlain by the Rocky Tank Conglomerate Member.|Comprises laminated, uniform, unfossiliferous ripple-free lacustrine sandstone.|23-JAN-17
77329|Rangrai Limestone Member|68005|5|Briefly described|p54, p147.|Early Carboniferous|Early Carboniferous|[Mis-spelling of Rangari]. Of Campbell and Engel (1962). Occurs within the upper sandstone units of the Tulcumba Sandstone.||Unit in Tulcumba Sandstone.|||Laterally extensive and fossiliferous; fine-grained oolitic crinoidal limestone and minor bioclastic limestone.|
37450|Rankin Granite|23214|6|Mentioned|p248|||Replaced by Dunkeld Granite.||||||
28167|Rasp Ridge Gneiss|6823|5|Briefly described|p203, 205-208, 210-211, 213, 214,|Palaeoproterozoic|Palaeoproterozoic|Previously interpreted as volcanic in origin.  Here interpreted as a deformed granite. Metamorphosed during the 1640-1660 Ma thermal event reaching upper amphibolite to granulite conditions and producing melt segregations in some parts of the Gneiss. Features a metamorphic age of 1603 +/- 17 Ma and magmatic age of 1682+/-7 Ma (U-Pb zircon SHRIMP)  as derived from Love (1992). Petrography discussed in detail. See also  p220-224, 226, 232-236.|1682+/-7 Ma,1688 +/- 18 Ma (U-Pb magmatic age)|Thackaringa Group|||Medium to coarse grained, biotite foliated, K-feldspar megacryst and garnet gneiss.|26-MAR-22
28167|Rasp Ridge Gneiss|22553|5|Briefly described|p75,fig2p77|Statherian|Statherian|part of Willyama Supergroup.||||||17-SEP-15
28167|Rasp Ridge Gneiss|22575|6|Mentioned|p179 Fig.2|||of the Thackaringa Group||||||
28167|Rasp Ridge Gneiss|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|Age of unit 1690 Ma||||||07-NOV-08
28167|Rasp Ridge Gneiss|22752|6|Mentioned|p 277|||||||||
28167|Rasp Ridge Gneiss|22771|6|Mentioned|Table12.2p45,45|||||||||
28167|Rasp Ridge Gneiss|22788|6|Mentioned|p48|||||||||
28167|Rasp Ridge Gneiss|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Lateral equivalent is Himalaya Formation. Max. thickness: >700m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
28167|Rasp Ridge Gneiss|22884|6|Mentioned|p44|||Geological province: Broken Hill Domain.  Correlates with Ameroo Gneiss in the Olary Domain.||||||26-MAR-09
28167|Rasp Ridge Gneiss|22965|5|Briefly described|p13,14,Fig1||Statherian|||||||
28167|Rasp Ridge Gneiss|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
28167|Rasp Ridge Gneiss|22967|6|Mentioned|p39||Statherian|||||||
28167|Rasp Ridge Gneiss|23025|6|Mentioned|Fig1p75|||||||||
28167|Rasp Ridge Gneiss|23248|5|Briefly described|p168, Fig2p169, 180||Statherian|Max Age: ~1690 Ma.||||||
28167|Rasp Ridge Gneiss|23347|5|Briefly described|p51 Tb. 1, p55|Statherian|Statherian|Of Lady Louise Suite. Age: 1682+/-3Ma (Page et al 2000).  Formation-type amphibolites and felsic intrusives.||||||24-MAR-09
28167|Rasp Ridge Gneiss|23461|5|Briefly described|p204 Fig. 3|||Of the Thackaringa Group.||||||23-JUN-08
28167|Rasp Ridge Gneiss|24197|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. Age: 1688+/-18Ma. Geological province: Broken Hill Inlier.||||||07-FEB-11
28167|Rasp Ridge Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|Parent: Thackaringa Group.||||||17-SEP-15
28167|Rasp Ridge Gneiss|38969|4|Described|p208|||||||||
28167|Rasp Ridge Gneiss|39662|2|Defined|p421|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28167|Rasp Ridge Gneiss|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28167|Rasp Ridge Gneiss|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28167|Rasp Ridge Gneiss|39849|6|Mentioned|Table 2|||||||||
28167|Rasp Ridge Gneiss|40290|6|Mentioned|p1|||||||||
28167|Rasp Ridge Gneiss|40822|6|Mentioned|Fig.2|||||||||
28167|Rasp Ridge Gneiss|41093|6|Mentioned|p252|||||||||
28167|Rasp Ridge Gneiss|41630|6|Mentioned|Fig.1.3|||||||||
28167|Rasp Ridge Gneiss|41633|6|Mentioned|Fig.2.2|||||||||
28167|Rasp Ridge Gneiss|42261|6|Mentioned|Fig 1 P530|||||||||
28167|Rasp Ridge Gneiss|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28167|Rasp Ridge Gneiss|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28167|Rasp Ridge Gneiss|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28167|Rasp Ridge Gneiss|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28167|Rasp Ridge Gneiss|42537|4|Described|p11|||||||||
28167|Rasp Ridge Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
28167|Rasp Ridge Gneiss|42897|5|Briefly described|Fig.3, P321|||||||||
28167|Rasp Ridge Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
28167|Rasp Ridge Gneiss|43086|6|Mentioned|Fig.3|||||||||
28167|Rasp Ridge Gneiss|43264|5|Briefly described|Map Legend||Paleoproterozoic|of Willyama Supergroup.||||||17-SEP-15
28167|Rasp Ridge Gneiss|43266|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43267|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43270|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43271|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43272|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43274|5|Briefly described|Map Legend||Paleoproterozoic|of Thackaringa Group.||||||07-NOV-08
28167|Rasp Ridge Gneiss|43485|6|Mentioned|2-3||Proterozoic|||||||
28167|Rasp Ridge Gneiss|43572|6|Mentioned|Fig.3.2 p6|||||||||
28167|Rasp Ridge Gneiss|46598|6|Mentioned|p303|||||||||
28167|Rasp Ridge Gneiss|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 Kyong Formation and Cues Formation.||||||31-MAY-07
28167|Rasp Ridge Gneiss|50606|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Part of the Potosi Supersuite. Geological Province: Broken Hill Block. Age: 1682-1690 +/- 7Ma (U-Pb).||||||07-NOV-08
28167|Rasp Ridge Gneiss|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Geological Province: Broken Hill Block.||||||07-NOV-08
28167|Rasp Ridge Gneiss|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Intrusive rocks.  Age: 1683+/-3Ma.  Geological Province: Broken Hill Domain.||||||
28167|Rasp Ridge Gneiss|61606|5|Briefly described|p4 Fig.2|||Age: 1682+/-3Ma||||||18-MAY-06
28167|Rasp Ridge Gneiss|61735|5|Briefly described|p647, p634, p635 Fig. 1, p637|Paleoproterozoic|Paleoproterozoic|Magmatic age: 1683+/-3Ma. Maximum metamorphic age: 1609+/-7 Ma U/Pb SHRIMP. Felsic gneiss unit of the Broken Hill Domain. S-type. See also p636 Fig. 2.||||||04-JUN-15
28167|Rasp Ridge Gneiss|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1683+/-3Ma. Geological province: Broken Hill Domain.||||||24-FEB-10
28167|Rasp Ridge Gneiss|62373|5|Briefly described|p503 Fig.2|||Geological Province: Curnamona Province/Broken Hill Domain.||||||
28167|Rasp Ridge Gneiss|62473|6|Mentioned|p73|Paleoproterozoic|Paleoproterozoic|Age: 1682+/-3Ma.||||||17-JUN-09
28167|Rasp Ridge Gneiss|62535|5|Briefly described|p666 Fig.3, p672-673|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1683 +/- 3 Ma.||||Conformable metagranitoid.|
28167|Rasp Ridge Gneiss|62536|5|Briefly described|p633-637, 639-641, 647-648, 654, 658|||Broken Hill area. A concordant sill. Hanging wall and footwall unit of the orebody. Felsic magmatism in this unit was coeval with that of Hores Gneiss. Earlier dating has this unit at 1697 +/- 12 Ma; other age determinations discussed. Metamorphosed c.1609-1595 Ma. Protolith debated; several workers regard it as a (S-type) granite.|1683 +/- 3 Ma (protolith).|Broken Hill Group.|||Mainly quartz-K feldspar-plagioclase-biotite gneiss; megacrysts less abundant than Alma Gneiss and locally absent. Contains no stratiform mineralisation.|
28167|Rasp Ridge Gneiss|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1683 +/- 3 Ma.|||Intrudes Thackaringa Group.||
28167|Rasp Ridge Gneiss|62728|5|Briefly described|p26|||Of Silver City Suite. Geochemically similar to Alma Gneiss. Geological Province: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
28167|Rasp Ridge Gneiss|63102|5|Briefly described|p13, p40|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. Also referred to as Rasp Ridge Granite in text. See Rasp Ridge Granite Gneiss.|1682+\-3 Ma|||Intrudes Thackaringa Group.||22-OCT-19
28167|Rasp Ridge Gneiss|63110|6|Mentioned|p1130|Statherian|Statherian|Age: 1682+/-3Ma (Page et al., 2000a).||||||
28167|Rasp Ridge Gneiss|63186|5|Briefly described|p67 Fig. 3, p68|Paleoproterozoic|Paleoproterozoic|Crystallisation age: 1683+/- Ma and 1591+/-17 Ma (monazite mean). Geological Province: Broken Hill Domain, Curnamona Province. Felsic rocks.||||||07-NOV-08
28167|Rasp Ridge Gneiss|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringe Group. Age: 1682+/-3ma. Geological Province: Broken Hill Block-Euriowie Block. Quartzo-feldspathic gneiss.  See also p29 Fig. 11.||||||07-NOV-08
28167|Rasp Ridge Gneiss|63866|4|Described|p36-p38, p41, p49|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Appears as the rasp Ridge granite gneiss on p41.|1683 +/- 3 Ma (Page et al., 2005a)|Silver City Suite||Intrudes the Broken Hill Group.|S-type granitic gneiss.|
28167|Rasp Ridge Gneiss|64097|5|Briefly described|p302|Paleoproterozoic|Paleoproterozoic|Of Willis et al (1983). Superseded by Rasp Ridge Granite Gneiss.||||||07-FEB-11
28167|Rasp Ridge Gneiss|64316|5|Briefly described|p531, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Ages: 1682+/-7Ma, 1697+/-12Ma, 1688+/-16Ma and 1683+/-3Ma (all SHRIMP U-Pb). Geological Province: Broken Hill Block.||||||07-FEB-11
28167|Rasp Ridge Gneiss|64726|6|Mentioned|p83 Fig.2.|||||||||
28167|Rasp Ridge Gneiss|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Intrudes Thackaringa Group.||
28167|Rasp Ridge Gneiss|64896|6|Mentioned|p1392 Fig. 3|||Geological Province: Curnamona Province.||||||
28167|Rasp Ridge Gneiss|65681|4|Described|pp733-747.|Paleoproterozoic|Paleoproterozoic|Three identified retrograde shear zones are weakly developed. Aligned K-feldspar megacrysts and metasedimentary xenoliths indicate magmatic flow, suggesting igneous origin. Has rapakivi structure.|1697 +/- 12 Ma (Nutman & Ehlers, 1998).|Unit in Willyama Supergroup. Previously regarded as unit in Thackaringa Group.|||Medium- to fine-grained quartz-K-feldspar-plagioclase-biotite gneiss with well-developed gneissosity; locally containing abundant K-feldspar megacrysts, 10-25 mm long, subhedral to anhedral, wrapped by biotite-sillimanite foliation; commonly augen.|16-MAY-13
28167|Rasp Ridge Gneiss|66302|6|Mentioned|p38, p41|Statherian|Statherian|Olary Domain, Curnamona Province. Age is similar to that of the Woman-in-White Amphibolite. [also referred to incorrectly as the Rasp Ridge granite gneiss on p38)|1683 +/- 3 Ma (Page et al, 2005a)|Silver City Suite||Intrudes the Broken Hill Group.||
28167|Rasp Ridge Gneiss|66857|5|Briefly described|p971.|Paleoproterozoic|Paleoproterozoic|Deformed granitoids, not sedimentary rocks or felsic volcaniclastics.||Unit in Willyama Supergroup.|||Quartzo-feldspathic gneiss.|
28167|Rasp Ridge Gneiss|70014|5|Briefly described|Map legend|||Small-scale folds and a strong mineral lineation are typical; local compositional layering (possibly bedding). Ba-rich leucocratic calc-silicate phases, "spotted quartz" phases, and leucocratic quartz-feldspar phases are associated with the gneiss in places. Also contains thin, elongate basic gneiss bodies. The gneisses are interpreted as metamorphosed dacitic to rhyodacitic volcanics and minor subvolcanic intrusives.||Unit in Thackaringa Group.||Overlies Kyong Formation. Is overlain by Allendale Metasediments (Broken Hill Group).|Typically a medium- to coarse-grained quartz-K-feldspar-plagioclase-biotite ("granitic") gneiss, with a well-developed biotite gneissosity. Some sporadic to abundant garnet, and sillimanite-rich variants. Feldspar megacrysts normally absent.|
28167|Rasp Ridge Gneiss|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Curnamona Province.|1683 +/- 3 Ma.|||||
28167|Rasp Ridge Gneiss|73524|5|Briefly described|p4, p5 Fig.3|Statherian|Statherian|Protolith crystallisation age of 1697+/-12 SHRIMP U-Pb zircon (Nutman and Ehlers, 1998). Re-dating resulted in igneous crystallisation age of 1683+/-3 Ma and metamorphic age of c.1600 Ma (Page et al., 2005b).|1697+/-12 Ma, 1683+/-3 Ma, ca. 1600 Ma|Silver City Suite||||
28167|Rasp Ridge Gneiss|73575|6|Mentioned|p831 Fig.5, p835|||||||||
36143|Rasp Ridge Gneiss Formation|23461|6|Mentioned|p202|||||||||
28951|Rathluba Seam|34048|6|Mentioned|p28|||Tomago C.M.||||||
28951|Rathluba Seam|36158|6|Mentioned|p159|||||||||
28951|Rathluba Seam|37167|6|Mentioned|Table 1|||||||||
28951|Rathluba Seam|39292|6|Mentioned|Fig. 6.3|||||||||
28951|Rathluba Seam|40396|6|Mentioned|p13|||||||||
28951|Rathluba Seam|45090|6|Mentioned|p222|||L. Tatarian||||||
31247|Rathluba beds|43491|14|Not recorded|VII/52||Permian|||||||
75989|Ravendale Sandstones|65381|6|Mentioned|p689 Fig. 2|Late Devonian|Late Devonian|Variation on Ravendale Formation.||||||07-MAR-12
31057|Ravensfield Member|43474|14|Not recorded|p7||Artinskian|||||||
74534|Ravenswood Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Gp. Includes Wyelba, Copplestone and Glen Bower Members. Laminated tuffaceous mudstone, cryptalgal laminate, interbedded mudstone, micritic limestone with carbonate nodules, quartz litharenite and biohermal limestone...||||||09-SEP-08
32255|Rawsons Pass Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|glw7||||||
32255|Rawsons Pass Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
23936|Rawsons Pass Granite|42726|5|Briefly described|map legend|Silurian||Reserved 1976. Listed No Longer Required 1989. Var. on name appeared in unpub. ref. RC90/050.||||||
83481|Raymond Terrace dacite|73487|6|Mentioned|p567, p568 Fig.3, p578-579, p585|||Early mapping (Rattigan, 1966) suggested a slightly younger age than the Paterson Volcanics (328 Ma). Also referred to as Raymond Terrace dacite quarry. See also p581 Fig.10, p582 Fig.11. Implied to be of  Italia Road Formation in heading p578.||||||01-SEP-22
39228|Receptaculites australis bed|23898|5|Briefly described|p272 Fig.3|||Informal name. See Receptaculites Limestone Member.||||||
39228|Receptaculites australis bed|24250|5|Briefly described|p106 Fig.3, p107|||Of theTaemas Limestone. Informal name for zone of massive grey limestone at boundary of Bloomfield Limestone Member and Receptaculites Limestone Member. Referred to as R. australis bed in text||||||18-JUN-08
41348|Red Cliff Coal Measure|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Claystone, siltstone, conglomerate, breccia, sandstone, coal. Equivalent to Ipswich Coal Measures.||||||20-JUL-04
28956|Red Cliff coals|41550|6|Mentioned|Fig.13|||||||||
31361|Red Hill Group (NSW)|41630|6|Mentioned|p13|||Mineral deposit category of Andrews (1922).||||||
37160|Red Hill Member|23522|5|Briefly described|p248 Fig 4|Emsian|Pragian|||||||
37160|Red Hill Member|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Molong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
41351|Red Range Microleuco granite|60079|5|Briefly described|Map Legend|Early Triassic|Permian|Microleucogranite.||||||
82637|Red Range Suite|71628|6|Mentioned|p14:23|||||Kingsgate Supersuite.||||
34181|Redan Gneiss""|22641|5|Briefly described|p689|||Age of unit 1560 Ma||||||
25436|Redbank Creek Seam|42182|6|Mentioned|p299|||||||||
25436|Redbank Creek Seam|42648|5|Briefly described|p37|||||||||
31949|Redcliff Coal Measures|43881|14|Not recorded|p103||Triassic|Should be Red Cliff Coal Measures.||||||
31949|Redcliff Coal Measures|60281|5|Briefly described|Fig. 18 Appendix 1|Late Triassic|Early Triassic|Misspelt - see Red Cliff Coal Measures. Of the Ipswich Coal Measures.  Lithic conglomerate and breccia, sandstone, siltstone, coal.  Max. thickness: >100m.||||||17-MAR-05
31949|Redcliff Coal Measures|60995|5|Briefly described|p52 Tb. 1|Late Triassic|Early Triassic|Of the Ipswich Coal Measures. Lithic conglomerate and breccia, sandstone, siltstone, coal. Max. thickness: >100m. Geological Province: Clarence-Moreton Basin.||||||
31949|Redcliff Coal Measures|69297|5|Briefly described|p487 fig 5.38|Late Triassic|Late Triassic|Clarence-Moreton Basin. More than 100m thick. ||||Overlies the Evans Head Coal Measures.|Lithic conglomerate and breccia, sandstone, siltstone and coal.|
39651|Reedy Creek Formation|24398|5|Briefly described|p264, p259 Fig. 2|Eastonian|Eastonian|Geological Province: Lachlan Fold Belt.||||||
31265|Reedy Creek Limestone""|43512|14|Not recorded|p102-104||Early Ordovician|Mapped only (M.Ord)||||||
30790|Reid's Mistake Formation|43344|14|Not recorded|p85||Permian|||||||
30790|Reid's Mistake Formation|43447|14|Not recorded|diag.p26|||Boolaroo Sub-Group||||||
30790|Reid's Mistake Formation|43448|14|Not recorded|p224|||On table only. Unit of Boolaroo Subgroup (Newcastle Coal Measures)||||||
35099|Reids Mistake Tuff|22969|5|Briefly described|p 40|||||||||
35099|Reids Mistake Tuff|23055|6|Mentioned|p24|||See also Reids Mistake Formation p23.||||||
34497|Renmark Beds""|22799|6|Mentioned|p25|||||||||
40366|Renmark Beds, Upper|23921|5|Briefly described|p1109|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.  Informal-see Renmark Group.||||||
28961|Renmark Group Upper|42133|6|Mentioned|Fig.7 P315|||||||||
28961|Renmark Group Upper|42134|5|Briefly described|Fig.5 P338|||||||||
73527|Renmark Group beds, lower|10010|6|Mentioned|p15|||Informal - see Renmark Group. Flood plain and swamp deposits in the Murray Basin. ||||||
40368|Renmark Group beds, upper|23921|5|Briefly described|p1114|Middle Miocene|Middle Miocene|lGeoloigcal Province: Murray Basin.  This is known as the Olney Formation.||||||
34496|Renmark Group""|22799|6|Mentioned|p25|||Of Lawrence (1975).||||||
73528|Renmark Group, upper|10010|6|Mentioned|p15, p19|||Informal - see Renmark Group. Generally refers to the Olney Formation. Overlain by Calivil Formation; overlie Geera Clay. Geological Province: Murray Basin.||||||13-AUG-07
40367|Renmark beds, Upper|23921|5|Briefly described|p1109 Table 1|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.  Informal-see Renmark Group||||||
40367|Renmark beds, Upper|73118|6|Mentioned|p83|||Murray Basin, SA. Included in Olney Formation in VIC.||||||
72970|Renmark beds, lower|61314|5|Briefly described|p129|Oligocene|Paleocene|Informal - see Renmark beds. Consist of freshwater deposits - quartzitic sand, silt (carbonaceous, calcareous or dolomitic), clay (carbonaceous) and lignite. Geological Province: Murray Basin.||||||
72971|Renmark beds, upper|10010|6|Mentioned|p15|||Informal and possibly misspelt? See Renmark Group. ||||||
72971|Renmark beds, upper|61314|5|Briefly described|p129|||Informal - Renmark beds. More argillaceous and carbonaceous than the lower Renmark beds, and increasingly marine towards the top of the Renmark sequence. Geological Province: Murray Basin.||||||
72976|Rewaa Group|61377|5|Briefly described|p149 Fig. SU8|||Misspelling of Rewan Group. Geological Province: Gunnedah Basin.||||||07-FEB-11
35260|Rhyhope Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
26870|Rhylstone Tuff|42726|5|Briefly described|map legend|Carboniferous||Misspelling of Rylstone Tuff.||||||
78590|Rickaby's Creek Gravel|65195|5|Briefly described|p4, p4 Fig.2|Tertiary|Tertiary|Alluvial deposits. Considered to be a conglomerate derived from a braided stream environment. Found on and to the east of the Lapstone Monocline. Overlies Hawkesbury Sandstone in the Lapstone Structural Complex and overlies Wianamatta Group to the east; suggesting deposition after significant exhumation and presumably uplift on the Lapstone Monocline. Appears as Rickaby's Creek Gravels in p4 text.||||||
83573|Rider Seam|73304|6|Mentioned|p71|||Of the Wallabella Coal Member[?].||||||
83289|Ridgeway intrusive complex|73154|6|Mentioned|p84|Late Ordovician|Late Ordovician||~455 Ma emplacement age.|||||
30650|Rifle Range Tuff|43346|2|Defined|p5|||||||||19-JAN-10
23939|Rileys Peak basanite|36557|6|Mentioned|p657|||||||||
26123|Rileys Ridge Rhyodacite Member|37986|2|Defined|p312|Late Silurian|Late Silurian|||||||
26123|Rileys Ridge Rhyodacite Member|68592|6|Mentioned|p1141|||Hutton (1981), who defined two subtly different variants of dacitic ignimbrite (the other being Pulpit Rock Dacite Member).||Unit in Bindook Complex.||||
25445|Rivertree Granite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
25445|Rivertree Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
25445|Rivertree Granite|33476|2|Defined|p88|Triassic|Triassic|||||||
25445|Rivertree Granite|33480|6|Mentioned|p240|||Refers age dating||||||
25445|Rivertree Granite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
25445|Rivertree Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
25445|Rivertree Granite|39627|6|Mentioned|Appendix|||||||||
25445|Rivertree Granite|43008|5|Briefly described|map legend|||||||||
25445|Rivertree Granite|69639|4|Described|p2, p6, p8, p170, p175-p180, p223, p239|Triassic|Triassic|New England Orogen. Spatially related to the Stanthorpe Granite. Previously believed to intrude the Koreelan Creek Granodiorite.  Sample locality, petrography, and geochronology is described. Hosts polymetallic (Zn-Ag) mineralisation.|249.1 +/- 1.3 Ma|Stanthorpe Suite||Intrudes the Koreelan Creek Granodiorite, the Emu Creek Formation and the Razorback Creek Mudstone.|Undeformed, highly porphyritic granite.|
25445|Rivertree Granite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
25445|Rivertree Granite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Olenekian|New England Orogen.|249.1 +/- 1.3 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
25445|Rivertree Granite|71628|6|Mentioned|p16:25|||Thomson (1973). Name changed (this study) to Rivertree Syenogranite to reflect better the composition.||||||
25445|Rivertree Granite|72528|5|Briefly described|p110.|Middle Triassic|Early Triassic|Also mentioned  as Rivertree pluton, p90.|249.1+/-1.3 Ma|||Cut by epithermal-like polymetallic veins.||
82643|Rivertree Granodiorite|71628|6|Mentioned|p16:25|||Offenberg (1968). Name changed (this study) to Rivertree Syenogranite to reflect better the composition.||||||
82642|Rivertree Suite|71628|6|Mentioned|p16:26|||||Cullendore Supersuite.||||
31093|Rix's Creek Formation|43477|4|Described|p15,20,47,49,Pl.3|||(Tomago Coal Measures) See also Lexicon||||||
31093|Rix's Creek Formation|48830|14|Not recorded|p.10|||is really synonym of Tomago Coal Measures.||||||
26875|Rock Flat Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Rock Flat.||||||
32183|Rock Flat Tonalite|22815|4|Described|p83|||||||||
32183|Rock Flat Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Mila Suite.||||||
35864|Rock Holes Member|23336|6|Mentioned|p2, p25|||Of the Snake Cave Sandstone. Conglomeratic quatzite and vein quartz in boulder form. Possibly Emsian - Eifelian in age.  Darling Basin?||||||21-MAR-06
35864|Rock Holes Member|50129|5|Briefly described|p20|||Of the Snake Cave Sandstone.||||||
35864|Rock Holes Member|66623|5|Briefly described|p194.|||Name used (Warris 1967) for lower conglomeratic parts of then Snake Cave Sandstone (now Wana Karnu Group) sequence. Not recognised in this study.||Unit in Wana Karnu Group.|||Conglomerates.|
35864|Rock Holes Member|67562|6|Mentioned|p102|||||Of the Snake Cave Sandstone.|||Conglomerate.|
74861|Rockdale Volcanics|61793|4|Described|p341, p342 Fig. 1(b), p343 Tb. 1, p344-7|Late Permian|Late Permian|Of Emmaville Volcanics. Thickness: 1200m. Geological Province: New England Fold Belt. Ignimbrite with subordinate breccia and air fall tuffs.||||||07-FEB-11
70507|Rockford Member|62095|6|Mentioned|p257|||Abbreviated version of Rockford Ignimbrite Member.||||||
82787|Rockisle Granite|71628|6|Mentioned|p19:151|||Rosenbaum et al. (2012). Now Rockisle Granodiorite.||||||
74023|Rockisle Suite|71628|5|Briefly described|p2: 34, 37, 46, 52, 54, 62; p3: 3, 40-41|||See also 3: 49, 77; p19-152. Landenberger (1996)'s definition included 21 units. The author here has declined giving their lithologies: see p3-3. Has similarities with some units in the Dorrigo Mountain Complex and Moona Plains Complex. Comprised the Rockisle and Kimberley Park intrusions; in this study the Rockisle Suite is unassigned to any Supersuite.|||Rockisle Granodiorite.||Primarily granodiorite with minor monzogranite, with trace amphibole and an absence of garnet.|
38468|Rocklands volcanics|23309|5|Briefly described|p5, 80-81, fig. 1.3, Tb 2.28||Early Devonian|Age: 410 +/- 3Ma.||||||
38468|Rocklands volcanics|24133|5|Briefly described|p20 Fig. 8|Early Devonian|Early Devonian|Informal.  Geological Province: Lachlan Fold Belt.||||||
38468|Rocklands volcanics|61183|5|Briefly described|p71 Fig. 45|||Informal - see Rocklands Volcanics.||||||
29255|Rockley Formation""|40328|6|Mentioned|p167|||||||||
73682|Rockley Volcanic Member|63278|5|Briefly described|p156|Early Gisbornian|Darriwilian|Of the Rockley Volcanics. Succeeds Mozart Chert (Murry and Stewart, 2001). Consists of a package of volcaniclastic material with metabasalt, amphibolite and ultramafic rocks. Geological Province: Rockley-Gulgong Volcanic Belt, LFB.||||||10-APR-13
40225|Rocksberg greenstones|38681|5|Briefly described|p35|Early Permian|Early Permian|Geological Province: New England Fold Belt||||||
31161|Rocky Creek "Series"|43491|14|Not recorded|pVI/9||Carboniferous|= Upper Kuttung Group||||||
68985|Rocky Creek Conglomerate""|60299|5|Briefly described|p209|Carboniferous|Carboniferous|Informal - see Rocky Creek Conglomerate. Geological Province: Rocky Creek Block.||||||
40470|Rocky Creek Conglomerate, lower|24603|6|Mentioned|p895 Fig. 16|||Informal - see Rocky Creek Conglomerate.  See also p868.  Geological Province: Tamworth Belt.||||||
82644|Rocky Creek Granite (NSW)|71628|6|Mentioned|p10: 1, 8|||Included in the Boxwell Suite by Blevin (unpublished). Renamed the Dry Creek Granodiorite in this study, as the name Rocky Creek Granite is already in use (in Queensland).||||||
77396|Rocky Creek Granodiorite|70217|5|Briefly described|v, p1 tbl 1.1, p32-p37, p74, p75, p87|Wuchiapingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from this volume. Petrography, zircon morphology and SHRIMP results discussed in detail.  |257.3 +/- 1.5 Ma (SHRIMP U-Pb)|Boxwell Suite||Intrudes the Texas Beds.|Mildly porphyritic quartz monzodiorite with approximately 70 percent plagioclase, 15 percent quartz, 10 percent alkali feldspar, 5 percent biotite and 2 percent amphibole.|
77396|Rocky Creek Granodiorite|70876|5|Briefly described|p78|Permian|Permian|SHRIMP date is derived from Waltenberg et al, 2015. [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|257.3 +/- 1.5 Ma (SHRIMP U-Pb zircon)|Boxwell Suite||||
77396|Rocky Creek Granodiorite|71628|6|Mentioned|p10: 8|||Renamed the Dry Creek Granodiorite in this study, as the name Rocky Creek Granite is already in use (in Queensland).||||||
68986|Rocky Creek conglomerate""|60299|6|Mentioned|p230|||Informal - see Rocky Creek Conglomerate||||||
82649|Rocky Glen Suite|71628|5|Briefly described|p4-58|||||Bundarra Supersuite.|Rocky Glen Monzogranite.|||
32923|Rocky Peak Granite|48878|4|Described|p.10-11|Devonian|Silurian|On many pages. p.4,12,15,20,38. Silurian+Devonian emplaced in later stages of Bowning Orogeny.||||||
32628|Rocky Pic Granite|46568|14|Not recorded|p.423,425||Silurian|(I55-16/Michelago).||||||
82653|Rocky River Leucoadamellite|71628|6|Mentioned|p8-8|||Binns et al. (1967), after unpublished work by Joyce (1964) and Ransley (1970). Replaced by Blackfellows Gully Leucoadamellite (Leitch et al., 1971 after unpublished work by Flood, 1971).||||||
82654|Rocky River Suite|71628|5|Briefly described|p11: 2, 26, 29, 31, 33, 35|||||Bungulla Supersuite.|Rocky River Monzogranite.|||
68866|Rocky River monzogranite|60422|5|Briefly described|p386, p387, p390 Fig. 4|||Informal - see Rocky River Monzogranite. Of the Bungulla-type granite (Moonbi Supersuite).||||||05-MAY-05
68866|Rocky River monzogranite|71628|6|Mentioned|p11: 24-25|||Mustard (2001, 2004). Broadly equivalent to the current Bungulla Monzogranite.||||||
28972|Rolling Grounds Andesite|34403|5|Briefly described|p146|||||||||
28972|Rolling Grounds Andesite|45147|6|Mentioned|M176|||||||||
38232|Rombo Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Geological Province: Sydney Basin||||||
38312|Rombo seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Same as the Rombo Coal Member?   Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
28974|Rookery Limestone""|39618|6|Mentioned|p70|||||||||
83962|Ropers Creek Monzogranite Phase|71628|5|Briefly described|p11-4; p15: 35, 48, 60, 63-64, 67-69,71|||See also p15: 115. New unit, after a local creek; differentiated geochemically. This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Previously part of Stanthorpe Monzogranite. Location of some outcrops is given. Geochemistry described: is geochemically assigned to Jenners Suite.||Mount Lindesay Monzogranite.||Abuts (probably) Undercliffe Falls, Bookookoorara and Jenners Monzogranites.|High-K, I-type granite.|
34082|Rosedale Shale""|22590|6|Mentioned|Fig3 P754||Emsian|||||||
34082|Rosedale Shale""|23214|6|Mentioned|p204|||Now included in Limekilns Formation.||||||
38932|Rosehill Granite""|24417|6|Mentioned|p100|||Name abandoned - still included as part of the Mortray Hill Granite Complex.||||||
79856|Rosemorder Granite|71889|5|Briefly described|p8, p25-p34, p48, p73|||Extends from the southern end of the Ardlethan Granite. This name is now obsolete as these rocks are instead recognised as the northerly continuation of the Ganmain Granite. Geochemistry is briefly discussed.||||||
79856|Rosemorder Granite|72083|5|Briefly described|p19-22, p38|Silurian|Silurian|Trigg (2016). A NW-SE trending elongate granite body immediately to the S of the Ardlethan Granite. Similar to the Sprys Tank Granite; hence the inferred age. Includes (tentatively) an outcrop of cordierite-bearing porphyritic granite previously mapped (Trigg, ?2016) as Ardlethan Granite; discussed. Contains NE-trending elongate bodies (?dykes) of Boblegigbie Granite.||||Is possibly intruded by Boblegigbie Granite.|Medium-grained equigranular biotite granite; possible altered cordierite.|
81254|Rosemorder granite|72083|6|Mentioned|p22 Photo.9||||||||Cordierite-phyric granite.|
41328|Rough Creek Gneiss|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Greymare Complex"". Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
41328|Rough Creek Gneiss|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
41340|Rough Creek gneissic granite|60086|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Maragle Bathylith (Batholith?).||||||07-NOV-08
82647|Roumalla Monzogranite|71628|6|Mentioned|p4-51|||Bryant and Chappell (2010). Status as a separate unit is unclear; boundaries have not been mapped. Named after Roumalla homestead.||||||
82676|Round Hill gabbro|6823|6|Mentioned|p203, 211, 212, 220, 233, 234, 235|Palaeoproterozoic|Palaeoproterozoic|Shown as Round Hill Metagabbro p211 Tbl 4, p212 Tbl 5, and Round Hill Gabbro p220.|ca. 1600-1570 Ma|||||26-MAR-22
38002|Round Hill metagabbro|24307|6|Mentioned|p970|||||||||
34131|Round Mountain Granite|22636|6|Mentioned|p473||Triassic|Should probably be Round Mountain Adamellite?||||||05-FEB-08
34131|Round Mountain Granite|24123|5|Briefly described|p3|||||||||
34131|Round Mountain Granite|71628|6|Mentioned|p17-32|||Ashley et al. (1995). Now Round Mountain Leucomonzogranite.||||||
73982|Round Mountain Supersuite|68111|5|Briefly described|p969 Table 1.|Late Triassic|Middle Triassic||||Includes Round Mountain Leucoadamellite, Yarrahapinni Adamellite and Carrai Granodiorite.|||04-NOV-14
73982|Round Mountain Supersuite|69639|6|Mentioned|p118, p224||||||Includes the Carrai Suite.|||
40253|Round Mountain group|38842|5|Briefly described|p286|Triassic|Triassic|Geological Province: New England Fold Belt. Age: 225 +/- 10Ma||||||
40253|Round Mountain group|71628|6|Mentioned|p19-44|||Flinter (1982).||||||
39411|Rouse Granite|24126|6|Mentioned|p278|||||||||
72960|Rowena Formation, Lower|63121|6|Mentioned|p231, p234 Fig. 7|||Informal - see Rowena Formation.||||||
72957|Rowena Formation, lower|63121|5|Briefly described|p223|Early Ordovician|Early Ordovician|Informal - see Rowena Formation.||||||13-MAR-07
28980|Ruby Creek Granite""|33476|6|Mentioned|p80|||Refers incorrect usage.||||||22-NOV-07
38337|Ruby Creek granite|23763|5|Briefly described|p543 Fig. 1|Early Triassic|Late Permian|In the Moonbi Supersuite.   Geological Province: New England Fold Belt.||||||22-NOV-07
38337|Ruby Creek granite|71628|6|Mentioned|p15: 79, 105|||Phillips (1968). Now Ruby Creek Leucogranite.||||||
69970|Ruby Creek granites|61783|6|Mentioned|p296|||Informal name.  Occurs as stocks within the Stanthorpe granite.||||||
26881|Rugby Granite|42726|5|Briefly described|map legend|Silurian||||||||
26881|Rugby Granite|68592|5|Briefly described|p1371|||Chappell et al. (1991). Now included in Wallah Granite.||||||
31162|Rutherford Shale|43491|14|Not recorded|pVII/44||Permian|See also Lexicon||||||
30791|Rutherford Stage|43344|14|Not recorded|p84|||Now called Rutherford Formation||||||
30791|Rutherford Stage|43440|14|Not recorded|p91|||Ref.to David 1950. See also Lexicon||||||
30791|Rutherford Stage|43477|14|Not recorded|p15,Pl.3|||Ref. to David||||||
30791|Rutherford Stage|44861|14|Not recorded|p228,245||Early Permian|||||||
25458|Rydal Sub-Group""|32999|6|Mentioned|p38|||Refers Conolly (1962)||||||
34687|Rydal Subgroup|22859|5|Briefly described|p217|||(Conolly 1969a,b).||||||
70054|Rydal Subgroup""|22857|6|Mentioned|p217|Devonian|Devonian|Former subdivision of the Lambie Group (Connolly (1969a.b). ||||||
39414|Rylstone tuff|24126|6|Mentioned|p295|||||||||
73725|Ryrie Sandstone|63290|6|Mentioned|p395, p396 Fig. 3|Llandovery|Llandovery|Of Yalmy Group.||||||
30792|Saddleback Dolerite|43344|14|Not recorded|p77|||See also Lexicon||||||
31094|Saddleback latite|43477|14|Not recorded|p19||Permian|Unit in Gerringong Volcanics||||||
81556|Saddleback latite Member|71542|6|Mentioned|p25|Late Permian|Late Permian|Of southern Sydney Basin.||Unit of Gerringong Volcanics.||Within Broughton Formation.||20-OCT-21
26885|Saint Andrews Beds|29986|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
26885|Saint Andrews Beds|40136|6|Mentioned|p15|||||||||
26885|Saint Andrews Beds|40328|6|Mentioned|p213|||||||||
26885|Saint Andrews Beds|43500|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) (M.Ord)||||||
26885|Saint Andrews Beds|48958|6|Mentioned|Plate 1|||||||||
26885|Saint Andrews Beds|68003|5|Briefly described|p24 Fig.3-e. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion. Coeval with Toongi Group. See also reference to Saint Andrews beds (p143).||||||
30793|Saint John's Beds|43344|14|Not recorded|p110|||||||||
30793|Saint John's Beds|43385|14|Not recorded|p172||Wenlock|||||||
30793|Saint John's Beds|44970|14|Not recorded|p11,32, map||Silurian|||||||
30794|Saint John's Church Beds|43344|14|Not recorded|p113||Silurian|||||||
30794|Saint John's Church Beds|44970|2|Defined|p32,51,54,70,72-76||Silurian|See also Lexicon||||||
73554|Saint Johns Beds|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Grouped with Fairbairn Group, Mount Pleasant Porphyry, London Bridge Formation in legend. Saint is St. in text. Calcareous shale, limestone, sandstone, tuff, porphyry, altered acid lavas. BMR map symbol: Smf.||||||
32817|Saltwater Creek Sandstone Member|48830|14|Not recorded|p.8,12,15|||||||||
26132|Sandal Formation|22857|5|Briefly described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Part of Derriwong Group? Sandstone, siltstone, conglomerates, ?andesites. Contains shelly fossils. Max. thickness: ~1.5km. ||||||
26132|Sandal Formation|24417|5|Briefly described|p50|Devonian|Devonian|||||||
26132|Sandal Formation|35503|2|Defined|p207|Early Devonian|Early Devonian|New name refs Kemezys (1976)Prob.Early Devonian||||||
26132|Sandal Formation|40328|6|Mentioned|p38|||||||||
27562|Sandon Beds|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27562|Sandon Beds|31694|6|Mentioned|p343|||P347||||||
27562|Sandon Beds|31802|6|Mentioned|p137|||Refers Leitch et al. (1971). M. - U.Palaeozoic||||||
27562|Sandon Beds|31806|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27562|Sandon Beds|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27562|Sandon Beds|34350|6|Mentioned|p13|||Early Palaeozoic.||||||
27562|Sandon Beds|35264|6|Mentioned|p13|||||||||
27562|Sandon Beds|36528|6|Mentioned|p175|||||||||
27562|Sandon Beds|36961|6|Mentioned|p217|||||||||
27562|Sandon Beds|38288|5|Briefly described|Table 1|||||||||
27562|Sandon Beds|39214|5|Briefly described|Fig.15|||||||||
27562|Sandon Beds|39331|6|Mentioned|Fig.10-1|||||||||
27562|Sandon Beds|40328|6|Mentioned|p193|||||||||
27562|Sandon Beds|40514|6|Mentioned|p4|||||||||
27562|Sandon Beds|41990|6|Mentioned|Fig.2 P12|||||||||
27562|Sandon Beds|42547|5|Briefly described|p41|||Superseded by Sandon Formation, 1977.||||||
27562|Sandon Beds|50016|5|Briefly described|p353|Carboniferous|Carboniferous|Geological Province: New England Fold Belt||||||
27562|Sandon Beds|69323|5|Briefly described|p41,48|Carboniferous|Devonian|Geological province: New England Orogen.||||Intruded by Khatoun Tonalite. Cut by Regional Felsic Dyke Swarm.||
27562|Sandon Beds|71280|5|Briefly described|p402, p404, p411-412|||Armidale district. Also referred to as Sandon Association (p402).||Tablelands Complex.|||Defined by abundant chert layers.|
27562|Sandon Beds|71628|6|Mentioned|p19-77|||See Sandon beds.||||||
27562|Sandon Beds|71703|6|Mentioned|p192|||Of Korsch (1978). ||||May have concealed boundary with Girrakool Beds.||
38252|Sandon beds metabasalt|23790|5|Briefly described|p10 Fig. 2|Early Carboniferous|Early Carboniferous|Name variation for Sandon beds?   Geological Province: Central Block||||||
68867|Sandy Creek Syenogranite|60422|5|Briefly described|p387 Fig. 2, p388 Tb. 1|Early Triassic|Late Permian|Of the Bungulla-type granite (Moonbi Supersuite).  Fine- to coarse-grained syenogranite. I-type.||||||23-MAR-15
68867|Sandy Creek Syenogranite|71628|6|Mentioned|p15-92|||Mustard (2004). Renamed Sandy Creek Monzogranite in this study.||||||
68868|Sandy Creek syenogranite|60422|5|Briefly described|p386, p387, p390 Fig. 4|||Of the Bungulla-type granite (Moonbi Supersuite).||||||
38273|Sandy Flat Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse-grained, even-textured biotite-hornblende monzogranite with pink feldspar.  An I-type granitoid.||||||22-NOV-07
38273|Sandy Flat Monzogranite|23812|5|Briefly described|p20 Tb.2|Early Triassic|Early Triassic|Age: 247-245Ma (Rb-Sr).||||||
38273|Sandy Flat Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||247 - 244 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38273|Sandy Flat Monzogranite|69639|4|Described|p1, p5, p8, p26, p87-p92, p221, p240|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described.|253.6 +/- 1.1 Ma (SHRIMP)|Bolivia Range Suite||Intruded by the Bungulla Monzogranite.|Relatively unaltered, massive, coarse-grained, alkali feldspar-rich biotite granite (syenogranite).|
38273|Sandy Flat Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Changhsingian|Wuchiapingian|New England Orogen.|253.6 +/- 1.1 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38273|Sandy Flat Monzogranite|71628|6|Mentioned|p14-28|||Henley et al. (2001) after Barnes (1987 unpublished). Originally Sandy Flat Adamellite (Shaw, 1964); later Sandy Flat Leucoadamellite (Flinter, 1982). Now Sandy Flat Leucomonzogranite (this study).||||||
82538|Sandy Flat Suite|71628|5|Briefly described|p14-29|||||Kingsgate Supersuite.|Sandy Flat Leucomonzogranite.|||
36471|Sapling Flat Igneous Complex""|23550|5|Briefly described|p504|||- First name for Wangrah Suite.||||||
79216|Sapling Point Volcanics|68592|5|Briefly described|p473 Fig.97|Silurian|Silurian|Moignard (1970). Name replaced by Hawkins Volcanics.||||Is overlain by Wyelba Member (Glen Bower Formation).||
28174|Sara Beds|35173|6|Mentioned|p102|||||||||
28174|Sara Beds|35264|2|Defined|p15|Permian|Permian|||||||
28174|Sara Beds|36411|6|Mentioned|p269|||Refs Korsch 1978 for definition.||||||
28174|Sara Beds|37808|6|Mentioned|Fig.2|||||||||
28174|Sara Beds|39627|6|Mentioned|p269|||||||||
28174|Sara Beds|40246|6|Mentioned|Fig.1|||||||||
28174|Sara Beds|61805|6|Mentioned|p439 Fig. 2|||Informal. Geological Province: New England Orogen.||||||17-NOV-08
27893|Sawpit Gully Member|33476|6|Mentioned|Table 4|||||||||
27893|Sawpit Gully Member|39279|4|Described|p370|Late Permian|Late Permian|||Of Drake Volcanics.||Overlies Hampden Member. Overlain by Fairfield Creek Member.|Andesitic breccias and tuffs.|13-NOV-15
27893|Sawpit Gully Member|40505|6|Mentioned|p83|||||||||
27893|Sawpit Gully Member|40773|6|Mentioned|p462|||||||||
27893|Sawpit Gully Member|42378|6|Mentioned|Table 1 P10|||||||||
28223|Scammels Granite|34404|6|Mentioned|p101|||Meatamorphic aureole||||||
28223|Scammels Granite|40328|4|Described|p210|||||||||
28223|Scammels Granite|42726|5|Briefly described|map legend|Early Devonian|Silurian|464.  Of the Scammels Suite (Boggy Plain Supersuite).||||||08-FEB-05
28223|Scammels Granite|45087|5|Briefly described|p19|||Chemical analyses||||||
28223|Scammels Granite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Corryong Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
28223|Scammels Granite|60085|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|||||||
31484|Scammels Suite|42726|5|Briefly described|map legend|Early Devonian|Silurian|Of the Boggy Plain Supersuite.  Contains Scammels Granite (informal name).||||||08-FEB-05
42393|Scarborough Formation|60281|6|Mentioned|p11|||||||||
35221|Scarbourough Sandstone|22969|4|Described|Fig 4.1b|Early Triassic|Late Permian|Clifton Subgroup||||||
29730|Scoot Quartzite""|43032|6|Mentioned|p108|||refers to Iten & Carter (1951)||||||
25466|Scotch Derry Seam|39292|6|Mentioned|Fig. 6.3|||||||||
25466|Scotch Derry Seam|45090|6|Mentioned|p223|||Lower Tatarian||||||
74761|Scotts Graig Conglomerate|61964|5|Briefly described|p14 Fig. 4|Pragian|Pragian|Misspelt - see Scotts Craig Conglomerate.||||||
33603|Scrubhut Volcanics|48600|14|Not recorded|p7,Plate 3.|||Relatively flat-lying sequence of rhyolite to dacite tuffs, lapilli tuffs and minor flows. Name from Scrubhut Creek, tributary of Severn River.||||||
31000|Seaham Glacial Beds""|43451|14|Not recorded|Map Legend||Carboniferous|See also Lexicon||||||
31226|Seaham Sandstone|43477|14|Not recorded|p21,56||Permian|Unit of Newcastle Coal Measures||||||
80159|Seamount Basalt""|70601|5|Briefly described|p43-45, p47-48, p50-54, p57|Cambrian|Cambrian|A postulated mid to upper Cambrian seamount on which the Narooma Chert succession was deposited. Narooma Terrane. Informal term to avoid confusion with "Tomakin Basalt" in the Albury-Bega basin succession in the Melville Point area.||||Underlies Narooma Chert.|Basalt, contains limestone clasts, volcanic breccias, foliated greenstone, greenstone breccia.|
30933|Seckolds Limestone Member|43417|4|Described|Map Legend|||||||||
79217|Sentry Box Adamellite|68592|6|Mentioned|p1368|||Of Yacopetti (1987), for a body included in the Wyangala Batholith by Stevens (1955). Named after a local shepherds' hut. Subsequently renamed Sentry Box Granite to accord with standard plutonic rocks nomenclature.||||||
82788|Sepoy Monzogranite Phase|71628|5|Briefly described|p4: 1, 3-5, 18, 21-22|||Herein assigned as a subunit of Copeton Monzogranite. Southern New England Orogen. Unmapped; extent unknown but considered restricted. Geochemistry described. Source of hard rock aggregate for the Copeton Dam.||Copeton Monzogranite.|||A comparatively fine-grained biotite monzogranite.|
28995|Seven Mile Formation|30650|5|Briefly described|p317|||||||||
28995|Seven Mile Formation|33326|6|Mentioned|p446|||Fauna.||||||
28995|Seven Mile Formation|34554|5|Briefly described|p232|||||||||
28995|Seven Mile Formation|43400|2|Defined|178,184,map|Middle Devonian|Early Devonian|Lower and Early Middle Devonian||||||
28995|Seven Mile Formation|43406|14|Not recorded|p42||Early Devonian|(Tamworth Group)||||||
28995|Seven Mile Formation|43428|14|Not recorded|p138|||||||||
28995|Seven Mile Formation|61765|6|Mentioned|p62|||||||||07-FEB-11
83963|Severnlea Monzogranite Phase|71628|5|Briefly described|p15: 35, 102-105, 115|||This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.||Severn River Monzogranite.||||
82605|Shalimar Suite|71628|5|Briefly described|p8-104|||||Uralla Supersuite.|Shalimar Granodiorite.|||
82432|Shallow Lagoon Monzogranite|71628|4|Described|p1-11; p2: 3, 61-65, 67-71; p3: 4|||See also p3: 33-34, 86. New name, after a local watercourse. Uncertainty exists concerning the nature and even the need for this unit (discussed). The author herein assigns this unit to the Shallow Lagoon Suite of the Hillgrove Supersuite but 'for practical purposes' retains it in the Woodburn Complex of the Bakers Creek Supersuite.[??!] Occurs ~25 km SE of Uralla. Crops out as rounded boulders on rounded hills and swampy basins. This age of c.292 Ma by Rosenbaum et al.(2012) may relate to this unit or the Eastlake Monzogranite. Geochemistry briefly described.|292.1 +/- 2.9 Ma.|Woodburn Complex.||Almost entirely surrounds Hillview Gabbro and The Knobs Tonalite. Intrudes Sandon beds. Abuts Eastlake Monzogranite.|A contaminated or hybrid unit: massive, biotite(-amphibole) monzogranite.|
82433|Shallow Lagoon Suite|71628|5|Briefly described|p2-68|||The author says there is an immediate need for a review of the necessity for this unit.||Hillgrove Supersuite.|Shallow Lagoon Monzogranite.||S-type.|
25473|Shannons Flat Granodiorite""|36413|6|Mentioned|p82|||||||||
69720|Shannons Flat Monzogranite|24222|5|Briefly described|p16|||Isotope data given.  Geological Province: Murrumbidgee Batholith, Lachlan Fold Belt.||||||04-FEB-08
30795|Shepherd's Hill Formation|43344|14|Not recorded|p85||Permian|||||||
74762|Shepherds Hill Volcanics""|61964|5|Briefly described|p61, p73|||Previously named Ural Vocanics (Griffin (1959, 1960); renamed by Rayner (1961,1969). Formerly of "Lake Cargelligo Group" (Griffin 1959, 1960). Ural Volcanics name re-instated by Pogson (1968), Goldberry and Pogson (1977). Est. thickness: ~4km (Trigg 1987)||||||28-JAN-09
32627|Shoalhaven Granite|46568|14|Not recorded|p.423,425||Carboniferous|Carboniferous-Devonian. = Boro Granite. (I55-16/Michelago).||||||
67925|Shoalhaven Group, Lower|60281|6|Mentioned|p11|||Informal - see Shoalhaven Group.||||||
67925|Shoalhaven Group, Lower|60285|6|Mentioned|p180 Fig.1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
42218|Shoalhaven Group, Upper|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
42218|Shoalhaven Group, Upper|60285|6|Mentioned|p180 Fig.1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
42218|Shoalhaven Group, Upper|73494|5|Briefly described|p541|Permian|Permian|Southern Sydney Basin. Late Permian.|||||Sedimentary rocks containing detritus from an offshore volcanic arc.|
70010|Shoalwater sandstones|61779|5|Briefly described|p251|||Informal name. Contains abundant quartz, a predominance of metamorphic lithic grains and widespread detrital muscovite. In the Shoalwater terrane. Geological Province: New England Fold Belt.||||||
25476|Shume Beds""|41528|6|Mentioned|p50|||||||||
25476|Shume Beds""|41821|6|Mentioned|p36|||Superseded by Shume Formation in 1978||||||
82817|Shuttleton Rhyolite|72958|6|Mentioned|p29|||[Abbreviation of Shuttleton Rhyolite Member?]. Hosted in the Shume Formation.||||||
35125|Signal Hill Member|23055|5|Briefly described|Fig13p25,36-40|||||||||
79218|Silicic Breccia Member|68592|6|Mentioned|p884, p887-8, p890|||Superseded. Of Cas et al. (1981). See Kowmung Formation (p725-6, p728, p731 Fig.132, 757-8, p821, p742, p874, p884-891).||||Overlies Quartzo-Feldspathic Sandstone Member.||
30844|Silver Gully Agglomerate|43385|14|Not recorded|p175|Early Devonian|Early Devonian|||||||
30844|Silver Gully Agglomerate|43400|14|Not recorded|p177,179,181||Couvinian|Now called Silver Gully Formation. Ref. to Benson 1918. (M.Devn)||||||
23971|Silver King Formation|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
23971|Silver King Formation|22575|6|Mentioned|p179 Fig.2|||Of the Pumamoota Subgroup, Broken Hill Group, Broken Hill Block.||||||11-JUN-08
23971|Silver King Formation|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23971|Silver King Formation|22771|6|Mentioned|p42,Table12.2p45|||||||||
23971|Silver King Formation|22857|4|Described|p42, p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group). Max. thickness: 400 m in type section, up to 300 m south-west of Broken Hill. Geological Province: Willyama Fold Belt.|||||Interlayered thick to thin (2-100m) basic gneiss bodies and pelitic to psammopelitic metasediment; minor, lenticular medium to fine-grained quartz-feldspar-biotite gneiss bodies; rare ferruginous quartz and quartz-gahnite bodies.|01-JUN-15
23971|Silver King Formation|22884|5|Briefly described|p45|||Of the Broken Hill Group. Correlates with the upper amphibolite unit of the Weekeroo Formation (provisionally). Geological province: Broken Hill Domain.||||||26-MAR-09
23971|Silver King Formation|22965|6|Mentioned|Fig 1||Statherian|Part of the Purnamoota Subgroup||||||
23971|Silver King Formation|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
23971|Silver King Formation|22967|6|Mentioned|p39||Statherian|||||||
23971|Silver King Formation|23025|6|Mentioned|Fig1p75|||||||||
23971|Silver King Formation|23160|6|Mentioned|fig1|||||||||
23971|Silver King Formation|23248|5|Briefly described|Fig2p169|||||||||
23971|Silver King Formation|23461|5|Briefly described|p204 Fig.3|||||||||
23971|Silver King Formation|24307|5|Briefly described|p975|Proterozoic|Proterozoic|Parent: Broken Hill Group||||||
23971|Silver King Formation|38969|4|Described|p209|||||||||
23971|Silver King Formation|39662|2|Defined|p430|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23971|Silver King Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23971|Silver King Formation|40290|6|Mentioned|Fig.2|||||||||
23971|Silver King Formation|40822|6|Mentioned|Fig.2|||||||||
23971|Silver King Formation|41093|6|Mentioned|p252|||||||||
23971|Silver King Formation|41145|6|Mentioned|Fig.4|||||||||
23971|Silver King Formation|41630|6|Mentioned|p38|||||||||
23971|Silver King Formation|41633|6|Mentioned|p141|||||||||
23971|Silver King Formation|42181|6|Mentioned|Fig,1 P252|||||||||
23971|Silver King Formation|42261|6|Mentioned|Fig 1 P530|||||||||
23971|Silver King Formation|42537|6|Mentioned|Fig.2 P5|||||||||
23971|Silver King Formation|43052|6|Mentioned|Fig.4.22|||||||||
23971|Silver King Formation|43086|6|Mentioned|Fig.3|||||||||
23971|Silver King Formation|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
23971|Silver King Formation|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23971|Silver King Formation|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23971|Silver King Formation|43572|6|Mentioned|Fig.3.2 p6|||||||||
23971|Silver King Formation|43583|5|Briefly described|Table 1,p2139|||||||||
23971|Silver King Formation|46598|5|Briefly described|p304|||||||||
23971|Silver King Formation|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Purnamoota Subgroup (Broken Hill Group). Overlain by Sundown Group. Underlain by Freyers Metasediments.||||||31-MAY-07
23971|Silver King Formation|50606|5|Briefly described|p1.1|||Geological Province: Broken Hill Block. Of the Broken Hill Group.||||||
23971|Silver King Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group). Geological Province: Broken Hill Block.||||||07-NOV-08
23971|Silver King Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Purnamoota Subgroup (Broken Hill Group). Geological Province: Broken Hill Domain.||||||
23971|Silver King Formation|61606|5|Briefly described|p4 Fig.2|||Of the Broken Hill Group.||||||18-MAY-06
23971|Silver King Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Broken Hill Group.||||
23971|Silver King Formation|63102|5|Briefly described|p13|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Purnamoota Subgroup.||||
23971|Silver King Formation|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
23971|Silver King Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province. ||Purnamoota Subgroup||||
23971|Silver King Formation|70014|5|Briefly described|Map legend|||Also includes rare ferruginous quartz and quartz-gahnite bodies.||Unit in Purnamoota Subgroup.||Overlies Freyers Metasediments. Is overlain by Sundown Group.|Interlayered thick to thin (2-100m) basic gneiss bodies and pelitic to psammopelitic metasediment (becoming more psammitic towards the Formation top) with minor, lenticular medium- to fine-grained quartz-feldspar-biotite gneiss bodies.|
83476|Silver King metadolerites|73482|6|Mentioned|p422 Fig.3|||Sills.||Lady Louise Suite||||
29001|Silver Spud Beds|36961|6|Mentioned|p216|||Misspelling of Silver Spur?||||||
35255|Silverwater Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
38343|Silverwood Association|23763|5|Briefly described|p543 Fig. 1|Devonian|Silurian|Geological Province: New England Fold Belt.||||||
41356|Silverwood Association""|60079|5|Briefly described|Map Legend|Devonian|Silurian|Includes: Willowie Creek beds.||||||
25479|Singleton "Coal Measures"|35926|6|Mentioned|p15|||||||||
29810|Singleton Group|43050|5|Briefly described|p16|||Misspelling of Singleton Supergroup?||||||
29810|Singleton Group|69297|6|Mentioned|p501|Changhsingian|Capitanian|Sydney Basin. |||Includes the Tomago Coal Measures and the Newcastle Coal Measures.|||
26898|Singleton Super Group|22969|4|Described|Fig 4.1a|||||||||
26898|Singleton Super Group|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Geological Province: Sydney Basin.||||||
26898|Singleton Super Group|29942|3|Fully described|p12|||||||||
26898|Singleton Super Group|32266|6|Mentioned|p24|||||||||
26898|Singleton Super Group|33867|6|Mentioned|Fig.1|||See also Fig.2.||||||
26898|Singleton Super Group|37082|6|Mentioned|p161|||||||||
26898|Singleton Super Group|37086|5|Briefly described|p181,183,185,Fig.1,3||Permian|Preferred name Singleton Supergroup.||||||
26898|Singleton Super Group|39287|6|Mentioned|Fig. 2.5|||||||||
26898|Singleton Super Group|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26898|Singleton Super Group|40256|6|Mentioned|p304|||||||||
26898|Singleton Super Group|40883|6|Mentioned|p9|||||||||
26898|Singleton Super Group|42214|6|Mentioned|p467|||||||||
83666|Singorimbah intrusions|73581|6|Mentioned|p27|||Informally named (Carlton, 2016).|||||Group of shallow mafic intrusions.|
41659|Skeletar Foramtion|44244|6|Mentioned|p232|||Misspelt - see Skeletar Formation.||||||
29725|Slate Formation""|43032|6|Mentioned|p55|||Refers to Thomson (1953). Superseded by Great Cobar Slate.||||||
67916|Sloggetts Granite|42726|5|Briefly described|map legend|Carboniferous|Carboniferous|38.  Of the Sloggetts Suite.  Not intended as a formal name.||||||07-FEB-05
34603|Smelter Beds""|22815|5|Briefly described|p37|Ludlow|Ludlow|Of Woodhill (1965) unpubl. Now included in Quidong Limestone.||||||
76969|Smokey Cape Monzogranite|71628|6|Mentioned|p17-99|||Chappell and Bryant (1994, unpublished). Now Smoky Cape Syenogranite.||||||
83070|Smokey Cape Monzonite|73197|6|Mentioned|p482|Triasic|Triassic|New England Orogen, southern. A-type granitoid.||||||
39359|Smoky Cape Adamellite|24120|5|Briefly described|p6|Triassic|Triassic|||||||
39359|Smoky Cape Adamellite|71628|6|Mentioned|p17-99|||Leitch (1972). Now Smoky Cape Syenogranite.||||||
82659|Smoky Cape Suite|71628|5|Briefly described|p17-100|||Coastal Granite Association.|||Smoky Cape Syenogranite.|||
77882|Snake Cave Formation|65759|6|Mentioned|p114 Fig.2|||Fluvial. (Is this the same as Snake Cave Sandstone?)||||||
28123|Snake Cave Sandstone Formation|42298|6|Mentioned|p29 (p101a)|Devonian||Same as Snake Cave Sandstone.||||||
28123|Snake Cave Sandstone Formation|67562|6|Mentioned|p112 Fig.15|||See also Snake Cave Sandstone.||||||
78275|Snake Sandstone|67562|6|Mentioned|p104 Fig.10|||See also Snake Cave Sandstone.||||||
70583|Snapper Point Formation""|62368|5|Briefly described|p391 Fig.10|||Informal - see Snapper Point Formation.||||||
25482|Snapper Point sandstones|36147|6|Mentioned|Plate 2|||||||||
25482|Snapper Point sandstones|36148|6|Mentioned|Photo 1|||||||||
26143|Snodgrass Adamellite|22815|4|Described|p56|Silurian|Silurian|||||||
26143|Snodgrass Adamellite|41905|2|Defined|p54|Silurian||Reserved as Snodgrass||||||
26143|Snodgrass Adamellite|41933|4|Described|Map legend|Late Silurian||||||||
26143|Snodgrass Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||of Dalgety Suite.||||||
26143|Snodgrass Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab20.||||||
26143|Snodgrass Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
40928|Snow Member|50230|4|Described|Map legend|Ludlow|Wenlock|Of the Yass Formation (Douro Group).  Massive olive-green mudstone, very fine-grained sandstone, sporadic fossils and carbonate nodules.  Interbedded with Copplestone Member within the Yass Formation.||||||10-MAY-04
69162|Snowy Bluff Volcanics|60423|5|Briefly described|p381|Early Carboniferous|Late Devonian|Bimodal volcanism. Geological Province: Central Vicotrian Magmatic Province.||||||
25483|Snowy Gap Adamellite|22815|4|Described|p45|Silurian|Silurian|||||||
25483|Snowy Gap Adamellite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25483|Snowy Gap Adamellite|35109|2|Defined|p67|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25483|Snowy Gap Adamellite|35263|6|Mentioned|Table 3|||||||||
25483|Snowy Gap Adamellite|40328|4|Described|p210|||||||||
25483|Snowy Gap Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
25483|Snowy Gap Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab10.||||||
25483|Snowy Gap Adamellite|60078|6|Mentioned|Map Legend||Silurian|||||||
69603|Snowy Province Volcanics|61155|5|Briefly described|p19|Early Miocene|Early Miocene|In Southeastern NSW.||||||
40789|Snowy Province basalts|50126|6|Mentioned|p76|||Informally referring to basalts within the Snowy Province.||||||
40790|Snowy Volcanic Province basalts|50126|5|Briefly described|p69|Early Miocene|Early Miocene|Age: 23 to 17 Ma. Informally referring to basalts within the Snowy Volcanic Province.||||||
23977|Sodwalls adamellite|36600|6|Mentioned|Table 1|||||||||
39409|Sofala volcanics|23309|6|Mentioned|p390|||||||||
39409|Sofala volcanics|24126|6|Mentioned|p210|||Informal.||||||
23978|Soldiers Hill Member|42712|4|Described|Fig3p10, Table1p14|Late Silurian|Late Silurian|Member of Vale Creek Volcanics||||||17-NOV-17
36146|Sooley Volcanics|50234|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Mount Fairy Group. Interbedded with Joppa Formation.||||||
36146|Sooley Volcanics|67820|6|Mentioned|p136 Fig.3|Late Silurian|Silurian|||Mount Fairy Group.||||
36146|Sooley Volcanics|68592|6|Mentioned|p779|||Shortening of Sooley Volcanic Member. See Sooley Volcanic Member.||||||
39400|Sourges shale|24126|6|Mentioned|p141|||||||||
29011|South Head Quartzite""|32999|6|Mentioned|p43|||Refers Sylvester(1966 unpubl.)||||||
77330|Southern Moonbi Supersuite|68005|5|Briefly described|p67.|||Of Bryant (2001) who subdivided the Moonbi Supersuite into two Supersuites.|||Includes Inlet Monzonite; Attunga Creek, Moonbi, Bendemeer, Walcha Road, Congi Creek, Campbells Hill, Standbye and Looanga Monzogranites; Limbri Leucomonzogranite; Back Creek Tonalite.||Medium- to coarse-grained with prominent pink K-feldspar crystals, and minor titanite and magnetite grains.|
77330|Southern Moonbi Supersuite|71628|5|Briefly described|p7: 6, 11, 20, 26, 28, 33; p15-1|||Bryant et al. (2002).||Moonbi Supersuite.||||
26325|Spicers Creek Adamellite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Young Batholith. Intrusive. Adamellite. S-type. BMR map code: Sys.||||||
26325|Spicers Creek Adamellite|39660|6|Mentioned|p450|||||||||
26325|Spicers Creek Adamellite|40328|4|Described|p210|||||||||
26325|Spicers Creek Adamellite|45147|2|Defined|M241|Late Silurian|Late Silurian|Prob.Late Silurian||||||
25489|Spicers Creek Granite|42726|5|Briefly described|map legend|Silurian||436. Variation on Spicers Creek Adamellite.||||||
26905|Spirifer Yassensis Limestone|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
29014|Spirifer yassensis"" limestone|37273|6|Mentioned|p248|||||||||
41660|Spring Creek Conglomerate""|44244|6|Mentioned|p167|||Informal term for Spring Creek Conglomerate - both now superseded by several redefinitions of various units that now form the Gloucester Coal Measures.   See p168 Table 2 for clarification.  See also Spring Cr. Conglomerate.||||||26-AUG-04
75861|Spring Creek Limestone|5253|6|Mentioned|p101.|||||||||
37179|Spring Creek limestone""|23522|6|Mentioned|p256|||Renamed Moore Creek Limestone.||||||
30744|Spring Gully Limestone|43362|14|Not recorded|Map Legend|||(Provisional first edition)||||||
79219|Spring Road Adamellite|68592|6|Mentioned|p1518|||Of Gibson (1973), for the northern end of a pluton which subsequently was renamed Spring Road Granite (Chappell et al., 1991) and later enlarged and assigned to Whick Whack Suite by Blevin (2011). See references to Spring Road Granite (p1482, p1508-1511, p1518-1522).||||||
80004|Springdale Sandstone|70684|5|Briefly described|p54 Fig.27|Late Devonian|Late Devonian|Cootamundra district, Junee-Narromine Volcanic Belt.|||||Largely fluviatile sedimentary rocks.|
24500|Springponds Granodiorite|40132|2|Defined|p238|Early Devonian|Early Devonian|||||||
24500|Springponds Granodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Greenish-grey, massive, equigranular to weakly porphyritic, medium-grained pyroxene-hornblende-biotite tonalite. High magnetic response.||||||19-JUN-08
24500|Springponds Granodiorite|68592|6|Mentioned|p1610, p1642|||Carr et al. (1979). Now incorporated, with Wylora Quartz Gabbro, into Springponds Tonalite on the basis of similar composition, texture and geophysical response.||||||
67849|Springvale Coal|50113|6|Mentioned|p108|||Informal name. Also the name of a coal company. Underlain by granites of the Bathurst Batholith. Geological Province: Lachlan Fold Belt.||||||
74763|Square Head Beds""|61964|5|Briefly described|p64|||Of Wynn (1962), Pogson (1968) and Clare et al (1997) - for rocks with a rich, and well-preserved marine faunal  assemblage from minor rubbly outcrops of  Crossleys Tank Fm. Upgrade to Square Head Formation stems from this study. Underlie Ural Volcanics.||||||27-OCT-08
33860|Square Head beds|22638|6|Mentioned|p69|Devonian|Devonian|||||||
38233|Stafford Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Geological Province: Sydney Basin||||||
29018|Standbye Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
29018|Standbye Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
29018|Standbye Adamellite|31140|6|Mentioned|p55|||||||||
29018|Standbye Adamellite|35257|6|Mentioned|Fig.17|||||||||
29018|Standbye Adamellite|43091|5|Briefly described|Map Legend|||||||||
68972|Stanhope seam|60290|5|Briefly described|p16, 46 Fig.20|Early Permian|Early Permian|Informal name for member of Greta Coal Measures. Coal split by a conglomerate-sandstone. Peat deposited in inactive areas of braidplain and channels. Geological Province: Cranky Corner Basin.||||||07-FEB-11
68972|Stanhope seam|60293|5|Briefly described|p107, p108 Fig.1|||Of Greta Coal Measures. Vitrinite reflectance of organic matter described.||||||
68972|Stanhope seam|60297|5|Briefly described|p172 Fig.3|Permian|Permian|Of the Greta Coal Measures. Thickness: 2.8m. Geological Province: Cranky Corner Basin.||||||05-DEC-07
82790|Stanthorpe Complex|71628|3|Fully described|p1:7, 15; p5: 2; p15: 1-4, 32-116;|Middle Triassic|Early Triassic|See also  p11: 2, 4-6, 38-39; p12: 1-2, 4, 10-12, 17; p14: 2; p16: 1-2, 4, 6-7, 9-10, 13, 18, 26, 28; p19: 5-6, 8-9, 20, 22, 59, 66-67, 71, 80-82, 98, 133, 159, 163-164. Donchak et al. (2007), who intimated this name was interchangeable with Stanthorpe Granite. In this study, incorporates most granites historically referred to as Stanthorpe Monzogranite. Named after the town of Stanthorpe (Qld). Extends 60 km N-S and ~50 km E-W. Exposure is generally good. Includes blocks of Bookookoorara Monzogranite. Numerous age determinations (249 - 238 Ma) are discussed. Lithology, mineralogy detailed. Geochemistry briefly summarised. Associated with Sn-Mo-W and Au mineralisations (described). RELATED UNITS (continued): Encloses Bookookoorara and Boonoo Monzogranites. Is intruded by Warroo Monzogranite Phase. Is faulted against Bungulla Monzogranite, Granite Hills Complex. Abuts Karonstadt Complex, Undercliffe Falls, Blacksmiths Creek Monzogranites; Thomkins Gully Monzogranite Phase; and Tenterfield Creek Leucosyenogranite. Is overlain locally by Marburg Supergroup.|250-247 Ma (Chisholm et al., 2014).|Stanthorpe Supersuite.|Benalla, Ruby Creek, Amiens, Severn River, Jenners, Surface Hill, Carrols Creek Suites; Mount Lindesay Monzogranites.|Intrudes Texas beds; Silverwood Group; Wallangarra, Drake Volcanics; Gilgurry Mudstone; Bungulla, Ballandean and Rocky River Monzogranites. See COMMENTS for more.|Composite unit of pale pink/grey/off-white, fine- to coarse-grained, equigranular to porphyritic, K-feldspar-rich, biotite(-hornblende) monzogranite-leucomonzogranite borderline to syenogranite-leucosyenogranite; locally aplitic leucogranite.|
82791|Stanthorpe Granite Group|71628|6|Mentioned|p1:8; p11: 1, 5, 11, 40; p15:1, 6, 9, 16|||See also p15: 20, 23, 26, 46-47, 53, 73, 77, 98, 107. Blevin and Chappell (1996), who differentiated this grouping from the Moonbi Granite Group, both within the Moonbi Supersuite. Stanthorpe area.||||||
38335|Stanthorpe Granite group|23763|6|Mentioned|p543|||Informal. Geological Province: New England Fold Belt.||||||22-NOV-07
38335|Stanthorpe Granite group|60422|6|Mentioned|p386|||Of the Moonbi Supersuite (New England Batholith). ||||||
68803|Stanthorpe Group|24512|6|Mentioned|p7|||Mentioned in context of the 'Stanthorpe Group of granites'. Of the Moonbi Supersuite.||||||
38272|Stanthorpe Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse-grained, equigranular phase of this monzogranite; undifferentiated phase also.  An I-type granitoid.||||||20-DEC-04
38272|Stanthorpe Monzogranite|23812|5|Briefly described|p24, p102, p103|Early Triassic|Early Triassic|Of the Moonbi Supersuite (of Chappell and Bryant (1994) and Chapell et al (1999)). Intrudes the Dundee Rhyodacite and the Bungulla Monzogranite.  Age: 242-237MA (Rb-Sr).||||||
38272|Stanthorpe Monzogranite|61789|6|Mentioned|p304|||May be a informal version of Stanthorpe Adamellite.||||||
38272|Stanthorpe Monzogranite|61790|6|Mentioned|p315, p318|||Refers to a part within the Stanthorpe Adamellite. Mafic, porphyritic phase.||||||18-SEP-09
38272|Stanthorpe Monzogranite|68005|5|Briefly described|p133.|Triassic|Triassic|Eight varieties have been mapped in places, mainly based on textural differences.||Unit in Moonbi Supersuite.|||Coarse-grained, even-textured to weakly porphyritic, pale pink to buff, biotite-poor leucogranite with scattered fine-grained saccharoidal leucogranite.|
38272|Stanthorpe Monzogranite|71628|5|Briefly described|p1-12; p5: 6, 8; p11: 2, 10-11, 24, 26|||See also p11: 37, 39; p12: 3, 12; p15: 32, 34-37, 39, 41, 43, 46-47, 49, 52-53, 58, 61-65, 67-69, 73, 75, 77, 81-82, 92, 98, 101, 105, 107; p16: 1, 3, 5, 8, 10-12, 16, 19-20, 26; p19: 6, 19-20, 23, 59, 62, 70, 131, 133, 159-160, 162-163, 173-175. Henley et al. (2001), after unpublished work by Barnes (1987). Comprises multiple pulses of geochemically distinct magmas, hence is now Stanthorpe Complex and Cullendore Supersuite. Previously included rocks now named Accommodation Creek Monzogranite.||||Intrudes Palgrave Monzogranite. Is faulted against Bungulla and Rocky River Monzogranites. Abuts Cullendore Syenogranite.||
37005|Stanthorpe Plutonic Suite|38837|6|Mentioned|p235|||Geological Province: New England Fold Belt||||||
37005|Stanthorpe Plutonic Suite|44244|6|Mentioned|p291|||Of Korsch (1977).||||||
37005|Stanthorpe Plutonic Suite|44450|6|Mentioned|p35|||||||||
37005|Stanthorpe Plutonic Suite|50014|6|Mentioned|p253|||Geological Province: New England Fold Belt||||||
37005|Stanthorpe Plutonic Suite|71628|6|Mentioned|p15: 34, 83, 107|||Korsch (1977). A series of broadly N-trending granites. Now the Stanthorpe Complex.||||||
74786|Stanthorpe Syenogranite|61790|6|Mentioned|p315|||Not intended as a formal name, refers to phase of Stanthorpe Adamellite.||||||
74786|Stanthorpe Syenogranite|71628|6|Mentioned|p15-32|||Sivell and Passmore (1999) for part of what is now the Stanthorpe Complex.||||||
82789|Stanthorpe adamellite|71628|6|Mentioned|p15: 32|||Phillips (1968). Subsequently Stanthorpe Adamellite, Stanthorpe Monzogranite and now Stanthorpe Complex.||||||
69971|Stanthorpe granite|61783|6|Mentioned|p296|||Informal name. Contains stocks of Ruby Creek granites.||||||27-JAN-06
29019|Stanthorpe leucogranites|37148|6|Mentioned|p132|||||||||
38338|Stanthorpe leucomonzogranite|23763|5|Briefly described|p543 Fig. 1|Early Triassic|Late Permian|Parent: Moonbi Supersuite.   Geological Province: New England Fold Belt.||||||
38338|Stanthorpe leucomonzogranite|71628|6|Mentioned|p15: 32, 105|||Mustard (2001). Now included in Surface Hill Leucomonzogranite of the Stanthorpe Complex.||||||
82792|Stanthorpe"" granite|71628|6|Mentioned|p15: 32, 37, 81; p16: 18|||Saint-Smith (1913, 1914). Also appears as 'Stanthorpe' Granite (Saint-Smith, 1914). Now part of Stanthorpe Complex.||||||
32185|Stanton Rock Adamellite|22815|4|Described|p81|||||||||
32185|Stanton Rock Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Stanton Rock Suite.||||||
24503|Starvation Point Adamellite|36443|5|Briefly described|map legend|Pridolian|Pridolian|Of Coodravale I-type Suite. Of Young Batholith. Intrusive. Adamellite. I-type. BMR map code: Syp.||||||
24503|Starvation Point Adamellite|39660|6|Mentioned|p450|||||||||
24503|Starvation Point Adamellite|40328|4|Described|p210|||||||||
24503|Starvation Point Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah2||||||
24503|Starvation Point Adamellite|45147|2|Defined|M242|Late Silurian|Late Silurian|Prob.Late Silurian||||||
24503|Starvation Point Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
26908|Starvation Point Granite|42726|5|Briefly described|map legend|Silurian||435. Variation on Starvation Point Adamellite.||||||
30416|State Mine Formation|43146|6|Mentioned|Fig.2 p41|||Misspelling of State Mine Creek Group.||||||
27573|Station "D" Adamellite|30938|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
34500|Stephen Beds|22771|6|Mentioned|Table12.2p45|||||||||
34500|Stephen Beds|22857|5|Briefly described|p45 Tb. 12.2|||Of Cordwell and Williams (1962). Now part of the Paragon and Sundown Groups.||||||
28151|Stewartfield Granodiorite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Granodiorite, adamellite. S-type. BMR map code: Sms.||||||
28151|Stewartfield Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb5. Misspelling of Stewartsfield Granodiorite.||||||
28151|Stewartfield Granodiorite|45147|6|Mentioned|M196|||This is a misspelling on Tantangarra map, of Stewartsfield Granodiorite.||||||
28151|Stewartfield Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
31852|Stewartfields Adamellite|45003|6|Mentioned|p54|||Misspelling of Stewarts Field Adamellite [or Stewartsfield Adamellite?]||||||
31253|Stitts Member|43511|14|Not recorded|p131-2,134,141-4,147||Late Devonian|Member of Womboyne Formation||||||
74765|Stitts Member""|61964|6|Mentioned|p114, p125|Late Devonian|Late Devonian|Of Conolly (1966). Of the former "Mountain Creek Formation " (Cocoparra Group); then renamed the "Jimberoo Member" of "Womboyne Formation" (Cocoparra Group).||||||28-JAN-09
40729|Stockingbingal Formation|23309|6|Mentioned|p390|||||||||
72983|Stockrington tuff|62033|5|Briefly described|p25 (Table)|||Of Adamstown Formation (Newcastle Coal Measures). Overlain by Australasian seam; overlies Montrose seam. Geological Province: Sydney Basin. Informal name.||||||14-MAR-07
24506|Stokefield Diorite|23214|6|Mentioned|p85|||Superseded by Stokefield Metagabbro. Originally included as part of Carcoar Granite (now Carcoar Granodioirite).||||||
24506|Stokefield Diorite|39663|6|Mentioned|Table 2|||Reserved 1978. Richardson.||||||
34299|Stokefield Diorite""|22679|6|Mentioned|p 46|||||||||
34248|Stokefield Metagabbro""|22679|6|Mentioned|p 11|||||||||
34642|Stoney Creek Adamellite""|22815|6|Mentioned|p82|||Obsolete. Now called Egan Peaks Adamellite.||||||
80303|Stoney Tank Formation""|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|Geophysical signature: low magnetic intensity and shows only very slight contrast with adjacent sedimentary rocks in aeromagnetic data. Boundaries are based on existing geological mapping.||Kopyje Group.|||Argillaceous, quartzose and calcareous sandstone and siltstone with limestone interbeds.|
41661|Stratford Coal Measures""|44244|5|Briefly described|p167|Late Permian|Late Permian|Supersedes the "Broad Gully Formation", "Spring Creek Conglomerate" and the "Craven Coal Measures".  Now part of the Gloucester Coal Measures.  See also Stratford Coal Measures.||||||
77608|Strathaven Complex|71628|6|Mentioned|p12-17|||An informal assignation by Blevin (pers. comm., 2014) to the unit identified as Po, located near the northern boundary of Grafton-Maclean 1:250 000 Metallogenic Sheet (Henley et al., 2001). The name is reserved in ASUD.||||||
82635|Strathaven Suite|71628|5|Briefly described|p12-18|||New name.||Sailor Jack Supersuite.|Strathaven Monzogranite.|||
83657|Streamers Trachyte|73581|6|Mentioned|p7|||Marker unit separating the Governors Chair Volcanics and Superbus Basalt, absent in places.||||||
31640|Streamville Suite|42726|5|Briefly described|map legend||Silurian|||||||
26915|Stringy Road Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Stringy Road Granodiorite.||||||
38289|Strockrington Tuff|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Of the Adamstown Formation.   Geological Province: Sydney Basin||||||
82662|Stroud Mountain Suite|71628|6|Mentioned|p19-156||||||Stroud Mountain Microgranite.|||
69374|Stroud Mountain porphyry|50099|6|Mentioned|p18|||Informal name. See also Stroud Mountain quartz-feldspar porphyry.||||||
69374|Stroud Mountain porphyry|71628|6|Mentioned|p19-156|||Sutherland and Graham (2003).||||||
69375|Stroud Mountain quartz-feldapar porphyry|50099|6|Mentioned|p18|||Informal name. See also Stroud Mountain porphyry.||||||
83964|Stroud Mountain quartz-feldspar porphyry|71628|6|Mentioned|p19-156|||Of Sutherland and Graham (2003).||||||
29026|Stroud Volcanics|32379|6|Mentioned|Fig.3|||||||||
29026|Stroud Volcanics|32671|6|Mentioned|Map legend|Permian|Permian|||||||
29026|Stroud Volcanics|32868|6|Mentioned|p210|||||||||
29026|Stroud Volcanics|34169|6|Mentioned|p252|||Correlation||||||
29026|Stroud Volcanics|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
29026|Stroud Volcanics|39302|6|Mentioned|Fig. 17.2|||||||||
29026|Stroud Volcanics|39308|6|Mentioned|p482|||||||||
29026|Stroud Volcanics|40872|6|Mentioned|Fig.2|||||||||
29026|Stroud Volcanics|41347|4|Described|Table 3|||||||||
29026|Stroud Volcanics|41348|5|Briefly described|Map legend|Permian|Permian|felsic, intermediate and minor mafic volcanics.||||||16-DEC-04
29026|Stroud Volcanics|42182|6|Mentioned|p301|||||||||
29026|Stroud Volcanics|47056|6|Mentioned|Fig.2 P523|||||||||
41662|Stroud Volcanics""|44244|6|Mentioned|p164|||Superseded by the Alum Mountain Volcanics.  In the Stroud-Gloucester Syncline.||||||
29257|Sturts Meadow Siltstone|34814|6|Mentioned|Table 1|||Misspelling of Sturts Meadows?||||||
77581|Sugarloaf Complex|71628|6|Mentioned|p13: 2, 21|||Name reserved in ASUD by Blevin (6/11/2012); previously in unpublshed work by Lewis (1973).||||||
29028|Sugarloaf Creek Tuff""|32585|6|Mentioned|Fig.3|||||||||
29028|Sugarloaf Creek Tuff""|45147|6|Mentioned|M303|||||||||
82794|Sugarloaf Leucogranite|71628|6|Mentioned|p14: 3|||Mikulski (1973). Now part of Glen Garry Microleucosyenogranite.||||||
31163|Sulcor Formation|43491|4|Described|pV/13||Middle Devonian|||||||
22916|Summer Hill Formation|23214|5|Briefly described|p70|||Now included in the Oakdale Formation.||||||
22916|Summer Hill Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
35252|Summerland Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
26153|Sunlight Creek Mudstone Member|22815|3|Fully described|p26, fig10|Early Ordovician|Early Ordovician|Age: Darriwilian||||||
26153|Sunlight Creek Mudstone Member|22857|4|Described|p422 App. 1, Tb. A1.5|Late Ordovician|Early Ordovician|Of the Warbisco Shale. Homogeneous grey shale and siltstone, or interlayered black siliceous siltstone and pale-brown to white siltstone and fine arenite. Rich graptolite fauna, conodonts. Geological Province: Monaro Forearc Basin. ||||||
26153|Sunlight Creek Mudstone Member|42647|2|Defined|p20|Gisbornian||Supersedes Sunlight Creek Formation (used on the Bendoc map). Age: Late Ordovician (early Gisbornian||||||
26153|Sunlight Creek Mudstone Member|60541|6|Mentioned|p49|||Basal member of Warbisco Shale (Bendoc Group) - upgraded to formation status as Sunlight Creek Formation (Orth et al 1995).  Type section included.||||||
26919|Sunnyside Granite|42726|5|Briefly described|map legend|Silurian||Blayney area.||||||08-MAR-16
37220|Sunnyside Granodiorite|23214|6|Mentioned|p167|||Replaced by Mandurama Ponds Granodiorite.||||||
34296|Sunnyside Granodiorite""|22679|6|Mentioned|p 46|||Of Close (1978).||||||08-MAR-16
32506|Sunnyside mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
76053|Surat Sandstone|65119|5|Briefly described|Fig 2 p503|Early Cretaceous|Early Cretaceous|Surat Basin. Includes siltstone, mudstone and sandstone. See Surat Siltstone p512.||||||07-MAR-12
68869|Surface Hill Syenogranite|60422|5|Briefly described|p387-391,  Fig. 2, p388 Tb. 1|||Of the Stanthorpe-type granite (Moonbi Supersuite). Fine- to coarse-grained syenogranite, very fine-grained microgranite, strongly porphyritic microgranite. I-type.||||||23-MAR-15
68870|Surface Hill syenogranite|60422|5|Briefly described|p386, p387, p390 Fig. 4|||Informal - see Surface Hill Syenogranite. Of the Stanthorpe-type granite (Moonbi Supersuite).||||||
68870|Surface Hill syenogranite|71628|6|Mentioned|p11-24; p15-109|||Mustard (2004). Broadly equivalent to the current Stanthorpe Monzogranite. Appears as Surface Hill syenogranite on p15-105. See Surface Hill Leucomonzogranite.||||||
77332|Sutcliff Conglomerate|68005|5|Briefly described|p147.|Carboniferous|Carboniferous|||Unit in Tangaratta Formation.|||Polymictic orthoconglomerate, siltstone and lithic sandstone.|
70380|Sutton Forest basanite|60997|5|Briefly described|p139 Fig. 1|Middle Jurassic|Early Jurassic|Informal name. Geological Province: Sydney Basin.||||||
42323|Sutton granite|24270|6|Mentioned|p1610|||Geological Province: Lachlan Fold Belt.||||||07-DEC-04
31320|Swain's Gully Limestone|43538|14|Not recorded|p2,3,21,25||Visean|Lower Carboniferous fauna (L.Visean)||||||
29687|Swamp Oak beds""|43017|5|Briefly described|Fig.2,p374|||||||||
41331|Swampy Plain Metamorphics|60085|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
42039|Swampy Plains Metamorphics|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Pre-Cratonic Province. Slate, phyllite, sandstone.||||||09-NOV-04
82664|Swan Brook Suite|71628|6|Mentioned|p19-157||||||Swan Brook Granite.|||
30973|Swansea Conglomerate|43440|14|Not recorded|p49|||Unit of Newcstle Coal Measures||||||
30973|Swansea Conglomerate|43477|14|Not recorded|p21,23,56|||||||||
68852|Swatchfield intrusive|24518|6|Mentioned|p68|||Informal name.||||||
34268|Sydney Basin succession|22678|6|Mentioned|Fig1p712,Fig3p714||Permian|Informal term.||||||
29034|Sydney Coal Measures""|30006|6|Mentioned|p7|||||||||
25505|Sydney Sub-Group|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
25505|Sydney Sub-Group|24157|5|Briefly described|p209 Fig.19|||Informal name referring to the Illawarra Coal Measures. Geological Province: Sydney Basin||||||
25505|Sydney Sub-Group|29900|6|Mentioned|p165|||||||||
25505|Sydney Sub-Group|29901|4|Described|p169|||||||||
25505|Sydney Sub-Group|30006|4|Described|p9|||Stratigraphic column on P5.||||||
25505|Sydney Sub-Group|31062|6|Mentioned|p478|||Triassic. On Table||||||
25505|Sydney Sub-Group|31128|6|Mentioned|Table 1|||||||||
25505|Sydney Sub-Group|31879|5|Briefly described|p294|||Permian||||||
25505|Sydney Sub-Group|31887|6|Mentioned|p5|||||||||
25505|Sydney Sub-Group|32945|6|Mentioned|p84|||See also P85. Permian||||||
25505|Sydney Sub-Group|33869|6|Mentioned|Fig.2|||||||||
25505|Sydney Sub-Group|34060|6|Mentioned|p24|||Perm.||||||
25505|Sydney Sub-Group|34205|6|Mentioned|p15|||||||||
25505|Sydney Sub-Group|34335|6|Mentioned|p369|||Permian. Previously "Illawarra C.M."||||||
25505|Sydney Sub-Group|34399|6|Mentioned|p312|||||||||
25505|Sydney Sub-Group|34569|6|Mentioned|p8|||Permian. See also Fig.2||||||
25505|Sydney Sub-Group|34605|4|Described|p372|||Stratigraphic units||||||
25505|Sydney Sub-Group|34607|6|Mentioned|p23|||||||||
25505|Sydney Sub-Group|36042|6|Mentioned|Fig.18|||||||||
25505|Sydney Sub-Group|36220|4|Described|p38|||See also P49 & Table 1.||||||
25505|Sydney Sub-Group|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
25505|Sydney Sub-Group|36593|6|Mentioned|Fig.2|||||||||
25505|Sydney Sub-Group|37089|5|Briefly described|p208|||||||||
25505|Sydney Sub-Group|37090|6|Mentioned|p219|||||||||
25505|Sydney Sub-Group|39307|6|Mentioned|Table 22.1|||||||||
25505|Sydney Sub-Group|39308|5|Briefly described|p514|||||||||
25505|Sydney Sub-Group|39309|5|Briefly described|p124|||||||||
25505|Sydney Sub-Group|42182|5|Briefly described|p300|||||||||
25505|Sydney Sub-Group|43320|14|Not recorded|p9,28,29,31|||Upper part of Illawarra Coal Measures||||||
25505|Sydney Sub-Group|43383|14|Not recorded|p20,Fig.5||Permian|||||||
25505|Sydney Sub-Group|45090|6|Mentioned|p28|||Relationship of rock units||||||
33564|Sydney basalts|44716|14|Not recorded|p160|||||||||
34688|Tableland Complex|22859|6|Mentioned|p220|||(Runnegar 1974). Probable misspelling of Tablelands Complex.||||||
34688|Tableland Complex|71628|6|Mentioned|p14-1|||See also Tablelands Complex (p1: 1-2; p4-5; p7: 2, 31; p8-1; p9-3; p14-1; p18: 1-2).||||||
70052|Tableland Complex""|22857|6|Mentioned|p220|Carboniferous||Informal name (Runnegar, 1974) for rocks east of the Peel Fault in the New England Fold Belt which include Texas beds, "Coffs Harbour Association", Gundahl Complex, Cara Formation, "Sandon Association". The rocks from several tectonostratigraphic terranes||||||
68419|Tablelands Complex""|44093|6|Mentioned|p58|||Structural term of Kosch (1977) for the "New England Tablelands" of Harrington's classification (1974). Not a formal stratigraphic unit.||||||
31948|Tabulam Beds|43881|14|Not recorded|p38|Jurassic|Triassic|Now called Tabulam Group. See also Lexicon.||||||
33220|Tabulam group|44546|14|Not recorded|p26|||||||||
31164|Taemas Group|43491|14|Not recorded|pV/12|||Included with Black Range Group in "Murrumbidgee Group" (Sussmilch 1914)||||||
39821|Taemas Limestone, middle - upper|24250|6|Mentioned|p103|||Informal - see Taemas Limestone. Term used in title of study||||||
25507|Taemas Series""|35386|6|Mentioned|p48|||Refers David(1950)||||||
25507|Taemas Series""|45147|6|Mentioned|M311|||||||||
29037|Taemas Stage|32483|6|Mentioned|p31|||Refers Browne (1959)||||||
29037|Taemas Stage|68592|6|Mentioned|p980|||Of Browne (1959). Raised to Formation status by Pedder et al. (1970).||Unit in Murrumbidgee Series.||||
75942|Taggarts Ignimbrite Member|65902|5|Briefly described|p195 Fig.2|Carboniferous|Carboniferous|Of Currabubula Formation. See also Taggarts Mountain Member and Taggarts Mountain Ignimbrite, both mentioned in this article; both are shortened forms of the formal name Taggarts Mountain Ignimbrite Member.||||||09-MAR-12
24006|Taggarts Mountain Ignimbrite|42547|5|Briefly described|p23|||Variation on Taggarts Mountain Ignimbrite Member. Equivalent of Plagyan Rhyolite?||||||
24006|Taggarts Mountain Ignimbrite|64631|5|Briefly described|p51.|Bashkirian|Bashkirian|See also discussion of Currabubula Fm p54.|316.1 Ma.|Unit in Currabubula Formation.||||
24006|Taggarts Mountain Ignimbrite|65902|5|Briefly described|p195 Fig.2|Carboniferous|Carboniferous|Shortened form of Taggarts Mountain Ignimbrite Member. See also Taggarts Ignimbrite Member, another shortened form in this article.||||||09-MAR-12
70508|Taggarts Mountain Member|62095|5|Briefly described|p251|Late Carboniferous|Late Carboniferous|Of the Currabubula Formation. Age: 319Ma. Geological Province: Werrie Block/Tamworth Belt. See also Plate 1.||||||
70508|Taggarts Mountain Member|65902|5|Briefly described|p197,199, 202, Fig. 6|Carboniferous|Carboniferous|Of Currabubula Formation. See also Taggarts Mountain Ignimbrite and Taggarts Ignimbrite Member. All three are variations of the formal name, Taggarts Mountain Ignimbrite Member.||||||09-MAR-12
30845|Tait's Creek Formation|43385|14|Not recorded|p179,180||Early Permian|||||||
31165|Taits Creek "glacial beds"|43491|14|Not recorded|pVII/45||Permian|||||||
29038|Talbragar Formation""|29870|6|Mentioned|p13|||Refs. Dulhunty 1973, Ward 1975.||||||
35408|Talbragar Fossil Fish bed|23170|4|Described|p331|Late Jurassic|Late Jurassic|of Purlawaugh Formation, Surat Basin.||||||
35408|Talbragar Fossil Fish bed|68003|5|Briefly described|p61, p127.|Late Jurassic|Late Jurassic|Very limited, discontinuous outcrop (800 m strike length). Abundant, perfectly preserved freshwater fish and flora fossils. NB: protected site.||Unit in Purlawaugh Formation.|||A hard limonitic, laminated, light to mid-brown  cherty-shale containing Jurassic plant and fish fossils.|
35408|Talbragar Fossil Fish bed|68135|5|Briefly described|p52 Fig.2b, p55 Fig.3, p62-63|Tithonian|Oxfordian|Southern Surat Basin. Age supported by fossil fish assemblage. Also contains diverse insect fauna. 60-100cm thick. Species discussed in some detail. Appears squeezed into Fig.2b as TFB with Talbragar fish beds as the elaboration in the Legend.|151.55 +/- 4.27 Ma (SHRIMP)|Purlawaugh Formation.|||Hard, fine limonitic cherty shale, fossiliferous mudstone: largely reworked from underlying sandstones, and interbedded with thin tuffs (very fine-grained ash falls).|15-SEP-17
32383|Talbragar fish-beds|43905|14|Not recorded|p87||Jurassic|Flora||||||
35073|Talbragar fossil fish bed|23043|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|of Purlawaugh Formation.||||||
74766|Taleeban Granite""|61964|6|Mentioned|p53|||Informal name used by Chappell et al (1991) for the southern end of the Erigolia Granite batholith (their granite No. 502). Included in Kikoira Granite by Pogson et al. (1967).||||||
76970|Tallawudjah Leucomonzogranite|69639|4|Described|p3, p6, p8, p106-p111|Late Triassic|Late Triassic|New England Orogen. SHRIMP age is interpreted as a magmatic crystallisation date. Sample locality, petrography, and geochronology is described. I-type geochemistry. Thought to be Permian by GSNSW prior to derivation of the provided SHRIMP date. See also p118, p128, p223-p224, p237.|229.9 +/- 1.4 Ma (SHRIMP, U-Pb)|||Intrudes the Coramba Formation. Overlain by the Bundamba Group.|Medium- to fine-grained granite with minor hydrothermal quartz veins and minor coarser variants.|06-MAR-19
76970|Tallawudjah Leucomonzogranite|71628|6|Mentioned|p17-68|||Chisholm et al. (2014) after unpublished work by Chappell and Bryant (1994). Initially Tallawudjah Leucoadamellite (Korsch, 1978). Now Tallawudjah Leucosyenogranite.||||||
80789|Tallawudjah Monzogranite|69639|6|Mentioned|p3|Triassic|Triassic|New England Orogen.|229.9 +/- 1.4 Ma (SHRIMP, U-Pb)|||||06-MAR-19
27238|Tallebung Group|730|6|Mentioned|p22 Fig.5.|Ordovician|Ordovician|||||||11-NOV-14
27238|Tallebung Group|9548|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Palisthan Formation.||||||
27238|Tallebung Group|22508|6|Mentioned|p2||Late Ordovician|Lachlan Fold Belt||||||
27238|Tallebung Group|22704|5|Briefly described|p52|Caradocian|Arenigian|||||||
27238|Tallebung Group|22768|6|Mentioned|Fig16.8p168||Ordovician|||||||
27238|Tallebung Group|22857|5|Briefly described|p132, p412 App. 1 Tb. A1.4.|Late Ordovician|Early Ordovician|Includes the Currawalla and Eulendool Formations, and Marobee Conglomerate. Max. thickness: 8km. Geological Province: Wagga Marginal Basin. See also p168 Fig. 16.8.||||||
27238|Tallebung Group|23088|6|Mentioned|p651 Fig 1|||||||||
27238|Tallebung Group|23171|5|Briefly described|Fig8p29|Late Ordovician|Early Ordovician|||||||
27238|Tallebung Group|23245|6|Mentioned|p132|||||||||
27238|Tallebung Group|29987|6|Mentioned|p10|||||||||
27238|Tallebung Group|32087|6|Mentioned|p9|||||||||
27238|Tallebung Group|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
27238|Tallebung Group|32672|6|Mentioned|p671|||||||||
27238|Tallebung Group|34404|6|Mentioned|Fig.3.8|||Upper Ordovician||||||
27238|Tallebung Group|34449|4|Described|Table 2-1|||U.Ordovician||||||
27238|Tallebung Group|35163|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
27238|Tallebung Group|39064|6|Mentioned|p2|||||||||
27238|Tallebung Group|39772|6|Mentioned|p20|||||||||
27238|Tallebung Group|40136|5|Briefly described|p41|||||||||
27238|Tallebung Group|40677|5|Briefly described|p25|||||||||
27238|Tallebung Group|40682|5|Briefly described|Fig.1|||||||||
27238|Tallebung Group|41394|2|Defined|p19|Ordovician||||||||
27238|Tallebung Group|41395|6|Mentioned|Map legend|Ordovician||||||||
27238|Tallebung Group|41528|2|Defined|p23|Late Ordovician|Early Ordovician|||||||
27238|Tallebung Group|41529|6|Mentioned|Map legend|Ordovician||||||||
27238|Tallebung Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27238|Tallebung Group|41821|2|Defined|p19|Late Ordovician|Early Ordovician|||||||
27238|Tallebung Group|42144|6|Mentioned|p603|||||||||
27238|Tallebung Group|42566|5|Briefly described|p44|||||||||
27238|Tallebung Group|42954|6|Mentioned|p68|||||||||
27238|Tallebung Group|43032|6|Mentioned|p23|||||||||
27238|Tallebung Group|43089|5|Briefly described|Map Legend|||||||||
27238|Tallebung Group|43263|6|Mentioned|Map Legend||Ordovician|of Wagga Metamorphics.||||||
27238|Tallebung Group|43384|14|Not recorded|Map Legend||Ordovician|||||||
27238|Tallebung Group|43389|14|Not recorded|Map Legend||Late Ordovician|||||||
27238|Tallebung Group|43479|14|Not recorded|p77,78,94||Late Ordovician|||||||
27238|Tallebung Group|43774|6|Mentioned|Fig.1,p2|||||||||
27238|Tallebung Group|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
27238|Tallebung Group|61964|5|Briefly described|p20, p30, p31|Late Ordovician|Early Ordovician|Obsolete. Rocks included in Bendoc + Wagga Gps. Originally for slates, with subord.sandstones + qtzites near Tallebung. Formalised by Trigg (1987).||||||
27238|Tallebung Group|63019|5|Briefly described|p920|Ordovician|Ordovician|Formerly contained, in part, rocks of the Wagga Group. Sequence of submarine sedimentary rocks. Geological Province: Lachlan Orogen.||||||23-JAN-07
27238|Tallebung Group|65469|6|Mentioned|p20, App A-VI 5|||Lachlan Orogen. Previously mapped east of Nymagee, superseded by the Bendoc Group (Colquhoun et al., 2004). ||||||
27238|Tallebung Group|67322|5|Briefly described|p18, p39|Katian|Early Ordovician|Colquhoun, Hendrickx and Meakin (in Colquhoun et al. 2005) recommended suppression of the name Tallebung Group as  the concept of the unit (Trigg 1987) appeared to include strata of both Early to Middle Ordovician age (Wagga Group equivalents) and Late Ordovician age, indicated by the presence of probable Eastonian graptolites. Outcrops at The Meadows Tank and at Illewong are reassigned to the Clements Formation.||||||
27238|Tallebung Group|69801|6|Mentioned|p18|||Central Lachlan Orogen. Obsolete terminology of Trigg, 1987; replaced by the Wagga Group.||||||
27238|Tallebung Group|70950|6|Mentioned|p1029|||Geological province: Central Lachlan Orogen. No longer current.||||||
27238|Tallebung Group|71069|5|Briefly described|p71|Late Ordovician|Early Ordovician|Obsolete name, replaced by the Bendoc Group.|||Includes the Eulendool Formation and Palisthan Formation.||Shale and quartzose sandstone sequences.|
81360|Tallong Tillite|70096|6|Mentioned|p221|||Of southern Sydney Basin.||||||
22943|Tallwood Monzonite|22679|3|Fully described|p 38|Ordovician|Ordovician|||||||
22943|Tallwood Monzonite|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
22943|Tallwood Monzonite|23202|6|Mentioned|Fig.1||Ordovician|||||||
22943|Tallwood Monzonite|23214|2|Defined|p96|Late Ordovician|Late Ordovician|Intrudes both the Weemalla Formation and Forest Reefs volcanics. Exposed as boulders <0.5m across which consist of medium grained biotite-clinopyroxene monzonite at the type section.||||||
22943|Tallwood Monzonite|43653|5|Briefly described|Map Legend||Ordovician|||||||
22943|Tallwood Monzonite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Porphyritic clinopyroxene monzonite and monzodiorite.||||||17-JUL-08
22943|Tallwood Monzonite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
22943|Tallwood Monzonite|63286|6|Mentioned|p304|Ordovician|Ordovician|Renamed as the Tallwood Intrusive Complex.||||||07-FEB-11
22943|Tallwood Monzonite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
22943|Tallwood Monzonite|73154|4|Described|p78 Tb.1, p79-80, p82, p84, p89 Tb.2|Llandovery|Late Ordovician|Molong structural belt. Shoshonitic affinity.|444+/-4 Ma, 443.6+/-3.7 Ma Pb/U zircon SHRIMP|||Intrudes Forest Reefs Volcanics|Small dioritic to monzonitic and syenitic intrusives. Includes pink, medium grained rock with plagioclase, biotite and altered clinopyroxene in an interstitial groundmass of K-feldspar and very rare late quartz.|
22943|Tallwood Monzonite|73431|6|Mentioned|p364-365, p366 Fig.3|Late Ordovician|Late Ordovician|Lachlan Orogen.||||Faulted against Browns Creek Intrusive Complex||
31835|Talmo Quartz Porphyrite|45003|14|Not recorded|p124|||||||||
83694|Taltawongee Group|73430|6|Mentioned|p494|Middle Cambrian|Early Cambrian|Koonenberry Belt. Deformed in Delamerian Orogeny.|||||Sedimentary unit.|
77146|Tambar Intrusives|68003|5|Briefly described|p48. |||Identified by Bean (1974) but not mapped because of its local extent.||Unit in Garrawilla Volcanics.||||
37429|Tamberamboro Granodiorite|23214|6|Mentioned|p174|||Now included in Wologorong Granite.  Possibly misspelt - see also Tamboramboro Granite and Tumboramboro Granite complex.||||||
79211|Tamboramboro Granodiorite|68592|6|Mentioned|p1593|||Packham (1968). Now Tumboramboro Granite.||||||
68973|Tamby Formation|60293|5|Briefly described|p107, p108 Fig.1|||Misspelt - see Tamby Creek Formation.||||||
68973|Tamby Formation|65107|5|Briefly described|p289|Upper Pennsylvanian|Upper Pennsylvanian|Overlies the Seaham Formation, age: 303.7+/-2.4 to 300.3+/-2.4Ma, from SHRIMP U-Pb zircons. Constrains a counter clockwise rotation, postdates Carboniferous-Permian Boundary.||||||16-JAN-12
70416|Tamworth Association|61003|5|Briefly described|p225|||Informal name. Older than the Sandon, Woolomin and Coffs Harbour Associations. ||||||
34072|Tamworth Belt|22612|6|Mentioned|423, 432, 433|Carboniferous|Devonian|Geol province New England Orogen||||||
34072|Tamworth Belt|67669|6|Mentioned|p14|||Geological province: New England Fold Belt.||||||
30881|Tamworth Cherts|43397|14|Not recorded|p209, map||Devonian|||||||
30880|Tamworth Common Cherts|43397|14|Not recorded|p209|Middle Devonian|Early Devonian|Ref.to Benson 1915||||||
40227|Tamworth Group, lower|38686|6|Mentioned|p55|||Geological Province: New England Fold Belt||||||
30846|Tamworth Series|43385|14|Not recorded|p174,175|Early Devonian|Early Devonian|||||||
30846|Tamworth Series|43396|14|Not recorded|p165-176|||||||||
30846|Tamworth Series|43397|14|Not recorded|p209|Middle Devonian|Early Devonian|||||||
30846|Tamworth Series|43399|14|Not recorded|p189,190,195,196|||||||||
30846|Tamworth Series|43400|14|Not recorded|p175,176,177|Middle Devonian|Early Devonian|Now called Tamworth Group||||||
30846|Tamworth Series|43417|14|Not recorded|Map Legend|||||||||
30846|Tamworth Series|44565|14|Not recorded|p234|||||||||
30846|Tamworth Series|44861|14|Not recorded|p244||Devonian|||||||
30882|Tamworth beds|43397|14|Not recorded|p213|||||||||
30882|Tamworth beds|43491|14|Not recorded|pIII/14|Middle Devonian|Early Devonian|||||||
30935|Tamworth formation|43418|14|Not recorded|Map Legend|||||||||
33949|Tanabutta Group|22529|6|Mentioned|p1|Silurian|Silurian|Misspelt when indexed. Use Tannabutta Group, p6.||||||
33949|Tanabutta Group|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Silurian|Silurian|Capertree High. Location in text includes p1100 Fig.5. Interpreted in cross section as overlying the Sofala Volcanics in an anticline, northern Capertree high.||||Underlies the Roxburgh Formation, Carwell Creek Formation, Riversdale Volcanics, Buckaroo Conglomerate.||
33951|Tanawarra Shale|22529|5|Briefly described|1|||Misspelt when indexed. Use Tanwarra Shale p6. Parent Mumbil Group||||||
70040|Tangerang Volcanics""|22857|6|Mentioned|ERRATA sheet for p482|||Informal - see Tangerang Volcanics, superseded by Tangerang Formation.||||||
29044|Tangorin Coal|41226|6|Mentioned|Fig.8|||||||||
68974|Tangorin seam|60290|5|Briefly described|p16, 46 Fig.20|Early Permian|Early Permian|Informal name for member of Greta Coal Measures. Coal. Marine influenced peat swamp. Geological Province: Cranky Corner Basin.||||||07-FEB-11
68974|Tangorin seam|60293|5|Briefly described|p110|||Of Greta Coal Measures. Vitrinite reflectance of organic matter described.||||||
30989|Tantitha Intrusive Complex|43441|4|Described|14|||Age: pre Middle Devonian||||||08-JAN-10
30989|Tantitha Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||
30989|Tantitha Intrusive Complex|68003|5|Briefly described|p23, p24 Fig.3-e. |Late Ordovician|Early Ordovician|Lachlan Fold Belt, Brigalow Belt South Bioregion. See also reference to Tantitha Ultrabasic Complex (p148). [Both names are erroneous; the formal name is Tantitha Ultramafic Complex].||||Possibly intrudes Girilambone Group; has been intruded by Yeoval Complex.|Ultramafics.|
30989|Tantitha Intrusive Complex|70036|5|Briefly described|Map legend|Ordovician|Ordovician|Lachlan Fold Belt. Included in a mapped unit of strongly deformed gabbro, pyroxenite and granite. Mis-spelt as Tantithia.||||||
77147|Tantitha Ultrabasic Complex|68003|5|Briefly described|p148.|Ordovician|Ordovician|Lachlan Fold Belt. See also references to Tantitha Intrusive Complex (p23, p24 Fig.3-e). [Both names are erroneous; the formal name is Tantitha Ultramafic Complex].|||||Gabbro and pyroxenite with minor granitic intrusions.|
34621|Tantitha Ultramafics""|22831|6|Mentioned|p 23|||||||||
70509|Tara Formation|62095|6|Mentioned|p278 Appdx.|||Of Hockley (1966) and Dawson (1988). Now incorporated into Woodton Formation.||||||
70509|Tara Formation|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.|||||Fine-grained laminated deposits composed predominantly of volcanic ash, subordinate mudstone.|
70509|Tara Formation|68005|5|Briefly described|p141.|Stephanian|Namurian|Informal name. Listed as a Member of the Currabubula Formation; invalid, even for an informal unit.||Unit in Currabubula Formation.|||Fine-grained laminated deposits composed predominantly of volcanic ash, subordinate mudstone.|
70509|Tara Formation|73264|6|Mentioned|p1389 Fig.11|Devonian|Silurian|Lachlan Orogen. Previously inferred to be a correlative of the Saint Arnaud Group, but more probably Silurian-Devonian age.||||||
29047|Tara Grandiorite|41905|6|Mentioned|p61|||||||||
29047|Tara Grandiorite|46829|6|Mentioned|p18|||||||||
29047|Tara Grandiorite|49705|5|Briefly described|p36|||||||||
79468|Tarcoon Plutonic Complex|70602|5|Briefly described|p65-67,71-74,78|Early Devonian|Late Silurian|Also called "Tarcoon Suite Granitoids" p66, Tarcoon Plutonic Suite p78. Aeromagnetic map data given.|||Includes Bobelah Granite, Sainsbury Park Granite, Compton Downs Granite, Gongolgon Granite, Mount Kelly Granite.|Intrudes Girilambone Group.|Granitoids|
79468|Tarcoon Plutonic Complex|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature of undifferentiated intrusions: many oval to elongate areas of variable magnetic intensity, typically showing irregular texture or banded patterns. These lie within an overall lozenge-shaped complex, elongate in an ENE orientation, and are bounded by major structures. Gravity values are moderate.|||Bobelah, Compton Downs, Mount Kelly and Gongolgon Granites.||I-type granitoids including biotite-?hornblende granodiorite, syenogranite, biotite monzogranite, local microgranite, rhyolite and gabbro. Granite is locally foliated and epidotised.|
78377|Tarcoon plutonic complex|69002|6|Mentioned|p12|||Informal name.|~416 Ma for Compton Downs Granite.||Includes the Compton Downs Granite.|||28-NOV-13
73553|Tarpaulin Creek Sandstone Member|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Of Uriarra Volcanics. Ashstone.||||||
83965|Taylors Adamellite|71628|6|Mentioned|p8-82; p17: 36-37|||Leitch et al. (1971), Henley et al. (2000); mentioned in the map legend. Originally the Culaden Granodiorite of Wood (1982). Reserved as Taylors Monzogranite in ASUD, but named in this study as Culaden Granodiorite because of precedence.||||||
26932|Teamster Formation|29991|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26932|Teamster Formation|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group||||||
27583|Teamsters Creek Beds|30261|6|Mentioned|Table 1|||Marinoan age||||||
27583|Teamsters Creek Beds|30908|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Marinoan. Part of Torrowangee Group||||||
27583|Teamsters Creek Beds|34469|6|Mentioned|p109|||Upper Proterozoic. Table||||||
27583|Teamsters Creek Beds|34563|3|Fully described|p64|||Stratigraphy P58||||||
27583|Teamsters Creek Beds|34812|6|Mentioned|Table 1|||||||||
27583|Teamsters Creek Beds|43502|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Marinoan stage of U.Proterozoic||||||
29050|Teamsters Creek Beds""|34812|6|Mentioned|p15|||Subdivision of Torrowangee Group||||||
35628|Tekum Creek Basalt|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Noonthorange Subgroup. Porphyritic metabasalt.||||||01-DEC-08
35628|Tekum Creek Basalt|66929|5|Briefly described|Map legend|||||Unit in Noonthorangee Subgroup.|||Porphyritic metabasalt.|
78175|Teltawangee Group|68822|6|Mentioned|p330|||Continental slope turbidites.||||||
30503|Teltawongee Beds|22683|6|Mentioned|94 fig 2|||||||||
30503|Teltawongee Beds|23336|5|Briefly described|p11|Middle Cambrian|Early Cambrian|Overlain by Mount Daubeny Formation.||||||21-MAR-06
30503|Teltawongee Beds|23380|5|Briefly described|p107|Middle Cambrian|Early Cambrian|Cof Wonaminta Block. Preferred name Teltawongee beds. Age given in Fig.2 as Late Precambrian to Early cambrian.||||||
30503|Teltawongee Beds|43192|6|Mentioned|p64,67|||Misspelling of Teltawongee beds.||||||
30503|Teltawongee Beds|50618|5|Briefly described|p249 Fig. 2|Middle Cambrian|Early Cambrian|See also Teltawongee beds.||||||
30503|Teltawongee Beds|64169|5|Briefly described|p19|||The accepted version of this name is Teltawongee beds.  Underlies Paddys Creek beds (Palgamurtie Subgroup, Ponto Group). Has well-defined bedding.||||||14-MAY-08
30503|Teltawongee Beds|64685|5|Briefly described|Map Legend|Middle Cambrian|Proterozoic|Monotonous dark grey to buff brown fine to medium-grained soft-weathering turbiditic quartzofeldspathic arenites. Clear younging direction based on graded bedding in more continuous exposures. Rare beds of grey, green and maroon slate.||||||
30503|Teltawongee Beds|67322|6|Mentioned|p10|||Of Mills (1992); renamed Teltawongee Group (Mills, in Greenfield et al.,2010).||||||
29560|Teltawongee beds|22580|5|Briefly described|p87|Cambrian|Cambrian|||||||07-MAR-16
29560|Teltawongee beds|22671|5|Briefly described|Table1p833,Fig1p835|Middle Cambrian|Early Cambrian|Mainly turbidites.  Geological Province: Kanmantoo Fold Belt.||||||17-JAN-06
29560|Teltawongee beds|22772|5|Briefly described|Table13.1|Middle Cambrian|Early Cambrian|||||||
29560|Teltawongee beds|22857|5|Briefly described|Tb 13.1 (insert p70), p90 Fig. 14.7B|Cambrian|Early Cambrian|Turbidites. Contains a lithological variant called Copper Mine Range beds. Correlate with Kanmantoo Group. Geological Province: Kanmantoo Fold Belt. See also p75, p99 and p404 and 406 App. 1 Tb. A1.4.||||||
29560|Teltawongee beds|22858|6|Mentioned|p75,81,Fig14.7bp90-1|||||||||
29560|Teltawongee beds|23224|5|Briefly described|p6|Middle Cambrian|Early Cambrian|||||||
29560|Teltawongee beds|23309|5|Briefly described|p366||Cambrian|||||||
29560|Teltawongee beds|23469|6|Mentioned|Fig 3 p 320|||||||||
29560|Teltawongee beds|24599|5|Briefly described|p494, p495 Fig. 2|Early Cambrian|Early Cambrian|See also p496.  Geological Province: Koonenberry Belt.||||||
29560|Teltawongee beds|42982|5|Briefly described|p333|||||||||
29560|Teltawongee beds|43192|3|Fully described|p63,Table 1 p61.|Middle Cambrian|Early Cambrian|Includes Copper Mine Range beds of Pogson and Scheibner (1971). Equivalent to Kanmantoo Group of S.A.||||||27-NOV-08
29560|Teltawongee beds|43213|5|Briefly described|p63|Middle Cambrian|Early Cambrian|Turbidites. Folded into tight upright folds during Delamerian Orogeny (late Middle Cambrian).||||Overlies Kara beds. Is correlated with Gnalta Group.||
29560|Teltawongee beds|44093|5|Briefly described|p47, p109-110|Early Paleozoic|Early Paleozoic|See also p145 and p148. Unconformable clastic sediments and basic volcanics. Fault contact with Ponto beds. Formerly part of the "Wonominta beds". Contains lithological variant Copper Mine Range beds. Geological Province: Kanmantoo Fold Belt.||||||07-NOV-08
29560|Teltawongee beds|50618|5|Briefly described|p248 Fig. 1|Middle Cambrian|Early Cambrian|Geological Province: Wonominta Block.||||||
29560|Teltawongee beds|60567|5|Briefly described|p39|||||||||19-NOV-04
29560|Teltawongee beds|60990|5|Briefly described|p85-86|Middle Cambrian|Early Cambrian|Coeval with the Gnalta Group. Turbidite slope-trough facies. Biogeographic implications discussed.||||||
29560|Teltawongee beds|62793|5|Briefly described|p270|||Formerly called Wonominta beds in this area. Deformed and metamorphosed sediments in Northern Koonenberry Belt. Unconformably overlain in the east by Morden Formation, the basal unit of Kayrunnera Group.||||||
29560|Teltawongee beds|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Turbiditic arenites and minor slate/phyllite.||||||
29560|Teltawongee beds|63789|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Monotonous dark grey to buff-brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flakes and minor grey, green and maroon slate units. Strongly cleaved with tight to isoclinal folds. Clear graded bedding.||||||
29560|Teltawongee beds|63790|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Monotonous dark grey to buff brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flakes. Strongly cleaved with tight to isoclinal folds.||||||
29560|Teltawongee beds|63793|5|Briefly described|p19 Table 1, p21, p33-34, 36.|||Formerly part of Wonominta beds (Warris 1967). Equivalent to Kanmantoo Group in eastern Mount Lofty Ranges, SA. Slope deposits, coeval with near-shore deposits of Gnalta Group to the west.||Unit in Wonominta beds.|Includes Copper Mine Range beds.|Faulted against Kara beds and Ponto Group.|Dark gey slate, turbidite sandstones witrh graded bedding and Bouma sequence structures; coarse detrital mica flakes common; contains sponge spicules, vertical worm tubes.|19-JAN-15
29560|Teltawongee beds|64168|5|Briefly described|p30, p31|Middle Cambrian|Early Cambrian|Geological Province: Koonenberry Belt. Turbiditic slope deposits.||||||01-JUL-08
29560|Teltawongee beds|64169|6|Mentioned|p18, p20 Fig. 9|Middle Cambrian|Early Cambrian|Geological Province: Mount Daubeny Basin. See also Teltawongee Beds.||||||20-MAY-08
29560|Teltawongee beds|64671|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Conformably overlie Kara beds; faulted against Ponto beds. Monotonous dk. grey to buff brown fine- to med.-gr. turbiditic quartzofeldspathic arenites+detrital mica flakes;strongly cleaved-tight to isoclinally folded. Rare beds of grey, green, maroon slate||||||
29560|Teltawongee beds|64680|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group. Monotonous dark grey to buff brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flakes. Strongley cleaved and tight to isoclinally folded.||||||01-DEC-08
29560|Teltawongee beds|64682|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Monotonous dark grey to buff brown, fine to medium-grained turbiditic quartzofeldspathic arenites and lesser phyllite with detrital mica flakes.||||||
29560|Teltawongee beds|64683|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Monotonous dark grey to buff brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flakes. Strongly cleaved and tight to isoclinally folded.||||||
29560|Teltawongee beds|64684|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group. Monotonous dark grey to buff brown fine to medium-grained tubiditic quartzofeldspathic arenites with detrital mica flakes. Strongly cleaved and tight to isoclinally folded.||||||01-DEC-08
29560|Teltawongee beds|64686|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group. Montonous dark grey to buff brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flackes. Strongly cleaved and tight to isoclinally folded.||||||08-DEC-08
29560|Teltawongee beds|64687|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Conformably overlie western Kara beds, faulted against Ponto Group. Monotonous dark grey to buff brown fine to medium-grained turbiditic quartzofeldspathic arenites with detrial mica flakes.||||||
29560|Teltawongee beds|65381|5|Briefly described|p688, 691, 689 fig 2|Middle Cambrian|Early Cambrian|Of the Wertago zone, Broken Hill; slope turbidites. Tight upright folded turbiditic sandstones.||||||07-MAR-12
29560|Teltawongee beds|66623|6|Mentioned|p31, p33.|||Approximate equivalents with units of Teltawongee Group.||||||
29560|Teltawongee beds|66929|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|||||Overlies Kara beds. Faulted against Ponto Group.|Monotonous dark grey to buff brown, fine- to medium-grained, turbiditic quartzofeldspathic arenites with detrital mica flakes; rare beds of grey, green and maroon slate.|
29560|Teltawongee beds|66933|5|Briefly described|Map legend|||Kayrunnera Zone, Delamerian Fold Belt. Strongly cleaved and tight to isoclinally folded. Weak magnetic signature.||||Overlies Kara beds. Faulted against Ponto Group.|Monotonous dark grey to buff brown fine- to medium-grained turbiditic quartzofeldspathic arenites with detrital mica flakes; rarer beds of grey, green and maroon slate.|
29560|Teltawongee beds|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Broughton Vale (geophysical basement) Zone. Interpreted equivalent to sedimentary and volcanic rocks in the Wirryilka, Budgeree, Mazar and Kimberley (geophysical basement) Zones.|||||Dark grey to buff brown, fine- to medium-grained quartzofeldspathic sandstone with detrital mica flakes.|
29560|Teltawongee beds|70210|5|Briefly described|p1, p23, p27, p40-41|||Koonenberry-Tibooburra district. Intruded by a granite dated at 423.1 +/- 2.4 Ma (also given as 424.1 +/- 2.7 Ma and 422.7 +/- 6.5 Ma).||||||
74917|Teltawongee phyllites|64671|5|Briefly described|Map legend||Early Cambrian|Informal reference to phyllites within the Teltawongee beds - which represent a narrow zone of of suspected fine-grained magnetite.||||||
78578|Teltawoongee Group|68731|6|Mentioned|p119|||Koonenberry Belt.|||Includes the Nundora Formation.|||
30826|Temi Coal Measures|43383|14|Not recorded|p19|||||||||
69152|Temora Complex|60423|5|Briefly described|p372|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt. Probable misspelling of Narraburra Complex.||||||19-FEB-09
78522|Temora granodiorite|68111|5|Briefly described|p970|||Used as the reference zircon for analyses in this study. Black et al. (2003).||||||
25523|Temperance Chert|29456|6|Mentioned|Fig.2|||||||||
25523|Temperance Chert|31019|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25523|Temperance Chert|33325|5|Briefly described|Table 1|||||||||
25523|Temperance Chert|35109|6|Mentioned|p17|||||||||
25523|Temperance Chert|36512|6|Mentioned|p21|||||||||
25523|Temperance Chert|36534|6|Mentioned|p223|||||||||
25523|Temperance Chert|40328|6|Mentioned|p67|||||||||
25523|Temperance Chert|40497|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25523|Temperance Chert|40498|6|Mentioned|p330|||||||||
25523|Temperance Chert|43491|4|Described|pIII/14||Ordovician|U/lies conf. Nine Mile Shale.||||||
25523|Temperance Chert|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Kiandra Beds (Molong Volcanics Rise). Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
35105|Ten Foot band|23055|6|Mentioned|p24|||(Warbrooke 1981) unpubl.||||||
74862|Tent Hill Volcanics''|61793|5|Briefly described|p347|||Was previously suggested in regional geological maps (Brunker and Chestnut, 1976; Barnes and Willis, 1989). Makes up a large proportion of the newly defined Yarramundi Andesite.||||||07-FEB-11
82795|Tenterfield Creek Leucosyenogranite|71628|5|Briefly described|p12: 5; p15: 33, 57, 65; p19: 159-162|||New name, incorporating numerous un-named felsic granites several kilometres NW of Tenterfield. Named after a local watercourse. Distribution described at some length. Unassigned due to uncertainties surrounding relationships with other units. Geochemistry described.||Tenterfield Creek Suite.||Intrudes Wallangarra Volcanics and Dundee Rhyodacite. Abuts Bungulla Monzogranite and Stanthorpe Granite.|Pale pink, medium-grained, slightly porphyritic to uneven-grained-equigranular, biotite leucosyenogranite.|
82796|Tenterfield Creek Suite|71628|6|Mentioned|p19: 161||||||Tenterfield Creek Leucosyenogranite.|||
77364|Tenterfield Limestone|68006|6|Mentioned|p115.|||Ray et al. (2003). N and NW of Torrington. One of several limestones included in the Texas beds.||||||
39931|Teralba Conglomerate, lower|24158|5|Briefly described|p172 Fig.3|||Geological Province: Sydney Basin. Max Thickness: 40m||||||
39930|Teralba Conglomerate, upper|24158|5|Briefly described|p172 Fig.3|||Geological Province: Sydney Basin||||||
82496|Terrible Vale Porphyrite|71628|6|Mentioned|p8: 65, 67|||Binns et al. (1967). Included in Terrible Vale Porphyritic Microtonalite of Flood (1971 unpublished).||||||
73698|Tettenhall Monzonite|63286|5|Briefly described|p302, 304|Ordovician|Ordovician|Renamed the Tettenhall Intrusive Complex. Consists of gabbroic to monzontic intrusions that include equigranular rocks.||||||07-FEB-11
38000|Thackaringa Group, Lower|24307|5|Briefly described|p968 Fig. 3|||Informal name - see Thackaringa Group||||||
37946|Thackaringa Group, Upper|24307|5|Briefly described|p968 Fig. 3|||Informal name - see Thackaringa Group||||||
70624|Thackaringa Group, upper|62373|6|Mentioned|p508|||Informal reference to the upper part of the Thackaringa Group.||||||
32649|Thackaringa pegmatites|46595|14|Not recorded|p.306|||Age of muscovite contained in pegmatite is 495 m.y. (H54-15,I54-3).||||||
35373|Thakeringa Group|23196|6|Mentioned|p830|||||||||
76046|Thalaka Granite Suite|66934|6|Mentioned|Map legend|Early Devonian|Early Devonian|Informal name. |||Includes Yadabal Lagoon and Thalaka granites.|||
80439|Thalaka granodiorite suite|70718|6|Mentioned|p3, p94|||Informal name, derived from geophysics.||||||30-MAY-19
26936|Tharwa Granite|42726|5|Briefly described|map legend|Silurian||Variation on Tharwa Adamellite.||||||
69453|The Brothers Granitoids|69188|5|Briefly described|p7, p9|Late Triassic|Late Triassic|High level/subvolcanic laccoliths, plugs, sills and dykes. Intrudes indurated and deformed interbedded sediments and volcanics of the Lorne Basin.|212.5 +/- 1.6 Ma (magmatic age)||||Fine- to medium-grained diorite, pyroxene-bearing granodiorite, microgranite and leucocratic graphic granite and granophyre; alkali-rich; A-type.|16-APR-20
69453|The Brothers Granitoids|71628|6|Mentioned|p17: 71, 75-76, 78, 81, 84, 87|||Raymond (year not given). Included The Laurieton Granites group of Chappell and Bryant (1994 unpublished). Now The Brothers Suite.||||||
79110|The Brothers quartzite|69635|5|Briefly described|p88-95|||Informal name. Stratigraphic unit shown as Budgery Sandstone Member, Narrama Formation. North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age. No worm burrows or other fossils have been noted in the unit.|497+/-25 Ma|||Detrital age spectrum similar to other Girilambone Group samples.|Sample: Quartzite that represents partially recrystallised quartz-rich sandstone.|
82436|The Knobs Tonalite|71628|5|Briefly described|p2: 62-65, 68, 70-71; p3-33|||New name, after a local hill. 25 km SE of Uralla. Two bodies within the Complex. Geochemistry briefly described.||Woodburn Complex.||Intrudes Sandon beds. Abuts Hillview Gabbro and Eastlake Monzogranite. Is enclosed by Shallow Lagoon Monzogranite.|Hornblende(-biotite) and clinopyroxene(-hornblende-biotite) tonalite.|
82685|The Ridge Suite|71628|6|Mentioned|p19-163||||||The Ridge Monzogranite.|||
69947|The Tops|61214|5|Briefly described|p172 Fig 2|Westphalian|Westphalian|Member of Lark Hill Formation - name abbreviated  - informal.  Of the Boomi Block.||||||
68780|The Valley Tank Arenite|60648|6|Mentioned|p44, p46|Eifelian|Emsian|Abbreviation of The Valley Tank Arenite Member? See also The Valley Tank Pebbly Arenite and The Valley Tank Member. Coarse-grained pebbly arenite.  See also p52 Tb. 2.||||||26-APR-05
35872|The Valley Tank Member|23336|5|Briefly described|p15, p17 Fig. 12, p27-28|||of Coco Range Sandstone.  Max. thickness: ~170m.||||||21-MAR-06
35872|The Valley Tank Member|60648|5|Briefly described|p42 Fig. 2|Eifelian|Emsian|Of the Coco Range Sandstone.  Abbreviation of The Valley Tank Arenite Member? See also The Valley Tank Member and The Valley Tank Pebbly Arenite Member.||||||
35872|The Valley Tank Member|67562|5|Briefly described|p101|Frasnian|Emsian|Sourced from the Broken Hill area and Neoproterozoic strata to the south. Also shown as The Valley Tank Arenite Member, Fig.9 p103.||Of Coco Range Formation.|||Fluvial pebbly coarse-grained fan deposits.|01-OCT-15
68781|The Valley Tank Pebbly Arenite Member|60648|5|Briefly described|p44|Eifelian|Emsian|Of the Coco Range Sandstone.  Abbreviation of The Valley Tank Arenite Member? See also The Valley Tank Member and The Valley Tank Member. Max. thickness: ~150m.  Geological Province: Darling Basin.||||||26-APR-05
70153|The Valley Tank arenite member|23336|6|Mentioned|p16|||Informal reference to The Valley Tank Member.  Coarse-grained, pebbly.||||||
80156|Therebri Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin. Shown only as Therebri. Ending assumed from references to other Coal Members in text.||Maules Creek Formation.||||28-SEP-17
80157|Thiess Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area. Shown only as Thiess. Ending assumed from references to other Coal Members in text.||Rowan Formation. ||||28-SEP-17
38447|Thologolong granite|24133|6|Mentioned|p22|||Geological Province: Lachlan Fold Belt.||||||
34269|Thompson Formation""|22679|6|Mentioned|p 27|||Of Chin (1972).  Now Kangaloolah Volcanics.||||||
80270|Thompson Granite|65469|6|Mentioned|p43, p52, p55 fig 3-19, p62, p67|||Lachlan Orogen.||||||
37409|Thompsons Formation|23214|6|Mentioned|p142|||||||||
27585|Thorndale Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
27585|Thorndale Gneiss|22857|5|Briefly described|p45 Tb. 12.2|||Renamed Thorndale Composite Gneiss (Stephens, 1995) as part of the Willyama Supergroup. Referred to as Erewhon Suite by Archibald (1978) and Suite 2 by Stevens, Stroud et al (1979, 1980).||||||
27585|Thorndale Gneiss|22966|5|Briefly described|p2,Fig 1||Proterozoic|Early rift stage of development.||||||
27585|Thorndale Gneiss|30908|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Lower to Middle Proterozoic||||||23-DEC-09
27585|Thorndale Gneiss|33262|6|Mentioned|PB222|||||||||
27585|Thorndale Gneiss|39638|6|Mentioned|Table 1|||||||||
27585|Thorndale Gneiss|39662|6|Mentioned|Table 1|||Refers Cordwell and Williams (1962)||||||
27585|Thorndale Gneiss|43502|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|(Provisional Edition) Part of Willyama Complex||||||07-NOV-08
27585|Thorndale Gneiss|63110|6|Mentioned|p1129 Fig. 8|||Comprises metasedimentary and quartzo-feldspathic gneiss.||||||11-JUN-08
27585|Thorndale Gneiss|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
34510|Thorndale Suite|22771|6|Mentioned|Table12.2p45|||||||||
34510|Thorndale Suite|22857|5|Briefly described|p45 Tb. 12.2|||Of Archibald (1978). Uncertain how it relates to present Thorndale Composite Gneiss?||||||
76850|Thornedale Composite Gneiss|65681|6|Mentioned|p734 Fig.1.|||Broken Hill Block.||||||
38460|Thowgla Creek granite|24133|6|Mentioned|p57|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
38455|Thowgla Granite|24133|6|Mentioned|p51|||||||||
39367|Thrumster slate|24124|6|Mentioned|p3|||Informal - see Thrumster Formation.||||||
68024|Thuddungra laterite|23366|6|Mentioned|p12|||Informal reference to lateritic deposits in the Thuddungra Mine in Young.||||||
82797|Thulimbah Monzogranite Phase|71628|5|Briefly described|p15: 35, 46, 49, 52, 57-58, 60, 64|||See also p15: 68-72, 82, 86, 115; p19: 83, 163. New unit, after the locality of Thulimbah; differentiated geochemically. This subunit does not 'technically' qualify as a Phase according to stratigraphic naming conventions. Previously part of Stanthorpe Monzogranite. Crops out from 5km N of Thulimbah to ~1km SE of Ruby Creek; forms well-exposed boulder strewn small domes. Geochemistry detailed: is geochemically assigned to Thulimbah Suite. Is spatially associated with several Mo-Sn-W deposits (listed). RELATED UNITS (continued): Abuts Ridge, Severn River and Jenners Monzogranites, Cullendore Syenogranite, Karonstadt Complex and Ruby Creek Leucogranite. is faulted against The Ridge Monzogranite. Is overlain locally by Marburg Subgroup.||Mount Lindesay Monzogranite.||Intrudes Silverwood Group and Undercliffe Falls Monzogranite (and is faulted against the latter). Partially encloses (?is intruded by) Donnellys Castle Leucomonzogranite. See COMMENTS for more.|Light pink, medium-grained, seriate to fine-grained, porphyritic (marginal) K-feldspar-rich monzogranite-syenogranite. Comparatively mafic unit. Likely a contaminated and/hybrid I-type.|
82798|Thulimbah Suite|71628|6|Mentioned|p15: 35|||The Thulimbah Monzogranite Phase (of Mount Lindesay Monzogranite) is geochemically assigned to this Suite.||||||
79212|Thuralilly Suite|68592|6|Mentioned|p1677||||||||Biotite granites.|
39268|Thurungly granite|24233|6|Mentioned|p257 Fig.5, p259|||Informal name.||||||
73934|Tia Suite|71628|5|Briefly described|p3-87|||||Hillgrove Supersuite.|Tia Granodiorite.|||
83046|Tia granodiorites|73202|6|Mentioned|p637|Asselian|Kasimovian|New England Orogen, southern. Zircon U-Pb crystallisation age from Collins et al., (1993). [Misspelling of Tia Granodiorite?]|302 +/- 4 Ma U-Pb zircon|Hillgrove Plutonic Supersuite||||
76172|Tibooburra Group|66623|6|Mentioned|p99, 101.|||A division (Andrews 1922) of Torrowangee Series.||||||
76173|Tibooburra Series|66623|6|Mentioned|p54, 99, 101|||Named by Andrews (1922). Formerly part of Torrowangee Series (Mawson 1912). Subsequently divided into Wonominta Beds by Warris (1967), Wonominta Complex (Scheibner 1973) and Tibooburra beds (Mills 1992).||||||
30502|Tibooburra beds|22700|6|Mentioned|p775|Middle Devonian|Ordovician|of Thomson Fold Belt.||||||
30502|Tibooburra beds|43192|6|Mentioned|Fig. 1 p59|||Invalid name.||||||
30502|Tibooburra beds|50618|5|Briefly described|p248 Fig. 1|Middle Devonian|Ordovician|Geological Province: Wonominta Block.||||||
30502|Tibooburra beds|66623|6|Mentioned|p45.|||Named by Mills (1992). Formerly part of Torrowangee Series (Mawson 1912), Mount Browne Series and Milparinka Group (Andrews 1922), Wonominta Beds (Warris 1967), Wonominta Complex (Scheibner 1972). Now Depot Glen Formation (this study).||||||
78579|Tibooburra suite|68731|5|Briefly described|p213 Fig 3.118, p215|Pridoli|Wenlock||428-420 Ma (Greenfield, Gilmore, and Mills 2010).|||||
73721|Tidbinbilla Formation|63290|6|Mentioned|p403|Llandovery|Llandovery|NOT of Yalmy Group. Younger unit.||||||11-FEB-08
73726|Tidbinbilla formation|63290|6|Mentioned|p395|||Informal. Consists of angular-grains and detrital mudstone.||||||
30796|Tighe's Hill Formation|43344|14|Not recorded|p85|||||||||
30796|Tighe's Hill Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Lambton Subgroup (Newcastle Coal Measures)||||||
35152|Tighs Hill Formation|23055|6|Mentioned|Fig11p23|||||||||
82799|Tilbuster Suite|71628|5|Briefly described|p8-107|||||Uralla Supersuite.|Tilbuster Granodiorite.|||
34641|Tilga Granodiorite""|22815|6|Mentioned|p81|||Obsolete. Renamed Badja Granodiorite.||||||
26943|Tilmunda Adamellite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
26943|Tilmunda Adamellite|35257|6|Mentioned|Fig.17|||||||||
26943|Tilmunda Adamellite|71628|6|Mentioned|p4: 2, 7, 53|||Chesnut et al. (1973). Chappell (1978) referred to it as Tilmunda Granite.||||||
29058|Tilmunda Granite|33781|6|Mentioned|Table 1|||||||||
29058|Tilmunda Granite|35192|6|Mentioned|Fig.1|||||||||
29058|Tilmunda Granite|38821|5|Briefly described|p183|||||||||
29058|Tilmunda Granite|71628|6|Mentioned|p4: 46, 48, 50, 53|||Chappell (1978). Previously Tilmunda Adamellite (Chesnut et al., 1973). In this study it becomes Tilmunda Syenogranite Phase of Pringles Monzogranite.||||||
32508|Timbarra mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
78372|Tinchelooka diorite|68823|6|Mentioned|p376 Fig.3, p378 Fig.4|Emsian|Emsian|New name; informal?(Glen et al 2010; Hegarty 2010). Louth area. Bulbous area of high magnetic intensity.|402 Ma|||||
78372|Tinchelooka diorite|69002|5|Briefly described|p9, p13, Map 1b|Emsian|Emsian|Informal name. Occurs on the Tinchelooka 1:100k map sheet as a bulbous-shaped area of high magnetic intensity interpreted as an intrusion. Zircons were extracted from a mineral exploration drill hole at the north-east end of the intrusion.|~402 SHRIMP-IIe (Geoscience Australia)||||Quartz diorite|
78372|Tinchelooka diorite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen.?High magnetic intensity||||||
78372|Tinchelooka diorite|69043|5|Briefly described|p3, p5-6, p11, p91, p93-99, p118|Middle Devonian|Middle Devonian|Tringadee area, Thomson Orogen. c.100km WNW of Bourke. Characterised by variable but high aeromagnetic response. An unusual age for this region.|401.8 +/- 3.1 Ma.||||Massive, undeformed, fine- to medium-grained, plagioclase-phyric quartz diorite, micromonzonite; pervasively altered.|
78372|Tinchelooka diorite|69541|5|Briefly described|p645 Fig.1(b)|Early Devonian|Early Devonian|Thomson Orogen.|402 Ma.|||||
78372|Tinchelooka diorite|71860|5|Briefly described|p7|||Informal name. Age is a SHRIMP U-Pb date.|401.8 +/- 3.1 Ma (Bodorkos et al. 2013)||||Quartz diorite.|
78372|Tinchelooka diorite|72522|6|Mentioned|p29.|Early Devonian|Early Devonian|With Conlea porphyry, age determined to be indistinguishable from the date of samples from the 52172127 volcaniclastic sandstone (Nimrod TDH6; 398.3 +/- 2.3 Ma). Ref. Bodorkos et al., 2013.||||||
78372|Tinchelooka diorite|73179|6|Mentioned|p1155|Emsian|Emsian|Southern Thomson.|401.8 +/- 3.1 Ma|||||
26947|Tingaringi Granite|42726|5|Briefly described|map legend|Silurian||Variation/misspelling of Tingaringy Granodiorite?||||||
32267|Tingaringi Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb19. Misspelling of Tingaringy Granodiorite?||||||
32267|Tingaringi Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
32267|Tingaringi Granodiorite|72571|5|Briefly described|p90, p92, p96-99|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.|||||Mafic cordierite granite with ilmenite.|
31644|Tingaringi Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31644|Tingaringi Suite|72571|6|Mentioned|p90|||Of the Tasmanides of eastern Australia.||||||
30045|Tingha Formation|43188|6|Mentioned|p217|||Invalid name. Tingha Adamellite has priority.||||||
35054|Tingha-Gilgai group|23050|4|Described|p76|||Informally used to refer to a group of Tin leads.||||||
35437|Tinja Formation""|23170|6|Mentioned|p62|Early Devonian|Early Devonian|||||||
73258|Tinowon Sandstone|60363|5|Briefly described|p22 Fig. 2, p24|Permian|Permian|Geological Province: Bowen Basin.||||||
73259|Tinowon sandstone|60363|6|Mentioned|p22|Permian|Permian|Informal - see Tinowon Sandstone p24.||||||17-NOV-15
29062|Tintern Aplite|42726|5|Briefly described|map legend|||||||||
72797|Titringo Creek Siltstone|62740|5|Briefly described|p371|Middle Eocene|Middle Eocene|Of the Nerriga Sub-Group. Lacustrine deposits.||||||06-FEB-07
40254|Tobermory group|38842|5|Briefly described|p286|Permian|Permian|Geological Province: New England Fold Belt. Age: 285 +/- 15Ma||||||
72757|Toggannoggra Rhyolite|61818|5|Briefly described|p85|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
28183|Togganoggra Rhyolite|42497|5|Briefly described|Map legend|Pridolian|Ludlovian|Misspelling of Toggannoggra Rhyolite Member?||||||
31008|Tolga Formation|43479|14|Not recorded|p126|||||||||
26949|Toll Bar Group|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26949|Toll Bar Group|32671|6|Mentioned|Map legend|Permian|Permian|||||||
26949|Toll Bar Group|34043|4|Described|p451|||||||||
26949|Toll Bar Group|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
26949|Toll Bar Group|34292|6|Mentioned|p32|||See also P33, Tables 1 & 3. Permian||||||
26949|Toll Bar Group|34447|6|Mentioned|Table 5.2|||||||||
26949|Toll Bar Group|37065|6|Mentioned|p33|||||||||
26949|Toll Bar Group|37094|5|Briefly described|p241|||||||||
26949|Toll Bar Group|43440|14|Not recorded|p82,86,90|||Correlated with Mulbring Siltstone. Ref. to Hanlon 1953. See also Lexicon||||||
26949|Toll Bar Group|61201|6|Mentioned|p5 Table 1,|||Now Toll Bar Formation.||||||
82607|Tolleys Gully Suite|71628|5|Briefly described|p8: 111|||||Uralla Supersuite.|Tolleys Gully Leucomonzogranite.|||
80935|Tollingo granodiorite|70751|6|Mentioned|p12|Lochkovian|Pridoli|||||||16-MAR-19
80935|Tollingo granodiorite|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||May intrude Kopyje Group and Babinda Volcanics.||
77703|Tom Groggin Gabbro|60308|6|Mentioned|p38|Wenlock|Wenlock|"Important stratigraphic unit with contentious age" Preferred age quoted.|424 Ma|||||
38461|Tom Groggin granite|24133|6|Mentioned|p57|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
38461|Tom Groggin granite|24551|6|Mentioned|p233|||Of the Tom Groggin Suite.||||||
68202|Tomago Coal Measures, Lower|60281|6|Mentioned|p61|||Informal - see Tomago Coal Measures.||||||
68206|Tomago Coal Measures, Upper|60281|6|Mentioned|p61|||Informal - see Tomago Coal Measures.||||||
72980|Tomago Coal Measures, lower|61315|6|Mentioned|p176|||Informal - see Tomago Coal Measures. ||||||
72980|Tomago Coal Measures, lower|73625|6|Mentioned|p2|Permian|Permian|Newcastle coalfield, Sydney Basin.||||Overlies Mulbring Siltstone. Is overlain by upper Tomago Coal Measures.||
68204|Tomago Coal Measures, upper|60281|6|Mentioned|p8, p61|||Informal - see Tomago Coal Measures.||||||22-MAR-05
68204|Tomago Coal Measures, upper|73625|6|Mentioned|p2|Permian|Permian|Newcastle coalfield, Sydney Basin.||||Overlies lower Tomago Coal Measures. Is overlain by Waratah Sandstone.||
29063|Tomago Sand Beds|32917|6|Mentioned|p125|||Groundwater investigations||||||
30797|Tomago Stage|43344|14|Not recorded|unknown|||reference not on card||||||
30797|Tomago Stage|43440|14|Not recorded|p90|||Ref.to David 1950||||||
30797|Tomago Stage|43477|14|Not recorded|p15,16,22,Pl.3|||Ref.to David||||||
30797|Tomago Stage|44855|14|Not recorded|p25||Late Permian|||||||
25538|Tomago Thin Seam|39292|6|Mentioned|Fig.6.3|||||||||
25538|Tomago Thin Seam|42182|6|Mentioned|p297|||||||||
30948|Tomago series|43425|14|Not recorded|p5||Permian|||||||
80162|Tomakin Basalt""|70601|5|Briefly described|p37, p43-5, p47-48, p51, p54|Middle Cambrian|Middle Cambrian|Melville Point. Informal term for this basin-floor unit in the Albury-Bega basin succession, to avoid confusion with "Seamount Basalt" in the Narooma Terrane. Stratigraphic position mirrors Eagle Peak Basalt. Age from Dookie gabbro (reasons given).||||Conformably underlies "Melville Chert". Is faulted against Adaminaby Group.|Seafloor pillow lava basalt; 30 m-wide greenstone composed of flattened basalt pillows. Back-arc basin magmatic affinity; tholeiitic basalt.|
34597|Tombong beds""|22815|6|Mentioned|p35|||Superseded by Tombong Formation.||||||
25539|Tomingley Beds|29986|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25539|Tomingley Beds|40136|6|Mentioned|p15|||||||||
25539|Tomingley Beds|43500|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) (M.Ord)||||||
25539|Tomingley Beds|48958|6|Mentioned|Plate 1|||||||||
70051|Tongarra coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
70348|Toogawoolah Group|60993|6|Mentioned|p8 Tb. 2|||Geological Province: Clarence-Moreton Basin.||||||
78650|Tooggannoggra Rhyolite Member|69159|5|Briefly described|Map legend|Pragian|Lochkovian|||Unit in Long Flat Volcanics.||Overlies Kadoona Dacite Member. Is overlain by Kain Porphyry Member.|Cream, grey and black, medium-grained, moderately crystal-rich, densely-welded rhyolitic ignimbrite; minor intercalated non-welded tuff and volcanic sandstone; rare siltstone.|07-SEP-15
41563|Toogong basalt|50616|6|Mentioned|p286 Fig. 9||Miocene|Informal name.||||||
24530|Toolamanang Volcanics|36285|2|Defined|p55|Silurian|Silurian|See also Fig.2.& 3.||||||
24530|Toolamanang Volcanics|39660|6|Mentioned|p450|||||||||
24530|Toolamanang Volcanics|40106|4|Described|p593|||||||||
35438|Toolamanang Volcanics""|23170|6|Mentioned|p69|||Superseded by Toolamanang Formation.||||||
42037|Toolong Beds|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Pre-Cratonic Province. Mudstone, siltstone, sandstone (slightly metamorphosed).||||||09-NOV-04
74636|Toongi trachyte|64329|5|Briefly described|p15|||One of a number of alkaline bodies forming part of a relatively extensive alkaline volcanic complex  in Dubbo region; comprised dominantly of K-feldspar, albite and aegerine microphenocrysts in a very fine-grained groundmass of similar composition.||||||29-JUL-08
39406|Toongie Group|24126|6|Mentioned|p198|||||||||
74767|Tooronga Chert""|61964|6|Mentioned|p83|||Widely mapped by geologists in the 1980s in basal part of Ural Volcanics in the Yelkin to Browns Reef area. Name probably obsolete? Rocks may now be included in the Bootoowa Fossil Member ||||||
35763|Top-Crossing Sandstone|23859|5|Briefly described|p931 Fig 3|||See Top-Crossing Sandstone Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
37310|Tops Ignimbrite|24010|6|Mentioned|p390|||||||||
40583|Tops Rhyolite Member|24605|2|Defined|p931, p943, p953 App.1|Westphalian|Westphalian|Of the Lark Hill Formation. Age: 316.3 +/- 2.1 Ma. Thickness at type locality: ~12m. Geological Province: New England Orogen.||||||
29069|Torrowangee Series tillite|33336|6|Mentioned|p245|||||||||
29447|Torrumbarry Clay Member""|42966|6|Mentioned|Table 29 p183|||Of Shepparton Formation, as a synonym for Torrumbarry Clay.||||||10-NOV-08
32658|Tottem's Hill Tuff Formation|46547|14|Not recorded|Not recorded|||||||||
73671|Tottenham Volcanics|63278|6|Mentioned|p145 Fig. 1|||||||||07-FEB-11
73671|Tottenham Volcanics|70684|6|Mentioned|p3, p54|||||||||
73671|Tottenham Volcanics|72495|5|Briefly described|p217-218|||Of Glen et al. (2004). Described by Suppel (1974) [as Tottenham Formation] and Sherwin (1996) [as Tottenham Subgroup]. Coincides with a north-western gravity high in the Junee-Narromine volcanic belt.|||||Includes mafic schist.|24-MAR-20
38467|Touzells granodiorite|24133|6|Mentioned|p93|||Informal - see Touzells Granodiorite.  Geological Province: Lachlan Fold Belt.||||||
29072|Towgon Grange Granodiorite|23799|5|Briefly described|p117|||Of the Towgon Suite (Clarence River Supersuite).||||||
29072|Towgon Grange Granodiorite|23811|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Clarence River Plutonic Suite.  Medium- to coarse-grained, equigranular to weakly porphyritic, hornblende-biotite granodiorite, tonalite, quartz diorite and diorite.||||||20-DEC-04
29072|Towgon Grange Granodiorite|23812|5|Briefly described|p21 Tb.2, p18|Late Permian|Late Permian|Of Clarence River Plutonic Suite.||||||
29072|Towgon Grange Granodiorite|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
29072|Towgon Grange Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
29072|Towgon Grange Granodiorite|35875|6|Mentioned|p14|||||||||
29072|Towgon Grange Granodiorite|42719|6|Mentioned|p14|||||||||
29072|Towgon Grange Granodiorite|60079|5|Briefly described|Map Legend|Permian|Permian|Of the Clarence River Suite.  Granodiorite, tonalite, quartz-diorite, diorite.||||||20-JUL-04
29072|Towgon Grange Granodiorite|61795|6|Mentioned|p368|Early Triassic|Late Permian|Geological Province: New England Fold Belt. I-type granites.||||||17-NOV-08
29072|Towgon Grange Granodiorite|68008|6|Mentioned|p333|||Geochemistry mentioned.||||||
29072|Towgon Grange Granodiorite|68111|5|Briefly described|p968 Tb.1|Wuchiapingian|Wuchiapingian|Ar-Ar dating of hornblende by Bryant et al. (1997).|ca. 257.5 Ma|Of the Clarence River Supersuite.||||22-OCT-14
29072|Towgon Grange Granodiorite|70217|5|Briefly described|p72, p73 tbl 14.1|Wuchiapingian|Wuchiapingian|New England Orogen. Ages are similar to the Mount Ephraim Granodiorite. |c. 257.5 Ma (Ar/Ar, Bryant et al,  1997a)|Clarence River Supersuite||||
29072|Towgon Grange Granodiorite|71628|6|Mentioned|p9: 1-2, 4, 35|||Brunker and Chesnut (1976). Was included in the Clarence River Plutonic Suite of Shaw and Flood (1981). The lithology is not included on p9: 1-2. Renamed Towgon Grange Tonalite (Waltenberg et al., 2016) better to reflect the dominant composition. Is excluded from Clarence River Supersuite in this study.||||||
83623|Town Amphibolites|73575|6|Mentioned|p826|||Interpreted to be a single unit with the Consols Amphibolites. See also Township Amphibolite p830 Fig.4.||||||
24533|Towneys Creek Adamellite|22815|4|Described|p78|||||||||
24533|Towneys Creek Adamellite|36413|2|Defined|p117|Devonian|Devonian|||||||
24533|Towneys Creek Adamellite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Jerangle Igneous Complex. Biotite adamellite. GSNSW map code: gjt.||||||
24533|Towneys Creek Adamellite|39626|6|Mentioned|p276|||||||||
24533|Towneys Creek Adamellite|40328|4|Described|p211|||||||||
24533|Towneys Creek Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Glenbog Suite.||||||20-MAY-08
24533|Towneys Creek Adamellite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
83624|Township Amphibolite|73575|6|Mentioned|p830 Fig.4|||See also Town Amphibolites p826.||||||
31757|Towrang Formation|22857|5|Briefly described|ERRATA sheet for p177, p480, p482|Late Silurian|Late Silurian|Supersedes Towrang beds and "Towrang beds". Shale, siltstone, chert, quartz arenite, quartzite.||||||
31757|Towrang Formation|43834|4|Described|p29||Late Silurian|+1000m thick.||||||
31757|Towrang Formation|61762|6|Mentioned|p19 Fig. 2(a)||Late Silurian|||||||
31757|Towrang Formation|68592|6|Mentioned|p815, p827, p1174|||Jones et al. (1995). Superseded: now Covan Creek Formation.||||||
31757|Towrang Formation|71069|6|Mentioned|p168|||Obsolete name replaced by the Covan Creek Formation. ||||||
79213|Towrang Granodiorite|68592|6|Mentioned|p1763|||Said to be of O'Reilly (1972). [Her version, in fact, was Towrang granodiorite]. Current mapping has led to it being incorporated into the Lockyersleigh Granite.||||||
70039|Towrang beds""|22857|6|Mentioned|ERRATA sheet for p177, p480, p482|||Superseded by Towrang Formation - see ERRATA insert.||||||
77325|Tranquille Dacite|68005|5|Briefly described|p139.|Stephanian|Namurian|||Unit in Willuri Formation.|||Purple-red, welded to unwelded, rhyolitic ignimbrite.|
32400|Trealmont Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Quartzite.||||||
26183|Trelawney Beds|13995|5|Briefly described|p72|Ordovician|Ordovician|Northeast NSW. Tabulate coral species, described by Hall (1975), listed.||||||
26183|Trelawney Beds|30911|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26183|Trelawney Beds|30983|5|Briefly described|p76|||||||||
26183|Trelawney Beds|31216|2|Defined|p77|Ordovician|Ordovician|||||||
26183|Trelawney Beds|31999|6|Mentioned|p133|||Late Ordovician.||||||
26183|Trelawney Beds|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26183|Trelawney Beds|32672|6|Mentioned|p672|||||||||
26183|Trelawney Beds|33002|6|Mentioned|p417|||Tectonic history||||||
26183|Trelawney Beds|33004|6|Mentioned|p187|||||||||
26183|Trelawney Beds|34397|6|Mentioned|p230|||||||||
26183|Trelawney Beds|34575|6|Mentioned|p642|||Ordovician. See also P643||||||
26183|Trelawney Beds|35118|6|Mentioned|p440|||||||||
26183|Trelawney Beds|35137|6|Mentioned|p88|||||||||
26183|Trelawney Beds|35554|6|Mentioned|p5|||||||||
26183|Trelawney Beds|36512|6|Mentioned|p21|||||||||
26183|Trelawney Beds|37727|6|Mentioned|Fig.1|||||||||
26183|Trelawney Beds|39331|6|Mentioned|Table 10-1|||See also Fig.10-1||||||
26183|Trelawney Beds|40127|6|Mentioned|p10|||||||||
26183|Trelawney Beds|40136|5|Briefly described|p41|||||||||
26183|Trelawney Beds|43407|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
26183|Trelawney Beds|43419|4|Described|p112,113||Ordovician|Fossils. 9 miles SE Tamworth||||||
26183|Trelawney Beds|48940|6|Mentioned|p8|||Refers Philip (1966)||||||
25552|Trelawney Beds""|35554|6|Mentioned|Table 2|||||||||
25552|Trelawney Beds""|67322|5|Briefly described|Fig.5; p39|Katian|Katian|Obsolete. (Phillip 1966; Webby 1988): comprises limestone clasts (Eastonian age) within the Drik Drik Formation. Occurs in the Tamworth-Neminha region. See also reference to 'Trelawney beds' (p27).||||Emplaced within the Drik Drik Formation. Unconformably overlies the Haedon Formation.|Comprises limestone clasts.|22-FEB-18
78657|Trelawney arenite""|67322|6|Mentioned|Fig.5|Early Ordovician|Early Ordovician|This age range is for the 'protoliths' of allochthonous blocks later redeposited into younger sediments.||||||22-FEB-18
78612|Trelawney beds|65398|6|Mentioned|p21|||Possible time equivalent of the limestone units of Glen Bell Formation.||||||
78612|Trelawney beds|71091|5|Briefly described|p147, p162, p164|Ordovician|Ordovician|SE of Tamworth. Subsequently recognised as allochthonous limestone blocks containing Late Ordovician corals (briefly described), within the Early Devonian Drik Drik Formation. Early-middle Katian.||||||
78656|Trelawney beds""|67322|5|Briefly described|p27|Late Ordovician|Late Ordovician|Packham (1969) reported a Bendigonian graptolite in sediment associated with this unit, which is now considered as Eastonian allochthonous blocks emplaced in Early Devonian Drik Drik Formation. See also reference to 'Trelawney Beds' (p39).|||||Limestone, clastic sediments.|22-FEB-18
78656|Trelawney beds""|73492|5|Briefly described|p704, p706|Late Ordovician|Late Ordovician|||Drik Drik Formation|||Allochthonous limestone.|
34627|Trewilga Beds""|22831|6|Mentioned|p 34|||Replaced by Mumbidgle Formation||||||
34627|Trewilga Beds""|24417|5|Briefly described|p42|||Now included as the Forbes Group.||||||
34629|Trewilga Formation""|22831|6|Mentioned|p 34|||These rocks now included in the Forbes Group (mostly the Mumbidgle Formation).||||||
68509|Triangle Group""|44093|5|Briefly described|p116|Gisbornian|Darriwilian|Min Age: early Gisbornian. Informal name used by Fowler and Iwata (1995) for Ordovician arenite and tuff in the Molong Volcanic Arc area.||||||
37411|Tricketts Arch Limestone Member|23214|5|Briefly described|p145|Late Silurian|Late Silurian|Now designated as undifferentiated Hollanders Formation. Max. thickness 90m.||||||
39809|Trilobite Bed, Lower""|24248|6|Mentioned|p52|||Of Mitchell (1887). Now included within Yarwood Siltstone. Member of the Black Bog Shale.||||||
39809|Trilobite Bed, Lower""|71656|6|Mentioned|p25|||Now Yarwood Siltstone Member. Initally called the 'Lower Trilobite Bed' (Mitchell, 1887 and others). Diverse record of brachiopods, corals and bryozoa.||||||
79835|Trilobite Bed, Middle|13996|6|Mentioned|p147|||Bowning. Echinoderm taxa Table.||||||
39810|Trilobite Bed, Middle""|24248|6|Mentioned|p52|||Of Mitchell (1887). Superseded by Rainbow Hill Member (Rosebank Shale).||||||
39810|Trilobite Bed, Middle""|71656|6|Mentioned|p26|||Of Etheridge and Mitchell (1895,1897) and others. Now Rainbow Hill Member.||||||
79836|Trilobite Bed, Upper|13996|6|Mentioned|p137|Pridoli|Pridoli|Bowning, near Yass. Subsequently renamed the Elmside Formation. Contains conulariids (species listed).||||||
39813|Trilobite Bed, Upper""|24248|5|Briefly described|p53|||Of Mitchell (1887). Now included within Elmside Formation.||||||
39813|Trilobite Bed, Upper""|71656|6|Mentioned|p27|||Informal or obsolete name for upper part of Elmside Formation.||||||
40942|Trilobite bed, Lower""|50230|6|Mentioned|Map legend|Ludlow|Ludlow|Informal name.  Superseded by Yarwood Siltstone Member (Black Bog Shale, Hatton Corner Group).||||||10-MAY-04
40942|Trilobite bed, Lower""|64238|6|Mentioned|Map legend|Silurian|Silurian|Former name for Yarwood Siltstone Member of Black Bog Shale ((Hattons Corner Group)...........name now obsolete.||||||
40946|Trilobite bed, Middle""|50230|6|Mentioned|Map legend|Ludlow|Ludlow|Informal and superseded - see Rainbow Hill Member (Rosebank Shale).||||||
40946|Trilobite bed, Middle""|64238|6|Mentioned|Map legend|Silurian|Silurian|Former name for Rainbow Hill Member of Rosebank Shale (Hattons Corner Group)...........name now obsolete.||||||
40941|Trilobite bed, Upper|64238|6|Mentioned|Map legend|Silurian|Silurian|[Said to be] former name for Rosebank Shale (Hattons Corner Group)...........name now obsolete.||||||13-JAN-17
40944|Trilobite bed, Upper""|50230|5|Briefly described|Map legend|Lochkovian|Lochkovian|Informal name for limestone lenses of the Hattons Corner Group.||||||10-MAY-04
38311|Triple seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
38311|Triple seam|44244|6|Mentioned|p327|||In the Stroud-Gloucester Syncline.||||||
38951|Troffs Formation""|24417|6|Mentioned|p147|||||||||
72900|Troffs Formation, upper|62569|5|Briefly described|p606|||Informal name. Geological Province: Lachlan Fold Belt. Contains brachiopods of middle Pragian-early Emsian age.||||||10-AUG-07
25555|Trundle Beds""|22831|6|Mentioned|p 42|||||||||
25555|Trundle Beds""|24417|6|Mentioned|p78|||Superseded by Trundle Group.||||||
25555|Trundle Beds""|35609|6|Mentioned|p11|||||||||
25555|Trundle Beds""|36066|6|Mentioned|p4|||Refers McClatchie 1971.||||||
25555|Trundle Beds""|37258|6|Mentioned|p2|||||||||
25555|Trundle Beds""|41528|6|Mentioned|p35|||||||||
25555|Trundle Beds""|42566|6|Mentioned|p100|||||||||
37436|Trunkey Formation|23214|6|Mentioned|p202|||Informal name superseded.||||||
25556|Trunkey Series""|40328|6|Mentioned|p162|||||||||
29080|Tucklan Beds|24126|5|Briefly described|p3|Early Devonian|Early Devonian|||||||
29080|Tucklan Beds|29909|6|Mentioned|p137|||||||||
29080|Tucklan Beds|29993|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
29080|Tucklan Beds|30910|6|Mentioned|Map legend|Devonian|Silurian|Siluro - Devonian ?||||||
29080|Tucklan Beds|31381|6|Mentioned|p52|||||||||
29080|Tucklan Beds|31726|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
29080|Tucklan Beds|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
29080|Tucklan Beds|32047|6|Mentioned|Fig.1|||||||||
29080|Tucklan Beds|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
29080|Tucklan Beds|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
29080|Tucklan Beds|34059|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
29080|Tucklan Beds|36534|6|Mentioned|p225|||||||||
29080|Tucklan Beds|37727|5|Briefly described|p90|||||||||
29080|Tucklan Beds|39663|6|Mentioned|Table 1|||||||||
29080|Tucklan Beds|40328|5|Briefly described|p139|||||||||
29080|Tucklan Beds|43355|14|Not recorded|Map Legend|Devonian|Silurian|Provisional Edition||||||
29080|Tucklan Beds|43356|14|Not recorded|Map Legend|Devonian|Silurian|||||||
29080|Tucklan Beds|43405|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
29080|Tucklan Beds|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
29080|Tucklan Beds|43494|5|Briefly described|p7|Ordovician|Ordovician|Superseded by Tucklan Formation.  Age has also been inferred as Devonian (Pickett 1982).||||||16-MAR-06
35422|Tucklan Beds""|23170|6|Mentioned|p46|||Divided into Tucklan Formation and Dungeree Volcanics.||||||
78489|Tucklen beds|66191|6|Mentioned|p496|Ordovician|Ordovician|Presumed cause of a strong gravity low in southernmost Gunnedah Basin.||||||08-NOV-13
37398|Tuffaceous Trilobite Bed""|23214|3|Fully described|p111|Wenlock|Llandovery|Informal unit of Boree Creek Formation. Consists of thin bedded, calcareous, and tuffaceous sandstone and thin shale layers, rich in trilobite and ostracodes.||||||
37410|Tuglow Formation|23214|6|Mentioned|p145|||Renamed Hollanders Formation of Mumbil Group.||||||
37415|Tuglow Formation""|23214|6|Mentioned|p146|||Informal - see Hollanders Formation.||||||
26959|Tuglow Granite|42712|4|Described|Table 1 p13|Carboniferous|Early Carboniferous|Variation on Tuglow Adamellite.||||||
26959|Tuglow Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
26959|Tuglow Granite|68592|6|Mentioned|p1768, p1774|||Originally Tuglow Adamellite of Packham (1968). Appears as Tuglow Granite of the Tuglow Suite in Chappell et al. (1991). Superseded by Kanangra Granite (Scheibner, 1973 after Shiels, 1959).||||||
75933|Tullyangela Granite|66300|5|Briefly described|p52, pp64-69.|Late Devonian|Late Devonian|This age is indistinguishable from Grassy Gully Rhyolite Member of Yalwal Volcanics, indicating at least local exposure of plutonic equivalents of the Late Devonian volcanic succession in southern MOSS VALE area.|382.4 +/- 3.0 Ma.|||Intrudes Adaminaby Group. Is unconformably overlain by Nowra Sandstone and Berry Siltstone.|Includes fine- to medium-grained, melanocratic clinopyroxene-hornblende quartz diorite.|
75933|Tullyangela Granite|70661|4|Described|vii, viii, p6, p121-123, p245|Frasnian|Frasnian|Temporally associated with Grassy Gully Rhyolite Member. Named for Tullyangela Creek. Type locality mentioned. Outcrops as low convex boulders, pebble sized float and debris. Distribution, structure and geochemistry discussed briefly.|382.4 +/- 3 Ma (SHRIMP U-Pb)|||Intrudes Adaminaby Group, overlain by Nowra Sandstone, Berry Siltstone|Fine to medium grained, equigranular quartz diorite containing mafic and felsic phases. Thin veins of leucogranite occur throughout the mafic phases of this unit.|
75933|Tullyangela Granite|71303|5|Briefly described|map legend|Frasnian|Frasnian||||||Equigranular, fine- to medium-grained quartz diorite. Dark grey, mafic phase in a cross-cutting relationship with pink to orange, leucocratic phase.|
35106|Tulootaba Formation|23055|6|Mentioned|Fig13 p25, 26|||||||||17-APR-14
83662|Tumbarumba basalt|73581|6|Mentioned|p25|||Snowy Mountains Volcanic Province. Located around the Tumbarumba township.||||||
35264|Tumbi Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
77669|Tumblong Oolite|66498|6|Mentioned|p43|Lochkovian|Lochkovian|||||||
77669|Tumblong Oolite|68297|5|Briefly described|p175, 183, 192|Emsian|Lochkovian|NSW. Of Pickett et al. 1985. Includes thelodont scales resembling Turinia polita, typical of basal Lochkovian in Europe||||||
37428|Tumboramboro Granite complex|23214|5|Briefly described|p174|||Now included in the Wologorong Granite. Possibly misspelt - see also Tamberamboro Granodiorite and Tamboramboro Granite.||||||
25559|Tumut Pond serpentinite|37192|6|Mentioned|p3973|||||||||
83485|Tumut Serpentinites|73483|6|Mentioned|p407 Fig.1|||||||||
40937|Turallo Quartz Diorite|50234|5|Briefly described|Map Legend|Emsian|Pragian|Greenish grey, massive hornblende monzodiorite.||||||12-MAY-04
31645|Turallo Suite|42726|5|Briefly described|Map Legend||Carboniferous|||||||
31645|Turallo Suite|44093|5|Briefly described|p217 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||
25560|Turi Greywacke|34555|6|Mentioned|Table 4.2|||||||||
25560|Turi Greywacke|37987|6|Mentioned|p224|||||||||
25560|Turi Greywacke|43400|14|Not recorded|map opp.p.188|Early Carboniferous|Late Devonian|||||||
25560|Turi Greywacke|43406|14|Not recorded|p45,46|||||||||
77253|Turill seam""|68004|6|Mentioned|p220.|||Medium to high ash content. Potentially mineable coal suitable for domestic thermal market. See also reference to Turill Coal Member p61.||||||
76175|Turkey Creek Diatreme|66623|6|Mentioned|p233.|||||||||
79214|Turon Grits|68592|5|Briefly described|p1748|Late Devonian|Late Devonian|Watkins, in Pogson and Watkins, 1998. In the Bathurst 1:250 000 map area. A possible correlate of Cookbundoon Formation.||Unit in Lambie Group.||||
40239|Turon Head Tonalite|38823|6|Mentioned|p206|||||||||
38547|Turondale Formation, lower|24394|6|Mentioned|p172, p178|||Not intended as a formal name - see Turondale Formation.||||||
38551|Turondale Formation, middle|24394|6|Mentioned|p172|||Not intended as a formal name - see Turondale Formation.||||||
38548|Turondale Formation, upper|24394|6|Mentioned|p172, p177|||Not intended as a formal name - see Turondale Formation.||||||
38254|Turondale formation|23738|6|Mentioned|p252|||Informal name - see Turondale Formation.||||||
38254|Turondale formation|43494|6|Mentioned|p25|||Informal see Turondale Formation. Overlies Chesleigh Formation where the Cookman Formation is missing.||||||
26963|Tuross Head Granodiorite|32673|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early to Middle Devonian||||||15-FEB-05
26963|Tuross Head Granodiorite|35289|4|Described|p17|||||||||
26963|Tuross Head Granodiorite|36411|6|Mentioned|p270|||Refers Chalker & Bembrick 1977 for definition.||||||
26963|Tuross Head Granodiorite|40328|4|Described|p211|||||||||
26963|Tuross Head Granodiorite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moruya Igneous Complex. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
34460|Tuross Tonalite|22779|5|Briefly described|Table 1|||||||||
34460|Tuross Tonalite|24517|5|Briefly described|p48|||Of the Moruya Suite and Tuross Head pluton.||||||
82691|Tuting Suite|71628|6|Mentioned|p19-165||||||Tuting Monzogranite.|||
41246|Twelve Mile Creek Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Lithic arenite, shale rhyolite, limestone.||||||
79957|Twin Tanks Metamorphics|71251|6|Mentioned|p3|||Yowah-Cunnamulla area. Map symbol (Ett) implies Cambrian age inferred.||||||26-APR-18
79957|Twin Tanks Metamorphics|71864|6|Mentioned|p3|||||||||
79957|Twin Tanks Metamorphics|71965|5|Briefly described|p896,899,901-904,906,911,913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Can be observed as irregular domains of curved trends of low magnetic intensity. Spatially associated with Hungerford Granite, and may represent domains of country rock or remnants of the same metasedimentary protolith. Minimum age provided by Hungerford Granite, dated at 419.2+\-2.5 Ma (Cross et al., 2015).|419.5 +/- 2.5 (age of an intrusion)|||Intruded by Tinchelooka Diorite. Correlatable with Warratta Group, Tongo Formation, Thomson beds, Werewilka Formation and Nebine Metamorphics.|Gneiss, schist.|28-MAY-20
79957|Twin Tanks Metamorphics|72915|6|Mentioned|p5, p17|||Basement rock intersected by the Congararra 1 borehole match this lithology. May be intrinsically related to the Hungerford Granite. Map symbol suggests Cambrian age.|||||Mica schist, gneiss and minor granite|
83266|Two-Thirty Porphyry|73287|5|Briefly described|p663, p666 Fig.3, p667 Fig.4|Ordovician|Ordovician|See also Two-Thirty porphyry.|448.0+/-4.4 Ma|Two-Thirty intrusive complex|||Sparse to crystal-crowded porphyritic textures; subhedral K-feldspar rims euhedral plagioclase and forms clusters; disseminated mineralisation and minor pyrite veinlets.|
83263|Two-Thirty breccia|73287|5|Briefly described|p666 Fig.3, p670, p672, p676-677, 680|Llandovery|Llandovery|Dated molybdenite is coeval with the post-mineralisation Zero porphyry in Two-Thirty igneous complex, interpreted as product of a late hydrothermal overprint. Part of the breccia body is inferred to be offset by a fault. Location in text includes p669 Fig.7. See also Two-Thirty Breccia p666 Fig.3, p667 Fig.4, Two-Thirty breccia complex.|438.9+/-1.4 Ma Re-Os (Mo)||||Subvertical, dominantly polymict magmatic-hydrothermal breccia.|
37308|Tycannah Rhyodacite|24010|6|Mentioned|p381|||||||||
80790|Tyringham East granite|69639|4|Described|p3, p6, p8, p112-p117|Triassic|Triassic|New England Orogen. Informal name. Sample locality, petrography, and geochronology is described, U-Pb SHRIMP magmatic crystallisation age. I-type geochemistry. See also p124, p223-p224, p241.|236.5 +/- 1.6 Ma||||Mineralised, moderately altered, fine- to medium-grained dark-grey granodiorite with minor quartz-filled fractures.|06-MAR-19
80790|Tyringham East granite|71628|6|Mentioned|p17-51|||Informal name; Chisholm et al. (2014). Renamed and formalised as Tyringham East Granodiorite in this study.||||||
77254|Ukebung Member|68004|5|Briefly described|p137.|||Moderate-high prospectivity for kaolin.||Unit in Purlawaugh Formation.||||
31055|Ulladulla mudstone|43474|14|Not recorded|p57|||||||||
31055|Ulladulla mudstone|43477|14|Not recorded|p18||Permian|||||||
34246|Ullandra Granite|22685|6|Mentioned|p728|Silurian|Silurian|Age is Middle Silurian.||||||17-JAN-06
34498|Umberumberka-type granite|22771|6|Mentioned|p50|||||||||
83563|Unanderra Coal|73304|6|Mentioned|p74|||[Probably a variation of Unanderra Coal Member]. Sydney Basin, southern.||Illawarra Coal Measures||||
70049|Unanderra coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Pheasants Nest Formation (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
25567|Undercliff Falls Adamellite|35518|6|Mentioned|Table 2|||Caesium analysis. Misspelling of Undercliffe Falls Adamellite?||||||
25567|Undercliff Falls Adamellite|42378|6|Mentioned|Table 1 P11|||||||||
77775|Undercliff Falls Granite|67818|5|Briefly described|p131, Fig. 2|Middle Triassic|Middle Triassic|Northern New England region. U/Pb zircon SHRIMP age (Hughes, 1993).|245.4 Ma|||||
74787|Undercliffe Falls Granodiorite|61790|6|Mentioned|p315, p318, p319, p320, p321|||Not intended as a formal name, more of a petrology descriptor, phase of Undercliffe Falls Adamellite.||||||
74787|Undercliffe Falls Granodiorite|71628|6|Mentioned|p11-36; p16-19|||Sivell and Passmore (1999). Said in this study to be invalid.||||||
27920|Undercliffe Falls Porphyritic Adamellite|30787|6|Mentioned|p49|||Differentation index||||||
27920|Undercliffe Falls Porphyritic Adamellite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
27920|Undercliffe Falls Porphyritic Adamellite|33476|6|Mentioned|p59|||||||||
27920|Undercliffe Falls Porphyritic Adamellite|34423|3|Fully described|p292|||Petrography, chemical analysis p293.||||||22-NOV-07
27920|Undercliffe Falls Porphyritic Adamellite|71628|6|Mentioned|p11: 9, 36|||Phillips (1964). Renamed Undercliffe Falls Adamellite by Thomson (1973, 1976), including the similar Bungulla Porphyritic Adamellite. Stanthorpe-Liston area.||||||
74788|Undercliffe Falls Syenogranite|61790|6|Mentioned|p315|||Not intended as a formal name, more of a petrology descriptor.||||||
74788|Undercliffe Falls Syenogranite|71628|6|Mentioned|p11: 36|||Sivell and Passmore (1999). Said in this study to be invalid.||||||
37432|Undifferentiated Turondale & Waterbeach Formation|23214|3|Fully described|p191|Early Devonian|Early Devonian|Of the Crudine Group. Not a valid stratigraphic name.||||||
31652|Ungarie Suite|24233|6|Mentioned|p253 Fig.1|||Geological Province: Lachlan Orogen.||||||
31652|Ungarie Suite|24417|5|Briefly described|p3|Silurian|Silurian|||||||
31652|Ungarie Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31652|Ungarie Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
31652|Ungarie Suite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
31652|Ungarie Suite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|Includes: Cookaburragong Granodiorite, Currah Granite, Charcoal Tank Granite, Ungarie Granite.||||||13-JUL-04
31652|Ungarie Suite|70777|6|Mentioned|p52, p79|||Of Chappell et al., 1991 before being subsumed into the Koetong Suite of the Koetong Supersuite (Blevin, 2004; Colquhoun et al., 2005).||||||
31652|Ungarie Suite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
31652|Ungarie Suite|71069|6|Mentioned|p75|||||||||
74768|Ungarie Suite""|61964|5|Briefly described|p37|||Suite of Chappell et al (1991). Contained the "Bland Granite" (of Chappell et al 1991) which later became Ungarie and Yalgogrin Granites of the Koetong Suite. Ungarie Suite abandoned in favour of redefined Koetong Suite.||||||
37949|Upper Albite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
31371|Upper Bingara ophiolite|43560|6|Mentioned|p235|||Informal name. Variation on Bingara Melange?||||||
30907|Upper Blythesdale Sub-Group|43404|14|Not recorded|Table p11,20|Cretaceous|Jurassic|||||||
30850|Upper Burindi Group|43385|14|Not recorded|p176,177||Tournaisian|Ref.to Voisey 1952||||||
30850|Upper Burindi Group|43399|14|Not recorded|p189|||=Lower Kuttung Gp. Ref.to Voisey 1952,1958||||||
30850|Upper Burindi Group|48600|14|Not recorded|Plate 3|||||||||
30799|Upper Chesleigh Formation|23214|5|Briefly described|p150|||Informal Name.||||||
30799|Upper Chesleigh Formation|43344|14|Not recorded|p153|||||||||
30658|Upper Chocolate Shales""|43346|14|Not recorded|p2|||||||||
31166|Upper Clarence Beds|43491|14|Not recorded|pVIII/16,17||Triassic|||||||
35143|Upper Fern Valley Coal|23055|6|Mentioned|Fig4p11|||||||||
30734|Upper Hawkesbury Sandstone|43358|14|Not recorded|p48||Triassic|||||||
31979|Upper Hume Series|43857|6|Mentioned|p324||Late Silurian|||||||
31911|Upper Kuttung Glacials|43870|14|Not recorded|p158||Late Carboniferous|Geomagnetic readings.||||||
30848|Upper Kuttung Group|43385|14|Not recorded|p176,177||Late Carboniferous|||||||
30848|Upper Kuttung Group|43491|14|Not recorded|pVI/10|||||||||
30848|Upper Kuttung Group|44855|14|Not recorded|p18||Carboniferous|||||||
30848|Upper Kuttung Group|48600|14|Not recorded|Plate 3|||||||||
30849|Upper Kuttung beds|43385|14|Not recorded|p176||Late Carboniferous|||||||
30962|Upper Kuttung glacials|43439|14|Not recorded|p409||Late Carboniferous|||||||
29092|Upper Loxton Sand""|41511|6|Mentioned|p22|||||||||
30932|Upper Luton Formation|43417|4|Described|Map Legend|||||||||
30642|Upper Marine Series""|43316|14|Not recorded|p15|||||||||
30642|Upper Marine Series""|43317|14|Not recorded|p6|||||||||
30642|Upper Marine Series""|43346|14|Not recorded|p1|||||||||
30642|Upper Marine Series""|43879|14|Not recorded|p254||Permian|||||||
30642|Upper Marine Series""|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
34512|Upper Olney Formation""|22799|6|Mentioned|p32|||Of Brodie, 1993. Conformable with and laterally intercalated with the Geera Clay.||||||
37947|Upper Pelitic Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
78867|Upper Pilot coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Boolaroo Formation||||
29094|Upper Purlawaugh Formation|41290|6|Mentioned|p226|||||||||
34508|Upper Renmark Beds""|22799|6|Mentioned|p28|||Of Thornton (1974).||||||
34735|Upper Renmark Group|22893|6|Mentioned|p25 fig9|Tertiary|Tertiary|||||||
34735|Upper Renmark Group|67061|6|Mentioned|p554 Fig.10.|Miocene||Murray Basin.||||||
34514|Upper Renmark Group""|22799|6|Mentioned|p32|||Of Kellett (1989).||||||
35871|Upper Snake Cave Sandstone|23336|5|Briefly described|p15|||Informal - see Snake Cave Sandstone.||||||21-MAR-06
31222|Upper Trilobite Bed|43857|5|Briefly described|p324|||Of Mitchell (1886)||||||
31222|Upper Trilobite Bed|68592|6|Mentioned|p1885-6|||Former name for the upper part of the Elmside Formation.||||||
32538|Upper Trilobite Bed""|33117|6|Mentioned|p.84|||Siluro-Devonian?||||||
32538|Upper Trilobite Bed""|61120|6|Mentioned|p11.|Lochkovian|Lochkovian|Not a formal name. Source of Paciphacops latigenalis.||||||
30798|Upper Wianamatta Group|43344|14|Not recorded|p20|||||||||
25572|Upper Wianamatta Stage|34224|6|Mentioned|p33|||Refers David, T.W.E. (1950)||||||
33876|Upper Willyama Supergroup|73516|6|Mentioned|p2, p3 Fig.1|||Curnamona Province.||||Unconformably underlies Benagerie Volcanic Suite||
31254|Ural Range Complex|43511|14|Not recorded|p138|||Ref.to Conolly 1962||||||
26189|Uralba Beds|13995|5|Briefly described|p72|Ordovician|Ordovician|Northeast NSW. Tabulate coral species, described by Hall (1975), listed.||||||
26189|Uralba Beds|31216|2|Defined|p76|Ordovician|Ordovician|||||||
26189|Uralba Beds|33703|6|Mentioned|p207|||||||||
26189|Uralba Beds|35311|6|Mentioned|p207|||||||||
26189|Uralba Beds|39331|6|Mentioned|Table 10-1|||See also Fig.10-1||||||
26189|Uralba Beds|40127|6|Mentioned|p10|||||||||
26189|Uralba Beds|40136|5|Briefly described|p41|||||||||
80009|Uralba beds""|71091|5|Briefly described|p147, p164|Ordovician|Ordovician|E of Manilla. Obsolete; rocks now included in Glen Bell Formation (Vickery et al., 2010). Corals briefly described. Early-middle Katian.||||||
38355|Uralla (Plutonic) Suite|23812|6|Mentioned|p63|||Informal name - see Uralla Plutonic Suite.||||||
40261|Uralla Granitoid Suite|38905|6|Mentioned|p302 Fig.1|||Geological Province: New England Fold Belt||||||
40255|Uralla Plutonic Suite""|38842|6|Mentioned|p285|||Geological Province: New England Fold Belt||||||
69987|Uralla Suite granitoids|61773|6|Mentioned|p139|||Informal reference to granitoid rocks of the Uralla Plutonic Suite.||||||
83050|Uralla Suites|73202|6|Mentioned|p639 Fig.10|Early Triassic|Early Triassic|New England Orogen, southern. Felsic I-type granitoids. [Misspelling of Uralla Suite?]|ca 249 Ma|||||
68809|Uralla granites|24513|6|Mentioned|p10|||Informal reference to granites within the Uralla Supersuite.||||||
38333|Uralla suite|23763|6|Mentioned|p543|||Informal.  Geological Province: New England Fold Belt.||||||
81793|Uralla volcanics''|69323|5|Briefly described|p1,3,13-19.21,27,41,70-71|Lopingian|Lopingian|Geological province: New England Orogen. SHRIMP U-Pb zircon geochronology of GA 2120074 (crystal-rich rhyolitic ignimbrite) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 256+\-1.3 Ma. Sample details, SHRIMP analyses, zircon characteristics and geochronology results are discussed.|256+\-1.3 Ma (SHRIMP U-Pb; this study)|Unit of Wandsworth Volcanic Group.||Intruded by Khatoun Tonalite, Uralla Granodiorite, Wilhelmshohe Tonalite.||03-DEC-19
24056|Urambie Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Urambie Granodiorite.||||||
80050|Uringalla Granodiorite|70661|6|Mentioned|p6, 81|||Discontinued because it has been recognised as the northern extension of the Glenrock Granodiorite. Also referred to as the Uringalla Granite (p78)||||||21-SEP-17
24058|Urisino beds""|41012|3|Fully described|p143|||||||||
29097|Ursino Beds|41117|5|Briefly described|p436|||Misspelling of Urisino?||||||
78369|Utah Lake complex|69002|6|Mentioned|p9|||||||||
78368|Utah Lake plutonic complex|69002|6|Mentioned|p9, Map 1b|||Informal name. Includes a cluster of non-outcropping, non-magnetic granites in the southern half of the Wanaaring 1:100k map sheet and onto the northern  part of the Utah Lake map sheet. The only age for this complex is that of the Barrona granite (389 Ma, recalculated K-Ar; Richards and McDougall 1986).|||Includes the Barrona granite.|||
78368|Utah Lake plutonic complex|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen.?Low-magnetic intensity granites||||||
78368|Utah Lake plutonic complex|69043|6|Mentioned|p11|||Thomson Orogen.||||||
78368|Utah Lake plutonic complex|69541|6|Mentioned|p644 Fig.1(a)|||||||||
38985|Uuendoo Rhyolite|23861|6|Mentioned|p6 Tb. 1|Visean|Visean|Misspelt - see Yuendoo Rhyolite.  Geological Province: New England Orogen.||||||
27597|Vale Creek Volcanics|33742|6|Mentioned|p117|||Refers Edenborough (1967 unpub.)||||||
27597|Vale Creek Volcanics|42712|4|Described|8, Table 1 p14; p16|Early Devonian|Late Silurian|Within Campbells/Kildrummie Group.||||||
83966|Valery Adamellite|71628|6|Mentioned|p3-2|||Merged into the Glenifer Adamellite by Pogson and Hitchins (1973).||||||
39825|Vales Point seam|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Moon Island Beach Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
39825|Vales Point seam|62033|5|Briefly described|p25 (Table)|||Of Moon Island Beach Formation (Newcastle Coal Measures). Overlies Wallarah seam. Geological Province: Sydney Basin. Informal name.||||||14-MAR-07
81794|Valla Granite|69323|5|Briefly described|p71|Triassic|Triassic|Geological province: New England Orogen. Part of a flush of c. 230 Ma plutonic magmatism in the New England Orogen with 'Kindee Creek tonalite' and Yarrahappini Adamellite.|230.7+\-1.6 Ma|||Broadly coeval (and comagmatic?) with 'Kindee Creek tonalite' and Yarrahappini Adamellite.||
77883|Valley Tank Member|65759|6|Mentioned|p114 Fig.2|Emsian|Emsian|||||||
77883|Valley Tank Member|67870|5|Briefly described|p62|Devonian|Devonian|Darling Basin. Appears only as Valley Tank (braided).||Snake Cave Sandstone.||||
27921|Vaux Seam|29941|6|Mentioned|p14|||||||||
27921|Vaux Seam|42078|6|Mentioned|Table 1 P5|||||||||
27921|Vaux Seam|42182|6|Mentioned|p299|||||||||
27921|Vaux Seam|42648|5|Briefly described|p37|||||||||
29100|Vegetable Creek Volcanics|31749|6|Mentioned|Fig. 1|||||||||
29100|Vegetable Creek Volcanics|34288|6|Mentioned|p295|||Permian||||||
25577|Verulam Oolite|30074|6|Mentioned|p11|||||||||
25577|Verulam Oolite|32869|6|Mentioned|p169|||Mb. of Wootton Beds||||||
41663|Verulam Oolite Lens""|44244|6|Mentioned|p73|||Informal - see Verulam Oolite Member - now everywhere referred to the Verulam Oolite Member of the Wootton beds.||||||26-AUG-04
41665|Verulam Oolite Member (of the Wootton beds)|44244|5|Briefly described|p73|||Of Campbell and McKelvey (1972) modified from Engel 1966 after K.S.W. Campbell.  Term now used for the widespread oolite in the Barrington district as well as the Verulam Oolite Lens within the Lostock Sandstone Member of the Flagstaff Formation.||||||26-AUG-04
41664|Verulam Oolite Member of the Wootton beds|44244|5|Briefly described|p73, p128|||A term used for the widespread oolite in the Barrington district as well as the Verulam Oolite Lens within the Lostock Sandstone Member of the Flagstaff Formation.||||||
27599|Vickery Conglomerate|29870|6|Mentioned|Table 1|||||||||
27599|Vickery Conglomerate|30911|6|Mentioned|Map legend|Permian|Permian|||||||
27599|Vickery Conglomerate|31882|5|Briefly described|p245|||||||||
27599|Vickery Conglomerate|32671|6|Mentioned|Map legend|Permian|Permian|||||||
27599|Vickery Conglomerate|32944|6|Mentioned|Fig.2|||See also PP700-702. Perm. Nandewar Gp.||||||
27599|Vickery Conglomerate|34043|5|Briefly described|p449|||L.Perm.||||||
27599|Vickery Conglomerate|36570|6|Mentioned|p77|||||||||
27599|Vickery Conglomerate|36940|6|Mentioned|p129|||||||||
27599|Vickery Conglomerate|37094|6|Mentioned|p240|||||||||
27599|Vickery Conglomerate|39288|6|Mentioned|Fig. 3.3|||||||||
27599|Vickery Conglomerate|43409|14|Not recorded|Map Legend|||Now superseded by 'Vickery Beds'||||||
27599|Vickery Conglomerate|43429|14|Not recorded|Map Legend|||Absent from sheet area||||||
38236|Victorian Tunnel Coal|23717|5|Briefly described|p118 Fig. 2|||Misspelt - see Victoria Tunnel Coal.||||||
75991|Violet Hills Member|65382|4|Described|p714|Visean|Visean|Appears to be member of Yagon Siltstone. Age of 330.6 +/- 4.6 Ma given from Roberts et al., 1995.||||||
38458|Wabba granite|24133|6|Mentioned|p57|||Informal name.  Geologocal Province: Lachlan Fold Belt.||||||
23116|Wadbilliga Adamellite|22815|4|Described|p73,74|||||||||
23116|Wadbilliga Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bemboka Suite.||||||
26977|Wadbilliga Granite|42726|5|Briefly described|map legend|Early Devonian||128.  Of the Bemboka Suite (Bemboka Supersuite).||||||07-FEB-05
32684|Wagga Group|22508|6|Mentioned|p2||Late Ordovician|Lachlan Fold Belt||||||
32684|Wagga Group|22638|2|Defined|p16|Late Ordovician|Early Ordovician|New name. Unconformably overlain by the Walleroobie Volcanics.||||||08-APR-09
32684|Wagga Group|22685|5|Briefly described|Fig1p729||Ordovician|Siltstone, sandstone and quartz-mica schist.||||||17-JAN-06
32684|Wagga Group|22857|6|Mentioned|p132|||Rhyodacitic ignimbrites and tuffs, limestone lenses. Max. thickness: 3.5km. Geological Province: Canberra-Yass Shelf. ||||||
32684|Wagga Group|23245|6|Mentioned|p132|||||||||
32684|Wagga Group|24007|5|Briefly described|p325|Ordovician|Ordovician|||||||
32684|Wagga Group|24037|6|Mentioned|p424 Fig.1|||Geological Province: Lachlan Fold Belt.||||||
32684|Wagga Group|24215|5|Briefly described|p805|||Geological Province:  Lachlan Fold Belt||||||
32684|Wagga Group|24233|5|Briefly described|p252, p253 Fig.1, p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
32684|Wagga Group|24417|3|Fully described|p9|Ordovician|Ordovician|Previously referred to as "Wagga Metamorphics".||||||
32684|Wagga Group|44192|5|Briefly described|Map Legend|Late Ordovician|Early Ordovician|||||||
32684|Wagga Group|50191|6|Mentioned|p4, 17|Silurian|Late Ordovician|||||||
32684|Wagga Group|50385|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
32684|Wagga Group|50554|5|Briefly described|Map legend|Ordovician|Ordovician|Quartzose sandstone, siltstone, chert, and shale.||||||
32684|Wagga Group|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Metasediments.||||||
32684|Wagga Group|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Includes: Clements Formation, Humbug Sandstone.||||||13-JUL-04
32684|Wagga Group|60902|5|Briefly described|p876|Early Ordovician|Early Ordovician|Overlain by the Bendoc Group. Geological Province: Girilambone-Wagga Terrane.||||||
32684|Wagga Group|61964|4|Described|p14 Fig. 4, p19, p137|Gisbornian|Lancefieldian|Incorporates former Tallebung Group. Orig. included Humbug Sandstone (now part of Clements Fm); Wagga Group also replaces Tallebung Group to north of CARGELLIGO sheet. Quartzose turbiditic sandstone + slate. Overlain by the Bendoc Group.Geophysics (p222).||||||08-APR-09
32684|Wagga Group|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Clements Formation with its two members: Milby Chert and Doongala Chert.||||||
32684|Wagga Group|63019|5|Briefly described|p920|Ordovician|Ordovician|In part formerly of the Tallebung Group. Strongly deformed. Unconformably overlain by Boothumble Formation. Geological Province: Lachlan Orogen.||||||23-JAN-07
32684|Wagga Group|63289|5|Briefly described|p364|Ordovician|Ordovician|Geological Province: Kiandra Volcanic Belt. Consists of quartz-rich sequences.||||||07-FEB-11
32684|Wagga Group|63290|6|Mentioned|p388, p399, p404|||Overlain by Bendoc Group.||||||28-JAN-09
32684|Wagga Group|63891|5|Briefly described|p237|Ordovician|Ordovician|Includes Clements Formation.||||||
32684|Wagga Group|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Clements Formation. Quartzose sandstone, siltstone, chert and shale; locally metamorphosed and phyllitic.||||||
32684|Wagga Group|64962|5|Briefly described|p202|Paleozoic|Paleozoic|Dominantly metasedimentary rocks.||||||08-APR-09
32684|Wagga Group|65469|5|Briefly described|p16, p18-p20, p43|Late Ordovician|Middle Ordovician|Lachlan Orogen. Deformed during the early Silurian Benambran Orogeny.  See also p52, p62, p133, p136, p328, p337, App A-VI 3.|||Includes the Clements Formation.|Overlain by the Bendoc Group. Intruded by the Koetong Suite.||
32684|Wagga Group|65890|6|Mentioned|p157 Fig.2|Ordovician|Ordovician|||||||
32684|Wagga Group|67060|6|Mentioned|p503. |||Includes Adaminaby Superterrane turbidites.||||||
32684|Wagga Group|67106|6|Mentioned|p681, 683|||||||||
32684|Wagga Group|67107|6|Mentioned|p686, 698||||||||Quartz-rich turbiditic sedimentary rocks.|
32684|Wagga Group|67322|4|Described|p4 Fig.2, p13-14, p18, p20, p39; Fig.5|Late Ordovician|Early Ordovician|Albury-Bega Terrane. Age determined from conodonts in chert horizons interbedded with sandstone. Described as Lower to Upper Ordovician on p18. Warren et al. (1995) introduced the term Wagga Group in the Cootamundra area; Hendrickx and Colquhoun noted that Warren et al's sequence 1 is in fact part of Bendoc Group. Now defined by Hendrickx and Colquhoun (in Colquhoun et al. 2005), the Wagga Group includes units cropping out NW of Condobolin that were previously included in the Tallebung Group by Trigg (1987). Occurs in the Cargelligo region.|||Clements Formation.|Overlain by the Bendoc Group.|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.|22-FEB-18
32684|Wagga Group|67803|5|Briefly described|p34|Ordovician|Ordovician|The Wagga and Girilambone Groups and western Adaminaby Group (with overlying shales) constitute the Girilambone-Wagga Terrane in the Wagga Basin. These are in situ deposits.|||||Includes cherts and black shales.|
32684|Wagga Group|67847|6|Mentioned|p21, p54|Middle Ordovician|Early Ordovician|Wagga Basin. ||||||
32684|Wagga Group|68466|5|Briefly described|p64-66|Late Ordovician|Early Ordovician|Albury-Bega Terrane.|||Clements Formation.||Predominantly quartz-rich turbidites. Cherts are comparatively rare.|
32684|Wagga Group|68592|6|Mentioned|p298, p307||||||Includes Clements Formation.|||
32684|Wagga Group|68822|6|Mentioned|p334|||||||||
32684|Wagga Group|69002|6|Mentioned|p13|||||||Overlain by the Bendock Group.||
32684|Wagga Group|69043|6|Mentioned|p50|Ordovician|Ordovician|||||Is overlain by Walleroobie Volcanics, presumably unconformably.||
32684|Wagga Group|69160|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Clements Formation.||Quartzose sandstone, siltstone, chert and shale; locally metamorphosed and phyllitic.|
32684|Wagga Group|69161|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Clements Formation.|Is in faulted contact with overlying Bootheragandra Group.|Quartzose sandstone, siltstone, chert and shale; locally metamorphosed and phyllitic.|
32684|Wagga Group|69162|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Clements Formation.|Is overlain unconformably by Bootheragandra Group.||
32684|Wagga Group|69163|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Clements Formation.|Is overlain unconformably by Bootheragandra Group.||
32684|Wagga Group|69164|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Clements Formation.|||
32684|Wagga Group|69540|5|Briefly described|p640||||||Includes Clements Formation.||Quartz-rich turbidites.|
32684|Wagga Group|69541|6|Mentioned|p652-653|Early Ordovician|Early Ordovician|Top of the Group is latest Darriwilian.||||Is overlain by Bendoc Group.||
32684|Wagga Group|69668|5|Briefly described|p927, p929 Fig.2, p931|Middle Ordovician|Early Ordovician|Albury-Bega terrane.|||Includes Clements Formation.|Shown as equivalent to Adaminaby Group, Girilambone Group.|Quartz-rich turbidites; minor chert.|12-JUN-20
32684|Wagga Group|69801|6|Mentioned|p18, p32, p39, p59, p65, p78, p110, p135|Ordovician|Ordovician|Central Lachlan Orogen. Formerly the Tallebung Group of Trigg (1987).||||Intruded by the Urambie Granodiorite, Collingullie Granite, Green Hills Granodiorite and the Nest Hill Granite.||
32684|Wagga Group|70178|6|Mentioned|p13||||||||Siliciclastic sediments.|
32684|Wagga Group|70684|6|Mentioned|p7 Fig.1, p13, p54|Ordovician|Ordovician||||||Turbidites.|
32684|Wagga Group|70718|5|Briefly described|p44|Late Ordovician|Early Ordovician|Wagga-Omeo Zone, Murray Basin.|||||Locally metamorphosed quartzose siltstone, sandstone, quartz-mica schist, pelite and chert, with minor quartzite, hornfels and graphitic schist.|
32684|Wagga Group|70751|5|Briefly described|p4-p6, p12, p15|Gisbornian|Lancefieldian|Age is derived from Colquhoun, Hendrickx & Meakin 2005. Deformed in the early Silurian by the Benambran Orogeny.|||||Turbiditic sedimentary rocks.|
32684|Wagga Group|70777|5|Briefly described|p16, p53, p60|Ordovician|Ordovician|||||Intruded by the Wargin, Yalgogrin and Buddigower  Granites.||
32684|Wagga Group|70941|6|Mentioned|p15|||Wagga Metamorphic Belt||||Correlated (tentatively) with the Girrilambone Group, correlated with the Pinnak Sandstone.||
32684|Wagga Group|70950|6|Mentioned|p1028-1029, 1046|Late Ordovician|Early Ordovician|Geological province: Central Lachlan Orogen. Turbiditic sedimentary rocks that form basement to the Lachlan Orogen|||Includes Eulendool Formation.|||
32684|Wagga Group|71039|6|Mentioned|p6, p28|Ordovician|Ordovician|||||||
32684|Wagga Group|71069|6|Mentioned|p52, p59, p72|||Central Lachlan Orogen.||||Equivalent to the Adaminaby Group. Conformably overlain by the Bendoc Group.||
32684|Wagga Group|71285|6|Mentioned|p552 Fig.9|||||||||
32684|Wagga Group|71693|5|Briefly described|Map legend; p2.|Ordovician|Ordovician|Turbiditic sedimentary sequence.|||Clements Formation.|Is overlain by Bendoc Group. Lateral equivalent of Girilambone Group.|Quartzose siltstone, sandstone, quartz-mica schist, pelite, chert, locally metamorphosed; minor quartzite, graphitic schist, hornfels.|
32684|Wagga Group|71700|5|Briefly described|p8, CD|Middle Ordovician|Early Ordovician||||Includes the Doongala Chert.|Equivalent to the Milby Chert Member of the Clements Formation.||
32684|Wagga Group|71889|5|Briefly described|p7-p17, p44, p58, p67-p68|||This group outcrops poorly and is generally covered by younger sediment; most outcrops are along road cuttings and in rare borrow pits;outcrop locations are provided. Hosts graptolite fossils which are the basis for including black shales from Narrandera in this group as opposed to the Bendoc Group. This unit is (in part) interpreted ass turbidite deposits.|||||Biotite schist, foliated feldspathic sandstone and black shales.|
32684|Wagga Group|72082|5|Briefly described|p4, p23, p33|Middle Ordovician|Middle Ordovician|Mud-rich turbiditic rocks. Confident but limited evidence for Darriwilian age.||||Is intruded by the Junee Reefs and Wantabadgery Granites.|Metasedimentary sequences.|
32684|Wagga Group|72083|5|Briefly described|p7-12, p18, p24, p26-27, p34 Fig.5|||See also p35, p53 Fig.8, p56. Poor outcrops: forms scattered exposure of cleaved basement rocks in the study area, typically obscured by soil-covered rolling rises.||||Is overlain unconformably by Square Head Formation and Walleroobie Volcanics. Is intruded by Moombooldool Granite.|Intercalated cleaved shales and variably micaceous and quartzose metasandstone; less typically, strongly folded grey-blue phyllite and schist (after black shale?) with intercalated fine-grained metasandstone beds.|31-AUG-19
32684|Wagga Group|72084|5|Briefly described|p2, p6 Fig.5a, p7-8, p23, p44-45|Ordovician|Ordovician|||||Is faulted against the Currawalla Shale. Is intruded by Wantabadgery, Collingullie and Ganmain Granites.|Metasedimentary sequence, including well-sorted quartzose metasandstone and metasiltstone.|
32684|Wagga Group|72296|5|Briefly described|p6, p9|Late Ordovician|Early Ordovician|Wagga Metamorphic Belt.|||Clements Formation.|Correlated with the Girilambone Group.||
32684|Wagga Group|72495|6|Mentioned|p217-218, p234, p236|Ordovician|Ordovician|Coincides in part with the south-western gravity high that is centered on 34degrees S.||||Faulted against the Gidginbung Volcanics and the Temora Volcanics.||24-MAR-20
32684|Wagga Group|72908|5|Briefly described|p3-5, p11, p28, p31|Gisbornian|Lancefieldian|Lachlan Orogen, central. Lancefieldian to early Gisbornian.|||Clements Formation||Turbiditic sedimentary rocks, contains black shale/carboniferous units, deformed and metamorphosed.|
32684|Wagga Group|73082|6|Mentioned|p30||||||||Metasediments.|
32684|Wagga Group|73140|6|Mentioned|p495|||Proposed to be incorporated into, and superseded by the Adaminaby Group.|||Clements Formation|||
32684|Wagga Group|73264|6|Mentioned|p1390 Fig.12|||Albury Bega Terrane, west. Shown as Wagga Gp.||||||
33989|Wagga Group Metasediments|22434|6|Mentioned|11 fig 14|Ordovician|Ordovician|Geological province: Lachlan Fold Belt.||||||28-JAN-09
34178|Wagga Metamorphics""|22638|6|Mentioned|p16|||Superseded by Wagga Group||||||24-AUG-04
34178|Wagga Metamorphics""|24417|6|Mentioned|p9|||Superseded by Wagga Group.||||||
28262|Wagga metamorphics|29907|6|Mentioned|p6|||||||||
28262|Wagga metamorphics|29910|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
28262|Wagga metamorphics|33004|6|Mentioned|p142|||||||||
28262|Wagga metamorphics|35070|6|Mentioned|p27|||See also P165.||||||
28262|Wagga metamorphics|35185|6|Mentioned|p227|||||||||
28262|Wagga metamorphics|35609|6|Mentioned|p59|||||||||
28262|Wagga metamorphics|41126|6|Mentioned|p24|||||||||
74769|Wagga metamorphics""|61964|6|Mentioned|p19|||Term used for rocks within the "Wagga Metamorphic Belt" (Scheiber 1976; Gilligan and Scheiber 1978). ||||||
38030|Wagga-Omeo Metamorphic Complex|24310|5|Briefly described|p1041|||Probably an informal name -see Omeo Metamorphic Complex.||||||28-JAN-09
38030|Wagga-Omeo Metamorphic Complex|60904|5|Briefly described|p775 Fig. 2, p793|||Composite name. Informal reference to Omeo Metamorphic Complex.||||||17-JAN-07
68696|Wagga-Omeo metamorphics|22857|5|Briefly described|p414 App.1 Tb.A1.5|Late Ordovician|Early Ordovician|Informal name. Includes the Wagga Group. Quartz-rich greywackes and arenites, siltstone, mudstone, black shale, minor chert. See also p412 App.1 Tb.A1.5. ||||||
68696|Wagga-Omeo metamorphics|44093|5|Briefly described|pp169-172|Ordovician|Ordovician|Informal name.  Metasediments. Geological Province: Lachlan Fold Belt.||||||25-JAN-06
80163|Wagonga Chert|70601|5|Briefly described|p53-54|||Could be laterally transitional with Warbisco Shale. Adaminaby and Bendoc Group sediments within the basin margin, emplaced thrust sheets of Wagonga Chert and deposited olistostromal deposits of the Bogolo Formation.||Wagonga Group|||Chert.|28-SEP-17
34569|Wagonga Formation""|22815|6|Mentioned|p15|||No longer in use.||||||
31199|Wagonga Series|43477|14|Not recorded|p11||Cambrian|Ref.to David||||||
31199|Wagonga Series|67322|6|Mentioned|p26|||Of Browne (1949). Renamed the Wagonga Group by Glen (1994).||||||22-FEB-18
25582|Wagonga Series""|35289|6|Mentioned|p10|||||||||
31198|Wagonga cherts|43477|14|Not recorded|p11||Cambrian|||||||
39652|Wahringa Limestone|24398|6|Mentioned|p265|Late Ordovician|Late Ordovician|Possibly misspelt (or abbreviation of) Wahringa Limestone Member?  Geological Province: Lachlan Fold Belt.||||||
38262|Wahringa Limestone member|23739|6|Mentioned|p212|||Informal name - see Wahringa Limestone Member||||||
38262|Wahringa Limestone member|72263|5|Briefly described|p516-518|Middle Ordovician|Middle Ordovician|Geological province: Lachlan Orogen. Autochthonous limestone unit within the Fairbridge Volcanics.||Unit of Fairbridge Volcanics.||||
39653|Wahringa Member|24398|6|Mentioned|p259|||Abbreviation of Wahringa Limestone Member?  Geological Province: Lachlan Fold Belt.||||||
69675|Walcha Province Volcanics|61155|5|Briefly described|p19|Middle Eocene|Early Eocene|Overlain by Doughboy Province Volcanics. In the Kempsey area.||||||
69975|Walcha suite|61794|6|Mentioned|p360|||Informal name.||||||
29105|Wallace Shale Formation|35258|6|Mentioned|p109|||||||||
39814|Wallace Shale boulder bed|24249|6|Mentioned|p93|||Informal name - see Wallace Shale||||||
23123|Wallagaraugh Adamellite|22815|4|Described|p70|||||||||
23123|Wallagaraugh Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Wallagaraugh Suite.||||||
70004|Wallanbah formation|61766|6|Mentioned|p68|||Informal - see Wallanbah Formation. Geological Province: Tamworth Belt.||||||
80791|Wallangara Volcanics|69639|5|Briefly described|p44, p62|Changhsingian|Changhsingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop. Intruded by the Sailor Jack Granite (magmatic crystallisation U-Pb SHRIMP age 253.1+/-1.5 Ma).|253 +/- 2.4 Ma (Cross et al, 2009)|Wandsworth Volcanic Group||Unconformably overlies the Texas Beds.||06-MAR-19
83576|Wallara Seam|73304|6|Mentioned|p75|||[Probably a misspelling and variation; see Wallarah coal seam].||||||
30997|Wallarah Tuff|43448|14|Not recorded|p235|||||||||
30998|Wallarah Volcanic Member|43448|14|Not recorded|p230|||||||||
35118|Wallarah coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam in the Moon Island Beach Formation (Newcastle Coal Measures).||||||
35118|Wallarah coal seam|23055|5|Briefly described|p32|||||||||
35118|Wallarah coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Moon Island Beach Formation||||
80048|Wallarawang Subgroup|70661|6|Mentioned|p187|||Not present in map area (Moss Vale)||Illawarra Coal Measures||||
35414|Wallareen Formation""|23170|6|Mentioned|p29|||of Lue Beds.||||||
30847|Wallarobba Beds|43385|14|Not recorded|p177 Table||Visean|Ref.to David & Sussmilch 1919||||||
30976|Wallarobba Conglomerate|43440|14|Not recorded|p66|||||||||
30976|Wallarobba Conglomerate|43447|14|Not recorded|Table 1,p9||Carboniferous|||||||
30976|Wallarobba Conglomerate|44833|14|Not recorded|p118|||See also Lexicon.||||||
30976|Wallarobba Conglomerate|44861|14|Not recorded|p227||Carboniferous|||||||
41666|Wallarobba Conglomerate""|44244|6|Mentioned|p82|||Superseded by Wallarobba Conglomerate Member.||||||
37454|Wallerawang Coal Measures|23214|6|Mentioned|p265|||Superseded by Illawarra Coal Measures.||||||
29106|Wallerawang Sub-Group|42182|6|Mentioned|Table 1|||||||||
25587|Walli Andesite""|39655|6|Mentioned|M1|||Now given group status||||||
30819|Walli Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
40375|Walli-Mount Pleasant Andesites|24334|5|Briefly described|p49 Tb.1|Arenig|Late Cambrian|Age: 470 - 495 Ma.||||||
34146|Wallibree Formation|22616|6|Mentioned|Fig.1 p670|Carboniferous|Devonian|||||||
34146|Wallibree Formation|22736|6|Mentioned|Fig.7 p628|Famennian|Famennian|Misspelling of Walibree Formation.||||||
34146|Wallibree Formation|44093|5|Briefly described|p67 Fig 6.6|Devonian|Devonian|Of the Southern Hastings Block. Geological Province: New England Fold Belt.||||||
26197|Wallingalair Group|22519|6|Mentioned|p3|||||||||
26197|Wallingalair Group|22768|6|Mentioned|p178|Emsian|Ludlow|||||||
26197|Wallingalair Group|22831|3|Fully described|p 63||Pragian|||||||
26197|Wallingalair Group|22857|5|Briefly described|p178, p448 App.1, Tb.A1.6|Early Devonian|Late Silurian|Geological Province: Bogan Gate Terrace.||||||
26197|Wallingalair Group|23522|5|Briefly described|p249 Fig 5|Emsian|Lochkovian|||||||
26197|Wallingalair Group|24417|5|Briefly described|p78|||Name superseded by Trundle Group||||||30-JUN-06
26197|Wallingalair Group|42489|5|Briefly described|Map legend|Emsian|Pridoli|||||||
26197|Wallingalair Group|42714|5|Briefly described|Fig.1 P25|Early Devonian||||||||
26197|Wallingalair Group|43441|4|Described|30|Middle Devonian|Early Devonian|||||||08-JAN-10
26197|Wallingalair Group|44093|5|Briefly described|p178 App. 1|Early Devonian|Silurian|In the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
26197|Wallingalair Group|44160|5|Briefly described|map legend|Emsian|Lochkovian|||||||08-JAN-10
26197|Wallingalair Group|46522|2|Defined|p60|Early Devonian||||||||
26197|Wallingalair Group|46524|5|Briefly described|p104|||||||||
26197|Wallingalair Group|46525|6|Mentioned|Fig.1 P143|||||||||
26197|Wallingalair Group|46528|5|Briefly described|Map legend|Early Devonian||||||||
26197|Wallingalair Group|62569|5|Briefly described|p606, p611|Early Devonian|Early Devonian|Originally grouped with Yarra Yarra Creek and Trundle Gps of Lochkovian-Emsian age by Talent et al (1997) - now interpreted as Givetian. Unconformable below Hervey Gp in east. Probably unconformable on Derriwong Gp. Geol.Prov: LFB. Fossil fish occurences.||||||10-AUG-07
26197|Wallingalair Group|63291|6|Mentioned|p419 Fig. 2|||||||||
26197|Wallingalair Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26197|Wallingalair Group|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
26197|Wallingalair Group|71040|5|Briefly described|p12 Fig.7, p25-26|Devonian|Devonian|Age has been reassessed from late Early Devonian to probable Late Devonian, based on fossil fish fauna from (only) one site; implications discussed.||||Is overlain unconformably by Hervey Group.||
38916|Wallingalair Group""|24417|6|Mentioned|p69|||Name became redundant after defintion of Derriwong and Trundle Groups.||||||
38918|Wallingalair beds""|24417|5|Briefly described|p73|||Previously included parts of the Yarrabandai Formation.||||||
38917|Wallingalair"" Group|24417|6|Mentioned|p69|||See "Wallingalair Group".||||||
29107|Wallingarah Formation|35095|3|Fully described|p110|||Variation of Wallingarah Creek?||||||
29107|Wallingarah Formation|37757|6|Mentioned|p29|||||||||
29107|Wallingarah Formation|37794|6|Mentioned|Table 1|||||||||
29107|Wallingarah Formation|38304|6|Mentioned|p83|||||||||
29107|Wallingarah Formation|43194|5|Briefly described|p96 Tb 8.1, p121|Middle Triassic|Early Triassic|Superseded name for the Napperby Formation in the Merriwa-Binnaway-Ballimore region of the Gunnedah Basin.||||||
29107|Wallingarah Formation|43494|6|Mentioned|p13|Jurassic|Jurassic|Of Loughnan and Evans (1978). Equivalent to Napperby Formation.||||||16-MAR-06
29107|Wallingarah Formation|61377|5|Briefly described|p152|Triassic|Triassic|Name for part of Napperby Fm to east of Coonamble Embayment; comprises Rivers Sst Mbr (lower) + Boothenba Sst Mbr (upper), separated by a significant undifferentiated middle section of sltst + sst. Overlain by Purlawaugh Fm. Geol.Prov: Surat Basin.||||||07-FEB-11
30974|Wallis Creek Sub-Group|43440|14|Not recorded|p35,fig.4-3|||Unit of Tomago Coal Measures||||||
70408|Walloon Coal Measures, upper|60999|5|Briefly described|p164|Middle Jurassic|Middle Jurassic|Informal name - see Walloon Coal Measures. Geological Province: Clarence-Moreton Basin.||||||11-DEC-07
31966|Walloon sandstones|43881|14|Not recorded|p41||Jurassic|Sandstones in Walloon Coal Measures.||||||
35214|Walls Creek Formation|22969|5|Briefly described|Fig 2.2||Permian|Possibly misspelt.||||||
29109|Walters Range group|42521|5|Briefly described|p15, Fig.1 p14|||Accidental variation on Walters Range Group?||||||
31227|Wandandian mudstone|43477|14|Not recorded|p18|||Ref.to David. Nowra. Marine Permian. U/lies Nowra grits and o/lies Conjola beds||||||
82696|Wandera Suite|71628|6|Mentioned|p19-167||||||Wandera Leucosyenogranite.|||
29807|Wandravandian Siltstone|43050|5|Briefly described|p6|||Misspelling of Wandrawandian Siltstone||||||
25592|Wandrawandian beds|36148|6|Mentioned|p274|||||||||
30869|Wandrawandian formation|43377|14|Not recorded|p143|||Formation of Shoalhaven Group||||||
31095|Wandrawandian siltstone|24079|6|Mentioned|p432|||Informal/misspelt - see Wandrawandian Siltstone.||||||
31095|Wandrawandian siltstone|43477|14|Not recorded|p19|||Unit of Shoalhaven Group. O/lain by Nowra sandstone.Marine Permian||||||
69989|Wandsworth Volcanic group|61773|5|Briefly described|p139 Fig.4|||Informal - see Wandsworth Volcanic Group.||||||
41074|Wandsworth Volcanics|24366|6|Mentioned|p19|||||||||
41074|Wandsworth Volcanics|69639|5|Briefly described|p133, p211|||||Wandsworth Volcanic Group||Intruded by the Llangothlin Monzogranite and Attunga Creek Monzogranite.||
41074|Wandsworth Volcanics|70217|5|Briefly described|p49, p60, p66|Late Permian|Late Permian|New England Orogen.|256-252 Ma|Wandsworth Volcanic Group||||
41074|Wandsworth Volcanics|70876|5|Briefly described|p2|||||||||
41074|Wandsworth Volcanics|71628|5|Briefly described|p8: 13, 25, 28; p10-9; p11-11; p15-67|||See also p19: 55, 77, 142. Superseded: see Wandsworth Volcanic Group. Hosts Sn mineralisation.|||Dundee Rhyodacite, Wallangarra Volcanics.|Is intruded by Glenreach, Gwydir River, Bungulla and Llangothlin Monzogranites.||
41074|Wandsworth Volcanics|73197|6|Mentioned|p476 Fig.7|Middle Triassic|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase.|~265-240 Ma||||Volcanics.|
24075|Wang Wauk Beds|36057|2|Defined|p342|Devonian|Devonian|Prob. Devonian||||||
24075|Wang Wauk Beds|39660|6|Mentioned|p450|||||||||
24075|Wang Wauk Beds|40883|6|Mentioned|Fig.2|||||||||
24075|Wang Wauk Beds|47056|6|Mentioned|Fig.2 P523|||||||||
24075|Wang Wauk Beds|50263|5|Briefly described|Map Legend|Late Devonian|Devonian|Underlies: Darts Creek Mudstone.  Geological Province: Eastern Myall Block.||||||
41595|Wang Wauk beds|22857|4|Described|p500 App.1 Tb.A1.7|Late Devonian|Late Devonian|Lithic arenite, siliceous siltstone, mudstone and minor quartzite. Max. thickness: 2200m.||||||
41595|Wang Wauk beds|44093|5|Briefly described|p231 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
41595|Wang Wauk beds|44244|4|Described|p196|Devonian|Devonian|Max. thickness: 2200m.  Conformably underlies the Darts Ceek Mudstone.  Geological Province: Myall Block.||||||16-AUG-04
41595|Wang Wauk beds|61766|5|Briefly described|p67|Early Carboniferous|Late Devonian|Upgraded to Wang Wauk Formation. Geological Province: Tamworth Belt||||||
70003|Wang Wauk formation|61766|6|Mentioned|p68|||Informal - see Wang Wauk Formation. Geological Province: Tamworth Belt.||||||
76044|Wanganella granodiorite|66934|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Jawbone Creek Granodiorite Suite.|||Biotite granodiorite, interpreted as an I-type granite.|
76044|Wanganella granodiorite|70718|4|Described|p60-p64, p69, 95, 120|Devonian|Ludlow|Age derived from Kemp and Carlton 2014. Intersected by drillhole Bundy No.1. Appears to intrude the Booroorban granite; however radiometric ages suggest that the Wanganella granodiorite is older than the Booroorban granodiorite, this could be resolved if it is found the units do not physically cut one another; alternatively emplacement of the Booroorban granite may have stoped surrounding sediments leaving the older Wanganella granodiorite in place.|421+/- 3 Ma (LAICPMS)|Jawbone Creek granodiorite suite||Intrudes the Yadabal Lagoon granite.||30-MAY-19
37301|Wanganui Andesite|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Of Clifden Formation.  Overlain by Eastons Arm Rhyolite.  Geological Province: New England Orogen.||||||
37301|Wanganui Andesite|24010|6|Mentioned|p381|Carboniferous|Carboniferous|Age: 319.2+/-2.8Ma.||||||
37301|Wanganui Andesite|24603|5|Briefly described|p868 Fig. 3|Namurian|Namurian|Of the Clifden Formation.  Age: 319.2+/-3.2Ma.  Geological Province: Tamworth Belt.||||||
37301|Wanganui Andesite|24605|6|Mentioned|p949 App.1|||Superseded by Wanganui Andesite Member||||||
37301|Wanganui Andesite|50613|5|Briefly described|p219|Namurian||Of the Clifden Formation.  Age: ~325Ma.||||||24-FEB-05
37301|Wanganui Andesite|61214|5|Briefly described|p172, p173|Namurian|Namurian|Of Clifden Formation. Age: 319.2+/-2.8Ma (SHRIMP). Geol.Prov: Boomi Block (present only in central and southern parts of area). Abbreviated member name in Fig. 2?||||||23-JAN-06
37301|Wanganui Andesite|61767|5|Briefly described|p78|Namurian|Namurian|Geological Province: Tamworth Belt.||||||
37301|Wanganui Andesite|68003|5|Briefly described|p137.|Carboniferous|Carboniferous|Tamworth Belt (North), New England Fold Belt.||Unit in Clifden Formation.|||Unwelded, dark grey, ignimbritic, pyroxene andesite.|
37301|Wanganui Andesite|68005|5|Briefly described|p144.|Carboniferous|Carboniferous|||Unit in Clifden Formation.|||Unwelded, dark grey, ignimbritic pyroxene andesite.|
24558|Wangrah Adamellite|23550|5|Briefly described|p504|||Subdivisions of the former Sapling Flat Igneous Complex. Superseded by Wangrah Granite.||||||11-FEB-08
24558|Wangrah Adamellite|36413|2|Defined|p101|Devonian|Devonian|||||||
24558|Wangrah Adamellite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Sapling Flat Igneous Complex. Biotite adamellite, texturally variable, minor marginal porphyries. GSNSW map code: gsw.||||||
24558|Wangrah Adamellite|39626|6|Mentioned|p276|||||||||
24558|Wangrah Adamellite|40328|4|Described|p211|||Also mentioned on P210||||||
42210|Wangrah granite|24456|6|Mentioned|p328, 329 Tb.1|||Informal reference to part of the Wangrah Suite.||||||26-NOV-04
25595|Wantabadgery Granodiorite|22606|6|Mentioned|P830|||||||||
25595|Wantabadgery Granodiorite|24119|5|Briefly described|p36|Silurian|Silurian|||||||
25595|Wantabadgery Granodiorite|41563|6|Mentioned|p513|||||||||
25595|Wantabadgery Granodiorite|68310|6|Mentioned|p240|||Wagga Batholith. Chemical analysis of schistose enclaves tabulated.|||||S-type granite.|
34191|Wantabadgery Granodiorite""|22638|6|Mentioned|p50|||Superseded by Wantabadgery Granite and Junee Reefs Granite||||||
36979|Wantabdery Granite|23721|5|Briefly described|Map Legend|Silurian|Silurian|Misspelt - Wantabadgery Granite.||||||
76176|Wara Karnu Group|66623|6|Mentioned|p209.|||Mis-print of Wana Karnu Group.||||||
31009|Waratah arenites|43448|14|Not recorded|p231|||||||||
31200|Waratah sandstone horizon|43477|14|Not recorded|p22|||Quote of Jones (unpubl.)||||||
75821|Waraweena volcanics|65756|6|Mentioned|p30, p31 Fig. 4|||Accidental informal name? from discussion of basaltic volcanic rocks found in drill intercepts in Waraweena area. No outcrop and geological relationships are unknown.||||||
78655|Warbisco Group|67322|5|Briefly described|p13|Late Ordovician|Late Ordovician|Widespread in the Albury-Bega Terrane of the Lachlan Orogen.|||||Includes black shale.|22-FEB-18
69993|Warbro beds|61771|5|Briefly described|p116|||See also Warbro Formation - probably used informally in text. Geological Province: Northern Hastings Terrane.||||||25-JAN-06
30851|Ward's River Conglomerate|43385|14|Not recorded|p179||Sakmarian|||||||
30851|Ward's River Conglomerate|43447|14|Not recorded|p28|||||||||
40256|Wards Mistake group|38842|5|Briefly described|p286|Early Triassic|Late Permian|Geological Province: New England Fold Belt. Age: 245 +/- 5Ma||||||
29506|Waree Creek Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Canangle Subgroup (Catombal Group). Fine-grained arenite and siltstone. Max. thickness: 185m. Geological Province: Hervey Basin.||||||
29437|Warina Sand""|42966|6|Mentioned|p91|||Same as Warina Sand.||||||
68790|Warina Sands|23884|6|Mentioned|p156 Fig. 13.3|||Geological Province: Murray Basin. Probably misspelt - see Warina Sand.||||||
30931|Warlands Creek Tuff Member|43417|4|Described|Map Legend||Late Carboniferous|||||||
30931|Warlands Creek Tuff Member|62095|6|Mentioned|p279 Appdx.|||Of Manser (1967, 1968). Superseded by Warlands Creek Volcanic Member.||||||31-JAN-08
76188|Warnu Kanu Group|66623|6|Mentioned|p206.|||Mis-print of Wana Karnu Group.||||||
78883|Waroo Limestone Member|65214|6|Mentioned|p272|Early Devonian|Early Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||Taemas Limestone||||19-MAY-14
31011|Warrabundah Ash|43461|14|Not recorded|Table p621||Siegenian|||||||
27252|Warraderry Porphyry|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|||||||
27252|Warraderry Porphyry|29910|6|Mentioned|Map legend|Devonian|Devonian|||||||
27252|Warraderry Porphyry|36411|6|Mentioned|p270|||Refers Bowman 1977.||||||
27252|Warraderry Porphyry|40328|4|Described|p212|||||||||
38938|Warraderry Porphyry""|24417|6|Mentioned|p112|||Superseded by Grenfell Granite.  Originally described, along with "Bogalong Granodiorite", to subdivide Grenfell Granite - but now abandoned.||||||
39385|Warraderry porphyry|24125|5|Briefly described|p87|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
37163|Warratra Formation|23522|5|Briefly described|p248 Fig 4|Emsian|Lochkovian|||||||
37163|Warratra Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Mudgee. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
37163|Warratra Formation|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4|Early Devonian|Early Devonian|||Queens Pinch Group||||
80801|Warratra Shale|71924|6|Mentioned|p3|||Has fauna similar to Rosedale Shale.||||||
23143|Warratta Sandstone Member|61312|6|Mentioned|p78|||Of the Cadna-owie Formation. May contain reservoir quality sands in NSW.||||||
23143|Warratta Sandstone Member|66623|6|Mentioned|p247.|||Morton (1982); approximate equivalent in Tibooburra-Milparinka area for Namur Sandstone. Obsolete term. See Warratta Group.||Unit in Gum Vale Formation.||||
78379|Warraweena volcanics|64681|4|Described|p1-23|||||||||
78379|Warraweena volcanics|68823|5|Briefly described|p380-381, p390-391, p394, p404-405|Ediacaran|Ediacaran|Burton et al. (2008). New name; informal? Suggested crystallisation from a magma derived from melting of mafic rocks in older continental crust: continental margin arc. Also in p376,378 Figs.3,4.|576.9 +/- 5.6 Ma, U-Pb zircon (Glen et al. 2013).||||Basalt, calc-alkaline andesite; locally pillowed.|23-JUL-15
78379|Warraweena volcanics|69002|5|Briefly described|p2, p3, p6, p12, Map 1b, Legend|Ediacaran|Cryogenian||~600-580 Ma, U-Pb||||Basaltic andesite flows.|
78379|Warraweena volcanics|69042|5|Briefly described|map legends|Ordovician|Neoproterozoic|WV. Thomson Orogen? Zone of linear magnetic anomalies. Basaltic andesite flows.||||||
78379|Warraweena volcanics|69540|5|Briefly described|p639-641|||Inferred age of 576 +/- 5.6 Ma (Glen et al., 2013) is called into question on the basis of the zircons used.|||||Basaltic to andesitic rocks.|
78379|Warraweena volcanics|69541|5|Briefly described|p644-649|Neoproterozoic|Neoproterozoic|Bourke arc. Zircon peak age.|577 Ma.|||||
78379|Warraweena volcanics|71360|5|Briefly described|Map legend|Paleozoic|Paleozoic|Geophysical signature: a narrow trend of moderate to high magnetic intensity with tight to isoclinal folding interpreted. Crystal-rich andesite/basaltic andesite as flows, tuffs and agglomerates form similar magnetic features on the Enngonia 1:250 000 map sheet, where this unit is more extensive along strike.|||||Amygdaloidal basalt grading to dolerite, carbonaceous, pyritic, intermediate to mafic crystal tuff.|
25601|Warrawoona"" Sandstone Member|37094|6|Mentioned|p242|||||||||
27253|Warree Creek Beds|32151|2|Defined|p215|Early Carboniferous|Early Carboniferous|See also p213 [Variation/misspelling of Waree Creek Shale of Conolly 1963 - from cards. CEBFeb95]||||||07-FEB-22
69679|Warrend Formation|61155|5|Briefly described|p19|Pleistocene|Late Pliocene|Overlies Come By Chance Formation; overlain by Walgett Formation. Age: 2.0-<1.0Ma. Thickness: 12m. In the Walgett area.||||||
30937|Warrigundi Complex|43418|14|Not recorded|Map Legend|||||||||
40471|Warrigundi Volcanic Complex|24603|6|Mentioned|p870|||Geological Province: Tamworth Belt.||||||
40471|Warrigundi Volcanic Complex|68004|6|Mentioned|p65.|||Werrie Basin. Viscous felsic lavas around the Piallaway and Mount Terrible volcanic centres. See also reference to Warrigundi Igneous Complex p117.||||||
30936|Warrigundi alkaline intrusives|43418|14|Not recorded|Map Legend|||||||||
27927|Warroo Limestone|24005|5|Briefly described|p293|Early Devonian|Early Devonian|Of Taemas Limestone. Geological Province: Lachlan Fold Belt||||||
27927|Warroo Limestone|24250|6|Mentioned|p110|||Abbreviation of Warroo Limestone Member||||||
27927|Warroo Limestone|30069|6|Mentioned|p12|||Map on P12||||||
27927|Warroo Limestone|30125|4|Described|p12|||See also P5-stratigraphy,P9 trilobite species,P13-98 description.||||||
27927|Warroo Limestone|33327|5|Briefly described|p173|||Unit of Taemas Fm. See also Fig.2.||||||
27927|Warroo Limestone|33481|6|Mentioned|p11|||||||||
27927|Warroo Limestone|35858|6|Mentioned|p209|||||||||
27927|Warroo Limestone|37012|6|Mentioned|p13|||||||||
27927|Warroo Limestone|38378|6|Mentioned|p152|||||||||
27927|Warroo Limestone|41773|5|Briefly described|p20|||||||||
27927|Warroo Limestone|42033|6|Mentioned|p656|||||||||
27927|Warroo Limestone|45078|6|Mentioned|p4|||See also P12,17-140 for brachiopod descriptions.||||||
27927|Warroo Limestone|47038|6|Mentioned|Fig.1|||||||||
27927|Warroo Limestone|50077|6|Mentioned|p19|||||||||
27927|Warroo Limestone|68592|6|Mentioned|p1031|||Of Browne (1959); the topmost unit in her Taemas Stage. When Offenberg (1974) raised the latter to Formation status, it became Warroo Limestone Member.||||||
39819|Warroo Limestone Member, lower|24250|6|Mentioned|p112|||Informal name - see Warro Limestone Member||||||
74785|Warroo Monzogranite|61789|4|Described|p304, p310|Early Triassic|Early Triassic|Small intrusions encompassed by Stanthorpe Adamellite. Strongly porphyritic biotite-hornblende monzogranite.||||||
74785|Warroo Monzogranite|61790|6|Mentioned|p318, p319, p321|||One of a group of hybrid monzogranite suites. ||||||
74785|Warroo Monzogranite|71628|6|Mentioned|p15-82; p19: 80, 87|||Sivell and Passmore (1999) after Passmore (unpublished, 1998). Mis-spelt as Waroo Monzogranite. Is included (this study) in the Karonstadt Complex as Warroo Monzogranite Phase.||||||
77263|Warrumbungle Igneous Complex|68004|6|Mentioned|p202.|||||||||
29122|Warrumbungle Volcanics|35045|6|Mentioned|p110|||||||||
29122|Warrumbungle Volcanics|43535|14|Not recorded|p134||Tertiary|||||||
29122|Warrumbungle Volcanics|60267|4|Described|p16-18|Middle Miocene|Middle Miocene|Composed of alkali basalt-hawaiite-mugearite magma, and mildly potassic trachyte magma.  Overlies the Pilliga Sandstone.||||||12-AUG-04
29122|Warrumbungle Volcanics|70036|5|Briefly described|Map legend|||Included in a mapped unit of Tertiary volcanic rocks: trachyte, basalt, nephelinite, syenite, rhyolite, monzonite and tuff.||||||
29122|Warrumbungle Volcanics|71890|4|Described|vi-vii, p1, p4-6, p8, p10|Langhian|Burdigalian|Formed by intermittent eruptions of lava flows, domes, pyroclastic material and emplacement of syn-volcanic intrusions. An older age compilation dated this unit as ranging from 17.4 to13.7 +/- 0.3 Ma (K-Ar, Vasconcelos et al, 2008). Subdivided into 20 informal unnamed units. Geomorphology is variable and units may exhibit columnar joints. Lithological description for multiple samples provided. See also p17-p19, p22-p24, p26-p27, p31-p34, p47-p52.|18 - 15.2 Ma +/- 0.3 (Ar-Ar, Cohen, 2007)||Includes the Chalk Mountain Formation.|Overlies the Garrawilla Volcanics. Disconformably overlies the Purlawaugh Formation.|Porphyritic to equigranular or aphantic coherent alkaline lithologies from basalt to rhyolite; subvolcanic intrusions; massive to weakly bedded pyroclastic deposits; polymictic volcaniclastic mudstone, sandstone, conglomerate and breccia.|
31323|Warrumbungle lavas|43534|14|Not recorded|p394||Miocene|U.Mioc. (about 13.5 my by K-A)||||||
41567|Warrumbungle trachytes|60267|6|Mentioned|p30|||Informal reference to the trachytes of the Warrumbungle Volcanics.||||||
41568|Warrumbungle volcano trachytes|60267|6|Mentioned|p25|||Informal reference to the trachytes of the Warrumbungle Volcanics.||||||12-AUG-04
29123|Watchbox Granite|35257|6|Mentioned|p99|||Variation of Watch Box?||||||
29737|Water Tower Formation|43032|5|Briefly described|Table 1,p8|||Rayner 1969||||||
38550|Waterbeach formation|24394|6|Mentioned|p172, 178|||Informal see Waterbeach Formation.  Maximum thickness: 512m.||||||
29124|Waterfall Creek Volcanics""|32999|6|Mentioned|p36|||Refers Jongsma (1968)||||||
23153|Watergums Adamellite|22815|4|Described|p95|Late Devonian|Late Devonian|||||||
23153|Watergums Adamellite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Gabo Suite.||||||
26989|Watergums Granite|23027|6|Mentioned|p51|||||||||
26989|Watergums Granite|23550|5|Briefly described|p505|||A-type granite.||||||
26989|Watergums Granite|42726|5|Briefly described|map legend|Middle Devonian||Reserved as Watergums Adamellite.||||||
26989|Watergums Granite|63605|5|Briefly described|p997|||Of the Gabo Suite. Age: 395+/-4Ma Pragian) which puts into dispute the accepted age of the complex (Eifelian to Givetian). Comagmatic with Boyd Volcanic Complex.||||||07-FEB-11
26989|Watergums Granite|71206|6|Mentioned|p373, 377-379|||Lachlan Fold Belt.|395 Ma.|Gabo Suite.|||Aluminous A-type granite.|
26989|Watergums Granite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. A-type.  Hf isotope data included.|388 Ma|||||
70655|Watermark Formation, Upper|61313|6|Mentioned|p105|||Informal name - see Watermark Formation. Delta-front facies.||||||
70653|Watermark Formation, lower|61313|5|Briefly described|p91, p105|||Informal - see Watermark Formation. Forms an intensely bioturbated upward fining sequence of sandy siltstone, dark grey siltstone and claystone; shallow marine facies.||||||
70654|Watermark Formation, upper|61313|6|Mentioned|p103|||Informal name - see Watermark Formation. Delta-front facies.||||||
37404|Wattle Creek boulder bed|23214|5|Briefly described|p131|Pridoli|Pridoli|Informal name. Of Wallace Shale.||||||
33940|Wattle Dale greisens|22490|5|Briefly described|9|||||||||
34385|Wauchope Limestone|22736|6|Mentioned|p625||Early Permian|See also Wauchope Formation p611.||||||
73727|Waugoola group|63290|6|Mentioned|p385|Llandovery|Llandovery|Informal: see Waugoola Group.||||||
30975|Wave Hill Conglomerate|43440|14|Not recorded|p49|||Unit of Newcastle Coal Measures.||||||19-DEC-06
30975|Wave Hill Conglomerate|43477|14|Not recorded|p21,53||Permian|||||||
82423|Wave Hill Tonalite|71628|4|Described|p9: 4, 12, 16-17, 19, 21-28, 30-31|||New name (this study), after a local station; emphasises the low-K nature of these rocks. Occurs ~5km W of Baryulgil. Outcrop is variable; scattered, highly weathered rubble to excellent. Lithologies detailed; geochemistry described.|249.7 Ma (Rb-Sr biotite; Shaw and Flood, 1993).|Dumbudgery Creek Complex.||Intrudes Silverwood Group. Abuts Gordonbrook Serpentinite and Yugilbar Gabbro.|Grey, medium-grained, speckled tonalitic rocks; grey, medium-grained, biotite-hornblende granodiorite; trondhjemite, leucotonalite, leucogranodiorite. I-type.|
35136|Wave Hill Tuff|23055|6|Mentioned|Fig4 p11|||||||||11-APR-14
33760|Waverly Creek Formation|24345|6|Mentioned|p87|||||||||
33760|Waverly Creek Formation|50129|4|Described|p15, p23, p24|Givetian|Givetian|Contains 2 members. Unconformably overlies the Snake Cave Sandstone. Overlain by the Ravendale Formation. Geological Province: Bancannia Trough, Darling Basin. See also Waverly Creek beds.||||||
33760|Waverly Creek Formation|61213|5|Briefly described|p318, p319 Fig. 3|Givetian|Givetian|Geological Province: Darling Basin.||||||
33760|Waverly Creek Formation|66623|6|Mentioned|p216.|||Defined by Neef (2004a), beneath Ravendale Formation. Not recognised in this redefinition of the Ravendale Formation.|||Included basal Rocky Tank Conglomerate Member and Ramparts Creek Sandstone Member.|||
33760|Waverly Creek Formation|67562|6|Mentioned|p97 Fig.4, p102|||Best developed W of Mootwingee Fault; rarely present to the E.|||Includes basal Rocky Tank Conglomerate Member and Ramparts Creek Sandstone Member.|Unconformably overlies Snake Cave Sandstone. Is overlain by Ravendale Formation.||23-JAN-17
36364|Waverly Creek beds|23469|5|Briefly described|p 322|Givetian|Eifelian|Of Mulga Downs Group.||||||
36364|Waverly Creek beds|24345|6|Mentioned|p94|Late Devonian|Middle Devonian|Geological Province: Wonominta Block.||||||
36364|Waverly Creek beds|50129|6|Mentioned|p23|||Of Neef & Bottrill 2001. See also Waverly Creek Formation||||||
35266|Webb Park Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
77326|Webbs Consols Granite|68005|6|Mentioned|p45 Fig.3-J, p64, pp68-70.|||Of the New England Batholith. Tamworth Belt. One of a group of highly fractionated leucogranites. Because they are hard to classify, Bryant et al. (2002) have tentatively reclassified this unit as part of the Uralla Supersuite. Perhaps see also reference to Webbs Consols Leucogranite, which appears suddenly in Appendix 4 (p134).||||||
77326|Webbs Consols Granite|68006|6|Mentioned|p128.|||||||||
35488|Weddin Formation|23217|5|Briefly described|p16, p17-8||Late Devonian|Of the Hervey Group.||||||07-MAR-06
35488|Weddin Formation|23392|2|Defined|p14||Famennian|Supersedes Weddin Sandstone, Mandagery Sandstone (in part) and Bumberry Formation (in part) and Eurow Formation (in part). Large fish fossil assemblage. Of the Hervey Group. Geological Province: Lachlan Fold Belt. Max Thickness: 1200m||||||
37110|Weddin Formation""|23392|6|Mentioned|p15|||||||||
37110|Weddin Formation""|24417|5|Briefly described|p144|||Superseded by Weddin Sandstone.||||||
31293|Weddin Range Limestone|43513|14|Not recorded|p90|||||||||
38961|Weddin Sandstone Members|24417|6|Mentioned|p149|||Not intended as a formal name - probably refers to Weddin Sandstone.||||||
72901|Weddin Sandstone""|62569|5|Briefly described|p607 Fig. 2|Late Devonian|Late Devonian|Within the Hervey Group of Conolly (1965, 1969). Informal - see Weddin Sandstone. ||||||
39380|Weddin sandstone|24125|5|Briefly described|p46|||Informal. - see Weddin Sandstone.  Of the Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
31310|Wee Jasper limestone|43529|14|Not recorded|p235|||(late Siegenian) Ref.to Brown 1959||||||
33396|Weebar Hill Leucitite|24417|3|Fully described|p151|Middle Miocene|Middle Miocene|Age: 12.9+/-0.4Ma.  Max. thickness: 110m.||||||
33396|Weebar Hill Leucitite|50554|5|Briefly described|Map legend|Tertiary|Tertiary|Olivine leucitite lava flows, scoria breccia.||||||21-JUN-04
33396|Weebar Hill Leucitite|60009|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
26992|Weedalion Granite|42726|5|Briefly described|map legend|Late Devonian||Misspelling and variation of Weedallion Granophyre?||||||
70625|Weekeroo group|62373|5|Briefly described|p515|||Informal group in the metabasite suite of the Curnamona Province - part of the Montstephen Metabasalt.||||||
38914|Weelah Formation""|24417|6|Mentioned|p66|||Informal - see Weelah Formation.||||||
34406|Weemala Formation|22704|5|Briefly described|p62|Early Ordovician||Overlies Coombing Formation. Also Fig6(b),p61||||||
34406|Weemala Formation|73154|5|Briefly described|p77 Fig.3|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Molong Volcanic Belt.||||Underlies Forest Reefs Volcanics.|Shale, conglomerate.|
73749|Weemala Volcanics|63293|6|Mentioned|p475|||||||||07-FEB-11
37224|Weemalla Beds|23214|6|Mentioned|p54|||Replaced by Weemalla Formation.||||||
37224|Weemalla Beds|60417|6|Mentioned|p174|||Informal. See Weemalla beds, Weemalla Formation.||||||
31392|Weemalla Beds""|43569|6|Mentioned|p480|||Informal||||||
67992|Weemalla beds|60417|6|Mentioned|p153|||Superseded by Weemalla Formation.||||||
67993|Weemalla beds""|60417|6|Mentioned|p156||Darriwilian|||||||
68971|Weerie Basalt|60292|5|Briefly described|p103|Early Permian|Late Carboniferous|Age: 300+/-8 Ma. Geological Province: Gunnedah Basin.||||||
35627|Weinteriga Creek beds|64169|5|Briefly described|p19, p20 Fig. 9|||Of the Palgamurtie Subgroup (Ponto Group). Overlain by Grasmere beds; underlain by Paddys Creek beds. Consist exclusively of of sandy phyllite. Geological Province: Koonenberry Belt.||||||20-MAY-08
35627|Weinteriga Creek beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group). Sequence occurs  between Grasmere beds and Paddys Creek beds. Psammitic phyllite sequence, largely non-magnetic.||||||26-NOV-08
35627|Weinteriga Creek beds|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Overlian by Grasmere beds, underlain by Bendee beds. Psammitic phyllite sequence, largely non-magnetic.||||||
35627|Weinteriga Creek beds|64682|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Of Palgamurtie Subgroup. Psammitic phyllite sequence, largely non-magnetic, between the Grasmere and Bendee subsequences.||||||27-NOV-08
35627|Weinteriga Creek beds|66623|6|Mentioned|p84.|||Formerly portion of Wonominta beds (Warris 1967), then renamed  Weinteriga Creek Formation (Buckley 2000). Redefined in this study.||Unit in Palgamurtie Subgroup.||||
35627|Weinteriga Creek beds|66929|5|Briefly described|Map legend|||||Unit in Palgamurtie Subgroup.||Overlies Bendee beds. Is overlain by Grasmere beds.|Psammitic phyllite sequence, largely non-magnetic.|
80046|Weirimunga Quartz Monzonite|70661|6|Mentioned|p125|||Of Kaag (1991) and Chown (1992) , both BSc hons theses (unpub.). Superseded by Touga Granite.||||||21-SEP-17
38317|Weismantels seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Dewrang Group in the Gloucester Basin coal sequence.   Geological Province: New England Fold Belt||||||
74770|Weja Hill Leucitite""|61964|5|Briefly described|p145|||Of Scott (2000b). An outlier of main body of leucitite originally called "Lake Cudgelligo Leucite Basalt" (Stonier 1894) - incl. with the latter and renamed Tullibigeal Leucitite.Source of hard-rock aggregate.||||||
35765|Welcome Volcanics|23859|5|Briefly described|p931 Fig 3|||See Welcome Volcanic Member. Of Emmaville Volcanics. Geological Province New England Fold Belt.||||||
70512|Well Gully Ignimbrite|62095|6|Mentioned|p260 Tb. 1|||Abbreviated version of Well Gully Ignimbrite Member. See also Well Gully Member.||||||
70513|Well Gully Member|62095|5|Briefly described|p259 Fig. 10|Late Carboniferous|Late Carboniferous|Abbreviated version of Well Gully Ignimbrite Member.  Age: 305.7+/-2.7Ma. See also Well Gully Ignimbrite.||||||29-MAY-06
28175|Wellingrove Granodiorite|22490|5|Briefly described|4|Early Triassic|Late Permian|Parent Uralla Plutonic Suite Geol province New England Fold Belt||||||
28175|Wellingrove Granodiorite|23050|5|Briefly described|p17 Table 2||Triassic|of Uralla Plutonic Suite. Age: no dating, probably similar to Tingha Adamellite.||||||
28175|Wellingrove Granodiorite|23051|5|Briefly described|Map Legend|Early Triassic|Late Permian|of Uralla Plutonic Suite.||||||
28175|Wellingrove Granodiorite|23811|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Uralla Plutonic Suite.  Coarse-grained, porphyritic to equigranular hornblende-biotite granodiorite to monzonite.||||||20-DEC-04
28175|Wellingrove Granodiorite|23812|4|Described|p22 Tb.2, p69|||Of Uralla Plutonic Suite.  Probably Permo-Triassic in age.||||||
28175|Wellingrove Granodiorite|29988|6|Mentioned|Map legend|Permian|Permian|||||||
28175|Wellingrove Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28175|Wellingrove Granodiorite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Uralla Suite. Monzogranite/granodiorite.||||||20-JUL-04
28175|Wellingrove Granodiorite|62534|5|Briefly described|p11 (legend), p24|Early Triassic|Late Permian|Of the Uralla Supersuite. Hosted by Emmaville Volcanics. Magnetics/radiometrics discussed.||||||07-FEB-11
28175|Wellingrove Granodiorite|66660|6|Mentioned|p347|||Unit in Uralla Supersuite. Has high Zr content. geochemistry compared with Newholme Monzogranite.||||||07-OCT-15
28175|Wellingrove Granodiorite|70217|4|Described|v, p1 tbl 1.1, p38-p42, p44, p75, p87|Wuchiapingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from this volume. Intrudes volcanic rocks equivalent to the Wandsworth Volcanic Group. Petrography, zircon morphology and SHRIMP results discussed in detail.|256.1 +/- 1.4 Ma (SHRIMP U-Pb)|Llangothlin Suite|||Quartz monzonite consisting of approximately 35 percent plagioclase, 35 percent alkali feldspar, 15 percent amphibole and 10 percent quartz.|
28175|Wellingrove Granodiorite|71628|6|Mentioned|p8-16|||Pogson and Hitchins (1973). Named after the village of that name. Now the Wellingrove Monzogranite (this study).||||||
33941|Wellingrove limonite|22490|5|Briefly described|15|||||||||
33941|Wellingrove limonite|23812|6|Mentioned|p143|||Informal name.||||||
31264|Wellington Formation""|43512|14|Not recorded|p100-1,104||Late Devonian|Mapped only||||||
37321|Wellington Volcanics|23309|6|Mentioned|p171-177|||See also Wellington Volcanic Group.||||||
37321|Wellington Volcanics|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
37321|Wellington Volcanics|61161|6|Mentioned|p126, p125|||Former name of Wellington Volcanic Group and used interchangeably with it.||||||
37321|Wellington Volcanics|67847|6|Mentioned|p10 fig 2.3|Upper Devonian|Upper Devonian|||||||
37321|Wellington Volcanics|70629|6|Mentioned|p986|Late Devonian|Late Devonian|Melbourne Zone.||||||
32659|Wellwood Tuff Formation|46547|14|Not recorded|Not recorded|||||||||
25611|Weltie Sandstone|23097|5|Briefly described|p595|||||||||
25611|Weltie Sandstone|29621|6|Mentioned|Table 1|||||||||
25611|Weltie Sandstone|34449|6|Mentioned|p128|||||||||
25611|Weltie Sandstone|35287|6|Mentioned|p2|||||||||
25611|Weltie Sandstone|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
25611|Weltie Sandstone|39618|6|Mentioned|Table 1|||||||||
25611|Weltie Sandstone|43032|5|Briefly described|Table 1,p9|||Brunker (1969)||||||
25611|Weltie Sandstone|46032|14|Not recorded|p.413|Late Ordovician||Probably pre U.Ord.||||||
25611|Weltie Sandstone|70941|6|Mentioned|p12|||||||||
25611|Weltie Sandstone|72296|5|Briefly described|p6|||See p6 for the complicated evolution of this unit's name and relationships with the Girilambone Group.||||||
32243|Welumba Adamellite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah5||||||
32243|Welumba Adamellite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
29130|Wenhams Formation|41054|6|Mentioned|p153|||See also Fig.2. Misspelling of Wenham Formation?||||||
73663|Wenlock limestones|63278|6|Mentioned|p157|||Informal name. Of the Sofala Volcanics. Geological Provience: Rockley-Gulgong Volcanic Belt, LFB.||||||07-FEB-11
38471|Wentworth group|23309|5|Briefly described|p5 Fig. 1.3|Early Devonian|Silurian|Informal-see Wentworth Group.||||||
38471|Wentworth group|24133|5|Briefly described|p20 Fig. 8|Early Devonian|Silurian|Informal.  Geological Province: Lachlan Fold Belt.||||||
30820|Werrie Basalts|43384|14|Not recorded|Map Legend||Early Permian|||||||
30820|Werrie Basalts|43385|14|Not recorded|p179||Sakmarian|||||||
30820|Werrie Basalts|43407|14|Not recorded|Map Legend||Early Permian|(Provisional Edition)||||||
30820|Werrie Basalts|43408|14|Not recorded|Map Legend|||||||||
30820|Werrie Basalts|43409|14|Not recorded|Map Legend||Early Permian|||||||
30820|Werrie Basalts|43417|4|Described|Map Legend||Permian|||||||
30820|Werrie Basalts|43440|14|Not recorded|p82,91|||Equivalent to Dalwood Group||||||
30820|Werrie Basalts|43477|14|Not recorded|p28,29,31|||Equivalent to Gyarran Volcanics||||||
30820|Werrie Basalts|43491|14|Not recorded|pVII/54||Permian|||||||
30820|Werrie Basalts|44835|14|Not recorded|p46,53,Pl.1||Permian|||||||
30820|Werrie Basalts|48600|14|Not recorded|p6|||||||||
37848|Werrie Volcanics|24040|5|Briefly described|p475|Early Permian|Early Permian|These rocks form the Warrigundi Volcanic Centre.||||||13-NOV-08
37848|Werrie Volcanics|61801|6|Mentioned|p405|||Probably misspelt and should be Werrie Basalt.||||||
37848|Werrie Volcanics|68822|6|Mentioned|p338|||Beneath the Sydney Basin. Shows some relic supra-subduction zone component in the melt.||||||
69973|Werrie basalt|61801|6|Mentioned|p403 Fig.1|||Informal - see Werrie Basalt.||||||
40226|Werrie volcanics|38681|6|Mentioned|p35|||Geological Province: New England Fold Belt||||||
80257|Werrikimbe Volcanic Complex|70939|5|Briefly described|p826|Triassic|Triassic|Northern Hastings Block.|226 +/- 3 Ma.|||||
68987|Werriko Limestone|60299|5|Briefly described|p228 Tb.5|Pliocene|Pliocene|Age: ~3 Ma. Palaeopole position given.||||||
68987|Werriko Limestone|67061|6|Mentioned|p554 Fig.10.|Pleistocene|Pliocene|Otway Basin.||||Overlies Whalers Bluff Formation.||
29445|Werrikooian Series|42966|6|Mentioned|p155|||Synonym of undifferentiated Loxton-Parilla Sands.||||||
70048|Wertago-Cootawundy Series""|22857|6|Mentioned|p436 App 1, Tb.A1.6|||Superseded by Mount Daubeny Formation.||||||
25613|Wesley Park Sandstone Member|38690|4|Described|p289|||Formerly Wesley Park Tuffs.||||||
35173|West Borehole seam|23055|6|Mentioned|Fig23 p37|||||||||17-APR-14
38988|West Lynee Rhyolite|23861|6|Mentioned|p6 Tb. 1|||Misspelt - see West Lynne Rhyolite.||||||
40589|West Lynne Andesite Tuff|24605|6|Mentioned|p948 App.1|||Superseded by West Lynne Rhyodacite Member.||||||
40589|West Lynne Andesite Tuff|68005|6|Mentioned|p146.|Carboniferous|Carboniferous|||Unit in Caroda Formation.||||
37296|West Lynne Rhyodacite|24010|5|Briefly described|p379|||||||||
37296|West Lynne Rhyodacite|24603|6|Mentioned|p871|||Geological Province: Tamworth Belt.||||||
37296|West Lynne Rhyodacite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|||||||
38980|West Lynne Rhyolite|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Of Caroda Formation.  Geological Province: New England Orogen.||||||
29534|West Lynne Serpentinite|23053|6|Mentioned|p21,75|||||||||
29534|West Lynne Serpentinite|43277|5|Briefly described|Map Legend||Late Ordovician|of Lachlan Fold Belt.||||||
29534|West Lynne Serpentinite|72296|1|Redefined|p18, p32, p36-38, p57, p59, p76|||Redefined here after Watkins and Meakin (1996). Named after Westlynn [sic] property and homestead. Type area is a 50m x 200m outcrop at Lat -31.4857 degrees Long 147.0322 degrees, ~17km NW of Nyngan. Associated with a narrow 10km-long NNW-trending linear magnetic anomaly, possibly the western limb of a fold structure (discussed); here the unit is assigned to the entire magnetic feature. Mostly subsurface. Origin uncertain; possibly a slice of original (seafloor) basement to the Girilambone Group. Associated with lateritic Ni-Co, Pt and Sc mineralisation.|||||Serpentinised dunite and harzburgite with augite and olivine, as well as magnetite from the serpentinisation of olivine, and later antigorite. High magnetic intensity.|
83567|West Wallarah Seam|73304|6|Mentioned|p68|||[Probably a variation of West Wallarah coal seam].||||||
83565|West Wallarah coal seam|73304|6|Mentioned|p66|||Local name used at Mandalong to define the seam formed by the westerly convergence of the Wallarah and Great Northern seams.||||overlies Awaba Tuff in Mandalong DDH 95.||
39375|West Wyalong granite|24125|5|Briefly described|p3|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
81787|Westella Granite|71345|6|Mentioned|p22|||Occurs west of, and is younger than Glenariff Granite.||||||02-DEC-19
81787|Westella Granite|72951|6|Mentioned|p1022|||Of Black (2007). Former name for Byrock Granite.|416.8+/-2.5 Ma|||||
26996|Westerley Leucogranite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
37456|Western Coal Measures|23214|6|Mentioned|p267|||Superseded by Illawarra Coal Measures.||||||
68872|Western Crystal Tuff""|60424|5|Briefly described|p355|||Now referred to as Western Volcanic Succession - not a formal name. Quartz-plagioclase-phyric volcanic rocks + quartz-chlorite-sericite +/- biotite schist.||||||
31456|Western Sands""|23050|5|Briefly described|p 82 Fig.17|Late Permian|Late Permian|of Black Jack Group, Gunnedah Basin||||||
31456|Western Sands""|43582|6|Mentioned|Fig.5,p16||Late Permian|||||||
31456|Western Sands""|61313|5|Briefly described|p98 Fig. G10|Late Permian|Late Permian|Informal name for a unit in Black Jack Group. Geological Province: Gunnedah Basin. See also p100.||||||
31456|Western Sands""|61377|5|Briefly described|p154 Fig. SU9|Late Permian|Late permian|Informal name for part of the Black Jack Group. Geological Province: Gunnedah Basins.||||||07-FEB-11
83486|Western Wambidgee Serpentinite Melange|73483|5|Briefly described|p407-409, p412-413, p415 Fig.5-6|Ordovician|Cambrian|Lachlan Orogen. Part of the Wambidgee Serpentinite Belt, but physically separate from the main WSB and located 7.2km west of Coolac. Mappable length of 3.8km and width of 1.1km. Comprises thrust slices of the Wambidgee Serpentinite Belt, Frampton Volcanics, Blowering Formation. U-Pb zircon age of 487+/-3 Ma dates oceanic crust formation in the serpentinite belt using a sample previously dated by Graham et al., (1996) to 398+/-19 Ma. Abbreviated to WWSM. See also p411 Fig.3.|487+/-3 Ma U-Pb zircon||||Imbricate thrust package containing metasedimentary rocks, metabasalts, metagabbros, and a large ultramafic component of serpentinite including plagiogranite within schistose serpentinite.|
25615|Westley Park Tuff Member|29900|6|Mentioned|p166|||||||||
25615|Westley Park Tuff Member|32945|6|Mentioned|p85|||Permian||||||
25615|Westley Park Tuff Member|34292|6|Mentioned|Table 2|||Permian. Gerringong Volc.||||||
25615|Westley Park Tuff Member|36220|6|Mentioned|p16|||See also Table 1.||||||
25615|Westley Park Tuff Member|43345|14|Not recorded|p3 Table 1||Permian|||||||
25615|Westley Park Tuff Member|43346|2|Defined|p5|||||||||
25615|Westley Park Tuff Member|43491|14|Not recorded|pVII/51||Permian|See also Lexicon||||||
31096|Westley Park tuff|43477|14|Not recorded|p41|||||||||
31211|Westley Park tuff member|43477|14|Not recorded|p19||Permian|Unit of Broughton tuff. (Gerringong Volcanics)||||||
70516|Wheelihans Gap Member|62095|5|Briefly described|p259 Fig. 10|Carboniferous|Carboniferous|Variation/abbreviation of Wheelihans Ignimbrite Member. See also the abbreviated Wheelihans Ignimbrite. Age: 327Ma.||||||31-JAN-08
70515|Wheelihans Ignimbrite|62095|6|Mentioned|p260 Tb. 1|||Variation/abbreviation of Wheelihans Ignimbrite Member. See also Wheelohans Gap Member. Age 327.4+/-3.7Ma.||||||31-JAN-08
31657|Wheeo Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
31657|Wheeo Suite|68592|6|Mentioned|p1354|||Chappell et al. (1991). The name Wheeo has prior usage: this unit is superseded and its plutons are attributed to the Burrawinda, Gunning and Hovells Suites.||||||
38846|Whinfell Chert Member|22857|5|Briefly described|p414 App. 1 Tb. A1.5|Gisbornian|Darriwillian|Of the Ballast Formation. Nodular and bedded cherts, shale and siltstone. Max. thickness: >40m. Geological Province: Canbelego Block. ||||||
38846|Whinfell Chert Member|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
38846|Whinfell Chert Member|67322|5|Briefly described|p19; Fig.5|Darriwilian|Darriwilian|Felton (1981). This unit, along with the Alandoon Chert, are correlatives of the thick persistent ribbon chert within the Ballast Formation. Occurs in the Canbelego (Sussex-Byrock) region.||Of the Ballast Formation.||||22-FEB-18
38846|Whinfell Chert Member|68466|5|Briefly described|p65-66|Middle Ordovician|Middle Ordovician|Hermidale Terrane.||Ballast Formation.||Correlates with Mugincoble Chert.|Thick persistent packages of ribbon chert tens of metres thick.|
38846|Whinfell Chert Member|69668|5|Briefly described|p929 Fig.2, p931|Middle Ordovician|Middle Ordovician|Hermidale terrane, central NSW.||Unit in Ballast Formation.|||Thick persistent packages of ribbon chert tens of metres thick.|
24098|Whipstick Adamellite|22815|4|Described|p81|||||||||
24098|Whipstick Adamellite|37772|6|Mentioned|Fig.6|||||||||
24098|Whipstick Adamellite|40269|6|Mentioned|Fig.6|||||||||
24098|Whipstick Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Whipstick Suite.||||||
70474|White Rocks Ignimbrite|62095|6|Mentioned|p260 Tb. 1|Late Carboniferous|Late Carboniferous|Abbreviated version of White Rocks Ignimbrite Member. Age: 315.3+/-3.5Ma.||||||30-MAY-06
70475|White Rocks Tuff Member|62095|6|Mentioned|p274 Appdx.|||Of Dawson (1988) and Davies (1988). Superseded by White Rocks Ignimbrite Member.||||||31-JAN-08
70475|White Rocks Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Tuff.|
70475|White Rocks Tuff Member|68005|6|Mentioned|pp139-140.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.||||
35041|Whitlow Gold Group|23050|4|Described|p62|||Formal name NOT intended.||||||
78366|Whittabrenah Shale|69001|6|Mentioned|p16|||(Morton 1982).||||Equivalent to the Bulldog Shale.||
26999|Why Worry Granite|42726|5|Briefly described|map legend|Early Devonian||126.  Of the Wologorong Suite (Bemboka Supersuite).  Formal name not intneded.  Reserved as Why Worry Tonalite.||||||08-FEB-05
42537|Whybro seam, Lower|24423|5|Briefly described|p270|Permian|Permian|Of Mount Leonard Formation. Contains megaspores descirbed here.||||||
31167|Wianamatta Formation""|43491|14|Not recorded|pVIII/15a||Triassic|See also Lexicon||||||
29141|Wianamatta Group sandstones|31296|6|Mentioned|p38|||||||||
72981|Wianamatta Group, lower|61315|6|Mentioned|p176|Middle Triassic|Middle Triassic|Informal - see Wianamatta Group. Contains the Ashfield Shale. ||||||
31168|Wianamatta stage|43491|14|Not recorded|pVIII/17||Triassic|||||||
31168|Wianamatta stage|44861|14|Not recorded|p233|||||||||
25623|Wiarborough Formation|22857|4|Described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Lambie Group. Polymictic to oligomictic conglomerates. Max. thickness: 400m. Geological Province: Lambie Basin.||||||
25623|Wiarborough Formation|22859|6|Mentioned|p217|||||||||
25623|Wiarborough Formation|32999|3|Fully described|p41|||Geol. map P41||||||
25623|Wiarborough Formation|34481|6|Mentioned|Map legend|Late Devonian|Late Devonian|Misspelling of Wiaborough Formation||||||
25623|Wiarborough Formation|35655|6|Mentioned|p209|||Stratigraphy. Misspelling of Wiaborough?||||||
25623|Wiarborough Formation|50234|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Lambie Group.  Purplish, lithic pebble to cobble conglomerate and coarse-grained , pebbly lithic-quartz sandstone. Overlain by and interbedded with Cookbundoon Formation.  Underlies: Tarlo Formation.  Also overlies: Strathaird Formation.||||||13-MAY-04
25623|Wiarborough Formation|63633|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Lambie Group. Red conglomerate, fluviatile conglomerate, pebbly sandstone, red siltstone, sandstone.||||||
25623|Wiarborough Formation|68592|6|Mentioned|p1722|||Of Scheibner (1973). Approximately equivalent to the Strathaird Formation but differentiated by a lack of marine fossils. The name is discontinued (reasons given) and replaced largely by Cowpers Creek Conglomerate.||||||
70105|Widdenbrook Conglomerate|61529|5|Briefly described|p854 Fig. 1b|Triassic|Triassic|Geological Province: Sydney Basin||||||17-FEB-06
34437|Widdin Brooks Conglomerate|22749|6|Mentioned|p 196|||||||||
29454|Widgelli Member""|42966|6|Mentioned|Table 30 p196|||Superseded by Widgelli Pedoderm.||||||
29453|Widgelli Parna""|42966|6|Mentioned|Table 30 p196|||Synonym of Widgelli Pedoderm.||||||
76135|Wilandra beds|63793|5|Briefly described|p18, p30.|||Davidson (1981). Correlated with Kara beds to the north. |||||Low-grade slates, quartz sandstones, dolomites, volcanics and pyritic siltstones.|
81168|Wilga Downs Metamorphics|72296|5|Briefly described|p9|||Longman and Meares (1971).||||Overlain unconformably by Currawynnia Formation. Equivalent to the Caro Schist.||
41075|Wilhemshohe Tonalite|24366|6|Mentioned|p18 Fig. 11|||||||||
78306|Wilkawilina Limestone|68735|5|Briefly described|p233 Fig.2|||Misspelt Wilkawillina Limestone: see references p233-234.||||||10-APR-17
80450|Wilkurra granite|70718|5|Briefly described|p66|Devonian|Silurian|SHRIMP ages are derived from Wilde, 2000. SHRIMP age is interpreted as the emplacement age of this granite. Emplacement associated with the Bowning Orogeny.|417 +/- 6 Ma, 423 +/- 6 Ma and 428+/- 15 Ma|||||
31409|Willawarra Dacite|62095|6|Mentioned|p280 Appdx.|||Of Lowe (1971). Superseded by Willawarra Rhyodacite of Kelk (1986) and now replaced by Willawarra Rhyodacite Member.||||||30-MAY-06
31409|Willawarra Dacite|68003|5|Briefly described|p135.|Carboniferous|Carboniferous|New England Fold Belt.|||||Rhyodacite.|
31409|Willawarra Dacite|68005|5|Briefly described|p141.|Stephanian|Namurian|||Unit in Currabubula Formation.|||Rhyodacite.|
70518|Willawarra Rhyodacite|62095|6|Mentioned|p280 Appdx.|||Of Kelk (1986). Superseded Willawarra Dacite of Lowe (1971). Now replaced by Willawarra Rhyodacite Member.||||||31-JAN-08
40987|Willdamar Granodiorite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Massive to foliated hornblende-biotite granodiorite.||||||12-MAY-04
40987|Willdamar Granodiorite|68592|6|Mentioned|p1664, p1672|Early Silurian|Early Silurian|Name used in the Bishopthorpe Suite chapter instead of Willdamar Tonalite (q.v. p1312-1314, p1316-1320, p1350-1353).||||Is intruded by Bishopthorpe Suite.||
78194|Williams Creek Granite|68822|6|Mentioned|p330|||SHRIMP zircon U-Pb (Black 2007. Geological Survey NSW Report 2007/298 unpublished)|515.1 +/- 2.7 Ma , SHRIMP zircon U-Pb (Black 2007)|||||
26217|Williamsdale Volcanics|32820|5|Briefly described|p5|||||||||
26217|Williamsdale Volcanics|36413|2|Defined|p45|Late Silurian|Late Silurian|||||||
26217|Williamsdale Volcanics|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Rhyodacitic tuff, massive. Includes unnamed minor rhyolitic intrusions (Swm). Interfingers with Colinton Volcanics. GSNSW map code: Sw.||||||
26217|Williamsdale Volcanics|39626|6|Mentioned|p276|||||||||
26217|Williamsdale Volcanics|40328|4|Described|p136|||||||||
26217|Williamsdale Volcanics|49690|6|Mentioned|p4-5, p7 |||Of Richardson (1979). Reduced to Member status (Williamsdale Dacite Member of Colinton Volcanics) in this Record.|||||A thick, massive, dacitic ashflow tuff.|
31853|Willona Granodiorite|45003|6|Mentioned|p56|||Misspelling of Willoona Granodiorite||||||
27005|Willoona Granodiorite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Foliated contaminated granodiorite. BMR map symbol: gmw.||||||
27005|Willoona Granodiorite|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
27005|Willoona Granodiorite|34544|6|Mentioned|p186|||||||||
27005|Willoona Granodiorite|40328|4|Described|p212|||||||||
31201|Willow Series|43477|14|Not recorded|p28,32,37||Permian|Ref.to Hanlon 1948. Equivalent to Gyarran Volcs. Lower stage correlative with Lower Marine Series.||||||
24108|Willowie Creek Beds|38755|4|Described|p66|||See also Fig.1.||||||
24108|Willowie Creek Beds|43745|6|Mentioned|Fig.4,p13|||||||||
77328|Willowie Diorite|62757|5|Briefly described|p14|Early Triassic|Early Triassic|Ashford area.  Age: 244.3+/-2.5Ma. See also "Willowrie diorite".||||||
77328|Willowie Diorite|68005|5|Briefly described|pp70-71, p136, p170.|Triassic|Triassic|Informal name: Brown (2003). Western margin of Bundarra Supersuite, SW of Ashford. Produces an intense magnetic high, indicating a plug-like structure. Pale green radiometric response, indicating moderate abundance with Th greater than K and U.||||||29-OCT-12
77328|Willowie Diorite|71628|6|Mentioned|p19-171|||Dawson et al. (2004) for a small mafic body SW of Ashford, within the Bundarra Supersuite. Name changed in this study to Willowrie Diorite.||||||
82705|Willowrie Creek Suite|71628|6|Mentioned|p19-171||||||Willowrie Diorite.|||
73107|Willowrie diorite""|62534|6|Mentioned|p6, p10 (legend)|Triassic|Permian|Informal name for a diorite plug which is surrounded by a radial swarm of dykes. These dykes have intruded the Bundarra Supersuite and Texas beds. Geological Province:Central Block. See also p22.||||||07-FEB-11
73107|Willowrie diorite""|62757|5|Briefly described|p19 Appx.|Early Triassic|Early Triassic|Informal name for diorite body recognised by Brown (2006) in the Ashford area - hosted by the Bundarra Supersuite. See also Willowie Diorite.||||||29-OCT-12
32648|Willyama Gneisses|46595|14|Not recorded|p.283|||(H54-15,I54-3).||||||
76842|Willyama Group|66800|6|Mentioned|p928.|||Broken Hill Block. Laing (1990) proposed a temporal correlation between this unit and Etheridge Group and Maronan Supergroup; grouped into Diamantina Orogen on basis of broadly similar sedimentation, orogeny and cratonisation.||||||
76842|Willyama Group|69591|6|Mentioned|p67|||||||Correlated with Etheridge Group (QLD).||
76842|Willyama Group|72459|6|Mentioned|p115|||Isotopically and chemically viable source for S-type granites in the Olary Domain.||||||
39205|Willyama Group, Lower|23731|14|Not recorded|p17|||Informal.||||||
32106|Willyama Metamorphics|43964|14|Not recorded|p217|||||||||
32652|Willyama metamorphics|46595|14|Not recorded|Not recorded|||||||||
82800|Wilsons Creek Porphyrite|71628|6|Mentioned|p8: 65, 67|||Binns et al. (1967). Included in Terrible Vale Porphyritic Microtonalite of Flood (1971 unpublished). Subsequently the Manuka Farm Porphyritic Microtonalite (Chesnut et al., 1973).||||||
42219|Wilton Formation, Lower Shoreface|24313|5|Briefly described|p23|Early Permian|Early Permian|Informal reference to part of Wilton Formation. Geological Province: Sydney Basin. Underlies: Tongarra Coal.||||||30-NOV-04
38157|Wilton Formation, Upper|24342|6|Mentioned|p52|||Formal name not intended.  See Wilton Formation.||||||
27006|Winburn Granite (NSW)|33006|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
37446|Winburndale Member|23214|6|Mentioned|p241|||Now included in Slowmans Creek Conglomerate.||||||
37449|Winburndale Member""|23214|6|Mentioned|p242|||Informal. Now included in Slowmans Creek Conglomerate.||||||
26221|Windellama Limestone|5178|6|Mentioned|p106 Fig.1, p108-109|Lochkovian||||||||
26221|Windellama Limestone|13996|6|Mentioned|p130|Silurian|Silurian|Contains a small number of isolated occurrences of Pridoli-aged conodonts.||||||
26221|Windellama Limestone|22768|6|Mentioned|p179|||||||||
26221|Windellama Limestone|22857|5|Briefly described|p179, p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Superseded by Windellama Limestone Member. Of the Fernleigh Group. Max. thickness: 150m. Geological Province: Bindook Rise.||||||22-JAN-13
26221|Windellama Limestone|23522|5|Briefly described|p248 Fig 4|Pragian|Pridoli|||||||
26221|Windellama Limestone|30735|4|Described|p43|||||||||
26221|Windellama Limestone|30736|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
26221|Windellama Limestone|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
26221|Windellama Limestone|32068|3|Fully described|p33|||||||||
26221|Windellama Limestone|32623|2|Defined|p2|Early Devonian|Early Devonian|Superseded by RDEF as Windellama Limestone Member 84/24454.||||||
26221|Windellama Limestone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
26221|Windellama Limestone|33326|6|Mentioned|p442|||Fauna. Emsian.||||||
26221|Windellama Limestone|33434|6|Mentioned|p35|||||||||
26221|Windellama Limestone|37270|6|Mentioned|p198|||||||||
26221|Windellama Limestone|37727|6|Mentioned|p9|||||||||
26221|Windellama Limestone|39568|6|Mentioned|p77|||||||||
26221|Windellama Limestone|41804|6|Mentioned|p167|||||||||
26221|Windellama Limestone|42032|6|Mentioned|p485|||||||||
26221|Windellama Limestone|42033|6|Mentioned|p651|||||||||
26221|Windellama Limestone|50095|6|Mentioned|p129||Late Silurian|Contains Amydrotaxis sp. (conodont). NSW.||||||11-FEB-08
26221|Windellama Limestone|61859|5|Briefly described|p17-19|||Windellama district. Brachiopod species listed.|||||Richly fossiliferous, locally silicified limestone.|
26221|Windellama Limestone|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the  Bindook Group. Well-bedded fossiliferous limestone. A fossiliferous base passeds up into relatively poorly fossilferous dark grey, more massive limestone.||||||16-JUN-08
26221|Windellama Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Bungonia. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26221|Windellama Limestone|68297|5|Briefly described|p190|Lochkovian|Lochkovian|Includes Lochkovian vertebrate fossil fauna.||||||
26221|Windellama Limestone|68592|6|Mentioned|p231, p1093|||Source of first (black) marble to be quarried in NSW, at Brayton; also produced lime. Reduced to Member status (of Tangerang Formation) by Jones, Carr et al. (1984).||||||
26221|Windellama Limestone|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dktw. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot. [Should this be Windellama Limestone Member?]||Tangerang Formation||Erosional at base. Overlain by unnamed member near base of Tangerang Formation.|Well-bedded, fossiliferous limestone at the base passes up into poorly fossiliferous dark grey massive limestone.|
26221|Windellama Limestone|70542|5|Briefly described|Map Legend|Devonian|Devonian|[Should this be Windellama Limestone Member?]||Tangerang Formation|||Well-bedded, fossiliferous limestone at the base passes up into poorly fossiliferous dark grey massive limestone.|
26221|Windellama Limestone|73143|6|Mentioned|p8|||Contains conodonts, Caudicriodus postwoschmidti identified by Mawson (1986) and reassigned to Ca. woschmidti by Drygant (2010).||||||
70037|Windellama Limestone""|22857|6|Mentioned|ERRATA sheet for p482|||Informal - see Wildellama Limestone, superseded by Windellama Limestone Member.||||||
82801|Winders Hill Suite|71628|6|Mentioned|p19: 173||||||Winders Hill Granodiorite.|||
76045|Windouran Swamp granodiorite|66934|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Jawbone Creek Granodiorite Suite.|||Interpreted as an I-type, biotite granodiorite.|
76045|Windouran Swamp granodiorite|70718|5|Briefly described|p60-p64, p120|Ludlow|Ludlow|Hay and Deniliquin 1:250 000 sheet area. Informal name, interpreted from geophysics. Aeromag. character: Magnetically zoned with peak amplitude of approximately 110 nT. Anomaly is 5×12 km wide. Interpreted as I-type granite, similar to Wanganella granodiorite.

||Jawbone Creek granodiorite suite||Intrudes the Thalaka granite.||30-MAY-19
69153|Windover Quartz Monzodiorirte|60423|5|Briefly described|p372 Fig. 3|Early Devonian|Early Devonian|Age: ~417Ma (U-Pb). Of the Narraburra Complex. Geological Province: Lachlan Fold Belt.||||||
24113|Wingecarribee peat|36220|6|Mentioned|Table 33|||||||||
80049|Wingello Basalts|70661|6|Mentioned|p231|Cenozoic|Cenozoic|Of Woolnough (1910). Name no longer used.||||||21-SEP-17
33253|Winton Series|44414|14|Not recorded|p110|||Freshwater. Ref. to Dunstan's 1916||||||
33253|Winton Series|44432|14|Not recorded|p62-64,66,89||Cretaceous|||||||
33253|Winton Series|44861|14|Not recorded|p234,235,266|||||||||
33253|Winton Series|44877|14|Not recorded|p173||Cretaceous|||||||
33253|Winton Series|63979|5|Briefly described|p54|||Of Dunstan (1916). Dunstan considered that Winton Series overlay the Rolling Downs Formation (now Group). Also written as "Winton Series".||||||27-NOV-13
33253|Winton Series|69023|5|Briefly described|p105|||Of Dunstan (1916), for freshwater sediments with coal seams, in bores around Winton, Qld. Later Winton Formation (Whitehouse, 1955).||||||
80251|Wirrinya Suite|67847|5|Briefly described|p60 fig 3.3.4|Middle Devonian|Middle Devonian|A-type intrusive rocks. ||||||
39384|Wirrinya granite|24125|5|Briefly described|p87|||Informal name.  Geological Province: Lachlan Fold Belt.||||||
76179|Wittabrenna Shale|66623|6|Mentioned|p260.|||Informal name used by Morton (1982). Formerly Wittabrenna Beds and part of Oornoo Beds (Rose and Brunker 1969); subsequently Doncaster Member (Exon 1976 after Vine and Day 1965).||||||
70036|Wittabrenna beds|22857|6|Mentioned|p544 App.1 Tb.A1.12|||Around Tibooburra area, but known as Doncaster Member (Wallumbilla Formation, Rolling Downs Group) elsewhere. Mudstone. Geological Province: Eromanga Basin.||||||
34441|Wogarda Formation|22750|5|Briefly described|p 228||Early Devonian|Tamworth Group. Misspelling of Wogarda Argillite?||||||
31233|Wogardi Argillite|43479|14|Not recorded|p151||Early Devonian|||||||
25641|Wolgan seam|36058|6|Mentioned|p3|||||||||
25641|Wolgan seam|37093|4|Described|p234|||||||||
25641|Wolgan seam|40166|6|Mentioned|p348|||||||||
26227|Wollar Sandstone|22857|6|Mentioned|p315 Fig. 22.8|||||||||
26227|Wollar Sandstone|22865|6|Mentioned|Fig22.8p315|||||||||
26227|Wollar Sandstone|24126|5|Briefly described|p81|||||||||
26227|Wollar Sandstone|29870|4|Described|p13|||||||||
26227|Wollar Sandstone|30455|6|Mentioned|p4|||See also P10,12||||||
26227|Wollar Sandstone|30458|6|Mentioned|p21|||||||||
26227|Wollar Sandstone|30460|6|Mentioned|p4|||See also P12,13. Of Narrabeen Group||||||
26227|Wollar Sandstone|30466|6|Mentioned|p10|||Triassic age||||||
26227|Wollar Sandstone|30610|2|Defined|p325|Middle Triassic|Early Triassic|Lower to Middle Triassic.||||||
26227|Wollar Sandstone|31276|6|Mentioned|p144|||Microflora||||||
26227|Wollar Sandstone|31326|6|Mentioned|p35|||Triassic conglomerates||||||
26227|Wollar Sandstone|32136|6|Mentioned|p36|||Miospores||||||
26227|Wollar Sandstone|34254|6|Mentioned|p488|||Late Permian - Middle Triassic||||||
26227|Wollar Sandstone|35095|4|Described|p110|||||||||
26227|Wollar Sandstone|35901|6|Mentioned|p4|||||||||
26227|Wollar Sandstone|36899|6|Mentioned|p1092|||||||||
26227|Wollar Sandstone|37794|6|Mentioned|Table 1|||||||||
26227|Wollar Sandstone|38304|6|Mentioned|p84|||||||||
26227|Wollar Sandstone|38614|6|Mentioned|p11|||||||||
26227|Wollar Sandstone|39693|6|Mentioned|p17|||||||||
26227|Wollar Sandstone|41266|6|Mentioned|Fig.3|||||||||
26227|Wollar Sandstone|41290|6|Mentioned|p231|||||||||
26227|Wollar Sandstone|43017|5|Briefly described|Fig.1,p372|||||||||
26227|Wollar Sandstone|43194|5|Briefly described|p96 Tb 8.1, p116|Early Triassic|Early Triassic|Replaced by Digby Formation||||||
26227|Wollar Sandstone|43323|14|Not recorded|p61,62,65-69,71|||Suggested microflora equivalent to uppermost Narrabeen Gp.i.e. upper Scythian or lower Anisian.||||||
26227|Wollar Sandstone|43350|14|Not recorded|p 402|||See also Lexicon||||||
26227|Wollar Sandstone|43553|14|Not recorded|p297|||||||||
26227|Wollar Sandstone|43554|14|Not recorded|p29|||||||||
26227|Wollar Sandstone|43556|14|Not recorded|p350|||||||||
26227|Wollar Sandstone|46937|6|Mentioned|Fig.10|||||||||
26227|Wollar Sandstone|49010|6|Mentioned|Fig.4|||Gunnedah Basin||||||
26227|Wollar Sandstone|49011|6|Mentioned|Fig.3|||Gunnedah Basin||||||
26227|Wollar Sandstone|61377|5|Briefly described|p149 Fig. SU8|||Geological Province: Gunnedah Basin.||||||07-FEB-11
26227|Wollar Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Mullaley Sub-basin, Gunnedah Basin. See also reference to Wollar Sandstone Member (p42).||||Unconformably overlies Black Jack Formation. Is overlain by Napperby Formation.||
77160|Wollar Sandstone Member|68003|5|Briefly described|p42.|Triassic|Triassic|See also reference to Wollar Sandstone (p57 Fig.3-n).||Unit in Digby Formation.||||
77160|Wollar Sandstone Member|68004|5|Briefly described|p176.|Early Triassic|Early Triassic|Considered prospective for hydrocarbons. Has excellent reservoir properties.||Unit in Digby Formation.||||
39413|Wollar sandstone|24126|6|Mentioned|p278|||Informal - see Wollar Sandstone.||||||
31169|Wollarobba Conglomerates|43491|14|Not recorded|pVI/5,6||Carboniferous|Quote of Sussmilch 1935 p94. Part of Kuttung Series||||||
82802|Wollomombi Adamellite|71628|6|Mentioned|p3: 2, 13|||Of Hensel (1982). Appears to form part of the Abroi Granodiorite.||||||
82803|Wollomombi Granite|71628|6|Mentioned|p17: 32|||Kennedy (1965). Later the Round Mountain Adamellite of Binns (1966). Now Round Mountain Leucomonzogranite.||||||
82804|Wollomombi Monzogranite|71628|6|Mentioned|p3: 3-4|||Included in the Hillgrove Supersuite by Chappell and Bryant (1994: unpublished). The author considers that this unit is unwarranted.||||||
31280|Wollongong Sandstone|43491|14|Not recorded|no card|||(no card)||||||
80051|Wollumbi Formation|70661|6|Mentioned|p7|Ordovician|Ordovician|Of Pribyl (1986) BSc Hons (unpub.)||||||21-SEP-17
35760|Wollundi Mudstone|23859|5|Briefly described|p931 Fig 3|||See Wollundi Mudstone Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
25642|Wologorang Adamellite|41563|6|Mentioned|p509|||||||||
31464|Wologorong Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Bemboka Supersuite.  Contains the Wologorong Granite.||||||08-FEB-05
31464|Wologorong Suite|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||30-MAR-05
31464|Wologorong Suite|71069|6|Mentioned|p36|Early Devonian|Late Silurian|||Wologorong Supersuite||||
27620|Wologorong Tumboramboro Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|Silurian-Devonian||||||
35263|Wolstoncroft Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
73965|Wolumla Member|63605|5|Briefly described|p1004|||Part of the upper section of Merrimbula Group. Basal conglomerate unit.||||||07-FEB-11
30800|Wombeyan Marble|23275|6|Mentioned|p467, Fig14-7.5p470|||||||||
30800|Wombeyan Marble|43344|14|Not recorded|p32|||Probably a building stone term||||||
79221|Wombeyan Volcanics""|68592|6|Mentioned|p890|||Of Hansen (1979). Redefined as the Mares Forest Volcanics.||||||
34624|Wombin "Group"|22831|6|Mentioned|p 28|||||||||
34623|Wombin Group|22831|6|Mentioned|p 26|||||||||
39953|Wombin volcanics|24267|6|Mentioned|p1515|||Not intended as a formal name. Geological Province: Parkes-Narromine Belt||||||
74771|Womboyne Formation""|61964|6|Mentioned|p114|||Replaced "Mountain Creek Formation" of the Cocoparra Group, but not discussed further here. May be obsolete? ||||||
30735|Wondabyne sandstone|43358|14|Not recorded|p48,50||Triassic|(Hawkesbury Sandstone) slide||||||
27621|Wondalga Granite|29648|6|Mentioned|p13|||||||||
27621|Wondalga Granite|35257|6|Mentioned|p154|||||||||
27621|Wondalga Granite|37259|6|Mentioned|p5|||||||||
27621|Wondalga Granite|37544|6|Mentioned|Fig.10|||||||||
27621|Wondalga Granite|39331|6|Mentioned|p30|||Postdates schistosity||||||
27621|Wondalga Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27621|Wondalga Granite|40498|6|Mentioned|p368|||||||||
27621|Wondalga Granite|42726|5|Briefly described|map legend|Silurian||||||||
27621|Wondalga Granite|60086|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Maragle Bathylith (Batholith?).||||||07-NOV-08
27621|Wondalga Granite|67806|6|Mentioned|pp111-112|||I-type. Gold, located in shear systems in this unit, appears to post-date the intrusion by a significant time margin.||||||
82608|Wongalee Suite|71628|5|Briefly described|p8-113|||||Uralla Supersuite.|Wongalee Leucogranite.|||
78276|Wonominta Group|67562|6|Mentioned|p92, p102 Fig.8|Precambrian|Precambrian|Wonominta Group and Wonominta Beds both used in this article.||||||
70349|Woodenbong beds, upper|60993|6|Mentioned|p38|||Informal - see Woodenbong beds.||||||
29168|Woodland Seam|29941|6|Mentioned|p14|||||||||
76753|Woodlands Member (NSW)|32286|6|Mentioned|p50|||Refers Voisey & Williams (1964)||||||
77041|Woodlands Monzonite|71628|6|Mentioned|p13: 1; p19-12|||Reserved in ASUD by Blevin; but Woodlands Granite (Chappell et al., 1991) has priority. Now (this study) the Black Knob Monzogranite.||||||
82806|Woodlands Quartz Monzonite|71628|6|Mentioned|p13: 1; p19-12|||Hensel (unpublished, 1982), but Woodlands Granite (Chappell et al., 1991) has priority. Renamed in this study the Black Knob Monzogranite.||||||
30223|Woodlawn Group|24318|5|Briefly described|p20|Silurian|Silurian|||||||
30223|Woodlawn Group|43128|5|Briefly described|Fig.6,p476||Silurian|Misspelling of Woodlawn Volcanics?||||||
30223|Woodlawn Group|43157|6|Mentioned|p3|||||||||
83929|Woods monzonite|70278|6|Mentioned|p1611|||Associated with the Endeavour Cu-Au porphyry deposits in the Junee-Narromine volcanic belt.|439.1 +/- 4.5 Ma (SHRIMP; Butera et al., 2001).||||Microcrystalline to aphanitic, dark red K-feldspar and quartz monzonite pipe intrusion.|
70012|Woodsreef melange|61764|6|Mentioned|p46|||Informal - see Woodsreef Melange.||||||
70409|Woogaroo Subgroup""|60999|6|Mentioned|p173|||Informal - see Woogaroo Subgroup. ||||||
70361|Woogaroo sequence|60995|6|Mentioned|p54|||Informal reference to parts of the subgroup present on southwestern margin of the basin comprising basal Laytons Range Conglomerate overlain by inferred Raceview Formation equivalents ("Mill Creek Siltstone"). ||||||
70362|Wooli Road Formation|60995|5|Briefly described|p53 Fig. 4|||Replaced Mill Creek "Siltstone" of Ellice-Flint (1973) and itself now replaced by Laytons Range Conglomerate and Raceview Formation (Woogaroo Subgroup). Geological Province: Clarence-Moreton Basin.||||||
34468|Woolomin Association|22768|5|Briefly described|p181|||(Korsch 1977).||||||
34468|Woolomin Association|23245|6|Mentioned|p136|||||||||
34468|Woolomin Association|60937|6|Mentioned|p423 Fig. 2|||Geological Province: New England Fold Belt.||||||12-FEB-08
34468|Woolomin Association|61003|5|Briefly described|p224, p225|Carboniferous|Devonian|Informal name. Part of the Tablelands Complex of Korsch (1977).||||||
34468|Woolomin Association|63774|6|Mentioned|p1075, p1079, p1081, p1083, p1084|||Consists of red ribbon-bedded chert/jasper, basalt, dolerite and metabasalt with volcanic sandstone and argillite.||||||
34468|Woolomin Association|71628|5|Briefly described|p7-31; p18: 3, 8||||||Cascade Creek beds, Myra beds, Woolomin Formation.|Is intruded by Moonbi Monzogranite and Duncans Creek Trondhjemite.||
42341|Woolomin Association""|23720|5|Briefly described|Map legend|Devonian|Silurian|Includes the Myra beds.||||||
42341|Woolomin Association""|41348|5|Briefly described|Map legend|Early Paleozoic|Early Paleozoic|Includes: Cascade Creek beds, Myra beds, and Woolomin Formation.||||||07-NOV-08
42341|Woolomin Association""|44093|6|Mentioned|p59 Photo 2|||Informal name. Geological Province: New England Fold Belt.||||||
25650|Woolomin beds|37509|6|Mentioned|p504|||||||||
25650|Woolomin beds|37987|6|Mentioned|p231|||||||||
25650|Woolomin beds|43085|5|Briefly described|p41|||||||||
25650|Woolomin beds|43385|14|Not recorded|p171||Silurian|||||||
25650|Woolomin beds|43745|6|Mentioned|Fig.4,p13|||||||||
25650|Woolomin beds|60937|5|Briefly described|p424 Fig. 2|||||||||
25650|Woolomin beds|65398|6|Mentioned|p9|||Superseded term for the Woolomin Group.||||||
25650|Woolomin beds|71628|5|Briefly described|p4-38|||||||Is intruded by MacDonald River Monzogranite.|Cherts, jaspers, quartzites, conglomerates, greywackes, argillites, phyllites, spilites, limestones and volcanics.|
30801|Woolomin greywackes|43344|14|Not recorded|p99|||||||||
70417|Woolomin serpentinite|61003|6|Mentioned|p225|||Informal name. Found within the Woolomin Association.||||||
72956|Woolomol Limestone""|63118|6|Mentioned|p202|||Of Hill (1942).  Contains coral faunas.||||||
41711|Woolooma Formation, upper|44244|6|Mentioned|p64|||Informal - see Woolooma Formation.||||||
82805|Wooloomoombi Granodiorite|72313|6|Mentioned|p459 Table 2|||New England Orogen. S-type.  Hf isotope data included.|290 Ma|||||
27016|Woomagarma Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
27016|Woomagarma Granite|42726|5|Briefly described|map legend|Silurian||549.||||||
42223|Woonona Coal Measure|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Marrangaroo Conglomerate. Underlies: Basal Wilton Formation||||||
70047|Woonona coal seam|22857|6|Mentioned|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
73993|Worange Point Formation""|63605|5|Briefly described|p1000|||Informal - see Worange Point Formation. Term used by Glen and Lewis (1990) for a lower "sheet sandstone sequence", which was overlain by an upper "point bar sequence", the "Ben Boyd Formation". Together these now form the Worange Point Formation.||||||07-FEB-11
25652|Woronora Coal Member""|42787|6|Mentioned|p136|||||||||
40173|Wright Volcanics|24599|6|Mentioned|p495 Fig. 2|||||||||
41295|Wullwye Adamellite|60007|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Berridale Batholith.  Medium-grained, pink adamellite.||||||
28193|Wullwye Granite|42726|5|Briefly described|map legend|Silurian||Variation on Wullwye Granodiorite.||||||
77161|Wuuluman Plutonic Suite|68003|5|Briefly described|p17. |Carboniferous|Carboniferous|Lachlan Fold Belt. Post-tectonic granites.||||||
31454|Wuuluuman Suite|42726|5|Briefly described|Map legend||Carboniferous|Probable misspelling of Wuuluman.  Of the Bathurst Supersuite.  Contains the Wuuluuman Granite.||||||07-FEB-05
31454|Wuuluuman Suite|44093|5|Briefly described|p200 App. 1|Carboniferous|Carboniferous|Geological Province: Lachlan Fold Belt.||||||
27021|Wyalong Granite|24125|6|Mentioned|p63|||Geological Province: Lachlan Fold Belt.||||||
27021|Wyalong Granite|29907|6|Mentioned|p8|||||||||
27021|Wyalong Granite|29985|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27021|Wyalong Granite|43499|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
34194|Wyalong Granite""|22638|6|Mentioned|p54|||Superseded by Ungarie Granite||||||24-AUG-04
34194|Wyalong Granite""|24417|6|Mentioned|p52|||Now included in the "Ungarie Granite".||||||
34194|Wyalong Granite""|61964|5|Briefly described|p47|||Informally named extension of Ungarie Granite - name now superseded. ||||||
34195|Wyalong Granodiorite""|22638|6|Mentioned|p54|||Superseded by Ungarie Granite||||||24-AUG-04
34195|Wyalong Granodiorite""|24417|6|Mentioned|p52|||Now included in the "Ungarie Granite".||||||
37422|Wyangala Adamellite|23214|6|Mentioned|p159|||Replaced by Wyangala Granite.||||||
34292|Wyangala Adamellite""|22679|6|Mentioned|p 42|||||||||
35403|Wyangala Granodiorite|23214|6|Mentioned|p4 fig.2|||||||||
35403|Wyangala Granodiorite|23551|5|Briefly described|p491|||Of Wyangala Supersuite||||||
35403|Wyangala Granodiorite|43782|6|Mentioned|Map Diagram|Pridoli|Ludlow|of Wyangla Batholith. Probably misused - should be Wyangala Granite as referred to in Legend.||||||
29178|Wyangle Formation""|39331|4|Described|p36|||||||||
35357|Wyaralong limestone|23185|6|Mentioned|p157|||Equivalent of Moore Creek Limestone Member (Mawson and Talent 1994).||||||
82807|Wylie Creek Monzogranite Phase|71628|4|Described|p16: 2-3, 5, 9-10, 13, 20, 23-26, 28|||New name (this study); replaces the Cullendore Syenogranite of Chisholm et al. (2014). Named after a local homestead. Occurs 30 km NE of Stanthorpe. Not mapped: relationship with adjacent units is unknown. Has a distinct geophysical signature. Geochemistry described: is geochemically assigned to its own Suite; the Wylie Creek Suite.|246.9 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Cullendore Syenogranite.||Is overlain by Koreelah Conglomerate Member (Marburg Subgroup).|Pale pinkish grey or pale to dark grey, fine- to medium-grained, slightly-moderately porphyritic, leucocratic biotite K-feldspar-rich monzogranite-syenogranite.|
82808|Wylie Creek Suite|71628|5|Briefly described|p16-5|||One of two [sic] Suites to which the five 'Phases' of the Cullendore Syenogranite are assigned.||Cullendore Supersuite.||||
38234|Wylies Flat Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Pinegrove Formation.   Geological Province: Sydney Basin||||||
35443|Wylinga Formation""|23170|6|Mentioned|p82|||||||||
23272|Xmas Quartz Monzodiorite|23309|6|Mentioned|p447, Appendix 1|||G4, I-Type.||||||
23272|Xmas Quartz Monzodiorite|68116|6|Mentioned|Map 37.|||Code G450. Mentioned in the legend for Map 37 but does not appear on the map; nor in the Appendix.||||||
36120|Yabba granite|23454|5|Briefly described|p28|||||||||
36120|Yabba granite|24551|6|Mentioned|p232|||Of the Cooma Supersuite.||||||
36120|Yabba granite|64312|6|Mentioned|p437 Tb. 1|||Informal name - mentioned only as Yabba under a Victorian granites heading - barium content information.||||||
27025|Yackandandah Porphyritic Granite|23309|6|Mentioned|p447 Appendix 1|||Superseded by Yackandandah Granite.||||||
27025|Yackandandah Porphyritic Granite|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
77162|Yadbro Conglomerate|68003|5|Briefly described|p40.|Early Permian|Early Permian|[Mis-spelling of Yadboro Conglomerate].||Unit in Shoalhaven Group.||||
30520|Yahoo Peaks Composite Dome|23043|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
30520|Yahoo Peaks Composite Dome|23170|4|Described|p234|Middle Devonian|Middle Devonian|of Dulladerry Volcanics.||||||
38445|Yalmy group|23309|6|Mentioned|p93|||||||||
38445|Yalmy group|24133|5|Briefly described|p21|||Misspelt - see Yalmy Group.  Geological Province: Lachlan Fold Belt.||||||
38445|Yalmy group|60541|6|Mentioned|p16|||Informal - see Yalmy Group.||||||
38445|Yalmy group|60542|6|Mentioned|p17|Early Silurian|Early Silurian|Informal - see Yalmy Group.||||||
38445|Yalmy group|61161|6|Mentioned|p78|||Informal - see Yalmy Group.||||||
38445|Yalmy group|61163|6|Mentioned|p27|||Informal - see Yalmy Group.||||||
25659|Yalpunga Beds|29991|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
25659|Yalpunga Beds|34469|6|Mentioned|p107|||Table. See P117. Cretaceous||||||
25659|Yalpunga Beds|39211|6|Mentioned|Fig.7|||Correlation||||||
25659|Yalpunga Beds|43501|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition) Part of Rolling Downs Group||||||
25659|Yalpunga Beds|66623|6|Mentioned|p264, p266.|||Name replaced by Yalpunga beds. The lower half correlates with Allaru Mudstone; the upper half with Winton Formation.||||||
76180|Yalpunga Formation|66623|6|Mentioned|p264.|||Informal name used by Morton (1982). Correlates with Allaru Mudstone.||||||
70034|Yalpunga beds|22857|6|Mentioned|p552 App.1 Tb.A1.13|Cenomainian|Cenomainian|In the Tibooburra area, same rocks as Winton Formation?||||||
30659|Yalwal Stage|43346|14|Not recorded|p1|||See also Lexicon||||||
30659|Yalwal Stage|43491|14|Not recorded|pV/15||Late Devonian|||||||
30659|Yalwal Stage|43870|14|Not recorded|p326||Late Devonian|||||||
32027|Yalwal Stage Basalts|43870|14|Not recorded|p301||Late Devonian|Palaeomagnetic readings.||||||
31170|Yalwal freshwater bed|43491|14|Not recorded|pV/15||Late Devonian|||||||
23283|Yambulla Adamellite|22815|4|Described|p71|||||||||
23283|Yambulla Adamellite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Wallagaraugh Suite.||||||
31668|Yammatree Suite|42726|5|Briefly described|Map Legend|||||||||
31668|Yammatree Suite|44192|5|Briefly described|Map Legend|||||||||
31668|Yammatree Suite|69801|6|Mentioned|p52|||Eastern Lachlan Orogen.|||Includes the Yammatree Granite.|||
31159|Yancawinna Beds|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group||||||
31219|Yanco Glen Beds|43502|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group.||||||23-DEC-09
27028|Yancowinna Sub-Group|30261|4|Described|Table 1|||Sturtian age||||||
27028|Yancowinna Sub-Group|33004|6|Mentioned|p136|||||||||
27028|Yancowinna Sub-Group|34812|3|Fully described|p67|||||||||
27028|Yancowinna Sub-Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27028|Yancowinna Sub-Group|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
27028|Yancowinna Sub-Group|37931|6|Mentioned|p531|||||||||
35682|Yandenberry beds|64671|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Palgamurtie Subgroup (Ponto Group). Metasediment sequence with magnetic pelitic phyllites, non-magnetic psammitic and pelitic phyllits, minor cherty tuff, minor chlorite.||||||26-NOV-08
35682|Yandenberry beds|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Palgamurtie Subgroup. Metasediment sequence with magnetic pelitic phyllites, non-magnetic psammitic and pelitic phyllites, minor cherty tuff, minor dolerite.||||||
35682|Yandenberry beds|64687|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Palgamurtie Subgroup. Metasediment sequence with magnetic pelitic phyllites, non-magnetic psammitic and pelitic phyllites, minor cherty tuff, minor dolerite.||||||
35682|Yandenberry beds|66623|6|Mentioned|p93.|||Stevens et al. 2000. Included with Belah beds in this study's definition of the Yandenberry Formation.||||||
35682|Yandenberry beds|66929|5|Briefly described|Map legend|||||Unit in Palgamurtie Subgroup.|||Metasedimentary sequence with magnetic pelitic phyllites, non-magnetic psammitic and pelitic phyllites, minor cherty tuff, minor dolerite.|
73693|Yaranigh Limestone Member|63286|6|Mentioned|p308 Fig. 9|Eastonian|Gisbornian|Of the Fairbridge Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
39954|Yarimbah Chert Member|24267|4|Described|p1509||Early Ordovician|Parent: Nelungaloo Volcanics. Lies totally within the Nelungaloo Volcanics. Source of graptolites for dating. Geological Province: Parkes-Narromine Belt||||||
68819|Yarra Yarra Creek group|50077|6|Mentioned|p15|Early Devonian|Early Devonian|Informal name, or misspelt.||||||
81256|Yarra Yarra Group|72083|5|Briefly described|p36|Early Devonian|Early Devonian|Fossils indicate a stratigraphic break in the Lochkovian, consistent with the age of the Bindian Orogeny.||Cobar Supergroup.||Overlies Mineral Hill Volcanics and Talingaboolba Formation probably unconformably.||
27630|Yarrabin Adamellite|22815|4|Described|p45|Silurian|Silurian|||||||
27630|Yarrabin Adamellite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27630|Yarrabin Adamellite|36411|6|Mentioned|p270|||Refers White et al 1977 for definition.||||||
27630|Yarrabin Adamellite|40328|4|Described|p213|||||||||
27630|Yarrabin Adamellite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
27630|Yarrabin Adamellite|44092|5|Briefly described|map legend|Silurian|Silurian|gab12.||||||
27630|Yarrabin Adamellite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
26244|Yarrabin Granodiorite|35109|2|Defined|p63|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
81795|Yarrahappini Adamellite|69323|4|Described|p71|Triassic|Triassic|Geological province: New England Orogen. Part of a flush of c. 230 Ma plutonic magmatism in the New England Orogen with 'Kindee Creek tonalite' and Valla Granite.|228.4+\-1.7 Ma (Cross and Blevin 2013)|||Broadly coeval (and comagmatic?) with 'Kindee Creek tonalite' and Valla Granite.||
76067|Yarralumba Formation|66197|5|Briefly described|p631 Fig.3c||Ludlow|Canberra-Yass and Ngunawal Basins. Overlain by Laidlaw Volcanics. Underlain by Hawkins Volcanics. [misspelling of Yarralumla Fm].||||||13-MAR-12
34271|Yarraman Formation""|22679|6|Mentioned|p 29|||||||||
37178|Yarramanbully Limestone""|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Informal.||||||
35764|Yarramundi Andesite|23859|5|Briefly described|p931 Fig 3|||See Yarramundi Andesite Member. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
35764|Yarramundi Andesite|61793|4|Described|p341, p342 Fig. 1(b), p343 Tb. 1, p344-7|Late Permian|Late Permian|Of Emmaville Vols. Comfor. overlian by Dundee Rhyodacite Ignimbrite. Thick: 1750m. Geol P: New England Fold Belt. Consists of coherent lava, breccia, epiclasitc sandstones and ignimbrite facies. Interpreted to repersent a major andesitic stratovolcano.||||||07-FEB-11
37419|Yarran Cherts|23214|6|Mentioned|p154|||Now included in the Burgoon Formation.||||||
32826|Yarrangobilly Formation|48831|14|Not recorded|p.44,45,47-51|||||||||
30916|Yarrari Hill trachyte|43409|14|Not recorded|Map Legend|||See definition card||||||
68035|Yarrari Ignimbrite Member|50613|6|Mentioned|p230|||Probably misspelt - see Yarrari Pyroclastic Member.  Overlies Carramundra Member bed b.||||||
80258|Yarras Ophiolite|70939|6|Mentioned|p828|||||||||
75838|Yarras serpentinite|65317|5|Briefly described|p623-630, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Also referred to as Yarras complex. Located on western margin of Hastings Block, New England Orogen. Structures suggest Early Permian emplacement. Shown as Yarras Serpentinite in figs.||||||
33405|Yarrimbah Chert|63279|6|Mentioned|p167|||Name superseded by Yarrimbah Formation.||||||
33405|Yarrimbah Chert|67107|5|Briefly described|p688, 696|Early Ordovician|Early Ordovician|Peak Hill, c.45km N of Parkes. Appears as Yarimbah Formation on p688.||||Overlies Nelungaloo Volcanics.||
24640|Yarrimbah Chert Member|22831|3|Fully described|p 11|Early Ordovician|Early Ordovician|Nelungaloo Volcanics||||||
24640|Yarrimbah Chert Member|22857|4|Described|p416 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of the Nelungaloo Voclanics. Thinly bedded dark grey chert and laminated quartz siltstone with discontinuous basal conglomerate; contains graptolites. ||||||
24640|Yarrimbah Chert Member|23213|5|Briefly described|p23, Fig.10|Bendigonian|Lancefieldian|Age: Late Lancefieldian to Early Bendigonian. Oldest dated formation in the Junee-Narromine Volcanic Belt. Comparable to Hensleigh Siltstone. of Nelungaloo Volcanics.||||||
24640|Yarrimbah Chert Member|24125|5|Briefly described|p3|Ordovician|Ordovician|Of the Nelungaloo Volcanics.  Geological Province: Lachlan Fold Belt.||||||
24640|Yarrimbah Chert Member|40891|2|Defined|p4|Early Ordovician|Early Ordovician|Defn card held for Yarrimbah Chert.||||||
24640|Yarrimbah Chert Member|42262|6|Mentioned|p1817|||||||||
24640|Yarrimbah Chert Member|42489|5|Briefly described|Map legend|Bendigonian|Lancefieldian|||||||
24640|Yarrimbah Chert Member|42718|5|Briefly described|p1|||||||||
24640|Yarrimbah Chert Member|43441|4|Described|11, 21|Early Ordovician|Early Ordovician|||||||08-JAN-10
24640|Yarrimbah Chert Member|44160|5|Briefly described|Map Legend|Bendigonian|Lancefieldian|||||||08-JAN-10
24640|Yarrimbah Chert Member|46522|2|Defined|p14|Early Ordovician||||||||
24640|Yarrimbah Chert Member|46525|6|Mentioned|Fig.1 P143|||||||||
24640|Yarrimbah Chert Member|46528|5|Briefly described|Map legend|Ordovician||||||||
24640|Yarrimbah Chert Member|63286|6|Mentioned|p308 Fig. 9|Early Odrovician|Early Ordovician|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
38860|Yarrimbah Chert Member""|24417|5|Briefly described|p29|||Previously included as a member of the Nelungaloo Volcanics.  Now recognised as a separate unit overlying the Nelungaloo Volcanics and upgraded to formation status - see Yarrimbah Formation.||||||
72961|Yarrimbah Formation, lower|63121|5|Briefly described|p238|Early Ordovician|Early Ordovician|Informal - see Yarrimbah Formation. Contains allochthonous limestone clast with acrotretide brachiopods.||||||13-MAR-07
72959|Yarrimbah Formation, upper|63121|6|Mentioned|p226, p238|Bendigonian|Lancefieldian|||||||13-MAR-07
29188|Yarrow Creek Granite|35946|6|Mentioned|p29|||||||||
31912|Yarrowvitch basalt|43870|14|Not recorded|p90 Fig.5-10||Tertiary|||||||
27031|Yass Group|30069|6|Mentioned|p5|||||||||
27031|Yass Group|30332|6|Mentioned|Table 1|||Refers Link(1971). Will become Yass Subgroup of Douro Group||||||
27031|Yass Group|31852|5|Briefly described|p711|||U.Sil. See also P718-720, Figs. 1,2,4,5.||||||
27031|Yass Group|31918|5|Briefly described|p47|||Table 1.||||||
27031|Yass Group|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat nomenclature||||||
27031|Yass Group|33116|6|Mentioned|Fig.11|||Correlation||||||
27031|Yass Group|33325|5|Briefly described|Table 3|||||||||
27031|Yass Group|34692|6|Mentioned|p186|||||||||
27031|Yass Group|35070|6|Mentioned|p78|||||||||
27031|Yass Group|35386|6|Mentioned|p12|||Refers Link(1970)||||||
27031|Yass Group|37727|4|Described|p96|||See also P8.||||||
27031|Yass Group|37728|6|Mentioned|Table 4|||||||||
27031|Yass Group|39331|6|Mentioned|Fig.5-5|||||||||
27031|Yass Group|40328|6|Mentioned|Fig.16|||||||||
27031|Yass Group|42497|5|Briefly described|Map Legend|Wenlockian|Wenlockian|||||||
27031|Yass Group|43158|5|Briefly described|3||Late Silurian|Name now superseded by Yass Formation.  Age early Ludlovian.||||||
27031|Yass Group|43159|5|Briefly described|Fig.2p4,p6.|Ludlovian|Ludlovian|||||||
27031|Yass Group|45075|5|Briefly described|p5|||Fauna||||||
27031|Yass Group|45147|6|Mentioned|M123|||See also M154||||||
27031|Yass Group|68592|5|Briefly described|p429-430 Fig.89, p497-8, p503, p509|||Originally Yass Beds (Jenkins, 1879); later Yass Series (Brown, 1940), then Yass Member (of Douro Volcanics) by Brunker and Offenberg (1970). Next raised to Group [!] status by Link (1970, 1971), Link and Druce (1972); subsequently reduced to Sub-Group status by Pogson and Baker (1974), then to Formation status by Owen and Wyborn (1979).|||Included O'Briens Creek Sandstone and Cliftonwood Limestone.|Overlay Douro Volcanics. Was overlain by Hattons Corner Group.||
25668|Yass Group""|35386|6|Mentioned|p16|||Refers to Link(1970) now changed to Yass Sub-Group||||||
25668|Yass Group""|40328|6|Mentioned|p97|||See also P108||||||
31028|Yass beds|43470|14|Not recorded|p159||Wenlockian|See also Lexicon. Yass district. Early Wenlockian||||||
31028|Yass beds|43857|5|Briefly described|p318|||of Jenkins (1879). Same as Yass Series?||||||
31028|Yass beds|44861|14|Not recorded|p219,220|||||||||
40725|Yass formation|23309|6|Mentioned|p390|||||||||
31171|Yass-Bowning beds|43491|14|Not recorded|pIV/7||Silurian|||||||
74772|Yelkin beds""|61964|6|Mentioned|p67|||One of the former names for Preston Formation rocks, mapped originally with the Ural Volcanics. Informal - superseded by Preston Formation.||||||27-OCT-08
73976|Yellow Gap Micromonzogranite|69639|6|Mentioned|p133, p220|||||Oban Suite||Intruded by the Llangothlin Monzogranite.||
73976|Yellow Gap Micromonzogranite|71628|6|Mentioned|p14: 31|||Chappell and Bryant (1994 unpublished). Originally Yellow Gap Microadamellite (Neilson, 1974 unpublished). Now Yellow Gap Microleucomonzogranite (this study).||||||
82540|Yellow Gap Suite|71628|5|Briefly described|p14: 32|||||Kingsgate Supersuite.|Yellow Gap Microleucomonzogranite.|||
82710|Yellow Gully Suite|71628|6|Mentioned|p19: 175||||||Yellow Gully Leucosyenogranite.|||
27632|Yellow Mount Granite|29987|5|Briefly described|p13|||||||||
27632|Yellow Mount Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27632|Yellow Mount Granite|42566|6|Mentioned|p91|||used by Brunker 1968, 1973. Same as Yellow Mountain Granite.||||||
27632|Yellow Mount Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
27632|Yellow Mount Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
37175|Yellowman's Creek Formation|23522|5|Briefly described|p252|Devonian|Devonian|||||||
29786|Yellowman's Creek beds|43043|3|Fully described|p90||Early Devonian|Misspelling of Yellowmans Creek beds.||||||
30042|Yellowmans Creek Shale|43188|5|Briefly described|Fig.2 p197|||Misspelling of Yellowmans Creek Formation.||||||
27944|Yeoval Granite|22831|6|Mentioned|p 69|||||||||
27944|Yeoval Granite|23214|6|Mentioned|p209|||||||||
27944|Yeoval Granite|24126|5|Briefly described|p4|||||||||
27944|Yeoval Granite|29902|6|Mentioned|p4|||||||||
27944|Yeoval Granite|29904|6|Mentioned|p3|||||||||
27944|Yeoval Granite|29986|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27944|Yeoval Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
27944|Yeoval Granite|31993|6|Mentioned|p679|||||||||
27944|Yeoval Granite|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
27944|Yeoval Granite|32047|6|Mentioned|p12|||Refers mineralization||||||
27944|Yeoval Granite|32412|6|Mentioned|p92|||||||||
27944|Yeoval Granite|32485|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27944|Yeoval Granite|32708|6|Mentioned|Fig.1|||||||||
27944|Yeoval Granite|33284|6|Mentioned|p18|||Dev. Disseminated Cu deposits.||||||
27944|Yeoval Granite|33285|6|Mentioned|p86|||||||||
27944|Yeoval Granite|33326|6|Mentioned|p443|||Late Dev.||||||
27944|Yeoval Granite|33732|6|Mentioned|p115|||||||||
27944|Yeoval Granite|33833|6|Mentioned|p403|||||||||
27944|Yeoval Granite|34403|6|Mentioned|p147|||||||||
27944|Yeoval Granite|34404|6|Mentioned|Fig.3.4b|||||||||
27944|Yeoval Granite|34405|6|Mentioned|p124|||||||||
27944|Yeoval Granite|34406|6|Mentioned|p222|||Buchan orogenic phase.||||||
27944|Yeoval Granite|35128|6|Mentioned|p361|||Appears on figure||||||
27944|Yeoval Granite|39331|6|Mentioned|Fig.7-3|||||||||
27944|Yeoval Granite|40130|6|Mentioned|p197|||||||||
27944|Yeoval Granite|40328|4|Described|p213|||||||||
27944|Yeoval Granite|40365|6|Mentioned|p243|||See also P293||||||
27944|Yeoval Granite|40891|6|Mentioned|Fig.3|||||||||
27944|Yeoval Granite|42262|6|Mentioned|Fig. 2 P1810|||||||||
27944|Yeoval Granite|42726|5|Briefly described|map legend|Early Devonian||415.  Of the Yeoval Suite (Boggy Plain Supersuite).  Formal name not intended.||||||08-FEB-05
27944|Yeoval Granite|42993|5|Briefly described|p61|||||||||
27944|Yeoval Granite|43344|14|Not recorded|p175|||(Yeoval Granite mass) Dubbo area||||||
27944|Yeoval Granite|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
27944|Yeoval Granite|43500|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
27944|Yeoval Granite|43510|14|Not recorded|p39,49||Middle Devonian|See also Lexicon. Hervey Syncline area||||||
27944|Yeoval Granite|43525|14|Not recorded|map p124|||||||||
27944|Yeoval Granite|48958|6|Mentioned|Plate 1|||||||||
27944|Yeoval Granite|68004|6|Mentioned|p21. |Early Devonian|Early Devonian|Southwest Brigalow Belt South Bioregion.||||||
27944|Yeoval Granite|71206|6|Mentioned|p384|||Zr content 300 p.p.m.||Boggy Plain Supersuite.|||I-type granite.|
33878|Yeoval Granite Complex|22519|5|Briefly described|p7|Devonian|Devonian|||||||
33878|Yeoval Granite Complex|22831|4|Described|p 69|||||||||
33878|Yeoval Granite Complex|23214|5|Briefly described|p210|Devonian|Devonian|Within Boggy Plains Supersuite. See also page 215 Fig. 44.||||||
33878|Yeoval Granite Complex|24417|6|Mentioned|p104|||||||||
77163|Yeoval Plutonic Suite|68003|5|Briefly described|p26.|Devonian|Devonian|Granites. Poor magnetic response and weak gravity highs.||||||
39389|Yeoval granite|24126|6|Mentioned|p4|||Informal - see Yeoval Granite.||||||
39389|Yeoval granite|63291|6|Mentioned|p419 Fig. 2|||Informal name.||||||
39389|Yeoval granite|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
34089|Yeoval granite complex|22466|6|Mentioned|P8||Early Devonian|||||||
42325|Yeoval suite|24270|6|Mentioned|p1612|||Geological Province: Lachlan Fold Belt.  Of the Boggy Plain Supersuite.||||||09-MAR-05
67893|Yetholme Adamellite|24424|6|Mentioned|p540|Late Carboniferous|Late Carboniferous|||||||03-MAR-05
37451|Yetholme Granite|23214|5|Briefly described|p253|||Now divided into Durandale and Eusdale Granites.||||||
29192|Yetholme granite|34572|6|Mentioned|p81|||||||||
35262|Yeularbah Sandstone Member|23055|6|Mentioned|Fig13p25|||Name not clear in diagram.||||||
40585|Yeundoo Andesite Tuff|24605|6|Mentioned|p948 App.1|||Superseded by Yeundoo Rhyolite Member||||||
40586|Yeundoo Rhyolite|24605|6|Mentioned|p948 App.1|||Superseded by Yeundoo Rhyolite Member||||||
40584|Yeundoo Rhyolite Member|24605|2|Defined|p936 Fig.5, p948 App.1|Visean|Visean|Of the Caroda Formation. Maximum Thickness: 10m. Geological Province: New England Orogen.||||||
36470|Yewrangarah Suite|23550|5|Briefly described|p502, 503|||2 geochem analyses discussed.||||||30-MAR-17
79850|Yewrangra Granite|67820|5|Briefly described|p136|||Strongly fractionated. Has higher mineral potential than most granitoids on the Goulburn sheet.|||||A-type granite.|
83288|Yiddah Intrusive Complex|73154|5|Briefly described|p78 Tb.1|Llandovery|Llandovery|Junee-Narromine structural belt. 438.3+/-3.5 Ma zircon U-Pb age from Yiddah monzodiorite sample p89 Tb.2, referred to as Yiddah monzodiorite in text p84, p89, p92.|438.3+/-3.5 Ma zircon U-Pb||||Includes monzodiorite|
40731|Yiddah formation|23309|6|Mentioned|p390|||||||||
77705|Yoeval Complex|60308|6|Mentioned|p38|||||Boggy Plains Suite||||
30664|Yorkey's Creek Sandstone|43318|14|Not recorded|opp p6||Late Devonian|||||||
30664|Yorkey's Creek Sandstone|43320|14|Not recorded|Table 1||Late Devonian|||||||
34307|Young Batholith|22687|6|Mentioned|111 fig 2|||Geol province Lachlan Fold Belt||||||
30978|Young Wallsend Chert|43440|14|Not recorded|p49|||Unit of Newcastle Coal Measures||||||
30978|Young Wallsend Chert|43477|14|Not recorded|p21,52||Permian|Unit of Newcastle Coal Measures||||||
35157|Young Wallsend Coal Seam|23055|6|Mentioned|Fig11p23|||||||||
39373|Young granite|24125|5|Briefly described|p3|||Informal name.||||||
25675|Yowaka Granite|42726|5|Briefly described|map legend|Early Devonian||199.||||||29-AUG-12
27635|Yuendoo Andesite Tuff Member|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Part of Caroda Formation||||||
37295|Yuendoo Rhyolite|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Of Caroda Formation.  Geological Province: New England Orogen.||||||
37295|Yuendoo Rhyolite|24010|5|Briefly described|p379|||||||||
37295|Yuendoo Rhyolite|24348|5|Briefly described|p131, p133|Carboniferous|Carboniferous|Of Caroda Formation.||||||
37295|Yuendoo Rhyolite|24603|6|Mentioned|p897 Fig. 17|||||||||
37295|Yuendoo Rhyolite|60299|6|Mentioned|p231 Fig.12|Carboniferous|Carboniferous|Of the Caroda Formation.||||||
37295|Yuendoo Rhyolite|65107|6|Mentioned|Fig 11, 286-7|Carboniferous|Carboniferous|Shown in a Carboniferous age pole path for Tamworth Belt rocks, Rocky Creek Block.||||||
82427|Yugilbar Adamellite|71628|6|Mentioned|p9: 10|||Gutsche (1969).||||||
82425|Yugilbar Gabbro|71628|5|Briefly described|p9: 2, 10, 12, 16-17, 19, 23, 26-31|||See also p1: 11; p19: 176. New name (this study), from a local homestead. Applies to the mafic zone rocks (<58 wt% SiO2) within the Complex. Unassigned. Now excluded from, but was previously a constituent of, Clarence River Supersuite. Complex distribution described. Variable outcrop. Lithologies described in great detail. Geochemistry described.||Dumbudgery Creek Complex.||Intrudes Silverwood Group. Abuts Wave Hill Tonalite, Mount Carnham Granodiorite and Gordonbrook Serpentinite.|Composite unit of texturally heterogeneous coarse-grained (gabbros to quartz diorite) to fine-grained (basalt, basaltic andesite) mafic igneous rocks.|
35432|Yullundry Formation""|23170|6|Mentioned|p55|||||||||
35432|Yullundry Formation""|43494|6|Mentioned|p17|||Informal - see Yullundry Formation.||||||16-MAR-06
77323|Yunedoo Andesite Tuff|68005|5|Briefly described|p146.|Carboniferous|Carboniferous|[Mis-spelling of Yuendoo].||Unit in Caroda Formation.|||Andesitic ash-flow tuff.|
29515|Yuranigh Limestone|43782|6|Mentioned|Map Diagram|Gisbornian|Gisbornian|of Fairbridge Volcanics, Kenilworth Group. Error in use - should be referring to Yuranigh Limestone Member.||||||
38196|Yuranigh Limestone Members|23736|5|Briefly described|p12|Eastonian|Darriwilian|Probably misspelt.   Parent: Fairbridge Volcanics||||||
38263|Yuranigh Limestone member|23739|6|Mentioned|p212|||Informal name - see Yuranigh Limestone Member||||||
38263|Yuranigh Limestone member|72263|5|Briefly described|p516-518|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen. Autochthonous limestone unit within the Fairbridge Volcanics.||Unit of Fairbridge Volcanics.||||
79220|Yurrunga Coal Measures|64877|5|Briefly described|p296|Permian|Permian|Southern Sydney Basin.||Shoalhaven Group.||||
79220|Yurrunga Coal Measures|68592|5|Briefly described|p1779, p1785|Permian|Permian|||Unit in Shoalhaven Group.||Conformably overlies Tallong Conglomerate. Is overlain by Snapper Point Formation.||
33881|bimba suite|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill Olary Domain||||||
33882|calc - silicate suite|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Olary Domain||||||
40453|calc-silicate Suite|24592|6|Mentioned|p634|||Of the Willyama Supergroup. Geological Province: Curnamona Province. Infomal form of the informal Calc-silicate Suite.||||||
34931|conglomerate unit|22952|6|Mentioned|p178,Table1p179|||||||||
37465|exiguus bed|23214|5|Briefly described|p104 Fig. 24|Early Silurian|Early Silurian|Of Waugoola Group.  Informal name. See also "exiguus beds".||||||
37396|exiguus beds""|23214|4|Described|p110|Wenlock|Llandovery|Informal name. The intial 9m of the Glendalough Formation characterised by abundant Monograptus exiguus.||||||
34933|graded-bedded unit|22952|6|Mentioned|p178,Table1p179|||||||||
37222|grey unit""|23214|6|Mentioned|p46|||Renamed Mount Lewin Limestone Member.||||||
37223|island unit""|23214|6|Mentioned|p46|||Renamed Trilobite Hill Limestone Member.||||||
34650|lower Bellbird Creek Formation|22815|4|Described|p100|||Age: Frasnian||||||
34736|lower Olney Formation|22893|5|Briefly described|p25|Middle Miocene|Middle Eocene|Probably equivalent to Upper Renmark Formation||||||
35358|lower Yarrimie Formation|23185|6|Mentioned|p158|||||||||
35076|main lead""|23043|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
35076|main lead""|23170|4|Described|p348|Miocene|Miocene|||||||
34737|middle Olney Formation|22893|5|Briefly described|p25|Middle Miocene|Middle Eocene|Coeval with Murray Group calcarenites.||||||
34934|mottled clay unit""|22952|5|Briefly described|p178,Table1p179||Pleistocene|||||||
33880|pelite suite|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill - Olary Domain||||||
38982|peri Rhyolite|23861|5|Briefly described|p3|Namurian|Namurian|Typographical error - see Peri Rhyolite.  Geological Province: New England Orogen.||||||
34935|phosphorite unit|22952|6|Mentioned|p178,Table1p179|||||||||
33892|quartzo feldspathic suite|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Geol province Olary Domain||||||
37464|spiralis bed|23214|5|Briefly described|p104 Fig. 24|Early Silurian|Early Silurian|Of Waugoola Group.  Informal name. See also "spiralis beds".||||||
37395|spiralis beds""|23214|4|Described|p110|Wenlock|Llandovery|Overlies "exiguus beds" and is 33m of olive green shale containing Monograptus spiralis.||||||
34651|upper Bellbird Formation|22815|4|Described|p100|||Age: Frasnian||||||
34738|upper Olney Formation|22893|5|Briefly described|p25|Middle Miocene|Middle Eocene|Coeval with Murray Group calcarenites.||||||
77164|wandsworth volcanics|68003|6|Mentioned|p42.|||Formal name is Wandsworth Volcanic Group.||||||
