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
143|Adori Sandstone|12597|5|Briefly described|p492 Tb.1, p497, p499|Oxfordian|Oxfordian|Eromanga Basin. Also equivalent to lower Namur Sandstone and middle Algebuckina Sandstone.||Unit in Injune Creek Group.||Equivalent to Springbok Sandstone. Is overlain conformably by Westbourne Formation.|Mainly sub-labile to labile sandstone with minor pebble bands and coarse sandstone lenses.|
143|Adori Sandstone|13497|6|Mentioned|p115 fig 6.33, p146, p149|Late Jurassic|Middle Jurassic|Eromanga Basin.See also p150, p151, p153 fig 9.29, p154, ||||Overlies the Birkhead Formation. Overlain by the Westbourne Formation and the Namur Sandstone.||
143|Adori Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Jurassic|Late Jurassic|In Eromanga Basin.||||||
143|Adori Sandstone|22464|5|Briefly described|p9||Late Jurassic|Eromanga Basin, overlies Birkhead Formation, overlain by Westbourne Formation.||||||21-APR-08
143|Adori Sandstone|22883|6|Mentioned|P31|||||||||
143|Adori Sandstone|23054|6|Mentioned|Fig5p22|Tithonian|Tithonian|||||||
143|Adori Sandstone|23056|4|Described|17|||Geol province Eromanga Basin. Parent Injune Creek Group.||||||21-APR-08
143|Adori Sandstone|23155|6|Mentioned|p26|||The Adori Sandstone has not been recognised on STRZELECKI.||||||
143|Adori Sandstone|23375|4|Described|Fig2 p265||Tithonian|Laterally equivalent to part of Namur Sandstone. of Eromanga Basin.||||||
143|Adori Sandstone|23425|5|Briefly described|Plate 10.2|||Of Injune Creek Group, Eromanga Basin Province.||||||
143|Adori Sandstone|23430|4|Described|p523-524 Table 14.7|||Of Injune Creek Group. Eromanga Basin Province. Maximum thickness <33 m.||||||
143|Adori Sandstone|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Eromanga Basin. Of the Mooga Formation.||||||
143|Adori Sandstone|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Of Injune Creek Group. Geological Province: Great Artesian Basin.||||||
143|Adori Sandstone|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
143|Adori Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||17-DEC-04
143|Adori Sandstone|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Cooper Basin.||||||
143|Adori Sandstone|29591|6|Mentioned|Table 72|||||||||
143|Adori Sandstone|30024|6|Mentioned|p332|||||||||
143|Adori Sandstone|30102|6|Mentioned|p16|||Jurassic age. Unit of Injune Creek Group. See also P21,24,31.||||||
143|Adori Sandstone|30103|5|Briefly described|p9|||Middle to Upper Jurassic age. Table 3 on P9.||||||
143|Adori Sandstone|30104|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
143|Adori Sandstone|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
143|Adori Sandstone|30691|4|Described|p6|||See also P20,21,Table4,6.Middle-Upper Jurassic age.||||||21-APR-08
143|Adori Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
143|Adori Sandstone|30694|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
143|Adori Sandstone|30695|4|Described|Table 4|||||||||
143|Adori Sandstone|30699|6|Mentioned|p10|||Correlation table||||||
143|Adori Sandstone|30702|6|Mentioned|p48|||See also Fig.1. Stratigraphic table||||||
143|Adori Sandstone|30804|6|Mentioned|Table 2.|||||||||
143|Adori Sandstone|30853|5|Briefly described|Table 3|||Middle-Upper Jurassic age||||||
143|Adori Sandstone|30854|5|Briefly described|Table 4|||Middle-Upper Jurassic age||||||
143|Adori Sandstone|30855|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Middle - Upper Jurassic.M - U||||||
143|Adori Sandstone|30856|4|Described|Table 3|||On table 10. Middle-Upper Jurassic age||||||
143|Adori Sandstone|30857|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic. Part of Injune Creek Group.M - U||||||
143|Adori Sandstone|31116|6|Mentioned|p27|||||||||
143|Adori Sandstone|31120|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|31145|5|Briefly described|Table 1|||Middle - Upper Jurassic||||||
143|Adori Sandstone|31425|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper JurassicM - U||||||
143|Adori Sandstone|31431|5|Briefly described|Table 3|||M.-U.Jurassic||||||
143|Adori Sandstone|33067|4|Described|Table 1|Middle Jurassic|Middle Jurassic|Of the Injune Creek Group.  Labile sandstone.||||||07-JUL-04
143|Adori Sandstone|33069|4|Described|p7|||M.- U.Jur. Injune Cr. Gp.||||||21-APR-08
143|Adori Sandstone|33071|5|Briefly described|p6|||M.-U.Jur.||||||
143|Adori Sandstone|33075|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|33078|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
143|Adori Sandstone|33079|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
143|Adori Sandstone|33082|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
143|Adori Sandstone|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
143|Adori Sandstone|33087|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.- U.Jur.M - U||||||
143|Adori Sandstone|33088|4|Described|Table 3|||Injune Ck Gp.||||||
143|Adori Sandstone|33089|5|Briefly described|Table 2|||M-U.Jur.||||||
143|Adori Sandstone|33092|5|Briefly described|p9|||Stratigraphy||||||
143|Adori Sandstone|33367|6|Mentioned|p23|||||||||
143|Adori Sandstone|33449|4|Described|Table 1|||M.-U.Jur.||||||
143|Adori Sandstone|33638|6|Mentioned|p9|||||||||
143|Adori Sandstone|33639|5|Briefly described|Table 2|||||||||
143|Adori Sandstone|33648|6|Mentioned|p19|||Strat.||||||
143|Adori Sandstone|33672|5|Briefly described|p44|||Lithology||||||
143|Adori Sandstone|33673|4|Described|p291|||||||||
143|Adori Sandstone|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
143|Adori Sandstone|33825|4|Described|p9|||Lithology & correlation||||||
143|Adori Sandstone|33827|6|Mentioned|p13|||||||||
143|Adori Sandstone|33832|5|Briefly described|p11|||Strat. & correlation||||||
143|Adori Sandstone|33939|6|Mentioned|p412|||N-S subsurface usage||||||
143|Adori Sandstone|34065|4|Described|p7|||M.-U.Jur.||||||
143|Adori Sandstone|34091|4|Described|Table 1|||Jurassic. Injune Cr. Gp.||||||
143|Adori Sandstone|34134|6|Mentioned|Chart|||Located between P480/481.||||||
143|Adori Sandstone|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
143|Adori Sandstone|34218|5|Briefly described|Table 1|||See also Table 2. Middle - Upper Jurassic.||||||
143|Adori Sandstone|34386|6|Mentioned|p99|||Jurassic. See also PP100,101,102 etc.||||||
143|Adori Sandstone|34486|4|Described|Table 1|||See also Table 2. Upper Jurassic.||||||21-APR-08
143|Adori Sandstone|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
143|Adori Sandstone|34611|6|Mentioned|Fig.65|||Correlation||||||
143|Adori Sandstone|35239|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|35560|6|Mentioned|p289|||||||||
143|Adori Sandstone|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
143|Adori Sandstone|35663|5|Briefly described|p124|||||||||
143|Adori Sandstone|35811|5|Briefly described|Table 3|||||||||
143|Adori Sandstone|36243|6|Mentioned|Table 6A|||||||||
143|Adori Sandstone|36910|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|37608|3|Fully described|Table 1|||||||||
143|Adori Sandstone|37995|6|Mentioned|p62|||||||||
143|Adori Sandstone|39070|4|Described|p363|||||||||
143|Adori Sandstone|39276|6|Mentioned|Fig. 2|||||||||
143|Adori Sandstone|39445|5|Briefly described|Table 10|||||||||
143|Adori Sandstone|39478|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|39494|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|39846|6|Mentioned|Fig.2|||||||||
143|Adori Sandstone|39847|5|Briefly described|p36|||||||||
143|Adori Sandstone|39943|6|Mentioned|Table 8A|||||||||
143|Adori Sandstone|39988|6|Mentioned|Fig.2|||||||||
143|Adori Sandstone|39989|4|Described|p422|||||||||
143|Adori Sandstone|40030|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|40121|6|Mentioned|p446|||||||||
143|Adori Sandstone|40249|6|Mentioned|p41|||||||||
143|Adori Sandstone|40250|6|Mentioned|Fig.7|||||||||
143|Adori Sandstone|40544|6|Mentioned|p161|||||||||
143|Adori Sandstone|40670|6|Mentioned|Fig.9|||||||||
143|Adori Sandstone|40675|6|Mentioned|Table 8A|||||||||
143|Adori Sandstone|40687|3|Fully described|p414|||||||||
143|Adori Sandstone|40832|3|Fully described|p455|||||||||
143|Adori Sandstone|40833|6|Mentioned|p468|||||||||
143|Adori Sandstone|40910|6|Mentioned|Table 3|||||||||
143|Adori Sandstone|40926|6|Mentioned|Table 2|||||||||
143|Adori Sandstone|40962|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|41060|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|41061|6|Mentioned|p19|||||||||
143|Adori Sandstone|41062|6|Mentioned|Fig.5|||||||||
143|Adori Sandstone|41063|6|Mentioned|Fig.4|||||||||
143|Adori Sandstone|41064|6|Mentioned|p60|||||||||
143|Adori Sandstone|41084|5|Briefly described|Fig.2|||||||||
143|Adori Sandstone|41097|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|41099|6|Mentioned|p192|||||||||
143|Adori Sandstone|41123|6|Mentioned|p177|||||||||
143|Adori Sandstone|41175|5|Briefly described|p195|||||||||
143|Adori Sandstone|41177|6|Mentioned|Fig.2|||||||||
143|Adori Sandstone|41182|5|Briefly described|Fig.2|||||||||
143|Adori Sandstone|41183|6|Mentioned|Fig.3 p308|||||||||
143|Adori Sandstone|41186|4|Described|p207|||||||||
143|Adori Sandstone|41187|6|Mentioned|Fig.2|||||||||
143|Adori Sandstone|41198|6|Mentioned|Table 1|||||||||
143|Adori Sandstone|41214|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|41216|6|Mentioned|Fig.18|||||||||
143|Adori Sandstone|41219|4|Described|p345|||||||||
143|Adori Sandstone|41247|6|Mentioned|p126|||||||||
143|Adori Sandstone|41266|6|Mentioned|Fig.3|||||||||
143|Adori Sandstone|41286|5|Briefly described|p114|||||||||
143|Adori Sandstone|41681|6|Mentioned|p16|||||||||
143|Adori Sandstone|41724|6|Mentioned|p382|||||||||
143|Adori Sandstone|42061|4|Described|Fig,11 P159|||||||||
143|Adori Sandstone|42067|4|Described|p308|||See also Appendix 2||||||
143|Adori Sandstone|42071|6|Mentioned|p116|||||||||
143|Adori Sandstone|42084|6|Mentioned|Fig.3 P356|||||||||
143|Adori Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
143|Adori Sandstone|42446|4|Described|p12|||||||||
143|Adori Sandstone|42447|6|Mentioned|Fig. 2|||||||||
143|Adori Sandstone|42474|6|Mentioned|p25|||||||||
143|Adori Sandstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
143|Adori Sandstone|42520|5|Briefly described|p6|||||||||
143|Adori Sandstone|42746|6|Mentioned|p9, p10|||See also Fig.6 P8, Fig.7 P37||||||
143|Adori Sandstone|42749|5|Briefly described|p30|||see also Fig.2 P27||||||
143|Adori Sandstone|42999|5|Briefly described|Table 2,p90||Late Jurassic|||||||
143|Adori Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
143|Adori Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
143|Adori Sandstone|43105|5|Briefly described|Fig.9,p15.|||||||||
143|Adori Sandstone|43114|5|Briefly described|p12|||||||||
143|Adori Sandstone|43122|5|Briefly described|p11|||see also Fig. 2.||||||
143|Adori Sandstone|43591|6|Mentioned|p40|||||||||
143|Adori Sandstone|43628|6|Mentioned|Fig.13|Late Jurassic|Middle Jurassic|||||||
143|Adori Sandstone|43711|6|Mentioned|p18|||||||||
143|Adori Sandstone|44016|14|Not recorded|Map Legend||Middle Jurassic|||||||
143|Adori Sandstone|44019|14|Not recorded|Map Legend||Middle Jurassic|||||||
143|Adori Sandstone|44020|14|Not recorded|Tb.1,2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
143|Adori Sandstone|44021|2|Defined|p232-236||Middle Jurassic|Occurs in Eromanga Basin. Overlies Birkhead Formation; underlies Westbourne Formation. Plant impressions.||||||
143|Adori Sandstone|44022|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
143|Adori Sandstone|44023|4|Described|Tb.3,p12|Late Jurassic|Middle Jurassic|||||||
143|Adori Sandstone|44024|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
143|Adori Sandstone|44028|14|Not recorded|Fig.7,2 p514||Jurassic|Of Injune Creek Group. See Strat Table.||||||
143|Adori Sandstone|44031|14|Not recorded|Tb.2,p5,8||Jurassic|||||||
143|Adori Sandstone|44084|14|Not recorded|p32(Tb)||Middle Jurassic|Fossils. Eromanga Basin.||||||
143|Adori Sandstone|44129|14|Not recorded|p95-96||Jurassic|||||||
143|Adori Sandstone|44133|5|Briefly described|p110, 104 Fig. 9.11|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin. Conformably overlies: Birkhead Formation. Conformably underlies: Westbourne Formation.||||||
143|Adori Sandstone|44171|14|Not recorded|p194,195,197|||||||||
143|Adori Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
143|Adori Sandstone|44375|14|Not recorded|p312,map|||||||||
143|Adori Sandstone|44414|14|Not recorded|p114,115||Jurassic|||||||
143|Adori Sandstone|44415|14|Not recorded|Fig.1,p23|||||||||
143|Adori Sandstone|44668|14|Not recorded|p61|||||||||
143|Adori Sandstone|45071|3|Fully described|Table 15|||||||||
143|Adori Sandstone|45110|4|Described|p97|||See also Fig.5.||||||
143|Adori Sandstone|45168|6|Mentioned|p9|||||||||
143|Adori Sandstone|46791|6|Mentioned|Fig.6|||||||||
143|Adori Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
143|Adori Sandstone|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
143|Adori Sandstone|48919|4|Described|p62|||Jurassic||||||
143|Adori Sandstone|48920|3|Fully described|p50|||Part of Injune Creek Group.||||||21-APR-08
143|Adori Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
143|Adori Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
143|Adori Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Birkhead Formation; overlain by Westbourne Formation; lateral to Namur Sandstone. Geological Province: Eromanga Basin.||||||31-JAN-08
143|Adori Sandstone|61312|5|Briefly described|p71, p79 Table E2|||Of the Injune Creek Group. Fine- to medium-grained clayey sandstone and minor pebbly sandstone and siltstone. Geological Province: Eromanga Basin.||||||
143|Adori Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||13-MAR-09
143|Adori Sandstone|61613|6|Mentioned|p282 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
143|Adori Sandstone|61614|6|Mentioned|p290 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
143|Adori Sandstone|61615|6|Mentioned|p302 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
143|Adori Sandstone|62730|5|Briefly described|p352 Fig. 1|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
143|Adori Sandstone|63979|2|Defined|p37 Fig. 44|Oxfordian|Callovian|Conformable over [?under] Westbourne Formation; unconformable over Birkhead Fm; intertongues with Springbok Fm in places. Max. thickness: 55m. Geological Province: Eromanga Basin.Predominantly sandstone (fining upwards) + minor siltstone and conglomerate.||||||05-NOV-13
143|Adori Sandstone|64048|6|Mentioned|p64 Tb. 2, p70|||Geological Province: Eromanga Basin.||||||07-FEB-11
143|Adori Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Jurassic|Late Jurassic|Eromanga Basin.||||Underlies Westbourne Formation; overlies Birkhead Formation.||10-DEC-15
143|Adori Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Late Jurassic|Late Jurassic|Eromanga Basin. Equivalent to the Springbok Sandstone (Surat Basin).||||Is overlain by Westbourne Formation.||
143|Adori Sandstone|64856|5|Briefly described|p90-91|||Eromanga Basin unit, laterally equivalent to the Springbok Sandstone. Age APJ6. Overlies Birkhead Formation unconformably (time break in palynofloras).| | ||||28-NOV-17
143|Adori Sandstone|64857|6|Mentioned|p133|||Eromanga Basin. Younger than Springbok Sandstone based on palynology.||||||
143|Adori Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||17-FEB-10
143|Adori Sandstone|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Late Jurassic|Of Eromanga Basin. Overlain by Westbourne Formation.||||||08-MAR-12
143|Adori Sandstone|65489|5|Briefly described|p15, p49, p96, p155|Middle Jurassic|Middle Jurassic|Eromanga Basin. Fair reservoir quality. Oil reservoir accounting for 0.2% of the Basin's production.||||Overlies Birkhead Formation. Is overlain by Westbourne Formation.||
143|Adori Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. ||Unit in Injune Creek Group.||Overlies Birkhead Formation. Is overlain by Westbourne Formation.||
143|Adori Sandstone|66915|5|Briefly described|p6 Fig.3|Late Jurassic|Late Jurassic|Eromanga Basin.||||||
143|Adori Sandstone|67323|5|Briefly described|p87, p93 Fig.12.3, p95 Fig.12.5, p96|Late Jurassic|Late Jurassic|Eromanga Basin. A regionally extensive aquifer.||||Overlies Birkhead Formation. Is overlain by Westbourne Formation.||
143|Adori Sandstone|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1|Kimmeridgian|Kimmeridgian|Eromanga Basin. Maximum thickness of 55m. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Prospective unit for the storage of carbon dioxide. See also p108, p109, p111, p113, p114 fig ERO13, p115, p119, p304.||||Overlies the Birkhead Formation. Overlain by the Westbourne Formation.|Sandstone with minor siltstone and conglomerate.|
143|Adori Sandstone|67561|5|Briefly described|p52 Fig.2|Valanginian|Berriasian|Australian Spore-Pollen zonation: australiensis. See also misspelt Adoori Sandstone.||||||
143|Adori Sandstone|68135|5|Briefly described|p52 fig 2b, p54|Kimmeridgian|Oxfordian|Eromanga Basin. Contains plant macrofossils.||||Unconformably overlies Birkhead Formation. Overlain by Westbourne Formation.|Cross bedded sandstone.|13-SEP-17
143|Adori Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
143|Adori Sandstone|68731|6|Mentioned|pp209-211|||||||||
143|Adori Sandstone|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this terrestrial unit within the Algebuckina Sandstone and equivalent units.||||||04-NOV-13
143|Adori Sandstone|69019|5|Briefly described|p85 Fig.21.|Tithonian|Tithonian|Southern Eromanga Basin.||||Overlies Birkhead Formation. Is overlain by Westbourne Formation.||
143|Adori Sandstone|69023|6|Mentioned|p89 Fig.20|Tithonian|Tithonian|||||||
143|Adori Sandstone|69457|6|Mentioned|p41:3-4|||Eromanga Basin.||||||12-JUL-16
143|Adori Sandstone|69582|6|Mentioned|p65-p66|Late Jurassic|Late Jurassic|Eromanga Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Birkhead Formation. Overlain by the Westbourne Formation.|Sandstone.|
143|Adori Sandstone|69594|5|Briefly described|p519, p525-527, p532, p537, p573|Oxfordian|Oxfordian|Eromanga Basin. An extensive unit. Generally 15-50m thick; maximum 55m. Distinguishing from Birkhead Formation is difficult; has lower gamma log and higher resistivity log values than the latter. Discrimination from Westbourne Formation described. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated. Braided fluvial deposits. Is a minor hydrocarbon reservoir.||||Unconformably overlies Birkhead Formation. Is overlain conformably by Westbourne Formation. Laterally continuous/interfingers with Springbok Sandstone.|Fining-upwards, predominantly quartzose sandstone succession, becoming more labile up-section and having minor siltstone and conglomerate.|
143|Adori Sandstone|69673|6|Mentioned|p154, p155 fig 127|Jurassic|Jurassic|||||Overlies Birkhead Formation, overlain by Westbourne Formation||
143|Adori Sandstone|69790|6|Mentioned|p1063 Fig.2, p1066|Late Jurassic|Late Jurassic|Eromanga Basin.||||Unconformably overlies Birkhead Formation.||
143|Adori Sandstone|69797|5|Briefly described|p17 Fig.2|Late Jurassic|Late Jurassic|Geol. Prov: Eromanga Basin.||||||
143|Adori Sandstone|69946|3|Fully described|p11, p15-16, p57-58|Late Jurassic|Late Jurassic|Defined by Woolley (1941) from outcrops near Tambo. Name first published by Hill and Denmead (1960). Redefined by Exon (1966) as the sandstone above Birkhead Formation and below Westbourne Formation; he also remeasured the type section, an outcrop from Adori Hill, 35.4 km ENE of Tambo. In SA, restricted to N Cooper Basin and NE Pedirka Basin. Generally 20 - 130m thick. Wireline log correlations.||||Conformably overlies Birkhead Formation. Is overlain conformably by Westbourne Formation. Lateral equivalent of Namur and Algebuckina Sandstones.|Well-sorted, subrounded, cross-bedded, fine- to coarse-grained sandstone; local diagenetic calcite-cemented zones up to 45m thick in basal parts.|
143|Adori Sandstone|69947|5|Briefly described|p7-8, p13 Fig.7.2, p24 Fig.7.13, p28|Early Cretaceous|Late Jurassic|Eromanga Basin. Forms a couplet with Westbourne Formation, restricted to northern Cooper region and eastern-most Perdika region. Where Westbourne Formation is absent, the Adori and Namur Sandstones are amalgamated and called the Namur Sandstone.||||Overlies Birkhead Formation. Is overlain by Westbourne Formation gradationally, or Namur Sandstone.|Lower part is amalgamated fluvial sandstones, becoming finer-grained with siltstone and carbonaceous material.|07-FEB-18
143|Adori Sandstone|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Eromanga Basin. Aquifer: generally artesian.||Injune Creek Group.||Overlies Birkhead Formation. Is overlain by Westbourne Formation.||
143|Adori Sandstone|70823|5|Briefly described|p25-p27, p43, p78|Late Jurassic|Middle Jurassic|Eromanga Basin. Deposited in a braided fluvial environment.||||Overlies the Birkhead Formation. Overlain by the Westbourne Formation.||
143|Adori Sandstone|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Birkhead Formation. Overlain by the Westbourne Formation.||
143|Adori Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
143|Adori Sandstone|71342|3|Fully described|Ch1 p19, Ch5 p12, Ch5 p14-p16|Tithonian|Tithonian|Cooper Basin, Pedirka Basin. Woolley (1941) defined the Adori sandstone from outcrops in the Tambo area, however, Hill and Denmead (1960) were the first to publish the name. A type section was measured by Exon (1966) who also redefined the unit as the sandstone above the Birkhead Formation and below the Westbourne Formation. A type section outcrops on Adori Hill and was defined by Exon (1966). This unit is generally 20 to 130m thick in the Cooper region. A combined thickness for the Adori and Namur sandstones and the Westbourne Formation reaches a maximum thickness in excess of 290m. This unit is assigned to the Late Jurassic PJ6.1 palynozone. The Adori Sandstone is interpreted to have been deposited in a low-sinuosity fluvial system. See also Ch5 p57-p58, Ch7 p7, Ch7 p13, Ch8 p5, Ch8 p10, Ch8 p17-p18, Ch11 p2, Ch13 p4, Ch13 p9.||||Conformably overlies the Birkhead Formation. Conformably overlain by the Westbourne Formation. Equivalent to the Namur and Algebuckina Sandstones.|Well-sorted, subrounded, cross-bedded and fine to coarse-grained sandstone. Diagenetic calcite cemented zones up to 45m thick are developed locally in the basal sandstones.|
143|Adori Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Injune Creek Group.||Overlies Birkhead FZ. Is overlain by Westbourne FZ.||
143|Adori Sandstone|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Late Jurassic|Shown as located in the Eromanga Basin.||||Shown as unconformably overlying Birkhead Formation and underlying and laterally equivalent to Westbourne Formation.|Includes some fossil flora.|
143|Adori Sandstone|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil and gas.||||||
143|Adori Sandstone|73251|6|Mentioned|p62|Late Jurassic|Late Jurassic|Eromanga Basin. Deposited in a braided-meandering fluvial setting. Oil show.||||Underlain by Birkhead Formation. Overlain by Westbourne Formation. Equivalent to Namur Sandstone and Algebuckina Sandstone.||
143|Adori Sandstone|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil and gas.||||Underlain by Birkhead Formation. Overlain by Westbourne Formation. Equivalent to Mooga Formation.||
143|Adori Sandstone|73393|6|Mentioned|p21|Kimmeridgian|Kimmeridgian|Eromanga Basin.||Injune Creek Group||Overlain by Westbourne Formation.||
143|Adori Sandstone|73479|5|Briefly described|p156 Fig.2, p159|Jurassic|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 152 Ma|||Overlies Birkhead Formation, underlies Westbourne Formation||
4193|Ainslie Volcanics (WA)|23818|5|Briefly described|p45|Proterozoic|Proterozoic|Geological Province: Musgrave Block. Age: 1000 Ma.||||||18-APR-05
4193|Ainslie Volcanics (WA)|30388|6|Mentioned|p12|||Refers Sofoulis(1962) Lower part now Lilian Formation||||||
4193|Ainslie Volcanics (WA)|30390|6|Mentioned|p81|||||||||
4193|Ainslie Volcanics (WA)|31393|6|Mentioned|Pl.25|||M. Proterozoic. Chart only||||||
4193|Ainslie Volcanics (WA)|34537|6|Mentioned|p45|||||||||
198|Ajax Limestone|833|5|Briefly described|p176,178-9,182-4,186,190,192|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: AJX-M and AJX-N (Mount Scott Range). Correlable to Wilkawillini and Wirrapowie limestones. Includes M. etheridgi zone. See also p194-5,199-201,203,205.||Unit of Hawker Group.||Overlain by Billy Creek Formation. Underlain unconformably by Parachilna Formation.||
198|Ajax Limestone|22646|6|Mentioned|Fig 4 on p 102||Early Cambrian|Adelaide Geosyncline (West)||||||
198|Ajax Limestone|22650|6|Mentioned|p 159|Cambrian|Cambrian|Province - Adelaide Geosyncline.||||||
198|Ajax Limestone|22652|6|Mentioned|p 196|||||||||
198|Ajax Limestone|22766|5|Briefly described|Fig.2 p561, p561|Early Cambrian|Early Cambrian|||||||
198|Ajax Limestone|23211|6|Mentioned|Fig.2|||Of Hawker Group.||||||04-MAR-09
198|Ajax Limestone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
198|Ajax Limestone|23981|5|Briefly described|p8-9 Fig. 4, p62|Early Cambrian|Early Cambrian|Overlies Woodendinna Dolomite. Correlated with entire Kulpara Formation-Parara Limestone succession. Geol. Prov: Arrowie Basin. See also p10 Fig. 5 (lower, middle and upper).  Age is Atdabanian to Toyonian.||||||12-JUL-06
198|Ajax Limestone|24176|4|Described|p16, p23 Tb. 1|Early Cambrian|Early Cambrian|Grey siliceous limestone, pink argillaceous limestones, minor dolomites, oolitic limestones, calcareous shales, chalcedony nodules.  Max. thickness: 370m.  Geological Province: Mount Painter Province.||||||
198|Ajax Limestone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
198|Ajax Limestone|24481|5|Briefly described|p828, p829 Fig. 9|Cambrian|Cambrian|Overlies the Parachilna Formation. Overlain by the Billy Creek Formation.||||||
198|Ajax Limestone|29781|6|Mentioned|p48|||||||||
198|Ajax Limestone|29929|6|Mentioned|p225|||||||||
198|Ajax Limestone|30051|6|Mentioned|Fig.4|||||||||
198|Ajax Limestone|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
198|Ajax Limestone|30220|6|Mentioned|Fig.13|||||||||
198|Ajax Limestone|30374|6|Mentioned|Fig.5|||Correlation. Lower Cambrian age.||||||
198|Ajax Limestone|30375|6|Mentioned|Fig.1|||See also P203||||||
198|Ajax Limestone|30801|6|Mentioned|p5|||See also P6. Table. Lower Cambrian.||||||
198|Ajax Limestone|30807|6|Mentioned|p102|||Suggested mapping symbol||||||
198|Ajax Limestone|31388|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|31536|6|Mentioned|p8|||||||||
198|Ajax Limestone|31539|5|Briefly described|p14|||See also Fig. 4. Cambrian||||||
198|Ajax Limestone|31705|6|Mentioned|p27|||||||||17-JUL-06
198|Ajax Limestone|31923|6|Mentioned|p14|||||||||
198|Ajax Limestone|32343|6|Mentioned|Table 1|||See also Figs. 3,4,5.||||||
198|Ajax Limestone|32776|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|33035|6|Mentioned|p53|||||||||
198|Ajax Limestone|33655|6|Mentioned|p87|||L.Camb.||||||
198|Ajax Limestone|33734|5|Briefly described|p495|||Correlation. Trace fossils.||||||
198|Ajax Limestone|34122|6|Mentioned|p302|||||||||
198|Ajax Limestone|34268|6|Mentioned|p241|||Cambrian||||||
198|Ajax Limestone|34269|6|Mentioned|Fig.2|||Cambrian. Copper mineralization||||||
198|Ajax Limestone|34291|5|Briefly described|p7|||Cambrian. See also pp8,30,31,79||||||17-JUL-06
198|Ajax Limestone|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian.||||||
198|Ajax Limestone|34766|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|35003|6|Mentioned|p122|||Analysis||||||
198|Ajax Limestone|35051|6|Mentioned|p203|||Analysis.||||||
198|Ajax Limestone|35255|6|Mentioned|Fig.8|||||||||
198|Ajax Limestone|35395|6|Mentioned|p102|||Stratigraphy||||||
198|Ajax Limestone|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
198|Ajax Limestone|35798|6|Mentioned|p311|||||||||
198|Ajax Limestone|35835|6|Mentioned|p201|||||||||
198|Ajax Limestone|36081|6|Mentioned|Fig.1|||||||||
198|Ajax Limestone|36083|4|Described|p473|||||||||
198|Ajax Limestone|36198|6|Mentioned|Fig.I.2|||||||||
198|Ajax Limestone|36495|6|Mentioned|Fig.12|||||||||
198|Ajax Limestone|36622|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|37113|6|Mentioned|Fig.1|||||||||
198|Ajax Limestone|37627|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|37802|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|39130|6|Mentioned|p183|||||||||
198|Ajax Limestone|39131|6|Mentioned|p186|||||||||
198|Ajax Limestone|39675|6|Mentioned|Fig.2|||||||||
198|Ajax Limestone|39904|6|Mentioned|p11|||||||||
198|Ajax Limestone|40642|6|Mentioned|p163|||||||||
198|Ajax Limestone|40810|5|Briefly described|p13|||||||||
198|Ajax Limestone|40852|6|Mentioned|p33|||See also Fig.3.7||||||
198|Ajax Limestone|40856|5|Briefly described|p312|||||||||
198|Ajax Limestone|40994|6|Mentioned|p236|||||||||
198|Ajax Limestone|40998|6|Mentioned|p441|||||||||
198|Ajax Limestone|41457|6|Mentioned|p1|||||||||
198|Ajax Limestone|41526|6|Mentioned|p11|||||||||
198|Ajax Limestone|41801|6|Mentioned|Fig.4|||||||||
198|Ajax Limestone|42011|4|Described|Fig.13 P474|||||||||
198|Ajax Limestone|42094|6|Mentioned|p20|||||||||
198|Ajax Limestone|42192|6|Mentioned|p10|||||||||
198|Ajax Limestone|42222|6|Mentioned|Table 1 P5|||||||||
198|Ajax Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
198|Ajax Limestone|42266|6|Mentioned|p299|||||||||
198|Ajax Limestone|42267|6|Mentioned|Fig.1 P319|||||||||
198|Ajax Limestone|42440|6|Mentioned|p601|||||||||
198|Ajax Limestone|42458|5|Briefly described|p699|||||||||17-JUL-06
198|Ajax Limestone|42469|5|Briefly described|p25|||||||||
198|Ajax Limestone|43781|6|Mentioned|p4||Early Cambrian|||||||
198|Ajax Limestone|44133|5|Briefly described|p3, 22, 4 Fig. 7.2|Botomian|Early Cambrian|Conformably overlies: Parachilna Formation. Geological Province: Arrowie Basin.||||||
198|Ajax Limestone|45155|6|Mentioned|Fig.8|||||||||17-JUL-06
198|Ajax Limestone|46957|6|Mentioned|p165|||||||||
198|Ajax Limestone|47035|6|Mentioned|p85|||||||||
198|Ajax Limestone|50150|6|Mentioned|p86|Cambrian|Cambrian|Contains archaeocyath fossil fragments.||||||18-FEB-05
198|Ajax Limestone|60264|6|Mentioned|p579|Early Cambrian|Early Cambrian|In the Scotts Ranges locality.||||||
198|Ajax Limestone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
198|Ajax Limestone|60889|5|Briefly described|p247 Fig.4, p249 Fig.6, p250 Fig.7|Early Cambrian|Early Cambrian|Shown as lower Ajax Limestone and upper Ajax Limestone in Fig.7. Upper boundary of Ajaxlower Wilkawillina Limestone is unconformable (Flinders Unconformity in Fig.6).|>528 Ma.|Hawker Group||Unconformably overlies Woodendinna Dolomite. Is overlain by Warragee Mem||21-SEP-17
198|Ajax Limestone|60990|5|Briefly described|p83, p85|Botoman|Atdbanian|Ajax Mine and Mount Scott Range. Biogeographic correlation with Cymbric Vale Formation. Faunal links with Antarctica.||Hawker Group.||||
198|Ajax Limestone|62784|6|Mentioned|p20, p28|Early Cambrian|Early Cambrian|At Mount Scott Range (SA), contains fossils apparently identical to Mongolitubulus henrikseni recovered from Mernmerna Formation, Hawker Group, Arrowie Basin.||||||
198|Ajax Limestone|62790|6|Mentioned|p206|Early Cambrian|Early Cambrian|Occurs in Mount Scott Range, Flinders Ranges. Contains the oldest (Abadiella huoi Zone) phosphatocopids in Australia. Described by Bengston (1990) as Indianidae gen. et spec. indet. A.||||||
198|Ajax Limestone|63447|5|Briefly described|p962, p963, Fig.2|Early Cambrian|Early Cambrian|Bioherm complexes form major part of unit.||||Shown as lateral equivalent to Mernmerna Formation, Oraparinna Shale. Overlain by Billy Creek Formation.|Generally consists of platform-derived archaeocyathan-calci-microbe limestone with a predominance of rubbly and argillaceous limestone.|
198|Ajax Limestone|63569|6|Mentioned|p117 Fig.1, pp121-122, p124|Early Cambrian|Early Cambrian|Arrowie Basin. Contains trilobite taxa from the Abadiella huoi Zone.||||||
198|Ajax Limestone|64319|5|Briefly described|p354, p355, p356 Fig.2, p357 Fig.3   |Cambrian|Cambrian|Hosts most of the nonsulfide zinc and sulfide Zn-Pb mineralisation in the Flinders Ranges; mainly where this unit contacts the Callanna Group antiforms.|||Includes Woodendinna Dolomite, and Lower and Upper Wilkawillina Limestone.|Overlies Parachilna Formation.||
198|Ajax Limestone|64829|5|Briefly described|p1090|||Contains marine archaeocyathids and shows local red breccias and paleokarst features created during exposure and dissolution.||||||07-FEB-11
198|Ajax Limestone|65379|5|Briefly described|p643, p644|Cambrian|Cambrian|Of Hawker Group, Moralana Supergroup. Limestone, reefs, flat-topped, keep-up. Lower thick bedded and upper nodular limestone. N.B.  Asbestos deposit host, contains Greenwood asbestos occurrence.||||||
198|Ajax Limestone|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Mount Scott Range area.||||Overlies Pound Sandstone.||18-FEB-11
198|Ajax Limestone|65686|6|Mentioned|p415 Fig 4|Early Cambrian|Early Cambrian|||||||
198|Ajax Limestone|65892|5|Briefly described|p9 Fig.4, p41-43.  |Early Cambrian|Early Cambrian|Arrowie Basin. Contains superbly preserved archaeocyatha, usually silicified. 14 species are in common with Gnalta Group of western New South Wales.||Unit in Hawker Group.||Overlies Billy Creek Formation.||
198|Ajax Limestone|65925|5|Briefly described|Appendix 2.||||||||Flat-topped, keep-up reefal limestone. Lower thick-bedded and upper nodular limestone.|
198|Ajax Limestone|67907|6|Mentioned|p256-260|Cambrian|Cambrian|Arrowie Basin[?], Mount Scott Range. See Brock et al. (2006) and Topper et al. (2011). Contains the cap-shaped mollusc, Emargimantus angulatus.||||Conformably underlain by Parachilna Formation.|Carbonate dominated including grey to buff bioclastic (commonly silicified) and nodular mottled limestone.|
198|Ajax Limestone|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
198|Ajax Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
198|Ajax Limestone|69570|5|Briefly described|p420, p423, p428|||Mount Scott Range. Hosts the earliest known bradoriid taxon from east Gondwana.||||Partially equivalent to the Winnitinny Creek Member.||
198|Ajax Limestone|70082|6|Mentioned|p9|Early Cambrian|Early Cambrian|||||||
198|Ajax Limestone|70833|5|Briefly described|p176,178-9,182-4,186,190,192||Terreneuvian|Of Arrowie Basin. Key sections: AJX-M and AJX-N (Mount Scott Range). Correlable to Wilkawillini and Wirrapowie limestones. Includes M. etheridgi zone. See also p194-5,199-201,203,205.||||Overlain by Billy Creek Formation. Underlain unconformably by Parachilna Formation.||
198|Ajax Limestone|70835|5|Briefly described|p334-338, 340, 342-343, 346, 351, 353|Cambrian|Cambrian|Mount Scott Range, Flinders Ranges. 239m thick. Contains silicified macro-scale univalves of Helcionellid and other species; systematic paleontology descriptions; photographs.||||Overlies Parachilna Formation. Is overlain unconformably by Billy Creek Formation.|Shallow-water microbial, stromatolitic and laminated limestones, dolomitised and generally unfossiliferous; overlain by richly fossiliferous nodular limestone beds and red massive bioclastic limestones.|
198|Ajax Limestone|71102|6|Mentioned|p249,254,267, p271|Series 2|Terreneuvian|Of Arrowie Basin.||||Correlable to Mernmerna Formation, Wirrapowie Limestone and Wilkawillina Limestone.||05-SEP-19
198|Ajax Limestone|73255|6|Mentioned|p542 Fig.10|early Cambrian|early Cambrian|||||||
218|Alberga Limestone|30056|6|Mentioned|Table 2|||||||||
218|Alberga Limestone|30807|6|Mentioned|p101|||Suggested mapping symbol.||||||
218|Alberga Limestone|31532|4|Described|Table 1|||||||||
218|Alberga Limestone|31699|6|Mentioned|p132|||||||||
218|Alberga Limestone|31968|6|Mentioned|p8|||Refers Freytag et al. (1967). ? correlative Mangatitja Lst.||||||
218|Alberga Limestone|32418|6|Mentioned|p2|||||||||
218|Alberga Limestone|33937|6|Mentioned|p11|||||||||
218|Alberga Limestone|36966|6|Mentioned|p86|||||||||
218|Alberga Limestone|40003|5|Briefly described|Table 15|||||||||
218|Alberga Limestone|40926|6|Mentioned|Table 3|||||||||
218|Alberga Limestone|44133|5|Briefly described|p190 Fig. 10.30|Middle Miocene|Early Miocene|Geological Province: Lake Eyre Basin.||||||16-AUG-05
218|Alberga Limestone|44658|14|Not recorded|map legend||Tertiary|M.Tertiary. Contains Mt. Alice Conglomerate Member. (G53-15).||||||
218|Alberga Limestone|66131|5|Briefly described|p240, p242 Fig.2, p243, p245|Miocene|Miocene|Said to be "also regarded as member of the Etadunna Formation". Age from Fig.2 - stratigraphic correlation chart.||||Correlative of the Caldelga Limestone and Etadunna Formation.||
218|Alberga Limestone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
218|Alberga Limestone|68715|6|Mentioned|p30 Fig.5|Serravallian|Burdigalian|Tirari and northern Callabonna sub basins, Lake Eyre Basin.||||||05-MAR-14
218|Alberga Limestone|69019|5|Briefly described|p105 Fig.25.|Miocene|Miocene|Tirari Sub-basin.||||Overlies Etadunna Formation.||
218|Alberga Limestone|69023|6|Mentioned|p108|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
218|Alberga Limestone|70336|5|Briefly described|Map legend|Miocene|Miocene||||||Cream, greenish, buff, fine-grained and chalcedonic limestone and dolomite; minor green clay. Reworked laterite and pebbly limestone.|
251|Aldgate Sandstone|9124|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Heavy mineral banded quartzite and arkose with conglomerates.||||||11-JAN-10
251|Aldgate Sandstone|22869|5|Briefly described|P38, Fig2||Neoproterozoic|Equivalent of the Emeroo Subgroup.||||||03-FEB-09
251|Aldgate Sandstone|22889|5|Briefly described|37|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Aldgate Sandstone of the southern Mount Lofty Ranges p31.||||||
251|Aldgate Sandstone|23731|6|Mentioned|p27|||||||||
251|Aldgate Sandstone|23818|6|Mentioned|p59|||Equivalent of the Rhynie Sandstone.||||||
251|Aldgate Sandstone|29697|6|Mentioned|p7|||||||||
251|Aldgate Sandstone|29758|6|Mentioned|p101|||||||||
251|Aldgate Sandstone|29776|6|Mentioned|p82|||||||||
251|Aldgate Sandstone|30801|6|Mentioned|p5|||See also P6. Table. Torrensian age.||||||
251|Aldgate Sandstone|30802|5|Briefly described|Table 1|||On p13||||||07-NOV-22
251|Aldgate Sandstone|30807|6|Mentioned|p103|||Suggested mapping symbol||||||
251|Aldgate Sandstone|31292|6|Mentioned|p3|||Refers Wilson (1952). Equated with Rhynie Sst.||||||
251|Aldgate Sandstone|31321|6|Mentioned|p26|||Friable for artificial sand||||||
251|Aldgate Sandstone|31322|6|Mentioned|p32|||Artificial sand production||||||
251|Aldgate Sandstone|31923|6|Mentioned|p9|||||||||
251|Aldgate Sandstone|32032|6|Mentioned|p7|||Unit of Burra Gp. Fig.2||||||
251|Aldgate Sandstone|32194|6|Mentioned|p283|||||||||
251|Aldgate Sandstone|32508|6|Mentioned|p119|||||||||
251|Aldgate Sandstone|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
251|Aldgate Sandstone|32725|5|Briefly described|p4|||Stratigraphy & Correlation||||||
251|Aldgate Sandstone|33423|4|Described|p12|||||||||
251|Aldgate Sandstone|33547|6|Mentioned|Fig.6|||||||||
251|Aldgate Sandstone|33659|5|Briefly described|Fig.1|||Permeability.  See also P6.||||||
251|Aldgate Sandstone|34308|6|Mentioned|p189|||||||||
251|Aldgate Sandstone|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
251|Aldgate Sandstone|34535|6|Mentioned|Fig.19|||Equiv. Rhynie Sst.||||||
251|Aldgate Sandstone|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
251|Aldgate Sandstone|34586|6|Mentioned|p27|||Torrensian||||||
251|Aldgate Sandstone|35255|6|Mentioned|Fig.6|||||||||
251|Aldgate Sandstone|35270|6|Mentioned|Fig.3|||||||||
251|Aldgate Sandstone|35328|6|Mentioned|p11|||||||||
251|Aldgate Sandstone|35354|6|Mentioned|Fig.2|||Regional geology||||||
251|Aldgate Sandstone|36626|6|Mentioned|Fig.1|||||||||
251|Aldgate Sandstone|37461|5|Briefly described|p337|||See also Table 5.I||||||
251|Aldgate Sandstone|37622|6|Mentioned|p16|||||||||
251|Aldgate Sandstone|38004|6|Mentioned|p81|||||||||
251|Aldgate Sandstone|38157|6|Mentioned|Table III|||||||||
251|Aldgate Sandstone|38926|6|Mentioned|p26|||||||||
251|Aldgate Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
251|Aldgate Sandstone|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
251|Aldgate Sandstone|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
251|Aldgate Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
251|Aldgate Sandstone|40003|5|Briefly described|p57|||See also Table 16||||||
251|Aldgate Sandstone|40228|5|Briefly described|Fig.1|||||||||
251|Aldgate Sandstone|40294|6|Mentioned|p8|||See also Table 2||||||
251|Aldgate Sandstone|40442|5|Briefly described|p8|||||||||
251|Aldgate Sandstone|40456|6|Mentioned|Fig.2|||||||||
251|Aldgate Sandstone|40500|5|Briefly described|Fig.2|||||||||
251|Aldgate Sandstone|40501|6|Mentioned|p115|||||||||
251|Aldgate Sandstone|40503|5|Briefly described|Fig.1|||||||||
251|Aldgate Sandstone|41401|6|Mentioned|p29|||||||||
251|Aldgate Sandstone|41403|5|Briefly described|p43|||||||||
251|Aldgate Sandstone|41404|3|Fully described|p80|||||||||
251|Aldgate Sandstone|41494|6|Mentioned|p27|||||||||
251|Aldgate Sandstone|41526|6|Mentioned|p39|||||||||
251|Aldgate Sandstone|42093|5|Briefly described|p6|||||||||
251|Aldgate Sandstone|42098|5|Briefly described|Table 2 P54|||||||||
251|Aldgate Sandstone|42222|6|Mentioned|Table 1 P4|||||||||
251|Aldgate Sandstone|42505|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Torrensian)|||||||
251|Aldgate Sandstone|42733|5|Briefly described|map legend|Adelaidean||||||||
251|Aldgate Sandstone|42813|6|Mentioned|p16|||||||||
251|Aldgate Sandstone|43052|5|Briefly described|p177,Table 6.1|||Emeroo Subgroup.||||||03-FEB-09
251|Aldgate Sandstone|43190|5|Briefly described|Fig.2p29,Fig.3.||Neoproterozoic|Actually spelt Aldgate SS,Age "Torrensian",Adelaidean. Of Burra Group.||||||
251|Aldgate Sandstone|44133|6|Mentioned|p46|||||||||
251|Aldgate Sandstone|50615|5|Briefly described|p303 Fig. 2, p306 Fig. 4|||Geological Province: Adelaide Fold Belt.||||||
251|Aldgate Sandstone|61307|5|Briefly described|p5, p12|Torrensian|Torrensian|Of the Burra Group. Geological Province: Adelaide Fold Belt. See also p25 Fig. 14.||||||15-JAN-08
251|Aldgate Sandstone|64647|4|Described|p38 Fig. 1, p39, p39 Fig. 2, p40, p45|Neoproterozoic|Neoproterozoic|Of Emeroo Subgroup. Feldspathic sandstone with titaniferous haematite laminations and muscovite. Cross-laminated.||||||
251|Aldgate Sandstone|64769|6|Mentioned|p28|Neoproterozoic|Neoproterozoic|SA.||||||05-MAY-09
251|Aldgate Sandstone|71237|14|Not recorded|p9|||||||||
251|Aldgate Sandstone|71238|14|Not recorded|p2, 9|||||||||
251|Aldgate Sandstone|71240|14|Not recorded|p6, p9|||||||Correlated with Rhynie Sandstone.||
251|Aldgate Sandstone|71529|14|Not recorded|p3|||||||||
251|Aldgate Sandstone|72450|6|Mentioned|Brochure|||Together with the Montacute Dolomite are the oldest sedimentary rocks deposited on the Barossa Complex basement. Overlain by a number of younger rocks including siltstone, sandstone and quartzite units. Deformed by the Delamerian Orogeny.||||||
251|Aldgate Sandstone|73188|5|Briefly described|p316, p326, p340|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Emeroo Subgroup, Burra Group|||Feldspathic sandstone, siltstone; strongly metamorphosed in places.|
251|Aldgate Sandstone|74367|5|Briefly described|p18|||Adelaide Superbasin. Interpreted to be at the base of the Burra Group.||Burra Group||Unconformably overlies Mount Crawford Granite Gneiss||
262|Algebuckina Sandstone|12597|6|Mentioned|p492 Tb.1, p498-499|Early Cretaceous|Pliensbachian|NW Eromanga Basin.||||||
262|Algebuckina Sandstone|13497|6|Mentioned|p115 fig 6.33|Late Jurassic|Middle Jurassic|Eromanga Basin. ||||||
262|Algebuckina Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Jurassic|In Eromanga Basin.||||||
262|Algebuckina Sandstone|22613|6|Mentioned|p17|||Eromanga Basin||||||
262|Algebuckina Sandstone|22874|6|Mentioned|P18|||||||||
262|Algebuckina Sandstone|22883|5|Briefly described|P31, Fig2|Early Cretaceous|Early Jurassic|Lateral equivalent of Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation, underlying unit is Poolowanna Formation.||||||16-SEP-08
262|Algebuckina Sandstone|22922|6|Mentioned|33 fig 2|||||||||
262|Algebuckina Sandstone|23054|5|Briefly described|p21-3,36|Neocomian|Late Jurassic|||||||
262|Algebuckina Sandstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.||||||
262|Algebuckina Sandstone|23155|4|Described|p30|Early Cretaceous|Early Jurassic|||||||
262|Algebuckina Sandstone|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
262|Algebuckina Sandstone|23818|4|Described|p141 Fig.65, p144 Fig.66|Late Jurassic|Late Jurassic|Geological Province: Great Artesian Basin. Max. thickness: ~70 ft.||||||
262|Algebuckina Sandstone|23830|5|Briefly described|Fig. 3a|Jurassic|Jurassic|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
262|Algebuckina Sandstone|23849|5|Briefly described|p781|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
262|Algebuckina Sandstone|24067|5|Briefly described|p249 Fig.2|Mesozoic|Mesozoic|Geological Province: Officer Basin.||||||
262|Algebuckina Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|24112|5|Briefly described|p254 Fig.2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin||||||
262|Algebuckina Sandstone|24176|5|Briefly described|p19, p22 Tb. 1|Late Jurassic|Late Jurassic|Equivalent to Village Well Formation.  Geological Province: Mount Painter Province.||||||
262|Algebuckina Sandstone|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|24321|5|Briefly described|Map legend|Tithonian|Kimmeridgian|||||||11-JAN-10
262|Algebuckina Sandstone|24506|5|Briefly described|p17|Mesozoic|Mesozoic|Considered to prospective for gold and diamonds.||||||
262|Algebuckina Sandstone|29379|4|Described|p30|||Lithology. Upper Jurassic-Lower Cretaceous.||||||
262|Algebuckina Sandstone|29591|6|Mentioned|p79|||||||||
262|Algebuckina Sandstone|29660|6|Mentioned|p6|||||||||
262|Algebuckina Sandstone|30176|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|30177|6|Mentioned|p101|||||||||
262|Algebuckina Sandstone|30514|6|Mentioned|p102|||||||||
262|Algebuckina Sandstone|30804|6|Mentioned|p7|||On table 2||||||
262|Algebuckina Sandstone|30807|6|Mentioned|p102|||Suggested mapping symbol||||||
262|Algebuckina Sandstone|30917|6|Mentioned|p42|||||||||
262|Algebuckina Sandstone|30918|6|Mentioned|p81|||||||||
262|Algebuckina Sandstone|30919|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|30921|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early to Late Jurassic||||||
262|Algebuckina Sandstone|30924|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|31244|5|Briefly described|p3|||Jurassic||||||
262|Algebuckina Sandstone|31248|6|Mentioned|p60|||Palynology correlation||||||
262|Algebuckina Sandstone|31532|6|Mentioned|Table 1|||||||||
262|Algebuckina Sandstone|31699|4|Described|p133|||Upper Jurassic.||||||17-JAN-08
262|Algebuckina Sandstone|31923|6|Mentioned|p14|||||||||
262|Algebuckina Sandstone|32033|6|Mentioned|p2|||||||||
262|Algebuckina Sandstone|32313|6|Mentioned|p164|||||||||
262|Algebuckina Sandstone|33075|6|Mentioned|p451|||||||||
262|Algebuckina Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
262|Algebuckina Sandstone|33224|6|Mentioned|p69|||Palynology||||||
262|Algebuckina Sandstone|33491|4|Described|p56|||Mention Fig.2.||||||17-JAN-08
262|Algebuckina Sandstone|33523|4|Described|p26|||See also p9.||||||17-JAN-08
262|Algebuckina Sandstone|33820|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|33821|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|33822|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|33823|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|33824|5|Briefly described|p7|||Table 2||||||
262|Algebuckina Sandstone|33825|4|Described|p8|||Lithology.||||||17-JAN-08
262|Algebuckina Sandstone|33827|6|Mentioned|p7|||Table 2||||||
262|Algebuckina Sandstone|33828|5|Briefly described|p5|||Table 1||||||
262|Algebuckina Sandstone|33829|6|Mentioned|p263|||||||||
262|Algebuckina Sandstone|33832|5|Briefly described|p7|||Stratigraphy||||||
262|Algebuckina Sandstone|33931|6|Mentioned|p9|||U.Jur.||||||
262|Algebuckina Sandstone|33936|6|Mentioned|Fig.3A|||Jurassic.||||||
262|Algebuckina Sandstone|33938|6|Mentioned|p20|||||||||
262|Algebuckina Sandstone|33939|2|Defined|p386|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
262|Algebuckina Sandstone|33942|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|33964|6|Mentioned|p6|||Correlation||||||
262|Algebuckina Sandstone|33970|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|33971|5|Briefly described|p37|||Refers Wopfner et al. (1970)||||||
262|Algebuckina Sandstone|33976|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|34611|4|Described|p146|||Jurassic. See Fig.65.||||||
262|Algebuckina Sandstone|34766|6|Mentioned|p58|||||||||
262|Algebuckina Sandstone|35080|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
262|Algebuckina Sandstone|35548|5|Briefly described|p18|||||||||
262|Algebuckina Sandstone|35549|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|35628|6|Mentioned|Table 4|||||||||
262|Algebuckina Sandstone|36214|5|Briefly described|p58|||||||||
262|Algebuckina Sandstone|36733|6|Mentioned|p14|||See also P53.||||||
262|Algebuckina Sandstone|36895|6|Mentioned|p9|||||||||
262|Algebuckina Sandstone|36922|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|38022|6|Mentioned|Fig.4|||||||||
262|Algebuckina Sandstone|38068|4|Described|p71|||||||||
262|Algebuckina Sandstone|38604|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|38605|4|Described|p20|||See also Table 4.||||||
262|Algebuckina Sandstone|38814|6|Mentioned|Table 1|||||||||
262|Algebuckina Sandstone|39211|5|Briefly described|Fig.6|||See also Figs 10,14,15, etc. Correlation||||||
262|Algebuckina Sandstone|39352|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|39629|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|40003|5|Briefly described|p33|||See also Fig.8||||||
262|Algebuckina Sandstone|40220|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|40670|6|Mentioned|Fig.9|||||||||
262|Algebuckina Sandstone|40910|6|Mentioned|p15|||See also P26||||||
262|Algebuckina Sandstone|40911|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|40912|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|40925|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|40926|3|Fully described|p13|||||||||
262|Algebuckina Sandstone|41060|6|Mentioned|p2|||||||||
262|Algebuckina Sandstone|41061|6|Mentioned|p20|||||||||
262|Algebuckina Sandstone|41063|2|Defined|p46|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
262|Algebuckina Sandstone|41084|5|Briefly described|p81|||||||||
262|Algebuckina Sandstone|41085|3|Fully described|p87|||||||||
262|Algebuckina Sandstone|41125|6|Mentioned|Table 10|||||||||
262|Algebuckina Sandstone|41165|5|Briefly described|p363, Fig.15|||||||||
262|Algebuckina Sandstone|41175|6|Mentioned|p196|||||||||
262|Algebuckina Sandstone|41183|6|Mentioned|Fig.3 p308|||||||||
262|Algebuckina Sandstone|41186|5|Briefly described|p212|||||||||
262|Algebuckina Sandstone|41187|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|41216|6|Mentioned|p300|||||||||
262|Algebuckina Sandstone|41266|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|41361|6|Mentioned|p5|||||||||
262|Algebuckina Sandstone|41523|6|Mentioned|p271|||||||||
262|Algebuckina Sandstone|41681|6|Mentioned|p22|||||||||
262|Algebuckina Sandstone|41724|6|Mentioned|p381|||||||||
262|Algebuckina Sandstone|41950|5|Briefly described|Fig.2 P3|||||||||
262|Algebuckina Sandstone|42071|6|Mentioned|Fig.2A P116|||||||||
262|Algebuckina Sandstone|42084|6|Mentioned|Fig.3 P356|||||||||
262|Algebuckina Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
262|Algebuckina Sandstone|42099|6|Mentioned|p62|||||||||
262|Algebuckina Sandstone|42283|6|Mentioned|p89|||||||||
262|Algebuckina Sandstone|42293|6|Mentioned|Fig.2 P.18|||||||||
262|Algebuckina Sandstone|42341|6|Mentioned|Fig.7 P57|||||||||
262|Algebuckina Sandstone|42346|5|Briefly described|p77, Fig.2 p79|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42357|6|Mentioned|p11|||||||||
262|Algebuckina Sandstone|42375|6|Mentioned|Fig. 28 P125|||||||||
262|Algebuckina Sandstone|42463|6|Mentioned|Fig.4 P171|||||||||
262|Algebuckina Sandstone|42465|5|Briefly described|Map Legend|||||||||
262|Algebuckina Sandstone|42469|4|Described|p27|||||||||
262|Algebuckina Sandstone|42504|5|Briefly described|p81|||||||||
262|Algebuckina Sandstone|42520|5|Briefly described|p6|||||||||
262|Algebuckina Sandstone|42546|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42736|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42746|4|Described|p9|||See also Fig.2, Fig.6.||||||
262|Algebuckina Sandstone|42816|4|Described|p17|||||||||
262|Algebuckina Sandstone|42899|5|Briefly described|p347|||||||||
262|Algebuckina Sandstone|42905|5|Briefly described|p19|||see also Fig 5.3||||||
262|Algebuckina Sandstone|43035|6|Mentioned|p27|||||||||
262|Algebuckina Sandstone|43048|5|Briefly described|p21|||||||||
262|Algebuckina Sandstone|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone.||||||25-MAY-05
262|Algebuckina Sandstone|43085|5|Briefly described|Fig.5|||||||||
262|Algebuckina Sandstone|43094|5|Briefly described|p36|||||||||
262|Algebuckina Sandstone|43105|5|Briefly described|Fig.9,p15|||||||||
262|Algebuckina Sandstone|43258|5|Briefly described|Map Legend||Jurassic|||||||
262|Algebuckina Sandstone|43298|5|Briefly described|Map Legend||Jurassic|||||||
262|Algebuckina Sandstone|43591|5|Briefly described|p28,40||Jurassic|||||||
262|Algebuckina Sandstone|43743|6|Mentioned|Fig.2,p33|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|43840|5|Briefly described|Fig3 p12|||Cretaceous-Jurassic age||||||12-JUL-16
262|Algebuckina Sandstone|44133|5|Briefly described|p75 Fig. 8.13, 106-108|Early Cretaceous|Early Jurassic|Geological Province: Eromanga Basin. Overlies: Poolowanna Formation. Thickness: 750m. ||||||
262|Algebuckina Sandstone|44289|5|Briefly described|Map Legend||Neocomian|||||||
262|Algebuckina Sandstone|44658|14|Not recorded|map legend|||? Jurassic (G53-15).||||||
262|Algebuckina Sandstone|44689|14|Not recorded|map legend|||Andamooka, (H53-12). Equivalent. Cretaceous. (lower??).||||||
262|Algebuckina Sandstone|44935|5|Briefly described|Map Legend||Late Jurassic|||||||
262|Algebuckina Sandstone|45041|6|Mentioned|p114|||||||||
262|Algebuckina Sandstone|46791|6|Mentioned|Table 2|||||||||
262|Algebuckina Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
262|Algebuckina Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
262|Algebuckina Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
262|Algebuckina Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Middle Jurassic|Overlies Poolowanna Formation; underlies Cadna-owie Formation. Lateral to Hutton Sandstone, Birkhead Formation and Namur Sandstone but relationship(s) unclear. Geological Province: Eromanga  Basin.||||||31-JAN-08
262|Algebuckina Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Jurassic|Fluvial sandstone.||||||
262|Algebuckina Sandstone|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse sands and grits, ferruginous sandstones.||||||13-APR-05
262|Algebuckina Sandstone|61108|5|Briefly described|map legend|Cretaceous|Jurassic|Fluvial sandstone.||||||
262|Algebuckina Sandstone|61615|6|Mentioned|p302 Fig. 2|Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
262|Algebuckina Sandstone|61823|6|Mentioned|p118|Cretaceous|Jurassic|Mentioned only in terms of equivalents. Geological Province: Eromanga Basin||||||09-JUN-06
262|Algebuckina Sandstone|61836|5|Briefly described|p211|Jurassic|Jurassic|Kaolin-rich, thick sedimentary unit. Geological Province: Eromanga Basin.||||||05-OCT-06
262|Algebuckina Sandstone|62537|6|Mentioned|p191 Fig.2. |Late Jurassic|Middle Jurassic|Eromanga Basin.||||Overlies Hutton Sandstone and Poolowanna Formation. Is overlain by Namur Sandstone.||
262|Algebuckina Sandstone|63894|5|Briefly described|p169|Early Cretaceous|Jurassic|Aquifer. Underlies Cadna-owie Formation. Overlies Proterozoic rocks.||||||
262|Algebuckina Sandstone|63979|5|Briefly described|p37 Fig. 44|Callovian|Toarcian|Overlain by Cadna-owie Formation.||||||07-FEB-11
262|Algebuckina Sandstone|64197|6|Mentioned|p630 Fig.6|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Underlies the Cadna-owie Formation.||
262|Algebuckina Sandstone|64665|5|Briefly described|p53 Fig.2, pp61-62.|Early Cretaceous|Early Jurassic|Eromanga Basin. Equivalent to Hutton Sandstone further east.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Jurassic|Jurassic|Geological province: Eromanga Basin. Braided fluvial deposits. See also p10, p14 Fig. 17.||||||
262|Algebuckina Sandstone|65309|4|Described|pp14-15,  pp19-20.|Jurassic|Jurassic|Fairly weathered outcrops preserved on summit and scarps of mesas and buttes in southeast Musgrave Block. Also known as De Souza Sandstone and, in Queensland, as Hooray Sandstone. Commonly 7-15m thick. Deposited by braided streams in broad plains.||||Overlies basement granite and gneiss. Disconformably overlies Idracowra Sandstone. Overlies Cadna-owie Formation in much of the Eromanga Basin. Probably unconformably overlies Langra Formation.|Friable, white, poorly sorted, kaolinitic, medium quartz sandstone; lesser well-rounded vein quartz conglomerate and angular quartz grit sandstone. Strongly cross-bedded.|
262|Algebuckina Sandstone|65342|6|Mentioned|p9.|||Eromanga Basin. Max. thickness at least 620 m.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|65374|5|Briefly described|p30||Cretaceous|||||||
262|Algebuckina Sandstone|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Jurassic||||||Fluvial to marginal marine sandstone.|
262|Algebuckina Sandstone|65385|5|Briefly described|pS128 Fig.2, pS133, pS134 Fig.7|Early Cretaceous|Early Jurassic|Of Eromanga Basin. Overlain by Cadna-owie Formation. Unit shown to contain two unconformities: Late Jurassic and around Jurassic-Cretaceous boundary. Sandstone, fine to coarse-grained, with granulite and pebble layers, and shale intraclasts. ||||||
262|Algebuckina Sandstone|65489|5|Briefly described|p17, p55, p58-62, p88, p96, p137, p139|Late Jurassic|Early Jurassic|See also p151, p154-156, p158-160. Eromanga Basin. 800m thick. Fair to excellent source and reservoir potential. Contains a hot groundwater resource of 130 degrees C at 2km depth. A component of the main artesian aquifer. Appears as Algebuckina Formation on p55 and 96.||||Overlies Poolowanna Formation. Is overlain by Cadna-owie Formation.|Sandstones with intraformational shales and coals.|
262|Algebuckina Sandstone|65925|5|Briefly described|p139, Appendix 2.|Mesozoic|Mesozoic||||||Fine- to coarse-grained sandstone with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. |||||Sandstone.|
262|Algebuckina Sandstone|66623|6|Mentioned|p247, p252.|||Equivalent in part to the Namur Sandstone.||||||
262|Algebuckina Sandstone|67058|5|Briefly described|p499 Fig. 3|Mesozoic|Mesozoic|Fluvial white kaolinitic sand||||||
262|Algebuckina Sandstone|67120|5|Briefly described|Map legend|Cretaceous|Jurassic||||||Sandstone, fine to coarse-grained, with granule and pebble layers, and shale intraclasts.|
262|Algebuckina Sandstone|67462|5|Briefly described|Map legend.|Late Jurassic|Jurassic|Eromanga Basin.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|67474|5|Briefly described|p56|||coarse-grained, unconsolidated sandstone with conglomerate bands. Aquifer unit in Great Artesian Basin.||||||21-DEC-11
262|Algebuckina Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Early Jurassic|Eromanga Basin. Subsurface only. Replaces Namur and Hutton Sandstones as they lens out towards the margin of the Basin.||||Is overlain by Hutton Sandstone.|Undifferentiated alluvial and fluvial deposits, chiefly white, medium- to coarse-grained, quartzose and pebbly, kaolinitic.|
262|Algebuckina Sandstone|68128|5|Briefly described|p14, p27, p43, p53, p71, p77, p83|Mesozoic|Mesozoic|Gawler Craton.|||||Sandstone, fine to coarse-grained with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|68131|5|Briefly described|p2 Fig.1, p77|Cretaceous|Jurassic|Fluvial to marginal marine deposits. Mapped with Cadna-owie Formation as one unit.|||||Sandstone.|
262|Algebuckina Sandstone|68713|6|Mentioned|p22|Cretaceous|Jurassic|Fluvial sedimentation - mostly derived from the Bopeechee Regolith.||||||
262|Algebuckina Sandstone|68715|6|Mentioned|p30 Fig.5|Berriasian|Bajocian|Eromanga Basin.||||||
262|Algebuckina Sandstone|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (SW). Fluvial to lacustrine. Pre-Barremian age.||||||16-JAN-17
262|Algebuckina Sandstone|69001|5|Briefly described|p11, pp15-17, p27, p33, p36, pp71-73|Early Cretaceous|Jurassic|Equivalent to locally defined units of McMinn (1981b) and/or Morton (1982) such as the Gum Vale Beds or Gum Vale Formation. Recent interpretations by the NSW DPI broadly group the Namur Sandstone, Poolowanna Formation, Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, and Murta Formation as equivalents to Algebuckina Sandstone also.||||Underlain by the Easter Monday Formation. Equivalent to the Cadna-Owie Formation and the Gum Vale Beds.|Terrestrial sediments: dominantly moderate- to high energy, cross-bedded fluvial sandstone and conglomerate.|08-NOV-13
262|Algebuckina Sandstone|69004|6|Mentioned|p12, p15|Cretaceous|Jurassic|Eromanga Basin.||||||
262|Algebuckina Sandstone|69019|3|Fully described|p83 Fig.20, p85-87, p168.|Early Cretaceous|Early Jurassic|SW Eromanga Basin. Of Wopfner et al. (1970) after Freytag et al. (1967). Type area is ~3 km S of Algebuckina Hill. Thickness varies from 5 to 114 m. A significant regional aquifer. Has been affected by silcrete processes.||||Overlies Poolowanna Formation. Is overlain gradationally to disconformably by Cadna-owie Formation or Parabarana Sandstone.|White or greyish, medium- to coarse-grained widespread non-marine quartzose and kaolinitic fluvial sandstone.|
262|Algebuckina Sandstone|69023|5|Briefly described|p79, p87, p89-91, p191-192|Early Cretaceous|Early Jurassic|Eromanga Basin. From ~167 to ~192m thick. In W Eromanga Basin, passes laterally into Namur Sandstone. Stratigraphic wells intersection data.||||Overlies Epsilon Formation. Lateral equivalent of Namur Sandstone. Is overlain by Murta Formation, and conformably by Parabarana Sandstone and Cadna-owie Formation.||
262|Algebuckina Sandstone|69203|6|Mentioned|p12|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|69372|6|Mentioned|p38|Jurassic|Jurassic|Eromanga Basin.|||||Kaolinite and sandstone.|
262|Algebuckina Sandstone|69454|5|Briefly described|p38:3, 7 Fig.38.6; 38:12-15|Early Cretaceous|Jurassic|Eromanga Basin. Has fair to good reservoir potential, sealed by Cadna-owie Formation basal shale.||||Overlies Poolowanna Formation.||12-JUL-16
262|Algebuckina Sandstone|69457|4|Described|p41:2-8, 14-16|Early Cretaceous|Early Jurassic|Wopfner et al. (1970). A thick (757m ) unit, widely distributed along western Eromanga Basin. Mapped as De Souza Sandstone in KULGERA, FINKE and RODINGA map areas, and as Hooray Sandstone in ILLOGWA CREEK map area. Fluviatile deposits. Mainly exposed as mesas and buttes. Laterally equivalent to a succession consisting of Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation. Toarcian to Berriasian age. Contains a zone of manganese enrichment at Umbeara. Has significant petroleum source potential; contained a 15m residual oil column in Blamore-1. May form reservoirs sealed by "Murta Member"/Cadna-owie Formation; it has good to excellent porosity and permeability, and forms a major artesian aquifer.||||Conformably (locally disconformably/unconformably) overlies, and intertongues with, Poolowanna Formation. Is overlain conformably by Cadna-owie Formation.|A thick succession of fine- to coarse-grained, quartzic continental sandstone, with granule and pebble layers; minor shale and siltstone. Shale intraclasts are common in coarser beds. Contains a variety of plant macrofossils.|12-JUL-16
262|Algebuckina Sandstone|69554|6|Mentioned|p131|Jurassic|Jurassic|Northern Gawler Craton.||||||
262|Algebuckina Sandstone|69562|6|Mentioned|p667 Fig.4, p668|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|69594|6|Mentioned|p524|||||||Conformably ovelries Poolowanna Formation.||
262|Algebuckina Sandstone|69648|5|Briefly described|p20, p28, p33, map legend|Early Cretaceous|Late Jurassic|Of Eromanga Basin. Interpreted equivalents, with latest Jurassic to Early Cretaceous palynofloras, have been intersected in Maralinga drillholes 3B, 6, and 7 (Alley, 1993). Reworking of Algebuckina Sandstone contributes to unnamed Quaternary donga and playa lake sediments on OOLDEA.|||||Interpreted equivalents: off-white, kaolinitic clay, in part sandy to gritty, and sandstone; faceted pebbles occur at base, and muscovite and pyrite are locally present; unit passes up into carbonaceous clay, silt and sand.|
262|Algebuckina Sandstone|69673|6|Mentioned|p160, p161|||Good reservoir rock. ||||Overlain by Cadna-owie Formation, overlies Poolowanna Formation||
262|Algebuckina Sandstone|69797|5|Briefly described|p17 Fig.2|||Age: Middle Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
262|Algebuckina Sandstone|69946|3|Fully described|p11-17,p19,p38,p44,p51,p56-57,p62-67|Early Cretaceous|Early Jurassic|Sprigg (1958). Type locality defined, and a reference section near Mount Anna given, by Wopfner et al. (1970). Eromanga Basin. Lateral equivalents include Hutton, Adori and Namur Sandstones and Birkhead, Westbourne and Murta Formations in the Cooper region. Up to 800m thick.||||Intertongues with and overlies Poolowanna Formation. Correlated with De Souza Sandstone (NT). Is overlain conformably by Cadna-owie Formation.|White, fine- to coarse-grained quartzose sandstone with granule and pebble layers and shale intraclasts common in coarser beds; minor lenses of siltstone and shale are locally developed.|
262|Algebuckina Sandstone|69947|5|Briefly described|p3, p13 Fig.7.2|Late Jurassic|Middle Jurassic|Eromanga Basin. Sand-rich lowstand deposits form significant hydrocarbon reservoirs.||||||
262|Algebuckina Sandstone|69948|6|Mentioned|Figs.4.1, 18|||Eromanga Basin.||||Overlies Purni Formation and (locally) Crown Point Formation unconformably, and Poolowanna Formation conformably. Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|70336|5|Briefly described|Map legend|Cretaceous|Jurassic||||||Fine- to coarse-grained sandstone with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|70338|5|Briefly described|Map legend.|Cretaceous|Jurassic||||||Sandstone, fine- to coarse-grained, with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|70383|5|Briefly described|p45|||Eromanga Basin. Fluvial sediments.||||Is overlain by Cadna-owie Formation and Bulldog Shale.||
262|Algebuckina Sandstone|70789|5|Briefly described|p320-321, p325|Late Jurassic|Late Jurassic|Gawler Craton. AFT results tabulated; central ages from 166 +/- 174 Ma to a more robust 255 +/- 25 Ma. This name is used interchangeably with Algebuckina Formation (see references p318, p324, p326, p328-329).||||||
262|Algebuckina Sandstone|70821|5|Briefly described|p21|Early Cretaceous|Jurassic|Eromanga Basin.||||Lateral equivalent to Hooray Sandstone.|Strongly cross-bedded fluvial sandstone.|
262|Algebuckina Sandstone|70823|5|Briefly described|p43|Early Cretaceous|Late Jurassic|Eromanga Basin. ||||Overlain by the Namur Sandstone.||
262|Algebuckina Sandstone|70938|5|Briefly described|p807-808, p814, p816|Late Jurassic|Late Jurassic||||||Medium- to coarse-grained sandstone, silicified at the top and containing plant fossils.|
262|Algebuckina Sandstone|71321|4|Described|p1,4,9,15,24-27,30, 65-66,68|Neocomian|Early Jurassic|Of Eromanga Basin. Deposited in a braided fluvial environment (Alexander et al., 2006). Forms a major artesian aquifer and a potential hydrocarbon reservoir rock (Cotton, et al., 2006); also a key target for sediment-hosted uranium mineralisation (Wilson et al., 2012). See p25 for detailed lithological descriptions from field observations. Spore-pollen microfossil assemblage indicate an Early Jurassic to Early Cretaceous (Neocomian) age range (Krieg et al., 1995). Traditionally difficult to differentiate Cadna-owie Formation from the underlying Algebuckina Formation in the TIEYON area, and included as part of Algebuckina Formation in the TIEYON area.||||Confomably overlain by Cadna-owie Formation or Bulldog Shale. Correlable with De Souza Sandstone. Overlies the Poolowanna Formation and basement unconformably.|Sandstone, fine- to coarse-grained, quartzose, with granule and pebbly layers, and shale intraclasts. Minor lenses of siltstone and shale are locally developed.|24-OCT-19
262|Algebuckina Sandstone|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p8, Ch4 p25|Valanginian|Toarcian|Eromanga Basin. Hosts a major confined aquifer. First introduced by Sprigg (1958b) for 'A gently dipping sequence of cross-bedded grits and sandstones'. In 1970 Wopfner et al defined the type section. In the Northern Territory the Algebuckina Sandstone is correlated with the lower De Souza Sandstone. A maximum thickness of 800m is recorded in the Poolowanna Trough. Spore-pollen zone is given in Ch5 p57. Equivalent to the Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation. Seal and reservoir characteristics discussed in Ch11. See also Ch5 p11-p12, Ch5 p14, Ch5 p17, Ch5 p19, Ch5 p30-p31, Ch5 p38, Ch5 p44, Ch5 p51, Ch5 p56-p57, Ch5 p62-p67, Ch6 p5-p7, Ch6 p14, Ch6 p18, Ch7 p3, Ch7 p13, Ch8 p4, Ch8 p28, Ch9 p3-p4, Ch9 p9-p11, Ch9 p18, Ch9 p21, Ch11 p4, Ch12 tbl 12.1, Ch12 p12-p14, Ch14 p3, Ch14 p5-p7.||||Conformably overlies the Poolowanna Formation. Unconformably overlies the Purni Formation or the Mount Toondina Formation. Conformably overlain by the Cadna-owie Formation.|White, fine to coarse-grained quartzose sandstone with granule and pebble layers and shale intraclasts common in the coarser beds. Minor lenses of siltstone and shale also occur.|
262|Algebuckina Sandstone|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
262|Algebuckina Sandstone|71415|5|Briefly described|p12|Early Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||Laterally equivalent to Namur Sandstone.||
262|Algebuckina Sandstone|71416|5|Briefly described|Map legend.|Cretaceous|Jurassic||||||Sandstone, massive to low-angle trough cross-bedded, immature, poorly to moderately sorted, medium- to coarse-grained quartzose fluvial sandstones containing angular to subrounded granules and pebbles of milky vein quartz.|
262|Algebuckina Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Poolowanna FZ. Is overlain by Cadna-owie FZ.||
262|Algebuckina Sandstone|72461|6|Mentioned|p24|Mesozoic|Mesozoic|||||||
262|Algebuckina Sandstone|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
262|Algebuckina Sandstone|72478|5|Briefly described|p6, p25-26, p82-83[doc],|Early Cretaceous|Late Jurassic|See also p51, 61, p70, p74 [of the document]. Aquifer is discussed.|c. 152 Ma-130 Ma|||Unconformably overlies the Mt Toondina Formation. Unconformably underlies the Cadna-owie Formation.||29-MAR-21
262|Algebuckina Sandstone|73099|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Eromanga basin.||||Overlies Mount Toondina Formation unconformably. Is overlain conformably by Cadna-owie Formation (Neales River Group).|Grey, pebbly, medium to coarse quartz sandstone with white claystone interbeds; clayey sandstone.|
262|Algebuckina Sandstone|73251|6|Mentioned|p54, p62|Cretaceous|Jurassic|Eromanga Basin. Hosts an aquifer in the northern Lake Frome district[?]||||Equivalent to Murta Formation, Namur Sandstone, Westbourne Formation, Adori Sandstone, Birkhead Formation, and Hutton Sandstone.||
262|Algebuckina Sandstone|73281|6|Mentioned|Appendix (DIP)|Jurassic|Jurassic|See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
291|Allaru Mudstone|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 150-400m thick. Mis-spelt as Allura Mudstone in Tb.1.|||||Calcareous mudstone with interbeds of calcareous siltstone and fine-grained, partly calcareous labile sandstone; contains a rich marine fauna of bivalves, ammonites, gastropods and belemnites.|
291|Allaru Mudstone|13497|5|Briefly described|p115 fig 6.33|Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the  Alluru Mudstone on p146. See also p144 fig 9.2, p145, p146, p148-p154 .||Marree Subgroup||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Albian|In Eromanga Basin.||||||
291|Allaru Mudstone|22747|6|Mentioned|p15|||||||||
291|Allaru Mudstone|22857|5|Briefly described|p296-7 Tb.22.1, p314|Albian|Albian|Of the Rolling Downs Group. Black and grey claystone. Max. thickness: ~100m. (inc. Toolebuc Mudstone). Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p544 App.1 Tb.A1.12.||||||
291|Allaru Mudstone|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
291|Allaru Mudstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Mackunda Formation, underlying unit is Toolebuc Formation||||||
291|Allaru Mudstone|22912|5|Briefly described|33|||Geological province: Eromanga  Basin.||||||30-JAN-07
291|Allaru Mudstone|23054|6|Mentioned|Fig5p22|||||||||
291|Allaru Mudstone|23056|6|Mentioned|12 table 2|||||||||
291|Allaru Mudstone|23065|5|Briefly described|18|||Geological province: Carpentaria Basin. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Marree Subgroup (Neales River Group).||||||30-JAN-07
291|Allaru Mudstone|23155|4|Described|p32|Albian|Albian|Allaru Mudstone is laterally equivalent to the middle and upper parts of the Oodnadatta Formation, and the name Allaru Mudstone is only used when Toolebuc Formation is present.  The unit is Albian in age based on spore-pollen assemblages.||||||29-APR-10
291|Allaru Mudstone|23375|4|Described|Fig2 p265||Albian|Laterally equivalent to upper Oodnadatta Formation. In the Eromanga Basin.||||||30-JAN-07
291|Allaru Mudstone|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|23425|4|Described|Table 9.7 p394||Albian|Also see p378. Of Rolling Downs Group. Overlain by Normanton Formation; underlain by Toolebuc Formation - conformable. Geological Province Carpentaria Basin. Max. thickness 700 m.||||||16-SEP-08
291|Allaru Mudstone|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
291|Allaru Mudstone|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
291|Allaru Mudstone|23916|6|Mentioned|p534|Albian|Albian|||||||
291|Allaru Mudstone|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
291|Allaru Mudstone|24048|5|Briefly described|p76|||||||||
291|Allaru Mudstone|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|24085|5|Briefly described|p33, p36|Albian|Albian|||||||
291|Allaru Mudstone|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24175|5|Briefly described|p28, p17 Fig. 3|Albian|Albian|Supersedes Allaru Member.  Transitionally overlain by Mackunda Formation.  Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
291|Allaru Mudstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Cooper Basin.||||||
291|Allaru Mudstone|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|29591|6|Mentioned|Table 72|||||||||
291|Allaru Mudstone|30019|6|Mentioned|p2|||||||||
291|Allaru Mudstone|30020|5|Briefly described|p30|||||||||
291|Allaru Mudstone|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30103|6|Mentioned|p6|||||||||
291|Allaru Mudstone|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30446|6|Mentioned|p38|||||||||
291|Allaru Mudstone|30539|6|Mentioned|p28|||Late middle Albian age||||||
291|Allaru Mudstone|30584|4|Described|Table 1|||||||||
291|Allaru Mudstone|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30691|4|Described|p17|||See also Table4,6.Lower Cretaceous. Part of Wilgunya Sub-group.||||||30-JAN-07
291|Allaru Mudstone|30804|5|Briefly described|Table 2|||||||||
291|Allaru Mudstone|30853|5|Briefly described|Table 3|||Albian age.||||||
291|Allaru Mudstone|30854|4|Described|Table 4|||Upper Albian age||||||
291|Allaru Mudstone|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit of Rolling Downs Group||||||
291|Allaru Mudstone|30856|4|Described|Table 3|||Lower Cretaceous||||||
291|Allaru Mudstone|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|31098|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31121|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
291|Allaru Mudstone|31164|14|Not recorded|p8||Albian|Blue grey mudstone minor calcareous labilie sandstone and cone-in-cone limestone,marine.||||||
291|Allaru Mudstone|31168|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31208|6|Mentioned|Fig. 7|||||||||
291|Allaru Mudstone|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone and labile sandstone.||||||02-DEC-04
291|Allaru Mudstone|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
291|Allaru Mudstone|31432|4|Described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31433|5|Briefly described|p6|||L.Cretaceous||||||
291|Allaru Mudstone|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous||||||17-JUL-06
291|Allaru Mudstone|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32275|5|Briefly described|p9|||||||||
291|Allaru Mudstone|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32314|6|Mentioned|Fig. 4|||||||||
291|Allaru Mudstone|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32395|4|Described|p6|||Stratigraphic table||||||
291|Allaru Mudstone|32396|6|Mentioned|p6,8||Early Cretaceous|Palynomorphs ? Cenomanian. Marine.||||||
291|Allaru Mudstone|32553|4|Described|p38|||||||||
291|Allaru Mudstone|32705|6|Mentioned|p188|||||||||
291|Allaru Mudstone|32796|6|Mentioned|p303|||||||||
291|Allaru Mudstone|33016|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33017|6|Mentioned|p5|||||||||
291|Allaru Mudstone|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
291|Allaru Mudstone|33069|4|Described|p7|||L.-U. Cret. Rolling Downs Gp.||||||22-DEC-09
291|Allaru Mudstone|33072|4|Described|Table 1|||L.Cret.||||||
291|Allaru Mudstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33075|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
291|Allaru Mudstone|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||22-DEC-09
291|Allaru Mudstone|33088|4|Described|Table 3|||L.Cret.||||||
291|Allaru Mudstone|33089|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33092|6|Mentioned|p6|||Strat. table.||||||
291|Allaru Mudstone|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33150|4|Described|p8|||L.Cret.||||||
291|Allaru Mudstone|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
291|Allaru Mudstone|33175|6|Mentioned|p280|||||||||
291|Allaru Mudstone|33176|6|Mentioned|p171|||||||||
291|Allaru Mudstone|33177|6|Mentioned|p12|||||||||
291|Allaru Mudstone|33178|6|Mentioned|p11|||||||||
291|Allaru Mudstone|33179|6|Mentioned|Table 3|||||||||
291|Allaru Mudstone|33182|6|Mentioned|Fig.1|||L. Cretaceous||||||
291|Allaru Mudstone|33183|5|Briefly described|p227|||Underlies Normanton Formation.||||||30-JAN-07
291|Allaru Mudstone|33368|6|Mentioned|p24|||Geol.Map.||||||
291|Allaru Mudstone|33372|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33414|6|Mentioned|p212,213,Tb.|||part of Wilgunya Sub-Group||||||
291|Allaru Mudstone|33448|6|Mentioned|p6|||||||||
291|Allaru Mudstone|33449|6|Mentioned|p7|||||||||
291|Allaru Mudstone|33561|6|Mentioned|p102|||||||||
291|Allaru Mudstone|33638|5|Briefly described|Table 1|||Lower Cret.||||||
291|Allaru Mudstone|33639|5|Briefly described|p11|||L.Cret. See also Table 4||||||
291|Allaru Mudstone|33640|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33642|5|Briefly described|p145,147,151,Table 1|||||||||
291|Allaru Mudstone|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33648|6|Mentioned|p21|||Strat.||||||
291|Allaru Mudstone|33772|6|Mentioned|p13|||||||||
291|Allaru Mudstone|33773|6|Mentioned|p17|||||||||
291|Allaru Mudstone|33825|6|Mentioned|Table 4|||||||||
291|Allaru Mudstone|33832|5|Briefly described|p11|||Strat. and correlation||||||17-JUL-06
291|Allaru Mudstone|33900|6|Mentioned|p21|||||||||
291|Allaru Mudstone|33964|4|Described|p6|||||||||
291|Allaru Mudstone|34065|4|Described|p6|||L.Cret.||||||
291|Allaru Mudstone|34091|4|Described|Table 1|||L.Cretaceous. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34218|5|Briefly described|Table 2|||Lower Cretaceous.||||||
291|Allaru Mudstone|34356|6|Mentioned|p21|||Lower Cretaceous.||||||
291|Allaru Mudstone|34485|6|Mentioned|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34486|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34611|4|Described|Fig.65|||Wilgunya Sub-Group.||||||16-SEP-08
291|Allaru Mudstone|34619|6|Mentioned|p.160, Pl.22||Early Cretaceous|||||||
291|Allaru Mudstone|34811|4|Described|Table 1|||||||||
291|Allaru Mudstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35139|4|Described|Table.2|||||||||
291|Allaru Mudstone|35239|6|Mentioned|p258|||||||||
291|Allaru Mudstone|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35560|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
291|Allaru Mudstone|35811|5|Briefly described|Table 3|||||||||
291|Allaru Mudstone|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
291|Allaru Mudstone|36012|3|Fully described|Table 5|||See also p20.||||||17-JUL-06
291|Allaru Mudstone|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|36243|6|Mentioned|Table 6A|||||||||
291|Allaru Mudstone|36251|4|Described|p3|||||||||
291|Allaru Mudstone|36552|6|Mentioned|Fig.25|||||||||
291|Allaru Mudstone|36571|6|Mentioned|p98|||See also Table 4.||||||
291|Allaru Mudstone|37263|6|Mentioned|Fig.14|||||||||
291|Allaru Mudstone|37451|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|37608|3|Fully described|Table 1|||See also Table 2||||||
291|Allaru Mudstone|38226|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|38372|6|Mentioned|p651|||||||||
291|Allaru Mudstone|38373|6|Mentioned|p622|||||||||
291|Allaru Mudstone|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
291|Allaru Mudstone|38780|6|Mentioned|p17|||||||||
291|Allaru Mudstone|38814|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation.||||||25-AUG-04
291|Allaru Mudstone|39070|4|Described|p365|||||||||
291|Allaru Mudstone|39211|5|Briefly described|Fig.3|||See also Figs 9,11-16,19 etc. Correlation||||||
291|Allaru Mudstone|39445|5|Briefly described|Table 11|||||||||
291|Allaru Mudstone|39478|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39575|6|Mentioned|p103|||||||||
291|Allaru Mudstone|39708|6|Mentioned|p478|||||||||
291|Allaru Mudstone|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39846|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|39847|5|Briefly described|p40|||||||||
291|Allaru Mudstone|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39943|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|39989|4|Described|p424|||||||||
291|Allaru Mudstone|40121|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|40199|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|40249|6|Mentioned|p41|||||||||
291|Allaru Mudstone|40452|6|Mentioned|p2|||||||||
291|Allaru Mudstone|40623|5|Briefly described|p111|||||||||
291|Allaru Mudstone|40648|6|Mentioned|p12|||||||||
291|Allaru Mudstone|40670|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|40675|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|40687|3|Fully described|p418|||||||||
291|Allaru Mudstone|40801|6|Mentioned|p42|||||||||
291|Allaru Mudstone|40833|6|Mentioned|p468|||||||||
291|Allaru Mudstone|40926|6|Mentioned|p18|||||||||
291|Allaru Mudstone|41012|5|Briefly described|p137|||||||||
291|Allaru Mudstone|41060|6|Mentioned|Fig.3|||Generalized stratigrapgy||||||
291|Allaru Mudstone|41062|6|Mentioned|Fig.5|||||||||
291|Allaru Mudstone|41063|6|Mentioned|p40|||||||||
291|Allaru Mudstone|41064|6|Mentioned|Fig.4|||||||||
291|Allaru Mudstone|41084|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41086|3|Fully described|p98, Fig.3|||||||||
291|Allaru Mudstone|41087|3|Fully described|p127|||||||||
291|Allaru Mudstone|41088|6|Mentioned|p141|||||||||
291|Allaru Mudstone|41097|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|41099|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|41117|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41121|6|Mentioned|p179|||||||||
291|Allaru Mudstone|41165|5|Briefly described|p362|||See also Fig.15||||||
291|Allaru Mudstone|41175|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|41176|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|41177|6|Mentioned|p225|||||||||
291|Allaru Mudstone|41178|6|Mentioned|p242|||||||||
291|Allaru Mudstone|41182|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41183|6|Mentioned|Fig.3 p308|||||||||
291|Allaru Mudstone|41187|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41214|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41216|6|Mentioned|Fig.18|||||||||
291|Allaru Mudstone|41266|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41306|6|Mentioned|p4|||||||||
291|Allaru Mudstone|41307|6|Mentioned|p5|||||||||
291|Allaru Mudstone|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41523|3|Fully described|p279|||See also p281.||||||
291|Allaru Mudstone|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41568|5|Briefly described|p15|||||||||
291|Allaru Mudstone|42003|6|Mentioned|p141|||||||||
291|Allaru Mudstone|42061|5|Briefly described|p157|||See also Fig.11||||||
291|Allaru Mudstone|42071|6|Mentioned|p117|||See also Fig.2A p116||||||
291|Allaru Mudstone|42084|6|Mentioned|Fig.3 P356|||||||||
291|Allaru Mudstone|42085|6|Mentioned|Fig.2 P374|||||||||
291|Allaru Mudstone|42397|6|Mentioned|Fig.2 P3|||||||||
291|Allaru Mudstone|42429|6|Mentioned|Fig.10 P156|||||||||
291|Allaru Mudstone|42446|4|Described|p14|||||||||
291|Allaru Mudstone|42447|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
291|Allaru Mudstone|42520|5|Briefly described|p6|||||||||
291|Allaru Mudstone|42588|5|Briefly described|p115|||||||||
291|Allaru Mudstone|42637|5|Briefly described|p11|||||||||
291|Allaru Mudstone|42673|5|Briefly described|Fig.2, P184|||||||||
291|Allaru Mudstone|42746|6|Mentioned|Fig.6 P8|||||||||
291|Allaru Mudstone|42749|6|Mentioned|Fig.2 P27|||||||||
291|Allaru Mudstone|42804|5|Briefly described|p115|||||||||
291|Allaru Mudstone|43002|5|Briefly described|Fig.2,p135|||||||||
291|Allaru Mudstone|43004|5|Briefly described|Table 1,p179|||||||||
291|Allaru Mudstone|43105|6|Mentioned|p15|||||||||
291|Allaru Mudstone|43114|5|Briefly described|p16|||||||||
291|Allaru Mudstone|43122|5|Briefly described|Fig.2.|||||||||
291|Allaru Mudstone|43591|6|Mentioned|p40|||||||||
291|Allaru Mudstone|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
291|Allaru Mudstone|43630|6|Mentioned|p70|||also Fig.4||||||
291|Allaru Mudstone|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Gruop.||||||
291|Allaru Mudstone|44031|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|44034|4|Described|Tb.1,p2,4,5,9,10|||||||||
291|Allaru Mudstone|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44082|6|Mentioned|p3,4,10,12,20,24,28||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
291|Allaru Mudstone|44091|14|Not recorded|p60|||Part of Wilgunya Sub-Group.||||||
291|Allaru Mudstone|44098|14|Not recorded|p98||Cretaceous|||||||
291|Allaru Mudstone|44112|6|Mentioned|p82|||||||||
291|Allaru Mudstone|44133|5|Briefly described|p104 Fig. 9.11, 122|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Conformably underlies: Mackunda Formation.||||||
291|Allaru Mudstone|44308|14|Not recorded|p11|||||||||
291|Allaru Mudstone|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44807|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|45103|6|Mentioned|p8|||||||||
291|Allaru Mudstone|45110|6|Mentioned|Table 18|||||||||
291|Allaru Mudstone|45132|6|Mentioned|p17|||||||||
291|Allaru Mudstone|45145|3|Fully described|Table 5|||||||||
291|Allaru Mudstone|45161|6|Mentioned|p67|||||||||
291|Allaru Mudstone|46791|5|Briefly described|p48|||||||||
291|Allaru Mudstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
291|Allaru Mudstone|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
291|Allaru Mudstone|47042|6|Mentioned|p171|||||||||
291|Allaru Mudstone|48920|3|Fully described|p61|||Cretaceous age||||||
291|Allaru Mudstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
291|Allaru Mudstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
291|Allaru Mudstone|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|50332|5|Briefly described|p22|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
291|Allaru Mudstone|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, labile sandstone.||||||19-JUL-04
291|Allaru Mudstone|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Toolebuc Formation. Overlain by the Mackunda Formation. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, calcareous siltstone.||||||
291|Allaru Mudstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation. Overlain by Mackunda Formation. Interfingers laterally with Oodnadatta Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
291|Allaru Mudstone|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wallumbilla Formation.||
291|Allaru Mudstone|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of Rolling Downs Group. In Queensland, consists of mainly blue-grey mudstone with interbeds of thin calcareous siltstone. Forms marine deposits in deeper parts of the Eromanga Basin. Absent in NSW. Overlies Toolebuc Formation. See also p64, p67 Fig. E5||||||
291|Allaru Mudstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
291|Allaru Mudstone|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|62028|5|Briefly described|p10 Fig. 1|||||||||
291|Allaru Mudstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin?||||||11-FEB-10
291|Allaru Mudstone|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Age: ~96-~94Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
291|Allaru Mudstone|63113|6|Mentioned|p1219 Fig.8. |||||||Overlies Lawn Hill Formation.||
291|Allaru Mudstone|63979|2|Defined|p49, p51-52, Fig. 44|Albian|Albian|Top unit of Wilgunyah Subgroup (Rolling Downs Gp). Formerly Allaru Member (Wilgunyah Fm). Conformable on Toolebuc Formation or Wallumbilla Formation;conformable below Mackunda Fm. Max.thick: 400m. Detailed lithology provided. Geol.prov: Eromanga Basin|||||Primarily blue-grey mudstone (partly pyritic) and interbedded calcareous siltstone, cone-in-cone limestone and lesser sandstone.|29-APR-16
291|Allaru Mudstone|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Toolebuc Formation; is overlain by Mackunda Formation.||10-DEC-15
291|Allaru Mudstone|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
291|Allaru Mudstone|64820|5|Briefly described|pS6 Fig. 4|Albian|Albian|Of the Rolling Downs Group. Medium-grained galuconitic sandstone grading up into interbedded siltstone and sandstone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
291|Allaru Mudstone|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||17-FEB-10
291|Allaru Mudstone|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Toolebuc Formation. Overlain by Mackunda Formation.||||||08-MAR-12
291|Allaru Mudstone|65489|5|Briefly described|p49, p55, p58-59, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 300m thick. Appears as Allaru Formation on p155. Regional seal.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|65925|5|Briefly described|Appendix 2.|||||||||
291|Allaru Mudstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. ||Unit in Rolling Downs Group.|||Deeper marine shale and mudstone.|
291|Allaru Mudstone|66623|3|Fully described|p242, pp256-257, pp264-266.|Albian|Albian|Formerly a member of Wilgunya Formation (Casey 1959), Allaru Member (Vine and Day 1965), reinstated as a Formation (Vine et al. 1967). Very poorly exposed: mudstone-dominated and masked by silcrete gibbers. Thickness from 87 m to 270 m. Wide range of fossils. Partly equivalent to Griman Creek and Oodnadatta Formations,Yalpunga Formation, lower half of Yalpunga Beds, and to the diachronous base of Mackunda Formation.||Unit in Rolling Downs Group.||Is conformably overlain by Winton Formation. In QLD, overlies Toolebuc Formation and underlies Mackunda Formation. Gradationally overlies Coreena Member (Wallumbilla Formation).|Blue shale with interbedded buff to grey, calcareous, fossiliferous fine silty sandstone, siltstone and mudstone; local gypsiferous concretions of calcareous, chocolate-brown shale exhibit cone-in-cone structures.|07-JUN-13
291|Allaru Mudstone|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Carpentaria and Eromanga Basins.||||||
291|Allaru Mudstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.||Overlies Coreena Member of Wallumbilla Formation. Is overlain by Cordillo Silcrete.|Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Late Cretaceous|Late Cretaceous|See also p86-87, p92-93, p94 Fig.12.4, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Widespread shallow-marine deposits.||||Overlies Toolebuc Formation. Is overlain by Mackunda, Normanton Formations.|Mudstone, calcareous siltstone.|
291|Allaru Mudstone|67402|4|Described|p26, p26 tbl RRM4, p29, p29 fig PSA4|Albian|Albian|Eromanga Basin. Maximum thickness of 400m in the Eromanga Basin but may be up to 700m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. See also PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p123, p176, p177, p179 fig CRP/KRM6, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Mackunda Formation.|Consists primarily of marine mudstone interbedded with calcareous siltstone, very fine-grained, laminated sandstone, shale and limestone.|
291|Allaru Mudstone|67784|6|Mentioned|p28-29, p33|Albian|Albian|See also references to Allaru Formation (p25-26, p32).||||||08-FEB-18
291|Allaru Mudstone|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
291|Allaru Mudstone|68206|6|Mentioned|p32|Albian|Albian|NE Eromanga Basin. See also references to Allaru Formation (p31, 33).||||||
291|Allaru Mudstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
291|Allaru Mudstone|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation.||
291|Allaru Mudstone|68731|6|Mentioned|pp209-211|||||||||
291|Allaru Mudstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
291|Allaru Mudstone|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Winton and Mackunda Formations.||
291|Allaru Mudstone|69023|6|Mentioned|p89 Fig.20, p102, p105|Albian|Albian|||||Lateral equivalent of Oodnadatta Formation.||
291|Allaru Mudstone|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
291|Allaru Mudstone|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. This unit is a good potential seal. ||Rolling Downs Group||Overlies the Toolebuc Formation. Overlain by the Normanton Formation.|Mudstone, siltstone and claystone.|
291|Allaru Mudstone|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
291|Allaru Mudstone|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
291|Allaru Mudstone|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,17-18|Early Cretaceous|Early Cretaceous|Vine and Day (1965); Vine et al. (1967). Widely distributed: Eromanga and Carpentaria Basins. Entirely subsurface in NT. Quiet water, shallow-marine deposits; generally 200-300m thick, up to 400m. Laterally equivalent to middle and upper parts of Oodnadatta Formation; this latter name was previously used to describe the Allaru Mudstone in the NT. Late Albian to ?early Cenomanian age range from palynoflora. The basal part of this unit contains a 40m thick gas-charged interval, and has untested unconventional petroleum potential.||Wilgunya Subgroup.||Conformably overlies Toolebuc or Wallumbilla Formations. Is overlain conformably by Mackunda Formation. Correlative of Oodnadatta Formation.|Mostly blue-grey, partly pyritic mudstone with calcareous siltstone interbeds, cone-in-cone limestone; minor sandstone and limestone. Contains a rich fossil assemblage.|12-JUL-16
291|Allaru Mudstone|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Upper Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Toolebuc Formation. Overlain by the Normation Formation and the Mackunda Formation.|Mudstone.|
291|Allaru Mudstone|69594|4|Described|p518-519, p521-522, p526, p529-530|Albian|Albian|See also p531 Fig.7.11, p574. Vine et al. (1967); Vine and Day (1965). Carpentaria, Eromanga Basins. Generally 200-300m thick; up to 350-400m. Generally poor surface expression. Contains rich shallow-marine late Albian macrofauna and microfauna (listed and photographs). Seismic interpretations suggest a significant intraformational unconformity. Appears as Allaru Formation in Fig.7.11.||Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain (conformably) by Normanton, Winton and Mackunda Formations. Is correlated with the Oodnadatta Formation.|Claystone, siltstone, cone-in-cone calcareous mudstone, minor limestone, labile volcanic-derived sandstone, glauconitic sandstone and sporadic coquinite.|
291|Allaru Mudstone|69673|5|Briefly described|ix, p155 fig 127, p156|||Prospective for unconventional hydrocarbons. 200-300m thick.||Wilgunya Subgroup||Overlies Toolebuc Formation, overlain by Mackunda Formation|Mudstone, in parts pyritic with thin interbeds of calcareous siltstone, cone in cone limestone and minor very fine grained sandstone and concretionary limestone.|
291|Allaru Mudstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
291|Allaru Mudstone|69946|3|Fully described|p23, p26-27, p57, p94|Early Cretaceous|Early Cretaceous|Of Casey (1959), who assigned it as the uppermost Member of the Wilgunya Formation. Renamed Allaru Member by Vine and Day (1965); raised to Formation status as Allaru Mudstone by Vine et al. (1967). Type section is on the Richmond-Winton Road, from Richmond S to Twenty-Mile Creek. Its extent is limited by definition to the extent of the Toolebuc Formation. Generally 100-240m thick, to >600m. Late Albian. Wireline log correlations.||||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation. Passes laterally into Oodnadatta Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
291|Allaru Mudstone|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Toolebuc Formation.|Mudstone and calcareous siltstone.|
291|Allaru Mudstone|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone, calcareous siltstone.|20-JAN-22
291|Allaru Mudstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|20-JAN-22
291|Allaru Mudstone|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p30, p33|Early Cretaceous|Early Cretaceous|See also p80, p82. Surat Basin. Not an equivalent of Oodnadatta Formation.  87m thick in Toompine 1 well; 212.5m thick in Mirintu 1 petroleum well. Low-energy marine deposits. Biotas include benthic and nektonic molluscs, turtles, fish, pliosaurs and a dinosaur. Hydrostratigraphic properties.||Rolling Downs Group.||Conformably overlies Toolebuc Formation or Wallumbilla Formation. Is overlain conformably by Mackunda Formation.|Includes minor calcareous labile (volcanic) sandstone. Includes coquinite beds and hummocky crossbeds.|
291|Allaru Mudstone|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
291|Allaru Mudstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||24-OCT-19
291|Allaru Mudstone|71342|3|Fully described|Ch3 p4, Ch4 p25|Albian|Albian|Eromanga Basin. Originally named by Casey (1959) as the uppermost member of the Wilgunya Formation. Vine and Day (1965) assigned the name Allaru Member before Vine et al (1967) elevated the mudstone to formation status. Replaces the obsolete Tambo Formation. Casey (1959) assigned the type section on the Richmond-Winton road from Richmond south to Twenty-Mile Creek in Queensland. This unit is generally 100-240m thick in the Cooper region but reaches thicknesses in excess of 600m in the Patchawarra Trough. Deposited in a low energy, shallow marine environment. Spore-pollen zone is given in Ch5 p57. Forms a seal for the Coorikiana Sandstone. See also  Ch5 p23-p27, Ch5 p57, Ch7 p13, Ch11 p5.||||Conformably overlies the Toolebuc Formation. Conformably overlain by the Mackunda Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|71382|5|Briefly described|p4, p9, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 0-156.65m for a total of 156.65m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p22. See also p21-p23, p25, p27, App 3, 4.||||Overlies the Toolebuc Formation.|Mudstone interbedded with sandstone.|07-OCT-22
291|Allaru Mudstone|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
291|Allaru Mudstone|71855|4|Described|p2, p4-p5, p9-p10, p13, p15, p27|Cretaceous|Cretaceous|Eromanga and Carpentaria basins. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p33-p35, p50, p52-p53, p56-p57, p61-p62, p75.||||Conformably (gradationally) overlies the Toolebuc Formation.|Light grey, predominantly non-calcareous mudstone, and calcareous in part mudstone.|
291|Allaru Mudstone|71863|5|Briefly described|p4-p5, p7-p9|Albian|Albian|Eromanga Basin and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group||Conformably overlies the Toolebuc Formation. Overlain by the Normanton Formation, Mackunda Formation and the Winton Formation.||
291|Allaru Mudstone|72297|5|Briefly described|p753|||Eromanga Basin.||||Conformably overlies the Toolebuc Formation.||
291|Allaru Mudstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Toolebuc FZ. Is overlain by Mackunda or Normanhurst FZ.||
291|Allaru Mudstone|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.|||||Includes mudstone.|
291|Allaru Mudstone|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
291|Allaru Mudstone|73083|6|Mentioned|p62, p77|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Toolebuc Formation. Overlain by Normanton Formation.||
291|Allaru Mudstone|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Toolebuc Formation. Is overlain by Normanton Formation.||
291|Allaru Mudstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
291|Allaru Mudstone|73249|5|Briefly described|p319, p321||Albian|Eromanga Basin.||||Lateral equivalent to the Oodnadatta Formation, overlies the Allaru Formation, underlies the Mackunda Formation.|Siltstone and mudstone dominated.|
291|Allaru Mudstone|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
291|Allaru Mudstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 100 Ma|||Overlies Toolebuc Formation, underlies Mackunda Formation||
353|Amberoona Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Grey-green or dark grey laminated siltstone sometimes with slate, dolomite.||||||05-JUL-13
353|Amberoona Formation|22510|5|Briefly described|table1p37,41|||Of the Upalinna Subgroup.  Age: Marinoan. Northern Flinders Ranges||||||05-JUL-13
353|Amberoona Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
353|Amberoona Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Farina Subgroup (Umberatana Group). Age: <610Ma.||||||
353|Amberoona Formation|23054|5|Briefly described|p14-5|||||||||
353|Amberoona Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
353|Amberoona Formation|23411|6|Mentioned|Map Legend|||||||||
353|Amberoona Formation|23804|6|Mentioned|p17|||||||||
353|Amberoona Formation|23818|5|Briefly described|p64 Fig.22|Neoproterozoic|Neoproterozoic|Of the Farina Sub-Group.||||||
353|Amberoona Formation|24175|4|Described|p13|Neoproterozoic|Neoproterozoic|Of Farina Subgroup.  Shows pronounced angular unconformity with Tapley Hill Formation.  Overlain by Fortress Hill Formation (Yerelena Subgroup) in eastern area.   Max. thickness: 1700m.||||||
353|Amberoona Formation|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Farina Sub-Group.  Grey-green siltstones, minor shales and sandy limestones.  Overlies Balcoona Formation.  Intertongues with Angepena Formation.  Max. thickness: 1220m. Age is Marinoan.  Geological Province: Mount Painter Province.||||||
353|Amberoona Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Farina Subgroup||||||11-JAN-10
353|Amberoona Formation|29656|4|Described|Fig.3|||||||||
353|Amberoona Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
353|Amberoona Formation|30177|4|Described|p81|||See also p82.||||||17-JUL-20
353|Amberoona Formation|30261|6|Mentioned|Table 1|||Marinoan age||||||
353|Amberoona Formation|30801|6|Mentioned|p5|||See also P6. Table Marinoan||||||
353|Amberoona Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
353|Amberoona Formation|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|Rodda Beds approx equiv.Marinoan||||||
353|Amberoona Formation|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
353|Amberoona Formation|32823|6|Mentioned|p361|||||||||
353|Amberoona Formation|33474|6|Mentioned|Fig.2|||||||||
353|Amberoona Formation|34011|5|Briefly described|p67|||Sil.||||||
353|Amberoona Formation|34175|6|Mentioned|p36|||||||||
353|Amberoona Formation|34268|6|Mentioned|p241|||U.Prot.||||||
353|Amberoona Formation|34269|6|Mentioned|Table 1|||U.Prot.||||||
353|Amberoona Formation|34534|6|Mentioned|Fig.2.13|||Marinoan||||||
353|Amberoona Formation|34535|6|Mentioned|p69|||Fig.22||||||
353|Amberoona Formation|34766|6|Mentioned|p58|||||||||
353|Amberoona Formation|35255|6|Mentioned|Fig.7|||||||||
353|Amberoona Formation|35628|6|Mentioned|Table 2|||||||||
353|Amberoona Formation|36733|6|Mentioned|Table 5|||||||||
353|Amberoona Formation|37461|6|Mentioned|p341|||||||||
353|Amberoona Formation|37932|6|Mentioned|p546|||||||||
353|Amberoona Formation|38022|6|Mentioned|Fig.4|||||||||
353|Amberoona Formation|38157|6|Mentioned|p272|||||||||
353|Amberoona Formation|38329|6|Mentioned|p192|||||||||
353|Amberoona Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
353|Amberoona Formation|41364|5|Briefly described|p153|||||||||
353|Amberoona Formation|41405|3|Fully described|p174|||||||||
353|Amberoona Formation|41526|6|Mentioned|p43|||||||||
353|Amberoona Formation|41647|6|Mentioned|Fig.2|||||||||
353|Amberoona Formation|41770|6|Mentioned|Fig.1|||||||||
353|Amberoona Formation|42087|5|Briefly described|Fig.2 P15|||||||||
353|Amberoona Formation|42090|5|Briefly described|p25|||||||||
353|Amberoona Formation|42109|5|Briefly described|p23|||||||||
353|Amberoona Formation|42222|6|Mentioned|p17|||||||||
353|Amberoona Formation|42238|5|Briefly described|p77|||||||||
353|Amberoona Formation|42239|6|Mentioned|p161|||||||||
353|Amberoona Formation|43052|5|Briefly described|p190,Table 6.1|||||||||
353|Amberoona Formation|43845|5|Briefly described|p44|||||||||12-JUL-16
353|Amberoona Formation|44133|6|Mentioned|p100 Fig. 9.8|Adelaidian|Adeladian|||||||
353|Amberoona Formation|44289|5|Briefly described|Map Legend||Proterozoic|||||||
353|Amberoona Formation|44689|14|Not recorded|map legend|||Andamooka, (H53-12).||||||
353|Amberoona Formation|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Upalinna Subgroup (Umberatana Group).|Includes Wundowie Limestone Member.|Unconformably overlies Tapley Hill Formation.||15-APR-11
353|Amberoona Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Includes Enorama Shale. Green siltstones, yellow weathering gritty dolomites, calcareous grits and sandstones.||||||13-APR-05
353|Amberoona Formation|64797|5|Briefly described|p161, p162 Fig.9, p163, p166 Tb.7|||See also p168 Tb.11. S-isotope data.||||||
353|Amberoona Formation|64846|5|Briefly described|p197-200 Figs.2-5, p202 Tb.1, p203 |Cryogenian|Cryogenian|See also p205-206 Tb.2.||Of the Upalinna Subgroup.|||Shallow-water stromatolitic limestones with interbedded shales.|
353|Amberoona Formation|65493|5|Briefly described|p915-16,922,924, Fig 1,2,4,12, 14,17|Cryogenian|Cryogenian|Of Upalinna Subgroup. Overlies the Balcanoona Formation with a sharp unconformity, with cavities filled with sandstone, breccias. Stromatolitic limestone, grey calcareous shale and siltstone.||||||
353|Amberoona Formation|65925|5|Briefly described|Appendix 2.||||||||Shales, green, finely laminated, silty; with purple and grey silty shale.|
353|Amberoona Formation|67180|4|Described|p606, p609-610, Figs. 1, 2, 4, 7, 10|Cryogenian|Cryogenian|Marinoan age. Defined by Coats in Thompson et al. 1964. Presence not recognised by Coats and Blisset 1971. >240 m thickness in basinal settings such as the Illinawortina, rarely >100 m thickness in shallow water carbonate successions. ||Unit in Upalinna Subgroup||Conformably (gradationally) overlies Weetootla Dolomite Member, Yankaninna Formation. Conformably underlies Enorama Shale.|Grey coloured fine-grained, calcareous/dolomitic silts and shales, stromatolitic dolomite, poorly developed stromatolite beds.|
353|Amberoona Formation|67979|4|Described|p536, p529-531, p534, ,p541,p543,p545|Marinoan|Marinoan|Max thickness?: 190 m in Illinawortina area. Slightly deeper marine facies shift between this unit and its shallow marine carbonate correlative Etina Formation. Presented as Amb. Fm in Fig.5. See Figs.1, 2 and 5.||Upalinna Subgroup||conformably/gradationally overlies Yankaninna Fmn, Weetootla Dolomite; conformably overlain by Wundowie Limestone Member (Enorama Shale). Laterally correlates with Etina Formation.|deeper marine calcareous siltstone and sandstone succession; contains some sporadic and thin stromatolitic limestone beds in Illinawortina area|
353|Amberoona Formation|68068|5|Briefly described|Map legend|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Overlies Yankaninna Formation conformably.|Finely-laminated green to grey-green siltstone.|28-AUG-13
353|Amberoona Formation|69019|3|Fully described|p49, p50-51, p160.|Neoproterozoic|Neoproterozoic|Of Coats (1964); modified by Coats and Blissett (1971) to exclude the upper gritty pebble unit (assigned to Fortress Hill Formation by Preiss, 1987). Thickness from <350 m to c.1,000 m. Early to mid-Marinoan. Hosts the Billy Springs Mine (Zn-Pb-Cu-Ag) of limited economic outlook.||||Overlies Tapley Hill Formation unconformably. Is overlain disconformably by Fortress Hill Formation.|Basal calcareous lag or breccia; monotonous succession of laminated non-calcareous dark green or dark grey siltstone; some purple and grey slate; minor sandstone, limestone, dolomite.|
353|Amberoona Formation|69023|5|Briefly described|p67, p70-72|Neoproterozoic|Neoproterozoic|Defined by Coats (1964); redefined by Coats and Blissett (1971) to exclude the basal gritty pebble unit; this latter was subsequently included in the Fortress Hill Formation (Preiss, 1987). Preiss et al. (1988) placed the Amberoona Formation above the basal Marinoan unconformity. Early to mid-Marinoan. c.380m thick.||||Is faulted against Bolla Bollana Tillite and Balcanoona Formation (which also overlies it [??]).|Finely and evenly laminated non-calcareous green siltstone, with rare minor cross-bedding. Grey to yellow weathering discolouration near the exposed surface may represent pyrite bodies; moderately developed cleavage.|17-JUL-20
353|Amberoona Formation|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
353|Amberoona Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Onlaps an eroded surface of significant relief and includes a discontinuous basal lag.  Age shown more specifically as Marinoan [Cryogenian].||Of Upalinna Subgroup.|Unclear if includes Weetootla Dolomite Member or not.|Disconformably overlies Weetootla Dolomite Member.|Monotonous sequence of dark grey-green or dark grey, finely laminated siltstone, sometimes with purple and grey slate. Includes an upper, sandy buff-yellow dolostone (separately mapped). Slumped intraformational zones of regional extent.|23-JAN-19
353|Amberoona Formation|71237|2|Defined|p7, 10, 11, 12, 17|||||||||
353|Amberoona Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Shale, green, finely laminated, silty, purple and grey silty shale.|
353|Amberoona Formation|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian|Shown as Marinoan age. Northern Flinders Ranges.||Umberatana Group||||
353|Amberoona Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14-15, p22|Cryogenian|Cryogenian|LA-ICP-MS detrital zircon MDA of 1110+/-71 Ma from limited available data.||Upalinna Subgroup||||
381|Amphitheatre Group|730|4|Described|p23, p24, p27, p32.|Devonian|Devonian|Cobar Sub-basin, Darling Basin. Three deep-water turbidite sequences; lower thin-bedded unit is CSA Siltstone. Middle unit is sandier and more thickly-bedded, called Biddabirra Formation. Probably faulted over Kopyje Group.||||||11-NOV-14
381|Amphitheatre Group|5252|5|Briefly described|p61; p62 Fig.2; p63; throughout article.|Early Devonian|Pridoli|Of Cobar Supergroup, Cobar Basin. Includes outcrop of thin sandstones and reddish purple siltstones. Conformable but diachronous with overlying Winduck Group.||||||
381|Amphitheatre Group|22518|4|Described|Table 1, p 4, 10||Late Silurian|Darling Basin||||||
381|Amphitheatre Group|22768|5|Briefly described|p170-71|||||||||
381|Amphitheatre Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
381|Amphitheatre Group|22857|4|Described|p170, p436 App.1, Tb.A1.6|Devonian|Devonian|Of the Cobar Supergroup. Geological Province: Cobar Basin. Equivalents mentioned on p350 Fig. 24.5.||||||
381|Amphitheatre Group|22887|5|Briefly described|Fig.5 p12|Middle Devonian||||||||
381|Amphitheatre Group|22893|6|Mentioned|p90 fig4|||Name given to Cobar Supergroup rocks when describing Dolmoreve No.1 drill hole.||||||
381|Amphitheatre Group|22935|5|Briefly described|p253||Early Devonian|||||||
381|Amphitheatre Group|23054|6|Mentioned|p24|||||||||
381|Amphitheatre Group|23095|5|Briefly described|p610 (table 1)|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23096|6|Mentioned|p602|||Cobar Supergroup||||||
381|Amphitheatre Group|23098|5|Briefly described|p587|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23101|5|Briefly described|p567 (Fig 1)|||||||||
381|Amphitheatre Group|23171|5|Briefly described|p15,22,40|||||||||
381|Amphitheatre Group|23173|4|Described|Map Legend|Lochkovian||||||||
381|Amphitheatre Group|23522|5|Briefly described|p249 Fig 5|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23734|5|Briefly described|p12 Fig. 1|||Includes upper and lower mudstones and sandstones, the Biddabirra Formation, Shume Formation and the CSA Siltstone.||||||
381|Amphitheatre Group|24241|5|Briefly described|p15 Fig.2|Devonian|Silurian|Geological Province: Darling Basin.||||||17-MAR-05
381|Amphitheatre Group|29680|6|Mentioned|Fig.1|||||||||
381|Amphitheatre Group|29947|4|Described|p685|||||||||
381|Amphitheatre Group|29948|6|Mentioned|Fig.12|||||||||
381|Amphitheatre Group|29984|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|29987|6|Mentioned|p25|||||||||
381|Amphitheatre Group|30075|6|Mentioned|Fig.2|||||||||
381|Amphitheatre Group|32087|6|Mentioned|p17|||||||||
381|Amphitheatre Group|32619|6|Mentioned|p459|||Fauna||||||
381|Amphitheatre Group|32853|6|Mentioned|p58|||||||||
381|Amphitheatre Group|32865|6|Mentioned|p485|||||||||
381|Amphitheatre Group|32918|6|Mentioned|p12|||Refers Rade (1963 unpubl.)||||||
381|Amphitheatre Group|33004|6|Mentioned|p190|||||||||
381|Amphitheatre Group|33732|4|Described|p100|||||||||
381|Amphitheatre Group|34035|6|Mentioned|p544|||||||||
381|Amphitheatre Group|34057|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
381|Amphitheatre Group|34109|6|Mentioned|p165|||||||||
381|Amphitheatre Group|34400|5|Briefly described|p8|||Lower Devonian. See also P11.||||||
381|Amphitheatre Group|34403|4|Described|p148|||||||||
381|Amphitheatre Group|34404|6|Mentioned|Fig.3.8|||Lower - ?Middle Devonian||||||
381|Amphitheatre Group|34405|6|Mentioned|Fig.3.9|||Correlation Chart||||||
381|Amphitheatre Group|34406|6|Mentioned|p223|||||||||
381|Amphitheatre Group|34449|4|Described|p21|||L.- M.Devonian||||||
381|Amphitheatre Group|35232|6|Mentioned|p10|||||||||
381|Amphitheatre Group|35287|6|Mentioned|Table 1|||||||||
381|Amphitheatre Group|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area.||||||08-APR-09
381|Amphitheatre Group|35925|4|Described|p1|||||||||
381|Amphitheatre Group|36214|6|Mentioned|p57|||||||||
381|Amphitheatre Group|37798|6|Mentioned|p128|||||||||
381|Amphitheatre Group|38064|6|Mentioned|p39|||||||||
381|Amphitheatre Group|38292|3|Fully described|p3|||||||||
381|Amphitheatre Group|38593|6|Mentioned|p90|||||||||
381|Amphitheatre Group|39083|6|Mentioned|p30|||||||||
381|Amphitheatre Group|39618|6|Mentioned|Table 1|||||||||
381|Amphitheatre Group|40130|6|Mentioned|p205|||||||||
381|Amphitheatre Group|40595|6|Mentioned|Fig.7|||||||||
381|Amphitheatre Group|40676|6|Mentioned|p28|||||||||
381|Amphitheatre Group|41085|6|Mentioned|p88|||||||||
381|Amphitheatre Group|41090|6|Mentioned|Fig.1|||||||||
381|Amphitheatre Group|41126|6|Mentioned|p107|||||||||
381|Amphitheatre Group|41138|6|Mentioned|Map legend|Pragian|Lochkovian|Pragian-Lochkovian||||||
381|Amphitheatre Group|41276|6|Mentioned|p62|||||||||
381|Amphitheatre Group|41394|2|Defined|p59|middle Pragian|late Lochkovian|||||||
381|Amphitheatre Group|41395|6|Mentioned|Map legend|Pragian|Lochkovian|||||||
381|Amphitheatre Group|41410|5|Briefly described|p295|||||||||18-JAN-10
381|Amphitheatre Group|41528|2|Defined|p75|Early Devonian||||||||
381|Amphitheatre Group|41529|6|Mentioned|Map legend|Early Devonian||||||||
381|Amphitheatre Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
381|Amphitheatre Group|41821|4|Described|p32|||||||||
381|Amphitheatre Group|41872|6|Mentioned|p8|||||||||
381|Amphitheatre Group|42033|6|Mentioned|p652|||||||||
381|Amphitheatre Group|42144|5|Briefly described|p603|||||||||
381|Amphitheatre Group|42208|6|Mentioned|Fig.1 P305|||||||||
381|Amphitheatre Group|42521|5|Briefly described|p15, Figs|||||||||
381|Amphitheatre Group|42566|5|Briefly described|Fig.5 P11|||||||||
381|Amphitheatre Group|42907|6|Mentioned|Fig.8, P8|||||||||
381|Amphitheatre Group|42966|5|Briefly described|Fig. 25 p47|||||||||
381|Amphitheatre Group|42983|6|Mentioned|p343|||||||||
381|Amphitheatre Group|43032|3|Fully described|p64|||Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43090|5|Briefly described|Map legend|Pragian|Lochkovian|Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
381|Amphitheatre Group|43202|6|Mentioned|p17|||||||||
381|Amphitheatre Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
381|Amphitheatre Group|43369|14|Not recorded|Map Legend|||||||||
381|Amphitheatre Group|43379|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43380|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43381|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
381|Amphitheatre Group|43388|14|Not recorded|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43389|14|Not recorded|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43398|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Siluro-Dev.- L.Dev)||||||
381|Amphitheatre Group|43461|14|Not recorded|p619, table p621|Siegenian|Gedinnian|||||||
381|Amphitheatre Group|43479|14|Not recorded|p123,151|Middle Devonian|Early Devonian|||||||
381|Amphitheatre Group|43491|14|Not recorded|pV/14||Middle Devonian|||||||
381|Amphitheatre Group|43510|14|Not recorded|p46|||See also Lexicon||||||
381|Amphitheatre Group|43684|5|Briefly described|p253||Early Devonian|||||||
381|Amphitheatre Group|43757|5|Briefly described|p510|||||||||
381|Amphitheatre Group|43774|1|Redefined|p44-47||Devonian|||||||
381|Amphitheatre Group|43859|5|Briefly described|15|||Conformable under Winduck Group.||||||08-APR-09
381|Amphitheatre Group|44133|6|Mentioned|p45|Devonian|Devonian|||||||
381|Amphitheatre Group|46032|14|Not recorded|p.413|Middle Devonian|Early Devonian|= Amphitheatre Beds. (H55-14/Cobar).||||||
381|Amphitheatre Group|46973|6|Mentioned|p51|||||||||
381|Amphitheatre Group|47050|6|Mentioned|p244|||||||||
381|Amphitheatre Group|49038|6|Mentioned|p22|||||||||
381|Amphitheatre Group|49040|6|Mentioned|p6|||||||||
381|Amphitheatre Group|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Cobar Supergroup.  Informally divided into upper anf lower units. Geological Province: Cobar Basin.||||||
381|Amphitheatre Group|61213|5|Briefly described|p317 Fig. 2|Early Devonian|Early Devonian|Possibly interfingers with Winduck Group. Geological Province: Darling Basin.||||||
381|Amphitheatre Group|61311|5|Briefly described|p43 Table D1|Early Devonian|Late Silurian|Turbitdite sequence of rocks. Geological Province: Darling Basin.||||||
381|Amphitheatre Group|61314|5|Briefly described|p120|Early Devonian|Early Devonian|Of the Cobar Supergroup. Geological Province: Murray Basin.||||||
381|Amphitheatre Group|61817|5|Briefly described|p80|Early Devonian|Early Devonian|Deep-water turbidites.  Geological Province: Cobar Basin.||||||
381|Amphitheatre Group|61905|5|Briefly described|p136|||||||||
381|Amphitheatre Group|61964|6|Mentioned|p67|||Of the Cobar Supergroup. On THE MEADOWS map sheet area.||||||
381|Amphitheatre Group|63632|5|Briefly described|649|||Marine deposits comprising deep shelf and basin facies, westwards.||||||
381|Amphitheatre Group|64962|5|Briefly described|p202||Early Devonian|Geological province: Cobar Basin. Upper section comprises deep-water turbidites; lower section consists of turbidites, very minor volcanic rocks and minor limestone. Low-grade metasedimentary rocks host the McKinnon s mine.||||||
381|Amphitheatre Group|64967|5|Briefly described|p112 Fig. 1, p113, p114 Fig. 2|Emsian|Late Silurian|Geol.province: Darling Basin/Blantyre Sub-basin. Deeper marine deposits.Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113).||||||08-APR-09
381|Amphitheatre Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cobar. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
381|Amphitheatre Group|65469|5|Briefly described|p14-p17, p43|Early Devonian|Late Silurian|Lachlan Orogen. Informally sub-divided into an upper and lower component on p43, p55 and p62. See also p52, p55 fig 3-19, p62, p67, p81, p131, p341.|||Includes the CSA Siltstone, Shume Formation and the Biddabirra Formation.|||
381|Amphitheatre Group|67870|5|Briefly described|p58, p62|Early Devonian|Early Devonian|Western Darling Basin. Marine shelf and basin deposits.||||Is overlain unconformably by Mulga Downs Group.||
381|Amphitheatre Group|68823|6|Mentioned|p376 Fig.3, p377, p378 Fig.4, p404|Early Devonian|Late Silurian|Makes up most of the Cobar Basin. Lachlan and western Thomson Orogens. Sediments sourced mostly from the west; locally from Thule Granite to the south.|||Includes the Alley Sandstone Member.||Siliciclastic turbidites.|
381|Amphitheatre Group|69002|5|Briefly described|p11, p14, p15, Map 1b, Legend|Early Devonian|Early Devonian||||Includes the Biddabirra Formation.||Comprises siliclastic sedimentary rocks.|
381|Amphitheatre Group|69042|5|Briefly described|map legends|Early Devonian|Early Devonian|Dcs. Cobar Basin, Lachlan Orogen. Includes non-magnetic metasediments.||||||
381|Amphitheatre Group|69043|6|Mentioned|p11|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|69511|5|Briefly described|p1-2, p6, p14, p22|||Contains Lochkovian trilobites and brachiopods. Hosts an unnamed granite dated at c.423 Ma.||||Interfingers with Mount Halfway Volcanics. Is intruded by the 422.5 Ma Gilgunnia Granite. Is faulted against the Thule Granite.||
381|Amphitheatre Group|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
381|Amphitheatre Group|70037|5|Briefly described|p309 Fig.2, p310-311, p327|Early Devonian|Late Silurian|Rayner (1962). Previously the Amphitheatre Stage of Andrews (1913). Darling Basin. Marine deposits.||||Is overlain by or interfingers with Winduck Group.|Thin- to medium-bedded sandstone and thinly laminated siltstone, thin limestone beds and minor felsic volcanics; overlain by thin- to medium-bedded sandstone and siltstone overlain by coarse-grained beds.|
381|Amphitheatre Group|70383|6|Mentioned|p51|Devonian|Devonian|Cobar area. Thought to be a source of fossiliferous (fish) sandstone boulders in the Bulldog Shale.||||||
381|Amphitheatre Group|70602|6|Mentioned|p67 Fig 3|Devonian|Devonian|||Cobar Supergroup||||
381|Amphitheatre Group|70718|5|Briefly described|p20|Early Devonian|Early Devonian|Darling Basin. A deep to shallow marine depositional environment is interpreted for this group.||Cobar Supergroup||Overlain by the Winduck Group.|Clastic sediments.|
381|Amphitheatre Group|70751|5|Briefly described|p1, p5-p6, p12-p13, p15, p25-p26, p31|Devonian|Late Silurian|Cobar Superbasin, Kopyje Shelf. Can be subdivided into the informal lower and upper parts which are seperated by the Shume Formation.||Cobar Supergroup|||Fine- to medium-grained turbidites including quartz-rich and quartz-lithic sandstones and siltstones.|
381|Amphitheatre Group|70821|5|Briefly described|p11|Early Devonian|Late Silurian|Deep-water turbidites. Typically non-magnetic.||Cobar Supergroup.||||01-DEC-16
381|Amphitheatre Group|70876|5|Briefly described|p1, p16, p20, p76|||Cobar Basin. Deposited in a deep water marine environment.||Cobar Supergroup|Includes the Shume Formation.|Nonconformably overlies the Thule Granite.|Turbidite deposits.|
381|Amphitheatre Group|70941|6|Mentioned|p78 fig 32|Early Devonian|Early Devonian|||||Overlies the Great Cobar Slate and the CSA Siltstone.||
381|Amphitheatre Group|70950|5|Briefly described|p1028-1029,1033-1034,1038-1039, 1040|Early Devonian|Silurian|Geological province: Cobar Basin, Central Lachlan Orogen. Detailed mineralisation analysis provided.|||Includes Shume Formation.||Deep water fine- to medium-grained turbidites; Greywacke, siltstone, shale, felsic volcaniclastic units|
381|Amphitheatre Group|71039|5|Briefly described|p3, p6, p14-p16, p18-p19, p28|||Referred to as the Lower Amphitheatre Group on p14. Divided into the Northwestern, Northeastern and Southern portions in this study. See also p21, p23-26.|||Includes the Biddabirra Formation and the CSA Siltstone.|Intruded by the Gilgunnia Granite and the Boolahbone Granite.||09-MAR-23
381|Amphitheatre Group|71285|5|Briefly described|p538-539, p548-p549|Early Devonian|Late Silurian|Cobar region. Part of the Cobar Basin fill.||Cobar Supergroup.|Biddabirra Formation, CSA Siltstone.|||07-DEC-18
381|Amphitheatre Group|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Cobar Supergroup.|Biddabirra Formation.|||
381|Amphitheatre Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|Two informal units (Amphitheatre Group, lower and Amphitheatre Group, upper) are also mapped, but share the same lithological description in the Legend. In the Time-Space Plot, they unfortunately appear as Lower Amphitheatre Formation and Upper Amphitheatre Formation.||Cobar Supergroup.|Shume Formation, CSA Siltstone, Biddabirra Formation.|||
381|Amphitheatre Group|71860|6|Mentioned|p6|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|72908|5|Briefly described|p3-4, p18, p21|Lochkovian|Pridoli|Cobar Basin. Early Lochkovian minimum age.|||lower Amphitheatre Group, Shume Formation, upper Amphitheatre Group||Fine- to medium-grained turbidites.|
381|Amphitheatre Group|72958|6|Mentioned|p9, p11-12, p21, p29, p37|Pragian|Pridoli|Cobar Basin. Nymagee area. Present in the deepest part of the basin. Previously (McRae, 1987, Mathieson et al., 2016), considered the Shume Formation (of this Group) to be deposited in the Lochkovian to Pragian, on the basis of correlation with Pragian conodonts in the Lerida Limestone Member (Biddabirra Formation). This minimum age interpretation appears to be supported in the final discussion p60-61, although the maximum depositional age is only constrained as Pridoli, by dating of volcanics in autochthonous blocks.|||Shume Formation, 'upper' Amphitheatre Group, 'lower' Amphitheatre Group|Overlain by Buckambool Sandstone (Winduck Group). Equivalent to Mount Hope Group, Broken Range Group and Mouramba Group.||
381|Amphitheatre Group|73019|5|Briefly described|p429|Early Devonian|Early Devonian|Cobar Basin.||||Overlies Kopyje Group.|Deep-water turbidites.|
381|Amphitheatre Group|73143|5|Briefly described|p1-3, p8|Devonian|Silurian|Lachlan Orogen. Cobar Superbasin, northern. Host to the Endeavour Zn-Pb-Ag deposit. Upper and Lower Amphitheatre Group shown on p2.|||CSA Siltstone, Biddabirra Formation, Lower Amphitheatre Group, Upper Amphitheatre Group||Includes siltstone and limestone units.|
381|Amphitheatre Group|73174|5|Briefly described|p1036-1039|Early Devonian|Early Devonian|Cobar Basin. Interfingers with the Winduck Group representing increasing water depth to the east. Contains age-diagnostic brachiopod.||Cobar Supergroup|Biddabirra Formation, Alley Sandstone Member, CSA Siltstone, Shume Formation|||
381|Amphitheatre Group|73578|6|Mentioned|p2, p4, p11, p18|||Cobar Basin. [Written as Amphitheatre Group (lower) and Amphitheatre Group (upper) on p2].||Cobar Supergroup|Shume Formation|||
416|Andamooka Limestone|22645|6|Mentioned|Fig4 P204||Cambrian|||||||
416|Andamooka Limestone|22650|6|Mentioned|p 159|Cambrian|Cambrian|Province - Adelaide Geosyncline.||||||
416|Andamooka Limestone|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 4 of Early Cambrian. Correlate of Billy Creek Limestone, Hawker Group, and Todd River Dolomite.||||||
416|Andamooka Limestone|23805|5|Briefly described|p5 Fig. 3|Cambrian|Cambrian|||||||17-MAR-08
416|Andamooka Limestone|23818|5|Briefly described|p76|Cambrian|Cambrian|Underlying unit: Yarloo Shale.||||||
416|Andamooka Limestone|23981|5|Briefly described|p18, p78|Early Cambrian|Early Cambrian|Shallow marine sediments. Geological Province: Arrowie Basin.||||||04-FEB-08
416|Andamooka Limestone|24175|6|Mentioned|p15|Cambrian|Cambrian|||||||
416|Andamooka Limestone|24261|5|Briefly described|p1047 Fig.1|Cambrian|Cambrian|||||||17-MAR-08
416|Andamooka Limestone|24321|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Parent: Hawker Group.||||||11-JAN-10
416|Andamooka Limestone|24507|6|Mentioned|p23|||See also Andamooka Limestone, upper. Mineralisation and alteration at base of unit.||||||
416|Andamooka Limestone|30051|6|Mentioned|Fig.11|||||||||
416|Andamooka Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
416|Andamooka Limestone|31539|6|Mentioned|p9|||||||||
416|Andamooka Limestone|33474|6|Mentioned|Fig.3|||||||||
416|Andamooka Limestone|33932|6|Mentioned|p14|||L.Camb. Equiv. Wilkawillina Lst.||||||
416|Andamooka Limestone|33934|6|Mentioned|p2399|||||||||
416|Andamooka Limestone|34535|6|Mentioned|p76|||Cambrian||||||
416|Andamooka Limestone|34612|6|Mentioned|p90|||Equivalent. Corelation chart. Fig.33||||||
416|Andamooka Limestone|35255|6|Mentioned|Fig.8|||||||||
416|Andamooka Limestone|35548|5|Briefly described|p17|||||||||
416|Andamooka Limestone|35549|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
416|Andamooka Limestone|35835|6|Mentioned|p209|||||||||
416|Andamooka Limestone|36214|6|Mentioned|p60|||||||||
416|Andamooka Limestone|36507|6|Mentioned|p115|||||||||
416|Andamooka Limestone|36966|6|Mentioned|Fig.1|||||||||
416|Andamooka Limestone|37461|6|Mentioned|Fig.5.13|||||||||
416|Andamooka Limestone|38022|6|Mentioned|Fig.4|||||||||
416|Andamooka Limestone|38157|6|Mentioned|Table V|||||||||
416|Andamooka Limestone|39047|6|Mentioned|Table 2|||||||||
416|Andamooka Limestone|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
416|Andamooka Limestone|39629|6|Mentioned|Fig.1|||||||||
416|Andamooka Limestone|39808|6|Mentioned|p223|||||||||
416|Andamooka Limestone|40852|6|Mentioned|p33|||See also Table 3.1 and Fig.3.7||||||
416|Andamooka Limestone|41005|6|Mentioned|p419|||||||||
416|Andamooka Limestone|41493|5|Briefly described|Table 2|||||||||
416|Andamooka Limestone|42011|6|Mentioned|Fig.14 P458|||||||||
416|Andamooka Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
416|Andamooka Limestone|42247|5|Briefly described|Fig.3 P7|||||||||
416|Andamooka Limestone|42269|6|Mentioned|Fig.1 P335|||||||||
416|Andamooka Limestone|42346|5|Briefly described|p77, Fig.2 p79|Early Cambrian||||||||
416|Andamooka Limestone|42465|5|Briefly described|Map Legend|||||||||
416|Andamooka Limestone|42469|5|Briefly described|p25|||||||||
416|Andamooka Limestone|42546|5|Briefly described|Map legend|Cambrian||||||||
416|Andamooka Limestone|42723|5|Briefly described|map legend|Cambrian||||||||
416|Andamooka Limestone|42736|5|Briefly described|map legend|Neoproterozoic||||||||
416|Andamooka Limestone|43048|4|Described|Table 2.|||||||||
416|Andamooka Limestone|43052|5|Briefly described|Fig.5.16|||||||||
416|Andamooka Limestone|43085|5|Briefly described|Fig.5|||||||||
416|Andamooka Limestone|44133|5|Briefly described|p4 Fig. 7.2, 24|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Overlies: Yarloo Shale, Tent Hill Formation.||||||
416|Andamooka Limestone|44689|14|Not recorded|map legend|||(H53-12). Cambrian (lower??).||||||
416|Andamooka Limestone|44934|5|Briefly described|Map Legend||Cambrian|||||||
416|Andamooka Limestone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
416|Andamooka Limestone|60889|5|Briefly described|p249 Fig.6, p250 Fig.7|||Shown as upper Andamooka Limestone and lower Andamooka Limestone in Fig.6.||||Overlain (?) by middle Wilkawillina Limestone.||21-SEP-17
416|Andamooka Limestone|60955|5|Briefly described|Map Legend|Cambrian|Cambrian|Cavernous, massive limestone and dolomitic shale.||||||
416|Andamooka Limestone|64559|6|Mentioned|p977 Fig. 11|Cambrian|Cambrian|||||||
416|Andamooka Limestone|64696|5|Briefly described|p133 Fig.14|Cambrian|Cambrian|||||||
416|Andamooka Limestone|65686|6|Mentioned|p413, p415 Fig 4|Cambrian|Cambrian|Arrowie Basin, Stuart Shelf.||||||07-MAY-12
416|Andamooka Limestone|67127|6|Mentioned|p104|Cambrian|Cambrian|South Australia.||||Unconformably overlies the Wilpena Group.||
416|Andamooka Limestone|67344|6|Mentioned|p264 Tb.3, p266 |Cambrian|Cambrian|Of the Arrowie Basin. Unmetamorphosed Cambrian series 2 formation. Shallow-water marine carbonate deposit. Stromatolites are common. Bulk organic carbon isotopic composition almost identical with Emu Bay Shale.||||||
416|Andamooka Limestone|67536|5|Briefly described|Map Legend|Drumian|Ediacaran||ca. 564 +/- 61 Ma - 526 +/- 4 Ma||||Marine shelf to basinal carbonate, minor basal sandstone and tuff.|
416|Andamooka Limestone|69946|6|Mentioned|p38|||||||Is overlain unconformably by Boorthanna Formation.||
416|Andamooka Limestone|71102|5|Briefly described|p242,249,254,256,258,269|||Of Arrowie Basin. Intersected section: SCYW-791A (drill core, Stuart Shelf), |||||Limestone, often recrystallised/dolomitised. Locally sandy/pyritic. Massive to bedded and flaggy. Occasional vughs.|
416|Andamooka Limestone|71129|6|Mentioned|p134|||Adelaide Geosyncline.||||Overlies the Tent Hill Formation.||
416|Andamooka Limestone|71342|6|Mentioned|Ch5 p38|Cambrian|Cambrian|Arckaringa Basin.||||||
501|Appila Tillite|22510|5|Briefly described|table 1, p36,38|||Of the Yudnamutana Subgroup.  Mid-north and Southern Flinders Ranges. Age: Sturtian||||||13-OCT-04
501|Appila Tillite|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
501|Appila Tillite|22830|6|Mentioned|P27||Adelaidean|||||||
501|Appila Tillite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group).||||||
501|Appila Tillite|22889|6|Mentioned|p34 & p35|||||||||
501|Appila Tillite|22926|6|Mentioned|39 fig 2|Neoproterozoic|Neoproterozoic|||||||
501|Appila Tillite|23818|5|Briefly described|p34 Fig.8, p64 Fig.22|||Geological Province: Willyama Block. Of the Umberatana Group.||||||
501|Appila Tillite|24400|5|Briefly described|p155 Tb.2|Adelaidean|Adelaidean|||||||03-MAR-05
501|Appila Tillite|24507|6|Mentioned|p23|||In contact with Tindelpina Shale. In the Oodla Wirra area.||||||
501|Appila Tillite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||07-JAN-10
501|Appila Tillite|24584|5|Briefly described|p14 Fig. 2|Neoproterozoic|Neoproterozoic|||||||
501|Appila Tillite|29778|6|Mentioned|p167|||||||||
501|Appila Tillite|29780|4|Described|p31|||||||||
501|Appila Tillite|29837|4|Described|p76|||||||||
501|Appila Tillite|30052|6|Mentioned|Fig.5|||See also Fig.6 Proterozoic age.||||||
501|Appila Tillite|30261|6|Mentioned|Table 1|||Sturtian age||||||
501|Appila Tillite|30798|5|Briefly described|p114|||||||||
501|Appila Tillite|30799|6|Mentioned|p1|||Stratigraphic relations with Benda Siltstone.||||||
501|Appila Tillite|30801|6|Mentioned|p5|||Sturtian. See also P6. Table.||||||
501|Appila Tillite|30802|6|Mentioned|p12|||||||||
501|Appila Tillite|30807|6|Mentioned|p103|||Suggested map symbol||||||
501|Appila Tillite|30810|6|Mentioned|p2|||||||||
501|Appila Tillite|32146|6|Mentioned|Fig.3|||||||||
501|Appila Tillite|32506|6|Mentioned|Fig.1|||||||||
501|Appila Tillite|32510|6|Mentioned|Table 1|||||||||
501|Appila Tillite|32547|6|Mentioned|Fig.2|||Sturtian. Umberatana Gp.||||||
501|Appila Tillite|32635|5|Briefly described|p3|||Sturtian||||||
501|Appila Tillite|32724|6|Mentioned|Fig.1|||Correlation. Sturtian||||||
501|Appila Tillite|32777|6|Mentioned|p5|||||||||
501|Appila Tillite|33474|6|Mentioned|Fig.2|||||||||
501|Appila Tillite|34535|6|Mentioned|Fig.22|||Sturtian||||||
501|Appila Tillite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
501|Appila Tillite|34537|6|Mentioned|Fig.8|||Sturtian||||||
501|Appila Tillite|34587|6|Mentioned|p36|||||||||
501|Appila Tillite|34812|6|Mentioned|Table 8|||||||||
501|Appila Tillite|35255|6|Mentioned|p13|||||||||
501|Appila Tillite|35628|6|Mentioned|Table 2|||||||||
501|Appila Tillite|36048|6|Mentioned|p379|||||||||
501|Appila Tillite|36126|6|Mentioned|Fig.1|||||||||
501|Appila Tillite|36253|6|Mentioned|Fig.3-2|||||||||
501|Appila Tillite|36625|6|Mentioned|Fig.1|||||||||
501|Appila Tillite|36733|6|Mentioned|Table 5|||||||||
501|Appila Tillite|36833|6|Mentioned|Fig.1|||||||||
501|Appila Tillite|37461|4|Described|p339|||See also Table 5.I||||||
501|Appila Tillite|37932|3|Fully described|p541|||||||||
501|Appila Tillite|38157|6|Mentioned|Table IV|||||||||
501|Appila Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
501|Appila Tillite|40294|6|Mentioned|p43|||||||||
501|Appila Tillite|41404|6|Mentioned|Fig.24|||||||||
501|Appila Tillite|41405|3|Fully described|p146|||Mention p204.||||||14-MAY-07
501|Appila Tillite|41500|6|Mentioned|Fig.1|||||||||
501|Appila Tillite|41526|6|Mentioned|p8|||||||||
501|Appila Tillite|42098|5|Briefly described|p53|||||||||
501|Appila Tillite|42109|6|Mentioned|Fig.1 P19|||||||||
501|Appila Tillite|42222|5|Briefly described|p16|||||||||
501|Appila Tillite|42469|6|Mentioned|p22|||Sturtion (Adelaidian) of Umberatana Group||||||
501|Appila Tillite|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
501|Appila Tillite|42720|6|Mentioned|map legend|Sturtian||||||||
501|Appila Tillite|42736|5|Briefly described|map legend|Neoproterozoic||||||||
501|Appila Tillite|42813|5|Briefly described|p18|||||||||
501|Appila Tillite|43052|5|Briefly described|p183,Table 6.1|||||||||
501|Appila Tillite|43560|6|Mentioned|p233|||||||||
501|Appila Tillite|43742|6|Mentioned|Fig.2,p39||Neoproterozoic|||||||
501|Appila Tillite|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||06-DEC-04
501|Appila Tillite|44660|14|Not recorded|map legend|||Sturtian, lithology.||||||
501|Appila Tillite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Sturtian.||||||
501|Appila Tillite|44934|6|Mentioned|Map Legend||Adelaidean|||||||
501|Appila Tillite|46865|6|Mentioned|p50|||||||||
501|Appila Tillite|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Tillite; quartzite; siltstone.||||||
501|Appila Tillite|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
501|Appila Tillite|62096|5|Briefly described|p289, p290 Fig. 3g|Neoproterozoic|Neoproterozoic|Deeply weathered siltstones and tillites.||||||
501|Appila Tillite|62903|6|Mentioned|p729, p730 Fig.1|Sturtian|Sturtian|Adelaide Rift Complex. Sturtian glaciation (Preiss et al. 1998) correlates with Areyonga Formation. Presented in text as Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites. Presented in figure as Sturt/Applia.||Yudnamutana Subgroup||Sturtian glacial units overlain by Tapley Hill Formation||
501|Appila Tillite|64797|5|Briefly described|p153 Fig.2, p158, p162 Fig.9, p163 Tb.5 |||See also p164 Fig.11, p168 Tb.11, p169 Fig.12. S-isotope data. International correlations.||||||
501|Appila Tillite|65925|5|Briefly described|Appendix 2.||||||||Tillite; quartzite; siltstone. Massive, grey.|
501|Appila Tillite|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||||Underlies the Tapley Hill Formation; equivalent to the Wilyerpa Formation.||26-APR-12
501|Appila Tillite|70334|6|Mentioned|p90|||Includes vein-hosted gold mineralisation. See also Apilla Tillite p20, p47.||Of Umberatana Group.||||
501|Appila Tillite|70819|5|Briefly described|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley. Deposited during the Sturtian Glaciation.||Yudnamutana Subgroup.||Disconformably overlies Kadlunga Slate. Is overlain by Wilyerpa Formation.|Glaciomarine deposits: massive rock containing isolated clasts (dropstones) of variable sizes, shapes and lithologies, set in a poorly-sorted, fine-grained, silty-sandy matrix.|
501|Appila Tillite|71237|14|Not recorded|p7, 8, 9, 17|||||||||
501|Appila Tillite|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
501|Appila Tillite|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Tillite; quartzite; siltstone.|09-DEC-21
501|Appila Tillite|73103|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Tillite; quartzite; siltstone. Massive, grey.|
501|Appila Tillite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Tillite; quartzite; siltstone. Massive, grey.|
501|Appila Tillite|74367|5|Briefly described|p6, p7 Fig.6, p9, p11, p14-16, p20-21||Cryogenian||667+/-6 Ma LA-ICP-MS detrital zircon MDA|Yudnamurtana Subgroup||||
540|Arburee Rhyolite|22629|6|Mentioned|p158|Calymmian|Calymmian|||||||
540|Arburee Rhyolite|24474|3|Fully described|p38|||Of the Glyde Hill Volcanic Complex.  Formerly included in Wheepool Rhyolite (Blissett, 1975, 1977, 1980, 1985); later demonstrated by Giles (1977, 1980) as unrelated.  Conformably overlies/intrudes Mangaroongah Dacite.  Geol. Province: Gawler Craton.||||||
540|Arburee Rhyolite|30984|2|Defined|p14|Proterozoic|Proterozoic|||||||
540|Arburee Rhyolite|41974|6|Mentioned|p411|||||||||
540|Arburee Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
540|Arburee Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
540|Arburee Rhyolite|43052|5|Briefly described|p111|||of Glyde Hill Volcanics Complex||||||
540|Arburee Rhyolite|43071|6|Mentioned|p14|||||||||
540|Arburee Rhyolite|43094|5|Briefly described|p23|||of Glyde Hill Volcanic Complex||||||
540|Arburee Rhyolite|69649|5|Briefly described|p20|Mesoproterozoic|Mesoproterozoic|Blissett included this unit within the Wheepool Rhyolite, but Giles demonstrated it is a localised, unrelated lava.||Unit in Glyde Hill Volcanic Complex.||Conformably overlies and intrudes Mangarooongah Dacite.|Purple-grey weathering to a characteristic orange, porphyritic rhyolite with coarse K-feldspar and medium-grained quartz phenocrysts.|24-FEB-15
540|Arburee Rhyolite|70659|6|Mentioned|p7, p8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.|||Localised felsic lava flow with coherent core and autobrecciated margins; close to source vent.|
540|Arburee Rhyolite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Wheepool Rhyolite. Underlain by, and laterally equivalent to Karkulta Rhyolite.||
540|Arburee Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
600|Arkaroola Subgroup|22553|6|Mentioned|p77|||Part of the Adelaidean sequence.||||||11-SEP-07
600|Arkaroola Subgroup|22589|6|Mentioned|p129||Cryogenian|||||||
600|Arkaroola Subgroup|22725|6|Mentioned|p241|Cambrian|Neoproterozoic|Part of the Callana Group.||||||11-SEP-07
600|Arkaroola Subgroup|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
600|Arkaroola Subgroup|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Callanna Group. Name and spelling not to be confused with Arkarula Formation.||||||
600|Arkaroola Subgroup|22926|6|Mentioned|42|||||||||
600|Arkaroola Subgroup|23054|6|Mentioned|p10,33|||||||||
600|Arkaroola Subgroup|23282|6|Mentioned|p51|||May be equivalent to Younghusband Conglomerate.||||||
600|Arkaroola Subgroup|24175|3|Fully described|p8|Neoproterozoic|Neoproterozoic|Of Callanna Group.||||||18-APR-13
600|Arkaroola Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Callanna Group.||||||11-JAN-10
600|Arkaroola Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~840-830 Ma. Of Callana Group. Geological Province: Adelaide Fold Belt.||||||07-JAN-10
600|Arkaroola Subgroup|24586|5|Briefly described|p51 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaidean Geosyncline.||||||
600|Arkaroola Subgroup|37854|6|Mentioned|p8|||||||||
600|Arkaroola Subgroup|38004|6|Mentioned|p82|||||||||
600|Arkaroola Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
600|Arkaroola Subgroup|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
600|Arkaroola Subgroup|39490|6|Mentioned|p10|||||||||
600|Arkaroola Subgroup|40294|3|Fully described|p32|||See also p9.||||||11-SEP-07
600|Arkaroola Subgroup|41401|6|Mentioned|Table 4|||||||||
600|Arkaroola Subgroup|41402|6|Mentioned|p39|||||||||
600|Arkaroola Subgroup|41403|6|Mentioned|p43|||See also Table 5.||||||11-SEP-07
600|Arkaroola Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
600|Arkaroola Subgroup|42223|5|Briefly described|p37|||||||||
600|Arkaroola Subgroup|42238|5|Briefly described|p71|||||||||
600|Arkaroola Subgroup|42720|5|Briefly described|map legend|Willouran||||||||
600|Arkaroola Subgroup|42813|4|Described|p14|||Of Callanna Group.||||||11-SEP-07
600|Arkaroola Subgroup|43052|4|Described|p172|||Of Callanna Group.||||||11-SEP-07
600|Arkaroola Subgroup|43742|6|Mentioned|p42|||||||||
600|Arkaroola Subgroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|Of the Callanna Group.||||||12-JUL-16
600|Arkaroola Subgroup|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
600|Arkaroola Subgroup|60718|5|Briefly described|p53 Fig. 4,|||||Of Callanna Group.|Includes Wywyana Formation, Paralana Quartzite, Wootana Volcanics, Noranda Volcanics, Black Knob Marble, and a diapiric breccia.|||15-APR-11
600|Arkaroola Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Unnamed volcanics. Possibly equivalent to Wooltana Volcanics.||||||23-DEC-09
600|Arkaroola Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Callanna Group.||||||11-SEP-07
600|Arkaroola Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, p57.|Willouran|Willouran|Confined to a graben structure, possibly formed during the extensional event represented by Wooltana Volcanics. Colour scheme shown for interpretation of Curnamona seismic sections. Written as SubGroup.||Unit in Callanna Group.|Includes Paralana Quartzite, Wywyana Formation and Wooltana Volcanics.|Is overlain by Curdimurka Subgroup.||
600|Arkaroola Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in lower Callanna Group.|Includes Wooltana Volcanics.|Unconformably overlies Pandurra Formation. Is unconformably overlain by Curdimurka Subgroup. Is intruded by Gairdner Dyke Swarm.|Sandstone, conglomerate, carbonates, basalt.|
600|Arkaroola Subgroup|62724|5|Briefly described|p17 Fig. 4, p21|Willouran|Willouran|Includes Cutana beds. Geological Province: Broken Hill Domain.||||||07-FEB-11
600|Arkaroola Subgroup|62993|5|Briefly described|p30|Neoproterozoic|Neoproterozoic||||Includes Paralana Quartzite, Wywyana Formation, Wooltana Volcanics|Correlated with Cutana Beds/beds in part.|Clean quartzites, mafic igneous rocks and calc-silicates.|19-DEC-21
600|Arkaroola Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes Cutana beds. South Australian equivalent of Poolamacca Group of NSW. Basal quartzite and conglomerate, carbonate and basalt.||||||10-SEP-07
600|Arkaroola Subgroup|64793|6|Mentioned|p284 Fig.3|||Adelaide Rift Complex||Unit in Callanna Group.|Includes Coominaree Dolomite, Wooltana Volcanics and Beda Volcanics.|||
600|Arkaroola Subgroup|64796|5|Briefly described|p183 fig 2, p187, p190 Fig.8|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex||Unit in Callanna Group.|Includes Younghusband Conglomerate, Coominaree Dolomite, Wooltana Volcanics, Black Knob Marble.||Large blocks of calcitic marble.|
600|Arkaroola Subgroup|64797|6|Mentioned|p153 Fig.2,p163,p164 Fig.11,p169 Fig.12|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
600|Arkaroola Subgroup|65338|6|Mentioned|p59.|||Adelaide Fold Belt.|||Includes Paralana Quartzite.|||
600|Arkaroola Subgroup|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf||||||
600|Arkaroola Subgroup|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Of Callanna Group. Includes Coominaree Dolomite. ||||||
600|Arkaroola Subgroup|65925|5|Briefly described|p124 Fig.3.|||||Unit in Callanna Group.|Includes Wywyana Formation and Wooltana Volcanics.|||
600|Arkaroola Subgroup|66884|6|Mentioned|p36, p41 Fig.3|||Age: Willouran. Represents lowermost strata of Adelaide fold belt sedimentary sequence. Diapiric breccia (clasts cm to hundreds of m) are crosscut and intercalated by post-Callanna stratigraphy throughout Willouran and Flinders Ranges.||Callanna Group|||Megabreccia.|14-DEC-16
600|Arkaroola Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Callanna Group.|Paralana, Wywyana, Wooltana Formations.|||
600|Arkaroola Subgroup|68068|5|Briefly described|Map legend|Willouran|Willouran|Adelaide Geosyncline.||Unit in Callanna Group.|Includes Paralana Quartzite.|||
600|Arkaroola Subgroup|69019|5|Briefly described|p36.|Neoproterozoic|Neoproterozoic|Has 5 recognised Formations, only one of which is named here.||Unit in Callanna Group.|Includes Black Knob Marble.|||
600|Arkaroola Subgroup|69023|5|Briefly described|p63|Neoproterozoic|Neoproterozoic|Forbes et al. (1981); included the three lowermost Formations of Callanna Group. Only the lowest occurs in this map area.||Unit in Callanna Group.|Includes Paralana Quartzite.|||
600|Arkaroola Subgroup|69666|6|Mentioned|p33||||||Wooltana Volcanics.|||
600|Arkaroola Subgroup|69873|5|Briefly described|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||Is intruded by Gairdner Dyke Swarm.||
600|Arkaroola Subgroup|70334|5|Briefly described|p39|||Geological province: Gawler Craton. Of Adelaide Geosyncline.||Unit of Callana Group.|Incldues Beda Basalt and Backy Point Formation.|||
600|Arkaroola Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Willouran [basal Cryogenian].||Callanna Group.|Includes Paralana Quartzite, Wywyana Formation, Wooltana Volcanics.|||18-JAN-19
600|Arkaroola Subgroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Willouran||Of Callanna Group.||||
600|Arkaroola Subgroup|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.||Callanna Group.||||
600|Arkaroola Subgroup|71236|6|Mentioned|p28|||||||Equivalent to the Beda Volcanics.||
600|Arkaroola Subgroup|72492|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Described as croping out primarily in the Peak and Denison Ranges and in the Mt. Painter region of the northeastern FlindersRanges.",,,|c. 830 Ma based on U-Pb and Sm-Nd dating|Callanna Group||Underlies Curdimurka Subgroup.|Includes siliciclastic sediments, carbonates, evaporites and minor volcanic flows.|16-SEP-20
600|Arkaroola Subgroup|73086|6|Mentioned|p18, p30|||||||Potentially correlates to Gillen Formation (Bitter Springs Group).||
600|Arkaroola Subgroup|73222|6|Mentioned|p6-7|Tonian|Tonian|Adelaide Rift Complex. Lower part of the Callanna Group. Outcrops primarily in the Gammon Ranges near Mount Painter and Arkaroola.||Callanna Group, Warrina Supergroup|Wooltana Volcanics, Noranda Volcanics, Wywyana Formation, Black Knob Marble, Paralana Quartzite, Shanahan Conglomerate Member|Overlain by Curdimurka Subgroup.||
600|Arkaroola Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p20|Tonian|Tonian|Minimum age of deposition constrained by the Wooltana Volcanics (830+/-5 Ma; Preiss, 2000).||Callanna Group|Paralana Quartzite, Wywyana Formation, Wooltana Volcanics|||
637|Arrowie Formation|24176|4|Described|p21, p22 Tb. 1|Late Pleistocene|Pleistocene|See also p38, Appendix.  Lime-coated gravels in red-brown clay.  Possibly equivalent to Callabonna Clay.  Geological Province: Mount Painter Province.||||||
637|Arrowie Formation|30056|6|Mentioned|p148|||||||||
637|Arrowie Formation|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
637|Arrowie Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
637|Arrowie Formation|30920|6|Mentioned|Map legend|Pleistocene|Pleistocene|Equivalent ? Coonarbine Formation||||||
637|Arrowie Formation|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Sub-angular, lime-coated gravel in red-brown clay (possibly includes gravels of other ages).|
668|Arumbera Sandstone|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red-brown sandstone, siltstone, conglomerate sandstone; fossiliferous. Geological Province: Amadeus Basin.||||||16-JUN-09
668|Arumbera Sandstone|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Silty sandstone, siltstone.||||||
668|Arumbera Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|12951|6|Mentioned|p143|||Amadeus Basin.||||Lower part correlated with Elkera Formation, Georgina Basin.||
668|Arumbera Sandstone|22561|4|Described|p18|Neoproterozoic|Neoproterozoic|Age: 570-580 Ma (estimated base age p18).||||||18-JUL-06
668|Arumbera Sandstone|22563|6|Mentioned|p55|||||||||
668|Arumbera Sandstone|22564|5|Briefly described|p59|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22565|4|Described|p71 & Table 1|||Approx. thickness measured from seismic data - 740 m thick||||||
668|Arumbera Sandstone|22566|4|Described|p82 &p74|Early Cambrian|Neoproterozoic|Stratigraphic relationships described p82.  Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22567|6|Mentioned|p91|||||||||
668|Arumbera Sandstone|22646|4|Described|p 100|Cambrian|Neoproterozoic|informal name - lower Arumbera Sandstone is mentioned (p 101).||||||18-JUL-06
668|Arumbera Sandstone|22649|6|Mentioned|Fig 1 on p 138|Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22650|6|Mentioned|p 159|Cambrian||Parent - Pertaoorrta Group.||||||
668|Arumbera Sandstone|22651|4|Described|p 176|Neoproterozoic|Neoproterozoic|Informally divided into upper and lower Arumbera Sandstone. Forms the base of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22652|5|Briefly described|p 195|||||||||
668|Arumbera Sandstone|22653|6|Mentioned|p 228||Cambrian|||||||
668|Arumbera Sandstone|22654|6|Mentioned|p 245|||||||||
668|Arumbera Sandstone|22746|5|Briefly described|p519, p529|Neoproterozoic III|Neoproterozoic III|||||||
668|Arumbera Sandstone|22762|5|Briefly described|p369|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22763|5|Briefly described|p398|Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22804|4|Described|p441-451|Cambrian|Neoproterozoic|Of Pertaoorrta Group.  Informally divided into upper and lower Arumbera Sandstone.||||||18-JUL-06
668|Arumbera Sandstone|22805|4|Described|p471-472|Neoproterozoic|Neoproterozoic|||||||
668|Arumbera Sandstone|22807|6|Mentioned|p500|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22816|5|Briefly described|p10 Fig. 4|Cambrian|Neoproterozoic|Amadeus Basin||||||
668|Arumbera Sandstone|22824|5|Briefly described|p533|||Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22826|4|Described|p571|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22828|6|Mentioned|p591|||||||||
668|Arumbera Sandstone|22901|6|Mentioned|76 fig 2|||Geol province Amadeus Basin||||||
668|Arumbera Sandstone|22907|6|Mentioned|42|||Geol province Amadeus Basin||||||
668|Arumbera Sandstone|23250|5|Briefly described|p1124 Fig.2|Early Cambrian|Neoproterozoic III|Subdivided informally into Unit 1,2,3 and 4. Correlate of Bonney Sandstone, Rawnsley Quartzite, Uratanna Formation and Hawker Group.||||||
668|Arumbera Sandstone|23282|6|Mentioned|p65|||Geol. Prov:  Amadeus Basin. May be equivalent to Narana Formation.||||||18-JUL-06
668|Arumbera Sandstone|23287|6|Mentioned|Fig.4|||Age: Upper Ediacaran. of Amadeus Basin.||||||07-MAY-13
668|Arumbera Sandstone|23314|5|Briefly described|333||Neoproterozoic III|||||||
668|Arumbera Sandstone|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Neoproterozoic|||||||
668|Arumbera Sandstone|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
668|Arumbera Sandstone|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Of Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|24111|5|Briefly described|p214 Fig. 9|Cambrian|Neoproterozoic|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||
668|Arumbera Sandstone|24301|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin||||||
668|Arumbera Sandstone|24334|5|Briefly described|p48 Tb.1|Early Cambrian|Neoproterozoic|Age: 530 - 560 Ma.||||||18-JUL-06
668|Arumbera Sandstone|24442|6|Mentioned|p38|||Geological Province: Victoria Basin.||||||
668|Arumbera Sandstone|29721|6|Mentioned|Table 44|||||||||
668|Arumbera Sandstone|29972|6|Mentioned|Table 1|||Lower Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|30220|6|Mentioned|Fig.13|||||||||
668|Arumbera Sandstone|30258|6|Mentioned|Fig.2|||Cambrian age. Part of Pertaoorrta Group.||||||05-SEP-18
668|Arumbera Sandstone|30313|6|Mentioned|p56|||||||||
668|Arumbera Sandstone|30374|6|Mentioned|Fig.5|||Correlation.||||||05-SEP-18
668|Arumbera Sandstone|30544|6|Mentioned|p48|||On map legend.||||||05-SEP-18
668|Arumbera Sandstone|30659|6|Mentioned|p87|||Proterozoic-Cambrian age||||||
668|Arumbera Sandstone|30660|6|Mentioned|Table 1|||Lower Cambrian age||||||
668|Arumbera Sandstone|30661|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
668|Arumbera Sandstone|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
668|Arumbera Sandstone|31026|5|Briefly described|p61|||||||||
668|Arumbera Sandstone|31973|6|Mentioned|p3|||Correlation||||||
668|Arumbera Sandstone|32720|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean.||||||05-SEP-18
668|Arumbera Sandstone|33025|6|Mentioned|p928|||Precamb.-Camb.||||||
668|Arumbera Sandstone|33307|6|Mentioned|Fig.6|||||||||
668|Arumbera Sandstone|33625|6|Mentioned|p187|||||||||
668|Arumbera Sandstone|33655|5|Briefly described|p101|||L.Camb.||||||
668|Arumbera Sandstone|33734|5|Briefly described|p495|||Refers Daily (1972). Trace fossils.||||||
668|Arumbera Sandstone|33761|6|Mentioned|p146|||Adelaidean - Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|34111|4|Described|Table 2|||See also Table 4. Cambrian||||||
668|Arumbera Sandstone|34287|6|Mentioned|p42|||||||||
668|Arumbera Sandstone|34433|6|Mentioned|p17|||||||||
668|Arumbera Sandstone|34442|5|Briefly described|Table 1|||Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|34488|4|Described|Table 1|||See also pp10,16. Cambrian||||||18-JUL-06
668|Arumbera Sandstone|34557|6|Mentioned|p357|||||||||
668|Arumbera Sandstone|34579|6|Mentioned|p15|||Cambrian. See also pp16,17.||||||05-SEP-18
668|Arumbera Sandstone|35088|6|Mentioned|p91|||Also Fig.2.||||||
668|Arumbera Sandstone|35102|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|35136|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|35221|6|Mentioned|p14|||||||||
668|Arumbera Sandstone|35222|6|Mentioned|p10|||||||||
668|Arumbera Sandstone|35798|6|Mentioned|p310|||||||||
668|Arumbera Sandstone|35805|6|Mentioned|Fig.3|||||||||
668|Arumbera Sandstone|35863|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|36014|6|Mentioned|p151|||||||||
668|Arumbera Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
668|Arumbera Sandstone|36898|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|37015|6|Mentioned|p75|||||||||
668|Arumbera Sandstone|37371|6|Mentioned|p387|||||||||
668|Arumbera Sandstone|37462|4|Described|Table 4.IX|||||||||
668|Arumbera Sandstone|37627|6|Mentioned|p185|||||||||
668|Arumbera Sandstone|37818|6|Mentioned|p81|||||||||
668|Arumbera Sandstone|37928|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|37929|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|38445|6|Mentioned|p102|||||||||
668|Arumbera Sandstone|38606|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|38885|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Early Cambrian - Late Proterozoic.||||||05-SEP-18
668|Arumbera Sandstone|39210|5|Briefly described|p38|||See also p54.||||||05-SEP-18
668|Arumbera Sandstone|39583|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|39757|6|Mentioned|p1607|||||||||
668|Arumbera Sandstone|39898|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|White, grey and purple-brown sandstone at base; siltstone in middle; purple-brown to pale brown sandstone at top. Geological Province: Amadeus Basin.||||||14-FEB-06
668|Arumbera Sandstone|39931|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|40105|6|Mentioned|p311|||See also P319||||||
668|Arumbera Sandstone|40254|6|Mentioned|p284|||||||||
668|Arumbera Sandstone|40740|3|Fully described|p15|||See also P||||||
668|Arumbera Sandstone|40810|4|Described|p3|||||||||
668|Arumbera Sandstone|40852|6|Mentioned|p34|||||||||
668|Arumbera Sandstone|40906|6|Mentioned|Fig.9|||||||||
668|Arumbera Sandstone|40998|6|Mentioned|p431|||||||||
668|Arumbera Sandstone|41005|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41018|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41115|4|Described|p1388|||Formerly Eninta Formation.||||||18-JUL-06
668|Arumbera Sandstone|41190|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|41203|5|Briefly described|p25|||See also p47.||||||05-SEP-18
668|Arumbera Sandstone|41224|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41233|3|Fully described|p15|||||||||
668|Arumbera Sandstone|41270|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|41429|5|Briefly described|p246|||||||||
668|Arumbera Sandstone|41618|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41711|6|Mentioned|p262|||||||||
668|Arumbera Sandstone|41717|5|Briefly described|p355|||||||||
668|Arumbera Sandstone|41801|4|Described|p210|||||||||
668|Arumbera Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
668|Arumbera Sandstone|42059|5|Briefly described|p130|||||||||
668|Arumbera Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
668|Arumbera Sandstone|42504|5|Briefly described|p76|||||||||
668|Arumbera Sandstone|42643|6|Mentioned|p21|||Amadeus Basin||||||
668|Arumbera Sandstone|42661|6|Mentioned|p130|||||||||
668|Arumbera Sandstone|42886|4|Described|p223|||see also Fig.2 p219.||||||05-SEP-18
668|Arumbera Sandstone|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Sandstone, siltstone, shale; marine fossils.  Age: 590-500Ma. Geological province: Amadeus Basin.||||||23-JAN-08
668|Arumbera Sandstone|43011|6|Mentioned|Table 2,p12|||||||||
668|Arumbera Sandstone|43225|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Of Pertaoorrta Group.||||||22-DEC-09
668|Arumbera Sandstone|43230|6|Mentioned|p9||Cambrian|Reservoir target.||||||
668|Arumbera Sandstone|43503|6|Mentioned|11-50|Atdabanian||from Ediacaran to||||||
668|Arumbera Sandstone|43595|5|Briefly described|p548,Fig.5-33,549|Cambrian|Adelaidean|||||||
668|Arumbera Sandstone|43646|6|Mentioned|Fig.3,p554|Early Cambrian|Precambrian|||||||
668|Arumbera Sandstone|43648|6|Mentioned|Fig.27,p509|||||||||
668|Arumbera Sandstone|43649|6|Mentioned|p457|||||||||
668|Arumbera Sandstone|43756|6|Mentioned|p542|||||||||
668|Arumbera Sandstone|43781|6|Mentioned|p4||Cambrian|Interval of mixed magnetic polarity||||||
668|Arumbera Sandstone|44111|6|Mentioned|p.58 Fig. 2|||in Amadeus Basin. Presented as Arumbera 1 & 2 and Arunbera [sic] 3 & 4 in Fig. 2.||||||
668|Arumbera Sandstone|44133|6|Mentioned|p42|||Also listed as upper Arumbera Sandstone.||||||
668|Arumbera Sandstone|44335|4|Described|p.10||Cambrian|Table 2.||||||
668|Arumbera Sandstone|44336|14|Not recorded|map legend||Cambrian|Cambrian pt of Pertaoorrta Gp. SG/53-3.||||||
668|Arumbera Sandstone|44402|5|Briefly described|map legend||Cambrian|Of Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|44433|14|Not recorded|map legend||Cambrian|||||||
668|Arumbera Sandstone|44484|14|Not recorded|Tb.2|||||||||
668|Arumbera Sandstone|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
668|Arumbera Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
668|Arumbera Sandstone|45041|4|Described|p57|||Refers Wells et al. (1967). L.Camb.||||||
668|Arumbera Sandstone|45102|6|Mentioned|p43|||See also p49.||||||05-SEP-18
668|Arumbera Sandstone|45155|6|Mentioned|p34|||Amadeus Basin. See also Figs 7 & 8||||||
668|Arumbera Sandstone|46730|5|Briefly described|p17|||Of Pertaoorrta Group.||||||
668|Arumbera Sandstone|46865|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|46903|6|Mentioned|p53|||||||||
668|Arumbera Sandstone|46928|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|46957|6|Mentioned|p165|||||||||
668|Arumbera Sandstone|47035|6|Mentioned|p83|||||||||
668|Arumbera Sandstone|48639|4|Described|p.6||Early Cambrian|Lower Cambrian. See page 1,4,16, Pl.1,Sh.3.||||||
668|Arumbera Sandstone|48865|14|Not recorded|Fig.4,opp.p.10|||Unit of Pertaoorrta Group (F53-13).||||||
668|Arumbera Sandstone|48890|4|Described|p.31||Cambrian|See also Tables, Figs, Plates. Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|48963|6|Mentioned|Fig.3|||||||||
668|Arumbera Sandstone|50246|5|Briefly described|p8-9, p20 Fig. 2|Early Cambrian|Neoproterozoic|Conformably overlain by Todd River Dolomite. A cyclical red-brown mudstone and sandstone comprising four upward coarsening members spanning Neoproterozoic-Cambrian boundary.||||||07-FEB-11
668|Arumbera Sandstone|60287|5|Briefly described|p384|Early Cambrian|Early Cambrian|Thickness: 200 m.||||||
668|Arumbera Sandstone|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red-brown sandstone, siltstone, conglomeratic sandstone; fossiliferous. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|60674|5|Briefly described|Map legend|Cambrian|Neoproterozoic|Brown, thinly-bedded, fine and medium micaceous feldspathic sandstone; minor pebble conglomerate and micaceous siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
668|Arumbera Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
668|Arumbera Sandstone|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Buff dolomitic limestone, silicified limestone, massive grey calcareous sandstone, chert.   Geological Province: Amadeus Basin.||||||20-OCT-05
668|Arumbera Sandstone|61518|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Brown, thin bedded fine-and medium grained micaceous feldspathic sandstone; minor pebble conglomerate and micaceous siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
668|Arumbera Sandstone|61732|3|Fully described|p4 Fig. 3, p99|Cambrian|Marinoan|Formerly "Arumbera Greywacke". Once part of Pertaoorta Formation (now Pertaoorrta Group). Conformably overlies the Julie Fm; overlain by Hugh River Shale, Todd River and Giles Creek Dolomites. Thick: 2km. Geol.Prov: See also p5 Tb. 1, p91.||||||17-APR-13
668|Arumbera Sandstone|62359|6|Mentioned|p554|||Geological Province: northern Amadeus Basin. ||||||
668|Arumbera Sandstone|62376|5|Briefly described|p18|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
668|Arumbera Sandstone|62379|5|Briefly described|p7 Fig. 2, p24|Middle Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Unit close to the Neoproterozoic-Cambrian border with age of: ~540Ma. Palaeomagnetic data.||||||10-FEB-09
668|Arumbera Sandstone|62453|5|Briefly described|p12 Fig. 8|Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|62595|5|Briefly described|pp8-9, p29 Fig.6, p30 Fig.7.|Cambrian|Neoproterozoic|Contains a variety of non-skeletal metazoan fossils, contemporaneous with Ediacara fauna, and a wealth of trace fossils in upper parts. 1000-1200 Ma detrital zircons reflect uplift of the Musgrave Block during the Petermann Orogeny between 570-530 Ma.||||Is conformably overlain by Todd River Dolomite.|A cyclical red-brown mudstone and sandstone unit consisting of four upward-coarsening members; massive, fine- to medium-grained, dirty sandstone into laminated shales, siltstones and rare carbonates.|
668|Arumbera Sandstone|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Arumbera.||||overlies Julie Formation||
668|Arumbera Sandstone|62984|5|Briefly described|p14|||Correlated with Central Mount Stuart Formation. Geological Province: Amadeus Basin.||||||23-JAN-07
668|Arumbera Sandstone|63397|6|Mentioned|p15|||Geological Province: Amadeus Basin.||||||23-JUL-07
668|Arumbera Sandstone|63458|6|Mentioned|p897 Fig.19. |Cambrian|Ediacaran|Amadeus Basin. Appears only as Arumbera 1&2, 3&4.||||Overlies Julie Formation.||
668|Arumbera Sandstone|63562|4|Described|p338 fig 3, p341, p345-8, p351-352|Early Cambrian|Ediacaran|Of Amadeus Basin. Either distal facies of foreland basin sediments, or reworked "autocannibalised" foreland sediments. Most zircons in it are 1.2-1.0 Ga, suggesting a source in Musgrave Inlier.||||Overlies Julie Formation. Correlated with Mount Baldwin Formation. Overlain by Todd River Dolomite.|Cross-bedded, fine- to medium-grained, red-brown quartz sandstone. Contains trace fossils.|
668|Arumbera Sandstone|64068|6|Mentioned|p51, 56, 224|||Amadeus Basin. Correlated in part with Central Mount Stuart Formation, part 3-4 with Octy Formation, Neutral Junction Formation, southern Georgina Basin.||||||
668|Arumbera Sandstone|64103|6|Mentioned|p401|Early Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|64625|5|Briefly described|p244-245, p250-251|Cambrian|Neoproterozoic|Amadeus Basin||||Disconformably overlies Julie Formation, overlain by Giles Creek Dolomite|Deep red sandstone.|
668|Arumbera Sandstone|64778|6|Mentioned|p13, 15-16, 18, 22|Neoproterozoic|Neoproterozoic|Amadeus Basin. Thermal history summarised. Max. palaeotemperature analysis summary.|590-560 Ma.|||||
668|Arumbera Sandstone|64794|6|Mentioned|p238 fig 2|Early Cambrian|Ediacaran|||||||
668|Arumbera Sandstone|64797|6|Mentioned|p153 Fig.2|Cambrian|Ediacaran|Amadeus Basin. Lithology not shown in diagram.||||||
668|Arumbera Sandstone|64809|4|Described|p1-2, p3 Fig.2, p6 Fig.4, p11 Fig.10   |Early Cambrian|Late Proterozoic|See also p12, p13 Fig.13, p15 Fig.15. Hydrocarbon reservoir; a principal exploration objective. Sourced from Musgrave Province to N and NE; deposited in predominantly deltaic environment.||Unit in Pertaoorrta Group.||Conformably (gradationally) overlies Julie Formation.|Molasse sediments: ridge-forming sandstone, recessive siltstone; contains trace fossils.|
668|Arumbera Sandstone|65233|3|Fully described|p3 Fig. 2, p7|Early Cambrian|Late Neoproterozoic|Basal unit of Pertaoorrta Group. Conformable on Julie Formation. Geological province: Amadeus Basin/Carmichael Sub-basin. Divided into 2 main depositional successions of 800m and 500m thicknesses; but max. thickness is 2000m in NE. Fluvio-deltaic.||||||07-FEB-11
668|Arumbera Sandstone|65237|6|Mentioned|p5|||Mentioned only as a correlative of the Elkera Formation in the southern Georgina Basin. Geological province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|65256|6|Mentioned|p19|Cambrian||Of the northern Amadeus Basin. Correlated with Mount Currie Conglomerate.||||||
668|Arumbera Sandstone|65272|5|Briefly described|p319, p320|Early Cambrian|Ediacaran|Amadeus Basin. Deposited during the Petermann Ranges Orogeny (570-530 Ma).||||||
668|Arumbera Sandstone|65341|5|Briefly described|pp17-18.|Ediacaran|Ediacaran|Amadeus Basin. Contains elements of the Mount Skinner fauna, similar to the Tops Member of Central Mount Stuart Formation. Upper parts also correlated with Octy Formation.||||||
668|Arumbera Sandstone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 386 m.||||Overlies Julie Formation (equivalent). Is overlain by Todd River Dolostone.||
668|Arumbera Sandstone|65365|5|Briefly described|p10 Fig. 4|Cambrian|Ediacaran|Amadeus Basin. Shown to include an unconformity above the known Ediacara fauna.||||||
668|Arumbera Sandstone|65366|5|Briefly described|p23 Fig. 3|Cambrian|Ediacaran|Amadeus Basin. Shown to include an unconformity above the known Ediacara fauna.||||||
668|Arumbera Sandstone|65410|6|Mentioned|p74.|||Amadeus Basin. Makes up Supersequence 4.||||||
668|Arumbera Sandstone|66589|6|Mentioned|p178|Early Cambrian|Early Cambrian|Case studies cited; not visited in the field by the authors of this study.||||||
668|Arumbera Sandstone|67326|5|Briefly described|p2-6, p13, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. Intersected by stratigraphic drillhole LA05DD01. Composite log.||Pertaoorrta Group.||Overlies Julie Formation. Is overlain by Todd River Dolostone and Chandler Formation.||
668|Arumbera Sandstone|67565|4|Described|p5 Fig.3, p39, p46.|Tommotian|Ediacaran|Amadeus Basin. Includes the unit previously mapped (Ranford, 1969) as Eninta Sandstone in the Gardiner Range. Thickness c.1200 m. Braided stream and prograding deltaic sediments probably sourced from highlands produced by the 570-530 Petermann Orogeny in the Musgrave Block. Sparse Ediacaran macrofauna towards the base; diverse Cambrian ichnofauna towards the top.||||Overlies the Pertatataka Formation and the Bitter Springs Formation unconformably.|Red-brown to purple-brown, thinly-bedded, fine- and medium-grained ferruginous, micaceous, feldspathic sandstone with minor pebble conglomerate and micaceous siltstone.|
668|Arumbera Sandstone|67620|6|Mentioned|p5, 22|Cambrian|Ediacaran|Amadeus Basin. In the correlation table on p5, is shown as two units: Arumbera 1 and 2, overlain by Arumbera 3 and 4. Mis-spelt as Arumberia Sandstone on p22; contains the microbial mat structure named Arumberia[sic].||||Overlies Julie Formation.||
668|Arumbera Sandstone|67856|5|Briefly described|p338 fig 4-30, p345, 346|Cambrian|Ediacaran|Shown in two parts. Includes unconformity. Contains a late Proterozoic metazoan fauna.||Of Pertaoorta Group.||Overlies Julie Formation.||
668|Arumbera Sandstone|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
668|Arumbera Sandstone|68271|5|Briefly described|p696|Ediacaran|Ediacaran|Adelaide Rift Complex. Similar lithology and taxa to Bonney Sandstone. Interpreted stratigraphic age of c. 600 Ma. Sediments like dervied from Musgrave Block.|c. 600 Ma|||||
668|Arumbera Sandstone|68323|5|Briefly described|p1-10, p12-13, p15|Early Cambrian|Neoproterozoic|Mineralogy detailed: dominated by carbonate, with lesser phengite and quatrz. Tray screem imagery.||Pertaoorrta Group.||Is overlain by Tempe Formation.|Carbonate-rich.|
668|Arumbera Sandstone|69437|5|Briefly described|p22:4-5, 8-10, 14|Early Cambrian|Ediacaran|Amadeus Basin, Centralian A Superbasin. Supersequence 4. The lower part is correlated with lower part of Yuendumu Sandstone. The upper part is included in the Centralian B Superbasin. Contains uneconomic sediment-hosted Cu occurrences.||||Overlies Inindia beds and Julie Formation. Is overlain by Namatjira, Tempe Formations and Todd River Dolostone. Equivalent to Central Mount Stuart Formation and (probably) to Carnegie Formation.|Sandstone, siltstone, shale and minor conglomerate.|12-JUL-16
668|Arumbera Sandstone|69438|3|Fully described|p23:2-8, 17-18, 20-21, 23-30, 43, 50, 53|Early Cambrian|Ediacaran|See also 23:59-60. Defined by Wells et al. (1967) as the basal Formation of the Pertaoorrta Group. Had several earlier names. Thins to the W. Comprises two fluvio-deltaic successions of upward-coarsening siltstone and sandstone, separated by a disconformity. Total thickness up to 1300m. Amadeus Basin. Forms prominent red-brown strike ridges. Includes the former Eninta Sandstone. Provenance briefly discussed; detrital zircons suggest mainly from the Musgrave Province to the S. Contains Ediacaran fauna, ichnospecies and shelly fossils. The position of the Neoproterozoic-Cambrian boundary within this unit is briefly discussed. Is overlain disconformably by Chandler Formation and Hugh River Shale, and unconformably by Tempe Formation. Contains dispersed, non-economic copper mineralisation in Namatjiras prospect (Areyonga Copper Deposit), and elsewhere eg (Ellery Creek). Has provided numerous gas shows. Reservoirs are sealed by Chandler Formation salt and possibly Tempe Formation or Giles Creek Dolostone shales.||Pertaoorrta Group.||Overlies Julie Formation conformably to disconformably. Correlative of Winnall beds and possibly Carnegie Formation. Is overlain by and interfingers with Todd River Dolostone and Namatjira Formation.|Red-brown to purple-brown, thinly-bedded, fine- and medium-grained, ferruginous, micaceous feldspathic sandstone, with minor pebble conglomerate, micaceous siltstone and dolostone.|12-JUL-16
668|Arumbera Sandstone|69439|6|Mentioned|p24:9|||Amadeus Basin. The uppermost parts of this unit contain the trace fossil Planolites ballandus Webby, which is also preserved in the Yuendumu Sandstone (Ngalia Basin).||||||12-JUL-16
668|Arumbera Sandstone|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
668|Arumbera Sandstone|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
668|Arumbera Sandstone|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Neoproterozoic|Eastern Amadeus Basin.||||||12-JUL-16
668|Arumbera Sandstone|69606|5|Briefly described|p4 fig 2, p16, p19|Cambrian|Ediacaran|Deposited during the Petermann Orogeny. Reservoir of the Pertatataka petroleum system. Amadeus Basin.||||Overlies the Julie Formation, overlain by the Upper Pertaoorta Group. Lower part is correlated with the Carnegie Formation.|Black shales and sandstone.|
668|Arumbera Sandstone|69673|5|Briefly described|p65, p76, p82, p84, p86, p91, p98, p99, |Cambrian|Ediacaran |Hosts dingo and orange gas prospects.||Pertaoorrta Group||Overlain by Namatjira Formation, Todd River Dolostone, correlates with Carnegie Formation, disconformably overlain by Chandler Formation, overlies Julie Formation|Sub-arkosic to quartzic, very fine to coarse graine, locally pebbly sandstone, some siltstone and shale.|
668|Arumbera Sandstone|69937|6|Mentioned|p34|Early Cambrian|Neoproterozoic|||||Overlies Julie Formation.||
668|Arumbera Sandstone|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Entirely of Supersequence 4 in the northern Amadeus Basin. Correlable to Mount Currie Conglomerate/Ayers Rock Arkose, and Winnall Beds.||||Underlain unconformably by Julie Formation.||
668|Arumbera Sandstone|70094|6|Mentioned|p80|||Detrital zircons from this and other units were analysed to establish similar provenances for Harts Range Group, Amadeus and Georgina Basins.||||||
668|Arumbera Sandstone|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Ediacaran|Arunta Province, Amadeus Basin.||||Lateral equivalent to Winnall Group.||
668|Arumbera Sandstone|70749|5|Briefly described|p52-53|Cambrian|Cambrian|Amadeus Basin. Deposited during the Petermann Orogeny. Contains abundant 1300-900 Ma aged detrital zircons.||||||
668|Arumbera Sandstone|70752|5|Briefly described|p126 Fig.1|Proterozoic|Proterozoic|||Pertaoorrta Group.|||Fossiliferous reddish-brown sandstone; siltstone with rare dolostone.|
668|Arumbera Sandstone|70790|6|Mentioned|p271|||||||Equivalent to Bonney Sandstone.||
668|Arumbera Sandstone|70839|5|Briefly described|p329-330,341-343,345|Cambrian|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Well-dated biostratigraphically and straddles the Ediacaran-Cambrian boundary. Interpreted as part of an immature deltaic succession.||Unit of Pertaoorrta Group.||Basal unit of Pertaoorrta Group.||12-AUG-19
668|Arumbera Sandstone|71001|6|Mentioned|p20 Fig.4, p23, 27|||Amadeus Basin. Carbon isotope correlation graph.||||Unconformably overlies Julie Formation.|Terrestrial sandstone.|
668|Arumbera Sandstone|71080|5|Briefly described|p20,  p29 fig 20, p30, 31|Ediacaran|Ediacaran|Amadeus Basin, NT. Arumberia locally common. Supersequence 4. Reservoir for Dingo Gas field in eastern Amadeus.||||Equivalent to the Carnegie Formation.|Dominantly sandstone. Some shale.|04-FEB-19
668|Arumbera Sandstone|71088|6|Mentioned|p1, p10, p12, p15, p17, p25|Cambrian|Ediacaran|Amadeus Basin. Coeval with the Petermann Orogeny. Displays late Paleoproterozoic peaks in geochronology analyses.||||Overlies the Julie Formation. Equivalent to the Maurice Formation.||01-MAY-23
668|Arumbera Sandstone|71114|5|Briefly described|p170-171, p172-175, p178-9|Terreneuvian|Ediacaran|Amadeus Basin. Age based on rare occurrences of small shelly fossils, and trace fossil Plagiogmus. Deposited in a fluvio-deltaic to basinal environment. 298m thick in Dingo 1 well.|~541-521 Ma|||Conformably overlain by Todd River Dolostone.||14-FEB-18
668|Arumbera Sandstone|71279|5|Briefly described|p353, p355 Fig.2, p358, p365-366|Early Cambrian|Ediacaran|See also p368-370, p372, p376-381, p382. Amadeus Basin. A relatively oxidised unit. Linear magnetic anomalies discussed in detail; magnetic modelling. Appears as Arumbera Shale in Tb.1 (p382).|ca 545-521 Ma (Schmid et al., 2016)|Pertaoorrta Group.|||Sandstone, siltstone, mudstone.|27-OCT-17
668|Arumbera Sandstone|71800|5|Briefly described|p26-p27|Early Cambrian|Ediacaran|Amadeus Basin.||||Overlies the Julie Formation. Overlain by the Todd River Dolostone. Correlative of Winnall beds.|Sandstone and quartz sandstone.|03-MAY-23
668|Arumbera Sandstone|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Equivalent to Winnall beds. Underlain by Inindia beds or Julie Formation.||
668|Arumbera Sandstone|71842|5|Briefly described|p2-3,9|Early Cambrian|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Divided into four informal unnamed units.||||Underlain by Julie Formation. Correlable to Amadeus Basin Early Cambrian rocks and Carnegie Formation.||08-JAN-20
668|Arumbera Sandstone|72358|6|Mentioned|p118|Series 2|Ediacaran|Of Amadeus Basin.||||||
668|Arumbera Sandstone|72369|5|Briefly described|p20-21|||Of Amadeus Basin. SHRIMP U-Pb dating by Maidment (2005) and Buick et al (2005) indicate detrital provenance spectra sominated by c. 1200-1000 Ma zircons, indicating a Musgrave Province source. Possibly correlable to Puna Kura Kura Formation.||Unit of Pertaoorrta Group.||||
668|Arumbera Sandstone|72374|6|Mentioned|p12|||Of Amadeus Basin. Correlated with Eninta Sandstone, in part.||||||11-OCT-19
668|Arumbera Sandstone|72375|5|Briefly described|p31|Early Cambrian|Late Neoproterozoic|Of Amadeus Basin. Depositional age constrained to late Neoproterozoic to early Cambrian (Edgoose, 2013; Kositcin et al., 2015).||||Underlain by Julie Formation.||
668|Arumbera Sandstone|72489|6|Mentioned|p5 Fig.4|||Only shown on p5 Fig.4. Geological field images. Same as Arumbera Formation as indicated in the Fig.4. notes.||||Partially overlies Julie Formation.|Includes sandstone.|
668|Arumbera Sandstone|72516|6|Mentioned|p90|Cambrian|Cambrian|Amadeus Basin. Age correlative of the Mount Baldwin Formation.||||||02-JUN-21
668|Arumbera Sandstone|72601|5|Briefly described|p3, p7, p25|Cambrian|Ediacaran|Amadeus Basin. Unit records the Precambrian-Cambrian boundary in the eastern Amadeus Basin by the first appearance of a Cambrian trace fossil assemblage.||||Underlain, unconformably in part, by the Julie Formation. Equivalent to Carnegie Formation, Mu Formation and Winnall beds.||
668|Arumbera Sandstone|73085|4|Described|piii, p1, p3, p7, p11, p13, p27|early Cambrian|Ediacaran|Amadeus Basin. [Written as ?Arumbera Sandstone on p3]. Lithology is here described from a 81-metre-thick equivalent in drillhole LA05DD01. Sandstone below the silicified, altered sandstone breccia at the base of the Tempe Formation were revised to be Arumbera Sandstone equivalents. Partly overlain, equivalent to and underlain by Namatjira Formation.||Pertaoorrta Group [and equivalents?]||Partly underlain by Julie Formation and Inindia beds. Overlain by Tempe Formation[?], Giles Creek Dolostone, Chandler Formation. Partly overlain by and equivalent to Todd River Dolostone.|[Possibly] finely laminated, red, fine-grained sandstone and minor siltstone with buff to grey reduction spots and common intervals of grey-green, fine-grained sandstone without reduction spots and white to pink variably kaolinised sandstone.|
668|Arumbera Sandstone|73086|6|Mentioned|p3, p5, p133|Ediacaran|Ediacaran|Amadeus Basin. Partly included in Supersequence IV. Preserves the Precambrian/Cambrian boundary.||||Underlain by Julie Formation and Inindia beds. Equivalent to Winnall Group.||
668|Arumbera Sandstone|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||||Underlain by Julie Formation.||
668|Arumbera Sandstone|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Neoproterozoic|Amadeus Basin.||||Conformably overlies the Julie Formation.||
803|Avondale Clay|23394|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
803|Avondale Clay|23818|5|Briefly described|p212 Fig.108, p227|Early Pleistocene|Early Pleistocene|Geological Province: Great Artesian Basin. Max. thickness: 250 ft.||||||05-AUG-08
803|Avondale Clay|24176|5|Briefly described|p22 Tb. 1, p20|Early Pleistocene|Early Pleistocene|Green to grey clay, ferruginous mottling.  Overlain by Telford Gravel.  Max. thickness: 161m.   Geological Province: Mount Painter Province.||||||
803|Avondale Clay|29780|6|Mentioned|p51|||||||||
803|Avondale Clay|30055|6|Mentioned|p152|||||||||
803|Avondale Clay|30056|6|Mentioned|p137|||||||||
803|Avondale Clay|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
803|Avondale Clay|30177|5|Briefly described|p107|||Pleistocene age.||||||
803|Avondale Clay|30754|6|Mentioned|p22|||Stratigraphic Table||||||
803|Avondale Clay|30807|6|Mentioned|p101|||Suggested map symbol||||||
803|Avondale Clay|30920|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
803|Avondale Clay|34180|6|Mentioned|p212|||Lower Pleistocene.||||||
803|Avondale Clay|36081|6|Mentioned|p445|||||||||
803|Avondale Clay|38605|6|Mentioned|p31|||||||||
803|Avondale Clay|39349|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene to Pleistocene||||||
803|Avondale Clay|40003|5|Briefly described|Table 5|||||||||
803|Avondale Clay|44133|6|Mentioned|p242|Quaternary|Quaternary|Corellated with the Willawortina Formation. ||||||
803|Avondale Clay|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
803|Avondale Clay|65925|5|Briefly described|Appendix 2.||||||||Clay, grey; sandy clay, with vertical mottling.|
803|Avondale Clay|69023|6|Mentioned|p125|||On COPLEY map.||||Correlated with Willawortina Formation.||
854|Backstairs Passage Formation|22573|6|Mentioned|p 53|||||||||
854|Backstairs Passage Formation|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Carrickalinga Head Formation. Overlain by Talisker Calc Siltstone||||||
854|Backstairs Passage Formation|22643|5|Briefly described|p193, fig3,6,7|Early Cambrian|Early Cambrian|||||||
854|Backstairs Passage Formation|22830|6|Mentioned|P25||Cambrian|||||||
854|Backstairs Passage Formation|22840|6|Mentioned|Table1 P38|||||||||
854|Backstairs Passage Formation|23023|6|Mentioned|p1799|||||||||
854|Backstairs Passage Formation|23317|5|Briefly described|380 Fig.2|||||||||
854|Backstairs Passage Formation|23539|5|Briefly described|Fig 1 p 467|||||||||
854|Backstairs Passage Formation|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||
854|Backstairs Passage Formation|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Of Kanmantoo Group.  Geological Province: Adelaide Fold Belt.||||||18-JUL-06
854|Backstairs Passage Formation|24195|5|Briefly described|p48|Early Cambrian|Early Cambrian|Geological Province: Adelaide Geosyncline||||||
854|Backstairs Passage Formation|24465|4|Described|p349|Early Cambrian|Early Cambrian|Of the Keynes Subgroup (Kanmantoo Gp). Contains the Tungkillo Mbr.  The Campana Creek Mbr is included for the first time - until now regarded as the top part of the Carrickalinga Head Fm.  Maximum thickness: 1100m. Overlain by Talisker Fm.||||||19-JAN-05
854|Backstairs Passage Formation|30377|2|Defined|p204|Early Cambrian|Early Cambrian|||||||
854|Backstairs Passage Formation|30378|6|Mentioned|p431|||||||||
854|Backstairs Passage Formation|30380|6|Mentioned|Table 1|||Correlation||||||
854|Backstairs Passage Formation|30381|6|Mentioned|p215|||Now part of Inman Hill Sub-group||||||
854|Backstairs Passage Formation|35255|6|Mentioned|Fig.8|||||||||
854|Backstairs Passage Formation|36836|6|Mentioned|Table 1|||||||||
854|Backstairs Passage Formation|38873|4|Described|Table 2|||||||||
854|Backstairs Passage Formation|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
854|Backstairs Passage Formation|39909|6|Mentioned|p5|||||||||
854|Backstairs Passage Formation|40228|5|Briefly described|p39|||||||||
854|Backstairs Passage Formation|40442|6|Mentioned|Table 1|||||||||
854|Backstairs Passage Formation|40454|5|Briefly described|p46|||||||||
854|Backstairs Passage Formation|40455|5|Briefly described|p71|||||||||
854|Backstairs Passage Formation|40856|6|Mentioned|Fig.23.6|||||||||
854|Backstairs Passage Formation|41494|5|Briefly described|p30|||||||||
854|Backstairs Passage Formation|41853|6|Mentioned|p199|||||||||
854|Backstairs Passage Formation|41947|6|Mentioned|p16|||||||||
854|Backstairs Passage Formation|42222|5|Briefly described|p21|||||||||
854|Backstairs Passage Formation|42225|6|Mentioned|Fig.4 P224|||||||||
854|Backstairs Passage Formation|42243|5|Briefly described|p211|||||||||
854|Backstairs Passage Formation|42270|4|Described|p362|||See also Fig.2||||||
854|Backstairs Passage Formation|42271|5|Briefly described|p385|||||||||
854|Backstairs Passage Formation|42272|5|Briefly described|p404|||||||||
854|Backstairs Passage Formation|42499|5|Briefly described|Map legend|Cambrian||||||||
854|Backstairs Passage Formation|42505|5|Briefly described|Map legend|Cambrian||||||||
854|Backstairs Passage Formation|42788|5|Briefly described|Fig.14 P148|||Of Kanmantoo Group.||||||27-MAY-08
854|Backstairs Passage Formation|43703|6|Mentioned|p75|||||||||
854|Backstairs Passage Formation|43759|6|Mentioned|p445|||||||||
854|Backstairs Passage Formation|44133|5|Briefly described|p4 Fig. 7.2, 15|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
854|Backstairs Passage Formation|60712|5|Briefly described|p27, p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Kanmantoo Group.||||||
854|Backstairs Passage Formation|60965|6|Mentioned|p201|||Contains highly weathered and kaolinised metasandstones and meta siltstones.||||||
854|Backstairs Passage Formation|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Feldspathic metasandstone, minor metasiltstone.||||||
854|Backstairs Passage Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Kanmantoo Group.  Includes marble units. Underlies Karinya Shale and Talisker Calc-Siltstone. Geological Province: Adelaide Fold Belt.||||||15-JAN-08
854|Backstairs Passage Formation|61838|6|Mentioned|p221|||Includes sandstones.||||||
854|Backstairs Passage Formation|63848|6|Mentioned|p531,  p534 Fig.4.|||Contains a trilobite trackway.|||Includes Campana Creek Member.|Overlies Carrickalinga Head Formation. Is overlain by Talisker Formation.||
854|Backstairs Passage Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Kanmantoo Trough. Thick-bedded, dark and light grey feldspathic metasandstone. Stacked planar and contorted beds, mudstone interbeds. Grades up-sequence to laminated and x-bedded metasandstone.||||||23-DEC-09
854|Backstairs Passage Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kanmantoo Group.||Overlies Carrickalinga Head Formation. Is overlain by Talisker Formation.||
854|Backstairs Passage Formation|65664|4|Described|pp1095-6, pp1101-8, Tabs.1-4,  Figs.5-6|Early Cambrian|Early Cambrian|Close lithological similarities to Middleton Sandstone.||Of Keynes Subgroup.|Includes Campana Creek Member.|Overlies Carrickalinga Head Formation. Unconformably overlain by Talisker Formation.|Dominated by relatively shallow water sandstone.|09-MAY-12
854|Backstairs Passage Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Carrickalinga Formation. Is unconformably overlain by Talisker Formation.||
854|Backstairs Passage Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kanmantoo Group.||||
854|Backstairs Passage Formation|68735|5|Briefly described|p235 Fig.3, p239|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
854|Backstairs Passage Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
854|Backstairs Passage Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Sandstone, laminated, crossbedded, minor siltstone interbeds. Widespread siltstone unit at base.|09-DEC-21
854|Backstairs Passage Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Thick-bedded, dark and light grey (feldspathic) metasandstone. Stacked planar and contorted beds, mudstone interbeds. Grades up-sequence to laminated and cross-bedded metasandstone.|
854|Backstairs Passage Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Keynes Subgroup, Kanmantoo Group|||Cross-bedded feldspathic sandstone.|
855|Backy Point Formation|22629|6|Mentioned|fig4p151|||on map||||||
855|Backy Point Formation|23719|6|Mentioned|p24|||||||||
855|Backy Point Formation|23818|6|Mentioned|p52|||||||||
855|Backy Point Formation|30801|6|Mentioned|p5|||On table. See also p6. Willouran age||||||15-JAN-19
855|Backy Point Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
855|Backy Point Formation|32507|6|Mentioned|Table 3|||||||||
855|Backy Point Formation|33468|6|Mentioned|Fig.3|||Early ? Adelaidean. See also Fig.6||||||
855|Backy Point Formation|33470|6|Mentioned|Table 1|||||||||
855|Backy Point Formation|33474|6|Mentioned|Fig.4|||||||||
855|Backy Point Formation|34116|6|Mentioned|p16|||To replace Pandurra Formation||||||
855|Backy Point Formation|34535|6|Mentioned|p52|||||||||
855|Backy Point Formation|35772|6|Mentioned|p8|||||||||
855|Backy Point Formation|38157|6|Mentioned|Table II|||||||||
855|Backy Point Formation|42546|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Willouran)|||||||
855|Backy Point Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
855|Backy Point Formation|43052|4|Described|p144|||||||||
855|Backy Point Formation|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Fluvial sandstone and conglomerate.||||||26-MAY-05
855|Backy Point Formation|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
855|Backy Point Formation|43298|5|Briefly described|Map Legend||Adelaidean|||||||
855|Backy Point Formation|44660|14|Not recorded|map legend|||Willouran, lithology.||||||
855|Backy Point Formation|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Callanna Group. Fluvial sandstone and conglomerate.||||||
855|Backy Point Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
855|Backy Point Formation|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Of the Callanna Group. Fluvial sandstone and conglomerate.||||||06-JUN-05
855|Backy Point Formation|65390|5|Briefly described|p18|||Cultana area, Moonta Domain. Coarse fluvial clastics. Unconformably overlies Pandurra Formation; intercalated with Beda Volcanics.||||||
855|Backy Point Formation|65483|5|Briefly described|p19, Fig 2|Neoproterozoic|Neoproterozoic|Unconformably overlies the Cultana Subsuite. Fluvial sandstone, is interlayered with the Beda Volcanics.||||||28-JAN-11
855|Backy Point Formation|67027|5|Briefly described|p349 Fig.2, p351 Table 1.|Mesoproterozoic|Mesoproterozoic||||||Coarse-grained sandstone, interbedded with Beda Volcanics.|
855|Backy Point Formation|68131|6|Mentioned|p89|Neoproterozoic|Neoproterozoic|||||||
855|Backy Point Formation|68158|5|Briefly described|p4|||||||Unconformably overlies Moonabie Formation, Hiltaba Suite.|Thin-bedded sandstone with cobbles.|
855|Backy Point Formation|69666|4|Described|p24, p26-29, p31, p39|Neoproterozoic|Neoproterozoic|Crawford and Forbes (1969). Referred to as Backy Point Beds by Mason et al. (1978). Exposed around the Cultana Inlier, NE Eyre Peninsula. Conglomerate clasts sourced from Cultana Subsuite, Gawler Range Volcanics, Pandurra and Moonabie Formations. Geological and HyLogger TIR and SWIR logs.||||Interbedded with Beda Basalt.|White, red to purple, fine- to coarse-grained feldspathic and lithic fluvial sandstone to conglomerate with minor interbeds of red, brown and green micaceous siltstone.|
855|Backy Point Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone; conglomerate, pink to red, locally haematitic.|
855|Backy Point Formation|70334|4|Described|p2,8,17,20,38-43,47,76,81,88-89|Tonian|Tonian|Geological province: Gawler Craton. Of Cariewerloo Basin, Stuart Shelf. Best exposed along the coast of Cultana Inlier at Backy Point, Two Hummock Point and north of Douglas Point. Extends in the subsurface N-S from Cultana Fault west to North Whyalla Hills, northwards onto AUGUSTA AND TORRENS. Deposition during early Willouran (early Neoproterozoic), after uplift of the Cultana Inlier. Contemporaneous with Gairdner Dolerite. Locally intrudes the Cultana Subsuite as a haematised sandstone dyke (Blisset et al., 1989).||||Overlain unconformably by Tapley Hill Formation. Underlain unconformably by Moonabie Formation or Cultana Subsuite or pandurra Formation. Interlayered with Beda Basalt.|Red-purple gritty sandstone; red, purple and pink, medium- to very coarse grained and feldspathic, contains Cultana Subsuite and Moonabie Formation clasts and conglomerate.|
855|Backy Point Formation|70659|6|Mentioned|p10, p14|Neoproterozoic|Neoproterozoic|||||||
855|Backy Point Formation|70816|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Gawler Ranges region.||||||
855|Backy Point Formation|70948|6|Mentioned|p974|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
855|Backy Point Formation|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown as isolated outcrop in the south east of the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2). Shown as Willouran age [?Tonian].||||Shown as age equivalent to Gairdner Dolerite. Partially equivalent to Beda Basalt.|Medium to coarse-grained arkosic sandstone with minor basaltic lavas.|
855|Backy Point Formation|71129|4|Described|p1,15, p53, 64,95,98-103,106-107|Tonian|Tonian|Of Stuart Shelf. Associated with lithospheric rifting during Willouran Epoch (Preiss, 1987). See p98 for various outcrop locations. Deposited in a fluvial enviroment. A number of informal names introduced by exploration companies are correlatives, these include: Stony Dam Conglomerate, McLeay Beds or Moonlight Conglomerate or Elizabeth Creek Conglomerate (p101 this study). Combined thickness with Beda Basalt indicates thickening from west to east. Preserved thicknesses in drillhole in SIX MILE HILL ranged from 30-60m, and up to 142.2m (PACMINEX J 12 drillhole). Original thickness is unknown as it was exposed to erosion on the Stuart Shelf during Burra Group deposition in the Adelaide Geosyncline (Preiss 2000). Inferred age is c. 827 Ma, based on interlayer nature with Beda BAsalt, and that Beda BAsalt is correlable to the 827+\-6 Ma Gairdner Dolerite. See also p109,183,184,187,207-208,225,227.|c. 827 Ma|Unit of Callanna Group.||Unconformably overlain by Tapley Hill Formation. Intercalated with Beda Basalt. Underlain by Pandurra Formation or Gawler Range Volcanics.|Fluvial sandstones; reddish-brown to purple-grey, medium- to coarse-grained, moderately- to poorly-sorted, partly gritty to pebbly, conglomerates and minor siltstones.|13-NOV-19
855|Backy Point Formation|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age given as Willouran.||||Interbedded with Beda Basalt.|Medium- to coarse-grained arkosic sandstone with minor basaltic lavas (Beda Basalt).|
855|Backy Point Formation|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age given as Willouran.||||Interbedded with Beda Basalt.|Medium- to coarse-grained arkosic sandstone with heavy mineral laminations and trough cross-bedding; local granule to cobble conglomerate.|
855|Backy Point Formation|71235|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||
855|Backy Point Formation|71236|5|Briefly described|v, p3 fig 2, p5-p6|Neoproterozoic|Neoproterozoic|Cultana Inlier, Gawler Craton. This unit has undergone haematite alteration. See also  p12, p18, p20-p21, p28-p29.||||Unconformably overlies the Cultana Subsuite. Interlayered with the Beda Volcanics.|Haematised fluvial sandstone.|
855|Backy Point Formation|71712|6|Mentioned|p411, p413 Fig 2, p415|Tonian|Tonian|Includes silicified Pandurra Formation clasts.||||Interfingered with Beda Basalt.|Feldspathic arenites.|
855|Backy Point Formation|71895|6|Mentioned|APP4. p4,|||See also the Backy Point Beds.||||||
855|Backy Point Formation|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Transitional to Backy Point Formation. Overlain by Brighton Limestone.||
855|Backy Point Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone; conglomerate, pink to red, locally haematitic.|
855|Backy Point Formation|73227|6|Mentioned|p24-25|||Sturtian.||Umberatana Group||Overlain by Tapley Hill Formation. Equivalent to Beda Basalt.|Sandstones and conglomerates.|
855|Backy Point Formation|73234|6|Mentioned|p4, p6|early Neoproterozoic|early Neoproterozoic|Stuart Shelf, Six Mile Hill. Coarse clastic fluvial sediments.||Callanna Group||||
926|Balcanoona Formation|22510|1|Redefined|table1p37, p40|||Age: Sturtian. Redefined to exclude the upper, bedded dolomite member of original definition.||||||26-NOV-22
926|Balcanoona Formation|23176|6|Mentioned|p12|||||||||
926|Balcanoona Formation|23314|5|Briefly described|331 Fig.2|||||||||
926|Balcanoona Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
926|Balcanoona Formation|23411|6|Mentioned|Map Legend|||||||||
926|Balcanoona Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
926|Balcanoona Formation|23731|5|Briefly described|p26|Adelaidean|Adelaidean|Pale grey dolomite and dolomite marble.||||||
926|Balcanoona Formation|23804|6|Mentioned|p16|||||||||
926|Balcanoona Formation|23818|4|Described|p64 Fig.22, p68|Neoproterozoic|Neoproterozoic|Of the Farina Sub-Group. Overlying unit: Angepena Formation. Underlying unit: Tapley Hill Formation. Intertongues with Tapley Hill and Angepena Formations.||||||18-APR-05
926|Balcanoona Formation|24176|4|Described|p13, p25 Tb. 1|Adelaidean|Adelaidean|See also p29.  Of Farina Sub-Group (Umberatana Group).  Equivalent to Brighton Limestone.  Represents northerly extension of Etina Limestone Member (Willochra Sub-Group). Age: Sturtian.  Max. thickness: 520m.  Geological Province: Mount Painter Province.||||||
926|Balcanoona Formation|29656|4|Described|Fig.3|||||||||
926|Balcanoona Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
926|Balcanoona Formation|30177|2|Defined|p130|Adelaidean|Adelaidean|See also p79-81. Type section: Nepouie Creek, approximately five and a half miles southwest of Wooltana Homestead, lat. 30degrees28'16"S long. 139degrees21'29"E to lat. 30degrees28'20"S long 139degrees21'38"E||||||25-NOV-22
926|Balcanoona Formation|30801|6|Mentioned|p5|||Sturtian. See also P6. On table only||||||
926|Balcanoona Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
926|Balcanoona Formation|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|Rodda Beds approx equiv.Marinoan||||||
926|Balcanoona Formation|31797|6|Mentioned|Fig. 2|||Adelaidean. Yudnamutana Sub-Gp.||||||
926|Balcanoona Formation|32720|6|Mentioned|Table 1|||||||||
926|Balcanoona Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
926|Balcanoona Formation|32724|4|Described|p518|||Sturtian. See also P519||||||
926|Balcanoona Formation|32726|6|Mentioned|p187|||Stromatolites||||||
926|Balcanoona Formation|33474|6|Mentioned|Fig.2|||||||||
926|Balcanoona Formation|34011|5|Briefly described|p67|||Sil.||||||
926|Balcanoona Formation|34069|6|Mentioned|p4|||||||||
926|Balcanoona Formation|34269|6|Mentioned|Table 1|||U.Prot.||||||
926|Balcanoona Formation|34535|6|Mentioned|p68|||||||||
926|Balcanoona Formation|34766|6|Mentioned|p58|||||||||
926|Balcanoona Formation|34957|6|Mentioned|p395|||||||||
926|Balcanoona Formation|35255|6|Mentioned|Fig.7|||||||||
926|Balcanoona Formation|35628|6|Mentioned|Table 2|||||||||
926|Balcanoona Formation|36137|6|Mentioned|p15|||||||||
926|Balcanoona Formation|36733|6|Mentioned|Table 5|||||||||
926|Balcanoona Formation|37461|4|Described|p339|||||||||
926|Balcanoona Formation|38329|6|Mentioned|p192|||||||||
926|Balcanoona Formation|39320|6|Mentioned|p380|||||||||
926|Balcanoona Formation|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
926|Balcanoona Formation|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
926|Balcanoona Formation|41405|3|Fully described|p171|||See also P161||||||
926|Balcanoona Formation|41526|6|Mentioned|p32|||See also P43||||||
926|Balcanoona Formation|42101|6|Mentioned|p84|||||||||
926|Balcanoona Formation|42222|5|Briefly described|p17|||||||||
926|Balcanoona Formation|43052|5|Briefly described|p189,Table 6.1|||||||||
926|Balcanoona Formation|44133|6|Mentioned|p100 Fig. 9.8|Adelaidean|Adelaidean|||||||05-JUL-13
926|Balcanoona Formation|64846|5|Briefly described|p197-203, p205 Tb.2, p208 Fig.10      |Cryogenian|Cryogenian|The northern part of an extensive carbonate platform across the Adelaide Geosyncline. The major part of this study. Carbon isotope details. Prograding reef facies.||Of the Nepouie Subgroup.|||Basal dolomite megabreccia facies under reef facies; shallow-water stromatolites.|
926|Balcanoona Formation|65379|5|Briefly described|p647|||A pale-grey dolomite and dolomitic marble with blue-grey stromatolitic limestone at the base. Hosts talc deposit.||||||
926|Balcanoona Formation|65493|4|Described|p907, 910-16, 919-24, Fig 1-9,11,13-16|Cryogenian|Cryogenian|Of Nepouie Subgroup, Umberatana Group. Contact with underlying Tapley Hill Formation variable from gradational to erosional. Stromatolitic limestone with edgewise conglomerate interbeds, dolomite, minor shale. Giant prograding reef complex.~1000m thick. Erosional surface at top resulting from regression, at the Sturtian-Marinoan boundary.  ||||||
926|Balcanoona Formation|65925|5|Briefly described|p124 Fig.3, Appendix 2.|||||Unit in Umberatana Group.|||Dolomite, pale grey; limestone, dark grey, algal, oolitic.|
926|Balcanoona Formation|67180|4|Described|p600-612|Cryogenian|Cryogenian|Sturtian age. Type section at Nepouie Creek. 150 - 1000m thick. Defined by Coats and Blisset 1971. Unconformable (erosional) contact with overlying Yankaninna Formation marks the Sturtian-Marinoan boundary. Can be divided into upper and lower units. Reef lithofacies include basal fore-reef talus or slope deposit, biological reef core or skeletal framework, stromatolitic framework, sheet cavity bearing grainstone, platform facies. See also Oodnaminta Reef Complex. ||Unit in Nepouie Subgroup||Underlies, interbedded with and laterally equivalent to the Angepena Formation; overlies and equivalent to the Tapley Hill Formation; stratigraphically correlated to the Brighton Limestone.|Stromatolitic limestones; ooidal limestones; columnar and branching, domal and laminar stromatolitic dolomites; microbial limestone, interbedded shale and limestone, intraclastic conglomerate limestone, fenestral fabrics; planar sheet cavities.|
926|Balcanoona Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Nepouie Subgroup.||||
926|Balcanoona Formation|67979|4|Described|p528, p530, p531, p533, p541, p545|Sturtian|Sturtian|Previously thought to correlate with Brighton Limestone of Adelaide area (Mawson and Sprigg 1950). In Northern Flinders Ranges, the Sturtian-Marinoan Series boundary is found to coincide with an erosion surface which directly overlies the lateral and time-equivalent Angepena Formation, Balcanoona Formation and Tapley Hill Formation. See Figs.1 and 2.||Nepouie Subgroup||Overlain by Angepena Formation in Nepouie Creek area and by Yankaninna Formation in Oodnaminta Hut area (Preiss et al. 1998); is unconformably overlain by Weetootla Dolomite Member (Fig.2).|shallow marine platform carbonates|
926|Balcanoona Formation|68068|5|Briefly described|Map legend|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Nepouie Subgroup.||Unconformably overlies Bolla Bollana Tillite. Is unconformably overlain by Yankaninna Formation.|Brown-weathering pale grey dolomite, strongly recrystallised obscuring most original layering; locally metasomatically altered to talc, tremolite, scapolite and chlorite schists; basal conglomerate c. 1 m thick; rare relict stromatolite 'ghosts'.|
926|Balcanoona Formation|69019|3|Fully described|p43, p46, p48-49, p134, p165.|Neoproterozoic|Neoproterozoic|Defined by Coats (in Coats and Blissett, 1971); revised by Preiss et al. (1998). Type section at Nepouie Springs. Only occurs within Flinders Ranges. Hosts Australia's major source of talc, at Mount Fitton area. Similar to Brighton Limestone at the southern end of the Adelaide Geosyncline. Has potential for dimension stone extraction.||Basal unit in Nepouie Subgroup.||Overlies Bolla Bollana Tillite unconformably or disconformably. Is overlain conformably by Tapley Hill Formation, and disconformably by Upalinna Subgroup.|Pale grey recrystallised dolomite with a distinctive yellowish to brownish weathering rind; fine- to medium-grained; essentially massive and marble-like.|
926|Balcanoona Formation|69023|4|Described|p66-72, p137, p146, p161-162, p164|Neoproterozoic|Neoproterozoic|Defined by Coats (in Coats and Blissett, 1971); revised by Preiss et al. (1998) to exclude the upper, bedded dolomite member of the original definition. Type section at Nepouie Springs. Over 1000m thick. Includes relict stromatolites. Underwent hydrothermal magnesian alteration; minor magnesite occurrences, but hosts Australia's major (up to 90%) source of talc. Exhibits incipient karst, pronounced relief and rounded boulder-clad terrain. Patterned dolomite has potential for dimension stone.||Unit in Nepouie Subgroup.||Unconformably overlies Bolla Bollana Tillite. Is faulted against Amberoona Formation. Is overlain unconformably by Yankaninna Formation.|Grey dolomitic marble with a distinctive yellowish to brownish weathering rind; strongly recrystallised and essentially massive; karst and clay-filled paleokarst features; local stylolitic bands; basal clast-supported cobble conglomerate.|
926|Balcanoona Formation|70021|5|Briefly described|p97-98|Cryogenian|Cryogenian|Northern Adelaide Fold Belt. Shallow back-reef platform facies. No hematitic lithologies or shales are present.|<658 Ma.||Oodnaminta Reef Complex.|Lateral equivalent of Angepena Formation.|Micritic, oolitic and intraclastic dolomites. Fenestral lithologies, microbial stalactitic structures, present.|
926|Balcanoona Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. In the south, this Formation includes ~20km length of a giant reef complex (the "Oodnaminta Reef") with a relief of ~1km to the E of Wortupa Well. In the north (Mount Fitton area), recrystallisation has obscured most original bedding and the unit is rarely stromatolitic. Age shown more specifically as Sturtian [Cryogenian].||Of Nepouie Subgroup.||Unconformably overlies Tapley Hill Formation. Is overlain unconformably by Yankaninna Formation (Upalinna Subgroup).|Stromatolitic, oolitic dolomite, pale grey weathering to yellowish-brown; basal conglomerate ~1m thick. Locally strongly recrystallised, or metasomatically altered to talc, tremolite, scapolite or chlorite schist.|23-JAN-19
926|Balcanoona Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Dolomite, pale grey; limestone, dark grey, algal, oolitic.|
926|Balcanoona Formation|72489|6|Mentioned|p12 Fig.9, p13 Fig.10|Cryogenian|Cryogenian|||||||
926|Balcanoona Formation|72601|6|Mentioned|p5, p25|||Biostratigraphic inferences suggest this unit may correlate to part of the Aralka Formation.||Umberatana Group||||
926|Balcanoona Formation|72613|5|Briefly described|p1-3, p5, p8, p10-11, p14-17|Cryogenian|Cryogenian |Shown as Sturtian age. Deposited in a reefal to back-reefal environment.||Umberatana Group||Underlying and laterally equivalent (in part) to the Angepena Formation. Conformably overlies and laterally equivalent to Tapley Hill Formation.|Dolomitic, stromatolitic and non stromatolitic boundstones.|
926|Balcanoona Formation|73086|6|Mentioned|p72, p78|||Adelaide Rift Complex.||||Possibly correlates to Aralka Formation.||
935|Balcoracana Formation|22766|5|Briefly described|Fig.2 p561, 562, 566|Middle Cambrian|Middle Cambrian|||||||
935|Balcoracana Formation|22857|5|Briefly described|p90 Fig. 14.7B||Late Cambrian|Of the Lake Frome Group. Geological Province: Arrowie Basin.||||||
935|Balcoracana Formation|22858|6|Mentioned|Fig14.7bp90-1|||||||||
935|Balcoracana Formation|23562|5|Briefly described|p295 Fig 2|Cambrian|Cambrian|||||||
935|Balcoracana Formation|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Of the Lake Frome Group.||||||
935|Balcoracana Formation|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
935|Balcoracana Formation|24176|4|Described|p17, p23 Tb. 1|Late Cambrian|Late Cambrian|Of the Lake Frome Group.  Red, fine-grained sandstone and siltstone.  Overlain by Pantapinna Sandstone; underlain by Moodlatana Formation.  Max. thickness: 135m  Geological Province: Mount Painter Province.||||||
935|Balcoracana Formation|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Of Lake Frome Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
935|Balcoracana Formation|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
935|Balcoracana Formation|30801|6|Mentioned|p5|||Lake Frome Group. See alsi P6. On table only||||||
935|Balcoracana Formation|30802|5|Briefly described|p11|||Middle Cambrian age||||||
935|Balcoracana Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
935|Balcoracana Formation|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
935|Balcoracana Formation|33474|6|Mentioned|Fig.3|||||||||
935|Balcoracana Formation|33932|6|Mentioned|Fig.2|||||||||
935|Balcoracana Formation|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
935|Balcoracana Formation|33973|6|Mentioned|Fig.2|||||||||
935|Balcoracana Formation|34269|6|Mentioned|Table 1|||Cambrian||||||
935|Balcoracana Formation|34610|6|Mentioned|p178|||Lake Frome Group||||||
935|Balcoracana Formation|34612|6|Mentioned|p95|||Cambrian. Correlation chart. Fig.33||||||
935|Balcoracana Formation|35255|6|Mentioned|Fig.8|||||||||
935|Balcoracana Formation|36198|6|Mentioned|Fig.I.2|||||||||
935|Balcoracana Formation|38701|6|Mentioned|p123|||||||||
935|Balcoracana Formation|40856|6|Mentioned|Fig.23.6|||||||||
935|Balcoracana Formation|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
935|Balcoracana Formation|42090|6|Mentioned|p26|||||||||
935|Balcoracana Formation|42222|6|Mentioned|Table 1 P5|||||||||
935|Balcoracana Formation|42225|6|Mentioned|Fig.4 P224|||||||||
935|Balcoracana Formation|42269|5|Briefly described|p337|||||||||
935|Balcoracana Formation|42440|6|Mentioned|Fig.2 P602|||||||||
935|Balcoracana Formation|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
935|Balcoracana Formation|44133|5|Briefly described|p4 Fig. 7.2, 5, 28, 30|Middle Cambrian|Middle Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 280m. Conformably overlies Moodlatana Formation.||||||
935|Balcoracana Formation|60889|5|Briefly described|p245 Fig.2,p247 Fig.4,p249,p252 Fig.10|Middle Cambrian|Middle Cambrian|Transgressive. Thickness: 460 m. Arrowie Basin. Shown as Balcoracana Fm.||Lake Frome Group||Overlies Moodlatana Formation. Is overlain by Pantapinna Sandstone.|Cyclic succession of red shales and siltstones with thin beds of stromatolitic carbonate.|
935|Balcoracana Formation|60959|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Lake Frome Group. Red and green micaceous siltstone, shale, carbonate cycles.||||||23-DEC-09
935|Balcoracana Formation|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Lake Frome Group.||Overlies Moodlatana Formation. Is overlain by Pantapinna Sandstone.|Redbeds.|
935|Balcoracana Formation|62787|6|Mentioned|p82 Fig. 3|Middle Cambrian|Middle Cambrian|Geological Province: Arrowie Basin (SA).||||||07-FEB-11
935|Balcoracana Formation|63569|5|Briefly described|p117 Fig.1|Middle Cambrian|Middle Cambrian|Arrowie Basin. Thickness 460 m.||Unit in Lake Frome Group.||||
935|Balcoracana Formation|64829|5|Briefly described|p1084-5 Figs.1,  2|Late Cambrian|Middle Cambrian|Unit discussed in the context of soilscapes and palaeosols. Geological province: Arrowie Basin.||||||07-FEB-11
935|Balcoracana Formation|65313|5|Briefly described|p577, p576 Fig. 5,  p578 Fig. 6|Middle Cambrian|Middle Cambrian|Age: Leiopyge laevigata zone from trilobites in uppermost part of unit in Lake Frome 3 well, eastern Arrowie Basin. Shown as Arcadian age in Fig. 6.|~ 504 Ma.|Of Lake Frome Group.||Overlies Moodlatana Formation; underlies Pantapinna Sandstone.||26-MAR-12
935|Balcoracana Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Lake Frome Group.||Overlies Moodlatana Formation. Is overlain by Pantapinna Sandstone.||
935|Balcoracana Formation|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.||Of Lake Frome Group.||Underlain by Moodlatana Formation.||16-FEB-11
935|Balcoracana Formation|65686|5|Briefly described|p411,  p409 Fig 2|Middle Cambrian|Middle Cambrian|Arrowie Basin, 460m thick.||||||
935|Balcoracana Formation|65892|5|Briefly described|p7 Fig.3, p9 Fig.4, p11, p48. |Middle Cambrian|Middle Cambrian|Arrowie Basin. 460m thick. Transgressive unit.||Unit in Lake Frome Group.||Overlies Moodlatana Formation. Is overlain by Pantapinna Sandstone.|Cyclic succession of red shales and siltstones with thin beds of stromatolitic carbonates.|
935|Balcoracana Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Middle Cambrian|Middle Cambrian|Trilobite tracks.||Unit in Lake Frome Group.|||Very micaceous siltstone, shale, carbonate; arkosic sandstone, fine-grained and cross-bedded.|
935|Balcoracana Formation|66518|5|Briefly described|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||Unit in Lake Frome Group.||Overlies Moodlatana Formation and is overlain by Pantapinna Sandstone.||06-FEB-14
935|Balcoracana Formation|68735|4|Described|p233 Fig.2, p234-p236, p238|Middle Cambrian|Middle Cambrian|Arrowie Basin. ~ 460 m thick. Contains ripples, mudcracks, and halite clasts. Suggested shallow subtidal to supratidal depositional environment.||Of the Lake Frome Group.||Underlain by the Moodlatana Formation. Overlain by the Pantapinna Sandstone.|Comprises a cyclic succession of shallowing upwards packages of red shales and very micaceous siltstones (with abundant arthropod tracks) that pass up into thin horizons of cryptomicrobial laminated and stromatolitic carbonates.|10-APR-17
935|Balcoracana Formation|68993|5|Briefly described|p543, p544 Fig.1|Middle Cambrian|Middle Cambrian|Arrowie Basin.||Of the Lake Frome Group.||Equivalent to the Coobowie Limestone.||
935|Balcoracana Formation|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
935|Balcoracana Formation|72449|5|Briefly described|p2 Map Legend|Cambrian|Cambrian|||||Overlies Moodlatana Formation and underlies Pantapinna Sandstone.|Repetitively bedded red-brown mica-rich siltstone and shale with thin limestone bands; ripple marks, mudcracks and salt casts are common.|
935|Balcoracana Formation|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||Lake Frome Group||Underlain by Moodlatana Formation. Overlain by Pantapinna Sandstone.||
947|Baldry Rhyolite|24474|3|Fully described|p40|||Predominantly on GAIRDNER area - included by Blissett (1980) in Wheepool Rhyolite.  However, Giles (1977, 1980) interpreted this unit to be a local rhyolite overlying the Bunburn Dacite.  Geological Province: Gawler Craton.||||||
947|Baldry Rhyolite|30984|2|Defined|p13|Proterozoic|Proterozoic|||||||
947|Baldry Rhyolite|41974|6|Mentioned|Fig.1 P408|||||||||
947|Baldry Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
947|Baldry Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
947|Baldry Rhyolite|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
947|Baldry Rhyolite|43071|6|Mentioned|p14|||||||||
947|Baldry Rhyolite|43094|5|Briefly described|p26|||||||||
947|Baldry Rhyolite|67909|5|Briefly described|p126-130|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Shows intense flow deformation (sheath folds) in the interior of the unit. Volcanic textures and emplacement mechanism tabulated.||Glyde Hill Volcanic Complex.|||Includes autobreccia zones.|
947|Baldry Rhyolite|69649|5|Briefly described|p23-24|Mesoproterozoic|Mesoproterozoic|Blissett (1980) included this unit in the Wheepool Rhyolite; Giles (1977, 1980) interpreted it as a separate local unit.||Unit in Glyde Hill Volcanic Complex.||Overlies Bunburn Dacite.|White to off-white rhyolite showing semi-continuous flow-banding, with medium-grained quartz phenocrysts, flattened lithic and pumice fragments, and abundant spherulites and lithophysae in a densely welded rhyolitic ignimbrite.|24-FEB-15
947|Baldry Rhyolite|70659|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.||||
947|Baldry Rhyolite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Nuckulla Basalt. Underlain by Bunburn Dacite.||
947|Baldry Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
964|Balhannah Shale Member|22869|6|Mentioned|P38|||||||||
964|Balhannah Shale Member|30801|6|Mentioned|p5|||Torrensian. See also P6. On table only.||||||
964|Balhannah Shale Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
964|Balhannah Shale Member|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
964|Balhannah Shale Member|33423|4|Described|p12|||Strat.||||||
964|Balhannah Shale Member|33951|6|Mentioned|p7|||Soil development discussed||||||
964|Balhannah Shale Member|34320|5|Briefly described|p169|||Lithology & structure||||||
964|Balhannah Shale Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
964|Balhannah Shale Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
964|Balhannah Shale Member|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
964|Balhannah Shale Member|40294|6|Mentioned|p35|||||||||
964|Balhannah Shale Member|40442|6|Mentioned|p8|||||||||
964|Balhannah Shale Member|41404|4|Described|p105|||||||||
964|Balhannah Shale Member|42222|6|Mentioned|p14|||||||||
964|Balhannah Shale Member|43052|6|Mentioned|p179|||of Woolshed Flat Shale||||||
1009|Balparana Sandstone|22510|5|Briefly described|p40, Table 1|||Age: Marinoan.  Equivalent to the Grampus Quartzite in the northern Flinders Ranges.||||||13-OCT-04
1009|Balparana Sandstone|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
1009|Balparana Sandstone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group).||||||
1009|Balparana Sandstone|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
1009|Balparana Sandstone|23818|5|Briefly described|p64 Fig.22, p72|Neoproterozoic|Neoproterozoic|Of the Yerelina Sub-Group. Max thickness: 300 ft.||||||
1009|Balparana Sandstone|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Yerelina Sub-Group.  Feldspathic sandstone with quartz granules and pebbles.  Overlies Mount Curtis Tillite.  Equivalent of Elatina Formation.  Max. thickness: 215m. Age is Marinoan.  Geological Province: Mount Painter Province.||||||
1009|Balparana Sandstone|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
1009|Balparana Sandstone|30177|2|Defined|p132, ?321|Adelaidean|Adelaidean|See also p87. Type section Approximately a quarter of a mile west of Mount Saturday, lat 30degrees07'31"S long. 139degrees15'50"E to lat. 30degrees07'42"S long.139degrees15'41"E.||Yerelina Sub-Group||||08-DEC-22
1009|Balparana Sandstone|30261|6|Mentioned|Table 1|||Marinoan age||||||
1009|Balparana Sandstone|30801|6|Mentioned|p5|||Marinoan. See also P6. On table only||||||
1009|Balparana Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
1009|Balparana Sandstone|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
1009|Balparana Sandstone|33474|6|Mentioned|Fig.2|||||||||
1009|Balparana Sandstone|34535|5|Briefly described|p72|||||||||
1009|Balparana Sandstone|34812|6|Mentioned|p134|||||||||
1009|Balparana Sandstone|35255|6|Mentioned|Fig.7|||||||||
1009|Balparana Sandstone|36137|5|Briefly described|p16|||Palaeomagnetism discussed.||||||
1009|Balparana Sandstone|36733|6|Mentioned|Table 5|||||||||
1009|Balparana Sandstone|37461|6|Mentioned|p342|||||||||
1009|Balparana Sandstone|37932|5|Briefly described|p546|||See also p544.||||||09-JUN-22
1009|Balparana Sandstone|38157|6|Mentioned|Table IV|||||||||
1009|Balparana Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
1009|Balparana Sandstone|41236|6|Mentioned|p65|||||||||
1009|Balparana Sandstone|41405|3|Fully described|p198|||||||||
1009|Balparana Sandstone|42222|6|Mentioned|p18|||||||||
1009|Balparana Sandstone|42239|6|Mentioned|p161|||||||||
1009|Balparana Sandstone|42542|5|Briefly described|p8|||||||||
1009|Balparana Sandstone|43052|5|Briefly described|p190,Table 6.1|||of Yerelina Subgroup||||||
1009|Balparana Sandstone|68241|6|Mentioned|p20 Fig.1|||||||||
1009|Balparana Sandstone|69019|3|Fully described|p51, p53-54.|Neoproterozoic|Neoproterozoic|Defined by Coats (in Coats and Blissett, 1971); type section just W of Mt Saturday (Flinders Ranges) where it is ~130 m thick.||Unit in Yerelina Subgroup.||Conformably overlies Mount Curtis Tillite. Is overlain conformably by Ketchowla Siltstone.|White medium-grained well sorted gritty feldspathic sandstone; lenticular conglomerate.|
1009|Balparana Sandstone|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||Of Yerelina Subgroup.|||Feldspathic, well-sorted, medium-grained white sandstone; gritty, lenticular bedding, some graded- and cross-bedding; minor quartz granules and pebbles.|23-JAN-19
1009|Balparana Sandstone|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Sandstone, pale grey, medium-grained, siltstone, minor, grit and pebble lenses.|
1011|Balta Granite|22430|6|Mentioned|p2||Proterozoic|||||||
1011|Balta Granite|22629|6|Mentioned|p157|||||||||
1011|Balta Granite|22851|6|Mentioned|13|||||||||
1011|Balta Granite|23054|6|Mentioned|p33|||||||||
1011|Balta Granite|23123|5|Briefly described|p404||Mesoproterozoic|||||||
1011|Balta Granite|23480|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Age: 1584+/-18 Ma (U-Pb)||||||07-NOV-08
1011|Balta Granite|24197|5|Briefly described|p30, p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: ~1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
1011|Balta Granite|34830|2|Defined|p11|Late Precambrian|Late Precambrian|||||||
1011|Balta Granite|36244|6|Mentioned|p2|||Defined by Benbow & Flint 1979.||||||
1011|Balta Granite|36733|6|Mentioned|p49|||||||||
1011|Balta Granite|38604|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1011|Balta Granite|38605|6|Mentioned|p15|||See also Table 2.||||||
1011|Balta Granite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Post-Kimban Orogeny. 1550 - 1450Ma.||||||
1011|Balta Granite|41405|6|Mentioned|p154|||||||||
1011|Balta Granite|42469|5|Briefly described|p21|||Billa Kalina SH53-07||||||
1011|Balta Granite|42723|5|Briefly described|map legend|Mesoproterozoic||||||||
1011|Balta Granite|43048|4|Described|Table 1.|||||||||
1011|Balta Granite|43052|5|Briefly described|Table 5.6|||of Hiltaba Suite||||||
1011|Balta Granite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Anorogenic granitoids. Geological Province: Mt Woods Inlier.||||||26-MAY-05
1011|Balta Granite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1011|Balta Granite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
1011|Balta Granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||
1011|Balta Granite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1600-1580Ma. Dominantly anorogenic granitoids. Geological Province: Mount Woods Inlier.||||||
1011|Balta Granite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Geological Province: Mt Woods Inlier. Age: 1598-1575 Ma.||||||23-JUN-05
1011|Balta Granite|64132|6|Mentioned|p1419 Fig.3. |Mesoproterozoic|Mesoproterozoic|||Unit in Hiltaba Suite.|||Mafic intrusions.|
1011|Balta Granite|64133|6|Mentioned|p1446 Fig.4|Mesoproterozoic|Mesoproterozoic|||Unit in Hiltaba Suite.||||
1011|Balta Granite|64135|5|Briefly described|p1501, p1504. |||Central Mount Woods inlier.|1586 +/- 3 Ma (U-Pb zircon age).|Unit in Hiltaba Suite.||||
1011|Balta Granite|65376|6|Mentioned|p147.|||||Unit in Hiltaba Suite.||||
1011|Balta Granite|65390|5|Briefly described|p13, p22 Fig. 3, p26 Tb. 1|Calymmian|Calymmian|Mount Woods Domain. Of Hiltaba Suite. Even-grained and porphyritic granite and adamellite, brick-red granite, hybrid granite and (?) diorite. Conflicting ages given: a SHRIMP U-Pb age of 1584 +/- 18 Ma (Fanning, 1987) and a Rb-Sr age of  ~1540 - 1450 Ma (Ambrose and Flint, 1981).||||||
1011|Balta Granite|66302|5|Briefly described|p45|Calymmian|Calymmian||1584 +/- 18 Ma (U-Pb, Finlay, 1993)|Hiltaba Suite||Intrudes the Mount Woods Complex and the Engenina Adamellite.|Granite.|
1011|Balta Granite|72459|6|Mentioned|p51|Mesoproterozoic|Mesoproterozoic||1584 +/- 18 Ma|||||
1011|Balta Granite|72949|6|Mentioned|p34|Calymmian|Statherian|[Abbreviation of Balta Granite Suite?].|1584 +/- 18 Ma|||||
1011|Balta Granite|73155|5|Briefly described|p265, p267-269, p273, p275, p284-285|Calymmian|Calymmian|Mount Woods Domain. Equivalent to Hiltaba Suite and Gawler Range Volcanics. Contains mylonitic bands at Moonlight Shear Zone. Appears to crosscut western end of Skylark Fault detachment structure. See also p280. Balta Granite Suite also used.|1584 +/- 18 Ma|Hiltaba Suite||Faulted against Skylark Metasediments.|Includes diorites, granodiorites and granites, and a pink K-feldspar-rich equigranular granite.|
1138|Barossa Complex|22629|6|Mentioned|p145|||||||||
1138|Barossa Complex|22643|5|Briefly described|p183, fig3p187|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
1138|Barossa Complex|22869|5|Briefly described|P38, Fig2, Fig6||Paleoproterozoic|||||||07-NOV-08
1138|Barossa Complex|23023|6|Mentioned|Fig1p1798|||||||||
1138|Barossa Complex|23818|5|Briefly described|p32|||Overlying unit: Burra Group (unconformable).||||||19-JUL-06
1138|Barossa Complex|24425|6|Mentioned|p16|||Fractured rock aquifer.||||||
1138|Barossa Complex|29697|6|Mentioned|p7|||||||||
1138|Barossa Complex|30377|6|Mentioned|p201|||||||||
1138|Barossa Complex|31292|6|Mentioned|p2|||Refers Parkin et al. (1969)||||||
1138|Barossa Complex|31321|6|Mentioned|p15|||Mineral deposits||||||
1138|Barossa Complex|31322|6|Mentioned|p23|||Stratigraphy||||||
1138|Barossa Complex|31923|6|Mentioned|p6|||||||||
1138|Barossa Complex|32032|6|Mentioned|p6|||||||||
1138|Barossa Complex|32791|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|33004|6|Mentioned|p126|||||||||
1138|Barossa Complex|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
1138|Barossa Complex|33423|4|Described|p12|||Precamb. See P10.||||||
1138|Barossa Complex|33473|6|Mentioned|p4|||Precambrian||||||
1138|Barossa Complex|33547|6|Mentioned|Fig.6|||||||||
1138|Barossa Complex|34308|6|Mentioned|p189|||||||||
1138|Barossa Complex|34535|6|Mentioned|p57|||||||||
1138|Barossa Complex|34536|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1138|Barossa Complex|34537|5|Briefly described|p32|||||||||
1138|Barossa Complex|34612|6|Mentioned|p95|||||||||
1138|Barossa Complex|34720|6|Mentioned|p329|||||||||
1138|Barossa Complex|35090|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|35232|6|Mentioned|Fig.2|||||||||
1138|Barossa Complex|35354|6|Mentioned|p46|||||||||
1138|Barossa Complex|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
1138|Barossa Complex|36626|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|36816|5|Briefly described|Table 1|||See also Fig.2||||||
1138|Barossa Complex|36834|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|36835|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|37461|6|Mentioned|Table 5.I|||||||||
1138|Barossa Complex|37853|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|38107|6|Mentioned|Fig.2|||||||||
1138|Barossa Complex|39350|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1138|Barossa Complex|39351|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1138|Barossa Complex|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1138|Barossa Complex|39840|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|39842|6|Mentioned|Fig.1|||||||||
1138|Barossa Complex|40003|5|Briefly described|Table 16|||||||||
1138|Barossa Complex|40228|5|Briefly described|Fig.1|||||||||
1138|Barossa Complex|40294|6|Mentioned|Table 2|||||||||
1138|Barossa Complex|40456|6|Mentioned|Fig.2|||||||||
1138|Barossa Complex|40500|5|Briefly described|Fig.2|||Mention p129.||||||31-OCT-22
1138|Barossa Complex|40501|6|Mentioned|p115|||||||||
1138|Barossa Complex|40503|4|Described|p112|||||||||
1138|Barossa Complex|41125|6|Mentioned|p55|||||||||
1138|Barossa Complex|41402|6|Mentioned|p39|||||||||
1138|Barossa Complex|41404|6|Mentioned|Table 11|||||||||
1138|Barossa Complex|41494|6|Mentioned|p30|||||||||
1138|Barossa Complex|41526|6|Mentioned|p27|||||||||
1138|Barossa Complex|42505|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
1138|Barossa Complex|42733|5|Briefly described|map legend|Proterozoic||||||||
1138|Barossa Complex|43052|5|Briefly described|p102|||||||||
1138|Barossa Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, calcsilicate. Geological Province: Mt Lofty Ranges.||||||07-NOV-08
1138|Barossa Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
1138|Barossa Complex|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
1138|Barossa Complex|43759|6|Mentioned|p450||Paleoproterozoic|||||||07-NOV-08
1138|Barossa Complex|44133|6|Mentioned|p47 Fig. 7.17|||||||||
1138|Barossa Complex|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: >1590Ma (metamorphic age). Layered paragneiss, calcsilicate, orthogneiss, minor felsic to mafic dykes. Largely retrogressed to phyllonite.||||||07-NOV-08
1138|Barossa Complex|60965|5|Briefly described|p201|Archean|Archean|Schists and gneisses.  In the Fleurieu Peninsula region.||||||10-DEC-09
1138|Barossa Complex|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Layered paragneiss, calcsilicate, orthogneiss and minor dykes of granite, pegmatite and amphibolite. Largely retrogressed to phyllonite. Age: >1590 Ma (metamorphic age).||||||07-NOV-08
1138|Barossa Complex|63020|6|Mentioned|p972 Fig. 1b, p973|||Includes metamorphic rocks that form the basement of Adelaidean and Cambrian cover sequences of the Adelaide Rift Complex. See also p974 Fig. 2. ||||||
1138|Barossa Complex|64130|5|Briefly described|p1378 Fig.1 |Paleoproterozoic|Paleoproterozoic||~1715 Ma|||||
1138|Barossa Complex|64233|4|Described|p21, p22 Fig. 2, p25|Mesoproterozoic|Paleoproterozoic|Underwent high-grade metamorphism at ~1590-1580Ma. Consists of 5 Palaeo-Mesoproterozoic inliers in SA - Houghton, Warren, Oakbank, Aldgate, Myponga Inliers. Poly-deformed metasediments, orthogneiss, migmatites, pegmatites and post-defomational intrusives.Depositional age of Houghton Inlier said to be ~1740-1715 Ma.||||||09-FEB-17
1138|Barossa Complex|64647|4|Described|p38 Fig. 1, p39, p46, p48, p39|Paleoproterozoic|Paleoproterozoic|Overlain unconformably by Burra, Umberatana and Wilpena Groups. Coarse-grained sillimanite-muscovite schist and gneiss. Geological Province: Houghton Inlier.||||||10-DEC-09
1138|Barossa Complex|65220|6|Mentioned|p20, p21, p19 Fig.1|Mesoproterozoic|Mesoproterozoic|Shows evidence of deformation event at 1590-1580 Ma||||||10-DEC-09
1138|Barossa Complex|65376|6|Mentioned|p9 Fig.1.2. |Paleoproterozoic|Paleoproterozoic|||||||
1138|Barossa Complex|66302|6|Mentioned|p72, p75, p77 Fig.21, p77, p88|||Underwent high-grade metamorphism and deformation between 1590-1580 Ma (U-Pb LA-ICPMS). ||||Probably equivalent to the Willyama Supergroup.||
1138|Barossa Complex|67536|5|Briefly described|Map Legend|Statherian|Statherian|Mount Lofty Ranges Inliers.|ca. 1590 Ma; 1587 +/- 22 Ma||||Paragneiss, calcsilicate and orthogneiss, metamorphism ca. 1590 Ma and intrusive aplite 1587 +/- 22 Ma.|
1138|Barossa Complex|67900|6|Mentioned|p31|||Underwent Early Mesoproterozoic high-T metamorphism and associated deformation.||||||
1138|Barossa Complex|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
1138|Barossa Complex|68158|6|Mentioned|p2, p5||||1740-1650 Ma.|||||
1138|Barossa Complex|68811|5|Briefly described|p83|Precambrian|Precambrian|Overlain by tillites, quartzites, dolomites, phyllites, slates and siltstones.|||||Schist and micaceous gneisses.|
1138|Barossa Complex|69255|5|Briefly described|p769-790|||Located immediately adjacent to the Tasman Line. Underwent high-grade metamorphism between 1590-1580 Ma and further metamorphism around 1625 +/- 9 Ma. This article discusses timing, P-T conditions and evolution of metamorphic history of the Complex and other crustal domains.|||||Includes granulite-facies metapelites.|
1138|Barossa Complex|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1700 Ma|||||
1138|Barossa Complex|70659|5|Briefly described|p3|Mesoproterozoic|Palaeoproterozoic|Basement inliers within the Neoproterozoic Adelaide Geosyncline. Metamorphosed at ~1590-1580 Ma.|||||Granulite-facies metamorphosed metapelitic rocks.|
1138|Barossa Complex|71237|14|Not recorded|p9, |||||||||
1138|Barossa Complex|71238|14|Not recorded|p2, 9|Archean|Archean|||||||
1138|Barossa Complex|72949|6|Mentioned|p33, p37|||Stratigraphic unit or geological province?||||||24-DEC-21
1138|Barossa Complex|73092|5|Briefly described|p1-3, p5, p8, p11|Proterozoic|Proterozoic|Proterozoic basement of the Adelaide Rift Complex. Yorke Peninsula region. Represents the reworked eastern margin of the Gawler Craton. Ages are of magmatic crystallisation; metamorphic ages include 1629 +/- 17 Ma, 1638 +/- 10 Ma, 1650 +/- 23 Ma. Dated samples are augen gneiss from Houghton Inlier. Southeastern-most exposure of pre-Neoproterozoic crust in Australia. Deposition of metasedimentary protoliths occurred between 1730-1655 Ma. Deposition was synchronous with that of the Willyama Supergroup and onset of the Kimban Orogeny in the Gawler Craton.|1709 +/- 25 Ma, 1678 +/- 30 Ma||||Metasedimentary and meta-igneous gneisses, including calcsilicate, quartzofeldspathic, psammopelitic, and pelitic gneisses.|
1138|Barossa Complex|73188|5|Briefly described|p308, p314, p316, p326-327, p349-351|ca Statherian|ca Statherian|Adelaide and Mount Lofty Ranges region. Crystalline basement. A comparatively more resistant paragneiss from this unit composes Mount Gawler. Main structural grain trends north-south to northwest-southeast.|ca 1.7 Ga||||Includes paragneiss, metasedimentary and intrusive rocks deformed and metamorphosed at amphibolite to granulite facies.|
1138|Barossa Complex|73235|6|Mentioned|p52|Calymmian|Statherian||c. 1715-1580 Ma|||||
1138|Barossa Complex|73262|6|Mentioned|p580|||Basement in the Warren and Oakbank inliers within the Mount Lofty Ranges.|ca 1600 Ma|||Intruded by Mount Crawford Granite Gneiss.||27-JAN-23
1138|Barossa Complex|73512|6|Mentioned|p8|||||||||
1138|Barossa Complex|73644|6|Mentioned|p3 Fig.2|Paleoproterozoic|Paleoproterozoic||c. 1700-1650 Ma|||||
1138|Barossa Complex|74367|6|Mentioned|p16|||||||||
1408|Belair Subgroup|22510|5|Briefly described|table1 p37|Adelaidean|Adelaidean|Age: Sturtian. Top of Burra Group.||||||13-OCT-04
1408|Belair Subgroup|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
1408|Belair Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Burra Group. Age: >700Ma.||||||
1408|Belair Subgroup|22889|4|Described|p35-37 & p39|Adelaidean|Adelaidean|The Belair Subgroup remains unchanged in it's type area near Adelaide, but is redefined in the Mid-North to include the Mintaro Shale and it's redefined Leasingham Quartzite Member.||||||
1408|Belair Subgroup|23869|4|Described|p20|||Of the Burra Group.||||||
1408|Belair Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||07-JAN-10
1408|Belair Subgroup|32720|6|Mentioned|Table 1|||||||||
1408|Belair Subgroup|32722|6|Mentioned|Fig.3|||Adelaidean||||||
1408|Belair Subgroup|35232|6|Mentioned|p5|||See also Table.1||||||
1408|Belair Subgroup|36733|6|Mentioned|Table 5|||||||||
1408|Belair Subgroup|37238|6|Mentioned|p363|||||||||
1408|Belair Subgroup|37461|4|Described|p338|||See also Table 5.I||||||
1408|Belair Subgroup|38157|6|Mentioned|Table 1|||||||||
1408|Belair Subgroup|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
1408|Belair Subgroup|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
1408|Belair Subgroup|39351|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
1408|Belair Subgroup|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
1408|Belair Subgroup|39643|6|Mentioned|p3|||||||||
1408|Belair Subgroup|40228|5|Briefly described|Fig.1|||||||||
1408|Belair Subgroup|40294|6|Mentioned|p41|||See also P58||||||
1408|Belair Subgroup|40442|6|Mentioned|Fig.4|||||||||
1408|Belair Subgroup|40456|6|Mentioned|Fig.2|||||||||
1408|Belair Subgroup|40500|5|Briefly described|p138|||||||||
1408|Belair Subgroup|40852|6|Mentioned|Fig.3.2|||||||||
1408|Belair Subgroup|40910|6|Mentioned|p10|||||||||
1408|Belair Subgroup|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
1408|Belair Subgroup|41401|6|Mentioned|p32|||||||||
1408|Belair Subgroup|41404|4|Described|p118|||||||||
1408|Belair Subgroup|41405|5|Briefly described|Fig.54|||Mention P125||||||
1408|Belair Subgroup|41494|6|Mentioned|p31|||||||||
1408|Belair Subgroup|42098|5|Briefly described|p53|||||||||
1408|Belair Subgroup|42222|4|Described|p15|||||||||
1408|Belair Subgroup|42243|5|Briefly described|p211|||||||||
1408|Belair Subgroup|42272|5|Briefly described|p408|||||||||
1408|Belair Subgroup|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Sturtian)|||||||
1408|Belair Subgroup|42720|5|Briefly described|map legend|Sturtian|Torrensian|||||||
1408|Belair Subgroup|42733|5|Briefly described|map legend|Adelaidean||||||||
1408|Belair Subgroup|42813|5|Briefly described|p17|||of Burra Group||||||
1408|Belair Subgroup|43052|5|Briefly described|p183,Table 6.1|||of Burra Group||||||
1408|Belair Subgroup|43190|5|Briefly described|Fig.2p29.Fig3.|||of Burra Group.||||||
1408|Belair Subgroup|61237|5|Briefly described|p36|||Contains the importnant building stone known as Glen Osmond Bluestone, quarried from the subgroup's shale, in the foothills of Adelaide (SA).||||||
1408|Belair Subgroup|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Burra Group. Includes the Kadlunga Slate, Gilbert Range Quartzite and Mintaro Shale. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
1408|Belair Subgroup|62592|5|Briefly described|p50 Table 5.1, pp57-58.|Sturtian|Sturtian|Adelaide Geosyncline.||Unit in Burra Group.||Overlies Bungarider Subgroup.|Sandstone, siltstone.|
1408|Belair Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in upper Burra Group.|||Sandstone.|
1408|Belair Subgroup|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of the Burra Group. Represents regressive/transgressive deposits in the Mintaro Shale, Gilbert Range Quartzite and Kadlunga Slate.||||||07-FEB-11
1408|Belair Subgroup|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|||Unit in Burra Group.|Includes Mintaro Shale.|||
1408|Belair Subgroup|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
1408|Belair Subgroup|65925|5|Briefly described|Appendix 2.||||||||Siltstone, dark grey, laminated with minor sandstone, dolomite interbeds; quartzite, fine to coarse, feldspathic, cross bedded, minor siltstone interbeds; slate.|
1408|Belair Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Burra Group.||||
1408|Belair Subgroup|70405|6|Mentioned|p1, p50, p51 table 4, p79, p97|Cryogenian|Cryogenian|||Burra Group|Includes Mintaro Shale, Gilbert Range Quartzite, Kadlunga Slate|||
1408|Belair Subgroup|70660|6|Mentioned|p34 fig 19e|||||||||
1408|Belair Subgroup|70819|6|Mentioned|p11, 13, 16, 28|Neoproterozoic|Neoproterozoic|Clare Valley.||Burra Group.|Leasingham, Gilbert Range Quartzites; Mintaro Shale; Kadlunga Slate.|Unconformably overlies Bungarider Subgroup. Is overlain unconformably by Yudnamutana Subgroup (Umberatana Group).||
1408|Belair Subgroup|72450|5|Briefly described|Brochure map|||||Burra Group|||Laminated, grey siltstone.|
1408|Belair Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, dark grey and sandstone, minor dolomite interbeds.|09-DEC-21
1408|Belair Subgroup|73188|5|Briefly described|p315-316, p325-326, p329-330, p340|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Quartzose of this unit forms the summit of Mount Magnificent.||Burra Group|Mitcham Quartzite||Includes arkose, siltstone and quartzite.|
1408|Belair Subgroup|74367|5|Briefly described|p3, p7 Fig.6, p8|Tonian|Tonian|||Burra Group|Mitcham Quartzite, Mintaro Shale, Gilbert Range Quartzite, Kadlunga Slate|||
1415|Belfast Mudstone|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1362m.||Sherbrook Group.||Overlies Flaxman Formation. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|12796|4|Described|p458, p456 Fig. 2|Santonian|Coniacian|Of the Sherbrook Group. Glauconitic dark mudstones. Interfingers with and underlies Nullawarre Greensand; overlies Flaxman Formation. Geological Province: Otway Basin/Port Campbell Embayment. ||||||
1415|Belfast Mudstone|22674|5|Briefly described|Fig.2 p719|Santonian|Cenomanian|||||||
1415|Belfast Mudstone|22875|3|Fully described|p42|Campanian|Cenomanian|Of the Sherbrook Group.||||||27-MAR-07
1415|Belfast Mudstone|22930|6|Mentioned|50|||||||||
1415|Belfast Mudstone|22944|5|Briefly described|Fig3|||||||||
1415|Belfast Mudstone|23818|4|Described|p164, 165|Late Cretaceous|Late Cretaceous|Overlain by Paaratte Formation; underlain by Flaxman Formation. Geological Province: Otway Basin. Max. thickness: ~1000 ft.||||||27-MAR-07
1415|Belfast Mudstone|23830|6|Mentioned|Fig. 6|||Geological Province: Gambier Embayment, Otway Basin.||||||
1415|Belfast Mudstone|24314|5|Briefly described|p61 Fig.2|Santonian|Turonian|Geological Province: Otway Basin. Max. Thickness 362m. Of the Sherbrook Group.||||||30-NOV-04
1415|Belfast Mudstone|24405|5|Briefly described|p6|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin.||||||
1415|Belfast Mudstone|24453|5|Briefly described|p809 Fig.2|Campanian|Coniacin|Of Sherbrook Group. Overlain by Paaratte Formation and Nullawarre Greensand, overlies Flaxman Formation. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|24551|6|Mentioned|p245|||Of the Sherbrook Group||||||
1415|Belfast Mudstone|24562|5|Briefly described|p1, 8 Fig. 2|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.  Maximum Thickness: >1810m.||||||
1415|Belfast Mudstone|29697|6|Mentioned|Fig.11|||||||||
1415|Belfast Mudstone|29856|5|Briefly described|p38|||||||||
1415|Belfast Mudstone|30454|6|Mentioned|p26|||See also Fig.1||||||
1415|Belfast Mudstone|30499|6|Mentioned|p12|||Stratigraphy||||||
1415|Belfast Mudstone|30578|6|Mentioned|p7|||||||||
1415|Belfast Mudstone|30754|6|Mentioned|Table 12|||Stratigraphic table||||||
1415|Belfast Mudstone|31372|6|Mentioned|p17|||||||||
1415|Belfast Mudstone|31424|6|Mentioned|Plate 1|||On composite bore log||||||
1415|Belfast Mudstone|31624|6|Mentioned|p101|||See also Table 15-1||||||
1415|Belfast Mudstone|31714|6|Mentioned|p33|||||||||
1415|Belfast Mudstone|31920|4|Described|p51|||U.Cret. Of the Sherwood Group. See Table 3-2,3.||||||27-MAR-07
1415|Belfast Mudstone|31922|6|Mentioned|p187|||||||||
1415|Belfast Mudstone|32162|6|Mentioned|p58|||||||||
1415|Belfast Mudstone|32344|6|Mentioned|Fig.2|||||||||
1415|Belfast Mudstone|32894|5|Briefly described|p286|||U. Cret.||||||
1415|Belfast Mudstone|32896|6|Mentioned|Encl. 7.1|||U.Cret.||||||
1415|Belfast Mudstone|32897|6|Mentioned|p183|||||||||
1415|Belfast Mudstone|32898|6|Mentioned|Table 2-1|||||||||
1415|Belfast Mudstone|33155|6|Mentioned|p115|||||||||
1415|Belfast Mudstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
1415|Belfast Mudstone|33936|6|Mentioned|Fig.6|||||||||
1415|Belfast Mudstone|33940|6|Mentioned|Fig.21-1|||Turonian - Santonian.||||||
1415|Belfast Mudstone|33943|6|Mentioned|p380|||||||||
1415|Belfast Mudstone|34063|6|Mentioned|p3|||Table. U.Cret.||||||
1415|Belfast Mudstone|34308|6|Mentioned|Fig.85|||U.Cret.||||||
1415|Belfast Mudstone|34611|5|Briefly described|p164|||Fig.80.||||||
1415|Belfast Mudstone|34759|6|Mentioned|p59|||||||||
1415|Belfast Mudstone|34987|6|Mentioned|p174|||||||||
1415|Belfast Mudstone|36913|6|Mentioned|p78|||||||||
1415|Belfast Mudstone|38625|6|Mentioned|Table 2|||||||||
1415|Belfast Mudstone|39923|6|Mentioned|p357|||||||||
1415|Belfast Mudstone|40003|5|Briefly described|p43|||See also Fig.10||||||
1415|Belfast Mudstone|40560|5|Briefly described|Fig.3|||||||||
1415|Belfast Mudstone|40947|6|Mentioned|p3|||||||||
1415|Belfast Mudstone|41016|5|Briefly described|p214|||||||||
1415|Belfast Mudstone|41185|6|Mentioned|p177|||See also Fig. 5||||||
1415|Belfast Mudstone|41269|5|Briefly described|p245|||||||||
1415|Belfast Mudstone|41642|6|Mentioned|p244|||||||||
1415|Belfast Mudstone|41704|6|Mentioned|p100|||||||||
1415|Belfast Mudstone|41714|5|Briefly described|p301|||See also Fig.2||||||
1415|Belfast Mudstone|41726|5|Briefly described|p421|||||||||
1415|Belfast Mudstone|41868|4|Described|p533|||||||||
1415|Belfast Mudstone|41936|6|Mentioned|p75|||||||||
1415|Belfast Mudstone|42152|5|Briefly described|p15|||See also Fig.11||||||
1415|Belfast Mudstone|42361|3|Fully described|p15|Santonian|Cenomanian|Formation status preferred herein to Member status used by many in Victoria.||||||
1415|Belfast Mudstone|42524|5|Briefly described|Fig.3 P27|||||||||
1415|Belfast Mudstone|42545|6|Mentioned|p9|||Otway Basin||||||
1415|Belfast Mudstone|42555|5|Briefly described|p285|||||||||
1415|Belfast Mudstone|42599|5|Briefly described|Fig.3 P614|||||||||
1415|Belfast Mudstone|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
1415|Belfast Mudstone|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 85-90 Ma||||||
1415|Belfast Mudstone|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
1415|Belfast Mudstone|43208|5|Briefly described|map legend|Santonian|Turonian|Of Sherbrook Group.||||||
1415|Belfast Mudstone|43219|5|Briefly described|Fig.3,p6.|Santonian|Turonian|of Sherbrook Group||||||
1415|Belfast Mudstone|43590|4|Described|p13|Campanian|Turonian|||||||
1415|Belfast Mudstone|43660|5|Briefly described|p14,Fig.6,p15||Late Cretaceous|||||||
1415|Belfast Mudstone|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
1415|Belfast Mudstone|43744|6|Mentioned|Fig.3,p3|||||||||
1415|Belfast Mudstone|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
1415|Belfast Mudstone|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
1415|Belfast Mudstone|43814|6|Mentioned|Fig.3,p115|||||||||
1415|Belfast Mudstone|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
1415|Belfast Mudstone|44133|5|Briefly described|p146|Campanian|Turonian|Basal unit of Paarette Formation. Of the Sherbrook Group. Thickness: 1355m+.||||||
1415|Belfast Mudstone|48581|2|Defined|p33|||See also p1,27-29,31,25,39,40,Fig.4,6,Pl.1,2. (J54-12/Port Campbell).||||||
1415|Belfast Mudstone|48624|14|Not recorded|p5,7,Fig.2|||(J65-6/Benara).||||||
1415|Belfast Mudstone|48625|14|Not recorded|p7|||(J54-6/Benara).||||||
1415|Belfast Mudstone|48911|3|Fully described|p18|||Upper Cretaceous||||||
1415|Belfast Mudstone|48977|6|Mentioned|Fig.5|||||||||
1415|Belfast Mudstone|49060|5|Briefly described|Fig.33|||||||||
1415|Belfast Mudstone|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
1415|Belfast Mudstone|61017|5|Briefly described|p5 Fig. 2, p6|Santonian|Coniacian|Of the Sherbrook Group. Provides the regional seal for oil. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
1415|Belfast Mudstone|61182|3|Fully described|p16, p83-84|Campanian|Turonian|Of Sherbrook Gp. Conformable over Flaxman Fm, and Waarre Fm in some areas; overlain by Nullawarre Greensand. Geol.Prov: Otway Basin. Formerly regarded as part of Paarratte Fm. Marine to marginal marine, largely light grey to black mudstone; fossils occur.||||||
1415|Belfast Mudstone|61470|5|Briefly described|p28 Fig. 5|Campanian|Coniacian|Of the Sherbrook Group. Overlies Flaxman Formation; underlies the Skull Creek Mudstone and Nullawarre Greensand, with which it also interfingers. Geological Province: Otway Basin.||||||12-OCT-05
1415|Belfast Mudstone|61547|6|Mentioned|p461 Fig.2, p462. |Campanian|Turonian|||Unit in Sherbrook Group.||Overlies Flaxman Formation and Waarre Sandstone. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
1415|Belfast Mudstone|61625|5|Briefly described|p475, p476 Fig. 1, p476, p477, p480|Late Creatceous|Late Cretaceous|Was first nominated as a member of the Paaratte Formation by Bock and Glenie (1965); however Reynolds (1971) reinststed formation status. Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
1415|Belfast Mudstone|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61628|5|Briefly described|p509 Fig. 3, p510|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
1415|Belfast Mudstone|63122|5|Briefly described|p17 Fig. 4.3|Campanian|Turonian|Of the Sherbrook Group. Max. thickness: 1362m. Geological Province: Otway Basin. ||||||
1415|Belfast Mudstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p81|Santonian|Turonian|Previously Belfast Mudstone Member of Paaratte Fm.(Sprigg 1986); upgraded by Williamson et al (1987). Overlies Waarre Fm; conformably underlies Paaratte Fm; intertongues with Nullawarre Greensand. Age: 91-83Ma. Max.thickness: 1362m. Geol.Prov: Otway Basin||||||
1415|Belfast Mudstone|63125|5|Briefly described|p113|||Geological Province: Otway Basin. Composed of terrigenous DOM (dispersed organic matter) rich in inertinite and lean in vitrinite. ||||||
1415|Belfast Mudstone|63129|6|Mentioned|p134|||Geological Province: Otway Basin.||||||30-JAN-08
1415|Belfast Mudstone|63130|5|Briefly described|p143|||Geological Province: Otway Basin. Acts as a seal in relation to Waarre Sandstone.||||||06-FEB-08
1415|Belfast Mudstone|63269|5|Briefly described|p605-607, p616|Late Cretaceous|Late Cretaceous|Otway Basin. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Sherbrook Group.||||
1415|Belfast Mudstone|63431|5|Briefly described|p677 Fig. 2|Coniacian|Turonian|Of the Sherbrook Group. Overlies Flaxman Formation and Waarre Sandstone. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|66245|5|Briefly described|p5, p6 Fig.5, pp68-69 Fig.D5.|Maastrichtian|Coniacian|The authors decribe this unit as a 'grab-bag' for anything that cannot be distinguished, and call for more work to be done on this unit and the Sherbrook Group.||Unit in Sherbrook Group.||Is intercalated with Nullawarre Greensand. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
1415|Belfast Mudstone|67367|5|Briefly described|p131 Fig.2, p133, pp152-153.|Late Cretaceous|Late Cretaceous|Poor potential as hydrocarbon source rock. Rapid and significant deposition caused hydrocarbon generation and expulsion from Waarre Formation source rocks, and increased the maturity of the Eumeralla Formation.|c.85 Ma.|Unit in Sherbrook Group.||||
1415|Belfast Mudstone|69297|5|Briefly described|p78, p79, p84, p98, p115|Campanian|Coniacian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Potential seal for the Waarre and Flaxman Formation reservoirs. ||Sherbrook Group |Includes the Thylacine Sandstone Member and the Mourum Member.|Overlies the Flaxman Formation. Overlain by the Paaratte Formation and the Nullawarre Greensand.|Mudstone and siltstone.|
1415|Belfast Mudstone|69651|5|Briefly described|p10, p15, p32-34, p38|Late Cretaceous|Late Cretaceous|Most widely distributed seal in the Otway Basin; seals Waarre and Flaxman Formation reservoirs. Modelling diagrams.||Sherbrook Group.|Thylacine Member.|Overlies Flaxman Formation unconformably and Nullawarre Greensand. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4; p5|Late Cretaceous|Late Cretaceous|See also Regional: p7-8, p10. Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Interpreted geochemically to be a moderately good source in Breaksea Reef 1. Contains an important petroleum reservoir in its [informal] "Thylacine Sandstone Member". Provides a regional seal for reservoirs within Flaxman and Waarre Formations. Appears also as Belfast Formation on p10.||Sherbrook Group.||Overlies Banoon Member (Flaxman Formation). Is overlain by Nullawarre Greensand. Is equivalent to Mount Salt Formation.||
1415|Belfast Mudstone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4; p4-5|Santonian|Coniacian|Otway Basin. Equivalent rocks in the Sorell Basin are potential intraformational seals.||Sherbrook Group.||Overlies Flaxman Formation. Is overlain by Mount Salt Formation.||
1415|Belfast Mudstone|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Santonian|Coniacian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
1415|Belfast Mudstone|70880|6|Mentioned|p77|Campanian|Coniacian|Otway Basin.||||||
1415|Belfast Mudstone|70942|14|Not recorded|p118|||Stratigraphy.||||||
1415|Belfast Mudstone|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
1415|Belfast Mudstone|71437|6|Mentioned|p157|||[Abbreviation of Belfast Mudstone Member]||Of Paaratte Formation.||||
1415|Belfast Mudstone|73357|5|Briefly described|p20-21, p31, p45|Santonian|Coniacian|Otway Basin. Correlated with multiple biozones including Phyllocladidites mawsonii Spore-Pollen Zone and Conosphaeridium striatoconum Dinocyst Zone in lower part, and Isabelidinium cretaceum Dinocyst Zone in upper part. Belfast Mudstone equivalent p47.||Of Sherbrook Group.||Overlies Flaxman Formation, underlies Nullawarre Greensand, Skull Creek Mudstone.|Includes shales.|
1415|Belfast Mudstone|73383|5|Briefly described|p3, p11 Tb.3.9, p21-22, p27, p200, p248|Santonian|Turonian|Otway Basin. Interpreted as equivalent to chemostratigraphic package S5-P4 which was only identified in the Penryn-1 well, or to the S5-P5 package. Lithologies based on geochemistry using the ChemLith classification includes sandstone, argillaceous and calcareous sandstone, mudstone, limestone and calcareous limestone; and using the Herron classification (1988) includes Fe-sand, shale, Fe-shale, wacke. See also vi, p68, p119, p134, p261-262.||Sherbrook Group||Overlies Flaxman Formation, underlies Nullawarre Greensand|Shelfal siltstones and marine shales.|
1415|Belfast Mudstone|73385|5|Briefly described|p5|Santonian|Turonian|Otway Basin.||Sherbrook Group||Overlies Flaxman Formation, underlies Nullawarre Greensand.|Shelfal siltstones and marine shales.|
1415|Belfast Mudstone|73386|4|Described|p4, p6, p10-11, Attachment A1|Santonian|Coniacian|Otway Basin. Thickens offshore. Middle to outer shelf, open marine prodelta depositional environment. Partly a facies variant of the underlying Flaxman Formation and overlying Paaratte Formation. Designated type section is from 1501 m to 1685 m in Port Campbell-1. Diachronous unit, extends from Phyllocladidites mawsonii to Tricolporites apoxyexinus spore-pollen zones.||Sherbrook Group||Conformably overlies Flaxman Formation, underlies Nullawarre Greensand|Dark grey to black, pyritic, silty mudstone that becomes sandier to the northwest of the Otway Basin. Occasional thin, upward coarsening sandstone interbeds.|
1415|Belfast Mudstone|73594|5|Briefly described|p4-5, p13, p24-25, p27, p30-32, p67|Santonian|Turonian|Otway Basin. Forms a regionally extensive top seal to the the Upper Waarre play, the Thylacine Member and Flaxman Formation. [Misspelt Belfast Formation p27?]||Sherbrook Group|Thylacine Member|Overlies Flaxman Formation, underlies Nullawarre Greensand. Unconformably underlies Skull Creek Mudstone locally.|Prodelta silty mudstones.|
1546|Bethel Shale Member|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Saddleworth Formation.||||||
1546|Bethel Shale Member|23818|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|Of the Saddleworth Formation. Overlying unit: Belair Sub-Group (sharp contact).||||||
1546|Bethel Shale Member|30801|6|Mentioned|p5|||See also P6. Table only.||||||
1546|Bethel Shale Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
1546|Bethel Shale Member|34535|6|Mentioned|p60|||||||||
1546|Bethel Shale Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
1546|Bethel Shale Member|36623|6|Mentioned|Fig.1|||||||||
1546|Bethel Shale Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
1546|Bethel Shale Member|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
1546|Bethel Shale Member|41404|5|Briefly described|p110|||||||||
1546|Bethel Shale Member|43052|5|Briefly described|p181,Table 6.1|||of Saddleworth Formation||||||
1568|Bibliando Tillite Member|41404|6|Mentioned|p118|||||||||
1568|Bibliando Tillite Member|41405|3|Fully described|p161|||||||||
1626|Billa Kalina Clay Member|31532|5|Briefly described|Table 1|||Also p316. Type section discussed. Correlated with Etadunna Formation.||||||
1626|Billa Kalina Clay Member|36213|6|Mentioned|p85|||||||||
1626|Billa Kalina Clay Member|36966|4|Described|p85|||||||||
1626|Billa Kalina Clay Member|38604|6|Mentioned|Map legend|Miocene|Miocene|||||||
1626|Billa Kalina Clay Member|38605|6|Mentioned|p30|||||||||
1626|Billa Kalina Clay Member|42375|6|Mentioned|p79, p86|||Billa Kalina Basin. Member of Mirikata Formation.||||||
1626|Billa Kalina Clay Member|42465|5|Briefly described|Map Legend|||||||||
1626|Billa Kalina Clay Member|42469|5|Briefly described|p40|||||||||
1626|Billa Kalina Clay Member|42723|5|Briefly described|map legend|Miocene||||||||
1626|Billa Kalina Clay Member|43048|4|Described|Table 3.|||||||||
1626|Billa Kalina Clay Member|44133|4|Described|p190 Fig. 10.30|Miocene|Miocene|Geological Province: Billa Kalina Basin. Of the Mirikata Formation. Gradationally overlies Danae Conglomerate Member. Thickness: 6m. Gradationally underlies: Millers Creek Dolomite Member.||||||
1626|Billa Kalina Clay Member|64696|5|Briefly described|p133 Figs.13,14 |Miocene|Miocene|||Of the Mirikata Formation.||||
1626|Billa Kalina Clay Member|66520|5|Briefly described|p11-12. |Tertiary|Tertiary|10 m thick.||Unit in Mirikata Formation.|||Green clay, minor quartz grains.|
1626|Billa Kalina Clay Member|67462|5|Briefly described|Map legend.|Miocene|Miocene|Billa Kalina Basin.||Unit in Mirikata Formation.||||
1626|Billa Kalina Clay Member|68715|6|Mentioned|p30 Fig.5|Serravallian|Langhian|Billa Kalina Basin.||||||
1645|Billy Creek Formation|22631|6|Mentioned|p178|Cambrian|Cambrian|||||||
1645|Billy Creek Formation|22688|5|Briefly described|127|||||||||
1645|Billy Creek Formation|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|Age of unit: 522.8+/-1.8 Ma.||||||25-JUL-06
1645|Billy Creek Formation|22772|5|Briefly described|Table13.1|Early Cambrian|Early Cambrian|||||||12-JUN-20
1645|Billy Creek Formation|22857|5|Briefly described|Tb. 13.1 (insert p70), p90 Fig. 14.7B|Early Cambrian|Early Cambrian|Of the Lake Frome Group. Age: >509Ma. Geological Province: Arrowie Basin. Should not be confused with Billy Brook Formation (Dalwood Group). See also p92.||||||
1645|Billy Creek Formation|22858|6|Mentioned|p92,Fig14.7bp90-1|||||||||
1645|Billy Creek Formation|23282|6|Mentioned|p72|||May correlate with Observatory Hill Formation. of Arrowie Basin.||||||
1645|Billy Creek Formation|23818|5|Briefly described|p51 Fig.16, p94|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||
1645|Billy Creek Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Comprises 2 units: lower unit (Erudina Member) contains red and green sandstones and siltstones with predom. green, calcareous, micaceous mudstones. Overlies Narina Greywacke; underlies Wirrealpa Limestone and Aroona Limestone. Age of Tuff: 522.8+/-1Ma.||||||12-JUL-06
1645|Billy Creek Formation|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
1645|Billy Creek Formation|24138|5|Briefly described|p31|Cambrian|Cambrian|Fosiliferous dolomitic limestone suceeded by micaceous shale with minor sandstone and dolomite beds. Deltaic with marine incursions. Geological Province: Adelaide Geosyncline.||||||
1645|Billy Creek Formation|24176|4|Described|p17, p23 Tb. 1|Cambrian|Cambrian|Chocolate shale, siltstone.  Max. thickness: 360m.  Geological Province: Mount Painter Province.||||||
1645|Billy Creek Formation|24281|5|Briefly described|p7|||Geological Province: Arrowie Basin.||||||
1645|Billy Creek Formation|24334|5|Briefly described|p48 Tb.1|Early Cambrian|Early Cambrian|Age: 512 - 525 Ma.||||||25-JUL-06
1645|Billy Creek Formation|24465|5|Briefly described|p343, p345 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
1645|Billy Creek Formation|24481|5|Briefly described|p829 Fig. 9|||Overlies the Ajax Limestone.||||||
1645|Billy Creek Formation|24484|5|Briefly described|p798 Fig. 1, p803|Cambrian|Cambrian|Unconformably overlies the Upper Wilkawillina Limestone. Overlain by the Aroona Creek Limestone.||||||
1645|Billy Creek Formation|29929|6|Mentioned|Fig.1|||||||||
1645|Billy Creek Formation|30051|6|Mentioned|Fig.4|||See also Fig.12. Middle Cambrian age.||||||
1645|Billy Creek Formation|30176|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1645|Billy Creek Formation|30801|6|Mentioned|p5|||Lower Cambrian. See also P6. Table only.||||||
1645|Billy Creek Formation|30802|5|Briefly described|p11|||Cambrian.||||||
1645|Billy Creek Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
1645|Billy Creek Formation|30874|6|Mentioned|p5|||||||||
1645|Billy Creek Formation|31539|6|Mentioned|Fig. 28|||See also P98 Fig. 2||||||
1645|Billy Creek Formation|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
1645|Billy Creek Formation|32669|6|Mentioned|p523|||L. Cambrian||||||
1645|Billy Creek Formation|33474|6|Mentioned|Fig.3|||||||||
1645|Billy Creek Formation|33932|6|Mentioned|p18|||||||||
1645|Billy Creek Formation|33934|6|Mentioned|Fig.2|||Camb.||||||
1645|Billy Creek Formation|33972|6|Mentioned|Fig.2|||||||||
1645|Billy Creek Formation|33973|6|Mentioned|p18|||||||||
1645|Billy Creek Formation|34185|4|Described|p129|||||||||
1645|Billy Creek Formation|34268|6|Mentioned|p241|||Cambrian||||||
1645|Billy Creek Formation|34269|6|Mentioned|Table 1|||||||||
1645|Billy Creek Formation|34535|6|Mentioned|Fig.16|||||||||
1645|Billy Creek Formation|34612|6|Mentioned|p105|||Trilobites. See also correlation chart. Fig.33||||||
1645|Billy Creek Formation|34766|6|Mentioned|p58|||||||||
1645|Billy Creek Formation|34812|6|Mentioned|Table 9|||||||||
1645|Billy Creek Formation|35255|6|Mentioned|Fig.8|||||||||
1645|Billy Creek Formation|35373|6|Mentioned|Fig.2|||||||||
1645|Billy Creek Formation|35395|5|Briefly described|p102|||Stratigraphy||||||
1645|Billy Creek Formation|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
1645|Billy Creek Formation|35577|6|Mentioned|Fig.2|||||||||
1645|Billy Creek Formation|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
1645|Billy Creek Formation|35835|4|Described|p197|||Discussion of stratigraphy and nomenclature.||||||
1645|Billy Creek Formation|35954|4|Described|p1229|||See also Fig.2.||||||
1645|Billy Creek Formation|36081|6|Mentioned|Fig.1|||||||||
1645|Billy Creek Formation|36083|5|Briefly described|p473|||||||||
1645|Billy Creek Formation|36137|6|Mentioned|p11|||||||||
1645|Billy Creek Formation|36198|6|Mentioned|p249|||See also Fig.I.2||||||
1645|Billy Creek Formation|36495|1|Redefined|p118|Middle Cambrian|Early Cambrian|Early to Middle Cambrian.||||||
1645|Billy Creek Formation|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
1645|Billy Creek Formation|37113|6|Mentioned|Fig.1|||||||||
1645|Billy Creek Formation|37461|6|Mentioned|p345|||||||||
1645|Billy Creek Formation|37802|6|Mentioned|p71|||||||||
1645|Billy Creek Formation|38004|6|Mentioned|Table 1|||||||||
1645|Billy Creek Formation|38068|4|Described|p69|||See also Fig.4.||||||
1645|Billy Creek Formation|38108|6|Mentioned|Table 1|||||||||
1645|Billy Creek Formation|38701|6|Mentioned|p123|||||||||
1645|Billy Creek Formation|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1645|Billy Creek Formation|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||21-SEP-17
1645|Billy Creek Formation|40254|6|Mentioned|Fig.7|||||||||
1645|Billy Creek Formation|40455|6|Mentioned|Fig.2|||||||||
1645|Billy Creek Formation|40852|6|Mentioned|p33|||||||||
1645|Billy Creek Formation|40856|6|Mentioned|Fig.23.6|||||||||
1645|Billy Creek Formation|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1645|Billy Creek Formation|41401|6|Mentioned|p32|||||||||
1645|Billy Creek Formation|41457|6|Mentioned|Fig.1|||||||||
1645|Billy Creek Formation|41496|5|Briefly described|p52|||||||||
1645|Billy Creek Formation|41526|6|Mentioned|p61|||||||||
1645|Billy Creek Formation|42011|6|Mentioned|p459|||||||||
1645|Billy Creek Formation|42090|6|Mentioned|p26|||||||||
1645|Billy Creek Formation|42141|6|Mentioned|Table 2 P571|||||||||
1645|Billy Creek Formation|42192|6|Mentioned|p10|||||||||
1645|Billy Creek Formation|42213|6|Mentioned|p474|||||||||
1645|Billy Creek Formation|42225|6|Mentioned|p223|||||||||
1645|Billy Creek Formation|42266|6|Mentioned|Fig.2 P292|||||||||
1645|Billy Creek Formation|42269|4|Described|p335|||||||||
1645|Billy Creek Formation|42357|5|Briefly described|p10|||||||||
1645|Billy Creek Formation|42440|6|Mentioned|Fig.2 P602|||||||||
1645|Billy Creek Formation|42573|5|Briefly described|Fig.1 P190|||||||||
1645|Billy Creek Formation|42779|5|Briefly described|Table 1 P287|||||||||
1645|Billy Creek Formation|43011|6|Mentioned|Table 2,p12|||||||||
1645|Billy Creek Formation|43052|5|Briefly described|Table 2.1|||||||||
1645|Billy Creek Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||01-JUN-05
1645|Billy Creek Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
1645|Billy Creek Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
1645|Billy Creek Formation|43759|6|Mentioned|p452|||||||||
1645|Billy Creek Formation|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
1645|Billy Creek Formation|44093|5|Briefly described|p138 App. 1|Middle Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||12-JUN-20
1645|Billy Creek Formation|44133|5|Briefly described|p4 Fig. 7.2, 17|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
1645|Billy Creek Formation|44882|14|Not recorded|p149||Cambrian|In French||||||
1645|Billy Creek Formation|45102|6|Mentioned|p46|||See also P48||||||
1645|Billy Creek Formation|45155|6|Mentioned|Fig.8|||||||||
1645|Billy Creek Formation|50244|6|Mentioned|p101|||||||||
1645|Billy Creek Formation|60418|6|Mentioned|p134 Fig.1|||||||||
1645|Billy Creek Formation|60889|4|Described|p245 Fig.2, p249, p252-4|Early Cambrian|Early Cambrian|Thickness: >2000 m. Common shale partings, hummocky cross-stratification, scarce mudcracks and trilobite tracks associated with sand beds suggests they are attached shoreface deposits. Correlation with Kanmantoo Group (Stansbury Basin) and alternative views are presented in text (p249). Arrowie Basin.|Tuff bed 522.8 +/- 1.8 Ma.||Basal Coads Hill Member, Edeowie Limestone Member.|Coads Hill Member and Edeowie Limestone Member of Billy Creek Formation overlie Moorowie Formation. Is overlain by Wirrealpa Limestone.|Clastic red bed deposition: red, largely deltaic, sandstones and siltstones. The base changes from dominantly carbonate to dominantly clastic sedimentation. Majority consists of impermeable red-brown siltstone; anhydrite and shales.|21-SEP-17
1645|Billy Creek Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||
1645|Billy Creek Formation|60955|5|Briefly described|Map Legend|||Equivalent of Yarrawurta Shale.||||||
1645|Billy Creek Formation|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Lake Frome Group. Red siltstone and sandstone.||||||23-DEC-09
1645|Billy Creek Formation|60990|5|Briefly described|p81, p83 Fig.2|Botoman|Botoman|Flinders Ranges. SHRIMP SL13 U-Pb tuff age. Tuff age using the QGNG standard is 529.6 +/- 1.8 Ma (Jago and Haines 1998) which accords better with biostratigraphy.|522.8 ¿ 1.8 Ma (Gravestock and Shergold 2001)|||||
1645|Billy Creek Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Arrowie Basin.||||||03-JUN-05
1645|Billy Creek Formation|62270|5|Briefly described|p496, p502|Early Cambrian|Early Cambrian|Includes Coads Hill and Warragee Members. Contains Emuellids (Trilobite family). In Flinders Ranges.||||||18-MAY-06
1645|Billy Creek Formation|62592|5|Briefly described|p50 Table 5.1, p59.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Moralana Supergroup.||Overlies Hawker Group. Is overlain by Wirrealpa Limestone.|Redbeds.|
1645|Billy Creek Formation|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Includes Edeowie Limestone Member and Eregunda Sandstone Member.||||Overlies Oraparinna Shale unit of Hawker Group. Is overlain by Wirrealpa Limestone.||20-MAR-12
1645|Billy Creek Formation|63447|6|Mentioned|p962,p963 Fig.2 |Early Cambrian|Early Cambrian|||||Overlies Ajax Limestone, Oraparinna Shale, Narina Greywacke all of Hawker Group.||
1645|Billy Creek Formation|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Redbeds with tuffs.||||||10-SEP-07
1645|Billy Creek Formation|63569|4|Described|pp116-120, p122|Early Cambrian|Early Cambrian|Type locality at Angorichina Station. Thickness 900 m. |Includes a tuff unit dated at 522.8 +/- 8 Ma.||Includes Edeowie Limestone Member, Eregunda Sandstone Member, Warragee Member.|Is overlain by Wirrealpa Limestone.|Red beds; tuff.|
1645|Billy Creek Formation|64319|6|Mentioned|p357 Fig.3 |||||||||
1645|Billy Creek Formation|64829|5|Briefly described|p1083, p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. Age: 522.8+/-1.8Ma (Pb/U on tuff). Geological province: Arrowie Basin. Has associated palaeosols.||||||07-FEB-11
1645|Billy Creek Formation|65313|5|Briefly described|p576, Fig. 5, p577, p578 Fig. 6|Middle Cambrian|Early Cambrian|Includes tuff near base dated 522.8 +/- 1.8 Ma by U/Pb SHRIMP. Ten Mile Creek section, eastern Arrowie Basin. Age supported by pedostratigraphy.||||||
1645|Billy Creek Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||||Overlies Narina Greywacke. Is overlain by Wirrealpa Limestone.||
1645|Billy Creek Formation|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Lake Frome area.||||Overlies Oraparinna Shale. Underlies Wirrealpa Limestone.||18-FEB-11
1645|Billy Creek Formation|65686|5|Briefly described|p411, 413 p409 Fig 2|Early Cambrian|Early Cambrian|Age is of included tuff bed. Arrowie Basin. 900m thick.|522 +/- 1.8 Ma.|||||07-MAY-12
1645|Billy Creek Formation|65892|4|Described|p7 Fig.3, p9 Fig.4, p10, p12, p27-28.|Early Cambrian|Early Cambrian|See also p39 Fig.21, p41-42. Arrowie Basin. 900m thick. Contains emuellid trilobite Balcoracania dailyi.|c.525 Ma.||Includes Coads Hill, Edeowie Limestone, Warragee, and Eregunda Sandstone, Members.|Is overlain by Wirrealpa Limestone.|Red, largely deltaic, sandstones and siltstones.|
1645|Billy Creek Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||522.8 +/- 1.8 Ma.||||Siltstone, shale, dolomite, with tuff beds.|
1645|Billy Creek Formation|66518|5|Briefly described|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||||Unconformably overlies Moorowie Formation. Is overlain by Wirrealpa Limestone.||06-FEB-14
1645|Billy Creek Formation|67030|6|Mentioned|p412 Fig. 7, p413 Tab. 2|Ediacaran|Ediacaran|Magnetic information presented for comparison (Klootwijk 1980). Abbreviated as Billy Ck Fm.||||||26-APR-12
1645|Billy Creek Formation|67536|5|Briefly described|Map Legend|Stage 2|Stage 2||ca. 523 +/- 2 Ma||||Shallow marine to terrestrial redbeds, peritidal to marine limestone|
1645|Billy Creek Formation|67870|5|Briefly described|p5, p9, p17, p21, p23|Cambrian|Cambrian|Arrowie Basin. c.200m thick.||||Overlies Wilkawillina Limestone.||
1645|Billy Creek Formation|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges.||||Overlain unconformably by Wirrealpa Formation. Underlain unconformably by Mernmerna Formation, and infills incised valleys into Wilkawillina Limestone.||
1645|Billy Creek Formation|68735|4|Described|pp231-239|Early Cambrian|Early Cambrian|Arrowie Basin. The base of this Formation is correlated with the bases of both the Minlaton Formation and the Kanmantoo Group. ~ 900 m thick.|||Includes the Nildottie Siltstone Member and Erudina Siltstone Member.|Overlies Hawker Group. Is overlain by Wirrealpa Limestone.|Dominantly a red bed succession of deltaic sandstones and siltstones.|10-APR-17
1645|Billy Creek Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
1645|Billy Creek Formation|69982|6|Mentioned|p15, p40|Early Cambrian|Early Cambrian|Arrowie Basin. Same age as Mooracoochie Volcanics. Mentioned in the context of dating the Innanmincka Formation by trilobite tracks similar to those in this unit.||||||
1645|Billy Creek Formation|70031|6|Mentioned|p250|||487+\-5 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||||||
1645|Billy Creek Formation|70833|6|Mentioned|p183,190,200-201|Series 2|Series 2|Of Arrowie Basin. Key section: BALC (Balcoracana Gorge, Bunkers Range).||||Overlain by Wirrealpa Limestone. Underlain by Hawker Group.||
1645|Billy Creek Formation|70835|6|Mentioned|p335-336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.|||Edeowie Limestone Member, Eregunda Sandstone Member.|Overlies Edeowie Limestone Member; and Ajax Limestone unconformably.||
1645|Billy Creek Formation|71102|5|Briefly described|p251,267|Series 2|Series 2|Of Arrowie Basin.|||Includes Edeowie Limestone.|Underlain by Oraparinna Shale, or disconformably by Wilkawillina Limestone..||
1645|Billy Creek Formation|72429|4|Described|p949, p951-952, p966, p968, p971-973|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Measured thickness exceeds 287 m. Outcrop is restricted to highly irregular patches along the foothills and in shallow drainage gullies cutting through the Cenozoic outwash fans passing to Lake Frome plains. Constituent lithologies are discussed in further detail, including mineral composition, textures and depositional environments. See also p961.||||Overlies the Moorowie Formation, Hawker Group.|Red bed succession. Red-brown to green micaceous shales with thin interbeds of silty sandstone and buff flaggy dolostone capped by purple shales. Arthropod tracks, flute and ripple marks, with rare casts after halite.|
1645|Billy Creek Formation|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Shallow water environment.||||Overlies Oraparinna Shale and underlies Wirrealpa Limestone.|Red-brown siltstone and sandstone with mudcracks. Salt casts and ripple marks; includes a thin volcanic ash layer close to top.|
1645|Billy Creek Formation|73177|5|Briefly described|p1114||||522.8 +/- 1.8 Ma.|Moralana Supergroup.||||
1645|Billy Creek Formation|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||||Unconformably underlain by Moorowie Formation (Hawker Group). Overlain by Wirrealpa Limestone.||
1645|Billy Creek Formation|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Balcoracania flindersi trilobite fossils.|522.8 +/- 1.8 Ma|||Overlies the Oraparinna Shale, underlies the Wirrealpa Limestone.|Includes ash layer.|
1653|Billy Springs Formation|23315|5|Briefly described|p345|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Cross-bedded feldspathic quartzite and sandstone.||||||07-FEB-07
1653|Billy Springs Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
1653|Billy Springs Formation|24586|5|Briefly described|p51, p52 Fig. 3|||Of the Wilpena Group (Heysen Supergroup). Intertongues with Bonney Sandstone and Wonoka Formation (northern Flinders Ranges).  See also p50 Fig. 1.||||||05-JUL-06
1653|Billy Springs Formation|41429|1|Redefined|p239|||Type section: Coats (in Coats and Blissett, 1971) proposed the area between Tardlapinna Well and Village Well as type section (from lat. 29degrees56'35"S, long. 139degrees20'41"E to lat. 29degrees52'20"S, long. 139degrees10'27"E), where the Billy Springs Formation is at least 4 800 m thick.||||||26-NOV-22
1653|Billy Springs Formation|42222|6|Mentioned|p20|||||||||
1653|Billy Springs Formation|42410|4|Described|p2|||||||||
1653|Billy Springs Formation|43052|5|Briefly described|p194,Table 6.1|||Of Wilpena Group.||||||30-SEP-08
1653|Billy Springs Formation|60889|6|Mentioned|p249 Fig.6.|Neoproterozoic|Neoproterozoic||~550 Ma.|||Interleaves with Rawnsley Quartzite.|Siltstone.|
1653|Billy Springs Formation|61732|5|Briefly described|p39|||||||||07-FEB-11
1653|Billy Springs Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Pound Subgroup.||||
1653|Billy Springs Formation|64319|5|Briefly described|p356 Fig.2 |Middle Cambrian|Middle Cambrian|Shown in Fig. 2 as overlying Ajax Limestone, BUT the authors have confused this unit [currently of the Wilpena Group] with Billy Creek Formation [which does overlie Ajax Ls].|||||Shale and siltstone.|
1653|Billy Springs Formation|68271|4|Described|p693-697|Ediacaran|Ediacaran|Adelaide Rift Complex; NE Flinders Ranges. Coats and Blisset 1971 assigned a thickness of at least 4800m thick at type section (Mount Freeling syncline in the area between Tardlapinna Well and Village Well from lat. 29 56'35''S, long. 139 20'41''E to lat. 29 52'20''S, long. 139 10'27''E), but was readjusted to c. 2900 m at type section by Pell (1989) and Reid (1992) to exclude section assigned as Rawnsley Quartzite. Probably formed within restricted depocentre passing into slope setting due to local late Ediacaran extension. Lithological descriptions provided based on previous workers at different type locations (see p693-694). Thought to represent glaciogenic sediments deposited during the Billy Springs glaciation based on lithological constraints; variety of stones of differing lithology occur in finely layered sediment (see p697-698). Correlable to Ediacaran stratotypic upper Wilpena Group.||||Underlain conformably by Wonoka Formation. Overlain by Chace Quartzite Member, Rawnsley Quartzite.|Grey-green fine sandstone, quartzite, marble and dolomite, overlain by grey-green slate, quartzite and minor lenticular marbles.|
1653|Billy Springs Formation|68274|6|Mentioned|p12 Fig.1.6, p13|||Rift complex.||||||
1653|Billy Springs Formation|68277|6|Mentioned|p103|Neoproterozoic|Neoproterozoic|May have been glaciated in the mid-Ediacaran interval; contains possible ice-rafting features.||||||
1653|Billy Springs Formation|68713|5|Briefly described|p19, p23|||Contains internationally renowned trace meso-scale fauna.||Of the upper Wilpena Group.||||13-JAN-17
1653|Billy Springs Formation|69019|3|Fully described|p30-31, p33, p59-60 Pl.10h, p61-63, p142|Neoproterozoic|Neoproterozoic|Originally Billy Springs Beds (Coats, in Coats et al., 1969 and Coats and Blissett, 1971); upgraded to Formation status by Preiss (1987); further revised to exclude the uppermost units and attribute them (Uratanna Formation and Western Spur Limestone) to the Hawker Group. Intruded by 2 undifferentiated mafic intrusives. Appears as Billy Springs Fm in p30, p33. Considered a distal, basinal facies equivalent to Pound Subgroup. Hosts the Ooloo (or Rieck's) Mine (Pb-Ag) and the Gilead P. Beck Mine (Pb-Cu-Zn), both uneconomic .||||Equivalent to Rawnsley Quartzite.|A very thick succession of green siltstone and sandstone with lenticular interbeds of diamictite, minor stromatolitic dolostone and ooid grainstone.|
1653|Billy Springs Formation|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline. The four facies are mapped separately. Intraformational disconformities.||Of Pound Subgroup.||Equivalent to Rawnsley Quartzite.|Monotonous finely-laminated siltstone; cross-bedded ooid grainstone, intraformational, conglomeratic and stromatolitic limestone and sandstone; basal ooid grainstone; greyish siltstone parasequences below pale yellow, medium-grained sandstone.|23-JAN-19
1653|Billy Springs Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14, p16-17, p22-23|Ediacaran|Ediacaran|Youngest Neoproterozoic formation of the Adelaide Rift Complex.|564+/-25 Ma LA-ICP-MS detrital zircon MDA|Pound Subgroup||||
1729|Birkhead Formation|12597|5|Briefly described|p492 Tb.1, p499, p501|Callovian|Callovian|Senior et al. (1978). Eromanga Basin. Commercially inferior coal deposits.||Unit in Injune Creek Group.|||Sub-labile to labile partly calcareous sandstone and siltstone with minor carbonaceous mudstone and coal.|
1729|Birkhead Formation|13497|5|Briefly described|p115, p130, p136, p138|Late Jurassic|Middle Jurassic|Eromanga Basin. Deposited in a high-sinuosity fluvial, overbank or lacustrine environment. This formation is an oil source rock. Interpreted to be a capillary seal above the Hutton oil reservoir. See also p138 fig 8.17, p141, p142, p146, p149-p151, p153 fig 9.28, p169, p184, p216.||||Overlies the Hutton Sandstone. Overlain by the Adori Sandstone.|Sandstones, siltstone, shale and minor coal.|
1729|Birkhead Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Jurassic|Middle Jurassic|In Eromanga Basin.||||||
1729|Birkhead Formation|22464|5|Briefly described|p9||Middle Jurassic|Eromanga Basin, overlies Hutton Sandstone, overlain by Adori Sandstone||||||
1729|Birkhead Formation|22839|6|Mentioned|P33|||||||||
1729|Birkhead Formation|22883|5|Briefly described|P31, Fig2|Late Jurassic|Middle Jurassic|Overlying unit is Namur Sandstone, underlying unit is Hutton Sandstone||||||
1729|Birkhead Formation|23036|6|Mentioned|7|||||||||
1729|Birkhead Formation|23054|6|Mentioned|Fig5p22|Kimmeridgian|Callovian|||||||
1729|Birkhead Formation|23056|4|Described|13|||Geol province Eromanga Basin. Injune Creek Group||||||
1729|Birkhead Formation|23154|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Geological Province - Eromanga Basin.||||||
1729|Birkhead Formation|23155|4|Described|p26 & Fig14 on p27|Late Jurassic|Middle Jurassic|The Birkhead Formation intertongues with the Hutton Sandstone.||||||
1729|Birkhead Formation|23340|6|Mentioned|12|||||||||
1729|Birkhead Formation|23356|5|Briefly described|26 Tab.2|Late Jurassic|Late Jurassic|||||||
1729|Birkhead Formation|23375|4|Described|Fig2 p265||Callovian|of Eromanga Basin.||||||
1729|Birkhead Formation|23425|5|Briefly described|Plate 10.2|||Of Injune Creek Group, Eromanga Basin.||||||
1729|Birkhead Formation|23430|4|Described|p523-524 Table 14.7|||Of Injune Creek Group. Eromanga Basin Province. Maximum thickness <130 m.||||||
1729|Birkhead Formation|23731|6|Mentioned|p71|||Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|23799|5|Briefly described|p48 Fig. 3|Callovian|Bathonian|Of Injune Creek Group.  Geological Province: Surat Basin.||||||
1729|Birkhead Formation|23818|5|Briefly described|p141 Fig.65, p142|Late Jurassic|Middle Jurassic|Geological Province: Great Artesian Basin. Max. thickness: 300 ft.||||||
1729|Birkhead Formation|23830|5|Briefly described|Fig. 3a|Jurassic|Jurassic|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||12-SEP-05
1729|Birkhead Formation|23883|5|Briefly described|p129 Fig. 11.2|Jurassic|Jurassic|Of the Injune Creek Group.  Geological Province: Great Australian Superbasin.||||||
1729|Birkhead Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Of Injune Creek Group. Geological Province: Great Artesian Basin.||||||
1729|Birkhead Formation|24092|5|Briefly described|p8 Fig.3|||Of Injune Creek Group. Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|24175|5|Briefly described|p17 Fig. 3|Kimmeridgian|Callovian|Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|24282|6|Mentioned|p11|||Cooper-Eromanga Basin.||||||
1729|Birkhead Formation|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
1729|Birkhead Formation|24482|5|Briefly described|p44|||Geological Province: Eromanga Basin.||||||
1729|Birkhead Formation|29393|6|Mentioned|Table 4|||Jurassic.||||||
1729|Birkhead Formation|29591|6|Mentioned|Table 15|||||||||
1729|Birkhead Formation|29721|6|Mentioned|p137|||||||||
1729|Birkhead Formation|29961|5|Briefly described|p14|||||||||
1729|Birkhead Formation|30024|6|Mentioned|p332|||||||||
1729|Birkhead Formation|30102|5|Briefly described|p21|||Jurassic - Cretaceous age. Unit of Injune Creek Group. See also P25||||||
1729|Birkhead Formation|30103|5|Briefly described|Tb.p9||Middle Jurassic|||||||
1729|Birkhead Formation|30104|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|30461|6|Mentioned|p100|||||||||
1729|Birkhead Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
1729|Birkhead Formation|30540|6|Mentioned|Fig.6|||||||||
1729|Birkhead Formation|30691|4|Described|p15|||See also p20,22.Table 4,6. Middle Jurassic. Part of Injune Creek Group.||||||17-JAN-08
1729|Birkhead Formation|30692|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|30694|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|30695|4|Described|Table 4|||Middle Jurassic age.||||||
1729|Birkhead Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic.||||||17-JAN-08
1729|Birkhead Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
1729|Birkhead Formation|30702|6|Mentioned|p52|||See also Fig.1,2 & Table 1. See strat.table.||||||
1729|Birkhead Formation|30804|6|Mentioned|Table 2|||||||||
1729|Birkhead Formation|30853|5|Briefly described|Table 3|||Middle Jurassic||||||
1729|Birkhead Formation|30854|4|Described|Table 4|||Middle Jurassic age.||||||
1729|Birkhead Formation|30855|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|Unit in Injune Creek Group||||||
1729|Birkhead Formation|30856|4|Described|Table 3|||See also p10. Middle Jurassic age.||||||17-JAN-08
1729|Birkhead Formation|30857|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|Part of Injune Creek Group||||||
1729|Birkhead Formation|30921|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early to Late Jurassic||||||
1729|Birkhead Formation|31116|6|Mentioned|p27|||||||||
1729|Birkhead Formation|31120|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|31145|5|Briefly described|Table 1|||Mid Jurassic||||||
1729|Birkhead Formation|31425|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|31431|5|Briefly described|Table 3|||M.-U.Jurassic||||||
1729|Birkhead Formation|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
1729|Birkhead Formation|32138|6|Mentioned|p396|||||||||
1729|Birkhead Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
1729|Birkhead Formation|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7||||||
1729|Birkhead Formation|32797|6|Mentioned|Table 4|||M.-U. Jur.||||||
1729|Birkhead Formation|33067|4|Described|Table 1|||Of the Injune Creek Group.||||||07-JUL-04
1729|Birkhead Formation|33069|4|Described|p7|||Part of Injune Creek Group.||||||22-DEC-09
1729|Birkhead Formation|33070|4|Described|Table 2|||Mid. Jur.||||||
1729|Birkhead Formation|33071|5|Briefly described|p6|||M.-U.Jur.||||||
1729|Birkhead Formation|33075|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|33078|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33079|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33080|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33082|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33086|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33087|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||22-DEC-09
1729|Birkhead Formation|33088|4|Described|Table 3|||Mid.Jur.||||||
1729|Birkhead Formation|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
1729|Birkhead Formation|33090|4|Described|Table 4|||Mid.Jur.||||||
1729|Birkhead Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
1729|Birkhead Formation|33094|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33176|5|Briefly described|p175|||Correlation||||||
1729|Birkhead Formation|33367|3|Fully described|p17|||Equiv. Walloon Coal Measures.||||||08-NOV-13
1729|Birkhead Formation|33371|4|Described|p58|||Equiv. Walloon Coal Measures.||||||17-JAN-08
1729|Birkhead Formation|33449|4|Described|Table 1|||Mid Jurassic.||||||21-APR-08
1729|Birkhead Formation|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
1729|Birkhead Formation|33638|5|Briefly described|Table 1|||||||||
1729|Birkhead Formation|33639|5|Briefly described|Table 2|||||||||
1729|Birkhead Formation|33640|4|Described|Table 3|||M.-U.Jur.||||||
1729|Birkhead Formation|33643|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
1729|Birkhead Formation|33672|5|Briefly described|p44|||Lithology||||||
1729|Birkhead Formation|33673|4|Described|p287|||See also p291.||||||17-JAN-08
1729|Birkhead Formation|33774|6|Mentioned|p54|||Refers Mollan et al. (1972). Now Walloon Coal Measures.||||||
1729|Birkhead Formation|33820|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
1729|Birkhead Formation|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
1729|Birkhead Formation|33822|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|33824|6|Mentioned|p7|||Table 2||||||
1729|Birkhead Formation|33825|5|Briefly described|Table 3,p10|||Strat. table. Lithology||||||
1729|Birkhead Formation|33827|6|Mentioned|p7|||See also Table 2||||||
1729|Birkhead Formation|33828|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|33832|5|Briefly described|p11|||Strat. & correlation||||||
1729|Birkhead Formation|33936|6|Mentioned|Fig.3A|||Jurassic.||||||
1729|Birkhead Formation|33977|6|Mentioned|p19|||Geological sections through Gidgealpa Field.||||||
1729|Birkhead Formation|33998|6|Mentioned|p31|||||||||
1729|Birkhead Formation|34065|4|Described|p7|||M.Jur.||||||
1729|Birkhead Formation|34091|4|Described|Table 1,p7|||Part of Injune Creek Group.||||||
1729|Birkhead Formation|34134|6|Mentioned|p482|||Middle Jurassic||||||
1729|Birkhead Formation|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
1729|Birkhead Formation|34218|5|Briefly described|Table 1|||Middle Jurassic. See also Table 2.||||||
1729|Birkhead Formation|34386|6|Mentioned|p97|||See also PP98,99,100 etc.||||||
1729|Birkhead Formation|34408|6|Mentioned|p185|||On Table||||||
1729|Birkhead Formation|34486|4|Described|Table 1|||See also Table 2. Middle Jurassic.||||||21-APR-08
1729|Birkhead Formation|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
1729|Birkhead Formation|34611|6|Mentioned|Fig.65|||Correlation chart||||||
1729|Birkhead Formation|34613|4|Described|Table 4|||||||||
1729|Birkhead Formation|35067|6|Mentioned|Fig.4|||||||||
1729|Birkhead Formation|35239|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|35560|6|Mentioned|p289|||||||||
1729|Birkhead Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
1729|Birkhead Formation|35663|6|Mentioned|p124|||||||||
1729|Birkhead Formation|35811|5|Briefly described|Table 3|||||||||
1729|Birkhead Formation|36243|6|Mentioned|Table 6A|||||||||
1729|Birkhead Formation|36910|6|Mentioned|p66|||||||||
1729|Birkhead Formation|36912|6|Mentioned|p72|||||||||
1729|Birkhead Formation|36924|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|37065|5|Briefly described|p38|||||||||
1729|Birkhead Formation|37116|4|Described|p312|||||||||
1729|Birkhead Formation|37117|6|Mentioned|p312|||||||||
1729|Birkhead Formation|37287|6|Mentioned|p36|||||||||
1729|Birkhead Formation|37608|3|Fully described|Table 1|||||||||
1729|Birkhead Formation|37703|6|Mentioned|p2240|||||||||
1729|Birkhead Formation|37995|6|Mentioned|p62|||||||||
1729|Birkhead Formation|38068|4|Described|p71|||||||||
1729|Birkhead Formation|38226|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|38730|6|Mentioned|p29|||||||||
1729|Birkhead Formation|38779|6|Mentioned|p7|||||||||
1729|Birkhead Formation|39070|4|Described|p363|||||||||
1729|Birkhead Formation|39276|6|Mentioned|Fig. 2|||||||||
1729|Birkhead Formation|39445|5|Briefly described|Table 10|||||||||
1729|Birkhead Formation|39478|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|39494|6|Mentioned|p129|||See also Fig.3||||||
1729|Birkhead Formation|39846|6|Mentioned|p45|||||||||
1729|Birkhead Formation|39847|5|Briefly described|p35|||||||||
1729|Birkhead Formation|39943|6|Mentioned|Table 8A|||||||||
1729|Birkhead Formation|39988|6|Mentioned|p288|||||||||
1729|Birkhead Formation|39989|4|Described|p422|||||||||
1729|Birkhead Formation|40003|5|Briefly described|p33|||||||||
1729|Birkhead Formation|40030|6|Mentioned|p126|||See also Fig.3||||||
1729|Birkhead Formation|40121|6|Mentioned|p446|||||||||
1729|Birkhead Formation|40249|6|Mentioned|p41|||||||||
1729|Birkhead Formation|40250|4|Described|p31|||||||||
1729|Birkhead Formation|40540|6|Mentioned|p150|||||||||
1729|Birkhead Formation|40541|3|Fully described|p109|||||||||
1729|Birkhead Formation|40544|6|Mentioned|p156|||||||||
1729|Birkhead Formation|40666|4|Described|p356|||||||||
1729|Birkhead Formation|40670|6|Mentioned|p212|||||||||
1729|Birkhead Formation|40675|6|Mentioned|Table 8A|||||||||
1729|Birkhead Formation|40687|3|Fully described|p414|||||||||
1729|Birkhead Formation|40832|3|Fully described|p455|||||||||
1729|Birkhead Formation|40833|6|Mentioned|p468|||||||||
1729|Birkhead Formation|40910|6|Mentioned|Table 3|||||||||
1729|Birkhead Formation|40926|6|Mentioned|Table 2|||||||||
1729|Birkhead Formation|40962|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|41060|5|Briefly described|p2|||||||||
1729|Birkhead Formation|41061|6|Mentioned|p19|||||||||
1729|Birkhead Formation|41062|6|Mentioned|p27,p34|||See also Fig.5||||||
1729|Birkhead Formation|41063|6|Mentioned|p40|||||||||
1729|Birkhead Formation|41064|6|Mentioned|p60|||||||||
1729|Birkhead Formation|41084|5|Briefly described|Fig.2|||||||||
1729|Birkhead Formation|41085|6|Mentioned|p87|||||||||
1729|Birkhead Formation|41097|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|41099|6|Mentioned|p192|||||||||
1729|Birkhead Formation|41123|6|Mentioned|p180|||||||||
1729|Birkhead Formation|41164|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|41165|6|Mentioned|p373|||See also Fig.18,Fig.20||||||
1729|Birkhead Formation|41175|4|Described|p195|||See also Fig.1||||||
1729|Birkhead Formation|41176|6|Mentioned|p206|||||||||
1729|Birkhead Formation|41177|6|Mentioned|p222|||||||||
1729|Birkhead Formation|41182|5|Briefly described|Fig.2|||||||||
1729|Birkhead Formation|41183|6|Mentioned|p310|||||||||
1729|Birkhead Formation|41184|6|Mentioned|p347|||||||||
1729|Birkhead Formation|41186|4|Described|p205|||||||||
1729|Birkhead Formation|41187|5|Briefly described|p216|||||||||
1729|Birkhead Formation|41189|6|Mentioned|p249|||||||||
1729|Birkhead Formation|41196|4|Described|p108|||||||||
1729|Birkhead Formation|41198|6|Mentioned|Table 1|||||||||
1729|Birkhead Formation|41212|6|Mentioned|p203|||||||||
1729|Birkhead Formation|41214|6|Mentioned|p254|||||||||
1729|Birkhead Formation|41216|6|Mentioned|p300|||See also Fig.18||||||
1729|Birkhead Formation|41219|4|Described|p345|||||||||
1729|Birkhead Formation|41247|6|Mentioned|p119|||||||||
1729|Birkhead Formation|41266|6|Mentioned|Fig.3|||||||||
1729|Birkhead Formation|41286|4|Described|p114|||||||||
1729|Birkhead Formation|41707|5|Briefly described|p161|||||||||
1729|Birkhead Formation|41712|6|Mentioned|Fig.4|||||||||
1729|Birkhead Formation|41724|6|Mentioned|p381|||||||||
1729|Birkhead Formation|41992|4|Described|Fig.2 P183|||||||||
1729|Birkhead Formation|42007|5|Briefly described|Fig.2 P182|||||||||
1729|Birkhead Formation|42008|6|Mentioned|Fig.5 P268|||||||||
1729|Birkhead Formation|42061|4|Described|Fig,11 P159|||||||||
1729|Birkhead Formation|42067|4|Described|p308|||See also appendix 2.||||||17-JAN-08
1729|Birkhead Formation|42071|6|Mentioned|p117|||||||||
1729|Birkhead Formation|42084|6|Mentioned|Fig.3 P356|||||||||
1729|Birkhead Formation|42085|6|Mentioned|Fig.2 P374|||||||||
1729|Birkhead Formation|42187|6|Mentioned|Fig.5 P322|||||||||
1729|Birkhead Formation|42395|5|Briefly described|Fig.13 P83|||||||||
1729|Birkhead Formation|42397|5|Briefly described|p10|||||||||
1729|Birkhead Formation|42446|4|Described|p11|||||||||
1729|Birkhead Formation|42447|5|Briefly described|p5 + Fig. 1|||||||||
1729|Birkhead Formation|42474|6|Mentioned|p25|||||||||
1729|Birkhead Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
1729|Birkhead Formation|42520|5|Briefly described|p6|||||||||
1729|Birkhead Formation|42648|5|Briefly described|p42|||||||||
1729|Birkhead Formation|42746|4|Described|p10|||See also Fig.6.||||||17-JAN-08
1729|Birkhead Formation|42749|4|Described|p27, p29|||see also Fig.2 p27.||||||17-JAN-08
1729|Birkhead Formation|42999|5|Briefly described|Table 2,p90|Late Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
1729|Birkhead Formation|43002|5|Briefly described|Fig.2,p135|||||||||
1729|Birkhead Formation|43004|5|Briefly described|Table 1,p179|||||||||
1729|Birkhead Formation|43105|5|Briefly described|p15|||||||||
1729|Birkhead Formation|43114|5|Briefly described|p10|||||||||
1729|Birkhead Formation|43122|5|Briefly described|p7|||see also Fig. 2.||||||
1729|Birkhead Formation|43591|6|Mentioned|p40|||||||||
1729|Birkhead Formation|43628|6|Mentioned|Fig.3|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|43711|6|Mentioned|p20|||||||||
1729|Birkhead Formation|44016|14|Not recorded|Map Legend||Middle Jurassic|||||||
1729|Birkhead Formation|44019|14|Not recorded|Map Legend||Middle Jurassic|||||||
1729|Birkhead Formation|44020|14|Not recorded|Tb.1,2|Late Jurassic|Middle Jurassic|Of Injune Creek Grup.||||||
1729|Birkhead Formation|44021|2|Defined|p232-236||Middle Jurassic|Lower part of Injune Creek Group. Conformably overlies Hutton Sandstone; Overlain in Eromanga Basin by Adori Sandstone; in Surat Basin overlain by Westbourne Formation. Plants and spores.||||||13-MAR-14
1729|Birkhead Formation|44022|14|Not recorded|Map Legend||Middle Jurassic|||||||
1729|Birkhead Formation|44023|4|Described|Tb.3,p11||Middle Jurassic|||||||
1729|Birkhead Formation|44028|14|Not recorded|Fig.2,p514,509||Jurassic|Of Injune Creek Group. See Strat Table.||||||
1729|Birkhead Formation|44031|14|Not recorded|Tb.2,p5,8||Jurassic|||||||
1729|Birkhead Formation|44084|14|Not recorded|p32(Tb)||Middle Jurassic|||||||
1729|Birkhead Formation|44133|5|Briefly described|p110, 104 Fig. 9.11|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin. Intertongues and overlies: Hutton Sandstone. Overlain by the Namur or Adori Sandstone.||||||13-MAR-14
1729|Birkhead Formation|44171|14|Not recorded|p194,195,197,198|||Name discontinued. May be replaced by Walloon Coal Measures.||||||
1729|Birkhead Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
1729|Birkhead Formation|44390|14|Not recorded|p6,9,10,13,15,16,Tb1|Middle Jurassic|Early Jurassic|||||||
1729|Birkhead Formation|44391|14|Not recorded|Map Legend||Middle Jurassic|||||||
1729|Birkhead Formation|44414|14|Not recorded|p111,112,114||Cretaceous|||||||
1729|Birkhead Formation|44415|14|Not recorded|Fig.1,p23|||||||||
1729|Birkhead Formation|45071|3|Fully described|Table 15|||||||||
1729|Birkhead Formation|45110|2|Defined|p95|Middle Jurassic|Middle Jurassic|||||||
1729|Birkhead Formation|45168|6|Mentioned|p9|||||||||
1729|Birkhead Formation|46791|6|Mentioned|Fig.6|||||||||
1729|Birkhead Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
1729|Birkhead Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
1729|Birkhead Formation|46984|6|Mentioned|p154|||||||||
1729|Birkhead Formation|48900|4|Described|p53|||Middle Jurassic.||||||
1729|Birkhead Formation|48919|2|Defined|p58|Middle Jurassic|Middle Jurassic|See also p59-61.||||||17-JAN-08
1729|Birkhead Formation|48920|3|Fully described|p49|||Part of Injune Creek Group.||||||21-APR-08
1729|Birkhead Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
1729|Birkhead Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
1729|Birkhead Formation|60386|6|Mentioned|p299||Middle Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
1729|Birkhead Formation|60717|5|Briefly described|p40 Fig. 2, p42|Late Jurassic|Middle Jurassic|Overlies and interfingers with Hutton Sandstone; overlain by Namur and Adori Sandstones. Geological Province: Eromanga Basin.||||||31-JAN-08
1729|Birkhead Formation|60993|5|Briefly described|p31, p6 Fig. 2|||Westerly lateral extension of the Walloon Coal Measures but more sandy and less coaly in composition. Both units are of the Injune Creek Group. Geological Province: Surat and Eromanga Basins. ||||||28-AUG-12
1729|Birkhead Formation|61015|6|Mentioned|p44|||Includes Callamurra Member?||||||19-APR-05
1729|Birkhead Formation|61312|5|Briefly described|p71, p79 Table E2|Late Jurassic|Middle Jurassic|Of the Injune Creek Group. Fine-grained sandstone, siltstone and carbonaceous mudstone, with some coal. Geological Province: Eromanga Basin.||||||09-APR-13
1729|Birkhead Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||13-MAR-09
1729|Birkhead Formation|61613|6|Mentioned|p282, p284, p282 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
1729|Birkhead Formation|61614|6|Mentioned|p289, p294, p295, p297, p290 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin. Contain coals and shales.||||||17-MAR-09
1729|Birkhead Formation|61615|6|Mentioned|p302 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
1729|Birkhead Formation|62537|6|Mentioned|p191 Fig.2. |Late Jurassic|Middle Jurassic|Eromanga Basin.||||Overlies Hutton Sandstone. Is overlain by Murta Formation.||
1729|Birkhead Formation|62730|5|Briefly described|p352 Fig. 1|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
1729|Birkhead Formation|63218|6|Mentioned|p211 Fig.2. |Middle Jurassic|Middle Jurassic|Surat Basin.||Unit in Injune Creek Group.||||
1729|Birkhead Formation|63748|6|Mentioned|p23|||Geological province: Eromanga Basin. Equivalent of Walloon Coal Measures in the Clarence-Moreton Basin.||||||07-FEB-11
1729|Birkhead Formation|63979|2|Defined|p35|Callovian|Bathonian|Conformable on Hutton Sandstone; unconformable below Adori Sandstone. Max. thickness:110m. Interbedded sandstone and siltstone, minor mudstone + shale, predominantly v. fine- to medium-grained + a few beds of coarse-grained sandstone. In Eromanga Basin.||||||07-FEB-11
1729|Birkhead Formation|64048|5|Briefly described|p64 Tb. 2, p69|Jurassic|Jurassic|Geological Province: Eromanga Basin. Possesses hydrocarbon source potential. Rich in Type III kerogen and vitrinite is more common than inertinite.||||||07-FEB-11
1729|Birkhead Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Jurassic|Middle Jurassic|Eromanga Basin.||||Underlies Namur Sandstone Member and Adori Sandstone; overlies Hutton Sandstone.||10-DEC-15
1729|Birkhead Formation|64232|5|Briefly described|p12|Jurassic|Jurassic|Geological Province: Eromanga Basin. Coal occurs in deeper parts of the basin in this unit.||||||24-JUL-08
1729|Birkhead Formation|64665|5|Briefly described|p53 Fig.2, pp61-62.|Middle Jurassic|Middle Jurassic|Eromanga Basin. Equivalent to Walloon Subgroup in Surat Basin. Deposited in low energy fluvial to paludal environment. Hosts thin, uneconomic coals.||||Overlies Hutton Sandstone.||
1729|Birkhead Formation|64856|5|Briefly described|p88, p90-91, p102|||Should be restricted to Eromanga Basin. Laterally continuous with Walloon Coal Measures. Palynoflora suggest time break before overlying Adori Sandstone.| | ||||28-NOV-17
1729|Birkhead Formation|65096|6|Mentioned|p368|||||||The lower beds of the Birkhead Formation are equivalent to the Walloon Coal Measures.||
1729|Birkhead Formation|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Overbank and lacustrine-swamp deposits.||||||17-FEB-10
1729|Birkhead Formation|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Middle Jurassic|Of Eromanga Basin. Overlies Hutton Sandstone.||||||08-MAR-12
1729|Birkhead Formation|65489|5|Briefly described|p15, p24, p45-47, p49, p62, p73-74, p96|Middle Jurassic|Middle Jurassic|See also p152, p154-158, p160. Eromanga Basin. 120m thick. Hydrocarbon source rock. Variable reservoir quality. Hosts gas indication. Oil reservoir accounting for 6% of the Basin's production. Represents distal extent of volcanic-arc sediment from the east. Intraformational shale regional seal.||||Overlies Hutton Sandstone. Is overlain by Adori Sandstone.|Includes meandering fluvial sandstones and organic-rich shales.|
1729|Birkhead Formation|65925|5|Briefly described|p15, Appendix 2.||||||||Dark grey and brown siltstone; mudstone; buff, fine- to medium-grained sandstone; minor coal seams.|
1729|Birkhead Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. ||Unit in Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Adori Sandstone.||
1729|Birkhead Formation|66915|5|Briefly described|p6 Fig.3, p12|Middle Jurassic|Middle Jurassic|Eromanga Basin.||||||
1729|Birkhead Formation|67323|5|Briefly described|p87-88, p93 Fig.12.3, p95 Fig.12.5|Middle Jurassic|Middle Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin.||||Overlies Hutton Sandstone. Is overlain by Adori Sandstone.|Contains coal.|
1729|Birkhead Formation|67402|4|Described|p26, p26 tbl RRM4, p108|Early Cretaceous|Early Jurassic|Eromanga Basin. Deposited in a fluvial to fluvio-lacustrine environment during a series of regressive-transgressive cycles. Maximum thickness of 110m. Demonstrated hydrocarbon seal for the Hutton Sandstone. See also p109, p113 fig ERO12, p113, p115, p123||||Overlies the Hutton Sandstone. Overlain by the Adori Sandstone.|Interbedded sequence of siltstone, sandstone and claystone with minor mudstone and shale.|
1729|Birkhead Formation|67561|6|Mentioned|p53 Fig.3, p58-p62.|||||||||
1729|Birkhead Formation|68068|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Eromanga Basin. Subsurface only. Lacustrine, paludal, fluvial (meandering river).||||Overlies Hutton Sandstone. Is overlain by Namur Sandstone.|Dark grey-brown siltstone with minor mudstone and buff sandstone; carbonaceous, sideritic, burrows, root casts and mottling; interbedded with coal as thin beds and stringers.|
1729|Birkhead Formation|68117|5|Briefly described|p346|Middle Jurassic|Middle Jurassic|Western Surat Basin.||Injune Creek Group.||Equivalent to Walloon Subgroup.||
1729|Birkhead Formation|68135|5|Briefly described|p52 fig 2b, p54|Callovian|Bathonian|Eromanga Basin. Contains plant macrofossils.||||Overlies Hutton Sandstone. Is overlain unconformably by Adori Sandstone.|Interbedded sandstone and siltstone.|14-SEP-17
1729|Birkhead Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
1729|Birkhead Formation|68731|6|Mentioned|pp209-211|||||||||
1729|Birkhead Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
1729|Birkhead Formation|69019|5|Briefly described|p85 Fig.21.|Kimmeridgian|Callovian|Southern Eromanga Basin.||||Overlies Hutton Sandstone. Is overlain by Adori Sandstone.||
1729|Birkhead Formation|69023|5|Briefly described|p79, p89 Fig.20, p91, p163, p191-192|Late Jurassic|Middle Jurassic|Defined by Exon (1966) from outcrop in Tambo area, Qld. Stratigraphic wells intersection data.||||Conformably overlies and intertongues with Hutton Sandstone. Is overlain conformably by Namur Sandstone.|Dark brown to dark grey, carbonaceous and sideritic, bioturbated siltstone and mudstone interbedded with buff, fine- to medium-grained sandstone containing thin basal pebble lags, and thin laterally discontinuous coal seams.|
1729|Birkhead Formation|69457|6|Mentioned|p41:3-4|||Eromanga Basin.||||||12-JUL-16
1729|Birkhead Formation|69582|6|Mentioned|p65-p66|Late Jurassic|Late Jurassic|Eromanga Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Hutton Sandstone. Overlain by the Adori Sandstone.|Sandstone.|
1729|Birkhead Formation|69594|4|Described|p519, p525-526, p531-532, p537, p544-545|Callovian|Bartonian|See also p573. Restricted to the Eromanga Basin by Green et al. (1997). The type section, 573-684m in AOP Westbourne 1 (Exon, 1966), was revisd to include an additional 61m underlying that interval in nearby GSQ Augathella 2-3R (Green et al., 1989). Commonly 40-100m thick; maximum 110m. Fluvio-lacustrine deposits. Highly diachronous lower boundary. Hosts important hydrocarbons.||||Conformably overlies Hutton Sandstone. Is overlain unconformably by Namur and Adori Sandstones. Laterally continuous with/equivalent to Walloon Coal Measures.|Interbedded labile to sublabile sandstone and siltstone, with minor mudstone and shale. Sandstones are increasingly lithic, with strong volcanogenic input, particularly in the east.|
1729|Birkhead Formation|69673|6|Mentioned|p154, p155 fig 127|Jurassic|Jurassic|||||Overlies Hutton Sandstone, overlain by Adori Sandstone||
1729|Birkhead Formation|69790|5|Briefly described|p1061-1062, p1064-1066|Middle Jurassic|Middle Jurassic|Eromanga Basin. Freshwater lacustrine environment.||||Is overlain unconformably by Adori Sandstone. Grades into Walloon Subgroup (to the E).||
1729|Birkhead Formation|69797|5|Briefly described|p17 Fig.3|Late Jurassic|Middle Jurassic|Oil discoveries reservoired in channel sands, at base. The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are coals and carbonaceous shales of Birkhead Formation, organic-rich shales and siltstones of Murta Formation and highly carbonaceous shales of Poolowanna Formation. Age approximated from figure. Geol. Prov: Eromanga Basin.||||||17-JAN-17
1729|Birkhead Formation|69946|3|Fully described|p11-16, p56-58, p61, p74-82|Late Jurassic|Middle Jurassic|Exon (1966). Informally referred to as Walloon Coal Measures (Reeves, 1947) or Walloon Formation, but Exon's definition stands. His type section is the interval 573 - 684m in Westbourne 1. Provenance ages of <1000 Ma and 950 Ma. Subsurface distribution mentioned. Up to >150m thick. Wireline log correlations. Sedimentary facies log.||||Intertongues with Algebuckina Sandstone and underlying Hutton Sandstone. Is overlain conformably by Namur and Adori Sandstones.|Interbedded dark grey and brown siltstone, mudstone and buff, fine- to medium-grained sandstone with thin, lenticular coal seams (<0.3m thick); volcanogenic lithics and labile minerals occur.|
1729|Birkhead Formation|69947|4|Described|p3,p5-8,p13 Fig.7.2, p22-28 Figs.7.11-17|Late Jurassic|Middle Jurassic|Eromanga Basin. Widespread lacustrine facies. A regional sequence boundary separates this unit from the underlying Hutton Sandstone. Potential for stratigraphic traps. Oil accumulations occur in two discrete intervals. Paleogeography maps. Generalised stratigraphic section.||||Overlies Hutton Sandstone. Is overlain by Adori Sandstone or conformably by Namur Sandstone.|Reworked sandstones, fine-grained and organic-rich deposits.|
1729|Birkhead Formation|69948|6|Mentioned|Figs.4.13-14, 18|||Eromanga Basin. Seismic sections across the Gidgealpa and Big Lake Fields.||||||
1729|Birkhead Formation|70374|5|Briefly described|p809 figure 1,|Callovian|Bathonian|||Injune Creek Group||Overlies Hutton Sandstone. Shown as lateral equivalent of Walloon Coal Measures.||28-SEP-16
1729|Birkhead Formation|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Eromanga Basin.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Adori Sandstone or Hooray Sandstone.||
1729|Birkhead Formation|70823|4|Described|p25-p27, p43-p44, p78|Middle Jurassic|Middle Jurassic|Eromanga Basin. Deposited in a meandering-anastamosing fluvial or lacustrine or overbank environments.||||Overlies and interfingers with the Hutton Sandstone. Overlain by the Adori Sandstone.|Sandstone, siltstone, shale and coal.|
1729|Birkhead Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Hutton Sandstone. Overlain by the Adori Sandstone.||
1729|Birkhead Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Hutton Sandstone. Grades laterally into the Adori Sandstone. Overlain by the Namur Sandstone.||24-OCT-19
1729|Birkhead Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p20-p21|Tithonian|Callovian|Eromanga  Basin. First named by Exon (1966). This unit was previously informally referred to as the Walloon Coal Measures (Reeves, 1947) or the Walloon Formation from the western Surat Basin and Clarence-Moreton Basin. A type section in Westbourne 1 in Queensland is mentioned. Lithology and petrography are described in detail. A maximum thickness of >150m occurs in the Patchawarra and Nappamerri troughs. Age derived from palynology. Deposited in a lacustrine and coal swamp environment that was cut by meandering fluvial channels. Spore-pollen zone is given in Ch5 p57. Sedimentary characteristics and palaeoenvironment are discussed in some detail. A complete sedimentary facies is log is given in Ch5 p77. Sequence stratigraphy is detailed in Ch7. Forms a seal over the Hutton Sandstone. Reservoir and seal characteristics discussed in Ch11. This unit is one of the primary sources of petroleum production in the Eromanga Basin. See also Ch5 p12-p15, Ch5 p17, Ch5 p30-p31, Ch5 p56-p58, Ch5 p73-p81, Ch6 p5, Ch7 p3, Ch7 p5-p8, Ch7 p10, Ch7 p13, Ch7 p22-p28, Ch8 p2-p4, Ch8 p8, Ch8 p10, Ch8 p15-p16, Ch8 p28, Ch9 p5, Ch9 p10-p11, Ch10 p3, Ch10 tbl 10.1, Ch10 p6-p7, Ch10 p13, Ch10 p15, Ch10 p17-p19, Ch11 p2-p4, Ch11 p7-p8, Ch11 p15, Ch12 p2, Ch12 p5-p6, Ch12 p12, Ch12 p14-p15, Ch13 p2-p3, Ch13 p4, Ch13 p6-p9, Ch13 p11, Ch13 p39-p40, Ch14 p2, Ch14 p5-p7.||||Conformably overlies the Hutton Sandstone. Conformably overlain by the Namur and Adori Sandstones. Equivalent to the Algebuckina Sandstone.|Interbedded dark grey and brown siltstone, mudstone and buff, fine to medium-grained sandstone with thin, lenticular coal seams.|
1729|Birkhead Formation|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
1729|Birkhead Formation|71863|5|Briefly described|p4|||Eromanga Basin. Potential petroleum source (although the majority is derived from the underlying Cooper Basin units).||||||
1729|Birkhead Formation|72297|5|Briefly described|p700, p739, p743|Cretaceous|Jurassic|Eromanga Basin. Crops out from Injune NW to near Blackall. Petroleum source rock potential. Gas flows probably sourced from Permian coal measures. A relatively competent seal over Hutton Sandstone oil reservoirs.||||Correlative of Walloon Coal Measures.|Contains thin (up to 1.5m thick) coal seams.|
1729|Birkhead Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores in QLD/NSW.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Adori Sandstone.||
1729|Birkhead Formation|72921|5|Briefly described|p15 Fig.2.|Middle Jurassic|Middle Jurassic|Shown as located in the Eromanga Basin.||||Overlies and is partly laterally equivalent to Durabilla Formation and shown as unconformably underlying Adori Sandstone.|May include sandstone and shale and some fossil flora.|
1729|Birkhead Formation|73147|6|Mentioned|p141|||Eromanga Basin. Contains spinose acritarchs, indicating marine transgression south from the Carpentaria, across the Eromanga and into the Surat, Basin.||||||
1729|Birkhead Formation|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil and gas, hydrocarbon source.||||||
1729|Birkhead Formation|73249|6|Mentioned|p319|Cretaceous|Jurassic|Eromanga Basin.||||||
1729|Birkhead Formation|73251|6|Mentioned|p49, p55-56, p62|Late Jurassic|Middle Jurassic|Eromanga Basin. Good source rock; capable of generating hydrocarbons that could migrate into the overlying sequence. Deposited in a fluviolacustrine, backswamp setting. Contains[?] oil and has gas shows.||||Underlain by [and equivalent to?] Hutton Sandstone. Overlain by Adori Sandstone and Namur Sandstone. Equivalent to Algebuckina Sandstone.||
1729|Birkhead Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Source rock that hosts oil and gas.||||Underlain by Hutton Sandstone. Overlain by Mooga Formation and Adori Sandstone.||
1729|Birkhead Formation|73393|6|Mentioned|p21|Oxfordian|Bathonian|Eromanga Basin.||Injune Creek Group||Underlain by Hutton Sandstone. Equivalent to Walloon Coal Measures and Eurombah Formation.||
1729|Birkhead Formation|73479|4|Described|p156 Fig.2, p159, p163, p179|Late Jurassic|Late Jurassic|Eromanga Basin. Fluvial-lacustrine depositional environment.|ca 157 Ma|||Overlies Birkhead Formation, underlies Mooga Sormation, Adori Sandstone|Includes a sandstone channel facies embedded in floodplain and lacustrine shales.|
1901|Blanche Point Formation|22525|5|Briefly described|p35,36,39||Eocene|||||||
1901|Blanche Point Formation|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
1901|Blanche Point Formation|22541|4|Described|Table 1, Fig 1,3,7||Late Eocene|||||||
1901|Blanche Point Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
1901|Blanche Point Formation|22822|6|Mentioned|P11||Tertiary|||||||
1901|Blanche Point Formation|23010|6|Mentioned|p340|||||||||
1901|Blanche Point Formation|23331|5|Briefly described|1089 Fig.2|Late Eocene|Late Eocene|||||||
1901|Blanche Point Formation|23489|4|Described|p44|Oligocene|Eocene|||||||
1901|Blanche Point Formation|23768|5|Briefly described|p28 Fig.5, p123|Late Eocene|Late Eocene|Geological Province: St Vincent Basin.  See also p101, p123.||||||11-SEP-09
1901|Blanche Point Formation|23802|5|Briefly described|p21 Fig. 2|||Siliceous layers - glaucony grains - turreted gastropods.||||||12-NOV-08
1901|Blanche Point Formation|24397|5|Briefly described|p234 Tb. 2|Eocene|Eocene|Geological Province: St. Vincent Basin.||||||
1901|Blanche Point Formation|30250|6|Mentioned|p2|||See also Fig.2||||||
1901|Blanche Point Formation|32117|6|Mentioned|Fig.2|||||||||
1901|Blanche Point Formation|34825|6|Mentioned|p14|||Re age dates.||||||
1901|Blanche Point Formation|35542|6|Mentioned|p2|||||||||
1901|Blanche Point Formation|35689|2|Defined|p18|late Eocene|late Eocene|||||||
1901|Blanche Point Formation|35697|6|Mentioned|p90|||||||||
1901|Blanche Point Formation|36119|6|Mentioned|p52|||||||||
1901|Blanche Point Formation|36127|4|Described|p11|||See also p7.||||||23-JUN-08
1901|Blanche Point Formation|36200|6|Mentioned|p8|||See also Table 1.||||||
1901|Blanche Point Formation|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
1901|Blanche Point Formation|36490|6|Mentioned|p189|||Wrongly originally entered for NT.||||||
1901|Blanche Point Formation|36500|6|Mentioned|Fig.4|||||||||
1901|Blanche Point Formation|37311|6|Mentioned|p18|||||||||
1901|Blanche Point Formation|37324|6|Mentioned|p11|||||||||
1901|Blanche Point Formation|38107|4|Described|p25|||||||||
1901|Blanche Point Formation|38621|1|Redefined|p3|late Eocene|late Eocene|||||||
1901|Blanche Point Formation|38622|6|Mentioned|p8|||||||||
1901|Blanche Point Formation|38699|6|Mentioned|p12|||||||||
1901|Blanche Point Formation|38702|6|Mentioned|p127|||||||||
1901|Blanche Point Formation|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
1901|Blanche Point Formation|40148|6|Mentioned|p161|||||||||
1901|Blanche Point Formation|40152|6|Mentioned|p10|||||||||
1901|Blanche Point Formation|40238|4|Described|p325|||||||||
1901|Blanche Point Formation|40429|6|Mentioned|p26|||||||||
1901|Blanche Point Formation|40453|6|Mentioned|p61|||||||||
1901|Blanche Point Formation|40778|5|Briefly described|p529|||||||||
1901|Blanche Point Formation|40877|4|Described|p46|||||||||
1901|Blanche Point Formation|40969|6|Mentioned|p8|||||||||
1901|Blanche Point Formation|40970|6|Mentioned|p16|||||||||
1901|Blanche Point Formation|41025|6|Mentioned|Fig.2|||||||||
1901|Blanche Point Formation|41495|4|Described|p43|||||||||
1901|Blanche Point Formation|41513|6|Mentioned|p35|||||||||
1901|Blanche Point Formation|41517|6|Mentioned|p137|||||||||
1901|Blanche Point Formation|41520|4|Described|Fig.5|||||||||
1901|Blanche Point Formation|41626|6|Mentioned|p54|||||||||
1901|Blanche Point Formation|42461|6|Mentioned|p87|late Eocene||||||||
1901|Blanche Point Formation|42477|5|Briefly described|p191|||||||||
1901|Blanche Point Formation|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
1901|Blanche Point Formation|42506|5|Briefly described|Map legend|Eocene||Age: Tertiary.||||||23-JUN-08
1901|Blanche Point Formation|42574|6|Mentioned|Fig.2 P242|||||||||
1901|Blanche Point Formation|42733|5|Briefly described|map legend|Tertiary||||||||
1901|Blanche Point Formation|43026|6|Mentioned|p589|||||||||
1901|Blanche Point Formation|43053|5|Briefly described|Map Legend|Miocene|Eocene|Marine limestone. Geological Province: St Vincent Basin.||||||25-MAY-05
1901|Blanche Point Formation|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
1901|Blanche Point Formation|43298|6|Mentioned|Map Legend|Miocene|Eocene|||||||
1901|Blanche Point Formation|43667|6|Mentioned|Fig.3,p12||Late Eocene|||||||
1901|Blanche Point Formation|43675|6|Mentioned|p339|||||||||
1901|Blanche Point Formation|44133|5|Briefly described|p168, 165 Fig. 10.11|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Includes: Tuketja Member, Gull Rock Member, Perkana Member.||||||
1901|Blanche Point Formation|49060|6|Mentioned|p74|||||||||
1901|Blanche Point Formation|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Includes: Tuit Member, Perkana Member, Tuketja Member.||||||
1901|Blanche Point Formation|60953|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Saint Vincent Basin.||||||
1901|Blanche Point Formation|60958|5|Briefly described|Map Legend|Eocene|Eocene|Silty limestone and calcareous siltstone with sandy siltstone interlayers. Geological Province: Saint Vincent Basin.||||||23-DEC-09
1901|Blanche Point Formation|61108|5|Briefly described|map legend|Miocene|Eocene|Geological Province: St Vincent Basin.||||||
1901|Blanche Point Formation|61121|5|Briefly described|Map legend|Eocene|Eocene|Silty limestone and clacareous siltstone with sandy siltstone interlayers; abundant 'Spirocolpus' (Turtella).  Geological Province: St. Vincent Basin.||||||23-DEC-09
1901|Blanche Point Formation|61155|5|Briefly described|p3, p17|Early Oligocene|Late Eocene|Contains distinctive silicified horizons. Overlies Tortachilla Limestone; underlies Chinaman Gully Formation in south east part of basin. Age: 39.5-36.5Ma. Geological Province: St Vincent Basin.||||||03-MAR-10
1901|Blanche Point Formation|62896|5|Briefly described|p87|Oligocene|Late Eocene|Geological Province: St Vincent Basin.||||||07-FEB-11
1901|Blanche Point Formation|63740|5|Briefly described|p87|Oligocene|Eocene|Includes Gull Rock Member. Geological province: St Vincent Basin.||||||07-FEB-11
1901|Blanche Point Formation|64282|5|Briefly described|Map legend|Eocene|Eocene|Geolocial Province: St Vincent Basin. Silty limestone and calcareous siltstone with sandy siltstone interlayers; abundant Spirocolpus (Turritella).||||||24-JUL-08
1901|Blanche Point Formation|64397|5|Briefly described|p232 Fig. 1A, p233|Eocene|Eocene|Comprises Tuketja, Gull Rock, Perkana and Tuit Members. Unconformable on Tortachilla Limestone. Fossiliferous and biosiliceous marls and mudstones; commonly silicified. Geological province: St Vincent Basin.||||||
1901|Blanche Point Formation|64993|5|Briefly described|p26|||Geological province: St Vincent Basin. Contains a molluscan assemblage, preserved as moulds, in its upper level (Tuit Member).||||||
1901|Blanche Point Formation|65375|4|Described|p34 Fig.7, p35. |Eocene|Eocene|Correlates with lower part of Rogue Formation. Abundant Spirocolpus (Turritella) fossils; Late Eocene age. Previously included in Blanche Point Limestone or upper Muloowurtie Formation. Age given as Tertiary but fossils indicate Late Eocene age.||||Overlies or partly intertongues with Muloowurtie Formation. Grades into Rogue Formation.|A c.4m thick bed of fossiliferous silty limestone and calcareous siltstone.|
1901|Blanche Point Formation|65891|5|Briefly described|p221 Fig.5, p222, p228 Fig.11, p233. |Paleogene|Paleogene|St Vincent Basin. Highly siliceous. Has marked fluctuations between epifaunal and infaunal foraminifera. Includes Tuketja, Gull Rock, Perkana and Tuit Members. Overlies Tortachilla Limestone; is disconformably overlain by Chinaman Gully Formation.||||||
1901|Blanche Point Formation|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||Is overlain by the Chinaman Gully Formation.||
1901|Blanche Point Formation|66194|5|Briefly described|p584-5|Late Eocene|Late Eocene|St Vincent Basin; marine.||||||09-MAR-12
1901|Blanche Point Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eastern Saint Vincent Basin.||||||
1901|Blanche Point Formation|68715|6|Mentioned|p31 Fig.5|Bartonian|Lutetian|St Vincent Basin.||||||
1901|Blanche Point Formation|68811|6|Mentioned|p178 Table 38, p88|Tertiary|Tertiary|Misspelt as Blanch Point Formation in Fig. 50 p88.||||Overlies the Maslin Sands. Overlain by the Port Willunga Formation.||15-APR-20
1901|Blanche Point Formation|70382|5|Briefly described|p29 Fig 3|Eocene|Eocene|Yorke Peninsula region.|||||Mudstone, glauconitic, calcareous; spicular chert; calcareous mudstone and spongolite.|
1901|Blanche Point Formation|70660|4|Described|p3, p8-p12, p15, p17-p20|Priabonian|Eocene|This name has superseded the Blanche Point Marls. Contains four members. This unit is highly fossiliferous with much aragonite preserved. See also  p25-p26, p33, p46.|||Includes the Tuketja Member, Gull Rock Member, Perkana Member and the Tuit Member.|Overlain by the Chinaman Gully Formation.||
1901|Blanche Point Formation|70722|5|Briefly described|p217-218,227|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.|||Includes Tuit, Perkana, Gull Rock and Tuketja members.|Overlain by Chinaman Gully Formation. Underlain by Tortachilla Limestone.||
1901|Blanche Point Formation|72450|5|Briefly described|Brochure, Brochure map|Eocene|Eocene|Crops out at the in the seaside cliffs at Blanche Point and Port Noarlunga. Contains abundant marine fossils including conical and turreted gastropods. In drillholes where unweathered the unit is dark grey to black. Recognised elsewhere in auger hole cuttings of new vineyards.|||||Pale calcareous silt and sand with layers of limestone and chert.|
1901|Blanche Point Formation|73107|5|Briefly described|Map legend.|Eocene|Eocene||||||Silty limestone and calcareous siltstone with sandy siltstone interlayers. Abundant Spirocolpus (Turritella).|
1901|Blanche Point Formation|73188|5|Briefly described|p: 319-320, 322, 333-336, 345, 351, 356|Late Eocene|Late Eocene|St Vincent Basin. Deposited in a fully marine environment.|||Tuit Member, Perkana Member, Gull Rock Member, Tuketja Member|Underlain by Tortachilla Limestone. Disconformably overlain by Chinaman Gully Formation.|Calcareous and siliceous silty marine shelf sediments.|
1918|Blanchetown Clay|2967|5|Briefly described|p14, 48-53, 74, 155, 159, 166, 169, 205|Pleistocene|Pliocene|Firman (1965). Western Murray Basin. Up to 34m thick. See also p207, 280, 283, 285, 304, 318, 322, 327, 331, 333-334.||||Is separated from the underlying Parilla Sand by the Karoonda Surface. Is overlain locally by Tyrrell Beds.|Lacustrine sequence of olive-grey clay, silt and minor interbedded fine sand.|
1918|Blanchetown Clay|10010|5|Briefly described|p12 Fig. 3, p16|Pleistocene|Pleistocene|Fine-grained lacustrine deposits of Lake Bungunnia. Geological Province: Murray Basin.||||||13-AUG-07
1918|Blanchetown Clay|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|22799|2|Defined|p39|Late Pliocene|Late Pliocene|||||||
1918|Blanchetown Clay|22857|5|Briefly described|p352 Fig. 24.8|Early Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
1918|Blanchetown Clay|22893|3|Fully described|p52 table3||Pleistocene|Generally 2-5m thick, up to 20m.||||||
1918|Blanchetown Clay|22941|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|23089|5|Briefly described|p649|||||||||
1918|Blanchetown Clay|23560|6|Mentioned|p165|||||||||
1918|Blanchetown Clay|23818|5|Briefly described|p210, p212 Fig.108|Middle Pleistocene|Early Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|23884|6|Mentioned|p153|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|24043|5|Briefly described|p525|||||||||
1918|Blanchetown Clay|24465|5|Briefly described|p351 Fig.1|Quaternary|Quaternary|||||||
1918|Blanchetown Clay|24566|5|Briefly described|p114|Pliocene|Pliocene|||||||
1918|Blanchetown Clay|24574|6|Mentioned|p706|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|29591|6|Mentioned|Table 20|||||||||
1918|Blanchetown Clay|29697|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|30145|6|Mentioned|p183|||||||||
1918|Blanchetown Clay|30750|6|Mentioned|p1|||Pleistocene age||||||
1918|Blanchetown Clay|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30753|4|Described|p15|||Lower Pleistocene age||||||
1918|Blanchetown Clay|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See also P22,23,31,41,42||||||
1918|Blanchetown Clay|30755|6|Mentioned|p169|||Tectonic map.||||||
1918|Blanchetown Clay|30758|6|Mentioned|p66|||Stratigraphy||||||
1918|Blanchetown Clay|30807|6|Mentioned|p101|||Suggested map symbol.||||||
1918|Blanchetown Clay|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30994|6|Mentioned|Fig. 1|||||||||
1918|Blanchetown Clay|30996|3|Fully described|p32|||Contains dolomite & limestone members.||||||03-FEB-09
1918|Blanchetown Clay|31240|5|Briefly described|p64|||Pleistocene||||||
1918|Blanchetown Clay|31319|5|Briefly described|p157|||Pleistocene||||||
1918|Blanchetown Clay|31345|6|Mentioned|p294|||||||||
1918|Blanchetown Clay|31554|6|Mentioned|p14|||||||||
1918|Blanchetown Clay|31741|6|Mentioned|p6|||||||||
1918|Blanchetown Clay|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|32007|4|Described|p159|||Palaeontology fully discussed||||||
1918|Blanchetown Clay|32099|6|Mentioned|p229|||||||||
1918|Blanchetown Clay|32323|6|Mentioned|p9|||Pleistocene||||||
1918|Blanchetown Clay|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
1918|Blanchetown Clay|32432|6|Mentioned|Fig.2|||See also Table 1||||||
1918|Blanchetown Clay|32433|6|Mentioned|p80|||See also Table 2||||||
1918|Blanchetown Clay|32439|6|Mentioned|p99|||||||||
1918|Blanchetown Clay|32861|5|Briefly described|Table 1|||Lithology||||||
1918|Blanchetown Clay|32862|5|Briefly described|Table 3|||Pleistocene||||||
1918|Blanchetown Clay|32864|6|Mentioned|Fig. 5|||||||||
1918|Blanchetown Clay|33048|6|Mentioned|p195|||See also P196||||||
1918|Blanchetown Clay|33051|6|Mentioned|p187|||||||||
1918|Blanchetown Clay|33725|6|Mentioned|p10|||Small sinkholes.||||||
1918|Blanchetown Clay|33826|6|Mentioned|p42|||Strat. table||||||
1918|Blanchetown Clay|34069|6|Mentioned|p1|||See also Fig.2. Pleist.||||||
1918|Blanchetown Clay|34114|4|Described|p50|||Pleistocene||||||
1918|Blanchetown Clay|34180|6|Mentioned|p212|||Lower - Middle Pleistocene.||||||
1918|Blanchetown Clay|34459|4|Described|p11|||||||||
1918|Blanchetown Clay|34460|4|Described|p164|||Lithology. Table 2||||||
1918|Blanchetown Clay|34461|5|Briefly described|p49|||Pleistocene||||||
1918|Blanchetown Clay|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|34690|6|Mentioned|p1|||||||||
1918|Blanchetown Clay|34758|6|Mentioned|p27|||||||||
1918|Blanchetown Clay|34933|6|Mentioned|p58|||||||||
1918|Blanchetown Clay|35029|6|Mentioned|p166|||||||||
1918|Blanchetown Clay|35071|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35097|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35131|6|Mentioned|p8|||||||||
1918|Blanchetown Clay|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|35232|5|Briefly described|Table.4|||||||||
1918|Blanchetown Clay|35272|4|Described|p283|||||||||
1918|Blanchetown Clay|35541|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|37619|6|Mentioned|p2|||||||||
1918|Blanchetown Clay|37661|6|Mentioned|p8.2.1|||||||||
1918|Blanchetown Clay|37796|6|Mentioned|p161|||||||||
1918|Blanchetown Clay|37873|4|Described|p2|||||||||
1918|Blanchetown Clay|38068|6|Mentioned|p76|||||||||
1918|Blanchetown Clay|38605|6|Mentioned|p30|||||||||
1918|Blanchetown Clay|39322|6|Mentioned|p404|||||||||
1918|Blanchetown Clay|39329|6|Mentioned|Fig.1|||||||||
1918|Blanchetown Clay|40003|6|Mentioned|Table 8|||||||||
1918|Blanchetown Clay|40215|6|Mentioned|p56|||||||||
1918|Blanchetown Clay|40380|6|Mentioned|p221|||||||||
1918|Blanchetown Clay|40597|6|Mentioned|Fig.3|||||||||
1918|Blanchetown Clay|40779|6|Mentioned|Fig.2|||||||||
1918|Blanchetown Clay|40820|5|Briefly described|p141|||||||||
1918|Blanchetown Clay|41206|5|Briefly described|p370|||||||||
1918|Blanchetown Clay|41478|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|41537|6|Mentioned|p350|||||||||
1918|Blanchetown Clay|41848|4|Described|p358|||Includes Bungunnia Limestone and Irymple Member. Age: Pleistocene.||||||20-OCT-08
1918|Blanchetown Clay|41868|6|Mentioned|p552|||||||||
1918|Blanchetown Clay|42125|5|Briefly described|p139|||||||||
1918|Blanchetown Clay|42130|6|Mentioned|Fig.3 P265|||||||||
1918|Blanchetown Clay|42131|5|Briefly described|p287|||||||||
1918|Blanchetown Clay|42132|6|Mentioned|p295|||||||||
1918|Blanchetown Clay|42134|6|Mentioned|Fig.3 P335|||||||||
1918|Blanchetown Clay|42137|6|Mentioned|Fig.2 P368|||||||||
1918|Blanchetown Clay|42389|5|Briefly described|p71|||||||||
1918|Blanchetown Clay|42443|6|Mentioned|p4|||||||||
1918|Blanchetown Clay|42499|5|Briefly described|Map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42509|5|Briefly described|p2|||||||||
1918|Blanchetown Clay|42510|5|Briefly described|p35|||||||||
1918|Blanchetown Clay|42512|6|Mentioned|p68|||||||||
1918|Blanchetown Clay|42513|6|Mentioned|p98|(IV) A||||||||13-MAY-13
1918|Blanchetown Clay|42514|6|Mentioned|p116|||||||||
1918|Blanchetown Clay|42515|6|Mentioned|p134|||||||||
1918|Blanchetown Clay|42516|6|Mentioned|p152|||||||||
1918|Blanchetown Clay|42518|5|Briefly described|p185|||||||||
1918|Blanchetown Clay|42519|6|Mentioned|p205|||||||||
1918|Blanchetown Clay|42592|6|Mentioned|p280|||||||||
1918|Blanchetown Clay|42717|5|Briefly described|map legend|Pleistocene||||||||
1918|Blanchetown Clay|42720|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42813|5|Briefly described|p25|||||||||
1918|Blanchetown Clay|42827|4|Described|p358|||||||||
1918|Blanchetown Clay|42867|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|42881|4|Described|Fig.3, P84|||||||||
1918|Blanchetown Clay|42966|1|Redefined|p205|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|43052|5|Briefly described|Table 2.1|||||||||
1918|Blanchetown Clay|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Sandy clay. Overlain by Bungunnia Limestone.||||||25-MAY-05
1918|Blanchetown Clay|43073|5|Briefly described|p17,Table 4|||||||||
1918|Blanchetown Clay|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
1918|Blanchetown Clay|43655|5|Briefly described|p40-846|||||||||
1918|Blanchetown Clay|43669|4|Described|p8-9|||||||||
1918|Blanchetown Clay|43682|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|43791|6|Mentioned|p372, Fig1|||||||||
1918|Blanchetown Clay|43804|6|Mentioned|Fig.2,p49|||||||||
1918|Blanchetown Clay|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Interfingers with Chowilla Sand. Thickness: 20m. Geological Province: Murray Basin. ||||||
1918|Blanchetown Clay|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Lacustrine deposits - poorly cosolidated to friable, well-laminated, green-grey, red-brown clay; silty, sandy, calcareous and gypsiferous.||||||03-FEB-09
1918|Blanchetown Clay|44191|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|||||||
1918|Blanchetown Clay|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
1918|Blanchetown Clay|49040|6|Mentioned|p12|||||||||
1918|Blanchetown Clay|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Fluvial: clayey sand, sandstone, sand.||||||11-JAN-10
1918|Blanchetown Clay|60540|5|Briefly described|p1000 Fig.2,p1000,p1009 Fig.5,|Pleistocene|Pliocene||||||Lacustrine clay.|
1918|Blanchetown Clay|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Sandy clay. Overlain by: Bungunnia Limestone.||||||
1918|Blanchetown Clay|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Sandy clay. Underlies Bungunnia Limestone.||||||01-JUN-05
1918|Blanchetown Clay|61155|5|Briefly described|p18|Late Pliocene|Late Pliocene|Overlies Loxton-Parilla Sands in central area of basin. Variably overlain by Monoman Formation, Lowen Sand, Woorinen Formation and Shepparton Formation. Age: ~2.0Ma. Geological Province: Murray Basin.||||||03-MAR-10
1918|Blanchetown Clay|61207|5|Briefly described|p280 Fig. 2|Pleistocene|Late Pliocene|Lacustrine sediments. Overlies Loxton-Parilla Sands. Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Lacustrine clays. Geological Province: western Murray Basin.||||||
1918|Blanchetown Clay|61822|5|Briefly described|p107|Pleistocene|Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61964|5|Briefly described|p161|||Overlies the Pliocene "Karoonda surface". Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Deposited in fluvio-lacustrine environment, within a shallow lake.||||||
1918|Blanchetown Clay|63893|5|Briefly described|p191, p185, p184|||Fluvial. With Loxton-Parilla Sands, underlies lowest units of Shepparton Formation. With Loxton-Parilla Sands, underlies bentonite deposits. Geol Prov: Murray Basin.||||||
1918|Blanchetown Clay|64961|5|Briefly described|p259|Quaternary|Quaternary|First formally defined by Firman (1973). Overlain by Bungunnia Limestone; unconformably overlies Karrona Surface over Loxton-Parilla Sand in central/eastern part of basin. Thickness is variable: <40m; typically 1-10m. Geol.province: Murray Basin.||||||10-NOV-10
1918|Blanchetown Clay|65552|5|Briefly described|p5 Fig.3, p6, p23 App.2|Late Pliocene|Late Pliocene|Murray Basin unit. Contains minor gypsum. Overlies Loxton Sands, Parilla Sand, Loxton-Parilla Sands and Norwest Bend Formation. Underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
1918|Blanchetown Clay|65901|6|Mentioned|p181|||May be correlative with possible Pooraka Formation sediments at River Glen Marina, Murray River.||||||
1918|Blanchetown Clay|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Firman 1973.||||||
1918|Blanchetown Clay|66287|5|Briefly described|p25 Fig. 2, p28, 31,33, 42, Fig 4,5,7|Late Pliocene|Late Pliocene|Palaeomag studies on clays from base of unit constrain minimum age for underlying Loxton-Parilla Sands to between 3.4 and 2.4 Ma. Part of the Lake Bungunnia sedimentary fill.||||Overlies the Loxton-Parilla Sands in places.||20-APR-12
1918|Blanchetown Clay|67179|4|Described|p581, p584|Calabrian|Gelasian|Deposited in a large freshwater lake (Lake Bungunnia) due to damming of ancient Murray River in the Late Pliocene (Brown and Stevenson 1991, Cupper et al. 2003). Late Pliocene-Quaternary.|ca 2.4 - 1.2 Ma (McLaren et al. 2009).|||Overlies the Loxton Sand in NW Murray Basin.||28-MAY-13
1918|Blanchetown Clay|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
1918|Blanchetown Clay|68116|5|Briefly described|Appendix, Maps 1-11, 14.|Pleistocene|Pliocene|Early Pleistocene minimum age.|||||Laminated greenish-grey and red-brown clay and silty clay, locally calcareous and gypsiferous; minor interbedded quartz sand, ostracod sand; contains calcareous, gypsiferous and siliceous nodules.|
1918|Blanchetown Clay|68189|6|Mentioned|p27 Tb.3.2|||||||Possibly overlain by the Shepparton Formation?||
1918|Blanchetown Clay|68194|6|Mentioned|p24|Pliocene|Pliocene|Murray Basin.||Unit in Wunghnu Group.||||
1918|Blanchetown Clay|68548|5|Briefly described|p13|Pleistocene|Pliocene|Late Pliocene to Early Pleistocene.||||Is overlain by Bungunnia Limestone.|Lacustrine clays.|
1918|Blanchetown Clay|68715|6|Mentioned|p31 Fig.5|Ionian|Zanclean|Murray Basin.||||||
1918|Blanchetown Clay|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Woorinen Formation. Underlain by the Loxton Sand.||
1918|Blanchetown Clay|70718|5|Briefly described|p25, p26,  p129|Quaternary|Quaternary|Fine grained lacustrine deposits in Lake Bungunnia.||||Disconformably overlies Loxton Sand.||
1918|Blanchetown Clay|71248|2|Defined|p1,2||Pleistocene|||||||
1918|Blanchetown Clay|72445|5|Briefly described|App.7 p7 Fig.4, p7.|Quaternary|Pliocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). Described, along with Loxton-Parilla Sands, Shepparton Formation, as fluvio lacustrine.||||Shown as unconformably overlying Loxton-Parilla Sands and partially equivalent to Bungunnia Limestone.||
1918|Blanchetown Clay|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Alluvial and lacustrine clay.|
1918|Blanchetown Clay|73228|4|Described|p50-53, p55-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluviolacustrine and coastal-shallow marine depositional environments. Identified in Cooltong 1, Loxton 1 and Overland Corner 1 drillholes. Capped by Bungunnia Limestone. Ooid-rich layers are commonly found in the upper portion; these sometimes define a transitional zone with the overlying unit.||||Underlain by Loxton Sand, Bookpurnong Formation, Karoonda Surface, upper Norwest Bend Formation, and Chowilla Sand.|Poorly laminated, or occasionally very finely laminated, clays and sandy clays, and minor quartz sand.|
1918|Blanchetown Clay|73229|5|Briefly described|p66-67, p70-72, p75|Pleistocene|Late Pliocene|Murray Basin. [Analysed using pXRF; see article].|||||Includes clay, greenish grey, sandy; limestone, thin; quartz sand; clay, green-grey, mottled, sandy.|
1918|Blanchetown Clay|73496|5|Briefly described|Map legend|Pleistocene|Pleistocene|||Wunghnu Group|||Lacustrine to fluvial silty or sandy clay; nonmagnetic; moderate to high K, Th, and U where not covered by other units; occupies distinct topographic lows typically less than 60 m ASL.|
1918|Blanchetown Clay|73505|4|Described|p2, p12-13, p36|Pliocene|Pliocene|Murray Basin. Deposited in Lake Bungunnia. Basal contact is partly erosional, upper contact is conformable. Low radiometric response. No detectable magnetic response.||Wunghnu Group||Overlies Parilla Sand, Calivil Formation|Lacustrine clay.|
1988|Blue Hills Sandstone|22746|6|Mentioned|Fig.3 p515|Ordovician|Ordovician|||||||
1988|Blue Hills Sandstone|22922|6|Mentioned|34|||||||||
1988|Blue Hills Sandstone|23282|2|Defined|p83|Early Silurian|Late Ordovician|Informally used as 'Policeman Well Sandstone' by Packham & Webby (1969). Krieg (1973) introduced Blue Hills Sandstone. The overlying 'Cartu beds' & 'Mintabie beds' are taken as synonyms. Age: Late Ordovician to Early Silurian 445-435Ma. of Munda Group.||||||
1988|Blue Hills Sandstone|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
1988|Blue Hills Sandstone|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|||||||
1988|Blue Hills Sandstone|23858|5|Briefly described|p917|Ordovician|Cambrian|Overlying Unit Mimili Formation. Geological Province: Officer Basin. Max. thickness: 800 m.||||||
1988|Blue Hills Sandstone|24067|5|Briefly described|p249|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
1988|Blue Hills Sandstone|24112|5|Briefly described|p254 Fig.2|Early Silurian|Late Ordovician|Of the Munda Group. Geological Province: Officer Basin||||||
1988|Blue Hills Sandstone|30544|6|Mentioned|p47|||||||||
1988|Blue Hills Sandstone|30807|6|Mentioned|p102|||Suggested map symbol.||||||
1988|Blue Hills Sandstone|30921|6|Mentioned|Map legend|Ordovician|Ordovician|Cambro-Ordovician.||||||
1988|Blue Hills Sandstone|30923|6|Mentioned|Map legend|Cambrian|Cambrian|Cambro-Ordovician||||||
1988|Blue Hills Sandstone|31457|6|Mentioned|p13|||||||||
1988|Blue Hills Sandstone|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
1988|Blue Hills Sandstone|33738|6|Mentioned|p58|||||||||
1988|Blue Hills Sandstone|35628|4|Described|Table 3|||||||||
1988|Blue Hills Sandstone|36096|6|Mentioned|Fig.3|||||||||
1988|Blue Hills Sandstone|36491|6|Mentioned|Fig.2|||||||||
1988|Blue Hills Sandstone|36895|6|Mentioned|p9|||||||||
1988|Blue Hills Sandstone|36920|6|Mentioned|Table 1|||||||||
1988|Blue Hills Sandstone|38022|6|Mentioned|Fig.4|||||||||
1988|Blue Hills Sandstone|38329|6|Mentioned|p194|||||||||
1988|Blue Hills Sandstone|40003|5|Briefly described|Table 15|||||||||
1988|Blue Hills Sandstone|40136|5|Briefly described|p18|||||||||
1988|Blue Hills Sandstone|40926|6|Mentioned|p12|||||||||
1988|Blue Hills Sandstone|42346|5|Briefly described|Fig.4 P82|Middle Ordovician||||||||
1988|Blue Hills Sandstone|43052|5|Briefly described|Fig.2.10|||||||||
1988|Blue Hills Sandstone|43085|5|Briefly described|Fig.7|||||||||
1988|Blue Hills Sandstone|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
1988|Blue Hills Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
1988|Blue Hills Sandstone|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
1988|Blue Hills Sandstone|43743|6|Mentioned|Fig.2,p33|Early Silurian|Late Ordovician|||||||
1988|Blue Hills Sandstone|44109|5|Briefly described|p22 Fig. 25|Ordovician|Ordovician|Geological Province: central Officer Basin.||||||
1988|Blue Hills Sandstone|44133|5|Briefly described|p40-41, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Overlies conformably the Indulkana Shale. ||||||07-NOV-08
1988|Blue Hills Sandstone|45149|6|Mentioned|p43|||See also Table 1 and P15.||||||
1988|Blue Hills Sandstone|49792|5|Briefly described|Fig.5|||||||||
1988|Blue Hills Sandstone|65313|6|Mentioned|p580 Fig. 8|Silurian|Silurian|Officer Basin.||Munda Group.||Overlies Indulkana Shale.||26-MAR-12
1988|Blue Hills Sandstone|71146|5|Briefly described|p6|Llandovery|Late Ordovician|Officer Basin.||Munda Group||Overlies the Indulkana Shale and the Mount Chandler Sandstone. Unconformably overlain by the Mimili Formation.|Sandstone.|
1988|Blue Hills Sandstone|72478|6|Mentioned|p8|Early Silurian|Late Ordovician|Officer Basin.|c. 445-437 Ma|Munda Group||Overlies the Indulkana Shale. Unconformably underlies the Mimili Formation and the Boorthanna Formation.||
1988|Blue Hills Sandstone|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Sandstone, red-brown, fine- to medium-grained, kaolinitic, with pebble beds; trace fossils, cross-bedded.|
1988|Blue Hills Sandstone|73235|6|Mentioned|p60|||||||||
2026|Blyth Dolomite|22889|4|Described|p33|Adelaidean|Adelaidean|Parent  - Emeroo Subgroup.  Former Parent Unit - River Wakefield Subgroup, see p33 for details.||||||
2026|Blyth Dolomite|32725|6|Mentioned|p6|||Geological map.||||||
2026|Blyth Dolomite|35328|6|Mentioned|p11|||Previously Blyth Dolomite Beds||||||
2026|Blyth Dolomite|37371|6|Mentioned|p382|||See also P377||||||
2026|Blyth Dolomite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
2026|Blyth Dolomite|40294|3|Fully described|p33|||||||||
2026|Blyth Dolomite|41404|4|Described|p92|||||||||
2026|Blyth Dolomite|42222|6|Mentioned|p13|||||||||
2026|Blyth Dolomite|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
2026|Blyth Dolomite|70819|5|Briefly described|p11, 13, 18-19|Neoproterozoic|Neoproterozoic|Western Clare Valley.||Emeroo Subgroup.||Gradationally overlies Anama Siltstone Member (Rhynie Sandstone). Is overlain by River Wakefield Formation.|Shallow-marine deposits: buff to grey coloured, stongly foliated, sheared and recrystallised to a sugary dolomite marble.|
2026|Blyth Dolomite|73188|6|Mentioned|p321|||Alma Fault scarp.||||||
2026|Blyth Dolomite|74367|6|Mentioned|p7 Fig.6|||||Emeroo Subgroup||||
2060|Boco Formation|22772|4|Described|p53,64-65,Table13.1|Cryogenian|Cryogenian|||||||
2060|Boco Formation|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Wendalpa Subgroup (Poolamacca Group). Dolomite, limestone, minor sandstone, contains stromatolites. Overlain by Wilangee Basalt. See also p53, p398 App. 1 Tb.A1.3.||||||
2060|Boco Formation|30261|4|Described|Table 1|||Willouran age||||||
2060|Boco Formation|30918|6|Mentioned|p80|||||||||
2060|Boco Formation|33004|6|Mentioned|p135|||||||||
2060|Boco Formation|34812|3|Fully described|p55|||||||||
2060|Boco Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2060|Boco Formation|35692|6|Mentioned|p23|||||||||
2060|Boco Formation|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
2060|Boco Formation|36733|6|Mentioned|Table 5|||||||||
2060|Boco Formation|37461|6|Mentioned|p335|||||||||
2060|Boco Formation|37854|6|Mentioned|Table 1|||||||||
2060|Boco Formation|37931|4|Described|p532|||||||||
2060|Boco Formation|38157|6|Mentioned|Table II|||||||||
2060|Boco Formation|39214|6|Mentioned|Table 1|||||||||
2060|Boco Formation|40294|6|Mentioned|p8|||||||||
2060|Boco Formation|41403|5|Briefly described|p50|||||||||
2060|Boco Formation|42222|5|Briefly described|p11|||||||||
2060|Boco Formation|42223|6|Mentioned|Fig.2 P36|||||||||
2060|Boco Formation|43265|5|Briefly described|Map Legend||Neoproterozoic|of Wendalpa Subgroup.||||||
2060|Boco Formation|43269|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
2060|Boco Formation|62724|5|Briefly described|p17 Fig. 4|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
2060|Boco Formation|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|Appears as Bocco Formation on p39.||Unit in Wendalpa Subgroup.||Is overlain by Wilangee Basalt.|Stromatolitic limestone.|
2060|Boco Formation|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Wendalpa Subgroup.||Overlies Christine Judith Conglomerate. Is overlain by Wilangee Basalt.|Quartz sandstone with well-rounded grains, minor chert, localised limestone and minor stromatolites.|
2060|Boco Formation|72461|6|Mentioned|p16 fig 9|||||||||
2176|Bonney Sandstone|7931|5|Briefly described|p98, p99 Fig. 2|Ediacaran|Ediacaran|Of the Pound Subgroup. Shallow marine to fluvial siliciclastics.||||||07-FEB-11
2176|Bonney Sandstone|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Parent -  Pound Subgroup.  Age - Ediacarian in text.||||||
2176|Bonney Sandstone|22927|5|Briefly described|40|||Geological province: Adelaide Geosyncline.||||||19-NOV-07
2176|Bonney Sandstone|23211|6|Mentioned|p44,46 Fig.2|||Of Pound Subgroup.||||||20-JAN-09
2176|Bonney Sandstone|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Wilpena Group. Correlate of Arumbera Sandstone.||||||19-NOV-07
2176|Bonney Sandstone|23287|6|Mentioned|Fig.2-4|||Age: Upper Ediacarian. Of Pound Subgroup. In the Adelaide Geosyncline.||||||19-NOV-07
2176|Bonney Sandstone|23804|6|Mentioned|p17|||||||||
2176|Bonney Sandstone|23854|5|Briefly described|p864|||Of Wilpena Group||||||
2176|Bonney Sandstone|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone. Of the Wilpena Group. Underlain by Wonoka Formation. Overlain by Rawnsley Quartzite.||||||20-JAN-09
2176|Bonney Sandstone|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Wonoka Formation. Overlain by the Rawnsley Quartzite. Geological Province: Adelaide Fold Belt.||||||19-NOV-07
2176|Bonney Sandstone|24484|5|Briefly described|p803 Fig. 3|Neoproterozoic|Neoproterozoic|Overlies the Puttapa Conglomerate. Overlain by the Rawnsley Quartzite.||||||
2176|Bonney Sandstone|24586|5|Briefly described|p51 Fig. 2, p52 Fig. 3|Adelaidean|Adelaidean|Of the Pound Subgroup ((Wilpena Group). Intertongues with Billy Springs Formation, and upper part of Wonoka Formation. Geological Province: Adelaide Geosyncline.||||||20-JAN-09
2176|Bonney Sandstone|36011|6|Mentioned|p13|||||||||
2176|Bonney Sandstone|37015|6|Mentioned|Fig.2|||||||||
2176|Bonney Sandstone|37627|6|Mentioned|p186|||||||||
2176|Bonney Sandstone|38157|6|Mentioned|Table V|||Also mentioned in Table XI.||||||
2176|Bonney Sandstone|38970|6|Mentioned|p105|||Upgrade of Bonney Sandstone Member.||||||
2176|Bonney Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
2176|Bonney Sandstone|41236|5|Briefly described|p63|||||||||
2176|Bonney Sandstone|41424|5|Briefly described|p299|||||||||
2176|Bonney Sandstone|41429|3|Fully described|p242|||||||||
2176|Bonney Sandstone|41794|6|Mentioned|Fig.2|||||||||
2176|Bonney Sandstone|41801|6|Mentioned|p219|||||||||
2176|Bonney Sandstone|42028|6|Mentioned|p137|||||||||
2176|Bonney Sandstone|42095|5|Briefly described|Fig.3 P31|||||||||
2176|Bonney Sandstone|42222|6|Mentioned|p20|||||||||
2176|Bonney Sandstone|42240|6|Mentioned|Fig.2 P165|||||||||
2176|Bonney Sandstone|42241|5|Briefly described|p179|||||||||
2176|Bonney Sandstone|43052|5|Briefly described|p194,Table 6.1|||Of Pound Subgroup.||||||19-NOV-07
2176|Bonney Sandstone|43622|6|Mentioned|p38|Neoproterozoic||||||||
2176|Bonney Sandstone|43650|6|Mentioned|Fig.2,p444|||||||||
2176|Bonney Sandstone|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Wilpena Group||||||12-JUL-16
2176|Bonney Sandstone|60418|5|Briefly described|p134 Fig.1|Neoproterozoic|Neoproterozoic|Of Pound Group.||||||19-NOV-07
2176|Bonney Sandstone|60889|6|Mentioned|p250 Fig.7|||||||||
2176|Bonney Sandstone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Pound Subgroup. Red micaceous siltstone and sandstone parasequences, mud clasts and mudcracks.||||||23-DEC-09
2176|Bonney Sandstone|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||10-MAY-07
2176|Bonney Sandstone|61308|5|Briefly described|p7|Proterozoic|Proterozoic|||||||
2176|Bonney Sandstone|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||
2176|Bonney Sandstone|61732|3|Fully described|p4 Fig. 3, p48-49|Marinoan|Marinoan|Of Pound Subgroup (Wilpena Group). Contains Ediacaran Member. Overlies Wonoka Formation; overlain by Rawnsley Quartzite. Age: 556+/-24Ma. Geol.Prov: Adelaide Rift Complex. See also p5 Tb. 1||||||07-FEB-11
2176|Bonney Sandstone|62085|6|Mentioned|p20 fig 5|Ediacaran|Ediacaran|||Wilpena Group||||
2176|Bonney Sandstone|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Wilpena Group.||Overlies Wonoka Formation. Is overlain by Rawnsley Quartzite.|Red sandstone.|
2176|Bonney Sandstone|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Of Pound Group. Includes Patsy Hill Member.||||||
2176|Bonney Sandstone|63569|6|Mentioned|p118 Fig. 2|Neoproterozoic|Neoproterozoic|||Unit in Pound Group.|Includes Patsy Hill Member.|||
2176|Bonney Sandstone|64455|4|Described|p140, p138 Fig. 1|Early Cambrian|Early Cambrian|Of Pound Subgroup. Age: 556+/-24Ma (Preiss, 2000. SHRIMP). Contains rare, simple surface trace fossils. Pink, red sandstone, dark mauve siltstone. Horizontal burrows.||||||29-JAN-09
2176|Bonney Sandstone|64460|5|Briefly described|p197, p198|||Overlain by Chase Quartzite Member of Rawnsley Quartzite. Maroon-brown sandstone. See p197 for more lithological information.||||||
2176|Bonney Sandstone|65892|4|Described|p16, p28, p32-34, p39. |Ediacaran|Ediacaran|Flinders Ranges. Informally called "Red Pound" to distinguish it from overlying "White Pound", i.e. Rawnsley Quartzite.|c.560 Ma.|Unit in Wilpena Group.||Overlies Wonoka Formation. Is overlain by Rawnsley Quartzite.|Flaggy, red to brown, silty and feldspathic sandstone.|
2176|Bonney Sandstone|65925|5|Briefly described|Appendix 2.||||||||Sandstone, fine to medium grained, occasionally coarse, flaggy to medium bedded, silty and feldspathic, cross bedded, ripple marks, small scale slumps, mudcracks, intraclasts; siltstone; quartzite.|
2176|Bonney Sandstone|66569|5|Briefly described|p860, p861 fig.2, p862,|Ediacaran|Ediacaran|Of Wilpena Group; shallow marine and estuarine sediments; underlies Rawnsley Quartzite; overlies Wonoka Formation; youngest Ar-Ar age for detrital muscovite of 601+/-17 Ma.||||||
2176|Bonney Sandstone|67030|5|Briefly described|p409,  Fig. 2|Ediacaran|Ediacaran|Age from detrital muscovites: 601 +/- 17 Ma (Ar-Ar, Haines et al. 2004). Age from zircon grain: 556 +/- Ma 24 Ma (U-Pb, Ireland et al. 1998). May indicate penecontemporaneous volcanism.|556 +/- 24 Ma.|||Overlies the Wonoka Formation, underlies the Rawnsley Quartzite.||26-APR-12
2176|Bonney Sandstone|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of the Pound Subgroup.||Overlain by Chace Quartzite Member (Rawnsley Quartzite). Underlain by Wonoka Formation.||
2176|Bonney Sandstone|67620|5|Briefly described|p2, 5|Ediacaran|Ediacaran|Adelaide Rift Complex. Contains the microbial mat structure named Arumberia.||Pound Subgroup.||Overlies Wonoka Formation. Is overlain by Rawnsley Quartzite. Correlates with Yurabi Formation (WA).||
2176|Bonney Sandstone|68030|3|Fully described|p239-240|Ediacaran|Ediacaran|Flinders Ranges. 300-400 m thick in the central Flinders Ranges. Base of the Ediacaran Member represents a sequence boundary with 5-10m deep channels and regional 1-5km wide, 50-250m deep canyon incisions into Chace Quartzite Member, and locally well into Bonney Sandstone. Canyons were likely cut and filled syndepositionally with Ediacara Member.||Unit of Pound Subgroup.||Overlain unconformably by Chace Quartzite Member, infilled with Ediacara Member. Underlain unconformably by Wonoka Formation.|Transgressive shallow marine sandstone and carbonates at the base, overlain by deeper water siltstone and fine sandstone shallowing and coarsen upward, and alluvial, red, poorly sorted, sandy mudstones.|
2176|Bonney Sandstone|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Pound Subgroup.||||
2176|Bonney Sandstone|68244|6|Mentioned|p666|Neoproterozoic|Neoproterozoic|Southern Australia. ContainsTungussia julia, a stromatolite biostratigraphic marker that correlates  Bonney Sandstone to Julie Formation (Central Australia) and Egan Formation.||||||
2176|Bonney Sandstone|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Wilpena Group||Underlain by Wonoka Formation. Overlain by Rawnsley Quartzite.|Includes sandstone and siltstone.|
2176|Bonney Sandstone|68270|5|Briefly described|p683,684|Ediacaran|Ediacaran|Adelaide Rift Complex. 556+24 Ma maximum depositional age (detrital zircon), Bonney Sandstone (Ireland et al. 1998).||Unit of Wilpena Group.||||
2176|Bonney Sandstone|68271|5|Briefly described|p695-696|||Adelaide Rift Complex. One detrital zircon indicating an age of 556+\-24 Ma (Ireland et al.1998), representing an imprecise maximum depositional time. Similar lithology and taxa to Arumbera Sandstone.|||Includes Patsy Hill Member.|Underlain by Wonoka Formation.||
2176|Bonney Sandstone|68731|6|Mentioned|p212|Neoproterozoic|Neoproterozoic|Late Neoproterozoic age. A detrital zircon age population with a major peak in the range 1100-1180 Ma has been found for a sample from the Bonney Sandstone (Ireland et al. 1998).||||||
2176|Bonney Sandstone|69019|6|Mentioned|p61.|Neoproterozoic|Neoproterozoic|Mawson's (1938) informal subdivision of his Pound Quartzite into a lower red sandstone member and an upper white quartzite member was formalised by Forbes (1971) who defined them as Bonney Sandstone Member and Rawnsley Quartzite Member respectively. These were later (Jenkins, 1975) elevated to Formation status (within the Pound Subgroup).||||||
2176|Bonney Sandstone|70031|5|Briefly described|p245|Ediacaran|Ediacaran|Adelaide Geosyncline. ||Unit of Pound Subgroup.||Lower unit of Pound Subgroup. Overlain by Rawnsley Quartzite. Underlain by Wonoka Formation.||
2176|Bonney Sandstone|70082|6|Mentioned|p2,13|Ediacaran|Ediacaran|Flinders Ranges. Contains red beds.||||||
2176|Bonney Sandstone|70334|6|Mentioned|p78|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Deposited in coastal sand flats or a tidal delta environment.||||||
2176|Bonney Sandstone|70382|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex.||||||
2176|Bonney Sandstone|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Pound Subgroup.|||Fine- to medium-grained, occasionally coarse, sandstone, flaggy to medium-bedded, silty and feldspathic, cross-bedded, ripple marks, small-scale slumps, mudcracks, intraclasts; siltstone; quartzite.|23-JAN-19
2176|Bonney Sandstone|70407|5|Briefly described|p111|||Sequence boundary at base.||Of Pound Subgroup||Wonoka Formation grades up into this unit near Mount Goddard, but the contact is disconformable near diapirs.||
2176|Bonney Sandstone|70416|6|Mentioned|p75|||The basal part comprises the former Wonoka Formation.||||||
2176|Bonney Sandstone|70744|5|Briefly described|p941|Neoproterozoic|Neoproterozoic|Delamerian Orogen; northern Flinders Ranges. Contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga).||||||
2176|Bonney Sandstone|70790|4|Described|p257-273|Ediacaran|Ediacaran|Adelaide Rift Complex. The type locality is in Bunyeroo Gorge. Measured section and photographs. Detailed facies analysis and interpretation. Part of a progradational, fluvially dominated deltaic system with minor wave and tidal influences.|556 +/- 24 Ma (maximum depositional age).|Wilpena Group.||Overlies Wonoka Formation. Is overlain unconformably by Chace Member (Rawnsley Quartzite). Equivalent to Punkerri, Arumbera Sandstones.|A lower 75m interval of interbedded fissile silty mudstones and very fine-grained sandstone, then 75m of amalgamated sandstones, topped by c.85m of muddy siltstones interbedded with sandstones.|23-JAN-19
2176|Bonney Sandstone|70839|5|Briefly described|p342-343|Ediacaran|Ediacaran|Of Adelaide Rift Complex. Mid-Ediacaran age (c. 560 Ma) based on position within biostraphically dated succession (Preiss, 2000).|c. 560 Ma|||||
2176|Bonney Sandstone|71250|5|Briefly described|p69-70|Ediacaran|Ediacaran|Central Flinders Ranges.||Pound Subgroup.||Overlies Wonoka Formation. Is overlain disconformably by Chace Quartzite Member and locally Ediacara Member (Rawnsley Quartzite).|Red siliciclastics.|
2176|Bonney Sandstone|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shallow deltaic and tidal environments. Shown in image on p1, 'Northern rim of Wilpena Pound from Bunyeroo Valley lookout' (photo 042165).||||Overlies Wonoka Formation and underlies Wilkawillina Limestone, Rawnsley Quartzite.|Red mica-rich silty sandstone; ripple marks, mud-cracks impressions and mud-cracks. Repeated 20-30 m cycles of siltstone to thick cross-bedded sandstone are common.|
2176|Bonney Sandstone|72451|6|Mentioned|p4 Fig. 1|||Shown only as Bonney sst.||||||
2176|Bonney Sandstone|72489|6|Mentioned|p4, p5 Fig.4|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Only shown on p13 Fig.10. Temporal relationships diagram.|||Includes Patsy Hill Member.|Partially overlies Wonoka Formation.|Includes sandstone.|
2176|Bonney Sandstone|73059|6|Mentioned|p1061|||Contains late Mesoproterozoic detrital zircons.||Adelaide Rift Complex.||||
2176|Bonney Sandstone|73222|5|Briefly described|p6-8, p11-12, p14, p16, p18, p23-24, p26|Ediacaran|Ediacaran|Adelaide Rift Complex.||Pound Subgroup, Wilpena Group, Heysen Supergroup|Patsy Hill Member|||
2176|Bonney Sandstone|73236|6|Mentioned|p40|||Flinders Ranges.||Wilpena Group, Heysen Supergroup||||
2176|Bonney Sandstone|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||||Overlies the Wonoka Formation, underlies the Ediacara Member||
2176|Bonney Sandstone|73264|6|Mentioned|p1386, p1387 Fig.10|||Adelaide Rift Complex. Zircon populations at 1500-2100 Ma, main zircon peak at 1764 Ma, secondary population at 800-1300 Ma with peak at 1109 Ma.||||||
2176|Bonney Sandstone|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p19-20, p22-23|Ediacaran|Ediacaran|Detrital muscovite age of 601+/-17 Ma may approach true age of deposition (Haines et al., 2004). See also p14, p16-17.|579+/-32 Ma LA-ICP-MS detrital zircon MDA|Pound Subgroup||||
2203|Bookpurnong Formation|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|See also Bookpurnong beds. Geological Province: Murray Basin.||||||13-AUG-07
2203|Bookpurnong Formation|22773|5|Briefly described|Fig24.8p352,354|Pliocene|Miocene|||||||
2203|Bookpurnong Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Late Miocene|Passes laterally into the Loxton and Parilla Sands. Geological Province: Murray Basin.||||||
2203|Bookpurnong Formation|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
2203|Bookpurnong Formation|23768|5|Briefly described|p27, p33, p47|||Geological Province: Murray Basin. Overlain by Norwest Bend Formation.  see also p28 Fig. 5.||||||11-SEP-09
2203|Bookpurnong Formation|24551|6|Mentioned|p450|||Supersedes Bookpurnong Beds||||||
2203|Bookpurnong Formation|30996|4|Described|p30|||||||||
2203|Bookpurnong Formation|41511|5|Briefly described|p18|||See also mention p20.||||||29-JUL-08
2203|Bookpurnong Formation|42127|5|Briefly described|p222|||||||||
2203|Bookpurnong Formation|42966|6|Mentioned|p152|||Synonym for Bookpurnong beds||||||
2203|Bookpurnong Formation|44133|5|Briefly described|p161, 152 Fig. 10.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin. ||||||
2203|Bookpurnong Formation|60540|5|Briefly described|p999,p1000 Fig.2,p1002 Fig.4,p1020 |Pliocene|Pliocene|Brown and Stephenson (1991), Rogers et al. (1995). Previously Bookpurnong Beds. Zanclean age, based on biostratigraphy? Low-energy, shallow-marine deposits.||||Conformably overlain by the Loxton Sand. Onlaps [overlies] the Murray Supergroup.|Variable fossiliferous, shallow marine, glauconitic clays and marls.|06-FEB-18
2203|Bookpurnong Formation|60785|6|Mentioned|p184 Fig.1, p196.  |Zanclean|Zanclean|South Australia. Has yielded fossil cetacean elements.||||||
2203|Bookpurnong Formation|61185|5|Briefly described|p58|Late Miocene|Late Miocene|Name used interchangeably with Bookpurnong Beds. Marine sediments. Geological Province: Murray Basin.||||||07-FEB-11
2203|Bookpurnong Formation|63887|5|Briefly described|p20, p21, p21 Fig. 1|Pleistocene|Late Miocene|Shallow marine depositional environment. Consists of clays with occasional sandy, silty, carbonaceous and calcareous beds.||||||
2203|Bookpurnong Formation|64237|5|Briefly described|p19 Fig.2b|Late Miocene|Late Miocene|Superseded Bookpurnong Beds of Lawrence (1961) - revised by Rogers et al (1995). Overlies the Murray Group.||||||29-JUL-08
2203|Bookpurnong Formation|66286|5|Briefly described|p179, pp189-190.|Pliocene|Miocene|Refers to the mud-rich sediments underlying the Loxton-Parilla sands. Deposited during a marine transgression-regression into the Murray Basin. Lacks high carbonate, fossil and glauconite content of other occurrences. 1.5 - 3m blanket under Wimmera Plain.||||Overlies Loddon River Group. Is overlain by or interfingers with Loxton-Parilla sands.|Shallow marine clays and marls; grey to brown muds; pinnate cracks filled with kaolinite common; local goethite-rich lenticular mottles.|
2203|Bookpurnong Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||||||
2203|Bookpurnong Formation|68548|5|Briefly described|p13|Pliocene|Miocene|Late Miocene to Early Pliocene.||||Overlain by the Loxton Sand.|Succession of variably fossiliferous, shallow marine, glauconitic clays and marls.|
2203|Bookpurnong Formation|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||||||
2203|Bookpurnong Formation|68716|5|Briefly described|p39 Fig.3, p40, p43, p44 Fig.7|||Aquitard - extremely low permeability.||||Overlain by the Loxton Sand and Monoman Formation. Underlain by the Pata Formation.||
2203|Bookpurnong Formation|71593|4|Described|p52-p54|Pliocene||This unit is only a few metres thick generally.||||Overlain by the Loxton Sand.|Clay to marl with occasional shell fragments or mica flakes.|
2203|Bookpurnong Formation|72445|5|Briefly described|App.1; App.2.|Pliocene||App.2 is a .csv format file . Identified in Stavely 09,11,14. Accidently assigned to Murray Group in Stavely 11? Shown as ungrouped elsewhere. Minimum age from overlying units.||||Overlain by Calivil Formation, Loxton Sand (sharp contact). Overlies Renmark Group (gradational contact), Murray Group (sharp contact).|Includes glauconitic marl, fine sand and silt; marl with lesser sand and mud; silt with marl and limestone.|
2203|Bookpurnong Formation|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Marl, clay, sand.|
2203|Bookpurnong Formation|73228|4|Described|p50, p52-58, p62|Early Pliocene|Late Miocene|Murray Basin. Shallow marine, lower shoreface depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1 and Overland Corner 1 drillholes. Outcrops are limited to a small area; type section near Loxton, SA. Subsurface thickness of up to 50 m. Subsurface distribution is a broad arc in the deeper, central sections of the Murray Basin. Considered to have formed on the lower-shoreface (offshore) following major marine inundation of the area.||||Underlain by Murray Group. Overlain by Loxton Sand and Blanchetown Clay.|Brown or greenish grey marl, silty clay and minor fine sand, with relatively high carbonate contents. Includes glauconite, shell/mollusc fragments and bryozoa.|
2203|Bookpurnong Formation|73229|5|Briefly described|p66-67, p70-72, p74-75|Early Pliocene|Late Miocene|Murray Basin. [Analysed using pXRF; see article]. Shallow marine.|||||Marl; silty clay; minor fine-grained sand, glauconitic.|
2291|Boorthanna Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Arkaringa Basin||||||
2291|Boorthanna Formation|22613|6|Mentioned|p17|Permian|Carboniferous|||||||
2291|Boorthanna Formation|22614|5|Briefly described|map|Permian|Carboniferous|||||||
2291|Boorthanna Formation|22922|6|Mentioned|33 fig 2|||||||||
2291|Boorthanna Formation|23054|4|Described|p17-9,35|Asselian||||||||
2291|Boorthanna Formation|23282|6|Mentioned|p84 Fig 6.2|||of Arckaringa Basin.||||||
2291|Boorthanna Formation|23288|6|Mentioned|Fig.5|||of Marla area.|||||Glacigene sequence with more marine facies towards the top.|29-MAR-21
2291|Boorthanna Formation|23829|5|Briefly described|p370|Permian|Permian|Geological Province: Arckaringa Basin.||||||
2291|Boorthanna Formation|24112|5|Briefly described|p254 Fig.2, p257 Tb.1, p260|Early Permian|Early Silurian|||||||
2291|Boorthanna Formation|24175|6|Mentioned|p15|Permian|Permian|||||||
2291|Boorthanna Formation|24321|5|Briefly described|Map legend|Permian|Permian|||||||11-JAN-10
2291|Boorthanna Formation|30511|6|Mentioned|p47|||||||||
2291|Boorthanna Formation|30544|6|Mentioned|p52|||||||||
2291|Boorthanna Formation|30924|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
2291|Boorthanna Formation|32204|4|Described|p5|||Details of Refraction Survey & P8 L.Perm.||||||
2291|Boorthanna Formation|33523|4|Described|p21|||||||||
2291|Boorthanna Formation|33525|2|Defined|p4|Permian|Permian|||||||
2291|Boorthanna Formation|33971|6|Mentioned|p34|||Similar to Crown Pt. Fm.||||||
2291|Boorthanna Formation|33976|6|Mentioned|Fig.2|||Correlative? Crown Point Formation.||||||
2291|Boorthanna Formation|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
2291|Boorthanna Formation|35315|6|Mentioned|p4|||||||||
2291|Boorthanna Formation|35845|6|Mentioned|Fig.25|||||||||
2291|Boorthanna Formation|36491|6|Mentioned|Fig.2|||||||||
2291|Boorthanna Formation|36733|3|Fully described|p53|||See also P14.||||||
2291|Boorthanna Formation|36966|6|Mentioned|Fig.1|||||||||
2291|Boorthanna Formation|37851|6|Mentioned|p12|||||||||
2291|Boorthanna Formation|37855|6|Mentioned|p4|||||||||
2291|Boorthanna Formation|37917|3|Fully described|p469|||||||||
2291|Boorthanna Formation|38022|6|Mentioned|Fig.4|||||||||
2291|Boorthanna Formation|38604|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
2291|Boorthanna Formation|38605|4|Described|p17|||See also Table 3.||||||
2291|Boorthanna Formation|39265|6|Mentioned|Fig. 3|||||||||
2291|Boorthanna Formation|39352|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
2291|Boorthanna Formation|39904|6|Mentioned|p14|||||||||
2291|Boorthanna Formation|40637|6|Mentioned|Fig.2|||||||||
2291|Boorthanna Formation|40912|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous-Permian||||||
2291|Boorthanna Formation|41183|6|Mentioned|Fig.3 p308|||||||||
2291|Boorthanna Formation|41491|5|Briefly described|p168|||||||||
2291|Boorthanna Formation|41689|6|Mentioned|Table 1|||||||||
2291|Boorthanna Formation|41950|6|Mentioned|Fig.3 P4|||||||||
2291|Boorthanna Formation|42102|6|Mentioned|p86|||||||||
2291|Boorthanna Formation|42465|5|Briefly described|Map legend|||||||||
2291|Boorthanna Formation|42469|4|Described|p27|||||||||
2291|Boorthanna Formation|42546|5|Briefly described|Map legend|Permian|Carboniferous|||||||
2291|Boorthanna Formation|42547|5|Briefly described|Fig.24 P79|||||||||
2291|Boorthanna Formation|42723|5|Briefly described|map legend|Permian||||||||
2291|Boorthanna Formation|42736|5|Briefly described|map legend|Permian|Carboniferous|||||||
2291|Boorthanna Formation|42746|5|Briefly described|Fig.2 P4|||||||||
2291|Boorthanna Formation|43048|4|Described|Table 2.|||||||||
2291|Boorthanna Formation|43049|6|Mentioned|p21|||||||||
2291|Boorthanna Formation|43052|5|Briefly described|Table 2.1|||||||||
2291|Boorthanna Formation|43053|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arckaringa Basin.||||||25-MAY-05
2291|Boorthanna Formation|43258|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
2291|Boorthanna Formation|43298|6|Mentioned|Map Legend|Permian|Carboniferous|||||||
2291|Boorthanna Formation|43657|6|Mentioned|Fig.3,p4|Permian|Carboniferous|||||||
2291|Boorthanna Formation|43690|6|Mentioned|Fig.2,p157|||||||||
2291|Boorthanna Formation|43743|6|Mentioned|Fig.2,p33||Early Permian|||||||
2291|Boorthanna Formation|44109|5|Briefly described|p22 Fig. 27||Carboniferous|Geological Province: central Officer Basin.||||||
2291|Boorthanna Formation|44133|5|Briefly described|p44, 65 Fig. 8.3, 73|Permian|Carboniferous|Also listed as lower Boorthanna Formation. Geological Province: Arckaringa Basin. Overlain by Stuart Range Formation.||||||
2291|Boorthanna Formation|44289|5|Briefly described|Map Legend||Asselian|||||||
2291|Boorthanna Formation|44695|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
2291|Boorthanna Formation|44935|5|Briefly described|Map Legend|Permian|Carboniferous|Arckaringa Basin and Mulgathing Trough||||||
2291|Boorthanna Formation|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arcaringa Basin.||||||
2291|Boorthanna Formation|61108|5|Briefly described|map legend|Permian|Carboniferous|Glaciomarine, fluvioglacial and fluviolacustrine till, clay, silt, sand and gravel, indurated and coal-bearing in Ackaringa Basin. Geological Province: Arckaringa Basin.||||||
2291|Boorthanna Formation|62893|6|Mentioned|p18|||Arckaringa Basin.||||Equivalent to Coolardie Formation.||
2291|Boorthanna Formation|64696|5|Briefly described|p133 Fig.14|Permian|Permian|||||||
2291|Boorthanna Formation|65489|5|Briefly described|p137, p151|Permian|Permian|Arckaringa Basin. 420m thick.||||Is overlain by Stuart Range Formation.||
2291|Boorthanna Formation|66520|5|Briefly described|p11-12. |Permian|Permian|Gawler Craton. 283 m thick.||||Unconformably overlies basement rocks.|Glacial mudstone, fine sandy mudstone and fine sandstone.|
2291|Boorthanna Formation|69203|6|Mentioned|p12, p14, p24|Permian|Permian||||||Includes (basal) conglomerate.|
2291|Boorthanna Formation|69454|5|Briefly described|p38:4, 6|Asselian|Asselian|Arckaringa Basin.||||Correlated with Crown Point Formation (Pedirka Basin).||12-JUL-16
2291|Boorthanna Formation|69554|6|Mentioned|p131|Permian|Permian|Northern Gawler Craton.||||||
2291|Boorthanna Formation|69673|6|Mentioned|p153 fig 125|||||||Overlain by Stuart Range Formation||
2291|Boorthanna Formation|69946|3|Fully described|p2-3, p36, p38-41, p45|Asselian|Late Carboniferous|Townsend and Ludbrook (1975); replaces the informal Lake Phillipson beds of Ludbrook (1967). Type section is the interval 739.1 - 1158.2m in Boorthanna 1.  Diamictite shows distinctive gamma ray and neutron log signatures. Up to 419m thick. Arckaringa Basin. Appears as Boorthana Formation on p38.||||Unconformably overlies Observatory Hill, Cootanoorina Formations and Andamooka Limestone. Is overlain conformably by Stuart Range Formation. Equivalent to Merrimelia Formation, Tirrawarra Sandstone.|Basal thick, massive to crudely bedded diamictite, overlain by medium- to coarse-grained sandstone grading into siltstone or silty shale.|
2291|Boorthanna Formation|70938|5|Briefly described|p807-808, p815|||Arckaringa Basin.|||||Coarse clastic detritus.|
2291|Boorthanna Formation|71043|5|Briefly described|p106|||Gawler Craton.|||||Diamictite with shale intercalations.|
2291|Boorthanna Formation|71342|4|Described|Ch5 p2-p3, Ch5 p30|Early Permian|Late Carboniferous|Arckaringa Basin. Deposited in a glacial environment. Proposed by Townsend and Ludbrook (1975) to replace the informal Lake Phillipson beds of Ludbrook (1967). A type section is nominated in core from Boorthanna 1. Maximum thickness of 419m. See also Ch5 p36, Ch5 p38-p41, Ch5 p45, Ch11 p6.||||Unconformably overlies the Observatory Hill Formation and the Cootanoorina Formation. Intertongues with or is conformably overlain by the Stuart Range Formation.|Thick, massive to crudely bedded diamictite overlain by sandstone. The diamictite is sandy to bouldery, homogenous with scattered quartz and feldspar. The upper sandstone is medium to coarse-grained grading into siltstone or silty shale.|
2291|Boorthanna Formation|72476|6|Mentioned|p36 Fig.9|||Officer Basin. Time-temperature thermal history diagram.||||||
2291|Boorthanna Formation|72478|6|Mentioned|p6, p8, p25-27|Early Permian|Early Permian|Arckaringa Basin. See also Fig.7 p70.|c. 290 Ma-280 Ma|||Underlies the Stuart Range Formation. Unconformably overlies the Mimili Formation and the Blue Hills Sandstone.||29-MAR-21
2291|Boorthanna Formation|73099|5|Briefly described|Map legend.|Permian.|Late Carboniferous|Arckaringa Basin.||||Is overlain by Mount Toondina Formation.|Sandy and pebbly claystone and siltstone, clayey and silty very fine to very coarse sandstone with lithic fragments, conglomerate, minor carbonate.|
2291|Boorthanna Formation|73398|5|Briefly described|p4, 25, 28-29|Permian|Permian|Continental glacial environment.|<300 Ma.|||Is overlain unconformably by Cadna-owie Formation.|Diamictite.|
2298|Bopeechee Clay|30749|2|Defined|p3|middle Pleistocene|middle Pleistocene|See also P4||||||
2298|Bopeechee Clay|38068|6|Mentioned|p76|||||||||
2311|Borda Formation|22485|4|Described|p51 , Fig 2|Early Cretaceous|Early Cretaceous|informaly divided into upper and lower Borda Formation.||||||17-SEP-08
2311|Borda Formation|22663|5|Briefly described|S97-1 and 2 p2||Early Cretaceous|||||||01-MAR-10
2311|Borda Formation|24553|5|Briefly described|p37|||Geological Province: Duntroon Sub-basin. Marine sands. Contains thick shales which act as a seal.||||||07-FEB-11
2311|Borda Formation|42545|3|Fully described|p6|Barremian||||||||17-SEP-08
2311|Borda Formation|43026|5|Briefly described|Table 1,p586|||||||||
2311|Borda Formation|43814|6|Mentioned|Fig.3,p115|||||||||
2311|Borda Formation|44133|4|Described|p140|Albian|Barremian|Previously assigned to the Madura Formation. Conformably overlain by the Ceduna Formation. Conformably overlies Neptune Formation. Thickness: 1712m.||||||17-SEP-08
2311|Borda Formation|61544|5|Briefly described|p367 Fig.3, p374.|Albian|Berriasian|Ceduna and Duntroon Sub-basins, Bight Basin. Post-rift fluvio-deltaic source rocks, primarily with gas source potential.||||Overlies Neptune Formation. Is overlain by Ceduna Formation.||24-APR-17
2311|Borda Formation|63124|5|Briefly described|p72|||Paralic fluviolacustrine unit . Geological Province: Duntroon Basin. Equivalent to Eumeralla Formation.||||||
2350|Boston Bay Silcrete|29780|6|Mentioned|p50|||||||||
2350|Boston Bay Silcrete|32438|6|Mentioned|p42|||||||||
2364|Boucaut Volcanics|22631|6|Mentioned|p177|Cryogenian|Cryogenian|Age:780 Ma||||||
2364|Boucaut Volcanics|22889|4|Described|p33|||It is considered likely that the Boucaut Volcanics represents the same volcanic episode as the Jarrold Basalt Member of the Rhynie Sandstone.  The age of this event is given by a U-Pb zircon date of 777+/- Ma on rhyolite from the Boucaut Volcanics.||||||
2364|Boucaut Volcanics|23282|6|Mentioned|p54|||Of Adeliade Fold Belt. May be equivalant to Cadlareena Volcanics.||||||03-FEB-09
2364|Boucaut Volcanics|23557|5|Briefly described|p98|Cryogenian|Cryogenian|Age: 777+/-7Ma (SHRIMP U-Pb zircon).||||||
2364|Boucaut Volcanics|23562|5|Briefly described|p293|Neoproterozoic|Neoproterozoic|Age: 777+/-7 Ma.||||||
2364|Boucaut Volcanics|23869|5|Briefly described|p15 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
2364|Boucaut Volcanics|24400|5|Briefly described|p155 Tb.2, p156|Adelaidean|Adelaidean|Age: <777+/-7Ma. Of Burra Group.||||||
2364|Boucaut Volcanics|24401|5|Briefly described|p101|||Age: 777+/-7Ma. Geological Province: Adelaide Geosyncline||||||03-MAR-05
2364|Boucaut Volcanics|24509|5|Briefly described|p41 Fig. 2b|Neoproterozoic|Neoproterozoic|Rhyolite, andesite, trachyte and minor basalt.||||||03-APR-17
2364|Boucaut Volcanics|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
2364|Boucaut Volcanics|24599|6|Mentioned|p491|||Geological Province: Adelaide Fold Belt.||||||
2364|Boucaut Volcanics|24604|6|Mentioned|p903|||Geological Province: Adelaide Fold Belt.||||||
2364|Boucaut Volcanics|30808|2|Defined|p6|Cambrian|Cambrian|||||||
2364|Boucaut Volcanics|36534|6|Mentioned|p221|||||||||
2364|Boucaut Volcanics|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
2364|Boucaut Volcanics|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
2364|Boucaut Volcanics|41403|4|Described|p54|||||||||
2364|Boucaut Volcanics|42101|6|Mentioned|p84|||||||||
2364|Boucaut Volcanics|42222|4|Described|p34|||See also Table 1||||||
2364|Boucaut Volcanics|42223|4|Described|p34|||See also Table 1||||||
2364|Boucaut Volcanics|42224|6|Mentioned|p51|||||||||
2364|Boucaut Volcanics|42720|5|Briefly described|map legend|Willouran||||||||
2364|Boucaut Volcanics|42760|5|Briefly described|p3|||||||||
2364|Boucaut Volcanics|42813|3|Fully described|p14|||Of the Arkaroola Subgroup.||||||14-MAY-07
2364|Boucaut Volcanics|43052|5|Briefly described|p172,Table 6.1|||||||||
2364|Boucaut Volcanics|44133|5|Briefly described|p51 Fig. 7.18|Adelaidian|Adeladian|Rhyolite, minor basalt.||||||
2364|Boucaut Volcanics|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Emeroo Subgroup. Acid and basic volcanic rocks.||||||
2364|Boucaut Volcanics|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Acid and basic volcanic rock.||||||
2364|Boucaut Volcanics|61238|6|Mentioned|p48|Neoproterozoic|Neoproterozoic|Age: 777+/-7 Ma.||||||10-MAY-07
2364|Boucaut Volcanics|61732|5|Briefly described|p4 Fig. 3, p37|Torrensian|Torrensian|Of the Burra Group. Age: 777+/-7Ma. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
2364|Boucaut Volcanics|62453|5|Briefly described|p5 Fig. 3, 12 Fig. 8|Cryogenian|Cryogenian|Of the Burra Group. Age: 777 +/- 7Ma. Geological Province: Officer Basin.||||||
2364|Boucaut Volcanics|62664|5|Briefly described|p137, p139, p150.|Neoproterozoic|Neoproterozoic||783 +/- 42 Ma (Fanning et al. 1989)||||Rhyolite.|
2364|Boucaut Volcanics|63022|5|Briefly described|p1015|||Basal unit of the Burra Group. Age: >700Ma. ||||||
2364|Boucaut Volcanics|64647|5|Briefly described|p44|Torrensian|Torrensian|Age: 777+/-7Ma.||||||
2364|Boucaut Volcanics|64793|5|Briefly described|p283, p284 Fig.3, p285, p295|Neoproterozoic|Neoproterozoic|Of Adelaide Rift COmplex. Occurs at the base of, or within, Rhynie Sandstone.|777 +/- 7 Ma (Preiss, 1999).|||||03-APR-17
2364|Boucaut Volcanics|64796|5|Briefly described|p183 Fig.2, p184|Cryogenian|Cryogenian|Lies at the base or within Rhynie Sandstone.|777 +/- 7 Ma (Preiss, 2000).|Rhynie Sandstone||||
2364|Boucaut Volcanics|65363|6|Mentioned|p8, p37.|||Possible correlative of Keene Basalt in Western Australia.|777 +/- 7 Ma (Barovich et al. 2001).|||||
2364|Boucaut Volcanics|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of lowermost Burra Group. 777 +/-7 Ma U-Pb (Preiss & Cowley, 1999).||||||
2364|Boucaut Volcanics|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Of lowermost Burra Group. Dated at 777 +/- 7 Ma U-Pb (Preiss & Cowley, 1999)||||||
2364|Boucaut Volcanics|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Southeastern margin of Adelaide Province. Produced in the Boucaut Event, ME 27 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.775 Ma.|||||
2364|Boucaut Volcanics|67454|5|Briefly described|p564.|Neoproterozoic|Neoproterozoic|At or below the base of the Burra Group.|777 +/- 7 Ma (U-Pb SHRIMP zircon: Preiss 2000).|||||04-MAY-12
2364|Boucaut Volcanics|67536|5|Briefly described|Map Legend|Cryogenian|Cryogenian||ca. 777 +/- 7 Ma||||Felsic to mafic volcanic rocks.|
2364|Boucaut Volcanics|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
2364|Boucaut Volcanics|69666|6|Mentioned|p24, p26|Neoproterozoic|Neoproterozoic|S of Olary.||||||
2364|Boucaut Volcanics|70025|5|Briefly described|p27|||Adelaide Geosyncline. Bimodal volcanism coeval with sedimentation in the Smithton Basin in Tasmania.|777+\-7 Ma|||||
2364|Boucaut Volcanics|70657|5|Briefly described|p53, p56, p58, p69|Neoproterozoic|Neoproterozoic|Considered to represent early stages of extensional rifting of the Adelaide Geosyncline. Affected by NE-trending shearing (described). Appears as Boucaut volcanics on p69.|~777 Ma.|||Exteruded at or below the base of the Burra Group.|Rhyolitic volcanics.|
2364|Boucaut Volcanics|71001|6|Mentioned|p22|||Adelaide Rift Complex.|777 +/- 7 Ma (Barovich and Foden, 2000).||||Felsic.|
2364|Boucaut Volcanics|72601|6|Mentioned|p6|Tonian|Tonian|Geochronologic constraint by Preiss (2000); however, this date was later considered unreliable by Fanning and Link (2008).|777 +/- 7 Ma SHRIMP U-Pb|Burra Group||||
2364|Boucaut Volcanics|73090|5|Briefly described|Appendix.|Neoproterozoic|Neoproterozoic||||||Rhyolite, andesite and trachyte.|
2364|Boucaut Volcanics|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Rhyolite and minor basalt.|09-DEC-21
2364|Boucaut Volcanics|73188|6|Mentioned|p346|Neoproterozoic|Neoproterozoic|||||||
2364|Boucaut Volcanics|73262|4|Described|p580-587|Tonian|Tonian|Adelaide Rift Complex. Significant because this is one of the few volcanic units within the complex. Lies at the base of the Burra Group. Geochron is U-Pb zircon LA-ICP-MS crystallisation age. Marks the third phase of [Rodinian] rifting. The source of previous age data is obscure or unsupported [e.g., grey literature]. Occurs within the southeastern part of the Nackara Arc. The majority of outcrops are isolated and many are sheared along the northeast-trending Anabama Shear Zone. Authors do not consider this unit to be related to comparable rocks from [north?]western North America but possibly with those in the southwestern United States. [See article for whole rock geochemistry].|788 +/- 6 Ma|Burra Group, Warrina Supergroup|||Deformed and metamorphosed bimodal volcanics dominated by pale pink to grey rhyolite with less common amygdaloidal andesite and basalt.|
2364|Boucaut Volcanics|74367|5|Briefly described|p7 Fig.6, p8, p12, p18, p20|Tonian|Tonian|Of the Nackara Arc. Currently considered to be within or below the Rhynie Sandstone. Detailed mapping of type section area needed to clarify stratigraphic position. Ages of 783+/-42 Ma (Drexel and Preiss, 1993) and 777+/-7 Ma in Preiss (2000) have never been formally published with verifiable results; more recent analysis from Armistead et al., (2020). Current geochronology suggests volcanics within the Kooringa Member are equivalent. Initial correlation with Gairdner Dolerite proven to be incorrect, was based on an unpublished age of the Boucaut Volcanics (Drexel and Preiss, 1993).|ca. 788 Ma LA-ICP-MS U-Pb igneous zircon|Emeroo Subgroup|||Silicic.|
2453|Boxing Bay Formation|6111|6|Mentioned|p23 Fig.1, p24 Fig.2|Early Cambrian|Early Cambrian|.||||Overlies Emu Bay Shale.||17-SEP-12
2453|Boxing Bay Formation|22458|6|Mentioned|p527||Cambrian|||||||
2453|Boxing Bay Formation|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 500 m. Overlies Emu Bay Shale||||||17-FEB-11
2453|Boxing Bay Formation|22766|4|Described|Fig 2 p561|Early Cambrian|Early Cambrian|||||||
2453|Boxing Bay Formation|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin.||||||
2453|Boxing Bay Formation|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Toyonian|||||||
2453|Boxing Bay Formation|23818|5|Briefly described|p87 Fig.33, p105|Cambrian|Cambrian|Of the Kangaroo Island Group. Max. thickness: 3000 ft.||||||
2453|Boxing Bay Formation|33332|6|Mentioned|p11|||L.Camb.||||||
2453|Boxing Bay Formation|33471|6|Mentioned|Fig.1|||||||||
2453|Boxing Bay Formation|34612|5|Briefly described|p105|||Cambrian. Fig.33||||||
2453|Boxing Bay Formation|35255|6|Mentioned|Fig.8|||||||||
2453|Boxing Bay Formation|36198|6|Mentioned|Fig.I.2|||||||||
2453|Boxing Bay Formation|38873|4|Described|Table 3|||See also Fig.8||||||
2453|Boxing Bay Formation|40856|6|Mentioned|Fig.23.6|||||||||
2453|Boxing Bay Formation|41947|6|Mentioned|Fig.2 P17|||||||||
2453|Boxing Bay Formation|42225|6|Mentioned|p221|||||||||
2453|Boxing Bay Formation|42269|5|Briefly described|p336|||||||||
2453|Boxing Bay Formation|42272|6|Mentioned|p412|||||||||
2453|Boxing Bay Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 12, 17|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kangaroo Island Group.||||||
2453|Boxing Bay Formation|45102|6|Mentioned|p48|||||||||
2453|Boxing Bay Formation|62785|6|Mentioned|p43, p44 Fig.1|Middle Cambrian|Early Cambrian|North coast Kangaroo Island. Conformably overlies Emu Bay Shale.||||||20-MAR-12
2453|Boxing Bay Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Geological Province: Stansbury Basin. Pink and grey sandstone, red-brown arkose and carbonate-cemented polymict conglomerate. Clasts include micritic and archaeocyathid limestone, gneiss, granite, amphibolite and quartzite.||||||23-DEC-09
2453|Boxing Bay Formation|64829|6|Mentioned|p11-2|Cambrian|Cambrian|On Kangaroo Island.||||||07-FEB-11
2453|Boxing Bay Formation|65375|5|Briefly described|p33.|Middle Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies Emu Bay Shale.||
2453|Boxing Bay Formation|65625|4|Described|p126, 103|Middle Cambrian|Early Cambrian|Thickness: 2500ft.||Of Kangaroo Island Group.||Conformably overlies Emu Bay Shale.|Red quartzites and interbedded shales, flagstones and conglomerates. Red gniessic granite boulders.|13-APR-11
2453|Boxing Bay Formation|65667|5|Briefly described|p1222, p1223|Middle Cambrian|Early Cambrian|||||Conformably overlies Emu Bay Shale and underlies Bald Rock Beds.|Basal part comprises laminated arkosic sandstones containing trace fossils and abundant, large-scale soft-sediment slumping.|27-MAR-12
2453|Boxing Bay Formation|65892|6|Mentioned|p9 Fig.4, p22. |Middle Cambrian|Early Cambrian|North Coast of Kangaroo Island.||||Overlies Emu Bay Shale.||
2453|Boxing Bay Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kangaroo Island Group.||||
2453|Boxing Bay Formation|66761|4|Described|p244, 245-246, 248-249, 252-254|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Sharply but conformably overlies the Emu Bay Shale along the coast. At least 511m thickness reported but top not exposed. Abundant trace fossils.|||||Red brown feldspathic sandstone and arkose.|14-MAR-12
2453|Boxing Bay Formation|67344|5|Briefly described|p260 Fig.1, p261|Early Cambrian|Early Cambrian|Lower to Middle Cambrian age. ~ 510m thick. Abundant trace fossils and evidence of soft sediment slumping are suggestive of rapid sub-tidal deposition.||||Conformably overlies Emu Bay Shale.|Red-brown feldspathic sandstone and arkose.|
2453|Boxing Bay Formation|69372|6|Mentioned|p27 fig. 5, p34 fig. 12, p37|Cambrian|Cambrian|Forms bedrock in some regions. Pebbles interpreted to be from this unit are found in Cape Jervis Formation.||Kangaroo Island Group||Underlies Cape Jervis Formation.|Dominated by sandstone. Shows glaciation striations and textures.|
2453|Boxing Bay Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Pink and grey sandstone, red-brown arkose and carbonate-cemented polymict conglomerate. Clasts include micritic and archaeocyathid limestone, gneiss, granite, amphibolite, sandstone and quartzite.|
2453|Boxing Bay Formation|73247|5|Briefly described|p204-207, p209-210|||Part of the eastern succession of the Kangaroo Island Group. Contains abundant arthropod tracks and archaeocyaths in limestone clasts.||Kangaroo Island Group||Underlain by Emu Bay Shale. Equivalent to Smith Bay Shale and Kanmantoo Group.||
2453|Boxing Bay Formation|75071|6|Mentioned|p213|Cambrian|Cambrian|Kangaroo Island.||||||
2480|Braemar Iron Formation|23818|6|Mentioned|p34 Fig.8|||Geological Province: Willyama Block.||||||18-JAN-05
2480|Braemar Iron Formation|30178|6|Mentioned|p19|||||||||
2480|Braemar Iron Formation|30799|6|Mentioned|p1|||Stratigraphic relations with Benda Siltstone.||||||
2480|Braemar Iron Formation|30801|6|Mentioned|p5|||Sturtian. Table P5-6||||||
2480|Braemar Iron Formation|30802|6|Mentioned|p12|||||||||
2480|Braemar Iron Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
2480|Braemar Iron Formation|30810|6|Mentioned|p2|||||||||
2480|Braemar Iron Formation|32510|6|Mentioned|Table 1|||||||||
2480|Braemar Iron Formation|33224|6|Mentioned|p48|||||||||
2480|Braemar Iron Formation|33474|6|Mentioned|p537|||||||||
2480|Braemar Iron Formation|33794|4|Described|p11|||See also PP12-18||||||
2480|Braemar Iron Formation|34534|6|Mentioned|p60|||Refers Mirams,1962||||||
2480|Braemar Iron Formation|34537|6|Mentioned|Fig.8|||Sturtian||||||
2480|Braemar Iron Formation|35255|6|Mentioned|p13|||||||||
2480|Braemar Iron Formation|36003|5|Briefly described|p1030|||||||||
2480|Braemar Iron Formation|36833|6|Mentioned|Fig.1|||||||||
2480|Braemar Iron Formation|37461|6|Mentioned|Table 5.I|||||||||
2480|Braemar Iron Formation|37932|6|Mentioned|p537|||||||||
2480|Braemar Iron Formation|38157|6|Mentioned|Table IV|||||||||
2480|Braemar Iron Formation|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2480|Braemar Iron Formation|40294|6|Mentioned|p41|||||||||
2480|Braemar Iron Formation|40852|6|Mentioned|Fig.3.2|||||||||
2480|Braemar Iron Formation|42813|6|Mentioned|p18|||||||||
2480|Braemar Iron Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of the Umbertatana Group. Sturtian.||||||
2480|Braemar Iron Formation|61556|5|Briefly described|p9-10 Figure, p11|Adelaidean|Adelaidean|In Mount Lofty ranges, Adelaide Syncline. Tillitic unit.||||||21-NOV-07
2480|Braemar Iron Formation|68276|6|Mentioned|p69|||"Nackara arc. Associated with the Sturtian glaciation. The ""Iron Formation"" is omitted."||||Conformably overlies Pualco Tillite. Is overlain disconformably by Wilyerpa Formation.|Haematite-jaspilite interrupted by thin units of ferruginous diamictite. Sorted sandstones occur within the diamictite complexes.|
2480|Braemar Iron Formation|71237|14|Not recorded|p9|||||||||
2492|Bramfield Granite|31248|4|Described|p6|||Petrographic description||||||
2543|Bridgewater Formation|2967|6|Mentioned|p54|||Boutakoff (1963). A regressive coastal dune sequence.||||||
2543|Bridgewater Formation|10010|5|Briefly described|p14 Fig. 5f, p16|Quaternary|Quaternary|Carbonate-rich. Geological Province: Murray Basin.||||||13-AUG-07
2543|Bridgewater Formation|22489|5|Briefly described|p12||Pleistocene|||||||
2543|Bridgewater Formation|22552|6|Mentioned|p 32|||||||||
2543|Bridgewater Formation|22867|6|Mentioned|P27|||||||||
2543|Bridgewater Formation|22870|6|Mentioned|P32|||||||||
2543|Bridgewater Formation|22875|6|Mentioned|p86|||||||||
2543|Bridgewater Formation|23322|5|Briefly described|957 Fig.2|Pleistocene|Pliocene|Geological Province: Gambier Basin.||||||07-SEP-09
2543|Bridgewater Formation|23418|6|Mentioned|p14|||||||||
2543|Bridgewater Formation|23482|5|Briefly described|p9|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23492|6|Mentioned|p7 Fig. 2.|||||||||
2543|Bridgewater Formation|23537|5|Briefly described|p 440|||||||||
2543|Bridgewater Formation|23560|5|Briefly described|p152|Cretaceous|Cretaceous|||||||
2543|Bridgewater Formation|23719|5|Briefly described|p30|||||||||
2543|Bridgewater Formation|23731|6|Mentioned|p29|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23779|5|Briefly described|p621|||||||||
2543|Bridgewater Formation|23818|5|Briefly described|p213, 228|||Geological Province: Murray Basin. Underlying unit: Coomandook Formation and Nullarbor Limestone. Max. thickness: 250 ft.||||||
2543|Bridgewater Formation|23879|5|Briefly described|p20|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23908|6|Mentioned|p6|Pleistocene|Pleistocene| Geological Province: Gawler Craton.||||||
2543|Bridgewater Formation|23921|5|Briefly described|p1109 Table 1, p1111|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
2543|Bridgewater Formation|23932|5|Briefly described|p687|Holocene|Pleistocene|||||||
2543|Bridgewater Formation|24038|5|Briefly described|p439 Fig.2|Pliocene|Pliocene|Geological Province: Port Phillip Basin||||||
2543|Bridgewater Formation|24358|5|Briefly described|p32 Fig.1|Pleistocene|Pleistocene|Geological Province: Eucla Basin. Maximum Thickness: 15m.||||||17-MAR-05
2543|Bridgewater Formation|24363|6|Mentioned|p37 Fig.1|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|24410|5|Briefly described|p6|Pleistocene|Pleistocene|Includes bouldery conglomerate with flint.||||||24-NOV-09
2543|Bridgewater Formation|24508|5|Briefly described|p30|Quaternary|Quaternary|Consists of relict, calcareous sand dunes formed during the last interglacial period.  Geological Province: Gawler Craton.||||||23-DEC-09
2543|Bridgewater Formation|24551|6|Mentioned|p305, 306, 343, p734 Table 17.4|||Superseded by Bridgewater Group.  Max thickness: 200m.||||||
2543|Bridgewater Formation|24585|6|Mentioned|p33 (photo)|||||||||
2543|Bridgewater Formation|29591|6|Mentioned|p92|||||||||
2543|Bridgewater Formation|29664|6|Mentioned|p2|||||||||
2543|Bridgewater Formation|29665|6|Mentioned|p79|||||||||
2543|Bridgewater Formation|29697|6|Mentioned|p2|||||||||
2543|Bridgewater Formation|29825|5|Briefly described|p18|||||||||
2543|Bridgewater Formation|29829|6|Mentioned|p178|||||||||
2543|Bridgewater Formation|29866|6|Mentioned|p84|||||||||
2543|Bridgewater Formation|29891|5|Briefly described|p107|||||||||
2543|Bridgewater Formation|29892|6|Mentioned|p77|||||||||
2543|Bridgewater Formation|30514|6|Mentioned|p102|||||||||
2543|Bridgewater Formation|30522|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|30578|5|Briefly described|p14|||||||||
2543|Bridgewater Formation|30580|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|30752|6|Mentioned|p5|||||||||
2543|Bridgewater Formation|30754|6|Mentioned|p20|||See also P22,24,27. Geological map||||||
2543|Bridgewater Formation|30756|6|Mentioned|p4|||||||||
2543|Bridgewater Formation|30758|6|Mentioned|p66|||Stratigraphy||||||
2543|Bridgewater Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
2543|Bridgewater Formation|30825|6|Mentioned|p32|||||||||
2543|Bridgewater Formation|30922|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|30928|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|30932|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|31241|4|Described|p101|||Middle Pleistocene||||||
2543|Bridgewater Formation|31248|4|Described|p57|||||||||
2543|Bridgewater Formation|31312|6|Mentioned|p71|||||||||
2543|Bridgewater Formation|31320|6|Mentioned|p14|||Quaternary||||||
2543|Bridgewater Formation|31624|4|Described|p98|||Pleistocene. See also p131.||||||22-FEB-19
2543|Bridgewater Formation|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
2543|Bridgewater Formation|31629|6|Mentioned|Fig. 5.1|||Recent to Pleistocene||||||
2543|Bridgewater Formation|31746|6|Mentioned|p197|||||||||
2543|Bridgewater Formation|31850|3|Fully described|p39|||||||||
2543|Bridgewater Formation|31920|6|Mentioned|p59|||See also Table 3-1. Pleistocene||||||
2543|Bridgewater Formation|31923|6|Mentioned|p16|||||||||
2543|Bridgewater Formation|32432|5|Briefly described|Table 1|||||||||
2543|Bridgewater Formation|32438|6|Mentioned|p42|||||||||
2543|Bridgewater Formation|32561|6|Mentioned|Fig.4|||||||||
2543|Bridgewater Formation|32767|6|Mentioned|p66|||||||||
2543|Bridgewater Formation|32859|5|Briefly described|p69|||See also Figs. 1,2.||||||
2543|Bridgewater Formation|33109|5|Briefly described|p83|||Main aquifer system P84||||||
2543|Bridgewater Formation|33160|6|Mentioned|p301|||See also P304||||||
2543|Bridgewater Formation|33224|6|Mentioned|Fig.32|||See also Fig.36. Photo.||||||
2543|Bridgewater Formation|33716|3|Fully described|p20|||See also Table 2.||||||
2543|Bridgewater Formation|33798|6|Mentioned|p98|||See also Fig.2||||||
2543|Bridgewater Formation|34180|6|Mentioned|p212|||Middle Pleistocene||||||
2543|Bridgewater Formation|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|34658|5|Briefly described|p98|||||||||
2543|Bridgewater Formation|34758|6|Mentioned|Table 1|||||||||
2543|Bridgewater Formation|34827|6|Mentioned|p12|||||||||
2543|Bridgewater Formation|34954|5|Briefly described|p198|||||||||
2543|Bridgewater Formation|34988|3|Fully described|p291|||||||||
2543|Bridgewater Formation|35029|6|Mentioned|p168|||||||||
2543|Bridgewater Formation|35066|6|Mentioned|p218|||||||||
2543|Bridgewater Formation|35097|6|Mentioned|p15|||||||||
2543|Bridgewater Formation|35147|6|Mentioned|p127|||||||||
2543|Bridgewater Formation|35238|6|Mentioned|p86|||||||||
2543|Bridgewater Formation|35271|6|Mentioned|p67|||||||||
2543|Bridgewater Formation|35272|6|Mentioned|p283|||||||||
2543|Bridgewater Formation|35274|6|Mentioned|p424|||||||||
2543|Bridgewater Formation|35285|6|Mentioned|p414|||||||||
2543|Bridgewater Formation|35290|6|Mentioned|p45|||||||||
2543|Bridgewater Formation|35368|6|Mentioned|p69|||||||||
2543|Bridgewater Formation|35579|6|Mentioned|p67|||||||||
2543|Bridgewater Formation|35672|6|Mentioned|p11|||||||||
2543|Bridgewater Formation|35712|4|Described|p24|||||||||
2543|Bridgewater Formation|35722|6|Mentioned|p6|||Stratigraphy.||||||
2543|Bridgewater Formation|35772|4|Described|Table 1|||||||||
2543|Bridgewater Formation|36355|6|Mentioned|p132|||||||||
2543|Bridgewater Formation|36499|6|Mentioned|p51|||||||||
2543|Bridgewater Formation|36624|6|Mentioned|Fig.1|||||||||
2543|Bridgewater Formation|37500|6|Mentioned|p385|||||||||
2543|Bridgewater Formation|37548|6|Mentioned|p131|||||||||
2543|Bridgewater Formation|37850|6|Mentioned|Fig.2|||||||||
2543|Bridgewater Formation|37863|5|Briefly described|p195|||||||||
2543|Bridgewater Formation|38068|6|Mentioned|p76|||||||||
2543|Bridgewater Formation|38699|5|Briefly described|Fig.10|||||||||
2543|Bridgewater Formation|38932|5|Briefly described|p99|||See also Fig.4||||||
2543|Bridgewater Formation|39077|6|Mentioned|p25|||||||||
2543|Bridgewater Formation|39329|6|Mentioned|p485|||||||||
2543|Bridgewater Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|39352|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|39839|6|Mentioned|p48|||||||||
2543|Bridgewater Formation|40003|5|Briefly described|p44|||||||||
2543|Bridgewater Formation|40226|6|Mentioned|p52|||||||||
2543|Bridgewater Formation|40230|6|Mentioned|p7|||||||||
2543|Bridgewater Formation|40440|5|Briefly described|p103|||||||||
2543|Bridgewater Formation|40442|6|Mentioned|p35|||||||||
2543|Bridgewater Formation|40445|5|Briefly described|p48|||||||||
2543|Bridgewater Formation|40448|5|Briefly described|p43|||||||||
2543|Bridgewater Formation|40521|6|Mentioned|Fig.2|||||||||
2543|Bridgewater Formation|40525|6|Mentioned|p172|||||||||
2543|Bridgewater Formation|40555|6|Mentioned|p51|||||||||
2543|Bridgewater Formation|40561|6|Mentioned|p8|||||||||
2543|Bridgewater Formation|40643|5|Briefly described|p145|||||||||
2543|Bridgewater Formation|40829|5|Briefly described|p14|||||||||
2543|Bridgewater Formation|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|40942|4|Described|p20|||||||||
2543|Bridgewater Formation|40980|6|Mentioned|p335|||||||||
2543|Bridgewater Formation|41206|5|Briefly described|p367|||Mention P365||||||
2543|Bridgewater Formation|41499|6|Mentioned|p70|||||||||
2543|Bridgewater Formation|41511|6|Mentioned|p23|||||||||
2543|Bridgewater Formation|41521|3|Fully described|p241|||||||||
2543|Bridgewater Formation|41599|6|Mentioned|p192|||||||||
2543|Bridgewater Formation|41619|6|Mentioned|Map legend|Pleistocene||||||||
2543|Bridgewater Formation|41642|6|Mentioned|Fig.8.6|||||||||
2543|Bridgewater Formation|41769|6|Mentioned|p50|||||||||
2543|Bridgewater Formation|41848|3|Fully described|p366|||||||||
2543|Bridgewater Formation|41868|5|Briefly described|p549|||See also p554 and p578.||||||22-FEB-19
2543|Bridgewater Formation|41940|6|Mentioned|p38|||||||||
2543|Bridgewater Formation|42097|6|Mentioned|p40|||||||||
2543|Bridgewater Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
2543|Bridgewater Formation|42292|5|Briefly described|p8|||See also Fig. 3 P12||||||
2543|Bridgewater Formation|42318|5|Briefly described|p8|||||||||
2543|Bridgewater Formation|42404|6|Mentioned|p32|||||||||
2543|Bridgewater Formation|42466|5|Briefly described|Map Legend|||||||||
2543|Bridgewater Formation|42475|4|Described|p23|||||||||
2543|Bridgewater Formation|42601|6|Mentioned|Fig.2 p15|||||||||
2543|Bridgewater Formation|42622|6|Mentioned|p15|||||||||
2543|Bridgewater Formation|42635|5|Briefly described|p94|||||||||
2543|Bridgewater Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
2543|Bridgewater Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
2543|Bridgewater Formation|42738|5|Briefly described|map legend|Quaternary||||||||
2543|Bridgewater Formation|42827|4|Described|p366|||see also Table 9.3||||||
2543|Bridgewater Formation|42966|2|Defined|p223|Late Pleistocene|Early Pleistocene|||||||
2543|Bridgewater Formation|43026|5|Briefly described|Table 1,p586|||||||||
2543|Bridgewater Formation|43049|4|Described|p23|||||||||
2543|Bridgewater Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||25-MAY-05
2543|Bridgewater Formation|43071|5|Briefly described|p17|||||||||
2543|Bridgewater Formation|43073|5|Briefly described|Table 4|||||||||
2543|Bridgewater Formation|43195|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|see also commentary on back of map.||||||
2543|Bridgewater Formation|43231|6|Mentioned|p12|||||||||
2543|Bridgewater Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|43590|4|Described|p35||Quaternary|||||||
2543|Bridgewater Formation|44133|5|Briefly described|p220 Fig. 11.2, 222|Pleistocene|Pleistocene|Geological Province: Eucla Basin. ||||||
2543|Bridgewater Formation|44864|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|46802|6|Mentioned|Table 1|||||||||
2543|Bridgewater Formation|46839|6|Mentioned|p86|||See also Fig.3||||||
2543|Bridgewater Formation|46909|6|Mentioned|p83|||See also Fig.2||||||
2543|Bridgewater Formation|48911|6|Mentioned|Chart 1|||||||||
2543|Bridgewater Formation|49038|4|Described|Table 2|||Briefly described P33||||||
2543|Bridgewater Formation|50154|2|Defined|p140||Late Pleistocene|Overlies the Whalers Bluff Formation. Age: oldest dunes dated at 0.69 Ma. Consists of poorly consolidated fine- to coarse- grained calcarenite.||||||15-MAY-13
2543|Bridgewater Formation|50155|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Palaeo-beach ridges; calcarenite||||||
2543|Bridgewater Formation|50156|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||
2543|Bridgewater Formation|50157|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Overlies Whalers Bluff Formation. Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||25-JUN-04
2543|Bridgewater Formation|50158|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||
2543|Bridgewater Formation|50159|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50160|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcareous sand, calcarenite||||||16-JUN-04
2543|Bridgewater Formation|50161|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50162|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50163|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50164|5|Briefly described|Map Legend|Quaternary|Quaternary|Palaeo-beach ridges; calcarenite.||||||
2543|Bridgewater Formation|60707|5|Briefly described|p612 Fig. 1c|Pleistocene|Pleistocene|Calcarenites.||||||
2543|Bridgewater Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||
2543|Bridgewater Formation|60958|5|Briefly described|Map Legend|Holocene|Pleistocene|Medium-grained, large scale cross-bedded calcarenite and calcareous aeolianite with numerous palaeosol horizons and capped by calcrete.||||||
2543|Bridgewater Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Soft, white to cream-fawn fine to medium-grained aeolian calcarenite. Multiple coalescing horizons of calcrete. Tabular foresets  with interbeds of silt. Underlies: Wiabuna Formation.||||||15-MAY-13
2543|Bridgewater Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||
2543|Bridgewater Formation|61121|5|Briefly described|Map legend|Pleistocene|Pleistocene|Medium-grained, large-scale calcarenite and calcareous aeolianite, numerous paleosol horizons;capped by thick laminar to powdery or bouldery calcrete. Cavernous in places with abundant rhizomorphs and solution pipes. Upper and lower members differentiated||||||07-JUN-05
2543|Bridgewater Formation|61155|5|Briefly described|p6, p17|Pleistocene|Pleistocene|Series of beach ridge/dune complexes. Overlies Coomandook Formation (Polda Basin and Aire Peninsula) and Wannaeue Formation in Melbourne area. Geological Province: Otway and Murray Basins/coastal margins; Polda Basin, Eyre Peninsula. See also p18.||||||03-MAR-10
2543|Bridgewater Formation|61181|5|Briefly described|p136, p183|Pleistocene|Pleistocene|Largely derived from Tertiary bryozoal limestone, siliceous sand and lime fixed by groundwater percolation. Composition and hardness vary from place to place. Underlies Malanganee Sands. ||||||
2543|Bridgewater Formation|61307|5|Briefly described|p34, p65 Fig. 29|Tertiary|Tertiary|Includes calcareous sandstones. See also p71-75 Figs. 32-36.||||||15-JAN-08
2543|Bridgewater Formation|62068|5|Briefly described|p136,p137,|||[Misspelling of Bridgewater Group?]||||Unconformably overlies Nelson Bay Formation. Appears to say this unit is?mid-?late Pliocene on p37, but they may be referring to the Hanson Plain Sands equivalent.|Series of consolidated cross-bedded dune sands.|
2543|Bridgewater Formation|62893|4|Described|Map Legend, p22-25, p38, p40|Pleistocene|Pleistocene|Reflects widespread coastal and inland dune and loess deposits. Forms spectacular cliffs near Sheringa and low undulating terrain inland. Maximum thickness of over 140 m, although much thinner (less than 1 m) away from the coast. Divided into [informal] lower and upper members. Calcarenite horizons constitute important freshwater aquifers. Overlies and blankets both Tertiary sediments and Archaean-Proterozoic basement. Intertongues with and is laterally equivalent to the Glanville Formation.||||Disconformably overlain by Semaphore Sand. Equivalent to Glanville Formation.|Calcareous aeolianite dunes and associated calcrete horizons.|
2543|Bridgewater Formation|62898|5|Briefly described|p197, p205|Pleistocene|Pleistocene|In Eyre Peninsula, S.A.||||||
2543|Bridgewater Formation|63124|5|Briefly described|p92, p93|||Unconformably overlies Green Point Member (Gambier Limestone). May overlie Camelback Member (Gambier Limestone) unconformably.  Geological Province: Otway Basin. ||||||
2543|Bridgewater Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Aeolian: dune deposits, calcarenite.|
2543|Bridgewater Formation|64282|5|Briefly described|Map legend|Pleistocene|Pleistocene|Medium-grained, lg.scale X-bedded calcarenite + calcareous aeolianite with numerous palaeosol horizons, capped by thick, laminar to powdery or bouldery calcrete; cavernous in places with abundant rhizomorphs and solution pipes; preserved dune morphology.||||||23-DEC-09
2543|Bridgewater Formation|65375|4|Described|p32, p38, pp40-41, p56.|Pleistocene|Pleistocene|Originally applied to Portland aeolianites and limestones; subsequently for calcareous dunes and bioclastic barrier shoreline complexes in S.A. Described in detail in Notes. Covers >90 % of Yorke Peninsula land area. Supplies town water for Warooka.|<0.78 Ma to 22,400 +/- 800 years.|||Unconformably overlies Cape Jervis Formation and Hindmarsh Clay. Is overlain by Saint Kilda Formation. Locally capped with calcrete.|Three units: medium-to coarse-grained, large-scale foreset bedded calcarenite with interlayered red-brown sandy clay paleosols; shells of the Glanville Formation; and an upper unit of fine- to medium-grained aeolianite and bioclastic calcarenite.|
2543|Bridgewater Formation|65376|5|Briefly described|p9 Fig.1.2. |Pleistocene|Pleistocene||||||Eolian calcareous sand, with calcrete.|
2543|Bridgewater Formation|65715|5|Briefly described|p15 Tb.8, p25|Neogene|Neogene|Six unnamed subunits recognised by Gill (1967, 1976) and elevated to group rank by Reeckman and Gill (1981). Here demoted to formation rank.||||||
2543|Bridgewater Formation|65921|5|Briefly described|p1, p2 (map legend).|Pleistocene|Pleistocene|Large coastal sand dunes. Occurs as a 50m cliff sequence at Pennington Bay. Contains over 30 caves: karren, sea caves and dolines are common.|||||Aeolian calcarenite variably cemented by pedogenic and vadose diagenetic processes and affected by karstic solution.|
2543|Bridgewater Formation|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Pale yellow-cream calcareous gritty sandstone; aeolian calcarenite. Ripon Calcrete occurs within this unit.||||||
2543|Bridgewater Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Boutakoff and Sprigg 1953. Raised to Group in 1981, but reinstated as Formation herein.||||||
2543|Bridgewater Formation|66287|5|Briefly described|p35, 38, 40, Fig 11, 16|Pleistocene|Pleistocene|Forms a strandplain up to 100 km inland from the modern coastline; includes 13 coastal barriers.|||||Prograding calcareous sediments.|20-APR-12
2543|Bridgewater Formation|66761|5|Briefly described|p244, 246|Pleistocene|Pleistocene|26 m interval in PIRSA stratigraphic hole Investigator 1 where it overlies the White Point Conglomerate. Calcareous aeolianite.||||||14-MAR-12
2543|Bridgewater Formation|67462|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Saint Vincent Basin.||||||
2543|Bridgewater Formation|68116|5|Briefly described|Maps 29, 38, 47-48, 50, 54-55, 57.|Pleistocene|Pleistocene|Also occurs in the Appendix.|||||Calcarenite: medium to coarse grained shell fragments and minor quartz; consolidated, thin interbedded red palaeosols, minor hard calcrete capping, prominent dune cross-bedding; coastal dune deposits.|
2543|Bridgewater Formation|68131|5|Briefly described|p2 Fig.1, p7, p17, p42, p66, p71, p84|Pleistocene|Pleistocene|Aeolian sediments.|||||Calcareous sand, with calcrete.|
2543|Bridgewater Formation|68211|6|Mentioned|p28 Fig.1|Quaternary|Quaternary|||||||06-AUG-13
2543|Bridgewater Formation|68715|6|Mentioned|p31 Fig.5|Pleistocene|Pleistocene|St Vincent Basin.||||||
2543|Bridgewater Formation|68811|5|Briefly described|p67, p69, p112,113, p114, p130|Quaternary|Quaternary|See also p156 app 1, p170 tbl 31, p193 tbl 47. ||||Overlies the Uley Formation, Brighton Group and the Fyansford Formation.|Sandy sediments.|16-APR-20
2543|Bridgewater Formation|68990|6|Mentioned|p459|||Sheard (1978, 1990).|||||Sands.|
2543|Bridgewater Formation|68991|5|Briefly described|p465 Fig.2, pp467-469, p471 Fig.5|Pleistocene|Pleistocene|Upper Pleistocene age. ~ 0-100 m thick. Represents stacked coastal-dune deposits. Thermoluminescence dating of quartz grains and loess at Warrnambool gave ages ranging between 160-67 ka (Sherwood et al. 1994; Brooke 2001).|93 +/- 11 ka|||Disconformably underlain by the Port Campbell Limestone, Hesse Clay, Dog Trap Bay Sand and Cove Sand.|Comprises partially lithified, yellowish grey, cross-bedded medium-grained calcarenite of shell fragments and minor quartz grains.|20-JUL-15
2543|Bridgewater Formation|69048|6|Mentioned|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.||||||
2543|Bridgewater Formation|69297|6|Mentioned|p79|Pleistocene|Pleistocene|Otway Basin. ||||Unconformably overlies the Gambier Limestone and the Coomandook Formation.||
2543|Bridgewater Formation|69372|6|Mentioned|p28 fig. 6, p34 fig. 12|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|70029|5|Briefly described|p151-153,156,158-159,161-163,165|Pleistocene|Pleistocene|First identified at Cape Bridgewater in western VIC (Boutakoff 1963). Represented by late early Pleistocene [Marine Isotope Stage (MIS) 23 at 933 ka] to Holocene barrier shoreline successions deposited during sea-level highstands. Up to nine morphologically distinct, relict coastal barrier landforms preserved in the Mount Gambier coastal plain that trend sub[parallel to the modern coastline. Can be correlated to barrier landforms in the Robe coastal plain, 100km NW of Mount Gambier based on lateral continuity.||||Underlain unconformably by Gambier Limestone and Coomandook/Werrikoo Limestone.|Cool water, temperate sedimentary carbonates.|
2543|Bridgewater Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Holocene|Holocene|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||||Overlies Coomandook Formation.||
2543|Bridgewater Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Holocene|Holocene|Gambier Embayment and Voluta Trough.||||Overlies Coomandook Formation.||
2543|Bridgewater Formation|70337|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Shown as having two unnamed members in parts.|||||Bioclastic barrier shoreline deposits, silica-rich, with heavy minerals, shallow sub-tidal. Coastal, cross-bedded, aeolian calcarenite with paleosol horizons and capped by calcrete.|08-JAN-16
2543|Bridgewater Formation|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Calc-arenite.|
2543|Bridgewater Formation|70893|6|Mentioned|p3 fig 1b|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|71419|5|Briefly described|p22|||Calcareous sandstone.||||Overlies Gellibrand Marl.||
2543|Bridgewater Formation|73026|6|Mentioned|p26|||||||||
2543|Bridgewater Formation|73027|6|Mentioned|p26, p31, p39|||Outcrops at Wanna.||||||
2543|Bridgewater Formation|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Four constituent parts/facies, called members but obviously not intended as stratigraphic units, are described and mapped separately. The Glanville Formation separates the topmost from the third member.||||Is interbedded with the Glanville Formation.|Medium-grained, large-scale cross-bedded calcarenite and calcareous aeolianite with numerous paleosol horizons and capped by thick laminar to powdery or boulder calcrete. Cavernous in places. Preserved dune morphology.|
2543|Bridgewater Formation|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Brownish aeolian calcarenite.|
2543|Bridgewater Formation|73122|5|Briefly described|p23, 27-28|Quaternary|Quaternary|Central Williams Island.|||||Travertine and calcareous aeolianite.|
2543|Bridgewater Formation|73228|4|Described|p50, p56-57, p60, p62|Pleistocene|Late Pliocene|Murray Basin. Outcrops as an extensive sequence of subparallel linear ridges in the southwest and is contiguous with sediments on the Gambier coastal plain. Consists of subtidal, intertidal and aeolian dune facies. Characterised by a sparse faunal assemblage comprising benthic and rare planktonic foraminifera, echinoderms, bivalves, bryozoans and articulated tidal bivalves. Variations in depositional environment are reflected in the degree of cross-bedding, from gentle (near-shore) to steep (aeolian).|||||Well-sorted, fine- to medium-grained bioclastic carbonate sand, commonly laminated and well cemented.|
2543|Bridgewater Formation|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
2543|Bridgewater Formation|73292|6|Mentioned|p955, p963|Pleistocene|Pleistocene||||||Eolianites of consolidated Quaternary sand dunes.|
2543|Bridgewater Formation|73302|6|Mentioned|p34|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|73356|6|Mentioned|p3|Pleistocene|Pliocene|||||Unconformably underlain by Heytesbury Group.|Shallow marine sediments and basalts.|
2543|Bridgewater Formation|73383|5|Briefly described|p3|Pliocene|Pliocene|||||Overlies Heytesbury Group, underlies Newer Volcanics.|Sandstones.|
2543|Bridgewater Formation|73385|5|Briefly described|p3-5|Pleistocene|Pliocene|Otway Basin. Overlies late-Miocene unconformity.||||Unconformably overlies Heytesbury Group, Bridgewater Formation, underlies Newer Volcanics.|Shallow marine and nearshore sandstones.|
2543|Bridgewater Formation|73386|5|Briefly described|p2, p4-5, p7, p14, iii|Pleistocene|Pliocene|Otway Basin. Deposited following widespread tectonic uplift in the Pliocene.|||Albert Park Aeolianite, Armstrong Sand, Moyne Alluvium, Port Fairy Calcarenite, Sunnyside Sand, Warrnambool Aeolianite, Bats Ridge Member, Descartes Bay Member, Duquesne Member.|Overlies Heytesbury Group, underlies Newer Volcanics|Shallow marine sediments, sequence of relatively thin localised units.|
2543|Bridgewater Formation|73493|5|Briefly described|p715 Fig.2, p717, p718 Fig.5|Pleistocene|Pliocene|Cover sequence.||||Overlies Donington Suite|Includes calc-arenite.|
2543|Bridgewater Formation|73594|5|Briefly described|p4, p6|Pliocene|Pliocene|Otway Basin. See also Bridgewater Bay Group p6.||||Underlies Newer Volcanics|Shallow marine and nearshore sandstones.|
2543|Bridgewater Formation|73634|6|Mentioned|p7|||Williams Island, Jussieu Peninsula. Age given as Tertiary.||||||
2557|Brighton Limestone|9124|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||11-JAN-10
2557|Brighton Limestone|22510|5|Briefly described|table1,p38,40,41|||Age: Sturtian. Redefined to exclude upper bedded dolomite member.||||||
2557|Brighton Limestone|22581|6|Mentioned|p44||Neoproterozoic|Questionable identification||||||
2557|Brighton Limestone|22589|6|Mentioned|p129||Cryogenian|||||||
2557|Brighton Limestone|22921|5|Briefly described|38|||||||||
2557|Brighton Limestone|23054|6|Mentioned|p15|||||||||
2557|Brighton Limestone|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Correlate of Sunderland Formation and Tapley Hill Formation (Umberatana Group) and Aralka Formation and Ringwood Member.||||||
2557|Brighton Limestone|23314|5|Briefly described|331 Fig.2|||||||||
2557|Brighton Limestone|23719|4|Described|p26|Neoproterozoic|Adelaidean|See also page 25 table 7. Of Farina Subgroup. Overlain by Willochra Subgroup. Underlain by Tapley Hill Formation. Geological Province: Gawler Craton. Max. thickness: 70 m.||||||22-JUN-09
2557|Brighton Limestone|23818|5|Briefly described|p64 Fig.22, p68|Adelaidean|Adelaidean|Of the Farina Sub-Group. Underlying unit: Tapley Hill Formation.||||||
2557|Brighton Limestone|24175|5|Briefly described|p13|Neoproterozoic|Neoproterozoic|Of Farina Subgroup.  Overlies Tapley Hill Formation.||||||14-DEC-06
2557|Brighton Limestone|24176|5|Briefly described|p25 Tb. 1|Adelaidean|Adelaidean|Equivalent to Balcanoona Formation.  Age is Sturtian.  Geological Province: Mount Painter Province.||||||
2557|Brighton Limestone|24195|6|Mentioned|p42|||Overlying Unit: Purple Series||||||
2557|Brighton Limestone|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||
2557|Brighton Limestone|29780|3|Fully described|p94|||||||||
2557|Brighton Limestone|30048|4|Described|p131|||||||||
2557|Brighton Limestone|30051|6|Mentioned|p12|||||||||
2557|Brighton Limestone|30052|6|Mentioned|Fig.6|||See also P91.||||||
2557|Brighton Limestone|30053|5|Briefly described|p113|||See also Fig.1||||||
2557|Brighton Limestone|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|30378|6|Mentioned|p431|||||||||
2557|Brighton Limestone|30514|5|Briefly described|p100|||||||||
2557|Brighton Limestone|30757|6|Mentioned|p2|||||||||
2557|Brighton Limestone|30801|6|Mentioned|p5|||Sturtian. Table P5-6||||||
2557|Brighton Limestone|30802|6|Mentioned|p14|||||||||
2557|Brighton Limestone|30807|6|Mentioned|p103|||Suggested map symbol||||||
2557|Brighton Limestone|31022|4|Described|Fig. 3|||See also Fig. 4.||||||
2557|Brighton Limestone|31322|6|Mentioned|p30|||Limestone deposits||||||
2557|Brighton Limestone|31923|6|Mentioned|p10|||||||||
2557|Brighton Limestone|32144|6|Mentioned|p123|||Palaeotemperature||||||
2557|Brighton Limestone|32481|6|Mentioned|p8|||Stratigraphy described||||||
2557|Brighton Limestone|32506|6|Mentioned|Fig.1|||||||||
2557|Brighton Limestone|32510|6|Mentioned|Table 1|||||||||
2557|Brighton Limestone|32551|5|Briefly described|p101|||U.Sturtian||||||
2557|Brighton Limestone|32720|6|Mentioned|Table 1|||||||||
2557|Brighton Limestone|32721|6|Mentioned|Fig.3|||Stromatolite||||||
2557|Brighton Limestone|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
2557|Brighton Limestone|32723|6|Mentioned|p99|||||||||
2557|Brighton Limestone|32724|4|Described|p512|||Sturtian. See also p513-517.||||||01-JUL-08
2557|Brighton Limestone|32727|6|Mentioned|p12|||||||||
2557|Brighton Limestone|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
2557|Brighton Limestone|33423|4|Described|p13|||||||||
2557|Brighton Limestone|33474|6|Mentioned|Fig.2|||||||||
2557|Brighton Limestone|33989|6|Mentioned|p495|||U.Precambrian||||||
2557|Brighton Limestone|34202|6|Mentioned|p1057|||See also P1058. Precambrian.||||||
2557|Brighton Limestone|34407|6|Mentioned|p101|||Lithology||||||
2557|Brighton Limestone|34535|5|Briefly described|p68|||Fig.22||||||
2557|Brighton Limestone|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|34615|6|Mentioned|p7|||Shown on Figure||||||
2557|Brighton Limestone|34812|6|Mentioned|p110|||||||||
2557|Brighton Limestone|34959|6|Mentioned|p282|||||||||
2557|Brighton Limestone|35003|6|Mentioned|p122|||||||||
2557|Brighton Limestone|35051|5|Briefly described|p202|||||||||
2557|Brighton Limestone|35255|5|Briefly described|p9|||See also Fig.6.||||||
2557|Brighton Limestone|35675|6|Mentioned|p31|||||||||
2557|Brighton Limestone|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
2557|Brighton Limestone|36212|6|Mentioned|Fig.3|||||||||
2557|Brighton Limestone|36625|6|Mentioned|Fig.1|||||||||
2557|Brighton Limestone|36731|6|Mentioned|p124|||||||||
2557|Brighton Limestone|36733|6|Mentioned|Table 5|||See also P52.||||||
2557|Brighton Limestone|37461|4|Described|p339|||See also Table 5.I||||||
2557|Brighton Limestone|37932|6|Mentioned|p547|||||||||
2557|Brighton Limestone|38157|6|Mentioned|Table IV|||||||||
2557|Brighton Limestone|38290|6|Mentioned|p20|||See also P59.||||||
2557|Brighton Limestone|38873|4|Described|Table 2|||||||||
2557|Brighton Limestone|39210|6|Mentioned|Table 4|||||||||
2557|Brighton Limestone|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
2557|Brighton Limestone|39349|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|39351|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
2557|Brighton Limestone|39866|6|Mentioned|Table 2|||||||||
2557|Brighton Limestone|40003|5|Briefly described|Table 16|||||||||
2557|Brighton Limestone|40294|6|Mentioned|p49|||||||||
2557|Brighton Limestone|40442|6|Mentioned|p10|||||||||
2557|Brighton Limestone|40448|5|Briefly described|p38|||||||||
2557|Brighton Limestone|40852|5|Briefly described|p27|||||||||
2557|Brighton Limestone|40856|5|Briefly described|p312|||||||||
2557|Brighton Limestone|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
2557|Brighton Limestone|41401|5|Briefly described|p29|||||||||
2557|Brighton Limestone|41405|3|Fully described|p168|||||||||
2557|Brighton Limestone|41493|6|Mentioned|Table 1|||||||||
2557|Brighton Limestone|41494|6|Mentioned|Fig.2|||||||||
2557|Brighton Limestone|41526|6|Mentioned|p17|||||||||
2557|Brighton Limestone|42090|5|Briefly described|p25|||||||||
2557|Brighton Limestone|42093|5|Briefly described|p6|||See also Fig.2||||||
2557|Brighton Limestone|42222|5|Briefly described|p17|||||||||
2557|Brighton Limestone|42235|4|Described|p140|||See also Fig.3||||||
2557|Brighton Limestone|42237|6|Mentioned|p98|||||||||
2557|Brighton Limestone|42238|5|Briefly described|Table 1 P74|||||||||
2557|Brighton Limestone|42243|5|Briefly described|p211|||||||||
2557|Brighton Limestone|42268|6|Mentioned|Fig.4 P329|||||||||
2557|Brighton Limestone|42272|6|Mentioned|p403|||||||||
2557|Brighton Limestone|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Sturtian)|||||||
2557|Brighton Limestone|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
2557|Brighton Limestone|42736|5|Briefly described|map legend|Neoproterozoic||||||||
2557|Brighton Limestone|42788|6|Mentioned|p148|||||||||
2557|Brighton Limestone|42882|5|Briefly described|Fig.7 P12|||of Umberatana Group||||||
2557|Brighton Limestone|43052|5|Briefly described|Table 6.1|||of Umberatana Group||||||
2557|Brighton Limestone|43622|6|Mentioned|p38|Neoproterozoic||||||||
2557|Brighton Limestone|44133|6|Mentioned|p50 |||||||||
2557|Brighton Limestone|44198|5|Briefly described|p14||Proterozoic|||||||
2557|Brighton Limestone|44660|14|Not recorded|map legend|||Sturtian, lithology.||||||
2557|Brighton Limestone|44934|6|Mentioned|Map Legend||Adelaidean|||||||
2557|Brighton Limestone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Nepouie Subgroup. Stromatolitic, oolitic and intraclast limestone; massive, partly cross bedded, commonly with erosional base.||||||23-DEC-09
2557|Brighton Limestone|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Nepouie Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
2557|Brighton Limestone|62903|5|Briefly described|p729, p730 Fig.1|||Adelaide Rift Complex. Sag-phase sedimentation.||||Brighton Limestone and Upalinna Subgroup, Lower, overlie the Tapley Hill Formation.||
2557|Brighton Limestone|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Umberatana Group.||||
2557|Brighton Limestone|64282|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Geosyncline. Grey interbedded siltstone and calcareous sandstone with thin sequence of bedded coarsely crystalline marble; no sedimentary structures preserved.||||||23-DEC-09
2557|Brighton Limestone|64797|5|Briefly described|p153 Fig.2, p159-163, p164 Fig.11 |||See also p166 Tb.8, p168 Tb.11, p169 Fig.12, p172 Tb.13. S-isotope data.||||||
2557|Brighton Limestone|64846|6|Mentioned|p198|Cryogenian|Cryogenian|The southern and central parts of an extensive carbonate platform across the Adelaide Geosyncline.|||||Limestones.|
2557|Brighton Limestone|65493|6|Mentioned|p923|||Presents evidence of low sea level, late-Sturtian. ?Correlated with Balcanoona Formation.||||||
2557|Brighton Limestone|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||||Underlies the Willochra Subgroup (Angepena Formation); overlies and is equivalent to the Tapley Hill Formation.||26-APR-12
2557|Brighton Limestone|67180|5|Briefly described|p600|Cryogenian|Cryogenian|Mawson and Sprigg (1950) defined the Sturtian-Marinoan Time Series boundary at the upper contact of this unit; however this is generally a gradational boundary and is therefore difficult to constrain chronostratigraphically. ||||Equivalent to Balcanoona Formation.||
2557|Brighton Limestone|67979|6|Mentioned|p528|Sturtian|Sturtian|The Sturtian-Marinoan Series boundary was first defined at the uppermost contact of the Brighton Limestone south of Adelaide. Regional inconsistency of this unit makes reliable placement of Sturtian-Marinoan Series boundary away from type area difficult. Previously thought to correlate with Balcanoona Formation in Northern Flinders Ranges (Mawson and Sprigg 1950). ||||||
2557|Brighton Limestone|69019|6|Mentioned|p49.|Neoproterozoic|Neoproterozoic|Southern Adelaide Geosyncline. Has many similarities with Balcanoona Formation.||||||
2557|Brighton Limestone|69023|6|Mentioned|p67|||Southern end of the Adelaide Geosyncline. Has many similarities with Balcanoona Formation.||||||
2557|Brighton Limestone|70031|4|Described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Lower interglacial succession; waning stages of Sturtian glaciation. Thickness: 30m. Shoaling up condtions from the underlying Tapley Hill Formation, and restricted to the western margin of the marine basin.||Unit of Nepouie Subgroup.||Uppermost unit of Nepouie Subgroup. Overlain by Angepena Formation./Upalinna Subgroup. Underlain by Tapley Hill Formation.|Ooid grainstone, stromatolite bioherms and dolostone.|
2557|Brighton Limestone|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges (local occurences), Stuart Shelf and Kulpara-Adelaide region.||||||
2557|Brighton Limestone|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Limestone, massive, oolitic, stromatolitic, ripple marks. Colour from blue-grey at base to reddish-grey at top.|
2557|Brighton Limestone|70334|4|Described|p2,20,22-23,38,47,50-54,77|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Part of a transgressive-regressive sequence with the Tapley Hill Formation, following Sturtian glacial maximum and eustatic sea level rise from melting of extensive ice sheets. Ooid grainstone and stromatolitic limestone deposited during basin shallowing/drop in relative sea level. Contains columnar, and domal stromatolites and cryptomicrobial mats, with intraclast breccia beds of tabular limestone and dolomite fragments. Regressive sequence.||Unit of Nepouie Subgroup.|Includes Bald member.|Unconformably overlain by Whyalla Sandstone or Wilmington Formation. Underlain by Tapley Hill Formation.|Pink, grey and buff stromatolitic limestone; sandy, silty or dolomitic and is blocky to flaggy, poorly-bedded or cross-bedded.|14-OCT-19
2557|Brighton Limestone|71129|5|Briefly described|p15,116,126,208|Cryogenian|Cryogenian|Of Stuart Shelf. Previously known as the Bald Member of the Tapley Hill Formation. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation. ||||Overlain by Angepena Formation.||
2557|Brighton Limestone|71237|14|Not recorded|p7, 9|||||||||
2557|Brighton Limestone|71241|14|Not recorded|p12,p9|||||||||
2557|Brighton Limestone|71895|5|Briefly described|p10|||Stuart Shelf. This unit represents shallowing marine conditions.||Umberatana Group||Conformably (gradationally) overlies the Tapley Hill Formation. Overlain by the Whyalla Sandstone.||
2557|Brighton Limestone|72247|5|Briefly described|p40,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Overlain disconformably by Angepena Formation. Underlain unconformably by Beda Basalt or Backy Point Formation.||
2557|Brighton Limestone|72450|5|Briefly described|Brochure map|||||Umberatana Group|||Massive oolitic limestone.|
2557|Brighton Limestone|72601|6|Mentioned|p5|||Adelaide Rift Complex. Possibly correlates with Ringwood Member (Aralka Formation) but this inference is tenuous.||||||
2557|Brighton Limestone|73086|6|Mentioned|p72|||Adelaide Rift Complex.||||Conformably underlain by Tapley Hill Formation. Correlates to Ringwood Member (Aralka Formation).||
2557|Brighton Limestone|73107|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||||Grey interbedded siltstone and calcareous sandstone with thin sequence of bedded coarsely crystalline marble. No sedimentary structures preserved.|
2557|Brighton Limestone|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Limestone, massive, oolitic, stromatolitic, ripple marks. Colour from blue-grey at base to reddish grey at top.|
2557|Brighton Limestone|73188|5|Briefly described|p315-316, p326-327, p330|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Nepouie Subgroup, Umberatana Group||[Conformably] underlain by Tapley Hill Formation.|Oolitic limestone.|
2557|Brighton Limestone|73226|6|Mentioned|p3||||||||Includes microbiolaminites.|
2557|Brighton Limestone|73227|6|Mentioned|p24-25|||Sturtian.||Umberatana Group||Underlain by Tapley Hill Formation.|Oolitic and stromatolitic limestone.|
2557|Brighton Limestone|73234|5|Briefly described|p6|Cryogenian|Cryogenian||c. 650 Ma|Umberatana Group|||Carbonaceous-dolomitic siltstone[?] and carbonate rocks.|
2557|Brighton Limestone|73236|4|Described|p36, p38, p47|Cryogenian|Cryogenian|Shallow marine sedimentary rocks. Not present in Hallett Cove map area. Late Sturtian; represents post-glacial transgression. Deposition under conditions of post-rift thermal subsidence.|c. 660-645 Ma|Nepouie Subgroup, Umberatana Group, Heysen Supergroup||Underlain by Tapley Hill Formation. Overlain by Angepena Formation (Upalinna Subgroup).|Blue-grey, oolitic and sandy limestone.|
2557|Brighton Limestone|74367|6|Mentioned|p7 Fig.6|||||||||
2585|British Empire Granite|22631|6|Mentioned|p176|Ashgill|Ashgill|442+/-6 Ma||||||
2585|British Empire Granite|22725|6|Mentioned|p241||Cambrian|||||||
2585|British Empire Granite|23775|5|Briefly described|p722 Fig 1||Ordovician|||||||22-SEP-09
2585|British Empire Granite|24546|5|Briefly described|p2 - 4 Fig.3|Paleozoic|Paleozoic|Includes coarse leucogranite znc granodiorite. Geological Province: Adelaide Fold Belt.||||||07-NOV-08
2585|British Empire Granite|24593|5|Briefly described|p614, p619-620|Ordovician|Ordovician|Formerly Mudnawatana Granite, assumed then to be Ordovician (Coats and Blissett, 1971).  But possibly of Cambrian age depending on assumed age of Delamerian Orogeny at the time (Sandiford, 1998).  Age: ~440 Ma.  Two phases: S-type and I-type granites.||||||06-APR-22
2585|British Empire Granite|35397|4|Described|p96|||Petrography described on p97.||||||23-JAN-19
2585|British Empire Granite|36244|6|Mentioned|p2|||Refers to Teale 1979.||||||
2585|British Empire Granite|41258|6|Mentioned|p22|||Formerly Mudnawatana Granite||||||
2585|British Empire Granite|44133|5|Briefly described|p55-56 Table 7.3|Silurian|Ordovician|Geological Province: Mount Painter Inlier. Fine to medium grained muscovite granite. Age: 442 +/- 6Ma. S-Type.||||||28-SEP-12
2585|British Empire Granite|61523|5|Briefly described|p9 Fig.2|Cambrian|Cambrian|Rounded tors of the Younger Granite Suite. Geological Provice: Mount Painter Inlier.||||||
2585|British Empire Granite|62962|5|Briefly described|p2283, p2283 Fig. 1(c), p2284 Fig. 2|Paleozoic|Paleozoic|Geological Province: Mount Painter Province. Age: between 449 and 441Ma (U-Pb isochron). A pegmatoidal garnet-muscovite granite. S-Type. See also p2285.||||||07-FEB-11
2585|British Empire Granite|63141|5|Briefly described|p544, p562, p566|||Intrusive I-type granite. Age: 440 Ma. Also, age for the I-phase: 441+/-1Ma (U-Pb monazite; Elburg et al 2003).||||||06-APR-22
2585|British Empire Granite|65313|5|Briefly described|p577|Llandovery|Late Ordovician|U-Pb isochron dates 446.3 +/- 2.2 and 441.1 +/- 2.1 Ma.||||||26-MAR-12
2585|British Empire Granite|67430|6|Mentioned|p36, 39, 56, 58|Ordovician|Ordovician|Elburg et al. (2003). Mount Painter Inlier.|~460-440 Ma.||||One of a suite of leucogranites and pegmatites. S-type. Contains K-feldspar, quartz, muscovite, garnet, and accessory tourmaline.|
2585|British Empire Granite|67536|5|Briefly described|Map Legend|Lochkovian|Katian|Kanmantoo Province; basement to Murray Basin.|ca. 442 +/- 6 Ma - 427 +/- 133 Ma||||Late/post-Delamerian felsic intrusive rocks.|
2585|British Empire Granite|68205|5|Briefly described|p85|||Emplaced/intruded during an Orodvician tectonic event 440-460 Ma. Peraluminous in composition and related to Paralana Granodiorite. Restricted to the batholith in the Mt Painter Inlier.|||||Granite; muscovite+\-granite.|
2585|British Empire Granite|68715|6|Mentioned|p32 Fig.6|||Mawson Plateau.||||||
2585|British Empire Granite|69019|5|Briefly described|p71, p145.|Silurian|Ordovician|Mt. Painter Inlier. Considered by Teale (1979) as comagmatic with Mudnawatana Tonalite.|442 +/- 6 Ma (Rb-Sr; Teale and Mortimer 1995).|||||
2585|British Empire Granite|69023|5|Briefly described|p76, p147|||Mount Painter Inlier: Mawson Plateau, ~20km N of Arkaroola. Considered by Teale (1979) to be comagmatic with Mudnawatana Tonalite, which had a Rb-Sr age determined by Teale and Mortimer (1995) of 427 +/- 133 Ma.|442 +/- 6 Ma Rb-Sr: Teale and Mortimer (1995).|||||
2585|British Empire Granite|69562|5|Briefly described|p671 Tb.5, p673 Fig.5||||455 +/- 8 Ma (Edburg et al. 2003).||||Granite batholith with S-type intruded by I-type.|
2585|British Empire Granite|70383|5|Briefly described|p44|Late Ordovician|Late Ordovician|Mawson Plateau, Mount Painter Inlier. Isotope geochemistry indicates a crustal source for the melt.|c.450-440 Ma (McLaren et al., 2006).|||||
2585|British Empire Granite|70384|5|Briefly described|Map legend.|Silurian|Ordovician|The three facies are mapped separately.|448 +/- 7 Ma (garnet) to ~440 Ma (monazite).||||Medium- to coarse-grained low melt granite, alkaline, S-type, microcline, quartz, muscovite and rare garnet, post-tectonic. Fine- to medium-grained, equigranular I-type granite. Highly radioactive granite, as determined by aerial radiometric survey.|
2585|British Empire Granite|72459|5|Briefly described|p58, p67-68, p73, p90-93, p98, p100|Delamerian|Mesoproterozoic|Mt Painter/Babbage inliers. Originally defined by Teale (1979). Together with the Mudnawatana Tonalite, the Gordon Springs Granodiorite and the Paralana granodiorite forms so called group 3 of this study. Outcrops as a ""tadpole-shaped"" pluton in the central Mount Painter Inlier. This unit can be quite heterogenous as demonstrated by mapping of Paul (1998). Appears in radiometrics as an ovoid pink body in central Mt Painter Inlier grading into a thin blue-white tail. Chemistry is discussed.|||||Muscovite bearing granite with minor biotite and garnet.|
2585|British Empire Granite|73061|6|Mentioned|p1068|Llandovery|Late Ordovician|Mount Painter Province, Mount Painter Inlier. S-type granite.|440-450 Ma||||Granite.|
2585|British Empire Granite|73251|6|Mentioned|p36-37|earliest Silurian|Late Ordovician|Flinders Ranges, Mount Painter and Mount Babbage inliers. Source of uranium for deposits on the Paralana High Plains.|c. 442 Ma|||||
2585|British Empire Granite|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
2617|Broken Hill Group|6823|6|Mentioned|p203, 205, 210, 221, 234, 236|Palaeoproterozoic|Palaeoproterozoic||ca >1690 Ma|Willyama Supergroup|Includes the Hores Gneiss.|||26-MAR-22
2617|Broken Hill Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent WIllyama Supergroup Geol province Broken Hill - Olary Domain||||||
2617|Broken Hill Group|22500|4|Described|p 1, 3, 13, 14|||Of the Willyama Supergroup.||||||18-JAN-07
2617|Broken Hill Group|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
2617|Broken Hill Group|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
2617|Broken Hill Group|22588|6|Mentioned|p85|||||||||
2617|Broken Hill Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
2617|Broken Hill Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22665|6|Mentioned|P231|||||||||
2617|Broken Hill Group|22720|6|Mentioned|p 168|||||||||
2617|Broken Hill Group|22771|5|Briefly described|p40-42,48|||||||||
2617|Broken Hill Group|22789|6|Mentioned|p50|||||||||
2617|Broken Hill Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Supersedes the Broken Hill Suite.  Max. thickness: 2000m. Geological Province: Willyama Fold Belt.|Age: 1690+/-5 Ma|Of Willyama Supergroup||||11-MAR-10
2617|Broken Hill Group|22884|5|Briefly described|p40 Fig1, p43 Fig. 3||Paleoproterozoic|||||||26-MAR-09
2617|Broken Hill Group|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22956|6|Mentioned|p147||Proterozoic|||||||
2617|Broken Hill Group|22959|4|Described|p95||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22960|5|Briefly described|p92||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22962|5|Briefly described|p73||Statherian|||||||
2617|Broken Hill Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Fullarton River Group of the Mt Isa Maronan Supergroup, and the lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
2617|Broken Hill Group|22964|5|Briefly described|p54,55,56||Proterozoic|||||||
2617|Broken Hill Group|22965|6|Mentioned|p13,14,Fig1||Statherian|||||||
2617|Broken Hill Group|22966|5|Briefly described|p2,3,4||Proterozoic|Rift stage of development.||||||
2617|Broken Hill Group|22967|5|Briefly described|p25,6,30-2,9,41,2,5,||Statherian|||||||
2617|Broken Hill Group|23025|6|Mentioned|p76|||||||||
2617|Broken Hill Group|23039|6|Mentioned|p166||Statherian|||||||
2617|Broken Hill Group|23093|5|Briefly described|p619|||||||||
2617|Broken Hill Group|23160|5|Briefly described|p870 fig1|||||||||
2617|Broken Hill Group|23196|6|Mentioned|p830|||||||||
2617|Broken Hill Group|23223|5|Briefly described|p42|||Informally divided into upper and lower.  Of the informal Upper Willyama Supergroup.  In the Curnamona Province.||||||18-JAN-07
2617|Broken Hill Group|23248|5|Briefly described|Fig2p169, 179|||||||||
2617|Broken Hill Group|23346|6|Mentioned|48|||||||||
2617|Broken Hill Group|23347|5|Briefly described|p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
2617|Broken Hill Group|23461|5|Briefly described|p202|||||||||
2617|Broken Hill Group|23476|5|Briefly described|p50|||Underlain by the  'Bimba Formation'.||||||29-MAY-07
2617|Broken Hill Group|23565|5|Briefly described|p195|||||||||
2617|Broken Hill Group|23912|5|Briefly described|p779|||Of the Willyama Supergroup.||||||
2617|Broken Hill Group|23966|5|Briefly described|p1309|Proterozoic|Proterozoic|Age: 1690 +/- 5Ma.||||||
2617|Broken Hill Group|24197|5|Briefly described|p62, p132|||Of the Willyama Supergroup. Shallow marine unit. Includes Hores Gneiss and Silver King Formation. Geological province: Broken Hill Block.||||||07-FEB-11
2617|Broken Hill Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
2617|Broken Hill Group|38969|4|Described|p208|||||||||
2617|Broken Hill Group|39662|2|Defined|p422|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39674|6|Mentioned|p204|||||||||
2617|Broken Hill Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39849|6|Mentioned|p87|||||||||
2617|Broken Hill Group|39883|6|Mentioned|p380|||||||||
2617|Broken Hill Group|40290|6|Mentioned|p1|||||||||
2617|Broken Hill Group|40595|6|Mentioned|p85|||||||||
2617|Broken Hill Group|40822|6|Mentioned|Fig.2|||||||||
2617|Broken Hill Group|41093|4|Described|p253|||||||||
2617|Broken Hill Group|41145|5|Briefly described|p827|||||||||
2617|Broken Hill Group|41630|5|Briefly described|p6|||See also Table 1.5.||||||
2617|Broken Hill Group|41633|6|Mentioned|p145|||||||||
2617|Broken Hill Group|41651|6|Mentioned|p189|||||||||
2617|Broken Hill Group|41652|6|Mentioned|p193|||||||||
2617|Broken Hill Group|42098|6|Mentioned|p57|||||||||
2617|Broken Hill Group|42171|6|Mentioned|p142|||||||||
2617|Broken Hill Group|42181|6|Mentioned|Fig,1 P252|||||||||
2617|Broken Hill Group|42261|6|Mentioned|p529|||See also Fig.1 P530||||||
2617|Broken Hill Group|42286|6|Mentioned|p7|||||||||
2617|Broken Hill Group|42323|4|Described|p3-4|||Depositional age 1680-1690 Ma.||||||29-MAY-07
2617|Broken Hill Group|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42537|4|Described|p12|||||||||
2617|Broken Hill Group|42595|6|Mentioned|Fig. 2 P5|||||||||
2617|Broken Hill Group|42672|5|Briefly described|p372|||||||||
2617|Broken Hill Group|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42813|6|Mentioned|p9|||||||||
2617|Broken Hill Group|42819|5|Briefly described|p316|||||||||
2617|Broken Hill Group|42897|5|Briefly described|Fig.3 P321|||||||||
2617|Broken Hill Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
2617|Broken Hill Group|43052|5|Briefly described|p82,Fig.4.22|||Of Willyama Supergroup. Deposition at about 1690+/-5 Ma.||||||18-JAN-07
2617|Broken Hill Group|43086|6|Mentioned|p3|||||||||
2617|Broken Hill Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|43264|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43572|5|Briefly described|p5|||||||||
2617|Broken Hill Group|43583|4|Described|p2138||Proterozoic|Age: 1690+/-5 Ma.  Of Willyama Supergroup.||||||18-JAN-07
2617|Broken Hill Group|43591|6|Mentioned|p162|||||||||
2617|Broken Hill Group|43595|5|Briefly described|p355|||||||||
2617|Broken Hill Group|44195|6|Mentioned|p349|||||||||
2617|Broken Hill Group|46598|4|Described|p303|||||||||
2617|Broken Hill Group|50045|4|Described|p115 Fig. 2, p116, p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Sundown Group; underlain by Thackaringa Group. Age: 1690 Ma. Includes Purnamoota Subgroup. Package of pelitic to psammopelitic metasediments and minor calc-silicate rocks,|Age: 1690 Ma|||||10-DEC-09
2617|Broken Hill Group|50606|5|Briefly described|p1.1|||Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||27-JUL-04
2617|Broken Hill Group|50619|5|Briefly described|p174 Fig 1, p175|Paleoproterozoic|Paleoproterozoic|Conformably overlies the Thackaringa Group; conformably overlain by the Sundown Group.  Geological Province: Broken Hill Block.||Of the Willyama Supergroup||||28-FEB-13
2617|Broken Hill Group|60485|5|Briefly described|p27 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Domain.||||||07-NOV-08
2617|Broken Hill Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
2617|Broken Hill Group|61605|5|Briefly described|p769|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill domain.||||||07-NOV-08
2617|Broken Hill Group|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||
2617|Broken Hill Group|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Age: ca.1693-1683 Ma. Discussed from a geochronological aspect. Geological province: Broken Hill Domain. See also p636 Fig. 2.||||||04-JUN-15
2617|Broken Hill Group|61736|4|Described|p663|Paleoproterozoic|Paleoproterozoic|Comprises Allendale Metasediments, Parnell Formation, Freyers Metasediments and Hores Gneiss. Geological province: Broken Hill Domain.||||||24-FEB-10
2617|Broken Hill Group|61908|5|Briefly described|p146|||Geological Province: Broken Hill Block.||||||
2617|Broken Hill Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province. ||||||
2617|Broken Hill Group|62373|6|Mentioned|p502, p503|Paleoproterozoic|Paleoproterozoic|In Broken Hill region, NSW. Geological Province: Curamona Province/Broken Hill Domain.||||||07-NOV-08
2617|Broken Hill Group|62473|5|Briefly described|p72, p74|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||17-JUN-09
2617|Broken Hill Group|62535|5|Briefly described|p663-667, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, SE Curnamona Province. Time-equivalent to the Prize Supersequence. Hosts rich strata-bound Pb-Zn-Ag mineralization.|~1695-1685 Ma.|Willyama Supergroup.|Hores Gneiss.|||
2617|Broken Hill Group|62536|5|Briefly described|p633-636, 638, 643-644, 646-647, 655|||See also p658. Broken Hill area. The upper part of this unit hosts the Pb-Zn-Ag orebody. The package was deposited within a period of 10 m.y. Similar zircon provenance ages as Sundown Group and upper Paragon Group.|1693 +/- 4 Ma to 1685 +/- 3 Ma (dep'n).|Willyama Supergroup.|Allendale, Freyers Metasediments; Parnell Formation; Hores, Rasp Ridge Gneisses.|Is overlain by Sundown Group.||
2617|Broken Hill Group|62592|5|Briefly described|p14, p16 Fig.2.2.|||Formed during crustal extension. Hosts the 300 mt Broken Hill Pb-Zn-Ag deposit.||Unit in Willyama Supergroup.|Includes Allendale and Fryers Metasediments; Purnamoota Subgroup; Silver King Formation and Ettlewood Calc-silicate Member.|Intruded by Lady Louise Suite. Is overlain by Sundown Group.|Metasediments, mafic and felsic igneous rocks.|
2617|Broken Hill Group|62728|5|Briefly described|p25 Fig. 2|||Geological Province: Curnamona Province.||||||07-FEB-11
2617|Broken Hill Group|62993|5|Briefly described|p1, 2, 4, 8, 12, 14,  18, 19, 35, 37, 39|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.Broken Hill Group equivalents in the Olary Domain discussed p6.||Willyama Supergroup|Includes Purnamoota Subgroup, Allendale Metasediments|Correlated with parts of the Saltbush Group.||19-DEC-21
2617|Broken Hill Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
2617|Broken Hill Group|63102|5|Briefly described|p6,9-11,13-14,26-27,30,32-34,36,38|||Geological province: Broken Hill Domain, Curnamona Province. See also p44, p53, ,58-60.|||Includes Parnell Formation and Hores Gneiss.|Equivalent to Oonatra Creek Formation and Plumbago Formation.||22-OCT-19
2617|Broken Hill Group|63110|6|Mentioned|p1129 Fig. 8, p1131|||Comprises metasedimentary and metavolcanic rocks.||||||11-JUN-08
2617|Broken Hill Group|63186|5|Briefly described|p66, p67, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1695 Ma and 1594+/-17 Ma (monazite mean). Geological Province: Broken Hill Domain, Curnamona Province. Intruded by Rasp Ridge and Hores Gneisses.||||||07-NOV-08
2617|Broken Hill Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasediments, garnetiferous, quartzo-feldspathic gneiss, amphibolite, minor garnet and gahnite-rich rocks, BIF in Broken Hill Domain; unnamed equivalents in Olary Domain, including Bimba Formation.||||||07-NOV-08
2617|Broken Hill Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments, Parnell Formation, Hores Gneiss and Silver King Formation. Overlain by Sundown Group; overlies Thackaringa Group. .  Age at top: 1686+/-3ma for topmost unit (Hores Gneiss). ||||||07-NOV-08
2617|Broken Hill Group|63866|4|Described|p34-p36, p38, p40|||Broken Hill Domain, Curnamona Province. Is greatly thinned or completely absent in the Olary Domain. Hosts the Broken Hill Deposit the worlds largest Pb-Zn-Ag deposit.||Willyama Supergroup|Includes the Purnamoota Subgroup and the Allendale Metasediments.|Intruded by the Rasp Ridge Gneiss. Equivalent to the Saltbush Group.||
2617|Broken Hill Group|64097|5|Briefly described|p302, p324|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metaseds, Parnell Fm, Freyers Metaseds+Hores Gneiss.Overlies Thackaringa Group. Age: ca1693-1685Ma. Geol.prov: Broken Hill Domain/Curnamona Province. Comprises siliciclastic metasediments with distinctive Potosi-type gneiss at 2 levels||||||07-FEB-11
2617|Broken Hill Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
2617|Broken Hill Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of lower Willyama Supergroup. Includes Purnamoota Subgroup and Allendale Metasediments. Overlies Thackaringa Gp. Hosts Broken Hill ore body. Geol.Prov: Broken Hill Block||||||07-FEB-11
2617|Broken Hill Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
2617|Broken Hill Group|64725|6|Mentioned|p58 Fig.2. |||||||||
2617|Broken Hill Group|64741|4|Described|p299-300, p309, p310|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments and the Purnamoota Subgp. Overlies Himalaya Fm (Thackeringa Gp); overlain by Sundown Gp. Max. thickness: 2000m. Geological province: Broken Hill Domain (restricted in Olary Domain). Manganiferous.||Of Willyama Supergroup||||07-FEB-11
2617|Broken Hill Group|64742|5|Briefly described|p319, p323, p328, p330. |Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1695-1685 Ma.|Unit in Willyama Supergroup.|Includes Ettlewood Calc-Silicate Member, Allendale Metasediments, Parnell Formation, Freyers Metasediments and Hores Gneiss.|||
2617|Broken Hill Group|64743|6|Mentioned|pp339-340, p342, p344 Fig.5. |Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|64744|6|Mentioned|p353 Fig.4, p358, p363.|Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments. Geological province: Broken Hill Domain.||||||07-FEB-11
2617|Broken Hill Group|65220|6|Mentioned|p21 Fig.4|Statherian|Statherian|and equivalents, 1685-1680 Ma||||||10-DEC-09
2617|Broken Hill Group|65407|6|Mentioned|p239 Fig.3|||||||||
2617|Broken Hill Group|65681|6|Mentioned|p734 Fig. 1.|||Broken Hill Block.||||||
2617|Broken Hill Group|65887|6|Mentioned|p51-53|||Fe-rich amphibolites from this unit are spatially and temporally associated with felsic rocks of Hores Gneiss, which has been dated at 1685 +/- 3 Ma. Is overlain by Sundown and Paragon Groups.||||||
2617|Broken Hill Group|65925|5|Briefly described|Appendix 2.||||||||Sulfide-rich ironstone; marble; plagioclase-rich metasediment; calc-silicate; siliciclastic pelite; BIF; variably brecciated amphibolite.|
2617|Broken Hill Group|66302|5|Briefly described|p8, p35-37, p39-40|||Olary Domain, Curnamona Province.||Willyama Supergroup|Includes the Allendale Metasediments and the Purnamoota Subgroup|Equivalent to the Saltbush Group.|Quartz-rich sandstone and mudstone metasedimentary rocks.|
2617|Broken Hill Group|66800|5|Briefly described|p933.|||Hosts stratabound massive sulfide mineralisation. Age of metavolcanics is given (c.1690 Ma). High-grade metamorphism dated at 1600 +/- 8 Ma.|1690 +/- 5 Ma (Page and Laing 1992).||||Includes amphibolite-facies felsic volcanics.|
2617|Broken Hill Group|66857|5|Briefly described|p972 Fig.2, p976.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Contains quartzo-feldspathic metasedimentary rocks derived from an A-type felsic igneous source; supporting an intracratonic rift setting for the development of the Willyama Supergroup.||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||See also p33-34. Broken Hill Domain, Curnamona Province. Deposited during intra-continental extension.|~1720-1685 Ma.||Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments.|Overlies Thackeringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1690 Ma|Of the Willyama Supergroup.|||Siliciclastic metasediments including calcsilicates, garnet- and gahnite-bearing rocks and calc-albites.|
2617|Broken Hill Group|67653|5|Briefly described|p4|||Geological province: Curnamona Province. ||Unit of Willyama Supergroup.||||
2617|Broken Hill Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||28-AUG-13
2617|Broken Hill Group|68126|4|Described|p6, p25-26, p29-31|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Thins and wedges out to the west.|~1695-1685 Ma (Stevens et al., 2008).|Willyama Supergroup.|Ettlewood Calc-silicate member.|Overlies Thackaringa Group. Is overlain by Sundown Group. Equivalent to Saltbush Group.|Siliciclastic metasediments and minor calc-silicates, garnet-rich BIF, quartz-gahnite rock and garnet-quartz rock.|
2617|Broken Hill Group|68315|6|Mentioned|p766|||Broken Hill district, Curnamona Province. Cut by the Stephens Creek Shear Zone.|||||Upper amphibolite-facies metapelites and felsic gneisses.|
2617|Broken Hill Group|69654|6|Mentioned|p3|||Curnamona Province.||||||
2617|Broken Hill Group|69999|5|Briefly described|p3,p9-10 Photos 12-13,p12-15,p17-18,p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Middle, rift-deepening, marine transgressive sedimentation with increased magmatic input. Represents much of the amphibolite facies for the Olarian Orogeny. Garnet-bearing rather than orthopyroxene-bearing, unlike Thackaringa Group: discussed.|||Includes Ettlewood Calc-silicate Member and Silver King Metadolerites.||Includes abundant basal calc-silicate rocks and abundant mafic igneous rocks in the upper parts.|
2617|Broken Hill Group|70000|5|Briefly described|p31, p33-34, p36-38|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Allendale Metasediments and Purnamoota Subgroup.|Conformably overlies Thackaringa Group. Is overlain by Sundown Group.|Includes siliciclastic, pelite-dominated rocks.|
2617|Broken Hill Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.|Includes basal Allendale Metasediments and Purnamoota Subgroup.|Overlies Thackaringa Group. Is overlain by Sundown Group.|Mostly comprises metasediments and interbedded quartzo-feldspathic and basic gneisses of the Purnamoota Subgroup. Zoned calc-silicate nodules are common in the metasediments.|
2617|Broken Hill Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Allendale Metasediments and Purnamoota Subgroup.|Overlies Thackaringa Group. Is overlain by Sundown Group.|Metasedimentary rock with two units of quartzofeldspathic to garnetiferous quartzofeldspathic gneiss. Calc-silicate and/or basic gneiss common in places.|
2617|Broken Hill Group|70405|5|Briefly described|P2, p15, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1680 Ma- 1700 Ma|Wilyama Supergroup|Includes, Purnamoota Subgroup, Allendale metasediments|Intruded by Lady Louise Suite, correlated with (tentatively) Oonartra Creek Formation|Glacial and glaciomarine diamictite, sandstone, siltstone ironstone and conglomerate.|
2617|Broken Hill Group|70657|4|Described|p5, p6 Fig.1, p10, p11 Fig.5, p12|Statherian|Statherian|See also,p13 Fig.6, p15-17, p20, p30-31, p33-34, p37, p39-41, p44, p51, p58, p64-66. Curnamona Province; Broken Hill, Mulyungarie Domains. Shown as Broken Hill Group and equivalents in Figs. 1 and 5. Age inferred from Fig.4. Coeval magmatism includes both felsic and mafic components. Related in time to the ~1685 Ma Parnell Formation and the Lady Louise Suite (e.g. Woman-in-White Amphibolite).|~1700-1685 Ma|Willyama Supergroup|Purnamoota Subgroup, Allendale Metasediments.|Overlies Himalaya Formation (Thackaringa Group), Plumbago Formation. Underlies Sundown Group. Intruded by Parnell Gneiss and Silver City Suite. With Sundown Group, is equivalent to Saltbush Group.||
2617|Broken Hill Group|70658|5|Briefly described|p2, 7-8, 15-16, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1693-1685 Ma.|Willyama Supergroup.|Allendale Metasediments; Purnamoota Subgroup.|(Upper part is) equivalent to Raven Hill Subgroup.||
2617|Broken Hill Group|71262|6|Mentioned|p5 Fig 2|||||||||
2617|Broken Hill Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
2617|Broken Hill Group|72435|6|Mentioned|p715||||||Hores Gneiss|||
2617|Broken Hill Group|72454|5|Briefly described|p2 Fig.2,  p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain.||Willyama Supergroup|Includes Ettlewood Calc-silicate Member||Includes calc-silicates.|
2617|Broken Hill Group|72461|4|Described|p5-6, p13, p16|||Magmatism including volcanism and intrusion were syn-genetic with deposition of this group. Magmatism ended with emplacement of the Broken Hill ore body at the top of the group at 1685 Ma.||Willyama Supergroup|Includes the Hores Gneiss, Allendale Metasediments, Parnell Gneiss, and the Freyers Metasediments.|Overlies the Thackaringa Group. Overlain by the Sundown Group.|Fine grained sedimentarty rocks including shale and minor horizons of calcium- or magnesium-bearing rocks (limestones).|
2617|Broken Hill Group|73021|6|Mentioned|p224, 226|||||Willyama Supergroup.|Hores Gneiss; Bimbo, Plumbago Formations.|||
2617|Broken Hill Group|73243|6|Mentioned|p52-53, p58-59, p61, p64, p66-67, p72|Statherian|Statherian|Broken Hill block-Euriowie block. Amphibolite bodies are mostly concordant or near-concordant with bedding, interpreted as sills. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites. Shown on p52 Fig.1, p53 Fig.2 and p76.||Willyama Supergroup|||Contains amphibolite sills emplaced during or immediately after deposition.|
2617|Broken Hill Group|73308|4|Described|p605-607, 611-612, 618, 622|||Broken Hill Block. Hydrothermal plumes are proposed as the source of much of these magnetite deposits.|c.1693-1685 Ma.|Willyama Supergroup.|Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments.|Is overlain by Sundown Group.|Metasediments including BIFs; contain small amounts of bedding-controlled magnetite.|
2617|Broken Hill Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province. Broken Hill Domain, Mulyungarie Domain.||Willyama Supergroup, upper|Allendale Metasediments, Purnamoota Subgroup|Underlies Sundown Group||
2617|Broken Hill Group|73482|5|Briefly described|p419, p422-423, p425-427, p430, p432-433|||Areas of stratigraphy are parallel to the andalusite-sillimanite isograd, in other areas the isograd crosses stratigraphy. Hosts pegmatitic masses. See also p424 Fig.4, p429 Fig.8.||Willyama Supergroup|Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments|Overlies Thackaringa Group, underlies Sundown Group|Metasediments. Andalusite and silimanite metamorphic grades, partially melted in parts.|
2617|Broken Hill Group|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Fluviatile to shallow marine successions.||Willyama Supergroup||Underlain by Thackaringa Group. Overlain by Sundown Group.||
2617|Broken Hill Group|73524|5|Briefly described|p2-4|Statherian|Statherian|Rift-phase metasediments.|1693-1685 Ma|lower Willyama Supergroup|Freyers Metasediments, Hores Gneiss, Parnell Formation, Allendale Metasediments||Metasedimentary rocks.|
2617|Broken Hill Group|73575|5|Briefly described|p828 Fig.2, p835-836, p838-839, p841|Statherian|Statherian|See also p829 Fig.3, p830, p832.||Willyama Supergroup|Allendale Metasediments, Purnamoota Subgroup|Overlies Thackaringa Group, underlies Sundown Group||
2637|Brooks Member|39047|4|Described|p806|||||||||
2637|Brooks Member|41125|6|Mentioned|Fig.18|||||||||
2637|Brooks Member|41493|5|Briefly described|Table 2|||||||||
2637|Brooks Member|42022|6|Mentioned|p5|||||||||
2672|Brown Hill Subgroup|24465|5|Briefly described|p346 Fig.3|||Together with Wattaberri Subgroup, replaced by Bollaparudda Subgroup.||||||19-JAN-05
2672|Brown Hill Subgroup|36836|6|Mentioned|Table 1|||||||||
2672|Brown Hill Subgroup|41253|6|Mentioned|p57|||||||||
2672|Brown Hill Subgroup|60712|5|Briefly described|p30 Fig. 3|Early Cambrian|Early Cambrian|Of Daily and Milnes (1972, 1973). Of the Kanmantoo Group.  Includes the Tunkalilla and Balquhidder Formations.||||||
2697|Bruce Formation|29780|6|Mentioned|p51|||||||||
2718|Brunette Limestone|24303|4|Described|p42|Miocene|Miocene|Max. Thickness: 4.6m. Max. Thickness in BRUNETTE DOWNS: 18m (Randal, 1966)||||||
2718|Brunette Limestone|24304|5|Briefly described|Map legend|Miocene|Miocene|White chalcedonic limestone with chert nodules and chalcedony; minor sandstone.||||||
2718|Brunette Limestone|32418|6|Mentioned|p2|||||||||
2718|Brunette Limestone|34151|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
2718|Brunette Limestone|34441|4|Described|Table 1|||Tertiary. pp15,18||||||02-AUG-06
2718|Brunette Limestone|36213|6|Mentioned|p86|||||||||
2718|Brunette Limestone|36335|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
2718|Brunette Limestone|44221|14|Not recorded|p87,88,89,90,102|||||||||
2718|Brunette Limestone|44222|14|Not recorded|p119||Miocene|Miocene?||||||
2718|Brunette Limestone|44283|14|Not recorded|p.8,9.||Tertiary|Alroy Sheet. (E53-15).||||||
2718|Brunette Limestone|44284|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44285|14|Not recorded|p.9|||May have been deposited in similar marine environment to Austral Downs Limestone.||||||
2718|Brunette Limestone|44301|2|Defined|map, p.9,10||Tertiary|Brunette Downs sheet. (E53-11).||||||
2718|Brunette Limestone|44302|14|Not recorded|map legend||Tertiary|Nodular white limestone, minor quartz sandstone and conglomerate fossiliferous Tertiary; laterite.||||||
2718|Brunette Limestone|44441|2|Defined|p.10||Cenozoic|opp.p.6,Tb.1,map. (E53-16).||||||19-NOV-08
2718|Brunette Limestone|44442|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44473|14|Not recorded|p.12, opp. p.7|||(E53-7).||||||
2718|Brunette Limestone|44474|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44482|14|Not recorded|opp.p.6|||(E53-12).||||||
2718|Brunette Limestone|44965|14|Not recorded|Not recorded|||||||||
2718|Brunette Limestone|45032|14|Not recorded|p8,12||Tertiary|Tb.1., Pl.1.||||||
2718|Brunette Limestone|45052|4|Described|p136|||Cainozoic||||||
2718|Brunette Limestone|45064|4|Described|Table 1|||||||||
2718|Brunette Limestone|45148|4|Described|p24|||||||||
2718|Brunette Limestone|48925|6|Mentioned|p13|||Fauna. Miocene ? age||||||
2718|Brunette Limestone|60637|5|Briefly described|Map legend|||White chalchedonic limestone with chert nodules, chachedony, some sandstone.||||||
2718|Brunette Limestone|60703|6|Mentioned|p714, p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
2718|Brunette Limestone|61155|5|Briefly described|p16|Middle Miocene||Age: <11.5Ma. Thickness: 12m.  Geological region: Barkly Tableland.||||||03-MAR-10
2718|Brunette Limestone|62657|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Limestone: cherty and chalcedonic||||||
2718|Brunette Limestone|64068|5|Briefly described|p79, p43|Cenozoic|Cenozoic|Central Georgina Basin. Coeval with Austral Downs Limestone, but occupies a distinct drainage system. Lower part correlated with Poodyea Formation.||||||
2718|Brunette Limestone|64443|5|Briefly described|iii, p5 Fig.3, p6 Tb.1, p18-24, p31|Neogene|Miocene|Max 18m thick. Lithologically identical with Austral Downs Limestone; distinguished geographically: this unit is within drainage areas centred on lakes in south-central BRUNETTE DOWNS.||||Unconformably overlies Camooweal Dolostone, Ranken Limestone and Wonarah Formation.|Limestone, silicified to chert and chalcedony. Characteristic features include rhizoliths, Cambrian pebbles, alveolar texture, circum- and intragranular cracks.|14-MAY-14
2718|Brunette Limestone|65336|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Cherty and chalcedonic limestone. Unconformably overlies Camooweal Dolostone of Barkly Group.||||||
2718|Brunette Limestone|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In BRUNETTE DOWNS, ALROY and RANKEN areas. May correlate with Cleanskin beds, Austral Downs Limestone and Golliger beds.||||||
2718|Brunette Limestone|65344|5|Briefly described|p3 Fig. 2, p7 Tables 1, 2, p13, 45-47|Miocene|Miocene|Of the Barkly Sub-basin, Georgina Basin. Thickness: 6.5m in BN04DD01. See thin section descriptions for detail.||||Overlies the Anthony Lagoon beds.||03-MAY-12
2718|Brunette Limestone|67144|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67149|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67150|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67352|4|Described|v,p23,p25,p34-35,p38-40,p47,p51,p69|Miocene|Miocene|Noakes and Traves (1954). From 5 to 18 m thick.||||Overlies Anthony Lagoon Formation unconformably.|Massive, nodular to brecciated or tuffaceous, pale grey terrestrial carbonate rocks: dolomicrosparstone or mixed calci/dolomicrosparstone; selectively silicified to chert, megaquartz and chalcedony.|
2718|Brunette Limestone|69443|6|Mentioned|p28:22|Miocene|Miocene|||||Unconformably overlies Anthony Lagoon Formation.||12-JUL-16
2718|Brunette Limestone|69458|5|Briefly described|p42:19-21|||Noakes and Traves (1954). Up to 18m thick. Scattered rubbly outcrops with local prominent outcrops of strongly silicified limestone. Contains rhizoliths, petrified plant roots, minor alveolar texture, clay cutans, and rare Microidium.||||Overlies Golliger beds and (unconformably) Anthony Lagoon Formation. Is correlated with the Austral Downs Limestone.|Massive, nodular to brecciated or tuffaceous, pale grey terrestrial carbonate rocks: calci/dolomicrosparstone, selectively silicified to white, purple-brown and/or red/brown nodular chert, megaquartz and chalcedony.|14-SEP-18
2718|Brunette Limestone|72516|6|Mentioned|p98|Neogene|Neogene|Western and central Georgina Basin. Interpreted to be an age equivalent of the Waite Formation of the Waite Basin.||||||09-JUN-21
2796|Buckleboo Granite|33557|6|Mentioned|p12|||||||||
2796|Buckleboo Granite|65390|5|Briefly described|p26 Tb.1|Calymmian|Calymmian|Of Hiltaba Suite. Pinkish, coarse-grained granite-adamellite, minor porphyritic varieties and minor aplite dykes. Aged 1477 +/- 34 Ma (Rb-Sr: Webb et al., 1986).||||||
2796|Buckleboo Granite|66302|6|Mentioned|p46||||1586 +/- 6 Ma (SHRIMP, Fraser and Neumann, 2010)|Hiltaba Suite||||
2796|Buckleboo Granite|67028|6|Mentioned|p362, p364 Tb.1, p365, p373|Calymmian|Calymmian|information on magnetic characteristics presented. Kokatha-type.||Hiltaba Suite Granitoids||||10-AUG-15
2873|Bulgunnia Diorite|31731|6|Mentioned|p122|||Description of Muckanippie gold prospect||||||
2876|Bull Creek Loam|38290|5|Briefly described|p59|||||||||
2891|Bulldog Shale|12597|5|Briefly described|p492 Tb.1, p499-500|Albian|Aptian|SW Eromanga Basin. 200-320m thick.|||||Includes a basal organic mudstone, 25m thick, with a distinctive gamma-ray response.|
2891|Bulldog Shale|13497|5|Briefly described|p115 fig 6.33, p151-p154, p170-p171|Early Cretaceous|Early Cretaceous|Eromanga Basin. Forms a regional oil and gas seal. ||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Coorikiana Sandstone and the Oodnadatta Formation.||
2891|Bulldog Shale|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Marree Subgroup||||
2891|Bulldog Shale|22874|6|Mentioned|P18|||||||||
2891|Bulldog Shale|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Coorikiana Sandstone, underlying unit is Wyandra Sandstone Member||||||
2891|Bulldog Shale|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
2891|Bulldog Shale|22922|6|Mentioned|33 fig 2|||||||||
2891|Bulldog Shale|23054|4|Described|p21,24-5|||||||||
2891|Bulldog Shale|23056|6|Mentioned|12 table 2|||||||||
2891|Bulldog Shale|23123|5|Briefly described|p404||Cretaceous|||||||
2891|Bulldog Shale|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Marree Subgroup of the Neales River Group.||||||
2891|Bulldog Shale|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age Determinations discussed on p 30.||||||
2891|Bulldog Shale|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
2891|Bulldog Shale|23341|6|Mentioned|18|||||||||
2891|Bulldog Shale|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Wallumbilla Formation. Of Eromanga Basin.||||||31-JAN-08
2891|Bulldog Shale|23818|5|Briefly described|p141 Fig.65, p144 Fig.66, p156|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Neales River Group. Underlying unit: Cadna-owie Formation. Max. thickness: 1500 ft.||||||
2891|Bulldog Shale|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
2891|Bulldog Shale|23849|5|Briefly described|p777|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|23879|5|Briefly described|p20|Early Cretaceous|Early Cretaceous|Max. thickness: 110m.||||||
2891|Bulldog Shale|23982|5|Briefly described|p57|||Of Neales River Group.  Geological Province: Great Artesian Basin.||||||
2891|Bulldog Shale|24085|5|Briefly described|p33, p38, p41|Albian|Albian|Geological Province: Eromanga Basin.||||||16-MAR-05
2891|Bulldog Shale|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24112|5|Briefly described|p254 Fig.2, p270|Early Cretaceous|Early Cretaceous|Max. Thickness: 2000m. Geological Province: Eromanga Basin||||||
2891|Bulldog Shale|24175|3|Fully described|p22, p17 Fig. 3|Albian|Aptian|Dark grey, bioturbated shaly mudstone with silty and very fine sandy layers. Locally includes Wilpoorinna Breccia Member at its base.  Geological Province: Eromanga Basin.||||||16-SEP-08
2891|Bulldog Shale|24204|5|Briefly described|p263 Fig.4, p266 Fig.7|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24321|5|Briefly described|Map legend|Maastrichtian|Maastrichtian|Parent: Neales River Group (of the Marree Subgroup).||||||
2891|Bulldog Shale|24392|5|Briefly described|p140, p142|Albian|Aptian|Overlies the Cadna-owie Formation disconformably. Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24506|5|Briefly described|p17|Mesozoic|Mesozoic|Marine mudstone.||||||
2891|Bulldog Shale|29379|4|Described|p28|||Information on lithology. Lower Cretaceous.||||||
2891|Bulldog Shale|29651|6|Mentioned|p25|||||||||
2891|Bulldog Shale|30540|6|Mentioned|Fig.6|||||||||
2891|Bulldog Shale|30803|6|Mentioned|p1|||Cretaceous||||||
2891|Bulldog Shale|30804|6|Mentioned|p10|||See also Table 1||||||
2891|Bulldog Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
2891|Bulldog Shale|30917|6|Mentioned|p42|||See also P53||||||
2891|Bulldog Shale|30919|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|30921|6|Mentioned|Map legend|Turonian|Albian|Neocomian - Turonian||||||
2891|Bulldog Shale|30924|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|31208|6|Mentioned|p46|||See also Fig. 7||||||
2891|Bulldog Shale|31244|6|Mentioned|Table 1|||Lower Cretaceous. See also P6.||||||
2891|Bulldog Shale|31251|6|Mentioned|p75|||Microflora & Microplankton||||||
2891|Bulldog Shale|31699|4|Described|p133|||Lower Cretaceous||||||
2891|Bulldog Shale|31923|6|Mentioned|p14|||||||||
2891|Bulldog Shale|32033|6|Mentioned|p2|||||||||
2891|Bulldog Shale|32313|6|Mentioned|p165|||||||||
2891|Bulldog Shale|32314|6|Mentioned|Fig. 4|||||||||
2891|Bulldog Shale|33017|6|Mentioned|p5|||||||||
2891|Bulldog Shale|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
2891|Bulldog Shale|33224|6|Mentioned|Fig.33|||Photo.||||||
2891|Bulldog Shale|33490|6|Mentioned|p30|||Correlation. Cretaceous sediments||||||
2891|Bulldog Shale|33491|4|Described|p56|||Mention Fig.2||||||
2891|Bulldog Shale|33521|5|Briefly described|p8|||||||||
2891|Bulldog Shale|33523|6|Mentioned|p17|||||||||
2891|Bulldog Shale|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
2891|Bulldog Shale|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
2891|Bulldog Shale|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
2891|Bulldog Shale|33824|6|Mentioned|p12|||Table 2||||||
2891|Bulldog Shale|33825|5|Briefly described|p8|||Strat. table. Lithology||||||
2891|Bulldog Shale|33827|6|Mentioned|p13|||Table 2||||||
2891|Bulldog Shale|33828|6|Mentioned|p5|||Table 1||||||
2891|Bulldog Shale|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
2891|Bulldog Shale|33832|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|33933|6|Mentioned|Fig.4|||||||||
2891|Bulldog Shale|33936|6|Mentioned|Fig.3A|||Cret.||||||
2891|Bulldog Shale|33938|6|Mentioned|p38|||O'lain by Eyre Fm.||||||
2891|Bulldog Shale|33939|6|Mentioned|p385|||L.Cret.||||||
2891|Bulldog Shale|33971|5|Briefly described|p37|||See also Fig. 15.||||||
2891|Bulldog Shale|33976|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|34136|6|Mentioned|Fig.|||Lower Cretaceous.||||||
2891|Bulldog Shale|34611|6|Mentioned|Fig.66|||Cretaceous||||||
2891|Bulldog Shale|34830|6|Mentioned|p9|||||||||
2891|Bulldog Shale|34984|5|Briefly described|p322|||||||||
2891|Bulldog Shale|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||08-MAY-13
2891|Bulldog Shale|36213|6|Mentioned|p85|||||||||
2891|Bulldog Shale|36214|5|Briefly described|p58|||||||||
2891|Bulldog Shale|36494|6|Mentioned|p155|||||||||
2891|Bulldog Shale|36552|6|Mentioned|p60|||||||||
2891|Bulldog Shale|36571|6|Mentioned|p101|||See also Table 4.||||||
2891|Bulldog Shale|36733|6|Mentioned|p14|||||||||
2891|Bulldog Shale|36922|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|36966|6|Mentioned|p83|||||||||
2891|Bulldog Shale|38022|6|Mentioned|p29|||||||||
2891|Bulldog Shale|38068|4|Described|p72|||||||||
2891|Bulldog Shale|38199|6|Mentioned|p426|||||||||
2891|Bulldog Shale|38604|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|38605|4|Described|p24|||See also Table 4.||||||
2891|Bulldog Shale|38814|6|Mentioned|Table 1|||||||||
2891|Bulldog Shale|39211|6|Mentioned|p11|||Correlation Coreena Mb in Qld. See also Fig. 6,10,12, etc.||||||
2891|Bulldog Shale|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
2891|Bulldog Shale|39630|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|39914|6|Mentioned|p2|||||||||
2891|Bulldog Shale|40003|6|Mentioned|Fig.9|||||||||
2891|Bulldog Shale|40058|6|Mentioned|p4|||||||||
2891|Bulldog Shale|40199|6|Mentioned|p16|||||||||
2891|Bulldog Shale|40220|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|40670|6|Mentioned|Fig.9|||||||||
2891|Bulldog Shale|40681|6|Mentioned|p13|||||||||
2891|Bulldog Shale|40801|6|Mentioned|p84|||||||||
2891|Bulldog Shale|40910|6|Mentioned|p15|||||||||
2891|Bulldog Shale|40911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|40912|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|40926|3|Fully described|p16|||||||||
2891|Bulldog Shale|41060|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41062|6|Mentioned|Fig.5|||||||||
2891|Bulldog Shale|41064|6|Mentioned|p62,p67|||||||||
2891|Bulldog Shale|41084|5|Briefly described|Fig.2|||||||||
2891|Bulldog Shale|41085|3|Fully described|p88|||||||||
2891|Bulldog Shale|41086|3|Fully described|p98|||||||||
2891|Bulldog Shale|41087|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41088|6|Mentioned|p143|||||||||
2891|Bulldog Shale|41098|4|Described|p176|||||||||
2891|Bulldog Shale|41117|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41165|6|Mentioned|p360|||See also Fig.15||||||
2891|Bulldog Shale|41175|6|Mentioned|Fig.1|||||||||
2891|Bulldog Shale|41177|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41182|3|Fully described|p289|||||||||
2891|Bulldog Shale|41183|6|Mentioned|Fig.3 p308|||||||||
2891|Bulldog Shale|41184|6|Mentioned|p347|||||||||
2891|Bulldog Shale|41187|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41216|6|Mentioned|Fig.18|||||||||
2891|Bulldog Shale|41266|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41276|6|Mentioned|p62|||||||||
2891|Bulldog Shale|41288|6|Mentioned|Fig.7|||||||||
2891|Bulldog Shale|41361|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41427|6|Mentioned|p84|||||||||
2891|Bulldog Shale|41523|3|Fully described|p275|||||||||
2891|Bulldog Shale|41950|5|Briefly described|Fig.2 P3|||||||||
2891|Bulldog Shale|42071|6|Mentioned|p117|||||||||
2891|Bulldog Shale|42099|6|Mentioned|Fig.2 P63|||||||||
2891|Bulldog Shale|42293|4|Described|p17|Albian|Aptian|||||||
2891|Bulldog Shale|42346|4|Described|p78, Fig.3 p80|||Part of Maree Subgroup.||||||16-SEP-08
2891|Bulldog Shale|42375|5|Briefly described|Fig.5 P24,|Late Cretaceous|Jurassic|Eromanga Basin. See also Table 1 p11, Fig.28 p125.||||||
2891|Bulldog Shale|42395|5|Briefly described|Fig.13 P83|||||||||
2891|Bulldog Shale|42465|5|Briefly described|Map Legend|||||||||
2891|Bulldog Shale|42469|4|Described|p35|||||||||
2891|Bulldog Shale|42520|5|Briefly described|p6|||||||||
2891|Bulldog Shale|42546|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
2891|Bulldog Shale|42602|6|Mentioned|Fig.2 P20|||||||||
2891|Bulldog Shale|42723|5|Briefly described|map legend|Aptian||||||||
2891|Bulldog Shale|42736|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
2891|Bulldog Shale|42746|4|Described|p12|||See also Fig.6||||||
2891|Bulldog Shale|42804|6|Mentioned|p118|||||||||
2891|Bulldog Shale|42816|5|Briefly described|p18|||||||||
2891|Bulldog Shale|42899|5|Briefly described|p349|||||||||
2891|Bulldog Shale|42905|5|Briefly described|p20|||Of Marree Subgroup.||||||16-SEP-08
2891|Bulldog Shale|43048|4|Described|Table 3.|||In the Marree Subgroup.||||||17-JAN-08
2891|Bulldog Shale|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||25-MAY-05
2891|Bulldog Shale|43085|5|Briefly described|Fig.6|||||||||
2891|Bulldog Shale|43202|5|Briefly described|p17||Cretaceous|||||||
2891|Bulldog Shale|43258|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|43298|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|43591|6|Mentioned|p40,165||Early Cretaceous|||||||
2891|Bulldog Shale|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
2891|Bulldog Shale|43681|4|Described|p295||Early Cretaceous|||||||
2891|Bulldog Shale|43743|6|Mentioned|Fig.2,p33||Early Cretaceous|||||||
2891|Bulldog Shale|43840|5|Briefly described|Fig3 p12||Cretaceous|||||||12-JUL-16
2891|Bulldog Shale|44133|4|Described|p45, 117, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Marree Subgroup. Includes: Wilpoorinna Breccia Member. Maximum Thickness: ~340m. Conformably underlies: Coorikiana Sandstone.||||||08-MAY-13
2891|Bulldog Shale|44289|5|Briefly described|Map Legend||Albian|||||||
2891|Bulldog Shale|44658|14|Not recorded|map legend|||Neoc.-Albian (G53-15).||||||
2891|Bulldog Shale|44934|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|44935|5|Briefly described|Map Legend||Aptian|||||||
2891|Bulldog Shale|45132|6|Mentioned|p14|||||||||
2891|Bulldog Shale|46791|6|Mentioned|p44|||Time equivalent of Wallumbilla Formation||||||
2891|Bulldog Shale|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
2891|Bulldog Shale|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
2891|Bulldog Shale|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
2891|Bulldog Shale|60564|5|Briefly described|p4, p5|||Overlain by the Alpha Mudstone.||||||
2891|Bulldog Shale|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Coorikiana Sandstone. Lateral to Wallumbilla Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
2891|Bulldog Shale|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||27-APR-05
2891|Bulldog Shale|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Of the Marree Subgroup.||||||13-APR-05
2891|Bulldog Shale|61014|6|Mentioned|p533, p543. |Early Cretaceous|Early Cretaceous|Eromanga Basin. Open marine conditions.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone.||21-JAN-15
2891|Bulldog Shale|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marine mudstone.||||||
2891|Bulldog Shale|61560|5|Briefly described|p491|Early Cretaceous|Early Cretaceous|Contains the Mt Toondina impact structure.  Geological Province: Arckaringa Basin (SA). ||||||
2891|Bulldog Shale|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
2891|Bulldog Shale|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
2891|Bulldog Shale|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
2891|Bulldog Shale|61836|5|Briefly described|p211|Cretaceous|Cretaceous|Overlies Cadna-Owie Formation. Geological Province: Eromanga Basin.||||||05-OCT-06
2891|Bulldog Shale|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
2891|Bulldog Shale|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation and Namur Sandstone. Is overlain by Oodnadatta and Toolebuc Formations.||
2891|Bulldog Shale|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
2891|Bulldog Shale|63124|6|Mentioned|p62|||Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|63894|5|Briefly described|p169, p179-180|Cretaceous|Cretaceous|Overlies Cadna-owie Formation. Marine mudstone and aquitard, fractured. Penetrated by spring mounds forming hard carbonate caps on top of pedestal of the shale. Surrounding areas is eroded and forms the Bulldog Shale plain.||||||
2891|Bulldog Shale|63979|6|Mentioned|p48, Fig. 44|Albian|Barremian|SA unit that equates to lower section of Wallumbilla Formation in Qld.||||||07-FEB-11
2891|Bulldog Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin. Coeval with Wallumbilla Formation.||Unit in Marree Subgroup.||Underlies the Coorikiana Sandstone, overlies the Cadna-owie Formation.||
2891|Bulldog Shale|64696|5|Briefly described|p133 Fig.14|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|64778|6|Mentioned|p13, 16-17, 19-20|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins. Max. palaeotemperature analysis summary.||||||
2891|Bulldog Shale|65194|6|Mentioned|p46|||Of Marree Subgroup. Aquitard.||||||
2891|Bulldog Shale|65238|5|Briefly described|p5 Fig. 6, p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Marine deposits.||||||17-FEB-10
2891|Bulldog Shale|65309|5|Briefly described|p6 Table 1, p15, p19.|Cretaceous|Cretaceous|Flat-lying, widespread unit of an early Cretaceous marine incursion in Eromanga Basin.||||Overlies Algebuckina Sandstone in a few scattered exposures on summits of mesas.|Pale yellow to white, massive to laminated, very fine siltstone; locally silicified to porcellanite.|
2891|Bulldog Shale|65342|6|Mentioned|p9.|||Eromanga Basin. Max. thickness at least 237m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
2891|Bulldog Shale|65376|6|Mentioned|p140 Fig.4.22.|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|65385|4|Described|pS128 Fig.2, pS133, pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Mudstone, minor silt to fine-grained sandstone intervals. Overlies Cadna-owie Formation. Overlain by Coorikiana Sandstone.||||||08-MAR-12
2891|Bulldog Shale|65489|5|Briefly described|p55, p59, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 320m thick. Regional seal to Cadna-owie Formation.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone or Oodnadatta Formation.||
2891|Bulldog Shale|65689|5|Briefly described|pp154-155, p160|Albian|Aptian|Eromanga Basin. Fossiliferous; diverse range of microfossils, bivalve molluscs, gastropods, ammonites, belemnites; large quantities of wood; a range of plesiosaur taxa; fish. Glendonites indicate cold conditions/high latitudes.||Unit in Marree Subgroup.|||Sequence of shallowly dipping marine strata, mainly mudstones and claystones; coquinoid layers common; isolated sandy deposits. Extensive opal deposits, typically associated with severe leaching and weathering.|
2891|Bulldog Shale|65925|5|Briefly described|p9, p47, p49, Appendix 2.|Cretaceous|Cretaceous|Eromanga Basin. Contains abundant organic matter.||||Is unconformably overlain by Eyre Formation and Namba Formation.|Grey, bioturbated, fossiliferous and shaly mudstone; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|66131|6|Mentioned|p247, p248 Fig.6|||Crops out in flanks of many hills (and mound springs).||||||
2891|Bulldog Shale|66303|5|Briefly described|pp27-28.|Early Cretaceous|Early Cretaceous|Widespread unit in Eromanga Basin. Early Aptian to middle Albian. Correlated with Cyclosporites hughesii and Crybelosporites striatus spore-pollen zones, and extends into the Coptospora paradoxa spore-pollen zone.||||Overlies Cadna-owie Formation. Is overlain by Eyre Formation.|Dark grey, bioturbated and fossiliferous shaly mudstone.|
2891|Bulldog Shale|66518|5|Briefly described|p19, p23.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Acts as a seal for migrating hydrocarbons from significant resources in the north of the Basin.||Unit in Marree Subgroup.||Overlies Cadna-owie Formation and Parabarana Sandstone. Is overlain by Oodnadatta Formation and locally by Coorikiana Sandstone.|Greenish-grey to bluish-grey mudstones.|
2891|Bulldog Shale|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. ||Unit in Neales River Group.||Overlies Toolebuc Formation. Is overlain by Mackunda or Normanton Formations.|Deeper marine shale and mudstone.|
2891|Bulldog Shale|66623|6|Mentioned|p254, p258, p260.|||Laterally equivalent to Wallumbilla Formation and Doncaster Member in NSW.||||Overlies Wyandra Sandstone Member.||
2891|Bulldog Shale|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone and Oodnadatta Formation.||
2891|Bulldog Shale|67474|5|Briefly described|p56|Cretaceous|Cretaceous|Confining unit for the main Great Artesian Basin aquifer. Grey marine shaly mudstone.||||||21-DEC-11
2891|Bulldog Shale|67561|5|Briefly described|p51-54, p57 Fig.6, p58, p64, p65|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression.||||Underlain by the Wyandra Sandstone Member. Correlative of the Wallumbilla Formation.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
2891|Bulldog Shale|67578|6|Mentioned|p334, p336 Fig.3|Cretaceous|Cretaceous|||||Is overlain unconformably by Eyre Formation.||
2891|Bulldog Shale|67784|6|Mentioned|p26, p28 table 1|||Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone.||08-FEB-18
2891|Bulldog Shale|68068|5|Briefly described|Map legend|Albian|Aptian|Eromanga Basin. Open marine, shallow to moderate depth; very cold, ?seasonal periglacial, conditions.||Unit in Marree Subgroup.||Overlies Parabarana Sandstone conformably to unconformably. Is overlain by Coorikiana Sandstone.|Laminated marine clay to silt, sandy lenses; dark grey to dark grey-brown, bioturbated, mid-unit concretions and exotic lonestones; glendonites; fossiliferous (molluscs, forams, wood, microflora, fish teeth, vertebrates).|18-NOV-14
2891|Bulldog Shale|68157|6|Mentioned|p8|Early Cretaceous|Early Cretaceous|core sample anaysed in this paper is a Bulldog Shale equivalent||||||07-NOV-14
2891|Bulldog Shale|68206|6|Mentioned|p27, 36-38|Albian|Aptian|S Eromanga Basin. Suggests that the South Pole was not ice-free during the Early Cretaceous (discussed).|||||Contains glendonites and dropstones.|
2891|Bulldog Shale|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
2891|Bulldog Shale|68715|6|Mentioned|p30 Fig.5|Albian|Aptian|Eromanga Basin.||||||
2891|Bulldog Shale|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Albian|Barremian|Eromanga Basin (SW). Opal-bearing. Marine. The opal layer is typically found within cracks and joints proximal to the interface between heavily weathered shale.||Of the Rolling Downs Group.|||Kaolinite rich.|20-JAN-22
2891|Bulldog Shale|68821|5|Briefly described|p292, pp295-297, p307, p309|Albian|Aptian|Lower Cretaceous age. Equivalent to the Wallumbilla Formation and the Doncaster Member. Contains ubiquitous disseminated pyrite. Marine depositional environment.||Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises of sandstone and siltstone.|
2891|Bulldog Shale|69001|5|Briefly described|p11, p16, p17, p35, p63, p69, pp72-73|Early Cretaceous|Early Cretaceous|Marine sediments. Pyritic and organic-rich.||Of the Maree Subgroup.||Equivalent to the Whittabrenah Shale.|Comprises grey fossiliferous mudstone-siltstones with regressive marine sandstones.|
2891|Bulldog Shale|69004|6|Mentioned|p12, p15|Cretaceous|Jurassic|Eromanga Basin.||||||
2891|Bulldog Shale|69019|4|Described|p83 Fig.20, p85 Fig.21, p93-97, p167.|Albian|Aptian|Of Freytag (1966). SW Eromanga Basin. Formerly Marree Formation. Max. thickness 277 m. Hosts minor deposits of celestite and barite. Has lonestone casts (dropstones) abundant in lower third of the unit.||Unit in Marree Subgroup.|Includes Wilpoorinna Breccia Member.|Conformably overlies Cadna-owie Formation and Parabarana Sandstone. Is overlain conformably by Coorikiana Sandstone.|Grey to dark grey, laminated to thinly planar, bedded to poorly bedded shale; highly bioturbated in many areas; contains ellipsoidal carbonate concretions, esp. towards the base where cone-in-cone limestone pods also occur.|
2891|Bulldog Shale|69023|4|Described|p77, p87, p89 Fig.20, p93-94, p96-97|Albian|Aptian|See also p99-100, p103-104, p110, p119, p126, p151, p191-192, p204. Defined by Freytag (1966). Eromanga Basin. Up to 336.4m thick. Diverse animal, plant and microfossil remains are described. Local silcrete capping. Is a seal for the Parabarana Sandstone aquifer. Stratigraphic wells intersection data.|c.105 Ma.|Unit in Marree Subgroup.||Conformably overlies Parabarana Sandstone and Cadna-owie Formation. Passes laterally into Wallumbilla Formation. Is overlain conformably by Coorikiana Sandstone.|Grey to dark grey shale with carbonate concretions; laminated to poorly bedded, commonly highly bioturbated; contains glendonites, lonestones (?dropstones) and occasional pyrite-marcasite nodules or bands; basal silty to sandy section.|
2891|Bulldog Shale|69203|5|Briefly described|p11-12, p57|Cretaceous|Cretaceous||||||Clay and shale, mudstone and fine-grained sandstone; local extremely hard white potch layers.|
2891|Bulldog Shale|69457|5|Briefly described|p41:3-8, 10, 14-15|Early Cretaceous|Early Cretaceous|Freytag (1966). Eromanga Basin. This name has previously (and inappropriately) been used to describe the Wallumbilla Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals.||Marree Subgroup.||Disconformably overlies De Souza Sandstone. Is overlain by Coorikiana Sandstone.|Contains diverse fossil assemblages, as well as glendonite nodules and dropstones.|12-JUL-16
2891|Bulldog Shale|69554|6|Mentioned|p131|Cretaceous|Cretaceous|Northern Gawler Craton.||||||
2891|Bulldog Shale|69562|6|Mentioned|p662 Tb.2, p664 Tb.4, p666 Fig.3|Cretaceous|Cretaceous|See also p667 Fig.4, p668, p679-680, p682 Fig.11. Electrical conductivity value used in forward modelling: 1000 mS/m.||Unit in Marree Subgroup.|||Highly conductive pyritic black muds.|
2891|Bulldog Shale|69568|5|Briefly described|p443-444|Cretaceous|Cretaceous|Lake Frome region, Eromanga Basin. Non-marine.||||Is overlain unconformably by Eyre Formation.|Blue-grey, silty bioturbated clay mudstone with abundant organic matter.|
2891|Bulldog Shale|69673|6|Mentioned|p155 fig 127, p159|Cretaceous|Cretaceous|||||Overlies Mount Anna Sandstone Member, overlain by Coorikiana Sandstone, correlated with Wallumbilla Formation||
2891|Bulldog Shale|69742|5|Briefly described|p787, 788, p790, 793|Cretaceous|Cretaceous|Great Artesian Basin. Coober Pedy. Marine. Geochemistry discussed.|||||Kaolinite-dominated shale with quartz, smectite and illite.|
2891|Bulldog Shale|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
2891|Bulldog Shale|69946|3|Fully described|p19, p21-24, p38, p56-57, p94, p99-111|Early Cretaceous|Early Cretaceous|Freytag (1966), for the dark grey shale between Cadna-owie Formation and Coorikiana Sandstone. Type section is outcrop 8km S of Bulldog Creek. Large clasts include Adelaidean slate, quartzite, laminated siltstone and Gawler Range Volcanics. From c.200 to >340 m thick. Early Aptian to mid Albian. Fossil groups listed. Wireline log correlations.||Basal unit in Marree Subgroup.||Conformably overlies Cadna-owie Formation. Is overlain conformably by Coorikiana Sandstone. Lateral equivalent of Wallumbilla Formation.|Dark grey, bioturbated and fossiliferous mudstone, with minor interbeds of micaceous siltstone and very fine-grained sandstone; pyrite and diagenetic carbonate nodules; glendonite nodules in outcrop; local lonestones and layers with fossil wood.|
2891|Bulldog Shale|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Coorikiana Sandstone.|Thick, fossiliferous mudstones and siltstones.|
2891|Bulldog Shale|69948|6|Mentioned|p4; Figs.4.1, 18|||Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Oodnadatta Formation.|Marine shales.|
2891|Bulldog Shale|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Grey, bioturbated, fossiliferous and shaly mudstone; minor silt to very fine-grained sandstone intervals.|12-JAN-16
2891|Bulldog Shale|70338|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|70383|5|Briefly described|p45, p51-52|Early Cretaceous|Early Cretaceous|Marine deposits. Contains fossiliferous (fish) Devonian sandstone boulders; thought to originate from the Amphitheatre and Mulga Downs Groups, and been transported NW to South Australia during the Permian glaciation, and later reworked into the basal Bulldog Shale.||||Overlies Cadna-owie Formation.||
2891|Bulldog Shale|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin. Open marine deposits; shallow to moderate depth. Fossils include molluscs, forams, petrified wood, microflora, fish teeth and vertebrates. Maximum depositional age from detrital zircons.|< ~110 Ma (SHRIMP U-Pb).|Marree Subgroup.||Overlies Cadna-owie Formation. Is overlain gradationally by Coorikiana Sandstone.|Dark grey to dark grey-brown, laminated clay to silt, sandy lenses, bioturbated; mid-unit limestone concretions and exotic glacial dropstones and cone-in-cone limestone pods. Glendonites in lower midsection (periglacial).|
2891|Bulldog Shale|70789|5|Briefly described|p318, p320 Fig.4, p326, p328|Early Cretaceous|Early Cretaceous|Eromanga Basin. Aptian-early Albian. Thickness varies from <100m to maximum of 500m. An aquitard.|125-106 Ma.|||Overlies Cadna-owie Formation.|Pyritic, carbonaceous and glauconitic shales and mudstones.|
2891|Bulldog Shale|70821|5|Briefly described|p21 Fig.2.6, p23, p82, p117|Early Cretaceous|Early Cretaceous|Eromanga Basin. Highly conductive.||Marree Subgroup.||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone. Equivalent to Wallumbilla Formation.||
2891|Bulldog Shale|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 320m thick. Deposited in an open marine, transgressive environment.||||Overlies the Cadna-owie Formation. Overlain by the Coorikiana Sandstone.||
2891|Bulldog Shale|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
2891|Bulldog Shale|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
2891|Bulldog Shale|71043|5|Briefly described|p106|||Gawler Craton.|||||Claystone, shale, ferruginous sandstone.|
2891|Bulldog Shale|71321|4|Described|p1,4,15,24-29,65|Albian|Early Aptian|Of Eromanga Basin. Crops out on the eastern and southern margin of TIEYON mapsheet. Depositional environment: marine shelf affected by high-latitude storms. Highstand systems tract following peak marine transgression during the Early Cretaceous. Micro-paleontological studies indicate an early Aptian to mid-Albian age (Krieg, et al., 1995). highly weathered in outcrop, mudstones bleached white to beige with shaly fissility, or have undergone iron oxidation.||||Underlain by Cadna-owie Formation or Algebuckina Formation. Overlain by the Oodnadatta Formation. Equivalent to Wallumbilla Formation and Rumbalara Shale.|Dark grey, laminated to massive, bioturbated and fossiliferous mudstone, with minor interbeds of micaceous siltstone and finely cross-laminated to irregularly interlaminated, fine-grained sandstone.|24-OCT-19
2891|Bulldog Shale|71342|4|Described|Ch1 p19, Ch4 p4, Ch4 p8, Ch5 p19-p24|Albian|Aptian|This unit was first defined by Freytag (1966) as the dark grey shale between the Cadna-owie Formation and the Coorikiana Sandstone. Freytag also defined the type section as outcropping 8km south of Bulldog Creek. Lithology is discussed in detail. This unit has a maximum thickness in excess of 340m in the Moomba area. Age assigned on the basis of palynology and fossil assemblage. Sedimentology and palaeoenvironment are discussed in detail. Spore-pollen zone is given in Ch5 p57. On the basis of spore-pollen zones, two major marine transgressions are inferred. See also  Ch5 p30, Ch5 p32-p33, Ch5 p38, Ch5 p100-p112, Ch6 p7-p8, Ch6 p10, Ch6 p14, Ch6 p19-p20, Ch7 p9, Ch7 p13, Ch8 p7, Ch8 p10, Ch8 p25-p26, Ch9 p20, Ch9 p21, Ch11 p4-p5, Ch14 p5.||Marree Subgroup||Conformably overlies the Cadna-owie Formation or the Algebuckina Sandstone. Conformably overlain by the Coorikiana Sandstone. Overlain by the Oodnadatta Formation.|Darl grey, bioturbated and fossiliferous mudstone with minor interbeds of micaceous siltstone and very fine-grained sandstone.|
2891|Bulldog Shale|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
2891|Bulldog Shale|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.||Overlies Cadna-owie FZ. Is overlain by Coorikiana Sandstone.||
2891|Bulldog Shale|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|72461|6|Mentioned|p24|Mesozoic|Mesozoic|||||||
2891|Bulldog Shale|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
2891|Bulldog Shale|72478|4|Described|p1, p6, p9-12, p18, p24-26|Middle Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in lower-energy, flood-plain, lacustrine and swamp environments. 80m was intersected in GOMA DH1 and GOMA DH3. Appears as a thin layer in GOMA DH2. Overlies an extremely hard massive quartzite interpreted as a correlative of the Pindyin Sandstone. See also p51, 69, 70, 72-75 [of the document].||||Overlies the Cadna-owie Formation. Unconformably overlies the Marla Group.|Fine-grained, sandstone, siltstone and coal.|29-MAR-21
2891|Bulldog Shale|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Marree Subgroup.||Overlies Cadna-owie Formation.|Kaolinised and porcellanitic claystone with layers of silt to very fine sand; surficial lag of quartz and quartzite pebbles to boulders.|
2891|Bulldog Shale|73153|6|Mentioned|p285|Aptian|Aptian|Holotype material[?] (SAM P17926) for Kakuru kujani (an indeterminate averostran or tetanuran) was recovered from this unit in South Australia.||||||
2891|Bulldog Shale|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
2891|Bulldog Shale|73203|6|Mentioned|p647, p649-650, p653|||Hosts opal at both Andamooka and Cobber Pedy.||||||
2891|Bulldog Shale|73249|4|Described|p316-323, p324 Fig.4, p325-338|Albian|Aptian|Eromanga Basin. Maximum age of early Aptian, minimum age of mid-Albian. Up to 340m thick in the central Eromanga Basin, ~200m thick on average. Deposited in an epicontinental marine environment, period of shallow marine transgression. Fossils include molluscs, gastropods, ammonites, belemnites and marine reptile remains (Drexel and Priess, 1955). Dominant clay mineral is montmorillonite, quartz is also widely abundant, mineralogy varies between lower and upper parts of the unit as well as laterally between drill holes. Deposited in a more arid, warmer envionment than the Cadna-owie Formation. Sediment sources interpreted to be from active volcanoes to the east, mix of felsic to mafic igneous rocks.||||Conformably overlies the Cadna-owie Formation, conformably underlies the Coorikiana Sandstone, lateral equivalent of the Wallumbilla Formation.|Marine sediments, composed of reduced dark grey bioturbated and fossiliferous mudstone with interbeds of siltstone to very fine sandstone, on average 200m thick.|
2891|Bulldog Shale|73251|4|Described|[See comments]|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Contains sandstone-hosted U deposit. Includes oil-prone organic facies. Marine depositional environment that are at least partly shallow-marginal marine. Contains Bulldog [organic] facies 1. [See article for organic petrology descriptions]. p: 36-37, 40, 42-45, 47-48, 50, 52-54, 56-58, 62.||||Underlain by Parabarana Sandstone unconformably, and Cadna-owie Formation. Overlain by Oodnadatta Formation and Coorikiana Sandstone. Equivalent to Wallumbilla Formation.|Grey siltstone with thin beds of ferruginised siltstone and subordinate fine-grained sandstone.|
2891|Bulldog Shale|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
2891|Bulldog Shale|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil and gas.||||Underlain by Cadna-owie Formation. Overlain by Coorikiana Sandstone. Equivalent to Wallumbilla Formation.||
2891|Bulldog Shale|73398|5|Briefly described|p1-9, 12-15, 20-30|Early Cretaceous|Early Cretaceous|Eromanga Basin. Overlying the Prominent Hill IOCG deposit, this unit contains up to c.5000 ppm Cu; the authors conclude this resulted from downwards leaching of Cu from the upper, oxidised part of the unit or from physical transport/deposition of Cu-bearing phases. Marine deposits. Geochemical concentration/depth diagrams. Geochemistry, weathering analysed in great detail.|<125 Ma.|||Conformably overlies Cadna-owie Formation.|Reduced dark grey mudstone with minor interbeds of siltstone and fine sandstone. Top 50-70m intensely weathered. Bioturbated and fossiliferous.|
2891|Bulldog Shale|73479|5|Briefly described|p156 Fig.2, p159, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine depositional environment.|ca 125-108 Ma|||Overlies Cadna-owie Formation, underlies Coorikiana Sandstone||
3003|Bungalow Granodiorite|22834|6|Mentioned|P39|||||||||
3003|Bungalow Granodiorite|23719|5|Briefly described|p19 Table 5|Calymmian|Statherian|Age: 1601+/-14 Ma (Rb-Sr). Part of Lincoln Complex. Geological Province: Gawler Craton.||||||05-MAR-08
3003|Bungalow Granodiorite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
3003|Bungalow Granodiorite|40448|6|Mentioned|Table 1|||||||||
3003|Bungalow Granodiorite|40644|6|Mentioned|p133|Paleoproterozoic|Paleoproterozoic|Presented as the informal Bungalow granodiorite.  Age: ca. 1675Ma. general age information included.||||||02-JUN-09
3003|Bungalow Granodiorite|43052|5|Briefly described|Table 4.4|||Of Lincoln Complex.||||||05-MAR-08
3003|Bungalow Granodiorite|50605|5|Briefly described|p(i), p1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1601 +/- 14Ma (Rb-Sr). Of the Moody Suite (Younger Lincoln Supersuite).||||||07-NOV-08
3003|Bungalow Granodiorite|71862|6|Mentioned|p15|||Originally included in the Moody Suite of Parker, 1993.||||||
3026|Bungunnia Limestone|10010|5|Briefly described|p12 Fig. 3|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||13-AUG-07
3026|Bungunnia Limestone|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
3026|Bungunnia Limestone|22799|5|Briefly described|p24 Fig.10|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|22857|5|Briefly described|p352 Fig. 24.8|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
3026|Bungunnia Limestone|22893|5|Briefly described|fig9p27|||||||||
3026|Bungunnia Limestone|23560|6|Mentioned|p152|||||||||
3026|Bungunnia Limestone|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|24176|6|Mentioned|p20|Pleistocene|Pleistocene|Of Firman (1965).||||||
3026|Bungunnia Limestone|24551|5|Briefly described|p338 Fig. 11.2, 340, 609.|Middle Pleistocene|Early Pleistocene|||||||
3026|Bungunnia Limestone|30056|6|Mentioned|Table 2|||||||||
3026|Bungunnia Limestone|30177|6|Mentioned|p106|||Pleistocene age.||||||
3026|Bungunnia Limestone|30750|6|Mentioned|p1|||Pleistocene age||||||
3026|Bungunnia Limestone|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|30753|4|Described|p15|||Middle Pleistocene age||||||
3026|Bungunnia Limestone|30754|2|Defined|Appendix 1|middle Pleistocene|middle Pleistocene|See also P22,31||||||
3026|Bungunnia Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
3026|Bungunnia Limestone|30918|6|Mentioned|p84|||||||||
3026|Bungunnia Limestone|30996|6|Mentioned|p38|||Refers Roberts (1968), Firman (1971)||||||
3026|Bungunnia Limestone|31741|6|Mentioned|p6|||||||||
3026|Bungunnia Limestone|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|31848|6|Mentioned|p12|||Quaternary||||||
3026|Bungunnia Limestone|32426|4|Described|p141|||See also P140||||||
3026|Bungunnia Limestone|32861|5|Briefly described|Table 1|||||||||
3026|Bungunnia Limestone|32862|5|Briefly described|Table 3|||Pleistocene||||||
3026|Bungunnia Limestone|33826|6|Mentioned|p42|||Strat. table||||||
3026|Bungunnia Limestone|34114|4|Described|p50|||Pleistocene||||||
3026|Bungunnia Limestone|34180|6|Mentioned|p212|||Middle Pleistocene.||||||
3026|Bungunnia Limestone|34459|4|Described|p11|||Pleistocene||||||
3026|Bungunnia Limestone|34461|5|Briefly described|p49|||||||||
3026|Bungunnia Limestone|34758|6|Mentioned|Table 1|||||||||
3026|Bungunnia Limestone|34954|6|Mentioned|p199|||||||||
3026|Bungunnia Limestone|35097|6|Mentioned|Fig.4|||||||||
3026|Bungunnia Limestone|35131|6|Mentioned|p8|||||||||
3026|Bungunnia Limestone|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|35232|6|Mentioned|Table 4|||||||||
3026|Bungunnia Limestone|35272|4|Described|p284|||||||||
3026|Bungunnia Limestone|35274|6|Mentioned|p425|||||||||
3026|Bungunnia Limestone|37873|4|Described|p2|||||||||
3026|Bungunnia Limestone|38068|6|Mentioned|p76|||||||||
3026|Bungunnia Limestone|39329|6|Mentioned|Fig.1|||||||||
3026|Bungunnia Limestone|40380|6|Mentioned|p221|||||||||
3026|Bungunnia Limestone|40820|5|Briefly described|p142|||||||||
3026|Bungunnia Limestone|41848|5|Briefly described|p358|||At top of Blanchetown Clay sequence. Age Pleistocene||||||
3026|Bungunnia Limestone|41868|6|Mentioned|p579|||||||||
3026|Bungunnia Limestone|42125|6|Mentioned|p139|||||||||
3026|Bungunnia Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
3026|Bungunnia Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
3026|Bungunnia Limestone|42137|6|Mentioned|Fig.2 P368|||||||||
3026|Bungunnia Limestone|42592|6|Mentioned|p280|||||||||
3026|Bungunnia Limestone|42635|5|Briefly described|p94|||||||||
3026|Bungunnia Limestone|42717|6|Mentioned|map legend|Pleistocene||||||||
3026|Bungunnia Limestone|42813|6|Mentioned|p25|||||||||
3026|Bungunnia Limestone|42827|5|Briefly described|p359|||see also Table 9.1||||||
3026|Bungunnia Limestone|42881|4|Described|Fig.3, P84|||||||||
3026|Bungunnia Limestone|42966|1|Redefined|Table 34 p209|Early Pleistocene||||||||
3026|Bungunnia Limestone|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Lacustrine dolomitic limestone. Underlain by Blanchetown Clay.||||||
3026|Bungunnia Limestone|43073|5|Briefly described|Table 4|||||||||
3026|Bungunnia Limestone|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
3026|Bungunnia Limestone|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
3026|Bungunnia Limestone|43655|5|Briefly described|p40-846|||||||||
3026|Bungunnia Limestone|43791|6|Mentioned|p372, Fig1|||||||||
3026|Bungunnia Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
3026|Bungunnia Limestone|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 3m. At the top of the Chowilla Sand and the Blanchtown Clay. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|49040|6|Mentioned|Fig.6|||||||||
3026|Bungunnia Limestone|60540|5|Briefly described|p1000 Fig.2,p1000,|Pleistocene|Pleistocene|||||Incised into the underlying Loxton Sand|Dolostone.|
3026|Bungunnia Limestone|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Overlies: Blanchetown Clay. Lacustrine dolomitic limestone.||||||
3026|Bungunnia Limestone|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Lacustrine dolomitic limestone. Overlies Blanchetown Clay.||||||01-JUN-05
3026|Bungunnia Limestone|61181|5|Briefly described|p137|Pleistocene|Pleistocene|Lacustrine deposits occur between ridges of Parilla Sand. Dolomitic limestone of this formation is interbedded with clay and sand. In the Mallee region.||||||
3026|Bungunnia Limestone|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Of the Wunghnu Group. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Variably dolomitic limestone.||||||
3026|Bungunnia Limestone|64961|5|Briefly described|p259, p269 Fig. 9|Quaternary|Quaternary|Overlies Blanchetown Clay. Geological province: Murray Basin. Thin, lacustrine carbonate unit, restricted in distribution. Indicated by 'BL' in Figure 9. ||||||
3026|Bungunnia Limestone|65552|5|Briefly described|p5 Fig. 3|Quaternary|Quaternary|Limestone of the central and western Murray Basin. Overlies Blanchetown Clay; underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
3026|Bungunnia Limestone|66287|5|Briefly described|Fig 2,4,5|Late Pliocene|Late Pliocene|With the Blanchetown Clay and the Chowilla Sand, part of the Lake Bungunnia sedimentary fill.||||Underlies the Bakara Soil and overlies the Blanchetown Clay.||20-APR-12
3026|Bungunnia Limestone|68548|5|Briefly described|p13, p13 Fig.2|Pleistocene|Pleistocene|Early to Middle Pleistocene age.||||Overlies Blanchetown Clay.|Dolostones.|
3026|Bungunnia Limestone|71248|2|Defined|p1, 2|||||||||
3026|Bungunnia Limestone|72445|6|Mentioned|App.7 p7, p7 Fig.4.|Quaternary|Quaternary|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying and partially equivalent to Blanchetown Clay.|Shown as limestone.|
3026|Bungunnia Limestone|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Lacustrine limestone.|
3026|Bungunnia Limestone|73228|4|Described|p50, p56-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin. Thickness: 1-3 m. Caps the Blanchetown Clay.|||||Interlaminated calcite, dolomite and magnesite, including an abundance of pisolitic and ooid grainstones, as well as ostracod-rich sands.|
3026|Bungunnia Limestone|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
3054|Bunyip Sand|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
3054|Bunyip Sand|30750|6|Mentioned|p4|||||||||
3054|Bunyip Sand|30751|6|Mentioned|Map legend|Recent|Recent|||||||
3054|Bunyip Sand|30752|6|Mentioned|Table 1|||||||||
3054|Bunyip Sand|30753|4|Described|p14|||Recent age||||||
3054|Bunyip Sand|30754|2|Defined|Appendix 1|Recent|Recent|See also P22,42. Stratigraphic table||||||
3054|Bunyip Sand|30755|6|Mentioned|p169|||Tectonic map||||||
3054|Bunyip Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
3054|Bunyip Sand|30996|6|Mentioned|p42|||Refers Firman (1966). See also P 48. Time eq. Coonambidgal Fm.||||||
3054|Bunyip Sand|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
3054|Bunyip Sand|32432|6|Mentioned|Fig.2|||See also Table 1||||||
3054|Bunyip Sand|32861|5|Briefly described|Table 1|||Recent||||||
3054|Bunyip Sand|33826|6|Mentioned|p42|||Strat. table||||||
3054|Bunyip Sand|34180|6|Mentioned|p212|||See also P217. Recent.||||||
3054|Bunyip Sand|34459|5|Briefly described|p11|||Recent||||||
3054|Bunyip Sand|34758|6|Mentioned|Fig.2|||||||||
3054|Bunyip Sand|35071|6|Mentioned|Table 1|||||||||
3054|Bunyip Sand|35097|6|Mentioned|Fig.4|||||||||
3054|Bunyip Sand|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3054|Bunyip Sand|35232|6|Mentioned|p14|||||||||
3054|Bunyip Sand|38068|6|Mentioned|Fig.8|||Murray Basin||||||
3054|Bunyip Sand|40226|6|Mentioned|Fig.2|||||||||
3054|Bunyip Sand|42264|6|Mentioned|p11|||||||||
3054|Bunyip Sand|42966|2|Defined|Table 38 p273|Quaternary||||||||
3054|Bunyip Sand|44133|5|Briefly described|p220 Fig. 11.2, 253|Holocene|Middle Pleistocene|Geological Province: Murray Basin. ||||||
3054|Bunyip Sand|49038|4|Described|Table 2|||||||||
3057|Burbrook Sandy Loam|38290|4|Described|p72|||||||||
3075|Burkitt Granite|22834|6|Mentioned|P39|||||||||
3075|Burkitt Granite|23818|5|Briefly described|p31|Calymmian|Calymmian|Geological Province: Gawler Block. Age: 1590 Ma. Unconformably overlain by Corunna Conglomerate.||||||02-JUN-09
3075|Burkitt Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
3075|Burkitt Granite|30806|5|Briefly described|Table 1|||||||||
3075|Burkitt Granite|30807|6|Mentioned|p103|||Suggested map symbol||||||
3075|Burkitt Granite|31320|6|Mentioned|Fig.1|||Carpentarian||||||
3075|Burkitt Granite|32435|6|Mentioned|Fig.1|||||||||
3075|Burkitt Granite|32437|6|Mentioned|Fig.2|||||||||
3075|Burkitt Granite|32438|6|Mentioned|Fig.2|||||||||
3075|Burkitt Granite|32507|6|Mentioned|Table 3|||||||||
3075|Burkitt Granite|33224|6|Mentioned|p51|||||||||
3075|Burkitt Granite|33468|6|Mentioned|p205|||1590my||||||
3075|Burkitt Granite|33470|6|Mentioned|Table 1|||||||||
3075|Burkitt Granite|33557|6|Mentioned|p12|||||||||
3075|Burkitt Granite|34537|6|Mentioned|p31|||Precamb.||||||
3075|Burkitt Granite|35255|6|Mentioned|p19|||||||||
3075|Burkitt Granite|35298|5|Briefly described|Table 1|||||||||
3075|Burkitt Granite|36073|6|Mentioned|Fig.3|||||||||
3075|Burkitt Granite|36507|6|Mentioned|p117|||||||||
3075|Burkitt Granite|39802|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3075|Burkitt Granite|40445|6|Mentioned|p53|||||||||
3075|Burkitt Granite|40448|5|Briefly described|Table 4|||||||||
3075|Burkitt Granite|40644|6|Mentioned|p124 Fig. 3,  p133|Paleoproterozoic|Paleoproterozoic|Included in the Lincoln Complex grouping. Age: ca. 1675Ma.||||||07-NOV-08
3075|Burkitt Granite|41667|6|Mentioned|Fig.4|||||||||
3075|Burkitt Granite|43052|4|Described|Table 4.4|||Of Moody Suite.||||||06-AUG-08
3075|Burkitt Granite|44660|14|Not recorded|map legend||Carpentarian|Carpentarian, lithology.||||||
3075|Burkitt Granite|48894|6|Mentioned|p71|||1500 +/-70 Ma||||||23-JUL-13
3075|Burkitt Granite|50605|5|Briefly described|p(i), p1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1655 +/- 61Ma (Rb-Sr). Of the Moody Suite (Younger Lincoln Supersuite).||||||07-NOV-08
3075|Burkitt Granite|65221|5|Briefly described|p27, p28 Fig.3, p31 Fig.6b|Palaeoproterozoic|Palaeoproterozoic|Hornblende bearing granitic gneiss, Rb-Sr age of 1655Ma, K-Ar age of 1687Ma. Considered late Syn or post Kimban Orogeny. Spencer Domain.||||||10-MAR-10
3075|Burkitt Granite|65915|4|Described|p4 Fig.3, p6, p9 Tb.2, p14-16, p18|Statherian|Statherian|Relatively continuous outcrops of low tors. Unfoliated, medium-grained hornblende-bearing granite, with prominent, large tabular feldspar phenocrysts. Has a prominent magnetic high. Previously dated at 1654 +/- 13 Ma (Rb-Sr whole rock: Stewart, in Neumann, 1999). SHRIMP U-Pb zircon discordia upper intercept of 1742+/-42 Ma reported here defined as magmatic age; lower intercept at 512 +/- 120 Ma may indicate an episode of partial isotope resetting.||||||
3075|Burkitt Granite|66302|6|Mentioned|p29|Statherian|Statherian|Ages are of igneous crystallisation by Fraser and Neumann (2010). This granite is highly radiogenic with a whole rock uranium abundance of 37 ppm. |1742 +/- 42 Ma and 1755 +/- 19 Ma (SHRIMP U-Pb)|Moody Suite||||
3075|Burkitt Granite|68158|5|Briefly described|p4|||||Lincoln Complex.|||Hornblende granite.|
3075|Burkitt Granite|68208|5|Briefly described|p32 Fig.3, p33, p34 Fig.5, p39|Paleoproterozoic|Paleoproterozoic|Highly magnetic, appears to intrude the Cooyerdoo Granite (from geophysics), Kimban-aged.||||||
3075|Burkitt Granite|70027|6|Mentioned|p71|Statherian|Statherian|Geological province: Gawler Craton. Possible source of ca. 1790-1750 Ma zircons associated with the Warramboo magnetite gneiss.|ca. 1755 Ma|||||
3075|Burkitt Granite|70286|6|Mentioned|p891|Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1742 +/- 42 Ma (Fraser and Neumann, 2010).|||||
3075|Burkitt Granite|70721|6|Mentioned|p63|||Intrudes the Spencer Domain of the Gawler Craton.|c. 1750-1745 Ma|||||
3075|Burkitt Granite|71129|5|Briefly described|p17,40-41|Statherian|Statherian|Geological Province: Gawler Craton. Contains zircon ages including 1742+\-42 Ma and 1755+\-19 Ma (Fraser and Neumann, 2010).|c. 1750 Ma|Unit of Moola Suite.||||
3075|Burkitt Granite|71235|5|Briefly described|p1, p3, p6, p19|Palaeoproterozoic|Palaeoproterozoic|Potentially a source of Uranium for mineralisation in the Corunna Conglomerate.||||Overlain by the Corunna Conglomerate.||16-MAR-23
3075|Burkitt Granite|71317|6|Mentioned|p15|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
3075|Burkitt Granite|71322|5|Briefly described|p100|||Eastern Gawler Craton.|1742 +/- 42 Ma (Fraser and Neumann, 2010).|||||
3075|Burkitt Granite|71859|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|||||||
3075|Burkitt Granite|71862|2|Defined|p6-p7, p9, p15, p22, p25|Statherian|Statherian|Named after Burkitt Hill, 12km northwest of Iron Knob, Corunna Station, Eyre Peninsula. Outcrops as low hills, tors and scattered small outcrops. The type locality is an outcrop of large tors directly south of Iron Knob-Yardea Road, ~11.5km west from Corunna Station comprising an area extending 100m radially from 689045mE, 6385491mN, GDA94, Zone 53. In the subsurface extends c. 14km south in TMI imagery and is intersected in RDD002 (drillhole 229989) between 15-481m. In TMI imagery this unit is characterised by a pronounced magnetic high. Age is poorly constrained as zircons are metamict due to high U concentrations. Geochemistry is discussed. See also p28-p29, p41-p44, p53-p54. An additional age of 1742 +/- 42 Ma is also derived from Fraser and Neumann, 2010.|1755 +/- 19 Ma (Fraser and Neumann, 2010)|Moola Suite||Intrudes (interpreted) the Cooyerdoo Granite and Sleaford Complex. Unconformably overlain by the Corunna Conglomerate.|Medium to coarse-grained, orange-pink, slightly porphyritic K-feldspar-quartz-plagioclase-hornblende-magnetite granite.|18-APR-23
3075|Burkitt Granite|72058|6|Mentioned|p172|||Gawler Craton. Surrounds the Middleback Ranges. Emplaced during the Kimban Orogeny. Dates are derived from  Fraser and Neumann, 2010; Fraser et al, 2010.|1742 +/- 42 Ma; 1755 +/- 19 Ma|||||
3075|Burkitt Granite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
3075|Burkitt Granite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|A K/Ar age of 1687 Ma is also given.|1655 +/- 61 Ma (Rb/Sr).|Moola Suite.|||Hornblende granite, medium-grained, equigranular, massive.|
3075|Burkitt Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1755+/-19 Ma|Moola Suite|||Felsic intrusive.|
3106|Burra Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
3106|Burra Group|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Slates, greywackes, quartzites, dolomites and dolomite arenites.||||||11-JAN-10
3106|Burra Group|22510|5|Briefly described|table1 p37|||Age: Willouran- Torrension in age.||||||
3106|Burra Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
3106|Burra Group|22589|6|Mentioned|p129||Neoproterozoic|||||||
3106|Burra Group|22631|6|Mentioned|p177, fig2 p170|Cryogenian|Cryogenian|||||||
3106|Burra Group|22643|5|Briefly described|p183, fig3p187|Cryogenian|Cryogenian|||||||
3106|Burra Group|22677|6|Mentioned|Fig.2 p735||Neoproterozoic|||||||
3106|Burra Group|22725|6|Mentioned|p241|Cambrian|Neoproterozoic|overlies Callana Group||||||
3106|Burra Group|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|||||||
3106|Burra Group|22787|6|Mentioned|p42|||||||||
3106|Burra Group|22802|6|Mentioned|p871|||Age: <780Ma||||||
3106|Burra Group|22830|6|Mentioned|P25||Adelaidean|||||||
3106|Burra Group|22857|5|Briefly described|p65, Tb. 13.1 (insert p70-71)|Sturtian|Torrensian|Of the Warrina Supergroup. Divided into 4 subgroups: Belair, Mundallio, River Wakefield, Emeroo Subgroups.||||||
3106|Burra Group|22869|5|Briefly described|P37, Fig2||Neoproterozoic|||||||
3106|Burra Group|22884|6|Mentioned|p40 Fig1|Neoproterozoic|Neoproterozoic|||||||26-MAR-09
3106|Burra Group|22889|4|Described|p30-40|Adelaidean|Adelaidean|New stratigraphic classification and correlation of the Burra Group is proposed.||||||
3106|Burra Group|22901|6|Mentioned|76 fig 2|||Geol province Adelaide Rift Complex||||||
3106|Burra Group|22907|6|Mentioned|41|||Geol province Adelaide Rift Complex||||||
3106|Burra Group|22926|5|Briefly described|37|||Geol. province: Adelaide Geosyncline. Overlain by Umberatana Group.||||||17-JAN-07
3106|Burra Group|22947|6|Mentioned|p16|||Mentioned under - Adelaide Geosyncline Geodevelopments.||||||
3106|Burra Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23023|6|Mentioned|p1797|||||||||
3106|Burra Group|23054|5|Briefly described|p11,33-4|||||||||
3106|Burra Group|23205|6|Mentioned|p133|||of Warrina Supergroup.||||||
3106|Burra Group|23211|6|Mentioned|Fig.1|||||||||
3106|Burra Group|23288|6|Mentioned|p143 Fig.18|||Equivalent of Finke beds. of Adelaide Geosyncline.||||||
3106|Burra Group|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Subdivided into Upper, Middle and Lower Burra Group. Includes Skillogalee Dolomite.||||||07-FEB-07
3106|Burra Group|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|23411|6|Mentioned|Map Legend|||||||||
3106|Burra Group|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province Curnamona Province.||||||
3106|Burra Group|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
3106|Burra Group|23719|4|Described|p24|Neoproterozoic|Adelaidean|See also page 25 table 7. Overlain by Umberatana Group; underlain by Callana Group. Geological Province: Gawler Craton.||||||17-JAN-07
3106|Burra Group|23818|4|Described|p34 Fig.8|Adelaidean|Adelaidean|Underlain by Barossa Complex. Geological Province: Willyama Block. Max. thickness: 20 000 ft. Age: oldest member is ~1000 Ma.||||||17-JAN-07
3106|Burra Group|23869|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23913|5|Briefly described|p110 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Adelaidean Geosyncline.  Unconformably overlain by Umberatana Group.||||||05-JUL-13
3106|Burra Group|24045|5|Briefly described|p533 Fig.2|Adelaidean|Adelaidean|||||||
3106|Burra Group|24175|3|Fully described|p10|Neoproterozoic|Neoproterozoic|Underlain by Callana Group. Max. thickness: 8470m.||||||20-FEB-07
3106|Burra Group|24176|3|Fully described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Age is Torrensian. Overlies upper Callanna Beds; underlies Umberatana Group. Geological Province: Mount Painter Province.||||||16-SEP-08
3106|Burra Group|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Mundallio and Emeroo Subgroups.||||||
3106|Burra Group|24362|6|Mentioned|p41|||||||||
3106|Burra Group|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|24400|5|Briefly described|p155 Tb.2, p156|Adelaidean|Adelaidean|Age: <777+/-7Ma. Includes Boucat Volcanics. Overlies Callana Group, overlain by Umberatana Group.||||||05-FEB-08
3106|Burra Group|24481|5|Briefly described|p829 Fig. 9|||Overlain by the Umberatana Group.||||||
3106|Burra Group|24484|5|Briefly described|p798 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~780-730 Ma. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
3106|Burra Group|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Warrina Supergroup. Includes Skillogalee Dolomite. Geological Province Adelaide Geosyncline.||||||05-JUL-06
3106|Burra Group|24593|5|Briefly described|p612 Fig. 1a|||Geological Province: Mount Painter Inlier.||||||
3106|Burra Group|29656|4|Described|Fig.3|||||||||
3106|Burra Group|29697|6|Mentioned|p7|||||||||
3106|Burra Group|29758|6|Mentioned|p101|||||||||
3106|Burra Group|29763|6|Mentioned|p45|||||||||
3106|Burra Group|29776|6|Mentioned|p82|||||||||
3106|Burra Group|29778|6|Mentioned|p167|||||||||
3106|Burra Group|29780|6|Mentioned|p21|||||||||
3106|Burra Group|29781|6|Mentioned|Fig.5|||||||||
3106|Burra Group|29831|5|Briefly described|p175|||||||||
3106|Burra Group|29835|6|Mentioned|p177|||||||||
3106|Burra Group|29838|6|Mentioned|p4|||||||||
3106|Burra Group|29840|6|Mentioned|Fig.3|||||||||
3106|Burra Group|30028|6|Mentioned|Fig.4|||||||||
3106|Burra Group|30051|6|Mentioned|Fig.1|||Proterozoic age.||||||
3106|Burra Group|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
3106|Burra Group|30090|6|Mentioned|p4|||||||||
3106|Burra Group|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|30177|4|Described|p64|||See also p65-66.||||||17-JAN-07
3106|Burra Group|30190|6|Mentioned|Fig.1|||||||||
3106|Burra Group|30255|5|Briefly described|p213|||Torrensian age. See also Fig.2, p217.||||||17-JAN-07
3106|Burra Group|30713|6|Mentioned|p106|||||||||
3106|Burra Group|30782|6|Mentioned|p70|||Stratigraphy||||||
3106|Burra Group|30798|6|Mentioned|p116|||||||||
3106|Burra Group|30799|6|Mentioned|p2|||Stratigraphy and terminology.||||||
3106|Burra Group|30801|6|Mentioned|p5|||Table p5-6. Torrensian age.||||||10-NOV-16
3106|Burra Group|30802|5|Briefly described|p7|||See also p8 and p13. Torrensian age.||||||17-JAN-07
3106|Burra Group|30807|6|Mentioned|p103|||Suggested map symbol||||||
3106|Burra Group|30808|6|Mentioned|Fig.2|||||||||
3106|Burra Group|30810|6|Mentioned|p2|||||||||
3106|Burra Group|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31022|6|Mentioned|Fig. 4|||||||||
3106|Burra Group|31109|5|Briefly described|p16|||See also p18. Map. Upper Proterozoic.||||||17-JAN-07
3106|Burra Group|31292|6|Mentioned|p3|||Refers Thomson et al. (1964)||||||
3106|Burra Group|31698|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31923|5|Briefly described|p8|||||||||
3106|Burra Group|31965|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31967|6|Mentioned|p.4|||||||||
3106|Burra Group|31971|6|Mentioned|p9|||||||||
3106|Burra Group|32031|6|Mentioned|Fig. 2|||||||||
3106|Burra Group|32032|6|Mentioned|p7|||||||||
3106|Burra Group|32146|6|Mentioned|p349|||Refers Thomson et al. (1964)||||||
3106|Burra Group|32319|6|Mentioned|p109|||Copper mineralization||||||
3106|Burra Group|32322|6|Mentioned|p109|||||||||
3106|Burra Group|32364|6|Mentioned|p17|||See also Fig.2,3||||||
3106|Burra Group|32419|6|Mentioned|p82|||||||||
3106|Burra Group|32424|6|Mentioned|p16|||||||||
3106|Burra Group|32501|6|Mentioned|p1|||Host rocks for fluorite. Also P2||||||
3106|Burra Group|32508|6|Mentioned|p119|||||||||
3106|Burra Group|32510|6|Mentioned|p106|||||||||
3106|Burra Group|32547|4|Described|p60|||Torrensian||||||
3106|Burra Group|32635|5|Briefly described|p5|||||||||
3106|Burra Group|32720|6|Mentioned|p5|||Middle Riphean Correlation. See also P7.||||||
3106|Burra Group|32721|6|Mentioned|p96|||||||||
3106|Burra Group|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
3106|Burra Group|32723|6|Mentioned|p96|||||||||
3106|Burra Group|32724|6|Mentioned|Fig.1|||Correlation||||||
3106|Burra Group|32726|6|Mentioned|p201|||Stromatolites||||||
3106|Burra Group|32727|6|Mentioned|p30|||||||||
3106|Burra Group|32823|6|Mentioned|p361|||||||||
3106|Burra Group|33004|6|Mentioned|p136|||||||||
3106|Burra Group|33033|6|Mentioned|p69|||||||||
3106|Burra Group|33404|5|Briefly described|p108|||Proterozoic.||||||
3106|Burra Group|33405|6|Mentioned|p141|||||||||
3106|Burra Group|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
3106|Burra Group|33423|4|Described|p12|||||||||
3106|Burra Group|33468|6|Mentioned|p209|||Willouran - Torrensian||||||
3106|Burra Group|33473|6|Mentioned|p2|||Adelaidean||||||
3106|Burra Group|33474|6|Mentioned|Fig.2|||||||||
3106|Burra Group|33490|6|Mentioned|p11|||Stratigraphy||||||
3106|Burra Group|33551|6|Mentioned|Fig.1|||Proterozoic||||||
3106|Burra Group|33577|6|Mentioned|p80|||Geol. map.||||||
3106|Burra Group|33691|6|Mentioned|p131|||||||||
3106|Burra Group|33693|6|Mentioned|p153|||||||||
3106|Burra Group|33726|6|Mentioned|p11|||||||||
3106|Burra Group|33794|6|Mentioned|p7|||See also Fig.2||||||
3106|Burra Group|33956|4|Described|p1040|||||||||
3106|Burra Group|33957|5|Briefly described|p35|||||||||
3106|Burra Group|34175|5|Briefly described|p37|||||||||
3106|Burra Group|34176|6|Mentioned|p51|||||||||
3106|Burra Group|34181|6|Mentioned|p43|||||||||17-JAN-22
3106|Burra Group|34202|6|Mentioned|p1056|||See also PP1057,1058. Precambrian.||||||
3106|Burra Group|34266|6|Mentioned|p9|||Adelaidean System||||||
3106|Burra Group|34287|6|Mentioned|p39|||||||||
3106|Burra Group|34291|6|Mentioned|p11|||Adelaide System. Adelaidean||||||
3106|Burra Group|34318|6|Mentioned|p86|||||||||
3106|Burra Group|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
3106|Burra Group|34483|6|Mentioned|p113|||Age: 900 - 1050my for lower sediments.||||||17-JAN-07
3106|Burra Group|34534|6|Mentioned|Fig.2.13|||||||||
3106|Burra Group|34535|3|Fully described|p54|||Adelaidean||||||
3106|Burra Group|34536|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian - Sturtian||||||
3106|Burra Group|34537|6|Mentioned|Fig.8|||Torrensian||||||
3106|Burra Group|34586|6|Mentioned|p27|||Torrensian. Mineralization. Drill holes.||||||
3106|Burra Group|34587|6|Mentioned|p36|||Torrensian||||||
3106|Burra Group|34718|6|Mentioned|p13|||||||||
3106|Burra Group|34719|6|Mentioned|p374|||||||||
3106|Burra Group|34766|6|Mentioned|Fig.2|||||||||
3106|Burra Group|34812|6|Mentioned|p4|||||||||
3106|Burra Group|34833|6|Mentioned|p76|||||||||
3106|Burra Group|34844|6|Mentioned|Fig.2|||||||||
3106|Burra Group|34942|6|Mentioned|p105|||||||||
3106|Burra Group|34958|6|Mentioned|p87|||||||||
3106|Burra Group|34979|6|Mentioned|p33|||||||||
3106|Burra Group|34985|6|Mentioned|p309|||||||||
3106|Burra Group|35090|6|Mentioned|p29|||||||||
3106|Burra Group|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|35217|6|Mentioned|Fig.1|||||||||
3106|Burra Group|35232|6|Mentioned|p5|||See also Table.1||||||
3106|Burra Group|35255|5|Briefly described|p9|||See also p13 and Fig.3.||||||17-JAN-07
3106|Burra Group|35270|6|Mentioned|p4|||||||||
3106|Burra Group|35327|6|Mentioned|Fig.1|||||||||
3106|Burra Group|35328|6|Mentioned|p9|||Stratigraphy||||||
3106|Burra Group|35353|6|Mentioned|Fig.2|||Regional geology||||||
3106|Burra Group|35354|6|Mentioned|p46|||||||||
3106|Burra Group|35357|6|Mentioned|p21|||||||||
3106|Burra Group|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
3106|Burra Group|35565|6|Mentioned|p21|||Mapping and stratigraphy||||||
3106|Burra Group|35675|6|Mentioned|Fig.1|||Location plan & regional geology.||||||
3106|Burra Group|35893|6|Mentioned|p714|||||||||
3106|Burra Group|35904|6|Mentioned|p6|||||||||
3106|Burra Group|36003|6|Mentioned|p1030|||||||||
3106|Burra Group|36081|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36083|6|Mentioned|Table 1|||||||||
3106|Burra Group|36096|6|Mentioned|Fig.3|||||||||
3106|Burra Group|36126|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36137|5|Briefly described|p3|||||||||
3106|Burra Group|36212|5|Briefly described|p3|||||||||
3106|Burra Group|36245|6|Mentioned|p9|||||||||
3106|Burra Group|36253|6|Mentioned|Fig.3-2|||||||||
3106|Burra Group|36514|6|Mentioned|p55|||||||||
3106|Burra Group|36623|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36626|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36731|6|Mentioned|p123|||||||||
3106|Burra Group|36733|4|Described|p38|||||||||
3106|Burra Group|36833|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36835|6|Mentioned|p31|||||||||
3106|Burra Group|36837|6|Mentioned|Fig.2|||||||||
3106|Burra Group|36838|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36839|6|Mentioned|p61|||||||||
3106|Burra Group|36898|6|Mentioned|p182|||||||||
3106|Burra Group|37113|6|Mentioned|Fig.1|||||||||
3106|Burra Group|37238|6|Mentioned|Table 1|||||||||
3106|Burra Group|37371|6|Mentioned|p382|||||||||
3106|Burra Group|37461|5|Briefly described|p336|||See also p332.||||||17-JAN-07
3106|Burra Group|37501|6|Mentioned|p415|||||||||
3106|Burra Group|37854|2|Defined|p13|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|37932|6|Mentioned|p539|||||||||
3106|Burra Group|38004|6|Mentioned|p82|||||||||
3106|Burra Group|38068|4|Described|p68|||See also Fig.4.||||||
3106|Burra Group|38157|6|Mentioned|Table 1|||||||||
3106|Burra Group|38243|6|Mentioned|p359|||||||||
3106|Burra Group|38581|6|Mentioned|p252|||||||||
3106|Burra Group|38703|6|Mentioned|p131|||||||||
3106|Burra Group|38704|6|Mentioned|p133|||||||||
3106|Burra Group|38926|3|Fully described|p25|||||||||
3106|Burra Group|39210|6|Mentioned|Table 3|||||||||
3106|Burra Group|39320|6|Mentioned|p375|||||||||
3106|Burra Group|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian to Sturtian||||||
3106|Burra Group|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|39350|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian to Sturtian||||||
3106|Burra Group|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3106|Burra Group|39352|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Torrensian||||||
3106|Burra Group|39490|6|Mentioned|p10|||||||||
3106|Burra Group|39635|6|Mentioned|Fig.2|||||||||
3106|Burra Group|39724|6|Mentioned|Fig.6|||||||||
3106|Burra Group|39762|6|Mentioned|Table 1|||||||||
3106|Burra Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3106|Burra Group|40003|5|Briefly described|Table 2|||||||||
3106|Burra Group|40105|6|Mentioned|p311|||||||||
3106|Burra Group|40225|3|Fully described|Map sheet|||||||||
3106|Burra Group|40228|5|Briefly described|Fig.1|||||||||
3106|Burra Group|40257|6|Mentioned|p287|||||||||
3106|Burra Group|40294|3|Fully described|p32|||||||||
3106|Burra Group|40442|4|Described|p8|||||||||
3106|Burra Group|40448|5|Briefly described|p38|||||||||
3106|Burra Group|40456|6|Mentioned|Fig.2|||||||||
3106|Burra Group|40500|6|Mentioned|p142|||||||||
3106|Burra Group|40501|6|Mentioned|p115|||||||||
3106|Burra Group|40595|6|Mentioned|Fig.8|||||||||
3106|Burra Group|40763|5|Briefly described|p204|||||||||
3106|Burra Group|40852|5|Briefly described|p26|||||||||
3106|Burra Group|40906|6|Mentioned|Fig.9|||||||||
3106|Burra Group|40910|6|Mentioned|p10|||||||||
3106|Burra Group|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|40985|6|Mentioned|p403|||||||||
3106|Burra Group|41256|6|Mentioned|p7|||||||||
3106|Burra Group|41364|6|Mentioned|p152|||||||||
3106|Burra Group|41400|6|Mentioned|p27|||||||||
3106|Burra Group|41401|6|Mentioned|p32|||||||||
3106|Burra Group|41402|6|Mentioned|p36|||||||||
3106|Burra Group|41404|3|Fully described|p73|||||||||
3106|Burra Group|41494|5|Briefly described|p31|||||||||
3106|Burra Group|41647|6|Mentioned|p834|||||||||
3106|Burra Group|41770|6|Mentioned|p249|||||||||
3106|Burra Group|42028|6|Mentioned|p137|||||||||
3106|Burra Group|42087|5|Briefly described|Fig.2 P15|||||||||
3106|Burra Group|42088|5|Briefly described|p546|||||||||
3106|Burra Group|42090|6|Mentioned|p19|||||||||
3106|Burra Group|42093|6|Mentioned|p6|||||||||
3106|Burra Group|42098|4|Described|p51|||||||||
3106|Burra Group|42109|6|Mentioned|Fig.1 P19|||||||||
3106|Burra Group|42167|6|Mentioned|p118|||||||||
3106|Burra Group|42215|5|Briefly described|p442|||See also Fig.2||||||
3106|Burra Group|42222|4|Described|p13|||||||||
3106|Burra Group|42223|4|Described|p37|||See also Fig.2||||||
3106|Burra Group|42235|4|Described|p134|||See also Fig.3||||||
3106|Burra Group|42236|6|Mentioned|Fig.2 P106|||||||||
3106|Burra Group|42237|4|Described|p85|||See also Figs. 1 and 2||||||
3106|Burra Group|42238|4|Described|p72|||||||||
3106|Burra Group|42239|6|Mentioned|Fig.2 P151|||||||||
3106|Burra Group|42243|5|Briefly described|p211|||||||||
3106|Burra Group|42271|6|Mentioned|p372|||||||||
3106|Burra Group|42272|4|Described|p398|||||||||
3106|Burra Group|42274|5|Briefly described|p450|||||||||
3106|Burra Group|42357|6|Mentioned|p8|||||||||
3106|Burra Group|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Torrensian)|||||||
3106|Burra Group|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
3106|Burra Group|42546|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Willouran)|||||||
3106|Burra Group|42643|6|Mentioned|Fig. 4 P19|||||||||
3106|Burra Group|42720|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42721|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42723|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42733|6|Mentioned|map legend|Adelaidean||||||||
3106|Burra Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
3106|Burra Group|42760|6|Mentioned|p3|||||||||
3106|Burra Group|42761|5|Briefly described|Fig.2 P8|||||||||
3106|Burra Group|42762|6|Mentioned|p14|||see also Fig.1 P15||||||
3106|Burra Group|42788|5|Briefly described|p140|||||||||
3106|Burra Group|42813|4|Described|p15|||||||||
3106|Burra Group|42882|5|Briefly described|Table 1 P3|||Of the Warrina Supergroup.||||||17-JAN-07
3106|Burra Group|43048|6|Mentioned|p12|||||||||
3106|Burra Group|43052|4|Described|p177|||See also Table 6.1||||||
3106|Burra Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite.||||||26-MAY-05
3106|Burra Group|43057|6|Mentioned|Fig.2.24|||||||||
3106|Burra Group|43094|5|Briefly described|p33|||||||||
3106|Burra Group|43190|5|Briefly described|p29, Fig.2.|||||||||
3106|Burra Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
3106|Burra Group|43298|5|Briefly described|Map Legend||Adelaidean|||||||
3106|Burra Group|43390|14|Not recorded|p8|||||||||
3106|Burra Group|43595|5|Briefly described|p543-545||Neoproterozoic|||||||
3106|Burra Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
3106|Burra Group|43845|5|Briefly described|Fig3 p43, 41||Neoproterozoic|||||||12-JUL-16
3106|Burra Group|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline||||||
3106|Burra Group|44133|5|Briefly described|p46, 51 Fig. 7.18, 52|Adelaidian|Adeladian|Siltstone, sandstone, dolomite.||||||
3106|Burra Group|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
3106|Burra Group|44659|5|Briefly described|map legend|||Torrensian-Sturtian, lithology.||||||06-DEC-04
3106|Burra Group|44660|14|Not recorded|map legend|||Torrensian, lithology.||||||
3106|Burra Group|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
3106|Burra Group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
3106|Burra Group|45155|6|Mentioned|Fig.7|||Adelaide geosyncline||||||
3106|Burra Group|46798|6|Mentioned|p102|||||||||
3106|Burra Group|46865|6|Mentioned|Table 2|||||||||
3106|Burra Group|47009|6|Mentioned|p330|||||||||
3106|Burra Group|47012|6|Mentioned|p332|||||||||
3106|Burra Group|49792|6|Mentioned|Fig.5|||||||||
3106|Burra Group|50327|6|Mentioned|p307|||Contains the Rhynie Sandstone.||||||07-FEB-11
3106|Burra Group|50615|5|Briefly described|p302|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|60718|4|Described|p48, p49 Fig. 1, p52, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Comprises Emeroo, Mundallio and Bungarider Subgroups.|Unconformably underlies Umberatana Group.||15-APR-11
3106|Burra Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite.||||||05-JUL-13
3106|Burra Group|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Myrtle Springs Formation, Witchelina Quartzite.||||||
3106|Burra Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Warrina Supergroup.||||||
3106|Burra Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|||||||17-JAN-07
3106|Burra Group|61153|5|Briefly described|p344-345 Fig. 1|||Unconformably overlain by the Sturt Tillites; unconformably overlies the Gairdner Dyke Swarm. Geological Province: Adelaide Geosyncline.||||||
3106|Burra Group|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Includes Saddleworth Formation.||||||
3106|Burra Group|61263|6|Mentioned|p469|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|61307|6|Mentioned|p5, p20|Torrensian|Torrensian|Includes: Saddleworth Fm, Stonyfell Quartzite, Woolshed Flat Shale, Skillogalee Dolomite and Aldgate Sandstone. Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|61308|5|Briefly described|p6|Adelaidean|Adelaidean|Dolomite, quartzite, siltstone.||||||
3106|Burra Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Sturtian|Torrensian|Includes the Belair Subgroup; and the 777+/-7Ma Boucaut Volcanics. Contains microfossils. Geological Province: Adelaide Rift Complex/Stuart Shelf. See also p25, p68, p131.||||||05-JUL-13
3106|Burra Group|62453|5|Briefly described|p11 Fig. 7, 12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||05-JUL-13
3106|Burra Group|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp57-58.|Sturtian|Torrensian|Colour scheme shown for interpretation of Curnamona seismic sections.||Unit in Warrina Supergroup.|Includes Emeroo, Mundallio, Bungarider and Belair Subgroups.|Unconformably overlies Callanna Group.||
3106|Burra Group|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Upper part of Warrina Supergroup.|Includes Emeroo and Belair Subgroups.|Unconformably overlies Callanna Group. Is unconformably overlain by Umberatana Group.||
3106|Burra Group|62724|4|Described|p16, p17 Fig. 4|Torrensian|Torrensian|Includes the Bungarider and Belair Subgroups. Siltstone, sandstone, dolomite, magnesite, conglomerate. Geological Province: Curnamona Province.||||||07-FEB-11
3106|Burra Group|62962|5|Briefly described|p2284 Fig. 2, p2296 Tab. 6|Adelaidean|Adelaidean|Age: 777+/-7Ma (Preiss, 2000). Thickness: 3300m, estimated. Geological Province: Mount Painter Province. Consists of sandstone, quartzite, carbonate, siltstone and shale.||||||07-FEB-11
3106|Burra Group|63020|5|Briefly described|p973, p974 Fig. 2|Neoproterozoic|Neoproterozoic|Basement rocks of the Warren Inlier. Includes Emeroo Subgroup. ||||||
3106|Burra Group|63022|5|Briefly described|p1015|Neoproterozoic|Neoproterozoic|Of the Adelaide Rift Complex. Includes Boucaut Volcanics at base. Age: between 777+/-7 (SHRIMP U-Pb) and 700Ma. ||||||
3106|Burra Group|63102|5|Briefly described|p7-8,43,45-46,53|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province. Intruded by late mafic intrusives c. 472-431 Ma.|||||Siltstone, sandstone, dolomite, magnesite and conglomerate.|22-OCT-19
3106|Burra Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Undifferentiated: siltstone, sandstone, minor dark grey dolomite.||||||10-SEP-07
3106|Burra Group|64319|5|Briefly described|p354, p355, p356 Fig.2, p357 Fig.3,   |Neoproterozoic|Neoproterozoic|Hosts the Billy Springs deposit of both non-sulfide zinc and sulfide Zn-Pb mineralisation.||||Overlies Callanna Group. Is overlain by Umberatana Group.|Consists predominantly of quartzites, shales and dolomites.|
3106|Burra Group|64400|6|Mentioned|p4|||In the Adelaide Rift Complex.||||||07-FEB-11
3106|Burra Group|64647|5|Briefly described|p38 Fig. 1, p40, p41, p48|Adelaidean|Adelaidean|Overlain by Umberatana, Wilpean, Normanville and Kanmantoo Groups.||||||05-JUL-13
3106|Burra Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Adelaide Geosyncline between Centralian 1 and Centralian 2 events.||||||
3106|Burra Group|64793|6|Mentioned|p284 fig 3, p285 Fig.4, p290, p293, p295|||Adelaide Rift Complex. Age inferred from Fig.3.|c.778 - c.745 Ma.||Includes Rhynie Sandstone; River Wakefield and Emeroo Subgroups; Skillogalee Dolomite.|||
3106|Burra Group|64796|4|Described|p181, p183 fig 2, p185-193, p195-204|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex. Base is first influx of coarse clastics after Curdimurka Subgroup. Top is unconformity under Sturt Tillite. Generalised stratigraphic column on p.191.||Warrina Supergroup|Includes Emeroo Subgroup, Kalachalpa Formation, Rhynie Sandstone and Skillogalee Dolomite.||Sedimentary rocks.|
3106|Burra Group|64797|5|Briefly described|p151, p153 Fig.2,  p158, p160 Fig.8 |||See also p163-166, p167 Tb.10, p168 Tb.11, p169 Fig.12, p172 Tb.13. Adelaide Rift Complex. S-isotope data.|770||Includes Kalachalpa Formation and Skillogalee Dolomite.|||
3106|Burra Group|64801|5|Briefly described|p110|Neoproterozoic|Neoproterozoic|||Warrina Supergroup.|Skillogalee Dolomite.|Overlies the Callanna Group. Is overlain by Umberatana Group.|Largely siliciclastic, but contains widespread beds of magnesite intraclast conglomerate.|
3106|Burra Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3 |Cryogenian|Cryogenian|||||||
3106|Burra Group|65363|6|Mentioned|p9.|||Adelaide Rift Complex. Correlated with Kanpa Formation in Western Australia on basis of tentative identification of Baicalia burra in that unit.||||||
3106|Burra Group|65365|5|Briefly described|p1, 7, p9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Northern Adelaide Rift Complex. Includes Kalachalpa Formation and Boucaut Volcanics. Includes stromatolite assemblages.||||||16-MAR-12
3106|Burra Group|65366|5|Briefly described|p19, 21, p23 Fig. 3, p24|Cryogenian|Cryogenian|Adelaide Rift Complex. Includes Boucaut Volcanics, stromatolite assemblages.||||||
3106|Burra Group|65375|6|Mentioned|p25.||||||Includes Emeroo Subgroup.|||
3106|Burra Group|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|65379|5|Briefly described|p643|||Includes Opaminda Formation, Skillogalee Dolomite, Woolshed Flat Shale and Stonyfell Quartzite. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
3106|Burra Group|65493|6|Mentioned|p908, 909 Fig 1,2|Cryogenian|Cryogenian|Adelaidian units of the Flinders Ranges.||||||
3106|Burra Group|65925|5|Briefly described|pp123-124, Appendix 2.||||||Includes Humanity Seat, Opaminda, Myrtle Springs Formations; Woodnamoka Phyllite; Blue Mine Conglomerate; Wortupa Quartzite and Skillogalee Dolomite.||Siltstone, laminated; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross bedding; dolomite, blue-grey to pale pink, lenticular.|
3106|Burra Group|66464|5|Briefly described|p167, p168 Fig.2|Tonian|Tonian|Adelaide Rift Complex. Basal carbonates with evaporites and clastics; siltstone, sandstone and dolostone.||||||
3106|Burra Group|66518|5|Briefly described|p19 Fig.4, p23.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform. C.700m of this unit underlies c.550m of Umberatana Group in an 11 x 14 km basin west of Kalkaroo in a potential geothermal project.||||Unconformably overlies Callanna Group. Is overlain unconformably by Umberatana Group.||
3106|Burra Group|66522|5|Briefly described|p19, 20, 21.|Neoproterozoic|Neoproterozoic|Major changes in thickness, facies and differential erosion of the Group's units across the Nackara Arc were controlled by two major faults that were active during sedimentation. Age constrained by dating of underlying Rook Tuff (see age field).|Between 802 +/- 10 Ma  and  c.660 Ma.||Includes Skillogalee Dolomite, Bungarider Subgroup..|Overlies Curdimurka Subgroup. Is overlain by a Sturtian glacial succession.||24-SEP-15
3106|Burra Group|66884|4|Described|p36-39, p41 Fig.3, p43 Fig. 4, p44|Neoproterozoic|Neoproterozoic|Eastern Willouran Ranges.||Warrina Supergroup|Bungarider Subgroup, Mundallio Subgroup, Emeroo Subgroup|Overlies Callanna Group.||14-DEC-16
3106|Burra Group|66948|5|Briefly described|p19|Cryogenian|Cryogenian||c.800-700 Ma|||Equivalent to the lower Burra Group.||
3106|Burra Group|67180|5|Briefly described|p600, p601 Fig.1, p607|Neoproterozoic|Neoproterozoic|Established by Thomson et al (1964). Poor age constraints||||Overlies the Callanna Group, underlies the Umberatana Group.||
3106|Burra Group|67454|5|Briefly described|p564.|Neoproterozoic|Neoproterozoic|Correlated with Hussar Formation, Officer Basin (WA).||||||
3106|Burra Group|67502|6|Mentioned|p46, p57.||Cryogenian|Of the Adelaide Geosyncline. Suggested to have a time correlation with the Black River Dolomite (Calver, 1998).|||Skillogalee Dolomite.|||26-MAY-14
3106|Burra Group|67536|6|Mentioned|Map Legend||||||||Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite; fluviodeltaic sandstone and conglomerate.|
3106|Burra Group|67870|5|Briefly described|p5, p9-10, p13, p17, p20-21, p23-25|Neoproterozoic|Neoproterozoic|See also p29-30, p32-34. Adelaide Rift System. Produces a series of high amplitude, continuous, subparallel seismic reflections.|||Emeroo, Mundallio, Bungarider, Belair Subgroups.|Overlies Callanna Group. Is overlain unconformably by Umberatana Group.|Sandstone, arkose, dolostone, siltstone.|
3106|Burra Group|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as Callanna/Burra Group equivalents, including Pindyin Sandstone.||||Equivalent to Pindyin Sandstone|Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, dolomite, minor chert and quartzite.|
3106|Burra Group|67979|6|Mentioned|p528, p530 Fig.1|Cryogenian|Cryogenian|Geol. Prov: Adelaide Geosyncline (as defined by Thomson et al. 1964 and subsequent revisions)||||is overlain by Umberatana Group; overlies Callanna Group||22-SEP-14
3106|Burra Group|68030|6|Mentioned|p238|||Flinders Ranges.||Unit of Warrina Supergroup.||||
3106|Burra Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
3106|Burra Group|68243|6|Mentioned|p659, p654 |Torrensian|Torrensian|Adelaide Rift Basin.|< ca. 777 Ma|||||
3106|Burra Group|68270|5|Briefly described|p683|Cryogenian|Tonian|Adelaide Rift Complex. |||Includes Skillogalee Dolomite.|Overlain by Umberatana Group. Underlain by Callanna Group.||
3106|Burra Group|68271|5|Briefly described|p694,696|||Adelaide Rift Complex.|||Includes Skillogalee Dolomite.|||
3106|Burra Group|68713|5|Briefly described|p19, p23|||Variable exposure, from near 100% to partly obscured.||||Unconformably underlain by the Callanna Group.||
3106|Burra Group|69019|5|Briefly described|p38-41, p143.|Neoproterozoic|Neoproterozoic|Torrensian age; Adelaide Geosyncline. Thickness from 2,540 m to 8,470 m.|||Includes Emeroo, Mundallio and Bungarider Subgroups.|Overlies Callanna Group.||
3106|Burra Group|69255|6|Mentioned|p771|Neoproterozoic|Neoproterozoic|Earliest succession in the Adelaide region.||||||
3106|Burra Group|69438|6|Mentioned|p23:14|||Northern Adelaide Fold Belt.||||Lower part of this unit is correlated with Johnnys Creek beds (Amadeus Basin).||12-JUL-16
3106|Burra Group|69606|6|Mentioned|p10|||Adelaide Rift Complex. ||||Correlates with the Finke beds.||
3106|Burra Group|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|69873|5|Briefly described|p82-83|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||Correlated with lower Togari Group (Tas).||
3106|Burra Group|69937|6|Mentioned|p8|||Adelaide Geosyncline.||||Lower part correlated with Johnnys Creek Member (Bitter Springs Formation).||
3106|Burra Group|70000|5|Briefly described|p39||||Between 810 Ma and 700 Ma.||||Fluviatile to shallow marine sequences.|
3106|Burra Group|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
3106|Burra Group|70323|6|Mentioned|p213,220|||Adelaide Geosyncline.||||Overlain by Umberatana Group.||
3106|Burra Group|70334|6|Mentioned|p19-20,38|||Geological province: Gawler Craton. Of Adelaide Geosyncline.||||||
3106|Burra Group|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Warrina Supergroup.|Includes Emeroo, Mundallio, Bungarider Subgroups.|Unconformably overlies Callanna Group. Is overlain  unconformably by Umberatana Group (Heysen Supergroup).||18-JAN-19
3106|Burra Group|70405|5|Briefly described|p1, 14 figure 6, p50, p79, p97|Neoproterozoic|Neoproterozoic||||Includes Belair Subgroup, Mintaro Shale, Gilbert Range Quartzite, Kadlunga Slate||Siltstone, sandstone, dolomite, magnesite, conglomerate.|
3106|Burra Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Torrensian - Sturtian||Of Warrina Supergroup.||||
3106|Burra Group|70416|5|Briefly described|p80|||Adelaide Rift Complex. Contains the stromatolite Tungussia wilkatanna.||||||
3106|Burra Group|70657|5|Briefly described|p8, p9 Fig.3, p50, p54|Neoproterozoic|Neoproterozoic|Curnamona Province.||||Is overlain unconformably by Umberatana Group.|Siltstone, sandstone, dolomite, magnesite, conglomerate; low-grade metamorphosed.|
3106|Burra Group|70658|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup.|||Siltstone, sandstone, dolomite, magnesite, conglomerate.|
3106|Burra Group|70660|5|Briefly described|p46|||||||Overlain by the North Maslin Sand.||
3106|Burra Group|70790|6|Mentioned|p258|Neoproterozoic|Neoproterozoic||~777-700 Ma.|||||
3106|Burra Group|70819|6|Mentioned|p11, 13|Neoproterozoic|Neoproterozoic|Clare Valley.|||Emeroo, Mundallio, Bungarider, Belair Subgroups.|||
3106|Burra Group|71129|5|Briefly described|p101-103,107|||Of Adelaide Geosycline. Deposited during the Torrensian, contemporaneous with erosion of Beda Basalt and Backy Point Formation on the Stuart Shelf.||||||
3106|Burra Group|71237|14|Not recorded|p8, 9 |||||||||
3106|Burra Group|71238|14|Not recorded|p1,2, 9|||||||||
3106|Burra Group|71239|14|Not recorded|p3, 5, 9|||||||||
3106|Burra Group|71240|14|Not recorded|p5, p6, p7, 9-10|||New name.||||||
3106|Burra Group|71322|5|Briefly described|p52 Fig.1|Neoproterozoic|Neoproterozoic||||||Laminated siltstone; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross-bedding; blue-grey to pale pink, lenticular dolomite.|
3106|Burra Group|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3106|Burra Group|71529|14|Not recorded|p2, 3|||||||||
3106|Burra Group|71711|6|Mentioned|p401, p402 Fig 10|||Contains abundant 1650-1500 Ma and 1200-1000 Ma detrital zircons.|||Includes Skillogalee Dolomite.|||
3106|Burra Group|72369|5|Briefly described|p43|||Of Adelaide Rift Complex. Lower part can be correlated with Johnnys Creek Formation, Bitter Springs Group (Amadeus Basin) (Grey et al 2011, Hill et al 2011).||||||
3106|Burra Group|72375|5|Briefly described|p13|||Of Adelaide Rift Complex.||||Correlable with Johnnys Creek Formation.||
3106|Burra Group|72429|5|Briefly described|p958|||||||||
3106|Burra Group|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Subsurface only in the map area. Shown as part of diapir formation diagram, p1.||||Overlies Callanna Group and underlies Pualco Tillite.|Undifferentiated siltstone, sandstone and dolomite.|
3106|Burra Group|72450|5|Briefly described|Brochure map||||c. 750 Ma||Includes the Belair Subgroup, Mitcham Quartzite, Saddleworth Formation, Stonyfell Quartzite, Woolshed Flat Shale, Montacute Dolomite and Aldgate Sandstone.|||
3106|Burra Group|72461|6|Mentioned|p19|||Deposited during a period of rifting, not Describedribed in NSW.|c. 830-770 Ma|||||
3106|Burra Group|72478|6|Mentioned|Fig. 7 p70|||||||||
3106|Burra Group|72489|6|Mentioned|p4 Fig.3|Tonian|Tonian|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||Overlies the Callanna Group.||14-SEP-20
3106|Burra Group|72601|6|Mentioned|p6||||||Boucaut Volcanics|||
3106|Burra Group|72613|6|Mentioned|p2 fig 1|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges.||||||
3106|Burra Group|73086|6|Mentioned|p39, p57|||Adelaide Rift Complex. Contains the first appearance of the acritarch Cerebrosphaera buickii in the Adelaide Rift Complex, which is temporally constrained by the underlying Rock Tuff (795 +/- 6 Ma, TIMS U-Pb).||||Underlain by Callanna Group. May partly correlate to Johnnys Creek Formation (Bitter Springs Group) and Wallara Formation.||
3106|Burra Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
3106|Burra Group|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, shale and sandstone, minor dolomite.|09-DEC-21
3106|Burra Group|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears in the Legend as CALLANNA/BURRA GROUP EQUIVALENTS and mapped as one unit. Said to include Pindyin Sandstone, but does not specify to which Group it belongs.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Presented as Callanna/Burra Group equivalents. Mapped as one unit. Includes Pindyin Sandstone (but which Group contains it is not mentioned). Subsurface.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, laminated; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross-bedding; dolomite, blue-grey to pale pink, lenticular.|
3106|Burra Group|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Mapped as one unit and named in the Map Legend as CALLANNA/BURRA GROUP EQUIVALENTS. Said to include Pindyin Sandstone, but it is not spelled out which Group is the Parent.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73188|5|Briefly described|[See comments]|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Accommodation space provided by eastward-dipping listric extensional faults. Fluvial, deltaic, lagoonal and marine shelf environments. p: 305, 315-316, 319, 321, 323-325, 327, 330, 339-341, 352, 354.|||Belair Subgroup, Bungarider Subgroup, Mundallio Subgroup, Emeroo Subgroup, and units therein|Disconformably[?] underlain by River Broughton Beds.|Mixed siliciclastic and carbonate rocks.|
3106|Burra Group|73222|5|Briefly described|p5-6, p20|Tonian|Tonian|Adelaide Rift Complex. Torrensian to Sturtian Thickness: 3,000 to 8,000 m. Represents the opening of the rift into a shallow ocean.||Warrina Supergroup|||Shale, siltstone, heavy mineral laminated sandstone and dolomite.|
3106|Burra Group|73227|6|Mentioned|p23|||||||||
3106|Burra Group|73234|6|Mentioned|p5|||||||||
3106|Burra Group|73236|6|Mentioned|p47|Tonian|Tonian|Torrensian. Deposited in fluvial, marginal marine and marine shelf settings. Represents the oldest sedimentary rocks in the Adelaide area.|c. 800-700 Ma||||Sand, silt and dolomite.|
3106|Burra Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably underlain by Callanna Group. Unconformably overlain by Umberatana Group.|Metasediments.|
3106|Burra Group|73262|5|Briefly described|p580, p582-583, p586|[Tonian?]|[Tonian?]|Adelaide Rift Complex. Shallow marine depositional environment for basal strata interbedded with the Boucaut Volcanics. Age of the Boucaut Volcanics constrains the base of the Burra Group to 788+/-6 Ma.||Warrina Supergroup|Boucaut Volcanics|Underlain by Callanna Group.|Siltstone, shale, sandstone, dolomite. Includes mudstone and some cross-bedded sandstones.|30-JAN-23
3106|Burra Group|74367|4|Described|p3, p5-6, p7 Fig.6, p13, p17-18, p20|||Proximal marine to marine formations. Age is constrained by deposition after the Mount Crawford Granite Gneiss (812+/-6 Ma).||Warrina Supergroup|Emeroo Subgroup, Mundallio Subgroup, Bungarider Subgroup, Belair Subgroup|Unconformably overlies Wooltana Volcanics, Mount Crawford Granite Gneiss. Overlies Callanna Group|Dominated by clastic and carbonate rocks.|
3106|Burra Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
3162|Burrungule Member|22875|5|Briefly described|p26 Table1|||||||||
3162|Burrungule Member|23671|3|Fully described|p2|Middle Eocene|Middle Eocene|Carbonaceous clay with occasional silt and coarse sand interbeds. Disconformably overlain by Gambier Limestone. Max. thickness: ~90ft.||||||05-FEB-08
3162|Burrungule Member|23818|5|Briefly described|p174 Fig.84, p176|Middle Eocene|Middle Eocene|Of the Tartwaup Formation. Geological Province: Otway Basin. Max. thickness: 34 ft. Contains many small planktonic foraminifera.||||||
3162|Burrungule Member|24551|5|Briefly described|p292 Fig. 10.3|||Of the Wangerrip Group.||||||
3162|Burrungule Member|29355|6|Mentioned|p188|||||||||
3162|Burrungule Member|29591|6|Mentioned|p92|||||||||
3162|Burrungule Member|29697|6|Mentioned|Fig.11|||||||||
3162|Burrungule Member|30179|6|Mentioned|p32|||||||||
3162|Burrungule Member|30514|6|Mentioned|p108|||Late Eocene to early Middle Miocene age||||||
3162|Burrungule Member|30754|6|Mentioned|p12|||See also P14. Stratigraphic table.||||||
3162|Burrungule Member|30917|6|Mentioned|p54|||||||||
3162|Burrungule Member|31245|4|Described|p78|||See also p80. Fauna. Lithology||||||31-JAN-07
3162|Burrungule Member|31246|6|Mentioned|p56|||M. Eocene||||||
3162|Burrungule Member|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
3162|Burrungule Member|31920|4|Described|p57|||See also Fig. 3-2, 3,4,5. Eocene||||||
3162|Burrungule Member|31922|6|Mentioned|Table 3|||||||||
3162|Burrungule Member|32116|6|Mentioned|p51|||||||||
3162|Burrungule Member|32117|6|Mentioned|Fig.2|||||||||
3162|Burrungule Member|32119|6|Mentioned|p483|||Eocene||||||
3162|Burrungule Member|32120|5|Briefly described|p275|||Eocene or fauna||||||
3162|Burrungule Member|33109|6|Mentioned|p84|||Refers aquifers||||||
3162|Burrungule Member|33224|6|Mentioned|p69|||Palynology||||||
3162|Burrungule Member|33716|6|Mentioned|p15|||||||||
3162|Burrungule Member|33938|6|Mentioned|p48|||Refs. McGowran et al (1971) & Harris (1971).||||||
3162|Burrungule Member|34295|6|Mentioned|p30|||Eocene. fauna||||||
3162|Burrungule Member|34308|5|Briefly described|p176|||U.Eocene. See Fig.84||||||
3162|Burrungule Member|35066|6|Mentioned|Fig.8.9|||||||||
3162|Burrungule Member|37548|5|Briefly described|p131|||||||||
3162|Burrungule Member|38068|6|Mentioned|Fig.7|||||||||
3162|Burrungule Member|38903|5|Briefly described|Table 2|||||||||
3162|Burrungule Member|39408|6|Mentioned|Fig.5|||||||||
3162|Burrungule Member|40003|5|Briefly described|p44|||See also Fig.10||||||
3162|Burrungule Member|40555|6|Mentioned|Fig.4|||||||||
3162|Burrungule Member|41517|6|Mentioned|p134|||||||||
3162|Burrungule Member|41520|5|Briefly described|Fig.12|||||||||
3162|Burrungule Member|41626|6|Mentioned|p63|||||||||
3162|Burrungule Member|41769|5|Briefly described|p25|||||||||
3162|Burrungule Member|41868|5|Briefly described|p535|||||||||
3162|Burrungule Member|42827|5|Briefly described|Fig 8.9|||||||||
3162|Burrungule Member|47054|6|Mentioned|p491|||||||||
3162|Burrungule Member|60538|5|Briefly described|p470, Fig. 10, 471 Fig. 10|Early Eocene|Early Eocene|Of the Dilwyn Formation. Geological Province: Otway Basin.||||||31-JAN-07
3162|Burrungule Member|61155|5|Briefly described|p18|Middle Eocene|Early Eocene|Of the Tartwaup Formation. Max. thickness: 300m. Geological Province: Otway Basin (Gambier Embayment).||||||03-MAR-10
3162|Burrungule Member|61182|6|Mentioned|p25|||Defined by Harris (1965) for the basal mudstone unit of Nirranda Group in the South Australian part of the Otway Basin. Significantly different in age and stratigraphic relationships to Burrungule Formation of Blake (1980) in Victoria. ||||||
3162|Burrungule Member|63124|6|Mentioned|p88|||Of Harris (1966). Of the Tartwaup Formation - a synonym of Pember Mudstone (Wangerrip Group). ||||||
3270|Cadelga Limestone|30055|6|Mentioned|p153|||||||||
3270|Cadelga Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
3270|Cadelga Limestone|30921|6|Mentioned|Map legend|Miocene|Miocene|||||||
3270|Cadelga Limestone|33820|6|Mentioned|Map legend|Miocene|Miocene|||||||
3270|Cadelga Limestone|33827|6|Mentioned|p19|||Table 1||||||
3270|Cadelga Limestone|33937|4|Described|p5|||See also PP6-11.||||||
3270|Cadelga Limestone|35793|6|Mentioned|Fig.2|||||||||
3270|Cadelga Limestone|39445|5|Briefly described|Table 14|||||||||
3270|Cadelga Limestone|39908|6|Mentioned|p10|||||||||
3270|Cadelga Limestone|40926|6|Mentioned|Table 3|||||||||
3270|Cadelga Limestone|41098|6|Mentioned|p177|||||||||
3270|Cadelga Limestone|41165|6|Mentioned|Fig.21|||||||||
3270|Cadelga Limestone|42746|5|Briefly described|p17|||||||||
3270|Cadelga Limestone|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||25-MAY-05
3270|Cadelga Limestone|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
3270|Cadelga Limestone|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
3270|Cadelga Limestone|44133|5|Briefly described|p194, 190 Fig. 10.30|Early Pliocene|Late Miocene|Geoloigcal Province: Lake Eyre Basin. Thickness: 5m. ||||||
3270|Cadelga Limestone|45145|6|Mentioned|Table 7|||||||||
3270|Cadelga Limestone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
3270|Cadelga Limestone|60080|5|Briefly described|Map legend|Pliocene|Miocene|Limestone, chalcedony and greenish silty-sandstone. Overlies Whitula Formation.||||||03-MAY-13
3270|Cadelga Limestone|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Lake Eyre Basin.||||||
3270|Cadelga Limestone|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||
3270|Cadelga Limestone|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Overlies the Doonbarra Formation. Age: 22-12 Ma. Thickness in Queensland: 5 m. Geological Province: Lake Eyre Basin and southwest Queensland.||||||03-OCT-13
3270|Cadelga Limestone|64197|6|Mentioned|p630 Fig.6|Pliocene|Miocene|Eromanga Basin.||||Unconformably overlies the  Etadunna Formation.||
3270|Cadelga Limestone|66131|5|Briefly described|p240, p245|Miocene|Miocene|||Of the Whitula Formation.||Overlies Doonbarra Formation. Correlative of the Etadunna Formation and the Alberga Limestone Member.|Cherty and dolomitic lacustrine limestone up to 5m thick.|
3270|Cadelga Limestone|67119|5|Briefly described|Map legend.|Pliocene|Miocene|Lacustrine deposits.|||||Pale, cherty, dolomitic limestone.|
3270|Cadelga Limestone|69019|6|Mentioned|p105 Fig.25.|Miocene|Miocene|Callabonna Sub-basin.||||||
3270|Cadelga Limestone|69023|6|Mentioned|p108|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
3270|Cadelga Limestone|69599|5|Briefly described|p584, p601-602|Pliocene|Pliocene|In SA. Correlatives in the Farrars Syncline (CANTERBURY 250k sheet) and isolated thin limestone units near Haddon Corner. <5m thick. Lacustrine deposits. Has silcrete development.||||Overlies Doonbara (and locally interdigitates with it) and Whitula Formations.|Limestone and dolomitic limestone with subordinate silty sandstone.|
3270|Cadelga Limestone|73106|5|Briefly described|Map legend.|Pliocene|Miocene||||||Limestone, pale, cherty, dolomitic, lacustrine.|
3284|Cadna-owie Formation|730|6|Mentioned|p24, p25.|||Paralic.||||||11-NOV-14
3284|Cadna-owie Formation|12597|4|Described|p492 Tb.1, p499|Barremian|Early Cretaceous|Eromanga Basin. Up to 110m thick. Contains marine bivalves, gastropods, dinoflagellates and arenaceous foraminifera.|||Includes Mount Anna Sandstone, and Wyandra Sandstone, Members.|Conformably overlies Hooray Sandstone, Murta Member and Algebuckina Sandstone.|Siltstone and silty mudstone with interbeds of fine-grained labile sandstone and minor glauconite grading upwards to quartzose sandstone; overlain by Wyandra Sandstone Member (q.v.).|
3284|Cadna-owie Formation|13497|5|Briefly described|p50, p66-p67, p216|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p115, p115 fig 6.33, p138 fig 8.17, p141, p146, p149-p152, p154 .||||Overlies the Murta Formation. Overlain by the Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|13516|5|Briefly described|p167 fig 10,  p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member|||
3284|Cadna-owie Formation|22839|6|Mentioned|P33|||||||||
3284|Cadna-owie Formation|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Barremian|Valanginian|Known as the Gum Vale beds in Tibooburra area. Max. thickness: 130m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p314.||||||
3284|Cadna-owie Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Late Jurassic|||||||
3284|Cadna-owie Formation|22874|6|Mentioned|P18|||||||||
3284|Cadna-owie Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Wallumbilla Formation, underlying unit is Murta Formation||||||
3284|Cadna-owie Formation|22912|5|Briefly described|33|||Geol. province: Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|22922|6|Mentioned|33 fig 2|||||||||
3284|Cadna-owie Formation|23054|5|Briefly described|p21,23-4|Aptian|Aptian|||||||
3284|Cadna-owie Formation|23056|6|Mentioned|93 table 5|||Geol province Eromanga Basin||||||
3284|Cadna-owie Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Neales River Group.||||||
3284|Cadna-owie Formation|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age Neocomian-Aptian. Formerly named as `Transition Beds' the new name Cadna-owie Formation was first used by Wopfner et al (1970).  On STRZELECKI the unit is underlain by Murta Formation (conformity).||||||
3284|Cadna-owie Formation|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
3284|Cadna-owie Formation|23375|4|Described|Fig2 p264,265,267,269,271,277|Barremian|Valanginian|Geol. Prov:  Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|23425|6|Mentioned|p391.|||Variation of Cadna-Owie Formation.||||||
3284|Cadna-owie Formation|23430|4|Described|p523 + p524 Table 14.7|||Eromanga Basin Province.||||||16-SEP-08
3284|Cadna-owie Formation|23818|4|Described|p141 Fig.65, p144 Fig.66, p156|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Neales River Group. Max. thickness: 250 ft. Overlying unit: Bulldog Shale.||||||
3284|Cadna-owie Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
3284|Cadna-owie Formation|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
3284|Cadna-owie Formation|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
3284|Cadna-owie Formation|24067|5|Briefly described|p249 Fig.2|Mesozoic|Mesozoic|Geological Province: Officer Basin.||||||
3284|Cadna-owie Formation|24092|6|Mentioned|p5|||Geological Province: Great Artesian Basin.||||||
3284|Cadna-owie Formation|24112|5|Briefly described|p254 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin||||||
3284|Cadna-owie Formation|24175|3|Fully described|p19, p17 Fig. 3|Aptian|Neocomian|Thin transgressive sequence of sandstone, siltstone and shale.  Lies transitionally between Bulldog Shale above and Algebuckina Sandstone below.  Max. thickness: 50m.||||||
3284|Cadna-owie Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member.  Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24243|5|Briefly described|p3 Fig.2|Early Cretaceous|Early Cretaceous|Of Blythesdale Group.||||||
3284|Cadna-owie Formation|24321|5|Briefly described|Map legend|Barremian|Neocomian|Of theNeales River Group.||||||03-AUG-06
3284|Cadna-owie Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24392|5|Briefly described|p139, p144 Appendix 1|Valanginian|Berriasian|Locally known as Parabarana Sandstone. See also page 140 Fig.1. Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24507|6|Mentioned|p27|||Oil production has commenced from this unit. Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24510|6|Mentioned|p48|||Includes Livingston Tillite Member.||||||
3284|Cadna-owie Formation|29379|4|Described|p30|||Lithology. Early-Lower Cretaceous.||||||
3284|Cadna-owie Formation|29591|6|Mentioned|Fig.22|||||||||
3284|Cadna-owie Formation|29659|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|29660|6|Mentioned|p6|||||||||
3284|Cadna-owie Formation|29838|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|30024|6|Mentioned|p335|||See also Fig.3.||||||
3284|Cadna-owie Formation|30075|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|30512|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|30804|6|Mentioned|p7|||See also P10 and Table 1.||||||
3284|Cadna-owie Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
3284|Cadna-owie Formation|30917|6|Mentioned|p42|||||||||
3284|Cadna-owie Formation|30919|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|30920|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|30924|6|Mentioned|Map legend|Aptian|Aptian|||||||
3284|Cadna-owie Formation|31208|6|Mentioned|p46|||See also Fig. 7||||||
3284|Cadna-owie Formation|31244|6|Mentioned|p3|||Lower Cretaceous||||||
3284|Cadna-owie Formation|31249|6|Mentioned|p63|||||||||
3284|Cadna-owie Formation|31251|6|Mentioned|p74|||Microfloral assemblage in type section||||||
3284|Cadna-owie Formation|31697|6|Mentioned|p5|||L.Cretaceous||||||
3284|Cadna-owie Formation|31699|4|Described|p133|||L.Cretaceous||||||
3284|Cadna-owie Formation|32033|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|32204|4|Described|p8|||Details of Refraction and p8.  L.Cret.||||||03-AUG-06
3284|Cadna-owie Formation|32205|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|32275|6|Mentioned|p8|||Refers Wopfner Freytag & Heath (1970)||||||
3284|Cadna-owie Formation|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|32314|6|Mentioned|Fig. 4|||||||||
3284|Cadna-owie Formation|33017|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
3284|Cadna-owie Formation|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33490|6|Mentioned|p30|||Correlation||||||
3284|Cadna-owie Formation|33491|4|Described|p56|||Mention Fig.2||||||
3284|Cadna-owie Formation|33521|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|33523|4|Described|p27|||||||||
3284|Cadna-owie Formation|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33824|6|Mentioned|p12|||Table 2||||||
3284|Cadna-owie Formation|33825|6|Mentioned|p8|||Lithology||||||
3284|Cadna-owie Formation|33827|5|Briefly described|p13|||Table 2||||||
3284|Cadna-owie Formation|33828|6|Mentioned|p5|||Table 1||||||
3284|Cadna-owie Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
3284|Cadna-owie Formation|33844|6|Mentioned|p35|||Refers Wopfner (1969)||||||
3284|Cadna-owie Formation|33933|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|33936|6|Mentioned|Fig.3a|||Cretaceous.||||||
3284|Cadna-owie Formation|33938|6|Mentioned|p46|||||||||
3284|Cadna-owie Formation|33939|2|Defined|p394|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33964|4|Described|p6|||Cretaceous||||||
3284|Cadna-owie Formation|33971|6|Mentioned|p24|||See also P25 & Fig.15.||||||
3284|Cadna-owie Formation|33976|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|34611|3|Fully described|p156|||Fig.65. Correlation chart. Cretaceous.||||||16-SEP-08
3284|Cadna-owie Formation|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
3284|Cadna-owie Formation|35239|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|35548|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|35549|6|Mentioned|Fig.8|||Now called Marree Formation||||||
3284|Cadna-owie Formation|35560|6|Mentioned|p292|||||||||
3284|Cadna-owie Formation|35628|4|Described|Table 4|||||||||
3284|Cadna-owie Formation|35663|6|Mentioned|p124|||||||||
3284|Cadna-owie Formation|35793|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
3284|Cadna-owie Formation|36214|5|Briefly described|p58|||||||||
3284|Cadna-owie Formation|36243|6|Mentioned|Table 6A|||||||||
3284|Cadna-owie Formation|36251|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|36494|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|36552|6|Mentioned|p59|||||||||
3284|Cadna-owie Formation|36571|6|Mentioned|Table 4|||||||||
3284|Cadna-owie Formation|36733|6|Mentioned|p14|||See also P53.||||||
3284|Cadna-owie Formation|36895|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|36912|6|Mentioned|p75|||||||||
3284|Cadna-owie Formation|36920|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|36922|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|36966|6|Mentioned|p83|||||||||
3284|Cadna-owie Formation|37776|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|37995|6|Mentioned|p66|||||||||
3284|Cadna-owie Formation|38022|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|38068|4|Described|p72|||||||||
3284|Cadna-owie Formation|38199|6|Mentioned|p428|||||||||
3284|Cadna-owie Formation|38604|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|38605|6|Mentioned|p20|||See also Table 4.||||||
3284|Cadna-owie Formation|38814|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|39070|4|Described|p364|||||||||
3284|Cadna-owie Formation|39211|5|Briefly described|p23|||See also Figs 4,7,8,10,13-15 etc. Correlation||||||
3284|Cadna-owie Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
3284|Cadna-owie Formation|39445|5|Briefly described|Table 10|||||||||
3284|Cadna-owie Formation|39630|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|39846|6|Mentioned|p44|||||||||
3284|Cadna-owie Formation|39847|5|Briefly described|p37|||||||||
3284|Cadna-owie Formation|39914|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|39943|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|39988|6|Mentioned|p291|||||||||
3284|Cadna-owie Formation|39989|4|Described|p423|||||||||
3284|Cadna-owie Formation|40003|6|Mentioned|p33|||See also Fig.8||||||
3284|Cadna-owie Formation|40030|6|Mentioned|p132|||||||||
3284|Cadna-owie Formation|40121|6|Mentioned|p446|||||||||
3284|Cadna-owie Formation|40199|4|Described|p25|||||||||
3284|Cadna-owie Formation|40220|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40249|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|40544|6|Mentioned|p157|||||||||
3284|Cadna-owie Formation|40670|6|Mentioned|Fig.9|||||||||
3284|Cadna-owie Formation|40675|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|40681|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40687|3|Fully described|p417|||||||||
3284|Cadna-owie Formation|40832|3|Fully described|p456|||||||||
3284|Cadna-owie Formation|40833|6|Mentioned|p468|||||||||
3284|Cadna-owie Formation|40910|6|Mentioned|p16|||||||||
3284|Cadna-owie Formation|40911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|40926|3|Fully described|p16|||||||||
3284|Cadna-owie Formation|40962|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|41060|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|41061|6|Mentioned|Fig.6|||Generalized stratigraphy||||||
3284|Cadna-owie Formation|41063|5|Briefly described|p40|||||||||
3284|Cadna-owie Formation|41064|6|Mentioned|p60|||||||||
3284|Cadna-owie Formation|41084|5|Briefly described|p81|||||||||
3284|Cadna-owie Formation|41085|3|Fully described|p87|||||||||
3284|Cadna-owie Formation|41086|3|Fully described|p104; Fig.3|||||||||
3284|Cadna-owie Formation|41088|6|Mentioned|p140|||||||||
3284|Cadna-owie Formation|41089|6|Mentioned|p156|||||||||
3284|Cadna-owie Formation|41097|6|Mentioned|p165|||||||||
3284|Cadna-owie Formation|41098|4|Described|p175|||||||||
3284|Cadna-owie Formation|41165|5|Briefly described|p360|||||||||
3284|Cadna-owie Formation|41175|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|41176|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|41177|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|41179|6|Mentioned|p262|||||||||
3284|Cadna-owie Formation|41182|6|Mentioned|p287|||||||||
3284|Cadna-owie Formation|41183|6|Mentioned|p310|||||||||
3284|Cadna-owie Formation|41184|6|Mentioned|p328|||||||||
3284|Cadna-owie Formation|41186|4|Described|p212|||||||||
3284|Cadna-owie Formation|41214|6|Mentioned|p257|||||||||
3284|Cadna-owie Formation|41216|6|Mentioned|p305|||||||||
3284|Cadna-owie Formation|41219|4|Described|p347|||Mention p351.||||||03-AUG-06
3284|Cadna-owie Formation|41247|6|Mentioned|p126|||||||||
3284|Cadna-owie Formation|41266|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|41361|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|41523|5|Briefly described|p271,p275|||||||||
3284|Cadna-owie Formation|41535|6|Mentioned|p368|||||||||
3284|Cadna-owie Formation|41681|6|Mentioned|p22,p3|||||||||
3284|Cadna-owie Formation|41705|6|Mentioned|p116|||||||||
3284|Cadna-owie Formation|41707|5|Briefly described|p163|||||||||
3284|Cadna-owie Formation|41712|6|Mentioned|p282|||||||||
3284|Cadna-owie Formation|41724|5|Briefly described|p382|||||||||
3284|Cadna-owie Formation|41950|5|Briefly described|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42061|4|Described|Fig,11 P159|||||||||
3284|Cadna-owie Formation|42064|6|Mentioned|Fig.4 P.170|||||||||
3284|Cadna-owie Formation|42067|4|Described|Appendix 2|||||||||
3284|Cadna-owie Formation|42090|6|Mentioned|p28|||||||||
3284|Cadna-owie Formation|42283|6|Mentioned|p89|||||||||
3284|Cadna-owie Formation|42293|5|Briefly described|Fig.3 P.19|||||||||
3284|Cadna-owie Formation|42341|6|Mentioned|Fig.7 P57|||||||||
3284|Cadna-owie Formation|42346|5|Briefly described|Fig.3 P80|Jurassic||||||||
3284|Cadna-owie Formation|42375|6|Mentioned|Fig. 28 P125, Table1|Late Cretaceous|Jurassic|Eromanga Basin||||||
3284|Cadna-owie Formation|42395|5|Briefly described|Fig.13 P83|||||||||
3284|Cadna-owie Formation|42397|6|Mentioned|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42429|5|Briefly described|Fig.3 P155|||||||||
3284|Cadna-owie Formation|42446|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|42447|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|42465|5|Briefly described|Map Legend|||||||||
3284|Cadna-owie Formation|42469|4|Described|p31|||||||||
3284|Cadna-owie Formation|42474|6|Mentioned|p25|||||||||
3284|Cadna-owie Formation|42520|5|Briefly described|p6|||||||||
3284|Cadna-owie Formation|42602|6|Mentioned|Fig.2 p20|||||||||
3284|Cadna-owie Formation|42746|4|Described|p10|||See also Fig.6, Fig.2||||||
3284|Cadna-owie Formation|42749|5|Briefly described|p31, Fig.9 p31|||see also Fig.2 p27||||||03-AUG-06
3284|Cadna-owie Formation|42816|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|42905|5|Briefly described|p19|||see also Fig 5.3||||||
3284|Cadna-owie Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
3284|Cadna-owie Formation|43002|5|Briefly described|Fig.2,p135|||||||||
3284|Cadna-owie Formation|43004|5|Briefly described|Table 1,p179|||||||||
3284|Cadna-owie Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone and siltstone.||||||25-MAY-05
3284|Cadna-owie Formation|43071|6|Mentioned|p20|||||||||
3284|Cadna-owie Formation|43085|5|Briefly described|Fig.6|||||||||
3284|Cadna-owie Formation|43094|5|Briefly described|p36|||||||||
3284|Cadna-owie Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
3284|Cadna-owie Formation|43114|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|43122|5|Briefly described|p23|||see also Fig. 2.||||||
3284|Cadna-owie Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43591|6|Mentioned|p40|||||||||
3284|Cadna-owie Formation|43602|4|Described|191|||Geological Province: Eromanga Basin.||||||16-SEP-08
3284|Cadna-owie Formation|43743|6|Mentioned|Fig.2,p33||Early Cretaceous|||||||
3284|Cadna-owie Formation|43840|5|Briefly described|Fig3 p12|||Cretaceous-Jurassic age||||||12-JUL-16
3284|Cadna-owie Formation|44133|4|Described|p112, 104 Fig. 9.11|Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Previously named 'Transition beds'. Thickness: up to 100m.  Overlies: Murta Formation. Onlaps Algebuckina Sandstone.||||||11-NOV-13
3284|Cadna-owie Formation|44289|5|Briefly described|Map Legend||Aptian|||||||
3284|Cadna-owie Formation|44658|14|Not recorded|map legend|||Neoc.-Albian (G53-15).||||||
3284|Cadna-owie Formation|45110|6|Mentioned|p107|||||||||
3284|Cadna-owie Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
3284|Cadna-owie Formation|45168|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|46791|6|Mentioned|Fig.11|||||||||
3284|Cadna-owie Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
3284|Cadna-owie Formation|46939|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
3284|Cadna-owie Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
3284|Cadna-owie Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Contains Wyandra Sandstone Member. Overlies Murta Formation and part of Algebuckina Sandstone; overlain by Wallumbilla Formation and Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
3284|Cadna-owie Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse sands and grits, ferruginous sandstones.||||||
3284|Cadna-owie Formation|61014|5|Briefly described|pp532-533, p545, p550.|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Fluvio-lacustrine conditions characterised by internal drainage and infill of large interior cratonic lakes.|||Includes Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone, siltstone, calcareous sandstone and pebbly sandstone.||||||
3284|Cadna-owie Formation|61312|4|Described|p73, p64, p67 Fig.E5|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone and Warratta Sandstone Members. The top of the unit has been called "Main Datum". Shale, minor sandstone. Overlain by Wallumbilla Fm. Geol. Prov: Eromanga Basin. Equivalent in the Surat Basin is Bungil Fm.||||||
3284|Cadna-owie Formation|61560|6|Mentioned|p492||Cretaceous|During its deposition this unit was impacted by the Tookoonooka meterorite fragment(s) a large circular structure in the Mesozoic strata of the Eromanga Basin. ||||||
3284|Cadna-owie Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Includes Wyrandra Sandstone Member. Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
3284|Cadna-owie Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|Misspelling of Cadna-Owie Formation.||||||14-APR-08
3284|Cadna-owie Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Murta Formation and Namur Sandstone. Is overlain by Wallumbilla Formation and Bulldog Shale.||
3284|Cadna-owie Formation|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member. Geological Province: Eromanga Basin.||||||21-APR-08
3284|Cadna-owie Formation|63450|5|Briefly described|p83|Cretaceous|Jurassic |May be equivalent to the upper part of Longsight Sandstone, which was renamed Cadna-owie Formation by Mond and Harrison (1978). Overlain by Rolling Downs Group. Geological province: Georgina Basin.||||||07-FEB-11
3284|Cadna-owie Formation|63894|5|Briefly described|p169|Early Cretaceous|Jurassic|Aquifer. Overlies Algebuckina Sandstone. Underlies Bulldog Shale.||||||
3284|Cadna-owie Formation|63979|2|Defined|p46, Fig. 44|Barremian|Valanginian|Contains Mount Anna Sandstone Mbr at top (SA), Wyandra Sandstone Mbr (Qld). Informally subdivided into upper + lower Cadna-owie Fm. Overlies Algebuckina Sst.Thick: 90m.Geol.p: Eromanga Basin. Interbedded sandstone, siltstone, silty mudstone + mudstone.||||||07-FEB-11
3284|Cadna-owie Formation|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlain by Bulldog Shale and Wallumbilla Formation; overlies Hooray and Algebuckina Sandstones.||10-DEC-15
3284|Cadna-owie Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Marks the transition from fluvio-lacustrine and deltaic, to paralic and marine, environments.||||Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone.||
3284|Cadna-owie Formation|64696|5|Briefly described|p133 Fig.14|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|64778|6|Mentioned|p13|Jurassic|Jurassic|Pedirka and Simpson Desert Basins.||||||
3284|Cadna-owie Formation|64783|6|Mentioned|p85 Figs.3 and 4|||||||||15-NOV-17
3284|Cadna-owie Formation|64856|5|Briefly described|p98|||Eromanga Basin unit, laterally equivalent to the Bungil Formation.| | ||||31-JAN-13
3284|Cadna-owie Formation|65194|6|Mentioned|p46, p48|||Main aquifer in the Great Artesian Basin. Separated from Eyre Formation by clay-rich rocks of the Marree Subgroup.||||||
3284|Cadna-owie Formation|65238|5|Briefly described|p10|Early Cretaceous|Late Jurassic|See also variations on this name: Cadna Owie Formation and Cadnaowie Formation in the figures. Eromanga basin. Fine grained sandstone, siltstone and claystone with minor limestone||||||
3284|Cadna-owie Formation|65309|6|Mentioned|pp14-15. |||||||Is overlain by Algebuckina Sandstone in much of the Eromanga Basin.||
3284|Cadna-owie Formation|65342|5|Briefly described|pp9-10.|||Eromanga Basin. Max. thickness at least 59 m.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.|Sandstone, siltstone.|
3284|Cadna-owie Formation|65374|5|Briefly described|p30||Cretaceous|||||||
3284|Cadna-owie Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Jurassic||||||Fluvial to marginal marine sandstone.|
3284|Cadna-owie Formation|65385|5|Briefly described|pS133, pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Includes Trinity Well Sandstone Member and Wyandra Sandstone Member. Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation.||||||08-MAR-12
3284|Cadna-owie Formation|65489|5|Briefly described|p49, p55-58, p61, p96, p155-156, p160|Early Cretaceous|Early Cretaceous|Eromanga Basin. 80m thick. Oil and gas shows. Regional sand sheet with good to excellent reservoir quality. Intraformational siltstone  seal.||||Overlies Murta Formation. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|65925|5|Briefly described|p20, p57, Appendix 2.|Cretaceous|Cretaceous|Frome Embayment, Eromanga Basin. Equivalent to Mount Anna Sandstone and Parabarana Sandstone. Discharge area for GAB aquifer via diffuse upwards leakage and mound springs.||||Is overlain by Bulldog Shale.|Sandstone, siltstone and carbonaceous claystone; minor conglomerate.|
3284|Cadna-owie Formation|66303|5|Briefly described|pp27-28.|Early Cretaceous|Early Cretaceous|Stratigraphically equivalent to Parabarana Sandstone. A thin, fine-grained unit widely recognised in Eromanga Basin. Correlated with Foraminisporis wonthaggiensis spore-pollen zone.|||Includes Livingston Tillite Member.|Is overlain by Bulldog Shale.|Pale grey siltstone and fine-grained sandstone, with minor carbonaceous claystone intervals; local diamictites, pebbles and coarse breccia layers.|
3284|Cadna-owie Formation|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||||Is overlain by Bulldog Shale. Age-equivalent to Parabarana Sandstone in the northern Eromanga Basin.|Sands and silts.|06-FEB-14
3284|Cadna-owie Formation|66520|5|Briefly described|p11-12. |Cretaceous|Cretaceous|Gawler Craton. 18 m thick.|||||Feldspathic sandstone.|
3284|Cadna-owie Formation|66529|5|Briefly described|p10, p12 Fig.5, p16 |||Eromanga Basin. Appears on p16 as (Cadna-owie and Hooray Sandstones).|||Includes Wyandra Sandstone Member.|Overlies Hooray, Algebuckina and Murta Sandstones. Is overlain by Neales River and Rolling Downs Groups.|Marine sandstone.|
3284|Cadna-owie Formation|66623|3|Fully described|p102, pp238-245, pp250-255. |Early Cretaceous|Early Cretaceous|Preferential weathering of the dominant calcareous and fine-grained lithologies results in largely sandstone outcrops. Thickness varies to 260 m but this may include Murta Formation. Contains a wide range of fossils. Deposited in a variety of environments. Hosts glacial dropstones. Equivalent to top of Gum Vale Beds and lower Wittabrenna Beds, and to Pelican Well and Bungil Formations.||In SA, unit in Neales River Group.|Includes Wyandra Sandstone Member.|Overlies Namur Sandstone and Murta Formation; locally incised into Algebuckina Sandstone. Is disconformably overlain by Doncaster Membr (Wallumbilla Formation). Is overlain by Marree Formation in SA.|Erosion-resistant calcareous sandstone and siltstone; subordinate weathered grey shale and siltstone; minor pebbly sandstone and conglomerate.|11-NOV-13
3284|Cadna-owie Formation|66915|5|Briefly described|p4-6, p9, p11 Fig.7|Cretaceous|Cretaceous|Eromanga Basin. The "C-Horizon" is often referred to as "top Cadna-owie Formation". A readjustment of terminology is required, therefore it is better to understand the "C-Horizon" to represent "Base Wallumbilla" rather than "top Cadna-owie", or "top Bungil" or "top Gilbert River" or top whatever other unit underlies the Wallumbilla Formation in that area. See also Wallumbilla Formation.|||Wyandra Sandstone Member at top|Is overlain by Wallumbilla Formation.||12-JAN-17
3284|Cadna-owie Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous rocks are mapped separately.|||Includes Wyandra Sandstone.||Marine, calcareous sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; ferruginous calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous|Includes three un-named but separately mapped sub-units.|||Includes Wyandra Sandstone.||Marine, calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|18-NOV-14
3284|Cadna-owie Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; local pebbly sandstone and conglomerate interbeds and ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.|Overlies Namur Sandstone. Is overlain by Doncaster Member of Rolling Downs Group.|Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67323|5|Briefly described|p87, p93 Fig.12.3, p95|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Wallumbilla Formation.||
3284|Cadna-owie Formation|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1, p106|Aptian|Valanginian|Eromanga Basin. Deposited in a paralic or shallow marine environment. Maximum thickness of 10m. See also  p108 fig ERO4, p108-p110, p111 fig ERO8, p113 fig ERO12, p114 fig ERO13, p115.|||Includes the Wyandra Sandstone Member.|Overlies the Lower Cadna-owie Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.|Upwards coarsening sequence of interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|67784|5|Briefly described|p25-26|Aptian|Neocomian|Northern Eromanga Basin.||||Is overlain by Doncaster Member (Wallumbilla Formation).|Sandstone|08-FEB-18
3284|Cadna-owie Formation|68068|6|Mentioned|Map legend|||Time equivalent to the Parabarana Sandstone to the south.||||||18-NOV-14
3284|Cadna-owie Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Jurassic|Fluvial to marginal marine deposits. Mapped with Algebuckina Sandstone as one unit.|||||Sandstone.|
3284|Cadna-owie Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.|Includes the Trinity Well Sandstone Member.|||
3284|Cadna-owie Formation|68715|6|Mentioned|p30 Fig.5|Barremian|Valanginian|Eromanga Basin.||||||
3284|Cadna-owie Formation|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (SW and NE). Fluvial to shallow marine. Pre-Barremian age.||||||16-JAN-17
3284|Cadna-owie Formation|68821|5|Briefly described|p292 Fig.1, p295, p297 Fig.3|Cretaceous|Cretaceous|Eromanga Basin. Lower Cretaceous age. Fluvial-paralic. Equivalent to the Bungil Formation. Contains diamictite deposits at its base.|||||Comprises quartz rich sandstones and conglomerates.|
3284|Cadna-owie Formation|69001|5|Briefly described|p2 Fig.1B, p11, pp16-18, pp35-37, p63|Early Cretaceous|Early Cretaceous|Terrestrial to marine transition sediments. Of the Eromanga Basin. Calcite induration is common (but not diagnostic) in parts of weathered Cadna-owie Formation. Includes locally defined units by McMinn (1981b) and/or Morton (1982) such as the Gum Vale Beds or Gum Vale Formation.||||Equivalent to the Algebuckina Sandstone and the Gum Vale Beds.|Comprises sandstones, siltstones, and some conglomerate.|
3284|Cadna-owie Formation|69019|3|Fully described|p56-57 Pl.9, p85, p87-91, p168.|Aptian|Valanginian|Eromanga Basin. Of Freytag et al. (1967) and Wopfner et al. (1970); formerly 'Transition Beds' of Whitehouse (1955). Type section in ~3 km WSW of Algebuckina Hill. Often associated with ferricrete capping. A significant regional aquifer.||Unit in Neales River Group.|Includes Mount Anna Sandstone Member, Livingston Tillite Member and Trinity Well Sandstone Member.|Overlies Murta Formation and Algebuckina Sandstone; Bunyeroo Formation unconformably. Is equivalent to Parabarana Sandstone. Is overlain by Bulldog Shale gradationally and by Wallumbilla Formation.|Grey siltstone coarsening upwards into fine- to medium-grained sandstone; sandstone interbeds commonly calcitic; near basal siltstone commonly carbonaceous; locally a basal pebbly interval; contains exotic lonestones to 1 m.|
3284|Cadna-owie Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p90, p92-95|Aptian|Valanginian|See also p99, p101, p191-192. Freytag et al. (1967) and Wopfner et al. (1970); previously the Transition Beds of Whitehouse (1955). Contrasts with Parabarana Sandstone are discussed. Thickness to c.69m. Stratigraphic wells intersection data.||||Overlies Murta Formation. Is overlain conformably by Bulldog Shale (Marree Subgroup).|Contains fossil ice-wedges.|
3284|Cadna-owie Formation|69203|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69454|5|Briefly described|p38:3, 13, 14 Fig.38.9|Cretaceous|Cretaceous|Eromanga Basin. Potential hydrocarbon trap, either by sealing Algebuckina Sandstone reservoirs or by having its own sandstone reservoirs sealed by the Wallumbilla Formation shales.||||||12-JUL-16
3284|Cadna-owie Formation|69457|3|Fully described|p41:2-3, 5-9, 16|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970). Equivalent to the Transition beds of Whitehouse (1955). Eromanga Basin. Lacustrine to restricted/marginal marine, minor fluviatile and subtidal shallow marine deposits. 81m thick (>100m in Cooper Basin). Possibly equivalent to the upper part of De Souza Sandstone. Late Valanginian to early Aptian age from dinocysts and acritarchs. Hydrocarbon source potential is briefly discussed. May form a seal for underlying Algebuckina Sandstone reservoirs, and its own shoreline sandstone reservoirs in the NT may be sealed by the Wallumbilla Formation.|||Includes Mount Anna, Trinity Well, Wyandra, Sandstone Members.|Conformably overlies Algebuckina and Hooray Sandstones and Murta Formation. Is overlain conformably by Bulldog Shale and Wallumbilla Formation. Lateral equivalent of Wallumbilla Formation.|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone; minor claystone. Parallel bedding and coarsening-upwards intervals typical. Local pebble layers, diamictites and coarse breccia layers.|23-JAN-19
3284|Cadna-owie Formation|69554|6|Mentioned|p131|Cretaceous|Cretaceous|Northern Gawler Craton.||||||
3284|Cadna-owie Formation|69562|6|Mentioned|p666 Fig.3, p667 Fig.4, p668|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69568|6|Mentioned|p443|Cretaceous|Cretaceous|Lake Frome region, Eromanga Basin. A transitional depositional environment from terrestrial to marine.|||||Fine-grained, pale grey siltstone and sandstone with minor carbonaceous claystone intervals.|
3284|Cadna-owie Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|69594|4|Described|p519, p526-528, p532-533, p538, p573|Barremian|Valanginian|Wopfner et al. (1970). Eromanga Basin. Subsurface. 60-90m thick. Paralic to shallow-marine deposits. Is a minor hydrocarbon reservoir. An important, shallow aquifer.|||Wyandra Sandstone Member.|Overlies Murta Formation and Hooray Sandstone transitionally. Is overlain by Doncaster Member (Wallumbilla Formation). Lateral equivalent to Bungil Formation.|Lower part consists of silty mudstone, siltstone and lithic to quartzose and sublabile sandstone with the proportion of sandstone increasing upwards; the upper part is mainly sublabile to lithic sandstone with minor siltstone near the top.|
3284|Cadna-owie Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
3284|Cadna-owie Formation|69673|5|Briefly described|p154, p155 fig 127, p159, p161 fig 131|Cretaceous|Cretaceous|Age derived from Palynoflora. Some source potential for oil and gas.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member, Murta Member|Overlies Murta Formation, Algebuckina Sandstone, overlain by Wallumbilla Formation|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone, minor claystone typically with parallel bedding and upwards coarsening intervals.|
3284|Cadna-owie Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
3284|Cadna-owie Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.|||Includes Wyandra Sandstone Member.|||23-JAN-19
3284|Cadna-owie Formation|69946|2|Defined|p17, p19-20, p44, p56-58, p94, p96-98|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970), for the mappable interval between Algebuckina Sandstone and Bulldog Shale. Previously the Transition beds of Whitehouse (1955), for a unit that records the transition from terrestrial to marine conditions. Eromanga Basin. Type section is Big Cadna-owie Spring, 5.5km SSW of Mount Dutton. Upper boundary is strongly diachronous, younging towards the Basin margin. Typically 10-20m thick, to a maximum of >115m. Includes marine and non-marine fossils. Wireline log correlations. Lateral equivalent of Village Well and Pelican Well Formations and Parabarana Sandstone.|||Includes Wyandra, Mount Anna and Trinity Well, Sandstone Members.|Overlies Murta Formation gradationally and Algebuckina Sandstone. Is overlain conformably by Bulldog Shale or Wallumbilla Formation. See Comments.|Subsurface: pale grey siltstone with very fine- to fine-grained sandstone interbeds and minor carbonaceous claystone; pebbly layers, diamictites and coarse breccia layers around the Basin margin. Outcrop: minor calcareous sandstone beds with ooids.|
3284|Cadna-owie Formation|69947|5|Briefly described|p8-9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin. Marks transition from terrestrial to marine deposition.|||Wyandra Sandstone Member.|Conformably overlies Murta Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Mudstone, siltstone, sandstone.|
3284|Cadna-owie Formation|69948|6|Mentioned|p4; Figs.4.1-2, 13-20|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin). Seismic sections across the Gidgealpa, Dullingari, Poolowanna and Big Lake Fields, and other structures.||||Overlies Murta Formation or Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Fine-grained sandstone with coarse-grained sandstone beds and pale grey siltstone; minor conglomerate.|
3284|Cadna-owie Formation|70383|5|Briefly described|p45, p52|Early Cretaceous|Berriasian|Transgressive, marginal marine deposits. Maximum age from age of Sprigg Diamictite Member.|||Includes Sprigg Diamictite Member, Livingston Tillite Member.|Overlies Algebuckina Sandstone. Equivalent to Parabarana Sandstone.||15-JAN-19
3284|Cadna-owie Formation|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin. This unit is the distal Basin-wide equivalent to the rangelands-proximal Parabarana Sandstone. Age shown more specifically as Neocomian to Aptian.||Of Neales River Group.|Includes Livingston Tillite, Sprigg Diamictite, Trinity Well Sandstone, Members.|Equivalent to Parabarana Sandstone.|Mostly subsurface: yellow-brown, fine-grained, calcitic quartz sandstone; coarse-grained buff-yellow gritstone lenses; lower zone more silty, grey, carbonaceous. Sandy beds usually ferruginous, locally gravelly or bouldery.|23-JAN-19
3284|Cadna-owie Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit, Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone. Un-named unit is ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.|||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone.|
3284|Cadna-owie Formation|70789|5|Briefly described|p318, p320 Fig.4, p328|Early Cretaceous|Early Cretaceous|Eromanga Basin. Transgressive, fluvial to marginal marine deposits. Consistent thickness of 50-80m. A major aquifer in the Basin.||||Is overlain by Bulldog Shale.|Sandstones and siltstones.|
3284|Cadna-owie Formation|70821|4|Described|p21-22, p32-33, p72, p80, p82, p86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Poorly expressed or unrecognised in the southern Thomson region. Late Valanginian-Early Aptian acritarchs and dinoflagellates indicate fresh to brackish water, lacustrine to restricted, marginal marine environments. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrostratigraphic properties.|||Includes Wyandra Sandstone Member.|Overlies Algebuckina, Namur, Hooray (unconformably), Mooga Sandstones and Crowl Creek Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Fairly well-bedded siltstone, fine to medium lithic sandstone and intraformational conglomerate; thin coaly layers, dark mudstone and layers of kaolin-like material, possibly altered tuff are also present. Volcanogenic components increase up-section.|23-JAN-19
3284|Cadna-owie Formation|70823|5|Briefly described|p41, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also Cadnowie Formation [which is a mis-spelling of this formation]. Age is a minimum depositional age.|c. 126 Ma|||Overlies the Murta Formation. Overlain by the Wallumbilla Formation and the Bulldog Shale.||
3284|Cadna-owie Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Murta Formation and the Hooray and Namur Sandstones. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.|Mount Anna Sandstone Member.|||
3284|Cadna-owie Formation|71043|5|Briefly described|p106|||Gawler Craton.|||||Shale, minor sandstone.|
3284|Cadna-owie Formation|71251|5|Briefly described|p7-8, p11, p15, p17, p19-20, p29, p49|||Eromanga Basin. 65m total thickness in Eulo 1 borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity diagrams.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone or (where that unit is absent) Nebine Metamorphics. Is overlain by Wallumbilla Formation.|Fine quartzose sandstone, and dark grey mudstone with carbonaceous flecks; basal conglomerate composed of quartz and basement lithic fragments.|
3284|Cadna-owie Formation|71321|4|Described|p1,15,24-28,65|Early Aptian|Valanginian|Of Eromanga Basin. Deposited under shallow-water, marginal marine conditions. Marks the onset of Early Cretaceous marine transgression (Alexander, et al., 2006; Krieg, et al., 1995; Wopfner, et al., 1970) i.e. westward transgression of a marine epicontinental seaway (Keireg et al., 1995). Paleontological data indicate Valanginian to early Aptian age (Krieg, et al., 1995). Traditionally difficult to differentiate Cadna-owie Formation from the underlying Algebuckina Formation in the TIEYON area, and included as part of Algebuckina Formation in the TIEYON area.||||Conformably underlain by Algebuckina Sandstone. Underlain by the Murta Formation.|Outcrop: Fine- to medium-grained, quartzose sandstones, minor mica, feldspar, heavy minerals, pyrite; glauconite, calcareous beds with ooids. Subsurface: pale grey siltstone with fine-grained sandstone interbeds and minor carbonaceous claystones.|24-OCT-19
3284|Cadna-owie Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p4, Ch4 p8-p9|Aptian|Valanginian|Eromanga Basin. This unit was first named the Transition beds by Whitehouse (1955) as it records the transition from terrestrial to marine conditions. This name was first assigned by Wopfner et al (1970) to the mappable interval between the Algebuckina Sandstone and the Bulldog Shale. This units type section is located at Big Cadna-owie Spring and was defined by Wopfner et al., 1970. Hosts a major confined aquifer. Petrography is discussed. This unit is typically 10-20m thick around the basin margin, increasing to 75-100m in the deeper parts of the basin and reaches a maximum thickness in excess of 115m in the Nappamerri Trough. Age based on palynology. This unit is interpreted to have been deposited in shoreface and beach environments and members have been interpreted to have been deposited in fluviodeltaic environments. Sedimentary characteristics are discussed. Spore-pollen zone is given in Ch5 p57. Thermal history briefly described in Ch9.. Laterally equivalent to the Pelican Well Formation and the Parabarana Sandstone.See also Ch4 p20-p27, Ch5 p12, Ch5 p19-p21, Ch5 p24, Ch5 p30, Ch5 p32, Ch5 p38, Ch5 p56-p58, Ch5 p97-p99, Ch6 p7-p8, Ch7 p8-p9, Ch7 p11, Ch7 p13, Ch8 p6, Ch8 p10, Ch8 p23-p24, Ch9 p7, Ch9 p12, Ch9 p18, Ch9 p21, Ch9 p23, Ch10 tbl 10.1, Ch10 p8, Ch10 p17-p20, Ch11 p2, Ch11 p4-p5, Ch12 p12-p14, Ch13 p2, Ch13 p4, Ch13 p8-p9, Ch14 p5.|||Includes the Wyandra Sandstone Member, Mount Anna Sandstone Member, Trinity Well Sandstone Member and the Livingston Tillite Member.|Conformably overlies the Murta Formation. Unconformably overlies the Mount Toondina Formation. Overlies the Algebuckina Sandstone. Overlain by the Bulldog Shale and the Wallumbilla Formation.|Pale grey siltstone with very fine to fine-grained sandstone interbeds and minor carbonaceous claystone. Pebbly layers, diamictites and coarse breccia also occurs.|
3284|Cadna-owie Formation|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3284|Cadna-owie Formation|71415|5|Briefly described|p11-14|Valanginian|Valanginian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Terrestrial to marine transition sediments (Exon and Senior 1976). LA-ICPMS zircon age populations dominated by Neoproterozoic to Cambrian c. 600 to 316 Ma, and subordiante Mesoproterozoic c. 1300-250 Ma.||||Overlain by Rolling Downs Group. Underlain by Namur Sandstone.||19-AUG-19
3284|Cadna-owie Formation|71863|5|Briefly described|p5|Aptian|Valanginian|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlies the Murta Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|71864|6|Mentioned|p14, p17||||||Includes the Wyandra Sandstone Member.|||
3284|Cadna-owie Formation|72297|6|Mentioned|p742|||Eromanga Basin. Petroleum reservoir.||||||
3284|Cadna-owie Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Upper part: main confined aquifers, generally producing flowing artesian water bores.||Neales River Group.|Wyandra Sandstone Member.|Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla FZ.||
3284|Cadna-owie Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
3284|Cadna-owie Formation|72478|5|Briefly described|p6, p8-p10, p12, p25-26,|Early Cretaceous|Early Cretaceous|Eromanga Basin. Represents a marine transgressive phase. See also p51, Fig.7 p70, p72-74, p82-83 [of the document], where described as Cadnaowie sandstone, Cadnaowie sands, Cadnaowie Formation.|c. 130-114 Ma|||Underlies the Bulldog Shale. Unconformably overlies the Algebuckina Sandstone.|Grey sandstone, fine to very-fine sandstone with locally developed coarse sandstone interbeds and carbonaceous claystones.|29-MAR-21
3284|Cadna-owie Formation|72915|6|Mentioned|p27||||||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|72921|6|Mentioned|p16.|||Interpreted as correlative with a variety of units across the Clarence-Moreton, Surat and Eromanga Basins. [All the other units named are Jurassic, and most don't correlate with each other so there is some confusion about the intended meaning here]||||||
3284|Cadna-owie Formation|73090|5|Briefly described|Appendix.|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Marree Subgroup.||Overlies Algebuckina Sandstone conformably and Mount Toondina Formation unconformably.|Ferruginised or kaolinised gritty quartz sandstone; fossil wood.|
3284|Cadna-owie Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|73203|6|Mentioned|p651-652|Early Cretaceous|Early Cretaceous|[Also misspelt as Cadna-Owie Formation]. A major aquifer host across the Great Artesian Basin. Found in the Jundah 1 well, central Queensland.||||||
3284|Cadna-owie Formation|73249|4|Described|p316-319, p320 Fig.2, p321-338|Barremian|Valanginian|Eromanga Basin. Minimum age of early Barremian. Depositional environments transition from continental (fluvio-deltaic to tidal) to shallow marine, period of marine transgression. Typically 60m thick, can be 10m thick at basin margins and up to 115m thick in the Nappamerri Trough. Dominant mineral phases are kaolinite and quartz, montmorillonite is also present. Deposited in a cold continental, humid climate. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks from the west and south. [Locations in text include p321 Tb.1 and p324 Fig.4.]|||Mount Anna Sandstone Member|Conformably underlies the Bulldog Shale.|Siltstone with interbedded sandstone and mudstone, sandstone dominated with lesser clay-rich horizons, typically 60m thick.|
3284|Cadna-owie Formation|73251|5|Briefly described|p:36-37, 40, 43, 48-50, 52-54, 56-57, 62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Potential hydrocarbon reservoir and fairway. Contains hydrocarbon accumulations to which the Murta Formation contributed. Non-marine to marginal marine depositional setting. Contains Bulldog [organic] facies 1 [see article].|||Wyandra Sandstone Member|Underlain by Murta Formation and Namur Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation. Equivalent to Parabarana Sandstone.||
3284|Cadna-owie Formation|73281|6|Mentioned|Appendix (DIP)|||Cadna-owie Formation reinterpreted as Cadna-Owie Formation [to indicate capitalisation of both components is considered preferable in this work?]. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
3284|Cadna-owie Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|Underlain by Namur Sandstone and Murta Member. Overlain by Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|73398|5|Briefly described|p1-5, 7-8, 10-11, 13, 16, 19, 21-30|Early Cretaceous|Early Cretaceous|Eromanga Basin. Overlying the Prominent Hill IOCG deposit, this unit contains up to c.5000 ppm Cu; the authors conclude this was due to transport/deposition of mineralised sediments from underlying mineralised rock. Continental fluvial environment. One of the largest confined aquifers in the Great Australian Basin. Geochemistry, weathering analysed in great detail.|140-125 Ma.|||Unconformably overlies Boorthanna Formation. Is overlain conformably by Bulldog Shale.|Interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|73479|5|Briefly described|p156 Fig.2, p159, p164 Fig.7, p165-166|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-shallow marine depositional environment. See also p175.|ca 140-126 Ma||Wyandra Sandstone Member|Overlies Namur Sandstone, Murta Member, underlies Wyandra Sandstone Member, Bulldog Shale||
3312|Calca Granite|22430|6|Mentioned|p2||Proterozoic|||||||
3312|Calca Granite|24197|5|Briefly described|p30, p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: ~1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
3312|Calca Granite|24358|5|Briefly described|p32|Mesoproterozoic|Mesoproterozoic|Geological region: Eucla Basin.||||||27-FEB-15
3312|Calca Granite|36624|6|Mentioned|p54|||||||||
3312|Calca Granite|42716|5|Briefly described|Map legend|Mesoproterozoic||||||||
3312|Calca Granite|42738|6|Mentioned|map legend|Mesoproterozoic||||||||
3312|Calca Granite|43049|5|Briefly described|p15|||Of Hiltaba Suite.||||||06-AUG-08
3312|Calca Granite|43052|5|Briefly described|Table 5.6|||of Hiltaba Suite||||||
3312|Calca Granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||
3312|Calca Granite|60496|5|Briefly described|p22 Fig. 1, p23|Mesoproterozoic|Mesoproterozoic|A high quality monumental/building stone.||||||
3312|Calca Granite|60707|5|Briefly described|p611||Mesoproterozoic|Of the Hiltaba Suite. Distinctive dark-pink to red, undeformed massive granite, predomiantly alkali feldspar and quartz.  Intrudes the Investigator Granite Gneiss.  Age: 1456+/-26ma (Rb-Sr, Webb et al 1982).  Geological Province: Gawler Craton.||||||10-MAR-05
3312|Calca Granite|62893|6|Mentioned|Map Legend, p16|Middle Proterozoic|Middle Proterozoic|||||||
3312|Calca Granite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: ~1583+/-11Ma. Geological Province: Gawler Craton (Nuyts Domain).||||||10-AUG-07
3312|Calca Granite|63866|5|Briefly described|p19|Calymmian|Calymmian|Coulta Domain, Gawler Craton. |1583 +/- 11 Ma (Fanning et al., 2007)|Hiltaba Suite||||
3312|Calca Granite|64769|6|Mentioned|p28|||Dimension stone mined from the Hiltaba Granite Suite. SA.||||||05-MAY-09
3312|Calca Granite|65376|5|Briefly described|p147, pp150-151.|||A monumental stone, extensively used a facing stone, notably for Parliament House, Canberra.|1583 +/- 10 Ma.|Unit in Hiltaba Suite.|||Red, coarse-grained granite; very fine-grained hematite scattered throughout the feldspars.|
3312|Calca Granite|65390|5|Briefly described|p26 Tb. 1|Calymmian|Calymmian|Of Hiltaba Suite. Distinctive, red, coarse-grained granite; abundant, very fine-grained hematite. Aged 1456 +/- 26 Ma (Rb-Sr: Webb et al.,1986).||||||
3312|Calca Granite|66302|6|Mentioned|p46||||1583 +/- 10 Ma (SHRIMP, Fanning 2007)|Hiltaba Suite||||
3312|Calca Granite|68131|5|Briefly described|p71-72, p74|Mesoproterozoic|Mesoproterozoic|Flinders Island, Nuyts Domain, Gawler Craton. Intrudes basement. Is hosted by granodiorite gneiss and granite.|1584 +/- 10 Ma (Fanning et al., 2006).|Hiltaba Suite.||||
3312|Calca Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Gawler Craton, southwest. [Tyringa?].|1584 +/- 10 Ma|||||24-DEC-21
3313|Calcutteroo kimberlite|41402|5|Briefly described|p41|||||||||
3322|Calivil Formation|2967|4|Described|p14, p15 Fig.2.2, p17-20, 22-23, 26-37|Pliocene|Miocene|Macumber (1973). Eastern Murray Basin. The type section is from 77m to 95m in the Mines Department Calivil No. 2 bore. Locally, these sediments occupy valleys incised into Renmark Group units. A main regional aquifer (semi-confined). Misprinted as Cavil Formation twice on p110. Hydrochemistry (""salinity"") detailed. See also p40-41, 43, 45-46, 77-88, 90-91, 93-97, 101-102, 105, 108-113, 117, 128, 132, 135, 137, 139-152, 155, 178, 181, 336-337.||Wunghnu Group.||Is separated from the underlying Olney Formation (Renmark Group) by the Mologa Surface. Is overlain by Shepparton Formation, Parilla Sand and Yando Clay.|Valley-fill, fluviatile coarse-grained quartz gravel, pebbles.|
3322|Calivil Formation|10010|5|Briefly described|p12 Fig. 3, p17|Early Pliocene|Late Miocene|Of Wunghnu Group. Overlies upper part of Renmark Group. Grades upwards into Shepparton and Coonambidgal Formations. Geological Province: Murray Basin. Considered to be fluvial counterpart of Loxton-Parilla Sands.||||||13-AUG-07
3322|Calivil Formation|22756|3|Fully described|P13, P31||Tertiary|||||||
3322|Calivil Formation|22773|5|Briefly described|Fig24.8p352,354|||||||||
3322|Calivil Formation|22782|6|Mentioned|p15|||||||||
3322|Calivil Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Early Pliocene|Of the Wunghnu Group. A porous fluvio-lacustrine unit that is an important basin-wide aquifer. At the margins of the basin this unit contains conglomerate as well as sands. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|22886|5|Briefly described|p36|Early Pliocene|Late Miocene|||||||
3322|Calivil Formation|22887|2|Defined|p34, Fig.6 p13|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22893|3|Fully described|p29 fig9 table3|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22971|4|Described|p26, p27|||Max. thickness: <25m. Geological Province: Murray Basin.||||||19-JAN-06
3322|Calivil Formation|23089|5|Briefly described|p649|||||||||
3322|Calivil Formation|23164|4|Described|p15|Oligocene|Eocene|||||||
3322|Calivil Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
3322|Calivil Formation|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23305|4|Described|p52|||Of Macumber (1972). Overlain by Newer Volcanics. Geological Province: Lachlan Fold Belt. Max. thickness: 4 m.||||||09-OCT-08
3322|Calivil Formation|23884|5|Briefly described|p153, p155 Fig.13.2|||Geological Province: Murray Basin. Of the Wunghnu Group.||||||28-APR-05
3322|Calivil Formation|23921|4|Described|p1109, p1114|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
3322|Calivil Formation|24043|5|Briefly described|p525|Pliocene|Pliocene|||||||
3322|Calivil Formation|24103|5|Briefly described|p139 Fig.3, p143 Fig.6|Tertiary|Tertiary|Middle Tertiary.||||||
3322|Calivil Formation|24105|5|Briefly described|p155|Miocene|Miocene|||||||
3322|Calivil Formation|24106|5|Briefly described|p185|Pliocene|Late Miocene|||||||
3322|Calivil Formation|24107|6|Mentioned|p224|||||||||
3322|Calivil Formation|24108|5|Briefly described|p242|Pliocene|Late Miocene|Geological Province: Murray Basin. Overlying Unit: Shepparton Formation.||||||
3322|Calivil Formation|24177|3|Fully described|p71|Late Miocene|Late Eocene|Interfingers with Parilla Sand. Overlies the Renmark Group. Overlain by the Newer Volcanics and Shepparton Volcanics. Interpretation of age varies. Geological Province: Murray Basin.||||||
3322|Calivil Formation|24219|5|Briefly described|p870|||||||||
3322|Calivil Formation|24232|5|Briefly described|p227, p231|Tertiary|Tertiary|||||||
3322|Calivil Formation|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24383|4|Described|p10, 18|Pliocene|Oligocene|Age: 40 - 5Ma. Overlying Unit: Newer Volcanic Group. Underlying Unit: Castlemaine Group. Underlain by  White Hills Gravel, which provided source material for Calivil Formation. Geological Province: Lachlan Fold Belt||||||07-JUL-20
3322|Calivil Formation|24384|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24385|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24386|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate||||||
3322|Calivil Formation|24387|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24388|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate; nonmagnetic.||||||
3322|Calivil Formation|24439|5|Briefly described|p8, p23|||See also p9 Fig. 3. Author disputes presence of this unit in BENDIGO as defined by Macumber (1991) - see p. 37.  Fluvial deposits.||||||14-SEP-05
3322|Calivil Formation|24440|5|Briefly described|Map legend|||||||||
3322|Calivil Formation|24551|5|Briefly described|p322, 321, 421, 543|||Of the Murray Group.  Max thickness: 50m.||||||
3322|Calivil Formation|31713|6|Mentioned|p16|||||||||
3322|Calivil Formation|31746|6|Mentioned|p197|||In reference to Macumber (1972).||||||25-JUN-13
3322|Calivil Formation|31951|3|Fully described|p7|||||||||
3322|Calivil Formation|31953|6|Mentioned|p9|||||||||
3322|Calivil Formation|32232|6|Mentioned|p19|||||||||
3322|Calivil Formation|34735|6|Mentioned|p30|||||||||
3322|Calivil Formation|34757|6|Mentioned|p45|||||||||
3322|Calivil Formation|34813|5|Briefly described|p63|||Also mentioned on P62||||||
3322|Calivil Formation|35091|4|Described|p8|||Also p29.||||||07-JUL-20
3322|Calivil Formation|35172|4|Described|p127|||||||||
3322|Calivil Formation|35187|6|Mentioned|Table1|||||||||
3322|Calivil Formation|35242|6|Mentioned|p94|||||||||
3322|Calivil Formation|39329|6|Mentioned|p483|||||||||
3322|Calivil Formation|39330|6|Mentioned|p487|||||||||
3322|Calivil Formation|39446|6|Mentioned|p49|||||||||
3322|Calivil Formation|39967|6|Mentioned|p41|||||||||
3322|Calivil Formation|40520|6|Mentioned|Fig.5|||||||||
3322|Calivil Formation|40599|5|Briefly described|p19|||||||||
3322|Calivil Formation|40664|6|Mentioned|p248|||||||||
3322|Calivil Formation|40820|6|Mentioned|Fig.4|||||||||
3322|Calivil Formation|41068|5|Briefly described|p67|||||||||
3322|Calivil Formation|41765|4|Described|p36|||||||||
3322|Calivil Formation|41868|5|Briefly described|p551|||||||||
3322|Calivil Formation|42125|5|Briefly described|p137|||See also Fig.5||||||
3322|Calivil Formation|42126|6|Mentioned|p149,p151|||||||||
3322|Calivil Formation|42130|6|Mentioned|Fig.3 P265|||||||||
3322|Calivil Formation|42133|6|Mentioned|p302|||||||||
3322|Calivil Formation|42134|4|Described|p339|||||||||
3322|Calivil Formation|42137|6|Mentioned|p370|||||||||
3322|Calivil Formation|42138|6|Mentioned|p392|||||||||
3322|Calivil Formation|42454|4|Described|p11|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42455|5|Briefly described|Map legend|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42509|6|Mentioned|p4|||||||||
3322|Calivil Formation|42827|6|Mentioned|p271|||refers to Macumber (1972)||||||
3322|Calivil Formation|42881|4|Described|Fig.3, P84|||||||||
3322|Calivil Formation|42966|2|Defined|p179|Pliocene|Late Miocene|Of the Wunghnu Group.||||||09-OCT-08
3322|Calivil Formation|43198|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43199|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43211|4|Described|p4,Fig.5 p15,27-8|Oligocene|Eocene|||||||
3322|Calivil Formation|43260|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
3322|Calivil Formation|43261|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43493|4|Described|32|Oligocene|Eocene|||||||
3322|Calivil Formation|43601|6|Mentioned|p224||Early Pliocene|||||||
3322|Calivil Formation|43655|5|Briefly described|p40-846|||||||||
3322|Calivil Formation|43780|6|Mentioned|p6|||||||||
3322|Calivil Formation|43791|6|Mentioned|p372, Fig1|||||||||
3322|Calivil Formation|43804|6|Mentioned|Fig.2,p49|||||||||
3322|Calivil Formation|43846|5|Briefly described|14||Oligocene|||||||
3322|Calivil Formation|44188|5|Briefly described|Map Legend|Pliocene|Pliocene|Geological province: Murray Basin. Fluvial deposits- poorly consolidated pale grey, poorly sorted coarse to granular quartz sand, conglomerate with white kaolinitic matrix.||||||25-JUN-13
3322|Calivil Formation|44931|5|Briefly described|Map Legend|Tertiary|Tertiary|Alluvial clay and sand, and minor gravel.||||||14-JUN-06
3322|Calivil Formation|49038|4|Described|Table 2|||Briefly described p26||||||07-JUL-20
3322|Calivil Formation|49040|6|Mentioned|p12|||||||||
3322|Calivil Formation|50154|5|Briefly described|p133|Pliocene|Late Miocene|Overlies the Renmark Group. Geological Province: Murray Group.||||||
3322|Calivil Formation|60451|4|Described|p30, 95 Fig. 61, 98, 253|Pliocene|Eocene|Age: 40-6Ma, but not directly dated.  Palynology indicates max age. Overlain by Miocene-Pliocene units. Interfingers with the Renmark, Murray and Wunghnu Groups. Underlies: Parilla Sand, Shepparton Formation, Newer Volcanics.||||||24-JUN-14
3322|Calivil Formation|60452|4|Described|p35|Cenozoic|Cenozoic|First named by Macumber (1973), then called Calivil Sand (Lawrence, 1975) but reverted to original name of Calivil Formation (Tickell & Humphreys, 1980). Overlies Castlemaine Group, diconformably overlies Renmark Group. Overlain by Shepparton Formation.||||||19-NOV-08
3322|Calivil Formation|60454|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequences.||||||07-NOV-08
3322|Calivil Formation|60456|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence; poorly sorted gravel, sand and minor kaolinitic clay.||||||07-NOV-08
3322|Calivil Formation|60457|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads': often richly auriferous; poorly sorted gravel, sand and minor kaolinitic clay.||||||25-JUN-13
3322|Calivil Formation|60458|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads'.||||||07-NOV-08
3322|Calivil Formation|60459|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic alluvium now entirely buried beneath younger units.||||||07-NOV-08
3322|Calivil Formation|60461|5|Briefly described|Map legend|Miocene|Oligocene|Of the Murray Group.  River valley deposits - Powlett Plains deep lead and colluvium: interbedded clay, silty clay, silt and subangular to subrounded fine to coarse-grained quartz sand, reef quartz and metasediment gravel, minor ligneous clay.||||||28-SEP-04
3322|Calivil Formation|60462|5|Briefly described|Map Legend|Neogene|Neogene|Poorly sorted fine to coarse grained terrestrial sand: magnetic where ferruginised with responses to 20 nT; where cropping out thorium high.||||||15-SEP-04
3322|Calivil Formation|60491|4|Described|p16, p21|||Interfingers with the Parilla Sand. Consists of fluvial and fluviolacustrine quartzose sand and gravel.||||||
3322|Calivil Formation|60492|5|Briefly described|Map Legend|Miocene|Miocene|Alluvium: gravel, sand, silt, conglomerate.||||||
3322|Calivil Formation|60529|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||
3322|Calivil Formation|60581|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60582|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||23-NOV-04
3322|Calivil Formation|60583|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60584|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60585|4|Described|p28|Pliocene|Late Eocene|Disconformably overlain by the Moorabool Viaduct Sand. Consists of poorly to moderately sorted polymictic cobbles, pebbles, sand and clay that have been ferruginised or silicified.||||||
3322|Calivil Formation|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||25-NOV-04
3322|Calivil Formation|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Deep lead fluvial deposits: no distinctive magnetic responses.||||||
3322|Calivil Formation|60599|5|Briefly described|p15, p85|Late Eocene|Middle Miocene|Of the Wunghnu Group. Fluvial sediments. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|61160|5|Briefly described|p150|Pliocene|Miocene|Buried auriferous gravels or deep leads within this unit are present in valleys of the upper Ovens River and Morses Creek in BUFFALO. ||||||
3322|Calivil Formation|61163|6|Mentioned|p99|||Of Wunghnu Gp. Overlies Shepparton Fm. Poorly sorted gravels with abundance of sandstone clasts now fragile due to in-situ weathering; vein quartz clasts are subangular to subrounded. Economically important due to placer gold content. Geol Prov: LFB||||||05-JUL-07
3322|Calivil Formation|61174|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||07-FEB-11
3322|Calivil Formation|61175|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61176|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61177|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61185|2|Defined|p57-62, p15, p64|Pliocene|Late Miocene|Of Macumber (1973). Of Wunghnu Gp. Reworked White Hills Gravel and colluvial seds. Under Shepparton Fm and Newer Volcanics; disconf. over Renmark Gp; conform. over/interfingers with Parilla Sand. Subsurface in NAGAMBIE. See Calivil Sand. Auriferous.||||||07-FEB-11
3322|Calivil Formation|61701|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61702|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61703|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61822|6|Mentioned|p107|Neogene|Neogene|||||||
3322|Calivil Formation|61964|3|Fully described|p14 Fig. 4p141-143|Pliocene|Late Miocene|Of Murray Group? Fluvial gravels, sands and fine-grained sands  pale grey, poorly sorted medium- to coarse-grained quartz sand/sandstone with a white kaolinitic clay matrix. Unconformably overlies Olney Formation (Renmark Group). Geol. Prov: Murray Basin||||||09-OCT-08
3322|Calivil Formation|62370|5|Briefly described|p447, p452 Fig.4|Early Pliocene|Late Miocene|Fluvial deep-lead infill of sand and cobble conglomerate, and includes pallid clay and ferruginous clasts, recycled pebbles and locally eroded bedrock, in some areas has a magnetic ferricrete cap. Unconformably underlies Shepparton Formation.||||||
3322|Calivil Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix;interbedded siltstone and claystone; silicified and ferruginised duricrust common.||||||13-MAY-13
3322|Calivil Formation|64314|5|Briefly described|p498 Fig. 3, p502 Fig. 7|Late Miocene|Late Eocene|Of Macumber (1973). Thickness: ~30m. Use also in the compound name Yaloak/Calivill Formation. See also p500 Fig. 5, p501.||||||
3322|Calivil Formation|64568|5|Briefly described|Map legend|Silurian|Silurian|Geol.Prov: Murray Basin. [Note: map symbol suggests Tertiary age]. Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust is common.||||||24-JUN-14
3322|Calivil Formation|64612|6|Mentioned|p28|Cainozoic|Cainozoic|||||||07-FEB-11
3322|Calivil Formation|64823|5|Briefly described|p1011|||Paleochannel deposits. Geological province: Murray Basin.||||||
3322|Calivil Formation|65552|5|Briefly described|p2, p5 Fig.3, p6-8, p13, p15, p19|Early Pliocene|Late Miocene|See also p24 App.3, p26 App.5. Of Wanghnu Group, eastern Murray Basin. Medium to coarse grained quartz sand/sandstone with locally thick kaolin lenses. Overlies Olney Formation (Renmark Group), conformably underlies Shepparton and Coonambidgal Formations.||||||
3322|Calivil Formation|65715|5|Briefly described|p11 Tb.7, p11-12, 14, 16, 26, 27|Miocene|Miocene|Included in Wunghnu Group by Lawrence (1975). Correlated with older Murray Group by Holdgate and Gallagher (2003). Overlies Werribee Formation. Underlies Newer Volcanics. Younger than White Hills Gravel. Distribution modified see p14.||||||06-FEB-15
3322|Calivil Formation|65969|5|Briefly described|p27 Tb.3.3, p30-1|Miocene|Oligocene|Murray Basin. Erosional contact with underlying Olney Formation. Of Murray Group. Typically clay and silt interbedded with sand and gravel. Fines to the north of the BENDIGO 1:250 000 sheet. Occurs in paleotopographic lows and fills paleovalleys. Up to 70 m thick. Extensively worked for gold near Bendigo. Minor areas have magnetic responses to 15 nT; no distinctive radiometric response.||||||
3322|Calivil Formation|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Correlative of (obsolete) Loddon River Group. Previously included in Wunghnu Group (1975), but shown to correlate with Murray Group (Holdgate & Gallagher 2003). See also Macumber 1991.||||||15-MAY-13
3322|Calivil Formation|67179|6|Mentioned|p581|Pliocene|Miocene|Fluvial valley fill east of study area.||||Interfingers with the Loxton Sand (lateral equivalent).||
3322|Calivil Formation|68116|5|Briefly described|Appendix, Maps 22-24, 30-32, 40-41, 50.|Miocene|Oligocene||||||Conglomerate, sandstone, silt, clay: brown to pale colours; poorly sorted; clasts variably rounded; predominant vein quartz clasts; cross-bedding prominent.|
3322|Calivil Formation|68140|5|Briefly described|p1699|Pliocene|Pliocene|No outcrop. In hydraulic conductivity with the underlying Renmark Formation throughout much of the Riverine Province; they commonly form a single aquifer, and are referred to in this article as Calivil-Renmark Formation (see references p1698, p1699, p1702, pp1705-1708).||||Underlain by the Renmark Formation.|Sands.|09-FEB-18
3322|Calivil Formation|68189|5|Briefly described|p4, p26-29, p33|Miocene|Oligocene|River valley depositional environment. Upstream time equivalent of the younger part of the Olney Formation. Truncated by the Mologa Surface. Hosts alluvial Au won in ST ARNAUD in the near surface and where it forms deep leads.||||Nonconformably underlain by the White Hills Gravel.|Comprises mud, subangular to subrounded sand, reef quartz gravel.|
3322|Calivil Formation|68194|5|Briefly described|p9, p17, p21, p23, p25-26, p35-36, p40|Pliocene|Pliocene|See also p44, p55. Macumber (1972). Preserved on hills and rises, overlying weathered bedrock or Parilla Sand. Regolith and remote sensing profiles described. Age given as Eocene on p55.||Unit in Murray Group.||Lateral facies equivalent of Geera Clay.|Alluvial sands in paleovalleys, and gravels overlying bedrock highs.|
3322|Calivil Formation|68203|6|Mentioned|p11|Pliocene|Miocene|Deposition coincided with the first of two uplifts (~15-20m) of the Cadell Fault.||||||
3322|Calivil Formation|69162|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69164|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69798|6|Mentioned|p4 Fig.2|Pliocene|Pliocene|Murray Basin.||Wunghnu Group.||||
3322|Calivil Formation|70718|5|Briefly described|p17, p25|Cenozoic|Cenozoic|Is one of the primary aquifers in the Hay map sheet area. Misspellt as the Calival Formation on p25.||||Overlain by the Loxton Sand. Overlies the Upper Renmark Beds [Olney Formation]. Transitionally overlain by the Shepparton Formation.|Relatively coarse and poorly sorted fluvial sands and muddy overbank deposits.|30-MAY-19
3322|Calivil Formation|71419|5|Briefly described|p8 Fig 2, p14, p17-18.|Miocene|Miocene|Fluvial sediments derived from the Western Uplands. Source for later marine deposits i.e. Sandringham Sandstone.||||Overlain by Sandringham Sandstone.|Contains conglomerate consisting almost exclusively of vein quartz clasts.|02-FEB-18
3322|Calivil Formation|71593|5|Briefly described|p52, p54|||||Wunghu Group||||
3322|Calivil Formation|72445|5|Briefly described|App.1; App.2; App.7 p7-8, p7 Fig.4.|Pliocene|Miocene|Characterised by the organic-poor nature of the sands that are a major component of this formation. Said to be non-marine. App.2 is a .csv format file.  Identified in Stavely 05,07,11,12. Partially equivalent to Torrumbarry Clay, Bookpurnong beds/Formation.||Wunghnu Group ? Of Murray Group (App 2)||Underlies Woorinen Formation (gradational), Loxton Sand (sharp or gradational contact), Shepparton Formation. Overlies Olney, Bookpurnong Formations (sharp contacts).|Shown as including sand, gravel, lignite, mud and conglomerate.|
3322|Calivil Formation|73118|5|Briefly described|p81|Pliocene|Miocene|Extensive blanket underlies much of the Riverine Plain and N fringes of the Murray Basin. Deposited in valley-fill, alluvial-fan, fluviolacustrine and braided-channel environments.||Wunghnu Group.|||Poorly consolidated, pale grey, poorly sorted coarse to granular quartz sand, conglomerate, with white kaolinitic matrix; thick intercalations of carbonaceous clay.|
3322|Calivil Formation|73228|6|Mentioned|p56, p62|Pliocene|Late Miocene|Fluvial counterpart of the Loxton Sand.||||Underlain by upper Renmark Group.|Coarse and poorly sorted fluvial sands and muddy overbank deposits.|
3322|Calivil Formation|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
3322|Calivil Formation|73497|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Fluvial deposits: no distinctive magnetic or radiometric response.|
3322|Calivil Formation|73505|4|Described|p2, p11, p13, p36|Miocene|Late Eocene|Murray Basin. Nonmarine, occurs in palaeotopographic lows. Lateral equivalents interfinger with the Geera Clay. Minor areas where channels have magnetic responses to 15 nT.||Murray Group||Overlies Olney Formation with erosional contacts, onshore equivalent to Geera Clay, underlies Parilla Sand, Blanchetown Clay|Fluvial sand and mud, gravel, coarsening to the south.|
3330|Callabonna Clay|22887|6|Mentioned|p50|||Could represent the Pleistocene to Recent boundary (Firman, 1970)||||||
3330|Callabonna Clay|24176|6|Mentioned|p21|Quaternary|Quaternary|Possibly equivalent to Arrowie Formation.||||||
3330|Callabonna Clay|30056|6|Mentioned|Table 4|||||||||
3330|Callabonna Clay|30749|2|Defined|p2|late Pleistocene|late Pleistocene|||||||
3330|Callabonna Clay|30754|4|Described|p35|||See stratigraphic table on P22||||||
3330|Callabonna Clay|30758|6|Mentioned|p66|||Stratigraphy||||||
3330|Callabonna Clay|30804|6|Mentioned|p14|||See Table 1||||||
3330|Callabonna Clay|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|30921|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene to Recent||||||
3330|Callabonna Clay|30924|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene - Recent||||||
3330|Callabonna Clay|31699|6|Mentioned|p131|||Late Pleistocene||||||
3330|Callabonna Clay|31966|6|Mentioned|p6|||||||||
3330|Callabonna Clay|32432|6|Mentioned|Table 1|||||||||
3330|Callabonna Clay|33820|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|33821|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene - Recent||||||
3330|Callabonna Clay|33822|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|33823|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|33824|6|Mentioned|Table 2|||||||||
3330|Callabonna Clay|33825|6|Mentioned|p7|||Refers Firman (1970)||||||
3330|Callabonna Clay|33827|6|Mentioned|Table 1|||||||||
3330|Callabonna Clay|33828|6|Mentioned|Table 1|||||||||
3330|Callabonna Clay|35772|6|Mentioned|p13|||||||||
3330|Callabonna Clay|38068|6|Mentioned|p77|||||||||
3330|Callabonna Clay|38107|6|Mentioned|Table 1|||See also Table 4.||||||
3330|Callabonna Clay|38605|6|Mentioned|p41|||||||||
3330|Callabonna Clay|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3330|Callabonna Clay|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|40442|6|Mentioned|p38|||See also Fig.23.||||||
3330|Callabonna Clay|40910|6|Mentioned|p19|||||||||
3330|Callabonna Clay|40911|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3330|Callabonna Clay|40926|6|Mentioned|p30|||Mention Table 3||||||
3330|Callabonna Clay|41520|5|Briefly described|Fig.5|||||||||
3330|Callabonna Clay|41619|6|Mentioned|Map legend|Pleistocene||||||||
3330|Callabonna Clay|42721|6|Mentioned|map legend|Pleistocene||||||||
3330|Callabonna Clay|42723|6|Mentioned|map legend|Holocene|Pleistocene|||||||
3330|Callabonna Clay|42733|5|Briefly described|map legend|Quaternary||||||||
3330|Callabonna Clay|42966|4|Described|p214|||||||||
3330|Callabonna Clay|43094|6|Mentioned|p40|||||||||
3330|Callabonna Clay|44133|6|Mentioned|p242|||A thin deposit overlying the Pooraka Formation.||||||
3330|Callabonna Clay|65922|5|Briefly described|p25 Tb. 4|Quaternary|Quaternary|||||||
3330|Callabonna Clay|70337|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, red-brown, sandy, clayey sand.|
3338|Callanna Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
3338|Callanna Group|22510|5|Briefly described|table1 p37|||Age: Willouran- Torrensian||||||20-OCT-10
3338|Callanna Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
3338|Callanna Group|22589|6|Mentioned|p129,30|Cryogenian||||||||
3338|Callanna Group|22631|5|Briefly described|fig2 p170|Neoproterozoic|Neoproterozoic|||||||
3338|Callanna Group|22643|6|Mentioned|p190|||||||||
3338|Callanna Group|22677|6|Mentioned|Fig.2 p735||Neoproterozoic|||||||
3338|Callanna Group|22772|4|Described|p63,65,Table13.1|Cryogenian|Cryogenian|||||||
3338|Callanna Group|22857|5|Briefly described|Tb. 13.1 (insert p70-71), p63|Willouran|Willouran|Now included in the Warrina Supergroup.||||||
3338|Callanna Group|22889|6|Mentioned|p33|||||||||
3338|Callanna Group|22922|5|Briefly described|32|Neoproterozoic|Neoproterozoic|Age: Torrensian - Willouran||||||
3338|Callanna Group|22927|4|Described|41|||Geol province Adelaide Geosyncline. Max thickness 500 m. Overlying unit Bunyeroo Formation||||||
3338|Callanna Group|22947|6|Mentioned|p16|||Mentioned under - Adelaide Geosyncline Geodevelopments.||||||
3338|Callanna Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
3338|Callanna Group|23054|6|Mentioned|p10|||||||||
3338|Callanna Group|23177|6|Mentioned|p28|||||||||
3338|Callanna Group|23205|6|Mentioned|p133|||of Warrina Supergroup. Adelaide Geosyncline.||||||
3338|Callanna Group|23211|6|Mentioned|Fig.2|||||||||
3338|Callanna Group|23282|6|Mentioned|p53|||Contains stromatolites (A.australica) also in Coominaree Dolomite.||||||
3338|Callanna Group|23315|5|Briefly described|p344|||Includes a basal quartzite overlain by dolomitic marbles and evaporites as well as basalts, rhyolites and tuffs. Max. thickness 1.3km.||||||13-FEB-08
3338|Callanna Group|23351|5|Briefly described|283|||||||||
3338|Callanna Group|23478|5|Briefly described|p27|||||||||
3338|Callanna Group|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
3338|Callanna Group|23869|5|Briefly described|p15 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
3338|Callanna Group|24045|5|Briefly described|p554 Table 1|||Age: Willouran||||||
3338|Callanna Group|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin [?very unlikely]||||||20-OCT-10
3338|Callanna Group|24175|3|Fully described|p6, 7|Neoproterozoic|Neoproterozoic|Of Warrina Supergroup. Overlain by Burra Group. Max. thickness: 7000m.||||||20-FEB-07
3338|Callanna Group|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Curdimurka and Arkaroola Subgroups.||||||
3338|Callanna Group|24362|6|Mentioned|p41|||||||||
3338|Callanna Group|24506|6|Mentioned|p19 Fig. 5|Neoproterozoic|Neoproterozoic|||||||19-SEP-05
3338|Callanna Group|24586|5|Briefly described|p50, p51 Fig. 1, p52 Fig. 2|Adelaidean|Adelaidean|Of Warrina Supergroup. Includes the Curdimurka and Arkaroola Subgroups. Geological Province Adelaide Geosyncline.||||||13-FEB-08
3338|Callanna Group|31109|5|Briefly described|p10|||See also p12, 14, Map. Upper Proterozoic||||||17-SEP-18
3338|Callanna Group|36212|6|Mentioned|Fig.2|||||||||
3338|Callanna Group|37854|2|Defined|p8|Adelaidean|Adelaidean|Willouran||||||
3338|Callanna Group|37932|6|Mentioned|p539|||||||||
3338|Callanna Group|38004|6|Mentioned|p82|||||||||
3338|Callanna Group|38581|6|Mentioned|p252|||See also p266.||||||18-JAN-19
3338|Callanna Group|38704|6|Mentioned|p133|||||||||
3338|Callanna Group|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran to Sturtian.||||||18-JAN-19
3338|Callanna Group|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
3338|Callanna Group|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
3338|Callanna Group|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
3338|Callanna Group|39490|6|Mentioned|p10|||||||||
3338|Callanna Group|39635|6|Mentioned|Fig.2|||||||||
3338|Callanna Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3338|Callanna Group|39904|6|Mentioned|p9|||||||||
3338|Callanna Group|40225|3|Fully described|Map sheet|||||||||
3338|Callanna Group|40257|6|Mentioned|Fig.2|||||||||
3338|Callanna Group|40294|3|Fully described|p27|||||||||
3338|Callanna Group|41402|6|Mentioned|p42|||||||||
3338|Callanna Group|41403|6|Mentioned|p66|||||||||
3338|Callanna Group|41404|6|Mentioned|p73|||||||||
3338|Callanna Group|41405|6|Mentioned|p125|||||||||
3338|Callanna Group|41429|6|Mentioned|p230|||||||||
3338|Callanna Group|41496|5|Briefly described|Fig.1|||||||||
3338|Callanna Group|41526|6|Mentioned|p14|||||||||
3338|Callanna Group|42357|6|Mentioned|p8|||||||||
3338|Callanna Group|42546|5|Briefly described|Map legend|||||||||
3338|Callanna Group|42720|5|Briefly described|map legend|Marinoan||||||||
3338|Callanna Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
3338|Callanna Group|42813|4|Described|p14|||||||||
3338|Callanna Group|43052|4|Described|p172|||||||||
3338|Callanna Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Evaporitic clastics and carbonates.||||||26-MAY-05
3338|Callanna Group|43094|5|Briefly described|p33|||||||||
3338|Callanna Group|43190|6|Mentioned|p29|||Flinders Ranges||||||
3338|Callanna Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
3338|Callanna Group|43390|14|Not recorded|p8|||||||||
3338|Callanna Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
3338|Callanna Group|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
3338|Callanna Group|43845|5|Briefly described|Fig4 p44, 41,46||Neoproterozoic|||||||12-JUL-16
3338|Callanna Group|44133|5|Briefly described|p46, 51 Fig. 7.18, 52, 101|Adelaidian|Adelaidean|Brecciated siltstone, sandstone, dolomite, basalt, intrusive breccia.||||||17-SEP-18
3338|Callanna Group|60718|4|Described|p48, p49 Fig. 1, p50, 52|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Includes Curdimurka and Arkaroola Subgroups.|Unconformably underlies Umberatana Group.||15-APR-11
3338|Callanna Group|60889|5|Briefly described|p246|Neoproterozoic|Neoproterozoic|Source of more than 100 diapiric structures occuring in the Adelaide Geosyncline. This extensive diapirism influenced Lower Cambrian sedimentation. Age: middle Neoproterozoic.||||||
3338|Callanna Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Evaporitic clastics and carbonates.||||||
3338|Callanna Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Warrina Supergroup. Includes: Curdimurka Subgroup.||||||
3338|Callanna Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Includes Backy Point Formation. Evaporitic clastic and carbonate rock.||||||
3338|Callanna Group|61153|5|Briefly described|p344-345 Fig. 1|||Unconformably overlain by the Sturt Tillites; unconformably overlies the Gairdner Dyke Swarm. Geological Province: Adelaide Geosyncline.||||||25-JAN-06
3338|Callanna Group|61238|4|Described|p44 Fig. 1, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Includes felsic Oolda Wirra Volcanics. Siltstone, sandstone, ripple marks, halite casts, heavy mineral lamination, carbonates, evaporites.||||||14-MAY-07
3338|Callanna Group|61716|5|Briefly described|p642|||Geological Province: Adelaide Rift Complex.||||||10-MAY-06
3338|Callanna Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Willouran|Willouran|Includes the 802+/-10Ma Rook Tuff. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
3338|Callanna Group|62085|6|Mentioned|p19 Fig.4|Neoproterozoic|Neoproterozoic|Willouran.|||||Diapiric breccia, including sedimentary and mafic xenoclasts.|
3338|Callanna Group|62453|5|Briefly described|p11 Fig. 7, 12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||05-JUL-13
3338|Callanna Group|62592|5|Briefly described|p50 Table 5.1.|Willouran|Willouran|Adelaide Geosyncline.||Unit in Warrina Supergroup.|Includes Arkaroola and Curdimurka Subgroups.|Is unconformably overlain by Burra Group.||
3338|Callanna Group|62724|4|Described|p16, p17 Fig. 4|Willouran|Willouran|Includes the Arkaroola Subgroup. Geological Province: Broken Hill Domain/Curnamona Province, but absent in the Bimbowrie Inlier.||||||07-FEB-11
3338|Callanna Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Here represents undifferentiated rocks - diapirically emplaced brecciated sandstone, siltstone carbonate, basalt.||||||10-SEP-07
3338|Callanna Group|64319|5|Briefly described|p354-355; p356, 357 Figs.2,3; p362   |Cryogenian|Tonian|Most zinc mineralisation in the Flinders Ranges occurs where antiforms of this unit contact the Ajax Limestone. Other ages, also from volcanic rocks in the Group, include 827 +/- 6 Ma (Wingate et al., 1998) and 802 +/- 10 Ma (Fanning et al., 1986).|849 +/- 31 Ma (Cooper and Compston, 1971).|||Is overlain by Burra Group.|Heterogeneous assemblage of volcanic rocks and sabkha-related carbonates and evaporites.|
3338|Callanna Group|64647|5|Briefly described|p40|||Comprise immature and evaporite-bearing fine- to medium-grained clastics, mafic and minor felsic volcanics, and abundant carbonates.||||||05-JUL-13
3338|Callanna Group|64793|6|Mentioned|p284 fig 3, p285, p293, p295|||Age inferred from Fig.3.|c.840 - c.780 Ma.||Includes Arkaroola and Curdimurka Subgroups.|||
3338|Callanna Group|64794|6|Mentioned|p244|||||||||
3338|Callanna Group|64796|5|Briefly described|p183-203|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex. Generalised stratigraphic column on p. 190.||Warrina Supergroup|Includes Arkaroola and Curdimurka Subgroups.||Sedimentary rocks.|
3338|Callanna Group|64797|5|Briefly described|p151, p153 Fig.2, p158, p160 Fig.8|||See also p163-167, p168 Tb.11, p169 Fig.12, p172 Tb.13. Adelaide Rift Complex. S-isotope data.|||Includes Curdimurka Subgroup; Duff Creek beds, Coominaree Dolomite, Rockwater beds and War Loan beds.|||
3338|Callanna Group|64801|5|Briefly described|p110-113|Neoproterozoic|Neoproterozoic|Deposition in an early rift setting. Age from Rook Tuff (constituent).|802 +/- 10 Ma (Fanning et al., 1986).|Warrina Supergroup.|Include Rook Tuff.|Is overlain by Burra Group.|Redbeds and carbonates with evaporite affinities, casts and pseudomorphs of halite, gypsum and an array of soda minerals, and trachytic basalts.|18-JAN-19
3338|Callanna Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3|Cryogenian|Cryogenian|||||||
3338|Callanna Group|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
3338|Callanna Group|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf||||||
3338|Callanna Group|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Arkaroola and Curdimurka Subgroups.||||||19-MAR-12
3338|Callanna Group|65376|6|Mentioned|p229 Fig.6.39.|Neoproterozoic|Neoproterozoic|||||||
3338|Callanna Group|65379|5|Briefly described|p643|Neoproterozoic|Neoproterozoic|Parent of Curdimurka Subgroup. A major stratigraphic subdivision of the Adelaide Geosyncline. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
3338|Callanna Group|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic||||Includes Rook Tuff.|||
3338|Callanna Group|65493|6|Mentioned|p908, 909 Figs 1,2|Cryogenian|Cryogenian|Adelaidean units of the Flinders Ranges.||||||05-JUL-13
3338|Callanna Group|65892|6|Mentioned|p44. |Neoproterozoic|Neoproterozoic|Source of copper ore in Blinman mine.||||||
3338|Callanna Group|65925|5|Briefly described|p124 Fig.3, Appendix 2.||||||Includes Paralana Quartzite and Arkaroola Subgroup.||Siltstone, locally carbonaceous; sandstone, locally stromatolitic, ripple marks, halite casts, heavy mineral lamination; carbonates; evaporites; basalt, minor acid and intermediate volcanics.|
3338|Callanna Group|66464|5|Briefly described|p167, p168 Fig.2|Tonian|Tonian|Adelaide Rift Complex. Evaporites, siltstone, sandstone, carbonate, basalt, diapiric breccia.||||||
3338|Callanna Group|66518|6|Mentioned|p19 Fig.4.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably underlies Burra Group.||
3338|Callanna Group|66522|5|Briefly described|p20 Fig.2, p22.|Neoproterozoic|Neoproterozoic|Clasts occur in the Skillogalee Dolomite-dominated breccia of the Burra Diapir, suggesting it has been emplaced from below.|Lower Adelaidean.||||A friable crocidolitic siltstone clast in the Burra open cut is interpreted to originate from this unit.|
3338|Callanna Group|66884|4|Described|p36, p39 Fig.2, p43 Fig.4|Cryogenian|Cryogenian|Age: Willouran. Represents lowermost strata of Adelaide fold belt sedimentary sequence. Diapiric breccia (clasts cm to hundreds of m) are crosscut and intercalated by post-Callanna stratigraphy throughout Willouran and Flinders Ranges.|c. 850-800 Ma||Arkaroola Subgroup, Curdimurka Subgroup|Is overlain by Burra Group; unconformably overlies Archaean and Mesoproterozoic crystalline basement.|Assemblage of brecciated, siliciclastic, carbonate and mafic igneous to volcanic rocks that were originally interbedded with evaporites (now absent at surface).|18-JAN-19
3338|Callanna Group|67180|6|Mentioned|p601 Fig.1|Neoproterozoic|Neoproterozoic|||||Underlies Burra Group.||
3338|Callanna Group|67536|6|Mentioned|Map Legend||||||||Evaporitic clastics and carbonate rocks; fluvial sandstone and conglomerate.|
3338|Callanna Group|67870|4|Described|p5, p9, p13, p15, p17-18, p20-21, p23-26|Neoproterozoic|Neoproterozoic|See also p29-30, p32-34. Adelaide Rift System. c.500-c.750m thick. Highly reflective in seismic section, largely due to the Beda Volcanics. Raised over 3500m along the Yadlamalka (thrust) Fault.|||Arkaroola, Curdimurka Subgroups.|Overlies Pandurra Formation. Is overlain by Burra Group.|Sandstone, shale, siltstone, salt (anhydrite, halite, gypsum). Includes a number of volcanic units (basalt, rhyolite, tuff).|
3338|Callanna Group|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as Callanna/Burra Group equivalents, including Pindyin Sandstone||||Equivalent to Pindyin Sandstone|Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, dolomite, minor chert and quartzite.|
3338|Callanna Group|67979|5|Briefly described|p528, p530 Fig.1|Cryogenian|Neoproterozoic|Geol. Prov: Adelaide Geosyncline (as defined by Thomson et al. 1964 and subsequent revisions)|||Curdimurka Subgroup|is overlain by Burra Group||22-SEP-14
3338|Callanna Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
3338|Callanna Group|68068|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||Includes Arkaroola Subgroup.|||
3338|Callanna Group|68270|5|Briefly described|p683|Tonian|Tonian|Adelaide Rift Complex. Intruded by 802+\-10 Ma Gairdner Dyke Swarm (Fanning et al., 1986).||||Overlain by Burra Group. Underlain by basement.||
3338|Callanna Group|68713|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Limited and disjointed exposures.||||Unconformably overlain by the Burra Group.||
3338|Callanna Group|69019|5|Briefly described|p36-38, p142-143.|Neoproterozoic|Neoproterozoic|Willouran age; oldest rocks in Adelaide Geosyncline. Mostly disrupted with diapiric structures.|||Arkaroola and Curdimurka Subgroups.|Is overlain by Burra Group.||
3338|Callanna Group|69023|6|Mentioned|p63-64, p146-147|||Coats and Blissett (1971).|||Includes Arkaroola Subgroup.|||
3338|Callanna Group|69438|5|Briefly described|p23:11|||Adelaide Fold Belt.|||Coominaree Dolomite.|Is correlated with the Bitter Springs Formation (Amadeus Basin).||12-JUL-16
3338|Callanna Group|69666|6|Mentioned|p24, p27|Neoproterozoic|Neoproterozoic|||||||
3338|Callanna Group|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession [but mis-spelt as Calanna Group].||||||
3338|Callanna Group|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
3338|Callanna Group|70383|6|Mentioned|p45|||Near Blinman, these rocks are overlain by Permian glacigene sediments.||||||
3338|Callanna Group|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Warrina Supergroup.|Include Arkaroola Subgroup.|Is overlain unconformably by Burra Group.||18-JAN-19
3338|Callanna Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Willouran||Of Warrina Supergroup.|Includes Arkaroola Subgroup, Curdimurka Subgroup.|||
3338|Callanna Group|70790|5|Briefly described|p258, p260 Fig.2|Neoproterozoic|Neoproterozoic||~802-777 Ma.||||Includes evaporites.|
3338|Callanna Group|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.|||Arkaroola, Curdimurka Subgroups.|Is overlain by Burra Group.||
3338|Callanna Group|71129|5|Briefly described|p17,98,101,107,207|Tonian|Tonian|Geological Province: Gawler Craton. [Misspelt as Calanna Group on p98]. Oldest group of the Adelaide Geosyncline.|||Includes Backy Point Formation and Beda Basalt.||Sediments and mafic volcanics.|13-NOV-19
3338|Callanna Group|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Warrina Supergroup.|Includes Pindyin Sandstone.|||
3338|Callanna Group|71317|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||24-MAR-21
3338|Callanna Group|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3338|Callanna Group|72429|4|Described|p949, p952, p958, p969, p974|Neoproterozoic|Neoproterozoic|Adelaide Rift. Mount Chambers Gorge, unknown in mapped exposures, but form bulk of siliciclastic, carbonate, and basic igneous xenoclast rock types in diapiric breccias. Other xenoclastic rocks include: mauve, pink, blue-green, pale grey micaceous siltstone with abundant halite casts. Dark-weathered, cream-white dolostones with quartz granule laminae. Rare amygdaloidal basalt. Textures discussed further.|||||Xenoclast rocks assigned to this unit include: medium to coarse-grained, heavy-mineral laminated, finely cross-bedded quartzite grading to coarse arkose with quartz and red feldspar granules.|
3338|Callanna Group|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shown as part of diapir formation diagram, p1.  Shown in Oraparinna and Enorama Diapirs. Deposited in shallow, restricted seas, coastal lagoons and saline lakes.|800 Ma.||||Includes diapiric breccia rock with carbonate cement. Rafts of sandstone, siltstone;  volcanic ash layers, rare dolomite, stromatolitic. Salt casts abundant throughout. Rafts of basalt, dolerite.|
3338|Callanna Group|72461|6|Mentioned|p19|||||||||
3338|Callanna Group|72473|6|Mentioned|p4|||||||||
3338|Callanna Group|72478|6|Mentioned|p8|Torrensian|Neoproterozoic|Officer Basin. Age described as Willouran to Torrensian.|c. 820 Ma-760 Ma||Includes the Pindyin Sandstone, Alinya Formation, Cadlareena Volcanics and the Coominaree Dolomite.|Unconformably underlies the Lake Maurice Group, Chambers Bluff Tillite..||24-MAR-21
3338|Callanna Group|72489|6|Mentioned|p4 Fig.3|Tonian|Tonian|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||Underlies the Burra Group.||14-SEP-20
3338|Callanna Group|72492|5|Briefly described|p1-2, p17, p18|Neoproterozoic|Neoproterozoic|[Overall subject of this paper]. Depositional environments discussed. Previously been interpreted as lacustrine and highly alkaline.|c. 800 Ma||Includes Curdimurka Subgroup, Arkaroola Subgroup||Includes cyclically alternating siliciclastic sediments, carbonates, evaporites and minor volcanic flows. Major outcrop areas occur in the Peake and Denison Ranges, the Willourian Ranges, the Worumba Anticline and the Spalding Inlier.|16-SEP-20
3338|Callanna Group|73086|6|Mentioned|p57|||Adelaide Rift Complex.|||Rock Tuff|Overlain by Burra Group.||
3338|Callanna Group|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, locally carbonaceous; sandstone and local conglomerate; carbonates, locally stromatolitic; evaporite mineral casts. Basalt, minor felsic volcanics.|09-DEC-21
3338|Callanna Group|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears in the Legend as CALLANNA/BURRA GROUP EQUIVALENTS and mapped as one unit. Said to include Pindyin Sandstone, but does not specify to which Group it belongs.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3338|Callanna Group|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Presented as Callanna/Burra Group equivalents. Mapped as one unit. Includes Pindyin Sandstone (but which Group contains it is not mentioned). Subsurface.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3338|Callanna Group|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Mapped as one unit and named in the Map Legend as CALLANNA/BURRA GROUP EQUIVALENTS. Said to include Pindyin Sandstone, but it is not spelled out which Group is the Parent.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3338|Callanna Group|73188|6|Mentioned|p352|||Willouran Trough. Flinders and Willouran ranges; not represented in the Adelaide region. Over 6 km thick.|||||Mixed siliciclastic-carbonate and evaporitic rift sediments.|
3338|Callanna Group|73222|5|Briefly described|p5-7, p11-12, p16-18, p20, p24-27|Tonian|Tonian|Adelaide Rift Complex, base. Willouran to Torrensian. Thickness: ca 130 to 8,400 m (Preiss, 1987). Deposited in a highly restricted marginal marine sabkha during the early stages of rifting. Mobilisation of evaporites within this unit began as early as the Willouran. Autochthonous [in original depositional position] in the Willouran and Gammon ranges. Previously interpreted as the only unit preserved as intrasalt inclusions within the diapiric breccia (diapiric to allochthonous salt) in the Flinders Ranges; however, Ediacaran units were identified in the Patawarta Diapir (Wonoka Formation and Patsy Hill Member).||Warrina Supergroup|Curdimurka Subgroup, Arkaroola Subgroup, and units therein||Layered evaporite sequence composed of evaporite, siliciclastic, carbonate (mostly dolomite), igneous and metamorphic rocks.|
3338|Callanna Group|73227|6|Mentioned|p23|||||||||
3338|Callanna Group|73234|6|Mentioned|p5-6||||||Backy Point Formation|||
3338|Callanna Group|73236|6|Mentioned|p46|Tonian|Tonian|Deposited in rift basins.|c. 830-800 Ma||||Evaporitic mixed clastic-carbonate sediments.|
3338|Callanna Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably overlain by Burra Group.|Metasediments.|
3338|Callanna Group|73262|5|Briefly described|p580-583, p586|[Tonian?]|[Tonian?]|||Warrina Supergroup|Rook Tuff|Overlain by Boucaut Volcanics (Burra Group).|Siltstone, sandstone, stromatolite, carbonate, evaporite, basalt, minor acid and intermediate volcanics.|
3338|Callanna Group|74367|4|Described|p3, p5-6, p7 Fig.6, p13, p17-18, p20|Tonian|Tonian|Syn-rift. See also p22.|ca. 850-790 Ma|Warrina Supergroup|Arkaroola Subgroup, Curdimurka Subgroup|Underlies Burra Group|Dominated by clastic and carbonate rocks. Includes evaporitic rocks and mafic volcanic rocks.|
3338|Callanna Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
3412|Campana Creek Member|22643|5|Briefly described|p193, fig6|Early Cambrian|Early Cambrian|Age: Botomian.||||||
3412|Campana Creek Member|24465|4|Described|p348|Early Cambrian|Early Cambrian|Originally included in Carrickalinga Head Formation.  Now included in the Backstairs Passage Formation.  Overlies the Blowhole Creek Member. Unit may be thicker than originally described, due to faulting/shears removing part of section.|||||Mostly laminated to cross-bedded fine- to medium-grained sandstone with subordinate siltstone. Conglomeratic sandstone ~2/3 of way up in Karinya Syncline.|06-NOV-15
3412|Campana Creek Member|30377|4|Described|p204|||135 m thick in type section. Up to 535 m at Sedan Hill in Karinya Syncline.||||||06-NOV-15
3412|Campana Creek Member|30378|6|Mentioned|p432|||||||||
3412|Campana Creek Member|30381|6|Mentioned|Fig.4|||||||||
3412|Campana Creek Member|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3412|Campana Creek Member|40454|6|Mentioned|Table 1|||||||||
3412|Campana Creek Member|41947|6|Mentioned|Fig.2 P17|||||||||
3412|Campana Creek Member|42243|5|Briefly described|p211|||||||||
3412|Campana Creek Member|42270|5|Briefly described|p362|||See also Fig.6||||||
3412|Campana Creek Member|43759|6|Mentioned|p446|||||||||
3412|Campana Creek Member|44133|5|Briefly described|p7 Fig. 7.4, 15|||Of the Carrickalinga Head Formation (Kanmantoo Group). Maximum Thickness: 535m. Overlain by: Backstairs Passage Formation.||||||
3412|Campana Creek Member|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of Carrickalinga Head Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||15-JAN-08
3412|Campana Creek Member|63848|5|Briefly described|p531,  p534 Fig.4.|||South coast of Fleurieu Peninsula. Contains possible hyolithids.||Unit in Backstairs Passage Formation.||||
3412|Campana Creek Member|65664|5|Briefly described|p1101-4, Tabs.1-4, p1106 Fig.5|Early Cambrian|Early Cambrian|||Of Backstairs Passage Formation.||||09-MAY-12
3506|Cape Jervis Formation|22458|4|Described|p523, Fig.1 p524||Permian|||||||
3506|Cape Jervis Formation|22528|6|Mentioned|p43 Fig2||Late Paleozoic|||||||07-NOV-08
3506|Cape Jervis Formation|22573|6|Mentioned|p 47|||||||||
3506|Cape Jervis Formation|22857|6|Mentioned|p238|Permian|Carboniferous|Correlated with Urana Formation sediments in infrabasins beneath Murray Basin.||||||
3506|Cape Jervis Formation|22863|6|Mentioned|p238|||||||||
3506|Cape Jervis Formation|22887|6|Mentioned|p29, Fig.5 p12|||Equivalent to Urana Formation||||||
3506|Cape Jervis Formation|22893|6|Mentioned|p21|Permian|Permian|||||||
3506|Cape Jervis Formation|23981|5|Briefly described|p24|Permian|Carboniferous|Glacial deposits.||||||
3506|Cape Jervis Formation|24360|5|Briefly described|p54|Permian|Permian|Geological Province: Yorke Peninsula, Gawler Craton||||||
3506|Cape Jervis Formation|24465|5|Briefly described|p351 Fig.1|Permian|Carboniferous|||||||
3506|Cape Jervis Formation|42100|6|Mentioned|p74|||||||||
3506|Cape Jervis Formation|42547|4|Described|p85|||||||||
3506|Cape Jervis Formation|43052|5|Briefly described|Table 2.1|||||||||
3506|Cape Jervis Formation|43053|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Troubridge Basin.||||||25-MAY-05
3506|Cape Jervis Formation|43195|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|See also commentary on back of map.||||||
3506|Cape Jervis Formation|43200|5|Briefly described|p6||Permian|Troubridge Basin||||||
3506|Cape Jervis Formation|43258|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
3506|Cape Jervis Formation|43298|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
3506|Cape Jervis Formation|44133|5|Briefly described|p65 Fig. 8.4, 66 Fig. 8.6|Permian|Carboniferous|Geological Province: Troubridge Basin. Formerly Cape Jervis Beds. Overlain by Point Ellen Formation..||||||
3506|Cape Jervis Formation|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Troubridge Basin.||||||
3506|Cape Jervis Formation|60958|5|Briefly described|Map Legend|Permian|Permian|Diamictite of unconsolidated yellow-green siltstone, sandstone, sandy limestone and grit with rounded pebbles, boulders and residual erratics. Geological Province: Troubridge Basin.||||||23-DEC-09
3506|Cape Jervis Formation|61108|5|Briefly described|map legend|Permian|Carboniferous|Glaciomarine, fluvioglacial and fluviolacustrine till, clay, silt, sand and gravel, indurated and coal-bearing in Ackaringa Basin. Geological Province: Troubridge Basin.||||||
3506|Cape Jervis Formation|61121|5|Briefly described|Map legend|Permian|Permian|Diamictite of unconsolidated yellow-green siltstone, sandstone, sandy limestone and grit with rounded pebbles, boulders and residual erratics. Abundant pollen and spores.  Uppermost part is glacio-marine siltstone and foraminifers.  Age is Sakmarian.||||||23-DEC-09
3506|Cape Jervis Formation|62893|6|Mentioned|p18|||Troubridge Basin.||||Equivalent to Coolardie Formation.||
3506|Cape Jervis Formation|64282|5|Briefly described|Map legend|Carboniferous|Carboniferous|Geol.Prov: St Vincent Basin. Includes an upper unnamed sandstone member. Diamictite of unconsolidated yellow-green siltstone, sandstone, sandy limestone and grit with rounded pebbles, boulders and residual erratics of Cambrian Kanmantoo Gp; includes rare||||||24-JUL-08
3506|Cape Jervis Formation|64397|5|Briefly described|p232 Fig. 1A|Permian|Permian|Sand and clay with pebbles and boulders. Geological province: St Vincent Basin.||||||
3506|Cape Jervis Formation|64769|6|Mentioned|p28|Permian|Permian|Finniss River Sandstone is a dimensions stone that is mined from this formation.||||||05-MAY-09
3506|Cape Jervis Formation|65375|4|Described|p28, pp31-33, p50.|Permian|Late Carboniferous|Southern Yorke Peninsula.Formerly Cape Jervis beds (Ludbrook 1967). Deposited in glacio-lacustrine, glacio-fluvial and restricted marine environments. Widely intersected in drillholes, but thickness varies widely and outcrops are limited. Erratics suggest west and northwestward glacial movement.||||Unconformably overlies Yuruga Formation. Is unconformably overlain by Port Willunga Formation, Hindmarsh Clay and Bridgewater Formation.|Diamictites, massive, mainly green-grey silts with erratics of granite, sandstone, metamorphic basement and Kanmantoo Group metasediments.|18-JAN-17
3506|Cape Jervis Formation|66623|5|Briefly described|p231.|Permian|Permian|Poorly consolidated periglacial deposits of the southern Mount Lofty Ranges and beneath the Murray Basin. Correlated with Urana Formation and Yanna Tank Formation in NSW.||||||
3506|Cape Jervis Formation|69372|3|Fully described|p24-39 |Sakmarian|Gzhelian|Troubridge Basin. 5 facies recognised in type section. Comparisons made between type section at Cape Jervis, Fleurieu Peninsula and sections examined on Kangaroo Island. Glacigene sediments. Glacial erosional features common (dropstones etc). Some sediments interpreted as turbidites. Includes Sakmarian age dropstones (foraminiferal assemblages) in uppermost facies at type section.||||Underlies Wisanger Basalt and Kingscote Limestone. Overlies Stokes Bay Sandstone, Boxing Bay Formation and Kanmantoo Group.|Interbedded glacigene coarse sandstone, clay, sandy clay and conglomerate; common horizontal bedding and intraformal slumping with strong trough and planar cross bedding; rip up clasts. Pebbles of limestone, quartzite and granodiorite.|18-JAN-17
3506|Cape Jervis Formation|70382|5|Briefly described|p28, p34|Permian|Permian|Geological province: Troubridge Basin.  Crops out across Fleurieu Peninsula, Kangaroo Island and southern Yorke Peninsula. Includes Granite boulders (likely from Delamarian granites e.g. Encounter Bay Granite) and Kanmantoo Group sediment boulders found here were likely remobilised and transported via Permian glaciers. |||||Dominantly diamictite, with granitic boulders e.g. Encounter Bay Granite, and boulders of Kanmantoo Group sediments.|
3506|Cape Jervis Formation|70660|5|Briefly described|p11-p12, p33, p42|Permian|Carboniferous|Deposited in a glaciomarine environment.||||Overlain by the North Maslin Sand.|Diamictite and glaciolacustrine sediments with dropstones.|
3506|Cape Jervis Formation|72450|5|Briefly described|Brochure map|Permian|Carboniferous||c. 300 Ma||||Pebbly and bouldery claystone, sandy, laminated claystone with dropstones.|
3506|Cape Jervis Formation|73107|5|Briefly described|Map legend.|Permian|Carboniferous|Clasts include Kanmantoo Group metasediments and Cambro-Ordovician megacrystic granite, granite gneiss and aplite sourced from the east. Uppermost glacio-marine siltstone with foraminifera. Sakmarian. Mapped separately is an un-named subunit of kaolinised fluviatile sandstone; white kaolinised gritty sand and claystone with wood fragments and fossil leaf remains; tabular cross-bedded; fluviatile sands.|||||Diamictite of unconsolidated yellow-green siltstone, sandstone, sandy limestone and grit with rounded pebbles, boulders and residual erratics; includes rare silicified glaciofluvial outwash sediments. Abundant pollen and spores.|
3506|Cape Jervis Formation|73188|5|Briefly described|[See comments]|Permian|Carboniferous|Troubridge Basin. Widespread. Occupies deeply scoured glacial valleys on Fleurieu Peninsula and Kangaroo Island and under Backstairs Passage. p: 314, 317-320, 335, 341, 343-345, 349, 351, 354-355, 359.|||||Diamictic, sandy and shaly facies with dropstones.|
3506|Cape Jervis Formation|73236|4|Described|p35-45|Permian|Carboniferous|Glacial sediments. Contains erratics of the Sturt Tillite and ABC Range Quartzite [and Seacliff Sandstone, Marino Arkose Member, Wilmington Formation, and Encounter Bay Granite].||||Disconformably overlain by Hallett Cove Sandstone.|Pebbly and bouldery clay, including flow till lenses; massive weakly indurated, medium-grained sandstone; soft, grey, laminated shale with dropstones; massive clayey-sandy matrix diamictite, lodgement till in glacial valley bottom.|
3506|Cape Jervis Formation|73292|6|Mentioned|p955|Permian|Permian||||||Glacigene sediments.|
3507|Cape Kersaint Granite|32457|6|Mentioned|p97|||||||||
3572|Carappee Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
3572|Carappee Granite|41325|6|Mentioned|Fig.2|||||||||
3572|Carappee Granite|41327|2|Defined|p2|Proterozoic||||||||
3572|Carappee Granite|42738|5|Briefly described|map legend|Mesoproterozoic||||||||
3572|Carappee Granite|43052|5|Briefly described|Table 4.4|||Of ?Lincoln Complex.||||||05-MAR-08
3572|Carappee Granite|50605|5|Briefly described|p(i), p1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1689 +/- 59Ma (U-Pb). Of the Younger Lincoln Supersuite.||||||07-NOV-08
3572|Carappee Granite|62893|4|Described|Map Legend, p4-5, p14, p29|Early Proterozoic|Early Proterozoic|U-Pb zircon age of 1689 +/- 59 Ma, although there was evidence of radiogenic lead loss (Flint et al. 1988).||Lincoln Complex|||Tabular feldspar granite, foliated with feldspar phenocrysts and megacrystic granite gneiss.|
3572|Carappee Granite|65922|5|Briefly described|p9|Statherian|Statherian|Included in Ifould Complex for which an age of ~1685-1670 Ma is given.||||||
3572|Carappee Granite|66302|6|Mentioned|p27|Statherian|Statherian|Also dated at 1689 +/- 59 by Flint et al. (1988).|1720 +/- 3 Ma (Fraser and Neumann, 2010)|Moody Suite||||
3572|Carappee Granite|70721|6|Mentioned|p63|||||||||
3572|Carappee Granite|71859|5|Briefly described|p1|||Southern Gawler Craton.||||||
3572|Carappee Granite|71862|4|Described|p2, p7, p11, p13, p23|Statherian|Statherian|Outcrops extensively 35km southwest of Kimba on the Eyre Peninsula at Carappee Hill and on the western edge of Darke Peak Range in the central Eyre Peninsula. Originally a part of the now obsolete Lincoln Complex. Age is interpreted as the age of magmatic crystallisation. See also p33-p34, p42, p58-p60.|1720 +/- 3 Ma (Fraser and Neumann, 2010)|Pinbong Suite||Intrudes (presumably) the Hutchison Group.|Medium- to coarse-grained megacrystic quartz-feldspar-biotite granite.|
3619|Carisbrooke Sand|22541|6|Mentioned|Fig 3|||||||||
3619|Carisbrooke Sand|23418|6|Mentioned|p14 Fig.4|||||||||
3619|Carisbrooke Sand|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
3619|Carisbrooke Sand|29697|6|Mentioned|Table 7|||||||||
3619|Carisbrooke Sand|30180|6|Mentioned|p116|||||||||
3619|Carisbrooke Sand|30757|6|Mentioned|p4|||||||||
3619|Carisbrooke Sand|30918|6|Mentioned|p86|||||||||
3619|Carisbrooke Sand|31655|4|Described|p103|||Hydrogeology||||||
3619|Carisbrooke Sand|32509|5|Briefly described|p9|||From drillhole||||||
3619|Carisbrooke Sand|33057|5|Briefly described|p10|||Plio.-Pleist. Refers Lindsay (1969) Geol. Section.||||||
3619|Carisbrooke Sand|34295|4|Described|p40|||Pliocene - Pleistocene sands||||||
3619|Carisbrooke Sand|35097|6|Mentioned|Fig.4|||||||||
3619|Carisbrooke Sand|35906|6|Mentioned|p5|||See also Fig.2 & Table 1.||||||
3619|Carisbrooke Sand|37853|6|Mentioned|Fig.2|||||||||
3619|Carisbrooke Sand|38107|4|Described|p45|||||||||
3619|Carisbrooke Sand|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
3619|Carisbrooke Sand|40003|5|Briefly described|Table 11|||||||||
3619|Carisbrooke Sand|40442|4|Described|p35|||||||||
3619|Carisbrooke Sand|40453|6|Mentioned|Fig.2|||||||||
3619|Carisbrooke Sand|41025|6|Mentioned|Fig.2|||||||||
3619|Carisbrooke Sand|41513|6|Mentioned|p45|||||||||
3619|Carisbrooke Sand|41520|5|Briefly described|Fig.6|||||||||
3619|Carisbrooke Sand|42498|5|Briefly described|Map legend|early Pleistocene|late Pliocene|||||||
3619|Carisbrooke Sand|42506|5|Briefly described|Map legend|Pleistocene||||||||
3619|Carisbrooke Sand|42733|5|Briefly described|map legend|Quaternary||||||||
3619|Carisbrooke Sand|44133|5|Briefly described|p165 Fig. 10.11|Pliocene|Pliocene|Geological Province: Saint Vincent Basin.||||||
3619|Carisbrooke Sand|61155|5|Briefly described|p17|Late Pliocene|Late Pliocene|Age: 3-1.5Ma. Partly overlies and interfingers with both Dry Creek and Hallett Cove Sandstones; overlain by Hindmarsh Clay. Geological Province: St Vincent Basin.||||||03-MAR-10
3640|Carnadinna Surface|42816|6|Mentioned|p23|||||||||
3640|Carnadinna Surface|67120|5|Briefly described|Map legend|Tertiary|Tertiary|Developed on Mesozoic and Paleozoic units.|||||Ferricrete duricrust.|
3640|Carnadinna Surface|73099|5|Briefly described|Map legend.|Pliocene|Eocene|Meramangye and Tallaringa Palaeochannels.|||||Ferricrete; dark brown ferruginous duricrust developed on Mesozoic and Palaeozoic units; overlain by reworked ironstone (maghemite) gravel spreads.|
3659|Carpa Granite|22834|6|Mentioned|P39|||||||||
3659|Carpa Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
3659|Carpa Granite|37461|6|Mentioned|p322|||||||||
3659|Carpa Granite|37811|6|Mentioned|Fig.10|||||||||
3659|Carpa Granite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3659|Carpa Granite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3659|Carpa Granite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3659|Carpa Granite|39802|6|Mentioned|Legend|||On map legend relating to orogenies.||||||
3659|Carpa Granite|40448|6|Mentioned|p34|||||||||
3659|Carpa Granite|40644|5|Briefly described|p124 Fig. 3,  p132|Mesoproterozoic|Paleoproterozoic|Included in the Lincoln Complex grouping.  Intrudes Middle Camp Granite. Age: 1677+/-125Ma (see p132 Fig. 16).||||||07-NOV-08
3659|Carpa Granite|40942|6|Mentioned|p11|||||||||
3659|Carpa Granite|41667|5|Briefly described|p12|||||||||
3659|Carpa Granite|42738|5|Briefly described|map legend|Mesoproterozoic||||||||
3659|Carpa Granite|43052|4|Described|p81,Table 4.4|||Of Moody Suite.||||||05-MAR-08
3659|Carpa Granite|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1677 +/- 125Ma (Rb-Sr). Of the Moody Suite (Younger Lincoln Supersuite).||||||07-NOV-08
3659|Carpa Granite|62893|6|Mentioned|Map Legend, p14|Early Proterozoic|Early Proterozoic|Of Parker (1983). Found near Elbow Hill.||||||
3659|Carpa Granite|65376|5|Briefly described|pp83-85. |||||Unit in Moody Suite.|||Massive, generally non-foliated, garnet-bearing, S-type adamellite.|
3659|Carpa Granite|66302|6|Mentioned|p14|Neoarchean|Neoarchean|Cleve Domain, Gawler Craton. SHRIMP age given is considered somewhat unreliable as it is based on 4 analyses of poor quality zircon. |2518 +/-8 Ma (Fraser and Neumann, 2010)|Moody Suite||||
3659|Carpa Granite|68208|6|Mentioned|p32|||Part of what was previously known as the Narridy Creek granite.||||||
3659|Carpa Granite|70721|6|Mentioned|p63||||c. 2515 Ma|||||
3659|Carpa Granite|71318|5|Briefly described|p3,41-42|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton. Sample GSSA 2017969 (granite) yielded an interpreted (LA-ICPMS weighted mean 207Pb/206Pb) magmatic crystallisation age of 2490+\-23 Ma (within uncertainty of 2513+\-47 Ma age of Fraser and Neumann 2010). Pb loss trends at c. 1720 Ma is consistent with those reported by Fanning et al. (2007) and indicates effects of metamorphism during Kimban Orogeny. Zircon characteristics, petrography, U-Pb isotopic results and geochronological interpretation are provided.|||||Coarse-grained holocrystalline textured granite largely consisting of quartz and potassium feldspar with minor garnet and plagioclase.|10-DEC-19
3659|Carpa Granite|71859|2|Defined|p1-p2, p6-p7, p16-p29, p36-p37|Neoarchean|Neoarchean|Southern Gawler Craton. First used by Rutland et al (1981) and subsequently on the WHYALLA 1:250k map sheet of Parker and Flint (1983) and described in the accompanying explantory notes (Parker and Fanning 1998 but was never formally defined. The name is presumably derived from the Carpa Homestead or Carpa Waterhole. The type locality is herein defined as the exposures extending around Carpa Homestead (656245 m E 6263081m N AGD66), and Sunny Brae Homestead (656778 m E 6262041 m N AGD66). Previously assigned to the palaeoproterozoic Lincoln Complex before geochronology recognised it as part of the Sleaford Complex. This unit is high silica, magnesian, alkali-calcic to peraluminous. Geochemistry suggests this unit has a significant mantle component although the more evolved parts have a greater crustal component suggesting possible mesoarchean reworking of basement. Occurs as scattered outcrops in the Cleve Hills west of Cowell. Geochemistry analyses and results are discussed. In contact with the Coolanie Gneiss, Minbrie Gneiss and the Hutchison group [although the nature of these contacts is not provided].|c. 2520-2515 Ma (magmatic cry.)|Sleaford Complex||Faulted against the Middle Camp Granite.|Massive, unfoliated to weakly foliated, medium-grained, quartz-K-feldspar-plagioclase-biotite-muscovite granite to granodiorite.|05-APR-23
3659|Carpa Granite|71862|6|Mentioned|p2, p8, p12, p15|Neoarchean|Neoarchean|Originally a part of the now obsolete Lincoln Complex.|c. 2520 Ma|||||12-APR-23
3659|Carpa Granite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Archean|Metamorphosed at 1724 Ma (U-Pb).|2517 - 2513 Ma (crystallisation).||||Granite, pink, medium-grained, equigranular, quartz-feldspar-biotite-muscovite +/- garnet, weakly foliated.|
3744|Casterton Formation|12781|6|Mentioned|p385-386, 402|Early Cretaceous|Jurassic|Penola Trough, W Otway Basin. A thin (up to 60m) and ""rather enigmatic"" unit, difficult to correlate seismically or stratigraphically.||||Unconformably overlies Kanmantoo Group (basement). Is overlain unconformably by Pretty Hill Formation (Crayfish Group).||
3744|Casterton Formation|22674|4|Described|p718, Fig.2 p719|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|22686|6|Mentioned|Fig3p745|Berriasian|Tithonian| Geological Province: Otway Basin.||||||17-JAN-06
3744|Casterton Formation|22875|3|Fully described|p31|Early Cretaceous|Early Cretaceous|Otway Group.||||||22-DEC-08
3744|Casterton Formation|22930|6|Mentioned|50|||||||||
3744|Casterton Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|23427|6|Mentioned|Table 11.2 p418.|||Possibly informal.||||||
3744|Casterton Formation|23911|4|Described|p95 Fig. 9B|Tithonian|Tithonian|Geological Province: Otway Basin.  Overlying Unit: Crayfish Subgroup. Of the Otway Group.||||||
3744|Casterton Formation|24164|6|Mentioned|p16|Jurassic|Jurassic|Near Otway Basin (western Victoria) age typically about 160 Ma (Mitchell et al. 1997)|||||Basalt|
3744|Casterton Formation|24209|5|Briefly described|p152|Berriasian|Late Jurassic|Geological Province: Penola Trough (Otway Basin).||||||
3744|Casterton Formation|24314|5|Briefly described|p61 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Otway Basin. Max. Thickness ?500m.||||||30-NOV-04
3744|Casterton Formation|24323|5|Briefly described|p135|Late Jurassic|Late Jurassic|Geological Province: Otway Basin||||||
3744|Casterton Formation|24453|4|Described|p808, p809 Fig.2|Early Cretaceous|Late Jurrasic|Fluvial sandstones, conglomerates and minor siltstones, coals, tuffs and basalt. Of Otway Group. Geological Province: Otway Basin.||||||27-JUN-14
3744|Casterton Formation|24551|5|Briefly described|p240, Fig. 9.2, 241|Early Cretaceous|Late Jurassic|Maximum Thickness: 230m.  Of the Otway Group.||||||
3744|Casterton Formation|24562|5|Briefly described|p8 Fig. 2|Berriasian|Late Jurassic|Of the Otway Supergroup.  Geological Province: Otway Basin.||||||
3744|Casterton Formation|41726|5|Briefly described|p420|||||||||
3744|Casterton Formation|42153|5|Briefly described|p352|||See also Fig.2||||||
3744|Casterton Formation|42361|6|Mentioned|p4|||Used 1989, but Casterton beds preferred herein.||||||
3744|Casterton Formation|43171|5|Briefly described|2-8|Tithonian|Kimmeridgian|)f Otway Supergroup. Age: 150Ma.||||||22-DEC-08
3744|Casterton Formation|43195|5|Briefly described|Map Legend||Late Jurassic|See also commentary on back of map.||||||
3744|Casterton Formation|43208|5|Briefly described|map legend|Berriasian|Oxfordian|Of Otway Group.||||||
3744|Casterton Formation|43219|5|Briefly described|Fig.3,p6.|Tithonian|Oxfordian|Of Otway Group.||||||22-DEC-08
3744|Casterton Formation|43590|4|Described|p7|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|43744|6|Mentioned|Fig.3,p3|||||||||
3744|Casterton Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
3744|Casterton Formation|44133|5|Briefly described|p142, 94 Fig. 9.2|Cretaceous|Jurassic|Geological Province: Otway Basin. Previosly recorded as 'Unit T', 'Basal Unit', 'Casterton Group undifferentiated'.||||||
3744|Casterton Formation|50154|5|Briefly described|p123, p131||Jurassic|Geological Province: Otway Basin. Age: ~150 Ma. Units that have been described range from Jurassic well into the Early Cretaceous. In need of revision due to uncertain age and status.||||||
3744|Casterton Formation|60126|4|Described|p4-8|Valanginian|Valanginian|Predominantly composed of carbonaceous shales with minor interbedded sltst. sst, volcaniclastics, basalt flows.  Age based on spore-pollen content of samples from Sawpit-1 well, incl. Gagiella mutabilis, a dinoflagellate which occurs precisely in this era||||||
3744|Casterton Formation|61017|5|Briefly described|p5 Fig. 2, p6|Tithonian|Callovian|Of the Otway Group. Non-marine lacustrine to fluvial sediments, with potential as excellent source rocks for hydrocarbons. Geological Province: Otway Basin.||||||07-FEB-11
3744|Casterton Formation|61182|3|Fully described|p11, p82-83|||Formerly Casterton Beds. Base of the Otway Group. Unconformably overlain by Pretty Hill Formation. Basalt with minor pyroclastics and sediments. Max. thickness: 536m. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61470|5|Briefly described|p28 Fig. 5|Tithonian|Callovian|Of the Otway Group. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61528|5|Briefly described|p819|Berriasian|Kimmeridgian|Overlain by Crayfish Group rocks or Eumeralla Formation. Age: ~146-134 Ma. Max. thickness: >1000m. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61547|6|Mentioned|p461. |Berriasian|Kimmeridgian|Lacustrine sediments; the initial sediments in the Penola Trough. ||||Is overlain by Pretty Hill Formation.||
3744|Casterton Formation|61622|4|Described|p436, p436 Fig. 2, p438 Fig. 4|Early Cretaceous|Late Jurrasic|Of Crayfish Group. Thickness: 60 to 500m.  Geological Province: Otway Basin. Lacustrine carbonaceous mudstones, sandstones and minor coals and volcaniclastics.||||||07-FEB-11
3744|Casterton Formation|61623|6|Mentioned|p447, p449 Fig. 4|Late Jurassic|Late Jurassic|Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|61626|5|Briefly described|p486 Fig. 2|Jurassic|Jurassic|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|61627|5|Briefly described|p500 Fig. 2|Late Jurassic|Late Jurassic|Includes Pretty Hill and Laria Formations, Katnooke Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
3744|Casterton Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Jurassic|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|63122|5|Briefly described|p17 Fig. 4.3|Late Jurassic|Late Jurassic|Max. thickness: 60m. Geological Province: Otway Basin.||||||13-DEC-07
3744|Casterton Formation|63124|5|Briefly described|p55-57, p48 Fig. 5.1, p49 Fig. 5.2|Early Cretaceous|Late Jurassic|Originally Casterton Beds, then C.Formation, C.Beds, C.Group, C.beds; now established as Casterton Fm. Unconformable below Crayfish Group; unconformably overlain by Pretty Hill Formation. Age: 150-142Ma. Max.thick: 500m. Geol.Prov:Otway Basin.See also p55||||||
3744|Casterton Formation|63125|5|Briefly described|p104, p116 Tb. 7.6|||Overlain by Pretty Hill Formation. Geological Province: Otway Basin||||||
3744|Casterton Formation|63130|5|Briefly described|p141|||Geological Province: Otway Basin.||||||31-JAN-08
3744|Casterton Formation|63150|5|Briefly described|p95|||Plant microfossils are abundant in claystone and coal, and only absent in any sandstone sections. Geological province: Otway Basin.||||||
3744|Casterton Formation|63267|5|Briefly described|p485 Fig.2, p486 Fig.3, p489-492, p497|Early Cretaceous|Late Jurassic|Penola Trough, Otway Basin. Lacustrine-fluvial deposits. Hydrocarbon source potential (elaborated).||||Is overlain unconformably by Pretty Hill Formation.||
3744|Casterton Formation|63269|5|Briefly described|p603-606, p616, p618, p622, p624|Early Cretaceous|Early Cretaceous|Otway Basin. Lacustrine deposits. Became overmature for gas generation from Late Cretaceous onwards. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Otway Group.||Is overlain unconformably by Pretty Hill Formation.|Mainly carbonaceous shales, with minor interbedded volcanics and sandstone.|
3744|Casterton Formation|63431|5|Briefly described|p676, p677 Fig. 2|Late Jurassic|Late Jurassic|Overlain by Crayfish Group. Lacustrine. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
3744|Casterton Formation|64570|5|Briefly described|p852|Middle Jurassic|Middle Jurassic|Age: 170-160Ma (K-Ar). Geological Province: Otway Basin. Basaltic lavas.||||||22-DEC-08
3744|Casterton Formation|66245|5|Briefly described|p6 Fig.5, p42.|Berriasian|Kimmeridgian|Oldest sediments in the Otway Basin: locally-derived sands, and muds from a more distant source, deposited in locally deep lakes that eventually formed a through-going rift.||Basal unit in Otway Group.|||Fluvial sandstones, floodplain and lacustrine claystones; some coals.|
3744|Casterton Formation|67367|5|Briefly described|p131 Fig.2, pp131-132.|Late Jurassic|Middle Jurassic|Fluvio-lacustrine shales. Hydrocarbon source rock. Assigned to the Austral 1 petroleum sub-system.||Unit in Otway Group.|||Interbedded carbonaceous mudstones.|
3744|Casterton Formation|68135|5|Briefly described|p52 fig 2b |Early Cretaceous|Kimmeridgian|South Australian margin and Tasmania. Plant macrofossils present.|||||Interbedded siltstone and sandstone.|14-SEP-17
3744|Casterton Formation|68189|5|Briefly described|p19 Fig.8, p25|Jurassic|Jurassic|Upper Jurassic age.||Of the Otway Group.|||Comprises basalt and mafic volcaniclastic material.|
3744|Casterton Formation|69297|5|Briefly described|p79, p98-p100, p104, p400|Valanginian|Valanginian|Torquay Sub-basin, Otway Basin.  Deposited in a fluvio-lacustrine environment. Interpreted to be thermally overmature for oil and gas generation.  ||Crayfish Subgroup||Overlain by the Sawpit Shale and Sawpit Sandstone.|Mudstone and shale.|
3744|Casterton Formation|69651|5|Briefly described|p10, p50|Early Cretaceous|Late Jurassic|Fluvio-lacustrine deposits.||Otway Group.||Is overlain unconformably by Pretty Hill Formation (Crayfish Subgroup).|Shales.|
3744|Casterton Formation|70077|5|Briefly described|Nelson:Fig.2. Regional:Fig.4;p4,p6-7,p9|Early Cretaceous|Early Cretaceous|Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Source rocks of the Austral 1 Petroleum System.||Otway Group.||Is overlain by Pretty Hill Formation or Sawpit Shale/Sawpit Sandstone.|Lacustrine sediments and interbedded flow basalts.|
3744|Casterton Formation|70379|5|Briefly described|p717, p719, p721, p724-732|Early Cretaceous|Early Cretaceous|Central Otway Basin. Distribution was restricted to rapidly subsiding, structurally controlled depocentres in the W of the Basin. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Berriasian to early Valanginian.|c. 152-139 Ma.|Crayfish Group.||Is overlain by Sawpit Shale (equivalent) and McEachern Sandstone.|Volcaniclastic and lacustrine deposits.|
3744|Casterton Formation|70880|6|Mentioned|p77|Berriasian|Tithonian|Otway Basin.||||||
3744|Casterton Formation|71266|6|Mentioned|p614 Fig.3|Berriasian|Tithonian|Otway Basin.||||||
3744|Casterton Formation|73356|5|Briefly described|p. 1-2, 4-6, 8-11, 13-16, 19-21,24-27,29|Berriasian|Tithonian|Otway Basin. Upper boundary is unconformable in many instances (cf. Warrong Trough) but is shown to be conformable in the Sawpit-1 well (Penola Trough).||Otway Group||Overlain by Sawpit Formation (conformably), including McEachern Member (disconformably), and Pretty Hill Formation (unconformably) (all of Crayfish Subgroup).||
3744|Casterton Formation|73357|5|Briefly described|p15-16, p45, p47|Berriasian|Berriasian|Otway Basin. Sparse, poorly preserved palynomorph assemblages, or barren of palynomorphs. Assigned to the Ruffordiaspora australiensis Spore-Pollen Zone, wholly terrestrial palynofloras with common fern spores and moderately frequent freshwater algae. May be entirely represented by R. australiensis zone.||Of Otway Group.||Underlies Pretty Hill Formation.|Contains sandy lithologies.|
3744|Casterton Formation|73383|5|Briefly described|p3, p7-8, p11-12, p15, p27, p38, p45|Berriasian|Tithonian|Otway Basin. Approximately equivalent to chemostratigraphic Sequence S0, subdivided into five packages. Defined by high Nb values (generally 20 ppm and above), mixed terrigenous clastic and alkaline volcanic composition. Likely includes coal in parts, and some intervals have high Mo and S concentrations interpreted as deposition in anoxic conditions or in a marine environment/marine incursion. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, limestone, calcareous limestone and igneous rock; and using the Herron classification (1988) includes shale, Fe-shale, Fe-sand, lith-arenite and wacke. See also iii, vi, p55-58, p65-66, p103-106, p112-117, p167, p176, p187-190, p198, p233-236, p241-246, p295, p322, p342-343.||Otway Group||Unconformably underlies Pretty Hill Formation, Crayfish Subgroup|Lacustrine mudstones and alluvial sandstones with initial basaltic volcanics.|
3744|Casterton Formation|73385|5|Briefly described|p3, p5|Berriasian|Tithonian|Otway Basin. Deposited in predominantly NW-SE grabens and half-grabens of limited extent, deposition facilited by a series of lakes within individual depocentres, that became linked to an active fluvio-lacustrine system.||Otway Group||Underlies Pretty Hill Formation.|Lacustrine mudstones and alluvial sandstones with initial basaltic volcanics. Primarily comprised of locally derived sands and far-sourced muds.|
3744|Casterton Formation|73386|4|Described|p2, p4, p6-8, Attachment A1|Berriasian|Tithonian|Otway Basin. Oldest sedimentary unit in basin, unconformably overlies Paleozoic basement. Deposited in half graben structures, distribution restricted to Early Cretaceous depocentres. Conformably underlies Crayfish Subgroup and Sawpit Formation in the western Victorian Otway Basin, unconformable in the central basin. Type section defined between 2220 m and 2450 m in Casterton-1 (Morton et al., 1994). Basalt and tuff deposits dominant in the central Otway Basin, carbonaceous facies are more common in the west. Belongs to the Retriletes watherooensis Spore-Pollen Zone and Lower Ruffordiaspora australiensis Spore-Pollen Subzone of Partridge (2006), corresponds to the S0 chemostratigraphic sequence of Forbes et al. (2020).||Otway Group||Underlies Crayfish Subgroup, Sawpit Formation, McEachern Member|Characterised by lacustrine shales with interbeds of sandstone and siltstone, with much of the sediment associated with basaltic volcanics, includes initial basaltic volcanics.|
3744|Casterton Formation|73594|5|Briefly described|p3-4, p8, p38, p41, p44, p49-55, p66-67|Berriasian|Tithonian|Otway Basin. Deposited in isolated freshwater lakes, stratigraphy is likely to be unique in each half-graben. Up to 500m thick. Restricted to the area west of Warrnambool. See also p45 Fig.5.19, p59.||Otway Group||Underlies Pretty Hill Formation, Crayfish Subgroup|Carbonaceous shales, coals, siltstones and sandstones with minor basalt and trachyte.|
3851|Cecilia Conglomerate|30807|6|Mentioned|p101|||Suggested map symbol||||||
3851|Cecilia Conglomerate|31699|4|Described|p132|||Mid Tertiary||||||
3851|Cecilia Conglomerate|40926|6|Mentioned|Table 3|||||||||
3851|Cecilia Conglomerate|44658|14|Not recorded|map legend||Tertiary|M.Tertiary. (G53-15).||||||
3856|Ceduna Formation|22485|4|Described|p51 , Fig 2|Late Cretaceous|Early Cretaceous|||||||
3856|Ceduna Formation|22663|6|Mentioned|S97-1 and 2 p3|||||||||
3856|Ceduna Formation|23792|5|Briefly described|Fig.D4|Cenomanian|Albian|Equivalent to Blue Whale supersequence. Overlies Upper Borda Formation. Overlain by Platypus Formation. Geological Province: Bight Basin.||||||
3856|Ceduna Formation|24201|5|Briefly described|p373 Fig. 2|Cenomanian|Albian|||||||
3856|Ceduna Formation|24338|5|Briefly described|p938 Fig. 2|Cenomanian|Albian|Overlain by the Platypus Formation. Overlies the Borda Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
3856|Ceduna Formation|24350|5|Briefly described|Fig. 4 Appdx|Cenomanian|Albian|Part of Blue Whale Supersequence.||||||
3856|Ceduna Formation|24443|5|Briefly described|Fig.7|Cenomanian|Albian|Overlies Upper Borda Formation. Overlain by Platypus Formation. Geological Province: Bight Basin.||||||03-FEB-05
3856|Ceduna Formation|24553|5|Briefly described|p36,  Figs. 7 and 8|||Geological Province: Duntroon Sub-basin. Highly porous rocks. Significant oil shows. Part of the Blue Whale Supersequence.||||||07-FEB-11
3856|Ceduna Formation|42075|5|Briefly described|Fig.10 p250|||||||||21-JAN-16
3856|Ceduna Formation|42545|2|Defined|p7|Albian||||||||
3856|Ceduna Formation|43026|5|Briefly described|Table 1, p586|||||||||21-JAN-16
3856|Ceduna Formation|43672|6|Mentioned|p330|Cenomanian|Albian|||||||
3856|Ceduna Formation|43814|6|Mentioned|Fig.3,p115|||||||||
3856|Ceduna Formation|44133|4|Described|p140-141|Mesozoic|Mesozoic|Conformably overlies: Borda Formation. Overlain by Platypus Formation. Previously assigned to Madura Formation. Thickness: 513m.||||||
3856|Ceduna Formation|61544|5|Briefly described|p367 Fig.3, p374.|Albian|Albian|Bight Sub-basin. Post-rift fluvio-deltaic source rocks, primarily with gas source potential.||||Overlies Borda Formation. Is overlain by Platypus Formation.||
3856|Ceduna Formation|61630|6|Mentioned|p555 Fig. 3, p556, p557|Late Cretaceous|Early Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
3856|Ceduna Formation|63124|5|Briefly described|p72|||Deltaic unit. Geological Province: Duntroon Basin. Equivalent to Eumeralla Formation.||||||31-JAN-08
3856|Ceduna Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Cenomanian|Albian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lower and upper deltal plains. See also p39 fig 2.14, p58, p60, p64.||||Overlies the Madura Formation and the Upper Borda Formation. Overlain by the Platypus Formation. Equivalent to the Toondi Formation.|Sandstone.|
3856|Ceduna Formation|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Cenomanian|Albian|Bight Basin.||||Overlies Overlies Upper Borda Formation. Is overlain by Platypus Formation.||
3895|Chambers Bluff Tillite|22649|6|Mentioned|p 143|||Rb-Sr age 651+/-87 Ma p 143.  Province - Officer Basin.||||||
3895|Chambers Bluff Tillite|22746|5|Briefly described|Fig.3 p515|Cryogenian|Cryogenian|||||||
3895|Chambers Bluff Tillite|22901|5|Briefly described|78|||Geol province Officer Basin. Overlying unit Ungoolya Group.||||||30-SEP-08
3895|Chambers Bluff Tillite|22922|5|Briefly described|32|Neoproterozoic|Neoproterozoic|Sturtian age.||||||
3895|Chambers Bluff Tillite|23282|2|Defined|p54||Neoproterozoic|Age: Sturtian Epoch. of Wilson (1952). Lupton and Turkey Hill beds in western Officer Basin considered synonymous.||||||
3895|Chambers Bluff Tillite|23287|6|Mentioned|Fig.4|||Age: Upper Cryogenian. of Eastern Officer Basin.||||||
3895|Chambers Bluff Tillite|23288|6|Mentioned|p128 Fig.5,18|||0f Central and Eastern Officer Basin.||||||24-SEP-08
3895|Chambers Bluff Tillite|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Cryogenian|Geological Province: Officer Basin.||||||
3895|Chambers Bluff Tillite|24067|5|Briefly described|p249 Fig.2|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
3895|Chambers Bluff Tillite|24111|5|Briefly described|p215|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
3895|Chambers Bluff Tillite|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin||||||
3895|Chambers Bluff Tillite|31698|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
3895|Chambers Bluff Tillite|31970|6|Mentioned|p16|||||||||
3895|Chambers Bluff Tillite|31971|6|Mentioned|p9|||||||||
3895|Chambers Bluff Tillite|35628|4|Described|Table 2|||||||||
3895|Chambers Bluff Tillite|36096|6|Mentioned|Fig.3|||||||||
3895|Chambers Bluff Tillite|36920|6|Mentioned|Table 1|||||||||
3895|Chambers Bluff Tillite|37932|6|Mentioned|p537|||||||||
3895|Chambers Bluff Tillite|38157|6|Mentioned|Table VIII|||||||||
3895|Chambers Bluff Tillite|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
3895|Chambers Bluff Tillite|40910|6|Mentioned|p11|||||||||
3895|Chambers Bluff Tillite|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3895|Chambers Bluff Tillite|40945|6|Mentioned|Fig.3|||||||||
3895|Chambers Bluff Tillite|41404|6|Mentioned|p121|||||||||
3895|Chambers Bluff Tillite|41405|3|Fully described|p201|||||||||
3895|Chambers Bluff Tillite|41581|5|Briefly described|p123|||||||||
3895|Chambers Bluff Tillite|42096|6|Mentioned|p37|||||||||
3895|Chambers Bluff Tillite|42410|6|Mentioned|p3|||||||||
3895|Chambers Bluff Tillite|42522|5|Briefly described|p167|||||||||
3895|Chambers Bluff Tillite|43052|4|Described|p198,Table 6.2|||||||||
3895|Chambers Bluff Tillite|43595|5|Briefly described|p549||Late Adelaidean|||||||
3895|Chambers Bluff Tillite|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
3895|Chambers Bluff Tillite|44133|6|Mentioned|p38|||||||||
3895|Chambers Bluff Tillite|44535|4|Described|map legend||Proterozoic|(G/53-9). Unit of Sturtian Series. Proterozoic.||||||
3895|Chambers Bluff Tillite|45149|6|Mentioned|p21|||See also Table 1 and P17.||||||
3895|Chambers Bluff Tillite|49792|5|Briefly described|Fig.5|||||||||
3895|Chambers Bluff Tillite|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Diamictite, quartzite.||||||
3895|Chambers Bluff Tillite|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Diamictite and quartzite. Age and correlation uncertain.||||||
3895|Chambers Bluff Tillite|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Sturtian|Sturtian|Age may be Marinoan? Geological Province: eastern Officer Basin. See also p145 Fig. 51.||||||07-FEB-11
3895|Chambers Bluff Tillite|62453|5|Briefly described|p5 Fig. 3, 12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
3895|Chambers Bluff Tillite|63397|4|Described|p5, 10|Neoproterozoic|Neoproterozoic|The tillite is about 520 m thick and contains yellow/pale green, pebbly, silty diamictite in the lower part and a thin bed of quartzite with minor limestone. Unconformably overlain by Wantapella Volcanics.||||||23-JUL-07
3895|Chambers Bluff Tillite|64103|6|Mentioned|p400 Fig. 3, p404|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
3895|Chambers Bluff Tillite|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Officer Basin during the Centralian 2 event (~700-635 Ma)||||||
3895|Chambers Bluff Tillite|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|||||||
3895|Chambers Bluff Tillite|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
3895|Chambers Bluff Tillite|64970|6|Mentioned|p719 Fig. 2|Sturtian|Sturtian|Geological Province: Officer Basin.||||||27-MAY-09
3895|Chambers Bluff Tillite|65102|6|Mentioned|p367-8|||Eastern Officer Basin. Correlated with Sturtian or Marinoan glacial sediments in Amadeus Basin and Adelaide Geosyncline. Lithologically and stratigraphically similar to Lupton and Turkey Hill Formations.||||||
3895|Chambers Bluff Tillite|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Eastern Officer Basin||||||
3895|Chambers Bluff Tillite|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Eastern Officer Basin||||||
3895|Chambers Bluff Tillite|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Eastern Officer Basin. Part of Supersequence 2.||||||
3895|Chambers Bluff Tillite|67120|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Tillite, gritty siltstone, pale brown and green, interbedded with white feldspathic sandstone and quartzite.|
3895|Chambers Bluff Tillite|67536|6|Mentioned|Map Legend||||||||Diamictite, quartzite.|
3895|Chambers Bluff Tillite|68270|4|Described|p677-678,682-684,687-688|Cryogenian|Cryogenian|Eastern Officer Basin. Type section is 9.6km N/NW of Chambers Bluff, lat 27'01'21"S, long, 133'10'14"E. Up to 610m thick in the type area (far corner NE Officer Basin; Preiss 1987, 1993; Morton 1997). Reference section from Nicholson-2 well (Morton 1997; Eyles et al. 2007). Glacio-lacustrine, fluvio-glacial and glacio-marine deposit. Contains poorly preserved fragments of the acritarch Cerebrosphaera buickii, a regional biostratigraphic marker that could be used for global correlation. Correlative to Sturt Tillite.||||Overlain unconformably by Wantapella Volcanics. Underlain by Alinya Formation and Cadlareena Volcanics equivalent.|Diamictite, sandstone; minor dolomite, partly stromatolitic.|03-JUL-19
3895|Chambers Bluff Tillite|68277|6|Mentioned|p96, 103|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||Possible correlative of Wahlgu Formation (WA).||
3895|Chambers Bluff Tillite|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
3895|Chambers Bluff Tillite|69438|5|Briefly described|p23:17, 19|||Officer Basin.|651 +/- 87 Ma (Rb-Sr: Freeman et al., 1991).|||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
3895|Chambers Bluff Tillite|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Tillite, gritty siltstone, pale brown and green, interbedded with white feldspathic sandstone and quartzite.|
3895|Chambers Bluff Tillite|72478|6|Mentioned|p8|Sturtian|Sturtian|Officer Basin.|c. 720 Ma|||Unconformably overlies the Alinya Formation. Unconformably overlain by the Wantapella Volcanics.||24-MAR-21
3895|Chambers Bluff Tillite|73086|6|Mentioned|p101, p167|Ediacaran|Tonian|Officer Basin. Age is also constrained by the ca 660-635 Ma Marinoan glaciation.|651 +/- 87 Ma Rb-Sr|||Correlates to Olympic Formation.||
3913|Chara Limestone|39804|6|Mentioned|Fig.2|||||||||
3975|Childera Dacite|24474|3|Fully described|p36-37|||Of the Glyde Hill Volcanic Complex.  Overlain conformably by Mangaroongah Dacite.  Max. thickness:>200m.  Geological Province: Gawler Craton.  See also p37 Fig. 2.||||||
3975|Childera Dacite|30984|2|Defined|p15|Proterozoic|Proterozoic|||||||
3975|Childera Dacite|40430|6|Mentioned|p8|||||||||
3975|Childera Dacite|41974|6|Mentioned|p409|||||||||
3975|Childera Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
3975|Childera Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
3975|Childera Dacite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Reddish-brown, purplish-grey and greenish-grey dacite;  scattered feldspar phenocrysts in granular felsi or aphanitic matrix.  Grades to rhyodacite upwards.||||||07-APR-05
3975|Childera Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
3975|Childera Dacite|43052|5|Briefly described|p111|||of Glyde Hill Volcanics Complex||||||
3975|Childera Dacite|43071|4|Described|p12,Table 2|||of Gawler Range Volcanics||||||
3975|Childera Dacite|43094|4|Described|Table 4.|||of Glyde Hill Volcanic Complex||||||
3975|Childera Dacite|50605|5|Briefly described|p(ii), 8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Lower Gawler Range Volcanics. Age: 1592 +/- 17Ma (U-Pb).||||||
3975|Childera Dacite|66302|6|Mentioned|p33|||||||||
3975|Childera Dacite|67909|5|Briefly described|p126-128, 130|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Appears as Childera Rhyolite on p130. Volcanic textures and emplacement mechanism tabulated.||Glyde Hill Volcanic Complex.|||Includes autobreccia zones and intercalated layers of breccia.|
3975|Childera Dacite|69649|6|Mentioned|p18|||Correct spelling of unit name. Only used once. See misspelling Childara Dacite pp17-19.||||||
3975|Childera Dacite|70659|5|Briefly described|p6-8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.|||Dacite separated by volcaniclastic intervals of tuffaceous mudstone, crystal and pumice rich sandstone and breccia.|
3975|Childera Dacite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Lowermost unit of the Glyde Hill Volcanic Complex. Overlain by Mangaroongah Dacite.||
3975|Childera Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
4023|Chitanilga Volcanic Complex|24346|5|Briefly described|p99|Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics.||||||
4023|Chitanilga Volcanic Complex|24474|6|Mentioned|p36|||Geological Province: Gawler Craton.||||||
4023|Chitanilga Volcanic Complex|29838|2|Defined|p10|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4023|Chitanilga Volcanic Complex|30809|6|Mentioned|Fig.1|||||||||
4023|Chitanilga Volcanic Complex|30984|6|Mentioned|p7|||||||||
4023|Chitanilga Volcanic Complex|35107|6|Mentioned|Fig.3|||||||||
4023|Chitanilga Volcanic Complex|37461|6|Mentioned|p325|||||||||
4023|Chitanilga Volcanic Complex|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4023|Chitanilga Volcanic Complex|40241|6|Mentioned|Fig.1|||||||||
4023|Chitanilga Volcanic Complex|40644|6|Mentioned|p124 Fig. 3,  p136|Mesoproterozoic|Mesoproterozoic|Age: 1525+/-14Ma (see Table 4, p135).||||||13-AUG-08
4023|Chitanilga Volcanic Complex|41972|6|Mentioned|Table 3 P378|||||||||
4023|Chitanilga Volcanic Complex|42721|5|Briefly described|map legend|Carpentarian||||||||
4023|Chitanilga Volcanic Complex|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
4023|Chitanilga Volcanic Complex|43052|4|Described|p111|||Of Gawler Range Volcanics.||||||02-JUN-09
4023|Chitanilga Volcanic Complex|43071|5|Briefly described|p12|||Rb/Sr isochron of 1558+/-15 Ma||||||
4023|Chitanilga Volcanic Complex|43094|4|Described|p16|||see also Table 2.||||||
4023|Chitanilga Volcanic Complex|65390|6|Mentioned|p26 Tb. 1|||Intruded by 'Granite, Kokatha'.||||||
4023|Chitanilga Volcanic Complex|65922|5|Briefly described|p16|Calymmian|Calymmian|Also referred to as Chitanilga Complex. Name, in the 'Kokatha' area of South Australia, for the 'older' or 'lower' Gawler Range Volcanics.||||||
4023|Chitanilga Volcanic Complex|67900|5|Briefly described|p20, 30-31|Mesoproterozoic|Mesoproterozoic|Kokatha, Gawler Craton. Appears also as CVC.||Lower Gawler Range Volcanics.|||Ranges through basalt, andesite, dacite, rhyodacite and rhyolite. The felsic units are direct fractionates of the mafic units.|
4023|Chitanilga Volcanic Complex|67909|5|Briefly described|p125-127, 130-132, 140-141|Mesoproterozoic|Mesoproterozoic|Blissett (1975). Kokatha area. Simplified log.|||Lake Gairdner Rhyolite, Chandabooka Dacite.||Lower part contains m-thick vesicular/amygdaloidal basalt to basaltic andesite, with interlayered felsic ignimbrite in layers up to tens of metres thick. Upper part is mainly felsic lavas and ignimbrites; minor intermediate lavas.|
4023|Chitanilga Volcanic Complex|69649|5|Briefly described|p16|||Branch (1978). Common petrogenesis with Glyde Hill Volcanic Complex.||Unit in Gawler Range Volcanics.||||
4023|Chitanilga Volcanic Complex|70659|5|Briefly described|p5, p6 fig 2, p8|Mesoproterozoic|Mesoproterozoic|Total area extent of 120 km2.||||Overlain by Lake Gairdner Rhyolite|Mafic lavas, rhyolitic to dacitic lavas interlayered with andesitic lavas, and ignimbrites. The lowermost sequence consists of basaltic to basaltic-andesite lavas with amygdaloidal flow tops, interbedded with rhyolitic ignimbrites.|06-FEB-17
4023|Chitanilga Volcanic Complex|70738|6|Mentioned|p186-187|||Gawler Craton.|||||Locally includes a basal section (up to 1000m thick) of basalt (porphyritic and amygdaloidal textures common), basaltic andesite and andesite.|
4023|Chitanilga Volcanic Complex|70816|5|Briefly described|p4-5|||Kokatha-NW Lake Gairdner area, Gawler Ranges.||Unit of lower Gawler Range Volcanics.||Overlain by Lake Gairdner Rhyolite.|Basaltic to andesitic lavas interlayered with rhyolitic ignimbrite and volcaniclastic sediment, overlain by rhyolitic to dacitic lavas interlayered wih andesitic lavas|
4023|Chitanilga Volcanic Complex|72090|5|Briefly described|p12|||Gawler Craton.|||||Rhyolite to rhyodacite, andesite, basalt, welded tuff, breccia.|
4023|Chitanilga Volcanic Complex|72462|6|Mentioned|p8|||Gawler Craton.||||||
4023|Chitanilga Volcanic Complex|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
4023|Chitanilga Volcanic Complex|74361|6|Mentioned|p173-174|||Allen et al. (2008). Gawler Craton.||Gawler Range Volcanics.||||
4042|Chowilla Sand|23818|5|Briefly described|p212 Fig.108|Early Pleistocene|Early Pleistocene|Geological Province: Murray Basin. Of the Blanchetown Clay.||||||18-APR-05
4042|Chowilla Sand|24551|5|Briefly described|p338 Fig. 11.2, 340|Middle Pleistocene|Late Pliocene|||||||
4042|Chowilla Sand|30145|6|Mentioned|p183|||||||||
4042|Chowilla Sand|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See stratigraphic table on p22.||||||31-MAR-09
4042|Chowilla Sand|30994|6|Mentioned|Fig. 1|||||||||
4042|Chowilla Sand|30996|3|Fully described|p39|||Refers Firman (1971).||||||31-MAR-09
4042|Chowilla Sand|31345|6|Mentioned|p294|||||||||
4042|Chowilla Sand|31385|6|Mentioned|Table 4|||||||||
4042|Chowilla Sand|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4042|Chowilla Sand|32007|6|Mentioned|Fig. 2|||Pleistocene||||||
4042|Chowilla Sand|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
4042|Chowilla Sand|32861|5|Briefly described|Table 1|||||||||
4042|Chowilla Sand|33048|6|Mentioned|p197|||||||||
4042|Chowilla Sand|33826|6|Mentioned|p42|||Strat. table||||||
4042|Chowilla Sand|34180|6|Mentioned|p212|||Lower Pleistocene.||||||
4042|Chowilla Sand|34459|4|Described|p11|||Pleistocene||||||
4042|Chowilla Sand|34758|6|Mentioned|Table 1|||||||||
4042|Chowilla Sand|35232|6|Mentioned|p15|||||||||
4042|Chowilla Sand|37873|4|Described|p2|||||||||
4042|Chowilla Sand|38068|5|Briefly described|p76|||||||||
4042|Chowilla Sand|40003|6|Mentioned|Table 8|||||||||
4042|Chowilla Sand|41537|6|Mentioned|p350|||||||||
4042|Chowilla Sand|41848|6|Mentioned|p353|||Only on stratigraphic table p353, not in text||||||
4042|Chowilla Sand|42125|5|Briefly described|p138|||||||||
4042|Chowilla Sand|42443|6|Mentioned|p4|||||||||
4042|Chowilla Sand|42827|5|Briefly described|Table 9.1|||||||||
4042|Chowilla Sand|42966|1|Redefined|Table 31 p199|Pleistocene||||||||
4042|Chowilla Sand|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 10m. Geological Province: Murray Basin. Equivalent to Irymple Member. Interfingers with Blanchetown Clay.||||||20-NOV-17
4042|Chowilla Sand|64961|5|Briefly described|p260|||Name used interchangeably with Chowilla Sand Member. Of Blanchetown Clay. Well-sorted sand unit considered as, etc; sand is possibly reworked Loxton-Parilla Sand (see p260).||||||21-APR-09
4042|Chowilla Sand|66287|5|Briefly described|p28,31, Fig 4-5,10|Late Pliocene|Late Pliocene|Similar in appearance to the Loxton-Parilla Sands, but occupies a higher stratigraphic level. With the Blanchetown Clay and the Bungunnia Limestone, part of the Lake Bungunnia sedimentary fill. Included in the Blanchetown Clay by Firman (1965, 1973).||||||25-FEB-13
4042|Chowilla Sand|73228|6|Mentioned|p50, p56, p59|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluvial.||||Unconformably underlain by Karoonda Surface. Overlain by Blanchetown Clay.|Dark-yellow to pale-yellow fine quartz-sand.|
4042|Chowilla Sand|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
4045|Christies Beach Formation|22525|4|Described|p37,41||Pleistocene|||||||
4045|Christies Beach Formation|22941|6|Mentioned|p290|||||||||
4045|Christies Beach Formation|23489|4|Described|p47|Pleistocene|Pleistocene|Geological Province: Noarlunga Embayment.||||||
4045|Christies Beach Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4045|Christies Beach Formation|39522|6|Mentioned|p86|||||||||
4045|Christies Beach Formation|43682|6|Mentioned|p290|||||||||
4045|Christies Beach Formation|44198|2|Defined|p46|Late Pleistocene|Late Pleistocene|||||||
4045|Christies Beach Formation|44199|2|Defined|p594,596-597|Quaternary|Neogene|Age late Tertiary-Quaternary.||||||
4045|Christies Beach Formation|65901|6|Mentioned|p176 Tab.1,p185|||Of Ward (1966). Equivalent to Pooraka Formation||||||
4045|Christies Beach Formation|70660|5|Briefly described|p3, p10-p11, p29-p30|Late Pleistocene|Late Pleistocene|Also known as the Pooraka Formation. See also p32, p37, p40-p42, p46.||||Overlies the Ochre Cove Formation. Overlain by the Heatherdale Shale.||
4045|Christies Beach Formation|72450|6|Mentioned|Brochure, Brochure map|Quaternary|Quaternary|Originated from coalescing alluvial fans discharged by flooding events up to 100 000 years ago. Dips westwards at a low angle away from the Wllunga Fault. Besy exposed in cliffs at Sellicks Beach.|||||Reddish brown to chocolate-brown clay and loam with abundant discontinuous lenses of gravel containg pebbles of bedrock.|
4045|Christies Beach Formation|73188|5|Briefly described|[See comments]|Pleistocene|Pleistocene|St Vincent Basin, Willunga Embayment. Interpreted as distal sediments sourced from erosion of the rising Mount Lofty Ranges. Records the last significant uplift on a number of Adelaide's faults. p: 319-320, 337-338, 345-346, 349, 351, 358-359.||||Equivalent to Pooraka Formation.|Alluvial fans, clay, sand, gravel, and wind-blown sand; lacking ferruginous and siliceous induration.|
4120|Clayton River Silcrete|38602|6|Mentioned|Fig.2|||||||||
4120|Clayton River Silcrete|40926|6|Mentioned|p26|||Mention Table 3||||||
4120|Clayton River Silcrete|43094|5|Briefly described|p38|||||||||
4144|Clevedale Migmatite|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
4144|Clevedale Migmatite|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
4144|Clevedale Migmatite|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
4144|Clevedale Migmatite|22588|6|Mentioned|p85|||||||||
4144|Clevedale Migmatite|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
4144|Clevedale Migmatite|22771|5|Briefly described|Table12.2p45,47|||||||||
4144|Clevedale Migmatite|22857|5|Briefly described|p45 Tb. 12.2, p392 App.1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 425m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
4144|Clevedale Migmatite|22884|6|Mentioned|p41, p43 Fig. 3|||Geological province: Broken Hill Domain.  Correlates with Morialpa Migmatite in the Olary Domain.||||||26-MAR-09
4144|Clevedale Migmatite|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|22962|6|Mentioned|p74||Statherian|||||||
4144|Clevedale Migmatite|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Gandry Dam Gneiss (Mt Isa Maronan Supergroup) and lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
4144|Clevedale Migmatite|22965|6|Mentioned|Fig 1||Statherian|||||||
4144|Clevedale Migmatite|22966|6|Mentioned|Fig1||Proterozoic|Early rift stage of devlopment.||||||
4144|Clevedale Migmatite|22967|5|Briefly described|p25,6,39,41||Statherian|||||||
4144|Clevedale Migmatite|23025|6|Mentioned|Fig1p75|||||||||
4144|Clevedale Migmatite|23160|6|Mentioned|fig1|||||||||
4144|Clevedale Migmatite|23248|5|Briefly described|Fig2p169|||||||||
4144|Clevedale Migmatite|23347|6|Mentioned|p52|||Geological province: Broken Hill Domain. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
4144|Clevedale Migmatite|24307|5|Briefly described|p967 Fig. 2|Proterozoic|Proterozoic|||||||
4144|Clevedale Migmatite|38969|4|Described|p204|||||||||
4144|Clevedale Migmatite|39662|2|Defined|p411|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|39883|6|Mentioned|p380|||||||||
4144|Clevedale Migmatite|40290|6|Mentioned|Fig.2|||||||||
4144|Clevedale Migmatite|40822|6|Mentioned|Fig.2|||||||||
4144|Clevedale Migmatite|41093|4|Described|p251|||||||||
4144|Clevedale Migmatite|41145|6|Mentioned|Fig.4|||||||||
4144|Clevedale Migmatite|41630|5|Briefly described|p6|||Mention p65||||||10-OCT-06
4144|Clevedale Migmatite|42261|6|Mentioned|Fig 1 P530|||||||||
4144|Clevedale Migmatite|42537|6|Mentioned|Fig.2 P5|||||||||
4144|Clevedale Migmatite|42595|6|Mentioned|Fig. 2 P5|||||||||
4144|Clevedale Migmatite|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Clevedale Migmatite, NSW.||||||07-NOV-08
4144|Clevedale Migmatite|42897|5|Briefly described|Fig.3, P321|||||||||
4144|Clevedale Migmatite|42942|6|Mentioned|p17|||Of Willyama Supergroup.||||||11-JUN-08
4144|Clevedale Migmatite|43052|6|Mentioned|Fig.4.22|||||||||
4144|Clevedale Migmatite|43086|6|Mentioned|Fig.3|||||||||
4144|Clevedale Migmatite|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43572|6|Mentioned|Fig.3.2 p6|||||||||
4144|Clevedale Migmatite|43583|5|Briefly described|Table 1, p2139|||||||||
4144|Clevedale Migmatite|46598|5|Briefly described|p303|||||||||
4144|Clevedale Migmatite|50045|5|Briefly described|p116 Fig. 3, p114 Fig. 1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Thorndale Composite Gneiss.||||||31-MAY-07
4144|Clevedale Migmatite|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Metasedimentary pelitic to psammitic migmatite.  Geological Province: Broken Hill Block.||||||07-NOV-08
4144|Clevedale Migmatite|60485|5|Briefly described|p28 Fig. 2|||Not of the Thackaringa Group. Geological Province: Broken Hill Domain.||||||23-JUN-08
4144|Clevedale Migmatite|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||18-MAY-06
4144|Clevedale Migmatite|61735|5|Briefly described|p635 Fig. 1, p653|Paleoproterozoic|Paleoproterozoic|Overlain by Thorndale Composite Gneiss. See also p636 Fig. 2.||||||30-JUN-09
4144|Clevedale Migmatite|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological province: Olary Domain.||||||
4144|Clevedale Migmatite|62535|6|Mentioned|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||||||
4144|Clevedale Migmatite|62536|5|Briefly described|p635-636, 653|||Broken Hill area.||||Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
4144|Clevedale Migmatite|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
4144|Clevedale Migmatite|63102|5|Briefly described|p13-15|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
4144|Clevedale Migmatite|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
4144|Clevedale Migmatite|63866|5|Briefly described|p36||||c. 1710 Ma (Max. deposition)|Willyama Supergroup||||
4144|Clevedale Migmatite|64097|5|Briefly described|p303, p325|Paleoproterozoic|Paleoproterozoic|Underlies Thorndale Composite Gneiss. Geological province: Broken Hill Domain/Curnamona province. Partially melted metasediments with or without albitic alteration.||||||07-FEB-11
4144|Clevedale Migmatite|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-FEB-11
4144|Clevedale Migmatite|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
4144|Clevedale Migmatite|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Underlies Thorndale Composite Migmatite. Geological province: Broken Hill Domain. Comprises partially melted clastic metasediments distinguished by thin layers or laminae of albitised metasediments; magnetite-bearing.G55||||||07-FEB-11
4144|Clevedale Migmatite|64743|6|Mentioned|p339 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
4144|Clevedale Migmatite|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Broken Hill Domain. High-grade metasedimentary rocks.||Unit in Willyama Supergroup.||Overlies Redan Gneiss. Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
4144|Clevedale Migmatite|65681|6|Mentioned|p734 Fig.1.|||Broken Hill Block.||||||
4144|Clevedale Migmatite|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |ca. 1710 (U-Pb zircon)|Thackaringa Group||Overlain by the Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|70000|5|Briefly described|p34-35|Statherian|Statherian|Among the oldest outcropping units in the Broken Hill Domain. Protolith was relatively sandy shallow marine sedimentary rocks with a possible evaporitic or hypersaline component represented by albitic horizons.||Unit in Thorndale Composite Gneiss.|||Metasedimentary gneiss and migmatite +/- albitic horizons hosting ubiquitous sills and dykes of basic gneiss.|
4144|Clevedale Migmatite|70014|5|Briefly described|Map legend|||Bedding extensively disrupted and mainly thin and discontinuous.||Unit in Willyama Supergroup.||Is overlain by Thorndale Composite Gneiss.|Mainly migmatite to quartzo-feldspathic composite gneiss (commonly leucocratic). Minor basic gneiss and vey rare, thin, plagioclase-quartz rock and medium-grained biotite-rich quartzo-feldspathic gneiss.|
4144|Clevedale Migmatite|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thorndale Composite Gneiss.|||Migmatite to migmatitic composite gneiss; minor basic gneiss, rare plagioclase-quartz rock and biotite-rich quartzofeldspathic gneiss.|
4144|Clevedale Migmatite|70657|5|Briefly described|p10 Fig.4, p12, p13 Fig.6, p15, p34|Statherian|Statherian|Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|> ~1705 Ma|Thorndale Composite Gneiss (Thackaringa Group ).||Overlies Redan Gneiss.||
4144|Clevedale Migmatite|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
4144|Clevedale Migmatite|72461|6|Mentioned|p16 fig 9|||||||||
4144|Clevedale Migmatite|73243|6|Mentioned|p52 Fig.1, p53 Fig.2 p59|||Broken Hill block-Euriowie block. Some amphibolite bodies appear to transgress bedding, interpreted as dykes emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Willyama Supergroup|||Contains amphibolite dykes.|
4144|Clevedale Migmatite|73308|6|Mentioned|p607 Fig.1|||||Willyama Supergroup.||||
4144|Clevedale Migmatite|73482|6|Mentioned|p422 Fig.3|||||Thorndale Composite Gneiss||||
4144|Clevedale Migmatite|73512|6|Mentioned|p7|||||Willyama Supergroup||||
4144|Clevedale Migmatite|73524|6|Mentioned|p5 Fig.3|||||Thackaringa Group||||
4144|Clevedale Migmatite|73575|6|Mentioned|p828 Fig.2, p829 Fig.3|||||Thorndale Composite Gneiss||||
4157|Clifton Formation|22674|5|Briefly described|Fig.2 p719|Early Miocene|Early Oligocene|||||||
4157|Clifton Formation|22875|5|Briefly described|p65|Early Miocene|Early Oligocene|Heytesbury Group.||||||24-JUL-08
4157|Clifton Formation|22944|5|Briefly described|Fig3|||||||||
4157|Clifton Formation|23230|5|Briefly described|Table4-1p40||Oligocene|||||||
4157|Clifton Formation|23249|5|Briefly described|p147 Fig.2||Late Oligocene|Equivalent to middle Gambier Limestone. Plankton fossil assemblage is the age determinant. In the Otway Basin.||||||16-MAY-13
4157|Clifton Formation|23307|5|Briefly described|Map Legend|Miocene|Miocene|Of Heytesbury Group||||||
4157|Clifton Formation|23322|5|Briefly described|957 Fig.2|Late Oligocene|Late Oligocene|Of the Heytesbury Group. Geological Province: Otway Basin.||||||07-SEP-09
4157|Clifton Formation|23402|3|Fully described|p32, p31 fig. 18, p7 Tb. 1|Miocene|Miocene|Thickness: 15m. Geological Province: Otway Basin.||||||24-JUL-08
4157|Clifton Formation|23768|5|Briefly described|p28 Fig.5, p69|Early Miocene|Early Miocene|Geological Province: Otway Basin.  See also p78 Fig. 22, p81.||||||11-SEP-09
4157|Clifton Formation|24056|5|Briefly described|p84 Fig. 2|Miocene|Oligocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
4157|Clifton Formation|24551|5|Briefly described|p246, 304|Miocene|Oligocene|Of the Heytesbury Group.||||||
4157|Clifton Formation|24562|5|Briefly described|p8 Fig. 2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
4157|Clifton Formation|29823|5|Briefly described|p14|||||||||
4157|Clifton Formation|29856|6|Mentioned|p36|||||||||
4157|Clifton Formation|30576|5|Briefly described|Table 2|||||||||
4157|Clifton Formation|30578|5|Briefly described|p12|||||||||
4157|Clifton Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4157|Clifton Formation|30675|5|Briefly described|p253|||Lithology & radioactivity||||||
4157|Clifton Formation|30932|6|Mentioned|Map legend|Miocene|Oligocene|Part of Gellibrand Marl. Oligocene-Miocene.||||||19-SEP-18
4157|Clifton Formation|31036|1|Redefined|p211|Oligocene|Oligocene|See also p199, 209, Table 9-1. Unit of Heytesbury Group.||||||04-APR-07
4157|Clifton Formation|31372|6|Mentioned|Fig. 2|||||||||
4157|Clifton Formation|31396|6|Mentioned|p1185|||||||||
4157|Clifton Formation|31424|4|Described|p14|||Description is from a core.||||||
4157|Clifton Formation|31625|6|Mentioned|Fig. 5.2|||Oligocene - Miocene||||||
4157|Clifton Formation|31922|6|Mentioned|Fig.2|||||||||
4157|Clifton Formation|32120|6|Mentioned|p279|||Oligocene fauna.||||||19-SEP-18
4157|Clifton Formation|32220|6|Mentioned|p9|||||||||
4157|Clifton Formation|32852|6|Mentioned|Fig. 2|||||||||
4157|Clifton Formation|33155|4|Described|p122|||||||||
4157|Clifton Formation|33229|6|Mentioned|p246|||||||||
4157|Clifton Formation|33940|6|Mentioned|p414|||||||||
4157|Clifton Formation|34954|6|Mentioned|Fig.35|||||||||
4157|Clifton Formation|35066|3|Fully described|p210|||Described p222.||||||04-APR-07
4157|Clifton Formation|35274|6|Mentioned|p423|||||||||
4157|Clifton Formation|36305|6|Mentioned|p358|||||||||
4157|Clifton Formation|36913|6|Mentioned|p81|||||||||
4157|Clifton Formation|38444|6|Mentioned|p302|||||||||
4157|Clifton Formation|38625|6|Mentioned|Table 2|||||||||
4157|Clifton Formation|41016|5|Briefly described|Table 1|||||||||
4157|Clifton Formation|41185|6|Mentioned|Fig.4|||||||||
4157|Clifton Formation|41269|5|Briefly described|p246|||||||||
4157|Clifton Formation|41398|6|Mentioned|p3|||||||||
4157|Clifton Formation|41639|5|Briefly described|p11|||||||||
4157|Clifton Formation|41642|6|Mentioned|Fig.8.6|||||||||
4157|Clifton Formation|41701|6|Mentioned|Map legend|Oligocene||||||||
4157|Clifton Formation|41704|6|Mentioned|Fig.3|||||||||
4157|Clifton Formation|41714|6|Mentioned|Fig.2|||||||||
4157|Clifton Formation|41726|6|Mentioned|Fig.5|||||||||
4157|Clifton Formation|41769|4|Described|p30|||||||||
4157|Clifton Formation|41868|5|Briefly described|p578|||||||||
4157|Clifton Formation|42079|6|Mentioned|Fig.2 p264|||See also Fig.10, p272||||||19-SEP-18
4157|Clifton Formation|42318|6|Mentioned|Fig.2 p10|||||||||19-SEP-18
4157|Clifton Formation|42452|5|Briefly described|Map legend|early Miocene|late Oligocene|||||||
4157|Clifton Formation|42453|4|Described|p17|||Superseded Kawarren limestone in 1974.||||||
4157|Clifton Formation|42524|5|Briefly described|Fig.3 P27|||||||||
4157|Clifton Formation|42635|6|Mentioned|p91|||||||||
4157|Clifton Formation|42827|3|Fully described|p284|||||||||
4157|Clifton Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
4157|Clifton Formation|43171|6|Mentioned|5-8|||Of Heytesbury Group. Age: 15-30Ma||||||
4157|Clifton Formation|43208|5|Briefly described|map legend|Early Miocene|Late Oligocene|Of Heytesbury Group.||||||
4157|Clifton Formation|43590|4|Described|p24|Early Miocene|Early Oligocene|||||||
4157|Clifton Formation|43604|6|Mentioned|p145|||||||||
4157|Clifton Formation|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
4157|Clifton Formation|43702|6|Mentioned|p407|Miocene|Oligocene|||||||
4157|Clifton Formation|43733|6|Mentioned|Fig.2.11,p65|Miocene|Oligocene|||||||
4157|Clifton Formation|43744|6|Mentioned|Fig.3,p3|||||||||
4157|Clifton Formation|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
4157|Clifton Formation|46802|6|Mentioned|Table 1|||||||||
4157|Clifton Formation|48581|14|Not recorded|p14|||||||||
4157|Clifton Formation|48911|6|Mentioned|Chart 1|||Correlation||||||
4157|Clifton Formation|50154|5|Briefly described|p135|||Of Heytesbury Group.||||||
4157|Clifton Formation|50371|5|Briefly described|Map Legend|Tertiary|Tertiary|Swamp and strand-line deposits; quartz, sand, clay and calcarenite.||||||11-JUN-04
4157|Clifton Formation|60421|5|Briefly described|p417|Early Miocene|Late Oligocene|Of the Heytesbury Group.||||||
4157|Clifton Formation|60538|5|Briefly described|p471 Fig. 10|||||||||
4157|Clifton Formation|60563|6|Mentioned|p47|||||||||
4157|Clifton Formation|60581|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60582|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60583|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60584|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60585|4|Described|p30|Early Miocene|Late Oligocene|Of the Heytesbury Group. Disconformably overlain by the Gellibrand Marl. Medium to coarse grained sandy calcarenite.||||||
4157|Clifton Formation|60785|5|Briefly described|p184 Fig.1, pp188-189.  |Chattian|Chattian|Eastern margin of Port Campbell Embayment, Otway Basin. Below unnamed nodule horizon, shell Sr/Sr age of 27.4 Ma (Holdgate and Gallagher, 2003). Sr/Sr age of 24.0 Ma immediately above the nodule layer. Foraminifera zone P21b-P22. Has yielded well-preserved isolated fossil cetacean elements: teeth, ribs and bone fragments.|||||Medium coarse-grained calcarenite, with about 10% quartz and limonite sand. At the Kawarren quarry, consists of friable, pale yellow limestone interbedded with harder crystalline bands. All fossils from the more friable calcarenite layers.|
4157|Clifton Formation|61155|5|Briefly described|p3, p18|Early Miocene|Late Oligocene|Of the Heytesbury Group. Coals and clastics deposits. Overlain by Gellibrand Marl. Max. thickness: 90m. Geological Province: Gippsland Basin and Otway Basin (Tyrendarra and Port Campbell Embayments).||||||25-JUN-13
4157|Clifton Formation|61182|3|Fully described|p28, p26, p33|Early Miocene|Early Oligocene|Of Heytesbury Group. Formerly Clifton beds. Calder River Limestone (Aire district) is incorporated. Disconformable over Narrawaturk Marl and Demons Bluff Fm; grades up into Gellibrand Marl. Medium to coarse-grained calcarenite, bryozoans, shell fragments.||||||04-FEB-08
4157|Clifton Formation|61623|6|Mentioned|p449 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|61624|5|Briefly described|p465, p466, p466 Fig. 2, p467, p471|Oligocene|Oligocene|Of Haytesbury Group. Overlain by Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||16-MAY-13
4157|Clifton Formation|61626|6|Mentioned|p486 Fig. 2|Miocene|Oligocene|Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|61628|5|Briefly described|p509 Fig. 3|Early Miocene|Early Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|62896|6|Mentioned|p88|||||||||07-FEB-11
4157|Clifton Formation|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||Heytesbury Group.||||
4157|Clifton Formation|63740|5|Briefly described|p88|||Geological province: Otway Basin.||||||07-FEB-11
4157|Clifton Formation|65316|5|Briefly described|p598,603|Aquitanian|Chattian|Thought to be a correlative of the Point Addis Limestone and Jan Juc Marl; in the Otway Basin. Age from strontium isotope stratigraphy on forams.| 27.8  - 22.4 Ma.|Basal unit of the Heytesbury Group.||||23-APR-12
4157|Clifton Formation|65715|5|Briefly described|p14 Tb.8|Miocene|Oligocene|Of Heytesbury Group.||||||
4157|Clifton Formation|66002|4|Described|p12, p13 Tb.9, p16, p26 Fig.7, p69-74|Neogene|Neogene|Of Heytesbury Group. Defined by Glenie 1971. Impure limestone. Outcrops around the Glenaire flats. Calcarenite, generally medium- to coarse-grained fragments of bryozoans, molluscs and echinoids, minor quartz and limonite sand. Moderately well bedded. Cementation variable||||||
4157|Clifton Formation|66012|3|Fully described|p17-18|Oligocene|Oligocene|Of Heytesbury Group. Littoral to shallow-marine sandy unit. Overlain by Gellibrand Marl. Laterised quartz sand, fossiliferous calcarenite, and brown sandy and silty clay. Strandline deposits. Up to 15m thick| | ||||13-JUN-13
4157|Clifton Formation|66245|5|Briefly described|p6 Fig.5. |Burdigalian|Rupelian|||Unit in Heytesbury Group.||Is overlain by Gellibrand Marl.||
4157|Clifton Formation|67061|6|Mentioned|p546 Fig.3.|Oligocene|Oligocene|||Unit in Heytesbury Group.||||
4157|Clifton Formation|67366|5|Briefly described|p103 Fig.2. |Oligocene|Oligocene|||Unit in Heytesbury Group.||Unconformably overlies Narrawaturk Marl. Is overlain by Gellibrand Marl.|Shallow marine calcareous sandstone and limestone.|
4157|Clifton Formation|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
4157|Clifton Formation|68116|5|Briefly described|Appendix, Maps 39-40, 49, 55.|Miocene|Oligocene||||||Calcarenite: generally medium to coarse grained, fragments of bryozoans, molluscs and echinoids, minor quartz and limonite sand; moderately bedded, alternating poorly and well-cemented beds; shallow marine and minor beach and near shore deposits.|
4157|Clifton Formation|68991|5|Briefly described|p465, p465 Fig.2|Miocene|Oligocene|Lower Miocene minimum age. < 20 m thick and of shallow-marine origin.|||||Comprises medium- to coarse-grained calcarenite.|
4157|Clifton Formation|69297|5|Briefly described|p79, p98|Chattian|Chattian|Otway Basin. ||Heytesbury Group||Unconformably overlies the Narrawaturk Marl, Upper. Overlain by the Gellibrand Marl.|Limestones.|
4157|Clifton Formation|69651|5|Briefly described|p10|Miocene|Oligocene|||Heytesbury Group.||Unconformably overlies Narrawaturk Marl, Mepunga and Demons Bluff Formations. Is overlain by Gellibrand Marl.||
4157|Clifton Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Oligocene|Oligocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Narrawaturk Marl. Is overlain by Gellibrand Marl.||
4157|Clifton Formation|70880|6|Mentioned|p77|Miocene|Oligocene|Otway Basin.||||||
4157|Clifton Formation|70942|4|Described|p126, 119|||||||||17-FEB-17
4157|Clifton Formation|71437|4|Described|Fig. 1 opp 154, p155, p160-161|Oligocene|Oligocene|of Baker (1953). Transgressive sand deposit.||Base of Heytesbury Group.||Sharp or transitional to overlying Gellibrand Marl.|Limonitic sandy limestone to glauconitic limestone, limonitic quartz sand.|
4157|Clifton Formation|73357|5|Briefly described|p30, p44, p46, p48|Chattian|Chattian|Otway Basin. Correlated with Proteacidites tuberculatus Spore-Pollen Zone and Operculodinium Dinocyst Superzone, nearshore to offshore marine depositional environments.||Of Heytesbury Group.||Overlies Narrawaturk Marl, underlies Gellibrand Marl.||
4157|Clifton Formation|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Oligocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P2 which has lower Ti/Cr values than the underlying or overlying packages. Lithologies based on geochemistry using the ChemLith classification includes calcareous limestone and calcareous sandstone, and using the Herron classification (1988) includes Fe-shale, Fe-sand. See also vi, p11 Tb.3.9, p34, p107, p117, p131, p137, p246, p258, p264.||Heytesbury Group||Overlies Nirranda Group, underlies Gellibrand Marl|Limestones.|
4157|Clifton Formation|73385|5|Briefly described|p5|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Narrawaturk Marl, underlies Gellibrand Marl.|Shallow to open marine limestones.|
4157|Clifton Formation|73386|4|Described|p4, p6, p14, Attachment A1|Chattian|Chattian|Otway Basin. Clastics in sandy facies around the margin of the basin supplied by rivers to the north and east. Depositional environment transitions from paralic coastal environments to high-energy outer shelf environments where clastic poor limestones were deposited in the south and west. Associated with the Middle Proteacidites tuberculatus Spore-Pollen Subzone.||Heytesbury Group||Overlies Narrawaturk Marl, Nirranda Group, underlies Gelilbrand Marl|Sandy limestone, which may be dolomitic or contain thin horizons of phosphate and limonite nodules, limestone and ferruginous sandy marl.|
4157|Clifton Formation|73486|6|Mentioned|p511 Fig.2, p516|Burdigalian|Chattian|Otway Basin.||Heytesbury Group||||
4157|Clifton Formation|73594|5|Briefly described|p4|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Underlies Gellibrand Marl|Marine limestones.|
4173|Clinton Formation|22541|6|Mentioned|p 12, 19, Fig 1|Miocene|Middle Eocene|||||||
4173|Clinton Formation|22587|6|Mentioned|p79 Fig.7|Early Oligocene|Middle Eocene|||||||
4173|Clinton Formation|23719|5|Briefly described|p28|||Formerly Clinton Coal Measures.||||||
4173|Clinton Formation|23802|5|Briefly described|p21 Fig. 2|||Carbonaceous clay, silt and sand with brown lignitic coal.||||||
4173|Clinton Formation|33057|5|Briefly described|p10|||Refers Harris (1966). Section.||||||
4173|Clinton Formation|33423|6|Mentioned|p22|||Strat. table.||||||
4173|Clinton Formation|36127|6|Mentioned|p9|||||||||
4173|Clinton Formation|36500|6|Mentioned|Fig.4|||||||||
4173|Clinton Formation|37324|6|Mentioned|p11|||||||||
4173|Clinton Formation|38107|4|Described|p24|||See also p18.||||||23-JUN-09
4173|Clinton Formation|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4173|Clinton Formation|40442|4|Described|p25|||||||||
4173|Clinton Formation|40453|5|Briefly described|p57|||Also mention on p57.||||||13-SEP-18
4173|Clinton Formation|41025|6|Mentioned|Fig.2|||||||||
4173|Clinton Formation|41513|6|Mentioned|p45|||||||||
4173|Clinton Formation|41517|6|Mentioned|Fig.5|||||||||
4173|Clinton Formation|41520|5|Briefly described|Fig.5|||||||||
4173|Clinton Formation|42498|5|Briefly described|Map legend|Eocene|Eocene|||||||
4173|Clinton Formation|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
4173|Clinton Formation|42574|6|Mentioned|Fig.2 P242|||||||||
4173|Clinton Formation|42733|5|Briefly described|map legend|Tertiary||||||||
4173|Clinton Formation|44133|4|Described|p164, 152 Fig. 10.2|Early Oligocene|Middle Eocene|Geological Province: Saint Vincent Basin. Overlain by South Maslin Sand. Thickness: >70m. Includes: Bumbunga Sand Member, Condowie Silt Member, Kooliata Coal Member. ||||||
4173|Clinton Formation|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Clastics and coals. Age: 45-~38.5Ma. Thickness: 60m. Geological Province: St Vincent Basin.||||||03-MAR-10
4173|Clinton Formation|61837|5|Briefly described|p216|Late Eocene|Late Eocene|Includes lenticular very-fine sands, clays and lignites. Geological Province: St Vincent Basin.||||||03-JUL-06
4173|Clinton Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Western St Vincent Basin. Age shown as Lutetian to Bartonian.||||||
4173|Clinton Formation|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle to Late Eocene in age (from Fig.2 - stratigraphic correlation chart).||||||
4173|Clinton Formation|66194|5|Briefly described|p584, p579, 593|Late Eocene|Late Eocene|Late Eocene. In Hope Valley Reservoir.||||||09-MAR-12
4173|Clinton Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eastern Saint Vincent Basin.||||||
4173|Clinton Formation|68715|6|Mentioned|p31 Fig.5|Eocene|Eocene|St Vincent Basin.||||||
4173|Clinton Formation|70660|6|Mentioned|p7, p11, p22||||||||Lignitic sedimentary rocks.|
4173|Clinton Formation|73188|5|Briefly described|p314, p320, p333|Middle Eocene|Middle Eocene|St Vincent Basin. Adelaide Plains, northern.|||||Glauconitic limestone[?].|
4311|Coladding granite|30518|6|Mentioned|p90|||Age 1580 m.y.||||||
4380|Colville Sandstone|22613|6|Mentioned|p21|||||||||
4380|Colville Sandstone|23768|5|Briefly described|p28 Fig.5, p73|Balcombian|Balcombian|Geological Province: Eucla Basin. See also p113.||||||11-SEP-09
4380|Colville Sandstone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
4380|Colville Sandstone|24347|5|Briefly described|p114|||||||||
4380|Colville Sandstone|30012|6|Mentioned|p20|||||||||
4380|Colville Sandstone|30268|6|Mentioned|p44|||||||||
4380|Colville Sandstone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
4380|Colville Sandstone|30952|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
4380|Colville Sandstone|30967|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
4380|Colville Sandstone|30974|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|31562|5|Briefly described|p13|||See also p10.||||||02-JUL-08
4380|Colville Sandstone|31636|6|Mentioned|p10|||||||||
4380|Colville Sandstone|31850|4|Described|p38|||Definition summary||||||
4380|Colville Sandstone|31902|4|Described|Table 1|||Lower  Miocene. Fig.1||||||02-JUL-08
4380|Colville Sandstone|31904|5|Briefly described|p8|||equiv. to gradation of Nullarbor limestone.||||||
4380|Colville Sandstone|31906|4|Described|p8|||Refers Lowry (1968). Table 1||||||
4380|Colville Sandstone|31914|6|Mentioned|p99|||Plate 10||||||
4380|Colville Sandstone|31915|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|32552|2|Defined|p10|early Miocene|early Miocene|See also p12, 36, 37, 40 etc.||||||02-JUL-08
4380|Colville Sandstone|32648|6|Mentioned|p32|||Miocene||||||
4380|Colville Sandstone|32750|4|Described|p306|||||||||
4380|Colville Sandstone|33586|4|Described|Table 1|||See also p15.||||||02-JUL-08
4380|Colville Sandstone|33587|6|Mentioned|p11|||||||||
4380|Colville Sandstone|33588|6|Mentioned|p11|||||||||
4380|Colville Sandstone|33589|4|Described|p12|||Middle Miocene||||||
4380|Colville Sandstone|33591|6|Mentioned|p10|||||||||
4380|Colville Sandstone|33592|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4380|Colville Sandstone|33595|4|Described|Table 1|||||||||
4380|Colville Sandstone|34742|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|35097|6|Mentioned|Fig.4|||||||||
4380|Colville Sandstone|35496|4|Described|Table 1|||Also on p22.||||||02-JUL-08
4380|Colville Sandstone|35772|6|Mentioned|p11|||||||||
4380|Colville Sandstone|36200|6|Mentioned|p15|||||||||
4380|Colville Sandstone|36701|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4380|Colville Sandstone|36890|3|Fully described|p416|||||||||
4380|Colville Sandstone|36902|6|Mentioned|p24|||||||||
4380|Colville Sandstone|38016|6|Mentioned|p92|||||||||
4380|Colville Sandstone|38482|6|Mentioned|p24|||||||||
4380|Colville Sandstone|38553|6|Mentioned|p43|||||||||
4380|Colville Sandstone|38602|6|Mentioned|p2|||||||||
4380|Colville Sandstone|39322|6|Mentioned|Fig.3|||||||||
4380|Colville Sandstone|42108|6|Mentioned|p322|||||||||
4380|Colville Sandstone|42265|6|Mentioned|p4|||? Replaced by Yarle Sandstone January 1990||||||
4380|Colville Sandstone|43065|5|Briefly described|p93|||||||||
4380|Colville Sandstone|44145|4|Described|p550 tab 4-27, p555,p556-7, p548|Early Miocene|Early Miocene|Northern margin Eucla Basin. Age from foraminifera fauna. Max known thickness 23m. Type section in creek 27 km west of Lake Colville.||||Grades laterally into Plumridge Formation (north) and Nullarbor Limestone (south).|Calcareous sandstone; lesser calcarenite, shale, siltstone and granule conglomerate.|08-OCT-15
4380|Colville Sandstone|44365|5|Briefly described|map legend||Early Miocene|||||||
4380|Colville Sandstone|44864|6|Mentioned|Map Legend||Miocene|||||||
4380|Colville Sandstone|45149|4|Described|p63|||See also Table 1, p16.||||||02-JUL-08
4380|Colville Sandstone|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Thin calcareous sandstone. Partly overlain and interfingers with Nullarbor Limestone. Age: 18.5-14.5Ma. Thickness: 25m. Geological Province: Eucla Basin.||||||03-MAR-10
4380|Colville Sandstone|62369|5|Briefly described|p410 Fig.4|Middle Miocene|Early Miocene|Geological Province: Eucla Basin||||||
4380|Colville Sandstone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Miocene|Miocene|Geological Province: Eucla Basin.||||||08-FEB-10
4380|Colville Sandstone|65942|2|Defined|p77-78|||Equal to Nullarbor Limestone.||Of Eucla Group.||||
4380|Colville Sandstone|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|Middle Miocene|Early Miocene|Eucla Basin. Up to 25m thick. Potential carbon dioxide storage reservoir.||||Equivalent to the Plumridge Formation. Grades into and interfingers with the Nullarbor Limestone.|Calcareous sandstone, minor siltstone, claystones and calcarenites.|
4380|Colville Sandstone|69648|6|Mentioned|p25|||Of Lowry (1968, 1970). A conceptually [Yarle Sandstone] equivalent sediment in the northwestern part of the Eucla Basin, is believed to be pre-Tertiary in age (Benbow, 1990b).||||||
4380|Colville Sandstone|70397|5|Briefly described|p2-3,12|Middle Miocene|Middle Miocene|Eucla Basin. Depositional environment: intertidal and supratidal; cool-temperate, open-marine shelf.||Unit of Eucla Group.||Underlain by Wilson Bluff Limestone. Laterally grades outboard (S-ward) into Nullarbor Limestone.||
4380|Colville Sandstone|70771|5|Briefly described|p5|||||||Grades laterally into (equivalent to) the Rawlinna Member.|Calcareous sandstones.|
4380|Colville Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, calcarenite, sandstone|
4380|Colville Sandstone|71361|5|Briefly described|p5, p18|Middle Miocene|Early Miocene|Eucla Basin. This unit is lithologically similar to the Nullarbor Limestone but with higher siliciclastic content.||||Equivalent to (grades into) the Nullarbor Limestone.||
4468|Coobowie Limestone|22766|5|Briefly described|Fig.2 p561|Middle Cambrian|Middle Cambrian|||||||
4468|Coobowie Limestone|23981|5|Briefly described|p23, p32|Early Cambrian|Early Cambrian|Ooidal to peloidal packstone, wavy bedded and nodular skeletal/peloidal wackestone, and nodular lime mudstone; thrombolites present. Conformably overlies Moonan Fm. Geol.Prov: Stansbury Basin (Yorke Peninsula) Presented only as Coobowie on p8-9 Fig. 4.||||||03-MAY-13
4468|Coobowie Limestone|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
4468|Coobowie Limestone|30374|6|Mentioned|Fig.3|||Middle Cambrian age. Correlation||||||
4468|Coobowie Limestone|33972|6|Mentioned|p13|||||||||
4468|Coobowie Limestone|35255|6|Mentioned|Fig.8|||||||||
4468|Coobowie Limestone|42222|6|Mentioned|Table 1 P4|||||||||
4468|Coobowie Limestone|42225|4|Described|p225|||||||||
4468|Coobowie Limestone|42269|6|Mentioned|Fig.1 P335|||||||||
4468|Coobowie Limestone|44133|5|Briefly described|p4 Fig. 7.2, 17, 28|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
4468|Coobowie Limestone|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Sandy, oolitic, fossiliferous limestone, minor calcareous siltstone and basal glauconitic sandstone. Geological Province: Stansbury Basin.||||||23-DEC-09
4468|Coobowie Limestone|61121|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Sandy, oolitic, fossiliferous limestone, minor calcareous siltstone and basal glauconitic sandstone; with small skeletal fossils and trilobite 'Pagetia'. Geological Province: Stansbury Basin.||||||23-DEC-09
4468|Coobowie Limestone|62787|5|Briefly described|p80, p82 Fig. 3|Middle Cambrian|Middle Cambrian|Geological Province: Stansbury Basin (SA).||||||07-FEB-11
4468|Coobowie Limestone|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Sandy, oolitic, fossiliferous limestone, minor calcareous siltstone and basal glauconitic sandstone. Small skeletal fossils and trilobite 'Pagetia'.||||||24-JUL-08
4468|Coobowie Limestone|65375|4|Described|p27 Fig.5, p31.|Cambrian|Cambrian|Contains first appearance of Pagetia sp. in the area.||||Overlies Moonan Formation. Is overlain by Yuruga Formation and Cape Jervis Formation.|Oolitic, fossiliferous limestone. Basal 1m thick glauconitic sandstone grades upwards into sandy, glauconitic, occasionally peloidal limestone. Upper part is medium-bedded, oolitic to silty with possible thrombolites.|
4468|Coobowie Limestone|65686|6|Mentioned|p411, 413|Middle Cambrian|Middle Cambrian|Stansbury Basin, Yorke Peninsula.||||||07-MAY-12
4468|Coobowie Limestone|65892|5|Briefly described|p9 Fig.4, p12. |Middle Cambrian|Middle Cambrian|Stansbury Basin, Yorke Peninsula. Contains Pagetia trilobites.||||Overlies Moonan Formation. Is overlain by Yuruga Formation. Correlative of Balcoracana Formation.||
4468|Coobowie Limestone|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Middle Cambrian|Middle Cambrian|Stansbury Basin.||||||
4468|Coobowie Limestone|68993|5|Briefly described|p544 Fig.1|Middle Cambrian|Middle Cambrian|Yorke Peninsula. Contains probable early Middle Cambrian fossils.||||Equivalent to the Balcoracana Formation.||28-JUL-15
4468|Coobowie Limestone|70382|5|Briefly described|p29 Fig 3|Cambrian|Cambrian|Yorke Peninsula region.|||||Limestone, silty, oolitic; basal glauconitic sandstone.|
4468|Coobowie Limestone|71102|6|Mentioned|p254|||Of Stansbury Basin.||||||
4468|Coobowie Limestone|73107|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Stansbury Basin.|||||Sandy, oolitic, fossiliferous limestone, minor calcareous siltstone and basal glauconitic sandstone. Small skeletal fossils and trilobite Pagetia. Subsurface only.|
4583|Coomandook Formation|23322|5|Briefly described|957 Fig.2|Pleistocene|Pliocene|Geological Province: Gambier Basin.||||||07-SEP-09
4583|Coomandook Formation|23818|5|Briefly described|p212 Fig.108, p213|Early Pleistocene|Early Pleistocene|Geological Province: Otway Basin. Overlying unit: Bridgewater Formation. Underlying unit: Parilla Sand.||||||
4583|Coomandook Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
4583|Coomandook Formation|29591|6|Mentioned|p92|||||||||
4583|Coomandook Formation|29697|6|Mentioned|p22|||||||||
4583|Coomandook Formation|29892|6|Mentioned|p79|||||||||
4583|Coomandook Formation|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See also Stratigraphic table p22. p24,28.||||||04-SEP-19
4583|Coomandook Formation|31241|4|Described|p101|||Lower Pleistocene||||||
4583|Coomandook Formation|32116|4|Described|p45|||||||||
4583|Coomandook Formation|32859|4|Described|p69|||L.Pleist.||||||
4583|Coomandook Formation|33566|6|Mentioned|p373|||See also p379.||||||01-NOV-22
4583|Coomandook Formation|33798|6|Mentioned|p98|||Fig.2||||||
4583|Coomandook Formation|34180|5|Briefly described|p212|||Lower Pleistocene.||||||
4583|Coomandook Formation|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4583|Coomandook Formation|34758|6|Mentioned|Table 1|||||||||
4583|Coomandook Formation|35066|6|Mentioned|p218|||||||||
4583|Coomandook Formation|35097|6|Mentioned|p123|||||||||
4583|Coomandook Formation|38068|6|Mentioned|p76|||||||||
4583|Coomandook Formation|38699|6|Mentioned|p29|||||||||
4583|Coomandook Formation|38932|4|Described|p99|||See also Fig.4||||||
4583|Coomandook Formation|39077|6|Mentioned|p27|||||||||
4583|Coomandook Formation|40003|5|Briefly described|p44|||See also Table 10||||||
4583|Coomandook Formation|41511|6|Mentioned|p24|||||||||
4583|Coomandook Formation|41520|5|Briefly described|Fig.12|||||||||
4583|Coomandook Formation|41599|6|Mentioned|p192|||||||||
4583|Coomandook Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
4583|Coomandook Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
4583|Coomandook Formation|42827|5|Briefly described|Fig 8.9|||||||||
4583|Coomandook Formation|42966|1|Redefined|p210|Early Pleistocene|Pliocene|||||||
4583|Coomandook Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Shallow marine, fossiliferous sandy limestone and calcareous sand.||||||25-MAY-05
4583|Coomandook Formation|43073|4|Described|p13,Table 4|||||||||
4583|Coomandook Formation|43195|5|Briefly described|Map Legend||Early Pleistocene|see also commentary on back of map.||||||
4583|Coomandook Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
4583|Coomandook Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
4583|Coomandook Formation|44133|5|Briefly described|p220-222|Early Pleistocene|Early Pleistocene|Maximum Thickness: 75m. ||||||
4583|Coomandook Formation|46839|6|Mentioned|Fig.3|||||||||
4583|Coomandook Formation|49038|4|Described|Table 2|||Briefly described P33||||||
4583|Coomandook Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Shelly and gravelly beach deposits.||||||
4583|Coomandook Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Marine strandline gravel and shellbeds.||||||
4583|Coomandook Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Overlies Whalers Bluff Formation; overlain by Bridgewater Formation. Geological Province: Otway Basin (Gambier Embayment).||||||03-MAR-10
4583|Coomandook Formation|63124|6|Mentioned|p93|||Unconformably overlies Green Point Member (Gambier Limestone). ||||||
4583|Coomandook Formation|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
4583|Coomandook Formation|68715|6|Mentioned|p31 Fig.5|Ionian|Zanclean|Murray Basin.||||||
4583|Coomandook Formation|69297|6|Mentioned|p79|Pleistocene|Pliocene|Otway Basin. ||||Unconformably overlies the Narracoorle Limestone Member. Unconformably overlain by the Bridgewater Formation.|Sandstone.|
4583|Coomandook Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Pleistocene|Pliocene|Otway Basin: Gambier Embayment and Voluta Trough.||||Overlies Gambier Limestone. Is overlain by Bridgewater Formation.||
4583|Coomandook Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Holocene|Pliocene|Gambier Embayment and Voluta Trough.||||Overlies Gambier Limestone (Heytesbury Group). Is overlain by Bridgewater Formation.||
4583|Coomandook Formation|73228|6|Mentioned|p50, p56-57, p59|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia.||||Unconformably underlain by Karoonda Surface.||
4583|Coomandook Formation|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
4595|Coombool Member|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
4595|Coombool Member|22799|3|Fully described|p21|Albian|Aptian|Monash Formation||||||
4595|Coombool Member|22857|5|Briefly described|p548 App.1 Tb.A1.12|Albian|Aptian|Of the Monash Formation. Green-grey chloritic volcanolithic siltstone, sandstone and shale. Max. thickness: >150m. Geological Province: Berri Basin. See also p350 Fig. 24.5.||||||
4595|Coombool Member|22887|4|Described|Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12. Renmark Trough||||||
4595|Coombool Member|22893|5|Briefly described|table5 fig4||Early Cretaceous|||||||
4595|Coombool Member|24551|6|Mentioned|p270|||Of the Monash Formation||||||
4595|Coombool Member|33488|2|Defined|p10|Early Cretaceous|Early Cretaceous|See also p11.||||||01-NOV-22
4595|Coombool Member|33490|4|Described|p10|||See also p25. Albian||||||01-NOV-22
4595|Coombool Member|35232|6|Mentioned|Table.2|||||||||
4595|Coombool Member|39211|6|Mentioned|p38|||Fig.23||||||
4595|Coombool Member|42966|1|Redefined|Table 7 p67|Albian|Aptian|of Monash Formation||||||
4595|Coombool Member|43052|5|Briefly described|Table 2.1|||of Monash Formation.||||||01-NOV-22
4595|Coombool Member|43218|4|Described|Fig.3,p22|Albian|Albian|Of Monash Formation,||||||
4595|Coombool Member|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
4595|Coombool Member|49038|5|Briefly described|p23|||||||||
4595|Coombool Member|49040|6|Mentioned|p8|||||||||
4595|Coombool Member|61314|5|Briefly described|p123, p129|Albian|Albian|Upper part of the Monash Formation. A terrestrial sequence of rocks - consisting of lithic sandstone, shale and siltstone. Overlies the Merreti Member. Geological Province: western Murray Basin.||||||
4595|Coombool Member|68189|6|Mentioned|p25, p33|Aptian|Albian|Of the Murray Basin.||Of the Monash Formation.||||
4595|Coombool Member|73228|5|Briefly described|p50-54|Early Cretaceous|Early Cretaceous|Berri Basin. Fluvial lacustrine depositional environment. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes. Distribution is more widespread than Pyap Member, overlapping older sediments and intervening basement ridges.||Monash Formation||Underlain by Merreti Member. Overlain by Warina Sand, Renmark Group.|Fluviolacustrine claystone and siltstone with minor interbeds of highly lithic sandstone.|
4595|Coombool Member|73229|5|Briefly described|p66-68, p70-72, p74|Early Cretaceous|Early Cretaceous|Berri Basin. [Analysed using pXRF; see article].||Monash Formation.|||Fluviolacustrine claystone and siltstone with minor interbeds of highly lithic sandstone.|01-NOV-22
4596|Coomunga Formation|23818|5|Briefly described|p226 Fig.121|Early Pleistocene|Early Pleistocene|||||||
4596|Coomunga Formation|34180|6|Mentioned|p226|||Lower Pleistocene.||||||
4596|Coomunga Formation|35772|6|Mentioned|p13|||||||||
4598|Coonambidgal Formation|2967|5|Briefly described|p40, 107|||Lawrence (1966, 1975). Murray Basin.|||||Brown and grey clays; a terrace with large wavelength meander scroll.|
4598|Coonambidgal Formation|10010|5|Briefly described|p16|Quaternary|Pliocene|Grades downwards into Calivil Formation  Geological Province: Murray Basin.||||||20-FEB-09
4598|Coonambidgal Formation|22531|5|Briefly described|p22|||||||||
4598|Coonambidgal Formation|22532|5|Briefly described|map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|22756|6|Mentioned|P39|||||||||
4598|Coonambidgal Formation|22782|6|Mentioned|p15|||||||||
4598|Coonambidgal Formation|22799|3|Fully described|p58|Holocene|Late Pleistocene|Age: <14 000 years BP.||||||21-MAY-08
4598|Coonambidgal Formation|22887|2|Defined|p47|Holocene|Holocene|||||||
4598|Coonambidgal Formation|22893|3|Fully described|p62,63 table3,11||Holocene|Unconsolidated. Broken up into older and younger alluvial terraces.||||||
4598|Coonambidgal Formation|23164|5|Briefly described|p16|||||||||
4598|Coonambidgal Formation|23166|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23167|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23168|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23169|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
4598|Coonambidgal Formation|23603|5|Briefly described|p12|||||||||
4598|Coonambidgal Formation|23604|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23605|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23606|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23607|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|23921|5|Briefly described|p1109 Table 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24103|6|Mentioned|p139 Fig.3|||||||||
4598|Coonambidgal Formation|24107|6|Mentioned|p224|||||||||
4598|Coonambidgal Formation|24133|6|Mentioned|p51|||Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24177|3|Fully described|p77|Recent|Recent|Defined by Lawrence (1966) from type locality in NSW. Disconformably overlies the Shepparton Formation. Geological Province: Murray Basin.||||||17-JUN-09
4598|Coonambidgal Formation|24178|6|Mentioned|p18|Devonian|Ordovician|||||||
4598|Coonambidgal Formation|24232|5|Briefly described|p226 Fig.2, p227|||||||||
4598|Coonambidgal Formation|24326|5|Briefly described|Map legend|Recent|Pleistocene|||||||
4598|Coonambidgal Formation|24439|5|Briefly described|p8, p18|Quaternary|Quaternary|Fluvial sediments of Lawrence (1966).  Diachronous with Shepperton Formation.  See also p47 Fig. 22, Appendix 2.||||||
4598|Coonambidgal Formation|24440|5|Briefly described|Map legend|||||||||
4598|Coonambidgal Formation|24551|5|Briefly described|p338 Fig. 11.2, 342|Holocene|Late Pleistocene|Of the Wunghnu Group.||||||
4598|Coonambidgal Formation|29860|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|29898|6|Mentioned|p213|||||||||
4598|Coonambidgal Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30750|6|Mentioned|p4|||||||||
4598|Coonambidgal Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30753|4|Described|p14|||Recent age||||||
4598|Coonambidgal Formation|30754|2|Defined|Fig.33|Recent|Recent|||||||
4598|Coonambidgal Formation|30755|6|Mentioned|p169|||Tectonic map||||||
4598|Coonambidgal Formation|30758|6|Mentioned|p66|||Riverine||||||
4598|Coonambidgal Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
4598|Coonambidgal Formation|30906|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30934|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30936|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30996|3|Fully described|p48|||Age discussed.||||||21-MAY-08
4598|Coonambidgal Formation|31654|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31713|5|Briefly described|p17|||||||||
4598|Coonambidgal Formation|31741|6|Mentioned|p6|||||||||
4598|Coonambidgal Formation|31742|5|Briefly described|p6|||Upper Cainozoic||||||
4598|Coonambidgal Formation|31745|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31746|6|Mentioned|p197|||||||||
4598|Coonambidgal Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|32007|6|Mentioned|Fig. 2|||||||||
4598|Coonambidgal Formation|32432|6|Mentioned|Fig.2|||Table 1||||||
4598|Coonambidgal Formation|34180|6|Mentioned|p212|||Recent||||||
4598|Coonambidgal Formation|34735|4|Described|p41|||Also mention p8||||||
4598|Coonambidgal Formation|34758|6|Mentioned|p27|||||||||
4598|Coonambidgal Formation|34986|6|Mentioned|p339|||||||||
4598|Coonambidgal Formation|35091|4|Described|p18|||||||||
4598|Coonambidgal Formation|35097|6|Mentioned|Fig.4|||||||||
4598|Coonambidgal Formation|35111|6|Mentioned|p2|||||||||
4598|Coonambidgal Formation|35174|6|Mentioned|p167|||||||||
4598|Coonambidgal Formation|35187|6|Mentioned|Table1|||||||||
4598|Coonambidgal Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
4598|Coonambidgal Formation|35232|5|Briefly described|Table.4|||||||||
4598|Coonambidgal Formation|35272|3|Fully described|p280|||||||||
4598|Coonambidgal Formation|37871|4|Described|p13|||||||||
4598|Coonambidgal Formation|37873|4|Described|p4|||||||||
4598|Coonambidgal Formation|37881|6|Mentioned|p16|||||||||
4598|Coonambidgal Formation|37882|4|Described|p7|||||||||
4598|Coonambidgal Formation|37883|6|Mentioned|p11|||||||||
4598|Coonambidgal Formation|37884|6|Mentioned|p14|||||||||
4598|Coonambidgal Formation|37885|5|Briefly described|p6|||||||||
4598|Coonambidgal Formation|38068|5|Briefly described|p79|||||||||
4598|Coonambidgal Formation|38879|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|39858|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|39860|5|Briefly described|p33|||||||||
4598|Coonambidgal Formation|40226|6|Mentioned|p51|||||||||
4598|Coonambidgal Formation|40522|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|41765|4|Described|p42|||||||||
4598|Coonambidgal Formation|41848|3|Fully described|p355|||Use of name has been varied. Here basal "Monoman Formation is not distinguished.||||||
4598|Coonambidgal Formation|41849|6|Mentioned|p409|||Age Pleistocene-Recent||||||
4598|Coonambidgal Formation|41868|6|Mentioned|p552|||||||||
4598|Coonambidgal Formation|42125|6|Mentioned|p139|||||||||
4598|Coonambidgal Formation|42128|5|Briefly described|p227|||See also Fig.2||||||
4598|Coonambidgal Formation|42184|6|Mentioned|Fig.2 P348|||||||||
4598|Coonambidgal Formation|42264|4|Described|p9|||See also Fig.3||||||
4598|Coonambidgal Formation|42454|5|Briefly described|p12|||Maximum age: 25 000BP.||||||20-OCT-08
4598|Coonambidgal Formation|42455|5|Briefly described|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|42827|3|Fully described|p356|||see also Table 9.1||||||
4598|Coonambidgal Formation|42966|1|Redefined|p276|Holocene|Late Pleistocene|Of Wunghnu Group.||||||13-AUG-07
4598|Coonambidgal Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|||||||25-MAY-05
4598|Coonambidgal Formation|43258|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43261|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43298|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43493|5|Briefly described|32-38|Recent|Pleistocene|Radiocarbon date: 25 000 years BP.||||||20-OCT-08
4598|Coonambidgal Formation|43655|5|Briefly described|p40-846|||||||||
4598|Coonambidgal Formation|44133|5|Briefly described|p254 Fig. 11.28|Holocene|Holocene|||||||
4598|Coonambidgal Formation|44185|5|Briefly described|Map legend.|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|44186|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44187|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44188|5|Briefly described|Map Legend|Holocene|Pleistocene|Geological province: Murray Basin. Fluvial/alluvial deposits.||||||20-OCT-08
4598|Coonambidgal Formation|44191|5|Briefly described|Map Legend|Holocene|Late Pleistocene|||||||
4598|Coonambidgal Formation|46909|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
4598|Coonambidgal Formation|60005|5|Briefly described|Map legend|Holocene|Holocene|Fluvial, lacustrine: clay, sand, sandy clay.||||||11-JAN-10
4598|Coonambidgal Formation|60452|4|Described|p41-42|Quaternary|Quaternary|Alluvial deposits.||||||
4598|Coonambidgal Formation|60461|5|Briefly described|Map legend|Pleistocene|Pleistocene|Alluvial flood plain and fan deposits, channel sands and clay playettes; clay, silt, fine to coarse-grained sand, gravel.||||||
4598|Coonambidgal Formation|60491|4|Described|p23|Quaternary|Quaternary|Deposited by modern day streams and consists of unconsolidated grey-brown silt, clay, gravel and sand.||||||22-NOV-04
4598|Coonambidgal Formation|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene| Alluvium of modern day streams and recent ancestors: sand, silt, clay.||||||30-SEP-04
4598|Coonambidgal Formation|60529|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||14-JUN-06
4598|Coonambidgal Formation|60591|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60592|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60593|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60595|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60596|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60597|5|Briefly described|Map Legend|Recent|Pliocene|Nonmagnetic with dendritic, moderately magnetic responses (10-20 nT) coinciding with present and prior streams; low K, Th, and variable U.||||||
4598|Coonambidgal Formation|60599|2|Defined|p24 Tb. 4, p95-96|Quaternary|Quaternary|Of Wunghnu Group. Includes Cobram Sand. Pale grey-brown silt +clay or fine- to coarse-g.qtz+ lithic sand, silt/clay; parts contain well-rounded qtz pebbles + ironstone fragments. Disconformable on Shepparton Formation; unconformable on Newer Volcanics. ||||||
4598|Coonambidgal Formation|60953|5|Briefly described|Map Legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||11-MAY-05
4598|Coonambidgal Formation|61108|5|Briefly described|map legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||
4598|Coonambidgal Formation|61163|5|Briefly described|p99, p109|||Term often used to include all the Quaternary alluvium in the Riverine Plains, but it is in fact a geomorphic unit and not primarily defined from its lithology.||||||
4598|Coonambidgal Formation|61185|2|Defined|p20 Fig. 5, p57, p64, p69-73|Recent|Pliocene|Of Lawrence (1966). Considered to now include Cobram Sand (Lawrence 1975). Deposits of existing streams cut into older Shepparton Formation sediments. Nonconformable on Strathbogie Granite. Actively deposited today.||||||07-FEB-11
4598|Coonambidgal Formation|61701|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61702|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61703|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61704|6|Mentioned|Map legend|Quaternary|Quaternary|From stream deposits derived from Strathbogie Granite; high K, variable Th; sediments deposited by the Goulburn River have moderate to high K, low Th.||||||12-FEB-15
4598|Coonambidgal Formation|61964|5|Briefly described|p143, p177|Quaternary|Quaternary|Of the Wunghnu Group. Associated with the Shepparton Formation. Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|64612|6|Mentioned|p56|||Name no longer used. Lawrence (1966).||||||07-FEB-11
4598|Coonambidgal Formation|65552|5|Briefly described|p2,p5-7,p12-13,p17,p19; p24,27 App.3,6 |Quaternary|Early Pliocene|Of Wanghnu Group. Poorly consolidated, mottled, variegated clay and silty lenses of sand and gravel. Hosts silica sand and minor clay deposits. With Shepparton Formation, overlies Calivil Formation and is the uppermost sequence in the Murray Basin.||||||
4598|Coonambidgal Formation|65715|6|Mentioned|p17|||Lapsed into disuse by GSV.||||||
4598|Coonambidgal Formation|65969|5|Briefly described|p27 Tb.3.3, p30|Quaternary|Quaternary|Fluvial mud and sand. Conformably overlies other units. Underlain by Karoonda Surface. Fills current river valleys and debouchments onto the Murray Valley. No magnetic response; mostly Th-rich but variable radiometric response, depending on source rocks.||||||
4598|Coonambidgal Formation|66002|6|Mentioned|p18|||Disused name. Use extended beyond type section and lithology, to all modern-day alluvial sediments N of Great Dividing Range, so GSV has dropped name.||||||
4598|Coonambidgal Formation|66287|6|Mentioned|p30 Fig. 8|Holocene|Pleistocene|||||||
4598|Coonambidgal Formation|67179|5|Briefly described|p580 Fig.1b, p581, 582|Holocene|Pleistocene|Laid down under arid climate by 'ancestral streams' that are precursors to current rivers in the region. See VandenBerg (1997d) and Macumber (1991).||||Conformably overlies the Shepparton Formation.||
4598|Coonambidgal Formation|68194|5|Briefly described|p24, p35|Holocene|Pleistocene|Butler (1958); Lawrence (1966). Channel and floodplain sediments, including alluvial sediments currently being deposited in the south of the map area. Appears as Coonambigil on p35.||||Overlies Shepparton Formation.||
4598|Coonambidgal Formation|68716|6|Mentioned|p39 Fig.3, p40|||||||Underlain by the Monoman Formation.||
4598|Coonambidgal Formation|69089|5|Briefly described|Map legend|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|70718|5|Briefly described|p25|||Alluvial fan formation. See also misspelling Coonabidgal Formation p23.||||Overlies Calivil Formation gradationally.||
4598|Coonambidgal Formation|70961|14|Not recorded|p133|||Refers to Lawrence (1966).||||||
4598|Coonambidgal Formation|73188|6|Mentioned|p320|Holocene|Holocene|Murray Basin.|||||Sand, clay, gravel, loam.|
4598|Coonambidgal Formation|73228|6|Mentioned|p62|Quaternary|Pliocene|||||||
4598|Coonambidgal Formation|73496|5|Briefly described|Map legend|Holocene|Pleistocene|[misspelt in map legend as Coornambidgal]||Wunghnu Group|||Nonmagnetic; high total count, K, Th, U; occupies regional topographic lows.|
4598|Coonambidgal Formation|73505|5|Briefly described|p2, p12-13|Quaternary|Quaternary|Murray Basin. Conformably overlies other units. Fills active river valleys. Often high K, Th radiometric response. No detectable magnetic response.|||||Fluvial mud and sand.|
4602|Coonarbine Formation|23154|6|Mentioned|Map Legend|Holocene|Pleistocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
4602|Coonarbine Formation|23155|5|Briefly described|p37|||Aeolian sediments. Type area is on FROME.  The unit intertongues with alluvial sediments of Strzelecki Creek.||||||
4602|Coonarbine Formation|30056|2|Defined|p146|early Recent|late Pleistocene|Late Pleistocene - Early Recent||||||
4602|Coonarbine Formation|30920|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4602|Coonarbine Formation|36620|5|Briefly described|Fig.1|||See also P24.||||||
4602|Coonarbine Formation|38605|6|Mentioned|p34|||||||||
4602|Coonarbine Formation|38682|6|Mentioned|p4|||||||||
4602|Coonarbine Formation|39085|6|Mentioned|p13|||||||||
4602|Coonarbine Formation|39804|6|Mentioned|Fig.2|||||||||
4602|Coonarbine Formation|40757|6|Mentioned|p76|||||||||
4602|Coonarbine Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4602|Coonarbine Formation|40926|6|Mentioned|Table 3|||||||||
4602|Coonarbine Formation|41125|5|Briefly described|Table 10|||||||||
4602|Coonarbine Formation|41537|6|Mentioned|Fig.2|||||||||
4602|Coonarbine Formation|42090|3|Fully described|p40|||||||||
4602|Coonarbine Formation|43053|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||25-MAY-05
4602|Coonarbine Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
4602|Coonarbine Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
4602|Coonarbine Formation|44133|5|Briefly described|p247, 244 Table 11.3|Holocene|Pleistocene|Maximum Thickness: 50m. ||||||
4602|Coonarbine Formation|46815|6|Mentioned|p250|||Refers to type sections.||||||
4602|Coonarbine Formation|46833|6|Mentioned|Fig.2|||||||||
4602|Coonarbine Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials in interdunal areas.||||||28-APR-05
4602|Coonarbine Formation|61108|5|Briefly described|map legend|Quaternary|Quaternary|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials (including calcrete) in interdunal areas.||||||31-MAY-05
4602|Coonarbine Formation|61155|5|Briefly described|p17|Holocene|Pleistocene|Overlies the Eurinilla Formation. Age: <1.0Ma.  Geological Province: Tarkarooloo Basin.||||||03-MAR-10
4602|Coonarbine Formation|65925|5|Briefly described|p18.|Holocene|Pleistocene|Youngest unit in Callabonna Sub-basin. Up to 50m thick. Aeolian cross-beds; longitudinal dunes to 15m high and wind-eroded claypans. Older dunes contain calcareous paleosols and more clay than younger dunes.|||||Aeolian sands of red-coated, frosted quartz grains, yellow to orange grains, clay pellets and gypsum flakes.|
4602|Coonarbine Formation|66131|6|Mentioned|p240, p247|Holocene|Pleistocene|Linear dunes of Late Pleistocene to Holocene age. Strzelecki Desert. Called Simpson Sand in Simpson Desert.||||Equivalent to Simpson Sand.||
4602|Coonarbine Formation|66518|6|Mentioned|p19 Fig.4.|Cenozoic|Cenozoic|Lake Eyre Basin.||||Overlies Eurinilla Formation and equivalents, and Millyera Formation.||
4602|Coonarbine Formation|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. Transverse dunes. 'Badlands' erosional pattern. Locally burrowed, with land snail shells and Aboriginal artefacts.||||Interdigitates with Simpson Sand.|Loosely to moderately indurated, red-brown to yellow-brown silt to medium sand; unbedded or with medium to small-scale cross-bedding; high percentage of clay pellets and gypsum grains; sometimes loosely cemented by carbonate palaeosols.|
4602|Coonarbine Formation|69019|5|Briefly described|p124.|Holocene|Pleistocene|Of Callen (1981). Aeolian sand in longitudinal or transverse dunes and interdune sand sheets.|||||Red-brown to yellow-brown and siliceous; subangular to subrounded frosted grains from silt to medium-sand sizes, usually with ferruginous coating; loosely cemented by regolith carbonate.|
4602|Coonarbine Formation|69023|5|Briefly described|p131-132, p140|Pleistocene|Pleistocene|Of Callen (1981). Aeolian sand in longitudinal or transverse dunes and interdune sand sheets. Mis-spelt as Coonabine on p140.|||||Sand grains are siliceous, frosted, fine-grained, rather poorly sorted, subangular to subrounded, and tend to have a ferruginous coating.|
4602|Coonarbine Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
4602|Coonarbine Formation|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Abundant clay parna and gypsum yields eroding "badlands" terrain. The burrowed paleosols contain land snail shells and Aboriginal artefacts.|||||Siliceous silt to medium sand, unbedded or with medium- to small-scale cross-bedding, loosely to  moderately indurated, red-brown to yellow-brown; transverse dunes. Local loosely cemented-carbonate burrowed paleosols.|
4602|Coonarbine Formation|72456|5|Briefly described|Map Legend|Holocene|Pleistocene|Marree 1:250k map sheet.|||||Dune sand, red coated, frosted quartz grains, yellow to orange, clay pellets, gypsum flakes. Aeolian.|
4602|Coonarbine Formation|72457|6|Mentioned|p91|Holocene||Callabonna Sub-basin. Aeolian deposits and Holocene palaeobeach ridges.||||||
4602|Coonarbine Formation|73251|6|Mentioned|p36, p62|Cenozoic|Cenozoic|Lake Eyre Basin, Callabonna Sub-basin / Poontana Trough. Thermally sub-mature. Depositional environments include aeolian dune fields and regolith.||||Underlain by Eurinilla Formation and Millyera Formation.||
4603|Coonatto Member|29780|6|Mentioned|p51|||||||||
4616|Coonigan Formation|12066|5|Briefly described|p13|Cambrian|Cambrian|||||||
4616|Coonigan Formation|22671|5|Briefly described|Table1p833,Fig2p837||Middle Cambrian|Of the Gnalta Group. Shale, limestone, sandstone.||||||17-JAN-06
4616|Coonigan Formation|22857|5|Briefly described|p90 Fig. 14.7B|Middle Cambrian|Early Cambrian|Of the Gnalta Group. White shale; limestone, shale, sandstone. Max. thickness: 115m. Geological Province: Mount Wright Block. See also p404 App. 1 Tb. A1.4||||||
4616|Coonigan Formation|22858|6|Mentioned|Fig14.7bp90-1|||||||||
4616|Coonigan Formation|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4616|Coonigan Formation|30908|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Lower Middle Cambrian. Part of Gnalta Group.||||||23-DEC-09
4616|Coonigan Formation|31507|6|Mentioned|p181|||||||||
4616|Coonigan Formation|31705|6|Mentioned|p27|||||||||
4616|Coonigan Formation|32948|4|Described|p110|||Re. fossil locality.||||||11-SEP-07
4616|Coonigan Formation|34469|6|Mentioned|p109|||Lower & Middle Cambrian. Gnalta Group.||||||27-NOV-08
4616|Coonigan Formation|34889|6|Mentioned|Fig. 2|||Also P117||||||
4616|Coonigan Formation|38692|6|Mentioned|p139|||||||||
4616|Coonigan Formation|39214|4|Described|p10|||||||||
4616|Coonigan Formation|40136|6|Mentioned|p34|||||||||
4616|Coonigan Formation|40455|6|Mentioned|Fig.2|||||||||
4616|Coonigan Formation|40642|6|Mentioned|p169|||See also P171 and P174||||||
4616|Coonigan Formation|41109|6|Mentioned|p184|||||||||
4616|Coonigan Formation|41810|6|Mentioned|Fig.3|||||||||
4616|Coonigan Formation|42070|6|Mentioned|p4|||||||||
4616|Coonigan Formation|42206|4|Described|p257|||See also Fig.1||||||
4616|Coonigan Formation|43192|5|Briefly described|p64||Middle Cambrian|Of Gnalta Group.||||||11-SEP-07
4616|Coonigan Formation|43501|14|Not recorded|Map Legend|Middle Cambrian|Early Cambrian|(Provisional Edition) Part of Cinaltra Group.||||||27-NOV-08
4616|Coonigan Formation|43502|14|Not recorded|Map Legend||Middle Cambrian|(Provisional Edition) Part of Gnalta Group (Lower Middle Cambrian).||||||23-DEC-09
4616|Coonigan Formation|43704|6|Mentioned|p67|||||||||
4616|Coonigan Formation|44133|5|Briefly described|p28|Templetonian|Templetonian|||||||
4616|Coonigan Formation|47035|6|Mentioned|p89|||||||||
4616|Coonigan Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Bancannia Shelf. NSW.  Contains fauna of Ordian age.||||||
4616|Coonigan Formation|60990|5|Briefly described|p81-82 |Middle Cambrian|Middle Cambrian|||Gnalta Group. ||Disconformably overlies the Cymbric Vale Formation.||
4616|Coonigan Formation|62787|5|Briefly described|p81, p82 Fig. 3|||Includes First Discovery Limestone Member. Unconformably underlain by Cymbric Vale Formation.||||||07-FEB-11
4616|Coonigan Formation|63489|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Shale with minor limestone.||||||
4616|Coonigan Formation|63789|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Gnalta Group. Shale and siltstone with minor limestone.||||||
4616|Coonigan Formation|63793|5|Briefly described|p23.|Middle Cambrian||At least 113 m thick. Contains trilobites and brachiopods.||Top unit in Gnalta Group. ||Overlies Cymbric Vale Formation.|Shales, siltstones and limestones.|
4616|Coonigan Formation|64671|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Gnalta Group.  Shale with minor limestone.||||||
4616|Coonigan Formation|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Of the Gnalta Group. Sahel and siltstone with minor limestone; abundant trilobite, brachiopod and algal fossils.||||||27-NOV-08
4616|Coonigan Formation|64680|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Gnalta Group. Shale with minor limestone.||||||
4616|Coonigan Formation|66623|3|Fully described|pp56-58, pp61-65, p144. |Middle Cambrian|Middle Cambrian|Defined by Warris (1967). Formerly part of lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934). Ordian-early Templetonian. Stratigraphic equivalent of Pincally and Wydjah Formations. Thickness >130 m. Outcrops very poorly. Contains trilobites in upper shale and siltstone, and oncolites in the lower.||Unit in Gnalta Group.|Includes First Discovery Limestone Member.|Disconformably overlies Cymbric Vale Formation. Is unconformably or disconformably overlain by Nuchea Conglomerate.|White to very light brown shale and interbedded siltstone, massive-style bedding.|
4616|Coonigan Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.||Overlies Cymbric Vale Formation.|Shale and siltstone with minor limestone.|
4616|Coonigan Formation|66929|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian||||||Shale; minor limestone.|
4616|Coonigan Formation|67322|4|Described|p5, p8-9, p28; Fig.5|Middle Cambrian|Early Cambrian|Of Warris (1967). Age from upper Ordian trilobites. Occurs in the Mount Wright-Mutawintji region. Underlies the Delamerian unconformity.||Topmost unit of the Gnalta Group.|First Discovery Limestone Member|Disconformably overlies Cymbric Vale Formation.|Basal limestone and shale, overlain by fossiliferous limestones, and c.14 m of white micaceous shale at the top which contains a diverse trilobite fauna.|21-FEB-18
4616|Coonigan Formation|69573|6|Mentioned|p656, 657, 659, 661, 670|||Gnalta Shelf. Features Cambrian Stage 5 fossil sites.||||||
4616|Coonigan Formation|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Koonenberry Belt.||Unit in Gnalta Group.||||
4616|Coonigan Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|||Gnalta Group|||Shale and siltstone with minor limestone.|20-JAN-22
4616|Coonigan Formation|70752|5|Briefly described|p127, p129, p131, p135, p139-140|||Koonenberry Belt. Linguliformean brachiopods have close affinity with those in Giles Creek Dolostone (NT).|||First Discovery Limestone Member.|||
4616|Coonigan Formation|70838|5|Briefly described|p269|Cambrian|Cambrian|Koonenberry Belt. Shown as lateral equivalent to First Discovery Limestone. Both overlie a tuff dated at 510 +/- 2.3 Ma.||Gnalta Group.|First Discovery Limestone.|Overlies Cymbric Vale Formation.||
4633|Coorabin Coal Measures|22773|5|Briefly described|Fig24.5p350|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|22857|5|Briefly described|p518 App.1 Tb.A1.9||Late Permian|Includes the Nowranie Creek, Loughmore and Narrow Plain Formations. Geological Province: Ovens Graben of the Tasman Epicratonic Province. See also p350 Fig.24.5..||||||
4633|Coorabin Coal Measures|22893|6|Mentioned|fig4 p9|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|23836|5|Briefly described|p93|Late Permian|Late Permian|Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|24551|6|Mentioned|p212|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|32315|6|Mentioned|Fig. 2|||||||||
4633|Coorabin Coal Measures|34418|5|Briefly described|p502|||||||||
4633|Coorabin Coal Measures|35498|3|Fully described|p142|||New units defined on P144||||||
4633|Coorabin Coal Measures|35767|6|Mentioned|p31|||||||||
4633|Coorabin Coal Measures|36172|6|Mentioned|Appendix|||||||||
4633|Coorabin Coal Measures|36329|6|Mentioned|p62|||||||||
4633|Coorabin Coal Measures|37065|6|Mentioned|p35|||||||||
4633|Coorabin Coal Measures|37101|4|Described|p261|||||||||
4633|Coorabin Coal Measures|38293|4|Described|p20|||||||||
4633|Coorabin Coal Measures|39929|6|Mentioned|p276|||||||||
4633|Coorabin Coal Measures|40324|6|Mentioned|p53|||||||||
4633|Coorabin Coal Measures|40520|6|Mentioned|Fig.5|||||||||
4633|Coorabin Coal Measures|41226|6|Mentioned|Table 1|||||||||
4633|Coorabin Coal Measures|42454|6|Mentioned|p19|||Oaklands Basin.||||||
4633|Coorabin Coal Measures|42547|5|Briefly described|p83|||||||||
4633|Coorabin Coal Measures|42648|5|Briefly described|p39|||||||||
4633|Coorabin Coal Measures|42966|4|Described|p64|||||||||
4633|Coorabin Coal Measures|43218|5|Briefly described|p27||Late Permian|Ovens Graben.||||||
4633|Coorabin Coal Measures|43841|4|Described|8||Late Permian|Unconformable over Urana Fm, unconformable under Jerilderie Fm. Mostly coal that totals up to 20m.||||||
4633|Coorabin Coal Measures|44340|14|Not recorded|p.3,4||Permian|I/55-14.||||||
4633|Coorabin Coal Measures|44341|14|Not recorded|map legend||Permian|Shale and mudstone with coal sandstone bands.||||||
4633|Coorabin Coal Measures|49040|6|Mentioned|p12|||||||||
4633|Coorabin Coal Measures|61314|5|Briefly described|p128|Late Permian|Late Permian|Upward-fining sequence of conglomerate, sandstone, siltstone, mudstone, carbonaceous clay and coal. Overlain by the Jerilderie Formation. Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|69798|5|Briefly described|p4, p7, p11-18|Late Permian|Early Permian|Oaklands Basin. Seismic profiles. Late Permian. Fine-grained units in the upper part provide a seal for lower reservoirs. Fluvial-point bar depositional environment.|||Nowranie Creek, Loughmore, Narrow Plain, Formations.|Unconformably overlies the Urana Formation. Is overlain disconformably by Jerilderie Formation.||06-FEB-18
4633|Coorabin Coal Measures|70125|5|Briefly described|p396|Permian|Permian|Oaklands Basin. 80m thick.||||Overlies Urana Formation. Is overlain by Jerilderie Formation.||
4650|Coorong dolomite|30411|6|Mentioned|p.212.|||||||||
4650|Coorong dolomite|30412|6|Mentioned|p212|||||||||
4650|Coorong dolomite|33653|6|Mentioned|p589|||||||||
4650|Coorong dolomite|36015|6|Mentioned|p823|||See also P814,815.||||||
4658|Cootanoorina Formation|23054|5|Briefly described|p17,34||Early Cambrian|||||||
4658|Cootanoorina Formation|33523|4|Described|p20|||||||||
4658|Cootanoorina Formation|33525|2|Defined|p4|Devonian|Devonian|Prob. Devonian||||||
4658|Cootanoorina Formation|33971|6|Mentioned|Fig.18|||||||||
4658|Cootanoorina Formation|33976|6|Mentioned|Fig.2|||||||||
4658|Cootanoorina Formation|35149|5|Briefly described|Table.1|||||||||
4658|Cootanoorina Formation|36733|6|Mentioned|p13|||||||||
4658|Cootanoorina Formation|41276|5|Briefly described|p61|||||||||
4658|Cootanoorina Formation|41492|5|Briefly described|p158|||||||||
4658|Cootanoorina Formation|42723|6|Mentioned|map legend|Paleozoic||||||||07-NOV-08
4658|Cootanoorina Formation|43048|5|Briefly described|p14|||||||||
4658|Cootanoorina Formation|44133|5|Briefly described|p37, 4 Fig. 7.2|Late Carboniferous?|Early Paleozoic|Geological Province: Eastern Officer Basin. Maximum Thickness: 880m. ||||||07-NOV-08
4658|Cootanoorina Formation|44289|5|Briefly described|Map Legend||Early Cambrian|||||||
4658|Cootanoorina Formation|64783|6|Mentioned|p101|||Arckaringa Sub-Basin.||||||15-NOV-17
4658|Cootanoorina Formation|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em4.|||||Aeolian, fluvial and evaporitic to tidal sandstone to mudstone; marine limestone and dolomite.|
4658|Cootanoorina Formation|69946|6|Mentioned|p38|||||||Overlies Relief Sandstone. Is overlain unconformably by Boorthanna Formation.||
4658|Cootanoorina Formation|71342|6|Mentioned|Ch5 p38|Cambrian|Cambrian|Arckaringa Basin.||||||
4665|Copa Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 167m.||Sherbrook Group.||Unconformably overlies Eumeralla Formation. Is overlain by and abuts Waarre Formation.||
4665|Copa Formation|22932|6|Mentioned|22|||||||||
4665|Copa Formation|24314|5|Briefly described|p61.Fig.2|Turonian|Cenomanian|Geological Province: Otway Basin. Max. Thickness 167m. Of the Shipwreck Supergroup [should be Shipwreck Subgroup].||||||10-MAR-09
4665|Copa Formation|24562|5|Briefly described|p8 Fig. 2|Cenomanian|Cenomanian|Geological Province: Otway Basin.  Of the Shipwreck Sub-group.||||||
4665|Copa Formation|42361|2|Defined|p12, p18|Cenomanian|Albian|Age stated as Late Cretaceous (Late Albian to Cenomanian).||||||07-APR-09
4665|Copa Formation|42545|6|Mentioned|p19|||Otway Basin||||||
4665|Copa Formation|43171|6|Mentioned|5-8|||Of Sherbrook Group. Age: 95-100+Ma||||||
4665|Copa Formation|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
4665|Copa Formation|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
4665|Copa Formation|43744|6|Mentioned|Fig.3,p3|||||||||
4665|Copa Formation|43814|6|Mentioned|Fig.3,p115|||||||||
4665|Copa Formation|44133|5|Briefly described|p146|Cenomanian|Cenomanian|Underlies Waarre Sandstone. Thickness: 167m. Of the Sherbrook Group. Geological Province: Otway Basin. ||||||
4665|Copa Formation|61547|6|Mentioned|p461 Fig.2 |Turonian|Cenomanian|||Unit in Shipwreck Subgroup.||Is overlain by Waarre Sandstone.||
4665|Copa Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
4665|Copa Formation|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
4665|Copa Formation|63122|5|Briefly described|p17 Fig. 4.3|Cenomanian|Cenomanian|Of the Sherbrook Group. Unconformable over Eumeralla Formation. Max. thickness: 167m. Geological Province: Otway Basin. ||||||
4665|Copa Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p77|Cenomanian|Cenomanian|Of Morton (1990) - replacing part of Belfast Mudst.(Kopsen and Scholefield 1990). Later part of Waarre Fm. but here reinstated. Of Shipwreck Subgroup (Sherbrook Gp). Overlain by Waarre Sst; overlies Eumeralla Fm. Age:97-91Ma. Max.thick: 51m.In Otway Basin||||||
4665|Copa Formation|63129|5|Briefly described|p134|||Overlain by Waarre Sandstone. Geological Province: Otway Basin. Contains shales that act as seals.||||||30-JAN-08
4665|Copa Formation|63431|5|Briefly described|p677 Fig. 2|Turonian|Cenomanian|Of the Shipwreck Subgroup. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
4665|Copa Formation|67061|6|Mentioned|p546 Fig.3.|Turonian|Turonian|||Unit in Sherbrook Group.||||
4665|Copa Formation|69297|6|Mentioned|p79|Turonian|Cenomanian|Otway Basin. ||||Unconformably overlies the Eumeralla Formation. Overlain by the Waarre Formation.||
4665|Copa Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Late Cretaceous|Late Cretaceous|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||Sherbrook Group.||Overlies Eumeralla Formation. Is overlain by Waarre Formation.||
4665|Copa Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Turonian|Turonian|Gambier Embayment and Voluta Trough.||Sherbrook Group.||Overlies Eumeralla Formation. Is overlain by Waarre Formation.||
4673|Copley Quartzite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
4673|Copley Quartzite|23818|6|Mentioned|p59|||Equivalent of the Rhynie Sandstone.||||||
4673|Copley Quartzite|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Burra Group.  Quartzite, red sandstone, minor dolomite and shale.  Age is Torrensian.  Max. thickness: >1980m.  Overlain by Skillogalee Dolomite; underlain by Callana Beds.  Geological Province: Mount Painter Province.||||||
4673|Copley Quartzite|24484|5|Briefly described|p799 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
4673|Copley Quartzite|29656|4|Described|Table 1|||||||||
4673|Copley Quartzite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
4673|Copley Quartzite|30177|6|Mentioned|p64|||||||||
4673|Copley Quartzite|30801|6|Mentioned|p5|||Torrensian. P5-6 table only.||||||
4673|Copley Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
4673|Copley Quartzite|31539|6|Mentioned|Fig. 6|||||||||
4673|Copley Quartzite|32403|6|Mentioned|p93|||||||||
4673|Copley Quartzite|32720|6|Mentioned|Table 1|||||||||
4673|Copley Quartzite|32722|6|Mentioned|Fig.3|||Stromatolite||||||
4673|Copley Quartzite|32724|6|Mentioned|Fig.1|||Correlation||||||
4673|Copley Quartzite|34175|6|Mentioned|p36|||||||||
4673|Copley Quartzite|34268|6|Mentioned|p241|||U.Prot.||||||
4673|Copley Quartzite|34269|6|Mentioned|Table 1|||U.Prot.||||||
4673|Copley Quartzite|34535|6|Mentioned|p59|||Equiv. Rhynie Sst.||||||
4673|Copley Quartzite|35255|6|Mentioned|p37|||||||||
4673|Copley Quartzite|35328|6|Mentioned|p11|||||||||
4673|Copley Quartzite|36083|6|Mentioned|Table 1|||||||||
4673|Copley Quartzite|36137|6|Mentioned|p10|||Used to refer to both Copley quartzite & Wortupa quartzite.||||||
4673|Copley Quartzite|36733|6|Mentioned|Table 5|||See also P12.||||||
4673|Copley Quartzite|37461|6|Mentioned|Table 5.I|||||||||
4673|Copley Quartzite|37854|6|Mentioned|p7|||See also P15.||||||
4673|Copley Quartzite|38157|6|Mentioned|Table III|||||||||
4673|Copley Quartzite|38926|5|Briefly described|p33|||||||||
4673|Copley Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
4673|Copley Quartzite|40294|6|Mentioned|Table 1|||||||||
4673|Copley Quartzite|41400|6|Mentioned|p28|||||||||
4673|Copley Quartzite|41404|3|Fully described|p88|||||||||
4673|Copley Quartzite|41405|6|Mentioned|p126|||||||||
4673|Copley Quartzite|42222|6|Mentioned|Table 1 P5|||||||||
4673|Copley Quartzite|42779|5|Briefly described|Table 1 P287|||||||||
4673|Copley Quartzite|43011|6|Mentioned|Table 2,p12|||||||||
4673|Copley Quartzite|43052|5|Briefly described|p177|||||||||
4673|Copley Quartzite|62428|5|Briefly described|p351 Tb. 6||Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
4673|Copley Quartzite|65925|5|Briefly described|Appendix 2.||||||||Quartzite; siltstone.|
4673|Copley Quartzite|71237|14|Not recorded|p10|||||||||
4673|Copley Quartzite|71239|14|Not recorded|p4, p10|||||||||
4673|Copley Quartzite|71240|14|Not recorded|p6, p10|||||||Correlated with Rhynie Sandstone.||
4673|Copley Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p16, p20|Tonian|Tonian|LA-ICP-MS detrital zircon MDA of 1129+/-51 Ma is much older than the true depositional age.||Emeroo Subgroup||||
4714|Cordillo Silcrete|22912|6|Mentioned|34|||||||||
4714|Cordillo Silcrete|23155|6|Mentioned|p36|||From the Innamincka Dome on the eastern Innamincka map sheet.  Data from STRZELECKI suggest that this material could well be mainly late Tertiary, not Oligocene-Miocene as suggested by Wopfner (1974).||||||
4714|Cordillo Silcrete|24204|6|Mentioned|p270|Eocene|Eocene|Geological Province: Poolowanna Trough.||||||
4714|Cordillo Silcrete|38605|6|Mentioned|p35|||||||||
4714|Cordillo Silcrete|39322|6|Mentioned|p396|||||||||
4714|Cordillo Silcrete|40910|6|Mentioned|p17|||||||||
4714|Cordillo Silcrete|40911|6|Mentioned|Map legend|Oligocene|Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4714|Cordillo Silcrete|40926|3|Fully described|p25|||||||||
4714|Cordillo Silcrete|41098|5|Briefly described|p177|||||||||
4714|Cordillo Silcrete|42375|6|Mentioned|p21|||? Lake Eyre Basin. ? Oligocene.||||||
4714|Cordillo Silcrete|42469|5|Briefly described|p46|||used by Wopfner, 1978.||||||
4714|Cordillo Silcrete|42746|5|Briefly described|p19|||||||||
4714|Cordillo Silcrete|42905|5|Briefly described|p23, Fig 5.3|||||||||
4714|Cordillo Silcrete|44133|6|Mentioned|p202|||||||||
4714|Cordillo Silcrete|61836|5|Briefly described|p211||Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
4714|Cordillo Silcrete|65238|6|Mentioned|p6|Eocene|Eocene|||||||
4714|Cordillo Silcrete|65925|6|Mentioned|p139.|||||||||
4714|Cordillo Silcrete|66131|5|Briefly described|p242 Fig.2, p245, p249, p259|Oligocene|Eocene|Occurs in upper Cordillo Surface. Called Cordillo Silcrete Surface on p245. Developed over the Eyre Formation.||Of the Cordillo Surface.||Overlain by the Doonbarra Formation.||
4714|Cordillo Silcrete|66623|1|Redefined|p239, pp266-283.|Oligocene|Oligocene|Redefined and discussed in detail. Followed deep weathering of Eyre Formation and exists over much of inland Australia. Forms a resistant cap on escarpments, producing flat crests and mesas. More weakly silicified sandstones are mapped as Eyre Formation.||||Grades downwards into Eyre Formation. Locally overlain unconformably by Doonbara Formation. Forms capping over Winton Formation.|Variably siliceous, sheet-like bodies of silica-indurated sandstone and some conglomerate, now mainly comprising chalcedonic and locally opaline rocks; light grey to pale orange-brown.|05-JUN-13
4714|Cordillo Silcrete|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|19-SEP-11
4714|Cordillo Silcrete|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-SEP-13
4714|Cordillo Silcrete|67209|5|Briefly described|Map legend.|Paleogene|Paleogene|Two un-named sub-units with differing lithologies are mapped separately.||||Overlies Allaru Mudstone.|Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|69019|6|Mentioned|p118.|Miocene|Oligocene|Developed widely across northern and central SA.||||||
4714|Cordillo Silcrete|69023|6|Mentioned|p120|||See also Cordillo Surface (p108). Developed in the top of the Eyre Formation. Silcrete genesis and timing discussed in detail.||||||
4714|Cordillo Silcrete|69946|5|Briefly described|p29, p129|Oligocene|Oligocene|Caps Eyre Formation to produce prominent mesas. Gently folded and tilted during Early Oligocene. Reworked into the Mirackina Conglomerate.||||||
4714|Cordillo Silcrete|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|70648|5|Briefly described|Map Legend|Neogene|Paleogene||||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-JAN-22
4714|Cordillo Silcrete|70649|5|Briefly described|Map Legend|Neogene|Paleogene|2 un-named units: Light grey highly siliceous silcrete, conglomeratic in places; commonly columnar and massive. Pale brown to grey moderately siliceous silcrete with common relict sedimentary features including bedding and pebbles.|||Includes 2 un-named units.||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|71321|6|Mentioned|p65|Oligocene|Late Eocene|Of Eromanga Basin. Nomenclature after Wopfner (1974, 1978).||||||
4714|Cordillo Silcrete|71342|6|Mentioned|Ch5 p29, Ch5 p130|Oligocene|Eocene|Lake Eyre Basin. This unit was gently folded and tilted during the Oligocene.||||Overlies the Eyre Formation.||
4714|Cordillo Silcrete|73234|6|Mentioned|p13|Early Oligocene|Late Eocene|Correlated with the topographically high-lying silcrete surface named 'Tent Hill surface' by Twidale et al. (1970).||||||
4721|Coreena Member|12597|4|Described|p492 Tb.1, p493 Fig.2, p495 Fig.3|Albian|Albian|See also p498, p499. E Eromanga Basin. 50-200m thick. Fossil wood and worm burrows are common in the upper part of the sequence. Also equivalent to upper part of Bulldog Shale and lower part of Oodnadatta Formation.||Unit in Wallumbilla Formation.||Overlies Doncaster Member. Equivalent to Coorikiana Formation. Is overlain by Surat Siltstone.|Interbedded mudstone, siltstone, and fine-grained, thickly-bedded lithic sandstone which is commonly glauconitic and calcareous; belemnite coquinites and marine molluscs also recorded in this sequence.|
4721|Coreena Member|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||Of Wallumbilla Formation||||
4721|Coreena Member|22757|5|Briefly described|Table6,p11||Early Cretaceous|165 m. Wallumbilla Formation, Rolling Downs Group, Surat Basin.||||||
4721|Coreena Member|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of Wallumbilla Formation (Rolling Downs Group); in the Tibooburra area these rocks are included in Oornoo beds. Equivalent to Surat Siltstone (Surat Basin). Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p544 App.1 Tb.A1.12.||||||
4721|Coreena Member|22865|5|Briefly described|Table22.1p296-7|Albian|Aptian|||||||
4721|Coreena Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province. Maximum thickness <245 m.||||||
4721|Coreena Member|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group).  Geological Province: Great Australian Superbasin.||||||
4721|Coreena Member|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Wallumbilla Formation. Geological Province: Great Artesian Basin.||||||
4721|Coreena Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|24251|6|Mentioned|p245|||Parent: Wallumbilla Formation||||||
4721|Coreena Member|30024|6|Mentioned|p331|||||||||
4721|Coreena Member|30042|5|Briefly described|p5|||Faunas correlation.||||||
4721|Coreena Member|30691|4|Described|p17|||See also P21,Table 4,6. Lower -Upper Cretaceous||||||
4721|Coreena Member|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
4721|Coreena Member|30696|4|Described|Table 4|||Albian||||||
4721|Coreena Member|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30700|6|Mentioned|p28|||Lower Cretaceous age. Unit of Wallumbilla Formation||||||
4721|Coreena Member|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30853|6|Mentioned|p10|||Correlate in Wallumbilla Formation||||||
4721|Coreena Member|30854|4|Described|Table 4|||Lower Cretaceous.||||||
4721|Coreena Member|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31098|5|Briefly described|Table 1|||L.Cretaceous||||||
4721|Coreena Member|31116|4|Described|p43|||See also P44||||||
4721|Coreena Member|31208|6|Mentioned|Table 1|||See also Figs. 3, 5, 6, 7.||||||
4721|Coreena Member|31209|6|Mentioned|p159|||||||||
4721|Coreena Member|31376|6|Mentioned|Table 104|||||||||
4721|Coreena Member|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31430|6|Mentioned|p10|||L.Cretaceous. See also P11||||||
4721|Coreena Member|31432|4|Described|Table 1|||L.Cretaceous||||||
4721|Coreena Member|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32314|6|Mentioned|Fig. 4|||||||||
4721|Coreena Member|32796|6|Mentioned|p302|||||||||
4721|Coreena Member|32797|4|Described|Table 4|||Lower Cretaceous||||||
4721|Coreena Member|33016|6|Mentioned|p1|||On table||||||
4721|Coreena Member|33017|6|Mentioned|p5|||||||||
4721|Coreena Member|33070|4|Described|Table 2|||L.Cret.||||||
4721|Coreena Member|33071|6|Mentioned|p6|||L.Cret.||||||
4721|Coreena Member|33072|4|Described|Table 1|||||||||
4721|Coreena Member|33075|6|Mentioned|Table 1|||||||||
4721|Coreena Member|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33088|4|Described|Table 3|||Wallumbilla Fm.||||||
4721|Coreena Member|33090|4|Described|Table 4|||L.Cret.||||||
4721|Coreena Member|33091|5|Briefly described|p9|||Stratigraphy||||||
4721|Coreena Member|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
4721|Coreena Member|33182|6|Mentioned|p192|||||||||
4721|Coreena Member|33372|6|Mentioned|p20|||||||||
4721|Coreena Member|33414|6|Mentioned|p212,Tb.||Cretaceous|Part of Wallumbilla Formation.||||||
4721|Coreena Member|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
4721|Coreena Member|33449|4|Described|Table 1|||L.Cret.||||||
4721|Coreena Member|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33639|5|Briefly described|Table 2|||Wallumbilla Fm. L.Cret.||||||
4721|Coreena Member|33640|4|Described|Table 2|||L.Cret.||||||
4721|Coreena Member|33642|2|Defined|p144|Early Cretaceous|Early Cretaceous|Brief formal definition by Day 1967. Now part of Wallumbilla Formation. Underlain by Doncaster Member and overlain by Allaru Mudstone. Dominantly pelecypod fauna, basal has marine fossils. Lower part is Early Albian, upper part is possibly Middle Albian.||||||08-MAY-13
4721|Coreena Member|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|34613|4|Described|Table 4|||||||||
4721|Coreena Member|35793|6|Mentioned|Fig.3|||||||||
4721|Coreena Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
4721|Coreena Member|36251|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|36552|6|Mentioned|p61|||||||||
4721|Coreena Member|36571|6|Mentioned|p98|||See also Table 4.||||||
4721|Coreena Member|36581|6|Mentioned|p464|||||||||
4721|Coreena Member|37995|4|Described|p66|||||||||
4721|Coreena Member|38199|6|Mentioned|p426|||||||||
4721|Coreena Member|38226|6|Mentioned|Table 1|||||||||
4721|Coreena Member|38814|6|Mentioned|Table 1|||||||||
4721|Coreena Member|39070|4|Described|p365|||||||||
4721|Coreena Member|39211|5|Briefly described|Fig.3|||Correlation P11. See also Figs 7-9,11-16 etc.||||||
4721|Coreena Member|39212|4|Described|p18|||||||||
4721|Coreena Member|39215|6|Mentioned|p53|||||||||
4721|Coreena Member|39216|6|Mentioned|p56|||||||||
4721|Coreena Member|39478|6|Mentioned|Table 1|||||||||
4721|Coreena Member|39708|6|Mentioned|p478|||||||||
4721|Coreena Member|39847|5|Briefly described|p39|||||||||
4721|Coreena Member|39942|6|Mentioned|p468|||||||||
4721|Coreena Member|39989|4|Described|p424|||||||||
4721|Coreena Member|40199|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|40245|6|Mentioned|Table 2|||||||||
4721|Coreena Member|40249|6|Mentioned|p38|||Mention P41||||||
4721|Coreena Member|40687|3|Fully described|p418|||||||||
4721|Coreena Member|40801|6|Mentioned|p46|||See also P85||||||
4721|Coreena Member|40832|3|Fully described|p457|||||||||
4721|Coreena Member|40833|6|Mentioned|p468|||||||||
4721|Coreena Member|40926|6|Mentioned|Table 2|||||||||
4721|Coreena Member|41012|5|Briefly described|p137|||||||||
4721|Coreena Member|41064|6|Mentioned|p62|||||||||
4721|Coreena Member|41086|3|Fully described|p104, Fig.3|||||||||
4721|Coreena Member|41087|3|Fully described|p126|||||||||
4721|Coreena Member|41088|5|Briefly described|p141|||||||||
4721|Coreena Member|41117|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|41178|6|Mentioned|p242|||||||||
4721|Coreena Member|41198|6|Mentioned|Table 1|||||||||
4721|Coreena Member|41219|6|Mentioned|Fig.4|||||||||
4721|Coreena Member|41266|6|Mentioned|Fig.3|||||||||
4721|Coreena Member|42071|6|Mentioned|p117|||||||||
4721|Coreena Member|42429|5|Briefly described|p155|||||||||
4721|Coreena Member|42494|5|Briefly described|Table 1 P24|||||||||
4721|Coreena Member|42673|5|Briefly described|Fig.2, P184|||||||||
4721|Coreena Member|43008|5|Briefly described|map legend|||of Wallumbilla Formation||||||
4721|Coreena Member|43989|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
4721|Coreena Member|44082|6|Mentioned|p22,Tb.34||Albian|Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
4721|Coreena Member|44099|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
4721|Coreena Member|44374|14|Not recorded|p10-12||Cretaceous|Contains Aptian and Albian species. Aptian species, remanie (reworked) fossils from Doncaster Member. Basal part in early Albian time. Member of Wilgunya Formation.||||||
4721|Coreena Member|44414|14|Not recorded|p110-112,114||Cretaceous|Cretaceous correlation in Northern Eromanga Basin. Correlated with Ranmoor Member.||||||
4721|Coreena Member|45110|2|Defined|p119|middle Albian|middle Albian|See also Table 18, p24 & 43. Member of Wallumbilla Formation.||||||01-MAY-19
4721|Coreena Member|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
4721|Coreena Member|45145|6|Mentioned|Table 5|||||||||
4721|Coreena Member|46791|4|Described|p44|||||||||
4721|Coreena Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
4721|Coreena Member|46939|6|Mentioned|Fig.1|||||||||
4721|Coreena Member|46984|6|Mentioned|Table 1|||||||||
4721|Coreena Member|48920|3|Fully described|p60|||Lower Cretaceous age||||||
4721|Coreena Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
4721|Coreena Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
4721|Coreena Member|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Of Wallumbilla Formation. Overlies Doncaster Member. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|61312|5|Briefly described|p64, p67 Fig.E5|Albian|Albian|Of the Wallumbilla Formation. Siltstone and fine sandstone interbedded with mudstone of the Doncaster Member. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
4721|Coreena Member|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||Unit in Wallumbilla Formation.||Overlies Doncaster Member.||
4721|Coreena Member|63979|6|Mentioned|p48, Fig. 44|||Of Wallumbilla Formation. Overlies Doncaster Member.||||||07-FEB-11
4721|Coreena Member|64048|6|Mentioned|p72|Early Cretaceous|Early Cretaceous|Of the upper Wallumbilla Formation. Geological Province: Eromanga Basin.||||||07-FEB-11
4721|Coreena Member|64856|3|Fully described|p99-101|Albian|Albian|Named by Vine (1966); defined by Vine et al. (1967) with a type area at Coreena Station near Barcaldine. Top of Wallumbilla Formation, but originally defined in Eromanga Basin. Is overlain by Surat Siltstone. Siltstone with lesser mudstone and minor coal. Associated with palynofloral unit APK4, and in Eromanga Basin APK5 contains dinoflagellate assemblages equivalent to unit ADK19.| | ||||28-NOV-17
4721|Coreena Member|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.||Wallumbilla Formation.||Overlies the Doncaster Member. Underlies the Surat Siltstone||22-MAR-12
4721|Coreena Member|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation? Underlies the Surat Siltstone, overlies the Doncaster Member.||||||
4721|Coreena Member|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||Of Wallumbilla Formation?||||||
4721|Coreena Member|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation. Underlies the Surat Siltstone, overlies the Doncaster Member, Surat Basin||||||
4721|Coreena Member|65119|6|Mentioned|Fig 14 p 521|||Present in the Flinton 1 and MacIntyre 1 wells.||||||07-MAR-12
4721|Coreena Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
4721|Coreena Member|66623|3|Fully described|p239, p242, pp256-264.|Albian|Aptian|Formerly Tambo Formation (Rose et al. 1967), Oornoo Sandstone (Morton 1982), part of Oornoo Beds (Rose and Brunker 1969). Equivalent to Coorikiana Sandstone (SA) and Ranmoor Member (QLD). Sandy and calcareous units crop out moderately. Contains a very wide range of fossils and intense bioturbation. Matrix cement in sandstones is 40%-50% calcite. Nearshore deposition.||Unit in Wallumbilla Formation.||Gradationally overlies, and is disconformable over, Doncaster Member. Is gradationally overlain by Allaru Mudstone.|Fine- to medium-grained, calcareous and glauconitic, blue-grey (weathering to buff) sandstones; local cone-in-cone calcite and mudstone pebbles; large spherical concretions abundant; fibrous gypsum veins ubiquitous.|07-JUN-13
4721|Coreena Member|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Wallumbilla Formation||||
4721|Coreena Member|67133|5|Briefly described|p17|Early Cretaceous|Early Cretaceous|Shallow lagoon and swamp (regressive) deposits.||Wallumbilla Formation.||Overlies Doncaster Member.||
4721|Coreena Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Doncaster Member.|Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Doncaster Member of Wollumbilla Formation. Is overlain by Allaru Mudstone.|Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67784|6|Mentioned|p26, p28, p31|Albian|Albian|Age derived from Sr isotopic data. Mis-spelt as Coorena Member on p31.||Walumbilla Formation||Overlies Doncaster Member. Is overlain by Toolebuc Formation.||08-FEB-18
4721|Coreena Member|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Unit in Wallumbilla Formation.||Conformably overlies Doncaster Member.|Siltstone interbedded with mudstone and minor, very fine- to fine-grained lithic sandstone and thin coal seams.|
4721|Coreena Member|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||||
4721|Coreena Member|68206|6|Mentioned|p32|Albian|Albian|NE Eromanga Basin.||||||
4721|Coreena Member|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.||
4721|Coreena Member|68593|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.|Siltstone interbedded with mudstone and minor, very fine- to fine-grained lithic sandstone. Thin coal seams in places.|
4721|Coreena Member|68734|5|Briefly described|p218 Fig.2|Albian|Aptian|Eromanga Basin (NE). Marine to coastal paralic.||Of the Wallumbilla Formation.||||
4721|Coreena Member|69457|5|Briefly described|p41:3, 10|Early Cretaceous|Early Cretaceous|Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
4721|Coreena Member|69594|5|Briefly described|p519, p526, p528, p538, p550|Albian|Aptian|Eastern Eromanga, northern Surat Basins. Deposited during regression in shallow-marine coastal mudflats, lagoons and swamps. Modest fossil fauna.||Wallumbilla Formation.||Conformably overlies Doncaster Member. Is overlain by Toolebuc Formation and (conformably) the Surat Siltstone. Laterally equivalent to Ranmoor Member. Correlated with Styx Coal Measures.|Mudstone, siltstone, sandstone, minor coquinite, interbedded calcareous units and intraformational conglomerates.|
4721|Coreena Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Wallumbilla Formation||Overlies Doncaster Member||
4721|Coreena Member|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||Unit in Wallumbilla Formation.||||
4721|Coreena Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|Includes un-named unit.||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions. Un-named unit is grey to pale brown cone-in-cone limestone and calcareous mudstone.|
4721|Coreena Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Wallumbilla Formation|||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p31, p33, p72|Early Cretaceous|Early Cretaceous|See also p79-80, p82, p85-89, p115-116. Eromanga and Surat Basins. Varying thicknesses given (30-123m) from wells. Middle to Late Albian age. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrochemistry mentioned, hydrostratigraphic properties.||Wallumbilla Formation.||Conformably overlies Doncaster Member. Is overlain by Toolebuc Formation or Surat Siltstone. Equivalent to upper Bulldog Shale.|Labile sandstone, siltstone and mudstone, locally calcareous; locally coquinite.|
4721|Coreena Member|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Albian.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.||
4721|Coreena Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
4721|Coreena Member|71251|5|Briefly described|p11-12, p15, p17, p49, p51|||Eromanga Basin. Natural gamma wireline log. Conductivity diagram.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|71863|5|Briefly described|p5|Albian|Aptian|Eromanga Basin.||Wallumbilla Formation||Overlies the Doncaster Member. Overlain by the Toolebuc Formation.||
4721|Coreena Member|71864|6|Mentioned|p13-p14, p17|||Could not be distinguished in GSQ Eulo 2 borehole.||Wallumbilla Formation||||
4721|Coreena Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Wallumbilla FZ.||Overlies Doncaster Member. Is overlain by Toolebuc FZ.||
4752|Corrodgery Formation|22643|5|Briefly described|fig3p187, fig6|Early Cambrian|Early Cambrian|||||||
4752|Corrodgery Formation|23981|5|Briefly described|p8-9 Fig.4, p23|Toyonian|Toyonian|Calcareous red and green-grey, micaceous, feldspathic sandstone. Max. thickness: 85m. Geological Province: Stansbury Basin (Yorke Peninsula). Presented only as Corrodgery in figure.  See also p23-24.||||||
4752|Corrodgery Formation|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
4752|Corrodgery Formation|35255|6|Mentioned|Fig.8|||||||||
4752|Corrodgery Formation|36244|6|Mentioned|p2|||Refers Thomson et al.1976.||||||
4752|Corrodgery Formation|42222|6|Mentioned|Table 1 P4|||||||||
4752|Corrodgery Formation|42225|4|Described|p223|||||||||
4752|Corrodgery Formation|42269|6|Mentioned|Fig.1 P335|||||||||
4752|Corrodgery Formation|44133|5|Briefly described|p4 Fig. 7.2, 17|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
4752|Corrodgery Formation|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Dary grey to red-brown siltstone and fine-grained sandstone.  Geological Province: Stansbury Basin.||||||23-DEC-09
4752|Corrodgery Formation|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Dark grey to red-brown siltstone and fine-grained sandstone; siltstone with bioturbation and organic debris. Sandstone is cross-bedded with rip-up intraclasts. Geological Province: Stansbury Basin.||||||23-DEC-09
4752|Corrodgery Formation|65375|4|Described|p27 Fig.5, p28 Fig.6, p30. |Cambrian|Cambrian|Contains no skeletal fossils. Abundant acritarchs suggest correlation with Tempe Formation in Amadeus Basin.||||Overlies Ramsay Limestone. Is unconformably overlain by Stansbury Limestone.|Mainly massive, layered to laminated dark grey siltstone with bioturbation and occasional debris beds; upper part mainly massive, cross-bedded, graded sandstone with thin red-brown siltstone interlayers.|
4752|Corrodgery Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Ramsay Limestone. Is overlain by Stansbury Formation.||
4752|Corrodgery Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||||||
4752|Corrodgery Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
4759|Corundum Creek Schist Member|23411|6|Mentioned|Map Legend|||||||||
4759|Corundum Creek Schist Member|23818|6|Mentioned|p37|||||||||
4759|Corundum Creek Schist Member|24176|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of Freeling Heights Quartzite.  Geological Province: Mount Painter Province.||||||07-NOV-08
4759|Corundum Creek Schist Member|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4759|Corundum Creek Schist Member|30177|2|Defined|p124|Paleoproterozoic|Paleoproterozoic|Type section: Yudnamutana Creek, 2.8 miles south-southwest of Freeling Heights,
lat. 30degrees 11'01"S long. 139degrees22'08"E to lat. 30degrees 11'01"S long. 139degrees23'13"E.||||||24-NOV-22
4759|Corundum Creek Schist Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
4759|Corundum Creek Schist Member|34537|6|Mentioned|p37|||||||||
4759|Corundum Creek Schist Member|34726|6|Mentioned|p101|||||||||
4759|Corundum Creek Schist Member|35255|6|Mentioned|Fig.24|||||||||
4759|Corundum Creek Schist Member|65925|5|Briefly described|Appendix 2.||||||||Schist, sandy; quartzite; muscovite-biotite and corundum-spinel schists.|
4874|Crayfish Subgroup|22944|5|Briefly described|Fig3|||||||||
4874|Crayfish Subgroup|23911|4|Described|p93, p95 Fig. 9B|||Geological Province: Otway Basin.  Max. Thickness: >4500m. Underlain by Casterton Formation. Overlain by  Eumeralla Formation. Of the Otway Group.||||||14-APR-08
4874|Crayfish Subgroup|24453|4|Described|p808, p809 Fig.2|Hauterivian|Berriasian|Fluvial sandstones, conglomerates and minor silstones, coals, tuffs and basalt. Of Otway Group. Geological Province: Otway Basin.||||||07-FEB-11
4874|Crayfish Subgroup|24551|6|Mentioned|p245|||||||||
4874|Crayfish Subgroup|42361|4|Described|p4|||||||||
4874|Crayfish Subgroup|42545|5|Briefly described|Fig.4 P15|||||||||
4874|Crayfish Subgroup|43660|5|Briefly described|p14,Fig.6,p15||Early Cretaceous|||||||
4874|Crayfish Subgroup|43747|5|Briefly described|p5||Early Cretaceous|||||||
4874|Crayfish Subgroup|43814|6|Mentioned|Fig.3,p115|||||||||
4874|Crayfish Subgroup|50154|5|Briefly described|p44, p169|||Also known as Pretty Hill Formation. Of the Otway Group. Geological Province: Otway Basin.||||||24-AUG-04
4874|Crayfish Subgroup|61017|5|Briefly described|p5|Barremian|Bernasian|Of the Otway Group. Non-marine lacustrine to fluvial sediments. Unconformably overlain by Eumeralla Formation. Province: Otway Basin.||||||07-FEB-11
4874|Crayfish Subgroup|61182|6|Mentioned|p12|||May have superseded Crayfish Group?||||||18-FEB-08
4874|Crayfish Subgroup|61470|5|Briefly described|p28 Fig. 5|Barremian|Berriasian|Of the Otway Group.  Includes Pretty Hill and Laira Formations and the Katnook Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
4874|Crayfish Subgroup|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Includes Katnook Sandstone, Pretty Hill and Laira Formations. Geological Province: Otway Basin.||||||
4874|Crayfish Subgroup|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Otway Group.|Pretty Hill, Laira Formations; Katnook Sandstone.|||
4874|Crayfish Subgroup|65715|6|Mentioned|p10|||Includes conglomerate similar to Ballark Conglomerate.||||||
4874|Crayfish Subgroup|66245|5|Briefly described|p6 Fig.5, p42.|Barremian|Berriasian|Among the oldest sediments in the Otway Basin: locally-derived sands, and muds from a more distant source.||Unit in Otway Group.|Includes Pretty Hill and Laira Formations and Katnook Sandstone.|||
4874|Crayfish Subgroup|67367|5|Briefly described|p131 Fig.2, pp131-132. |Early Cretaceous|Early Cretaceous|Hydrocarbon source rocks, deposited in rifted half-grabens, for virtually all onshore hydrocarbons in South Australia. Assigned to the Austral 1 petroleum sub-system. ||Unit in Otway Group.|Includes Laira and Pretty Hill Formations, and Katnook Sandstone.|||
4874|Crayfish Subgroup|69297|6|Mentioned|p79|Aptian|Valanginian|Otway Basin. ||Otway Group|Includes the Casterton Formation, Sawpit Shale, Sawpit Sandstone, Pretty Hill Formation, Laira Formation and the Katnook Sandstone.|||
4874|Crayfish Subgroup|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Otway Group.|Pretty Hill, Laira Formations; Katnook Sandstone.|Unconformably overlies Casterton Formation. Is overlain unconformably by Eumeralla Formation.||
4874|Crayfish Subgroup|70077|5|Briefly described|Regional: Fig.4; p9|Early Cretaceous|Early Cretaceous|Otway Basin: Robe-Penola Trough. Source rocks of the Austral 1 Petroleum System.||Otway Group.|Sawpit Shale, Sawpit Sandstone, Pretty Hill and Laira Formations, Katnook Sandstone.|||
4874|Crayfish Subgroup|73356|6|Mentioned|p. v-2, p4, p11, p17, p29|||Otway Basin. Basal boundary is unconformable in many instances (cf. Warrong Trough) but is shown to be conformable in the Sawpit-1 well (Penola Trough).||Otway Group|Sawpit Formation, Pretty Hill Formation, Laira Formation, Katnook Sandstone|Underlain by Casterton Formation. Unconformably overlain by Windermere Sandstone.||
4874|Crayfish Subgroup|73357|6|Mentioned|p17, p43, p45, p47|Barremian|Berriasian|Otway Basin.||Otway Group|Includes Pretty Hill Formation|||
4874|Crayfish Subgroup|73383|4|Described|p3-4, p6, p7 Tb.3.1, p15-16, p25, p27|Barremian|Berriasian|Otway Basin. Approximately equivalent to chemostratigraphic Sequence S1, defined by generally higher Cr/Mg and lower Y/Nb and Ti/Cr values than the overlying Sequence S2. Significant lateral variation in lithology. May contain intra-formation unconformities based on large and abrupt geochemical changes. Lithologies based on geochemistry using the ChemLith classification includes mudstone, argillaceous and calcareous sandstone, limestone, calcareous limestone; and using the Herron classification (1988) includes shale, Fe-sand, Fe-shale, wacke, lith-arenite. See also vi, p1, p8, p11, p126-129, p253-256.||Otway Group|Pretty Hill Formation, Laira Formation, Katnook Sandstone|Overlies Casterton Formation, unconformably underlies Eumeralla Formation|Includes fluvial channel sandstones, lacustrine mudstones and alluvial sandstone. Both arkosic and lithic-rich.|
4874|Crayfish Subgroup|73385|5|Briefly described|p3, p5-6, p9, p12 Fig.4.9, p16|Barremian|Valanginian|Otway Basin. Deposited in predominantly NW-SE grabens and half-grabens of limited extent, deposition facilited by a series of lakes within individual depocentres, that became linked to a fluvio-lacustrine system. Crayfish Subgroup isopach grid used to define Early Cretaceous depocentres and highs. Location in text includes p15 Fig.4.13.||Otway Group|Laira Formation, Pretty Hill Formation, Katnook Sandstone|Overlies Casterton Formation, underlies Eumeralla Formation, Windermere Sandstone.|Includes fluvial channel sandstones, lacustrine mudstones and alluvial sandstone. Primarily comprised of locally derived sands and far-sourced muds.|
4874|Crayfish Subgroup|73386|4|Described|p1-2, p4-9, v, Attachment A1|Barremian|Berriasian|Otway Basin. Latest Berriasian maximum age. Conformable with Casterton Formation in the western Victorian Otway Basin, unconformable in the central basin. Primarily of fluvial and lacustrine depositional environments, syn-rift sequence and deposited in half grabens in the northern and western onshore Otway Basin. Limited available evidence suggests it is unlikely the Crayfish Subgroup is present offshore beyond areas adjacent to the coast. Corresponds to the Upper Ruffordiaspora australiensis to Upper Foraminisporis wonthaggiensis Spore-Pollen subzones of Partridge (2006), and the S1 chemostratigraphic sequence (Forbes et al., 2020).||Otway Group|Laira Formation, Pretty Hill Formation, Sawpit Formation, Katnook Sandstone|Overlies Casterton Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone, equivalent to the Crayfish Group in South Australia|Sequence of sandstones, siltstones and shales.|
4874|Crayfish Subgroup|73594|4|Described|p3-4, p36, p38, p41-46, p49-50, p52|Barremian|Berriasian|Otway Basin. Deposited in a series of half-grabens with the stratigraphy of each depocentre likely unique. Low-relief erosional surface forms the boundary with the Eumeralla Formation. Originally Crayfish Group (Kopsen and Scholefield (1990), renamed by Morton (1990) to Crayfish Subgroup and divided into four sub-ubits based on seismic character.||Otway Group|Katnook Sandstone, Pretty Hill Formation, Laira Formation|Overlies Casterton Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone|Fluvial channel sandstones, lacustrine mudstones and alluvial sandstones.|
4874|Crayfish Subgroup|75065|6|Mentioned|p157|||Otway Basin.||||Correlates with Tyers River Subgroup.||
4976|Cuddapan Formation|13497|4|Described|v, vi, xii, p65, p104, p112|Norian|Carnian|Cooper Basin. Originally defined by Powis (1989) and Channon and Wood (1989) who applied the name as a replacement to the informal Beanbush beds of Price et al. (1985). An unpublished type section was proposed by Channon and Wood (1989), however a published type section by Powis (1989) has precedence. Channon and Wood assigned a reference section in Paning 1. Maximum thickness of 67m in Beanbush 1. Sedimentary features and palaeoenvironment are briefly discussed. Reservoir characteristics discussed. See also p114-p115, p119, p157 tbl 10.1, p167, p168 fig 10.12.||Nappamerri Group||Equivalent to the Peera Peera Formation. Unconformably or disconformably overlies the Tinchoo Formation. Disconformably overlain by the Poolowanna Formation or the Hutton Sandstone.|Basal white sandstone, minor mudstone and interbeds of grey siltstone and coal interbeds.|
4976|Cuddapan Formation|13516|6|Mentioned|p171 fig 12|Late Triassic|Late Triassic|In Eromanga Basin.||||||
4976|Cuddapan Formation|22839|6|Mentioned|P33|Late Triassic|Middle Triassic|||||||
4976|Cuddapan Formation|22883|6|Mentioned|P29|||||||||
4976|Cuddapan Formation|23155|6|Mentioned|Fig 8 on p16|||Age uncertain, perhaps Triassic to Jurassic.||||||
4976|Cuddapan Formation|23375|4|Described|Fig2 p265||Norian|In the Eromanga Basin.||||||17-JAN-08
4976|Cuddapan Formation|24210|5|Briefly described|p133 Fig. 2|Early Jurassic|Late Triassic|||||||
4976|Cuddapan Formation|42008|2|Defined|p275|Rhaetian|Carnian|See also Fig.4, Fig.5, Fig.3. Paly zones APT4 and APT5. Found in Windorah Trough, Patchawarra Trough. Intended to replace all other Late Triassic units in the region including Beanbush Beds, Morney Beds, 'Upper Triassic Unit' and Lamdina Formation. Correlated with Peera Peera Formation, Poolowanna Trough, Simpson Desert Basin, and lower parts of the Leigh Creek Coal Measures.||||||09-APR-15
4976|Cuddapan Formation|42085|6|Mentioned|Fig.2 P374|||||||||
4976|Cuddapan Formation|42746|5|Briefly described|Fig.2 P4|||||||||
4976|Cuddapan Formation|43052|6|Mentioned|Table 2.1|||||||||
4976|Cuddapan Formation|43105|5|Briefly described|p14|||||||||
4976|Cuddapan Formation|44133|5|Briefly described|p65 Fig.8.3, 93, 86|Upper Triassic|Triassic|Geological Province: Cooper Basin. Unconformably overlies: Tinchoo Formation, Nappamerri Group. Overlain by Poolowanna Formation(u).||||||17-JAN-08
4976|Cuddapan Formation|60386|6|Mentioned|p299|Late Triassic|Late Triassic|Cooper/Eromanga Basin. Non-marine.||||||
4976|Cuddapan Formation|60717|5|Briefly described|p40 Fig. 2|Late Triassic|Carnian|Unconformable contacts with the Nappamerri Group below and Poolowanna Formation above. Floodplain and alluvial deposits.||||||17-JAN-08
4976|Cuddapan Formation|61613|6|Mentioned|p282 Fig. 2|Late Triassic|Late Triassic|Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
4976|Cuddapan Formation|61614|6|Mentioned|p290 Fig. 2|Late Triassic|Late Triassic|Geological Province: Simpson Basin.||||||17-MAR-09
4976|Cuddapan Formation|61615|6|Mentioned|p302 Fig. 2|Early Jurassic|Late Triassic|||||||07-FEB-11
4976|Cuddapan Formation|62730|5|Briefly described|p352 Fig. 1|Early Jurassic|Late Triassic|Geological Province: Eromanga Basin.||||||08-APR-08
4976|Cuddapan Formation|63978|5|Briefly described|p25|Late Triassic|Late Triassic|Overlies Gilpeppee Member of Tinchoo Formation in the Cooper Basin. Geological province: Eromanga Basin.||||||07-FEB-11
4976|Cuddapan Formation|63979|2|Defined|p30, Fig. 44|Rhaetian|Carnian|Unconformable on Gilpeppee Member (Tinchoo Fm) in Cooper Basin. Max. thickness:50m. Unconformably/disconformably overlain by Poolowanna Fm. Geol.prov: Eromanga Basin. Comprises lower sandstone and upper interbedded carbonaceous siltstone, mudstone + coal.||||||07-FEB-11
4976|Cuddapan Formation|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
4976|Cuddapan Formation|64197|6|Mentioned|p625 Fig.1c|Late Triassic|Late Triassic|Eromanga Basin.||||||
4976|Cuddapan Formation|64665|6|Mentioned|p53 Fig.2.|Late Triassic|Late Triassic|||||||
4976|Cuddapan Formation|65489|5|Briefly described|p48-49, p55, p96, p129, p132, p155|Late Triassic|Late Triassic|Eromanga Basin. Overlies Cooper Basin. Hydrocarbon source rock. Hosts an oil discovery, but no economic oil or gas fields discovered yet in SA.||||Is overlain unconformably by Poolowanna Formation.||
4976|Cuddapan Formation|66915|5|Briefly described|p6 Fig.3|Early Jurassic|Late Triassic|Eromanga Basin. Shown as Cuddapan Formation (upper) and Cuddapan Formation (lower).||||||
4976|Cuddapan Formation|68731|5|Briefly described|p200 Fig 3.110, pp207-211|Late Triassic|Late Triassic|Basal Eromanga Basin. Subdivided into upper and lower parts.||||Unconformably underlain by the Nappamerri Group, Tinchoo Formation and the Gilpeppee Member.||10-MAY-16
4976|Cuddapan Formation|69454|5|Briefly described|p38:4, 8-9|Rhaetian|Carnian|Eromanga Basin. Originally considered to be the uppermost unit in the Cooper Basin; reassigned to basal Eromanga Basin by Draper (2002).||||Correlated with Peera Peera Formation (Pedirka Basin).||12-JUL-16
4976|Cuddapan Formation|69457|5|Briefly described|p41:3|Late Triassic|Late Triassic|Eromanga and Cooper Basins.||||Is overlain unconformably by Poolowanna Formation.||12-JUL-16
4976|Cuddapan Formation|69594|5|Briefly described|p519, p524, p545, p572|Late Triassic|Late Triassic|Powis (1989). Eromanga Basin. Occurs in several isolated depocentres. 20-55m thick. Highly sinuous fluvial environment with overbank and coal swamp deposits locally. Distribution areas briefly discussed.||||Is overlain unconformably or disconformably by Poolowanna Formation. Equivalent to (upper) Peera Peera Formation.|Sublabile to quartzose sandstone in its lower part, with interbedded dark grey carbonaceous siltstone, mudstone and coal dominant in upper parts.|
4976|Cuddapan Formation|69673|6|Mentioned|p153 fig 125|||||||||
4976|Cuddapan Formation|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Eromanga Basin.||||||
4976|Cuddapan Formation|69797|5|Briefly described|p17 Fig.2|Late Triassic|Late Triassic|Age: Carnian - Rhaetian (approximated from figure).||||||
4976|Cuddapan Formation|69946|5|Briefly described|p9, p36, p51-52, p54|Late Triassic|Late Triassic|Northern Patchawarra Trough. Locally overlies Cooper Basin.||||Unconformably overlies Tinchoo Formation.|Sandstone; minor siltstone and coal.|
4976|Cuddapan Formation|69947|6|Mentioned|p13 Fig.7.2|Early Jurassic|Late Triassic|||||||
4976|Cuddapan Formation|70317|6|Mentioned|p33|Late Triassic|Late Triassic|||||Unconformably overlies Tinchoo Formation (Nappamerri Group).||
4976|Cuddapan Formation|70823|5|Briefly described|p33, p40, p43-p44, p75, p78-p79|Upper Triassic|Late Triassic|Cooper Basin. Deposited in floodplain or meandering fluvial environments. Formerly referred to as the Bluebush beds (Price et al., 1985).||||Unconformably overlies the Tinchoo Formation and the Nappamerri Group. Unconformably overlain by the Poolowanna Formation.||
4976|Cuddapan Formation|70824|5|Briefly described|p7, p9|Rhaetian|Rhaetian|Cooper Basin. Deposited as floodplain or meandering fluvial deposits.||||Unconformably overlies the Tinchoo Formation.||
4976|Cuddapan Formation|70946|5|Briefly described|p1087, p1089|Late Triassic|Late Triassic|Northern Patchawarra Trough. Overlies the Cooper Basin. Deposited in a floodplain and meandering fluvial environment.||||Unconformably overlies Tinchoo Formation.||08-OCT-18
4976|Cuddapan Formation|71342|5|Briefly described|Ch5 p9, Ch5 p30|Rhaetian|Carnian|North Patchawarra Trough, Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a meandering fluvial or floodplain environment. See also  Ch5 p36, Ch5 p52, Ch5 p54, Ch7 p13, Ch9 p11.||||Unconformably overlies the Tinchoo Formation. Unconformably overlain by the Poolowanna Formation.|Sandstone, minor siltstone and coal.|
4976|Cuddapan Formation|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin.||||||
4976|Cuddapan Formation|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.||||||
4976|Cuddapan Formation|73251|6|Mentioned|p62|Late Triassic|Late Triassic|Floodplain and meandering fluvial depositional environments. Hydrocarbon source rock with oil shows.||||||
4976|Cuddapan Formation|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin.||||||
4976|Cuddapan Formation|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Fluvial-unconformity depositional environment. Only present in local areas of the basin.|ca 210 Ma|||Unconformably overlies Tinchoo Formation, Nappamerri Group, unconformably underlies Poolowanna Formation||
5034|Cunyarie Granite|34537|6|Mentioned|Fig.7|||Carp.||||||
5034|Cunyarie Granite|66302|6|Mentioned|p46|Calymmian|Statherian|Igneous crystallisation age. Cleve domain|1598 +/- 7 Ma (SHRIMP, Fraser and Neumann, 2010)|||||23-AUG-18
5050|Curdlawidny Siltstone Member|42247|2|Defined|p5|Early Cambrian||Reserved as Curdlawidny||||||
5050|Curdlawidny Siltstone Member|42465|5|Briefly described|Map Legend|||||||||
5050|Curdlawidny Siltstone Member|42469|3|Fully described|p27|||||||||
5050|Curdlawidny Siltstone Member|44133|5|Briefly described|p24|||Of the Andamooka Limestone. Maximum Thickness: 22m. ||||||
5082|Currency Creek Formation|38290|2|Defined|p40|early Pleistocene|early Pleistocene|||||||
5082|Currency Creek Formation|65901|6|Mentioned|p176 Tab.1|||Of Maud (1972). Equivalent to Pooraka Formation||||||
5100|Cutana beds|22631|6|Mentioned|p177|||||||||
5100|Cutana beds|23351|5|Briefly described|283|||||||||
5100|Cutana beds|42223|6|Mentioned|Fig.2 P36|||||||||
5100|Cutana beds|42813|4|Described|p14|||Of Arkaroola Subgroup.||||||10-SEP-07
5100|Cutana beds|61239|6|Mentioned|p56|||Contains basal quartzite units.||||||
5100|Cutana beds|62724|5|Briefly described|p16, p17 Fig. 4|Willouran|Willouran|Of Arkaroola Subgroup (Callanna Group) mature quartz sandstone. Geological Province: Olary Domain/Curnamona Province (South Australia).||||||07-FEB-11
5100|Cutana beds|62993|5|Briefly described|p22, p30|Neoproterozoic|Neoproterozoic|Shown as Cutana Beds p30.||||Correlated with Arkaroola Subgroup|Clean quartzites, mafic igneous rocks and calc-silicates.|
5100|Cutana beds|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Arkaroola Subgroup. In the Radium Hill area.||||||10-SEP-07
5100|Cutana beds|65925|5|Briefly described|Appendix 2.||||||||Quartzite; schist; siltstone.|
5198|Daralingie Formation|13497|3|Fully described|iv, v, vi, xi, xii, p63, p69 fig 6.1|Kungurian|Kungurian|Cooper Basin. Originally the Daralingie beds of Gatehouse 1972 before Morton and Gatehouse (1985) raised it to formation status. Name derived from Daralingie Waterhole on Strzelecki Creek. A type section is given.  Maximum thickness of more than 100m in the Nappamerri Trough. Depositional environment and sedimentology is briefly discussed.  A cross section of where this unit contacts the Roseneath Shale is given on p99.  Reservoir characteristics discussed. See also p70, p93, p96, p99-p102, p119, p132, p146, p149, p157, p159, p161, p163-p164, p171, p175, p181-p182, p193, p204-p205.||Gidgealpa Group||Conformably overlies the Roseneath Shale. Unconformably overlain by the Toolachee Formation.|Light grey to black carbonaceous and micaceous siltstone and mudstone with interbedded light grey to brown fine to very fine-grained sandstone. Minor coal seams and carbonaceous partings and streaks occur.|
5198|Daralingie Formation|13516|6|Mentioned|p147, fig 5|Late Permian|Late Permian|From Cooper Basin||||||
5198|Daralingie Formation|22527|6|Mentioned|p 1|||||||||
5198|Daralingie Formation|22839|6|Mentioned|P33|||||||||
5198|Daralingie Formation|22883|6|Mentioned|P29|||||||||
5198|Daralingie Formation|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin. Of the Gidgealpa Group.||||||17-JAN-08
5198|Daralingie Formation|23155|4|Described|p22|Early Permian|Early Permian|Pollen and spores indicate an Early Permian age for the Formation.  On STRZELECKI the unit is overlain by Toolachee Formation (disconformity) and underlain by Roseneath Shale.||||||
5198|Daralingie Formation|23375|4|Described|Fig2 p265,285||Kungurian|Of Cooper Basin.||||||17-JAN-08
5198|Daralingie Formation|24199|5|Briefly described|p512 Fig. 2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
5198|Daralingie Formation|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Roseneath Shale.  Geological Province: Cooper Basin.||||||
5198|Daralingie Formation|33331|6|Mentioned|p40|||||||||
5198|Daralingie Formation|37287|6|Mentioned|p36|||||||||
5198|Daralingie Formation|40056|1|Redefined|p10|Early Permian|Early Permian|||||||
5198|Daralingie Formation|41288|6|Mentioned|p159|||||||||
5198|Daralingie Formation|42006|6|Mentioned|Fig.1 P21|||||||||
5198|Daralingie Formation|42085|6|Mentioned|Fig.2 P374|||||||||
5198|Daralingie Formation|42746|5|Briefly described|p6|||||||||
5198|Daralingie Formation|43570|5|Briefly described|Fig.2,p535,544-5|Ufimian|Kungurian|||||||
5198|Daralingie Formation|43628|6|Mentioned|p348|||||||||
5198|Daralingie Formation|44133|5|Briefly described|p65 Fig. 8.3, 85|Kazanian|Kungurian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Overlies Roseneath Shale. Maximum Thickness: 100m.||||||18-FEB-08
5198|Daralingie Formation|60717|5|Briefly described|p40 Fig. 2|Kungurian|Kungurian|Appears also as Daralingie Group in text - probably mis-named? Geological Province: Cooper Basin.||||||18-FEB-08
5198|Daralingie Formation|61614|6|Mentioned|p290 Fig. 2|Late Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
5198|Daralingie Formation|61615|5|Briefly described|p302, p302 Fig. 2, p304|Late Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin. Glacial deposits.||||||07-FEB-11
5198|Daralingie Formation|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
5198|Daralingie Formation|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||18-FEB-08
5198|Daralingie Formation|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Roseneath Shale.||
5198|Daralingie Formation|62730|5|Briefly described|p352 Fig. 1|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||18-FEB-08
5198|Daralingie Formation|63978|2|Defined|p16, Fig. 3|Middle Permian|Middle Permian|Formerly "Daralingie beds".Transitional on Roseneath Shale; disconformable below Toolachee Fm. Max.thickness: 96m. Interbedded siltstone, mudstone,coal + minor sandstone - siltst/mudst. are carbonaceous + micaceous. Further lith.included. In Cooper Basin.||||||07-FEB-11
5198|Daralingie Formation|64048|5|Briefly described|p64 Tb. 2|||Geological Province: Cooper Basin. Fluvio-deltaic deposits.||||||07-FEB-11
5198|Daralingie Formation|64197|6|Mentioned|p625 Fig.1c|Permian|Permian|Cooper Basin. [See also reference to the superseded Daralingie Beds: p630 Fig.7].||||Overlies Roseneath Shale.||
5198|Daralingie Formation|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Cooper Basin.||||Overlies Roseneath Shale.||
5198|Daralingie Formation|65489|5|Briefly described|p15, p48-49, p96, p131-132, p143|Kungurian|Kungurian|Cooper Basin. Gas reservoir accounting for 1% of the Basin's production. Mis-spelt as Daralinge on p48.||Topmost unit in Gidgealpa Group.||Overlies Roseneath Shale. Is overlain unconformably by Toolachee Formation.|Fluviodeltaic sediments.|
5198|Daralingie Formation|65925|5|Briefly described|Appendix 2.||||||||Sandstone, siltstone and coal. Fluvio-deltaic.|
5198|Daralingie Formation|67402|5|Briefly described|p90, p90 fig CPR4|||Cooper Basin. 50-100m thick. Proximal lake margin, lacustrine-deltaic and near-lake shoreline depositional environments. See also p91 tbl CPR1, p92, p93, p96, p101, p101 tbl CPR2.||Gidgealpa Group||Overlies the Roseneath Shale. Unconformably overlain by the Toolachee Formation.|Interbedded siltstone and mudstone, coal and minor very fine to fine-grained sandstone.|
5198|Daralingie Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p206, p207|Guadalupian|Cisuralian|Previously the Daralingie beds. Morton and Gatehouse (1985). Deposited during regression of the Roseneath Lake. > 95 m thick in the southern Nappamerri Trough. Includes rocks previously incorporated in the Toolachee Formation.||Of the Gidgealpa Group.||Conformably underlain by the Roseneath Shale. Intertongues with the Roseneath Shale. Disconformably overlain by the Toolachee Formation.|Comprises interbedded carbonaceous and micaceous siltstone, mudstone, coal and minor fine sandstone with a white kaolinitic matrix and some carbonaceous inclusions.|
5198|Daralingie Formation|69023|5|Briefly described|p81-82, p150-151|Permian|Permian|Cooper Basin. Gas reserves. Fluvio-deltaic sediments. Thickness variations indicate mid-Permian fault reactivation (the Daralingie Unconformity).||Unit in Gidgealpa Group.||Is overlain disconformably by Toolachee Formation.||
5198|Daralingie Formation|69454|5|Briefly described|p38:4|Wordian|Wordian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
5198|Daralingie Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Toolachee Formation, overlies Roseneath Shale||
5198|Daralingie Formation|69797|5|Briefly described|p17 Fig.2||Early Permian|Age: Kungarian - ? Ufimian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
5198|Daralingie Formation|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Kungurian|Cooper Basin. Fluviodeltaic sediments.||Unit in Gidgealpa Group.||Overlies Roseneath Shale. Is overlain unconformably by Toolachee Formation.||
5198|Daralingie Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
5198|Daralingie Formation|70317|6|Mentioned|p33, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Roseneath Shale. Is overlain unconformably by Toolachee Formation.||
5198|Daralingie Formation|70823|4|Described|iv, p6, p14|Capitanian|Wordian|Cooper Basin. Coal thickness, Seismic reflection and palynological characteristics briefly discussed. On average up to 50m thick but reaches up to 130m thick in the Nappamerri Trough. Deposited in a fluvio-deltaic setting. Hosts a commercial reservoir. See also p25-p27, p40-p41, p54, p64-p70, p78-p81, p83.||Gidgealpa Group||Conformably overlies the Roseneath Shale. Disconformably overlain by the Toolachee Formation.|Interbedded carbonaceous and micaceous siltstone, mudstone, coal and minor sandstone.|
5198|Daralingie Formation|70824|4|Described|p2, p5, p7-p9, p19|Capitanian|Wordian|Cooper Basin. Hosts good to excellent source rocks. Up to 130m thick. Deposited in a fluviodeltaic environment. Outcrop characteristics, areal extent and source rock geochemistry are discussed. See also  p84, p86-92, p108-p110, p113, p123.||||Overlies the Roseneath Shale. Unconformably overlain by the Toolachee Formation.|Interbedded carbonaceous and micaceous siltstone, mudstone, coal and minor sandstone.|
5198|Daralingie Formation|70946|5|Briefly described|p1087, p1089-1090|Permian|Early Permian|Cooper Basin. Deposited in a fluvio-deltaic environment.||Gidgealpa Group.||Overlies Roseneath Shale. Is overlain unconformably by Toolachee Formation.||08-OCT-18
5198|Daralingie Formation|71265|5|Briefly described|p589|Wordian|Capitanian|Cooper Basin.||Gidgealpa Group.||Overlies Roseneath Shale. Is overlain unconformably by Toolachee Formation.||
5198|Daralingie Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9|Kazanian|Kazanian|Cooper Basin. Deposited in a fluviodeltaic environment. Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p36, Ch5 p45, Ch5 p54, Ch7 p13.||Gidgealpa Group||Unconformably overlain by the Toolachee Formation.||
5198|Daralingie Formation|71701|5|Briefly described|p155|Capitanian|Wordian|Cooper Basin.||Gidgealpa Group||Overlies the Roseneath Shale. Unconformably overlain by the Toolachee Formation.||
5198|Daralingie Formation|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments. The NE-SW strike-slip Daralingie Event reactivated faults and eroded much of the formation. Contains gas, hydrocarbon source.||||Unconformably underlies the Toolachee Formation.||
5198|Daralingie Formation|73244|6|Mentioned|p85-86|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine environment. Gas and source rock.||||||
5198|Daralingie Formation|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Fluviodeltaic depositional environment. Hydrocarbon source rock that contains[?] gas. Capped by the Daralingie Unconformity.||Gidgealpa Group||Underlain by Roseneath Shale.||
5198|Daralingie Formation|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin. Source rock that hosts gas.||||Underlain by Epsilon Formation. Unconformably overlain by Toolachee Formation. Equivalent to Roseneath Shale.||
5198|Daralingie Formation|73479|5|Briefly described|p156 Fig.2, p159, p161, p164|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine depositional environment. In places a significant portion was eroded during Daralingie event (258 Ma).|ca 258 Ma|||Unconformably underlies Toolachee Formation||
5198|Daralingie Formation|73495|6|Mentioned|p499|Captainian|Captainian|||||Underlain by Roseneath Shale.||
5300|Dean Quartzite|22506|6|Mentioned|p130 Fig.4|Cryogenian|Tonian|||||||
5300|Dean Quartzite|22561|6|Mentioned|p15|||||||||
5300|Dean Quartzite|22562|5|Briefly described|p33|||Equivalent to Heavitree Quartzite.||||||08-AUG-06
5300|Dean Quartzite|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
5300|Dean Quartzite|22803|5|Briefly described|p423|||||||||
5300|Dean Quartzite|22804|5|Briefly described|p441|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|22805|5|Briefly described|p464|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|22826|5|Briefly described|p568|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|23716|6|Mentioned|p4|||Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|24301|4|Described|p14, p7 Tb. 2,|Neoproterozoic|Neoproterozoic|Undated but is suggested to be equivalent to the Neoproterozoic Heavitree Quartzite. Overlain by Pinyinna beds.  Geological Province: Amadeus Basin.||||||16-JUN-09
5300|Dean Quartzite|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Medium- to coarse-grained, thick-bedded to massive white quartzite and quartz sandstone; minor conglomerate and fine-grained sheared quartzite. Geological Province: Amadeus Basin.||||||16-JUN-09
5300|Dean Quartzite|24496|5|Briefly described|p21 Tb.2|Neoproterozoic|Neoproterozoic| Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|30389|6|Mentioned|Table 1|||Mid Proterozoic age. Lithology.||||||
5300|Dean Quartzite|30390|5|Briefly described|p32|||||||||
5300|Dean Quartzite|30602|6|Mentioned|p658|||||||||
5300|Dean Quartzite|30670|6|Mentioned|p67|||Upper Proterozoic age||||||
5300|Dean Quartzite|30815|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5300|Dean Quartzite|30817|4|Described|p9|||See also p14. Correlated with Heavitree Quartzite.||||||08-AUG-06
5300|Dean Quartzite|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5300|Dean Quartzite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5300|Dean Quartzite|31991|6|Mentioned|p298|||Correlation with Heavitree Quartzite.||||||
5300|Dean Quartzite|33307|6|Mentioned|Fig.6|||||||||
5300|Dean Quartzite|33468|6|Mentioned|p214|||||||||
5300|Dean Quartzite|33588|6|Mentioned|p6|||||||||
5300|Dean Quartzite|34945|6|Mentioned|p356|||||||||
5300|Dean Quartzite|35038|6|Mentioned|p368|||||||||
5300|Dean Quartzite|35102|6|Mentioned|p1|||||||||
5300|Dean Quartzite|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5300|Dean Quartzite|36526|6|Mentioned|p154|||||||||
5300|Dean Quartzite|36886|6|Mentioned|p196|||||||||
5300|Dean Quartzite|36887|5|Briefly described|p208|||||||||
5300|Dean Quartzite|37460|6|Mentioned|p175|||||||||
5300|Dean Quartzite|37707|6|Mentioned|p24|||||||||
5300|Dean Quartzite|38157|6|Mentioned|Table VI|||||||||
5300|Dean Quartzite|39210|5|Briefly described|p40|||||||||
5300|Dean Quartzite|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
5300|Dean Quartzite|39565|6|Mentioned|p31|||||||||
5300|Dean Quartzite|40740|6|Mentioned|p1|||||||||
5300|Dean Quartzite|41190|6|Mentioned|Fig.4|||||||||
5300|Dean Quartzite|41270|6|Mentioned|Table 1|||||||||
5300|Dean Quartzite|41717|6|Mentioned|Fig.2|||||||||
5300|Dean Quartzite|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
5300|Dean Quartzite|41852|6|Mentioned|Table 1|||||||||
5300|Dean Quartzite|41884|6|Mentioned|p70|||||||||
5300|Dean Quartzite|42059|6|Mentioned|p130|||||||||
5300|Dean Quartzite|42082|6|Mentioned|Fig.3 P323|||||||||
5300|Dean Quartzite|42504|5|Briefly described|p67|||||||||
5300|Dean Quartzite|42643|6|Mentioned|p20|||Amadeus Basin||||||
5300|Dean Quartzite|42794|6|Mentioned|p9|||||||||
5300|Dean Quartzite|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Quartzite. sandstone, conglomerate, metaquartzite, kyanite schist.  Geological province: Amadeus Basin.||||||23-JAN-08
5300|Dean Quartzite|43035|4|Described|p17|||||||||
5300|Dean Quartzite|43442|6|Mentioned|p14||Neoproterozoic|C.820 Ma (Korsh & Kennard,1991)||||||
5300|Dean Quartzite|43503|6|Mentioned|50||Proterozoic|||||||
5300|Dean Quartzite|43697|6|Mentioned|p28|||||||||
5300|Dean Quartzite|44109|5|Briefly described|p164|||Together with the Townsend Quartzite, unconformably overlies the Musgrave Block units, forming the basal units of of southwestern Amadeus Basin and Northern Officer Basin.  ||||||
5300|Dean Quartzite|44139|5|Briefly described|p286, 285 Fig. 3-69|||Occurs north of Woodroffe Thrust. Correlated with Heavitree Quartzite by Wells & others (1970). Unconformably overlies Olia Gneiss and Mount Harris Volcanics. Thick sequence of quartzite and conglomerate; deformed and schistose, and metamorphosed to greenschist or amphibolite facies.| | ||||05-MAR-18
5300|Dean Quartzite|44342|6|Mentioned|p.9|||SG/53-5.||||||
5300|Dean Quartzite|44439|2|Defined|p.4,6-8,Tb.1, map||Neoproterozoic|Upper Proterozoic. (G52-2).||||||
5300|Dean Quartzite|44440|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|44493|4|Described|p.9-12,14, map||Neoproterozoic|U.Prot.Bloods Range sheet. (G53-3).||||||22-DEC-09
5300|Dean Quartzite|44494|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|44495|4|Described|p.5, map||Neoproterozoic|U.Prot.Ayers Rock sheet. (G52-8). See p.7,9, for details.||||||
5300|Dean Quartzite|44496|5|Briefly described|map legend||Neoproterozoic|Schistose quartzite, Upper Proterozoic.||||||17-JUL-06
5300|Dean Quartzite|44499|14|Not recorded|opp.p.6, Tb.1|||||||||
5300|Dean Quartzite|45041|4|Described|p20|||Proterozoic||||||
5300|Dean Quartzite|45149|6|Mentioned|Table 1|||Page 19.||||||
5300|Dean Quartzite|45170|6|Mentioned|p9|||||||||
5300|Dean Quartzite|48842|2|Defined|p.13||Neoproterozoic|p.1,5,8,10-13,26-7,30,32,Pls.3,7. Tb.I. Correlates with Heavitree Quartzite. U.Proterozic.||||||10-JUL-13
5300|Dean Quartzite|48863|14|Not recorded|p.13||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|48864|2|Defined|p.23||Neoproterozoic|Tb.1. On many pages. p.1,9,10,12,14,15-17,20,25,30,33,36-39,41-45,47,49,50,52,Pl.4,5,6,7,8,10,11,12,13. U.Prot. (G52-2,3,7,8).||||||
5300|Dean Quartzite|48865|14|Not recorded|Pl.9|||Prelim.map Ayers Rock 1:250,000 (G52-8).||||||
5300|Dean Quartzite|48963|6|Mentioned|Fig.3|||||||||
5300|Dean Quartzite|49833|6|Mentioned|p8|||||||||
5300|Dean Quartzite|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies: Mount Harris Basalt.  Underlies: Pinyinna beds.||||||22-DEC-09
5300|Dean Quartzite|50321|5|Briefly described|Map Legned|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Underlies: Pinyinna beds.  .||||||09-JUN-04
5300|Dean Quartzite|60572|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Crystalline quartz sandstone, rare quartz conglomerate and quartz-muscovite-kyanite layers.  Geological Province: Amadeus Basin.||||||23-DEC-09
5300|Dean Quartzite|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Deformed basal sediments of Amadeus Basin.||||||22-FEB-05
5300|Dean Quartzite|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Crystalline quartz sandstone, rare vein quartz pebble conglomerate, quartz-kyanite-muscovite layers, red/purple crystalline quartz sandstone, feldspathic sandstone. Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz Sandstone. Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|60683|4|Described|p24-25, p9 Tb. 1, p22, p23|Neoproterozoic|Neoproterozoic|Recrystallised, thick-bedded to massive quartz sandstone; rare quartz conglomerate and quartz-kyanite-muscovite layers. Conformably overlain by Pinyinna beds, Bloods Range beds.  Age: probably c.850Ma. max. thickness: ~100m.  Geol. Prov: Amadeus Basin.||||||20-APR-05
5300|Dean Quartzite|61154|4|Described|p17-18, p5 Tb. 1|Neoproterozoic|Neoproterozoic|Age: ~850Ma. Max. thickness: ~60m. Overlain by/interleaved with Pinyinna beds; unconformably overlies Tjauwata Gp and Pitjantjatjara Supersuite. Geol. Prov: Amadeus Basin. See also p42 App.||||||19-JUL-05
5300|Dean Quartzite|61306|5|Briefly described|p32, p61|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|White crystalline quartz sandstone, quartz muscovite schist. Geological Province: Amadeus Basin.||||||23-DEC-09
5300|Dean Quartzite|61733|6|Mentioned|p47 Fig.3 |||Amadeus Basin.||||||
5300|Dean Quartzite|62359|5|Briefly described|p547-548, p550|Middle Neoproterozoic|Middle Neoproterozoic|Overlain by Pinyinna Beds. Age: ~750Ma. Geological Province: Amadeus Basin. Equivalent to Heavitree Quartzite. ||||||
5300|Dean Quartzite|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
5300|Dean Quartzite|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|62453|6|Mentioned|p16|||Age: 850Ma. Overlies Kukial Sandstone.||||||
5300|Dean Quartzite|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzite, sandstone, conglomerate. Metamorphosed in part to Kyanite schist and quartzite. Underlies Pinyinna Beds and Bitter Springs Formation.||||||14-AUG-06
5300|Dean Quartzite|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzite, sandstone, conglomerate. Metamorphosed in part to kyanite schist and quartzite.||||||
5300|Dean Quartzite|62989|5|Briefly described|p39, p40|||Unconformably overlies basement of the Musgrave Province, and Kulail Quartzite (basal unit of Amadeus Basin). Equivalent of Heavitree Quartzite. Geological Province: Amnadeus Basin. Shallow marine deposits.||||||25-JAN-07
5300|Dean Quartzite|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
5300|Dean Quartzite|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally.||||||09-DEC-08
5300|Dean Quartzite|64809|5|Briefly described|p1, p3 Fig.2|Proterozoic|Proterozoic||||||Transgressive marine sands.|
5300|Dean Quartzite|65102|6|Mentioned|p363, Figure 4-38, p365, 372|Neoproterozoic|Neoproterozoic|Amadeus Basin. Correlated with Robert Formation, Townsend Formation, Pindyin beds all Officer Basin.||||||
5300|Dean Quartzite|65233|5|Briefly described|p2, p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
5300|Dean Quartzite|65256|4|Described|p17, p4, p6 Tb.1, p8, p16, p21, p37|Cryogenian|Tonian|Basal Amadeus Basin. Conformably overlies (grades into or interfingers with) Kulail Sandstone; disconformably overlies Tjauwata Group; unconformably overlies Bloods Range Formation, Pottoyu Granite Suite, Imbumbunna Granite; conformably underlies Pinyinna beds; correlative of Heavitree Quartzite; onlapped by Larapinta Group. Recrystallised, well sorted, equigranular, massive to thickly bedded quartz sandstone, rare quartz conglomerate. Probably >50m thick; strongly deformed in areas. 850 Ma (poorly constrained).||||||25-MAR-15
5300|Dean Quartzite|67128|6|Mentioned|p30|||Southern Amadeus Basin.||||||
5300|Dean Quartzite|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Unconformably overlies Arunta Complex. Is overlain by Pinyinna beds and Bitter Springs Formation.||
5300|Dean Quartzite|67553|6|Mentioned|p71|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
5300|Dean Quartzite|67856|4|Described|p342, p338, 335, 337, 344, 348|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970 etc. Base of Amadeus Basin. Type section not defined. 1200m thick. Age inferred from stratigraphic position. Mostly fluvial grading upwards to marine shelf?||||Laterally equivalent to Heavitree quartzite. Overlies Wingelina Complex (unconformably).|Fine to coarse grained quartzite; sandstone; minor conglomerate; partly metamorphosed.|
5300|Dean Quartzite|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
5300|Dean Quartzite|68270|4|Described|p683|Tonian|Tonian|Amadeus Basin.||||Overlain by Pinyinna beds. Underlain by basement.||03-JUL-19
5300|Dean Quartzite|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
5300|Dean Quartzite|68733|6|Mentioned|p190|||Amadeus Basin.|||||Texturally mature sandstone; fluvial to shallow-marine.|05-DEC-17
5300|Dean Quartzite|68996|6|Mentioned|p6|Neoproterozoic|Mesoproterozoic|Deposition ~1040-800 Ma?||||||
5300|Dean Quartzite|69003|6|Mentioned|p60-61|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
5300|Dean Quartzite|69031|5|Briefly described|p4, p6 Fig.4, p8|||Basal unit in the southern Amadeus Basin.||||Locally overlies Kulail Sandstone. Is overlain by Bitter Springs Formation. Equivalent to Heavitree Quartzite.|A lithic and feldspathic unit.|
5300|Dean Quartzite|69091|6|Mentioned|p134 Fig.6.2|||||||||26-SEP-14
5300|Dean Quartzite|69153|6|Mentioned|500k_geologyp08_lut.csv||Neoproterozoic|Lithology description shared with Heavitree Quartzite|||||Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
5300|Dean Quartzite|69436|5|Briefly described|p21:4, 9, 11, 17-19|Neoproterozoic|Neoproterozoic|Olia Chain, Amadeus Basin. Involved in thin- and thick-skinned deformation by the Petermann Orogeny, with a metamorphic assemblage of kyanite-muscovite-quartz +/- tourmaline, with rare staurolite. Is structurally interleaved with Tjauwata Group in the Wankari Detachment Zone of the Petermann Nappe Complex. Two K-Ar muscovite (metamorphism) ages of 586 +/- 5 Ma and 568 +/- 5 Ma (Close et al., 2003) have been obtained from within the Piltardi Detachment Zone.||||Overlies Amputjuta Dacite and Hull Suite. Is locally overlain (thrust fault contact) by Mount Harris Basalt and interleaved with Pinyinna beds.||12-JUL-16
5300|Dean Quartzite|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 1.||||Is overlain by Pinyinna beds. Correlated with Heavitree Quartzite.||12-JUL-16
5300|Dean Quartzite|69438|4|Described|p23:2-5, 8-10, 18, 44, 59-60|Cryogenian|Cryogenian|Extensively exposed in the SW margin of the Amadeus Basin. Shallow-marine deposits. 100-300m thick. Metamorphosed to amphibolite-grade facies, decreasing to greenschist facies to the N. Maximum deposition age from detrital zircons; minimum age from a U-Pb baddeleyite age (Glikson et al., 1996) of a spilite with affinities to those in the overlying Bitter Springs Formation. Has promising Neoproterozoic hydrocarbon reservoirs, sealed by Gillen Member salt.|Between 1050-1000 Ma and c.820 Ma. |||Conformably (gradationally) overlies Kulail Sandstone. Correlated with Heavitree Quartzite. Is overlain conformably (gradationally) by Pinyinna beds.|Widespread, sheet-like, uniform deposits of quartz sandstone; local intense silicification where the unit is exposed.|12-JUL-16
5300|Dean Quartzite|69439|6|Mentioned|p24:2|||Amadeus Basin.||||Correlative of Heavitree and Vaughan Springs Quartzites.||12-JUL-16
5300|Dean Quartzite|69440|6|Mentioned|p25:2|||Amadeus Basin. Inferred to correlate with Munyu Sandstone (Murraba Basin).||||||12-JUL-16
5300|Dean Quartzite|69606|5|Briefly described|p2, p4 fig 2, p19|Cryogenian|Cryogenian|Southern Amadeus Basin. Potential reservoir rocks.||||Overlies the Kulail Sandstone. Overlain by the Gillen Member, Bitter Springs Formation. Is equivalent to the Heavitree Quartzite.|Sandstone and quartzite.|
5300|Dean Quartzite|69673|4|Described|p63, p84, p85, p88, p89, p101|||||||Correlated with Heavitree Quartzite, overlies Kulail Sandstone, overlain by Pinyinna beds, Gillen Member|Fine to coarse grained orthoquartzite, arkosic quartzite with minor shale and conglomerate.|
5300|Dean Quartzite|69926|6|Mentioned|p156, 176, 178|||Basal quartzite in the southern Amadeus Basin. Overlies the Mulga Park Subdomain of the Musgrave Block.||||Correlated with Heavitree Quartzite.|May include Mn-rich quartzites found overlying amphibolites.|
5300|Dean Quartzite|70018|4|Described|p234-240|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the southern Amadeus Basin. Correlable to Heavitree Quartzite in the northern Amadeus Basin. Deposition occurred during post-rift subsidence after initial uplift of Musgrave Block in a braod intracratonic basin between Musgrave Block and Arunta region. Thinly to thickly bedded (50-100m) and crops out in the southwestern Amadeus Basin where it commonly forms prominent ridges and escarpments. Zircon data show two broad peaks representing a mixture between sediments derived from the Musgrave Block and Arunta Region.||||Overlain by Pinyanna Beds. Underlain by Kulail Sandstone.|Massive, clean, white, schistose sericitic quartzite.|
5300|Dean Quartzite|70416|5|Briefly described|p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||Correlated with Heavitree Quartzite.||
5300|Dean Quartzite|70634|4|Described|500k_geolgyp08_lut.csv|Neoproterozoic|Neoproterozoic|Included with Heavitree Quartzite in file (undivided).|||||Quartz sandstone, sandstone, and conglomerate; kyanite schist locally.|
5300|Dean Quartzite|70793|4|Described|500k_interpgeop14_lut.csv + geochron|Cryogenian|Neoproterozoic|Of Amadeus Basin (Phase 1), Centralian Superbasin. Occurs on the SW margin of the Amadeus Basin. Events: Alice Springs Orogeny (450-295 Ma); Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199404 (quartzite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1120+\-29 Ma. See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred; biostrat).|||Underlain by Kulail Sandstone. Equivalent to Heavitree Quartzite.|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
5300|Dean Quartzite|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
5300|Dean Quartzite|70839|5|Briefly described|p328-334,336|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Basal unit of Supersequence 1; Equivalent to Kulail Sandstone, and Heavitree Quartzite to the north. Exposed as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Detrital zircon age spectrum range between c. 2.8 and 1.04 Ga; major late paleoproterozoic age component at c. 1.88-1.62 Ga (peaks at c. 1.69 and 1.73 Ga) and major Mesoproter0zoic age component between 1.35 and 1.04 Ga (Warakurna Supersuite). Peaks at 1.2 [derived from Pitjantjatjara Supersuite; Musgrave orogeny] and 1.31 Ga [Wankanki Supersuite; Giles event]). Minor peaks at c. 2.8, 2.5 and 2.4 Ga, and a small age cluster between c. 1.48 and 1.4 Ga (Papulankutja Supersuite, west Musgrave).|Max dep age: 1039+\-35 Ma (207Pb/206Pb)|||Overlain by Bitter Springs Formation or Pinyanna beds. Correlable to Kulail Sandstone and Heavitree Quartzite.||
5300|Dean Quartzite|71080|5|Briefly described|p23, p29 Fig 20, p30|Tonian|Tonian|Southern Amadeus Basin. Supersequence 1.||||Correlated with Heavitree Formation, Amadeus Basin; Munyu Sandstone, Murraba Basin.|Dominantly sandstone.|
5300|Dean Quartzite|71088|6|Mentioned|p6, p8, p10, p17|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Part of Supersequence 1.|c. 1200-1150 Ma|||||
5300|Dean Quartzite|71170|5|Briefly described|p114, p122|Mesoproterozoic|Mesoproterozoic|15m thick sequence directly above basement. Metamorphic muscovite is dated at 598 +/- 3 Ma. P-T conditions during metamorphism are estimated.|||||Fine-medium grained quartzite.|
5300|Dean Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, schist, sandstone, quartzite|
5300|Dean Quartzite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199404 (quartz-rich sandstone) yielded a weighted mean 207Pb/206Pb age of 1120+\-29 Ma, interpreted as maximum depositional age of sandstone. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|976-827 Ma (inferred)|||Overlain by Bitter Springs Group. Underlain by  Kulail Sandstone. Correlable with Heavitree Quartzite, Vaughan Springs Quartzite.|Fine- to coarse-grained, white to grey-blue paraquartzite; commonly thickly bedded and devoid of sedimentary structures; locally contains heavy mineral bands; sandstone, lesser siltstone and conglomerate; commonly intensely silicified.|
5300|Dean Quartzite|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
5300|Dean Quartzite|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1120+/-29 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained quartz sandstone.|
5300|Dean Quartzite|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||Equivalent to Heavitree Formation. Overlain by Pinyanna beds or Gillen Formation. Underlain by and grades into Kulail Sandstone or basement.||
5300|Dean Quartzite|71842|5|Briefly described|p2-3|Cryogenian|Cryogenian|Of Amadeus Basin.||||Overlain by Bitter Springs Group. Correlable to Heavitree Quartzite.||
5300|Dean Quartzite|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Informal grouping of mostly time-equivalent silicilastic units. Grouped with Kulail Sandstone, Heavitree Quartzite, and Vaughan Springs Quartzite. Min age  from biostratigraphy.|||||Informal grouping description: Quartz sandstone, sandstone, and conglomerate; kyanite schist locally [probably only in Dean Quartzite].|
5300|Dean Quartzite|72094|5|Briefly described|p3 Fig 2, p7|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Strongly folded ridges of Dean Quartzite interleaved with Tjauwata Group rhyolite-dominant rocks.||
5300|Dean Quartzite|72375|4|Described|p5|Tonian|Stenian|Of Amadeus Basin. Inferred max depositional age of c. 1040-820 Ma, based on age of underlying Tjauwata Group (c. 1090-1040 Ma; Close et al., 2005), and the similar geochemical affinities with Johnnys Creek Formation basalts and the c. 824 Ma Amata Dolerite. ||||Underlain by Tjauwata Group. Correlable with Heavitree Formation.||
5300|Dean Quartzite|72601|6|Mentioned|p3|Tonian|Tonian|Amadeus Basin. Found in the southern part of the basin.||||Overlain by Gillen Formation (Bitter Springs Group).||
5300|Dean Quartzite|73085|6|Mentioned|p1|Tonian|Tonian|||||Partly underlain by Kulail Sandstone. Partly overlain by Pinyinna beds and Gillen Formation (Bitter Springs Group). Equivalent to Heavitree Formation.||
5300|Dean Quartzite|73086|6|Mentioned|p3, p7, p9, p15, p18, p145|||Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Restricted to exposures in the southwest of the basin. Exposed for ~400 km along the south-western margin of the basin.||||Correlates to Heavitree Formation. Conformably overlain by Pinyinna beds.||
5300|Dean Quartzite|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Equivalent to Heavitree Quartzite, conformably underlies the Bitter Springs Group and Gillen Formation.||
5300|Dean Quartzite|73346|6|Mentioned|p2, p5, p14|Tonian|Tonian|Amadeus Basin. Outcrops of sandstone originally assigned to this unit east of the Giles Mulga Park Road [in the Cobb Embayment] were reinterpreted as the basal succession of the Cobb Formation.||||||
5300|Dean Quartzite|73437|6|Mentioned|p151-152|Neoproterozoic|Neoproterozoic|Amadeus Basin. (U-Th)/He zircon cooling ages of 531+/-72 Ma and 546+/-52 Ma. K-Ar muscovite cooling ages of 568+/-5 Ma and 586+/-5 Ma from Scrimgeour et al., (1999).||||||
5489|Dilwyn Formation|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Maximum thickness 593m.||Wangerip Group.||Overlies Pember Mudstone, locally unconformably. Is overlain unconformably by Narrawaturk Marl.||
5489|Dilwyn Formation|22587|6|Mentioned|p79 Fig.7|Early Eocene|Late Paleocene|Of the Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|22674|5|Briefly described|Fig.2 p719|Early Eocene|Early Eocene|||||||
5489|Dilwyn Formation|22875|3|Fully described|p14|Early Eocene|Early Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
5489|Dilwyn Formation|23230|4|Described|Table4-1p40, 41|Eocene||||||||
5489|Dilwyn Formation|23238|5|Briefly described|p106||Tertiary|||||||
5489|Dilwyn Formation|23242|6|Mentioned|Fig11-4.1p158||Paleocene|||||||
5489|Dilwyn Formation|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|23322|5|Briefly described|957 Fig.2|Middle Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin.||||||07-SEP-09
5489|Dilwyn Formation|23402|5|Briefly described|p31|Early Eocene|Late Paleocene|||||||
5489|Dilwyn Formation|23778|5|Briefly described|p668|||Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|24038|5|Briefly described|p439 Fig.2|Paleocene|Paleocene|Geological Province: Torquay Basin||||||12-JAN-10
5489|Dilwyn Formation|24056|5|Briefly described|p85|Paleocene|Paleocene|Of Wangerrip Group. Geological Basin: Otway Basin.||||||24-JUL-08
5489|Dilwyn Formation|24202|5|Briefly described|p313 Fig 2|Middle Eocene|Late Paleocene|Of the Wangerrip Group.  Geological Province: Gambier Sub-basin.||||||
5489|Dilwyn Formation|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Geological Province: Otway Basin. Max. Thickness 593m. Of the Wangerrip Group.||||||30-NOV-04
5489|Dilwyn Formation|24397|5|Briefly described|p245|||Overlain by Sturgess Point Member. Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|24455|5|Briefly described|p327|Early Eocene|Late Paleocene|Composed mainly of dark brown, carbonaceous sandy clay and silt, interbedded with fine- to medium-grained, clean to clayey sand , with minor coarse sand and gravel. Conformably overlies the Pebble Point Formation. Max. thickness: 150 See also p321 Fig. 1.||||||22-MAR-05
5489|Dilwyn Formation|24551|5|Briefly described|p246, 295, p732 Table 17.2|Eocene|Paleocene|Of the Wangerrip Group. Underlain by Pember Mudstone Member. Overlain by Burrungule Member. Max thickness: 1000m.||||||16-APR-07
5489|Dilwyn Formation|24562|5|Briefly described|p8 Fig. 2|Eocene|Eocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|29355|6|Mentioned|p188|||||||||
5489|Dilwyn Formation|29823|6|Mentioned|p14|||||||||
5489|Dilwyn Formation|29824|4|Described|p16|||||||||
5489|Dilwyn Formation|29825|5|Briefly described|p18|||||||||
5489|Dilwyn Formation|29856|6|Mentioned|p36|||||||||
5489|Dilwyn Formation|30576|6|Mentioned|Table 1|||||||||
5489|Dilwyn Formation|30578|4|Described|p8|||||||||
5489|Dilwyn Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5489|Dilwyn Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||16-APR-07
5489|Dilwyn Formation|30676|5|Briefly described|p12|||||||||
5489|Dilwyn Formation|30905|6|Mentioned|p149|||||||||
5489|Dilwyn Formation|30932|6|Mentioned|Map legend|Eocene|Paleocene|Equivalent Dartmoor Formation, Palaeocene to Eocene.||||||22-SEP-18
5489|Dilwyn Formation|31036|1|Redefined|p208|Paleocene|Paleocene|See also p199. Table 9-1. Unit of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|31245|5|Briefly described|p68|||Middle Palaeocene. Unit of Wangerrip Group. See also p82.||||||16-APR-07
5489|Dilwyn Formation|31246|6|Mentioned|p56|||See also p57.||||||22-SEP-18
5489|Dilwyn Formation|31372|4|Described|p11|||See also p2, p9.||||||16-APR-07
5489|Dilwyn Formation|31424|4|Described|p14|||See also p7. Described from core.||||||16-APR-07
5489|Dilwyn Formation|31534|6|Mentioned|p363|||See also Table 19-3||||||
5489|Dilwyn Formation|31624|5|Briefly described|p105|||Lithology||||||
5489|Dilwyn Formation|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
5489|Dilwyn Formation|31920|6|Mentioned|p60|||||||||
5489|Dilwyn Formation|31922|6|Mentioned|p166|||||||||
5489|Dilwyn Formation|32115|4|Described|p1|||Early Tertiary. See also Fig.1||||||
5489|Dilwyn Formation|32117|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|32120|6|Mentioned|p274|||Palaeocene fauna||||||
5489|Dilwyn Formation|32220|6|Mentioned|p9|||||||||
5489|Dilwyn Formation|32227|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32232|6|Mentioned|p19|||||||||
5489|Dilwyn Formation|32234|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32235|6|Mentioned|p34|||||||||
5489|Dilwyn Formation|32240|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32852|6|Mentioned|p10|||||||||
5489|Dilwyn Formation|32898|6|Mentioned|p29|||See also Table 2-1||||||
5489|Dilwyn Formation|33319|6|Mentioned|p167|||Fauna||||||
5489|Dilwyn Formation|33938|6|Mentioned|p48|||Refers Harris (1965).||||||
5489|Dilwyn Formation|33940|6|Mentioned|p414|||||||||
5489|Dilwyn Formation|34063|6|Mentioned|p2|||Paleocene. Table||||||
5489|Dilwyn Formation|34343|5|Briefly described|p97|||||||||
5489|Dilwyn Formation|34360|6|Mentioned|p11|||||||||
5489|Dilwyn Formation|34988|6|Mentioned|Table 9.4|||||||||
5489|Dilwyn Formation|35066|3|Fully described|p205|||||||||
5489|Dilwyn Formation|35285|6|Mentioned|p414|||||||||
5489|Dilwyn Formation|35722|6|Mentioned|p4|||Stratigraphy.||||||
5489|Dilwyn Formation|36305|6|Mentioned|p358|||||||||
5489|Dilwyn Formation|36366|6|Mentioned|p5|||||||||
5489|Dilwyn Formation|36913|6|Mentioned|p81|||||||||
5489|Dilwyn Formation|37548|4|Described|p129|||||||||
5489|Dilwyn Formation|38625|6|Mentioned|Table 2|||||||||
5489|Dilwyn Formation|38663|6|Mentioned|Fig.1|||||||||
5489|Dilwyn Formation|38932|5|Briefly described|p97|||See also Fig.4||||||
5489|Dilwyn Formation|39408|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|39446|6|Mentioned|p34|||||||||
5489|Dilwyn Formation|40003|5|Briefly described|p44|||||||||
5489|Dilwyn Formation|40230|6|Mentioned|p6|||||||||
5489|Dilwyn Formation|40521|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|40555|6|Mentioned|p51|||||||||
5489|Dilwyn Formation|40796|6|Mentioned|p218|||||||||
5489|Dilwyn Formation|41016|5|Briefly described|p214|||||||||
5489|Dilwyn Formation|41043|6|Mentioned|p95|||See also p99.||||||22-SEP-18
5489|Dilwyn Formation|41185|6|Mentioned|p178|||See also Fig.4||||||
5489|Dilwyn Formation|41269|5|Briefly described|p246|||||||||
5489|Dilwyn Formation|41517|6|Mentioned|p134|||||||||
5489|Dilwyn Formation|41642|6|Mentioned|p219|||||||||
5489|Dilwyn Formation|41701|6|Mentioned|Map legend|Eocene||||||||
5489|Dilwyn Formation|41704|6|Mentioned|Fig.3|||||||||
5489|Dilwyn Formation|41714|6|Mentioned|p301|||||||||
5489|Dilwyn Formation|41726|6|Mentioned|p421|||See also p427.||||||16-APR-07
5489|Dilwyn Formation|41769|4|Described|p22|||See also p23.||||||16-APR-07
5489|Dilwyn Formation|41868|4|Described|p535|||See also p548.||||||16-APR-07
5489|Dilwyn Formation|42079|6|Mentioned|Fig.2 P264|||||||||
5489|Dilwyn Formation|42152|6|Mentioned|p15|||||||||
5489|Dilwyn Formation|42318|5|Briefly described|p8|||||||||
5489|Dilwyn Formation|42361|6|Mentioned|p16|||||||||
5489|Dilwyn Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
5489|Dilwyn Formation|42524|5|Briefly described|Fig.3 p27|||||||||22-SEP-18
5489|Dilwyn Formation|42555|5|Briefly described|Fig.2 p285|||||||||22-SEP-18
5489|Dilwyn Formation|42599|5|Briefly described|Fig.3 p614|||||||||22-SEP-18
5489|Dilwyn Formation|42827|3|Fully described|p279|||Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5489|Dilwyn Formation|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 45-65Ma||||||
5489|Dilwyn Formation|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map. Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43208|5|Briefly described|map legend||Early Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43219|5|Briefly described|Fig.3,p6.||Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43590|4|Described|p18||Early Eocene|||||||
5489|Dilwyn Formation|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
5489|Dilwyn Formation|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
5489|Dilwyn Formation|43744|6|Mentioned|Fig.3,p3|||||||||
5489|Dilwyn Formation|43797|5|Briefly described|p201||Eocene|||||||
5489|Dilwyn Formation|43799|5|Briefly described|p185|||||||||
5489|Dilwyn Formation|43814|6|Mentioned|Fig.3,p115|||||||||
5489|Dilwyn Formation|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
5489|Dilwyn Formation|44133|5|Briefly described|p154, 152 Fig. 10.2|Middle Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin. Interfingers with Pember Mudstone. Thickness: 740m. ||||||
5489|Dilwyn Formation|47054|6|Mentioned|p490|||||||||
5489|Dilwyn Formation|48911|3|Fully described|p25|||||||||
5489|Dilwyn Formation|48977|6|Mentioned|Fig.5|||||||||
5489|Dilwyn Formation|60538|5|Briefly described|p470, 471 Fig. 10, 474 Fig. 13|Early Eocene|Early Eocene|Includes: Burrungule Member at top (but may? be base of Mepunga Sand Formation above). Geological Province: Otway Basin.||||||31-JAN-07
5489|Dilwyn Formation|60563|6|Mentioned|p45|||||||||16-JUN-05
5489|Dilwyn Formation|61017|5|Briefly described|p5 Fig. 2|Lutetian|thanetian|Of the Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61155|5|Briefly described|p3, p18|Middle Eocene|Late Paleocene|Of the Wangerrip (Knight) Group. Thick paralic sequences of sediments. Overlies Pebble Point Formation; interfingers with Eastern View Formation and Pember Mudstone. Max. thickness: 500m. Geological Province: Otway Basin.||||||03-MAR-10
5489|Dilwyn Formation|61181|6|Mentioned|p183|||Contains relatively pure sands for various forms of silica. Geological Province: Otway Basin. ||||||
5489|Dilwyn Formation|61182|3|Fully described|p19, p22-23, p32|Early Eocene|Early Eocene|Formerly Dilwyn Clay. Of Wangerrip Gp. Geol.Prov: Otway Basin. Considered by some to include Pember Mudstone which here is treated as a separate formation. Conformably overlies Pember Mudstone and Eumeralla Fm; overlain by Nirranda Gp. Lithology included.||||||06-JAN-10
5489|Dilwyn Formation|61470|5|Briefly described|p28 Fig. 5|Lutetian|Thanetian|Of the Wangerrip Group. Overlies and interfingers with Pember Mudstone.  Geological Province: Otway Basin.||||||12-OCT-05
5489|Dilwyn Formation|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Wangerrip Group.||Overlies Pember Mudstone.||
5489|Dilwyn Formation|61622|5|Briefly described|p436 Fig. 2|Eocene|Eocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61623|6|Mentioned|p449 Fig. 4|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|61626|5|Briefly described|p486, p486 Fig. 2|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|61627|5|Briefly described|p500 Fig. 2|Eocene|Eocene|Of Wangerrip Group. Underlain by Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|62896|5|Briefly described|p88, p89|Early Eocene|Late Paleocene|Of the Wangerrip Group. Consists predominantly of quartz sand, often silty or clayey, sandy silt and clay, mudstone and clay.||||||07-FEB-11
5489|Dilwyn Formation|63122|5|Briefly described|p17 Fig. 4.3|Middle Eocene|Early Eocene|Of the Wangerrip Group. Max. thickness: 593m. Geological Province: Otway Basin. ||||||
5489|Dilwyn Formation|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p89|Middle Eocene|Early Eocene|Supersedes Dilwyn "Clay", "Dartmoor Formation",  Knight Fm. Prob.syn.with Tartwaup Fm. Of Wangerrip Gp. Overlies Sherbrook Gp and Pember Sst. Over Narrawaturk + Gellibrand Marls + Greenways and Camelback Mbrs (Gambier Lst). Age: ~55-~48Ma. Max.thick: 593m||||||
5489|Dilwyn Formation|63129|6|Mentioned|p139|||Geological Province: Otway Basin. May contain potential reservoirs.||||||30-JAN-08
5489|Dilwyn Formation|63130|5|Briefly described|p146|||Overlain by Narrawaturk Marl. Geological Province: Otway Basin.||||||06-FEB-08
5489|Dilwyn Formation|63150|5|Briefly described|p99|||Contains plant microfossils. Geological province: Otway Basin.||||||
5489|Dilwyn Formation|63269|5|Briefly described|p605|Eocene|Eocene|Otway Basin.||Wangerrip Group.||||
5489|Dilwyn Formation|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Topmost unit of the Wangerrip Group. Geological Province: Penola Trough/Otway Basin.||||||26-JUN-13
5489|Dilwyn Formation|63740|5|Briefly described|p88|Early Eocene|Late Paleocene|Of Wangerrip Group. Geological province: Otway Basin. Consists predominantly of quartz sand, often silty or clayey, sandy silt and clay, mudstone and shale.||||||07-FEB-11
5489|Dilwyn Formation|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Wangerrip Group. Includes Pember Mudstone Member. Called Dilwyn Clay by Baker (1953).||||||
5489|Dilwyn Formation|66002|4|Described|p10 Tb.7, p10 Tb.8, p11, p16, p26 Fig.7|Eocene|Eocene|Of Wangerrip Group. Called Dilwyn Clay by Baker (1953). Outcrops indistinguishable from Wiridjil Gravel or Moomowroong Sand. VandenBerg (2009) recommends that inland outcrops be mostly reassigned to Wiridjil Gravel. Overlies Gellibrand Marl. Sandy clay and silt||||||28-MAY-13
5489|Dilwyn Formation|66012|4|Described|p4, p6, p10 Tb.1, p17, p27, p30 Tb.3|Eocene|Paleocene|Seen in water bores. Channel gravel deposits and clean quartz sand, with thin interbeds of clayey sand and brown coal. Unconformably overlain by Heytesbury Group. 40m thick. Fluvial and swamp deposit. Northern extension of Wangerrip Group and probably Olney Formation| | ||||16-FEB-15
5489|Dilwyn Formation|66245|5|Briefly described|p6 Fig.5. |Lutetian|Thanetian|||Unit in Wangerrip Group.||Overlies Pember Mudstone and Eastern View Formation.||
5489|Dilwyn Formation|67061|6|Mentioned|p546 Fig.3.|Eocene|Eocene|||Unit in Wangerrip Group.||||
5489|Dilwyn Formation|67366|5|Briefly described|p103 Fig.2. |Eocene|Eocene|||Unit in Wangerrip Group.||Overlies Pember Mudstone. Is unconformably overlain by Mepunga Formation.|Shallow to nearshore marine sandstone and shale.|
5489|Dilwyn Formation|67367|5|Briefly described|p131 Fig.2. |Middle Eocene|Early Eocene|||Unit in Wangerrip Group.||||
5489|Dilwyn Formation|68211|6|Mentioned|p28 Fig.1|Neogene|Paleogene|||||||
5489|Dilwyn Formation|68811|5|Briefly described|p110, p130, p156 app 1, p192 tbl 46|Tertiary|Tertiary|Hosts a confined aquifer. Up to 800m thick.  ||||Overlain by Gambier Limestone.|Interbedded quartz sand, finer grained sediment and clay horizons.|16-APR-20
5489|Dilwyn Formation|69297|5|Briefly described|p79, p98|Lutetian|Ypresian|Otway Basin.||Wangerrip Group||Overlies the Pember Mudstone. Unconformably overlain by the Mepunga Formation.|Siltstone and shale.|
5489|Dilwyn Formation|69651|5|Briefly described|p10|Eocene|Eocene|||Wangerrip Group.||Overlies Pember Mudstone. Is overlain unconformably by Mepunga, Demons Bluff and Eastern View Formations. Locally abuts Eastern View Formation.||
5489|Dilwyn Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin.||Wangerrip Group.||Partly equivalent to and partly overlies Pember Mudstone. Is overlain by Mepunga Formation.||
5489|Dilwyn Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Pember Mudstone. Is overlain by Mepunga Formation (Nirranda Group).||
5489|Dilwyn Formation|70193|6|Mentioned|p285 fig 3|||||||||
5489|Dilwyn Formation|70880|6|Mentioned|p77|Eocene|Eocene|Otway Basin.||||||
5489|Dilwyn Formation|71266|6|Mentioned|p614 Fig.3|Eocene|Eocene|Otway Basin.||||||
5489|Dilwyn Formation|71437|4|Described|Fig. 1 opp 154, p155, p159-161|Paleocene|Paleocene|[After Dilwyn Clay of Baker (1953)] Mainly of near-shore to lagoonal, brackish to fresh-water environment.||Upper unit of Wangerrip Group.|Includes Pember Mudstone Member, Dartmoor Sand Member.|Transitional or interfingering with Dartmoor Sand Member.|Laminated micaceous shales with minor layers of dolomite and clean to silty well-sorted quartz sands.|
5489|Dilwyn Formation|73357|5|Briefly described|p24, p28-29, p44, p46, p48|Bartonian|Ypressian|Otway Basin. Correlated with multiple biozones including Malvacipollis diversus Spore-Pollen Zone in lower part, Achilleodinium biformoides Dinocyst Zone in upper part. Often marginal to nearshore marine depositional environments, and Nothofagidites asperus Spore-Pollen Zone in upper part with variable non-marine to nearshore marine depositional environments.||Of Wangerrip Group?||Overlies Pember Mudstone, underlies Mepunga Formation.||
5489|Dilwyn Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p24-25, p213, p246-247|Eocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P9 which has low Th/Sc values and high Si/Al values, Fe and P concentrations decrease upwards. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, and using the Herron classification (1988) includes quartz arenite, Fe-sand, sub-litharenite and subarkose. See also vi, p11 Tb.3.9, p82, p118, p131, p137-138, p258, p264-265.||Wangerrip Group||Overlies Pember Mudstone, underlies Nirranda Group, Mepunga Formation|Quartz-rich sandstone.|
5489|Dilwyn Formation|73385|5|Briefly described|p5|Eocene|Eocene|Otway Basin.||Wangerrip Group||Overlies Pember Mudstone, underlies Nirranda Group, Mepunga Formation.|Shallow marine and nearshore sandstones.|
5489|Dilwyn Formation|73386|4|Described|p4, p6, p12-13, Attachment A1|Bartonian|Ypressian|Otway Basin. Fluvial-deltaic to shallow-marine (inner shelf) depositional environment. Exhibits a stacked, aggradational stratal geometry that is thickest in the Portland Trough. Lower Malvacipollis diversus to Lower Nothofagidites asperus spore-pollen subzones.||Wangerrip Group||Overlies Pember Mudstone, underlies Mepunga Formation, Nirranda Group|Sandstones and mudstones, characterised by a sequence of clean, blocky marginal marine sandstones which transition upwards to a series of prograding parasequence sets.|
5489|Dilwyn Formation|73594|5|Briefly described|p4|Eocene|Eocene|Otway Basin.||Wangerrip Group||Overlies Pember Mudstone|Shallow marine and nearshore sandstones.|
5593|Doncaster Member|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3|Barremian|Barremian|See also p497-498, p499. Eromanga Basin. 100-200m thick.||Unit in Wallumbilla Formation.||Equivalent to lower part of Bulldog Shale.|Marine carbonaceous mudstone with minor siltstone and fine-grained labile glauconitic sandstone; rich fauna, predominantly molluscs, in the calcareous strata; fossil logs locally common.|
5593|Doncaster Member|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Wallumbilla Formation||||
5593|Doncaster Member|22757|5|Briefly described|Table6,p11||Early Cretaceous|275 m. Wallumbilla Formation, Rolling Downs Group, Surat Basin.||||||
5593|Doncaster Member|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Aptian|Aptian|Of the Wallumbilla Formation (Rolling Downs Group). Siltstone and fine sandstone. Become the Wittabrenna beds in Tibooburra area. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6.||||||
5593|Doncaster Member|22865|5|Briefly described|Table22.1p296-7|Aptian|Aptian|||||||
5593|Doncaster Member|23183|6|Mentioned|p222|||||||||
5593|Doncaster Member|23224|5|Briefly described|p3||Aptian|Of McMinn 1981. Hosts Opal Deposits in White Cliffs. Of Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
5593|Doncaster Member|23430|4|Described|p523 + p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province.||||||
5593|Doncaster Member|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation, Eromanga Basin.||||||14-APR-08
5593|Doncaster Member|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Geological Province: Great Australian Superbasin.||||||
5593|Doncaster Member|23982|5|Briefly described|p57|||Of the Wallumbilla Formation. Geological Province: Great Artesian Basin.||||||14-APR-08
5593|Doncaster Member|24085|5|Briefly described|Not recorded|Albian|Aptian|Of Wallumbilla Formation.||||||
5593|Doncaster Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|30020|6|Mentioned|p40|||||||||
5593|Doncaster Member|30021|6|Mentioned|p87|||||||||
5593|Doncaster Member|30024|6|Mentioned|p331|||||||||
5593|Doncaster Member|30042|4|Described|p4|||Description of cores DM Wanaarine DDH1 & DM Weilmoringle DDH1.||||||
5593|Doncaster Member|30443|6|Mentioned|p2|||Map legend, also on P4. Aptian age.||||||
5593|Doncaster Member|30446|6|Mentioned|p39|||||||||
5593|Doncaster Member|30691|4|Described|p17|||See also P19,21,Table 4,6,7. Lower-Upper Cretaceous||||||
5593|Doncaster Member|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
5593|Doncaster Member|30696|4|Described|Table 4|||Aptian age||||||
5593|Doncaster Member|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30854|4|Described|Table 4|||Lower Cretaceous||||||
5593|Doncaster Member|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
5593|Doncaster Member|31116|4|Described|p43|||See also P44||||||
5593|Doncaster Member|31208|6|Mentioned|Table 1|||See also Figs.2,3,5,6,7. Aptian.||||||
5593|Doncaster Member|31209|6|Mentioned|p159|||||||||
5593|Doncaster Member|31376|6|Mentioned|Table P4|||||||||
5593|Doncaster Member|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31432|4|Described|Table 1|||L.Cretaceous||||||
5593|Doncaster Member|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32314|6|Mentioned|Fig. 4|||||||||
5593|Doncaster Member|32797|4|Described|Table 4|||L.Cret.||||||
5593|Doncaster Member|33016|6|Mentioned|p1|||On table||||||
5593|Doncaster Member|33017|6|Mentioned|p2|||||||||
5593|Doncaster Member|33070|4|Described|Table 2|||||||||
5593|Doncaster Member|33071|6|Mentioned|p6|||L.Cret.||||||
5593|Doncaster Member|33072|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33075|6|Mentioned|p445|||||||||
5593|Doncaster Member|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33088|4|Described|Table 3|||Wallumbilla Fm.||||||
5593|Doncaster Member|33090|4|Described|Table 4|||L.Cret.||||||
5593|Doncaster Member|33091|5|Briefly described|p9|||Stratigraphy||||||
5593|Doncaster Member|33092|5|Briefly described|p6|||Strat. table||||||
5593|Doncaster Member|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
5593|Doncaster Member|33368|6|Mentioned|p25|||Strat.table.||||||
5593|Doncaster Member|33372|6|Mentioned|p20|||||||||
5593|Doncaster Member|33414|6|Mentioned|p212|||Part of Wallumbilla Formation.||||||
5593|Doncaster Member|33448|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33449|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33638|5|Briefly described|Table 1|||||||||
5593|Doncaster Member|33639|5|Briefly described|Table 2|||.Cret.||||||14-APR-08
5593|Doncaster Member|33640|4|Described|Table 2|||L.Cret.||||||
5593|Doncaster Member|33642|6|Mentioned|147-8,151,Tb.1,Fig.2|||Refes Vine & Day (1965).  Contains Roma fauna.||||||
5593|Doncaster Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33646|6|Mentioned|p16|||Geol. history.||||||
5593|Doncaster Member|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33648|6|Mentioned|p21|||Stratigraphy.||||||
5593|Doncaster Member|33672|6|Mentioned|p44|||||||||
5593|Doncaster Member|33673|6|Mentioned|p287|||||||||
5593|Doncaster Member|34091|5|Briefly described|Table 1|||L.Cret.||||||
5593|Doncaster Member|34172|6|Mentioned|p54|||||||||
5593|Doncaster Member|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|34613|4|Described|Table 4|||||||||
5593|Doncaster Member|35239|6|Mentioned|p265|||||||||
5593|Doncaster Member|35560|6|Mentioned|p291|||||||||
5593|Doncaster Member|35663|6|Mentioned|p126|||||||||
5593|Doncaster Member|35793|6|Mentioned|Fig.3|||||||||
5593|Doncaster Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
5593|Doncaster Member|36251|6|Mentioned|Fig.2|||||||||
5593|Doncaster Member|36552|6|Mentioned|p59|||||||||
5593|Doncaster Member|36571|6|Mentioned|p101|||See also Table 4||||||
5593|Doncaster Member|36574|6|Mentioned|p602|||||||||
5593|Doncaster Member|37608|6|Mentioned|p324|||||||||
5593|Doncaster Member|37995|4|Described|p66|||||||||
5593|Doncaster Member|38199|6|Mentioned|p426|||||||||
5593|Doncaster Member|38226|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|38373|6|Mentioned|p619|||||||||
5593|Doncaster Member|38374|6|Mentioned|p605|||||||||
5593|Doncaster Member|38814|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|39070|4|Described|p364|||||||||
5593|Doncaster Member|39211|5|Briefly described|Fig.3|||See also Figs 7-9,11-16, etc. Correlation||||||
5593|Doncaster Member|39212|4|Described|p18|||Excursion site. See also P40||||||
5593|Doncaster Member|39215|6|Mentioned|p53|||||||||
5593|Doncaster Member|39216|6|Mentioned|p55|||Fauna||||||
5593|Doncaster Member|39478|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|39846|6|Mentioned|p44|||||||||
5593|Doncaster Member|39847|6|Mentioned|p38|||||||||
5593|Doncaster Member|39989|4|Described|p423|||||||||
5593|Doncaster Member|40199|6|Mentioned|Fig.2|||||||||
5593|Doncaster Member|40245|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40249|6|Mentioned|p38|||Mention P41||||||
5593|Doncaster Member|40541|4|Described|p111|||||||||
5593|Doncaster Member|40666|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40687|3|Fully described|p418|||||||||
5593|Doncaster Member|40801|6|Mentioned|p65|||||||||
5593|Doncaster Member|40832|3|Fully described|p457|||||||||
5593|Doncaster Member|40833|6|Mentioned|p468|||||||||
5593|Doncaster Member|40926|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40962|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|41064|6|Mentioned|p60,p62|||See also Fig.4||||||
5593|Doncaster Member|41086|3|Fully described|Fig.3|||||||||
5593|Doncaster Member|41088|6|Mentioned|p143|||||||||
5593|Doncaster Member|41196|6|Mentioned|Fig.1|||||||||
5593|Doncaster Member|41198|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|41219|6|Mentioned|Fig.4|||||||||
5593|Doncaster Member|41266|6|Mentioned|Fig.3|||||||||
5593|Doncaster Member|41523|6|Mentioned|p276|||||||||
5593|Doncaster Member|42071|6|Mentioned|p117|||||||||
5593|Doncaster Member|42429|5|Briefly described|Fig.3 P155|||||||||
5593|Doncaster Member|42446|6|Mentioned|p20|||||||||
5593|Doncaster Member|42494|5|Briefly described|Table 1 P24|||||||||
5593|Doncaster Member|42673|5|Briefly described|Fig.2, P184|||||||||
5593|Doncaster Member|43008|5|Briefly described|map legend|||of Wallumbilla Formation.||||||14-APR-08
5593|Doncaster Member|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
5593|Doncaster Member|43989|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
5593|Doncaster Member|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
5593|Doncaster Member|44082|6|Mentioned|p6,8,10,16,22,26,34||Aptian|Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
5593|Doncaster Member|44087|14|Not recorded|p4,opp.7|||||||||
5593|Doncaster Member|44089|14|Not recorded|not on card|||||||||
5593|Doncaster Member|44099|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
5593|Doncaster Member|44346|14|Not recorded|p4|||||||||
5593|Doncaster Member|44373|14|Not recorded|p19-21|||Contains new species of ammonite Lithancylus Australia||||||
5593|Doncaster Member|44374|14|Not recorded|p10-12||Aptian|Remanie (reworked) fossils from this, in Coreena Member preferred explanation to extending time ranges of Roma or Tambo species.||||||
5593|Doncaster Member|44376|14|Not recorded|p3,4,12-14,16,20,22,|||p24. Of Wallumbilla Formation. Fossils.||||||
5593|Doncaster Member|44406|14|Not recorded|p4,opp.p6|||Basal member of Wilgunya Formation.||||||
5593|Doncaster Member|44408|14|Not recorded|p4,opp.p6|||||||||
5593|Doncaster Member|44414|14|Not recorded|p111,112,114||Cretaceous|||||||
5593|Doncaster Member|44417|2|Defined|p416-418,420|||Aptian fossils.||||||
5593|Doncaster Member|44668|14|Not recorded|p59,63|||||||||
5593|Doncaster Member|44915|14|Not recorded|p18||Early Cretaceous|Ref. to Vine and Day 1965.||||||
5593|Doncaster Member|45104|6|Mentioned|p35|||||||||
5593|Doncaster Member|45110|2|Defined|p115|Aptian|Aptian|Member of Wallumbilla Fm., formerly Wilgunya Fm. See also P10.||||||
5593|Doncaster Member|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
5593|Doncaster Member|46791|4|Described|p44|||||||||
5593|Doncaster Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
5593|Doncaster Member|46939|6|Mentioned|Fig.1|||||||||
5593|Doncaster Member|46984|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
5593|Doncaster Member|48919|4|Described|p71|||See also P72. L.Cretaceous||||||
5593|Doncaster Member|48920|3|Fully described|p58|||See also Table 8. Refers Vine & Day (1965).||||||14-APR-08
5593|Doncaster Member|48951|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
5593|Doncaster Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
5593|Doncaster Member|60331|5|Briefly described|p34 Fig.3|Aptian|Aptian|Of the Wallumbilla Formation. Overlain by Jones Valley Member and Coreena Member. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|61312|5|Briefly described|p64, p67 Fig.E5|Aptian|Aptian|Of the Wallumbilla Formation. Mudstone. Interbedded with siltstone and fine sandstone of the Coreena Member. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
5593|Doncaster Member|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||Unit in Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|63979|6|Mentioned|p48, Fig. 44|||Of Wallumbilla Formation. Underlies Coreena Member.||||||07-FEB-11
5593|Doncaster Member|64856|3|Fully described|p98-101|Aptian|Aptian|Vine and Day (1965). Lower Member of Wallumbilla Formation. Forms the lower part of Wilgunya Formation in the northern Eromanga Basin. Comprises mainly mudstone with subordinate siltstone, sandstone. Associated with palynofloral unit APK3, contains late Aptian faunas, and dinoflagellate assemblages equivalent to units ADK17 and 18.| | ||||28-NOV-17
5593|Doncaster Member|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Wallumbilla Formation. Underlies the Coreena Member; overlies the Bungil Formation.||||||22-MAR-12
5593|Doncaster Member|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation? Underlies the Coreena Member, Overlies the Bungil Formation.||||||
5593|Doncaster Member|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||Of Wallumbilla Formation?||||||
5593|Doncaster Member|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation. Underlies the Coreena Member, Overlies the Bungil Formation in the Surat Basin.||||||
5593|Doncaster Member|65119|6|Mentioned|p512 Fig 6, p521 Fig 14|||Present in the Cabawin 1, Flinton 1 and MacIntyre 1 wells.||||||07-MAR-12
5593|Doncaster Member|65384|5|Briefly described|S116, S118|||Probably Aptian. Of Wallumbilla Formation. Dominated by a marine shelf depositional environment.||||||21-DEC-10
5593|Doncaster Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
5593|Doncaster Member|66623|3|Fully described|p239, p242, pp256-261.|Aptian|Aptian|Correlates with superseded Wittabrenna and Oornoo Beds (Rose and Brunker 1969) and informal Wittabrenna Shale (Morton 1982). Hosts the White Cliffs opal field. Very poorly exposed. Thickness from 150 m to 300 m. Contains a wide range of fossils.||Unit in Wallumbilla Formation.||Disconformably overlies Cadna-owie Formation. Is disconformably and gradationally overlain by Coreena Member.|Grey, muddy sandstone and siltstone; local large spherical calcareous concretions and cone-in-cone carbonate; black shale and minor sandstone with abundant dropstones; black pyritic and bioturbated mudstone, claystone, shale, micritic limestone.|07-JUN-13
5593|Doncaster Member|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Wallumbilla Formation||||
5593|Doncaster Member|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67133|5|Briefly described|p17|Early Cretaceous|Early Cretaceous|Deposited during a rapid transgression episode.||Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Is overlain by Coreena Member.|Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Cadna-owie Formation. Is overlain by Coreena Member of Wallumbilla Formation.|Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67784|5|Briefly described|p25, p26, p28-33|Aptian|Aptian|Age derived from biostratigraphy. 120-150m thick. Northern Eromanga Basin.||Wallumbilla Formation||Overlies Cadna-owie Formation. Is overlain by Jones Valley Member/Coreena Member.|Thick mudstone unit|08-FEB-18
5593|Doncaster Member|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Unit in Wallumbilla Formation.||Is overlain conformably by Coreena Member.|Mudstone with subdominant siltstone.|
5593|Doncaster Member|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||||
5593|Doncaster Member|68206|6|Mentioned|p32-33|Aptian|Aptian|Carpentaria, NE Eromanga Basins.||Wallumbilla Formation.||||
5593|Doncaster Member|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|68593|5|Briefly described|p4, p46|Early Cretaceous|Early Cretaceous|||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.|Mudstone with subordinate siltstone.|
5593|Doncaster Member|68734|5|Briefly described|p218 Fig.2|Aptian|Barremian|Eromanga Basin (NE) and Surat Basin. Shallow marine.||Of the Wallumbilla Formation.||||16-JAN-17
5593|Doncaster Member|68821|6|Mentioned|p295|||Surat Basin. Equivalent to the Bulldog Shale.|||||Comprises pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
5593|Doncaster Member|69001|6|Mentioned|p30|Cretaceous|Cretaceous|||Of the Rolling Downs Group.||||
5593|Doncaster Member|69379|5|Briefly described|map legend|Cretaceous|Cretaceous|||Of Wallumbilla Formation|||Carbonaceous mudstone, siltstone, minor siltstone [?]; some glauconitic and calcareous; shelly fossils|03-SEP-14
5593|Doncaster Member|69457|5|Briefly described|p41:3, 10|Early Cretaceous|Early Cretaceous|Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
5593|Doncaster Member|69594|4|Described|p519, p526, p528-529, p538|Albian|Barremian|Vine et al. (1965). Eromanga, northern Surat Basins. Previously known as the Blackdown Formation of Laing and Power (1959); Woods (1961). 50-60m thick in outcrop; may be up to 150m thick subsurface. Has an abundant and diverse fossil fauna (listed). Represents maximum flooding of the Great Australian Superbasin with shallow-marine to basinal-marine deposits with contemporary volcanic detritus.||Basal Wallumbilla Formation.||Conformably overlies Cadna-owie, Bungil, Gilbert River Formations. Is overlain conformably by Jones Valley, Coreena Members.|Mudstone, siltstone, concretionary limestone and lesser labile and glauconitic sandstone. Sporadically fossiliferous.|
5593|Doncaster Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Wallumbilla Formation||Overlies Wyandra Sandstone Member, overlain by Coreena Member||
5593|Doncaster Member|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||Unit in Wallumbilla Formation.||||
5593|Doncaster Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|||Marine mudstone and subordinate siltstone.|20-JAN-22
5593|Doncaster Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|||Marine mudstone and lesser siltstone.|20-JAN-22
5593|Doncaster Member|70720|5|Briefly described|p6, p24-25|Aptian|Aptian|Eromanga Basin.||Wallumbilla Formation.||Nonconformably overlies Granite Springs Granite. Is overlain by Coreena Member.||
5593|Doncaster Member|70821|4|Described|p21-22 Figs.2.6-7, p28, p30-31, p33, p72|Early Cretaceous|Early Cretaceous|See also p80, p82, p86-89, p111-112, p115-116. Eromanga and Surat Basins. Varying thicknesses given (65-241m) from wells. Shallow to deep marine deposits. Contains a diverse, mostly marine, biota (molluscs, reptiles, fish). Appears as Doncaster Formation on p30. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Highly conductive. Hydrostratigraphic properties.||Wallumbilla Formation.||Overlies Wyandra Sandstone Member (Cadna-owie Formation), Hooray Sandstone or Minmi Member (Bungil Formation). Is overlain conformably by Coreena Member. Equivalent to lower Bulldog Shale.|Mudstone, dark, glauconitic; minor sandstone and siltstone; partly calcareous.|
5593|Doncaster Member|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Aptian.||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
5593|Doncaster Member|71251|5|Briefly described|p11-13, p15, p17, p49|||Eromanga Basin. Natural gamma wireline log. Conductivity diagram.||Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|71863|5|Briefly described|p5|Aptian|Aptian|Eromanga Basin.||Wallumbilla Formation||Overlies the Wyandra Sandstone Member. Overlain by the Coreena Member.||
5593|Doncaster Member|71864|6|Mentioned|p13-p14, p17|||Could not be distinguished in GSQ Eulo 2 borehole.||Wallumbilla Formation||||
5593|Doncaster Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Wallumbilla FZ.||Overlies Cadna-owie and Bungil FZs; Kumbarilla and Ronlow beds. Is overlain by Coreena Member.||
5593|Doncaster Member|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous|Hosts White Cliffs opal.||Wallumbilla Formation||||
5603|Donington Suite|24197|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Age: ~1850Ma. Geological province: Gawler Craton. Same as the Donington Granitoid Supersuite?||||||07-FEB-11
5603|Donington Suite|24360|6|Mentioned|p54|||Equivalents of Donington Suite. Geological Province: Gawler Craton.||||||
5603|Donington Suite|24505|5|Briefly described|p4, p5 Fig. 1|||Granitoids. Geological Province: Gawler Craton.||||||
5603|Donington Suite|24508|5|Briefly described|p30|Proterozoic|Paleoproterozoic|Series of intrusives ranging in composition from gabbronorite to leucogranite and including charnockites. Geological Province: Gawler Craton.||||||23-DEC-09
5603|Donington Suite|24585|6|Mentioned|p32|||Includes the Gleesons Landing Granite.||||||
5603|Donington Suite|41682|6|Mentioned|p14|||||||||
5603|Donington Suite|50605|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1840Ma.||||||07-NOV-08
5603|Donington Suite|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
5603|Donington Suite|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartz-gabbronorite, hypersthene gneissic granite, syenogranite, adamellite, granodiorite, tonalite, megacrystic granitoid gneiss. 1855-1850Ma. Geological Province: Gawler Craton.||||||07-NOV-08
5603|Donington Suite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Acid to mafic intrusives. Emplacement: ~1850Ma (U-Pb Zircon). Includes gabbronorite, enderbite, charnockite and alkali granite, plus granite gneiss. Geological Province: Gawler Craton.||||||12-JAN-10
5603|Donington Suite|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-gabbronorite, hypersthene gneissic granite, syenogranite, adamellite, grandiorite, tonalite, megacrystic granitoid gneiss.  Age: 1855-1850Ma. Geological Province: Gawler Craton.||||||07-NOV-08
5603|Donington Suite|61393|5|Briefly described|p169. |Paleoproterozoic|Paleoproterozoic|Granitic terrane.|1850 Ma.|||||
5603|Donington Suite|61522|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
5603|Donington Suite|61725|5|Briefly described|p890|Paleoproterozoic|Paleoproterozoic|See also Donington Suite granitoids.||||||07-NOV-08
5603|Donington Suite|62729|5|Briefly described|p39 Fig. 1b, p40|Paleoproterozoic|Paleoproterozoic|Age: ~1850 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
5603|Donington Suite|63223|5|Briefly described|p16, p17 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma. Forms an extensive batholith extending from southern Yorke Peninsula to the Olympic Dam region. Intrudes Corny Point Paragneiss.||||||08-JUL-13
5603|Donington Suite|63398|5|Briefly described|p663|Paleoproterozoic|Paleoproterozoic|Age: ca 1855-1849Ma (Zang 2002b, 2006). See also Fig. 2. ||||||07-NOV-08
5603|Donington Suite|63866|4|Described|p5, p19-p20, p31|Orosirian|Orosirian|Cleve and Spencer Domains, Gawler Craton. Age range is derived from several U-Pb zircon ages via TIMS, SHRIMP and Kober evaporation methods. The quartz gabbronorite from this unit is the QGNG standard of ANU. Rocks were derived from fractionation of mafic magma that incorporated significant crustal material.|c. 1850-1840 Ma||Includes the Middlecamp Granite and the Refuge Rock Granite.|Intrudes the Hutchison Group. Intruded by the Tournefort mafic dykes.|Quartz gabbronorite to evolved leucogranites.|
5603|Donington Suite|64130|5|Briefly described|p1378 Fig.1, p1379, p1380 Fig.2   |Paleoproterozoic|Paleoproterozoic|See also p1381, p1384, p1836 Fig.5, p1388 Fig.6. Eastern margin of Gawler Craton.|ca. 1850 Ma|||||
5603|Donington Suite|64132|5|Briefly described|p1418, pp1420-1421, p1424, p1432. |Paleoproterozoic|Paleoproterozoic|Oldest known basement lithologic units in the Olympic Dam district.|1860 +/- 4 to 1850 +/- 3.5 Ma (Jagodzinski 2005).|||Is overlain nonconformably by Pandurra Formation.|Voluminous, intensely deformed syntectonic granitoids.|
5603|Donington Suite|64133|5|Briefly described|p1443-1445, p1449, p1456-1457|Paleoproterozoic|Paleoproterozoic|Se also p1460 Tb.5, p1464 Fig.15.|Between 1860 +/- 4 Ma and 1850 +/- 3.5 Ma.||||Voluminous syntectonic granitoids.|
5603|Donington Suite|64137|5|Briefly described|p1542 Fig.1  |Paleoproterozoic|Paleoproterozoic|||||||
5603|Donington Suite|64233|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Age: ~1850Ma. Magmatic unit on SW tip of Yorke Peninsula.||||||07-NOV-08
5603|Donington Suite|64282|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geol Prov: Gawler Craton/Yorke Peninsula. Age: 1855-1850Ma. Quartz-gabbronorite, hypersthene gneissic granite, syenogranite, adamellite, granodiorite, tonalite, megacrystic granitoid gneiss.||||||07-NOV-08
5603|Donington Suite|64313|5|Briefly described|p450, p457|Paleoproterozoic|Paleoproterozoic|Intrusive magmatic complex of dominantly granitic + monzonitic rocks - ranging from gabbro, gabbronorite, charnockite, granodiorite to alkali granite; also includes Colbert Granite formerly known as Colbert Suite. Age: 1850Ma. Geol. prov: Gawler Craton.||||||09-FEB-10
5603|Donington Suite|64576|6|Mentioned|p625 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: c. 1850Ma.||||||
5603|Donington Suite|64722|5|Briefly described|Fig. 2 p3-6, p13, 26|Orosirian|Orosirian|Geochemical data suggest a convergent plate margin depositional setting.|1865-1845 Ma.|||||11-APR-12
5603|Donington Suite|64741|6|Mentioned|p298, p299 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1860-1850Ma. Geological province: Gawler Craton. Intrusives.||||||07-FEB-11
5603|Donington Suite|65219|4|Described|p26-30|Paleoproterzoic|Paleoproterzoic|U/Pb zircon ages for the Suite span ~14 m.y., from ~1858 Ma. Shear zones, dykes and other structural fabrics constrain the age to >1846 Ma, and demonstrate the ~1850 Ma Cornian Orogeny, prior to the 1730-1690 Kimban Orogeny.||||||22-SEP-09
5603|Donington Suite|65221|5|Briefly described|p26, p32|Palaeoproterozoic|Palaeoproterozoic|Granitic to charnockitic intrusives c.1850||||||21-SEP-09
5603|Donington Suite|65375|4|Described|pp12-15, p18, pp44-45.|Paleoproterozoic|Paleoproterozoic|Spencer Domain. Formerly Donington Granitoid Suite (Schwarz 2003). Dominates the basement in southern portion of Yorke Peninsula. Type locality at Cape Donington. Shows four distinct deformation structures and fabrics.|c.1855-1835 Ma.||Includes Gleesons Landing and Royston Granites and Jussieu Metadolerite.|Intruded by Jussieu Metadolerite.|Mafic intrusives, quartz gabbronorite, hypersthene gneissic granite, syenogranite, adamellite, granodiorite and megacrystic granitoid gneiss.|
5603|Donington Suite|65376|5|Briefly described|p8 Fig.1.1, p54, p70. |Paleoproterozoic|Paleoproterozoic|A granitic batholith outcropping in southern Gawler Craton with equivalents along a strike length of >600 km. High-grade metamorphism and complex deformation from 1730-1700 Kimban Orogeny. Revised geochronology implies rapid emplacement.|c.1850 +/- 2 Ma.||Includes Colbert Granite and Memory Cove Charnockite.||Contains a range of lithologies including charnockite, gabbronorite and granodiorite through to megacrystic granites, as well as co-magmatic dykes.|
5603|Donington Suite|65483|6|Mentioned|p17 Fig. 1|Palaeoproterozoic|Palaeoproterozoic|||||||
5603|Donington Suite|65485|6|Mentioned|p42, Fig 1|Paleoproterozoic|Paleoproterozoic|c.1850 Ma granitoids of this Suite are juxtaposed against the Sleaford Complex and Hutchison Group by the Kalinjala Shear Zone.||||||19-MAR-12
5603|Donington Suite|65772|6|Mentioned|p228-229, p229 Fig.2, p234 Fig.8|Orosirian|Orosirian|~1850 Ma. Also referred to as Donington Granitoid suite on p228.||||||
5603|Donington Suite|65915|5|Briefly described|p2, p3 Fig.2, p5-6, p18|Orosirian|Orosirian|Granites. Also referred to as Donington Granitoid Suite in Fig.2. Includes previously named Lincoln Complex rocks. ~1850 Ma.||||||
5603|Donington Suite|65922|5|Briefly described|p9, p13 Fig. 4, p30|Orosirian|Orosirian|Age of ~1850-1840 Ma given. Included in Lincoln Complex, Gawler region. Apparently restricted to east of the Kalinjala Mylonite Zone.||||||
5603|Donington Suite|66302|4|Described|p6,  p26- p29, p34, p57, p62, p87, p88|Orosirian|Orosirian|Spencer and Olympic Domains, Gawler Craton. [see also references for Donington Granitoid Suite: p4 Fig.3, p8]. Distribution and geochemistry discussed. Intruded during the Cornian Orogeny. Believed to have been intruded in a compressional magmatic arc environment or produced in a back arc environment which was then accreted onto the Gawler Craton. Age derived from SHRIMP dating of its constituent units. |ca. 1850 Ma||Includes the Memory Cove Charnockite, Gleesons Landing Granite, Royston Granite and the Colbert Granite.|Intrudes the Hutchison Group.|Mafic gabbro-norite to evolved leucogranites.|
5603|Donington Suite|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Gawler Craton. Likely source of zircons of this age found in Kooringa Member.|c.1850 Ma.|||||
5603|Donington Suite|66761|5|Briefly described|p244, 246|Paleoproterozoic|Paleoproterozoic|Present in PIRSA stratigraphic hole Investigator 1. 55m interval. Granite gneiss. Overlain by Winulta Formation.||||||14-MAR-12
5603|Donington Suite|66882|5|Briefly described|p102 Fig.2, p107, p114 Figs.11 & 12|Orosirian|Orosirian|See also p117, p119-120. A possible but minor source of sediments and zircons in Cleve Group.|c.1850 Ma  |||||
5603|Donington Suite|66916|5|Briefly described|p9, p14, p16|Paleoproterozoic|Paleoproterozoic|Basement in E Gawler Craton. Includes the granite at Punt Hill, regarded as a passive host for the Cu-Au-Zn-Pb mineralisation. Also includes the granite that hosts the IOCG mineralisation at Carrapateena.|c.1850 Ma.|||||
5603|Donington Suite|67058|5|Briefly described|p476, p491.|Paleoproterozoic|Paleoproterozoic|Emplacement was synchronous with the Cornian Orogeny, and followed by a period of widespread sedimentation.|c.1850 Ma.|||||
5603|Donington Suite|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 1850 Ma|||||
5603|Donington Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Voluminous: intrusions along a 600km N-trending belt throughout the eastern Gawler Craton; may have been part of an (accretionary) continental magmatic arc.|1850 +/- 2 Ma.|||||
5603|Donington Suite|67536|5|Briefly described|Map Legend|Orosirian|Orosirian|Gawler Craton.|1853 +/- 4 Ma - 1850 +/- 7 Ma||||Gneissic gabbronorite, charnockite and alkali-feldspar granite and mafic dykes.|
5603|Donington Suite|67581|6|Mentioned|p44 Fig.8, p45||||1860-1845 Ma.|||||
5603|Donington Suite|67721|5|Briefly described|p34, p35 Fig.6|Orosirian|Orosirian||c. 1850 Ma|||||
5603|Donington Suite|68131|4|Described|p2 Fig.1, p3 Tb.1, p5-8, p10, p15, p17|Paleoproterozoic|Paleoproterozoic|See also p20, p23, p27, p32, p40, p42-56, p61. Associated with the Neill Event and the Kimban Orogeny. Mapped with Middlecamp Granite and Moody Suite as a single unit. Issues of contamination by foreign zircons are dealt with in some detail. The age of 1848 +/- 8 Ma for a leucosome in the Corny Point Paragneiss, interpreted to be the crystallisation age of the leucosome, supports the conclusion of Zang and Fanning (2001) that the Donington Suite underwent upper amphibolite metamorphism at c.1850 Ma. Further dating indicates metamorphic recrystallisation during the Kimban Orogeny (1730-1700 Ma), possible isotopic disturbance during emplacement of the Hiltaba Suite, further resetting or new zircon growth at c.350 Ma, and recent Pb-loss due to weathering.|1846 +/- 3 Ma.||Gleesons Landing, Royston Granites; Corny Point Paragneiss; Wanna Megacrystic Granite Gneiss; Jussieu Metadolerite; Memory Cove Charnockite.|Is intruded by Spilsby Suite.|Felsic and lesser mafic igneous intrusive rocks; includes pegmatite and migmatite. Foliated biotite syenogranite; foliated megacrystic hornblende-biotite adamellite; intensely sheared augen gneiss.|13-MAY-20
5603|Donington Suite|68158|5|Briefly described|p5, p14-16|||Extends from SE Eyre Peninsula to the Olympic Dam region. Also includes the mafic Jussieu Dykes. Appears as Donnington Suite on p5. Sm-Nd values.|~1860-1850 Ma.||||Includes granite, gneiss, charnockite and gabbronorite.|
5603|Donington Suite|69004|5|Briefly described|p16, p18|Proterozoic|Proterozoic|Gawler Craton. Referred to as the Donington Granitoid Suite on p18.|||||Dominantly granitic gneiss, charnockite and quartz-bearing gabbronorite.|
5603|Donington Suite|69048|5|Briefly described|p2-3, p53|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula. Separated from the Sleaford Complex to the west by the Kalinjala Shear Zone.|c.1850 Ma.|||||
5603|Donington Suite|69203|5|Briefly described|p10|||Eastern Gawler Craton.|1860-1850 Ma.||||A large-volume felsic intrusive suite.|
5603|Donington Suite|69554|6|Mentioned|p128, 130, 139|||Mortimer et al. (1988). Eastern Gawler Craton.|c.1850 Ma.|||||
5603|Donington Suite|69591|6|Mentioned|p105 Fig.2.98|||Appears in a diagram of the geodynamic setting of ~1870-1820 Ma eastern Australia.||||||
5603|Donington Suite|69649|6|Mentioned|p6 Fig.4,|||||||||
5603|Donington Suite|70286|6|Mentioned|p884|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.|c.1860-1850 Ma.|||||
5603|Donington Suite|70382|5|Briefly described|p27, p32, p34, p35|Orosirian|Orosirian|Southern Yorke Peninsula region. Likely direct source for some of Quartoo Sand Member inherited zircon in the Eocene.|1846 +\- 23 Ma|||Overlain by the Wallaroo Group.|Granite gneiss.|
5603|Donington Suite|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1850 Ma|||||
5603|Donington Suite|70511|6|Mentioned|p86-87|Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1850 Ma.|||Surrounds (?is intruded by) Roxby Downs Granite.||
5603|Donington Suite|70657|5|Briefly described|p44|Orosirian|Orosirian|Gawler Craton. Unlikely as a source of sediments for Willyama Supergroup due to detrital zircon age spectrum in the latter unit.|c.1850 Ma.|||||
5603|Donington Suite|70721|5|Briefly described|p63, p71, p73|||Intruded and deformed during the Carnian Orogeny at c. 1850 Ma.|c. 1850 Ma||Includes the Royston Granite.|||
5603|Donington Suite|70738|6|Mentioned|p187-188|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Hosts the Wirrda Well Cu-Au prospect.|c.1850 Ma.||||Voluminous granitoids.|
5603|Donington Suite|70893|6|Mentioned|p3 fig 1a|Orosirian|Orosirian||c. 1850 Ma|||||
5603|Donington Suite|70947|5|Briefly described|p960, 961|Orosirian|Orosirian|Geological province: Gawler Craton. Intruded by Hiltaba Suite granites.|1850 Ma|||Intruded by Hiltaba Suite granites.||
5603|Donington Suite|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Miltalie Gneiss and older than Bosanquet Formation.||
5603|Donington Suite|71043|6|Mentioned|p104|Orosirian|Orosirian|Gawler Craton.|1850 Ma.|||||
5603|Donington Suite|71129|5|Briefly described|p14,17-18,23, p35, 203|Orosirian|Orosirian|Geological Province: Spencer and Olympic domains, Gawler Craton. Juvenile intrusive magmatism associated with c. 1850 Ma Cornian Orogeny, affecting the Olympic and Spence domains. Basement to Moonabie and Wandearah formations.|c. 1850 Ma|||Overlain by Wallaroo Group. Contemporaneous with Bosanquet Formation.||13-NOV-19
5603|Donington Suite|71235|6|Mentioned|p13||||c. 1850 Ma (Fanning et al, 2007)|||||
5603|Donington Suite|71236|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|||||||
5603|Donington Suite|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Spencer and Olympic Domains, Gawler Craton.|1850 Ma|||||
5603|Donington Suite|71322|5|Briefly described|p136|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.||||||
5603|Donington Suite|71341|6|Mentioned|p179 fig 1, p188 fig 7, p198|Palaeoproterozoic|Palaeoproterozoic|Misspelt as the Donington Suit on p198.|ca. 1870-1850 Ma|||||
5603|Donington Suite|71348|6|Mentioned|p201|Orosirian|Orosirian|Geological province: Gawler Craton.||||||
5603|Donington Suite|71534|5|Briefly described|p295-296,300-301,303|Orosirian|Orosirian|Geological province: Gawler Craton. Emplacement is associated with c. 1850-1830 Ma Cornian Orogeny and ensuing short-lived deformation and metamorphism, adjacent to Cooyerdoo Granite and associated Mesoarchean rocks and broadly corresponds in location to the Kalinjala Shear Zone.. Whole rock Nd isotope data suggest incorporation of ancient crust, however Hf isotope data indicates mantle input into Paleoproterozoic magmatism, resulting from lithospheric extension.|1850 Ma|||||
5603|Donington Suite|71536|6|Mentioned|p99|||||||||
5603|Donington Suite|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
5603|Donington Suite|71712|6|Mentioned|p410 Fig 1, p411|Orosirian|Orosirian|Also known as Donington granitoids on p411? Metamorphosed during 1730-1690 Ma Kimban Orogeny.|1850 Ma|||||
5603|Donington Suite|71859|5|Briefly described|p1-p6|||Southern Gawler Craton, Spencer and Olympic domains. Emplaced during the Cornian Orogeny.|c. 1850 Ma|||||
5603|Donington Suite|71862|5|Briefly described|p2-p4, p6, p12, p16, p21|||Emplaced during the Cornian Orogeny along the eastern margin of the Gawler Craton. Originally a part of the now obsolete Lincoln Complex.|c. 1850 Ma|||Faulted against the Sleaford Complex and the Hutchison Group.||
5603|Donington Suite|71895|4|Described|p10-p12, p28, p49, p51|Paleoproterozoic|Paleoproterozoic|This unit is interpreted as the basement of the Punt Hill region. Unconformably overlain by equivalents of the Wandearah Formation and Wallaroo Group rocks. Alteration,  mineralisation, spectral analysis and 3D geological models are discussed. See also  p55-p57, p61-p63, p89-p92, p116, p142-p144, APP1. p6-p7, APP1. p12-p13,  APP1. p16-p17,APP1. p19,  APP4. p4, APP4. p8, APP8. p201-p202. See also the Donington Granitoid Suite. Petrographic descriptions for numerous samples provided.|c. 1850 Ma|||Overlain by the Wallaroo Group.|Granites including monzogranites.|
5603|Donington Suite|72058|5|Briefly described|p172-p173, p174, p184, p186, p192|||Spencer Domain, Gawler Craton. Syn-orogenic. Emplaced during the Cornian Orogeny.|~1850 Ma||||Myrmekitic granitoids, mafic and felsic intrusives.|16-MAR-21
5603|Donington Suite|72090|6|Mentioned|p9-p10, p11|Orosirian|Orosirian|Eastern Gawler Craton.|1850 Ma|||||
5603|Donington Suite|72459|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Lincoln/Cleve domains of the Gawler Craton. Delineated in geophysics by ellipsoid anomalies of varying magnetic strength.||||||
5603|Donington Suite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
5603|Donington Suite|72484|5|Briefly described|p2, 5, 23|||Associated with the compressive Cornian Orogeny. Is cut by post-compresson Tournefort mafic dykes dated at 1812 +/- 15 Ma.|~1.85 Ga.||||Extensive emplacement of high-grade metamorphosed granites and charnockites.|
5603|Donington Suite|72488|5|Briefly described|p2 Fig.1, p3-7, 12 Fig.9, p14, 16|||Eastern Gawler Craton. Forms part of the basement to the Olympic Dam District. Hosts IOCG deposits (eg Wirrda Well). SHRIMP U-Pb zircon age of a granite by Jagodzinski (2005). An LA-ICP-MS age of hematite from granite breccia was determined at 1598.9 +/- 6.3 Ma (this study). Appears also as Donington Suite Granite or Donington granite.|1849.6 +/- 3.5 Ma.|||Is intruded by the Hiltaba Suite. Is overlain unconformably by the Gawler Range Volcanics.|Granitoid rocks; mylonite at shear zones.|
5603|Donington Suite|72949|6|Mentioned|p34|Orosirian|Orosirian||1.85 Ga|||||
5603|Donington Suite|73026|5|Briefly described|p4 fig1.2, p5, p7, p9-10,|Paleoproterozoic|Paleoproterozoic|Occurs along the eastern margin of the Gawler Craton on the Eyre Peninsula/Yorke Peninsula. Extends some 600km from the sothern most coastal outcrops to the vicinity of Olympic Dam. Enriched in elevated incompatible elements and LREE. See also  p13, p16, p18-p19, p24, p30.|c. 1850 Ma||Includes the Jussieu Metadolerite.||Granite gniess, metadolerite.|
5603|Donington Suite|73027|5|Briefly described|p4-p7, p9-10, p13-14|Palaeoproterozoic|Palaeoproterozoic|Eastern Eyre Peninsula/Yorke Peninsula. Within this suite the c. 1855-1840 Ma Cornian Orogeny is defined. See also p18 fig 2.4, p29, p45, p48.|c. 1860-1845 Ma||Includes the Jusseiu Metadolerite, Wanna Megacrystic Gneiss and the Memory Cove Charnockite.||Granite gneiss, metadolerite, migmatised granitic gneiss.|
5603|Donington Suite|73030|6|Mentioned|p2148-2150|Orosirian|Orosirian|Gawler Craton, Olympic Cu-Au Province.|ca. 1850 Ma|||||
5603|Donington Suite|73092|6|Mentioned|p1-2, p15, p18, p34, p41|Orosirian|Orosirian|Yorke Peninsula region.|c. 1850 Ma||Gleesons Landing Granite|||
5603|Donington Suite|73103|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.||||||
5603|Donington Suite|73104|6|Mentioned|p2||||||||Includes meta-igneous rocks.|
5603|Donington Suite|73107|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gawler Craton: Yorke Peninsula, islands of Investigator Strait and DDH Investigator 1.|1855-1850 Ma.||Royston Granite, Gleesons Landing Granite, Corny Point Paragneiss.||Quartz gabbronorite, hypersthene gneissic granite, syenogranite, adamellite, granodiorite, tonalite, megacrystic granitoid gneiss.|11-FEB-23
5603|Donington Suite|73110|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map below the main PORT AUGUSTA map.||||||
5603|Donington Suite|73122|5|Briefly described|p17-21, 23, 26-29, 34-35, 38-42|Palaeoproterozoic|Palaeoproterozoic|Yorke Peninsula and offshore islands, eastern Gawler Craton. Emplaced during the Cornian Orogeny.|1850-1843 Ma.|||Is intruded by Tournefort Metadolerite.|Fractionated series of felsic magmas including granite to charnockite.|
5603|Donington Suite|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
5603|Donington Suite|73155|6|Mentioned|p264 Fig.1|Orosian|Orosian|Gawler Craton.|1850 Ma|||||
5603|Donington Suite|73162|6|Mentioned|p449, Fig.1|Paleoproterozoic|Paleoproterozoic||1850 Ma|||||
5603|Donington Suite|73165|6|Mentioned|p619-620 Fig. 1, p621, p634-635, 638|Paleoproterozoic|Paleoproterozoic|Gawler Craton, eastern. Emplaced during compressional deformation in the Cornian Orogeny.|ca 1850 Ma||||Igneous rocks of mafic to felsic composition.|
5603|Donington Suite|73166|6|Mentioned|p644, 645, Fig. 1|Paleoproterozoic|Paleoproterozoic|Gawler Craton, eastern.|ca 1.85 Ga||||Granite and diorite intrusions, brecciated. Minor host rock in the Acropolis prospect.|
5603|Donington Suite|73234|6|Mentioned|p19|Orosirian|Orosirian|Eyre Peninsula, north-eastern. Age from Reid and Hand (2012)[?].|c. 1850 Ma||||Granitoids.|
5603|Donington Suite|73235|6|Mentioned|p52-53, p58|Orosirian|Orosirian|Gawler Craton. Olympic and Spencer regions.|1850 Ma|||||
5603|Donington Suite|73256|4|Described|p557-576|Orosirian|Orosirian|Gawler Craton, eastern. Continental back arc setting. High-grade contractional deformation (during Cornian Orogeny). Interpreted as derived from a mixture of mafic melt and crustal material. Hosts major IOCG deposits in the eastern part of the craton. [See article for petrographic descriptions, whole-rock geochemistry, and zircon morphological and compositional characterisation].|ca 1850 Ma||||Ranges in composition from gabbro, gabbronorite, charnockite, granodiorite to alkali granite.|
5603|Donington Suite|73298|6|Mentioned|p1073|Orosian|Orosian|Gawler Craton, eastern margin. Spencer and Olympic domains. Emplaced during the Cornian Orogeny.|ca 1850-1830 Ma|||||
5603|Donington Suite|73302|6|Mentioned|p33||||c.1850 Ma.|||||
5603|Donington Suite|73493|5|Briefly described|p711-713, p716-717, p722-723, p727|Orosirian|Orosirian|Gawler Craton, eastern. Co-magmatic with Jussieu Metadolerite. Associated with the Cornian Orogeny. See also p714 Fig.1, p715 Fig.2, p718 Fig.5, p725 Fig.12.|ca 1850 Ma|||Underlies Wallaroo Suite, Bridgewater Formation, intruded by Daly Head Metadolerite|Granitic to charnockitic. Includes orthogneiss.|
5603|Donington Suite|73525|5|Briefly described|p18-19|Orosirian|Orosirian|Gawler Craton.|ca. 1855-1845 Ma||Carcase Rock Granite, Memory Cove Charnockite, Colbert Granite, Gleesons Landing Granite, Jussieu Metadolerite, Royston Granite|||
5603|Donington Suite|73634|5|Briefly described|p1-8, 14, 16-17|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula, Gawler Craton. Associated with the Cornian Orogeny.|c.1850 Ma.|||Is intruded by Tournefort Metadolerite dykes.|Voluminous granites: pink granite gneiss, mafic megacrystic gneiss, quartz gabbronorite gneiss, quartz feldspar gneiss.|
5603|Donington Suite|73644|5|Briefly described|p2-3, p13-15|Paleoproterozoic|Paleoproterozoic|Emplaced and deformed during the Cornian Orogeny.|c. 1850 Ma||||Syenogranites, adamellites and granodiorites.|
5603|Donington Suite|74361|6|Mentioned|p163, 173|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Deformed by the Kimban Orogeny (~1730-1690 Ma).|~1850 Ma.|||||
5622|Doonbara Formation|22730|4|Described|p567-70|Miocene|Oligocene|after Wopfner 1974||||||
5622|Doonbara Formation|23336|5|Briefly described|p4|Miocene|Miocene|||||||21-MAR-06
5622|Doonbara Formation|29658|6|Mentioned|p5|||||||||
5622|Doonbara Formation|29660|6|Mentioned|p7|||||||||
5622|Doonbara Formation|30055|6|Mentioned|p153|||||||||
5622|Doonbara Formation|30056|6|Mentioned|p140|||||||||
5622|Doonbara Formation|30921|6|Mentioned|Map legend|Miocene|Miocene|||||||
5622|Doonbara Formation|30924|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
5622|Doonbara Formation|33820|6|Mentioned|Map legend|Miocene|Miocene|Prob. Miocene||||||
5622|Doonbara Formation|33827|6|Mentioned|p14|||See also Table 1||||||
5622|Doonbara Formation|33828|6|Mentioned|p11|||||||||
5622|Doonbara Formation|33937|4|Described|p6|||See also p7.||||||13-MAR-19
5622|Doonbara Formation|35149|6|Mentioned|Fig.4|||||||||
5622|Doonbara Formation|35691|6|Mentioned|p5|||||||||
5622|Doonbara Formation|35793|6|Mentioned|Fig.2|||||||||
5622|Doonbara Formation|38605|6|Mentioned|p35|||||||||
5622|Doonbara Formation|39322|6|Mentioned|Fig.3|||||||||
5622|Doonbara Formation|39445|5|Briefly described|Table 14|||||||||
5622|Doonbara Formation|39908|6|Mentioned|p10|||||||||
5622|Doonbara Formation|40910|6|Mentioned|p19|||||||||
5622|Doonbara Formation|41098|6|Mentioned|p177|||||||||
5622|Doonbara Formation|42746|5|Briefly described|p17|||||||||
5622|Doonbara Formation|42905|5|Briefly described|p23, Fig 5.3|||||||||
5622|Doonbara Formation|43053|5|Briefly described|Map Legend|Pleistocene|Tertiary|Undifferentiated Early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||25-MAY-05
5622|Doonbara Formation|43258|5|Briefly described|Map Legend|Pliocene|Paleocene|||||||
5622|Doonbara Formation|43298|6|Mentioned|Map Legend|Pleistocene|Tertiary|||||||
5622|Doonbara Formation|44133|5|Briefly described|p194, 190 Fig. 10.30|Early Pliocene|Late Miocene|Geological Province: Lake Eyre Basin. Thickness: 40m.||||||03-MAY-13
5622|Doonbara Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
5622|Doonbara Formation|60080|5|Briefly described|Map legend|Pliocene|Miocene|Brick-red ferruginous pisolitic silty-sandstone. Interfingers with Cadelga Limestone in the Haddon Syncline.||||||03-MAY-13
5622|Doonbara Formation|60953|5|Briefly described|Map Legend|Miocene|Eocene|Alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||27-APR-05
5622|Doonbara Formation|61108|5|Briefly described|map legend|Pleistocene|Paleocene|Undifferentiated early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silcreted or ferricreted. Geological Province: Lake Eyre Basin.||||||02-JUN-05
5622|Doonbara Formation|66131|4|Described|p240, p242 Fig.2, p245, p249.|Miocene|Miocene|~7-40 m thick. Pisolitic ferricrete is extensively developed in this unit in the northeastern and central parts of the Lake Eyre Basin.||||Overlies Eyre Formation or Cordillo Silcrete. Overlain by the Cadelga Limestone. equivalent to the Whitula Formation in Qld.|Pisolitic, ferruginous fine to medium sand.|25-AUG-22
5622|Doonbara Formation|66623|3|Fully described|pp270-272, pp282-284.|Miocene|Oligocene|Youngest lithified sedimentary rock in Koonenberry Belt: Late Oligocene - Early Miocene. Wopfner (1974) tentatively correlated with basal Etadunna Formation (in SA) and Namba Formation. Uplift of Cordillo Silcrete and Eyre Formation led to accelerated fluvial erosion and deposition of tens of metres of sandstone and conglomerate at the foot of fault scarps.||||Unconformably overlies Cordillo Silcrete.|Basal ferruginous silcrete conglomerate with reworked silcrete clasts; succeeded by distinctive brick-red, friable, ferruginous quartzose sandstone and granule conglomerate with maghemite pisoliths; bedding irregular, generally less than 20cm thick.|03-JUN-13
5622|Doonbara Formation|66922|5|Briefly described|Map legend|Neogene|Neogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|67119|5|Briefly described|Map legend.|Pliocene|Miocene|Fluvial facies.|||||Fine- to medium-grained, pisolitic and ferruginous sand.|
5622|Doonbara Formation|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|19-SEP-11
5622|Doonbara Formation|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|20-SEP-13
5622|Doonbara Formation|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|69001|6|Mentioned|p2 Fig.1B, p23, p23 Fig.13|Neogene|Neogene|||||||
5622|Doonbara Formation|69019|6|Mentioned|p105 Fig.25.|Miocene|Miocene|Callabonna Sub-basin.||||||
5622|Doonbara Formation|69023|6|Mentioned|p108|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
5622|Doonbara Formation|69599|5|Briefly described|p584, p601-602|Pliocene|Miocene|A thin, sporadically outcropping unit, mainly in SA and NSW but extending into QLD. Thickness generally 7-10m, but up to 40m.||||Is overlain by, and locally interdigitates with, Cadelga Limestone. Correlated with Whitula, Poodyea Formations; Horse Creek, Noranside, Austral Downs Limestones; and Mount Coley Sinter.|Silty, commonly pisolitic, ferruginous sandstone.|
5622|Doonbara Formation|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|70336|5|Briefly described|Map legend|Pliocene|Miocene||||||Pisolitic and ferruginous, fine- to medium-grained sand. Fluvial facies.|
5622|Doonbara Formation|70648|5|Briefly described|Map Legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|18-JAN-22
5622|Doonbara Formation|70649|5|Briefly described|Map Legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|18-JAN-22
5622|Doonbara Formation|71415|6|Mentioned|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
5622|Doonbara Formation|73106|5|Briefly described|Map legend.|Pliocene|Miocene||||||Sand, pisolitic and ferruginous, fine to medium-grained. Fluvial facies.|
5716|Dry Creek Sand|22541|6|Mentioned|p 7, Fig 3, 7|||||||||
5716|Dry Creek Sand|35159|6|Mentioned|Table.1|||||||||
5716|Dry Creek Sand|37853|6|Mentioned|Fig.2|||||||||
5716|Dry Creek Sand|38107|6|Mentioned|p71|||||||||
5716|Dry Creek Sand|40453|5|Briefly described|p58|||||||||
5716|Dry Creek Sand|41025|6|Mentioned|Fig.2|||||||||
5716|Dry Creek Sand|41520|5|Briefly described|Fig.7|||||||||
5716|Dry Creek Sand|44133|4|Described|p170, 165 Fig. 10.11|Pliocene|Pliocene|Geological Province: Saint Vincent Basin. Formerly Dry Creek Sands. Underlies and intertounges with Hallet Cove Sandstone. Thickness may exceed 60m.||||||
5716|Dry Creek Sand|60785|5|Briefly described|p184 Fig.1, p195.  |Piacenzian|Piacenzian|South Australia. Has yielded a fossil cetacean periotic.|||||Shelly sand.|
5716|Dry Creek Sand|66131|6|Mentioned|p242 Fig.2|Pliocene|Pliocene|Late Pliocene in age (from Fig.2 - stratigraphic correlation chart).||||||
5716|Dry Creek Sand|73188|5|Briefly described|p320, p345, p357|Pliocene|Pliocene|St Vincent Basin, Adelaide Plains Sub-basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
5752|Duddo Limestone|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 42, 155-156|Miocene|Oligocene|Lawrence (1966). Western Murray Basin. Up to 130m thick. A major (water) aquifer. See also p158.||Murray Group.||Overlies Ettrick Marl conformably and diachronously. Is separated from the unconformably overlying Bookpurnong beds by the Mologa Surface. Grades laterally into Winnambool Formation.|Buff-coloured, bryozoal calcarenite, with interbedded layers of calcisiltite and calcilutite.|
5752|Duddo Limestone|10010|5|Briefly described|p12 Fig. 3||Early Miocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
5752|Duddo Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
5752|Duddo Limestone|22799|2|Defined|p32|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Late Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
5752|Duddo Limestone|22887|5|Briefly described|Fig.6 p13||Early Miocene|||||||
5752|Duddo Limestone|22893|6|Mentioned|p27 fig9|Miocene|Miocene|||||||
5752|Duddo Limestone|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
5752|Duddo Limestone|23226|6|Mentioned|p889|||Of Murray Group.||||||
5752|Duddo Limestone|23417|6|Mentioned|p6|||||||||
5752|Duddo Limestone|23884|5|Briefly described|p155 Fig. 13.2|Early Miocene|Early Miocene|Geological Province: Murray Basin. Of the Murray Group.||||||
5752|Duddo Limestone|23909|6|Mentioned|p298|||||||||
5752|Duddo Limestone|24551|5|Briefly described|p322 Fig. 10.29, 520, p731 Table 17.1|||Of the Murray Group.  Geological Province: Murray Basin.  Max thickness: 130m.||||||
5752|Duddo Limestone|29591|6|Mentioned|Table 20|||||||||
5752|Duddo Limestone|29898|6|Mentioned|p216|||||||||
5752|Duddo Limestone|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5752|Duddo Limestone|30754|6|Mentioned|p13|||Used in deeper parts of basin where Morgan & Mannum indistinguishable||||||
5752|Duddo Limestone|30934|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene & Miocene||||||
5752|Duddo Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
5752|Duddo Limestone|31745|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
5752|Duddo Limestone|31746|3|Fully described|p195|||||||||
5752|Duddo Limestone|34360|6|Mentioned|p11|||||||||
5752|Duddo Limestone|34813|6|Mentioned|p62|||||||||
5752|Duddo Limestone|35285|5|Briefly described|p413|||||||||
5752|Duddo Limestone|37809|6|Mentioned|p7|||||||||
5752|Duddo Limestone|37873|6|Mentioned|p1|||||||||
5752|Duddo Limestone|39329|6|Mentioned|Fig.1|||||||||
5752|Duddo Limestone|39929|6|Mentioned|Fig.3|||||||||
5752|Duddo Limestone|40820|6|Mentioned|Fig.4|||||||||
5752|Duddo Limestone|41511|6|Mentioned|p20|||||||||
5752|Duddo Limestone|41537|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|41868|5|Briefly described|p551|||||||||
5752|Duddo Limestone|42125|6|Mentioned|p136|||||||||
5752|Duddo Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
5752|Duddo Limestone|42137|6|Mentioned|p369|||||||||
5752|Duddo Limestone|42827|3|Fully described|p269|||Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|42881|4|Described|Fig.3, P84|||||||||
5752|Duddo Limestone|42966|2|Defined|Table 23, p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|43655|5|Briefly described|p40-846|||||||||
5752|Duddo Limestone|43791|6|Mentioned|p372, Fig1|||||||||
5752|Duddo Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
5752|Duddo Limestone|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|46909|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|49038|5|Briefly described|p26|||||||||
5752|Duddo Limestone|49040|6|Mentioned|p11|||||||||
5752|Duddo Limestone|50154|2|Defined|p129, p135-136|Early Miocene|Late Oligocene|Of the Murray Group. Max. thickness: 127m. Lies conformably over and interfingers with Ettrick Marl. Disconformably overlain by Parilla Sand or Bookpurnong beds. Nonconformably overlies the Glenelg River Metamorphic Complex in parts.||||||15-SEP-04
5752|Duddo Limestone|50155|5|Briefly described|Map Legend|Miocene|Oligocene|Calcarenite, bryozoal limestone||||||
5752|Duddo Limestone|50156|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50157|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ettrick Marl and Dergholm Granite. Overlain by Parilla Sand and Whalers Bluff Formation. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50158|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50159|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50160|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlain by Lowan Sand. Overlies Glenelg River Metamorphic Complex and Hypatia Formation. Marine deposit of bryozoal limestone and calcarenite||||||25-JUN-04
5752|Duddo Limestone|50161|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous. Of the Murray Group.||||||26-AUG-04
5752|Duddo Limestone|50162|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||22-JUN-04
5752|Duddo Limestone|50163|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ferres Creek Tonalite, Glenelg River Metamorphic Complex, Dergholm Granite and Nangeela Formation. Overlain by Shepparton Formation, Parilla and Lowan Sands. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50164|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||24-JUN-04
5752|Duddo Limestone|60421|5|Briefly described|p409, 413 Fig. 3, 414 Fig. 4|Middle Miocene|Late Oligocene|Underlies: Dorodong Sands. Overlies: Bacchus Marsh Formation.||||||
5752|Duddo Limestone|61314|5|Briefly described|p129|Miocene|Miocene|Of the Murray Group. Geological Province: western part of Murray Basin.||||||
5752|Duddo Limestone|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976).Max.thickness:130m. Suggested here that this Victoria nomenclature be replaced by the South Australia mappable units of Mannum, Finniss, Glensforlan, Bryant Creek and Pata Fm, as they are recognisable in subsurface Victoria.  ||||||
5752|Duddo Limestone|64237|5|Briefly described|p17, p18, p19|Early Miocene|Early Miocene|Of Lawrence (1966). Retained as formal unit through the Lawrence (1975) and Lawrence and Abele(1988) name revisions where it overlay Netherby Marl. Appears to have been excluded from the Murray Supergp...........................reinstated in SA Murray Gp||||||15-JUL-08
5752|Duddo Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
5752|Duddo Limestone|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Of Murray Group. Defined by Lawrence 1966.||||||
5752|Duddo Limestone|66286|5|Briefly described|pp178-179, pp188-189.|Miocene|Oligocene|Contains a variety of goethite-replaced marine fossils including bryozoans, echinoids and foraminifera. 1 - 2 m thick. Open marine shelf or shallow marine deposit.||Unit in Murray Group.|||Limestones of skeletal debris admixed with varying proportions of quartz sand, micrite, and calcareous clay. Well-indurated, fossiliferous, dusky-brown to yellow goethite-rich laminated duricrust with c.10% pisoliths and ooliths.|
5752|Duddo Limestone|66287|6|Mentioned|p30 Fig. 8, p31|Middle Miocene|Middle Miocene|Victorian equivalent of the Murray Group Limestones of South Australia.||||Underlies Bookpurnong Beds.||20-APR-12
5752|Duddo Limestone|67179|6|Mentioned|p579|||||||||
5752|Duddo Limestone|68116|5|Briefly described|Appendix, Maps 29, 38.|Langhian|Chattian||||||Calcarenite, bryozoal limestone.|
5752|Duddo Limestone|68189|6|Mentioned|p29|||||Of the Murray Group.||||
5752|Duddo Limestone|70961|14|Not recorded|p136|||Geological section.||||||
5752|Duddo Limestone|71593|4|Described|p52, p54|Miocene|Oligocene|Murray Basin.||Murray Group||Interfingered with the Ettrick Formation and the Winnambool Formation. Unconformably overlain by the Loxton Sand and Bookpurnong Formation.|Pale bioclastic limestone.|
5752|Duddo Limestone|72445|5|Briefly described|App.6 p2 Fig.1; App.7 p7 Fig.4.|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976). See also Duddo Limestone Member, App.7 p7 text.||Murray Group||Unconformably overlies Renmark Group and is laterally equivalent with Winnambool Formation.|Includes marl and marly limestone.|
5752|Duddo Limestone|73118|6|Mentioned|p17, 21, 24, 34|||Drill core summary logs.||||Overlies Ettrick Formation. Is overlain by Loxton-Parilla Sands, and Shepparton Formation.||
5752|Duddo Limestone|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
5763|Duff Creek Formation|23818|5|Briefly described|p38 Fig.10|Adelaidean|Adelaidean|Equivalent to the Callanna Beds. Max. thickness: 18 000 ft. Overlying unit: Mount Margaret Quartzite (unconformable).||||||18-APR-05
5763|Duff Creek Formation|29840|6|Mentioned|p504|||||||||
5763|Duff Creek Formation|30177|6|Mentioned|p47|||||||||
5763|Duff Creek Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
5763|Duff Creek Formation|31798|4|Described|p95|||Willouran||||||
5763|Duff Creek Formation|33474|6|Mentioned|p540|||||||||
5763|Duff Creek Formation|33939|6|Mentioned|p387|||U.Prot.||||||
5763|Duff Creek Formation|34535|4|Described|p54|||Equiv. Callanna Beds||||||
5763|Duff Creek Formation|34537|6|Mentioned|Fig.10|||Adelaidean||||||
5763|Duff Creek Formation|36733|6|Mentioned|p12|||||||||
5763|Duff Creek Formation|44658|14|Not recorded|map legend|||(G53-15). Willouran.||||||
5763|Duff Creek Formation|71239|6|Mentioned|p4|||Of Reyner (1955). Renamed the Duff Creek beds herein.||||||
5783|Duke Member|40448|5|Briefly described|Table 3|||Informal name.||||||
5856|Duntroon Group|42075|5|Briefly described|Fig 10 P250|||||||||
5856|Duntroon Group|42545|6|Mentioned|p4|||Used by Stagg 1990||||||
5856|Duntroon Group|44133|6|Mentioned|p134|||Unsure if formal units yet?||||||
5878|Dutton Suite|22629|5|Briefly described|fig2 p147,148|||U-Pb ages of 2459+/-15, 2558+/-27, and 2517+/-14 Ma||||||
5878|Dutton Suite|23491|6|Mentioned|p17|||||||||
5878|Dutton Suite|23791|5|Briefly described|p2|Archean|Archean|Parent: Sleaford Complex.  Geological Province: Gawler Craton.||||||07-NOV-08
5878|Dutton Suite|24508|5|Briefly described|p30|||Juxtapositioned with Carnot Gneisses.   Geological Province: Gawler Craton.||||||23-DEC-09
5878|Dutton Suite|24526|5|Briefly described|p95, p96 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Sleaford Complex.  Granite and granodiorite.  Age: >2400Ma.  Geological Province: Gawler Craton.  See also p98 Fig. 4.||||||07-NOV-08
5878|Dutton Suite|40448|5|Briefly described|p26 Table 2, p34|Paleoproterozoic|Neoarchean||2337+/-71Ma, 2334+/-109Ma Rb/Sr|Of Sleaford Complex.|Includes Coulta Granodiorite, Kiana Granite, Whidbey Granite.|||
5878|Dutton Suite|41667|6|Mentioned|p2|||||||||
5878|Dutton Suite|41972|6|Mentioned|p365|||||||||
5878|Dutton Suite|43052|4|Described|p38,Table 3.1|||Of Sleaford Complex.||||||04-MAR-09
5878|Dutton Suite|50605|5|Briefly described|p4.2, 8.7|||Of the Sleaford Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
5878|Dutton Suite|60534|5|Briefly described|p573 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: ~2400 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
5878|Dutton Suite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 2517-2459Ma. Late orogenic granitoids.||||||07-NOV-08
5878|Dutton Suite|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Sleaford Complex. Undifferenciated granitoids, emplaced during late stage of Sleafordian Orogeny. Geological Province: Gawler Craton.||||||12-JAN-10
5878|Dutton Suite|61108|5|Briefly described|map legend|Paleoproterozoic|Archean|Late orogenic granite and granodiorite. Age: 2517-2459 Ma.||||||07-NOV-08
5878|Dutton Suite|63223|5|Briefly described|p16|Archean|Archean|Age: 2520-2500Ma. Includes Coulta Granodiorite. Geological Province: Gawler Craton.||||||07-NOV-08
5878|Dutton Suite|63224|6|Mentioned|p10|||Intrusives. Geological Province: Gawler Craton.||||||07-FEB-08
5878|Dutton Suite|63866|5|Briefly described|p3, p18|||Coulta Domain, Gawler Craton. |c. 2520 Ma (Fanning et al., 2007)|||||
5878|Dutton Suite|64130|6|Mentioned|p1379 |Neoarchean|Neoarchean||c.2520-2500 Ma|||||
5878|Dutton Suite|64131|5|Briefly described|p1401|||||Of the Sleaford Complex|||Weakly deformed granites.|
5878|Dutton Suite|64828|5|Briefly described|p1065 Fig. 2|||Age: ca.2480-2420Ma ( the Sleafordian Orogeny). Supracrustal intrusives.||||||04-MAR-09
5878|Dutton Suite|65376|6|Mentioned|p15.|||||Unit in Sleaford Complex.|Includes Kiana and Whidbey Granites and Coulta Granodiorite.|Intrudes Wangary Gneiss and Hall Bay Volcanics.||
5878|Dutton Suite|65390|5|Briefly described|p19, 20, p23 Fig.3|Neoarchean|Neoarchean|Granitoid intrusives in the Coulta Domain, Gawler Craton. Includes Coulta Granodiorite which has a U-Pb zircon age of 2517 +/- 14 Ma. Faulted against Carnot Gneisses; sheared against Sleaford Complex.||||||
5878|Dutton Suite|65485|6|Mentioned|p42|Archean|Archean|Upper crustal intrusives. Of Sleaford Complex.||||||
5878|Dutton Suite|65922|5|Briefly described|p12|Siderian|Siderian|Southern Eyre Peninsula, SA. Magmatic age of ~2450 Ma (Daly et al. 1998) given. May be equivalent to non-garnetiferous gneiss within the Sleaford Complex.||||||
5878|Dutton Suite|66302|6|Mentioned|p10, p11, p13, p14, p205, p56, p60|Neoarchean|Neoarchean|Age derived from constituent unit SHRIMP age. ||Sleaford Complex|Includes the Coulta Granodiorite, Kiana Granite and the Whidbey Granite.|||
5878|Dutton Suite|67058|5|Briefly described|p476.|Neoarchean|Neoarchean|Southern Gawler Craton. Intrusives.||Unit in Sleaford Complex.||||
5878|Dutton Suite|67536|5|Briefly described|Map Legend|Siderian|Neoarchean|Gawler Craton.|2517 +/- 14 Ma - 2459 +/- 15 Ma||||Granite and granodiorite.|02-APR-14
5878|Dutton Suite|69048|5|Briefly described|p1, p3|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula.|c.2500-2400 Ma.||Kiana Granite.|||
5878|Dutton Suite|70027|5|Briefly described|p56-58|Neoarchean|Neoarchean|Geological province: Gawler Craton. Supracrustal intrusives, including S-type granites.|ca. 2519-2420 Ma|Unit of Sleaford Complex.||||
5878|Dutton Suite|70382|6|Mentioned|p32|Paleoproterozoic|Paleoproterozoic|Geological province: eastern Gawler Craton.  Possible source for some of Quartoo Sand Member inherited zircon.|~2420 Ma||||Granite|
5878|Dutton Suite|71859|5|Briefly described|p2, p6-p7, p9-p10, p14, p28|||Southern Gawler Craton.||Sleaford Complex|Includes the Coulta Granodiorite, Kiana Granite and Whidbey Granite.|||
5878|Dutton Suite|72459|6|Mentioned|p51|Archaean|Archaean|Coulta/Cleve domains.|2460-2560 Ma|||||
5878|Dutton Suite|73026|5|Briefly described|p9, p18|Paleoproterozoic|Paleoproterozoic||c. 2440 Ma||||Granite, granitoids.|
5878|Dutton Suite|73027|5|Briefly described|p9,, p18 fig 2.4|Palaeoproterozoic|Archaean|southern Eyre Peninsula.|c. 2440 Ma||||Granite, granitoids.|
5878|Dutton Suite|73104|5|Briefly described|p1, p3-5, p51-52, p76|Siderian|Siderian|Peraluminous S-type metagranites. Geochron represents magmatic crystallisation ages. Contain older inherited zircons (2522 +/- 14 Ma), indicating the presence of an underlying Mesoarchean basement. Unit intrudes and was [possibly] derived from basement by partial melting. Records metamorphism relating to the Sleaford Orogeny (2425 +/- 10 Ma) and Kimban Orogeny (1716 +/- 7 Ma). [Article includes petrographic description].|c. 2480-2470 Ma|Sleaford Complex|Kiana Granite||Gneiss and metasediments. Includes pale brown, fine- to medium-grained and seriate-textured to sparsely porphyritic metamonzogranite.|
5878|Dutton Suite|73230|6|Mentioned|p15|||||Sleaford Complex|Kiana Granite|||
5878|Dutton Suite|73235|6|Mentioned|p53|||Gawler Craton. Spencer, Cleve and Coulta regions.||||||
5878|Dutton Suite|73256|6|Mentioned|p559|||||Sleaford Complex|||Medium- to high-grade metamorphics.|
5941|Echidna Formation|22485|5|Briefly described|p51 , Fig 2|Early Cretaceous|Late Jurassic|||||||
5941|Echidna Formation|23792|5|Briefly described|Fig.D4|Berriasian|Tithonian|Equivalent to Minke supersequence. Overlain by Neptune Formation. Geological Province: Bight Basin.||||||
5941|Echidna Formation|24201|5|Briefly described|p373 Fig. 2|Berriasian|Tithonian|||||||
5941|Echidna Formation|24338|5|Briefly described|p938 Fig. 2|Berriasian|Tithonian|Overlain by the Neptune Formation. Overlies the Polda Formation Equivalent. Formation is Fm in text. Geological Province: Bight Basin.||||||
5941|Echidna Formation|24350|5|Briefly described|Fig. 4 Appdx|Berriasian|Tithonian|Part of the Minke Supersequence. ||||||
5941|Echidna Formation|24443|5|Briefly described|Fig.7|Berriasian|Tithonian|Overlies unamed Polda Formation equivalent. Overlain by Neptune Formation.  Geological Province: Bight Basin.||||||03-FEB-05
5941|Echidna Formation|24553|5|Briefly described|p37, Figs. 7, and 8|Cretaceous|Cretaceous|Age is Tithonian - Berriasian. Geological Province: Duntroon Sub-basin. Fluvial to paralic sandstones. Part of the Minke Supersequence.||||||07-FEB-11
5941|Echidna Formation|42545|3|Fully described|p4|Neocomian||Supersedes Echidna beds (used 1977, but not recorded by this database). Reserved 1976 as Echidna.||||||
5941|Echidna Formation|43026|5|Briefly described|Table 1,p586|||||||||
5941|Echidna Formation|43052|5|Briefly described|Table 2.1|||||||||
5941|Echidna Formation|43814|6|Mentioned|Fig.3,p115|||||||||
5941|Echidna Formation|44133|5|Briefly described|p139|Neocomian|Neocomian|Formerly 'Echidna beds'.||||||
5941|Echidna Formation|61544|6|Mentioned|p367 Fig.3. |Berriasian|Tithonian|||||Overlies an un-named unit equivalent to Polda Formation. Is overlain by Neptune Formation.||
5941|Echidna Formation|61630|6|Mentioned|p555 Fig. 3, p557|Early Cretaceous|Late Jurassic|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
5941|Echidna Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p58, p60|Berriasian|Kimmeridgian|Duntroon Sub-basin. ||||Overlain by the Neptune Formation.|Shale.|
5941|Echidna Formation|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Berriasian||Duntroon Sub-basin, Bight Basin. Underlying units unknown: not penetrated by any wells.||||Is overlain by Neptune Formation.||
5972|Ediacara Member|7931|5|Briefly described|p99 Fig. 2|Ediacaran|Ediacaran|Within the Rawnsley Quartzite.||||||07-FEB-11
5972|Ediacara Member|23282|6|Mentioned|p89|||Of Adelaide Fold Belt.||||||20-JAN-09
5972|Ediacara Member|37461|5|Briefly described|p343|||||||||
5972|Ediacara Member|37627|6|Mentioned|p186|||||||||
5972|Ediacara Member|38970|4|Described|p105|||||||||
5972|Ediacara Member|39675|6|Mentioned|Fig.3|||||||||
5972|Ediacara Member|40537|6|Mentioned|p328|||||||||
5972|Ediacara Member|41001|6|Mentioned|p169|||||||||
5972|Ediacara Member|41424|6|Mentioned|p299|||||||||
5972|Ediacara Member|41429|3|Fully described|p243|||||||||
5972|Ediacara Member|42222|5|Briefly described|p20|||||||||
5972|Ediacara Member|42433|6|Mentioned|p178|||Of Rawnsley Quartzite.||||||20-JAN-09
5972|Ediacara Member|43052|5|Briefly described|p194,Table 6.1|||Of Rawnsley Quartzite.||||||20-JAN-09
5972|Ediacara Member|43595|5|Briefly described|p547|||||||||
5972|Ediacara Member|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Wilpena Group||||||12-JUL-16
5972|Ediacara Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Rawnsley Quartzite. Massive sandstone, laminated siltstone, fine grained sandstone. Thickness: 100-300m.||||||
5972|Ediacara Member|61732|5|Briefly described|p4, p28 Fig. 13|Ediacaran|Ediacaran|Of the Rawnsley Quartzite (Pound Subgroup, Wilpena Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
5972|Ediacara Member|62085|6|Mentioned|p15 Fig.1|Ediacaran|Ediacaran|Contains Spriggina floundersi fossils.||Unit in Rawnsley Quartzite.||||
5972|Ediacara Member|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Early Cambrian|Of Rawnsley Quartzite. Underlain by Chase Quartzite Member. Red siltstone, quartzite. Type Ediacara assemblage. Horizontal burrows. ||||||
5972|Ediacara Member|64460|5|Briefly described|p195, p197, p198-199|||Of Rawnsley Quartzite. Fossiliferous. Erosive base of unit.||||||
5972|Ediacara Member|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
5972|Ediacara Member|64801|6|Mentioned|p111|Neoproterozoic|Neoproterozoic|Displays a variety of fossil forms.||Rawnsley Quartzite.||||
5972|Ediacara Member|64829|5|Briefly described|p1102|Neoproterozoic|Neoproterozoic|Of Rawnsley Quartzite. Demonstrates "old elephant skin texture" biogenic sedimentary structures.||||||07-FEB-11
5972|Ediacara Member|65892|5|Briefly described|p28-29, p34, p38. |Late Neoproterozoic|Late Neoproterozoic|Contains Ediacara fauna in interbedded siltstone and sandstone packages. Deposited as channel/submarine canyon fill succession and as a deltaic/prodeltaic succession.||Unit in Rawnsley Quartzite.|||White, very fine-grained, interbedded sandstone and siltstone.|
5972|Ediacara Member|66569|5|Briefly described|p861 fig.2, p862,|Ediacaran|Ediacaran|Within Rawnsley Quartzite, Wilpena Group; hosts the famous metazoan fossil assemblage; implied age of ~555 Ma.||||||
5972|Ediacara Member|67484|5|Briefly described|p294 Tb.1, p299 Tb.2|Ediacaran|Ediacaran|Adelaide Rift Complex. Appears in Tb.1 as Ediacaran member. Hosts Palaeopascichnus (Gehling and Droser, 2009) fossils.||Of Rawnsley Quartzite.||Overlies Chace Quartzite Member.||
5972|Ediacara Member|67620|5|Briefly described|p5, 22|Ediacaran|Ediacaran|Adelaide Rift Complex. Contains abundant elephant skin wrinkle structures (microbial mats).||Rawnsley Quartzite.||Overlies Chace Quartzite Member.||
5972|Ediacara Member|68030|3|Fully described|p239, p242|Ediacaran|Ediacaran|Flinders Ranges. Contains Ediacaran biota. Ranges between 5-300m in thickness. Base of the Ediacaran Member represents a sequence boundary with 5-10m deep channels and regional 1-5km wide, 50-250m deep canyon incisions into Chace Quartzite Member, and locally well into Bonney Sandstone. Canyons were likely cut and filled syndepositionally with Ediacara Member. Deltaic succession, prograding from the NW infilling canyons and valleys. Fossils are restricted in storm sandstone beds in upper half of Ediacara Member. Can be subdivided into multiple facies and parasequences (see p240-241). See p241-243 for in depth discussion of Ediacaran biota.||Unit of Rawnsley Quartzite.||Overlain by upper Rawnsley Quartzite. Infills incised canyons within Chace Quartzite Member and Bonney Sandstone.|LST massive unit sandstone with basal, angular sandstone breccias filling step-sided channels within valley incisions, followed by well-laminated clayey sandstones in the deepest channels indicationg a MFS.|26-JUN-19
5972|Ediacara Member|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Appears as Ediacaran Member.||Rawnsley Quartzite.||||
5972|Ediacara Member|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Rawnsley Quartzite, Wilpena Group|||Includes sandstone and siltstone.|
5972|Ediacara Member|68271|5|Briefly described|p694-695|||Adelaide Rift Complex. Hosts the type Ediacara assemblage.||Unit of Rawnsley Quartzite.|||Brown siltstone and flaggy sandstone.|
5972|Ediacara Member|70082|6|Mentioned|p13|Ediacaran|Ediacaran|Adelaide Geosyncline.||||||
5972|Ediacara Member|70334|5|Briefly described|p78|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Turdiditic sands and silts deposited within submarine channels  incised into Rawnsley Quartzite. Contains some of the earliest preserved multicellular organisms which evolved following the thawing of the Earth after the global glaciation event in the Marinoan.|||||Turbiditc sands and silts.|
5972|Ediacara Member|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Rawnsley Quartzite.|||Fine to coarse-grained orthoquartzite, thin to very thick beds, fossiliferous, ripple marks, mudcracks, clay intraclasts; pale green to red-brown, interbedded laminated siltstone.|23-JAN-19
5972|Ediacara Member|70407|6|Mentioned|p112|||||Of Rawnsley Quartzite.||||
5972|Ediacara Member|70790|5|Briefly described|p258 Fig.1, p259, p270|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of Rawnsley Quartzite.||||23-JAN-19
5972|Ediacara Member|71080|6|Mentioned|p21|Ediacaran|Ediacaran|South Australia. Tubular body fossils compared with similar features in Murraba Formation.||Rawnsley Quartzite||||
5972|Ediacara Member|71250|5|Briefly described|p68-70, 72-75|||A local deltaic succession. Contains Ediacaran seafloor fossils; a community of ""juvenile"" forms is described in detail.",,||Rawnsley Quartzite.||Overlies Chace Quartzite Member and (locally) Bonney Sandstone.|Two repeating facies of dark red to maroon interbedded sands and silts, underlying white, massively bedded quartzites (feldspathic sandstones).|
5972|Ediacara Member|72449|5|Briefly described|p1, p2 Map legend|Neoproterozoic|Neoproterozoic|||Within lower part of Rawnsley Quartzite.|||Siltstone, fossil bearing sandstone grading up into white cross-bedded quartzite.|
5972|Ediacara Member|73255|6|Mentioned|p534 Fig.2, p542 Fig.10|Ediacaran|Ediacaran|Contains Pambikalbae hasenohrae and Dickinsonia costata vendobiont fossils.||||Overlies the Bonney Sandstone, underlies the Rawnsley Quartzite.||
6029|Elatina Formation|7931|5|Briefly described|p99 Fig. 2|Ediacaran|Ediacaran|||||||07-FEB-11
6029|Elatina Formation|14019|6|Mentioned|p19|||Geological Province: Adelaide Geosyncline.  Correlated with Moonlight Valley Tillite (Grey and Corkeran, 1998).||||||
6029|Elatina Formation|22510|5|Briefly described|p40|||Of the Yerelina Subgroup. Dominated by shallow-water sandstone but contains lenticular diamictite units that are clearly of glacial origin.  Age: Marinoan.||||||13-FEB-08
6029|Elatina Formation|22631|6|Mentioned|p178|||Age: Marinoan||||||02-MAY-13
6029|Elatina Formation|22677|4|Described|p733, Fig.2 p735|Neoproterozoic|Neoproterozoic|||||||
6029|Elatina Formation|22911|5|Briefly described|37|||||||||
6029|Elatina Formation|23250|5|Briefly described|p1122, p1124 Fig.2||Cryogenian|of Umberatana Group. Correlate of Whyalla Sandstone and Olympic Formation.||||||
6029|Elatina Formation|23287|6|Mentioned|Fig.3,4|||Marinoan tillites. Age: Cryogenian. Adelaide Geosyncline.||||||02-MAY-13
6029|Elatina Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
6029|Elatina Formation|23411|6|Mentioned|Map Legend|||||||||
6029|Elatina Formation|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|||||||
6029|Elatina Formation|23719|5|Briefly described|p26|Neoproterozoic|Adelaidean|Of Umberatana Group. Geological Province: Gawler Craton.||||||
6029|Elatina Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
6029|Elatina Formation|23818|4|Described|p64 Fig. 22, p70|Neoproterozoic|Neoproterozoic|Uppermost unit of the Willochra Sub-Group. Max. thickness: 800 ft. Overlying unit: Wilpena Group.||||||18-APR-05
6029|Elatina Formation|23913|3|Fully described|p107, p110 Fig. 2|Adelaidean|Adelaidean|Age: 650-600 Ma. Geological Province: Central Flinders Zone.  Max thickness: 500m. Underlying Unit: Trezona Formation. Overlying Unit: Nuccaleena Formation. Of the Umberatana Group.||||||14-APR-08
6029|Elatina Formation|24138|5|Briefly described|p10 Fig. 1.1|Precambrian|Precambrian|Contains glacial deposits. Geological Province: Adelaide Geosyncline.||||||
6029|Elatina Formation|24175|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic|Of the Umberatana Group.   Coarse-grained brownish sandstone.  Max. thickness: 125m.||||||
6029|Elatina Formation|24176|4|Described|p12, p24 Tb. 1|Adelaidean|Adelaidean|Of the Willochra Sub-Group. Greywacke, sandstone. Max. thickness: 275m.  Age is Marinoan. Geological Province: Mount Painter Province.||||||13-FEB-08
6029|Elatina Formation|24195|5|Briefly described|p45 Fig.3|||Of the Elatina Formation. Geological Province: Adelaide Geosyncline.||||||01-SEP-08
6029|Elatina Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Willochra Subgroup||||||
6029|Elatina Formation|24400|5|Briefly described|p155 Tb.2|Adelaidean|Adelaidean|||||||
6029|Elatina Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Trezona Formation. Overlain by the Nuccaleena Formation. Geological Province: Adelaide fold belt.||||||14-APR-08
6029|Elatina Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
6029|Elatina Formation|29780|5|Briefly described|p41|||||||||
6029|Elatina Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6029|Elatina Formation|30177|4|Described|p84|||||||||
6029|Elatina Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
6029|Elatina Formation|30802|4|Described|Table 1|||Marinoan age||||||
6029|Elatina Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
6029|Elatina Formation|32146|6|Mentioned|Fig.3|||||||||
6029|Elatina Formation|32505|6|Mentioned|Table 3|||||||||
6029|Elatina Formation|32720|6|Mentioned|p6|||Age. Correlation.||||||
6029|Elatina Formation|33474|6|Mentioned|Fig.2|||||||||
6029|Elatina Formation|33729|6|Mentioned|p82|||||||||
6029|Elatina Formation|34116|6|Mentioned|p20|||||||||
6029|Elatina Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
6029|Elatina Formation|34268|6|Mentioned|p241|||U.Prot.||||||
6029|Elatina Formation|34269|6|Mentioned|Table 1|||Upper Proterozoic. Mn deposit.||||||
6029|Elatina Formation|34291|6|Mentioned|p16|||See also PP17,18,74. Adelaidean||||||
6029|Elatina Formation|34534|6|Mentioned|p61|||Important marker bed||||||
6029|Elatina Formation|34535|4|Described|p71|||See also Fig.22. Base is top of Farina Sub-Group.||||||13-FEB-08
6029|Elatina Formation|35075|6|Mentioned|p77|||||||||
6029|Elatina Formation|35255|5|Briefly described|p10|||See also Fig.4.||||||
6029|Elatina Formation|35317|6|Mentioned|p398|||||||||
6029|Elatina Formation|35582|6|Mentioned|p51|||||||||
6029|Elatina Formation|35586|6|Mentioned|p28|||In reference to boundary Umberatana Group/Wilpena Group.||||||
6029|Elatina Formation|36048|6|Mentioned|p379|||||||||
6029|Elatina Formation|36137|6|Mentioned|p16|||||||||
6029|Elatina Formation|36245|6|Mentioned|Fig.1|||||||||
6029|Elatina Formation|36731|6|Mentioned|p124|||||||||
6029|Elatina Formation|36733|6|Mentioned|Table 5|||||||||
6029|Elatina Formation|36898|6|Mentioned|p181|||See also P196.||||||
6029|Elatina Formation|37015|6|Mentioned|p68|||See also Fig.2.||||||
6029|Elatina Formation|37461|4|Described|p342|||See also Table 5.I||||||
6029|Elatina Formation|37627|6|Mentioned|p181|||||||||
6029|Elatina Formation|37932|6|Mentioned|p545|||||||||
6029|Elatina Formation|38022|6|Mentioned|Fig.4|||||||||
6029|Elatina Formation|38157|6|Mentioned|Table IV|||||||||
6029|Elatina Formation|38641|4|Described|p624|||||||||
6029|Elatina Formation|39210|6|Mentioned|Table 4|||||||||
6029|Elatina Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6029|Elatina Formation|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6029|Elatina Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6029|Elatina Formation|40257|6|Mentioned|p297|||Mention Fig.2||||||
6029|Elatina Formation|40442|6|Mentioned|p10|||||||||
6029|Elatina Formation|40448|5|Briefly described|p38|||||||||
6029|Elatina Formation|40852|6|Mentioned|Fig.3.2|||||||||
6029|Elatina Formation|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
6029|Elatina Formation|41005|6|Mentioned|p419|||Mention Fig.2||||||
6029|Elatina Formation|41405|3|Fully described|p186|||||||||
6029|Elatina Formation|41429|6|Mentioned|p214|||||||||
6029|Elatina Formation|41526|6|Mentioned|p27|||||||||
6029|Elatina Formation|41581|5|Briefly described|p119|||||||||
6029|Elatina Formation|41957|5|Briefly described|p67|||||||||
6029|Elatina Formation|42098|5|Briefly described|Table 2 P54|||||||||
6029|Elatina Formation|42222|6|Mentioned|Table 1 P4|||||||||
6029|Elatina Formation|42235|5|Briefly described|p140|||||||||
6029|Elatina Formation|42238|5|Briefly described|Table 1 P74|||||||||
6029|Elatina Formation|42239|4|Described|p150|||||||||
6029|Elatina Formation|42240|6|Mentioned|Fig.2 P165|||||||||
6029|Elatina Formation|42338|5|Briefly described|p152|||||||||
6029|Elatina Formation|42410|6|Mentioned|p3|||||||||
6029|Elatina Formation|42522|5|Briefly described|p164|||||||||
6029|Elatina Formation|42542|5|Briefly described|p8|||||||||
6029|Elatina Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
6029|Elatina Formation|42600|6|Mentioned|p7|||Umberatana Group||||||
6029|Elatina Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
6029|Elatina Formation|42779|5|Briefly described|Table 1 P287|||||||||
6029|Elatina Formation|42882|5|Briefly described|Fig.7 P12, Table1 P3|||Of Umberatana Group.||||||13-FEB-08
6029|Elatina Formation|43011|6|Mentioned|Table 2,p12|||||||||
6029|Elatina Formation|43052|5|Briefly described|p189,Table 6.1|||of Willochra Subgroup||||||
6029|Elatina Formation|43560|6|Mentioned|p227|||Age: approx. 600 ma||||||
6029|Elatina Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
6029|Elatina Formation|43833|6|Mentioned|541||Vendian|Age basal Vendian.  Known to be within Adelaide Geosyncline.||||||
6029|Elatina Formation|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
6029|Elatina Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
6029|Elatina Formation|44689|14|Not recorded|map legend||Adelaidean|Andamooka. (H53-12).||||||
6029|Elatina Formation|44934|6|Mentioned|Map Legend||Adelaidean|||||||
6029|Elatina Formation|45041|6|Mentioned|p45|||||||||
6029|Elatina Formation|46865|6|Mentioned|p44|||||||||
6029|Elatina Formation|60682|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Geosyncline.||||||
6029|Elatina Formation|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Upalinna Subgroup (Umberatana Group).||||15-APR-11
6029|Elatina Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Purple and white fine and gritty sandstones, purple siltstones with red granules.||||||
6029|Elatina Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Yerelina Subgroup. Medium grained arkosic sandstone, sandy siltstone. Clasts and dropstones.||||||
6029|Elatina Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
6029|Elatina Formation|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic|Neoproterozoic|Galciogenic deposits. Geological Province: Adelaide Fold Belt.||||||20-APR-06
6029|Elatina Formation|61732|5|Briefly described|p28 Fig. 13, p97|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Glacial deposits. Geological Province: Adelaide Rift Complex. See also p150.||||||07-FEB-11
6029|Elatina Formation|62085|4|Described|p13-30|Cryogenian|Cryogenian|||Umberatana Group||Unconformably overlies Yaltipena Formation. Overlain by Nuccaleena Formation disconformably.|Glacial diamictite, sandstone.|
6029|Elatina Formation|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
6029|Elatina Formation|62516|6|Mentioned|p896|||||||||
6029|Elatina Formation|62592|5|Briefly described|p50 Table 5.1, p59.|Marinoan|Marinoan|Adelaide Geosyncline. Unit is too thin to resolve seismically from the Upalinna Subgroup.||Unit in Yerelina Subgroup.|||Sandstone.|
6029|Elatina Formation|62869|6|Mentioned|p631 Fig. 6|||||||||
6029|Elatina Formation|62903|5|Briefly described|p729, p731, p732|Marinoan|Marinoan|Adelaide Rift Complex. An age of either 635 or 580 Ma remains compatible with present geochronological data.||||correlated with Crole Hills Diamictite and Cottons Breccia||
6029|Elatina Formation|63397|6|Mentioned|p10|||||||||
6029|Elatina Formation|63458|6|Mentioned|p873, p897 Fig.19.|Cryogenian|Cryogenian|||Unit in Yerelina Subgroup.||Correlated with Moonlight Valley Tillite.||
6029|Elatina Formation|63674|5|Briefly described|p9|||Has been correlated with the Cottons Breccia and Croles Hill Diamictite of King Island, TAS.||||||
6029|Elatina Formation|63762|5|Briefly described|p19|||In S.A.||||||07-FEB-11
6029|Elatina Formation|64068|5|Briefly described|p48|Cryogenian||Flinders Ranges. Its top is the base of the Ediacaran.|||||Diamictite.|05-APR-12
6029|Elatina Formation|64103|5|Briefly described|p397, p400, p404|||Of Adelaide Rift Complex. May correlate with infomal units in the Vines Fm. Geological Province: Officer Basin.||||||07-FEB-11
6029|Elatina Formation|64400|5|Briefly described|p12|||Marinoan glacial unit of the Umberatana Group. Overlain by Nuccaleena Dolomite. In the Adelaide Rift Complex.||||||07-FEB-11
6029|Elatina Formation|64455|5|Briefly described|p137, p139, p140|||Umberatana Group. Overlain by Nuccaleena Formation. Glaciogenic rocks.||||||29-JAN-09
6029|Elatina Formation|64625|6|Mentioned|p256 |Marinoan|Marinoan|||||Overlies Trezona Formation||
6029|Elatina Formation|64797|5|Briefly described|p153 Fig.2, p159, p163, p164 Fig.11 |||See also p166 Tb.8, p169 Fig.12, p170, p172 Tb.13. S-isotope data. International correlations.||||Correlated with Fortress Hill Formation.||
6029|Elatina Formation|64801|6|Mentioned|p112|Neoproterozoic|Neoproterozoic|||||||
6029|Elatina Formation|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
6029|Elatina Formation|64846|5|Briefly described|p197 Fig.2,p198 Fig.3,p199,p208 Fig.10  |Cryogenian|Cryogenian|Marinoan glaciation.||Of the Yerelina Subgroup.||||
6029|Elatina Formation|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
6029|Elatina Formation|65366|6|Mentioned|p24|||Typifies younger glaciation (Marinoan).||||||19-MAR-12
6029|Elatina Formation|65493|5|Briefly described|p908, Fig 1,2|Ediacaran|Ediacaran|Of Yerelina Subgroup. Age: 635 Ma by correlation with Ghaub (Namibia) and Nantuo (South China) Formations. Others prefer ~580 Ma age. Overlies the Enorama Shale unconformably. Glacigenic sands and diamictites.||||||02-MAY-13
6029|Elatina Formation|65892|5|Briefly described|p32-33, p37, p39. |Cryogenian|Cryogenian|Adelaide Geosyncline. Deposited during Marinoan glaciation. Clasts variable, dominated by basic igneous rocks, possibly from the Enorama Diapir.|c.620 Ma.|||Is overlain by Seacliff Sandstone.|Reddish tillite grading up into muddy siltstone at the top.|
6029|Elatina Formation|65925|5|Briefly described|Appendix 2.||||||||Sandstone, arkosic, medium grained, red-brown, slumped, ripple cross laminated; siltstone, sandy, red, dropstones and minor beds of diamictite with cobble to boulder size clasts of dolomite, basalt, dolerite, tuff.|
6029|Elatina Formation|66464|4|Described|p167, p170-175|Cryogenian|Cryogenian|Adelaide Rift Complex. Overlies Yaltipena Formation. Syn-glacial deposits ranging from debris flows and turbidites to ice-contact tillites and laminated siltstones. Contact with Nuccaleena Formation marks the onset of post-glacial transgression.||||||
6029|Elatina Formation|66569|5|Briefly described|p860, p861 fig.2,||Cryogenian|Of Yerelina Subgroup; disconformably to unconformably underlies Nuccaleena Formation.||||||
6029|Elatina Formation|67030|5|Briefly described|p408-9, Fig.2, p412 Fig.7, p413 Tb.2|Cryogenian|Cryogenian|Age of 580 Ma (Calver et al. 2004) based on correlation with Tasmanian sequences is considered more likely than alternate age of 635 Ma (inferred by global correlation). Magnetic information presented for comparison (Schmidt et al. 2009).|580 Ma (Calver et al. 2004) correlation|Willochra Subgroup|Reynella Siltstone Member|Overlies Wilmington Formation, underlies Nuccaleena Formation and Seacliff Sandstone.||26-APR-12
6029|Elatina Formation|67180|5|Briefly described|p600, p608, p601 Fig.1, p611 Fig.10|Cryogenian|Cryogenian|Marinoan age. Possible correlation with the Ghaub Formation (ca 635 Ma) in Namibia. Formerly included in Willochra Subgroup of Coats and Blisset (1971)?. ||Unit in Yerelina Subgroup||Unconformably overlies the Enorama Shale.|Glacial deposit.|
6029|Elatina Formation|67454|6|Mentioned|p570.|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Marinoan glacigenic unit correlated with Wahlgu Formation. However, the combination of low palaeolatitudes and glacial strata remains enigmatic.||||||04-MAY-12
6029|Elatina Formation|67484|6|Mentioned|p294 Tb.1, p296|Cryogenian|Cryogenian|Adelaide Rift Complex.||Of the Umberatana Group.||Overlain by the Nuccaleena Formation. Underlain by the Tapley Hill Formation.||
6029|Elatina Formation|67620|5|Briefly described|p5|Cryogenian|Cryogenian|Adelaide Rift Complex.||Umberatana Group.||Overlies Tapley Hill Formation. Is overlain by Nuccaleena Formation.||
6029|Elatina Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Yerelina Subgroup.||||
6029|Elatina Formation|67912|5|Briefly described|p13|Ediacaran|GSSP Ediacaran|Flinders Ranges.|635 Ma.|||Is overlain by Nuccaleena Formation.|Glacial tillite.|
6029|Elatina Formation|67979|5|Briefly described|p528|Marinoan|Marinoan|Of Marinoan glacial succession. Correlated with dated Namibian and Chinese glacial successions, giving possble age constraint of ~635 Ma||Yerelina Subgroup|||glaciogenic|
6029|Elatina Formation|68030|6|Mentioned|p236-p237,239|Cryogenian|Cryogenian|Flinders Ranges. Glacial/tillitic deposit.  Dyson (1985) reported parallel, ribbed structures resembling frond-like fossils.||||Underlain by Trezona Formation.||26-JUN-19
6029|Elatina Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.||||
6029|Elatina Formation|68241|5|Briefly described|p16, pp19-25, p30, p32, p33 Fig.3|||Shows considerable lithological and thickness variation. Dropstones occur up to 1 m across about 2 m below the top of the Elatina Formation in the Mt Burns area. Between 100-200 m to over 1500 m thick.||||Disconformably overlain by the Nuccaleena Formation. Underlain by the Enorama Shale. Correlative of the Alberta Conglomerate and Elatina Formation. Overlain by the Dering Silstone.||26-MAY-17
6029|Elatina Formation|68243|6|Mentioned|p656|||||||Possible correlative of the Cottons Breccia?||
6029|Elatina Formation|68244|6|Mentioned|p662|Cryogenian|Cryogenian|||||||21-JUN-19
6029|Elatina Formation|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Yerelina Subgroup||Unconformably overlain by Seacliff Sandstone (Wilpena Group).|Include sandstone/siltstone and diamictite.|
6029|Elatina Formation|68270|5|Briefly described|p677-681,683-p684,687|Cryogenian|Cryogenian|Adelaide Rift Complex. Correlable to Boondawari Formation, Wahlgu Formation, Pioneer Sandstone and Olympic Formation, Inindia beds, Boord Formation, Mount Davenport Diamictite Member, Boko Formation, Oorabra Arkose, Sun Hill Arkose, Black Stump Arkose and Little Burke Tillite. Low palaeolatitudes (<10deg) were recorded in Elatina Fm by McWilliams and McElhinny 1980, Embleton and Williams 1986) and later confirmed by Schmidt and Williams (1995), Sohl et al. (1999) and Williams (2008).||Unit of Umberatana Group.||||03-JUL-19
6029|Elatina Formation|68271|6|Mentioned|p697|Cryogenian|Cryogenian|Glaciogenic.||||||
6029|Elatina Formation|68274|5|Briefly described|p10, p12 Fig.1.6, 13|Cryogenian|Cryogenian|Deposited during the Marinoan glaciation. Occurs immediately below the defined lower boundary of the Ediacaran Period.|850 Ma (base of the Period).|||Glaciogenic deposits.||
6029|Elatina Formation|68275|6|Mentioned|p59|||||||Overlies Trezona Formation. Is overlain by Nuccaleena Formation.||
6029|Elatina Formation|68276|6|Mentioned|p68|Neoproterozoic|Neoproterozoic|"The ""Formation"" is omitted."||||||
6029|Elatina Formation|68277|5|Briefly described|p96, 98, 102-103, 106|Neoproterozoic|Neoproterozoic|Flinders Ranges. Glacial deposits with continent-wide correlative units. Paleomagnetism data and inferred tectonic orientations during Ediacaran glaciations discussed. Deposition was in low to moderate palaeolatitudes.||||Correlated with Wahlgu Formation (WA).|Sandstones.|
6029|Elatina Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
6029|Elatina Formation|69017|6|Mentioned|p96|||||||Is overlain by Nuccaleena Formation.|Basal glacial diamictites grading up into sandstones with lesser diamictite toward the top. Locally, flaser-bedded sandstone, granule conglomerates and muddy siltstone unconformably overlie the diamictites.|
6029|Elatina Formation|69437|5|Briefly described|p22:7|Cryogenian|Cryogenian|Adelaide Fold Belt. Discussion of age of the Elatina glaciation, start of the Ediacaran, and possibility of a third Ediacaran glacial event.||||Is overlain by Nuccaleena Formation.||12-JUL-16
6029|Elatina Formation|69441|6|Mentioned|p26:1|||Adelaide Fold Belt.||||Correlated with Moonlight Valley Tillite (Wolfe Basin).||12-JUL-16
6029|Elatina Formation|69442|6|Mentioned|p27:4|||Adelaide Fold Belt.||||Correlated with Moonlight Valley Tillite (Wolfe Basin).||12-JUL-16
6029|Elatina Formation|69841|6|Mentioned|p7, p19|||||||Is overlain by Cumberland Creek Dolostone. Correlative of Cottons Breccia.||
6029|Elatina Formation|69873|6|Mentioned|p74, p82-84|Ediacaran|Ediacaran|||||Is correlated with Cottons Breccia (Tas).||
6029|Elatina Formation|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
6029|Elatina Formation|70031|4|Described|p245-246,250-251|Cryogenian|Cryogenian|Adelaide Geosyncline. Glaciogenic succession marking the start of the Elatina glaciation. Boulders from the base of the Elatina Formation were "bulldozed" into the Yaltipena Formation by ice action (Lemon and Reid 1998; Williams et al., 2008). Ca. 635 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.|635 Ma|Unit of Yerelina Subgroup.||Entirely comprises the Yerelina Subgroup. Overlain by  Wilpena Group/Nuccaleena Formation. Underlain unconformably (SB) by Upalinna Subgroup/Trezona Formation and Yaltipena Formation.||
6029|Elatina Formation|70082|5|Briefly described|p1-9,15-16|Cryogenian|Cryogenian|Flinders Ranges and Kulpara-Adelaide region. Type section: (possibly? Not explicitly mentioned on p2) Below basal Ediacaran stratotype monument on Enorama Creek (S31.33150, E138.63339). Contains red beds, periglacial paleosols and moraine till. Characterised by carbonate nodules, soft sediment deformation and brecciation at Hallett Cove, interpreted to be caused by methane seeps (Kennedy et al., 2008). Hosts an array of supratidal to alluvial paleosols in the Reynella Siltstone includes Gelisols with sand wedge polygons formed near Hallett Cove in an arid frigid continental paleoclimate like that of modern Antarctica.|||Includes Reynella Siltstone Member.|||
6029|Elatina Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, arkosic, medium-grained, red-brown, slumped, ripple cross-laminated; siltstone, sandy, red, dropstones and minor beds of diamictite with cobble to boulder sized clasts of dolomite, basalt, dolerite, tuff.|
6029|Elatina Formation|70334|4|Described|p2,20,29-31,54,56,77,79|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline. Deposited in a periglacial deltaic-lacustrine setting in an arid palaeoenvironment (Preiss, 1987). Contain granules of quartz, feldspar and Gawler Range Volcanics, indicating a Gawler Craton source region. Contemporaneous with Whyalla Sandstone.||Unit of Yerelina Subgroup.|Includes Reynella Siltstone Member.|Contemporaneous with Whyalla Sandstone.|Fine- to medium-grained sandstone and lithic sandstone which contains interbeds of a red-brown to purple-red massive siltstone and lithic siltstone.|
6029|Elatina Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Marinoan [Cryogenian].||Of Yerelina Subgroup.|||Red-brown, medium-grained, arkosic sandstone, slumped, ripple cross-laminated; red sandy siltstone, dropstones and minor beds of diamictite with cobble to boulder sized clasts of dolomite, basalt, dolerite, tuff.|23-JAN-19
6029|Elatina Formation|70407|5|Briefly described|p103 Fig 2, p112, 105|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Wilpena Group. Previously included in Willochra Subgroup.|Includes Reynella Siltstone Member.|Capped by Nuccaleena Formation. Basal unconformity.||23-JAN-19
6029|Elatina Formation|71129|5|Briefly described|p15,107,118,126-127,129,208|Cryogenian|Cryogenian|Of Adelaide Geosyncline. Glacial to periglacial clastic sedimentation in a shallowing rift during Marinoan Epoch.|||Includes Reynella Siltstone Member.|Correlable with Whyalla Sandstone.||
6029|Elatina Formation|71237|14|Not recorded|p10, 17|||||||||
6029|Elatina Formation|71241|14|Not recorded|p12, 13, 15, p9-10, 17|||Orroroo sheet area.||||||
6029|Elatina Formation|71288|6|Mentioned|p136, 139-140|Neoproterozoic|Neoproterozoic|Paleopole positions from this unit locate Australia in low latitudes in the late Neoproterozoic.|645-635 Ma.|||||
6029|Elatina Formation|72247|5|Briefly described|p40,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.|||Includes Reynalla Siltstone Member.|Underlain by Angepena Formation. Transitional to Whyalla Sandstone.||
6029|Elatina Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Return to glacial conditions.||||Overlies Trezona Formation and underlies Nuccaleena Formation.|Red-brown medium-grained sandstone and red pebbly sandy siltstone of glacial origin.|
6029|Elatina Formation|72450|5|Briefly described|Brochure map|||||Umberatana Group|||Pink-brown sandstone with red granule bands.|
6029|Elatina Formation|72451|6|Mentioned|p4 Fig. 1|Late Proterozoic|Late Proterozoic|Adelaidean age. Appears only in Figure 1.||||||
6029|Elatina Formation|72473|6|Mentioned|p4-6|||Associated with the Marinoan glaciation. [Informal lower and upper subdivisions mentioned].|||||Massive, pink, fine - medium grained arkosic sandstone, overlain by a red-brown, massive, pebbly to bouldery sandy siltstone interpreted as a tillite.|
6029|Elatina Formation|72489|6|Mentioned|p3|Ediacaran|Ediacaran|Marinoan glacial deposits.||||Partially overlies Trezona Formation.|Glacial deposits.|
6029|Elatina Formation|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian |Shown as Marinoan age. Northern Flinders Ranges. Glacial deposits.||Umberatana Group||||
6029|Elatina Formation|73086|6|Mentioned|p101, p113, p167|||Adelaide Rift Complex.||||Correlates to Olympic Formation.||
6029|Elatina Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, arkosic, medium-grained, red-brown, slumped, ripple cross-laminated; siltstone, sandy, red, dropstones and minor beds of diamictite with cobble to boulder size clasts of dolomite, basalt, dolerite, tuff.|
6029|Elatina Formation|73180|6|Mentioned|p47|Neoproterozoic|Neoproterozoic|Finders Ranges, Elatina Creek. Elatina glaciation.|||||Glaciogenic sediments.|
6029|Elatina Formation|73227|5|Briefly described|p25-28, p30|||Adelaide Rift Complex, Torrens Hinge Zone. Marioan. Interfingering of this unit with Whyalla Sandstone represents probable glaciomarine incursions into the otherwise terrestrial environment of the Stuart Shelf. Paleomagnetic studies demonstrate that hematite was deposited very early, pre-dating lithification.||Umberatana Group||Underlain by Brighton Limestone. Overlain by Nuccaleena Formation. Equivalent to Whyalla Sandstone and Yudnapinna beds.|Dominantly shallow marine sandstones including tidal rhythmites, with lesser diamictite lenses of glacial origin.|
6029|Elatina Formation|73234|6|Mentioned|p20-21|||Adelaide Rift Complex. Contains a large proportion of zircons derived from the Musgrave Province.||||||
6029|Elatina Formation|73236|4|Described|p36-39, p47|Ediacaran[?]|Ediacaran[?]|Marine sedimentary rocks. Elatina glaciation.|c. 640-635 Ma|Yerelina Subgroup, Umberatana Group, Heysen Supergroup|Reynella Siltstone Member|Underlain by Wilmington Formation (Upalinna Subgroup). [Unconformably] overlain by Seacliff Sandstone (Sandison Subgroup, Wilpena Group).|Reddish brown, fine- to medium-grained sandstone with granule layers.|
6029|Elatina Formation|73255|6|Mentioned|p534 Fig.2|Cryogenian|Cryogenian|Marinoan tillite.||||Overlies the Trezona Formation, underlies the Nuccaleena Formation.||
6029|Elatina Formation|74367|5|Briefly described|p6-9, p11, p14, p16-17, p20, p22-24|Cryogenian|Cryogenian|Deposited during Marinoan Glaciation. Coeval with Whyalla Sandstone.|671+/-52 Ma LA-ICP-MS detrital zircon MDA|Yerelina Subgroup||||
6073|Elkera Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Interbedded siltstone, dolomite, sandstone and shale; stromatolitic dolomite at top. Underlies: Errarra beds. Overlies: Grant Bluff Formation.||||||01-NOV-04
6073|Elkera Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Errarra Formation, Mount Baldwin Formation. Overlies: Grant Bluff Formation.||||||
6073|Elkera Formation|12951|5|Briefly described|p143,  fig 4|Neoproterozoic|Neoproterozoic|Georgina Basin.||Top of the Mopunga Group.||Correlates with lower Arumbera Sandstone of Amadeus Basin. Unconformably overlain by Mount Baldwin Formation, Adam Shale.|Silty turbidites.|
6073|Elkera Formation|22646|6|Mentioned|p 101|Neoproterozoic|Neoproterozoic|Informal name - lower Elkera Formation used p 101.  Situated in the Georgina Basin.||||||07-MAY-13
6073|Elkera Formation|23314|5|Briefly described|331 Fig.2|||||||||
6073|Elkera Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||24-MAR-05
6073|Elkera Formation|38157|6|Mentioned|Table IX|||||||||
6073|Elkera Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Siltstone to sandstone, micaceous, laminated to thin bedded, blue grey to dusky red; dolostone horizons. Geological Province: Georgina Basin.||||||15-NOV-05
6073|Elkera Formation|40906|4|Described|p56|||||||||
6073|Elkera Formation|41005|6|Mentioned|Fig.2|||||||||
6073|Elkera Formation|41801|5|Briefly described|p215|||See also p218.||||||15-AUG-06
6073|Elkera Formation|42059|6|Mentioned|Fig.2 P131|||||||||
6073|Elkera Formation|42504|5|Briefly described|Table 4 P73|||||||||
6073|Elkera Formation|42643|6|Mentioned|p21|||||||||
6073|Elkera Formation|42956|5|Briefly described|p29|||Of Mopunga Group.||||||15-AUG-06
6073|Elkera Formation|47035|6|Mentioned|p85|||||||||
6073|Elkera Formation|48990|2|Defined|p10|Adelaidean|Adelaidean|||||||19-APR-22
6073|Elkera Formation|60122|6|Mentioned|p9|||Formerly of the Grant Bluff Formation but excluded with revision of the unit (Walter 1980).  In the Supersequence 4.||||||15-AUG-06
6073|Elkera Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin. Underlies: Mount Baldwin Formation, Errarra Formation. Overlies: Grant Bluff Formation. Interbedded siltstone, dolomite, sandstone and shale, stromatolitic dolomite.||||||17-NOV-04
6073|Elkera Formation|61022|5|Briefly described|p15 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||20-APR-05
6073|Elkera Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Siltstone, sandstone: micaceous, laminated to thin-bedded; minor dolostone, some stromatolitic. Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
6073|Elkera Formation|61732|3|Fully described|p5 Tb. 1, p109-110|Ediacaran|Ediacaran|Of Mopunga Gp. Overlies Grant Bluff Fm; underlies Central Mount Stuart Fm ( according to Fig. 40 but stated to be unconformably beneath Mount Baldwin Fm. p109). Thick: 270m. Geol.Prov: Georgina Basin. See also p65,  p106.||||||07-FEB-11
6073|Elkera Formation|62376|5|Briefly described|p53|Early Cambrian|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
6073|Elkera Formation|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlies Grant Bluff Formation; overlain by and intertongues with lower Central Mount Stuart Formation. Geological Province: Georgina Basin. Consists of carbonates, immature clastics and evaporites.||||||23-JAN-07
6073|Elkera Formation|63562|6|Mentioned|p338 fig 3, p345 fig 7, p352 Fig.10|Ediacaran|Ediacaran|Of Georgina Basin.||||Overlies Grant Bluff Formation.||
6073|Elkera Formation|64068|3|Fully described|p51, 52, 55,  viii|Ediacaran|Ediacaran|Of Mopunga Group. Formerly included in upper part of Grant Bluff Formation of Smith (1964). See also Tops Member of Central Mount Stuart Formation.||Of Mopunga Group.||Conformable on Grant Bluff Formation. Is disconformably overlain by Mount Baldwin Formation or Red Heart Dolostone.|Interbedded siltstone and dolostone, locally stromatolitic; quartz arenite to shale, locally evaporitic.|07-MAY-13
6073|Elkera Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Georgina Basin during the Centralian 3 event (~600-544 Ma)||||||
6073|Elkera Formation|64812|5|Briefly described|p237 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||07-FEB-11
6073|Elkera Formation|64813|5|Briefly described|p256 Fig. 3|Neoproeterozoic|Neoproterozoic|Unconformably overlain by Mount Baldwin Formation. Geological Province: southern Georgina Basin.||||||11-FEB-09
6073|Elkera Formation|65237|5|Briefly described|p5|||Of Mopunga Gp. Overlies Grant Bluff Fm; unconformably overlain by Mount Baldwin Fm in the south. Geol.prov: southern Georgina Basin. Immature clastic rocks + evaporites; silty, turbiditic rocks. Correlates with lower Arumbera Sandstone in Amadeus Basin||||||07-FEB-11
6073|Elkera Formation|65338|5|Briefly described|p iv, pp63-64.|Ediacaran|Ediacaran|This unit has not been mapped separately from the Central Mount Stuart Formation in MOUNT PEAKE.||Unit in Mopunga Group.||Is overlain by Central Mount Stuart Formation.|Carbonate, clastic and evaporitic rocks.|
6073|Elkera Formation|65341|6|Mentioned|p2 Fig.2, p16. |||||Unit in Mopunga Group.||Is overlain by Mount Baldwin Formation.||
6073|Elkera Formation|69437|5|Briefly described|p22:4-5, 7-8|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequences 3 & 4. Peritidal to shallow-marine deposits.||Mopunga Group.||Overlies Grant Bluff Formation. Upper part is correlated with Central Mount Stuart Formation.||12-JUL-16
6073|Elkera Formation|69438|6|Mentioned|p23:20|||Georgina Basin.||||Correlated with Julie Formation (Amadeus Basin).||12-JUL-16
6073|Elkera Formation|69443|4|Described|p28:7, 10-11, 15|Ediacaran|Ediacaran|Walter (1980); modified by Freeman (1986) who included the silty sandstone/granule orthoquartzite where the stromatolitic dolostone is absent. Southern Georgina Basin. Generally recessive. 70-270m thick. Partial lateral equivalent of Andagera and Central Mount Stuart Formations. Peritidal to shallow-marine deposits.||Mopunga Group.||Conformably and gradationally overlies Grant Bluff Formation. Is overlain conformably by Central Mount Stuart Formation, and disconformably by Mount Baldwin Formation or Red Heart Dolostone.|A succession of interbedded siltstone, quartz sandstone to sublithic sandstone, and shale; capped by dolostone (locally with columnar stromatolites) which is locally evaporitic. Locally includes a silty sandstone and a granule orthoquartzite bed.|12-JUL-16
6073|Elkera Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |270m thick.||Mopunga Group||Overlies Grant Bluff Formation, overlain by Andagera Formation|Interbedded siltstone, sandstone and shale, capped by dolostone.|
6073|Elkera Formation|71621|5|Briefly described|p30|||Of Georgina Basin. Said to have an unconformable and in part faulted contact with the Xanten Granodioritie [although the exact nature of this contact isn't provided].||||||02-FEB-19
6073|Elkera Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Georgina Basin.||||Overlies the Grant Bluff Formation.||
6073|Elkera Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains rare halite pseudomorphs; ichnofossils, local columnar stromatolites, microbial mat fragments.||Mopunga Group||Overlies the Grant Bluff Formation.|Interbedded siltstone, dolostone; quartz-arenite, sublitharenite, mudstone; granule quartz sandstone; planar bedded, low-angle cross stratified; micaceous.|
6073|Elkera Formation|72516|3|Fully described|p12-13, p15-16, p61, p87-90|Ediacaran|Ediacaran|Georgina Basin, occurs in HUCKITTA, northeastern ALCOOTA and MOUNT PEAKE map sheets in addition to the JERVOIS RANGE SPECIAL. Outcrops along the Jervois and Johansen ranges. Type section is defined at Valley Bore in Jervois Range (Walter, 1980).  Based on new field work rocks previously assigned to the Grant Bluff Formation in the Charlotte Fault Zone are reassigned to this unit.  Contains ichnofossils, local columnar stromatolites and microbial mat fragments. 270m thick, 70m thick in Jinka. Deposited in a peritidal to shallow marine environment. Faulted against the Oorabra Arkose. Equivalent to the Central Mount Sutart Formation and the Julie Formation. See also  p95, p154-155, p173, p186, p218.||Mopunga Group||Conformably to gradationally overlies the Grant Bluff Formation. Unconformably overlies the Thring Granite. Disconformably overlain by the Mount Baldwin Formation or the Red Heart Dolostone.|Interbedded siltstone, dolostone; quartz-arenite, sublitharenite, mudstone; granule quartz sandstone; planar bedded, low-angle cross-stratified; micaceous; rare hailte pseudomorphs.|19-APR-22
6073|Elkera Formation|73086|6|Mentioned|p133|||Georgina Basin.||||Correlates to Julie Formation.||
6118|Elyuah Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Brown and green shale, basal pebbly conglomerate. Underlies: Grant Bluff Formation. Overlies: Arunta Block units.||||||01-NOV-04
6118|Elyuah Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Grant Bluff Formation. Overlies: Oorabra Arkose. Shale, pebbly sandstone.||||||
6118|Elyuah Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Georgina Basin.  Age - Ediacarian in text.||||||
6118|Elyuah Formation|22649|5|Briefly described|p 152|||Consists of mudrocks ressembling the Peratatataka Formation.  Province - Georgina Basin.||||||
6118|Elyuah Formation|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
6118|Elyuah Formation|23844|5|Briefly described|p37|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||30-SEP-08
6118|Elyuah Formation|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|24442|6|Mentioned|p49|||Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|33111|6|Mentioned|p38|||||||||
6118|Elyuah Formation|35005|5|Briefly described|p145|||||||||
6118|Elyuah Formation|37572|5|Briefly described|p154|||See also Fig.8||||||
6118|Elyuah Formation|38157|6|Mentioned|Table IX|||||||||
6118|Elyuah Formation|39210|4|Described|p51|||||||||
6118|Elyuah Formation|40538|6|Mentioned|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Shale with interbeds of silty sandstone and a basal pebble conglomerate. Geological Province: Georgina Basin.||||||15-NOV-05
6118|Elyuah Formation|40906|4|Described|p21|||||||||
6118|Elyuah Formation|41005|6|Mentioned|Fig.2|||||||||
6118|Elyuah Formation|41429|6|Mentioned|p247|||||||||
6118|Elyuah Formation|41801|6|Mentioned|p218|||||||||
6118|Elyuah Formation|42059|6|Mentioned|Fig.2 P131|||||||||
6118|Elyuah Formation|42504|5|Briefly described|Table 4 P73|||||||||
6118|Elyuah Formation|42643|6|Mentioned|Fig.4 P19|||||||||
6118|Elyuah Formation|44327|14|Not recorded|p.7,8,18|||(F53-11). Tb.I. part of Mopunga Gp. basal arkose, sh.slight disconf.on Mt.Cornish Fm.&unconf. on PreCamb.metamorphic & igneous rocks.||||||
6118|Elyuah Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|||||||15-AUG-06
6118|Elyuah Formation|45052|4|Described|p68|Adelaidean|Adelaidean|Unit of Mopunga Group.||||||30-SEP-08
6118|Elyuah Formation|45102|6|Mentioned|p45|||See also p49.||||||15-AUG-06
6118|Elyuah Formation|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
6118|Elyuah Formation|48844|2|Defined|p.20-30||Neoproterozoic|On many pages. p.1,16,17,20-30, F.14,26,58,67, Pl.8. (new name). U.Proterozoic. Contains Oorabra Arkose Mem.Overlain by Grant Bluff Fm. Correl.with Pertatataka Fm. (F53-11).||||||15-AUG-06
6118|Elyuah Formation|48901|14|Not recorded|Not recorded||Adelaidean|Pt. Mopunga Gp. Defn on Tech.File F/53-11.||||||
6118|Elyuah Formation|48990|1|Redefined|p11|Adelaidean|Adelaidean|||||||
6118|Elyuah Formation|49036|6|Mentioned|p6|||||||||
6118|Elyuah Formation|60122|4|Described|p12-13|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Redefined by Walter (1980) to exclude the then constituent Oorabra Arkose Member.  Disconformably overlies Wonnadinna Dolostone an||||||13-MAR-17
6118|Elyuah Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin. Underlies: Grant Bluff Formation. Overlies: Oorabra Arkose. Basal pebbly sandstone, brown and green shale.||||||
6118|Elyuah Formation|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Mopunga Group.  Mudstone, siltstone; thin basal sandstone or pebbly arkose (Keepera Ridges only).||||||
6118|Elyuah Formation|60668|5|Briefly described|Fig. 23a|||Quartz arenite and quartz greywacke.  Geological Province: Georgina Basin. ||||||
6118|Elyuah Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Dark grey to black mudstone with thin fine-grained sandstone interbeds; basal conglomerate. Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Mudstone, siltstone; thin basal sandstone or pebbly arkose.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||11-OCT-05
6118|Elyuah Formation|61732|3|Fully described|p5 Tb. 1, p108|Ediacaran|Ediacaran|Of Mopunga Gp. Formerly included Oorabra Arkose which is now excluded from this unit. Transitionally overlain by Grant Bluff Fm. Max. thickness: 90m (est.). Geol.Prov: Georgina Basin. See also p106, p108 Fig. 40.||||||13-MAR-17
6118|Elyuah Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Mopunga Group. Geological Province: Georgina/Ngalia Basin. Shale, interlaminated, fissile chocolate brown and green; interbedded carbonate rocks.||||||
6118|Elyuah Formation|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlain by Grant Bluff Formation. Geological Province: Georgina Basin. Includes black mudstones.||||||23-JAN-07
6118|Elyuah Formation|63562|6|Mentioned|p338 fig 3, p352 Fig.10|Ediacaran|Ediacaran|Of Georgina Basin. Mis-spelt as Eluyah in Fig.7.||||Overlies Oorabra Arkose. Is overlain by Grant Bluff Formation.||
6118|Elyuah Formation|64068|3|Fully described|p49, p162, p19, p viii,  p x|Ediacaran|Ediacaran|Hosts galena mineralisation. Shales give this unit a moderately high, K-dominant radiometric signature. Unconformable on Palaeoproterozoic units.||Of Mopunga Group.||Disconformable above Boko Formation, Oorabra Arkose. Conformable above Gnallan-a Gea Arkose. Comformably and gradationally overlain by Grant Bluff Formation.|Green, red and grey micaceous shale and siltstone; minor quartz sandstone in outcrop; thin basal sandstone or pebbly arkose.|04-APR-12
6118|Elyuah Formation|65237|5|Briefly described|p5|||Basal unit of the Mopunga Group. Gradational with Grant Bluff Formation above. Geological province: southern Georgina Basin. Black mudstone.||||||07-FEB-11
6118|Elyuah Formation|65338|4|Described|p iv, p62, p64.|Ediacaran|Ediacaran|Georgina Basin. Locally interdigitates with Gnallan-a-gea Arkose. Typically recessive or non-outcropping.||Unit in Mopunga Group.||Dis- or un-conformably overlies Boko Formation. Is overlain by Grant Bluff Formation.|Laminated, fissile, black, chocolate brown to green, predominantly micaceous shale; locally a basal arkosic pebble conglomerate; intervals of calcrete; interbedded, fine-grained, flaggy sandstone.|
6118|Elyuah Formation|65341|5|Briefly described|p5, pp14-15. |||Shallow marine, mostly below wave base, depositional environment. Very recessive and rarely exposed.||Unit in Mopunga Group.||Unconformably overlies Oorabra Arkose and Boko Formation. Is overlain conformably by Grant Bluff Formation.|Subsurface: dark grey to black micaceous mudstone with thin, fine-grained micaceous sandstone interbeds, basal conglomerate; surface: rare outcrop of red and white mudstone.|
6118|Elyuah Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.|Shale, interlaminated, fissile chocolate-brown and green; interbedded carbonate rocks.|
6118|Elyuah Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.|Shale, interlaminated, fissile chocolate brown and green; interbedded carbonate rocks.|
6118|Elyuah Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Mopunga Group.||Is overlain by Grant Bluff Formation.||12-JUL-16
6118|Elyuah Formation|69443|5|Briefly described|p28:7, 9-10, 34|Ediacaran|Ediacaran|Southern Georgina Basin. Associated with epigenetic base metal mineralisation in Mount Skinner area.||Mopunga Group.||Overlies Boko Formation unconformably, and Gnallan-a-Gea Arkose gradationally (also interdigitates with it). Is overlain by Grant Bluff Formation.||12-JUL-16
6118|Elyuah Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |210m thick.||Mopunga Group||Overlain by Grant Bluff Formation|Shale and siltstone.|
6118|Elyuah Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Georgina Basin.||||Overlain by the Grant Bluff Formation.||
6118|Elyuah Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains intermediate spheroidal acritarchs, large organic amorphous fragments.||Mopunga Group||Overlain by the Grant Bluff Formation.|Basal sandstone, pebbly arkose, conglomerate, laminated micaceous shale, siltstone, interbedded black micaceous shale, micaceous sandstone, minor quartz sandstone.|
6118|Elyuah Formation|72516|3|Fully described|p13, 15-16, p63, p88|Ediacaran|Ediacaran|Georgina Basin. On the JERVOIS RANGE SPECIAL outcrops as a recessive unit. Type section is located near the eastern end of the Dulcie Range in northern JINKA. Contains intermediate spheroidal acritarchs; large organic amorphous fragments. 82-108m thick. Deposited in a low-energy, shallow to moderately deep-marine environment. Petrography and fossils are discussed.  Equivalent to the Gnallan-a-Gea Arkose of the southern Georgina Basin and the lower Pertatataka Formation of the Amadeus Basin. See also p186, p188, p218.||Mopunga Group||Disconformably overlies the Oorabra Arkose; unconformably overlies the Unca Granite. Conformably overlain by the Grant Bluff Formation.|Basal sandstone, pebbly arkose, conglomerate; laminated micaceous shale, siltstone; interbedded black micaceous shale, micaceous sandstone; minor quartz sandstone.|19-APR-22
6118|Elyuah Formation|73086|6|Mentioned|p118, p122|||Georgina Basin, south-eastern.||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
6152|Emu Bay Shale|5249|4|Described|p31, p39|Early Cambrian|Early Cambrian|Type section at Emu Bay. Rapidly deposited, probably within a suboxic environment. Contains exceptionally well-preserved fossils including Anomalocaris. Age is Tsanglangpuian (mid-Early Cambrian).||||Conformably overlies White Point Conglomerate.||20-MAR-12
6152|Emu Bay Shale|6111|5|Briefly described|p22-29.|Early Cambrian|Early Cambrian|Type section crops out on east side of Emu Bay. Richly fossiliferous in Burgess Shale-type fauna; forms a Lagerstatte at Big Gully. Apparently shallow water depositional environment.||||Overlies White Point Conglomerate, locally unconformably. Is overlain by Boxing Bay Formation.|Shale.|17-SEP-12
6152|Emu Bay Shale|7992|4|Described|165, 166|Early Cambrian|Early Cambrian|Of Point Marsden Group, beds. Overlies Stokes Bay Sandstone. Contains index fossils Redlichia and Lusatiops. 300-400 feet thick grey shales with interbedded quartzites. Apparently continues around Emu Bay, where overlain by White Point Limestone.||||||12-JAN-10
6152|Emu Bay Shale|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 55 m. Overlies White Point Conglomerate. Overlain by Boxing Bay Formation.||||||04-MAY-11
6152|Emu Bay Shale|22643|5|Briefly described|fig3p187, fig6|Early Cambrian|Early Cambrian|||||||
6152|Emu Bay Shale|22766|4|Described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
6152|Emu Bay Shale|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin.||||||
6152|Emu Bay Shale|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Toyonian|||||||
6152|Emu Bay Shale|23818|5|Briefly described|p87 Fig.33, p105|Cambrian|Cambrian|Of the Kangaroo Island Group. Geological Province: Adelaide Geosyncline. Max. thickness: 500 ft.||||||18-APR-05
6152|Emu Bay Shale|23981|6|Mentioned|p22, p64|||Lagoonal deposits on Kangaroo Island. Together with White Point Conglomerate is correlated with Oraparinna Shale.||||||04-FEB-08
6152|Emu Bay Shale|32669|6|Mentioned|p523|||L.Camb.||||||
6152|Emu Bay Shale|33332|6|Mentioned|p11|||L.Camb.||||||
6152|Emu Bay Shale|33471|6|Mentioned|Fig.1|||||||||
6152|Emu Bay Shale|34610|6|Mentioned|p171|||Refers Daily (1956)||||||
6152|Emu Bay Shale|34612|5|Briefly described|p105|||Correlation chart. Lower Cambrian||||||
6152|Emu Bay Shale|35255|6|Mentioned|Fig.8|||||||||
6152|Emu Bay Shale|35487|6|Mentioned|p21|||Source of Crustacea and annelid worms||||||
6152|Emu Bay Shale|35835|6|Mentioned|p209|||||||||
6152|Emu Bay Shale|36198|6|Mentioned|Fig.I.2|||||||||
6152|Emu Bay Shale|38701|6|Mentioned|p123|||||||||
6152|Emu Bay Shale|38873|4|Described|Table 3|||See also Fig.8||||||
6152|Emu Bay Shale|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
6152|Emu Bay Shale|40856|6|Mentioned|Fig.23.6|||||||||
6152|Emu Bay Shale|41106|5|Briefly described|p168|||||||||
6152|Emu Bay Shale|41947|6|Mentioned|p16|||||||||
6152|Emu Bay Shale|42192|6|Mentioned|p15|||||||||
6152|Emu Bay Shale|42225|6|Mentioned|Fig.4 P224|||||||||
6152|Emu Bay Shale|42268|5|Briefly described|p325|||||||||
6152|Emu Bay Shale|42269|6|Mentioned|Fig.1 P335|||||||||
6152|Emu Bay Shale|42272|6|Mentioned|p413|||||||||
6152|Emu Bay Shale|44133|5|Briefly described|p4 Fig. 7.2, 6, 12, 17|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kangaroo Island Group.||||||
6152|Emu Bay Shale|45102|6|Mentioned|p47|||||||||
6152|Emu Bay Shale|60264|6|Mentioned|p588|Early Cambrian|Early Cambrian|||||||
6152|Emu Bay Shale|60990|6|Mentioned|p89|Early Cambrian|Early Cambrian|Contains the Type species of Estaingia bilobata Pocock (described in detail).||||||
6152|Emu Bay Shale|62270|5|Briefly described|p496, p505, p506 Fig. 4|Early Cambrian|Early Cambrian|Contains Emuellids (Trilobite family).  In Emu Bay,  Kangaroo Island.||||||
6152|Emu Bay Shale|62784|6|Mentioned|p36|Early Cambrian|Early Cambrian|Kangaroo Island, SA. Contains complete carapaces of Isoxys, described by Glaessner (1979).||||||
6152|Emu Bay Shale|62785|5|Briefly described|p43, p44 Fig.1|Early Cambrian|Early Cambrian|Type section in Emu Bay, Kangaroo Island. A Lagerstatte including trilobites, brachiopods and hyoliths occurs at Big Gully. Fauna compared with Shackleton Limestone, Antarctica.||||Unconformably overlies White Point Conglomerate and conformably underlies Boxing Bay Formation.||20-MAR-12
6152|Emu Bay Shale|63569|5|Briefly described|p122, p131|Early Cambrian|Early Cambrian|Kangaroo Island. Includes type species of Estaingia bilobata Pocock 196 4. Early Cambrian.||||||
6152|Emu Bay Shale|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Geological Province: Stansbury Basin. Flaggy purple shale with abundant trilobite tracks and moulds. Sandy limestone and burrow-mottled limestone bed at the base.||||||24-JUL-08
6152|Emu Bay Shale|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies White Point Conglomerate. Is overlain by Boxing Bay Formation.||
6152|Emu Bay Shale|65625|4|Described|p126, 103|Middle Cambrian|Early Cambrian|Fauna includes trilobites, crustaceans and annelids. Redlichia, Lusatiops, ?Acrothele, Hyolithes.||Of Kangaroo Island Group.||Conformable over White Point Conglomerate; conformable under Boxing Day Formation.|Brown and purple micaceous shales, flagstones; minor interbedded reddish quartzites.|13-APR-11
6152|Emu Bay Shale|65667|4|Described|p1221-p1223|Early Cambrian|Early Cambrian|Has two Lagerstatte sites: Big Gully, and Buck Quarry where ~60 m thick. Age: correlated with the traditional lower Cambrian (Series 2) Pararaia janeae trilobite Zone of South Aust., mid Canglangpuan Stage of China and the mid-late Botoman of Siberia.||||Conformably underlies Boxing Bay Formation and unconformably overlies White Point Conglomerate along coast|Dark grey, sporadically pyritic, highly fossiliferous mudstone, siltstone, sandstone, conglomerate.|10-DEC-12
6152|Emu Bay Shale|65686|6|Mentioned|p411, 414|Early Cambrian|Early Cambrian|Kangaroo Island. Fossiliferous.||||||07-MAY-12
6152|Emu Bay Shale|65892|5|Briefly described|p9 Fig.4, p21-22, p24. |Early Cambrian|Early Cambrian|North Coast of Kangaroo Island. Type section at Emu Bay is 55m thick. Fossils are abundant but of low diversity. Presence of Holyoakia and other trilobites allows correlation with Shackleton Limestone in Antarctica.||||Overlies White Point Conglomerate unconformably. Is overlain conformably by Boxing Bay Formation.|Dark grey silty shales with thin sandstone interbeds; minor conglomerate; fossiliferous.|
6152|Emu Bay Shale|65921|6|Mentioned|p1|Cambrian|Cambrian|Contains trilobites at Big Gully.||Of the Kangaroo Island Group.||||
6152|Emu Bay Shale|66761|3|Fully described|p243-246, 248-255|Early Cambrian|Early Cambrian|78m thick along coast. Base of unit is a sequence boundary.||Of Kangaroo Island Group.|||Basal conglomerate with fine sandstone and mudstone (containing the fossil Lagerstatte within basal 10 m) above; sandstone and conglomerate above.|14-MAR-12
6152|Emu Bay Shale|67344|4|Described|p259-269|Early Cambrian|Early Cambrian|Cambrian Series 2, Stage 4. Contains exceptionally well-preserved fauna. Deposited in a proximal inner shelf setting, possibly semi-enclosed, adjacent to an active tectonic margin. ~ 78m thick. Lagerstatte confined to the lowermost 10m of the Formation. Of the Stansbury Basin.||||Overlies Marsden Formation paraconformably. Conformably overlain by the Boxing Bay Formation.|Dark grey silty shale.|17-SEP-14
6152|Emu Bay Shale|69372|6|Mentioned|p27 fig. 5, p34 fig. 12|Cambrian|Cambrian|||Kangaroo Island Group|||Shale.|
6152|Emu Bay Shale|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Flaggy purple shale with abundant trilobite tracks and moulds. Sandy limestone and burrow-mottled limestone bed at the base.|
6152|Emu Bay Shale|73247|5|Briefly described|p204-207, p209-210|Cambrian (Stage 4)|Cambrian (Stage 4)|Part of the eastern succession of the Kangaroo Island Group. Contains the internationally recognised Konservat-Lagerstatte at Big Gully in the basal 10 to 15 m. Fossil evidence is used to correlate the unit with the Smith Bay Shale from the western succession.||Kangaroo Island Group||Unconformably underlain by Marsden Sandstone. Overlain by Boxing Bay Formation. Correlates to Smith Bay Shale. Equivalent to Kanmantoo Group.|Fossiliferous shales and interbedded quartzites.|03-FEB-23
6152|Emu Bay Shale|75071|5|Briefly described|p206-207, 209, 211-214|Early Cambrian|Early Cambrian|Hosts the richest Burgess Shale-type fossil assemblage in the Southern Hemisphere. The product of siliciclastic sedimentation in a nearshore setting with a localised deeper-water mini-basin. V/Al2O3 and Ba/Al2O3 paleoredox proxy diagrams.|||||Dark grey, fawn-weathering, micaceous, slightly calcareous, fossiliferous laminated mudstone with associated siltstone and sandstone interbeds.|
6174|Encounter Bay Granite|22530|6|Mentioned|p693|Late Cambrian|Middle Cambrian|||||||
6174|Encounter Bay Granite|23996|5|Briefly described|p354|Cambrian|Cambrian|Age: 508+/-14Ma.  Geological Province: Adelaide Fold Belt.||||||16-MAR-22
6174|Encounter Bay Granite|24465|5|Briefly described|p351 Fig.1|Cambrian|Cambrian|||||||
6174|Encounter Bay Granite|29872|6|Mentioned|p77|||||||||
6174|Encounter Bay Granite|30381|6|Mentioned|p226|||See also p213,214,228,235,Fig.4||||||16-MAR-22
6174|Encounter Bay Granite|30398|5|Briefly described|p259|||||||||
6174|Encounter Bay Granite|32146|6|Mentioned|p369|||||||||
6174|Encounter Bay Granite|32196|6|Mentioned|p149|||Synon. "Encounter Bay Granite"||||||
6174|Encounter Bay Granite|32457|4|Described|p88|||||||||
6174|Encounter Bay Granite|35358|6|Mentioned|p18|||Age dating||||||
6174|Encounter Bay Granite|36833|6|Mentioned|p23|||||||||
6174|Encounter Bay Granite|38873|6|Mentioned|Fig.3|||||||||
6174|Encounter Bay Granite|38927|6|Mentioned|p54|||||||||
6174|Encounter Bay Granite|39524|6|Mentioned|p67|||||||||
6174|Encounter Bay Granite|40442|6|Mentioned|p17|||||||||
6174|Encounter Bay Granite|40454|4|Described|p43|||||||||
6174|Encounter Bay Granite|40695|6|Mentioned|p13|||||||||
6174|Encounter Bay Granite|40763|4|Described|p208|||||||||
6174|Encounter Bay Granite|42100|6|Mentioned|p71|||||||||
6174|Encounter Bay Granite|42154|5|Briefly described|p335|||||||||
6174|Encounter Bay Granite|42271|6|Mentioned|p372|||||||||
6174|Encounter Bay Granite|42273|5|Briefly described|p422|||||||||
6174|Encounter Bay Granite|42813|6|Mentioned|p24|||||||||
6174|Encounter Bay Granite|42971|5|Briefly described|p153|||||||||
6174|Encounter Bay Granite|43781|6|Mentioned|p3|||K/Ar Age: 504+/-8 Ma, 495+/-6 Ma||||||
6174|Encounter Bay Granite|67536|5|Briefly described|Map Legend|Tremodocian|Ediacaran|Kanmantoo Province; basement to Murray Basin.|ca. 564 +/- 57 Ma - 486 +/- 6 Ma||||Pre/syn-Delamerian felsic intrusive rocks.|
6174|Encounter Bay Granite|69372|6|Mentioned|p25|||Clasts of this unit are found in the Cape Jervis Formation.||||||
6174|Encounter Bay Granite|70382|6|Mentioned|p34|Early Ordovician|Cambrian|Felsic intrusive magmatic phase during the late stages of, and immediately post-dating Cambrian Delamerian Orogeny (Foden et al., 2002, 2006; Preiss 1995).|~510-480 Ma||||A-type granite.|
6174|Encounter Bay Granite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Granite, megacrystic and even-grained. Comagmatic and metasedimentary enclaves. I-type to marginally S-type, syn-tectonic.|09-DEC-21
6174|Encounter Bay Granite|73236|6|Mentioned|p41|||Occurs as erratics in Cape Jervis Formation.||||||
6192|Eninta Sandstone|22651|6|Mentioned|p 174|||equivalent to Arumbera Sandstone.||||||
6192|Eninta Sandstone|29721|6|Mentioned|p44|||||||||
6192|Eninta Sandstone|31973|6|Mentioned|p3|||Correlation||||||
6192|Eninta Sandstone|33307|6|Mentioned|Fig.6|||||||||
6192|Eninta Sandstone|34442|5|Briefly described|Table 1|||Camb.||||||
6192|Eninta Sandstone|35088|6|Mentioned|p96|||||||||
6192|Eninta Sandstone|35102|6|Mentioned|Fig.2|||||||||
6192|Eninta Sandstone|35136|6|Mentioned|p140|||||||||
6192|Eninta Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
6192|Eninta Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
6192|Eninta Sandstone|40740|5|Briefly described|p12|||||||||
6192|Eninta Sandstone|40810|6|Mentioned|p3|||||||||
6192|Eninta Sandstone|40852|6|Mentioned|Fig.3.7|||||||||
6192|Eninta Sandstone|41224|6|Mentioned|Fig.2|||||||||
6192|Eninta Sandstone|41233|5|Briefly described|p16|||Is considered to belong to Arumbera Sandstone||||||
6192|Eninta Sandstone|42141|6|Mentioned|Table 2 P571|||||||||
6192|Eninta Sandstone|43011|6|Mentioned|Table 2,p12|||||||||
6192|Eninta Sandstone|43649|6|Mentioned|p457|||||||||
6192|Eninta Sandstone|43781|6|Mentioned|p4|||||||||
6192|Eninta Sandstone|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
6192|Eninta Sandstone|44484|14|Not recorded|p.10,14, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
6192|Eninta Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|45041|4|Described|p52|||||||||
6192|Eninta Sandstone|45155|6|Mentioned|p28|||See also P34||||||
6192|Eninta Sandstone|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
6192|Eninta Sandstone|48863|14|Not recorded|Not recorded|||||||||
6192|Eninta Sandstone|48865|14|Not recorded|Not recorded|||||||||
6192|Eninta Sandstone|48963|6|Mentioned|Fig.3|||||||||
6192|Eninta Sandstone|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Red brown sandstone, silty sandstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
6192|Eninta Sandstone|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
6192|Eninta Sandstone|67565|6|Mentioned|p39.|Early Cambrian|Neoproterozoic|These strata, previously mapped (Ranford, 1969) in the Gardiner Range, are now included in the Arumbera Sandstone.||||||
6192|Eninta Sandstone|69437|6|Mentioned|p22:10|Cambrian|Cambrian|Amadeus Basin.||||||12-JUL-16
6192|Eninta Sandstone|69438|4|Described|p23:3, 24, 27, 53|Early Cambrian|Early Cambrian|Wells et al. (1965). Forms a prominent strike ridge in the Gardiner Range Anticline, Amadeus Basin. The type area was defined in MOUNT LIEBIG map, but the unit is subsumed into Arumbera Sandstone.||Pertaoorrta Group.|||Sandstone with minor siltstone and conglomerate. Generally thin-bedded, cross-bedded, micaceous, feldspathic and immature. Local beds of conglomerate, with clasts predominantly of chert and carbonate rocks.|12-JUL-16
6192|Eninta Sandstone|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
6192|Eninta Sandstone|72369|5|Briefly described|p20-21|||Of Amadeus Basin. Possibly correlable to Puna Kura Kura Formation.||Unit of Pertaoorrta Group.||||
6192|Eninta Sandstone|72374|5|Briefly described|iii,p3-4,12-14|Early Cambrian|Neoproterozoic|Of Amadeus Basin. Typically thinly-bedded, crossbedded, micaceous, feldspathic and immature (Edgoose 2013), with basal conglomerates. Originally mapped and interpreted to be laterally equivalent to Arumbera Sandstone and Quandong Conglomerate (Ranford and Cook, 1964). Sample HB16ND276 (sandstone) yielded an interpreted maximum depositional age of 1021+\-9 Ma. Dominant zircon population between c. 1205 to 1000 Ma (peak c. 1162 Ma) likely derived from Musgrave Province (either directly or reworking from underlying stratigraphy). Subordinate c. 1900-1380 Ma zircon age spectrum likely sourced from the Aileron and Warumpi provinces to the north, and Musgrave Province to the south. Archean c. 2756-2400 Ma zircons likely sourced from terranes from east Gondwana, or the North Australian Craton.||Unit of Pertaoorrta Group.|||Sandstone with minor siltstone and conglomerate.|11-OCT-19
6221|Epsilon Formation|13497|3|Fully described|iv, v, viii, x, xi, xii|Kungurian|Artinskian|Cooper Basin. Defined by Gatehouse 1972. The name is derived from the Epsilon Parish in Carruthers County, South West Queensland. Originally included in the Moomba Formation bnefore Gatehouse raised it to formation status in 1972. A type section is mentioned. Petrography discussed briefly. Maximum thickness of 156m in the Nappamerri Trough. A cross section is provided on p96 with detailed lithology information for this unit.  Sandstones were deposited in a fluvio-deltaic or shoreline environment. Hosts economic gas deposits. See also  xiii, p58, p61, p69 fig 6.1, p70-p71, p93-p98, p101, p119, p131, p132, p144 fig 9.2, p148-p151, p157, p159-p163, p164 fig 10.6, p169-p170, p174-p175, p182, p191, p193-p196, p204-p205.||Gidgealpa Group||Conformably overlies the Murteree Shale. Intertongues with and is conformably overlain by the Roseneath Shale. Unconformably (or disconformably) overlain by the Toolachee Formation.|Thinly bedded, fine to medium-grained, moderately to very well sorted, quartzose sandstone with dark grey-brown carbonaceous siltstone and shale and thin to occasionally thick coal seams.|
6221|Epsilon Formation|13516|6|Mentioned|p147, fig 5|Late Permian|Late Permian|From Cooper Basin||||||
6221|Epsilon Formation|22527|6|Mentioned|p 1|||||||||
6221|Epsilon Formation|22839|6|Mentioned|P33|||||||||
6221|Epsilon Formation|22883|6|Mentioned|P29|||||||||
6221|Epsilon Formation|22909|5|Briefly described|42|||||||||
6221|Epsilon Formation|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Parent - Gidgealpa Group.||||||
6221|Epsilon Formation|23155|4|Described|p21|Early Permian|Early Permian|The Roseneath Shale is diachronous, younging southwest.  On STRZELECKI the unit is overlain by Daralingie Formation and underlain by Epsilon Formation.||||||
6221|Epsilon Formation|23375|4|Described|Fig2 p265,285|Kungurian|Artinskian|In the Cooper Basin.||||||17-JAN-08
6221|Epsilon Formation|23832|4|Described|p329|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
6221|Epsilon Formation|24199|5|Briefly described|p512 Fig.2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
6221|Epsilon Formation|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group. Overlies the Murteree Shale. Geological Province: Cooper Basin.  See also p132.||||||14-APR-08
6221|Epsilon Formation|24212|5|Briefly described|p67 Fig. 3, p69|Early Permian|Early Permian|Age: <280Ma.  Geological Province: Cooper Basin.||||||
6221|Epsilon Formation|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
6221|Epsilon Formation|29389|6|Mentioned|p18|||Permian.||||||
6221|Epsilon Formation|29391|6|Mentioned|Table 5|||See P23.||||||
6221|Epsilon Formation|29518|6|Mentioned|p24|||||||||
6221|Epsilon Formation|29721|6|Mentioned|p172|||||||||
6221|Epsilon Formation|29729|6|Mentioned|p268|||||||||
6221|Epsilon Formation|30540|6|Mentioned|p65|||Reservoir||||||
6221|Epsilon Formation|30544|6|Mentioned|p53|||||||||
6221|Epsilon Formation|30825|6|Mentioned|p37|||||||||
6221|Epsilon Formation|30873|2|Defined|p13|Permian|Permian|Part of Gidgealpa Group||||||
6221|Epsilon Formation|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
6221|Epsilon Formation|32696|6|Mentioned|Fig.4|||Refers Gatehouse (1972)||||||
6221|Epsilon Formation|33074|6|Mentioned|p260|||||||||
6221|Epsilon Formation|33331|6|Mentioned|p39|||||||||
6221|Epsilon Formation|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
6221|Epsilon Formation|33976|6|Mentioned|Fig.5|||||||||
6221|Epsilon Formation|34839|6|Mentioned|Fig.2|||||||||
6221|Epsilon Formation|35067|6|Mentioned|Fig.4|||||||||
6221|Epsilon Formation|35068|6|Mentioned|Fig.3|||Discussed P58.||||||
6221|Epsilon Formation|35279|6|Mentioned|Fig.5|||||||||
6221|Epsilon Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
6221|Epsilon Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
6221|Epsilon Formation|35845|4|Described|p24|||Lithology and depositional environments. See also p66.||||||17-JAN-08
6221|Epsilon Formation|36099|6|Mentioned|p191|||||||||
6221|Epsilon Formation|36910|6|Mentioned|p62|||||||||
6221|Epsilon Formation|36917|6|Mentioned|Fig.1|||||||||
6221|Epsilon Formation|37287|6|Mentioned|p36|||||||||
6221|Epsilon Formation|37855|6|Mentioned|Fig.2|||||||||
6221|Epsilon Formation|37917|6|Mentioned|Fig.2|||||||||
6221|Epsilon Formation|38977|6|Mentioned|p1424|||||||||
6221|Epsilon Formation|39252|5|Briefly described|p20|||||||||
6221|Epsilon Formation|39254|5|Briefly described|p46|||See also P47||||||
6221|Epsilon Formation|39261|6|Mentioned|Fig. 9|||||||||
6221|Epsilon Formation|39264|6|Mentioned|Fig. 13|||||||||
6221|Epsilon Formation|39276|6|Mentioned|Fig. 2|||||||||
6221|Epsilon Formation|39445|5|Briefly described|Table 8|||||||||
6221|Epsilon Formation|39478|6|Mentioned|Table 1|||||||||
6221|Epsilon Formation|39494|6|Mentioned|Fig.3|||||||||
6221|Epsilon Formation|40030|6|Mentioned|Fig.3|||||||||
6221|Epsilon Formation|40249|6|Mentioned|p45|||||||||
6221|Epsilon Formation|40544|6|Mentioned|Fig.4|||||||||
6221|Epsilon Formation|41099|6|Mentioned|p190|||||||||
6221|Epsilon Formation|41123|6|Mentioned|p180|||||||||
6221|Epsilon Formation|41131|5|Briefly described|Table 1|||||||||
6221|Epsilon Formation|41164|6|Mentioned|Table 1|||||||||
6221|Epsilon Formation|41183|6|Mentioned|Fig.3 p308|||||||||
6221|Epsilon Formation|41189|6|Mentioned|p249|||||||||
6221|Epsilon Formation|41198|6|Mentioned|Table 1|||||||||
6221|Epsilon Formation|41223|6|Mentioned|p408|||||||||
6221|Epsilon Formation|41226|6|Mentioned|Table 1|||||||||
6221|Epsilon Formation|41247|6|Mentioned|p117|||||||||
6221|Epsilon Formation|41267|6|Mentioned|p256|||||||||
6221|Epsilon Formation|41288|6|Mentioned|p159|||||||||
6221|Epsilon Formation|41595|6|Mentioned|Fig.4|||||||||
6221|Epsilon Formation|41689|6|Mentioned|Table 1|||||||||
6221|Epsilon Formation|42085|6|Mentioned|Fig.2 P374|||||||||
6221|Epsilon Formation|42256|6|Mentioned|Fig.1 P243|||||||||
6221|Epsilon Formation|42395|5|Briefly described|Fig.13 P83|||||||||
6221|Epsilon Formation|42746|5|Briefly described|p6|||||||||
6221|Epsilon Formation|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
6221|Epsilon Formation|43002|5|Briefly described|Fig.2,p135|||||||||
6221|Epsilon Formation|43018|5|Briefly described|Table 1,p386|||||||||
6221|Epsilon Formation|43105|5|Briefly described|Fig.7,p13|||||||||
6221|Epsilon Formation|43570|5|Briefly described|Fig.2,p535,544|Kungurian|Artinskian|||||||
6221|Epsilon Formation|43628|6|Mentioned|Fig.3||Early Permian|||||||
6221|Epsilon Formation|43711|6|Mentioned|p20|||||||||
6221|Epsilon Formation|44133|4|Described|p65 Fig. 8.3, 84|Kungurian|Kungurian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlies: Murteree Shale. Up to 140m thick. Overlain by the Roseneath Shale.||||||
6221|Epsilon Formation|46849|6|Mentioned|Fig. 7|||||||||
6221|Epsilon Formation|60386|6|Mentioned|p296|Kungurian|Artinskian|Cooper Basin. Non-marine, coal.||||||
6221|Epsilon Formation|60717|5|Briefly described|p40 Fig. 2|Kungurian|Artinskian|Of Gidgealpa Group. Overlies Murteree Shale; underlies Roseneath Shale. Thickness: 140m. Geological Province: Cooper Basin.||||||31-JAN-08
6221|Epsilon Formation|61015|6|Mentioned|p45|Triassic|Triassic|Gas discovered in this formation.||||||
6221|Epsilon Formation|61614|6|Mentioned|p290 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
6221|Epsilon Formation|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304|Early Permian|Early Permian|Of Gidgealpa Group. Conformbaly underlain by Parchawarra Formation. Geological Province: Cooper Basin.||||||07-FEB-11
6221|Epsilon Formation|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
6221|Epsilon Formation|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
6221|Epsilon Formation|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Murteree Shale. Is overlain by Roseneath Shale.||
6221|Epsilon Formation|63832|6|Mentioned|p131 fig 2|Kungurian|Kungurian|Cooper Basin.||||||
6221|Epsilon Formation|63978|2|Defined|p14, Fig. 3|Early Permian|Early Permian|Conformably overlies Murteree Shale; conformably underlies Roseneath Shale. Unconformably overlain by Toolachee Fm. in places. Sandstone, siltstone, mudstone and coal (extensive), variably proportioned - more lith. given. Max. thick: 92m. Cooper Basin||||||07-FEB-11
6221|Epsilon Formation|64048|5|Briefly described|p63, p64 Tb. 2, p66|||Some hydrocarbons; contains 13 gas and liquid fields. Geological Province: Cooper Basin.||||||07-FEB-11
6221|Epsilon Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Permian|Middle Permian|Cooper Basin.||||Overlies Murteree Shale; is overlain by Roseneath Shale.||10-DEC-15
6221|Epsilon Formation|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Contains hydrocarbon source rocks and reservoirs.||||Overlies Murteree Shale. Is overlain by Roseneath Shale.||
6221|Epsilon Formation|65489|5|Briefly described|p15, p48-49, p96, p131-132, p143|Kungurian|Kungurian|Cooper Basin. 140m thick. Gas reservoir accounting for 4% of the Basin's production.||Unit in Gidgealpa Group.||Overlies Murteree Shale. Is overlain by Roseneath Shale.|Fluviodeltaic sediments.|
6221|Epsilon Formation|65925|5|Briefly described|Appendix 2.||||||||Shale, siltstone, sandstone and coal. Fluvio-deltaic, lacustrine, with transgressive and regressive successions.|
6221|Epsilon Formation|67402|5|Briefly described|p43 tbl HPB1, p90|||Cooper Basin. Highly prospective formation for the storage of carbon dioxide. Roughly 50-100m thick. Sandstones were deposited in a shoreface to lacustrine/deltaic environment whereas the finer grained units were deposited in inter-distributary and floodplain environments. See also p90 fig CPR4, p91 tbl CPR1, p92, p93, p96, p99 fig CPR14, p101, p101 tbl CPR2.||Gidgealpa Group||Overlies the Murteree Shale. Overlain by the Roseneath Shale.|Thinly bedded, fine to medium-grained, moderately to very well sorted sandstone, with carbonaceous siltstone, mudstone and thin coal beds.|
6221|Epsilon Formation|68068|5|Briefly described|Map legend|Early Permian|Early Permian|Cooper Basin (subsurface only).||Topmost unit in Gidgealpa Group.||Conformably ovelies Murteree Shale.|Off-white, fine-grained, ripple-laminated, thinly-bedded sandstone, locally thick with interlaminated siltstone, or thin with interbedded mudstone and coal; three depositional cycles: base and top upward-coarsening sandstone; middle is coal dominant|
6221|Epsilon Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Guadalupian|Cisuralian|Gatehouse (1972). Along with the Murteree Shale and Roseneath Shale, the Epsilon Formation unit replaces the Moomba Formation. ~ 30-156 m thick. Contains Kungurian palynofloras (Price 1997). Detailed lithology discussed.||Of the Gidgealpa Group.||Conformably underlain by the Murteree Shale. Conformably overlain by the Roseneath Shale. Unconformably overlain by the Toolachee Formation. Intertongues with the Roseneath Shale.|Comprises sandstone, siltstone, mudstone, and coal in varying proportions in shoreface, deltaic and lacustrine deposits in three depositional stages.|
6221|Epsilon Formation|69023|4|Described|p79, p82, p85, p191-192|Permian|Permian|Defined by Gatehouse (1972). Cooper Basin. Gas reserves. ~27 to >45m of fluvio-deltaic sediments. Diachronous: Early to Late Permian, younging to the W. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation, and Murteree Shale conformably. Is overlain by Algebuckina and Namur Sandstones.|Basal and top units are thinly-bedded, fine- to medium-grained quartz sandstones; dark grey-brown, carbonaceous and slightly pyritic siltstone and mudstone; extensive but generally thin (<0.3 - 3m) coal seams.|
6221|Epsilon Formation|69454|5|Briefly described|p38:4|Kungurian|Kungurian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
6221|Epsilon Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Roseneath Shale, overlies Murteree Shale, Patchawarra Formation||
6221|Epsilon Formation|69797|5|Briefly described|p17 Fig.2|Early Permian|Early Permian|Age: Artinskian - Kungurian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
6221|Epsilon Formation|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Artinskian|Cooper Basin. Fluviodeltaic sediments.||Unit in Gidgealpa Group.||Overlies Murteree Shale. Is overlain by Roseneath Shale.||
6221|Epsilon Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
6221|Epsilon Formation|70317|6|Mentioned|p33, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Murteree Shale. Is overlain by Roseneath Shale.||
6221|Epsilon Formation|70823|4|Described|iv, p6, p14-p15|Roadian|Kungurian|Cooper Basin. Seismic reflection characteristics briefly discussed. Up to 190m thick. Deposited in fluviodeltaic, lacustrine and peat swamp environments. Palynology is discussed briefly as are outcrop characteristics. This unit contains a wide distribution of good reservoirs, however it is considered less predictable for exploitation than the Patchawarra and Toolachee formations. See also p25-p27, p40-p41, p54, p58-p64, p78-p80, p82.||Gidgealpa Group||Conformably overlies the Murteree Shale. Intertongues and is conformably overlain by the Roseneath Shale. Unconformably overlain by the Toolachee Formation.|Fine to medium-grained quartzose sandstone interbedded with dark grey-brown carbonaceous siltstone and shale, and thin to occasionally thick coal seams.|
6221|Epsilon Formation|70824|4|Described|p2, p5, p7-p9, p19|Roadian|Kungurian|Cooper Basin. Hosts good to excellent source rocks. This unit has an average thickness of 50m but reaches up to 190m thick in the Nappamerri Trough. Deposited in fluviodeltaic and lacustrine with peat swamp environments. Outcrop characteristics and source rock geochemistry discussed. See also p32, p59, p66-p77, p108-p110, p113, p122-p123.||||Overlies the Murteree Shale. Overlain by the Roseneath Shale.|Fine to medium-grained quartzose sandstone interbedded with dark grey-brown carbonaceous siltstone and shale and thin to occasionally thick coal seams.|
6221|Epsilon Formation|70946|5|Briefly described|p1087, p1089-1091, p1096|Permian|Early Permian|Cooper Basin. Fluvio-deltaic tight sands. HyLogging was combined with XRD and core petrology to target fracture stimulation. Deposited in lacustrine with interbedded fluvio-deltaic transgressive/regressive shoreface environments.||Gidgealpa Group.||Overlies Murteree Shale. Is overlain by Roseneath Shale.||08-OCT-18
6221|Epsilon Formation|71265|5|Briefly described|p589|Wordian|Kungurian|Cooper Basin.||Gidgealpa Group.||Overlies Murteree Shale; locally Patchawarra Formation. Is overlain by Roseneath Shale.||
6221|Epsilon Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36|Kazanian|Kungurian|Cooper Basin. Deposited in a fluviodeltaic environment.  Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p45, Ch5 p54, Ch7 p13, Ch10 tbl 10.1-p7, Ch10 p19.||Gidgealpa Group||Overlies the Murteree Shale. Unconformably overlain by the Toolachee Formation.||
6221|Epsilon Formation|71701|5|Briefly described|p155, p170|Roadian|Kungurian|Cooper Basin.||Gidgealpa Group||Overlies the Murteree Shale. Overlain by the Roseneath Shale.||
6221|Epsilon Formation|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Cooper Basin.||||||
6221|Epsilon Formation|72297|6|Mentioned|p739, p742|||Cooper Basin. A petroleum source and reservoir rock; also contains gas.||||||
6221|Epsilon Formation|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments. Contains gas.||||||
6221|Epsilon Formation|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface environment. Gas.||||||
6221|Epsilon Formation|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Fluviodeltaic with local transgressive/regressive shoreface depositional environments. Contains[?] gas.||Gidgealpa Group||Underlain by and equivalent to Murteree Shale. Overlain by Roseneath Shale.||
6221|Epsilon Formation|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin. Hosts gas.||||Underlain by Patchawarra Formation. Overlain by Daralingie Formation. Equivalent to Murteree Shale.||
6221|Epsilon Formation|73479|5|Briefly described|p156 Fig.2, p159, p161, p163-164|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface depositional environment.|ca 262 Ma|||Overlies Patchawarra Formation||
6221|Epsilon Formation|73495|6|Mentioned|p497, p499-500|Guadalupian|Guadalupian|Cooper Basin. Part of the REM succession.||||Underlain by Murteree Shale. Overlain by Roseneath Shale.||
6237|Ernabella Adamellite|23818|6|Mentioned|p41|||||||||
6237|Ernabella Adamellite|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Age: 1120 Ma (Webb, 1985). Of the Kulgera Suite.  Geological Province: Musgrave Block.||||||
6237|Ernabella Adamellite|33889|5|Briefly described|p390|||Proterozoic||||||
6237|Ernabella Adamellite|33891|5|Briefly described|p543|||K/Ar ages.||||||
6237|Ernabella Adamellite|33892|6|Mentioned|p167|||1122+-98my. See also Fig.1.||||||
6237|Ernabella Adamellite|33994|6|Mentioned|p383|||1120+-100my||||||
6237|Ernabella Adamellite|34537|6|Mentioned|p41|||||||||
6237|Ernabella Adamellite|34604|4|Described|p253|||Refers Gemuts (1965) & Wilson (1960) P250||||||
6237|Ernabella Adamellite|35323|6|Mentioned|p404|||||||||
6237|Ernabella Adamellite|36792|6|Mentioned|p28|||||||||
6237|Ernabella Adamellite|40229|6|Mentioned|p27|||||||||
6237|Ernabella Adamellite|43052|5|Briefly described|p162|||of Kulgera Suite?||||||
6237|Ernabella Adamellite|45085|6|Mentioned|p13|||Age discussed. Isochron of 1,120 +/- 100m.y. with initial Sr87/86 0.7106||||||
6237|Ernabella Adamellite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Kulgera Suite. See also Ernabella Charnockite.||||||
6237|Ernabella Adamellite|69926|6|Mentioned|p157 Fig.1, p177-178|||||||||
6287|Etadunna Formation|9862|5|Briefly described|Map Legend|Tertiary|Tertiary|Flaggy dolomite, green clay, sandstone and siltstone.||||||
6287|Etadunna Formation|22587|6|Mentioned|p78|Early Miocene|Early Miocene|||||||
6287|Etadunna Formation|22912|4|Described|32|||||||||
6287|Etadunna Formation|23394|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6287|Etadunna Formation|23818|5|Briefly described|p174 Fig.84|Early Miocene|Early Miocene|Geological Province: Great Artesian Basin.||||||
6287|Etadunna Formation|24175|3|Fully described|p38, p32 Fig. 6|Pliocene|Late Oligocene|Age range given as above but "most probably largely Early Miocene".  Type section in Lake Eyre Bore 4.  Max. thickness: 44.5m.  Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|24176|6|Mentioned|p22 Tb. 1|Cenozoic|Cenozoic|Geological Province: Mount Painter Province.||||||19-NOV-08
6287|Etadunna Formation|24321|5|Briefly described|Map legend|Miocene|Miocene|Equivalent to Millers Creek Dolomite Member (of Mirkata Formation).  Includes the Moolarina Member.||||||
6287|Etadunna Formation|29427|6|Mentioned|p53|||||||||
6287|Etadunna Formation|29431|6|Mentioned|p23|||||||||
6287|Etadunna Formation|29659|6|Mentioned|p8|||||||||
6287|Etadunna Formation|29660|6|Mentioned|p5|||||||||
6287|Etadunna Formation|29897|6|Mentioned|p282|||||||||
6287|Etadunna Formation|30054|6|Mentioned|p803|||||||||
6287|Etadunna Formation|30055|6|Mentioned|p153|||||||||
6287|Etadunna Formation|30056|6|Mentioned|p135|||||||||
6287|Etadunna Formation|30061|6|Mentioned|p6|||?Late Olegocene.||||||
6287|Etadunna Formation|30163|6|Mentioned|p658|||||||||
6287|Etadunna Formation|30177|4|Described|p106|||Tertiary age.||||||
6287|Etadunna Formation|30514|6|Mentioned|p102|||||||||
6287|Etadunna Formation|30518|6|Mentioned|p88|||Tertiary age||||||
6287|Etadunna Formation|30540|6|Mentioned|Fig.6|||||||||
6287|Etadunna Formation|30804|5|Briefly described|p13|||See also Table 1||||||
6287|Etadunna Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
6287|Etadunna Formation|30918|6|Mentioned|p82|||||||||
6287|Etadunna Formation|30919|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|30920|6|Mentioned|Map legend|Miocene|Miocene|Equivalent of Namba Formation||||||
6287|Etadunna Formation|31532|4|Described|Table 1|||||||||
6287|Etadunna Formation|31699|4|Described|p132|||Mid Tertiary||||||
6287|Etadunna Formation|31968|6|Mentioned|p8|||Refers Stirton et al. (1961)||||||
6287|Etadunna Formation|32121|6|Mentioned|p422|||||||||
6287|Etadunna Formation|32275|6|Mentioned|p9|||||||||
6287|Etadunna Formation|32418|6|Mentioned|p2|||||||||
6287|Etadunna Formation|32652|6|Mentioned|p279|||||||||
6287|Etadunna Formation|33569|6|Mentioned|p63|||||||||
6287|Etadunna Formation|33819|6|Mentioned|p3|||||||||
6287|Etadunna Formation|33820|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33822|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33823|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33824|6|Mentioned|p13|||Table 1 & 2||||||
6287|Etadunna Formation|33827|6|Mentioned|p14|||See also Table 1||||||
6287|Etadunna Formation|33828|6|Mentioned|p4|||See also Table 1||||||
6287|Etadunna Formation|33937|5|Briefly described|p1|||||||||
6287|Etadunna Formation|33938|6|Mentioned|p20|||||||||
6287|Etadunna Formation|34180|6|Mentioned|Fig.108|||?Oligocene.||||||
6287|Etadunna Formation|34308|6|Mentioned|p200|||Correlation chart. Batesfordian - Balcombian||||||
6287|Etadunna Formation|34615|6|Mentioned|p10|||||||||
6287|Etadunna Formation|34754|6|Mentioned|p32|||||||||
6287|Etadunna Formation|34996|6|Mentioned|p145|||||||||
6287|Etadunna Formation|35003|6|Mentioned|p122|||Analysis||||||
6287|Etadunna Formation|35080|6|Mentioned|p12|||||||||
6287|Etadunna Formation|35187|6|Mentioned|Table1|||||||||
6287|Etadunna Formation|35772|6|Mentioned|p9|||||||||
6287|Etadunna Formation|35857|6|Mentioned|p197|||||||||
6287|Etadunna Formation|36213|6|Mentioned|p83|||||||||
6287|Etadunna Formation|36966|6|Mentioned|p81|||||||||
6287|Etadunna Formation|37062|6|Mentioned|p199|||||||||
6287|Etadunna Formation|37678|6|Mentioned|p237|||||||||
6287|Etadunna Formation|37754|6|Mentioned|p101|||||||||
6287|Etadunna Formation|38068|6|Mentioned|Fig.7|||||||||
6287|Etadunna Formation|38371|6|Mentioned|p666|||||||||
6287|Etadunna Formation|38605|6|Mentioned|p30|||||||||
6287|Etadunna Formation|38982|5|Briefly described|p64|||||||||
6287|Etadunna Formation|39085|6|Mentioned|p13|||||||||
6287|Etadunna Formation|39322|6|Mentioned|Fig.2|||||||||
6287|Etadunna Formation|39352|6|Mentioned|Map legend|early Pleistocene|middle Miocene|Middle Miocene to Early Pleistocene||||||
6287|Etadunna Formation|39521|6|Mentioned|p119|||||||||
6287|Etadunna Formation|40150|6|Mentioned|Fig.1|||||||||
6287|Etadunna Formation|40754|6|Mentioned|p10|||||||||
6287|Etadunna Formation|40755|5|Briefly described|App.3.1|||||||||
6287|Etadunna Formation|40756|5|Briefly described|p1|||||||||
6287|Etadunna Formation|40757|3|Fully described|p78|||||||||
6287|Etadunna Formation|40758|6|Mentioned|p87|||||||||
6287|Etadunna Formation|40910|6|Mentioned|p19|||||||||
6287|Etadunna Formation|40926|6|Mentioned|p28|||||||||
6287|Etadunna Formation|41098|6|Mentioned|p178|||||||||
6287|Etadunna Formation|41165|5|Briefly described|p365|||||||||
6287|Etadunna Formation|41537|6|Mentioned|p348|||||||||
6287|Etadunna Formation|41600|6|Mentioned|p827|||||||||
6287|Etadunna Formation|42340|6|Mentioned|p25|Miocene|Oligocene|||||||
6287|Etadunna Formation|42375|4|Described|p25-29|||Lake Eyre Basin Defined Stirton 1961.||||||
6287|Etadunna Formation|42390|5|Briefly described|Fig.2 P335|||||||||
6287|Etadunna Formation|42469|5|Briefly described|p39|||||||||
6287|Etadunna Formation|42477|5|Briefly described|p184, 192, 196|||||||||
6287|Etadunna Formation|42508|5|Briefly described|p74|||||||||
6287|Etadunna Formation|42592|5|Briefly described|Fig.4 P270|||Type locality indicated p272.||||||18-SEP-06
6287|Etadunna Formation|42746|5|Briefly described|p17|||Lake Eyre Basin. See also Fig.2 p4.||||||18-SEP-06
6287|Etadunna Formation|42784|6|Mentioned|p485|||||||||
6287|Etadunna Formation|42813|6|Mentioned|p24|||||||||
6287|Etadunna Formation|43035|6|Mentioned|p27|||||||||
6287|Etadunna Formation|43041|5|Briefly described|Fig.1,p590|||||||||
6287|Etadunna Formation|43048|5|Briefly described|p22|||||||||
6287|Etadunna Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||25-MAY-05
6287|Etadunna Formation|43071|5|Briefly described|p17|||||||||
6287|Etadunna Formation|43094|5|Briefly described|p38|||||||||
6287|Etadunna Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
6287|Etadunna Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
6287|Etadunna Formation|43681|6|Mentioned|p297||Miocene|||||||
6287|Etadunna Formation|44133|4|Described|p193, 187, 190 Fig. 10.30|Late Miocene|Late Oligocene|Correlates with the Neuroodla Formation. Geoloigcal Province: Lake Eyre Basin. Overlies Eyre Formation. Includes: Mampuwordu Sand, Muloorina Member. Thickness: 80m. ||||||
6287|Etadunna Formation|44221|14|Not recorded|p.93||Miocene|Miocene?||||||
6287|Etadunna Formation|44223|14|Not recorded|p.151,158||Oligocene|Fig.2.||||||
6287|Etadunna Formation|44224|14|Not recorded|p.1,5,27|Early Miocene|Late Oligocene|late Oligocene or early Miocene (H/54-5).||||||
6287|Etadunna Formation|44225|14|Not recorded|p.45|||(H/54-5).||||||
6287|Etadunna Formation|44238|14|Not recorded|p.225,227,228|Early Miocene|Late Oligocene|Fig.3. U.Olig.- L.Miocene.||||||
6287|Etadunna Formation|44829|6|Mentioned|p40|||On SA card.||||||
6287|Etadunna Formation|44934|6|Mentioned|Map Legend|Miocene|Eocene|||||||
6287|Etadunna Formation|45128|6|Mentioned|p53|||||||||
6287|Etadunna Formation|45145|6|Mentioned|p37|||See also Table 7.||||||
6287|Etadunna Formation|45155|6|Mentioned|p46|||||||||
6287|Etadunna Formation|46802|6|Mentioned|Table 1|||||||||
6287|Etadunna Formation|46833|6|Mentioned|p56|||||||||
6287|Etadunna Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Late Oligocene|Late Oligocene|Contains abundant gastrapod fossils. Overlain by the Wipajiri Formation. Age: 25.7-24.2 Ma. Geological Province: Lake Eyre Basin (Tirari Sub-basin).||||||12-APR-05
6287|Etadunna Formation|60785|5|Briefly described|p197.|||A correlate of the Namba Formation.|24 - 28 Ma (Woodburne et al. 1993).|||Correlate of the Namba Formation.||
6287|Etadunna Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|61119|5|Briefly described|p124, p129, pp132-135, pp143-4, p146||Cenozoic|Older than Wipajiri Formation [underlies]. Freshwater lake deposits. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
6287|Etadunna Formation|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Age: 21-12.5Ma. Thickness: 50m. Geological Province: Lake Eyre Basin.||||||03-MAR-10
6287|Etadunna Formation|61517|5|Briefly described|p312|Miocene|Miocene|Dolomitic limestone.||||||
6287|Etadunna Formation|64197|6|Mentioned|p627, p630 Fig.6|Middle Miocene|Middle Miocene|Unconformably overlies the Eyre Formation.||||||
6287|Etadunna Formation|65194|5|Briefly described|p49, p171|Miocene|Oligocene|Lake Eyre Basin. Dolomitic lacustrine deposits - these sediments form sheet or blanket cover sequences and palaeovalley infill.||||||
6287|Etadunna Formation|65684|6|Mentioned|p807|Late Oligocene|Late Oligocene|Age confirmed as Oligocene by magnetostratigraphy (Woobdurne et al, 1994).||||||
6287|Etadunna Formation|65925|5|Briefly described|p17, Appendix 2.|||Tirari Sub-basin. Equivalent to Namba Formation.|||||White dolomite and limestone with green and grey Mg rich claystone and fine-grained sand.|
6287|Etadunna Formation|66131|4|Described|p240, p242-245, p249, p255, p259|Miocene|Oligocene|Tirari Sub-basin. Between 25-80 m thick. Contains abundant fossils. Type section at Lake Palankarina.|||Includes Mampuwordu Sand, Muloorina Member.|Overlies Eyre Formation. Disconformably overlain by the Katipiri Formation. Correlative of the Caldelga Limestone and Alberga Limestone Member. ?Overlain by the Waite Formation.|Comprises white dolomite and limestone overlain by Mg-rich green and grey claystone and fine sand. Intraformational conglomerate and bioturbation are widespread. Silcrete capping.|
6287|Etadunna Formation|66573|5|Briefly described|Throughout the article.|Miocene|Oligocene|Disconformably overlies the Eyre Formation; is overlain unconformably by Tirari Formation. Grey dolomitic marls and shales. 26.1 - 23.6 Ma.||||||
6287|Etadunna Formation|66623|6|Mentioned|p282.|||Wopfner (1974) tentatively correlated at least the base of this unit with the Doonbara Formation in NSW.||||||21-MAY-13
6287|Etadunna Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.|||Includes Muloorina Member and Mampuwordu Sand.|||
6287|Etadunna Formation|67578|5|Briefly described|p333, p335-339, p342-344.|Miocene|Oligocene|Lake Eyre Basin. Originally defined by Stirton et al. (1961). Lacustrine facies. Age range determined from a single Rb/Sr isotope analysis, as well as foraminiferal assemblages (latest Oligocene to Middle Miocene). Thickness exceeds 20m in drill core. Affected by widespread post-depositional silicification.||||Unconformably overlain by the Eyre Formation.|Consists of white-grey, fine-grained chemical and clastic sediments. Channel sands occur in the upper part of the Formation at several locations.|
6287|Etadunna Formation|68068|5|Briefly described|Map legend|||Callabonna Sub-basin, Lake Eyre Basin. Occurs W & NW of Callabonna sheet.Equivalent to the Namba Formation to the east and southeast.||||||25-NOV-14
6287|Etadunna Formation|68715|6|Mentioned|p30 Fig.5|Langhian|Burdigalian|Tirai and northern Callabonna sub basins, Lake Eyre Basin.|||Muloorina Member.|||07-APR-17
6287|Etadunna Formation|68821|4|Described|p296|Serravallian|Chattian|Consists largely of immature fluvio-lacustrine sand, silt, and clay deposited in an alkaline and anoxic environment. Includes levels of pyritic laminated carbonaceous mud and fossils - gastropods, ostracods, algae, fish, reptiles, birds and mammals.|26 - 12 Ma|||Locally underlain by the Eyre Formation.|Consists of quartz (< 50%), kaolinte (< 40%), feldspar (< 15%), mica (< 15%), smectite(< 5%), illite (a few %), palygorskite and dolomite, gypsum and alunite.|
6287|Etadunna Formation|69019|3|Fully described|p83 Fig.20, p105 Fig.25, p110-113.|Miocene|Oligocene|Tirari Sub-basin, Lake Eyre Basin. Of Stirton et al. (1961). Type section is on western shores of Lake Palankarinna. Thickness to 44 m. Age is from a specimen of palygorskite clay. Has developed a porcellanite horizon.|c.25 Ma (Rb-Sr, Norrish and Pickering 1983)||Includes Muloorina Member.|Overlies Mirackina Conglomerate; unconformably overlies Eyre Formation. Is overlain by Yardinna Claystone, Alberga Limestone and Wipajiri Formation. Contemporaneous with Namba Formation.|Sandy claystone and sand with silty and gypseous clay and flaggy dolomite below bedded sandstone; overlain by  sand, silt and clay, cross-bedding throughout, and local intercalated dolomite nodules and beds.|
6287|Etadunna Formation|69023|5|Briefly described|p87, p108, p117-118, p120, p125, p193|||Stratigraphic wells intersection data.|||Includes Muloorina Member.|Time-equivalent of Namba Formation.||
6287|Etadunna Formation|69458|5|Briefly described|p42:16, 19, 22|Miocene|Oligocene|Lake Eyre Basin. Extensive shallow, alkaline lacustrine to fluvial deposits. Lower parts contain a vertebrate assemblage with affinities with the Pwerte Marnte Marnte fauna.||||Correlated with Ulta Limestone.|Interbedded sandstone, siltstone, shale and locally developed dolostone.|12-JUL-16
6287|Etadunna Formation|69572|6|Mentioned|p1188, 1190|Miocene|Oligocene|Contains fossils of the oldest (24 m.y.) phascolarctid koalas. Other species and locations tabulated.||||||
6287|Etadunna Formation|69946|5|Briefly described|p29, p129|Miocene|Oligocene|Tirari Sub-basin, Lake Eyre Basin. Callen et al. (1995). On p129, shown in two parts: Etadunna Formation (Lower) and Etadunna Formation (Upper).|||||Carbonate and clastics from evaporation of magnesian lakes.|
6287|Etadunna Formation|70321|6|Mentioned|p153-154|Oligocene|Oligocene|Contains the only late Oligocene terrestrial-mammal fossil assemblage radiometrically dated.||||||
6287|Etadunna Formation|71317|5|Briefly described|p144|||||||Equivalent to the Garford Formation.||
6287|Etadunna Formation|71342|5|Briefly described|Ch5 p29, Ch5 p130|Miocene|Oligocene|Lake Eyre Basin. |||||Carbonates and clastic rocks.|
6287|Etadunna Formation|72456|5|Briefly described|Map Legend|Pliocene|Oligocene|Marree 1:250k map sheet.|||||White dolomite and limestone with green and grey Mg rich claystone and fine-grained sand.|
6287|Etadunna Formation|73234|6|Mentioned|p23|||Lake Eyre Basin.||||Equivalent to Neuroodla Formation.||
6287|Etadunna Formation|73479|6|Mentioned|p156 Fig.2|Neogene|Neogene|Lake Eyre Basin.||||Overlies Eyre Formation||
6307|Etina Formation|22510|5|Briefly described|p39, table1|||Of the Upalinna Subgroup.  Upper part of this unit reassigned to Enorama Shale, including Wundowie Limestone Member.||||||05-JUL-13
6307|Etina Formation|22631|6|Mentioned|p178|||Age: Marinoan||||||05-JUL-13
6307|Etina Formation|22915|6|Mentioned|15|||||||||
6307|Etina Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Of Umberatana Group. Correlate of Aralka Formation, Limbla Member and Angepena Formation equivalent.||||||18-SEP-06
6307|Etina Formation|23314|5|Briefly described|331 Fig.2|||||||||
6307|Etina Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
6307|Etina Formation|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological province: Central Flinders Zone.  Of the Umberatana Group.  Overlies Tapley Hill Formation; overlain by Enorama Shale.||||||18-SEP-06
6307|Etina Formation|24175|5|Briefly described|p13|||Of Umberatana Group.  Distinctive grey, sandy limestone and dolomite.  Max. thickness: 50m.||||||
6307|Etina Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Umberatana Group.||||||
6307|Etina Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Tapley Formation. Overlain by the Enorama Shale.  Geological Province: Adelaide Fold Belt.||||||18-SEP-06
6307|Etina Formation|29780|5|Briefly described|p40|||||||||
6307|Etina Formation|30198|6|Mentioned|p96|||See also Table 2 - aquifers and lithology||||||
6307|Etina Formation|30802|4|Described|Table 1|||Marinoan age.||||||18-SEP-06
6307|Etina Formation|32146|6|Mentioned|Fig.3|||||||||
6307|Etina Formation|32481|6|Mentioned|p21|||Stratigraphy on P23||||||
6307|Etina Formation|32505|6|Mentioned|Table 3|||||||||
6307|Etina Formation|32720|6|Mentioned|Table 1|||||||||
6307|Etina Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
6307|Etina Formation|32723|6|Mentioned|p113|||See also P116||||||
6307|Etina Formation|32724|4|Described|p518|||Marinoan||||||
6307|Etina Formation|32726|6|Mentioned|p190|||Stromatolites||||||
6307|Etina Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
6307|Etina Formation|34291|6|Mentioned|p11|||See also pp13,17,71 etc. Upper Marinoan.||||||18-SEP-06
6307|Etina Formation|34534|6|Mentioned|Fig.2.13|||||||||
6307|Etina Formation|35075|6|Mentioned|p77|||||||||
6307|Etina Formation|35255|6|Mentioned|Fig.7|||||||||
6307|Etina Formation|35582|6|Mentioned|Fig.2|||||||||
6307|Etina Formation|36245|6|Mentioned|p5|||||||||
6307|Etina Formation|37461|4|Described|p341|||See also Table 5.I||||||
6307|Etina Formation|38157|6|Mentioned|Table IV|||||||||
6307|Etina Formation|39210|6|Mentioned|Table 4|||||||||
6307|Etina Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6307|Etina Formation|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6307|Etina Formation|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
6307|Etina Formation|40225|6|Mentioned|Map sheet|||||||||
6307|Etina Formation|40294|3|Fully described|p51|||||||||
6307|Etina Formation|40852|5|Briefly described|p28|||||||||
6307|Etina Formation|40910|6|Mentioned|p12|||||||||
6307|Etina Formation|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6307|Etina Formation|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
6307|Etina Formation|41405|3|Fully described|p181|||||||||
6307|Etina Formation|41496|5|Briefly described|Fig.1|||||||||
6307|Etina Formation|42090|6|Mentioned|p18|||||||||
6307|Etina Formation|42098|5|Briefly described|Table 2 P54|||||||||
6307|Etina Formation|42109|5|Briefly described|p23|||||||||
6307|Etina Formation|42222|5|Briefly described|p17|||||||||
6307|Etina Formation|42238|5|Briefly described|Table 1 P74|||||||||
6307|Etina Formation|42239|6|Mentioned|Fig.2 P151|||||||||
6307|Etina Formation|42882|5|Briefly described|p10, Table1 p3|||Of Umberatana Group.||||||18-SEP-06
6307|Etina Formation|43052|5|Briefly described|p189,Table 6.1|||||||||
6307|Etina Formation|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
6307|Etina Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
6307|Etina Formation|46865|6|Mentioned|Table 2|||||||||
6307|Etina Formation|60889|6|Mentioned|p251|Neoproterozoic|Neoproterozoic|Residual oil saturation (in core 2, Moorowie-1).||||||
6307|Etina Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Cycles of thick, grey, oolitic and stromatolitic limestone with intervening grey-green siltstone.||||||
6307|Etina Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
6307|Etina Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
6307|Etina Formation|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||||
6307|Etina Formation|62592|5|Briefly described|p50 Table 5.1, p58.|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Overlies Sunderland Formation. Is overlain by Enorama Shale.|Sandy limestone, siltstone.|
6307|Etina Formation|64797|5|Briefly described|p153 Fig.2, p161, p162 Fig.9|||See also p164 Fig.11, p166 Tb.8, p168 Tb.11, p169 Fig.12. Eastern Adelaide Rift Complex. S-isotope data.||||Overlies Willochra Subgroup||
6307|Etina Formation|64801|5|Briefly described|p110 Fig.2, p111-113, p117|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Onlaps the Enorama Diapir (described in detail).||Umberatana Group.|||Carbonate platform deposits. Includes columnar stromatolites (Tungussia etina).|
6307|Etina Formation|65892|5|Briefly described|p33 Fig.18.|Late Neoproterozoic|Late Neoproterozoic|||Unit in Umberatana Group.||Overlies Sunderland Formation. Is overlain by Enorama Shale.||
6307|Etina Formation|65925|5|Briefly described|Appendix 2.||||||||Limestone, sandy, grey, oolitic, stromatolitic, trough cross bedding; interbedded with siltstone, grey-green. Local diapir derived conglomerate.|
6307|Etina Formation|66464|4|Described|p167, p171-174, p177|Cryogenian|Cryogenian|Adelaide Rift Complex. Pre-glacial. Shallow-marine sandstone, oolites and microbial reefs. There are grainstones and stromatolite facies south of the Blinman fold axis and siltstone, shale and olistostromes to the north.||||||
6307|Etina Formation|67180|6|Mentioned|p609|Cryogenian|Cryogenian|Preiss 1987 - intertongues with the upper portions of the Angepena Formation.||||Intertongues with Angepena Formation.||
6307|Etina Formation|67979|4|Described|p529, p530, p531, p538, p542-543, p545|Marinoan|Marinoan|In Central Flinders Ranges. Platformal carbonate deposits. Shallow marine carbonate facies shift between this unit and its slightly deeper marine correlative Amberoona Formation. Previously regarded as correlative with Yankaninna Formation of Northern Ranges (Preiss et al. 1998). See Figs.1 and 2.||Upalinna Subgroup||gradationally overlies Sunderland Formation and erosionally overlain by Wundowie Limestone Member (Enorama Shale) in central regions. Laterally correlates with Amberoona Formation in north.|shallow marine limestones and sandy-limestones|
6307|Etina Formation|68275|6|Mentioned|p59|||||||Is overlain by Enorama Formation.||
6307|Etina Formation|70031|4|Described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Upper interglacial, transgressive succession in the central Flinders Ranges. Thickness: 760m. Represented by a reef complex to the NE.||Unit of Upalinna Subgroup.||Overlain by Enorama Shale. Intertongues with Angepena Formation.|Sandy, oolitic and stromatolitic limestones.|
6307|Etina Formation|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges.||||||
6307|Etina Formation|70334|5|Briefly described|p77|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Carbonate platform sucession.||||Intertongues with Angepena Formation.||
6307|Etina Formation|70407|5|Briefly described|p103 Fig 2, p112|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Umberatana Group.||||
6307|Etina Formation|70416|6|Mentioned|p80|||Overlies Carnegie Formation. Is overlain by Maurice Formation.||||||
6307|Etina Formation|71237|14|Not recorded|p10, 12, 17|||||||||
6307|Etina Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shallow marine. Hosts the 'Great Wall of China' feature.||||Overlies Sunderland Formation and underlies Enorama Shale.|Cycles of thick, grey, oolitic and stromatolitic limestone with intervening grey-green shale. Limestone is often sandy, cross-bedded and contains pebble conglomerate lenses near Enorama Diapir.|
6307|Etina Formation|72473|6|Mentioned|p4|||||||||
6307|Etina Formation|73086|6|Mentioned|p78, p91|||Adelaide Rift Complex.||||May correlate to Ringwood and Limbla members (Aralka Formation).||
6307|Etina Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Limestone, sandy, grey, oolitic, stromatolitic, trough cross-bedding; interbedded with siltstone, grey-green. Local diapir derived conglomerate.|
6307|Etina Formation|73255|6|Mentioned|p534 Fig.2|Cryogenian|Cryogenian|Contains Tungussia etina fossils.||||Underlies the Enorama Formation.||
6324|Ettlewood Calc-Silicate Member|22500|4|Described|p 3, 10, 13|||Of the Broken Hill Group.||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|22553|5|Briefly described|fig2p77,p81|Proterozoic|Proterozoic|||||||
6324|Ettlewood Calc-Silicate Member|22575|6|Mentioned|p179 Fig.2|||Of the Broken Hill Group.||||||11-JUN-08
6324|Ettlewood Calc-Silicate Member|22720|6|Mentioned|p 168|||||||||
6324|Ettlewood Calc-Silicate Member|22771|6|Mentioned|Table12.2p45,45|||||||||
6324|Ettlewood Calc-Silicate Member|22884|6|Mentioned|p43 Fig. 3, p45|||Close affinity to the Meningie Well Formation.||||||26-MAR-09
6324|Ettlewood Calc-Silicate Member|22960|6|Mentioned|p90||Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|22965|6|Mentioned|Fig 1||Statherian|||||||
6324|Ettlewood Calc-Silicate Member|22967|6|Mentioned|p39||Statherian|||||||
6324|Ettlewood Calc-Silicate Member|38969|4|Described|p208|||||||||
6324|Ettlewood Calc-Silicate Member|39662|2|Defined|p424|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|39849|6|Mentioned|p86|||See also Table 2.||||||
6324|Ettlewood Calc-Silicate Member|40290|6|Mentioned|Fig.2|||||||||
6324|Ettlewood Calc-Silicate Member|40822|6|Mentioned|Fig.2|||||||||
6324|Ettlewood Calc-Silicate Member|41093|6|Mentioned|p252|||||||||
6324|Ettlewood Calc-Silicate Member|41630|6|Mentioned|Fig.1.3|||||||||
6324|Ettlewood Calc-Silicate Member|42181|4|Described|p251|||See also Fig.1.||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|42261|6|Mentioned|Fig 1 P530|||||||||
6324|Ettlewood Calc-Silicate Member|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42537|4|Described|p13|||||||||
6324|Ettlewood Calc-Silicate Member|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Ettlewood Calc-Silicate Member, NSW.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42813|6|Mentioned|p9|||||||||
6324|Ettlewood Calc-Silicate Member|43086|6|Mentioned|Fig.3|||same as Ettlewood Calcsilicate Member||||||
6324|Ettlewood Calc-Silicate Member|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Allendale Metasediments.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Allendale Metasediments.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|43572|6|Mentioned|Fig.3.2 p6|||||||||
6324|Ettlewood Calc-Silicate Member|46598|4|Described|p304|||||||||
6324|Ettlewood Calc-Silicate Member|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Allendale Metasediments (Broken Hill Group, Willyama Supergroup).||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|60485|5|Briefly described|p26|||Of the Allendale Metasediments.  See also Ettlewood Calc-silicate Member.||||||03-MAR-05
6324|Ettlewood Calc-Silicate Member|61606|5|Briefly described|p4 Fig.2|||Of the Allendale Metasediments.||||||18-MAY-06
6324|Ettlewood Calc-Silicate Member|61735|5|Briefly described|p635 Fig. 1, p639, p658|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group). Age: 1693+/-4Ma U/Pb SHRIMP deposition of tuffaceous sediment. Presented as Ettlewood CS only in Fig. 1.||||||04-JUN-15
6324|Ettlewood Calc-Silicate Member|61736|6|Mentioned|p665, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group). Age: 1693+/-4Ma. Geological province: Broken Hill Domain. Displays poly-metallic mineralization.||||||24-FEB-10
6324|Ettlewood Calc-Silicate Member|62535|5|Briefly described|p663, p665 Fig.2,|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, SE Curnamona Province. Regionally developed. Hosts polymetallic mineralization (Zn-Pb-Ag-Cu-Co-W). A metasiltstone immediately overlying this unit was dated at 1693 +/- 4 Ma, virtually identical with Bimba Formation. See also p666 Fig.3, p668, p671-674.||Allendale Metasediments.||Equivalent to the Bimba Formation.||
6324|Ettlewood Calc-Silicate Member|62536|5|Briefly described|p633, 636, 638-639, 641, 644-645, 658|||Broken Hill area. Contains significant concentrations of W and Zn as well as minor Pb and Zn.|1693 +/- 4 Ma.|Allendale Metasediments.||Is overlain by Parnell Formation.|Tuffaceous metasedimentary rocks: layered, diopside- and/or clinozoisite-rich, calc-silicate rocks. Locally, grey graphitic metasiltstone, which overlies and underlies the calc-silicate rock, is tuffaceous and zircon-datable.|
6324|Ettlewood Calc-Silicate Member|62993|6|Mentioned|p6, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Ettlewood Calcsilicate Member Equivalent discused p6.||Allendale Metasediments||Correlated with Bimba Formation||
6324|Ettlewood Calc-Silicate Member|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Within the Broken Hill Group. Pale, planar to irregularly layered epidote and clinopyroxene-rich calc-silicate in Broken Hill Domain; unnamed equivalents in Olary Domain.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments. Age: ~1695Ma. Occurs in lenses of layered cliozoisite-quartz rich rock, engulfed by pegmatitic granitoid. Mentioned in Abstract also.  See also p10 Fig. 3.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|63866|4|Described|p36, p38, p40|||Broken Hill Domain, Curnamona Province. Appears as the Ettlewood calc-silicate member on p38. An adjacent tuffaceous metasiltstone was dated at 1693 +/- 4 Ma (Page et al., 2005a).||Allendale Metasediments||Equivalent to the Plumbago Formation.|Metamorphosed carbonate.|
6324|Ettlewood Calc-Silicate Member|64097|5|Briefly described|p302 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (lower Broken Hill Group). Age: 1693+/-4Ma. Written as Ettlewood CS.||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|64741|4|Described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (Broken Hill Group). Geol.prov: Broken Hill Domain. Continues into the Olary Domain as the Bimba Formation. See p309 for detailed description for the "Bimba-Ettlewood" unit; correlations have also been made with Portia Fm.||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|64742|6|Mentioned|pp320-321, p323. ||||1693 Ma.|Unit in Broken Hill Group.||||
6324|Ettlewood Calc-Silicate Member|64944|5|Briefly described|p26, p28 Fig. 1, , p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (Broken Hill Group). Equivalent to the marker unit, Bimba Formation, in the Olary Domain. Geological province: western Broken Hill Domain||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|66302|4|Described|p36 Fig.9, p37, p38-p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Also misspelt as the Ettlewood calc-silicate member on p39.  |1693 +/- 4 Ma (Page et al, 2005)|Allendale Metasediments||Equivalent to the Bimba Formation.|Metamorphosed carbonate with tuffaceous metasiltstone.|
6324|Ettlewood Calc-Silicate Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain. The rank [Member] is omitted.||Allendale Metasediments.||||
6324|Ettlewood Calc-Silicate Member|70000|6|Mentioned|p36|||Mis-spelt as Ettelwood Calc-silicate Member.||Unit in Allendale Metasediments.||||
6324|Ettlewood Calc-Silicate Member|70014|5|Briefly described|Map legend|||||Unit in Allendale Metasediments.|||Small pods and thin, elongate, tabular, conformable bodies. Thinly-bedded, fine to coarse quartz-plagioclase-clinopyroxene-amphibole-epidote rocks, pale brown or grey-green in colour, interpreted as metamorphosed impure dolomitic limestone.|
6324|Ettlewood Calc-Silicate Member|70657|4|Described|p10 Fig.4, p13 Fig.6, p14-17, p33,p37-41|Statherian|Statherian|See also p43-44, p65. Curnamona Province; Broken Hill Domain. Appears as Bimba Formation + Ettlewood Calcsilicate Member in Fig.4. Is presented also as Ettlewood Calc-silicate Member in Fig.6 and on p17 and p38. Highly anomalous in Pb, Zn, Ag, Co and locally Au. Similar to Bimba Formation.|1693 +/- 3 Ma.|Allendale Metasediments||Equivalent to Bimba Formation (Larry Macs Subgroup).||
6324|Ettlewood Calc-Silicate Member|70658|5|Briefly described|p6, 15-16, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Allendale Metasediments.|||Sulphidic calc-silicate unit.|
6324|Ettlewood Calc-Silicate Member|73308|6|Mentioned|p607 Fig.1|||For reasons of space in the diagram, appears as Ettlewood CS.|1693 +/- 4 Ma.|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain. Correlated with Bimba Formation.|1693+/-4 Ma maximum depositional age|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73482|5|Briefly described|p422 Fig.3, p432, p436 Fig.16|Statherian|Statherian|Abbreviated as Ettlewood CS p422 Fig.3.|1693+/-4 Ma|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian||1693+/-4 Ma|Allendale Metasediments||||
6337|Ettrick Formation|2967|6|Mentioned|p24|||Ludbrook (1957). Renamed Ettrick Marl (see references p14, p15 Fig.2.2, p24) and assigned to the Murray Group by Lawrence (1966).||||||
6337|Ettrick Formation|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6337|Ettrick Formation|22587|6|Mentioned|p79 Fig.7|Late Oligocene|Early Oligocene|||||||
6337|Ettrick Formation|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province Murray Basin. Overlying unit Lower Mannum Formation||||||
6337|Ettrick Formation|22773|5|Briefly described|p351,Fig24.8p352|Oligocene|Oligocene|||||||
6337|Ettrick Formation|22799|2|Defined|p30|Early Miocene|Oligocene|Murray Group.||||||13-AUG-07
6337|Ettrick Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Early Miocene|Oligocene|Basal conglomerate of the Murray Group. Composed of sand and silt. Equivalent of Compton Conglomerate. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
6337|Ettrick Formation|22887|5|Briefly described|Fig.6 p13||Early Oligocene|||||||
6337|Ettrick Formation|22893|5|Briefly described|fig4 p9|||||||||
6337|Ettrick Formation|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6337|Ettrick Formation|23179|6|Mentioned|Fig.2|Early Miocene|Late Oligocene|Murray Supergroup||||||
6337|Ettrick Formation|23226|6|Mentioned|p889,890,891,894|||Of Murray Supergroup.||||||
6337|Ettrick Formation|23671|6|Mentioned|p3|||Disconformably overlies the Renmark Beds.||||||
6337|Ettrick Formation|23768|5|Briefly described|p28 Fig.5|Miocene|Oligocene|Geological Province: Murray Basin.||||||11-SEP-09
6337|Ettrick Formation|23818|5|Briefly described|p174 Fig.84, p180|Oligocene|Oligocene|Geological Province: Murray Basin. Overlying units: Buccleuch Group and Renmark Beds.[this seems unlikely CEBDec 2013] Contains foraminifer Massilina torquayensis.||||||03-DEC-13
6337|Ettrick Formation|23884|5|Briefly described|p153, p155 Fig.13.2|Early Oligocene|Early Oligocene|Geological Province: Murray Basin||||||
6337|Ettrick Formation|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
6337|Ettrick Formation|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Ettrick Formation not included.  Geological Province: Murray Basin.||||||
6337|Ettrick Formation|29591|6|Mentioned|Table 20|||||||||
6337|Ettrick Formation|29697|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|29828|6|Mentioned|p25|||||||||
6337|Ettrick Formation|29898|6|Mentioned|p216|||||||||
6337|Ettrick Formation|30751|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|30753|4|Described|Table 2|||Oligocene age||||||
6337|Ettrick Formation|30754|6|Mentioned|p14|||Stratigraphic table. See also P42 section||||||
6337|Ettrick Formation|30758|6|Mentioned|p66|||Oliogocene. Marine transgression||||||
6337|Ettrick Formation|30918|6|Mentioned|p85|||||||||
6337|Ettrick Formation|31241|6|Mentioned|p99|||Equivalent in age to Gambier Lst.||||||
6337|Ettrick Formation|31625|6|Mentioned|Fig. 5.2|||Oligocene||||||
6337|Ettrick Formation|31746|6|Mentioned|p194|||||||||
6337|Ettrick Formation|31848|5|Briefly described|p15|||Oligocene - Miocene||||||
6337|Ettrick Formation|31850|6|Mentioned|p36|||||||||
6337|Ettrick Formation|31851|4|Described|p12|||Lithostratigraphy.||||||
6337|Ettrick Formation|31922|6|Mentioned|p173|||||||||
6337|Ettrick Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
6337|Ettrick Formation|32432|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|32653|6|Mentioned|p285|||||||||
6337|Ettrick Formation|32859|4|Described|p69|||Oligocene||||||
6337|Ettrick Formation|32862|6|Mentioned|Fig. 3|||Section from boreholes||||||
6337|Ettrick Formation|32864|6|Mentioned|Fig. 5|||||||||
6337|Ettrick Formation|33224|6|Mentioned|Fig.35|||Photo.||||||
6337|Ettrick Formation|33490|4|Described|p10|||See also p27. Oligocene -Miocene.||||||28-JUL-08
6337|Ettrick Formation|33798|6|Mentioned|p98|||Fig.2||||||
6337|Ettrick Formation|33834|5|Briefly described|p11|||||||||
6337|Ettrick Formation|33982|6|Mentioned|p116|||||||||
6337|Ettrick Formation|34029|5|Briefly described|Table 1|||Oligo-Miocene||||||
6337|Ettrick Formation|34114|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6337|Ettrick Formation|34295|5|Briefly described|p36|||Oligocene||||||
6337|Ettrick Formation|34296|4|Described|p97|||Olig.- Miocene. Lithology||||||
6337|Ettrick Formation|34308|5|Briefly described|p180|||Correlation chart. Olig.- L.Miocene||||||
6337|Ettrick Formation|34418|4|Described|p506|||Equivalent||||||
6337|Ettrick Formation|34461|5|Briefly described|p52|||Oligocene||||||
6337|Ettrick Formation|34758|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|35071|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|35232|6|Mentioned|p11|||See also Table 3.||||||
6337|Ettrick Formation|35541|6|Mentioned|p13|||||||||
6337|Ettrick Formation|37132|5|Briefly described|p368|||||||||
6337|Ettrick Formation|38068|6|Mentioned|Fig.7|||||||||
6337|Ettrick Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
6337|Ettrick Formation|38601|6|Mentioned|p7|||||||||
6337|Ettrick Formation|39329|6|Mentioned|Fig.1|||||||||
6337|Ettrick Formation|39929|6|Mentioned|p268|||||||||
6337|Ettrick Formation|40003|5|Briefly described|p38|||||||||
6337|Ettrick Formation|40033|6|Mentioned|p228|||||||||
6337|Ettrick Formation|41478|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|41511|5|Briefly described|p18|||||||||
6337|Ettrick Formation|41517|6|Mentioned|p139|||||||||
6337|Ettrick Formation|41520|5|Briefly described|Fig.11|||||||||
6337|Ettrick Formation|42125|5|Briefly described|p135|||See also Fig.5||||||
6337|Ettrick Formation|42126|6|Mentioned|p156|||||||||
6337|Ettrick Formation|42127|5|Briefly described|p219|||See also Fig.3||||||
6337|Ettrick Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
6337|Ettrick Formation|42130|6|Mentioned|Fig.3 P265|||||||||
6337|Ettrick Formation|42132|6|Mentioned|Fig.5 P298|||||||||
6337|Ettrick Formation|42134|6|Mentioned|Fig.3 P335|||||||||
6337|Ettrick Formation|42137|4|Described|p370|||See also Table 1||||||
6337|Ettrick Formation|42138|6|Mentioned|p388|||||||||
6337|Ettrick Formation|42443|5|Briefly described|p6|||||||||
6337|Ettrick Formation|42623|6|Mentioned|p2|||aquitard||||||
6337|Ettrick Formation|42717|5|Briefly described|map legend|Miocene|Oligocene|||||||
6337|Ettrick Formation|42881|4|Described|Fig.3, P84|||||||||
6337|Ettrick Formation|42966|2|Defined|p116|Early Miocene|Oligocene|Of Murray Group.||||||13-AUG-07
6337|Ettrick Formation|43073|4|Described|Table 3|||||||||
6337|Ettrick Formation|43195|5|Briefly described|Map Legend||Oligocene|See also commentary on back of map.||||||
6337|Ettrick Formation|43383|14|Not recorded|p29||Oligocene|||||||
6337|Ettrick Formation|43466|14|Not recorded|p3,fig.2,Pl.1|||Equivalent to SA||||||
6337|Ettrick Formation|43467|14|Not recorded|p3,20,25,31,32|||||||||
6337|Ettrick Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
6337|Ettrick Formation|43686|6|Mentioned|Fig.5,p233|||||||||
6337|Ettrick Formation|43780|6|Mentioned|p5|||||||||
6337|Ettrick Formation|43791|6|Mentioned|p372, Fig1|||||||||
6337|Ettrick Formation|43804|6|Mentioned|Fig.2,p49|||||||||
6337|Ettrick Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Early Miocene|Early Oligocene|Geological Province: Murray Basin. ||||||
6337|Ettrick Formation|44191|5|Briefly described|Map Legend||Late Oligocene|||||||
6337|Ettrick Formation|46802|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|46839|6|Mentioned|p82|||||||||
6337|Ettrick Formation|49038|4|Described|Table 2|||Briefly described p26.||||||19-SEP-18
6337|Ettrick Formation|49040|6|Mentioned|p11|||||||||
6337|Ettrick Formation|60785|5|Briefly described|p184 Fig.1, p195. |Chattian|Chattian|South Australia. Has yielded several fossil cetacean heterodont teeth.|||||Glauconitic marl, calcareous clay, and mudstone, with silt and sand.|
6337|Ettrick Formation|61155|5|Briefly described|p18||Early Oligocene|Of the Murray group. Glauconitic marls; diachronous. Overlain by Gambier Limestone; interfingers with Duddo Limestone and Geera Clay in central Murray Basin. Age: 32-14.9Ma. Max. thickness: 50m. Geological Province: Murray Basin. See also p3. p4.||||||03-MAR-10
6337|Ettrick Formation|61314|5|Briefly described|p129|Oligocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6337|Ettrick Formation|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit,  the Geera Clay and Winnambool Formation into their new Murray Supergroup. These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
6337|Ettrick Formation|63460|5|Briefly described|p837, p839 Fig. 2b|Erly Miocene|Late Oligocene|Overlain by Mannum Fm. Passes laterally into Winnambool Formation and Geera Clay to the north and east. Max. thickness" 40m. Geological province: Murray Basin. Dark grey-greenish, glauconitic calcareous clay and marl. ||||||
6337|Ettrick Formation|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Marl.||||||
6337|Ettrick Formation|64237|4|Described|p17,p18,p18|Oligocene|Oligocene|Formerly part of the now obsolete Glenelg Group together with Compton Conglomerate; now incorporates Compton Conglomerate (obsolete) and is the basal unit of Murray Group ( in South Australia).||||||18-SEP-09
6337|Ettrick Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Late Oligocene|Deposited during the final stages of an Oligocene-Miocene marine incursion. Contemporaneous with Geera Clay, Murray Group and Winnambool, Olney Formations. Locally underlies Murray Group. Overlies Buccleuch beds.||||||
6337|Ettrick Formation|67462|5|Briefly described|Map legend.|||Murray Basin.||||||
6337|Ettrick Formation|68140|6|Mentioned|p1701|Neogene|Paleogene|Middle Tertiary age.||||||
6337|Ettrick Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Rupelian|Murray Basin.||Murray Group.||||07-APR-17
6337|Ettrick Formation|70718|5|Briefly described|p24|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies.||||||
6337|Ettrick Formation|70961|14|Not recorded|p136|||Geological section.||||||
6337|Ettrick Formation|71248|14|Not recorded|p2||Oligocene|||||||
6337|Ettrick Formation|71593|4|Described|p52-p54|Miocene|Oligocene|Murray Basin. Palynology in Stavely 14 linked ot Ettrick Fm.||Murray Group||Interfingered with the Geera Clay, Olney Formation and the Calivil Formation.|Muddy shallow marine marl.|19-SEP-18
6337|Ettrick Formation|72445|5|Briefly described|App.7 p2, p5, p7 Fig.4, p19-20; App.2.|Middle Miocene|Early Oligocene|See also App.1, App.6 p1 Tb.1, p2 Fig.1, p4. Mentioned in text as marls in the far west of the Murray Basin (see Truswell 1987, Macphail & Truswell 1989). Identified in Stavely 08,11,14,16. App.6 sample in Stavely 11 include a high diversity of marine bioclast types including abundant bryozoans. A Middle Miocene M5 zone (16.39-15.73 Ma) determined from foraminifera(p.4, but table 1 gives M6 zone 15.10-14.78 Ma). Early Oligocene spore/pollen zone identified in samples from Stavely 14 (App.7).|16.39 - 14.78 Ma min age.|Murray Group||Shown as underlying Gambier Limestone. Overlies Renmark Group (unconformity), Olney Formation (gradational or sharp contact), Compton Conglomerate. Laterally equivalent with Geera Clay.|Including glauconitic marl, sand and limestone. Includes lesser silt and mud.|
6337|Ettrick Formation|73107|5|Briefly described|Map legend.|||Murray Basin. Equivalent to an un-named Oligocene unit of silicified dolomitic calcilutite, boulders of which are washed up at Cape Hart, Point Reynolds, Cape Linois and Cape Gantheaume.||||||
6337|Ettrick Formation|73118|5|Briefly described|p17, 24, 30, 34, 45, 82|||Murray Basin. Drill core summary logs. <30m thick. Almost entirely concealed. Deposited in shallow-marine, restricted platform to lagoonal environments.||Murray Group.||Overlies Olney Formation. Is overlain by Duddo Limestone and Geera Clay.|Weakly lithified grey, green glauconitic, highly fossiliferous calcareous clay (marl), silt, sandy skeletal clay, thin micritic limestone intercalations. Contains abundant and diverse faunas.|
6337|Ettrick Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.||||||
6337|Ettrick Formation|73228|4|Described|p50, p52-57, p60|Middle Miocene|Late Paleocene|Murray Basin. From the lower Murray Group. Estuarine and marginal marine depositional environments. Represents a transgressive phase of shallow-marine shelf environment. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes.||Murray Group, lower||Underlain by Renmark Group including Olney Formation. Overlain by Gambier Limestone.|Grey to green glauconitic and fossiliferous marl, calcareous clay and mudstone, and silt and fine quartz sand, as well as skeletal debris.|
6337|Ettrick Formation|73229|5|Briefly described|p66-67, p70-72, p74|Early Miocene|Late Oligocene|Murray Basin. [Analysed using pXRF; see article]. From the lower Murray Group.||Murray Group, lower|||Includes clayey limestone with interbedded clay and calcareous, glauconitic shelly fragments; glauconitic, fossiliferous marl; calcareous clay and mudstone; silt; fine-grained sand.|
6345|Eucla Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Middle Eocene|||||||
6345|Eucla Group|22613|6|Mentioned|p18|||||||||
6345|Eucla Group|24563|6|Mentioned|p485|Tertiary|Tertiary|||||||
6345|Eucla Group|32552|4|Described|p56-108|||Mid.-L.Miocene||||||21-JAN-16
6345|Eucla Group|32648|6|Mentioned|p32|||Tertiary||||||
6345|Eucla Group|32750|6|Mentioned|p307|||Distribution map||||||
6345|Eucla Group|33595|4|Described|Table 1|||||||||
6345|Eucla Group|34232|6|Mentioned|p75|||Miocene. Origin of cavities.||||||
6345|Eucla Group|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
6345|Eucla Group|36200|6|Mentioned|p6|||||||||
6345|Eucla Group|36890|3|Fully described|p412|||||||||
6345|Eucla Group|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
6345|Eucla Group|38553|6|Mentioned|p44|||||||||
6345|Eucla Group|42075|5|Briefly described|Fig.10 P250|||||||||
6345|Eucla Group|42335|5|Briefly described|p325|||||||||
6345|Eucla Group|42959|5|Briefly described|p58 Fig.3|||||||||
6345|Eucla Group|43026|5|Briefly described|Table 1,p586|||||||||
6345|Eucla Group|43040|5|Briefly described|Fig.2,p861|||||||||
6345|Eucla Group|43065|6|Mentioned|p92|||||||||
6345|Eucla Group|43814|6|Mentioned|Fig.3,p115|||||||||
6345|Eucla Group|44133|5|Briefly described|p178|Tertiary|Tertiary|Geological Province: Eucla Basin. ||||||
6345|Eucla Group|49060|5|Briefly described|Fig.15|||||||||
6345|Eucla Group|61155|5|Briefly described|p3|||Marine clastics and carbonates deposited offshore in the Great Australian Bight.||||||03-MAR-10
6345|Eucla Group|62369|5|Briefly described|p409, p410 Fig.4|Middle Miocene|Pliocene|Carbonates veneered by Roe Calcarenite. Geological Province: Eucla Basin. See also p416.||||||01-FEB-16
6345|Eucla Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
6345|Eucla Group|65942|4|Described|p74, Fig.6 p75|Early Miocene|Middle Eocene|Includes Hampton Sandstone, Wilson Bluff Limestone, Toolinna Limestone, Abrakurrie Limestone, Nullarbor Limestone, Colville Sandstone||||||28-MAY-10
6345|Eucla Group|66131|6|Mentioned|p242 Fig.2|Holocene|Eocene|||||||
6345|Eucla Group|67789|6|Mentioned|p34-35|||Eucla Basin. A suite of sedimentary rocks extending southwards below the modern continental shelf.|||Wilson Bluff, Abrakurrie, Nullarbor Limestones.|||
6345|Eucla Group|69632|5|Briefly described|p26|Cenozoic|Cenozoic|Lowry (1970).|||Includes the Abrakurrie Limestone and the Nullarbor Limestone.|Overlies Bight Basin Group.||09-OCT-18
6345|Eucla Group|69648|5|Briefly described|p4, p21, map legend|Miocene|Eocene|Eucla Basin. Marine, temperate-water, platform, carbonates dominate the basin.|||Wilson Bluff Limestone, Nullarbor Limestone||Marine platform bioclastic carbonates.|
6345|Eucla Group|70397|6|Mentioned|p1,3|||Eucla Basin.|||Includes Nullarbor Limestone, Colville Sandstone, Garford Formation, Ooldea sands, Abrakurrie Limestone, Wilson Bluff Limestone and Hampton Sandstone.|Overlain by the Nullarbor Limestone.||29-JUL-19
6345|Eucla Group|70771|5|Briefly described|p2-p3, p27|||Eucla Basin. [The author herein assigns a number of units to this group, however this is obsolete terminology].|||Includes the Wilson Bluff Limestone, Abrakurrie Limestone, Nullarbor Limestone and the Roe Calcarenite.||Calcareous sandstones and limestones.|
6345|Eucla Group|70772|6|Mentioned|p1-p2, p6-7, p22, p36, p41|Eocene|Eocene|Bight Basin.||||Unconformably overlies the Madura Formation.||
6345|Eucla Group|70802|5|Briefly described|500k_interpgeop14_lut.csv|Miocene|Miocene|Of Eucla Basin. Events: Timorese Collision (20-0.01 Ma).|23.03-5.333 Ma (inferred)||||Bioclastic limestone with basal sandstone|
6345|Eucla Group|70826|6|Mentioned|p7 tbl 4|Miocene|Oligocene|Eucla Basin.||||||
6345|Eucla Group|71270|4|Described|2_5m_interpgeop15_lut.csv|Miocene|Miocene|Of Eucla Basin. Events: Timorese Collision (20 - 0.01 Ma); Mid-Miocene transgression, 15 Ma (15 - 15 Ma).|23.03-5.333 Ma (biostrat)||||Bioclastic limestone with basal sandstone|
6345|Eucla Group|71361|5|Briefly described|ii, p15-p16, p21, p160|Cenozoic|Cenozoic|Eucla Basin. [NB This group is currently out of use and the author references older literature - Lowry 1970].|||Includes the Nullarbor Limestone, Wilson Bluff Limestone and the Abrakurrie Limestone.|||
6345|Eucla Group|71618|6|Mentioned|p124-125,127, 133|Cenozoic|Cenozoic|Geological province: Eucla Basin.|||Includes Wilsons Bluff, Abrakurrie and Nullarbor limestones.|||05-SEP-19
6345|Eucla Group|71789|6|Mentioned|p99, 100|||||||||
6345|Eucla Group|72034|5|Briefly described|500k_interpgeop16_lut|Miocene|Oligocene|Eucla Basin. Age from biostratigraphy.|||||Bioclastic limestone with sandstone near basin margin.|
6363|Eumeralla Formation|12781|5|Briefly described|p385-387, 391-392|Early Cretaceous|Early Cretaceous|Penola Trough, W Otway Basin. Excellent reservoir sands and shale seals.||Otway Supergroup.|Windermere Sandstone Member.|Overlies Katnook Sandstone (Crayfish Group). Is overlain unconformably by Waarre and Copa Formations (Sherbrook Group).||
6363|Eumeralla Formation|12796|5|Briefly described|p456 Fig. 2|Albian|Albian|Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|22476|6|Mentioned|p952|||||||||
6363|Eumeralla Formation|22674|4|Described|p718, Fig.2 p719|Albian|Aptian|See also Fig.8 p725. Of Otway Supergroup.||||||
6363|Eumeralla Formation|22686|5|Briefly described|Fig3p745,746-47|Aptian|Albian| Geological Province: Otway Basin.||||||17-JAN-06
6363|Eumeralla Formation|22875|3|Fully described|p34|Aptian|Valanginian|Of the Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|22914|6|Mentioned|17|||||||||
6363|Eumeralla Formation|22930|6|Mentioned|50|||||||||
6363|Eumeralla Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Early Cretaceous|||||||
6363|Eumeralla Formation|23427|5|Briefly described|Table 11.2 p418.|||||||||
6363|Eumeralla Formation|23911|4|Described|p93, p95 Fig. 9B|Albian|Aptian|Geological Province: Otway Basin.  Max. Thickness: >2500m.  Underlain by Crayfish Subgroup. Of the Otway Group.||||||30-JAN-08
6363|Eumeralla Formation|24056|4|Described|p85|Early Cretaceous|Early Cretaceous|Of Otway Group.  Geological Basin: Otway Basin.||||||
6363|Eumeralla Formation|24113|5|Briefly described|p278|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.  Of the Otway Supergroup.  Overlain by Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|24209|5|Briefly described|p154|||Interbedded siltstones, sandstones and coals.  Geological Province: Penola Trough (Otway Basin).||||||
6363|Eumeralla Formation|24284|6|Mentioned|p15 Fig.2|||In the Otway Basin.||||||24-APR-07
6363|Eumeralla Formation|24314|5|Briefly described|p61 Fig.2|Cenomanian|Hauterivian|Geological Province: Otway Basin. Of the Otway Supergroup.||||||30-NOV-04
6363|Eumeralla Formation|24323|5|Briefly described|p135|Albian|Aptian|Unconformably overlies the Crayfish Group and the Casterton Formation. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|24405|5|Briefly described|p6|||Geological Province: Otway Basin. Equivalent to Strzelecki Formation (Gippsland Basin).||||||
6363|Eumeralla Formation|24453|4|Described|p808, p809 Fig.2|Albian|Aptian|High energy braided river environment. Contains diverse vertebrate and invertebrate fossils. Overlies Windemere Sandstone Member and Crayfish Subgroup. Of Otway Group. Geological Province: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|24455|6|Mentioned|p327|||Overlain unconformably in some areas by Dilwyn Formation.||||||
6363|Eumeralla Formation|24507|6|Mentioned|p26|Albian|Aptian|Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|24551|5|Briefly described|p241, 243, 245, 250, 635|Albian|Aptian|Interfingers with the Pretty Hill Sandstone and the Geltwood Beech Formation. Overlain by Waarre Formation.||||||24-APR-07
6363|Eumeralla Formation|24561|5|Briefly described|p27, p41|||Geological Province: Otway Basin. Includes volcanigenic sediments.||||||26-JUN-13
6363|Eumeralla Formation|24562|5|Briefly described|p8 Fig. 2|Aptian|Aptian|Geological Province: Otway Basin.  Of the Otway Supergroup.  Maximum Thickness: 900m.||||||
6363|Eumeralla Formation|29856|6|Mentioned|p37|||||||||
6363|Eumeralla Formation|30576|5|Briefly described|Table 2|||||||||
6363|Eumeralla Formation|30578|6|Mentioned|p5|||See also Tables 1 and 2.||||||
6363|Eumeralla Formation|30905|6|Mentioned|p148|||||||||
6363|Eumeralla Formation|32898|6|Mentioned|Table 2-1|||||||||
6363|Eumeralla Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
6363|Eumeralla Formation|33940|6|Mentioned|p400|||L.Cret.||||||
6363|Eumeralla Formation|35290|6|Mentioned|p23|||||||||
6363|Eumeralla Formation|36499|6|Mentioned|p17|||Refers Reynolds et al 1966.||||||
6363|Eumeralla Formation|36913|6|Mentioned|Fig.2|||||||||
6363|Eumeralla Formation|38625|6|Mentioned|Table 2|||||||||
6363|Eumeralla Formation|39315|6|Mentioned|Fig.7|||||||||
6363|Eumeralla Formation|40560|5|Briefly described|Fig.3|||Mention p4.||||||24-APR-07
6363|Eumeralla Formation|41016|5|Briefly described|p214|||||||||
6363|Eumeralla Formation|41185|5|Briefly described|p177|||See Also Fig.4||||||
6363|Eumeralla Formation|41269|5|Briefly described|p245|||||||||
6363|Eumeralla Formation|41642|6|Mentioned|p218|||||||||
6363|Eumeralla Formation|41704|5|Briefly described|p99|||||||||
6363|Eumeralla Formation|41714|4|Described|p300|||See also p303.||||||24-APR-07
6363|Eumeralla Formation|41726|5|Briefly described|p420|||See also p422, p425.||||||24-APR-07
6363|Eumeralla Formation|41868|4|Described|p532,p533|||||||||
6363|Eumeralla Formation|41936|6|Mentioned|p77|||||||||
6363|Eumeralla Formation|42075|5|Briefly described|Fig.13 P252|||||||||
6363|Eumeralla Formation|42152|4|Described|p10|||See also p38.||||||24-APR-07
6363|Eumeralla Formation|42153|5|Briefly described|p352|||||||||
6363|Eumeralla Formation|42318|5|Briefly described|p6|||||||||
6363|Eumeralla Formation|42361|3|Fully described|p8|Albian|Aptian|||||||
6363|Eumeralla Formation|42415|6|Mentioned|p177|||||||||
6363|Eumeralla Formation|42524|4|Described|p27|||||||||
6363|Eumeralla Formation|42545|5|Briefly described|p18|||In the Otway Basin.||||||24-APR-07
6363|Eumeralla Formation|42555|5|Briefly described|Fig.2 P285|||||||||
6363|Eumeralla Formation|42599|5|Briefly described|Fig.3 P614|||||||||
6363|Eumeralla Formation|42601|6|Mentioned|Fig.2 p15|||||||||
6363|Eumeralla Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
6363|Eumeralla Formation|43171|4|Described|2-8|Albian|Aptian|Of the Otway Supergroup. Age: 100-120Ma.||||||24-APR-07
6363|Eumeralla Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|43208|5|Briefly described|map legend|Albian|Aptian|Of Otway Group.||||||
6363|Eumeralla Formation|43219|5|Briefly described|Fig.3,p6.|Albian|Aptian|Of the Otway Group.||||||24-APR-07
6363|Eumeralla Formation|43590|3|Fully described|p9|Albian|Aptian|||||||
6363|Eumeralla Formation|43744|6|Mentioned|Fig.3,p3|||||||||
6363|Eumeralla Formation|43783|6|Mentioned|Fig14, p11|||?Albian age||||||
6363|Eumeralla Formation|43784|6|Mentioned|Fig10, p12|||?Albian age||||||
6363|Eumeralla Formation|43814|6|Mentioned|Fig.3,p115|||||||||
6363|Eumeralla Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
6363|Eumeralla Formation|44133|4|Described|p145-146|Albian|Barremian|Of the Otway Supergroup. Geological Province: Otway Basin. Conformably overlies Windermere Sandstone Member. Thickness: 2350m. ||||||
6363|Eumeralla Formation|48911|3|Fully described|p13|Cretaceous|Cretaceous|||||||24-APR-07
6363|Eumeralla Formation|48977|6|Mentioned|Fig.5|||||||||
6363|Eumeralla Formation|49060|5|Briefly described|Fig.33|||||||||
6363|Eumeralla Formation|50043|5|Briefly described|p2, p10, 12|Early Albian|Late Aptian|A ?protoceratopsian ulna was recovered from this unit at Dinosaur Cove East.||Of Otway Group.||||27-MAR-12
6363|Eumeralla Formation|50154|2|Defined|p25, p131-132|Early Cretaceous|Early Cretaceous|Of the Otway Group. Unconformably overlain by Parilla Sand. Geological Province: Otway Basin. Interbedded mudstone and feldspathic sandstone and conglomerate.||||||15-SEP-04
6363|Eumeralla Formation|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Fluvial; sandstone, siltstone, minor conglomerate, coal.||||||
6363|Eumeralla Formation|50156|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Overlies Nangeela Formation. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50157|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Overlain by Renmark Group and Ettrick Marl. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal.||||||26-JUN-13
6363|Eumeralla Formation|50158|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50160|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains and coal.||||||26-JUN-13
6363|Eumeralla Formation|50161|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50162|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50163|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|60563|5|Briefly described|p45, p47|Early Cretaceous|Early Cretaceous|Includes Barwon River Member.||||||16-JUN-05
6363|Eumeralla Formation|61017|5|Briefly described|p5|Albian|Aptian|Of the Otway Group. Lacustrine to flood plain sediments. Unconformably overlies the Crayfish Subgroup. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
6363|Eumeralla Formation|61182|3|Fully described|p13-14, p83|||Of Otway Group. Together with Pretty Hill Formation, unconformable over Casterton Fm. Thick monotonous sequence of volcanilithic sandstone, siltstone, mudstone, intraformational mudclast conglomerate and minor coal; plant fossils. Geol.Prov: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|61470|5|Briefly described|p28 Fig. 5|Albian|Aptian|Of the Otway Group. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|61528|5|Briefly described|p820|Albian|Hauterivian|Overlies Casterton Formation. Geological Province: Otway Basin. See also p821 Fig.2||||||
6363|Eumeralla Formation|61547|5|Briefly described|pp461-462, pp472-473. |Albian|Barremian|Deposited in a fluvio-lacustrine environment.|||Includes Windermere Sandstone Member.|Is unconformably overlain by the Sherbrook Group.|Consists of interbedded volcanigenic lithic sandstones, siltstones, coals and claystones.|26-JUN-13
6363|Eumeralla Formation|61553|6|Mentioned|p606.|||Chronostratigraphic equivalent of, with strong lithological similarity to, the Otway Megasequence (Bass Basin).||||||
6363|Eumeralla Formation|61622|5|Briefly described|p436, p438, p436 Fig. 2, p438 Fig. 4|Early Cretaceous|Early Cretaceous|Thickness 2500m. Geological Province: Otway Basin. Carbonaceous mudstones with minor sandstones and coal interbeds.||||||26-JUN-13
6363|Eumeralla Formation|61623|5|Briefly described|p447, p449, p450, p451, p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Otway Group. Includes Heathfield Member. Geological Province: Otway Basin.||||||07-APR-09
6363|Eumeralla Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p489|Albian|Aptian|Of Otway Group. Geological Province: Otway Basin. Non-marine.||||||07-APR-09
6363|Eumeralla Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
6363|Eumeralla Formation|63122|5|Briefly described|p17 Fig. 4.3, p20, p40|Albian|Barremian|Of the Otway Supergroup.Unconformably overlain by Copa Formation and Waarre Sandstone; overlies Crayfish Group.  Max. thickness: 2350m. Geological Province: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p70-73|Albian|Barremian|Of Reynolds et al (1966). Includes basal Windermere Sandstone Member. Unconformably overlies Crayfish Gp; underlies Sherbrook Gp. Age:125-97Ma. Max. thickness: >2500m. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|63125|5|Briefly described|p108|Cretaceous|Cretaceous|Of the Otway Supergroup. Geological Province: Otway Basin. Contains a thick potential oil source sequence in the lower section characterised by thin bituminous coal seams up to 1m thick. ||||||
6363|Eumeralla Formation|63129|5|Briefly described|p127|||Geological Province: Otway Basin. Shales of this unit act as a top seal for the Windermere Sandstone Member.||||||30-JAN-08
6363|Eumeralla Formation|63130|6|Mentioned|p141, p143|||Overlain by Waarre Sandstone. Geological Province: Otway Basin. Primary hydrocarbon source for the Waarre Sandstone.||||||06-FEB-08
6363|Eumeralla Formation|63150|5|Briefly described|p95, p96|||Plant microfossils are abundant in claystone and coal, and only absent in any sandstone sections. Geological province: Otway Basin.||||||
6363|Eumeralla Formation|63267|5|Briefly described|p485 Fig.2, p486 Fig.3, p491, p496|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Very thick sequence. Significance of faults discussed.||Otway Supergroup.|Windermere Sandstone Member.|Unconformably overlies Katnook Sandstone.||
6363|Eumeralla Formation|63269|5|Briefly described|p603, p605-606, p616, p618, p623-624|Albian|Aptian|Otway Basin. Thick, post-rift, fluvio-deltaic succession. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Otway Group.||Unconformably overlies Katnook Sandstone. Is overlain unconformably by Waarre Formation (Sherbrook Group).||
6363|Eumeralla Formation|63431|5|Briefly described|p677 Fig. 2|Albian|Hauterivian|Part of the Otway Supergroup. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
6363|Eumeralla Formation|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Fluvial, braided stream deposits.||Otway Group.|||Volcanolithic sandstone, siltstone, mudstone, with feldspar and quartz grains, fine- to medium-grained.|
6363|Eumeralla Formation|63446|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Unit in Otway Group.|||Fluvial: lithic sandstone, siltstone, minor conglomerate, coal.|
6363|Eumeralla Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Otway Basin. Coal measures are present in this unit.||||||24-JUL-08
6363|Eumeralla Formation|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64570|5|Briefly described|p858|||Of Otway Group. Age: 102.6+/-1.1Ma (K-Ar). Geological Province: Gippsland Basin.||||||22-DEC-08
6363|Eumeralla Formation|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; alluvial deposits. bright red in RGB due to K-feldspar content. Nonmagnetic.||||||
6363|Eumeralla Formation|64616|3|Fully described|p142-143, p298|Early Cretaceous|Early Cretaceous|North of Tyers; at least 200m thick. Unit in Otway Group. Here includes rocks formerly assigned to Exalt Member (Rintoul Creek Formation). Has distinct and characteristic pink colour in RGB radiometric image. Gradationally overlies Locmany Formation. Mainly thick-bedded, medium- to coarse-grained, quartzose to (K-feldspar rich) lithic sandstone; mudstone, mud-clast conglomerate. The relatively rare fossils include coalified logs and charcoal. Geophysical characteristics given.||||||
6363|Eumeralla Formation|65715|4|Described|p9 Tb.6, p10, p15|Cretaceous|Cretaceous|Of Otway Group. Extended by VandenBerg et al (2006) to include Early Cretaceous arkoses of the Gippsland outcrops of Otway Group. Fluvial. Overlies and interfingers with Barwon River Conglomerate. Unconformaby overlain by Murraduc Basalt. Early Cretaceous.||||||
6363|Eumeralla Formation|65973|6|Mentioned|p14, p20|Aptian|Albian|Otway Basin. Strong affinities with the Strzelecki Group of the Gippsland Basin. Proven gas generator.||Otway Group||||
6363|Eumeralla Formation|66002|5|Briefly described|p9 Tb.6, p11, p16|Mesozoic|Mesozoic|Of Otway Group. Overlain by Wangerrip Group.  Defined by Reynolds et al. 1966. See also VandenBerg 2009.||||||16-FEB-17
6363|Eumeralla Formation|66181|5|Briefly described|p310 Fig.5|Albian|Hauterivian|Overlies the Tyers River Subgroup, in the Otway Group.||||||
6363|Eumeralla Formation|66244|5|Briefly described|p5.|||Formerly Wonthaggi Formation; re-named the Eumeralla Formation by VandenBerg et al. (2006) and VandenBerg (2008); it has identical mineralogical and radiometric RGB image characteristics across southern Victoria. Because of its entrenched use in the petroleum industry, the Wonthaggi Formation name is retained for Eumeralla Formation-equivalent rocks in the Gippsland Basin.||||||
6363|Eumeralla Formation|66245|5|Briefly described|p6 Fig.5, p30, p45. |Albian|Aptian|Fining westwards, indicating rift-opening from that direction. Source of Austral 2 petroleum system, after deposition of the thick clastic Sherbrook Group provided the necessary overburden to mature source intervals near the base of the Eumeralla Formation. A thin, often well-bedded sheet facies.||Uppermost unit in Otway Group.|||Dominantly fluvial sand, much of it derived from volcaniclastic sources to the east and northeast.|
6363|Eumeralla Formation|67061|5|Briefly described|p545, p546 Fig.3, pp549-551, p559.|Albian|Barremian|Deposition in fluvial channels. Maximum proven thickness c.3 km. A major stratigraphic break at the top of this Formation records regional uplift and exhumation beginning between 100 and 95 Ma; up to 2-3 km of this unit were eroded from the Otway Ranges.||Unit in Otway Group.|||A thick sequence of volcanigenic sandstones, with finer-grained sandstones, mudstones and shales.|16-MAR-12
6363|Eumeralla Formation|67366|5|Briefly described|p103 Fig.2, p104. |Albian|Aptian|Over 3000 m of fluvial-lacustrine sediments deposited during a quiescent period between two rifting events. Blankets the entire Otway Basin; is the primary source of hydrocarbons in the Port Campbell Embayment (onshore) and Shipwreck Trough (offshore).||Upper unit in Otway Supergroup.|||Volcaniclastic sandstone, shale and coal.|
6363|Eumeralla Formation|67367|5|Briefly described|p131 Fig.2, pp132-133, p155.|Albian|Aptian|Fluvial and coaly facies. Primary hydrocarbon source interval for the gas in Port Campbell Embayment and Shipwreck Trough. Assigned to the Austral 2 petroleum sub-system. The gas is considered to have been derived mainly from two coaly horizons, although organic-rich mudstones and shales have also contributed. Hydrocarbons have probably migrated up critically stressed, mostly NW trending, fault planes until they reached the Waarre Formation reservoir.||Unit in Otway Group.||||
6363|Eumeralla Formation|67541|6|Mentioned|p76 Fig.1|||||||||
6363|Eumeralla Formation|68116|5|Briefly described|Appendix, Maps 29, 38, 49-50, 54-55.|Early Cretaceous|Early Cretaceous||||||Sandstone, mudstone, mud-clast conglomerate, minor coal: blue-green to grey; arkose to feldsarenite; fine to medium grained, mostly medium to thick-bedded, cross-bedded.|
6363|Eumeralla Formation|68189|6|Mentioned|p3, p19 Fig.8, p25|Albian|Aptian|||Of the Otway Group.||||27-JUN-14
6363|Eumeralla Formation|69297|5|Briefly described|p79, p98, p99, p101, p103|Albian|Aptian|Otway Basin. Potential source rock in the Torquay Sub-basin of the Otway Basin. See also p104, p112, p143, p147, p150.||Otway Group|Includes the Windermere Sandstone Member and the Heathfield Sandstone Member.|Unconformably overlies the Katnook Sandstone. Overlain by the Waarre Formation and unconformably overlain by the Copa Formation. Equivalent to the Otway Megasequence.|Siltstone.|
6363|Eumeralla Formation|69651|5|Briefly described|p10, p12-13, p25, p49|Early Cretaceous|Early Cretaceous|Fluvial to lacustrine deposits. A key source rock in the Otway Basin.||Otway Group.||Unconformably overlies Katnook Sandstone (Crayfish Subgroup). Is overlain unconformably by Waarre Formation (Sherbrook Group).|Lithic sandstone with thin interbeds of carbonaceous shale; includes coaly facies towards the top.|
6363|Eumeralla Formation|69879|5|Briefly described|p424, p430-431|Albian|Albian|Otway Basin. Time-equivalent and lithologically similar to the Otway Megasequence. Believed to be source rock for hydrocarbon reservoirs of Thylacine gas-condensate field.|||||Carbonaceous siltstone and coal.|
6363|Eumeralla Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).|||Windermere Sandstone Member.|Overlies Katnook Sandstone.||
6363|Eumeralla Formation|70076|5|Briefly described|Regional: p5|Albian|Aptian|Otway Basin. A proven gas-generating unit.||||Time-equivalent to Strzelecki Group (Gippsland Basin).||
6363|Eumeralla Formation|70077|5|Briefly described|Nelson:Fig.2. Regional: Fig.4, p6, p8-11|Albian|Albian|Otway Basin. The primary source for Austral 2 Petroleum System gas in the Port Campbell and Shipwreck Trough area. Has intraformational seals and provides seal to the Victorian part of the Penola Trough gas reservoirs.||Otway Group.|Heathfield and Windermere, Sandstone Members.|Overlies Katnook Sandstone or Pretty Hill Formation. Is overlain by Copa or Waarre Formations.|Includes coaly units.|
6363|Eumeralla Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Albian|Albian|Gambier Embayment and Voluta Trough.||Otway Group.||Is overlain by Copa Formation.||
6363|Eumeralla Formation|70193|6|Mentioned|p284 Fig 1, 2, p285 fig 3|Albian||Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
6363|Eumeralla Formation|70379|5|Briefly described|p723-727, p732|Early Cretaceous|Early Cretaceous|Otway Basin. There is an apparent overall thickening of this unit towards the centre of the Penola Trough, indicating activity on major faults at the time. Up to 1200m of sediments was eroded following late Albian-Cenomanian uplift. Barremian to Albian.||||Unconformably overlies Laira Formation. Is overlain by Sherbrook Group or (locally) Wangerrip Group.|Comparatively high-energy fluvial sediments.|
6363|Eumeralla Formation|70836|6|Mentioned|p473-474, 482|Albian|Aptian|Contains a nearly complete ulna from an indeterminate megaraptoran similar to Australovenator from the Winton Formation in QLD.||||||
6363|Eumeralla Formation|70880|6|Mentioned|p77|Albian|Aptian|Otway Basin.||||||
6363|Eumeralla Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
6363|Eumeralla Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
6363|Eumeralla Formation|71419|5|Briefly described|p8 Fig 2, p16 Fig 17|Cretaceous|Cretaceous|Fluvial sediments. ||Of Otway Group.||||
6363|Eumeralla Formation|71601|6|Mentioned|p120, p121|Albian|Hauterivian|Dinosaur Cove, Flat Rocks, both Vic. Ankylosaurian remains have been identified.||||||
6363|Eumeralla Formation|72050|5|Briefly described|p233 Fig.2, 235-238, 240, 241 Fig.11|Albian|Aptian|Blanketed the whole of the Otway Basin. Rapidly deposited to an original thickness exceeding four kms. Believed to be the source rock for Late Cretaceous offshore gas-fields. See also p242.|||Heathfield Sandstone; Windermere Sandstone Member.||Shales, siltstones, coals and argillaceous sandstones.|
6363|Eumeralla Formation|73153|5|Briefly described|p284-290, p292|Albian|Albian|Otway Basin. A nearly complete middle cervical vertebra assigned to elaphrosaurinae was recovered from the unit at Cape Otway. Area was high latitude at the time of deposition. Deposited in a river channel-dominated, fluvial palaeoenvironment including braided river systems. The theropod fauna from this unit includes indeterminate tetanurans, megaraptorans, tyrannosauroids, indeterminate maniraptorans, and unenlagiine dromaeosaurids.||Otway Group|||Volcanogenic sandstones and claystones.|
6363|Eumeralla Formation|73217|5|Briefly described|p1007-1009, 1013, 1016-1017, 1019-1023|Early Cretaceous|Early Cretaceous|Eastern Otway Basin. Hosts extensive NE-oriented folds; the St George Anticline and Artillery Rocks folds and fracture sets are described in detail.|c.113-100 Ma.|||Is overlain by Eastern View Formation.|Volcaniclastic sandstone.|
6363|Eumeralla Formation|73356|6|Mentioned|p2-4, p9, p14-17, p22, p28-29|Albian|Albian|Deposited during a period of regional sag.||Otway Group||||
6363|Eumeralla Formation|73357|6|Mentioned|p17-19|Albian|Barremian|Otway Basin. Lower part correlated with Pilosisporites notensis Spore-Pollen Zone of Morgan et al., (2002a), largely terrestrial palynofloras. Upper part correlated with Crybelosporites striatus Spore-Pollen Zone and Coptospora paradoxa Zone, moderately frequent expression of brackish/marinal marine depositional environments. Uppermost part correlated to late Albian Phimopollenites pannosus Spore-Pollen Zone.||Of Otway Group.||Overlies Pretty Hill Formation.||
6363|Eumeralla Formation|73383|4|Described|p3-4, p7 Tb.3.1, p9, p16-18, p20-22, p25|Cenomanian|Aptian|Otway Basin. Equivalent to chemostratigraphic sequences S2 to S4. Contains high Ti/Cr values and volcanogenic content in Sequence S2, lower Ti/Cr values and a subtle increase in Si/Al values in S3, and is quartz-rich in S4. Winchester and Floyd (1977) classification of sequences to a uniform andesitic-dacitic composition. Non-marine, but higher S concentrations in upper parts may be linked to marine incursions. Lithologies based on geochemistry using the ChemLith classification includes limestone, calcareous mudstone, calcareous and argillaceous sandstones, calcareous limestone and igneous rocks; and using the Herron classification (1988) includes shale, Fe-sand, Fe-shale, lith-arenite, wacke, subarkose and quartz arenite. See also vi, p8 Tb.3.3, p11, p25-27, p35-41, p45-49, p58-62, p68-88, p96-100, p107-110, p119-126, p136-137, p140-153, p165-167, p168-171, p176-179, p190-194, p201-218, p225-229, p236-239, p248-253, p263-264, p267-278, p322-323.||Otway Group|Windermere Sandstone, Heathfield Sandstone|Unconformably overlies Crayfish Subgroup, Laira Formation, unconformably underlies Sherbrook Group, Waarre Formation|Volcaniclastic and subsidiary siliciclastic material. Includes fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits, and more quartzose sandstone subunits.|
6363|Eumeralla Formation|73385|5|Briefly described|p3, p4 Fig.2.1, p5-6, p19-25, p28|Albian|Aptian|Otway Basin, outcrops in the Merino High, Barangarook High and Otway Ranges. Extensive unit deposited across the basin during a period of regional sag, thickens significantly south of the Mussel-Tartwaup Fault Zone.||Otway Group||Overlies Crayfish Subgroup, Laira Formation, Windamere Sandstone, underlies Waarre Formation, Sherbrook Group, interbedded with Heathfield Sandstone, Hawkesdale Volcanics.|Primarily composed of fluvial sands derived from volcanic sources. Contains fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
6363|Eumeralla Formation|73386|4|Described|p2-3, p4, p6-9, p13, Attachment A1|Albian|Barremian|Otway Basin. Late Barremian maximum age. Varies between 1500 m and 3000 m in thickness, thins from east to west and thins northwards due to erosion. Maximum thickness of approx. 7800 m in the Shipwreck Trough and southern edge of Mussel Platform. Fluvial and overbank depositional environments, sediments derived largely from the products of explosive dacitic volcanism. Contains the Cyclosporites hughesii, Crybelosporites striatus, Coptospora paradoxa and Phimopollenites pannosus spore-pollen zones of Partridge (2006). Chemostratigraphy identified three sequences within the formation, Sequence S2, S3 and S4 (Forbes et al., 2020). Overlies Paleozoic basement where the Crayfish Subgroup is absent.||Otway Group|Windermere Sandstone, Heathfield Sandstone, Killara coal measures|Unconformably overlies Crayfish Subgroup, Laira Formation, Katnook Sandstone, unconformably underlies Waarre Formation, Sherbrook Group|Sequence of fine- to medium-grained sandstones with interbedded mudstones, comprising quartz-poor volcanogenic derived sediments. Includes a basal sandstone member and black coals in lower part.|
6363|Eumeralla Formation|73594|4|Described|p3-4, p27-28, p34-44, p48-51, p66-67|Albian|Barremian|Otway Basin. Late Barremian to Albian in age. Fluvial, high latitude environment. Angular unconformity with Sherbrook Group in places of Cenomanian uplift such as the Otway Ranges. Locally over 2500 m thick onshore, estimated to be over 6000m thick offshore. Framework proposed by Kopsen and Schofield (1990) is used in this study, divides formation into upper, middle and lower units based on seismic character. Principal source of gas found in Late Cretaceous reservoirs. See also viii, p8, p14-15, p25, p45 Fig.5.19, p55, p59.||Otway Group|Windermere Member, Killara Coal Measures, Heathfield Member|Unconformably overlies Crayfish Subgroup. Conformably underlies Sherbrook Group, locally underlies Skull Creek Mudstone and unconformably underlies Waarre Formation.|Fine to medium-grained volcanogenic sandstones of predominantly litharenites and feldspathic litharenites with interbedded mudstones and coals, sporadic quartzose sandstones. Locally includes massive lacustrine clays in basal section.|
6363|Eumeralla Formation|75065|6|Mentioned|p157-159|||Constantine (2001). Otway Basin. Appears as Eumeralla Subgroup on p157.||||Correlates with Korumburra Subgroup.||
6379|Eurelia bed|39635|6|Mentioned|p463|||Informal name by Rowlands et al. (1978)||||||
6382|Euriowie Subgroup|22553|6|Mentioned|p83|Proterozoic|Proterozoic|||||||
6382|Euriowie Subgroup|22772|4|Described|p66,Table13.1|Neoproterozoic III|Cryogenian|||||||
6382|Euriowie Subgroup|22857|5|Briefly described|p66, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Of the Torrowangee Group. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
6382|Euriowie Subgroup|36733|6|Mentioned|Table 5|||||||||
6382|Euriowie Subgroup|38157|6|Mentioned|p261|||||||||
6382|Euriowie Subgroup|41405|5|Briefly described|p204|||||||||
6382|Euriowie Subgroup|43268|5|Briefly described|Map Legend||Neoproterozoic|Of the Torrowangee Group.||||||11-SEP-07
6382|Euriowie Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Siltstone, minor sandstone, limestone, sandy limestone and conglomerate. South Australian equivalent is Farina Subgroup.||||||11-SEP-07
6382|Euriowie Subgroup|70000|5|Briefly described|p34, p39|Neoproterozoic|Neoproterozoic|Represents interglacial sedimentation during marine transgressions caused possibly by eustatic sea level rise from melting of ice sheets. Mined at Torrowangee quarries for flux for the Broken Hill smelter.||Unit in Torrowangee Group.|Includes Wammerra, Mitchie Well, Tanyarto, Yowahro, Floods Creek, Formations.|Overlies Yancowinna Subgroup. Is overlain unconformably by Teamsters Creek Subgroup.|Limestone, dolomite and calcareous siltstone and sandstone.|
6382|Euriowie Subgroup|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Torrowangee Group.|Includes Wammerra, Mitchie Well, Tanyarto, Yowahro and Floods Creek Formations; Corona Dolomite.|Overlies Yancowinna Subgroup. Is overlain by Teamsters Creek Subgroup.|Calcareous sedimentary rocks with interbedded sandstone and siltstone; includes dolomite, marl and conglomerate of marine origin.|
6416|Evergreen Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498, p501|Aalenian|Pliensbachian|N Surat and Mulgildie Basins. Thickness to 260m.|||Includes Boxvale Sandstone Member.|Conformably overlies Precipice Sandstone.|Siltstone; mudstone, locally highly carbonaceous, with well-preserved plant impressions; and labile to sub-labile sandstone; also contains an acritarch-bearing oolitic ironstone horizon.|
6416|Evergreen Formation|13516|5|Briefly described|p159, 167, 168, 169, 170-174, 139|Early Jurassic|Early Jurassic|From Eromanga and Surat Basins|||Includes Boxvale Sandstone Member, Westgrove Ironstone Member|||
6416|Evergreen Formation|22464|6|Mentioned|p9|Middle Jurassic|Early Jurassic|Eromanga Basin, overlies Precipice Formation||||||
6416|Evergreen Formation|22757|5|Briefly described|Table6,p12|Early Jurassic|Early Jurassic|250 m. Also Table5,p10. as 255 m. Ipswich-Moreton Basin.||||||
6416|Evergreen Formation|22857|4|Described|p295, p296-7 Tb 22.1, p546 Tb A1.12|Middle Jurassic|Early Jurassic|Of the Bundamba Group. Lacustrine shale, siltstone and sandstone interleaved with fluviatile Boxvale Sandstone Member (Qld.). Geological Province: Surat Basin. See also p314. ||||||
6416|Evergreen Formation|22865|4|Described|p295,Table22.1p296-7|Aalenian|Pliensbachian|||||||
6416|Evergreen Formation|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
6416|Evergreen Formation|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
6416|Evergreen Formation|23037|5|Briefly described|p34,47,114,117,8||Jurassic|||||||
6416|Evergreen Formation|23050|5|Briefly described|p82 Fig.17|Early Jurassic|Early Jurassic|of Surat Basin.||||||
6416|Evergreen Formation|23053|6|Mentioned|Fig10p17|Toarcian|Pliensbachian|||||||
6416|Evergreen Formation|23056|6|Mentioned|8 table 1B|||Geol province Eromanga Basin||||||
6416|Evergreen Formation|23799|3|Fully described|p51, p10 Tb. 1|Toarcian|Pliensbachian|Includes the former "Evergreen Shales" and Boxvale Sandstone as a member. Conformably overlies Precipice Sst; part unconformably overlies Chahpingah Meta-Igneous Complex; a subunit overlies the Tondahra Granite also. Geological Province: Surat Basin.||||||19-AUG-08
6416|Evergreen Formation|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
6416|Evergreen Formation|23841|4|Described|p448|||Geological Province: Great Artesian Basin.||||||
6416|Evergreen Formation|23883|5|Briefly described|p129 Fig. 11.2|Early Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
6416|Evergreen Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
6416|Evergreen Formation|24068|4|Described|p269|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin.  Maximum thickness: 200m.||||||
6416|Evergreen Formation|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||
6416|Evergreen Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
6416|Evergreen Formation|24159|5|Briefly described|p148 Fig.2, p151|Early Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Hutton Sandstone. Underlying Unit: Precipice Sandstone.||||||
6416|Evergreen Formation|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
6416|Evergreen Formation|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|24615|5|Briefly described|CD|Jurassic|Jurassic|[Je, Je/o].  Labile and sublabile, fine- to medium-grained sandstone, carbonaceous mudstone, siltstone and minor coal;  local oolitic ironstone.||||||
6416|Evergreen Formation|29385|6|Mentioned|p80|||Also P81.Jurassic||||||
6416|Evergreen Formation|29387|6|Mentioned|p30|||Also Table 5.||||||
6416|Evergreen Formation|29389|6|Mentioned|p19|||Early Jurassic.||||||
6416|Evergreen Formation|29393|6|Mentioned|Table 4|||Jurassic.||||||
6416|Evergreen Formation|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
6416|Evergreen Formation|29489|6|Mentioned|p11|||||||||
6416|Evergreen Formation|29496|6|Mentioned|p21|||||||||
6416|Evergreen Formation|29591|6|Mentioned|p69|||||||||
6416|Evergreen Formation|29721|6|Mentioned|p246|||||||||
6416|Evergreen Formation|29958|6|Mentioned|p13|||||||||
6416|Evergreen Formation|29960|5|Briefly described|p2|||||||||
6416|Evergreen Formation|29961|5|Briefly described|p14|||||||||
6416|Evergreen Formation|30022|6|Mentioned|p38|||||||||
6416|Evergreen Formation|30102|6|Mentioned|p17|||Correlation with basal Hutton Sandstone.||||||
6416|Evergreen Formation|30103|6|Mentioned|p10|||||||||
6416|Evergreen Formation|30232|6|Mentioned|p667,668,677||Early Jurassic|||||||
6416|Evergreen Formation|30451|3|Fully described|p72|||See also p73. Jurassic age.||||||07-APR-08
6416|Evergreen Formation|30455|6|Mentioned|p5|||See also P13||||||
6416|Evergreen Formation|30456|6|Mentioned|p95|||||||||
6416|Evergreen Formation|30457|6|Mentioned|p96|||||||||
6416|Evergreen Formation|30458|6|Mentioned|p3|||Jurassic age||||||
6416|Evergreen Formation|30460|6|Mentioned|p5|||Jurassic age||||||
6416|Evergreen Formation|30462|6|Mentioned|p356|||||||||
6416|Evergreen Formation|30464|6|Mentioned|Fig.1|||iniospores||||||
6416|Evergreen Formation|30465|6|Mentioned|p4|||||||||
6416|Evergreen Formation|30466|6|Mentioned|p5|||Jurassic age||||||
6416|Evergreen Formation|30472|6|Mentioned|p132|||Pollen distribution.||||||
6416|Evergreen Formation|30474|6|Mentioned|p251|||Correlation chart||||||
6416|Evergreen Formation|30494|6|Mentioned|p9|||||||||
6416|Evergreen Formation|30508|6|Mentioned|p81|||See also P90. Early Jurassic palynology||||||
6416|Evergreen Formation|30691|6|Mentioned|p15|||On Table 4||||||
6416|Evergreen Formation|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30695|4|Described|Table 3|||Lower Jurassic age||||||
6416|Evergreen Formation|30696|4|Described|Table 4|||Lower Jurassic age||||||
6416|Evergreen Formation|30698|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30699|5|Briefly described|p52|||Structure map. See also stratigraphy p53.||||||18-SEP-18
6416|Evergreen Formation|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30702|6|Mentioned|Fig.1|||See Stratigraphic Table||||||
6416|Evergreen Formation|30854|4|Described|Table 4|||Lower Jurassic age||||||
6416|Evergreen Formation|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|30915|6|Mentioned|p98|||||||||
6416|Evergreen Formation|30916|6|Mentioned|p97|||||||||
6416|Evergreen Formation|31116|4|Described|p21|||L. Jurassic. See also p1.||||||18-SEP-18
6416|Evergreen Formation|31117|5|Briefly described|p379|||Jurassic. Lithology.||||||18-SEP-18
6416|Evergreen Formation|31118|6|Mentioned|p313|||Refers Casey et al. (1966)||||||
6416|Evergreen Formation|31120|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|31304|5|Briefly described|p628|||Lithology in drill hole.||||||
6416|Evergreen Formation|31369|6|Mentioned|Table 4|||Jurassic||||||
6416|Evergreen Formation|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|31659|6|Mentioned|p74|||Jurassic||||||
6416|Evergreen Formation|32136|5|Briefly described|p3|||Late Toarcian age for upper section. Jur. miospores.||||||18-SEP-18
6416|Evergreen Formation|32137|6|Mentioned|p355|||Refers oolite beds||||||
6416|Evergreen Formation|32138|6|Mentioned|p396|||||||||
6416|Evergreen Formation|32182|4|Described|p3|||Jurassic||||||
6416|Evergreen Formation|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32276|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32712|6|Mentioned|p127|||See also Table 1||||||
6416|Evergreen Formation|32715|6|Mentioned|p1186|||Re oil||||||
6416|Evergreen Formation|32797|4|Described|Table 4|||L. Jur.||||||
6416|Evergreen Formation|33059|4|Described|p113|||L.Jur.||||||
6416|Evergreen Formation|33071|4|Described|p6|||L.Jur.||||||
6416|Evergreen Formation|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33088|4|Described|Table 3|||Injune Ck.Gp.||||||
6416|Evergreen Formation|33090|4|Described|Table 4|||L.Jur.||||||
6416|Evergreen Formation|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33192|6|Mentioned|p21|||||||||
6416|Evergreen Formation|33367|5|Briefly described|Table 1|||||||||
6416|Evergreen Formation|33381|5|Briefly described|p117|||Correl. chart. L. Jur. Constituent formations. See also p119.||||||18-SEP-18
6416|Evergreen Formation|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33530|5|Briefly described|Table 1|||Lower Jurassic.||||||18-SEP-18
6416|Evergreen Formation|33639|6|Mentioned|p10|||||||||
6416|Evergreen Formation|33672|4|Described|p41|||||||||
6416|Evergreen Formation|33673|4|Described|p291|||||||||
6416|Evergreen Formation|33675|4|Described|p412|||Lithology.||||||
6416|Evergreen Formation|33728|6|Mentioned|p38|||||||||
6416|Evergreen Formation|33774|3|Fully described|p48|||||||||
6416|Evergreen Formation|33971|6|Mentioned|Appendix 1|||Palynology. Doubtful about Formation assignment.||||||
6416|Evergreen Formation|34001|6|Mentioned|p18|||In Noona No.1 Well||||||
6416|Evergreen Formation|34065|6|Mentioned|p10|||L.Jur.||||||
6416|Evergreen Formation|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
6416|Evergreen Formation|34172|6|Mentioned|p53|||||||||
6416|Evergreen Formation|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|34212|6|Mentioned|p2|||Jurassic. See also PP8,14 etc.||||||
6416|Evergreen Formation|34213|6|Mentioned|p356|||See also P360.||||||
6416|Evergreen Formation|34452|6|Mentioned|p1|||L.Jurassic. See also PP2,3,4,5 etc||||||
6416|Evergreen Formation|34507|6|Mentioned|p87|||||||||
6416|Evergreen Formation|34613|4|Described|Table 4|||||||||
6416|Evergreen Formation|34618|6|Mentioned|p9|||||||||
6416|Evergreen Formation|34905|6|Mentioned|p531|||||||||
6416|Evergreen Formation|35079|6|Mentioned|Fig.3|||||||||
6416|Evergreen Formation|35095|6|Mentioned|p116|||||||||
6416|Evergreen Formation|35148|4|Described|p415|||See also Fig.1 and Table 1.||||||
6416|Evergreen Formation|35157|6|Mentioned|p518|||||||||
6416|Evergreen Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
6416|Evergreen Formation|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
6416|Evergreen Formation|35811|5|Briefly described|Table 5|||||||||
6416|Evergreen Formation|35901|6|Mentioned|p17|||||||||
6416|Evergreen Formation|35937|6|Mentioned|Fig.5|||||||||
6416|Evergreen Formation|36111|6|Mentioned|p34|||||||||
6416|Evergreen Formation|36113|6|Mentioned|p21|||||||||
6416|Evergreen Formation|36233|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|36236|6|Mentioned|p183|||||||||
6416|Evergreen Formation|36241|6|Mentioned|p110|||||||||
6416|Evergreen Formation|36243|6|Mentioned|Table 6A|||||||||
6416|Evergreen Formation|36333|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|36570|6|Mentioned|p26,p55|||See also Table 1.||||||
6416|Evergreen Formation|36574|6|Mentioned|p599|||||||||
6416|Evergreen Formation|36613|6|Mentioned|p1876|||||||||
6416|Evergreen Formation|36643|6|Mentioned|p61|||||||||
6416|Evergreen Formation|36708|6|Mentioned|p52|||||||||
6416|Evergreen Formation|36825|6|Mentioned|p14|||||||||
6416|Evergreen Formation|36905|6|Mentioned|p20|||||||||
6416|Evergreen Formation|36914|6|Mentioned|p87|||||||||
6416|Evergreen Formation|36919|6|Mentioned|p160|||||||||
6416|Evergreen Formation|36926|6|Mentioned|p162|||||||||
6416|Evergreen Formation|37065|5|Briefly described|p38|||||||||
6416|Evergreen Formation|37117|5|Briefly described|p313|||||||||
6416|Evergreen Formation|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|37288|6|Mentioned|p41|||||||||
6416|Evergreen Formation|37463|6|Mentioned|p479|||||||||
6416|Evergreen Formation|37618|6|Mentioned|p26|||||||||
6416|Evergreen Formation|37994|6|Mentioned|p144|||||||||
6416|Evergreen Formation|37995|4|Described|p62|||||||||
6416|Evergreen Formation|37996|6|Mentioned|p71|||||||||
6416|Evergreen Formation|38205|6|Mentioned|p96|||||||||
6416|Evergreen Formation|38226|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|38358|6|Mentioned|Fig.1|||||||||
6416|Evergreen Formation|38373|6|Mentioned|p617|||||||||
6416|Evergreen Formation|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|39070|4|Described|p362|||||||||
6416|Evergreen Formation|39212|4|Described|p15|||p24 Petroleum reservoir. See also P36 excursion site.||||||18-SEP-18
6416|Evergreen Formation|39215|6|Mentioned|p53|||||||||
6416|Evergreen Formation|39218|6|Mentioned|p48|||Flora||||||
6416|Evergreen Formation|39315|6|Mentioned|Fig.5|||||||||
6416|Evergreen Formation|39445|5|Briefly described|p127|||Depositional environment. See also Table 10.||||||18-SEP-18
6416|Evergreen Formation|39478|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|39494|6|Mentioned|p137|||||||||
6416|Evergreen Formation|39505|6|Mentioned|p179|||||||||
6416|Evergreen Formation|39632|6|Mentioned|p209|||||||||
6416|Evergreen Formation|39757|6|Mentioned|p1601|||||||||
6416|Evergreen Formation|39815|6|Mentioned|p444|||||||||
6416|Evergreen Formation|39847|6|Mentioned|p35|||||||||
6416|Evergreen Formation|39907|6|Mentioned|F15|||||||||
6416|Evergreen Formation|39943|6|Mentioned|Table 8A|||||||||
6416|Evergreen Formation|39989|6|Mentioned|p426|||||||||
6416|Evergreen Formation|40030|6|Mentioned|p135|||||||||
6416|Evergreen Formation|40121|6|Mentioned|p446|||||||||
6416|Evergreen Formation|40245|6|Mentioned|Table 2|||||||||
6416|Evergreen Formation|40249|6|Mentioned|p38|||||||||
6416|Evergreen Formation|40250|4|Described|p29|||||||||
6416|Evergreen Formation|40540|6|Mentioned|p150|||||||||
6416|Evergreen Formation|40541|3|Fully described|p108|||||||||
6416|Evergreen Formation|40544|6|Mentioned|p161|||||||||
6416|Evergreen Formation|40623|5|Briefly described|p72|||Briefly described p109.||||||18-SEP-18
6416|Evergreen Formation|40666|4|Described|p355|||||||||
6416|Evergreen Formation|40675|6|Mentioned|Table 8A|||||||||
6416|Evergreen Formation|40687|3|Fully described|p412|||||||||
6416|Evergreen Formation|40688|6|Mentioned|p424|||||||||
6416|Evergreen Formation|40767|5|Briefly described|p14|||||||||
6416|Evergreen Formation|40832|3|Fully described|p254|||||||||
6416|Evergreen Formation|40833|6|Mentioned|p468|||||||||
6416|Evergreen Formation|40953|6|Mentioned|p19|||||||||
6416|Evergreen Formation|40962|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41060|6|Mentioned|p2|||||||||
6416|Evergreen Formation|41061|6|Mentioned|p19|||||||||
6416|Evergreen Formation|41064|6|Mentioned|p60|||||||||
6416|Evergreen Formation|41097|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41159|6|Mentioned|Fig.4|||||||||
6416|Evergreen Formation|41177|6|Mentioned|p223|||||||||
6416|Evergreen Formation|41187|6|Mentioned|Fig.2|||||||||
6416|Evergreen Formation|41188|6|Mentioned|p232|||||||||
6416|Evergreen Formation|41198|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41210|3|Fully described|p158|||||||||
6416|Evergreen Formation|41211|6|Mentioned|p179|||||||||
6416|Evergreen Formation|41246|6|Mentioned|Map legend|Jurassic||||||||
6416|Evergreen Formation|41247|6|Mentioned|p127|||||||||
6416|Evergreen Formation|41266|6|Mentioned|Fig.3|||||||||
6416|Evergreen Formation|41455|6|Mentioned|p68|||||||||
6416|Evergreen Formation|41591|6|Mentioned|p17|||||||||
6416|Evergreen Formation|41725|6|Mentioned|p400|||||||||
6416|Evergreen Formation|41747|6|Mentioned|p469|||||||||
6416|Evergreen Formation|41992|4|Described|Fig.2 P183|||||||||
6416|Evergreen Formation|42007|5|Briefly described|Fig.2 P182|||||||||
6416|Evergreen Formation|42067|4|Described|Apendix 2|||See also p311.||||||18-SEP-18
6416|Evergreen Formation|42157|6|Mentioned|p377|||||||||
6416|Evergreen Formation|42248|6|Mentioned|p410|||||||||
6416|Evergreen Formation|42316|6|Mentioned|p8|||||||||
6416|Evergreen Formation|42463|6|Mentioned|Fig.5 P172|||||||||
6416|Evergreen Formation|42493|5|Briefly described|p17, Fig.1 p18|||||||||
6416|Evergreen Formation|42634|6|Mentioned|p12|||||||||
6416|Evergreen Formation|42865|6|Mentioned|p18|||||||||
6416|Evergreen Formation|42893|6|Mentioned|p12|||||||||
6416|Evergreen Formation|42911|5|Briefly described|p13|||||||||
6416|Evergreen Formation|43000|5|Briefly described|Fig.5,p112|||||||||
6416|Evergreen Formation|43002|5|Briefly described|Fig.2,p135|||||||||
6416|Evergreen Formation|43004|5|Briefly described|Table 1,p179|||||||||
6416|Evergreen Formation|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
6416|Evergreen Formation|43185|6|Mentioned|6||Jurassic|||||||
6416|Evergreen Formation|43582|6|Mentioned|Fig.5,p16,28||Early Jurassic|||||||
6416|Evergreen Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
6416|Evergreen Formation|43714|6|Mentioned|Fig.3,p5||Early Jurassic|||||||
6416|Evergreen Formation|43851|14|Not recorded|Tb p106,111,113||Early Jurassic|||||||
6416|Evergreen Formation|43923|6|Mentioned|p4||Jurassic|||||||
6416|Evergreen Formation|43982|14|Not recorded|Map Legend|||||||||
6416|Evergreen Formation|43983|14|Not recorded|p2,Fig.1|||||||||
6416|Evergreen Formation|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|43994|14|Not recorded|Map Legend|||||||||
6416|Evergreen Formation|43997|14|Not recorded|p114|||||||||
6416|Evergreen Formation|43998|4|Described|p14,17,map||Early Jurassic|||||||
6416|Evergreen Formation|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
6416|Evergreen Formation|44026|14|Not recorded|p123,124||Jurassic|||||||
6416|Evergreen Formation|44028|14|Not recorded|Fig.2,p512||Jurassic|See Strat Table.||||||
6416|Evergreen Formation|44031|14|Not recorded|p9,11||Early Jurassic|||||||
6416|Evergreen Formation|44032|14|Not recorded|p462,map,p463,464|||Surat Basin,= to Marburg Formation of Moreton Basin. Inlcudes Westgrove Ironside Member and Boxvale Sandstone Member.||||||
6416|Evergreen Formation|44084|14|Not recorded|p18,0,22,24,26,28,32||Early Jurassic|||||||
6416|Evergreen Formation|44091|14|Not recorded|p57||Jurassic|||||||
6416|Evergreen Formation|44115|14|Not recorded|p17-24|||||||||
6416|Evergreen Formation|44116|14|Not recorded|p28,33|||||||||
6416|Evergreen Formation|44118|14|Not recorded|Map Legend||Jurassic|||||||
6416|Evergreen Formation|44124|14|Not recorded|p4|||||||||
6416|Evergreen Formation|44129|14|Not recorded|p95-96||Jurassic|||||||
6416|Evergreen Formation|44169|2|Defined|Tb.1,p9,map|||||||||
6416|Evergreen Formation|44170|2|Defined|p21-23,32,25,40,map||Early Jurassic|Tb.1.||||||
6416|Evergreen Formation|44174|14|Not recorded|p345,347-349||Early Jurassic|||||||
6416|Evergreen Formation|44207|14|Not recorded|p115|||||||||
6416|Evergreen Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
6416|Evergreen Formation|44379|14|Not recorded|p21|||||||||
6416|Evergreen Formation|44381|14|Not recorded|p7|||||||||
6416|Evergreen Formation|44390|14|Not recorded|p9,13,15,16,Tb.1||Early Jurassic|||||||
6416|Evergreen Formation|44391|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|44415|14|Not recorded|Fig.2,p23|||||||||
6416|Evergreen Formation|44419|14|Not recorded|p274,278||Jurassic|||||||
6416|Evergreen Formation|44420|14|Not recorded|p1,3-5,9-11,18,20,22|||p26,Fig.14||||||
6416|Evergreen Formation|44421|14|Not recorded|p,6,10-17,19-21||Jurassic|||||||
6416|Evergreen Formation|44422|14|Not recorded|p149,153||Jurassic|||||||
6416|Evergreen Formation|44426|14|Not recorded|p12||Early Jurassic|Early Jurassic on spore data. Contains spores, bone fragments and leaves, including Pagiophyllum, Cladophlebis, Coniopteris, Otozamites and Nilssonia.||||||
6416|Evergreen Formation|44525|14|Not recorded|p520|||||||||
6416|Evergreen Formation|44573|14|Not recorded|p97||Jurassic|||||||
6416|Evergreen Formation|44636|2|Defined|p161,164,165,167||Early Jurassic|||||||
6416|Evergreen Formation|44637|14|Not recorded|Table||Jurassic|||||||
6416|Evergreen Formation|44640|14|Not recorded|p30|||||||||
6416|Evergreen Formation|44644|14|Not recorded|p18|||||||||
6416|Evergreen Formation|44668|14|Not recorded|p59,60|||||||||
6416|Evergreen Formation|44742|14|Not recorded|p91|||Lower part correlated with Razorback Beds on palynological evidence.||||||
6416|Evergreen Formation|44787|14|Not recorded|Tb.123,125,diag.p126||Jurassic|||||||
6416|Evergreen Formation|44805|14|Not recorded|p388|||||||||
6416|Evergreen Formation|45071|3|Fully described|Table 15|||||||||
6416|Evergreen Formation|45073|6|Mentioned|p58|||Geological history||||||
6416|Evergreen Formation|45110|3|Fully described|p90|||See also p13 and p24.||||||18-SEP-18
6416|Evergreen Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
6416|Evergreen Formation|46984|6|Mentioned|p154|||See also Table 1.||||||
6416|Evergreen Formation|46989|5|Briefly described|Table 1|||||||||
6416|Evergreen Formation|48900|4|Described|p51|||Lower Jurassic.||||||
6416|Evergreen Formation|48919|4|Described|p45|||See also p46-53. Jurassic.||||||18-SEP-18
6416|Evergreen Formation|48920|5|Briefly described|p44|||||||||
6416|Evergreen Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
6416|Evergreen Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
6416|Evergreen Formation|50190|5|Briefly described|p37, 85|Jurassic|Jurassic|Contains oolitic ironstone units. Geological Province: Mulgildie Basin.||||||06-APR-05
6416|Evergreen Formation|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|50301|5|Briefly described|Map Legend|Jurassic|Jurassic|Ironstone, sandstone, siltstone, mudstone.||||||09-JUN-04
6416|Evergreen Formation|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Surat Basin||||||
6416|Evergreen Formation|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Mudstone, siltstone, sandstone, ironstone, minor coal.||||||
6416|Evergreen Formation|50598|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium grained sandstone, carbonaceous mudstone, siltstone and minor coal.||||||21-JUL-04
6416|Evergreen Formation|60281|5|Briefly described|p27|||Geological Province: Surat Basin, Cecil Plains Sub-basin.||||||
6416|Evergreen Formation|60282|5|Briefly described|p11, p39|Jurassic|Jurassic|Contains oolitic ironstone units.  Geological Province: Mulgildie Basin.||||||13-APR-05
6416|Evergreen Formation|60993|6|Mentioned|p17, p6 Fig. 2|||Correlates with Marburg Subgroup units. Geological Province: Surat Basin.||||||
6416|Evergreen Formation|60997|5|Briefly described|p140|||Includes the Boxvale Member. Geological Province: Surat Basin. ||||||
6416|Evergreen Formation|60998|5|Briefly described|p145|||Supersedes "Evergreen Shale". Comprises the original "Evergreen Shale", Boxvale Sandstone, Westgrove Ironstone Member and overlying shale sequence. Overlies Precipice Sandstone; underlies Hutton Sandstone.||||||
6416|Evergreen Formation|60999|5|Briefly described|p176, p178 Fig. 10|||Includes the basal oolitic Westgrove Ironstone Member. Lowermost part broadly correlates with Gatton Sandstone.  Geological Province: Surat Basin.||||||
6416|Evergreen Formation|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Gatton Sandstone. See also p255 Figs. 23, 24 and 25. ||||||
6416|Evergreen Formation|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|mudstone, siltstone and fine-grained sublabile to labile sandstone; oolitic chamositic ironstone at the base.||||||
6416|Evergreen Formation|61310|6|Mentioned|p22|||Together with the Hutton Sandstone, correlated with Marburg Formation and "Upper Bundamba Unit".||||||
6416|Evergreen Formation|61377|5|Briefly described|p139, p148 Tb. |Early Jurassic|Early Jurassic|Major lacustrine shale/sltst/sst sequence; good hydrocarbon source rock - incl: Boxvale Sst Mbr (good reservoir sst). Conformably overlies Precipice Fm providing a good reservoir seal; conformably overlain by Hutton Sst. Geol.Prov:Surat Basin.||||||07-FEB-11
6416|Evergreen Formation|61611|6|Mentioned|p265 Fig. 3|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||13-MAR-09
6416|Evergreen Formation|61832|5|Briefly described|p187|Jurassic|Jurassic|On the MUNDUBERRA sheet.  Overlain by Hutton Sandstone; overlies Precipice Sandstone. Geological Province: Surat Basin.||||||03-JUL-06
6416|Evergreen Formation|63218|6|Mentioned|p211 Fig.2. |Early Jurassic|Early Jurassic|Surat Basin.|||Includes Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|63748|6|Mentioned|p23|||Correlative of Marburg Subgroup.  Geological province: Surat Basin.||||||07-FEB-11
6416|Evergreen Formation|63979|6|Mentioned|p33, Fig. 44|Toarcian|Toarcian|Overlies Precipice Sandstone. Geological province: Surat Basin. Time-equivalent of Poolowanna Formation.||||||07-FEB-11
6416|Evergreen Formation|64197|6|Mentioned|p630 Fig.7|Early Jurassic|Early Jurassic|||||Underlies Hutton Sandstone; overlies Precipice Sandstone.||
6416|Evergreen Formation|64398|5|Briefly described|Map legend|Jurassic|Jurassic|Pale grey to greenish grey, flaggy, fine- to medium-grained, micaceous, labile to sublabile sandstone; pale green or khaki mudstone, carbonaceous mudstone; minor white siltstone and coal.||||||18-AUG-08
6416|Evergreen Formation|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Overlain by Hutton Sst.  Flaggy, fine/med.-gr.micaceous, labile to sublabile sst; mudstone, carb.mudst.; minor siltst+coal. Fine lithic sst, siltst, mudst, oolitic or pelletal ironstone.Mudst., siltst.and fine-gr.sublabile sst; oolitic ironstone at base.||||||19-AUG-08
6416|Evergreen Formation|64665|5|Briefly described|p53 Fig.2, p60, p61.|Early Jurassic|Early Jurassic|Eromanga and Surat Basins. Lateral equivalent of upper part of Poolowanna Formation. Correlates with Ma Ma Creek Member (Clarence-Moreton Basin) and Brighton beds (Southern Nambour Basin). With the Precipice Sandstone, forms the first of six cyclothems in the Surat Basin.|||Includes Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.|Contains thin coals.|
6416|Evergreen Formation|64856|4|Described|p46 Fig.4, p76, p79, p81-85|Toarcian|Pleinsbachian|Surat Basin. Contains the Boxvale Sandstone, and the Westgrove Ironstone, Members. Conformably overlies the Precipice Sandstone and locally unconformably overlies Moolayember Formation of Bowen Basin /basement. Is overlain by Hutton Sandstone. Sandstone, siltstone, mudstone, shale. Age from palynoflora (units APJ21, 22, 3).| | ||||28-NOV-17
6416|Evergreen Formation|64857|4|Described|p130-132, p113 Fig.3|||Contains Boxvale Sandstone Member and Westgrove Ironstone Member. Conformably overlies Precipice Sandstone. Surat Basin.||||||
6416|Evergreen Formation|64858|5|Briefly described|p183-187, p181 Tb. 1|||Basal Surat Basin unit in the west, southwest and south of the basin.||||||30-NOV-09
6416|Evergreen Formation|64859|6|Mentioned|p195|||||||||
6416|Evergreen Formation|65003|5|Briefly described|p8||Early Jurassic|Of Surat Basin.||||Overlies the Precipice Sandstone.||
6416|Evergreen Formation|65096|6|Mentioned|p373|||Surat Basin. Along with Hutton Sandstone, compared with the  Marburg sub-group [sic] of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||||
6416|Evergreen Formation|65112|5|Briefly described|p327; 328; Fig 11 p324, p329|Lower Jurassic|Lower Jurassic|Unit from Surat and Eromanga Basins, deposited in non-marine conditions.|194.5-178 Ma.|||Underlies the Hutton Sandstone and overlies the Precipice Sandstone.||22-MAR-12
6416|Evergreen Formation|65113|5|Briefly described|Fig 4 p340|Middle Jurassic|Early Jurassic|Overlies Precipice Sandstone, underlies Hutton Sandstone.||||||
6416|Evergreen Formation|65114|5|Briefly described|p385 Fig.3|Middle Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|65116|5|Briefly described|p454-5, Fig 2 p437|Middle Jurassic|Early Jurassic|Underlies the Hutton Sandstone, Overlies the Precipice Sandstone, Surat Basin. Lithic sandstone, mudstone and minor coal. Upward coarsening and progradational sequence. ||||||
6416|Evergreen Formation|65117|5|Briefly described|p466, 7, 9, 470, 2, 4, Fig 4 p465|Toarcian|Pliensbachian|Surat Basin. Includes Boxvale Sandstone Member, Westgrove Ironstone Member., Overlies the Precipice Sandstone with gradational contact. Up to 300m thick. More widespread than Precipice Sandstone.||||||
6416|Evergreen Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 4-5, 6-19|Early Jurassic|Early Jurassic|Surat Basin. Siltstone, mudstone, lithic to quartzose sandstone, minor oolithic ironstone, coal. Up to 260 m thick. Age: 188-198Ma. Fission Track age: 116+/-6 Ma . Present in Cockatoo Creek Well.||||||
6416|Evergreen Formation|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlies Precipice Sandstone. Overlain by Hutton Sandstone.||||||08-MAR-12
6416|Evergreen Formation|65388|3|Fully described|p211-213, 204, 210, 17, 19, 42, 43, 46|Toarcian|Pliensbachian|Surat Basin, Mulgildie Basin.  Jensen & others (1964) defined the Evergreen Formation to include the "Evergreen Shales" as the lower unit, the overlying Boxvale Sandstone as a member and an upper mudstone, siltstone and sandstone containing an oolitic basal member (now Westgrove Ironstone Member).  Thickness 30-307m.  Conformably overlies Precipice Sandstone. Unconformably overlies Nogo beds, and Narayen beds, Torsdale Volcanics. Laterally continuous with the lower part of the Marburg Subgroup, Moreton Basin. Overlain by Hutton Sandstone. Palynofloras are largely Pliensbachian-Toarcian (Early Jurassic) and associated with units  APJ22, and APJ32. See also p208, 210, 289||||||
6416|Evergreen Formation|65489|6|Mentioned|p24|||Craton-derived sediment; potential reservoir.||||||
6416|Evergreen Formation|66529|6|Mentioned|p12 Fig.5 |||Eromanga Basin.|||Includes Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|66915|5|Briefly described|p6 Fig.3, p12|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
6416|Evergreen Formation|67133|5|Briefly described|p1-3, p5, p10-11, p19-21|Jurassic|Jurassic|Seal for Hutton Sandstone. Represents change from braided to meandering fluvial system of deposition. 29 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (25-97%) and kaolinite (2-35%) is the dominant clay mineral. Mixed-layer clays vary from smectite-rich to illite-rich.|||Boxvale Sandstone Member, Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone. Is overlain by Hutton Sandstone.|Sandstones and mudstones.|
6416|Evergreen Formation|67402|4|Described|p146 fig SRT3, p147 fig SRT5|Bajocian|Pliensbachian|Surat and Mulgildie Basins. Potential conventional seal for carbon dioxide storage. Deposited in fresh-water lacustrine, meandering streams or deltal depositional environments. Generally less than 100m thick. Mistakenly referred to as the Evergreen Sandstone on p154. See also p148, p149 fig SRT7, p151, p152, p154, p155 fig SRT17, p156, p159, p160, p162, p252, p253, p306.|||Includes the Boxvale Member|Overlies the Precipice Sandstone and Boxvale Sandstone. Overlain by the Hutton Sandstone.|Sandstone, carbonaceous mudstone and siltstone, shale and coal.|
6416|Evergreen Formation|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Hutton Sandstone. Underlain by Precipice Sandstone.||
6416|Evergreen Formation|68003|5|Briefly described|p57 Fig.3-n, p58 Fig.3-o.|Early Jurassic|Early Jurassic|Bowen Basin. See also reference to [superseded] Evergreen Sandstone.||||Overlies Precipice Sandstone and, locally, unconformably overlies Napperby Formation. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|68004|5|Briefly described|p87, p172.|Early Jurassic|Early Jurassic|Surat Basin. Hydrocarbon reservoir in Queensland; targeted for oil/gas exploration in New South Wales from the 1960s; only minor fluorescence and low level gas shows. Excellent reservoir; exploration targetting limited to very northern part of the Basin in NSW.||||||
6416|Evergreen Formation|68008|4|Described|p233, p236-238, p240, p297|Early Jurassic|Early Jurassic|Jensen et al. (1964), for Jurassic sediments between Precipice Sandstone and Hutton Sandstone in the Surat Basin. Included Evergreen Shales (Whitehouse, 1953) and Boxvale Sandstone (Reeves, 1947). Surat and Mulgildie Basins. Fresh-water fluvial and lacustrine deposits. 105-260m thick. Age from microflora. The oolitic ironstone is a time marker linking this Formation to Landsborough Sandstone, Brighton beds and Tiaro Coal Measures. Has zones of deep weathering.||||Conformably overlies Precipice Sandstone. Is overlain conformably by Hutton Sandstone.|White and grey, fine-grained quartzose flaggy sandstone and siltstone, overlain by a ferruginous oolite horizon 3-4m thick, above which is thin-bedded, cream, friable flaggy sandstone. Local grey-black carbonaceous shale, siltstone and minor coal.|
6416|Evergreen Formation|68117|5|Briefly described|p346|Early Jurassic|Early Jurassic|Surat Basin.|||Westgrove Ironstone Member.|||
6416|Evergreen Formation|68135|5|Briefly described|p52 Fig.2b, p59, p64|Toarcian||Surat Basin (QLD). Vertebrate body parts, invertebrate and plant macrofossils throughout; including the freshwater plesiosaur Siderops.||||Overlies Precipice Sandstone. Is overlain unconformably by Hutton Sandstone|Silty sandstone with oolitic ironstone beds.|14-SEP-17
6416|Evergreen Formation|68139|6|Mentioned|p23, 32|Early Jurassic|Early Jurassic|Surat Basin. A regional seal.|||Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
6416|Evergreen Formation|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Hutton and Precipice Sandstones, are all mapped under the symbol, Jb.||||||
6416|Evergreen Formation|68576|4|Described|Q_4: p3, p12, p14, p17, p22|Early Jurassic|Early Jurassic|Surat Basin. Fluvio-lacustrine or prograding lacustrine delta deposits. Is locally capped by 27 Ma basalt from the Buckland volcano. Pliensbachian to Toarcian.|||Westgrove Ironstone Member, Boxvale Sandstone Member.|Conformably overlies Precipice Sandstone. Is overlain conformably by Hutton Sandstone.|Green-grey sandstone, carbonaceous mudstone and argillite, minor carbonaceous siltstone, shale and coal; then the Boxvale Sandstone Member; then dark green to black mudstone (laminated with sandstone, siltstone and shale) and fine-grained sandstone.|
6416|Evergreen Formation|68679|6|Mentioned|p312-313, p338|Jurassic|Jurassic|Northern New England Orogen.||||||
6416|Evergreen Formation|69457|5|Briefly described|p41:2-3|||NE Eromanga Basin and Surat Basin.|||Overlies Precipice Sandstone.|Lateral equivalent of (part) Poolowanna Formation.||12-JUL-16
6416|Evergreen Formation|69582|5|Briefly described|p36, p38|Lower Jurassic|Lower Jurassic|Surat Basin.||||Overlies the Precipice Sandstone. Overlain by the Hutton Sandstone.|Sandstone.|
6416|Evergreen Formation|69594|4|Described|p519, p524, p534-535, p536 Fig.7.17|Toarcian|Pliensbachian|See also p539, p544-546, p572. Whitehouse (1955), for the shales between the Precipice Sandstone and Boxvale Sandstone of Reeves (1947); redefined by Jensen et al. (1964) to include also the Boxvale Sandstone Member and the Westgrove Ironstone Member. Eromanga, northern Surat Basins. 10-40m, up to 307m, thick. Lacustrine, or meandering streams and deltas, deposits. A secondary-importance Surat Basin reservoir for oil condensate, gas and LPG.|||Boxvale Sandstone Member, Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone. Is overlain by Hutton Sandstone. Laterally equivalent to the lower Marburg Subgroup and the Poolowanna Formation.|Fine sandstone, carbonaceous mudstone, lesser carbonaceous siltstone, shale and coal; overlain by the Boxvale Sandstone Member (mostly quartzose sandstone); then mudstone interlaminated with sandstone and shale and fine-grained labile sandstone.|
6416|Evergreen Formation|69633|4|Described|p1-5, p7-12, p14, p20-21|Early Jurassic|Early Jurassic|Surat Basin. Lacustrine sediments. Seal for the Precipice Sandstone hydrocarbon reservoir. GSQ Chinchilla 4 and Roma 8 core logs detailed (Appendix 4 & 5). The authors argue that at least part of the lowest c.58m of this unit, ie below the Boxvale Sandstone Member, should be assigned to the Precipice Sandstone. Palynology detailed. Data from sections from well completion reports are included in Appendix 1.|||Boxvale Sandstone, Westgrove Ironstone, Members.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|69681|5|Briefly described|p74-87|Early Jurassic|Early Jurassic|Yields oil in the Moonie field. Most of the core samples used for this study are from this unit and the Precipice Sandstone. Regarded as a seal for Precipice Sandstone CO2 geostorage.||||Overlies Precipice Sandstone.|Mainly interbedded sandstones, siltstones and shales.|
6416|Evergreen Formation|69682|4|Described|p92-110|Early Jurassic|Early Jurassic|Surat Basin. Potential intraformational seal to CO2 reservoir. Up to 307m thick. Mineralogy discussed in detail.|||Includes Boxvale Sandstone Member and Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone.|Basal very fine to medium-grained sandstone, overlain by carbonaceous silt and mudstone, shale, oolitic ironstone and minor coal.|
6416|Evergreen Formation|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Eromanga Basin.|||Includes Westgrove Ironstone Member.|||
6416|Evergreen Formation|69946|6|Mentioned|p75|||||||||
6416|Evergreen Formation|69947|6|Mentioned|p23 Fig.7.12|||Surat Basin. Craton-derived sediments.||||||
6416|Evergreen Formation|70374|6|Mentioned|p809 figure 1|Bajocian|Pliensbachian|Surat Basin.|||Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||17-JAN-22
6416|Evergreen Formation|70628|6|Mentioned|p952 fig 4|Toarcian|Pliensbachian|Shown only as 'Evergreen' in fig 4. Along with Precipice Sandstone, forms part of the J-sequence (Hoffman et al 2009) of the Surat Basin.||||Overlies Precipice Sandstone. Underlies Hutton Sandstone.||
6416|Evergreen Formation|70821|5|Briefly described|p80|||Eromanga, Surat Basins.|||Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|71282|6|Mentioned|p457 Fig.1, p460|||Appears just as Evergreen in Fig.1.||||||
6416|Evergreen Formation|71342|6|Mentioned|Ch5 p74|||Surat Basin.||||||
6416|Evergreen Formation|71805|4|Described|p75-p79, p84, p86-p87|Toarcian|Toarcian|Eromanga Basin and northern Surat Basin. This unit is interpreted to have been deposited in a lacustrine or locally marine environment. In sequence stratigraphy of Hoffman et al (1997) the base of this unit is equivalent to S20 and the top S30. Placement of boundary with underlying Precipice Sandstone discussed.|||Includes Boxvale Sandstone Member and Westgrove Ironstone Member.|Conformably overlies the Precipice Sandstone. Overlain by the Hutton Sandstone.|Fine- to medium-grained, lithic, argillaceous sandstones, carbonaceous shales, siltstones and rarer thin discontinuous coal bands.|16-MAY-19
6416|Evergreen Formation|71806|4|Described|p483-p486, p500|Jurassic|Jurassic|Surat Basin. This unit is alluvial to lacustrine. Displays some evidence of marine influence including chamositic oolite layers, wavy to symmetrical ripples and brackish-tolerant acritarchs.|||Westgrove Ironstone Member and Boxvale Sandstone Member.|Overlies the Precipice Sandstone.||
6416|Evergreen Formation|72297|5|Briefly described|p712, p726, p745, p748|Early Jurassic|Early Jurassic|Surat-Mulgildie Basins. Iron deposits occur at Dawsonvale in the Mundubbera area. Is quarried for dimension stone (various applications listed) at Einsvold. Fair to good potential hydrocarbon source rock. Produced gas at the Grafton Range gasfield. Seal for Precipice Sandstone reservoirs; traps are structural-stratigraphic (briefly described),|||Boxvale Sandstone Member.||Grey to dark grey shales and mudstones; oolitic ironstone occurs in two distinct subunits in flat-lying sandstone.|
6416|Evergreen Formation|72298|5|Briefly described|p801|Jurassic|Triassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW).|||Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|72921|4|Described|p8, 9-10, p15-17, p20, 21 Fig.7, p23.|Early Jurassic|Early Jurassic|Of Surat Basin in Queensland. Forms a regional seal above the Precipice Sandstone reservoir, but lithology is vertically and lateraly variable. Shows evidence of marine influence. Shallow marine to lacustrine. Evergreen Formation and its correlatives are found across the Clarence-Moreton, Surat and Eromanga Basins. See also p23 Fig.9, p28, p32, p35, p42, p45, p48-p52, p54 Fig.29, p63, p66.|||Includes Westgrove Ironstone Member, Boxvale Sandstone Member|Conformably overlies Precipice Sandstone and underlies Hutton Sandstone with transitional contact.|Includes acritarchs, proximal and distal deltaic deposits, tidal bundles, chamositic oolites, pelecypods, anoxic black shales and tempestites.|
6416|Evergreen Formation|73113|5|Briefly described|p. 3, 19, 22-24, 31, 36-37, 41, 46...|||Surat Basin. Includes the Boxvale Sandstone [Boxvale Sandstone Member]. Groundwater model divides unit into upper and lower layers separated by the Boxvale Sandstone. Tight aquitard. More locations: p. 49, 60, 67, 69, 78-80, 87-88, 98, 115-116, 119, 148, 152-153, 171-172, 191.||||Underlain by Precipice Sandstone. Overlain by Hutton Sandstone.||
6416|Evergreen Formation|73147|6|Mentioned|p127|Early Jurassic|Early Jurassic||||Westgrove Ironstone Member|||
6416|Evergreen Formation|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
6416|Evergreen Formation|73393|6|Mentioned|p19-22|Toarcian|Pliensbachian|Surat and Eromanga Basins. An almost complete Jurassic tetrapod amphibian, Siderops kehli, was recovered from this unit (Kolane cattle station, SE QLD) along with two partially articulated freshwater plesiosaur specimens.|||Westgrove Ironstone Member|Underlain by Precipice Sandstone. Overlain by Hutton Sandstone.|Contains oolitic ironstone.|
6416|Evergreen Formation|73600|4|Described|p189-192, p194-203, p205|Toarcian|Pliensbachian|Surat Basin. Maximum thickness of ca 300 m. Gradational lower boundary. Palynology was previously used for biostratigraphic age constraint. Two new CA-TIMS zircon ages of 179.91 +/- 0.06 Ma and 184.61 +/- 0.33 Ma from tuffs; these corroborate palynological interpretations. A U-Pb detrital zircon age of 176.6 +/- 2.0 Ma was reported by Todd et al. (2019). Various detrital zircon maximum depositional ages are presented, which support the CA-TIMS tuff age. Complex sediment sourcing dominated by the Thomson Orogen. The presence of glauconite suggests marine influence.|179.91 +/- 0.06 Ma U-Pb CA-TIMS||Westgrove Ironstone Member, Boxvale Sandstone Member|Conformably underlain by Precipice Sandstone. Overlain by Hutton Sandstone.|Fine-grained sandstones and mudstones. Contains scattered tuffs.|
6451|Eyre Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146, p151|Tertiary|Tertiary|Lake Eyre Basin.||||Unconformably overlies the Mount Howie Sandstone and the Winton Formation. Unconformably overlain by the Namba Formation.|Fluvial sandstone with a basal conglomerate.|
6451|Eyre Formation|22442|6|Mentioned|p54|Tertiary|Tertiary|||||||
6451|Eyre Formation|22495|6|Mentioned|P222|Eocene|Paleocene|||||||
6451|Eyre Formation|22587|4|Described|p71|Middle Eocene|Paleocene|||||||
6451|Eyre Formation|22671|6|Mentioned|Fig2p837|Tertiary|Tertiary|Sandstone sediments.||||||17-JAN-06
6451|Eyre Formation|22700|6|Mentioned|p775|Tertiary|Tertiary|Of Thomson Fold Belt.||||||18-SEP-06
6451|Eyre Formation|22712|5|Briefly described|p132|Tertiary|Tertiary|||||||
6451|Eyre Formation|22730|4|Described|p557,66,67|Eocene|Paleocene|After Wopfner 1974.||||||18-SEP-06
6451|Eyre Formation|22773|5|Briefly described|p355|||||||||
6451|Eyre Formation|22857|5|Briefly described|p355|Middle Eocene|Paleocene|Thickness: ~30m in SA borehole near border. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|22912|5|Briefly described|32|||Geol province Lake Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|23154|5|Briefly described|Map Legend|Middle Eocene|Late Paleocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
6451|Eyre Formation|23155|4|Described|p33|Tertiary|Tertiary|Location of type section is advised p33. Unit does not crop out on STRZELECKI, but is present over all of the area. Overlying unit - Namba Formation (disconformity).  Underlain by Winton Formation (disconformity).||||||03-MAY-13
6451|Eyre Formation|23224|5|Briefly described|p3|Eocene|Paleocene|May correlate to Tertiary cover over White Cliffs Opal fields.||||||07-MAR-06
6451|Eyre Formation|23336|6|Mentioned|4|||||||||
6451|Eyre Formation|23339|5|Briefly described|4|Tertiary|Tertiary|||||||
6451|Eyre Formation|23380|5|Briefly described|p107-108|Eocene|Paleocene|||||||
6451|Eyre Formation|23477|5|Briefly described|p49 Fig 3|Tertiary|Tertiary|Geological Province: Curnamona Province.||||||
6451|Eyre Formation|23478|5|Briefly described|p28|Eocene|Paleocene|||||||
6451|Eyre Formation|23889|5|Briefly described|p18|Paleogene|Paleogene|||||||07-NOV-08
6451|Eyre Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6451|Eyre Formation|24175|3|Fully described|p32, p32 Fig. 6|Eocene|Paleocene|Unconformably overlain by Etadunna Formation. Max. thickness: ~100 m. Geological Province: Lake Eyre Basin.||||||03-MAY-13
6451|Eyre Formation|24176|5|Briefly described|p19, p22 Tb. 1|Tertiary|Tertiary|Freshwater sands and gravels - calcareous sandstone, quartzite; agate, quartz and chert pebbles. Corresponds to the Murnpeowie Formation defined by Forbes (1966).||||||26-NOV-08
6451|Eyre Formation|24204|5|Briefly described|p263 Fig.4|Tertiary|Tertiary|Geological Province: Eyre Basin.||||||
6451|Eyre Formation|24321|5|Briefly described|Map legend|Early Eocene|Late Paleocene|Geological Province: Lake  Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|24345|5|Briefly described|p82, 84-85 Fig.2|Eocene|Paleocene|||||||
6451|Eyre Formation|29658|6|Mentioned|p5|||||||||
6451|Eyre Formation|29660|6|Mentioned|p4|||||||||
6451|Eyre Formation|30054|5|Briefly described|p803|||||||||
6451|Eyre Formation|30055|6|Mentioned|p160|||||||||
6451|Eyre Formation|30056|6|Mentioned|p125|||See also p129, p134.||||||18-SEP-06
6451|Eyre Formation|30176|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6451|Eyre Formation|30540|6|Mentioned|Fig.6|||||||||
6451|Eyre Formation|30804|4|Described|p12|||Lithology. See also Table 1||||||
6451|Eyre Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
6451|Eyre Formation|30919|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30920|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6451|Eyre Formation|31850|6|Mentioned|p33|||||||||
6451|Eyre Formation|32121|6|Mentioned|p422|||||||||
6451|Eyre Formation|32275|6|Mentioned|p9|||||||||
6451|Eyre Formation|33568|6|Mentioned|p48|||||||||
6451|Eyre Formation|33820|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33821|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33822|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33823|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
6451|Eyre Formation|33824|6|Mentioned|p7|||See also p12, Tables 1 and 2.||||||18-SEP-06
6451|Eyre Formation|33825|5|Briefly described|p8|||Strat. table. Lithology||||||
6451|Eyre Formation|33827|5|Briefly described|p14|||See also Table 1||||||
6451|Eyre Formation|33828|6|Mentioned|p11|||Table 1||||||
6451|Eyre Formation|33831|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33832|6|Mentioned|p6|||Strat.||||||
6451|Eyre Formation|33937|6|Mentioned|p1|||||||||
6451|Eyre Formation|33938|2|Defined|p18|early Tertiary|early Tertiary|||||||
6451|Eyre Formation|33971|6|Mentioned|p37|||Strat. section Fig. 15.||||||
6451|Eyre Formation|34882|6|Mentioned|Fig. 1|||||||||
6451|Eyre Formation|35187|6|Mentioned|Table1|||||||||
6451|Eyre Formation|35793|6|Mentioned|p237|||||||||
6451|Eyre Formation|36554|6|Mentioned|p1647|||||||||
6451|Eyre Formation|36618|5|Briefly described|Table 1|||||||||
6451|Eyre Formation|36620|5|Briefly described|Fig.1|||See also p24.||||||18-SEP-06
6451|Eyre Formation|36922|6|Mentioned|Fig.3|||||||||
6451|Eyre Formation|36966|6|Mentioned|p81|||||||||
6451|Eyre Formation|37062|6|Mentioned|p182|||||||||
6451|Eyre Formation|37607|6|Mentioned|p333|||See also Fig.4.||||||
6451|Eyre Formation|37776|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|38022|6|Mentioned|p29|||||||||
6451|Eyre Formation|38226|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|38557|5|Briefly described|p291|||||||||
6451|Eyre Formation|38605|6|Mentioned|p35|||||||||
6451|Eyre Formation|38740|5|Briefly described|p306|||||||||
6451|Eyre Formation|39084|6|Mentioned|p22|||||||||
6451|Eyre Formation|39085|6|Mentioned|p13|||||||||
6451|Eyre Formation|39087|6|Mentioned|p15|||||||||
6451|Eyre Formation|39322|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|39352|6|Mentioned|Map legend|Miocene|Paleocene|Miocene to Palaeocene||||||
6451|Eyre Formation|39445|5|Briefly described|Table 14|||See also Fig.11.2||||||
6451|Eyre Formation|39478|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|39949|6|Mentioned|p274|||||||||
6451|Eyre Formation|40220|6|Mentioned|p7|||||||||
6451|Eyre Formation|40395|6|Mentioned|p313|||||||||
6451|Eyre Formation|40595|6|Mentioned|p93|||||||||
6451|Eyre Formation|40756|6|Mentioned|p1|||||||||
6451|Eyre Formation|40757|6|Mentioned|p75|||||||||
6451|Eyre Formation|40910|6|Mentioned|p17|||||||||
6451|Eyre Formation|40911|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene-Eocene||||||
6451|Eyre Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40926|3|Fully described|p22|||||||||
6451|Eyre Formation|40950|6|Mentioned|p250|||||||||
6451|Eyre Formation|40982|6|Mentioned|p363|||||||||
6451|Eyre Formation|41085|6|Mentioned|Fig.8|||||||||
6451|Eyre Formation|41098|4|Described|p177|||||||||
6451|Eyre Formation|41125|6|Mentioned|p34|||||||||
6451|Eyre Formation|41165|5|Briefly described|p364|||Mention  Fig.21||||||
6451|Eyre Formation|41184|6|Mentioned|p347|||||||||
6451|Eyre Formation|41198|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|41517|6|Mentioned|p140|||||||||
6451|Eyre Formation|41535|6|Mentioned|p368|||||||||
6451|Eyre Formation|41600|6|Mentioned|p816|||||||||
6451|Eyre Formation|42084|6|Mentioned|Fig.3 P356|||||||||
6451|Eyre Formation|42090|3|Fully described|p14|||See also Table 2.||||||18-SEP-06
6451|Eyre Formation|42340|5|Briefly described|p25|Eocene|Late Paleocene|||||||07-NOV-08
6451|Eyre Formation|42375|3|Fully described|p21-25, p29|early Oligocene?|Paleocene|Geological province: Birdsville Basin.||||||18-SEP-06
6451|Eyre Formation|42469|5|Briefly described|p35, p43, p44|||||||||
6451|Eyre Formation|42475|6|Mentioned|p20|||Birdsville Basin||||||
6451|Eyre Formation|42496|5|Briefly described|Fig.3 P132|||||||||
6451|Eyre Formation|42508|5|Briefly described|p66, p74|||||||||
6451|Eyre Formation|42541|6|Mentioned|p220|||||||||
6451|Eyre Formation|42543|5|Briefly described|Fig.4 P6|||||||||
6451|Eyre Formation|42592|5|Briefly described|Fig. 4 P270|||||||||
6451|Eyre Formation|42746|4|Described|p13|||See also Fig.2, Fig.9||||||
6451|Eyre Formation|42905|5|Briefly described|p23|||see also Fig.5.3||||||
6451|Eyre Formation|42957|6|Mentioned|p40|||||||||
6451|Eyre Formation|42999|6|Mentioned|p98|||||||||
6451|Eyre Formation|43035|5|Briefly described|p27|||||||||
6451|Eyre Formation|43048|5|Briefly described|p22|||||||||
6451|Eyre Formation|43052|5|Briefly described|Table 2.1|||||||||
6451|Eyre Formation|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||25-MAY-05
6451|Eyre Formation|43071|5|Briefly described|p17|||||||||
6451|Eyre Formation|43094|5|Briefly described|p38|||||||||
6451|Eyre Formation|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|44041|6|Mentioned|p242|||||||||
6451|Eyre Formation|44133|4|Described|p192, 124, 190 Fig. 10.30|Middle Eocene|Late Paleocene|Geological Province: Lake Eyre Basin. Includes the Macumba Sandstone, Murnpowie Formation. Overlain unconformably by the Etadunna and Namba Formations.||||||
6451|Eyre Formation|44934|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6451|Eyre Formation|45145|6|Mentioned|Table 7|||||||||
6451|Eyre Formation|46800|4|Described|p112|||See also p114.||||||18-SEP-06
6451|Eyre Formation|46802|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|46833|6|Mentioned|p53|||||||||
6451|Eyre Formation|46854|6|Mentioned|p242|||||||||
6451|Eyre Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6451|Eyre Formation|46911|5|Briefly described|p113|||Analyses of weathered profiles and parent rocks.||||||
6451|Eyre Formation|60648|6|Mentioned|p42|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|60955|5|Briefly described|Map Legend|Miocene|Eocene|Carbonaceous sandstones, siltstones, mudstones.||||||
6451|Eyre Formation|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61155|5|Briefly described|p2, p17|Middle Eocene|Late Paleocene|Sediments spread in thin sheets over large areas of the Birdsville Basin. Age: ~62-~42Ma. Max. thickness: 120m (in Lake Eyre Basin). Geological province: Oodnadatta area, Lake Eyre Basin and Tarkarooloo Basin.||||||03-MAR-10
6451|Eyre Formation|61823|5|Briefly described|p118|Middle Eocene|Paleocene|Overlain by Namba Formation. Age is Palaeogene.  Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61824|5|Briefly described|p128|Paleogene|Paleogene|Age is uncertain - it is also suggested that the rocks may be Mesozoic.||||||07-NOV-08
6451|Eyre Formation|61825|5|Briefly described|p138|Late Cretaceous|Late Cretaceous|Quartz and kaolin-rich sediments.  Overprinted by the "Cordillo Silcrete".  Geological Province:  Eromanga Basin.||||||
6451|Eyre Formation|62376|5|Briefly described|p84|Tertiary|Tertiary |Geological Province: Pedirka Basin.||||||09-FEB-10
6451|Eyre Formation|62724|5|Briefly described|p16 Fig. 2|Tertiary|Tertiary|Sandstone. Geological Province: Curnamona Province.||||||07-FEB-11
6451|Eyre Formation|63102|4|Described|p8,62,67,71,73|Late Eocene|Late Paleocene|Geological province: Curnamona Province. Of Callabonna Sub-basin. Deposited in palaeochannels incised into weathered basement rocks in the area north of the Ranges but occurs as a more widespread sheet facies further to the north. Southern channelled facies sourced from erosion of weather basement rocks in the Olary Domain and is dominated by clay (kaolinite) mineralogy.||||Overlain by Namba Formation.|Carbonaceous sand; very fine to coarse, moderately sorted, subrounded to subangular, with minor clay lenses.|
6451|Eyre Formation|63789|5|Briefly described|Map Legend|Tertiary|Tertiary|Predominatly coarse-grained quartozse sandstone, derived in part fom decayed granites with lesser fine sandstone and fine conglomeratic lenses with highly polished pebbles including fossil wood.||||||
6451|Eyre Formation|63793|5|Briefly described|p30, p49.|Eocene|Paleocene|Earliest Tertiary; apparently locally derived.|||||Soft, white, friable, flat-lying, gritty sandstones.|
6451|Eyre Formation|64047|5|Briefly described|p60, p61|Middle Eocene|Late Paleocene|Broad correlation with Marion Formation is indicated.  Upper section is probably equivalent to Glendower Formation.||||||
6451|Eyre Formation|64197|6|Mentioned|p627, p630 Fig.6|Late Eocene|Late Palaeocene|||||Unconformably overlies the Winton Formation. Is overlain unconformably by Etadunna Formation.||
6451|Eyre Formation|64679|5|Briefly described|Map legend|Tertiary|Tertiary|Quartz sandstone, siltstone, claystone and conglomerate; commonly silicified.||||||11-AUG-09
6451|Eyre Formation|64682|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone and silty or clay rich sandstone.||||||
6451|Eyre Formation|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
6451|Eyre Formation|64964|5|Briefly described|p160|Eocene|Paleocene|Thickness: 80m. Comprises fine-grained brown sandstone and clay with some boulders of Devonian sandstone. No fossils apart from a few worm burrows.||||||08-APR-09
6451|Eyre Formation|65194|5|Briefly described|p44-50|Eocene|Eocene|Fluvial sands. Overlain by Namba Formation. Fining-upward, braided-river sequences of angular, quartz-rich, poorly sorted sands interbedded with kaolinitic clays.||||||
6451|Eyre Formation|65238|5|Briefly described|p7 Fig. 8|Tertiary|Tertiary |Geological province: Eyre Basin. Fluvial and aeolian deposits.||||||
6451|Eyre Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 191 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Winton Formation.|Carbonaceous sandstone, siltstone, mudstone.|
6451|Eyre Formation|65484|5|Briefly described|p 28, 30, Fig 2|Tertiary|Tertiary|Tectonically  tilted exposure, laterally equivalent to sediments hosting Four Mile mineralisation. Later stages include silcrete development.||||||01-MAY-15
6451|Eyre Formation|65489|6|Mentioned|p60|||||||Unconformably overlies Winton Formation.||
6451|Eyre Formation|65925|4|Described| pp16-21, p47-69,  p139, Appendix 2.|Eocene|Latest Paleocene|Callabonna Sub-basin. Organic-rich sands host uranium deposits. Basal unit of Lake Eyre Basin. Fills a network of paleochannels.|Two-stage deposition: c.55-49 Ma and c.45-37 Ma.||Includes Murnpeowie Formation.|Unconformably overlies Bulldog Shale. Is disconformably overlain by Namba Formation.|Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Has silcrete cap. Braided streams.|
6451|Eyre Formation|66131|4|Described|p240-245, p248-253, p255, p258-259|Eocene|Paleocene|Widespread throughout Lake Eyre Basin. Latest Paleocene to Middle Eocene age based on palynological dating. ~100m thick. Plant fossils widespread. Largely deposited by braided streams.||||Correlative of the Glendower and Marion Formations. Equivalent to Mount Sarah Sandstone. Overlain by the Etadunna and Doonbarra Formations. Disconformably overlain by the Namba Formation.|Sandstone, carbonaceous clays and conglomerates. Lignite and clay, sometimes with root horizons, leaf beds and cross-bedding, are common. Diagnostic basal polished gravel.|
6451|Eyre Formation|66303|6|Mentioned|pp27-28, p31 Fig.5.|Paleogene|Paleogene|Lake Eyre Basin. Early Late Paleocene (Lygistepollenites balmei Zone) to Early Oligocene (Upper Nothofagidites asperus Zone). Uplifted, eroded and redeposited from Late Paleocene to Late Eocene. ||||Overlies Bulldog Shale. Is disconformably overlain by Namba Formation.||
6451|Eyre Formation|66518|5|Briefly described|p19 Fig.4, p20.|Cenozoic|Cenozoic|Basal unit in the Callabonna Sub-basin within Lake Eyre Basin. Fluvial sediments and alluvium. ||||Unconformably underlies Namba Formation.||
6451|Eyre Formation|66573|5|Briefly described|p873, p874 Fig.5, p875 Tb.2|Eocene|Paleocene|Disconformably overlain by the Etadunna Formation. Red claystones and silcretized sandstones.||||||
6451|Eyre Formation|66623|3|Fully described|p239, p248, pp268-276.|Eocene|Late Paleocene|Formerly Eyrian Series (Woolnough and David 1926). Equivalent to Glendower and Marion Formations; partly to Mount Sarah and Willalinchina Sandstones. Contains small polished erratic pebbles from underlying Cretaceous sequence. More strongly silicified sandstones are mapped as Cordillo Silcrete. Forms regional angular unconformity over variety of Cretaceous basement rocks. Top of this formation is marked by a palaeosol (Cordillo Surface, Wopnfer 1974) with silcrete cap (Cordillo Silcrete, Wopnfer 1978). Erosion of silcrete cap and Eyre Formation formed the overlying Doonbara Formation.|||In South Australia, incorporates Murnpeowie Formation and Macumba Sandstone.|Locally unconformably overlies Namur Sandstone and Easter Monday Formation. Grades upwards into Cordillo Silcrete. Is overlain unconformably by Doonbara Formation.|Sequence of mature quartz sandstones with local beds and laminae of distinctive and diagnostic, highly glossy, well-rounded, low-sphericity discoidal quartz pebble conglomerate  with subordinate black chert, yellow agate and silicified wood.|30-MAY-13
6451|Eyre Formation|66917|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66920|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66921|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67119|5|Briefly described|Map legend.|Eocene|Paleocene|Braided stream deposits.|||||Pyritic, carbonaceous sand, silt- to small cobble-sized grains, with beds of lignite and clay (montmorillonite, kaolinite and illite).|
6451|Eyre Formation|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|19-SEP-11
6451|Eyre Formation|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|20-SEP-13
6451|Eyre Formation|67209|5|Briefly described|Map legend.|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.||||Overlies Rolling Downs Group.|Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67462|5|Briefly described|Map legend.|Paleogene|Paleogene|Lake Eyre Basin.||||||
6451|Eyre Formation|67562|6|Mentioned|p105 Fig.11|Eocene|Eocene||||||Kaolinitic fine-grained sandstone.|
6451|Eyre Formation|67578|5|Briefly described|p333-334, p336-337, p341-342, p344, p347|Eocene|Paleocene|Birdsville Basin. Multi-channel or braided stream deposits. Upper part widely affected by post-depositional silicification.||||Unconformably overlies Bulldog Shale.|Yellow and yellow-orange cross-bedded sands and thin grey-brown silty-clay.|
6451|Eyre Formation|68068|5|Briefly described|Map legend|Middle Eocene|Late Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Gravel clasts include quartz, chalcedony, silicified wood, silcrete; occasional leaf impressions, often lignitic in drill sections. Commonly silcreted.||||Overlies Mulligan Dam Regolith.|Basal gravel of highly-polished well-rounded clasts, consolidated but not cemented; fluvial quartz sand, rounded to angular, fine- to coarse-grained, grit beds common, occasional laminated lacustrine silt and clay.|
6451|Eyre Formation|68157|6|Mentioned|p1, p13-16|Paleogene|Paleogene|Hosts Four Mile East, Honeymoon and Goulds Dam sandstone-hosted uranium deposits. Includes detrital zircons aged ~1.58 Ga, ~900 Ma and ~485 Ma.|||||Includes coarse-grained sandstone.|
6451|Eyre Formation|68203|6|Mentioned|p9 Fig.6|||Mount Lofty Ranges.||||Is faulted against Willawortina Formation.||
6451|Eyre Formation|68713|6|Mentioned|p23||||||||Fluvial-paludal sediment dominated by fine-grained quartz sand and silt, and has been overprinted by groundwater silcrete.|
6451|Eyre Formation|68715|6|Mentioned|p29, p31, p32 Fig.6|Paleogene|Paleogene|Lake Eyre Basin. Fluvial and aeolian deposits.||||Is overlain unconformably by Namba Formation.||07-APR-17
6451|Eyre Formation|68821|3|Fully described|p296, p297 Fig.3, p307, p310|Lutetian|Danian|< 120 m thick. Fluvial and locally lacustrine sedimentary rocks. Locally abundant wood fragments, and contains large trunks of fossil trees.|62 - 42 Ma|||Locally overlain by the Etadunna Formation and Namba Formation. Unconformably underlain by the Bulldog Shale Formation, Oodnadatta Formation, and Winton Formation.|Includes conglomerate, pyritic mature quartz sandstone with interbeds of clay lenses (44% kaolinite) and shale pebbles, carbonaceous and micaceous siltstone, dolomitic siltstone and lignite.|03-OCT-13
6451|Eyre Formation|69001|5|Briefly described|p2 Fig.1B, p16, p18 Fig.8, p22 p23|Eocene|Paleocene|Late Paleocene to Middle Eocene age. Fluvial sediments. Previously incorrectly correlated with the Gum Vale Beds and Gum Vale Formation.|||||Comprises dominantly fluvial sandstone, carbonaceous clastics and quartzose conglomerates.|
6451|Eyre Formation|69019|4|Described|p83, p94, p104-110 Figs.20,24-26.|Eocene|Paleocene|Of Wopfner et al. (1974) after the term 'Eyrian Series' of Woolnough and David (1926); also previously known as Murnpeowie Formation (Forbes, 1966). Extensive sandy flood plain deposits. Thickness from <10 to >170 m. Has developed silcrete-porcellanite horizons. Of interest to explorers for biogenic coal seam gas. See also Pl.20, p119.||||Disconformably overlies Winton Formation. Is overlain unconformably by Namba and Etadunna Formations. Faulted against Marree Subgroup.|Well-washed, mature, moderately sorted quartz sand; grit beds common; comnmonly carbonaceous and pyritic, with lignite interbeds towards the base.|
6451|Eyre Formation|69023|4|Described|p79, p87, p101, p105-106, p108-120|Eocene|Paleocene|See also p122-123, p125, p143-144, p153, p162-163, p193. Defined by Wopfner et al. (1974); previously Eyrian Series of Woolnough and David (1926), and Murnpeowie Formation of Forbes (1966). Seven reference areas are described in the definition; two are mentioned here. Lake Eyre Basin. c.62m thick. Plant matter is commonly preserved. A measured section is provided. Deposited as a widespread fluvial sand sheet. Weathering has formed porcellanite and a silcrete cap. Probable source (with Namba Formation) of Yandruwantha Sand. Potential supply of construction sand and road gravel. Stratigraphic wells intersection data.||||Conformably overlies Mulligan Dam Regolith. Disconformably overlies Winton Formation or Bulldog Shale. Is overlain unconformably by Namba Formation.|Black, grey and brown coloured. Well-washed, mature, fine- to medium-grained, moderately sorted sand with subrounded grains; commonly carbonaceous and pyritic; interbeds of lignite towards the base. Local silcrete and calcite cemented zones.|
6451|Eyre Formation|69458|5|Briefly described|p42:16|Eocene|Paleocene|Lake Eyre Basin. Extensive shallow, braided stream system deposits with local swamp and lake settings.|||||Basal conglomerate with highly polished, resistant pebble clasts overlain by cross-bedded, mature pyritic and carbonaceous coarse-grained sandstone; lignite and clay units, containing plant fossils, occur.|12-JUL-16
6451|Eyre Formation|69562|5|Briefly described|p662 Tb.2, p663 Fig.2, p664 Tb.4|Eocene|Paleocene|See also p666 Fig.3, p667 Fig.4, p668-669, p674-676, p679-684. Lake Eyre Basin. Deposition in paleovalleys. Hosts more than 90% of known (U) mineralisation in Lake Frome area; highly permeable sands: 5 sq.m/day measured. Rich in organic material (plants and pyrite) for reductants. Electrical conductivity value used in forward modelling: 200-500 mS/m.|c.55 Ma.|||Overlies Marree Subgroup. Is overlain by Namba Formation.|Mature, fine- to coarse-grained, unconsolidated, carbonaceous, pyritic sands; occasional lignitic sandy lenses near the base.|06-APR-22
6451|Eyre Formation|69568|5|Briefly described|p441, 443-444|Eocene|Paleocene|Lake Frome region; basal Lake Eyre Basin. Hosts the Beverley North uranium deposits. Occurs in S-N paleochannels, commonly incised into underlying strata. Two depositional stages: ~55-49 Ma and ~45-37 Ma. Drill-core logs.||||Unconformably overlies Bulldog Shale. Is overlain disconformably by Namba Formation.|Dominantly fluvial and lacustrine deposits, characterised by pyritic carbonaceous mature sands of very fine to pebble size; includes coal seams; regionally capped by silcrete lenses.|
6451|Eyre Formation|69599|5|Briefly described|p584, p599-600|Eocene|Paleocene|Senior (1979) and Senior and Mabbutt (1979) included under this name all Eyre Formation equivalents in the SW corner of QLD; Draper (2002) excepted the Marion Formation. Capped by silcrete and laterite of the Canaway profile.||||Correlated (at least partly) with Moonie, Glendower, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||
6451|Eyre Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
6451|Eyre Formation|69946|5|Briefly described|p29, p125, p129|Eocene|Paleocene|Lake Eyre Basin. Wopfner et al. (1974). Up to 140m thick. Weathering down to 60m. Local Cordillo Silcrete caps produce prominent mesas.|||||Fluvial, fine- to medium-grained quartz sandstone with lignite interbeds and a basal conglomerate which includes reworked Late Cretaceous sediment.|
6451|Eyre Formation|69947|5|Briefly described|p13 Fig.7.2|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
6451|Eyre Formation|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70383|5|Briefly described|p45, p62|Paleogene|Paleogene|Lake Eyre Basin. Fluvial sediments.||||Is overlain by Namba Formation.||
6451|Eyre Formation|70384|5|Briefly described|Map legend.|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Dominantly a braided stream and floodplain deposit. Palynology age range: late Paleocene to middle Eocene. Rare leaf fossils in silt or clay layers; variably lignitic near base (+/- pyrite). Reddish horizons and silcrete mark paleosols.|||||Quartz sand, rounded to angular, fine- to coarse-grained; grit beds common, cross-bedded channel fill; occasional laminated lacustrine silt and clay; basal gravel with highly polished, well-rounded clasts. Consolidated, rarely cemented.|
6451|Eyre Formation|70649|5|Briefly described|Map Legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70651|5|Briefly described|Map Legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70652|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial sandstone. In-situ regolith and transported sediments also described.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70657|5|Briefly described|p9 Fig.3, p68, p72, p77-80|Neogene|Paleogene|Cover sequence in Olary Domain. Deposition in palaeochannels incised into weathered basement rocks, or as widespread sheet facies. Hosts roll-front U mineralisation (described) near the Benagerie Ridge. Late Eocene to late Paleocene.||||Is overlain by Namba Formation.|Sandstone; carbonaceous sand, fine to coarse, subrounded to subangular, and minor clay (mainly kaolinite) lenses.|
6451|Eyre Formation|70658|6|Mentioned|p14|Tertiary|Tertiary||||||Sandstone.|
6451|Eyre Formation|70821|5|Briefly described|p25|Eocene|Eocene|Previously the Eyre Gravel (eg Lovering et al., 1972) [misquoted as the Eyre gravel in this study]. Lake Eyre Basin (SA). Is equivalent to the dendritic ridges formed by the Glendower Formation in Queensland and NSW.|||||Silcrete and ferricrete.|
6451|Eyre Formation|70823|5|Briefly described|p46-p47|Middle Eocene|Paleocene|Interpreted to have been deposited in a braided stream fluvial setting.|||||Carbonaceous sand, silt and gravel with some lignite and clay beds.|
6451|Eyre Formation|71342|4|Described|Ch1 p6, Ch5 p29, Ch5 p130, Ch7 p13|Eocene|Paleocene|Lake Eyre Basin. Hosts a major confined aquifer. Deposited in a fluvial environment. Up to 140m thick in the Cooper region. ||||Overlain by the Cordillo Silcrete. Unconformably overlies the Winton Formation. Unconformably overlain by the Namba Formation.|Fine to medium-grained, quartz sandstone with lignite interbeds and a basal conglomerate.|
6451|Eyre Formation|71415|5|Briefly described|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
6451|Eyre Formation|72456|5|Briefly described|Map Legend|Eocene|Paleocene|Marree 1:250k map sheet. Deposited in a braided stream environment.|||||Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with bands of lignite and clay. Clays are montmorillite, kaolinite and illite.|
6451|Eyre Formation|72457|5|Briefly described|p91|Eocene|Palaeocene|Callabonna sub-basin.||||Is overlain by Namba Formation.|Fluvial sands and gravels.|
6451|Eyre Formation|72461|6|Mentioned|p24|Cenozoic|Cenozoic|||||||
6451|Eyre Formation|73090|6|Mentioned|p6|Eocene|Palaeocene|||||||
6451|Eyre Formation|73106|5|Briefly described|Map legend.|Eocene|Paleocene||||||Pyritic carbonaceous sand; grain size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Braided streams.|
6451|Eyre Formation|73188|6|Mentioned|p345|Eocene|Paleocene|Similar to North Maslin Sand.||||||
6451|Eyre Formation|73251|4|Described|p36-38, p40-48, p50-51, p53, p56-58, p62|Eocene|Eocene|Lake Eyre Basin (widespread), Callabonna Sub-basin (basal unit). Potential detrital U reductant and potential shallow hydrocarbon source rock. Sandstone hosts U mineralisation at Four Mile East, Goulds Dam, Honeymoon, Oban, and Pepegoona. Thermally sub-mature. Includes oil-prone organic facies. Depositional environments include non-marine, meandering fluvial, fluviolacustrine, peat swamp, and floodplains. Sediment recovery in drill holes was poor, especially where the sands are clean (clay-free). Thickness in drill holes ranges from ca 23 m to 45 m thickening eastwards. Contains Eyre [organic] facies 1, 2, and 3. [See article for organic petrology descriptions].||||Unconformably overlain by Namba Formation.|Amalgamated fine- to medium-grained quartz sandstone (both clean and carbonaceous), lignite and carbonaceous mudstone.|
6451|Eyre Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
6451|Eyre Formation|73479|5|Briefly described|p156 Fig.2|Paleogene|Paleogene|Lake Eyre Basin.||||Unconformably overlies Winton Formation, underlies Etadunna Formation|Fresh water coarse sand.|
6459|Eyrian Formation|23336|5|Briefly described|p5|Eocene|Eocene|Overlies Mulga Downs Group||||||21-MAR-06
6459|Eyrian Formation|33938|6|Mentioned|p19|||Refers Whitehouse (1954).||||||
6459|Eyrian Formation|43995|14|Not recorded|Tb.p9||Tertiary|||||||
6459|Eyrian Formation|44269|14|Not recorded|p18||Cenozoic|Early Cainozoic.||||||19-NOV-08
6459|Eyrian Formation|44509|14|Not recorded|p342-343|||||||||
6459|Eyrian Formation|44542|14|Not recorded|p30|||||||||
6459|Eyrian Formation|44587|14|Not recorded|p373-386|||Not listed on white card.||||||
6661|Finke Group|22566|6|Mentioned|p79|||Geological province - Warburton Basin||||||
6661|Finke Group|22760|5|Briefly described|p340|Late Devonian|Late Devonian|||||||
6661|Finke Group|22762|5|Briefly described|p376|||The distal equivalent of the Pertnjara Group.||||||
6661|Finke Group|22763|6|Mentioned|Fig 3 on p389|||||||||
6661|Finke Group|22824|6|Mentioned|p530|||||||||
6661|Finke Group|22825|6|Mentioned|Fig 1 on p542|||||||||
6661|Finke Group|22826|6|Mentioned|p576|||||||||
6661|Finke Group|23858|5|Briefly described|p916|||Geological Province: Amadeus Basin. Max. thickness: >1000 m.||||||
6661|Finke Group|24301|6|Mentioned|p22|||||||||
6661|Finke Group|24302|5|Briefly described|Map Legend|Devonian|Devonian|Includes the Horseshoe Bend shale. Geological Province: Amadeus Basin. Mistakenly shown as Ordovician, but map symbol and Explanatory Notes indicate Devonian age.||||||25-OCT-06
6661|Finke Group|29442|6|Mentioned|p103|||||||||
6661|Finke Group|30544|6|Mentioned|p46|||Devonian age||||||
6661|Finke Group|31566|6|Mentioned|p244|||Devonian||||||
6661|Finke Group|31567|4|Described|p273|||See also p274-293. Refers Wells et al. (1964, 1966, 1967, 1970).||||||18-SEP-06
6661|Finke Group|32640|6|Mentioned|p241|||||||||
6661|Finke Group|33832|6|Mentioned|p8|||Refers Wells et al. (1970) and Youngs (1973).||||||18-SEP-06
6661|Finke Group|33964|6|Mentioned|p5|||Correlation. Refers Wells et al.(1966).||||||
6661|Finke Group|33971|6|Mentioned|p46|||Strat. table.||||||
6661|Finke Group|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also p16.||||||18-SEP-06
6661|Finke Group|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
6661|Finke Group|35102|6|Mentioned|p4|||||||||
6661|Finke Group|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
6661|Finke Group|36751|6|Mentioned|p490|||||||||
6661|Finke Group|39565|6|Mentioned|p32|||||||||
6661|Finke Group|40642|6|Mentioned|p163|||||||||
6661|Finke Group|40910|6|Mentioned|p13|||||||||
6661|Finke Group|40911|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
6661|Finke Group|40926|6|Mentioned|p12|||||||||
6661|Finke Group|41018|6|Mentioned|Fig.1|||||||||
6661|Finke Group|41125|6|Mentioned|Fig.24|||||||||
6661|Finke Group|41708|6|Mentioned|Fig.1|||||||||
6661|Finke Group|42296|6|Mentioned|p44|||||||||
6661|Finke Group|42504|5|Briefly described|p80|||||||||
6661|Finke Group|42699|5|Briefly described|map legend|Devonian||||||||
6661|Finke Group|42940|5|Briefly described|Plate 2|Devonian|Devonian|Sandstone, shale, siltstone, conglomerate.  Age: 410-360Ma. Geological province: Amadeus Basin.||||||23-JAN-08
6661|Finke Group|43035|4|Described|p24|||||||||
6661|Finke Group|43052|5|Briefly described|Table 2.1|||||||||
6661|Finke Group|44133|4|Described|p43, 44|Carboniferous?|Late Devonian|Overlies: Mereenie Sandstone. Includes: Polly Conglomerate, Langra Formation, Horseshoe Bend Shale. Lateral equivalent to Pertnjara Group.||||||
6661|Finke Group|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Devon-Carbon.||||||
6661|Finke Group|44335|4|Described|p.11|Carboniferous|Devonian|Table 2. p.10, Dev-Carb.||||||
6661|Finke Group|44336|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-3. Dev-Carbon.||||||
6661|Finke Group|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
6661|Finke Group|44343|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carbon.||||||
6661|Finke Group|44393|4|Described|p.3,7,8,Tb.1|Carboniferous|Devonian|Correlated with Pertnjara Group. Dev-Carb.||||||
6661|Finke Group|44394|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
6661|Finke Group|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
6661|Finke Group|45041|4|Described|p103|||See also p104-111. Devonian||||||18-SEP-06
6661|Finke Group|45097|6|Mentioned|p28|||Approx. same age as Pertnjara Group.||||||
6661|Finke Group|47050|5|Briefly described|p240|||||||||
6661|Finke Group|48865|2|Defined|p.28-29||Paleozoic|On many pages. p.3-5,21,27,34,35,36,40,45,Fig.14,47-51,53,Pl.10,11. Includes Idracowra Sandstone, Horseshoe Bend Shale, Langra Fm, Polly Cong. (G53-5,6).||||||07-NOV-08
6661|Finke Group|48880|14|Not recorded|p.20|Carboniferous|Devonian|(map). Devn-Carb.||||||
6661|Finke Group|48890|4|Described|p.50-52|Carboniferous|Devonian|See also Tb.1, Tb.3, Fig.4, Pl.16. Dev - Carb.||||||
6661|Finke Group|48963|6|Mentioned|Plate 5|||||||||
6661|Finke Group|50372|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Amadeus Basin. Includes: Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.||||||
6661|Finke Group|60678|5|Briefly described|Map legend|Devonian|Devonian|Fine to medium quartz sandstone, minor siltstone and shale, pebble and boulder conglomerate.  Geological Province: Amadeus Basin.||||||11-JAN-05
6661|Finke Group|61154|5|Briefly described|p34|||Sedimentary succession. Onlaps the Musgrave basement. Geological Province: Amadeus Basin.||||||18-SEP-06
6661|Finke Group|62609|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, shale, siltstone, conglomerate. Underlies De Souza Sandstone.||||||14-AUG-06
6661|Finke Group|62620|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, shale, siltstone, conglomerate.||||||
6661|Finke Group|64334|5|Briefly described|p42|Devonian|Devonian|Deposition was synchronous with the main phase of the Alice Springs Orogeny.|||||Thick wedges of generally coarsening-upward non-marine clastic sediments.|
6661|Finke Group|64778|6|Mentioned|p13, 15-17, 19-21, 23, 32|Devonian|Devonian|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary.|390-354 Ma.|||||
6661|Finke Group|64809|6|Mentioned|p3 |||Southern Amadeus Basin.||||||
6661|Finke Group|65232|5|Briefly described|p10 Fig 9.|||Combined age for Finke Group and Pertnjara Group shown as Late Devonian to Late Carboniferous||||||09-FEB-10
6661|Finke Group|65233|5|Briefly described|p13|Devonian|Devonian|Overlain by Horsebend Shale. Max. thickness: 400m. Coarse alluvial facies.||||||07-FEB-11
6661|Finke Group|65309|4|Described|pp13-14, p16, pp18-20.|Frasnian|Givetian|Southeast Amadeus Basin. Interfingers with Pertnjara Group. A typical locally-sourced, upward-fining basin-fill sequence resulting from minor uplift from the Alice Springs Orogeny.|||Includes Polly Conglomerate, Langra Formation, Horseshoe Bend Shale and Idracowra Sandstone.|Unconformably overlies basement.||
6661|Finke Group|66589|6|Mentioned|p180|Late Devonian|Late Devonian|Case studies cited; not visited in the field by the authors of this study.||||||
6661|Finke Group|69436|6|Mentioned|p21:20|||Amadeus Basin. Deposited during a single pulse of exhumation early in the 450-300 Ma Alice Springs Orogeny.||||||12-JUL-16
6661|Finke Group|69438|5|Briefly described|p23:2-4, 20, 38, 40-42|Late Devonian|Late Devonian|This author claims that the name Finke River Sandstone was first used by Chewings (1914) [who in fact used the names Finke River sandstones and Finke River sandstones formation]. The current name, Finke Group, applies to the Devonian succession underlying the Pedirka and Eromanga Basins but overlying basement rocks of the Musgrave Province or older successions of the Amadeus Basin. Southeast and south-central Amadeus Basin. Sediment supply was from the S and SW (Musgrave province) for the lowest three Formations; the upper unit was supplied from the N (Arunta Region). Unfossiliferous; age not well constrained.|||Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.|Correlative of, and interdigitates with, Pertnjara Group.||12-JUL-16
6661|Finke Group|69449|5|Briefly described|p34:2 Fig.34.2; 34:5-7|Devonian|Devonian|Eastern Amadeus Basin, with equivalents in the western Warburton Basin that are just over 1000m thick. Synorogenic deposition in response to largely compressional deformation during the Alice Springs Orogeny.|||Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.|Overlies Mereenie Sandstone.||12-JUL-16
6661|Finke Group|69458|6|Mentioned|p42:8|Devonian|Devonian|Amadeus Basin.||||||12-JUL-16
6661|Finke Group|69606|6|Mentioned|p10|Devonian|Devonian|Amadeus Basin. ||||||
6661|Finke Group|69673|6|Mentioned|p67, p86, p149 fig 120||||||Includes Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone|Correlated with Pertnjara Group||
6661|Finke Group|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.|||Polly Conglomerate, Langra Formation, Idracowra Sandstone, Horseshoe Bend Shale.|||
6661|Finke Group|71342|6|Mentioned|Ch9 p3, Ch9 p9, Ch9 p11|Devonian|Devonian|Thermal history briefly described (Ch9 p3). See also Ch9 p16-p17, Ch9 p20.||||Unconformably overlies the Mereenie Sandstone. Unconformably overlain by the Crown Point and Purni Formations.||
6661|Finke Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
6661|Finke Group|73085|6|Mentioned|p1|late Devonian|late Devonian||||Horseshore Bend Shale / Idracowra Sandstone, Langra Formation, Polly Conglomerate|Equivalent to Pertnjara Group.||
6661|Finke Group|73281|6|Mentioned|Appendix (DIP)|Permian|Permian|[Also written as Finke Group?]. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
6695|Fitton Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Granite tillite in south-east.||||||
6695|Fitton Formation|22510|5|Briefly described|p38|||Age: Sturtian||||||
6695|Fitton Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
6695|Fitton Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group).||||||
6695|Fitton Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
6695|Fitton Formation|23411|6|Mentioned|Map Legend|||||||||
6695|Fitton Formation|23818|4|Described|p64 Fig.22, p65|Neoproterozoic|Neoproterozoic|Lowermost unit of the Yudnamutana Sub-Group. Max. thickness: ~10 000 ft. Overlying unit: Bolla Bollana Formation. Interfingers with the Bolla Bollana Formation.||||||
6695|Fitton Formation|24176|4|Described|p11, p25 Tb. 1|Adelaidean|Adelaidean|Of Yudnamutana Sub-Group (Umberatana Group).  Calc-silicate metasediments, quartzites, boulder beds.  Overlain by Bolla Bollana Formation.  Age is Sturtian.  Max. thickness: 2960m.  Geological Province: Mount Painter Province.||||||
6695|Fitton Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Overlain by Bolla Bollana Formation. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
6695|Fitton Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
6695|Fitton Formation|30177|4|Described|p71|||||||||
6695|Fitton Formation|30621|6|Mentioned|p501|||Precambrain glaciation - Stratigraphy.||||||
6695|Fitton Formation|30801|6|Mentioned|p5|||Table P5-6||||||
6695|Fitton Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
6695|Fitton Formation|30920|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
6695|Fitton Formation|32364|6|Mentioned|p17|||||||||
6695|Fitton Formation|32724|6|Mentioned|Fig.1|||Sturtian. Correlation||||||
6695|Fitton Formation|33474|6|Mentioned|Fig.2|||||||||
6695|Fitton Formation|34535|4|Described|p65|||See Fig.22||||||
6695|Fitton Formation|35255|6|Mentioned|Fig.7|||||||||
6695|Fitton Formation|36137|5|Briefly described|p11|||||||||
6695|Fitton Formation|36253|6|Mentioned|Fig.3-2|||||||||
6695|Fitton Formation|36733|6|Mentioned|Table 5|||||||||
6695|Fitton Formation|37932|5|Briefly described|p539|||||||||
6695|Fitton Formation|38157|6|Mentioned|Table IV|||||||||
6695|Fitton Formation|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
6695|Fitton Formation|41364|6|Mentioned|p152|||||||||
6695|Fitton Formation|41405|3|Fully described|p129|||||||||
6695|Fitton Formation|41647|5|Briefly described|p834|||||||||
6695|Fitton Formation|41770|6|Mentioned|Fig.1|||||||||
6695|Fitton Formation|42222|5|Briefly described|p16|||||||||
6695|Fitton Formation|43052|5|Briefly described|p183,Table 6.1|||of Yudnamutana Subgroup||||||
6695|Fitton Formation|65925|5|Briefly described|Appendix 2.||||||||Conglomerate; arkose, pebbly; quartzite, white, massive, interbedded with silty shale.|
6695|Fitton Formation|68068|5|Briefly described|Map legend|Sturtian|Sturtian|Adelaide Geosyncline.|||Includes Hamilton Creek Member.|Is overlain gradationally by Bolla Bollana Tillite.|Dark grey laminated siltstone, minor quartzite, sparse lithic clasts, gravel to cobble sized; has occasional beds and lenses of scapolitic and amphibolitic calc-silicate tillite and siltstone.|
6695|Fitton Formation|69019|4|Described|p41-45, p134, p144.|Neoproterozoic|Neoproterozoic|Of Coats (1962); revised by Preiss (1987) and Young and Gostin (1989). Flinders Ranges. Rests unconformably on crystalline basement. Thickness to c.1,500 m.  Early Sturtian age.||Basal unit in Yudnamutana Subgroup.|Includes Hamilton Creek Member.|Is overlain conformably by Bolla Bollana Tillite.|Mainly finely laminated to massive, grey to brownish-grey meta-siltstone; dropstones in lower part; bands and lenses of conglomerate, dolomitic sandstone, marble, calc-silicate and quartz sandstone.|
6695|Fitton Formation|69023|4|Described|p50, p61-62, p64-65, p77, p137, p146-147|Neoproterozoic|Neoproterozoic|Defined by Coats (1962). The type section was revised by Preiss (1987); an informally named 'member' was formally named Hamilton Creek Member by Young and Gostin (1989). Thickness from <600m to ~1500m. Early Sturtian age, based on stratigraphic grounds: no radiometric dating. Displays low relief to almost flat areas. Supplied by sulphide-bearing hot brine sea-floor emanations.||Unit in Yudnamutana Subgroup.|Includes Hamilton Creek Member.|Unconformably overlies Golden Pole and Con Bore Granites. Is overlain gradationally by Bolla Bollana Tillite.|Mainly finely-laminated to massive, grey to brownish-grey meta-siltstone; occasional dropstones in lower part; includes a stretched-boulder conglomerate and a calc-silicate tillite.|
6695|Fitton Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. The four facies are mapped separately. Age shown more specifically as Sturtian [Cryogenian].||Yudnamutana Subgroup.|Hamilton Creek Member.|Is overlain gradationally by Bolla Bollana Tillite.|Dark grey, laminated conglomeratic siltstone and diamictite; minor quartzite, sparse gravel to boulder dropstones. Quartzite conglomerate or tillite. Calc-silicate: sparse beds and lenses, scapolitic and amphibolitic diamictite or siltstone. Arkose.|21-JAN-19
6695|Fitton Formation|71237|2|Defined|p7, 8, 10, 17|||||||||
6695|Fitton Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Conglomerate, arkose, pebbly; quartzite, whit, massive, interbedded with silty shale.|
6733|Flaxman Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 620m.||Sherbrook Group.||Unconformably overlies Waarre Formation. Abuts Timboon Sandstone and Belfast Mudstone. Is overlain by Paaratte Formation.||
6733|Flaxman Formation|12796|4|Described|p457, p456 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Formerly "Flaxman Beds" (Bain 1961). Includes the Banoon Member. Overlain by Belfast Mudstone. Geological Province: Otway Basin.||||||30-JAN-08
6733|Flaxman Formation|22470|5|Briefly described|p13 Fig. 17|Turonian|Turonian|Of Sherbrook Group.||||||
6733|Flaxman Formation|22674|5|Briefly described|Fig.2 p719|Coniacian|Cenomanian|||||||
6733|Flaxman Formation|22875|3|Fully described|p38|Cenomanian|Cenomanian|Of the Sherbrook Group.||||||07-MAR-07
6733|Flaxman Formation|22932|6|Mentioned|22|||||||||
6733|Flaxman Formation|23818|5|Briefly described|p164|Late Cretaceous|Late Cretaceous|Overlain by Belfast Formation. Underlain by Waarre Formation. Geological Province: Otway Basin.||||||08-MAY-07
6733|Flaxman Formation|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group.  Geological Basin: Otway Basin.||||||
6733|Flaxman Formation|24284|6|Mentioned|p15 Fig.2|||Otway Basin.||||||02-DEC-04
6733|Flaxman Formation|24314|5|Briefly described|p61 Fig.2|Turonian||Geological Province: Otway Basin. Of the Sherbrook Group.||||||
6733|Flaxman Formation|24453|5|Briefly described|p809 Fig.2|Santonian|Coniacin|Of Sherbrook Group. Overlain by Belfast Mudstone, overlies Waare Formation. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|24551|6|Mentioned|p245|||Of the Sherbrook Group||||||
6733|Flaxman Formation|30576|5|Briefly described|Table 2|||||||||
6733|Flaxman Formation|30578|5|Briefly described|p7|||||||||
6733|Flaxman Formation|30580|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
6733|Flaxman Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||08-MAY-07
6733|Flaxman Formation|30905|6|Mentioned|Table 7.3|||||||||
6733|Flaxman Formation|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Wangerrip Group.||||||08-MAY-07
6733|Flaxman Formation|31036|1|Redefined|p200|early Tertiary|early Tertiary|See also p200, Table 9-1. Refers Black and Glenie (1965).||||||07-MAR-07
6733|Flaxman Formation|31424|4|Described|p19|||See also p7. Described from core.||||||07-MAR-07
6733|Flaxman Formation|32896|6|Mentioned|Encl.7.1.|||Upper Cretaceous.||||||08-MAY-07
6733|Flaxman Formation|33936|6|Mentioned|Fig.6|||||||||
6733|Flaxman Formation|34611|5|Briefly described|p164|||Upper Cretaceous||||||
6733|Flaxman Formation|34987|4|Described|p170|||||||||
6733|Flaxman Formation|35722|6|Mentioned|p3|||Stratigraphy.||||||
6733|Flaxman Formation|36913|6|Mentioned|p81|||||||||
6733|Flaxman Formation|40947|6|Mentioned|p4|||||||||
6733|Flaxman Formation|41016|5|Briefly described|p214|||||||||
6733|Flaxman Formation|41269|5|Briefly described|p245|||||||||
6733|Flaxman Formation|41642|4|Described|p244|||||||||
6733|Flaxman Formation|41701|6|Mentioned|Map legend|Cretaceous||||||||
6733|Flaxman Formation|41704|6|Mentioned|Fig.3|||||||||
6733|Flaxman Formation|41769|5|Briefly described|p12|||||||||
6733|Flaxman Formation|41868|6|Mentioned|p533|||||||||
6733|Flaxman Formation|42152|6|Mentioned|p13|||||||||
6733|Flaxman Formation|42318|6|Mentioned|Fig.2 P10|||||||||
6733|Flaxman Formation|42361|1|Redefined|p13|Cenomanian|late Albian|New type section proposed in Flaxmans 1, Victoria. Late Cretaceous (Late Albian to Cenomanian) age.||||||31-JAN-08
6733|Flaxman Formation|42524|5|Briefly described|Fig.3 P27|||||||||
6733|Flaxman Formation|42545|6|Mentioned|p19|||In the Otway Basin.||||||08-MAY-07
6733|Flaxman Formation|42555|5|Briefly described|p284|||||||||
6733|Flaxman Formation|42599|5|Briefly described|Fig.3 P614|||||||||
6733|Flaxman Formation|42827|4|Described|p244|||see also Table 7.12||||||
6733|Flaxman Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
6733|Flaxman Formation|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 85-90 Ma.||||||08-MAY-07
6733|Flaxman Formation|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
6733|Flaxman Formation|43208|5|Briefly described|map legend|Coniacian|Cenomanian|Of Sherbrook Group.||||||
6733|Flaxman Formation|43590|4|Described|p13|Santonian|Cenomanian|||||||
6733|Flaxman Formation|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
6733|Flaxman Formation|43744|6|Mentioned|Fig.3,p3|||||||||
6733|Flaxman Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
6733|Flaxman Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
6733|Flaxman Formation|43814|6|Mentioned|Fig.3,p115|||||||||
6733|Flaxman Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
6733|Flaxman Formation|44133|5|Briefly described|p146|Santonian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin. Thickness: 619m.||||||
6733|Flaxman Formation|49060|5|Briefly described|Fig.33|||||||||
6733|Flaxman Formation|61016|6|Mentioned|p13|||Geological Province: Otway Basin.||||||20-APR-05
6733|Flaxman Formation|61017|5|Briefly described|p5 Fig. 2, p6|Coniacian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
6733|Flaxman Formation|61182|3|Fully described|p16, p160-161|Santonian|Cenomanian|Supersedes Flaxman Beds. Of Sherbrook Group. Conformably overlies Waarre Formation; conformably overlain by Belfast Mudstone. Geol.Prov: Otway Basin. Mudstone, siltstone, fine- to coarse-grained sandstone; ironstone, siderite, dolerite, thin coal present.||||||04-FEB-08
6733|Flaxman Formation|61230|5|Briefly described|p317, pp325-326, pp329-342.         |Late Turonian|Late Turonian|Of the Otway Delta. Delta front to prodelta conditions. TOC values vary from high to very high.||Unit in Sherbrook Group.||Overlies the Waarre Formation. Is overlain by Belfast Mudstone (Formation).|Dark grey mudstone with a significant (3 - 15%) sand fraction; glauconitic; granule-sized sand grains, mollusc debris and woody material occur occasionally in lower 100 m.|
6733|Flaxman Formation|61470|5|Briefly described|p28 Fig. 5|Coniacian|Turonian|Of the Sherbrook Group. Overlies Waarre Formation; underlies the Belfast Mudstone. Geological Province: Otway Basin.||||||12-OCT-05
6733|Flaxman Formation|61471|6|Mentioned|p34|||Geological Province: Otway Basin.||||||
6733|Flaxman Formation|61547|6|Mentioned|p461 Fig.2, p462. |Turonian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Sandstone. Is overlain by Belfast Mudstone.||
6733|Flaxman Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
6733|Flaxman Formation|61625|5|Briefly described|p476 Fig. 1, p477, p478 Fig. 3|Late Cretaceous|Late Cretaceous|Named Flaxman Fromation by Bock and Glenie (1965). Of Sherbrook Group. Geological Province: Otway Basin. Fine-grained grey-brown sandstone with occasional coarse sandstone interbeds.||||||07-FEB-11
6733|Flaxman Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
6733|Flaxman Formation|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
6733|Flaxman Formation|63122|5|Briefly described|p17 Fig. 4.3|Santonian|Turonian|Of the Sherbrook Group. Max. thickness: 620m. Geological Province: Otway Basin. ||||||
6733|Flaxman Formation|63124|5|Briefly described|p48 Fig. 5.1, p49 Fig. 5.2, p80|||Earlier referred to as Flaxmans Formation (Reynolds et al 1966 and Wopfner et al (1971). Max. thickness: 620m. Geological Province: Otway Basin.||||||
6733|Flaxman Formation|63125|6|Mentioned|p121 Tb. 7.11|||Geological Province: Otway Basin||||||
6733|Flaxman Formation|63129|5|Briefly described|p137|||Geological Province: Otway Basin. Shales within this unit may act as regional seals.||||||30-JAN-08
6733|Flaxman Formation|63130|5|Briefly described|p143|||Geological Province: Otway Basin. Its reservoirs are sealed by Belfast Mudstone, or by intra-Parratte Formation shales. ||||||
6733|Flaxman Formation|63269|5|Briefly described|p605-607, p616, p618|Late Cretaceous|Late Cretaceous|Otway Basin. Details of natural gas, oils and oil stains in named wells tabulated. Oil-source correlation.||Sherbrook Group.||||
6733|Flaxman Formation|63431|5|Briefly described|p677 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Overlies Waarre Sandstone. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|66245|5|Briefly described|p6 Fig.5, p21 Fig.23, p68 Fig.D4.|Turonian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Formation.||
6733|Flaxman Formation|67061|6|Mentioned|p546 Fig.3.|Turonian|Turonian|||Unit in Sherbrook Group.||||
6733|Flaxman Formation|67366|5|Briefly described|p103 Fig.2. |Coniacian|Turonian|||Unit in Sherbrook Group.|Includes Banoon Member.|Overlies Waarre Formation. Is overlain by Belfast Formation.|Shelf to open marine shale.|
6733|Flaxman Formation|67367|5|Briefly described|p131 Fig.2. |Late Cretaceous|Late Cretaceous|Has potential as a viable hydrocarbon source rock.||Unit in Sherbrook Group.||||
6733|Flaxman Formation|69297|5|Briefly described|p78, p79, p83, p84, p98, p115|Turonian|Turonian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Shales may act as intraformational seals. Potential reservoir in the Sorell Basin.   ||Shipwreck Supersequence|Includes the Banoon Member|Overlies the Waarre Formation. Overlain by the Belfast Mudstone.|Siltstone and mudstone.|
6733|Flaxman Formation|69651|5|Briefly described|p10, p15, p31-34|Late Cretaceous|Late Cretaceous|Turonian. Marine, marginal marine and coastal plain sediments. Reservoirs sealed by Belfast Mudstone; shale units may act as intraformational seals.||Sherbrook Group.||Overlies Waarre Formation. Is overlain unconformably by Belfast Mudstone.|Includes shales.|
6733|Flaxman Formation|69879|5|Briefly described|p424|Turonian|Turonian|Otway Basin. Hydrocarbon reservoir in the Thylacine gas-condensate field. More deeply buried sediments are possibly hydrocarbon source.||||Overlies Waarre Formation.|Marine sandstone.|
6733|Flaxman Formation|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p5|Late Cretaceous|Late Cretaceous|See also Regional: p8, p10. Otway Basin. Distal equivalents in the Nelson Sub-basin may be important petroleum reservoirs, and shales provide intraformational seals.||Sherbrook Group.|Banoon Member.|Overlies Waarre Formation. Is overlain by Mount Salt Formation or Belfast Mudstone.||
6733|Flaxman Formation|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p4-5|Coniacian|Turonian|Otway Basin. Equivalent sandstones in Sorell Basin are potential reservoirs.||Sherbrook Group.||Overlies Waarre Formation. Is overlain by Mount Salt Formation or Belfast Mudstone.||
6733|Flaxman Formation|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Turonian|Turonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.|||Includes Banoon Member?|||
6733|Flaxman Formation|70880|6|Mentioned|p77|Turonian|Turonian|Otway Basin.||||||
6733|Flaxman Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
6733|Flaxman Formation|71437|4|Described|p157|Coniacian|Cenomanian|Previously Flaxman's Beds. Marine littoral to shallow neritic; minor paralic; lagoonal to tidal flat.||Of Wangerrip Group.||Overlies Waarre Sandstone. Sharp or transitional contact with overlying Belfast Mudstone Member.|Glauconitic and limonitic sandstone, minor siderite.|
6733|Flaxman Formation|73357|5|Briefly described|p20, p31, p45, p47|Coniacian|Turonian|Otway Basin. Correlated with Phyllocladidites mawsonii Spore-Pollen Zone, and Palaeohystrichophora infusorioides Dinocyst Zone marking a marine transgression with marginal to shallow marine facies.||Of Sherbrook Group.||Overlies Waarre Formation, underlies Belfast Mudstone.||
6733|Flaxman Formation|73383|5|Briefly described|vi, p3, p11 Tb.3.9, p134-135, p262|Coniacian|Turonian|Otway Basin. Possibly equivalent to the mudstone-dominant chemostratigraphic package S5-P3, only identified in the Penryn-1 well in this study.||Sherbrook Group||Overlies Waarre Formation, underlies Belfast Mudstone.|Shallow marine and nearshore sandstones. Mudstone and shale based on geochemistry.|
6733|Flaxman Formation|73385|5|Briefly described|p5|Coniacian|Turonian|Otway Basin.||Sherbrook Group||Overlies Waare Formation, underlies Belfast Mudstone.|Shallow marine and nearshore sandstones.|
6733|Flaxman Formation|73386|4|Described|p4, p6, p10-11, Attachment A1|Coniacian|Turonian|Otway Basin. Deposited in a lower delta plain environment, considered as the first marine transgressive unit in the Sherbrook Group. Type section defined between 2340 m and 2483 m in Port Campbell-2 (Partridge, 2001). Occurs within Phyllocladidites mawsonii Spore-Pollen Zone. Onshore, predominantly restricted to the Port Campbell and Tyrendarra embayments. Originally termed Flaxman Beds, also termed Waarre Formation unit D.||Sherbrook Group||Conformably overlies Waarre Formation, conformably underlies Belfast Mudstone|Interbedded sand/shale unit containing dark grey silty mudstones and fine grained grey brown sandstones, with distinctive coarse sand to pebble-sized 'floating quartz'.|
6733|Flaxman Formation|73594|5|Briefly described|p4-5, p15-16, p25-28, p31-32|Coniacian|Turonian|Otway Basin. Very heterogeneous. Marks a widespread marine transgression. Intersection of the unit in Port Campbell-2 well designated as the type section (BMR, 1964). Banoon Member (Partridge, 2001) may be present at the top of the unit, reliable marker of boundary with the Belfast Mudstone. Unit is absent at the crest of some elevated fault blocks in the Port Campbell Embayment.||Sherbrook Group||Overlies Waarre Formation, underlies Belfast Mudstone, Nullawarre Greensand. Unconformably underlies Thylacine Member|Upward-fining sequence of interbedded silty mudstones and fine-grained sandstones including pebbly mudstones at base, glauconitic and sideritic shales and siltstones.|
6822|Fork Tree Limestone|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Kanmantoo Group. Massive and bedded calc-dolomite.||||||
6822|Fork Tree Limestone|22531|6|Mentioned|p15|||||||||
6822|Fork Tree Limestone|22581|6|Mentioned|Fig.2,p37|||Of the Normanville Group. In the Kanmantoo Basin. Overlies Sellick Hill Formation. Overlain by Heatherdale Shale||||||12-FEB-07
6822|Fork Tree Limestone|22643|5|Briefly described|fig3p187|Early Cambrian|Early Cambrian|||||||
6822|Fork Tree Limestone|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
6822|Fork Tree Limestone|22857|5|Briefly described|p88 Fig. 14.7A, p97|Early Cambrian|Early Cambrian|Of the Normanville Group. ||||||
6822|Fork Tree Limestone|22858|6|Mentioned|p97|||||||||
6822|Fork Tree Limestone|23482|5|Briefly described|p9|Early Cambrian|Early Cambrian|||||||
6822|Fork Tree Limestone|23731|6|Mentioned|p28|Early Cambrian|Early Cambrian|||||||
6822|Fork Tree Limestone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
6822|Fork Tree Limestone|23827|6|Mentioned|p260 Fig.3|||||||||
6822|Fork Tree Limestone|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5, p26|Early Cambrian|Early Cambrian|Coalesced bioherms with similar archaeocyathan fauna to that of upper Sellick Fill Fm. Different lithologies given for various parts of basin. Overlies Sellick Hill Fm; underlies Heatherdale Shale and Truro Volcs. Max.thick:300m. Geol.P: Stansbury Basin.||||||03-MAY-13
6822|Fork Tree Limestone|24465|6|Mentioned|p358|Early Cambrian|Early Cambrian|Of Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
6822|Fork Tree Limestone|30052|6|Mentioned|Fig.3|||Cambrian age.||||||
6822|Fork Tree Limestone|30801|6|Mentioned|p5|||Lower Cambrian. Table p5-6.||||||12-FEB-07
6822|Fork Tree Limestone|30805|6|Mentioned|p1|||||||||
6822|Fork Tree Limestone|32551|5|Briefly described|p100|||Camb. lithology||||||
6822|Fork Tree Limestone|33953|6|Mentioned|Fig.4|||||||||
6822|Fork Tree Limestone|34014|5|Briefly described|p22|||Cambrian||||||
6822|Fork Tree Limestone|34612|6|Mentioned|Fig.33|||Cambrian. Correlation chart||||||
6822|Fork Tree Limestone|35255|6|Mentioned|Fig.8|||||||||
6822|Fork Tree Limestone|36731|6|Mentioned|p125|||||||||
6822|Fork Tree Limestone|38873|6|Mentioned|Table 2|||||||||
6822|Fork Tree Limestone|39806|6|Mentioned|p207|||||||||
6822|Fork Tree Limestone|40442|6|Mentioned|p15|||See also Table 1.||||||
6822|Fork Tree Limestone|40455|5|Briefly described|p69|||||||||
6822|Fork Tree Limestone|40810|5|Briefly described|p13|||||||||
6822|Fork Tree Limestone|40852|6|Mentioned|p33|||||||||
6822|Fork Tree Limestone|41103|6|Mentioned|Fig.1|||||||||
6822|Fork Tree Limestone|41526|6|Mentioned|p61|||||||||
6822|Fork Tree Limestone|42093|5|Briefly described|p6|||See also Fig.2||||||
6822|Fork Tree Limestone|42192|6|Mentioned|p6|||||||||
6822|Fork Tree Limestone|42222|6|Mentioned|Table 1 P4|||||||||
6822|Fork Tree Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
6822|Fork Tree Limestone|42232|4|Described|p283|||||||||
6822|Fork Tree Limestone|42266|6|Mentioned|p290|||||||||
6822|Fork Tree Limestone|42268|6|Mentioned|p331|||||||||
6822|Fork Tree Limestone|42270|6|Mentioned|p353|||||||||
6822|Fork Tree Limestone|42272|5|Briefly described|p404|||||||||
6822|Fork Tree Limestone|42488|5|Briefly described|p185, Fig.2 p187|||||||||
6822|Fork Tree Limestone|43190|5|Briefly described|p34.|||Of Normanville Group.||||||
6822|Fork Tree Limestone|43703|6|Mentioned|p75|Botoman|Atdabanian|||||||
6822|Fork Tree Limestone|43759|4|Described|p446|||||||||
6822|Fork Tree Limestone|44133|5|Briefly described|p4 Fig. 7.2, 6|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group.||||||
6822|Fork Tree Limestone|60712|5|Briefly described|p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||
6822|Fork Tree Limestone|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Adelaide Fold Belt.||||||15-JAN-08
6822|Fork Tree Limestone|63848|5|Briefly described|p532,  p534 Fig.4.|Atdabanian|Atdabanian|Contains archaeocyathids.||Unit in Normanville Group.||Overlies Sellick Hill Formation. Is overlain by Heatherdale Shale.||
6822|Fork Tree Limestone|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Normanville Group.||Overlies Sellick Hill Formation. Is overlain by Heatherdale Shale.||
6822|Fork Tree Limestone|65686|6|Mentioned|p411, 420|Early Cambrian|Early Cambrian|Of the Fleurieu Peninsula.||||||07-MAY-12
6822|Fork Tree Limestone|65892|5|Briefly described|p9 Fig.4, p15, p17, p19. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. An archaeocyath-rich lower member consists of coalesced bioherms, and a strikingly mottled, 30m thick, upper member contains rare brachiopods and hyolithids. Extensively recrystallised.||Unit in Normanville Group.||Conformably overlies Sellick Hill Formation. Is overlain conformably by Heatherdale Shale and Truro Volcanics.|Massive pale grey limestone.|
6822|Fork Tree Limestone|66761|5|Briefly described|p246, 254|Cambrian|Cambrian|Fleurieu Peninsula. Rocks contain archaeocyaths. Correlated with Mount McDonnell Formation on Kangaroo Island.||||Underlies the Heatherdale Shale, overlies the Sellick Hill Formation.||14-MAR-12
6822|Fork Tree Limestone|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Of the Normanville Group.||||
6822|Fork Tree Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
6822|Fork Tree Limestone|70660|5|Briefly described|p40|Early Cambrian|Early Cambrian|||||||
6822|Fork Tree Limestone|70833|5|Briefly described|p200,202|Cambrian|Cambrian|Of Eastern Stansbury Basin. Includes K. rostrata zone. Equivalent to lower parts of Wilkawillina and Wirrapowie and Ajax limestones.||||Overlain by Heatherdale Shale. Underlain by Sellick Hill Formation.||
6822|Fork Tree Limestone|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Pale grey limestone with Archaeocyaths.|
6822|Fork Tree Limestone|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Normanville Group|||Archaeocyathan limestone.|
6822|Fork Tree Limestone|73247|6|Mentioned|p205, p207|Cambrian (Stage 2)|Cambrian (Stage 2)|Fleurieu Peninsula. Correlated with the McDonnell Formation based on archaeocyath assemblage from a thin oolitic limestone.||||Underlain by Sellick Hill Formation. Overlain by Heatherdale Shale. Equivalent to Parara Limestone.||
6841|Fortress Hill Formation|22510|5|Briefly described|p40,table1|||Age: Marinoan. Nackara Arc.||||||
6841|Fortress Hill Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
6841|Fortress Hill Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group).||||||
6841|Fortress Hill Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
6841|Fortress Hill Formation|23411|6|Mentioned|Map Legend|||||||||
6841|Fortress Hill Formation|23818|5|Briefly described|p72|Adelaidean|Adelaidean|Lowermost unit of the Yerelina Sub-Group. Equivalent unit with the Gumbowie Arkose Member.||||||
6841|Fortress Hill Formation|24175|4|Described|p13|Neoproterozoic III|Neoproterozoic|Of Yerelina Subgroup.  Slaty sequence containing scattered dropstones, minor thin conglomerate, medium-grained pebbly sandstone and diamictite.  Overlies Amberoona Formation; overlain by Mount Curtis Tillite.  Max. thickness: 760m.||||||
6841|Fortress Hill Formation|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Yerelina Sub-Group.  Grey-green siltstone, minor quartzite, lenses of gritty limestone.  Underlies Mount Curtis Tillite.  Max. thickness: 1830m. Age is Marinoan.  Geological Province: Mount Painter Province.||||||
6841|Fortress Hill Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Yerelina Subgroup||||||
6841|Fortress Hill Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6841|Fortress Hill Formation|30177|2|Defined|p132|Adelaidean|Adelaidean|See also p85. Type section Approximately half a mile north of Mount Saturday, lat. 30degrees06'53"S long. 139degrees 16'27"E to lat. 30degrees07'27"S long. 139degrees 15'34"E. Thickness 300ft (90m).||||||25-NOV-22
6841|Fortress Hill Formation|30261|6|Mentioned|Table 1|||Marinoan age||||||
6841|Fortress Hill Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
6841|Fortress Hill Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
6841|Fortress Hill Formation|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
6841|Fortress Hill Formation|33474|6|Mentioned|Fig.2|||||||||
6841|Fortress Hill Formation|34535|5|Briefly described|p72|||Equiv. Gumbowie Arkose Member||||||
6841|Fortress Hill Formation|34812|6|Mentioned|Table 8|||||||||
6841|Fortress Hill Formation|35255|6|Mentioned|Fig.7|||||||||
6841|Fortress Hill Formation|36137|5|Briefly described|p16|||Palaeomagnetism discussed.||||||
6841|Fortress Hill Formation|36733|6|Mentioned|Table 5|||||||||
6841|Fortress Hill Formation|37461|5|Briefly described|p342|||||||||
6841|Fortress Hill Formation|37932|5|Briefly described|p546|||See also P544.||||||
6841|Fortress Hill Formation|38157|6|Mentioned|Table IV|||||||||
6841|Fortress Hill Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
6841|Fortress Hill Formation|41405|4|Described|p197|||||||||
6841|Fortress Hill Formation|42222|6|Mentioned|p18|||||||||
6841|Fortress Hill Formation|42238|5|Briefly described|Table 1 P74|||||||||
6841|Fortress Hill Formation|42239|6|Mentioned|p161|||||||||
6841|Fortress Hill Formation|42542|5|Briefly described|p8|||||||||
6841|Fortress Hill Formation|43052|5|Briefly described|p190,Table 6.1|||of Yerelina Subgroup||||||
6841|Fortress Hill Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
6841|Fortress Hill Formation|64797|6|Mentioned|p163, p166 Tb.7|||Base of Marinoan glacial deposits (in Mount Saturday section).||Unit in Umberatana Group.||Correlated with Elatina Formation.||
6841|Fortress Hill Formation|68241|6|Mentioned|p20 Fig.1|||||||||
6841|Fortress Hill Formation|69019|4|Described|p51-53.|Neoproterozoic|Neoproterozoic|Of Coats and Blissett (1971). c. 1,070 m thick at the type section ~1 km north of Mt. Saturday in Flinders Ranges.||Unit in Yerelina Subgroup.||Disconformably overlies Amberoona Formation. Is overlain conformably by Gumbowie Arkose.|Grey gritty siltstones containing sparsely scattered cobbles, some facetted; intraformational lenses of gritty and pebbly limestone and sandstone; local outcrops of a hornfels band.|
6841|Fortress Hill Formation|69023|6|Mentioned|p70|||Preiss (1987). Includes a gritty pebble unit that had been basal within the Amberoona Formation of Coats (1964), but excised by Coats and Blissett (1971).||||||
6841|Fortress Hill Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Local slumping and erosion at base. Some outcrop includes a dark-hued hornfels band. North of Mount Livingston, varve-like laminations and fine-grained, basal, brown-weathering pink quartzite occur. Age shown more specifically as Marinoan [Cryogenian].||Of Yerelina Subgroup.||Unconformably overlies Trezona Formation.|Gritty siltstone, grey-green weathering to reddish-brown, finely laminated; gritty and pebbly sandstone and limestone lenses; sparse well-rounded quartz grains; rare dropstones; occasionally weakly pyritic. Sandstone interbeds (separately mapped).|23-JAN-19
6841|Fortress Hill Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, gritty, dolomitic lenses and cobbles.|
6841|Fortress Hill Formation|74367|6|Mentioned|p7 Fig.6|||||Yerelina Subgroup||||
6907|Freshwater Limestone|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Great Artesian Basin.||||||
6907|Freshwater Limestone|34180|6|Mentioned|p212|||Middle Pleistocene||||||
6976|Gambier Limestone|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6976|Gambier Limestone|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin. Maximum thickness 400m.||Heytsbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|22541|6|Mentioned|Fig 16|||||||||
6976|Gambier Limestone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Late Eocene|||||||
6976|Gambier Limestone|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province West Otway Basin. Overlying unit Heytesbury Group||||||
6976|Gambier Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
6976|Gambier Limestone|22799|5|Briefly described|p23 Fig.7|Early Miocene|Oligocene|Glenelg Group||||||
6976|Gambier Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6976|Gambier Limestone|22887|5|Briefly described|Fig.6 p13||Late Oligocene|Of Murray Group, Murray Basin.||||||03-FEB-09
6976|Gambier Limestone|22893|5|Briefly described|fig4 p9|||||||||
6976|Gambier Limestone|22913|6|Mentioned|29|||||||||
6976|Gambier Limestone|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6976|Gambier Limestone|23249|5|Briefly described|Fig.2|||Informally divided into Upper/Middle and Lower Gambier Limestone.||||||
6976|Gambier Limestone|23322|4|Described|955, 957|Middle Miocene|Middle Eocene|Geological Province: Gambier Basin.||||||07-SEP-09
6976|Gambier Limestone|23671|6|Mentioned|p2|||Overlies the Compton Conglomerate; disconformably overlies the Burrungule Member.||||||16-AUG-04
6976|Gambier Limestone|23731|6|Mentioned|p20, p27|Miocene|Oligocene|||||||
6976|Gambier Limestone|23768|5|Briefly described|p28 Fig.5, p69|Miocene|Oligocene|Geological Province: Gambier Basin. See also p89, p154.||||||29-MAR-05
6976|Gambier Limestone|23818|5|Briefly described|p174 Fig.84, p177|Middle Miocene|Oligocene|Geological Province: Otway Basin. Max. thickness: 500 ft.||||||
6976|Gambier Limestone|23879|5|Briefly described|p19|||||||||
6976|Gambier Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Oligocene|Late Oligocene|Geological Province: Murray Basin. Of the Murray Group.||||||
6976|Gambier Limestone|24160|6|Mentioned|p18|Middle Miocene|Middle Miocene|Hosts a calcium bentonite deposit below weathered Newer Volcanics.||||Is overlain by Newer Volcanics.||
6976|Gambier Limestone|24202|5|Briefly described|p313 Fig.2|Middle Miocene|Early Oligocene|Geological Province: Gambier Sub-basin.  See also p314.||||||
6976|Gambier Limestone|24314|5|Briefly described|p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin. Max. Thickness 400m. Of the Heytesbury Group.||||||30-NOV-04
6976|Gambier Limestone|24363|5|Briefly described|p37|Early Miocene|Oligocene|max. thickness: 400 m. Age: 38-15 Ma.||||||
6976|Gambier Limestone|24410|6|Mentioned|p6|Late Oligocene|Early Miocene|||||||
6976|Gambier Limestone|24551|6|Mentioned|p296, 555, 625|||||||||
6976|Gambier Limestone|24562|5|Briefly described|p15 Fig. 4|Tertiary|Late Cretaceous|Geological Province: Otway Basin.||||||
6976|Gambier Limestone|29591|6|Mentioned|p90|||||||||
6976|Gambier Limestone|29654|6|Mentioned|p101|||||||||
6976|Gambier Limestone|29666|6|Mentioned|p22|||||||||
6976|Gambier Limestone|29697|6|Mentioned|p2|||||||||
6976|Gambier Limestone|29828|6|Mentioned|p25|||||||||
6976|Gambier Limestone|29866|6|Mentioned|p84|||||||||
6976|Gambier Limestone|29891|5|Briefly described|p77|||||||||
6976|Gambier Limestone|29892|6|Mentioned|p77|||||||||
6976|Gambier Limestone|29894|6|Mentioned|p27|||||||||
6976|Gambier Limestone|30179|6|Mentioned|p33|||Oligocene - Miocene age||||||
6976|Gambier Limestone|30184|6|Mentioned|p173|||||||||
6976|Gambier Limestone|30514|6|Mentioned|p108|||||||||
6976|Gambier Limestone|30520|6|Mentioned|p41|||Groundwater||||||
6976|Gambier Limestone|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6976|Gambier Limestone|30751|6|Mentioned|Map legend|Oligocene|Eocene|Miocene-Eocene||||||
6976|Gambier Limestone|30753|4|Described|Table 2|||Middle Miocene to Upper Eocene age.||||||07-SEP-18
6976|Gambier Limestone|30754|5|Briefly described|p13|||Strat.tables p14,22. See also p20,24,28. Map, block diag.,section.||||||07-SEP-18
6976|Gambier Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
6976|Gambier Limestone|30828|6|Mentioned|p113|||||||||
6976|Gambier Limestone|30917|6|Mentioned|p26|||||||||
6976|Gambier Limestone|30918|6|Mentioned|p85|||||||||
6976|Gambier Limestone|30932|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene to Miocene||||||
6976|Gambier Limestone|30996|6|Mentioned|Fig. 3|||||||||
6976|Gambier Limestone|31241|4|Described|p99|||See also P101. Equ. in age to Ettrick Fm.||||||
6976|Gambier Limestone|31245|6|Mentioned|p81|||||||||
6976|Gambier Limestone|31372|6|Mentioned|Fig. 2|||||||||
6976|Gambier Limestone|31424|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|31515|6|Mentioned|p292|||||||||
6976|Gambier Limestone|31517|6|Mentioned|p1|||Fossil sites of decapods.||||||
6976|Gambier Limestone|31624|2|Defined|p96|Tertiary|Tertiary|||||||
6976|Gambier Limestone|31625|6|Mentioned|Fig. 5.2|||Oligocene- Miocene||||||
6976|Gambier Limestone|31629|6|Mentioned|Fig.5.2|||Miocene-Oligocene||||||
6976|Gambier Limestone|31746|6|Mentioned|p195|||||||||
6976|Gambier Limestone|31848|6|Mentioned|p15|||Refers Ludbrook (1969)||||||
6976|Gambier Limestone|31851|6|Mentioned|p10|||Also P15||||||
6976|Gambier Limestone|31920|4|Described|p59|||Oligocene. Sponge spicule mb. See also Figs 3-2,4.||||||
6976|Gambier Limestone|31922|6|Mentioned|Table 3|||||||||
6976|Gambier Limestone|31923|6|Mentioned|p16|||||||||
6976|Gambier Limestone|32116|4|Described|p45|||Oligocene. See also p46-47.||||||01-NOV-22
6976|Gambier Limestone|32344|6|Mentioned|p121|||||||||
6976|Gambier Limestone|32552|6|Mentioned|p184|||Longfordian||||||
6976|Gambier Limestone|32570|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32601|6|Mentioned|p682|||||||||
6976|Gambier Limestone|32653|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|32841|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32859|4|Described|p69|||L.Miocene||||||
6976|Gambier Limestone|32860|5|Briefly described|p91|||Lower Pliocene.||||||07-SEP-18
6976|Gambier Limestone|32894|6|Mentioned|p287|||Olig.-Miocene||||||
6976|Gambier Limestone|32895|6|Mentioned|p328|||Tertiary||||||
6976|Gambier Limestone|32897|6|Mentioned|Fig. 7-1|||||||||
6976|Gambier Limestone|32898|6|Mentioned|p27|||See also Table 2-1||||||
6976|Gambier Limestone|33109|6|Mentioned|p84|||Main aquifer system||||||
6976|Gambier Limestone|33236|6|Mentioned|p19|||Olig. - Miocene||||||
6976|Gambier Limestone|33490|4|Described|p10|||See also p27. Oligocene - Miocene.||||||07-SEP-18
6976|Gambier Limestone|33579|6|Mentioned|p52|||||||||
6976|Gambier Limestone|33712|6|Mentioned|p9|||See also Fig.1. Oligo. - Mioc. Refers Ludbrook (1961).||||||
6976|Gambier Limestone|33713|4|Described|p27|||See also p28.||||||07-SEP-18
6976|Gambier Limestone|33716|3|Fully described|p15|||See also pp16 & 20 & Table 2.||||||07-SEP-18
6976|Gambier Limestone|33798|6|Mentioned|p98|||Fig.2||||||
6976|Gambier Limestone|33940|6|Mentioned|p414|||||||||
6976|Gambier Limestone|33943|6|Mentioned|p379|||||||||
6976|Gambier Limestone|34180|6|Mentioned|p212|||Tertiary||||||
6976|Gambier Limestone|34185|6|Mentioned|p131|||Protected from marine erosion in Pliocene.||||||
6976|Gambier Limestone|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6976|Gambier Limestone|34308|3|Fully described|p177|||Aldingian - Balcombian. Correlation chart||||||
6976|Gambier Limestone|34418|4|Described|p506|||||||||
6976|Gambier Limestone|34421|6|Mentioned|p261|||See also P262||||||
6976|Gambier Limestone|34524|5|Briefly described|p105|||||||||
6976|Gambier Limestone|34615|6|Mentioned|p3|||||||||
6976|Gambier Limestone|34658|5|Briefly described|p98|||||||||
6976|Gambier Limestone|34954|6|Mentioned|Fig.33|||Analysis.||||||
6976|Gambier Limestone|34958|6|Mentioned|p88|||||||||
6976|Gambier Limestone|34988|6|Mentioned|p294|||||||||
6976|Gambier Limestone|35018|5|Briefly described|p29|||||||||
6976|Gambier Limestone|35051|6|Mentioned|p203|||Analysis.||||||
6976|Gambier Limestone|35066|6|Mentioned|p210|||||||||
6976|Gambier Limestone|35097|6|Mentioned|Fig.4|||||||||
6976|Gambier Limestone|35147|6|Mentioned|p127|||||||||
6976|Gambier Limestone|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6976|Gambier Limestone|35232|6|Mentioned|p11|||||||||
6976|Gambier Limestone|36492|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|37500|6|Mentioned|p385|||||||||
6976|Gambier Limestone|37548|6|Mentioned|p131|||||||||
6976|Gambier Limestone|38068|6|Mentioned|Fig.7|||||||||
6976|Gambier Limestone|38070|6|Mentioned|Fig.12|||Otway Basin||||||
6976|Gambier Limestone|38663|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38699|6|Mentioned|p8|||||||||
6976|Gambier Limestone|38826|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38903|5|Briefly described|Table 2|||||||||
6976|Gambier Limestone|38932|5|Briefly described|p98|||See also Fig.4.||||||07-SEP-18
6976|Gambier Limestone|39077|6|Mentioned|Table 2|||||||||
6976|Gambier Limestone|39329|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|39408|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|39923|6|Mentioned|p354|||||||||
6976|Gambier Limestone|39929|6|Mentioned|Fig.3|||||||||
6976|Gambier Limestone|40003|5|Briefly described|p44|||||||||
6976|Gambier Limestone|40032|6|Mentioned|p225|||||||||
6976|Gambier Limestone|40125|6|Mentioned|p353|||||||||
6976|Gambier Limestone|40230|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40298|6|Mentioned|p432|||||||||
6976|Gambier Limestone|40429|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|40521|6|Mentioned|p307|||||||||
6976|Gambier Limestone|40555|6|Mentioned|p51|||||||||
6976|Gambier Limestone|40556|6|Mentioned|p61|||||||||
6976|Gambier Limestone|40557|6|Mentioned|p169|||||||||
6976|Gambier Limestone|40560|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40561|6|Mentioned|p8|||||||||
6976|Gambier Limestone|40829|5|Briefly described|p14|||||||||
6976|Gambier Limestone|40877|5|Briefly described|p55|||||||||
6976|Gambier Limestone|40947|6|Mentioned|p3|||||||||
6976|Gambier Limestone|40980|6|Mentioned|p335|||||||||
6976|Gambier Limestone|41076|6|Mentioned|p63|||||||||
6976|Gambier Limestone|41185|6|Mentioned|Fig.5|||||||||
6976|Gambier Limestone|41517|6|Mentioned|p138|||||||||
6976|Gambier Limestone|41518|6|Mentioned|p146|||||||||
6976|Gambier Limestone|41519|6|Mentioned|p172|||||||||
6976|Gambier Limestone|41520|5|Briefly described|Fig.12|||||||||
6976|Gambier Limestone|41578|6|Mentioned|p7|||||||||
6976|Gambier Limestone|41599|6|Mentioned|p191|||||||||
6976|Gambier Limestone|41626|6|Mentioned|p54|||||||||
6976|Gambier Limestone|42097|6|Mentioned|p40|||||||||
6976|Gambier Limestone|42125|5|Briefly described|p136|||||||||
6976|Gambier Limestone|42127|5|Briefly described|p223|||||||||
6976|Gambier Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
6976|Gambier Limestone|42137|6|Mentioned|p370|||||||||
6976|Gambier Limestone|42335|5|Briefly described|p338|||||||||
6976|Gambier Limestone|42457|6|Mentioned|p170|||||||||
6976|Gambier Limestone|42594|5|Briefly described|p247|||Oligocene-Miocene||||||
6976|Gambier Limestone|42599|5|Briefly described|Fig.3 P614|||Cooper Basin.||||||07-SEP-18
6976|Gambier Limestone|42601|6|Mentioned|Fig.2 p15|||||||||
6976|Gambier Limestone|42717|6|Mentioned|map legend|Miocene|Oligocene|||||||
6976|Gambier Limestone|42827|6|Mentioned|p285|||||||||
6976|Gambier Limestone|42881|4|Described|Fig.3, p84|||||||||01-NOV-22
6976|Gambier Limestone|42966|2|Defined|Table 15, p126|Early Miocene|Late Oligocene|Of Murray Group, Murray Basin & Glenelg Group, Otway Basin.||||||03-FEB-09
6976|Gambier Limestone|43073|5|Briefly described|p11|||||||||
6976|Gambier Limestone|43171|6|Mentioned|5|||Of Heytesbury Group.||||||03-FEB-09
6976|Gambier Limestone|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map. Of Heytesbury Group.||||||
6976|Gambier Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43298|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43383|14|Not recorded|p29||Early Miocene|||||||
6976|Gambier Limestone|43466|14|Not recorded|p3,Pl.1|||Equivalent to SA||||||
6976|Gambier Limestone|43467|14|Not recorded|p3,20,31,32|||||||||
6976|Gambier Limestone|43660|6|Mentioned|Fig.7,p16|||||||||
6976|Gambier Limestone|43667|6|Mentioned|Fig.3,p12|Early Miocene|Early Oligocene|||||||
6976|Gambier Limestone|43686|6|Mentioned|Fig.5,p233|||||||||
6976|Gambier Limestone|43733|6|Mentioned|p30||Tertiary|||||||
6976|Gambier Limestone|43744|6|Mentioned|Fig.3,p3|||||||||
6976|Gambier Limestone|43791|6|Mentioned|p372, Fig1|||||||||
6976|Gambier Limestone|43797|5|Briefly described|p201|Miocene|Oligocene|||||||
6976|Gambier Limestone|43799|5|Briefly described|p185|||||||||
6976|Gambier Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
6976|Gambier Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
6976|Gambier Limestone|44133|4|Described|p156, 259, 268|Miocene|Miocene|Thickness: 400m. Of the Heytesbury Group. Geological Province: Gambier Basin. Includes: Greenways Member, Camelback Member, Green Point Member, Naracoorte Limestone Member.||||||
6976|Gambier Limestone|46802|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|46839|6|Mentioned|p81|||||||||
6976|Gambier Limestone|46899|6|Mentioned|p13|||Thermal conductivity||||||
6976|Gambier Limestone|46909|6|Mentioned|p83|||||||||
6976|Gambier Limestone|48624|14|Not recorded|p4,6,Fig.2|||(J54-6/Benara).||||||
6976|Gambier Limestone|48625|14|Not recorded|p4,5|||(J54-6/Kennion). map opp.p.1.||||||
6976|Gambier Limestone|48911|6|Mentioned|Chart 1|||Heytesbury Gp.||||||
6976|Gambier Limestone|49038|5|Briefly described|p26|||||||||
6976|Gambier Limestone|49040|6|Mentioned|p11|||||||||
6976|Gambier Limestone|50133|5|Briefly described|p3, Fig.1|Mid Miocene|Late Eocene|Also called Mount Gambier Limestone (superseded term) in this article (at p6, p8 Tb 1, p11 Tb.2). Major & trace element geochemistry for 2 samples given.|||Includes Camelback Member.||Fossiliferous carbonate|27-MAR-12
6976|Gambier Limestone|60538|5|Briefly described|p471 Fig. 10, 473 Fig. 12|||Of the Nirranda Group.||||||
6976|Gambier Limestone|60785|6|Mentioned|p184 Fig.1. |Chattian|Chattian|South Australia.|||Includes the Camelback Member.|||
6976|Gambier Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61155|5|Briefly described|p18|Middle Miocene|Early Oligocene|Murray Group. Overlies Ettrick Formation; overlain by Mannum Formation. Age: 27.5-~24Ma to ~33-15Ma. Interfingered with Naracoorte Limestone. Thickness: 100m. Geological Province: Murray and Otway Basin.||||||03-MAR-10
6976|Gambier Limestone|61547|6|Mentioned|p461 Fig.2. |Miocene|Eocene|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|61622|5|Briefly described|p436 Fig. 2|Miocene|Eocene|Of Heytsbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|62640|6|Mentioned|p76.|||Tertiary. Restricted cave development is due to substantial intergranular porosity and permeability; hence considerable groundwater flow through the limestone matrix and less flow through karst conduits.||||||
6976|Gambier Limestone|63122|5|Briefly described|p17 Fig. 4.3|Early Miocene|Late Eocene|Of the Heytesbury Group. Max. thickness: 400m. Geological Province: Otway Basin. ||||||
6976|Gambier Limestone|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29, p91|Miocene|Late Eocene|Of the Heytesbury Group. Supersedes "Mount Gambier Limestone". Comprises Greenways, Gellibrand, Camelback, and Green Point Members, and Naracoorte Limestone Member. Max. thickness: 400m. Geological Province: Otway Basin.||||||
6976|Gambier Limestone|63129|6|Mentioned|p139|||Geological Province: Otway Basin. Surface aquifer.||||||30-JAN-08
6976|Gambier Limestone|63222|5|Briefly described|p40, p41|||Dimension stone from the South East, S.A.||||||01-MAR-10
6976|Gambier Limestone|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Of the Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|63887|5|Briefly described|p21 Fig. 1|||||||||
6976|Gambier Limestone|64769|6|Mentioned|p28|Miocene|Miocene|Material mined is named the Gambier Stone. SA.||||||06-MAY-09
6976|Gambier Limestone|64966|5|Briefly described|p137, p144|Middle Miocene|Late Oligocene|Of the Heytesbury Group. Max. thickness: 400m. Major fossiliferous unit with strong erosional unconformity at the top. Geol.province: Gambier Basin. Equivalent to Mannum Limestone in Murray Basin. Forms bedrock platform beneath most of Lacepede Shelf.||||||07-FEB-11
6976|Gambier Limestone|65374|6|Mentioned|p35|||||||||
6976|Gambier Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
6976|Gambier Limestone|65891|5|Briefly described|p221 Fig.5, p229.|Paleogene|Paleogene|Western Otway Basin. Rupelian age. Pure and temporally persistent neritic carbonate unit. Same suite of planktonic foraminifera as Aldinga Member, but with higher numbers plus Globoturborotalita brevis. ||||||
6976|Gambier Limestone|68211|5|Briefly described|p28, p28 Fig.1, p29|Langhian|Bartonian|Occurs extensively in the Gambier Basin and southwestern Murray Basin. Produced as  a dimension stone and sold under the trade name: Compton Sandstone.|c. 40 - 15 Ma, (White 1996)||||Dolomitic rock.|
6976|Gambier Limestone|68811|6|Mentioned|p110, p130, p156 app 1, p192 tbl 46|Tertiary|Tertiary|Hosts an unconfined aquifer. Also referred to informally as the Gambier limestone on p156 app 1.  ||||Overlies the Dilwyn Formation.||
6976|Gambier Limestone|69297|5|Briefly described|p79|Langhian|Rupelian|Otway Basin.||Heytesbury Group|Includes the Greenways Member, Camelback Member, Green Point Member and the Narracoorle Limestone Member.|Overlies the Narrawaturk Marl. Unconformably overlain by the Bridgewater Formation or the Coomandook Formation.|Limestones.|
6976|Gambier Limestone|70029|5|Briefly described|p151-153,165|Miocene|Oligocene|Affected by localised regional uplift related to volcanism (Mount Burr volcanics), and defines a broad dome near volcanic centres, rising from sea level to 60m APSL east of mount Gambier. Subaerially exposed, karstified marine abrasion surface in which dolines and depressions are common.||||Overlain unconformably by Bridgewater Formation.||04-SEP-19
6976|Gambier Limestone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||Heytesbury Group.|Naracoorte Limestone, Green Point, Camelback and Greenways Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Miocene|Gambier Embayment and Voluta Trough.||Heytesbury Group.|Greenways, Camelback, Green Point and Naracoorte Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|72445|6|Mentioned|App.7 p7 Fig.4.|Oligocene|Oligocene|See also Gambier Limestone Member in text.||Murray Group||||
6976|Gambier Limestone|73118|6|Mentioned|p17|||||||||
6976|Gambier Limestone|73228|4|Described|p50, p52, p56|Middle Miocene|Late Early Oligocene|Murray Basin. Open shelf environment. Identified in Cooltong 1 drillhole.||||Underlain by Ettrick Formation. Overlain by Mannum Formation, Murray Group.|Includes grey, cream bryozoal limestone, dolomitic in part, with minor glauconite.|
6976|Gambier Limestone|73229|5|Briefly described|p66-67, p70-71, p74|Middle Miocene|Early Miocene|Murray Basin. [Analysed using pXRF; see article]. Incuded in group of early Oligocene to Middle Miocene units p67.|||||Includes limestone, bryzoal, grey-cream, dolomitic in part, minor glauconite.|01-NOV-22
6976|Gambier Limestone|73383|6|Mentioned|p82, p213|||Limestone and sub-litharenite lithologies based on geochemistry using the ChemLith classification and the Herron classification (1988).||||||
7059|Gawler Range Volcanics|1418|5|Briefly described|p20,22,25|||Geological province: Gawler Craton. Of Eyre Peninsula. Igneous activity likely resulting in shallow crustal hydrothermal activity leading to formation of siliceous breccia in low hills south of Nankivel Dam and 4.5 km WNW of Peterlumbo Hill, northern Eyre Peninsula, raising potential for epithermal-style gold mineralisation. 40Ar/39Ar dating of K-feldspar from porphyritic dacite is c. 900-700 Ma, interpreted to be timing of alteration or recrystallisation.||||||
7059|Gawler Range Volcanics|22515|6|Mentioned|p405|||||||||
7059|Gawler Range Volcanics|22517|6|Mentioned|P295|Calymmian|Statherian|||||||
7059|Gawler Range Volcanics|22613|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|22614|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|22629|4|Described|fig2p147,157,158|Calymmian|Calymmian|Age: 1590Ma.||||||04-MAR-09
7059|Gawler Range Volcanics|22631|6|Mentioned|p173|Calymmian|Calymmian|age: 1590Ma||||||
7059|Gawler Range Volcanics|22645|6|Mentioned|P205||Calymmian|Age of unit is 1592+/-2 Ma||||||
7059|Gawler Range Volcanics|22690|6|Mentioned|P305||Calymmian|Age of unit is 1592 Ma||||||
7059|Gawler Range Volcanics|22771|5|Briefly described|p36,50|||||||||
7059|Gawler Range Volcanics|22811|6|Mentioned|p605|||||||||
7059|Gawler Range Volcanics|22852|6|Mentioned|7|||||||||
7059|Gawler Range Volcanics|22857|6|Mentioned|p36|||||||||
7059|Gawler Range Volcanics|22873|6|Mentioned|P9||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|22923|6|Mentioned|19|||||||||
7059|Gawler Range Volcanics|23054|6|Mentioned|p14,24|||||||||
7059|Gawler Range Volcanics|23175|6|Mentioned|Fig.1||Mesoproterozoic|Gawler Craton||||||
7059|Gawler Range Volcanics|23204|6|Mentioned|p1363|||||||||
7059|Gawler Range Volcanics|23205|6|Mentioned|p43|||Age: 1600-1500Ma.||||||
7059|Gawler Range Volcanics|23248|6|Mentioned|p169|||||||||
7059|Gawler Range Volcanics|23397|6|Mentioned|p464 Fig.3|||||||||
7059|Gawler Range Volcanics|23445|5|Briefly described|p444|||||||||
7059|Gawler Range Volcanics|23481|5|Briefly described|p18|||See also Upper Gawler Range Volcanics and Lower Gawler Range Volcanics. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|23490|6|Mentioned|p22||Mesoproterozoic|Gawler Craton Province.||||||
7059|Gawler Range Volcanics|23719|4|Described|p22|Mesoproterozoic|Mesoproterozoic|See also page 22 table 6. Overlain by Pandurra Formation. Geological Province: Gawler Craton.||||||18-JAN-07
7059|Gawler Range Volcanics|23731|6|Mentioned|p43|||Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|23805|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|23818|5|Briefly described|p24 Fig.4|Calymmian|Calymmian|Geological Province: Gawler Block. Age: 1535 Ma.||||||
7059|Gawler Range Volcanics|24168|5|Briefly described|p634|Mesoproterozoic|Paleoproterozoic|Age : 1592+/-2Ma.||||||07-NOV-08
7059|Gawler Range Volcanics|24169|5|Briefly described|p672|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
7059|Gawler Range Volcanics|24176|6|Mentioned|p12|Carpentarian|Carpentarian|Age given as Carpentarian.||||||
7059|Gawler Range Volcanics|24197|6|Mentioned|p72|||Geological Province: Gawler Craton. Referred to as GRV in text.||||||07-FEB-11
7059|Gawler Range Volcanics|24217|4|Described|p831|Proterozoic|Proterozoic|Geological Province: Gawler Craton||||||
7059|Gawler Range Volcanics|24261|5|Briefly described|p1047 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton||||||
7059|Gawler Range Volcanics|24296|5|Briefly described|p1251 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1590 Ma. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|24346|4|Described|p97|Mesoproterozoic|Mesoproterozoic|New stratigraphic framework interpreted.||||||
7059|Gawler Range Volcanics|24356|4|Described|p1592|Mesoproterozoic|Mesoproterozoic|Continental intraplate felsic volcanics; dacite and rhyolite, with minor andesite and basalt.  Comagmatic with Hiltaba Suite.  Age: ca.1592Ma. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|24365|6|Mentioned|p4, 5 Fig.2|||||||||09-MAR-05
7059|Gawler Range Volcanics|24422|5|Briefly described|p87|Mesoproterozoic|Mesoproterozoic|Age: ca. 1600-1580 Ma. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|24424|5|Briefly described|p539 Tb.4|Calymmian|Calymmian|Age: 1585-1595 Ma. Palaeomagnetic poles given.||||||04-FEB-05
7059|Gawler Range Volcanics|24472|5|Briefly described|p4, p5. Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1590 Ma.||||||
7059|Gawler Range Volcanics|24475|6|Mentioned|p46|||||||||
7059|Gawler Range Volcanics|24476|4|Described|p545, p546 Fig. 1|Mesoproterozoic|Mesoproterozoic|Exposed Thickness: > 1km. Age: 1.59 Ga. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|24505|5|Briefly described|p4|||Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|24522|6|Mentioned|p82|Paleoproterozoic|Paleoproterozoic|Age: 1.6-1.55Ga.  Geological Province: Gawler Craton.||||||07-NOV-08
7059|Gawler Range Volcanics|24526|6|Mentioned|p97 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1592-1591Ma.  Geological Province: Gawler Craton. See also p96 Fig. 2.||||||07-NOV-08
7059|Gawler Range Volcanics|24597|5|Briefly described|p526, p528 Fig. 3|Mesoproterozoic|Mesoproterozoic|Age: ca1600-1590Ma. Geological Province: Gawler Craton.||||||10-MAR-10
7059|Gawler Range Volcanics|24606|6|Mentioned|p963|||||||||
7059|Gawler Range Volcanics|29838|2|Defined|p7|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7059|Gawler Range Volcanics|29873|5|Briefly described|p143|||Structural emphasis||||||
7059|Gawler Range Volcanics|30075|6|Mentioned|p11|||||||||
7059|Gawler Range Volcanics|30177|6|Mentioned|p54|||Lower Proterozoic?||||||
7059|Gawler Range Volcanics|30806|5|Briefly described|Table 1|||||||||
7059|Gawler Range Volcanics|30807|6|Mentioned|p103|||Suggested map symbol||||||
7059|Gawler Range Volcanics|30809|6|Mentioned|p5|||||||||
7059|Gawler Range Volcanics|30845|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|30918|6|Mentioned|p39|||||||||
7059|Gawler Range Volcanics|30984|6|Mentioned|p7|||||||||
7059|Gawler Range Volcanics|31034|6|Mentioned|Fig. 1|||Also mention on Fig. 2||||||
7059|Gawler Range Volcanics|31313|5|Briefly described|p196|||||||||
7059|Gawler Range Volcanics|31320|6|Mentioned|p13|||Carpentarian||||||
7059|Gawler Range Volcanics|31540|5|Briefly described|p8|||Carpentarian||||||
7059|Gawler Range Volcanics|31923|6|Mentioned|p5|||||||||
7059|Gawler Range Volcanics|32435|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|32436|6|Mentioned|p120|||||||||
7059|Gawler Range Volcanics|32437|6|Mentioned|Fig.2|||||||||
7059|Gawler Range Volcanics|32438|6|Mentioned|Fig.2|||||||||
7059|Gawler Range Volcanics|32507|6|Mentioned|Table 3|||||||||
7059|Gawler Range Volcanics|33004|6|Mentioned|p127|||||||||
7059|Gawler Range Volcanics|33468|6|Mentioned|p212|||See also Figs 2,6||||||
7059|Gawler Range Volcanics|33470|4|Described|p463|||||||||
7059|Gawler Range Volcanics|33472|6|Mentioned|p470|||||||||
7059|Gawler Range Volcanics|33479|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|33557|5|Briefly described|p12|||Refers Blissett (1975)||||||
7059|Gawler Range Volcanics|33727|6|Mentioned|p35|||||||||
7059|Gawler Range Volcanics|33828|6|Mentioned|p9|||||||||
7059|Gawler Range Volcanics|34287|6|Mentioned|p37|||||||||
7059|Gawler Range Volcanics|34535|6|Mentioned|Fig.16|||Carp.||||||
7059|Gawler Range Volcanics|34537|5|Briefly described|p31|||Carp.||||||
7059|Gawler Range Volcanics|34685|6|Mentioned|p353|||||||||
7059|Gawler Range Volcanics|34812|6|Mentioned|p89|||||||||
7059|Gawler Range Volcanics|34834|6|Mentioned|p219|||||||||
7059|Gawler Range Volcanics|34904|6|Mentioned|Fig. 1|||||||||
7059|Gawler Range Volcanics|35002|6|Mentioned|p28|||||||||
7059|Gawler Range Volcanics|35078|4|Described|p255|||Discussed throughout.||||||
7059|Gawler Range Volcanics|35107|6|Mentioned|p199|||||||||
7059|Gawler Range Volcanics|35130|6|Mentioned|p7|||||||||
7059|Gawler Range Volcanics|35255|5|Briefly described|p9|||See also Fig.3.||||||
7059|Gawler Range Volcanics|35270|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|35298|5|Briefly described|Table 1|||||||||
7059|Gawler Range Volcanics|35495|6|Mentioned|p341|||||||||
7059|Gawler Range Volcanics|35565|6|Mentioned|p22|||Stratigraphic drilling||||||
7059|Gawler Range Volcanics|35705|4|Described|p13|||Geochemistry discussed.||||||
7059|Gawler Range Volcanics|35706|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|36073|6|Mentioned|Fig.3|||||||||
7059|Gawler Range Volcanics|36214|6|Mentioned|p60|||||||||
7059|Gawler Range Volcanics|36507|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|36733|6|Mentioned|p49|||||||||
7059|Gawler Range Volcanics|37238|6|Mentioned|p368|||||||||
7059|Gawler Range Volcanics|37325|6|Mentioned|p7|||||||||
7059|Gawler Range Volcanics|37372|6|Mentioned|p18|||||||||
7059|Gawler Range Volcanics|37461|6|Mentioned|p309|||||||||
7059|Gawler Range Volcanics|37621|6|Mentioned|p14|||||||||
7059|Gawler Range Volcanics|37811|6|Mentioned|p225|||||||||
7059|Gawler Range Volcanics|38068|6|Mentioned|Fig.3|||P64||||||
7059|Gawler Range Volcanics|38157|6|Mentioned|p267|||||||||
7059|Gawler Range Volcanics|38604|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7059|Gawler Range Volcanics|38605|6|Mentioned|p15|||See also Table 2.||||||
7059|Gawler Range Volcanics|39047|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7059|Gawler Range Volcanics|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|39488|6|Mentioned|p2|||||||||
7059|Gawler Range Volcanics|39490|6|Mentioned|p11|||||||||
7059|Gawler Range Volcanics|39762|6|Mentioned|Table 1|||||||||
7059|Gawler Range Volcanics|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|39872|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|39901|6|Mentioned|p13|||||||||
7059|Gawler Range Volcanics|39949|5|Briefly described|p272|||||||||
7059|Gawler Range Volcanics|40003|5|Briefly described|p54|||||||||
7059|Gawler Range Volcanics|40105|6|Mentioned|p317|||||||||
7059|Gawler Range Volcanics|40241|6|Mentioned|p115|||||||||
7059|Gawler Range Volcanics|40430|6|Mentioned|p7|||||||||
7059|Gawler Range Volcanics|40447|6|Mentioned|p66|||||||||
7059|Gawler Range Volcanics|40448|5|Briefly described|p32|||||||||
7059|Gawler Range Volcanics|40490|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|40644|4|Described|p120 Fig. 2, p121|||Consists predominantly of acid ash flows (Ignimbrites) which are intensely welded, and acid lavas. Geological province: Gawler Craton.||||||02-JUN-09
7059|Gawler Range Volcanics|40942|6|Mentioned|p13|||||||||
7059|Gawler Range Volcanics|41085|6|Mentioned|p88|||||||||
7059|Gawler Range Volcanics|41125|6|Mentioned|Fig.17|||||||||
7059|Gawler Range Volcanics|41239|6|Mentioned|p95|||||||||
7059|Gawler Range Volcanics|41256|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|41402|6|Mentioned|p35|||||||||
7059|Gawler Range Volcanics|41404|6|Mentioned|p89|||||||||
7059|Gawler Range Volcanics|41405|6|Mentioned|p128|||||||||
7059|Gawler Range Volcanics|41493|6|Mentioned|Table 1|||||||||
7059|Gawler Range Volcanics|41499|5|Briefly described|Fig.1|||||||||
7059|Gawler Range Volcanics|41609|6|Mentioned|Fig.1|||||||||
7059|Gawler Range Volcanics|41619|6|Mentioned|Map legend|Holocene||||||||
7059|Gawler Range Volcanics|41667|6|Mentioned|p6|||||||||
7059|Gawler Range Volcanics|41833|6|Mentioned|p585|||||||||
7059|Gawler Range Volcanics|41953|6|Mentioned|p132|||||||||
7059|Gawler Range Volcanics|41957|5|Briefly described|p66|||||||||
7059|Gawler Range Volcanics|41972|4|Described|p377|||||||||
7059|Gawler Range Volcanics|41974|4|Described|p407|||||||||
7059|Gawler Range Volcanics|41995|6|Mentioned|p16|||||||||
7059|Gawler Range Volcanics|42022|6|Mentioned|p3|||||||||
7059|Gawler Range Volcanics|42095|6|Mentioned|p29|||||||||
7059|Gawler Range Volcanics|42167|6|Mentioned|Fig.2 P115|||||||||
7059|Gawler Range Volcanics|42222|6|Mentioned|p19|||||||||
7059|Gawler Range Volcanics|42224|6|Mentioned|p61|||||||||
7059|Gawler Range Volcanics|42239|6|Mentioned|p152|||||||||
7059|Gawler Range Volcanics|42283|5|Briefly described|p80|||||||||
7059|Gawler Range Volcanics|42292|6|Mentioned|Fig.1 P9|||||||||
7059|Gawler Range Volcanics|42341|4|Described|p53|Mesoproterozoic||||||||
7059|Gawler Range Volcanics|42357|6|Mentioned|p8|||1590Ma||||||
7059|Gawler Range Volcanics|42368|5|Briefly described|p48|Mesoproterozoic||||||||
7059|Gawler Range Volcanics|42404|6|Mentioned|p32|||||||||
7059|Gawler Range Volcanics|42465|5|Briefly described|Map Legend|||||||||
7059|Gawler Range Volcanics|42466|5|Briefly described|Map Legend|||||||||
7059|Gawler Range Volcanics|42468|5|Briefly described|p3, Fig.1 p2|||||||||
7059|Gawler Range Volcanics|42469|4|Described|p14|||"Older" sequence, KINGOONYA 1:250 000 sheet Mesoproterozoic.||||||18-JAN-07
7059|Gawler Range Volcanics|42470|6|Mentioned|p17|||||||||
7059|Gawler Range Volcanics|42475|5|Briefly described|p15|||||||||
7059|Gawler Range Volcanics|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
7059|Gawler Range Volcanics|42570|5|Briefly described|p542|||||||||
7059|Gawler Range Volcanics|42624|5|Briefly described|p30|||||||||
7059|Gawler Range Volcanics|42716|5|Briefly described|Map legend|Mesoproterozoic||||||||
7059|Gawler Range Volcanics|42721|5|Briefly described|map legend|Carpentarian||||||||
7059|Gawler Range Volcanics|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|||||||07-APR-05
7059|Gawler Range Volcanics|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
7059|Gawler Range Volcanics|42777|5|Briefly described|p291|||||||||
7059|Gawler Range Volcanics|42779|5|Briefly described|p283|||||||||
7059|Gawler Range Volcanics|42816|6|Mentioned|p10|||||||||
7059|Gawler Range Volcanics|42934|5|Briefly described|p520|||||||||
7059|Gawler Range Volcanics|43048|5|Briefly described|p17|||||||||
7059|Gawler Range Volcanics|43049|5|Briefly described|p13|||||||||
7059|Gawler Range Volcanics|43052|3|Fully described|p107|||Age of about 1592 Ma.||||||18-JAN-07
7059|Gawler Range Volcanics|43071|5|Briefly described|p12|||see also Table 2.||||||
7059|Gawler Range Volcanics|43086|6|Mentioned|p1|||||||||
7059|Gawler Range Volcanics|43094|4|Described|p15|||||||||
7059|Gawler Range Volcanics|43141|6|Mentioned|p63,Fig.1|||||||||
7059|Gawler Range Volcanics|43202|6|Mentioned|p17||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|43561|6|Mentioned|Fig.3,p1434|||1595-1985 Ma||||||
7059|Gawler Range Volcanics|43583|6|Mentioned|p2163|||Age: 1600 Ma||||||
7059|Gawler Range Volcanics|43595|5|Briefly described|p76,Fig.3-46,p352|||Age: 1.6 Ga||||||
7059|Gawler Range Volcanics|43621|6|Mentioned|p27|||||||||
7059|Gawler Range Volcanics|43634|6|Mentioned|p12|||||||||
7059|Gawler Range Volcanics|43650|6|Mentioned|p443||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|43651|5|Briefly described|p431||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|43652|6|Mentioned|p393||Neoproterozoic|||||||
7059|Gawler Range Volcanics|43839|5|Briefly described|p29, Fig2 p30|||In Gawler Craton||||||12-JUL-16
7059|Gawler Range Volcanics|44660|14|Not recorded|map legend||Carpentarian|Carpentarian, lithology.||||||
7059|Gawler Range Volcanics|44695|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|44934|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7059|Gawler Range Volcanics|44935|5|Briefly described|Map Legend||Proterozoic|||||||
7059|Gawler Range Volcanics|50081|5|Briefly described|p42|Calymmian|Calymmian|Age: ~1600-1575 Ma. Geological Province: Gawler Craton.||||||24-FEB-05
7059|Gawler Range Volcanics|50127|6|Mentioned|p48 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|50130|5|Briefly described|p4 Fig.3|Mesoproterozoic|Mesoproterozoic|Age: 1590 Ma. Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|||||||07-FEB-11
7059|Gawler Range Volcanics|50605|6|Mentioned|p1.1|||Geological Province: Gawler Craton & Curnamona Province.||||||
7059|Gawler Range Volcanics|60484|5|Briefly described|p33 Fig. 1|||Divided into Upper and Lower units in the map figure. Geological Province: Gawler Craton.||||||10-MAR-10
7059|Gawler Range Volcanics|60496|5|Briefly described|p22 Fig. 1, p23|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|60515|6|Mentioned|p115, p122 Tb.1|||Gawler Craton. Abbreviated to GRV in Tb.1.|c.1600-1580 Ma.|||||
7059|Gawler Range Volcanics|60657|5|Briefly described|p13 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Geological Province: Gawler Craton.||||||10-MAY-05
7059|Gawler Range Volcanics|60704|5|Briefly described|p685, p686 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||11-APR-05
7059|Gawler Range Volcanics|60707|6|Mentioned|p612|Mesoproterozoic|Mesoproterozoic|Age: 1592Ma (Fanning et al 1988).||||||
7059|Gawler Range Volcanics|60900|6|Mentioned|p897|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma.  In South Australia.||||||
7059|Gawler Range Volcanics|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
7059|Gawler Range Volcanics|61307|5|Briefly described|p36 Fig. 17|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||15-JAN-08
7059|Gawler Range Volcanics|61393|5|Briefly described|p166 Fig.1, p169, p177. |Mesoproterozoic|Mesoproterozoic|Upper and Lower parts are mapped separately in Fig.1. Voluminous felsic, and subordinate mafic, magmatic rocks. |c.1590 Ma.|||||
7059|Gawler Range Volcanics|61411|6|Mentioned|p3.|||||||||
7059|Gawler Range Volcanics|61412|6|Mentioned|p51.|||||||||
7059|Gawler Range Volcanics|61522|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|Age: ~1595-1575Ma. Geological Province: Gawler Craton.||||||02-JUN-06
7059|Gawler Range Volcanics|61556|5|Briefly described|p9-10 Figure|Carpentarian|Carpentarian|||||||
7059|Gawler Range Volcanics|61560|5|Briefly described|p486|Mesoproterozoic|Mesoproterozoic|Dacitic lavas. Age: ca.1590Ma. These rocks contain the Acraman impact crater on the Eyre Peninsula (SA), with shatter cones proving its origin; the depression contains Lake Acraman.||||||
7059|Gawler Range Volcanics|61565|5|Briefly described|p607, p611 Fig.7|Mesoproterozoic|Mesoproterozoic|Age: 1.59Ga.  Geological Province: Gawler Craton.||||||20-APR-06
7059|Gawler Range Volcanics|61659|4|Described|p30 Fig.1, p31, pp37-38.  |Mesoproterozoic|Mesoproterozoic|Gawler Craton. Co-magmatic with Hiltaba Suite. S.G. = 2.59 +/- 0.09. Has high (1000 - 1200 nT) continuous magnetic response.|1589-1578 Ma (Daly et al. 1998).|||Overlies part of the Mulgathing Complex.||
7059|Gawler Range Volcanics|61732|6|Mentioned|p39, p40|||Geological Province: Gawler Craton.||||||07-FEB-11
7059|Gawler Range Volcanics|61733|5|Briefly described|p57-58|||One of the world's largest felsic extrusive magmatic events: over 100,000 km2.|c.1595 Ma.||||Voluminous rhyolites, dacites and basalts.|
7059|Gawler Range Volcanics|61735|6|Mentioned|p654|||In S.A.||||||30-JUN-09
7059|Gawler Range Volcanics|61736|6|Mentioned|p665|||Geological province: Gawler Craton.||||||
7059|Gawler Range Volcanics|61864|6|Mentioned|p16 fig 3|||||||||
7059|Gawler Range Volcanics|61936|6|Mentioned|p204|||Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|62535|6|Mentioned|p665|||Gawler Craton.||||||
7059|Gawler Range Volcanics|62536|5|Briefly described|p654|||Likely synchronous with magmatism in the Broken Hill area.|~1600 Ma.||||Felsic magmatism.|
7059|Gawler Range Volcanics|62592|6|Mentioned|pp74.|||Gawler Craton. Coeval with Gawler Range Volcanics.||||||
7059|Gawler Range Volcanics|62641|6|Mentioned|p277 Fig.1, p287 Fig.10(c). |||Interpreted as extensional inboard expression of outboard S-dipping subduction.|1.59 Ga.||||Rhyolites, dacites and basalts.|
7059|Gawler Range Volcanics|62727|5|Briefly described|p9|Mesoproterozoic|Paleoproterozoic|Includes the Corunna Conglomerate. Uranium-enriched rocks.  Geological Province: Gawler Craton.||||||07-NOV-08
7059|Gawler Range Volcanics|62729|5|Briefly described|p39 Fig. 1b, p40|Mesoproterozoic|Mesoproterozoic|Age: 1590 to ~1575 Ma. Mainly mafic rocks. Geological Province: Gawler Craton.||||||25-JAN-07
7059|Gawler Range Volcanics|62893|6|Mentioned|p15, p28-29|Calymmian|Calymmian|Extensive anorogenic extrusives.|ca 1592 Ma|||Equivalent to Hiltaba Suite.||
7059|Gawler Range Volcanics|62963|5|Briefly described|p28, p29|Mesoproterozoic|Mesoproterozoic|Includes the Yardea Dacite. Age: ~1592+/-3Ma.  Geological province: Gawler Craton, Yorke Peninsula region.||||||
7059|Gawler Range Volcanics|62978|5|Briefly described|p161|Mesoproterozoic|Mesoproterozoic|Essentially undeformed units. Age: ~1590Ma. Geological Province: Gawler Craton.||||||07-FEB-11
7059|Gawler Range Volcanics|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Geological Province: Gawler Craton.||||||10-AUG-07
7059|Gawler Range Volcanics|63067|5|Briefly described|p2 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Dacite, rhyodacite, rhyolite, basalt, andesite, felsic pyroclastic rocks.||||||
7059|Gawler Range Volcanics|63102|5|Briefly described|p42|||Geological province: Gawler Craton. Temporally equivalent to Bimbowrie Supersuite.||||||
7059|Gawler Range Volcanics|63223|5|Briefly described|p17 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||30-APR-07
7059|Gawler Range Volcanics|63275|5|Briefly described|p13-18.|Early Mesoproterozoic|Early Mesoproterozoic|Gawler Craton.||||||
7059|Gawler Range Volcanics|63398|5|Briefly described|p670|Mesoproterozoic||Geological Province: Gawler Craton. ||||||
7059|Gawler Range Volcanics|63776|6|Mentioned|p1089, p1092|||Geological Province: Gawler Craton.||||||
7059|Gawler Range Volcanics|63866|5|Briefly described|p3, p7, p10, p13, p19-p21|Mesoproterozoic|Mesoproterozoic|Associated with mineralisation in the gawler craton and comprises extensive gold-onlu and IOCG+U mineralisation.|ca. 1600-1575 Ma|||Overlain by the Pandurra Formation.||
7059|Gawler Range Volcanics|64130|5|Briefly described|p1377-1378 Fig.1, p1380 Fig.2      |Mesoproterozoic|Mesoproterozoic|See also p1383, p1836 Fig.5, p1387-1392. Comagmatic with Hiltaba Volcanics. Ages suggest eruption over short period.|1592+/-3 Ma(upper)-1591+/-3 Ma (lower).|||Comagmatic with the Hiltaba Suite. Associated with the Corunna Conglomerate and Mentor Formation.|Upper part consists of dominantly felsic volcanic rocks (dacite-rhyodacite-rhyolite). Lower part contains sequences of basalt, andesite, dacite, rhyodacite and rhyolite.|
7059|Gawler Range Volcanics|64131|4|Described|p1397-1411        |||Hosts the sub-economic Acropolis occurrence, and the Prominent Hill deposit. Petrophysical properties.|ca. 15.9 Ga||Includes the Yardea Dacite.|Comagmatic with the Hiltaba Suite. Intrudes and is interlayered with the coeval Corunna Conglomerate.|Comprises a lower sequence of rhyodacite, rhyolites and basalts and an upper sequence of rhyodacite and rhyolite.|
7059|Gawler Range Volcanics|64132|5|Briefly described|pp1415-1421, p1424, p1430, p1432-1434.  |Mesoproterozoic|Mesoproterozoic|Gawler Craton. Generally flat-lying and essentially unmetamorphosed units. Comagmatic with the Hiltaba Suite.|1591 +/- 10 Ma.|||Is overlain unconformably by Pandurra Formation.|Large-volume, felsic-dominated bimodal igneous province.|
7059|Gawler Range Volcanics|64133|5|Briefly described|p1441-1449, p1456-1458, p1460-1465   |||Most precise age, from the central Gawler Craton.|1591 +/- 3 Ma (Fanning et al., 1988).||||Felsic dominated bimodal volcanic sequences. Contains both I- and A-type compositions.|
7059|Gawler Range Volcanics|64135|5|Briefly described|p1499, p1501, p1504. |Mesoproterozoic|Mesoproterozoic|Central and eastern Gawler Craton. Voluminous, bimodal, subaerial and submarine volcanism with associated hydrothermal alteration, brecciation and IOGC mineralisation. |c.1600 - 1580 Ma (Ferris et al. 2002).|||||
7059|Gawler Range Volcanics|64137|5|Briefly described|p1542 Fig.1, p1543,   |Mesoproterozoic|Mesoproterozoic|Associated with what the authors refer to as Hiltaba Association Granites [formal names are Hiltaba Granite, part of Hiltaba Suite].||||||
7059|Gawler Range Volcanics|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. See also p451 Fig.2a.||||||09-FEB-10
7059|Gawler Range Volcanics|64576|6|Mentioned|p625, p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ca. 1592Ma. ||||||
7059|Gawler Range Volcanics|64722|5|Briefly described|Fig. 2 p3-6, p14|Calymmian|Calymmian|Geochemical data indicate a within-plate, possibly backarc, tectonic setting.|1600-1575 Ma.|||Coeval with and genetically related to A-type felsic plutons of the Hiltaba Suite.|Bimodal unit containing felsic and mafic lavas and ignimbrites.|11-APR-12
7059|Gawler Range Volcanics|64725|6|Mentioned|p55, p58 Fig.2. |||Large-scale bimodal magmatism.||||||
7059|Gawler Range Volcanics|64739|6|Mentioned|p264 Fig.1, p265 Table 1, p266. |Mesoproterozoic|Mesoproterozoic|Gawler Craton. Shown as Upper and Lower Gawler Range Volcanics in Fig.1.|1589-1578 Ma.|||||
7059|Gawler Range Volcanics|64740|6|Mentioned|p284 Fig.1, p285, pp293-294.|Mesoproterozoic|Mesoproterozoic|An enriched felsic suite associated with postulated near margin continental back-arc setting at the northern margin of Archean Gawler Craton. Shown as Upper and Lower Gawler Range Volcanics in Fig.1.||||Intrudes and overlies St Peter Suite.||29-MAR-12
7059|Gawler Range Volcanics|64741|6|Mentioned|p299 Fig. 2, p311|||Geological province: Gawler Craton.||||||07-FEB-11
7059|Gawler Range Volcanics|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Mesoproterozoic|Volcanics have been informally subdivided into Upper and Lower Gawler Range Volcanics. Geological province: Gawler Craton.||||||04-MAR-09
7059|Gawler Range Volcanics|65219|6|Mentioned|p27 Fig.1|||||||||22-SEP-09
7059|Gawler Range Volcanics|65220|5|Briefly described|p19-22, Fig.4, Fig.1|Mesoproterozoic|Mesoproterozoic|1590-1580 Ma, High temperature magmatism and enriched geochemical signature. Also informally subdivided into three units in Fig.1 - Upper, Lower and Lower (mafic).||||||10-DEC-09
7059|Gawler Range Volcanics|65221|5|Briefly described|p25, 26, 32|Mesoproterozoic|Mesoproterozoic|Intrudes Wallaroo Group, Moonabie Formation and McGregor Volcanics||||||21-SEP-09
7059|Gawler Range Volcanics|65375|6|Mentioned|p13, p24.|||||||||
7059|Gawler Range Volcanics|65376|5|Briefly described|p9 Fig.1.2, p10, pp138-146.|Mesoproterozoic|Mesoproterozoic|One of the world's largest felsic volcanic provinces (25,000 km2). Hosts the Central Gawler Gold Province. Mineralisation during the late stages of porphyritic rhyolite intrusion occurred c.1595 Ma.|1604 +/- 11 Ma to 1583 +/- 12 Ma|||Co-magmatic with Hiltaba Suite.|Lower part has a variable assemblage from basalt and andesite to dacite, rhyodacite and rhyolite; upper part has massive porphyritic dacite and rhyodacite.|
7059|Gawler Range Volcanics|65385|6|Mentioned|pS128 Fig.2, pS129, pS131-132, pS135|Calymmian|Calymmian|1593 +/-3 Ma (Fanning et al., 1988).||||||08-MAR-12
7059|Gawler Range Volcanics|65390|5|Briefly described|p17-9, p22 Fig. 3, 24, 26|Statherian|Statherian|Dominant Proterozoic outcropping unit on the Gawler Craton. Dominantly felsic lavas and ignimbrites, with minor mafic lavas. Intruded by Hiltaba Suite. This unit and Hiltaba Suite emplaced between 1595 and 1575 Ma. Unconformably underlies Pandurra Formation.||||||
7059|Gawler Range Volcanics|65455|6|Mentioned|p9 Fig. 5|||||||||
7059|Gawler Range Volcanics|65483|6|Mentioned|p17, Fig. 1|Calymmian|Calymmian|Coeval with  Hiltaba Suite granites.||||||
7059|Gawler Range Volcanics|65772|6|Mentioned|p228, p229 Fig.2|Calymmian|Calymmian|1595-1575 Ma||||||
7059|Gawler Range Volcanics|65892|6|Mentioned|p38. |Mesoproterozoic|Mesoproterozoic|The suggested source of the thin layer of porphyritic rhyolite fragments found in the Bunyeroo Formation, Central Flinders Ranges, after a bolide impact at Lake Acraman.||||||
7059|Gawler Range Volcanics|65915|5|Briefly described|p3 Fig.2, p4 Fig.3, p18|Calymmian|Calymmian|~1590 Ma. Its extensive cover may obscure the extent of ~3150 Ma crust.||||||
7059|Gawler Range Volcanics|65922|4|Described|p9-13, p16-23, p29 Fig. 6, p31-32|Calymmian|Calymmian|Split into lower (including Bittali Rhyolite and Waganny Dacite) and upper (Nonning and Yannabie Rhyodacites, Eucarro and Yardea Dacites, Paney Rhyolite) sequences; in this map the boundary is the base of the Nonning Rhyodacite. Intrudes Warrow Quartzite and Sleaford Complex. Has U-Pb zircon ages of 1591 +/-3 Ma (Waganny Dacite) and 1592 +/-3 Ma (Yardea Dacite); possibly erupted over less than 5 My.||||||
7059|Gawler Range Volcanics|65925|6|Mentioned|p12, p15.|||Uranium-rich felsic volcanics. Compositionally similar to Benagerie Volcanics. ||||||
7059|Gawler Range Volcanics|66302|5|Briefly described|p23, p32-33, p41-42, p44-45, p48, p52|Calymmian|Calymmian|Harris Greenstone and Nuyts Domains, Gawler Craton. Maximum thickness of 1.5km. Ages are derived from Fanning et al. (1988), Creaser (1995) and Johnson and Cross (1995). See also p56, p69-70, p72, p74-75, p84, p92.|1592 +/- 3 Ma to 1591 +/- 3 Ma||Includes the Ealbara Rhyolite||Felsic volcanics.|
7059|Gawler Range Volcanics|66519|6|Mentioned|pp31-32.|Early Mesoproterozoic|Early Mesoproterozoic|Gawler Craton. Associated with a major tectonic/tectonothermal episode; associated with major mineral systems including Cu-Au-U-rare earth elements and Au-only mineralisation.|c.1595 Ma.|||||
7059|Gawler Range Volcanics|66520|5|Briefly described|p9, p15-17.  |Mesoproterozoic|Mesoproterozoic|Mafic rocks. Basalts are enriched in all REE.|c.1592 Ma.||||Basalt.|
7059|Gawler Range Volcanics|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Gawler Craton. Likely source of zircons of this age found in Kooringa Member.|c.1590 Ma.|||||
7059|Gawler Range Volcanics|66537|6|Mentioned|p11, p15.|Proterozoic|Proterozoic|To the west of Cariewerloo Basin, this unit is likely source of sediments of Pandurra Formation.||||||
7059|Gawler Range Volcanics|66569|5|Briefly described|p859,||Mesoproterozoic|Includes Yardea Dacite.||||||
7059|Gawler Range Volcanics|66575|6|Mentioned|p948-949.|||Coeval with Hiltaba Suite. Felsic.||||||
7059|Gawler Range Volcanics|66882|6|Mentioned|p102 Fig.2, p117|Calymmian|Calymmian||c.1590 Ma|||||
7059|Gawler Range Volcanics|66916|5|Briefly described|p7, p9, p10 Fig.4, p16|Calymmian|Calymmian|Part of the Olympic IOCG Province. Appears to have acted as a relatively impermeable barrier, confining higher grade mineralisation at Punt Hill to the contact with underlying sedimentary pile.|c.1590-1580 Ma.||||Includes felsic crystal-lithic tuffs and volcaniclastics; variably hematite-altered.|
7059|Gawler Range Volcanics|67027|4|Described|p348, pp349-351. |Mesoproterozoic|Mesoproterozoic|Palaeomagnetic data is discussed.|1592 +/- 3 Ma (U-Pb zircon: Fanning et al. 1988).|||Is intruded by Hiltaba Suite. Is overlain by Pandurra Formation.|Massive, pink, porphyritic rhyolite and dacite.|
7059|Gawler Range Volcanics|67028|4|Described|p361-362, p367, p372-3|Calymmian|Calymmian|Gawler Craton. Information on magnetic characteristics presented, indicating Devonian magnetic overprint. Age of eruption from Fanning et al. (1988), include both A-type and I-type volcanics, dominantly felsic, can be divided into upper (Kokatha-type) and lower (Roxby Downs-type, more oxidised) groups.|1590 Ma, 1592 +/- 2 Ma||Black Yardea Dacite, Bittali Rhyolite, Eucarro Dacite, Yannabie Rhyodacite, Paney Rhyolite, Yardea Dacite, Eucarro Rhyolite.|Intruded by Hiltaba Suite Granitoids at ~1575 Ma. Co-magmatic with Hiltaba Suite Granitoids.|Dacite-rhyodacite-rhyolite lava domes and flows; ignimbrites with thick intercalated sequences of basaltic lavas; porphyritic dacite sheets predominantly ignimbrite in origin; magnetite, ilmenite and titanomagnetite|10-AUG-15
7059|Gawler Range Volcanics|67058|5|Briefly described|p477 Fig. 1|Mesoproterozoic|Mesoproterozoic|Gawler Craton|1590 Ma|||||19-APR-12
7059|Gawler Range Volcanics|67127|5|Briefly described|p104|||Enriched in REE, Y and fluorine. Whole rock geochemistry suggests that high fluorine concentration in the melt caused REE to behave incompatibly during magmatic crystallisation, thus producing an REE-rich late stage fluid.||||Coeval with the Hiltaba Suite.|Rhyolites.|
7059|Gawler Range Volcanics|67181|5|Briefly described|p616 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|1590 Ma|||||
7059|Gawler Range Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p36|||Central and northern Gawler Craton. Erupted during the Hiltaba Event.|1592 +/- 3 Ma.|||||
7059|Gawler Range Volcanics|67462|5|Briefly described|Map legend.|||||||||
7059|Gawler Range Volcanics|67536|5|Briefly described|Map Legend|Calymmian|Statherian|Gawler Craton. Informally subdivided into four parts. Inheritance, Cultana ca. 1670Ma |1597 +/- 8 Ma - 1589 +/- 16 Ma||||Mafic to felsic volcanic rocks: dacite and rhyodacite (upper); mafics, dacite to rhyolite, andesite, basalt (lower).|
7059|Gawler Range Volcanics|67540|6|Mentioned|p25, p37|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Contemporaneous with granitic magmatism of Hiltaba Suite.||||||
7059|Gawler Range Volcanics|67581|6|Mentioned|p44 Fig.8, p45|||Gawler Craton.|1600-1575 Ma.|||||
7059|Gawler Range Volcanics|67621|6|Mentioned|p211-212, 222-224|||Gawler Craton.|1592 +/- 2 Ma (Turner, 1975).|||Co-magmatic with Hiltaba Granite Suite.||
7059|Gawler Range Volcanics|67721|6|Mentioned|p32 Fig.1|||||||||
7059|Gawler Range Volcanics|67870|5|Briefly described|p11, p13, p15, p20, p24|Mesoproterozoic|Mesoproterozoic|Produces strong, subhorizontal to gently-dipping seismic reflections.|c.1585 Ma.|||Unconformably overlies the Wallaroo Group.||
7059|Gawler Range Volcanics|67900|5|Briefly described|p17-20, 22, 28, 30-32|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Shares geochronological, geochemical and isotopic affinities (elaborated in this study), with the upper part of the Benagerie Volcanic Suite, implying joint membership of a formerly contiguous silicic large igneous province. Several age determinations tabulated. Also appears as GRV. See also references to Lower Gawler Range Volcanics (p19-20, 30-31, 33) and Upper Gawler Range Volcanics (p19-20, 30, 33).|1591 +/- 3 Ma (TIMS; Fanning et al.,1988).|||Is overlain by Benagerie Volcanic Suite.|A-type.|
7059|Gawler Range Volcanics|67909|4|Described|p124-126, 137-141|Mesoproterozoic|Mesoproterozoic|Gawler Silicic-dominated Large Igneous Province. Emplaced over ~2 m.y. Subaerial intracontinental emplacement. After the first mention, it appears in text as GRV. Essentially undeformed and unmetamorphosed.|1592-1591 Ma.||Gawler Range Volcanics, lower and Gawler Range Volcanics, upper. Yardea Dacite.|Co-magmatic with, and locally intruded by, Hiltaba Suite.|Voluminous felsic lavas and ignimbrites, and minor mafic to intermediate units.|
7059|Gawler Range Volcanics|67912|6|Mentioned|p13 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
7059|Gawler Range Volcanics|67980|5|Briefly described|p548 Fig.1b, p566|Calymmian|Calymmian|Extrusive equivalent of Hiltaba Suite.|c.1590 Ma (Fanning et al., 1998).|||||
7059|Gawler Range Volcanics|68030|6|Mentioned|p238|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
7059|Gawler Range Volcanics|68100|6|Mentioned|p32, 34|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|1600-1580 Ma|||||
7059|Gawler Range Volcanics|68126|5|Briefly described|p3, p21|||Gawler Craton. Geochemically similar to Benagerie Volcanics.|||Waganny and Yardea Dacites.||Includes fine-grained rhyolites with phenocrysts of embayed quartz; displays flow banding.|
7059|Gawler Range Volcanics|68128|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|c. 1593 Ma|||||
7059|Gawler Range Volcanics|68131|5|Briefly described|p2 Fig.1, p82, p92-93|Mesoproterozoic|Mesoproterozoic||c.1595-1580 Ma.|||Intrudes Muckanippie Anorthosite.|Acid and lesser basic volcanic rocks.|
7059|Gawler Range Volcanics|68158|5|Briefly described|p4-5||||~1595 Ma.||Moonaree, Pondanna, Waganny Dacites; Paney, Yannabie, Eucarro, Nonning, Bittali Rhyolites.|||
7059|Gawler Range Volcanics|68208|6|Mentioned|p39, p31 Fig.1, p32 Fig.3|Mesoproterozoic|Mesoproterozoic||c. 1593 Ma|||||
7059|Gawler Range Volcanics|68269|6|Mentioned|p673|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Affected by the c. 90-km diameter Acraman impact structure.||||||
7059|Gawler Range Volcanics|68714|6|Mentioned|p16|||||||Overlain by the Pandurra Formation.||
7059|Gawler Range Volcanics|68715|6|Mentioned|p28|||Radiogenic granitic rocks; potential source areas for U.||||||07-APR-17
7059|Gawler Range Volcanics|69003|6|Mentioned|p48 Fig.57|||South Australian Craton. Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.||||||
7059|Gawler Range Volcanics|69004|4|Described|p12, p16, p18|Mesoproterozoic|Palaeoproterozoic|Gawler Craton. Co-magmatic with the Hiltaba Suite. Forms a massive felsic volcanic province. Over 25 000km ^2 of outcrop occurs across the region. The source of widespread Cu-Au-U mineralisation across the Gawler Craton. Sub-divided into Upper and Lower parts on p18.|~1590 Ma||||Dacitic to rhyolitic volcanics, ignimbrites and interlayered basaltic flows.|
7059|Gawler Range Volcanics|69019|5|Briefly described|p30 Fig.10, p58.|Calymmian|Calymmian|Gawler Craton. Mafic and felsic volcanics. Clasts containing shocked quartz, evidence of Acraman bolide impact, occur in Bunyeroo Formation in Flinders Ranges area.|c.1600-1590 Ma.|||||
7059|Gawler Range Volcanics|69023|6|Mentioned|p27 Fig.8, p52|||Gawler Craton.||||||
7059|Gawler Range Volcanics|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.||||||
7059|Gawler Range Volcanics|69091|6|Mentioned|p206|||||||||
7059|Gawler Range Volcanics|69203|6|Mentioned|p59||||c.1590 Ma.|||||
7059|Gawler Range Volcanics|69255|5|Briefly described|p788|Calymmian|Calymmian|Part of a large, mainly felsic, magmatic system which included also the Hiltaba Suite intrusives. Associated with IOCG mineralisation.|1592 Ma.|||Correlated with Benagerie Ridge Volcanics.|Felsic volcanics with minor mafic units.|
7059|Gawler Range Volcanics|69554|6|Mentioned|p128|Mesoproterozoic|Mesoproterozoic|Central Gawler Craton. Part of a voluminous felsic large igneous province. Associated with a number of Au and Ag-Au deposits.|c.1590 Ma.|||||
7059|Gawler Range Volcanics|69591|6|Mentioned|p109 Fig.2.106, p110|||Appears in a diagram of the geodynamic setting of ~1620-1570 Ma eastern Australia. Coeval with Hiltaba Granite.|~1595-1575 Ma.|||||
7059|Gawler Range Volcanics|69648|6|Mentioned|p34|||||||||
7059|Gawler Range Volcanics|69649|5|Briefly described| p16-26, p5, p6 Fig.4, p7, p8 Fig.6, p26|Mesoproterozoic|Mesoproterozoic|See also p34, p36, p41-42, p49, p58. Obscures the E boundary of the Nuyts Domain. An integral part of the deformation/tectonic history of the W Gawler Craton. |1595-1575 Ma.||Includes Waganny and Yardea Dacites; Chitanilga Volcanic Complex; Glyde Hill Volcanic Complex.||Subaerial felsic volcanics, dominantly as lava flows, domes and dykes, with minor ashflow and ignimbrite layers.|23-FEB-15
7059|Gawler Range Volcanics|69650|6|Mentioned|p1|||Gawler Craton.||||||04-FEB-16
7059|Gawler Range Volcanics|69654|6|Mentioned|p1, 11, 25|||Gawler Craton.||||||
7059|Gawler Range Volcanics|69666|6|Mentioned|p24, p28|Mesoproterozoic|Mesoproterozoic||||Roopena Volcanics.|||
7059|Gawler Range Volcanics|69742|6|Mentioned|p790|Mesoproterozoic|Mesoproterozoic|May be silica source for opal in Mintabie Beds.||||||
7059|Gawler Range Volcanics|69748|6|Mentioned|p180|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|~1.6 Ga.||||Bimodal.|
7059|Gawler Range Volcanics|69946|6|Mentioned|p19, p21|Mesoproterozoic|Mesoproterozoic|Clasts of this unit occur in Bulldog Shale and Mount Anna Sandstone Member (Cadna-owie Formation).||||||
7059|Gawler Range Volcanics|70027|5|Briefly described|p56,58|Calymmian|Calymmian|Geological province: Gawler Craton. Emplaced into Gawler Craton ca. 1600-1570 Ma post-Kimban Orogeny. Coeval with Hiltaba Suite.|ca. 1600-1570 Ma|||||
7059|Gawler Range Volcanics|70286|6|Mentioned|p883-886, 891-892|Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton.|c.1595-1587 Ma.||||Bimodal but dominantly felsic A-type magmatism.|
7059|Gawler Range Volcanics|70334|4|Described|p2-3,8,10,12-13,17,37,51,53-54,75-77,87|Calymmian|Calymmian|Geological province: Gawler Craton. Extensive felsic volcanism over the central-eastern Gawler Craton during early Mesoproterozoic (~1590 Ma) in response to lithospheric extension ans extensive intracrustal melting. Two models for the development of the Gawler Range Volcanics include underplating of mafic material from a mantle plume generating mafic magmatism during a development phase, followed by consequential high heat flow and lower crustal melting generating voluminous felsic magmatism during mature phase (Giles, 1980, Giles, 1988, Blissett et al., 1993, Betts et al., 2007); or a far-field continental back-arc setting accompanied locally by regional-scale high-temperature metamorphism and compressional deformation (Hand et al., 2007, Wade et al., 2012). Separated into two main packages: the lower GRV (mafic and felsic volcanics) and upper GRV (felsic volcanics; Blissett et al., 1993, Allen et al., 2003). Hosts several mineralisation styles, including IOCG-U, Pb-Zn skarn or epithermal mineralisation. See also p84.|~1590-1575 Ma|||Underlain by Moonabie Formation. Intruded by Hiltaba Suite.|Mafic package: basalt to andesite, felsic package: rhyolite to dacite.|14-OCT-19
7059|Gawler Range Volcanics|70382|6|Mentioned|p33|||Geological province: Gawler Craton. Associated with Hiltaba Suite||||||
7059|Gawler Range Volcanics|70405|6|Mentioned|p12 figure 4|Mesoproterozoic|Mesoproterozoic||1590 Ma |||||
7059|Gawler Range Volcanics|70502|6|Mentioned|p17-18, 25|||Gawler Craton. Described as a plausible magmatic metal source for the Olympic Dam IOCG deposit.|1.59 Ga.|||Intrudes Roxby Downs Granite and Olympic Dam Breccia Complex.|Felsic and mafic volcanics.|
7059|Gawler Range Volcanics|70511|5|Briefly described|p86-87, 91, 96, 98|Mesoproterozoic|Mesoproterozoic|Central and eastern Gawler Craton.|1591 Ma (Fanning et al., 1988).|||Intrudes Roxby Downs Granite and Olympic Dam Breccia Complex.|The lower part includes mafic (picritic and doleritic) and felsic lavas, felsic ignimbrites and other pyroclastic facies; the upper part is dominated by three large-volume rhyolite lavas. Flat-lying or gently dipping; unmetamorphosed.|
7059|Gawler Range Volcanics|70657|6|Mentioned|p48|||Gawler Craton. Temporal relationship with the Ninnerie Supersuite (Curnamona Province).|||||I-A type.|
7059|Gawler Range Volcanics|70658|6|Mentioned|p34|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|c.1592 Ma.||||Bimodal.|
7059|Gawler Range Volcanics|70659|4|Described|p1-14, p36-37, p42-43, p47-49, p57-59|Mesoproterozoic|Mesoproterozoic|Gawler Craton; also underlies Cariewerloo Basin and Stuart Shelf. Broadly synchronous with the Olarian Orogeny. Associated with granites of the Hiltaba and Munjeela Suites.|c.1590-1586 Ma||Includes Roopena Basalt, Fresh Well Formation, Angle Dam Volcanics, Ealbara Rhyolite, Konkaby Basalt, Bittali Rhyolite, Waganny Dacite|Equivalent to Benagerie Volcanic Suite and associated Ninnerie Supersuite.|Dacite to rhyolite, ignimbrites and tuffs with minor basalt. A-type.|
7059|Gawler Range Volcanics|70721|6|Mentioned|p63-p64|Mesoproterozoic|Mesoproterozoic||c. 1590 Ma (McAveny and Wade, 2015)|||||
7059|Gawler Range Volcanics|70738|5|Briefly described|p185-189, 191, 193-197|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Abbreviated to GRV in text after first couple of mentions. Maximum preserved thickness of 1.5 km. Exclusively sub-aerial volcanism. Former-olivine-bearing mafic units are examined in detail: lithologies, photomicrographs, geochemistry; major and trace element values.|c.1595-1575 Ma.|||Cogenetic with Hiltaba Suite.|Felsic-dominated; upper part comprises thick (250-300m), widespread rhyolitic and dacitic lavas; lower part ranges from basalt (10%) to dacite and rhyolite (90%) as lavas, ignimbrites and minor volcaniclastic facies.|
7059|Gawler Range Volcanics|70789|5|Briefly described|p316, p318 Fig.2, p319-322, p326, p328|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Abbreviated to GRV for most of the article. AFT results tabulated; central age 366 +/- 13 Ma.|c.1593 Ma.||||Extensive silicic lava flows.|
7059|Gawler Range Volcanics|70816|5|Briefly described|p1,4|Calymmian|Calymmian|Gawler Ranges region. Distributed over >25 000 km2 of the Gawler Craton, with a total extent (including subsurface) estimated at ~90,000 km2. Includes an unnamed sequence of felsic lava, ignimbrite and tuffaceous sediments. Intersected in drillhole RC 1 (number 20540)|~1590-1586 Ma||Includes Eucarro Rhyolite, Roopena Basalt.|Equivalent to the Benagerie Volcanic Suite|A-type felsic and lesser mafic volcanics.|30-MAY-19
7059|Gawler Range Volcanics|70829|6|Mentioned|p28, 34|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Mostly resistive, but with a large conductor at a depth of 80 km.|1595 Ma.|||Equivalent to Benagerie Volcanics.||
7059|Gawler Range Volcanics|70858|6|Mentioned|p31|||Gawler  Craton.|1595-1575 Ma.|||||
7059|Gawler Range Volcanics|70893|6|Mentioned|p1, p3 fig 1|Mesoproterozoic|Late Paleoproterozoic|A-type geochemical signatures. ||||||
7059|Gawler Range Volcanics|70947|5|Briefly described|p961|Calymmian|Calymmian|Geological province: Gawler Craton. Intruded by Hiltaba Suite granites.|ca. 1590 Ma|||Intruded by Hiltaba Suite granites.|Includes felsic feldspar-phyric lavas.|
7059|Gawler Range Volcanics|70948|6|Mentioned|p973, 975, 984|||Geological province: Gawler Craton.||||||
7059|Gawler Range Volcanics|71037|5|Briefly described|p20-21, p22-23 Fig.2, p24-p25|Mesoproterozoic|Mesoproterozoic|See also p26 Fig.5, p27 Fig.6.|c. 1590 -  Ma.||Includes Angle Dam Volcanics,Fresh Well Formation, Roopena Basalt, Spearfelt Rhyodacite, Eucarro Rhyolite and 4 unnamed subunits.|Co-magmatic with Hiltaba Suite.|Rhyodacite, rhyolite, dacite, basalt, tuff, siltstone, sandstone, mudstone, granitic and volcanic breccia.|
7059|Gawler Range Volcanics|71043|5|Briefly described|p104, p107|Calymmian|Calymmian|Gawler Craton. Flint et al. (1993). 25,000 km2 outcrop.|c.1595-1570 Ma.|||||
7059|Gawler Range Volcanics|71129|5|Briefly described|p1-2,14,16,18-19,35, 25,47-48,92|Calymmian|Calymmian|Geological Province: Gawler Craton. Abbreviated as GRV in text. A-type felsic and lesser mafic volcanism extruded c. 1595-1587 Ma (Allen et al., 2003, Allen et al., 2008, Jagodzinski et al., 2016) over Paleoproterozoic basement, associated with Munjeela and Hiltaba suites. Dominates the central part of the Gawler Craton. Coherent and fragmental felsic volcanics erupted from effusive-explosive volcanic centre/s, presumably in a predominantly subaerial environment, as well as basaltic lavas and volcaniclastic sediments erupted in a subaqueous environment. See also p94,98-99,101,109,114,116,122,149,152,187,203,206-207,210,225,227.|1595-1587 Ma||Includes Eucarro Rhyolite, Fresh Well Formation, Roopena Basalt, Angle Dam Volcanics and Spearfelt Volcanics.|Underlain unconformably by Broadview Schist.||13-NOV-19
7059|Gawler Range Volcanics|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Rhyodacite, rhyolite, dacite, basalt, tuff, siltstone, sandstone, mudstone, granitic and volcanic breccia.|
7059|Gawler Range Volcanics|71169|5|Briefly described|p78|Calymmian|Calymmian|Gawler Craton. Erupted during the Hiltaba Event.|1595-1575 Ma||||A-type felsic volcanic rocks.|
7059|Gawler Range Volcanics|71211|6|Mentioned|p1, p190, p197|||||||||
7059|Gawler Range Volcanics|71235|5|Briefly described|p1, p3-p8, p22|Mesoproterozoic|Mesoproterozoic|||||Intrudes the Corunna Conglomerate.|Porphyritic rhyolite.|16-MAR-23
7059|Gawler Range Volcanics|71236|5|Briefly described|iv, p1-p2, p30-p31, p34|Mesoproterozoic|Mesoproterozoic|Temporally and genetically associated with numerous IOCG deposits and prospects, including Olympic Dam, Prominent Hill, Oak Dam, Acropolis, Wirrda Well, Moonta-Wallaroo and Carrapateena. Hosts the Prominent Hill deposit.||||||
7059|Gawler Range Volcanics|71317|4|Described|p1-p2, p14-p16, p19-p21, |Mesoproterozoic|Mesoproterozoic|Gawler Craton. Deposited in association with magmatism of the Hiltaba Suite in a continental back arc setting. Referred to as the GRV on p114 and p143. See also p54, p56, p113-pl14, p134, p143, p146, p155, p158, p169, p175-p177, p191.|c. 1595-1587 Ma (Allen et al., 2003 and 2008)||Includes the Bittali Rhyolite, Eucarro Rhyolite, Mount Friday Formation, Yardea Dacite.|Overlies the Peter Pan Supersuite, Tunkillia Suite and Saint Peter Suite.|A-type felsic and lesser mafic volcanic rocks.|
7059|Gawler Range Volcanics|71322|5|Briefly described|p3, p91, p99-100, p135-137, p144, p147|Mesoproterozoic|Mesoproterozoic|This c.1595-1570 Ma magmatic event produced significant alteration in the central-northern Eyre peninsula and the eastern Gawler Craton. Associated with high level, epithermal Ag mineralisation at the Peterlumbo and Paris prospects. See also p185. Monzogranite porphyry at Peterlumbo Prospect dated at 1593+/-8 Ma, also rhyodacite 1597+/-14 Ma.|1593 +/- 8 Ma (porphyry); 1597 +/- 14 Ma (dacite).||||Includes a sericite-chlorite altered monzogranite porphyry, and a grey fine-grained rhyodacite.|14-DEC-21
7059|Gawler Range Volcanics|71341|6|Mentioned|p179 fig 1|Mesoproterozoic|Mesoproterozoic||ca. 1590 Ma|||||
7059|Gawler Range Volcanics|71342|5|Briefly described|Ch5 p19|Mesoproterozoic|Mesoproterozoic|Gawler Craton. ||||||
7059|Gawler Range Volcanics|71348|6|Mentioned|p200-201|Calymmian|Calymmian|Geological province: Gawler Craton.|1595-1575 Ma|||||
7059|Gawler Range Volcanics|71414|4|Described|p42-43, p47-48|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Lithological description based on MSDP01 core. Periods of mafic volcanism leading to stacked basaltic flows. Hiatus in basalt eruption replaced with middle felsic volcanics, lava flows and sills. Thickness exceeds 1,100 m in Six Mile Hill area, c.f. ~250 m in Roopena area. Shown as GRV in Fig 1.|~1590 Ma||Includes Eucarro Rhyolite, Spearfelt Rhyodacite, Roopena Basalt, Fresh Well Formation, Angle Dam Volcanics, and unnamed felsic units.|Underlain unconformably by Paleoproterozoic basement. Overlain by flat-lying Neoproterozoic sediments of the Stuart Shelf, Tertiary silcrete, and Quaternary alluvial and colluvial sediments.|Unit1: massive, homogenous dacite. Unit2: basalt flow units, volcanoclastic sandstone. Unit3: coarse-grained dacite. Unit4: basalt flow units, volcaniclastic sandstone. Unit5: massive, crystal-rich rhyolite. Unit6: altered fine-grained dacite.|
7059|Gawler Range Volcanics|71418|5|Briefly described|p20,22,25|||Geological province: Gawler Craton. Of Eyre Peninsula. Igneous activity likely resulting in shallow crustal hydrothermal activity leading to formation of siliceous breccia in low hills south of Nankivel Dam and 4.5 km WNW of Peterlumbo Hill, northern Eyre Peninsula, raising potential for epithermal-style gold mineralisation. 40Ar/39Ar dating of K-feldspar from porphyritic dacite is c. 900-700 Ma, interpreted to be timing of alteration or recrystallisation.||||||
7059|Gawler Range Volcanics|71534|5|Briefly described|p294-296,301-302|Calymmian|Calymmian|Geological province: Gawler Craton. Ferroan, A-type felsic compositions with a subordinate mafic component and variable Sm-Nd and Lu-Hf isotopic composition reflecting crustal contamination of a mafic source by a heterogeneous crustal column (Allen et al., 2008; Belousova et al., 2009; Flint et al., 1993; Wade et al., 2012). Associated with renewed mantle input post-Kimban Orogeny. More evolved Hf isotope data show significant crustal melting.|c. 1595-1575 Ma|||||
7059|Gawler Range Volcanics|71559|5|Briefly described|p14, p15 Fig 2, p16|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. See also Upper Gawler Range Volcanics and Lower Gawler Range Volcanics.||||||29-MAY-19
7059|Gawler Range Volcanics|71618|6|Mentioned|p135|Calymmian|Calymmian|Geological province: Gawler Craton. Possible, but unlikely source of ~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|c. 1590 Ma|||||
7059|Gawler Range Volcanics|71712|6|Mentioned|p410 Fig 1, p411, p413 Fig 2|Calymmian|Calymmian|Underlies a "considerable" part of the Cariewerloo Basin.|1595-1575 Ma|||Coeval with Hiltaba Suite. Contemporaneous with Roopena Basalt.||31-MAR-20
7059|Gawler Range Volcanics|71859|5|Briefly described|p4-p6|Mesoproterozoic|Mesoproterozoic|Southern Gawler Craton. Comagmatic with the Hiltaba Suite. Age range also derived from Jagodzinski et al., 2016.|c. 1595-1587 Ma (Allen et al., 2008)|||||05-APR-23
7059|Gawler Range Volcanics|71862|5|Briefly described|p3-p4, p8, p12, p21, p52|Calymmian|Calymmian|Central Gawler Craton. Co-magmatic with the Hiltaba Suite. Age is also derived from Jagodzinski et al 2016.|c. 1595-1585 Ma (Allen et al 2008)|||Intrudes the Peter Pan Supersuite.|Felsic volcanic rocks.|
7059|Gawler Range Volcanics|71895|4|Described|p10-p12, p26, p51, p55|Mesoproterozoic|Mesoproterozoic|Misspelt as the Gawler Range Volcanic on p10. Alteration and mineralisation are discussed.  Spectral analysis is provided. Referred to as GRV on p89-92. See also p57, p63, p89-p92, p116, p142-p144, p150-p151, APP1. p6-p11, APP1. p14-p15, APP1. p19, APP4. p4, APP4. p8, APP5. p63, p83, p86, p88, p90, p111, p113, p116, p127, p143,. APP6 p174-p177, p183-p184, APP8. p203. Intersected in drillhole GHDD01, GHDD0, WDDD01, WPDD01 and PDDD01. Petrographic descriptions are provided for several samples of this unit.|c. 1590 Ma|||Overlies the Wallaroo Group. Unconformably overlain by the Pandurra Formation.|Felsic volcaniclastic rocks including tuffs.|
7059|Gawler Range Volcanics|72058|6|Mentioned|p170-p171|Mesoproterozoic|Mesoproterozoic|Middleback Ranges, Gawler Craton.|~1600 Ma|||||
7059|Gawler Range Volcanics|72065|5|Briefly described|p103-106,108-109,111-120|Calymmian|Calymmian|Geological province: Gawler Craton. Abbreviated as GRV in text. Comagmatic with Hiltaba Suite; together known as the Mesoproterozoic Gawler LIP. Emplacement age at ~1595.5 Ma (zircon, U-Pb, IDTIMS, Jagodzinski et al., 2016). Relatively undeformed, dominantly exposed in the central part of Gawler Craton. Estimated magma volume in excess of 25000 km^2.|||Includes Yardea Dacite, Mount Double ignimbrite, Eucarro Rhyolite, Bitalli Rhyolite, Waganny Dacite.|||10-JAN-20
7059|Gawler Range Volcanics|72090|4|Described|p1-p2, p7-p10, p11, p14-p17, p19|Calymmian|Calymmian|Gawler Craton. Hosts colloform banded quartz-sulfide veins providing evidence of epithermal mineralisation. Referred to through out the text as GRV. Extrusive equivalents of the Hiltaba Suite. Distinguished from Sleaford Complex and Peter Pan Supersuite rocks on the basis of geochemistry. See also p55, p61, p64-p65, p73, p78, p81, p91, p93, p98, p107-p108, p110, p113-p115, p117-p118.|c. 1595-1587 Ma|||Overlies the Tunkillia Suite and St Peter Suite.|High temperature, A and I-type felsic volcanics and lesser mafic volcanics. Greyish orange, porphyritic, fine-grained dacitic dyke.|
7059|Gawler Range Volcanics|72237|5|Briefly described|p28,30-31|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.|1595-1575 Ma||Includes Pandurra Formation, Eucarro Rhyolite, Fresh Well Formation, Roopena Basalt, Angle Dam Dacite.|||
7059|Gawler Range Volcanics|72454|6|Mentioned|p1, 2, 20, 49,53-54|Mesoproterozoic|Mesoproterozoic|Mostly abbreviated to GRV.||||||
7059|Gawler Range Volcanics|72459|5|Briefly described|p6-p7, p10, p16-19, p21,|Mesoproterozoic|Mesoproterozoic|Nuyts Subdomain. Comagmatic with the Hiltaba Granite. Petrographic descriptions of constituent lithologies are provided. Appears as GRV through the text. See also p23, p46, p48-53.|1592 +/- 2 Ma (U-Pb; Fanning, 1997)||Includes the Bittali Rhyolite, Eucarro Dacite, Yardea Dacite, Nonning Rhyodacite and the Paney Rhyolite.||Basalts, dacites, rare andesites, rhyodacites and rhyolites.|
7059|Gawler Range Volcanics|72461|6|Mentioned|p6||||c. 1590 Ma|||||
7059|Gawler Range Volcanics|72462|5|Briefly described|p1-2, p5, p7-8, p10|Calymmian|Calymmian|Gawler Craton. A-type felsic rocks. Part of a silicic large igneous province; originally contiguous with the Benagerie Volcanic Suite and Ninnerie Supersuite. Hosts Ag-Pb mineralisation at Point Brown. Described in terms of upper and lower portions; the lower includes felsic and mafic lavas, ignimbrites and tuffs, and the upper consists of three regionally extensive thick, felsic lava flows.|1590-1586 Ma||Eucarro Rhyolite, Yardea Dacite, Pondanna Dacite Member, Moonaree Dacite Member||Bimodal volcanics including felsic and mafic lavas, ignimbrites and tuffs.|
7059|Gawler Range Volcanics|72463|6|Mentioned|p2-3, p6|Mesoproterozoic|Mesoproterozoic|May by underlain by Corunna Conglomerate.||||Unconformably underlain by Broadview Schist.||
7059|Gawler Range Volcanics|72464|5|Briefly described|p1, 3, 6, 8, 10, 24, 27-28|Mesoproterozoic|Mesoproterozoic|Nankivel Dam area, Gawler Craton. The southern margin of this unit contains Ag-Pb-Zn-Au-Cu mineralised subvolcanic hydrothermal alteration systems. A sample of K-feldspar gave an age of c.900-700 Ma, for either the timing of alteration or recrystallisation.|||||Includes coarsely porphyritic dacite and rhyolite units.|
7059|Gawler Range Volcanics|72484|6|Mentioned|p3|||Eyre Peninsula, Gawler Craton.|1597-1589 Ma.|||||
7059|Gawler Range Volcanics|72488|5|Briefly described|p1, 2 Fig.1, p4-7, 16-17|||Eastern Gawler Craton. Voluminous, bi-modal extrusives. Likely emplaced in a post-subduction switch from compressional to extensional setting. Usually abbreviated to GRV in the text.|1591 +/- 10 Ma (Creaser and Cooper, 1993).|||Unconformably overlies Mulgathing Metamorphic Complex, Donington Suite and Wallaroo Group. Co-magmatic with Hiltaba Suite.|Felsic lavas: rhyolite, dacite, ignimbrite; with minor interbedded clastic facies.|
7059|Gawler Range Volcanics|72949|6|Mentioned|p32, p34-39, p41-42|Calymmian|Calymmian|Gawler Craton, Olympic Domain, Mount Woods Inlier. Voluminous hot (~950-1,100 oC), A-type, F-rich lavas. Part of the Gawler Siliceous Large Igneous Province.|c. 1.595-1.587 Ga.||lower Gawler Range Volcanics, upper Gawler Range Volcanics|||
7059|Gawler Range Volcanics|73026|5|Briefly described|p5-6, p10-11, p13|Mesoproterozoic|Mesoproterozoic|Forms part of a felsic large igneous province estimated to occupy some 100,000km^3.|c. 1590 Ma|||Overlies the Mulgathing Complex and the Sleaford Complex.||
7059|Gawler Range Volcanics|73027|6|Mentioned|p10-13|Calymmian|Calymmian|Forms part of a felsic large igneous province estimated to occupy some 100,000km^3.|c. 1592 Ma||||Dominantly felsic although minor basalts are presents.|
7059|Gawler Range Volcanics|73030|6|Mentioned|p2148-2150, p2152|Calymmian|Calymmian|Gawler Craton. High-temperature, A- and I-type magmatism, and lesser mafic volcanics. Constitutes the extrusive equivalent of the Hiltaba Suite and Munjeela Suite. Voluminous felsic magmatism resulted from both fractional crystallization and widespread crustal melting.|ca. 1595 to 1587 Ma|||Equivalent to Hiltaba Suite and Munjeela Suite.||
7059|Gawler Range Volcanics|73061|6|Mentioned|p1077|||Gawler Craton.||||||
7059|Gawler Range Volcanics|73104|6|Mentioned|p2-4, p6, p25-26, p39, p41, p45-46, p72|Mesoproterozoic|Mesoproterozoic|[Abbreviated to GRV].|||||Includes rhyolitic to andesitic dykes and sills, porphyritic felsic intrusions.|
7059|Gawler Range Volcanics|73110|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map below the main PORT AUGUSTA map.||||||
7059|Gawler Range Volcanics|73118|6|Mentioned|p73|||Adelaide Fold Belt.|1590 Ma.|||||
7059|Gawler Range Volcanics|73130|6|Mentioned|[poster]|Calymmian|Calymmian|Extrusion occurred after the formation of the Itiledoo Basin. [The name upper Gawler Range Volcanics was also used].|c.1595-1585 Ma||||Extrusive rocks.|
7059|Gawler Range Volcanics|73155|5|Briefly described|p263-265, p274, p277-279, p282-287|Calymmian|Calymmian|Gawler Craton, central. Faulted against Paleo- to Mesoproterozoic metasedimentary and igneous rocks of the Mount Woods Domain. Linear to lobate magnetic horizons interpreted as volcanic successions of Gawler Range Volcanics. Occurs in several belts throughout the Mount Woods Domain, deposited in half graben basins within the upper plate of the Mount Woods Metamorphic Core Complex.|ca. 1591-1587 Ma, ca. 1592 Ma|||Faulted against Blue Duck Group.|Lower grade, upper crustal rocks including variable dacite to rhyolite units with lesser basalt and basaltic andesite in sedimentary and volcanic successions.|
7059|Gawler Range Volcanics|73162|6|Mentioned|p447-453, p459-460|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Part of Gawler Silicic Large Igneous Province. Undeformed but emplaced broadly synchronous with localised deformation in the Kararan Orogeny. Co-magmatic with Hiltaba Suite.|1595-1587 Ma||lower Gawler Range Volcanics, upper Gawler Range Volcanics|Wandearah and Moonabie formations are onlapped unconformably by Gawler Range Volcanics.|Felsic volcanics, includes tholeiitic basalts.|
7059|Gawler Range Volcanics|73165|6|Mentioned|p619-621, 637|Calymmian|Calymmian|Gawler Craton. Bimodal magmatism that occurred during period of regional deformation.|ca 1592 Ma||||Bimodal magmatism.|
7059|Gawler Range Volcanics|73166|5|Briefly described|p644, 645, 647, 654, 656|Mesoproterozoic|Mesoproterozoic|Gawler Silicic Large Igneous Province, Gawler Craton. Contemporaneous with Hiltaba Suite. U-Pb dating of apatite to ca 1590 Ma is consistent with formation and initial alteration of the iron oxide-apatite association shortly after emplacement of Gawler Range Volcanics and intrusion of Hiltaba Suite granite. U-Pb dating of xenotime and Th-Pb dating of monazite inclusions to ca 1370 Ma record a distinct thermal/fluid event that may relate to 1370 +/- 54 Ma monazite at Oak Dam East prospect, potentially relates to the East Kootenay Orogeny at ca 1370 Ma in Laurentia. Cambrian Pb loss/resetting affected xenotime and monazite ages likely caused by Delamerian Orogeny.|ca 1.6 Ga, 1.59 Ga|||Intruded by Hiltaba Suite|Felsic and minor intermediate lavas, ignimbrites and sills/dykes. Main host rock of the Acropolis prospect, contains massive, coarse-grained veins of a magnetite-apatite assemblage, partially replaced by a hematite assemblage.|
7059|Gawler Range Volcanics|73227|6|Mentioned|p34|Mesoproterozoic|Mesoproterozoic|Knutson et al. (1992) suggested this unit was a source of metals for sediment-hosted sulfide mineralisation in the region.||||||
7059|Gawler Range Volcanics|73230|6|Mentioned|p5, p8, p12|Mesoproterozoic|Mesoproterozoic|May be related to gold-bearing quartz veins in the Harris Greenstone Domain.||||||
7059|Gawler Range Volcanics|73233|6|Mentioned|p27 Fig.1, p30|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
7059|Gawler Range Volcanics|73234|6|Mentioned|p4-5, p19-20|Calymmian|Calymmian|Associated with the Hiltaba Suite and contemporaneous with Fresh Well Formation.|c. 1590 Ma||||Felsic to mafic extrusives.|
7059|Gawler Range Volcanics|73235|6|Mentioned|p52-54, p59-61, p63|Calymmian|Calymmian|Gawler Craton. Fluid flow modelling suggests this unit would act as an aquitard, promoting hydrothermal alteration of the underlying lithologies and focusing fluid flow through any fault or fracture zones penetrating the volcanics. Original distribution was much greater than the current exposed outcrop. Provided subvolcanic hydrothermal systems that act as the energy source for mineral systems. Hosts gold mineralisation in the Tarcoola mineral field of the Kararan (Gawler Range Volcanics) gold mineral system and in the Olympic mineral field of the Kararan (Hiltaba Suite) gold mineral system. Features mylonitic deformation associated with a N/S-trending structure in the southern Gawler Range Volcanics region.|1596-1587 Ma||||Includes felsic dykes.|
7059|Gawler Range Volcanics|73249|5|Briefly described|p316, p317 Fig.1, p335, p338|Mesoproterozoic|Mesoproterozoic|Abbreviated to GRV in text. Uplifted before or during the very early Cretaceous, potential sediment source for the Lower Cretaceous Eromanga Basin.|||||Felsic volcanic rocks, predominantly rhyolite and dacite, minor basalts.|
7059|Gawler Range Volcanics|73252|6|Mentioned|p4|||Gawler Craton.||||||
7059|Gawler Range Volcanics|73256|4|Described|p557-576|Calymmian|Calymmian|[Also written as GRV]. Gawler Craton. Subduction zone setting. Regional compression, locally interpreted as extensional and compressional environment of emplacement. Spatially and temporally associated with IOCG and Au [other] mineralisation. Geochemically similar to A-type magmas; typically high in silica, and enriched in REEs and high-field-strength elements (HFSE). Geochemical composition of zircon may be useful for distinguishing this unit from the coeval Hiltaba Suite. [See article for petrographic descriptions, whole-rock geochemistry, and zircon morphological and compositional characterisation].|ca 1595-1587 Ma|||Coeval with Hiltaba Suite.||
7059|Gawler Range Volcanics|73263|6|Mentioned|p591-592, p601, p603|||[Also written as GRV]. Gawler Craton. Well exposed in the north and sporadically exposed elsewhere.||||Equivalent to Hiltaba Suite.||
7059|Gawler Range Volcanics|73298|6|Mentioned|p1072 Fig.1, p1073, p1078 Fig.6|||Gawler Craton.||||||
7059|Gawler Range Volcanics|73302|6|Mentioned|p32-34, 54|Mesoproterozoic|Mesoproterozoic|With the Hiltaba Suite, represents a large igneous province.|c.1595-1575 Ma.|||||
7059|Gawler Range Volcanics|73429|6|Mentioned|p105, p114|Calymmian|Calymmian|Gawler Craton.|c. 1590-1580 Ma|||||
7059|Gawler Range Volcanics|73493|6|Mentioned|p711-712, p714 Fig.1, p716 Fig.3, p727|Calymmian|Calymmian|Gawler Craton. See also p726 Fig.13, p728.|ca 1595-1575 Ma|||||
7059|Gawler Range Volcanics|73516|6|Mentioned|p2|Calymmian|Calymmian|Gawler Craton.|1592 Ma|||||
7059|Gawler Range Volcanics|73524|6|Mentioned|p4|||Gawler Craton. Correlative of Benagerie Ridge Volcanics.||||||
7059|Gawler Range Volcanics|74361|4|Described|p162-164, 166, 168-169, 171, 173|Mesoproterozoic|Mesoproterozoic|See also p175-177. Central and eastern Gawler Craton. One of the major sources of the ""bedded clastic facies"" in the Olympic Dam Breccia Complex. After the first page, it is mostly referred to as GRV throughout the article. ~1595-1587 Ma|Emplaced at 1594.73 +/- 0.30 Ma.||Chitanilga Volcanic Complex.|Is intruded by Roxby Downs Granite. Co-magmatic with Hiltaba Suite.|Very thick but spatially restricted felsic and subordinate mafic volcanics, followed by thick, voluminous felsic lavas.|
7059|Gawler Range Volcanics|74367|6|Mentioned|p4, p23|Calymmian|Calymmian||ca. 1590 Ma|||||
7090|Geera Clay|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 50, 158|Miocene|Oligocene|Lawrence (1966). Murray Basin. 170m thick. A significant aquiclude. See also p178-179, 231, 285, 300, 304, 315, 318, 320.||Murray Group.||Overlies Renmark Group. Is overlain by Winnambool Formation. Is separated from the overlying Parilla Sand by the Mologa Surface. Grades westwards into the Ettrick Marl.|Sparingly fossiliferous, dark grey to black clay.|
7090|Geera Clay|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Late Oligocene|Of the Murray Group. Overlain by Renmark beds. Geological Province: Murray Basin.||||||13-AUG-07
7090|Geera Clay|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|22773|5|Briefly described|p351,Fig24.8p352|||||||||
7090|Geera Clay|22799|2|Defined|p31|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
7090|Geera Clay|22857|5|Briefly described|p351, p353 Fig. 24.9|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|22887|5|Briefly described|Fig.6 p13|Miocene|Oligocene|||||||
7090|Geera Clay|22893|3|Fully described|p28 fig8a,9 table3|Miocene|Miocene|||||||
7090|Geera Clay|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
7090|Geera Clay|23226|6|Mentioned|p889,890,891|||Of Murray Supergroup.||||||
7090|Geera Clay|23884|5|Briefly described|p153, p155 Fig.13.2|Miocene|Oligocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|23909|6|Mentioned|p298|||||||||
7090|Geera Clay|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|24100|6|Mentioned|p99|||Geological Province: Murray Basin.||||||19-APR-05
7090|Geera Clay|24177|5|Briefly described|p69|Middle Miocene|Late Oligocene|Renmark Group grades westward into this deposit (Lawrence, 1975). Geological Province: Murray Basin.||||||
7090|Geera Clay|24551|6|Mentioned|p322 Fig. 10.29|||Of the Murray Group.||||||
7090|Geera Clay|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Geera Clay not included.  Geological Province: Murray Basin.||||||
7090|Geera Clay|29591|6|Mentioned|Table 20|||||||||
7090|Geera Clay|29898|6|Mentioned|Table 20|||||||||
7090|Geera Clay|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7090|Geera Clay|30934|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
7090|Geera Clay|30936|6|Mentioned|Map legend|Eocene|Eocene|||||||
7090|Geera Clay|31741|6|Mentioned|p6|||||||||
7090|Geera Clay|31746|3|Fully described|p195|||||||||
7090|Geera Clay|31747|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|34735|4|Described|p32|||Also mention P31.||||||
7090|Geera Clay|34813|6|Mentioned|p62|||||||||
7090|Geera Clay|37796|6|Mentioned|p164|||||||||
7090|Geera Clay|37809|6|Mentioned|p7|||||||||
7090|Geera Clay|38601|4|Described|p7|||||||||
7090|Geera Clay|39329|6|Mentioned|Fig.1|||||||||
7090|Geera Clay|39929|4|Described|p267|||||||||
7090|Geera Clay|40820|6|Mentioned|Fig.4|||||||||
7090|Geera Clay|41423|6|Mentioned|p284|||||||||
7090|Geera Clay|41511|6|Mentioned|p20|||||||||
7090|Geera Clay|41868|6|Mentioned|p551|||||||||
7090|Geera Clay|42125|5|Briefly described|p134|||See also Fig.5||||||
7090|Geera Clay|42126|6|Mentioned|p149|||||||||
7090|Geera Clay|42130|6|Mentioned|p271|||||||||
7090|Geera Clay|42132|6|Mentioned|p295|||||||||
7090|Geera Clay|42133|6|Mentioned|p301|||||||||
7090|Geera Clay|42134|4|Described|p339|||||||||
7090|Geera Clay|42137|4|Described|p372,p376|||See also Table 3||||||
7090|Geera Clay|42138|6|Mentioned|p388|||||||||
7090|Geera Clay|42375|5|Briefly described|p26|early Miocene|late Oligocene|Murray Basin||||||
7090|Geera Clay|42509|5|Briefly described|p2|||||||||
7090|Geera Clay|42510|5|Briefly described|p35|||||||||
7090|Geera Clay|42511|6|Mentioned|Fig.2 P55|||||||||
7090|Geera Clay|42512|6|Mentioned|p68|||||||||
7090|Geera Clay|42514|6|Mentioned|p116|||||||||
7090|Geera Clay|42515|6|Mentioned|p134|||||||||
7090|Geera Clay|42517|5|Briefly described|p169|||||||||
7090|Geera Clay|42518|5|Briefly described|p185|||||||||
7090|Geera Clay|42519|6|Mentioned|p205|||||||||
7090|Geera Clay|42720|5|Briefly described|map legend|Miocene|Oligocene|||||||
7090|Geera Clay|42813|5|Briefly described|p24|||||||||
7090|Geera Clay|42827|3|Fully described|p269|||Of Murray Group.||||||03-FEB-09
7090|Geera Clay|42881|4|Described|Fig.3, P84|||||||||
7090|Geera Clay|42966|2|Defined|p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||03-FEB-09
7090|Geera Clay|43655|5|Briefly described|p40-846|||||||||
7090|Geera Clay|43669|4|Described|p22|Middle Miocene|Early Miocene|||||||
7090|Geera Clay|43780|6|Mentioned|p5|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|43790|5|Briefly described|p383|||||||||
7090|Geera Clay|43791|5|Briefly described|p371|||||||||
7090|Geera Clay|43804|5|Briefly described|p47|Miocene|Oligocene|||||||
7090|Geera Clay|44133|5|Briefly described|p159|Middle Miocene|Early Miocene|Of the Muray Group. Geological Province: Murray Basin. ||||||
7090|Geera Clay|44188|5|Briefly described|Map Legend|Late Miocene|Late Oligocene|Geological province: Murray Basin. Poorly consolidated, plastic to friable, black, grey dark green clay, silt, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; local sandy dolomitic intercalations.||||||15-MAY-08
7090|Geera Clay|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|47060|6|Mentioned|p183|||||||||
7090|Geera Clay|49038|4|Described|Table 2|||||||||
7090|Geera Clay|49040|5|Briefly described|p12|||See also P11||||||
7090|Geera Clay|50154|5|Briefly described|p135|||Of the Murray Group.||||||
7090|Geera Clay|60452|5|Briefly described|p33|Middle Miocene|Late Oligocene|Marine Deposits.||||||
7090|Geera Clay|60491|4|Described|p21|||Of the Murray Group. Conformably overlies the Olney Formation. Geological Province: Murray Basin.||||||
7090|Geera Clay|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
7090|Geera Clay|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Of the Murray group. Carbonaceous silts and minor carbonates. Interfingers with Olney Formationand ettrick Formation. Max. thickness: 150m.  Geological Province: Murray Basin.||||||03-MAR-10
7090|Geera Clay|61181|5|Briefly described|p153 Fig. 47|||Carbonaceous clay. ||||||
7090|Geera Clay|61314|5|Briefly described|p129|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit and the Ettrick and Winnambool Formations into their new Murray Supergroup.  These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
7090|Geera Clay|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Geological province: Murray Basin. Bioturbated, dark grey to black, slightly calcareous and poorly fossiliferous clay. Equivalent to Winnambool and Ettrick Formations. ||||||
7090|Geera Clay|63777|6|Mentioned|p1104 Fig. 1, p1105|||Geological Province: Murray Basin.||||||18-MAR-09
7090|Geera Clay|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Lagoonal and marginal marine muddy facies.||||||
7090|Geera Clay|64237|5|Briefly described|p17, p18|Late Oligocene|Late Oligocene|Included in the Murray Group stratigraphic scheme by Lawrence (1966), retained through the various revisions of the Murray Group up to Murray Supergroup; and is now included in the reinstated Murray Group in South Australia.||||||
7090|Geera Clay|64823|5|Briefly described|p1011|Late Miocene|Paleocene|Clays and marls. Geological province: Murray Basin||||||
7090|Geera Clay|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Oligocene|Clay/claystone with occasional dolomite. Deposited during a marine incursion. Unconformably underlies Loxton-Parilla Sands and Bookpurnong beds. Contemporaneous with Murray Group and Winnambool, Ettrick and Olney Formations.||||||
7090|Geera Clay|65719|5|Briefly described|p7|Miocene|Oligocene|In Murray Basin. Lateral equivalent of Mystic Park Formation. Marginal marine or paralic.||||||10-MAY-12
7090|Geera Clay|66573|6|Mentioned|p873|Miocene|Miocene|Murray Basin. Marine.||||||
7090|Geera Clay|67127|6|Mentioned|p73|||||||Overlies the Renmark Group. Underlies the Parilla Sand.||
7090|Geera Clay|67179|6|Mentioned|p579|||||||||
7090|Geera Clay|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||Unit in Murray Group.||||
7090|Geera Clay|68140|5|Briefly described|p1700 Fig.1, p1701, p1704 Fig.5|Neogene|Paleogene|Up to 75m thick. Acts as an effective aquitard. Middle Tertiary age.|||||Comprises massive clays with minor sand and silt layers.|09-FEB-18
7090|Geera Clay|68189|5|Briefly described|p27 Tb.3.2, p29|Miocene|Oligocene|Depositional environment: marginal marine, lagoonal, tidal flats. The Geera Clay is the only part of the Murray Group previously recorded in ST ARNAUD. It is an important barrier which separates water flows between the Parilla Sand and Renmark Groups.||Of the Murray Group.||Underlain by the Olney Formation. Overlain by the Parilla Sand.|Comprises plastic black-green mud and sand; glauconitic.|
7090|Geera Clay|68194|5|Briefly described|p23|Miocene|Oligocene|Lawrence (1966). Murray Basin. Over 50m thick.||Unit in Murray Group.||Lateral facies equivalent of Calivil Formation.|Glauconitic claystone and interbedded dolomitic siltstone.|
7090|Geera Clay|68715|6|Mentioned|p31 Fig.5|Miocene|Miocene|Murray Basin. Early to Middle Miocene age.||Murray Group.||||07-APR-17
7090|Geera Clay|70718|4|Described|p24-p25, p103|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies. Improperly concatenated as Geera Formation on p24. Approximately 150m thick. Silt and sand are primarily terriginous in origin.||Murray Group|||Black, olive grey, dark-grey or dark-green silty mud, silt and clay with minor dark sand.|
7090|Geera Clay|71593|6|Mentioned|p52-p54|||||||||
7090|Geera Clay|72445|5|Briefly described|.App.1, App.2; App.6 p1, p3-4, p6; App.7|Miocene|Oligocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). See also App. 7 p2, p4, p16-18. Identified in Stavely 12,16. App.6, App.7 propose Early Miocene Geera Clay at 65m in Stavely 11, but this is identified as Olney Formation, Renmark Group in well logs.||Murray Group||Underlies Port Campbell Limestone,conformity; Calivil Formation, sharp contact; Loxton Sand. Overlies Carrolls Amphibolite,sharp contact; Winnambool Formation, gradational; Renmark Group, unconformity|Includes carbonaceous fine sand and (black) clays, grey and mottled silty mud.|
7090|Geera Clay|73118|5|Briefly described|p17, 37, 45, 48, 61, 82|||Glenelg Zone, Western Victoria. Drill core summary logs. 170m thick; mainly <50m. Entirely concealed. Deposited in shallow and marginal marine, interdistributary bay, lagoonal and tidal flat environments.||Murray Group.||Overlies Ettrick, Olney Formations and Saint Arnaud Group. Is overlain by Bookpurnong Beds and Loxton-Parilla Sands.|Poorly consolidated, black to dark green silt, clay, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; locally includes sandy dolomitic intercalations. Abundant low-diversity faunas.|
7090|Geera Clay|73188|6|Mentioned|p320|Miocene|Miocene|Murray Basin.|||||Clay.|
7090|Geera Clay|73228|4|Described|p50, p55-57, p60|Middle Miocene|Late Early Oligocene|Murray Basin. Muddy lagoonal and marginal marine / tidal environments [although Fabris 2003 provided a different interpretation]. Represents marine incursions within the Murray Group.||Murray Group|||Black to grey-green, carbonaceous, pyritic clay and silt with minor sand and glauconite and sparse marine fossils.|
7090|Geera Clay|73229|6|Mentioned|p67|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
7090|Geera Clay|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
7090|Geera Clay|73505|4|Described|p2, p11, p13-14, p36|Miocene|Late Eocene|Murray Basin. Mostly deposited in a marginal marine environment, includes intertital and estuarine deposits. Interfingers with lateral equivalents of the Calivil Formation. No detectable magnetic response.||Murray Group||Overlies Norval Regolith, offshore equivalent to Calivil Formation, underlies Bookpurnong beds|Marginal marine, marine to nonmarine clay, 100 m thick.|
7107|Gellibrand Marl|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin. Maximum thickness 26m.||Heytsbury Group.||Overlies Compton Conglomerate conformably and Narrawaturk Marl unconformably. Is overlain by Gambier Limestone.||
7107|Gellibrand Marl|22875|5|Briefly described|p68|Middle Miocene|Early Oligocene|Of the Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|22944|5|Briefly described|Fig3|||||||||
7107|Gellibrand Marl|23230|5|Briefly described|Table4-1p40, Fig4-3p46|||||||||
7107|Gellibrand Marl|23307|5|Briefly described|Map Legend|Miocene|Miocene|Of Heytesbury Group||||||
7107|Gellibrand Marl|23322|5|Briefly described|957 Fig.2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||07-SEP-09
7107|Gellibrand Marl|23909|5|Briefly described|p291|Miocene|Miocene|Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|24056|5|Briefly described|p84 Fig. 2|Miocene|Oligocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
7107|Gellibrand Marl|24314|5|Briefly described|p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin. Max. Thickness 28m. Of the Heytesbury Group.||||||30-NOV-04
7107|Gellibrand Marl|24551|5|Briefly described|p246, 584, p732 Table 17.2|Miocene|Oligocene|Of the Heytesbury Group.  Max thickness: 450m.||||||
7107|Gellibrand Marl|24562|5|Briefly described|p8 Fig. 2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|29823|5|Briefly described|p14|||||||||
7107|Gellibrand Marl|29856|6|Mentioned|p36|||||||||
7107|Gellibrand Marl|30576|6|Mentioned|Table 1|||||||||
7107|Gellibrand Marl|30578|5|Briefly described|p12|||||||||
7107|Gellibrand Marl|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7107|Gellibrand Marl|30675|5|Briefly described|p253|||Lithology & radioactivity||||||
7107|Gellibrand Marl|30865|6|Mentioned|p315|||Middle Miocene||||||
7107|Gellibrand Marl|30932|6|Mentioned|Map legend|Miocene|Oligocene|Equivalent in part to Gambier Lst. Oligocene-Miocene||||||
7107|Gellibrand Marl|31036|1|Redefined|p212|Tertiary|Tertiary|Unit of Heytesbury Gp. See also p199, Table 19-1.||||||09-MAY-07
7107|Gellibrand Marl|31583|6|Mentioned|p18|||Section||||||
7107|Gellibrand Marl|31625|6|Mentioned|Fig. 5.2|||Oligocene- Miocene||||||
7107|Gellibrand Marl|31922|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|32499|6|Mentioned|p111|||||||||
7107|Gellibrand Marl|33940|6|Mentioned|p414|||||||||
7107|Gellibrand Marl|34954|6|Mentioned|Fig.35|||||||||
7107|Gellibrand Marl|35066|3|Fully described|p211|||p223.||||||09-MAY-07
7107|Gellibrand Marl|35262|6|Mentioned|p4|||||||||
7107|Gellibrand Marl|35274|6|Mentioned|p422|||||||||
7107|Gellibrand Marl|35290|6|Mentioned|p38|||||||||
7107|Gellibrand Marl|36499|6|Mentioned|p43|||||||||
7107|Gellibrand Marl|36913|6|Mentioned|p81|||||||||
7107|Gellibrand Marl|37385|6|Mentioned|p9|||||||||
7107|Gellibrand Marl|38625|6|Mentioned|Table 2|||||||||
7107|Gellibrand Marl|39967|4|Described|p43|||||||||
7107|Gellibrand Marl|40947|6|Mentioned|p3|||||||||
7107|Gellibrand Marl|41016|5|Briefly described|p214|||||||||
7107|Gellibrand Marl|41185|6|Mentioned|Fig.4|||||||||
7107|Gellibrand Marl|41269|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|41398|6|Mentioned|p1|||||||||
7107|Gellibrand Marl|41642|6|Mentioned|Fig.8.6|||||||||
7107|Gellibrand Marl|41701|6|Mentioned|Map legend|Miocene||||||||
7107|Gellibrand Marl|41704|6|Mentioned|Fig.3|||||||||
7107|Gellibrand Marl|41714|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|41726|6|Mentioned|Fig.5|||||||||
7107|Gellibrand Marl|41769|4|Described|p33|||||||||
7107|Gellibrand Marl|42079|6|Mentioned|Fig.2 P264|||See also Fig.10, p272||||||
7107|Gellibrand Marl|42371|6|Mentioned|p42|Janjukian||||||||
7107|Gellibrand Marl|42452|5|Briefly described|Map legend|middle Miocene|late Oligocene|||||||
7107|Gellibrand Marl|42453|4|Described|p17|||||||||
7107|Gellibrand Marl|42524|5|Briefly described|Fig.3 P27|||||||||
7107|Gellibrand Marl|42635|6|Mentioned|p89|||(Fyansford Formation)||||||
7107|Gellibrand Marl|42827|3|Fully described|p285|||Of the Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
7107|Gellibrand Marl|43195|6|Mentioned|Map Legend|Middle Miocene|Late Eocene|of Heytesbury Group.||||||
7107|Gellibrand Marl|43208|5|Briefly described|map legend|Middle Miocene|Oligocene|Of Middle Oligocene - Middle Miocene age. Of Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|43219|5|Briefly described|Fig.3,p6.|Miocene|Oligocene|Of Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|43590|4|Described|p24|Middle Miocene|Early Oligocene|||||||
7107|Gellibrand Marl|43604|5|Briefly described|p145,Fig.2|||||||||
7107|Gellibrand Marl|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
7107|Gellibrand Marl|43667|6|Mentioned|Fig.3,p12|Middle Miocene|Early Miocene|||||||
7107|Gellibrand Marl|43733|6|Mentioned|Fig.2.11,p65||Oligocene|||||||
7107|Gellibrand Marl|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
7107|Gellibrand Marl|44133|4|Described|p156|Early Oligocene|Early Oligocene|Of the Heytesbury Group. Geological Province: Gambier Basin. Underlies Camelback Member of the Gambier Limestone. Thickness: 7m.||||||
7107|Gellibrand Marl|44186|5|Briefly described|Map Legend||Miocene|||||||
7107|Gellibrand Marl|48911|6|Mentioned|Chart 1|||||||||
7107|Gellibrand Marl|48977|6|Mentioned|Fig.5|||||||||
7107|Gellibrand Marl|50154|5|Briefly described|p135|||Of the Heytesbury Group.||||||25-AUG-04
7107|Gellibrand Marl|60421|5|Briefly described|p417|Middle Miocene|Oligocene|Of the Heytesbury Group.||||||
7107|Gellibrand Marl|60452|6|Mentioned|p15|||Used as an age indicator in the phrase 'post Gellibrand Marl (late Miocene)'.||||||26-JUN-13
7107|Gellibrand Marl|60563|5|Briefly described|p46|||Of the Heytesbury Group. Overlain by the Port Campbell Limestone.||||||16-JUN-05
7107|Gellibrand Marl|60581|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||
7107|Gellibrand Marl|60582|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||23-NOV-04
7107|Gellibrand Marl|60583|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||23-NOV-04
7107|Gellibrand Marl|60584|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||
7107|Gellibrand Marl|60585|4|Described|p30|Early Miocene|Late Oligocene|Disconformably overlain by the Newer Volcanics and Hanson Plain Sand. Overlies the Clifton Formation. Consists of massive, calcareous clay and marl; and thin to medium beds of calcarenite.||||||
7107|Gellibrand Marl|60785|5|Briefly described|p184 Fig.1, p188.  |Burdigalian|Aquitanian|Of the Otway Basin. The middle section has yielded one well-preserved isolated fossil cetacean tooth.|||||Marl, calcareous silt, clay, and sand with minor calcarenite layers.|
7107|Gellibrand Marl|61136|6|Mentioned|p27|||||||||
7107|Gellibrand Marl|61155|5|Briefly described|p18|Late Miocene|Early Miocene|Of the Heytesbury Group. Overlies the Clifton Formation. Max. thickness: 1300m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments).||||||03-MAR-10
7107|Gellibrand Marl|61181|6|Mentioned|p133|||Overlies Maude Formation; overlain by Port Campbell Limestone. ||||||
7107|Gellibrand Marl|61182|3|Fully described|p26-p27, p28, p177|Middle Miocene|Early Miocene|Of Heytesbury Gp. Formerly Gellibrand Clays and Gellibrand Clay. Incorporates Fishing Point Marl and "Upper Glen Aire Clay". Overlies Demons Bluff Fm and Clifton Fm. and disconformable on Dilwyn Fm also; underlies Port Campbell Lst. Max. thickness: 406m. ||||||
7107|Gellibrand Marl|61185|6|Mentioned|p58|||Unnamed sediments described as post-Gellibrand Marl sediments.||||||07-FEB-11
7107|Gellibrand Marl|61547|6|Mentioned|p461 Fig.2. |Miocene|Eocene|||Unit in Heytesbury Group.||Overlies Narrawaturk Marl. Is overlain by Gambier Limestone.||
7107|Gellibrand Marl|61622|5|Briefly described|p436 Fig. 2|Miocene|Eocene|Of Heytsbury Group. Geological Province: Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|61623|6|Mentioned|p449 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61624|5|Briefly described|p465, p466 Fig. 2, p471|Early Miocene|Early Miocene|Of Haytesbury Group. Underlain by Clifton Formation. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61626|5|Briefly described|p487, p486 Fig. 2, p488 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Early Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|62068|5|Briefly described|p135, Fig.2,|Early Miocene|Early Miocene|||||Unconformably overlain by the Hanson Plain Sands||
7107|Gellibrand Marl|62899|6|Mentioned|p46|Miocene|Miocene|On the Leigh River, SA.||||||
7107|Gellibrand Marl|63122|5|Briefly described|p17 Fig. 4.3|Early Miocene|Late Eocene|Of the Heytesbury Group. Max. thickness: 28m. Geological Province: Otway Basin. ||||||
7107|Gellibrand Marl|63124|3|Fully described|p49 Fig. 5.2, p93|Miocene|Late Eocene|Of the Heytesbury Group. Initially called "Gellibrand beds". Unconformably overlies Dilwyn Formation; conformably overlain by Camelback Member of Gambier Limestone. Age: ~32Ma. Max. thickness: 18m. Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||Heytesbury Group.||||
7107|Gellibrand Marl|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Of the Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|63739|5|Briefly described|p46, p48|Middle Miocene|Middle Miocene|Contains ostracod assemblages on the Leigh River.||||||01-JUL-08
7107|Gellibrand Marl|64314|5|Briefly described|p500 , p502 Fig. 7|Early Miocene|Early Miocene|Marine sediments. Coded as GM in figure.||||||21-OCT-08
7107|Gellibrand Marl|65715|4|Described|p14 Tb.8, p16|Miocene|Oligocene|First used by Tate and Dennant (1893) p126 as Gellibrand beds. Of Torquay Group and Heytesbury Groups? Overlies Batesford Limestone, Clifton Springs Tuff. Underlies Black Rock Sandstone. Offshore quiet water facies. Senior synonym of Fyansford Clay and Puebla Formation.||||||
7107|Gellibrand Marl|66002|4|Described|p12, p13 Tb.9, p16, p26 Fig.7|Miocene|Miocene|Of Heytesbury Group. Called Gellibrand Clay by Baker (1953). Defined by Glenie 1971. Underlies Black Rock Sandstone. Calcareous silty clay and clayey silt, minor fine- to coarse-grained shelly calcarenite beds. Massive to moderately well bedded. Contains fossils||||||
7107|Gellibrand Marl|66012|4|Described|p18|Miocene|Oligocene|Of Heytesbury Group. Overlies Clifton Formation. Overlain by Port Campbell Limestone. Oligocene to middle Miocene| | ||||13-JUN-13
7107|Gellibrand Marl|66245|5|Briefly described|p6 Fig.5. |Tortonian|Rupelian|||Unit in Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.||
7107|Gellibrand Marl|67061|6|Mentioned|p546 Fig.3.|Miocene|Oligocene|||Unit in Heytesbury Group.||||
7107|Gellibrand Marl|67366|5|Briefly described|p103 Fig.2. |Miocene|Miocene|||Unit in Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.|Open marine marl and calcareous mudstone.|
7107|Gellibrand Marl|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
7107|Gellibrand Marl|68116|5|Briefly described|Appendix, Maps 40-41, 48-51, 54-55.|Miocene|Chattian||||||Marl, mudstone, sandstone, calcarenite, minor lignite, ligneous clay: marl blue-green and yellow; abundant carbonate nodules; contains shelly fossils and microfossils; lignite dark brown; contains spores and pollen.|
7107|Gellibrand Marl|68991|5|Briefly described|p465, p465 Fig.2|Miocene|Oligocene|Cliff-forming unit with a middle Miocene minimum age. Maximum thickness: 406 m thick.||||Conformably overlain by the Port Campbell Limestone.|Consists mainly of marine, grey calcareoous silty clay to clayey silt, with glauconite pellets and some calcarenite interbeds.|
7107|Gellibrand Marl|69297|5|Briefly described|p79, p98|Serravallian|Chattian|Otway Basin. ||Heytesbury Group||Overlies the Clifton Formation. Overlain by the Port Campbell Limestone.|Marl.|
7107|Gellibrand Marl|69651|5|Briefly described|p10|Miocene|Oligocene|||Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone and unconformably by Hanson Plain Sand.||
7107|Gellibrand Marl|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.||
7107|Gellibrand Marl|70880|6|Mentioned|p77|Miocene|Oligocene|Otway Basin.||||||
7107|Gellibrand Marl|70909|14|Not recorded|p62|||Distribution.||||||
7107|Gellibrand Marl|71266|6|Mentioned|p614 Fig.3|Miocene|Oligocene|Otway Basin.||||||
7107|Gellibrand Marl|71419|4|Described|p8 Fig 2, p16-17, p21-22|Miocene|Miocene|Originally 'Gellibrand-beds' of Tate and Dennant (1893). Described by them as 'Blue clay from 80 to 90 feet thick, highly fossiliferous; yellowish clay 20 to 30 feet' in cliffs west of the Gellibrand River mouth. This section designated as the type section by Baker (1953).||||Overlain by Sandringham Sandstone, Bridgewater Formation.||02-FEB-18
7107|Gellibrand Marl|71437|4|Described|Fig. 1 opp 154, p155,p160-162|Miocene|Miocene|Marine, widespread. ||Of Heytesbury Group.|Includes Rutledge Marl Member.|Transitional to overlying Port Campbell Limestone.|Marl.|
7107|Gellibrand Marl|71593|6|Mentioned|p51|||||||||
7107|Gellibrand Marl|72445|5|Briefly described|App 2; App.6 p1 Tb.1, p3.|Early Miocene|Early Miocene|App.2 is a .csv format file. Identified in Stavely 01. sample from 73m gives Early Miocene M4 zonal age (17.54 - 16.39 Ma GTS2012 timescale) deeper sample also Early Miocene based on foraminifera.||Heytesbury Group|||Includes bioturbated silty to sandy marl with lesser mud and shell fragments. Some intervals of cleaner sand in Stavely 01.|
7107|Gellibrand Marl|73357|5|Briefly described|p30, p44, p46, p48|Langhian|Chattian|Otway Basin. Correlated with Proteacidites tuberculatus Spore-Pollen Zone and Operculodinium Dinocyst Superzone, nearshore to offshore marine depositional environments. Upper part correlated to Triporopollenites bellus Spore-Pollen Zone.||Of Heytesbury Group.||Overlies Clifton Formation, underlies Port Campbell Limestone.||
7107|Gellibrand Marl|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Oligocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P3 which has high Ti/Cr and low Cr/Nb values. Lithologies based on geochemistry using the ChemLith classification includes limestone and calcareous limestone, and using the Herron classification (1988) includes Fe-shale, shale, Fe-sand and wacke. See also vi, p11 Tb.3.9, p34, p107, p130-131, p137, p257, p264.||Heytesbury Group||Overlies Nirranda Group, Narrawaturk Marl, Clifton Formation, underlies Port Campbell Limestone|Marls and calcareous mudstones.|
7107|Gellibrand Marl|73385|5|Briefly described|p5|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Narrawaturk Marl, Clifton Formation, underlies Port Campbell Limestone.|Open marine marls and calcareous mudstones.|
7107|Gellibrand Marl|73386|4|Described|p4, p6, p14, Attachment A1|Miocene|Oligocene|Otway Basin. Abundant planktonic foraminifera. Low-energy inner shelf depositional environment where there was clastic input, outer shelf environment in the Portland area. Belongs to the Middle Proteacidites tuberculatus to Lower Triporopollenites bellus spore-pollen subzones, late Oligocene to middle Miocene.||Heytesbury Group||Overlies Clifton Formation, Narrawaturk Marl, Nirranda Group, underlies Port Campbell Limestone|Dominated by marl with sporadic horizons of calcarenite, chalks and calcsiltites.|
7107|Gellibrand Marl|73486|4|Described|p509, p511-512, p516-517, p519, p526-530|Tortonian|Chattian|Otway Basin. Gradationally transitions into Port Campbell Limestone. Common to abundant foraminifera of outer shelf depositional conditions, top lies in the middle Miocene M6/N9/E1 zones at Brumbys 1 drillhole. See also p534-535.|ca 14-15 Ma|Heytesbury Group||Overlies Clifton Formation, underlies Port Campbell Limestone|Compact fossiliferous dark greenish grey marl in upper part, with well-preserved bryozoans, scaphopods, bivalves, foraminifera, ostracods and echinoids. Made up of carbonate, quartz silt, muscovite, kaolinite, anatase.|
7107|Gellibrand Marl|73594|5|Briefly described|p4|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Clifton Formation, underlies Port Campbell Limestone|Marine marls and calcareous mudstones.|
7182|Gidgealpa Group|13497|5|Briefly described|iv, p26, p69 fig 6.1, p70, |||Cooper Basin. Entirely non-marine. Hosts coal measures. See also p75, p102, p119, p131, p159, p204.|||Includes the Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie Formation, Toolachee Formation|Conformably overlain by the Nappamerri Group.||
7182|Gidgealpa Group|13516|6|Mentioned|p147, fig 5|Late Permian|Early Permian|From Cooper Basin||||||
7182|Gidgealpa Group|22839|6|Mentioned|P33|Early Permian|Late Carboniferous|||||||
7182|Gidgealpa Group|22883|6|Mentioned|P31|Early Permian|Late Carboniferous|||||||
7182|Gidgealpa Group|23154|6|Mentioned|Map Legend|Early Permian||Geological Province - Cooper Basin.  Max age ? Late Carboniferous.||||||
7182|Gidgealpa Group|23155|4|Described|p14|Late Permian|Carboniferous|Formerly excluded from the Gidgealpa Group the Merrimelia Formation is now included within the unit, see p14.||||||
7182|Gidgealpa Group|23832|4|Described|p327|Permian|Permian|Supersedes Gidgealpa Formation. Geological Province: Cooper Basin.||||||
7182|Gidgealpa Group|23858|6|Mentioned|p919|||||||||
7182|Gidgealpa Group|24210|5|Briefly described|p133 Fig. 2|Late Permian|Late Carboniferous|Geological Province: Cooper Basin.||||||
7182|Gidgealpa Group|29217|14|Not recorded|?|||||||||
7182|Gidgealpa Group|29387|6|Mentioned|Table 2|||Refs to Gatehouse(1972)||||||
7182|Gidgealpa Group|29721|6|Mentioned|Table 137|||||||||
7182|Gidgealpa Group|30511|6|Mentioned|p47|||||||||
7182|Gidgealpa Group|30515|6|Mentioned|p67|||See also P68||||||
7182|Gidgealpa Group|30519|6|Mentioned|p67|||See also P68||||||
7182|Gidgealpa Group|30540|6|Mentioned|p65|||||||||
7182|Gidgealpa Group|30544|6|Mentioned|p46|||On stratigraphic table||||||
7182|Gidgealpa Group|30804|6|Mentioned|p7|||See also Table 1||||||
7182|Gidgealpa Group|30873|2|Defined|p10|Permian|Permian|See also p11-15.||||||17-JAN-08
7182|Gidgealpa Group|31591|3|Fully described|p54|||See also p55. Early to U.Permian. Formations listed.||||||17-SEP-08
7182|Gidgealpa Group|32696|6|Mentioned|Fig.4|||Refers Gatehouse (1972)||||||
7182|Gidgealpa Group|32715|6|Mentioned|p1176|||Re oil||||||
7182|Gidgealpa Group|33074|5|Briefly described|p260|||||||||
7182|Gidgealpa Group|33078|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
7182|Gidgealpa Group|33079|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
7182|Gidgealpa Group|33130|6|Mentioned|p61|||||||||
7182|Gidgealpa Group|33131|6|Mentioned|p78|||on Fig.||||||
7182|Gidgealpa Group|33331|6|Mentioned|p40|||||||||
7182|Gidgealpa Group|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972).||||||17-SEP-08
7182|Gidgealpa Group|33827|6|Mentioned|Table 2|||||||||
7182|Gidgealpa Group|33832|6|Mentioned|p9|||Correlation||||||
7182|Gidgealpa Group|33844|6|Mentioned|p36|||||||||
7182|Gidgealpa Group|33971|6|Mentioned|p40|||Petroleum potential.||||||
7182|Gidgealpa Group|34839|6|Mentioned|p108|||||||||
7182|Gidgealpa Group|35067|6|Mentioned|Fig.4|||||||||
7182|Gidgealpa Group|35068|6|Mentioned|p54|||||||||
7182|Gidgealpa Group|35151|6|Mentioned|Fig.7|||||||||
7182|Gidgealpa Group|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
7182|Gidgealpa Group|35573|6|Mentioned|p33|||||||||
7182|Gidgealpa Group|35845|4|Described|p23|||||||||
7182|Gidgealpa Group|36099|6|Mentioned|p191|||||||||
7182|Gidgealpa Group|36643|6|Mentioned|p61|||||||||
7182|Gidgealpa Group|36917|6|Mentioned|p143|||||||||
7182|Gidgealpa Group|36920|6|Mentioned|p169|||||||||
7182|Gidgealpa Group|37065|6|Mentioned|p32|||||||||
7182|Gidgealpa Group|37287|6|Mentioned|p36|||||||||
7182|Gidgealpa Group|37565|6|Mentioned|Fig.8|||||||||
7182|Gidgealpa Group|37855|6|Mentioned|Fig.2|||||||||
7182|Gidgealpa Group|37917|6|Mentioned|p470|||||||||
7182|Gidgealpa Group|38226|6|Mentioned|Table 1|||||||||
7182|Gidgealpa Group|38977|6|Mentioned|p1422|||||||||
7182|Gidgealpa Group|39252|5|Briefly described|p20|||See also p13 and Fig.15.||||||17-JAN-08
7182|Gidgealpa Group|39254|5|Briefly described|p45|||||||||
7182|Gidgealpa Group|39255|6|Mentioned|p51|||||||||
7182|Gidgealpa Group|39261|6|Mentioned|Fig. 9|||||||||
7182|Gidgealpa Group|39276|6|Mentioned|Fig. 2|||||||||
7182|Gidgealpa Group|39445|6|Mentioned|Table 7|||See also P101, Tables 8 & 9.||||||17-SEP-08
7182|Gidgealpa Group|39478|6|Mentioned|Table 1|||||||||
7182|Gidgealpa Group|39494|6|Mentioned|Fig.3|||||||||
7182|Gidgealpa Group|40003|6|Mentioned|Table 7|||||||||
7182|Gidgealpa Group|40030|6|Mentioned|Fig.3|||||||||
7182|Gidgealpa Group|40056|6|Mentioned|p9|||||||||
7182|Gidgealpa Group|40249|6|Mentioned|p45|||||||||
7182|Gidgealpa Group|40544|6|Mentioned|Fig.4|||||||||
7182|Gidgealpa Group|40637|6|Mentioned|Fig.2|||||||||
7182|Gidgealpa Group|41097|6|Mentioned|p165|||||||||
7182|Gidgealpa Group|41131|4|Described|p333|||||||||
7182|Gidgealpa Group|41166|4|Described|p377|||||||||
7182|Gidgealpa Group|41183|6|Mentioned|Fig.3 p308|||||||||
7182|Gidgealpa Group|41198|6|Mentioned|Table 1|||||||||
7182|Gidgealpa Group|41267|6|Mentioned|p256|||||||||
7182|Gidgealpa Group|41288|6|Mentioned|Fig.7|||||||||
7182|Gidgealpa Group|41491|6|Mentioned|p180|||See also Fig.8||||||
7182|Gidgealpa Group|41536|6|Mentioned|p373|||||||||
7182|Gidgealpa Group|42006|6|Mentioned|Fig.3 P23|||||||||
7182|Gidgealpa Group|42084|6|Mentioned|Fig.3 P356|||||||||
7182|Gidgealpa Group|42085|6|Mentioned|Fig.2 P374|||||||||
7182|Gidgealpa Group|42547|5|Briefly described|p80|||||||||
7182|Gidgealpa Group|42746|5|Briefly described|Fig.2 P4|||See also Fig.6 p35.||||||17-JAN-08
7182|Gidgealpa Group|42999|6|Mentioned|Fig.7,p91|||||||||
7182|Gidgealpa Group|43004|5|Briefly described|Table 1,p179|||||||||
7182|Gidgealpa Group|44133|5|Briefly described|p78-79, 82|Late Permain|Late Carboniferous|Geological Province: Cooper Basin. Underlies: Nappamerri Group. Thickness: >1200m.||||||
7182|Gidgealpa Group|46849|6|Mentioned|Fig. 7|||||||||
7182|Gidgealpa Group|48995|6|Mentioned|Fig.3|||||||||
7182|Gidgealpa Group|60717|5|Briefly described|p40 Fig. 2|Tatarian|Late Carboniferous|Underlies the Nappamerri Group. Includes Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie and Toolachee Formations. Geological Province: Cooper Basin.||||||31-JAN-08
7182|Gidgealpa Group|61614|6|Mentioned|p290 Fig. 2|Late Permian|Late Carboniferous|Includes; Toolachee, Daralingie, Epsilon, Patchawarra and Merrimelia Formations, Murtetree Shale and Tirrawarra Sandstone. Geological Province: Cooper Basin.||||||
7182|Gidgealpa Group|61615|6|Mentioned|p302 Fig. 2|Late Permian|Late Carboniferous|Includes; Merrimelia, Tirrawarra, Patchawarra, Epsilon and Daralingie Formation, Murteree and Roseneath Shales. Geological Province: Cooper Basin.||||||07-FEB-11
7182|Gidgealpa Group|61616|6|Mentioned|p329, p330 Fig. 2|Late Permian|Late Carboniferous|Includes Patchawarra, Toolachee, Merrimelia, epsilon and Daralingie Formations, Murteree and Roseneath Shale. Geological Province: Cooper Basin.||||||
7182|Gidgealpa Group|62537|6|Mentioned|p191 Fig.2. |||Cooper Basin.|||Includes Merrimelia, Patchawarra, Epsilon, Daralingie and Toolachee Formations; Tirrawarra Sandstone; Murteree and Roseneath Shales.|Is overlain by Nappamerri Group.||
7182|Gidgealpa Group|63978|2|Defined|p9|Late Permian|Early Permian|Superseded Gidgealpa Fm. Incl: Tirrawarra Sst+ Patchawarra +Toolachee Fms. Moomba Fm.originally included. Conformable under Nappamerri Gp. Max.thick:>800m.Cooper Basin. Detailed lithology included.||||||07-FEB-11
7182|Gidgealpa Group|64048|5|Briefly described|p63|||Geological Province: Patchawarra Trough.||||||07-FEB-11
7182|Gidgealpa Group|65489|5|Briefly described|p11, p24-25, p48, p96, p130-131, p143|Kungurian|Late Carboniferous|Cooper Basin.|||Includes Merrimelia, Epsilon, Daralingie, Patchawarra, Toolachee Formations; Tirrawarra Sandstone; Murteree and Roseneath Shales.|Is overlain unconformably by Nappamerri Group.||
7182|Gidgealpa Group|67402|6|Mentioned|p90, p90 fig CPR4|Late Permian|Late Carboniferous|See also p91, p95, p96, p98, p100, p104, p105, p303.|||Includes the Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie Formation and the Toolachee Formation.|Overlain by the Nappamerri Group, Arrabury Formation.||
7182|Gidgealpa Group|68068|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Cooper Basin (subsurface only).|||Includes Merrimelia, Tirrawarra, Patchawarra and Epsilon Formations and Murteree Shale.|||
7182|Gidgealpa Group|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p207|Lopingian|Cisuralian|Kapel (1966). Nomenclatural history and subdivision outlined, from Gray and McKellar (2002). First applied to a succession of Permian sedimentary rocks in the Coopers Creek Basin and included three subunits. ~ 50-800 + m thick.|||Includes Toolachee Formation, Daralingie Formation, Roseneath Shale, Epsilon Formation, Murteree Shale, Patchawarra Formation, Tirrawarra Sandstone, Merrimelia Formation.|||04-JUL-14
7182|Gidgealpa Group|69019|5|Briefly described|p82.|Permian|Carboniferous|Southern Cooper Basin.|||||Fluvio-glacial deposits overlain by peat-swamp and flood-plain facies (coaly), followed by lacustrine sediments with intervening fluvio-deltaic units.|
7182|Gidgealpa Group|69023|4|Described|p81-85, p151|Permian|Carboniferous|Cooper Basin. Originally Gidgealpa Formation; when raised to Group status, the underlying Merrimelia Formation was excluded (Martin, 1967; Gatehouse, 1972). Subsequently included again: Callen et al. (1994), Gravestock et al. (1995), and this study. Later included Tirrawarra Sandstone. The Group has been defined (Gravestock et al., 1995) as the Cooper Basin succession of Formations that unconformably overlies Middle Carboniferous and older units and is overlain by Late Permian to Triassic Nappamerri Group (conformably) or younger sedimentary rocks (disconformably).|||Includes Merrimelia, Patchawarra, Epsilon, Daralingie and Toolachee Formations; Tirrawarra Sandstone; Murteree and Roseneath Shales.|Is overlain by Nappamerri Group conformably, and by Toolachee Formation unconformably.||
7182|Gidgealpa Group|69454|5|Briefly described|p38:4, 6, 8|Changhsingian|Asselian|Cooper Basin. The units from Patchawarra Formation upwards are lateral equivalents of Purni Formation (Pedirka Basin).|||Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree, Roseneath Shales.|Is overlain by Nappamerri Group.||12-JUL-16
7182|Gidgealpa Group|69673|6|Mentioned|p151, p153 fig 125||||||Includes Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie Formation, Toolachee Formation|||
7182|Gidgealpa Group|69728|6|Mentioned|p285|Permian|Late Carboniferous|Cooper Basin.|||Tirrawarra, Patchawarra, Moomba and Toolachee Formations.|||
7182|Gidgealpa Group|69797|5|Briefly described|p17 Fig.2|Late Permian|Late Carbonfierous|Geol. Prov: Cooper Basin.|||Toolachee Formation, Daralingie Formation, Roseneath Shale, Epsilon Formation, Murteree Shale, Patchawarra Formation, Tirrawarra Sandstone, Merrimelia Formation|||17-JAN-17
7182|Gidgealpa Group|69946|5|Briefly described|p9, p45, p54|Permian|Late Carboniferous|Cooper Basin.|||Includes Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree and Roseneath Shales.|Is overlain conformably by Nappamerri Group.||
7182|Gidgealpa Group|69947|5|Briefly described|p13 Fig.7.2|Triassic|Carboniferous|Cooper Basin.|||Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree, Roseneath Shales.|Is overlain by Nappamerri Group.||
7182|Gidgealpa Group|69948|6|Mentioned|p3-4|Permian|Late Carboniferous|Cooper Basin. Basement to Eromanga Basin in the northern Cooper region.||||||
7182|Gidgealpa Group|69982|6|Mentioned|p8||||||Includes Merrimelia Formation.|||
7182|Gidgealpa Group|70317|6|Mentioned|p33|Late Permian|Late Carboniferous|Cooper Basin.|||Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree, Roseneath Shales.|Is overlain by Nappamerri Group.||
7182|Gidgealpa Group|70823|4|Described|iv, p1-p3, p6, p20|Ladinian|Gzhelian|Cooper Basin. Is the primary source of petroleum production in the Cooper Basin and additionally also hosts extensive tight gas accumulations. Deposited in a glacial environment. Up to 1700m thick in the Nappamerri Trough and over 750m thick in the Patchawarra Trough. See also p49-p51, p54, p70, p75, p82.|||Includes the Merrimelia Formation, Patchawarra Formation, Epsilon Formation, Daralingie Formation, Toolachee Formation, Roseneath Shale, Murteree Shale and the Tirrawarra Sandstone.|Conformably overlain by the Nappamerri Group.||
7182|Gidgealpa Group|70824|5|Briefly described|p1-p3, p5, p8, p37, p48, p108, p113|Permian|Pennsylvanian|Cooper Basin. Hosts extensive tight gas accumulations. Consists of glacial deposits transitioning to peat swamp, fluvial and lacustrine deposits.||||||
7182|Gidgealpa Group|70946|5|Briefly described|p1087, p1089|Late Permian|Late Carboniferous|Cooper Basin.|||Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree, Roseneath Shales.|||08-OCT-18
7182|Gidgealpa Group|71265|5|Briefly described|p589|Changhsingian|Gzhelian|Cooper Basin.|||Merrimelia, Patchawarra, Epsilon, Daralingie, Toolachee Formations; Tirrawarra Sandstone; Murteree, Roseneath Shales.|Is overlain by Nappamerri Group.||
7182|Gidgealpa Group|71342|5|Briefly described|Ch3 p18, Ch4 p3-p4|Late Permian|Late Carboniferous|Cooper Basin. See also  Ch5 p9, Ch5 p45, Ch5 p54, Ch7 p13.|||Includes the Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie Formation and Toolachee Formation.|||
7182|Gidgealpa Group|71701|5|Briefly described|p155|Permian|Carboniferous|Cooper Basin.|||Includes the Merrimelia Formation, Tirrawarra Sandstone, Patchawarra Formation, Murteree Shale, Epsilon Formation, Roseneath Shale, Daralingie Formation and Toolachee Formation.|Overlain by the Nappamerri Group.||
7182|Gidgealpa Group|73251|6|Mentioned|p62|Lopingian|Late Carboniferous|Cooper Basin. Non-marine and marginal marine depositional environments.|||Toolachee Formation, Daralingie Formation, Roseneath Shale, Epsilon Formation, Murteree Shale, Patchawarra Formation, Tirrawarra Sandstone, Merrimelia Formation|Overlain by Arrabury Formation including Callamurra Member.||
7182|Gidgealpa Group|73495|6|Mentioned|p498-500, p503|Lopingian|Upper Pennsylvanian|Cooper Basin. Up to 1200 m thick.|||Merrimelia Formation, Patchawarra Formation|||
7195|Gilbert Range Quartzite|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Of the Belair Subgroup (Burra Group).||||||22-FEB-07
7195|Gilbert Range Quartzite|29395|5|Briefly described|p2|||See also Fig.5.||||||
7195|Gilbert Range Quartzite|29780|6|Mentioned|p29|||||||||
7195|Gilbert Range Quartzite|29831|6|Mentioned|p175|||||||||
7195|Gilbert Range Quartzite|30801|6|Mentioned|p5|||Table p5-6.||||||22-FEB-07
7195|Gilbert Range Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
7195|Gilbert Range Quartzite|32510|6|Mentioned|Table 1|||||||||
7195|Gilbert Range Quartzite|33474|6|Mentioned|Fig.2|||||||||
7195|Gilbert Range Quartzite|34535|6|Mentioned|Fig.19|||Of the Belair Sub-Gp.||||||22-FEB-07
7195|Gilbert Range Quartzite|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
7195|Gilbert Range Quartzite|34587|5|Briefly described|p36|||||||||
7195|Gilbert Range Quartzite|36623|6|Mentioned|Fig.1|||||||||
7195|Gilbert Range Quartzite|36625|6|Mentioned|Fig.1|||||||||
7195|Gilbert Range Quartzite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
7195|Gilbert Range Quartzite|41404|4|Described|p118|||||||||
7195|Gilbert Range Quartzite|41526|6|Mentioned|p47|||||||||
7195|Gilbert Range Quartzite|42098|6|Mentioned|p53|||||||||
7195|Gilbert Range Quartzite|42222|6|Mentioned|p15|||||||||
7195|Gilbert Range Quartzite|42720|6|Mentioned|map legend|Sturtian|Torrensian|||||||
7195|Gilbert Range Quartzite|43052|5|Briefly described|p183,Table 6.1|||Of Belair Subgroup.||||||22-FEB-07
7195|Gilbert Range Quartzite|44659|5|Briefly described|map legend|||Sturtian, lithology.||||||
7195|Gilbert Range Quartzite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Sturtian.||||||
7195|Gilbert Range Quartzite|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of the Belair Subgroup (Burra Group). Transitional with Mintaro Shale below and Kadlunga Slate above.||||||07-FEB-11
7195|Gilbert Range Quartzite|70405|5|Briefly described|p50|Cryogenian|Cryogenian|||Belair Subgroup|||Medium to coarse grained quartzite beds with thin siltstone intercalations. Approximately 200m thick.|
7195|Gilbert Range Quartzite|70819|6|Mentioned|p11, 13, 28|Neoproterozoic|Neoproterozoic|Clare Valley. Forms the ridge to the east of the Valley. Shallow marine deposits.|c.700 Ma.|Belair Subgroup.||Overlies Mintaro Shale. Is overlain by Kadlunga Slate.||
7195|Gilbert Range Quartzite|71237|14|Not recorded|p9, 17|||||||||
7195|Gilbert Range Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14-15, p20|Tonian|Tonian|MDA is likely close to the true depositional age (pre-Sturtian Glaciation).|731+/-34 Ma LA-ICP-MS detrital zircon MDA|Belair Subgroup||||
7206|Giles Complex|22445|5|Briefly described|p16||Stenian|Musgrave Block||||||
7206|Giles Complex|22635|6|Mentioned|p492||Stenian|||||||
7206|Giles Complex|22716|5|Briefly described|table4, p238|Stenian|Stenian|Age: 1080 Ma||||||
7206|Giles Complex|22804|6|Mentioned|p442|||Age - 1100-1200 Ma.||||||
7206|Giles Complex|23400|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
7206|Giles Complex|23483|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|23716|5|Briefly described|p4|||See also page 6 Table 1, also page 18.||||||
7206|Giles Complex|23818|6|Mentioned|p39|||Geological Province: Musgrave Block.||||||
7206|Giles Complex|23892|5|Briefly described|p42 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
7206|Giles Complex|24115|5|Briefly described|p31 Fig.28|Mesoproterozoic|Mesoproterozoic|Age: 1078+/-5 Ma (U-Pb)||||||
7206|Giles Complex|24168|6|Mentioned|p639|Mesoproterozoic|Mesoproterozoic|Age: ca 1080Ma||||||03-AUG-09
7206|Giles Complex|24169|6|Mentioned|p674|||||||||
7206|Giles Complex|24197|5|Briefly described|p97|||Overlain by Bentley Supergroup.||||||07-FEB-11
7206|Giles Complex|24301|6|Mentioned|p29|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block||||||
7206|Giles Complex|24442|5|Briefly described|p28 Fig.1|Mesoproterozoic|Mesoproterozoic|Age: 1080Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Age: ~1080 Ma. Over 20 massive and layered mafic-ultramafic intrusive bodies. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24499|5|Briefly described|Map legend|||||||||
7206|Giles Complex|24522|5|Briefly described|p80 Fig. 2|||Age: 1078Ma (Glikson et al 1996). Geological Province: Musgrave Block (Centralian Superbasin). See also p81 Fig. 3, p85-86.||||||03-AUG-09
7206|Giles Complex|24535|5|Briefly described|p16, p19 Fig.15|Mesoproterozoic|Mesoproterozoic|Of Musgrave Complex. U-Pb ages  ~1075 Ma for mafic intrusives rocks of this complex.||||||26-NOV-13
7206|Giles Complex|30202|6|Mentioned|p146|||||||||
7206|Giles Complex|30385|6|Mentioned|Table 1|||||||||
7206|Giles Complex|30386|4|Described|p13|||||||||
7206|Giles Complex|30388|6|Mentioned|p20|||On Table 1 P20||||||
7206|Giles Complex|30389|4|Described|p8|||Middle Proterozoic||||||
7206|Giles Complex|30390|4|Described|p100|||See also p101-193.||||||19-SEP-06
7206|Giles Complex|30391|5|Briefly described|p455|||||||||
7206|Giles Complex|30399|6|Mentioned|p657|||||||||
7206|Giles Complex|30513|6|Mentioned|p44|||||||||
7206|Giles Complex|30602|6|Mentioned|p658|||||||||
7206|Giles Complex|30703|6|Mentioned|p76|||Magnetic properties||||||
7206|Giles Complex|30704|4|Described|p45|||Precambrian age. See also p46-61.||||||19-SEP-06
7206|Giles Complex|30705|6|Mentioned|p517|||Precambrian age. See also P518-520||||||
7206|Giles Complex|30706|4|Described|p51|||Precambrian layered intrusions. See also p52-58.||||||19-SEP-06
7206|Giles Complex|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
7206|Giles Complex|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
7206|Giles Complex|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|31069|6|Mentioned|p187|||Refers Nesbitt et al. (1970)||||||
7206|Giles Complex|31070|6|Mentioned|p546|||||||||
7206|Giles Complex|31071|6|Mentioned|p375|||||||||
7206|Giles Complex|31072|5|Briefly described|p77|||See also p78, 79||||||19-SEP-06
7206|Giles Complex|31323|5|Briefly described|p1009|||||||||
7206|Giles Complex|31393|6|Mentioned|Pl.25|||||||||
7206|Giles Complex|31923|6|Mentioned|p6|||||||||
7206|Giles Complex|31970|4|Described|p13|||?Equivalents described||||||
7206|Giles Complex|32147|5|Briefly described|p165|||||||||
7206|Giles Complex|32192|4|Described|p158|||1000-1100my||||||
7206|Giles Complex|32280|4|Described|p115|||Mineralogy. See also p116-125.||||||19-SEP-06
7206|Giles Complex|32548|6|Mentioned|p71|||||||||
7206|Giles Complex|32692|6|Mentioned|p186|||Olivine cell dimensions||||||
7206|Giles Complex|32694|6|Mentioned|p1109|||||||||
7206|Giles Complex|33244|6|Mentioned|p1009|||||||||
7206|Giles Complex|33468|6|Mentioned|Fig.7|||||||||
7206|Giles Complex|33478|6|Mentioned|p451|||||||||
7206|Giles Complex|34208|6|Mentioned|p280|||||||||
7206|Giles Complex|34287|6|Mentioned|p32|||||||||
7206|Giles Complex|34364|6|Mentioned|Fig.1|||||||||
7206|Giles Complex|34537|6|Mentioned|p39|||||||||
7206|Giles Complex|34604|6|Mentioned|p254|||Age.||||||
7206|Giles Complex|34608|6|Mentioned|p4|||Middle Proterozoic||||||
7206|Giles Complex|34685|6|Mentioned|p353|||||||||
7206|Giles Complex|34688|6|Mentioned|p341|||||||||
7206|Giles Complex|34689|6|Mentioned|p137|||||||||
7206|Giles Complex|34718|6|Mentioned|p12|||||||||
7206|Giles Complex|34834|6|Mentioned|p221|||||||||
7206|Giles Complex|34995|6|Mentioned|p79|||||||||
7206|Giles Complex|35308|6|Mentioned|p451|||||||||
7206|Giles Complex|35323|4|Described|p404|||||||||
7206|Giles Complex|35468|6|Mentioned|p21|||||||||
7206|Giles Complex|35469|6|Mentioned|p46|||Also shown on Fig.9||||||
7206|Giles Complex|35495|6|Mentioned|p341|||||||||
7206|Giles Complex|35628|6|Mentioned|p10|||||||||
7206|Giles Complex|35726|6|Mentioned|p102|||||||||
7206|Giles Complex|36308|6|Mentioned|p211|||||||||
7206|Giles Complex|36458|6|Mentioned|p471|||||||||
7206|Giles Complex|36551|6|Mentioned|p115|||See also P24.||||||
7206|Giles Complex|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|36886|3|Fully described|p201|||||||||
7206|Giles Complex|36964|6|Mentioned|p247|||||||||
7206|Giles Complex|37697|6|Mentioned|p189|||||||||
7206|Giles Complex|37707|6|Mentioned|p25|||||||||
7206|Giles Complex|37818|6|Mentioned|p77|||||||||
7206|Giles Complex|38490|6|Mentioned|p308|||||||||
7206|Giles Complex|38761|6|Mentioned|p41|||||||||
7206|Giles Complex|38995|6|Mentioned|p9|||||||||
7206|Giles Complex|39888|6|Mentioned|p464|||See also pP475.||||||19-SEP-06
7206|Giles Complex|40229|6|Mentioned|p24|||||||||
7206|Giles Complex|40309|6|Mentioned|p90|||||||||
7206|Giles Complex|40583|6|Mentioned|p449|||||||||
7206|Giles Complex|41074|4|Described|p174|||||||||
7206|Giles Complex|41594|5|Briefly described|p72|||Also mention p30.||||||19-SEP-06
7206|Giles Complex|41638|6|Mentioned|p6|||||||||
7206|Giles Complex|41640|5|Briefly described|p9|||||||||
7206|Giles Complex|41957|6|Mentioned|p66|||||||||
7206|Giles Complex|42325|4|Described|p6-7|||||||||
7206|Giles Complex|42330|4|Described|p1443|||||||||
7206|Giles Complex|42337|4|Described|p2|||||||||
7206|Giles Complex|42775|5|Briefly described|Fig.13 P323|||||||||
7206|Giles Complex|42794|6|Mentioned|p3|||||||||
7206|Giles Complex|42940|6|Mentioned|p1|||||||||
7206|Giles Complex|43052|4|Described|p160|||Age of 1200 - 1185 Ma||||||
7206|Giles Complex|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Basic to ultrabasic intrusive complex.||||||26-MAY-05
7206|Giles Complex|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7206|Giles Complex|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7206|Giles Complex|43561|5|Briefly described|Fig.3,1434,1436,1438|||||||||
7206|Giles Complex|43591|6|Mentioned|p193|||||||||
7206|Giles Complex|43609|2|Defined|p13|Stenian|Stenian|SHRIMP U/Pb ages 1052 - 1078 Ma||||||11-SEP-08
7206|Giles Complex|43644|6|Mentioned|p592|||||||||
7206|Giles Complex|43688|5|Briefly described|p174|||||||||
7206|Giles Complex|43691|5|Briefly described|p147|||||||||
7206|Giles Complex|43692|5|Briefly described|p127||Proterozoic|||||||
7206|Giles Complex|43693|5|Briefly described|p107|||||||||
7206|Giles Complex|43694|5|Briefly described|p91|||||||||
7206|Giles Complex|43695|5|Briefly described|p69||Neoproterozoic|||||||
7206|Giles Complex|43696|5|Briefly described|p41|||||||||
7206|Giles Complex|43728|3|Fully described|p1-73|Neoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|43806|6|Mentioned|p365|||||||||
7206|Giles Complex|43969|14|Not recorded|Map Legend|||||||||
7206|Giles Complex|43971|14|Not recorded|p54||Archean|||||||07-NOV-08
7206|Giles Complex|44109|4|Described|p1|Mesoproterozoic|Mesoproterozoic|Consists of massive, partly deformed and recrystallised, layered mafic-ultramafic intrusions emplaced in the southern granulite-facies zone of   Musgrave Block.  Age: 1078+/-3Ma. ||||||
7206|Giles Complex|44139|6|Mentioned|p283-286|||Comprises several isolated sheet-like bodies of layered-basic plutonic rocks. Includes (in WA) Jameson Range, Blackstone Range, Michael Hills and Hinckley Range Gabbros. Intrudes Bentley Supergroup.| | ||||05-MAR-18
7206|Giles Complex|45087|5|Briefly described|p210|||See also p211. Chem. analyses.||||||19-SEP-06
7206|Giles Complex|45139|14|Not recorded|?|||||||||
7206|Giles Complex|45149|6|Mentioned|p19|||||||||
7206|Giles Complex|47055|5|Briefly described|p513|||||||||
7206|Giles Complex|49833|5|Briefly described|p7|||||||||
7206|Giles Complex|50607|6|Mentioned|p1.1|||Geological Province: Musgrave Block.||||||
7206|Giles Complex|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite.  Age: ~1078Ma.||||||
7206|Giles Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Generally mafic. Geological Province: Musgrave Block.||||||22-FEB-05
7206|Giles Complex|60662|5|Briefly described|Map legend|||Variably magnetic mafic-ultramafic intrusives.||||||22-FEB-05
7206|Giles Complex|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Occurred during the Giles Event from 1080-1040Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Geological Province: Musgrave Block.||||||
7206|Giles Complex|60683|4|Described|p19, p10 Tb. 1|Mesoproterozoic|Mesoproterozoic|Extensive suite of massive layered mafic to ultramafic intrusions; pyroxenite and norite. Age: 1078+/-3Ma (Sun et al 1996). In NT and SA within the Musgrave Block.||||||03-AUG-09
7206|Giles Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1078Ma. Basic to ultrabasic layered intrusive complex.||||||
7206|Giles Complex|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Basic to ultrabasic layered intrusive complex. Age: 1078 Ma.||||||
7206|Giles Complex|61154|4|Described|p13, p15|Mesoproterozoic|Mesoproterozoic|Extensive suite of massive layered maific to ultramafic intrusions, emplaced within the granulite facies terrane of the central to western Musgrave Block. Age: 1080-1040Ma. Geological Province: Musgrave Block. See also p3, p31.||||||
7206|Giles Complex|61339|6|Mentioned|Map legend|||See also in Solid Geology Sketch Map.||||||21-SEP-05
7206|Giles Complex|61340|6|Mentioned|Summary chart/Map legend|||Age: ~1080Ma.||||||
7206|Giles Complex|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Age: ~1078Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|61524|5|Briefly described|p16|||Large, layered mafic-ultramafic intrusives. Age: 1080 Ma. Geological Province: Musgrave Province.||||||
7206|Giles Complex|61733|5|Briefly described|p45-46|||Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|||||Layered mafic intrusive bodies.|
7206|Giles Complex|61864|4|Described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Also part of Warrakurna large igneous province. Main focus for Ni-Cu mineralisation. More detail of metamorphism on p18.|~1080 Ma||||Extensive voluminous mafic/ultramafic sequence (vertically stacked magma chambers with associated feeder dykes).|
7206|Giles Complex|62428|5|Briefly described|p351 Tb. 6|||Age: 1078+/-5Ma (SHRIMP U-Pb). Palaeomagnetic data.||||||10-FEB-09
7206|Giles Complex|62989|6|Mentioned|p39|||Rocks are geochemically similar to Mount Harris Basalt.||||||25-JAN-07
7206|Giles Complex|63224|6|Mentioned|p9|Neoproterozoic|Neoproterozoic|||||||02-MAY-07
7206|Giles Complex|63465|5|Briefly described|p551, p554|||Consists of a series of partly deformed and recrystallised layered mafic-ultramafic intrusions, mafic and felsic dykes, coeval mafic and felsic volcanic rocks; includes recrystallised gabbro troctolitic, gabbroic and ultramafic intrusions. Musgrave Block||||||03-AUG-09
7206|Giles Complex|64645|5|Briefly described|p16, p16 Fig. 2, p17, p18, p19|Mesoproterozoic|Mesoproterozoic|Age: 1080Ma. Geological Province: Musgrave Province. Mafic - ultramafic rocks.||||||
7206|Giles Complex|64722|5|Briefly described|Fig. 2 p3-6, p17, 22|Stenian|Stenian|Musgrave Inlier. U-Pb zircon age determined from a leucogranite interpreted as part of the intrusion.|1078 +/- 3 Ma.||||Mafic-ultramafic layered intrusions.|11-APR-12
7206|Giles Complex|64745|5|Briefly described|p376, p377, p370, p371, p373 Fig. 3|Stenian|Stenian|Mafic-ultramafic; layered intrusions are generally fault bound; Ni-PGE prospective. Age: 1.08 Ga. Geol. Prov: Fregon Domain, Musgrave Province. See also Giles Intrusions. Geol. Prov: Warakurna Large Igneous Province.||||||18-SEP-09
7206|Giles Complex|64831|5|Briefly described|p1128 Figs. 1, 2|||Layered mafic and ultramafic intrusions. See also pages 1130,1133.||||||
7206|Giles Complex|65256|6|Mentioned|p4-5, p21, p27, p31|Stenian|Stenian|Western Musgrave Block. Layered mafics to ultramafics, emplaced deeply into continental crust. 1078 Ma; coeval with Alcurra dolerite.||||||
7206|Giles Complex|65309|6|Mentioned|p5 Fig.6. |||||||||
7206|Giles Complex|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Mafic to ultramafic intrusive rocks.|
7206|Giles Complex|65385|6|Mentioned|pS131 Tab.2|Stenian|Stenian|1080-1040 Ma.||||||08-MAR-12
7206|Giles Complex|65693|6|Mentioned|p3.|Mesoproterozoic|Mesoproterozoic|Term used (Daniels 1974) to refer to Warakurna Supersuite or Giles Event.||||||
7206|Giles Complex|65906|6|Mentioned|p3, p6, p7|Mesoproterozoic|Mesoproterozoic|Mafic and ultramafic layered intrusions. Folded and subsequently cut by 1075 +/- 7 Ma Giles Event granite dykes. Is part of Warakurna Supersuite. Is overlain by Tollu Group.||||||
7206|Giles Complex|66256|6|Mentioned|p17 Fig.13|||Musgrave Province.||||||
7206|Giles Complex|66526|5|Briefly described|p15, p24.|||Mafic and ultramafic intrusions in the Musgrave Province of the Warakurna Large Igneous Province. Significant for their size and mineralisation. Age of a (?) sill associated with Bell Rock intrusion.|1078 +/- 3 Ma minimum.|||||
7206|Giles Complex|67128|5|Briefly described|p5 Fig.4|||Warakurna Large Igneous Province. Also (and in this Report, more commonly) called Giles intrusions (p6-7, p10-11, p15, p18-21). At least 20 sheet-like bodies across the Musgrave Province; described in some detail. Forms ranges with parallel ridges that correspond to aeromagnetic and gravity highs.|||||Ultramafic, gabbroic and troctolitic layered intrusions.|
7206|Giles Complex|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|~1080-1040 Ma.|||||
7206|Giles Complex|67462|5|Briefly described|Map legend.|||||||||
7206|Giles Complex|67536|5|Briefly described|Map Legend|Stenian|Stenian|Coompana Block. Informally subdivided into three parts. Rocks mapped as equivalent to the Giles Complex have an age of ca. 1078 - 1073 Ma ? These comprise gabbro and reversely magnetised bodies, possibly mafic or ultramafic.|ca. 1078 - 1073 Ma ?||||Massive anorthosite; non-magnetic to weakly magnetic; layered ultramafic and mafic sills with contrasting magnetic character; massive to weakly layered mafic to ultramafic rocks, commonly basal to layered sills; non-magnetic to weakly magnetic.|
7206|Giles Complex|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Mafic to ultramafic intrusive rocks.|
7206|Giles Complex|69003|5|Briefly described|p48 Fig.57, p51, p74|Mesoproterozoic|Mesoproterozoic|Cogenetic with the c.1068 Ma Nebo-Babel intrusion which hosts the world-class magmatic Ni-Cu-PGE sulfide deposit. A gabbroic intrusive is related to the Tollu Cu-Co prospect. Also included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|1078 Ma.|Warakurna Supersuite.||||
7206|Giles Complex|69091|6|Mentioned|p117 Fig.5.15, p142, p203|||See Giles Suite.|||||Ultramafics.|26-SEP-14
7206|Giles Complex|69153|6|Mentioned|Rocks.csv|||Sample descriptions|||||Norite, including coarse-grained norite; gabbronorite, including coarse-grained olivine gabbronorite; dunite; dolerite; olivine orthopyroxenite; lherzolite; pyroxene peridotite|
7206|Giles Complex|69436|5|Briefly described|p21:1, 10-12, 21|Mesoproterozoic|Mesoproterozoic|Central and western Musgrave Province. An extensive suite of massive, layered mafic to ultramafic intrusions emplaced within granulite-facies terranes. A single outcrop occurs in NT, SW of the Mann Ranges on a hill at the SA border; has more significant subsurface extent. Supergene enrichment of lateritised rocks of this unit in SA has produced Ni accumulations very close to the NT border. Hosts the Nebo-Babel Ni-Cu(-PGE) deposit in WA. Geochronology by Sun et al. (1996) and Howard et al. (2011) respectively.|1078 +/- 3 Ma and 1076 +/- 4 Ma.|Warakurna Supersuite.|||A medium- to coarse-grained pyroxenite with minor gabbro. Contains pseudotachylite, but no pervasive fabric. Locally capped by calcrete, laterite, chalcedony and pale brown jasper.|12-JUL-16
7206|Giles Complex|69437|5|Briefly described|p22:11|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the granulite-facies terrane of the C-W Musgrave Province.|||||Layered mafic and ultramafic intrusions.|12-JUL-16
7206|Giles Complex|69640|6|Mentioned|p174|||||||||
7206|Giles Complex|69648|6|Mentioned|p11|||Giles Complex and Tollu Volcanics, of western Musgrave Block (Fanning 1997 and Fanning et al. 2007), are compared to mafic magmatism in Proterozoic rocks in undifferentiated basement underlying Officer Basin.||||||
7206|Giles Complex|69926|6|Mentioned|p157|||Musgrave Block.|||||Layered ultramafic igneous complex.|
7206|Giles Complex|69937|5|Briefly described|p16, p34|||One of the possible sediment sources for the Amadeus Basin.|1090-1040 Ma.|||||
7206|Giles Complex|70083|6|Mentioned|p206-207|||Musgrave Inlier.|1085-1040 Ma.||Alcurra Dolerite.||Mafic and ultramafic rocks.|
7206|Giles Complex|70316|6|Mentioned|p120|||Warakurna LIP.|1073 +/- 5 Ma; 1058 +/- 14 Ma.|||||
7206|Giles Complex|71321|5|Briefly described|p5,11,22,54,64,66-67|Stenian|Stenian|Geological province: Musgrave Province. Variably deformed mafic-ultramafic layered intrusions associated with c. 1085-1040 Ma Giles Event (p11 for references). Considered to be prospective for Ni, Cu, Co, Cr, PGE, V and Ti. Sample of amphibolite facies meta-ultramafic rock (partly mylonitised hornblende-orthopyroxene-olivine-phlogopite-magnetite) of possible cumulate nature recovered from drillhole TIE RC 80 from 6-36m interval (Tucker et al., 2012) which may belong to Giles Complex. This sample was likely deformed and mylonitised during Neoproterozoic-Cambrian Petermann Orogeny. This sample is only known in this drillhole, and does not crop out in the study area. See p54 for geochmical breakdown of the ultramafic intrusion suspected to be of Giles Complex.|1085-1040 Ma|||||
7206|Giles Complex|71322|5|Briefly described|p11, p26, p28|||Summary log for drillhole DD10WOD007.|||||Anorthosite, leucogabbro, leucogabbronorite, gabbro, gabbronorite, olivine gabbro, troctolite, pyroxenite.|
7206|Giles Complex|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||~1080 Ma.|||Correlated with Alcurra Dolerite.||
7206|Giles Complex|71536|6|Mentioned|p69, p78||||c. 1080 Ma|||||
7206|Giles Complex|72238|5|Briefly described|p34, 35|Stenian|Stenian|Mafic-ultramafic intrusions that are prospective for orthomagmatic Ni-Cu - platinum group elements (PGE) mineralisation (Howard et al. 2009). Associated with coeval Alcurra Dolerite.||||||17-SEP-19
7206|Giles Complex|72476|6|Mentioned|p25 Fig.2|||Musgrave Province.||||||
7206|Giles Complex|72934|6|Mentioned|p12|||Musgrave Province. Part of the Warakurna large igneous province/Ngaanyatjarra Rift[?].||||||
7206|Giles Complex|73225|5|Briefly described|p5|||Warakurna Large Igneous Province.|c.1074 Ma.|||Correlated with Giants Head and Warbla Suites (Warakurna Supersuite).||
7206|Giles Complex|73232|6|Mentioned|p5|Stenian|Stenian|Musgrave Province. [Emplaced] during the Giles Event.|c. 1085-1030 Ma||Alcurra Dolerite|Intrudes Birksgate Complex and Pitjantjatjara Supersuite.|Includes mafic rocks.|
7315|Glanville Formation|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|23719|5|Briefly described|p31|Late Pleistocene|Late Pleistocene|See also page 30 table 9. Underlying unit Ripon Calcrete. Geological Province: Gawler Craton. Max. thickness 1 m.||||||
7315|Glanville Formation|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Otway Basin||||||
7315|Glanville Formation|23887|6|Mentioned|p204|||||||||
7315|Glanville Formation|29697|6|Mentioned|Table 7|||||||||
7315|Glanville Formation|30080|3|Fully described|p2|||Reference section given.||||||08-APR-09
7315|Glanville Formation|30752|6|Mentioned|p5|||Middle Pleistocene littoral deposit.||||||07-SEP-18
7315|Glanville Formation|30754|5|Briefly described|p22|||Stratigraphic table. See also p28,36.||||||07-SEP-18
7315|Glanville Formation|30756|6|Mentioned|p2|||||||||
7315|Glanville Formation|30807|6|Mentioned|p101|||Suggested map symbol.||||||07-SEP-18
7315|Glanville Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
7315|Glanville Formation|31655|6|Mentioned|Table 1|||Geology & hydrology.||||||07-SEP-18
7315|Glanville Formation|31850|3|Fully described|p39|||||||||
7315|Glanville Formation|31921|4|Described|p6|||||||||
7315|Glanville Formation|33330|6|Mentioned|p168|||||||||
7315|Glanville Formation|33423|6|Mentioned|p14|||Stratigraphy.||||||
7315|Glanville Formation|34180|6|Mentioned|p212|||Middle Pleistocene||||||
7315|Glanville Formation|34181|6|Mentioned|p42|||||||||
7315|Glanville Formation|34758|6|Mentioned|Table 1|||||||||
7315|Glanville Formation|35028|6|Mentioned|p337|||||||||
7315|Glanville Formation|35159|6|Mentioned|Fig.3|||||||||
7315|Glanville Formation|35772|6|Mentioned|Table 1|||||||||
7315|Glanville Formation|36894|6|Mentioned|Fig.2|||||||||
7315|Glanville Formation|38068|6|Mentioned|p76|||||||||
7315|Glanville Formation|38699|6|Mentioned|p29|||||||||
7315|Glanville Formation|38700|6|Mentioned|p43|||||||||
7315|Glanville Formation|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|39522|6|Mentioned|p91|||||||||
7315|Glanville Formation|39835|4|Described|p281|||||||||
7315|Glanville Formation|40003|5|Briefly described|Table 11|||||||||
7315|Glanville Formation|40149|6|Mentioned|p122|||||||||
7315|Glanville Formation|40219|3|Fully described|p2|||||||||
7315|Glanville Formation|40442|6|Mentioned|p35|||||||||
7315|Glanville Formation|40448|5|Briefly described|p43|||||||||
7315|Glanville Formation|40502|5|Briefly described|p83|||||||||
7315|Glanville Formation|40643|6|Mentioned|p149|||||||||
7315|Glanville Formation|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|40942|4|Described|p21|||||||||
7315|Glanville Formation|40976|5|Briefly described|p280|||||||||
7315|Glanville Formation|41078|6|Mentioned|p47|||||||||
7315|Glanville Formation|41151|6|Mentioned|p14|||||||||
7315|Glanville Formation|41245|6|Mentioned|p33|||||||||
7315|Glanville Formation|41292|6|Mentioned|p52|||||||||
7315|Glanville Formation|41362|6|Mentioned|p14|||||||||
7315|Glanville Formation|42292|6|Mentioned|Fig.2 P10|||||||||
7315|Glanville Formation|42466|5|Briefly described|Map Legend|||||||||
7315|Glanville Formation|42475|4|Described|p24|||||||||
7315|Glanville Formation|42498|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|42506|5|Briefly described|Map legend|Pleistocene||||||||
7315|Glanville Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
7315|Glanville Formation|42733|5|Briefly described|map legend|Quaternary||||||||
7315|Glanville Formation|42738|5|Briefly described|map legend|Quaternary||||||||
7315|Glanville Formation|42966|6|Mentioned|p228|||||||||
7315|Glanville Formation|43049|5|Briefly described|p26|||||||||
7315|Glanville Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Peritidal to shallow marine shelly clay, calcarenite, coquina.||||||25-MAY-05
7315|Glanville Formation|43195|5|Briefly described|Map Legend|Late Pleistocene||see also commentary on back of map. Middle to Late Pleistocene in age.||||||
7315|Glanville Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
7315|Glanville Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
7315|Glanville Formation|44133|5|Briefly described|p220 Fig. 11.2, 227-228|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|44864|6|Mentioned|Map Legend||Holocene|||||||
7315|Glanville Formation|46839|6|Mentioned|p86|||Refers to Firman 1973.||||||
7315|Glanville Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Peritidal to shallow marine shelly clay, calcarenite, coquina.||||||
7315|Glanville Formation|60958|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Seperates upper and lower members of the Bridgewater Formation. Mottled, yellow-brown sandy marl and fossiliferous limestone.||||||
7315|Glanville Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Marine to intertidal shelly sand and clay, locally calcarenited at top. Calcreted foredunes of medium to coarse-grained skeletal carbonate sand.||||||12-JAN-10
7315|Glanville Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Peritidal to shallow marine shelly clay, calcarenite and coquina.||||||
7315|Glanville Formation|61121|5|Briefly described|Map legend|Pleistocene|Pleistocene|Separates upper and lower (unnamed) members of the Bridgewater Formation. Mottle, yellow-brown sandy marl and fossiliferous limestone; basal conglomerate, middle fossil-poor marl and an upper shelly bed. Age: 0.13-0.1Ma. (Strontium isotope).||||||
7315|Glanville Formation|61155|5|Briefly described|p17|Holocene|Late Pliocene|Overlies Port Ellen Formation. Age: <2Ma. Geological Province: Eucla Basin.||||||03-MAR-10
7315|Glanville Formation|62893|4|Described|Map Legend, p23-25|Pleistocene|Pleistocene|Reflects intertidal to subtidal settings. Subsurface only (within Kimba mapsheet area). Intertongues with and is laterally equivalent to the Bridgewater Formation.|ca 0.11 Ma|||Disconformably overlain by Semaphore Sand. Equivalent to Bridgewater Formation.|Richly fossiliferous shelly sand and clay.|
7315|Glanville Formation|63124|6|Mentioned|p93|||Geological Province: Gambier Basin.||||||
7315|Glanville Formation|64282|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||07-SEP-18
7315|Glanville Formation|64966|6|Mentioned|p145|||Specimen of Katelysia rhytiphora (fossil mollusc) found in an exposure of this unit on Hindmarsh Island near the mouth of the Murray River. Unit referred to as the Last Interglacial Glanville Formation in this study.||||||07-FEB-11
7315|Glanville Formation|65375|4|Described|p7, p38, pp40-42.|Pleistocene|Pleistocene|Dominant bivalves, some still joined, are Anadara, Glycimeris and Katelysia; in situ corals occur at the base of the bed. Age range 0.125 - 0.1 Ma form Sr isotopes. The 0.045 Ma minimum age is from C14 dating (Daily et al. 1976)|c.125,000 - 45,000 years.|||Separates lower and upper parts of Bridgewater Formation.|A thin (<1 m)shell bed with abundant bivalves and other fossils; locally with a lower layer of silty limestone or a calcite conglomerate layer.|07-SEP-18
7315|Glanville Formation|65901|6|Mentioned|p177|||Interfingers with Pooraka Formation. Coastal.||||||08-MAR-12
7315|Glanville Formation|65921|6|Mentioned|p1, p2 (map legend).|Quaternary|Quaternary|Episodes of high sea level are marked by the fossil-bearing sediments of this Formation.||||||
7315|Glanville Formation|68131|6|Mentioned|p66|Pleistocene|Pleistocene|Coffin Bay Peninsula.||||||
7315|Glanville Formation|69372|6|Mentioned|p34 fig. 12|Pleistocene|Pleistocene|||||||
7315|Glanville Formation|70029|6|Mentioned|p166|||A succession of shelly coastal facies from western Eyre Peninsula, South Australia (Belperio et al. 1995; Murray-Wallace 2002).||||||
7315|Glanville Formation|70334|5|Briefly described|p63, p65|||Marine sedimentation deposited in the Adelaide region (Firman, 1966, Ludbrook, 1976, Cann, 1978).||||Equivalent to Mambray Formation.||14-OCT-19
7315|Glanville Formation|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||132,000 +/- 6,000 yrs BP (TL).||||Clay, mottled, shelly; calcarenite, skeletal, coquina.|
7315|Glanville Formation|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Fossils include oysters, corals, paired bivalves (Fulvia tenuicostata, Katelysia and Anadara) and turreted gastropods.|0.13-0.1 Ma (Sr isotope).|||Is interbedded with the Bridgewater Formation.|Mottled, yellow-brown sandy marl and fossiliferous limestone. Basal conglomerate, middle fossil-poor marl and upper shelly bed.|
7315|Glanville Formation|73292|4|Described|p952-955, p957, p58 Fig.3, p960-965|Late Pleistocene|Late Pleistocene|Crops out or is in shallow subcrop along the coastline of southern Australia. Last interglacial age, indicates relative sea level reached 2-5m APSL. Shallow marine facies with diverse molluscan faunal assemblages, at Peesey Swamp dominated by Katelysia, Chlamys and Fulvia species in life position, and foraminifera including Marginopora vertebralis. Paleoenvironments of low- to medium-energy sheltered sandflats to a shallow-water seaway inferred, paleowater depth of up to 4m during the Last Interglacial Maximum (MIS 5e). Capped by pedogenically modified units with strongly indurated calcretes and rhizoliths on the southern Yorke Peninsula. Additional AAR ages of 117.5 +/- 4.5 ka and 115.0 +/- 5.4 ka (Pan et al., 2018), 113 +/- 8 ka, 112 +/- 10 ka, 122 +/- 1 ka.|127.3 +/- 2.1 ka, 115.0 +/- 5.4 ka, 112 +/- 10 ka|||Unconformably overlies the Point Turton Limestone, southern Yorke Peninsula.|Partially consolidated, in places strongly indurated, richly fossiliferous medium- to very coarse-grained, mixed quartz-skeletal carbonate sand. Commonly capped by a strongly indurated calcrete.|
7387|Glendower Formation|23493|6|Mentioned|p16 Tb. 1|Pliocene|Pliocene|Of Whitehouse (1954).  Correlated with Lynd Formation.  On HUGHENDEN Sheet.||||||
7387|Glendower Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
7387|Glendower Formation|24013|5|Briefly described|p17 Tb. 1|Tertiary|Tertiary|Correlated with the Lynd Formation.||||||
7387|Glendower Formation|29660|6|Mentioned|p7|||||||||
7387|Glendower Formation|30103|5|Briefly described|p9|||Table 3 on p9. Early Tertiary age.||||||31-AUG-20
7387|Glendower Formation|30104|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|30853|5|Briefly described|Table 3|||Tertiary||||||
7387|Glendower Formation|30855|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|30856|4|Described|Table 4|||See p12. Tertiary.||||||31-AUG-20
7387|Glendower Formation|30857|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31144|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31145|5|Briefly described|Table 1|||Tertiary.||||||
7387|Glendower Formation|31430|5|Briefly described|Table 1|||Tertiary||||||
7387|Glendower Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
7387|Glendower Formation|31432|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|31436|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31438|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31441|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31443|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31553|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|32553|4|Described|p38|||||||||
7387|Glendower Formation|33067|4|Described|Table 1|Tertiary|Tertiary|Quartz sandstone, sandy conglomerate, minor siltstone, silcrete.||||||07-JUL-04
7387|Glendower Formation|33069|4|Described|p7|||Tertiary||||||
7387|Glendower Formation|33072|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|33074|6|Mentioned|p262|||||||||
7387|Glendower Formation|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33081|6|Mentioned|p26|||||||||
7387|Glendower Formation|33082|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33083|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33087|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33088|4|Described|Table 4|||Tertiary||||||
7387|Glendower Formation|33089|4|Described|Table 2|||Tertiary||||||
7387|Glendower Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
7387|Glendower Formation|33095|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33150|5|Briefly described|p13|||Possible equiv. Floraville & Bulimba Fms.||||||
7387|Glendower Formation|33182|6|Mentioned|p193|||||||||
7387|Glendower Formation|33449|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|33639|5|Briefly described|Table 2|||Tertiary.||||||
7387|Glendower Formation|33640|4|Described|Table 2|||Tertiary||||||
7387|Glendower Formation|33644|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33647|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33648|6|Mentioned|p21|||Stratigraphy.||||||
7387|Glendower Formation|33938|6|Mentioned|p48|||Refers Whitehouse (1954).||||||
7387|Glendower Formation|34065|4|Described|p6|||||||||
7387|Glendower Formation|34091|5|Briefly described|Table 1|||Tertiary. See also P9||||||
7387|Glendower Formation|34217|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|34218|4|Described|p11|||See also pp12,14,17, Table 1. Tertiary.||||||31-AUG-20
7387|Glendower Formation|34485|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|34486|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|34487|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|34948|6|Mentioned|p317|||||||||
7387|Glendower Formation|35187|6|Mentioned|Table1|||||||||
7387|Glendower Formation|35322|6|Mentioned|p418|||||||||
7387|Glendower Formation|36966|6|Mentioned|p92|||||||||
7387|Glendower Formation|37607|4|Described|p333|||See also Fig.4.||||||
7387|Glendower Formation|39322|6|Mentioned|Fig.3|||||||||
7387|Glendower Formation|39445|5|Briefly described|Table 14|||||||||
7387|Glendower Formation|40584|6|Mentioned|p435|||||||||
7387|Glendower Formation|40675|6|Mentioned|Table 8A|||||||||
7387|Glendower Formation|41710|6|Mentioned|p222|||||||||
7387|Glendower Formation|42084|6|Mentioned|Fig.3 P356|||||||||
7387|Glendower Formation|42447|6|Mentioned|Fig.10|||||||||
7387|Glendower Formation|42999|6|Mentioned|p98|||||||||
7387|Glendower Formation|43008|5|Briefly described|map legend|||||||||
7387|Glendower Formation|43995|14|Not recorded|Tb.p9||Tertiary|||||||
7387|Glendower Formation|44016|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44017|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44018|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44019|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44020|14|Not recorded|p8,11,14-5,Tb.1,Fig2||Tertiary|||||||
7387|Glendower Formation|44042|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44067|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44089|4|Described|Tb.1,p6,8,map||Tertiary|||||||
7387|Glendower Formation|44091|14|Not recorded|p65||Tertiary|||||||
7387|Glendower Formation|44098|14|Not recorded|p98||Tertiary|||||||
7387|Glendower Formation|44099|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44123|14|Not recorded|p388-390|||||||||
7387|Glendower Formation|44133|5|Briefly described|p190 Fig. 10.30|Late Eocene|Late Paleocene|Geological Province: Waite Basin.||||||
7387|Glendower Formation|44251|14|Not recorded|p4||Pliocene|Correlated with Lynd Formation. Ref. to Laing and Power 1959.||||||
7387|Glendower Formation|44252|14|Not recorded|p397|||||||||
7387|Glendower Formation|44269|14|Not recorded|p17,18||Cenozoic|||||||19-NOV-08
7387|Glendower Formation|44295|14|Not recorded|p6||Pliocene|||||||
7387|Glendower Formation|44373|14|Not recorded|p20|||Map only.||||||
7387|Glendower Formation|44377|14|Not recorded|p19|||See also Lexicon.||||||
7387|Glendower Formation|44587|14|Not recorded|p376,,381|||Boulders of 'billy'.||||||
7387|Glendower Formation|44800|4|Described|p16,18,53,map||Tertiary|(Early Tertiary)||||||
7387|Glendower Formation|45009|14|Not recorded|p73||Pliocene|||||||
7387|Glendower Formation|45110|5|Briefly described|p129|||||||||
7387|Glendower Formation|45145|6|Mentioned|Table 7|||||||||
7387|Glendower Formation|46802|6|Mentioned|p136|||||||||
7387|Glendower Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
7387|Glendower Formation|48908|14|Not recorded|Tb.1||Tertiary|||||||
7387|Glendower Formation|49011|6|Mentioned|p28|||||||||
7387|Glendower Formation|60080|5|Briefly described|Map legend|Oligocene|Paleocene|Quartzose sandstone, sandy conglomerate with quartz, agate and chert clasts, minor siltstone; silcrete. Overlies Winton Formation; underlies Whitula Formation.||||||16-SEP-08
7387|Glendower Formation|61155|5|Briefly described|p17|Middle Eocene|Late Paleocene|Sediments spread in thin sheets over large areas of the Birdsville Basin. Max. thickness: 70m. See also p2, p3.||||||03-MAR-10
7387|Glendower Formation|61312|5|Briefly described|p66|Tertiary|Tertiary|Quartzose, arenaceous and conglomeratic fluviatile deposits. Found particularly in the Milparinka-Tibooburra district. Geological Provnce: Eromanga Basin.||||||
7387|Glendower Formation|63979|5|Briefly described|p55|Tertiary|Tertiary|Overlies the Winton Formation. Geological province: Eromanga Basin.||||||07-FEB-11
7387|Glendower Formation|64047|2|Defined|p60-61||Middle Eocene|Unconformable on Winton Fm; overlain by Whitula Fm. Max. thickness: 145m. Geol.prov: Eromanga Basin. Contains quartzose sandstone, quartz pebble conglomerate, sandy conglomerate and minor siltstone ans mudstone;  reworked clasts of Winton Fm. at base..||||||16-APR-08
7387|Glendower Formation|66131|5|Briefly described|p240, p242 Fig.2|Eocene|Paleocene|Late Paleocene to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||Correlative of the Eyre Formation.||
7387|Glendower Formation|66623|6|Mentioned|p273.|||Lateral equivalent of Eyre Formation.||||||
7387|Glendower Formation|67561|6|Mentioned|p54, p56||||||||Comprises quartzose sandstone, quartz pebble conglomerate, sandy conglomerate and minor siltstone and mudstone.|
7387|Glendower Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
7387|Glendower Formation|68901|5|Briefly described|p7 Fig. ii|Quaternary|Paleogene||||||Quartzose sandstone, conglomerate; commonly silcretised.|26-SEP-18
7387|Glendower Formation|69599|5|Briefly described|p580, p584, p599-600, p650|Eocene|Paleocene|Lake Eyre Basin. Formerly the Glendower Series. Now applies to all similar sedimentary packages covering the Eromanga Basin. Semicontinuous belt from E of Hughenden to near Longreach. Up to 170m thick. Fluvial valley fill sediments. No known fossils. Capped by silcrete and laterite of the Featherby Surface. RELATED UNITS (continued): Also correlated (at least partly) with Eyre, Moonie, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||||Unconformably overlies Winton Formation. Is overlain by Whitula Formation and, locally, by Sturgeon Basalt. See COMMENTS for more.|Quartz sandstone, pebble conglomerate, sandy conglomerate and sudordinate siltstone and mudstone. Upper parts are heavily silcretised in most areas.|
7387|Glendower Formation|69952|5|Briefly described|p16|Paleogene|Paleogene||||||Quartzose sandstone, conglomerate; commonly silcretised.|
7387|Glendower Formation|70720|6|Mentioned|p6|||||||Overlies Winton Formation.||
7387|Glendower Formation|70821|5|Briefly described|p15, p25-26, p33, p80, p82, p86,p115-116|Eocene|Eocene|Originally the Glendower Series of Bryan and Jones (1946); [misquoted in this study as the Glendower series]. Lake Eyre Basin (NSW and QLD). Forms a series of dendritic silcrete ridges, equivalent to the Eyre Formation in SA. Highly resistive. Forms slope deposits of scree or colluvium of gravel to boulder-sized fragments. 52m thick in Mirintu 1 petroleum well. Hydrostratigraphic properties.||||Unconformably overlies Winton Formation. Equivalent to Eyre Formation.|Silcreted and inverted palaeochannels of sandstone and conglomerate.|
7429|Glenloth Granite|22613|6|Mentioned|p29|Archean|Archean|||||||07-NOV-08
7429|Glenloth Granite|22629|5|Briefly described|fig2p147,160|Paleoproterozoic|Archean|||||||07-NOV-08
7429|Glenloth Granite|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: 2435, 2460, 2499 Ma. Parent: Mulgathing Complex.||||||07-NOV-08
7429|Glenloth Granite|24505|5|Briefly described|p8, p9 Tb. 1|Archean|Archean|Of the Mulgathing Complex.  Hosts vein quartz mineralisation.  Age: ~2500Ma.  Geological Province: Gawler Craton.||||||07-NOV-08
7429|Glenloth Granite|30809|6|Mentioned|p6|||Includes age||||||
7429|Glenloth Granite|33468|5|Briefly described|p204|||Age||||||
7429|Glenloth Granite|33727|4|Described|p35|||Incl. dating||||||
7429|Glenloth Granite|37461|6|Mentioned|p315|||||||||
7429|Glenloth Granite|38605|6|Mentioned|p13|||||||||
7429|Glenloth Granite|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7429|Glenloth Granite|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
7429|Glenloth Granite|40644|5|Briefly described|p124 Fig. 3, p126, p127|Paleoproterozoic|Paleoproterozoic|Included in the Mulgathing Complex grouping.  Age range: 2232+/-338Ma to 2299+/-41Ma.||||||07-NOV-08
7429|Glenloth Granite|41972|6|Mentioned|p365|||||||||
7429|Glenloth Granite|42465|5|Briefly described|Map Legend|||||||||
7429|Glenloth Granite|42469|5|Briefly described|p10|||||||||
7429|Glenloth Granite|42721|5|Briefly described|map legend|Proterozoic||||||||
7429|Glenloth Granite|42722|5|Briefly described|map legend|Proterozoic|Proterozoic|Pink and cream foliated granite with pods and irregular bands of calc-silicate hornfels.||||||07-APR-05
7429|Glenloth Granite|43052|4|Described|p45,Table 3.2|||Of Mulgathing Complex. Minimum age of 2299+/-41 Ma.||||||02-JUN-09
7429|Glenloth Granite|43071|4|Described|p8,Table 2||Paleoproterozoic|||||||07-NOV-08
7429|Glenloth Granite|43094|4|Described|p14|||||||||
7429|Glenloth Granite|43839|6|Mentioned|p29|||Now considered to be deformed Hiltaba Suite granite||||||12-JUL-16
7429|Glenloth Granite|44935|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
7429|Glenloth Granite|48894|6|Mentioned|p73|||1930+-200my||||||
7429|Glenloth Granite|50605|5|Briefly described|p8.7|||Of the Mulgathering Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
7429|Glenloth Granite|60484|5|Briefly described|p33 Fig. 1|||At Yarlbrinda Hill this rock is now mapped as the Tunkillia Suite.  Geological Province: Gawler Craton. See also p35.||||||17-MAR-05
7429|Glenloth Granite|60704|5|Briefly described|p686 Fig.1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
7429|Glenloth Granite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 2499-2435Ma. Synorogenic gneissic granite to granodiorite.||||||07-NOV-08
7429|Glenloth Granite|61108|5|Briefly described|map legend|Paleoproterozoic|Archean|Synorogenic gneissic granite to granodiorite. Age: 2499-2435 Ma.||||||07-NOV-08
7429|Glenloth Granite|61659|6|Mentioned|p31 Fig.2. ||||2500 Ma (Daly et al. 1998).|||||
7429|Glenloth Granite|63866|5|Briefly described|p18|||Harris Greenstone Belt, Gawler Craton.||||Intrudes the Lake Harris Komatiite.||
7429|Glenloth Granite|64130|6|Mentioned|p1379 |Neoarchean|Neoarchean||c.2520-2500 Ma|||||
7429|Glenloth Granite|64137|5|Briefly described|p1542 Fig.1, p1543  |Archean|Archean|Hosts the Glenloth goldfield. Neodymium isotope data.||Unit in Mulgathing Complex.||||
7429|Glenloth Granite|64576|6|Mentioned|p625 Fig. 2|Archaean|Archaean|||||||
7429|Glenloth Granite|64722|5|Briefly described|p12|Siderian|Neoarchean|Emplaced into the Mulgathing Complex, Gawler Province, at 2500 Ma.||||||
7429|Glenloth Granite|64739|6|Mentioned|p265 Table 1. |||Gawler Craton.|2500 Ma.|||||
7429|Glenloth Granite|65376|5|Briefly described|p127 Fig.4.5, p190, pp194-197.|Paleoproterozoic|Archean||2509 +/- 23 Ma to 2458 +/- 10 Ma.|Unit in Mulgathing Complex.||Discordant contact with Lake Harris Komatiite. Veins intrude Hopeful Hill Basalt.|Poorly-exposed, well-foliated, quartz-feldspar gneiss; locally forms thin foliated quartz diorite to granodiorite dykes.|
7429|Glenloth Granite|65390|5|Briefly described|p14, p22 Fig. 3|Paleoproterozoic|Neoarchean|Of Harris Greenstone and Wilgena Domains, Gawler Craton. Acid intrusives syn-tectonic with Christie and Kenella Gneisses. Age c. 2500 Ma. Sheared and fractured; hosts gold mineralisation.||||||
7429|Glenloth Granite|65772|6|Mentioned|p229 Fig.2|Archean|Archean|||||||
7429|Glenloth Granite|66302|5|Briefly described|p10-p13, p61, p61 Fig.14, p85|Siderian|Neoarchean|Christie and Wilgena Domains, Gawler Craton. Interpreted to have been intruded in a convergent tectonic setting on the basis of its geochemistry. |2499 +/-11 Ma (SHRIMP U-Pb, Fanning 1997)|Mulgathing Complex|||Medium to coarse-grained, leucocratic gneiss or gneissic granitoid ranging in composition from granite to monzogranite and granodiorite.|
7429|Glenloth Granite|67058|5|Briefly described|p476.|Neoarchean|Neoarchean|Central Gawler Craton.|c.2500 Ma.|Unit in Mulgathing Complex.||||
7429|Glenloth Granite|67536|5|Briefly described|Map Legend|Siderian|Neoarchean|Gawler Craton.|2499 +/- 11 Ma - 2435 +/- 17 Ma||||Gneissic granite to granodiorite.|
7429|Glenloth Granite|68128|6|Mentioned|p2, p5-6|Palaeoproterozoic|Archaean|Gawler Craton. An Additional U-Pb zircon date of 2436 +/- 9 Ma is derived from Fanning et al, 2007.|2318 +/- 55 Ma (Rb-Sr, Webb, 1978)|Mulgathing Complex||||31-JAN-23
7429|Glenloth Granite|68208|6|Mentioned|p31 Fig.2|Paleoproterozoic|Neoarchean||Crystallisation age ~2510 Ma|Of Mulgathing Complex||||
7429|Glenloth Granite|69649|5|Briefly described|p9, p7, p8 Fig.6, p35, p51|Archean|Archean|Also appears on p7 as Glenolith Granite. Syn-tectonic acid intrusives; part of Harris Greenstone Domain.|2440 Ma. U-Pb (Daly and Fanning, 1990).|Unit in Mulgathing Complex.|||Granite to granodiorite; poorly to well foliated, medium- to coarse-grained, pinkish-brown to grey.|23-FEB-15
7429|Glenloth Granite|70789|5|Briefly described|p316, p318 Fig.2, p321|Archean|Archean|Part of the crystalline basement to the Gawler Craton. Syn-sedimentary intrusion. Appears as Glenloth granite in Fig.2. AFT results tabulated; central ages from 282 +/- 15 Ma to 330 +/- 9 Ma.||Mulgathing Complex.||||
7429|Glenloth Granite|71859|6|Mentioned|p28||||c. 2510 Ma|||||
7429|Glenloth Granite|73230|4|Described|p6-8, p11, p15|Neoarchean[?]|Neoarchean|Gawler Craton. Domain: Harris Greenstone. Hosts gold mineralisation in quartz veins, which is thought to be related to Hiltaba Suite magmatism. Metamorphism at c. 2436 Ma. Includes compositional layering within the granite interpreted to represent primary magmatic flow banding [magmatic foliation].|c. 2509-2507 Ma (magmatic)|Mulgathing Complex||Intrudes Kenella Gneiss, Lake Harris Komatiite, Hopeful Hill Basalt, and South Lake Gabbro.|Pink-brown to grey granite to granodiorite and quartz monzonite with quartz, microcline and plagioclase. Magmatic foliation.|
7429|Glenloth Granite|73235|6|Mentioned|p53, p61, p64|||Gawler Craton. Wilgena and Harris Greenstone regions. Hosts gold mineralisation in the Labyrinth mineral field of the Kararan (Gawler Range Volcanics) gold mineral system, and Fabian, Royal Tiger, Glen Markie, and Kingfisher gold mineralisation in the Glenloth mineral field of the same gold mineral system. Has a vague spatial relationship with mineralisation, which has yet to be clearly defined.||||||
7456|Glyde Formation|30385|4|Described|p8|||||||||
7456|Glyde Formation|30388|4|Described|Table 1|||Middle Proterozoic. Table 1 on P8. Pussy Cat Group.||||||
7456|Glyde Formation|30390|4|Described|p50|||||||||
7456|Glyde Formation|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7456|Glyde Formation|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Of Pussy Cat Group.||||||
7456|Glyde Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7456|Glyde Formation|36551|6|Mentioned|Table 31|||||||||
7456|Glyde Formation|36886|4|Described|p199|||||||||
7456|Glyde Formation|65256|6|Mentioned|p14, p32|||Of the Pussy Cat Group. A succession of interlayered siltstone, shale, dolomite and epidotised amygdaloidal basalt. May be equivalent to Tjuninanta Formation of Tjauwata Group.||||||
7456|Glyde Formation|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.||Unit in Pussy Cat Group.|||Mafic volcanic, volcaniclastic and clastic rocks.|11-APR-12
7456|Glyde Formation|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Mapped as three separate but un-named units.|1072 - 1065 Ma.|Unit in Pussy Cat Group.|||Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; ahpyric rhyolitic and trachydacitic volcanic siltstone and mudstone; interlayered sandstone, well- to very poorly-sorted conglomerate, and basalt.|
7456|Glyde Formation|67375|4|Described|p19 Fig.11, p38 Table 1, p47. |Mesoproterozoic|Mesoproterozoic|The volcaniclastic metasedimentary rocks of the lower part of this unit were deposited in a volcanically active alluvial to fluviolacustrine environment.|1071-1065 Ma.|Unit in Pussy Cat Group.||Intercalated with and overlies Kathleen Ignimbrite. Is overlain by Wururu Rhyolite or Gurgadi Basalt.|Low-grade metamorphic, volcaniclastic sedimentary rocks: mudstones, siltstones and shales; arkosic or calcareous sandstones, and diamictites; overlain by amygdaloidal metabasaltic lavas.|
7456|Glyde Formation|67553|4|Described|p20-21,40,44,48-51,94,97-100,104-106|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Depositional age at 1070+\-5 Ma (GSWA 195723) coeval with eruption of Kathleen Ignimbrite. Juxtaposed against diamictite in the upper Mount Palgrave Group as a result of NW-trending faulting and reactivation of earliers sub-volcanic block faults at <1055+\-10 Ma. Outcrop as a conspicuous, recessive, NNE-trending band along the northern side of the Mount Glyde Ranges. Lower siliciclastic section deposited in a volcanically active alluvial to fluviolacustrine environment. Upper section was erupted and deposited subaerially, and entered bodies of water forming local occurrences of pepperites and hyaloclastics. Underwent moderate temperature, LP metamorphism.|1070+\-5 Ma|Unit of Pussy Cat Group.||Uppermost unit of Pussy Cat Group. Overlain by Wururu Rhyolite or Gurgadi Basalt/Cassidy Group. Intruded by the Kathleen Ignimbrite.|Massive to laminated mudstones, siltstones, and shales; well to poorly sorted, partly arkosic or calcareous sandstones; conglomerates; and very poorly sorted, matrix-supported diamictites. Extrusive amygdaloidal to massive metabasaltic lava.|06-AUG-19
7456|Glyde Formation|68995|5|Briefly described|p15, p49 Fig.25|||Primarily erupted in a sub-aerial environment, but locally some lavas entered small water bodies where they formed peperites and hyaloclastites.||Pussy Cat Group||Overlies the Kathleen Ignimbrite.|Massive and amygdaloidal, mostly aphyric, basaltic lavas intercalated with minor amounts of metasedimentary rocks, including siltstone, quartzite and siliceous microbialites.|
7456|Glyde Formation|68996|5|Briefly described|p7|Mesoproterozoic|Mesoproterozoic|||Pussy Cat Group|||Mafic volcanic and volcaniclastic sedimentary rocks.|
7456|Glyde Formation|69003|5|Briefly described|p51|Mesoproterozoic|Mesoproterozoic|Southern Talbot Sub-basin.||Pussy Cat Group.||Intercalated with Glyde Formation.|Volcaniclastic rocks and minor amygdaloidal basalt; intercalated with flow-banded ignimbrites of the Kathleen Ignimbrite.|
7456|Glyde Formation|69091|5|Briefly described|p71 Fig.4.14, p76|||Talbot Sub-basin||Pussy Cat Group|||Basalt dominated sequence and volcaniclastic dominated sequence.|
7456|Glyde Formation|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample description includes: metamafic volcanic rock; dark-coloured; fine-grained volcaniclastics (mudflow and floodplain deposits) with a dominantly mafic volcanic source; altered by contact metamorphism to biotite-rich microgranofelses; meta-igneous mafic volcanic; meta-sedimentary.||Pussy Cat Group|||Vesicular and amygdaloidal basalt, andesite, and basaltic andesite; interbedded with siliciclastic rocks; epidotized|
7456|Glyde Formation|69655|6|Mentioned|p57|||||Bentley Supergroup||||
7456|Glyde Formation|69729|5|Briefly described|p82|||Bedrock of Talbot Sub-basin.||Pussy Cat Group.|||Volcaniclastics- and basalt-dominated sequences.|
7456|Glyde Formation|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The two facies are mapped separately.|c.1065 Ma.|Pussy Cat Group.|||Vesicular and amygdaloidal basalt, and minor basaltic andesite, interbedded with fine- to coarse-grained siliciclastic rocks, epidotised; vesicular and amygdaloidal basalt, basaltic andesite and andesite, locally plagioclase-phyric (section only).|
7456|Glyde Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Three facies associations are mapped separately.|1071-1047 Ma.|Pussy Cat Group.||Overlies Mount Waugh Formation. Is overlain by Wururu Rhyolite. Is intruded by Warakurna Supersuite.|Typically vesicular and amygdaloidal basalt, and minor basaltic andesite; interbedded with fine- to coarse-grained siliciclastic rocks; epidotised.|
7456|Glyde Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Bentley Supergroup|||Vesicular and amygdaloidal basalt plagioclase porphyritic basalt, basalt, basaltic andesite and andesite. Diamictite with sub-rounded to angular, mafic-felsic volcanic clasts. Medium-fine grained siliclastic rocks; rare calc-silicate rocks.|
7456|Glyde Formation|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Basalt, and minor basaltic andesite, plagioclase porphyritic basalt, vesicular and magdaloidal basalt, andesite, medium- to fine-grained siliciclastic rocks; rare calc-silicate rocks, diamictite, evaporite horizons and microbialites.|
7456|Glyde Formation|71211|5|Briefly described|p26-p28, p30, p86|||See also p87 fig 3.2, p135, p137 fig 4.2, p138, p216. ||||Overlies the Cleghorne Formation. Intruded by the Rowland Suite.|Massive basalt and interbedded volcaniclastic rocks.|
7456|Glyde Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||ash tuff, shale, siltstone, basalt|
7456|Glyde Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Basalt; vesicular, amyddaloidal, palgioclase porphyritic, and minor basaltic andesite; diamictite, medium- to fine-grained siliciclastics, evaporites and microbialites.|
7456|Glyde Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Pussy Cat Group|||Typically vesicular and amygdaloidal basalt, and minor basaltic andesite; interbedded with fine- to coarse-grained siliciclastic rocks; epidotized.|
7456|Glyde Formation|72443|6|Mentioned|p738|||||Pussy Cat Group||||
7458|Glyde Hill Volcanic Complex|24346|5|Briefly described|p99|Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics.||||||
7458|Glyde Hill Volcanic Complex|24356|6|Mentioned|p1593 Fig. 1|||||||||
7458|Glyde Hill Volcanic Complex|24474|3|Fully described|p36|||Of the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
7458|Glyde Hill Volcanic Complex|29838|2|Defined|p12|Mesoproterozoic|Mesoproterozoic|||||||
7458|Glyde Hill Volcanic Complex|30984|2|Defined|p7|Proterozoic|Proterozoic|Unit members defined||||||
7458|Glyde Hill Volcanic Complex|35107|6|Mentioned|p200|||||||||
7458|Glyde Hill Volcanic Complex|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7458|Glyde Hill Volcanic Complex|40644|6|Mentioned|p124 Fig. 3, p136|Mesoproterozoic||Age: 1565+/-124Ma (see table 4, p135).||||||13-AUG-08
7458|Glyde Hill Volcanic Complex|41972|6|Mentioned|Table 3 P378|||||||||
7458|Glyde Hill Volcanic Complex|42721|5|Briefly described|map legend|Carpentarian||||||||
7458|Glyde Hill Volcanic Complex|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Includes: Yantea Rhyodacite, Nuckulla Basalt, Bunburn Dacite, Wheepool Rhyolite, Mangaroongah Dacite and Childera Dacite of the Gawler Volcanics.||||||02-JUN-09
7458|Glyde Hill Volcanic Complex|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
7458|Glyde Hill Volcanic Complex|43052|4|Described|p111|||see also Fig.5.3.||||||
7458|Glyde Hill Volcanic Complex|43071|5|Briefly described|p12,Table 2|||||||||
7458|Glyde Hill Volcanic Complex|43094|4|Described|p22|||see also Table 4.||||||
7458|Glyde Hill Volcanic Complex|64131|6|Mentioned|p1411 |||Subaerial mafic volcanic centre exposed in the Gawler Range Volcanics. Unmineralised.||||||
7458|Glyde Hill Volcanic Complex|65922|5|Briefly described|p16|Calymmian|Calymmian|Also referred to as Glyde Hill Complex. Name, in the Lake Everard area of South Australia, for the 'older' or 'lower' Gawler Range Volcanics.||||||
7458|Glyde Hill Volcanic Complex|67900|5|Briefly described|p20, 30-31|Mesoproterozoic|Mesoproterozoic|Lake Everard, Gawler Craton. Also appears as GHVC.||Lower Gawler Range Volcanics.|||Ranges through basalt, andesite, dacite, rhyodacite and rhyolite. The felsic units are direct fractionates of the mafic units.|
7458|Glyde Hill Volcanic Complex|67909|4|Described|p125-127, 129-130, 140-141|Mesoproterozoic|Mesoproterozoic|Blissett (1975). Lake Everard. Simplified log. Units range from 10km to 80km across.||Gawler Range Volcanics, lower.|Childera, Mangaroongah, Bunburn, Whyeela Dacites; Yandoolka, Wheepool, Baldry Rhyolites; Waurea Pyroclastics; Nuckulla Basalt; Yantea Rhyodacite.|Is cut by Moonamby Dyke Suite.|Dominantly (>90%) porphyritic felsic units; minor andesite and very minor basalt.|
7458|Glyde Hill Volcanic Complex|69649|4|Described|p16-25|Mesoproterozoic|Mesoproterozoic|Defined by Blissett (1975). Lake Everard area. Common petrogenesis with Chitanilga Volcanic Complex. Giles (1977) defined 11 constituents.||Unit in lower Gawler Range Volcanics.|Includes Childara, Mangaroongah, Bunburn and Whyeela Dacites; Arburee, Karkulta and Baldry Rhyolites; Nuckulla Basalt; Yantea Rhyodacite.||A series of dacite, rhyodacite and rhyolite units: strongly welded crystal and/or vitric and/or lithic ashflow tuffs, lava domes, localised lava flows, plugs and dykes.|26-FEB-15
7458|Glyde Hill Volcanic Complex|70659|5|Briefly described|p5-6, p8|Mesoproterozoic|Mesoproterozoic|Other constituents include localised lava flows (Arburee Rhyolite, Karkulta Rhyolite and Whyeela Dacite), localised pyroclastic units (Waurea Pyroclastics and an unnamed unit), and a basaltic sequence of limited extent (Nuckulla Basalt). Crops out over 5000 km2 S of Lake Everard.|||Includes Childera Dacite, Manganroongah Dacite, Bunburn Dacite, Yantea Rhyolite, Wheepool Rhyolite. See Comments for others.||Mafic to felsic volcanic sequences, dominated by felsic lavas interbedded with polymict breccia and pumiceous and crystal-rich volcaniclastic facies with minor basalt.|
7458|Glyde Hill Volcanic Complex|70738|6|Mentioned|p186-187|||Gawler Craton. Crops out in Lake Everard area.|||Nuckulla Basalt.|||
7458|Glyde Hill Volcanic Complex|70816|5|Briefly described|p4-5|||Lake Everard area, Gawler Ranges.||Unit of lower Gawler Range Volcanics.|Includes Whyeela Dacite, Yantea Rhyolite, Nuckulla Basalt, Baldry Rhyolite, Bunburn Dacite, Waurea Pyroclastics, Wheepool, Arburee and Karkulta Rhyolites, Mangaroongah Dacite, Childera Dacite|||
7458|Glyde Hill Volcanic Complex|71317|5|Briefly described|p96, p112|||||||||
7458|Glyde Hill Volcanic Complex|72090|5|Briefly described|p12|||Gawler Craton. Also includes the Baldry Rhyolite, Bunburn Dacite, Waurea Pyroclastics, Wheepool Rhyolite, Arburee Rhyolite, Karkulta Rhyolite, Mangaroongah Dacite and Childera Dacite.|||Includes the Whyeela Dacite, Yantea Rhyolite, Nuckulla Basalt.|||
7458|Glyde Hill Volcanic Complex|72462|6|Mentioned|p8|||Gawler Craton.||||||
7458|Glyde Hill Volcanic Complex|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
7458|Glyde Hill Volcanic Complex|73162|6|Mentioned|p459|||||lower Gawler Range Volcanics|||Includes minor, discontinuous epiclastic sedimentary packages 0.2-1.5 m thick separating lavas.|
7460|Gnalta Group|12066|5|Briefly described|p13|Cambrian|Cambrian|Includes the Pincally Formaiton, Wydjah Formation and Wyarra Shale.||||||
7460|Gnalta Group|22671|5|Briefly described|p832-33,Fig2p837|Middle Cambrian|Early Cambrian|Comprises: Mount Wright Volcanics, Cymbric Vale  and Coonigan Formations. Consists of volcanics and shallow marine sediments including limestones. Geological Province: Kanmantoo Fold Belt. Geol. Prov: Kanmantoo Fold Belt.||||||16-MAY-13
7460|Gnalta Group|22857|5|Briefly described|p75, p90 Fig. 14.7B|Middle Cambrian||See also p404 App. 1 Tb. A1.4.||||||
7460|Gnalta Group|22858|6|Mentioned|p75,83|||||||||
7460|Gnalta Group|23833|5|Briefly described|p256 Table 1|Cambrian|Cambrian|||||||
7460|Gnalta Group|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
7460|Gnalta Group|30683|6|Mentioned|Table 1|||||||||
7460|Gnalta Group|30908|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower - Middle Cambrian||||||
7460|Gnalta Group|31507|6|Mentioned|p181|||||||||
7460|Gnalta Group|31705|6|Mentioned|p27|||||||||
7460|Gnalta Group|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7460|Gnalta Group|32672|5|Briefly described|p671|||||||||
7460|Gnalta Group|32677|4|Described|p7||Early Cambrian|||||||
7460|Gnalta Group|32948|6|Mentioned|p110|||||||||
7460|Gnalta Group|33000|6|Mentioned|p2|||||||||
7460|Gnalta Group|33004|6|Mentioned|p140|||||||||
7460|Gnalta Group|34469|6|Mentioned|p109|||Table. Lower & Middle Cambrian||||||
7460|Gnalta Group|35235|6|Mentioned|p209|||||||||
7460|Gnalta Group|35320|6|Mentioned|p463|||||||||
7460|Gnalta Group|36534|6|Mentioned|p227|||||||||
7460|Gnalta Group|39214|5|Briefly described|p9|||||||||
7460|Gnalta Group|40595|6|Mentioned|Fig.7|||||||||
7460|Gnalta Group|40642|6|Mentioned|p171|||||||||
7460|Gnalta Group|41457|6|Mentioned|p1|||||||||
7460|Gnalta Group|41810|6|Mentioned|p111|||||||||
7460|Gnalta Group|42206|5|Briefly described|p257|||See also Fig.1||||||
7460|Gnalta Group|42982|5|Briefly described|Table 1,p333|||||||||
7460|Gnalta Group|43192|4|Described|p63,Table 1 p61.|Middle Cambrian|Early Cambrian|Time equivalent to Teltawongee Beds?||||||
7460|Gnalta Group|43213|5|Briefly described|p63|||Folded into tight upright folds during Delamerian Orogeny (late Middle Cambrian).||||Correlated with Teltawongee beds.|Mafic to silicic volcanics, sandstone and carbonates.|
7460|Gnalta Group|43263|6|Mentioned|Map Legend||Early Cambrian|||||||
7460|Gnalta Group|43502|14|Not recorded|Map Legend|Middle Cambrian|Early Cambrian|(Provisional Edition) Inc. Coonigan Formation,Cymbric Vale Formation,Mount Wright Volcs(L-L.M.Camb)||||||
7460|Gnalta Group|43704|4|Described|p67|Middle Cambrian|Early Cambrian|||||||
7460|Gnalta Group|44093|5|Briefly described|p143 App. 1|Early Cambrian|Early Cambrian|Calc-alkaline volcanics, limestone and clastic sediments. Geological Province: Kanmantoo Fold Belt.||||||
7460|Gnalta Group|47026|6|Mentioned|Fig.5|||||||||
7460|Gnalta Group|50618|5|Briefly described|p248 Fig. 1|Middle Cambrian|Early Cambrian|Geological Province: Wonominta Block.||||||
7460|Gnalta Group|60567|5|Briefly described|p39|||||||||
7460|Gnalta Group|60648|5|Briefly described|p43 Fig. 3|Early Paleozoic|Early Paleozoic|Geological Province: Darling Basin.||||||07-NOV-08
7460|Gnalta Group|60990|5|Briefly described|p81, p86|Middle Cambrian|Early Cambrian||||Mount Wright Volcanics, Cymbric Vale Formation and Coonigan Formation.|Considered to be coeval with the Teltawongee beds by Mills(1992)||
7460|Gnalta Group|61311|5|Briefly described|p43 Table D1|Early Paleozoic|Precambrian|Marine carbonates, volcanics and clastics. Geological Province: Darling Basin.||||||07-NOV-08
7460|Gnalta Group|62787|4|Described|p76 Fig. 1, p80|Middle Cambrian|Early Cambrian|Includes Wyarra Shale, Wydjah, Coonigan and Pincally Formations, Mount Wright Volcanics. Unconf. Overlain by Nootumbulla Sandstone. Geological province: Koonenberry Belt.||||||16-MAY-13
7460|Gnalta Group|62795|6|Mentioned|p347, p348 Fig.1|Middle Cambrian|Middle Cambrian|Unconformably underlies Mutawintji Group.||||||
7460|Gnalta Group|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Basic, intermediate and acid volcanics, shale, carbonate.||||||
7460|Gnalta Group|63789|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Includes Coonigan Formation, Cymbric Vale Formation and Mount Wright Volcanics.||||||08-DEC-08
7460|Gnalta Group|63793|5|Briefly described|p18,20,22.|Middle Cambrian|Early Cambrian|Formerly part of Wonominta beds (Warris 1967). Contains archaeocyathans. Shallow-water, near-shore facies coeval with Teltawongee beds, slope deposits to the east.||Unit in Wonominta beds.|Includes Mount Wright Volcanics, Cymbric Vale Formation and Coonigan Formation.|Is unconformably overlain by Mootwingee Group.||19-JAN-15
7460|Gnalta Group|64168|5|Briefly described|p30, p31|Early Cambrian|Early Cambrian|Age: 525Ma. Geological Province: Koonenberry Belt. Shows calc-alkaline volcanism.||||||01-JUL-08
7460|Gnalta Group|64671|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Includes Coonigan and Cymbric Vale Formations. Unconformably overlain by Mootwingee Group; fault bounded against Ponto beds and Mount Arrowsmith Volcanics.||||||
7460|Gnalta Group|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Comprises Mount wright Volcanics, Cymbric Vale and Coonigan Formations.||||||
7460|Gnalta Group|64680|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Includes Coonigan and Cymbric Vale Formations, and Mount Wright Volcanics. Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale, carbonates.||||||
7460|Gnalta Group|64684|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale carbonates.||||||16-MAY-13
7460|Gnalta Group|64686|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale, carbonate.||||||08-DEC-08
7460|Gnalta Group|65381|6|Mentioned|p691, Fig 2|Middle Cambrian|Early Cambrian|||||||
7460|Gnalta Group|65892|6|Mentioned|p43. |||Western New South Wales. Contains 13 species of archaeocyatha in common with Cymbric Vale Formation in South Australia.||||||
7460|Gnalta Group|66623|1|Redefined|pp56-73, p v, p44. |Late Cambrian|Early Cambrian|Formerly the lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934); redefined as Gnalta Group by Warris (1967); again redefined (this study) to include clastic and volcaniclastic rocks on southwestern flanks of Mount Arrowsmith Inlier because of age, felsic volcaniclastic content and geographic position. 500m to c.3800m thick. Low-grade metamorphosed. Coeval with Ponto Group.|||Includes Mount Wright Volcanics; Cymbric Vale, Coonigan, Pincally and Wydjah Formations; and Wyarra Shale.|Is unconformably or disconformably overlain by Nuchea Conglomerate. Fault-bound against Pimbilla Tank Group.|Calc-alkaline volcanic rocks (andesite, dacite), tuff, chert, mudstone, siltstone, limestone and dolostone with oncolites, sandstone; minor conglomerate.|
7460|Gnalta Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Pincally and Wydjah Formations and Wyarra Shale.||Undifferentiated fossiliferous shale, carbonate and siltstone.|
7460|Gnalta Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Mount Wright Volcanics, Cymbric Vale and Coonigan Formations.||Undifferentiated fossiliferous shale, carbonate and siltstone.|
7460|Gnalta Group|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Narrow zone of low magnetic intensity with rare moderately-magnetic lenticular trends.|||||Shale, carbonate and siltstone.|
7460|Gnalta Group|66929|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|||||Faulted against Ponto Group and Mount Arrowsmith Volcanics. Is unconformably overlain by Mootwingee Group.|Basic, intermediate, felsic volcanics; shale; carbonate.|
7460|Gnalta Group|67105|5|Briefly described|p650, 652-655, 659, 661|Cambrian|Cambrian|Wonnaminta Zone (arc and forearc), Koonenberry Belt. Delamerian Orogeny Cycle deposits. Contains Templetonian stage trilobites (~508 Ma; Percival, 2010).|||Mount Wright Volcanics, Cymbric Vale Formation.||Includes calc-alkaline volcanics, and volcaniclastic rocks.|
7460|Gnalta Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes basal Mount Wright Volcanics, Pincally and Wydjah Formations, and Wyarra Shale.||Fossiliferous shale, carbonate and siltstone; regionally metamorphosed to prehnite-pumpellyite facies; sandstone and conglomerate; andesitic lavas|20-SEP-13
7460|Gnalta Group|67322|5|Briefly described|p3 Fig.1, p5, p8-9; Fig.5|Series 3|Series 2|Koonenberry Belt, Delamerian Orogen. Of Warris (1967); redefined by Percival, in Greenfield et al. (2010). Age from p20 Fig.5 (Strat. column). Occurs in the Mount Wright-Mutawintji area.|||Mount Wright Volcanics, Coonigan Formation, Wydjah Formation, Pincally Formation, Cymbric Vale Formation, Wyarra Shale||Mostly shallow-water lithologies.|22-FEB-18
7460|Gnalta Group|69445|5|Briefly described|p30:17|Early Cambrian|Early Cambrian|Gnalta Shelf, western NSW.|||Mount Wright Volcanics, Cymbric Vale Formation.|Correlated with Kalkarindji Suite.||12-JUL-16
7460|Gnalta Group|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Interpreted equivalent to sedimentary and volcanic rocks in the Wirryilka (geophysical basement) Zone. Thought to have accumulated in close proximity to the Mount Wright Volcanic Arc, which was active along the E margin of Gondwana at the time.|||Includes Mount Wright Volcanics, Cymbric Vale and Coonigan Formations.|||
7460|Gnalta Group|70210|5|Briefly described|p1|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district.|||Cymbric Vale Formation.|||
7460|Gnalta Group|70296|6|Mentioned|p2|||Koonenberry District.|||Includes the Cymbric Vale Formation.|||22-JAN-21
7460|Gnalta Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Mount Wright Volcanics, Cymbric Vale Formation.||Fossiliferous shale, carbonate and siltstone; undifferentiated andesitic lavas, felsic ignimbrites, reworked tuffs, and associated intrusions; regionally metamorphosed to prehnite-pumpellyite facies.|20-JAN-22
7460|Gnalta Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Coonigan Formation, Cymbric Vale Formation, Mount Wright Volcanics.||Fossiliferous shale, carbonate and siltstone; andesitic lavas, felsic ignimbrites, reworked tuffs, and associated intrusions; regionally metamorphosed to prehnite-pumpellyite facies.|
7460|Gnalta Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
7460|Gnalta Group|70838|5|Briefly described|p267 Fig.1, p268-269, p271|Cambrian|Cambrian|NW Koonenberry Belt. Possible tectonic settings discussed. Maximum depositional age is poorly constrained. Deformed during the Delamerian Orogeny (c.500 Ma).|||Mount Wright Volcanics; Cymbric Vale, Coonigan Formations.|Is overlain unconformably by Mutawintji Group.|Volcanic and sedimentary sequences.|
7460|Gnalta Group|71262|5|Briefly described|p3, p5 Fig 2, p10|Middle Cambrian|Early Cambrian||||Includes Mount Wright Volcanics||Calc-alkaline volcanic and associated sedimentary rocks.|
7460|Gnalta Group|71593|5|Briefly described|p188|Early Cambrian|Early Cambrian|Koonenberry Province.|c. 511-506 Ma|||||
7460|Gnalta Group|71965|5|Briefly described|p894|Cambrian|Cambrian|Geological province: Koonenberry Belt, Delamerian Orogen. Volcanism c. 510 Ma associated with development of the Mount Wright continental magmatic arc (Greenfield et al., 2010; Greenfield et al., 2011).||||||
7460|Gnalta Group|71966|6|Mentioned|p990,999|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
7460|Gnalta Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Undifferentiated fossiliferous shale, carbonate and siltstone.|09-DEC-21
7460|Gnalta Group|73177|5|Briefly described|p1098, 1100, 1114, 1115 Fig.17|Middle Cambrian|Early Cambrian||||Mount Wright Volcanics, Cymbric Vale Formation.|||30-AUG-22
7460|Gnalta Group|73430|6|Mentioned|p494|Middle Cambrian|Early Cambrian|Koonenberry Belt. Deformed by the Delamerian Orogeny.|||||Sedimentary unit.|
7596|Gordon Springs Granodiorite|35397|4|Described|p96|||Petrography described on p97.||||||23-JAN-19
7596|Gordon Springs Granodiorite|36244|6|Mentioned|p2|||Refers to Teale 1979.||||||
7596|Gordon Springs Granodiorite|44133|5|Briefly described|p55-56 Table 7.3|||Geological Province: Mount Painter Inlier. Fine grained granodiorite. I-Type.||||||
7596|Gordon Springs Granodiorite|70384|5|Briefly described|Map legend.|Ordovician|Ordovician|Similar dykes intrude the British Empire Granite.|462 +/- 4 Ma (U-Pb zircon).|||Probable correlative of Mudnawatana Tonalite.|White to grey, medium-grained, equigranular granodiorite to tonalite.|
7596|Gordon Springs Granodiorite|72459|6|Mentioned|p67|Delamerian|Mesoproterozoic|Originally defined by Teale (1979). Together with the Paralana granodiorite, the Mudnawatana Tonalite and the British Empire Granite forms so called group 3 of this study. Chemically very similar to the Mudnawatana Tonalite and the Paralana granodiorite and on that basis group these 3 units together into the Paralana granodiorite.||||||
7596|Gordon Springs Granodiorite|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
7646|Goyder Formation|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Silty sandstone, siltstone, limestone, dolomite.  Geological Province: Amadeus Basin.||||||04-NOV-04
7646|Goyder Formation|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Sandstone, limestone, siltstone; fossiliferous.||||||
7646|Goyder Formation|12891|5|Briefly described|p732|Late Cambrian|Late Cambrian|Geological province: Amadeus Basin. Lithology possibly analogous with Point Wakefield beds in Wiso Basin.||||||07-FEB-11
7646|Goyder Formation|22560|6|Mentioned| p5|||||||||
7646|Goyder Formation|22561|4|Described|p21|Late Cambrian|Neoproterozoic|Includes sequence boundary between the lower and upper Goyder Formation, which marks a significant change in depositional patterns within the basin.||||||06-FEB-08
7646|Goyder Formation|22565|5|Briefly described|p71 & Table 1||Cambrian|Thickness at Areyonga Creek measured from surface expression - 330m thick.  Approx. thickness measured from seismic data - 350m.||||||
7646|Goyder Formation|22566|5|Briefly described|p84|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22646|5|Briefly described|p 104|Cambrian|Cambrian|informally devided into upper and lower Goyder Formation p 104.||||||13-SEP-18
7646|Goyder Formation|22650|5|Briefly described|p 160|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22651|4|Described|p 188|Late Cambrian|Middle Cambrian|Of Pertaoorrta Group. Informally devided into upper and lower Goyder Formation p171. The upper Goyder Formation contains late Cambrian trilobites, this suggests a significant time break between it and the lower Goyder which contains Mindyallan fauna.||||||21-SEP-06
7646|Goyder Formation|22655|6|Mentioned|p 253|||informally devided into upper and lower Goyder Formation p255.||||||
7646|Goyder Formation|22656|6|Mentioned|Fig 5 on p 283|||||||||
7646|Goyder Formation|22657|5|Briefly described|p 285|||Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22758|6|Mentioned|Fig 2 on p305|||||||||
7646|Goyder Formation|22760|6|Mentioned|p337|||||||||
7646|Goyder Formation|22762|6|Mentioned|p364|Cambrian|Cambrian|||||||
7646|Goyder Formation|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22804|6|Mentioned|p429|Early Ordovician|Cambrian|Of Pertaoorrta Group.  Informally devided into upper and lower Goyder Formation.||||||21-SEP-06
7646|Goyder Formation|22805|5|Briefly described|p470||Late Cambrian|||||||
7646|Goyder Formation|22807|6|Mentioned|p500|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22824|5|Briefly described|p533|||Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22826|4|Described|p572|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Of Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|29591|5|Briefly described|Table 23|||||||||
7646|Goyder Formation|29721|6|Mentioned|Table 44|||||||||
7646|Goyder Formation|29972|6|Mentioned|Table 1|||Upper Cambrian||||||
7646|Goyder Formation|30258|6|Mentioned|Fig.2|||Cambrian age.  Part of Pertaoorta Group.||||||21-SEP-06
7646|Goyder Formation|30544|6|Mentioned|p48|||||||||
7646|Goyder Formation|31572|6|Mentioned|p21|||U.Cambrian. Correlation chart 1.||||||
7646|Goyder Formation|32469|6|Mentioned|p531|||||||||
7646|Goyder Formation|33307|6|Mentioned|Fig.6|||||||||
7646|Goyder Formation|33625|6|Mentioned|p189|||||||||
7646|Goyder Formation|33738|6|Mentioned|p47|||||||||
7646|Goyder Formation|33761|6|Mentioned|p146|||Cambrian||||||
7646|Goyder Formation|34111|5|Briefly described|Table 2|||Cambrian. See also pp6,15,20.||||||21-SEP-06
7646|Goyder Formation|34186|6|Mentioned|p1988|||Upper Cambrian. See also Figs.3,4,8.||||||
7646|Goyder Formation|34442|5|Briefly described|Table 1|||Camb. p8||||||21-SEP-06
7646|Goyder Formation|34579|4|Described|Table 2|||Cambrian. See also pp16,17.||||||21-SEP-06
7646|Goyder Formation|35102|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|35805|6|Mentioned|Fig.3|||||||||
7646|Goyder Formation|36198|6|Mentioned|p295|||See also Fig.III.2||||||
7646|Goyder Formation|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7646|Goyder Formation|38885|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7646|Goyder Formation|39210|5|Briefly described|p38|||||||||
7646|Goyder Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
7646|Goyder Formation|39583|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7646|Goyder Formation|39757|6|Mentioned|p1607|||||||||
7646|Goyder Formation|39931|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7646|Goyder Formation|40136|6|Mentioned|p36|||||||||
7646|Goyder Formation|40740|3|Fully described|p44|||Mention p5.||||||21-SEP-06
7646|Goyder Formation|40810|4|Described|p7|||||||||
7646|Goyder Formation|40852|6|Mentioned|p34|||||||||
7646|Goyder Formation|40906|6|Mentioned|Fig.11|||||||||
7646|Goyder Formation|40998|6|Mentioned|Fig.1|||||||||
7646|Goyder Formation|41018|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41115|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41190|6|Mentioned|Fig.4|||||||||
7646|Goyder Formation|41203|5|Briefly described|p30|||||||||
7646|Goyder Formation|41224|6|Mentioned|p430|||||||||
7646|Goyder Formation|41621|5|Briefly described|Map legend|Cambrian||||||||
7646|Goyder Formation|41717|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
7646|Goyder Formation|41819|6|Mentioned|Map legend|Cambrian||||||||
7646|Goyder Formation|41820|3|Fully described|p7|||||||||
7646|Goyder Formation|42037|5|Briefly described|Table 3 P79|||||||||
7646|Goyder Formation|42060|6|Mentioned|Fig.5 P140|||||||||
7646|Goyder Formation|42082|6|Mentioned|Fig.3 P323|||||||||
7646|Goyder Formation|42354|4|Described|p6|Late Cambrian||||||||
7646|Goyder Formation|42504|5|Briefly described|p112|||||||||
7646|Goyder Formation|42886|5|Briefly described|Fig.1 P218|||||||||
7646|Goyder Formation|42940|5|Briefly described|p1 Plate8|||||||||
7646|Goyder Formation|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|43503|6|Mentioned|11-50|Payntonian|Mindyallan|||||||
7646|Goyder Formation|43646|6|Mentioned|Fig.3,p554||Late Cambrian|||||||
7646|Goyder Formation|43648|6|Mentioned|Fig.27,p509|||||||||
7646|Goyder Formation|43649|6|Mentioned|p457|||||||||
7646|Goyder Formation|43781|6|Mentioned|p4|||||||||
7646|Goyder Formation|43807|5|Briefly described|p352|||||||||
7646|Goyder Formation|44395|14|Not recorded|p.8||Cambrian|Correlates with Cleland Sandstone.||||||
7646|Goyder Formation|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
7646|Goyder Formation|44433|14|Not recorded|map legend||Cambrian|||||||
7646|Goyder Formation|44457|14|Not recorded|p.6||Late Cambrian|Amadeus Basin. Upper Cambrian. (Mindyallan).||||||
7646|Goyder Formation|44484|14|Not recorded|p.10,14, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44497|4|Described|p.10, Table 1||Cambrian|SF/53-13.||||||
7646|Goyder Formation|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44505|14|Not recorded|p.7,11,12, Table 1||Cambrian|Of Pertaoorrta Group.||||||
7646|Goyder Formation|44506|14|Not recorded|map legend||Cambrian|||||||
7646|Goyder Formation|45041|4|Described|p58|||Refers Prichard and Quinlan (1962). U.Camb.||||||21-SEP-06
7646|Goyder Formation|45115|6|Mentioned|p7|||||||||
7646|Goyder Formation|45130|6|Mentioned|p14|||||||||
7646|Goyder Formation|45148|6|Mentioned|Fig.4|||Amadeus Basin||||||
7646|Goyder Formation|45155|6|Mentioned|Fig.8|||||||||
7646|Goyder Formation|46826|5|Briefly described|p345|||||||||
7646|Goyder Formation|46928|6|Mentioned|Table 1|||||||||
7646|Goyder Formation|48639|14|Not recorded|p.5||Cambrian|See also page, 1,4,6,17,Pl.1,Sh.2.||||||
7646|Goyder Formation|48838|2|Defined|p.16, Tb.1||Late Cambrian|U.Cam.||||||
7646|Goyder Formation|48862|14|Not recorded|p.17|||Now superseded by Goyder Member. (F52-15).||||||
7646|Goyder Formation|48863|2|Defined|p.23||Late Cambrian|Tb.1. opp.p.7,p.5,9,14,16,19,20,24,25,33,43,Pl.10,11,15,16. Upper Cambrian. (G52-4,G53-1).||||||
7646|Goyder Formation|48865|14|Not recorded|Fig.4|||(G52-4,F53-13).||||||
7646|Goyder Formation|48890|4|Described|p.42||Cambrian|See also Tables, Figs, Plates. pt. Pertaoorta Gp.||||||
7646|Goyder Formation|48963|6|Mentioned|p30|||Fig.3||||||
7646|Goyder Formation|50246|5|Briefly described|p20 Fig. 2|Cambrian|Cambrian|Sandstone, limestone.||||||07-FEB-11
7646|Goyder Formation|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Silty sandstone, siltstone, limestone, dolomite. Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Yellow-brown, partly micaceous, kaolinitic sandstone; minor stromatolitic limestone, oolitic dolostone and siltstone. Geological Province: Amadeus Basin.||||||13-SEP-18
7646|Goyder Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
7646|Goyder Formation|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, siltstone, calcareous.  Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Yellow-brown, partly micaceous, kaolinitic sandstone; minor stromatolitic limestone, oolitic dolostone and siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
7646|Goyder Formation|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin. ||||||
7646|Goyder Formation|62379|4|Described|p13|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin. Shale, siltstone, sandstone, limestone, dolostone.||||||
7646|Goyder Formation|62595|6|Mentioned|p28 Fig.4, p29 Fig.6.|Late Cambrian|Late Cambrian|Amadeus Basin. Relative probability plots of detrital zircon data are shown.|||||Sandstone, limestone.|
7646|Goyder Formation|62794|5|Briefly described|p289 Fig.2|Late Cambrian|Late Cambrian|Topmost unit of Pertaoorrta Group. Underlies Pacoota Sandstone of the Larapinta Group.||||||
7646|Goyder Formation|63562|4|Described|p338 fig 3, p340-341, p346-349|Late Cambrian|Late Cambrian|See also p352 fig 10, p355. Of Amadeus Basin. Zircons from lower part were mostly 1.2-0.9 Ga suggesting Musgrave Inlier as source. Also has a peak at 0.55 Ga with no apparent source other than the Lachlan Fold Belt, more than 1000 km to the E.||||Overlies Shannon Formation. Is overlain by Pacoota Sandstone.|Includes dolomite, calcarenite.|
7646|Goyder Formation|64068|6|Mentioned|p65, 67, 69, 70, 71, 225|||Amadeus Basin. Lower part correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone, southern Georgina Basin. Upper part correlated with Chatsworth Limestone. ||||||
7646|Goyder Formation|64334|6|Mentioned|p45|||Detrital zircon ages and provenances discussed.||||||
7646|Goyder Formation|64778|6|Mentioned|p13, 18, 21, 33|Cambrian|Cambrian|Amadeus Basin.||||||
7646|Goyder Formation|64809|4|Described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Late Cambrian|Late Cambrian|See also p13 Fig.13, p15 Fig.15. Widespread transgressive deposits.||Unit in Pertaoorrta Group.|||Silty sandstone, limestone|
7646|Goyder Formation|65233|3|Fully described|p3 Fig. 2, p9|Late Cambrian|Late Cambrian|Of Pertaoorrta Gp. Gradationally related to clastic succession below. Max.thick: 600m. Amadeus Basin. Basal carbonate-clastic unit with overlying sandstone (Lower Goyder Fm, 300m); upper sst/siltstone (Upper Goyder Fm, 300m) with unconformity between.||||||13-SEP-18
7646|Goyder Formation|65342|5|Briefly described|p4.|||Amadeus Basin.Max. thickness at least 145 m.||||Overlies Shannon Formation. Is overlain by Pacoota Sandstone.|Yellow-brown, partly micaceous kaolinitic sandstone.|
7646|Goyder Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Topmost unit in Pertaoorrta Group.||Overlies Shannon Formation. Is overlain by Pacoota Sandstone (Larapinta Group).||
7646|Goyder Formation|67126|5|Briefly described|p1, p3-9, p11-13, p20, p26, p33, p36-37|Middle Cambrian|Middle Cambrian|Amadeus Basin. Poor gas shale candidate: very low organic carbon content. Rock Eval analysis, Rock Eval Temperature Programme: Pyrolysis, Thermovaporisation, Pyrolysis Gas Chromatography results presented in detail.||||||
7646|Goyder Formation|67128|6|Mentioned|p30|||Northeastern Amadeus Basin.||||||
7646|Goyder Formation|67326|5|Briefly described|p2|Late Cambrian|Late Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Cleland, Petermann and Deception Sandstones, Hugh River Shale, Jay Creek Limestone and Shannon Formation. Is overlain by Pacoota Sandstone.||
7646|Goyder Formation|67565|4|Described|pp40-41, p47.|Late Cambrian|Late Cambrian|Peritidal sand and minor carbonate deposited during a marine transgression. Poorly exposed. Thickness decreases from 550 m near Stokes Pass, to 90 m in the west.||||Conformably overlies Petermann and Cleland Sandstones.|Dominantly a yellow-brown or buff, partly micaceous, fine to medium kaolinitic sandstone; thinly-bedded, cross-bedded and moderately well-sorted, with rippled surfaces; local thin stromatolitic limestone bed.|
7646|Goyder Formation|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
7646|Goyder Formation|68316|5|Briefly described|p778 Fig.1, p783 Fig.4, p784|Series 2|Series 2|Amadeus Basin.|c. 520 Ma (Zhao et al. 1992)|Of the Pertaoorta Group.||Underlain by the Arumbera Formation.||
7646|Goyder Formation|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Late Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
7646|Goyder Formation|69437|5|Briefly described|p22:10|Furongian|Series 3|Amadeus Basin.||||Overlies Cleland, Petermann Sandstones, Deception Formation. Is overlain by Pacoota Sandstone.||12-JUL-16
7646|Goyder Formation|69438|3|Fully described|p23:2-3,6-8,24-25,30-34,43,53,55-56,61|Late Cambrian|Late Cambrian|Defined by Pritchard and Quinlan (1962); redefined as a Member of the then Pertaoorrta Formation by Wells et al. (1965). Subsequently restored to Formation rank within the Pertaoorrta Group by Ranford et al. (1965). Up to 600m thick in Ooraminna Sub-basin, Amadeus Basin. A significant unconformity separates the lower and upper parts of the Formation. Grades laterally into Cleland Sandstone. Is overlain unconformably by Pacoota Sandstone. Various fossils listed. Sediment source was mainly from the Musgrave Province with lesser Arunta Region input. Hosts the Owen Springs uneconomic Cu-Pb-Zn occurrences. Drilled for oil, gas and shale oil in Johnstone West-1 and Surprise-1 wells, successfully. Has low shale gas potential.||Uppermost Pertaoorrta Group.||Conformably overlies Shannon Formation, Hugh River Shale, Jay Creek Limestone (also partial lateral equivalent), Cleland Sandstone and (also interfingers with) Petermann Sandstone.|A 300m interval of medium to thick interbeds of dolomitic ooid grainstone and cross-bedded sandstone, with  minor siltstone, calcareous mudstone, cryptalgalaminite, and intraclastic conglomerate, under 300m of fine to coarse sandstone and siltstone.|12-JUL-16
7646|Goyder Formation|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
7646|Goyder Formation|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Amadeus Basin.||||||12-JUL-16
7646|Goyder Formation|69573|6|Mentioned|p661|||Amadeus Basin.||||||
7646|Goyder Formation|70744|6|Mentioned|p944-945|Early Cambrian|Early Cambrian|Amadeus Basin. Detrital zircon age distribution graph.||||||
7646|Goyder Formation|70749|6|Mentioned|p54|||Amadeus Basin.||Pertaoorrta Group.||||
7646|Goyder Formation|70752|5|Briefly described|p126 Fig.1|Cambrian|Cambrian|||Pertaoorrta Group.|||Silty sandstone with minor siltstone; fossiliferous and stromatolitic dolostone with minor limestone.|
7646|Goyder Formation|71114|5|Briefly described|p171, p170 fig 1b, p172-180|Stage 10||Across entire Amadeus Basin. Unit includes a hiatus between carbonate-rich lower succession and sandstone-rich  upper succession with poor age control. Deposited between ~511 and 490 Ma. Marks rising sea level with flooding of nearshore sandstones and siltstones and subsequent deposition of shallow marine carbonates. 188m thick in Dingo 1 well. Age of the unit ranges from Guzhangian to Stage 10 based on trilobite biostratigraphy.||||Overlies Shannon Formation, Jay Creek Limestone and Petermann Sandstone.|Sandstone, siltstone, carbonates; alternating siltstones and dolostones indicate basin-wide transgression.|14-FEB-18
7646|Goyder Formation|71279|5|Briefly described|p355 Fig.2, p363, p365-366, p382 Tb.1|Late Cambrian|Late Cambrian|Amadeus Basin. Modelled magnetic properties.||Pertaoorrta Group.|||Limestone. See also p353.|27-OCT-17
7646|Goyder Formation|71800|5|Briefly described|p26-p27|Late Cambrian|Late Cambrian|Amadeus Basin.||||Overlies the Shannon Formation. Unconformably overlain by the Pacoota Sandstone.|Calcarenite.|
7646|Goyder Formation|71898|4|Described|iii, p1, p3, p17-p19|Late Cambrian|Late Cambrian|Amadeus Basin. This unit was defined by Pritchard and Quinlan (1962) before being redefined as a member of the then Pertaoorrta Formation by Wells et al (1965). Ranford et al (1965) subsequently restored the unit to formation status and included it in the Pertaoorrta Group. SHRIMP age is interpreted to be a maximum depositional age and is only slightly older than a terminal Cambrian (Payntonian; 491-488Ma) age derived from palynological evidence. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed. This unit has a maximum thickness of 600m in the northeast Amadeus Basin. This unit is subdivided into a lower and upper unit both deposited in shallow subtidal to intertidal environments. Dated sample is from within the unit, well below the contact with overlying Pacoota Sst and many hundreds of  m above Petermann Sst.|505 +/- 6 Ma (SHRIMP U-Pb)|Pertaoorrta Group|Includes the Goyder Formation, lower and Goyder Formation, upper.|Conformably (transitional) overlies the Petermann Sandstone. Unconformably overlain by the Pacoota Sandstone.|Fine- to medium-grained sandstone.|19-NOV-18
7646|Goyder Formation|72358|5|Briefly described|p116-121,123-125|Furongian|Furongian|Of Amadeus Basin. Laterally extensive across the Amadeus Basin, marking rising sea level and regional flooding. Inconsistencies regarding historical logging and stratigraphic position in legacy well interpretations e.g. lower contact at ~1170m in Alice 1, vs 761m in Wallaby 1, 7km E of Alice 1, but with similar GR log patterns. Equivalent to Georlina Limestone in the Georgina Basin.||||Overlain by Pacoota Sandstone. Overlies the Shannon Formation.|Shallow marine carbonates.|10-JAN-20
7646|Goyder Formation|72369|5|Briefly described|p26|||Of Amadeus Basin.||||Overlain unconformably by Pacoota Sandstone.||
7646|Goyder Formation|72489|5|Briefly described|p3-6, p7 Fig.6, p8, p9, p11,p12|Furongian|Guzhangian|Located in the Amadeus Basin. Age based on trilobite stratigraphy. Formed during periods of intense continental chemical weathering.||||Overlain by Julie Formation. [Said to be overlain by Wonoka Fm but this unit in Adelaide Rift Complex]|Carbonate.|
7646|Goyder Formation|72516|6|Mentioned|p93|Cambrian|Cambrian|Amadeus Basin.||||Lower part equivalent to the Arrinthrunga Formation.||08-JUN-21
7646|Goyder Formation|73085|6|Mentioned|p1, p4|late Cambrian|late Cambrian|||Pertaoorrta Group [and equivalents?]||Overlain by Pacoota Sandstone (Larapinta Group).||
7672|Grampians Group|22531|4|Described|p19|Silurian|Ordovician|||||||
7672|Grampians Group|22532|5|Briefly described|map legend|Silurian|Ordovician|||||||
7672|Grampians Group|22628|5|Briefly described|p115, fig3p111|||||||||
7672|Grampians Group|22708|6|Mentioned|p212|||||||||
7672|Grampians Group|22768|5|Briefly described|p141,146,184|Early Devonian|Late Silurian|||||||
7672|Grampians Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
7672|Grampians Group|22857|5|Briefly described|p141, p166, p183|Early Devonian|Late Silurian|Equivalents mentioned on p350 Fig. 24.5. Geological Province: Kanmantoo Fold Belt, Grampians Basin. ||||||
7672|Grampians Group|22887|5|Briefly described|Fig.5 p12|Middle Devonian|Silurian|||||||
7672|Grampians Group|22893|6|Mentioned|fig4 p9|||Describing an equivalent to this unit.||||||
7672|Grampians Group|23061|6|Mentioned|293 fig 1|||Underlying unit Saint Arnaud Beds||||||
7672|Grampians Group|23110|5|Briefly described|p502|||||||||
7672|Grampians Group|23229|4|Described|p24-5|||||||||
7672|Grampians Group|23231|6|Mentioned|Fig5-4p51|||||||||
7672|Grampians Group|23232|5|Briefly described|p62|||||||||
7672|Grampians Group|23234|5|Briefly described|p85|Mesozoic|Late Devonian|||||||
7672|Grampians Group|23235|5|Briefly described|p68|Devonian|Silurian|||||||
7672|Grampians Group|23236|6|Mentioned|Fig10-1.2p99|||||||||
7672|Grampians Group|23247|4|Described|Fig12-1.1p182, 183-4|Early Devonian|Late Silurian|||||||
7672|Grampians Group|23306|6|Mentioned|Map legend|||||||||
7672|Grampians Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
7672|Grampians Group|23309|4|Described|p76-83, 203-208, 349|||||||||
7672|Grampians Group|23402|3|Fully described|p25, p7 Tb. 1|Silurian|Silurian|Previously mapped on WILLAURA as 'Willaura Sandstones' (Spencer-Jones, 1965), later modified to 'Willaura Sandstone' (Buckland, 1987).   Age: 412.6+/-3.5Ma (U-Pb zircon).   Unconformably overlies Wickliffe Rhyolite and Glenthompson Sandstone.||||||
7672|Grampians Group|23417|6|Mentioned|p6 Fig.4||Silurian|||||||
7672|Grampians Group|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
7672|Grampians Group|23857|5|Briefly described|p907|Silurian|Silurian|||||||
7672|Grampians Group|23918|6|Mentioned|p1327|||Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|23991|5|Briefly described|p188 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|24002|5|Briefly described|p227 fig. 1|Ordovician|Ordovician|Age: 425Ma.||||||21-OCT-08
7672|Grampians Group|24100|6|Mentioned|p98 Fig. 4|||Geological Province: Stawell Zone.||||||19-APR-05
7672|Grampians Group|24311|5|Briefly described|p1061, p1059 Fig. 2|Silurian|Silurian|||||||
7672|Grampians Group|24323|5|Briefly described|p138|Silurian|Silurian|||||||
7672|Grampians Group|24383|6|Mentioned|p56 Tb.6|||||||||
7672|Grampians Group|24581|5|Briefly described|p811|Ludlovian|Late Ordovician|Geological Province: Kanmantoo Fold Belt.||||||
7672|Grampians Group|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|29889|6|Mentioned|p141|||||||||
7672|Grampians Group|30329|6|Mentioned|p30|||On table P30||||||
7672|Grampians Group|30522|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Lower Carboniferous to Upper Devonian||||||
7672|Grampians Group|30579|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|30928|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|30934|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|31161|5|Briefly described|PA11|||||||||
7672|Grampians Group|32001|6|Mentioned|p77|||||||||
7672|Grampians Group|32865|6|Mentioned|p486|||||||||
7672|Grampians Group|33232|3|Fully described|p71|||||||||
7672|Grampians Group|33236|6|Mentioned|p24|||U.Dev. _ L.Carb.||||||
7672|Grampians Group|33238|5|Briefly described|p640|||||||||
7672|Grampians Group|33394|6|Mentioned|p78|||||||||
7672|Grampians Group|33602|6|Mentioned|Table 1|||||||||
7672|Grampians Group|33608|6|Mentioned|p45|||||||||
7672|Grampians Group|33940|6|Mentioned|p416|||||||||
7672|Grampians Group|34990|6|Mentioned|p435|||||||||
7672|Grampians Group|35013|6|Mentioned|p390|||||||||
7672|Grampians Group|35099|6|Mentioned|p325|||||||||
7672|Grampians Group|35112|6|Mentioned|Table.1|||||||||
7672|Grampians Group|35278|6|Mentioned|p349|||||||||
7672|Grampians Group|35281|6|Mentioned|p19|||||||||
7672|Grampians Group|36534|6|Mentioned|p221|||||||||
7672|Grampians Group|36732|6|Mentioned|p300|||||||||
7672|Grampians Group|37501|5|Briefly described|p407|||||||||
7672|Grampians Group|38070|5|Briefly described|p97|||||||||
7672|Grampians Group|38367|6|Mentioned|p158|||See also Fig.1||||||
7672|Grampians Group|38436|6|Mentioned|p420|||||||||
7672|Grampians Group|39291|6|Mentioned|p214|||||||||
7672|Grampians Group|39331|6|Mentioned|Fig.0-3|||See Fig.0-3||||||
7672|Grampians Group|39446|6|Mentioned|p11|||See also P65||||||
7672|Grampians Group|39967|4|Described|p33|||||||||
7672|Grampians Group|40172|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|40761|6|Mentioned|p215|||See also p225.||||||07-SEP-18
7672|Grampians Group|40887|6|Mentioned|p25|||||||||
7672|Grampians Group|40947|6|Mentioned|p4|||||||||
7672|Grampians Group|41002|5|Briefly described|p183|||||||||
7672|Grampians Group|41563|6|Mentioned|p516|||||||||
7672|Grampians Group|41571|4|Described|p38|||||||||
7672|Grampians Group|41572|6|Mentioned|p3|||||||||
7672|Grampians Group|41585|4|Described|p141|||||||||
7672|Grampians Group|41637|6|Mentioned|p210|||||||||
7672|Grampians Group|41641|6|Mentioned|p191|||||||||
7672|Grampians Group|42119|5|Briefly described|p524|||||||||
7672|Grampians Group|42745|5|Briefly described|p3, p6|||Also P9.||||||
7672|Grampians Group|42827|6|Mentioned|p141|||see also Table 4.3||||||
7672|Grampians Group|42966|5|Briefly described|Fig. 25 p47|||||||||
7672|Grampians Group|42971|5|Briefly described|p142|||||||||
7672|Grampians Group|43027|5|Briefly described|p601|||||||||
7672|Grampians Group|43193|5|Briefly described|p71,78.|||Minimum age: Late Silurian-earliest Devonian.||||||
7672|Grampians Group|43218|4|Described|Fig.3 p22, p25|Early Devonian|Late Silurian|||||||
7672|Grampians Group|43461|14|Not recorded|table p625|Early Carboniferous|Late Devonian|||||||
7672|Grampians Group|43547|14|Not recorded|Table p153,154|Famennian|Frasnian|||||||
7672|Grampians Group|43627|5|Briefly described|p2, p6|||Age: 410 Ma.||||||21-OCT-08
7672|Grampians Group|43753|5|Briefly described|p621-624|Early Carboniferous|Late Silurian|||||||
7672|Grampians Group|43846|4|Described|9, 11|Early Devonian|Late Silurian|Intrusives into group aged around 400Ma.||||||21-OCT-08
7672|Grampians Group|44093|5|Briefly described|p47, p91|Early Devonian|Late Silurian|See also p102 Fig 10.3. Geological Province: Kanmantoo Fold Belt.||||||08-MAR-05
7672|Grampians Group|44186|5|Briefly described|Map Legend||Silurian|||||||
7672|Grampians Group|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficult and Red Man Bluff Sub-Groups.||||||13-JUN-06
7672|Grampians Group|44931|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone, minor conglomerate and mudstone. Undifferentiated for this interpretation.||||||14-JUN-06
7672|Grampians Group|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|48911|6|Mentioned|p7|||Lithology||||||
7672|Grampians Group|49038|6|Mentioned|p22|||||||||
7672|Grampians Group|49040|6|Mentioned|p6|||||||||
7672|Grampians Group|50154|2|Defined|p17, p18 Fig3.1, p110-113|Ludlow|Early Silurian|Max. thickness: 3700m. Overlies the Gringegalgona Granite and unconformably overlies the Nargoon Group. Unconformably overlain by the Rocklands Volcanic Group. Geological Province: Lachlan Fold Belt.||||||15-SEP-04
7672|Grampians Group|50155|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone||||||
7672|Grampians Group|50156|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50157|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50158|5|Briefly described|Map Legend|Silurian||Unconformably overlies Nargoon Group. Overlain by Barangaroo Ignimbrite. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||25-JUN-04
7672|Grampians Group|50159|5|Briefly described|Map Legend|Silurian||Overlies Nargoon Group. Overlain by Barangaroo Ignimbrite, Parilla Sand and Shepparton Formation. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50160|5|Briefly described|Map Legend|Silurian||||||||16-JUN-04
7672|Grampians Group|50161|5|Briefly described|Map Legend|Silurian||Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50162|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone.||||||21-OCT-08
7672|Grampians Group|50163|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone||||||
7672|Grampians Group|50371|5|Briefly described|Map Legend|Silurian|Silurian|Includes the Willaura Sandstone.||||||21-JUN-04
7672|Grampians Group|50546|6|Mentioned|p1232 Fig.1a|||||||||
7672|Grampians Group|60412|6|Mentioned|p237||||499 +/- 2 Ma (40Ar-39Ar biotite).||||Sandstones.|
7672|Grampians Group|60421|5|Briefly described|p408 Fig. 1, 416, 418 Fig. 5|Silurian|Silurian|||||||
7672|Grampians Group|60451|4|Described|p20, 24, 75, 142-143|Silurian|Silurian|Age: ~425-415Ma Maximum Thickness: ~3700m. Includes Red Man Bluff Subgroup, Silverband Formation.||||||
7672|Grampians Group|60454|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||
7672|Grampians Group|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz-rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, cross and trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60457|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||24-SEP-04
7672|Grampians Group|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, trough or trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60459|5|Briefly described|Map Legend|Silurian|Ordovician|Includes: Mount Difficult Sub-Group, Red Man Bluff Sub-Group, Silverband Formation.||||||
7672|Grampians Group|60491|6|Mentioned|p13 Fig.5|||||||||
7672|Grampians Group|60543|5|Briefly described|Map legend|Devonian|Silurian|Terrestrial to marine sandstone with lesser conglomerate and siltstone.||||||23-DEC-09
7672|Grampians Group|61180|5|Briefly described|p5|Early Devonian|Silurian|Overlies Saint Arnaud Beds.||||||
7672|Grampians Group|61181|5|Briefly described|p153 Fig. 47|Devonian|Devonian|Sandstone and shale. ||||||
7672|Grampians Group|61183|3|Fully described|p7, p23-24, p28-33|Early Silurian|Ordovician|Incl: Red Man Bluff Subgp(lower), Silverband Fm(middle) and Difficult Subgp(upper). Fluvial/shallow marine lower quartzo-feldspathic to micaceous sst; intervening micaceous mudst. and upper quartzose sst package. Overlain by Rocklands Volcs. Thick:~3700m.||||||
7672|Grampians Group|61186|6|Mentioned|p76|||Source of the Grampians Sandstone dimension stone in Victoria quarried in the Heatherlie quarry which lies within the Serra Sandstone Formation of the Grampians Group. ||||||
7672|Grampians Group|61187|5|Briefly described|p4, p5 Fig.3, p6, p9, p69. |Silurian||Glenelg Zone, Melbourne Terrane. Marginal marine to terrestrial deposition on the Delamerian Craton. Folded during Benambran Orogeny. Early Devonian A-type volcanics were deposited over this deformed and eroded Group.|||Includes Willaura Sandstone.|||
7672|Grampians Group|61410|5|Briefly described|p7 Fig.2, p8-9|Silurian|Ordovician|Overlies the Glenelg Zone. Crops out as a series of spectacular rugged strike ranges. Hosts only scattered small amounts of gold mineralisation.||||Intruded by the Mafeking Granodiorite|Includes conglomerate hosting minor auriferous quartz veins.|
7672|Grampians Group|61726|5|Briefly described|p924 Fig.3|Silurian|Silurian|||||||
7672|Grampians Group|61749|6|Mentioned|p11, p14|Silurian|Silurian|Includes Red Man Bluff and Mount Difficulty Subgroup seperated by Silverband Formation. Fluvial to shallow marine sequence.||||||21-JAN-10
7672|Grampians Group|61752|4|Described|p10|Silurian|Ordovician|Fluvial to marginal marine sequence. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
7672|Grampians Group|61841|5|Briefly described|p242, p244|Silurian|Silurian|Sediments on the Dundas Tablelands. Overlain by Rocklands Volcanic Group.||||||
7672|Grampians Group|62741|5|Briefly described|p678 Fig. 1, p682|Silurian|Silurian|Predominantly sandstone. A cover sequence overlying a Cambrian basement possibly deposited in Late Ordovician?||||||
7672|Grampians Group|62755|5|Briefly described|p876 Fig. 1|Silurian|Silurian|Sandstone, siltstone. See also p885 Fig. 8. See also misspelt Grampian Group.||||||
7672|Grampians Group|63124|5|Briefly described|p52|Early Devonian|Late Silurian|Thick sequence of quartzose sandstone, red siltstone and shale with minor conglomerate. ||||||
7672|Grampians Group|63446|5|Briefly described|Map legend|Silurian|Silurian||||||Marine, fluvial: sandstone, minor conglomerate, siltstone.|
7672|Grampians Group|63457|5|Briefly described|p123, p125.|||>3.5 km thickness of fluviatile and shallow marine sequences, sourced from Delamerian Highlands to the W (in the Adelaide Fold Belt). Forms two major strike ridges: the Serra and Victoria Ranges.|||||More than 3.5 km thick, including fluviatile and shallow-marine sedimentary sequences.|
7672|Grampians Group|63599|5|Briefly described|p976|Silurian|Silurian|||||||
7672|Grampians Group|64314|5|Briefly described|p495 Fig. 2a, p502|Silurian|Silurian|||||||
7672|Grampians Group|64541|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, occasional scattered or lag horizions of vein quartz pebbles; laminated, cross-laminated and trough cross-laminated; thin to thickly bedded; shallow marine trace fossils.||||||07-FEB-11
7672|Grampians Group|64597|6|Mentioned|p760 Fig.1. |||||||||
7672|Grampians Group|64610|5|Briefly described|Map legend|Silurian|Ordovician|Includes Red Man Bluff and Mount Difficult Subgroups.  Predominantly sandstones, and conglomerates.||||||12-NOV-08
7672|Grampians Group|64616|6|Mentioned|p343 Fig.23|||||||||
7672|Grampians Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Grampians. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
7672|Grampians Group|65313|5|Briefly described|p580, p576|Silurian|Silurian|Quartzites are poorly fossiliferous, riverine and minor intertidal facies. Silurian paleosols studied.||||||26-MAR-12
7672|Grampians Group|65665|6|Mentioned|p1144 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|66002|5|Briefly described|p5, p5 Tb.3|Silurian|Silurian|Includes Mount Difficult Subgroup, Silverband Formation and Red Man Bluff Subgroup. Defined by Spencer-Jones, 1965. Revised Cayley & Taylor, 1997. Formerly called Grampians sandstone series (Selwyn, 1862) and Grampian sandstone group (Selwyn and Ulrich, 1866)||||||
7672|Grampians Group|66769|5|Briefly described|117, 148|Silurian|Silurian|Grampians-Stavely Zone. Fluvial to shallow marine siliciclastics. Deformed in the Late Silurian-early Devonian. Restricted to Moyston Fault footwall; deposited in a shallow-marine foreland-basin depocentre.||||||
7672|Grampians Group|67104|5|Briefly described|p631 Fig.2, p635, p646, |Early Silurian|Late Ordovician|Confined to the area immediately west of the Moyston Fault. Younger than the Leap Year Group.|ca. 425 Ma|||||
7672|Grampians Group|67127|6|Mentioned|p73|Devonian|Devonian|Forms basement below the WIM 150 heavy mineral deposit.||||Underlies the Renmark Group.||
7672|Grampians Group|67847|6|Mentioned|p10 fig 2.3, p81|Silurian|Silurian|||||||
7672|Grampians Group|68116|5|Briefly described|Appendix, Maps 21, 22, 29, 30, 38.|Early Devonian|Late Ordovician||||||Sandstone, quartz-rich to micaceous or feldspathic; mudstone; minor polymict conglomerate.|05-JUN-14
7672|Grampians Group|68298|5|Briefly described|p220-222|Pragian|Pragian|Includes Early Devonian possible tetrapod trackways. Pragian age based on isotopic evidence. ||||||
7672|Grampians Group|70211|5|Briefly described|p3|Silurian|Late Ordovician|Fluvial to shallow-marine siliciclastic rocks.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70493|6|Mentioned|p56||Late Ordovician|Grampians-Stavely Zone, Lachlan Orogen.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70877|4|Described|p10, p12-p13, p170-p171|Silurian|Late Ordovician|Grampians-Stavely Zone. Deposited in fluvial to shallow marine environments. Thickest and most structurally complex close to the eastern edge of the Grampians-Stavely Zone.||||Overlies the Nargoon Group and the Rocklands Volcanics. Intruded by the Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Sandstone and siltstone.|
7672|Grampians Group|70904|14|Not recorded|p 38|||Stratigraphy.||||||
7672|Grampians Group|70967|6|Mentioned|p3-4, 10-11, 13|Silurian|Late Ordovician|Cayley and Taylor (1997). Fluvial to shallow-marine siliciclastic rocks. Structurally complex.|||||Sandstones and conglomerate.|
7672|Grampians Group|71040|5|Briefly described|p3, p6, p22|||W of the Moyston Fault, but has characteristics of the Lachlan Orogen, including Silurian to Early Devonian sedimentation and deformation. Age given as probably Silurian.||||Is overlain unconformably by Rocklands Volcanics.|Fluvial to shallow-marine deposits.|
7672|Grampians Group|71419|6|Mentioned|p16 Fig 17|Silurian|Silurian|Fluvial and paralic sediments.||||||
7672|Grampians Group|71593|4|Described|p8-p9, p12, p24, p44-p48|Silurian|Ordovician|Silurian. See also p57, p59, p62, p68-p70, p73-p75, p77-p78, p80-p85, p92, p95, p98-p100, p102, p133, p138-p139, p166, p169, p179, p195, p202-p203.|ca. 440 Ma|||Overlain by the Rocklands Volcanic Group. Unconformably overlies the Nargoon Group.|Fluvial to shallow marine red bed sandstone and mudstone.|
7672|Grampians Group|72445|5|Briefly described|p2-3, p9-10, p12, p16, App.1, App.7.|Silurian|Late Ordovician|See also App.2; App.5, App.7 p6 Fig.3. Contains significant structural complexity. Identified in STAVELY02. App.2 is a .csv format file. Also overlies the Nargoon Group.||||Overlies Mount Stavely Volcanic Complex, also in faulted or sheared contact. Intruded by Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Dominantly sandstone to conglomeratic sandstone with 0.7-2.3 m lenses of conglomerate. Includes fluvial to shallow marine siliciclastic rocks; sandstone and conglomerate.|15-OCT-20
7672|Grampians Group|73059|6|Mentioned|p1059|Late Ordovician|Late Ordovician|Grampians-Stavely Zone.||||||
7672|Grampians Group|73118|5|Briefly described|p6-8, 14, 19, 42, 48, 53, 64-72, 74|Silurian|Silurian|Glenelg Zone, Western Victoria. A terrestrial to marginal marine sequence. Features basal subhorizontal cataclastic zones; underwent repeated thrusting and extensional faulting.|||Wartook Sandstone.|Is overlain by Rocklands Rhyolite, Shepparton Formation or Loxton-Parilla Sands. Is intruded by Victoria Valley Granite. Is metamorphosed locally by Duchembegarra Granite.|Includes massive to banded quartz sandstones, and intraclast conglomerate.|
7672|Grampians Group|73576|6|Mentioned|p818|Devonian|Devonian|||||||
7672|Grampians Group|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
7675|Grampus Quartzite|22510|5|Briefly described|p40, table1|||Age: Marinoan.  Grades up into and intertongues with the Ketchowla Siltstone.||||||13-OCT-04
7675|Grampus Quartzite|23818|5|Briefly described|p64 Fig.22, p72|Neoproterozoic|Neoproterozoic|Of the Yerelina Sub-Group. Overlying unit: Wilpena Group. Equivalent to the Balparana Sandstone.||||||19-JAN-05
7675|Grampus Quartzite|24507|6|Mentioned|p23|||System of quartz-ladder veins, developed within a thick, competent quartzite layer.||||||
7675|Grampus Quartzite|29778|6|Mentioned|p167|||||||||
7675|Grampus Quartzite|29780|5|Briefly described|p42|||||||||
7675|Grampus Quartzite|30801|6|Mentioned|p5|||Marinoan. Table P5-6. Lenticular member? in Pepuarta Tillite||||||
7675|Grampus Quartzite|30807|6|Mentioned|p102|||Suggested map symbol||||||
7675|Grampus Quartzite|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
7675|Grampus Quartzite|34535|6|Mentioned|Fig.22|||Yerelina Sub-Group||||||
7675|Grampus Quartzite|36126|6|Mentioned|Fig.1|||||||||
7675|Grampus Quartzite|37461|6|Mentioned|p342|||See also Table 5.I||||||
7675|Grampus Quartzite|37932|6|Mentioned|p546|||||||||
7675|Grampus Quartzite|38110|6|Mentioned|p2|||||||||
7675|Grampus Quartzite|38157|6|Mentioned|Table IV|||||||||
7675|Grampus Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
7675|Grampus Quartzite|41405|4|Described|p200|||||||||
7675|Grampus Quartzite|41500|6|Mentioned|Fig.1|||||||||
7675|Grampus Quartzite|42098|5|Briefly described|p54|||||||||
7675|Grampus Quartzite|42109|5|Briefly described|Fig.1 P19|||||||||
7675|Grampus Quartzite|42222|6|Mentioned|p18|||||||||
7675|Grampus Quartzite|42542|5|Briefly described|p8|||||||||
7675|Grampus Quartzite|42720|5|Briefly described|map legend|Marinoan||||||||
7675|Grampus Quartzite|42813|5|Briefly described|p21|||of Yerelina Subgroup.||||||30-SEP-08
7675|Grampus Quartzite|43052|5|Briefly described|p192,Table 6.1|||Of Yerelina Subgroup.||||||30-SEP-08
7675|Grampus Quartzite|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
7675|Grampus Quartzite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Marinoan.||||||
7675|Grampus Quartzite|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Quartzite, arenaceous, with conglomerate.||||||
7675|Grampus Quartzite|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
7675|Grampus Quartzite|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||Yerelina Subgroup||Overlies Pepuarta Tillite.||26-APR-12
7675|Grampus Quartzite|68241|6|Mentioned|p20 Fig.1|||||||||
7675|Grampus Quartzite|71237|14|Not recorded|p9, 17|||||||||
7675|Grampus Quartzite|71241|14|Not recorded|p13, 17, p9|||Burra sheet area.||||||
7675|Grampus Quartzite|73227|6|Mentioned|p36|||Adelaide Superbasin. May have been a lateral fluid conduit.||||||
7680|Grange Burn Formation|23768|5|Briefly described|p30 Fig.6, p27|Early Pliocene|Late Miocene|Geological Province: Otway Basin.  See also p33, p162.||||||30-MAR-05
7680|Grange Burn Formation|23909|5|Briefly described|p291|Pliocene|Pliocene|||||||
7680|Grange Burn Formation|24551|5|Briefly described|p306, 581||Early Pliocene|||||||
7680|Grange Burn Formation|30393|6|Mentioned|p309|||||||||
7680|Grange Burn Formation|31516|6|Mentioned|p49|||||||||
7680|Grange Burn Formation|33160|6|Mentioned|p300|||See also P303||||||
7680|Grange Burn Formation|34988|6|Mentioned|Table 9.4|||||||||
7680|Grange Burn Formation|35066|3|Fully described|p215|||||||||
7680|Grange Burn Formation|35271|6|Mentioned|Fig.2|||||||||
7680|Grange Burn Formation|38070|6|Mentioned|Fig.12|||Otway Basin||||||
7680|Grange Burn Formation|40756|6|Mentioned|Fig.1.2|||Entered as SA unit. Probably should be VIC.||||||
7680|Grange Burn Formation|40759|5|Briefly described|p70|||||||||
7680|Grange Burn Formation|41043|6|Mentioned|p98|||||||||
7680|Grange Burn Formation|41075|6|Mentioned|p22|||||||||
7680|Grange Burn Formation|41398|6|Mentioned|p3|||||||||
7680|Grange Burn Formation|41537|6|Mentioned|p350|||||||||
7680|Grange Burn Formation|42827|3|Fully described|p289||Tertiary|see also Fig 8.9||||||
7680|Grange Burn Formation|44238|14|Not recorded|Fig.3||Pliocene|||||||
7680|Grange Burn Formation|45128|6|Mentioned|p55|||Originally wrongly entered as a NT unit.||||||
7680|Grange Burn Formation|48911|6|Mentioned|Chart 1|||||||||
7680|Grange Burn Formation|60421|5|Briefly described|p409, 418 Fig. 5|Pliocene|Upper Miocene|||||||
7680|Grange Burn Formation|60785|5|Briefly described|p184 Fig.1, pp186-187.  |Zanclean|Messinian|Of the Otway Basin. Foraminifera dates indicate N17 age (Mallett, 1977). The overlying basalt is dated to 4.35 Ma with K-Ar (Turnbull et al., 1965)Sr/Sr dates from the base indicate 4.0-5.0 Ma max. age (Dickinson et al., 2002). Isolated, rolled, polished and broken fossil cetacean elements.||||Disconformably overlies the Muddy Creek Marl Member.|The base is marked by a phosphatic nodule bed horizon. Shelly marl and sandy to pebbly limestone.|
7680|Grange Burn Formation|61207|5|Briefly described|p280 Fig. 2|Early Pliocene|Early Pliocene|Marls (rich in molluscs) and sands. Underlie the Newer Volcanics, and/or Dorodong Sands. Age: 5.5-4.7Ma; generally considered to be Kalimnan. Geological Province: onshore Otway Basin. See also p283 Fig. 3, p286-287.||||||12-JAN-06
7680|Grange Burn Formation|61841|5|Briefly described|p242|||Marine sediments.  Age: is post-Eocene. Geological Province: Otway Basin.||||||03-JUL-06
7680|Grange Burn Formation|63446|5|Briefly described|Map legend|Pliocene|Miocene||||||Marine: shell beds, sandy limestone, calcareous sand.|
7680|Grange Burn Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Otway Basin.||||||
7680|Grange Burn Formation|68116|5|Briefly described|Appendix, Map 38.|Zanclean|Messinian||||||Shell beds, shelly marl, sandy limestone, calcareous sand.|05-JUN-14
7764|Greenhill Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Stonyfell Quartzite of the Bungarider Subgroup.||||||
7764|Greenhill Member|36835|6|Mentioned|p31|||||||||
7764|Greenhill Member|41404|6|Mentioned|Fig.23|||||||||
7764|Greenhill Member|43052|5|Briefly described|p181,Table 6.1|||of Stonyfell Quartzite||||||
7764|Greenhill Member|73188|6|Mentioned|p328|Neoproterozoic|Neoproterozoic|||Stonyfell Quartzite, Bungarider Subgroup, Burra Group||||
7767|Greenpatch Metajaspilite|23818|6|Mentioned|p28|||Of the Hutchinson "Group". Geological Province: Gawler Block.||||||
7767|Greenpatch Metajaspilite|34537|6|Mentioned|p28|||||||||
7767|Greenpatch Metajaspilite|38068|5|Briefly described|p66|||||||||
7767|Greenpatch Metajaspilite|61556|5|Briefly described|p8|||Contains calcite and/or dolomite but no sideratite and may be equated with Lower Middleback Quartzite. See also Figure on p9-10.||||||21-NOV-07
7831|Grindstone Range Sandstone|22766|5|Briefly described|Fig.2 p561|Middle Cambrian|Middle Cambrian|||||||
7831|Grindstone Range Sandstone|22857|5|Briefly described|p90 Fig. 14.7B|Early Ordovician|Early Ordovician|Of the Lake Frome Formation. Range is Rg. In text of figure. Geological Province: Arrowie Basin. ||||||
7831|Grindstone Range Sandstone|22858|6|Mentioned|Fig14.7bp90-1|||||||||
7831|Grindstone Range Sandstone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Youngest formation of the Lake Frome Group.||||||
7831|Grindstone Range Sandstone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
7831|Grindstone Range Sandstone|24138|5|Briefly described|p32|Cambrian|Cambrian|Quartzite and sandstone. Geological Province: Adelaide Geosyncline.||||||
7831|Grindstone Range Sandstone|24176|4|Described|p17-18, p23 Tb. 1|Late Cambrian|Late Cambrian|Of the Lake Frome Group.  White quartzite and minor red sandstone.  Overlies Pantapinna Sandstone.   Max. thickness: 610m.  Geological Province: Mount Painter Province.||||||
7831|Grindstone Range Sandstone|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Of Lake Frome Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
7831|Grindstone Range Sandstone|30176|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7831|Grindstone Range Sandstone|30801|6|Mentioned|p5|||Lake Frome Group. Table P5-6||||||
7831|Grindstone Range Sandstone|30802|5|Briefly described|p11|||Cambrian age||||||
7831|Grindstone Range Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
7831|Grindstone Range Sandstone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
7831|Grindstone Range Sandstone|31923|6|Mentioned|p11|||||||||
7831|Grindstone Range Sandstone|33474|6|Mentioned|Fig.3|||||||||
7831|Grindstone Range Sandstone|33932|6|Mentioned|Fig.2|||||||||
7831|Grindstone Range Sandstone|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
7831|Grindstone Range Sandstone|33973|6|Mentioned|Fig.2|||||||||
7831|Grindstone Range Sandstone|34269|6|Mentioned|Table 1|||Cambrian||||||
7831|Grindstone Range Sandstone|34612|5|Briefly described|p96|||Cambrian. Correlation chart. Fig.33.||||||
7831|Grindstone Range Sandstone|35255|6|Mentioned|Fig.8|||See also P19.||||||
7831|Grindstone Range Sandstone|36198|6|Mentioned|Fig.I.2|||||||||
7831|Grindstone Range Sandstone|38068|6|Mentioned|p69|||||||||
7831|Grindstone Range Sandstone|38329|6|Mentioned|p209|||||||||
7831|Grindstone Range Sandstone|40852|6|Mentioned|Fig.3.7|||||||||
7831|Grindstone Range Sandstone|42090|5|Briefly described|p26|||||||||
7831|Grindstone Range Sandstone|42222|6|Mentioned|Table 1 P5|||||||||
7831|Grindstone Range Sandstone|42225|6|Mentioned|Fig.4 P224|||||||||
7831|Grindstone Range Sandstone|42269|5|Briefly described|p338|||||||||
7831|Grindstone Range Sandstone|42440|6|Mentioned|Fig.2 P602|||||||||
7831|Grindstone Range Sandstone|43052|5|Briefly described|Table 2.1|||||||||
7831|Grindstone Range Sandstone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
7831|Grindstone Range Sandstone|44133|5|Briefly described|p30, 4 Fig. 7.2, 28|Iverian|Early Paleozoic|Geological Province: Arrowie Basin. Of the Lake Frome Group. Maximum Thickness: 750m. ||||||07-NOV-08
7831|Grindstone Range Sandstone|60889|4|Described|p245 Fig.2, p247 Fig.4, p249|Middle Cambrian|Middle Cambrian|Thickness: 600 m. Arrowie Basin.||Lake Frome Group||Overlies Pantapinna Sandstone.|Cross-bedded sandstone with some horizons of extremely well-rounded quartzite pebbles and cobbles towards top of exposed section.|
7831|Grindstone Range Sandstone|60959|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Lake Frome Group. Cross-bedded mature quartz arenite with minor feldspar and volcanic lithic clasts.||||||
7831|Grindstone Range Sandstone|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Lake Frome Group.||Overlies Pantapinna Sandstone.||
7831|Grindstone Range Sandstone|63569|5|Briefly described|p117 Fig.1|Middle Cambrian|Middle Cambrian|Arrowie Basin. Thickness 600 m.||Unit in Lake Frome Group.||||
7831|Grindstone Range Sandstone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Ordovician|Late Cambrian|Unit discussed in the context of soilscapes and palaeosols. See also Grindstone Range Formation. Age is Tremadocian. Has associated palaeosols.||||||07-FEB-11
7831|Grindstone Range Sandstone|65313|5|Briefly described|p577, p576, p578 Fig. 6, p573 Fig. 2|Tremadocian|Tremadocian|New Tremadocian age this paper based on pedostratigraphy. Paleocurrents to N and E indicate Gawler Craton as source terrane.||Of Lake Frome Group.||Overlies Pantapinna Sandstone, Arrowie Basin.||26-MAR-12
7831|Grindstone Range Sandstone|65375|5|Briefly described|p33.|Middle Cambrian|Middle Cambrian|||Unit in Lake Frome Group.||Overlies Pantapinna Sandstone.||
7831|Grindstone Range Sandstone|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.||Top unit of Lake Frome Group.||||16-FEB-11
7831|Grindstone Range Sandstone|65686|5|Briefly described|p409 Fig 2|Middle Cambrian|Middle Cambrian|Arrowie Basin. 600m thick.||||||
7831|Grindstone Range Sandstone|65892|5|Briefly described|p7 Fig.3. |Middle Cambrian|Middle Cambrian|Arrowie Basin. 600m thick. See also [superseded] Grindstone Range Formation (p9 Fig.4, p11).||Unit in Lake Frome Group.||Overlies Pantapinna Sandstone.|Cross-bedded sandstone; some horizons of extremely well-rounded quartzite pebbles and cobbles towards the top.|
7831|Grindstone Range Sandstone|65925|5|Briefly described|p14 Fig.2.2.|Middle Cambrian|Middle Cambrian|||Unit in Lake Frome Group.||||
7831|Grindstone Range Sandstone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||Unit in Lake Frome Group.||Overlies Pantapinna Sandstone.||
7831|Grindstone Range Sandstone|68735|4|Described|p233 Fig.2, p236, p238|Middle Cambrian|Middle Cambrian|Arrowie Basin. See also Grindstone Range Formation. ~ 550 m thick, although the top of this formation is not exposed. Cross-bedding rose diagrams.||Uppermost unit of the Lake Frome Group.|Includes the Dawson Hill Member.|Underlain by the Pantapinna Sandstone.|Lower: well-bedded, well-sorted and fine-grained sandstone with abundant planar cross-bedding and some trough bedding. Upper: Dawson Hill Member.|10-APR-17
7831|Grindstone Range Sandstone|68993|5|Briefly described|p543|Middle Cambrian|Middle Cambrian|This current name is used as often as not, and within the same paragraph, as the name Grindstone Range Formation. Arrowie Basin. Lower 368 m: shallow marine origin (includes trilobite tracks and other trace fossils). Upper: fluvial conditions, with the possible exception of the top 10 m, which may have a littoral or shallow marine origin.||Of the Lake Frome Group.|Includes the Dawson Hill Member in its upper part.|||
7831|Grindstone Range Sandstone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
7831|Grindstone Range Sandstone|72449|5|Briefly described|p2 Map legend|Cambrian|Cambrian|||||Overlies Pantapinna Sandstone.|Cross-bedded sandstone with quartzite pebble conglomerate in the upper part.|
7831|Grindstone Range Sandstone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||Lake Frome Group||Underlain by Pantapinna Sandstone.||
7831|Grindstone Range Sandstone|73255|6|Mentioned|p534 Fig.2|Ordovician|Ordovician|[Ordovician? age shown on p534 Fig.2]||||Overlies the Pantapinna Sandstone.||
7848|Gubberamunda Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497|Tithonian|Kimmeridgian|Mis-spelt as Gubbermunda in Tb.1. The permeable sandstones form a major fresh-water subsurface aquifer. Thickness generally <100m.||||Grades laterally into Hooray Sandstone. Interfingers with upper part of Pilliga Sandstone; equivalent to Kumbarilla beds.|Quartzose sub-labile sandstone with minor siltstone and mudstone beds.|
7848|Gubberamunda Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Late Jurassic|In Surat Basin, Eromanga Basin.||||||
7848|Gubberamunda Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Late Jurassic|200 m. Surat Basin||||||
7848|Gubberamunda Sandstone|22857|5|Briefly described|p296-7 Tb.22.1, p314|Tithonian|Oxfordian|Of the Injune Creek Group. Merges with the Pilliga Sandstone from NSW. Geological Province: Surat Basin. See also p546 App.1 Tb.A1.12.||||||
7848|Gubberamunda Sandstone|22865|4|Described|p314,Table22.1p296-7|Early Cretaceous|Late Jurassic|||||||
7848|Gubberamunda Sandstone|23056|6|Mentioned|9|||Geol province Eromanga Basin||||||
7848|Gubberamunda Sandstone|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Great Artesian Basin. Of the Blythesdale Group.||||||
7848|Gubberamunda Sandstone|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
7848|Gubberamunda Sandstone|24068|4|Described|p270 Table 2|Late Jurassic|Late Jurassic|Geological Province: Surat Basin.  Maximum thickness: 250m.||||||
7848|Gubberamunda Sandstone|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
7848|Gubberamunda Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|29387|6|Mentioned|Table 5|||||||||
7848|Gubberamunda Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
7848|Gubberamunda Sandstone|29591|6|Mentioned|p77|||||||||
7848|Gubberamunda Sandstone|29698|6|Mentioned|p65|||||||||
7848|Gubberamunda Sandstone|29721|6|Mentioned|Table 246|||||||||
7848|Gubberamunda Sandstone|30021|6|Mentioned|p89|||||||||
7848|Gubberamunda Sandstone|30024|6|Mentioned|p332|||||||||
7848|Gubberamunda Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
7848|Gubberamunda Sandstone|30694|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|30695|4|Described|Table 4|||Upper Jurassic age||||||
7848|Gubberamunda Sandstone|30696|4|Described|Table 4|||Middle to Upper Jurassic age||||||
7848|Gubberamunda Sandstone|30697|6|Mentioned|p34|||Major aquifer present||||||
7848|Gubberamunda Sandstone|30700|6|Mentioned|p22|||Map. Jurassic-Cretaceous||||||
7848|Gubberamunda Sandstone|30701|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|30702|6|Mentioned|p48|||See also P49-51, Fig.1,2,Table 1||||||
7848|Gubberamunda Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
7848|Gubberamunda Sandstone|31097|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|31098|5|Briefly described|Table 1|||||||||
7848|Gubberamunda Sandstone|31116|4|Described|p38|||See also Table 2. Jurassic||||||
7848|Gubberamunda Sandstone|31369|6|Mentioned|Table 4|||||||||
7848|Gubberamunda Sandstone|32136|6|Mentioned|p9|||Miospores||||||
7848|Gubberamunda Sandstone|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.-U.JurassicM - U||||||
7848|Gubberamunda Sandstone|32276|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
7848|Gubberamunda Sandstone|32797|4|Described|Table 4|||||||||
7848|Gubberamunda Sandstone|33070|4|Described|Table 2|||U.Jur.||||||
7848|Gubberamunda Sandstone|33071|6|Mentioned|p6|||L.Cret.||||||
7848|Gubberamunda Sandstone|33075|6|Mentioned|p451|||||||||
7848|Gubberamunda Sandstone|33080|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33090|4|Described|Table 4|||U.Jur.||||||
7848|Gubberamunda Sandstone|33091|5|Briefly described|p10|||Stratigraphy||||||
7848|Gubberamunda Sandstone|33094|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33367|4|Described|p11|||See also Table 1.||||||
7848|Gubberamunda Sandstone|33371|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|33451|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33672|6|Mentioned|p44|||||||||
7848|Gubberamunda Sandstone|33828|6|Mentioned|Table 3|||||||||
7848|Gubberamunda Sandstone|33939|6|Mentioned|p412|||Unit of Blythesdale Gp.||||||
7848|Gubberamunda Sandstone|33971|6|Mentioned|p36|||See also Fig.29.||||||
7848|Gubberamunda Sandstone|34212|6|Mentioned|p2|||Jurassic||||||
7848|Gubberamunda Sandstone|34254|6|Mentioned|p489|||||||||
7848|Gubberamunda Sandstone|34543|6|Mentioned|p98|||||||||
7848|Gubberamunda Sandstone|34611|6|Mentioned|Fig.65|||Correlation chart. Blythesdale Group||||||
7848|Gubberamunda Sandstone|34613|4|Described|Table 4|||||||||
7848|Gubberamunda Sandstone|35793|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|36243|6|Mentioned|Table 7A|||||||||
7848|Gubberamunda Sandstone|36570|6|Mentioned|Table 1|||Also mention P55.||||||
7848|Gubberamunda Sandstone|37117|5|Briefly described|p313|||||||||
7848|Gubberamunda Sandstone|37993|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|37995|4|Described|p64|||||||||
7848|Gubberamunda Sandstone|38068|6|Mentioned|p71|||||||||
7848|Gubberamunda Sandstone|38199|6|Mentioned|p428|||||||||
7848|Gubberamunda Sandstone|39211|5|Briefly described|Fig.3|||||||||
7848|Gubberamunda Sandstone|39212|4|Described|p38|||Excursion site. Aquifers. See also P16 & 25||||||
7848|Gubberamunda Sandstone|39315|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|39445|5|Briefly described|Table 10|||||||||
7848|Gubberamunda Sandstone|39494|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|39943|6|Mentioned|Table 9A|||||||||
7848|Gubberamunda Sandstone|40030|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|40245|6|Mentioned|Table 2|||||||||
7848|Gubberamunda Sandstone|40249|6|Mentioned|p38|||||||||
7848|Gubberamunda Sandstone|40250|6|Mentioned|Fig.7|||||||||
7848|Gubberamunda Sandstone|40540|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|40541|3|Fully described|p110|||||||||
7848|Gubberamunda Sandstone|40544|6|Mentioned|Fig.6|||||||||
7848|Gubberamunda Sandstone|40623|5|Briefly described|p108|||||||||
7848|Gubberamunda Sandstone|40666|4|Described|p357|||||||||
7848|Gubberamunda Sandstone|40675|6|Mentioned|Table 9A|||||||||
7848|Gubberamunda Sandstone|40687|6|Mentioned|p417|||||||||
7848|Gubberamunda Sandstone|40926|6|Mentioned|p13|||||||||
7848|Gubberamunda Sandstone|41060|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|41064|6|Mentioned|p60|||||||||
7848|Gubberamunda Sandstone|41187|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|41210|5|Briefly described|Fig.3|||||||||
7848|Gubberamunda Sandstone|41216|6|Mentioned|Fig.18|||||||||
7848|Gubberamunda Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
7848|Gubberamunda Sandstone|41247|6|Mentioned|Fig.7|||||||||
7848|Gubberamunda Sandstone|41266|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|41681|6|Mentioned|p7|||||||||
7848|Gubberamunda Sandstone|41992|4|Described|Fig.2 P183|||||||||
7848|Gubberamunda Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
7848|Gubberamunda Sandstone|42493|5|Briefly described|p20, Fig. 1 p18|||||||||
7848|Gubberamunda Sandstone|42494|5|Briefly described|Table 1 P24|||||||||
7848|Gubberamunda Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
7848|Gubberamunda Sandstone|42950|6|Mentioned|p41|||||||||
7848|Gubberamunda Sandstone|43000|5|Briefly described|Fig.5,p112|||of Blythesdale Group||||||
7848|Gubberamunda Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
7848|Gubberamunda Sandstone|43404|14|Not recorded|Table p4||Late Jurassic|||||||
7848|Gubberamunda Sandstone|43539|14|Not recorded|p398|||||||||
7848|Gubberamunda Sandstone|43602|6|Mentioned|207|||In Surat Basin||||||
7848|Gubberamunda Sandstone|43982|14|Not recorded|Map Legend||Late Jurassic|||||||
7848|Gubberamunda Sandstone|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
7848|Gubberamunda Sandstone|43991|5|Briefly described|p50|Cretaceous|Jurassic|Part of Blythesdale "Group".||||||
7848|Gubberamunda Sandstone|43994|14|Not recorded|Map Legend|||||||||
7848|Gubberamunda Sandstone|43995|14|Not recorded|p13,57,58,Fig.5|||Part of Blythesdale Group.||||||
7848|Gubberamunda Sandstone|43998|4|Described|p16,map|Cretaceous|Jurassic|||||||
7848|Gubberamunda Sandstone|44021|14|Not recorded|p232-234,236,238|||Ref. to Saltern Creek No.1 Well. At 1750-1850' =Adori Sandstone (not Gubberamunda Sandstone).||||||
7848|Gubberamunda Sandstone|44022|14|Not recorded|Map Legend||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44023|4|Described|Tb.3,p12||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44027|14|Not recorded|p110||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44028|14|Not recorded|Fig.2,p512,513||Jurassic|Equivalent of Pilliga Sandstone. See Strat Table.||||||
7848|Gubberamunda Sandstone|44031|14|Not recorded|p10,11,12||Late Jurassic|Artesian water.||||||
7848|Gubberamunda Sandstone|44088|14|Not recorded|p6|||Possibly equivalent to part of Blythesdale Group?||||||
7848|Gubberamunda Sandstone|44091|14|Not recorded|p57||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44124|14|Not recorded|p1,2,6,10,25|||||||||
7848|Gubberamunda Sandstone|44171|14|Not recorded|p194,197,198|||||||||
7848|Gubberamunda Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
7848|Gubberamunda Sandstone|44371|14|Not recorded|Map Legend||Jurassic|||||||
7848|Gubberamunda Sandstone|44375|14|Not recorded|p310|||Aquifer.||||||
7848|Gubberamunda Sandstone|44377|14|Not recorded|p1-5,8,11,22,map||Late Jurassic|Fluviatile (probably Late Jurassic)||||||
7848|Gubberamunda Sandstone|44381|14|Not recorded|p8|||||||||
7848|Gubberamunda Sandstone|44414|14|Not recorded|p114|Cretaceous|Jurassic|||||||
7848|Gubberamunda Sandstone|44415|14|Not recorded|Fig.2,p23|||||||||
7848|Gubberamunda Sandstone|44636|14|Not recorded|p167(Tb)||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
7848|Gubberamunda Sandstone|45071|4|Described|Table 15|||||||||
7848|Gubberamunda Sandstone|45110|2|Defined|p99|Late Jurassic|Late Jurassic|See also p24 and Fig.5.||||||18-SEP-18
7848|Gubberamunda Sandstone|46791|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7848|Gubberamunda Sandstone|46984|6|Mentioned|Table 1|||||||||
7848|Gubberamunda Sandstone|48606|14|Not recorded|p21|||(G/55-12).||||||
7848|Gubberamunda Sandstone|48919|4|Described|p67|||U.Jurassic||||||
7848|Gubberamunda Sandstone|48920|6|Mentioned|Table 7|||Refers Day (1964)||||||
7848|Gubberamunda Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
7848|Gubberamunda Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin.||||||
7848|Gubberamunda Sandstone|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|61000|5|Briefly described|p186 Fig. 4|Tithonian|Tithonian|Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
7848|Gubberamunda Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|63979|6|Mentioned|p40|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
7848|Gubberamunda Sandstone|64197|6|Mentioned|p630 Fig.7|Cretaceous|Jurassic|||||Underlies Orallo Formation; overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Surat Basin.||||Overlies Westbourne Formation. Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|64856|3|Fully described|p79, p91, p92 Fig.43, p94-95|Tithonian|Tithonian|Surat Basin. Of Day (1964) after Reeves (1947). Type area near Bungil Creek, c.35km N of Roma. Conformably overlies the Westbourne Formation, locally disconformably. Transitionally overlain by Orallo Formation. Age from palynofloral units APJ62, APK1. Max thickness 298m. Virtually uncemented quartzose sandstone.| | ||||29-NOV-17
7848|Gubberamunda Sandstone|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Westbourne Formation, Surat Basin.||||||
7848|Gubberamunda Sandstone|64858|6|Mentioned|p187-188|||Referred to as Gubberamunda Formation on tables and figures.||||||30-NOV-09
7848|Gubberamunda Sandstone|65112|5|Briefly described|p323|Jurassic|Jurassic|||||Overlies Westbourne Formation; underlies Orallo Formation.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
7848|Gubberamunda Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Westbourne Formation, underlies the Orallo.||||||
7848|Gubberamunda Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
7848|Gubberamunda Sandstone|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Orallo Formation, Overlies the Westbourne Formation, Surat Basin.||||||
7848|Gubberamunda Sandstone|65117|6|Mentioned|p463|||Surat Basin. Overlies Westbourne Formation. ||||||
7848|Gubberamunda Sandstone|65119|5|Briefly described|Table 1, Fig 7-8, 13-14, 16-19|Late Jurassic|Late Jurassic|Age: 149-153 Ma. Fission Track age: 131+/-11 Ma .Quartzose to clayey lithic sandstone, some conglomerate and siltstone, up to 300m thick. See also Gubberamunda Formation p503, Gubberamunda Siltstone p512||||||07-MAR-12
7848|Gubberamunda Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Injune Creek Group. Is overlain by Southlands and Orallo Formations.||
7848|Gubberamunda Sandstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|67133|5|Briefly described|p2, p5, p16, p18-21|Late Jurassic|Late Jurassic|16 samples of this unit were analysed by XRD and optical microscopy for this study. Meandering stream deposits. Quartz is the main component (30-90%); feldspars vary (8-28%) with plagioclase always dominant. Kaolinite (up to 30%) is the dominant clay mineral. The small concentrations (only a few percent) of mixed-layer clays are smectite-rich.||||Overlies Westbourne Formation. Is overlain conformably by Orallo Formation.|Medium- to coarse-grained, largely quartzose, poorly sorted sandstone with minor conglomerates and siltstones.|
7848|Gubberamunda Sandstone|67402|4|Described|p146 fig SRT3, p148|Barremian|Tithonian|Surat Basin. Deposited in a braided and meandering stream system. Maximum thickness of 200m. See also p154 fig SRT15/16, p156.||Blythesdale Group||Overlies the Westbourne Formation. Overlain by the Orallo Formation.|Quartzose sandstone with lesser conglomerate, siltstone and mudstone.|
7848|Gubberamunda Sandstone|67669|5|Briefly described|p11|Late Jurassic|Late Jurassic|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Orallo Formation. Underlain by Westbourn Formation.||
7848|Gubberamunda Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Overlies Injune Creek Group. Is overlain by Blythesdale Group.||
7848|Gubberamunda Sandstone|68117|6|Mentioned|p346|Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Tithonian|Surat Basin (QLD).||||Unconformably overlies Westbourne Formation. Is overlain by Orallo Formation|Cross-bedded sandstone.|14-SEP-17
7848|Gubberamunda Sandstone|68139|6|Mentioned|p23|Early Cretaceous|Late Jurassic|Surat Basin.||||Overlies Westbourne Formation. Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
7848|Gubberamunda Sandstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Late Jurassic|Surat Basin.||||Unconformably overlies Westbourne Formation (Injune Creek Group). Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|69574|6|Mentioned|p34|Early Cretaceous|Late Jurassic|||||||
7848|Gubberamunda Sandstone|69582|5|Briefly described|p36, p38|Early Cretaceous|Late Jurassic|Surat Basin.||||Unconformably overlies the Westbourne Formation. Overlain by the Orallo Formation.|Sandstone.|
7848|Gubberamunda Sandstone|69594|4|Described|p519, p527, p537, p573|Berriasian|Tithonian|Reeves (1947); Day (1964). Northern Surat Basin. The type section is 35km N of Roma, in Bungil Creek. Generally ~100m thick, up to 298m. Meandering and braided stream deposits.||||Overlies Westbourne Formation conformably (locally disconformably). Is overlain transitionally by Orallo Formation. Equivalent to Hooray Sandstone and parts of Kumbarilla beds.|Quartzose to sublabile sandstone, lesser conglomerate, siltstone, mudstone and claystone.|
7848|Gubberamunda Sandstone|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
7848|Gubberamunda Sandstone|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Northern Surat Basin.||||||
7848|Gubberamunda Sandstone|70628|6|Mentioned|p952 fig 4|Kimmeridgian|Kimmeridgian|Shown only as 'Gubberamunda' in fig 4. Along with Springbok Formation, Westbourne [Formation],  forms part of the L-sequence (Hoffman et al 2009) of the Surat Basin.||||Overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|70821|5|Briefly described|p21 Fig.2.6, p80|Early Cretaceous|Jurassic|Surat Basin. Aquifer: generally artesian.||||Overlies Westbourne Formation. Is overlain by Orallo and Southlands Formations.||
7848|Gubberamunda Sandstone|70836|6|Mentioned|p474|Late Jurassic|Late Jurassic|Lightning Ridge area, Surat Basin.||||Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|71282|6|Mentioned|p457 Fig.1|||The lithology is omitted in Fig.1.||||||
7848|Gubberamunda Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
7848|Gubberamunda Sandstone|72297|6|Mentioned|p761|||Temperatures in its aquifers highlight a broad heat anomaly through the Carpentaria and Eromanga Basins; potential for geothermal energy.||||||
7848|Gubberamunda Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Orallo and Southlands FZs.||
7848|Gubberamunda Sandstone|72921|5|Briefly described|p15 Fig.2, p24.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland. Described as a 'shallower aquifer' [presumably than Hutton Sandsotne].||||Unconformably overlies Westbourne Formation and partially underlies Orallo Formation.||
7848|Gubberamunda Sandstone|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 69, 80, 88...|||Surat Basin. Regional aquifer. More locations: p. 98, 116-117, 119, 123, 129, 146, 151-152, 158, 160, 167, 169-173, 177-178, 191.||||Underlain by Westbourne Formation.||
7848|Gubberamunda Sandstone|73193|6|Mentioned|p369|Berriasian|Tithonian|Surat Basin.||||Unconformably underlain by Westbourne Formation (Injune Creek Group). Overlain by Orallo Formation.||
7861|Gull Rock Member|22525|6|Mentioned|p37||Eocene|Superseded by Blanche Point Formation.||||||24-JUL-08
7861|Gull Rock Member|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
7861|Gull Rock Member|22541|4|Described|p 22, Fig 1, 7|||Blanche Point Formation||||||
7861|Gull Rock Member|23802|5|Briefly described|p21 Fig. 2|||Parent: Blanche Point Formation.||||||
7861|Gull Rock Member|30250|2|Defined|p2|late Eocene|late Eocene|||||||
7861|Gull Rock Member|35542|6|Mentioned|p3|||||||||
7861|Gull Rock Member|35689|2|Defined|p19|late Eocene|late Eocene|||||||
7861|Gull Rock Member|36127|5|Briefly described|p11|||See also P7.||||||
7861|Gull Rock Member|36244|6|Mentioned|p2|||Defined by Cooper 1977,1979.||||||
7861|Gull Rock Member|37324|6|Mentioned|p11|||||||||
7861|Gull Rock Member|38107|4|Described|p28|||||||||
7861|Gull Rock Member|38621|1|Redefined|p4|late Eocene|late Eocene|||||||
7861|Gull Rock Member|38699|6|Mentioned|p18|||||||||
7861|Gull Rock Member|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7861|Gull Rock Member|40238|5|Briefly described|p125|||||||||
7861|Gull Rock Member|40429|6|Mentioned|Fig.2|||||||||
7861|Gull Rock Member|40453|6|Mentioned|Fig.5|||||||||
7861|Gull Rock Member|40778|6|Mentioned|p529|||||||||
7861|Gull Rock Member|40877|5|Briefly described|p47|||||||||
7861|Gull Rock Member|40969|6|Mentioned|p7|||||||||
7861|Gull Rock Member|41025|6|Mentioned|Fig.3|||||||||
7861|Gull Rock Member|41495|6|Mentioned|p44|||||||||
7861|Gull Rock Member|41513|6|Mentioned|p44|||||||||
7861|Gull Rock Member|41520|5|Briefly described|Fig.5|||||||||
7861|Gull Rock Member|41626|6|Mentioned|p54|||||||||
7861|Gull Rock Member|42498|6|Mentioned|Map Legend|Eocene|Eocene|||||||
7861|Gull Rock Member|42506|5|Briefly described|Map legend|Eocene||Age Tertiary.||||||24-JUL-08
7861|Gull Rock Member|42574|6|Mentioned|Fig.2 P242|||||||||
7861|Gull Rock Member|42733|5|Briefly described|map legend|Tertiary||||||||
7861|Gull Rock Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Of the Blanche Point Formation. Overlies: Tuketja Member. Underlies: Perkana Member.||||||
7861|Gull Rock Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Balance Point Formation.||||||
7861|Gull Rock Member|62896|5|Briefly described|p87|Oligocene|Late Eocene|Of Blanche Point Formation. Geological Province: St Vincent Basin.||||||07-FEB-11
7861|Gull Rock Member|63740|5|Briefly described|p87|Oligocene|Eocene|Of Blanche Point Formation. Geological Province: St Vincent Basin.||||||07-FEB-11
7861|Gull Rock Member|64397|5|Briefly described|p233 Fig. 2|Late Eocene|Late Eocene|Hard (silica-rich) and soft (carbonate-rich) layers. Geological province: St Vincent Basin.||||||
7861|Gull Rock Member|65891|5|Briefly described|p222 Fig.7, p228 Fig.11.|Paleogene|Paleogene|Unit in Blanche Point Formation, between Tuketja (below) and Perkana Members. Spirocolpus-rich.||||||
7861|Gull Rock Member|70660|4|Described|p8-p9, p12, p17-p19|Priabonian|Priabonian|See also p25-p26, p33, p46.||Blanche Point Formation||Overlies the Tuketja Member. Overlain by the Perkana Member. Conformably overlain by the Rogue Formation.|Strongly hard-soft banded and highly siliceous, grey-black fossiliferous mudstone and marl.|
7861|Gull Rock Member|70722|5|Briefly described|p218|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.||Unit of Blanche Point Formation.||Overlain by Perkana Member. Underlain by Tuketja Member.||
7861|Gull Rock Member|73188|6|Mentioned|p320|Late Eocene|Late Eocene|St Vincent Basin.||Blanche Point Formation||||
7874|Gumbowie Arkose|22510|4|Described|p40, table1|||Intertongues with the Pepuarta Tillite.  Age: Marinoan. Nackara Arc.||||||13-OCT-04
7874|Gumbowie Arkose|23818|5|Briefly described|p64 Fig.22|Neoproterozoic|Neoproterozoic|Of the Yerelina Sub-Group.||||||
7874|Gumbowie Arkose|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
7874|Gumbowie Arkose|34535|6|Mentioned|Fig.22|||||||||
7874|Gumbowie Arkose|37461|5|Briefly described|p342|||See also Table 5.I||||||
7874|Gumbowie Arkose|38110|1|Redefined|p2|Adelaidean|Adelaidean|||||||
7874|Gumbowie Arkose|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
7874|Gumbowie Arkose|41405|4|Described|p200|||||||||
7874|Gumbowie Arkose|41500|6|Mentioned|Fig.1|||||||||
7874|Gumbowie Arkose|42098|5|Briefly described|p54|||||||||
7874|Gumbowie Arkose|42109|5|Briefly described|Fig.1 P19|||||||||
7874|Gumbowie Arkose|42222|6|Mentioned|p18|||||||||
7874|Gumbowie Arkose|42542|5|Briefly described|p8|||||||||
7874|Gumbowie Arkose|42720|5|Briefly described|map legend|Marinoan||||||||
7874|Gumbowie Arkose|42813|5|Briefly described|p21|||of Yerelina Subgroup||||||
7874|Gumbowie Arkose|43052|5|Briefly described|p192,Table 6.1|||Of Yerelina Subgroup.||||||30-SEP-08
7874|Gumbowie Arkose|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Arkosic sandstone.||||||14-MAY-07
7874|Gumbowie Arkose|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
7874|Gumbowie Arkose|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||Yerelina Subgroup||Overlies Enorama Shale; underlies Pepuarta Tillite.||26-APR-12
7874|Gumbowie Arkose|68241|6|Mentioned|p20 Fig.1|||||||||
7874|Gumbowie Arkose|69019|4|Described|p51-52.|Neoproterozoic|Neoproterozoic|Defined by Mirams (in Thomson et al.,1964) as 'arkosic sandstone'; type section W of Gumbowie Siding where it is 75 m thick.||Unit in Yerelina Subgroup.||Conformably overlies Fortress Hill Formation; is overlain conformably by Mount Curtis Tillite.|White to off-white, medium- to coarse-grained, lenticular bedded arkosic sandstone; locally pebbly and cross-bedded.|
7874|Gumbowie Arkose|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||Of Yerelina Subgroup.|||White to off-white, medium- to coarse-grained, lenticular bedded arkosic sandstone; locally pebbly and cross-bedded.|23-JAN-19
7874|Gumbowie Arkose|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Sandstone, arkosic.|
7874|Gumbowie Arkose|73227|6|Mentioned|p36|||Adelaide Superbasin. May have been a lateral fluid conduit.||||||
7982|Hallett Cove Sandstone|9124|5|Briefly described|Map Legend|Pliocene|Pliocene|Marine sands, sandy limestones.||||||07-APR-05
7982|Hallett Cove Sandstone|22541|5|Briefly described|p 36, 37, Table 1|||||||||
7982|Hallett Cove Sandstone|23418|6|Mentioned|p14 Fig.4|||||||||
7982|Hallett Cove Sandstone|23489|4|Described|p44|Pliocene|Pliocene|Of Ochre Cove Formation - note: this seems incorrect?||||||23-JUN-08
7982|Hallett Cove Sandstone|23818|5|Briefly described|p174|Pliocene|Pliocene|Geological Province: St. Vincent Basin.||||||
7982|Hallett Cove Sandstone|30014|6|Mentioned|p28|||||||||
7982|Hallett Cove Sandstone|30807|6|Mentioned|p101|||Suggested map symbol||||||
7982|Hallett Cove Sandstone|31655|6|Mentioned|Table 1|||Geology & hydrology||||||
7982|Hallett Cove Sandstone|31919|6|Mentioned|p33|||U.Pliocene||||||
7982|Hallett Cove Sandstone|31923|6|Mentioned|p17|||||||||
7982|Hallett Cove Sandstone|33330|4|Described|p167|||Upper Pliocene.||||||23-JUN-08
7982|Hallett Cove Sandstone|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
7982|Hallett Cove Sandstone|33423|6|Mentioned|p14|||Stratigraphy.||||||
7982|Hallett Cove Sandstone|34295|6|Mentioned|p39|||Pliocene. Fauna||||||
7982|Hallett Cove Sandstone|34536|6|Mentioned|Map legend|Pliocene|Pliocene|Equiv.||||||
7982|Hallett Cove Sandstone|35097|6|Mentioned|p30|||||||||
7982|Hallett Cove Sandstone|35689|6|Mentioned|Plate 7|||||||||
7982|Hallett Cove Sandstone|36127|6|Mentioned|p7|||||||||
7982|Hallett Cove Sandstone|36500|6|Mentioned|Fig.4|||||||||
7982|Hallett Cove Sandstone|38068|6|Mentioned|Fig.7|||||||||
7982|Hallett Cove Sandstone|38107|4|Described|p37|||||||||
7982|Hallett Cove Sandstone|38605|6|Mentioned|p30|||||||||
7982|Hallett Cove Sandstone|38699|6|Mentioned|p24|||||||||
7982|Hallett Cove Sandstone|38700|6|Mentioned|p38|||||||||
7982|Hallett Cove Sandstone|38873|4|Described|p29|||||||||
7982|Hallett Cove Sandstone|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7982|Hallett Cove Sandstone|39352|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
7982|Hallett Cove Sandstone|39522|6|Mentioned|p85|||||||||
7982|Hallett Cove Sandstone|39631|6|Mentioned|p2|||||||||
7982|Hallett Cove Sandstone|40003|5|Briefly described|Table 11|||See also p47 and Table 12.||||||23-JUN-08
7982|Hallett Cove Sandstone|40217|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
7982|Hallett Cove Sandstone|40238|6|Mentioned|Fig.1|||||||||
7982|Hallett Cove Sandstone|40442|6|Mentioned|p28|||||||||
7982|Hallett Cove Sandstone|40453|5|Briefly described|p58|||||||||
7982|Hallett Cove Sandstone|40877|6|Mentioned|Fig.3|||||||||
7982|Hallett Cove Sandstone|41025|5|Briefly described|Fig.1|||||||||
7982|Hallett Cove Sandstone|41495|6|Mentioned|p44|||||||||
7982|Hallett Cove Sandstone|41513|6|Mentioned|p40|||||||||
7982|Hallett Cove Sandstone|41520|5|Briefly described|Fig.6|||||||||
7982|Hallett Cove Sandstone|41521|6|Mentioned|p241|||||||||
7982|Hallett Cove Sandstone|42498|6|Mentioned|Map Legend|Pliocene|Pliocene|||||||
7982|Hallett Cove Sandstone|42506|5|Briefly described|Map legend|Pliocene||Age: Tertiary.||||||23-JUN-08
7982|Hallett Cove Sandstone|42731|5|Briefly described|map legend|Pliocene||||||||
7982|Hallett Cove Sandstone|42732|5|Briefly described|map legend|Pliocene||||||||
7982|Hallett Cove Sandstone|42733|5|Briefly described|map legend|Tertiary||||||||
7982|Hallett Cove Sandstone|42966|6|Mentioned|p178|||||||||
7982|Hallett Cove Sandstone|43052|5|Briefly described|Table 2.1|||||||||
7982|Hallett Cove Sandstone|44133|4|Described|p67, 170|Pliocene|Pliocene|Overlies Cape Jervis Formation. Geological Province: Saint Vincent Basin. Thickness: 4m+. Overlies and intertongues with Dry Creek Sand. Underlies Burnham Limestone.||||||23-JUN-08
7982|Hallett Cove Sandstone|44198|2|Defined|p21|Pliocene|Pliocene|||||||
7982|Hallett Cove Sandstone|44199|14|Not recorded|p594, 595, 597|Pliocene|Pliocene|U.L.Plio.-L.M.Pliocene.||||||
7982|Hallett Cove Sandstone|44200|6|Mentioned|p.354, 355|||||||||
7982|Hallett Cove Sandstone|44691|4|Described|map legend||Pliocene|(I/53-12). Pliocene.||||||
7982|Hallett Cove Sandstone|48788|14|Not recorded|Not recorded|||||||||
7982|Hallett Cove Sandstone|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Marine fossiliferous limestone and calcareous sandstone.||||||
7982|Hallett Cove Sandstone|60958|5|Briefly described|Map Legend|Pliocene|Pliocene|Red-brown calcareous sandstone and siltstone, sandy limestone. Geological Province: Saint Vincent Basin.||||||
7982|Hallett Cove Sandstone|61108|5|Briefly described|map legend|Pliocene|Pliocene|Marine fossiliferous limestone and calcareous sandstone.||||||
7982|Hallett Cove Sandstone|61121|5|Briefly described|Map legend|Pliocene|Pliocene|Red-brown calcareous sandstone and siltstone, sandy limestone, oyster-rich bed with gastropods and bivalves 'Anodontia'.  Geological  Province: St. Vincent Basin.||||||06-JUN-05
7982|Hallett Cove Sandstone|64282|5|Briefly described|Map legend|Pliocene|Pliocene|Geological Province: St Vincent Basin. Red-brown calcareous sandstone and siltstone; sandy limestone; oyster-rich bed with gastropods and bivalves (Anodontia).||||||24-JUL-08
7982|Hallett Cove Sandstone|65375|4|Described|p34 Fig.7, p37.|Pliocene|Pliocene|Thickness varies locally from 3m to 30m. Locally capped with calcrete.||||Unconformably overlies Port Willunga Formation. Is unconformably overlain by Hindmarsh Clay or soil. On southern Wardang Island, overlies Cape Jervis Formation and Wardang Volcanics Member.|Transgressive,red-brown calcareous sandstone and sandy limestone; locally contains an oyster-bed with gastropods, bivalves and other fossils.|
7982|Hallett Cove Sandstone|65921|6|Mentioned|p2 (map legend)|Tertiary|Tertiary|||||||
7982|Hallett Cove Sandstone|66131|6|Mentioned|p242 Fig.2|Pliocene|Pliocene|Late Pliocene.||||||
7982|Hallett Cove Sandstone|67462|5|Briefly described|Map legend.|Neogene|Neogene|Saint Vincent Basin.||||Is overlain by Point Ellen Formation and Burnham Limestone.||
7982|Hallett Cove Sandstone|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|St Vincent Basin. Late Miocene Maximum age.||||||
7982|Hallett Cove Sandstone|70660|5|Briefly described|p3, p9-p10, p12, p21 fig 11c, p32, p46|Pliocene|Pliocene|||||Overlies the Port Willunga Formation. Overlain by the Burnham Limestone.|Calcareous sandstone and sands, sometimes conglomeratic, with large bivalves and gastropods and other invertebrates.|
7982|Hallett Cove Sandstone|72450|5|Briefly described|Brochure map|Pliocene|Pliocene||||||Calcareous fossiliferous sandstone.|
7982|Hallett Cove Sandstone|73107|5|Briefly described|Map legend.|Pliocene|Pliocene||||||Red-brown calcareous sandstone and siltstone, sandy limestone, oyster-rich beds with gastropods and bivalves; Anodontia.|
7982|Hallett Cove Sandstone|73188|5|Briefly described|[See comments]|Pliocene|Pliocene|St Vincent Basin. Marine environment. p: 319-320, 322, 336, 345-346, 350-351, 356-359.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
7982|Hallett Cove Sandstone|73236|4|Described|p36, p38, p42-43, p46, p48|Pliocene|Pliocene|Coastal sediments. Deposited in littoral zone. Fossils include bivalves such as oysters, and the large, multi-chambered foraminifer Marginopora.|c. 5-2 Ma|||Disconformably underlain by Cape Jervis Formation. Overlain by Ochre Cove Formation.|Calcareous sandstone with bivalve and large foraminiferal fossils.|
8159|Hawker Group|7931|5|Briefly described|p99 Fig. 2|Early Cambrian|Early Cambrian|Unconformably overlies the Wilpena Group - represented in figure as HG.||||||07-FEB-11
8159|Hawker Group|22631|6|Mentioned|p178|Cambrian|Cambrian|||||||
8159|Hawker Group|22766|4|Described|Fig.2 p561, p561||Tommotian|||||||
8159|Hawker Group|22772|5|Briefly described|Table 13.1|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|22857|5|Briefly described|Tb 13.1 (insert p70), p90 Fig. 14.7B|Early Cambrian|Early Cambrian|Of the Morolana Supergroup [missp. of Moralana]. Age: <545Ma. Geological Province: Arrowie Basin. See also p92, p404 App.1 Tb.A1.4.||||||04-MAY-10
8159|Hawker Group|22858|5|Briefly described|p92,Fig14.7bp90-1||Early Cambrian|||||||
8159|Hawker Group|22921|5|Briefly described|37|||Underlain by Wilpena Group.||||||12-FEB-07
8159|Hawker Group|22949|5|Briefly described|p27|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|23178|6|Mentioned|Fig.1||Cambrian|||||||
8159|Hawker Group|23211|5|Briefly described|Fig.1,2||Cambrian|||||||
8159|Hawker Group|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 2-4 of Early Cambrian. Correlate of Andamooka Limestone, Arumbera Sandstone and Todd River Dolomite.||||||
8159|Hawker Group|23282|6|Mentioned|p95|||||||||
8159|Hawker Group|23287|6|Mentioned|Fig.2,3|||Age: Lower Cambrian.||||||
8159|Hawker Group|23315|5|Briefly described|p346|Cambrian|Cambrian|||||||
8159|Hawker Group|23351|6|Mentioned|283|||||||||
8159|Hawker Group|23731|6|Mentioned|p20, p28, p72|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|23818|5|Briefly described|p51 Fig.16|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||
8159|Hawker Group|23825|5|Briefly described|p253|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
8159|Hawker Group|23830|5|Briefly described|Fig. 2|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
8159|Hawker Group|23981|5|Briefly described|p18, p19|||Fossiliferous marine carbonate, siltstone and sandstone. Disconformably overlies Uratanna Formation; disconformably overlain by Billy Creek Formation (Lake Frome Group).||||||
8159|Hawker Group|24176|5|Briefly described|p27|Middle Cambrian|Middle Cambrian|Intruded by Nantawarrinna Diapir.||||||
8159|Hawker Group|24321|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|24334|5|Briefly described|p48 Tb.1|Early Cambrian|Early Cambrian|Age: 530 - 545 Ma||||||
8159|Hawker Group|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
8159|Hawker Group|24484|6|Mentioned|p800|||||||||
8159|Hawker Group|24586|5|Briefly described|p51 Fig. 1|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Includes Parachilna and Uratanna Formations. Geological Province: Adelaide Geosyncline.||||||05-JUL-06
8159|Hawker Group|29780|6|Mentioned|p47|||||||||
8159|Hawker Group|29929|6|Mentioned|Fig.1|||||||||
8159|Hawker Group|30028|6|Mentioned|Fig.4|||||||||
8159|Hawker Group|30051|6|Mentioned|Fig.12|||See also Fig.1. Lower Cambrian age.||||||
8159|Hawker Group|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|30378|6|Mentioned|p431|||Lower Cambrian age||||||
8159|Hawker Group|30544|5|Briefly described|p49|||Early Cambrian age||||||
8159|Hawker Group|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
8159|Hawker Group|30802|4|Described|p11|||Cambrian age||||||
8159|Hawker Group|31022|6|Mentioned|Fig. 4|||||||||
8159|Hawker Group|31321|6|Mentioned|p14|||L. Cambrian. Mineral deposits.||||||
8159|Hawker Group|31322|6|Mentioned|p23|||L. Cambrian. Limestone deposits||||||
8159|Hawker Group|31344|6|Mentioned|p2|||||||||
8159|Hawker Group|31730|6|Mentioned|p99|||Geochem. Stream sediment sampling.||||||
8159|Hawker Group|31797|6|Mentioned|Fig. 2|||L.Cambrian||||||
8159|Hawker Group|31923|6|Mentioned|p10|||||||||
8159|Hawker Group|32504|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|32547|4|Described|p60|||L.Camb.||||||
8159|Hawker Group|32720|6|Mentioned|Table 1|||L.Camb.||||||
8159|Hawker Group|32722|6|Mentioned|Fig.3|||Stromatolite. L.Camb.||||||
8159|Hawker Group|33004|6|Mentioned|p138|||||||||
8159|Hawker Group|33210|6|Mentioned|Fig.1|||||||||
8159|Hawker Group|33474|6|Mentioned|Fig.3|||||||||
8159|Hawker Group|33490|6|Mentioned|p11|||Stratigraphy||||||
8159|Hawker Group|33932|4|Described|p14|||||||||
8159|Hawker Group|33934|4|Described|Fig.2|||L. Camb.||||||
8159|Hawker Group|33954|6|Mentioned|p97|||L.Camb.  See also Fig.4||||||
8159|Hawker Group|33972|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|33973|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|34185|6|Mentioned|p129|||||||||
8159|Hawker Group|34202|6|Mentioned|p1058|||Cambrian Formations||||||
8159|Hawker Group|34291|6|Mentioned|Fig.5|||||||||
8159|Hawker Group|34535|6|Mentioned|Fig.16|||Cambrian||||||
8159|Hawker Group|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|34612|6|Mentioned|p85|||Lower Cambrian. Correlation chart. Fig.33||||||
8159|Hawker Group|34718|5|Briefly described|p13|||||||||
8159|Hawker Group|34812|6|Mentioned|Table 9|||||||||
8159|Hawker Group|34836|6|Mentioned|p70|||||||||
8159|Hawker Group|34957|6|Mentioned|p396|||||||||
8159|Hawker Group|35255|6|Mentioned|Fig.7|||||||||
8159|Hawker Group|35395|6|Mentioned|p102|||Stratigraphy||||||
8159|Hawker Group|35582|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|35835|6|Mentioned|p201|||||||||
8159|Hawker Group|35954|6|Mentioned|p1229|||See also Fig.2.||||||
8159|Hawker Group|36083|6|Mentioned|Table 1|||||||||
8159|Hawker Group|36137|4|Described|p5|||||||||
8159|Hawker Group|36198|6|Mentioned|p249|||See also Fig.I.2||||||
8159|Hawker Group|36495|6|Mentioned|p117|||||||||
8159|Hawker Group|36622|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|36731|5|Briefly described|p124|||||||||
8159|Hawker Group|36898|6|Mentioned|Fig.4|||||||||
8159|Hawker Group|37461|6|Mentioned|Table 5.I|||||||||
8159|Hawker Group|37501|6|Mentioned|p415|||||||||
8159|Hawker Group|37572|6|Mentioned|p165|||||||||
8159|Hawker Group|37802|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|37932|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|38004|6|Mentioned|p82|||||||||
8159|Hawker Group|38068|6|Mentioned|Fig.4|||||||||
8159|Hawker Group|38157|6|Mentioned|Table 1|||||||||
8159|Hawker Group|38329|6|Mentioned|p201|||||||||
8159|Hawker Group|38704|6|Mentioned|p133|||||||||
8159|Hawker Group|39210|6|Mentioned|Table 3|||||||||
8159|Hawker Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8159|Hawker Group|39349|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8159|Hawker Group|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8159|Hawker Group|39490|6|Mentioned|Fig.1(6)|||||||||
8159|Hawker Group|40003|5|Briefly described|Table 16|||||||||
8159|Hawker Group|40254|6|Mentioned|Fig.7|||||||||
8159|Hawker Group|40294|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|40431|6|Mentioned|p12|||||||||
8159|Hawker Group|40672|6|Mentioned|p2|||||||||
8159|Hawker Group|40763|5|Briefly described|p206|||||||||
8159|Hawker Group|40831|6|Mentioned|p2|||||||||
8159|Hawker Group|40852|6|Mentioned|p32|||||||||
8159|Hawker Group|40856|5|Briefly described|p312|||||||||
8159|Hawker Group|40906|6|Mentioned|Fig.9|||||||||
8159|Hawker Group|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8159|Hawker Group|41005|6|Mentioned|p418|||||||||
8159|Hawker Group|41236|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|41401|5|Briefly described|p32|||||||||
8159|Hawker Group|41402|5|Briefly described|p41|||||||||
8159|Hawker Group|41457|6|Mentioned|p1|||||||||
8159|Hawker Group|41496|6|Mentioned|p52|||||||||
8159|Hawker Group|41526|6|Mentioned|p11|||||||||
8159|Hawker Group|41794|6|Mentioned|Fig.2|||||||||
8159|Hawker Group|41996|6|Mentioned|Fig.1 P5|||||||||
8159|Hawker Group|42011|6|Mentioned|Fig.2 P457|||||||||
8159|Hawker Group|42028|6|Mentioned|Fig.1 P136|||||||||
8159|Hawker Group|42090|6|Mentioned|p25|||||||||
8159|Hawker Group|42141|6|Mentioned|Table 2 P571|||||||||
8159|Hawker Group|42167|6|Mentioned|Fig.2 P115|||||||||
8159|Hawker Group|42192|6|Mentioned|p14|||||||||
8159|Hawker Group|42213|5|Briefly described|p471|||See also Fig.2||||||
8159|Hawker Group|42222|4|Described|p20|||||||||
8159|Hawker Group|42225|6|Mentioned|Fig.4 P224|||||||||
8159|Hawker Group|42226|5|Briefly described|p231|||See also Table 1||||||
8159|Hawker Group|42233|6|Mentioned|p249|||||||||
8159|Hawker Group|42239|6|Mentioned|Fig.2 P151|||||||||
8159|Hawker Group|42240|6|Mentioned|Fig.2 P165|||||||||
8159|Hawker Group|42266|6|Mentioned|Fig.2 P292|||||||||
8159|Hawker Group|42269|6|Mentioned|p335|||||||||
8159|Hawker Group|42272|6|Mentioned|p414|||||||||
8159|Hawker Group|42357|5|Briefly described|p10|||||||||
8159|Hawker Group|42458|5|Briefly described|p698|||||||||
8159|Hawker Group|42465|5|Briefly described|Map Legend|||||||||
8159|Hawker Group|42469|6|Mentioned|p25|||||||||
8159|Hawker Group|42546|5|Briefly described|Map legend|Cambrian||||||||
8159|Hawker Group|42573|5|Briefly described|Fig.1 P190|||||||||
8159|Hawker Group|42736|5|Briefly described|map legend|Cambrian||||||||
8159|Hawker Group|42763|5|Briefly described|Fig.2 P21|||||||||
8159|Hawker Group|42779|5|Briefly described|Table 1 P287|||||||||
8159|Hawker Group|42882|5|Briefly described|Table 1 P3|||Of Moralana Supergroup.||||||12-FEB-07
8159|Hawker Group|43011|6|Mentioned|Table 2,p12|||||||||
8159|Hawker Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone.||||||25-MAY-05
8159|Hawker Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
8159|Hawker Group|43298|6|Mentioned|Map Legend||Cambrian|||||||
8159|Hawker Group|43622|6|Mentioned|p37-38|Early Cambrian||||||||
8159|Hawker Group|43759|6|Mentioned|p452|||||||||
8159|Hawker Group|43845|5|Briefly described|Fig2 p42||Early Cambrian|||||||12-JUL-16
8159|Hawker Group|44133|5|Briefly described|p20, 27, 30|||Geological Province: Arrowie Basin.||||||
8159|Hawker Group|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
8159|Hawker Group|44660|14|Not recorded|map legend||Early Cambrian|L.Cambrian.||||||
8159|Hawker Group|45102|6|Mentioned|p43|||See also P47||||||
8159|Hawker Group|60418|5|Briefly described|p133|Early Cambrian|Early Cambrian|Carbonate dominated. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
8159|Hawker Group|60718|5|Briefly described|p48 Fig. 1|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||13-FEB-08
8159|Hawker Group|60889|4|Described|p246-7, p251, p253-4|Early Cambrian|Early Cambrian|Thickness: 3,400 m in Nepabunna region (trough) and continuously thinning westward; 42m in Moorowie-1. Fossils largely restricted to lower part. Arrowie Basin. Constituents continued: Nepabunna Siltstone, Bunker Sandstone, Narina Greywacke.|||Parachilna, Mernmerna (lower, upper), Bendieuta, Moorowie Formations; Woodendinna Dolomite; Ajax, Wilkawillina (lower, middle, upper), Wirrapowie Limestones; Midwerta, Oraparinna Shales. see Comments.||Carbonate-dominated sedimentation. Fractured, vuggy dolomites form potential reservoirs.|21-SEP-17
8159|Hawker Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||
8159|Hawker Group|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Moralana Supergroup.||||||
8159|Hawker Group|60990|5|Briefly described|p83 Fig.2|Botoman|Atdbanian||||Parachilna, Mernmerna Formations; Ajax, Wirrapowie, Wilkawillina Limestones; Woodendinna Dolomite; Narina Greywacke; Bunkers Sandstone; Oraparinna Shale.|||
8159|Hawker Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate; minor basinal sandstone. Geological Province: Arrowie Basin.||||||
8159|Hawker Group|61732|5|Briefly described|p51|Cambrian|Cambrian|Overlies lower part pf Wonoka Formation.||||||07-FEB-11
8159|Hawker Group|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Early Cambrian|Palaeomagnetic data.||||||10-FEB-09
8159|Hawker Group|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, p59.|Early Cambrian|Early Cambrian|Colour scheme shown for interpretation of Curnamona seismic sections. Produces dominant, persistent seismic reflections with well-defined top and base.||Basal unit in Moralana Supergroup.|Includes Parachilna and Mern Merna Formations; Woodendinna Dolomite; Wirrapowie and Wilkawillina Limestones and Oraparinna Shale.|Disconformably overlies Wilpena Group. Is overlain by Billy Creek Formation.|Carbonate dominated, including archaeocyathan limestone.|
8159|Hawker Group|62664|5|Briefly described|p138 Fig.2.|Cambrian|Early Cambrian|||||Unconformably overlies Wilpena Group of Heysen Supergroup.|Siltstone, carbonates, sandstone.|
8159|Hawker Group|62724|5|Briefly described|p22|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||07-FEB-11
8159|Hawker Group|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Includes Wilkawillina Limestone, Mernmerna Formation, Bunkers Sandstone and Oraparinna Shale. Overlies Neoproterozoic Pound Group.|||Includes Wilkawillina Limestone, Mernmerna Formation, Bunkers Sandstone and Oraparinna Shale.|Overlies Neoproterozoic Pound Group.||20-MAR-12
8159|Hawker Group|63447|5|Briefly described|p962, p964 |Early Cambrian|Early Cambrian||||Includes Moorowie Formation, Wilkawillina Limestone, Mernmerna Formation, Parara Limestone, Oraparinna Shale, Uratanna Formation, Parachilna Formation, Bunkers Sandstone, Narina Greywacke.|Overlain by Billy Creek Formation.||
8159|Hawker Group|63458|6|Mentioned|p897 Fig.19. |Cambrian|Cambrian|||||Overlies Wilpena Group.||
8159|Hawker Group|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Fossiliferous limestone, shale and sandstone.||||||10-SEP-07
8159|Hawker Group|63569|6|Mentioned|pp117-119, p136|Early Cambrian|Early Cambrian|Arrowie Basin.|||Includes Wilkawillina Limestone, Mernmerna Formation, Bunkers Sandstone and Oraparinna Shale.|||
8159|Hawker Group|64455|6|Mentioned|p138 Fig. 1|||Includes Parachilna Formation.||||||29-JAN-09
8159|Hawker Group|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
8159|Hawker Group|65313|6|Mentioned|p578 Fig. 6|Cambrian|Cambrian|Flinders Ranges area.|||Includes Parachilna Formation, Wilkawillina Limestone, Bunkers Sandstone, Oraparinna Shale.|Underlies Billy Creek Formation.||26-MAR-12
8159|Hawker Group|65375|5|Briefly described|p33.|Cambrian|Cambrian|Correlative with Normanville Group.|||Includes Uratanna, Parachilna, Mernmerna Formations; Woodendinna Dolomite; Lower Wilkawillina Limestone; Bunkers Sandstone; Oraparinna Shale and Narina Greywacke.|||
8159|Hawker Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
8159|Hawker Group|65379|5|Briefly described|p643|||Of Moralana Supergroup, includes Ajax Limestone. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
8159|Hawker Group|65892|5|Briefly described|p8, p9 Fig.4, p11. |Early Cambrian|Early Cambrian|Arrowie Basin. Carbonate dominated. Fossils are largely restricted to the lower part of the succession. Also includes Bunkers Sandstone; Nepabunna Siltstone; Narina Geywacke.|||Includes Parachilna, Bendieuta, Mernmerna and Moorowie Formations; Ajax, Wirrapowie and Wilkawillina Limestones; Woodendinna Dolomite; Midwerta and Oraparinna Shales; and others: see Comments.|||
8159|Hawker Group|65925|5|Briefly described|Appendix 2.||||||||Limestone, siltstone, shale; lesser sandstone, greywacke.|
8159|Hawker Group|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.|||Includes Wilkawillina Limestone, Mernmerna and Moorowie Formations.|||
8159|Hawker Group|67030|6|Mentioned|p412 Fig. 7, p413 Tab. 2|Ediacaran|Ediacaran|Magnetic information presented for comparison (Klootwijk 1980).||||||
8159|Hawker Group|67484|6|Mentioned|p294 Tb.1|Cambrian|Cambrian|Adelaide Rift Complex.||||Overlies Pound Subgroup (Wilpena Group).||
8159|Hawker Group|67536|5|Briefly described|Map Legend|Drumian|Ediacaran||ca. 564 +/- 61 Ma - 526 +/- 4 Ma||||Marine shelf to basinal carbonate, minor basal sandstone and tuff.|
8159|Hawker Group|67620|6|Mentioned|p5|Cambrian|Cambrian|Adelaide Rift Complex.||||Overlies Rawnsley Quartzite (Pound Subgroup).||
8159|Hawker Group|67870|5|Briefly described|p5, p9-10, p13, p15, p17, p20-21, p23-25|Cambrian|Cambrian|See also p29-30, p32-34. Arrowie Basin. Source of the bituminous hydrocarbons recovered from this unit; potential reservoir.|||Parachilna Formation, Wilkawillina Limestone.||Sandstone, siltstone, limestone, dolostone.|
8159|Hawker Group|67979|6|Mentioned|p530 Fig.1|Cambrian|Cambrian|Cambrian sediments||||overlies Wilpena Group||
8159|Hawker Group|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges.|||Includes Mernmerna Limestone, Wilkawillina Limestone, Woodendinna Dolomite, Parachilna Formation and Uratanna Formation.|Underlain by Pound Subgroup and Wilpena Group.||
8159|Hawker Group|68713|5|Briefly described|p19|Early Cambrian|Early Cambrian||||Includes the Western Spur Limestone.|||
8159|Hawker Group|68735|5|Briefly described|p231, p232, p234, p235 Fig.3, p238, p239|Early Cambrian|Early Cambrian|Arrowie Basin.  Also includes these constituents: Nepabunna Siltstone; Narina Greywacke; Bunkers Sandstone. The top of this Group can be correlated with the Parara Limestone, Koolywurtie Member, and the top of the Normanville Group. Dominated by a complex succession of mainly shelf carbonates and subordinate clastics.|||Ajax, Wilkawillina, Wirrapowie Limestones; Oraparinna, Midwerta Shales; Bendieuta, Mernmerna, Parachilna, Moorowie Formations;  and Woodendinna Dolomite. See Comments for other constituents.|Is overlain by Billy Creek Formation.||10-APR-17
8159|Hawker Group|68993|5|Briefly described|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin. Also includes Wilkawillina Limestone, Upper; Wilkawillina Limestone, Lower; and Woodendinna Dolomite.|||Includes Ajax and Wirrapowie Limestones; Narina Greywacke; Oraparinna and Midwerta Shales; Moorowie, Mernmerna, Parachilna, and Bendieuta Formations; Bunkers Sandstone; Nepabunna Siltstone.|||28-JUL-15
8159|Hawker Group|69019|5|Briefly described|p61, p66-69, p144.|Early Cambrian|Early Cambrian|Arrowie Basin. A carbonate-dominated succession with 3 depositional cycles. Undeformed in this map area.||Unit in Moralana Supergroup.|Includes Uratanna Formation and Western Spur Limestone.|||
8159|Hawker Group|69570|5|Briefly described|p421, p423|Cambrian|Cambrian|Arrowie Basin, northern Flinders ranges. Bradoriids are sampled from a stratigraphic section in this unit (Moro) which is located 5km south of Moro Gorge on the north-eastern limb of the Arrowie Syncline.||||||
8159|Hawker Group|69666|6|Mentioned|p27 Fig.3|Phanerozoic|Phanerozoic|||||||
8159|Hawker Group|69982|6|Mentioned|p15|Early Cambrian|Early Cambrian|Same age as Mooracoochie Volcanics.||||||
8159|Hawker Group|70031|6|Mentioned|p250|||487+\-5 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||||||
8159|Hawker Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Early Cambrian|Early Cambrian|||Of Moralana Supergroup.||||
8159|Hawker Group|70790|6|Mentioned|p258|Early Cambrian|Early Cambrian||~530-525 Ma.|||||
8159|Hawker Group|70833|4|Described|p176,178,184,186,190,200,203,205|Series 2|Terreneuvian|Of Arrowie Basin. Represents approximately 4200 m of carbonate-dominated formations cropping out in broad synclinal tracts in the central part of the Arrowie Basin. Equivalent to sequence set E1 of Gravestock, 1995.|||Includes Iraparinna Shale, Mernmerna Formation, Bunkers Sandstone, Ajax Lst, Wilkawillina and Wirrapowie limestones, Woodendinna Dolostone, and Parachilna Formation.|Overlain by Billy Creek Formation. Underlain disconformably by Uratanna Formation.||
8159|Hawker Group|70835|6|Mentioned|p333-337, 340|Cambrian|Cambrian|Flinders Ranges, Arrowie Basin. Contains new taxa of helcionelloid molluscs. Deposition occurred in a variety of intracratonic shelf environments: carbonate shoals and bioherm complexes, slope deposits, and basinal facies. Deformed during the Ross-Delamerian and Petermann Orogenies.|||Wilkawillina Limestone, Mernmerna Formation, Bunkers Sandstone, Oraparinna Shale.|||
8159|Hawker Group|71102|6|Mentioned|p249|||Of Arrowie Basin.||||||
8159|Hawker Group|72429|4|Described|p949, p951, p954, p958, p966-977|Cambrian|Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Widely mapped and described at a regional scale across the Flinders Ranges sector of the Arrowie Basin. Significantly thinner across the Moorowie Syncline compared with the 885m composite section in the Moorowie area and thick succession exposed along the Adelaide Rift axis. Previously explored for hydrocarbons. Intersected in the Moorowie 1 drill hole.|||Includes the Wilkawillina Limestone,  Mernmerna Formation, Moorowie Formation, Oraparinna Shale|Underlies the Billy Creek Formation. Unconformably overlies Brachina Formation, faulted against Tapley Hill Formation.|Dominated by a complex interplay of shallow-marine carbonates with adjacent marine-trough lithofacies, overprinted by silty-to-arenaceous siliciclastics shed from cratons in the hinterlands, or from emergent salt domes.|
8159|Hawker Group|73222|6|Mentioned|p5-6, p11, p16, p23-24|Cambrian|Early Cambrian|Adelaide Rift Complex.||Moralana Supergroup||||
8159|Hawker Group|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.|||Moorowie Formation, Mernmerna Formation, Wilkawillina Limestone|Unconformably overlain by Billy Creek Formation.||
8159|Hawker Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
8214|Heatherdale Shale|22531|6|Mentioned|p15|||||||||
8214|Heatherdale Shale|22581|6|Mentioned|Fig.2,p37|||Of the Normanville Group.  In the Kanmantoo Basin. Overlies Fork Tree Limestone. Overlain by Truro Volcanics.||||||12-FEB-07
8214|Heatherdale Shale|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
8214|Heatherdale Shale|22671|6|Mentioned|p848||Early Cambrian|Underlies the Kanmantoo Group. Max Age: 526 (+/-) 4 Ma.||||||18-JAN-06
8214|Heatherdale Shale|22755|6|Mentioned|p556|||||||||
8214|Heatherdale Shale|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|Age of unit 526+/-4 Ma.||||||15-JAN-08
8214|Heatherdale Shale|22830|6|Mentioned|P25|||||||||
8214|Heatherdale Shale|22857|5|Briefly described|p94|Early Cambrian|Early Cambrian|Age: 526+/-6Ma (SHRIMP zircon). ||||||
8214|Heatherdale Shale|22858|6|Mentioned|p94||Early Cambrian|Max Age: 526 (+/-) 6 Ma.||||||
8214|Heatherdale Shale|23309|5|Briefly described|p27,45|||||||||
8214|Heatherdale Shale|23539|5|Briefly described|p 467|||||||||
8214|Heatherdale Shale|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
8214|Heatherdale Shale|23827|5|Briefly described|p260|Cambrian|Cambrian|||||||
8214|Heatherdale Shale|23854|5|Briefly described|p864|||Of Normanville Group.||||||
8214|Heatherdale Shale|23981|4|Described|p8-9 Fig. 4, p10 Fig. 5, p26|Early Cambrian|Early Cambrian|Supersedes Heatherdale Shales. Of Normanville Gp. Pyritic, calcareous shale and siltstone. Ages: 526+/4Ma, and 526+/-1.6Ma. Lower part is 300m thick. Geol.Prov: Stansbury Basin. Over Fork Tree Lst; interfingers with Truro Volca; overlain by Carrickalinga.||||||04-FEB-08
8214|Heatherdale Shale|24465|6|Mentioned|p358|Early Cambrian|Early Cambrian|Of Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
8214|Heatherdale Shale|30051|6|Mentioned|Fig.1|||||||||
8214|Heatherdale Shale|30052|6|Mentioned|Fig.3|||Cambrian age.||||||
8214|Heatherdale Shale|30377|5|Briefly described|p202|||Lower Cambrian age||||||
8214|Heatherdale Shale|30378|6|Mentioned|p432|||||||||
8214|Heatherdale Shale|30381|6|Mentioned|Fig.4|||||||||
8214|Heatherdale Shale|30801|6|Mentioned|p5|||Lower Cambrian. Table p5-6.||||||12-FEB-07
8214|Heatherdale Shale|30805|6|Mentioned|p1|||||||||
8214|Heatherdale Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
8214|Heatherdale Shale|32547|6|Mentioned|p60|||L.Camb. Equiv. Unit of Hawker Gp.||||||12-FEB-07
8214|Heatherdale Shale|32551|5|Briefly described|p100|||Cambrian lithology.||||||15-JAN-08
8214|Heatherdale Shale|33224|6|Mentioned|Fig.37|||Photo.||||||
8214|Heatherdale Shale|33332|4|Described|p10|||See also pp 12 and 15. Lower Cambrian.||||||15-JAN-08
8214|Heatherdale Shale|33471|5|Briefly described|p555|||||||||
8214|Heatherdale Shale|33953|6|Mentioned|Fig.4|||Cambrian||||||
8214|Heatherdale Shale|34014|5|Briefly described|p23|||Cambrian||||||
8214|Heatherdale Shale|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Equiv.||||||
8214|Heatherdale Shale|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian||||||
8214|Heatherdale Shale|35255|6|Mentioned|Fig.8|||||||||
8214|Heatherdale Shale|36731|6|Mentioned|p125|||||||||
8214|Heatherdale Shale|38873|6|Mentioned|Table 2|||||||||
8214|Heatherdale Shale|39489|6|Mentioned|p8|||||||||
8214|Heatherdale Shale|39806|5|Briefly described|p207|||||||||
8214|Heatherdale Shale|40442|5|Briefly described|p16|||Also mention on Table 1.||||||
8214|Heatherdale Shale|40454|6|Mentioned|Table 1|||||||||
8214|Heatherdale Shale|40455|5|Briefly described|p69|||||||||
8214|Heatherdale Shale|40763|5|Briefly described|p206|||||||||
8214|Heatherdale Shale|40852|6|Mentioned|p33|||||||||
8214|Heatherdale Shale|40856|5|Briefly described|p312|||||||||
8214|Heatherdale Shale|41103|6|Mentioned|p261|||||||||
8214|Heatherdale Shale|41526|6|Mentioned|p39|||See also p61||||||12-FEB-07
8214|Heatherdale Shale|41853|6|Mentioned|p195|||See also p199.||||||12-FEB-07
8214|Heatherdale Shale|42192|6|Mentioned|p7|||||||||
8214|Heatherdale Shale|42222|6|Mentioned|p21|||||||||
8214|Heatherdale Shale|42225|6|Mentioned|Fig.4 P224|||||||||
8214|Heatherdale Shale|42232|6|Mentioned|p283|||||||||
8214|Heatherdale Shale|42266|5|Briefly described|p291|||||||||
8214|Heatherdale Shale|42268|6|Mentioned|p330|||||||||
8214|Heatherdale Shale|42270|5|Briefly described|p353|||See also Fig.3||||||
8214|Heatherdale Shale|42272|5|Briefly described|p404|||||||||
8214|Heatherdale Shale|42488|4|Described| 185, Fig.2 P187|||||||||
8214|Heatherdale Shale|43190|5|Briefly described|Fig.2p29,p34.|||U-Pb zircon age in tuff bed at Sellicks Hill: 526 +/-4 Ma. Of Normanville Group.||||||15-JAN-08
8214|Heatherdale Shale|43192|6|Mentioned|p63|||Of the Normanville Group.||||||12-FEB-07
8214|Heatherdale Shale|43560|6|Mentioned|Table 1,p231||Botoman|Age: 526+/-4 Ma (Early Cambrian).||||||12-FEB-07
8214|Heatherdale Shale|43703|6|Mentioned|p75||Botoman|||||||
8214|Heatherdale Shale|43759|4|Described|p446||Early Cambrian|||||||
8214|Heatherdale Shale|43781|6|Mentioned|p3|||||||||
8214|Heatherdale Shale|44133|5|Briefly described|p4 Fig. 7.2, 6, 14|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group.||||||
8214|Heatherdale Shale|50154|5|Briefly described|p58|Early Cambrian|Early Cambrian|Age: 524 +/- 6 Ma (U/Pb). Of the Normanville Group.||||||
8214|Heatherdale Shale|60567|5|Briefly described|p41|||Of the upper part of the Normanville Group.||||||
8214|Heatherdale Shale|60712|5|Briefly described|p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||
8214|Heatherdale Shale|61307|5|Briefly described|p6 Fig. 3, p23|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Adelaide Fold Belt.||||||15-JAN-08
8214|Heatherdale Shale|63848|4|Described|p531, p532, p533 Fig.2, p534 Fig.4.|Early Cambrian|Early Cambrian|Dated by a tuff in its upper part by Cooper et al. (1992) at 526 +/- 4 Ma; recalculated by Jenkins et al.|522.0 +/- 2.1 Ma (Jenkins et al. 2002).|Unit in Normanville Group.||Overlies Fork Tree Limestone. Is overlain by Carrickalinga Head Formation.|Mainly pale- to dark-grey laminated phyllite with interbedded lava (including pillow lava), tuffs, and volcaniclastic sediments.|
8214|Heatherdale Shale|64571|6|Mentioned|p828|Early Cambrian|Early Cambrian|Age: 526+/-4Ma (SHRIMP). SA.||||||15-DEC-08
8214|Heatherdale Shale|65375|5|Briefly described|p33, p55.|Early Cambrian|Early Cambrian|Stansbury Basin, Yorke Peninsula. Possible hydrocarbon source rock (TOC max. = 2.43%, mean = 0.64%).||Unit in Normanville Group.||Overlies Fork Tree Limestone.||
8214|Heatherdale Shale|65379|5|Briefly described|p643, p644, p646|Cambrian|Cambrian|Of Normanville Group, Moralana Supergroup. Shales; limestone with rare trilobites, hyoliths, sponge spicules, gastropods and worm tracks. N.B. Asbestos deposit host, contains Dutton 2 asbestos prospect.||||||07-MAR-12
8214|Heatherdale Shale|65664|5|Briefly described|p1096, p1103|Early Cambrian|Early Cambrian||Tuff dated at 522 +/ - 2 Ma.|Of Normanville Group.||||09-MAY-12
8214|Heatherdale Shale|65686|5|Briefly described|p420||Cambrian|Stansbury Basin.|522 +/- 2 Ma from tuff horizon.|||Overlain unconformably by Kanmantoo Group.||07-MAY-12
8214|Heatherdale Shale|65892|4|Described|p9 Fig.4, p15, p17, p19. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. Age from a tuff bed; recalculated from 526 +/- 4 Ma (Cooper et al., 1992). Rare fossils include hyoliths, helcionellids, lingulate brachiopods and arthropods. Trace fossils locally abundant.|522 +/- 2 Ma (Pb-U SHRIMP; Jenkins et al., 2002).|Unit in Normanville Group.||Conformably overlies Fork Tree Limestone. Is disconformably overlain by Carrickalinga Head Formation.|Lower calcareous member and an upper black shale and siltstone unit; nodules and stringers of black phosphate common locally.|
8214|Heatherdale Shale|66623|5|Briefly described|p430.|||||||Is overlain by Carrickalinga Head Formation.|Well-bedded and laminated muddy limestones and calcareous siltstones and mudstones.|
8214|Heatherdale Shale|66761|5|Briefly described|p254|Cambrian|Cambrian|Deepwater shale. Fleurieu Peninsula. Younger than Fork Tree Limestone, older than Kanmantoo Group.||||||14-MAR-12
8214|Heatherdale Shale|67344|5|Briefly described|p264|Cambrian|Cambrian|~335m thick. Deposited in a more distal, outer ramp setting. Age defined by the partly contemporaneous Emu Bay Shale.|||||Succession of dark grey calcareous shale and siltstone, variously pyritic and rich in nodular phosphate.|
8214|Heatherdale Shale|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Of the Normanville Group.||||
8214|Heatherdale Shale|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
8214|Heatherdale Shale|70125|6|Mentioned|p400 Tb.5||||526 Ma (tuff: Haines and Flottmann, 1998).|||||
8214|Heatherdale Shale|70660|5|Briefly described|p35, p37-p40, p46|Early Cambrian|Early Cambrian|This unit is in unconformable contact with the Port Willunga Formation [however the author doesn't state what their relationship is].||||Overlies the Christies Beach Formation. Unconformably overlain by the Port Willunga Formation.||
8214|Heatherdale Shale|70744|6|Mentioned|p941|||Delamerian Orogen. Contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga).||||||
8214|Heatherdale Shale|70833|5|Briefly described|p200,202|Cambrian|Cambrian|Of Eastern Stansbury Basin. Deepwater facies, recording relatively slow continuous basinal depositional cycles. Includes D. odyssei and M. etheridgei zones in the upper and lower parts of the section respectively. Equivalent to Parara Limestone, and Mernmerna Formation and Ajax Limestone (D. odessei zone), and to Wilkawillina (Hideaway Well and Winnitinny Creek members) and Wirrapowie limestones (M. etheridgei zone).||||Overlain unconformably by Kanmantoo Group. Underlain by Fork Tree Limestone.||
8214|Heatherdale Shale|71102|6|Mentioned|p254|||Of Stansbury Basin.||||||
8214|Heatherdale Shale|71593|5|Briefly described|p22|||||||Overlain by the Kanmantoo Group.||
8214|Heatherdale Shale|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Dark grey, slaty siltstone with black phosphate nodules.|
8214|Heatherdale Shale|73059|6|Mentioned|p1061|||||Normanville Group.||||
8214|Heatherdale Shale|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Pyritic, calcareous shale and siltstone; thin tuff bed.|09-DEC-21
8214|Heatherdale Shale|73188|5|Briefly described|p315-316, p336-338, p353, p356, p358|Early Cambrian|Early Cambrian|Mount Lofty Ranges. Extensional tectonism commenced during deposition.||Normanville Group||Disconformably overlain by Kanmantoo Group.|Carbonaceous siltstone.|
8214|Heatherdale Shale|73247|6|Mentioned|p205|Cambrian (Stage 4)|Cambrian (Stage 3)|Fleurieu Peninsula.||||Underlain by Fork Tree Limestone. Unconformably overlain by Kanmantoo Group.||
8214|Heatherdale Shale|73264|6|Mentioned|p1387 Fig.10|||||Normanville Group||||
8214|Heatherdale Shale|73430|5|Briefly described|p492||||514.98+/-0.22 Ma (Betts et al., 2018)|Normanville Group|||Thin-bedded turbidites.|
8214|Heatherdale Shale|74367|5|Briefly described|p19|Early Cambrian|Early Cambrian|Age revised from 526+/-4 Ma (COOPER et al., 1992), which was revised to 522+/-2 Ma (Jenkins et al., 2002) and later revised by Betts et al., (2018).|514.98+/-0.22 Ma U-Pb SHRIMP zircon|Normanville Group, top||Stratigraphically equivalent to Mernmerna Formation.||
8219|Heathfield Sandstone Member|22674|5|Briefly described|Fig.2 p719|Albian|Albian|||||||
8219|Heathfield Sandstone Member|24551|5|Briefly described|p251||Albian|||||||
8219|Heathfield Sandstone Member|24562|5|Briefly described|p6|||Geological Province: Otway Basin.||||||
8219|Heathfield Sandstone Member|41269|5|Briefly described|p245|||||||||
8219|Heathfield Sandstone Member|41642|6|Mentioned|Table 7.4|||||||||
8219|Heathfield Sandstone Member|41726|6|Mentioned|p422|||||||||
8219|Heathfield Sandstone Member|42152|6|Mentioned|Fig.2 P4|||||||||
8219|Heathfield Sandstone Member|42827|5|Briefly described|Table 7.4|||||||||
8219|Heathfield Sandstone Member|61329|6|Mentioned|p121|||||||||
8219|Heathfield Sandstone Member|63124|5|Briefly described|p70|||Of the Eumeralla Formation and in wide usage, but not yet formally defined. No designated type section. Geological Province: Otway Basin.||||||
8219|Heathfield Sandstone Member|70077|5|Briefly described|Regional: Fig.4|Albian|Aptian|Otway Basin: Robe-Penola Trough.||Eumeralla Formation.||||
8219|Heathfield Sandstone Member|72050|6|Mentioned|p243|||Is described as ""a member of the Eumeralla Formation"" but is given the formal rank only on p243. A possible reservoir target in the Tantanoola Trough. See references to Heathfield Sandstone on p233 Fig.2, 235-236, 238.||||||
8311|Heytesbury Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Eocene|||||||
8311|Heytesbury Group|22626|6|Mentioned|446 fig 10|Early Miocene|Early Miocene|Geol province West Otway Basin. Overlying unit Naracoorte Limestone Member, underlying unit Gambier Limestone||||||
8311|Heytesbury Group|22674|5|Briefly described|p718, Fig.2 p719|Late Miocene|Early Oligocene|||||||
8311|Heytesbury Group|22875|4|Described|p65-72, p26-27, p59, 135, 149-151|Late Miocene|Early Oligocene|Age: ~7-29 Ma. Apatite fission track ages: 7.9+/-1.3 Ma, 6.2+/-2.3 Ma||||||19-SEP-18
8311|Heytesbury Group|22938|6|Mentioned|p233|||||||||
8311|Heytesbury Group|22944|5|Briefly described|Fig3|Miocene|Oligocene|||||||
8311|Heytesbury Group|23226|5|Briefly described|p889|||Separated from Murray basin by Padthaway Ridge Paleozoic Basement. of Gambier Basin.||||||26-JUN-13
8311|Heytesbury Group|23230|4|Described|Table4-1p40, 42, 44|Miocene|Eocene|||||||
8311|Heytesbury Group|23249|5|Briefly described|p143 Fig.2||Miocene|Of Otway Basin.||||||24-JUL-08
8311|Heytesbury Group|23307|5|Briefly described|Map Legend|Miocene|Miocene|||||||
8311|Heytesbury Group|23322|5|Briefly described|957 Fig.2|Miocene|Oligocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
8311|Heytesbury Group|23417|6|Mentioned|p6|||||||||
8311|Heytesbury Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
8311|Heytesbury Group|23792|5|Briefly described|p26|Recent|Eocene|Carbonates and siliciclastics. Geological Province: Otway Basin||||||26-JUN-13
8311|Heytesbury Group|23939|6|Mentioned|Fig.5|||May be Late Oligocene to Middle Miocene in age.||||||
8311|Heytesbury Group|24056|5|Briefly described|p84, p87|||Geological Basin: Otway Basin.||||||
8311|Heytesbury Group|24200|5|Briefly described|p423 Fig. 15, 16.|||Heytesbury Group Equivalents discussed throughout text.||||||
8311|Heytesbury Group|24314|5|Briefly described|p60, p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24323|5|Briefly described|p136 Fig. 3|Miocene|Oligocene|Unconformably overlies the Nirranda Group. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24344|5|Briefly described|p69|Miocene|Oligocene|||||||
8311|Heytesbury Group|24551|5|Briefly described|p246|Miocene|Oligocene|Consists of: Clifton Formation, Gellibrand Marl, Port Campbell Limestone.||||||
8311|Heytesbury Group|24562|5|Briefly described|p8, 35 Fig. 2|Miocene|Oligocene|Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24563|6|Mentioned|p485|Tertiary|Tertiary|||||||
8311|Heytesbury Group|29355|6|Mentioned|p179|||||||||
8311|Heytesbury Group|29823|5|Briefly described|p14|||||||||
8311|Heytesbury Group|29856|6|Mentioned|p41|||||||||
8311|Heytesbury Group|30522|6|Mentioned|Map legend|Miocene|Oligocene|Oligo-Miocene||||||
8311|Heytesbury Group|30576|5|Briefly described|Table 2|||||||||
8311|Heytesbury Group|30578|6|Mentioned|p9|||||||||
8311|Heytesbury Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
8311|Heytesbury Group|30928|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
8311|Heytesbury Group|30932|6|Mentioned|Map legend|Tertiary|Tertiary|Equivalent Glenelg Group and Nirranda Group in part.||||||
8311|Heytesbury Group|31036|1|Redefined|p210|late Tertiary|middle Tertiary|Middle to Late Tertiary. See also Table 19-1.||||||
8311|Heytesbury Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
8311|Heytesbury Group|31534|6|Mentioned|p369|||See also Table 19-3||||||
8311|Heytesbury Group|31625|6|Mentioned|Fig. 5.2|||Oligocene-Miocene||||||
8311|Heytesbury Group|31746|6|Mentioned|p194|||||||||
8311|Heytesbury Group|32162|6|Mentioned|p58|||See also Fig. 5||||||
8311|Heytesbury Group|32499|6|Mentioned|p107|||Miocene||||||
8311|Heytesbury Group|33135|5|Briefly described|p17|||||||||
8311|Heytesbury Group|33230|6|Mentioned|Encl.12.1|||Olig. - Miocene||||||
8311|Heytesbury Group|33807|6|Mentioned|p97|||||||||
8311|Heytesbury Group|33940|6|Mentioned|p414|||||||||
8311|Heytesbury Group|34063|6|Mentioned|p2|||Olig.-Mioc. Table||||||
8311|Heytesbury Group|34954|6|Mentioned|Fig.35|||||||||
8311|Heytesbury Group|35013|6|Mentioned|p393|||||||||
8311|Heytesbury Group|35066|4|Described|p208|||p221.||||||31-JAN-07
8311|Heytesbury Group|35262|6|Mentioned|p4|||||||||
8311|Heytesbury Group|35271|6|Mentioned|p66|||||||||
8311|Heytesbury Group|35274|6|Mentioned|p423|||||||||
8311|Heytesbury Group|35285|6|Mentioned|p414|||||||||
8311|Heytesbury Group|35290|6|Mentioned|p38|||||||||
8311|Heytesbury Group|35722|6|Mentioned|p4|||Stratigraphy.||||||
8311|Heytesbury Group|36499|6|Mentioned|p43|||||||||
8311|Heytesbury Group|36913|6|Mentioned|p79|||||||||
8311|Heytesbury Group|37385|6|Mentioned|p9|||||||||
8311|Heytesbury Group|37548|6|Mentioned|p131|||||||||
8311|Heytesbury Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
8311|Heytesbury Group|38625|6|Mentioned|p272|||||||||
8311|Heytesbury Group|38717|5|Briefly described|p20|||||||||
8311|Heytesbury Group|39315|6|Mentioned|Fig.7|||||||||
8311|Heytesbury Group|39967|6|Mentioned|p44|||||||||
8311|Heytesbury Group|41016|5|Briefly described|Mention|||||||||
8311|Heytesbury Group|41043|6|Mentioned|p97|||||||||
8311|Heytesbury Group|41185|5|Briefly described|p175|||||||||
8311|Heytesbury Group|41269|5|Briefly described|p246|||||||||
8311|Heytesbury Group|41487|5|Briefly described|p625|||||||||
8311|Heytesbury Group|41701|6|Mentioned|Map legend|early Miocene||||||||
8311|Heytesbury Group|41704|6|Mentioned|p100|||||||||
8311|Heytesbury Group|41714|6|Mentioned|p301|||||||||
8311|Heytesbury Group|41726|6|Mentioned|p421|||||||||
8311|Heytesbury Group|41769|5|Briefly described|p30|||||||||
8311|Heytesbury Group|41868|5|Briefly described|p535|||||||||
8311|Heytesbury Group|42075|5|Briefly described|Fig.13 P252|||||||||
8311|Heytesbury Group|42152|6|Mentioned|Fig.2 P4|||||||||
8311|Heytesbury Group|42184|6|Mentioned|Fig.2 P348|||||||||
8311|Heytesbury Group|42318|6|Mentioned|p8|||||||||
8311|Heytesbury Group|42453|6|Mentioned|p20|||||||||
8311|Heytesbury Group|42524|5|Briefly described|Fig.3 P27|||||||||
8311|Heytesbury Group|42827|4|Described|p282|||see also Fig 8.10||||||
8311|Heytesbury Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
8311|Heytesbury Group|43171|6|Mentioned|2-8|Middle Miocene|Late Oligocene|Age 10-30 Ma||||||
8311|Heytesbury Group|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map.||||||
8311|Heytesbury Group|43208|5|Briefly described|map legend|Late Miocene|Oligocene|Of Middle Oligocene to Late Miocene age.||||||24-JUL-08
8311|Heytesbury Group|43219|5|Briefly described|Fig.3,p6.|Miocene|Oligocene|||||||
8311|Heytesbury Group|43590|4|Described|p23|||||||||
8311|Heytesbury Group|43604|6|Mentioned|p144,Fig.1|Miocene|Oligocene|||||||
8311|Heytesbury Group|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
8311|Heytesbury Group|43686|5|Briefly described|p233|||||||||
8311|Heytesbury Group|43733|6|Mentioned|Fig.2.11,p65|Pliocene|Miocene|||||||
8311|Heytesbury Group|43744|6|Mentioned|Fig.3,p3|||||||||
8311|Heytesbury Group|43783|6|Mentioned|Fig14, p11|Neogene|Late Oligocene|||||||
8311|Heytesbury Group|43784|6|Mentioned|Fig10, p12|Neogene|Late Oligocene|||||||
8311|Heytesbury Group|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
8311|Heytesbury Group|44133|5|Briefly described|p156|Middle Miocene|Late Eocene|Geological Province: Gambier Basin. Includes: Gambier Limestone, Gellibrand Marl.||||||04-FEB-08
8311|Heytesbury Group|44135|6|Mentioned|p49|Miocene|Late Oligocene|Mentioned in the context of correlates.||||||07-DEC-09
8311|Heytesbury Group|44186|5|Briefly described|Map Legend||Miocene|||||||
8311|Heytesbury Group|46802|6|Mentioned|Table 1|||||||||
8311|Heytesbury Group|48581|4|Described|p37|||See also p12,13,28,39. Fig.4,6,7,Pl.1,2. (J54-12/Port Campbell).||||||
8311|Heytesbury Group|48911|3|Fully described|p26|Late Eocene|Miocene|||||||03-JUL-06
8311|Heytesbury Group|48977|6|Mentioned|p1,p2|||See also P59, Table 3||||||
8311|Heytesbury Group|49060|5|Briefly described|Fig.33|||||||||
8311|Heytesbury Group|50154|5|Briefly described|p26, p135|||Geological Province: Otway Basin. Includes: Clifton Formation, Gellibrand Marl and Port Campbell Limestone.||||||
8311|Heytesbury Group|60421|5|Briefly described|p408 Fig. 1, 409|Oligocene|Upper Eocene|Overlies: Wangerrip Group. Includes: Gellibrand Marl, Clifton Formation, Port Campbell Formation.||||||31-JAN-07
8311|Heytesbury Group|60451|5|Briefly described|p95 Fig. 61|||||||||
8311|Heytesbury Group|60538|5|Briefly described|p470, 473 Fig. 12, 474 Fig. 13|Miocene|Late Oligocene|Limestone, marl, littoral deposits. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|60563|5|Briefly described|p45|Miocene|Oligocene|Mostly carbonates. Includes Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|60581|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||
8311|Heytesbury Group|60582|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||
8311|Heytesbury Group|60583|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||23-NOV-04
8311|Heytesbury Group|60584|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||23-NOV-04
8311|Heytesbury Group|60585|5|Briefly described|p29|Middle Miocene|Late Oligocene|Includes: Clifton Formation, Gellibrand Marl, Port Campbell Limestone.||||||
8311|Heytesbury Group|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Includes: Clifton Formation, Gellibrand Marl, and Port Campbell Limestone.  Consists of littoral to deep marine bryozoan carbonates and clastics. Geological Province: Otway Basin.||||||03-MAR-10
8311|Heytesbury Group|61182|4|Described|p24, p27-28, p36|Late Miocene|Late Oligocene|Comprises Clifton Fm, Gellibrand Marl and Port Campbell Lst; Hanson Plain Sand has been included by some authors; excluded here. Mostly shelf carbonates and only minor terrigenous sediments. Max. thick: 698m. Disconformable over Nirranda Gp. Age: 29-5Ma. ||||||
8311|Heytesbury Group|61185|5|Briefly described|p58|||Marine sediments. Geological Province: Otway Basin.||||||07-FEB-11
8311|Heytesbury Group|61528|6|Mentioned|p827|||||||||
8311|Heytesbury Group|61547|6|Mentioned|pp461-462. |Miocene|Eocene|||||Overlies Nirranda Group.||
8311|Heytesbury Group|61607|6|Mentioned|p5 Fig. 2|Cenozoic|Oligocene|Geological Province: Otway Basin.||||||12-MAR-09
8311|Heytesbury Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
8311|Heytesbury Group|61622|4|Described|p436, p437, p436 Fig. 2|Miocene|Eocene|Includes Gellibrand Marl and Gambier Limestone. Geological Province: Otway Basin. Thin marls and carbonates deposited in mid to inner shelf environment.||||||07-FEB-11
8311|Heytesbury Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes; Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61624|5|Briefly described|p465, p466, p466 Fig. 2, p467, p469|Miocene|Oligocene|Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61626|5|Briefly described|p487, p486 Fig. 2, p489 Fig. 6, p493|Miocene|Oligocene|Includes; Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Includes Compton Conglomerate, Gellibrand Marl and Gambier Limestone. Geological Province: Otway Basin.||||||07-FEB-11
8311|Heytesbury Group|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Early Oligocene|Includes; Clifton Formation, Gellibrand Marl, Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61841|5|Briefly described|p242|Eocene|Paleocene|Dominantly marine limestone and marl.  Geological Province: Otway Basin.||||||03-JUL-06
8311|Heytesbury Group|62370|6|Mentioned|p464 Fig.12|||Marine carbonates.||||||
8311|Heytesbury Group|62896|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
8311|Heytesbury Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
8311|Heytesbury Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Early Miocene|Late Eocene|Includes Gambier Limestone, Compton Conglomerate and Gellibrand Marl. Geological Province: Otway Basin. ||||||
8311|Heytesbury Group|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29|Miocene+|Late Eocene|Incl: Gambier Limestone, Compton Conglomerate and Gellibrand Marl. In Otway Basin/ Gambier Basin. Group name - previously used for the Victorian Clifton Formation, Gellibrand Marl and Port Campbell Limestone, of which only G.Marl occurs in South Australia||||||
8311|Heytesbury Group|63125|6|Mentioned|p103|||Geological Province: Otway Basin||||||
8311|Heytesbury Group|63173|5|Briefly described|p342 Fig. 9.2|Recent|Late Oligocene|Geological Province: Otway Basin, offshore.||||||07-FEB-11
8311|Heytesbury Group|63269|5|Briefly described|p604-605|Miocene|Oligocene|Otway Basin.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone.|Unconformably overlies Nirranda Group. Is overlain unconformably by Hanson Plain Sand.||
8311|Heytesbury Group|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Includes Gambier Limestone and Gellibrand Marl.||||||07-FEB-11
8311|Heytesbury Group|63446|5|Briefly described|Map legend|Miocene|Miocene||||||Marine: calcarenite, marl, silt.|
8311|Heytesbury Group|65316|6|Mentioned|p598|||In the Otway Basin.|||Includes the Clifton Formation.|||23-APR-12
8311|Heytesbury Group|65715|4|Described|p14 Tb.8, p16|Miocene|Oligocene|Includes Gellibrand Marl and Clifton Formation. Called Heytesbury Formation by Baker (1950). In Port Campbell Embayment. Marine.||||||
8311|Heytesbury Group|66002|5|Briefly described|p10 Tb.7, p12, p13 Tb.9, p16, p26 Fig.7|Neogene|Neogene|Includes Port Campbell Limestone, Gellibrand Marl and Clifton Formation. Defined by Glenie 1971. Modified from Heytesbury Formation of Baker (1950)||||||
8311|Heytesbury Group|66012|4|Described|p4, p6, p10 Tb.1, p17-18, p27, p30 Tb.3|Neogene|Paleogene|Intersected in boreholes. Includes Clifton Formation, Gellibrand Marl & Port Campbell Limestone. Overlies Dilwyn Formation. Underlies Moorabool Viaduct Sand & Newer Volcanic Group. Calcareous quartz sand, sandy limestone, limestone, marl, & calcareous clay. Up to 55m thick| | ||||16-FEB-15
8311|Heytesbury Group|66245|5|Briefly described|p6 Fig.5, p8. |Messinian|Rupelian|Coastal and shallow marine, progradational sequence of carbonates. Helped in building out the present day shelf.|||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|67061|6|Mentioned|p546 Fig.3, p557.|Miocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|67366|6|Mentioned|p103 Fig.2. |Miocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|Unconformably overlies Nirranda Group.||
8311|Heytesbury Group|67367|5|Briefly described|p130, p131 Fig.2. |Oligocene|Oligocene|Carbonates. The unit is relatively thin across most of the inner shelf of the Otway Basin, hence little or no hydrocarbon was generated during the Late Tertiary. Its rapid thickening across the outer shelf has rapidly matured the Austral 2 source rocks (Eumeralla Formation).|||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|68116|5|Briefly described|Appendix, Maps 38-39, 47-48.|Miocene|Oligocene||||||Calcarenite, marl, silt.|
8311|Heytesbury Group|68189|6|Mentioned|p26|||||||||
8311|Heytesbury Group|69297|4|Described|p78, p79, p81, p98, p112, p115, p116|Tortonian|Rupelian|Otway Basin. Coastal plain to open marine siliciclastic and carbonate sediments. Potential seal of the Nirranda and Wangerrip Group reservoirs. |||Includes the Gambier Limestone, Clifton Formation, Gellibrand Marl and the Port Campbell Limestone.|Overlies the Nirranda Group. Unconformably overlain by the Hanson Plain Sand, Coomnandook Formation and the Bridgewater Formation.|Marls and fine-grained limestones.|
8311|Heytesbury Group|69651|5|Briefly described|p6, p10, p12, p33, p38|Miocene|Eocene|Otway Basin. Mixed carbonate/siliciclastic rocks. Carbonates are potential seals. Modelling diagrams.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone.|Unconformably overlies Nirranda Group. Is overlain unconformably by Hanson Plain Sand.|Marls and fine-grained limestone.|
8311|Heytesbury Group|69879|5|Briefly described|p418, p424|Miocene|Oligocene|Strahan Sub-basin, Sorell Basin. Shown as Heytesbury Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Nirranda Group.|Nannofossil ooze/chalk carbonates with quartzitic sand sub-unit. Outer shelf carbonate, including fossiliferous reefal limestone.|
8311|Heytesbury Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough.|||Gambier, Port Campbell Limestones; Gellibrand Marl; Clifton Formation.|Overlies Nirranda Group.||
8311|Heytesbury Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p5|Miocene|Oligocene|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources. Similarly, equivalent marls and fine-grained limestones are potential regional seals, eg to Nirranda and Wangerrip Groups reservoirs.|||Gambier Limestone.|Overlies Nirranda Group. Is overlain by Coomandook Formation.||
8311|Heytesbury Group|70379|6|Mentioned|p724-727|||Otway Basin.||||Overlies Nirranda Group.||
8311|Heytesbury Group|70909|14|Not recorded|p62||Miocene|||||||
8311|Heytesbury Group|71419|6|Mentioned|p22|||Stated in this article to be upgraded from Heytesbury Formation to Group by Glenie (1971). [The Heytesbury Group appears in Baker (1953) Fig.1 p126].||||||02-FEB-18
8311|Heytesbury Group|71437|5|Briefly described|Fig. 1 opp 154, p155, p159|Pliocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl, Port Campbell Limestone, Moorarbool Viaduct Formation.||Limestone-marl-sandy limestone suite.|
8311|Heytesbury Group|71593|5|Briefly described|p51|Miocene|Oligocene|||||||
8311|Heytesbury Group|72445|5|Briefly described|App 1; App.2; App.5; App.6 p1, p3.|Miocene|Oligiocene|Murray and Otway basins. App.2 is a .csv format file. Identified in Stavely 01. A diverse inner to middle shelf benthic foraminiferal assemblage is present. Samples include planktic and benthic foraminifera.|||Includes Port Campbell Limestone and Gellibrand Marl.|Shown as overlying Moornambool Metamorphic Complex with sharp contact, and conformably underlying Wunghnu Group.|Bioturbated silty to sandy marl with lesser mud and shell fragments. Some intervals of cleaner sand.  Sandy to muddy calcareous marl with some muddier sections and abundant shell fragments.|15-OCT-20
8311|Heytesbury Group|73356|6|Mentioned|p3, p16|Miocene|Oligocene|||||Unconformably underlain by Nirranda Group. Unconformably overlain by Bridgewater Formation.|Marine marls and limestones.|
8311|Heytesbury Group|73357|6|Mentioned|p44, p46, p48|Tortonian|Chattian|Otway Basin.|||Includes Clifton Formaiton, Gellibrand Marl, Port Campbell Limestone.|Overlies Nirranda Group, underlies Whalers Bluff Group.||
8311|Heytesbury Group|73383|4|Described|p3, p7 Tb.3.1, p10, p137, p264|Miocene|Oligocene|Otway Basin. Equivalent to chemostratigraphic Sequence S6, primarily defined by high Ca values. Lithologies based on geochemistry using the ChemLith classification includes limestone and calcareous limestone, and using the Herron classification (1988) includes shale and Fe-shale.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group, underlies Bridgewater Formation|Carbonate units including limestones, marls and calcareous mudstones.|
8311|Heytesbury Group|73385|5|Briefly described|p3-5|Miocene|Oligocene|Otway Basin. Overlies regional intra-Oligocene unconformity, underlies late-Miocene unconformity.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Unconformably overlies Nirranda Group, unconformably underlies Bridgewater Formation.|Marine marls and limestones.|
8311|Heytesbury Group|73386|4|Described|p1-2, p4-7, p14, iii, Attachment A1|Tortonian|Chattian|Otway Basin. Covers basin west of the Otway Ranges, thins towards basin margins. Deposited in setting of post-rift subsidence, inversion. Top of Heytesbury Group is an unconformity, marked by uplift, folding and erosion at the end of the Miocene. Overlain by units of Pliocene to Pleistocene age. Contains Middle Proteacidites tuberculatus to Upper Triporopollenites bellus spore-pollen zones, chemostratigraphic sequence S6 of Forbes et al. (2020). Appears as Heystesbury Group p6.|||Port Campbell Limestone, Gellibrand Marl, Clifton Formation|Unconformably overlies Nirranda Group, underlies Bridgewater Formation|Marine marls and limestones.|
8311|Heytesbury Group|73486|5|Briefly described|p510, p511 Fig.2, p528|Miocene|Oligocene|Otway Basin. Represents final megacycle of sediment accumulation in basin.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group, underlies Hanson Plain Sand, Hesse Clay||
8311|Heytesbury Group|73594|5|Briefly described|p4-6|Miocene|Oligocene|Otway Basin. Onshore thickness of 200-400m, up to 1750m thick at the seaward end of the Shipwreck Trough. Erosion of the uppermost part in the late Miocene.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group|Marine marls and limestones.|
8370|Hiltaba Granite|22430|6|Mentioned|p2||Proterozoic|||||||
8370|Hiltaba Granite|24197|5|Briefly described|p30|||Of the Hiltaba Suite (Roxby Downs type). Geological Province: Gawler Craton.||||||07-FEB-11
8370|Hiltaba Granite|29838|6|Mentioned|p6|||||||||
8370|Hiltaba Granite|30809|6|Mentioned|p5|||||||||
8370|Hiltaba Granite|30984|6|Mentioned|p10|||||||||
8370|Hiltaba Granite|33468|5|Briefly described|p204|||Age. See also P205||||||
8370|Hiltaba Granite|33557|6|Mentioned|p32|||||||||
8370|Hiltaba Granite|34904|6|Mentioned|Fig. 1|||||||||
8370|Hiltaba Granite|35107|6|Mentioned|p199|||||||||
8370|Hiltaba Granite|35255|6|Mentioned|p7|||||||||
8370|Hiltaba Granite|36507|6|Mentioned|p117|||||||||
8370|Hiltaba Granite|37461|6|Mentioned|p325|||||||||
8370|Hiltaba Granite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8370|Hiltaba Granite|39901|6|Mentioned|p15|||||||||
8370|Hiltaba Granite|39911|6|Mentioned|p4|||||||||
8370|Hiltaba Granite|39949|5|Briefly described|p271|||||||||
8370|Hiltaba Granite|40241|6|Mentioned|p115|||||||||
8370|Hiltaba Granite|40430|6|Mentioned|p8|||||||||
8370|Hiltaba Granite|40445|6|Mentioned|p54|||||||||
8370|Hiltaba Granite|41125|6|Mentioned|p42|||||||||
8370|Hiltaba Granite|41499|5|Briefly described|Fig.1|||||||||
8370|Hiltaba Granite|41972|6|Mentioned|p364|||||||||
8370|Hiltaba Granite|41974|5|Briefly described|p407|||||||||
8370|Hiltaba Granite|42283|6|Mentioned|p80|||||||||
8370|Hiltaba Granite|42536|6|Mentioned|p3|||Kingoonya bedrock drilling||||||
8370|Hiltaba Granite|42721|5|Briefly described|map legend|Carpentarian||||||||
8370|Hiltaba Granite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Pink leucocratic biotite granite and adamellite, locally porphyritic; scattered aplite and microgranite veins.||||||07-APR-05
8370|Hiltaba Granite|43071|4|Described|p15,Table 2|||Rb/Sr isochron of 1510+/-38 Ma.||||||
8370|Hiltaba Granite|43094|4|Described|p32|||||||||
8370|Hiltaba Granite|43583|6|Mentioned|p2163|||Age: 1600 Ma||||||
8370|Hiltaba Granite|48894|6|Mentioned|p73|||1730my||||||
8370|Hiltaba Granite|50605|5|Briefly described|p(ii), 1.3, 8.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite.||||||
8370|Hiltaba Granite|62978|6|Mentioned|p167|||Age: ~1550Ma. In the Wilgena Domain. Geological Province: Gawler Craton. See also the informal Hiltaba granite.||||||07-FEB-11
8370|Hiltaba Granite|64135|6|Mentioned|p1501, p1504|Mesoproterozoic|Mesoproterozoic|||Unit in Hiltaba Suite.||||26-SEP-14
8370|Hiltaba Granite|69019|6|Mentioned|p29 Fig.9.|||Gawler Craton. Geochemistry is briefly described.||||||
8370|Hiltaba Granite|69023|5|Briefly described|p26|||Gawler Craton. Geochemistry outlined.|||||Includes microgranite.|
8370|Hiltaba Granite|69591|5|Briefly described|p110|||Gawler Craton. Coeval with waning stages of the Isan Orogeny. Coeval with Gawler Range Volcanics.|~1595-1575 Ma.||||Voluminous A-type granites.|
8370|Hiltaba Granite|70334|5|Briefly described|p87|||Geological province: Gawler Craton. May potentially host skarn mineralisation, particularly Pb-Zn skarn associated with Au-Cu mineralisation.||||||
8370|Hiltaba Granite|71235|5|Briefly described|p1|||Potentially a source of Uranium for mineralisation in the Corunna Conglomerate.||||||
8370|Hiltaba Granite|71317|4|Described|p20, p54-p55, p58|||Highly magnetic. Contacts with the Eucarro Rhyolite are well exposed north of Barber Hill and south of Narlaby Well in Peltabinna. Intruded by felsic dykes in the north west of Peltabinna. See also p96, p113, p115, p117, p146, p162, p170, p173/||Hiltaba Suite||Intrudes the Eucarro Rhyolite and the Pondanna Dacite Member.|Leucocratic granite.|
8370|Hiltaba Granite|72459|5|Briefly described|p6-p7, p10, p13, p16-17, p21-22,|Mesoproterozoic|Mesoproterozoic|Potentially identified in magnetics to the west of the Gawler Range Volcanics in the Nuyts Subdomain. Comagmatic with the Gawler Range Volcanics. Appears as Hiltaba granite on p6 and as Hiltaba Granites throughout the text. See also p29, p33, p36-39, p46, p50-51.|ca. 1581 - 1595 Ma|||||
8370|Hiltaba Granite|72462|6|Mentioned|p7|Calymmian|Calymmian|[Written as Hiltaba Granites].||||||
8373|Himalaya Formation|6823|5|Briefly described|p205, 207-208|Palaeoproterozoic|Palaeoproterozoic|U-Pb SHRIMP maximum depositional ages of Love (1992).|1762 +/- 17 Ma; 1793 +/- 22 Ma (Max dep, U-Pb)|Thackaringa Group||||26-MAR-22
8373|Himalaya Formation|22553|5|Briefly described|p75,fig2p77|Statherian|Statherian|Part of Willyama Supergroup.||||||11-JUN-08
8373|Himalaya Formation|22575|6|Mentioned|p179 Fig.2|||Of the Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|22641|5|Briefly described|Fig. 2 p689, p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|22720|6|Mentioned|p 168|||Of the Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|22771|6|Mentioned|Table12.2p45,45|||||||||
8373|Himalaya Formation|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Lateral equivalent of Rasp Ridge Gneiss. Max. thickness: 1000m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
8373|Himalaya Formation|22884|6|Mentioned|p43 Fig. 3|||Of the Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|22965|6|Mentioned|p13, Fig1||Statherian|Part of the Thackaringa Group.||||||
8373|Himalaya Formation|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
8373|Himalaya Formation|22967|6|Mentioned|p39||Statherian|||||||
8373|Himalaya Formation|23025|6|Mentioned|Fig1p75|||||||||
8373|Himalaya Formation|23160|6|Mentioned|fig1|||||||||
8373|Himalaya Formation|23223|5|Briefly described|p39|||Described in article as 'upper albite - Himalaya Formation (UA-HF)'. Within the Willyama Supergroup.||||||16-JAN-07
8373|Himalaya Formation|23248|5|Briefly described|Fig2p169|||||||||
8373|Himalaya Formation|23461|5|Briefly described|p204 Fig. 3|||Of Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|24307|5|Briefly described|p973|Proterozoic|Proterozoic|Of the Thackaringa Group.   Geological Province: Broken Hill Block||||||16-JAN-07
8373|Himalaya Formation|38969|4|Described|p206|||||||||
8373|Himalaya Formation|39662|2|Defined|p420|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39674|6|Mentioned|p204|||||||||
8373|Himalaya Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39849|6|Mentioned|Table 2|||||||||
8373|Himalaya Formation|40290|6|Mentioned|p1|||||||||
8373|Himalaya Formation|40822|6|Mentioned|Fig.2|||||||||
8373|Himalaya Formation|41093|6|Mentioned|p252|||||||||
8373|Himalaya Formation|41145|6|Mentioned|Fig.4|||||||||
8373|Himalaya Formation|41630|6|Mentioned|p45|||||||||
8373|Himalaya Formation|41633|6|Mentioned|p141|||||||||
8373|Himalaya Formation|42261|6|Mentioned|Fig 1 P530|||||||||
8373|Himalaya Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42537|4|Described|p11|||||||||
8373|Himalaya Formation|42595|6|Mentioned|Fig. 2 P5|||||||||
8373|Himalaya Formation|42813|6|Mentioned|p10|||Of Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|42897|5|Briefly described|p323|||see also Fig.3, p321.||||||16-JAN-07
8373|Himalaya Formation|43052|6|Mentioned|Fig.4.22|||||||||
8373|Himalaya Formation|43086|6|Mentioned|Fig.3|||||||||
8373|Himalaya Formation|43264|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
8373|Himalaya Formation|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43267|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43572|6|Mentioned|Fig.3.2 p6|||||||||
8373|Himalaya Formation|46598|5|Briefly described|p303|||||||||
8373|Himalaya Formation|50045|5|Briefly described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Thackaringa Group (Willyama Supergroup). Overlain by Broken Hill Group (Allendale Metasediments); underlain by Cues Formation.||||||31-MAY-07
8373|Himalaya Formation|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Himalaya Suite. Geological Province: Broken Hill Block. Age: 1750-1860Ma (U-Pb). Intruded by Potosi Supersuite.||||||07-NOV-08
8373|Himalaya Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
8373|Himalaya Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
8373|Himalaya Formation|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: <1710+/-5Ma and >1704+/-3Ma (Page et al 2000a,b). Geological Province: Broken Hill-Olary region.||||||07-NOV-08
8373|Himalaya Formation|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|61735|5|Briefly described|p635 Fig. 1, p636 Fig.2,  639|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Ages: </-1710-1700Ma and >1690+/-11Ma. Max depositional age ~1730 Ma, metamorphic age from rutile 1595+/-6 Ma U/Pb SHRIMP.||||||04-JUN-15
8373|Himalaya Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Olary Domain.||||||
8373|Himalaya Formation|62373|6|Mentioned|p508|||||||||
8373|Himalaya Formation|62473|5|Briefly described|p72|Paleoproterozoic|Paleoproterozoic|Age: ca.1710Ma. Thin bedded quartz-albite rocks.||||||17-JUN-09
8373|Himalaya Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1730-c.1720 Ma.|Thackaringa Group.||||
8373|Himalaya Formation|62536|5|Briefly described|p636, 639-642, 655|||Broken Hill area. Metamorphosed at 1595 +/- 6 Ma. Appears only as Himalaya on p636.|~1730 Ma (MDA).|Thackaringa Group.|||Extensive quartz-albite metasedimentary rocks; some with climbing ripples indicate sandstone progenitors.|
8373|Himalaya Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
8373|Himalaya Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group||||15-DEC-21
8373|Himalaya Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
8373|Himalaya Formation|63110|6|Mentioned|p1132|||Albite-rich rocks.||||||11-JUN-08
8373|Himalaya Formation|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: 1710-1700Ma. Mentioned in Abstract also. See also p9, p10 Fig. 3.. ||||||07-NOV-08
8373|Himalaya Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province.|<1704 Ma|Thackaringa Group||||
8373|Himalaya Formation|64097|5|Briefly described|p303, p317|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Ages: ca1798+/-15Ma, 1762+/-17Ma, ca1720Ma (all zircon). Max. age considered to be close to +1730Ma.||||||07-FEB-11
8373|Himalaya Formation|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
8373|Himalaya Formation|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|64742|6|Mentioned|p321 Fig.3. ||||<1710-1700 Ma.|Unit in Thackaringa Group.||||
8373|Himalaya Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Thackaringa Group||Overlies the Cues Formation. Overlain by the Allendale Metasediments.||
8373|Himalaya Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Thackaringa Group.||||
8373|Himalaya Formation|68126|5|Briefly described|p31|Paleoproterozoic|Paleoproterozoic||||||Medium-grained saccharoidal leucocratic psammitic and albitic metasediment. Variably-interbedded albite-quartz rich rocks, composite gneiss, basic gneiss, horizons of thinly-beded quartz-magnetite rock. Pyrite-rich rocks towards bottom.|
8373|Himalaya Formation|70000|5|Briefly described|p34-36|Statherian|Statherian|Hosts cobalt-rich pyritic horizons at Pyrite Hill and Big Hill. Protolith probably sandy marine shelf sediments with variable evaporitic or hypersaline component.||Unit in Thackaringa Group.||Overlies Cues Formation.||
8373|Himalaya Formation|70014|5|Briefly described|Map legend|||Plagioclase-quartz rocks are well-bedded (beds 20 - 30mm thick), with rare scour-and-fill and crossbed structures. Thin to thick (0.5 - 10m) horizons of thinly-bedded quartz-magnetite rock also occur with the plagioclase-quartz rocks. In some areas the Formation consists of thin interbeds of plagioclase-quartz rocks within metasediments or metasedimentary composite gneiss.||Unit in Thackaringa Group.||Overlies Cues Formation. Is overlain by Allendale Metasediments (Broken Hill Group).|Extensive bodies of medium-grained, saccharoidal leucocratic sodic plagioclase-quartz(-K-feldspar)(-biotite) rocks, with variably developed interbedded metasedimentary composite gneiss, and basic gneiss; pyrite-rich rocks occur towards the base.|
8373|Himalaya Formation|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thackaringa Group.||Overlies Cues FZ.|Albite-quartz +/- K feldspar +/- biotite rock, with variably interbedded metasedimentary composite gneiss and basic gneiss; horizons of quartz-magnetite rock; locally pyritic.|
8373|Himalaya Formation|70405|6|Mentioned|p9 table 1, p40|Paleoproterozoic|Paleoproterozoic||1700 Ma|Thackaringa Group||||
8373|Himalaya Formation|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|~1700 Ma.|Thackaringa Group||Overlies Cues Formation. Underlies Allendale Metasediments (Broken Hill Group). Is intruded by Georges Bore Granite Gneiss and Rasp Ridge Granite Gneiss of Silver City Suite.||
8373|Himalaya Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Thackaringa Group.||||
8373|Himalaya Formation|72004|6|Mentioned|p85|||Broken Hill region.||Unit of Thackaringa Group.||Uppermost unit of the Thackaginga Group.||
8373|Himalaya Formation|72461|6|Mentioned|p13, p16-17|||||Thackaringa Group||Overlies the Cues Formation. Overlain by the Allendale Metasediments.||
8373|Himalaya Formation|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Thackaringa Group||Overlies Cues Formation||
8373|Himalaya Formation|73482|6|Mentioned|p422 Fig.3|||||Thackaringa Group||||
8373|Himalaya Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p831 Fig.5|Statherian|Statherian||<1710-1700 Ma, >1690+/-11 Ma|Thackaringa Group||Overlies Cues Formation, underlies Allendale Metasediments||
8381|Hindmarsh Clay|22541|6|Mentioned|Fig 3|||||||||
8381|Hindmarsh Clay|22867|6|Mentioned|P26||Quaternary|||||||
8381|Hindmarsh Clay|22888|6|Mentioned|P36|||||||||
8381|Hindmarsh Clay|23418|6|Mentioned|p14 Fig.4|||||||||
8381|Hindmarsh Clay|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|23719|6|Mentioned|p31|||||||||
8381|Hindmarsh Clay|23818|6|Mentioned|p190 Fig.94|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|23828|5|Briefly described|p94|Recent|Pleistocene|Geological Province: St Vincent Basin.  Maximum thickness: 122m.||||||
8381|Hindmarsh Clay|29367|6|Mentioned|Fig.1|||||||||
8381|Hindmarsh Clay|29395|6|Mentioned|p6|||Pleistocene.||||||
8381|Hindmarsh Clay|29400|6|Mentioned|Fig.2|||Quaternary.||||||
8381|Hindmarsh Clay|29591|6|Mentioned|p103|||||||||
8381|Hindmarsh Clay|29697|6|Mentioned|p51|||||||||
8381|Hindmarsh Clay|30080|6|Mentioned|p2|||||||||
8381|Hindmarsh Clay|30180|6|Mentioned|p116|||||||||
8381|Hindmarsh Clay|30752|6|Mentioned|p3|||Formed in fluviatile environment close to sea level||||||
8381|Hindmarsh Clay|30757|6|Mentioned|p4|||Refers Firman (1966)||||||
8381|Hindmarsh Clay|30807|6|Mentioned|p101|||Suggested map symbol||||||
8381|Hindmarsh Clay|31655|6|Mentioned|Table 1|||Geology & hydrology||||||
8381|Hindmarsh Clay|31708|4|Described|p13|||See also soil sections P14, 15 & Stress dependence of modules P21, 23.||||||
8381|Hindmarsh Clay|31921|6|Mentioned|Fig.3|||||||||
8381|Hindmarsh Clay|32438|6|Mentioned|p42|||||||||
8381|Hindmarsh Clay|33057|5|Briefly described|p8|||Pleistocene. Section P10||||||
8381|Hindmarsh Clay|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
8381|Hindmarsh Clay|33423|6|Mentioned|p14|||Stratigraphy. Shallow acquifer P23.||||||
8381|Hindmarsh Clay|34180|6|Mentioned|p216|||Lower Pleistocene.||||||
8381|Hindmarsh Clay|34181|4|Described|p45|||Pleistocene||||||
8381|Hindmarsh Clay|34295|6|Mentioned|p41|||Pleistocene - Recent. Fauna||||||
8381|Hindmarsh Clay|34308|6|Mentioned|Fig.94|||Pleist.||||||
8381|Hindmarsh Clay|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|35097|6|Mentioned|Fig.4|||||||||
8381|Hindmarsh Clay|35159|6|Mentioned|Fig.2|||||||||
8381|Hindmarsh Clay|35906|6|Mentioned|p5|||See also Fig.2 & Table 1.||||||
8381|Hindmarsh Clay|36500|6|Mentioned|Fig.4|||||||||
8381|Hindmarsh Clay|37853|6|Mentioned|Fig. 2|||||||||
8381|Hindmarsh Clay|38068|6|Mentioned|Fig.8|||||||||
8381|Hindmarsh Clay|38107|4|Described|p46|||See also P19.||||||
8381|Hindmarsh Clay|38602|6|Mentioned|Fig.2|||||||||
8381|Hindmarsh Clay|38605|6|Mentioned|p30|||||||||
8381|Hindmarsh Clay|38700|6|Mentioned|p39|||||||||
8381|Hindmarsh Clay|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
8381|Hindmarsh Clay|39352|6|Mentioned|Map legend|early Pleistocene|early Pleistocene|||||||
8381|Hindmarsh Clay|40003|5|Briefly described|p47|||See also Table 11||||||
8381|Hindmarsh Clay|40219|5|Briefly described|p2|||||||||
8381|Hindmarsh Clay|40442|6|Mentioned|p35|||||||||
8381|Hindmarsh Clay|40453|6|Mentioned|Fig.2|||||||||
8381|Hindmarsh Clay|40502|5|Briefly described|p83|||||||||
8381|Hindmarsh Clay|40926|6|Mentioned|Table 3|||||||||
8381|Hindmarsh Clay|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|40942|4|Described|p20|||||||||
8381|Hindmarsh Clay|41119|6|Mentioned|p5|||||||||
8381|Hindmarsh Clay|41151|4|Described|p9|||||||||
8381|Hindmarsh Clay|41292|6|Mentioned|Fig.1|||||||||
8381|Hindmarsh Clay|41520|5|Briefly described|Fig.5|||||||||
8381|Hindmarsh Clay|41943|5|Briefly described|p72|||||||||
8381|Hindmarsh Clay|42457|6|Mentioned|p163|||||||||
8381|Hindmarsh Clay|42466|6|Mentioned|Map legend|||||||||
8381|Hindmarsh Clay|42475|6|Mentioned|p24|||||||||
8381|Hindmarsh Clay|42498|5|Briefly described|Map legend|late Pleistocene|early Pleistocene|||||||
8381|Hindmarsh Clay|42506|5|Briefly described|Map legend|Pleistocene||||||||
8381|Hindmarsh Clay|42733|5|Briefly described|map legend|Quaternary||||||||
8381|Hindmarsh Clay|44133|4|Described|p220 Fig. 11.2, 241|Pleistocene|Tertiary|Thickness: 70m+. Overlain by: Keswick Clay, Pooraka Formation. Geological Provinces: Saint Vincent and Adelaide Basins. ||||||
8381|Hindmarsh Clay|44660|14|Not recorded|map legend||Pleistocene|Pleistocene, lithology.||||||
8381|Hindmarsh Clay|60958|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Basal gravel layer. Middle mottled red-brown to orange clay and upper fluvial and alluvial red-brown silty sandstone. (correlates to Ardrossan Clay and Sandrock?)||||||
8381|Hindmarsh Clay|61070|6|Mentioned|Map Legend|Quaternary|Quaternary|||||||12-JAN-10
8381|Hindmarsh Clay|61121|5|Briefly described|Map legend|Pleistocene|Pleistocene|Basal gravel layer; middle mottled red-brown to orange clay; upper fluvial to alluvial red-brown silty sandstone. Age: 0.78Ma.||||||
8381|Hindmarsh Clay|61155|5|Briefly described|p6, p17|Pleistocene|Pleistocene|Widespread alluvial fan deposits in Spencer Gulf and Gulf of St Vincent areas. Overlies Carisbrooke Sand and partly over Hallett Cove Sandstone also. Age: <1.0Ma. Geological Province: St Vincent Basin.||||||03-MAR-10
8381|Hindmarsh Clay|62898|5|Briefly described|p198|||Hematite-rich unit.  See also the informally named  "Hindmarsh Clay".||||||
8381|Hindmarsh Clay|64282|5|Briefly described|Map legend|Pleistocene|Pleistocene|Age: 0.78Ma. Basal gravel layer,  middle mottled red-brown to orange clay, and an upper fluvial and alluvial red-brown silty sandstone.  Alluvial, fluvial and lacustrine sediments.||||||24-JUL-08
8381|Hindmarsh Clay|65375|4|Described|pp32-33, p36, pp38-40. |Pleistocene|Pleistocene|Equivalent to the informal names 'Ardrossan Clays and Sandrock' (Tepper 1879), Ardrossan Soil (Daily et al. 1976), Ardrossan Clays (Wilson 1991). Probably deposited in alluvial fan, valley flat, playa lake and fluvial channel settings. Outcrops on east and west coasts of Yorke Peninsula. The breccia unit contains clasts of Winulta and Kulpara Formations.||||Unconformably overlies Winulta Formation, Cape Jervis Formation, North Maslin Sand and Port Willunga Formation. Is unconformably overlain by Bridgewater Formation.|Unconsolidated to semi-consolidated, mottled, mainly red-brown clay and sandy clay with granules and gravels;  massive, unsorted alluvial-fan breccia.|
8381|Hindmarsh Clay|65901|5|Briefly described|p176 Tab.1|||Firman (1967) considers Ngaltinga Clay, Ochre Cove Formation, Kurrajong Formation and Sleaford Formation to be included in Hindmarsh Clay.||||||08-MAR-12
8381|Hindmarsh Clay|66131|6|Mentioned|p242 Fig.2|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|66194|6|Mentioned|p580|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|67462|5|Briefly described|Map legend.||Pliocene|Saint Vincent Basin.||||||
8381|Hindmarsh Clay|68715|6|Mentioned|p31 Fig.5|Piacencian|Piacencian|St Vincent Basin.||||||
8381|Hindmarsh Clay|68811|6|Mentioned|p86|Quaternary||Underlies Quaternary sediments [Saint Kilda Formation, Semaphore Sands]. Aquitard.|||||Highly impermeable clay.|15-APR-20
8381|Hindmarsh Clay|69372|6|Mentioned|p34 fig. 12|Pleistocene|Pleistocene|||||||
8381|Hindmarsh Clay|70334|5|Briefly described|p3,61-62,64,83|Pleistocene|Pleistocene|Of Flinders Ranges, Baroota Plain, Spencer Gulf areas. Thickness: 60-86m in Baroota Plain, thickness uncertain in Spencer Gulf. Does not outcrop on CULTANA, but shown in seismic to be widespread in Spencer Gulf area. Alluvial fan, valley flat and playa lake environments.||||Overlain by Mambray Formation or Telford Gravel.|Consolidated mottled clay and sandy clay with sand and gravel lenses.|14-OCT-19
8381|Hindmarsh Clay|70382|5|Briefly described|p29 Fig 3|Pleistocene|Pleistocene|Yorke Peninsula region.|||||Consolidated mottled clay and sandy clay|
8381|Hindmarsh Clay|70660|6|Mentioned|p40|||||||||
8381|Hindmarsh Clay|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Consolidated mottled clay and sandy clay with sand and gravel lenses, aeolian sand, gypseous and pelletal clay dunes and calcareous palaeosols. Alluvial and colluvial red-brown sandy clay with sand and gravel beds.|
8381|Hindmarsh Clay|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Includes the Brunhes-Matuyama polarity transition (0.78 Ma).||||Equivalent to Ardrossan Clay and Sandrock.|Basal gravel layer. Middle mottled red-brown to orange clay; upper fluvial and alluvial red-brown silty sandstone. Alluvial, fluvial and lacustrine sediments.|
8381|Hindmarsh Clay|73188|5|Briefly described|[See comments]|Pleistocene|Pleistocene|St Vincent Basin, Adelaide-Golden Grove Embayment. May interfinger with Ochre Cove Formation. Interpreted as distal sediments sourced from erosion of the rising Mount Lofty Ranges. Gravel lenses are prominent in some areas, such as at Redbanks. p: 319-320, 322, 331, 345-346, 349-351, 357-359.||||Overlain by Keswick Clay.|Clay-rich with limited coarse clastic input.|
8381|Hindmarsh Clay|73236|4|Described|p36-38, p43, p48|Pleistocene|Pleistocene|Floodplain and lacustrine sediments. Boundary with overlying Keswick Clay is indicated by a subtle but persistent colour change. [Article alludes to an uppermost clay unit; unclear].|c. 2-0.13 Ma|||Underlain by Ochre Cove Formation. Overlain by Keswick Clay.|Blue-grey and red mottled clay and sandy clay; off-white, weakly consolidated sand with strong ferruginous mottling.|
8381|Hindmarsh Clay|73292|6|Mentioned|p954|Middle Pleistocene|Early Pleistocene|Evidence of Cambrian rocks thrust over the Hindmarsh Clay due to Late Pleistocene reverse faulting.||||||
8476|Hooray Sandstone|730|6|Mentioned|p24, p25.|||Fluviatile.||||||11-NOV-14
8476|Hooray Sandstone|8187|5|Briefly described|Map legend|Mesozoic|Mesozoic|Sandstone, siltstone, shale, conglomerate.||||||21-JUN-04
8476|Hooray Sandstone|8217|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone, siltstone, shale, conglomerate.||||||
8476|Hooray Sandstone|9694|5|Briefly described|Map Legend|Cretaceous|Jurassic|Deeply weathered sandstone, feldspathic sandstone, siltstone, basal conglomerate.||||||
8476|Hooray Sandstone|12597|5|Briefly described|p492 Tb.1, p497, p499, p501|Early Cretaceous|Kimmeridgian|Eromanga Basin. 100-200m thick. Coal reported (John, 1985) at top of the Formation in GSQ Wyandra No. 1.||||Equivalent to Murta Member and upper Namur Sandstone Member, and Algebuckina Sandstone.|Interbedded quartzose to sub-labile sandstone and siltstone.|
8476|Hooray Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Late Jurassic|In Eromanga Basin.||||||
8476|Hooray Sandstone|22464|5|Briefly described|p9|Early Cretaceous|Late Jurassic|Eromanga Basin, overlain by Cadna-Owie Formation.||||||16-SEP-08
8476|Hooray Sandstone|22826|6|Mentioned|p576|Early Cretaceous|Late Jurassic|Geological Province - Eromanga Basin.||||||
8476|Hooray Sandstone|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Valanginian|Tithonian|Pale medium to coarse-grained quartzose sandstone. Equivalent of Mooga Sandstone (Surat Basin). Max. thickness: 200m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
8476|Hooray Sandstone|22865|4|Described|p295,Table22.1p296-7|Neocomian|Tithonian|||||||
8476|Hooray Sandstone|22954|6|Mentioned|Fig3p9||Cretaceous|||||||
8476|Hooray Sandstone|23056|4|Described|23|||Geol province Eromanga Basin.||||||16-SEP-08
8476|Hooray Sandstone|23375|4|Described|Fig2 p265, 291|Valanginian|Tithonian|Laterally equivalent to Namur Sandstone and Murta Formation. In the Eromanga Basin.||||||11-MAY-17
8476|Hooray Sandstone|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
8476|Hooray Sandstone|23430|4|Described|p523 + p524 Table 14.7|||Underlain by Westbourne Formation - unconformable. Eromanga Basin Province.||||||26-SEP-06
8476|Hooray Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Jurassic|Geological Province: Great Australian Superbasin.||||||
8476|Hooray Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
8476|Hooray Sandstone|24047|6|Mentioned|p109 Appendix 2|||Geological Province: Eromanga Basin.||||||
8476|Hooray Sandstone|24092|6|Mentioned|p5|||Geological Province: Great Artesian Basin.||||||
8476|Hooray Sandstone|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
8476|Hooray Sandstone|29591|6|Mentioned|p69|||||||||
8476|Hooray Sandstone|30020|6|Mentioned|p33|||||||||
8476|Hooray Sandstone|30021|6|Mentioned|p89|||||||||
8476|Hooray Sandstone|30022|6|Mentioned|p28|||||||||
8476|Hooray Sandstone|30024|6|Mentioned|p331|||||||||
8476|Hooray Sandstone|30102|4|Described|p25|||See also p26,28,29. Upper Jurassic - Lower Cretaceous age.||||||26-SEP-06
8476|Hooray Sandstone|30103|6|Mentioned|p8|||||||||
8476|Hooray Sandstone|30104|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
8476|Hooray Sandstone|30510|6|Mentioned|p103|||||||||
8476|Hooray Sandstone|30691|4|Described|p6|||See also p15-17,20,21,Table 4,6. Jurassic - Cretaceous age||||||26-SEP-06
8476|Hooray Sandstone|30692|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Lower Cretaceous to Upper Jurassic||||||
8476|Hooray Sandstone|30694|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30695|4|Described|Table 4|||Upper Jurassic to Lower Cretaceous age.||||||16-SEP-08
8476|Hooray Sandstone|30699|6|Mentioned|p56|||Map||||||
8476|Hooray Sandstone|30702|6|Mentioned|p48|||See also Fig.1. Stratigraphic table||||||
8476|Hooray Sandstone|30853|5|Briefly described|Table 3|||Upper Jurassic to Cretaceous||||||
8476|Hooray Sandstone|30854|4|Described|Table 4|||Upper Jurassic-Lower Cretaceous age.||||||
8476|Hooray Sandstone|30855|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30856|4|Described|Table 3|||Upper Jurassic-Lower Cretaceous age.||||||
8476|Hooray Sandstone|30857|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic-Lower Cretaceous||||||
8476|Hooray Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
8476|Hooray Sandstone|31097|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|31098|5|Briefly described|Table 1|||U. Jurassic -  L. Cretaceous||||||
8476|Hooray Sandstone|31116|6|Mentioned|p43|||||||||
8476|Hooray Sandstone|31145|5|Briefly described|Table 1|||U. Jurassic - L. Cretaceous||||||
8476|Hooray Sandstone|31244|6|Mentioned|p8|||||||||
8476|Hooray Sandstone|31425|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic to L.Cretaceous||||||
8476|Hooray Sandstone|31430|5|Briefly described|Table 1|||U.Jurassic-L.Cretaceous.||||||
8476|Hooray Sandstone|31431|5|Briefly described|Table 3|||U.Jurassic - L.Cretaceous||||||
8476|Hooray Sandstone|31432|4|Described|Table 1|||U.Jurassic - L.Cretaceous.||||||16-SEP-08
8476|Hooray Sandstone|31436|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31438|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Lower Cretaceous to Upper Jurassic||||||
8476|Hooray Sandstone|31441|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31443|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31553|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|32138|6|Mentioned|p398|||||||||
8476|Hooray Sandstone|32275|6|Mentioned|p8|||Refers Galloway & Senior (1971)||||||
8476|Hooray Sandstone|32314|6|Mentioned|Fig. 4|||||||||
8476|Hooray Sandstone|32490|6|Mentioned|Table 1|||Equivalent Ronlow Beds?||||||
8476|Hooray Sandstone|33017|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|33067|4|Described|Table 1|Early Cretaceous|Late Jurassic|Sublabile sandstone, quartz sandstone, conglomerate.||||||07-JUL-04
8476|Hooray Sandstone|33069|4|Described|p7|||U.Jur. and L.Cret.||||||26-SEP-06
8476|Hooray Sandstone|33071|4|Described|p2|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33072|4|Described|Table 1|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33075|5|Briefly described|p445|||||||||
8476|Hooray Sandstone|33078|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic - L.Cretaceous||||||
8476|Hooray Sandstone|33079|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33080|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33082|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33083|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33086|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
8476|Hooray Sandstone|33087|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.- L.Cret.||||||
8476|Hooray Sandstone|33088|4|Described|Table 3|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33089|4|Described|Table 2|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33095|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33169|6|Mentioned|p322|||||||||
8476|Hooray Sandstone|33176|6|Mentioned|p177|||||||||
8476|Hooray Sandstone|33182|6|Mentioned|Table 1|||L.Cret.- U.Jur.||||||
8476|Hooray Sandstone|33183|6|Mentioned|p233|||||||||
8476|Hooray Sandstone|33448|4|Described|Table 1|||U.Jur.-L.Cret.||||||11-JAN-10
8476|Hooray Sandstone|33449|4|Described|Table 1|||J.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
8476|Hooray Sandstone|33523|6|Mentioned|p27|||||||||
8476|Hooray Sandstone|33638|5|Briefly described|Table 1|||||||||
8476|Hooray Sandstone|33639|5|Briefly described|Table 2|||U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33640|4|Described|Table 3|||L.Jur.||||||
8476|Hooray Sandstone|33643|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33644|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33646|6|Mentioned|p12|||||||||
8476|Hooray Sandstone|33647|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33648|6|Mentioned|p19|||Stratigraphy.||||||
8476|Hooray Sandstone|33672|5|Briefly described|p44|||Lithology.||||||
8476|Hooray Sandstone|33673|6|Mentioned|p287|||||||||
8476|Hooray Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
8476|Hooray Sandstone|33964|6|Mentioned|p6|||Equivalent Transition Beds & Cadna-owie Formation.||||||
8476|Hooray Sandstone|34065|4|Described|p6|||U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|34091|5|Briefly described|Table 1|||Jur. - L.Cret.  See also P9||||||
8476|Hooray Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
8476|Hooray Sandstone|34174|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34218|4|Described|Table 1|||See also Table 2. Upper Jurassic - Lower Cretaceous.||||||
8476|Hooray Sandstone|34254|6|Mentioned|p491|||||||||
8476|Hooray Sandstone|34485|4|Described|Table 1|||Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34486|4|Described|Table 1|||Lower Cretaceous||||||
8476|Hooray Sandstone|34487|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
8476|Hooray Sandstone|35139|6|Mentioned|p17|||||||||
8476|Hooray Sandstone|35239|6|Mentioned|Fig.4|||||||||
8476|Hooray Sandstone|35457|6|Mentioned|p623|||||||||
8476|Hooray Sandstone|35560|4|Described|p290|||||||||
8476|Hooray Sandstone|35663|5|Briefly described|p126|||||||||
8476|Hooray Sandstone|35793|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
8476|Hooray Sandstone|35811|5|Briefly described|Table 3|||||||||
8476|Hooray Sandstone|35936|6|Mentioned|p615|||||||||
8476|Hooray Sandstone|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
8476|Hooray Sandstone|36243|6|Mentioned|Table 6A|||||||||
8476|Hooray Sandstone|36251|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|36473|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8476|Hooray Sandstone|36580|6|Mentioned|p469|||||||||
8476|Hooray Sandstone|37116|6|Mentioned|p310|||||||||
8476|Hooray Sandstone|37451|6|Mentioned|Table 2|||||||||
8476|Hooray Sandstone|37603|6|Mentioned|p444|||||||||
8476|Hooray Sandstone|37608|3|Fully described|Table 1|||||||||
8476|Hooray Sandstone|37995|6|Mentioned|p65|||||||||
8476|Hooray Sandstone|38199|5|Briefly described|p423|||Palynology||||||
8476|Hooray Sandstone|38226|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|38532|4|Described|Fig.4|||||||||
8476|Hooray Sandstone|38814|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|39070|4|Described|p364|||||||||
8476|Hooray Sandstone|39211|5|Briefly described|p23|||See also Figs 4,6-8,14,15 etc. Correlation||||||
8476|Hooray Sandstone|39212|6|Mentioned|p25|||Aquifer||||||
8476|Hooray Sandstone|39445|5|Briefly described|Table 10|||||||||
8476|Hooray Sandstone|39478|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|39846|6|Mentioned|p45|||||||||
8476|Hooray Sandstone|39847|5|Briefly described|p37|||||||||
8476|Hooray Sandstone|39898|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Medium to coarse quartz sandstone with kaolinitic cement. Upper part altered to ironstone.||||||14-FEB-06
8476|Hooray Sandstone|39943|6|Mentioned|Table 8A|||||||||
8476|Hooray Sandstone|39988|6|Mentioned|p289|||||||||
8476|Hooray Sandstone|39989|4|Described|p422|||||||||
8476|Hooray Sandstone|40121|6|Mentioned|p446|||||||||
8476|Hooray Sandstone|40199|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|40249|6|Mentioned|p41|||||||||
8476|Hooray Sandstone|40250|6|Mentioned|Fig.7|||||||||
8476|Hooray Sandstone|40538|5|Briefly described|Map legend|Cretaceous|Jurassic|Quartz arenite to quartz wacke, kaolinitic, poorly bedded, white.||||||15-NOV-05
8476|Hooray Sandstone|40670|6|Mentioned|Fig.9|||||||||
8476|Hooray Sandstone|40675|6|Mentioned|Table 8A|||||||||
8476|Hooray Sandstone|40687|3|Fully described|p416|||||||||
8476|Hooray Sandstone|40801|6|Mentioned|p29|||||||||
8476|Hooray Sandstone|40832|3|Fully described|p456|||||||||
8476|Hooray Sandstone|40833|6|Mentioned|p468|||||||||
8476|Hooray Sandstone|40906|4|Described|p30|||||||||
8476|Hooray Sandstone|40962|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41060|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|41061|6|Mentioned|p21|||||||||
8476|Hooray Sandstone|41062|6|Mentioned|Fig.5|||||||||
8476|Hooray Sandstone|41064|6|Mentioned|p60,p65|||||||||
8476|Hooray Sandstone|41097|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41177|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|41182|5|Briefly described|Fig.2|||||||||
8476|Hooray Sandstone|41186|4|Described|p209|||||||||
8476|Hooray Sandstone|41187|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|41198|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41216|6|Mentioned|Fig.18|||||||||
8476|Hooray Sandstone|41246|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|41247|6|Mentioned|p126|||See also Fig.4||||||
8476|Hooray Sandstone|41266|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|41361|6|Mentioned|p5|||||||||
8476|Hooray Sandstone|41523|6|Mentioned|p271|||||||||
8476|Hooray Sandstone|41681|4|Described|p2|||See also pp16,22.||||||26-SEP-06
8476|Hooray Sandstone|41686|6|Mentioned|p64|||||||||
8476|Hooray Sandstone|41707|5|Briefly described|p163|||||||||
8476|Hooray Sandstone|42067|4|Described|p309|||||||||
8476|Hooray Sandstone|42071|6|Mentioned|Fig.2A P116|||||||||
8476|Hooray Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
8476|Hooray Sandstone|42412|6|Mentioned|p228|||||||||
8476|Hooray Sandstone|42446|4|Described|p13|||||||||
8476|Hooray Sandstone|42447|5|Briefly described|p5 + Fig. 1|||||||||
8476|Hooray Sandstone|42474|5|Briefly described|p25|||||||||
8476|Hooray Sandstone|42493|6|Mentioned|p20|||Eromanga Basin.||||||
8476|Hooray Sandstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
8476|Hooray Sandstone|42504|5|Briefly described|p83|||or De Sousa Sandstone||||||
8476|Hooray Sandstone|42746|6|Mentioned|p9|||||||||
8476|Hooray Sandstone|42749|4|Described|p31, Fig.7 p30|||see also Fig.2 p27.||||||26-SEP-06
8476|Hooray Sandstone|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Sandstone, pebbly sandstone, siltstone.  Geological province: Amadeus Basin.||||||23-JAN-08
8476|Hooray Sandstone|42999|5|Briefly described|Table 2,p90|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
8476|Hooray Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
8476|Hooray Sandstone|43035|6|Mentioned|p27|||||||||
8476|Hooray Sandstone|43105|5|Briefly described|Fig.9,p15.|||||||||
8476|Hooray Sandstone|43114|5|Briefly described|p13|||||||||
8476|Hooray Sandstone|43122|5|Briefly described|p20|||see also Fig. 2.||||||
8476|Hooray Sandstone|43565|6|Mentioned|p422|Late Jurassic|Early Jurassic|||||||
8476|Hooray Sandstone|43602|4|Described|191|||In Eromanga Basin.||||||16-SEP-08
8476|Hooray Sandstone|43748|6|Mentioned|p7|Late Jurassic|Early Jurassic|Eromanga Basin.||||||19-DEC-11
8476|Hooray Sandstone|44019|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44020|14|Not recorded|p13,15,Tb.1,2,3|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44022|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44023|4|Described|Tb.3,p12|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44028|14|Not recorded|Fig.2,p514|Cretaceous|Jurassic|See Strat Table.||||||
8476|Hooray Sandstone|44042|14|Not recorded|Map Legend|Early Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44082|14|Not recorded|Table p34|||||||||
8476|Hooray Sandstone|44084|14|Not recorded|p32|Late Jurassic|Middle Jurassic|||||||
8476|Hooray Sandstone|44099|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44133|6|Mentioned|p110|Cretaceous|Cretaceous|Superseded by Namur Sandstone.||||||
8476|Hooray Sandstone|44337|5|Briefly described|Map Legend|Cretaceous|Jurassic|Lithology.||||||
8476|Hooray Sandstone|44362|6|Mentioned|p12|||||||||
8476|Hooray Sandstone|44375|14|Not recorded|p311,312|||||||||
8476|Hooray Sandstone|44415|14|Not recorded|p22,Fig.1,p23|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|45071|3|Fully described|Table 15|||||||||
8476|Hooray Sandstone|45103|6|Mentioned|p5|||||||||
8476|Hooray Sandstone|45110|2|Defined|p106|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous. See also Fig.5.||||||
8476|Hooray Sandstone|45168|6|Mentioned|p6|||||||||
8476|Hooray Sandstone|46791|5|Briefly described|p42|||||||||
8476|Hooray Sandstone|46881|6|Mentioned|Table 2|||||||||
8476|Hooray Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
8476|Hooray Sandstone|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
8476|Hooray Sandstone|46959|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|48919|4|Described|p65|||U.Jur. - L.Cert.||||||
8476|Hooray Sandstone|48920|3|Fully described|p55|||Middle Jurassic-Lower Cretaceous age.||||||16-SEP-08
8476|Hooray Sandstone|48992|6|Mentioned|p38|||||||||
8476|Hooray Sandstone|48997|6|Mentioned|p6|||||||||
8476|Hooray Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
8476|Hooray Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
8476|Hooray Sandstone|49027|4|Described|p21|||||||||
8476|Hooray Sandstone|50372|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Eromanga Basin. Medium grained, poorly sorted kaolinitic quartz sandstone.||||||22-JUN-04
8476|Hooray Sandstone|60122|5|Briefly described|p33, p35|Jurassic|Jurassic|Subsumed both the Tarlton Fm and Longsight Sst. (Mond and Harrison, in Senior et al 1978) - although prominent outcrops previously mapped as Tarlton Formation are now assigned to Kelly Creek Formation.  Unconformably overlies Ethabuka Sandstone.||||||17-MAY-05
8476|Hooray Sandstone|60551|5|Briefly described|Map Legend|Cretaceous|Jurassic|Geological Province: Eromanga Basin. Sandstone, feldspathic sandstone, siltstone, basal boulder conglomerate.||||||17-NOV-04
8476|Hooray Sandstone|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes Namur and  Murta Members.|Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|61312|5|Briefly described|p71, p64, p67 Fig.E5|Early Cretaceous|Late Jurassic|Name now restricted to the "Lower Hooray Sandstone" - fluvial sst. sequence. The original "Upper Hooray Sandstone" has been replaced by Cadna-owie Fm. Upper section considered to be equivalent to Mooga Fm. Geol Prov: Eromanga Basin||||||16-JUN-06
8476|Hooray Sandstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||13-MAR-09
8476|Hooray Sandstone|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
8476|Hooray Sandstone|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
8476|Hooray Sandstone|61823|5|Briefly described|p118|Cretaceous|Jurassic|Geological Province:  Eromanga Basin.||||||
8476|Hooray Sandstone|62028|5|Briefly described|p10 Fig. 1|||Includes the Namur Sandstone Member.||||||26-FEB-08
8476|Hooray Sandstone|62029|6|Mentioned|p15|||||||||
8476|Hooray Sandstone|62376|5|Briefly described|p53|Tertiary|Mesozoic|Geological Province: Georgina Basin||||||09-FEB-10
8476|Hooray Sandstone|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
8476|Hooray Sandstone|63450|5|Briefly described|p83|Cretaceous|Jurassic |May contain Cadna-owie Formation (in upper section) as the unit previously mapped as Longsight Sandstone was renamed Hooray Sandstone. Overlain by Rolling Downs Group.||||||07-FEB-11
8476|Hooray Sandstone|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of Rolling Downs Group. Thickness: 30m. Medium-grained cross-bedded white sandstone with some white vein quartz and quartzite pebble conglomerate at the base.Surface exposures often as ferruginised sandstone and conglom.||||||26-NOV-08
8476|Hooray Sandstone|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of Rolling Downs Group. Medium-grained cross-bedded white quartz sandstone with some white vein quartz and quartzite pebble conglomerate at base. Thickness: 30 m.||||||
8476|Hooray Sandstone|63979|2|Defined|p41, Fig. 44|Valanginian|Tithonian|Lower+upper sections originally informally designated as ""Namur Sst Mbr" and "Murta Mbr" respectively (both now upgraded). Thick: 165m. Mainly sandstone+lesser siltstone and mudstone, minor coal. Overlain by Cadna-owie Fm;underlain by Westbourne Fm.||||||07-FEB-11
8476|Hooray Sandstone|64048|6|Mentioned|p64 Tb. 2, p70|||Geological Province: Eromanga Basin.||||||07-FEB-11
8476|Hooray Sandstone|64068|6|Mentioned|p78|||Georgina Basin.||||Unconformably overlies Ethabuka Sandstone.||05-APR-12
8476|Hooray Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Early Cretaceous|Late Jurassic|Eromanga Basin.|||Includes Namur Sandstone Member and Murta Member.|Overlies Birkhead and Westbourne Formations. Is overlain by Cadna-owie Formation.||10-DEC-15
8476|Hooray Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Rolling Downs Group. Medium-grained cross-bedded white quartz sandstone with some white vein quartz and quartzite pebble conglomerate at the base. Thickness: 30m.||||||
8476|Hooray Sandstone|64856|6|Mentioned|p94-97|||Eromanga Basin. Correlated with Gubberamunda Sandstone of Surat Basin. Upper part grades into Mooga Sandstone.| | ||||29-NOV-17
8476|Hooray Sandstone|65238|5|Briefly described|p10|||Contains Murta Member. Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
8476|Hooray Sandstone|65309|6|Mentioned|p14.|Jurassic|Jurassic|Known in South Australia as Algebuckina Sandstone, and in Northern Territory as De Souza Sandstone.||||||
8476|Hooray Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Westbourne Formation. Overlain by Cadna-owie Formation.||||||08-MAR-12
8476|Hooray Sandstone|65489|6|Mentioned|p49, p96|Cretaceous|Jurassic|Eromanga Basin. Source and reservoir rocks.||||||
8476|Hooray Sandstone|66529|5|Briefly described|p10, p12 Fig.5, p16  |||Eromanga Basin. |||||Sandstone.|
8476|Hooray Sandstone|66623|6|Mentioned|p240.|||Lithologically and stratigraphically identical with Namur Sandstone in NSW and SA.||||||
8476|Hooray Sandstone|66915|5|Briefly described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Late Jurassic|Eromanga Basin.||||||12-JAN-17
8476|Hooray Sandstone|67323|5|Briefly described|p87-88, p93 Fig.12.3, p95 Fig.12.5, p96|Early Cretaceous|Late Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin; also probable reservoir (the unit is one of the main continuous aquifers in the region).||||Overlies Westbourne Formation. Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1|Early Cretaceous|Early Jurassic|Eromanga Basin. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Maximum thickness of 165m. Prospective unit for the storage of carbon dioxide. See also p106, p109, p111 fig ERO8, p113 fig ERO12, p114 fig ERO13, p115, p120, p304.||||Overlies the Westbourne Formation. Overlain by the Lower Cadna-owie Formation. Equivalent to the Namur Sandstone and Murta Formation.|Sandstones interbedded with siltstone, mudstone and minor coal.|
8476|Hooray Sandstone|67561|6|Mentioned|p53 Fig.3, p67|||Correlative of the Livingston Tillite Member.||||||
8476|Hooray Sandstone|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Jurassic|Surat Basin.||||Is overlain by Bungil Formation.||
8476|Hooray Sandstone|68004|5|Briefly described|p174.|||Major aquifer for water production; excellent quality reservoir. Sealed by Wallumbilla Formation shales. A major hydrocarbon exploration target.||||||
8476|Hooray Sandstone|68135|5|Briefly described|p52 Fig.2b|Early Cretaceous|Tithonian|Eromanga Basin.||||Unconformably overlies Westbourne Formation.|Predominantly sandstone.|
8476|Hooray Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
8476|Hooray Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
8476|Hooray Sandstone|68731|6|Mentioned|pp209-211|||||||||
8476|Hooray Sandstone|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (NE). Fluvial.||||||
8476|Hooray Sandstone|69443|6|Mentioned|p28:30|||Eromanga Basin.||||Unconformably overlies Ethabuka Sandstone.||12-JUL-16
8476|Hooray Sandstone|69457|5|Briefly described|p41:3-4, 6-7|Early Cretaceous|Early Cretaceous|NE Eromanga Basin. This name was used in the ILLOGWA CREEK map area (Shaw and Freeman, 1985) and TOBERMOREY and HAY RIVER map areas (Mond and Harrison in Senior et al., 1978). It appears that it is to be superseded by the Algebuckina Sandstone.||||Is overlain conformably by Cadna-owie Formation.|Mesa-forming planar to cross-bedded, medium-coarse sandstone and minor mudstone, siltstone and conglomerate.|12-JUL-16
8476|Hooray Sandstone|69582|5|Briefly described|p29, p65-p66|||Eromanga Basin. Intersected in GSQ Julia Creek 1 and in GSQ Longreach 2 drillholes.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.|Sandstone, mudstone.|
8476|Hooray Sandstone|69594|4|Described|p519, p526-528, p532-533, p537-538, p573|Hauterivian|Tithonian|Woolley (1941); Hill and Denmead (1960). Eromanga Basin. Reference section in GSQ Tambo 2 (Wallin, 1974). Cannot be divided in E and N parts of the Basin; in SW QLD, it had been divided into a lower Namur Sandstone Member and an overlying Murta Member (both superseded). Petroleum companies include basal Cadna-owie Formation in their idea of the Murta Member. 90-165m thick. Braided fluvial deposits. A significant hydrocarbon reservoir. An important, shallow aquifer. RELATED UNITS (continued); Equivalent to Gubberamunda Sandstone, Orallo Formation and Mooga Sandstone (grades into the last).||||Overlies Westbourne Formation conformably to unconformably. Is overlain transitionally by Cadna-owie Formation. Lower part interfingers with lower Southlands Formation. See COMMENTS for more.|Sublabile to quartzose sandstone, with subordinate siltstone and mudstone and sporadic minor coal seams.|
8476|Hooray Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Eromanga Basin.||||||
8476|Hooray Sandstone|69946|6|Mentioned|p16|||||||||
8476|Hooray Sandstone|69947|5|Briefly described|p29 Fig.7.18|||||||Is overlain by McKinlay Member (Murta Formation). ?Correlates with Namur Sandstone.||07-FEB-18
8476|Hooray Sandstone|70821|4|Described|p21-22,p28,p30-31,p33,p72,p79-83,p85-86|Early Cretaceous|Jurassic|Woolley (1941), Exon (1966). Eromanga Basin. Formerly part of Rolling Downs Group. A major aquifer in the Great Artesian Basin: one of the two main groundwater resources in the area. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrochemistry mentioned, hydrostratigraphic properties.||||Overlies Birkhead and Westbourne Formations (Injune Creek Group). Is overlain by Cadna-owie Formation or Doncaster Member (Wallumbilla Formation). Lateral equivalent to Algebuckina Sandstone.|Sub-labile, quartz sandstone with minor conglomerate.|
8476|Hooray Sandstone|70823|6|Mentioned|p78|Cretaceous|Jurassic|Eromanga Basin.||||||
8476|Hooray Sandstone|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
8476|Hooray Sandstone|70860|6|Mentioned|p280-281|||Great Artesian Basin. Part of the uppermost aquifer in the Basin. Is presented also as Cadna-owie - Hooray Sandstone aquifer. Fluvial, paralic and littoral sediments.|||||Quartzose and lithic sandstone.|
8476|Hooray Sandstone|71251|5|Briefly described|p13, p15, p17, p20, p49, p51|||Natural gamma wireline log. Conductivity diagram. An artesian aquifer with very high water pressures.||||Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|71342|5|Briefly described|Ch5 p16-p17|||The lower part of this unit is equivalent to the Namur Sandstone and the upper part is equivalent to the Murta Formation. ||||||
8476|Hooray Sandstone|71382|5|Briefly described|p4, p12, p16-p17, p19, p25|Cretaceous|Late Jurassic|Eromanga Basin. Intersected in GSQ Julia 1 from 310.49m-320.05m for a total of 9.56m thickness. An aquifer occurs within this unit where it was intersected. Temp log and stratlog are provided. See also p27-p28, App 3, 4.||||Overlies the Millungera Basin - quartzite 81261. Overlain by the Wallumbilla Formation.|Yellowish-brown, medium to coarse-grained, well-sorted and subnrounded quartzose sandstone, medium grey mudstone laminae also occur.|
8476|Hooray Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
8476|Hooray Sandstone|71863|5|Briefly described|p5|Valanginian|Tithonian|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
8476|Hooray Sandstone|71864|6|Mentioned|p14, p17|||Waterbores intersect this unit which has a very high artesian groundwater flow.||||||
8476|Hooray Sandstone|72297|6|Mentioned|p742, p761|||Eromanga Basin. Petroleum reservoir. A major aquifer with excellent prospects for HSA (hot sedimentary aquifer) geothermal energy.||||||
8476|Hooray Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Cadna-owie FZ.||
8476|Hooray Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown with Namur Sandstone as located in the Eromanga Basin.||||Unconformably overlies Westbourne Formation.||
8476|Hooray Sandstone|73113|6|Mentioned|p207|||Great Artesian Basin.||||||
8476|Hooray Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains oil.||||||
8476|Hooray Sandstone|73203|6|Mentioned|p652|Jurassic|Jurassic|||||||
8476|Hooray Sandstone|73343|6|Mentioned|p337|Cretaceous|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Westbourne Formation. Overlain by Murta Member. Equivalent to Namur Sandstone.||
8476|Hooray Sandstone|73479|5|Briefly described|p156 Fig.2|Cretaceous|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.||||Overlies Westbourne Formation, underlies Murta Member||
8484|Hope Valley Sand|40446|6|Mentioned|p51|||||||||
8504|Horseshoe Bend Shale|22760|5|Briefly described|p340|||Parent - Finke Group.  Age - may be Famennian.||||||
8504|Horseshoe Bend Shale|22826|6|Mentioned|p576|Devonian|Devonian|||||||
8504|Horseshoe Bend Shale|23858|5|Briefly described|p916|Late Devonian|Middle Devonian|Of Finke Group. Overlying Unit Idracowra Sandstone. Underlying Unit Langra Conglomerate. Geological Province: Amadeus Basin.||||||
8504|Horseshoe Bend Shale|24301|4|Described|p22, p7 Tb. 2|Devonian|Devonian|Of Finke Group. Overlies Langra Formation, underlies Idacowra Sandstone. Maximum thickness: 566m. Geological Province: Amadeus Basin.||||||
8504|Horseshoe Bend Shale|30544|6|Mentioned|Fig.5|||||||||
8504|Horseshoe Bend Shale|31566|6|Mentioned|p244|||Devonian.||||||
8504|Horseshoe Bend Shale|31567|3|Fully described|p285|||Refers Wells et al. (1966).||||||
8504|Horseshoe Bend Shale|33844|6|Mentioned|Table 1|||||||||
8504|Horseshoe Bend Shale|33971|3|Fully described|p30|||Refers Wells et al. (1966).||||||
8504|Horseshoe Bend Shale|34111|5|Briefly described|Table 2|||Devonian - Carboniferous||||||
8504|Horseshoe Bend Shale|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
8504|Horseshoe Bend Shale|35102|6|Mentioned|Fig.17|||||||||
8504|Horseshoe Bend Shale|41125|6|Mentioned|p40|||||||||
8504|Horseshoe Bend Shale|42504|6|Mentioned|p81|||||||||
8504|Horseshoe Bend Shale|42699|5|Briefly described|map legend|Devonian||||||||
8504|Horseshoe Bend Shale|42940|6|Mentioned|Plate 5|||||||||
8504|Horseshoe Bend Shale|43035|5|Briefly described|p25|||of Finke Group||||||
8504|Horseshoe Bend Shale|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone.||||||
8504|Horseshoe Bend Shale|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Dev-Carb. pt. of Finke Group.||||||
8504|Horseshoe Bend Shale|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
8504|Horseshoe Bend Shale|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carbon.||||||
8504|Horseshoe Bend Shale|44393|4|Described|p.6,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Part of Finke Group. Dev-Carb.||||||
8504|Horseshoe Bend Shale|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
8504|Horseshoe Bend Shale|45041|4|Described|p104|||Devonian||||||
8504|Horseshoe Bend Shale|48865|2|Defined|p.4,5,Fig.33||Paleozoic|On many figures. Fig.4,21,27,38,29,31,32,36,39,41,52,Pl.5,10,11. Unit of Finke Group. (G53-3,6).||||||07-NOV-08
8504|Horseshoe Bend Shale|48890|4|Described|p.52|Carboniferous|Devonian|Pt. Finke Gp. Dev-Carb.||||||
8504|Horseshoe Bend Shale|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. C||||||10-AUG-06
8504|Horseshoe Bend Shale|65309|4|Described|p6 Table 1, pp13-14, p19.|Devonian|Devonian|Very distinctive unit, with isolated exposures in northeast map area. Most outcrops only a few metres thick. Contains a relative abundance of halite pseudomorphs and detrital biotite, implying arid conditions during deposition.||Unit in Finke Group.||Is overlain by Idracowra Sandstone.|Fine to very fine, chocolate-brown, biotitic quartz sandstone or siltstone.|
8504|Horseshoe Bend Shale|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 86 m.  Seen as having potential as an insulating layer for geothermal energy.||||Overlies Langra Sandstone. Is overlain by Idracowra Sandstone.||
8504|Horseshoe Bend Shale|65489|6|Mentioned|p63|||Potential to act as a seal.||||||
8504|Horseshoe Bend Shale|69438|3|Fully described|p23:2-3, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Most widespread unit of the Group, but most poorly exposed. Is 92m thick at the type locality N of Horseshoe Bend homestead. Up to 310m thick elsewhere. Lithology described in some detail. Appears as Horshoe Bend Shale on 23:3.||Finke Group.||Conformably overlies Langra Formation. Is overlain transitionally by Idracowra Sandstone.|Red-brown and lesser green siltstone, with minor thin interbeds of fine sandstone.|12-JUL-16
8504|Horseshoe Bend Shale|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Langra Formation. Is overlain by Idracowra Sandstone.||12-JUL-16
8504|Horseshoe Bend Shale|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Langra Formation||
8504|Horseshoe Bend Shale|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
8504|Horseshoe Bend Shale|73085|6|Mentioned|p1|late Devonian|late Devonian|[Unclear relationship with Idracowra Sandstone].||Finke Group||Underlain by Langra Formation. Equivalent to Brewer Conglomerate (Pertnjara Group).||
8561|Humanity Seat Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
8561|Humanity Seat Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Emeroo Subgroup (Burra Group).||||||
8561|Humanity Seat Formation|22869|6|Mentioned|P45|||||||||
8561|Humanity Seat Formation|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Humanity Seat Formation of the northern Flinders Ranges.||||||
8561|Humanity Seat Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
8561|Humanity Seat Formation|23411|6|Mentioned|Map Legend|||||||||
8561|Humanity Seat Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
8561|Humanity Seat Formation|23818|4|Described|p54|||Overlying unit: Callanna Beds, Upper (unconfromable). Underlying unit: Wooltana Volcanics (unconformable). Max. thickness: 6000 ft. Forms the uppermost unit of the Callanna Beds, Lower.||||||18-APR-05
8561|Humanity Seat Formation|24176|4|Described|p9, p26 Tb. 1|Adelaidean|Adelaidean|Of Callanna Beds.  Sandstones, quartzites, purple and grey shale partings.  Max. thickness: >2075m.  Age is Willouran.  Overlies Wootana Volcanics.  Geological Province: Mount Painter Province.||||||
8561|Humanity Seat Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlain by Blue Mine Conglomerate. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
8561|Humanity Seat Formation|24593|5|Briefly described|p613 Fig. 1b|||Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
8561|Humanity Seat Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
8561|Humanity Seat Formation|30177|2|Defined|p127|Adelaidean|Adelaidean|See also p57-59. Type area: Between Barraranna Gorge and Humanity Seat Trig.||||||25-NOV-22
8561|Humanity Seat Formation|30801|6|Mentioned|p5|||Lower Callanna Beds. Table P5-6||||||
8561|Humanity Seat Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
8561|Humanity Seat Formation|31388|6|Mentioned|Fig.1|||||||||
8561|Humanity Seat Formation|32724|6|Mentioned|Fig.1|||Correlation||||||
8561|Humanity Seat Formation|32776|6|Mentioned|Fig.2|||||||||
8561|Humanity Seat Formation|33004|6|Mentioned|p135|||||||||
8561|Humanity Seat Formation|33474|6|Mentioned|Fig.4|||||||||
8561|Humanity Seat Formation|34535|5|Briefly described|p59|||L.Callanna Beds||||||
8561|Humanity Seat Formation|34812|6|Mentioned|p134|||||||||
8561|Humanity Seat Formation|35255|6|Mentioned|p13|||||||||
8561|Humanity Seat Formation|36083|5|Briefly described|p472|||||||||
8561|Humanity Seat Formation|36733|6|Mentioned|Table 5|||||||||
8561|Humanity Seat Formation|37854|6|Mentioned|Table 1|||||||||
8561|Humanity Seat Formation|37932|6|Mentioned|Fig.2|||||||||
8561|Humanity Seat Formation|38157|6|Mentioned|Table III|||||||||
8561|Humanity Seat Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
8561|Humanity Seat Formation|40294|6|Mentioned|p9|||||||||
8561|Humanity Seat Formation|41403|6|Mentioned|p43|||||||||
8561|Humanity Seat Formation|41404|3|Fully described|p86|||||||||
8561|Humanity Seat Formation|41405|6|Mentioned|Fig.55|||||||||
8561|Humanity Seat Formation|43052|5|Briefly described|p179,Table 6.1|||of Emeroo Subgroup||||||
8561|Humanity Seat Formation|65925|5|Briefly described|p124 Fig.3.|||||Unit in Burra Group.|||Quartzite, heavy mineral lamination, salt casts; conglomerate.|
8561|Humanity Seat Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Emeroo Subgroup.||Is overlain ?conformably by Woodnamoka Phyllite.|Sandstone, medium-grained, heavy mineral laminations; shale; evaporites as rare halite clasts.|18-JAN-19
8561|Humanity Seat Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p16, p20|Tonian|Tonian|Detrital zircon MDA is much older than the true depositional age.|1053+/-114 Ma LA-ICP-MS detrital zircon MDA|Emeroo Subgroup||Correlated with Top Mount Sandstone||
8610|Hutton Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498-499|Callovian|Aalenian|Eromanga and Mulgildie Basins. An important aquifer. Up to 250m thick.||||Conformably overlies Poolowanna Formation. Equivalent to Algebuckina Sandstone.|Well-sorted, cross-bedded, quartzose to sub-labile fluvial sandstone, with minor thin conglomerate bands and thin beds of siltstone and mudstone.|
8610|Hutton Sandstone|13497|4|Described|ix, p26, p89, p104, p112|Jurassic|Jurassic|Eromanga Basin. Deposited in a low sinuosity fluvial environment. Disconformably overlies the Arrabury Formation.  Overlain by the Birkhead Formation and Algebuckina Sandstone. Disconformably overlain by the Cuddapan Formation. See also p114-p115, p136, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p154, p171-p172, p184, p216.||||Overlies the Patchawarra Formation and the Poolowanna Formation. Unconformably overlies the Tinchoo Formation.||
8610|Hutton Sandstone|13516|6|Mentioned|p159, 167, 169, 170, 171,172,173, 139|Middle Jurassic|Middle Jurassic|Eromanga and Surat Basins||||||
8610|Hutton Sandstone|22464|6|Mentioned|p9||Middle Jurassic|Eromanga Basin, overlain by Birkhead Formation.||||||18-SEP-18
8610|Hutton Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Middle Jurassic|Thickness: 290 m. Also Table5, p10. as 260 m. Ipswich-Moreton Basin.||||||17-JAN-08
8610|Hutton Sandstone|22839|6|Mentioned|P33|||||||||
8610|Hutton Sandstone|22857|5|Briefly described|p295, p296-7 Tb 22.1, p546 Tb.A1.12|Bajocian|Aalenian|Of the Bundamba Group. Sequence of stacked quartzose braided stream sands. Max. thickness: 200m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314.||||||
8610|Hutton Sandstone|22865|4|Described|p295,Table22.1p296-7|Bajocian|Aalenian|||||||
8610|Hutton Sandstone|22883|5|Briefly described|P28, Fig2|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|22924|6|Mentioned|49|||||||||
8610|Hutton Sandstone|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|23050|4|Described|p23 Table 4|Middle Jurassic|Early Jurassic|In the Surat Basin. Age: Palynology data indicates an Early to Middle Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|23051|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|In the Surat Basin.||||||17-JAN-08
8610|Hutton Sandstone|23053|6|Mentioned|Fig10p17|Toarcian|Toarcian|||||||
8610|Hutton Sandstone|23054|6|Mentioned|Fig5p22|||||||||
8610|Hutton Sandstone|23056|4|Described|12|||Geol province Eromanga Basin||||||
8610|Hutton Sandstone|23154|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province - Eromanga Basin.||||||
8610|Hutton Sandstone|23155|4|Described|p26 & Fig 14 on p27|Middle Jurassic|Early Jurassic|On southern STRZELECKI the Hutton Sandstone passes into Algebuckina Sandstone.||||||
8610|Hutton Sandstone|23375|4|Described|Fig2 p265|Callovian|Aalenian|In the Eromanga Basin.||||||17-JAN-08
8610|Hutton Sandstone|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
8610|Hutton Sandstone|23430|4|Described|p523-524 Table 14.7|Middle Jurassic|Early Jurassic|Eromanga Basin Province.  Maximum thickness <120 m.||||||
8610|Hutton Sandstone|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
8610|Hutton Sandstone|23799|5|Briefly described|p52|Middle Jurassic|Middle Jurassic|Correlative of Heifer Creek Sandstone (Clarence-Moreton Basin).  Geological Province:Surat Basin.||||||
8610|Hutton Sandstone|23818|5|Briefly described|p140, p144 Fig.66|Jurassic|Jurassic|Geological Province: Great Artesian Basin. Dated upon palynological evidence.||||||
8610|Hutton Sandstone|23830|5|Briefly described|Fig. 3a|Jurassic|Jurassic|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||12-SEP-05
8610|Hutton Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
8610|Hutton Sandstone|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
8610|Hutton Sandstone|24068|4|Described|p269|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin.  Maximum thickness: 245m.||||||
8610|Hutton Sandstone|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
8610|Hutton Sandstone|24159|5|Briefly described|p148, Fig. 2, p152|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Walloon Coal Measures. Underlying Unit: Evergreen Formation.||||||
8610|Hutton Sandstone|24175|5|Briefly described|p17 Fig. 3|Callovian|Aalenian|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24210|5|Briefly described|p133 Fig. 2||Middle Jurassic|Unconformable over Poolowanna Formation.  Geological Province: Eromanga Basin.  See also p132.||||||
8610|Hutton Sandstone|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|24243|5|Briefly described|p3 Fig.2|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|24282|6|Mentioned|p11|||Cooper-Eromanga Basin.||||||
8610|Hutton Sandstone|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
8610|Hutton Sandstone|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium-grained sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|24615|5|Briefly described|CD|Jurassic|Jurassic|[Jh].  Fine- to medium-grained, sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|29385|6|Mentioned|p80|||Also p82. Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|29387|6|Mentioned|p30|||Also Table 5. Jurassic.||||||
8610|Hutton Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
8610|Hutton Sandstone|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
8610|Hutton Sandstone|29591|5|Briefly described|p79|||||||||
8610|Hutton Sandstone|29721|6|Mentioned|Table 246|||||||||
8610|Hutton Sandstone|29869|6|Mentioned|p34|||See also Fig.1||||||
8610|Hutton Sandstone|29870|6|Mentioned|p15|||||||||
8610|Hutton Sandstone|29961|4|Described|p14|||||||||
8610|Hutton Sandstone|30024|6|Mentioned|p332|||||||||
8610|Hutton Sandstone|30102|4|Described|p17|||See also p18-21. Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30103|6|Mentioned|p8|||||||||
8610|Hutton Sandstone|30133|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|30451|4|Described|p74|||See also p75. Late Lower and Early Middle Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|30455|6|Mentioned|p13|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30456|6|Mentioned|p95|||||||||
8610|Hutton Sandstone|30457|6|Mentioned|p96|||||||||
8610|Hutton Sandstone|30458|6|Mentioned|p3|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30460|6|Mentioned|p6|||See also p15,21, Table 4. Lower Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30461|6|Mentioned|p100|||||||||
8610|Hutton Sandstone|30464|6|Mentioned|p4|||miospores.||||||18-SEP-18
8610|Hutton Sandstone|30465|6|Mentioned|p4|||||||||
8610|Hutton Sandstone|30466|6|Mentioned|p5|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30472|6|Mentioned|p132|||Pollen distribution.||||||18-SEP-18
8610|Hutton Sandstone|30474|6|Mentioned|p132|||Pollen distribution.||||||18-SEP-18
8610|Hutton Sandstone|30508|6|Mentioned|p81|||See also p90.||||||18-SEP-18
8610|Hutton Sandstone|30540|6|Mentioned|Fig.6|||||||||
8610|Hutton Sandstone|30691|4|Described|p6|||See also p15,21,Table 4. Lower Jurassic age||||||17-JAN-08
8610|Hutton Sandstone|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30695|4|Described|Table 3|||Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30696|4|Described|Table 4|||Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30698|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30699|6|Mentioned|p53|||Early Jurassic. Stratigraphy||||||
8610|Hutton Sandstone|30700|6|Mentioned|p22|||Lower Jurassic. Map||||||
8610|Hutton Sandstone|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30702|6|Mentioned|p48|||See also Fig.1. Stratagraphic table||||||
8610|Hutton Sandstone|30804|6|Mentioned|p10|||On Table 1.||||||18-SEP-18
8610|Hutton Sandstone|30853|5|Briefly described|Table 3|||Lower to Middle Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|30854|4|Described|Table 4|||Lower Jurassic age||||||
8610|Hutton Sandstone|30855|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|Lower - Middle Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|30856|4|Described|Table 3|||Lower Jurassic||||||
8610|Hutton Sandstone|30857|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|30915|6|Mentioned|p98|||||||||
8610|Hutton Sandstone|30921|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early - Late Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|31098|6|Mentioned|p5|||L.Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|31116|4|Described|p24|||See also p10. Jurassic||||||17-JAN-08
8610|Hutton Sandstone|31117|5|Briefly described|p379|||Lithology. Jurassic||||||
8610|Hutton Sandstone|31118|6|Mentioned|p311|||||||||
8610|Hutton Sandstone|31120|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|31121|6|Mentioned|p390|||||||||
8610|Hutton Sandstone|31122|6|Mentioned|p344|||||||||
8610|Hutton Sandstone|31145|5|Briefly described|Table 1|||L. - Mid. Jurassic||||||
8610|Hutton Sandstone|31304|6|Mentioned|Fig. 1|||||||||
8610|Hutton Sandstone|31369|4|Described|p26|||Triassic. See also p27.||||||17-JAN-08
8610|Hutton Sandstone|31431|5|Briefly described|Table 2|||L.-M.Jurassic||||||
8610|Hutton Sandstone|31432|4|Described|Table 1|||L.Jurassic||||||
8610|Hutton Sandstone|31436|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|31553|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32040|6|Mentioned|p885|||Stratigraphic sequence.||||||18-SEP-18
8610|Hutton Sandstone|32136|6|Mentioned|p3|||Aalenian (Late Liassic) miospores.||||||18-SEP-18
8610|Hutton Sandstone|32138|6|Mentioned|p396|||||||||
8610|Hutton Sandstone|32182|4|Described|p4|||Jurassic. See also p5.||||||17-JAN-08
8610|Hutton Sandstone|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
8610|Hutton Sandstone|32490|6|Mentioned|Table 1|||Equivalent Ronlow Beds?||||||
8610|Hutton Sandstone|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7.||||||18-SEP-18
8610|Hutton Sandstone|32797|4|Described|Table 4|||L. Jur.||||||
8610|Hutton Sandstone|33059|4|Described|Table 1|||See also Fig.4. L-M.Jur.||||||
8610|Hutton Sandstone|33067|4|Described|Table 1|Early Jurassic|Early Jurassic|Quartz sandstone, minor siltstone, shale.||||||07-JUL-04
8610|Hutton Sandstone|33069|4|Described|p7|||L.Jur.||||||
8610|Hutton Sandstone|33070|4|Described|Table 2|||Lower Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|33071|4|Described|p6|||L.Jur.||||||
8610|Hutton Sandstone|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33080|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
8610|Hutton Sandstone|33082|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33086|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33087|6|Mentioned|Map legend||Early Jurassic|||||||
8610|Hutton Sandstone|33088|4|Described|Table 3|||Injune Ck.Gp.||||||
8610|Hutton Sandstone|33089|5|Briefly described|Table 2|||L.Jur.||||||
8610|Hutton Sandstone|33090|4|Described|Table 4|||L.Jur.||||||
8610|Hutton Sandstone|33091|5|Briefly described|p10|||Stratigraphy||||||
8610|Hutton Sandstone|33092|5|Briefly described|p6|||Strat. Table||||||
8610|Hutton Sandstone|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33096|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33367|5|Briefly described|Table 1|||See also p3.||||||18-SEP-18
8610|Hutton Sandstone|33371|6|Mentioned|Fig.2|||||||||
8610|Hutton Sandstone|33381|6|Mentioned|Table 1|||L.-M. Jur.||||||
8610|Hutton Sandstone|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33530|5|Briefly described|Table 1|||Lower - Middle Jurassic||||||
8610|Hutton Sandstone|33638|5|Briefly described|Table 1|||||||||
8610|Hutton Sandstone|33639|5|Briefly described|Table 2|||L. Jur.||||||
8610|Hutton Sandstone|33640|4|Described|Table 3|||L.Jur.||||||
8610|Hutton Sandstone|33643|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33644|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33646|6|Mentioned|p12|||||||||
8610|Hutton Sandstone|33647|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33648|6|Mentioned|p19|||Stratigraphy.||||||
8610|Hutton Sandstone|33672|5|Briefly described|p44|||Lithology.||||||
8610|Hutton Sandstone|33673|6|Mentioned|p291|||Good reservoir potential.||||||
8610|Hutton Sandstone|33674|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|33762|6|Mentioned|p369|||Late Jurassic||||||
8610|Hutton Sandstone|33774|6|Mentioned|p40|||L.Jurassic. Faulting||||||
8610|Hutton Sandstone|33820|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
8610|Hutton Sandstone|33822|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33824|6|Mentioned|p7|||See also Table 2.||||||18-SEP-18
8610|Hutton Sandstone|33825|6|Mentioned|p9|||Lithology.||||||18-SEP-18
8610|Hutton Sandstone|33827|6|Mentioned|p7|||See also Table 2.||||||18-SEP-18
8610|Hutton Sandstone|33828|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|33832|5|Briefly described|p11|||Strat. and correlation.||||||17-JAN-08
8610|Hutton Sandstone|33936|6|Mentioned|Fig.3A|||Jurassic.||||||
8610|Hutton Sandstone|33971|6|Mentioned|Fig.29|||Strat. table.||||||
8610|Hutton Sandstone|33977|6|Mentioned|p9|||Lithology Equiv.||||||
8610|Hutton Sandstone|33998|6|Mentioned|p31|||||||||
8610|Hutton Sandstone|34065|4|Described|p7|||L.-M. Jur.||||||
8610|Hutton Sandstone|34091|5|Briefly described|Table 1|||L.Jur   See also P4||||||
8610|Hutton Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic.||||||
8610|Hutton Sandstone|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|34212|6|Mentioned|p2|||Jurassic||||||
8610|Hutton Sandstone|34218|4|Described|Table 1|||Lower - Middle Jurassic. See also Table 2.||||||
8610|Hutton Sandstone|34254|6|Mentioned|p481|||||||||
8610|Hutton Sandstone|34282|6|Mentioned|p95|||||||||
8610|Hutton Sandstone|34287|6|Mentioned|p70|||Jurassic||||||
8610|Hutton Sandstone|34386|6|Mentioned|p98,100-103,106-107|||Assemblages in. See also Figs.3,4,5,6,7.||||||
8610|Hutton Sandstone|34412|6|Mentioned|p108|||See also p109. Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|34452|6|Mentioned|p1|||L.Jurassic. See also pp2,3,4,5 etc||||||18-SEP-18
8610|Hutton Sandstone|34486|4|Described|Table 1|||Lower Jurassic. See also Table 2, p10||||||17-JAN-08
8610|Hutton Sandstone|34487|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|34507|6|Mentioned|p87|||||||||
8610|Hutton Sandstone|34611|6|Mentioned|p140|||Jurassic. See also Fig.65, Fig.66.||||||18-SEP-18
8610|Hutton Sandstone|34613|4|Described|Table 4|||||||||
8610|Hutton Sandstone|34743|6|Mentioned|p27|||||||||
8610|Hutton Sandstone|34905|6|Mentioned|p531|||||||||
8610|Hutton Sandstone|35030|6|Mentioned|p335|||||||||
8610|Hutton Sandstone|35067|6|Mentioned|Fig.4|||||||||
8610|Hutton Sandstone|35148|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|35157|6|Mentioned|p524|||||||||
8610|Hutton Sandstone|35239|6|Mentioned|p258|||||||||
8610|Hutton Sandstone|35457|6|Mentioned|p633|||||||||
8610|Hutton Sandstone|35560|4|Described|p288|||||||||
8610|Hutton Sandstone|35562|6|Mentioned|p295|||Stratigraphy.||||||18-SEP-18
8610|Hutton Sandstone|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
8610|Hutton Sandstone|35663|6|Mentioned|Fig.1|||Revised outcrop geology.||||||
8610|Hutton Sandstone|35811|5|Briefly described|Table 3|||See also Table 5.||||||
8610|Hutton Sandstone|35901|6|Mentioned|p17|||||||||
8610|Hutton Sandstone|35937|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|36233|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|36243|6|Mentioned|p74|||See also Table 6A.||||||
8610|Hutton Sandstone|36331|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|36333|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|||||||15-JUL-04
8610|Hutton Sandstone|36570|2|Defined|p26|Jurassic|Jurassic|See also p20, Fig.9, p55, Table 1, p34.||||||17-JAN-08
8610|Hutton Sandstone|36574|6|Mentioned|p599|||||||||
8610|Hutton Sandstone|36708|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|36825|6|Mentioned|p21|||||||||
8610|Hutton Sandstone|36910|6|Mentioned|p60|||||||||
8610|Hutton Sandstone|36914|6|Mentioned|p87|||||||||
8610|Hutton Sandstone|37116|6|Mentioned|p310|||||||||
8610|Hutton Sandstone|37117|5|Briefly described|p313|||||||||
8610|Hutton Sandstone|37119|5|Briefly described|p318|||||||||
8610|Hutton Sandstone|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|37287|6|Mentioned|p33|||||||||
8610|Hutton Sandstone|37288|6|Mentioned|p41|||||||||
8610|Hutton Sandstone|37451|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|37463|6|Mentioned|p479|||||||||
8610|Hutton Sandstone|37608|3|Fully described|Table 1|||||||||
8610|Hutton Sandstone|37703|6|Mentioned|p2240|||||||||
8610|Hutton Sandstone|37856|6|Mentioned|Table 3|||||||||
8610|Hutton Sandstone|37993|6|Mentioned|Fig.2|||||||||
8610|Hutton Sandstone|37994|6|Mentioned|p144|||||||||
8610|Hutton Sandstone|37995|4|Described|p64|||||||||
8610|Hutton Sandstone|38064|6|Mentioned|42|||||||||
8610|Hutton Sandstone|38068|6|Mentioned|p71|||||||||
8610|Hutton Sandstone|38205|6|Mentioned|p96|||||||||
8610|Hutton Sandstone|38358|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|38730|6|Mentioned|p29|||||||||
8610|Hutton Sandstone|38779|6|Mentioned|p7|||||||||
8610|Hutton Sandstone|39070|4|Described|p363|||||||||
8610|Hutton Sandstone|39212|4|Described|p37|||Excursion site. p24 petroleum reservoir. p25 aquifer. See also p16.||||||17-JAN-08
8610|Hutton Sandstone|39276|6|Mentioned|Fig. 2|||||||||
8610|Hutton Sandstone|39315|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|39445|5|Briefly described|Table 10|||||||||
8610|Hutton Sandstone|39478|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|39482|6|Mentioned|Fig.7|||||||||
8610|Hutton Sandstone|39494|6|Mentioned|p129|||See also Fig.3.||||||18-SEP-18
8610|Hutton Sandstone|39632|6|Mentioned|p209|||||||||
8610|Hutton Sandstone|39815|6|Mentioned|p444|||||||||
8610|Hutton Sandstone|39846|6|Mentioned|p44|||||||||
8610|Hutton Sandstone|39847|5|Briefly described|p35|||||||||
8610|Hutton Sandstone|39907|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|39943|6|Mentioned|Table 8A|||||||||
8610|Hutton Sandstone|39988|6|Mentioned|p288|||||||||
8610|Hutton Sandstone|39989|4|Described|p421|||||||||
8610|Hutton Sandstone|40003|5|Briefly described|p33|||||||||
8610|Hutton Sandstone|40030|6|Mentioned|p132|||||||||
8610|Hutton Sandstone|40121|6|Mentioned|p446|||||||||
8610|Hutton Sandstone|40245|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|40249|6|Mentioned|p38|||Mention p41.||||||18-SEP-18
8610|Hutton Sandstone|40250|4|Described|p30|||||||||
8610|Hutton Sandstone|40540|6|Mentioned|p151|||||||||
8610|Hutton Sandstone|40541|3|Fully described|p109|||||||||
8610|Hutton Sandstone|40544|6|Mentioned|p156|||||||||
8610|Hutton Sandstone|40623|5|Briefly described|p72|||See also p109.||||||18-SEP-18
8610|Hutton Sandstone|40642|6|Mentioned|p172|||||||||
8610|Hutton Sandstone|40666|4|Described|p356|||||||||
8610|Hutton Sandstone|40675|6|Mentioned|p306|||Mention Table 8A.||||||18-SEP-18
8610|Hutton Sandstone|40687|3|Fully described|p413|||||||||
8610|Hutton Sandstone|40767|6|Mentioned|p14|||||||||
8610|Hutton Sandstone|40832|3|Fully described|p455|||||||||
8610|Hutton Sandstone|40833|6|Mentioned|p468|||||||||
8610|Hutton Sandstone|40910|6|Mentioned|Table 3|||||||||
8610|Hutton Sandstone|40926|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|40953|4|Described|p19|||||||||
8610|Hutton Sandstone|40962|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|41060|5|Briefly described|p2|||Generalized stratigraphy||||||
8610|Hutton Sandstone|41061|6|Mentioned|p19|||||||||
8610|Hutton Sandstone|41062|6|Mentioned|p28,p34|||See also Fig.5.||||||18-SEP-18
8610|Hutton Sandstone|41063|6|Mentioned|p46|||||||||
8610|Hutton Sandstone|41064|6|Mentioned|p60|||||||||
8610|Hutton Sandstone|41084|5|Briefly described|Fig.2|||||||||
8610|Hutton Sandstone|41097|6|Mentioned|p166|||||||||
8610|Hutton Sandstone|41099|6|Mentioned|p185|||||||||
8610|Hutton Sandstone|41123|6|Mentioned|p177|||||||||
8610|Hutton Sandstone|41164|6|Mentioned|p422|||||||||
8610|Hutton Sandstone|41165|6|Mentioned|p373|||See also Fig.18, Fig.20.||||||18-SEP-18
8610|Hutton Sandstone|41175|6|Mentioned|p195|||||||||
8610|Hutton Sandstone|41176|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|41177|6|Mentioned|p222|||||||||
8610|Hutton Sandstone|41182|5|Briefly described|Fig.2|||||||||
8610|Hutton Sandstone|41183|6|Mentioned|p307|||||||||
8610|Hutton Sandstone|41186|4|Described|p204|||||||||
8610|Hutton Sandstone|41187|5|Briefly described|p216|||||||||
8610|Hutton Sandstone|41188|6|Mentioned|p235|||||||||
8610|Hutton Sandstone|41189|6|Mentioned|p249|||||||||
8610|Hutton Sandstone|41198|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|41210|5|Briefly described|p158|||||||||
8610|Hutton Sandstone|41212|6|Mentioned|p203|||||||||
8610|Hutton Sandstone|41214|6|Mentioned|p254|||||||||
8610|Hutton Sandstone|41216|6|Mentioned|Fig.18,p299|||||||||
8610|Hutton Sandstone|41219|4|Described|p345|||||||||
8610|Hutton Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
8610|Hutton Sandstone|41247|6|Mentioned|p119|||||||||
8610|Hutton Sandstone|41266|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|41281|6|Mentioned|p7|||||||||
8610|Hutton Sandstone|41286|6|Mentioned|p114|||||||||
8610|Hutton Sandstone|41536|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|41681|6|Mentioned|p16|||||||||
8610|Hutton Sandstone|41707|5|Briefly described|p161|||||||||
8610|Hutton Sandstone|41712|6|Mentioned|p272|||See also p289.||||||18-SEP-18
8610|Hutton Sandstone|41724|5|Briefly described|p381|||||||||
8610|Hutton Sandstone|41725|6|Mentioned|p407|||||||||
8610|Hutton Sandstone|41992|4|Described|Fig.2 P183|||||||||
8610|Hutton Sandstone|42006|6|Mentioned|Fig.3 P23|||See also Fig.4 p24, 25.||||||18-SEP-18
8610|Hutton Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
8610|Hutton Sandstone|42067|4|Described|Appendix 2|||||||||
8610|Hutton Sandstone|42071|6|Mentioned|p116|||||||||
8610|Hutton Sandstone|42084|6|Mentioned|Fig.3 P356|||||||||
8610|Hutton Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
8610|Hutton Sandstone|42248|6|Mentioned|p410|||||||||
8610|Hutton Sandstone|42263|6|Mentioned|p14|Jurassic|Jurassic|||||||13-AUG-08
8610|Hutton Sandstone|42357|6|Mentioned|p11|||||||||
8610|Hutton Sandstone|42395|6|Mentioned|p80|||||||||
8610|Hutton Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
8610|Hutton Sandstone|42446|4|Described|p11|||||||||
8610|Hutton Sandstone|42447|5|Briefly described|p5 + Fig. 1|||||||||
8610|Hutton Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
8610|Hutton Sandstone|42474|5|Briefly described|p25|||||||||
8610|Hutton Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
8610|Hutton Sandstone|42496|4|Described|p140|||||||||
8610|Hutton Sandstone|42520|5|Briefly described|p6|||||||||
8610|Hutton Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
8610|Hutton Sandstone|42746|4|Described|p10|||See also Fig.6||||||
8610|Hutton Sandstone|42749|4|Described|p29, Fig.3 p28|||see also Fig.2 p27.||||||17-JAN-08
8610|Hutton Sandstone|42911|5|Briefly described|p13|||||||||
8610|Hutton Sandstone|42999|5|Briefly described|Table 2,p90||Jurassic|||||||
8610|Hutton Sandstone|43000|5|Briefly described|Fig.5,p112|||||||||
8610|Hutton Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
8610|Hutton Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
8610|Hutton Sandstone|43105|5|Briefly described|p15|||||||||
8610|Hutton Sandstone|43114|5|Briefly described|p10|||||||||
8610|Hutton Sandstone|43122|5|Briefly described|p7|||see also Fig. 2.||||||
8610|Hutton Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
8610|Hutton Sandstone|43185|6|Mentioned|6||Jurassic|||||||
8610|Hutton Sandstone|43436|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
8610|Hutton Sandstone|43539|14|Not recorded|p396|||||||||
8610|Hutton Sandstone|43582|6|Mentioned|Fig.5,p16,28||Middle Jurassic|||||||
8610|Hutton Sandstone|43591|6|Mentioned|p40|||||||||
8610|Hutton Sandstone|43602|6|Mentioned|191|||||||||
8610|Hutton Sandstone|43628|6|Mentioned|Fig.3|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
8610|Hutton Sandstone|43711|6|Mentioned|p18|||||||||
8610|Hutton Sandstone|43851|14|Not recorded|Tb p106,111||Middle Jurassic|||||||
8610|Hutton Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
8610|Hutton Sandstone|43910|14|Not recorded|p19,20|||Correlated with Marburg Sandstone||||||
8610|Hutton Sandstone|43912|14|Not recorded|p2,4|||(Moonie No.1)||||||
8610|Hutton Sandstone|43923|6|Mentioned|p14||Jurassic|||||||
8610|Hutton Sandstone|43924|14|Not recorded|p1,2,15|||Liassic-Bajocian boundary in age.||||||
8610|Hutton Sandstone|43925|14|Not recorded|p31,40-2,49-50,|||Figs.3,4||||||
8610|Hutton Sandstone|43982|14|Not recorded|Map Legend|||||||||
8610|Hutton Sandstone|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|43993|14|Not recorded|p101||Triassic|Ref. to Reeves.||||||
8610|Hutton Sandstone|43994|14|Not recorded|Map Legend|||||||||
8610|Hutton Sandstone|43996|14|Not recorded|p89|||||||||
8610|Hutton Sandstone|43998|4|Described|p14,17,map||Early Jurassic|||||||
8610|Hutton Sandstone|44016|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44019|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44020|14|Not recorded|p15,Tb.1,2,3||Early Jurassic|||||||
8610|Hutton Sandstone|44021|14|Not recorded|p232-234|||||||||
8610|Hutton Sandstone|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44023|4|Described|Tb.3,p11||Early Jurassic|||||||
8610|Hutton Sandstone|44026|14|Not recorded|p123,123|||||||||
8610|Hutton Sandstone|44028|14|Not recorded|Fig.2,p509,512-514||Jurassic|See Strat Table.||||||
8610|Hutton Sandstone|44031|14|Not recorded|p6,8,9-11||Late Jurassic|Artesian water.||||||
8610|Hutton Sandstone|44032|14|Not recorded|p46,map,p463,464|||= to Marburg Formation. Of Moreton Basin.||||||
8610|Hutton Sandstone|44042|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44084|14|Not recorded|p20,22,32|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44116|14|Not recorded|p28|||||||||
8610|Hutton Sandstone|44124|14|Not recorded|p2,5,10,17-19|||||||||
8610|Hutton Sandstone|44129|14|Not recorded|p95-96||Jurassic|||||||
8610|Hutton Sandstone|44133|5|Briefly described|p109, 105 Fig. 9.12|Late Jurassic|Middle Jurassic|Intertounges with Poolowanna Formation. Intertounges and is overlain by the Birkhead Formation.||||||
8610|Hutton Sandstone|44163|4|Described|p10-14||Jurassic|||||||
8610|Hutton Sandstone|44170|14|Not recorded|p20||Early Jurassic|||||||
8610|Hutton Sandstone|44171|14|Not recorded|p194,195,197,198|||||||||
8610|Hutton Sandstone|44174|14|Not recorded|p345,347||Early Jurassic|||||||
8610|Hutton Sandstone|44207|14|Not recorded|p116|||||||||
8610|Hutton Sandstone|44208|14|Not recorded|p94||Jurassic|||||||
8610|Hutton Sandstone|44304|14|Not recorded|p1|||||||||
8610|Hutton Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
8610|Hutton Sandstone|44379|14|Not recorded|p21|||||||||
8610|Hutton Sandstone|44381|14|Not recorded|p7-8|||||||||
8610|Hutton Sandstone|44390|14|Not recorded|p6,9,10,13,15,Tb.1|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44391|14|Not recorded|Map Legend|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44414|14|Not recorded|p113-115||Jurassic|||||||
8610|Hutton Sandstone|44415|14|Not recorded|Figs.1,2,p23,24||Early Jurassic|||||||
8610|Hutton Sandstone|44419|14|Not recorded|p278||Jurassic|||||||
8610|Hutton Sandstone|44420|14|Not recorded|p1,3-5,9,10,22,27,29||Early Jurassic|Fig.14.||||||
8610|Hutton Sandstone|44421|14|Not recorded|p1,6,10,11,13,14,19,||Jurassic|p20-21||||||
8610|Hutton Sandstone|44422|14|Not recorded|p149,153|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44426|14|Not recorded|p12|||Pelecypods, indeterminate plant fragments; 'may extend into the Middle Jurassic'.||||||
8610|Hutton Sandstone|44525|14|Not recorded|p520|||||||||
8610|Hutton Sandstone|44566|14|Not recorded|p15,16,Pl.2|||||||||
8610|Hutton Sandstone|44567|14|Not recorded|p11,13,14,Pls.1,2|||||||||
8610|Hutton Sandstone|44568|14|Not recorded|p3,4,Pl.1|||||||||
8610|Hutton Sandstone|44573|14|Not recorded|p97||Jurassic|||||||
8610|Hutton Sandstone|44585|14|Not recorded|p45-Fig.2|||||||||
8610|Hutton Sandstone|44610|14|Not recorded|p49,Tb.1|||||||||
8610|Hutton Sandstone|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
8610|Hutton Sandstone|44627|14|Not recorded|p139,141-144||Jurassic|||||||
8610|Hutton Sandstone|44636|14|Not recorded|p165,166|Bajocian|Lias|(Late Liassic-Bajocian)||||||
8610|Hutton Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
8610|Hutton Sandstone|44640|14|Not recorded|p30|||||||||
8610|Hutton Sandstone|44727|14|Not recorded|p304|||Marburg equivalent North of Roma.||||||
8610|Hutton Sandstone|44787|14|Not recorded|p122,Tb.p123,125,126||Early Jurassic|||||||
8610|Hutton Sandstone|44819|14|Not recorded|p89||Jurassic|Marine, sparse microfauna indicating brackish marine conditions.||||||29-JUN-16
8610|Hutton Sandstone|44852|14|Not recorded|p78||Jurassic|||||||
8610|Hutton Sandstone|45071|6|Mentioned|p136|||||||||
8610|Hutton Sandstone|45073|6|Mentioned|p58|||Geol. history||||||
8610|Hutton Sandstone|45110|2|Defined|p92|Early Jurassic|Early Jurassic|See also p9,24 and Fig.5.||||||17-JAN-08
8610|Hutton Sandstone|45145|6|Mentioned|p21|||||||||
8610|Hutton Sandstone|45168|6|Mentioned|p6|||||||||
8610|Hutton Sandstone|46791|6|Mentioned|Fig.6|||||||||
8610|Hutton Sandstone|46881|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
8610|Hutton Sandstone|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
8610|Hutton Sandstone|46984|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|46989|5|Briefly described|Table 1|||||||||
8610|Hutton Sandstone|48606|14|Not recorded|p5,6,11,13,14,19,21|||(H/55-8 ; G/55-12). Pl.1, Sh.1: Pl.2.||||||
8610|Hutton Sandstone|48634|14|Not recorded|p6,21||Jurassic|See also Figs. 2,6, Pl.1,2 p5,19. Lower-Middle Jurassic. (G54-14).||||||
8610|Hutton Sandstone|48900|4|Described|p52|||Lower - Middle Jurassic.||||||
8610|Hutton Sandstone|48919|2|Defined|p53|Middle Jurassic|Early Jurassic|See also p54-55. Lower to Middle Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|48920|3|Fully described|p44|||Jurassic age.||||||19-AUG-08
8610|Hutton Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin.||||||18-SEP-18
8610|Hutton Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin.||||||18-SEP-18
8610|Hutton Sandstone|50190|5|Briefly described|p85|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
8610|Hutton Sandstone|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, carbonaceous siltstone, mudstone and rare conglomerate.||||||
8610|Hutton Sandstone|60114|6|Mentioned|p16|||Oil-bearing deposits.  Geological Province:  Cooper - Eromanga Basins.||||||21-JUL-04
8610|Hutton Sandstone|60281|5|Briefly described|p27|||Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|60282|5|Briefly described|p11|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
8610|Hutton Sandstone|60386|6|Mentioned|p299|Middle Jurassic|Early Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
8610|Hutton Sandstone|60717|5|Briefly described|p40 Fig. 2, p42|Middle Jurassic|Early Jurassic|Overlies Poolowanna Formation; underlies and partially interfingers with Birkhead Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
8610|Hutton Sandstone|60993|6|Mentioned|p17, p6 Fig. 2|||Correlates with Marburg Subgroup units. Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|60998|5|Briefly described|p144|||Overlies Evergreen Formation. ||||||
8610|Hutton Sandstone|60999|5|Briefly described|p177, p178 Fig. 10|||Partly equivalent to Walloon Coal Measures.  Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|61000|5|Briefly described|p183|Bajocian|Aalenian|Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Koukandowie Formation. See also p255 Figs. 23, 24 and 25. ||||||
8610|Hutton Sandstone|61015|6|Mentioned|p44|||||||||
8610|Hutton Sandstone|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium-grained, sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|61310|6|Mentioned|p22|||Together with the Evergreen Formation, correlated with Marburg Formation and "Upper Bundamba Unit".||||||
8610|Hutton Sandstone|61312|6|Mentioned|p71, p78|Middle Jurassic|Early Jurassic|Sandstone, minor shale. Productive reservoir unit. See also p72 Fig. E9.||||||
8610|Hutton Sandstone|61377|5|Briefly described|p151, p153, p142, p148|Middle Jurassic|Early Jurassic|Thick sequence of stacked quartzose braided stream sands. Ssts are good quality reservoirs sealed by Walloon C.M.above (conformable). Conformable on Evergreen Fm. Geol.Prov: Surat Basin||||||07-FEB-11
8610|Hutton Sandstone|61611|6|Mentioned|p265 Fig. 3|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
8610|Hutton Sandstone|61613|6|Mentioned|p282-284, p287, p288, p282 Fig. 2|Middle Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|61614|6|Mentioned|p289, p293, p297, p290 Fig. 2|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
8610|Hutton Sandstone|61615|5|Briefly described|p302, p302 Fig. 2, p306, p307|Late Jurassic|Jurassic|Geological Province: Eromanga Basin. Comprises thick succession of stacked fluvial channel sandstones.||||||07-FEB-11
8610|Hutton Sandstone|61832|5|Briefly described|p187|Jurassic|Jurassic|On the MUNDUBERRA sheet.  Overlain by Injune Creek Group; overlies Evergreen Formation. Geological Province: Surat Basin.||||||03-JUL-06
8610|Hutton Sandstone|62028|5|Briefly described|p10 Fig. 1|||||||||
8610|Hutton Sandstone|62537|6|Mentioned|p191 Fig.2. |Middle Jurassic|Early Jurassic|Eromanga Basin.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|62730|5|Briefly described|p352 Fig. 1|Middle Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
8610|Hutton Sandstone|63218|6|Mentioned|p211 Fig.2. |Middle Jurassic|Early Jurassic|Surat Basin.||||Overlies Evergreen Formation. Is overlain by Eurombah Formation.||
8610|Hutton Sandstone|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|63748|6|Mentioned|p23|||Correlative of Marburg Subgroup.  Geological province: Surat Basin.||||||07-FEB-11
8610|Hutton Sandstone|63979|2|Defined|p34, Fig. 44|Callovian|Toarcian|Informally subdivided into "lower and upper Hutton Sandstone".Conformable on Poolowanna Fm; conformably overlain by Birkhead Fm. Max thickness: 244m.Dominantly sandstone, +rare interbedded siltstone+mudstone (more so in lower section). In Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|64048|6|Mentioned|p64 Tb. 2, p70|||Geological Province: Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Jurassic|Early Jurassic|Eromanga, Surat/Bowen Basins.||||Eromanga/Cooper Basins: underlies Birkhead Formation; overlies Poolowanna Formation. Surat/Bowen Basins: overlies Evergreen Formation; underlies Eurombah Formation.||10-DEC-15
8610|Hutton Sandstone|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Over Evergreen Fm;under Mulgildie C.M. Poorly sorted, medium-grained, feldspathic sublabile sandstone (at base) and fine-grained , well-sorted quartzose sandstone (at top); minor dark grey carbomaceous siltstone, mudstone and rare pebbl;e conglomerate.||||||19-AUG-08
8610|Hutton Sandstone|64665|5|Briefly described|p53 Fig.2, p60, p61.|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins. Correlates with Heifer Creek Sandstone Member (Clarence-Moreton Basin). Equivalent to Algebuckina Sandstone (Eromanga Basin). With the Eurombah Formation and Walloon Subgroup, forms the second of six cyclothems in the Surat Basin.||||Overlies Poolowanna and Evergreen Formations. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|64856|3|Fully described|p79, p82, p83 Fig.29, p85-88|Bathonian|Aalenian|Reeves (1947) regarded this as the top member of the Bundamba Series. Redesignated as a Formation by Mollan et al. (1965) with a type section near Hutton Creek, 19km ENE of Injune. Surat Basin. Mainly sandstone with interbedded siltstone and shale, minor mudstone and coal, continuous with the top part of the Marburg Subgroup in the Moreton Basin. Up to 266m thick. Age from palynoflora (units APJ33, 41, 42). Overlies Evergreen Formation. Underlies Walloon Coal Measures or Eurombah Formation.| | ||||29-NOV-17
8610|Hutton Sandstone|64857|5|Briefly described|p132-133, p113 Fig.3|||Conformably overlies Evergreen Formation. Consists mainly of sandstone and interbedded siltstone, shale with minor mudstone and coal. Surat Basin.||||||
8610|Hutton Sandstone|64858|6|Mentioned|p181 Tb.1, 187|||Surat Basin.||||||30-NOV-09
8610|Hutton Sandstone|65003|5|Briefly described|p8||Jurassic|Of Surat Basin. ||||||
8610|Hutton Sandstone|65096|5|Briefly described|p368, p370 Fig.2, p372, p373|||Of the Surat Basin. Formation top sometimes difficult to distinguish on wireline log.  Along with Evergreen Formation, compared with the  Marburg sub-group [sic] of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||Gradationally overlain by the Eurombah Formation of the Walloon Subgroup||
8610|Hutton Sandstone|65112|5|Briefly described|p323; p328; Fig11 p324; Fig16 p328|Early Cretaceous|Jurassic||178-166 Ma.|||Underlies the Walloon Coal Measures, overlies the Evergreen Formation.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
8610|Hutton Sandstone|65113|5|Briefly described|Fig 4 p340|Middle Jurassic|Middle Jurassic|Overlies the Evergreen Formation and underlies the Walloon CM.||||||
8610|Hutton Sandstone|65114|5|Briefly described|p385 Fig.3, p389|Middle Jurassic||Part of the Surat Basin, base of unit commonly cut by reactivation of major extensional marginal faults ||||||
8610|Hutton Sandstone|65116|5|Briefly described|p455, Fig 2 p437|Middle Jurassic|Middle Jurassic|Medium- fine grained quartzose-sublithic sandstone. Underlies the Walloon CM; overlies the Evergreen Formation, Surat Basin.||||||06-MAR-12
8610|Hutton Sandstone|65117|5|Briefly described|p461, 469,470, Fig 4 p465, Tbl 1 p466|Middle Jurassic|Aalenian|Surat Basin, Potential reservoir unit. Up to 266m thick in study area. Overlies Evergreen Formation. Fine to medium grained quartzose lithic sandstone. Is both thick bedded and cross-bedded. Deposited by meandering streams.||||||
8610|Hutton Sandstone|65119|5|Briefly described|p513, fig 2, Table 1, Fig 6-19|Middle Jurassic|Middle Jurassic|Surat Basin. Quartzose to sublabile sandstone, some siltstone, mudstone, minor conglomerate.  Age:168-188Ma. Fission Track ages:105-166Ma.||||||07-MAR-12
8610|Hutton Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
8610|Hutton Sandstone|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Early Jurassic|Of Eromanga Basin. Overlies Poolowanna Formation.||||||08-MAR-12
8610|Hutton Sandstone|65388|3|Fully described|p213-214, p210 Fig 74|Middle Jurassic|Middle Jurassic|Surat, Mulgildie, Moreton and Eromanga Basins. First used by Reeves (1947) for sandstones as the top member of the "Bundamba Series" north-west of Injune. Mollan & others (1965) raised it to formation status.  It is the most widespread Jurassic unit in the Great Artesian Basin.  72-266m thick. Overlies Evergreen Formation in Mulgildie Basin. Is continuous into, and forms the upper part of the Marburg Subgroup in the Moreton Basin to the east. Is overlain by  Mulgildie Coal Measures or Eurombah Formation. Palynofloral assemblages range from units APJ33 to APJ42 (Aalenian to Bathonian) (Green & others, 1997; Price, 1997). Fine to medium-grained, cream or brown, well sorted argillaceous, micaceous quartzose sandstone interbedded with mudstone.||||||
8610|Hutton Sandstone|65489|5|Briefly described|p10-13, p15, p26, p47, p49, p61, p96|Middle Jurassic|Early Jurassic|See also p154-155, p157-160. Eromanga Basin. 230m thick. Good to excellent reservoir quality. Predominantly anticlinal traps. Gas and oil reservoir accounting for 61% and 57% respectively of the Basin's production. Appears as Hutton Formation on p96, and as Hutton sandstone on p157.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.|Braided fluvial sandstone.|
8610|Hutton Sandstone|65925|5|Briefly described|Appendix 2.||||||||White, fine- to coarse-grained sandstone; with minor dark grey lenticular carbonaceous siltstone and shale interbeds.|
8610|Hutton Sandstone|66188|6|Mentioned|441|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin. ||||Overlies Poolowanna and Evergreen Formations; overlies Moolayember Formation unconformably. Is overlain by Injune Creek Group.|Medium grained sandstone, non-marine.|
8610|Hutton Sandstone|66915|5|Briefly described|p6 Fig.3, p12|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
8610|Hutton Sandstone|67133|5|Briefly described|p1-3, p5, p11-13, p19-21|||A carbon geostorage target reservoir, sealed by Walloon Subgroup. Braided stream deposits. 73 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (25-94%) and kaolinite (2-37%) is the dominant clay mineral. Mixed-layer clays are smectite-rich.||||Overlies Evergreen Formation. Is overlain conformably by Walloon Subgroup.|White to light grey, fine- to medium-grained, sublabile to quartzose sandstone, with dark grey micaceous or carbonaceous siltstone interbeds.|
8610|Hutton Sandstone|67323|5|Briefly described|p87-88, p93 Fig.12.3, p95 Fig.12.5, p96|Middle Jurassic|Early Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin; also probable reservoir (the unit is one of the main continuous aquifers in the region).||||Overlies Poolowanna and Moolayember Formations. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|67402|4|Described|p26, p26 tbl RRM4, p36|Bathonian|Toarcian|Eromanga, Mulgildie and Surat Basins. Forms an extensive aquifer in the Surat Basin. Primary porosity has been partially occluded by quartz overgrowths, kaolinite, chlorite and calcite cement.  Fluvial to fluvio-lacustrine depositional environment.  Maximum thickness of 275m. Major hydrocarbon reservoir with a potential to store up to 5.8 megatonnes of carbon dioxide in the Eromanga Basin and 1198 megatonnes in the Surat Basin.  See also p36 fig VEM6, VEM7,p37, p43 tbl HPB1, p104, p108-p110, p111 fig ERO8, p113 , p114 fig ERO13, p115, p117, p118, p146 fig SRT3, p148, p151, p154, p155 fig SRT17, p156, p161, p162, p239, p252, p253, p306.|f|||Overlies the Upper Poolowanna Formation and the Evergreen Formation. Overlain by the Birkhead Formation or Walloon Subgroup.|Thick sandstone unit that is interbedded with siltstone, shale and minor mudstone and coal.|
8610|Hutton Sandstone|67561|6|Mentioned|p53 Fig.3|||||||||
8610|Hutton Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Wallon CM. Underlain by Evergreen Formation.||
8610|Hutton Sandstone|68003|5|Briefly described|p55 Fig.3-m, p57 Fig.3-n, p61-63, p127.|Middle Jurassic|Early Jurassic|Surat Basin. Stratigraphic equivalent of upper part of Purlawaugh Formation. Toarcian to Aalenian. Maximum known thickness 275 m. Forms hill tops and small cliffs.||||Overlies Evergreen Formation. Unconformably overlies Deriah Formation; paraconformably overlies Gragin Conglomerate. Is overlain conformably by Walloon Coal Measures.|Well-sorted, medium- to coarse-grained quartzose sandstone, with some siltstone and mudstone, fragments of coal and silicified wood; local conglomerate beds.|
8610|Hutton Sandstone|68004|5|Briefly described|pp173-174.|||Excellent hydrocarbon reservoir potential and a major exploration target in NSW. Sealed by Walloon Coal Measures. A major hydrocarbon-producing reservoir in the Eromanga Basin in SW Queensland.||||||
8610|Hutton Sandstone|68008|4|Described|p186, p236, p238-240, p297|Middle Jurassic|Early Jurassic|Appears to have been defined by Gray (1972); 275m thick in GSQ Monto 1-2R. The type section is in the Eddystone 250k sheet area. Surat and Mulgildie Basins. Forms a N-S trending belt 27 x 5 km. Has zones of deep weathering.||||Conformably and gradationally overlies Evergreen Formation. Faulted against and/or unconformably overlies Cynthia beds. Is overlain conformably and gradationally by Mulgildie Coal Measures.|Pale grey to white, well-bedded, quartzose sandstone, minor granule conglomerate, and thin sandy siltstone beds.|
8610|Hutton Sandstone|68068|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Eromanga Basin. Subsurface only. Mainly fluvial, with possible aeolian and lacustrine deposition. Palynological age. Is replaced by Algebuckina Sandstone as it pinches out at Eromanga Basin margin.||||Overlies Algebuckina Sandstone. Is overlain by Birkhead Formation.|White, fine- to very coarse-grained and conglomeratic quartzose sandstone, flat to cross-bedded; common reworked clasts and minor interbeds of mudstone; carbonaceous partings.|
8610|Hutton Sandstone|68117|5|Briefly described|p346, p348-349|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies Evergreen Formation. Is overlain by Eurombah Formation or, where absent, Durabilla Formation.||
8610|Hutton Sandstone|68135|5|Briefly described|p52 fig 2b, p57 fig 4, p62, p64|Callovian|Toarcian|Surat Basin (QLD) and Eromanga Basin. Age derived from fossils of Osmundacaulis. Vertebrate body parts present, eg the sauropod Rhoetosaurus brownei.||||Overlies Evergreen and Poolawanna Formations. Is overlain by Walloon Coal Measures (Surat Basin) or Birkhead Formation (Eromanga Basin).|Fossiliferous and cross-bedded, iron-rich sandstone.|14-SEP-17
8610|Hutton Sandstone|68139|6|Mentioned|p23-25, 32|Middle Jurassic|Early Jurassic|Surat Basin. A major aquifer. Hydrocarbons present are thought to be connected with fault leakage.||||Overlies Evergreen Formation. Is overlain by Walloon Subgroup (Injune Creek Group).||
8610|Hutton Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
8610|Hutton Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Evergreen Formation and Precipice Sandstone, are all mapped under the symbol, Jb.||||||
8610|Hutton Sandstone|68576|5|Briefly described|Q_4: p3, p12 Fig.14, p17, p22, p24|Middle Jurassic|Early Jurassic|Surat Basin. A widely-used aquifer in the Great Artesian Basin. Extends E into the Clarence-Moreton Basin and W into the Eromanga Basin. Sediments deposited by meandering streams on a broad floodplain.||||Conformably overlies Evergreen Formation. Is overlain by Walloon Coal Measures.|White to light grey, sub-labile to quartzose sandstone with interbedded siltstone, shale, minor mudstone and coal: partly arkosic, and with a higher proportion of siltstone and shale to the S.|
8610|Hutton Sandstone|68679|6|Mentioned|p312-313, p338|Jurassic|Jurassic|Northern New England Orogen.||||||
8610|Hutton Sandstone|68731|6|Mentioned|pp207-211|||||||Unconformably underlain by the Nappamerri Group and the Tinchoo Formation.||
8610|Hutton Sandstone|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
8610|Hutton Sandstone|69019|5|Briefly described|p85 Fig.21.|Middle Jurassic|Early Jurassic|Southern Eromanga Basin.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|69023|5|Briefly described|p79, p89 Fig.20, p90-91, p191-192|Middle Jurassic|Middle Jurassic|Defined by Reeves (1947) from outcrops in Roma (Qld); applied by Kapel (1966) to subsurface Early-Middle Jurassic sandstones in Eromanga Basin. Up to 260m thick. Equivalent to part of Algebuckina Sandstone. Stratigraphic wells intersection data.||||Overlies Patchawarra Formation unconformably, and overlies and intertongues with Poolowanna Formation. Is overlain conformably by Birkhead Formation.|White fine- to very coarse-grained quartzose sandstone, flat to planar cross-bedded; minor channel lag conglomerate and brown laminated and carbonaceous mudstone/siltstone interbeds. Local in situ duricrusts of calcrete and silcrete.|
8610|Hutton Sandstone|69457|5|Briefly described|p41:2-5|||Eromanga Basin. Lateral equivalent of lower Algebuckina Sandstone. ||||Conformably overlies, and locally intertongues with, Poolowanna Formation. Is overlain conformably by Cadna-owie Formation or disconformably by Bulldog Shale.||12-JUL-16
8610|Hutton Sandstone|69574|6|Mentioned|p23-24|Middle Jurassic|Early Jurassic|Surat Basin. A major regional aquifer.||||Is overlain by Walloon Subgroup.||
8610|Hutton Sandstone|69582|5|Briefly described|p36, p38, p65-p66|Middle Jurassic|Middle Jurassic|Surat Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Evergreen Formation and the Poolowanna Formation. Overlain by the Walloon Coal Measures and the Birkhead Formation.|Sandstone.|
8610|Hutton Sandstone|69594|4|Described|p519, p524-526, p531, p533-536,p545,p573|Bathonian|Aalenian|Reeves (1947). Eromanga, northern Surat Basins; originally defined in the latter. Kapel (1966) included Early and Middle Jurassic sandstones in the Cooper Basin region (probably included the Poolowanna Formation). Braided fluvial deposits. Mostly 90-210m thick; up to 266m. The most widespread Jurassic unit in the Great Australian Superbasin; constitutes the upper Marburg Subgroup in the Clarence-Moreton Basin. Late Toarcian to Callovian. The most important hydrocarbon reservoir in the Eromanga Basin, but minor in the Surat Basin. The most heavily used groundwater aquifer, and the main hot aquifer (geothermal energy) target, in the Basin.||||Conformably overlies Poolowanna (and intertongues with it) and Evergreen Formations. Is overlain conformably by Birkhead and Eurombah Formations and Walloon Coal Measures.|Quartzose to sublabile sandstones with interbedded siltstone and shale and minor coal and mudstone.|
8610|Hutton Sandstone|69633|5|Briefly described|p3-4, p7, p10, p14, p21, Appendix 6.|Middle Jurassic|Early Jurassic|Surat Basin. Fluviatile braided-stream sediments.||||Overlies Evergreen Formation. Is overlain by Walloon Coal Measures.||
8610|Hutton Sandstone|69673|6|Mentioned|p154, p155 fig 127|Jurassic|Jurassic|||||Overlies Poolowanna Formation, overlain by Birkhead Formation||
8610|Hutton Sandstone|69681|5|Briefly described|p74-87|Middle Jurassic|Early Jurassic|Generally high permeability, although permeability decreases by an order of magnitude below ~1500m. Potential for CO2 geostorage, sealed by Walloon Subgroup, discussed. Mineralogy and likely chemical changes from CO2 injection discussed.||||||
8610|Hutton Sandstone|69682|4|Described|p91-110|Middle Jurassic|Middle Jurassic|Laterally extensive: Surat Basin, extending into Moreton and Eromanga Basins. Average thickness 120-180m, to maximum of 266m. Mineralogy discussed in detail. Potential CO2 reservoir, but its immature mineralogy indicates potential geochemical reactivity during CO2 sequestration. ||||Overlies Evergreen Formation. Is overlain by Walloon Subgroup (Injune Creek Group).|Mica-rich, sublithic to quartzose, well-sorted, fine- to medium-grained sandstone, with interbedded siltstone and mudstone, rip-up clasts and pebble lags; minor coal and mudstone.|
8610|Hutton Sandstone|69790|6|Mentioned|p1062, p1064 Fig.3, p1066-1069, p1073|Middle Jurassic|Early Jurassic|See also p1077-1078. Surat Basin.||||Conformably overlies Evergreen Formation. Is overlain by Durabilla Formation.||
8610|Hutton Sandstone|69797|5|Briefly described|p17 Fig.2|||Age: Middle Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
8610|Hutton Sandstone|69946|3|Fully described|p10-15, p51, p57-58, p60-61, p68-78|Middle Jurassic|Middle Jurassic|Reeves (1947) used the name for a Member of the 'Bundamba series' in the Roma area (Qld). The name was applied to sandstone of 'Lower-Middle Jurassic age' in the Cooper region by Kapel (1966). Type section is an outcrop on Westgrove Station, N of Injune (Qld). Thickness from 40m to >360m, thickening northwards. Wireline log correlations.||||Intertongues with and overlies Poolowanna Formation. Intertongues with or is gradational into overlying Birkhead Formation. Passes laterally into Algebuckina Sandstone.|Mineralogically mature, fine- to coarse-grained quartzose sandstone with minor siltstone interbeds. Thin calcite and silica-cemented horizons occur in upper parts.|
8610|Hutton Sandstone|69947|5|Briefly described|p3, p5-7, p13 Fig.7.2, p16-17 Figs.7.5-6|Late Jurassic|Middle Jurassic|See also p21-27 Figs.7.10-16. Eromanga Basin. Sand-rich lowstand deposits form the principal hydrocarbon reservoirs throughout the Basin. Paleogeography maps. Generalised stratigraphic section.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.|Thick, laterally extensive, amalgamated sandstones.|
8610|Hutton Sandstone|69948|6|Mentioned|p3|||Cooper region, Eromanga Basin.||||||
8610|Hutton Sandstone|70036|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Surat Basin. Included in a mapped unit of fluvial and lacustrine sequences: lithic to quartzose sandstone, siltstone, mudstone, claystone and coal.||||||
8610|Hutton Sandstone|70374|5|Briefly described|p808, p809, figure 1,|Callovian|Aalenian|Previously considered Aalenian - Bathonian age. Radiometric dating of tuffs in overlying Walloon Coal Measures suggests Hutton Sandstone may extend into the Callovian.||||Overlies Evergreen Formation. Underlies Walloon Subgroup conformably. Underlies Eurombah, Durabilla, Birkhead Formations.||28-SEP-16
8610|Hutton Sandstone|70628|6|Mentioned|p951, 953, p952 Fig 4|Aalenian|Aalenian|Erosive base forms a sequence boundary for the K-sequence (Hoffman et al 2009) of the Surat Basin.||||Unconformably overlies Evergreen Formation. Comformably (gradationally?) underlies Durabilla Formation, Eurombah Formation, Walloon Subgroup.|Sandstone, erosive base, fluvial sediments fine upwards.|
8610|Hutton Sandstone|70725|6|Mentioned|p13|Middle Jurassic|Middle Jurassic|Surat Basin.||||Is overlain by Durabilla and Eurombah Formations (Walloon Subgroup).||
8610|Hutton Sandstone|70821|5|Briefly described|p21 Fig.2.6, p79-80|Jurassic|Jurassic|A high-quality aquifer in the Great Artesian Basin. Appears as Hutton Sandstone Formation in Fig.2.6. Hydrochemistry mentioned.||||Overlies Evergreen Formation. Is overlain by Birkhead Formation or Walloon Coal Measures (Injune Creek Group).||
8610|Hutton Sandstone|70823|5|Briefly described|p6, p43-p44, p78|Early Cretaceous|Early Jurassic|Eromanga Basin. See also Hutton Formation. Up to 230m thick. Deposited in a braided fluvial environment with some aeolian influence.||||Intertongues with the Namur Sandstone. Overlies the Poolowanna Formation. Overlain by and interfingers with the Birkhead Formation.||
8610|Hutton Sandstone|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Poolowanna Formation. Overlain by the Birkhead Formation.||
8610|Hutton Sandstone|71282|6|Mentioned|p456, p457 Fig.1, p460|||Amalgamated braided channels passing up into occasional meandering channels. Appears as Durabilla & Hutton Formation on p460.||||Is overlain by Durabilla Formation.||
8610|Hutton Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
8610|Hutton Sandstone|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3  p17-p18|Callovian|Aalenian|Eromanga Basin. First used by Reeves (1947) for a member of the 'Bundamba series'. It was subsequently redefined by Kapel (1966b) as sandstone of 'Lower-Middle Jurassic age' in the Cooper region. A type section outcropping on Westgrove station was designated by Reeves (1947). Age derived from palynology. Sedimentary features and palaeoenvironment are discussed in some detail. Spore-pollen zone is given in Ch5 p57. This unit was the source of the first discovery of commercial quantities of oil in the Eromanga Basin. A complete sedimentary facies log is given in Ch5 p68. Sequence stratigraphy detailed in Ch7 as is source rock potential and hydrocarbon geochemistry (Ch8). Seal and reservoir characteristics discussed in Ch11. This unit is one of the primary sources of petroleum production in the Eromanga Basin. See also Ch5 p12-p15, Ch5 p31, Ch5 p51, Ch5 p57-p58, Ch5 p67-p74, Ch5 p76, Ch6 p5-p6, Ch7 p3, Ch7 p5-p7, Ch7 p10, Ch7 p13, Ch7 p16, Ch7, Ch8 p p21, Ch7 p27, Ch8 p4, Ch8 p10, Ch8 p13-p14, Ch9 p5, Ch9 p11, Ch10 p3, Ch10 tbl 10.1, Ch10 p6-p8, Ch10 p14, Ch10 p17-p20, Ch11 p2-p5, Ch11 p7-p8, Ch11 p14, Ch12 p2, Ch12 p5, Ch12 p12, Ch12 p14, Ch13 p2-p4, Ch13 p6-p10, Ch13 p19, Ch13 p21, Ch13 p23-p24, Ch13 p37-p38, Ch14 p3, Ch14 p5-p7.||||Overlies the Poolowanna Formation. Conformably overlain by the Birkhead Formation. Equivalent to the Algebuckina Sandstone.|Fine to coarse-grained, planar to cross-bedded, quartzose sandstone with minor siltstone interbeds. Thin calcite and silica cemented horizons occur in the Hutton Sandstone.|
8610|Hutton Sandstone|71805|5|Briefly described|p76-p77, p86|Bajocian|Toarcian|Eromanga Basin and Northern Surat Basin.||||Overlies the Poolowanna Formation and the Evergreen Formation.||
8610|Hutton Sandstone|71806|6|Mentioned|p484-p485|Jurassic|Jurassic|Surat Basin.||||||
8610|Hutton Sandstone|72297|5|Briefly described|p739, p742-743, p745, p748, p751, p761|||The most important reservoir rock in the Eromanga Basin; sealed by Birkhead Formation. Gas produced from 31 fields. Minor oil reserves in fault-related traps. A major aquifer with excellent prospects for HSA (hot sedimentary aquifer) geothermal energy.||||||
8610|Hutton Sandstone|72298|5|Briefly described|p796, p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW). A source of groundwater in the Monto area. Main confined aquifers and confining beds, generally producing flowing artesian water bores.||||Overlies Poolowanna FZ and Boxvale Sandstone Member (Evergreen FZ) conformably and Moolayember FZ unconformably. Underlies Birkhead or Eurombah FZs (Injune Creek Group) and Walloon Coal Measures.||
8610|Hutton Sandstone|72921|4|Described|p8-14, p15 Fig.2, p16-25, p27-32.|Middle Jurassic|Middle Jurassic|First significant regional aquifer above proposed Precipice Sandstone CO2 storage reservoir in Surat Basin, but extends across the Clarence-Moreton and Eromanga Basins as well. Braided and meandering fluvial to deltaic depositional system interpreted. Mineralogy discussed. Sedimentology & facies discussed. See also p36-41, p42-54, p56, p59, p61-67, p69-72, p77-78, p80, p81 Fig.43, p83 Fig.44-45.||||Partially overlies and is laterally equivalent to Evergreen Fm, Poolawanna Fm, Marburg Fm, and partially underlies and is laterally equivalent to Durabilla Fm, Eurombah Fm and Birkhead Fm.|Includes fragments of volcanic rocks within the fine to medium-grained thick-bedded quartzose to sublabile sandstone and tuffaceous layers. Also includes siltstone, shale, minor coal and fossils.|
8610|Hutton Sandstone|73113|5|Briefly described|p. 19, 22-24, 26-27, 31, 36-37, 41...|||Surat Basin. Groundwater model divides unit into upper and lower layers. Lower layer = tight aquifer. Upper layer = partial aquifer. More locations: p. 49, 61, 67, 69, 76, 79-80, 93, 98, 116-117, 119, 123, 126-130, 147-149, 152-153, 158-160, 162, 164-173, 177, 179, 191-193, 200.||||Underlain by Evergreen Formation. Overlain by Durabilla Formation.|Upper portion is typically characterised by thick, indurated sandstones; lower portion comprises more thinly interbedded sandstone/siltstones.|
8610|Hutton Sandstone|73147|6|Mentioned|p128|Jurassic|Jurassic|Eromanga Basin.||||||
8610|Hutton Sandstone|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil, hydrocarbon source.||||||
8610|Hutton Sandstone|73193|6|Mentioned|p369|Callovian|Aalenian|Surat Basin.||||Overlain by Walloon Subgroup (Injune Creek Group).||
8610|Hutton Sandstone|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|73203|6|Mentioned|p652|||Found in the Jundah 1 well, central Queensland.||||||
8610|Hutton Sandstone|73251|6|Mentioned|p49, p62|Middle Jurassic|Middle Jurassic|Eromanga Basin. Deposited in a braided fluvial setting with aeolian influence. Contains[?] oil.||||Underlain by Poolowanna Formation. Overlain by [and equivalent to?] Birkhead Formation. Equivalent to Algebuckina Sandstone.||
8610|Hutton Sandstone|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Source rock that hosts oil.||||Underlain by Poolowanna Formation. Overlain by Birkhead Formation.||
8610|Hutton Sandstone|73393|6|Mentioned|p20-23|Bajocian|Aalenian|Surat and Eromanga Basins. Previously reported (in error) to have hosted the sauropod Rhoetosaurus brownei.||||Underlain by Evergreen Formation. Overlain by Birkhead Formation and Eurombah Formation (Injune Creek Group).||
8610|Hutton Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p164, p179|Jurassic|Jurassic|Eromanga Basin. Braided fluvial depositional environment.|ca 178-160 Ma|||Overlies Poolowanna Formation, underlies Birkhead Formation||
8610|Hutton Sandstone|73600|6|Mentioned|p190-191|Aalenian|Toarcian|Somewhat uniform thickness.||||Underlain by Evergreen Formation.||
8643|Idracowra Sandstone|22826|6|Mentioned|Fig 2 on p565|Devonian|Devonian|||||||
8643|Idracowra Sandstone|23858|5|Briefly described|p916||Late Devonian|Of Finke Group. Underlain by Horseshoe Bend Shale. Geological Province: Amadeus Basin.||||||27-SEP-06
8643|Idracowra Sandstone|30544|6|Mentioned|p51|||On map legend||||||
8643|Idracowra Sandstone|31566|6|Mentioned|p244|||Devonian.||||||
8643|Idracowra Sandstone|31567|3|Fully described|p288|||Refers Wells et al. (1966).||||||
8643|Idracowra Sandstone|33971|3|Fully described|p30|||Refers Wells et al. (1966)||||||
8643|Idracowra Sandstone|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
8643|Idracowra Sandstone|35102|6|Mentioned|Fig.17|||||||||
8643|Idracowra Sandstone|42504|5|Briefly described|p81|||||||||
8643|Idracowra Sandstone|42699|5|Briefly described|map legend|Devonian||||||||
8643|Idracowra Sandstone|43035|5|Briefly described|p26|||Of Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|44133|6|Mentioned|p44|||||||||
8643|Idracowra Sandstone|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Dev-Carb. Part of Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
8643|Idracowra Sandstone|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carb.||||||
8643|Idracowra Sandstone|44393|6|Mentioned|Fig.1|Devonian|Cambrian|Correlates with Santo Sandstone. Dev-Camb.||||||
8643|Idracowra Sandstone|45041|4|Described|p105|||Of the Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|48865|2|Defined|p.5.Fig.34|Carboniferous|Devonian|On many figures. Fig.4,21,29,33,35,Pl.10,11. Unit of Finke Group. Devn.Carb. (G53-5,6).||||||
8643|Idracowra Sandstone|48890|14|Not recorded|Tb.3,p.51,53|||Defn. on Tech.File E/53-8.||||||
8643|Idracowra Sandstone|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Fine to medium grained quartz sandstone.||||||
8643|Idracowra Sandstone|65309|4|Described|p6 Table 1, pp13-14. |Devonian|Devonian|Commonly exposed below Mesozoic sediments in basal parts of mesas. Usually less than 6m thick, but up to 50m in bores.||Unit in Finke Group.||Overlies Horseshoe Bend Shale. Is overlain disconformably by Algebuckina Sandstone.|Fine to medium quartz sandstone, white to pale yellow; thinly bedded, weakly kaolinitic.|
8643|Idracowra Sandstone|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 245 m.||||Overlies Horseshoe Bend Shale. Is overlain by Crown Point Formation.||
8643|Idracowra Sandstone|69438|3|Fully described|p23:2-3, 40-42|Late Devonian|Late Devonian|Wells et al. (1966). Includes the lateral equivalent, Santo Sandstone, which name has been abandoned. Amadeus Basin. It is 52m thick at the type section, 6.5km SSW of Idracowra Station; reaches 280m thick at Mount Hakea. Sediment supply was from the NW, unlike a SW source for the lower Finke Group.||Finke Group.||Transitionally overlies Horseshoe Bend Shale (locally disconformably).|Dominated by sedimentary cycles, average 2m thick, of typically white to pale grey medium-grained sandstone, some of which is pebbly. Contains mudclasts, current lineations and mudcracks.|12-JUL-16
8643|Idracowra Sandstone|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Horseshoe Bend Shale and (disconformably) Langra Formation.|Sandstone and claystone.|12-JUL-16
8643|Idracowra Sandstone|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Langra Formation||
8643|Idracowra Sandstone|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
8643|Idracowra Sandstone|73085|6|Mentioned|p1|late Devonian|late Devonian|[Unclear relationship with Horseshoe Bend Shale].||Finke Group||Underlain by Langra Formation. Equivalent to Brewer Conglomerate (Pertnjara Group).||
8643|Idracowra Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
8663|Illbillie Adamellite|23818|6|Mentioned|p40 Fig.11|||||||||
8663|Illbillie Adamellite|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8663|Illbillie Adamellite|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8663|Illbillie Adamellite|34537|6|Mentioned|p41|||||||||
8663|Illbillie Adamellite|35628|4|Described|Table 1|||Also P10||||||
8663|Illbillie Adamellite|43052|5|Briefly described|p162|||||||||
8663|Illbillie Adamellite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Southern granites Suite (Kulgera Supersuite).||||||
8663|Illbillie Adamellite|73090|5|Briefly described|Appendix.|Mesoproterozoic|Mesoproterozoic||||||Adamellite.|
8664|Illeroo Pedoderm|31532|3|Fully described|Table 1|||||||||
8684|Indulkana Shale|22746|5|Briefly described|Fig.3 p515|Ordovician|Ordovician|||||||
8684|Indulkana Shale|22922|6|Mentioned|34|||||||||
8684|Indulkana Shale|23282|2|Defined|p82||Late Ordovician|Informally introduced by Packham and Webby (1969) and use by Krieg (1973). Probably equiv. to Horn Valley Siltstone of Amadeus Basin. Age: Late Ordovician 450 - 455 Ma. of Munda Group, Officer Basin.||||||
8684|Indulkana Shale|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
8684|Indulkana Shale|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|||||||
8684|Indulkana Shale|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
8684|Indulkana Shale|24067|5|Briefly described|p249 Fig.2|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
8684|Indulkana Shale|24112|5|Briefly described|p254 Fig.2|Late Ordovician|Late Ordovician|Of the Munda Group. Geological Province: Officer Basin||||||
8684|Indulkana Shale|30540|6|Mentioned|p68|||Possible source rock||||||
8684|Indulkana Shale|30544|6|Mentioned|p49|||||||||
8684|Indulkana Shale|30807|6|Mentioned|p102|||Suggested map symbol.||||||
8684|Indulkana Shale|31457|6|Mentioned|p13|||||||||
8684|Indulkana Shale|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
8684|Indulkana Shale|33738|6|Mentioned|p48|||||||||
8684|Indulkana Shale|35628|4|Described|Table 3|||||||||
8684|Indulkana Shale|36096|6|Mentioned|Fig.3|||||||||
8684|Indulkana Shale|36128|6|Mentioned|p13|||||||||
8684|Indulkana Shale|36491|6|Mentioned|Fig.2|||||||||
8684|Indulkana Shale|36920|6|Mentioned|Table 1|||||||||
8684|Indulkana Shale|38022|6|Mentioned|Fig.4|||||||||
8684|Indulkana Shale|38329|6|Mentioned|p194|||||||||
8684|Indulkana Shale|40136|5|Briefly described|p28|||||||||
8684|Indulkana Shale|43052|5|Briefly described|Fig. 2.10|||||||||
8684|Indulkana Shale|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
8684|Indulkana Shale|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
8684|Indulkana Shale|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
8684|Indulkana Shale|43743|6|Mentioned|Fig.2,p33||Late Ordovician|||||||
8684|Indulkana Shale|44109|5|Briefly described|p22 Fig. 23|Ordovician|Ordovician|Geological Province: central Officer Basin.||||||
8684|Indulkana Shale|44133|4|Described|p40-41, 4 Fig. 7.2|Ordovician|Ordovician|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Overlies Mount Chandler Sandstone. Maximum Thickness: 60m. Age: 460 +/- 15-438 +/- 10 Ma (Webb, 1978, Womer et al , 1987). Underlies: Blue Hills Sandstone.||||||02-MAY-13
8684|Indulkana Shale|45149|6|Mentioned|p43|||See also Table 1 and P15.||||||
8684|Indulkana Shale|49792|5|Briefly described|Fig.5|||||||||
8684|Indulkana Shale|65313|5|Briefly described|p578, p579, p580 Fig. 6|Ordovician|Ordovician|Officer Basin. Ungoolya 1 well. ca 468 Ma from Horn Valley Sandstone correlation 460 +/- 15 Ma Rb-Sr isochron date.||Of Munda Group.||Overlies Mount Chandler Sandstone, underlies Blue Hills Sandstone.||26-MAR-12
8684|Indulkana Shale|71146|5|Briefly described|p6|Late Ordovician|Middle Ordovician|Officer Basin.||Munda Group||Overlies the Mount Chandler Sandstone. Overlain by the Blue Hills Sandstone.|Shale.|
8684|Indulkana Shale|72478|6|Mentioned|p8|Late Ordovician|Late Ordovician|Officer Basin.|c.450 Ma-445 Ma|Munda Group||Overlies the Mt Chandler Sandstone. Underlies the Blue Hills Sandstone.||25-MAR-21
8684|Indulkana Shale|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Shale, maroon, minor green, calcareous; thin white flaggy siliceous sandstone interbeds; rare limestone lenses. Rippled, dessicated, bioturbated.|
8710|Injune Creek Group|12597|5|Briefly described|p492 Tb.1, p496, p497, p499|Kimmeridgian|Callovian|Of Swarbrick (1973). Eromanga Basin.|||Includes Westbourne, Birkhead and Eurombah Formations; Adori and Springbok Sandstones; and Walloon Subgroup.|Conformably overlies Hutton Sandstone.||
8710|Injune Creek Group|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Jurassic|Middle Jurassic|In Surat Basin, Eromanga Basin.||||||
8710|Injune Creek Group|22857|5|Briefly described|p296-7 Tb.22.1, p314|Tithonian|Bajocian|Includes the Eurombah Formation, Walloon Coal Measures, Springbok, Pilliga and Gubberamunda Sandstones. Geological Province: Surat Basin.||||||
8710|Injune Creek Group|22865|4|Described|p314,Table22.1p296-7|Tithonian|Bajocian|||||||
8710|Injune Creek Group|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
8710|Injune Creek Group|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
8710|Injune Creek Group|23425|5|Briefly described|Plate 10.2|||||||||
8710|Injune Creek Group|23430|4|Described|p525|||Also see p524 Table 14.7. Eromanga Basin Province.||||||
8710|Injune Creek Group|23799|5|Briefly described|p48 Fig. 3|Callovian|Bathonian|Includes the Walloon Coal Measures and the Birkhead Formation.  Geological Province: Surat Basin.||||||
8710|Injune Creek Group|23883|5|Briefly described|p129 Fig. 11.2|Late Jurassic|Late Jurassic|Includes the Westbourne Fm., Adori Sandstone and Birkhead Formation.  Geological Province: Sydney Basin.||||||
8710|Injune Creek Group|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
8710|Injune Creek Group|24068|4|Described|p271|Late Jurassic|Middle Jurassic|Geological Province: Surat Basin.  Maximum thickness: 775m.||||||
8710|Injune Creek Group|24069|5|Briefly described|p284|Late Jurassic|Middle Jurassic|Geological Province: Surat Basin.||||||
8710|Injune Creek Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
8710|Injune Creek Group|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|29385|6|Mentioned|p80|||Also P81&82.Jurassic.||||||
8710|Injune Creek Group|29387|6|Mentioned|p30|||Table 5 also.||||||
8710|Injune Creek Group|29389|6|Mentioned|p19|||Middle Jurassic.||||||
8710|Injune Creek Group|29393|6|Mentioned|Table 4|||Jurassic.||||||
8710|Injune Creek Group|29591|5|Briefly described|p69|||||||||
8710|Injune Creek Group|29721|6|Mentioned|p246|||||||||
8710|Injune Creek Group|30021|6|Mentioned|p90|||||||||
8710|Injune Creek Group|30024|6|Mentioned|p331|||||||||
8710|Injune Creek Group|30102|4|Described|p21|||See also p22-25. Middle to Upper Jurassic age.||||||22-AUG-18
8710|Injune Creek Group|30103|5|Briefly described|p9|||Table 3 on p9. Middle to Upper Jurassic age.||||||22-AUG-18
8710|Injune Creek Group|30104|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|Middle to Upper Jurassic age.||||||
8710|Injune Creek Group|30457|6|Mentioned|p96|||||||||
8710|Injune Creek Group|30461|6|Mentioned|p100|||||||||
8710|Injune Creek Group|30508|6|Mentioned|p81|||See also p90. Early Jurassic palynology||||||22-AUG-18
8710|Injune Creek Group|30691|4|Described|p15|||See also Table 4||||||
8710|Injune Creek Group|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30694|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30695|4|Described|Table 4|||Middle to Upper Jurassic age||||||
8710|Injune Creek Group|30696|4|Described|Table 4|||Middle-Upper Jurassic age||||||
8710|Injune Creek Group|30698|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|30700|6|Mentioned|p22|||Middle-Upper Jurassic. Map||||||
8710|Injune Creek Group|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
8710|Injune Creek Group|30853|5|Briefly described|Table 3|||Middle to Upper Jurassic age||||||
8710|Injune Creek Group|30854|4|Described|Table 4|||Middle-Upper Jurassic||||||
8710|Injune Creek Group|30855|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|30856|4|Described|p10|||Lower to Upper Jurassic age. On Table 3||||||
8710|Injune Creek Group|30857|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8710|Injune Creek Group|30915|6|Mentioned|p98|||||||||
8710|Injune Creek Group|31098|6|Mentioned|p5|||M. - U. Jurassic||||||
8710|Injune Creek Group|31116|4|Described|p27|||See also Table 2. Jurassic||||||
8710|Injune Creek Group|31117|6|Mentioned|p378|||Jurassic||||||
8710|Injune Creek Group|31121|6|Mentioned|p385|||||||||
8710|Injune Creek Group|31369|6|Mentioned|Table 4|||Jurassic||||||
8710|Injune Creek Group|31425|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31430|5|Briefly described|Table 1|||M.-U.Jurassic||||||
8710|Injune Creek Group|31431|4|Described|Table 3|||M.-U.Jurassic||||||
8710|Injune Creek Group|31432|4|Described|Table 1|||Middle-Upper Jurassic||||||
8710|Injune Creek Group|31436|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31438|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|32040|6|Mentioned|p886|||Geological map||||||
8710|Injune Creek Group|32136|6|Mentioned|p3|||Basal section early Bajocian||||||
8710|Injune Creek Group|32138|6|Mentioned|p396|||||||||
8710|Injune Creek Group|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.-U.Jurassic||||||22-AUG-18
8710|Injune Creek Group|32797|4|Described|Table 4|||M.-U. Jur.||||||
8710|Injune Creek Group|33067|4|Described|Table 1|||Includes the Westbourne and Birkhead Formations and the Adori Sandstone.||||||07-JUL-04
8710|Injune Creek Group|33069|4|Described|p7|||M.-U.Jur.||||||
8710|Injune Creek Group|33070|4|Described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33071|4|Described|p6|||M.-U.Jur.||||||
8710|Injune Creek Group|33078|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33079|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.- U.Jur.||||||22-AUG-18
8710|Injune Creek Group|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33082|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33087|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33088|4|Described|Table 3|||Jurassic||||||
8710|Injune Creek Group|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33090|4|Described|Table 4|||Mid.-U.Jur.||||||
8710|Injune Creek Group|33092|5|Briefly described|p6|||Strat. table||||||
8710|Injune Creek Group|33094|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33096|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33176|6|Mentioned|p175|||||||||
8710|Injune Creek Group|33367|4|Described|Table 1|||See also p3. suggested type sect. p15.||||||22-AUG-18
8710|Injune Creek Group|33371|3|Fully described|p57|||||||||
8710|Injune Creek Group|33449|4|Described|Table 1|||Mid.-U.Jur.||||||
8710|Injune Creek Group|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|M.-U.Jur.||||||22-AUG-18
8710|Injune Creek Group|33638|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|33639|5|Briefly described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33640|4|Described|Table 3|||M.-U.Jur.||||||
8710|Injune Creek Group|33643|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33647|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33648|6|Mentioned|p14|||Equiv. Strat. Table.||||||
8710|Injune Creek Group|33672|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|33774|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|33825|6|Mentioned|Table 4|||||||||
8710|Injune Creek Group|33832|5|Briefly described|p11|||Strat. & correlation||||||
8710|Injune Creek Group|34061|6|Mentioned|p54|||||||||
8710|Injune Creek Group|34091|5|Briefly described|Table 1|||Jur.||||||
8710|Injune Creek Group|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
8710|Injune Creek Group|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|34212|6|Mentioned|p2|||Jurassic||||||
8710|Injune Creek Group|34254|6|Mentioned|p481|||||||||
8710|Injune Creek Group|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||
8710|Injune Creek Group|34543|6|Mentioned|p98|||||||||
8710|Injune Creek Group|34613|4|Described|Table 4|||||||||
8710|Injune Creek Group|34905|6|Mentioned|p531|||||||||
8710|Injune Creek Group|35148|6|Mentioned|Fig.1|||||||||
8710|Injune Creek Group|35239|6|Mentioned|Fig.4|||||||||
8710|Injune Creek Group|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
8710|Injune Creek Group|35560|4|Described|p289|||||||||
8710|Injune Creek Group|35562|6|Mentioned|p295|||Stratigraphy||||||
8710|Injune Creek Group|35663|6|Mentioned|p124|||||||||
8710|Injune Creek Group|35811|5|Briefly described|Table 3|||||||||
8710|Injune Creek Group|35937|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
8710|Injune Creek Group|36233|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|36243|6|Mentioned|p74|||See also Table 6A.||||||
8710|Injune Creek Group|36333|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|36570|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|36914|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|36939|6|Mentioned|p214|||||||||
8710|Injune Creek Group|37065|6|Mentioned|p39|||||||||
8710|Injune Creek Group|37116|6|Mentioned|p310|||||||||
8710|Injune Creek Group|37451|6|Mentioned|Table 2|||||||||
8710|Injune Creek Group|37608|3|Fully described|Table 1|||||||||
8710|Injune Creek Group|37993|6|Mentioned|p153|||||||||
8710|Injune Creek Group|37995|4|Described|p64|||||||||
8710|Injune Creek Group|38064|6|Mentioned|42|||||||||
8710|Injune Creek Group|38199|5|Briefly described|p421|||Palynology||||||
8710|Injune Creek Group|38205|6|Mentioned|p96|||||||||
8710|Injune Creek Group|38226|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|39212|6|Mentioned|p16|||P24-petroleum reservoir. P25-aquifer||||||
8710|Injune Creek Group|39315|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|39445|6|Mentioned|Table 10|||||||||
8710|Injune Creek Group|39478|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|39494|6|Mentioned|Fig.3|||See also Fig.5||||||
8710|Injune Creek Group|39847|6|Mentioned|p40|||||||||
8710|Injune Creek Group|39943|6|Mentioned|Table 8A|||||||||
8710|Injune Creek Group|40030|6|Mentioned|Fig.3|||||||||
8710|Injune Creek Group|40199|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|40249|6|Mentioned|p38|||||||||
8710|Injune Creek Group|40250|6|Mentioned|p35|||||||||
8710|Injune Creek Group|40541|6|Mentioned|p114|||||||||
8710|Injune Creek Group|40544|6|Mentioned|Fig.4|||See also Fig.6||||||
8710|Injune Creek Group|40623|5|Briefly described|p73|||||||||
8710|Injune Creek Group|40801|6|Mentioned|p29|||||||||
8710|Injune Creek Group|40832|6|Mentioned|p459|||||||||
8710|Injune Creek Group|41061|6|Mentioned|p19|||||||||
8710|Injune Creek Group|41064|6|Mentioned|p60|||||||||
8710|Injune Creek Group|41097|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|41175|6|Mentioned|p195|||||||||
8710|Injune Creek Group|41177|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|41198|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|41246|6|Mentioned|Map legend|Jurassic||||||||
8710|Injune Creek Group|41247|6|Mentioned|Fig.4|||See also Fig.7||||||
8710|Injune Creek Group|41266|6|Mentioned|Fig.3|||||||||
8710|Injune Creek Group|41681|6|Mentioned|p2|||||||||
8710|Injune Creek Group|41725|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|41992|4|Described|Fig.2 P183|||||||||
8710|Injune Creek Group|42007|6|Mentioned|Fig.2 P182|||||||||
8710|Injune Creek Group|42061|4|Described|Fig,11 P159|||||||||
8710|Injune Creek Group|42493|5|Briefly described|Fig. 1 P18|||||||||
8710|Injune Creek Group|42634|6|Mentioned|Table 8 P34|||||||||
8710|Injune Creek Group|42911|6|Mentioned|p38|||||||||
8710|Injune Creek Group|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
8710|Injune Creek Group|43122|5|Briefly described|Fig.2.|||||||||
8710|Injune Creek Group|43185|6|Mentioned|6||Jurassic|||||||
8710|Injune Creek Group|43539|14|Not recorded|p396,398|||gas||||||
8710|Injune Creek Group|43602|6|Mentioned|191|Late Jurassic|Middle Jurassic|In Eromanga Basin||||||
8710|Injune Creek Group|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44020|14|Not recorded|Tb.1|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44021|2|Defined|p232-234|Late Jurassic|Middle Jurassic|="Injune Creek Beds". Contains Birkhead Formation (Includes Springbok Sandstone Lens) and Westbourne Formation, Adori Sandstone (in Eromanga Basin). Is the sequence between Hutton and Gubberamunda Sandstones.||||||
8710|Injune Creek Group|44022|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44023|6|Mentioned|p11|||||||||
8710|Injune Creek Group|44028|14|Not recorded|p514||Jurassic|Lithological equivalent of the Injune Creek Beds. See Strat Table.||||||
8710|Injune Creek Group|44031|14|Not recorded|p6,8,9,11|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44042|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44099|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44129|14|Not recorded|p95-96||Jurassic|||||||
8710|Injune Creek Group|44171|14|Not recorded|p194,197|||||||||
8710|Injune Creek Group|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
8710|Injune Creek Group|44414|14|Not recorded|p114,|Cretaceous|Jurassic|||||||
8710|Injune Creek Group|44415|14|Not recorded|Fig.2,p23|||||||||
8710|Injune Creek Group|44637|14|Not recorded|p287-291||Jurassic|||||||
8710|Injune Creek Group|45071|6|Mentioned|p134|||On Table 15||||||
8710|Injune Creek Group|45110|3|Fully described|p93|||See also P6.||||||
8710|Injune Creek Group|46881|6|Mentioned|Table 2|||||||||
8710|Injune Creek Group|46937|6|Mentioned|Fig.10|||||||||
8710|Injune Creek Group|46939|6|Mentioned|p50|||See also Table 1.||||||
8710|Injune Creek Group|46984|6|Mentioned|p157|||See also Table 1.||||||
8710|Injune Creek Group|46989|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|48900|6|Mentioned|p53|||||||||
8710|Injune Creek Group|48919|4|Described|p55|||See also p56. Jurassic||||||22-AUG-18
8710|Injune Creek Group|48920|5|Briefly described|p47|||Jurassic||||||
8710|Injune Creek Group|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
8710|Injune Creek Group|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
8710|Injune Creek Group|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, siltstone, mudstone, coal, conglomerate.||||||
8710|Injune Creek Group|61312|5|Briefly described|p71, p79 Table E2|||In Queensland this unit occupies the interval between the Hutton and Hooray Sandstones; including, from base to top: Birkhead Formation, Adori Sandstone and Westbourne Formation. Geological Province: Eromanga Basin.||||||
8710|Injune Creek Group|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Middle Jurassic|Includes the Westbourne Formation and Springbok Sandstone. Grey-brown siltstone and shale, coal, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
8710|Injune Creek Group|61832|5|Briefly described|p187|Middle Jurassic|Jurassic|On the MUNDUBERRA sheet. Overlies Hutton Sandstone. Geological Province: Surat Basin.||||||03-JUL-06
8710|Injune Creek Group|62028|5|Briefly described|p10 Fig. 1|||||||||
8710|Injune Creek Group|63218|4|Described|p209, p211, p221.|Late Jurassic|Middle Jurassic|Surat Basin. Originally the informally-named Injune Creek Beds (Jensen 1921); subsequently renamed and formally defined as Injune Creek Group by Exon (1966); its stratigraphy was amended by Swarbrick et al. (1973). Includes a number of fluvial and lacustrine units.|||Includes basal Eurombah Formation; Walloon Subgroup; Birkhead Formation; Springbok Sandstone; and Westbourne Formation at the top.|||
8710|Injune Creek Group|64665|5|Briefly described|p53 Fig.2.|Late Jurassic|Middle Jurassic|Surat Basin.|||Includes Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|64856|6|Mentioned|p87|||Andesitic detritus common.| | ||||29-NOV-17
8710|Injune Creek Group|65003|5|Briefly described|p1, p6, p13, p16, p25||Jurassic|Of Surat Basin. Fluvatile and paludal sediments derived largely from volcanism. Contains discontinuous coal beds.||||?Underlies the Orallo Formation.||
8710|Injune Creek Group|65096|6|Mentioned|p368|||||||The lower beds of the Injune Creek Group are equivalent to the Walloon Coal Measures.||
8710|Injune Creek Group|65119|5|Briefly described|p526, Fig 2, table 1, Fig 7-12, 16-19|Late Jurassic|Middle Jurassic|Surat Basin. Includes the Walloon Coal Measures. Sandstone, siltstone, mudstone, coal and lithic sandstone. Alluvial deposition up to 1200m thick.  Age: 153-168 Ma. Fission Track age: 132-145 Ma.||||||07-MAR-12
8710|Injune Creek Group|65388|3|Fully described|p215-216; p 204 Fig72, p214||Middle Jurassic|Rocks conformably overlying the Hutton Sandstone in the south-west corner of the study area. Thickness 62m to at least 150m. Includes Eurombah Formation in SW Bungaban map sheet area, and Walloon Coal Measures. Age of lower part of Group is same as Walloon Coal Measures: late Middle Jurassic (Bathonian to Callovian), based on palynofloras attributed to units APJ42, APJ43 and APJ5 (Price, 1997).||||||
8710|Injune Creek Group|65489|6|Mentioned|p96|||Eromanga Basin.||||||
8710|Injune Creek Group|66529|5|Briefly described|p12 Fig.5|||Eromanga Basin. Is called Injune Group on p10.|||Includes Birkhead and Westbourne Formations and Adori Sandstone.|Overlies Hutton Sandstone. Is overlain by Namur, Hooray and Gubberamunda Sandstones.|Fine grained lacustrine sandstone, siltstone and shale.|
8710|Injune Creek Group|66623|6|Mentioned|p449.|Middle Jurassic|Middle Jurassic|Formerly Injune Creek beds. Surat Basin. Petrified tree-fern, Osmundacaulis hoskingii, found also in Tibooburra area, was first described from this unit by Gould (1973).||||||
8710|Injune Creek Group|66915|5|Briefly described|p6 Fig.3|Late Jurassic|Middle Jurassic|Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Coal Measures|||
8710|Injune Creek Group|67669|5|Briefly described|p11|Late Jurassic|Middle Jurassic|Of Bowen Basin.|||Includes Westbourn Fm, Springbok Sandstone and Wallon CM.|Overlain by Blythesdale Group. Underlain by Bundamba Group.||
8710|Injune Creek Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.|||Includes Eurombah Formation, Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|68117|5|Briefly described|p345-346, p348|Late Jurassic|Middle Jurassic|Formally defined by Exon (1966); previously the (informal) Injune Creek Beds of Jensen (1921). Redefined by Swarbrick, Gray and Exon (1973) who defined the basal Eurombah Formation, and included the Norwood Mudstone Member in the Westbourne Formation at the top. Drilling by Queensland Gas Company Limited has led to further redefinition of this unit in this study.|||Eurombah, Durabilla, Birkhead, Westbourne Formations; Springbok Sandstone.|||
8710|Injune Creek Group|68135|6|Mentioned|p55 fig 3, p59|Callovian|Bathonian|Northern Surat Basin.||||||14-SEP-17
8710|Injune Creek Group|68139|5|Briefly described|p23|Late Jurassic|Middle Jurassic|Surat Basin.|||Walloon Subgroup, Springbok Sandstone, Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Clarence-Moreton and Surat Basins. This unit, as well as the Mulgildie and the Walloon Coal Measures, are all mapped under the symbol, Ji.||||||
8710|Injune Creek Group|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.|||Includes Walloon Coal Measures, Springbok Sandstone, Westbourne Formation.|Overlies Hutton Sandstone.  Is overlain unconformably by Gubberamunda Sandstone.||22-OCT-19
8710|Injune Creek Group|68679|6|Mentioned|p312-313|Jurassic|Jurassic|Northern New England Orogen.||||||
8710|Injune Creek Group|69594|5|Briefly described|p519|||Northern Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain unconformably by Gubberamunda Sandstone.||
8710|Injune Creek Group|69681|6|Mentioned|p74 Fig.3|Late Jurassic|Middle Jurassic||||Includes Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|||
8710|Injune Creek Group|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Middle Jurassic|Surat Basin.|||Includes Walloon Subgroup; Springbok and Gubberamunda Sandstones; Westbourne Formation.|Overlies Hutton Sandstone.||
8710|Injune Creek Group|69790|6|Mentioned|p1063 Fig.2|Late Jurassic|Middle Jurassic|Northern Surat Basin.|||Includes Walloon Subgroup, Springbok Sandstone and Westbourne Formation.|||
8710|Injune Creek Group|70374|5|Briefly described|p808, p809 figure 1,|Jurassic|Jurassic||||Includes Birkhead, Eurombah, Westbourne Formations, Springbok Sandstone, Walloon Coal Measures.|||28-SEP-16
8710|Injune Creek Group|70821|5|Briefly described|p80|||Eromanga, Surat Basins.|||Birkhead, Westbourne, Eurombah Formations; Adori, Springbok, Pilliga Sandstones; Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain by Hooray Sandstone.||
8710|Injune Creek Group|71282|6|Mentioned|p456||||||Durabilla Formation [of Walloon Subgroup].|||22-AUG-18
8710|Injune Creek Group|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
8710|Injune Creek Group|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).|||Birkhead, Westbourne, Eurombah FZs; Adori, Springbok Sandstones; Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain by Namur, Hooray or Gubberamunda Sandstones.||
8710|Injune Creek Group|73193|6|Mentioned|p369|Tithonian|Callovian|Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Subgroup|Underlain by Hutton Sandstone. Unconformably overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|73393|6|Mentioned|p19-21|Tithonian|Bathonian|Surat and Eromanga Basins. Supersedes Injune Creek Beds.|||Walloon Coal MeasuresWestbourne Formation, Adori Sandstone, Springbok Sandstone, Walloon Coal Measures, Birkhead Formation, Eurombah Formation|Underlain by Hutton Sandstone.||
9003|Johanna River Sand|23010|6|Mentioned|p333-341|||||||||
9003|Johanna River Sand|24551|6|Mentioned|p305, 630|Middle Eocene|Middle Eocene|||||||
9003|Johanna River Sand|30185|6|Mentioned|p108|||Refers Taylor(1965)||||||
9003|Johanna River Sand|30576|5|Briefly described|Table 2|||||||||
9003|Johanna River Sand|30578|6|Mentioned|p9|||||||||
9003|Johanna River Sand|31245|4|Described|p81|||See also P82, 83||||||
9003|Johanna River Sand|31922|6|Mentioned|p166|||||||||
9003|Johanna River Sand|33155|5|Briefly described|p119|||||||||
9003|Johanna River Sand|33319|6|Mentioned|p167|||Fauna||||||
9003|Johanna River Sand|33412|6|Mentioned|p224|||M.Palaeocene||||||
9003|Johanna River Sand|35066|3|Fully described|p224|||||||||
9003|Johanna River Sand|38070|6|Mentioned|Fig.12|||Otway Basin||||||
9003|Johanna River Sand|38903|6|Mentioned|p2|||||||||
9003|Johanna River Sand|39923|6|Mentioned|p354|||||||||
9003|Johanna River Sand|40429|6|Mentioned|Fig.2|||||||||
9003|Johanna River Sand|41043|6|Mentioned|p95|||||||||
9003|Johanna River Sand|42318|5|Briefly described|p7|||||||||
9003|Johanna River Sand|42827|3|Fully described|p298|||see also Fig 8.12||||||
9003|Johanna River Sand|43590|6|Mentioned|p15|||Mapped in Dilwyn Formation||||||
9003|Johanna River Sand|43675|6|Mentioned|p334|||||||||
9003|Johanna River Sand|47054|5|Briefly described|Fig.3 P481|||||||||
9003|Johanna River Sand|48911|6|Mentioned|Chart 1|||||||||
9003|Johanna River Sand|61155|5|Briefly described|p18|Middle Eocene|Early Paleocene|Overlies Rotten Point Sand; underlies Browns Creek Clay. Age: 65.5-46.5Ma. Thickness: 40m. Geological Province: Aire Embayment.||||||
9003|Johanna River Sand|61182|5|Briefly described|p19|||Of Wangerrip Group. Isolated outcrop mapped as part of Dilwyn Formation together with Rotten Point Sand. Geological Province: Otway Basin. Lower part is coeval with Pebble Point Formation. ||||||
9023|Jones Valley Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province. Maximum thickness <8 m.||||||
9023|Jones Valley Member|23982|5|Briefly described|p58 Fig.18|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
9023|Jones Valley Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
9023|Jones Valley Member|32314|6|Mentioned|Fig. 4|||||||||
9023|Jones Valley Member|33016|6|Mentioned|p1|||On table||||||
9023|Jones Valley Member|33017|6|Mentioned|p6|||||||||
9023|Jones Valley Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
9023|Jones Valley Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
9023|Jones Valley Member|33368|6|Mentioned|p25|||Strat.table.||||||
9023|Jones Valley Member|33414|6|Mentioned|p212,Table.|||Part of Wallumbilla Formation.||||||
9023|Jones Valley Member|33638|5|Briefly described|Table 1|||||||||
9023|Jones Valley Member|33642|6|Mentioned|p147,148,Fig.2,Tb.1|||Refers Vine & Day (1965)||||||
9023|Jones Valley Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
9023|Jones Valley Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
9023|Jones Valley Member|33648|6|Mentioned|p21|||Strat.||||||
9023|Jones Valley Member|35239|6|Mentioned|p265|||||||||
9023|Jones Valley Member|35560|6|Mentioned|p291|||||||||
9023|Jones Valley Member|35793|6|Mentioned|Fig.3|||||||||
9023|Jones Valley Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
9023|Jones Valley Member|36552|6|Mentioned|p60|||||||||
9023|Jones Valley Member|36571|6|Mentioned|p101|||See also Table 4||||||
9023|Jones Valley Member|38007|6|Mentioned|p36|||||||||
9023|Jones Valley Member|38199|6|Mentioned|p428|||||||||
9023|Jones Valley Member|38814|6|Mentioned|Table 1|||||||||
9023|Jones Valley Member|39211|5|Briefly described|Fig.3|||Correlation. See also Figs 4,9,11 etc.||||||
9023|Jones Valley Member|40801|6|Mentioned|p39|||||||||
9023|Jones Valley Member|40926|6|Mentioned|Table 2|||||||||
9023|Jones Valley Member|41064|6|Mentioned|p67|||||||||
9023|Jones Valley Member|41266|6|Mentioned|Fig.3|||||||||
9023|Jones Valley Member|44082|6|Mentioned|Table p34||Aptian|Part of Wallumbilla Formation. Mention on correlation table of Queensland Cretaceous sediments.||||||
9023|Jones Valley Member|44087|14|Not recorded|p4,opp.7|||||||||
9023|Jones Valley Member|44089|14|Not recorded|Tb.1||Early Cretaceous|||||||
9023|Jones Valley Member|44346|14|Not recorded|p4|||||||||
9023|Jones Valley Member|44373|14|Not recorded|p20|||Map only.||||||
9023|Jones Valley Member|44374|14|Not recorded|p12||Aptian|||||||
9023|Jones Valley Member|44376|14|Not recorded|p6|||||||||
9023|Jones Valley Member|44406|14|Not recorded|p4,opp.p6|||Member of Wilgunya Formation.||||||
9023|Jones Valley Member|44408|14|Not recorded|p4,opp.p6|||||||||
9023|Jones Valley Member|44414|14|Not recorded|p111,112||Cretaceous|||||||
9023|Jones Valley Member|44417|2|Defined|p416,418-420|||Early Cretaceous fossils.||||||
9023|Jones Valley Member|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965.||||||
9023|Jones Valley Member|46791|6|Mentioned|p44|||||||||
9023|Jones Valley Member|46937|6|Mentioned|Fig.10|||||||||
9023|Jones Valley Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
9023|Jones Valley Member|48920|6|Mentioned|Table 8|||Refers Vine & Day (1965)||||||
9023|Jones Valley Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
9023|Jones Valley Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
9023|Jones Valley Member|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Of the Wallumbilla Formation. Overlies the Doncaster Member. Overlain by Ranmoor Member. Geological Province: Eromanga Basin||||||
9023|Jones Valley Member|66529|6|Mentioned|p12 Fig.5|||Presented as Jones V Mbr in figure, and does not appear elsewhere in article. Eromanga Basin.||Unit in Wallumbilla Formation.||||
9023|Jones Valley Member|66623|6|Mentioned|p260.|||Partially equivalent to Doncaster Member in NSW.||||||
9023|Jones Valley Member|67784|5|Briefly described|p25-26, p28-33|Albian|Aptian|Age derived from biostratigraphy. 5-8m thick. Northern Eromanga Basin. Shown as JVM on p29.||Wallumbilla Formation||Overlies Doncaster Member. Is overlain paraconformably by Ranmoor Member.|A distinctive glauconitic sandstone interval.|08-FEB-18
9023|Jones Valley Member|68206|5|Briefly described|p32-33|Aptian|Aptian|NE Eromanga Basin.||Wallumbilla Formation.||Is overlain by Ranmoor Member.|Glauconitic.|
9023|Jones Valley Member|69457|5|Briefly described|p41:10|||Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
9023|Jones Valley Member|69594|5|Briefly described|p522, p528|Aptian|Aptian|Northern Eromanga Basin; is not recognised elsewhere. Crops out in a narrow discontinuous band from N of Hughenden to NW of Richmond. No equivalent units have been identified. Contains late Aptian bivalves, ammonites and belemnites.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain conformably by Ranmoor Member.|Siltstone, mudstone, impure limestone, sandstone and intraformational conglomerate.|
9023|Jones Valley Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
9023|Jones Valley Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD). Appears (for reasons of space) as Jones V Mbr.||Wallumbilla FZ.||Overlies Doncaster Member. Is overlain by Ranmoor Member.||
9070|Julie Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Dolomite, limestone, lenses of sandstone and calcareous sandstone.||||||
9070|Julie Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
9070|Julie Formation|22561|4|Described|p15|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22566|5|Briefly described|p82|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
9070|Julie Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22649|6|Mentioned|p 150|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22650|6|Mentioned|Fig 2 on p 157|||||||||
9070|Julie Formation|22651|5|Briefly described|p 175|||||||||
9070|Julie Formation|22746|5|Briefly described|p513, p528|||See also Table 1 p524||||||
9070|Julie Formation|22762|6|Mentioned|p374|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22763|6|Mentioned|Table 1 on p386|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22804|6|Mentioned|p429|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22805|5|Briefly described|p464 & p475|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Amadeus Basin||||||
9070|Julie Formation|22824|6|Mentioned|Fig 7 on p536|||||||||
9070|Julie Formation|22826|6|Mentioned|p570|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22901|6|Mentioned|78|||Geol province Amadeus Basin||||||
9070|Julie Formation|22907|6|Mentioned|42|||Geol province Amadeus Basin||||||
9070|Julie Formation|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Correlate of Wonoka Formation.||||||
9070|Julie Formation|23287|6|Mentioned|Fig.4|||Age: Upper Ediacarian. of Amadeus Basin.||||||
9070|Julie Formation|23314|5|Briefly described|331 Fig.2|||||||||
9070|Julie Formation|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
9070|Julie Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
9070|Julie Formation|23806|6|Mentioned|p1122|||||||||
9070|Julie Formation|35798|6|Mentioned|p311|||||||||
9070|Julie Formation|35805|6|Mentioned|Fig.3|||||||||
9070|Julie Formation|35863|6|Mentioned|Table 1|||||||||
9070|Julie Formation|36898|6|Mentioned|p199|||||||||
9070|Julie Formation|37462|4|Described|Table 4.IX|||||||||
9070|Julie Formation|37928|6|Mentioned|Fig.4|||||||||
9070|Julie Formation|37929|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|38157|6|Mentioned|Table VI|||||||||
9070|Julie Formation|38243|6|Mentioned|p359|||||||||
9070|Julie Formation|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|39565|6|Mentioned|p32|||||||||
9070|Julie Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pale brown to red-brown sandstone overlain by oolitic dolomite. Geological Province: Amadeus Basin.||||||14-FEB-06
9070|Julie Formation|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|40105|6|Mentioned|p311|||||||||
9070|Julie Formation|40740|3|Fully described|p88|||Described p12.||||||28-SEP-06
9070|Julie Formation|40810|6|Mentioned|p3|||||||||
9070|Julie Formation|40906|6|Mentioned|Fig.9|||||||||
9070|Julie Formation|41005|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41039|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41115|5|Briefly described|p1389|||||||||
9070|Julie Formation|41190|6|Mentioned|Fig.4|||||||||
9070|Julie Formation|41203|5|Briefly described|p26|||||||||
9070|Julie Formation|41270|6|Mentioned|Table 1|||||||||
9070|Julie Formation|41429|5|Briefly described|p246|||||||||
9070|Julie Formation|41618|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41717|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41801|6|Mentioned|p219|||||||||
9070|Julie Formation|41852|6|Mentioned|Table 1|||||||||
9070|Julie Formation|42059|6|Mentioned|Fig.2 P131|||||||||
9070|Julie Formation|42082|6|Mentioned|Fig.3 P323|||||||||
9070|Julie Formation|42504|4|Described|p72|||||||||
9070|Julie Formation|42643|6|Mentioned|Fig.4 P19|||||||||
9070|Julie Formation|42845|6|Mentioned|Fig.2 P497|||||||||
9070|Julie Formation|42886|4|Described|p223|||see also Fig.2 p219.||||||28-SEP-06
9070|Julie Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Dolostone, limestone (both quartzose), sandstone, shale.  Geological province: Amadeus Basin.||||||23-JAN-08
9070|Julie Formation|43105|5|Briefly described|Fig.3,p8|||||||||
9070|Julie Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
9070|Julie Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
9070|Julie Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
9070|Julie Formation|43756|6|Mentioned|p542|||||||||
9070|Julie Formation|44111|6|Mentioned|p.58, Fig. 2|||in Amadeus Basin, presented as "Julie" only in Fig. 2.||||||
9070|Julie Formation|45155|6|Mentioned|Fig.7|||Amadeus Basin||||||
9070|Julie Formation|46730|5|Briefly described|p7|||Overain by Pertaoorrta Group; underlain by Cyclops Member. Geological Province: Amadeus Basin||||||28-SEP-06
9070|Julie Formation|46865|6|Mentioned|Fig.2|||Upgraded P51.||||||
9070|Julie Formation|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
9070|Julie Formation|47035|6|Mentioned|Fig.1|||||||||
9070|Julie Formation|48990|6|Mentioned|p11|||||||||
9070|Julie Formation|49796|6|Mentioned|Sect C BDF 28|||||||||
9070|Julie Formation|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Dolostone, limestone, sandstone - oolitic and stromatolitic.||||||07-FEB-11
9070|Julie Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pale brown to red-brown sandstone overlain by oolitic limestone.||||||
9070|Julie Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
9070|Julie Formation|61732|3|Fully described|p4 Fig. 3, p98|Marinoan|Marinoan|Conformably overlain by Arumbera Sandstone; overlies Pertatataka Formation. Max. thickness: 600m. Geological Province: Amadeus Basin. See also p5 Tb. 1, p26, p91.||||||07-FEB-11
9070|Julie Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
9070|Julie Formation|62379|5|Briefly described|p7 Fig. 2, p25|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Dolostone, limestone, siltstone, sandstone.||||||
9070|Julie Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Amadeus Basin.||||||
9070|Julie Formation|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||||Dolostone, limestone, sandstone, oolitic and stromatolitic.|
9070|Julie Formation|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Julie.||||overlies Pertatataka Formation; is overlain by Arumbera Sandstone||
9070|Julie Formation|63458|6|Mentioned|p873, p897 Fig.19, |Ediacaran|Ediacaran|Amadeus Basin.||||Overlies Pertatataka Formation. Correlated with Boonall Dolomite. Is overlain by Arumbera Sandstone.||
9070|Julie Formation|63562|6|Mentioned|p338 fig 3,p343, p346 fig 8,p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin.||||Is overlain by Arumbera Sandstone.|Shallow-water platform carbonates.|
9070|Julie Formation|64068|6|Mentioned|p51, 224|||Amadeus Basin. Correlated with Elkera Formation, Central Mount Stuart Formation, southern Georgina Basin.||||||
9070|Julie Formation|64625|5|Briefly described|p244-245, p247, p250-251|Neoproterozoic|Neoproterozoic|Amadeus Basin||||Overlies Pertatataka Formation gradationally. Is disconformably overlain by Arumbera Sandstone.|Dolomite with minor sandstone.|
9070|Julie Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
9070|Julie Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
9070|Julie Formation|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
9070|Julie Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Amadeus Basin. Rank not shown in diagram.||||||
9070|Julie Formation|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p10.|Proterozoic|Proterozoic|See also p15 Fig.15.||||Overlies Pertatataka Formation. Is overlain conformably (gradationally) by Arumbera Sandstone.|Dolostone, limestone, sandstone.|
9070|Julie Formation|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
9070|Julie Formation|65233|5|Briefly described|p3 Fig. 2, p7|Neoproterozoic|Neoproterozoic|Conformable on Pertatataka Formation. Geological province: Amadeus Basin.||||||07-FEB-11
9070|Julie Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
9070|Julie Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 21 m.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Pale brown to red-brown sandstone.|
9070|Julie Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Amadeus Basin||||||
9070|Julie Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Amadeus Basin||||||
9070|Julie Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3. May be correlated with the Boondawari Formation (Savory Sub-basin).||||||
9070|Julie Formation|65416|6|Mentioned|p146.|||Supersequence LP3. Suggested by Perincek (1996) to pre-date the Petermann Ranges Orogeny.||||||
9070|Julie Formation|67326|5|Briefly described|p2, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin. Up to 150m thick. Oolitic platform carbonates.||||Conformably overlies Pertatataka Formation. Is overlain unconformably by Arumbera Sandstone.|A widespread, fairly thin succession of ooid grainstone, dolostone and limestone.|
9070|Julie Formation|67484|5|Briefly described|p294 Tb.1|Ediacaran|Ediacaran|Amadeus Basin. Contains Tungussia julia (Grey and Corkeron, 1998) fossils. Mis-spelt as Julia on p299.||||Overlies Pertatataka Formation. Is correlated with Egan and Wonoka Formations and Boonall Dolomite.||
9070|Julie Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.||
9070|Julie Formation|67856|4|Described|p338 fig 4-30, p337, p345, 346|Neoproterozoic|Neoproterozoic|Carbonate unit.Could possibly correlate with Cluttterbuck Formation.||||Overlies Pertatataka Formation in central Amadeus Basin.||
9070|Julie Formation|68030|6|Mentioned|p239|||Amadeus Basin. Correlated to upepr carbonates in the Wonoka Formation.||||||
9070|Julie Formation|68244|6|Mentioned|p666|Neoproterozoic|Neoproterozoic|Central Australia. ContainsTungussia julia, a stromatolite biostratigraphic marker that correlates Julie Fm to Bonney Sandstone (SA) and Egan Formation.||||||
9070|Julie Formation|68270|5|Briefly described|p683-684|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by lower Arumbera Sandstone. Underlain by Perttatataka Formation.||
9070|Julie Formation|68277|6|Mentioned|p103|||Central Australia. Mid-Ediacaran age. Correlation based on stromatolites.||||Correlated with Egan Formation.||
9070|Julie Formation|68316|6|Mentioned|p778 Fig.1|||||||||
9070|Julie Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
9070|Julie Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
9070|Julie Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran||Amadeus Basin.|580 Ma.|||Equivalent to Egan Formation.||05-DEC-17
9070|Julie Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
9070|Julie Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||Is overlain by Carnegie Formation.||
9070|Julie Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Dolostone, limestone and siltstone with sandstone lenses.|12-JUL-16
9070|Julie Formation|69438|3|Fully described|p23:2-8, 17-18, 20, 24, 43, 60|Ediacaran|Ediacaran|Priess et al. (1978); formerly the Julie Member (of the Pertatataka Formation) of Wells et al. (1967). Raised to Formation status because of its wide distribution and usefulness as a marker interval. Amadeus Basin. Type section is at Ross River. 10-150m thick. Does not occur W of the Gardiner Range: apparently eroded before deposition of Arumbera Sandstone.||||Conformably overlies Pertatataka Formation. Is overlain conformably to disconformably by Arumbera Sandstone. Correlated with Rodda beds and lower Elkera Formation.|A widespread, relatively thin unit of dolostone, limestone (oolitic in part) and siltstone with sandstone lenses; contains sparse stromatolites.|12-JUL-16
9070|Julie Formation|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
9070|Julie Formation|69606|4|Described|p1, p4 fig 2, p5, p6 fig 3, p14|Ediacaran|Ediacaran|c. <500m thick. Previously the Julie Member of Wells et al, 1967. Potential reservoir and seal rock. Amadeus Basin. Age based on stratigraphic position and stromatolite fossil assemblage. Stromatolite fossil assemblage discussed in detail. Outcrop ranges from poor to moderate where it forms a series of low strike ridges of limestone and dolostone. Contact with the Pertatataka Formation is poorly exposed. See also p15 fig 8, p16, p19.||||Conformably and gradationally overlies the Pertatataka Formation. Overlain (locally unconformably) by the Carnegie Formation and Arumbera Sandstone.|Limestone and dolostone that vary from mictritic to ooid and peloidal packstone and grainstone, interbedded with poorly exposed silstone and sandstone that is stromatolitic and oolitic. Evaporites occur near the top of this formation.|14-SEP-22
9070|Julie Formation|69673|5|Briefly described|p63, p73, p84, p86, p88, p91, p99|||At a maximum 150m thick, can be as little as 10m. Sparse stromatolites in places. Potential reservoir rock.||||Overlain by Arumbera Sandstone|Dolostone, limestone and siltstone with sandstone lenses.|
9070|Julie Formation|69937|4|Described|v Fig.1, vi, p3 Tb.1, p32-34, p55-56|Neoproterozoic|Neoproterozoic|Amadeus Basin. Originally a Member of the Pertatataka Formation; upgraded to Formation status by Preiss et al. (1978) because of its wide distribution and usefulness as a marker bed. Likely zircon provenance discussed.|985 +/- 25 Ma (maximum depositional age).|||Conformably overlies the Pertatataka Formation. Is overlain by the Arumbera Sandstone.|Dominantly carbonate sequence (dolostone and limestone), with lesser lenses and beds of sandstone and occasional siltstone. Also contains thickly-bedded ooid grainstones.|
9070|Julie Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain unconformably by Arumbera Sandstone. Underlain by Pertatataka Formation.||
9070|Julie Formation|70416|5|Briefly described|p64, p65 Fig.2, p80|Ediacaran|Ediacaran|Amadeus Basin. Now includes part of the former Boord Formation. See Fig.2 for the history of this unit's stratigraphic relationships. Contains the stromatolite Tungussia julia.||||Overlies Pertatataka Formation. Is overlain by Winnall Group. Correlated with upper part of Inindia beds.||
9070|Julie Formation|70752|5|Briefly described|p126 Fig.1|Proterozoic|Proterozoic||||||Stromatolitic dolostone and limestone with lenses of sandstone and calcareous sandstone.|
9070|Julie Formation|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Carnegie Formation or Arumbera Sandstone or Pertaoorta Group. Underlain by Pertatataka Formation.||
9070|Julie Formation|71001|5|Briefly described|p18 Fig.2, p19-20, 27-28|Ediacaran|Ediacaran|Amadeus Basin. Shallow marine deposits. Carbon isotope correlation graph.|~582-565 Ma.|||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Shallow-marine dolostone.|
9070|Julie Formation|71080|6|Mentioned|p29 fig 20, p30|Ediacaran|Ediacaran|Amadeus Basin. Supersequence 3.|||||Dominantly carbonate-shale, marl in WA, carbonate in NT.|
9070|Julie Formation|71088|6|Mentioned|p8, p15|Neoproterozoic|Neoproterozoic|Amadeus Basin. Formerly the top carbonate unit of the now disused "Boord Formation". Overlain by the Carnegie Formation at the Boord Ridges (Haines et al., 2012). ||||Overlain by the Carnegie Formation and the Arumbera Sandstone.||
9070|Julie Formation|71279|5|Briefly described|p355 Fig.2, p366|Ediacaran|Ediacaran|Amadeus Basin.|||||Sandstone and dolostone.|
9070|Julie Formation|71344|4|Described|p1092, 1094, 1096 -1100, 1102-3|Ediacaran||Amadeus Basin. Stromatolite stratigraphy and carbon isotope chemostratigraphy gives depositional age constraints. Deposited as shallowing upward sequence in a shallow marine environment.|575-565 Ma.|Of Pertaoorta Package.||Conformable on the Pertatataka Formation.|Interbedded sandy limestones/dolostones and calcareous siltstones.|10-NOV-17
9070|Julie Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|985+/-25 Ma (MDA: U-Pb zircon SHRIMP)||||Gritty calcareous medium-grained sandstone.|
9070|Julie Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Pertatataka Formation. Overlain by the Carnegie Formation, Angas Hill Formation and the Arumbera Sandstone.||
9070|Julie Formation|71801|6|Mentioned|p230-p232, p234-p235, p237|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Pertatataka Formation. Overlain by the Arumbera Formation.|Shallow-marine limestone and dolostone.|
9070|Julie Formation|71810|5|Briefly described|Map legend.|Ediacaran|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Limestone, dolomite, siltstone, and sandstone; stromatolitic; common diagenetic silicification in carbonates.|
9070|Julie Formation|71841|5|Briefly described|p1-2|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Arumbera Sandstone. Underlain by Pertatataka Formation. Grades into Inindia beds.||
9070|Julie Formation|71842|5|Briefly described|p2-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).  Generally confined to the NE Amadeus Basin, and along northern margin in WA; disappears from outcrop westward from central northern margin.||||Overlain by Arumbera Sandstone. Underlain by Pertatataka Formation.||
9070|Julie Formation|72375|4|Described|p1-2,31-32|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Originally a member of Pertatataka Formation (Wells et al., 1967), then redefined and upgraded to Formation status due to wide distribution and importance as marker bed (Preiss et al., 1978). Contains thickly bedded ooid grainstone of shallow marine origin, indicating an upward-shallowing cycle following deposition fo the deeper water Pertatataka Formation. SHRIMP U-Pb zircon analysis by Kositin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 985+\-25 Ma, significantly older than the inferred depositional age of underlying pertatataka Formation (c. 575 Ma; Maidment 2005). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS AS13CJE027 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p30 for Hf isotopic results and interpretations). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS RD13CJE003 (calcareous sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p31-32 for Hf isotopic results and interpretations).||||Overlain by Arumbera Sandstone. Underlain conformably by Pertatataka Formation.|Predominantly carbonate rocks such as dolostone and limestone, with lenses and beds of sandstone and occasional siltstone.|04-DEC-19
9070|Julie Formation|72489|5|Briefly described|p3, p4 Fig.3, p5 Fig.4, p4, p6, p11|Ediacaran|Ediacaran|Located in the Amadeus Basin.  See also p7 Fig.6, p8. Correlated with Patsy Hill Member of Bonney Sandstone on basis of stromatolite form. Described as late-Ediacaran.||||Partially overlies Pertatataka Formation. Partially underlies Arumbera Sandstone. Partially underlies Goyder Formation.|Includes oolitic carbonate.|
9070|Julie Formation|72516|6|Mentioned|p90|Ediacaran|Ediacaran|Amadeus Basin.||||Equivalent to the Elkera Formation.||02-JUN-21
9070|Julie Formation|72601|5|Briefly described|p3, p7-8, p11-12, p14, p25|Ediacaran|Ediacaran|Amadeus Basin. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Underlain by Pertatataka Formation. Overlain, unconformably in part, by the Carnegie Formation, Mu Formation, Arumbera Sandstone and Winnall beds.||
9070|Julie Formation|73085|4|Described|piii, p1, p3, p5, p7, p11, p13-14, p27|Ediacaran|Ediacaran|Amadeus Basin. [Written as ?Julie Formation on p: 3, 7, 11, 13-14]. Contains diagnostic stromatolite taxa. Lithology is here described from a 6-metre-thick interval in drillhole LA05DD01 tentatively assigned to the unit that was previously assigned to the Arumbera Sandstone. Wavy laminae of the unit in drillhole LA05DD01 interpreted as possible stromatolites. Possible oolites also observed.||||Underlain by Pertatataka Formation [and equivalents]. Overlain by Arumbera Sandstone. Equivalent to Inindia beds.|[Possibly] grey to brown, massive or planar to wavy laminated, recrystallised carbonate rock.|
9070|Julie Formation|73086|2|Defined|p3, p5-6, p99, p122, p132-136, 143|Ediacaran|Ediacaran|[Defined herein. See also definition card, ASUD]. Post-glacial transgressive unit. Amadeus Basin. Part of Supersequence III. Type section: Ross River. Key localities: east of Phillipson Pound. Parts of the unit contain the diagnostic Tungussia julia stromatolite. Previously part of the Pertatataka Formation. A detrital zircon maximum depositional age (youngest grain) of 985 +/- 25 Ma (SHRIMP U-Pb) is significantly older than the inferred true depositional age.||||Conformably underlain by Pertatataka Formation. Overlain by Arumbera Sandstone. Correlates to Rodda beds, Marchinbar Sandstone, Elkera, Central Mount Stuart, Andagera, and Elcho Island formations.|Medium- to coarse-grained and sandy, dark grey dolostone with interbeds of pink, yellow and grey dolostone that are oolitic and sandy, and local dark grey and blue foetid limestone.|
9070|Julie Formation|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||||Underlain by Pertatataka Formation. Overlain by Arumbera Sandstone.||
9070|Julie Formation|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Conformably overlies the Pertatataka Formation, conformably underlies the Carnegie Formation and Arumbera Sandstone.||
9194|Kamileroi Limestone|24073|6|Mentioned|p378 Table 2|Early Cretaceous|Early Cretaceous|Superseded?  Geological Province: Carpentaria Basin.||||||
9194|Kamileroi Limestone|30020|6|Mentioned|p30|||||||||
9194|Kamileroi Limestone|33017|6|Mentioned|p8|||||||||
9194|Kamileroi Limestone|33175|6|Mentioned|p280|||Synonymous with Toolebuc. See P284.||||||
9194|Kamileroi Limestone|33176|6|Mentioned|Table 1|||||||||
9194|Kamileroi Limestone|33182|6|Mentioned|p190|||||||||
9194|Kamileroi Limestone|33183|6|Mentioned|p227|||||||||
9194|Kamileroi Limestone|33561|6|Mentioned|p102|||||||||
9194|Kamileroi Limestone|33642|6|Mentioned|p144|||Named by Laing & Power (1959) in the Carpentaria Basin.||||||
9194|Kamileroi Limestone|34356|6|Mentioned|p20|||||||||
9194|Kamileroi Limestone|36571|6|Mentioned|p95|||||||||
9194|Kamileroi Limestone|40801|6|Mentioned|p85|||||||||
9194|Kamileroi Limestone|41174|6|Mentioned|p117|||||||||
9194|Kamileroi Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
9194|Kamileroi Limestone|43995|14|Not recorded|Tb.p9||Cretaceous|||||||
9194|Kamileroi Limestone|44031|14|Not recorded|p3,Tb.1||Cretaceous|||||||
9194|Kamileroi Limestone|44082|6|Mentioned|Table p34||Albian|Mention on correlation table of Queensland Cretaceous sediments.||||||
9194|Kamileroi Limestone|44346|14|Not recorded|opp.p5|||||||||
9194|Kamileroi Limestone|44515|2|Defined|p28|||Lower Tambo age.||||||
9194|Kamileroi Limestone|44656|2|Defined|p325,328,Fig.48,T.10||Albian|||||||
9194|Kamileroi Limestone|44747|14|Not recorded|p5,8|||||||||
9194|Kamileroi Limestone|44807|4|Described|p8,9,map||Early Cretaceous|||||||
9194|Kamileroi Limestone|44989|14|Not recorded|p.126|||(E54-14).||||||
9194|Kamileroi Limestone|45004|14|Not recorded|p.8,14,15|||||||||
9194|Kamileroi Limestone|45011|14|Not recorded|p19|||Ref. to Laing and Power 1959.||||||
9194|Kamileroi Limestone|45145|6|Mentioned|Table 4|||||||||
9221|Kangaroo Island Group|5249|6|Mentioned|p31 |Cambrian|Cambrian|A foreland platform to basin regime that received orogenically induced sediments. Subsequent tectonics have obscured unit relationships within this Group.||||||
9221|Kangaroo Island Group|22581|5|Briefly described|Fig.2,p37||Cambrian|in the Kanmantoo Basin. Thickness: 2000m.||||||12-FEB-07
9221|Kangaroo Island Group|22643|5|Briefly described|p186, fig3p187|Early Cambrian|Early Cambrian|||||||
9221|Kangaroo Island Group|22755|4|Described|p548||Early Cambrian|In the Stansbury Basin.||||||12-FEB-07
9221|Kangaroo Island Group|22766|4|Described|Fig.2 p561, p563|Early Cambrian|Early Cambrian|||||||
9221|Kangaroo Island Group|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Age: <534Ma. Geological Province: Stansbury Basin. ||||||
9221|Kangaroo Island Group|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Tommotian|||||||
9221|Kangaroo Island Group|23309|5|Briefly described|p40|||||||||
9221|Kangaroo Island Group|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||
9221|Kangaroo Island Group|23981|5|Briefly described|p20|Early Cambrian|Early Cambrian|Platformal siliciclastic cover sequence.  Thickness: <2000m. Geological Province: margins of Gawler Craton.||||||12-FEB-07
9221|Kangaroo Island Group|30052|6|Mentioned|p91|||||||||
9221|Kangaroo Island Group|30381|6|Mentioned|p233|||||||||
9221|Kangaroo Island Group|34612|6|Mentioned|Fig.33|||Cambrian||||||
9221|Kangaroo Island Group|41853|6|Mentioned|p201|||||||||
9221|Kangaroo Island Group|42272|6|Mentioned|p411|||||||||
9221|Kangaroo Island Group|42903|5|Briefly described|p424|||Actually written as Kangaroo Is. Group||||||12-FEB-07
9221|Kangaroo Island Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Forms part of shallow marine mudstone, sandstone and conglomerate unit.||||||25-MAY-05
9221|Kangaroo Island Group|43190|5|Briefly described|Fig.1,p28.||Cambrian|See also Fig2, p29. Age early to ?middle Cambrian.||||||12-FEB-07
9221|Kangaroo Island Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
9221|Kangaroo Island Group|43298|6|Mentioned|Map Legend||Cambrian|||||||
9221|Kangaroo Island Group|44133|5|Briefly described|p6|||Includes: upper Smith Bay Shale, White Point Conglomerate, Emu Bay Shale, Boxing Bay Formation.||||||
9221|Kangaroo Island Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine mudstone, sandstone and conglomerate.||||||
9221|Kangaroo Island Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine mudstone, sandstone and conglomerate.||||||
9221|Kangaroo Island Group|62742|5|Briefly described|p699 Fig. 2|Middle Cambrian|Early Cambrian|Quartz-rich sandstone, conglomerate and mudstone.||||||
9221|Kangaroo Island Group|62744|5|Briefly described|p709 Fig. 2|Ordovician|Cambrian|||||||
9221|Kangaroo Island Group|64281|5|Briefly described|p28, p29|Cambrian|Cambrian|Overlies the Gawler Craton. Platformal sediments of mixed carbonate-terrigenous clastics juxtaposed against basinal equivalents of Kanmantoo Group which occurred during the Cambro-Ordovician Delamerian Orogeny.||||||23-DEC-09
9221|Kangaroo Island Group|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Includes Mount McDonnell Formation, Stokes Bay Sandstone, Smith Bay Shale, White Point Conglomerate, Emu Bay Shale and Boxing Bay Formation, and unddiferentiated rocks..||||||24-JUL-08
9221|Kangaroo Island Group|65375|5|Briefly described|p33.|Cambrian|Cambrian|Correlated with Moralana Supergroup from the base of the limestone unit within the Kulpara Formation.|||Includes Mount McDonnell and Boxing Bay Formations, Stokes Bay Sandstone, Smith Bay and Emu Bay Shales, and White Point Conglomerate.|||
9221|Kangaroo Island Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
9221|Kangaroo Island Group|65625|4|Described|p124, p103|Middle Cambrian|Early Cambrian|Conformable sequence ~4500ft thick.|||Includes, in ascending order, unnamed quartzite sandstone and shale 450ft thick, White Point Conglomerate, Emu Bay Shale, Boxing Bay Formation.|||13-APR-11
9221|Kangaroo Island Group|65664|6|Mentioned|p1097 Fig.1, p1105|||||||||
9221|Kangaroo Island Group|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Shallow marine shelf deposits. Maximum thickness ~2500m.|||Mount McDonnell Formation, Stokes Bay Sandstone, Smith Bay Shale, White Point Conglomerate, Emu Bay Shale, Boxing Bay Formation.||Conglomerates, sandstones and limestones.|
9221|Kangaroo Island Group|66761|5|Briefly described|p244, p245 Fig. 2|Cambrian|Cambrian|Constituents listed by Daily et al (1979). Cambrian Shelf succession or possibly deposited in small sub-basins.|||Includes Mount McDonnell Formation, Stokes Bay Sandstone, Smith Bay Shale, White Point Conglomerate, Emu Bay Shale and Boxing Bay Formation.|||14-MAR-12
9221|Kangaroo Island Group|68314|5|Briefly described|p754|Middle Cambrian|Early Cambrian||||||Quartz-rich sandstone, conglomerate and mudstone.|
9221|Kangaroo Island Group|69372|6|Mentioned|p27 fig. 5|Cambrian|||||Includes Emu Bay Shale, White Point Conglomerate, Stokes Bay Sandstone, Smith Bay Shale, Boxing Bay Formation, Mount McDonnell Formation.|||18-JAN-17
9221|Kangaroo Island Group|73247|5|Briefly described|p204, p206-207, p209|Cambrian (Series 2)|Cambrian (Series 2)|Fossiliferous successions along the north coast of Kangaroo Island. Divided into a western succession located between Snelling Beach and Smith Bay, and an eastern succession that extends from Emu Bay to Point Marsden. Eastern and western successions overlap in the Cape d'Estaing/Emu Bay area. Fossil evidence suggests the eastern and western successions are at least partly contemporaneous [which is why eastern and western distinction is thought to be more appropriate than upper and lower Kangaroo Island Group divisions]. Deposited as part of a fan delta system with proximal (eastern succession) and distal (western succession) components.|||Mount McDonnell Formation, Stokes Bay Sandstone, Smith Bay Shale, White Point Conglomerate, Marsden Sandstone, Emu Bay Shale, Boxing Bay Formation, and units therein|||02-FEB-23
9262|Kapunda Marble|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
9262|Kapunda Marble|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
9262|Kapunda Marble|34615|6|Mentioned|p7|||Shown on Figure.||||||
9262|Kapunda Marble|34959|6|Mentioned|p284|||||||||
9262|Kapunda Marble|35051|6|Mentioned|p203|||Analysis.||||||
9262|Kapunda Marble|40003|5|Briefly described|Table 4|||||||||
9262|Kapunda Marble|40499|6|Mentioned|p147|||||||||
9262|Kapunda Marble|42222|6|Mentioned|Table 1 P4|||||||||
9262|Kapunda Marble|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Karinya Syncline/Adelaide Fold Belt.||||||15-JAN-08
9262|Kapunda Marble|64769|6|Mentioned|p28|Cambrian|Cambrian|SA. Dimension stone name.||||||06-MAY-09
9262|Kapunda Marble|73188|6|Mentioned|p342|Cambrian|Cambrian|||||||
9325|Katipiri Formation|23054|6|Mentioned|p30|||||||||
9325|Katipiri Formation|24175|5|Briefly described|p43|Quaternary|Quaternary|Overlies both Kutjitara and Tirari Formations.||||||
9325|Katipiri Formation|24321|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||
9325|Katipiri Formation|29673|6|Mentioned|p330|||||||||
9325|Katipiri Formation|31699|6|Mentioned|p132|||Pleistocene. Preferable name to Katipiri Sands (re lithology)||||||
9325|Katipiri Formation|42124|6|Mentioned|p43|||||||||
9325|Katipiri Formation|42375|4|Described|p50-55|||Originally named Katipiri Sand. Amended herein. Lake Eyre Basin. Variation of Katipiri Formation,SA.||||||
9325|Katipiri Formation|42543|6|Mentioned|p4|||||||||
9325|Katipiri Formation|42746|5|Briefly described|Fig.9 P14|||Synonym for Katipiri Sand? See also p22.||||||01-SEP-20
9325|Katipiri Formation|42784|6|Mentioned|p487|||||||||
9325|Katipiri Formation|42883|6|Mentioned|p6|||||||||
9325|Katipiri Formation|43041|5|Briefly described|p589|||||||||
9325|Katipiri Formation|43042|5|Briefly described|p596|||||||||
9325|Katipiri Formation|44133|5|Briefly described|p245, 244 Table 11.3|Late Pleistocene|Middle Pleistocene|Maximum Thickness: 5m. ||||||
9325|Katipiri Formation|61119|5|Briefly described|p124, p128, p131, p137, p144, pp146-147||Pleistocene|Youngest unit discussed in this paper. Meandering river and, possibly saline, lake deposits. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
9325|Katipiri Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies the Kutjitara Formation; underlies the Kootaburra [Kootaberra]  Formation. Age: <1.5Ma. Geological Province: Lake Eyre Basin.||||||01-SEP-20
9325|Katipiri Formation|66131|5|Briefly described|p240, p243, p244 Fig.4, p246-247|Pleistocene|Pleistocene|Paleochannels underlying dunefields and cut into Tirari and Kutjitara Formations.||||Overlies Kutjitara Formation. Disconformably overlies Etadunna Formation. Correlative unit of the Eurinilla Formation.|Fluviolacustrine sediments and recessional shoreline dunes.|
9330|Katnook Sandstone|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 690m.||Crayfish Group.||Overlies Laira Formation. Is overlain unconformably by Eumeralla Formation.||
9330|Katnook Sandstone|22674|4|Described|p718, Fig.2 p719|Early Cretaceous|Barremian|||||||
9330|Katnook Sandstone|22686|5|Briefly described|Fig3p745|Aptian|Barremian|Of the upper Crayfish Group.  Geological Province: Otway Basin.||||||17-JAN-06
9330|Katnook Sandstone|24314|5|Briefly described|p61 Fig.2||Hauterivian|Geological Province: Otway Basin. Max. Thickness 690m. Of the Otway Supergroup.||||||30-NOV-04
9330|Katnook Sandstone|24453|5|Briefly described|p809 Fig.2|Hauterivian|Hauterivian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|24551|6|Mentioned|p245, 249|||Of the Crayfish Subgroup. Overlies: Laira Formation.||||||
9330|Katnook Sandstone|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
9330|Katnook Sandstone|42361|2|Defined|p8|Barremian|Barremian|||||||
9330|Katnook Sandstone|42545|5|Briefly described|Fig.4 P15|||||||||
9330|Katnook Sandstone|42599|5|Briefly described|Fig.3 P614|||||||||
9330|Katnook Sandstone|43171|6|Mentioned|5-6|||||||||
9330|Katnook Sandstone|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||
9330|Katnook Sandstone|43660|5|Briefly described|p14|||||||||
9330|Katnook Sandstone|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
9330|Katnook Sandstone|43744|6|Mentioned|Fig.3,p3|||||||||
9330|Katnook Sandstone|43747|5|Briefly described|p5||Early Cretaceous|||||||
9330|Katnook Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
9330|Katnook Sandstone|44133|5|Briefly described|p145|Hauterivian|Hauterivian|Geological Province: Otway Basin. Previously also known as 'Crayfish Group, Unit D'. Maximum Thickness: 530m. ||||||
9330|Katnook Sandstone|61017|5|Briefly described|p5 Fig. 2|Barremian|Barremian|Of the Crayfish Sungroup (Otway Group). Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61470|5|Briefly described|p28 Fig. 5|Barremian|Barremian|Of the Crayfish Subgroup (Otway Group). Overlies and interfingers with Laira Formation. Geological Province: Otway Basin.||||||
9330|Katnook Sandstone|61547|5|Briefly described|p459, p465, pp471-473.|Hauterivian|Hauterivian|On the hangingwall of the Pyrus Fault; juxtaposed against the Pretty Hill Sandstone in the footwall, allowing leaking of hydrocarbons. Consists of reworked Laira Formation.||Unit in the Crayfish Group||Overlies Laira Formation. Is overlain unconformably by the Windermere Sandstone Member.|Predominantly sandstone units with typical shale volumes of 5%, with frequent thin interbeds of shale rich units.|
9330|Katnook Sandstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
9330|Katnook Sandstone|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
9330|Katnook Sandstone|63122|5|Briefly described|p17 Fig. 4.3|Barremian|Hauterivian|Of the Crayfish Group. Max. thickness: 690m. Geological Province: Otway Basin. ||||||
9330|Katnook Sandstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p63-64|Hauterivian|Valanginian|Of Morton (1990). Formerly unnamed in Pretty Hill Sst (Wopfner et al (1971); also known as Geltwood Beach Mbr and G.B. Fm. Of Crayfish Gp.Overlies Laira Fm; unconformably overlain by Windermere Sst Mbr. Age:133-125Ma. Max. thickness: 690m. In Otway Basin.||||||
9330|Katnook Sandstone|63125|6|Mentioned|p116 Tb.7.6|||Geological Province: Otway Basin||||||
9330|Katnook Sandstone|63129|6|Mentioned|p131|||Geological Province: Otway Basin.||||||30-JAN-08
9330|Katnook Sandstone|63130|5|Briefly described|p143|||Geological Province: Otway Basin.||||||06-FEB-08
9330|Katnook Sandstone|63150|5|Briefly described|p96|||Geological province: Otway Basin. Availability of palynological criteria is vital for identification of this unit.||||||
9330|Katnook Sandstone|63267|5|Briefly described|p485 Fig.2|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin.||Crayfish Group.||Overlies Laira Formation. Is overlain unconformably by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Crayfish Subgroup.||||
9330|Katnook Sandstone|63431|5|Briefly described|p676, p677 Fig. 2|Hauterivian|Hauterivian|Topmost unit of Crayfish Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|66245|5|Briefly described|p6 Fig.5. |Barremian|Barremian|||Unit in Crayfish Subgroup.||Overlies Laira Formation.||
9330|Katnook Sandstone|67367|5|Briefly described|p131 Fig.2. |Barremian|Barremian|||Unit in Crayfish Subgroup.||||
9330|Katnook Sandstone|69297|5|Briefly described|p79|Barremian|Barremian|Otway Basin. ||Crayfish Subgroup||Overlies the Laira Formation. Unconformably Overlain by the Eumeralla Formation.|Sandstone.|
9330|Katnook Sandstone|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Overlies Laira Formation. Is overlain unconformably by Eumeralla Formation.||
9330|Katnook Sandstone|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Overlies Laira Formation. Is overlain by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|70077|5|Briefly described|Regional: Fig.4; p4|Barremian|Barremian|Otway Basin: Robe-Penola Trough. Higher energy fluvial sediments.||Crayfish Subgroup.||Overlies Laira Formation. Is overlain by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|70880|6|Mentioned|p77|Barremian|Barremian|Otway Basin.||||||
9330|Katnook Sandstone|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
9330|Katnook Sandstone|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
9330|Katnook Sandstone|72050|5|Briefly described|p233 Fig.2, 234-235|Barremian|Barremian|Has variable reservoir quality and patchy distribution.||Crayfish Group.|||A thin, discontinuous sandy unit.|
9330|Katnook Sandstone|73356|6|Mentioned|p1, p4, p29|Barremian|Barremian|||Crayfish Subgroup, Otway Group||Underlain by Laira Formation. Unconformably overlain by Windermere Sandstone.||
9330|Katnook Sandstone|73383|5|Briefly described|p3|Barremian|Barremian|Otway Basin.||Crayfish Subgroup|||Fluvial channel sandstones.|
9330|Katnook Sandstone|73385|5|Briefly described|p5|Barremian|Barremian|Otway Basin.||Crayfish Subgroup|||Fluvial channel sandstones.|
9330|Katnook Sandstone|73386|4|Described|p4, p8-9|Barremian|Barremian|Otway Basin. Associated with meandering fluvial to distal braided fluvial palaeoenvironments. Gradational and diachronous relationship with the underlying Laira Formation. Associated with the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone. Limited to the Penola Trough in South Australia, has not been intersected in Victoria. Type section defined between 1892 m and 1979 m in Katnook-2.||Crayfish Subgroup||Overlies Laira Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone|Dominant lithology is fine- to medium-grained sandstone with interbedded siltstone.|
9330|Katnook Sandstone|73594|5|Briefly described|p3-4, p16, p41-44, p47, p67|Barremian|Barremian|Otway Basin. Diachronous unit. Passes laterally into the Laira Formation. Type section defined in Katnook-1 well by Morton (1990). Defined by the upper F. wonthaggiensis spore-pollen zone. Becomes thicker and sandier westwards towards the St Claire Trough. High-sinuosity fluvial sandstone. Characterised by an apparent fluvial flow reversal when compared to the Pretty Hill and Eumeralla formations.||Crayfish Subgroup, uppermost unit||Overlies Laira Formation, Pretty Hill Formation. Unconformably underlies Windermere Member, Eumeralla Formation|Fine to medium grained cross bedded sandstone with reworked siltstone intraclasts and carbonaceous partings.|
9455|Keppoch Member|29892|6|Mentioned|p77|||||||||
9455|Keppoch Member|42966|5|Briefly described|p229|||of Padthaway Formation in Harris (1973).||||||
9477|Keswick Clay|22888|6|Mentioned|P36|||Previously informal name||||||
9477|Keswick Clay|23489|6|Mentioned|p47|||Equivalent of Ngaltinga Formation in the Noarlunga Embayment. Geological Province: Adelaide Plains Sub-basin.||||||
9477|Keswick Clay|23818|5|Briefly described|p216 Fig.112|Middle Pleistocene|Early Pleistocene|||||||
9477|Keswick Clay|30752|6|Mentioned|p3|||Formed in fluviatile environment close to sea level||||||
9477|Keswick Clay|30807|6|Mentioned|p101|||Suggested map symbol||||||
9477|Keswick Clay|33057|6|Mentioned|p8|||Refers Firman (1967,1969)||||||
9477|Keswick Clay|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
9477|Keswick Clay|33423|6|Mentioned|p14|||Strat.||||||
9477|Keswick Clay|34180|6|Mentioned|p216|||Lower - Middle Pleistocene. See also P217.||||||
9477|Keswick Clay|34181|4|Described|p44|||Pleistocene||||||
9477|Keswick Clay|38068|6|Mentioned|Fig.8|||||||||
9477|Keswick Clay|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
9477|Keswick Clay|40442|6|Mentioned|Fig.23|||||||||
9477|Keswick Clay|41119|2|Defined|p4|middle Pleistocene|middle Pleistocene|||||||
9477|Keswick Clay|41151|6|Mentioned|p11|||||||||
9477|Keswick Clay|41362|5|Briefly described|Fig.2|||||||||
9477|Keswick Clay|41506|5|Briefly described|Fig.2|||||||||
9477|Keswick Clay|42733|5|Briefly described|map legend|Quaternary||||||||
9477|Keswick Clay|44133|5|Briefly described|p242|Pleistocene|Pleistocene|Overlies: Hindmarsh Clay. Generally less than 6m thick.||||||
9477|Keswick Clay|65901|5|Briefly described|p176 Tab.1|Pleistocene|Pleistocene|Of Sheard and Bowman (1987). Equivalent to Ngaltinga Clay. Middle Pleistocene age.||||||08-MAR-12
9477|Keswick Clay|73188|5|Briefly described|[See comments]|Pleistocene|Pleistocene|St Vincent Basin and Mount Lofty Ranges. p: 319-320, 330-332, 346, 349, 351, 357-359.||||Underlain by Hindmarsh Clay. Equivalent to Ngaltinga Formation.|Smectite-rich clays characterised by gilgai structures.|
9477|Keswick Clay|73236|4|Described|p36-38, p43-44, p48|Pleistocene|Pleistocene|Floodplain and lacustrine sediments. Boundary with underlying Hindmarsh Clay is indicated by a subtle but persistent colour change.|c. 2-0.13 Ma|||Underlain by Hindmarsh Clay. Overlain by Pooraka Formation.|Blue-grey expansive clay, locally with gilgai structures.|
9569|Kilroo Formation|23282|6|Mentioned|p54|||of Polda Basin. May be equivalent to Cadlareena Volcanics.||||||
9569|Kilroo Formation|24553|5|Briefly described|p37|Proterozoic|Proterozoic|Geological Province: Polda Trough.||||||07-FEB-11
9569|Kilroo Formation|41363|2|Defined|p17|Proterozoic||Reserved as Kilroo||||||
9569|Kilroo Formation|42246|6|Mentioned|p16|||||||||
9569|Kilroo Formation|42716|6|Mentioned|Map legend|Neoproterozoic||||||||
9569|Kilroo Formation|42738|5|Briefly described|map legend|Neoproterozoic||||||||
9569|Kilroo Formation|43049|4|Described|p18|||||||||
9569|Kilroo Formation|43052|4|Described|p202|||||||||
9569|Kilroo Formation|43560|5|Briefly described|p233|||||||||
9569|Kilroo Formation|43671|6|Mentioned|p4||Neoproterozoic|||||||
9569|Kilroo Formation|44133|5|Briefly described|p72 Fig. 8.11|Neoproterozoic|Neoproterozoic|Geological Province: Polda Basin. Overlain by Polda Formation.||||||
9569|Kilroo Formation|62893|4|Described|Map Legend, p16-18, p29, p36|Late Proterozoic|Late Proterozoic|Polda Basin (probably the basal unit). Consists of three intervals of clastic sediments, two zones of amygdaloidal basalt and one thin (2.6 m) crystal tuff bed containing probable pumice clasts, glass shards and very angular fragments of quartz and feldspar. K-Ar plagioclase ages of 768 +/- 9 Ma and 764 +/- 42 Ma are considered magmatic ages (Fanning et al., 1986). The lowermost volcanic interval includes 10 separate flows which range in thickness from 0.5 to 24 m, and grade from massive at the base to medium/coarse-grained amygdaloidal basalt in the centre to vesicular, purplish brown at the top. Probably represents an intracratonic graben or rift valley with predominantly basic volcanism with sedimentation in arid, terrestrial fluvial systems and playa lakes. Displays cross-bedding, scour and fill, dewatering and flame structures, graded bedding and desiccation cracks.||||Unconformably overlain by Coolardie Formation.|Laminated red-brown siltstone and mudstone containing local anhydrite aggregates and veins; interbedded with basaltic volcanic units|
9569|Kilroo Formation|67536|6|Mentioned|Map Legend||||||||Claystone, siltstone, sandstone, halite, basalt.|
9569|Kilroo Formation|70027|6|Mentioned|p58|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Polda Basin.|||||Mixed clastics, evaporites and volcanics.|
9622|Kingston Greensand|24562|5|Briefly described|p55 Fig. 21|||Overlies: Knight Group.||||||
9622|Kingston Greensand|32898|6|Mentioned|Table 2-1|||||||||
9644|Kirton Point gneiss|37461|6|Mentioned|p322|||||||||
9686|Knotts Hill Sand|38290|4|Described|p75|||||||||
9715|Kokatha Granite|22430|6|Mentioned|p2||Proterozoic|||||||
9715|Kokatha Granite|33468|6|Mentioned|Fig.4|||||||||
9715|Kokatha Granite|33470|6|Mentioned|p463|||||||||
9715|Kokatha Granite|33557|6|Mentioned|p32|||||||||
9723|Koleroo Formation|31532|4|Described|p321|||||||||
9751|Kondoparinga Sandy Loam|38290|4|Described|p73|||||||||
9754|Kongal Rocks Granite|42275|6|Mentioned|Table 2 p474|||Geochemical analysis given.||||||23-AUG-18
9783|Koolunga Gravel|40037|6|Mentioned|p227|||||||||
9783|Koolunga Gravel|44133|5|Briefly described|p170, 165 Fig. 10.11|Pliocene|Pliocene|Geological Province: Saint Vincent Basin. Formerly Koolunga Gravels.||||||
9785|Koolywurtie Limestone Member|23981|5|Briefly described|p8-9 Fig. 4, p31|Early Cambrian|Early Cambrian|Of Parara Limestone. Complex stacked bioherms and flanking beds capped by fenestral, stromatolite-like Proaulopora boundstone. Different lithologies for various parts of basin. Max.thick:50m. Geol.Prov:Stansbury Basin. One outcrop known as "Teppers Knoll"||||||
9785|Koolywurtie Limestone Member|35255|6|Mentioned|Fig.8|||||||||
9785|Koolywurtie Limestone Member|36244|6|Mentioned|p2|||Refers Thomson et al.1976.||||||
9785|Koolywurtie Limestone Member|42225|4|Described|p221|||||||||
9785|Koolywurtie Limestone Member|42488|5|Briefly described|Fig.2 P187|||||||||
9785|Koolywurtie Limestone Member|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Parara Limestone.  Geological Province: Stansbury Basin.||||||14-APR-05
9785|Koolywurtie Limestone Member|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Parara Limestone. Contains bioherms of archaeocyaths (S. favus beds).  Age is Late Atdabanian to Botoman. Geological Province: Stansbury Basin.||||||06-JUN-05
9785|Koolywurtie Limestone Member|65686|6|Mentioned|p413|||||Of the Parara Limestone.||||07-MAY-12
9785|Koolywurtie Limestone Member|65892|6|Mentioned|p9 Fig.4, p24.|Early Cambrian|Early Cambrian|Appears as Koolywurtie Limestone (p24) and as Koolywurtie Member (p9 Fig.4). Yorke Peninsula. Probable source of archaeocyath-bearing clasts in early stage of deposition of White Point Conglomerate.||Unit in Parara Limestone.||||
9785|Koolywurtie Limestone Member|71102|5|Briefly described|p258|||Of Stansbury Basin.||Unit of Parara Limestone.||||
9785|Koolywurtie Limestone Member|73247|6|Mentioned|p207|Cambrian (Stage 4)|Cambrian (Stage 3)|Yorke Peninsula.||Parara Limestone||Equivalent to Mount McDonnell Formation.||03-FEB-23
9794|Koonunga Phosphorite Member|30052|6|Mentioned|p83|||Cambrian age.||||||
9794|Koonunga Phosphorite Member|30801|6|Mentioned|p5|||Lower Cambrian (Wanakanda Linestone) Table P5-6||||||
9794|Koonunga Phosphorite Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
9794|Koonunga Phosphorite Member|34959|6|Mentioned|p284|||||||||
9794|Koonunga Phosphorite Member|40442|5|Briefly described|p13|||||||||
9794|Koonunga Phosphorite Member|40852|6|Mentioned|p32|||||||||
9794|Koonunga Phosphorite Member|40856|5|Briefly described|p312|||||||||
9805|Kootaberra Formation|31532|2|Defined|p326|Cenozoic|Cenozoic|||||||19-NOV-08
9806|Kooyonga Formation|22541|6|Mentioned|p13|||||||||23-AUG-18
9806|Kooyonga Formation|42733|6|Mentioned|map legend|Tertiary||||||||
9864|Kuitpo Gravelly Sandy Loam|38290|4|Described|p71|||||||||
9889|Kulpara Formation|22643|5|Briefly described|p191, fig3|Early Cambrian|Early Cambrian|||||||
9889|Kulpara Formation|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
9889|Kulpara Formation|23482|5|Briefly described|p9|Early Cambrian|Early Cambrian|||||||
9889|Kulpara Formation|23719|5|Briefly described|p26|Cambrian|Cambrian|Formerly Kulpara Limestone. Geological Province: Gawler Craton.||||||
9889|Kulpara Formation|23731|5|Briefly described|p20, p28, p72|Early Cambrian|Early Cambrian|Of Hawker Group.  Geological Province: Stansbury Basin.||||||
9889|Kulpara Formation|23981|5|Briefly described|p8-9 Fig. 4, p21, p28, p31|Early Cambrian|Early Cambrian|Supersedes Kulpara Lst. On Yorke Pen. is of recrystallised/dolomitised limestone, stromatolites, interbedded oolite with common interclastic layers. Known as  "Marbles" of Tepper (1882). Conformable on Wimulta Fm. Max. thick: 370m; 25m at type section.||||||12-FEB-07
9889|Kulpara Formation|24360|5|Briefly described|p53|Cambrian|Cambrian|Geological Province: Yorke Peninsula, Gawler Craton||||||03-MAY-13
9889|Kulpara Formation|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
9889|Kulpara Formation|35255|6|Mentioned|Fig.8|||||||||
9889|Kulpara Formation|40852|6|Mentioned|p32|||||||||
9889|Kulpara Formation|40856|6|Mentioned|Fig.23.6|||||||||
9889|Kulpara Formation|41526|6|Mentioned|p36|||See also p61.||||||12-FEB-07
9889|Kulpara Formation|42222|6|Mentioned|Table 1 P4|||||||||
9889|Kulpara Formation|42225|4|Described|p220|||||||||
9889|Kulpara Formation|42232|5|Briefly described|284|||||||||
9889|Kulpara Formation|42498|5|Briefly described|Map legend|Late Cambrian|Early Cambrian|||||||
9889|Kulpara Formation|42506|5|Briefly described|Map legend|Early Cambrian||||||||
9889|Kulpara Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone.||||||25-MAY-05
9889|Kulpara Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
9889|Kulpara Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
9889|Kulpara Formation|44133|5|Briefly described|p3|Botomian|Atdabanian|Conformably underlies Parara Limestone.||||||
9889|Kulpara Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Spencer Shelf.||||||27-APR-05
9889|Kulpara Formation|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Dolomite massive to thick-bedded, vuggy and locally stromatolitic. Limestone thick-bedded, vuggy, locally oolitic with intraclasts and fossiliferous. Geological Province: Stansbury Basin.||||||22-APR-05
9889|Kulpara Formation|60990|6|Mentioned|p85|||Small shelly fossils demonstrate a strong faunal link between Australia and Antarctica during the Botoman.||||||
9889|Kulpara Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate. Geological Province: Arrowie Basin.||||||
9889|Kulpara Formation|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Upper limestone unit and lower dolomite unit.  Dolomite massive to thick bedded, vuggy and locally stromatolitic. Limestone thick bedded, vuggy, locally oolitic with intraclasts and fossiliferous. Geological Province: Stansbury Basin.||||||06-JUN-05
9889|Kulpara Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Upper thick-bedded limestone (Atdabanian archaeocyathids) and lower dolomite, locally stromatolitic.||||||03-MAY-13
9889|Kulpara Formation|65375|4|Described|pp26-29, p40, p54.|Cambrian|Cambrian|Thickness up to 355m. Dolomite deposited in tidal to nearshore subtidal carbonate platform; limestone contains abundant archaeocyaths. Dolomite quarried for flux in steel making.||||Overlies Winulta Formation. Dolomite unconformably overlain by Parara Limestone, separated by red ferruginous stromatolitic horizon.|Dolomite, massive to thick-bedded, vuggy and locally stromatolitic; limestone, thick-bedded, minor thin-bedded, locally oolitic and stratiform algal mats.|
9889|Kulpara Formation|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
9889|Kulpara Formation|65686|6|Mentioned|p418|||||||||
9889|Kulpara Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Winulta Formation. Is overlain by Parara Limestone.||
9889|Kulpara Formation|66761|5|Briefly described|p245-246, 245, 254|Cambrian|Cambrian|Underlies the Parara Limestone. Overlies the ?Wangkonda Formation in Investigator 1 (Kangaroo Island). Better known from Yorke Peninsula.||||||14-MAR-12
9889|Kulpara Formation|67536|6|Mentioned|Map Legend||||||||Marine shelf to basinal carbonate, minor basal sandstone.|
9889|Kulpara Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||||||
9889|Kulpara Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
9889|Kulpara Formation|70382|6|Mentioned|p28|||Geological province: Stansbury Basin. Deposited in marine  environment.||||Underlain by Winulta Formation. Overlain by Parara Formation.||
9889|Kulpara Formation|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
9889|Kulpara Formation|73103|5|Briefly described|Map legend.|Cambrian|Cambrian|Has the map symbol of Eok. Also appears with the symbol Eo1 as a combined unit with Winulta Formation.|||||Dolomite and limestone, stromatolitic and fenestral, micritic; ooid grainstone.|
9889|Kulpara Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Upper thick-bedded limestone (Atdabanian archaeocyathids) and lower dolomite, locally stromatolitic.|
9889|Kulpara Formation|73247|6|Mentioned|p205|Cambrian (Stage 2)|Cambrian (Stage 2)|"Yorke Peninsula. [Also written as ""Kulpara Formation"" in the Kangaroo Island Investigator 1 Big Gully section; inferred to indicate tentative correlation]."||||Underlain by Winulta Formation. Unconformably overlain by Parara Limestone. Partly equivalent to Mount McDonnell Formation.||
9947|Kutjitara Formation|23155|6|Mentioned|p36|||||||||
9947|Kutjitara Formation|24175|6|Mentioned|p42|Quaternary|Quaternary|Overlain by Katipiri Formation.||||||
9947|Kutjitara Formation|24321|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||
9947|Kutjitara Formation|42375|4|Described|p45-50|||Lake Eyre Basin.||||||
9947|Kutjitara Formation|42592|5|Briefly described|p270, 273|||See also p274. Typesection shown p272.||||||18-SEP-18
9947|Kutjitara Formation|42746|5|Briefly described|p22|||||||||
9947|Kutjitara Formation|42784|6|Mentioned|p494|||||||||
9947|Kutjitara Formation|43041|5|Briefly described|p591|||||||||
9947|Kutjitara Formation|61155|5|Briefly described|p17|Pleistocene|Late Pliocene|Overlies the Tirari Formation; underlies the Katipiri Formation. Age: 2.5-1.5Ma. Geological Province: Lake Eyre Basin.||||||
9947|Kutjitara Formation|66131|5|Briefly described|p240, p242, p246-247|Pleistocene|Pleistocene|Fluvio-lacustrine and aeolian conditions. May be middle Pleistocene or interglacial stage 7 based on thermoluminescence and electron spin resonance. Contains vertebrate fossils.||||Overlies Etadunna Formation. Forms channel fills cut into the Tirari Formation. Is overlain by Katipiri Formation.|Horizontally bedded fine sand and red mud interbedded with shallow channel fill sand, laminated gypsum sand and green clay.|
9947|Kutjitara Formation|66573|5|Briefly described|p873, p875 Tb.2|Pleistocene|Pleistocene|Overlies the Tirari Formation unconformably. Red gypsiferous claystones and sandstones.||||||
9947|Kutjitara Formation|68715|6|Mentioned|p30 Fig.5|Pleistocene|Pleistocene|Tirai and northern Callabonna sub basins, Lake Eyre Basin.||||||
9947|Kutjitara Formation|69023|6|Mentioned|p124|||Probably partly equivalent to Yandruwantha Sand.||||||
9969|Kyeema Clay|38290|5|Briefly described|p60|||||||||
9990|Lacepede Formation|22541|6|Mentioned|Fig 16|||Otway Formation||||||
9990|Lacepede Formation|23010|6|Mentioned|p340|||||||||
9990|Lacepede Formation|23249|6|Mentioned|Fig.2||Late Eocene|||||||
9990|Lacepede Formation|23322|5|Briefly described|962|Late Eocene|Middle Eocene|of McGowran (1973). Geological Province: Gambier Basin.||||||07-SEP-09
9990|Lacepede Formation|23818|5|Briefly described|p174 Fig.84, p177|Late Eocene|Middle Eocene|Geological Province: Otway Basin. Underlain by Kongorong Sand. Overlain by Gambier Limestone. Max. thickness: 37 ft.||||||09-DEC-08
9990|Lacepede Formation|24562|5|Briefly described|p15 Fig. 4|Late Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
9990|Lacepede Formation|29355|6|Mentioned|p188|||||||||
9990|Lacepede Formation|29591|6|Mentioned|p92|||||||||
9990|Lacepede Formation|29697|6|Mentioned|Fig.11|||||||||
9990|Lacepede Formation|30754|6|Mentioned|p13|||See also p14. Stratigraphic table.||||||09-DEC-08
9990|Lacepede Formation|31245|5|Briefly described|p82|||||||||
9990|Lacepede Formation|31247|6|Mentioned|p162|||Microplankton. Refers Traverse (1955)||||||
9990|Lacepede Formation|31624|6|Mentioned|p111|||M.-U.Eocene||||||
9990|Lacepede Formation|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
9990|Lacepede Formation|31850|6|Mentioned|p34|||||||||
9990|Lacepede Formation|31920|3|Fully described|p58|||Eocene. See also Fig.3-2,4,5.||||||
9990|Lacepede Formation|31922|6|Mentioned|p169|||||||||
9990|Lacepede Formation|32116|4|Described|p47|||||||||
9990|Lacepede Formation|32117|6|Mentioned|Fig.2|||||||||
9990|Lacepede Formation|32120|6|Mentioned|p276|||Eocene fauna||||||
9990|Lacepede Formation|32894|5|Briefly described|p287|||Eocene||||||
9990|Lacepede Formation|32895|6|Mentioned|p328|||Tertiary||||||
9990|Lacepede Formation|32897|6|Mentioned|p180|||U.Eocene||||||
9990|Lacepede Formation|32898|6|Mentioned|Table 2-1|||||||||
9990|Lacepede Formation|33109|6|Mentioned|p84|||Separates aquifers||||||
9990|Lacepede Formation|33224|6|Mentioned|p69|||Palynology||||||
9990|Lacepede Formation|33716|5|Briefly described|Table 2|||||||||
9990|Lacepede Formation|33798|6|Mentioned|Fig.2|||||||||
9990|Lacepede Formation|33938|6|Mentioned|p48|||Refs McGowran et al (1971) & Harris (1971).||||||
9990|Lacepede Formation|34308|4|Described|p177|||Johannian - Aldingan||||||
9990|Lacepede Formation|34658|5|Briefly described|p98|||||||||
9990|Lacepede Formation|35018|5|Briefly described|p29|||||||||
9990|Lacepede Formation|35066|6|Mentioned|p209|||||||||
9990|Lacepede Formation|35147|6|Mentioned|Table.1|||||||||
9990|Lacepede Formation|38068|6|Mentioned|Fig.7|||||||||
9990|Lacepede Formation|38903|5|Briefly described|Table 2|||||||||
9990|Lacepede Formation|39077|6|Mentioned|Table 2|||||||||
9990|Lacepede Formation|39408|6|Mentioned|Fig.5|||||||||
9990|Lacepede Formation|39923|6|Mentioned|p354|||||||||
9990|Lacepede Formation|40429|6|Mentioned|p28|||||||||
9990|Lacepede Formation|40557|6|Mentioned|p169|||||||||
9990|Lacepede Formation|41520|5|Briefly described|Fig.12|||||||||
9990|Lacepede Formation|41626|6|Mentioned|p54|||||||||
9990|Lacepede Formation|41627|5|Briefly described|p69|||||||||
9990|Lacepede Formation|42827|6|Mentioned|p283|||||||||
9990|Lacepede Formation|42966|5|Briefly described|p110, Fig.57|||Otway Basin||||||
9990|Lacepede Formation|43675|6|Mentioned|340|||||||||
9990|Lacepede Formation|43700|6|Mentioned|p24||Late Eocene|||||||
9990|Lacepede Formation|43813|6|Mentioned|p133|||||||||
9990|Lacepede Formation|46839|6|Mentioned|Fig.3|||||||||
9990|Lacepede Formation|47054|5|Briefly described|Fig.3 P481|||||||||
9990|Lacepede Formation|61155|5|Briefly described|p19|Early Oligocene|Middle Eocene|Overlies Kangarong Sand. Thickness: 200m. Geological Province: Otway Basin (Gambier Embayment). ||||||
9990|Lacepede Formation|65891|6|Mentioned|p221 Fig.5.|Rupelian|Bartonian|W Otway Basin.||||||
