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
39|Aberdare Conglomerate|12597|5|Briefly described|p491, p492 Tb.1|Rhaetian|Rhaetian|N Clarence-Moreton Basin. Basal, high energy fluvial deposits on top of eroded surface of Ipswich and Nymboida Basins.||Unit in Woogaroo Subgroup.|||Conglomerate, coarse lithic sandstone.|
39|Aberdare Conglomerate|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
39|Aberdare Conglomerate|22757|5|Briefly described|Table5,p10|Late Triassic|Late Triassic|Ipswich-Moreton Basin. 380+ m.||||||
39|Aberdare Conglomerate|23799|5|Briefly described|p46|Late Triassic|Late Triassic|Of Woogaroo Group.  Overlain by Raceview Formation.  Geological Province: Clarence-Moreton Basin.  See also p48 Fig. 3.||||||
39|Aberdare Conglomerate|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 40m.||||||
39|Aberdare Conglomerate|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
39|Aberdare Conglomerate|29385|6|Mentioned|p82|||Jurassic||||||
39|Aberdare Conglomerate|30086|5|Briefly described|p4|||Triassic. Part of Bundamba Group.||||||
39|Aberdare Conglomerate|30087|4|Described|p3|||See also P4. Unit of Bundamba Group||||||27-SEP-05
39|Aberdare Conglomerate|30302|6|Mentioned|p415|||Refers Staines(1964)||||||
39|Aberdare Conglomerate|30458|6|Mentioned|p1|||Late Triassic (Norian or Rhaetian). See also P39-40.||||||
39|Aberdare Conglomerate|30459|6|Mentioned|p309|||Triassic age||||||
39|Aberdare Conglomerate|30461|6|Mentioned|p100|||||||||
39|Aberdare Conglomerate|30464|6|Mentioned|p4|||Triassic microfossils||||||
39|Aberdare Conglomerate|30465|6|Mentioned|p4|||Triassic microfossils||||||
39|Aberdare Conglomerate|30470|6|Mentioned|p459|||||||||
39|Aberdare Conglomerate|30472|6|Mentioned|p132|||Pollen distribution.||||||
39|Aberdare Conglomerate|30474|6|Mentioned|p251|||Correlation chart P251||||||
39|Aberdare Conglomerate|30475|6|Mentioned|Fig.14.3|||||||||
39|Aberdare Conglomerate|30477|6|Mentioned|p461|||||||||
39|Aberdare Conglomerate|30478|6|Mentioned|p272|||||||||
39|Aberdare Conglomerate|30701|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||11-JAN-10
39|Aberdare Conglomerate|30915|6|Mentioned|p100|||||||||
39|Aberdare Conglomerate|30916|6|Mentioned|p99|||||||||
39|Aberdare Conglomerate|31118|4|Described|p320|||||||||
39|Aberdare Conglomerate|32136|6|Mentioned|p5|||Miospores||||||
39|Aberdare Conglomerate|32176|6|Mentioned|p2|||See also P3&4 & Figs. 2&3||||||
39|Aberdare Conglomerate|32179|6|Mentioned|p3|||Trias.||||||
39|Aberdare Conglomerate|32180|5|Briefly described|p6|||||||||
39|Aberdare Conglomerate|32491|5|Briefly described|p19||Late Triassic|||||||
39|Aberdare Conglomerate|32492|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
39|Aberdare Conglomerate|32801|6|Mentioned|p266|||||||||
39|Aberdare Conglomerate|33381|4|Described|p110|||See also P116-118. Triassic. Overlies Ipswich Coal Measures||||||28-NOV-05
39|Aberdare Conglomerate|33476|6|Mentioned|p99|||||||||
39|Aberdare Conglomerate|34010|6|Mentioned|Cor. chart|||Jurassic||||||
39|Aberdare Conglomerate|34235|6|Mentioned|p91|||||||||
39|Aberdare Conglomerate|34354|6|Mentioned|p3|||See also P12. Triassic.||||||
39|Aberdare Conglomerate|34457|6|Mentioned|p484|||Correlates with Borallon Beds||||||
39|Aberdare Conglomerate|34505|6|Mentioned|p3|||Bundamba Group. See also Figs.8-11||||||
39|Aberdare Conglomerate|35007|6|Mentioned|p76|||||||||
39|Aberdare Conglomerate|35079|6|Mentioned|p424|||||||||
39|Aberdare Conglomerate|35101|6|Mentioned|p51|||||||||
39|Aberdare Conglomerate|36237|6|Mentioned|Map legend|Late Jurassic|Late Triassic|Late Triassic to Early Jurassic||||||
39|Aberdare Conglomerate|36243|6|Mentioned|Table 8A|||||||||
39|Aberdare Conglomerate|36351|6|Mentioned|p373|||||||||
39|Aberdare Conglomerate|36354|4|Described|p371|||||||||
39|Aberdare Conglomerate|36779|6|Mentioned|p7|||||||||
39|Aberdare Conglomerate|36825|6|Mentioned|p12|||||||||
39|Aberdare Conglomerate|36899|6|Mentioned|p1085|||See also P1095.||||||
39|Aberdare Conglomerate|37122|5|Briefly described|Table 1|||||||||
39|Aberdare Conglomerate|37456|6|Mentioned|p268|||||||||
39|Aberdare Conglomerate|37463|6|Mentioned|p483|||||||||
39|Aberdare Conglomerate|37616|6|Mentioned|p33|||||||||
39|Aberdare Conglomerate|37812|6|Mentioned|p657|||||||||
39|Aberdare Conglomerate|38074|5|Briefly described|Table 1|||||||||
39|Aberdare Conglomerate|38076|6|Mentioned|Table 3|||||||||
39|Aberdare Conglomerate|38306|6|Mentioned|p509|||||||||
39|Aberdare Conglomerate|38307|4|Described|p521|||||||||
39|Aberdare Conglomerate|38441|6|Mentioned|Map legend|Rhaetian|Rhaetian|||||||
39|Aberdare Conglomerate|39445|5|Briefly described|Table 10|||||||||
39|Aberdare Conglomerate|39907|6|Mentioned|p8|||||||||
39|Aberdare Conglomerate|39943|6|Mentioned|Table 10A|||||||||
39|Aberdare Conglomerate|40434|6|Mentioned|p25|||||||||
39|Aberdare Conglomerate|40623|5|Briefly described|p34|||||||||
39|Aberdare Conglomerate|41591|5|Briefly described|p19|||||||||
39|Aberdare Conglomerate|41906|3|Fully described|Table 2 P17|||||||||
39|Aberdare Conglomerate|42248|6|Mentioned|p397|||||||||
39|Aberdare Conglomerate|42316|6|Mentioned|p5|||||||||
39|Aberdare Conglomerate|42336|5|Briefly described|p6|||||||||
39|Aberdare Conglomerate|42405|6|Mentioned|Table 3 P.7|||||||||
39|Aberdare Conglomerate|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundamba Group).||||||27-AUG-08
39|Aberdare Conglomerate|42869|5|Briefly described|Table 1, P33|||Of Woogaroo Subgroup.||||||27-AUG-08
39|Aberdare Conglomerate|42893|5|Briefly described|Fig.2 P7|||||||||
39|Aberdare Conglomerate|42894|5|Briefly described|Fig.1 P20|||||||||
39|Aberdare Conglomerate|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
39|Aberdare Conglomerate|43736|5|Briefly described|Table 1,p4|||||||||
39|Aberdare Conglomerate|43881|14|Not recorded|p134|||Orange card has 'conglomerate' listed||||||
39|Aberdare Conglomerate|43910|14|Not recorded|p1,3,14,17-18,Fig.2|||||||||
39|Aberdare Conglomerate|43991|6|Mentioned|p46|||Ref.to Wilson 1960||||||
39|Aberdare Conglomerate|43993|14|Not recorded|p97,102|||||||||
39|Aberdare Conglomerate|44026|14|Not recorded|p123|||||||||
39|Aberdare Conglomerate|44091|14|Not recorded|p51||Triassic|||||||
39|Aberdare Conglomerate|44432|14|Not recorded|p53||Late Triassic|||||||
39|Aberdare Conglomerate|44510|2|Defined|p252-7,260,Fig.35-6|||Unconformably overlies Ipswich Coal Measures.||||||
39|Aberdare Conglomerate|44542|14|Not recorded|p36|||||||||
39|Aberdare Conglomerate|44678|14|Not recorded|p1|||||||||
39|Aberdare Conglomerate|44734|14|Not recorded|p5,11-13,19|||Pine Mountain area.||||||
39|Aberdare Conglomerate|44771|14|Not recorded|p1,Fig.3,4|||Part of Bundamba Group.||||||
39|Aberdare Conglomerate|44774|2|Defined|p30,31||Late Triassic|Lowest unit of Bundamba Group. Conformably overlain by Raceview Formation, disconformably overlies Blackstone Formation. Now given formation status.||||||
39|Aberdare Conglomerate|44775|4|Described|p7,9,map 2||Late Triassic|||||||
39|Aberdare Conglomerate|44776|14|Not recorded|p3-5,Figs.3-5||Late Triassic|Member of Bundamba Group.||||||
39|Aberdare Conglomerate|44783|14|Not recorded|p13,16,17|||||||||
39|Aberdare Conglomerate|44884|4|Described|p1,2,3,4, Figs.1,7|||||||||
39|Aberdare Conglomerate|44885|14|Not recorded|p2,3,Fig.3|||||||||
39|Aberdare Conglomerate|45110|3|Fully described|Table 17|||||||||
39|Aberdare Conglomerate|48917|5|Briefly described|p13|||Stratigraphic Table. Upper Triassic||||||
39|Aberdare Conglomerate|60726|6|Mentioned|p16.|Late Triassic|Late Triassic|Ipswich area. Contains fossil Samarura sp.||||||
39|Aberdare Conglomerate|60993|5|Briefly described|p4, p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Pebble conglomerate, shale, siltstone; pink to brown claystone; minor coal. Overlain by Ripley Road Sandstone. Geol. Prov: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|60995|6|Mentioned|p54|||Equivalent to Laytons Range Conglomerate (Woogaroo Subgroup) in the type area.||||||
39|Aberdare Conglomerate|60996|5|Briefly described|p72, p74|||Unconformably overlain by Gatton Sandstone. Geological Province: Clarence-Moreton Basin. Equivalent of Laytons Range Conglomerate.||||||
39|Aberdare Conglomerate|60999|5|Briefly described|p164|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. See also p169.||||||
39|Aberdare Conglomerate|61002|5|Briefly described|p202|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|61005|6|Mentioned|p253, p254|||Equivalent to Laytons Range Conglomerate. See also p255 Figs. 23, 24 and 25. ||||||
39|Aberdare Conglomerate|61006|5|Briefly described|p278 Fig. 2|Triassic|Triassic|Conglomerate, labile sandstone, mudstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1.||||||
39|Aberdare Conglomerate|61310|6|Mentioned|p31|||Geological Province: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
39|Aberdare Conglomerate|64665|5|Briefly described|p53 Fig.2, p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin.||Basal unit in Woogaroo Subgroup.||Is overlain by Raceview Formation.|High energy conglomerate and sandstone.|
39|Aberdare Conglomerate|64856|6|Mentioned|p80|Rhaetian|Norian|Moreton Basin. Grades laterally into Precipice Sandstone to west. Base of Bundamba Group.| | ||||28-NOV-17
39|Aberdare Conglomerate|67402|5|Briefly described|p165 tbl LPB1|Norian|Norian|Clarence-Moreton Basin. See also p187, p188, p193, p223, p225.||Woogaroo Subgroup||Overlies the Blackstone Formation. Overlain by the Raceview Formation.|Conglomerates with minor coarse lithic sandstones.|
39|Aberdare Conglomerate|68679|5|Briefly described|p394|||||Woogaroo Subgroup.||Disconformably overlies Blackstone Formation (Brassall Subgroup).||
39|Aberdare Conglomerate|69594|4|Described|p519, p534, p543-547, p572|Late Triassic|Late Triassic|Northern Clarence-Moreton Basin. Is known as Laytons Range Conglomerate in NSW. In many places the unit is a single thin conglomerate; locally wedges out. The basal shale-siltstone is <1m thick and consists of weathered needles of iron carbonate in a pinkish Fe-rich matrix; it forms a consistent marker bed in many boreholes.||Woogaroo Subgroup.||Unconformably overlies Ipswich Coal Measures. Is overlain by Raceview Formation; both are equivalent to the Eddystone beds.|Pebble to cobble polymict conglomerate; some beds with rippled fine sandstone laminae, others extensively rooted, thin claystones in places; a pinkish grey shale and siltstone underlies conglomerate at base.|
39|Aberdare Conglomerate|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Northern Clarence-Moreton Basin area.||||||
52|Abernethy Basalt|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Of the Aranbanga Volcanic Group.||||||23-DEC-09
52|Abernethy Basalt|41738|2|Defined|p169|Late Triassic||Reserved as Abernethy.||||||05-MAR-08
52|Abernethy Basalt|41778|6|Mentioned|Table 1|||||||||
52|Abernethy Basalt|41790|5|Briefly described|p474|||||||||
52|Abernethy Basalt|42054|6|Mentioned|p272|||||||||
52|Abernethy Basalt|63821|5|Briefly described|p21|Late Triassic|Late Triassic|Part of the Aranbanga Volcanic Group. Age: 221+/-4Ma (K-Ar whole rock). Fine to coarse basalt with olivine phenocrysts.||||||07-FEB-11
52|Abernethy Basalt|65452|5|Briefly described|p36 Fig.17|Late Triassic|Late Triassic|Also appears in Fig.17 as Abernety Basalt. Trace elements briefly described; has "within plate" type pattern.||Aranbanga Volcanic Group.||||
52|Abernethy Basalt|68679|4|Described|p437, p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. An extensive unit. Up to ~40m thick. Has distinctive OIB-like trace element geochemistry.|221 +/- 4 Ma (K-Ar whole rock: Murray et al.,1989)|Aranbanga Volcanic Group.||Unconformably overlies Wigton Granite and Toogoolawah Group. Possibly part-equivalent to the Kinellan Basalt.|Fine- to medium-grained, sparsely porphyritic, olivine basalt lava with platy flow foliation.|
52|Abernethy Basalt|73450|5|Briefly described|p30, p34-35|||OIB-like geochemistry. May occur in the lower part of the Aranbanga Volcanic Group or may be older, belonging to the underlying Esk Trough sequence.|||||Olivine basalt.|
92|Adam Shale|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Green and red shale and sandstone, bioturbated.||||||
92|Adam Shale|12951|5|Briefly described|p143, p145 Fig 6|Early Cambrian|Early Cambrian|Georgina Basin.||||Laterally equivalent to Mount Baldwin Formation. Unconformably overlies Elkera Formation.|Siliciclastics.|
92|Adam Shale|22954|6|Mentioned|Fig3p9|Early Cambrian||||||||
92|Adam Shale|24111|5|Briefly described|p215 Fig. 11|Cambrian|Cambrian|Name appears as Adam only in text.  Geological Province: Georgina Basin.||||||
92|Adam Shale|35798|2|Defined|p312|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|37462|6|Mentioned|Fig.4.16|||||||||
92|Adam Shale|37928|6|Mentioned|Fig.4|||||||||
92|Adam Shale|37929|6|Mentioned|Fig.2|||||||||
92|Adam Shale|38157|6|Mentioned|p281, Table IX|||||||||
92|Adam Shale|39921|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|40856|6|Mentioned|Fig.23.6|||||||||
92|Adam Shale|40906|6|Mentioned|Fig.9|||||||||
92|Adam Shale|41103|6|Mentioned|p261|||||||||
92|Adam Shale|41388|6|Mentioned|p552|||||||||
92|Adam Shale|41524|6|Mentioned|Fig.3|||||||||
92|Adam Shale|41801|6|Mentioned|Fig.4|||||||||
92|Adam Shale|42059|6|Mentioned|Fig.2 P131|||||||||
92|Adam Shale|42956|5|Briefly described|p27|||||||||
92|Adam Shale|43595|5|Briefly described|p548,Fig.5-33,549||Early Cambrian|||||||
92|Adam Shale|45155|6|Mentioned|Fig.8|||||||||
92|Adam Shale|47035|6|Mentioned|p85|||||||||
92|Adam Shale|49027|5|Briefly described|p6|||||||||
92|Adam Shale|60122|6|Mentioned|p9, p11 Tb. 1|||Within Supersequence 4.  Disconformably overlain by Red Heart Dolostone.  See also p14.||||||11-MAY-05
92|Adam Shale|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group.  Shale; basal sandstone. Geological Province: southern Georgina Basin.||||||
92|Adam Shale|62983|6|Mentioned|p11|||Geological Province: Georgina Basin.||||||
92|Adam Shale|63450|4|Described|p78 Fig. 5, p80|Early Cambrian|Early Cambrian|Disconformably overlain by Red Heart Dolomite. Max. thickness: 16m. Geological province: Georgina Basin, West Toko Syncline. Comprises bioturbated red and green shale and sandstone; acritarchs.||||||07-FEB-11
92|Adam Shale|63562|6|Mentioned|p345|Early Cambrian|Ediacaran|Georgina Basin. ||||||
92|Adam Shale|64068|3|Fully described|p x, pp54-55, p57|Early Cambrian|Early Cambrian|Previously included in underlying Grant Bluff Formation. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Correlations: Mount Baldwin Formation, Octy Formation, Neutral Junction Formation, possibly Sylvester Sandstone.||Of Shadow Group.||Disconformably overlies Grant Bluff Formation and underlies Red Heart Dolostone.|Green and brown pyritic shale, black shale toward top; minor brown-grey sandstone.|04-APR-12
92|Adam Shale|64778|6|Mentioned|p13|Cambrian|Cambrian|Toko Syncline, Southern Georgina Basin.||||||
92|Adam Shale|64812|5|Briefly described|p237 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
92|Adam Shale|64813|5|Briefly described|p256 Fig. 3|Early Cambrian|Early Cambrian|Overlain by Red Heart Dolostone. Geological Province: southern Georgina Basin.||||||11-FEB-09
92|Adam Shale|65237|5|Briefly described|p3 Fig. 4|Early Cambrian|Early Cambrian|Interfingers with Mount Baldwin Formation. Geological province: southern Georgina Basin.||||||07-FEB-11
92|Adam Shale|65342|6|Mentioned|p7.|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|67323|5|Briefly described|p83|Cambrian|Cambrian|West Toko Syncline, Georgina Basin.||||Is overlain unconformably by Red Heart Dolomite.||
92|Adam Shale|67402|6|Mentioned|p213 fig GRG3|Early Cambrian|Early Cambrian|Georgina Basin. ||||Unconformably overlain by the Red Heart Dolomite.||
92|Adam Shale|67870|6|Mentioned|p43|Early Cambrian|Early Cambrian|Georgina Basin.||||||
92|Adam Shale|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.||12-JUL-16
92|Adam Shale|69443|3|Fully described|p28:7, 14-15; 28:38 Fig.28.36|Early Cambrian|Early Cambrian|Walter in Walter et al. (1979). Southern Georgina Basin. Generally recessive unit. 16m thick in its type section in cored drillhole BMR Hay River-11B. Marine, presumably below wave-base, deposits.||Shadow Group.||Disconformably overlies Grant Bluff Formation. Is overlain disconformably by Red Heart Dolostone. Is correlated with Mount Baldwin, Octy and Neutral Junction Formations, and ?Sylvester Sandstone.|Laminated pyritic shale with sandy laminations; minor medium-coarse sandstone. Contains acritarchs and bioturbated beds.|12-JUL-16
92|Adam Shale|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Red Heart Dolostone||
92|Adam Shale|69673|5|Briefly described|p114 fig 92, p116, p119 fig 94|||16m thick.||Shadow Group|||Laminated pyritic shale with sandy laminations and minor sandstone.|
92|Adam Shale|69917|6|Mentioned|p115|||Georgina Basin. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin.||||||
92|Adam Shale|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation.||02-JUN-21
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||
151|Age Creek Formation|22954|6|Mentioned|Fig3p9||Undillan|||||||
151|Age Creek Formation|23031|5|Briefly described|17|||||||||
151|Age Creek Formation|23408|5|Briefly described|p527|Middle Cambrian|Middle Cambrian|Contains platform and platform-edge carbonates.||||||15-JUN-09
151|Age Creek Formation|30479|6|Mentioned|Fig.7|||Stratigraphic relationships||||||
151|Age Creek Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
151|Age Creek Formation|31506|6|Mentioned|p119|||||||||
151|Age Creek Formation|33111|4|Described|p27,31|||||||||
151|Age Creek Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
151|Age Creek Formation|34659|6|Mentioned|p227|||||||||
151|Age Creek Formation|35054|6|Mentioned|Table 23|||||||||
151|Age Creek Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
151|Age Creek Formation|35139|4|Described|Table.2|||||||||
151|Age Creek Formation|35553|6|Mentioned|p77|||See also Appendix 2, description of Agnostid localities.||||||
151|Age Creek Formation|36234|6|Mentioned|p168|||||||||
151|Age Creek Formation|37572|4|Described|p157|||See also Fig.7||||||
151|Age Creek Formation|38446|6|Mentioned|Table 23|||||||||
151|Age Creek Formation|39445|5|Briefly described|Table 4|||See also p62||||||17-JUL-06
151|Age Creek Formation|39690|6|Mentioned|Table 1|||||||||
151|Age Creek Formation|40686|5|Briefly described|p407|||||||||
151|Age Creek Formation|40855|6|Mentioned|Fig.24.1|||||||||
151|Age Creek Formation|41129|6|Mentioned|Fig.8|||||||||
151|Age Creek Formation|41240|6|Mentioned|Fig.1|||||||||
151|Age Creek Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
151|Age Creek Formation|44210|4|Described|map, Tb.2|||out crop||||||
151|Age Creek Formation|44211|2|Defined|p92,96||Middle Cambrian|See also Lexicon. Confined to Undilla Basin.||||||
151|Age Creek Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
151|Age Creek Formation|44274|14|Not recorded|p11|||||||||
151|Age Creek Formation|44275|14|Not recorded|Map Legend|||||||||
151|Age Creek Formation|44441|14|Not recorded|p.8|||Interfingers with Camooweal Dolomite.||||||
151|Age Creek Formation|44920|14|Not recorded|Map Legend, Sheet 2||Middle Cambrian|||||||
151|Age Creek Formation|45012|14|Not recorded|p338|||No data.||||||
151|Age Creek Formation|45052|3|Fully described|p95|||M. Camb.||||||
151|Age Creek Formation|45054|6|Mentioned|p6|||M.Cambrian. Fossil locality||||||
151|Age Creek Formation|45079|6|Mentioned|p18|||||||||
151|Age Creek Formation|45119|6|Mentioned|p4|||||||||
151|Age Creek Formation|47058|6|Mentioned|p134|||||||||
151|Age Creek Formation|48906|14|Not recorded|Tb.1|||||||||
151|Age Creek Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation.  Geological Province: eastern Georgina Basin.||||||
151|Age Creek Formation|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
151|Age Creek Formation|64068|4|Described|p62, 63, 64, 139, 225|||Totts Creek, northeastern Georgina Basin. Hosts Pb and Zn in fractures and vugs. Correlated with to Arthur Creek Formation, Inca Formation, Quita Formation, Roaring Siltstone, Devoncourt Limestone.||Narpa Group.|||Flat-lying to gently-dipping vuggy chert after dolostone; almost entirely covered by black soil and 'ironstone' duricrust (up to 9.5% Pb).|21-MAR-16
151|Age Creek Formation|64443|6|Mentioned|p14, p41|Boomerangian|Floran|Correlative of Ranken Limestone; laterally interdigitates with Camooweal Dolostone.||||||
151|Age Creek Formation|65337|6|Mentioned|p68.|||Laterally interdigitates with Camooweal Dolostone.||||||
151|Age Creek Formation|67323|4|Described|GIS tbl, map; p72, p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Unconformably overlies Beetle Creek Formation. Lateral equivalent of Camooweal Dolomite. Is overlain by Split Rock Sandstone.|Dolomite, pelletal dolomite, dolomitic limestone, limestone, calcarenite and dolarenite, chert nodules.|
151|Age Creek Formation|69443|5|Briefly described|p28:16, 20, 23|Middle Cambrian|Middle Cambrian|Georgina Basin. Appears as Age Creek Limestone in 18:20.||Narpa Group.||Is overlain by and partially interfingers with Currant Bush Limestone. Correlated with Ranken Limestone.||12-JUL-16
151|Age Creek Formation|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
151|Age Creek Formation|69591|4|Described|p87-90, p96, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Up to 1200m thick. Carbonate ramp deposits. Contains rich faunas of phosphatic brachiopods and trilobites in limestone interbeds. Interdigitates with Camooweal Dolostone (to the W) and with parts of Thorntonia, Currant Bush, V Creek and Mail Change Limestones and Inca Formation (to the E and NE).||Narpa Group.||Unconformably overlies Beetle Creek Formation; disconformably overlies Thorntonia Limestone. Is overlain by Split Rock Sandstone. See COMMENTS for more.|Sandy clastic, pelletal and two-tone crystalline dolomite and limestone with interbeds of calcareous sandstone. Cross-bedding common, with foresets up to 15m thick.|
151|Age Creek Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Currant Bush Limestone.|Dolomite.|
151|Age Creek Formation|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan. ||of Narpa Group.||||
151|Age Creek Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
151|Age Creek Formation|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Currant Bush Limestone|Dolomite.|
156|Agnes Water Volcanics|9194|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Volcanic breccia, ignimbrite, intermediate to acid flows, acid tuff, and minor sandstone.  Overlies both Curtis Island Group and Biggenden Beds.||||||23-DEC-09
156|Agnes Water Volcanics|30655|3|Fully described|p14|||See also Table 1||||||
156|Agnes Water Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
156|Agnes Water Volcanics|38391|6|Mentioned|p10|||||||||
156|Agnes Water Volcanics|39445|5|Briefly described|Table 9, p121|||||||||27-JAN-06
156|Agnes Water Volcanics|39505|6|Mentioned|p167|||||||||
156|Agnes Water Volcanics|40247|6|Mentioned|p207|||||||||
156|Agnes Water Volcanics|40623|5|Briefly described|p80|||||||||
156|Agnes Water Volcanics|41738|6|Mentioned|p168|||||||||
156|Agnes Water Volcanics|44785|2|Defined|p147,149||Triassic|Pyroclastics, minor flows of rhyolite, trachyte, andesite, little sandstone and shale.||||||
156|Agnes Water Volcanics|44786|14|Not recorded|p193-202|||Mid-late Triassic.||||||
156|Agnes Water Volcanics|45087|5|Briefly described|p99|||Chemical analyses.||||||
156|Agnes Water Volcanics|65452|4|Described|p1-46|Late Triassic|Late Triassic|Stevens (1968). Covers c.1,000 km2. Divided into three stratigraphically separate volcano-sedimentary facies associations: basal mafic to intermediate; middle dacitic, and topmost rhyolitic, facies associations. Each described in detail. The latter two were caldera-producing.|228.6 +/- 1.7 Ma (U-Pb SHRIMP zircon).|||Overlies or is faulted against Shoalwater and Brooweena Formations or Gympie Group. Is overlain locally by Myrtle Creek Sandstone.|Basaltic to andesitic lavas, minor pyroclastic and epiclastic deposits. Overlain by caldera-forming dacitic ignimbrite then caldera-forming rhyolitic ignimbrite and lavas.|05-MAR-19
156|Agnes Water Volcanics|65668|5|Briefly described|p1, p2 Tb.1, p11-13|Triassic|Triassic|Bundaberg area. Age: 228.6 +/- 1.7 Ma (SHRIMP U-Pb zircon). Extensive pile of terrestrial volcanic and volcaniclastic rocks: basal mafic lavas and volcaniclastics; dacitic ignimbrite and volcaniclastics; rhyolitic ignimbrite; rhyolite to dacite domes and cryptodomes. Unit has a genetic link to Eurimbula Granite which intrudes it. Lies unconformably on Permian sediments of the Gympie Group. Is overlain by Myrtle Creek Sandstone. Is intruded by Eurimbula Granite.||||||
156|Agnes Water Volcanics|67203|4|Described|p1-4, p31, p35-37|Late Triassic|Middle Triassic|Widespread unit. Mafic to intermediate lavas are geochemically similar to those in Bobby Volcanics and Agnes Waters Volcanics: may have formed in one continuous >100km long volcanic field. Associated with an extensive silicic caldera complex. Possible source of some pyroclastic and epiclastic material in this study area. Contemporaneous intrusive activity included emplacement of Eurimbula and Mount Bania Granites and Moolyung Granodiorite.|228.6 +/- 1.7 Ma (Cross et al., 2009).|||Is correlated with Bobby and Mount Marcella Volcanics.|Includes moderately porphyritic, coherent, flow-banded rhyolite.|
156|Agnes Water Volcanics|67874|5|Briefly described|p14, p19, p28, p31|||Shares many similarities with the adjacent Bobby Volcanics.|228.6 +/- 1.7 Ma (Cross et al., 2009).|||||
156|Agnes Water Volcanics|68319|5|Briefly described|Map Legend|Late Triassic|Middle Triassic|Subdivided into 4 unnamed units. Age shown for youngest unit. See map legend for a detailed lithological description.|228.6 +/- 1.7 Ma U-Pb SHRIMP|||Shown to intrude Shoalwater Formation, and overlie Gympie Group on cross section.|Rhyolite; rhyolitic ignimbrite; volcaniclastic sandstone, dacitic ignimbrite; basaltic to andesitic lavas.|05-SEP-14
156|Agnes Water Volcanics|68421|5|Briefly described|Map Legend|Late Triassic|Middle Triassic|Triassic Igneous Province.|||||Basaltic to andesitic lavas, thin pyroclastic deposits, volcaniclastic sandstone to boulder conglomerate.|
156|Agnes Water Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
156|Agnes Water Volcanics|68679|5|Briefly described|p312-313, p434, p436, p441-443, p472|Late Triassic|Late Triassic|Agnes Water-Biloela region, northern New England Orogen. Occupies an area >60km x >35km. Includes four subunits grouped into three volcaniclastic facies associations (detailed on p443).|228.6 +/- 1.7 Ma (SHRIMP: Cross et al., 2009).||||Basal basaltic to andesitic lavas and thin volcaniclastics, then dacitic rocks with dome growth, fluvial sedimentation, caldera collapse and thick dacitic ignimbrite; finally thick rhyolitic ignimbrite, with rhyolitic lava domes and cryptodomes.|
156|Agnes Water Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|229+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
156|Agnes Water Volcanics|73450|6|Mentioned|p3, p11|late Triassic|late Triassic|Calc-alkaline in composition.||||||
188|Airport Quartz Diorite|23423|5|Briefly described|p239|||Of the Almaden Supersuite.||||||22-JUL-08
188|Airport Quartz Diorite|23503|5|Briefly described|Map Legend||Late Carboniferous|Of Almaden Supersuite.||||||22-JUL-08
188|Airport Quartz Diorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 298. I-Type.||||||
188|Airport Quartz Diorite|23616|6|Mentioned|p67|||Of Almaden Supersuite.||||||
188|Airport Quartz Diorite|40743|6|Mentioned|Fig.2|||||||||
188|Airport Quartz Diorite|41740|6|Mentioned|p222|||||||||
188|Airport Quartz Diorite|41824|6|Mentioned|p201|||||||||
188|Airport Quartz Diorite|43259|4|Described|Appendix 1,p37.||Carboniferous|||||||
188|Airport Quartz Diorite|60425|4|Described|p74, p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Airport Suite (Almaden Supersuite). I-type. Dark green, fine-grained quartz diorite; mafic inclusions common; very similar to mafic units of the Almaden Suite.||||||07-FEB-11
221|Albert Basalt|30604|6|Mentioned|p68|||||||||
221|Albert Basalt|30687|5|Briefly described|p65|||See also P66,77. Tertiary age||||||
221|Albert Basalt|30689|5|Briefly described|p76|||Also mention Table on P76||||||
221|Albert Basalt|31130|6|Mentioned|Fig. 2|||L. Miocene||||||
221|Albert Basalt|32923|5|Briefly described|p27|||Analysis P29.||||||
221|Albert Basalt|32924|6|Mentioned|p111|||Extrusive of Focal Peak Shield Volcano.||||||
221|Albert Basalt|33290|4|Described|p37|||Anal. p39.||||||23-JUL-08
221|Albert Basalt|35050|6|Mentioned|p130|||||||||
221|Albert Basalt|35296|6|Mentioned|p12|||Re stratigraphy||||||
221|Albert Basalt|36806|5|Briefly described|p131|||||||||
221|Albert Basalt|39445|5|Briefly described|Table 14|||||||||
221|Albert Basalt|39969|6|Mentioned|p2|||||||||
221|Albert Basalt|40623|5|Briefly described|p39|||||||||
221|Albert Basalt|40896|4|Described|p45|||||||||
221|Albert Basalt|43005|5|Briefly described|p213|||||||||
221|Albert Basalt|43161|6|Mentioned|32|||||||||
221|Albert Basalt|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
221|Albert Basalt|44813|14|Not recorded|p80,86,90||Tertiary|20-0 Ma.||||||
221|Albert Basalt|48917|6|Mentioned|p38|||One map symbol for all units of Lamington Volcanics||||||
221|Albert Basalt|61007|6|Mentioned|p293|||||||||
221|Albert Basalt|69599|5|Briefly described|p631, p640|||Focal Peak volcano, between the Main Range and Tweed volcanoes. Table of chemical analyses.|25-20 Ma.|||Underlies the Beechmont Basalt. Equivalent to the Kyogle Basalt in NSW.||
221|Albert Basalt|73450|4|Described|p92, p96, p98|||Associated with the Focal Peak volcano. Comprises numerous thin flows averaging about 10 m thick with maximum thickness of 440 m; thins to the northeast.|||||Alkaline to subalkaline basalts; commonly microphenocrystic in olivine and/or plagioclase with sparse amygdales.|
221|Albert Basalt|73581|5|Briefly described|p7|||||Focal Peak Volcanics||Underlies Lamington Volcanics||
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||
305|Allingham Formation|24227|5|Briefly described|p425|Pliocene|Pliocene|||||||
305|Allingham Formation|24228|5|Briefly described|p439|Pliocene|Pliocene|||||||
305|Allingham Formation|29428|6|Mentioned|p31|||||||||
305|Allingham Formation|29433|2|Defined|p379|Pliocene|Pliocene|||||||
305|Allingham Formation|29675|6|Mentioned|p45|||||||||
305|Allingham Formation|32652|6|Mentioned|p279|||||||||
305|Allingham Formation|34976|6|Mentioned|p127|||||||||
305|Allingham Formation|35622|6|Mentioned|p357|||||||||
305|Allingham Formation|37606|4|Described|p355|||||||||
305|Allingham Formation|37607|4|Described|p337|||See also Fig.7||||||
305|Allingham Formation|38371|6|Mentioned|p657|||||||||
305|Allingham Formation|38373|6|Mentioned|p624|||||||||
305|Allingham Formation|39445|5|Briefly described|Table 14|||||||||
305|Allingham Formation|41537|6|Mentioned|p352|||See also Fig.2||||||
305|Allingham Formation|42589|6|Mentioned|p171|||||||||
305|Allingham Formation|45145|6|Mentioned|Table 7|||||||||
305|Allingham Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
305|Allingham Formation|61155|5|Briefly described|p20|Early Pliocene|Late Miocene|Underlies Campaspe Formation. Thickness: 18m. In the Townsville area.||||||03-MAR-10
305|Allingham Formation|64569|6|Mentioned|p904|||Fossiliferous units.||||||
305|Allingham Formation|65684|4|Described|p807-811|Pliocene|Pliocene|Of Nulla Basalt Province. Terrigenous clays, silt, sand, calcareous sand and Chara limestone. No older than 5.2 Ma; underlies basalt dated 3.60 +/- 0.07 Ma and 3.63 +/- 0.04 Ma. Contains Bluff Downs local fauna, whose age is now less tightly constrained.||||||
305|Allingham Formation|69599|5|Briefly described|p580, p594|Pliocene|Pliocene|Archer and Wade (1976). Small outcrop area along Allingham and Spring Creeks. Up to 18m thick. Contains a diverse and abundant vertebrate fossil assemblage (the Bluff Downs Local Fauna). Postdates the middle-late Miocene Featherby Surface.||||Is overlain by the Allensleigh Basalt.|Terrigenous clay, sand, silt, calcareous sand and algal limestone.|
305|Allingham Formation|69789|5|Briefly described|p1042, p1045, p1057|Pliocene|Pliocene|Adjacent to Basalt River and Allingham Creek. Exposed thickness of 18m. Minimum age from overlying basalt. Includes vertebrate fauna.|>3.6 Ma.|||Overlies Southern Cross Formation and overlain by Bluff Downs Flow..|Characterised by lacustrine carbonates including algal limestone; contains a rich vertebrate fauna.|19-JUN-20
305|Allingham Formation|70321|6|Mentioned|p162|Pliocene|Pliocene|Allingham Creek area, NE Queensland; appears in text as Allingham Creek Formation. Mentioned in connection with the age of a fossil of a rare kangaroo, also found at Riversleigh.||||||
305|Allingham Formation|73115|6|Mentioned|p25, p75|||Nulla Basalt Province. Represents sedimentation in sub-distal to distal zones.||||||
325|Almaden Supersuite|12575|6|Mentioned|p781. |Permian|Late Carboniferous|I-type granite. Western Hodgkinson Province.||||||
325|Almaden Supersuite|23076|4|Described|p724, 727|Early Permian|Stephanian|303-292 M yr||||||
325|Almaden Supersuite|23291|4|Described|p44, p96 Tb. 3.11|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||
325|Almaden Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Late Carboniferous|||||||
325|Almaden Supersuite|23423|4|Described|p314 Table 7.4|Early Permian|Late Carboniferous|Age: ~303 Ma, ~280 Ma (Rb-Sr). I-type. Also see p239.||||||
325|Almaden Supersuite|23430|5|Briefly described|p497|||||||||
325|Almaden Supersuite|23500|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
325|Almaden Supersuite|23501|6|Mentioned|map legend|Late Carboniferous|Late Carboniferous|||||||
325|Almaden Supersuite|23502|6|Mentioned|Map Legend||Late Carboniferous|An unnamed unit (Cgd) in the Gurrumba Ring Complex is included in this supersuite.||||||
325|Almaden Supersuite|23503|5|Briefly described|Map Legend||Late Carboniferous|||||||
325|Almaden Supersuite|23506|5|Briefly described|Map Legend||Late Carboniferous|||||||
325|Almaden Supersuite|23616|4|Described|Table 3 p50, p67|||I-type supersuite. Isotopic granites ~300 Ma.  Hodgkinson Province.||||||
325|Almaden Supersuite|23617|5|Briefly described|p55|||I-Type granite.||||||
325|Almaden Supersuite|23713|5|Briefly described|p17, p27||Carboniferous|Age: ~300-310 Ma.||||||
325|Almaden Supersuite|24485|5|Briefly described|p40, p50 Tb.8|Late Carboniferous|Late Carboniferous|||||||
325|Almaden Supersuite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
325|Almaden Supersuite|42681|5|Briefly described|p21|||||||||
325|Almaden Supersuite|43060|4|Described|p92|||||||||
325|Almaden Supersuite|43083|4|Described|p118-9|||Granites of suite are about 300 Ma. I-type. Predominantly medium-grained biotite-hornblende granodiorite and hornblende-biotite granodiorite.||||||17-JUN-09
325|Almaden Supersuite|43087|6|Mentioned|p18|||||||||
325|Almaden Supersuite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Includes the Almaden Suite and Almaden Granodiorite.||||||15-JUN-06
325|Almaden Supersuite|43254|5|Briefly described|map legend|Early Permian|Late Carboniferous|Age Late Carboniferous to Early Permian?||||||
325|Almaden Supersuite|43285|5|Briefly described|Map Legend|||age Late Carboniferous-Early Permian?||||||
325|Almaden Supersuite|43625|6|Mentioned|p34|||||||||
325|Almaden Supersuite|44246|6|Mentioned|Map Legend|Early Permian|Early Carboniferous|(Middle Carboniferous - Early Permian)||||||
325|Almaden Supersuite|60425|3|Fully described|p60 Tb. 4, p74-75, p280-3 Appdx.|Early Permian|Late Carboniferous|Includes 5 named suites ((21 named granites)+ 4 unassigned  named granites. Age: ~303Ma-280Ma (Rb-Sr). Detailed lithology for granodiorite, granite, tonalite, quartz monzodiorite, quartz monzonite, quartz diorite, leucogranite, aplite. I-types.||||||07-FEB-11
325|Almaden Supersuite|61784|5|Briefly described|p297|||Contains amphibole and more calcic plagioclase than its companion supersuites in the Mount Surprise-Herberton Group. Of the Mount Surprise-Herberton Group.||||||25-JAN-06
325|Almaden Supersuite|62371|5|Briefly described|p472 Fig.3|Carboniferous|Carboniferous|I-type granite.||||||
325|Almaden Supersuite|63140|6|Mentioned|p572 fig 3|Carboniferous|Carboniferous||||||I-type.|
325|Almaden Supersuite|63154|5|Briefly described|p281 Fig. 3, p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province. I-type granite.||||||11-APR-07
325|Almaden Supersuite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Diorites of this unit occur in the Gurrumba Ring Complex.|||||Includes grey, fine- to medium-grained quartz diorite.|
325|Almaden Supersuite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Diorites of this unit occur in the Gurrumba Ring Complex.|||||Includes grey, fine- to medium-grained quartz diorite.|
325|Almaden Supersuite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Almaden, Ruddygore, Muldiva and Hiker Granodiorites; Harpers Tonalite; Long Gully Granite; Retire Monzodiorite; and Pepper Diorite.|||
325|Almaden Supersuite|68553|6|Mentioned|Map legend|Permian|Carboniferous|This unit (in part), as well as the Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk. It is also mapped (in part), as CPgk, with Badu Suite and parts of the Ingham, Leichhardt, O'Briens Creek and Ootann Supersuites, and various ungrouped Carboniferous-Early Permian plutonic units. Finally, it is mapped (in part), as Pgk, with Brodies Camp, Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
325|Almaden Supersuite|68576|6|Mentioned|Q_11: p12, p14, p16|||Petford area.||||||
325|Almaden Supersuite|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|303.7 +/- 1.4 Ma (LA-ICPMS/TIMS zircon age).||||I-type granitoids.|
325|Almaden Supersuite|69593|3|Fully described|p484-486, p487 Fig.6.10, p491, p502-504|||See also p508-510. Western Hodgkinson Province. Crops out over ~400 km2. Contains over 25 named and unnamed plutons, in several Suites. Contains most of the more mafic units in the Province. Associated with Cu mineralisation. Geochemistry described. Several age determinations given and discussed.|c.306 Ma to c.280 Ma.||Almaden Suite; Ruddygore Granodiorite.|Is intruded by Ootann Supersuite.|Porphyritic to equigranular (pyroxene-) biotite-hornblende granodiorite, quartz diorite, and minor biotite-pyroxene-hornblende quartz monzodiorite; commonly magnetite-bearing; titanite also relatively common. I-type.|
332|Alsace Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
332|Alsace Quartzite|22585|6|Mentioned|Fig3 P738|||Actually written as Alsace Qtz. in text.||||||17-JUL-06
332|Alsace Quartzite|23031|5|Briefly described|24|||Geol. Province: Mount Isa Fold Belt. Of the Myally Subgroup.||||||09-SEP-14
332|Alsace Quartzite|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||17-JUL-06
332|Alsace Quartzite|23396|5|Briefly described|p407 Fig.2|||Of Myally Subgroup (Haslingden Group).||||||17-JUL-06
332|Alsace Quartzite|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup. Geological Province: Western Fold Belt.||||||01-OCT-08
332|Alsace Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group). Overlies Eastern Creek Volcanics;  underlies Bortala Formation.||||||01-OCT-08
332|Alsace Quartzite|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|33900|4|Described|p12|||||||||
332|Alsace Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|38232|6|Mentioned|p84|||||||||
332|Alsace Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|39445|5|Briefly described|Table 2|||See also p40||||||17-JUL-06
332|Alsace Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group). Fine to coarse feldspathic sandstone and orthoquartzite. Overlies the Eastern Creek Volcanics.||||||15-JUN-06
332|Alsace Quartzite|39622|6|Mentioned|Fig.2|||||||||
332|Alsace Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
332|Alsace Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|40221|3|Fully described|p8|||||||||
332|Alsace Quartzite|40623|5|Briefly described|p99|||||||||
332|Alsace Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
332|Alsace Quartzite|41307|4|Described|p10|||||||||
332|Alsace Quartzite|42523|5|Briefly described|Fig. 2 P373|||||||||
332|Alsace Quartzite|45136|5|Briefly described|p49|||||||||
332|Alsace Quartzite|45166|5|Briefly described|p14|||See also p71||||||17-JUL-06
332|Alsace Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
332|Alsace Quartzite|47083|4|Described|p7|||Oldest member of Myally Subgroup (Haslingden Group). O'lying unit Bortala Fm - conformable. U'lying unit Pickwick Metabasalt Member - conformable.||||||17-JUL-06
332|Alsace Quartzite|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
332|Alsace Quartzite|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
332|Alsace Quartzite|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup. ||||||
332|Alsace Quartzite|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
332|Alsace Quartzite|63023|5|Briefly described|p1025 Fig. 2, p1208|Paleoproterozoic|Paleoproterozoic|Basal unit of Myally Subgroup (Haslingden Group). Overlies eastern Creek Volcanics (Haslingden Group). Age: 1779+/-5Ma. Geological Province: Leichhardt Superbasin. See also p1027 Tb. 1.||||||09-SEP-14
332|Alsace Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Underlain by Eastern Creek Volcanics, overlain by Bortala Formation. Geological Province: Leichhardt Superbasin. Consists of sandstone.||||||
332|Alsace Quartzite|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Myally Subgroup. Overlain by Bortalla Formation, underlain by Eastern Creek Volcanics. Age: 1779+/-5Ma.  Geological Province: Leichhardt Superbasin. Consists mostly of conglomerate.||||||07-FEB-11
332|Alsace Quartzite|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Appears as Alsace Qtz in Fig.2.||Of the Haslingden Group||Overlies Eastern Creek Volcanics. Is overlain by Bortala Formation.||
332|Alsace Quartzite|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Eastern Creek Volcanics. Is overlain by Bortala Formation.||
332|Alsace Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
332|Alsace Quartzite|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Leichhardt superbasin. Material properties detailed.||||||
332|Alsace Quartzite|63866|5|Briefly described|p58|||Leichhardt Superbasin.||Myally Supersequence||||
332|Alsace Quartzite|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.||Myally Subgroup|||Conglomerate.|
332|Alsace Quartzite|65505|6|Mentioned|979|Proterozoic|Proterozoic|Contains detrital zircons aged 1780 Ma.||||||
332|Alsace Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mount Isa Inlier, Leichhardt Superbasin.|1779 +/- 5 Ma (maximum depositional age).|Myally Subgroup.|||Fine to coarse feldspathic sandstone and orthoquartzite, minor siltstone.|
332|Alsace Quartzite|68732|5|Briefly described|p160, p161, p165 Fig.3|Statherian|Statherian|Shoreline facies deposited above fair-weather wave base. Of the Myally Supersequence. Maximum sedimentary depositional age.|1779 +/- 5 Ma|Of the Haslingden Group.|||Fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|30-NOV-17
332|Alsace Quartzite|69222|6|Mentioned|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||
332|Alsace Quartzite|69591|4|Described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Also appears as Alsace Formation. Part of Myally Supersequence. Tide-dominated shelf deposits.|1779 +/- 5 Ma (MDA: Neumann et al., 2006).|Myally Subgroup.||Is overlain by Lochness Formation.|Fine to coarse feldspathic sandstone and orthoquartzite, minor siltstone.|
332|Alsace Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Is overlain by Bortala Formation.|Fine- to coarse-grained feldspathic sandstone and orthoquartzite; minor siltstone.|
332|Alsace Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Is overlain by Bortala Formation.|Fine- to coarse-grained feldspathic sandstone and orthoquartzite; minor siltstone.|
332|Alsace Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1779+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
332|Alsace Quartzite|71799|4|Described|p150 fig 2, p152|Statherian|Statherian|Lawn Hill. Deposited under fluviatile to lacustrine conditions. Ages are derived from Neumann et al, 2006 and also includes a tuff horizon dated at 1773 +/- 2 Ma (Neumann et al, 2006.|1779 +/- 5 Ma (max. dep. Age)|Myally Supergroup||Overlies the Pickwick Metabasalt (Eastern Creek Volcanics)|Quartzite, sandstone and greywacke.|03-OCT-18
332|Alsace Quartzite|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|Rythmic coarsening up coastal offlap sequences transitional upward into regressive coastal to inshore (lagoonal)deltaic and fan fringe facies.||Of Myally Subgroup||Transitional to overlying Bortala Formation.|Arkose, feldspathic sandstone, quartz arenite; some basalt.|
332|Alsace Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Eastern Creek Volcanics and underlies Bortala Formation.||
332|Alsace Quartzite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Eastern Creek Volcanics and underlies Bortala Formation.||
332|Alsace Quartzite|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
332|Alsace Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Eastern Creek Volcanics. Overlain by Bortala Formation.||
332|Alsace Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
344|Alum Rock Conglomerate|22601|2|Defined|405, 403-405, 407|Permian|Permian|||||||
344|Alum Rock Conglomerate|30914|6|Mentioned|Map legend|Permian|Devonian|Devonian ? - Permian||||||
344|Alum Rock Conglomerate|37252|6|Mentioned|Map legend|Permian|Permian|||||||
344|Alum Rock Conglomerate|38806|6|Mentioned|p72|||||||||
344|Alum Rock Conglomerate|39252|5|Briefly described|p16|||||||||
344|Alum Rock Conglomerate|39445|5|Briefly described|Table 7|||See also p90, p93, Fig.8 and Table 8. Earliest Permian.||||||12-DEC-07
344|Alum Rock Conglomerate|42559|6|Mentioned|p9|||Used by Lucas in 1958. Superseded informally by Alum Rock beds herein.||||||
344|Alum Rock Conglomerate|43008|5|Briefly described|map legend|||||||||
344|Alum Rock Conglomerate|43745|6|Mentioned|p16|Sakmarian|Sakmarian|(Early Sak.-Late Sak.)||||||
344|Alum Rock Conglomerate|44543|2|Defined|p29|||Overlies Thanes Creek Slate. Lower Permian fossils.||||||
344|Alum Rock Conglomerate|44565|2|Defined|p230-233|||||||||
344|Alum Rock Conglomerate|48940|6|Mentioned|p49|||Refers Lucas (1958)||||||
344|Alum Rock Conglomerate|61772|6|Mentioned|p128||Early Permian|In New England Orogen.||||||27-MAY-08
344|Alum Rock Conglomerate|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, locally pebbly arenite, and minor siltstone; rhyolitic to locally dacitic breccia, tuff and some lava with minor calcareous arenite and limestone.||||||
344|Alum Rock Conglomerate|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, locally pebbly sandstone, and siltstone; rhyolitic to locally dacitic breccia, tuff and lava; minor calcareous arenite and limestone; locally fossiliferous.||||||
344|Alum Rock Conglomerate|63748|4|Described|p17, p49, p68|Sakmarian|Asselian|Of Lucas (1958); forms narrow outlier within Texas beds. Age: 291.3+/-2.8Ma. Lower conglomerate, pebbly arenite, arenite + minor siltstone, and upper rhyolitic to locally dacitic breccia, tuff with some lava with minor calcareous arenite and limestone.||||||07-FEB-11
344|Alum Rock Conglomerate|64098|5|Briefly described|p337|||Includes volcanic rocks.||||||
344|Alum Rock Conglomerate|65107|6|Mentioned|p287|Permian|Permian|Permian inlier in the Texas beds.||||||
344|Alum Rock Conglomerate|65114|5|Briefly described|p383 Tb.1|Cisuralian||Listed as Early Permian; 294-291 Ma; Tectonic unit: Southern New England Orogen, Barnard Basin, slivers in Texas Block; SHRIMP zircon ages on rhyolite from this unit yielded ages of 293.7 +/- 3.4 and 291.3 +/- 2.8 Ma||||||21-SEP-09
344|Alum Rock Conglomerate|67908|6|Mentioned|p283|Permian.|Permian.|Texas Orocline. Early Permian. Appears in text as Alum Rock Formation.|||||Conglomerate layers and interbedded arenite, siltstone and volcaniclastic layers.|
344|Alum Rock Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Bondonga, Pikedale, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
344|Alum Rock Conglomerate|68679|4|Described|p452, p455|Permian|Permian|First mapped by Lucas (1958). Forms a narrow, 20km long NW-trending belt, 30km NW of Stanthorpe; Silver Spur Subprovince, Woolomin Province. Contains Asselian-Sakmarian brachiopods at base and top.|291.3 +/- 2.8 Ma (SHRIMP: Roberts et al., 1996).|||Unconformably overlies Texas beds.|Lower half is brownish bedded conglomerate (mainly pebbles from Texas beds), pebbly lithic to volcaniclastic sandstone and minor siltstone; upper half is rhyolitic to dacitic breccia, tuff and some lava with minor calcareous sandstone and limestone.|
344|Alum Rock Conglomerate|68901|6|Mentioned|p8 Fig.iii|Permian|Permian|||||||26-SEP-18
344|Alum Rock Conglomerate|73421|6|Mentioned|p17|Sakmarian|Asselian|New England Orogen, southern. U-Pb zircon SHRIMP ages of 293.7+/-2.8 Ma and 291.3+/-2.8 Ma U-Pb (Roberts et al., 1996) adjusted to approx. 296 Ma and 294 Ma due to use of the SL13 standard, supports late Asselian to earliest Sakmarian age.|Approx. 294 Ma and 296 Ma U-Pb zircon SHRIMP|||||
344|Alum Rock Conglomerate|73487|5|Briefly described|p563, p582 Fig.11, p574 Fig.8, p585-586|Cisuralian|Cisuralian|New England Orogen, eastern limb of Texas Orocline. Referred to as Alum Rock Conglomerate volcanics p585-586.|ca 293 Ma (Roberts et al., 1996)||||Includes volcanic rocks.|
349|Amamoor beds|22845|1|Redefined|p7,28,34,42-7,69,71,|Early Carboniferous|Late Devonian|Contains 3 mapping subunits.  Correlates to the Mount Clara beds and Booloumba. beds.||||||
349|Amamoor beds|22846|6|Mentioned|p20,2,37,44,54,6,68|Carboniferous|Devonian|Intruded by the Neurum and Mount Mucki Complexes.||||||
349|Amamoor beds|23251|5|Briefly described|Table 1 p16, p5|Carboniferous|Late Devonian|Fossil assemblage includes Radiolaria. Informally subdivided into 3 divisions. DCa2 has no known fossils, hence age is inferred by other 2 divisions. North D'Aguilar Subprovince, Wandilla Province.||||||30-NOV-05
349|Amamoor beds|23608|6|Mentioned|p54|||Possibly misspelt. Also see Amamoor Beds.||||||
349|Amamoor beds|23799|5|Briefly described|p17, p122|||Geological Province: North D'Aguilar Subprovince.||||||
349|Amamoor beds|38805|6|Mentioned|Fig.1|||||||||
349|Amamoor beds|39252|5|Briefly described|p16|||||||||
349|Amamoor beds|40051|4|Described|p5|||||||||
349|Amamoor beds|40623|5|Briefly described|p53|||||||||
349|Amamoor beds|41917|6|Mentioned|p521|||||||||
349|Amamoor beds|42450|4|Described| 403|||||||||
349|Amamoor beds|42619|5|Briefly described|p29|||||||||
349|Amamoor beds|42695|5|Briefly described|Fig.2|Carboniferous|Devonian|||||||
349|Amamoor beds|42751|4|Described|p22|||||||||
349|Amamoor beds|43006|4|Described|Table 1,p239|||||||||
349|Amamoor beds|43077|5|Briefly described|p4|||||||||
349|Amamoor beds|43092|5|Briefly described|p20|||||||||
349|Amamoor beds|43100|3|Fully described|p12|Early Carboniferous|Late Devonian|||||||
349|Amamoor beds|43588|6|Mentioned|p30||Late Devonian|||||||
349|Amamoor beds|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
349|Amamoor beds|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
349|Amamoor beds|44928|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
349|Amamoor beds|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
349|Amamoor beds|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince. Buff shale, slate, siltstone and minor chert; locally phyllitic.||||||
349|Amamoor beds|61780|5|Briefly described|p256|||Consists of shale, pebbly mudstone, greywacke and impure limestone as well as basaltic flows, banded cherts and jasper.||||||
349|Amamoor beds|65380|6|Mentioned|p671|||May have been source of chert and siliceous sandstone in Keefton Formation. ||||||
349|Amamoor beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
349|Amamoor beds|68679|4|Described|p312-313, p320-321, p325-329, p331-332|Carboniferous|Late Devonian|See also p369, p386-387. Murphy et al. (1976). Northern New England Orogen. Forms a NNW-trending belt up to 20km wide from near Maleny to N of Kilkivan. Includes some rocks previously assigned to the Gympie Group. Previously included rocks now assigned to the early Permian Cambroon beds. An upper plate, deep-water marine succession/accretionary assemblage exposed by Late Carboniferous extension. RELATED UNITS (continued): Is faulted over and against Widgee Metamorphics and Mount Mia Serpentinite, and against Wongella Metamorphics and Kandanga Creek Megabreccia. Is thrust under Manumbar Metamorphics and Marumba beds. Separated from Gympie Group by a zone of tectonic melange. Is intruded by Gallangowan, Tungi Creek and Kingaham Creek Granodiorites. Equivalent to Booloumba beds and possibly the Neranleigh-Fernvale beds.||||Is overlain unconformably by Neara Volcanics, North Arm Volcanic Group and Cambroon beds. Is intruded by Gallangowan, Tungi Creek and Kingaham Creek Granodiorites. See COMMENTS for more.|Chert and basalt intercalations: mudstone and slate, phyllite, chert, jasper, siltstone and intervening greenstone (lenses).|
349|Amamoor beds|72297|6|Mentioned|p728|||A minor source of slate; quarried at Imbil.||||||
401|Anakie Metamorphic Group|22543|6|Mentioned|p62||Cambrian|||||||
401|Anakie Metamorphic Group|22557|4|Described|p567-572||Ordovician|||||||
401|Anakie Metamorphic Group|22800|6|Mentioned|p579|||||||||
401|Anakie Metamorphic Group|22844|6|Mentioned|p37,39|Cambrian|Neoproterozoic|||||||
401|Anakie Metamorphic Group|22847|5|Briefly described|p 7||Neoproterozoic|||||||
401|Anakie Metamorphic Group|22857|6|Mentioned|p133, p415 App. 1 Tb. A1.5|||Age suggested is Early Cambrian and perhaps Neoproterozoic.||||||
401|Anakie Metamorphic Group|22858|6|Mentioned|p78|||||||||
401|Anakie Metamorphic Group|22933|6|Mentioned|p24||Neoproterozoic|||||||
401|Anakie Metamorphic Group|23006|5|Briefly described|p447 Fig.2|Early Cambrian|Proterozoic|||||||
401|Anakie Metamorphic Group|23052|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||
401|Anakie Metamorphic Group|23078|5|Briefly described|p707 (Fig 1)|Early Cambrian|Neoproterozoic|||||||
401|Anakie Metamorphic Group|23080|5|Briefly described|p696 (Fig 2)|||||||||
401|Anakie Metamorphic Group|23081|5|Briefly described|p692||Proterozoic|||||||
401|Anakie Metamorphic Group|23161|4|Described|p5,6,50|||||||||
401|Anakie Metamorphic Group|23245|6|Mentioned|p133-4|Early Cambrian|Neoproterozoic|||||||
401|Anakie Metamorphic Group|23422|5|Briefly described|p168|||||||||
401|Anakie Metamorphic Group|23423|5|Briefly described|p267|||||||||
401|Anakie Metamorphic Group|23430|5|Briefly described|p461|||K-Ar ~500 Ma. Anakie Province.||||||
401|Anakie Metamorphic Group|23854|5|Briefly described|p857|Neoproterozoic|Neoproterozoic|Geological Province: Anakie Inlier.||||||
401|Anakie Metamorphic Group|42747|4|Described|p28, p32, Fig.2|||Supersedes Anakie Metamorphics.||||||01-MAY-07
401|Anakie Metamorphic Group|43029|5|Briefly described|Fig.1,p13|||||||||
401|Anakie Metamorphic Group|43121|5|Briefly described|p1|||Proterozoic or Early Cambrian age.||||||
401|Anakie Metamorphic Group|43147|5|Briefly described|p50|||Deformation age approx. 510 Ma.||||||
401|Anakie Metamorphic Group|43213|3|Fully described|p8-11,p16-17, p19-53, p130-140, p183-184|||See also p202-203. Main component of Anakie Inlier. Raised to Group status in this study (Withnall et al., 1995). Previously Anakie Series and Clermont Series (Jensen, 1921), Clermont Slates (Reid, 1936), and Anakie Metamorphics (GSQ, 1953). See also Anakie Metamorphics (p9, p15, p20, p30). Original age is uncertain; the c.560 Ma age, if deformational, implies Neoproterozoic formation. Deformed and metamorphosed c.510 Ma (K-Ar), corresponding with the Delamerian Orogeny. Deformation structures detailed. Minor reef deposits of gold have been worked (eg Belyando, Lucky Break). May have been mistakenly mapped as Ukalunda beds north of the Mount Coolon 1:250 000 sheet area. Chemical analyses detailed.|561 +/- 7 Ma (K-Ar whole-rock).||Includes Bathampton, Wynyard and Hurleys Metamorphics; Rolfe Creek Schist; Monteagle Quartzite; Scurvy Creek Meta-arenite.|Is overlain by Silver Hills Volcanics.||
401|Anakie Metamorphic Group|43861|1|Redefined|24-27|Late Cambrian|Early Cambrian|Raised to group status. Age: 554Ma (K-Ar), 510Ma (K-Ar); depositional age is Early Cambrian/Neoproterozoic||||||24-JUL-08
401|Anakie Metamorphic Group|44093|6|Mentioned|p48 (footnote)|||Deformation and metamorphism occurred at around 500Ma (K/Ar dating, Withnall, Fergusson and Green, 1996).||||||
401|Anakie Metamorphic Group|44245|5|Briefly described|Map Legend||Neoproterozoic|||||||
401|Anakie Metamorphic Group|60425|5|Briefly described|p115|||Consist of metapelite and quartz-rich metapsammite.||||||07-FEB-11
401|Anakie Metamorphic Group|60659|5|Briefly described|p8-9|Early Cambrian|Neoproterozoic|Tightly folded sequence of quartz-mica schist, knotted schist, phyllite, quartzite slate, lithic sandstone and minor unfossiliferous limestone and volcanics. Unconformably overlain by Ukalunda beds. Geological Province: Anakie Province.||||||07-FEB-11
401|Anakie Metamorphic Group|60705|6|Mentioned|p659|||Geological Province: Anakie Inlier||||||
401|Anakie Metamorphic Group|61211|5|Briefly described|p261|Neoproterozoic||Geological Province: southern Anakie Inlier.||||||
401|Anakie Metamorphic Group|64665|6|Mentioned|p54. |||Basement to Blair Athol Basin.||||||
401|Anakie Metamorphic Group|64851|5|Briefly described|Map legend|Cambrian|Neoproterozoic|Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed; plus two unnamed subunits - detailed lithology included.||||||
401|Anakie Metamorphic Group|64852|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Comprises two subunits: a lower quartzite and sub-feldspathic meta-arenite interbedded with meta-siltstone grading into fine-grained mica schist.||||||10-FEB-09
401|Anakie Metamorphic Group|65388|6|Mentioned|p189|||Unconformably overlain by Blenheim Formation on western side of Bowen Basin.||||||
401|Anakie Metamorphic Group|66084|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed.||||||
401|Anakie Metamorphic Group|66085|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Includes Bathampton Metamorphics, Monteagle Quartzite and Scurvy Creek Meta-arenite. ||||||
401|Anakie Metamorphic Group|66851|5|Briefly described|p915-924||Neoproterozoic|Affected by three periods of deformation, D2 the most intense. Its significance lies in its being the only exposure of basement to Drummond, Adavale, Cooper, Galilee and Eromanga Basins.|||Includes Rolfe Creek Schist, Monteagle Quartzite and Wynyard Metamorphics.||Succession of psammitic-pelitic metasedimentary and mafic meta-igneous rocks that have been affected by greenschist to amphibolite facies low-pressure metamorphism.|18-JAN-17
401|Anakie Metamorphic Group|67455|4|Described|p573, p583, p589, p591.|||Anakie Inlier. Protolith sediments were deposited on the rifted East Gondwana continental margin. Equivalent rocks occur in Cape River and Argentine Metamorphics, Charters Towers Province. Underwent metamorphic cooling at 500 Ma. Has an inferred age and detrital zircon age signature similar to the Halls Reward Metamorphics.|||||Metasedimentary rocks and accompanying interlayered mafic igneous units.|
401|Anakie Metamorphic Group|67848|5|Briefly described|p16.|||Protolith was a passive-margin succession of Neoproterozoic-Cambrian age. Tectonic setting resembles Broken River Province.||||Is faulted against the Fork Lagoon beds.||
401|Anakie Metamorphic Group|68329|5|Briefly described|Map legend.|Cambrian|Neoproterozoic||||||Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed.|
401|Anakie Metamorphic Group|68404|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province. Minimum Early Cambrian age.|||||Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed.|17-JUN-13
401|Anakie Metamorphic Group|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.|||Includes Bathampton, Wynyard and Hurleys Metamorphics; Rolfe Creek Schist; Monteagle Quartzite; Scurvy Creek Meta-arenite.|||
401|Anakie Metamorphic Group|68482|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Anakie Province.|||Includes Wynyard Metamorphics, Monteagle Quartzite, Rolfe Creek Schist, and Bathampton Metamorphics.|||
401|Anakie Metamorphic Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Anakie Province.||||||
401|Anakie Metamorphic Group|68679|6|Mentioned|p309, p364|Paleozoic|Neoproterozoic|Thomson Orogen.||||||
401|Anakie Metamorphic Group|68731|5|Briefly described|p118-122, p125-129, pp132-134, p217|Early Cambrian|Neoproterozoic|Anakie Province. Withnall et al. (1995) divided into six units  with the aid of aeromagnetic and isotopic data, Landsat images and aerial photographs. Contains well-defined metamorphic zones. See also Anakie Metamorphics.|||Includes the Wynyard Metamorphics, Monteagle Quartzite, Rolfe Creek Schist, Bathampton Metamorphics, Scurvy Creek Meta-arenite, and Hurleys Metamorphics.|Unconformably overlain by the Theresa Creek Volcanics. Overlain by the Ukalunda Formation.|Comprises metasedimentary and meta-igneous rocks of greenschist to amphibolite metamorphic grade.|
401|Anakie Metamorphic Group|68823|6|Mentioned|p404|||Anakie Inlier. Poorly known depositional age. Rocks are multiply deformed.|||Includes the Bathampton Metamorphics.|Faulted against Fork Lagoons beds.||
401|Anakie Metamorphic Group|68900|3|Fully described|p1-p2, p4-p7, p9-p10, p18, p23, p49-p50|Cambrian|Neoproterozoic|Replaced the Anakie Metamorphics. Protoliths interpreted to be primarily siltstone to very fine-grained sandstone. Mineralogy is discussed.||||Overlain by the Ukalunda Formation. Faulted against the Les Jumelles beds.|Pale green, chloritic, phyllitic to schistose rocks.|
401|Anakie Metamorphic Group|68901|6|Mentioned|p2, p5|Early Paleozoic|Neoproterozoic|Thomson Orogen.||||||26-SEP-18
401|Anakie Metamorphic Group|69379|5|Briefly described|map legend||Neoproterozoic|Minimum age: Cambrian?|||||Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed|
401|Anakie Metamorphic Group|69541|5|Briefly described|p645 Fig.1(b), p653-655|Cambrian|Neoproterozoic|Of Anakie Inlier. Multiply deformed. Appears as Anakie Metamorphic Complex on p655.|||Includes Bathampton and Wynyard Metamorphics.||Quartzite and schists; bracketed below by schist, serpentinite, calc-silicate and marble, mafic schist, metagabbro and iron oxide; and above by psamnmopelitic schists.|
401|Anakie Metamorphic Group|69599|6|Mentioned|p635|||Peak Range district.||||||
401|Anakie Metamorphic Group|69952|5|Briefly described|p4, p108, p115, p120, p125|Middle Cambrian|Neoproterozoic|Age attributed by Fergusson et al. (2001) based on detrital zircon and monazite. Deformed and metamorphosed at ~510 Ma.|||Includes Wynyard Metamorphics.|Is faulted against Les Jumelles beds. Is overlain unconformably by Theresa Creek Volcanics.||
401|Anakie Metamorphic Group|70033|5|Briefly described|p4|||Thomson Orogen.|||Wynyard Metamorphics|||
401|Anakie Metamorphic Group|70125|6|Mentioned|p403, p408||||||Bathampton Metamorphics.|||
401|Anakie Metamorphic Group|70499|5|Briefly described|p5|||Geological province: Anakie Inlier, Thomson Orogen. Comprises metasedimentary rocks in the Anakie Inlier, and oldest known rocks in the Thomson Orogen. Metamorphosed to amphibolite facies; peak metamorphism likely occurred during late Cambrian to early Silurian, potentially during late stages of the Ross-Delamarian Orogeny and Benambran Orogeny (Withnall et al., 1995; Offler et al., 2011; Wood and Lister, 2013; Oorloff et al., in review). Youngest concordant detrital zircon U-Pb ages are 575-580 Ma. Detrital monazite SHRIMP 208Pb/232Th age populations of ~580 and 540 Ma (Fergusson et al., 2001). Intruded by Retreat Batholith. Protoliths of the Anakie Metamorphic Group were deposited in the late Proterozoic to early to mid-Cambrian.||||Intruded by Retreat Batholith.||
401|Anakie Metamorphic Group|70740|4|Described|i, ii, p1, p2, p9-p10, p12-p14, |Late Devonian||Drummond Basin, Anakie Inlier. Defined as basement in the Drummond Basin. Distribution, structure and boundary criteria are discussed. Lithology and petrography are described in detail. Exact age is uncertain, may be at least partly Cambrian (Fergusson et al., 2001). Also intruded by Percy Douglas Tonalite, Wirralie Granodiorite. See also p17, p18, p20, p23, p24, p33, p34, p80, p126, p127, p128, p130.||||Faulted against the Les Jumelles beds. Equivalent to the Scurvy Creek Meta-arenite. Unconformably overlain by the Ukalunda Formation. Intruded by the Manaman Granodiorite.|Metamorphosed siltstones and very fine-grained sandstones that are pale green, chloritic and phyllitic to schistose.|
401|Anakie Metamorphic Group|70744|5|Briefly described|p939, p944-945, p947|Cambrian|Cambrian|Anakie Province. K/Ar age by Withnall et al. (1996). Youngest detrital zircon c.510 Ma. Detrital zircon age distribution graph.|c.480-450 Ma (estimated from Fig.7).|||Is intruded by Gem Park Granite.|Metasedimentary rocks.|
401|Anakie Metamorphic Group|70749|5|Briefly described|p42-43, p49, p51, p53-54|Cambrian|Neoproterozoic|Anakie Province. The lower part of this unit is characterised by abundant 1300-900 Ma (late Mesoproterozoic = Grenvillian) aged detrital zircons, and maximum depositional age of ~580 Ma or older; zircons sourced from Musgrave Province. The upper part has abundant 650-500 Ma zircons with a subordinate 1300-900 Ma group, and a maximum depositional age of 511-495 Ma; zircons sourced from rift-related and back-arc volcanism of the active Gondwana margin.|c.580-c.500 Ma.||Bathampton, Wynyard, Hurleys Metamorphics; Monteagle Quartzite; Scurvy Creek Meta-arenite, Rolfe Creek Schist.|||
401|Anakie Metamorphic Group|70856|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic||||Includes Bathampton Metamorphics.||Siltstone, fine sandstone, phyllite, schist, commonly cleaved and multiply deformed.|
401|Anakie Metamorphic Group|71966|5|Briefly described|p989-990|Cambrian|Neoproterozoic|Geological province: Anakie Province, Thomson Orogen.|||Includes Bathampton Metamorphics.|||
401|Anakie Metamorphic Group|72297|6|Mentioned|p696|||Forms the basement for the Blair Athol Coal Measures in the Blair Athol and Wolfgang Basins.||||||
401|Anakie Metamorphic Group|73035|5|Briefly described|Map legend|Cambrian|Neoproterozoic|Some polygons of this unit are uncertainly identifed, and the age is poorly defined.|||||Siltstone, fine-grained sandstone, phyllite, schist,  greenstone; foliated and multiply deformed. Mica schist, quartzite and phyllite.  Fine-grained, phyllitic, sublabile to labile meta-arenite and meta-siltstone. Detrital muscovite common.|
401|Anakie Metamorphic Group|73163|6|Mentioned|p468|||Anakie Province. Described as latest Neoproterozoic to early Paleozoic. May be one of the sediment sources for Joe Joe Group, Betts Creek Group.||||||
401|Anakie Metamorphic Group|73425|6|Mentioned|p16|Cambrian|Cambrian|Anakie Province, northeast Thomson Orogen.||||||
471|Annmore Quartz Monzodiorite|42614|6|Mentioned|Table 2 P11|||Reserved as Annmore Granodiorite. Accidental variation?||||||
471|Annmore Quartz Monzodiorite|42747|5|Briefly described|Fig.9, P38|||see also Table 1 P37||||||
471|Annmore Quartz Monzodiorite|43029|2|Defined|p21||Late Devonian|K-Ar ages of 359 Ma and 362 Ma. See also Fig.2,p16||||||
471|Annmore Quartz Monzodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
471|Annmore Quartz Monzodiorite|43213|3|Fully described|p96, p108-109, p116-121, p174-175, p177|Late Devonian|Late Devonian|See also p208, p210, p212, p233, p241, p243. See also Annmore Granodiorite (p97). Type locality and geophysical properties described. Component of the Retreat Batholith. Numerous small plugs of Hoy Basalt intrude along the boundary with Kilmarnock Granodiorite. Geochemistry, modal analyses and geophysics detailed. Appears as Annmore Quartz Diorite on p243.|359 Ma & 362 Ma (K-Ar biotite: Webb et al., 1963)||||Grey to light grey, fine- to coarse-grained, equigranular to porphyritic, ranging from granodiorite to gabbro; gradual increase in mafic character from E to W. Contains metasedimentary xenoliths.|
471|Annmore Quartz Monzodiorite|69599|5|Briefly described|p593|Devonian|Devonian|||||Is overlain unconformably by Red Mountain Formation.||
513|Aquarium Formation|22538|6|Mentioned|Fig3 P709|||||||||
513|Aquarium Formation|22670|6|Mentioned|55|||Geol province McArthur Basin||||||
513|Aquarium Formation|22853|3|Fully described|10|Proterozoic|Proterozoic|Geol. province: McArthur Basin. Of the Tawallah Group. Max thickness 200 m. Overlies Wununmantyala Sandstone.||||||18-JUL-06
513|Aquarium Formation|23065|6|Mentioned|15|||Geol province: McArthur Basin. Of theTawallah Group. Overlying unit: Settlement Creek Volcanics, underlying unit: Sly Creek Sandstone||||||18-JUL-06
513|Aquarium Formation|23395|5|Briefly described|p388 Fig.4|||||||||
513|Aquarium Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
513|Aquarium Formation|23776|5|Briefly described|p705 Fig 2|||Of Tawallah Group.||||||
513|Aquarium Formation|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
513|Aquarium Formation|23963|5|Briefly described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group||||||03-MAR-05
513|Aquarium Formation|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
513|Aquarium Formation|24179|5|Briefly described|p84 Fig. 2|||Overlies the Wunnunmantyala Formation.  Overlain by the Settlement Creek Volcanics.  Geological Province:  McArthur Basin.||||||
513|Aquarium Formation|32660|5|Briefly described|Table 4|||||||||
513|Aquarium Formation|32904|6|Mentioned|p89|||||||||
513|Aquarium Formation|35114|6|Mentioned|p203|||||||||
513|Aquarium Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|36012|3|Fully described|Table 2|||||||||
513|Aquarium Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|37568|5|Briefly described|p78|||||||||
513|Aquarium Formation|38042|6|Mentioned|p160|||||||||
513|Aquarium Formation|38584|6|Mentioned|p14|||||||||
513|Aquarium Formation|39445|5|Briefly described|Table 2|||||||||
513|Aquarium Formation|40489|6|Mentioned|p89|||||||||
513|Aquarium Formation|40691|5|Briefly described|p9|||||||||
513|Aquarium Formation|41721|3|Fully described|p21|Proterozoic|Proterozoic|Of the Tawallah Group. Conformably overlies Sly Creek Sandstone; conformably overlain by Settlement Creek Volcanics. Thickness: 70m. Medium to coarse, moderately sorted, subangular to subrounded, galuconitic sandstone. Geological province: McArthur Basin.||||||01-AUG-07
513|Aquarium Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
513|Aquarium Formation|42385|3|Fully described|p10, p8 Fig. 5, p9 tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Tawallah Group. Max. thickness: 200m. Red, purple and grey dolostones, in places recrystallised; thinly bedded dololutite, silty dololutite and fine- to medium-grained dolarenite.||||||18-SEP-07
513|Aquarium Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
513|Aquarium Formation|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Of Tawallah Group.||In schematic section, underlies Wununmantyala Sandstone; overlies Rosie Creek Sandstone Member (Sly Creek Sandstone).|Dolostones, dololutite, dolarenite, shale, sandstone. Detailed lithology given.|07-NOV-11
513|Aquarium Formation|42639|4|Described|p10 Table 4 p11|||||||||
513|Aquarium Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
513|Aquarium Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Dolostone, mudstone, sandstone, dololutite, dolarenite, pebble breccia.||||||19-OCT-05
513|Aquarium Formation|42812|3|Fully described|p17, Table 3|||Of Tawallah Group||||||18-JUL-06
513|Aquarium Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||18-JUL-06
513|Aquarium Formation|43036|3|Fully described|p21|||Of Tawallah Group.||||||18-JUL-06
513|Aquarium Formation|44287|14|Not recorded|opp.p.7|||Equiv.of Rosie Creek Sandstone.||||||
513|Aquarium Formation|44305|14|Not recorded|p.6,12,21; opp 6,18|||(E53-8).||||||
513|Aquarium Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
513|Aquarium Formation|44436|5|Briefly described|p.8, opp. p.7, map|||(E53-4).||||||02-DEC-04
513|Aquarium Formation|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Micaceous galuconitic siltstone, fine-grained quartz sandstone, minor dolomite, dolomitic siltstone.  Conformably overlain by Settlement Creek Volcanics.||||||07-NOV-08
513|Aquarium Formation|44530|14|Not recorded|p.9|||(D53-15).||||||
513|Aquarium Formation|45162|2|Defined|p27|Proterozoic|Proterozoic|||||||
513|Aquarium Formation|45166|5|Briefly described|p28|||||||||
513|Aquarium Formation|46804|6|Mentioned|p154|||||||||
513|Aquarium Formation|48894|6|Mentioned|p21|||1473my - 1601my (dated on glauconite)||||||
513|Aquarium Formation|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin||||||
513|Aquarium Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Wununmantyala Sandstone, underlain by Sly Creek Sandstone.||||||
513|Aquarium Formation|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Overlain by Serrlement Creek Dolerite. Brown to green, dolomitic, glauconitic siltstone, shale and minor sandstone; locally hornfelsed.||||||07-NOV-08
513|Aquarium Formation|63112|6|Mentioned|p1192, p1206 ||||||||Lower fine-grained sandstone and upper dololutites and dolomitic mudstone with glauconite, halite and anhydrite pseudomorphs.|
513|Aquarium Formation|63866|5|Briefly described|p54|||||Prize Supersequence||||
513|Aquarium Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
513|Aquarium Formation|64817|6|Mentioned|p353 Fig.4,p355 Fig.5,p367 Tb.2,p369  |||||Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
513|Aquarium Formation|65228|5|Briefly described|p21, Figs.02, 05-08.|||Formerly incorrectly mapped as underlying the Wunnunmantyala Sandstone in the MOUNT YOUNG area. Written as "Aquarium Formation" in Figs. 05 and 07.||Unit in Tawallah Group.||Overlies Wununmantyala Sandstone. Is overlain by Settlement Creek Volcanics. Shown as equivalent to Wuraliwuntya Member.||
513|Aquarium Formation|65337|6|Mentioned|p49.|||Southern McArthur Basin. Has fine- to medium-grained sandstone with amalgamated low-angle trough and hummocky cross-stratification, similar to the Tobacco Member of Crow Formation.||||||
513|Aquarium Formation|65340|1|Redefined|pp12-17, pp92-93.|||Revised definition in this study. Upper 15 m has fine parallel-laminated red/brown (oxic) mudstone, massive to locally disrupted. Storm-dominated restricted marine shelf environment. Was in sedimentological continuum with the Wollogorang Formation prior to intrusion of Settlement Creek Dolerite. Hornfelsed and locally brecciated within 1 to 10 m of overlying Settlement Creek Dolerite. Correlated with Wuraliwuntya Member of Wununmantyala Sandstone; and tentatively with Bonanza Creek, lower McCaw, Dhunganda and Yuduyudu Formations in northern McArthur Basin.|c.1740 - 1730 Ma.|Unit in Tawallah Group.||Overlies Wununmantyala Sandstone. Is nonconformably overlain by a sill of Settlement Creek Dolerite.|Upward-fining unit of fine sandstone, maroon, thick-bedded, glauconite and gypsum pseudomorphs; and dolomitic mudstone, glauconitic, micaceous and ferruginous, with fine sandstone and  intervals of dololutite and dolarenite, halite pseudomorphs.|
513|Aquarium Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur region, Leichhardt Superbasin||Tawallah Group.|||Glauconitic sandstone, brown siltstone|
513|Aquarium Formation|67352|6|Mentioned|p15 tab 2|||||||Overlain by Settlement Creek Volcanics.||
513|Aquarium Formation|69430|4|Described|p15:3, 10-12|Statherian|Statherian|Outcrops in the Batten Fault Zone and SW McArthur Basin, previously included in this unit, are now assigned to the McDermott Formation (Rawlings, 1999). Over 200m thick. Shallow-marine storm-dominated shelf deposits, shallowing upward into marginal marine or lacustrine saline sediments.||Tawallah Group.||Conformably and gradationally overlies Sly Creek Sandstone. Gradational contact with Wununmantyala Sandstone. Is overlain by the intrusive Settlement Creek Dolerite.|Siltstone, shale and fine sandstone: dolomitic, galuconitic and ferruginous; local evaporites.|12-JUL-16
513|Aquarium Formation|69591|5|Briefly described|p39, p58|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession. Shallow subaqueous deposits.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|Glauconitic sandstone, brown siltstone.|
513|Aquarium Formation|69673|6|Mentioned|p16 fig 13, p17 fig 14, p24|||||Tawallah Group||Overlain by Settlement Creek Dolerite, overlies Wununmantyala Sandstone, correlated with Wuraliwuntya Member||
513|Aquarium Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Sly Creek Sandstone. Is overlain by Settlement Creek Volcanics.|Glauconitic sandstone, fine- to medium-grained; glauconite and dolomitic siltstone; dolomitic siltstone; dolomite.|
513|Aquarium Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Southeastern McArthur Basin.||Tawallah Group||Overlies and is partially equivalent to Wununmantyala Sandstone and underlies Settlement Creek Dolorite.||
513|Aquarium Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolerite. Equivalent to Wuraliwuntya Member.||
513|Aquarium Formation|72912|5|Briefly described|p5 Fig.3, p19.|Statherian|Statherian|Located in the Southeastern McArthur Basin.||Tawallah Group||Overlies and is equivalent to Wununmantyala Sandstone and underlies Settlement Creek Dolorite.||
513|Aquarium Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolorite.||
513|Aquarium Formation|73083|6|Mentioned|p78|||||||Underlain by Wunnunmantyala Sandstone.||
513|Aquarium Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Tawallah Group.||Overlies Wununmantyala Sandstone. Is overlain by Settlement Creek Dolerite.||
526|Aramac Coal Measures|13516|6|Mentioned|p147, fig 5|Late Permian|Early Permian|From Galilee Basin||||||
526|Aramac Coal Measures|23430|4|Described|p519 Table 14.6|||Maximum thickness <250 m.||||||
526|Aramac Coal Measures|30915|6|Mentioned|Table|||On Table for Stratigraphic drilling||||||
526|Aramac Coal Measures|30916|6|Mentioned|p99|||||||||
526|Aramac Coal Measures|31120|6|Mentioned|p149|||||||||
526|Aramac Coal Measures|31121|6|Mentioned|p385|||||||||
526|Aramac Coal Measures|31122|2|Defined|p350|Early Permian|Early Permian|||||||
526|Aramac Coal Measures|31258|4|Described|p101|||re  petroleum prospects.||||||
526|Aramac Coal Measures|31860|6|Mentioned|p277|||See also P282||||||
526|Aramac Coal Measures|33372|4|Described|p16|||See also p22. From Hexham 1 and Aramac 1 wells.||||||31-JUL-08
526|Aramac Coal Measures|35457|4|Described|p628|||Also Fig.4 biostratigraphic relationships.||||||
526|Aramac Coal Measures|35845|6|Mentioned|Fig.25|||||||||
526|Aramac Coal Measures|36243|6|Mentioned|Table 5A|||||||||
526|Aramac Coal Measures|36921|4|Described|p184|||See also Table 1.||||||
526|Aramac Coal Measures|37451|6|Mentioned|Table 2|||See also P401||||||
526|Aramac Coal Measures|37610|3|Fully described|p301|||See also Fig.3.||||||
526|Aramac Coal Measures|39252|6|Mentioned|p13|||||||||
526|Aramac Coal Measures|39261|6|Mentioned|Fig. 9|||||||||
526|Aramac Coal Measures|39264|6|Mentioned|Fig. 13|||||||||
526|Aramac Coal Measures|39265|6|Mentioned|Fig. 3|||||||||
526|Aramac Coal Measures|39445|5|Briefly described|Table 7|||See also p92.||||||31-JUL-08
526|Aramac Coal Measures|39478|6|Mentioned|Table 1|||||||||
526|Aramac Coal Measures|39943|6|Mentioned|Table 7A|||||||||
526|Aramac Coal Measures|40123|6|Mentioned|p465|||||||||
526|Aramac Coal Measures|41116|5|Briefly described|p432|||||||||
526|Aramac Coal Measures|41198|6|Mentioned|Table 1|||||||||
526|Aramac Coal Measures|41689|6|Mentioned|Table 1|||||||||
526|Aramac Coal Measures|42187|6|Mentioned|Fig.3 P318|||||||||
526|Aramac Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
526|Aramac Coal Measures|42446|3|Fully described|p8|Early Permian||Boundaries changed. Younger age determined. Age: late Early Permian||||||
526|Aramac Coal Measures|42447|6|Mentioned|Fig.3|||||||||
526|Aramac Coal Measures|42474|6|Mentioned|p25|||||||||
526|Aramac Coal Measures|42648|5|Briefly described|p41|||||||||
526|Aramac Coal Measures|42999|5|Briefly described|Table1,p90|||||||||
526|Aramac Coal Measures|43018|6|Mentioned|p390|||||||||
526|Aramac Coal Measures|43105|5|Briefly described|p13|||||||||
526|Aramac Coal Measures|43114|5|Briefly described|p7|||||||||
526|Aramac Coal Measures|43812|6|Mentioned|Fig.3,p145|||||||||
526|Aramac Coal Measures|46849|6|Mentioned|Fig. 7|||||||||
526|Aramac Coal Measures|63713|5|Briefly described|p1505, p1507 Fig.2, p1534-1535|Sakmarian|Sakmarian|NW Koburra Trough and Lovelle depression, Galilee Basin. Late Early Permian. Favourable source and reservoir rocks: petroleum system described.||||Overlies Joe Joe Group.||
526|Aramac Coal Measures|64288|5|Briefly described|p532 Fig.1 |Sakmarian|Sakmarian|||Unit in Joe Joe Group.||Overlies Jochmus Formation. Is overlain by Reids Dome Beds.||
526|Aramac Coal Measures|64665|5|Briefly described|p53 Fig.2, p54, p56.|Early Permian|Early Permian|Galilee Basin. Only present at uneconomic depths; no significant hydrocarbon generation.||||Overlies Joe Joe Group.||
526|Aramac Coal Measures|65489|5|Briefly described|p141-148|Sakmarian|Asselian|Lovelle Depression, Galilee Basin. Lean to excellent gas-prone source rock sequence.||||Overlies Jochmus Formation. Is overlain by Betts Creek Beds.||
526|Aramac Coal Measures|66188|6|Mentioned|443, Fig 3,17|Early Permian|Late Carboniferous|||||||
526|Aramac Coal Measures|67323|5|Briefly described|p81, p84, p88-89, p92, p93 Fig.12.3|Permian|Permian|Galilee Basin. Hydrocarbon source potential, particularly for coal seam gas; also has suitable reservoir rocks.||||Overlies Jochmus Formation. Is overlain unconformably by Betts Creek beds.|Includes siltstone and carbonaceous coaly material.|
526|Aramac Coal Measures|67402|5|Briefly described|p124 fig GLL1, p125 tbl GLL1|Artinskian|Artinskian|Galilee Basin. Deposited in peat swamps and braided streams. Has good porosity but poor permeability. Mistakenly referred to as the Aramac Formation on p274. See also p127 fig GLL5, p132, p135, p137, p138, p144.||||Overlies the Jochmus Formation. Unconformably overlain by the Betts Creek beds.|Interbedded quartzose to sub-labile sandstone, mudstone and coal.|
526|Aramac Coal Measures|68731|5|Briefly described|p198, p199, pp200-201 Fig 3.110|Cisuralian|Cisuralian|Comprises eroded remnants of the uppermost Joe Joe Group - probably confined to the Sakmarian. A facies variant of the upper part of the Jochmus Formation.||Of the Joe Joe Group.||Unconformably overlain by the Weston beds.||
526|Aramac Coal Measures|69582|6|Mentioned|p65-p66|Cisuralian|Cisuralian|Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Jochmus Formation. Overlain by the Clematis Sandstone and the Colinlea Sandstone.|Siltstone, coal.|
526|Aramac Coal Measures|71265|5|Briefly described|p589-590|Artinskian|Artinskian|Not widespread; local to the Lovelle Depression and Hulton-Rand Structure, Galilee Basin.||Joe Joe Group.||Overlies Jochmus Formation. Is overlain unconformably by Rodney Creek Sandstone.||
526|Aramac Coal Measures|71276|5|Briefly described|p283, p286, p289, p291|Cisuralian|Cisuralian|Galilee Basin.||Joe Joe Group.||||
526|Aramac Coal Measures|71701|4|Described|p153, p155-p159|Kungurian|Artinskian|Central Western Area, Galilee Basin. Ages are CA-IDTIMS dates derived from Nicoll et al, 2016a and 2016b. Palynology is discussed in some detail. See also p163, p165-p167, p169-p170.|282.72 +/- 0.07 Ma and 282.41 +/- 0.08 Ma|Joe Joe Group||Overlain by the Betts Creek Group and the Rodney Creek Sandstone. Overlies the Jochmus Formation.||
526|Aramac Coal Measures|71710|5|Briefly described|p368, p370, p380, p386|Early Permian|Early Permian|northern Galilee Basin. Localised mire formation in depressions in between intervening highs associated with uplift along western basin margin hinterland induced by Bowen Basin extension.||||Palynologically correlatable to Carmila beds and Reid Dome beds in the Bowen Basin. Unconformably overlain by Betts Creek beds. Underlain by upper Jochmus Formation.||
526|Aramac Coal Measures|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Galillee Basin.||||||
526|Aramac Coal Measures|72088|4|Described|p8, p16-p18, p46, p91|Kungurian|Sakmarian|Lovelle Depression, Galileee Basin. Deposited in a deltaic to paludal setting.||Joe Joe Group||Conformably overlies the Jochmus Formation. Unconformably overlain by the Betts Creek beds.|Sandstone, siltstone, shale, mudstone and minor coal.|
526|Aramac Coal Measures|72297|5|Briefly described|p697, p747, p751|Permian|Permian|Galilee Basin. Coeval with Reids Dome beds. High-volatile bituminous coal; too deeply buried for economic mining. Contains significant hydrocarbon source rocks. Exploration target for CSG.||||||
526|Aramac Coal Measures|73163|5|Briefly described|p467|Kungurian|Cisuralian|Galilee Basin. Dating is of tuff beds within the coal measures. Coal measures are restricted to the Lovelle Depression and the Hulton-Rand Structure. Upper contact with the J and K seams represents a depositional hiatus.|282.72 +/- 0.07 Ma, 282.41 +/- 0.08 Ma|Joe Joe Group||Overlies the Jochmus Formation. Underlies the 'J and K' seams.|Sandstone, siltstone, shale and coal. Includes tuff beds.|
526|Aramac Coal Measures|73472|6|Mentioned|p115|Sakmarian|Sakmarian|Galilee Basin.||Joe Joe Group||Underlain by Jochmus Formation.||
526|Aramac Coal Measures|73495|6|Mentioned|p505-506|Kungurian|Artinskian|Galilee Basin. Tuffs dated to 282.72 Ma and 242.84 Ma[?] via U-Pb CA-TIMS by Nicoll et al. (2016).|282.72 Ma, 242.84 Ma[?] U-Pb CA-TIMS|||||
539|Arbroath beds|13516|5|Briefly described|p145 fig 3, p147 fig 5|Early Permian|Early Permian|From Roma Shelf, Bowen Basin. Age: APP21 - APP22||||||
539|Arbroath beds|42250|6|Mentioned|Fig.3 P30|Early Permian||||||||
539|Arbroath beds|64856|4|Described|p42, p45-47|Sakmarian|Sakmarian|Bowen Basin. Informal name. Siliciclastics and minor coal. Unconformably overlies Timbury Hills Formation. Unconformably overlain by Moolayember Formation. Age from palynoflora (units APP21, 22). Correlated with Reids Dome beds. Max thickness > 1149m.| | ||||28-NOV-17
539|Arbroath beds|64857|6|Mentioned|p113 Fig.3|||Bowen Basin.||||||
539|Arbroath beds|64858|6|Mentioned|p180 Fig.2|Early Permian|Early Permian|||||||30-NOV-09
539|Arbroath beds|66615|6|Mentioned|p2 Fig.1, p8|||Southern Taroom Trough, Bowen Basin.||||||
539|Arbroath beds|68679|5|Briefly described|p378, p381|||Green et al. (1997). Roma Shelf, Bowen Basin. 1149m thick. Half-graben, coal swamp, then alluvial deposits. |||||Shale and siltstone with lesser sandstone and conglomerate and minor coal.|
542|Arcadia Formation|22973|5|Briefly described|p13 Fig.2 (i)|Early Triassic|Early Triassic|||||||
542|Arcadia Formation|23161|6|Mentioned|p33|Triassic|Late Permian|||||||
542|Arcadia Formation|24093|4|Described|p177|Early Triassic|Early Triassic|Of the Rewan Group. Age: >241Ma.  Geological Province: Bowen Basin.  See also p176 Fig. 2.||||||
542|Arcadia Formation|31305|6|Mentioned|p571|||||||||
542|Arcadia Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
542|Arcadia Formation|35873|6|Mentioned|Fig.9|||||||||
542|Arcadia Formation|36121|6|Mentioned|p25|||||||||
542|Arcadia Formation|37262|6|Mentioned|p285|||||||||
542|Arcadia Formation|37274|6|Mentioned|p273|||||||||
542|Arcadia Formation|37612|6|Mentioned|Fig.3|||See also P284||||||
542|Arcadia Formation|38312|4|Described|p463|||||||||
542|Arcadia Formation|38373|6|Mentioned|p614|||||||||
542|Arcadia Formation|38374|6|Mentioned|p602|||||||||
542|Arcadia Formation|38375|6|Mentioned|p545|||||||||
542|Arcadia Formation|38518|6|Mentioned|Fig.3|||||||||
542|Arcadia Formation|38713|6|Mentioned|p330|||Formerly named Rewan Formation.||||||
542|Arcadia Formation|38955|4|Described|p315|||||||||
542|Arcadia Formation|39059|6|Mentioned|p590|||||||||
542|Arcadia Formation|39212|4|Described|p14|||Excursion site. See also p35.||||||16-NOV-15
542|Arcadia Formation|39445|5|Briefly described|Table 9|||||||||
542|Arcadia Formation|39491|6|Mentioned|p24|||||||||
542|Arcadia Formation|39611|6|Mentioned|Fig.2|||||||||
542|Arcadia Formation|39943|6|Mentioned|Table 5A|||||||||
542|Arcadia Formation|40999|6|Mentioned|p298|||||||||
542|Arcadia Formation|41056|6|Mentioned|p22|||||||||
542|Arcadia Formation|41101|6|Mentioned|p294|||||||||
542|Arcadia Formation|41191|6|Mentioned|Fig.3|||||||||
542|Arcadia Formation|41481|6|Mentioned|p860|||||||||
542|Arcadia Formation|42004|6|Mentioned|p149|||||||||
542|Arcadia Formation|42254|6|Mentioned|Fig.2 P223|||||||||
542|Arcadia Formation|42257|5|Briefly described|Table 1 P263|||||||||
542|Arcadia Formation|42477|5|Briefly described|p132|||||||||
542|Arcadia Formation|42586|5|Briefly described|p103|||||||||
542|Arcadia Formation|42911|5|Briefly described|p11|||of Rewan Group||||||
542|Arcadia Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
542|Arcadia Formation|43000|5|Briefly described|Fig.5,p112|||||||||
542|Arcadia Formation|43185|5|Briefly described|11||Triassic|||||||
542|Arcadia Formation|43714|6|Mentioned|p19|||||||||
542|Arcadia Formation|45095|2|Defined|p25|Triassic|Triassic|See also p26.||||||16-NOV-15
542|Arcadia Formation|45110|6|Mentioned|Table 13|||||||||
542|Arcadia Formation|62921|5|Briefly described|p877-878, p881-884|Early Triassic|Early Triassic|Jensen (1975). Bowen Basin. Contains a diversity of stereospondyls (Tetrapoda, Temnospondyli). Other vertebrate fauna listed. Deposition from meandering and anastomosing river systems onto large, vegetated alluvial plains.||Unit in Rewan Group.||Conformably overlies Sagittarius Sandstone. Is overlain unconformably by Glenidal Formation.|Dominantly red-brown massive mudstones (thick sequences of overbank deposits), interbedded with lesser, well-defined channel sandstones.|
542|Arcadia Formation|64856|4|Described|p68-69|||Of Rewan Group. Overlies Saggitarius Sandstone. Not clear whether the top of this formation coincides with the top of the Rewan Group. Dominantly mudstone and silty mudstone interbedded with lesser siltstone and sandstone.| | ||||31-JAN-13
542|Arcadia Formation|64857|4|Described|p124-126|Triassic|Triassic|Thick mudstone intervals with lesser siltstone and sandstone beds, contained within the Rewan Group.||||||
542|Arcadia Formation|65115|5|Briefly described|p420, 421, Fig 14 p421|Early Triassic|Early Triassic|Red mudstone with siltstone and fine-grained sandstone. Of the Rewan Group. Overlies the Brumby Sandstone Member, Saggitarius Sandstone.||||||
542|Arcadia Formation|68576|5|Briefly described|Q_4: p16, p20|||Bowen Basin.||Rewan Group.||Overlies Sagittarius Sandstone.|Mainly red-brown mudstone and silty mudstone interbedded with lesser amounts of green siltstone and very fine- to medium-grained sandstone.|
542|Arcadia Formation|68679|5|Briefly described|p377, p383|Triassic|Triassic|Jensen (1975). Bowen Basin. 520-800m thick. Meandering fluvial deposits with widespread palaeosol.||||Overlies Sagittarius Sandstone.|Red-brown mudstone and silty mudstone interbedded with green siltstone and fine- to medium-grained sandstone.|
542|Arcadia Formation|68731|6|Mentioned|p200, p201|||Probably a facies variant of the Dunda beds.||||||
542|Arcadia Formation|71710|6|Mentioned|p386|||Deposited during rapid subsidence of Bowen Basin, coeval with development of Rewan Group.||||||
542|Arcadia Formation|73304|6|Mentioned|p76|||||||||
542|Arcadia Formation|73625|5|Briefly described|p22|Permian|Permian|Bowen Basin.||Rewan Group.||Overlies Bandanna Formation.|Red-bed facies with locally-abundant bones, teeth and tracks from various groups of amphibians and reptiles.|
545|Archerfield Basalt Member|29720|6|Mentioned|p79|||||||||
545|Archerfield Basalt Member|31132|6|Mentioned|p150|||||||||
545|Archerfield Basalt Member|44687|2|Defined|p225,226||Oligocene|Lower member of Corinda Formation. At base. Age: ?Oligocene.||||||21-MAR-13
545|Archerfield Basalt Member|44703|14|Not recorded|Map||Tertiary|||||||
545|Archerfield Basalt Member|44704|14|Not recorded|p1,4-7,10|||||||||
545|Archerfield Basalt Member|44708|14|Not recorded|Sheets 1,2||Tertiary|||||||
545|Archerfield Basalt Member|45087|5|Briefly described|p155|||See also p171. Chemical analyses.||||||04-AUG-08
545|Archerfield Basalt Member|69599|5|Briefly described|p595, p645|Eocene|Eocene|Oxley Basin. ~60m thick. Both age determinations by Green and Stevens (1975). Cohen (2007) made similar determinations.|56.3 +/- 1.4 Ma and 55.0 +/- 2.1 Ma.|Basal Corinda Formation.|||Basalt with sporadic intercalated mudstone.|
556|Ardmore Chert Member|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of Thorntonia Limestone. Regionally extensive layer of rubbly black to white banded and convoluted chert and chert breccia that is well developed in the Quita Creek area and crops out in ther Ardmore Outlier.  Geological Province:  Georgina Basin.||||||
556|Ardmore Chert Member|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
556|Ardmore Chert Member|39690|6|Mentioned|p90|||||||||
556|Ardmore Chert Member|40856|6|Mentioned|Fig.23.6|||||||||
556|Ardmore Chert Member|45079|6|Mentioned|p35|||Map legend p35. Middle Cambrian age||||||18-JUL-06
556|Ardmore Chert Member|47058|6|Mentioned|Table 1 P125|||||||||
556|Ardmore Chert Member|69591|5|Briefly described|p90|||A thin (3-5m) unit, interpreted as the remnant of a substantial evaporite succession.||Beetle Creek Formation.|||Rubble and breccia, chert having replaced the evaporite.|
574|Argentine Metamorphics|22533|6|Mentioned|p47||Proterozoic|||||||
574|Argentine Metamorphics|22557|5|Briefly described|p568,9|Early Palaeozoic|Proterozoic|||||||09-MAY-16
574|Argentine Metamorphics|22630|5|Briefly described|p 38|||||||||
574|Argentine Metamorphics|22844|6|Mentioned|p6,25,27,31,37 fig3|||||||||
574|Argentine Metamorphics|22847|5|Briefly described|p 7|||||||||
574|Argentine Metamorphics|23049|6|Mentioned|p6 Fig.3|||||||||
574|Argentine Metamorphics|23083|5|Briefly described|p681||Early Paleozoic|||||||07-NOV-08
574|Argentine Metamorphics|23422|4|Described|p168|Cambrian|Neoproterozoic|Can be divided into six informal units. Geological Province: Cape River Province.||||||
574|Argentine Metamorphics|23423|5|Briefly described|p267|||||||||
574|Argentine Metamorphics|23430|4|Described|p459, 461-462|||Contains significant amounts of iron. Cape River Province.||||||
574|Argentine Metamorphics|23431|5|Briefly described|p537|||Cape River Province.||||||
574|Argentine Metamorphics|23509|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|||||||
574|Argentine Metamorphics|23617|5|Briefly described|p7|||||||||
574|Argentine Metamorphics|23893|5|Briefly described|p10|||Geological Province: Cape River Province.||||||
574|Argentine Metamorphics|24424|6|Mentioned|p524|||Geological Province: Lolworth-Ravenswood Province.||||||
574|Argentine Metamorphics|24577|5|Briefly described|p752 Fig. 2|Cambrian|Proterozoic|Unconformably overlain by the Wilkie Gray Group. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
574|Argentine Metamorphics|24611|5|Briefly described|p193|Proterozoic|Proterozoic|See also p194 Fig. 1.||||||
574|Argentine Metamorphics|24612|5|Briefly described|p8, p9 Fig.2|||Overlain by Laroona Formation. Geological Province: Burdekin Basin.||||||23-APR-08
574|Argentine Metamorphics|24613|5|Briefly described|p5, p6 Fig. 3|Early Devonian|Precambrian|Unconformably underlies Laroona Formation (Fanning River Group) in northern part of the Burdekin Basin. Contains a core of migmatites.||||||07-FEB-11
574|Argentine Metamorphics|24614|6|Mentioned|p194 Fig. 3|||Overlain by Keelbottom Group at Star homestead area.||||||07-FEB-11
574|Argentine Metamorphics|30914|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician.||||||
574|Argentine Metamorphics|31285|5|Briefly described|p79|||See also p81. ? Precambrian.||||||23-APR-08
574|Argentine Metamorphics|31999|6|Mentioned|p127|||See also Table 11||||||
574|Argentine Metamorphics|32140|6|Mentioned|p7|||||||||
574|Argentine Metamorphics|32169|6|Mentioned|Table 2|||Precambrian||||||
574|Argentine Metamorphics|32553|4|Described|p54|||||||||
574|Argentine Metamorphics|33002|6|Mentioned|p413|||Plate tectonics||||||
574|Argentine Metamorphics|35154|6|Mentioned|Fig.3|||||||||
574|Argentine Metamorphics|36061|6|Mentioned|p30|||||||||
574|Argentine Metamorphics|36472|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
574|Argentine Metamorphics|37565|6|Mentioned|p4|||||||||
574|Argentine Metamorphics|37570|5|Briefly described|p123|||||||||
574|Argentine Metamorphics|37573|6|Mentioned|p208|||||||||
574|Argentine Metamorphics|37609|6|Mentioned|p307|||||||||
574|Argentine Metamorphics|39445|6|Mentioned|Fig. 6|||See P66,Table 4||||||
574|Argentine Metamorphics|39686|6|Mentioned|p69|||||||||
574|Argentine Metamorphics|39689|6|Mentioned|p49|||||||||
574|Argentine Metamorphics|39734|6|Mentioned|p21|||||||||
574|Argentine Metamorphics|39735|6|Mentioned|p16|||||||||
574|Argentine Metamorphics|40746|6|Mentioned|Fig.2|||||||||
574|Argentine Metamorphics|40787|5|Briefly described|p321|||||||||
574|Argentine Metamorphics|40961|6|Mentioned|p239|||||||||
574|Argentine Metamorphics|41125|5|Briefly described|p54|||||||||
574|Argentine Metamorphics|41668|5|Briefly described|p6|||Also Mention on p49 and Fig.2.2.||||||23-APR-08
574|Argentine Metamorphics|41735|6|Mentioned|p284|||||||||
574|Argentine Metamorphics|41774|6|Mentioned|p31|||||||||
574|Argentine Metamorphics|42295|6|Mentioned|Fig.2 P5|||||||||
574|Argentine Metamorphics|42407|3|Fully described|p2|||||||||
574|Argentine Metamorphics|42474|4|Described|p28|||||||||
574|Argentine Metamorphics|42689|5|Briefly described|map legend|Early Paleozoic|Proterozoic|||||||07-NOV-08
574|Argentine Metamorphics|42690|5|Briefly described|map legend|Early Paleozoic|Paleoproterozoic|Early to Middle Proterozoic and/or Early Palaeozoic||||||07-NOV-08
574|Argentine Metamorphics|42692|5|Briefly described|map legend|Proterozoic||||||||
574|Argentine Metamorphics|42747|6|Mentioned|p34|||||||||
574|Argentine Metamorphics|43093|5|Briefly described|p11||Proterozoic|see also Fig.1.||||||
574|Argentine Metamorphics|43095|5|Briefly described|Plate 2.|||||||||
574|Argentine Metamorphics|43103|5|Briefly described|p17, Fig.6.|||||||||
574|Argentine Metamorphics|43120|6|Mentioned|p365|||||||||
574|Argentine Metamorphics|43213|5|Briefly described|p8, p46, p51|||Lolworth-Ravenswood Province. Potential equivalent of Anakie Metamorphic Group farther south: similar lithologically and structurally.||||Possible correlative of Anakie Metamorphic Group.|Metapelites, quartz-rich metapsammites and amphibolites with tholeiitic and alkaline basalt affinities.|
574|Argentine Metamorphics|43480|6|Mentioned|49||Devonian|||||||
574|Argentine Metamorphics|43589|6|Mentioned|p25||Proterozoic|Intruded by Pall Mall Granite.||||||23-APR-08
574|Argentine Metamorphics|44058|14|Not recorded|p103|||||||||
574|Argentine Metamorphics|44060|14|Not recorded|Map Legend||Precambrian|||||||
574|Argentine Metamorphics|44061|4|Described|Table 1||Precambrian|||||||
574|Argentine Metamorphics|45151|6|Mentioned|p4|||||||||
574|Argentine Metamorphics|48904|2|Defined|p10|Early Paleozoic|Precambrian|Precambrian or early Palaeozoic.||||||13-MAY-15
574|Argentine Metamorphics|60425|5|Briefly described|p115|||Consist of metapelite and quartz-rich metapsammite.||||||07-FEB-11
574|Argentine Metamorphics|61211|5|Briefly described|p262|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
574|Argentine Metamorphics|62074|5|Briefly described|p1|Early Cambrian|Neoproterozoic|Basement in Lolworth-Ravenswood Block. Multiply deformed; underwent high T/low P metamorphism in early to middle Ordovician.||||||
574|Argentine Metamorphics|62075|6|Mentioned|p9 Fig.2|Early Cambrian|Neoproterozoic|||||||
574|Argentine Metamorphics|62522|6|Mentioned|p28|||Unconformably overlain by Stud Formation; also overlain by undifferentiated Dotswood Group rocks. Includes schists.||||||
574|Argentine Metamorphics|63154|5|Briefly described|p285 Fig. 5|Cambrian|Early Cambrian|Geological province: Charters Towers Province.||||||
574|Argentine Metamorphics|65380|6|Mentioned|p679, p677 Fig.9|||Greenvale Province||||||
574|Argentine Metamorphics|66529|5|Briefly described|p24 |Neoproterozoic|Neoproterozoic|Basement to Burdekin Basin.|||||Sediments and volcanics.|
574|Argentine Metamorphics|67455|6|Mentioned|p574 Fig.1, p583.|||Charters Towers Province.||||||
574|Argentine Metamorphics|67848|5|Briefly described|p16.|||Charters Towers Province. Inversion and folding occurred in the Silurian, correlating with younger phases of the Benambran Orogeny.||||||
574|Argentine Metamorphics|68350|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.|||Includes Brinagee Schist and Paynes Lagoon Amphibolite.||Serpentinite, schist, clinopyroxenite, quartzite, banded-iron-formation.|
574|Argentine Metamorphics|68351|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.|||Includes Brinagee Schist and Paynes Lagoon Amphibolite.||Serpentinite, schist, clinopyroxenite, quartzite, banded-iron-formation.|
574|Argentine Metamorphics|68419|5|Briefly described|Map Legend|Ordovician|Neoproterozoic|Of the Cape River Province. Minimum age shown as possibly Ordovician. Also includes 5 unnamed units at its base.|||Includes Paynes Lagoon Amphibolite and Brinagee Schist.|||
574|Argentine Metamorphics|68420|5|Briefly described|Map Legend|Paleozoic|Neoproterozoic|Of the Cape River Province. Minimum age shown as possibly Ordovician. Includes 5 unnamed units at its base.|||Includes Paynes Lagoon Amphibolite and Brinagee Schist.|||
574|Argentine Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Charters Towers Province. This unit, as well as Running River and Charters Towers Metamorphics, are all mapped under the symbol, -P-Cr.||||||
574|Argentine Metamorphics|68576|5|Briefly described|Q_11: p38, p40|||Camel Creek Subprovince. Probably late Neoproterozoic or Cambrian.|||||Grey, fine-grained quartzite; muscovite schist with a strong platy foliation and a weak lineation.|
574|Argentine Metamorphics|68731|5|Briefly described|p123, pp143-145, p183, pp216-221|Early Ordovician|Neoproterozoic|Northern Charters Towers Province. First named by Wyatt et al. (1970) and described by Withnall and McLennan (1991), Hutton et al. (1997) and Fergusson et al. (2007). Detrital zircon age of ~ 500 Ma, determined (Fergusson et al. 2001, 2007).|< 500 Ma|||Non-conformably overlain by the Laroona Formation.|Comprises psammitic gneiss and schist.|13-MAY-16
574|Argentine Metamorphics|68822|6|Mentioned|p320 Fig.3, p323|Cambrian|Cambrian|Rift volcanics. Charters Towers Province, Thompson Orogen.||||||
574|Argentine Metamorphics|69591|5|Briefly described|p80|||Charters Towers Province. Mentioned as the only other unit in northern Queensland (apart from Sefton Metamorphics) that contains significant ironstone.|||||Contains significant amounts of ironstone.|
574|Argentine Metamorphics|69952|6|Mentioned|p4|||Maximum depositional age.|c.500 Ma (Fergusson et al., 2001).|||||
574|Argentine Metamorphics|70033|5|Briefly described|p4|||Thomson Orogen. Maximum depositional age: mid- to late Cambrian.|~500 Ma, Fergusson et al. 2007|||||
574|Argentine Metamorphics|70125|5|Briefly described|p392, p394-395, p408|Late Cambrian|Ediacaran|Northern Queensland. Zircon ages discussed. Probability density plot of U-Pb ages of detrital zircons is compared with that of other units. This age of c.485 Ma is derived from detrital zircons (490 Ma) and a 480 Ma granite intrusion.|c.485 Ma (Fergusson et al., 2007).|||||
574|Argentine Metamorphics|70744|5|Briefly described|p939, p943-945, p947|Cambrian|Cambrian|Charters Towers Province. Age for a clast in upper part of the unit which has a prominent Pacific-Gondwana (600-510 Ma) signature. Lower part aged at < c.900 Ma contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga); age distribution graph. Intruded by Ravenswood Batholith plutons aged 510-460 Ma.|c.500 Ma (estimated from Fig.7).|||||
574|Argentine Metamorphics|70749|5|Briefly described|p42-44, p49, p51-52|Cambrian|Neoproterozoic|Charters Towers Province. The lower part of this unit is characterised by abundant 1300-900 Ma (late Mesoproterozoic = Grenvillian) aged detrital zircons, and maximum depositional age of ~580 Ma or older; zircons sourced from Musgrave Province. The upper part (lower grade) has abundant 650-500 Ma zircons with a subordinate 1300-900 Ma group, and a maximum depositional age of 511-495 Ma.|~1000-~495 Ma (maximum depositional age).|||||
574|Argentine Metamorphics|70838|6|Mentioned|p276|Ediacaran|Ediacaran|Charters Towers Province.||||||
574|Argentine Metamorphics|70839|5|Briefly described|p342-343|Late Neoproterozoic|Late Neoproterozoic|Geological province: Charters Towers Province. Age inferred by Fergusson et al., 2007.||||||
574|Argentine Metamorphics|73425|5|Briefly described|p2, 15-16, 18|Neoproterozoic|Neoproterozoic|Withnall and McLennan (1991). Charters Towers Province, northeast Thomson Orogen. Is intruded by granites aged ~480 Ma.||||||
574|Argentine Metamorphics|73600|6|Mentioned|p202|||||||||
585|Argylla Formation|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Tewinga Group. Quartzite, sandstone, siltstone, Rhyodacite, rhyolite, dacite, feldspar porphyry. Underlies Marraba Volcanics.||||||30-JAN-07
585|Argylla Formation|22461|5|Briefly described|Fig 1 p464|||Also see Fig 2 p466.||||||
585|Argylla Formation|22498|6|Mentioned|Fig6 P239|||||||||
585|Argylla Formation|22522|5|Briefly described|p330,Fig2p332,335|Statherian|Statherian|Max Age: 1780 Ma; Min Age: 1760 Ma||||||
585|Argylla Formation|22623|6|Mentioned|p225,6||Proterozoic|||||||
585|Argylla Formation|22722|6|Mentioned|p267||Statherian|||||||
585|Argylla Formation|22723|6|Mentioned|p262||Statherian|||||||
585|Argylla Formation|22734|5|Briefly described|p292||Statherian|Overlain by Corella Formation.||||||30-JAN-07
585|Argylla Formation|22747|6|Mentioned|p6||Precambrian|See also Table1,p7. Unconformably overlain by Eastern Creek Volcanics. 10 000? m thick. ?lower part of Soldiers Cap Formation.||||||
585|Argylla Formation|23054|6|Mentioned|p9|||||||||
585|Argylla Formation|23071|5|Briefly described|p760|||||||||
585|Argylla Formation|23079|6|Mentioned|p701||Mesoproterozoic|||||||
585|Argylla Formation|23182|6|Mentioned|p231||Proterozoic|||||||
585|Argylla Formation|23192|6|Mentioned|Fig.2|||||||||
585|Argylla Formation|23205|6|Mentioned|p43|||Age: 1777Ma. of Mt Isa Inlier.||||||
585|Argylla Formation|23324|6|Mentioned|p469|||Underlies the Corella Formation.||||||07-FEB-07
585|Argylla Formation|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1770+/-20Ma.||||||30-JAN-07
585|Argylla Formation|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1781+/-3Ma.||||||30-JAN-07
585|Argylla Formation|23395|6|Mentioned|p383|||||||||
585|Argylla Formation|23518|4|Described|p10|Proterozoic|Proterozoic|Of Tewinga Group.  Geological Province: Kalkadoon-Ewen Province.||||||
585|Argylla Formation|23962|5|Briefly described|p1214|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Age: 1780-1760Ma.||||||
585|Argylla Formation|24197|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Of the Argylla Suite. Age: 1780Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
585|Argylla Formation|24253|5|Briefly described|p5, p6 Fig.2, p10 Fig.4|Proterozoic|Proterozoic|Age: 1783 Ma. Geological Province: Mount Isa Block.||||||
585|Argylla Formation|24255|5|Briefly described|p32 Fig.1, p33 Fig.2|||Geological Province: Eastern Succession, Mount Isa Block. Age: felsic-int. volcanics, pelitic schist 1783 Ma.||||||
585|Argylla Formation|24256|6|Mentioned|p54|||Geological Province: Mount Isa Block.||||||
585|Argylla Formation|24257|5|Briefly described|p67|Paleoproterozoic|Paleoproterozoic|Age: 1783 Ma. Geological Province: Eastern fold belt, Mount Isa Block.||||||07-NOV-08
585|Argylla Formation|24259|5|Briefly described|p105|Proterozoic|Proterozoic|Age:~ 1783 Ma. Geological Province: Mount Isa Block.||||||
585|Argylla Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlain by Magna Lynn Volcanics. Mainly felsic volcanics. Geological Province: Eastern Fold Belt.||||||
585|Argylla Formation|29550|5|Briefly described|p44|||||||||
585|Argylla Formation|29969|5|Briefly described|p393|||||||||
585|Argylla Formation|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
585|Argylla Formation|30108|6|Mentioned|p390|||||||||
585|Argylla Formation|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
585|Argylla Formation|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Tewinga Group.||||||25-AUG-04
585|Argylla Formation|30530|6|Mentioned|p515|||||||||
585|Argylla Formation|30531|6|Mentioned|p15|||Also mention P20 and P22||||||
585|Argylla Formation|30532|6|Mentioned|p113|||||||||
585|Argylla Formation|30534|6|Mentioned|p300|||See also p305.||||||30-JAN-07
585|Argylla Formation|30536|6|Mentioned|p100|||Proterozoic.||||||
585|Argylla Formation|30723|5|Briefly described|p340|||||||||
585|Argylla Formation|30725|6|Mentioned|Fig.?|||||||||
585|Argylla Formation|31704|6|Mentioned|p4|||Copper mineralization||||||
585|Argylla Formation|32041|6|Mentioned|p352|||||||||
585|Argylla Formation|32660|5|Briefly described|Table 5|||||||||
585|Argylla Formation|32770|6|Mentioned|p44|||Geological plan||||||
585|Argylla Formation|32951|6|Mentioned|Table 1|||||||||
585|Argylla Formation|32959|6|Mentioned|Fig.21|||||||||
585|Argylla Formation|33214|6|Mentioned|p1279|||See also Fig.1||||||
585|Argylla Formation|33561|6|Mentioned|p102|||||||||
585|Argylla Formation|33897|6|Mentioned|p1280|||||||||
585|Argylla Formation|33900|6|Mentioned|p7,15|||||||||
585|Argylla Formation|34834|6|Mentioned|p215|||||||||
585|Argylla Formation|35074|4|Described|p213|||Mentioned on p206.||||||30-JAN-07
585|Argylla Formation|35167|6|Mentioned|p153|||||||||
585|Argylla Formation|35286|4|Described|p145|||||||||
585|Argylla Formation|35295|6|Mentioned|p601|||||||||
585|Argylla Formation|35932|6|Mentioned|p454|||||||||
585|Argylla Formation|35950|6|Mentioned|p304|||||||||
585|Argylla Formation|36052|4|Described|p419|||See also Fig.2.||||||
585|Argylla Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
585|Argylla Formation|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
585|Argylla Formation|36963|6|Mentioned|p241|||||||||
585|Argylla Formation|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
585|Argylla Formation|37462|4|Described|Table4.VII|||||||||
585|Argylla Formation|37565|6|Mentioned|p11|||||||||
585|Argylla Formation|37568|6|Mentioned|p84|||||||||
585|Argylla Formation|37569|6|Mentioned|p92|||||||||
585|Argylla Formation|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|37862|6|Mentioned|p581|||||||||
585|Argylla Formation|38232|6|Mentioned|p82|||||||||
585|Argylla Formation|38234|4|Described|p101|||||||||
585|Argylla Formation|38235|6|Mentioned|p115|||||||||
585|Argylla Formation|38238|6|Mentioned|p135|||||||||
585|Argylla Formation|38276|6|Mentioned|Fig.1|||||||||
585|Argylla Formation|38350|4|Described|p7|||||||||
585|Argylla Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
585|Argylla Formation|38560|6|Mentioned|p114|||||||||
585|Argylla Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
585|Argylla Formation|38827|6|Mentioned|p109|||||||||
585|Argylla Formation|38833|6|Mentioned|p161|||||||||
585|Argylla Formation|38834|6|Mentioned|p162|||||||||
585|Argylla Formation|38900|6|Mentioned|Fig.2|||||||||
585|Argylla Formation|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Tewinga Group.  Contains the Marraba Volcanics.||||||25-AUG-04
585|Argylla Formation|39049|6|Mentioned|p840|||||||||
585|Argylla Formation|39202|5|Briefly described|p229|||||||||
585|Argylla Formation|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
585|Argylla Formation|39445|5|Briefly described|Table 2|||See also p35 and p39.||||||30-JAN-07
585|Argylla Formation|39492|6|Mentioned|p30|||||||||
585|Argylla Formation|39496|4|Described|p5|||||||||
585|Argylla Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
585|Argylla Formation|39559|6|Mentioned|Table 1|||||||||
585|Argylla Formation|39622|6|Mentioned|Fig.2|||||||||
585|Argylla Formation|39798|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle ProterozoicE - M||||||07-NOV-08
585|Argylla Formation|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
585|Argylla Formation|39937|6|Mentioned|p79|||||||||
585|Argylla Formation|40623|5|Briefly described|p95|||||||||
585|Argylla Formation|40648|3|Fully described|p7|||||||||
585|Argylla Formation|40783|6|Mentioned|p1009|||||||||
585|Argylla Formation|40840|6|Mentioned|Map legend|||||||||
585|Argylla Formation|40984|6|Mentioned|p389|||||||||
585|Argylla Formation|41031|6|Mentioned|p796|||||||||
585|Argylla Formation|41069|6|Mentioned|p453|||||||||
585|Argylla Formation|41125|6|Mentioned|p45|||||||||
585|Argylla Formation|41150|5|Briefly described|Fig.1|||||||||
585|Argylla Formation|41306|4|Described|p5|||||||||
585|Argylla Formation|41307|4|Described|p8|||||||||
585|Argylla Formation|41381|6|Mentioned|p323|||||||||
585|Argylla Formation|41464|6|Mentioned|Map legend|Proterozoic||||||||
585|Argylla Formation|41465|5|Briefly described|p11|||||||||
585|Argylla Formation|41556|6|Mentioned|Map legend|Proterozoic||||||||
585|Argylla Formation|41568|5|Briefly described|p4|||||||||
585|Argylla Formation|41614|6|Mentioned|p145|||||||||
585|Argylla Formation|41744|6|Mentioned|p406|||See also P409||||||
585|Argylla Formation|41761|5|Briefly described|p284|||||||||
585|Argylla Formation|41791|5|Briefly described|p247|||||||||
585|Argylla Formation|41978|5|Briefly described|p497|||||||||
585|Argylla Formation|41979|6|Mentioned|p523|||||||||
585|Argylla Formation|42166|5|Briefly described|p108|||||||||
585|Argylla Formation|42201|6|Mentioned|p292|||||||||
585|Argylla Formation|42365|5|Briefly described|Fig.3 P258|||Also Fig 21||||||
585|Argylla Formation|42438|5|Briefly described|Fig.1 P276|||||||||
585|Argylla Formation|42565|4|Described|Table 1 P6, P2|||||||||
585|Argylla Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Contains the Mount Frosty Member. Porphyritic felsic volcanics, appreciably magnetic; sandstone.||||||09-FEB-09
585|Argylla Formation|42781|5|Briefly described|Fig.3 P428|||see also Fig.1 p426, Fig.4 p429.||||||30-JAN-07
585|Argylla Formation|42818|5|Briefly described|p212|||see also Fig.2 p205.||||||30-JAN-07
585|Argylla Formation|42858|5|Briefly described|p672|||||||||
585|Argylla Formation|42859|5|Briefly described|p675|||||||||
585|Argylla Formation|42879|6|Mentioned|p213|||||||||
585|Argylla Formation|43052|5|Briefly described|p62|||||||||
585|Argylla Formation|43608|6|Mentioned|Fig.11,p11|||||||||
585|Argylla Formation|43615|6|Mentioned|p15|||1725+/-3 Ma||||||
585|Argylla Formation|43616|6|Mentioned|p3|||Age: 1780-1800 Ma.||||||30-JAN-07
585|Argylla Formation|43643|5|Briefly described|p612|||||||||
585|Argylla Formation|43734|6|Mentioned|p14|||||||||
585|Argylla Formation|43928|6|Mentioned|23,24|||||||||
585|Argylla Formation|44091|14|Not recorded|p10||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44195|6|Mentioned|p347,351|||||||||
585|Argylla Formation|44210|14|Not recorded|Tb.1,p8|||||||||
585|Argylla Formation|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44271|2|Defined|p25-6,28,31,33,37-8,|||p44-5,50-1,56.||||||
585|Argylla Formation|44275|14|Not recorded|Map Legend|||||||||
585|Argylla Formation|44276|2|Defined|Tb.1,p9,10,13,17,map|||||||||
585|Argylla Formation|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44278|2|Defined|Tb.1,p5,map`|||||||||
585|Argylla Formation|44279|2|Defined|p4,5,7,Tb.1,map||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44290|14|Not recorded|p437|||||||||
585|Argylla Formation|44361|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44362|4|Described|Tb.1,p5||Neoproterozoic|||||||
585|Argylla Formation|44517|14|Not recorded|p234,235|||||||||
585|Argylla Formation|44521|14|Not recorded|p10,37,map|||||||||
585|Argylla Formation|44552|14|Not recorded|p12|||||||||
585|Argylla Formation|44749|14|Not recorded|p26|||||||||
585|Argylla Formation|44751|14|Not recorded|p299-301|||||||||
585|Argylla Formation|44755|14|Not recorded|p90||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44765|14|Not recorded|p14,15,17,18||Paleoproterozoic|||||||07-NOV-08
585|Argylla Formation|44788|14|Not recorded|p6|||||||||
585|Argylla Formation|44806|14|Not recorded|p280-284|||Petrographic descriptions.||||||
585|Argylla Formation|44812|14|Not recorded|p6|||Forms shallow stony loam reddish brown soil.||||||
585|Argylla Formation|44918|14|Not recorded|p77|||||||||
585|Argylla Formation|44919|14|Not recorded|p596, Fig.||Carpentarian|||||||
585|Argylla Formation|44989|2|Defined|p62|||Tb.11,111. (E54-14,F54-2,6,10). On many pages.||||||
585|Argylla Formation|45136|3|Fully described|p17|||||||||
585|Argylla Formation|45161|4|Described|p19|||See also Table 5||||||
585|Argylla Formation|45166|4|Described|p19|||||||||
585|Argylla Formation|45287|14|Not recorded|p223,225-9|||Overlies Leichhardt Metamorphics; Overlain by Marraba Volcanics & Ballara Quartzite.||||||18-JUL-13
585|Argylla Formation|46801|6|Mentioned|p117|||See also Fig. 14||||||
585|Argylla Formation|46843|6|Mentioned|Fig.2|||||||||
585|Argylla Formation|46859|6|Mentioned|p311,312|||||||||
585|Argylla Formation|46919|6|Mentioned|p221|||||||||
585|Argylla Formation|46960|6|Mentioned|p216|||||||||
585|Argylla Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
585|Argylla Formation|46995|5|Briefly described|p267|||||||||
585|Argylla Formation|46996|6|Mentioned|p273|||||||||
585|Argylla Formation|49009|6|Mentioned|p5|||See also P8.||||||
585|Argylla Formation|49041|6|Mentioned|p3|||Mention Table 4||||||
585|Argylla Formation|50100|4|Described|p11, 13 Fig. 4, p16-17|Statherian|Statherian|Felsic ignimbrites and lavas with some sed. rocks, high level felsic intrusives (Bowlers Hole and Mairindi Creek Granites), and basaltic lavas. Unconformably overlies Leichhardt Volcs; Conformably overlies Magna Lynn Metabasalt. Overlain by Stanbroke Sst||||||06-FEB-07
585|Argylla Formation|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
585|Argylla Formation|50332|5|Briefly described|p10-16, p17-18, p50, p67|Paleoproterozoic|Paleoproterozoic|Unconformably underlain by Leichhardt Volcanics. Conformably underlain by Magna Lynn Metabasalt in the Kalkadoon-Ewen Province and Wonga Subprovince.  Age: 1800-1755Ma. Lower part is intruded by Bowlers Hole Granite.||||||18-JUL-13
585|Argylla Formation|50536|5|Briefly described|p1.4, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.  Of the Argylla Suite. Age: ~1746-1777 +/- 21Ma (U-Pb). Intruded by Wonga Suite.||||||07-NOV-08
585|Argylla Formation|50605|6|Mentioned|p11.1|||Geological Province: Mount Isa Inlier.||||||
585|Argylla Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Tewinga Group. Porphyritic felsic metavolcanics, meta-arenite.||||||
585|Argylla Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block and Eastern Fold Belt.||||||03-JUN-09
585|Argylla Formation|60665|6|Mentioned|p1147 Fig.1, p1151 Fig.2. |Statherian|Statherian||1785 Ma.|||||
585|Argylla Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma.  Geological Province: eastern Mount Isa Block.||||||07-NOV-08
585|Argylla Formation|61735|5|Briefly described|p658|||Of the Haslingden Group. Geological province: Mount Isa Inlier.||||||30-JUN-09
585|Argylla Formation|61922|5|Briefly described|p8, p9 Fig. 3|||Unconformably overlain by Ballara Quartzite and Marraba Volcanics.  Age: 1783+/-5Ma, 1781+/-3Ma. Geological Province: Mount Isa Inlier/Eastern Fold Belt. See also p15-16 Figs. 7 and 8. ||||||
585|Argylla Formation|61925|5|Briefly described|p56 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Malbon Group.Comprises Felsic volcanic suite with interbedded sandstone and siltstone. Conformably overlain by Marraba Volcanics. Age: 1783+/-5Ma. Max. thickness: >2000m. Geol.Prov: Leichhardt Superbasin, Mount Isa Inlier. See also p57 Fig. 2||||||18-JUL-13
585|Argylla Formation|61926|5|Briefly described|p70-71|Paleoproterozoic|Paleoproterozoic|Undifferentiated mafic and felsic schist, porphyritic rhyolite, quartz arenite, feldspathic quartzite, pelitic schist. Age: 1783+/-5Ma. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
585|Argylla Formation|61929|5|Briefly described|p127, p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Sedimentary and felsic volcanic rocks. Overlain by Marraba Volcanics. Age: 1783+/-5Ma. Geological Province: Leichhardt Basin.||||||07-NOV-08
585|Argylla Formation|61936|5|Briefly described|p190 Fig. 3|||A felsic volcanics suite interbedded with sandstone and siltstone. Conformably overlain by Marraba Volcanics. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p195 Fig. 6. ||||||
585|Argylla Formation|62047|5|Briefly described|p90 Fig.1||||c.1770+/-20|||||
585|Argylla Formation|62536|6|Mentioned|p658|||Mount Isa Inlier.||Haslingden Group.||||
585|Argylla Formation|63055|5|Briefly described|p12 Fig. 1|||Part of Cover Sequence 2.||||||
585|Argylla Formation|63109|6|Mentioned|p1113|||Rough age of 1780Ma.||||||30-SEP-08
585|Argylla Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||3000 m thick.|Between c.1840 and 1800 Ma.||||Porphyritic felsic volcanics, minor basalt, sandstone.|
585|Argylla Formation|63866|5|Briefly described|p60-p62, p65|Statherian|Statherian|Mary Kathleen Belt, Mitakoodi Anticline. Magmatism in the Mitakoodi Anticline has crystallisation ages of c. 1760 Ma (Page, OZCHRON).|1780-1775 Ma (Page, 1978; Page, OZCHRON)|||Overlain by the Marraba Volcanics. Apparently coeval with the Myally Supersequence. Intruded by the Wonga Suite.||
585|Argylla Formation|64248|6|Mentioned|p38 Fig.5, p45|Statherian|Statherian|Younging eastwards. Appears as Argylla formation on p45.|1781 +/- 3 to 1761 +/- 4 Ma.|||||
585|Argylla Formation|64249|5|Briefly described|p83|Paleoproterozoic|Paleoproterozoic|Age range of deposition: 1762-1742Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
585|Argylla Formation|64250|5|Briefly described|p7-8, p11 fig 3, p21-24, p27|||Widespread unit, apparently younging eastward from Kalkadoon-Leichhardt Belt (1781+/-3 Ma), through Boomarra Horst/Mary Kathleen Fold Belt (1774+/-4 Ma), to Cloncurry Fold Belt (1761+/-4Ma).||Tewinga Group||Overlies Magna Lynn Metabasalt. Overlain by Marraba Volcanics, and unconformably by Ballara Quartzite.|Felsic volcanics; minor fluvial sandstone.|
585|Argylla Formation|64251|6|Mentioned|p51 Fig. 1|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
585|Argylla Formation|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1790-1720Ma. Geological Province: Mount Isa Block.||||||
585|Argylla Formation|64744|5|Briefly described|p353 Fig.4, p354, pp356-357.  |Statherian|Statherian|Mount Isa Basin. Felsic volcanics. Mylonitised blocks occur in 1740 Ma granites.|1780-1760 Ma.||||Pelitic metasediments and rhyolitic volcanics; weakly deformed.|
585|Argylla Formation|65376|5|Briefly described|p231.|||Geochemically similar to Myola Volcanics and felsic units of Tidnamurkuna Volcanics.|c.1790 Ma.|||||
585|Argylla Formation|65387|5|Briefly described|p1, p3 Tb.1, p59-64|Statherian|Statherian|Kalkadoon-Leichhardt Belt. Magmatic extrusive age from a sample in Mary Kathleen 1:100 000 Sheet area. Equivalent to part of the sequence in Boomarra Horst dated at 1776 +/- 8 Ma.|1780 +/- 5 Ma SHRIMP zircon (Carson et al. 2008).||||Includes foliated rhyodacite.|
585|Argylla Formation|65396|5|Briefly described|p7, p16-17, p77-78, p82, p84, p91, p169|Statherian|Statherian|See also p171, p175, p177, p182-183, p187, p190-196, p197, p201-202, p439. Leichhardt Superbasin. Eastern Succession, Cover Sequence 2. Kalkadoon-Leichhardt Belt - Mary Kathleen Zone - Eastern Fold Belt. Appears as Argylla Volcanics on p191. Other ages given. Formations with detrital zircons from this unit are listed. Detrital zircon sources listed. Hosts numeous Cu+/- Au occurrences.|1781 +/- 3 Ma - 1762 +/- 3 Ma|Tewinga Group||Overlies Magna Lynn Metabasalt. Is unconformably overlain by Ballara Quartzite, Corella Formation, Marraba Volcanics. Is correlated with Double Crossing Metamorphics.|Felsic volcanics, minor sandstone/quartzite and mafic volcanics.|
585|Argylla Formation|65505|5|Briefly described|966, 976-981, Fig 1-3,5,8-9|Proterozoic|Proterozoic|Age:1777-1780 +/-4 Ma (multiple ages). Felsic volcanics: quartz feldspar porphyry, rhyolite, dacite, quartzite and pelitic schist. Lineated to mylonitised. Underlies the Ballara Quartzite.||||||
585|Argylla Formation|65755|6|Mentioned|p3 Fig.1|||||||||
585|Argylla Formation|66302|6|Mentioned|p63|Statherian|Statherian|Has similar chemistry to the Tidnamurkuna and Myola Volcanics. |ca. 1790-1780 Ma (Wyborn et al, 1987)|||||
585|Argylla Formation|66913|5|Briefly described|p170 fig 1, p172||||1700-1725 Ma|||Overlain by Marraba Volcanics.|Interbedded felsic volcanic rocks, sandstone, and siltstone.|
585|Argylla Formation|67323|4|Described|15-17, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Erupted during extension of Leichhardt Superbasin. Camooweal - Murphy, Kalkadoon-Leichhardt Domains, Mount Isa Inlier. Basement to western Mary Kathleen Domain. Difficult to distinguish from Leichhardt Volcanics in the field. Similar age to lower part of Boomarra Metamorphics. Three other, similar, geochronology ages by the same workers are given.|1779 +/- 3 Ma (Neumann et al., 2009).|||Is overlain unconformably by Ballara Quartzite. Is intruded by Wonga Suite.|Porphyritic rhyolitic to dacitic tuff, andesite, quartz feldspar porphyry, quartzite, schist, gneiss; minor siltstone, arkose, conglomerate and metabasalt.|
585|Argylla Formation|67497|6|Mentioned|p909|||See also Argylla Volcanics p911 Fig. 20||Implied to be of the Argylla Suite|||Rhyolitic volcanics.|
585|Argylla Formation|67539|4|Described|p10, p11|Statherian|Statherian|SHRIMP geochronology determined by Rod Page & Chris Carson (this project). Includes a rhyolite ignimbrite <200m thick. Strongly magnetic.|~ 1780 Ma|||Overlain by the Ballara Quartzite.|Rhyolitic ignimbrite (< 200m)characterised by very large feldspar crystal fragments.|
585|Argylla Formation|68021|5|Briefly described|p135 fig 4, p135, p136, 137|Statherian|Statherian|Inferred to be age equivalent to Eastern Creek Volcanics, although compositionally different. Shown as Argylla Volcanics in Fig 5 p137.|1780-1760 Ma|||Age equivalent to lower part of Marraba Volcanics, lower part of Myally Supersequence.|Felsic volcanics. Intruded by dolerite dykes.|
585|Argylla Formation|68146|5|Briefly described|p1, p6, p69, p194, p211|||Mary Kathleen Domain. Exposed as rubbly discontinuous bouldery outcrops along a low ridgeline. Appears on existing geological maps as Leichhardt Volcanics, but has a strong magnetic signature characteristic of Argylla Formation. [This age determination dates it as c.80 m.y. younger than the Leichhardt Volcanics.] Whole-rock Sm-Nd isotopic data tabulated.|1782 +/- 5 Ma crystallisation/extrusion age.||||Well-bedded, flow-banded rhyolite to rhyodacite. A glassy, dark grey aphyric matrix hosts minor disseminated dark, magnetic grains (?magnetite) and small flecks of subhedral pink K-feldspar.|
585|Argylla Formation|68542|5|Briefly described|p12, p16 fig 4|||||||Unconformably overlain by Ballara Quartzite|Felsic volcanics, ignimbrites|
585|Argylla Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with Magna Lynn Metabasalt under the symbol, -Pva.||||||
585|Argylla Formation|68575|5|Briefly described|p1, p70, p75, p82, p84, p124|||Possible source of youngest detrital zircons in Staveley Formation samples in this study.|c.1770-1780 Ma (Neumann et al., 2009).||||Includes rhyolites which are characteristically strongly magnetic.|
585|Argylla Formation|68576|4|Described|Q-2: p12, p16, p20|||Felsic volcanics and sediments; part of a bimodal volcanic suite overlying the 1860 Ma Leichhardt/Kalkadoon basement. Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier. Contemporaneous with Magna Lynn Metabasalt. Appears also as Argylla Volcs.|1790-1780 Ma.|||Is overlain unconformably by Ballara Quartzite.|Largely subaerial ignimbrites, commonly pinkish and quartz-phyric; regionally magnetic.|
585|Argylla Formation|68732|5|Briefly described|p165|Statherian|Statherian|Of the Myally Supersequence. Igneous crystallisation ages; comparable with similar rocks of the Lalor Beds.|1754+-8, 1762+-3, 1761+-4, 1782+-3, 1781+-3 Ma||||Includes felsic volcanic rocks.|30-NOV-17
585|Argylla Formation|69056|4|Described|p2-5, p13, p18, p23, p28, p52-53|Statherian|Statherian|See also Time-Space plot sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Magna Lynn Metabasalt. Basal cover sequence layer within Constantine (formerly Canobie) and Mary Kathleen Domains. Modelling values listed. Several age determinations listed. Some areas previously mapped as this unit have been reassigned to the lithologically-similar Bulonga Volcanics.|~1795 Ma - ~1775 Ma.|||Overlies Leichhardt Volcanics. Coeval with and partly underlies the Boomarra Metamorphics. Is overlain by Ballara Quartzite and Bulonga Volcanics. Intruded by Burstall Suite.|Typically brick-red felsic porphyries and minor sediments.|
585|Argylla Formation|69222|5|Briefly described|p222 Fig.2, p223|Statherian|Statherian|Kalkadoon-Leichhardt Fold Belt. Associated with the Leichhardt Rift Event.|1783 +/- 5 Ma (Page and Sun, 1998).|||Overlies Magna Lynn Metabasalt, overlain by Ballara Quartzite||09-FEB-18
585|Argylla Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Overlies Magna Lynn Metabasalt.||25-JAN-19
585|Argylla Formation|69591|4|Described|p29, p33-34, p36, p58, p105|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin, Mount Isa Province. Part of Guide, ?Myally Supersequences. Subaerial, local fluvial environment. Eruption may have been synchronous with Eastern Creek Volcanics.|1778 +/- 3 Ma (Neumann et al., 2009).|||Overlies Magna Lynn Metabasalt. Is overlain unconformably by Ballara Quartzite.|Porphyritic rhyolitic to dacitic tuff, andesite, quartz-feldspar porphyry, quartzite, schist, gneiss; minor siltstone, arkose, conglomerate and metabasalt. Highly magnetic.|
585|Argylla Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Four facies are mapped separately: rhyolitic tuff and siltstone; quartzite, some feldspathic and micaceous sandstone and minor siltstone; intrusive, magnetic, coarsely feldspar-phyric rhyolite and microgranite; metabasalt.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Four facies are mapped separately: rhyolitic tuff and siltstone; quartzite, some feldspathic and micaceous sandstone and minor siltstone; intrusive, magnetic, coarsely feldspar-phyric rhyolite and microgranite; metabasalt.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two facies are mapped separately.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two facies are mapped separately.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two un-named sub-units are mapped separately: quartzite, some feldspathic and micaceous sandstone and minor siltstone; sheared felsic and mafic metavolcanics with abundant aplite and pegmatite veins.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes two unnamed members: sheared felsic, mafic metavolcanics; and quartzite with some feldspathic and micaceous sandstone.|||Includes two unnamed members||Porphyritic rhyolite to dacite (flows and ignimbrites), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzofeldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1754+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Volcanic rock.|
585|Argylla Formation|71799|5|Briefly described|p150 fig 2, p151 fig 3, p153 tbl 1, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block. SHRIMP age derived from Carson et al, 2009 and Neumann et al, 2009a.|1780 +/- 4 Ma (SHRIMP)||||Silicic volcanics, porphyry.|
585|Argylla Formation|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1783 +/- 5 Ma; 1775 +/- 4 Ma|||||
585|Argylla Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Age given as U-Pb zircon igneous crystallisation age.|1781 Ma to 1754 Ma|||Overlies and is partially equivalent to Magna Lynn Metabasalt and is shown to be underlying Quilalar Formation and Ballara Quartzite.||
585|Argylla Formation|72596|6|Mentioned|p1, p4, p18, p24, p46, p49, p54, p63|Statherian|Statherian|Geochronologic constraint by Carson  et al. (2009, 2011) and Neumann et al. (2009).|ca. 1780 Ma SHRIMP|||Felsic volcanics are comagmatic with Bowlers Hole Granite. Partly underlies the Corella Formation.|Includes felsic volcanics and associated high-level intrusives.|
585|Argylla Formation|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Comprised of 2 informal lithological divisions within unit.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Comprised of 2 informal lithological divisions within unit.|||||Porphyritic rhyolite to dacite (flows and volcaniclastic rocks including ignimbrite), quartzose to feldspathic sandstone and minor siltstone; grade into mica schist and quartzo-feldspathic gneiss; minor conglomerate and metabasalt.|
585|Argylla Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain, Mary Kathleen Domain and Kalkadoon-Leichhardt Domain. Includes a sericitic, feldspathic and quartzose meta-arenite conglomerate marker bed and 4 other informal sub-units.||||Shown as older than the Malbon Group, Mary Kathleen Group and Stanbroke Sandstone.|Porphyritic rhyolite to dacite, quartzose to feldspathic sandstone + minor siltstone; grade into mica schist and quartzo-feldspathic gneiss, schist, gneiss; minor conglomerate, metabasalt. Intrusive, coarsely feldspar-phyric rhyolite + microgranite.|
585|Argylla Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain, Mary Kathleen Domain and Kalkadoon-Leichhardt Domain. Includes a sericitic, feldspathic and quartzose meta-arenite conglomerate marker bed and 4 other informal sub-units.||||Shown as older than the Malbon Group, Mary Kathleen Group and Stanbroke Sandstone.|Porphyritic rhyolite to dacite, quartzose to feldspathic sandstone + minor siltstone; grade into mica schist and quartzo-feldspathic gneiss, schist, gneiss; minor conglomerate, metabasalt. Intrusive, coarsely feldspar-phyric rhyolite + microgranite.|
585|Argylla Formation|72799|6|Mentioned|p4|||||||||
585|Argylla Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
585|Argylla Formation|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Statherian|Part of Leichhardt Superbasin. Located in the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Age range shown. Source of data not indicated.|1781 Ma to 1754 Ma|Guide Supersequence||Shown as overlying and partially equivalent to Magna Lynn Metabasalt.|Includes felsic volcanics.|
585|Argylla Formation|73042|6|Mentioned|p4|Statherian|Statherian|Mount Isa Province, Leichhardt Superbasin. Geochronology is reportadly a U-Pb zircon igneous crystallisation age range.|1754 to 1781 Ma (see Fig.1.2)|||Underlain by and partly equivalent to Magna Lynn Metabasalt.||
585|Argylla Formation|73137|5|Briefly described|p1-2, 6, 11, 16, 21, 35, 47, 51, 65-66|Statherian|Statherian|Interpreted to pre-date Birds Well Granite [proper]. An unnamed biotite granite from the northern part of Coolullah Station is similar in age (1777 +/- 5 Ma, magmatic crystallisation age) to this unit (previous date of 1782+/-5 Ma) which adds to the growing evidence for a significant intrusive component to the magmatism associated with this formation. Previous U-Pb ages from volcanic rocks of ~1775-1782 Ma; thus, maximum age of the unit is >1770 Ma. Associated magmatic activity is distinct from that of the Wonga Igneous Subprovince. See also p 90, 95, 99.|1782+/-5 Ma U-Pb SHRIMP|Tewinga Group||Unconformably overlain by Mary Kathleen Group. Equivalent to Boomarra Metamorphics.|Includes igneous rocks.|11-OCT-22
585|Argylla Formation|73413|6|Mentioned|p1-3, p5-6, p21-22, App.1|Statherian|Orosirian|Mount Isa Inlier. Included in Cover Sequence 2 of Foster and Austin (2008). Deposited on top of Kalkadoon-Leichhardt basement. [Age written as 1770-1780 Ma and 1800-1775 Ma]. U-Pb SHRIMP age of 1782 +/- 5 Ma reported by Carson et al. (2011), 1778 +/- 3 Ma by Neumann et al. (2009), 1777 +/- 7 Ma and 1771 +/- 17 Ma by Page (1978), and 1768 +/- 5 Ma by Mcgee et al. (2010)[Magee et al. (2012)].|1770-1800 Ma|||Underlain by Magna Lynn Metabasalt. Overlain by Ballara Quartzite.|Includes felsic volcanics.|
585|Argylla Formation|73525|5|Briefly described|p4, p17, p19 Fig.13, p20|Statherian|Statherian|Kalkadoon-Leichhardt and Mary Kathleen Domains. See also Argylla Suite.|1781+/-3 Ma, 1780+/-4 Ma, 1777+/-3 Ma||||Felsic extrusives, includes siliciclastics and mafic extrusives.|
585|Argylla Formation|73529|4|Described|p2 Fig.1, p4, p6 Fig.3|Statherian|Statherian|Mary Kathleen Domain. Sedimentary intervals deposited in a subaerial environment.|1782+/-3 Ma (Neumann et al., 2009)|||Overlies Magna Lynn Metabasalt, underlies Ballara Quartzite|Felsic volcanic succession consisting of rhyolite and high upper crustal intrusive rocks alongside subordinate sedimentary intervals including feldspathic sandstone and quartzite.|
585|Argylla Formation|73553|4|Described|p1-3, p6, p8, p14, p18-29, p45-46,|Statherian|Statherian|Mary Kathleen Domain, western. Argylla Igneous Province. Unconformably overlies Kalkadoon-Leichhardt Domain. Intruded by granites of Wonga Igneous Subprovince, and metadolerite. First defined by Carter et al., (1961), boundary was revised and 6 subunits delineated by 1:100 000-scale mapping (eg. Derrick et al., 1977a; Wilson et al., 1977). Included in Tewinga Group of Derrick et al., (1977a). Further subdivision into 12 subunits by GSQ mapping (2018). Distinct bimodal magmatic event with Magna Lynn Metabasalt; base defined as the first felsic volcanic flow overlying Magna Lynn Metabasalt. Multiple U-Pb SHRIMP zircon crystallisation ages provided. Most areas are easily distinguished on geophysical images. Mostly A-type. Also intruded by Bowlers Hole, Wimberu, and Birds Well granites, Lakeview Dolerite. Interpreted to be intruded by Mount Maggie, Winston Churchill, Natalie, Playboy, Scheelite, and Wonga Granite. Probably equivalent to Boomarra Metamorphics. See also p63, p65-66, p70, p74, p78, p82-83, p90, p95-96, p98, p101, p144, p177, p180, p221, p224, p228, p246, p258, p263.|1778+/-3, 1782+/-5 Ma U-Pb zircon SHRIMP|Argylla Suite||Conformably overlies Magna Lynn Metabasalt with local interfingering, unconformably underlies Ballara Quartzite, Corella Formation, Mary Kathleen Group, intruded by Mairindi Creek Granite|Dominated by extrusive and high-level intrusive felsic igneous rocks and quartzose to feldspathic sandstones. Includes wide variety of lithologies. Coherent rhyolitic lava flows and rhyolitic ignimbrite are the most widespread.|03-FEB-23
618|Armraynald beds|23425|4|Described|p384, Table 9.7 p393.|||Geological Province Karumba Basin.||||||
618|Armraynald beds|38291|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
618|Armraynald beds|38348|5|Briefly described|p25|||||||||
618|Armraynald beds|39556|5|Briefly described|Map legend|Pleistocene|Pliocene|Pleistocene to Pliocene||||||
618|Armraynald beds|39562|5|Briefly described|Map legend|Pleistocene|Pliocene|Part of the Trans-Australian Platform Cover. Alluvial deoposits of clay and silt, minor sand and travertine; black clay soils.||||||15-JUN-06
618|Armraynald beds|41307|4|Described|p19|||||||||
618|Armraynald beds|42637|6|Mentioned|p32|||||||||
618|Armraynald beds|44922|5|Briefly described|Map legend|Pleistocene|Pliocene|Clay and silt, minor sand: older alluvial deposits.||||||01-JUL-04
618|Armraynald beds|47083|5|Briefly described|p20||Quaternary|Maximum thickness: 30 m.||||||
618|Armraynald beds|50600|5|Briefly described|Map legend|Pleistocene|Pliocene|Clay, silt, minor sand and travertine, black clay soils; older alluvial deposits.||||||
618|Armraynald beds|61155|5|Briefly described|p16|Pleistocene|Late Pliocene|Together with Claraville and Wondoola beds thickness is 70m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
618|Armraynald beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Pleistocene|Pliocene||||||Clay and silt, minor sand and travertine; black clay soils; older alluvial deposits.|
618|Armraynald beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit and the Wondoola beds are mapped under the symbol TQ: alluvium and lacustrine deposits.||||||
618|Armraynald beds|69591|6|Mentioned|p29|Quaternary|Neogene|||||||
618|Armraynald beds|69599|5|Briefly described|p585, p603|Pleistocene|Pliocene|Carpentaria region. Up to 25m thick.||||Correlated with Claraville and Wondoola beds.|Silt, clay, sandy clay and minor sand and gravel.|
618|Armraynald beds|72414|4|Described|map sheet|Quaternary|Neogene|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||||Clay and silt, minor sand and travertine; black clay soils; older alluvial deposits.|
618|Armraynald beds|72415|4|Described|mapsheet|Quaternary|Neogene|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||||Clay and silt, minor sand and travertine; black clay soils; older alluvial deposits.|
618|Armraynald beds|72421|4|Described|mapsheet|Quaternary|Neogene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||||Clay and silt, minor sand and travertine; black clay soils; older alluvial deposits|10-DEC-19
618|Armraynald beds|72422|4|Described|mapsheet|Pleistocene|Pliocene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Clay and silt, minor sand and travertine; black clay soils; older alluvial deposits|
618|Armraynald beds|72799|6|Mentioned|p27|||||||||
623|Arnolds Ridge Felsite|38095|6|Mentioned|Table 6|||Informal unit.||||||
623|Arnolds Ridge Felsite|38658|6|Mentioned|p153|||||||||
623|Arnolds Ridge Felsite|40180|6|Mentioned|Table 1|||||||||
623|Arnolds Ridge Felsite|40735|6|Mentioned|Fig.2|||||||||
623|Arnolds Ridge Felsite|61147|5|Briefly described|p378 Fig.3. |||||||Is overlain by Baree Felsite.|Felsite and lava|
632|Arrinthrunga Formation|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, minor dolomite and sandstone-grainstone, algal boundstone, mudstone.||||||
632|Arrinthrunga Formation|9394|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Georgina Basin. Brown massive dolomite, yellow flaggy dolomite, blue-purple oolitic limestone, thin beds of siltstone and sandstone. Underlies: Tomahawk beds. Overlies: Arthur Creek beds.||||||01-NOV-04
632|Arrinthrunga Formation|9694|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Underlies Tomahawk beds. Overlies Arthur Creek Formation. Includes: Eurowie Sandstone Member. Grey dolomite and limestone, rare thin beds of siltstone and sandstone. Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|12891|5|Briefly described|p733 Fig. 2|Middle Cambrian|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
632|Arrinthrunga Formation|12951|5|Briefly described|p143,  p145 fig 6, p148, 149|Late Cambrian|Late Cambrian|Georgina Basin.||||Said to be lateral equivalent of Chabalowe Formation p148. Overlies Arthur Creek Formation.|Mixed carbonates and siliciclastics.|
632|Arrinthrunga Formation|22524|6|Mentioned|p41|Cambrian|Cambrian|||||||
632|Arrinthrunga Formation|22954|6|Mentioned|Fig3p9|Idamean|Mindyallan|||||||
632|Arrinthrunga Formation|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|24066|6|Mentioned|p237|||Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|24442|5|Briefly described|p45|Late Cambrian|Late Cambrian|Unit includes calcimudstone, microbial laminite, peloid/intraclast and ooid grainstone, stromatolite boundstone and quartzic limestone and their dolomitised equivalents, together with minor quartz sandstone.||||||
632|Arrinthrunga Formation|31572|6|Mentioned|Fig.|||Correlation chart 1. U.Cambrian||||||
632|Arrinthrunga Formation|32469|6|Mentioned|p532|||||||||
632|Arrinthrunga Formation|33103|6|Mentioned|Table 4|||||||||
632|Arrinthrunga Formation|33111|6|Mentioned|p17|||||||||
632|Arrinthrunga Formation|33738|6|Mentioned|p480|||||||||
632|Arrinthrunga Formation|35005|5|Briefly described|p145|||||||||
632|Arrinthrunga Formation|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|35139|4|Described|Table.2|||||||||
632|Arrinthrunga Formation|36234|6|Mentioned|p175|||||||||
632|Arrinthrunga Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
632|Arrinthrunga Formation|37572|4|Described|p161|||See also Fig.8 and P165||||||
632|Arrinthrunga Formation|38532|4|Described|Fig.4|||||||||
632|Arrinthrunga Formation|39210|6|Mentioned|p54|||||||||
632|Arrinthrunga Formation|39921|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|40102|6|Mentioned|p164|||||||||
632|Arrinthrunga Formation|40136|6|Mentioned|p40|||||||||
632|Arrinthrunga Formation|40538|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Dolostone and limestone, micrite to grainstone, oolitic, stromatolitic, intraclastic: minor silt or quartz-arenite interbeds. Geological Province: Georgina Basin.||||||15-NOV-05
632|Arrinthrunga Formation|40810|5|Briefly described|p14|||||||||
632|Arrinthrunga Formation|40906|4|Described|p26|||||||||
632|Arrinthrunga Formation|41204|6|Mentioned|p13|||||||||
632|Arrinthrunga Formation|41385|6|Mentioned|Fig.4|||||||||
632|Arrinthrunga Formation|41388|6|Mentioned|p552|||||||||
632|Arrinthrunga Formation|41524|3|Fully described|p19|||||||||
632|Arrinthrunga Formation|41525|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Dolostone and and limestone, peloidal, oolitic, stromatolititc, micritic; thin siltstone, sandstone, shale interbeds.||||||26-OCT-05
632|Arrinthrunga Formation|42059|5|Briefly described|Fig.2 P131|||See also p134||||||18-JUL-06
632|Arrinthrunga Formation|42060|6|Mentioned|Fig.5 P140|||||||||
632|Arrinthrunga Formation|42477|5|Briefly described|p32|||||||||
632|Arrinthrunga Formation|42504|5|Briefly described|Table 54 P79|||||||||
632|Arrinthrunga Formation|42643|3|Fully described|p30|Late Cambrian|Middle Cambrian|||||||
632|Arrinthrunga Formation|42644|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Dolostone and minor limestone, peloidal, oolitic, stromatolitic, intraclastic, sandy, recessive; dolomitic sandstone. Geological Province: Georgina Basin.||||||15-NOV-05
632|Arrinthrunga Formation|42956|5|Briefly described|p31 Fig.4|||||||||
632|Arrinthrunga Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
632|Arrinthrunga Formation|43807|6|Mentioned|p352|||||||||
632|Arrinthrunga Formation|44233|14|Not recorded|p.60||Early Cambrian|Fig.1. Upper Cambrian.||||||
632|Arrinthrunga Formation|44320|14|Not recorded|p.8,9,12,13,14||Late Cambrian|U.Camb. Table 1.||||||
632|Arrinthrunga Formation|44321|14|Not recorded|map legend||Late Cambrian|(F53-7). U.Camb.||||||
632|Arrinthrunga Formation|44327|14|Not recorded|p.10|||See also pages 11,13,14,16,17 for more details. Map. (F53-11).||||||
632|Arrinthrunga Formation|44328|14|Not recorded|map legend||Late Cambrian|Upper Cambrian.||||||
632|Arrinthrunga Formation|44334|14|Not recorded|map legend||Late Cambrian|Upper Cambrian.||||||
632|Arrinthrunga Formation|44358|4|Described|p9,Tb.1||Late Cambrian|||||||
632|Arrinthrunga Formation|44457|14|Not recorded|p.6||Late Cambrian|U.Cambrian. Outcrops on Elkedra sheet. (F53-7).||||||
632|Arrinthrunga Formation|44469|2|Defined|p.8, opp.p.6, Tb.I|||(F53-12). See also p.13,15,16, Tb.2. O/lies conf. Marqua Beds. Algae. Aquifers.||||||
632|Arrinthrunga Formation|44470|5|Briefly described|map legend||Late Cambrian|Upper Cambrian.||||||02-DEC-04
632|Arrinthrunga Formation|44852|14|Not recorded|p69||Early Cambrian|||||||
632|Arrinthrunga Formation|44920|14|Not recorded|Map Legend, Sheet 4||Late Cambrian|||||||
632|Arrinthrunga Formation|45052|2|Defined|p104|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
632|Arrinthrunga Formation|45155|6|Mentioned|Fig.8|||||||||
632|Arrinthrunga Formation|46740|14|Not recorded|p.187||Middle Cambrian|U.Cambrian.||||||
632|Arrinthrunga Formation|46897|6|Mentioned|p352|||||||||
632|Arrinthrunga Formation|46958|6|Mentioned|Fig.2|||||||||
632|Arrinthrunga Formation|47024|6|Mentioned|Table 2|||||||||
632|Arrinthrunga Formation|47058|6|Mentioned|p134|||||||||
632|Arrinthrunga Formation|48844|2|Defined|p.35-6|||On many pages. p.2,16,17,21,25,35-6,38-9,46,47,49-50, F.26,58,62,63,66-69, Pl.4,8. New name. (F53-11).||||||
632|Arrinthrunga Formation|48901|14|Not recorded|Not recorded||Late Cambrian|F53-4,7,12. U.Cambrian.||||||
632|Arrinthrunga Formation|49027|4|Described|p11|||||||||
632|Arrinthrunga Formation|60122|3|Fully described|p19, p4-5|Late Cambrian|Late Cambrian|Includes Eurowie Sst Mbr. Dolostone, limestone, minor qtz sst., sltst, shale, marl, conglom. Conf.overlies Arthur Cr Fm/Steamboat Sst; underlies Ninmaroo/Tomahawk Fms.  Laterally interfingers with Georgina Lst. Max.thick:975m. Geol. Prov: Georgina Basin.||||||11-MAY-05
632|Arrinthrunga Formation|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 975m. Disconformably underlies: Tomahawk Formation, Ninmaroo Formation. Conformably overlies: Chabalowe Formation, Steamboat Sandstone, Arthur Creek Formation. Dolostone, Limestone.||||||28-APR-05
632|Arrinthrunga Formation|60551|5|Briefly described|Map Legend|Late Cambrian|Cambrian|Includes: Eurowie Sandstone Member. Underlies: Tomahawk Beds. Overlies: Arthur Creek Formation. Geological province: Georgina Basin.  Grey dolomite and limestone, rare thin beds of siltstone and sandstone.||||||
632|Arrinthrunga Formation|60590|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate.  Conformably overlies the Steamboat Sandstone; overlain by the Tomahawk Formation.||||||23-DEC-09
632|Arrinthrunga Formation|60675|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Overlies Chabalowe and Arthur Creek Formations. Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate.||||||11-JAN-05
632|Arrinthrunga Formation|61022|5|Briefly described|p15 Fig. 2|Late Cambrian|Late Cambrian|Contains the Eurowie Sandstone Member and the Hagen Member. 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.||||||16-JUN-05
632|Arrinthrunga Formation|61404|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Narpa Group. Includes the Eurowie Sandstone Member. Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate. Geological Province: southern Georgina Basin.||||||
632|Arrinthrunga Formation|62376|5|Briefly described|p53|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin||||||09-FEB-10
632|Arrinthrunga Formation|62595|6|Mentioned|p28 Fig.4.|Late Cambrian|Late Cambrian|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
632|Arrinthrunga Formation|62658|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Narpa Group. Dolostone and limestone with siliceous nodules and concretions; minor quartz sandstone, siltstone and shale.||||||
632|Arrinthrunga Formation|62759|5|Briefly described|p1|Late Cambrian|Late Cambrian|Includes the Hagen Member.||||||01-FEB-07
632|Arrinthrunga Formation|62789|5|Briefly described|p128, p129 Fig. 2|Late Cambrian|Late Cambrian|Southern Georgina Basin. Pacific Oil & Gas spudded their Baldwin No. 1 exploration well in this unit and intersected its base at 470.4 m.|||Includes Eurowie Sandstone Member.||Limestone, dolomite.|28-MAR-12
632|Arrinthrunga Formation|62790|5|Briefly described|p209, 210|Late Cambrian|Late Cambrian|Southern Georgina Basin. 470.4 m thick in Pacific Oil & Gas Baldwin No. 1 well.||||Overlies Arthur Creek Formation.|Limestones and dolomites.|28-MAR-12
632|Arrinthrunga Formation|63450|5|Briefly described|p78 Fig. 5, p80|Late Cambrian|Middle Cambrian|Overlies the Marqua Formation. Thickness: 601m. Geological province: Georgina Basin, West Toko Syncline. Comprises a mixture of grainstones, algal boundstones, sandy conglomerate and intraclastic limestones. See also p81.||||||07-FEB-11
632|Arrinthrunga Formation|63562|5|Briefly described|p338 fig 3, p345 fig 7, p347 fig 9.|Late Cambrian|Middle Cambrian|See also p348-349, p351, p352 fig 10, p355. Of Georgina Basin. Deposited in a peritidal and restricted shallow subtidal marine environment. Detrital zircons peak at c.1.85 Ga suggesting a sediment source in Arunta Inlier.||||Overlies Arthur Creek Formation. Correlated with Shannon Formation. Is overlain disconformably by Tomahawk Formation.|A thick, well-bedded dolostone and limestone unit with rare siliciclastic beds including calcarenite.|06-DEC-17
632|Arrinthrunga Formation|64068|3|Fully described|p20, pp65-71, p81, p89|Late Cambrian|Late Cambrian|Mapped as Ninmaroo Formation by Noakes et al (1959).  Hosts base metal mineralisation. Interdigitates with Georgina Limestone and Chabalowe Formation at base. Basal part correlated with Chabalowe Formation, Hagen Member, Selwyn Range Limestone.||Of Narpa Group.|Includes Eurowie Sandstone Member in middle.|Conformably overlies Steamboat Sandstone, Chabalowe Formation, or Arthur Creek Formation. Disconformably overlain by Tomahawk and Ninmaroo Formations.|Locally silicified and evaporitic limestone and dolostone; minor quartz sandstone, siltstone, shale. Contains stromatolites.|04-APR-12
632|Arrinthrunga Formation|64443|4|Described|p2, p5 Fig.3, p6 Tb.1, p9, p17-18, p40|Late Cambrian|Middle Cambrian|Of Smith (1964); formerly Meeta beds (Nichols and Fehr 1964). Disconformably underlies Tomahawk Formation and Ninmaroo Formation; laterally interdigitates with Georgina Limestone. Max 975m thick. Forms prominent isolated hills.||Of the Narpa Group.||Conformably overlies Camooweal Dolostone, Arthur Creek Formation, Steamboat Sandstone, Chabalowe Formation and possibly Wonarah Formation. See Comments.|Dolostone and limestone with minor quartz sandstone, siltstone, shale. Features includes stromatolites, thrombolites, nodular evaporites, gypsum crystals, fenestrae.|14-MAY-14
632|Arrinthrunga Formation|64778|6|Mentioned|p13, 30, 33|Cambrian|Cambrian|Toko Syncline, Southern Georgina Basin.||||||
632|Arrinthrunga Formation|64812|5|Briefly described|p237 Fig. 2, p251|Late Cambrian|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
632|Arrinthrunga Formation|64813|5|Briefly described|p256 Fig. 3|Late Cambrian|Late Cambrian|Overlies Chabalowe Formation. Geological Province: southern Georgina Basin. Carbonate and siliciclastic rocks.||||||11-FEB-09
632|Arrinthrunga Formation|65237|5|Briefly described|p3 Fig. 4, p9|Late Cambrian|Late Cambrian|Overlies Arthur Creek Formation. Max. thickness: 700m in the Dulcie Syncline. Geological province: southern Georgina Basin. Mixed carbonate and siliciclastic sediments.||||||07-FEB-11
632|Arrinthrunga Formation|65337|6|Mentioned|p68.|Late Cambrian|Late Cambrian|||||Overlies Camooweal Dolostone.||
632|Arrinthrunga Formation|65341|5|Briefly described|p2 Fig.2, p18.|Late Cambrian|Late Cambrian|||||Conformably overlies Chabalowe Formation. Is disconformably overlain by Tomahawk Formation.|Carbonate-dominated.|
632|Arrinthrunga Formation|65342|5|Briefly described|p7.|||Georgina Basin. Max. thickness at least 456 m.|||Includes Eurowie Sandstone Member.||Dolostone, limestone; minor quartz sandstone, siltstone, shale, marl and conglomerate.|
632|Arrinthrunga Formation|65489|6|Mentioned|p125-126|Ordovician|Cambrian|Georgina Basin.||||Is overlain unconformably by Ninmaroo Formation.||
632|Arrinthrunga Formation|66767|5|Briefly described|p59|Cambrian|Cambrian|Southern Georgina Basin.||Narpa Group.|Eurowie Sandstone Member.|Overlies Chabalowe Formation.|A thick succession of peritidal, evaporitic and stromatolitic limestone and dolostone, with minor quartz sandstone, siltstone and shale.|
632|Arrinthrunga Formation|67323|5|Briefly described|p83, p90, p92 Fig.12.2|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. An aquifer; supplies water bores.||||Unconformably overlies Marqua Formation. Is overlain unconformably by Ninmaroo Formation.||
632|Arrinthrunga Formation|67402|4|Described|p25 tbl RRM3, p213 fig GRG3|Iverian|Undillian|Georgina Basin, West Toko Syncline. Maximum thickness of 622m. Deposited in a very shallow and intermittently emergent sea. See also p215, p217 tbl GRG2. ||||Overlies the Georgina Limestone. Unconformably overlies the Thorntonia Limestone or Hay River Formation. Unconformably overlain by the Ninmaroo Formation.|Carbonate and carbonate siliciclastic sequence.|
632|Arrinthrunga Formation|67870|6|Mentioned|p43|Late Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||
632|Arrinthrunga Formation|69437|5|Briefly described|p22:10, 15|Cambrian|Cambrian|Southern Georgina Basin. May have potential as a petroleum source rock.||||Overlies Chabalowe Formation and Steamboat Sandstone. Is overlain by Tomahawk, Ninmaroo Formations.||12-JUL-16
632|Arrinthrunga Formation|69443|4|Described|p28:7, 16, 18-19, 21, 24, 26, 31, 35-36|Late Cambrian|Late Cambrian|See also 28:38, 40, 45, 47. K.G. Smith (1964). Southern Georgina Basin. Very thick unit, forming low rubbly exposures to substantial ridges. Up to 975m thick; generally over 300m. Wide variety of sedimentary structures; fossiliferous. Shallow subtidal to peritidal deposits on a restricted carbonate platform, with intermittent local emergence. Laterally interdigitates with Georgina Limestone. Associated with the Box Hole-Turkey Creek Pb-Zn prospect and abandoned mine. Hosts the Trackrider Pb prospect. Basal black shale has high TOC: is a viable petroleum source rock. Has had hydrocarbon shows in drilled wells. Is being explored for oil shale and tight gas.||Narpa Group.|Eurowie Sandstone Member.|Overlies Chabalowe or Arthur Creek Formations and Steamboat Sandstone gradationally, and Camooweal Dolostone (Barkly Group) conformably. Is overlain disconformably by Tomahawk and Ninmaroo Formations.|Locally silicified and evaporitic limestone and dolostone, minor quartz sandstone, siltstone and shale.|12-JUL-16
632|Arrinthrunga Formation|69561|6|Mentioned|p33 fig 2|Iverian|Mindyallan|||||Overlies Chabalowe Formation, Steamboat Sandstone||
632|Arrinthrunga Formation|69591|6|Mentioned|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||||Overlies ("apparently") the Camooweal Dolostone.||
632|Arrinthrunga Formation|69673|4|Described|p103, p117, p126, p127, p129, p135, p136|||975m thick. Includes fossils of stromatolites, brachiopods, hyoliths, molluscs, ichnofossils and rare trilobites.||||Correlated with Shannon Formation, Conformably overlies Chabalowe Formation, Steamboat Sandstone, disconformably overlain by Tomahawk Formation, Ninmaroo Formation|Locally silicified and evaporitic limestone and dolostone; minor sandstone, siltstone and shale. Microbial, peloid, ooid mudstones.|
632|Arrinthrunga Formation|70380|6|Mentioned|p745|Series 4|Series 3|Southern Georgina Basin.||||||
632|Arrinthrunga Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin. Oil show.||Narpa Group|Includes Eurowie Sandstone Member|Overlies Steamboat Sandstone or Chabalowe Formation.||
632|Arrinthrunga Formation|70951|6|Mentioned|p1080|||Geological province: Georgina Basin. High reflectance measured.||||||
632|Arrinthrunga Formation|71800|5|Briefly described|p26-p27|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Overlies the Arthur Creek Formation.|Calcarenite.|
632|Arrinthrunga Formation|72321|5|Briefly described|Fig 2, p6 fig 3|Jiangshanian|Guzhangian|Elkedra Shelf/Dulcie Syncline, Toko Syncline, Georgina Basin.  Base older in Toko Syncline than Dulcie Syncline. Australian stages: Mindyallan to Iverian.||of Narpa Group.||Overlies Arthur Creek Foramtion in Baldwin 1.||
632|Arrinthrunga Formation|72358|5|Briefly described|p117, p125|||Of Georgina Basin. Equivalent to Jay Creek Limestone in the Amadeus Basin. G. reticulatus Zone is recorded in petroleum well Netting Fence 1 (Green & Balfe, 1980).||||||10-JAN-20
632|Arrinthrunga Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Includes fossil stromatolites, trilobites, brachiopods, hyoliths, molluscs and ichnofossils.||Narpa Group|Eurowie Sandstone Member|Overlies the Steamboat Sandstone.|Evaporitic dolostone, limestone, medium-thick bedded; minor quartz sandstone, siltstone, shale.|05-JUL-22
632|Arrinthrunga Formation|72516|3|Fully described|p11-12, p92-94, p154|Furongian|Furongian|Georgina Basin. Occurs in eastern BARROW CREEK, ELKEDRA, HUCKITTA, TOBERMORY, SANDOVER RIVER, AVON DOWNS, HAY RIVER, MOUNT WHELAN, GLENORMISTON and URANDANGI map sheets. In the Jervois Range Special it outcrops on both sides of the Lucy Creek Fault Zone and forms low rubbly exposures to substantial ridges. Contains fossil stromatolites, trilobites, brachiopods, hyoliths, molluscs, ichnofossils which suggest a Furongian age. <100m thick in mapped area, 975m thick elsewhere. Deposited in a shallow subtidal to peritidal, restricted carbonate platform with intermittent local emergence. Age correlations are interpreted with the Chabalowe Formation, Georgina Limestone. Stratigraphically equivalent ot the Mungerebar Limestone, Selwyn Range Limestone, O'Hara Shale, Pomegranate Limestone of the Georgina Basin. Also equivalent to the Cleland Sandstone, Petermann Sandstone, Deception Siltstone, Jay Creek Limestone, Shannon Formation and Goyder Formation of the Amadeus Basin. Additionally correlated with the Brady Gneiss of the Irindina Province.|ca 825 Ma (U-Pb SHRIMP max dep age)|Narpa Group|Includes the Eurowie Sandstone Member.|Disconformably overlain by the Tomahawk Formation. Conformably and gradationally overlies the Steamboat Sandstone and Arthur Creek Formation.|Medium- to thick-bedded evaporitic dolostone and limestone; minor siliciclastic quartz sandstone, siltstone, shale.|14-APR-22
632|Arrinthrunga Formation|73083|6|Mentioned|p10, p42, p75|Cambrian|Cambrian|Previously the Meeta beds.||||Underlain by Camooweal Dolostone.|Includes dolostone, limestone, quartz sandstone, siltstone, and shale.|
632|Arrinthrunga Formation|73591|6|Mentioned|p40|||Georgina Basin.||||||
645|Arthur Creek Formation|9694|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Underlies: Arrinthrunga Formation. Overlies: Mount Baldwin Formation, Errarra Formation. Geological Province: Georgina Basin. Shale, limestone, sandstone.||||||
645|Arthur Creek Formation|12891|5|Briefly described|p733 Fig. 2|Middle Cambrian|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
645|Arthur Creek Formation|12951|4|Described|p144-148 149-157|Middle Cambrian|Middle Cambrian|Georgina Basin. Some old informal terminology abandoned, but new informal subdivisions introduced, based on electric log response and lithology.||||Unconformably overlies Thorntonia Limestone.|Basal anoxic hot shale passing upwards into paler dolomitic beds with some conglomerate to east. Then a pale carbonate interval with dolomudstone dominant and some oolite and laminated silty dolostone at top.|
645|Arthur Creek Formation|22954|6|Mentioned|Fig3p9|||||||||
645|Arthur Creek Formation|24442|5|Briefly described|p45|Middle Cambrian|Middle Cambrian|Overlain by Steamboat Sandstone.  On SANDOVER RIVER sheet.  ||||||
645|Arthur Creek Formation|40538|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Calcareous siltstone, fossiliferous, poorly exposed, limestone interbeds and quartz arenaceous limestone at top. Geological Province: Georgina Basin.||||||15-NOV-05
645|Arthur Creek Formation|40906|2|Defined|p57|Middle Cambrian|Middle Cambrian|||||||
645|Arthur Creek Formation|41018|6|Mentioned|p239|||||||||
645|Arthur Creek Formation|41021|6|Mentioned|p261|||||||||
645|Arthur Creek Formation|41129|6|Mentioned|p16|||||||||
645|Arthur Creek Formation|41204|6|Mentioned|p13|||Formerly Sandover beds||||||
645|Arthur Creek Formation|41524|3|Fully described|p16|||||||||
645|Arthur Creek Formation|41525|5|Briefly described|Map legend|Middle Cambrian||Siltstone, fossiliferous, pale yellow, part silicified in outcrop; grey black, calcareous, carbonaceous, phosphatic and pyritic at depth.||||||07-MAY-13
645|Arthur Creek Formation|42059|5|Briefly described|Fig.2|||See also P134||||||
645|Arthur Creek Formation|42070|6|Mentioned|p4|||||||||
645|Arthur Creek Formation|42504|6|Mentioned|p21|||||||||
645|Arthur Creek Formation|42643|6|Mentioned|p26|||Supersedes Sandover Beds||||||
645|Arthur Creek Formation|42956|5|Briefly described|p31 Fig.4|||||||||
645|Arthur Creek Formation|42994|6|Mentioned|p7|||||||||
645|Arthur Creek Formation|44133|5|Briefly described|p42|||Overlies Errarra Formation.||||||
645|Arthur Creek Formation|47035|6|Mentioned|Fig.1|||||||||
645|Arthur Creek Formation|47058|6|Mentioned|p138|||Variation of Arthur Creek Formation, NT.||||||
645|Arthur Creek Formation|60122|1|Redefined|p17, p56 Appendix|Middle Cambrian|Middle Cambrian|Formerly Arthur Creek beds. Now incorporates part of Sandover beds of ELKEDRA, Marqua Fm. and "Upper Hay River Formation Member2" of TOBERMORY. Disconformably overliesThorntonia Lst or Red Heart Dolostone; conformably underlies Steamboat Sst, Chabalowe Fm||||||26-OCT-05
645|Arthur Creek Formation|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 457m. Conformably underlies Arrinthrunga Formation, Chabalowe Formation, Hagen Member, Steamboat Sandstone. Disconformably overlies Thorntonia Limestone. Dolostone.||||||26-OCT-05
645|Arthur Creek Formation|60551|5|Briefly described|Map Legend|Cambrian|Cambrian|Underlies: Arrinthrunga Formation. Overlies: Errarra Formation, Mount Baldwin Formation. Geological province: Georgina Basin.  Buff shale, laminated limestone, sandstone, dolomite.||||||
645|Arthur Creek Formation|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Dolostone, limestone (upper); foetid pyritic-carbonaceous black shale, laminated dolostone (lower part).  Overlies the Thorntonia Limestone; conformably overlain by Steamboat Sandstone.||||||25-NOV-04
645|Arthur Creek Formation|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies Chabalowe and Arrinthrunga Formations; overlies Thorntonia Limestone. Upper: dolostone, limestone. Lower: foetid pyritic- carbonaceous black shale, laminated dolostone.||||||12-JAN-05
645|Arthur Creek Formation|60684|6|Mentioned|p14|||||||||
645|Arthur Creek Formation|61022|5|Briefly described|p14, p15 Fig. 2|Middle Cambrian|Middle Cambrian|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
645|Arthur Creek Formation|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems. Geological Province: Georgina Basin.||||||
645|Arthur Creek Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Narpa Group. Divided into: upper dolostone, limestone; lower foetid pyritic-carbonaceous black shale, laminated dolostone. Geological Province: southern Georgina Basin.||||||
645|Arthur Creek Formation|61732|5|Briefly described|p113|Middle Cambrian|Middle Cambrian|Overlies Elkera Formation Huckitta 7 drillhole.  Geological Province: Georgina Basin.||||||07-FEB-11
645|Arthur Creek Formation|62376|5|Briefly described|p53|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin||||||09-FEB-10
645|Arthur Creek Formation|62759|5|Briefly described|p1|Middle Cambrian|Middle Cambrian|Overlain by Steamboat Sandstone. Geological Province: Georgina Basin. Includes shoals and sandy debris flows; contains extremely rich oil-prone microbial source rocks.||||||05-FEB-08
645|Arthur Creek Formation|62789|5|Briefly described|p128, p129 Fig. 2, p132|Middle Cambrian|Middle Cambrian|Fossiliferous mudstone, siltstone, limestone, minor sandstone. Contains diverse trilobite assemblage. In southern Georgina Basin, overlies early Middle Cambrian Thorntonia Limestone and underlies Upper Cambrian Chabalowe Formation.||||Overlies early Middle Cambrian Thorntonia Limestone and underlies Upper Cambrian Chabalowe Formation.|Fossiliferous mudstone, siltstone, limestone, minor sandstone.|28-MAR-12
645|Arthur Creek Formation|62790|4|Described|p206, 208, p210, p219, p220|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains a small bradoriid and phosphatocopid fauna.||||Underlies Arrinthrunga Formation and overlies Thorntonia Limestone.|Fossiliferous mudstone, siltstone, limestone, minor sandstone.|28-MAR-12
645|Arthur Creek Formation|62983|5|Briefly described|p11|Cambrian|Cambrian|Referred to informally as the lower Arthur Creek Formation. Extensive anoxic carbonaceous shale. Geological Province: Georgina Basin.||||||07-MAY-13
645|Arthur Creek Formation|63450|4|Described|p78 Fig. 5, p80-81|Middle Cambrian|Middle Cambrian|Thickness: >800m. Geological province: Georgina Basin, West Toko Syncline. Equivalent to upper Hay River Formation and Marqua Formation. Comprises a lower pyritic black shale and laminated dolostone lower unit and dolostone and limestone upper unit. Richly fossiliferous.||||||22-FEB-16
645|Arthur Creek Formation|63562|5|Briefly described|p338 fig 3, p348|Middle Cambrian|Middle Cambrian|Of Georgina Basin.||||Correlated with Giles Creek Dolomite. Is overlain by Arrinthrunga Formation.|Carbonate-rich.|06-DEC-17
645|Arthur Creek Formation|64068|4|Described|p59-63, 65,  67, 83  p86-91, p44, p ix|Middle Cambrian|Middle Cambrian|Fossiliferous. Potential hydrocarbon source rock. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Contains turquoise.  A detailed petrography is provided.||Of Narpa Group.|Now includes rocks formerly assigned to Marqua Formation, 'upper Hay River Formation Member 2' and some Sandover beds|Disconformably overlies Thorntonia Limestone. Conformably overlain by Steamboat Sandstone in Sth and by Chabalowe Formation in SW.|Anoxic shale below dolostone, limestone and siliciclastic mudstone.|05-APR-12
645|Arthur Creek Formation|64443|4|Described|iii, p6 Tb.1, p9, p40, 41. |Floran||Correlative of Wonarah Formation, Ranken Limestone, Camooweal Dolostone. Max 457m thick.||||Conformably underlies Arrinthrunga Formation; disconformably overlies Thorntonia Limestone or unconformably overlies undivided South Nicholson Group.|Foetid pyritic-carbonaceous black shale and laminated dolostone, overlain by dolostone and limestone; their contact is identifiable in drillholes. Has nodular evaporite, brecciated texture, fossils, disseminated pyrite.|14-MAY-14
645|Arthur Creek Formation|64778|6|Mentioned|p13, 25-26|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin. Potential hydrocarbon source.||||||
645|Arthur Creek Formation|64812|5|Briefly described|p236, p241-9, p251|Middle Cambrian|Middle Cambrian|Overlies Thorntonia Limestone. Geol.Prov: Georgina Basin. Described as Lower A.C. Formation, outer ramp facies of marine anoxic dolomite shale; and, Upper A.C.Fm, middle ramp facies grading to increasingly oxygenated, mixed clastic/ carbonate sediments.||||||07-FEB-11
645|Arthur Creek Formation|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Geol.prov:Georgina Basin.Comprises marine anoxic shale (outer ramp facies) grading into middle- + inner-ramp carbonate + clastic rocks. 'Hot shale' at base, rich in algal/bacterial organic matter, provides petroleum source/seal rocks for Georgina Basin.||||||11-FEB-09
645|Arthur Creek Formation|65237|4|Described|p3 Fig. 4, p6|Middle Cambrian|Middle Cambrian|Informally subdivided into upper/lower Arthur Creek Formations; oil prone rocks in lower part. Max.thickness: 400m in basin/800m in Toko Syncline. Geol.prov:Georgina Basin. Depositional environment details included. Contains E-log marker "Hot Shale".||||||07-FEB-11
645|Arthur Creek Formation|65239|5|Briefly described|p2|Middle Cambrian|Middle Cambrian|Unconformably overlies Thorntonia Limestone. Geological province: Georgina Basin.||||||
645|Arthur Creek Formation|65342|5|Briefly described|p7.|Middle Cambrian|Middle Cambrian|Georgina Basin. Max. thickness at least 457 m. Seen as having potential as an insulating layer for geothermal energy.|||||Dolostone, limestone in upper part; black, foetid, pyritic-carbonaceous shale in lower part.|
645|Arthur Creek Formation|65345|5|Briefly described|p6 Fig.5, p7, p14.|Cambrian|Cambrian|Southern Georgina Basin. Waterbore RN013015 contains a 3 m interval containing 16.9% P2O5.||||Unconformably overlies Thorntonia Limestone. Is overlain by Steamboat Sandstone.||
645|Arthur Creek Formation|65489|5|Briefly described|p124, p126-127|||Georgina Basin. Over 80,000 km2. Rich in algal/bacterial organic matter: provides the principal source/seal rocks of the Basin. 20-100m thick.|||||Anoxic, pyritic and carbonaceous, partly dolomitic shale.|
645|Arthur Creek Formation|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.|||Black shale and dolostone.|
645|Arthur Creek Formation|67126|5|Briefly described|p1-7, p10-16, p19, p22-25, p27-33|Middle Cambrian|Middle Cambrian|See also p36, p38. Georgina Basin. A source rock ("hot shale") worthy of serious consideration as a potential gas shale (reasons detailed). Rock Eval analysis, Rock Eval Temperature Programme: Pyrolysis, Thermovaporisation, Pyrolysis Gas Chromatography results presented in detail.||||||
645|Arthur Creek Formation|67352|6|Mentioned|p69|||||||||
645|Arthur Creek Formation|67402|6|Mentioned|p216|||Georgina Basin. Potential seal unit.|||||Dolomitic mudstone.|
645|Arthur Creek Formation|67870|5|Briefly described|p39, p43, p46-47, p50-53, p55|Middle Cambrian|Middle Cambrian|Western Georgina Basin. Includes an organic-rich, potential source-rock, unit. 4% TOC. Detailed modelling showing transformation ratios, expulsion mass (bulk) and expulsions mass for oil and gas.||Narpa Group.||Equivalent to the Devoncourt Limestone.|Organic-rich (8% TOC) shale, marl.|
645|Arthur Creek Formation|68518|6|Mentioned|p14|||In HUCKITTA (Freeman, 1986). Sandover beds will be shown mainly as this unit on 2nd ed of ELKEDRA (Stidolph and others, in. prep.)||||||30-JUN-14
645|Arthur Creek Formation|69206|6|Mentioned|p2-3|||Georgina Basin. Contains hydrocarbon source rocks.||||||
645|Arthur Creek Formation|69418|5|Briefly described|p3:31, 36|Middle Cambrian|Middle Cambrian|Georgina Basin. Hosts the Barrow Creek 1 and Arganara phosphate deposits (briefly described). The lower part of this unit has potentially prolific marine source rocks, particularly the basal "hot shale" facies, as well as considerable unconventional shale gas and oil potential. The upper part has shale gas potential.||||||12-JUL-16
645|Arthur Creek Formation|69437|5|Briefly described|p22:10-11, 15-16|Cambrian|Cambrian|Southern Georgina Basin, Centralian B Superbasin. Sequence 2. Deposition was in relatively deep, followed by relatively shallow restricted, marine conditions. An important potential petroleum source rock; also potential reservoir in the upper part. The lower part of this unit has considerable unconventional shale gas and oil potential, with shale gas potential in the upper part.||||Overlies Thorntonia Limestone. Is overlain by Steamboat Sandstone and Chabalowe Formation.|Pyritic-carbonaceous black shale, dolostone and minor siliciclastic rocks overlain by carbonate rocks and siliciclastic mudstone.|12-JUL-16
645|Arthur Creek Formation|69439|6|Mentioned|p24:10|||Georgina Basin.||||Lower part is correlated with the Bloodwood Formation (Ngalia Basin).||12-JUL-16
645|Arthur Creek Formation|69443|4|Described|p28:16-19, 22-25, 32, 41, 43, 45-47|Middle Cambrian|Middle Cambrian|Freeman (1986) after K.G. Smith (1964); modified by Kruse et al. (2002). Southern Georgina Basin. From <30m thick to over 483m (possibly 720m?). Richly fossiliferous: latest Ordian to Boomerangian. Dysoxic to anoxic deeper marine, shallowing upwards to restricted platform, deposits. Passes laterally into Wonarah Formation. Correlated with Anthony Lagoon Formation, Ranken Limestone and Camooweal Dolostone. Contains >1100 ppm Zn at depth in the Trackrider prospect area. Is associated with the phosphate deposits at Ammaroo and near Ooratippra. Forms a reservoir-seal couplet with underlying Thorntonia Limestone, as well as intraformational couplets in middle and upper parts of the Formation. Is a potentially world-class petroleum source rock. Also a potential petroleum reservoir, and its shales provide a regional seal. Has had hydrocarbon shows in drilled wells.||Narpa Group.||Disconformably overlies Thorntonia Limestone or Red Heart Dolostone. Is overlain conformably by Steamboat Sandstone and Chabalowe or Arrinthrunga Formations.|Foetid pyritic-carbonaceous black shale and laminated dolostone interval with minor dolomitic quartz sandstone and conglomerate; overlain by dolostone, limestone and minor quartzose dolostone and siliciclastic mudstone.|12-JUL-16
645|Arthur Creek Formation|69561|5|Briefly described|p33 fig 2, p34|Boomerangian|Templetonian|Trilobite fossil assemblage constrains age of underlying Thorntonita Limestone.||||Overlain by Steamboat Sandstone, Chabalowe Formation|Fossiliferous siltstone.|
645|Arthur Creek Formation|69573|6|Mentioned|p656, 659, 661|||Georgina Basin. Features Cambrian Stage 5 fossil sites.||||||
645|Arthur Creek Formation|69673|4|Described|p103,    p120, p123,   p128,  p131, p141|Cambrian|Cambrian |Georgina Basin. Petroleum source rock, potential as a conventional and unconventional reservoir rock also. Shale within this unit may form a hydrocarbon seal. More than 483m thick.||||Disconformably overlies Thorntonia Limestone, Red Heart Dolostone, conformably overlain by Steamboat Sandstone, Chabalowe Formation||
645|Arthur Creek Formation|70380|6|Mentioned|p745|Series 3|Series 3|Southern Georgina Basin.||||||
645|Arthur Creek Formation|70723|5|Briefly described|p22, p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Thorntonia Limestone, Overlain by Chabalowe Formation or Steamboat Sandstone.|Sandy limestone.|
645|Arthur Creek Formation|70752|6|Mentioned|p140-141|||Georgina Basin. Brachiopod species discussed.||||||
645|Arthur Creek Formation|70951|4|Described|p1069-1072,1074-1084||Wuliuan|Geological province: Georgina Basin. Base of Arthur Creek Formation interpreted as older in Dulcie Sycline (Templetonian/Stage 5) than in Toko Syncline (Floran/Drumian) and is characterised by regionally extensive organic-rich shales with high TOC across the southern basin depocenters from west to east (Dulcie Domain, older succession; Toko Domain, younger succession). Quartz and carbonate dominated in the Dulcie Domain, carbonate, white mica and quartz-dominated in Toko Domain.||Unit of Narpa Group.||Underlain by Thorntonia Limestone. Overlain by Steamboat Sandstone.|Characterised by regionally extensive basal organic-rich shales with high TOC. ?overlying units characterised by a mixture of quartz rich, calcite and dolomite mineralogy.|08-MAR-23
645|Arthur Creek Formation|71800|6|Mentioned|p26 fig 3|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Overlain by the Arrinthrunga Formation.||
645|Arthur Creek Formation|72321|4|Described|Fig 2, p3-4, p5, 6, 7|Guzhangian|Wulian|Dulcie Syncline, Toko Syncline, Georgina Basin. Diachronous. Youngs to East. Age range in Dulcie Syncline is latest Ordian to Undillan or younger, but Boomerangian sediments absent or thin. Age more restricted  in Toko Syncline from Floran, but up to Boomerangian (from agnostid trilobites).||of Narpa Group.||Overlain by Steamboat Sandstone in Toko Syncline. Lower part in Dulcie Syncline unconformably overlies Hay River Formation and correlates with Thorntonia Limestone, Undilla Sub-Basin.||
645|Arthur Creek Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites, brachiopods, echinoderms.||Narpa Group||Overlain by the Steamboat Sandstone. Disconformably overlies the Thorntonia Limestone.|Black shale; pyritic-carbonaceous, undulose laminated, flaser bedded; minor laminated dolostone; dolomitic sandstone, conglomerate; dolostone, limestone; minor mudstone; fossiliferous.|05-JUL-22
645|Arthur Creek Formation|72516|3|Fully described|p11-12, p91-93|Cambrian Series 3|Cambrian Series 3|Georgina Basin. Poorly to moderately exposed in ELKEDRA, HUCKITTA, TOBERMORY, HAY RIVER, SANDOVER RIVER and JERVOIS RANGE SPECIAL map sheets. Outcrops in the Jervois Range and north of the Johansen Range. Type section in cored drillhole NTGS99/1. Informally subdivided into an upper and lower interval. The lower interval was deposited in dysoxic to anoxic, deep marine environment whilst the upper interval was deposited in an aerobic, restricted, platformal marine environment above wave base. Contains fossil trilobites, brachiopods and echinoderms in the upper interval which indicate a Series 3 of the Cambrian depositional age. 250m thick in the map sheet area, 42-720m thick elsewhere. Interpreted to correlate wioth the Anthony Lagoon beds, Wonarah beds, Ranken Limestone, Camooweal Dolostone, Age Creek Formation, Currant Bush Limestone, V-Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Inca Formation, Devoncourt Limestone, Roaring Siltstone, Beetle Creek Formtion, Blazan Shale, Quita Formation, Selwyn Range Limestone, Giles Creek Dolostone, Hugh River Shale, Tempe Formation.||Narpa Group||Conformably and gradationally overlain by the Arrinthrunga Formation. Conformably overlain  by Steamboat Sandstone. Disconformably overlies the Thorntonia Limestone and Red Heart Dolostone.|Black shale; pyritic, carbonaceous, undulose-laminated, flaser bedded; minor laminated dolostone; dolomitic sandstone, conglomerate. Dolostone, limestone and minor mudstone.|14-APR-22
645|Arthur Creek Formation|73288|5|Briefly described|p697-700, 702-707, 709 Fig.10, 710-713|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Non-economic oil and gas shows have been recorded. Downhole (Hylogger) logs; scratch test results tabulated.||Narpa Group.||Unconformably overlies Thorntonia Limestone. Is overlain by the Chabalowe Formation.|Upward-shallowing sequence with basal marine anoxic dolomitic organic-rich shales (TOC up to 16 wt%), grading up to mixed clastic/carbonate sediments and capped by near-shoreline carbonate and quartz-rich sandstone.|07-MAR-23
648|Arthur Point Formation|42868|5|Briefly described|p18|||see also Fig.5 p18. Probably not variation on Arthur Creek Formation.||||||05-AUG-08
705|Ashford Coal Measures|22857|4|Described|p263, p538 App.1 Tb.A1.9|Early Permian|Early Permian|Arenite, argillite, cobble conglomerate; interbedded coal. Max. thickness: 300m. Equivalent of Greta Coal Measures. Geological Province: New England Fold Belt.||||||
705|Ashford Coal Measures|22864|6|Mentioned|p263|Artinskian|Artinskian|Stage B - 268-258 Ma.||||||20-AUG-18
705|Ashford Coal Measures|23050|4|Described|p14 Table 1|Early Permian|Early Permian|Age: Early Permian. Greta Coal Measures equivalent.||||||
705|Ashford Coal Measures|23051|5|Briefly described|Map Legend|Early Permian|Early Permian|||||||
705|Ashford Coal Measures|30133|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|30911|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|31694|6|Mentioned|p347|||||||||
705|Ashford Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|32672|6|Mentioned|p675|||||||||
705|Ashford Coal Measures|32920|5|Briefly described|p90|||||||||
705|Ashford Coal Measures|32944|6|Mentioned|p699|||See also p709. Lower Permian.||||||05-AUG-08
705|Ashford Coal Measures|34292|6|Mentioned|p28|||Permian||||||
705|Ashford Coal Measures|34350|6|Mentioned|p16|||See pp17,18. Permian. Correlation with Greta Coal Measures.||||||05-AUG-08
705|Ashford Coal Measures|34400|6|Mentioned|p9|||Permian||||||
705|Ashford Coal Measures|34556|4|Described|p269|||||||||
705|Ashford Coal Measures|35767|6|Mentioned|p56|||||||||
705|Ashford Coal Measures|36172|6|Mentioned|Appendix|||||||||
705|Ashford Coal Measures|36961|6|Mentioned|Table 1|||||||||
705|Ashford Coal Measures|37065|6|Mentioned|p29|||||||||
705|Ashford Coal Measures|37100|4|Described|p259|||||||||
705|Ashford Coal Measures|38064|6|Mentioned|p40|||||||||
705|Ashford Coal Measures|38806|6|Mentioned|p72|||||||||
705|Ashford Coal Measures|38958|5|Briefly described|p490|||||||||
705|Ashford Coal Measures|40245|6|Mentioned|Table 2|||||||||
705|Ashford Coal Measures|40246|6|Mentioned|p173|||||||||
705|Ashford Coal Measures|42182|5|Briefly described|p302|||||||||
705|Ashford Coal Measures|42748|6|Mentioned|Fig.3 P9|Permian||||||||
705|Ashford Coal Measures|42923|6|Mentioned|p43|||||||||
705|Ashford Coal Measures|43017|5|Briefly described|Fig.2,p374|||||||||
705|Ashford Coal Measures|43344|14|Not recorded|p11||Permian|New England central zone.||||||
705|Ashford Coal Measures|43384|14|Not recorded|Map Legend|Early Permian||||||||
705|Ashford Coal Measures|43436|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
705|Ashford Coal Measures|43984|14|Not recorded|p139|||Correlated with Greta Coal Measures.||||||
705|Ashford Coal Measures|44093|5|Briefly described|p238 App. 1|Early Permian|Early Permian|Age: Late Early Permian. Continental, coal measures. Geological Province: New England Fold Belt.||||||
705|Ashford Coal Measures|44565|2|Defined|p230-232|||See also Lexicon. Gangamopteris and Glosssopteris.||||||
705|Ashford Coal Measures|48784|14|Not recorded|?|||||||||
705|Ashford Coal Measures|48940|6|Mentioned|p18|||||||||
705|Ashford Coal Measures|61772|6|Mentioned|p128 Fig. 2, p130||Early Permian|In text, Coal Measures is C.M. Geological Province: Bowen Basin.||||||
705|Ashford Coal Measures|62534|6|Mentioned|p7|Early Permian|Early Permian|||||||07-FEB-11
705|Ashford Coal Measures|63347|5|Briefly described|p5 Fig. 2|Early Permian|Early Permian|Geological Province: New England Orogen. Felsic to andesitic volcanic and volcaniclastic rocks.||||||04-JUN-07
705|Ashford Coal Measures|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Fluvial sandstone, argillite, cobble conglomerate and interbedded coal horizons.||||||11-DEC-07
705|Ashford Coal Measures|68005|4|Described|p18, p22, pp36-42, p153, p170.|Early Permian|Early Permian|Central Block, New England Fold Belt. In part thrust under granite on its western side. Correlated with Greta Coal Measures of the Sydney Basin. 170 m thick at old colliery at Ashford. Intense multiphase structural deformation has reduced the coal fabric to a highly friable, non-cohesive material with greatly increased fines content.|||Includes Ashford, Bonshaw and Bukkulla Members.|Unconformably overlies Texas beds. Thrust faulted against Bundarra Supersuite.|Fluvial sandstones and shales, interbedded cobble conglomerate and coal horizons.|
705|Ashford Coal Measures|68006|5|Briefly described|p26, pp84-92.|Permian|Permian|A NE-striking belt, immediately east of northern Bundarra Supersuite, hosting significant coal deposits. Thrust at least 1.5 km under granite to its west by the Severn Thrust Fault. Resource discussed in detail.|||Includes Ashford and Bonshaw seams.||Fluvial sandstones and shales and interbedded cobble conglomerate and coal horizons.|
724|Astrea Formation|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
724|Astrea Formation|22781|4|Described|p21|Proterozoic|Proterozoic|Holroyd Group||||||
724|Astrea Formation|23420|5|Briefly described|p 143 table 4.4||Calymmian|In the Holroyd Group, Coen Inlier. Thickness 1500m. Age: 1563Ma (detrital zircon)||||||
724|Astrea Formation|23429|5|Briefly described|p435|||Of Holroyd Group.||||||
724|Astrea Formation|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group.||||||
724|Astrea Formation|42610|6|Mentioned|p12|||Reserved as Astrea Slate.||||||
724|Astrea Formation|43596|4|Described|p22, p19 Tb. 1||Proterozoic|Of Holroyd Group. Conformable on Sugarbag Creek Quartzite. Age: <1585Ma. Max. thickness: 1500m. Intruded by Ukin Granite, Gumhole Monzogranite and Kintore Granite.||||||15-JAN-09
724|Astrea Formation|43738|6|Mentioned|p48|||||||||
724|Astrea Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||24-JAN-05
724|Astrea Formation|63866|4|Described|p80|Calymmian|Calymmian|Savannah Province, Coen Region. Numeric age is interpreted as the maximum depositional age of this unit.|1560 +/- 22 Ma (U-Pb zircon)|Holroyd Group|||Light-grey, very fine-grained, laminated slate.|
724|Astrea Formation|69591|5|Briefly described|p77 Fig.2.75, p78-79 Tb.2.6|||Savannah Province, Coen Inlier. 1500m thick. Occurs S of Edward River.|<1563 Ma (maximum depositional age).|Holroyd Group.||Partly correlates with O'Lane Formation.|Slate, spotted graphitic metasiltstone, andalusite schist.|
724|Astrea Formation|71592|5|Briefly described|Appendix A.|||Savannah Province.|1560+/-22 Ma (MDA: U-Pb zircon SHRIMP)||||Slate.|
733|Atherton Basalt|23423|4|Described|p260|Quaternary|Pliocene|Underlain by Walsh Bluff Volcanics (unconformable). Atherton Subprovince.||||||20-AUG-08
733|Atherton Basalt|23497|5|Briefly described|Table 1|Holocene|Miocene|||||||
733|Atherton Basalt|23503|5|Briefly described|Map Legend|Holocene|Miocene|||||||
733|Atherton Basalt|23506|5|Briefly described|Map Legend|Holocene|Miocene|||||||
733|Atherton Basalt|23507|5|Briefly described|Map Legend|Holocene|Miocene|||||||
733|Atherton Basalt|23616|4|Described|Table 1B p11, p40||Cenozoic|Includes Culgar Basalt of Best (1962). Unconformably overlies the Hodgkinson Formation. Atherton Basalt Province.||||||19-NOV-08
733|Atherton Basalt|30505|4|Described|p7|||See also p9,10,11.Late ? Miocene or Pliocene to Recent age||||||20-AUG-08
733|Atherton Basalt|31832|6|Mentioned|Table 6|||||||||
733|Atherton Basalt|33205|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
733|Atherton Basalt|33695|6|Mentioned|Plate 1.|||||||||
733|Atherton Basalt|33963|6|Mentioned|Map legend|Permian|Permian|||||||
733|Atherton Basalt|34046|6|Mentioned|Table III|||Late Tert.||||||
733|Atherton Basalt|34998|6|Mentioned|p347|||||||||
733|Atherton Basalt|36353|6|Mentioned|p359|||||||||
733|Atherton Basalt|36563|6|Mentioned|Table 1|||||||||
733|Atherton Basalt|37607|6|Mentioned|Fig.6|||Table 1 and Fig. 9 show that Atherton province basalts vary in age from ~3 - 0.01 Ma.||||||26-MAR-13
733|Atherton Basalt|39445|5|Briefly described|Table 14|||||||||
733|Atherton Basalt|39998|6|Mentioned|Fig.11|||||||||
733|Atherton Basalt|40049|6|Mentioned|Fig.2|||||||||
733|Atherton Basalt|42658|4|Described|p41|||||||||
733|Atherton Basalt|43060|4|Described|p62,Table 1b|Quaternary|Pliocene|||||||
733|Atherton Basalt|43285|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
733|Atherton Basalt|43625|5|Briefly described|p48|Quaternary|Pliocene|Age: 1.7 Ma||||||
733|Atherton Basalt|43896|14|Not recorded|Map Legend|Quaternary|Tertiary|||||||
733|Atherton Basalt|43898|14|Not recorded|Map Legend||Cenozoic|||||||19-NOV-08
733|Atherton Basalt|43903|14|Not recorded|Map Legend|Recent|Pliocene|||||||
733|Atherton Basalt|43927|14|Not recorded|p9,13, opp.8|||||||||
733|Atherton Basalt|44068|14|Not recorded|p18|||||||||
733|Atherton Basalt|44246|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
733|Atherton Basalt|44292|14|Not recorded|Tb.1,opp.p8|||Correlated with Piebald Basalt.||||||
733|Atherton Basalt|44296|14|Not recorded|Map Legend|Pleistocene|Pliocene|||||||
733|Atherton Basalt|44329|14|Not recorded|p8,10|||||||||
733|Atherton Basalt|44330|14|Not recorded|Map Legend|||Undifferentiated Cainzoic.||||||
733|Atherton Basalt|44425|14|Not recorded|map|||||||||
733|Atherton Basalt|45014|14|Not recorded|Pl.38 (map)||Cenozoic|||||||19-NOV-08
733|Atherton Basalt|45025|3|Fully described|p106-113|Quaternary|Tertiary|Fully described and description of Vents.||||||
733|Atherton Basalt|45065|4|Described|Table 4|||||||||
733|Atherton Basalt|48976|6|Mentioned|p36|||||||||
733|Atherton Basalt|50387|5|Briefly described|Map Legend|Pleistocene|Pliocene|Dark grey to black, vesicular and massive olivine basalt||||||
733|Atherton Basalt|60425|3|Fully described|p42 Tb. 3|Holocene|Miocene|Also called Atherton Basalt Province or Quincan Province. Comprises 4 named basalts. Age: 7.1Ma. Max. thickness: ~300m. Unconformable on Barnard Metamorphics + Hodgkinson Fm. Detailed lithology included.||||||07-FEB-11
733|Atherton Basalt|61155|5|Briefly described|p20|Pleistocene|Late Pliocene|In eastern Cape York.||||||03-MAR-10
733|Atherton Basalt|66180|6|Mentioned|p280 Fig.1|||||||||10-MAY-12
733|Atherton Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Chudleigh, McIvor River, McLean, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
733|Atherton Basalt|68576|6|Mentioned|Q_11: p17|Pliocene|Pliocene|South of Mareeba.||||||
751|Auburn Complex|22757|6|Mentioned|p14|Triassic|Permian|||||||
751|Auburn Complex|23037|5|Briefly described|p111,112|Triassic|Carboniferous|||||||
751|Auburn Complex|29964|6|Mentioned|p7|||||||||
751|Auburn Complex|30692|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
751|Auburn Complex|31131|6|Mentioned|p157|||Upper Carboniferous||||||
751|Auburn Complex|32086|6|Mentioned|p328|||Middle Carboniferous granitoids.||||||05-AUG-08
751|Auburn Complex|32136|6|Mentioned|p2|||Carboniferous to Mesozoic. Geological  map.||||||05-AUG-08
751|Auburn Complex|33381|6|Mentioned|p118|||See also p121.||||||05-AUG-08
751|Auburn Complex|34408|6|Mentioned|p187|||||||||
751|Auburn Complex|38204|6|Mentioned|p71|||||||||
751|Auburn Complex|39212|6|Mentioned|p8|||||||||
751|Auburn Complex|40090|6|Mentioned|p83|||||||||
751|Auburn Complex|42547|5|Briefly described|p56|||||||||
751|Auburn Complex|43851|14|Not recorded|p107|Triassic|Carboniferous|||||||
751|Auburn Complex|43994|14|Not recorded|Map Legend|||||||||
751|Auburn Complex|43998|4|Described|p10,19,22,23|||Age: 240+/-10Ma; 300 Ma.||||||05-AUG-08
751|Auburn Complex|44170|14|Not recorded|p31|||Source material.||||||
751|Auburn Complex|44207|14|Not recorded|p115|||||||||
751|Auburn Complex|44218|14|Not recorded|p18|||||||||
751|Auburn Complex|44337|5|Briefly described|Map Legend||Carboniferous|Lithology.||||||
751|Auburn Complex|44360|14|Not recorded|p36|||||||||
751|Auburn Complex|44379|14|Not recorded|p18,21,23-25|||||||||
751|Auburn Complex|44381|14|Not recorded|p7,8|||||||||
751|Auburn Complex|44523|14|Not recorded|p648|||Contains prospect of gold. No age given.||||||
751|Auburn Complex|44551|14|Not recorded|p539|||||||||
751|Auburn Complex|44636|14|Not recorded|p162-164,166|||||||||
751|Auburn Complex|44640|14|Not recorded|On errata sheet|||||||||
751|Auburn Complex|44815|14|Not recorded|unknown (p313-346)|||||||||
751|Auburn Complex|45071|3|Fully described|p85|||See also Table 16. Dated 311 m.y.||||||
751|Auburn Complex|45110|4|Described|p66|||||||||
751|Auburn Complex|45686|14|Not recorded|p.358|||||||||
751|Auburn Complex|48600|14|Not recorded|p1,7-20|||Early Triassic granodiorite pluton.||||||
751|Auburn Complex|48919|4|Described|p74|||See also p75-76. Upper Carboniferous -Lower Permian.||||||05-AUG-08
751|Auburn Complex|50190|6|Mentioned|p17, 69|||Term used for Wingfield Adamellite in the Company Reports. Also used for Rawbell batholith in Company Reports.||||||
751|Auburn Complex|60282|6|Mentioned|p48|||Term used in Company reports for the gneissic diorite phase of the Rawbelle Batholith.||||||
751|Auburn Complex|65388|6|Mentioned|p18|||||||||
780|Austral Downs Limestone|8187|5|Briefly described|Map legend|Tertiary|Tertiary|Chert, limestone.||||||24-JUN-04
780|Austral Downs Limestone|8217|5|Briefly described|Map Legend|Tertiary|Tertiary|Chert, Limestone.||||||
780|Austral Downs Limestone|10116|5|Briefly described|Map Legend|Tertiary|Tertiary|Chalcedony, shale, tufa.||||||
780|Austral Downs Limestone|22954|6|Mentioned|Fig3p9||Tertiary|||||||
780|Austral Downs Limestone|24419|5|Briefly described|p19|Miocene|Miocene|Lacustrine limestone deposit cropping out within the western third of URANDANGI 1:250 000 sheet.||||||08-MAR-05
780|Austral Downs Limestone|24442|5|Briefly described|p45|Cenozoic|Cenozoic|Lacustrine deposits.  On the SANDOVER RIVER sheet.||||||
780|Austral Downs Limestone|31532|4|Described|Table 1|||||||||
780|Austral Downs Limestone|32418|6|Mentioned|p2|||||||||
780|Austral Downs Limestone|34395|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|34441|6|Mentioned|p15|||||||||
780|Austral Downs Limestone|35121|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|35139|4|Described|Table 2|||||||||
780|Austral Downs Limestone|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
780|Austral Downs Limestone|37607|5|Briefly described|p333|||See also Fig.4||||||
780|Austral Downs Limestone|38532|4|Described|Fig.1|||||||||
780|Austral Downs Limestone|38832|6|Mentioned|p157|||||||||
780|Austral Downs Limestone|39445|5|Briefly described|Table 14|||||||||
780|Austral Downs Limestone|39921|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|41298|6|Mentioned|Map legend|Miocene||||||||
780|Austral Downs Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
780|Austral Downs Limestone|44088|14|Not recorded|Tb.1,opp.p.6|||Similar to limestone on Betoota sheet.||||||
780|Austral Downs Limestone|44121|14|Not recorded|p6|||||||||
780|Austral Downs Limestone|44122|14|Not recorded|Fig.48,321|||||||||
780|Austral Downs Limestone|44133|5|Briefly described|p190 Fig. 10.30|Pliocene|Pliocene|||||||
780|Austral Downs Limestone|44168|14|Not recorded|Tb.1,p6,8|||Similar to Tertiary limestone on Birdsville sheet. Also on NT card.||||||
780|Austral Downs Limestone|44210|14|Not recorded|map, Tb.2|||||||||
780|Austral Downs Limestone|44212|14|Not recorded|p110|||Not on white card.||||||
780|Austral Downs Limestone|44221|14|Not recorded|p87,88,89,102|||||||||
780|Austral Downs Limestone|44222|14|Not recorded|p119,120|||||||||
780|Austral Downs Limestone|44273|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44275|14|Not recorded|Map Legend|||||||||
780|Austral Downs Limestone|44283|14|Not recorded|p.8|||Similar to Brunette Limestone.||||||
780|Austral Downs Limestone|44285|2|Defined|p.9,10||Tertiary|Tb.opp.p.6. Tertiary. Avon Downs. (F53-4). White nodular limestone and dolomite, some chert.||||||
780|Austral Downs Limestone|44291|2|Defined|Tb.1,opp.p6,10,map|||Equivalent to Horse Creek Formation. Overlies Wilgunya Formation.||||||
780|Austral Downs Limestone|44301|14|Not recorded|p.9|||(F53-4)||||||
780|Austral Downs Limestone|44308|14|Not recorded|p11,Tb.2||Tertiary|||||||
780|Austral Downs Limestone|44309|2|Defined|Tb.1,opp.p7,14,map||Tertiary|Fossils rare.||||||
780|Austral Downs Limestone|44312|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44313|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44326|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44334|14|Not recorded|map legend||Tertiary|Tertiary.||||||
780|Austral Downs Limestone|44351|2|Defined|p12-15,18-27,fig.13,||Tertiary|Pls.7-9,11. (Tertiary or Quaternary) Overlies Ninmaroo Formation. Possibly equivalent to Noranside Limestone.||||||
780|Austral Downs Limestone|44355|14|Not recorded|map legend||Tertiary|White nodular limestone and dolomite, some chert.||||||
780|Austral Downs Limestone|44358|4|Described|p12,Tb.1||Tertiary|Age assumed.||||||
780|Austral Downs Limestone|44361|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44362|4|Described|Tb.1,p13||Tertiary|||||||
780|Austral Downs Limestone|44457|2|Defined|p.9, Tb.1, map||Tertiary|Sandover River sheet. (F53-8).||||||
780|Austral Downs Limestone|44458|5|Briefly described|map legend|||Limestone; white, red, crystalline, layered algal(?), siliceous.  Tertiary (?).||||||16-NOV-04
780|Austral Downs Limestone|44469|2|Defined|opp.p.6, Tb.I|||(F53-12). Gastropods.||||||
780|Austral Downs Limestone|44470|5|Briefly described|map legend||Tertiary|||||||02-DEC-04
780|Austral Downs Limestone|44543|14|Not recorded|p35,36|||||||||
780|Austral Downs Limestone|45032|14|Not recorded|p8||Tertiary|Tb.1. Pl.1. Barkly Tableland.||||||
780|Austral Downs Limestone|45052|4|Described|p136|||Cainozoic||||||
780|Austral Downs Limestone|45145|6|Mentioned|Table 7|||||||||
780|Austral Downs Limestone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
780|Austral Downs Limestone|46958|6|Mentioned|Fig.2|||||||||
780|Austral Downs Limestone|48844|14|Not recorded|p.57|||||||||
780|Austral Downs Limestone|49027|4|Described|p22|||||||||
780|Austral Downs Limestone|50100|6|Mentioned|p23|Cenozoic|Cenozoic|||||||
780|Austral Downs Limestone|60122|5|Briefly described|p35|Cenozoic|Cenozoic|Pale grey limestone, silicified to red-brown and white chert and chalcedony toward the top.  Unconformably overlies Kelly Creek and Ninmaroo Formations. Max. thickness: 8m. Geological Province: Georgina Basin.  See also p4-5, p10 Tb. 1.||||||19-NOV-08
780|Austral Downs Limestone|60123|4|Described|p5|Quaternary|Tertiary|Limestone, silicified to chert and chalcedony. Unconformably overlies Ninmaroo Formation. Thickness: 8m.||||||05-AUG-08
780|Austral Downs Limestone|60590|5|Briefly described|Map legend|Cenozoic|Cenozoic|Limestone; cherty and chalcedonic.||||||23-DEC-09
780|Austral Downs Limestone|60675|5|Briefly described|Map legend|Tertiary|Tertiary|Limestone: cherty and chalcedonic.||||||11-JAN-05
780|Austral Downs Limestone|60703|6|Mentioned|p714, p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
780|Austral Downs Limestone|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Together with Noranside Limestone thickness is 35m. Geological Province: Georgina Basin.||||||03-MAR-10
780|Austral Downs Limestone|61404|5|Briefly described|Map legend|Neogene|Paleogene|Limestone: cherty and chalcedonic. Geological Province: southern Georgina Basin.||||||07-NOV-08
780|Austral Downs Limestone|62082|5|Briefly described|p19|Miocene|Miocene|Lacustrine deposits with a chert capping and associated duricrust. Overlies Aroota Lateritic Profile. Geological Province: Georgina and Arunta terrains.||||||07-FEB-11
780|Austral Downs Limestone|62658|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Limestone: cherty and chalcedonic.||||||
780|Austral Downs Limestone|63450|5|Briefly described|p78 Fig. 5, p83|Cenozoic|Cenozoic|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
780|Austral Downs Limestone|64047|5|Briefly described|p60, p61|Tertiary|Tertiary|Overlies Marion Formation. Geological province: Eromanga Basin.||||||16-APR-08
780|Austral Downs Limestone|64068|4|Described|pp79-81, p19, p42,  p ix|Miocene|Miocene|Austral Downs Basin. Overlies Georgina Basin rocks. Coeval with Brunette Limestone. Radiometrics indicate a signal sourced almost purely from U. Lower part correlated with Poodyea Formation.|||||Limestone, calcrete, chalcedony, chert, limestone breccia; minor sandstone, siltstone.|05-APR-12
780|Austral Downs Limestone|64443|5|Briefly described|p5 Fig.3, p6 Tb.1, p18-23, p31, p41 |Neogene|Miocene|Max 14m thick. Covers contact between Camooweal Dolostone and Arrinthrunga Formation. Lithologically identical with Brunette Limestone; distinguished geographically: this unit is within Georgina River drainage.||||Unconformably overlies Camooweal Dolostone.|Limestone, silicified to chert and chalcedony; characteristic features include rhizoliths and circum- and intragranular cracks.|14-MAY-14
780|Austral Downs Limestone|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In AVON DOWNS area. May correlate with Cleanskin beds, Brunette Limestone and Golliger beds.||||||
780|Austral Downs Limestone|65344|5|Briefly described|p13, p43-44|Cenozoic|Cenozoic|Of the Georgina Basin. See thin section descriptions for detail.||||||03-MAY-12
780|Austral Downs Limestone|66131|6|Mentioned|p242 Fig.2, p245|Miocene|Miocene|Late Miocene. Closely resembles Cadelga Limestone.||||||
780|Austral Downs Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Brackish lacustrine and spring limestone and chalcedony overlying limestone and ferruginous detritus.|
780|Austral Downs Limestone|67870|6|Mentioned|p43|Cenozoic|Cenozoic|Georgina Basin.||||||
780|Austral Downs Limestone|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
780|Austral Downs Limestone|69458|5|Briefly described|p42:20|Miocene|Miocene|Georgina River catchment and adjacent areas in Qld. Up to 35m thick. Forms prominent extensive plateaux with 7m high cliffs. Palaeopedogenic features are common.||||Overlies Ninmaroo Formation. Is correlated with the Brunette Limestone.|Pale grey, terrestrial lacustrine limestone, silicified to resistant, red-brown and white chert and chalcedony.|14-SEP-18
780|Austral Downs Limestone|69599|5|Briefly described|p584, p599-601|Miocene|Miocene|Noakes and Traves (1954). Austral Downs Basin. Up to 35m thick. Forms low plateaus. Fossils listed, none of which is age-diagnostic. Has Pliocene silcrete.||||?Overlies unconformably the Marion Formation. Correlated with Doonbara, Whitula and Poodyea Formations; Noranside and Horse Creek Limestones; and Mount Coley Sinter.|Basal 3m of spring-fed lacustrine limestone, pasing up into typical lacustrine limestones.|
780|Austral Downs Limestone|72516|6|Mentioned|p98|Neogene|Neogene|Southern Georgina Basin. Interpreted to be an age equivalent of the Waite Formation of the Waite Basin.||||||09-JUN-21
780|Austral Downs Limestone|73083|6|Mentioned|p10|Cenozoic|Cenozoic|||||||
814|Awinya dune sand|38302|6|Mentioned|Table 1|||Informal name||||||
814|Awinya dune sand|62102|5|Briefly described|p367 Tb. 1|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast.  Age: 486-430Ka (est.).||||||
825|Babalangee Amphibolite|23423|4|Described|p227-228|Cambrian|Proterozoic|Age: 642 Ma (K-Ar). Barnard Province.||||||
825|Babalangee Amphibolite|23430|5|Briefly described|p463|||Barnard Province.||||||
825|Babalangee Amphibolite|23497|5|Briefly described|Table 1||Neoproterozoic|of Barnard Province. Age: 642Ma (K-Ar). Intruded by Mission Beach Granite Complex and Bellenden Ker Granite.||||||
825|Babalangee Amphibolite|23507|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|||||||
825|Babalangee Amphibolite|30334|6|Mentioned|Table 111|||||||||
825|Babalangee Amphibolite|30914|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
825|Babalangee Amphibolite|36419|6|Mentioned|p400|||See also P405||||||
825|Babalangee Amphibolite|39445|5|Briefly described|Table 5|||See also P84||||||
825|Babalangee Amphibolite|39689|6|Mentioned|p56|||||||||
825|Babalangee Amphibolite|40787|6|Mentioned|p330|||||||||
825|Babalangee Amphibolite|43896|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
825|Babalangee Amphibolite|43903|14|Not recorded|Map Legend|||Devonian or Early Carboniferous(?)||||||
825|Babalangee Amphibolite|43927|2|Defined|p11,17,19,opp.8|||Evengrained plag.-hornblende amphibolite, nematoblastic texture. Devonian or Early Carboniferous?||||||
825|Babalangee Amphibolite|44258|14|Not recorded|p40,41|||Intrudes Barron River Metamorphics. Intruded by Mareeba Granite.||||||16-JUL-15
825|Babalangee Amphibolite|45025|4|Described|p51-2||Paleozoic|||||||07-NOV-08
825|Babalangee Amphibolite|60425|5|Briefly described|p6, p10|||Metasomatised by the Bellenden Ker Granite. Age (corrected): 642Ma (K-Ar Richards et al 1966).||||||07-FEB-11
825|Babalangee Amphibolite|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Barnard Province. This unit, as well as Barnard Metamorphics and Cowley Ophiolite Complex, are all mapped under the symbol, -Pob.||||||
825|Babalangee Amphibolite|68731|6|Mentioned|p159, p163|Neoproterozoic|Neoproterozoic|Barnard Province. DeKeyser (1964). Crops out over 20 km2 east of Babinda.|642 Ma, K-Ar (Richards et al. 1966)||||Contains ~75% hornblende, ~23% plagioclase (calcic andesite), and 1-2% titanite, apatite, epidote/clinozoisite and sulphide(s).|
825|Babalangee Amphibolite|70033|6|Mentioned|p52 Fig 8.1||Neoproterozoic|Age shown in map legend (Fig 8.1) as Neoproterozoic - Ordovician?||||||
845|Back Creek Group|13516|6|Mentioned|p147, fig 5|Late Permian|Early Permian|From Denison Trough, Bowen Basin||||||
845|Back Creek Group|22593|6|Mentioned|Table 1|||||||||
845|Back Creek Group|22757|4|Described|p8|Late Permian|Early Permian|Also Table3,p9, Table4,p10. Thickness: 400 m. Unconformable on Kuttung Formation. Conformably under Blackwater Group.||||||10-DEC-07
845|Back Creek Group|22857|6|Mentioned|p315 Fig. 22.8|||Geological Province: Gunnedah and Bowen Basins.||||||
845|Back Creek Group|22865|6|Mentioned|Fig22.8p315|||||||||
845|Back Creek Group|22973|5|Briefly described|p9 Fig.2 (d)|Late Permian|Late Permian|||||||
845|Back Creek Group|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
845|Back Creek Group|22987|6|Mentioned|p299|||||||||
845|Back Creek Group|22988|5|Briefly described|p303|||||||||
845|Back Creek Group|23002|5|Briefly described|p417|Permian|Permian|||||||
845|Back Creek Group|23003|5|Briefly described|p423 Table 1|Permian|Permian|||||||
845|Back Creek Group|23004|5|Briefly described|p431 Table 1|Permian|Permian|||||||
845|Back Creek Group|23037|4|Described|p19,23,4,9,40,1,9,50||Permian|Overlain by Goodedulla beds. Underlain by Mount Benmore Volcanics.||||||10-DEC-07
845|Back Creek Group|23042|4|Described|p12,35,48, 50-60, 115||Permian|Underlying unit Mount Bensmore Volcanics.||||||
845|Back Creek Group|23050|6|Mentioned|p81|||||||||
845|Back Creek Group|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
845|Back Creek Group|23161|4|Described|p26 table4 fig11||Early Permian|||||||
845|Back Creek Group|23430|5|Briefly described|p514-515|||Bowen Basin Province.||||||
845|Back Creek Group|24077|5|Briefly described|p410 Tb. 2|Late Permian|Early Permian|Geological Province: Bowen Basin.  See also p411 Tb. 3.||||||
845|Back Creek Group|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|BCG (acronym in figure) interpreted to represent Back Creek Group.  Age: >259Ma.  Geological Province: Bowen Basin.||||||
845|Back Creek Group|24159|5|Briefly described|p148 Fig.2, p147|Late Permian|Early Permian|Geological Province: Bowen Basin. Overlain by the Kianga Formation. Unconformably overlies the Kuttung Volcanics||||||
845|Back Creek Group|24241|5|Briefly described|p18|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
845|Back Creek Group|24615|5|Briefly described|CD|Permian|Permian|[Pb].  Predominantly massive, cleaved mudstone and siltstone (commonly with concretions), minor sandstone.||||||
845|Back Creek Group|29387|6|Mentioned|Table 4|||||||||
845|Back Creek Group|29591|6|Mentioned|p96|||||||||
845|Back Creek Group|29721|6|Mentioned|p65|||||||||
845|Back Creek Group|29735|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|29964|6|Mentioned|p5|||Permian||||||
845|Back Creek Group|30449|6|Mentioned|p1|||Faunal sequence||||||
845|Back Creek Group|30450|5|Briefly described|Fig.1|||Permian age.||||||
845|Back Creek Group|30451|6|Mentioned|p49|||See also P50||||||
845|Back Creek Group|30508|6|Mentioned|p85|||No workable coal. Stratigraphic information||||||
845|Back Creek Group|30546|6|Mentioned|p107|||Correlation. Permian age||||||
845|Back Creek Group|30696|4|Described|Table 3|||Lower-Upper Permian age||||||
845|Back Creek Group|30698|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|30699|6|Mentioned|p53|||Early to late Permian||||||
845|Back Creek Group|30701|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|31079|6|Mentioned|p5|||||||||
845|Back Creek Group|31116|6|Mentioned|p11|||||||||
845|Back Creek Group|31401|6|Mentioned|p30|||||||||
845|Back Creek Group|31656|4|Described|Table 1|||Permian||||||
845|Back Creek Group|31659|6|Mentioned|Table 2|||Correlation||||||
845|Back Creek Group|31690|5|Briefly described|p36|||Refers Derrington et al. (1959)||||||
845|Back Creek Group|31979|4|Described|Table 1|||See also Table 2. L.-U.Perm.||||||
845|Back Creek Group|31983|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|31984|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|32141|6|Mentioned|p154|||||||||
845|Back Creek Group|32193|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
845|Back Creek Group|32276|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|32493|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
845|Back Creek Group|32496|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
845|Back Creek Group|32556|4|Described|Table 3|||L.-U.Perm.||||||
845|Back Creek Group|32577|4|Described|p23|||Early & Late Perm.||||||
845|Back Creek Group|32797|6|Mentioned|p10|||||||||
845|Back Creek Group|32840|6|Mentioned|p6|||||||||
845|Back Creek Group|32944|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|33090|4|Described|Table 3|||Permian||||||
845|Back Creek Group|33091|5|Briefly described|p8|||Stratigraphy||||||
845|Back Creek Group|33094|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|33390|6|Mentioned|p3|||On Table.||||||
845|Back Creek Group|33451|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|33774|3|Fully described|p33|||Map.||||||23-SEP-08
845|Back Creek Group|34138|6|Mentioned|Cor.Chart|||Sakmarian - Kazanian||||||
845|Back Creek Group|34314|4|Described|Table 2|||L.- U.Permian. See also pp10,12.||||||03-SEP-18
845|Back Creek Group|34331|6|Mentioned|p458|||L.- U.Permian||||||
845|Back Creek Group|34389|4|Described|Table 2|||Permian.||||||
845|Back Creek Group|34390|4|Described|Table 2|||Permian||||||
845|Back Creek Group|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
845|Back Creek Group|34480|6|Mentioned|p489|||Lower, Upper Permian. See also P492||||||
845|Back Creek Group|34574|5|Briefly described|p115|||Lower part 260 my. Correlation||||||
845|Back Creek Group|34613|4|Described|p8|||Permian||||||
845|Back Creek Group|35008|6|Mentioned|p178|||||||||
845|Back Creek Group|35141|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|35266|6|Mentioned|p190|||||||||
845|Back Creek Group|35426|3|Fully described|p653|||||||||
845|Back Creek Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
845|Back Creek Group|35811|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|35822|6|Mentioned|p40|||||||||
845|Back Creek Group|35873|6|Mentioned|p2|||||||||
845|Back Creek Group|35940|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|36103|6|Mentioned|p145|||||||||
845|Back Creek Group|36241|6|Mentioned|p115|||||||||
845|Back Creek Group|36570|6|Mentioned|p77|||||||||
845|Back Creek Group|36739|2|Defined|p1|Permian|Permian|||||||
845|Back Creek Group|36925|4|Described|p179|||||||||
845|Back Creek Group|37070|6|Mentioned|p69|||||||||
845|Back Creek Group|37071|4|Described|p83|||||||||
845|Back Creek Group|37075|5|Briefly described|Table 1|||||||||
845|Back Creek Group|37076|6|Mentioned|p119|||||||||
845|Back Creek Group|37079|6|Mentioned|p137|||||||||
845|Back Creek Group|37121|5|Briefly described|Table 1|||||||||
845|Back Creek Group|37138|6|Mentioned|p94|||||||||
845|Back Creek Group|37565|6|Mentioned|p7|||||||||
845|Back Creek Group|37612|6|Mentioned|Fig.1|||See also P282||||||
845|Back Creek Group|37749|6|Mentioned|p184|||||||||
845|Back Creek Group|37858|6|Mentioned|p82|||||||||
845|Back Creek Group|37859|6|Mentioned|p68|||||||||
845|Back Creek Group|38081|5|Briefly described|Table 1|||||||||
845|Back Creek Group|38153|6|Mentioned|p368|||||||||
845|Back Creek Group|38204|4|Described|p71|||||||||
845|Back Creek Group|38365|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|38447|6|Mentioned|Map legend|Late Permian|Early Permian|Late Permian to Early Permian||||||
845|Back Creek Group|38518|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|39212|5|Briefly described|p10|||Coal deposits. p24 gas reservoir. See also p23.||||||03-SEP-18
845|Back Creek Group|39220|6|Mentioned|p43|||See also P44||||||
845|Back Creek Group|39252|6|Mentioned|Fig.13|||||||||
845|Back Creek Group|39260|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39261|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|39264|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39267|6|Mentioned|p232|||||||||
845|Back Creek Group|39268|6|Mentioned|p269|||||||||
845|Back Creek Group|39269|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39445|6|Mentioned|Table 8|||||||||
845|Back Creek Group|39494|6|Mentioned|Fig.5|||||||||
845|Back Creek Group|39943|6|Mentioned|Table 6A|||||||||
845|Back Creek Group|40030|6|Mentioned|Fig.5|||||||||
845|Back Creek Group|40093|3|Fully described|p26|||||||||
845|Back Creek Group|40094|6|Mentioned|p22|||||||||
845|Back Creek Group|40096|6|Mentioned|p2|||||||||
845|Back Creek Group|40249|6|Mentioned|p41|||||||||
845|Back Creek Group|40544|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|40571|4|Described|p31|||||||||
845|Back Creek Group|40574|5|Briefly described|p4|||||||||
845|Back Creek Group|40623|5|Briefly described|p80|||Briefly described p104.||||||03-SEP-18
845|Back Creek Group|40675|6|Mentioned|p306|||Mention Table 6A||||||
845|Back Creek Group|40767|6|Mentioned|p17|||||||||
845|Back Creek Group|40968|4|Described|p277|||||||||
845|Back Creek Group|41034|5|Briefly described|p366|||||||||
845|Back Creek Group|41188|5|Briefly described|p231|||||||||
845|Back Creek Group|41191|6|Mentioned|p283|||||||||
845|Back Creek Group|41210|5|Briefly described|Fig.3|||||||||
845|Back Creek Group|41246|6|Mentioned|Map legend|Permian||||||||
845|Back Creek Group|41247|6|Mentioned|Fig.7|||||||||
845|Back Creek Group|41290|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|41666|6|Mentioned|p1|||||||||
845|Back Creek Group|41725|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|41809|6|Mentioned|p63|||||||||
845|Back Creek Group|41922|4|Described|Table 1, P8|||||||||
845|Back Creek Group|41923|6|Mentioned|p21|||||||||
845|Back Creek Group|42091|6|Mentioned|p289|||||||||
845|Back Creek Group|42250|6|Mentioned|p26|||||||||
845|Back Creek Group|42258|4|Described|p275|||||||||
845|Back Creek Group|42463|6|Mentioned|Fig.5 P172|||||||||
845|Back Creek Group|42547|5|Briefly described|p46|||||||||
845|Back Creek Group|42614|5|Briefly described|p13|||Bowen Basin||||||
845|Back Creek Group|42634|5|Briefly described|Table 2 P10|||||||||
845|Back Creek Group|42641|6|Mentioned|p108|||||||||
845|Back Creek Group|42701|4|Described|p60|||||||||
845|Back Creek Group|42932|5|Briefly described|Fig.15|||||||||
845|Back Creek Group|42994|6|Mentioned|p263|||||||||
845|Back Creek Group|43000|4|Described|p107|||||||||
845|Back Creek Group|43002|5|Briefly described|Fig.2,p135|||||||||
845|Back Creek Group|43003|5|Briefly described|p168|||||||||
845|Back Creek Group|43017|5|Briefly described|Fig.2,p374|||||||||
845|Back Creek Group|43050|6|Mentioned|p55|||||||||
845|Back Creek Group|43099|5|Briefly described|p10|||||||||
845|Back Creek Group|43204|5|Briefly described|Map Legend|Late Permian|Late Permian|Clermont Basin||||||23-DEC-11
845|Back Creek Group|43213|5|Briefly described|p10, p74, p158-159, p239|Permian|Permian|Bowen Basin. Marine and transitional deposits, containing marine fossils and ice-rafted dropstones.|||Includes Blenheim Subgroup.|Overlies Bathampton Metamorphics and Greybank Volcanics.|Quartzose sandstone, quartzose pebble conglomerate.|
845|Back Creek Group|43474|14|Not recorded|p6,fig.2,22,68|Kazanian|Artinskian|||||||
845|Back Creek Group|43582|6|Mentioned|p28|||||||||
845|Back Creek Group|43714|6|Mentioned|p30|||||||||
845|Back Creek Group|43861|5|Briefly described|25, 28||Permian|||||||
845|Back Creek Group|43883|14|Not recorded|p18 Fig.4-3|||||||||
845|Back Creek Group|43982|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43988|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|43990|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43991|14|Not recorded|p46,50||Permian|Consists of several formations basal oneis Cracow Limestone, overlain by Gyranda Formation.||||||
845|Back Creek Group|43994|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43995|14|Not recorded|Table p9|Permian|Carboniferous|Comprises Mount Steel Formation, Passion Hill Formation, Acacia Formation, Orange Creek Formation, Oxtrack Formation.||||||
845|Back Creek Group|43998|4|Described|p6,11,12,18,map|Late Permian|Early Permian|=Middle Bowen Beds||||||
845|Back Creek Group|44000|14|Not recorded|p57|||||||||
845|Back Creek Group|44022|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|44118|14|Not recorded|Map Legend||Late Permian|||||||
845|Back Creek Group|44169|14|Not recorded|Tb.1,p6-8,map|||||||||
845|Back Creek Group|44170|4|Described|p6-8,12,22,29,31,35|Late Permian|Early Permian|Tb.1,map.||||||
845|Back Creek Group|44218|14|Not recorded|p17-19|Kazanian|Artinskian|||||||
845|Back Creek Group|44242|14|Not recorded|p14|||||||||
845|Back Creek Group|44245|5|Briefly described|Map Legend||Permian|||||||
845|Back Creek Group|44331|14|Not recorded|Map Legend|Late Permian|Early Permian|||||||
845|Back Creek Group|44381|14|Not recorded|p5,8,9|||||||||
845|Back Creek Group|44390|14|Not recorded|p16||Permian|||||||
845|Back Creek Group|44409|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|44419|14|Not recorded|p272||Permian|||||||
845|Back Creek Group|44424|14|Not recorded|p293-301|||||||||
845|Back Creek Group|44426|14|Not recorded|p11|||Equivalent of Middle Bowen Beds.||||||
845|Back Creek Group|44490|14|Not recorded|p48|||Fossils.||||||
845|Back Creek Group|44514|2|Defined|p27,28|||Contains Mount Steel Formation, Passion Hill Formation, Acacia Formation, Orange Creek Formation, Oxtrack Formation.||||||
845|Back Creek Group|44571|2|Defined|p204-205,207|||Overlies Camboon Andesite.||||||
845|Back Creek Group|44618|14|Not recorded|p511||Permian|Ref. to Malone et al. 1965||||||
845|Back Creek Group|44635|4|Described|p6-8,12,22,29,31,35,||Permian|Tb.1,map. Includes: Blenheim, Gebbie and Tiverton Formations.||||||
845|Back Creek Group|44640|14|Not recorded|p31|||||||||
845|Back Creek Group|44697|14|Not recorded|p91|||||||||
845|Back Creek Group|45031|14|Not recorded|p6-11, Fig.3||Permian|||||||
845|Back Creek Group|45043|14|Not recorded|p244||Permian|||||||
845|Back Creek Group|45071|6|Mentioned|p25|||||||||
845|Back Creek Group|45073|6|Mentioned|p58|||Geological history||||||
845|Back Creek Group|45095|6|Mentioned|p8|||||||||
845|Back Creek Group|45110|3|Fully described|Table 14|||See also Fig.5 and p24.||||||10-DEC-07
845|Back Creek Group|45151|5|Briefly described|Table 10|||See also Table 11 and p15.||||||03-SEP-18
845|Back Creek Group|48600|14|Not recorded|p8|||||||||
845|Back Creek Group|48881|14|Not recorded|p1,12,14,24-26,28,|||p33-4,45,48.  =Middle Bowen Beds.||||||
845|Back Creek Group|48898|2|Defined|p30|Late Permian|Early Permian|Lower - Upper Permian. See also pp1,2,7,8 etc.||||||10-DEC-07
845|Back Creek Group|48900|6|Mentioned|p84|||Table opposite. Lower - Upper Permian.||||||
845|Back Creek Group|48919|6|Mentioned|Table 3|||||||||
845|Back Creek Group|48922|4|Described|Table 2|||L.-U.Perm.||||||
845|Back Creek Group|49644|5|Briefly described|Table|||||||||
845|Back Creek Group|50213|5|Briefly described|Map legend|Permian|Permian|Includes Moah Creek beds, Boomer Formation and unnamed sediments.||||||
845|Back Creek Group|50214|5|Briefly described|Map Legend|Permian|Permian|Includes the Buffel Formation.||||||17-MAY-04
845|Back Creek Group|50215|5|Briefly described|Map Legend|Late Permian|Early Permian|Includes Barfield and Flat Top Formations and the Gyranda Subgroup (Wiseman and Banana Formations).||||||18-JUN-09
845|Back Creek Group|50273|5|Briefly described|Map legend|Late Permian|Early Permian|Includes: Buffel, Oxtrack, Barfield and Flat Top Formations.||||||18-MAY-04
845|Back Creek Group|50301|5|Briefly described|Map Legend|Late Permian|Early Permian|Includes: Buffel Formation, Oxtrack Formation, Barfield Formation, Flat Top Formation.||||||
845|Back Creek Group|50317|5|Briefly described|Map Legend|Permian|Permian|Includes Moah Creek beds.||||||09-JUN-04
845|Back Creek Group|50597|5|Briefly described|Map Legend|Permian|Permian|Undivided sedimentry rocks.||||||
845|Back Creek Group|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Overlies: Rookwood Volcanics, Mount Benmore Volcanics. Underlies: Duaringa Formation.||||||30-JUN-04
845|Back Creek Group|60115|5|Briefly described|p21 Fig. 1|Late Permian|Early Permian|Includes the Blair Athol Coal Measures. Geological Province: Bowen Basin and Comet Ridge.||||||04-FEB-08
845|Back Creek Group|60282|6|Mentioned|p6, p23|||Undivided only in this sheet area.  Passes laterally in to the Barfield Formation in the BANANA region.  References mostly made to Undivided Back Creek Group.||||||12-APR-05
845|Back Creek Group|60386|6|Mentioned|p296|Artinskian|Artinskian|Shown as Back CK GRP, Bowen/Sydney Basin. Deltaic - nearshore - shelf.||||||
845|Back Creek Group|60445|5|Briefly described|p6. p18, p25|||Consists of calcareous sandstone and mudstone. Intruded by Bundarra Granodiorite. Overlies Carmila beds.||||||16-MAY-06
845|Back Creek Group|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Exmoor Formation, Blenheim Formation, Gebbie Formation, Tiverton Formation.||||||
845|Back Creek Group|60475|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Predominantly massive, cleaved mudstone and siltstone, minor lithic sandstone.||||||
845|Back Creek Group|60479|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Predomiantly massive, cleaved mudstone and siltstone (commonly with concretions), minor lithic sandstone.||||||29-SEP-04
845|Back Creek Group|60480|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Boomer Formation, Yatton Limestone.||||||
845|Back Creek Group|60481|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Boomer Formation.||||||
845|Back Creek Group|60557|5|Briefly described|p20 Fig. 5c, p25|||Much of the outcrop of this unit west of the Fitzroy River was previously mapped as the Rannes beds.  Contains the Boomer Formation and Moah Creek beds.  Geological Province: Bowen Basin.||||||09-JUN-05
845|Back Creek Group|60659|5|Briefly described|p20|Late Permian|Early Permian|Includes Tiverton, Gebbie, Blenheim and Exmoor Formations. Geological Province: Bowen Basin.||||||07-FEB-11
845|Back Creek Group|61035|4|Described|p11, p15, p42, p68|Permian|Permian|Unconformably overlain by Styx Coal Measures. Geological Province: Bowen Basin. General lithology consists of sandstone, mudstone + subordinate carbonates, lower part is mudstone-dominated sequence.||||||07-FEB-11
845|Back Creek Group|61377|5|Briefly described|p150|Late Permian|Early Permian|Two lithologies: lower (marine) shale, sltst, minor sst, limest, coal (parts fossiliferous); upper (marginal marine to non-marine) dominantly sst, minor shale and sltst. Unconformable on Kuttung Fm; conformable below Kianga Fm.||||||07-FEB-11
845|Back Creek Group|61612|6|Mentioned|p270 Fig. 1|Late Permian|Early Permian|Includes Blair Athol Coal Measures. Geological Province: Bowen Basin.||||||13-MAR-09
845|Back Creek Group|61777|5|Briefly described|p224|||Sedimentary rocks.||||||07-FEB-11
845|Back Creek Group|61832|5|Briefly described|p187|Permian|Permian|Mudstone, sandstone, limestone. Geological Province: Bowen Basin.||||||
845|Back Creek Group|61917|5|Briefly described|Map legend|Late Permian|Early Permian|`||||||16-MAR-06
845|Back Creek Group|64197|6|Mentioned|p630 Fig.7|Permian|Permian|||||Underlies the Blackwater Group; overlies the Reids Dome Beds.||
845|Back Creek Group|64665|6|Mentioned|p62.|||Styx Basin.||||Is overlain unconformably by Styx Coal Measures.||
845|Back Creek Group|64855|6|Mentioned|p33|||Taroom Trough. Age information not given but implied to be Permian.||||||22-FEB-10
845|Back Creek Group|64859|6|Mentioned|p195, 196, 225|Permian|Permian|Gas source rocks.||||||
845|Back Creek Group|65003|6|Mentioned|p34|||||||||
845|Back Creek Group|65119|5|Briefly described|Fig 2 p503, Table 1 p504, fig 7-8,16-19|Late Permian|Early Permian|Bowen Basin. Carbon shale interbedded with coal, sandstone and siltstone. Tuffaceous siltstone and shale, tuff and sandstone. Upper part up to 2934 m thick. Lower part up to ~90m thick. Age: 251-268 Ma (form Fielding , 1990). Fission Track age: ~106-138 Ma.||||||03-SEP-18
845|Back Creek Group|65388|4|Described|p159-191, p20, 26, 27, 28, 31, 33, 35|Kungurian|Asselian|Bowen Basin. Name first used by Derrington and others (1959) and Derrington and Morgan (1960) for the Permian succession in the Cracow-Theodore area. Includes Buffel Formation, Yatton Limestone, Pindari, Oxtrack, Barfield, Flat Top, Boomer Formations. Previously mapped partly as Rannes beds and partly as Boomer Formation. Includes brachiopod and other fossils. Cleaved mudstones. Overlies Carmila beds, Mount Benmore Volcanics. Intruded by microsyenite at Mount Bora. Intruded by unnamed gabbro. See also pages 48, 55, 70, 74, 76,77, 84, 85, 106, 110, 138, 141, 144, 232, 339, 432-433, 437, 438, 439, 441, 446, 447.||||||
845|Back Creek Group|65706|4|Described|p11, p12; Tb.1 p14,15,16|Late Permian|Early Permian|Bowen Basin. Parts of this unit probably equivalent to Carmila beds and Calen Coal Measures; possibly unconformable on Lizzie Creek Volcanic Group.|||Includes Collinsville Coal Measures, Tiverton Formation, Gebbie Formation and Blenheim Formation.|Conformably underlies Blackwater Group.|Quartzose to lithic sandstone, siltstone, mudstone, carbonaceous shale, calcareous sandstone and siltstone, conglomerate, coal, limestone and sandy coquinite.|
845|Back Creek Group|66084|5|Briefly described|Map legend|Permian|Permian|Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.||||||
845|Back Creek Group|66086|5|Briefly described|Map legend|Permian|Permian|Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.||||||
845|Back Creek Group|66188|6|Mentioned|443,fig 17|Late Permian|Early Permian|Bowen Basin||||||
845|Back Creek Group|66615|6|Mentioned|p3, p4 Fig.2, p5 Fig.3, p7 Fig.4, p8, p9|||Bowen Basin. Overlies Early Permian Volcanics.||||||
845|Back Creek Group|67133|6|Mentioned|p2, p5, p8, p19|||Samples of this unit were analysed by XRD and optical microscopy for this study. Early to Middle Permian.|||Peawaddy Formation.|||
845|Back Creek Group|67402|6|Mentioned|p19 fig WSD3, WSD4|Early Permian|Early Permian|Bowen Basin. Potential seal or reservoir for carbon dioxide storage. See also p43 tbl HPB1, p48 fig BWS1, p50 fig BWS4, p53, p55, p56 tbl BWS2, p57, p61, p62, p80, p80 tbl BWN1, p82-p84, p144, p165 tbl LPB1. |||Includes the Tiverton Formation, Gebbie Formation, Collinsville Coal Measures, Blenheim Formation, Exmoor Formation|||
845|Back Creek Group|67669|5|Briefly described|p11|Late Permian|Early Permian|Of Bowen Basin.||||Overlain by Black Water Group.||
845|Back Creek Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Is overlain by Blackwater Group.||
845|Back Creek Group|68004|5|Briefly described|p67, p173.|Late Permian|Early Permian|Gunnedah-Bowen Basin. Initial deposits of this unit were in graben structures formed during an Early Permian rift phase. Later deposits occurred during a phase of thermal subsidence. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows. Unlike early deposits, upper parts have excellent reservoir potential. See also reference to Back Creek Formation p175.|||||Sandstones interbedded with (marine) shales.|
845|Back Creek Group|68006|6|Mentioned|p79.|Permian|Permian|Has good quality reservoir sandstones, prospective for petroleum.||||||
845|Back Creek Group|68008|5|Briefly described|p156-157, p292|||Formerly the Rannes beds.||||Overlies, and elsewhere is thrust under, Rookwood Volcanics.||
845|Back Creek Group|68359|5|Briefly described|p3, p7-10, p14-16, p18, p21-24, App.3, 8|Late Permian|Early Permian|Strathmuir Synclinorium, Bowen Basin. Gives high U-Th-K radiometric responses. Early to Late Permian. Predominantly marine to shallow-marine facies. Exhibits a "hot" radiogenic signature on ternary radiometric images: may be a suitable heat source for geothermal energy. The higher heat production value is attributed to radiogenic altered siltstone and claystone beds. Detailed lithologies and photographs of core; detailed lithology and geophysics log; thermal profile and heat flow model.||||Unconformably overlies Glenprairie beds. Is overlain by Styx Coal Measures.|Dominantly massive cleaved mudstone and minor lithic sandstone. Bioturbation common.|05-MAR-19
845|Back Creek Group|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin|||Includes Black Alley Shale, Peawaddy Formation, Colinlea Sandstone, Reids Dome beds.|Overlain unconformably by Blackwater Group. Underlain unconformably by Joe Joe Group.|Mudstone, siltstone, tuff, sandstone, coquinite, minor conglomerate, shale, and coal.|
845|Back Creek Group|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.|||Includes Black Alley Shale, Peawaddy Formation, Colinlea Sandstone.|Overlain by the Blackwater Group. Underlain by the Joe Joe Group.|Mudstone, sandstone, siltstone, coquinite, tuff and minor conglomerate.|
845|Back Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||Is overlain conformably by Blackwater Group.||
845|Back Creek Group|68679|5|Briefly described|p308, p311-313, p338, p343-344, p346-347|Permian|Permian|See also p349, p351, p353, p355, p357-360, p364, p373-374 Figs.5.66-68, p380, p419, p469. Bowen Basin. At its eastern margin, the Marlborough Province has been thrust over this Group during the Hunter-Bowen Orogeny. RELATED UNITS (continued): Is folded with and thrust against Leura Volcanics. Is thrust against and probably overlies Goodedulla beds.|||Barfield, Blenheim, Gebbie, Tiverton Formations; Moonlight Sandstone.|Overlies Mount Benmore Volcanics, Reids Dome beds. Is overlain by Blackwater Group. Is thrust under Rookwood Volcanics. Abuts the Carmila beds. Equivalent to Moah Creek beds. See COMMENTS  for more.||
845|Back Creek Group|68731|6|Mentioned|p173 Fig 3.85|||||||||
845|Back Creek Group|68900|6|Mentioned|p4|Permian|Permian|Drummond Basin.||||||
845|Back Creek Group|68901|6|Mentioned|p2 Fig i|Permian|Permian|||||||26-SEP-18
845|Back Creek Group|69379|5|Briefly described|map legend|Permian|Permian||||Colinlea Sandstone|||
845|Back Creek Group|69582|5|Briefly described|p57, p60|||Connors Arch. Thermal conductivity and geothermal energy potential are discussed. Intersected in GSQ St Lawrence 1.||||Conformably overlies the Carmila beds. Overlain by the Styx Coal Measures.|Massive cleaved mudstone and lithic sandstonee, deposited within a predominantly shallow marine environment.|
845|Back Creek Group|69594|6|Mentioned|p550|Permian|Permian|||||Is onlapped by the Styx Coal Measures.||
845|Back Creek Group|69599|5|Briefly described|p635|Permian|Permian|In the Nebo area, is intruded by Mount Bora.||||||
845|Back Creek Group|69681|6|Mentioned|p82|||||||||
845|Back Creek Group|69952|6|Mentioned|p75|Permian|Permian|||||||
845|Back Creek Group|70673|6|Mentioned|p9|Permian|Permian|||||||
845|Back Creek Group|70815|6|Mentioned|p3|||Bowen Basin.||||||
845|Back Creek Group|70856|5|Briefly described|Map Legend|Permian|Permian||||Includes Reids Dome beds, Cattle Creek Formation, Aldebaran Sandstone.|||
845|Back Creek Group|70857|5|Briefly described|Map Legend|Permian|Permian||||Includes Colinlea Sandstone, Peawaddy Formation, Black Alley Shale|Overlies Joe Joe Group, overlain by Blackwater Group||
845|Back Creek Group|71264|6|Mentioned|p581 Fig.4|Permian|Permian|Bowen Basin.||||||
845|Back Creek Group|72297|6|Mentioned|p700|||||||Is overlain unconformably by the Styx Coal Measures.||
845|Back Creek Group|73036|5|Briefly described|Map legend|Late Permian|Early Permian||||Includes Exmoor Formation, Blenheim Formation, Gebbie Formation, Tiverton Formation.||Quartzose to sublabile sst, siltst, mudst, rare limestone. Carbonaceous + micaceous labile sst, siltst, shale, coquinite, minor conglomerate. Quartzose to lithic ssst, sandy siltst, siltst, carbonaceous shale, calcareous sst + siltst; fossiliferous.|
845|Back Creek Group|73037|5|Briefly described|Map legend|Late Permian|Early Permian||||Exmoor Formation, Blenheim Formation, Gebbie Formation and Tiverton Formation||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73038|5|Briefly described|Map legend|Late Permian|Early Permian||||Includes Exmoor Formation.||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73040|5|Briefly described|Map legend|Late Permian|Early Permian||||||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73246|6|Mentioned|p189-190|Upper Permian|Lower Permian|Bowen Basin.|||Blenheim Subgroup, Exmoor Formation, German Creek Formation, Gebbie Subgroup, Collinsville Coal Measures, Tiverton Subgroup|Overlain by Blackwater Group including Moranbah Coal Measures and Fair Hill Formation.|Mudstone, sandstone, limestone and coal.|
845|Back Creek Group|73450|6|Mentioned|p55-56, p106|Permian|Permian|Bowen Basin.||||||
870|Badu Granite|23421|4|Described|Table 5.3 p164.|Early Permian|Late Carboniferous|Intrudes Torres Strait Volcanic Group and Horn Island Granite.  Of Badu Suite. Age: K-Ar 294+/-4Ma (Hawkesbury) 293+/-5Ma (Clarke Island) 302+/-5Ma (Madaduan PNG) 286+/-3Ma (Hammond Isl.)||||||
870|Badu Granite|23431|5|Briefly described|p536|||Also see p537.||||||
870|Badu Granite|30582|6|Mentioned|p9|||Carboniferous age.||||||
870|Badu Granite|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
870|Badu Granite|31528|6|Mentioned|p34|||||||||
870|Badu Granite|32564|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
870|Badu Granite|33771|6|Mentioned|p799|||||||||
870|Badu Granite|33876|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
870|Badu Granite|33877|4|Described|Table 1|||Upper Carboniferous.||||||19-AUG-08
870|Badu Granite|33880|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
870|Badu Granite|33883|4|Described|p12|||||||||
870|Badu Granite|34582|2|Defined|p530|Permian|Permian|See also p535, Table 1Probably Permian.||||||19-AUG-08
870|Badu Granite|36130|6|Mentioned|Fig.5|||||||||
870|Badu Granite|37614|4|Described|p240|||||||||
870|Badu Granite|39445|5|Briefly described|Table 12|||||||||
870|Badu Granite|39670|6|Mentioned|Fig.6|||||||||
870|Badu Granite|41272|5|Briefly described|M 1of1 C01|||See also M 1of1 E01||||||
870|Badu Granite|42547|5|Briefly described|p76|||||||||
870|Badu Granite|43567|5|Briefly described|p402||Late Carboniferous|||||||
870|Badu Granite|45076|6|Mentioned|p17|||U.Carb.  See also P40.||||||
870|Badu Granite|45144|6|Mentioned|p12|||||||||
870|Badu Granite|69593|5|Briefly described|p477 Tb.6.2|||Torres Strait region: Jardine Subprovince, Kennedy Igneous Association.||Badu Suite.||||
870|Badu Granite|72983|6|Mentioned|p5, p61|Artinskian|Gzhelian|Jardine Subprovince, Kennedy Igneous Association. Considered broadly co-magmatic with the Torres Strait Volcanic Group.|285-300 Ma K-Ar|||||
1007|Balnagowan Volcanic Member|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Doonside Formation.||||||
1007|Balnagowan Volcanic Member|24615|5|Briefly described|CD|Carboniferous|Devonian|[DCcd/b].  Basaltic to andesitic lava and volcaniclastic rocks, felsic volcaniclastic rocks, chert, mudstone, limestone.||||||
1007|Balnagowan Volcanic Member|41922|3|Fully described|Table 1 P11|||||||||
1007|Balnagowan Volcanic Member|42143|6|Mentioned|p592|||||||||
1007|Balnagowan Volcanic Member|42660|4|Described|App.3.2 p169|||Of Doonside Formation||||||
1007|Balnagowan Volcanic Member|42901|5|Briefly described|p404|||of Doonside Formation||||||
1007|Balnagowan Volcanic Member|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the  Doonside Formation (Curtis Island Group).||||||
1007|Balnagowan Volcanic Member|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Doonside Formation (Curtis Island Group)||||||
1007|Balnagowan Volcanic Member|60557|5|Briefly described|p23|Carboniferous|Devonian|Of the Doonside Formation (Curtis Island Group).||||||09-JUN-05
1007|Balnagowan Volcanic Member|68008|5|Briefly described|p4, p113, p166, p426, p465|Early Carboniferous|Devonian|||Doonside Formation.||Is intruded by Targinie Quartz Monzonite and Mount Hedlow Trachyte.||
1007|Balnagowan Volcanic Member|68679|4|Described|p318, p424|Mississippian|Devonian|Willmott, O'Flynn and Trezise (1986) applied this name to rocks now mapped as Chalmers Formation (Berserker Group); the name was later (Donchak and Holmes, 1991) applied to rocks within the Doonside Formation, E of the Yarrol Fault in the Gladstone area. The main exposure is a NNW-trending belt 20km long and up to 3km wide, from Balnagowan homestead to Cawarral. Deep-marine.||Doonside Formation.||Is intruded by Targinie Quartz Monzonite.|Mafic to intermediate lavas and clastics including basaltic tuff with some mudstone, chert and limestone. The lavas are massive and exhibit flow margin breccias and amygdaloidal textures.|
1020|Ban Ban Ultramafic Hornfels|35520|6|Mentioned|Table 2|||Silicate analysis.||||||
1020|Ban Ban Ultramafic Hornfels|36217|6|Mentioned|p206|||Published by Ashley & others 1979.||||||
1024|Banana Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
1024|Banana Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
1024|Banana Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pwyb].  Siltstone and shale with minor tuff and sandstone and rare coal.||||||
1024|Banana Formation|30141|5|Briefly described|p134|||||||||
1024|Banana Formation|30451|6|Mentioned|Fig.8|||See also P57,60||||||
1024|Banana Formation|35426|6|Mentioned|p659|||||||||
1024|Banana Formation|36739|6|Mentioned|p19|||||||||
1024|Banana Formation|37075|5|Briefly described|Table 1|||||||||
1024|Banana Formation|40093|6|Mentioned|p33|||||||||
1024|Banana Formation|41666|6|Mentioned|Fig.1|||||||||
1024|Banana Formation|43483|6|Mentioned|14||Permian|||||||
1024|Banana Formation|43994|14|Not recorded|Map Legend|||||||||
1024|Banana Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
1024|Banana Formation|44381|14|Not recorded|p6|||||||||
1024|Banana Formation|44514|2|Defined|p27,32,33||Late Permian|Conformably overlies Flat Top Formation. Overlain by Wiseman Formation.||||||
1024|Banana Formation|44571|2|Defined|p206-207,Fig.28|||||||||
1024|Banana Formation|44573|14|Not recorded|p98|||Use of name Banana to be discontinued. Part below conglomerate = Flat Top Formation; rest = Gyranda Formation.||||||25-AUG-08
1024|Banana Formation|44626|14|Not recorded|p83|||Age not given.||||||
1024|Banana Formation|44640|14|Not recorded|p32|||||||||
1024|Banana Formation|44746|14|Not recorded|p50|||||||||
1024|Banana Formation|45071|3|Fully described|Table 10|||||||||
1024|Banana Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Gyranda Subgroup (Back Creek Group). Siltstone and shale with minor tuff and lithic sandstone and rare coal.||||||18-JUN-09
1024|Banana Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Gyranda Subgroup (Blackwater Group).  Siltstone and shale with minor tuff and volcanlithic sandstone and rare coal.||||||
1024|Banana Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
1024|Banana Formation|64856|3|Fully described|p42, p50-51, p55-61, p63, p102|Late Permian|Late Permian|Bowen Basin. Conformably overlies Flat Top Formation and onlaps the Camboon and Combarngo Volcanics.  Is overlain by Burunga Formation and transitionally by Tinowon Formation. Age from palynoflora (unit APP5). Max thickness 526m. Correlated with lower part of Gyranda Formation.| | ||||28-NOV-17
1024|Banana Formation|64857|5|Briefly described|p119-121, p113 Fig.3|Late Permian|Late Permian|Eastern Bowen Basin. Mudstone interval grading up into the Scotia Coal Member in the north-east part of the southern Taroom Trough and the lower coal interval of the Burunga Formation in the south.||||||
1024|Banana Formation|64858|5|Briefly described|p181, p180 Fig.2, p183, p186 Fig.9|Late Permian|Late Permian|Bowen Basin. Occurs directly below the Burunga Formation in the southern Taroom Trough.||||||30-NOV-09
1024|Banana Formation|64859|5|Briefly described|p196, 225|Permian|Permian|Mainly marine mudstones. Gas source rocks.||||||
1024|Banana Formation|65112|6|Mentioned|p316; Fig 4 p314|Triassic|Late Permian|Post-extension stratigraphic sequences of the Taroom Trough. Overlies Flat Top Formation, underlies Scotia Coal Member.||||||22-MAR-12
1024|Banana Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Taroom Trough. Underlies Scotia Coal Member, overlies Flat Top Formation.||||||10-NOV-09
1024|Banana Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||21-SEP-09
1024|Banana Formation|65115|5|Briefly described|p414, 416, Fig 2 p403|Kazanian|Ufimian|Mudstone siltstone. Underlies the Scotia Coal Member, overlies the Flat Top Formation in the Taroom Trough, Bowen Basin. Part of Supersequence D.||||||
1024|Banana Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Scotia Coal Member and ?overlies the Flat Top Formation in the Taroom Trough, Bowen Basin.||||||
1024|Banana Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Scotia Member, ?overlies the Flat Top Formation in the Taroom Trough, Bowen Basin.||||||
1024|Banana Formation|65119|6|Mentioned|Fig 6 p512|||Present in the Cockatoo Creek 1, Wandoan 1 and Burunga 1 Wells.||||||
1024|Banana Formation|65388|5|Briefly described|p194-195, p161 Fig. 62, p163, 193|Late Permian|Late Permian|Of Gyranda Subgroup, Blackwater Group. Conformably overlies Flat Top Formation. Conformably overlain by Wiseman Formation. Intersected in GSQ Mundubbera 5 where it is 358m thick. Consists of silty mudstone and shale with minor tuff  - a reference section (Gray and Heywood, 1978). Max thickness of 526m in UOD Cockatoo Creek 1. Dominantly olive green mudstone and siltstone and lesser medium to coarse-grained feldspatholithic sandstone.||||||
1024|Banana Formation|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
1024|Banana Formation|67402|6|Mentioned|p21, p45|Capitanian|Capitanian|Bowen Basin. ||||Overlain by the Burunga Formation. Overlies the Oxtrack Formation.||
1024|Banana Formation|68679|5|Briefly described|p353, p377, p381-382|Permian|Permian|Derrington et al. (1959). Connors-Auburn Province. Taroom Trough, Bowen Basin. 526m thick. Lake or standing brackish water.||||Overlies Flat Top Formation. Is overlain by Wiseman and Burunga Formations.|Siltstone, shale, minor tuff and sandstone, rare coal.|
1032|Bandanna Formation|13516|5|Briefly described|p145 fig 3, p146, 160,161,152-3,156,157|Late Permian|Late Permian|From Denison Trough and Roma Shelf, Bowen Basin. Age: APP5006 - APP6|||May include Kaloola Member|||
1032|Bandanna Formation|22601|6|Mentioned|415|Permian|Permian|Geol province Bowen Basin||||||
1032|Bandanna Formation|22872|6|Mentioned|p535|||||||||
1032|Bandanna Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
1032|Bandanna Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
1032|Bandanna Formation|22978|6|Mentioned|p148 Fig.1|||||||||
1032|Bandanna Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
1032|Bandanna Formation|23060|5|Briefly described|17|||Geol province Bowen Basin||||||30-NOV-09
1032|Bandanna Formation|23359|5|Briefly described|77|||||||||
1032|Bandanna Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
1032|Bandanna Formation|24069|5|Briefly described|p284|Permian|Permian|Geological Province: Surat Basin.||||||
1032|Bandanna Formation|24077|5|Briefly described|p410 Tb. 2|||||||||
1032|Bandanna Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Blackwater Group.  Age: >251Ma.  Geological Province: Bowen Basin.||||||
1032|Bandanna Formation|24616|6|Mentioned|p35|||Geological Province: Bowen Basin.||||||
1032|Bandanna Formation|29387|6|Mentioned|Table 3|||Upper Permian.||||||
1032|Bandanna Formation|29391|6|Mentioned|Table 3|||See P18 & also Table 4 on P19.||||||
1032|Bandanna Formation|29393|6|Mentioned|Table 2|||Permian.||||||
1032|Bandanna Formation|29409|6|Mentioned|Table 1|||Equated with Rangal Coal Measures and upper part Burngrove Fm.||||||
1032|Bandanna Formation|29410|6|Mentioned|p273|||Testing for coal seams, Correlation diagram P275.||||||
1032|Bandanna Formation|29411|5|Briefly described|p201|||||||||
1032|Bandanna Formation|29721|6|Mentioned|Table 65|||||||||
1032|Bandanna Formation|30340|6|Mentioned|Table 3|||||||||
1032|Bandanna Formation|30341|6|Mentioned|p136|||Upper Permian age||||||
1032|Bandanna Formation|30508|6|Mentioned|p85|||No significant coal seams||||||
1032|Bandanna Formation|30545|6|Mentioned|Fig.2|||Tatarian||||||
1032|Bandanna Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
1032|Bandanna Formation|30826|6|Mentioned|Fig.1.|||||||||
1032|Bandanna Formation|30854|6|Mentioned|p8|||Refers Hill (1957)||||||
1032|Bandanna Formation|30915|6|Mentioned|p99|||||||||
1032|Bandanna Formation|30916|6|Mentioned|p98|||On table||||||
1032|Bandanna Formation|31084|6|Mentioned|p13|||See also P13, 21. Upper Permian||||||
1032|Bandanna Formation|31116|6|Mentioned|p11|||||||||
1032|Bandanna Formation|31120|4|Described|p153|||||||||
1032|Bandanna Formation|31121|6|Mentioned|p388|||||||||
1032|Bandanna Formation|31122|6|Mentioned|p352|||||||||
1032|Bandanna Formation|31258|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|31260|6|Mentioned|p16|||Facies analysis||||||
1032|Bandanna Formation|31303|5|Briefly described|p292|||See also Table 1||||||
1032|Bandanna Formation|31305|4|Described|p570|||Mention Table 1||||||
1032|Bandanna Formation|31369|4|Described|p26|||U.Permian||||||
1032|Bandanna Formation|31860|6|Mentioned|p277|||See also P282||||||
1032|Bandanna Formation|32139|6|Mentioned|p579|||||||||
1032|Bandanna Formation|32577|6|Mentioned|p24|||U.Perm.||||||
1032|Bandanna Formation|32578|6|Mentioned|p352|||Late Perm. Refers Power (1967)||||||
1032|Bandanna Formation|32689|6|Mentioned|Fig.2|||Refers Power (1967)||||||
1032|Bandanna Formation|32712|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|32729|6|Mentioned|p37|||Coal seams in drill holes||||||
1032|Bandanna Formation|32837|6|Mentioned|p170|||Refers Paten (1969)||||||
1032|Bandanna Formation|32840|6|Mentioned|Fig.1|||Stratigraphy & biostratigraphy. See also P31||||||
1032|Bandanna Formation|33059|4|Described|Table 1|||U.Perm.||||||
1032|Bandanna Formation|33366|6|Mentioned|Fig.3|||Perm.||||||
1032|Bandanna Formation|33368|4|Described|p10|||Map. Well log P.12. See also P13.||||||
1032|Bandanna Formation|33369|6|Mentioned|p214|||Jericho No.1. Strat. succession.||||||
1032|Bandanna Formation|33372|5|Briefly described|p21|||Correlative described from wells.||||||
1032|Bandanna Formation|33530|5|Briefly described|Table 1|||Upper Permian||||||
1032|Bandanna Formation|33675|4|Described|p412|||Lithology.||||||
1032|Bandanna Formation|33701|6|Mentioned|Fig.1|||Tatarian.||||||
1032|Bandanna Formation|33786|6|Mentioned|p17|||||||||
1032|Bandanna Formation|34132|6|Mentioned|p2|||Upper Permian||||||
1032|Bandanna Formation|34133|6|Mentioned|p28|||||||||
1032|Bandanna Formation|34212|6|Mentioned|p2|||Permian. See also P3.||||||
1032|Bandanna Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
1032|Bandanna Formation|35079|6|Mentioned|p424|||||||||
1032|Bandanna Formation|35148|4|Described|p414|||See also Table 1.||||||
1032|Bandanna Formation|35266|6|Mentioned|p192|||||||||
1032|Bandanna Formation|35457|4|Described|p633|||Also Fig.4 biostratigraphic relationships.||||||
1032|Bandanna Formation|35562|6|Mentioned|Table 5|||Biostratigraphy||||||
1032|Bandanna Formation|35845|6|Mentioned|Fig.25|||||||||
1032|Bandanna Formation|35873|6|Mentioned|p127|||||||||
1032|Bandanna Formation|35901|6|Mentioned|p1|||||||||
1032|Bandanna Formation|36103|4|Described|Table 1|||||||||
1032|Bandanna Formation|36104|6|Mentioned|p122|||||||||
1032|Bandanna Formation|36172|6|Mentioned|Appendix|||||||||
1032|Bandanna Formation|36233|5|Briefly described|p157|||See also Table 1.||||||
1032|Bandanna Formation|36241|4|Described|p125|||||||||
1032|Bandanna Formation|36243|6|Mentioned|Table 3A|||||||||
1032|Bandanna Formation|36739|6|Mentioned|p5|||||||||
1032|Bandanna Formation|36921|4|Described|p184|||See also Table 1.||||||
1032|Bandanna Formation|37065|6|Mentioned|p34|||||||||
1032|Bandanna Formation|37070|4|Described|p74|||||||||
1032|Bandanna Formation|37072|6|Mentioned|p91|||||||||
1032|Bandanna Formation|37074|3|Fully described|p105|||||||||
1032|Bandanna Formation|37450|6|Mentioned|p374|||||||||
1032|Bandanna Formation|37451|6|Mentioned|Table 2|||||||||
1032|Bandanna Formation|37610|5|Briefly described|p302|||See also Fig.4.||||||
1032|Bandanna Formation|37705|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|37724|6|Mentioned|p122|||||||||
1032|Bandanna Formation|37726|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|37858|6|Mentioned|p85|||||||||
1032|Bandanna Formation|37918|6|Mentioned|p474|||||||||
1032|Bandanna Formation|38092|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|38198|6|Mentioned|p414|||||||||
1032|Bandanna Formation|38312|4|Described|p463|||||||||
1032|Bandanna Formation|38603|6|Mentioned|p81|||||||||
1032|Bandanna Formation|38955|4|Described|p315|||||||||
1032|Bandanna Formation|38958|5|Briefly described|p493|||||||||
1032|Bandanna Formation|39212|6|Mentioned|p13|||||||||
1032|Bandanna Formation|39219|6|Mentioned|p46|||Microflora||||||
1032|Bandanna Formation|39252|5|Briefly described|p20|||See also P26||||||
1032|Bandanna Formation|39253|6|Mentioned|p34|||Mooga NL1 Well. See also P36||||||
1032|Bandanna Formation|39261|6|Mentioned|Fig.6|||See also Fig.9||||||
1032|Bandanna Formation|39263|6|Mentioned|Fig.1|||||||||
1032|Bandanna Formation|39264|6|Mentioned|Fig. 4|||||||||
1032|Bandanna Formation|39266|6|Mentioned|p225|||||||||
1032|Bandanna Formation|39272|6|Mentioned|p295|||||||||
1032|Bandanna Formation|39273|6|Mentioned|Fig. 2|||||||||
1032|Bandanna Formation|39275|5|Briefly described|p327|||||||||
1032|Bandanna Formation|39412|6|Mentioned|p1|||||||||
1032|Bandanna Formation|39423|6|Mentioned|Fig.1|||||||||
1032|Bandanna Formation|39445|5|Briefly described|Table 8|||||||||
1032|Bandanna Formation|39478|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|39494|6|Mentioned|Fig.5|||||||||
1032|Bandanna Formation|39611|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|39708|6|Mentioned|p477|||||||||
1032|Bandanna Formation|39813|6|Mentioned|Map legend|Permian|Carboniferous|Permo Carboniferous||||||
1032|Bandanna Formation|39815|6|Mentioned|Fig.10|||||||||
1032|Bandanna Formation|39942|6|Mentioned|p465|||||||||
1032|Bandanna Formation|39943|6|Mentioned|Table 5A|||||||||
1032|Bandanna Formation|40030|6|Mentioned|Fig.5|||||||||
1032|Bandanna Formation|40123|6|Mentioned|p465|||See also Fig.2||||||
1032|Bandanna Formation|40176|6|Mentioned|Table II|||||||||
1032|Bandanna Formation|40249|6|Mentioned|p41|||||||||
1032|Bandanna Formation|40250|6|Mentioned|Table 6|||||||||
1032|Bandanna Formation|40539|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|40540|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|40544|6|Mentioned|Fig.6|||||||||
1032|Bandanna Formation|40635|6|Mentioned|p39|||||||||
1032|Bandanna Formation|40675|6|Mentioned|Table 5B|||||||||
1032|Bandanna Formation|40687|6|Mentioned|Table 3|||||||||
1032|Bandanna Formation|40832|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|41116|4|Described|p432|||Briefly described Table 1||||||
1032|Bandanna Formation|41159|6|Mentioned|p340|||||||||
1032|Bandanna Formation|41173|6|Mentioned|p88|||||||||
1032|Bandanna Formation|41198|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|41225|6|Mentioned|p36|||||||||
1032|Bandanna Formation|41246|6|Mentioned|Map legend|Permian||||||||
1032|Bandanna Formation|41247|6|Mentioned|Fig.7|||||||||
1032|Bandanna Formation|41330|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|41474|6|Mentioned|p63|||||||||
1032|Bandanna Formation|41605|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|41666|6|Mentioned|p26|||||||||
1032|Bandanna Formation|41689|6|Mentioned|Table 1|||||||||
1032|Bandanna Formation|41707|6|Mentioned|p166|||||||||
1032|Bandanna Formation|41710|6|Mentioned|p222|||||||||
1032|Bandanna Formation|41725|6|Mentioned|Fig.2|||||||||
1032|Bandanna Formation|42008|6|Mentioned|p270|||||||||
1032|Bandanna Formation|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
1032|Bandanna Formation|42091|6|Mentioned|p284|||||||||
1032|Bandanna Formation|42187|6|Mentioned|p319|||||||||
1032|Bandanna Formation|42249|6|Mentioned|p23|||||||||
1032|Bandanna Formation|42250|6|Mentioned|Fig.4 P31|||||||||
1032|Bandanna Formation|42251|6|Mentioned|Fig.2 P38|||||||||
1032|Bandanna Formation|42254|6|Mentioned|p221|||||||||
1032|Bandanna Formation|42256|6|Mentioned|Fig.1 P243|||||||||
1032|Bandanna Formation|42309|6|Mentioned|p289|||||||||
1032|Bandanna Formation|42437|6|Mentioned|Fig.3 P822|||||||||
1032|Bandanna Formation|42446|6|Mentioned|p1|||||||||
1032|Bandanna Formation|42447|6|Mentioned|Fig. 2|||||||||
1032|Bandanna Formation|42474|6|Mentioned|p25|||||||||
1032|Bandanna Formation|42641|5|Briefly described|p109|||||||||
1032|Bandanna Formation|42648|6|Mentioned|p40|||||||||
1032|Bandanna Formation|42662|6|Mentioned|p84 Fig.4|||||||||
1032|Bandanna Formation|42856|5|Briefly described|Fig.2 P632|||||||||
1032|Bandanna Formation|42911|5|Briefly described|p11|||||||||
1032|Bandanna Formation|42999|5|Briefly described|Table 1,p90||Late Permian|||||||
1032|Bandanna Formation|43000|5|Briefly described|p113|||see also Fig.5,p112||||||
1032|Bandanna Formation|43017|5|Briefly described|Fig.3,p375|||||||||
1032|Bandanna Formation|43050|5|Briefly described|Fig.1,p5|||||||||
1032|Bandanna Formation|43105|5|Briefly described|p13|||||||||
1032|Bandanna Formation|43114|6|Mentioned|Table 2|||||||||
1032|Bandanna Formation|43185|5|Briefly described|6,10||Late Permian|||||||
1032|Bandanna Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
1032|Bandanna Formation|43812|6|Mentioned|Fig.3,p145|||||||||
1032|Bandanna Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
1032|Bandanna Formation|43917|14|Not recorded|p30,32|||||||||
1032|Bandanna Formation|43919|14|Not recorded|p41|||||||||
1032|Bandanna Formation|43977|14|Not recorded|p576,580|||||||||
1032|Bandanna Formation|43987|14|Not recorded|p269-271|||||||||
1032|Bandanna Formation|43995|14|Not recorded|Tb.p9,23,53,55,|Permian|Carboniferous|Figs.6,14||||||
1032|Bandanna Formation|44023|6|Mentioned|Tb.2|||||||||
1032|Bandanna Formation|44033|14|Not recorded|p3,Tb.1|||Correlated with Upper Permian sediments.||||||
1032|Bandanna Formation|44085|2|Defined|p4,11-13,15,17|||||||||
1032|Bandanna Formation|44091|14|Not recorded|p45|||Part of Upper Bowen Group in Springsure area.||||||
1032|Bandanna Formation|44096|2|Defined|Fig.26,p186-8,193|||||||||
1032|Bandanna Formation|44115|14|Not recorded|p17-21|||||||||
1032|Bandanna Formation|44116|14|Not recorded|p24|||||||||
1032|Bandanna Formation|44169|14|Not recorded|p6-8,11-13,Tb.1,map|Late Permian|Early Permian|||||||
1032|Bandanna Formation|44170|4|Described|p5,6,11,12,26,30-32||Late Permian|Tb.1,Tb.3||||||
1032|Bandanna Formation|44172|2|Defined|Tb.1,p1330,1334,1339||Tatarian|p133||||||
1032|Bandanna Formation|44218|14|Not recorded|p19|Tatarian|Kazanian|||||||
1032|Bandanna Formation|44219|14|Not recorded|p31|Tatarian|Kazanian|||||||
1032|Bandanna Formation|44243|14|Not recorded|p647||Late Permian|||||||
1032|Bandanna Formation|44421|14|Not recorded|p6,8,9||Permian|||||||
1032|Bandanna Formation|44422|14|Not recorded|p150,152||Early Permian|||||||
1032|Bandanna Formation|44577|14|Not recorded|p136-138|||||||||
1032|Bandanna Formation|44609|14|Not recorded|p66|||||||||
1032|Bandanna Formation|44610|14|Not recorded|p47,49|||||||||
1032|Bandanna Formation|44618|14|Not recorded|p511,513,517,518||Permian|Overlain by Rewan Formation and underlain by MacMillan Formation.||||||
1032|Bandanna Formation|44651|14|Not recorded|p117,123|||||||||
1032|Bandanna Formation|44701|14|Not recorded|p10|||||||||
1032|Bandanna Formation|44787|14|Not recorded|Tb.p123-25,diag.p127|||||||||
1032|Bandanna Formation|44855|14|Not recorded|p27|||||||||
1032|Bandanna Formation|44913|14|Not recorded|p53, Fig.1||Permian|||||||
1032|Bandanna Formation|45006|14|Not recorded|p6|||||||||
1032|Bandanna Formation|45031|14|Not recorded|p9,Fig.3||Permian|||||||
1032|Bandanna Formation|45095|6|Mentioned|Table 2|||Refers Hill (1957)||||||
1032|Bandanna Formation|45110|6|Mentioned|p52|||||||||
1032|Bandanna Formation|46849|6|Mentioned|p192|||||||||
1032|Bandanna Formation|46949|6|Mentioned|p97|||||||||
1032|Bandanna Formation|46989|5|Briefly described|Table 1|||||||||
1032|Bandanna Formation|48600|14|Not recorded|p13|||Springsure area.||||||
1032|Bandanna Formation|48606|14|Not recorded|p11,13,14,22,Pl.12|||(H/55-8, G/55-12).||||||
1032|Bandanna Formation|48626|14|Not recorded|p3,23-29,31,51,55,92||Permian|Fig.1,2,Pl.1. Overlain by Rewan Formation.||||||
1032|Bandanna Formation|48630|14|Not recorded|p1,4-6,17,18,20,21,|||Pls.1,2.||||||
1032|Bandanna Formation|48845|14|Not recorded|p38|||||||||
1032|Bandanna Formation|48847|14|Not recorded|p1,9,10|||Appears to contain both Middle Bowen Beds and Upper Bowen Coal Measures.||||||
1032|Bandanna Formation|48900|6|Mentioned|p39|||Upper Permian.||||||
1032|Bandanna Formation|48908|6|Mentioned|p8|||||||||
1032|Bandanna Formation|48919|6|Mentioned|p17|||||||||
1032|Bandanna Formation|48920|6|Mentioned|p87|||Palynology||||||
1032|Bandanna Formation|48995|6|Mentioned|Fig.3|||||||||
1032|Bandanna Formation|60115|5|Briefly described|p22|||Geological Province: Bowen Basin - in the Comet Ridge area. Contains key target coals for coal seam gas.||||||04-FEB-08
1032|Bandanna Formation|60286|4|Described|p277|Late Permian|Late Permian|Overlies Black Alley Shale. Alluvial plain. Geological Province: Bowen Basin.||||||
1032|Bandanna Formation|61232|6|Mentioned|p119 Tb.1, |||||||||
1032|Bandanna Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
1032|Bandanna Formation|61617|6|Mentioned|p346 Tb. 3|||Net coal thickness: 9m. Geological Province: Bowen Basin.||||||
1032|Bandanna Formation|62357|5|Briefly described|p524 Fig. 7|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
1032|Bandanna Formation|62921|6|Mentioned|p878 Fig.2|Changhsingian|Wuchiapingian|SE Galilee Basin.||Unit in Blackwater Group.||||
1032|Bandanna Formation|63832|6|Mentioned|p131 fig 2|Lopingian|Lopingian|Of Galilee Basin and west Bowen Basin.||||||
1032|Bandanna Formation|63978|5|Briefly described|p7|||Geological province: Denison Trough. Contact between this unit and the Rewan Group represents the traditional lithostratigraphic location of the Permo-Triassic boundary.||||||07-FEB-11
1032|Bandanna Formation|64099|5|Briefly described|p374 Fig 5|Permian|Permian|Underlies Sagittarius Sandstone. Geol Prov: Bowen Basin.||||||
1032|Bandanna Formation|64288|5|Briefly described|p532 Fig.1 |Changhsingian|Wuchiapingian|||||Overlies Black Alley Shale.||
1032|Bandanna Formation|64631|5|Briefly described|p44 Fig.2, p48 Fig.4.|Changhsingian|Wuchiapingian|Galilee and Bowen Basins. Biostratigraphic age control for base and top.||||Overlies Black Alley Shale.||
1032|Bandanna Formation|64665|6|Mentioned|p53 Fig.2, p56.|Late Permian|Late Permian|Galilee Basin. This unit is an extension of the upper parts of the Betts Creek beds, contiguous across the Springsure Shelf.||||||
1032|Bandanna Formation|64856|3|Fully described|p41-42, 62, p64 Fig.13, p66-71, p102|Late Permian|Late Permian|Hill (1957), after Bandanna homestead near Carnarvon Gorge. The lower part was excised and named the Black Alley Shale by Mollan et al. (1969). Bowen Basin. Overlies Black Alley Shale gradationally or, when absent, the Tinowon Formation. Overlain by Rewan Group. Datum for the top of the Permian. Top part correlated with Baralaba Coal Measures; lower part with Burunga Formation. Age from palynoflora (APP5, APP6). Max thick 173m. Mudstone, siltstone, sandstone and coal.| | ||||28-NOV-17
1032|Bandanna Formation|64857|5|Briefly described|p121-124, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Coaly formation overlying the Black Alley Shale.||||||
1032|Bandanna Formation|64858|6|Mentioned|p182, p181 Tb.1, p180 Fig.2, p186 Fig.11|Late Permian|Late Permian|Bowen Basin. Includes coal.||||||30-NOV-09
1032|Bandanna Formation|64859|5|Briefly described|p196, 226|Permian|Permian|Terrestrial coals, mudstones and sandstones. Minor gas source rocks.||||||
1032|Bandanna Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Denison Trough, Bowen Basin. Underlies Rewan Group and overlies Black Alley Shale.||||||14-SEP-09
1032|Bandanna Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Denison Trough. Overlies the Black Alley Shale.||||||
1032|Bandanna Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||21-SEP-09
1032|Bandanna Formation|65115|5|Briefly described|p418, 420, 421, Fig 2 p403, Fig 14 p421|Permian|Permian|Deltaic-fluvial coal measures. Underlies the Rewan Group in the Denison Trough in the Bowen Basin. Part of Supersequence F.||||||
1032|Bandanna Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Rewan Group in the Denison Trough of the Bowen Basin, overlies Black Alley Shale.||||||
1032|Bandanna Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Rewan Group in the Bowen Basin. Overlies Black Alley Shale, Denison Trough.||||||
1032|Bandanna Formation|65119|6|Mentioned|p526|Late Permian|Late Permian|Unit in Blackwater Group. With Baralaba Coal Measures, is the principal producer of liquid hydrocarbons in the Bowen and Surat Basins.||||||07-MAR-12
1032|Bandanna Formation|66188|6|Mentioned|431, Fig 3,17|Early Triassic|Late Permian |Correlative of Betts Creek Beds.||||||
1032|Bandanna Formation|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p5-8|||Denison and Southern Taroom Trough, Bowen Basin.||||||
1032|Bandanna Formation|67323|5|Briefly described|p84|Permian|Permian|Eastern Galilee Basin.||||Correlated with Betts Creek beds.||
1032|Bandanna Formation|67365|5|Briefly described|p83.|Late Permian|Late Permian|Is worked at the Fairview CSG field, 120 km north of Roma. High gas content (10-15 m3 per tonne). CSG is also extracted from these seams at Spring Gully gas field, where the seams have good gas contents and high permeabilities.||||||
1032|Bandanna Formation|67402|4|Described|p18 fig WSD2, p21, p23 fig CTM3|Wuchiapingian|Wuchiapingian|Bowen Basin. Deposited in a fluvial-deltaic environment. Generally <100m thick but may be up to 150m thick. Poor suitability for carbon dioxide storage or sealing due to poor reservoir quality. See also p45, p48, p50 fig BWS4, p52, p53-p57, p62, p64 fig BWW2, p65, p66 fig BWW4, p69, p72, p73, p124 fig GLL1, p125, p131 fig GLL12, p132, p134 fig GLL17, p136, p141, p272, p273. ||||Overlain by the Rewan Group. Overlies the Black Alley Shale.|Mudstone, siltstone, lithic sandstone, coal and tuff.|
1032|Bandanna Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Rewan Formation. Underlain by Black Alley Shale/Winnathoola CM. Equivalent to Rangal and Baralaba CM.||
1032|Bandanna Formation|68139|6|Mentioned|p32|Permian|Permian|Bowen Basin. Group 5 coals. Hosts coal seam gas-producing fields.||||||
1032|Bandanna Formation|68202|6|Mentioned|p176|Permian|Permian|Bowen Basin. Appears as Bundarra Formation.||||||
1032|Bandanna Formation|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-10, p13, p16 Tb.4|Lopingian|Lopingian|See also p17-19. Galilee Basin. Deposited on a coastal alluvial plain by a fluvio-deltaic system. Galilee Basin stratigraphic cross-sections, and mineralogy tables.|||||Laminated to massively bedded labile sandstone, interbedded with mudstones and siltstones.|
1032|Bandanna Formation|68576|5|Briefly described|Q_4: p3|Early Triassic|Early Triassic|Bowen Basin.||||Unconformably overlies Black Alley Shale. Is overlain ?unconformably by Rewan Group.||
1032|Bandanna Formation|68679|5|Briefly described|p377, p381, p383-384|Permian|Permian|Mollan et al. (1969). Bowen Basin. 370m thick. Non-marine fluvio-deltaic deposits: a delta system developed in a freshwater lake. Properties of the coal are described in some detail.||||Overlies Black Alley Shale. Is overlain by Rewan Group.|Fine- to coarse-grained feldspatholithic sandstone, siltstone, mudstone, carbonaceous mudstone, coal, oil shale.|
1032|Bandanna Formation|68731|5|Briefly described|p201 Fig 3.110|Early Triassic|Early Triassic|(Swarbrick 1974; Gray 1976; Allen and Fielding 2007). Deposited under paludal/lacustrine/fluviatile conditions.||||||09-MAY-16
1032|Bandanna Formation|69582|6|Mentioned|p66|||Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Colinlea Sandstone. Overlain by the Hutton Sandstone.|Sandstone.|
1032|Bandanna Formation|70815|6|Mentioned|p3-4, 6-7, 11|||Bowen Basin. Vitrinite reflectance values mapped.||||||
1032|Bandanna Formation|70837|5|Briefly described|p242,245|Triassic|Lopingian|Of Bowen Basin. U-Pb tuff date of 252.2+\-0.4 Ma from the top of the formation (Mundil etal., 2006), corresponding to P. microcorpus zone. Correlates to Base of APP6 (Changhsingian; See p244 Fig 3).|||Includes Kaloola member.|||
1032|Bandanna Formation|70878|5|Briefly described|p717-718, p720-721, p725-726|Permian|Permian|Bowen Basin. Age range from Kaloola Member. Calibration of palynological ages (D.parvithola Zone). The top of this unit marks the top of the Permian.|254.1+/-0.09 Ma - 252.54+/-0.04 Ma.||Kaloola Member.|Overlies Black Alley Shale. Is overlain unconformably by Rewan Formation.||
1032|Bandanna Formation|71265|5|Briefly described|p587, p589-590, p592, p599-607|Induan|Induan|Bowen and Galilee Basins. Represents a southerly-prograding fluvial-deltaic system during late-Lopingian regression. The tuffaceous lower section was reassigned as Burngrove Formation (equivalent) by Phillips et al. (2017). Highly variable lithology across the Basin. Sedimentary logs of CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Overlies Burngrove Formation. Is overlain by Rewan Group / Rewan Formation.|Massive to thickly bedded labile sandstone interbedded with mudstones and siltstones. Distinguished by a sharp decrease in volcanic ash layers.|
1032|Bandanna Formation|71276|3|Fully described|p284-298|Lopingian|Lopingian|Vine et al. (1965). Eastern, and central western, margins of the Galilee Basin. This unit is stated to have largely replaced the Blackwater Group (Mollan et al., 1969) which itself replaced the Cheshire Formation (Schneeberger, 1952). The type locality is on the Springsure Shelf. Deltaic (sometimes called paludal) deposits. Coal seam correlation. Overlies "Fort Cooper Coal Measures equivalent" and "Fair Hill Formation equivalent".||Blackwater Group.||Conformably overlies Burngrove Formation and Black Alley Shale. Is overlain unconformably by Rewan Formation. Correlative of Betts Creek beds.|Contains four major coal seams. Commonly contains calcareous minerals as well as minor illite, hematite and zeolite.|
1032|Bandanna Formation|71278|5|Briefly described|p322|Permian|Permian|Hill (1957). Apart from this sole occurrence, this unit appears throughout the article as Bandanna Coal Formation (p319-320, p322-323).|||||Grey to dark grey mudstone and siltstone beds, white fairly sorted sandstone and bituminous coal.|
1032|Bandanna Formation|71701|4|Described|p155-p158, p168-p169|Changhsingian|Changhsingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin. Also overlies the Burngrove Formation equivalent (informal unit). Intersected in CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Overlies the Black Alley Shale.||
1032|Bandanna Formation|71710|6|Mentioned|p367, 370, 381, 386|||Geological province: southern Galilee Basin. Lacustrine to paludal.||||Equivalent to the upper Betts Creek beds of the Galilee Basin.||
1032|Bandanna Formation|72088|4|Described|p8, p16, p18, p20-p21|Changhsingian|Changhsingian|Southern Galilee Basin and Bowen Basin. Deposited under paludal, lacustrine and fluvial conditions. Coal development is variable with the proportion of coal being substantially less near the western edge of the Springsure Shelf than near Moray Downs. Named for Bandanna Homestead in the Arcadia Valley south of Rolleston. The type area occurs on the Springsure Shelf at "the headwater of Rewan Home Creek, 3 miles south of Rewan Station". See also p38-p40, p43, p65, p68-p69, p91.||||Overlies the Colinlea Sandstone. Overlain by the Rewan Group.|Interbedded sandstone, siltstone, mudstone and coal.|
1032|Bandanna Formation|72297|5|Briefly described|p694-695, p697, p744, p750-752|Permian|Permian|SW Bowen Basin. Petroleum source from coals; also CSG in the Fairview and Spring Gully fields.||||Correlative of Betts Creek beds.|Includes antracite, and exceptionally rich oil shale in layers up to 1.5m thick.|
1032|Bandanna Formation|73113|5|Briefly described|p. 1, 19-20, 22-24, 26, 28-32, 37-38...|||Bowen Basin. Uppermost coal seam gas reservoir in the basin. Percentage coal varies from <5 % to 30%, mean ~14%. Coal seams average <2 m thick but may be up to 8 m thick. Better lateral continuity of coal seams than in the Walloon Coal Measures. Groundwater model divided the unit into a non-productive zone and upper and lower layers. Interbedded aquitard. More locations: p. 41, 49, 51-52, 59, 62, 88, 97-98, 100-101, 103-105, 107-108, 117, 119, 123-124, 127, 132, 134, 143, 146-148, 150, 152-154, 162, 165, 167, 169-170, 172, 174-175, 178-179, 191-196.||||Overlain by Rewan Group and unconformably by Precipice Sandstone.|Coal interbedded with fine-grained sandstone, mudstone and siltstone.|
1032|Bandanna Formation|73163|5|Briefly described|p467-468, p470-474, p476|Lopingian|Lopingian|Galilee Basin, Bowen Basin. Youngest Lopingian formation on the Springsure Shelf and equivalent to the upper part of the Betts Creek Group. Contains the A coal seam. Youngest single grain detrital zircon age of 233+/-13 Ma is problematic (too young), as is the youngest grouping (248.6 +/- 1.9 Ma) because overlying coal seam includes Dulhuntispora parvithola - index taxa for  Lopingian APP5 zone. Characteristised by restricted range of detrital zircon ages, felsic volcanic rocks of the New England Orogen are considered the primary contributor of detrital zircons.|c. 253-251.9 Ma|Betts Creek Group||Conformably overlies the 'Burngrove Formation equivalent'.Top equivalent to Yarrabee Tuff.|Sandstone, siltstone, coal seam. Highly variable composition, quartz is the major constituent, plagioclase and K-feldspar are common, includes zeolite.|
1032|Bandanna Formation|73304|5|Briefly described|p65, p71-73, p76, p78|Changhsingian|Changhsingian|Bowen Basin. [Top?] boundary marks a major extinction of peat-producing plants. Age from a tuff at the top of the unit. Method not stated.|252.2 +/- 0.4 Ma||Kaloola Member|||
1032|Bandanna Formation|73472|6|Mentioned|p115-116|Changhsingian|Changhsingian|Galilee Basin.||||Underlain by Black Alley Shale. Overlain by Rewan Group. Equivalent to Betts Creek beds.||
1032|Bandanna Formation|73625|5|Briefly described|p1-3, p5 Fig.3, p7, 12, 14, 18, 20-23|Permian|Permian|See also p25-26. Denison Trough, Bowen Basin. Graphic sedimentary logs. Extensive coastal plain to estuarine environments. One of the most economically important coal-bearing successions in Queensland. Basal and top boundaries detailed. Contains the Basin's final expression of the Glossopteris flora. Palaeoenvironmental changes detailed.|254-252.2 Ma.|||Overlies Black Alley Shale. Is overlain by  'Marker Mudstone' and Arcadia Formation (Rewan Group). Equivalent to Rangal and upper Baralaba Coal Measures.|Interbedded sandstones and mudrocks with common coal beds; abundant in situ plant roots; conglomerates and pebbly sandstones abundant in SW and SE margins of the Basin. Local thin tuff beds.|
1078|Baralaba Coal Measures|13516|5|Briefly described|p145 fig 3, p157|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5005 - APP6||||||
1078|Baralaba Coal Measures|22439|5|Briefly described|p15, Fig.2|Late Permian|Late Permian|Geological province: Taroom Trough, Bowen Basin.||||||25-AUG-08
1078|Baralaba Coal Measures|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|23003|5|Briefly described|p423 Table 1|Permian|Permian|Of the Blackwater Group.||||||26-AUG-08
1078|Baralaba Coal Measures|23004|5|Briefly described|p431 Table 1|Permian|Permian|Of the Blackwater Group.||||||26-AUG-08
1078|Baralaba Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
1078|Baralaba Coal Measures|23359|6|Mentioned|77|||||||||
1078|Baralaba Coal Measures|24159|5|Briefly described|p147|Late Permian|Late Permian|Parent: Blackwater Group. Geological Province: Bowen Basin.||||||
1078|Baralaba Coal Measures|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pwb].  Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate, tuff.||||||
1078|Baralaba Coal Measures|29411|5|Briefly described|p201|||||||||
1078|Baralaba Coal Measures|29723|6|Mentioned|p17|||||||||
1078|Baralaba Coal Measures|29727|6|Mentioned|p455|||||||||
1078|Baralaba Coal Measures|30137|4|Described|p2|||Upper Permian age.||||||
1078|Baralaba Coal Measures|30140|6|Mentioned|p2|||Upper Permian age||||||
1078|Baralaba Coal Measures|30141|5|Briefly described|p135|||||||||
1078|Baralaba Coal Measures|30448|6|Mentioned|p100|||||||||
1078|Baralaba Coal Measures|30451|3|Fully described|p62|||See also p63,64||||||26-AUG-08
1078|Baralaba Coal Measures|30460|6|Mentioned|p3|||See also P16,18,22,24,27. Fig.2||||||
1078|Baralaba Coal Measures|30546|6|Mentioned|p107|||Upper Permian age. Correlation||||||
1078|Baralaba Coal Measures|30743|3|Fully described|p21|||See also p22-34. Refers Reid (1944), Goscombe (1968)||||||26-AUG-08
1078|Baralaba Coal Measures|30916|6|Mentioned|p98|||||||||
1078|Baralaba Coal Measures|31079|6|Mentioned|p5|||See also Fig. 6||||||
1078|Baralaba Coal Measures|31088|6|Mentioned|p398|||||||||
1078|Baralaba Coal Measures|31116|4|Described|p11|||Upper Permian.||||||26-AUG-08
1078|Baralaba Coal Measures|31261|6|Mentioned|p518|||||||||
1078|Baralaba Coal Measures|31380|6|Mentioned|p131|||Refers Rigby(1972)||||||
1078|Baralaba Coal Measures|31391|6|Mentioned|p34|||See also P36.U.Permian||||||
1078|Baralaba Coal Measures|31531|6|Mentioned|Table 1|||U.Permian||||||
1078|Baralaba Coal Measures|31647|6|Mentioned|p354|||||||||
1078|Baralaba Coal Measures|31649|6|Mentioned|p57|||||||||
1078|Baralaba Coal Measures|32832|6|Mentioned|p4||Permian|||||||
1078|Baralaba Coal Measures|32834|6|Mentioned|p26|||See also Table 3||||||
1078|Baralaba Coal Measures|32835|6|Mentioned|p1|||Flora||||||
1078|Baralaba Coal Measures|32840|6|Mentioned|p10|||||||||
1078|Baralaba Coal Measures|32944|6|Mentioned|Fig.3|||Permian||||||
1078|Baralaba Coal Measures|33128|4|Described|p50|||Geochemistry. See also p52 and Figs. 2 and 5.||||||26-AUG-08
1078|Baralaba Coal Measures|33363|5|Briefly described|p115|||Upper Permian.||||||25-AUG-08
1078|Baralaba Coal Measures|33711|6|Mentioned|Table 3|||||||||
1078|Baralaba Coal Measures|33774|3|Fully described|p38|||Map||||||
1078|Baralaba Coal Measures|34094|5|Briefly described|p1-4,Figs.2,3,4||Late Permian|||||||
1078|Baralaba Coal Measures|34095|5|Briefly described|p3-6,26,Figs.5,6||Late Permian|||||||
1078|Baralaba Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
1078|Baralaba Coal Measures|34235|6|Mentioned|p92|||||||||
1078|Baralaba Coal Measures|34574|6|Mentioned|p115|||||||||
1078|Baralaba Coal Measures|35138|6|Mentioned|Fig.2-3|||||||||
1078|Baralaba Coal Measures|35266|6|Mentioned|p192|||||||||
1078|Baralaba Coal Measures|35426|3|Fully described|p659|||||||||
1078|Baralaba Coal Measures|35873|4|Described|p12|||||||||
1078|Baralaba Coal Measures|35901|6|Mentioned|p2|||||||||
1078|Baralaba Coal Measures|35937|6|Mentioned|p619|||||||||
1078|Baralaba Coal Measures|36172|6|Mentioned|Appendix|||||||||
1078|Baralaba Coal Measures|36241|6|Mentioned|p130|||||||||
1078|Baralaba Coal Measures|36243|6|Mentioned|Table 4A|||||||||
1078|Baralaba Coal Measures|36327|6|Mentioned|p8|||||||||
1078|Baralaba Coal Measures|36333|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|36739|6|Mentioned|p19|||||||||
1078|Baralaba Coal Measures|36825|6|Mentioned|p19|||||||||
1078|Baralaba Coal Measures|36925|6|Mentioned|Fig.1|||||||||
1078|Baralaba Coal Measures|36954|6|Mentioned|p114|||||||||
1078|Baralaba Coal Measures|37065|6|Mentioned|p32|||||||||
1078|Baralaba Coal Measures|37070|4|Described|p73|||||||||
1078|Baralaba Coal Measures|37075|5|Briefly described|Table 1|||||||||
1078|Baralaba Coal Measures|37400|6|Mentioned|Table 2|||||||||
1078|Baralaba Coal Measures|37858|6|Mentioned|p82|||||||||
1078|Baralaba Coal Measures|38153|6|Mentioned|p373|||||||||
1078|Baralaba Coal Measures|38358|6|Mentioned|p11|||||||||
1078|Baralaba Coal Measures|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|38603|6|Mentioned|p81|||||||||
1078|Baralaba Coal Measures|38951|6|Mentioned|p408|||||||||
1078|Baralaba Coal Measures|38958|5|Briefly described|p493|||||||||
1078|Baralaba Coal Measures|38971|4|Described|p543|||||||||
1078|Baralaba Coal Measures|39212|6|Mentioned|p14|||||||||
1078|Baralaba Coal Measures|39252|6|Mentioned|p26|||See also P28||||||
1078|Baralaba Coal Measures|39260|5|Briefly described|Fig.2|||||||||
1078|Baralaba Coal Measures|39261|6|Mentioned|Fig.6|||||||||
1078|Baralaba Coal Measures|39266|6|Mentioned|p221|||||||||
1078|Baralaba Coal Measures|39267|6|Mentioned|p240|||||||||
1078|Baralaba Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9.||||||25-AUG-08
1078|Baralaba Coal Measures|39777|6|Mentioned|p151|||||||||
1078|Baralaba Coal Measures|39943|6|Mentioned|Table 6A|||||||||
1078|Baralaba Coal Measures|40087|6|Mentioned|p234|||See also P237||||||
1078|Baralaba Coal Measures|40092|5|Briefly described|p51|||||||||
1078|Baralaba Coal Measures|40096|6|Mentioned|p2|||||||||
1078|Baralaba Coal Measures|40539|6|Mentioned|p164|||||||||
1078|Baralaba Coal Measures|40860|6|Mentioned|p109|||||||||
1078|Baralaba Coal Measures|41130|4|Described|p56|||||||||
1078|Baralaba Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
1078|Baralaba Coal Measures|41666|6|Mentioned|p26|||||||||
1078|Baralaba Coal Measures|41689|6|Mentioned|Table 1|||||||||
1078|Baralaba Coal Measures|42091|6|Mentioned|p284|||||||||
1078|Baralaba Coal Measures|42187|6|Mentioned|p319|||||||||
1078|Baralaba Coal Measures|42212|6|Mentioned|p329|||||||||
1078|Baralaba Coal Measures|42249|6|Mentioned|p23|||||||||
1078|Baralaba Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
1078|Baralaba Coal Measures|42251|5|Briefly described|p39|||||||||
1078|Baralaba Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
1078|Baralaba Coal Measures|42309|6|Mentioned|p257|||||||||
1078|Baralaba Coal Measures|42431|6|Mentioned|p234|||||||||
1078|Baralaba Coal Measures|42641|6|Mentioned|p115|||||||||
1078|Baralaba Coal Measures|42648|6|Mentioned|p40|||||||||
1078|Baralaba Coal Measures|42865|5|Briefly described|p18|||||||||
1078|Baralaba Coal Measures|42932|6|Mentioned|p4|||||||||
1078|Baralaba Coal Measures|43000|5|Briefly described|p113|||||||||
1078|Baralaba Coal Measures|43017|5|Briefly described|Fig.3,p375|||||||||
1078|Baralaba Coal Measures|43987|14|Not recorded|p270|||Banana-Cracow area||||||
1078|Baralaba Coal Measures|44118|14|Not recorded|Map Legend||Late Permian|||||||
1078|Baralaba Coal Measures|44129|14|Not recorded|p95-96||Permian|||||||
1078|Baralaba Coal Measures|44169|2|Defined|Tb.1,p6,8,12,map|||||||||21-DEC-11
1078|Baralaba Coal Measures|44170|2|Defined|p6,12-16,2,25,31,||Late Permian|Tb.1||||||
1078|Baralaba Coal Measures|44218|14|Not recorded|p19||Tatarian|||||||
1078|Baralaba Coal Measures|44242|14|Not recorded|p14|||||||||
1078|Baralaba Coal Measures|44243|14|Not recorded|p648-650||Late Permian|||||||
1078|Baralaba Coal Measures|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
1078|Baralaba Coal Measures|44381|14|Not recorded|p6,9|||||||||
1078|Baralaba Coal Measures|44426|14|Not recorded|p11||Late Permian|Prolific plant remains.||||||
1078|Baralaba Coal Measures|44578|14|Not recorded|p8||Late Permian|||||||
1078|Baralaba Coal Measures|44629|14|Not recorded|p560|||Cracow area. No age given.||||||
1078|Baralaba Coal Measures|44630|14|Not recorded|p493,494||Late Permian|||||||
1078|Baralaba Coal Measures|44631|14|Not recorded|p205||Late Permian|||||||
1078|Baralaba Coal Measures|44639|14|Not recorded|p56,65|||||||||
1078|Baralaba Coal Measures|44640|14|Not recorded|p30|||||||||
1078|Baralaba Coal Measures|44720|14|Not recorded|p388|||||||||
1078|Baralaba Coal Measures|44721|14|Not recorded|p28-36||Early Permian|||||||
1078|Baralaba Coal Measures|44814|14|Not recorded|p483|||||||||
1078|Baralaba Coal Measures|45031|14|Not recorded|p9||Permian|||||||
1078|Baralaba Coal Measures|45071|3|Fully described|Table 12|||||||||
1078|Baralaba Coal Measures|45095|6|Mentioned|p9|||||||||
1078|Baralaba Coal Measures|46949|6|Mentioned|Fig.3|||||||||
1078|Baralaba Coal Measures|48600|14|Not recorded|p9|||||||||
1078|Baralaba Coal Measures|48900|6|Mentioned|p84|||Table opposite.||||||
1078|Baralaba Coal Measures|48919|4|Described|p28|||See also p29.||||||25-AUG-08
1078|Baralaba Coal Measures|48947|5|Briefly described|p8|||||||||
1078|Baralaba Coal Measures|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate and tuff.||||||18-JUN-09
1078|Baralaba Coal Measures|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Blackwater Group. Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate and tuff.  Contains the Kaloola Member.||||||
1078|Baralaba Coal Measures|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Early Permian|Geological Province: Bowen Basin. Contains thickly developed coal seams up to 6m thick. Primary target for coal seam gas.||||||04-FEB-08
1078|Baralaba Coal Measures|60282|5|Briefly described|p7|||Overlie the Gyranda Formation.||||||
1078|Baralaba Coal Measures|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
1078|Baralaba Coal Measures|61617|6|Mentioned|p346 Tb. 3|||Net coal thickness: 19-35m. Geological Province: Bowen Basin.||||||11-FEB-09
1078|Baralaba Coal Measures|61782|6|Mentioned|p281|||||||||
1078|Baralaba Coal Measures|62357|5|Briefly described|p524 Fig. 7, p534|Late Permian|Late Permian|Geological Province: Bowen Basin. ||||||
1078|Baralaba Coal Measures|63713|6|Mentioned|p1523|||||||Equivalent to Bandana Formation.||
1078|Baralaba Coal Measures|64665|5|Briefly described|p52.|Late Permian|Late Permian|Bowen Basin. Low ash coal with good coking properties; high-volatile bituminous to anthracite.||||||
1078|Baralaba Coal Measures|64856|3|Fully described|p41-42, p56, p58, p60-63, p66-68, p102|Late Permian|Late Permian|Reid (1944) who later (1945) amended the name to 'Baralaba-Kianga Coal Measures' before reverting to the original form. Bowen Basin. Datum for the top of the Permian. Conformably overlies Burunga Formation. Transitional with overlying Rewan Group; locally overlain unconformably by Precipice Sandstone. Contains Kaloola Member. Age from palynoflora (APP5 and APP6). 556m thick. Sand-, silt-, mudstones; coal and tuff.| | ||||28-NOV-17
1078|Baralaba Coal Measures|64857|4|Described|p121-124, 134, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Coaly formation overlying the Wiseman Formation. Stated in article to be Permian, implied to be Late Permian because lies stratigraphically above Flat Top Formation.||||||
1078|Baralaba Coal Measures|64858|5|Briefly described|p182, p180 Fig.2, p186 Fig.11|Late Permian|Late Permian|Bowen Basin. Overlies Burunga Formation? Overlies Wiseman Formation in NE Taroom Trough.||||||30-NOV-09
1078|Baralaba Coal Measures|64859|5|Briefly described|p196, 226|Permian|Permian|Terrestrial coals, mudstones and sandstones. Minor gas source rocks.||||||
1078|Baralaba Coal Measures|65003|5|Briefly described|p2, p6, p27, p31, 32, 33-35||Permian|Of Bowen Basin. ||||Eastern equivalent of the Rangal Coal Measures. Unconformably overlain by the Rewan Formation||
1078|Baralaba Coal Measures|65112|6|Mentioned|p316; Fig 4 p314|Triassic|Late Permian|Part of Supersequence F. Unit in the Taroom Trough.||||Overlies the Burunga Formation, underlies the Rewan Group.||22-MAR-12
1078|Baralaba Coal Measures|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Taroom Trough. Overlies the Burunga Formation. Shown as Baralaba CM.||||||10-NOV-09
1078|Baralaba Coal Measures|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||21-SEP-09
1078|Baralaba Coal Measures|65115|5|Briefly described|p418, 420, Fig 2 p403|Tatarian|Tatarian|Underlies the Rewan Group in the Taroom Trough, Bowen Basin. Deltaic-fluvial coal measures. Part of Supersequence F.||||||
1078|Baralaba Coal Measures|65116|5|Briefly described|p447, Fig 2 P436|Late Permian|Late Permian|Underlies the Rewan Group and overlies the Burunga Formation in the Taroom Trough Bowen Basin.||||||
1078|Baralaba Coal Measures|65118|5|Briefly described|p483, Fig 2 p479|Permian|Permian|Underlies the Rewan Group in the Taroom Trough,Bowen Basin.||||||
1078|Baralaba Coal Measures|65119|6|Mentioned|p526, Fig 6 p512, Fig 14 p521|Late Permian|Late Permian|Unit in Blackwater Group. With Bandanna Formation, is the principal producer of liquid hydrocarbons in the Bowen and Surat Basins. Present in Flinton 1 well||||||07-MAR-12
1078|Baralaba Coal Measures|65388|4|Described|p196-198, p161 Fig. 62, p163, 193, 194|Late Permian|Late Permian|Conformably overlies Wiseman Formation of Gyranda Subgroup, Blackwater Group, Bowen Basin. Includes Kaloola Member. Top is mostly transitional with overlying Rewan Group, but unconformable in places. Palynofloras are identified with unit APP5 passing into APP6 near the top (Price, 1997). No formal type section and rocks crop out poorly. The lower 214m of the unit was intersected by GSQ Mundubbera 5 (Gray and Heywood, 1978), but there is no complete section.||||||
1078|Baralaba Coal Measures|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p6|||Southern Taroom Trough, Bowen Basin.||Of the Rewan Group ?||||
1078|Baralaba Coal Measures|67365|5|Briefly described|p83.|Late Permian|Late Permian|At Dawson Valley, contains up to 10 seams of thick, gassy coals with aggregate thickness of up to 30 m, at depths ranging from 300-1,000 m. Current (2009) CSG production of Dawson Valley operations is c.15 TJ per day. At the Peat gas field near Wandoan, 4 major coal seams with an aggregate thickness of 18.3 m produce (2009) 15 TJ per day. These same 4 seams supply CSG at the Scotia gas field to the north.||||||
1078|Baralaba Coal Measures|67402|5|Briefly described|p21, p45, p52, p57 tbl BWS3|Wuchiapingian|Wuchiapingian|Bowen Basin. Generally greater than 100m thick. See also p165 tbl LPB1, p272, p273.||||Overlain by the Rewan Group. Overlies the Burunga Formation.|Intraformational siltstones, mudstones and tuffs.|
1078|Baralaba Coal Measures|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Rewan Formation. Underlain by Gyranda Formation.||
1078|Baralaba Coal Measures|68139|6|Mentioned|p32|Permian|Permian|Bowen Basin. Group 5 coals. Hosts coal seam gas-producing fields.||||||
1078|Baralaba Coal Measures|68679|5|Briefly described|p353, p377, p381, p383-384|Permian|Permian|Mallett et al. (1983). Connors-Auburn Province. Denison Trough and Roma Shelf, Bowen Basin. 556m thick. Non-marine alluvial plain sediments. Properties of the coal are described in some detail.|||Kaloola Tuff Member.|Overlies Wiseman and Burunga Formations. Is overlain by the Rewan Group.|Fine- to medium-grained feldspatholithic sandstone, siltstone, mudstone, carbonaceous mudstone, siltstone, coal, tuff.|
1078|Baralaba Coal Measures|70330|6|Mentioned|p11 Fig.1|Late Permian|Late Permian|Bowen Basin. Appears as Rangal-Baralaba-Bandana Coal Measures.||||||
1078|Baralaba Coal Measures|70815|6|Mentioned|p3-4, 6-7, 11|||Bowen Basin. Vitrinite reflectance values mapped.||||||
1078|Baralaba Coal Measures|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin.|||Includes Kaloola member.|||
1078|Baralaba Coal Measures|70940|5|Briefly described|p844|Permian|Permian|Burunga Anticline, southern Bowen Basin.|252.5 Ma (Metcalfe et al., 2014).|Blackwater Group.||Overlies Yarrabee Tuff.||
1078|Baralaba Coal Measures|71276|6|Mentioned|p295-296|||||||Overlies Yarrabee Tuff.||
1078|Baralaba Coal Measures|72297|5|Briefly described|p694-695, p703, p744, p750|Permian|Permian|SE Bowen Basin. Numerous coal seams often split and coalesce. Indicative properties tabulated. Petroleum source, from coals. Produces structurally-trapped free CSG on the Burunga Anticline E of Wandoan, at Scotia and Peat.|||||Coal rank ranges from low-volatile bituminous to semianthracite, then decreases southwards through coking range.|
1078|Baralaba Coal Measures|73163|6|Mentioned|p468|||Bowen Basin.||||Overlies the Yarrabee Tuff.||02-FEB-22
1078|Baralaba Coal Measures|73305|6|Mentioned|p548 Fig.1|Late Permian|Late Permian|Bowen Basin. Taroom Trough, northeast.||||||
1078|Baralaba Coal Measures|73450|6|Mentioned|p55|||Bowen Basin.||||||
1078|Baralaba Coal Measures|73625|6|Mentioned|p5 Fig.3, p20-21|Permian|Permian|Eastern Bowen Basin.|||Kaloola Member.|Overlies Flat Top Formation. Is overlain by 'Marker Mudstone'/Rewan Group. Equivalent to Bandanna Formation.||
1084|Barambah Basalt|24382|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||23-DEC-09
1084|Barambah Basalt|30654|4|Described|p45|||See also P46,52,55,57-59. Pleistocene. Overlies Biggenden Beds||||||
1084|Barambah Basalt|32879|6|Mentioned|p12|||||||||
1084|Barambah Basalt|33143|6|Mentioned|p4|||Cainozoic||||||
1084|Barambah Basalt|33754|6|Mentioned|p59|||||||||
1084|Barambah Basalt|34097|6|Mentioned|p1|||U.Cainozoic||||||
1084|Barambah Basalt|38402|6|Mentioned|p73|||||||||
1084|Barambah Basalt|38403|5|Briefly described|p77|||||||||
1084|Barambah Basalt|38413|6|Mentioned|p82|||||||||
1084|Barambah Basalt|39445|5|Briefly described|Table 14|||||||||
1084|Barambah Basalt|39968|6|Mentioned|p83|||||||||
1084|Barambah Basalt|40245|6|Mentioned|Fig.6|||||||||
1084|Barambah Basalt|40475|5|Briefly described|p9|||||||||
1084|Barambah Basalt|40480|6|Mentioned|p39|||||||||
1084|Barambah Basalt|40623|5|Briefly described|p54|||Briefly described P70||||||
1084|Barambah Basalt|40919|6|Mentioned|Fig.2|||||||||
1084|Barambah Basalt|41738|6|Mentioned|p167|||||||||
1084|Barambah Basalt|42895|5|Briefly described|p76|||||||||
1084|Barambah Basalt|43008|5|Briefly described|map legend|||||||||
1084|Barambah Basalt|44750|5|Briefly described|p12,18||Pleistocene|||||||
1084|Barambah Basalt|44783|14|Not recorded|p2|||||||||
1084|Barambah Basalt|45440|4|Described|p.1,6,13,43,50|Cenozoic|Pleistocene|Tb.1. Of many pages.||||||19-NOV-08
1084|Barambah Basalt|61155|5|Briefly described|p20|Pleistocene|Pleistocene|Together with Berrembea and Hummock Basalts, overlies the Tarraran and Maroondan Melanephelinites. In the Bundaberg-Maryborough region.||||||03-MAR-10
1084|Barambah Basalt|61809|6|Mentioned|p457|Pleistocene|Pleistocene|Locally overlies all rocks in the area. Geological Province: New England Orogen.||||||
1084|Barambah Basalt|63821|5|Briefly described|p12, p26|Pleistocene|Pleistocene|Age: 600, 000 years old. Continental-derived olivine basalt.||||||07-FEB-11
1084|Barambah Basalt|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Berrembea and Hummock Basalts, are all mapped under the symbol, Qbs.||||||
1084|Barambah Basalt|69600|5|Briefly described|p669|Pleistocene|Pleistocene|Near Coalstoun Lakes, south of Bundaberg. Lava flowed from three vents; spread over a valley 3-5km wide and almost 100km long.|600 ka.||||Basalt lava flows, with lava tunnels and crater lakes.|
1093|Baree Felsite|38095|6|Mentioned|Table 6|||Informal unit.||||||
1093|Baree Felsite|38658|6|Mentioned|p153|||||||||
1093|Baree Felsite|40180|6|Mentioned|Table 1|||||||||
1093|Baree Felsite|40735|6|Mentioned|Fig.2|||||||||
1093|Baree Felsite|61147|5|Briefly described|p378 Fig.3. |||||||Overlies Arnolds Ridge Felsite.|Andesite-dacite lava.|
1113|Barmundoo Formation|42868|1|Redefined|p18||Middle Devonian|see also Fig.4 P17||||||
1113|Barmundoo Formation|42887|5|Briefly described|p257|||||||||
1113|Barmundoo Formation|61730|5|Briefly described|p1006|Early Carboniferous|Late Devonian|Forearc basin deposits originally designated as Late Silurian-Middle Devonian but now assigned a Late Devonian-earliest Carboniferous age and included as part of the Mount Alma Formation. Name is therefore no longer in use.||||||
1113|Barmundoo Formation|61761|5|Briefly described|p4, p5|Eifelian|Eifelian|Lateral equivalent of Capella Creek and Mount Holly Formations. Overlain by Mount Holly Formation (Morand, 1993a).||||||07-FEB-11
1117|Barnard Metamorphics|12575|5|Briefly described|p780, p784 Table 1.|Neoproterozoic|Neoproterozoic|Interpreted as an uplifted block of basement intruded by Ordovician granites. Separated from the Hodgkinson Province by the Russell-Mulgrave Shear. Apatite fission track analyses are detailed.|>470 Ma.|||||
1117|Barnard Metamorphics|22497|6|Mentioned|p105|||||||||
1117|Barnard Metamorphics|23422|5|Briefly described|p165|||||||||
1117|Barnard Metamorphics|23423|4|Described|p314 Table 7.4 + p226|Late Ordovician|Early Ordovician|Age: ~485 Ma, ~459 Ma, I and S-type granite. Barnard Province. Note: p314 only discusses the granitic rocks within the Barnard Metamorphics||||||23-DEC-04
1117|Barnard Metamorphics|23430|4|Described|p463-464|||Barnard Province.||||||
1117|Barnard Metamorphics|23431|6|Mentioned|p539|||||||||
1117|Barnard Metamorphics|23497|5|Briefly described|Table 1|Cambrian|Neoproterozoic|of Barnard Province. Faulted against Hodgkinson Fm rocks; cut by Tam O'Shanter, Dunk Island, and Bellenden Ker Granites, and Mission Beach Granite Complex.||||||
1117|Barnard Metamorphics|23507|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|||||||
1117|Barnard Metamorphics|23616|6|Mentioned|p82|||||||||
1117|Barnard Metamorphics|23619|6|Mentioned|p19|||||||||
1117|Barnard Metamorphics|23713|5|Briefly described|p35||Early Ordovician|Hodgkinson Province.||||||
1117|Barnard Metamorphics|30257|6|Mentioned|p106|||||||||
1117|Barnard Metamorphics|30914|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
1117|Barnard Metamorphics|31832|6|Mentioned|Table 6|||||||||
1117|Barnard Metamorphics|31999|6|Mentioned|Table 11|||||||||
1117|Barnard Metamorphics|32359|6|Mentioned|p731|||||||||
1117|Barnard Metamorphics|33220|6|Mentioned|p6|||||||||
1117|Barnard Metamorphics|36419|6|Mentioned|p395|||See also P396||||||
1117|Barnard Metamorphics|37574|6|Mentioned|Fig.6|||||||||
1117|Barnard Metamorphics|37575|4|Described|p178|||See also p183 and Fig.2.||||||17-SEP-18
1117|Barnard Metamorphics|37609|6|Mentioned|p309|||See also P311.||||||
1117|Barnard Metamorphics|37614|6|Mentioned|p230|||||||||
1117|Barnard Metamorphics|37721|6|Mentioned|Fig.1|||||||||
1117|Barnard Metamorphics|39445|5|Briefly described|Table 5|||See also p74 & p84.||||||17-SEP-18
1117|Barnard Metamorphics|39650|6|Mentioned|Fig.1|||||||||
1117|Barnard Metamorphics|39689|4|Described|p56|||||||||
1117|Barnard Metamorphics|40277|6|Mentioned|Fig.1|||||||||
1117|Barnard Metamorphics|40623|5|Briefly described|p87|||||||||
1117|Barnard Metamorphics|40787|5|Briefly described|p333|||||||||
1117|Barnard Metamorphics|41260|6|Mentioned|p125|||||||||
1117|Barnard Metamorphics|41425|6|Mentioned|p5|||||||||
1117|Barnard Metamorphics|41916|6|Mentioned|Fig.1|||||||||
1117|Barnard Metamorphics|42031|6|Mentioned|p757|||||||||
1117|Barnard Metamorphics|42407|6|Mentioned|p36|||||||||
1117|Barnard Metamorphics|42681|6|Mentioned|p12|||||||||
1117|Barnard Metamorphics|42747|5|Briefly described|p34|||||||||
1117|Barnard Metamorphics|42752|5|Briefly described|Fig.1 P44|||||||||
1117|Barnard Metamorphics|42810|5|Briefly described|p8|||||||||
1117|Barnard Metamorphics|42933|5|Briefly described|Fig.1|||||||||
1117|Barnard Metamorphics|43083|6|Mentioned|p182|||Tectonically juxtaposed against Hodgkinson Formation.||||||17-JUN-09
1117|Barnard Metamorphics|43121|5|Briefly described|Fig.1.|||||||||
1117|Barnard Metamorphics|43213|5|Briefly described|p8, p62|||Described by de Keyser (1965). Crops out along the coast near Innisfail, S of Cairns. Potential equivalent of Anakie Metamorphic Group farther south. Deformation in Late Ordovician to Early Silurian. Granite aged c.450 Ma (SHRIMP, Champion and Bultitude, 1993) intrudes the deformed rocks.|||||Includes metapsammite, metapelite, laminated greenstone and amphibolite, ultramafics and gneissic granite.|
1117|Barnard Metamorphics|43625|6|Mentioned|p71|||||||||
1117|Barnard Metamorphics|43896|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
1117|Barnard Metamorphics|43897|14|Not recorded|p91-102, Map|||Amphibolite facies equiv. of Hodgkinson Formation.||||||
1117|Barnard Metamorphics|43903|14|Not recorded|Map Legend||Mesoproterozoic|||||||
1117|Barnard Metamorphics|43927|14|Not recorded|p5-19, opp.8|||See also Lexicon||||||
1117|Barnard Metamorphics|44068|14|Not recorded|p9||Precambrian|||||||
1117|Barnard Metamorphics|44093|6|Mentioned|p129 Tb. 10.1|||||||||
1117|Barnard Metamorphics|44258|14|Not recorded|p11,23,40|||Suggested by De Keyser Middle Palaeozoic:Silurian-early Carboniferous.||||||
1117|Barnard Metamorphics|44268|14|Not recorded|p7,13,14|||||||||
1117|Barnard Metamorphics|44632|2|Defined|p78-79|||Among oldest rocks known in Queensland.||||||
1117|Barnard Metamorphics|44880|14|Not recorded|unknown (p195-208)|||||||||
1117|Barnard Metamorphics|44883|14|Not recorded|p111,112,127|||||||||
1117|Barnard Metamorphics|45025|3|Fully described|p49-51||Devonian|Devonian and possibly Late Silurian.||||||
1117|Barnard Metamorphics|45113|6|Mentioned|p118|||||||||
1117|Barnard Metamorphics|48850|14|Not recorded|p7,13,14|||||||||
1117|Barnard Metamorphics|48894|6|Mentioned|p60|||299, 310my.||||||
1117|Barnard Metamorphics|60425|5|Briefly described|p6, p13, p115|Late Ordovician|Early Ordovician|Interpreted as higher grade equivs.of Barron River Metamorphics; uplifted basement assemblage on SE margin of Hodgkinson Prov.Geol.prov: Barnard Prov. Predom'ly meta-arenite, quartzite, phyllite, etc.- detailed lith. Age: 486+/-10Ma,463+/-7Ma (SHRIMP).||||||07-FEB-11
1117|Barnard Metamorphics|62371|5|Briefly described|p470 Fig.1|Cambrian|Cambrian|Geological Province: Hodgkinson Province. See also p472 Fig.3||||||
1117|Barnard Metamorphics|63140|6|Mentioned|p570 fig 1, p572 fig 3|Cambrian|Cambrian|Hodgkinson province. Intruded by Early Ordovician S-type granites.|||||Middle to upper amphibolite facies schist and gneiss, locally migmatitic.|
1117|Barnard Metamorphics|63154|5|Briefly described|p281 Fig. 3|Cambrian|Cambrian|Age: ~540-~510Ma. Geological province: Hodgkinson Province. Intruded by S-type granites in Late Cambrian.||||||11-APR-07
1117|Barnard Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Barnard Province. This unit, as well as Babalangee Amphibolite and Cowley Ophiolite Complex, are all mapped under the symbol, -Pob.||||||
1117|Barnard Metamorphics|68731|5|Briefly described|p159, p160, p162, p163||Furongian|Barnard Province. Exhibits variations in metamorphic grade. Interpreted as higher grade equivalents of the Barron River Metamorphics. Minimum age constrained by the intrusive Tam O'Shanter Granite.|>455.7 +/- 3.6 Ma (Wormald, pers. comm., 2011).|||Extensively intruded by the Mission Beach Granite Complex and Tam O'Shanter Granite.|Comprises meta-arenite, phyllite, quartzite, greenstone, chlorite schist, quartz-muscovite schist, muscovite-chlorite and biotite-muscovite schist, gneiss, migmatitic gneiss and amphibolite.|09-MAY-16
1117|Barnard Metamorphics|69030|6|Mentioned|p6|Cambrian|Cambrian|Barnard Province.||||||
1117|Barnard Metamorphics|69592|6|Mentioned|p228, p230 Fig.4.3, p302-303|||Jones and Jones (1956). Pre-Hodgkinson Province continental crust. Occupies a discrete belt along the coast near Innisfail and on adjacent islands. Is intruded by Early Ordovician deformed granites.||||||
1117|Barnard Metamorphics|69952|5|Briefly described|p3|||Thomson Orogen. Exposed on the coast, S of Cairns. Is intruded by Ordovician granitoids aged 460-455 Ma.||||||
1117|Barnard Metamorphics|70033|4|Described|p2 Tb.i,p3 Fig i,p5,p52 Fig 8.1,p58-63|||Barnard Province. Sample lithology: amphibolite. SHRIMP U-Pb zircon age. Age shown in map legend (Fig 8.1) as Neoproterozoic - Ordovician?|451.8 +/- 2.6 Ma metamorphic/recrystallisation age|||In faulted contact to the west with the Hodgkinson Formation.|Dark greyish green, compositionally banded fine- to medium-grained amphibolite with numerous very thin to thin, irregular, pale coloured lenses and lenticles; protolith is uncertain.|03-APR-17
1117|Barnard Metamorphics|70207|4|Described|p1, p11, p52-58|||Barnard Province, Thomson Orogen. Emplaced by up-thrusting (Hunter-Bowen Orogeny) or transcurrent faulting (from Charters Towers region). Poorly exposed. Maximum depositional age; considerably younger than age of metamorphism/recrystallisation (451.8 +/- 2.6 Ma: Kositcin et al., 2015) and intrusions (~456 Ma). Tectonic intercalation of Hodgkinson and Barnard Province rocks may explain the discrepancy.|427.1 +/- 5.5 Ma (Kositcin et al., 2015).|||Is intruded by Tam O'Shanter Granite.|Multiply deformed sandstone, phyllite, quartzite, greenstone, chlorite schist, quartz-muscovite schist, muscovite-chlorite and biotite-muscovite schist, gneiss, migmatite and amphibolite. Greenschist to upper amphibolite facies.|
1117|Barnard Metamorphics|70345|6|Mentioned|p6, p27||||ca. 452 Ma (SHRIMP U-Pb)||||Amphibolite.|
1117|Barnard Metamorphics|71592|5|Briefly described|Appendix A.|||Barnard Province, Thomson Orogen.|427+/-5.5 Ma (MDA: U-Pb zircon SHRIMP)||||Schist, amphibolite.|
1117|Barnard Metamorphics|72298|6|Mentioned|p792|||Part of the basement to Quaternary sediments hosting aquifers in the Mulgrave River area.||||||
1117|Barnard Metamorphics|72983|6|Mentioned|p15|early Paleozoic|Neoproterozoic|||||||
1117|Barnard Metamorphics|73387|5|Briefly described|p2, p42-43, p46-47|||Barnard Province, Thomson Orogen. An amphibolite withinthis unit yielded a metamorphic age of 451.8 +/- 2.6 Ma (Kositcin et al., 2015). Rocks mapped as this unit at Etty Bay were reinterpreted as affiliated with the Hodgkinson Formation. Inferred to have been tectonically interleaved with the Hodgkinson Formation near Innisfail.||||||
1117|Barnard Metamorphics|73425|6|Mentioned|p16|Late Ordovician|Late Ordovician|Barnard Province, Thomson Orogen. Age of amphibolite.||||||
1117|Barnard Metamorphics|73595|6|Mentioned|p1134, 1143-1144|Silurian|Ordovician|Interpreted as either a sequence of uplifted basement rocks, or a continental ribbon rifted from the Australian continent during backarc extension and later re-accreted along the Russell-Mulgrave Fault.||||Is faulted against Hodgkinson Formation.||
1130|Barney Creek Formation|7071|5|Briefly described|p1|||Host to the giant HYC deposit. Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|14019|5|Briefly described|p4|Statherian|Statherian|Of the McArthur Group.  Age: 1639Ma (U-Pb zircon, Southgate et al, 2000).  Geological Province: Barney Creek Basin.||||||28-NOV-06
1130|Barney Creek Formation|22538|5|Briefly described|P710, P717||Statherian|Age of unit is 1640+/-4 Ma.||||||28-NOV-06
1130|Barney Creek Formation|22662|2|Defined|21-23 fig 2,24,25,28|Proterozoic|Proterozoic|Geol. province: McArthur Basin. Also on pages 29,30||||||20-JUL-06
1130|Barney Creek Formation|22664|5|Briefly described|33-37,39 fig 4, 42|Paleoproterozoic|Paleoproterozoic|Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin. Also on pages 45 and 47.||||||07-NOV-08
1130|Barney Creek Formation|22665|5|Briefly described|Table1, P229||Statherian|||||||
1130|Barney Creek Formation|22853|3|Fully described|21|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness 700 m. Underlain by Coxco Dolomite Member.||||||28-NOV-06
1130|Barney Creek Formation|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
1130|Barney Creek Formation|23195|6|Mentioned|p4|||Hosts the HYC deposit within dolomitic black shales.||||||
1130|Barney Creek Formation|23196|6|Mentioned|p829|||Referred to as HYC-Barney Creek Formation - ie. stating Barney Ck Fm is at HYC. In the McArthur Basin.||||||28-NOV-06
1130|Barney Creek Formation|23197|6|Mentioned|Fig.1, p850|||||||||
1130|Barney Creek Formation|23356|5|Briefly described|26 Tab.2|Statherian|Statherian|Age: 1700-1500Ma.||||||28-NOV-06
1130|Barney Creek Formation|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
1130|Barney Creek Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McArthur Group.||||||28-NOV-06
1130|Barney Creek Formation|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1640+/-3Ma.||||||28-NOV-06
1130|Barney Creek Formation|23398|5|Briefly described|p442|Statherian|Statherian|Age: 1639+/-3Ma.||||||28-NOV-06
1130|Barney Creek Formation|23408|6|Mentioned|p520|||Contains laminated dolomitic siltstones at the McArthur River deposit.||||||15-JUN-09
1130|Barney Creek Formation|23409|5|Briefly described|p556|||||||||
1130|Barney Creek Formation|23534|5|Briefly described|p2318|||Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|23776|5|Briefly described|p705 Fig 2|||Of Umbolooga Subgroup.||||||
1130|Barney Creek Formation|23809|5|Briefly described|p47 Fig. 42|Paleoproterozoic|Paleoproterozoic|Age: 1639+/-3Ma. Geological Province: McArthur Basin.  Correlates with Shillinglaw Formation (Ashburton Province), Campbell Springs Dolostone (Birrindudu basin) and Mount Parker Sandstone (Osmond Basin, W.A.).||||||07-NOV-08
1130|Barney Creek Formation|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlies the Teena Dolomite. Overlain by the Reward Dolomite.||||||
1130|Barney Creek Formation|23910|5|Briefly described|p291|Paleoproterozoic|Paleoproterozoic|Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|23937|5|Briefly described|p25 Tb. 2|||Of the McArthur Group.  Geological Province: McArthur Basin.  See also p92 Appendix 1.||||||13-APR-05
1130|Barney Creek Formation|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
1130|Barney Creek Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup||||||
1130|Barney Creek Formation|23968|5|Briefly described|p1345, 1347|||Geological Province: McArthur Basin.  Maximum Thickness: >700m.||||||
1130|Barney Creek Formation|24048|5|Briefly described|p37|||Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|24179|5|Briefly described|p83, 84 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1640 +/- 3 Ma, 1639 +/- 3 Ma and 1638 +/- 7 Ma (U-Pb).  Overlain by the Reward Formation.  Overlies the Teena Formation.  Geological Province:  McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|24308|5|Briefly described|p1006|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1130|Barney Creek Formation|24432|4|Described|p560 Tb.1|Statherian|Statherian|Age: 1640+/-3 Ma. Of Umbolooga Subgroup. Dolomitic siltstone, coarse sedimentary breccias, tuffaceous horizons and organic rich pyritic shale. Finely laminated, deep water deposition.||||||
1130|Barney Creek Formation|30272|6|Mentioned|p5|||Stratigraphic table p5.||||||28-NOV-06
1130|Barney Creek Formation|30318|6|Mentioned|p327|||||||||
1130|Barney Creek Formation|30344|6|Mentioned|Fig.4|||Part of Umbolooga Subgroup||||||
1130|Barney Creek Formation|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
1130|Barney Creek Formation|30354|5|Briefly described|p20|||||||||
1130|Barney Creek Formation|30363|6|Mentioned|p22|||||||||
1130|Barney Creek Formation|32144|6|Mentioned|p81|||Solvent extractable organic matter||||||
1130|Barney Creek Formation|32363|6|Mentioned|p330|||||||||
1130|Barney Creek Formation|32479|6|Mentioned|p1393|||||||||
1130|Barney Creek Formation|32658|3|Fully described|Table 2|||See also Fig. 3 and 4.||||||28-NOV-06
1130|Barney Creek Formation|32660|5|Briefly described|Table 4|||||||||
1130|Barney Creek Formation|32908|6|Mentioned|p20|||Mineralisation.||||||28-NOV-06
1130|Barney Creek Formation|33550|6|Mentioned|p272|||||||||
1130|Barney Creek Formation|33665|6|Mentioned|p368|||||||||
1130|Barney Creek Formation|33666|6|Mentioned|Table 1|||||||||
1130|Barney Creek Formation|35162|6|Mentioned|Table.1|||||||||
1130|Barney Creek Formation|35261|6|Mentioned|p316|||||||||
1130|Barney Creek Formation|36796|6|Mentioned|p2|||||||||
1130|Barney Creek Formation|37217|6|Mentioned|p649|||||||||
1130|Barney Creek Formation|37371|6|Mentioned|p368|||||||||
1130|Barney Creek Formation|37462|4|Described|Table4.IV|||Also briefly described p249.||||||28-NOV-06
1130|Barney Creek Formation|37568|6|Mentioned|p79|||||||||
1130|Barney Creek Formation|37569|6|Mentioned|p93|||||||||
1130|Barney Creek Formation|38042|6|Mentioned|p158|||||||||
1130|Barney Creek Formation|38582|6|Mentioned|p218|||||||||
1130|Barney Creek Formation|39122|6|Mentioned|p154|||||||||
1130|Barney Creek Formation|39561|6|Mentioned|Fig.5|||||||||
1130|Barney Creek Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|40088|6|Mentioned|p224|||||||||
1130|Barney Creek Formation|40105|6|Mentioned|p314|||||||||
1130|Barney Creek Formation|40109|6|Mentioned|p302|||||||||
1130|Barney Creek Formation|40259|6|Mentioned|Table 1|||||||||
1130|Barney Creek Formation|40691|5|Briefly described|p12|||||||||
1130|Barney Creek Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|41220|6|Mentioned|p366|||||||||
1130|Barney Creek Formation|41268|3|Fully described|p293|||||||||
1130|Barney Creek Formation|41277|6|Mentioned|Fig.2|||||||||
1130|Barney Creek Formation|41957|6|Mentioned|p68|||||||||
1130|Barney Creek Formation|42202|6|Mentioned|p519|||||||||
1130|Barney Creek Formation|42385|4|Described|p20|||See also Table 4 p16.||||||28-NOV-06
1130|Barney Creek Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
1130|Barney Creek Formation|42570|5|Briefly described|p546|||||||||
1130|Barney Creek Formation|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.|1690 +29/-25 Ma in tuff (Page, 1981)|Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Reward Dolomite; overlies Coxco Dolomite Member (Teena Dolomite).|Dolomitic, carbonaceous and pyritic shale and siltstone. Dololutite, rare sandstone. Detailed lithology given.|07-NOV-11
1130|Barney Creek Formation|42639|3|Fully described|p28, Table 5 p20|||||||||
1130|Barney Creek Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
1130|Barney Creek Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Siltstone and mudstone, thin-bedded to laminated, variously dolomitic, carbonaceous and pyritic; dololutite, tuffaceous mudstone, rare breccia and sandstone.||||||19-OCT-05
1130|Barney Creek Formation|42753|6|Mentioned|p2|||||||||
1130|Barney Creek Formation|42812|3|Fully described|p38, Table 4|||Of Umbolooga Subgroup (McArthur Group).||||||20-JUL-06
1130|Barney Creek Formation|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: Glyde River Sub-basin, McArthur Basin.||||||09-MAY-05
1130|Barney Creek Formation|42935|5|Briefly described|p528|||||||||
1130|Barney Creek Formation|43010|5|Briefly described|p128|||||||||
1130|Barney Creek Formation|43036|4|Described|p50|||Of Umbolooga Subgroup.||||||20-JUL-06
1130|Barney Creek Formation|43610|6|Mentioned|p20|||||||||
1130|Barney Creek Formation|45162|2|Defined|p98|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
1130|Barney Creek Formation|46968|6|Mentioned|Fig.2|||||||||
1130|Barney Creek Formation|60483|5|Briefly described|p7 Fig. 5, p8, p30|Paleoproterozoic|Paleoproterozoic|Of Umbolooga Subgroup (McArthur Group). Contains W-Fold and HYC Shale Members, and Cooley Dolomite Member. Age: 1640+/-3Ma, 1639+/-3Ma. Geological Province: McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|60553|5|Briefly described|p625|||Overlies the McArthur Group. Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|60558|5|Briefly described|p8 Fig. 6, p10, p13|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Includes Cooley Dolomite Member, HYC Pyritic Shale Member and W Fold Shale Member. Overlian by Reward Dolomite, underlian by Teena Dolomite.||||||
1130|Barney Creek Formation|62084|4|Described|p936 Fig.5, p939, p941-p942, p957 Fig.16|||Isa Superbasin. McArthur Basin. Hosts McArthur River (formerly HYC) deposit (Zn-Pb-Ag stratiform) at base of HYC Pyritic Shale Member. Shown as Barney Ck Fm or Barney Creek Fm in figures.|1640+/-3 Ma U-Pb SHRIMP Carr et al. 1996|McArthur Group|HYC Pyritic Shale Member||Variably dolomitic organic siltstones and shales; regional marine carbonates.|
1130|Barney Creek Formation|62285|5|Briefly described|p381, p382|||See also upper Barney Creek Formation.||||||
1130|Barney Creek Formation|63062|5|Briefly described|p38|||Of the McArthur Group. Geological Province: McArthur Basin. Lacustrine deposits with source rock potential for petroleum.||||||07-FEB-11
1130|Barney Creek Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1635 Ma.|Unit in River Supersequence.||||
1130|Barney Creek Formation|63866|5|Briefly described|p54|Statherian|Statherian|Isa Superbasin.|c. 1640-1638 Ma (Page et al., 2000)|||||
1130|Barney Creek Formation|64813|6|Mentioned|p269|Palaeoproterozoic|Paleoproterozoic|Geological province: McArthur Basin, N.T. ||||||
1130|Barney Creek Formation|64815|5|Briefly described|p4 Fig.2, p5 Fig.3, p6, p8 Tb.1|||See also p14 Tb.5, p17-19. HYC mineralisation occurs towards the top of this unit.||Of the Umbolooga Subgroup.|Includes Cooley Dolostone Member, W-Fold Shale Member and HYC Pyritic Shale Member.|||
1130|Barney Creek Formation|64816|5|Briefly described|p1, p2 Fig.1, p18-21|Statherian|Statherian|Possible source of a component of the oil in this study. Deposited in lacustrine or lagoon setting.|1640 +/- 3 Ma.|Unit in McArthur Group.||||
1130|Barney Creek Formation|64817|6|Mentioned|p353 Fig.4, p356 |Statherian|Statherian|Thickens into the Emu Fault and thins gradually to the west.|1640 +/- 3 Ma and 1639 +/- 3 Ma.|Of the Umbolooga Subgroup.|Includes Cooley Dolomite Member, W-Fold Shale Member, HYC Pyritic Shale Member.|||
1130|Barney Creek Formation|65228|4|Described|p7, p18, p32, p35, Table 1,Figs.02,04,22|Statherian|Statherian|McArthur Basin. Part of River Supersequence. Shows rapid lateral facies changes related to syn-sedimentary tectonism. 1640 Ma. Hosts McArthur River Ag-Pb-Zn mine. Measured section.|1640 +/- 3 to 1638 +/- 7 Ma.|Unit in Umbolooga Subgroup.|Includes W-Fold Shale, HYC Pyritic Shale, Cooley Dolomite Members.|||
1130|Barney Creek Formation|65337|6|Mentioned|p74.|||At the McArthur River deposit; stratiform base metal sulfide mineralisation from exhalation of metalliferous saline basinal fluids into a localised deep-water brine pool along a regional strike-slip fault system.||||||
1130|Barney Creek Formation|66843|5|Briefly described|p37 Tb.1, p38 Fig.10|||SHRIMP U-Pb zircon ages: Page and Sweet (1998).|1640+/-3 - 1638+/-7 Ma.|McArthur Group.||||
1130|Barney Creek Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Umbolooga Subgroup.||Overlies Teena Dolostone. Is overlain by Reward Dolostone.|Thinly-bedded to laminated, dolomitic, carbonaceous and pyritic shale and siltstone; dololutite, rare breccia and sandstone; gypsum casts.|
1130|Barney Creek Formation|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. Over 900 m thick.||Umbolooga Subgroup||Conformably overlies Coxco Dolostone Member or Teena Dolostone. Overlain by Reward Dolostone, conformably or disconformably.|Thinly bedded to laminated dolomitic, carbonaceous and pyritic shale and siltstone; dolomudstone, tuff; rare breccia and sandstone.|
1130|Barney Creek Formation|68733|6|Mentioned|p186-187|||||McArthur Group.||||04-DEC-17
1130|Barney Creek Formation|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.|1639+/-3 Ma, 1638+/-7 Ma.|Of McArthur Group.||||
1130|Barney Creek Formation|69418|5|Briefly described|p3:11, 13, 36|||McArthur Basin. Hosts sediment-hosted stratiform Zn-Pb-Ag deposits (described). Good potential hydrocarbon source rocks.|||||Black shale, siltstone, sandstone, chert, dolostone, micritic limestone and turbiditic rocks.|12-JUL-16
1130|Barney Creek Formation|69430|4|Described|p15:3, 14, 16, 18-19, 22-23, 32, 34-35|Statherian|Statherian|See also 15:37-39, 61-63. Southern McArthur Basin. 10m to over 900m thick. Largely recessive unit. Basinal shale deposited in actively subsiding sub-basins. Economically important: hosts various base metal occurrences, notably the world-class HYC (later McArthur River) deposit. Potential hydrocarbon source rock (up to 8% TOC) for small structural and diagenetic traps in the Batten Fault Zone. Has palaeo-hydrocarbon reservoirs: intervals contain extensive bitumen and other hydrocarbons.|1640 +/- 3 Ma (Pietsch et al., 1994).|Umbolooga Subgroup.|W-Fold Shale, HYC Pyritic Shale, Cooley Dolostone, Members.|Conformably and gradationally overlies Coxco Dolostone Member (Teena Dolostone). Is overlain conformably by Reward Dolostone. Time-equivalent of Saint Vidgeon Formation.|Thinly bedded to laminated, dolomitic, carbonaceous and pyritic shale and siltstone, dololutite, rare breccia and sandstone; occasional gypsum casts; talus slope breccia adjacent to Emu Fault. Locally abundant tuffs and breccias.|12-JUL-16
1130|Barney Creek Formation|69431|6|Mentioned|p16:25|||An equivalent unit was recognised in a succcession in the northern Tomkinson Province, hosting low-grade base metal mineralisation.||||||12-JUL-16
1130|Barney Creek Formation|69451|6|Mentioned|p35:13|||Potential petroleum source rock: TOC up to 8%.||McArthur Group.||||12-JUL-16
1130|Barney Creek Formation|69545|5|Briefly described|p99|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Host to the supergiant HYC Pb-Zn-Ag deposit. Black shales locally contain over 7% TOC.|1640 Ma|||Overlies Wollogorang Formation.|Unmetamorphosed carbonaceous, pyritic and tuffaceous shales and siltstones.|13-FEB-18
1130|Barney Creek Formation|69673|4|Described|p18, p24,p27, p33, p40, p43, p45, p47|||McArthur Basin, Batten Fault Zone. Significant unconventional shale gas and oil prospect. Late mature to overmature for oil generation in places. Potential as both conventional and unconventional reservoir and seal.|1640 +/- 3 Ma, 1639 +/- 3 Ma|Umbolooga Subgroup|Includes HYC Pyritic Shale Member, W-Fold Shale Member, Cooley Dolostone Member|Conformably overlies Coxco Dolostone Member, conformably overlain by Reward Dolostone, Correlated with Saint Vidgeon Formation|Finely laminated to thinly bedded dolomitic, carbonaceous and pyritic siltstone, shale and dolomudstone and locally abundant tuff beds and breccias.|
1130|Barney Creek Formation|71059|5|Briefly described|p7, p10|||Batten Trough, McArthur Basin. Estimated shale/tight gas/shale oil and condensate resources detailed.||McArthur Group.||||
1130|Barney Creek Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1638+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||HYC Pyritic Shale Member.||Ash tuff, non-tuffaceous shale. Upper stylolitic marker.|
1130|Barney Creek Formation|71606|5|Briefly described|p138|Statherian|Statherian|Batten Trough, McArthur Basin. Depositional age of 1640+\-7 Ma|1640+\-7 Ma|Unit of Umbolooga Subgroup.||||
1130|Barney Creek Formation|72248|4|Described|p145-149,153,155|||Of McArthur Basin. Hosts the giant HYC Zn-Pn-Ag deposit at McArthur River. Recessive stratigraphic unit deposited during a period of pronounced tectonically controlled basin subsidence (Brown et al., 1978; Neudert and McGeough, 1996; Bull, 1998).||Unit of Umbolooga Subgroup.|Includes HYC Pyritic Shale, W-Fold Shale Member and Cooley Dolomite Member.|Underlain by Teena Dolomite.|Finely laminated to thin-bedded, planar-laminated dolomitic, carbonaceous and locally pyritic siltstone.|
1130|Barney Creek Formation|72373|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Dated at 1639+\-3 Ma; partially overlaps in age with Baiguridji Formation (Ahmad et al 2013).||Unit of upper McArthur Group.||||01-OCT-19
1130|Barney Creek Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given including 1639+/-3 Ma, 1640+/-3 Ma.|1638+/-7 Ma.|Batten Subgroup||Overlies Coxco Dolostone and underlies Reward Dolostone.||
1130|Barney Creek Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin. Batten Fault Zone.|1640 +/- 3 Ma, 1639 +/- 3 Ma|Umbolooga Sub-group, McArthur Group|Cooley Dolostone Member, W-Fold Shale Member, HYC Pyritic Shale Member|Underlain by Coxco Dolostone Member. Overlain by Reward Dolostone.||
1130|Barney Creek Formation|72912|5|Briefly described|p5 Fig.3, p36, p37 Fig.14.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given including 1639+/-3 Ma, 1640+/-3 Ma.Described as one of the best source rocks in the McArthur Basin.|1638+/-7 Ma.|Batten Subgroup||Overlies Coxco Dolostone Member and underlies Reward Dolostone.||15-MAR-21
1130|Barney Creek Formation|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1638+/-7 Ma, 1639+/-3 Ma, 1640+/-3 Ma|Batten Subgroup, McArthur Group||Underlain by Coxco Dolostone Member. Overlain by Reward Dolostone.||
1130|Barney Creek Formation|73098|6|Mentioned|p4, p7, p15|||McArthur Basin. Organic petrolography performed on one sample from the Bing Bong 6 well. This sample was low in bitumen. [See report for bitumen/maceral description].|||||Includes black shale.|
1130|Barney Creek Formation|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report]. Informal reference to upper dolomitic shales. [Also alludes to original well logs reporting these rocks as Surprise Creek - Pyritic Shale].|||HYC Pyritic Shale Member|||
1130|Barney Creek Formation|73405|5|Briefly described|p228, 237-238, 239 Fig.7, p240-241|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Current interpretations as a restricted, deep marine paleoenvironment are challenged by biomarker resemblances to saline lacustrine systems (esp. Green River Formation, USA). Effects of putative marine incursions, or of microbial mats, are discussed.|1.64 Ga.|McArthur Group.|||Includes ubiquitous feldspar-rich dolomitic marlstones.|
1130|Barney Creek Formation|73412|4|Described|p1-2, 4, 8-9, 13, 16-17, 19-21|||Southern McArthur Basin. The most important Zn-Pb-Ag host unit in the Basin. Thick deposits accumulated in restricted sub-basins between Hot Spring Fault and Emu Fault Zone.|1640 +/- 3 Ma (Page and Sweet, 1998).|Umbolooga Subgroup.||Overlies Emmerugga and Teena Dolostones. Is overlain by Reward Dolostone.|Contains organic-rich and pyritic mudrocks (trap for Zn-Pb-Ag mineralised fluid transport).|
1163|Barramundi Igneous Suite|41978|6|Mentioned|p498|||||||||
1185|Barrier Granophyre|40896|4|Described|p51|||Briefly described P54||||||
1185|Barrier Granophyre|44778|14|Not recorded|p128,130,131,134,135|||(Post Triassic - pre Eocene or Oligocene poss Early Tertiary)||||||
1185|Barrier Granophyre|44781|14|Not recorded|p362|||||||||
1273|Baumans Camp Granite|23422|5|Briefly described|p181, p217 Table 6.11|Carboniferous|Carboniferous|Of Oweenee Supersuite.||||||
1273|Baumans Camp Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
1273|Baumans Camp Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 166. I-Type.||||||
1273|Baumans Camp Granite|23893|5|Briefly described|p19|Carboniferous|Carboniferous|Geological Province: Oweenee Batholith.||||||
1273|Baumans Camp Granite|42690|5|Briefly described|map legend|Carboniferous||||||||
1273|Baumans Camp Granite|42692|5|Briefly described|map legend|Carboniferous||||||||
1273|Baumans Camp Granite|43095|2|Defined|p43|Carboniferous||||||||
1273|Baumans Camp Granite|43259|4|Described|Appendix 1,p27.||Early Carboniferous|Early Carboniferous?||||||
1273|Baumans Camp Granite|43589|2|Defined|p20|Early Carboniferous|Early Carboniferous|Intrudes Argentine Metamorphics. In contact with Malmesbury Microgranite.||||||23-APR-08
1273|Baumans Camp Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Grey to cream, medium- to coarse-grained, equigranular to slightly porphyritic biotite granite; locally strongly greisenised.|
1273|Baumans Camp Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Grey to cream, medium- to coarse-grained, equigranular to slightly porphyritic biotite granite; locally strongly greisenised.|
1273|Baumans Camp Granite|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
1273|Baumans Camp Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
1283|Bayfield Granite|30811|6|Mentioned|p528|||||||||
1283|Bayfield Granite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
1283|Bayfield Granite|31659|3|Fully described|p92|||?Cretaceous||||||
1283|Bayfield Granite|32357|3|Fully described|p10|||Table 2||||||
1283|Bayfield Granite|32361|6|Mentioned|Map legend|Cretaceous|Permian|Permian or Cretaceous||||||
1283|Bayfield Granite|38081|5|Briefly described|Table 2|||||||||
1283|Bayfield Granite|38406|6|Mentioned|p13|||||||||
1283|Bayfield Granite|39445|5|Briefly described|Table 12|||||||||
1283|Bayfield Granite|41246|6|Mentioned|Map legend|Cretaceous|Permian|||||||
1283|Bayfield Granite|41576|6|Mentioned|p19|||||||||
1283|Bayfield Granite|41922|4|Described|Table 2, P12|||||||||
1283|Bayfield Granite|42660|5|Briefly described|p23|||||||||
1283|Bayfield Granite|61035|5|Briefly described|p19|||Consists of coarse-grained, equigranular biotite syenogranite. Defined by Kirkegaard and others (1970). Intrusion is bounded by a series of normal faults. Ages are not known but possilbly Cretaceous or Triassic.||||||07-FEB-11
1283|Bayfield Granite|68679|5|Briefly described|p410, p423-424, p426|||Southern part of the northern New England Orogen. ~155 km2 unit, bounded by normal faults, in the northeastern Yarrol Belt. Originally thought to be Cretaceous; now thought Permian (reasons given).|||||Leucocratic, coarse-grained, equigranular biotite granite, biotite-hornblende granite.|
1283|Bayfield Granite|69952|6|Mentioned|p75|Triassic|Late Permian|||||||23-NOV-15
1299|Baywulla Formation|30451|4|Described|p28|||Part of Caswell Creek Group||||||
1299|Baywulla Formation|31519|6|Mentioned|p914|||||||||
1299|Baywulla Formation|31586|6|Mentioned|p2|||Refers Maxwell (1960,1961), Jull (1965,1969)||||||
1299|Baywulla Formation|31659|6|Mentioned|p54|||Part of Caswell Creek Group.||||||
1299|Baywulla Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
1299|Baywulla Formation|32866|6|Mentioned|p30|||||||||
1299|Baywulla Formation|32867|6|Mentioned|p56|||||||||
1299|Baywulla Formation|32868|6|Mentioned|p200|||||||||
1299|Baywulla Formation|33728|6|Mentioned|p52|||||||||
1299|Baywulla Formation|33774|14|Not recorded|p19|||Stratigraphy||||||
1299|Baywulla Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
1299|Baywulla Formation|34155|6|Mentioned|p94|||Lower Carboniferous. Caswell Creek Group.||||||
1299|Baywulla Formation|34287|6|Mentioned|p111|||||||||
1299|Baywulla Formation|36528|6|Mentioned|p173|||||||||
1299|Baywulla Formation|39445|5|Briefly described|Table 6|||||||||
1299|Baywulla Formation|42547|4|Described|p51|||||||||
1299|Baywulla Formation|42583|6|Mentioned|p66|||||||||
1299|Baywulla Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
1299|Baywulla Formation|43983|14|Not recorded|p1-3,9,Figs.1,2|||||||||
1299|Baywulla Formation|44091|14|Not recorded|p37,47,Tb.3||Early Carboniferous|||||||
1299|Baywulla Formation|44360|2|Defined|p1-4,13,15,21-8,30-4|Namurian|Visean|Map. Unit of Caswell Creek Group. (late Visean-?early Namurian)||||||
1299|Baywulla Formation|44369|2|Defined|p168-171|||Limestone, Subgreywacke, conglomerate.||||||
1299|Baywulla Formation|44370|14|Not recorded|Tb.7,p219|||||||||
1299|Baywulla Formation|44372|6|Mentioned|p5-7||Visean|Overlies Tellebang Fromation. Underlies Branch Creek Formation.||||||
1299|Baywulla Formation|44379|14|Not recorded|p15|||Ref. to McKellar 1967.||||||
1299|Baywulla Formation|44486|14|Not recorded|p210,212,215|||Lithostrotion arundineum,Eth.||||||
1299|Baywulla Formation|44487|14|Not recorded|p199|||Cannindah Limestone proposed in lieu of Baywulla Formation in Monto-Old Cannindah area.||||||
1299|Baywulla Formation|44515|2|Defined|p29,30|||Overlies Black Mountain Formation.||||||
1299|Baywulla Formation|44833|14|Not recorded|p119-120|||Early Carboniferous faunal zones.||||||
1299|Baywulla Formation|44874|14|Not recorded|p102|||||||||
1299|Baywulla Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
1299|Baywulla Formation|46803|6|Mentioned|p148|||See also Fig. 4||||||
1299|Baywulla Formation|48926|6|Mentioned|p40|||See also P41 etc.||||||24-FEB-10
1299|Baywulla Formation|48940|6|Mentioned|p101|||||||||
1299|Baywulla Formation|66498|6|Mentioned|p47, 49|||Vertebrate microfauna fossils listed.||||||
1299|Baywulla Formation|68297|5|Briefly described|p197|Visean|Visean|Near Rockhampton.||||||
1299|Baywulla Formation|70050|6|Mentioned|p327, p337, p347|Visean|Visean|Monto area. Contains Cionodendron coral fossils (illustrations and systematic palaeontology).||||||
1304|Beacon Mudstone|30914|6|Mentioned|Map legend|Permian|Devonian|Devonian ? - Permian||||||
1304|Beacon Mudstone|31586|5|Briefly described|p6|||Correlation of Visean coral horizons||||||
1304|Beacon Mudstone|31587|5|Briefly described|p60|||Distribution of Lithostrotion||||||
1304|Beacon Mudstone|31802|6|Mentioned|p137|||Refers Lucas in Hill & Denmead (1960) M. - U.Pal.||||||
1304|Beacon Mudstone|34074|5|Briefly described|p258|||L.Carb.||||||
1304|Beacon Mudstone|34350|6|Mentioned|p17|||Carboniferous||||||
1304|Beacon Mudstone|34556|6|Mentioned|p269|||Lower Carboniferous||||||
1304|Beacon Mudstone|36961|6|Mentioned|Fig.5|||||||||
1304|Beacon Mudstone|37100|6|Mentioned|p259|||||||||
1304|Beacon Mudstone|37508|6|Mentioned|p503|||||||||
1304|Beacon Mudstone|37509|6|Mentioned|p504|||||||||
1304|Beacon Mudstone|40246|6|Mentioned|p164|||||||||
1304|Beacon Mudstone|40435|6|Mentioned|p52|||||||||
1304|Beacon Mudstone|40514|6|Mentioned|p5|||||||||
1304|Beacon Mudstone|42547|5|Briefly described|p41|||||||||
1304|Beacon Mudstone|44091|14|Not recorded|p40||Early Carboniferous|||||||
1304|Beacon Mudstone|44360|14|Not recorded|p33||Early Carboniferous|||||||
1304|Beacon Mudstone|44543|2|Defined|p28,30|||Overlies Thanes Creek Slate.||||||
1304|Beacon Mudstone|44564|2|Defined|p166|||On NSW and QLD cards||||||
1304|Beacon Mudstone|44565|14|Not recorded|p232||Early Carboniferous|On NSW and QLD cards.||||||
1304|Beacon Mudstone|44786|14|Not recorded|p193-202||Early Carboniferous|||||||
1304|Beacon Mudstone|44832|14|Not recorded|p8|||||||||
1304|Beacon Mudstone|45097|6|Mentioned|p23|||Refers Lucas (1959)||||||
1304|Beacon Mudstone|48940|6|Mentioned|Fig.14|||Refers Lucas (1959,1960)||||||
1304|Beacon Mudstone|50536|6|Mentioned|p11.1|||||||||
1340|Beaudesert beds|39445|5|Briefly described|Table 14|||||||||
1340|Beaudesert beds|40780|6|Mentioned|p17|||||||||
1340|Beaudesert beds|41906|5|Briefly described|p35|||||||||
1340|Beaudesert beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; 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.||||||
1340|Beaudesert beds|69599|5|Briefly described|p586, P595|Oligocene|Paleocene|Beaudesert Basin. Up to 200m thick. Fossils include fish scales and unstudied microflora; no age determination. RELATED UNITS (continued): Also correlated with Flinders Dolomite; Oakdale Sandstone; Elliott, Petrie, Lowmead Formations; Oxley Group.||||Unconformably overlies Walloon Coal Measures. Correlated (at least partly) with Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; see COMMENTS.|Three units: basal lacustrine granule conglomerate, sandstone and mudstone; several basalt lava flows interlayered with minor mudstone with dolerite sills; topmost lacustrine carbonaceous shale and quartz sandstone. Minor oil shale lenses.|
1372|Beechmont Basalt|30604|6|Mentioned|p66|||||||||
1372|Beechmont Basalt|30687|4|Described|p65|||See also P66,68,77. Tertiary age||||||
1372|Beechmont Basalt|30689|5|Briefly described|p76|||Also mention P73||||||
1372|Beechmont Basalt|31130|6|Mentioned|Fig. 2|||Lower Miocene||||||
1372|Beechmont Basalt|32923|6|Mentioned|p27|||||||||
1372|Beechmont Basalt|32924|4|Described|p112|||Tholeiitic basalt. Thickest N of Mt. Warning||||||
1372|Beechmont Basalt|33290|4|Described|p38|||Analysis P39.||||||
1372|Beechmont Basalt|35296|6|Mentioned|p12|||Statigraphy.||||||
1372|Beechmont Basalt|36806|6|Mentioned|p131|||||||||
1372|Beechmont Basalt|39445|5|Briefly described|Table 14|||||||||
1372|Beechmont Basalt|40623|5|Briefly described|p39|||||||||
1372|Beechmont Basalt|40896|4|Described|p5|||||||||
1372|Beechmont Basalt|43161|4|Described|12-37|||Dated: 20.5 - 23.5 Ma||||||
1372|Beechmont Basalt|44813|14|Not recorded|p8,86,90||Tertiary|21-8 Ma.||||||
1372|Beechmont Basalt|44818|6|Mentioned|p275|||||||||
1372|Beechmont Basalt|44871|2|Defined|p139|||||||||
1372|Beechmont Basalt|48917|6|Mentioned|p38|||One map symbol for all units of Lamington Volcanics||||||
1372|Beechmont Basalt|69599|5|Briefly described|p640|||Northern side of the Tweed volcano, centred on Mount Warning. Relationships indicate this volcano started erupting after the Focal Peak volcano.|c.24 Ma.|||Overlies the Mount Gillies Rhyolite. Approximate equivalent of Lismore Basalt  in NSW.||
1372|Beechmont Basalt|73450|5|Briefly described|p96, p99-100|||Associated with the Tweed Volcano. Up to 1000 m thick.||||Underlain by Chinghee Conglomerate.|Tholeiitic and minor alkaline basaltic lavas.|
1372|Beechmont Basalt|73581|5|Briefly described|p6|||Tweed Volcano. Underlies Binna Burra Rhyolite/Nimbin Rhyolite.||Lamington Volcanics, basal part|||Basalt lavas.|
1388|Beeswing Rhyolite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Parent: Aranbanga Volcanic Group.||||||23-DEC-09
1388|Beeswing Rhyolite|41738|2|Defined|p170|Late Triassic||Reserved as Beeswing||||||
1388|Beeswing Rhyolite|41790|6|Mentioned|p474|||||||||
1388|Beeswing Rhyolite|42054|6|Mentioned|p272|||||||||
1388|Beeswing Rhyolite|63821|5|Briefly described|p21|||Part of the Aranbanga Volcanic Group. Comprises rhyolitic to dacitic ignimbrite with several pyroclastic flow units.||||||07-FEB-11
1388|Beeswing Rhyolite|68679|5|Briefly described|p437, p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. Materials produced by two temporally close eruptions. Associated with the "Gayndah Centre".||Aranbanga Volcanic Group.||Overlies Woodmillar Andesite. Is overlain by Wetheron Basalt.|Basal bedded tuff only locally preserved; thick massive welded vitric ignimbrite with low crystal content and small, sparse lithic fragments; upper bedded tuff with planar and wavy bedding; upper ignimbrite. Ignimbrites rhyolitic to dacitic.|
1388|Beeswing Rhyolite|73450|5|Briefly described|p24, p30, p34-35|||[Also written as Beeswing Rhyolite?].||Aranbanga Volcanic Group|||Two crystal-poor ignimbrites separated by bedded tuffs and surge deposits.|
1389|Beetle Creek Formation|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia||||||||
1389|Beetle Creek Formation|23031|6|Mentioned|17|||Geol province Georgina Basin||||||
1389|Beetle Creek Formation|23374|6|Mentioned|p23|||Of Georgina Basin.||||||02-APR-07
1389|Beetle Creek Formation|23393|6|Mentioned|p22|||||||||
1389|Beetle Creek Formation|23517|5|Briefly described|p28|||Main phosphate horizon.||||||
1389|Beetle Creek Formation|24034|6|Mentioned|p9|Middle Cambrian|Middle Cambrian|Geological Province: Mount Isa Inlier.||||||
1389|Beetle Creek Formation|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Conformably overlies and interfingers with Thorntonia Limestone.  Variably phosphatic and comprises chert, silicified coquinite, chert breccia and conglomerate, siliceous and phosphatic siltstone and phosphorite. Geological Province: Georgina Basin.||||||12-APR-05
1389|Beetle Creek Formation|29940|6|Mentioned|p169|||||||||
1389|Beetle Creek Formation|30239|4|Described|p1193|||||||||
1389|Beetle Creek Formation|30242|5|Briefly described|p9|||Clay mineralogy||||||
1389|Beetle Creek Formation|30479|6|Mentioned|Fig.5|||See also Fig.6 and 7. Stratigraphic relationships||||||
1389|Beetle Creek Formation|30773|6|Mentioned|p266|||Middle Cambrian age||||||
1389|Beetle Creek Formation|30774|6|Mentioned|p1|||||||||
1389|Beetle Creek Formation|30775|6|Mentioned|p1|||||||||
1389|Beetle Creek Formation|30778|6|Mentioned|p1,12,Fig.5|||||||||
1389|Beetle Creek Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|31289|6|Mentioned|p704|||See also Fig. 1||||||
1389|Beetle Creek Formation|31342|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1389|Beetle Creek Formation|31396|6|Mentioned|Fig.3|||||||||
1389|Beetle Creek Formation|31504|5|Briefly described|p303|||M. Cambrian||||||
1389|Beetle Creek Formation|32466|6|Mentioned|p316|||Contains phosphate.||||||
1389|Beetle Creek Formation|32576|5|Briefly described|p49|||||||||
1389|Beetle Creek Formation|32952|4|Described|p1188|||See also pp1189-1194,1203 etc. L.M-Camb.||||||24-JUL-06
1389|Beetle Creek Formation|33111|4|Described|p6,31|||Mentioned p6.||||||
1389|Beetle Creek Formation|33482|5|Briefly described|p1|||Early Middle Cambrian. Phosphate in.||||||
1389|Beetle Creek Formation|33900|6|Mentioned|p19|||||||||
1389|Beetle Creek Formation|34287|6|Mentioned|Fig.3|||||||||
1389|Beetle Creek Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|34543|6|Mentioned|p98|||Middle Cambrian||||||
1389|Beetle Creek Formation|34754|6|Mentioned|p27|||||||||
1389|Beetle Creek Formation|34935|6|Mentioned|p274|||||||||
1389|Beetle Creek Formation|35001|6|Mentioned|Fig.45|||||||||
1389|Beetle Creek Formation|35004|6|Mentioned|Fig.60|||||||||
1389|Beetle Creek Formation|35054|6|Mentioned|Table 23|||||||||
1389|Beetle Creek Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|35139|4|Described|Table.2|||||||||
1389|Beetle Creek Formation|35146|6|Mentioned|p470|||||||||
1389|Beetle Creek Formation|35538|6|Mentioned|Fig.2|||||||||
1389|Beetle Creek Formation|35553|6|Mentioned|p56|||See also Appendix 2, description of Agnostid localities.||||||
1389|Beetle Creek Formation|35936|6|Mentioned|p615|||||||||
1389|Beetle Creek Formation|36234|6|Mentioned|p167|||||||||
1389|Beetle Creek Formation|36448|6|Mentioned|p395|||||||||
1389|Beetle Creek Formation|36525|6|Mentioned|Fig.4|||||||||
1389|Beetle Creek Formation|36645|5|Briefly described|p314|||See Fig.2,3, p307.||||||30-JAN-07
1389|Beetle Creek Formation|36751|6|Mentioned|p485|||||||||
1389|Beetle Creek Formation|36818|6|Mentioned|p203|||||||||
1389|Beetle Creek Formation|37271|6|Mentioned|p210|||||||||
1389|Beetle Creek Formation|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|37572|4|Described|p157|||See also p158,165 and Figs.7 and 8||||||24-JUL-06
1389|Beetle Creek Formation|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|38209|5|Briefly described|p176|||||||||
1389|Beetle Creek Formation|38350|6|Mentioned|p22|||||||||
1389|Beetle Creek Formation|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
1389|Beetle Creek Formation|38444|5|Briefly described|p105|||||||||
1389|Beetle Creek Formation|38445|5|Briefly described|p98|||||||||
1389|Beetle Creek Formation|38446|6|Mentioned|Table 23|||||||||
1389|Beetle Creek Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|39445|5|Briefly described|Table 4|||See also p62.||||||24-JUL-06
1389|Beetle Creek Formation|39690|6|Mentioned|Table 1|||||||||
1389|Beetle Creek Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|40038|6|Mentioned|p248|||||||||
1389|Beetle Creek Formation|40221|4|Described|p20|||||||||
1389|Beetle Creek Formation|40386|6|Mentioned|p429|||||||||
1389|Beetle Creek Formation|40623|5|Briefly described|p96|||||||||
1389|Beetle Creek Formation|40686|5|Briefly described|p407|||||||||
1389|Beetle Creek Formation|40852|6|Mentioned|p34|||||||||
1389|Beetle Creek Formation|40855|6|Mentioned|p329|||||||||
1389|Beetle Creek Formation|40856|5|Briefly described|p313|||||||||
1389|Beetle Creek Formation|40857|5|Briefly described|p268|||||||||
1389|Beetle Creek Formation|40858|5|Briefly described|p132|||||||||
1389|Beetle Creek Formation|41109|6|Mentioned|p184|||||||||
1389|Beetle Creek Formation|41129|6|Mentioned|p17|||See also Fig.8||||||
1389|Beetle Creek Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
1389|Beetle Creek Formation|41639|6|Mentioned|p3,p15|||||||||
1389|Beetle Creek Formation|42058|6|Mentioned|p122|||||||||
1389|Beetle Creek Formation|42070|6|Mentioned|p4|||||||||
1389|Beetle Creek Formation|42477|5|Briefly described|p65, 67|||||||||
1389|Beetle Creek Formation|42575|5|Briefly described|Fig.2 P335|||||||||
1389|Beetle Creek Formation|44091|14|Not recorded|p16,-18,Tb.1||Middle Cambrian|||||||
1389|Beetle Creek Formation|44112|6|Mentioned|p78|||||||||
1389|Beetle Creek Formation|44205|14|Not recorded|p33|||||||||
1389|Beetle Creek Formation|44209|14|Not recorded|p136||Cambrian|||||||
1389|Beetle Creek Formation|44210|2|Defined|Tb.2,p13,114|||||||||
1389|Beetle Creek Formation|44211|2|Defined|p96,98-99,101-103|||Lower part called "Yelvertoft Bed".||||||24-JUL-06
1389|Beetle Creek Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44274|14|Not recorded|p11|||Contemporaneous with Border Waterhole Formation.||||||
1389|Beetle Creek Formation|44275|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44276|2|Defined|Tb.2,p22|||||||||
1389|Beetle Creek Formation|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44529|14|Not recorded|p45||Middle Cambrian|Contains phosphate deposits.||||||
1389|Beetle Creek Formation|44757|6|Mentioned|p153,155|||||||||
1389|Beetle Creek Formation|44788|14|Not recorded|p27|||||||||
1389|Beetle Creek Formation|44878|14|Not recorded|p14||Middle Cambrian|||||||
1389|Beetle Creek Formation|44920|14|Not recorded|Map Legend,Sheet 2,4||Middle Cambrian|||||||
1389|Beetle Creek Formation|44989|14|Not recorded|Not recorded|||||||||
1389|Beetle Creek Formation|45044|14|Not recorded|p5,22||Middle Cambrian|||||||
1389|Beetle Creek Formation|45045|6|Mentioned|p7|||Trilobites||||||
1389|Beetle Creek Formation|45052|3|Fully described|p90|||M.Camb. Contains Yelvertoft Bed.||||||30-JAN-07
1389|Beetle Creek Formation|45055|6|Mentioned|p9|||Templetonian. See also P18,29,30,32,36||||||
1389|Beetle Creek Formation|45062|6|Mentioned|p7|||||||||
1389|Beetle Creek Formation|45079|3|Fully described|p22|||Lower Middle Cambrian age. See also p49||||||24-JUL-06
1389|Beetle Creek Formation|45114|6|Mentioned|p189|||||||||
1389|Beetle Creek Formation|45119|6|Mentioned|p4|||||||||
1389|Beetle Creek Formation|45161|6|Mentioned|p67|||||||||
1389|Beetle Creek Formation|45166|5|Briefly described|Table 15|||||||||
1389|Beetle Creek Formation|46792|6|Mentioned|p51|||Trilobite fauna||||||
1389|Beetle Creek Formation|47058|6|Mentioned|119|||||||||
1389|Beetle Creek Formation|48971|6|Mentioned|p10,18,21,25,27,29,|||p30.||||||
1389|Beetle Creek Formation|50100|5|Briefly described|p22, p75|Middle Cambrian|Middle Cambrian|Includes Monastery Creek Phosphorite Mbr. Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks; commonly contains abundant trilobite fossils.  Disconformably overlies Thorntonia Lst; overlain by Inca Fm.||||||20-JAN-05
1389|Beetle Creek Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin and Burke River Structural Belt.||||||11-MAY-05
1389|Beetle Creek Formation|60264|6|Mentioned|p575|||Superseded by/or previously Monastery Creek Formation?  Geological Province: Burke River Structural Belt.||||||02-APR-07
1389|Beetle Creek Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, chert, shale, phospharite, phosphatic siltstone.||||||
1389|Beetle Creek Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Contains fauna of Ordian age.||||||
1389|Beetle Creek Formation|61181|5|Briefly described|p163|Middle Cambrian|Early Cambrian|Contains large resources of phosphorites. In north-west Queensland. ||||||
1389|Beetle Creek Formation|62504|6|Mentioned|p4|Cambrian|Cambrian|Age: Templetonian.||||||
1389|Beetle Creek Formation|62788|6|Mentioned|p103, p105, p124|Middle Cambrian|Middle Cambrian|Western Queensland unit in which Xystridura templetonensis is the predominant fossil. This and other species support correlation of this unit with the Jigaimara Formation in NT.||||||
1389|Beetle Creek Formation|63450|5|Briefly described|p81, p87|||Contains Monastery Creek Phosphorite Member, also referred to as Monastery Creek Member.||||||07-FEB-11
1389|Beetle Creek Formation|64068|4|Described|p62, 54, 58, pp89-90|Middle Cambrian|Middle Cambrian|Diverse trilobite fauna. Correlated with (lower) Arthur Creek Formation.||Of Narpa Group.|Includes Monastery Creek Phosphorite Member at top.|Disconformably overlies Thorntonia Limestone. Conformably overlain by Inca Formation.|Calcareous and siliceous siltstone, chert, foetid dolomitic phosphatic limestone, calcareous phosphorite, siltstone.|05-APR-12
1389|Beetle Creek Formation|64443|6|Mentioned|p40.|||||||Correlative of Wonarah Formation.||14-MAY-14
1389|Beetle Creek Formation|65337|6|Mentioned|p60.|||Northeastern Georgina Basin. ||||||
1389|Beetle Creek Formation|65345|6|Mentioned|p1.|||Positive tests in 1965-1966 for phosphate identified this unit as a target.||||||
1389|Beetle Creek Formation|65489|5|Briefly described|p126-127|Cambrian|Cambrian|Georgina Basin. Hydrocarbon potential: TOC at 0.19-1.51%|||Includes Monastery Creek Member.||Phosphate-bearing unit.|
1389|Beetle Creek Formation|67127|6|Mentioned|p78|||Primary host for phosphorite REE deposits.||||||
1389|Beetle Creek Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Cambrian|Cambrian|Georgina Basin.||Narpa Group.||Overlies Thorntonia Limestone. Is overlain by Inca Formation and (unconformably) by Camooweal Dolomite, Age Creek Formation, Currant Bush Limestone and Inca Formation.|Chert, siliceous shale with trilobite fossils, basal conglomerate.|
1389|Beetle Creek Formation|67352|6|Mentioned|p69|||||||||
1389|Beetle Creek Formation|67499|6|Mentioned|p940|Cambrian|Cambrian|Overlies Proterozoic rocks with angular unconformity.||||||08-MAY-12
1389|Beetle Creek Formation|67870|5|Briefly described|p38, p44|Middle Cambrian|Middle Cambrian|Georgina Basin. An important source of phosphate.||||Unconformably overlies Thorntonia Limestone.|Siltstone, chert and shale.|
1389|Beetle Creek Formation|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
1389|Beetle Creek Formation|69443|6|Mentioned|p28:14, 16, 22-23|||||||Unconformably overlies Shadow Group. Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
1389|Beetle Creek Formation|69573|6|Mentioned|p656, 661|||Deeper-water sediments. Features Cambrian Stage 5 fossil sites.|||Monastery Creek Phosphorite Member.|||
1389|Beetle Creek Formation|69591|4|Described|p87-88, p90, p92-93, p96-97,p98 Fig.2.91|Cambrian|Cambrian|Georgina Basin. Beetle Creek, near May Downs homestead W of Mount Isa. Hosts phosphorite deposits. Contains a well-known trilobite fauna (species listed). Occurs as small erosional residuals up to 20m thick. Composed of three "members" [only one with a valid stratigraphic name].||Narpa Group.|Ardmore Chert Member, Yelvertoft Bed.|Conformably overlies or grades into Thorntonia Limestone. Is overlain by Inca Formation, and unconformably by Blazan Shale, Camooweal Dolomite, Swift Formation and Age Creek Formation.|Siliceous shale, chert, siltstone and fine sandstone with thin interbeds of limestone in places. Richly fossiliferous: has a well-known trilobite fauna.|
1389|Beetle Creek Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Undilla Sub-basin, Georgina Basin. Overlies Thorntonia Limestone. Is overlain by Inca Formation and Currant Bush Limestone.||
1389|Beetle Creek Formation|70864|6|Mentioned|p74 Fig 2||Paleozoic|Shown as a combined unit with Inca Formation||||||
1389|Beetle Creek Formation|72297|5|Briefly described|p732, p747|Middle Cambrian|Middle Cambrian|Georgina Basin. One of the two major producers of phosphate in QLD. TOC value of 0.19 - 1.51% reported.|||||Marine sequences of phosphorite (phosphatic siltstone) and chert, overlying limestone, sandstone and conglomerate.|
1389|Beetle Creek Formation|72321|6|Mentioned|Fig 2|Wulian|Wulian|Burke River Structural Belt, Undilla Sub-basin, Georgina Basin. Age Cambrian Series 3, Stage 5. Australian stage: Templetonian||of Narpa Group.||||
1389|Beetle Creek Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
1389|Beetle Creek Formation|73418|4|Described|p3, p4 fig 3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin. Dominantly apatitic (non-pelletal) mudstones in central and northern parts (Undilla Sub-basin) contain high contributions of terrigenous material and low REE concentrations. Largely pelletal phosphorites in southern parts (Burke River Structural Belt) can contain up to 0.5 wt% REE, and high concentrations of other elements that substitute into carbonate fluorapatite.||Narpa Group|Lower Siltstone Member, Monastery Creek Phosphorite Member|Overlies Thorntonia Limestone, underlies Inca Formation, Currant Bush Limestone|Phosphorite and shale units.|12-FEB-23
1425|Bellevue Conglomerate|29385|6|Mentioned|p81|||Triassic||||||
1425|Bellevue Conglomerate|30466|6|Mentioned|p3|||Triassic age||||||
1425|Bellevue Conglomerate|33769|5|Briefly described|p150|||||||||
1425|Bellevue Conglomerate|34261|6|Mentioned|p100|||Table||||||
1425|Bellevue Conglomerate|41906|6|Mentioned|p3|||||||||
1425|Bellevue Conglomerate|44076|14|Not recorded|p271-2|||Grades S laterally to Esk Beds.||||||
1425|Bellevue Conglomerate|44510|14|Not recorded|p253|||See also Lexicon.||||||
1429|Bellthorpe Andesite|22845|6|Mentioned|p82|Triassic|Triassic|||||||
1429|Bellthorpe Andesite|22846|6|Mentioned|p44||Triassic|Intruded by Neurum Complex.||||||
1429|Bellthorpe Andesite|30914|6|Mentioned|Map legend|Triassic|Permian|Misspelling of Belthorpe ? Permian to Triassic.||||||
1429|Bellthorpe Andesite|35101|3|Fully described|p28|||||||||
1429|Bellthorpe Andesite|35812|6|Mentioned|p568|||||||||
1429|Bellthorpe Andesite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
1429|Bellthorpe Andesite|39252|6|Mentioned|p27|||||||||
1429|Bellthorpe Andesite|39445|5|Briefly described|Table 9|||See also Fig.7||||||
1429|Bellthorpe Andesite|40051|4|Described|p6|||||||||
1429|Bellthorpe Andesite|40623|5|Briefly described|p53|||||||||
1429|Bellthorpe Andesite|43008|5|Briefly described|map legend|||||||||
1429|Bellthorpe Andesite|44925|5|Briefly described|Map Legend||Permian|||||||
1429|Bellthorpe Andesite|60077|5|Briefly described|Map legend|Early Permian|Early Permian|||||||
1429|Bellthorpe Andesite|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Permian|This unit, as well as the Brookfield and Gilla Volcanics, and unnamed volcanic units, are all mapped under the symbol, PRv.||||||
1429|Bellthorpe Andesite|68679|5|Briefly described|p428, p434, p436|Late Triassic|Late Triassic|Northern New England Orogen. <200m thick. May be comagmatic with Neurum Complex.||||Is mostly surrounded by the Neurum Complex.|Uniform, porphyritic (plagioclase and augite), massive andesitic lava.|
1501|Beril Peak Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Thickness: 250-300m. Geological Province: Georgetown Region.||||||08-JUL-15
1501|Beril Peak Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V27. Assumed to be I-Type.||||||
1501|Beril Peak Rhyolite|23619|4|Described|p31 Table 1||Carboniferous|Intruded by Caterpillar Microgranite. Eveleigh Volcanic Subgroup, of Newcastle Range Volcanic Group. Mosaic Gully Rhyolite, Yellow Jacket Rhyolite.||||||
1501|Beril Peak Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
1501|Beril Peak Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
1501|Beril Peak Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Eveleigh Volcanic Subgroup||||||
1501|Beril Peak Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
1501|Beril Peak Rhyolite|43740|4|Described|p13|||||||||
1501|Beril Peak Rhyolite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Of the Newcastle Range Volcanic Group).||||||
1501|Beril Peak Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|||Grey to brown crystal-free rhyolitic ignimbrite.|
1501|Beril Peak Rhyolite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.||Of the Eveleigh Volcanic Subgroup.|||Grey to brown crystal-free rhyolitic ignimbrite.|
1605|Big Watson Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 427. I-Type.||||||
1605|Big Watson Granodiorite|23713|5|Briefly described|p72 Appendix 2|||Intrudes Hodgkinson Formation. Of Almaden Supersuite.||||||
1605|Big Watson Granodiorite|42681|4|Described|p21|||Previously mapped as Almaden Granite. Reserved as Big Watson Granite.||||||
1605|Big Watson Granodiorite|43083|4|Described|p252|||Of Almaden Supersuite.||||||17-JUN-09
1605|Big Watson Granodiorite|43087|2|Defined|p84|Late Carboniferous||Of Almaden Supersuite[? map with 95/28086 says of Ootann Supersuite].||||||
1605|Big Watson Granodiorite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).  Hornblende?-biotite microgranite, hornblende-biotite granodiorite, hornblende?-biotite granite to granodiorite.||||||15-JUN-06
1605|Big Watson Granodiorite|43254|5|Briefly described|map legend|Early Permian|Late Carboniferous|Age Late Carboniferous to Early Permian? Of Almaden Supersuite.||||||
1605|Big Watson Granodiorite|43259|4|Described|Appendix 1,p46.|Permian|Carboniferous|||||||
1605|Big Watson Granodiorite|43625|6|Mentioned|p21|||||||||
1605|Big Watson Granodiorite|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Almaden Supersuite. Geological Province: Kennedy Province.  Medium to dark grey, fine to medium-grained, moderately to highly porphyritic hornblende-biotite granodiorite to monzogranite with scattered mafic enclaves to 15cm.||||||31-MAY-04
1605|Big Watson Granodiorite|60425|4|Described|p181, p280-1 Appdx. |Early Permian|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). I-type. Fine- to med-gr., mod'ly to highly porphyritic hornblende-biotite granodiorite to granite, with maifc enclaves to 15cm common; more lithological detail included.||||||07-FEB-11
1621|Bigie Formation|22438|4|Described|p535, Fig.3 p537|||Basal unit of Isa Superbasin. See also Fig.10a p546.||||||
1621|Bigie Formation|22457|5|Briefly described|P31|||||||||
1621|Bigie Formation|22498|5|Briefly described|Fig2 P235, P236|||||||||
1621|Bigie Formation|22585|5|Briefly described|Fig1 P736, Fig3|||||||||
1621|Bigie Formation|22665|6|Mentioned|P219, Table1|||||||||
1621|Bigie Formation|22680|6|Mentioned|83|||||||||
1621|Bigie Formation|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geol province: Mount Isa Fold Belt. Overlying units: McNamara Group, Suprise Creek Formation, Fiery Creek Volcanics; underlying unit: Quilalar Formation||||||07-NOV-08
1621|Bigie Formation|23393|4|Described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
1621|Bigie Formation|23395|6|Mentioned|p383|||||||||
1621|Bigie Formation|23396|5|Briefly described|p407 Fig.2|||||||||
1621|Bigie Formation|23397|5|Briefly described|p467 Fig.2|||||||||
1621|Bigie Formation|23399|6|Mentioned|p489|||||||||
1621|Bigie Formation|23406|5|Briefly described|p603, p607 Fig. 8|||Geological province: Lawn Hill Platform. See also Fig. 5.||||||16-JUN-09
1621|Bigie Formation|23408|5|Briefly described|p511, p513 Fig. 2, p523|||Of Hutton et al (1981) who formalised the subdivision of the McNamara Group and added this new formation together with Fiery Creek Volcanics at the base.||||||15-JUN-09
1621|Bigie Formation|23466|5|Briefly described|p267|||||||||
1621|Bigie Formation|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
1621|Bigie Formation|23767|5|Briefly described|p1954 Fig. 1a|||See also p1955.||||||
1621|Bigie Formation|23965|5|Briefly described|p1297|||Geological Province: Mount Isa Inlier.||||||
1621|Bigie Formation|24307|5|Briefly described|p978||Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
1621|Bigie Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1621|Bigie Formation|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince  (Mount Isa Orogen).||||||07-NOV-08
1621|Bigie Formation|24432|6|Mentioned|p562 Fig.2|Statherian|Statherian|||||||
1621|Bigie Formation|37459|2|Defined|p423|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
1621|Bigie Formation|38232|6|Mentioned|p85|||||||||
1621|Bigie Formation|38237|4|Described|p126|||||||||
1621|Bigie Formation|38310|6|Mentioned|p237|||||||||
1621|Bigie Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|38835|6|Mentioned|p164|||||||||
1621|Bigie Formation|39445|5|Briefly described|Table 2|||||||||
1621|Bigie Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Sandstones and conglomerates. Overlies the Quilalar Formation.||||||15-JUN-06
1621|Bigie Formation|39622|6|Mentioned|Fig.2|||||||||
1621|Bigie Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
1621|Bigie Formation|39925|6|Mentioned|p329|||||||||
1621|Bigie Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|40221|3|Fully described|p11|||||||||
1621|Bigie Formation|40840|6|Mentioned|Map legend|||||||||
1621|Bigie Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
1621|Bigie Formation|41307|4|Described|p12|||||||||
1621|Bigie Formation|41978|6|Mentioned|p502|||||||||
1621|Bigie Formation|41979|6|Mentioned|Fig.2 P512|||||||||
1621|Bigie Formation|42565|5|Briefly described|Table 1 P5, P4|||||||||
1621|Bigie Formation|42676|5|Briefly described|Fig.2 P41|||||||||
1621|Bigie Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, conglomerate.||||||09-FEB-09
1621|Bigie Formation|42818|5|Briefly described|Fig.2 P205|||||||||
1621|Bigie Formation|43608|6|Mentioned|Fig.11,p11|||||||||
1621|Bigie Formation|43616|6|Mentioned|p4|||||||||
1621|Bigie Formation|45166|4|Described|p28|||||||||
1621|Bigie Formation|47083|4|Described|p11||Proterozoic|Previously included in Fiery Creek Volcanics and 'Myally Beds'. Unconformably overlain by Surprise Creek Fm; overlies Quilalar Fm unconformably and Myally Subgp. Thickness: 800 m.||||||25-JUL-06
1621|Bigie Formation|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Western Fold Belt Province.||||||
1621|Bigie Formation|50332|5|Briefly described|p16, p20|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Quilalar Formation, overlain by Bigie Formation. Outcrops at eastern margin of Leichhardt River Subprovince. Consists of redbed sandstone, pebbly sanddtone and conglomerate.||||||07-FEB-11
1621|Bigie Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Overlies Quilalar formation at an angular unconformity. Conformably overlain by Fiery Creek Volcanics. Geological Province: Western Fold Belt.||||||17-DEC-07
1621|Bigie Formation|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
1621|Bigie Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
1621|Bigie Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
1621|Bigie Formation|61936|5|Briefly described|p194 Fig. 6|||Intercalated with Fiery Creek Volcanics. Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||
1621|Bigie Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Bigie Fm. Age: U-Pb SHRIMP (after Page et al. 2000)|overlying unnamed unit 1709+/-2 Ma|||||
1621|Bigie Formation|62535|5|Briefly described|p672|Statherian|Statherian|||||Is overlain unconformably by Surprise Creek Formation.||
1621|Bigie Formation|62988|5|Briefly described|p34|||Probably coeval with the ~1710Ma Fiery Event. Now grouped in the Big Supersequence. Geological Province: Calvert Superbasin (Mount Isa Inlier).||||||25-JAN-07
1621|Bigie Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Ages: 1762+/-18Ma, 1764+/-13Ma, 1783+/-5Ma. Unconformable on Quilalar Fm. Geological Province: Calvert Superbasin.  Rift-related immature conglomerates and sandstones. See also p1027 Tb. 1, p1031.||||||07-NOV-08
1621|Bigie Formation|63109|6|Mentioned|p1112, p1108 Fig. 3|||Overlain by Fiery Creek Volcanics and upper Peters Creek Volcanics. Geological Province: Calvert Superbasin. Consists of sandstone.||||||30-SEP-08
1621|Bigie Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlian by Fiery Creek Volcanics, underlian by Quilalar Formation. Thickness: ~500m.  Geological Province: Calvert Superbasin. Coarse- to medium-grained, poorly sorted pebble to cobblestone conglomerates and sandstone.||||||07-FEB-11
1621|Bigie Formation|63113|6|Mentioned|p1225 Fig.13. |||Calvert Superbasin. Part of Big supersequence.||Of the Myally Subgroup||Overlies ?unconformably Quilalar Formation. Is overlain by Fiery Creek Formation.||
1621|Bigie Formation|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Big supersequence||Overlies Quilalar Formation. Is overlain by Fiery Creek Volcanics.||
1621|Bigie Formation|63115|6|Mentioned|1279 Fig.4, p1281-1283, p1290.|||Calvert superbasin. High-permeability aquifer.||||||
1621|Bigie Formation|63116|6|Mentioned|p1297 Fig.2, p1299-1303, p1305-1309 |||Calvert superbasin. Material properties detailed. Aquifer.||||||
1621|Bigie Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. |Between c.1700 and 1670 Ma.||||Sandstone, conglomerate.|
1621|Bigie Formation|63866|5|Briefly described|p57-p58|Statherian|Statherian|Calvert Superbasin.|1709 +/- 3 Ma (Page and Sweet, 1998)|||(Possibly) coeval with the Fiery Creek Volcanics. Overlain by the Surprise Creek Formation, Warrina Park Quartzite, Torpedo Creek Quartzite and the Gunpowder Creek Formation.||
1621|Bigie Formation|64250|6|Mentioned|p11 fig 3, p16 fig.6, p19|||Western Fold Belt, Mount Isa Inlier. <1762 +/- 18 Ma.|c.1710 Ma.||||Sandstone and conglomerate.|
1621|Bigie Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
1621|Bigie Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
1621|Bigie Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
1621|Bigie Formation|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin.||||Uncomformable base.|Conglomerate, with cobble bed near base.|
1621|Bigie Formation|65228|5|Briefly described|p21, Figs.04, 10.|Statherian|Statherian|Part of the Big Supersequence.|c.1720 Ma.|||Is overlain unconformably by Surprise Creek Formation.||12-APR-18
1621|Bigie Formation|65337|6|Mentioned|p5. |||Calvert Superbasin.||||||
1621|Bigie Formation|65396|5|Briefly described|p82, p175, p187, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt.|c.1710 Ma.|||Overlain by Fiery Creek Volcanics.|Quartzite/sandstone and conglomerate with some mafic volcanics.|
1621|Bigie Formation|66824|6|Mentioned|p148|||||||Is overlain by Fiery Creek Volcanics. With Fiery Creek Volcanics, equivalent to Carter's Bore Rhyolite.||
1621|Bigie Formation|67323|4|Described|p8, p11, p13, p25, p33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Calvert Superbasin. Leichhardt River Domain, Mount Oxide Domain, Mount Isa Inlier. Fluvial deposits. Maximum depositional age of 1762 +/- 18 Ma said to be clearly much older than depositional age. |~1720-1710 Ma.|Of Big Supersequence||Unconformably overlies Quilalar Formation. Underlies Fiery Creek Volcanics.|Purple - brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate, red - brown siltstone.|
1621|Bigie Formation|68021|5|Briefly described|p135 fig 4, p136|Statherian|Statherian|Part of Big Supersequence, Calvert Superbasin, Western Succession. Follows major regional unconformity. Deposition in fault-angle depressions and fluviatile environments.||||Unconformably overlies Quilalar Formation, overlain by Fiery Creek Volcanics, intruded by Weberra Granite.|Fanglomerates and coarse sandstones.|
1621|Bigie Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Fiery Creek Volcanics under the symbol, -Pf.||||||
1621|Bigie Formation|68732|5|Briefly described|p161, p165 Fig.3, p166|Statherian|Statherian|Of the Big Supersequence. Detritus sourced from nearby Gin Granite. Maximum sedimentary depositional age.|1762 +/- 18, 1764 +/- 13, 1783 +/- 5 Ma||||Alluvial fan conglomerates and fluvial sandstones.|30-NOV-17
1621|Bigie Formation|69056|6|Mentioned|p2|||Mapped as one unit with Fiery Creek Volcanics.||||||
1621|Bigie Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the c. 1708 Ma Mount Isa Rift Event.||||Overlies Quilalar Formation, overlain by Carters Bore Rhyolite||09-FEB-18
1621|Bigie Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intertongues with Fiery Creek Volcanics. Is overlain by Surprise Creek Formation.||25-JAN-19
1621|Bigie Formation|69591|5|Briefly described|p29, p37-40, p56, p106|Paleoproterozoic|Paleoproterozoic|Mount Oxide, Leichhardt River Domains, Calvert Superbasin. Part of the Big Supersequence. Fluvial/delta fan deposits.|1762 +/- 18 Ma (MDA: Neumann et al., 2006).|||Overlies Peters Creek Volcanics.|Mostly cobble conglomerate and sandstone. Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate, red-brown siltstone.|
1621|Bigie Formation|70282|5|Briefly described|p544 Tb.1|||Cover sequence 3, Mount Isa.|1710-1709 Ma|||Overlain by Fiery Creek Volcanics|Conglomerate and sandstone.|13-FEB-18
1621|Bigie Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate and red-brown siltstone.|
1621|Bigie Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate and red-brown siltstone.|
1621|Bigie Formation|71592|5|Briefly described|Appendix A.|||Kalkadoon-Leichhardt Domain, Mount Isa Orogen.|1796+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
1621|Bigie Formation|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Weberer Granite and Fiery Creek Volcanics.||
1621|Bigie Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1725 Ma|||Overlain by the Fiery Creek Volcanics.|Red beds.|
1621|Bigie Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown, with Fiery Creek Volcanics, as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Unclear whether this unit or Fiery Creek Volcanics was dated. Age given as U-Pb zircon igneous crystallisation age.|1709 +/-3 Ma|||Shown as overlying Carrara Range Group and shown as unconformably underlying Surprise Creek Formation.||
1621|Bigie Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
1621|Bigie Formation|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Shown with Fiery Creek Volcanics. Lateral equivalents? Located in the Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt and the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1709+/-3 Ma|Big Supersequence||Shown as unconformably underlying Surprise Creek Formation and overlying Carrara Range Group, Quilalar Formation.|High energy clastic sediments.|
1621|Bigie Formation|73042|6|Mentioned|p4|Statherian|Statherian|Written as Fiery Creek Vol/Bigie Fm on chronostratigraphic diagram (Fig.1.2). South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age (although it is unclear whether this age is from the Fiery Creek Volcanics or Bigie Formation(?), or if these two units can be distinguished from one another).|1709 +/- 3 Ma (see comments and Fig.1.2)|||Unconformably overlain(?) by Surprise Creek Formation. Equivalent to Fiery Creek Volcanics(?).||
1621|Bigie Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
1621|Bigie Formation|73144|6|Mentioned|p9-10|||Calvert Superbasin. Part of the Big Supersequence.||||Partly interbedded with Fiery Creek Volcanics.||
1621|Bigie Formation|73525|5|Briefly described|p4, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domain.|1762+/-18 Ma maximum depositional age||||Medium-fine sandstone clastics.|
1637|Billicumidji Rhyolite Member|23065|5|Briefly described|15|||||||||
1637|Billicumidji Rhyolite Member|23398|5|Briefly described|p433|Orosirian|Orosirian|Of Cliffdale Volcanics. Age: 1851+/-3Ma.||||||25-JUL-06
1637|Billicumidji Rhyolite Member|24197|5|Briefly described|p22|||Of the Cliffdale Volcanics (Nicholson Suite). Geological province: Murphy Inlier.||||||07-FEB-11
1637|Billicumidji Rhyolite Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|36012|3|Fully described|Table 1|||See also p8.||||||25-JUL-06
1637|Billicumidji Rhyolite Member|36217|6|Mentioned|p206|||Published by Grimes & others 1979. Definition approved by Qld SNC.||||||
1637|Billicumidji Rhyolite Member|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|38584|4|Described|p9|||||||||
1637|Billicumidji Rhyolite Member|41721|5|Briefly described|p7|||Within the upper sequence of the Cliffdale Volcanics. Flow-banded alkali rhyolite and minor tuff. Geological Province: Muprhy Inlier.||||||06-AUG-08
1637|Billicumidji Rhyolite Member|45166|5|Briefly described|p71|||||||||
1637|Billicumidji Rhyolite Member|49001|2|Defined|p4|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|50536|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Of the Cliffdale Volcanics.||||||07-NOV-08
1637|Billicumidji Rhyolite Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Post-Barramundi basement||Cliffdale Volcanics|||Flow-banded and massive rhyolite lava and minor tuff|
1637|Billicumidji Rhyolite Member|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||Cliffdale Volcanics.||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group). Is intruded by Nicholson Granite Complex.|Alkali rhyolite lava, red, flow-banded, with numerous ashfall tuff horizons.|
1637|Billicumidji Rhyolite Member|72919|4|Described|p11|Orosirian|Orosirian|[Also written as Billicumidji Rhyolite]. Murphy Province. Approximately 2000 m thick. A SHRIMP U-Pb zircon age of 1851 +/- 3 Ma was reported by Page et al. (2000).|1851 +/- 3 Ma U-Pb SHRIMP|Cliffdale Volcanics|||Flow-banded porphyritic alkali rhyolite, tuff beds and several minor pyroclastic flow deposits.|
1663|Biloela Formation|24615|5|Briefly described|CD|Tertiary|Tertiary|[To].  Mudstone, siltstone, oil shale, carbonaceous mudstone and sandstone; minor lignite, coal and limestone.||||||
1663|Biloela Formation|38311|2|Defined|p450|early Tertiary|early Tertiary|||||||
1663|Biloela Formation|39445|5|Briefly described|Table 14|||Eocene. See also p150.||||||13-SEP-18
1663|Biloela Formation|39495|6|Mentioned|p142|||||||||
1663|Biloela Formation|39943|6|Mentioned|Table 13A|||||||||
1663|Biloela Formation|41246|6|Mentioned|Map legend|Tertiary||||||||
1663|Biloela Formation|50197|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
1663|Biloela Formation|50209|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
1663|Biloela Formation|50214|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
1663|Biloela Formation|50215|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, siltstone, oil shale, carbonaceous mudstone and sandstone; minor lignite, coal and limestone.||||||18-JUN-09
1663|Biloela Formation|50273|5|Briefly described|Map legend|Tertiary|Tertiary|Mudstone, siltstone, oil shale, carbonaceous mudstone and sandstone; minor lignite, coal and limestone.||||||
1663|Biloela Formation|50317|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, siltstone, oil shale, carbonaceous mudstone and sandstone; minor lignite, coal and limestone.||||||09-JUN-04
1663|Biloela Formation|50602|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, siltstone, oil shale, carbonaceous mudstone and sandstone, minor lignite, coal and limestone.||||||
1663|Biloela Formation|60557|5|Briefly described|p19 Fig. 5b, p28|Tertiary|Tertiary|||||||
1663|Biloela Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||03-MAR-10
1663|Biloela Formation|65388|4|Described|p222-225; p224 Fig. 78|Paleogene|Paleogene|Biloela Basin. Grimes (1980) revived the name "Biloela Beds". Noon (1982a) defined them as the Biloela Formation (mainly freshwater lacustrine). Type section in GSQ Monto 5 from 27.2-374m, near the eastern shore of Lake Victoria. Minimum age from basalt sill: K-Ar 25+/-4 Ma. Pollen not studied. Ostracode fauna early Tertiary. Mudstone, siltstone, oil shale and sandstone, and minor lignite, carbonaceous mudstone and limestone. ||||||
1663|Biloela Formation|67402|4|Described|p239, p242|Aldingan|Wangerripian|Biloela Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under lacustrine or fluvial conditions within a broad shallow graben. [Local SE Australian Stage names used for age. ~ Equivalent to Early to Late Eocene.]||||Overlies the Precipice Sandstone.|Silty and sandy mudstone and oil shale with minor sandstone and coal seams.|13-SEP-18
1663|Biloela Formation|68008|3|Fully described|p219-222, p233, p279-281, p290,p294,p296|||Defined by Noon (1982). Originally named the Biloela Beds by Kirkegaard et al. (1966); later mapped as unnamed Tertiary sediments (Kirkegaard et al. 1970; Dear et al. 1971). Grimes (1980) revived the name Biloela Beds. Occupies the Biloela Basin, 125 x 35 km. The type section is in GSQ Monto 5, from 27.2m to 374m. Age given is early Tertiary: ostracode fauna resembles that of The Narrows beds, with an upper limit of 25 +/- 4 Ma.||||Overlies Precipice Sandstone, and Callide Coal Measures unconformably.|Freshwater, lacustrine mudstone, siltstone, oil shale and sandstone; minor lignite, carbonaceous mudstone and limestone. The basal shale overlies basalt; an 11.7m thick basalt sill also occurs towards the bottom at 357.3 m.|
1663|Biloela Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, 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.||||||
1663|Biloela Formation|68679|6|Mentioned|p312-313, p398|Paleogene|Paleogene|Northern New England Orogen. Covers much of the Callide Basin fill.||||||
1663|Biloela Formation|69599|5|Briefly described|p590-591|Paleogene|Paleogene|Biloela Basin. >350m thick. Lacustrine to fluvial deposits within a shallow graben. Stratigraphic section. Eocene; local laterites produced by Miocene weathering. No economic oil shale or CSG. See reference to the erroneous Biloela beds (p585).|||||Silty and sandy mudstone, oil shale and minor coal and sandstone; deeply weathered and lateritised.|
1663|Biloela Formation|73450|6|Mentioned|p106|||||||||
1700|Binna Burra Rhyolite|22773|5|Briefly described|p345|||||||||
1700|Binna Burra Rhyolite|22857|5|Briefly described|p345|Cenozoic|Cenozoic|In the border region of Lamington National Park. Included in the central-volcano provinces of NSW. At least 5 individual flows each up to 100m thick occur in the type area near Binna Burra.||||||19-NOV-08
1700|Binna Burra Rhyolite|30604|6|Mentioned|p66|||||||||
1700|Binna Burra Rhyolite|30687|4|Described|p64|||See also p65,67,76,77. Miocene age.||||||03-SEP-18
1700|Binna Burra Rhyolite|30689|5|Briefly described|p76|||Also mention Table on p76.||||||03-SEP-18
1700|Binna Burra Rhyolite|31130|6|Mentioned|Fig. 2|||Lower Miocene||||||
1700|Binna Burra Rhyolite|32924|6|Mentioned|p113|||Refers McTaggart (1961)||||||
1700|Binna Burra Rhyolite|33290|4|Described|p37|||See also p38.||||||03-SEP-18
1700|Binna Burra Rhyolite|33751|6|Mentioned|p147|||||||||
1700|Binna Burra Rhyolite|35156|6|Mentioned|p8|||||||||
1700|Binna Burra Rhyolite|35296|6|Mentioned|p12|||Re stratigraphy.||||||
1700|Binna Burra Rhyolite|36806|6|Mentioned|p131|||||||||
1700|Binna Burra Rhyolite|39969|6|Mentioned|Fig.22|||||||||
1700|Binna Burra Rhyolite|40623|5|Briefly described|p39|||||||||
1700|Binna Burra Rhyolite|40780|5|Briefly described|p9|||||||||
1700|Binna Burra Rhyolite|40896|4|Described|p6|||||||||
1700|Binna Burra Rhyolite|42317|5|Briefly described|p2|||||||||
1700|Binna Burra Rhyolite|43161|4|Described|12, 19|||Dated: 20.5 to 23.5 Ma||||||
1700|Binna Burra Rhyolite|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
1700|Binna Burra Rhyolite|44813|14|Not recorded|p80||Tertiary|=Mount Lindsay Rhyolite.||||||
1700|Binna Burra Rhyolite|44818|6|Mentioned|p275|||||||||
1700|Binna Burra Rhyolite|44871|2|Defined|p140|Tertiary|Tertiary|Of Lamington Group.||||||
1700|Binna Burra Rhyolite|48917|6|Mentioned|p38|||Refers McTaggart (1961).||||||
1700|Binna Burra Rhyolite|69599|5|Briefly described|p631, p633 Fig.8.35, p640-641|||Northern side of the Tweed volcano, centred on Mount Warning. Resistant; forms cliff lines and waterfalls. Table of chemical analyses; REE diagram and comment. An age determination of 13.0 +/- 0.5 Ma (Wellman and McDougall, 1974) is "clearly aberrant".|23.9 +/- 0.2 Ma.|||Approximate equivalent of Nimbin Rhyolite in NSW.|Peraluminous or high-silica rhyolite.|
1700|Binna Burra Rhyolite|73450|4|Described|p99-101|Chattian|Chattian|Associated with the Tweed Volcano. Up to 500 m thick. Five separate lava flows have been identified, each up to 100 m thick. Separated from the Binna Burra Rhyolite by basalt (at least locally). Yielded an Ar-Ar sanidine age of 23.9 +/- 0.2 Ma (Cohen, 2007) and K-Ar feldspar ages of 20.8 +/- 0.4 Ma and 20.9 +/- 0.4 Ma (Ewart, 1982).|23.9 +/- 0.2 Ma Ar-Ar||||Coherent felsic lava and minor pyroclastic deposits including ash flow tuff and ash fall tuff.|
1700|Binna Burra Rhyolite|73581|5|Briefly described|p6|Oligocene|Oligocene|Tweed Volcano. Original K-Ar age of 20.9 Ma (Ewart, 1982) was reanalysed and produced an Ar-Ar age of 23.9+/-0.2 Ma (Cohen, 2007). Overlies Beechmont Basalt/Lismore Basalt.|23.9+/-0.2 Ma Ar-Ar (Cohen, 2007)||||Rhyolitic tuff and rhyolite lavas up to 100 m thick.|
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.|
1778|Black Diamond Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
1778|Black Diamond Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
1778|Black Diamond Granite|41235|6|Mentioned|Fig.2a|||||||||
1778|Black Diamond Granite|41740|6|Mentioned|p222|||||||||
1778|Black Diamond Granite|43259|6|Mentioned|Appendix 1,p34.||Carboniferous|of Emuford/Emu Granite.||||||
1778|Black Diamond Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Age: <313-315Ma. Pale pink, fine-gr. to pegmatitic, slightly porphyrytic to seriate, granophyric (topaz-fluorite-)biotite granite; I-type; + assoc'd Sn mineralisation; incl. in Emuford Granite on recent maps||||||07-FEB-11
1837|Black Snake Creek Granite|33476|2|Defined|p68|Triassic|Permian|Permian - Triassic. See also p53.||||||10-DEC-07
1837|Black Snake Creek Granite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
1837|Black Snake Creek Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
1837|Black Snake Creek Granite|43008|5|Briefly described|map legend|||||||||
1837|Black Snake Creek Granite|71628|4|Described|p11: 10-11; p19: 18-20, 25, 175|||Thomson (1976). Named after a local watercourse. Forms a roughly 3 x 2 km, poorly outcropping intrusion 13 km WSW of Drake. Geochemistry described. The c.252 Ma age determination is preliminary (unpublished, pers. comm.).|c.252 Ma (SHRIMP: Waltenberg and Blevin, 2017).|Black Snake Creek Suite.||Intrudes Postmans Creek Granodiorite (Dundee Rhyodacite) and Bungulla Monzogranite.|Grey-pink, medium-grained, porphyritic to equigranular leucogranite; finer-grained grey-pink saccharoidal marginal variant. Has transitional I-A type characteristics.|
1837|Black Snake Creek Granite|72528|4|Described|p2, p4 Tb.1.2, p78-83, p109, p127.|Lopingian|Lopingian|Magmatic crystallisation age determined. Lies northeast of Tenterfield, forming a small irregular pluton. Shown as part of the New England Orogen.|252.0+/-1.2 Ma U238/Pb206 (Pb207-corrected)|Black Snake Creek Suite||Intrudes Dundee Rhyodacite and intrudes Bungulla Monzogranite.|Dated sample is massive, pale pink, fine-grained, moderately porphyritic, leucocratic biotite monzogranite. I-type.|
1843|Black Stump Arkose|8187|5|Briefly described|Map legend|Adelaidean|Adelaidean|Arkose, pebbly arkose, siltstone, shale.  Overlies Yardida Tillite; underlies Thorntonia Limestone.||||||21-JUN-04
1843|Black Stump Arkose|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Arkose, pebbly arkose, siltstone, shale. Overlies: Yardida Tillite. Underlies: Wonnadinna Dolomite.||||||28-OCT-04
1843|Black Stump Arkose|22646|6|Mentioned|Fig 4 on p 102|||Georgina Basin.||||||
1843|Black Stump Arkose|24442|5|Briefly described|p49|Marinoan|Marinoan|Geological Province: Georgina Basin.||||||
1843|Black Stump Arkose|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
1843|Black Stump Arkose|35863|6|Mentioned|Table 1|||||||||
1843|Black Stump Arkose|37928|6|Mentioned|Fig.4|||||||||
1843|Black Stump Arkose|37929|5|Briefly described|p526|||||||||
1843|Black Stump Arkose|37930|6|Mentioned|p528|||||||||
1843|Black Stump Arkose|38157|6|Mentioned|Table IX|||||||||
1843|Black Stump Arkose|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
1843|Black Stump Arkose|40906|6|Mentioned|Fig.9|||||||||
1843|Black Stump Arkose|41405|6|Mentioned|p205|||||||||
1843|Black Stump Arkose|41801|6|Mentioned|Fig.4|||||||||
1843|Black Stump Arkose|45155|6|Mentioned|p28|||Correlation||||||
1843|Black Stump Arkose|46903|6|Mentioned|Fig.5|||Correlation chart||||||
1843|Black Stump Arkose|46959|6|Mentioned|p207|||||||||
1843|Black Stump Arkose|48990|2|Defined|p8|Adelaidean|Adelaidean|Formerly part of Field River Beds (Smith,1963) which have now been superseded.||||||25-JUL-06
1843|Black Stump Arkose|49027|5|Briefly described|p2|||||||||
1843|Black Stump Arkose|60122|4|Described|p4-5, p11 Tb. 1|Neoproterozoic|Neoproterozoic|Of Keepera Group. Red-brown to purple brown micaceous, fine to very coarse (to pebbly) arkose, sst and laminated micaceous mudst. Disconformably overlies Yardida Tillite; conformably underlies Wonnadinna Dolostone. Max. thick: >700m in type section.||||||
1843|Black Stump Arkose|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group.  Micaceous (to pebbly) arkose, sandstone, micaceous mudstone.||||||23-DEC-09
1843|Black Stump Arkose|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group.  Micaceous (to pebbly) arkose, sandstone, micaceous mudstone.  Geological Province: southern Georgina Basin.||||||
1843|Black Stump Arkose|63450|5|Briefly described|p78 Fig. 5|Neoproterozoic|Neoproterozoic|Together with Wonnadinna Dolomite overlies Yardida Tillite disconformably; grades up into Wonnadinna Dolomite. Geol.prov: Georgina Basin, West Toko Syncline. Coarse-grained arkose, sandstone and micaceous mudstone interpreted as glacial outwash deposits.||||||07-FEB-11
1843|Black Stump Arkose|63562|6|Mentioned|p344|||Of Georgina Basin.||||||
1843|Black Stump Arkose|64068|3|Fully described| p46, p viii, p18-19, p36|Cryogenian||Basal glacial outwash. Fairly high radiometric values from feldspathic and clay-rich sediments. Correlated with Sun Hill Arkose, Oorabra Arkose, Boko Formation, Olympic Formation, Pioneer Sandstone, Mount Doreen Formation.||Of Keepera Group.||Disconformable over Yardida Tillite. Conformable and gradational under Wonnadinna Dolostone.|Red-brown to purple-brown micaceous, fine to very coarse arkose, sandstone, laminated micaceous mudstone and siltstone.|18-JAN-16
1843|Black Stump Arkose|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Toko Syncline, Southern Georgina Basin.||||||
1843|Black Stump Arkose|65338|6|Mentioned|p60.|||||Unit in Keepera Group.||||
1843|Black Stump Arkose|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Feldspathic sandstone (locally pebbly), siltstone and shale.|
1843|Black Stump Arkose|68270|4|Described|p681-683,688|Cryogenian|Cryogenian|Southern Georgina Basin. Composite section: N flank Field River Anticline N of drillhole Hay River 7 (lat. 23'6'15"N, long. 137'51'18"E). Less than 700m thick. Proximal glacial outwash deposit related to Elatina glaciation. Correlative to Elatina Formation. Laterally equivalent to Sun Hill Arkose and Oorabra Arkose.||||Overlain by Wonnadinna Dolostone (paraconformity). Underlain disconformably by Yardida Tillite.|Poorly sorted, medium- to coarse-grained and pebbly arkose, with interbedded sandstone, laminated micaceous siltstone and shale and conglomerate.|03-JUL-19
1843|Black Stump Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Gnallan-a-gea and Sun Hill Arkoses, Little Burke and Yardida Tillites, are all mapped under the symbol, -P-Cg.||||||
1843|Black Stump Arkose|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Keepera Group.||Is overlain by Wonnadinna Dolostone.||12-JUL-16
1843|Black Stump Arkose|69438|6|Mentioned|p23:17|||Georgina Basin.||||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
1843|Black Stump Arkose|69443|4|Described|p28:7-9, 33; 28:38 Fig.28.36|Cryogenian|Cryogenian|Walter (1980). Georgina Basin. Over 700m thick. Proximal glacial outwash deposit. Exposed by Tarlton and Toomba Faults.||Keepera Group.||Disconformably overlies Yardida Tillite. Is overlain conformably and gradationally by Wonnadinna Dolostone.|Micaceous, fine to very coarse (to pebbly) arkose, sandstone, laminated micaceous mudstone and siltstone.|12-JUL-16
1843|Black Stump Arkose|69591|5|Briefly described|p94|||Toko Syncline. Up to 700m thick.||||Disconformably overlies Yardida Tillite. Is overlain disconformably by Gnallan-A-Gea Arkose.||
1843|Black Stump Arkose|69673|5|Briefly described|p114 fig 92, p115|Cryogenian|Cryogenian|More than 700m thick.||Keepera Group|||Arkose, sandstone, laminated micaceous mudstone and siltstone.|
1843|Black Stump Arkose|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Georgina Basin. Age from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
1843|Black Stump Arkose|73086|6|Mentioned|p101, p167|||Georgina Basin.||||Correlates to Olympic Formation.||
1871|Blackstone Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Brassal Subgroup||||
1871|Blackstone Formation|24082|5|Briefly described|p453|Late Triassic|Late Triassic|Of the Brassall Sub-Group.  Max. thickness: 240m.  Geological Province: Ipswich Basin.||||||
1871|Blackstone Formation|30086|5|Briefly described|p3|||Triassic||||||
1871|Blackstone Formation|30087|4|Described|p1|||Unit of Ipswich Coal Measures. See also P3||||||
1871|Blackstone Formation|30302|6|Mentioned|p415|||Refers Allen and Staines(1959)||||||
1871|Blackstone Formation|30458|6|Mentioned|p1|||See also P3-20,38-39||||||
1871|Blackstone Formation|30459|6|Mentioned|p309|||||||||
1871|Blackstone Formation|30461|6|Mentioned|p100|||||||||
1871|Blackstone Formation|30465|6|Mentioned|p1|||||||||
1871|Blackstone Formation|30466|6|Mentioned|p4|||Triassic age||||||
1871|Blackstone Formation|30470|6|Mentioned|p459|||||||||
1871|Blackstone Formation|30475|6|Mentioned|p166|||||||||
1871|Blackstone Formation|31300|6|Mentioned|p79,Pls.9,10|||See also P82. U.Triassic. Scoresbya dichoforma (Shirley)||||||
1871|Blackstone Formation|32136|6|Mentioned|p5|||Miospores. See also P8||||||
1871|Blackstone Formation|32176|6|Mentioned|p2|||Ipswich Coal Meas. Triassic||||||
1871|Blackstone Formation|32178|6|Mentioned|p2|||||||||
1871|Blackstone Formation|32179|6|Mentioned|p3|||Trias.||||||
1871|Blackstone Formation|32180|5|Briefly described|p6|||||||||
1871|Blackstone Formation|33381|4|Described|p110|||Triassic. See also PP112-117, 122 & map||||||
1871|Blackstone Formation|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
1871|Blackstone Formation|34355|6|Mentioned|p1,2,5,6||Triassic|||||||
1871|Blackstone Formation|34505|6|Mentioned|p1|||Ipswich Coal Measures||||||
1871|Blackstone Formation|35053|5|Briefly described|p35|||||||||
1871|Blackstone Formation|35647|6|Mentioned|p53|||||||||
1871|Blackstone Formation|35648|6|Mentioned|p13|||||||||
1871|Blackstone Formation|35913|6|Mentioned|p35|||||||||
1871|Blackstone Formation|36172|6|Mentioned|Appendix|||||||||
1871|Blackstone Formation|36351|6|Mentioned|p376|||||||||
1871|Blackstone Formation|36354|6|Mentioned|p371|||||||||
1871|Blackstone Formation|36779|6|Mentioned|p7|||||||||
1871|Blackstone Formation|36825|6|Mentioned|p13|||||||||
1871|Blackstone Formation|36899|6|Mentioned|p1095|||||||||
1871|Blackstone Formation|36941|6|Mentioned|p162|||||||||
1871|Blackstone Formation|37111|4|Described|p294|||||||||
1871|Blackstone Formation|37755|6|Mentioned|p80|||||||||
1871|Blackstone Formation|38074|5|Briefly described|Table 1|||||||||
1871|Blackstone Formation|38076|6|Mentioned|Table 3|||||||||
1871|Blackstone Formation|38306|6|Mentioned|p512|||||||||
1871|Blackstone Formation|38307|4|Described|p521|||||||||
1871|Blackstone Formation|38373|6|Mentioned|p615|||||||||
1871|Blackstone Formation|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
1871|Blackstone Formation|39445|5|Briefly described|Table 9|||||||||
1871|Blackstone Formation|39943|6|Mentioned|Table 12A|||||||||
1871|Blackstone Formation|40434|6|Mentioned|p25|||||||||
1871|Blackstone Formation|40623|5|Briefly described|p30|||||||||
1871|Blackstone Formation|41058|6|Mentioned|p51|||||||||
1871|Blackstone Formation|41906|3|Fully described|Table 2 p17|||||||||28-SEP-05
1871|Blackstone Formation|42187|6|Mentioned|p319|||||||||
1871|Blackstone Formation|42336|5|Briefly described|p4|||||||||
1871|Blackstone Formation|42405|6|Mentioned|Table 3 P.7|||||||||
1871|Blackstone Formation|42474|6|Mentioned|p30|||Bundamba||||||
1871|Blackstone Formation|42539|5|Briefly described|p183|||||||||
1871|Blackstone Formation|42648|5|Briefly described|p41|||Brassal Subgroup||||||
1871|Blackstone Formation|42932|6|Mentioned|p7|||||||||
1871|Blackstone Formation|43076|6|Mentioned|p19|||of Brassal Subgroup||||||
1871|Blackstone Formation|43910|14|Not recorded|p1,3|||||||||
1871|Blackstone Formation|43922|14|Not recorded|p325(strat table)326|||(well-preserved microflora) Top formation of Ipswich Coal Measures.||||||
1871|Blackstone Formation|43984|14|Not recorded|p129|||||||||
1871|Blackstone Formation|43995|14|Not recorded|Table p20||Triassic|Part of Ipswich Coal Measures.||||||
1871|Blackstone Formation|44030|14|Not recorded|p126,140||Late Triassic|||||||
1871|Blackstone Formation|44091|14|Not recorded|p51||Triassic|||||||
1871|Blackstone Formation|44250|14|Not recorded|p90|||||||||
1871|Blackstone Formation|44510|2|Defined|p252-257,260-262,|||Figs.35,36||||||
1871|Blackstone Formation|44542|2|Defined|p36||Middle Triassic|Overlies Cooneana Formation.||||||
1871|Blackstone Formation|44543|14|Not recorded|p27|||||||||
1871|Blackstone Formation|44573|14|Not recorded|p92|||||||||
1871|Blackstone Formation|44633|14|Not recorded|p2|||||||||
1871|Blackstone Formation|44734|14|Not recorded|p7,19|||Pine Mountain area.||||||
1871|Blackstone Formation|44771|14|Not recorded|p1,2,4,6,Fig.1||Triassic|Part of Ipswich Coal Measures.||||||
1871|Blackstone Formation|44774|6|Mentioned|p31|||Disconformably overlain Aberdare Conglomerate.||||||
1871|Blackstone Formation|44775|4|Described|p7,9,map 2||Triassic|||||||
1871|Blackstone Formation|44776|14|Not recorded|p3,7|||Member of Ipswich Coal Measures.||||||
1871|Blackstone Formation|44777|14|Not recorded|p55|||"No younger than basal Late Triassic and no older than Middle Triassic.||||||
1871|Blackstone Formation|44783|14|Not recorded|p13,16,17|||||||||
1871|Blackstone Formation|44884|4|Described|p1,2,Fig.1|||||||||
1871|Blackstone Formation|44885|14|Not recorded|p2,3|||||||||
1871|Blackstone Formation|60726|5|Briefly described|p1-4, throughout text.|Carnian|Carnian|Youngest Formation of the Ipswich Coal Measures. Contains a richly fossiliferous horizon: plants, freshwater bivalves, insects (listed) and dinosaur footprints.|||||Includes fossil-rich arenaceous siltstone layer about 15cm thick.|
1871|Blackstone Formation|67402|5|Briefly described|p222, p223, p224, p225|Carnian|Carnian|Ipswich Basin. Deposited in a floodplain to meandering river environment. May act as an unconventional seal. ||Brassall Subgroup||Overlies the Tivoli Formation. Overlain by the Aberdare Conglomerate.|Predominantly coal, carbonaceous mudstone with sandstone, siltstone and claystone.|
1871|Blackstone Formation|68679|5|Briefly described|p394-396|Late Triassic|Late Triassic|Ipswich Basin. Crops out on the limbs of the Bundamba Anticline. Up to 240m thick. River channel, peat swamp and flood plain deposits in a meandering stream system. One of the two major coal producers in the Ipswich Coalfield. Plant/insect interactions recorded; also tracks of labyrinthodonts and dinosaurs (elaborated).||Brassall Subgroup.||Is overlain unconformably by the Aberdare Conglomerate (Woogaroo Subgroup).|Shale, mudstone, siltstone, lenticular sandstone beds and coal. Seven main coal seams, thicker (4-10m) and more laterally extensive than Tivoli Formation seams hosting abundant thin persistent claystone bands (distal volcanic airfall deposits).|
1871|Blackstone Formation|72297|5|Briefly described|p698|Triassic|Triassic|Ipswich Basin.||Ipswich Coal Measures.|Thomas, Aberdare, Bluff, Four Feet, Bergin, Striped Bacon and Rob Roy seams.|||
1876|Blackwater Group|13516|5|Briefly described|p147 fig 5, p157|Late Permian|Late Permian|From Denison Trough, Bowen Basin||||Overlain gradationally by Rewan Group in Denison Trough. Diachronous boundary.||
1876|Blackwater Group|22593|6|Mentioned|Table 1|||||||||
1876|Blackwater Group|22757|4|Described|Table4,p10|||400 m thick. Conformable on Back Creek Group. Unconformably overlain by Rewan Formation||||||
1876|Blackwater Group|22857|6|Mentioned|p315 Fig. 22.8|||Geological Province: Gunnedah and Bowen Basins.||||||
1876|Blackwater Group|22865|6|Mentioned|Fig22.8p315|||||||||
1876|Blackwater Group|22973|5|Briefly described|p11 Fig.2(e)|Early Triassic|Early Triassic|||||||
1876|Blackwater Group|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
1876|Blackwater Group|22987|6|Mentioned|p299|||||||||
1876|Blackwater Group|22988|5|Briefly described|p303|||||||||
1876|Blackwater Group|22992|6|Mentioned|p329|||||||||
1876|Blackwater Group|22995|6|Mentioned|p361|||||||||
1876|Blackwater Group|23002|5|Briefly described|p417|Permian|Permian|||||||
1876|Blackwater Group|23003|5|Briefly described|p423 Table 1|Permian|Permian|||||||
1876|Blackwater Group|23004|5|Briefly described|p431 Table 1|Permian|Permian|||||||
1876|Blackwater Group|23037|6|Mentioned|Fig 3|Triassic|Late Permian|||||||
1876|Blackwater Group|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
1876|Blackwater Group|23161|5|Briefly described|p31 table4 fig11||Late Permian|||||||
1876|Blackwater Group|23356|5|Briefly described|26 Tab.2|Late Permian|Late Permian|||||||
1876|Blackwater Group|23430|5|Briefly described|p514-515|||Bowen Basin Province.||||||
1876|Blackwater Group|23444|5|Briefly described|p183|||||||||
1876|Blackwater Group|23769|4|Described|p862|Triassic|Permian|Geological Province: Bowen Basin.||||||
1876|Blackwater Group|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
1876|Blackwater Group|24071|5|Briefly described|p317 Table 1|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
1876|Blackwater Group|24077|5|Briefly described|p410 Tb. 2|Late Permian|Late Permian|Includes the Bandanna Formation.  Geological Province: Bowen Basin.||||||
1876|Blackwater Group|24093|4|Described|p177|Late Permian|Late Permian|Max. thickness: 1550m.   Geological Province: Bowen Basin.||||||
1876|Blackwater Group|24159|5|Briefly described|p147|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
1876|Blackwater Group|29387|6|Mentioned|Table 4|||||||||
1876|Blackwater Group|29409|6|Mentioned|Table 1|||Base recognised as top of Carnangarra Sandstone Member.||||||
1876|Blackwater Group|29567|6|Mentioned|p72|||Upper Permian||||||
1876|Blackwater Group|29591|5|Briefly described|p96|||||||||
1876|Blackwater Group|29721|6|Mentioned|Table 65|||||||||
1876|Blackwater Group|29727|6|Mentioned|p867|||||||||
1876|Blackwater Group|30448|6|Mentioned|p100|||||||||
1876|Blackwater Group|30450|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|30508|6|Mentioned|p85|||Seven boreholes drilled to test coal-bearing formations||||||
1876|Blackwater Group|30547|6|Mentioned|p426|||Correlation||||||
1876|Blackwater Group|30549|6|Mentioned|p26|||Upper Permian age||||||
1876|Blackwater Group|30691|4|Described|p14|||See also P21,Table 3,6. Upper Permian age||||||
1876|Blackwater Group|30692|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|30696|4|Described|Table 3|||Upper Permian age||||||
1876|Blackwater Group|30698|6|Mentioned|Map legend|Permian|Permian|||||||
1876|Blackwater Group|30699|6|Mentioned|p53|||Stratigraphy. Upper Permian age||||||
1876|Blackwater Group|30701|6|Mentioned|Map legend|Late Permian|Late Permian|||||||11-JAN-10
1876|Blackwater Group|30851|6|Mentioned|p366|||||||||
1876|Blackwater Group|30852|6|Mentioned|p171|||||||||
1876|Blackwater Group|30854|6|Mentioned|p8|||||||||
1876|Blackwater Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
1876|Blackwater Group|30915|6|Mentioned|p98|||||||||
1876|Blackwater Group|30916|6|Mentioned|p97|||||||||
1876|Blackwater Group|31079|6|Mentioned|p5|||||||||
1876|Blackwater Group|31084|6|Mentioned|p12|||See also P13, 16, 21. U. Permian||||||
1876|Blackwater Group|31087|6|Mentioned|p109|||||||||
1876|Blackwater Group|31088|6|Mentioned|p390|||||||||
1876|Blackwater Group|31115|6|Mentioned|p32|||Permian||||||
1876|Blackwater Group|31120|6|Mentioned|p148|||||||||
1876|Blackwater Group|31261|6|Mentioned|p518|||||||||
1876|Blackwater Group|31262|6|Mentioned|p3|||||||||
1876|Blackwater Group|31369|6|Mentioned|p3|||||||||
1876|Blackwater Group|31380|6|Mentioned|p131|||Refers Rigby(1972)||||||
1876|Blackwater Group|31401|6|Mentioned|Fig.1|||P30||||||
1876|Blackwater Group|31531|6|Mentioned|Table 1|||||||||
1876|Blackwater Group|31620|6|Mentioned|p87|||U.Permian||||||
1876|Blackwater Group|31656|4|Described|Table 1|||U.Permian||||||
1876|Blackwater Group|31687|6|Mentioned|p281|||Section||||||
1876|Blackwater Group|31689|6|Mentioned|p247|||Thickness data||||||
1876|Blackwater Group|31690|6|Mentioned|p37|||||||||
1876|Blackwater Group|31691|5|Briefly described|p427|||Upper Permian||||||
1876|Blackwater Group|31979|4|Described|Table 1|||See also Table 2. ?disconformable on Back Creek Group.||||||
1876|Blackwater Group|31983|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|31984|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32193|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32276|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32493|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32520|6|Mentioned|p103|||U.Permian||||||
1876|Blackwater Group|32553|4|Described|p40|||||||||
1876|Blackwater Group|32556|4|Described|Table 3|||U.Perm.||||||
1876|Blackwater Group|32577|4|Described|p23|||Permian. See also P27-29,41||||||
1876|Blackwater Group|32689|6|Mentioned|Fig.2|||Correlation table. Refers Malone et al. (1969)||||||
1876|Blackwater Group|32797|6|Mentioned|p10|||||||||
1876|Blackwater Group|32832|6|Mentioned|p7||Permian|||||||
1876|Blackwater Group|32834|6|Mentioned|Table 3|||||||||
1876|Blackwater Group|32835|6|Mentioned|p6|||Flora||||||
1876|Blackwater Group|32840|6|Mentioned|p10|||||||||
1876|Blackwater Group|32944|6|Mentioned|p703|||||||||
1876|Blackwater Group|33078|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33079|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33086|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33090|4|Described|Table 3|||U.Perm.||||||
1876|Blackwater Group|33091|5|Briefly described|p8|||Stratigraphy||||||
1876|Blackwater Group|33092|5|Briefly described|p6|||Strat. table||||||
1876|Blackwater Group|33094|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33096|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33132|6|Mentioned|Fig. 6|||||||||
1876|Blackwater Group|33250|6|Mentioned|p140|||||||||
1876|Blackwater Group|33251|6|Mentioned|p2|||||||||
1876|Blackwater Group|33366|6|Mentioned|Fig.3|||U.Perm.||||||
1876|Blackwater Group|33368|6|Mentioned|p10|||Correl. with Bandanna Fm.||||||
1876|Blackwater Group|33390|6|Mentioned|p3|||On Table.||||||
1876|Blackwater Group|33451|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33639|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|33640|5|Briefly described|Table 4|||||||||
1876|Blackwater Group|33646|6|Mentioned|p10|||Correlation. Palynological stage.||||||
1876|Blackwater Group|33648|6|Mentioned|p17|||Palynological division.||||||
1876|Blackwater Group|34132|6|Mentioned|p2|||Upper Permian. See also P5.||||||
1876|Blackwater Group|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
1876|Blackwater Group|34174|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|34276|6|Mentioned|p42|||||||||
1876|Blackwater Group|34314|4|Described|Table 2|||U.Permian. See PP10,12||||||
1876|Blackwater Group|34331|6|Mentioned|p458|||U.Permian||||||
1876|Blackwater Group|34389|4|Described|Table 2|||Upper Permian||||||
1876|Blackwater Group|34390|4|Described|Table 2|||Permian||||||
1876|Blackwater Group|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|34408|6|Mentioned|p185|||On Table||||||
1876|Blackwater Group|34480|6|Mentioned|p489|||Upper Permian. See also P492||||||
1876|Blackwater Group|34574|6|Mentioned|p115|||||||||
1876|Blackwater Group|34613|4|Described|Table 3|||||||||
1876|Blackwater Group|35138|6|Mentioned|p15|||||||||
1876|Blackwater Group|35266|6|Mentioned|p190|||||||||
1876|Blackwater Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
1876|Blackwater Group|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
1876|Blackwater Group|35822|6|Mentioned|p40|||||||||
1876|Blackwater Group|35845|6|Mentioned|p86|||||||||
1876|Blackwater Group|35873|6|Mentioned|p2|||||||||
1876|Blackwater Group|35901|6|Mentioned|p1|||||||||
1876|Blackwater Group|35913|6|Mentioned|p35|||||||||
1876|Blackwater Group|35914|6|Mentioned|p8|||||||||
1876|Blackwater Group|35937|6|Mentioned|p621|||||||||
1876|Blackwater Group|35940|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|36172|6|Mentioned|Appendix|||||||||
1876|Blackwater Group|36327|6|Mentioned|p3|||||||||
1876|Blackwater Group|36472|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|36570|6|Mentioned|p77|||||||||
1876|Blackwater Group|36739|6|Mentioned|p1|||||||||
1876|Blackwater Group|37065|6|Mentioned|p32|||||||||
1876|Blackwater Group|37071|5|Briefly described|p84|||||||||
1876|Blackwater Group|37072|6|Mentioned|p91|||||||||
1876|Blackwater Group|37073|6|Mentioned|p99|||||||||
1876|Blackwater Group|37075|5|Briefly described|Table 1|||||||||
1876|Blackwater Group|37076|4|Described|p120|||||||||
1876|Blackwater Group|37077|6|Mentioned|p131|||||||||
1876|Blackwater Group|37079|4|Described|p139|||||||||
1876|Blackwater Group|37080|6|Mentioned|p149|||||||||
1876|Blackwater Group|37096|6|Mentioned|p248|||||||||
1876|Blackwater Group|37400|6|Mentioned|p313|||||||||
1876|Blackwater Group|37458|6|Mentioned|p435|||||||||
1876|Blackwater Group|37565|6|Mentioned|p7|||||||||
1876|Blackwater Group|37610|5|Briefly described|p302|||||||||
1876|Blackwater Group|37612|6|Mentioned|Fig.1|||See also Fig.3 and P284.||||||
1876|Blackwater Group|37726|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|37749|6|Mentioned|p186|||||||||
1876|Blackwater Group|37804|6|Mentioned|p63|||||||||
1876|Blackwater Group|37858|6|Mentioned|p82|||||||||
1876|Blackwater Group|37859|6|Mentioned|p67|||||||||
1876|Blackwater Group|38153|6|Mentioned|p368|||||||||
1876|Blackwater Group|38365|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|38373|6|Mentioned|p613|||||||||
1876|Blackwater Group|38518|6|Mentioned|Fig.3|||||||||
1876|Blackwater Group|39212|5|Briefly described|p12|||Coal deposits. P24 gas reservoir. See also P11 & 23||||||
1876|Blackwater Group|39219|6|Mentioned|p47|||Microflora||||||
1876|Blackwater Group|39252|5|Briefly described|p20|||See aslo P26 & Fig.13||||||
1876|Blackwater Group|39261|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|39264|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|39267|6|Mentioned|p236|||||||||
1876|Blackwater Group|39268|6|Mentioned|p269|||||||||
1876|Blackwater Group|39412|6|Mentioned|p24|||||||||
1876|Blackwater Group|39445|6|Mentioned|Table 8|||||||||
1876|Blackwater Group|39494|6|Mentioned|Fig.5|||||||||
1876|Blackwater Group|40030|6|Mentioned|Fig.5|||||||||
1876|Blackwater Group|40095|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|40245|6|Mentioned|Table 2|||||||||
1876|Blackwater Group|40249|6|Mentioned|p41|||||||||
1876|Blackwater Group|40256|6|Mentioned|Fig.4|||||||||
1876|Blackwater Group|40544|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|40571|6|Mentioned|p29|||||||||
1876|Blackwater Group|40574|6|Mentioned|p4|||||||||
1876|Blackwater Group|40623|5|Briefly described|p80|||||||||
1876|Blackwater Group|40767|6|Mentioned|p17|||||||||
1876|Blackwater Group|41034|5|Briefly described|p366|||||||||
1876|Blackwater Group|41102|5|Briefly described|Mention|||||||||
1876|Blackwater Group|41159|6|Mentioned|p340|||||||||
1876|Blackwater Group|41188|5|Briefly described|p231|||Mention Fig.3||||||
1876|Blackwater Group|41191|6|Mentioned|p283|||||||||
1876|Blackwater Group|41211|6|Mentioned|p178|||||||||
1876|Blackwater Group|41246|6|Mentioned|Map legend|Permian||||||||
1876|Blackwater Group|41247|6|Mentioned|Fig.7|||||||||
1876|Blackwater Group|41290|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|41460|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|41474|6|Mentioned|p63|||||||||
1876|Blackwater Group|41475|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|42091|6|Mentioned|p284|||||||||
1876|Blackwater Group|42120|6|Mentioned|p412|||||||||
1876|Blackwater Group|42250|6|Mentioned|p31|||||||||
1876|Blackwater Group|42255|6|Mentioned|p234|||||||||
1876|Blackwater Group|42257|5|Briefly described|Table 1 P263|||||||||
1876|Blackwater Group|42259|6|Mentioned|p15|||||||||
1876|Blackwater Group|42614|6|Mentioned|p13|||Bowen Basin||||||
1876|Blackwater Group|42634|5|Briefly described|Table 2 P10|||||||||
1876|Blackwater Group|42641|6|Mentioned|p108|||||||||
1876|Blackwater Group|42701|4|Described|p68|||||||||
1876|Blackwater Group|42932|5|Briefly described|Fig.15|||||||||
1876|Blackwater Group|43000|5|Briefly described|p108|||||||||
1876|Blackwater Group|43002|5|Briefly described|Fig.2,p135|||||||||
1876|Blackwater Group|43016|6|Mentioned|p366|||||||||
1876|Blackwater Group|43017|5|Briefly described|Fig.2,p374|||||||||
1876|Blackwater Group|43185|6|Mentioned|13||Permian|||||||
1876|Blackwater Group|43474|14|Not recorded|fig.1,opp.p6||Kazanian|||||||
1876|Blackwater Group|43714|5|Briefly described|p8||Late Permian|||||||
1876|Blackwater Group|43982|14|Not recorded|Map Legend|||||||||
1876|Blackwater Group|43988|14|Not recorded|Map Legend||Permian|||||||
1876|Blackwater Group|43989|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|43990|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|43994|14|Not recorded|Map Legend||Late Permian|Includes Gyranda Formation.||||||
1876|Blackwater Group|43998|4|Described|p12,13,18,map||Late Permian|= Upper Bowen Coal Measures.||||||
1876|Blackwater Group|44022|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|44023|4|Described|Tb.2,p7||Late Permian|||||||
1876|Blackwater Group|44172|14|Not recorded|Tb.1,p1325||Tatarian|Ref. to BMR 1964. Equivalent of Bandanna Formation.||||||
1876|Blackwater Group|44245|5|Briefly described|Map Legend||Permian|||||||
1876|Blackwater Group|44331|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
1876|Blackwater Group|44390|14|Not recorded|p6,13||Permian|||||||
1876|Blackwater Group|44419|14|Not recorded|p272,273,275||Permian|||||||
1876|Blackwater Group|44421|14|Not recorded|p10||Permian|||||||
1876|Blackwater Group|44424|14|Not recorded|p293-301|||Overlies Blenheim Subgroup.||||||
1876|Blackwater Group|44618|14|Not recorded|p511||Permian|Ref. to Malone et al.1965. Includes: Rangal Coal Measures, Burngrove and Fairhill Formations.||||||
1876|Blackwater Group|44630|14|Not recorded|p494,496|||||||||
1876|Blackwater Group|44639|14|Not recorded|p56|||||||||
1876|Blackwater Group|44721|14|Not recorded|p28-36||Late Permian|||||||
1876|Blackwater Group|44814|14|Not recorded|p483|||Overlies Artinskian-Kazanian faunas.||||||
1876|Blackwater Group|45031|14|Not recorded|p6,9||Permian|||||||
1876|Blackwater Group|45071|3|Fully described|p63|||See also Table 12||||||
1876|Blackwater Group|45073|6|Mentioned|p58|||Geological history||||||
1876|Blackwater Group|45095|4|Described|p8|||||||||
1876|Blackwater Group|45110|3|Fully described|Table 14|||See also p24 and Fig.5.||||||18-JUN-09
1876|Blackwater Group|45151|5|Briefly described|Table 10|||See also Table 11 & P15. Contains part of former Upper Bowen C.M.||||||
1876|Blackwater Group|48898|2|Defined|p43|Late Permian|Late Permian|Previously Upper Bowen Beds. See also pp46,47 etc.||||||18-JUN-09
1876|Blackwater Group|48900|2|Defined|p40|Late Permian|Late Permian|||||||
1876|Blackwater Group|48919|5|Briefly described|p19|||U.Permian||||||
1876|Blackwater Group|48920|3|Fully described|p29|||Upper Permian age. See also palynology on p88.||||||18-JUN-09
1876|Blackwater Group|48922|4|Described|p22|||||||||
1876|Blackwater Group|48947|5|Briefly described|p8|||||||||
1876|Blackwater Group|48995|6|Mentioned|p37|||See also Fig.3.||||||
1876|Blackwater Group|49644|5|Briefly described|Table|||||||||
1876|Blackwater Group|50273|5|Briefly described|Map legend|Early Permian|Early Permian|Comprises Gyranda Subgroup and Baralaba Coal Measures.||||||18-MAY-04
1876|Blackwater Group|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Gyranda Subgroup, Barabala Coal Measures.||||||
1876|Blackwater Group|60282|5|Briefly described|p7|||Geological Province: Bowen Basin.||||||
1876|Blackwater Group|60472|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Includes: Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||||||
1876|Blackwater Group|60659|5|Briefly described|p20-21|Late Permian|Late Permian|Includes: Moranbah, Fort Cooper and Rangal Coal Measures. Terrestrial sediments including coal measures. Geological Province: Bowen Basin.||||||07-FEB-11
1876|Blackwater Group|61035|6|Mentioned|p16|||Geological Province: Bowen Basin. Consists of  feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashtone and cherty mudstone, carbonaceous mudstone and coal. Plant and wood fossils are common.||||||07-FEB-11
1876|Blackwater Group|61377|5|Briefly described|p149 Fig. SU8, p157-158|||Includes the Kianga Formation. See also Blackwater Formation (misspelling?). Shales and coals of this unit are rich in total organic carbon. Geological Province: Bowen and Surat Basins.||||||07-FEB-11
1876|Blackwater Group|62921|5|Briefly described|p878 Fig.2, p882-883|Changhsingian|Permian|Bowen Basin. |||Includes Black Alley Shale, Betts Creek Beds and Bandanna Formation.|Is overlain unconformably by Rewan Group but conformably by Rewan Formation.||
1876|Blackwater Group|64197|6|Mentioned|p630 Fig.7|Permian|Permian|||||Underlies the Rewan Group; overlies the Back Creek Group.||
1876|Blackwater Group|64856|6|Mentioned|p61|||| | ||||31-JAN-13
1876|Blackwater Group|64859|6|Mentioned|p195|Permian|Permian|||||||
1876|Blackwater Group|65119|5|Briefly described|p513, 526, Fig 2, 4-5,7-12,16-19|Late Permian|Late Permian|Bowen Basin. Interbedded carbon siltstone and shale, tuff, sandstone and coal. Marine, up to 1080m thick. Age: 248-251 Ma. Fission Track ages ~59-77 Ma. Present in the Cockatoo Creek Well. See also Black Water Group p504.||||||08-MAY-13
1876|Blackwater Group|65388|5|Briefly described|p193-202, p159, 191|Late Permian|Late Permian|Bowen Basin. The Blackwater Group (Mollan and others, 1969) is the succession of non-marine sediments recognised throughout the Bowen Basin between the marine Back Creek Group and the Rewan Formation (now Group), and earlier known as the Upper Bowen Coal Measures. Includes Moranbah Coal Measures.||||||
1876|Blackwater Group|65706|4|Described|p12, p16 Tb.1, p18 Tb.1|Late Permian|Late Permian|Bowen Basin. Lacustrine, fluvial and paludal sediments.||||Conformably overlies Back Creek Group; conformably underlies Rewan Group.|Feldspathic and lithic sandstone, quartzose sandstone, silty sandstone, calcareous sandstone, cherty mudstone, carbonaceous shale, coal, pebble and cobble conglomerate, tuff with commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|66086|5|Briefly described|Map legend|Permian|Permian|Includes Moranbah and Fort Cooper Coal Measures.||||||
1876|Blackwater Group|66615|6|Mentioned|p6|||In contact with the Moolayember Formation.||||||
1876|Blackwater Group|67133|6|Mentioned|p20-21|||||||Is overlain by Precipice Sandstone.||
1876|Blackwater Group|67402|5|Briefly described|p80, p82 fig BWN4, p84|Late Permian|Late Permian||||Includes the Moranbah Coal Measures, Fort Cooper Coal Measures and Rangal Coal Measures.||Coal deposits.|
1876|Blackwater Group|68003|6|Mentioned|p57 Fig.3-n.|||Bowen Basin.||||Overlies Back Creek Group. Is unconformably overlain by Rewan Group and Wandoan Formation.||
1876|Blackwater Group|68202|6|Mentioned|p176|Permian|Permian|Bowen Basin.|||Rangal Coal Measures.|||
1876|Blackwater Group|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
1876|Blackwater Group|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||||Unconformably overlain by the Rewan Formation. Unconformably underlain by the Black Alley Shale.|Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone, and coal; commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||||Underlain by the Black Alley Shale, Back Creek Group.|Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone and coal; commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||Conformably overlies Back Creek Group. Is overlain conformably by Rewan Group.||
1876|Blackwater Group|68679|5|Briefly described|p312-313, p347, p353, p364|Permian|Permian|See also p373-374 Figs.5.66-68. Northern New England Orogen.|||Moranbah, Fort Cooper, Rangal, Coal Measures.|Overlies Back Creek Group.||
1876|Blackwater Group|68731|6|Mentioned|p173 Fig 3.85|||||||||
1876|Blackwater Group|68901|6|Mentioned|p2 Fig. i|Permian|Permian|||||||26-SEP-18
1876|Blackwater Group|69379|5|Briefly described|map legend|Permian|Permian||||||Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone and coal; commonly abundant plant fossils and fossil wood|
1876|Blackwater Group|69681|6|Mentioned|p83 Fig.7|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
1876|Blackwater Group|69952|6|Mentioned|p85|Permian|Permian|||||||
1876|Blackwater Group|70330|6|Mentioned|p11|Late Permian|Late Permian|Bowen Basin.|||Moranbah, Fort Cooper, Rangal, Coal Measures.|||
1876|Blackwater Group|70673|6|Mentioned|p9|Permian|Permian|||||||
1876|Blackwater Group|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin.|||Includes Burngrove Formation.|||
1876|Blackwater Group|70857|5|Briefly described|Map Legend|Permian|Permian|||||Overlies Back Creek Group||
1876|Blackwater Group|70861|6|Mentioned|p37|Late Permian|Late Permian|Of Bowen Basin. |||Includes Rangal, Fort Cooper and Moranbah CM, Bandana, Burngrove, Fair Hill, Macmillan, German Creek and Peawaddy fms, Black Alley Shale, Kaloola Member.|||
1876|Blackwater Group|70940|5|Briefly described|p843-844|Permian|Permian|Bowen Basin. Late Permian.|||Moranbah, Fort Cooper, Rangal, Baralaba Coal Measures; Tinowon, Bandana, German Creek, MacMillan, Fair Hill, Burngrove, Flat Top, Gyranda Formations; Black Alley Shale; Kaloola Member.|||
1876|Blackwater Group|71264|6|Mentioned|p581 Fig.4|Permian|Permian|Bowen Basin.||||||
1876|Blackwater Group|71276|5|Briefly described|p285, p292|Permian|Permian|Mollan et al. (1969); previously the upper part of the Cheshire Formation of Schneeberger (1952). Type locality on the western side of Springsure Shelf, Galilee Basin. Use of this name is stated to have diminished in the Galilee Basin generally in favour of Bandanna Formation.|||Bandanna Formation,|Overlies Black Alley Shale.|Coal-bearing.|
1876|Blackwater Group|73036|5|Briefly described|Map legend|Late Permian|Late Permian||||Includes Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73037|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone. Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73038|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73040|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73246|6|Mentioned|p189-190|Upper Permian|Upper Permian|Bowen Basin. Contains major coal measures.|||Moranbah, Fort Cooper, and Rangal coal measures, Yarrabee Tuff, Burngrove Formation, Fair Hill Formation|Underlain by Back Creek Group including Exmoor Formation and German Creek Formation of Blenheim Subgroup. Overlain by Rewan Group.|Sandstone, siltstone, and coal seams.|
1876|Blackwater Group|73304|6|Mentioned|p72|||Bowen Basin.||||||
1876|Blackwater Group|73305|6|Mentioned|p547-548, p560|Late Permian|Late Permian|Bowen Basin. Stratigraphy varies across the basin reflecting periods of rifting and thermal subsidence that controlled sedimentation and relative sea level.|||Fort Cooper Coal Measures|||
1876|Blackwater Group|73472|6|Mentioned|p129|Permian|Permian|Bowen Basin. Includes at least three distinct tuff units.|||Platypus Tuff, Yarrabee Tuff, Black Alley Shale Tuff|||
1886|Blair Athol Coal Measures|22973|5|Briefly described|p9 Fig.2 (c)|Early Permian|Early Permian|||||||
1886|Blair Athol Coal Measures|22982|5|Briefly described|p269 Fig.4|Early Permian|Early Permian|||||||
1886|Blair Athol Coal Measures|23008|6|Mentioned|p460|||||||||
1886|Blair Athol Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
1886|Blair Athol Coal Measures|29732|6|Mentioned|p27|||||||||
1886|Blair Athol Coal Measures|29943|6|Mentioned|p46|||||||||
1886|Blair Athol Coal Measures|30914|6|Mentioned|Map legend|Permian|Permian|||||||
1886|Blair Athol Coal Measures|31079|6|Mentioned|p5|||||||||
1886|Blair Athol Coal Measures|31261|6|Mentioned|p518|||||||||
1886|Blair Athol Coal Measures|31262|6|Mentioned|p2|||||||||
1886|Blair Athol Coal Measures|31649|6|Mentioned|p57|||||||||
1886|Blair Athol Coal Measures|32493|6|Mentioned|Map legend|Permian|Permian|||||||
1886|Blair Athol Coal Measures|32520|6|Mentioned|p100|||L.Permian||||||
1886|Blair Athol Coal Measures|32577|4|Described|p23|||See also p24,34-36. Lower Permian.||||||11-SEP-08
1886|Blair Athol Coal Measures|32840|6|Mentioned|p10|||||||||
1886|Blair Athol Coal Measures|34389|4|Described|Table 2|||Permian||||||
1886|Blair Athol Coal Measures|35085|6|Mentioned|p27|||||||||
1886|Blair Athol Coal Measures|35138|6|Mentioned|p13|||||||||
1886|Blair Athol Coal Measures|35268|6|Mentioned|p22|||||||||
1886|Blair Athol Coal Measures|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin. Lithology described p184.||||||
1886|Blair Athol Coal Measures|35729|4|Described|p347|||||||||
1886|Blair Athol Coal Measures|35873|4|Described|p10|||||||||
1886|Blair Athol Coal Measures|35901|6|Mentioned|p6|||||||||
1886|Blair Athol Coal Measures|35937|6|Mentioned|p619|||||||||
1886|Blair Athol Coal Measures|36172|6|Mentioned|Appendix|||||||||
1886|Blair Athol Coal Measures|36327|6|Mentioned|p3|||||||||
1886|Blair Athol Coal Measures|36329|6|Mentioned|p60|||||||||
1886|Blair Athol Coal Measures|36739|6|Mentioned|p21|||||||||
1886|Blair Athol Coal Measures|36825|6|Mentioned|p19|||||||||
1886|Blair Athol Coal Measures|36899|6|Mentioned|p1090|||||||||
1886|Blair Athol Coal Measures|37065|6|Mentioned|p31|||||||||
1886|Blair Athol Coal Measures|37070|4|Described|p71|||||||||
1886|Blair Athol Coal Measures|37133|4|Described|p376|||||||||
1886|Blair Athol Coal Measures|37612|3|Fully described|p289|||See also p283 and Fig.3.||||||11-SEP-08
1886|Blair Athol Coal Measures|37726|6|Mentioned|Fig.2|||||||||
1886|Blair Athol Coal Measures|37859|6|Mentioned|p63|||||||||
1886|Blair Athol Coal Measures|38518|6|Mentioned|Fig.3|||||||||
1886|Blair Athol Coal Measures|38603|6|Mentioned|p81|||||||||
1886|Blair Athol Coal Measures|38958|5|Briefly described|p490|||||||||
1886|Blair Athol Coal Measures|39212|4|Described|p31|||Productive parts are Early Permian. Correlation. See also p8.||||||11-SEP-08
1886|Blair Athol Coal Measures|39252|5|Briefly described|p20|||||||||
1886|Blair Athol Coal Measures|39261|6|Mentioned|Fig.6|||||||||
1886|Blair Athol Coal Measures|39264|6|Mentioned|p156|||||||||
1886|Blair Athol Coal Measures|39266|5|Briefly described|Table 1|||Correlation||||||
1886|Blair Athol Coal Measures|39273|6|Mentioned|Fig. 4|||||||||
1886|Blair Athol Coal Measures|39280|5|Briefly described|p380|||||||||
1886|Blair Athol Coal Measures|39445|5|Briefly described|Table 8|||||||||
1886|Blair Athol Coal Measures|39777|6|Mentioned|p146|||||||||
1886|Blair Athol Coal Measures|39994|6|Mentioned|p201|||||||||
1886|Blair Athol Coal Measures|40635|6|Mentioned|p39|||||||||
1886|Blair Athol Coal Measures|41191|6|Mentioned|Fig.3|||||||||
1886|Blair Athol Coal Measures|41226|6|Mentioned|p22|||||||||
1886|Blair Athol Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
1886|Blair Athol Coal Measures|41272|5|Briefly described|M 1of1 B12|||||||||
1886|Blair Athol Coal Measures|41689|6|Mentioned|Table 1|||||||||
1886|Blair Athol Coal Measures|42187|6|Mentioned|Fig.4 P320|||||||||
1886|Blair Athol Coal Measures|42212|6|Mentioned|p329|||||||||
1886|Blair Athol Coal Measures|42249|6|Mentioned|Table 1 P22|||||||||
1886|Blair Athol Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
1886|Blair Athol Coal Measures|42252|5|Briefly described|p50|||||||||
1886|Blair Athol Coal Measures|42309|6|Mentioned|p257|||||||||
1886|Blair Athol Coal Measures|42641|6|Mentioned|Fig.3 P110|||||||||
1886|Blair Athol Coal Measures|42648|6|Mentioned|Fig.6 P41|||||||||
1886|Blair Athol Coal Measures|43204|5|Briefly described|Map Legend|Early Permian|Early Permian|||||||23-DEC-11
1886|Blair Athol Coal Measures|43213|4|Described|p34, p154-157, p239|Permian|Permian|Blair Athol Basin, on the W margin of the Bowen Basin. Includes rocks in the adjacent Springs and Miclere Basins. Composite type section (after Preston, 1985) described, particularly the coal seams.||||Overlies Bathampton Metamorphics. Correlated with Aldebaran Sandstone and Cattle Creek Formation.|130-150m of basal conglomerate and coarse-grained sandstone with interspersed carbonaceous shale and minor dirty coal seams, overlain by c.100m of sandstone, siltstone and coal (43m) with minor shale.|
1886|Blair Athol Coal Measures|43861|5|Briefly described|25||Permian|||||||
1886|Blair Athol Coal Measures|43987|14|Not recorded|p268,273,274|||||||||
1886|Blair Athol Coal Measures|43994|14|Not recorded|Map Legend|||||||||
1886|Blair Athol Coal Measures|43998|4|Described|p4,8,17,map||Permian|Unconformable on Anakie Metamorphics.||||||12-JAN-12
1886|Blair Athol Coal Measures|44243|14|Not recorded|p644||Permian|||||||
1886|Blair Athol Coal Measures|44250|14|Not recorded|p90|||See also Lexicon.||||||
1886|Blair Athol Coal Measures|44331|14|Not recorded|Map Legend||Permian|||||||
1886|Blair Athol Coal Measures|44337|5|Briefly described|Map Legend||Permian|Lithology.||||||
1886|Blair Athol Coal Measures|44622|14|Not recorded|p84|||Presence of glossopterid fructification Scutum is reported. See also Lexicon.||||||
1886|Blair Athol Coal Measures|44630|14|Not recorded|p493|||||||||
1886|Blair Athol Coal Measures|44732|14|Not recorded|p2|||||||||
1886|Blair Athol Coal Measures|45071|3|Fully described|p50|||See also Table 9.||||||
1886|Blair Athol Coal Measures|45073|6|Mentioned|p58|||Geological history||||||
1886|Blair Athol Coal Measures|46949|6|Mentioned|p98|||||||||
1886|Blair Athol Coal Measures|48843|14|Not recorded|p.19,39-42,45,62-63||Permian|(econ.geol.) (F55-11).||||||
1886|Blair Athol Coal Measures|48915|6|Mentioned|Table 1|||Permian||||||
1886|Blair Athol Coal Measures|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Of the Back Creek Group. Geological Province: northern Bowen Basin.||||||04-FEB-08
1886|Blair Athol Coal Measures|60386|6|Mentioned|p296|||Bowen/Sydney Basin.  Non-marine, coal.||||||
1886|Blair Athol Coal Measures|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Of Back Creek Group. Geological Province: Bowen Basin.||||||13-MAR-09
1886|Blair Athol Coal Measures|62043|6|Mentioned|p438.||||||||Local thick, areally restricted coal bodies.|
1886|Blair Athol Coal Measures|64665|6|Mentioned|p53 Fig.2.|Middle Permian|Early Permian|Bowen Basin.||||||
1886|Blair Athol Coal Measures|66085|5|Briefly described|Map legend|Permian|Permian|Sandstone, shale, mudstone, quartz-pebble to polymictic conglomerate and coal.||||||
1886|Blair Athol Coal Measures|68412|5|Briefly described|Map legend|Permian|Permian||||||Sandstone, shale, mudstone, quartz-pebble to polymictic conglomerate and coal.|
1886|Blair Athol Coal Measures|68679|5|Briefly described|p378, p383-384|Permian|Permian|Staines and Koppe (1980). Bowen Basin. Alluvial plain deposits. Properties of the coal are described in some detail.|||||Sandstone, coal, conglomerate, siltstone, mudstone.|
1886|Blair Athol Coal Measures|70815|6|Mentioned|p3|||Bowen Basin.||||||
1886|Blair Athol Coal Measures|71701|5|Briefly described|p170|||Bowen Basin. Encompasses an upper stage 4a palynoflora.||||||
1886|Blair Athol Coal Measures|72297|5|Briefly described|p694 Fig.10.8, p696|Permian|Permian|Blair Athol Basin. Up to 250m thick. Mining was expected to cease in 2013. An equivalent unit in the Wolfgang Basin is over 428m thick. Indicative properties of export thermal coal tabulated.|||Wolfgang seam.|Unconformably overlies the Anakie Metamorphic Group.|Dominated by conglomerate and sandstone with carbonaceous shale and thin coal seams.|
1928|Blantyre Sandstone|23499|5|Briefly described|map legend|Jurassic|Jurassic|Eromanga Basin||||||
1928|Blantyre Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
1928|Blantyre Sandstone|29591|6|Mentioned|Table 72|||||||||
1928|Blantyre Sandstone|30021|6|Mentioned|p87|||||||||
1928|Blantyre Sandstone|30102|6|Mentioned|p27|||See also P31||||||
1928|Blantyre Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
1928|Blantyre Sandstone|31121|4|Described|p389|||||||||
1928|Blantyre Sandstone|32138|6|Mentioned|p393|||||||||
1928|Blantyre Sandstone|32553|4|Described|p38|||||||||
1928|Blantyre Sandstone|33086|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
1928|Blantyre Sandstone|35560|6|Mentioned|p288|||||||||
1928|Blantyre Sandstone|35562|6|Mentioned|p298|||||||||
1928|Blantyre Sandstone|36243|6|Mentioned|Table 6A|||||||||
1928|Blantyre Sandstone|37608|3|Fully described|Table 1|||||||||
1928|Blantyre Sandstone|39445|5|Briefly described|Table 10|||||||||
1928|Blantyre Sandstone|39943|6|Mentioned|Table 8A|||||||||
1928|Blantyre Sandstone|40623|5|Briefly described|p112|||||||||
1928|Blantyre Sandstone|44081|14|Not recorded|p131||Jurassic|Probably Jurassic.||||||
1928|Blantyre Sandstone|44414|14|Not recorded|p114,115||Jurassic|||||||
1928|Blantyre Sandstone|48908|14|Not recorded|Tb.1||Jurassic|||||||
1928|Blantyre Sandstone|48995|5|Briefly described|p72|||Age and thickness only described.||||||
1928|Blantyre Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. ||||Unconformably overlies Moolayember Formation. Is overlain by Westbourne Formation.||
1928|Blantyre Sandstone|67323|5|Briefly described|p106|Jurassic|Jurassic|Mount Isa Inlier.||||||
1928|Blantyre Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Eromanga and Carpentaria Basins. This unit is mapped with the Eulo Queen Group under the symbol, Ju.||||||
1928|Blantyre Sandstone|69594|5|Briefly described|p527|Late Jurassic|Middle Jurassic|Casey (1970). NE Eromanga Basin. Age range from palynofloras. 40-90m thick. Deposited in fluvial and floodplain environments with local swamps.||||Laterally continuous with Ronlow beds. Is overlain unconformably by Gilbert River Formation locally.|Quartzose sandstone; minor mudstone, carbonaceous shales and coal.|
1928|Blantyre Sandstone|71394|5|Briefly described|p1, p5, p22|Jurassic|Jurassic|Galilee Basin. A field transect across this unit is provided and at each stop where it occurs it is described.||||Overlies the Warang Sandstone.|White, poorly sorted, quartzose, coarse- to very coarse-grained pebbly sandstone.|
1928|Blantyre Sandstone|72088|6|Mentioned|p25, p30|||Forms the majority of The Pyramid rock formation.||||Overlain by the Gilbert River Formation.||
1928|Blantyre Sandstone|72298|6|Mentioned|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD).||||||
1928|Blantyre Sandstone|73472|6|Mentioned|p114, p120, p122|Jurassic|Jurassic|||||||
1937|Blazan Shale|22954|6|Mentioned|Fig3p9|Undillan|Early Cambrian|||||||
1937|Blazan Shale|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Interfingers with Quita Formation.  Siltstone, shale, thin-bedded chert, fine-grained sandstone and rare beds of bituminous limestone.  Geological Province: Georgina Basin.||||||08-MAR-05
1937|Blazan Shale|30242|6|Mentioned|Fig.2|||||||||
1937|Blazan Shale|30479|6|Mentioned|p19|||See also Fig.3. Name should be dropped||||||
1937|Blazan Shale|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1937|Blazan Shale|33482|6|Mentioned|p6|||Equiv. Inca Formation||||||
1937|Blazan Shale|34287|6|Mentioned|Fig.3|||||||||
1937|Blazan Shale|35054|6|Mentioned|Table 23|||||||||
1937|Blazan Shale|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1937|Blazan Shale|35139|4|Described|Table.2|||||||||
1937|Blazan Shale|35553|6|Mentioned|p180|||Appendix containing description of Agnostid localities.||||||
1937|Blazan Shale|36234|6|Mentioned|p168|||||||||
1937|Blazan Shale|37572|4|Described|p158|||See also Fig.8||||||
1937|Blazan Shale|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
1937|Blazan Shale|38446|6|Mentioned|Table 23|||||||||
1937|Blazan Shale|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1937|Blazan Shale|39445|5|Briefly described|Table 4|||See also p62||||||25-JUL-06
1937|Blazan Shale|39690|6|Mentioned|Table 1|||||||||
1937|Blazan Shale|40856|5|Briefly described|p315|||||||||
1937|Blazan Shale|43105|5|Briefly described|Fig.4,p9.|||||||||
1937|Blazan Shale|44211|4|Described|p100,102|||See also Lexicon.||||||
1937|Blazan Shale|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
1937|Blazan Shale|44275|14|Not recorded|Map Legend|||||||||
1937|Blazan Shale|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
1937|Blazan Shale|45052|3|Fully described|p100|||M.Camb.||||||
1937|Blazan Shale|45079|5|Briefly described|p30|||Cambrian age||||||
1937|Blazan Shale|47058|6|Mentioned|p134|||||||||
1937|Blazan Shale|49027|5|Briefly described|p7|||||||||
1937|Blazan Shale|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin||||||11-MAY-05
1937|Blazan Shale|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Shaly siltstone.||||||
1937|Blazan Shale|63450|5|Briefly described|p78 Fig. 5, p81|Middle Cambrian|Middle Cambrian|Overlain by Georgina Limestone. Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
1937|Blazan Shale|64068|4|Described|p63, 62, 64, 69|Middle Cambrian|Middle Cambrian|Contains agnostine trilobites, brachiopods. Correlated with Arthur Creek Formation, Inca Formation, Roaring Siltstone, Devoncourt Limestone.||Of Narpa Group.||Disconformably overlies Beetle Creek Formation or Thorntonia Limestone. Conformably overlain by, and interdigitates with, Quita Formation.|Interbedded siliceous shale and sandstone; basal conglomerate.|05-APR-12
1937|Blazan Shale|64443|6|Mentioned|p40.|||||||Correlative of Wonarah Formation.||14-MAY-14
1937|Blazan Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin||Narpa Group|||Siliceous shale, chert, siltstone, fine arenite, conglomerate, dolomitic and bituminous limestone, phosphorite|
1937|Blazan Shale|67352|6|Mentioned|p69|||||||||
1937|Blazan Shale|67870|6|Mentioned|p43|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
1937|Blazan Shale|69443|5|Briefly described|p28:16, 22-23|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
1937|Blazan Shale|69591|5|Briefly described|p87, p90-91, p96, p98 Fig.2.91|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. 39-60m thick. Contains trilobite fossils. Is lithologically identical with the Inca Formation.||||Unconformably overlies Beetle Creek Formation; disconformably overlies Thorntonia Limestone. Is overlain disconformably by Quita Formation.|Siliceous shale with interbeds of sandstone and conglomerate near the base.|
1937|Blazan Shale|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Thorntonia Limestone. Overlain by Quita Formation.|Shale and siltstone.|
1937|Blazan Shale|72321|6|Mentioned|Fig 2|Drumian|Drumian|Toko Syncline, Georgina Basin. Australian stages: Floran to Undillan.||of Narpa Group.||||
1937|Blazan Shale|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
1937|Blazan Shale|73418|6|Mentioned|p3|||||Narpa Group||Lateral equivalent of Inca Formation||
1944|Blenheim Formation|22593|6|Mentioned|Table 1|||divided into informal Members||||||
1944|Blenheim Formation|22974|6|Mentioned|p17|||||||||
1944|Blenheim Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
1944|Blenheim Formation|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
1944|Blenheim Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||30-NOV-09
1944|Blenheim Formation|23161|4|Described|p29,30 table4|Early Permian|Early Permian|||||||
1944|Blenheim Formation|23430|5|Briefly described|p515|||||||||
1944|Blenheim Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
1944|Blenheim Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Back Creek Group.  Age: >259Ma.  Geological Province: Bowen Basin.||||||
1944|Blenheim Formation|29437|6|Mentioned|p136|||Permian||||||
1944|Blenheim Formation|30340|6|Mentioned|p2532|||Upper Permian age. Lithology||||||
1944|Blenheim Formation|30341|5|Briefly described|p143|||Upper Permian age||||||
1944|Blenheim Formation|31531|5|Briefly described|p13|||See also Table 1||||||
1944|Blenheim Formation|31687|6|Mentioned|p280|||Refers Dickins & Malone (1968)||||||
1944|Blenheim Formation|31690|6|Mentioned|p36|||||||||
1944|Blenheim Formation|32832|6|Mentioned|p1||Permian|||||||
1944|Blenheim Formation|32834|6|Mentioned|Table 3|||||||||
1944|Blenheim Formation|32945|6|Mentioned|p78|||See also PP79,80,81 & Fig.2 Permian||||||
1944|Blenheim Formation|32946|6|Mentioned|p910|||Bivalves||||||
1944|Blenheim Formation|32949|6|Mentioned|p441|||||||||
1944|Blenheim Formation|33711|6|Mentioned|Table 3|||||||||
1944|Blenheim Formation|33993|6|Mentioned|p311|||Permian||||||
1944|Blenheim Formation|34132|6|Mentioned|p5|||See also P2. Upper Permian||||||
1944|Blenheim Formation|35150|6|Mentioned|p422|||||||||
1944|Blenheim Formation|35160|6|Mentioned|p2|||||||||
1944|Blenheim Formation|35284|6|Mentioned|Fig.1|||||||||
1944|Blenheim Formation|35467|6|Mentioned|p177|||||||||
1944|Blenheim Formation|36739|6|Mentioned|Fig.2|||||||||
1944|Blenheim Formation|37079|6|Mentioned|p139|||||||||
1944|Blenheim Formation|37612|6|Mentioned|p282|||||||||
1944|Blenheim Formation|37918|6|Mentioned|p474|||||||||
1944|Blenheim Formation|38204|6|Mentioned|p80|||||||||
1944|Blenheim Formation|38917|6|Mentioned|p170|||||||||
1944|Blenheim Formation|39220|6|Mentioned|p43|||Fauna IV. See also P44||||||
1944|Blenheim Formation|39261|6|Mentioned|Fig.6|||||||||
1944|Blenheim Formation|39262|6|Mentioned|p121|||||||||
1944|Blenheim Formation|39267|4|Described|p234|||||||||
1944|Blenheim Formation|39273|6|Mentioned|p309|||||||||
1944|Blenheim Formation|39304|6|Mentioned|Photo 19.1|||||||||
1944|Blenheim Formation|39423|6|Mentioned|p53|||||||||
1944|Blenheim Formation|40093|6|Mentioned|p27|||||||||
1944|Blenheim Formation|40571|6|Mentioned|p36|||||||||
1944|Blenheim Formation|40685|5|Briefly described|p400|||||||||
1944|Blenheim Formation|40749|6|Mentioned|Fig.1|||||||||
1944|Blenheim Formation|41034|5|Briefly described|p367|||||||||
1944|Blenheim Formation|41191|6|Mentioned|Fig.3|||||||||
1944|Blenheim Formation|41246|6|Mentioned|Map legend|Permian||||||||
1944|Blenheim Formation|41666|6|Mentioned|p11|||||||||
1944|Blenheim Formation|41689|6|Mentioned|Table 1|||||||||
1944|Blenheim Formation|42120|6|Mentioned|p412|||||||||
1944|Blenheim Formation|42249|6|Mentioned|Table 1 P22|||||||||
1944|Blenheim Formation|42257|5|Briefly described|Table 1 P263|||||||||
1944|Blenheim Formation|42258|6|Mentioned|p275|||||||||
1944|Blenheim Formation|42378|5|Briefly described|p19|||||||||
1944|Blenheim Formation|42701|4|Described|p65|||||||||
1944|Blenheim Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
1944|Blenheim Formation|42994|6|Mentioned|p234|||||||||
1944|Blenheim Formation|43050|5|Briefly described|p4|||||||||
1944|Blenheim Formation|43099|6|Mentioned|Fig.2|||||||||
1944|Blenheim Formation|43213|5|Briefly described|p158|||The assigning of rocks to the Blenheim Subgroup by Olgers (1969) and Dickins and Malone (1973) was rejected by other authors who restrict the Subgroup to Formation status.|||Includes Scottville Member.|||
1944|Blenheim Formation|43475|14|Not recorded|p552-3,555||Permian|||||||
1944|Blenheim Formation|43882|14|Not recorded|p89|||Ref. to Malone et al.,1966a.(Homevale)||||||
1944|Blenheim Formation|44245|5|Briefly described|Map Legend||Permian|||||||
1944|Blenheim Formation|44409|14|Not recorded|Map Legend||Permian|||||||
1944|Blenheim Formation|44424|14|Not recorded|p293-301|||Now Blenheim Subgroup.||||||
1944|Blenheim Formation|44489|14|Not recorded|p69|||Abundant fossils.marine.||||||
1944|Blenheim Formation|44635|4|Described|p11,Tb.1,map||Late Permian|||||||
1944|Blenheim Formation|45031|14|Not recorded|p6|||Of Back Creek Group.||||||
1944|Blenheim Formation|48881|2|Defined|p1,8,12,22-24,45,Tb1||Late Permian|||||||
1944|Blenheim Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: northern Bowen Basin.||||||04-FEB-08
1944|Blenheim Formation|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Carbonaceous and micaceous labile sandstone, siltstone, shale, conquinite, minor conglomerate.||||||
1944|Blenheim Formation|60659|5|Briefly described|p20, p90|||Of the Back Creek Group. Carbonaceous and micaceous sandstone, siltstone, shale, coquinite and minor conglomerate. Locally rich in fossils with brachiopods, bivalves, gastropods, pectens and bryozoans. Geol Prov: Bowen Basin.||||||07-FEB-11
1944|Blenheim Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
1944|Blenheim Formation|61917|5|Briefly described|Map legend|Late Permian|Early Permian|Of the Back Creek Group. Carbonaceous and micaceous labile sandstone, siltstone, shale, coquinite, minor conglomerate.||||||
1944|Blenheim Formation|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Bowen Basin.||||Overlies Aldebaran Sandstone. Is overlain by Exmoor Formation.||
1944|Blenheim Formation|65388|4|Described|p189-190, 159, 170, 191|Wordian||Of Back Creek Group in northern Bowen Basin. Conformably overlies Gebbie Formation in eastern Bowen Basin. Unconformably overlies Silver Hills Volcanics, Anakie Metamorphic Group on western side of basin. Type section in Blenheim Creek. Thickness ranges from 700m in the type section to almost 1600m and deposited entirely in marine environments. Fossils tentatively correlated with Barfield Formation. Siltstone, pebbly sandstone to conglomerate and lithic to quartzose sandstone.||||||
1944|Blenheim Formation|65706|6|Mentioned|p16 Tbl.1,|Late Permian|Early Permian|||Of Back Creek Group.||||
1944|Blenheim Formation|67402|4|Described|p21, p45, p80 tbl BWN1, p84|Capitanian|Capitanian|Bowen Basin. See also p85 tbl BWN2, p165 tbl LPB1.||Back Creek Group||Overlies the Moonlight Sandstone. Overlain by the Fort Cooper and Moranbah Coal Measures.|Carbonaceous and micaceous labile sandstone, siltstone, shale, coquinite and minor conglomerate.|
1944|Blenheim Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by German Creek Formation. Underlain by Collinsville Coal Measures.||
1944|Blenheim Formation|68679|4|Described|p353, p378, p380-382|Permian|Permian|Jensen et al. (1966). Connors-Auburn Province. Bowen Basin. 725m thick. Offshore marine sediments.||Back Creek Group.|Moonlight Sandstone Member.|Unconformably overlies Collinsville Coal Measures and Gebbie Formation. Is overlain by Exmoor (progradationally) and German Creek Formations. Passes laterally into/equivalent to Maria Formation.|Micaceous siltstone (pebbly), labile sandstone, quartzose sandstone, prominent coquinite.|
1944|Blenheim Formation|71265|5|Briefly described|p589|Wuchiapingian|Wuchiapingian|Bowen Basin.||||Unconformably overlies Collinsville Coal Measures. Is overlain by Moranbah Coal Measures.||
1944|Blenheim Formation|71276|5|Briefly described|p294|Lopingian|Lopingian|Jensen, Gregory and Forbes (1966). Bowen Basin. In the Galilee Basin, this unit, with the Maria Formation, is known as the Ingelara Formation.||||||
1944|Blenheim Formation|71701|5|Briefly described|p155|Wuchiapingian|Wuchiapingian|Northern Area, Bowen Basin.||||Unconformably overlies the Collinsville Coal Measures. Overlain by the Moranbah Coal Measures.||
1944|Blenheim Formation|73036|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Carbonaceous and micaceous labile sandstone, siltstone, shale, coquinite, minor conglomerate.|
1944|Blenheim Formation|73037|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Carbonaceous and micaceous labile sandstone, siltstone, shale, coquinite, minor conglomerate.|
2168|Bondonga beds|22443|6|Mentioned|p863|||||||||
2168|Bondonga beds|23811|5|Briefly described|Map Legend|Sakmarian|Asselian|||||||11-JAN-10
2168|Bondonga beds|23812|5|Briefly described|p15|||||||||
2168|Bondonga beds|42378|6|Mentioned|Table 1 P9|||||||||
2168|Bondonga beds|60079|5|Briefly described|Map Legend|Permian|Early Permian|Conglomerate, sandstone, siltstone.||||||
2168|Bondonga beds|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic, locally pebbly arenite, clast to matrix supported sandy to muddy conglomerate, locally pebbly mudstone; minor siltstone; rare limestone and basalt.||||||
2168|Bondonga beds|63748|4|Described|p16, p17|Early Permian|Early Permian|Fault-bounded basin remnant enclosed within the Texas beds. Unconformably overlie Texas beds. Comprise massive orthoconglomerate, paraconglomerate, lithic arenite and minor siltstone. Also mentioned: p68.||||||07-FEB-11
2168|Bondonga beds|68005|5|Briefly described|p18, p22, pp35-36, p154, p170.|Early Permian|Early Permian|New England Fold Belt. Probable folding and local overturning apparent.||||Faulted against or unconformably overlies Texas beds.|Massive orthoconglomerate, paraconglomerate, lithic sandstone and minor siltstone.|
2168|Bondonga beds|68006|6|Mentioned|p26.|Permian|Permian|Marine sediments.||||||
2168|Bondonga beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Pikedale, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
2168|Bondonga beds|68679|5|Briefly described|p449 Fig.5.113, p451-452, p455|Permian|Permian|Occupies a linear, NW-trending fault-bounded basin remnant, from Mole valley (NSW) to N of Glen Lyon (QLD). The Queensland part is called the Glenlyon beds. Shown in a tectonic discrimination diagram (plots in the "ocean-floor" field) and a REE plot. Bedding is steeply dipping to overturned. Has early Permian marine fossils.||||Enclosed within Texas beds.|Includes massive conglomerate (with pebbles and cobbles of Texas beds), lithic sandstone and minor siltstone, pebbly mudstone and poorly fossiliferous limestone; thin, vesicular basalt with lobate probable pillow structures.|
2168|Bondonga beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||26-SEP-18
2168|Bondonga beds|70373|4|Described|p789-794 fig 3, p795-797 Tb 1, p798- 804|Permian|Early Permian|Shallow marine brachiopod fossils. Includes rhyolite dyke: quartz, altered K feldspar and plagioclase phenocrysts in aphanitic groundmass. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. Other ages obtained from this unit: 295+/-18 Ma 302.4+/-5.1Ma. All LA-ICP-MS on zircon. 1400m thick. Minimum age constrained by overlying Gibraltar Ignimbrite (251.6+/-3.2 Ma)|280.7+/-3 Ma  (LA-ICP-MS)|||Assumed to overlie Texas beds, contact probably faulted. Unconformably underlie Mosman Formation.Correlated with  Silver Spur, Pikedale, Terrica and Alum Rock beds. Cut by rhyolitic dyke.|Fine to coarse grained, graded and cross bedded sandstones. Massive clast and matrix supported conglomerates; clast-rich to clast poor mudstone matrix diamictite; slightly porphyritic basalt intruded.|
2168|Bondonga beds|71628|5|Briefly described|p10:3; p15:25; p17:4; p19: 110, 148, 168|Permian|Permian|Called the Silver Spur Beds by Shaw (1964).||||Is intruded by Apple Tree Gully Granodiorite, Racehorse Porphyry, Webbs Consols and Mole Leucogranites. Is faulted against Clive Leucomonzogranite and Dandahra Creek Leucosyenogranite.||
2182|Bonnor Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 351. I-Type.||||||
2182|Bonnor Creek Granite|23619|4|Described|p40 Table 2||Carboniferous|Also see p10. Cumbana Batholith Province.||||||
2182|Bonnor Creek Granite|41680|5|Briefly described|p106|||||||||
2182|Bonnor Creek Granite|42054|6|Mentioned|p272|||||||||
2182|Bonnor Creek Granite|42691|5|Briefly described|map legend|Paleozoic||||||||07-NOV-08
2182|Bonnor Creek Granite|43110|5|Briefly described|p53|||||||||
2182|Bonnor Creek Granite|43113|4|Described|Table 2 p25||Carboniferous|||||||
2182|Bonnor Creek Granite|43253|5|Briefly described|map legend||Carboniferous|||||||
2182|Bonnor Creek Granite|43259|4|Described|Appendix 1,p41.||Carboniferous|||||||
2182|Bonnor Creek Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
2182|Bonnor Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Claret Creek Supersuite.|||Hornblende-biotite granite to granodiorite; hydrothermally altered granodiorite, granite.|
2182|Bonnor Creek Granite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Pink to grey, hornblende-biotite granite to granodiorite.|
2193|Boogooramunya Granite|22846|6|Mentioned|p63||Triassic|Intruded by Boonara Granodiorite.||||||
2193|Boogooramunya Granite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||23-DEC-09
2193|Boogooramunya Granite|41738|6|Mentioned|p168|||Reserved as Boogooramunya||||||
2193|Boogooramunya Granite|41778|2|Defined|Table 3|Late Triassic||Described P376||||||
2193|Boogooramunya Granite|42054|6|Mentioned|p272|||||||||
2193|Boogooramunya Granite|43008|5|Briefly described|map legend|||||||||
2193|Boogooramunya Granite|63821|5|Briefly described|p32|Late Triassic|Late Triassic|Intrudes Boonara Granodiorite and Calgoa Diorite.||||||07-FEB-11
2193|Boogooramunya Granite|68679|5|Briefly described|p428-429|Late Triassic|Late Triassic|Northern New England Orogen.||||Intrudes Boonara Granodiorite, Calgoa Diorite.|Strongly altered, medium- to coarse-grained, leucocratic biotite granite to granophyre.|
2193|Boogooramunya Granite|72481|6|Mentioned|p429|||Topographically prominent occurrence southwest of Bundaberg.||||||
2209|Bool Creek beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
2209|Bool Creek beach sand|39495|6|Mentioned|p142|||||||||
2209|Bool Creek beach sand|62102|5|Briefly described|p367 Tb. 1|||Informal name for morphostratigraphic unit on southeast Queensland coast.||||||
2232|Booloumba beds|22845|1|Redefined|p7-9,36,39-42,6,74-7|Early Carboniferous|Late Devonian|Excludes Peters Creek Greenstone and Jimna Phyllite.  Correlates to Amamoor and Mount Clara beds.||||||
2232|Booloumba beds|23799|6|Mentioned|p18|||||||||
2232|Booloumba beds|38805|6|Mentioned|Fig.1|||||||||
2232|Booloumba beds|40051|4|Described|p5|||||||||
2232|Booloumba beds|41917|6|Mentioned|p521|||||||||
2232|Booloumba beds|43008|5|Briefly described|map legend|||||||||
2232|Booloumba beds|43077|5|Briefly described|p4|||||||||
2232|Booloumba beds|43588|6|Mentioned|p30||Late Devonian|||||||
2232|Booloumba beds|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
2232|Booloumba beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
2232|Booloumba beds|68679|5|Briefly described|p320-321, p326-327, p330-331, p387|||Murray et al. (1979); Sliwa (1994). North D'Aguilar Subprovince, northern New England Orogen. Occurs in a 20km-wide belt east of Jimna. An upper plate, deepwater marine succession exposed by late Carboniferous extension. Some rocks assigned to this unit by Murray et al. (1979) from the Bunya Phyllite (Murphy et al., 1976), were re-assigned as the Jimna Phyllite by Sliwa (1994). Contains upfaulted blocks of Peters Creek Greenstone. Probably equivalent to Amamoor beds.||||Encloses Peters Creek Greenstone. Is faulted against Cambroon beds, Jimna Phyllite and (probably) Cedarton Volcanics. Is intruded by Tungi Creek Granodiorite and Neurum Complex.|Deep-marine, simply deformed, interbedded meta-arenite, meta-argillite, green and red slate, quartzite and meta-basalt; the dominant rock association is interbedded, thin- to medium-bedded, fine-grained quartzose meta-arenite and meta-argillite.|
2233|Boomer Formation|22973|6|Mentioned|p7|||||||||
2233|Boomer Formation|23037|4|Described|p58,62,5,67,8,9,70,||Late Permian|Correlates to Moah Creek beds. Overlying unit Buck Creek Group.  Max. thickness 100 m.||||||
2233|Boomer Formation|23042|4|Described|p50,8,9,60,1, Fig 2||Permian|Of Back Creek Group. Max. thickness 300 m.||||||
2233|Boomer Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbm].  Lithic sandstone, siltstone, mudstone, rare conglomerate.||||||
2233|Boomer Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
2233|Boomer Formation|31656|4|Described|Table 1|||U.Permian||||||
2233|Boomer Formation|31658|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
2233|Boomer Formation|31659|4|Described|p68|Late Permian|Late Permian|Lithic sandstone, mudstone. See also Table 1.||||||08-OCT-08
2233|Boomer Formation|31979|4|Described|Table 1|||U.Perm.||||||
2233|Boomer Formation|31983|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
2233|Boomer Formation|32358|4|Described|p15|||Table 2||||||
2233|Boomer Formation|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
2233|Boomer Formation|32577|5|Briefly described|p23|||||||||
2233|Boomer Formation|34132|6|Mentioned|p2|||Upper Permian||||||
2233|Boomer Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
2233|Boomer Formation|35845|6|Mentioned|p86|||||||||
2233|Boomer Formation|36045|6|Mentioned|p333|||||||||
2233|Boomer Formation|36739|6|Mentioned|p17|||||||||
2233|Boomer Formation|37121|5|Briefly described|Table 1|||||||||
2233|Boomer Formation|38081|5|Briefly described|Table 1|||||||||
2233|Boomer Formation|39252|6|Mentioned|p21|||||||||
2233|Boomer Formation|39445|5|Briefly described|p105|||See also Table 8||||||
2233|Boomer Formation|41246|6|Mentioned|Map legend|Permian||||||||
2233|Boomer Formation|41475|6|Mentioned|p70|||||||||
2233|Boomer Formation|41922|4|Described|Table 1, P8|||||||||
2233|Boomer Formation|43017|6|Mentioned|p377|||||||||
2233|Boomer Formation|43994|14|Not recorded|Map Legend|||||||||
2233|Boomer Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
2233|Boomer Formation|44424|14|Not recorded|p293-301|||Part of Blenheim Subgroup.||||||
2233|Boomer Formation|45071|3|Fully described|Table 10|||See also p30.||||||13-APR-21
2233|Boomer Formation|48898|2|Defined|p39-42|Late Permian||See also pp1,7,17 etc. Name derived from the Boomer Range in the Duaringa Sheet area. Type section is in Leura Creek in the Duaringa 1:250,000 Sheet area (Grid references: base, 11662515; top, 11582441); it does not include the top part of the unit. The formation crops out mainly in the Boomer and Gogango Ranges.||||Unconformably to conformably overlies Back Creek Group. Overlain by Dinner Creek Conglomerate. Correlated with the Barfield and Flat Top Formations.|Interbedded very fine to medium-grained sandstone, dark siltstone, and carbonaceous claystone. The sandstone is thick-bedded in a few placeswhere it dominates the section; elsewhere siltstone is dominant.|13-APR-21
2233|Boomer Formation|48940|6|Mentioned|p19|||Refers Malone, Olgers & Kirkegaard (1969)||||||
2233|Boomer Formation|50213|5|Briefly described|Map legend|Permian|Permian|Of the Back Creek Group.  Lithic sandstone, siltstone, mudstone, rare conglomerate.||||||
2233|Boomer Formation|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Back Creek Group.||||||
2233|Boomer Formation|60480|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Of the Back Creek Group. Lithic sandstone, siltstone, mudstone, rare conglomerate.||||||
2233|Boomer Formation|60481|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Of the Back Creek Group. Lithic sandstone, siltstone, mudstone, rare conglomerate.||||||
2233|Boomer Formation|60557|5|Briefly described|p25|||Of the Back Creek Group.  Grey lithic sandstone.||||||09-JUN-05
2233|Boomer Formation|61035|5|Briefly described|p15, p39, p40, p41,  p42|Late Permian|Late Permian|Underlain by a unamned mudstone sequence. Geological Province: Bowen Basin. Consists of lithic sandstone and cleaved mudstone. Trace fossils are common.||||||07-FEB-11
2233|Boomer Formation|61782|5|Briefly described|p280|||Consists of arenites made up of acid tuff grains.||||||
2233|Boomer Formation|65388|4|Described|p183-185; p184, p46, 48, 55, 70, 141|Late Permian.|Late Permian|Bowen Basin. Defined from the Boomer and Gogango Ranges.  Reference section  along Anglewood Road. Up to 1000m thick. Correlated with Moah Creek beds, possibly Cottenham Sandstone Member or Flat Top Formation.  Overlies and is overlain by undivided Back Creek Group in places. Overthrust by Carmila beds. Age probably Late Permian. See also p163, 169, 173, 174, 176, 178, 437, 438||||||
2233|Boomer Formation|68008|6|Mentioned|p157, p179|||||||Probable correlative of Moah Creek beds.||
2233|Boomer Formation|68359|5|Briefly described|p8|Permian|Permian|Strathmuir Synclinorium, Bowen Basin. Early to Late Permian. Predominantly marine to shallow-marine facies.||||Unconformably overlies Glenprairie beds.|Contains abundant lithic sandstone as well as cleaved mudstone.|
2233|Boomer Formation|68679|5|Briefly described|p308, p344, p346, p353, p378, p380|||Mollan et al. (1969). Bowen Basin. Offshore marine turbidite fan deposits, interpreted as flysch. 1000m thick.||||Probably equivalent, at least in part, to Moah Creek beds. May correlate with Flat Top Formation or Cottenham Sandstone Member (Barfield Formation).|Lithic sandstone, cleaved mudstone.|
2257|Boonderoo beds|23430|5|Briefly described|p519|||Galilee Basin Province.||||||
2257|Boonderoo beds|30340|6|Mentioned|p2533|||Lower Permian age.||||||
2257|Boonderoo beds|39252|6|Mentioned|p13|||||||||
2257|Boonderoo beds|39943|6|Mentioned|Table 7A|||||||||
2257|Boonderoo beds|39989|6|Mentioned|p426|||||||||
2257|Boonderoo beds|39991|6|Mentioned|p428|||||||||
2257|Boonderoo beds|40123|6|Mentioned|p465|||||||||
2257|Boonderoo beds|41116|5|Briefly described|p431|||||||||
2257|Boonderoo beds|44081|5|Briefly described|p131|||Briefly described in French.||||||
2257|Boonderoo beds|67323|5|Briefly described|p84|Permian|Carboniferous|NE Galilee Basin.||||Is overlain unconformably by Betts Creek beds.||
2257|Boonderoo beds|68731|5|Briefly described|p199, p201 Fig 3.110|Early Permian|Late Carboniferous|Lithologically resembles the Jochmus Formation, which also contains glaciogene strata. ||||Unconformably overlain by the Betts Creek beds.||
2257|Boonderoo beds|71265|5|Briefly described|p589|Asselian|Kasimovian|NE Galilee Basin.||||Is overlain unconformably by Betts Creek Group.||
2257|Boonderoo beds|71394|5|Briefly described|p1|Early Permian|Early Permian|Galilee Basin. A field transect across this unit is provided and at each stop where it occurs it is described.||||Overlain by the Betts Creek beds. Overlies the Cape River beds.||
2257|Boonderoo beds|71701|5|Briefly described|p155|Asselian|Kasimovian|Northeastern Area, Galilee Basin.||||Unconformably overlain by the Betts Creek Group and the Warang Sandstone.||
2257|Boonderoo beds|71710|4|Described|p376, p379, p386|Early Permian|Early Permian|p376 in part reassigned to lower Jericho Formation. Described from Charters Towers-1, where it is now reassigned to Upper Jochmus Formation, but evidently still used in other areas. Varves and striated pebbles indicate some glacial influence. Age from biostratigraphic correlation with Jochmus Formation.||||Lithologically similar, and correlative to upper Jochmus Formation.|Mudstone with minor siltstone, sandstone and very minor conglomerate, carbonaceous shale, probably tuff and calcareous claystone.|16-NOV-20
2257|Boonderoo beds|72088|4|Described|p8, p18, p91|Sakmarian|Moscovian|North East Galilee Basin. Crops out in Porcupine Creek Gorge at the northern end of the Koburra Trough. Age equivalent to the upper Jericho and Jochmus formations. A glacial influence is indicated by striated and faceted pebbles.||||Unconformably overlain by the Betts Creek beds.|Interbedded sandstone, shale, siltstone, mudstone, conglomerate, tuff and minor coal.|
2257|Boonderoo beds|73472|4|Described|p114-117, p119, p131|Sakmarian|Kasimovian|Galilee Basin, north-eastern. Glacial depositional setting. Maximum thickness of 257 m (GSQ Hughenden 3-4 R core). Up to 172 m thick in outcrop within Porcupine Gorge.||||Unconformably underlain by Cape River Metamorphics (angular unconformity). Unconformably overlain by Betts Creek beds. Equivalent to Jericho and Jochmus formations (Joe Joe Group).|Interbedded sandstone, shales, mudstones, diamictites, and lesser conglomerates.|
2259|Boondooma Igneous Complex|22991|5|Briefly described|p324|Triassic|Permian|||||||
2259|Boondooma Igneous Complex|23799|3|Fully described|p78, p12 Tb. 1|Triassic|Permian|Previously included as part of Yarraman Complex (Hill and Denmead, 1960).  Parts intrude Chahpingah Meta-Igneous Complex and Fifer Creek Metamorphics.  Highly detailed lithology/petrology included in text.  See also p116.||||||
2259|Boondooma Igneous Complex|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
2259|Boondooma Igneous Complex|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
2259|Boondooma Igneous Complex|35101|3|Fully described|p73|||||||||
2259|Boondooma Igneous Complex|35161|6|Mentioned|p591|||||||||
2259|Boondooma Igneous Complex|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
2259|Boondooma Igneous Complex|36926|6|Mentioned|p165|||||||||
2259|Boondooma Igneous Complex|36954|6|Mentioned|p114|||||||||
2259|Boondooma Igneous Complex|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
2259|Boondooma Igneous Complex|37376|6|Mentioned|p491|||||||||
2259|Boondooma Igneous Complex|39445|5|Briefly described|Table 12|||||||||
2259|Boondooma Igneous Complex|39970|6|Mentioned|p61|||||||||
2259|Boondooma Igneous Complex|39998|6|Mentioned|Fig.18|||||||||
2259|Boondooma Igneous Complex|40475|6|Mentioned|Table 2|||||||||
2259|Boondooma Igneous Complex|40485|6|Mentioned|Fig.1|||||||||
2259|Boondooma Igneous Complex|40486|6|Mentioned|p84|||||||||
2259|Boondooma Igneous Complex|41917|6|Mentioned|p522|||||||||
2259|Boondooma Igneous Complex|42987|6|Mentioned|p31|||||||||
2259|Boondooma Igneous Complex|43008|5|Briefly described|map legend|||||||||
2259|Boondooma Igneous Complex|43858|5|Briefly described|32|||Intrudes Late Devonian - Early Carboniferous accretionary wedge sediments & metasediments||||||
2259|Boondooma Igneous Complex|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||
2259|Boondooma Igneous Complex|60077|5|Briefly described|Map legend|Triassic|Permian|Granodiorite, granite, diorite, adamellite, gabbro.||||||23-DEC-09
2259|Boondooma Igneous Complex|60371|5|Briefly described|Map Legend|Triassic|Triassic|Porphyritic biotite-hornblende granite; coarse-grained quartz-feldspar pegmatite; even grained biotite granite.||||||
2259|Boondooma Igneous Complex|64665|5|Briefly described|p57.|Triassic|Permian|Tarong Basin.||||Is overlain unconformably by Tarong beds.||
2259|Boondooma Igneous Complex|65003|5|Briefly described|p1, p5, p18, p22, p25, p26|Triassic|Permian|||||Intrudes the Maronghi Creek beds. Overlain by the Mooga Sandstone.||30-MAR-12
2259|Boondooma Igneous Complex|68679|5|Briefly described|p322-323, p397 Fig.5.77, p410, p413-416|Triassic|Permian|See also p472. Intrudes the Yarraman Subprovince. Proximity to this unit (and other named units) increases the metamorphic grade and intensity of deformation of rocks in the Fifer Creek Metamorphics. Forms W margin of Tarong Basin. Has lower Na2O and K2O and higher CaO. Geochemical plot. Numerous age determinations given within this range.|~277 Ma to ~215 Ma.|||Intrudes Chahpingah Meta-Igneous Complex, Maronghi Creek beds, Sugarloaf and Feifer Creek Metamorphics. Is overlain by Dangore Volcanics and Aranbanga Volcanic Group.|Fourteen phases described on p413-414; includes biotite granite, porphyritic biotite-hornblende granite, granodiorite, tonalite, quartz diorite, hydrothermally altered granite and kaolinised granite, pegmatite, dolerite. I-type; generally unfoliated.|
2259|Boondooma Igneous Complex|69582|5|Briefly described|p82, p86|Triassic|Permian|These rocks have anomalously low heat production relative to the mean crustal heat flow of the Australian continent. Rocks of this complex have been deeply weathered.|B|||Intrudes the Maronghi Creek beds.|Felsic rocks, granitioids and mafic intrusions.|
2259|Boondooma Igneous Complex|73450|6|Mentioned|p36|||||||Intruded by Toondahra Granite.||
2296|Booval Group|30058|6|Mentioned|p11|||||||||
2296|Booval Group|30086|6|Mentioned|p4|||Triassic||||||
2296|Booval Group|30087|4|Described|p3|||See also p4.||||||17-SEP-08
2296|Booval Group|31132|6|Mentioned|p148|||||||||
2296|Booval Group|32178|6|Mentioned|p2|||Tertiary||||||
2296|Booval Group|33368|6|Mentioned|p48|||Correl. with Petrie Fm.||||||
2296|Booval Group|33381|4|Described|p110|||See also pp115, 121. Tertiary.||||||17-SEP-08
2296|Booval Group|33881|5|Briefly described|p96|||||||||
2296|Booval Group|34070|6|Mentioned|p3|||Tertiary||||||
2296|Booval Group|34354|6|Mentioned|p3|||Tertiary. See also P12.||||||
2296|Booval Group|34505|6|Mentioned|p1|||Eocene - Oligocene. See also P3.||||||
2296|Booval Group|36779|6|Mentioned|p7|||||||||
2296|Booval Group|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
2296|Booval Group|37375|6|Mentioned|p474|||||||||
2296|Booval Group|38074|5|Briefly described|Table 1|||||||||
2296|Booval Group|38307|6|Mentioned|Fig.1|||||||||
2296|Booval Group|38441|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
2296|Booval Group|39445|6|Mentioned|Table 14|||||||||
2296|Booval Group|40247|6|Mentioned|p212|||||||||
2296|Booval Group|40623|5|Briefly described|p31|||||||||
2296|Booval Group|41906|3|Fully described|Table 4 p33|||||||||17-SEP-08
2296|Booval Group|42336|5|Briefly described|p6|||||||||
2296|Booval Group|42525|5|Briefly described|Map legend|Miocene|Paleocene|||||||
2296|Booval Group|43076|5|Briefly described|p11|||||||||
2296|Booval Group|43883|14|Not recorded|p18 Fig.4-3|||||||||
2296|Booval Group|44510|14|Not recorded|Fig.35|||||||||
2296|Booval Group|44581|14|Not recorded|p346|||Lies unconformably on Ipswich Coal Measures and Bundamba Group||||||
2296|Booval Group|44603|4|Described|p129-132||Cenozoic|(Early Cainozoic)||||||19-NOV-08
2296|Booval Group|44771|14|Not recorded|p3||Tertiary|||||||
2296|Booval Group|44775|14|Not recorded|Map 2||Tertiary|||||||
2296|Booval Group|44776|14|Not recorded|p1,4|Oligocene|Eocene|||||||
2296|Booval Group|44781|14|Not recorded|p355|||||||||
2296|Booval Group|44803|14|Not recorded|p149,153||Tertiary|Ref. to Hill and Denmead. (Early Tertiary)||||||
2296|Booval Group|61155|5|Briefly described|p19|Middle Eocene|Late Paleocene|Includes the Silkstone and Redbank Plains Formations.  In the Brisbane region.||||||03-MAR-10
2296|Booval Group|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley Group; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, 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.||||||
2296|Booval Group|68579|4|Described|p221,222|Oligocene|Eocene|Maximum observed thickness: 1046ft. Group recognises a continuity of deposition of alternating lacustrine and volcanic conditions from the base of the Redbank Plains Formation to the top of the Silkstone Formation.|||Includes Redbank Plains Formation, Silkstone Formation.|||26-APR-13
2296|Booval Group|69599|5|Briefly described|p586, p594|Eocene|Paleocene|Booval Basin. Capped by laterite and silcrete.|||Redbank Plains, Silkstone Formations.|Correlated with lower part of Oxley Group.||
2321|Border Waterhole Formation|23031|6|Mentioned|17|||Geological Province: Georgina Basin.||||||26-JUL-06
2321|Border Waterhole Formation|23393|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|23448|4|Described|p480|Cambrian|Cambrian|||||||
2321|Border Waterhole Formation|24419|6|Mentioned|p18|||Equivalent to Beetle Creek Formation on URANDANGI 1:250 000 sheet.||||||
2321|Border Waterhole Formation|29940|6|Mentioned|p169|||||||||
2321|Border Waterhole Formation|30479|6|Mentioned|p15|||See also fig.3. Author suggests name should be dropped.||||||26-JUL-06
2321|Border Waterhole Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2321|Border Waterhole Formation|31396|6|Mentioned|Fig.3|||||||||
2321|Border Waterhole Formation|33111|6|Mentioned|p26|||||||||
2321|Border Waterhole Formation|33482|6|Mentioned|p3|||Equiv. Beetle Creek Formation||||||
2321|Border Waterhole Formation|35001|6|Mentioned|p251|||||||||
2321|Border Waterhole Formation|35054|6|Mentioned|Table 23|||||||||
2321|Border Waterhole Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
2321|Border Waterhole Formation|36645|6|Mentioned|p308|||||||||
2321|Border Waterhole Formation|37572|4|Described|p157|||||||||
2321|Border Waterhole Formation|38291|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|38348|6|Mentioned|p24|||||||||
2321|Border Waterhole Formation|38446|6|Mentioned|Table 23|||||||||
2321|Border Waterhole Formation|39422|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Chert, siltstone, chert breccia, phophorite. Conformably overlain by Currant Bush Limestone; unconformably over rocks of the McNamara Group Top Rocky Rhyolite (Carrara Range Group).||||||10-JAN-05
2321|Border Waterhole Formation|39445|5|Briefly described|Table 4|||See also p62||||||26-JUL-06
2321|Border Waterhole Formation|39497|6|Mentioned|p14|||See also 16||||||26-JUL-06
2321|Border Waterhole Formation|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|40852|6|Mentioned|p37|||||||||
2321|Border Waterhole Formation|40856|5|Briefly described|p315|||||||||
2321|Border Waterhole Formation|41240|6|Mentioned|p112|||||||||
2321|Border Waterhole Formation|41639|5|Briefly described|p4|||||||||
2321|Border Waterhole Formation|43652|6|Mentioned|Fig.15,p393|||||||||
2321|Border Waterhole Formation|44211|14|Not recorded|p100|||||||||
2321|Border Waterhole Formation|44274|2|Defined|Tb.1,p7,11,13,map||Middle Cambrian|Overlies Camooweal Dolomite. On QLD and NT white cards. (Not according to Mt Drummond 250K map, 2006)||||||09-AUG-06
2321|Border Waterhole Formation|44275|14|Not recorded|Map Legend|||||||||
2321|Border Waterhole Formation|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
2321|Border Waterhole Formation|44482|14|Not recorded|p.11,15, opp.p.6;map|||(E53-12).||||||
2321|Border Waterhole Formation|44483|5|Briefly described|map legend||Middle Cambrian|Middle Cambrian.||||||
2321|Border Waterhole Formation|44920|14|Not recorded|Map Legend||Middle Cambrian|||||||
2321|Border Waterhole Formation|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||01-JUL-04
2321|Border Waterhole Formation|45032|14|Not recorded|p8,10||Middle Cambrian|Tb.1, Pl.1. (E53-12).||||||
2321|Border Waterhole Formation|45052|3|Fully described|p91|||M.Camb.||||||
2321|Border Waterhole Formation|45079|6|Mentioned|p22|||Lower Middle Cambrian age. Should be included in Beetle Creek Formation||||||
2321|Border Waterhole Formation|45166|5|Briefly described|Table 15|||||||||
2321|Border Waterhole Formation|46792|6|Mentioned|p51|||Trilobite fauna.||||||26-JUL-06
2321|Border Waterhole Formation|47058|6|Mentioned|Fig.8 P129|||||||||
2321|Border Waterhole Formation|50600|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlain by Thorntonia Limestone.  Chert, chert breccia, siltstone, phosporite.||||||28-JUN-04
2321|Border Waterhole Formation|61904|5|Briefly described|p132 Fig. 2|Cambrian|Cambrian|Carbonates. See also p134.||||||
2321|Border Waterhole Formation|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Bioclast and bioclast ooid rudstone, commonly chertified.||||||
2321|Border Waterhole Formation|64068|6|Mentioned|p185, p59, 225|||Of northeastern Georgina Basin. Correlated with Thorntonia Limestone. Broken Hill South identified small phosphate deposits in this unit straddling the NT-Queensland border.||||||21-MAR-16
2321|Border Waterhole Formation|64317|5|Briefly described|p589|||Of Stewart and Mitchell (1987); Lindsay and Brasier (2006). Consists of siliceous breccia bordering the interior edge of Thorntonia Limestone annulus structure.  Mainly chert clasts and clumps of semi-consolidated muddy sediments containing chert nodules.||||||23-SEP-08
2321|Border Waterhole Formation|65337|3|Fully described|p9 Fig.5, p64, p75.|Middle Cambrian|Middle Cambrian|Southeast MOUNT DRUMMOND area. Hosts the Highland Plains phosphate deposit; 84 Mt @ 13.4% P^20^5 (Cook and Shergold 1979). Reported fossils include Ordian-age trilobites, molluscs and hyoliths.||Unit in Narpa Group.||Unconformably overlies McNamara Group. Is overlain by Currant Bush Limestone.|Siliceous shale, siltstone, chertified limestone, bedded to nodular chert; basal quartz-lithic sandstone, granule to pebble conglomerate.|
2321|Border Waterhole Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group|||Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
2321|Border Waterhole Formation|69418|6|Mentioned|p3:31|||Georgina Basin. Hosts the Highland Plains phosphate deposit (briefly described).||||||12-JUL-16
2321|Border Waterhole Formation|69437|5|Briefly described|p22:9-10|Series 2|Series 2|Eastern Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 1.||||Correlated with Thorntonia Limestone.||12-JUL-16
2321|Border Waterhole Formation|69443|4|Described|p28:16, 19-20, 43|Middle Cambrian|Middle Cambrian|Opik (1960). Undilla Sub-basin, Georgina Basin. Outcrops are typically obscured by regolith of chert breccia and pebbles. 30-180m thick. Fossiliferous. Shallow-marine deposits. Hosts the Highland Plains phosphate deposit.||Narpa Group.||Unconformably overlies Lawn Hill Formation. Is overlain conformably or disconformably by the Currant Bush Limestone. Grades laterally into, and interfingers with, Thorntonia Limestone.|Siliceous shale, siltstone, grey and black chertified limestone (including bioclast floatstone and rudstone), irregularly bedded to nodular chert, chert breccia, chert conglomerate and a basal pebble conglomerate.|12-JUL-16
2321|Border Waterhole Formation|69446|6|Mentioned|p31:3|||Georgina Basin. Broadly age-equivalent to Daly River Group(Daly Basin).||||||12-JUL-16
2321|Border Waterhole Formation|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
2321|Border Waterhole Formation|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
2321|Border Waterhole Formation|69591|5|Briefly described|p88, p96|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||||
2321|Border Waterhole Formation|69673|5|Briefly described|p116, p117, p142|||180m thick.||Narpa Group|||Shale, siltstone, chertified limestone, chert and conglomerate.|
2321|Border Waterhole Formation|70380|6|Mentioned|p745|Stage 5|Stage 4|Undilla Sub-basin, Georgina Basin.||||||
2321|Border Waterhole Formation|72297|5|Briefly described|p732|Middle Cambrian|Middle Cambrian|Georgina Basin. One of the two major producers of phosphate in QLD.|||||Marine sequences of phosphorite (phosphatic siltstone) and chert, overlying limestone, sandstone and conglomerate.|
2321|Border Waterhole Formation|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Narpa Group.||Overlain by Camooweal Dolomite or Thorntonia Limestone. Underlain by Colless Volcanics.|Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|72415|4|Described|mapsheet|Early Ordovician|Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Narpa Group.||Overlain by Camooweal Dolomite or Thorntonia Limestone. Underlain by Colless Volcanics.|Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
2333|Boree Salt|41289|6|Mentioned|p211|||||||||
2333|Boree Salt|43105|5|Briefly described|p11|||||||||
2333|Boree Salt|62985|5|Briefly described|p16|Givetian|Givetian|Halite-dominated unit  deposited in a restricted basin. Unconformably overlain by Etonvale Formation. Geol. prov: Adavale Basin.||||||24-JAN-07
2333|Boree Salt|64783|4|Described|p99-100, p82, 84, 87,96, 97, 98, 104|Givetian|Givetian|Gerrad (1964) first named this unit, in AOP Boree-1, the Boree Formation. Tanner (1968) referred to it as the Boree Salt member (of the Etonvale Formation). Boreham and de Boer (1998) used the Boree Salt, showing the unit as separate to the Etonvale Formation. Its type section is 1919.6-2426.51 m in Boree-1 (Galloway, 1970). Up to 584m thick.||||Conformably overlies the Cooladdi Dolomite and Bury Limestone. Is overlain unconformably by Etonvale Formation.|Consists mostly of halite and includes minor amounts of claystone, calcareous siltstone and shale, limestone, gypsum, anhydrite and argillaceous sandstone. Also includes interbeds of potassium minerals such as sylvite and koenenite.|15-NOV-17
2333|Boree Salt|67402|4|Described|p167 fig ADV/WRR3|Givetian|Givetian|Adavale Basin. 584m thick. See also p168, p170, fig ADV/WRR7, p173 tbl ADV/WRR2, p175.||||Overlies or grades into the Cooladdi Dolomite.|Rock halite with minor claystone, calcareous siltstone and shale, limestone, gypsum, anhydrite and argillaceous sandstone.|
2333|Boree Salt|68731|5|Briefly described|p177 Fig 3.91, p180 Tb 3.3, p222|Late Devonian|Middle Devonian|Adavale Basin. ~ 77-584 m thick.||||Overlain by the Bury Limestone.|Comprises predominantly rock salt. Minor rock types include claystone, calcareous siltstone and shale, limestone, gypsum, anhydrite and argillaceous sandstone. Generally contains calcareous to dolomitic cements, and are grey to red and green.|
2347|Bortala Formation|22438|6|Mentioned|p549, Fig.12|||||||||
2347|Bortala Formation|22585|6|Mentioned|Fig3 P738|||Actually written as Bortala Fm.||||||26-JUL-06
2347|Bortala Formation|23031|5|Briefly described|p24|||Geol. province: Mount Isa Fold Belt. Of the Myally Subgroup. Overlying unit: Witworth Quartzite, underlying unit: Alsace Quartzite||||||26-JUL-06
2347|Bortala Formation|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||26-JUL-06
2347|Bortala Formation|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup.  Geological Province: Western Fold Belt.||||||
2347|Bortala Formation|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Alsace Quartzite; Underlies the Whitworth Quartzite.||||||25-AUG-04
2347|Bortala Formation|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|33900|4|Described|p12|||||||||
2347|Bortala Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|38232|6|Mentioned|p84|||||||||
2347|Bortala Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|39445|5|Briefly described|Table 2|||See also p40||||||26-JUL-06
2347|Bortala Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Flaggy, fine feldspathic siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey-green chert.Overlies the Alsace Quartzite.||||||15-JUN-06
2347|Bortala Formation|39622|6|Mentioned|Fig.2|||||||||
2347|Bortala Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
2347|Bortala Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|40221|3|Fully described|p8|||||||||
2347|Bortala Formation|40623|5|Briefly described|p99|||||||||
2347|Bortala Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
2347|Bortala Formation|41307|4|Described|p10|||||||||
2347|Bortala Formation|42503|6|Mentioned|p336|||||||||
2347|Bortala Formation|42523|5|Briefly described|Fig. 2 p373|||||||||26-JUL-06
2347|Bortala Formation|42676|5|Briefly described|Fig.2, P41|||||||||
2347|Bortala Formation|45136|3|Fully described|p24|||||||||
2347|Bortala Formation|45166|5|Briefly described|p14|||||||||
2347|Bortala Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
2347|Bortala Formation|47083|4|Described|p7|||Of Myally Subgroup of Haslingden Gp. O'lying unit: Whitworth Quartzite - conformable. U'lying: unit Alsace Quartzite - conformable. Maximum thickness: 500 m.||||||26-JUL-06
2347|Bortala Formation|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
2347|Bortala Formation|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
2347|Bortala Formation|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup. ||||||
2347|Bortala Formation|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
2347|Bortala Formation|63023|5|Briefly described|p1025 Fig. 2, p1029|Paleoproterozoic|Paleoproterozoic|Of Myally Subgroup (Haslingden Group). Age: 1773+/-2Ma. Overlies Alsace Quartzite; overlain by Whitworth Quartzite. Geological Province: Leichardt Superbasin. Comprises pink feldspathic sandstone, recessive siltstone and shale. See also p1027 Tb. 1.||||||07-NOV-08
2347|Bortala Formation|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Whitworth Quartzite, underlain by Alsace Quartzite. Geological Province: Leichhardt Superbasin. Consists of siltsone.||||||
2347|Bortala Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Haslingden Group||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.||
2347|Bortala Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
2347|Bortala Formation|63116|6|Mentioned|p1297 Fig.2, p1299-1301, p1305, p1308|||Leichhardt superbasin. Material properties detailed. A seal above the Eastern Creek Volcanics.||||||
2347|Bortala Formation|63866|5|Briefly described|p58|Statherian|Statherian|Leichhardt Superbasin. Numeric age is a maximum depositional date.|1773 +/- 3 Ma (Neumann et al., 2006)|Myally Supersequence||Overlain by the Quilalar Formation.||
2347|Bortala Formation|65505|6|Mentioned|979|Proterozoic|Proterozoic|Of the Leichhardt River Fault Trough. Age: 1773 +/-2 Ma.||||||
2347|Bortala Formation|67323|4|Described|GIS attrib tbl, Solid Geology Map, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Leichhardt Superbasin. Leichhardt River Domain, Mount Isa Inlier.|1773 +/- 2 Ma.|Myally Subgroup.||Overlies Eastern Creek Volcanics?|Flaggy, fine feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey - green chert.|
2347|Bortala Formation|68732|6|Mentioned|p160, p161, p165|Statherian|Statherian|Sedimentary depositional age from a volcaniclastic unit. Of the Myally Supersequence.|1773 +/- 2 Ma||||Mainly very fine-grained arkosic sandstones.|30-NOV-17
2347|Bortala Formation|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||09-FEB-18
2347|Bortala Formation|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Storm-dominated shelf deposits.|1773 +/- 2 Ma (Neumann et al., 2006).|Myally Subgroup.|||Flaggy, fine feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey-green chert.|
2347|Bortala Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.|Flaggy, fine-grained feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone and grey-green chert.|
2347|Bortala Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.|Flaggy, fine-grained feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone and grey-green chert.|
2347|Bortala Formation|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1780+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Mudstone.|
2347|Bortala Formation|71960|6|Mentioned|p105|||||||||
2347|Bortala Formation|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Stacked channel fills at base; generally heterolithic, inshore, transitional, tidal||Of Myally Subgroup|||Pebbly sandstone at base, overlain by siltstone-mudstone, siltstone-feldspathic sandstone, siltstone-mudstone; sandstone throughout.|
2347|Bortala Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Alsace Quartzite and underlies Lochness Formation.||
2347|Bortala Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Alsace Quartzite and underlies Lochness Formation.||
2347|Bortala Formation|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
2347|Bortala Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Alsace Quartzite. Overlain by Lochness Formation.||
2347|Bortala Formation|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
2360|Bottletree Formation|22623|6|Mentioned|p225||Proterozoic|Replaced by Kurbayia Migmatite?||||||18-JAN-07
2360|Bottletree Formation|23054|6|Mentioned|p9|||||||||
2360|Bottletree Formation|23363|5|Briefly described|344 Fig.3|Statherian|Statherian|Age: ~1790Ma.||||||18-JAN-07
2360|Bottletree Formation|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
2360|Bottletree Formation|23395|5|Briefly described|p385|Statherian|Statherian|Age: 1790+/-9Ma.||||||18-JAN-07
2360|Bottletree Formation|23396|5|Briefly described|p418|Statherian|Statherian|Age: 1790+/-9Ma.||||||18-JAN-07
2360|Bottletree Formation|23398|5|Briefly described|p456|Statherian|Statherian|Age: 1770-1780Ma.||||||18-JAN-07
2360|Bottletree Formation|23466|5|Briefly described|p265|||||||||
2360|Bottletree Formation|24197|5|Briefly described|p27, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Argylla Suite. Age: 1780Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
2360|Bottletree Formation|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2360|Bottletree Formation|24419|5|Briefly described|p16, p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Recrystallised felsic volcanics, interbedded schistose metagreywacke, medium-grained sericitic and feldspathic meta-arenite, and meta-arkose. Underlies the Haslingden Group.  Age: ~1790Ma (Page 1983).  Geol.Prov: Western Fold Belt. See also p15 Fig. 6.||||||07-NOV-08
2360|Bottletree Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlain by Mount Guide Quartzite.||||||
2360|Bottletree Formation|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
2360|Bottletree Formation|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2360|Bottletree Formation|37862|4|Described|p582|||||||||
2360|Bottletree Formation|38232|6|Mentioned|p82|||||||||
2360|Bottletree Formation|38234|4|Described|p103|||||||||
2360|Bottletree Formation|38310|6|Mentioned|p237|||||||||
2360|Bottletree Formation|38350|4|Described|p8|||||||||
2360|Bottletree Formation|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
2360|Bottletree Formation|38560|6|Mentioned|p114|||||||||
2360|Bottletree Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
2360|Bottletree Formation|38827|6|Mentioned|p109|||||||||
2360|Bottletree Formation|38834|6|Mentioned|p162|||||||||
2360|Bottletree Formation|38900|6|Mentioned|p55|||||||||
2360|Bottletree Formation|39202|5|Briefly described|p229|||||||||
2360|Bottletree Formation|39445|5|Briefly described|Table 2|||See also p35 and p39.  Age C1800 Ma.||||||30-JAN-07
2360|Bottletree Formation|39622|6|Mentioned|p19|||See also Fig.2||||||
2360|Bottletree Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
2360|Bottletree Formation|39934|6|Mentioned|Fig.3|||||||||
2360|Bottletree Formation|40840|6|Mentioned|Map legend|||||||||
2360|Bottletree Formation|41277|6|Mentioned|p83|||||||||
2360|Bottletree Formation|41381|6|Mentioned|p323|||||||||
2360|Bottletree Formation|41465|5|Briefly described|p11|||||||||
2360|Bottletree Formation|41978|6|Mentioned|p495|||||||||
2360|Bottletree Formation|41979|6|Mentioned|p533|||||||||
2360|Bottletree Formation|42523|5|Briefly described|p372|||||||||
2360|Bottletree Formation|42565|4|Described|Table 1 P6, P2|||||||||
2360|Bottletree Formation|42676|5|Briefly described|Fig.2 p41|||||||||25-JAN-19
2360|Bottletree Formation|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group. Age: ~1790Ma. Conglomerate, greywacke, felsic and mafic volcanics.||||||09-FEB-09
2360|Bottletree Formation|42818|4|Described|p206, Table 1 p207|||Of the Haslingden Group?||||||30-JAN-07
2360|Bottletree Formation|43052|5|Briefly described|p62|||||||||
2360|Bottletree Formation|43608|6|Mentioned|Fig.11,p11|||||||||
2360|Bottletree Formation|43616|6|Mentioned|p3|||||||||
2360|Bottletree Formation|43734|6|Mentioned|p14|||||||||
2360|Bottletree Formation|44195|6|Mentioned|p356 Fig.9|||||||||
2360|Bottletree Formation|45161|4|Described|p21|||||||||
2360|Bottletree Formation|45162|6|Mentioned|p11|||Originally wrongly entered as NT.||||||
2360|Bottletree Formation|45166|4|Described|p13|||See also p14.||||||18-JAN-07
2360|Bottletree Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
2360|Bottletree Formation|46995|5|Briefly described|p267|||||||||
2360|Bottletree Formation|46996|6|Mentioned|p273|||||||||
2360|Bottletree Formation|49009|2|Defined|p6|Proterozoic|Proterozoic|Mapped as Leichhardt Metamorphics, Argylla Formation, Mount Guide Quartzite (Carter and Opik).||||||18-JUL-13
2360|Bottletree Formation|49041|6|Mentioned|Table 4|||||||||
2360|Bottletree Formation|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Contains recrystallised felsic volcanics and interbedded schistose metagreywacke, medium-grained sericitic and feldspathic meta-arenite, and meta-arkose.  Unconformably overlain by the Haslingden Group.  Geological Province: Western Fold Belt Province.||||||18-JAN-07
2360|Bottletree Formation|50332|5|Briefly described|p10, p17|Paleoproterozoic|Paleoproterozoic|Overlain by the Haslingden Group. Age: 1800-1755Ma. Contains recrystallised felsic volcanics (dated at ~1790Ma by Page, 1983b) + interbedded sedimentary rocks.||||||07-FEB-11
2360|Bottletree Formation|50536|5|Briefly described|p1.4, 4.1, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Argylla Suite.  Age: 1790-1808 +/- 19Ma (U-Pb).||||||07-NOV-08
2360|Bottletree Formation|50605|6|Mentioned|p11.1|||Geological Province: Mount Isa Inlier.||||||
2360|Bottletree Formation|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
2360|Bottletree Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Felsic and mafic metavolcanics; greywacke conglomerate, greywacke.||||||
2360|Bottletree Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
2360|Bottletree Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
2360|Bottletree Formation|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1790+/-9Ma. ||||||07-NOV-08
2360|Bottletree Formation|61936|5|Briefly described|p193|||Deep marine deposits. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||
2360|Bottletree Formation|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: <1790Ma. Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
2360|Bottletree Formation|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Age: 1790+/-9Ma. (Page 1983). Included in the Guide Supersequence. Geological Province: Mount Isa Inlier.||||||07-NOV-08
2360|Bottletree Formation|63023|5|Briefly described|p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1790+/-9Ma. Geological Province: Leichhardt Superbasin. Dominated by felsic volcanic rocks. This unit together with Mount Guide Quartzite form the Guide Supersequence.||||||18-JUL-13
2360|Bottletree Formation|63109|6|Mentioned|p1111|||Proximal fluvial sandstone.||||||30-SEP-08
2360|Bottletree Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Mount Guide Quartzite. Age: 1790+/-9Ma (U/Pb zircon). Thickness: ca. 3000m, Composed of poorly sorted and immature, coarse-to fine grained sandstone, pebbly sandstone and conglomerate. Geological Province: Leichhardt Superbasin.||||||18-JUL-13
2360|Bottletree Formation|63114|6|Mentioned|p1253 Fig.2. |||||||Is overlain by Mount Guide Quartzite.||
2360|Bottletree Formation|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt. 3000m thick.|||||Conglomerate, greywacke, volcanics.|
2360|Bottletree Formation|63866|5|Briefly described|p58|Statherian|Orosirian|Leichhardt Superbasin. Numeric age is derived from Page, 1983.|1790 +/- 15 Ma (U-Pb zircon TIMS)||||Felsic and mafic volcanic rocks.|
2360|Bottletree Formation|64250|5|Briefly described|p17 fig 7, p11 fig 3, p19, p21, p22-24|||Leichhardt River Fault Trough, Western Fold Belt, Mount Isa Inlier.|1790 +/- 9 Ma||||Bimodal (felsic-dominated) volcanism.|14-MAR-18
2360|Bottletree Formation|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Age: 1790+/-9Ma.||||||07-FEB-11
2360|Bottletree Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
2360|Bottletree Formation|64742|6|Mentioned|p332.|||Mount Isa Inlier.|1780-1770 Ma.|||||
2360|Bottletree Formation|64834|5|Briefly described|p13 Fig.2, p35-36|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.||||Unconformable base.|Conglomerate, with cobble bed near base, and volcanics.|
2360|Bottletree Formation|65337|5|Briefly described|p5, p11. |||Leichhardt Superbasin; Leichhardt River Fault Trough.|1790 Ma (Blake and Stewart 1992).|||Is overlain by Haslingden Group.||
2360|Bottletree Formation|65376|5|Briefly described|p231.|||Geochemically similar to Myola Volcanics and felsic units of Tidnamurkuna Volcanics.|c.1790 Ma.|||||
2360|Bottletree Formation|65396|5|Briefly described|p16, p82, p175, p187, p190, p192-197|Statherian|Statherian|See also p241. Western Fold Belt. Leichhardt Superbasin. Cover Sequence 2. Formations with detrital zircons from this unit are listed.|1790 +/- 9 Ma|||Overlain by Mount Guide Quartzite.|Felsic and lesser mafic volcanics with some quartzite/sandstone.|
2360|Bottletree Formation|66302|6|Mentioned|p63|Statherian|Statherian|Has similar chemistry to the Tidnamurkuna and Myola Volcanics. |ca. 1790-1780 Ma (Wyborn et al, 1987)|||||
2360|Bottletree Formation|66529|6|Mentioned|p32, p34  |||Leichhardt Superbasin rift fill.|||||Shallow-marine siliciclastics and volcanic rocks.|
2360|Bottletree Formation|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1790 +/- 9 Ma (Page et al. 2000).|||||24-APR-12
2360|Bottletree Formation|67323|5|Briefly described|p12,13, p39, p107; GIS attrib tbl|Statherian|Statherian|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Leichhardt Superbasin. Oldest unit in Leichhardt River Domain, Mount Isa Inlier. Another age: 1808 +/- 19 Ma.|1790 +/- 9 Ma.|||In contact with Kalkadoon Granite at domain boundary.|Metabasalt, metarhyolite, quartzite, epidotic quartzite, metagreywacke, metasiltstone, mica schist, conglomerate.|
2360|Bottletree Formation|67539|5|Briefly described|p7|Statherian|Statherian|Correlated with areas previously considered 'basement'. Forms a distinctive strongly magnetic belt on regional magnetic images.|~ 1785 Ma||||Comprises metamorphosed, locally gneissic, felsic and acid meta-volcanics.|
2360|Bottletree Formation|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Part of Guide Supersequence, Leichhardt Superbasin, Western Succession.||||?Overlain by Mount Guide Quartzite.||
2360|Bottletree Formation|68146|6|Mentioned|p1, p194|||Coeval with c.1795 Ma Big Toby Granite and other units (listed).|1790 +10/-8 Ma; Page (1983).||||Intermediate volcanics.|
2360|Bottletree Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||Is overlain conformably by Haslingden Group.||
2360|Bottletree Formation|68575|6|Mentioned|p1, p82, p84, p124|||May be related to the subvolcanic intrusive Paper Tank Microgranite, 15km to the south and of a similar age.||||||
2360|Bottletree Formation|68732|6|Mentioned|p160, p161, p165 Fig.3|Statherian|Statherian|Of the Guide Supersequence. Igneous crystallisation age.|1790 +/- 9 Ma|Of the Haslingden Group.||||01-FEB-17
2360|Bottletree Formation|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|Statherian|Statherian|Leichhardt River Fault Trough. Part of a thick rift-sag sequence.|1790 +/- 9 Ma|||Overlain by Mount Guide Quartzite||09-FEB-18
2360|Bottletree Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Is overlain by Mount Guide Quartzite.||25-JAN-19
2360|Bottletree Formation|69591|5|Briefly described|p29, p33, p58|Paleoproterozoic|Paleoproterozoic|Basal stage of the Guide Supersequence. Subaerial, local fluvial environment.|1790 +/- 9 Ma (Page, 1983).|||Is overlain by Mount Guide Quartzite.|Metarhyolite, quartzite, epidotic quartzite, metagreywacke, metasiltstone, mica schist, conglomerate and minor metabasalt.|
2360|Bottletree Formation|70282|5|Briefly described|p544 Tb.1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||Overlain by Mount Guide Quartzite|Bimodal volcanics and clastic sedimentary rocks.|13-FEB-18
2360|Bottletree Formation|70283|5|Briefly described|p24|Statherian|Statherian|Basal Leichhardt River fault trough, Western fold belt, Mount Isa Inlier.|1790 +/- 9 Ma|||Overlain by Haslingden Group|Silicic volcanic rocks.|14-FEB-18
2360|Bottletree Formation|71348|6|Mentioned|p217|Statherian|Statherian|Geological province: North Australian Craton. Formed in a back-arc setting consistent with mafic and bimodal magmatism.|c. 1790 Ma|||||
2360|Bottletree Formation|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1790+/-9 Ma (crystallisation: zircon U-Pb TIMS).||||Rhyodacite.|
2360|Bottletree Formation|71799|5|Briefly described|p150 fig 2, p151 fig 3, p152, p153 tbl 1|Statherian|Statherian|Lawn Hill. Age is a TIMS magmatic U-Pb date.|1790 +/- 15 Ma (Page, 1983)|||Overlain by the Mount Guide Formation.|Silicic volcanics, porphyry.|
2360|Bottletree Formation|72526|5|Briefly described|p8 Fig.1.3.|Orosirian|Orosirian|Shown as located in the Leichhardt River Fault Trough of the Mount Isa Province.||||Underlies Mount Guide Quartzite.||
2360|Bottletree Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.  Two informal sub-units described.||||Shown as older than the Haslingden Group and younger than the Kalkadoon Granodiorite.|Mainly felsic metavolcanic rocks and subsidiary quartzite, epidotic quartzite, feldspathic to lithic sandstone, metasiltstone, mica  schist. Metabasalt, feldspathic sandstone and conglomerate. Granule to cobble, polymictic conglomerate.|
2360|Bottletree Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Two informal sub-units described.||||Shown as older than the Haslingden Group and younger than the Kalkadoon Granodiorite.|Mainly felsic metavolcanic rocks and subsidiary quartzite, epidotic quartzite, feldspathic to lithic sandstone, metasiltstone, mica  schist. Metabasalt, feldspathic sandstone and conglomerate. Granule to cobble, polymictic conglomerate.|
2360|Bottletree Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
2360|Bottletree Formation|72912|5|Briefly described|p5 Fig.3, p12.|Orosirian|Orosirian|Part of the Leichhardt Superbasin. Located in the Leichhardt River Fault Trough of the Mount Isa Province.||Guide Supersequence||Underlies Mount Guide Quartzite.|Includes felsic volcanics.|
2360|Bottletree Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||Overlain by Mount Guide Quartzite.||
2360|Bottletree Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
2360|Bottletree Formation|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13, p20|Statherian|Orosirian|Leichhardt River Domain.|1790+/-9 Ma, 1808+/-19 Ma crystallisation ages||||Felsic extrusives, minor mafic extrusives, siliciclastics, carbonaceous clastics.|
2360|Bottletree Formation|73553|6|Mentioned|p259|Statherian|Statherian|Western Fold Belt.|1790+/-9 Ma (Page, 1983b)||||Includes rhyodacite.|
2383|Bouldercombe Igneous Complex|41576|6|Mentioned|Table 6|||||||||
2383|Bouldercombe Igneous Complex|50209|5|Briefly described|Map Legend|Triassic|Permian|||||||
2383|Bouldercombe Igneous Complex|50212|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
2383|Bouldercombe Igneous Complex|50317|5|Briefly described|Map Legend|Triassic|Permian|||||||09-JUN-04
2383|Bouldercombe Igneous Complex|60557|5|Briefly described|p18 Fig. 5a|Late Triassic|Late Permian|Geochemically part of the Clarence River Supersuite.  Hornblende-bearing I-type granitoid dominated by granodiorite, tonalite and quartz diorite.  See also p19 Fig. 5b.||||||09-JUN-05
2383|Bouldercombe Igneous Complex|68008|2|Defined|p40,p123,p131,p225, p248, p330, p341-366|||See also p381, p436, p619-621. New name. Originally the Bouldercombe Complex (Kirkegaard et al., 1970). Later the Gracemere and Westwood Complexes (Wood, 1974; Ford et al., 1976). In this study it has been renamed the Bouldercombe Igneous Complex and subdivided into nine named units. The entire eastern lobe has had a number of names: Gracemere Complex (Wood, 1974: Ford et al., 1976), Gracemere Granite (Whitcher, 1975), and Gracemere Granodiorite (Dummett, 1978). Geophysics modelling.|||Flaggy, Kabra, Quartz Monzodiorites; Umbrella Granodiorite; Moonkan Granite; Gavial, Gracemere, Quarry Gabbros; Bundaleer Tonalite; Moonmera Porphyritic Granodiorite.|Intrudes Raspberry Creek Formation.||
2383|Bouldercombe Igneous Complex|68679|5|Briefly described|p410, p424-426|||Yarrol Province, southern part of the northern New England Orogen. A multiphase batholith.|||Bundaleer Tonalite; Gracemere, Gavial, Quarry Gabbros; Flaggy Quartz Monzodiorite; Umbrella Creek Granodiorite; Moonkan Granite.|Possibly intruded by Kabra Quartz Monzodiorite.|Undivided: augite-biotite-hornblende-quartz diorite. Cut by microgranite dykes, leucocratic biotite granite. See CONSTITUENTS for individual lithologies.|
2445|Box Gully Formation|23799|3|Fully described|p33, p14 Tb. 1|Permian|Permian|Of Cressbrook Creek Group.  Predominantly black or brown mudstone. Overlain by Buaraba Mudstone; underlain by Biarraville Formation.  Geological Province: Cressbrook Creek Subprovince  Max. thickness: ~1200m.  See also p61 Fig. 4.  See also p61 Fig. 4.||||||
2445|Box Gully Formation|23800|5|Briefly described|Map legend|Permian|Permian|Of the Cressbrook Creek Group.||||||
2445|Box Gully Formation|24560|5|Briefly described|Map legend|Permian|Permian|Of Cressbrook Creek Group.  Conglomerate, arenite, shale, andesitic volcanics; rare plant fragments.||||||
2445|Box Gully Formation|33381|4|Described|p108|||See also p111. Cressbrook Creek Group.||||||09-APR-08
2445|Box Gully Formation|39252|6|Mentioned|Fig.13|||||||||
2445|Box Gully Formation|39445|5|Briefly described|Table 8|||||||||
2445|Box Gully Formation|42525|5|Briefly described|Map legend|Early Permian?|Early Permian?|Of the Cressbrook Creek Group.||||||15-JUL-04
2445|Box Gully Formation|44555|4|Described|p224|||See also Lexicon. Conformably overlies Biarraville Formation.||||||
2445|Box Gully Formation|44786|14|Not recorded|p193-202||Permian|Middle Permian||||||
2445|Box Gully Formation|68679|5|Briefly described|p386|Guadalupian|Guadalupian|Cranfield et al. (2001). Cressbrook Basin. Shallow shelf or continental environment. ~1200m thick.||Cressbrook Creek Group.||Unconformably overlies Biarraville Formation. Is overlain conformably by Buaraba Mudstone.|Granule and pebble conglomerate (with angular to subrounded pebbles of quartz, rhyolite, metamorphics and arenite); non-calcareous sandstone, minor siltstone, shale (locally carbonaceous), and andesitic volcaniclastic rocks.|
2455|Boxvale Sandstone Member|12597|5|Briefly described|p492 Tb.1, p496|Toarcian|Toarcian|See also Boxvale Member (p501). N Surat Basin. Up to 90m thick.||Unit in Evergreen Formation.|||Thin sequence of sandstone, siltstone and coal.|
2455|Boxvale Sandstone Member|13516|5|Briefly described|p159 fig 8, p167, p169, p170, p172, p174|Early Jurassic|Early Jurassic|From Surat Basin||Of Evergreen Formation||||
2455|Boxvale Sandstone Member|22857|5|Briefly described|p296-7 Tb.22.1|||Of the Evergreen Formation (Bundamba Group). Geological Province: Surat Basin.||||||24-MAR-06
2455|Boxvale Sandstone Member|22865|4|Described|p314,Table22.1p296-7|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
2455|Boxvale Sandstone Member|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Of Evergreen Formation. Geological Province: Surat Basin.||||||
2455|Boxvale Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Of Evergreen Formation. Geological Province: Eromanga Basin.||||||
2455|Boxvale Sandstone Member|29393|6|Mentioned|Table 4|||Jurassic.||||||
2455|Boxvale Sandstone Member|29410|6|Mentioned|Fig.1|||||||||
2455|Boxvale Sandstone Member|29591|6|Mentioned|p69|||||||||
2455|Boxvale Sandstone Member|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
2455|Boxvale Sandstone Member|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|30699|6|Mentioned|p56|||Contains probable beach sands||||||
2455|Boxvale Sandstone Member|30702|6|Mentioned|Fig.1|||On Stratigraphic Table||||||
2455|Boxvale Sandstone Member|31116|4|Described|p21|||See also p1. L. Jurassic||||||10-MAR-19
2455|Boxvale Sandstone Member|31304|6|Mentioned|Fig. 1|||||||||
2455|Boxvale Sandstone Member|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33381|14|Not recorded|p117||Early Jurassic|Unit of Evergreen Formation.Correlation chart.||||||
2455|Boxvale Sandstone Member|33672|6|Mentioned|p41|||||||||
2455|Boxvale Sandstone Member|33673|4|Described|p291|||||||||
2455|Boxvale Sandstone Member|33675|4|Described|p412|||Lithology.||||||
2455|Boxvale Sandstone Member|33774|6|Mentioned|p48|||Stratigraphy||||||
2455|Boxvale Sandstone Member|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|34905|6|Mentioned|p531|||||||||
2455|Boxvale Sandstone Member|35095|6|Mentioned|p116|||||||||
2455|Boxvale Sandstone Member|35157|6|Mentioned|p523|||||||||
2455|Boxvale Sandstone Member|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
2455|Boxvale Sandstone Member|36111|6|Mentioned|p34|||||||||
2455|Boxvale Sandstone Member|36233|6|Mentioned|Table 1|||||||||
2455|Boxvale Sandstone Member|36243|6|Mentioned|Table 7A|||||||||
2455|Boxvale Sandstone Member|37995|6|Mentioned|p62|||||||||
2455|Boxvale Sandstone Member|39212|4|Described|p36|||Excursion site. Petroleum reservoir. See also p24.||||||10-MAR-19
2455|Boxvale Sandstone Member|39494|6|Mentioned|p137|||||||||
2455|Boxvale Sandstone Member|39943|6|Mentioned|Table 9A|||||||||
2455|Boxvale Sandstone Member|40030|6|Mentioned|Fig.5|||||||||
2455|Boxvale Sandstone Member|40249|6|Mentioned|p38|||Mention P41||||||
2455|Boxvale Sandstone Member|40250|4|Described|p29|||||||||
2455|Boxvale Sandstone Member|40541|4|Described|p108|||||||||
2455|Boxvale Sandstone Member|40544|6|Mentioned|Fig.6|||||||||
2455|Boxvale Sandstone Member|40666|4|Described|p356|||||||||
2455|Boxvale Sandstone Member|40832|5|Briefly described|p455|||||||||
2455|Boxvale Sandstone Member|41210|6|Mentioned|p158|||||||||
2455|Boxvale Sandstone Member|41247|6|Mentioned|p127|||||||||
2455|Boxvale Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
2455|Boxvale Sandstone Member|41725|6|Mentioned|p400|||||||||
2455|Boxvale Sandstone Member|41747|4|Described|p469|||||||||
2455|Boxvale Sandstone Member|42157|6|Mentioned|p377|||||||||
2455|Boxvale Sandstone Member|42493|5|Briefly described|Fig. 1 P18|||||||||
2455|Boxvale Sandstone Member|42911|5|Briefly described|p13|||of Evergreen Formation||||||
2455|Boxvale Sandstone Member|43000|5|Briefly described|Fig.5,p112|||of Evergreen Formation||||||
2455|Boxvale Sandstone Member|43185|6|Mentioned|14||Jurassic|||||||
2455|Boxvale Sandstone Member|43851|14|Not recorded|Tb p106,111||Early Jurassic|||||||
2455|Boxvale Sandstone Member|43982|14|Not recorded|Map Legend|||||||||
2455|Boxvale Sandstone Member|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
2455|Boxvale Sandstone Member|43994|14|Not recorded|Map Legend|||||||||
2455|Boxvale Sandstone Member|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44032|14|Not recorded|462,464|||Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44118|14|Not recorded|Map Legend||Jurassic|||||||
2455|Boxvale Sandstone Member|44169|2|Defined|Tb.1,p9,map|||||||||
2455|Boxvale Sandstone Member|44170|2|Defined|p21-23,32,map,Tb.1|||||||||
2455|Boxvale Sandstone Member|44174|14|Not recorded|p345,347||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44207|14|Not recorded|p116|||See also Lexicon.||||||
2455|Boxvale Sandstone Member|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
2455|Boxvale Sandstone Member|44381|14|Not recorded|p7|||||||||
2455|Boxvale Sandstone Member|44390|14|Not recorded|p6,9,15,16,Tb.1||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44391|14|Not recorded|Map Legend||Early Jurassic|Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44420|14|Not recorded|p14,15,18,21,27,29,|||Fig.14||||||
2455|Boxvale Sandstone Member|44421|14|Not recorded|p11,12,14,16,17||Jurassic|||||||
2455|Boxvale Sandstone Member|44422|14|Not recorded|p149 (Tb)||Jurassic|||||||
2455|Boxvale Sandstone Member|44426|14|Not recorded|p12||Early Jurassic|"On spore data the Precipice Sandstone and Evergreen Formation (including the Boxvale Sandstone Member) are regarded as of Lower Jurassic age.||||||
2455|Boxvale Sandstone Member|44636|14|Not recorded|p167(Tb)||Early Jurassic|Member of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44637|14|Not recorded|Table|||||||||
2455|Boxvale Sandstone Member|44787|14|Not recorded|Tb.p123,125,129||Jurassic|Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|45071|3|Fully described|Table 15|||||||||
2455|Boxvale Sandstone Member|45073|6|Mentioned|p58|||Geological history||||||
2455|Boxvale Sandstone Member|45110|3|Fully described|p91|||See also p41.||||||10-MAR-19
2455|Boxvale Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
2455|Boxvale Sandstone Member|46989|5|Briefly described|Table 1|||||||||
2455|Boxvale Sandstone Member|48900|4|Described|p51|||||||||
2455|Boxvale Sandstone Member|48919|4|Described|p45|||See also p46-53. Jurassic||||||10-MAR-19
2455|Boxvale Sandstone Member|48920|3|Fully described|p43|||Lower Jurassic age. Member of Evergreen Formation||||||
2455|Boxvale Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
2455|Boxvale Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
2455|Boxvale Sandstone Member|60998|5|Briefly described|p145|||Of Mollan et al (1972). Superseded Boxvale Sandstone. ||||||
2455|Boxvale Sandstone Member|60999|5|Briefly described|p178 Fig. 10|||Of the Evergreen Formation.  Geological Province: Surat Basin.||||||
2455|Boxvale Sandstone Member|61377|5|Briefly described|p151|Early Jurassic|Early Jurassic|Of the Evergreen Formation. Excellent reservoir sandstone reaching up to 60m thickness. Geological Province: Surat Basin.||||||07-FEB-11
2455|Boxvale Sandstone Member|64856|4|Described|p79, p82-85|Toarcian||Surat Basin. Fine to coarse grained, cross bedded, quartzose sandstone with carbonaceous siltstone, shale and coal interbeds. Contained in the Evergreen Formation. Age from relationship with overlying Westgrove Ironstone Member.| | ||||28-NOV-17
2455|Boxvale Sandstone Member|64857|5|Briefly described|p130-132, p113 Fig.3|||Member of the Evergreen Formation. Surat Basin. Friable quartzose sandstone.||||||
2455|Boxvale Sandstone Member|65117|5|Briefly described|p467, Fig 4 p465|Toarcian|Toarcian|Of Evergreen Formation, Surat Basin. Potential reservoir.  fine to medium grained sandstone with symmetrical ripples, hummocky cross stratification. Massive beds. Overlain by Westgrove Ironstone Member.||||||
2455|Boxvale Sandstone Member|65388|5|Briefly described|p211|||Of Jensen & others (1964). Part of Evergreen Formation, along with "Evergreen Shales".||||||
2455|Boxvale Sandstone Member|66529|6|Mentioned|p12 Fig.5 |||||Unit in Evergreen Formation.||||
2455|Boxvale Sandstone Member|67133|5|Briefly described|p11|Jurassic|Jurassic|Deposited as part of a prograding delta system.||Evergreen Formation.|||Fine- to coarse-grained, cross-bedded, quartzose sandstone.|
2455|Boxvale Sandstone Member|68576|5|Briefly described|Q_4: p14-15, p17, p22, p24|Early Jurassic|Early Jurassic|Surat Basin. Is locally capped by 27 Ma basalt from the Buckland volcano. Differs from other sandstones in the Evergreen Formation which are lithic-feldspathic.||Evergreen Formation.|||Fine- to coarse-grained, cross-bedded quartzose sandstone with some argillaceous clay matrix.|
2455|Boxvale Sandstone Member|69594|5|Briefly described|p535|||Jensen et al. (1964). Previously the Boxvale Sandstone of Reeves (1947), which was incorporated as a Member into the redefined Evergreen Formation. Prograding lacustrine delta deposits.||Evergreen Formation.||Is overlain by the Westgrove Ironstone Member.|Dominated by quartzose sandstone with very minor carbonaceous siltstone, shale and coal interbeds.|
2455|Boxvale Sandstone Member|69633|4|Described|p1, p3-7, p10-13, p20, Appendix 6.|Early Jurassic|Early Jurassic|Reeves (1947). Assigned to the Evergreen Formation by Jensen et al. (1964). Surat Basin. Contains acritarchs. GSQ Chinchilla 4 core log detailed. Palynology detailed.||Evergreen Formation.||Is overlain by Westgrove Ironstone Member.|Laterally restricted sandstones fed by incised fluvial feeder channels.|
2455|Boxvale Sandstone Member|69682|5|Briefly described|p92-94|Early Jurassic|Early Jurassic|Surat Basin.||Unit in Evergreen Formation.|||Quartzose, fine- to coarse-grained sandstone.|
2455|Boxvale Sandstone Member|70821|5|Briefly described|p80|||Eromanga, Surat Basins. Aquifer: generally artesian.||Evergreen Formation.||||
2455|Boxvale Sandstone Member|71805|6|Mentioned|p79-p80|||Surat Basin.||Evergreen Formation, upper||||15-MAY-19
2455|Boxvale Sandstone Member|71806|4|Described|p483, p485|||Surat Basin. Interpreted to have been deposited in a deltaic environment on the basis of coarsening-upwards nature in outcrop and abrupt capping by the Westgrove Ironstone Member.||Evergreen Formation.||Overlain by the Westgrove Ironstone Member.||
2455|Boxvale Sandstone Member|72297|5|Briefly described|p745|||Surat Basin. Deltaic deposits. Important in stratigraphic traps for hydrocarbons within the parent Formation.||Evegreen Formation.||||
2455|Boxvale Sandstone Member|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Evergreen FZ.||Is overlain by Hutton Sandstone.||
2455|Boxvale Sandstone Member|72921|5|Briefly described|p17.|Early Jurassic|Early Jurassic|Shows marine influence. May be characterised by hummocky cross-stratification. Described with Westgrove Ironstone Member. (Mollan et al., 1972; Exon et al., 1976; Fielding, 1996; McKellar, 1998; Turner et al., 2009; Brearley et al., 2018).||Evergreen Formation|||Sandstone that may include acritarchs, proximal and distal deltaic deposits, tidal bundles, chamositic oolites, pelecypods, anoxic black shales and tempestites.|
2455|Boxvale Sandstone Member|73113|6|Mentioned|p36, p69, p80|||||||||
2455|Boxvale Sandstone Member|73600|6|Mentioned|191|Toarcian|Toarcian|||Evergreen Formation||Overlain by Westgrove Ironstone Member.||
2458|Boxwood Ring Complex|23423|5|Briefly described|p307 Table 7.3|||||||||
2458|Boxwood Ring Complex|23616|6|Mentioned|Table 3 p51|||||||||
2458|Boxwood Ring Complex|39564|6|Mentioned|p9|||||||||
2458|Boxwood Ring Complex|45008|14|Not recorded|p28,30,35,Pl.6,9|||Structural Term||||||
2458|Boxwood Ring Complex|45014|14|Not recorded|p10,26,68,85,89,98,|||p136,Pl.25,40,Tb.1. Used as stuctural term.||||||
2458|Boxwood Ring Complex|60425|6|Mentioned|p47 Tb. 3|||Of Branch (1966) - in which he placed the outcrops of Boxwood Volcanics (Featherbed Volcanic Group). An alternative term of Boxwood Cauldron was introduced by Mackenzie et al (1993).||||||07-FEB-11
2459|Boxwood Volcanics|23423|4|Described|p307 Table 7.3||Late Carboniferous|Age: ~301 Ma (Rb-Sr). Featherbed Volcanic Group.||||||
2459|Boxwood Volcanics|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~301 Ma, Rb-Sr. of Featherbed Volcanic Group.||||||
2459|Boxwood Volcanics|23502|5|Briefly described|Map Legend||Late Carboniferous|of Featherbed Volcanic Group.||||||
2459|Boxwood Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V87. I-Type.||||||
2459|Boxwood Volcanics|23616|5|Briefly described|Table 3 p51||Late Carboniferous|Age Late Carboniferous (~301 Ma; Rb-Sr). Unit crops out within Boxwood Ring Complex & Boxwood Cauldron. Unconformable on Hodgkinson Fm, and cut by Sunnymount Granodiorite. Indicator granite & rhyolite dykes. Of Featherbed Volcanic Gp. Boxwood Cauldron.||||||30-MAR-15
2459|Boxwood Volcanics|23624|5|Briefly described|p23|||Of the Featherbed Volcanic Group.||||||22-APR-09
2459|Boxwood Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
2459|Boxwood Volcanics|31832|6|Mentioned|Table 6|||||||||
2459|Boxwood Volcanics|37613|6|Mentioned|Fig.1|||||||||
2459|Boxwood Volcanics|39445|5|Briefly described|Table 7|||||||||
2459|Boxwood Volcanics|39564|6|Mentioned|Table 5|||Originally (probably wrongly) entered for NSW.||||||
2459|Boxwood Volcanics|42547|5|Briefly described|p74|||||||||
2459|Boxwood Volcanics|43060|5|Briefly described|Fig.4A-B|||||||||
2459|Boxwood Volcanics|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Grey to dark grey, lithics-poor to free, crystal-rich dacitic ignimbrite; porphyritic dacite; minor medium-ash crystal tuff.||||||15-JUN-06
2459|Boxwood Volcanics|43259|4|Described|Appendix 1,p8.||Late Carboniferous|||||||
2459|Boxwood Volcanics|43626|4|Described|p10,42||Late Carboniferous|||||||
2459|Boxwood Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
2459|Boxwood Volcanics|43901|14|Not recorded|Map Legend||Late Permian|(Early Triassic)- Late Permian||||||
2459|Boxwood Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
2459|Boxwood Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
2459|Boxwood Volcanics|45008|4|Described|p12,28-30,37,42,Map|||||||||22-APR-09
2459|Boxwood Volcanics|45014|2|Defined|p40,88,90-1,Tb.1,|Late Carboniferous|Early Carboniferous|Pl.38. Probably Middle or Late Carboniferous.||||||
2459|Boxwood Volcanics|45025|4|Described|p70|Permian|Carboniferous|||||||
2459|Boxwood Volcanics|46845|6|Mentioned|Table 1|||||||||
2459|Boxwood Volcanics|60425|4|Described|p46 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Outcrops in Boxwood Ring Complex of Branch 91966) and Boxwood Cauldron of Mackenzie et al (1993). Unconformable on Hodgkinson Fm; cut by Sunnymount Granodiorite and Indicator Granite.||||||07-FEB-11
2459|Boxwood Volcanics|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Featherbed Volcanic Group.|||Grey to dark grey, welded, lithics-poor to lithics-free, crystal-rich, dacitic to rhyodacitic ignimbrite; subordinate porphyritic dacitic-rhyolitic? lava; minor medium-ash crystal tuff.|
2459|Boxwood Volcanics|69593|5|Briefly described|p485|Late Carboniferous|Late Carboniferous|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.||||
2465|Boyne River Granite|23799|6|Mentioned|p78|||Of Boondooma Igneous Complex.  Geological Province: Yarraman Subprovince.||||||
2465|Boyne River Granite|29958|6|Mentioned|p13|||||||||
2465|Boyne River Granite|35101|6|Mentioned|p73|||||||||
2465|Boyne River Granite|39970|6|Mentioned|p61|||||||||
2465|Boyne River Granite|43858|5|Briefly described|32|||||||||
2465|Boyne River Granite|43991|6|Mentioned|p46,50||Paleozoic|||||||07-NOV-08
2507|Brassal Subgroup|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Ipswich Coal Measures||Includes Tivoli Formation, Blackstone Formation||
2507|Brassal Subgroup|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
2507|Brassal Subgroup|40434|6|Mentioned|p25|||||||||
2507|Brassal Subgroup|40623|5|Briefly described|p30|||||||||
2507|Brassal Subgroup|41906|5|Briefly described|p22|||||||||
2507|Brassal Subgroup|42187|6|Mentioned|p319|||||||||
2507|Brassal Subgroup|42405|6|Mentioned|Table 3 P.7|||||||||
2507|Brassal Subgroup|42648|6|Mentioned|p42|||Ipswich Coal Measures||||||
2507|Brassal Subgroup|43076|6|Mentioned|p7|||of Ipswich Coal Measures||||||
2534|Brick Kiln Member|39493|2|Defined|p98|late Eocene|middle Eocene|Mid to late Eocene||||||
2534|Brick Kiln Member|40116|6|Mentioned|p29|||||||||
2534|Brick Kiln Member|41273|5|Briefly described|p207|||||||||
2534|Brick Kiln Member|41927|5|Briefly described|p64|||||||||
2534|Brick Kiln Member|42021|6|Mentioned|p327|||||||||
2534|Brick Kiln Member|71092|5|Briefly described|p232-233|Eocene|Eocene|Crocodilian fossil.||Rundle Formation.||||
2534|Brick Kiln Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
2541|Bridge Sandstone|33363|6|Mentioned|p116|||Refers. Allen (1967).||||||
2541|Bridge Sandstone|45095|6|Mentioned|p12|||Refers Reid (1944)||||||
2553|Briggs Granodiorite|24382|5|Briefly described|Map legend|Triassic|Permian|||||||23-DEC-09
2553|Briggs Granodiorite|41778|2|Defined|Table 1|Triassic|Permian|Described p372.||||||23-SEP-08
2553|Briggs Granodiorite|43008|5|Briefly described|map legend|||||||||
2553|Briggs Granodiorite|63821|5|Briefly described|p29|Triassic|Permian|Unconformably overlain by Mount Marcella Volcanics and some units of Aranbanga Volcanic Group. Intrudes Shoalwater Formation; intruded by Hogback ?Granodiorite (probably should be Granite). Hornblende-biotite granodiorite and biotite-hornblende tonalite.||||||07-FEB-11
2553|Briggs Granodiorite|68679|5|Briefly described|p421-422|||Gayndah-Gladstone belt. Lithologically similar to Yenda Granodiorite; may be continuous, but is offset 7km by Perry Fault. Continental volcanic arc setting interpreted. Fractional crystallisation was the major factor in its evolution.|||||Biotite-hornblende granodiorite, hornblende-biotite granite to granodiorite, tonalite; zoned with dioritic margins and more felsic granodiorite core; two granodioritic phases, both metaluminous to slightly peraluminous I-type.|
2553|Briggs Granodiorite|73450|6|Mentioned|p24|Triassic|late Paleozoic|||||Intruded by Hogback Granite.||
2579|Brisbane Tuff|22857|6|Mentioned|p284|Late Triassic|Late Triassic|||||||
2579|Brisbane Tuff|22861|6|Mentioned|p284|||||||||
2579|Brisbane Tuff|24082|6|Mentioned|p452|||Geological Province: Ipswich Basin.||||||
2579|Brisbane Tuff|30112|6|Mentioned|p111|||||||||
2579|Brisbane Tuff|30303|6|Mentioned|p323|||Upper Triassic correlation||||||
2579|Brisbane Tuff|30470|6|Mentioned|p457|||||||||
2579|Brisbane Tuff|30661|6|Mentioned|Table 1|||||||||
2579|Brisbane Tuff|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
2579|Brisbane Tuff|31130|6|Mentioned|Fig. 2|||||||||
2579|Brisbane Tuff|31133|6|Mentioned|p160|||See also p161. Triassic||||||
2579|Brisbane Tuff|33381|6|Mentioned|p113|||Triassic||||||
2579|Brisbane Tuff|33769|6|Mentioned|p150|||||||||
2579|Brisbane Tuff|33881|6|Mentioned|p96|||Quarried extensively.||||||
2579|Brisbane Tuff|34340|6|Mentioned|p462|||||||||
2579|Brisbane Tuff|34593|6|Mentioned|p539|||||||||
2579|Brisbane Tuff|35007|6|Mentioned|p75|||||||||
2579|Brisbane Tuff|35063|6|Mentioned|p80|||||||||
2579|Brisbane Tuff|35101|6|Mentioned|p47|||||||||
2579|Brisbane Tuff|35126|6|Mentioned|Map legend|Triassic|Triassic|||||||
2579|Brisbane Tuff|35156|4|Described|p6|||See also Table.2||||||
2579|Brisbane Tuff|35430|6|Mentioned|Fig.2|||Geological map.||||||
2579|Brisbane Tuff|35866|6|Mentioned|p400|||||||||
2579|Brisbane Tuff|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
2579|Brisbane Tuff|36354|6|Mentioned|p368|||||||||
2579|Brisbane Tuff|36440|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
2579|Brisbane Tuff|36779|6|Mentioned|p6|||||||||
2579|Brisbane Tuff|36961|6|Mentioned|Table 1|||||||||
2579|Brisbane Tuff|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
2579|Brisbane Tuff|38074|5|Briefly described|Table 1|||||||||
2579|Brisbane Tuff|38391|6|Mentioned|p10|||||||||
2579|Brisbane Tuff|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
2579|Brisbane Tuff|39079|5|Briefly described|p10|||||||||
2579|Brisbane Tuff|39445|6|Mentioned|Table 9|||||||||
2579|Brisbane Tuff|39943|6|Mentioned|Table 12A|||||||||
2579|Brisbane Tuff|40245|6|Mentioned|p185|||Mention Fig.2||||||
2579|Brisbane Tuff|40479|6|Mentioned|p32|||||||||
2579|Brisbane Tuff|40517|6|Mentioned|p358|||||||||
2579|Brisbane Tuff|40536|6|Mentioned|p281|||||||||
2579|Brisbane Tuff|40579|6|Mentioned|Map legend|late Carnian|late Carnian|||||||
2579|Brisbane Tuff|40623|5|Briefly described|p7|||||||||
2579|Brisbane Tuff|40780|4|Described|p5|||||||||
2579|Brisbane Tuff|41475|6|Mentioned|p72|||||||||
2579|Brisbane Tuff|41738|6|Mentioned|p168|||||||||
2579|Brisbane Tuff|41906|3|Fully described|Table 2 p19|||||||||27-NOV-15
2579|Brisbane Tuff|42316|5|Briefly described|p17|||||||||
2579|Brisbane Tuff|42336|6|Mentioned|p2|||||||||
2579|Brisbane Tuff|42403|6|Mentioned|p49|||||||||
2579|Brisbane Tuff|42525|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
2579|Brisbane Tuff|42665|5|Briefly described|p119|||||||||
2579|Brisbane Tuff|42669|5|Briefly described|p234|||||||||
2579|Brisbane Tuff|42893|6|Mentioned|p6|||||||||
2579|Brisbane Tuff|43008|5|Briefly described|map legend|||||||||
2579|Brisbane Tuff|43009|5|Briefly described|Map Legend|||||||||
2579|Brisbane Tuff|43076|5|Briefly described|p14|||see also p16.||||||
2579|Brisbane Tuff|43092|5|Briefly described|p31|||||||||
2579|Brisbane Tuff|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
2579|Brisbane Tuff|43870|14|Not recorded|p307,337||Middle Triassic|||||||
2579|Brisbane Tuff|43881|14|Not recorded|p37,51-3,57-8,63,||Triassic|p79-80,135,167. See also Lexicon.||||||
2579|Brisbane Tuff|43995|14|Not recorded|Table p10||Triassic|Part of Ipswich Coal Measures.||||||
2579|Brisbane Tuff|44026|14|Not recorded|p123||Triassic|Lateral equivalent of basal Kholo Sub-Group.||||||
2579|Brisbane Tuff|44030|14|Not recorded|p115,122,125,126,133|||May be equivalent to base of Tingalpa Formation.||||||
2579|Brisbane Tuff|44091|14|Not recorded|p52||Triassic|||||||
2579|Brisbane Tuff|44432|4|Described|p52,54||Middle Triassic|||||||
2579|Brisbane Tuff|44687|1|Redefined|p221,222|Late Triassic|Middle Triassic|Possibly equivalent of Kholo Subgroup. Previously a more extensive unit was called Brisbane Tuffs.||||||21-MAR-13
2579|Brisbane Tuff|44703|14|Not recorded|Map|||||||||
2579|Brisbane Tuff|44708|14|Not recorded|p3,5,24,Sheets 1-5||Middle Triassic|||||||
2579|Brisbane Tuff|44718|14|Not recorded|p102,104,106||Middle Triassic|||||||
2579|Brisbane Tuff|44756|14|Not recorded|p13,28,49||Triassic|||||||
2579|Brisbane Tuff|44783|14|Not recorded|p5-7,20,38,50|||||||||
2579|Brisbane Tuff|44786|14|Not recorded|p193-202|||||||||
2579|Brisbane Tuff|45018|14|Not recorded|Tb.SJ,p36|||||||||
2579|Brisbane Tuff|45070|6|Mentioned|Table 22|||||||||
2579|Brisbane Tuff|45087|5|Briefly described|p97|||Chemical analyses.||||||
2579|Brisbane Tuff|48917|6|Mentioned|p9|||Correlation||||||
2579|Brisbane Tuff|48928|6|Mentioned|p3|||||||||
2579|Brisbane Tuff|60281|5|Briefly described|p25|||Geological Province: Nambour Basin.||||||
2579|Brisbane Tuff|60299|5|Briefly described|p223|||||||||
2579|Brisbane Tuff|64665|6|Mentioned|p53 Fig.2.|Late Triassic|Late Triassic|Ipswich Basin.||||||
2579|Brisbane Tuff|64769|6|Mentioned|p24, p25 Fig 16 (b)|Early Jurassic|Early Jurassic|Pyroclastic flow deposit filling earlier stream channels.||||||05-MAY-09
2579|Brisbane Tuff|64833|5|Briefly described|p9-16|Late Triassic|Late Triassic|Welded tuff or ignimbrite. Thickness is possibly up to 200m.  Overlaid the Brisbane Metamorphics.||||||02-FEB-09
2579|Brisbane Tuff|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
2579|Brisbane Tuff|66855|6|Mentioned|p955.|||||||||
2579|Brisbane Tuff|67203|6|Mentioned|p3|Triassic|Triassic|||||||
2579|Brisbane Tuff|67402|5|Briefly described|p222|Carnian|Ladinian|Ipswich Basin.|||||Sub-aerial tuffaceous conglomerate and sandstone.|
2579|Brisbane Tuff|68327|5|Briefly described|Map legend.|Triassic|Triassic||||||Rhyolite tuff, welded tuff and agglomerate, minor sediments.|
2579|Brisbane Tuff|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
2579|Brisbane Tuff|68576|6|Mentioned|QLD_D1: p1-2, p4, p8, p10, p14-15, p17.|||Used in the abutments and bays of the second Victoria Bridge (South Bank); the Old Commissariat Store and Queens Wharf (North Bank); foundations for the Treasury Building and Old Government Printery Buildings; footings and perimeter walls of Parliament House; a retaining wall near the Wickham Terrace Windmill; the Adelaide Street-side wall of ANZAC Square; St. John's Cathedral; St. Martins House; the riverside low wall and the Petrie Bight retaining wall outside Customs House; base layers of the GPO building; St. Stephen's Cathedral; Alice Street wall and gateposts; Old Government House. Map location.||||||
2579|Brisbane Tuff|68679|5|Briefly described|p392-395, p433-434, p469|Late Triassic|Late Triassic|Basal unit in the Ipswich Basin: Brisbane/Beenleigh/offshore. Forms a narrow, NW-striking band ~50km long. Pyroclastic flow deposits filling a steep-sided valley. Up to 250m thick.|226.0 +/- 2.0 Ma (SHRIMP U-Pb: Cross, unpub.).|||Unconformably overlies Neranleigh-Fernvale beds.|Felsic volcanics: multiple rhyolitic ignimbrites (including welded ignimbrite), minor air fall tuff, surge deposits, conglomerate, volcanilithic sandstone and breccia; porphyritic.|
2579|Brisbane Tuff|69594|6|Mentioned|p519|||Ipswich Basin.||||Is overlain by Ipswich Coal Measures.||
2579|Brisbane Tuff|69599|5|Briefly described|p610|||Offshore Ipswich Basin. A 277m succession of carbonaceous sediments with several igneous intervals was intersected in APS Matjara 1 drilled 15km off Moreton Island; the igneous rocks compared with the Brisbane Tuff.|||||Includes tuff and tuffaceous shale.|
2579|Brisbane Tuff|69952|5|Briefly described|p2 Tb.i, p38, p42-46|Late Triassic|Late Triassic|New England Orogen. New Farm cliff in inner Brisbane. Part of the basal sequence of the Ipswich Basin. SHRIMP U-Pb zircon magmatic crystallisation age. Not comagmatic with Enoggera Granite, which may have been unroofed prior to this unit's eruption.|226.0 +/- 2.0 Ma (Cross et al., 2015).|||Unconformably overlies Neranleigh-Fernvale beds.|Pale pink, moderately welded rhyolitic ignimbrite; contains quartz and alkali feldspar fragments, pumice clasts, locally derived lithic fragments (dominantly black phyllite) and  charcoal.|
2579|Brisbane Tuff|71592|5|Briefly described|Appendix A.|||Bowen Basin.|226+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
2579|Brisbane Tuff|72297|5|Briefly described|p726|||Quarried at several places for dimension stone and used widely for road-making, kerbing, monuments, ornamental works, retaining walls and buildings.||||||
2579|Brisbane Tuff|73146|6|Mentioned|p15|||Has magnetic overprinting with a uniformly normal polarity and steep inclination.||||||
2579|Brisbane Tuff|73294|6|Mentioned|p1014|late Triassic|late Triassic|227.1 +/- 0.1 Ma age may be a maximum (detrital) age instead of an eruption age (Smith et al., 2017, 2018). Correlated with the base of the Ipswich Coal Measures, Craterisporites rotundus spore-pollen zone age (de Jersey and Hamilton, 1965).|227.1 +/- 0.1 Ma|||||
2579|Brisbane Tuff|73306|5|Briefly described|p564-566|Late Triassic|Late Triassic|||Nymboida Coal Measures.||Is overlain by the Brassall Subgroup. Probable equivalent to the Chillingham Volcanics.|Rhyolitic tuff.|
2579|Brisbane Tuff|73450|5|Briefly described|p38-39|Norian|Carnian|Valley-filling rhyolitic ignimbrite that forms the Kangaroo Point cliffs. A U-Pb SHRIMP zircon age of 226.0 +/- 2.0 Ma was reported by Cross et al. (2015).|226.0 +/- 2.0 Ma U-Pb SHRIMP||||Rhyolitic ignimbrite and[?] pyroclastic surge and airfall deposits.|
2586|Brittany Granite|22847|3|Fully described|p 40|||||||||
2586|Brittany Granite|23422|5|Briefly described|p173, p210 Table 6.6|||Of Brittany Supersuite.  Probably Ordovician.||||||
2586|Brittany Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 105. I-Type.||||||
2586|Brittany Granite|42245|2|Defined|p32|Ordovician||Reserved as Brittany Adamellite||||||
2586|Brittany Granite|42633|6|Mentioned|Table 1 P8|||||||||
2586|Brittany Granite|43093|4|Described|Appendix 1||Ordovician|||||||
2586|Brittany Granite|43259|4|Described|Appendix 1,p23.||Ordovician|Probably Ordovician.||||||
2586|Brittany Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
2609|Brodies Gap Rhyolite|23291|4|Described|p95 Tb. 3.10|Early Permian|Early Permian|Parent: Namarrong Volcanic Subgroup. Age: 283+/-3Ma. Thickness: Up to 1250m. Geological Province: Georgetown Region.||||||28-MAY-15
2609|Brodies Gap Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Namarrong Volcanic Subgroup, Newcastle Range Volcanic Group.||||||
2609|Brodies Gap Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V17. A-Type.||||||
2609|Brodies Gap Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
2609|Brodies Gap Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Namarrong Volcanic Subgroup.||||||
2609|Brodies Gap Rhyolite|43740|4|Described|p10|||||||||
2609|Brodies Gap Rhyolite|50198|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Nammarong Volcanic Subgroup.||||||
2609|Brodies Gap Rhyolite|68354|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Four facies/associations are mapped separately. Min age: Early Permian?||Unit in Nammarong Volcanic Subgroup.|||Grey to brown or purple crystal-rich rhyolitic ignimbrite with sparse biotite and locally abundant lithic clasts; locally polymictic rhyolitic volcanic rudite; rhyolitic volcanic lutite to crystal-rich volcanic arenite to rudite, rare limestone.|08-JUL-15
2609|Brodies Gap Rhyolite|69593|5|Briefly described|p512|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|290 Ma.|Newcastle Range Volcaniuc Group.|||A-type.|
2609|Brodies Gap Rhyolite|70207|5|Briefly described|p4, p11, p81-87|Permian|Permian|NE of Georgetown. Unit in the Kennedy Igneous Association. Crops out over ~240 km2 and has a preserved thickness of ~1,600m.|294.5 +/- 2.1 Ma (Kositcin et al., 2015).|Namarrong Volcanic Subgroup.|||A-type. Dominated by crystal-rich, welded, rhyolitic ignimbrite, with subordinate interbedded volcaniclastic rocks (mainly co-ignimbrite lag deposits), and rare sedimentary rocks (including limestone).|
2609|Brodies Gap Rhyolite|71592|5|Briefly described|Appendix A.||||295+/-2.1 Ma (SHRIMP U-Pb zircon).||||Rhyolite.|
2627|Brookfield Volcanics|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
2627|Brookfield Volcanics|33769|6|Mentioned|Fig.2|||Triassic or Permian||||||
2627|Brookfield Volcanics|35007|6|Mentioned|p75|||||||||
2627|Brookfield Volcanics|35812|6|Mentioned|p568|||See also Fig.2||||||
2627|Brookfield Volcanics|35866|6|Mentioned|p402|||||||||
2627|Brookfield Volcanics|36440|6|Mentioned|Map legend|Early Triassic|Late Permian|Early Triassic to Late Permian||||||
2627|Brookfield Volcanics|36779|5|Briefly described|p6|||||||||
2627|Brookfield Volcanics|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
2627|Brookfield Volcanics|38074|5|Briefly described|Table 1|||||||||
2627|Brookfield Volcanics|38307|6|Mentioned|p523|||||||||
2627|Brookfield Volcanics|38441|6|Mentioned|Map legend|Late Permian|Early Permian|Early - Late Permian||||||
2627|Brookfield Volcanics|39079|6|Mentioned|p8|||||||||
2627|Brookfield Volcanics|39252|6|Mentioned|p27|||||||||
2627|Brookfield Volcanics|39445|5|Briefly described|Table 9|||See also Fig.7||||||
2627|Brookfield Volcanics|40245|6|Mentioned|Table 1|||||||||
2627|Brookfield Volcanics|40623|5|Briefly described|p30|||||||||
2627|Brookfield Volcanics|41906|3|Fully described|TABLE 1 p11|Early Triassic|Late Permian|||||||29-SEP-05
2627|Brookfield Volcanics|42525|5|Briefly described|Map legend|Triassic|Permian|||||||
2627|Brookfield Volcanics|43076|5|Briefly described|p6|||||||||
2627|Brookfield Volcanics|44671|14|Not recorded|p247|||See also Lexicon.||||||
2627|Brookfield Volcanics|44703|14|Not recorded|Map||Permian|See also Lexicon.||||||
2627|Brookfield Volcanics|44708|14|Not recorded|p3,sheet 4||Permian|||||||
2627|Brookfield Volcanics|44718|14|Not recorded|p102|||Three ages given from field relationships -  pre-late Permian; late Permian or early Triassic; Middle Triassic. Correlated in age with Indooroopilly Intrusive Rhyolites.||||||
2627|Brookfield Volcanics|44783|14|Not recorded|Tb.1,p2|||||||||
2627|Brookfield Volcanics|44786|14|Not recorded|p193-202||Triassic|Early Triassic||||||
2627|Brookfield Volcanics|68553|6|Mentioned|Map legend|Triassic|Permian|This unit, as well as the Bellthorpe Andesite, Gilla Volcanics, and unnamed volcanic units, are all mapped under the symbol, PRv.||||||
2627|Brookfield Volcanics|68679|6|Mentioned|p394, p435|||||||||
2634|Brooks Creek Dolerite|45087|5|Briefly described|p171|||Chemical analyses.||||||
2647|Broomfield Granite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
2647|Broomfield Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
2647|Broomfield Granite|32774|5|Briefly described|Table 2|||Triassic||||||
2647|Broomfield Granite|35161|6|Mentioned|p592|||||||||
2647|Broomfield Granite|36954|6|Mentioned|p114|||||||||
2647|Broomfield Granite|39445|5|Briefly described|Table 12|||||||||
2647|Broomfield Granite|39505|6|Mentioned|p167|||||||||
2647|Broomfield Granite|41738|6|Mentioned|p173|||||||||
2647|Broomfield Granite|41778|6|Mentioned|Fig.2|||||||||
2647|Broomfield Granite|42894|6|Mentioned|p23|||||||||
2647|Broomfield Granite|43008|5|Briefly described|map legend|||||||||
2647|Broomfield Granite|45440|2|Defined|p.21,22,23,28,58-88||Triassic|Tb.1, Of many pages.  Originally "Childers" Granite.||||||
2647|Broomfield Granite|63821|4|Described|p33|Late Triassic|Late Triassic|Age: 226+/-16Ma (Rb-Sr). Intrudes undiv. Gympie group and Brooweena Formation. Comprises hornblende-biotite granite, granodiorite and tonalite.||||||07-FEB-11
2647|Broomfield Granite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
2647|Broomfield Granite|68679|5|Briefly described|p428, p430|Late Triassic|Late Triassic|NE of Mungore Cauldron, northern New England Orogen. May be continuous at depth with Musket Flat Granodiorite. Very extensive and lithologically variable. Probably structurally related to the Electra Fault.||||Intrudes Gympie Group and Brooweena Formation. Adjacent to Woowoonga Range Monzogranite.|Medium-grained biotite granite in central parts and marginal porphyritic tonalite and granodiorite.|
2652|Brooweena Formation|9194|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Sandstone, siltstone, mudstone, shale, conglomerate and tuff.  Overlain by Myrtle Creek Sandstone.||||||23-DEC-09
2652|Brooweena Formation|23251|6|Mentioned|Table 1 p10-11|||Fossil assemblage similar to Kin Kin beds. Maryborough? Province.||||||21-JUN-06
2652|Brooweena Formation|23841|5|Briefly described|p448|Triassic|Triassic|Geological Province: Gympie Basin.||||||
2652|Brooweena Formation|24078|5|Briefly described|p425 Tb. 1|Early Triassic|Early Triassic|Siltstone-sandstone-subgreywacke conglomerate series; olive green siltstone, fine to coarse sandstone.  Max. thickness: 2740m.  Geological Province: Gympie Basin.||||||
2652|Brooweena Formation|24382|5|Briefly described|Map legend|Triassic|Early Triassic|||||||
2652|Brooweena Formation|29651|6|Mentioned|Table 1|||||||||
2652|Brooweena Formation|30654|4|Described|p45|||See also P46,48,49,53,55,56,59. Lower Triassic age.||||||
2652|Brooweena Formation|30655|3|Fully described|p10|||See also Table 1||||||
2652|Brooweena Formation|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
2652|Brooweena Formation|32774|5|Briefly described|Table 2|||||||||
2652|Brooweena Formation|34009|6|Mentioned|p107|||Scythian [entered for WA. Should be Qld. CEBApr95]||||||
2652|Brooweena Formation|34010|6|Mentioned|Cor. chart|||M.Triassic||||||
2652|Brooweena Formation|35101|6|Mentioned|p35|||||||||
2652|Brooweena Formation|35161|6|Mentioned|p592|||||||||
2652|Brooweena Formation|36926|6|Mentioned|Fig.4|||||||||
2652|Brooweena Formation|36954|6|Mentioned|p114|||||||||
2652|Brooweena Formation|36961|6|Mentioned|Table 1|||||||||
2652|Brooweena Formation|37118|6|Mentioned|Fig.1|||||||||
2652|Brooweena Formation|37618|4|Described|p17|||||||||
2652|Brooweena Formation|38391|6|Mentioned|p9|||||||||
2652|Brooweena Formation|38397|6|Mentioned|Table 2|||||||||
2652|Brooweena Formation|38402|6|Mentioned|p72|||||||||
2652|Brooweena Formation|39252|6|Mentioned|p28|||||||||
2652|Brooweena Formation|39445|5|Briefly described|Table 9|||||||||
2652|Brooweena Formation|39505|6|Mentioned|p167|||||||||
2652|Brooweena Formation|40245|6|Mentioned|Table 2|||||||||
2652|Brooweena Formation|40247|6|Mentioned|Fig.3|||||||||
2652|Brooweena Formation|40623|5|Briefly described|p54|||Also Mention Table 2||||||
2652|Brooweena Formation|41736|6|Mentioned|p115|||||||||
2652|Brooweena Formation|41738|6|Mentioned|p173|||||||||
2652|Brooweena Formation|41778|6|Mentioned|Fig.2|||||||||
2652|Brooweena Formation|42492|6|Mentioned|p12|||||||||
2652|Brooweena Formation|42894|5|Briefly described|Fig.2 P22|||||||||
2652|Brooweena Formation|43006|5|Briefly described|p240|||||||||
2652|Brooweena Formation|43100|6|Mentioned|p38|||||||||
2652|Brooweena Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
2652|Brooweena Formation|43995|14|Not recorded|Table p10||Triassic|||||||
2652|Brooweena Formation|44075|14|Not recorded|p251|||||||||
2652|Brooweena Formation|44091|14|Not recorded|p52||Triassic|||||||
2652|Brooweena Formation|44239|2|Defined|p278-279|||Overlies Gympie Group.||||||
2652|Brooweena Formation|44241|14|Not recorded|Tb p4,5,12,Fig.1||Middle Triassic|Formerly Brooweena Series.||||||
2652|Brooweena Formation|44250|14|Not recorded|p90|||See also Lexicon.||||||
2652|Brooweena Formation|44385|14|Not recorded|p6|||||||||
2652|Brooweena Formation|44387|14|Not recorded|p17|||||||||
2652|Brooweena Formation|44574|14|Not recorded|p117|||Proposed correlation with the Oakey Creek unit on the basis of two species of Bakevellia.||||||
2652|Brooweena Formation|44616|14|Not recorded|p32,33,35||Early Triassic|Lithic and quartzose sandstone and siltstone and conglomerate, shale, trachytic volcanics, red siltstone, low porosity.||||||20-JUN-13
2652|Brooweena Formation|44622|14|Not recorded|p84|||Early Triassic marine macrofossils reported. See also Lexicon.||||||
2652|Brooweena Formation|44697|14|Not recorded|p91|||See also Lexicon.||||||
2652|Brooweena Formation|44750|14|Not recorded|p12||Triassic|||||||
2652|Brooweena Formation|44752|14|Not recorded|Fig.42,p298,301|||||||||
2652|Brooweena Formation|44753|5|Briefly described|p47,49,52-54|||||||||
2652|Brooweena Formation|44754|14|Not recorded|p10||Triassic|||||||
2652|Brooweena Formation|44762|14|Not recorded|opp.p34|||Section.||||||
2652|Brooweena Formation|44783|14|Not recorded|p2|||||||||
2652|Brooweena Formation|44785|14|Not recorded|p149||Middle Triassic|||||||
2652|Brooweena Formation|44814|14|Not recorded|p485,86|Middle Triassic|Early Triassic|||||||
2652|Brooweena Formation|45107|6|Mentioned|p6|||||||||
2652|Brooweena Formation|45440|4|Described|p.1,7,13,14,15,17-88||Early Triassic|Tb.1. Of many pages.  Of Ipswich Coal Measures. L. Triassic.||||||
2652|Brooweena Formation|60281|5|Briefly described|Fig. 30 App 1|Early Triassic|Early Triassic|Includes the Kin Kin beds.  Sandstone, shale, conglomerate, phyllite.  Max. thickness: ~3000m.  Geological Province: Maryborough Basin.||||||
2652|Brooweena Formation|63821|5|Briefly described|p16, p18, p36|Middle Triassic|Early Triassic|Intruded by Broomfield Granite. Geol.Prov: Gympie Prov. Contains marine and continental deposits:lower marine section is mainly fine-grained silty to shaly clastic sediments with rare limestone lenses; continental deposits are fluvial clastic sediments.||||||07-FEB-11
2652|Brooweena Formation|65452|6|Mentioned|p5-6|Middle Triassic|Early Triassic|||||Is overlain by, or faulted against, Agnes Water Volcanics.||
2652|Brooweena Formation|68319|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Gympie Province||||Unconformably overlain by Myrtle Creek Sandstone and Maryborough Formation? Unconformably overlies Gympie Group.|Medium to coarse-grained, thick-bedded sandstone (locally cross-bedded), siltstone, mudstone, shale, pebble to boulder conglomerate and some volcaniclastic rocks; locally hornfelsed near plutons.|
2652|Brooweena Formation|68332|5|Briefly described|Map legend.|Middle Triassic|Early Triassic|Gympie Province. Weak- to non-magnetic response.||||May be intruded by Moolyung Granodiorite?|Medium- to coarse-grained, thick-bedded sandstone (locally cross-bedded), siltstone, mudstone, shale, pebble to boulder conglomerate and some volcaniclastic rocks; locally hornfelsed near plutons.|26-MAR-15
2652|Brooweena Formation|68421|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Gympie Province.|||||Medium to coarse-grained, thick-bedded sandstone (locally cross-bedded), siltstone, mudstone, shale, pebble to boulder conglomerate and some volcaniclastic rocks; locally hornfelsed near plutons.|
2652|Brooweena Formation|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Gympie Province. This unit, as well as the Keefton and Traveston Formations, and the Kin Kin beds, are all mapped under the symbol, Rb.||||||
2652|Brooweena Formation|68679|5|Briefly described|p312-313, p370-371, p430|Middle Triassic|Early Triassic|Northern Gympie Province, Northern New England Orogen. Occurs in a N-trending belt on the eastern margin of the Gympie Group. Macrofloras in the upper parts are similar to those in the Toogoolawah Group (Esk Basin).||||Overlies the Gympie Group disconformably or unconformably; contact commonly sheared. Correlated with Keefton Formation. Is intruded by Musket Flat Granodiorite and Broomfield Granite.|Lower marine part is mainly fine-grained silty to shaly clastics with rare limestone lenses; the apparently conformable upper fluvial clastics contain quartz, feldspar and chert as the main clasts. Rare andesitic flows but no obvious pyroclastics.|
2652|Brooweena Formation|69582|5|Briefly described|p48, p53|Middle Triassic|Early Triassic|Gympie Province. Deposited in a shallow to deep marine environment. Outcrops extensively to the west of the Nambour-Maryborough basins. Thermal conductivity is provided. Intersected in GSQ Maryborough 1.||||Overlies the Gympie Group. Unconformably overlain by the Myrtle Creek Sandstone.|Siltstone.|
2652|Brooweena Formation|69594|6|Mentioned|p549, p561|||||||Is overlain unconformably by Grahams Creek Formation.||
2652|Brooweena Formation|73303|4|Described|p60 Fig.1, p61 Fig.2, p62-65, p67-70|Middle Triassic|Early Triassic|New England Orogen. Gympie Terrane, northern. Terrestrial alluvial fan depositional setting is inferred from basal polymict conglomerates, fines upwards into shallow marine facies in upper part with sediment derived from the New England Orogen. ca 313 Ma and ca 247 Ma detrital zircon maximum depositional ages from lower and upper parts. Age constrained by Lower Triassic bivalves and ammonoids in upper part, and Dicroidium odontopteroides plant fossils in uppermost part that indicate a Ladinian to earliest Carnian age. Numerous east-dipping thrust faults cause repitition of stratigraphy. See also p66 Fig.6.|252-236 Ma, ca 313 Ma, ca 247 Ma detrital zircon||lower Brooweena Formation, upper Brooweena Formation[?]|Overlies Teebar Formation.|Contains basal polymictic cobble conglomerate fining upwards to pebble conglomerate interbedded with coarse sandstone. Stratified pebble-granule conglomerate, sandstone and siltstone in lower part, medium-grained olive-green sandstone in upper part.|
2660|Broughton River Granodiorite|22847|3|Fully described|p 54|Early Devonian||||||||
2660|Broughton River Granodiorite|23422|4|Described|p176, p214 Table 6.8|Early Devonian|Early Devonian|Of Broughton River Supersuite.||||||
2660|Broughton River Granodiorite|23429|5|Briefly described|Fig 13.25(b) p446|||||||||
2660|Broughton River Granodiorite|23430|5|Briefly described|p480|||||||||
2660|Broughton River Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 471. I-Type.||||||
2660|Broughton River Granodiorite|41668|6|Mentioned|p33|||||||||
2660|Broughton River Granodiorite|42054|6|Mentioned|p272|||||||||
2660|Broughton River Granodiorite|42633|5|Briefly described|Table 1 P7|||||||||
2660|Broughton River Granodiorite|42750|2|Defined|p45|Early Devonian||K-Ar age of 408 +/- 30 Ma.||||||
2660|Broughton River Granodiorite|43093|4|Described|Appendix 1|||Rb/Sr age of 406+/-4Ma.||||||
2660|Broughton River Granodiorite|43259|4|Described|Appendix 1,p50.|Early Devonian|Late Silurian|Rb-Sr age is 406+/-4 Ma.||||||
2660|Broughton River Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
2660|Broughton River Granodiorite|62074|5|Briefly described|p3|Early Devonian|Early Devonian|Well-defined on radiometric images; low gravity reading. Youngest granitic intrusion in the area.|c.406 Ma (Huttton and Rienks, 1997).||||Composite pluton, with a felsic core surrounded by a mafic rim.|
2660|Broughton River Granodiorite|62075|6|Mentioned|p15 Fig.7|Early Devonian|Early Devonian|Ravenswood batholith. Appears as Broughton River granodiorite.||||||
2660|Broughton River Granodiorite|62521|5|Briefly described|p7 Tb. 1, p19-20|Devonian|Devonian|Age: 406+/-4Ma (Rb-Sr). Geological Province: Ravenswood Batholith. Equivalent to Prices Cattle Creek Granodiorite of Hartley and others (1989). Ranges from orthopyroxene-clinopyroxene-biotite-quartz monzodiorite to hornblende-biotite granite.||||||21-DEC-07
2660|Broughton River Granodiorite|68731|6|Mentioned|p150|||||||||
2660|Broughton River Granodiorite|69592|5|Briefly described|p293-294|||Ravenswood Batholith, Charters Towers Province. Well-defined gravity lows suggest deep-seated, steep-sided plutons.||Broughton River Suite.|||Medium-K to high-K granodiorite; a zoned/composite pluton with a lower-K core that was not produced by feldspar fractionation of the rest of the pluton; an orthopyroxene/clinopyroxene-bearing granite sheath around the eastern end.|
2709|Brumby Sandstone Member|31305|6|Mentioned|Fig. 1|||||||||
2709|Brumby Sandstone Member|34009|6|Mentioned|p110|||||||||
2709|Brumby Sandstone Member|35873|6|Mentioned|p16|||||||||
2709|Brumby Sandstone Member|37705|6|Mentioned|Fig.1|||||||||
2709|Brumby Sandstone Member|43185|5|Briefly described|11||Triassic|||||||
2709|Brumby Sandstone Member|43982|14|Not recorded|Map Legend|||||||||
2709|Brumby Sandstone Member|43990|14|Not recorded|Map Legend||Triassic|Part of Mimosa Group.||||||
2709|Brumby Sandstone Member|43994|14|Not recorded|Map Legend||Triassic|Part of the Mimosa Group.||||||
2709|Brumby Sandstone Member|44022|14|Not recorded|Map Legend||Triassic|||||||
2709|Brumby Sandstone Member|44023|4|Described|Tb.3||Triassic|||||||
2709|Brumby Sandstone Member|44337|5|Briefly described|Map Legend||Triassic|Lithology.||||||
2709|Brumby Sandstone Member|44390|14|Not recorded|p6,8,Tb.1||Early Triassic|Of Mimosa Group.||||||
2709|Brumby Sandstone Member|44391|14|Not recorded|Map Legend||Early Triassic|Part of Rewan Formation.||||||
2709|Brumby Sandstone Member|45071|3|Fully described|Table 14|||||||||
2709|Brumby Sandstone Member|48898|6|Mentioned|Fig.4|||Triassic||||||
2709|Brumby Sandstone Member|48900|2|Defined|p41|Triassic|Triassic|||||||
2709|Brumby Sandstone Member|48919|5|Briefly described|p29|||See also P30-32 L.Triassic||||||
2709|Brumby Sandstone Member|65115|5|Briefly described|p420, Fig 14 p421|Early Triassic|Early Triassic|unconformity at base. Of Saggitarius Sandstone, Rewan Group. Coarse-grained sandstone, minor mudstone. Underlies Arcadia Formation. Shown as Brumby Sandstone in Fig 14.||||||
2709|Brumby Sandstone Member|65118|6|Mentioned|p491|Early Triassic|Early Triassic|In the middle of the Rewan Group.||||||
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
2732|Bryden Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
2732|Bryden Formation|22845|6|Mentioned|p82|Triassic|Permian|||||||
2732|Bryden Formation|22846|6|Mentioned|p36,67|Middle Triassic|Early Triassic|||||||
2732|Bryden Formation|23440|4|Described|p140|Triassic|Triassic|Of Toogoolawah Group.||||||18-AUG-08
2732|Bryden Formation|23799|6|Mentioned|p36, p39|Middle Triassic|Early Triassic|See also p127.||||||
2732|Bryden Formation|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 1500m.||||||
2732|Bryden Formation|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Conglomerate, sandstone, shale, minor tuff.||||||
2732|Bryden Formation|30302|6|Mentioned|p414|||Lower to Middle Triassic||||||
2732|Bryden Formation|30473|6|Mentioned|p377|||Part of Toogoolawah Group. Refers Cranfield and Schwarzbock(1972)||||||
2732|Bryden Formation|30508|6|Mentioned|p91|||Palynology||||||
2732|Bryden Formation|31811|6|Mentioned|Fig. 1|||||||||
2732|Bryden Formation|35101|3|Fully described|p35|||||||||
2732|Bryden Formation|35161|6|Mentioned|p591|||||||||
2732|Bryden Formation|35427|6|Mentioned|p121|||||||||
2732|Bryden Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
2732|Bryden Formation|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
2732|Bryden Formation|36954|6|Mentioned|p114|||||||||
2732|Bryden Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
2732|Bryden Formation|37755|6|Mentioned|p79|||||||||
2732|Bryden Formation|38304|6|Mentioned|p83|||||||||
2732|Bryden Formation|39079|5|Briefly described|p8|||||||||
2732|Bryden Formation|39445|5|Briefly described|Table 9|||||||||
2732|Bryden Formation|39943|6|Mentioned|Table 12A|||||||||
2732|Bryden Formation|40051|4|Described|p8|||||||||
2732|Bryden Formation|40245|6|Mentioned|p182|||||||||
2732|Bryden Formation|40475|6|Mentioned|p7|||||||||
2732|Bryden Formation|40623|5|Briefly described|p65|||||||||
2732|Bryden Formation|41917|6|Mentioned|Fig.3 P528|||||||||
2732|Bryden Formation|42492|5|Briefly described|Table 2 P14|||||||||
2732|Bryden Formation|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
2732|Bryden Formation|43008|5|Briefly described|map legend|||||||||
2732|Bryden Formation|43009|5|Briefly described|Map Legend|||||||||
2732|Bryden Formation|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||18-AUG-08
2732|Bryden Formation|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Conglomerate, sandstone, shale.||||||23-DEC-09
2732|Bryden Formation|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Conglomerate, sandstone, shale, minor tuff||||||
2732|Bryden Formation|61782|5|Briefly described|p275, p277, p277 Fig. 3, p278|||Geological Province: Esk Trough. ||||||
2732|Bryden Formation|63821|6|Mentioned|p20|||Correlated with Gayndah Formation. Geological Province: Esk Trough.||||||07-FEB-11
2732|Bryden Formation|65668|6|Mentioned|p23|Middle Triassic|Early Triassic|Dated by palynology. Intruded by Avoca Creek Granodiorite.||||||
2732|Bryden Formation|67402|4|Described|p165 tbl LPB1, p204|Anisian|Anisian|Esk Trough. Only present in the eastern part of the Esk Trough. Deposited in a fluvial environment. Time equivalent of the Esk Formation. Contains a potential intraformational shale seal. Approximately 450m thick.  See also p205, p206 fig ESK/ABR6, p208, p209.||Toogoolawah Group||Conformably overlain by the Neara Volcanics.|Conglomerate, sandstone and shale.|
2732|Bryden Formation|68679|5|Briefly described|p326, p386, p389-391, p471|||Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Has a restricted, discontinuous outcrop on the E margin of the Esk Basin. Up to ~1500m thick locally. The type section, adjacent to Lake Somerset, has two subunits: a lower 410m dominated by shale and sandstone, and an upper 506m of mainly conglomerate. Differing stratigraphic interpretations discussed.||Toogoolawah Group.||Overlies Marumba beds. Is faulted against and unconformably overlies Northbrook beds.|Interbedded sandstone, shale and pebble to cobble conglomerate; thin tuff, coal lenses, trachyte, andesite and redbeds are also described.|
2732|Bryden Formation|72297|5|Briefly described|p712|Triassic|Triassic|Monsildale, 43km ESE of Nanango.|||||Mudstone and tuff, with quartz-calcite breccia and veins hosting cinnabar and native mercury.|
2732|Bryden Formation|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.||Toogoolawah Group.||||
2732|Bryden Formation|73450|6|Mentioned|p107|||||||||
2809|Buddawadda Basalt Member|23065|6|Mentioned|15|||Geol province Lawn Hill Subprovince. Parent Peters Creek Volcanics||||||
2809|Buddawadda Basalt Member|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2809|Buddawadda Basalt Member|23406|5|Briefly described|p601 Fig.3|||||||||
2809|Buddawadda Basalt Member|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
2809|Buddawadda Basalt Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|36012|3|Fully described|Table 3|||See also p16.||||||01-AUG-07
2809|Buddawadda Basalt Member|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||01-AUG-07
2809|Buddawadda Basalt Member|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|38237|6|Mentioned|Fig.3|||||||||
2809|Buddawadda Basalt Member|38584|4|Described|p15|||||||||
2809|Buddawadda Basalt Member|39925|6|Mentioned|Fig.9|||||||||
2809|Buddawadda Basalt Member|41721|6|Mentioned|p28|||Of Peters Creek Volcanics. Lower section has been named Buddawadda Basalt Member and is considered to be equivalent to Seigal Volcanics.  Contains vesicular and massive basaltic lavas with interbeds of fine and medium feldspathic and glauconitic sandstone||||||01-AUG-07
2809|Buddawadda Basalt Member|45166|5|Briefly described|p71|||||||||
2809|Buddawadda Basalt Member|49001|2|Defined|p7|Carpentarian|Carpentarian|Basal member of Peters Creek Volcanics.||||||
2809|Buddawadda Basalt Member|67323|5|Briefly described|Mount Isa Block Time-Space Plot.|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl. Camooweal-Murphy Domain, Mount Isa Inlier. Leichhardt Superbasin. Abbreviated to Buddawadda Bslt in the Time-Space Plot. See also Buddawaddah Basalt Member (p9).||Peters Creek Volcanics|||Vesicular, amygdaloidal and massive basalt; minor siltstone and sandstone|
2809|Buddawadda Basalt Member|69591|5|Briefly described|p33-34, p38|||Camooweal-Murphy Domain, Leichhardt Superbasin. Correlation with Seigal Volcanics is speculative.||Basal Peters Creek Volcanics.||Equated with the Eastern Creek Volcanics.||
2867|Bulgonunna Volcanic Group|22675|3|Fully described|p41|Early Permian|Late Carboniferous|||||||
2867|Bulgonunna Volcanic Group|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
2867|Bulgonunna Volcanic Group|23080|5|Briefly described|p695 (Fig 1)|||||||||
2867|Bulgonunna Volcanic Group|23161|4|Described|p17 table3|Early Permian|Late Carboniferous|Age: 304.7+/-6.2 Ma.||||||
2867|Bulgonunna Volcanic Group|23162|5|Briefly described|p876||Carboniferous|Of Oversby et al 1994. Correlate of Urannah Suite.||||||07-OCT-08
2867|Bulgonunna Volcanic Group|23430|5|Briefly described| p491, 495|||||||||
2867|Bulgonunna Volcanic Group|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V72. I-Type.||||||
2867|Bulgonunna Volcanic Group|41825|5|Briefly described|p205|||||||||
2867|Bulgonunna Volcanic Group|42474|5|Briefly described|p29|||Mount Coolon 1:250 000 sheet.||||||
2867|Bulgonunna Volcanic Group|42701|3|Fully described|p32|Late Carboniferous||Redefinition of Bulgonunna Volcanics of Malone et al 1964.||||||
2867|Bulgonunna Volcanic Group|43213|6|Mentioned|p149|Late Carboniferous|Late Carboniferous|See also Bulgonunna Volcanics (p169-170). Unconformably overlies the folded Drummond Basin succession.|c.300 Ma (McPhie et al.,1990; Black, 1994).|||||
2867|Bulgonunna Volcanic Group|43259|4|Described|Appendix 1,p7.|Early Permian|Late Carboniferous|Lower Association. Rb-Sr age 287+/-3 Ma.||||||
2867|Bulgonunna Volcanic Group|43391|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Geological Province: Coastal Ranges Igneous Province.||||||23-JUN-04
2867|Bulgonunna Volcanic Group|43727|5|Briefly described|p2||Late Carboniferous|U-Pb dating: 356 Ma||||||
2867|Bulgonunna Volcanic Group|43734|5|Briefly described|p1|||||||||
2867|Bulgonunna Volcanic Group|44245|5|Briefly described|Map Legend||Carboniferous|||||||
2867|Bulgonunna Volcanic Group|60298|6|Mentioned|p192|||Geological Province: New England Orogen. QLD.||||||17-DEC-07
2867|Bulgonunna Volcanic Group|60659|4|Described|p11, p15|Late carboniferous|Late Carboniferous|Unconformable on Mount Wyatt Formation. Age: 287+/-12Ma (Rb-Sr) and 305-293Ma (U-Pb zircon). Of the Bulgonunna Province (overlying Drummond Basins sequence). Further lithological detail included on p15.||||||07-FEB-11
2867|Bulgonunna Volcanic Group|61835|6|Mentioned|p193 Fig. 1|||||||||
2867|Bulgonunna Volcanic Group|62074|5|Briefly described|p2, p4|Permian|Late Carboniferous|Oversby et al. (1994). Crops out in the area S of the Burdekin Falls Dam. Mis-spelt as Bulgonumna on p2. Unconformably overlies the eastern margin of the folded Drummond Basin sequence. Mainly intra caldera felsic volcanism: thick ignimbrite sheets and only sparsely developed sedimentary rocks.|||||Thick felsic ignimbrites and rhyolitic to dacitic volcanics.|
2867|Bulgonunna Volcanic Group|65114|5|Briefly described|p383 Tb.1, p397|Cisuralian|Upper Carboniferous|305-294 Ma; Tectonic unit: NE part of the Drummond Basin; provides evidence for a major felsic event that started about 305 Ma and continued until at least 294 Ma||||||
2867|Bulgonunna Volcanic Group|65706|4|Described|p10, p14 Tbl.1, p15 Tbl.1,|Late Carboniferous|Late Carboniferous|Crops out near Burdekin Weir. Shortened to Bulgonunna Volcanics on p78 and 107.||||Unconformably overlies Cape River Metamorphics and Mount Windsor Volcanics; unconformably underlies Lizzie Creek Volcanic Group and Collinsville Coal Measures.|Rhyolitic to dacitic ignimbrite and lava flows and domes, with minor andesite and tuffaceous sediments.|
2867|Bulgonunna Volcanic Group|66086|5|Briefly described|Map legend|Carboniferous|Carboniferous|Intrusive rhyolite and felsic volcanics, extrusive rhyolite and rhyolite autobreccia; mainly grey, moderately crystal-rich dacitic ignimbrite, subsidiary buff crystal-poor rhyolitic ignimbrite.||||||
2867|Bulgonunna Volcanic Group|67669|6|Mentioned|p10-11|Late Carboniferous|Late Carboniferous|Of Bowen Basin. ||||||
2867|Bulgonunna Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Late Carboniferous|||||||
2867|Bulgonunna Volcanic Group|68679|5|Briefly described|p347, p362, p368, p375|Permian|Pennsylvanian|Northern New England Orogen. Produced during major extension ~300-290 Ma.|c.292 Ma.||Earlscliffe Dacite.||Silicic magmatism.|
2867|Bulgonunna Volcanic Group|68731|6|Mentioned|p193|||||||Underlain by the Mount Coolon Andesite.||
2867|Bulgonunna Volcanic Group|68822|5|Briefly described|p338|Sakmarian|Kasimovian||305 - 294 Ma|||||27-JUL-15
2867|Bulgonunna Volcanic Group|68900|6|Mentioned|p4, p26, p28|Early Permian|Late Carboniferous|Drummond Basin.||||||
2867|Bulgonunna Volcanic Group|68901|5|Briefly described|p2,3,5, p114-p115, p117-118, p121|Early Permian|Late Carboniferous|Kennedy Igneous Association. The rhyolitic ignimbrite (Earlscliffe Dacite) is probably intruded by Nostone Creek Granodiorite.|305-292 Ma (SHRIMP, Black, 1994; this volume)||Includes the Pyramid Rhyolite and Earlscliffe Dacite.||Sample - Rhyolitic ignimbrite.|16-NOV-18
2867|Bulgonunna Volcanic Group|69593|4|Described|p492-493, p495, p497, p509, p513||Late Carboniferous|Paluma and Burdekin Falls Subprovinces, Kennedy Igneous Association. Emplaced during a period of major extension; tectonics discussed. Some units' Sm-Nd isotope data tabulated.|~305-292 Ma.||Arundel, Bobby Dazzler, Collins Creek, Locharwood, Pinang, Pyramid Rhyolites; Earlscliffe, Smedley Dacites.||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
2867|Bulgonunna Volcanic Group|69952|5|Briefly described|p85, p131|Permian|Late Carboniferous|Thomson Orogen. Overlies the northern part of the Anakie Province. Range of ages by Black (1994) and Cross et al. (2012).|305-292 Ma.|||||
2867|Bulgonunna Volcanic Group|70740|4|Described|i, iii, p2, p5-p8, p27, p47, p48|Late Carboniferous|Late Carboniferous|Drummond Basin. Unnamed units and their relationships, distribution, ages and lithologies are discussed on pages 83-88. Mistakenly referred to as the Bulgonunna Volcanics on p87. Also includes the Whitestone Creek Dacite, Yacamunda Creek Dacite, Black Creek Rhyolite, Smedley Dacite, Pyramid Rhyolite, Arundel Rhyolite, Hidden Valley Rhyolite, Locharwood Rhyolite and the Bungobine Rhyolite. See also p49, p53 fig 27, p54, p55, p64-p66, p71-p74, p77, p80-p83, p87-p89, p92-p93, p95-p96, p98-p99, p102-p103, p105-p106, p109-p110, p112, p114 fig 69, p115-p125, p129, p130.|||Includes the Bobby Dazzler Rhyolite, Conway Volcanics, Collins Creek Rhyolite, Earlscliffe Dacite.|Unconformably overlies the Mount Wyatt Formation and the Bimurra Volcanics. Overlies Stones Creek Volcanics, Ukalunda Formation.||
2867|Bulgonunna Volcanic Group|71592|5|Briefly described|Appendix A.|||Drummond Basin.|292+/-2.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite, ignimbrite.|
2867|Bulgonunna Volcanic Group|71710|5|Briefly described|p385|Late Carboniferous|Late Carboniferous|Geological province: eastern Hinterland. Coincident with crustal thinning onset during formation of Bowen Basin and Lovelle Depression.||||Correlated with tuff horizons and syndepositional volcanism during deposition of upper Jericho and Jochmus formations.||22-MAY-19
2867|Bulgonunna Volcanic Group|73035|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Informally subdivided into 4 units. Some polygons are uncertainly identifed.|||||Intrusive rhyolite, felsic volcanics, extrusive rhyolite, rhyolite auto-breccia, ignimbrite. Coherent + autoclastic dacite; many extensive lava flows/domes. Fine-grained amygdaloidal basalt, minor mafic volcaniclastics, high-level mafic intrusives.|
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||
2917|Bulliwallah Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Lithic and feldspathic sandstone, with minor siltstone, mudstone and tuff. Max. thickness: 1800m. Geological Province: Drummond Basin.||||||21-OCT-08
2917|Bulliwallah Formation|30151|6|Mentioned|p13|||See also Fig.3 Upper Devonian? - Lower Carboniferous age.||||||
2917|Bulliwallah Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous.||||||21-OCT-08
2917|Bulliwallah Formation|32490|4|Described|Table 1|Late Carboniferous||L.Carb. part of Drummond Gp.||||||02-NOV-07
2917|Bulliwallah Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
2917|Bulliwallah Formation|32553|4|Described|p46|||||||||
2917|Bulliwallah Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
2917|Bulliwallah Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
2917|Bulliwallah Formation|34408|6|Mentioned|p185|||Early Carboniferous. On Table.||||||02-NOV-07
2917|Bulliwallah Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
2917|Bulliwallah Formation|35811|6|Mentioned|Fig.3|||||||||
2917|Bulliwallah Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
2917|Bulliwallah Formation|37573|4|Described|Table 2|||||||||
2917|Bulliwallah Formation|39445|5|Briefly described|Table 6|||||||||
2917|Bulliwallah Formation|41125|6|Mentioned|p42|||||||||
2917|Bulliwallah Formation|41710|5|Briefly described|p225|||||||||
2917|Bulliwallah Formation|42486|5|Briefly described|p201|||||||||
2917|Bulliwallah Formation|42547|5|Briefly described|Fig.17 p61|||||||||02-NOV-22
2917|Bulliwallah Formation|42701|6|Mentioned|Table 1, p.19|||Old stratigraphic term. Name doesn't apply in this area.||||||02-NOV-22
2917|Bulliwallah Formation|43105|6|Mentioned|p12|||||||||
2917|Bulliwallah Formation|45073|3|Fully described|p44|||Section p45. Refers de Bretizel (1966).||||||02-NOV-22
2917|Bulliwallah Formation|45151|5|Briefly described|Table 6|||||||||
2917|Bulliwallah Formation|48914|6|Mentioned|p35|||L.Carb.||||||
2917|Bulliwallah Formation|60659|4|Described|p14|Early Carboniferous|Early Carboniferous|Fluviatile/lacustrine deposits well-bedded qtz sst with interbedded lithic sst, feldspathic sst, olive-green mudstone, tuff+ volcanolithic sst. Conformably overlies Raymond + Star of Hope Fms; conform overlain; Natal Fm. Geol Prov: Drummond Basin.||||||18-JUN-13
2917|Bulliwallah Formation|61394|6|Mentioned|p968|||||||||
2917|Bulliwallah Formation|64315|6|Mentioned|p511|||Northern Drummond Basin equivalent of Ducabrook Formation of the southern Drummond Basin. Contains Gyracanthids and ?Acanthodes.||||||21-OCT-08
2917|Bulliwallah Formation|64849|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Fine to medium feldspathic quartz sandstone; minor olive mudstone, pebbly feldspathic quartz sandstone and algal limestone; poorly preserved plant fossils.||||||
2917|Bulliwallah Formation|64850|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Fine to medium feldspathic quartz sandstone, minor olive mudstone, pebbly feldspathic quartz sandstone and algal limestone; poorly preserved plant fossils.||||||09-FEB-09
2917|Bulliwallah Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Fine to medium feldspathic quartz sandstone; minor olive mudstone; pebbly feldspathic quartz sandstone and algal limestone; poorly preserved plant fossils.||||||10-FEB-09
2917|Bulliwallah Formation|66188|6|Mentioned|Fig 3, TB1, Fig 16-17|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
2917|Bulliwallah Formation|66498|6|Mentioned|p49|||Northern Drummond Basin.|||||Includes siltstone nodules containing fossil fish (species listed).|
2917|Bulliwallah Formation|67402|4|Described|p165 tbl LPB1, p196 fig DRM2|Visean|Visean|Drummond Basin. Deposited in a low energy fluvio-lacustrine environment. Greater than 600m thick. See also p197, p198 fig DRM3, p200, p201, p202, p203 fig DRM11.||||Overlies the Star of Hope Formation. Overlain by the Natal Formation.|Quartz, lithic and feldspathic sandstone interbedded with tuff, volcano-lithic sandstone and thin olive-green mudstones.|
2917|Bulliwallah Formation|68329|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Conformably overlies Star of Hope Formation. Is overlain conformably by Natal Formation.|Fine to medium feldspathic quartz sandstone; minor olive mudstone, pebbly feldspathic quartz sandstone and algal limestone; poorly preserved plant fossils.|
2917|Bulliwallah Formation|68413|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||Conformably underlain by the Star of Hope Formation.|Fine to medium feldspathic quartz sandstone; minor olive mudstone, pebbly feldspathic quartz sandstone and algal limestone; poorly preserved plant fossils.|
2917|Bulliwallah Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Ducabrook, Mount Rankin, Natal and Star of Hope Formations, are all mapped under the symbol, Cd3.||||||
2917|Bulliwallah Formation|68731|5|Briefly described|p191 Fig 3.102, p195|Mississippian|Mississippian|Drummond Basin. < 1800 m thick. Fossil fish are preserved and include actinopterygians, sacropterygians, Gyracanthides, and the acanthodiform Acanthodopsis ruselli (Burrow 2004). Detailed lithology discussed.||||Conformably underlain by the Star of Hope Formation. Overlain by the Natal Formation.|Comprises thin- to thick-bedded sandstone that ranges from quartz-lithic through feldspar-lithic to volcaniclastic and subordinate siltstone.|10-MAY-16
2917|Bulliwallah Formation|68900|2|Defined|p4, p37, p70-p73|Carboniferous|Carboniferous|Drummond Basin. Originally named by De Bretizel (1966) to recognize the lithological change between the fluvial Raymond Formation package and a volcanogenic sedimentary sequence in Bulliwallah Syncline. Olgers (1970) divided the package into a lower unit retaining the Bulliwallah Formation and an upper unit called the Natal Formation. The type area is defined as the Bulliwallah Range in SCARTWATER. This unit occurs in the northern Drummond Basin extending from the southern part of PAJINGO through NATAL DOWNS, SCARTWATER, MOUNT TUTAH and BULLIWALLAH. This unit is commonly well exposed and forms extensive low-lying outcrops with some large bouldery outcrops. This unit is readily identifiable by a uniformly high potassium signature on airborne radiometric images but is not visible in magnetics. This unit represents a fluvial sedimentary sequence sourced from uplifted volcanic terrain. Measured thickness is estimated at 2200m in the western limb of the Bulliwallah Syncline. Lycopod stems suggest an early Carboniferous age. This unit is probably a time equivalent of the Ducabrook Formation.||||Conformably overlies the Star of Hope Formation. Conformably overlain by the Natal Foramtion.|light grey to light tan, medium- to coarse-grained, laminated, moderately to well sorted, medium- to thick-bedded and trough cross bedded sandstone. Less common white to l;ight tan, laminated and thinly bedded siltstone is also present.|
2917|Bulliwallah Formation|71710|5|Briefly described|p370, p376 Fig 10, p377 Fig 11, p381|Early Carboniferous|Early Carboniferous|Geological province: northern Drummond Basin.||||Overlain by Natal Formation. Underlain by Star of Hope Formation. Equivalent to lower part of Ducabrook Formation in the southern Drummond Basin.||
2917|Bulliwallah Formation|73198|4|Described|p499-501, p505-511, p514-515|||Drummond Basin, north. Originally part of Cycle 3 of Olgers (1972); combined with Cycle 2 herein. Maximum thickness: 1800 m. Minimum thickness of 400 m. Relatively consistent thickness. Contact with underlying Star of Hope Formation is erosional but probably conformable. Most lithologically diverse unit in the basin succession. Fine plant debris, rootlet structures and bioturbation are locally present and rare shell fragments are also present. Fining-upward trend above a distinct gravel-sized interval in the middle of the sequence. [See article for petrographic descriptions and data].||||Conformably underlain by Star of Hope Formation. Conformably overlain by Natal Formation. Equivalent to Ducabrook Formation.|Quartz, lithic and feldspathic sandstones and lesser mudstone, sedimentary breccia, and conglomerate; common interbedded primary volcaniclastic beds of non-welded and both crystal- and ash-rich silicic tuffs and ignimbrites|02-NOV-22
2963|Bundamba Group|12597|5|Briefly described|p491, p492 Tb.1, p493 Fig.2|Bathonian|Rhaetian|Clarence-Moreton Basin.|||Includes Marbung and Woogaroo Subgroups and Laytons Range Conglomerate.|||
2963|Bundamba Group|13516|5|Briefly described|p159 fig 8, p163, p166, p168, p164|Early Jurassic|Late Triassic|From Clarence-Moreton Basin.|||Includes Woogaroo Subgroup, Marburg Subgroup|||
2963|Bundamba Group|22857|5|Briefly described|p281, p284, p296-7 Tb.22.1|Early Jurassic|Late Triassic|Comprises two subgroups: the Woogaroo Subgroup and the Marburg Subgroup. Geological Province: Surat and Clarence-Moreton Basins. See also p548 App.1 Tb.A1.12.||||||
2963|Bundamba Group|22861|5|Briefly described|p281,284|Jurassic|Late Triassic|||||||
2963|Bundamba Group|22865|4|Described|p314,Table22.1p296-7|Middle Jurassic||Comprises of: Woogaroo and Marburg Subgroups.||||||
2963|Bundamba Group|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
2963|Bundamba Group|22991|5|Briefly described|p324|Jurassic|Triassic|||||||
2963|Bundamba Group|23720|5|Briefly described|Map Legend|Middle Jurassic|Late Triassic|Polymictic and quartz conglomerate, quartz and quartz-lithic sandstone, fossil wood, sitlstone, claystone, minor coal.||||||15-DEC-04
2963|Bundamba Group|23799|3|Fully described|p46|Late Triassic|Middle Triassic|Formerly Ipswich and Walloon Beds (lower and upper coal measures) of Cameron (1905,1907) separated by unproductive sandstone,  Bundamba Beds or Grits.  Now redefined to include the Woogaroo Subgroup/Marburg Fm.  Geol. Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|23811|5|Briefly described|Map Legend|||Includes the Marburg and Woogaroo Subgroups. Geological Province: Clarence-Moreton Basin.||||||11-JAN-10
2963|Bundamba Group|23812|5|Briefly described|p35, p33 Fig.6|Early Jurassic|Late Triassic|Overlying unit: Walloon Coal Measures.  Geological  Province: Clarence-Moreton Basin.  Comprised of Marburg and Woogaroo Subgroups.||||||
2963|Bundamba Group|23843|4|Described|p455|Jurassic|Late Triassic|Geological Province: Moreton Basin.||||||
2963|Bundamba Group|23888|6|Mentioned|p262|||||||||
2963|Bundamba Group|24068|5|Briefly described|p270 Table 2|||Geological Province: Moreton Basin.||||||
2963|Bundamba Group|24081|6|Mentioned|p451|||Geological Province: Moreton Basin.||||||
2963|Bundamba Group|24127|5|Briefly described|p5|Jurassic|Triassic|||||||
2963|Bundamba Group|24129|5|Briefly described|p5|Jurassic|Triassic|||||||24-JAN-05
2963|Bundamba Group|24237|6|Mentioned|p6|||||||||
2963|Bundamba Group|24299|5|Briefly described|p3|Jurassic|Triassic|||||||
2963|Bundamba Group|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|29385|6|Mentioned|p80|||Incl.Marburg Ss,Ripley Road Ss,Raceview Fm & Aberdare Cngl.See P81,82.||||||
2963|Bundamba Group|29386|6|Mentioned|p454|||||||||
2963|Bundamba Group|29420|6|Mentioned|p98|||||||||
2963|Bundamba Group|29591|6|Mentioned|p85|||||||||
2963|Bundamba Group|29720|6|Mentioned|p79|||||||||
2963|Bundamba Group|29869|6|Mentioned|p33|||||||||
2963|Bundamba Group|29995|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
2963|Bundamba Group|30058|6|Mentioned|p3|||||||||
2963|Bundamba Group|30086|5|Briefly described|p4|||Triassic||||||
2963|Bundamba Group|30087|6|Mentioned|p3|||See also P4. Consists of Raceview Formation, Aberdare Conglomerate.||||||
2963|Bundamba Group|30131|6|Mentioned|p9|||||||||
2963|Bundamba Group|30302|6|Mentioned|p416|||Upper Jurassic to Middle Jurassic age.See also P414,415||||||
2963|Bundamba Group|30303|6|Mentioned|p322|||Unconformable on Crow's Nest Granite||||||
2963|Bundamba Group|30455|6|Mentioned|p5|||See also P12,17,21||||||
2963|Bundamba Group|30457|6|Mentioned|p96|||||||||
2963|Bundamba Group|30458|6|Mentioned|p1|||See also P19||||||
2963|Bundamba Group|30459|6|Mentioned|p309|||||||||
2963|Bundamba Group|30460|6|Mentioned|p5|||Upper Triassic age. See also P12,13,14,20,22,26||||||
2963|Bundamba Group|30463|6|Mentioned|p464|||Jurassic-Triassic||||||
2963|Bundamba Group|30464|6|Mentioned|Fig.1|||Jurassic-Triassic, see also P1||||||
2963|Bundamba Group|30465|6|Mentioned|p3|||||||||
2963|Bundamba Group|30466|6|Mentioned|Fig.1|||||||||
2963|Bundamba Group|30470|6|Mentioned|p457|||||||||
2963|Bundamba Group|30471|6|Mentioned|p129|||||||||
2963|Bundamba Group|30474|6|Mentioned|p247|||Microfloras||||||
2963|Bundamba Group|30475|5|Briefly described|p162|||Palynology||||||
2963|Bundamba Group|30477|6|Mentioned|p461|||||||||
2963|Bundamba Group|30478|6|Mentioned|p272|||||||||
2963|Bundamba Group|30508|6|Mentioned|p91|||Stratigraphy.||||||
2963|Bundamba Group|30517|6|Mentioned|p436|||||||||
2963|Bundamba Group|30565|6|Mentioned|p129|||||||||
2963|Bundamba Group|30655|6|Mentioned|p20|||||||||
2963|Bundamba Group|30687|5|Briefly described|p63|||See also P64,65,76,77. Lower Jurassic age||||||
2963|Bundamba Group|30785|6|Mentioned|p397|||||||||
2963|Bundamba Group|30914|6|Mentioned|Map legend|Jurassic|Triassic|Triassic to Jurassic||||||
2963|Bundamba Group|30915|6|Mentioned|p97|||||||||
2963|Bundamba Group|30916|6|Mentioned|p97|||||||||
2963|Bundamba Group|31118|4|Described|p311|||||||||
2963|Bundamba Group|31276|6|Mentioned|p151|||Correlation. Palynology||||||
2963|Bundamba Group|31450|6|Mentioned|p47|||||||||
2963|Bundamba Group|31811|6|Mentioned|Fig. 1|||||||||
2963|Bundamba Group|32136|6|Mentioned|p1|||Refers de Jersey (1971)||||||
2963|Bundamba Group|32176|6|Mentioned|p2|||See also P3||||||
2963|Bundamba Group|32179|6|Mentioned|p3|||Trias.||||||
2963|Bundamba Group|32180|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|32491|5|Briefly described|p19|||L.Jur.-U.Trias.||||||
2963|Bundamba Group|32492|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
2963|Bundamba Group|32801|6|Mentioned|Fig.9|||||||||
2963|Bundamba Group|32803|6|Mentioned|p94|||||||||
2963|Bundamba Group|32912|6|Mentioned|p157|||U.Trias.-L.Jurassic||||||
2963|Bundamba Group|32916|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
2963|Bundamba Group|33436|6|Mentioned|p233|||Jurassic||||||
2963|Bundamba Group|33476|6|Mentioned|Fig.10|||||||||
2963|Bundamba Group|33709|6|Mentioned|p104|||||||||
2963|Bundamba Group|33769|6|Mentioned|p150|||||||||
2963|Bundamba Group|33881|6|Mentioned|p96|||||||||
2963|Bundamba Group|34010|6|Mentioned|Cor. chart|||Upper Triassic||||||
2963|Bundamba Group|34134|6|Mentioned|p482|||Lower Jurassic||||||
2963|Bundamba Group|34254|6|Mentioned|p490|||||||||
2963|Bundamba Group|34261|14|Not recorded|Table p.100|||||||||
2963|Bundamba Group|34287|6|Mentioned|p158|||See also P171. Triassic||||||
2963|Bundamba Group|34340|3|Fully described|p465|||||||||
2963|Bundamba Group|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
2963|Bundamba Group|34400|5|Briefly described|p13|||||||||
2963|Bundamba Group|34452|6|Mentioned|p6|||U.Triassic||||||
2963|Bundamba Group|34505|6|Mentioned|p1|||Upper Triassic. See also P3.||||||
2963|Bundamba Group|34755|6|Mentioned|Map legend|Jurassic|Triassic|||||||
2963|Bundamba Group|35007|6|Mentioned|p75|||||||||
2963|Bundamba Group|35063|6|Mentioned|p80|||||||||
2963|Bundamba Group|35079|6|Mentioned|p424|||||||||
2963|Bundamba Group|35101|3|Fully described|p51|||||||||
2963|Bundamba Group|35126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
2963|Bundamba Group|35156|4|Described|p6|||See also Table.2||||||
2963|Bundamba Group|35188|6|Mentioned|p465|||||||||
2963|Bundamba Group|35428|6|Mentioned|p125|||Biostratigraphy||||||
2963|Bundamba Group|35648|6|Mentioned|p14|||||||||
2963|Bundamba Group|35937|6|Mentioned|Fig.4|||||||||
2963|Bundamba Group|36243|6|Mentioned|p74|||||||||
2963|Bundamba Group|36351|6|Mentioned|p373|||||||||
2963|Bundamba Group|36354|6|Mentioned|p366|||||||||
2963|Bundamba Group|36440|6|Mentioned|Map legend|Early Jurassic|Late Triassic|||||||
2963|Bundamba Group|36745|6|Mentioned|p71|||||||||
2963|Bundamba Group|36779|4|Described|p7|||||||||
2963|Bundamba Group|36825|6|Mentioned|p12|||||||||
2963|Bundamba Group|36899|6|Mentioned|p1095|||||||||
2963|Bundamba Group|36914|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|36954|6|Mentioned|p114|||||||||
2963|Bundamba Group|36961|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|37111|5|Briefly described|p292|||||||||
2963|Bundamba Group|37112|6|Mentioned|p298|||||||||
2963|Bundamba Group|37122|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
2963|Bundamba Group|37287|6|Mentioned|p36|||Mistakenly entered as in South Australia [CEBNov97]||||||
2963|Bundamba Group|37375|6|Mentioned|Fig.1|||||||||
2963|Bundamba Group|37616|6|Mentioned|p31|||||||||
2963|Bundamba Group|37812|6|Mentioned|p657|||||||||
2963|Bundamba Group|38064|5|Briefly described|p41|||||||||
2963|Bundamba Group|38074|5|Briefly described|Table 1|||||||||
2963|Bundamba Group|38076|6|Mentioned|Table 3|||||||||
2963|Bundamba Group|38306|6|Mentioned|p509|||||||||
2963|Bundamba Group|38307|6|Mentioned|p521|||||||||
2963|Bundamba Group|38358|6|Mentioned|p3|||||||||
2963|Bundamba Group|38441|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
2963|Bundamba Group|39079|5|Briefly described|p10|||||||||
2963|Bundamba Group|39445|6|Mentioned|Table 10|||||||||
2963|Bundamba Group|39494|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|39813|6|Mentioned|Map legend|Jurassic|Triassic|Triassic or Jurassic||||||
2963|Bundamba Group|39907|6|Mentioned|p5|||||||||
2963|Bundamba Group|40030|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|40051|6|Mentioned|p9|||||||||
2963|Bundamba Group|40245|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|40434|6|Mentioned|p25|||||||||
2963|Bundamba Group|40486|6|Mentioned|p84|||||||||
2963|Bundamba Group|40544|6|Mentioned|Fig.6|||||||||
2963|Bundamba Group|40579|6|Mentioned|Map legend|Early Jurassic|late Rhaetian|||||||
2963|Bundamba Group|40623|5|Briefly described|p36|||Mention Table 2||||||
2963|Bundamba Group|40896|6|Mentioned|p17|||||||||
2963|Bundamba Group|41099|6|Mentioned|Fig.9|||||||||
2963|Bundamba Group|41175|6|Mentioned|p195|||||||||
2963|Bundamba Group|41247|6|Mentioned|Fig.7|||||||||
2963|Bundamba Group|41535|6|Mentioned|Fig.2|||||||||
2963|Bundamba Group|41591|6|Mentioned|Fig.2|||||||||
2963|Bundamba Group|41631|5|Briefly described|p6|||||||||
2963|Bundamba Group|41906|5|Briefly described|p22|||||||||
2963|Bundamba Group|42248|5|Briefly described|p397|||See also Fig.2||||||
2963|Bundamba Group|42316|6|Mentioned|p7|||||||||
2963|Bundamba Group|42336|6|Mentioned|p4|||||||||
2963|Bundamba Group|42405|6|Mentioned|Table 3 P.7|||||||||
2963|Bundamba Group|42463|6|Mentioned|Fig.3 P170|||||||||
2963|Bundamba Group|42493|6|Mentioned|p20|||Moreton Basin||||||
2963|Bundamba Group|42525|5|Briefly described|Map legend|Middle Jurassic|Late Triassic|Includes the Woogaroo Sub-Group.||||||15-JUL-04
2963|Bundamba Group|42719|6|Mentioned|p15|||||||||
2963|Bundamba Group|42893|5|Briefly described|Fig.2 P7|||||||||
2963|Bundamba Group|42951|5|Briefly described|Fig.11|||||||||
2963|Bundamba Group|42987|6|Mentioned|p31|||||||||
2963|Bundamba Group|43001|6|Mentioned|Fig.3,p120|||||||||
2963|Bundamba Group|43072|6|Mentioned|p81|||||||||
2963|Bundamba Group|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Includes the Woogaroo and Marburg Subgroups. Geological Province: Clarence- Moreton Basin.||||||12-APR-05
2963|Bundamba Group|43161|6|Mentioned|36|||||||||
2963|Bundamba Group|43344|14|Not recorded|p13,102,104|Jurassic|Late Triassic|||||||
2963|Bundamba Group|43383|14|Not recorded|p24||Triassic|||||||
2963|Bundamba Group|43384|14|Not recorded|Map Legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|43404|14|Not recorded|p10|||||||||
2963|Bundamba Group|43453|14|Not recorded|Map Legend|Cretaceous|Triassic|(Provisional Edition)||||||
2963|Bundamba Group|43454|14|Not recorded|Map Legend|Cretaceous|Triassic|||||||
2963|Bundamba Group|43468|14|Not recorded|Map Legend|Jurassic|Triassic|Provisional Edition||||||
2963|Bundamba Group|43878|14|Not recorded|p85,86|||||||||
2963|Bundamba Group|43881|14|Not recorded|p2,6-7,29-38,170|||Incs.Mill Ck Stsn, Layton's Range Clm & Corindi Clm.Tabulam Gp is partial equiv.See also Lexicon.||||||
2963|Bundamba Group|43891|14|Not recorded|p312|||||||||
2963|Bundamba Group|43910|14|Not recorded|p1,2,7,10-1,13,17-20|||Should not be used in Great Artesian Basin. Spores and pollen grains from Bundamba Group. Fig. 2.||||||
2963|Bundamba Group|43911|14|Not recorded|p18|||||||||
2963|Bundamba Group|43918|14|Not recorded|p54,63,75|||||||||
2963|Bundamba Group|43919|14|Not recorded|p39,41|||||||||
2963|Bundamba Group|43920|14|Not recorded|p74,76|||||||||
2963|Bundamba Group|43921|14|Not recorded|p315,323|||||||||
2963|Bundamba Group|43922|14|Not recorded|p325,326|||Now dated as early Upper Triassic (from microflora)||||||
2963|Bundamba Group|43923|6|Mentioned|p1|||||||||
2963|Bundamba Group|43924|14|Not recorded|p2|||||||||
2963|Bundamba Group|43939|14|Not recorded|p106|||||||||
2963|Bundamba Group|43991|4|Described|p47,52||Triassic|Consists of Marburg Formation, Helidon Sandstone,"Swanbank Formation".||||||27-AUG-08
2963|Bundamba Group|43993|14|Not recorded|p95|||Ref. to Wilson 1958,1960.||||||
2963|Bundamba Group|43995|14|Not recorded|p8-63,Fig.3,4,5,9,13||Late Triassic|fig.15||||||
2963|Bundamba Group|43996|14|Not recorded|p88|||||||||
2963|Bundamba Group|43997|14|Not recorded|p113|||"This evidence on the age of the microfloras favours discontinuance of the term "Bundamba" to Jurassic sediments in the Surat Basin"||||||
2963|Bundamba Group|44028|14|Not recorded|Fig.2,p512||Jurassic|See Strat Table.||||||
2963|Bundamba Group|44030|14|Not recorded|p130|||||||||
2963|Bundamba Group|44031|14|Not recorded|Tb.2,p5,11||Early Jurassic|||||||
2963|Bundamba Group|44075|14|Not recorded|p251|||||||||
2963|Bundamba Group|44085|2|Defined|p4,13,16,17|||||||||
2963|Bundamba Group|44095|14|Not recorded|p283-6|||||||||
2963|Bundamba Group|44104|14|Not recorded|p280|||||||||
2963|Bundamba Group|44128|14|Not recorded|Tb.1,p426|||||||||
2963|Bundamba Group|44130|14|Not recorded|p281-283|||||||||
2963|Bundamba Group|44166|14|Not recorded|p14|||||||||
2963|Bundamba Group|44170|14|Not recorded|p20-22|||||||||
2963|Bundamba Group|44239|14|Not recorded|p279|||||||||
2963|Bundamba Group|44269|4|Described|p14-16,76,map||Triassic|||||||
2963|Bundamba Group|44346|14|Not recorded|p5|||||||||
2963|Bundamba Group|44375|14|Not recorded|Fig.45,p312|||||||||
2963|Bundamba Group|44377|14|Not recorded|p22|||||||||
2963|Bundamba Group|44450|4|Described|p28 Table 7|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|44510|2|Defined|p252-257|||Unconformably lies on Ipswich Coal Measures.||||||
2963|Bundamba Group|44542|14|Not recorded|p31|||||||||
2963|Bundamba Group|44554|14|Not recorded|p294-295|||See also Lexicon.||||||
2963|Bundamba Group|44572|14|Not recorded|p235|||||||||
2963|Bundamba Group|44581|14|Not recorded|p346|||||||||
2963|Bundamba Group|44608|14|Not recorded|p19|||||||||
2963|Bundamba Group|44610|14|Not recorded|p49,Tb.1|||||||||
2963|Bundamba Group|44633|14|Not recorded|p2|||||||||
2963|Bundamba Group|44654|14|Not recorded|Map Legend|||||||||
2963|Bundamba Group|44679|14|Not recorded|p272|||Moreton Basin; microflora gives early Upper Triassic age.||||||
2963|Bundamba Group|44680|14|Not recorded|p5|||||||||
2963|Bundamba Group|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
2963|Bundamba Group|44734|14|Not recorded|p5,11-13,19|||Pine Mountain area.||||||
2963|Bundamba Group|44752|14|Not recorded|p297|||||||||
2963|Bundamba Group|44771|14|Not recorded|p2,Fig.1||Triassic|||||||
2963|Bundamba Group|44774|4|Described|p30-32|||Covers whole of sediment interval between Ipswich and Walloon Coal Measures. Consists of basal Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone, which possibly grades up into Marburg Sandstone.||||||
2963|Bundamba Group|44775|4|Described|p7,9,map 2||Late Triassic|Includes Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone.||||||
2963|Bundamba Group|44776|14|Not recorded|p1,3||Late Triassic|||||||
2963|Bundamba Group|44783|14|Not recorded|p16,17,24,43|||||||||
2963|Bundamba Group|44784|14|Not recorded|map 3|||||||||
2963|Bundamba Group|44805|14|Not recorded|p388|||||||||
2963|Bundamba Group|44825|14|Not recorded|p53|||||||||
2963|Bundamba Group|44861|14|Not recorded|p266|||||||||
2963|Bundamba Group|44884|14|Not recorded|p2,3|||||||||
2963|Bundamba Group|44913|14|Not recorded|p53, Fig.1|||||||||
2963|Bundamba Group|45110|6|Mentioned|Table 18|||||||||
2963|Bundamba Group|46984|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|48585|4|Described|p7,8,10,14,15,Pl.1|||||||||
2963|Bundamba Group|48600|14|Not recorded|p6,14|||||||||
2963|Bundamba Group|48626|14|Not recorded|Fig.1|Jurassic|Triassic|||||||
2963|Bundamba Group|48900|6|Mentioned|p50|||||||||
2963|Bundamba Group|48917|6|Mentioned|p1|||Sandstone Leeds,targets or oil wells||||||
2963|Bundamba Group|48928|6|Mentioned|p7|||See also P15||||||
2963|Bundamba Group|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Includes: Woogaroo Subgroup, Marburg Subgroup.||||||
2963|Bundamba Group|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Moreton Basin||||||
2963|Bundamba Group|50631|5|Briefly described|Map Legend|Jurassic|Triassic|Includes: Helidon Sandstone, Marburg Formation.||||||
2963|Bundamba Group|60077|5|Briefly described|Map legend|Middle Jurassic|Late Triassic|Includes: Marburg Formation and Woogaroo Sub-Group.||||||
2963|Bundamba Group|60079|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|Sandstone, siltstone, claystone.||||||
2963|Bundamba Group|60281|5|Briefly described|p25, p28, Fig.18 App 1|Early Jurassic|Late Triassic|Subdivided into the Woogaroo and Marburg Subgroups.  Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|60993|5|Briefly described|p4, p6 Fig. 2|||Originally grouped with the Tabulam Group together with the Marburg Formation. The name now stands independently and is divided into the Marburg and Woogaroo Subgroups. Geol. Prov: Clarence-Moreton Basin. ||||||
2963|Bundamba Group|60995|4|Described|p52, p51 Fig. 3|Early Jurassic|Late Triassic|Now divided into the Woogaroo and Marburg Subgroups. Unconformably overlies Ipswich Coal. Mes. at Red Cliff and with Numboida Coal. Mes. at Nymboida; overlain by Walloon Coal. Mes. Geol. Prov: Clarence-Moreton Basin.||||||
2963|Bundamba Group|60996|5|Briefly described|p72, p129|Middle Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p133 Tb. 3.||||||
2963|Bundamba Group|60997|5|Briefly described|p139 Fig. 1|Callovian|Rhaetian|Comprises Marburg and Woogaroo Subgroups. See also p140 Fig. 2.||||||
2963|Bundamba Group|60999|5|Briefly described|p164|Early Jurassic|Late Triassic|Consists of the Woogaroo and Marburg Subgroups. Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61000|5|Briefly described|p181|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61002|5|Briefly described|p198 Fig 2|||Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61004|5|Briefly described|p232 Fig. 2|Jurassic|Triassic|Includes the lower Woogaroo and upper Marburg Subgroups. ||||||
2963|Bundamba Group|61310|4|Described|p20, p14 Fig. C5|Jurassic|Late Triassic|Mainly conglomerate and sandstone with mudstone, siltstone and minor coal, in a thick, non-marine, fluvial to lacustrine sequence. Overlies Nymboida Coal Measures and Chillingham Volcanics; overlain by Marburg Subgroup. Geol. Prov: Clarence-Moreton Basin.||||||27-AUG-08
2963|Bundamba Group|61775|6|Mentioned|p182 Fig. 1||Mesozoic|||||||
2963|Bundamba Group|63748|5|Briefly described|p21|||Comprises Marburg and Woogaroo Subgroups. Overlain by Walloon Coal Measures. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|63979|6|Mentioned|p31|||Geological province: Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|64289|5|Briefly described|p6 Fig. 2|Middle Jurassic|Late Triassic|Includes the Marburg and Woogaroo Subgroups. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|64665|5|Briefly described|p53 Fig.2, p57, p59.|Middle Jurassic|Late Triassic|Clarence-Moreton and Southern Nambour Basins.|||Includes Woogaroo and Marburg Subgroups.|Unconformably overlies Ipswich Coal Measures. Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|64769|5|Briefly described|p24|Early Jurassic|Late Triassic|Includes Helidon Sandstone. Geological Province: Ipswich Basin. QLD.||||||05-MAY-09
2963|Bundamba Group|64856|6|Mentioned|p80||Norian|Moreton Basin.| | ||||31-JAN-13
2963|Bundamba Group|65003|5|Briefly described|p7|||Of Clarence-Moreton Basin.||||Unconformably overlies the Ipswich Coal Measures. Overlain by Walloon Subgroup.|Mainly conglomerate and sandstone.|30-MAR-12
2963|Bundamba Group|67402|6|Mentioned|p187|||Clarence-Moreton Basin. |||Includes the Woogaroo Subgroup and the Marburg Subgroup|||
2963|Bundamba Group|67669|5|Briefly described|p11|Middle Jurassic|Early Jurassic|Of Bowen Basin.|||Includes Hutton Sandstone, Evergreen Fm and Precipice Sandstone.|Overlain by Injune Creek Group/Waloon Formation. Underlain by Mimosa Group.||
2963|Bundamba Group|68327|5|Briefly described|Map legend.|Jurassic|Triassic||||Includes Woogaroo Sub-Group and Marburg Formation.|||
2963|Bundamba Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Marburg and Woogaroo Subgroups, and Landsborough Sandstone, are all mapped under the symbol, RJb.|||Includes Marburg and Woogaroo Subgroups.|||
2963|Bundamba Group|68579|6|Mentioned|p221|||||||Overlain unconformably by Redbank Plains Formation.||26-APR-13
2963|Bundamba Group|68679|5|Briefly described|p395, p398||||||Woogaroo Subgroup.|Unconformably overlies Ipswich Coal Measures.||
2963|Bundamba Group|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Upper Triassic|Clarence-Moreton Basin. In excess of 1000m thick. Gas or oil mature in the Clarence-Moreton Basin, but with low total organic content. |||Includes the Woogaroo Subgroup and the Mauburg Subgroup.|Overlies the Ipswich Coal Measures. Overlain by the Walloon Coal Measures.||
2963|Bundamba Group|69594|5|Briefly described|p519, p544, p547|Early Jurassic|Rhaetian|Northern Clarence-Moreton Basin and southern Nambour Basin.|||Woogaroo, Marburg Subgroups.|Unconformably overlies Ipswich Coal Measures. Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|69639|6|Mentioned|p106, p224|Jurassic|Triassic|Clarence-Moreton Basin.|||Includes the Mill Creek Siltstone.|Overlies the Tallawudjah Leucomonzogranite.||
2963|Bundamba Group|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Triassic|Northern Clarence-Moreton Basin area.|||Includes Woogaroo and Marburg Subgroups.|||
2963|Bundamba Group|70821|5|Briefly described|p80|||Clarence-Moreton Basin.|||Woogaroo, Marburg Subgroups.|Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|71628|5|Briefly described|p17:68; p19:24|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||||Partly overlies Tallawudjah Leucosyenogranite. Unconformably overlies Cullens Creek Granodiorite.||
2963|Bundamba Group|71805|5|Briefly described|p76|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.|||Includes the Marburg Subgroup and the Woogaroo Subgroup.|||15-MAY-19
2963|Bundamba Group|72528|5|Briefly described|p90.|Jurassic|Jurassic||||Includes Koreela Conglomerate Member.|||
2963|Bundamba Group|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.|||Marburg Subgroup, Woogaroo Subgroup.|Is overlain by Walloon Coal Measures.||
2978|Bundarra Granodiorite|23052|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
2978|Bundarra Granodiorite|23161|4|Described|p47 table6|Early Cretaceous|Early Cretaceous|Ages: 121.8+/-6.3 Ma to 129.7+/-8.6Ma.||||||
2978|Bundarra Granodiorite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2978|Bundarra Granodiorite|31979|4|Described|p15|||Lower Cretaceous.||||||
2978|Bundarra Granodiorite|31983|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2978|Bundarra Granodiorite|34314|6|Mentioned|p12|||See P15||||||
2978|Bundarra Granodiorite|34389|4|Described|Table 2|||Cretaceous.||||||
2978|Bundarra Granodiorite|34480|6|Mentioned|p489|||See also P493||||||
2978|Bundarra Granodiorite|34573|6|Mentioned|p32|||Lower Cretaceous||||||
2978|Bundarra Granodiorite|35467|6|Mentioned|p187|||||||||
2978|Bundarra Granodiorite|37458|6|Mentioned|p440|||||||||
2978|Bundarra Granodiorite|39445|5|Briefly described|Table 12|||||||||
2978|Bundarra Granodiorite|41246|6|Mentioned|Map legend|Cretaceous||||||||
2978|Bundarra Granodiorite|42257|6|Mentioned|p261|||||||||
2978|Bundarra Granodiorite|42701|4|Described|p101|||||||||
2978|Bundarra Granodiorite|42932|6|Mentioned|Fig.17|||||||||
2978|Bundarra Granodiorite|43988|14|Not recorded|Map Legend||Early Cretaceous|||||||
2978|Bundarra Granodiorite|43994|14|Not recorded|Map Legend|||||||||
2978|Bundarra Granodiorite|43998|4|Described|p22|||Post-Permian?||||||
2978|Bundarra Granodiorite|44000|14|Not recorded|p37|||||||||
2978|Bundarra Granodiorite|44001|14|Not recorded|Map Legend||Mesozoic|||||||
2978|Bundarra Granodiorite|44002|14|Not recorded|Map Legend|||||||||
2978|Bundarra Granodiorite|44245|5|Briefly described|Map Legend||Cretaceous|||||||
2978|Bundarra Granodiorite|44331|14|Not recorded|Map Legend||Early Cretaceous|||||||
2978|Bundarra Granodiorite|44337|5|Briefly described|Map Legend||Cretaceous|Lithology.||||||
2978|Bundarra Granodiorite|44409|14|Not recorded|Map Legend||Mesozoic|||||||
2978|Bundarra Granodiorite|44635|4|Described|p8,13,14||Mesozoic|Formerly called Mount Flora granite.||||||
2978|Bundarra Granodiorite|45071|3|Fully described|Table 16|||||||||
2978|Bundarra Granodiorite|48841|2|Defined|p20,21,24,25,43,47,||Late Triassic|Outcrops near Middle Bowen Beds (Late Triassic or post-Triassic).p 49||||||
2978|Bundarra Granodiorite|48881|2|Defined|p5,8,24,33||Mesozoic|Hunter-Bowen orogen.||||||
2978|Bundarra Granodiorite|48898|6|Mentioned|p27|||L.Cret. See also P71||||||
2978|Bundarra Granodiorite|60445|5|Briefly described|p6. p18|||Intrudes the Back Creek Group.||||||
2978|Bundarra Granodiorite|60472|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Grey to pale pink, medium to coarse grained, even grained to porphyritic, leucocratic (titanite-hornblende-) biotite tonalite, quartz diorite and granodiorite.||||||
2978|Bundarra Granodiorite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
2978|Bundarra Granodiorite|65388|3|Fully described|p405-406, p403 Fig. 135|Early Cretaceous|Early Cretaceous|Defined by Jensen & others (1966). Intrudes Back Creek Group. Along with Gotthardt Granodiorite and the Mount Barker Granodiorite further west, all have produced metamorphic aureoles in surrounding sediments. Fission track zircon age range: 121.8+/-6.3Ma to 129.7+/-8.6Ma. Grey to locally pale pink, medium to coarse-grained, equigranular to porphyritic, leucocratic, titanite-bearing hornblende-biotite granodiorite to tonalite and quartz diorite.||||||
2978|Bundarra Granodiorite|69594|5|Briefly described|p566, p570, p571 Figs.7.45-46|Early Cretaceous|Early Cretaceous|South of the Urannah Batholith. Geochemistry plots and discussion.|~126 Ma (K-Ar biotite: Green and Webb, 1974).||||Locally foliated to gneissic.|
2978|Bundarra Granodiorite|70330|6|Mentioned|p11|||Bowen Basin.||||||
2978|Bundarra Granodiorite|73038|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Grey - locally pale pink, medium - coarse-grained, equigranular - porphyritic, leucocratic (titanite-hornblende-) biotite tonalite, quartz diorite + granodiorite; locally foliated + variably deformed + altered; minor aplite + microgranite dykes.|
2978|Bundarra Granodiorite|73040|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Grey to locally pale pink, medium to coarse-grained, equigranular to porphyritic, leucocratic (titanite-hornblende) biotite tonalite, quartz diorite and granodiorite; minor aplite and microgranite dykes.|
3008|Bungil Formation|730|6|Mentioned|p24.|||Paralic.||||||11-NOV-14
3008|Bungil Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p501|Aptian|Early Cretaceous|N Surat Basin. 100-300m thick.||||Equivalent to Drildool beds.|Labile sandstone, siltsone and mudstone with subordinate sub-labile quartzose sandstone and thin coal seams.|
3008|Bungil Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
3008|Bungil Formation|22757|5|Briefly described|Table6,p11||Early Cretaceous|120 m. Surat Basin.||||||
3008|Bungil Formation|22857|4|Described|p296-7 Tb.22.1, p546 App.1 Tb.A1.12|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Fine-grained lithic arenite, siltstone and mudstone. Contains three members in Qld. Max. thickness: <200m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
3008|Bungil Formation|22865|4|Described|p314,Table22.1p296-7|Barremian|Valanginian|||||||
3008|Bungil Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|of Surat Basin.||||||
3008|Bungil Formation|23053|6|Mentioned|Fig10p17,27|Aptian|Hauterivian|||||||
3008|Bungil Formation|23056|6|Mentioned|10|||Geol Province Eromanga Basin||||||
3008|Bungil Formation|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
3008|Bungil Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
3008|Bungil Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 180m.||||||
3008|Bungil Formation|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
3008|Bungil Formation|24085|5|Briefly described|p42 Tb.2|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
3008|Bungil Formation|24243|5|Briefly described|p23 Fig.3|Cretaceous|Cretaceous|||||||
3008|Bungil Formation|29387|6|Mentioned|Table 5|||||||||
3008|Bungil Formation|29393|6|Mentioned|Table 4|||||||||
3008|Bungil Formation|29591|6|Mentioned|Table 15|||||||||
3008|Bungil Formation|29721|6|Mentioned|p246|||||||||
3008|Bungil Formation|30020|6|Mentioned|p33|||||||||
3008|Bungil Formation|30021|6|Mentioned|p87|||||||||
3008|Bungil Formation|30022|6|Mentioned|p28|||||||||
3008|Bungil Formation|30024|6|Mentioned|p332|||||||||
3008|Bungil Formation|30446|6|Mentioned|p39|||||||||
3008|Bungil Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30695|4|Described|Table 4|||Lower Cretaceous age||||||
3008|Bungil Formation|30696|4|Described|Table 4|||Lower Cretaceous age||||||
3008|Bungil Formation|30697|6|Mentioned|p34|||Minor aquifer present||||||
3008|Bungil Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous age||||||
3008|Bungil Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||11-JAN-10
3008|Bungil Formation|30702|6|Mentioned|p52|||See also P48-51,Fig.1,2.||||||
3008|Bungil Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
3008|Bungil Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|31098|5|Briefly described|Table 1|||Lower Cretaceous||||||
3008|Bungil Formation|31116|4|Described|p41|||See also Table 2. Cretaceous||||||
3008|Bungil Formation|31208|6|Mentioned|Table 1|||See also Fig. 5||||||
3008|Bungil Formation|31369|6|Mentioned|Table 4|||Cretaceous||||||
3008|Bungil Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|32797|4|Described|Table 4|||L.Cret.||||||
3008|Bungil Formation|33070|4|Described|Table 2|||L.Cret.||||||
3008|Bungil Formation|33075|6|Mentioned|p451|||||||||
3008|Bungil Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33090|4|Described|Table 4|||L.Cret.||||||
3008|Bungil Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
3008|Bungil Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33367|6|Mentioned|p17|||||||||
3008|Bungil Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33672|6|Mentioned|p44|||||||||
3008|Bungil Formation|34613|4|Described|Table 4|||||||||
3008|Bungil Formation|35648|6|Mentioned|p18|||||||||
3008|Bungil Formation|35663|6|Mentioned|p130|||||||||
3008|Bungil Formation|35793|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
3008|Bungil Formation|35937|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|36243|6|Mentioned|Table 7A|||||||||
3008|Bungil Formation|36357|6|Mentioned|p77|||||||||
3008|Bungil Formation|36570|4|Described|p50|||See also Fig.9, p60.||||||23-SEP-18
3008|Bungil Formation|36574|6|Mentioned|p602|||||||||
3008|Bungil Formation|36827|6|Mentioned|p83|||||||||
3008|Bungil Formation|37117|5|Briefly described|p313|||||||||
3008|Bungil Formation|37597|6|Mentioned|p77|||||||||
3008|Bungil Formation|37856|6|Mentioned|Table 3|||||||||
3008|Bungil Formation|37994|6|Mentioned|p146|||||||||
3008|Bungil Formation|37995|4|Described|p66|||||||||
3008|Bungil Formation|38373|6|Mentioned|p621|||||||||
3008|Bungil Formation|39211|5|Briefly described|p31|||||||||
3008|Bungil Formation|39212|4|Described|p39|||Excursion site. See also p17.||||||23-SEP-18
3008|Bungil Formation|39215|6|Mentioned|p51|||Spore/pollen record||||||
3008|Bungil Formation|39216|6|Mentioned|p55|||Fauna||||||
3008|Bungil Formation|39218|6|Mentioned|p48|||||||||
3008|Bungil Formation|39315|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|39445|5|Briefly described|Table 10|||||||||
3008|Bungil Formation|39494|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|39943|6|Mentioned|Table 9A|||||||||
3008|Bungil Formation|40030|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|40245|6|Mentioned|Table 2|||||||||
3008|Bungil Formation|40249|6|Mentioned|p38|||||||||
3008|Bungil Formation|40250|6|Mentioned|Fig.1|||||||||
3008|Bungil Formation|40541|3|Fully described|p111|||||||||
3008|Bungil Formation|40544|6|Mentioned|Fig.6|||||||||
3008|Bungil Formation|40666|4|Described|p358|||||||||
3008|Bungil Formation|40675|6|Mentioned|Table 9A|||||||||
3008|Bungil Formation|40767|6|Mentioned|Fig.1|||||||||
3008|Bungil Formation|41057|6|Mentioned|p61|||||||||
3008|Bungil Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
3008|Bungil Formation|41064|6|Mentioned|p60|||||||||
3008|Bungil Formation|41187|6|Mentioned|Fig.2|||||||||
3008|Bungil Formation|41188|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|41210|5|Briefly described|Fig.3|||||||||
3008|Bungil Formation|41216|6|Mentioned|Fig.18,p299|||||||||
3008|Bungil Formation|41247|6|Mentioned|Fig.7|||||||||
3008|Bungil Formation|41266|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|41290|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|41330|6|Mentioned|p24|||||||||
3008|Bungil Formation|41681|6|Mentioned|p23|||||||||
3008|Bungil Formation|41992|4|Described|Fig.2 P183|||||||||
3008|Bungil Formation|42007|5|Briefly described|Fig.2 P182|||||||||
3008|Bungil Formation|42135|6|Mentioned|Fig.6 P357|||||||||
3008|Bungil Formation|42429|5|Briefly described|Fig.3 P155|||||||||
3008|Bungil Formation|42463|6|Mentioned|Fig.5 P172|||See also Fig.6 P173||||||
3008|Bungil Formation|42494|5|Briefly described|Table 1 P24|||Just says 'Bungil' on Table.||||||
3008|Bungil Formation|42634|6|Mentioned|Table 8 P34|||||||||
3008|Bungil Formation|42673|5|Briefly described|Fig.2, P184|||||||||
3008|Bungil Formation|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
3008|Bungil Formation|43002|5|Briefly described|Fig.2,p135|||||||||
3008|Bungil Formation|43564|6|Mentioned|p463|||||||||
3008|Bungil Formation|43582|6|Mentioned|Fig.5,p16||Early Cretaceous|||||||
3008|Bungil Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group||||||
3008|Bungil Formation|43714|5|Briefly described|p8||Early Cretaceous|||||||
3008|Bungil Formation|45103|6|Mentioned|p5|||||||||
3008|Bungil Formation|45110|3|Fully described|p110|||See also p9 and p24.||||||23-SEP-18
3008|Bungil Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
3008|Bungil Formation|46791|6|Mentioned|p34|||||||||
3008|Bungil Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
3008|Bungil Formation|46984|6|Mentioned|Table 1|||||||||
3008|Bungil Formation|48919|6|Mentioned|p70|||See also P71||||||
3008|Bungil Formation|48920|6|Mentioned|Table 7|||Refers to Exon & Vine (1970)||||||
3008|Bungil Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
3008|Bungil Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
3008|Bungil Formation|61312|6|Mentioned|p71|||Equivalent to the Cadna-owie Formation in the Eromanga Basin. Geological Province: Surat Basin.||||||
3008|Bungil Formation|61313|5|Briefly described|p98 Fig.G10|Cretaceous|Cretaceous|Paralic deposits. Geological Province: Surat Basin.||||||
3008|Bungil Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Labile sandstone, carbonaceous siltstone and mudstone. Overlies Pilliga Sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8, p154 Fig. SU9.||||||07-FEB-11
3008|Bungil Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
3008|Bungil Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Is overlain by Wallumbilla Formation.||
3008|Bungil Formation|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|||||Underlies Wallumbilla Formation; overlies Mooga Sandstone.||
3008|Bungil Formation|64665|6|Mentioned|p53 Fig.2.|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone.||
3008|Bungil Formation|64856|3|Fully described|p41, p79, p95, p97-100|Aptian|Valanginian|Exon and Vine (1970); corresponds to the Transition beds of Whitehouse (1955). Included in his Blythesdale Formation by Day (1964). Surat Basin. Datum for the top of the Jurassic. Contains Kingull, Minmi, Nullawurt Sandstone, Members (all of Day, 1964) and Claravale Sandstone Member (Mollan et al., 1972). Conformably overlies Mooga Sandstone, correlates with the Cadna-owie Formation in the Eromanga Basin. Is overlain by the Doncaster Member (Wallumbilla Formation). Age from palynoflora (units APK2, 3, uppermost APK1). Max. thickness 269m. Fine grained lithic sandstone, siltstone, mudstone.| | ||||28-NOV-17
3008|Bungil Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Mooga Sandstone, Surat Basin.||||||
3008|Bungil Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
3008|Bungil Formation|65112|6|Mentioned|p329; Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|135-101 Ma.|||Overlies the Mooga Sandstone, underlies the Doncaster Member of the Wallumbilla Formation.||22-MAR-12
3008|Bungil Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Underlies the Wallumbilla Formation and Doncaster Member, Overlies the Mooga Sandstone.||||||
3008|Bungil Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
3008|Bungil Formation|65116|5|Briefly described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies both the Wallumbilla Formation and Doncaster Member, Overlies the Mooga Formation in the Surat Basin.||||||
3008|Bungil Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 6-8, 14, 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Glauconitic to quartzose sandstone, siltstone and mudstone. Up to 270 m thick. Age: 135-116 Ma. Fission Track age: 108+/-6 Ma.||||||07-MAR-12
3008|Bungil Formation|65384|5|Briefly described|S116, S117, S118|||Probably Aptian. Includes Minmi Member. Of Surat Basin. Incorporates coastal plain and marine shelf depositional environments.||||||
3008|Bungil Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.|||Includes Kingull, Minmi, and Nullawurt Sandstone, Members.|Overlies Mooga Sandstone and Southlands Formation.||
3008|Bungil Formation|66623|6|Mentioned|p251.|||Packham et al. (2001). Surat Basin. Equivalent to the Cadna-owie Formation.||||||
3008|Bungil Formation|66915|5|Briefly described|p5, p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Surat Basin.||||Is overlain by Wallumbilla Formation.|Sandy.|12-JAN-17
3008|Bungil Formation|67133|5|Briefly described|p2, p5, p17, p19-21|Cretaceous|Cretaceous|Surat Basin. Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (38-46%) and feldspars (over 50%), with plagioclase always dominant. Kaolinite reaches 20%, and the mixed-layer clays are <4% and illite-rich. Deposited by a coastal fluvial system that graded into a shallow marine system.||||Overlies Mooga Sandstone.|Fine-grained lithic sandstones interbedded with siltstones and mudstones, with minor sublabile to quartzose sandstones.|
3008|Bungil Formation|67402|4|Described|p43 tbl HPB1, p146 fig SRT3, p148, p156|Barremian|Tithonian|Surat Basin. Highly prospective for the storage of carbon dioxide. Deposited in fluvial to shallow marine environments. Approximately 195m thick. ||Blythesdale Group||Overlies the Mooga Sandstone. Overlain by the Wallumbilla Formation.|Sandstone, siltstone and mudstone.|
3008|Bungil Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Wallumbilla Formation. Underlain by Mooga Silstone.||
3008|Bungil Formation|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation (Rolling Downs Group).||
3008|Bungil Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluviatile to paralic, grading to shallow marine in the upper part.||||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation.|Fine-grained lithic sandstone, siltstone and mudstone with subdominant coarse-grained quartzose sandstone; minor thin coal seams.|
3008|Bungil Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
3008|Bungil Formation|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone.||
3008|Bungil Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat and Eromanga Basins. This unit, as well as Orallo and Southlands Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
3008|Bungil Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone. Is overlain by Doncaster Member (Wallumbilla Formation).||
3008|Bungil Formation|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Early Cretaceous|A marine incursion occurred during deposition of this unit. A minor aquifer in the map area.||||Overlies Mooga Sandstone. Is overlain by Rolling Downs Group.|Fine-grained lithic sandstone, siltstone and mudstone with subordinate coarse-grained quartzose sandstone. Thin coal seams in places.|
3008|Bungil Formation|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|Surat Basin. Marine transgressive. Pre-Barremian age. Mis-spelt as Bungill Formation in Fig.2.||||||16-JAN-17
3008|Bungil Formation|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Surat Basin. Lower Cretaceous age. Equivalent to the Cadna-owie Formation.|||||Feldspar-rich sandstones.|
3008|Bungil Formation|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Mooga Sandstone. Overlain by the Wallumbilla Formation.||
3008|Bungil Formation|69594|4|Described|p519, p538, p573|Aptian|Valanginian|Exon and Vine (1970). Northern Surat Basin. Includes interbedded sandstones and mudstones along Bungil Creek N of Roma; these were assigned by Whitehouse (1955) to his Transition beds, and Day (1964) had placed them in his Blythesdale Formation. Up to 300m thick. Represents the initial marine transgression into the Surat Basin: fluviatile to paralic to shallow-marine sediments.|||Claravale Sandstone, Kingull, Nullawurt Sandstone, Minmi, Members.|Conformably overlies Mooga Sandstone. Is overlain conformably by the Doncaster Member (Wallumbilla Formation). Laterally equivalent to Cadna-owie Formation, and upper part of Kumbarilla beds.|Lithic sandstones, siltstones and common carbonaceous mudstones, with minor sublabile and quartzose sandstone. Upper parts of the Formation are glauconitic and sporadically fossiliferous.|
3008|Bungil Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
3008|Bungil Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
3008|Bungil Formation|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. The lower part of the Formation is included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal. The upper part is included in a mapped unit of a coastal plain sequence: lithic sandstone, siltstone, mudstone and coal.||||||
3008|Bungil Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.|||Kingull, Nullawurt Sandstone, Minmi, Members.|Overlies Mooga Sandstone, Southlands Formation. Is overlain by Wallumbilla Formation (Rolling Downs Group).||
3008|Bungil Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Valanginian-Barremian.||||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation.||
3008|Bungil Formation|71601|6|Mentioned|p120, p121, p123|Aptian|Aptian|South western Queensland. Includes basal ankylosaurian dinosaur Minmi paravertebra.|||Includes Minmi Member.|||
3008|Bungil Formation|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
3008|Bungil Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers, generally producing flowing artesian water bores.|||Kingull, Nullawurt Sandstone, Minmi Members.|Overlies Southlands FZ and Mooga Sandstone. Is overlain by Wallumbilla FZ (Rolling Downs Group).||
3008|Bungil Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88...|||Surat Basin. Partial aquifer. More locations: p. 116-117, 119, 146, 151-152, 160, 168-173, 177-178, 191.||||||
3008|Bungil Formation|73193|6|Mentioned|p369|Barremian|Hauterivian|Surat Basin.||||Underlain by Mooga Sandstone.||
3041|Bunya Mountains Lavas|36806|6|Mentioned|Table 4|||||||||
3045|Bunya Phyllite|22845|6|Mentioned|p36|Early Carboniferous|Late Devonian|||||||
3045|Bunya Phyllite|23799|6|Mentioned|p21|||||||||
3045|Bunya Phyllite|24418|6|Mentioned|p11|||Metasediments.||||||30-JUN-06
3045|Bunya Phyllite|29420|6|Mentioned|p98|||||||||
3045|Bunya Phyllite|29555|6|Mentioned|p12|||Precambrian||||||
3045|Bunya Phyllite|29720|6|Mentioned|p77|||||||||
3045|Bunya Phyllite|30776|6|Mentioned|p107|||Stratagraphic relations to Neranleigh-Fernvale beds unknown||||||29-SEP-05
3045|Bunya Phyllite|30797|5|Briefly described|Table 1|||Palaeozoic.||||||
3045|Bunya Phyllite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
3045|Bunya Phyllite|30915|6|Mentioned|p101|||||||||
3045|Bunya Phyllite|31131|5|Briefly described|p153|||Contact with Neranleigh-Fernvale Gp.||||||
3045|Bunya Phyllite|31133|4|Described|p159|||See also P160 ? Precambrian.||||||18-MAR-09
3045|Bunya Phyllite|31269|5|Briefly described|p137|||Palaeozoic ?||||||
3045|Bunya Phyllite|31271|5|Briefly described|p795|||||||||
3045|Bunya Phyllite|31370|6|Mentioned|p475|||||||||
3045|Bunya Phyllite|31823|6|Mentioned|p42|||||||||
3045|Bunya Phyllite|31999|6|Mentioned|p133|||||||||
3045|Bunya Phyllite|32610|4|Described|p42|||||||||
3045|Bunya Phyllite|33220|6|Mentioned|p5|||L.Pal.||||||
3045|Bunya Phyllite|33289|4|Described|p163|||See also PP164-166. L.Pal.||||||
3045|Bunya Phyllite|33381|6|Mentioned|p107|||Pre Permian||||||
3045|Bunya Phyllite|33769|6|Mentioned|p149|||||||||
3045|Bunya Phyllite|33881|5|Briefly described|p95|||||||||
3045|Bunya Phyllite|33902|6|Mentioned|Fig.|||?Sil.  On map.||||||
3045|Bunya Phyllite|34551|6|Mentioned|p229|||Equivalent Nambucca Phyllite||||||
3045|Bunya Phyllite|35007|5|Briefly described|p74|||||||||
3045|Bunya Phyllite|35053|5|Briefly described|p35|||||||||
3045|Bunya Phyllite|35101|3|Fully described|p12|||||||||
3045|Bunya Phyllite|35126|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
3045|Bunya Phyllite|35156|5|Briefly described|p4|||See also Table.2||||||
3045|Bunya Phyllite|35430|6|Mentioned|Table 1|||Interpretation of stratigraphic successions||||||
3045|Bunya Phyllite|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
3045|Bunya Phyllite|35866|6|Mentioned|p402|||||||||
3045|Bunya Phyllite|36237|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
3045|Bunya Phyllite|36238|6|Mentioned|Table 1|||||||||
3045|Bunya Phyllite|36440|6|Mentioned|Map legend|Late Carboniferous|Early Carboniferous|Early to Late Carboniferous||||||
3045|Bunya Phyllite|36497|6|Mentioned|p19|||||||||
3045|Bunya Phyllite|36528|6|Mentioned|p171|||||||||
3045|Bunya Phyllite|36547|6|Mentioned|Table 2|||||||||
3045|Bunya Phyllite|36779|5|Briefly described|p4|||||||||
3045|Bunya Phyllite|37252|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian-Carboniferous||||||
3045|Bunya Phyllite|37375|6|Mentioned|Fig.1|||||||||
3045|Bunya Phyllite|37376|6|Mentioned|Table 1|||||||||
3045|Bunya Phyllite|38067|5|Briefly described|p58|||||||||
3045|Bunya Phyllite|38074|5|Briefly described|Table 1|||||||||
3045|Bunya Phyllite|38079|6|Mentioned|p48|||||||||
3045|Bunya Phyllite|38391|6|Mentioned|p7|||||||||
3045|Bunya Phyllite|38441|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian - Early Carboniferous||||||
3045|Bunya Phyllite|38805|6|Mentioned|p79|||||||||
3045|Bunya Phyllite|39079|5|Briefly described|p6|||||||||
3045|Bunya Phyllite|39445|5|Briefly described|p79|||See also P84, Fig.7 & Table 6. Use of name. Unit in Neranleigh-Fernvale||||||
3045|Bunya Phyllite|40245|6|Mentioned|p182|||||||||
3045|Bunya Phyllite|40435|6|Mentioned|p47|||||||||
3045|Bunya Phyllite|40475|6|Mentioned|p3|||||||||
3045|Bunya Phyllite|40517|6|Mentioned|p369|||||||||
3045|Bunya Phyllite|40579|6|Mentioned|Map legend|Carboniferous|Devonian|Carboniferous to Devonian||||||
3045|Bunya Phyllite|40623|5|Briefly described|p6|||||||||
3045|Bunya Phyllite|41906|3|Fully described|TABLE 1 P11|||||||||
3045|Bunya Phyllite|41917|6|Mentioned|Fig.3 P528|||||||||
3045|Bunya Phyllite|42525|5|Briefly described|Map legend|Paleozoic|Paleozoic|Geological Province: D'Aguilar Block.||||||07-NOV-08
3045|Bunya Phyllite|42547|4|Described|p55|||||||||
3045|Bunya Phyllite|42619|6|Mentioned|p29|||||||||
3045|Bunya Phyllite|42970|5|Briefly described|Fig.2,p118|||||||||
3045|Bunya Phyllite|43006|6|Mentioned|Fig.1,p238|||||||||
3045|Bunya Phyllite|43076|5|Briefly described|p5|||||||||
3045|Bunya Phyllite|43385|14|Not recorded|p170||Ordovician|||||||
3045|Bunya Phyllite|44091|14|Not recorded|p13||Precambrian|||||||
3045|Bunya Phyllite|44128|14|Not recorded|Tb.1,p426,430|||||||||
3045|Bunya Phyllite|44211|14|Not recorded|p89|||||||||
3045|Bunya Phyllite|44431|2|Defined|p80-83,85-87,Fig.10|||Conformably overlies Rocksberg Greenstones. Undeformed fine grain pelitic metasediments.||||||
3045|Bunya Phyllite|44649|14|Not recorded|p133-135|||See also Lexicon.||||||
3045|Bunya Phyllite|44703|14|Not recorded|Map||Precambrian|||||||
3045|Bunya Phyllite|44708|14|Not recorded|p3,5,23,24,Sh.2-4,||Precambrian|Section.||||||
3045|Bunya Phyllite|44718|14|Not recorded|p100-1,104||Early Paleozoic|Parallel alternating bands of dark micaceous material with narrower bands of quartz mosaic with dispersed green chlorite. Foliation pronounced. Unfossiliferous.||||||07-NOV-08
3045|Bunya Phyllite|44783|14|Not recorded|p2,7-9,14,30,48,50|||Brisbane district.||||||
3045|Bunya Phyllite|44911|14|Not recorded|p2-5,11|||Part of Brisbane Metamorphics, Brown, fissile, mainly quartz and muscovite.||||||
3045|Bunya Phyllite|44912|14|Not recorded|E12-B-8,E12-B-7|||||||||
3045|Bunya Phyllite|45003|14|Not recorded|p349|||See also Lexicon||||||
3045|Bunya Phyllite|45087|5|Briefly described|p227|||Chem. analyses. See also P231, 233.||||||
3045|Bunya Phyllite|48917|6|Mentioned|p43|||Regional setting & structural map||||||
3045|Bunya Phyllite|48940|5|Briefly described|p7|||Refers Bryan & Jones (1950), Mathews (1954)||||||
3045|Bunya Phyllite|60077|5|Briefly described|Map legend|Paleozoic|Paleozoic|Phyllite, minor basic metavolcanics.||||||07-NOV-08
3045|Bunya Phyllite|63779|6|Mentioned|p1140|Carboniferous|Devonian|||||||
3045|Bunya Phyllite|68327|5|Briefly described|Map legend.|Paleozoic|Paleozoic||||||Phyllite, schist, minor lenses of greenstone.|
3045|Bunya Phyllite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Beenleigh and South D'Aguilar Subprovinces.||||||
3045|Bunya Phyllite|68576|5|Briefly described|QLD_D1: p8|||Quarried at Mount Coot-tha; used in retaining walls in King Edward Park and beside the Jacob's Ladder stairway.|||||Hornfelsed metasediments.|
3045|Bunya Phyllite|68679|5|Briefly described|p321-322, p330, p333, p409,p427,p470-471|Carboniferous|Carboniferous|Bryan and Jones (1950). South D'Aguilar Subprovince, northern New England Orogen. Detachment zone and lower plate accretionary assemblages. ~10km wide NNW-trending zone. Some rocks not continuous with this unit, which had been mapped by Murphy et al. (1976), were assigned to the Booloumba beds by Murray et al. (1979) but later re-assigned to the Jimna Phyllite (Sliwa, 1994). Deformation described in detail. No fossils or isotopic ages; is intruded by Triassic granitoids.||||Is intruded by Enoggera Granite, Samford and Mount Samson Granodiorites. Adjoins (at leat partly faulted against) the Neranleigh-Fernvale beds. Correlative of Anderson Creek and Jimna Phyllites.|A monotonous package of poly-deformed, thinly laminated chert and phyllite; ubiquitous quartz and quartz-chlorite veins, thin sedimentary chert laminations and differentiated siliceous laminations are characteristic. Lower greenschist facies.|
3045|Bunya Phyllite|69594|6|Mentioned|p546|Paleozoic|Paleozoic|Is overlapped by the Nambour Basin succession.||||||
3045|Bunya Phyllite|69952|5|Briefly described|p38|Carboniferous|Devonian|||||Is intruded by Enoggera Granite and Samford and Mount Samson Granodiorites.||23-NOV-15
3074|Burketown Formation|34356|6|Mentioned|p13|||||||||
3082|Burnett Formation|24076|5|Briefly described|p397 Fig. 2|Early Permian|Early Permian|Max. thickness: 1650m.  Geological Province: Yarrol Basin.||||||
3082|Burnett Formation|24491|5|Briefly described|p14|||Superseded?||||||
3082|Burnett Formation|29436|6|Mentioned|p317||Permian|||||||
3082|Burnett Formation|29728|6|Mentioned|p394|||||||||
3082|Burnett Formation|30450|6|Mentioned|Table 1|||Permian age||||||
3082|Burnett Formation|30451|4|Described|p36|||Early Permian age||||||
3082|Burnett Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
3082|Burnett Formation|31659|6|Mentioned|Table 2|||Correlation||||||
3082|Burnett Formation|32094|6|Mentioned|p383|||||||||
3082|Burnett Formation|32141|6|Mentioned|p153|||||||||
3082|Burnett Formation|32868|6|Mentioned|p202|||||||||
3082|Burnett Formation|32943|6|Mentioned|p87|||See also PP99,106. Fauna||||||
3082|Burnett Formation|32944|6|Mentioned|p699|||See also P709||||||
3082|Burnett Formation|32945|6|Mentioned|p87|||See also Fig.1||||||
3082|Burnett Formation|33711|6|Mentioned|Table 3|||||||||
3082|Burnett Formation|33774|6|Mentioned|p23|||L.Perm. Strat.||||||
3082|Burnett Formation|34085|6|Mentioned|Cor.chart|||Sakmarian||||||
3082|Burnett Formation|34132|6|Mentioned|p1|||Lower Permian. See also P4.||||||
3082|Burnett Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
3082|Burnett Formation|36045|6|Mentioned|p329|||||||||
3082|Burnett Formation|36333|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3082|Burnett Formation|36528|6|Mentioned|p174|||||||||
3082|Burnett Formation|36794|6|Mentioned|p386|||||||||
3082|Burnett Formation|37400|6|Mentioned|Table 2|||||||||
3082|Burnett Formation|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3082|Burnett Formation|39223|6|Mentioned|p238|||||||||
3082|Burnett Formation|39252|6|Mentioned|p13|||||||||
3082|Burnett Formation|39262|6|Mentioned|p134|||||||||
3082|Burnett Formation|39445|5|Briefly described|Table 7|||See also Table 8||||||
3082|Burnett Formation|39632|6|Mentioned|p221|||||||||
3082|Burnett Formation|41315|6|Mentioned|p150|||||||||
3082|Burnett Formation|42547|4|Described|p53|||||||||
3082|Burnett Formation|43008|5|Briefly described|map legend|||||||||
3082|Burnett Formation|43017|5|Briefly described|Fig.3,p375|||||||||
3082|Burnett Formation|43475|14|Not recorded|p552||Permian|Fauna||||||
3082|Burnett Formation|43882|14|Not recorded|p90||Sakmarian|Ammonites near Exmoor. Probably Sakmarian.||||||
3082|Burnett Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
3082|Burnett Formation|43983|14|Not recorded|p2,Fig.1|||||||||
3082|Burnett Formation|43998|4|Described|p19,map||Early Permian|||||||
3082|Burnett Formation|44091|14|Not recorded|p44,Tb.3,p47||Early Permian|||||||
3082|Burnett Formation|44360|14|Not recorded|p16,18||Early Permian|Overlies Rands Formation in Yarrol region.||||||
3082|Burnett Formation|44369|2|Defined|p169,171,LTb.6||Sakmarian|Greywacke, arkose.||||||
3082|Burnett Formation|44370|14|Not recorded|p217,219,Tb.7||Sakmarian|||||||
3082|Burnett Formation|44372|6|Mentioned|p5-7||Early Permian|Overlies Rands Formation. Underlies Yarrol Formation.||||||
3082|Burnett Formation|44378|14|Not recorded|p199|||Underlies Yarrol Formation.||||||
3082|Burnett Formation|44379|14|Not recorded|p16,18,25|||Equivalent in part to Youlambie Conglomerate.||||||
3082|Burnett Formation|44515|2|Defined|p30||Sakmarian|||||||
3082|Burnett Formation|45097|5|Briefly described|p23|||? Correlation with Youlambie Congl. See also correlation chart.||||||
3082|Burnett Formation|46803|6|Mentioned|p142|||Refers Maxwell (1974)||||||
3082|Burnett Formation|50190|6|Mentioned|p69|||||||||
3082|Burnett Formation|68008|5|Briefly described|p120, p123, p131, p481, p569|Permian|Permian|Maxwell (1959, 1960, 1964); Dear et al. (1971). Yarrol area. Combined with Rands Formation by Brown (1970) and Edwards (1974) but without a new stratigraphic name. Subsequently subsumed into the (upper part of the) Lorray Formation. Fossil species listed.||||||
3082|Burnett Formation|68679|6|Mentioned|p341|||Maxwell (1959) and other references. Yarrol area. Superseded; assigned to Lorray Formation.||||||
3148|Burrum Coal Measures|9194|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Greywacke, sandstone, mudstone, shale, coal: minor conglomerate and glauconitic sandstone.  Overlie Maryborough Formation; overlain by Elliot Formation.||||||23-DEC-09
3148|Burrum Coal Measures|23251|6|Mentioned|p24||Cretaceous|Nambour Basin or Maryborough Basin.||||||
3148|Burrum Coal Measures|23841|4|Described|p440 Fig. 2|Cretaceous|Cretaceous|Geological Province: Maryborough Basin.  Maximum thickness: 3000m.||||||
3148|Burrum Coal Measures|24382|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||||||
3148|Burrum Coal Measures|29651|3|Fully described|p9|||Mention Fig.1 & Table 1.||||||14-AUG-08
3148|Burrum Coal Measures|30654|4|Described|p51|||Lower Cretaceous age. Conformable on Maryborough Formation.||||||
3148|Burrum Coal Measures|30655|3|Fully described|p25|||See also Table 1||||||
3148|Burrum Coal Measures|30771|6|Mentioned|p3|||||||||
3148|Burrum Coal Measures|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3148|Burrum Coal Measures|31086|6|Mentioned|p37|||Lower Cretaceous. Fossil flora.||||||
3148|Burrum Coal Measures|32774|5|Briefly described|Table 2||Early Cretaceous|||||||
3148|Burrum Coal Measures|33165|6|Mentioned|Chart|||Correlation chart only||||||
3148|Burrum Coal Measures|33939|6|Mentioned|p393|||L.Cret.  Flora.||||||
3148|Burrum Coal Measures|34287|6|Mentioned|p183|||||||||
3148|Burrum Coal Measures|35053|5|Briefly described|p37|||||||||
3148|Burrum Coal Measures|35134|6|Mentioned|p579|||||||||
3148|Burrum Coal Measures|35688|6|Mentioned|Fig.2|||||||||
3148|Burrum Coal Measures|35813|6|Mentioned|p575|||||||||
3148|Burrum Coal Measures|35900|6|Mentioned|p449|||||||||
3148|Burrum Coal Measures|35937|6|Mentioned|p622|||||||||
3148|Burrum Coal Measures|36101|6|Mentioned|p171|||||||||
3148|Burrum Coal Measures|36327|6|Mentioned|p7|||||||||
3148|Burrum Coal Measures|36575|6|Mentioned|Fig.1|||||||||
3148|Burrum Coal Measures|36581|6|Mentioned|p462|||||||||
3148|Burrum Coal Measures|36772|6|Mentioned|p131|||See also P133, 134, 135||||||
3148|Burrum Coal Measures|36926|6|Mentioned|p165|||||||||
3148|Burrum Coal Measures|36961|6|Mentioned|Table 1|||||||||
3148|Burrum Coal Measures|37065|5|Briefly described|p41|||||||||
3148|Burrum Coal Measures|37114|6|Mentioned|p308|||||||||
3148|Burrum Coal Measures|37118|6|Mentioned|Fig.1|||||||||
3148|Burrum Coal Measures|37120|4|Described|p321|||||||||
3148|Burrum Coal Measures|37618|6|Mentioned|p15|||||||||
3148|Burrum Coal Measures|38308|6|Mentioned|p234|||||||||
3148|Burrum Coal Measures|38391|6|Mentioned|p11|||||||||
3148|Burrum Coal Measures|38397|4|Described|Table 2|||||||||
3148|Burrum Coal Measures|38402|6|Mentioned|p72|||||||||
3148|Burrum Coal Measures|39211|5|Briefly described|p41|||Albian. See Fig. 25||||||
3148|Burrum Coal Measures|39315|6|Mentioned|Fig.5|||||||||
3148|Burrum Coal Measures|39445|5|Briefly described|Table 11|||||||||
3148|Burrum Coal Measures|39505|6|Mentioned|p175|||||||||
3148|Burrum Coal Measures|39968|6|Mentioned|p76|||||||||
3148|Burrum Coal Measures|40245|6|Mentioned|Table 1|||||||||
3148|Burrum Coal Measures|40623|5|Briefly described|p54|||||||||
3148|Burrum Coal Measures|41057|6|Mentioned|p61|||||||||
3148|Burrum Coal Measures|41265|6|Mentioned|Map legend|Cretaceous||||||||
3148|Burrum Coal Measures|41736|6|Mentioned|Fig.1|||||||||
3148|Burrum Coal Measures|42187|5|Briefly described|p321|||||||||
3148|Burrum Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
3148|Burrum Coal Measures|42616|4|Described|p7|||||||||
3148|Burrum Coal Measures|42617|5|Briefly described|p16|||||||||
3148|Burrum Coal Measures|42648|5|Briefly described|Fig.7 P43|||||||||
3148|Burrum Coal Measures|42894|2|Defined|p33||middle Cretaceous|||||||
3148|Burrum Coal Measures|42895|6|Mentioned|p54|||||||||
3148|Burrum Coal Measures|43008|5|Briefly described|map legend|||||||||
3148|Burrum Coal Measures|43059|4|Described|Table 1|||see also p10.||||||14-AUG-08
3148|Burrum Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
3148|Burrum Coal Measures|43906|14|Not recorded|p330-331|||||||||
3148|Burrum Coal Measures|43984|14|Not recorded|p130|||||||||
3148|Burrum Coal Measures|43995|14|Not recorded|p8,Tb.p10,36||Late Cretaceous|||||||
3148|Burrum Coal Measures|44068|14|Not recorded|p15|||||||||
3148|Burrum Coal Measures|44078|14|Not recorded|p309|||||||||
3148|Burrum Coal Measures|44082|6|Mentioned|p22,34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
3148|Burrum Coal Measures|44117|14|Not recorded|p23|||||||||
3148|Burrum Coal Measures|44128|14|Not recorded|Tb.1,p426|||||||||
3148|Burrum Coal Measures|44167|14|Not recorded|map p22|||||||||
3148|Burrum Coal Measures|44239|14|Not recorded|p278|||||||||
3148|Burrum Coal Measures|44240|14|Not recorded|p333-339,340|||Conformable on Maryborough Formation. sandstone, shale, coal seams.||||||
3148|Burrum Coal Measures|44241|2|Defined|p1,3,8-10,12-4,30||Early Cretaceous|Fig.1, Tb.4. Conformable on Maryborough Formation. Divided into Lower and Upper Unproductive Measures and Middle Productive Measures.||||||
3148|Burrum Coal Measures|44360|14|Not recorded|p36|||(Early or early Late Cretaceous)||||||
3148|Burrum Coal Measures|44377|14|Not recorded|p15|||See also Lexicon.||||||
3148|Burrum Coal Measures|44380|14|Not recorded|p94|||||||||
3148|Burrum Coal Measures|44385|14|Not recorded|p6|||||||||
3148|Burrum Coal Measures|44591|14|Not recorded|unknown (1-17)|||Not listed on white card.||||||
3148|Burrum Coal Measures|44616|14|Not recorded|p32,33,35|Late Cretaceous|Aptian|Fine medium sandstone, greywacke, siltstone, coal seams, glauconitic sandstone. Low porosity.||||||
3148|Burrum Coal Measures|44638|14|Not recorded|p290|||||||||
3148|Burrum Coal Measures|44716|14|Not recorded|p75,105|||||||||
3148|Burrum Coal Measures|44738|14|Not recorded|p2|||||||||
3148|Burrum Coal Measures|44750|14|Not recorded|p12,17||Cretaceous|||||||
3148|Burrum Coal Measures|44752|14|Not recorded|p298,Fig.42||Cretaceous|||||||
3148|Burrum Coal Measures|44753|14|Not recorded|p47,49,52-54||Cretaceous|Succeeded by Maryborough Formation.||||||
3148|Burrum Coal Measures|44754|14|Not recorded|p6,13||Late Cretaceous|||||||
3148|Burrum Coal Measures|44783|14|Not recorded|p2|||||||||
3148|Burrum Coal Measures|44821|14|Not recorded|p33,35||Early Cretaceous|||||||
3148|Burrum Coal Measures|44828|14|Not recorded|p14|||Sandstone suitable for grinding.||||||
3148|Burrum Coal Measures|44852|14|Not recorded|p78||Early Cretaceous|||||||
3148|Burrum Coal Measures|44913|6|Mentioned|p57, Fig.3|||||||||14-APR-20
3148|Burrum Coal Measures|45107|6|Mentioned|p6|||||||||
3148|Burrum Coal Measures|45440|4|Described|p.2,7,14,35,38,39-87|||Tb.1. Of many pages. Aptian?||||||
3148|Burrum Coal Measures|60281|4|Described|p36, p37-38|Albian|Albian|Subdivided into 3 informal members - lower and upper "unproductive" members sandstones and siltstones and a middle "productive" member mainly of shale with thin coal seams. Conformably overlie Maryborough Fm. Max.thickness: 3km. See also Fig.30 App 1.||||||27-APR-05
3148|Burrum Coal Measures|61611|5|Briefly described|p264, p266, p265 Fig. 3|Early Cretaceous|Early Cretaceous|Fluviodeltaic/lacustrine sediments. Geological Province: Maryborough Basin.||||||13-MAR-09
3148|Burrum Coal Measures|62594|5|Briefly described|p546 Fig. 3|Early Cretaceous|Late Jurassic|Geological Province: Maryborough Basin.||||||14-AUG-08
3148|Burrum Coal Measures|63821|4|Described|p23, p24|||Overlies Maryborough Fm. Deltaic seds.with lower+upper sections of mainly intercalated sandstones and siltstones + minor shale, intraformational conglom.+ non-economic coal seams; mid section of shale + thin coal seams, minor siltstone+ rare sandstone.||||||07-FEB-11
3148|Burrum Coal Measures|64665|5|Briefly described|p53 Fig.2, p58.|Early Cretaceous|Early Cretaceous|Maryborough Basin. Low ash (4.4 to 12.5%); high volatile bituminous rank; good coking properties.||||Overlies Maryborough Formation.||
3148|Burrum Coal Measures|64714|4|Described|p2, p3-4 Fig. 1, p6-7|Early Cretaceous|Early Cretaceous|Overlie the Maryborough Formation. Unconformably overlain by Elliott Formation and Fairymead beds. Max. thickness: 3000m. Geological province: Maryborough Basin.||||||
3148|Burrum Coal Measures|67365|5|Briefly described|p88.|Early Cretaceous|Early Cretaceous|Maryborough Basin. High volatile coals.||||||
3148|Burrum Coal Measures|67402|4|Described|p165 tbl LPB1, p234, p235, p237|Early Cenomanian|Albian|Maryborough Basin. Deposited in a deltaic environment. Coal displays good coking qualities. Greater than 800m thick. ||||Overlies the Maryboroguh Formation.|Fine-medium grained sandstone, siltstone, shale, mudstone and coal.|
3148|Burrum Coal Measures|68008|6|Mentioned|p264|||Maryborough Basin.||||Age-equivalent to Stanwell Formation.||
3148|Burrum Coal Measures|68332|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Maryborough Basin.|||||Feldspatholithic labile sandstone, siltstone, mudstone, shale, coal, conglomerate, glauconitic sandstone.|
3148|Burrum Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Maryborough Basin.||||Conformably overlies Maryborough Formation.||
3148|Burrum Coal Measures|68679|5|Briefly described|p312-313, p472|Cretaceous|Cretaceous|Maryborough Basin, northern New England Orogen. Late Albian. Deformed in the early Palaeogene or Late Cretaceous.||||||
3148|Burrum Coal Measures|68811|5|Briefly described|p51|Cretaceous|Cretaceous|||||Unconformably overlain by the Fairymead Beds and the Elliott Formation.|Coal, greywacke, sandstone, mudstone, shale and minor conglomerate.|14-APR-20
3148|Burrum Coal Measures|69582|5|Briefly described|p48, p50-p53|Early Cretaceous|Early Cretaceous|Maryborough Basin. Fluvial-deltaic rocks. Thermal conductivity is provided. Intersected in GSQ Maryborough 16. Estimated to be around 600m thick.||||Unconformably overlies the Grahams Creek Formation. Overlies the Maryborough Formation.|Coal measures, sandstone and siltstone and minor shale.|
3148|Burrum Coal Measures|69594|5|Briefly described|p519, p548-550|Albian|Aptian|Hawthorne (1960); Cranfield (1993). Maryborough Basin. Fluviatile-lacustrine succession. Up to 3050m thick (in Pine Creek area). Sedimentary structures listed. Delta plain sediments. Steaming coal mining took place from 1866 to 1997; coking coal and CSG are being assessed/explored.||||Conformably overlies Maryborough Formation. Correlated with Styx Coal Measures.|Lower and upper parts: intercalated sandstone and siltstone with minor shale; sandstones highly variable with plagioclase 5-90% and quartz 5-40%. Middle part of the unit mainly shale with thin coal seams, minor siltstone and rare sandstone.|
3148|Burrum Coal Measures|69599|6|Mentioned|p587|||||||Is overlain unconformably by the Pemberton Grange Basalt, Fairymead beds, Elliott Formation and Takura beds.||
3148|Burrum Coal Measures|72297|5|Briefly described|p700, p751|Cretaceous|Cretaceous|Maryborough Basin. Has received little attention for its CSG potential.|||||Contains numerous, relatively thin coal seams.|
3148|Burrum Coal Measures|72298|5|Briefly described|p796|Mesozoic|Mesozoic|||||Is overlain by Elliott Formation and Fairymead beds.||
3148|Burrum Coal Measures|73570|6|Mentioned|p914, p915 Fig.4, p916, p917 Fig.5, p921|Early Cretaceous|Early Cretaceous|Maryborough Basin.|||||Sandstones.|
3190|Bury Limestone|22464|6|Mentioned|p9|Middle Devonian|Middle Devonian|Also p8. Adavale Basin.||||||
3190|Bury Limestone|22518|6|Mentioned|p 10|||||||||
3190|Bury Limestone|22604|6|Mentioned|p442|||of Log Creek Formation?, Emsian in age?||||||
3190|Bury Limestone|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|||||||
3190|Bury Limestone|29393|6|Mentioned|Table 1|||Middle Devonian.||||||
3190|Bury Limestone|35279|6|Mentioned|Fig.6|||||||||
3190|Bury Limestone|39478|6|Mentioned|Table 1|||||||||
3190|Bury Limestone|39480|6|Mentioned|p188|||||||||
3190|Bury Limestone|40322|6|Mentioned|Fig.3|||||||||
3190|Bury Limestone|41167|6|Mentioned|p397|||||||||
3190|Bury Limestone|41198|6|Mentioned|p35|||See also Table 1||||||
3190|Bury Limestone|41208|6|Mentioned|Fig.1|||||||||
3190|Bury Limestone|41289|6|Mentioned|p209|||||||||
3190|Bury Limestone|42031|5|Briefly described|Fig.3 P759|||||||||
3190|Bury Limestone|42999|5|Briefly described|Table1,p90|||||||||
3190|Bury Limestone|43004|5|Briefly described|Table 1,p179|||||||||
3190|Bury Limestone|43461|14|Not recorded|p618 table||Couvinian|in Adavale Basin||||||
3190|Bury Limestone|46881|6|Mentioned|Table 2|||||||||
3190|Bury Limestone|62985|5|Briefly described|p16|Givetian|Eifelian|Resulted from the marine transgression at the end of the Log Creek Formation being laid down. The lower part of this unit is laterally equivalent to upper Log Creek Formation. Unconformably overlain by Etonvale Formation. Geol. prov: Adavale Basin.||||||07-FEB-08
3190|Bury Limestone|64783|3|Fully described|p95-98, 82, 84, 86, 87, 93, 99, 100|Givetian|Eifelian|Before 1966, it was called the D3 Etonvale member. In 1966 Patterson referred to it as the Bury Limestone Member. In 1970, Galloway delimited the type section in PPC Bury-1 (2359-2647 m). In 1977, Paten gave it Formation status. Before 1977 was considered part of the Log Creek Formation. Age is late Eifelian to early-middle Givetian. Richly fossiliferous, largely undescribed.||||Conformably overlies Log Creek Formation. Lower part is laterally equivalent to the upper Log Creek Formation. Partly underlies the Cooladdi Dolomite.|Includes packstone, wackestone, calcareous siltstone and mudstone, and minor siliciclastic rocks.|15-NOV-17
3190|Bury Limestone|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3190|Bury Limestone|67402|5|Briefly described|p167 fig ADV/WRR3, p168, p170|Givetian|Eifelian|Adavale Basin. Deposited in an offshore marine environment. ||||Overlies the Log Creek Formation. Grades laterally into the Lissoy Sandstone and Cooladdi Dolomite.|Packstone, wackestone, fossiliferous limestone, calcareous silstone and mudstone/shale with minor siliciclastics.|
3190|Bury Limestone|68731|5|Briefly described|p177 Fig 3.91, p180 Tb 3.3|Late Devonian|Middle Devonian|Adavale Basin. Contains two distinct facies: limestone facies and limestone/shale facies. Corals (Alveolites, Thamnopora) stromatoporoids, scolecodonts, gastropods and the mollusc Tentaculites also occurs in this unit. < 300 m to 739.4 m thick.||||Underlain by the Boree Salt. Merges laterally with the Lissoy Sandstone and the top section of the Log Creek Formation.|Comprises packstone, wackestone, fossiliferous limestone, calcareous siltstone and mudstone, and limestone/shale facies.|
3190|Bury Limestone|73179|6|Mentioned|p1135 Fig.2, 1136|Givetian|Eifelian|Adavale Basin. Related to marine transgression in the southern and eastern parts of the basin.||||||26-SEP-22
3198|Bustlem Microgranite|23423|5|Briefly described|p315 Table 7.4||Early Permian|Age: 280 +/- 4 Ma (Rb-Sr). Lags Supersuite||||||
3198|Bustlem Microgranite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 432. A-Type.||||||
3198|Bustlem Microgranite|23616|5|Briefly described|p80||Permian|Age: 280+/-4 Ma (Rb-Sr).||||||
3198|Bustlem Microgranite|23713|5|Briefly described|p71 Appendix 2, p29||Early Permian|Intrudes Early Permian units of the Featherbed Volcanic Group. Age: 280+/-4 Ma (Rb-Sr). Of Lags Supersuite.||||||
3198|Bustlem Microgranite|42681|4|Described|p21|||Reserved as Bustlem Granite.||||||
3198|Bustlem Microgranite|43060|5|Briefly described|p113|||Age of 280+/-4 Ma.||||||
3198|Bustlem Microgranite|43083|5|Briefly described|p259|||Age of 280+/-4 Ma.Of Lags Supersuite. A-type.  Lithology included.||||||17-JUN-09
3198|Bustlem Microgranite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Medium pale grey to pink-grey, strongly porphyritic, augite?-fayalite-hypersthene (micro)granite. Age: 280+/-4Ma.||||||15-JUN-06
3198|Bustlem Microgranite|43254|5|Briefly described|map legend||Early Permian|of Lags Supersuite. Age 280+/-4 Ma.||||||
3198|Bustlem Microgranite|43259|4|Described|Appendix 1,p47.||Early Permian|Age is 280+/-4 Ma.||||||
3198|Bustlem Microgranite|43625|6|Mentioned|p21|||||||||
3198|Bustlem Microgranite|43626|6|Mentioned|p58|||||||||
3198|Bustlem Microgranite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 280 +/- 4 Ma (Rb-Sr). Geological Province: Kennedy Province. Medium to pale grey or pinkish grey, highly porphyritic augite?-fayalite-hypersthene microgranite.||||||31-MAY-04
3198|Bustlem Microgranite|60425|4|Described|p45 Tb. 3, p58 Tb. 4|Early Permian|Early Permian|Of Lags Supersuite. Age: 280+/-4Ma (Rb-Sr). Intrudes Wakara Volcanic Subgroup. A-type. Medium to pale grey, or pinkish grey, highly porphyritic augite?-fayalite-hypersthene microgranite.||||||07-FEB-11
3198|Bustlem Microgranite|62523|5|Briefly described|Map legend at p3-4|Early Permian|Early Permian|Medium-pale grey to pink-grey, strongly porphyritic augite?-fayalite-hypersthene (micro)granite. Age: 280+/-4Ma.||||||07-FEB-11
3198|Bustlem Microgranite|69593|5|Briefly described|p484, p510|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 Ma.|Lags Supersuite.|||A-type.|
3258|Cabbage Tree Creek beds|42895|6|Mentioned|p52|||||||||
3258|Cabbage Tree Creek beds|68421|5|Briefly described|Map Legend|Paleocene|Late Cretaceous||||||Coarse-grained sandstone containing shale fragments, pebble conglomerate, white to khaki mudstone, siltstone, shale and interbedded basalt.|
3265|Cadarga Creek Granodiorite|23037|4|Described|p99,100,108,133,135|Triassic|Late Permian|||||||
3265|Cadarga Creek Granodiorite|36333|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic.  Part of the Rawbelle batholith.||||||15-JUL-04
3265|Cadarga Creek Granodiorite|39445|5|Briefly described|Table 12|||||||||
3265|Cadarga Creek Granodiorite|41246|6|Mentioned|Map legend|Triassic|Permian|||||||
3265|Cadarga Creek Granodiorite|43008|5|Briefly described|map legend|||||||||
3265|Cadarga Creek Granodiorite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium grained biotite-hornblende granodiorite to monzogranite.||||||
3265|Cadarga Creek Granodiorite|64398|5|Briefly described|Map legend|Late Permian|Late Permian|Greenish-pink, medium-grained biotite-hornblende granodiorite to monzogranite.||||||
3265|Cadarga Creek Granodiorite|65388|3|Fully described|p302, p301 Fig 98, p306, 312|Early Triassic|Late Permian|Of Tandora Suite. In contact with the Delubra Gabbro along  western margin. Some net-veining suggests coeval emplacement. K-Ar ages (recalculated) of 242+/-2Ma (on biotite) and 258+/-8Ma (on hornblende) (Whitaker & others, 1974; Green, 1975). Aeromagnetic similarities suggest these units plus Hawkwood Gabbro may form a related complex. Greenish-pink medium-grained biotite-hornblende granodiorite, possibly grading into quartz monzodiorite. Also abbreviated as Cadarga Granodiorite on p312.||||||
3265|Cadarga Creek Granodiorite|68008|6|Mentioned|p435|||Rawbelle Batholith. May have undergone magma mingling with the adjacent Delubra Gabbro.||||||
3265|Cadarga Creek Granodiorite|68679|5|Briefly described|p416, p418, p420|||Southern part of the Rawbelle Batholith. Outcrop area ~90 km2. May form a complex with the Delubra and Hawkwood Gabbros. Geochemistry plot.|258 +/- 8 Ma (K-Ar hornblende).|Tandora Suite.|||A zoned pluton with a wide outer granodiorite zone surrounding inner granite and leucocratic granite core. Also described as dominantly biotite-hornblende granodiorite to monzogranite. Net-veining.|
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||
3318|Calen Coal Measures|23042|5|Briefly described|p52,3,105, Fig 2||Permian|Intruded by the Mount Jukes Igneous Complex. Underlying unit Carmila beds (un).||||||
3318|Calen Coal Measures|30508|6|Mentioned|p85|||Equivalent to Blenheim or Gebbie Sub-group.||||||
3318|Calen Coal Measures|30914|6|Mentioned|Map legend|Permian|Permian|||||||
3318|Calen Coal Measures|30915|6|Mentioned|p98|||||||||
3318|Calen Coal Measures|31688|6|Mentioned|p406|||Refers to drilling||||||
3318|Calen Coal Measures|32553|4|Described|p42|||||||||
3318|Calen Coal Measures|32554|6|Mentioned|Table 1|||||||||
3318|Calen Coal Measures|32555|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3318|Calen Coal Measures|32577|6|Mentioned|p23|||||||||
3318|Calen Coal Measures|35053|5|Briefly described|p38|||||||||
3318|Calen Coal Measures|35266|6|Mentioned|p202|||||||||
3318|Calen Coal Measures|35451|6|Mentioned|p209|||Source of materials for brick manufacture.||||||
3318|Calen Coal Measures|35467|6|Mentioned|p183|||||||||
3318|Calen Coal Measures|36045|6|Mentioned|p333|||||||||
3318|Calen Coal Measures|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3318|Calen Coal Measures|36906|6|Mentioned|p25|||||||||
3318|Calen Coal Measures|36938|5|Briefly described|p225|||See also Fig.1.||||||
3318|Calen Coal Measures|37070|6|Mentioned|p71|||||||||
3318|Calen Coal Measures|37095|6|Mentioned|p246|||||||||
3318|Calen Coal Measures|37097|4|Described|p250|||||||||
3318|Calen Coal Measures|37612|6|Mentioned|p289|||||||||
3318|Calen Coal Measures|37675|6|Mentioned|p2|||||||||
3318|Calen Coal Measures|39212|5|Briefly described|p9|||See P10||||||
3318|Calen Coal Measures|39252|6|Mentioned|p21|||||||||
3318|Calen Coal Measures|39445|5|Briefly described|Table 8|||||||||
3318|Calen Coal Measures|40574|6|Mentioned|p4|||||||||
3318|Calen Coal Measures|40577|3|Fully described|p50|||||||||
3318|Calen Coal Measures|40623|5|Briefly described|p105|||||||||
3318|Calen Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
3318|Calen Coal Measures|42187|6|Mentioned|p318|||||||||
3318|Calen Coal Measures|42281|5|Briefly described|p81|||||||||
3318|Calen Coal Measures|42648|6|Mentioned|p40|||||||||
3318|Calen Coal Measures|43987|14|Not recorded|p270,275|||||||||
3318|Calen Coal Measures|43994|14|Not recorded|Map Legend|||||||||
3318|Calen Coal Measures|43998|4|Described|p11,17,map||Permian|||||||
3318|Calen Coal Measures|44337|5|Briefly described|Map Legend||Early Permian|Lithology.||||||
3318|Calen Coal Measures|44409|14|Not recorded|Map Legend||Permian|||||||
3318|Calen Coal Measures|44635|4|Described|p11,15,Tb.1,map||Early Permian|||||||
3318|Calen Coal Measures|44728|14|Not recorded|p222|||||||||
3318|Calen Coal Measures|45071|3|Fully described|Table 9|||||||||
3318|Calen Coal Measures|45151|5|Briefly described|Table 10|||See also P15.||||||
3318|Calen Coal Measures|48881|2|Defined|p1,9,12,18,19,28,36,||Early Permian|p43||||||
3318|Calen Coal Measures|48915|6|Mentioned|Table 1|||Permian||||||
3318|Calen Coal Measures|48921|3|Fully described|p24|||Lower Permian age. See also Table 1||||||
3318|Calen Coal Measures|60787|5|Briefly described|p9|Permian|Permian|||||||
3318|Calen Coal Measures|61916|5|Briefly described|Map legend|Early Permian|Early Permian|Sandstone, siltstone, carbonaceous mudstone, coal.||||||
3318|Calen Coal Measures|61917|5|Briefly described|Map legend|Late Permian|Early Permian|Of the Back Creek Group. Sandstone, siltstone, carbonaceous mudstone , coal.||||||
3318|Calen Coal Measures|64665|5|Briefly described|p53 Fig.2, p57.|Early Permian|Early Permian|Calen Basin. Deposited in lower delta-plain environment with brief switches to upper delta-plain and fluvial regimes. Coal is low volatile bituminous rank with ash content of 16.2 to 21.4%, predominantly thermal. Is folded; dips are vertical locally.||||Unconformably overlies Lizzie Creek Volcanics and Camilla beds.||
3318|Calen Coal Measures|65388|4|Described|p191-193, p59, 60, 64, 135, 143, 362|Late Permian|Early Permian|Bowen Basin. Coal-bearing sedimentary rocks north of Mackay. Overlie Carmila beds. Correlated with Collinsville Coal Measures.  No type section. A probable thickness of between 300~420m. Sandstone, siltstone, shale and coal. Described as early Permian p193, but shown as late Permian p143.  Interpreted deposition as having occurred on a lower to upper delta plain with fluvial, overbank flats, swamps and channelled swamp environments. See also , 403, 420.||||||
3318|Calen Coal Measures|65706|4|Described|p11, p15 Tbl.1, p17 Tbl.1, p44, p136|Early Permian|Early Permian|Probably equivalent to parts of the Lizzie Creek Volcanic Group. Worked in Pindi Pindi area to supply brick clay until 1977.||||Overlies Carmila beds ?disconformably. Correlated with Collinsville Coal Measures (Back Creek Group); intruded by Urannah Igneous Complex.|Quartzose sandstone, siltstone, carbonaceous shale and mudstone, coal; volcanic and sedimentary rocks.|
3318|Calen Coal Measures|67402|6|Mentioned|p239, p250|Wordian|Artinskian|Calen Basin. Unsuitable reservoir for the storage of carbon dioxide. 300 to 400m thick. Deposited in a lower delta-plain with lesser upper delta-plain and braided river deposits. |||||Coarse-grained quartz sandstones, thin pebble conglomerate, interbedded sandstones and siltstones, claystones, carbonaceous shale and coal.|
3318|Calen Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||||
3318|Calen Coal Measures|68679|5|Briefly described|p347, p353, p360, p364, p380, p396|Permian|Permian|Laing and Hill (1960). Constitutes the sole unit in the Calen Basin, Northern New England Orogen. Late Permian. Outcrop area over 240 km2. 300-420m thick. Distinguished from underlying Carmila beds by lack of tuffaceous or other volcanic detritus. Delta plain sediments. Contains Glossopteris and Vertebraria.||||Overlies Carmila beds. Correlated with Collinsville Coal Measures (=Gebbie Subgroup).|Coarse quartz sandstone with cross-stratified thin pebble conglomerate, thin interbedded sandstone and siltstone, claystone, carbonaceous shale and coal.|
3318|Calen Coal Measures|68901|6|Mentioned|p2 Fig. i|Permian|Permian|||||||26-SEP-18
3318|Calen Coal Measures|69952|6|Mentioned|p85|Permian|Permian|||||||
3318|Calen Coal Measures|72297|5|Briefly described|p690, p695, p697|Permian|Permian|Koppe (1975). Forms the current ground surface near the coast, N of Mackay; Bowen Basin. Coal described.||||Overlies Lizzie Creek Volcanic Group and the Carmila beds.||
3346|Callide Coal Measures|12597|6|Mentioned|p498|Triassic|Triassic|||||||
3346|Callide Coal Measures|13516|6|Mentioned|p159 fig 8, p163, p164|Late Triassic|Late Triassic|From Callide Basin, Surat Basin||||||
3346|Callide Coal Measures|22977|5|Briefly described|p67 Fig.2|Triassic|Triassic|||||||
3346|Callide Coal Measures|24236|5|Briefly described|p364|Late Triassic|Middle Triassic|Overlain by Precipice Sandstone. Geological Province: Callide Basin.||||||
3346|Callide Coal Measures|24491|5|Briefly described|p12|Late Triassic|Late Triassic|See also p23.||||||
3346|Callide Coal Measures|24615|5|Briefly described|CD|Triassic|Triassic|[Rc].  Poorly sorted polymictic pebble to boulder conglomerate, sandstone, siltstone, coal seams, felsic tuff.||||||
3346|Callide Coal Measures|29591|6|Mentioned|p96|||||||||
3346|Callide Coal Measures|30059|4|Described|p5|||Triassic age.||||||
3346|Callide Coal Measures|30451|3|Fully described|p69|||Probably late Middle to early Upper Triassic age||||||
3346|Callide Coal Measures|30474|6|Mentioned|p252|||Term for lower coal-bearing section. See P249||||||
3346|Callide Coal Measures|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
3346|Callide Coal Measures|30915|6|Mentioned|p98|||||||||
3346|Callide Coal Measures|31659|6|Mentioned|p80|||Triassic||||||
3346|Callide Coal Measures|32354|6|Mentioned|p325|||||||||
3346|Callide Coal Measures|33128|6|Mentioned|p50|||Triassic||||||
3346|Callide Coal Measures|33728|6|Mentioned|Fig.1|||||||||
3346|Callide Coal Measures|34287|6|Mentioned|p158|||Triassic||||||
3346|Callide Coal Measures|35266|6|Mentioned|p192|||||||||
3346|Callide Coal Measures|35937|6|Mentioned|Fig.4|||||||||
3346|Callide Coal Measures|36172|6|Mentioned|Appendix|||||||||
3346|Callide Coal Measures|36235|6|Mentioned|p181|||See also Fig.1.||||||
3346|Callide Coal Measures|36329|6|Mentioned|p62|||||||||
3346|Callide Coal Measures|36825|6|Mentioned|p1|||||||||
3346|Callide Coal Measures|37065|5|Briefly described|p36|||||||||
3346|Callide Coal Measures|37109|4|Described|p283|||||||||
3346|Callide Coal Measures|37119|6|Mentioned|p319|||||||||
3346|Callide Coal Measures|38153|6|Mentioned|p366|||||||||
3346|Callide Coal Measures|38306|6|Mentioned|p509|||||||||
3346|Callide Coal Measures|38358|6|Mentioned|p11|||||||||
3346|Callide Coal Measures|38447|6|Mentioned|Map legend|Triassic|Triassic|||||||
3346|Callide Coal Measures|39445|5|Briefly described|Table 9|||||||||
3346|Callide Coal Measures|40115|4|Described|p15|||||||||
3346|Callide Coal Measures|40623|5|Briefly described|p83|||||||||
3346|Callide Coal Measures|41246|6|Mentioned|Map legend|Triassic||||||||
3346|Callide Coal Measures|42187|6|Mentioned|p319|||||||||
3346|Callide Coal Measures|42370|4|Described|p316|Rhaetian|Carnian|||||||
3346|Callide Coal Measures|42492|5|Briefly described|Table 2 P14|||||||||
3346|Callide Coal Measures|42648|5|Briefly described|p42, Fig.7 p43|||||||||
3346|Callide Coal Measures|43072|5|Briefly described|p80|||||||||
3346|Callide Coal Measures|43998|4|Described|p4,14,17,map||Triassic|||||||
3346|Callide Coal Measures|44382|14|Not recorded|p113|||See also Lexicon.||||||
3346|Callide Coal Measures|44432|14|Not recorded|p55,87||Middle Triassic|See also Lexicon.||||||
3346|Callide Coal Measures|44630|14|Not recorded|p492||Triassic|||||||
3346|Callide Coal Measures|44631|14|Not recorded|p205||Triassic|||||||
3346|Callide Coal Measures|44913|14|Not recorded|p57,Fig.3,68|||||||||
3346|Callide Coal Measures|50197|5|Briefly described|Map Legend|Triassic|Triassic|||||||
3346|Callide Coal Measures|50215|5|Briefly described|Map Legend|Triassic|Triassic|poorly sorted polymictic pebble to boulder conglomerate, sandstone, siltstone, coal seams, felsic tuff.||||||18-JUN-09
3346|Callide Coal Measures|61612|6|Mentioned|p270 Fig. 1|Late Triassic|Late Triassic|Geological Province: Callide Basin.||||||13-MAR-09
3346|Callide Coal Measures|61772|6|Mentioned|p129, p130 Fig. 5||Late Triassic|Contains tuffs.||||||24-SEP-08
3346|Callide Coal Measures|64665|5|Briefly described|p53 Fig.2, pp57-58, p62.|Late Triassic|Late Triassic|Callide Basin. Very sub-hydrous, with heterogeneous distributions of iron and phosphorus and low silica ash; sub-bituminous rank; feedstock for mine-mouth Callide power station; one of the lowest energy commercially exploited coals in Australia.|||Includes Callide Seam Member.|Is overlain disconformably by Precipice Sandstone.|Basal conglomerate, fining upwards with several coal seams, punctuated by matrix rich conglomerates, diamictites and breccias (debris flows).|
3346|Callide Coal Measures|67402|4|Described|p239, p242, p243|Rhaetian|Carnian|Callide Basin. Unsuitable reservoir for the storage of carbon dioxide. Up to 150m thick. Deposited in alluvial plain conditions in an inter-montane setting. ||||Overlain by the Precipice Sandstone.|Sandstone, siltstone, carbonaceous shale, mudstone, coal and conglomeratic and sandy volcanics.|
3346|Callide Coal Measures|67788|6|Mentioned|p27|Late Triassic|Late Triassic|Callide Basin, QLD.|||||Coal seams, interbedded sandstones.|
3346|Callide Coal Measures|68008|4|Described|p3, p218-222, p231, p233, p492|Late Triassic|Late Triassic|Jensen (1923); previously the Callide Series of Dunstan (1915). Half-graben sediment fill. Up to 150m thick. Late Carnian to early Rhaetian.||||Locally overlies Youlambie Conglomerate. Is overlain unconformably by Precipice Sandstone and Biloela Formation. Correlated with Ipswich Coal Measures.|Basal polymictic pebble to boulder conglomerate with thin interbeds of sandstone and siltstone and rare coal seams; local volcanic-rich horizons. Top part is interbedded sandstone and siltstone with four main coal-bearing horizons. Two debris flows.|
3346|Callide Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; Cynthia beds, and the Brisbane Tuff, are all mapped under the symbol, Rvs.||||||
3346|Callide Coal Measures|68679|4|Described|p312-313, p338, p388, p398|Late Triassic|Late Triassic|Murray et al. (2012). Callide Basin, Northern New England Orogen. Crops out around the periphery of the Basin as a belt up to 1km wide, and in a few deeply dissected valleys. Up to 150m thick. Previously (Dear et al., 1971) included the Precipice Sandstone, but the latter was excluded on palynological grounds by de Jersey (1974).|||Bottom, Callide, Sawmill, Marker Seams.|Is overlain disconformably or unconformably by the Precipice Sandstone.|Upward-fining, granule to pebble conglomerate, white and grey quartz-lithic sandstone, carbonaceous siltstone and shale, and seams of predominantly durainous, sub-bituminous steaming coal.|
3346|Callide Coal Measures|72297|5|Briefly described|p697-698, p700, p705|Late Triassic|Late Triassic|Callide Basin. Up to 180m thick. Subhydrous, subbituminous, low-sulfur coal. Indicative properties of export thermal coal tabulated.|||Marker, Callide, Sawmill and Bottom seams.|Is overlain disconformably by Precipice Sandstone.||
3348|Callide Seam|36825|6|Mentioned|p2|||||||||
3348|Callide Seam|40115|6|Mentioned|p13|||||||||
3348|Callide Seam|42187|6|Mentioned|p319|||||||||
3348|Callide Seam|42648|5|Briefly described|p42|||Callide Coal Measures||||||
3348|Callide Seam|68679|5|Briefly described|p398|Late Triassic|Late Triassic|Sub-bituminous coal, suitable for steam generation. Up to 20m thick. Open-cut mined. Informal subdivision of the coal measures (Reid 1945, 1947; Dear, McKellar & Tucker 1971; Flood 1985) recognised a basal conglomerate followed above by the Bottom, Sawmill, Callide and Marker seams.||Callide Coal Measures.||||30-APR-19
3353|Calliope beds|24076|5|Briefly described|p397 Fig. 2|Middle Devonian|Early Devonian|Max. thickness: 2135m.  Geological Province: Yarrol Basin.||||||
3353|Calliope beds|24399|6|Mentioned|p281|Devonian|Devonian|||||||
3353|Calliope beds|24420|5|Briefly described|p6|Middle Devonian|Late Silurian|||||||
3353|Calliope beds|24488|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
3353|Calliope beds|24489|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
3353|Calliope beds|24490|5|Briefly described|Map Legend|Devonian|Devonian|Volcaniclastic arenite, greywacke and conglomerate; andesitic crystal tuff and agglomerate; minor mudstone and limestone. Geological province: Calliope Block.||||||04-SEP-08
3353|Calliope beds|24491|4|Described|p15|Early Devonian|Early Devonian|||||||
3353|Calliope beds|24615|5|Briefly described|CD|Devonian|Silurian|[SDa].  Basaltic to andesitic (rarely dacitic and rhyolitic) volcaniclastic sandstone and conglomerate, limestone, siltstone, andesite.||||||
3353|Calliope beds|39987|6|Mentioned|p65|||||||||
3353|Calliope beds|41922|4|Described|Table 1, P11|||||||||
3353|Calliope beds|41925|6|Mentioned|p43|||||||||
3353|Calliope beds|42868|5|Briefly described|p17|||Superseded by Mount Holly Formation.||||||24-NOV-08
3353|Calliope beds|50096|6|Mentioned|p78|||Occurrence of Ozarkodina martinssoni auriformis (conodont).||||||29-NOV-04
3353|Calliope beds|50190|6|Mentioned|p5, 7, 10|Devonian|Devonian|Pyrite and chalcopyrite occur within andesite in these beds.||||||
3353|Calliope beds|50207|5|Briefly described|Map Legend|Early Devonian|Early Silurian|||||||
3353|Calliope beds|61392|6|Mentioned|p165 Fig. 2 (caption only)|||Part of 'Calliope Volcanic Assemblage' (Morand 1993).||||||07-FEB-11
3353|Calliope beds|61730|5|Briefly described|p994 Fig.1|Early Devonian|Late Silurian|Mainly conglomerate composed of sparsely porphyritic, amygdaloidal basalt and andesite clasts, with minor sandstone, mafic lavas, limestone, and rare siltstone. Geological Province: Yarrol Province. See also p1000, p1001.||||||
3353|Calliope beds|61808|5|Briefly described|p446|||||||||
3353|Calliope beds|63600|5|Briefly described|p900 Fig. 1, p915|Middle Devonian|Late Silurian|||||||07-FEB-11
3353|Calliope beds|67203|6|Mentioned|p6-7|Early Devonian|Late Silurian|Also appears as Calliope Beds on p10.||||||
3353|Calliope beds|68008|3|Fully described|p1, p10, p18-22, p50, p109, p113, p140|Early Devonian|Late Silurian|See also p143, p217, p279, p304, p329, p477, p487-488, p568-569, p573-574, p582, p600, p616. Dear et al. (1971). Combined with Mount Holly beds (Kirkegaard et al., 1970) by Morand (1993), but this latter unit has been re-mapped as Erebus beds and Mount Alma Formation. Yarrol Province. Forms discontinuous, elongate belt of rocks ~100km long and up to 5km wide, of low hills and poor outcrop. Thickness unknown. Geochemistry described; similarity with Folly Basalt (Nundle area, NWS) in terms of geochemistry and tectonic setting. Island arc deposits; coral species listed. Lockhovian to upper Pragian conodonts. Partial time-equivalent of Erebus and Craigilee beds. Micropaleontology table. Geophysics modelling.||||Is overlain by Nagoorin beds and unconformably by Mount Alma Formation. Is faulted against the Rockhampton Group and Nagoorin beds. Is intruded by Castletower Granite.|Conglomerate and breccia; minor sandstone, basaltic and andesitic lava, limestone and rare siltstone. Includes serpentinite, and inliers or fault blocks of Ordovician limestone.|
3353|Calliope beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Marble Waterhole, Craigilee, Munbooree and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
3353|Calliope beds|68679|5|Briefly described|p311-313, p338|Early Devonian|Late Silurian|Dear, MacKellar and Tucker (1971). Gladstone area. Forms a discontinuous belt 100km long and up to 5km wide. Previously included in the (now abandoned) Mount Holly beds. Includes a conglomerate that contains Late Ordovician and Devonian limestone clasts. Is partially coeval with Erebus and Craigilee beds.||||Is overlain unconformably by Mount Alma Formation.|A succession of mafic lava, volcaniclastics and limestone; conglomerate and breccia, poorly sorted, clast or matrix supported, are common.|
3353|Calliope beds|73143|6|Mentioned|p11, p18|Pragian|Pragian|Yarrol Basin. Contains Favosites grandipora tabulate coral and Aphyllum simplexum rugose coral (Blake, 2010).||||||
3353|Calliope beds|73450|6|Mentioned|p9, p67|Early Devonian|Early Devonian|||||Intruded by Castletower Granite and Goondicum Gabbro.||
3366|Cambalanga Tuff Member|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Parent: Johngboon Rhyolite.||||||14-AUG-08
3366|Cambalanga Tuff Member|41738|2|Defined|p171|Late Triassic||Reserved as Cambalanga.||||||14-AUG-08
3366|Cambalanga Tuff Member|42054|6|Mentioned|p272|||||||||
3366|Cambalanga Tuff Member|63821|5|Briefly described|p21, p22|||Of the Johngboon Rhyolite. (Aranbanga Volcanic Group). Crystal-poor (quartz dominant), non-welded tuff.||||||07-FEB-11
3366|Cambalanga Tuff Member|68679|5|Briefly described|p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. Unwelded lower Member of the Johngboon Rhyolite or co-ignimbrite air-fall deposit on Johngboon Rhyolite. Thickness estimates vary: 100-150m to 20m.||Johngboon Rhyolite.|||Poorly-exposed, pale green, friable, vitric-crystal intermediate tuff; fine-grained with quartz and rare feldspar crystal fragments in altered groundmass. Altered pumice fragments conspicuous (~70% in southern part).|
3366|Cambalanga Tuff Member|73450|6|Mentioned|p30|||||||||
3378|Camboon Volcanics|13516|6|Mentioned|p145 fig 3|Early Permian|Early Permian|From Taroom Shelf, Bowen Basin. Age: APP22.||||Overlain by Buffel Formation.||
3378|Camboon Volcanics|22439|5|Briefly described|p15, Fig.2|Early Permian|Early Permian|Taroom Trough, Bowen Basin.||||||
3378|Camboon Volcanics|22857|6|Mentioned|p258|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|22863|6|Mentioned|p242|||||||||
3378|Camboon Volcanics|22864|6|Mentioned|p256||Early Permian|||||||
3378|Camboon Volcanics|22973|6|Mentioned|p10|||||||||
3378|Camboon Volcanics|22975|5|Briefly described|p34 Fig.6|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|22980|5|Briefly described|p249 Fig.2|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|23037|4|Described|p10,24,30-42,48,52-9|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|23042|4|Described|p8|||||||||
3378|Camboon Volcanics|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||30-NOV-09
3378|Camboon Volcanics|23161|6|Mentioned|p23|||||||||
3378|Camboon Volcanics|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPvc].  Basaltic to andesitic lava and equivalent volcaniclastic rocks; subordinate felsic ignimbrite and other volcaniclastic rocks and minor lava; commonly deformed to schistose equivalents in the Gogango Deformed Zone.||||||
3378|Camboon Volcanics|29387|6|Mentioned|Table 4|||||||||
3378|Camboon Volcanics|34133|6|Mentioned|p29|||||||||
3378|Camboon Volcanics|38204|4|Described|p69|||||||||
3378|Camboon Volcanics|39262|6|Mentioned|p121|||||||||
3378|Camboon Volcanics|39267|6|Mentioned|p232|||||||||
3378|Camboon Volcanics|40090|6|Mentioned|p81|||||||||
3378|Camboon Volcanics|40091|4|Described|p69|||||||||
3378|Camboon Volcanics|40093|6|Mentioned|p26|||||||||
3378|Camboon Volcanics|40094|4|Described|p22|||||||||
3378|Camboon Volcanics|40096|6|Mentioned|p3|||||||||
3378|Camboon Volcanics|40623|5|Briefly described|p80|||||||||
3378|Camboon Volcanics|41246|6|Mentioned|Map legend|Permian||||||||
3378|Camboon Volcanics|41546|6|Mentioned|p157|||||||||
3378|Camboon Volcanics|41666|6|Mentioned|Fig.1|||||||||
3378|Camboon Volcanics|41725|6|Mentioned|Fig.2|||||||||
3378|Camboon Volcanics|42249|6|Mentioned|p21|||||||||
3378|Camboon Volcanics|42250|6|Mentioned|Fig.4 P31|||||||||
3378|Camboon Volcanics|42641|6|Mentioned|Fig.3 P110|||||||||
3378|Camboon Volcanics|42987|6|Mentioned|p25|||||||||
3378|Camboon Volcanics|43000|5|Briefly described|p106|||||||||
3378|Camboon Volcanics|43017|5|Briefly described|Fig.3,p375|||||||||
3378|Camboon Volcanics|43050|5|Briefly described|p30|||||||||
3378|Camboon Volcanics|43185|6|Mentioned|6,9||Early Permian|||||||
3378|Camboon Volcanics|43995|14|Not recorded|Table p9|Permian|Carboniferous|||||||
3378|Camboon Volcanics|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|50215|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes the Mount Bulgi Conglomerate Member.  Overlie the Torsdale Volcanics.||||||17-MAY-04
3378|Camboon Volcanics|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Includes the Gonyelinka Ignimbrite and Mount Bulgi Conglomerate Members.||||||18-MAY-04
3378|Camboon Volcanics|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes: Mount Bulgi Conglomerate Member, Gonyelinka Ignimbrite Member.||||||27-MAY-04
3378|Camboon Volcanics|50317|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|50597|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Basaltic to andesitic lava and volcaniclastic rocks.||||||
3378|Camboon Volcanics|50602|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Basaltic to andesitic lava and equivalent volcaniclastic rocks.||||||
3378|Camboon Volcanics|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
3378|Camboon Volcanics|60282|4|Described|p6|Early Permian|Late Carboniferous|Age: 291Ma and 293+/-3Ma (SHRIMP).||||||
3378|Camboon Volcanics|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Geological Province: Bowen Basin.||||||
3378|Camboon Volcanics|60298|5|Briefly described|p192|Early Permian|Late Carboniferous|Mafic. Geological Province: Bowen Basin.||||||17-DEC-07
3378|Camboon Volcanics|60386|6|Mentioned|p296|Artinskian|Asselian|Bowen/Sydney Basin. Non-marine.||||||
3378|Camboon Volcanics|61035|5|Briefly described|p5|Permian|Early Permian|In the Auburn Arch. Geological Province: Auburn Subprovince.||||||07-FEB-11
3378|Camboon Volcanics|61076|5|Briefly described|p188 Fig. 2|Early Permian|Early Permian|Age: <300Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
3378|Camboon Volcanics|61612|6|Mentioned|p270, p270 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Bowen Basin. QLD.||||||13-MAR-09
3378|Camboon Volcanics|61777|5|Briefly described|p224, p227-229, p230, p225 Tab. 1|Early Permian|Early Permian|Age: 298+/-3 and 308+/-6Ma (SHRIMP U/Pb). Geological Province: Yarrol Province. Mainly andesite, basalt and volcaniclastics. See p277-229 for detailed info.||||||07-FEB-11
3378|Camboon Volcanics|61782|5|Briefly described|p280|||Contain acid to intermediate volcanics and volcaniclastic sedimentary rocks.||||||
3378|Camboon Volcanics|61832|5|Briefly described|p187|Permian|Carboniferous|Hosts Cracow gold deposit. Geological Province: Bowen Basin.||||||28-MAY-08
3378|Camboon Volcanics|62357|5|Briefly described|p524 Fig. 7|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||
3378|Camboon Volcanics|64855|5|Briefly described|p28|Early Permian|Early Permian|||||||22-FEB-10
3378|Camboon Volcanics|64856|4|Described|p42-45, p49-50, p52-53, p102|Early Permian|Late Carboniferous|Taroom Trough, Bowen Basin. Supersedes Camboon Andesite. Max thickness 658m. Mainly andesite to basalt flows and tuffs. Essentially equivalent to Combarngo volcanics.  Age from palynoflora (unit APP12) and dates of 294 and 281 Ma from Runnegar (1979).| | ||||28-NOV-17
3378|Camboon Volcanics|64857|5|Briefly described|p114,116, p113 Fig.3, p115|Early Permian||Bowen Basin. Unconformably overlain by Buffel Formation. Text seems to imply an Early Permian age.||||||
3378|Camboon Volcanics|64858|6|Mentioned|p180 Fig.2|Early Permian|Early Permian|||||||30-NOV-09
3378|Camboon Volcanics|65112|5|Briefly described|p313; Fig 4 p314|Early Permian|Early Permian|Partly equivalent in age to Reids Dome beds in Denison Trough. Underlies the Buffel Formation in the Taroom Trough.||||||22-MAR-12
3378|Camboon Volcanics|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Taroom Trough. Underlies Buffel Formation.||||||
3378|Camboon Volcanics|65114|5|Briefly described|p383 Tb.1, p385 Fig.3, pg 394, 395|Cisuralian||ca 297-278Ma; of Bowen Basin-Taroom Trough; occurs below Buffel Formation; may extend down into the APP1 palynological zone; dates include K/Ar age of 277.9 +/- 4Ma near top of unit, 296.3 +/- 4 Ma (dates all referenced), max SHRIMP age 309.1 +/- 3.3Ma||||||
3378|Camboon Volcanics|65115|5|Briefly described|p405, 409, 411, Fig 2 p403, Fig 4a p406|Early Permian|Early Permian|Andesitic and basaltic flows, welded tuff, agglomerate, volcanic breccia, conglomerate, lithic sandstone and carbonaceous mudstone, up to 3000m thick. Ar-Ar dates 294-281 Ma (Runnegar 1979).||||||
3378|Camboon Volcanics|65116|5|Briefly described|Fig 2 p436|Early Permian|Early Permian|Taroom Trough, Bowen Basin. Underlies Buffel Formation.||||||
3378|Camboon Volcanics|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Buffel Formation in the Taroom Trough in the Bowen Basin.||||||06-MAR-12
3378|Camboon Volcanics|65119|5|Briefly described|p511, Fig 2, table 1, Fig 4-5,7-10,15-19|Early Permian|Early Permian|Bowen Basin. Andesite, basalt, dacite, rhyolite, tuffs and flows. Sandstone, siltstone, volcaniclastic conglomerate breccia.Up to ~3000m thick. Age: 268-280 Ma. Fission Track age: 77-174 Ma.||||||07-MAR-12
3378|Camboon Volcanics|65388|2|Defined|p20-32, p11, 14, 16 , 35, 36, 43, 123|Early Permian|Late Carboniferous|Includes Mount Bulgi Conglomerate Member at base. Disconformably overlies Torsdale Vocanics. Overlain by Buffel Formation, Back Creek Group, Woolein Formation or Oxtrack Formation. SHRIMP dates: 308+/-5 Ma near base, 297 +/-2 Ma. Formerly Camboon Andesite.  Camboon Volcanics of Briggs and Waterhouse (1982). Type section proposed - Delusion Creek.  Sometimes difficult to distinguish from Torsdale Volcanics. Contacts may be diachronous. Lithology: andesitic and basaltic lavas and volcaniclastics, but rhyolitic to dacitic lavas and volcaniclastics, including ignimbrite, and pebble to boulder conglomerate also present. Intruded by gabbro/diorite. See also p126, 166, 180, 338, 339, 432, 437, 439, 446, 447||||||
3378|Camboon Volcanics|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
3378|Camboon Volcanics|67133|5|Briefly described|p7|Permian|Permian|Basal unit of the Taroom Trough in the Bowen Basin. The sample analysed in this study was a highly weathered andesitic to dacitic crystal tuff, with alteration products including two types of smectite-rich clays and hematite.|||||Includes andesitic and basaltic lavas and tuffs.|
3378|Camboon Volcanics|67402|6|Mentioned|p21|Artinskian|Asselian|Bowen Basin. ||||Overlain by the Buffel Formation.||
3378|Camboon Volcanics|68008|5|Briefly described|p132, p138, p155-156, p292|||Text unclear: may include Mount Bulgi Conglomerate as basal unit [if so, should be Mount Bulgi Conglomerate Member]. Subaerially-erupted volcanics with similar mineralogy and textures to Rookwood Volcanics.||||Overlies Torsdale Volcanics.||
3378|Camboon Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Auburn Subprovince.||||||
3378|Camboon Volcanics|68679|4|Described|p312-313, p338, p343-344, p351-355, p360|Permian|Late Carboniferous|See also p372 Fig.5.64, p375, p379-381, p397, p407, p416, p419, p468-469. Camboon Volcanic Arc, Northern New England Orogen. Extends almost continuously ~200km from S of Cracow to the Capricorn Highway. Subaerial eruptions and fluvial, lacustrine or mass flow deposition in a volcanic landscape. Some marine fossil-bearing rocks E of the Auburn Subprovince, thought to be of this unit (Dear et al. 1971; Parfrey 1986), are now attributed to the Buffel Formation (Withnall et al., 2009). Various ages given. RELATED UNITS (continued): May have been partly coeval with Torsdale Volcanics. Probably part-correlated with Nogo beds. May be continuous with Combarngo Volcanics. Is intruded by Harrami Igneous Complex; Nulambie, Wingfield Granites. Source of Woolein Formation sediments.|297-c.295 Ma (Fanning et al., 2009).||Mount Bulgi Conglomerate Member.|Overlies Torsdale Volcanics. Is interleaved (as thrust slices) with overlying Woolein Formation and Back Creek Group. Underlies Buffel (unconformably) and Woolein Formations. See COMMENTS for more.|Mainly andesitic to basaltic lavas and volcaniclastics, with some rhyolitic to dacitic lavas and volcaniclastics including ignimbrite and pebble to boulder conglomerate. Alteration is relatively pervasive.|
3378|Camboon Volcanics|68822|5|Briefly described|p321, p337|Permian|Carboniferous|Late Carboniferous to Early Permian age.|||||Basaltic to rhyolitic.|
3378|Camboon Volcanics|70033|6|Mentioned|p2, p29|||Unit at base of Bowen Basin.||||||
3378|Camboon Volcanics|70837|5|Briefly described|p246|Cisuralian|Cisuralian|Of  Bowen Basin. SHRIMP ages of 295.2 and 297.1 Ma (Fanning etal., 2009). Corresponding to APP2 zone (Cisuralian-Guadalupian).||||||
3378|Camboon Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Dacite, ignimbrite.|
3378|Camboon Volcanics|71701|5|Briefly described|p170|Cisuralian|Cisuralian|Bowen Basin. Potential source of Cisuralian ash falls in the Galilee Basin. SHRIMP dates are derived from Fanning et al, 2009 and Nicoll et al, 2015.|297.1 +/- 3.3 and 295.2 +/- 6.2 (SHRIMP)|||||
3378|Camboon Volcanics|71702|6|Mentioned|179|||Arc-related rocks. Gympie Terrane.||||||
3378|Camboon Volcanics|72297|5|Briefly described|p710|||Near Cracow, hosts gold in quartz veins and zones of silicification.|||||Andesitic lavas, tuffs and coarse breccias.|
3378|Camboon Volcanics|73163|6|Mentioned|p467|||New England Orogen. Attribed to the initial, extensional stage of the Bowen Basin.||||||
3378|Camboon Volcanics|73197|6|Mentioned|p470-471, p472 Tb.2|Cisuralian|Gzhelian|New England Orogen, northern. Eastern margin of the Bowen Basin. Rift volcanic rocks. U-Pb zircon age from Withnall et al., (2009).|297.1 +/- 3.3 Ma, 295.2 +/- 6.2 Ma U-Pb zircon||||Volcanics.|
3378|Camboon Volcanics|73450|6|Mentioned|p55|||Bowen Basin.||||||
3394|Cameron Falls Member|40896|6|Mentioned|p5|||||||||
3394|Cameron Falls Member|41824|6|Mentioned|p201|||||||||
3394|Cameron Falls Member|43161|5|Briefly described|12|||||||||
3415|Campaspe Surface|23424|5|Briefly described|p340||Tertiary|||||||
3415|Campaspe Surface|37607|5|Briefly described|Fig.3|||||||||
3415|Campaspe Surface|69599|5|Briefly described|p584-586, p594|Pliocene|Pliocene|Grimes (1980), for the uniform ferricrete of the Campaspe Formation and other units in the region. Charters Towers region. Widespread duricrust.||||||
3415|Campaspe Surface|69789|6|Mentioned|p1041, p1044-1047|||A relict alluvial plain, 200-440m asl rising to the W.||||||22-JUN-20
3458|Candover Metamorphics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
3458|Candover Metamorphics|23518|5|Briefly described|p9 Fig. 3|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province.||||||
3458|Candover Metamorphics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Leichardt Subprovince.||||||07-NOV-08
3458|Candover Metamorphics|38560|2|Defined|p112|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3458|Candover Metamorphics|39495|6|Mentioned|p142|||||||||
3458|Candover Metamorphics|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
3458|Candover Metamorphics|40840|6|Mentioned|Map legend|||||||||
3458|Candover Metamorphics|45166|4|Described|p13|||||||||
3458|Candover Metamorphics|50100|5|Briefly described|p13 Fig.4|Orosirian|Orosirian|Age: ~1850Ma.  Geological Province: Western Fold Belt Province.||||||
3458|Candover Metamorphics|50332|5|Briefly described|p10, p16|Proterozoic|Proterozoic|Comprised of mica schist, quartzite, felsic to mafic metavolcanics and conglomerate.||||||07-FEB-11
3458|Candover Metamorphics|50536|6|Mentioned|p2.1|||Intruded by the Kalkadoon Supersuite.||||||
3458|Candover Metamorphics|63866|5|Briefly described|p57|Orosirian||Leichhardt River Fault Trough.|>1850 Ma|||||
3458|Candover Metamorphics|67323|6|Mentioned|Mount Isa Block Time-Space Plot; p39-40|||Leichhardt River Domain, Mount Isa Inlier. See also reference to Candover beds (GIS attrib tbl).||||||
3458|Candover Metamorphics|69591|5|Briefly described|p30, p32, p58|||Wilson and Derrick (1983). Kalkadoon-Leichhardt Domain, Mount Isa Province. Unconformably underlies Leichhardt Superbasin rocks.|||||Schist, quartzite, felsic and mafic volcanics.|
3458|Candover Metamorphics|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Metamorphics, minor mafic extrusives.|
3465|Cannibal Creek Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|300-270 Ma.|Unit in Whypalla Supersuite.||||
3465|Cannibal Creek Granite|23423|5|Briefly described|p301 Table 7.2|Permian|Carboniferous|||||||
3465|Cannibal Creek Granite|23430|5|Briefly described|p475|||||||||
3465|Cannibal Creek Granite|24086|6|Mentioned|p316|||||||||
3465|Cannibal Creek Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
3465|Cannibal Creek Granite|31435|6|Mentioned|p17|||||||||
3465|Cannibal Creek Granite|31832|6|Mentioned|Table 6|||||||||
3465|Cannibal Creek Granite|37614|6|Mentioned|p240|||||||||
3465|Cannibal Creek Granite|39445|5|Briefly described|Table 12|||||||||
3465|Cannibal Creek Granite|39689|6|Mentioned|p56|||See also P58||||||
3465|Cannibal Creek Granite|39822|6|Mentioned|p217|||||||||
3465|Cannibal Creek Granite|40277|5|Briefly described|p293|||||||||
3465|Cannibal Creek Granite|40278|6|Mentioned|p645|||||||||
3465|Cannibal Creek Granite|42304|3|Fully described|p15|Permian|Carboniferous|||||||
3465|Cannibal Creek Granite|42620|3|Fully described|p173|Early Permian|Devonian|Whypalla Supersuite||||||
3465|Cannibal Creek Granite|42658|6|Mentioned|p31|||||||||
3465|Cannibal Creek Granite|42968|5|Briefly described|Fig. 1,p91,p100|||||||||
3465|Cannibal Creek Granite|43083|4|Described|p127|||Of Whypalla Supersuite. Ages: 270 Ma and 275 Ma (Rb-Sr). granite predominantly of quartz, plagioclase and K-feldspar in roughly equal proportions.||||||17-JUN-09
3465|Cannibal Creek Granite|43625|5|Briefly described|p52,124,Appendix 6|||||||||
3465|Cannibal Creek Granite|43896|14|Not recorded|Map Legend||Permian|||||||
3465|Cannibal Creek Granite|43898|14|Not recorded|Map Legend||Carboniferous|||||||
3465|Cannibal Creek Granite|44425|14|Not recorded|p18,22,opp.11,map|||||||||
3465|Cannibal Creek Granite|45003|14|Not recorded|p30|||||||||
3465|Cannibal Creek Granite|45025|4|Described|p77-8||Permian|||||||
3465|Cannibal Creek Granite|45113|3|Fully described|p21|||Emphasis on petrography.||||||
3465|Cannibal Creek Granite|46845|6|Mentioned|Table 1|||||||||
3465|Cannibal Creek Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
3465|Cannibal Creek Granite|60357|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province. Muscovite-biotite granite.||||||
3465|Cannibal Creek Granite|61527|6|Mentioned|p795|||||||||
3465|Cannibal Creek Granite|66852|5|Briefly described|pp937-938.|||Shows evidence of syntectonic emplacement. Its northern end is regarded as the product of emplacement along WNW-ESE faults within the Desailly Structure.||Unit in Whypalla Supersuite.||||
3465|Cannibal Creek Granite|69592|5|Briefly described|p247-249|Permian|Permian|Central Palmer-Barron Subprovince. Deformation fabric photograph and diagrams.||||Intrudes Hodgkinson Formation.||
3465|Cannibal Creek Granite|69593|5|Briefly described|p477, p479, p482, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280-275 Ma.|Cannibal Creek Suite.|||S-type granite; contains enclaves that are peraluminous and silicic.|
3469|Cannindah Limestone|24076|5|Briefly described|p397 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Yarrol Basin.||||||
3469|Cannindah Limestone|31586|4|Described|p2|||See also corals p1. Previously Baywulla Fm.||||||01-OCT-08
3469|Cannindah Limestone|31587|3|Fully described|p57|||See also p58-76. Corals.||||||01-OCT-08
3469|Cannindah Limestone|33728|6|Mentioned|p52|||||||||
3469|Cannindah Limestone|36528|6|Mentioned|Fig.4|||||||||
3469|Cannindah Limestone|42002|5|Briefly described|p92|||||||||
3469|Cannindah Limestone|42547|4|Described|p51|||||||||
3469|Cannindah Limestone|43983|14|Not recorded|p2||Visean|See also Lexicon.||||||
3469|Cannindah Limestone|44360|14|Not recorded|p2,24,32||Early Carboniferous|Ref. to Maxwell 1960. Partly equivalent to Kolanga Creek Limestone Member. See also Lexicon.||||||
3469|Cannindah Limestone|44432|14|Not recorded|p34||Dinantian|||||||
3469|Cannindah Limestone|44487|2|Defined|p119,200-201||Visean|See also Lexicon. Name proposed in lieu of Baywulla Formation in Monto-Old Cannindah area. Rich coral fauna. (Visean-Probably M-U Visean)||||||
3469|Cannindah Limestone|46803|6|Mentioned|p143|||||||||
3469|Cannindah Limestone|68008|5|Briefly described|p90, p96, p104-105|Early Carboniferous|Early Carboniferous|Jull (1968). Old Cannindah area. Superseded by Rockhampton Group. Detailed facies description.|||||Oolitic/pisolitic limestone with relatively large intervals of sandstone or siltstone; large amalgamated reef complexes; tuffaceous intervals.|
3469|Cannindah Limestone|68679|6|Mentioned|p340|||Jull (1968) in the Old Cannindah area.||||||
3469|Cannindah Limestone|70050|5|Briefly described|p335, p337-344, p346-348, p352-354, p358|Visean|Visean|See also p365-367. Old Cannindah Homestead, Monto area. Contains Cionodendron and Australastraea coral fossils (illustrations and systematic palaeontology), including the holotypes of C. montoense and C. textum, and A. carinata.||||Upper part is correlated biostratigraphically with Kyndalyn Mudstone Member (Merlewood Formation).||16-APR-18
3497|Cape Hillsborough beds|36472|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
3497|Cape Hillsborough beds|36906|6|Mentioned|p25|||||||||
3497|Cape Hillsborough beds|39943|6|Mentioned|Table 13A|||See also Table 13D||||||
3497|Cape Hillsborough beds|41246|6|Mentioned|Map legend|Tertiary||||||||
3497|Cape Hillsborough beds|61155|5|Briefly described|p20|Middle Eocene|Middle Eocene|Overlain by Emerald, Exevale and/or Duaringa Formations. Max. thickness: 1300m. In the Fitzroy region.||||||03-MAR-10
3497|Cape Hillsborough beds|65706|4|Described|p12, p19 Tb.1|Paleogene|Late Cretaceous|Hillsborough Basin. Contains major oil shale deposits. Possible genetic relationship with the Mount Jukes Syenite Complex. ||||Unconformably overlies and is faulted against Campwyn Volcanics. Unconformably overlies Carmila beds.|Acid volcanics, conglomerate, shale, argillaceous sandstone, basalt, oil shale.|
3497|Cape Hillsborough beds|67402|5|Briefly described|p165 tbl LPB1, p210|Oligocene|Middle Eocene|Hillsborough Basin. Interpreted to have been deposited in fluvial or lacustrine depositional environments. Maximum thickness of 3000m. |||||Claystones, siltstone, conglomerate, shale, argillaceous sandstone, acid volcanics, basalt and oil shale.|
3497|Cape Hillsborough beds|68358|5|Briefly described|p3, p7-p8, p12-14, p16-20|Paleogene|Paleogene|Hillsborough Basin. 320.71m were intersected. No coal, aquifers or natural underground reservoirs were intersected. Temperature log, core photographs, detailed lithological descriptions, thermal conductivity results. Authors conclude the Hillsborough Basin is highly prospective for geothermal exploration.|||||A sequence of sandstone, mudstone, carbonaceous shale, and minor coal.|05-MAR-19
3497|Cape Hillsborough beds|69582|6|Mentioned|p41, p43, p45|Paleogene|Paleogene|Hillsborough Basin. On the basis of seismic data are interpreted to be 2100m thick onshore thinning towards the southern onshore boundary. Estimated to be 1300m thick in the vicinity of GSQ Bowen 1.|||||Fine- to coarse-grained andstone, mudstone, carbonaceous shale and minor coal.|
3497|Cape Hillsborough beds|69599|5|Briefly described|p585, p590|Oligocene|Eocene|Hillsborough Basin. Up to 1271m thick.|||||Acid volcanics, conglomerate, shale, argillaceous sandstone, basalt and oil shale.|
3497|Cape Hillsborough beds|73450|4|Described|p45, p71, p74|Rupelian|Priabonian|Basal 22 m are non-volcanogenic. Rhyolite flows are up to 30 m thick and exhibit flow banding, spherultic textures (some perlitic) and local auto-brecciation. Basaltic flows are variably porphyritc (plagioclase) to aphyric, amygdaloidal and originally olivine-bearing. Many deposits are reworked with cross bedding, scour and fill and imbrication; clasts up to 5 m in diameter indicate mass wasting. Deposition is interpreted to be on the flanks of a central volcano developed close to the margin of the Hillsborough Basin (not the Mount Jukes Intrusive Complex). K-Ar ages range from 31.0 +/- 0.8 Ma to 36.6 +/- 0.5 Ma.|Ranges from ca 31 - 36.6 Ma K-Ar||||Oil shale, limestone, fine sandstone, and rhyolitic and basaltic flows and pyroclastic deposits including ash flow tuffs and rheomorphic ignimbrite.|
3615|Cargoogie Oolite Member|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Crmc].  Oolitic limestone, minor sandstone and mudstone.||||||
3615|Cargoogie Oolite Member|31586|5|Briefly described|p5|||Corals. See also P7||||||
3615|Cargoogie Oolite Member|31657|5|Briefly described|p94|||U.Tournaisian to U.Visean||||||
3615|Cargoogie Oolite Member|31659|5|Briefly described|p52||Visean|Of the Malchi Formation (Rockhampton Group).||||||09-JUN-09
3615|Cargoogie Oolite Member|38406|6|Mentioned|p11|||||||||
3615|Cargoogie Oolite Member|39973|6|Mentioned|p4|||||||||
3615|Cargoogie Oolite Member|41576|4|Described|Table 1|||||||||
3615|Cargoogie Oolite Member|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
3615|Cargoogie Oolite Member|41925|6|Mentioned|p45|||||||||
3615|Cargoogie Oolite Member|42002|6|Mentioned|p94|||||||||
3615|Cargoogie Oolite Member|42547|5|Briefly described|p49, 50|||||||||
3615|Cargoogie Oolite Member|42583|6|Mentioned|p66|||Part of Malchi Fmn.||||||
3615|Cargoogie Oolite Member|44360|14|Not recorded|p30,31|||||||||
3615|Cargoogie Oolite Member|44388|2|Defined|p13-116||Visean|Member of Malchi Formation.||||||
3615|Cargoogie Oolite Member|45097|6|Mentioned|p23|||Fossils. Correlation chart||||||
3615|Cargoogie Oolite Member|46803|6|Mentioned|p148|||||||||
3615|Cargoogie Oolite Member|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Malchi Formation (Rockhampton Group).||||||17-MAY-04
3615|Cargoogie Oolite Member|68008|5|Briefly described|p90, p95|Early Carboniferous|Early Carboniferous|Fleming (1967). Not reliably recognised outside the Stanwell area. Detailed facies description.||Malchi Formation.||||
3615|Cargoogie Oolite Member|68679|5|Briefly described|p340|||Fleming (1967).||Malchi Formation.||||
3615|Cargoogie Oolite Member|70050|6|Mentioned|p328|||||Malchi Formation.||||
3620|Carl Creek Limestone|23031|5|Briefly described|31|||||||||
3620|Carl Creek Limestone|23393|5|Briefly described|p24|Oligocene|Oligocene|||||||
3620|Carl Creek Limestone|23425|4|Described|p383, Table 9.7 p393.|||Geological Province: Karumba Basin.||||||03-AUG-06
3620|Carl Creek Limestone|34061|6|Mentioned|p54|||||||||
3620|Carl Creek Limestone|35620|6|Mentioned|p299|||Location of middle to late Miocene kangaroo.||||||
3620|Carl Creek Limestone|36213|6|Mentioned|p86|||||||||
3620|Carl Creek Limestone|36228|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3620|Carl Creek Limestone|37607|6|Mentioned|p330|||See also p334 and Fig.5.||||||03-AUG-06
3620|Carl Creek Limestone|38291|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
3620|Carl Creek Limestone|38348|5|Briefly described|p25|||See also p24.||||||03-AUG-06
3620|Carl Creek Limestone|38373|6|Mentioned|p624|||||||||
3620|Carl Creek Limestone|38374|6|Mentioned|p606|||||||||
3620|Carl Creek Limestone|38528|6|Mentioned|p287|||||||||
3620|Carl Creek Limestone|39445|5|Briefly described|Table 14|||||||||
3620|Carl Creek Limestone|39497|6|Mentioned|p16|||||||||
3620|Carl Creek Limestone|39562|5|Briefly described|Map legend|early Miocene|late Oligocene|Massive limestone.   Part of the Trans-Australian Platform Cover.||||||15-JUN-06
3620|Carl Creek Limestone|39797|6|Mentioned|Map legend|Miocene|Miocene|||||||
3620|Carl Creek Limestone|41537|6|Mentioned|Fig.2|||||||||
3620|Carl Creek Limestone|42590|6|Mentioned|p204|||||||||
3620|Carl Creek Limestone|42637|6|Mentioned|p29|||||||||
3620|Carl Creek Limestone|44213|14|Not recorded|Map Legend||Tertiary|||||||
3620|Carl Creek Limestone|44238|14|Not recorded|p219-227,232|Early Miocene|Late Oligocene|See also Fig. 1,3,4,5,6. (L.Olig-Early Miocene).||||||
3620|Carl Creek Limestone|44274|2|Defined|Tb.1,p6,7,12,map||Tertiary|Rests on basement rocks and Thorntonia Limestone. (Tertiary or Late Cretaceous)||||||
3620|Carl Creek Limestone|44281|14|Not recorded|Map Legend||Tertiary|||||||
3620|Carl Creek Limestone|44351|14|Not recorded|p15,16|||Lacustrine,fossils.||||||
3620|Carl Creek Limestone|44482|14|Not recorded|opp.p.6|||(E53-12).||||||
3620|Carl Creek Limestone|44989|4|Described|p.102,127|||Renamed Verdon Limestone by Traves & Noakes 1954, but old name now re-established.||||||03-AUG-06
3620|Carl Creek Limestone|45128|6|Mentioned|p54|||||||||
3620|Carl Creek Limestone|45145|5|Briefly described|p37|||||||||
3620|Carl Creek Limestone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
3620|Carl Creek Limestone|47044|6|Mentioned|p191|||||||||
3620|Carl Creek Limestone|47083|5|Briefly described|p20|Early Miocene|Late Oligocene|||||||
3620|Carl Creek Limestone|50600|5|Briefly described|Map legend|Early Miocene|Late Oligocene|Basal calcite-cemented breccia overlain by a thick-bedded sandy calcirudite containing gastropod and vertebrate remains.||||||
3620|Carl Creek Limestone|60703|5|Briefly described|p704 Fig. 2|Miocene|Miocene|See also p725 Fig. 18 and p731 Fig.20||||||12-APR-05
3620|Carl Creek Limestone|61119|6|Mentioned|p124, p130, p132, p137, pp142-143, p146||Cenozoic|Spring-fed perennial stream and ephemeral pool deposits? Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
3620|Carl Creek Limestone|61155|5|Briefly described|p16|Miocene|Miocene|Overlain by Wyaaba and Falloch beds. Age: <21.5Ma Together with Gregory Downs Limestone thickness is 12m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
3620|Carl Creek Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Massive limestone.|
3620|Carl Creek Limestone|67402|5|Briefly described|p177 tbl CRP/KRM1||Longfordian|Karumba Basin. Deposited in a lacustrine environment. Unsuitable reservoir for the storage of carbon dioxide. See also p181 tbl CRP/KRM2, p239. Age probably equivalent to Aquitanian - Burdigalian.||||Overlies the Bulimba Formation. Unconformably overlain by the Wyaaba beds.|Micritic arenaceous limestone, claystone, chert and conglomerate.|17-SEP-18
3620|Carl Creek Limestone|69599|5|Briefly described|p585, p603, p651|Miocene|Oligocene|Riversleigh area, Carpentaria region. Forms escarpments and mesas. Lacustrine sediments. Contains many unnamed karst and lacustrine carbonate deposits (Oligocene to Holocene) containing abundant internationally significant vertebrate fauna (detailed account pp603-605). Silcrete weathered surface.||||Correlated with Carl Creek Limestone.||
3620|Carl Creek Limestone|71502|5|Briefly described|p1|Miocene|Oligocene|Some outcrops display Fe enrichment.||||Unconformably underlain by Thorntonia Limestone.|Freshwater carbonates including a basal calcite-cemented breccia overlain by thickly-bedded sandy calcrudites with gastropod and vertebrate remains.|
3624|Carlo Sandstone|8187|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
3624|Carlo Sandstone|8217|5|Briefly described|Map Legend|Ordovician|Ordovician|Sandstone.||||||
3624|Carlo Sandstone|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose sandstone, siltstone and mudstone clasts, minor mudstone.||||||
3624|Carlo Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|12951|5|Briefly described|p143 fig 4, p145 fig 6, p152|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
3624|Carlo Sandstone|13995|6|Mentioned|p76, p101|||Georgina Basin. Contains Middle Ordovician pelecypods.||||||
3624|Carlo Sandstone|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
3624|Carlo Sandstone|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
3624|Carlo Sandstone|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 150m.||||||
3624|Carlo Sandstone|24442|6|Mentioned|p49|||On TOBERMORY sheet.||||||
3624|Carlo Sandstone|33111|4|Described|p33|||||||||
3624|Carlo Sandstone|33657|6|Mentioned|p1|||||||||
3624|Carlo Sandstone|33738|6|Mentioned|p54|||||||||
3624|Carlo Sandstone|34252|6|Mentioned|Po.2|||Fossils||||||
3624|Carlo Sandstone|34454|5|Briefly described|Table 2|||M.Ordovician||||||
3624|Carlo Sandstone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
3624|Carlo Sandstone|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
3624|Carlo Sandstone|35139|4|Described|Table.2|||||||||
3624|Carlo Sandstone|36234|3|Fully described|p173|||See also Fig.1.||||||
3624|Carlo Sandstone|36243|6|Mentioned|Table 1A|||||||||
3624|Carlo Sandstone|36580|6|Mentioned|p469|||See also Fig.1||||||
3624|Carlo Sandstone|37572|4|Described|p163|||||||||
3624|Carlo Sandstone|38832|6|Mentioned|p157|||||||||
3624|Carlo Sandstone|39445|5|Briefly described|Table 4|||||||||
3624|Carlo Sandstone|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
3624|Carlo Sandstone|39943|6|Mentioned|Table 2B|||||||||
3624|Carlo Sandstone|40136|5|Briefly described|p20|||||||||
3624|Carlo Sandstone|40810|5|Briefly described|p15|||||||||
3624|Carlo Sandstone|41524|6|Mentioned|p23|||||||||
3624|Carlo Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
3624|Carlo Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
3624|Carlo Sandstone|43105|5|Briefly described|Fig.4,p9.|||||||||
3624|Carlo Sandstone|43236|6|Mentioned|p14||Ordovician|Georgina Basin||||||
3624|Carlo Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
3624|Carlo Sandstone|44308|14|Not recorded|p2,10||Ordovician|||||||
3624|Carlo Sandstone|44309|2|Defined|Tb.1,p5,12,17,map||Ordovician|Fossils. Conformably overlies Nora Formation. Overlain by Mithaka Formation to south. Unit of Toko Group.||||||
3624|Carlo Sandstone|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
3624|Carlo Sandstone|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
3624|Carlo Sandstone|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
3624|Carlo Sandstone|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||11-FEB-09
3624|Carlo Sandstone|44469|2|Defined|p.10, opp.p.6, Tb.I||Ordovician|(F53-12). See also p.15,16,Tb.2. Conf.on Nora Fm. Fossils.Mid.Ordovician. Unit of Toko Group.||||||
3624|Carlo Sandstone|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
3624|Carlo Sandstone|44848|14|Not recorded|p111|||||||||
3624|Carlo Sandstone|44852|14|Not recorded|p71||Ordovician|Middle Ordovician||||||
3624|Carlo Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
3624|Carlo Sandstone|45052|3|Fully described|p128|||Middle Ordovician||||||
3624|Carlo Sandstone|45118|6|Mentioned|p2,3|||||||||
3624|Carlo Sandstone|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
3624|Carlo Sandstone|46841|4|Described|p97|||||||||
3624|Carlo Sandstone|46897|6|Mentioned|Fig.3.|||||||||
3624|Carlo Sandstone|46940|6|Mentioned|p57|||||||||
3624|Carlo Sandstone|46959|6|Mentioned|Table 1|||||||||
3624|Carlo Sandstone|46973|6|Mentioned|Fig.3|||||||||
3624|Carlo Sandstone|47024|6|Mentioned|p1|||||||||
3624|Carlo Sandstone|48901|14|Not recorded|Not recorded||Ordovician|M. Ordovician. pt. Toko Group.||||||
3624|Carlo Sandstone|49027|4|Described|p18|||||||||
3624|Carlo Sandstone|60122|3|Fully described|p32-33, p10 Tb. 1|Middle Ordovician|Middle Ordovician|Of Toko Gp. Resistant, red-brown, well-sorted, fine to medium qtz sst and minor feldspathic sst, with prominent clay-pellet bed at base. Conformably overlies Nora Fm; unconf.underlies Mithaka Fm. and Poodyea Fm. Max. thick: 190m. See also p4-5, p28 Fig 33||||||
3624|Carlo Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Toko Group.  Quartzose and minor feldspathic sandstone.  Overlies the Nora Formation.||||||23-DEC-09
3624|Carlo Sandstone|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose and minor feldspathic sandstone. Geological Province: southern Georgina Basin.||||||12-OCT-05
3624|Carlo Sandstone|64068|3|Fully described|p77, p19|Late Ordovician|Late Ordovician|Forms resistant plateau capping. Conformably and gradationally overlies Nora Formation. Conformably and gradationally overlain by Mithaka Formation, or unconformably by Cravens Peak beds.||Of Toko Group.||Conformably and gradationally overlies Nora Formation. Conformably and gradationally overlain by Mithaka Formation, or unconformably by Cravens Peak beds.|Fine to medium quartz sandstone; minor feldspathic sandstone and siltstone; basal clay-pellet bed.|04-APR-12
3624|Carlo Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
3624|Carlo Sandstone|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|65489|5|Briefly described|p125|Ordovician|Ordovician|Georgina Basin.||||Overlies Nora Formation. Is overlain by Mithaka Formation.||
3624|Carlo Sandstone|67323|5|Briefly described|p83, p90, p92 Fig.12.2, p96|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. West Toko Syncline, Georgina Basin. Appears as Carlo Formation on p90 where its aquifer propeties are described.||Toko Group.||Overlies Nora Formation. Is overlain by Mithaka Formation.|Quartzose arenite, siltstone.|
3624|Carlo Sandstone|67402|6|Mentioned|p25, p25 tbl RRM3|Darriwillian|Castlemanian|Georgina Basin, West Toko Syncline. Maximum thickness of 178m. Assessed to be a potential unconventional seal for carbon dioxide storage. Misspelt as the Carlo Formation on p214. Deposited in a high energy barrier beach environment. See also p165 tbl LPB1, p213-p217. ||||Overlies the Nora Formation. Conformably overlain by the Mithaka Formation.|Quartzose sandstone.|
3624|Carlo Sandstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Nora Formation. Is overlain by Mithaka Formation.||12-JUL-16
3624|Carlo Sandstone|69443|4|Described|p28:7, 27-29, 46|Late Ordovician|Middle Ordovician|Casey in Smith (1963). Southern Georgina Basin. Resistant, range-capping unit. 22-190m thick. Sparse body fossils are listed; ichnofossils are relatively common and diverse throughout. Darriwilian to Sandbian age. Potential petroleum reservoir, sealed by Mithaka Formation.||Toko Group.||Conformably and gradationally overlies Nora Formation. Is overlain conformably and gradationally by Mithaka Formation, or unconformably by Cravens Peak beds.|Medium to thick beds of fine to medium quartz sandstone, and minor feldspathic sandstone and siltstone; various current features. Has a prominent basal clay-pellet bed.|12-JUL-16
3624|Carlo Sandstone|69458|5|Briefly described|p42:20|||Georgina Basin. Clasts of this unit occur in the Poodyea Formation.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
3624|Carlo Sandstone|69591|4|Described|p87, p95|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Up to 90m thick. Contains a sparse fossil fauna. Shallow coastal conditions associated with shoaling or barrier island formation are inferred.||Toko Group.||Conformably and transitionally overlies Nora Formation. Is overlain conformably and transitionally by Mithaka Formation.|Fine to medium quartz sandstone. Shows cross-stratification, flute casts and gouge marks, ichnofossils and bioturbation.|
3624|Carlo Sandstone|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
3624|Carlo Sandstone|69673|5|Briefly described|p114 fig 92, p118, p119 fig 94, p136|Ordovician|Ordovician|Up to 174m thick. Some reservoir potential.||Toko Group||Overlies Nora Formation, overlain by Mithaka Formation|Thickly to medium bedded, fine to medium grained quartz sandstone; minor siltstone.|
3624|Carlo Sandstone|70380|6|Mentioned|p745|Sandbian|Sandbian|Southern Georgina Basin.||||||
3631|Carlyon Creek Complex|22847|3|Fully described|p 46|Late Ordovician|Ordovician|||||||
3631|Carlyon Creek Complex|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 465.||||||
3631|Carlyon Creek Complex|42633|5|Briefly described|Table 1 P9|||NOT a variation on Carlyon Granodiorite, Antarctica. Reserved as Carlyon Creek Granite, May 1989.||||||
3631|Carlyon Creek Complex|42750|2|Defined|p38|Middle Ordovician|Early Ordovician|||||||
3631|Carlyon Creek Complex|43093|4|Described|Appendix 1|Late Ordovician|Ordovician|Middle Ordovician to Late Ordovician||||||
3631|Carlyon Creek Complex|43259|4|Described|Appendix 1,p49.||Ordovician|||||||
3631|Carlyon Creek Complex|43934|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
3631|Carlyon Creek Complex|62074|6|Mentioned|p3||||||||Comprises a mixture of several granitoid types, some with dioritic and gabbroic compositions.|
3631|Carlyon Creek Complex|62521|5|Briefly described|p10, p26|Middle Ordovician|Late Cambrian|Of the Lavery Creek Supersuite. Geological Province: Ravenswood Batholith. Produced by a mingling of mafic and felsic magmas.||||||21-DEC-07
3649|Carney Creek Quartz Diorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37. Reserved as Carney Creek Diorite.||||||
3649|Carney Creek Quartz Diorite|43029|2|Defined|p15||Devonian|see also Fig.2,p16||||||
3649|Carney Creek Quartz Diorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
3649|Carney Creek Quartz Diorite|43213|4|Described|p96-97, p102-104, p116-121, p175, p179|Devonian|Devonian|See also p208, p213, p231, p240. Type area described. Component of the Retreat Batholith. Similar to Stevenson Quartz Monzodiorite. Geochemistry, modal analyses detailed. Geophysics detailed.||||Intrudes Anakie Metamorphic Group. Is faulted against Silver Hills Volcanics.|Dark grey to greenish grey, fine- to medium-grained, variable in composition, from biotite-hornblende quartz diorite and quartz monzodiorite to hornblende diorite.|
3649|Carney Creek Quartz Diorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Dark to light grey, fine to medium-grained, biotite-hornblende quartz diorite, quartz monzodiorite and diorite.|
3679|Carrara Range Group|24442|5|Briefly described|p22 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||07-NOV-08
3679|Carrara Range Group|38835|6|Mentioned|p164|||||||||
3679|Carrara Range Group|39338|6|Mentioned|p351|||||||||
3679|Carrara Range Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes: Top Rocky Rhyolite, Mitchiebo Volcanics and Don Creek Sandstone.||||||03-AUG-06
3679|Carrara Range Group|39497|4|Described|p7|||||||||
3679|Carrara Range Group|39925|6|Mentioned|p331|||||||||
3679|Carrara Range Group|40840|6|Mentioned|Map legend|||||||||
3679|Carrara Range Group|45166|4|Described|p27|||Mention p8.||||||03-AUG-06
3679|Carrara Range Group|49018|2|Defined|p1|Carpentarian|Carpentarian|||||||
3679|Carrara Range Group|62659|5|Briefly described|Map Legend|Statherian|Statherian|||||||
3679|Carrara Range Group|65337|4|Described|p6 Fig.3,  p10 Table 3, pp11-12. |Paleoproterozoic|Paleoproterozoic|2500 m thick. Leichhardt Superbasin; Lawn Hill Platform. Correlative of Peters Creek Volcanics, Tawallah Group, Eastern Creek Volcanics and Fiery Creek Volcanics. Lower part has sediments and flood basalts; upper part, rhyolitic volcanics and epiclastics.|c.1790-1720 Ma.||Includes Don Creek Sandstone, Mitchiebo Volcanics, Gator Sandstone and Top Rocky Rhyolite.|Unconformably overlies Murphy Metamorphics and Connelly Volcanics. Is overlain unconformably by Surprise Creek Formation.|Basal fluvial quartzose sandstone and flood basalt succession, overlain unconformably by subaerial rhyolitic volcanic and proximal alluvial epiclastic rocks.|
3679|Carrara Range Group|69417|6|Mentioned|p2:5|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
3679|Carrara Range Group|69433|5|Briefly described|p18:2-3, 5-7, 10|Statherian|Statherian|Southern succession, Lawn Hill Platform. Unconformably overlies the Murphy Province succession.|||Don Creek, Gator Sandstones; Mitchiebo Volcanics; Top Rocky Rhyolite.|Is overlain unconformably by Surprise Creek Formation and McNamara Group. Correlative of Peters Creek Volcanics. Equivalent to the Tawallah Group.||12-JUL-16
3679|Carrara Range Group|69673|6|Mentioned|p3 fig 2, p51|Statherian|Statherian||||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone|||
3679|Carrara Range Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin, and Lawn Hill Platform, Mount Isa Inlier.||||Overlain unconformably by McNamara Group. Equivalent to Peters Creek Volcanics, correlable to Weberer Granite anf Fiery Creek Volcanics.||
3679|Carrara Range Group|72526|5|Briefly described|p5, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian||||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics and Don Creek Sandstone.|||
3679|Carrara Range Group|72527|4|Described|p1, p3,p7, p87, p147-148,p169, p193-194|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin.|||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics and Don Creek Sandstone.|Unconformably underlies Surprise Creek Formation and is laterally equivalent to Peters Creek Volcanics.|Includes Rhyolite clasts; the remaining clasts are dominated by sandstone, siltstone, mudstone, layered chert, milky vein quartz and possibly small fragments of mafic volcanics.|
3679|Carrara Range Group|72912|5|Briefly described|p5 Fig.3, p25-26.|Statherian|Statherian|Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Min age from dating Top Rocky Rhyolite, at the top of the Group.|min age c.1725 Ma.||Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone.|Shown as partially overlying Myally Subgroup and partially and unconformably underlying Fiery Creek Volcanics and Bigie Formation.||
3679|Carrara Range Group|72919|6|Mentioned|p3, p5|Paleoproterozoic|Paleoproterozoic||||Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone|Unconformably overlain by Surprise Creek Formation.||
3679|Carrara Range Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Calvert Superbasin. Age range indicated to be quite uncertain, with ? above and below.|||Drummond Formation, Surprise Creek Formation*, Top Rocky Rhyolite, Gator Sandstone, Mitchlebo Volcanics, Don Creek Sandstone.|||
3679|Carrara Range Group|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
3691|Carriers Well Formation|23032|4|Described|p16||Late Ordovician|||||||
3691|Carriers Well Formation|23423|6|Mentioned|p263|||Broken River Province.||||||
3691|Carriers Well Formation|23424|4|Described|Table 8.1 Fig 8.2/8.3 p332.||Ashgill|Age: Late Ordovician (Ashgill); corals & conodonts. Similar to Fork Lagoon Beds in Anakie Inlier. Faulted against Gray Ck Complex along Gray Ck Flt. Possibly underlain to E by Everetts Ck Volcanics. Camel Creek Subprovince.||||||
3691|Carriers Well Formation|23430|5|Briefly described|p470 + p478||Late Ordovician|Broken River Province.||||||
3691|Carriers Well Formation|23431|5|Briefly described|p541|||||||||
3691|Carriers Well Formation|23619|5|Briefly described|p35 Table 1||Late Ordovician|Broken River Province.||||||
3691|Carriers Well Formation|41260|3|Fully described|p10|||See also p143. Described p142.||||||04-MAY-15
3691|Carriers Well Formation|41675|6|Mentioned|p52|||||||||
3691|Carriers Well Formation|41679|6|Mentioned|Fig.1|||||||||
3691|Carriers Well Formation|41719|6|Mentioned|Fig.1|||||||||
3691|Carriers Well Formation|41739|6|Mentioned|Fig.1|||||||||
3691|Carriers Well Formation|42031|5|Briefly described|Fig.4 P761|||||||||
3691|Carriers Well Formation|42279|5|Briefly described|p27|||||||||
3691|Carriers Well Formation|42692|5|Briefly described|map legend|Ordovician||||||||
3691|Carriers Well Formation|42693|5|Briefly described|map legend|Ordovician||||||||
3691|Carriers Well Formation|42747|6|Mentioned|p36|||||||||
3691|Carriers Well Formation|42752|5|Briefly described|p45|||see also Fig.2 P46, Fig.3 P47.||||||
3691|Carriers Well Formation|42933|2|Defined|p15|Late Ordovician||||||||
3691|Carriers Well Formation|43083|6|Mentioned|p34|||Contains ooids.||||||17-JUN-09
3691|Carriers Well Formation|43113|4|Described|Table 1 p21||Late Ordovician|||||||
3691|Carriers Well Formation|43213|4|Described|p9, p59-60|Late Ordovician|Late Ordovician|Near Greenvale, Broken River Province. Has a dual provenance for its sediments. Ashgillian age.||||Overlies Everetts Creek Volcanics. Faulted against Gray Creek Complex. Correlated with Fork Lagoons beds.|Contains compositionally mature quartzose arenite intercalated with abundant volcaniclastic arenite and conglomerate; sporadic oolitic limestone.|
3691|Carriers Well Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
3691|Carriers Well Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
3691|Carriers Well Formation|43625|6|Mentioned|p21|||||||||
3691|Carriers Well Formation|50202|5|Briefly described|Map legend|Ordovician|Ordovician|Volcaniclastic arenite and breccia, siltstone, mudstone, chert.||||||
3691|Carriers Well Formation|61727|5|Briefly described|p942 Fig.1|Early Silurian|Late Ordovician|Geological Province: Broken River Province/Camel Creek Subprovince.||||||
3691|Carriers Well Formation|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Broken River Province/Camel Creek Subprovince.||||||
3691|Carriers Well Formation|65756|5|Briefly described|p26|Late Ordovician|Late Ordovician|Camel Creek Subprovince. Part of island arc sequence.||||||
3691|Carriers Well Formation|67455|5|Briefly described|p593.|Late Ordovician|Late Ordovician|Western margin of Camel Creek Subprovince. Accreted in Early Silurian contractional deformation.|||||Subduction-related, calc-alkaline island arc volcaniclastics.|
3691|Carriers Well Formation|67848|4|Described|p1, p2, pp4-6, pp7-16. |Late Ordovician|Late Ordovician|Western edge of Camel Creek Subprovince. Oldest rocks in the Subprovince. Part of an arc assemblage in collisional accretion. Melange development is characteristic. Maximum depositional age from detrital zircons. Geochemistry, and web address for geochemical data, are given. Correlative of Fork Lagoon beds.|454 +/- 13 Ma (Henderson et al. 2011) LA-ICPMS|||Has a transitional contact with Everetts Creek Volcanics.|Chert, shale, volcaniclastic and quartzose sandstones, micritic and oolitic limestone, volcanic breccia, basaltic/andesitic/dacitic flows (sporadically pillowed), dolerite dykes and peperite. Discontinuous limestone bodies are characteristic.|04-MAY-15
3691|Carriers Well Formation|68336|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician?|Camel Creek Subprovince, Broken River Province. The (commonly oolitic) limestone facies is mapped separately.|||||Volcaniclastic sandstone and breccia (debris flows and pyroclastics), siltstone, mudstone and chert; local quartzose sandstone and limestone (commonly oolitic).|
3691|Carriers Well Formation|68341|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician?|Camel Creek Subprovince, Broken River Province. The (commonly oolitic) limestone facies is mapped separately.|||||Volcaniclastic sandstone and breccia (debris flows and pyroclastics), siltstone, mudstone and chert; local quartzose sandstone and limestone (commonly oolitic).|
3691|Carriers Well Formation|68344|5|Briefly described|Map legend.|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.|||||Volcaniclastic arenite and breccia (debris flows and pyroclastics), siltstone, mudstone and chert; local quartzose arenite and limestone (commonly oolitic).|
3691|Carriers Well Formation|68553|6|Mentioned|Map legend; schematic diagram.|Silurian|Ordovician|Broken River Province. This unit, as well as Pelican Range and Wairuna Formations, Tribute Hills Arenite and Everetts Creek Volcanics, are all mapped under the symbol, OSb.||||||
3691|Carriers Well Formation|68576|5|Briefly described|Q_11: p34-35, p37-38|||W margin of the Camel Creek Subprovince, S of Greenvale. Probably debris flow deposits. Folded. Henderson et al. (2011) suggest that this unit was part of a Late Ordovician island arc that may have been accreted in the Early Silurian.||||Faulted against the Gray Creek Complex.|A strongly disrupted assemblage of volcanic breccia (volcanics, chert and siltstone in a chloritic matrix) and volcanilithic turbiditic sandstone, with pods of oolitic limestone up to 10m long.|
3691|Carriers Well Formation|68731|6|Mentioned|p221|||||||||
3691|Carriers Well Formation|68822|6|Mentioned|p335, p336 Fig.11||||||||Calcalkaline and tholeiitic basaltic to dacitic volcanics.|
3691|Carriers Well Formation|69030|5|Briefly described|p6|Ordovician|Ordovician|Camel Creek Subprovince (Broken River Province).|454 +/- 13 Ma (SHRIMP).|||||
3691|Carriers Well Formation|69079|6|Mentioned|p5|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.||||||
3691|Carriers Well Formation|69592|4|Described|p251 Fig.4.35, p252, p255-257, p259|Late Ordovician|Late Ordovician|See also p268, p272, p278. Western edge of Camel Creek Subprovince, Broken River Province. Part of the Lucky Springs Assemblage. Measured section of the type section nominated by Withnall et al. (1988) and Withnall (1993) is dominated by mafic flows and epiclastic rocks. Seen as a facies variant of Everetts Creek Volcanics. Geochemical plots and discussion. Island arc deposits close to a continental margin. Contains Katian fossils.|454 +/- 13 Ma (Henderson et al., 2011).|||Gradationally overlies Everetts Creek Volcanics.|Includes chert, shale, volcaniclastic and quartzose sandstone, micritic and oolitic limestone, volcanic breccia, basaltic, andesitic and dacitic flows and/or sills and peperite. Discontinuous limestone bodies are characteristic.|
3691|Carriers Well Formation|71091|5|Briefly described|p146-147, p164|||Apparently this unit is now interpreted as allochthonous limestones within the Wairuna Formation: see Zhen et al. (2015). Also referred to informally as Carriers Well formation and the Carriers Well limestone.|||||Includes limestones.|
3701|Carters Bore Rhyolite|22665|5|Briefly described|P221, Table1||Statherian|Age of unit is 1678+/2 Ma||||||
3701|Carters Bore Rhyolite|22680|6|Mentioned|83|||||||||
3701|Carters Bore Rhyolite|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
3701|Carters Bore Rhyolite|23396|5|Briefly described|p419|Statherian|Statherian|Age. 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23397|5|Briefly described|p469|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23398|5|Briefly described|p449|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23408|5|Briefly described|p513 Fig.2, p514 Fig. 4|||Of McNamara Group.||||||02-APR-07
3701|Carters Bore Rhyolite|23466|5|Briefly described|p268 Fig.2|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1678+/-2 Ma||||||02-NOV-07
3701|Carters Bore Rhyolite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
3701|Carters Bore Rhyolite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3701|Carters Bore Rhyolite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite.  Comagmatic and mainly intrusive.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
3701|Carters Bore Rhyolite|30534|6|Mentioned|p300|||See also p305.||||||03-AUG-06
3701|Carters Bore Rhyolite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|32660|5|Briefly described|Table 5|||||||||
3701|Carters Bore Rhyolite|32959|6|Mentioned|Fig.21|||||||||
3701|Carters Bore Rhyolite|33900|5|Briefly described|p13|||||||||
3701|Carters Bore Rhyolite|35074|6|Mentioned|Fig.2|||||||||
3701|Carters Bore Rhyolite|35167|2|Defined|p155|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|35286|4|Described|p145|||||||||
3701|Carters Bore Rhyolite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
3701|Carters Bore Rhyolite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|36548|6|Mentioned|p513|||||||||
3701|Carters Bore Rhyolite|37217|6|Mentioned|p650|||||||||
3701|Carters Bore Rhyolite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|37459|6|Mentioned|p423|||||||||
3701|Carters Bore Rhyolite|37462|4|Described|Table4.VII|||See also p244.||||||03-AUG-06
3701|Carters Bore Rhyolite|37565|5|Briefly described|p11|||||||||
3701|Carters Bore Rhyolite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|38234|4|Described|p104|||||||||
3701|Carters Bore Rhyolite|38237|6|Mentioned|p125|||||||||
3701|Carters Bore Rhyolite|38276|6|Mentioned|Fig.1|||||||||
3701|Carters Bore Rhyolite|38348|6|Mentioned|p6|||||||||
3701|Carters Bore Rhyolite|38350|4|Described|p14|||||||||
3701|Carters Bore Rhyolite|38560|6|Mentioned|p115|||||||||
3701|Carters Bore Rhyolite|38584|6|Mentioned|p17|||||||||
3701|Carters Bore Rhyolite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|38834|6|Mentioned|p162|||||||||
3701|Carters Bore Rhyolite|39202|6|Mentioned|p242|||||||||
3701|Carters Bore Rhyolite|39338|6|Mentioned|p352|||||||||
3701|Carters Bore Rhyolite|39445|5|Briefly described|Table 2|||Age: 1678 Ma. See also p36 and p41.||||||03-AUG-06
3701|Carters Bore Rhyolite|39497|6|Mentioned|p19|||||||||
3701|Carters Bore Rhyolite|39925|6|Mentioned|p335|||||||||
3701|Carters Bore Rhyolite|39934|6|Mentioned|Fig.3|||||||||
3701|Carters Bore Rhyolite|40105|6|Mentioned|p310|||||||||
3701|Carters Bore Rhyolite|40221|6|Mentioned|p6|||||||||
3701|Carters Bore Rhyolite|40811|6|Mentioned|p318|||||||||
3701|Carters Bore Rhyolite|40840|6|Mentioned|Map legend|||||||||
3701|Carters Bore Rhyolite|41277|6|Mentioned|Fig.5|||||||||
3701|Carters Bore Rhyolite|41298|6|Mentioned|Map legend|Carpentarian||||||||
3701|Carters Bore Rhyolite|41307|6|Mentioned|p13|||||||||
3701|Carters Bore Rhyolite|41381|6|Mentioned|p323|||||||||
3701|Carters Bore Rhyolite|41721|6|Mentioned|p28|||Correlated with Peters Creek Volcanics.||||||01-AUG-07
3701|Carters Bore Rhyolite|41791|6|Mentioned|p272|||||||||
3701|Carters Bore Rhyolite|41957|6|Mentioned|p68|||||||||
3701|Carters Bore Rhyolite|41978|6|Mentioned|p502|||||||||
3701|Carters Bore Rhyolite|41979|6|Mentioned|p514|||||||||
3701|Carters Bore Rhyolite|42367|5|Briefly described|p17|||Dated at 1678 Ma||||||
3701|Carters Bore Rhyolite|42565|5|Briefly described|Table 1 P5, P4|||||||||
3701|Carters Bore Rhyolite|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1880Ma. Porphyritic felsic volcanics.||||||09-FEB-09
3701|Carters Bore Rhyolite|43608|6|Mentioned|Fig.11,p11|||||||||
3701|Carters Bore Rhyolite|43615|6|Mentioned|p13|||Age. 1680+/-3 Ma. (SHRIMP).||||||03-AUG-06
3701|Carters Bore Rhyolite|44195|6|Mentioned|p350|||||||||
3701|Carters Bore Rhyolite|45161|6|Mentioned|p12|||||||||
3701|Carters Bore Rhyolite|45162|6|Mentioned|p11|||See also p45.||||||03-AUG-06
3701|Carters Bore Rhyolite|45166|4|Described|p27|||||||||
3701|Carters Bore Rhyolite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
3701|Carters Bore Rhyolite|46919|6|Mentioned|p222|||||||||
3701|Carters Bore Rhyolite|46960|6|Mentioned|p216|||||||||
3701|Carters Bore Rhyolite|47083|5|Briefly described|p11|||Overlain by Surprise Crk Fm, Mount Isa Group and McNamara Group; underlain by Haslingden Gp, and Quilalar Fm - unconformable.||||||03-AUG-06
3701|Carters Bore Rhyolite|48997|6|Mentioned|Fig.3|||||||||
3701|Carters Bore Rhyolite|49041|5|Briefly described|Table 1|||||||||
3701|Carters Bore Rhyolite|50100|6|Mentioned|p13 Fig.4|Statherian|Statherian|Geological Province: Western Fold Belt Province.||||||
3701|Carters Bore Rhyolite|50536|5|Briefly described|p1.5, 7.1, 8.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite. Age: 1678 +/- 2Ma (U-Pb-Shrimp).||||||07-NOV-08
3701|Carters Bore Rhyolite|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
3701|Carters Bore Rhyolite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic rhyolite.||||||
3701|Carters Bore Rhyolite|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
3701|Carters Bore Rhyolite|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Age: 1680-1670Ma. Felsic magmatism.||||||
3701|Carters Bore Rhyolite|61929|5|Briefly described|p128 Fig. 2|||||||||
3701|Carters Bore Rhyolite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. See also p196.||||||
3701|Carters Bore Rhyolite|62535|6|Mentioned|p672-673|Statherian|Statherian||1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Coeval with Sybella Granite. Age: ~1675-1670Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
3701|Carters Bore Rhyolite|63023|5|Briefly described|p1035|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: ca 1700Ma. Geological Province: Western Fold Belt. ||||||07-NOV-08
3701|Carters Bore Rhyolite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|||||||
3701|Carters Bore Rhyolite|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt. |Between c.1700 and 1670 Ma.|||Is intruded by Sybella Granite.||
3701|Carters Bore Rhyolite|63866|5|Briefly described|p58||||1678 +/- 2 Ma (Page and Sweet, 1998)|||||
3701|Carters Bore Rhyolite|64250|6|Mentioned|p16 fig 6, p11 fig 3, p21|||Western Fold Belt, Mount Isa Inlier. Shallow intrusion.|1678 +/- 2 Ma|||||
3701|Carters Bore Rhyolite|64744|6|Mentioned|p353 Fig.4, p358.|Statherian|Statherian|Mount Isa Basin.|1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|64834|5|Briefly described|p32|||Regionally occurring extrusion.|1678+/-2 Ma|||||
3701|Carters Bore Rhyolite|65228|6|Mentioned|pp20-21, Fig.04.|Statherian|Statherian|Mount Isa region.|1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|65396|5|Briefly described|p16, p82, p175, p190, p193, p241|Statherian|Statherian|Lawn Hill Platform, Western Fold Belt.|1678 +/- 2 Ma||||Rhyolite and mafic volcanics.|
3701|Carters Bore Rhyolite|66800|6|Mentioned|p933.|||Western Fold Belt, Mount Isa Inlier. Correlated with younger parts of Eastern Fold Belt on basis of SHRIMP data (Page and Sun 1998).||||||
3701|Carters Bore Rhyolite|66844|6|Mentioned|p245|Statherian|Statherian|Mount Isa region. Age from SHRIMP dating.|1678+\-2 Ma|||||
3701|Carters Bore Rhyolite|67323|5|Briefly described|GIS attrib tbl, p12, p34, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Isa Superbasin. Sybella/Leichhardt River Domain, Mount Isa Inlier. Shown as separating Lower and Upper parts of the Warrina Park Quartzite.|1678 +/- 2 Ma.|||Sybella Batholith rocks are same age.|Porphyritic rhyolite, minor basalt.|
3701|Carters Bore Rhyolite|68021|6|Mentioned|p135 fig 4, p136|Statherian|Statherian|Calvert Superbasin, Western Succession.|1678 Ma|||||
3701|Carters Bore Rhyolite|68146|6|Mentioned|p194||||c.1678 Ma (Page and Sweet, 1998).|||||
3701|Carters Bore Rhyolite|68732|5|Briefly described|p165 Fig.3, p167|Statherian|Statherian|Correlative with the Eastern Creek Volcanics. Igneous crystallisation ages.|1670 +/- 3, 1678 +/- 2 Ma|||||
3701|Carters Bore Rhyolite|69222|5|Briefly described|p222 Fig.2, p223|Statherian|Statherian|Leichhardt River Fault Trough.|1678 +/- 2 Ma (Page and Sweet, 1998).|||Overlies Bigie Formation, Fiery Creek Volcanics, overlain by Surprise Creek Formation||09-FEB-18
3701|Carters Bore Rhyolite|69591|5|Briefly described|p41, p43, p56, p107|||Mount Isa Province. Coeval with emplacement of the Sybella Granite at ~1678 Ma.|1678 +/- 3 Ma (Page and Sweet, 1998).||||Porphyritic rhyolite, minor basalt.|
3701|Carters Bore Rhyolite|70283|6|Mentioned|p25 |Statherian|Statherian|West of the Mount Isa fault zone.|~ 1680 Ma (Page, 1983).|||||14-FEB-18
3701|Carters Bore Rhyolite|70897|6|Mentioned|p41|||Source of 1680 Ma zircons in Mullera Formation.||||||
3701|Carters Bore Rhyolite|71369|6|Mentioned|p4|||||||||
3701|Carters Bore Rhyolite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1678+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
3701|Carters Bore Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon igneous crystallisation age.|1678+/-2 Ma|||Shown as unconformably and conformably overlying lower Gunpowder Creek Formation.||
3701|Carters Bore Rhyolite|72889|5|Briefly described|p20, p23-25, p28.|Statherian|Statherian|Magmatic age from Page and Sweet (1998). Co-magmatic with Sybella Batholith granites, and dolerite reported herein as 1674+/-2.4 Ma.|1678 +/- 2 Ma.|||Co-magmatic with dolerite reported herein.||
3701|Carters Bore Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1678 +/- 2 Ma|||Shown as unconformably overlying lower Gunpowder Creek Formation and older than Sybella Granite.||
3701|Carters Bore Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1678 +/- 2 Ma (see Fig.1.2)|||||
3701|Carters Bore Rhyolite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
3701|Carters Bore Rhyolite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1678+/-2 Ma crystallisation age||||Felsic extrusives.|
3756|Castle Hill Granite|23422|5|Briefly described|p219 Table 6.12|||Of Woodstock Suite.||||||
3756|Castle Hill Granite|23509|5|Briefly described|Map Legend||Permian|||||||
3756|Castle Hill Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 146. I-Type.||||||
3756|Castle Hill Granite|23893|5|Briefly described|p21|Permian|Permian|||||||
3756|Castle Hill Granite|40607|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3756|Castle Hill Granite|43259|4|Described|Appendix 1,p25.||Permian|||||||
3756|Castle Hill Granite|69593|5|Briefly described|p494, p513|Permian|Permian|Townsville region: Lolworth Batholith and Charters Towers Province. Sm-Nd isotope data tabulated.|~285-265 Ma (Rienks, 1997).|Woodstock Suite.|||I-type.|
3769|Casuarina beds|24615|5|Briefly described|CD|Tertiary|Tertiary|[Tc].  Mudstone, siltstone, shale, oil shale, sandstone, minor lignite, conglomerate and dolomite.||||||
3769|Casuarina beds|36210|3|Fully described|p263|||Variation of Casuarina-Narrows? Intended as informal name.||||||
3769|Casuarina beds|36243|6|Mentioned|Table 11A|||||||||
3769|Casuarina beds|36937|6|Mentioned|p229|||||||||
3769|Casuarina beds|39445|6|Mentioned|Chart 10,2|||Correlation||||||
3769|Casuarina beds|39943|6|Mentioned|Table 13A|||||||||
3769|Casuarina beds|41576|4|Described|p20|||See also Table 1||||||
3769|Casuarina beds|41577|6|Mentioned|Map legend|Tertiary||||||||
3769|Casuarina beds|41922|4|Described|Table 1, P8|||||||||
3769|Casuarina beds|50209|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
3769|Casuarina beds|50212|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
3769|Casuarina beds|60557|5|Briefly described|p19 Fig. 5b, p28|Tertiary|Tertiary|||||||
3769|Casuarina beds|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||03-MAR-10
3769|Casuarina beds|67402|5|Briefly described|p165 tbl LPB1, p184|Eocene|Eocene|Casuarina Basin. Interpreted to have been deposited in a fresh-water lake/swamp system. |||||Mudstone, siltstone, shale, sandstone, oil shale, minor lignite, conglomerate and dolomite also.|
3769|Casuarina beds|68008|4|Described|p273-275, p297|Oligocene|Eocene|Dunstan (1913) considered the sedimentary fill of the Casuarina Basin would be similar to that in The Narrows Graben. The name Casuarina beds was applied to the sequence in GSQ Rockhampton 1, drilled in 1978. Freshwater, lacustrine deposits; 561.5m thickness measured, elsewhere up to 900m indicated. Contains oil shale intervals; has been a source of salt (from brines) for many years.||||Unconformably overlies Erebus beds, Mount Alma Formation, Rockhampton and Berserker Groups. The lower part is (tentatively) correlated with The Narrows Group.|Basal conglomerate and sandstone, succeeded by mudstone, silty mudstone and oil shale with thin dolomite beds, topped by interbedded siltstone and mudstone.|
3769|Casuarina beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, 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.||||||
3769|Casuarina beds|68679|6|Mentioned|p312-313|Paleogene|Paleogene|Northern New England Orogen.||||||
3769|Casuarina beds|69599|5|Briefly described|p586, p589|Oligocene|Eocene|Casuarina Basin. 561m thick in GSQ Rockhampton 1 well; elsewhere may be up to 900m thick. Fluvial to ponded lacustrine sediments. RELATED UNITS (continued): Also correlated with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; Flinders Dolomite; see COMMENTS for more.|Mudstone, siltstone, shale, oil shale, sandstone with minor conglomerate and dolomite.|
3793|Catherine Sandstone|13516|5|Briefly described|p145 fig 3, p146 fig 4, p152, p156|Late Permian|Late Permian|From Denison Trough, Bowen Basin. Age APP5004||||||
3793|Catherine Sandstone|22601|6|Mentioned|413|Permian|Permian|Geol province Bowen Basin. Underlying unit Ingelara Formation||||||
3793|Catherine Sandstone|22872|6|Mentioned|p535, Fig.1 p536|||||||||
3793|Catherine Sandstone|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
3793|Catherine Sandstone|22980|6|Mentioned|p251|||||||||
3793|Catherine Sandstone|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
3793|Catherine Sandstone|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
3793|Catherine Sandstone|24077|5|Briefly described|p410 Tb. 2|Early Permian|Early Permian|Of the Gebbie Subgroup.  Feldspathitic lithic quartz sandstone, fine grained well sorted minor conglomerate.  Max. thickness: 150m.  Geological Province: Bowen Basin.||||||
3793|Catherine Sandstone|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: ~259Ma.  Geological Province: Bowen Basin.||||||
3793|Catherine Sandstone|29391|6|Mentioned|Table 3|||See P18.||||||
3793|Catherine Sandstone|29393|6|Mentioned|Table 2|||Permian.||||||
3793|Catherine Sandstone|29409|6|Mentioned|Table 1|||Postulated Crocker Sandstone equivalent.||||||
3793|Catherine Sandstone|29410|6|Mentioned|p274|||Geological map. Permian.||||||
3793|Catherine Sandstone|29721|6|Mentioned|p65|||||||||
3793|Catherine Sandstone|30340|6|Mentioned|Table 3|||||||||
3793|Catherine Sandstone|30341|5|Briefly described|p136|||Lower Permian age||||||
3793|Catherine Sandstone|30449|6|Mentioned|p5|||Brachiopods. See also P12,13,14||||||
3793|Catherine Sandstone|30450|6|Mentioned|Table 1|||Permian age||||||
3793|Catherine Sandstone|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
3793|Catherine Sandstone|30545|6|Mentioned|Fig.2|||Permian. See also P23||||||
3793|Catherine Sandstone|30546|6|Mentioned|p107|||Lower Permian||||||
3793|Catherine Sandstone|30826|6|Mentioned|Fig.1|||||||||
3793|Catherine Sandstone|30914|6|Mentioned|Map legend|Permian|Permian|||||||
3793|Catherine Sandstone|31115|6|Mentioned|p32|||Permian||||||
3793|Catherine Sandstone|31120|4|Described|p151|||See also p152. Correlative.||||||16-NOV-15
3793|Catherine Sandstone|31305|6|Mentioned|p573|||||||||
3793|Catherine Sandstone|31531|6|Mentioned|p11|||||||||
3793|Catherine Sandstone|32139|6|Mentioned|p582|||See Table||||||
3793|Catherine Sandstone|32577|5|Briefly described|p23|||L.Perm. See also P24,33.||||||
3793|Catherine Sandstone|32578|6|Mentioned|p350|||Stratigraphy||||||
3793|Catherine Sandstone|32689|6|Mentioned|Fig.2|||Refers Power (1967)||||||
3793|Catherine Sandstone|32840|5|Briefly described|p30|||Stratigraphy & biostratigraphy. See also Fig.1||||||
3793|Catherine Sandstone|32945|6|Mentioned|p76|||See also P811,82,89,91 & Fig.3. Correlation||||||
3793|Catherine Sandstone|33366|6|Mentioned|Fig.3|||Perm.||||||
3793|Catherine Sandstone|33701|6|Mentioned|Fig.1|||Kungurian||||||
3793|Catherine Sandstone|33745|6|Mentioned|p204|||See also Figs 6 & 7||||||
3793|Catherine Sandstone|34132|6|Mentioned|p2|||Upper Permian||||||
3793|Catherine Sandstone|34138|6|Mentioned|Cor.Chart|||Kungurian||||||
3793|Catherine Sandstone|34390|4|Described|Table 2|||Permian. Gebbie Subgroup.||||||
3793|Catherine Sandstone|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
3793|Catherine Sandstone|34568|6|Mentioned|p222|||Fauna||||||
3793|Catherine Sandstone|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
3793|Catherine Sandstone|35150|6|Mentioned|p422|||||||||
3793|Catherine Sandstone|35284|6|Mentioned|Fig.1|||||||||
3793|Catherine Sandstone|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
3793|Catherine Sandstone|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
3793|Catherine Sandstone|35811|5|Briefly described|Table 5|||||||||
3793|Catherine Sandstone|35845|6|Mentioned|Fig.25|||||||||
3793|Catherine Sandstone|35873|6|Mentioned|Fig.25|||||||||
3793|Catherine Sandstone|36103|4|Described|Table 1|||||||||
3793|Catherine Sandstone|36104|6|Mentioned|p122|||||||||
3793|Catherine Sandstone|36241|4|Described|p123|||||||||
3793|Catherine Sandstone|36243|6|Mentioned|Table 3A|||||||||
3793|Catherine Sandstone|36739|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|37070|6|Mentioned|p69|||||||||
3793|Catherine Sandstone|37072|6|Mentioned|p91|||||||||
3793|Catherine Sandstone|37450|6|Mentioned|p374|||||||||
3793|Catherine Sandstone|37610|6|Mentioned|Fig.4|||||||||
3793|Catherine Sandstone|37705|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|37724|6|Mentioned|Table 1|||||||||
3793|Catherine Sandstone|37726|3|Fully described|p147|||||||||
3793|Catherine Sandstone|37918|6|Mentioned|p474|||||||||
3793|Catherine Sandstone|38092|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|38312|4|Described|p461|||||||||
3793|Catherine Sandstone|39212|4|Described|p34|||Excursion site described. p24 gas reservoir. See also p11 & 35.||||||16-NOV-15
3793|Catherine Sandstone|39219|6|Mentioned|p46|||Microflora||||||
3793|Catherine Sandstone|39252|6|Mentioned|Fig.13|||||||||
3793|Catherine Sandstone|39261|6|Mentioned|Fig.6|||||||||
3793|Catherine Sandstone|39263|6|Mentioned|Fig.1|||See also Fig.2||||||
3793|Catherine Sandstone|39267|6|Mentioned|p239|||||||||
3793|Catherine Sandstone|39268|6|Mentioned|p270|||||||||
3793|Catherine Sandstone|39272|5|Briefly described|p295|||Correlation||||||
3793|Catherine Sandstone|39273|6|Mentioned|Fig. 2|||||||||
3793|Catherine Sandstone|39275|6|Mentioned|p332|||||||||
3793|Catherine Sandstone|39412|6|Mentioned|p21|||||||||
3793|Catherine Sandstone|39423|6|Mentioned|p47|||||||||
3793|Catherine Sandstone|39445|5|Briefly described|Table 8|||||||||
3793|Catherine Sandstone|39494|6|Mentioned|Fig.5|||||||||
3793|Catherine Sandstone|39611|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|39813|6|Mentioned|Map legend|Permian|Carboniferous|Permo Carboniferous||||||
3793|Catherine Sandstone|39815|6|Mentioned|Fig.10|||||||||
3793|Catherine Sandstone|39943|6|Mentioned|Table 5A|||||||||
3793|Catherine Sandstone|40030|6|Mentioned|p135|||||||||
3793|Catherine Sandstone|40256|6|Mentioned|Fig.4|||||||||
3793|Catherine Sandstone|40539|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|40544|6|Mentioned|Fig.6|||||||||
3793|Catherine Sandstone|41246|6|Mentioned|Map legend|Permian||||||||
3793|Catherine Sandstone|41247|6|Mentioned|Fig.7|||||||||
3793|Catherine Sandstone|41290|6|Mentioned|Fig.8|||||||||
3793|Catherine Sandstone|41330|6|Mentioned|Table 1|||||||||
3793|Catherine Sandstone|41605|6|Mentioned|Fig.2|||||||||
3793|Catherine Sandstone|41666|6|Mentioned|p12|||||||||
3793|Catherine Sandstone|41737|6|Mentioned|p351|||||||||
3793|Catherine Sandstone|41809|6|Mentioned|p64|||||||||
3793|Catherine Sandstone|42249|6|Mentioned|Table 1 P22|||||||||
3793|Catherine Sandstone|42250|6|Mentioned|Fig.4 P31|||||||||
3793|Catherine Sandstone|42251|6|Mentioned|Fig.2 P38|||||||||
3793|Catherine Sandstone|42254|6|Mentioned|p221|||||||||
3793|Catherine Sandstone|42437|6|Mentioned|Fig.3 P822|||||||||
3793|Catherine Sandstone|42578|5|Briefly described|Table 1 P124-125|||Name assumed. Actually spelt Catherine Ss.||||||
3793|Catherine Sandstone|42614|5|Briefly described|p13|||Bowen Basin||||||
3793|Catherine Sandstone|42641|6|Mentioned|p108|||||||||
3793|Catherine Sandstone|42662|6|Mentioned|p84 Fig.4|||||||||
3793|Catherine Sandstone|42856|5|Briefly described|Fig.2 P632|||||||||
3793|Catherine Sandstone|42911|6|Mentioned|p9|||||||||
3793|Catherine Sandstone|42994|6|Mentioned|p274|||||||||
3793|Catherine Sandstone|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
3793|Catherine Sandstone|43050|5|Briefly described|Fig.1,p5|||||||||
3793|Catherine Sandstone|43475|14|Not recorded|p553||Permian|||||||
3793|Catherine Sandstone|43714|6|Mentioned|p8|||||||||
3793|Catherine Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
3793|Catherine Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
3793|Catherine Sandstone|43977|14|Not recorded|p576-579|||See also Lexicon.||||||
3793|Catherine Sandstone|43987|14|Not recorded|p267,270,281|||||||||
3793|Catherine Sandstone|43990|14|Not recorded|Map Legend|||Part of Gebbie Sub-Group.||||||
3793|Catherine Sandstone|43994|14|Not recorded|Map Legend|||||||||
3793|Catherine Sandstone|43995|14|Not recorded|Tb.p9,15,40,53,Fig.6|Permian|Carboniferous|Fig.14||||||
3793|Catherine Sandstone|44023|6|Mentioned|p7|||||||||
3793|Catherine Sandstone|44085|2|Defined|Opp.p4,10|||||||||
3793|Catherine Sandstone|44091|14|Not recorded|p45,Tb.3,p47|||Part of Middle Bowen Group in Springsure area.||||||
3793|Catherine Sandstone|44096|2|Defined|Fig.26,p186-7,191-3|||||||||
3793|Catherine Sandstone|44127|14|Not recorded|p194|||Correlated with "Clarkei Bed".||||||
3793|Catherine Sandstone|44169|2|Defined|p6,7,12,13,Tb.1,map|||||||||
3793|Catherine Sandstone|44170|4|Described|p5,6,11,30-2,Tb.1,3||Early Permian|Part of Back Creek Group.||||||
3793|Catherine Sandstone|44172|2|Defined|p1320,1323,1327-8,||Kungurian|Denison Trough. p1330,1332-3,1337,1342,1343,Fig.2,Tb.1.||||||
3793|Catherine Sandstone|44173|14|Not recorded|p110 (Fig.1),112|||||||||
3793|Catherine Sandstone|44218|14|Not recorded|p19||Kungurian|Late Kungurian.||||||
3793|Catherine Sandstone|44219|14|Not recorded|p31||Kungurian|||||||
3793|Catherine Sandstone|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
3793|Catherine Sandstone|44419|14|Not recorded|p272||Permian|||||||
3793|Catherine Sandstone|44421|14|Not recorded|p6,8,9||Permian|||||||
3793|Catherine Sandstone|44422|14|Not recorded|p150,152,153||Early Permian|||||||
3793|Catherine Sandstone|44424|14|Not recorded|p293-301|||||||||
3793|Catherine Sandstone|44571|14|Not recorded|p207|||||||||
3793|Catherine Sandstone|44577|14|Not recorded|p136,138|||||||||
3793|Catherine Sandstone|44618|14|Not recorded|p511,514,517-8,520||Permian|||||||
3793|Catherine Sandstone|44651|14|Not recorded|p117,123|||||||||
3793|Catherine Sandstone|44855|14|Not recorded|p27|||||||||
3793|Catherine Sandstone|45006|14|Not recorded|Tb.1,p3,5-7,96,101-3|||||||||
3793|Catherine Sandstone|45031|14|Not recorded|p9, Fig.3||Permian|||||||
3793|Catherine Sandstone|45071|3|Fully described|Table 6|||||||||
3793|Catherine Sandstone|45110|6|Mentioned|p47|||||||||
3793|Catherine Sandstone|46849|6|Mentioned|Fig. 7|||||||||
3793|Catherine Sandstone|46989|5|Briefly described|Table 1|||||||||
3793|Catherine Sandstone|48626|4|Described|p1,3,24,31-2,34-5,50||Permian|p52,55,93,94,Pl.1,Fig.1,2.||||||
3793|Catherine Sandstone|48630|14|Not recorded|p5|||||||||
3793|Catherine Sandstone|48845|14|Not recorded|p37,38|||||||||
3793|Catherine Sandstone|48847|14|Not recorded|p1,10,Pl.2|||Top=top of Unit B.||||||
3793|Catherine Sandstone|48898|6|Mentioned|Fig.4|||L.Permian||||||
3793|Catherine Sandstone|48900|3|Fully described|p36|||Lower Permian||||||
3793|Catherine Sandstone|49644|5|Briefly described|Table|||||||||
3793|Catherine Sandstone|60286|4|Described|p277|Late Permian|Late Permian|Conformably overlies Ingelara Formation. Equivalent to German Creek Formation. Overlain by Peawaddy Formation. Coastal and deltaic. Geological Province: Bowen Basin.||||||09-FEB-05
3793|Catherine Sandstone|61313|6|Mentioned|p104 Table G1|||||||||
3793|Catherine Sandstone|61377|6|Mentioned|p156 Tb. SU2|Early Permian|Early Permian|A reservoir unit in Queensland.||||||07-FEB-11
3793|Catherine Sandstone|61609|6|Mentioned|p240|Permian|Permian|Overlain by Peawaddy Formation. Geological Province: Denison Trough.||||||07-FEB-11
3793|Catherine Sandstone|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
3793|Catherine Sandstone|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
3793|Catherine Sandstone|63713|5|Briefly described|p1507 Fig.2, p1508, p1522-1523, p1526|Wordian|Roadian|See also p1528-1531, p1533. Denison Trough, Bowen Basin. Graphic log. Well-log correlation.||||Overlies Ingelara Formation. Is overlain by Peawaddy Formation.||
3793|Catherine Sandstone|63832|6|Mentioned|p131 fig 2|Wordian|Wordian|West Bowen Basin. Appears in Fig.2 as Cath./Freit./Ing.||||||13-DEC-17
3793|Catherine Sandstone|64631|5|Briefly described|p48 Fig.4.|Capitanian|Wordian|Bowen Basin. See also p44 where shown with Freitag and Ingelara Fms. Some biostratigraphic age control indicated.||||Is overlain by Peawaddy Formation.||
3793|Catherine Sandstone|64665|6|Mentioned|p56. |||Equivalent to Colinlea Sandstone.||||||
3793|Catherine Sandstone|64857|5|Briefly described|p119, p113 Fig.3|Late Permian|Late Permian|Denison Trough, Bowen Basin.||||||
3793|Catherine Sandstone|65115|5|Briefly described|p414-415, 416, 417, 418, Fig 2 p403|Kazanian|Ufimian|Sandstone. Overlies the Ingelara Formation, underlies the Peawaddy Formation in the Denison Trough, Bowen Basin. Part of Supersequence D.||||||
3793|Catherine Sandstone|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Peawaddy Formation, ?overlies the Ingelara Formation, Denison Trough, Bowen Basin||||||06-MAR-12
3793|Catherine Sandstone|66615|6|Mentioned|p2 Fig.1|||Denison Trough, Bowen Basin.||||||
3793|Catherine Sandstone|67402|4|Described|p21, p64, p65, p69-p73|Capitanian|Capitanian|Bowen Basin. Approximately 40m thick.  Deposited in deltaic, paralic and shallow marine depositional environments. See also  p78, p79, p302.||||Overlies the Aldebaran Sandstone, Upper and the Ingelara Formation. Overlain by the Black Alley Shale and Peawaddy Formation.|Quartzose sandstone and siltstone.|
3793|Catherine Sandstone|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Peawaddy Formation. Underlain by Freitag Formation or Ingelara Formation?||
3793|Catherine Sandstone|68576|5|Briefly described|Q_4: p3|Lopingian|Lopingian|Bowen Basin.||||Overlies Ingelara Formation. Is overlain by Peawaddy Formation.||
3793|Catherine Sandstone|68679|5|Briefly described|p378, p380-382, p384|Permian|Permian|Phillips (1960). Northern Denison Trough, Bowen Basin. 160m thick. Shallow-marine delta deposits. Produces gas and minor condensate.||||Overlies Ingelara Formation. Is overlain by Peawaddy Formation. Passes [presumably vertically] into the Crocker Formation. Together they pass laterally into German Creek Formation.|Quartzose to sublabile sandstone, siltstone, mudstone; marine fossils.|
3793|Catherine Sandstone|68731|6|Mentioned|p201 Fig 3.110|Late Permian|Late Permian|Bowen Basin.||||||
3793|Catherine Sandstone|71265|5|Briefly described|p589-590, p595-596, p602, p606|Changhsingian|Wuchiapingian|Bowen and eastern Galilee Basins. Sedimentary log of GSQ Tambo 1-1A. Coastal deposits.||||Overlies Ingelara Formation. Is overlain by Peawaddy Formation.|Clean, well-sorted, structureless sandstones.|
3793|Catherine Sandstone|71276|5|Briefly described|p287-288, p294, p295 Fig.8, p296-297|Lopingian|Lopingian|Eastern side of the Springsure Shelf, and Denison Trough (Bowen Basin). Probable lateral equivalent of (part of) the Colinlea Sandstone.||||Overlies Ingelara Formation. Passes laterally into the Flat Top and German Creek Formations.||
3793|Catherine Sandstone|71701|5|Briefly described|p155-p156, p168|Changhsingian|Wuchiapingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Ingelara Formation. Overlain by the Peawaddy Formation.||
3793|Catherine Sandstone|72088|5|Briefly described|p8, p20, p38, p91|Wuchiapingian|Wuchiapingian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Ingelara Formation||
3793|Catherine Sandstone|73304|6|Mentioned|p78|||Bowen Basin, southern.||||||
3793|Catherine Sandstone|73305|6|Mentioned|p548 Fig.1|Late Permian|Late Permian|Bowen Basin. Denison Trough.||||||
3793|Catherine Sandstone|73472|6|Mentioned|p115|Wuchiapingian|Wuchiapingian|Galilee Basin.||||Underlain by Ingelara Formation. Overlain by Peawaddy Formation. Equivalent to Colinlea Sandstone||
3793|Catherine Sandstone|73625|5|Briefly described|p2-3, p5 Fig.3, p13, 18|Permian|Permian|Bowen Basin.||||Overlies Ingelara Formation. Is overlain by Peawaddy Formation.|Includes intensely bioturbated sandstone with interbedded and admixed siltstone.|
3854|Cedar Pocket Porphyry|23251|5|Briefly described|Table 5 p33||Late Triassic|Age: its relationship to the dacite feldspar porphyry of the Woondum Granite indicates a Late Triassic or younger age (Cranfield & Scott 1993).||||||30-NOV-05
3854|Cedar Pocket Porphyry|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
3854|Cedar Pocket Porphyry|35101|3|Fully described|p76|||||||||
3854|Cedar Pocket Porphyry|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
3854|Cedar Pocket Porphyry|39445|5|Briefly described|Table 12|||||||||
3854|Cedar Pocket Porphyry|41272|6|Mentioned|M 1of1 D16|||||||||
3854|Cedar Pocket Porphyry|41917|6|Mentioned|p522|||||||||
3854|Cedar Pocket Porphyry|42695|5|Briefly described|Fig.2|Triassic||||||||
3854|Cedar Pocket Porphyry|42751|5|Briefly described|p27|||see also Fig.1 P23||||||
3854|Cedar Pocket Porphyry|43100|4|Described|p57|Late Triassic|Early Triassic|||||||
3854|Cedar Pocket Porphyry|44928|5|Briefly described|Map Legend||Late Triassic|||||||
3854|Cedar Pocket Porphyry|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Porphyritic microgranite.||||||
3854|Cedar Pocket Porphyry|68679|5|Briefly described|p429|Late Triassic|Late Triassic|Northern New England Orogen. Forms a crescent-shaped body and three smaller bodies.||||Is intruded by the Woondum Granite.|High-level porphyritic microgranite.|
3855|Cedarton Volcanics|22845|4|Described|p70,73-77|Permian|Permian|After Mathews 1955, intruded by the Neurum Tonalite.  Possible correlation with Cambroon beds.||||||
3855|Cedarton Volcanics|22846|6|Mentioned|p44|Carboniferous|Devonian|Intruded by Neurum Complex.||||||
3855|Cedarton Volcanics|23251|6|Mentioned|p21, p36|||Of the South East Queensland Volcanic and Plutonic Province.||||||21-JUN-06
3855|Cedarton Volcanics|23542|5|Briefly described|Fig 1 p378|||Also see p377.||||||
3855|Cedarton Volcanics|23799|5|Briefly described|p125|Early Permian|Early Permian|Mafic and lesser felsic volcanics and coarse clastics.  Geological Province:  North D'Aguilar Subprovince.||||||
3855|Cedarton Volcanics|30914|6|Mentioned|Map legend|Permian|Permian|||||||
3855|Cedarton Volcanics|32945|6|Mentioned|p88|||Permian||||||
3855|Cedarton Volcanics|34475|6|Mentioned|p249|||See also P250. Lower Permian||||||
3855|Cedarton Volcanics|35101|3|Fully described|p27|||||||||
3855|Cedarton Volcanics|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
3855|Cedarton Volcanics|35866|6|Mentioned|p410|||||||||
3855|Cedarton Volcanics|36045|6|Mentioned|p330|||||||||
3855|Cedarton Volcanics|36528|6|Mentioned|p171|||Also mention P174.||||||
3855|Cedarton Volcanics|37252|6|Mentioned|Map legend|Permian|Permian|||||||
3855|Cedarton Volcanics|38391|6|Mentioned|p9|||||||||
3855|Cedarton Volcanics|38805|6|Mentioned|Fig.1|||||||||
3855|Cedarton Volcanics|39445|5|Briefly described|Table 8|||See also Fig.7||||||
3855|Cedarton Volcanics|40051|4|Described|p6|||||||||
3855|Cedarton Volcanics|40623|5|Briefly described|p53|||||||||
3855|Cedarton Volcanics|41272|6|Mentioned|M 1of1 D16|||||||||
3855|Cedarton Volcanics|42547|5|Briefly described|p55|||||||||
3855|Cedarton Volcanics|43006|4|Described|Table 1,p239|||||||||
3855|Cedarton Volcanics|43100|6|Mentioned|p80|||||||||
3855|Cedarton Volcanics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
3855|Cedarton Volcanics|44573|14|Not recorded|p96||Early Permian|Kia-Ora No.1. See also Lexicon.||||||
3855|Cedarton Volcanics|44925|5|Briefly described|Map Legend||Permian|||||||
3855|Cedarton Volcanics|60077|5|Briefly described|Map legend|Early Permian|Early Permian|Andesite, andesitic tuff.||||||
3855|Cedarton Volcanics|61780|5|Briefly described|p255, p256, p259, p264|||Includes mainly basaltic tuffs abd tuff-breccias with Permian marine fauna.||||||
3855|Cedarton Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with the Marumba, Northbrook and Cambroon beds and the Kandanga Creek Megabreccia, are all mapped under the symbol, Pn.||||||
3855|Cedarton Volcanics|68679|5|Briefly described|p321, p324, p326, p384, p387|Permian|Permian|Matthews (1955). Cressbrook Basin, northern New England Orogen. Occurs W of Beerwah, between the Conondale Range and the Stanley River floodplain. Cover basin sediments; probably no more than 300m thick. Has several similarities to Cambroon beds.||||Is correlated with Cambroon beds, and probably also Marumba beds and Kandanga Creek Megabreccia. Probably faulted against the Booloumba beds. Is intruded by the Neurum Complex.|Volcaniclastic sediments and mafic lavas; strongly altered to fine-grained epidote-rich and chlorite-rich assemblages.|
3855|Cedarton Volcanics|71702|6|Mentioned|179|||Backarc-rift related rocks.||||||
3863|Central Creek Granodiorite|42747|5|Briefly described|Fig.9 p38|||see also Table 1 P37. Reserved as Central Creek Granite.||||||01-SEP-14
3863|Central Creek Granodiorite|43029|2|Defined|p21||Devonian|see also Fig.2,p16||||||
3863|Central Creek Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
3863|Central Creek Granodiorite|43213|3|Fully described|p96-97, p108, p116-121, p175, p177-178|Devonian|Devonian|See also p208, p213-214, p233, p241-242. Type locality described. This unit is distinguished from Kilmarnock and Mount Newsome Granodiorites by the absence of hornblende, and geophysical characteristics. Precise age unknown: assigned to Devonian because of similarities with other components of the Retreat Batholith. Peraluminous. Geochemistry, modal analyses and geophysics detailed.||||Intrudes the Anakie Metamorphic Group. Is overlain unconformably by the Silver Hills Volcanics.|Pale grey to white, fine- to medium-grained biotite granite to granodiorite.|
3863|Central Creek Granodiorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey to white, fine to medium-grained, equigranular biotite granodiorite to granite.|
3929|Charters Towers Metamorphics|22533|6|Mentioned|p47||Proterozoic|||||||
3929|Charters Towers Metamorphics|22543|6|Mentioned|p62||Cambrian|||||||
3929|Charters Towers Metamorphics|22611|6|Mentioned|Fig2 P186||Cambrian|||||||
3929|Charters Towers Metamorphics|22630|5|Briefly described|p 6|||||||||
3929|Charters Towers Metamorphics|22713|6|Mentioned|p125|||||||||
3929|Charters Towers Metamorphics|22844|6|Mentioned|p6, Fig3|||||||||
3929|Charters Towers Metamorphics|22847|4|Described|p 5 -6|Middle Cambrian||||||||
3929|Charters Towers Metamorphics|23049|6|Mentioned|p6 Fig.3|||||||||
3929|Charters Towers Metamorphics|23083|5|Briefly described|p681||Early Paleozoic|||||||07-NOV-08
3929|Charters Towers Metamorphics|23422|4|Described|p169, p207 Table 6.3|Cambrian|Neoproterozoic|Geological Province: Cape River Province.||||||
3929|Charters Towers Metamorphics|23430|4|Described|p459-462|||Intruded by Bucklands Hill Diorite. Cape River Province.||||||
3929|Charters Towers Metamorphics|23431|5|Briefly described|p537|||Cape River Province.||||||
3929|Charters Towers Metamorphics|23509|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|||||||
3929|Charters Towers Metamorphics|23893|5|Briefly described|p11|Ordovician|Cambrian|Intruded by Bucklands Hill Diorite.  Geological Province: Cape River Province.||||||
3929|Charters Towers Metamorphics|24036|6|Mentioned|p2, p12, p13, p15|||Geological Province: North Drummond Basin. Biotite-schist.||||||
3929|Charters Towers Metamorphics|24424|6|Mentioned|p524|||Geological Province: Lolworth-Ravenswood Province.||||||
3929|Charters Towers Metamorphics|30151|4|Described|Table 1|||See also p9. Cambrian - Ordovician age.||||||07-OCT-08
3929|Charters Towers Metamorphics|30914|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
3929|Charters Towers Metamorphics|31285|4|Described|p79|||See also p81, 88. ? Precambrian.||||||07-OCT-08
3929|Charters Towers Metamorphics|31813|6|Mentioned|p16|||See also Table 2. Pre-Silurian||||||
3929|Charters Towers Metamorphics|31999|6|Mentioned|p127|||Camb.-Ord. See also Table 11||||||
3929|Charters Towers Metamorphics|32169|6|Mentioned|Table 2|||Palaeozoic||||||
3929|Charters Towers Metamorphics|32553|4|Described|p54|||||||||
3929|Charters Towers Metamorphics|33002|6|Mentioned|p412|||Plate tectonics||||||
3929|Charters Towers Metamorphics|34409|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
3929|Charters Towers Metamorphics|35304|6|Mentioned|p605|||||||||
3929|Charters Towers Metamorphics|36154|6|Mentioned|Fig.3|||||||||
3929|Charters Towers Metamorphics|36472|6|Mentioned|Map legend|Ordovician|Cambrian|Ordovician to Cambrian||||||
3929|Charters Towers Metamorphics|36561|6|Mentioned|Fig.1|||||||||
3929|Charters Towers Metamorphics|37144|6|Mentioned|p14|||||||||
3929|Charters Towers Metamorphics|37565|6|Mentioned|p4|||||||||
3929|Charters Towers Metamorphics|37570|5|Briefly described|p123|||||||||
3929|Charters Towers Metamorphics|37764|6|Mentioned|Fig.3|||||||||
3929|Charters Towers Metamorphics|39445|6|Mentioned|p66|||See also Table 4.||||||
3929|Charters Towers Metamorphics|39686|6|Mentioned|Fig.1|||||||||
3929|Charters Towers Metamorphics|39689|6|Mentioned|p49|||See also p61.||||||07-OCT-08
3929|Charters Towers Metamorphics|39734|6|Mentioned|p21|||||||||
3929|Charters Towers Metamorphics|39735|6|Mentioned|p16|||||||||
3929|Charters Towers Metamorphics|40746|5|Briefly described|p345|||||||||
3929|Charters Towers Metamorphics|40787|5|Briefly described|p321|||||||||
3929|Charters Towers Metamorphics|41272|5|Briefly described|M 1of1 A09|||See also M 1of1 K08||||||
3929|Charters Towers Metamorphics|41659|5|Briefly described|p366|||Mention p363.||||||07-OCT-08
3929|Charters Towers Metamorphics|41668|5|Briefly described|p6|||||||||
3929|Charters Towers Metamorphics|41774|6|Mentioned|p29|||||||||
3929|Charters Towers Metamorphics|42633|4|Described|p14|||||||||
3929|Charters Towers Metamorphics|42750|6|Mentioned|p33, p35, p37|||||||||
3929|Charters Towers Metamorphics|43093|5|Briefly described|p10|||see also Fig.1.||||||
3929|Charters Towers Metamorphics|43103|5|Briefly described|p17, Fig.6.|||||||||
3929|Charters Towers Metamorphics|43933|5|Briefly described|Map Legend||Neoproterozoic|||||||
3929|Charters Towers Metamorphics|43934|5|Briefly described|Map Legend||Neoproterozoic|||||||
3929|Charters Towers Metamorphics|44060|14|Not recorded|Map Legend||Early Paleozoic|||||||07-NOV-08
3929|Charters Towers Metamorphics|44061|4|Described|Table 1||Early Paleozoic|||||||07-NOV-08
3929|Charters Towers Metamorphics|44207|14|Not recorded|p115|||||||||
3929|Charters Towers Metamorphics|44699|14|Not recorded|p108|||Previously regarded as Precambrian, probably Silurian or Devonian equated with volcanics and sediments of Windsor Range Volcanics and Bletchington Park Beds.||||||
3929|Charters Towers Metamorphics|45151|6|Mentioned|p4|||||||||
3929|Charters Towers Metamorphics|48904|2|Defined|p12|Late Cambrian|Late Cambrian|Revision of Charters Towers Series. Cambrian - Ordovician.||||||10-FEB-09
3929|Charters Towers Metamorphics|48914|4|Described|p19|||Cambrian||||||
3929|Charters Towers Metamorphics|50552|5|Briefly described|p1048 Fig.2|Early Cambrian|Neoproterozoic|In Lolworth-Ravenswood Terrane.||||||24-NOV-04
3929|Charters Towers Metamorphics|61211|5|Briefly described|p262|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3929|Charters Towers Metamorphics|62074|5|Briefly described|p1-2|Early Cambrian|Neoproterozoic|Basement in Lolworth-Ravenswood Block. Multiply deformed; underwent high T/low P metamorphism in early to middle Ordovician. Paper (p1) says Charters Towers Metamorphics INCLUDES mafic bodies (Bucklands Hill Diorite).||||||11-AUG-15
3929|Charters Towers Metamorphics|62075|5|Briefly described|p7, p9 Fig.2, p11 Fig.3|Early Cambrian|Neoproterozoic|Part of the basement in the Lolworth-Ravenswood terrane.||||Is intruded by Bucklands Hill Diorite.|Amphibolite grade metasedimentary rocks.|
3929|Charters Towers Metamorphics|62521|5|Briefly described|p2|Early Ordovician|Late Cambrian|Intruded by units of the Ravenswood Batholith.||||||
3929|Charters Towers Metamorphics|63154|5|Briefly described|p285 Fig. 5|Cambrian|Early Cambrian|Geological province: Charters Towers Province.||||||
3929|Charters Towers Metamorphics|64852|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Mica schist, quartzite, quartz-feldspar-biotite gneiss, hornblende schist; cordierite, andalusite and staurolite hornfles, chlorite schist, marble.||||||
3929|Charters Towers Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Charters Towers Province. This unit, as well as Running River and Argentine Metamorphics, are all mapped under the symbol, -P-Cr.||||||
3929|Charters Towers Metamorphics|68576|5|Briefly described|Q_11: p41-42|||Thomson Province. Probably late Neoproterozoic or Cambrian. Mainly forms large screens within the Ravenswood Batholith.|||||Metasediments including muscovite-biotite schist.|
3929|Charters Towers Metamorphics|68731|5|Briefly described|p144, p145, p147, p150, p151 Fig 3.51|||Charters Towers Province. (Reid 1917; Wyatt et al. 1970, 1971; Peters 1987). Metamorphosed to predominantly amphibolite grade. Minimum age constrained by the intrusive Bucklands Hill Diorite.|>508 +/- 7 Ma (Fanning 1995)|||Intruded by the Bucklands Hill Diorite. Correlated with the Cape River Metamorphics on lithological grounds.|Comprises multiply deformed quartz-biotite-plagioclase schist, cordierite-quartz-biotite schist, meta-arenite, quartzite and minor amphibolite and calc-silicate.|10-MAY-16
3929|Charters Towers Metamorphics|68822|5|Briefly described|p324|Paibian|Stage 3|See also Charters Tower Metamorphics. Thompson Orogen.|ca. 507 +/- 12 Ma||||Mafic? Intrusive rocks.|
3929|Charters Towers Metamorphics|69952|5|Briefly described|p2 Tb.i, p5-6, p94-103|||Charters Towers Province, Thomson Orogen. Crops out along a 150 km E-W belt. Complex age distribution of zircons discussed. SHRIMP U-Pb zircon ages of maximum deposition and metamorphism, respectively. A monazite age of metamorphism is also given at 467.0 +/- 5.7 Ma (all by Cross et al., 2015). A contact metamorphic origin for these zircons is consistent with the age of the intruding Columbia Creek Conmplex granite dykes of 464 +/- 5 Ma (Hutton et al., 1994). The Bucklands Hill Diorite intrusion gives a minimum age of 508 Ma.|511 +/- 17 Ma; 465.9 +/- 6.0 Ma.|||Is intruded by Bucklands Hill Diorite.|Low pressure, high temperature rocks with sillimanite and migmatite, but no garnet. Includes quartz-biotite-plagioclase schist, a banded plagioclase-muscovite-biotite-quartz-?cordierite schist, quartzite and minor calc-silicate rocks.|
3929|Charters Towers Metamorphics|70740|6|Mentioned|p37|||||||||
3929|Charters Towers Metamorphics|70744|6|Mentioned|p947|||Intruded by Ravenswood Batholith plutons aged 510-460 Ma.||||||
3929|Charters Towers Metamorphics|70749|5|Briefly described|p42, p45-48, p51|Cambrian||Characterised by abundant 650-500 Ma zircons with a subordinate 1300-900 Ma group, and a maximum depositional age of 511-495 Ma. Zircons sourced from rift-related and back-arc volcanism of the active Gondwana margin.|511 +/- 17 Ma (maximum depositional age).|||Adjacent to (p42 implies is intruded by) Columbia Creek Supersuite.|Includes fine-grained plagioclase-muscovite-biotite-quartz schist with minor banding.|27-APR-18
3929|Charters Towers Metamorphics|71592|5|Briefly described|Appendix A.|||Charters Towers Province, Thomson Orogen.|464+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite, schist.|
3929|Charters Towers Metamorphics|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Charters Towers Province, Thomson Orogen. ||||||
3929|Charters Towers Metamorphics|73425|6|Mentioned|p2, 16, 18|Cambrian|Neoproterozoic|Wyatt et al. (1971). Charters Towers Province, northeast Thomson Orogen. Metamorphic zircon rims aged Middle Ordovician.||||||
3934|Chatsworth Limestone|22646|6|Mentioned|Fig 5 on p 105||Cambrian|Of the Georgina Basin.||||||02-APR-07
3934|Chatsworth Limestone|22954|4|Described|p8,10-1,Fig5p16||Payntonian|||||||
3934|Chatsworth Limestone|23553|5|Briefly described|p2276|Ordovician|Cambrian|Geological Province: Georgina Basin.||||||
3934|Chatsworth Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin. Maximum thickness: 460m.||||||11-JUN-08
3934|Chatsworth Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relations||||||
3934|Chatsworth Limestone|30598|6|Mentioned|p50|||||||||
3934|Chatsworth Limestone|30778|6|Mentioned|p5,Fig.5|||||||||
3934|Chatsworth Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|31572|3|Fully described|Fig. 1|Late Cambrian|Late Cambrian|Refers Casey (1959).||||||11-JUN-08
3934|Chatsworth Limestone|32576|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|32952|4|Described|p1188|||See also pp1190,1192,1193. M.-U. Cambrian||||||04-AUG-06
3934|Chatsworth Limestone|33111|4|Described|p33|||Mention p4.||||||04-AUG-06
3934|Chatsworth Limestone|33482|6|Mentioned|Fig.1|||Middle - Upper Cambrian||||||
3934|Chatsworth Limestone|33738|6|Mentioned|p49|||||||||
3934|Chatsworth Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
3934|Chatsworth Limestone|35139|4|Described|Table.2|||||||||
3934|Chatsworth Limestone|35936|6|Mentioned|p614|||||||||
3934|Chatsworth Limestone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|37572|4|Described|p160|||See also Fig.8||||||
3934|Chatsworth Limestone|38444|6|Mentioned|p106|||||||||
3934|Chatsworth Limestone|38446|5|Briefly described|p152|||||||||
3934|Chatsworth Limestone|38532|4|Described|Fig.1|||||||||
3934|Chatsworth Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
3934|Chatsworth Limestone|39445|5|Briefly described|Table 4|||See also p64.||||||02-APR-07
3934|Chatsworth Limestone|39690|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|40136|5|Briefly described|p21|||||||||
3934|Chatsworth Limestone|40810|5|Briefly described|p14|||||||||
3934|Chatsworth Limestone|40852|6|Mentioned|Fig.3.7|||||||||
3934|Chatsworth Limestone|41109|6|Mentioned|p184|||||||||
3934|Chatsworth Limestone|41306|6|Mentioned|p4|||||||||
3934|Chatsworth Limestone|41587|6|Mentioned|p913|||||||||
3934|Chatsworth Limestone|42058|4|Described|p115|||||||||
3934|Chatsworth Limestone|42139|6|Mentioned|Fig.9 P72|||||||||
3934|Chatsworth Limestone|42354|6|Mentioned|p11|Payntonian||See also p20. Age: Late Cambrian (early Payntonian).||||||11-JUN-08
3934|Chatsworth Limestone|43579|6|Mentioned|p367||Late Cambrian|||||||
3934|Chatsworth Limestone|43781|6|Mentioned|p18|||||||||
3934|Chatsworth Limestone|43807|5|Briefly described|p345-6|||||||||
3934|Chatsworth Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
3934|Chatsworth Limestone|43995|14|Not recorded|p62,7||Late Cambrian|||||||
3934|Chatsworth Limestone|44091|14|Not recorded|p17,Tb.1,p19||Late Cambrian|1d a mean.||||||
3934|Chatsworth Limestone|44211|2|Defined|p90,96,100,104,107||Late Cambrian|Rests above Pomegranate Limestone. Overlain by Ninmaroo Formation. (Franconian - Trempealeauan).||||||21-APR-09
3934|Chatsworth Limestone|44275|14|Not recorded|Map Legend|||||||||
3934|Chatsworth Limestone|44276|2|Defined|Tb.2,p20,22|||||||||
3934|Chatsworth Limestone|44277|14|Not recorded|Map Legend||Late Cambrian|||||||
3934|Chatsworth Limestone|44291|14|Not recorded|p7||Late Cambrian|||||||
3934|Chatsworth Limestone|44361|14|Not recorded|Map Legend||Late Cambrian|||||||
3934|Chatsworth Limestone|44362|4|Described|Tb.1,p9||Late Cambrian|||||||
3934|Chatsworth Limestone|44457|14|Not recorded|p.6||Late Cambrian|Upper Cambrian. (F53-10).||||||
3934|Chatsworth Limestone|44543|2|Defined|p32,33,36|Late Cambrian|Middle Cambrian|Overlies O'Hara Shale.||||||
3934|Chatsworth Limestone|44620|14|Not recorded|p88||Late Cambrian|Conodonts.||||||
3934|Chatsworth Limestone|44719|14|Not recorded|p143|||Upper two-thirds of the Upper Cambrian conodonts.||||||
3934|Chatsworth Limestone|44848|14|Not recorded|p110|||||||||
3934|Chatsworth Limestone|44920|14|Not recorded|Map Legend, Sheet4||Late Cambrian|||||||
3934|Chatsworth Limestone|45002|14|Not recorded|p18,20-22|||Late Cambrian fossils.||||||
3934|Chatsworth Limestone|45012|14|Not recorded|p6.31|||Upper Cambrian fauna.||||||
3934|Chatsworth Limestone|45044|14|Not recorded|p5||Late Cambrian|||||||
3934|Chatsworth Limestone|45051|5|Briefly described|Fig.3|||See also p1,4,5,9. Upper Cambrian age.||||||04-AUG-06
3934|Chatsworth Limestone|45052|2|Defined|p113|Late Cambrian|Late Cambrian|||||||
3934|Chatsworth Limestone|45053|6|Mentioned|p4|||Lithology equivalent Gola Beds||||||
3934|Chatsworth Limestone|45058|6|Mentioned|p8|||See also p23. Correlation with Clark Sandstone.||||||02-APR-07
3934|Chatsworth Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
3934|Chatsworth Limestone|45094|4|Described|p7|||||||||
3934|Chatsworth Limestone|45130|4|Described|p3|||||||||
3934|Chatsworth Limestone|45166|5|Briefly described|Table 15|||||||||
3934|Chatsworth Limestone|46887|6|Mentioned|p253|||||||||
3934|Chatsworth Limestone|46897|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|46958|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|48906|14|Not recorded|Tb.1,App.D|||||||||
3934|Chatsworth Limestone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Grey to dark grey and locally fossiliferous.  Overlies the O'Hara Shale.  ||||||
3934|Chatsworth Limestone|50244|5|Briefly described|p88, p89 Fig. 1, p92 Fig. 3, p95, p99|Cambrian|Cambrian|Includes Lily Creek Member. Geological Province: Georgina Basin. Carbonates, generally medium- to dark-grey or reddish grey limestones and marls with subhorizontal bedding. On p100 Fig. 7 also.||||||
3934|Chatsworth Limestone|60359|5|Briefly described|Map Legend|Ordovician|Cambrian|Limestone; minor breccia, marl.||||||
3934|Chatsworth Limestone|60419|5|Briefly described|p42|Late Cambrian|Late Cambrian|Contains echinoderms. Geological Province: Georgina Basin.||||||
3934|Chatsworth Limestone|62793|6|Mentioned|p272, p281, p282, p283|Late Cambrian|Late Cambrian|Contains conodont fossils including Prooneotodus terashimai, characteristic of the upper Iverian Stage of the Late Cambrian.||||Underlies Ninmaroo Formation.||21-MAR-12
3934|Chatsworth Limestone|63450|5|Briefly described|p78 Fig. 5, p82|Late Cambrian|Late Cambrian|Thickness: 500m. Geological province: Georgina Basin, Burke River Structural Belt. Contains calcareous siltstone, pelletal limestone, minor calcareous siltstone, calcareous sandstone, skeletal grainstones and intraformational breccia.||||||07-FEB-11
3934|Chatsworth Limestone|64068|3|Fully described|p70-71, p73, 74, p8, 225|Late Cambrian|Late Cambrian|Formerly Gola beds of Casey (1959). Thickness 158 m in type section. Max. 880 m. Paleopoles from this (and other) units define a major change in APWP.||Of Cockroach Group.|Includes Lily Creek Sandstone Member at top.|Conformably and gradationally overlies Pomegranate Limestone. Conformably and gradationally overlain by and may interdigitate with Ninmaroo Formation.|Limestone, calcareous siltstone, sandstone, quartzic dolostone, intraformational breccia and chert.|21-MAR-16
3934|Chatsworth Limestone|65489|5|Briefly described|p126-127|Late Cambrian|Late Cambrian|Burke River Structural Belt, Georgina Basin. Little hydrocarbon potential: TOC at 0.12%.||||Is overlain conformably by Ninmaroo Formation.||
3934|Chatsworth Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Late Cambrian|Late Cambrian|Burke River Structural Belt, Georgina Basin.||Cockroach Group.||Overlies Pomegranate Limestone. Is overlain by Ninmaroo Formation.|Thin-bedded, light to medium grey limestone (peloid grainstone), sandy and intraclast limestone, calcareous siltstone.|
3934|Chatsworth Limestone|67402|6|Mentioned|p216|||Georgina Basin. Potential seal unit.|||||Fine-grained limestone.|
3934|Chatsworth Limestone|67870|5|Briefly described|p39, p43-46|Cambrian|Cambrian|Georgina Basin. Part of a ~600m thick package with high amplitude discontinuous seismic reflections.||Cockroach Group.||||
3934|Chatsworth Limestone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Cockroach Group|||Thin-bedded, limestone (peloid grainstone), sandy and intraclast limestone and calcareous siltstone|
3934|Chatsworth Limestone|69443|5|Briefly described|p28:7, 25-26|Late Cambrian|Late Cambrian|Southern Georgina Basin. Contains trilobites and conodonts which indicate Iverian and Payntonian stages (Late Cambrian/Furongian).||Cockroach Group.||Is overlain conformably by Ninmaroo Formation.||12-JUL-16
3934|Chatsworth Limestone|69591|4|Described|p87, p92-93, p96-97|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. 300m thick at the type section, just south of Lily Creek, 2km S of Chatsworth Station (Shergold, 1980); cumulative thickness up to 610m. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Rich and diverse fauna (listed). Now includes rocks assigned to the Gola beds in the Momedah Anticline.||||Overlies Pomegranate Limestone. Is overlain conformably by Ninmaroo Formation.|Grey, thin-bedded calcarenite and calcilutite, sandy and oolitic limestone, coarse biosparite and coquinite, marly interbeds and common intraformational breccias. Chert (silicified limestone) in thin layers and nodules; silicified fossils locally.|
3934|Chatsworth Limestone|72297|6|Mentioned|p747-748|||Georgina Basin. TOC values indicate this unit has one of the best source rock potentials in the Burke River Structural Belt. Lacks permeability, so would be a good cap rock.||||||
3934|Chatsworth Limestone|72321|6|Mentioned|Fig 2|Jiangshanian|Jiangshanian|Burke River Structural Belt, Georgina Basin.  Australian stage: Iverian.||Of Cockroach Group.||||
3934|Chatsworth Limestone|72358|6|Mentioned|p117|||||||||
3981|Chillagoe Formation|12575|5|Briefly described|p780, p784 Table 1.|Early Devonian|Silurian|Hodgkinson Province. Strongly folded, faulted and intruded by granites in late Devonian, with widespread rhyolitic ignimbritic cauldron volcanism in Late Carboniferous to Permian. Apatite fission track analyses are detailed.|439-386 Ma.||||Mainly limestone.|
3981|Chillagoe Formation|13996|6|Mentioned|p141-142|Ludlow|Llandovery|Hodgkinson Basin. Hosts undescribed megalodont bivalves. Bivalve taxa distribution Table.||||||
3981|Chillagoe Formation|22611|6|Mentioned|P195|||||||||
3981|Chillagoe Formation|22811|6|Mentioned|p606|||of Hodgkinson Province||||||
3981|Chillagoe Formation|23032|6|Mentioned|p19|||||||||
3981|Chillagoe Formation|23039|6|Mentioned|p170||Paleozoic|||||||07-NOV-08
3981|Chillagoe Formation|23063|6|Mentioned|218|||||||||
3981|Chillagoe Formation|23076|5|Briefly described|p723|Devonian|Silurian|||||||
3981|Chillagoe Formation|23086|5|Briefly described|p664|||Hodgkinson Province.||||||
3981|Chillagoe Formation|23422|5|Briefly described|Plate 7.3|Early Carboniferous|Early Ordovician|||||||
3981|Chillagoe Formation|23423|4|Described|p302 Table 7.2|Early Devonian|Early Silurian|Hodgkinson Formation forms upper boundary, however relationship is transitional. Also see p232.  Underlying unit Mountain Creek Conglomerate (unconformable). Hodgkinson Province. Maximum thickness: 1200 m.||||||
3981|Chillagoe Formation|23424|5|Briefly described|p345|Early Devonian|Early Silurian|Hodgkinson Basin Province.||||||
3981|Chillagoe Formation|23426|5|Briefly described|p400 Fig 10.3|||||||||
3981|Chillagoe Formation|23430|4|Described|p471-473|||Hodgkinson Province.||||||
3981|Chillagoe Formation|23431|5|Briefly described|p539|||||||||
3981|Chillagoe Formation|23498|6|Mentioned|p21 table 1|||||||||
3981|Chillagoe Formation|23500|5|Briefly described|Map legend|Early Devonian|Early Silurian|Hodgkinson Province.||||||
3981|Chillagoe Formation|23501|5|Briefly described|map legend||Early Silurian|Age: Early Silurian - Early Devonian?||||||
3981|Chillagoe Formation|23502|5|Briefly described|Map Legend|Early Devonian|Early Silurian|Age: Early Silurian - Early Devonian?||||||
3981|Chillagoe Formation|23503|5|Briefly described|Map Legend|Early Devonian|Early Silurian|||||||
3981|Chillagoe Formation|23511|5|Briefly described|Map Legend|Early Devonian|Early Silurian|||||||
3981|Chillagoe Formation|23522|5|Briefly described|p250 Fig 6|Eifelian||||||||
3981|Chillagoe Formation|23616|4|Described|p5, Table 1C p14 p30|Early Devonian|Early Silurian|Faulted against Mulgrave Fm; faulted against or gradational transition into conformably overlying Hodgkinson Fm; intruded and hornfelsed by Permo-Carboniferous granitoids; overlain by volcanics of Featherbed Volcanic Group and by Glen Gordon Volcanics.||||||
3981|Chillagoe Formation|23617|6|Mentioned|p47|||||||||
3981|Chillagoe Formation|23624|4|Described|p9|||||||||
3981|Chillagoe Formation|23713|4|Described|p13|Early Devonian|Silurian|Hodgkinson Province.||||||
3981|Chillagoe Formation|24080|5|Briefly described|p445 Fig. 4|Devonian|Silurian|Volcanics, limestone, chert, sandstone and shale.  Geological Province: Laura Basin.||||||
3981|Chillagoe Formation|24086|5|Briefly described|p312 Fig. 1|Early Devonian|Early Devonian|||||||
3981|Chillagoe Formation|24213|5|Briefly described|p776 Fig. 1|Early Devonian|Early Silurian|||||||
3981|Chillagoe Formation|24485|3|Fully described|p3, p28 Tb.3a, p30 Tb.3b|Emsian|Llandovery|Faulted against the Kitoba Member. Geological Province: Hodgkinson Province||||||
3981|Chillagoe Formation|24486|5|Briefly described|Map legend|Early Devonian|Early Silurian|||||||
3981|Chillagoe Formation|24487|5|Briefly described|Map legend|||||||||
3981|Chillagoe Formation|29432|6|Mentioned|p56|||||||||
3981|Chillagoe Formation|29795|6|Mentioned|p271|||||||||
3981|Chillagoe Formation|30505|6|Mentioned|p4|||Upper Silurian to Lower Devonian||||||
3981|Chillagoe Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
3981|Chillagoe Formation|31453|6|Mentioned|p617|||||||||
3981|Chillagoe Formation|31822|6|Mentioned|p68|||Silurian - L.Devonian||||||
3981|Chillagoe Formation|31832|6|Mentioned|Table 6|||||||||
3981|Chillagoe Formation|31999|5|Briefly described|p143|||See also Table 11||||||
3981|Chillagoe Formation|32633|6|Mentioned|Fig. 1|||||||||
3981|Chillagoe Formation|33326|6|Mentioned|p448|||See also P449. Fauna.||||||
3981|Chillagoe Formation|33434|6|Mentioned|p22|||||||||
3981|Chillagoe Formation|33635|5|Briefly described|p758|||||||||
3981|Chillagoe Formation|33775|6|Mentioned|p756|||||||||
3981|Chillagoe Formation|33777|4|Described|p28|||Mention P26||||||
3981|Chillagoe Formation|33880|6|Mentioned|Map legend|Early Devonian|Early Silurian|L.Sil. - L.Dev.||||||
3981|Chillagoe Formation|34046|6|Mentioned|Table 1|||Late Sil.||||||
3981|Chillagoe Formation|34252|6|Mentioned|Ps.8|||Fossils||||||
3981|Chillagoe Formation|34346|6|Mentioned|p1|||||||||
3981|Chillagoe Formation|35008|5|Briefly described|p180|||||||||
3981|Chillagoe Formation|36101|6|Mentioned|p167|||||||||
3981|Chillagoe Formation|36299|5|Briefly described|p311|||||||||
3981|Chillagoe Formation|36527|6|Mentioned|p157|||||||||
3981|Chillagoe Formation|37565|6|Mentioned|Fig.6|||||||||
3981|Chillagoe Formation|37574|5|Briefly described|p195|||See also Fig.6||||||
3981|Chillagoe Formation|37575|3|Fully described|p176|||See also P183 & Fig.2. Formerly Chillagoe Group.||||||
3981|Chillagoe Formation|37727|4|Described|p45|||See also P22.||||||
3981|Chillagoe Formation|38573|6|Mentioned|p33|||||||||
3981|Chillagoe Formation|38688|5|Briefly described|p47|||||||||
3981|Chillagoe Formation|39445|5|Briefly described|p74|||See also P84 & Table 5||||||
3981|Chillagoe Formation|39650|6|Mentioned|Fig.1|||||||||
3981|Chillagoe Formation|39689|6|Mentioned|p54|||||||||
3981|Chillagoe Formation|39986|6|Mentioned|p75|||||||||
3981|Chillagoe Formation|39987|6|Mentioned|p66|||||||||
3981|Chillagoe Formation|39998|6|Mentioned|p191|||||||||
3981|Chillagoe Formation|40420|6|Mentioned|p84|||||||||
3981|Chillagoe Formation|40623|5|Briefly described|p87|||||||||
3981|Chillagoe Formation|40743|5|Briefly described|p310|||Mention Fig.1||||||
3981|Chillagoe Formation|40787|4|Described|p328|||||||||
3981|Chillagoe Formation|40892|4|Described|p74|||||||||
3981|Chillagoe Formation|40918|5|Briefly described|p102|||||||||
3981|Chillagoe Formation|40944|4|Described|p189|||||||||
3981|Chillagoe Formation|41272|5|Briefly described|M 1of1 E03|||See also M 1of1 A03||||||
3981|Chillagoe Formation|41425|5|Briefly described|p5|||||||||
3981|Chillagoe Formation|41569|6|Mentioned|p71|||||||||
3981|Chillagoe Formation|41772|4|Described|p435|||||||||
3981|Chillagoe Formation|41775|6|Mentioned|p71|||||||||
3981|Chillagoe Formation|41825|5|Briefly described|p204|||||||||
3981|Chillagoe Formation|42113|4|Described|p259|||||||||
3981|Chillagoe Formation|42500|4|Described|p12-91|||||||||
3981|Chillagoe Formation|42502|4|Described|p7|||||||||
3981|Chillagoe Formation|42620|3|Fully described|p64|||||||||
3981|Chillagoe Formation|42658|6|Mentioned|p16|||||||||
3981|Chillagoe Formation|42670|5|Briefly described|Figure 1 P26|||||||||
3981|Chillagoe Formation|42681|5|Briefly described|p17|||||||||
3981|Chillagoe Formation|42772|5|Briefly described|p16, Fig.18|||||||||
3981|Chillagoe Formation|42810|6|Mentioned|p8|||||||||
3981|Chillagoe Formation|43060|3|Fully described|p67|Early Devonian|Early Silurian|see also Table 5||||||
3981|Chillagoe Formation|43083|3|Fully described|p29, Table 4a.|Early Devonian|Early Silurian|Geological province: Hodgkinson Province.||||||17-JUN-09
3981|Chillagoe Formation|43087|5|Briefly described|p26, Fig.3|||||||||
3981|Chillagoe Formation|43098|5|Briefly described|p12|||||||||
3981|Chillagoe Formation|43103|6|Mentioned|p16|||||||||
3981|Chillagoe Formation|43124|6|Mentioned|p28|||||||||
3981|Chillagoe Formation|43151|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|43254|5|Briefly described|map legend|Early Devonian|Early Silurian|of Hodgkinson Province.||||||
3981|Chillagoe Formation|43285|5|Briefly described|Map Legend|Early Devonian|Early Silurian|||||||
3981|Chillagoe Formation|43461|14|Not recorded|p615||Silurian|||||||
3981|Chillagoe Formation|43530|14|Not recorded|p1038|||||||||
3981|Chillagoe Formation|43625|3|Fully described|p19,21|Early Devonian|Early Silurian|Fossiliferous limestones (M.Sil.-E.Dev.)||||||
3981|Chillagoe Formation|43626|6|Mentioned|p10|||||||||
3981|Chillagoe Formation|43729|6|Mentioned|p19|||||||||
3981|Chillagoe Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
3981|Chillagoe Formation|43896|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|43897|14|Not recorded|p91-2,98|Late Devonian|Middle Devonian|Middle to Late Devonian flysch deposits.||||||
3981|Chillagoe Formation|43898|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|43899|14|Not recorded|p276||Late Silurian|||||||
3981|Chillagoe Formation|43901|14|Not recorded|Map Legend||Late Silurian|(Early Devonian) - Late Silurian||||||
3981|Chillagoe Formation|43902|2|Defined|p116-121|||||||||
3981|Chillagoe Formation|43904|14|Not recorded|Map Legend|Late Silurian||(Early Devonian?)- Late Silurian||||||
3981|Chillagoe Formation|43927|14|Not recorded|p10|||||||||
3981|Chillagoe Formation|44043|14|Not recorded|p66|||Unconformably overlies Dargalong Metamorphics.||||||
3981|Chillagoe Formation|44068|14|Not recorded|p6,7|||Shallow  reef environment.||||||
3981|Chillagoe Formation|44091|14|Not recorded|p26,27,Tb.2,28,31||Silurian|||||||
3981|Chillagoe Formation|44246|5|Briefly described|Map Legend||Devonian|||||||
3981|Chillagoe Formation|44292|14|Not recorded|p14,17|||||||||
3981|Chillagoe Formation|44293|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|44294|2|Defined|p6,10,13,20,25,26|Early Devonian|Late Silurian|Tb.2||||||
3981|Chillagoe Formation|44296|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|44329|14|Not recorded|p5|||||||||
3981|Chillagoe Formation|44425|14|Not recorded|p3,11-12,16,22,31,|||opp.11,map. Fossils.||||||
3981|Chillagoe Formation|44542|14|Not recorded|p29|||||||||
3981|Chillagoe Formation|44843|14|Not recorded|p179|||||||||
3981|Chillagoe Formation|44880|14|Not recorded|unknown (p195-208)|||||||||
3981|Chillagoe Formation|45008|14|Not recorded|p11-115||Late Silurian|Late Silurian - ?Early Devonian||||||
3981|Chillagoe Formation|45009|14|Not recorded|p49,50|||Correlated with Kangaroo Hills Formation and Jack Limestone Member.||||||
3981|Chillagoe Formation|45014|14|Not recorded|p107||Silurian|||||||
3981|Chillagoe Formation|45025|2|Defined|p28-9|Early Devonian|Late Silurian|||||||
3981|Chillagoe Formation|45076|6|Mentioned|p56|||Structures||||||
3981|Chillagoe Formation|45113|6|Mentioned|p18|||||||||
3981|Chillagoe Formation|46879|6|Mentioned|p173|||||||||
3981|Chillagoe Formation|48850|14|Not recorded|Pl.14,15|||||||||
3981|Chillagoe Formation|48976|5|Briefly described|p4|||||||||
3981|Chillagoe Formation|60087|5|Briefly described|Map legend|Early Devonian|Late Silurian|Limestone, chert, sandstone, siltstone.||||||
3981|Chillagoe Formation|60332|6|Mentioned|p937|Devonian|Silurian|Contains conodonts.||||||
3981|Chillagoe Formation|60357|5|Briefly described|Map Legend|Early Devonian|Early Silurian|Geological Province: Hodgkinson Province.||||||
3981|Chillagoe Formation|60358|5|Briefly described|Map Legend|Early Devonian|Early Silurian|Geological Province: Hodgkinson Province.||||||18-AUG-04
3981|Chillagoe Formation|60425|3|Fully described|p13, p16 Tb. 1, p22-23, p45 Tb. 3|Emsian|Llandovery|Conformable below Hodgkinson Fm; unconformable below Featherbed Volcanic Gp (Jamtin Rhyolite), Nychum + Nanyeta Volcs. Geol.prov: Hodgkinson Prov. Intruded by Almaden Supersuite. Shallow marine shelf deposits - detailed lithology presented.See also p167.||||||07-FEB-11
3981|Chillagoe Formation|62371|5|Briefly described|p470 Fig.1|Early Devonian|Ordovician|Geological Province: Hodgkinson Province. See also p472 Fig.3||||||
3981|Chillagoe Formation|63140|4|Described|p569-583.|Silurian|Silurian|Major, trace and REE geochemistry are detailed. Sub-continental lithosphere sourced basalts. Hosts King Vol massive sulphide deposit.|c.555 Ma.||||Basalt and basaltic andesite, metamorphosed, fine-grained, occasionally pillowed and brecciated; interspersed with mature shallow-marine sedimentary rocks and limestones.|
3981|Chillagoe Formation|63154|5|Briefly described|p281 Fig. 3|Silurian|Silurian|Geological province: Hodgkinson Province.||||||11-APR-07
3981|Chillagoe Formation|64769|6|Mentioned|p26|Early Devonian|Silurian|QLD.||||||05-MAY-09
3981|Chillagoe Formation|65214|6|Mentioned|p279|Devonian|Devonian|QLD, Hodgkinson. Mis-spelt as Chillage on p275. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3981|Chillagoe Formation|68330|5|Briefly described|Map legend.|Early Devonian|Early Silurian|Hodgkinson Province. Two facies associations are mapped separately.|||||Labile arenite, conglomeratic arenite, mudstone, siltstone, minor conglomerate, calc-silicate rocks, skarn; polymictic conglomerate and conglomeratic arenite, minor labile arenite, mudstone, calc-silicate rocks.|
3981|Chillagoe Formation|68331|5|Briefly described|Map legend.|Early Devonian|Early Silurian|Hodgkinson Province. Two facies associations are mapped separately.|||||Labile arenite, conglomeratic arenite, mudstone, siltstone, minor conglomerate, calc-silicate rocks, skarn; polymictic conglomerate and conglomeratic arenite, minor labile arenite, mudstone, calc-silicate rocks.|
3981|Chillagoe Formation|68337|5|Briefly described|Map legend|Early Devonian?|Early Silurian|Seven facies associations are mapped separately.|||||Polymictic pebble to boulder conglomerate; conglomeratic arenite; quartzose arenite; fine- to medium-grained quartzite; fossiliferous limestone and limestone breccia, marble, calc-silicate rocks; metabasalt; chert and silicified mudstone.|
3981|Chillagoe Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Hodgkinson Province. ||||||
3981|Chillagoe Formation|68576|5|Briefly described|Q_11: p13-14, p16-17|Early Devonian|Silurian|Rocks formed on a rifted continental margin in a variety of environments from deep water to unstable carbonate ramps. Repetition of units by numerous thrusts complicates the geology. Telychian-Emsian. Hosts a variety of karst features as tourist attractions.|||||Limestone (locally allochthonous blocks), generally lime mud variably recrystallised to marble, locally fossiliferous; chert, siliciclastic sedimentary rocks, tholeiitic basalt.|
3981|Chillagoe Formation|68822|5|Briefly described|p320 Fig.3, p337|Early Devonian|Early Devonian|MORB volcanics. Hodgkinson Province. Shallow water depositional environment. Largely overturned with east dips and west youngings.|||||MORB volcanics.|27-JUL-15
3981|Chillagoe Formation|69030|5|Briefly described|p2, p6, p14|Early Devonian|Early Silurian|Chillagoe Subprovince, Hodgkinson Province. A narrow western belt of shallow marine rocks.|||||Shallow-marine sedimentary rocks (commonly limestone) and basalt.|
3981|Chillagoe Formation|69079|6|Mentioned|p3-4|||Hodgkinson Province.||||||
3981|Chillagoe Formation|69582|5|Briefly described|p70|Devonian|Silurian|Hodgkinson Province.||||Overlain by the Hodgkinson Formation.|Abundant limestones.|
3981|Chillagoe Formation|69592|4|Described|p230-236, p245, p296-298, p301-303|Devonian|Silurian|Mossman Orogen, Chillagoe Subprovince, Hodgkinson Province. Crops out as a discontinuous belt, 200km long and 200m to 10km wide, parallel to the Palmerville Fault. Limestone is characteristic and forms prominent bluffs and karst topography. Less-mature siliciclastic rocks. Lithologies described in detail. Diverse fossil fauna. Complex internal structure; strata generally overturned. Best considered as being dismembered into a set of imbricate thrust sheets. Several photographs. Geochemical plots.||||Structurally intercalated with Mulgrave Formation.|Limestone (apparent thickness ~1 km), chert, voluminous mafic volcanic rocks (substantial stratiform basalt sheets, associated geochemically-identical hypabyssal dolerite, and volcaniclastics), and quartzofeldspathic sandstone.|
3981|Chillagoe Formation|70207|5|Briefly described|p1, p74, p94, p96||Silurian|Thomson Orogen. Minimum age given as Early Devonian?.||||Structurally intercalated with Mulgrave Formation.||
3981|Chillagoe Formation|70345|6|Mentioned|p1, p3-4, p14|Devonian|Silurian|Of the Hodgkinson province.||||Faulted against the Hodgkinson Formation.||
3981|Chillagoe Formation|70673|6|Mentioned|p7|Early Devonian?|Silurian|||||||
3981|Chillagoe Formation|71031|5|Briefly described|p4, p70-p71, p73, p77|Lower Devonian|Early Silurian|Included in the Mossman Orogen by Henderson and Donchak (2013).||||Conformably overlain by the Mulgrave Formation.|Quartzofeldspathic sandstone, metabasalt, chert and limestone.|
3981|Chillagoe Formation|72297|5|Briefly described|p718, p726, p739|Silurian|Silurian|Hodgkinson Province. Hosts significant skarn-style base metal mineralisation associated with Late Carboniferous activity of the Kennedy Igneous Association. Marble formed by contact metamorphism is used for dimension stone for local and export markets. Numerous undeveloped wollastonite deposits occur in skarn-related calc-silicate alteration zones around granitic intrusions.||||Is intruded by Hammonds Creek Granodiorite.|Limestone.|
3981|Chillagoe Formation|72983|6|Mentioned|p15|Early Devonian|Silurian|Mossman Orogen.||||||
3981|Chillagoe Formation|73595|6|Mentioned|p1134|||Hodgkinson Province, Mossman Orogen.||||||
3991|Chillingham Volcanics|22857|4|Described|p284, p542 App.1 Tb.A1.11|Late Triassic|Early Triassic|Rhyolitic lavas, ignimbrites and airfall tuffs interbedded with non-marine strata, mainly conglomerate. Max. thickness: 200m. Geological Province: Ipswich Basin (under Clarence-Moreton Basin).||||||
3991|Chillingham Volcanics|22861|5|Briefly described|p284|||||||||
3991|Chillingham Volcanics|22865|6|Mentioned|Fig22.9p317|||||||||
3991|Chillingham Volcanics|23811|5|Briefly described|Map Legend|Norian|Carnian|Alkali basalt and andesite; basalt is massive and columnar-jointed; the andesite includes massive and banded varieties overlain by hyaloclastite. Geological Province: Clarence-Moreton Basin.||||||11-JAN-10
3991|Chillingham Volcanics|23812|5|Briefly described|p31, p35 Tb.4|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin. Maximum thickness: 1500m.||||||21-SEP-05
3991|Chillingham Volcanics|23888|6|Mentioned|p262|||||||||
3991|Chillingham Volcanics|24082|6|Mentioned|p452|||||||||
3991|Chillingham Volcanics|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|24299|5|Briefly described|p3|Triassic|Triassic|||||||
3991|Chillingham Volcanics|29995|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|30131|4|Described|p8|||Lithology||||||
3991|Chillingham Volcanics|30302|6|Mentioned|p414|||See also P415||||||
3991|Chillingham Volcanics|30687|4|Described|p63|||See also P64,65,76. Triassic age||||||
3991|Chillingham Volcanics|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|33004|6|Mentioned|p78|||See also P225||||||
3991|Chillingham Volcanics|33476|6|Mentioned|Fig.10|||||||||
3991|Chillingham Volcanics|33881|6|Mentioned|p96|||||||||
3991|Chillingham Volcanics|34340|3|Fully described|p542|||Triassic. See Table 6.1||||||29-SEP-05
3991|Chillingham Volcanics|34593|6|Mentioned|p539|||Triassic. Equivalent Copes Creek Tuff.||||||24-SEP-08
3991|Chillingham Volcanics|34755|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|35007|6|Mentioned|p75|||||||||
3991|Chillingham Volcanics|35126|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|35156|4|Described|p6|||See also Table.2||||||
3991|Chillingham Volcanics|37065|6|Mentioned|p36|||||||||
3991|Chillingham Volcanics|37112|5|Briefly described|p298|||||||||
3991|Chillingham Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|38074|5|Briefly described|Table 1|||||||||
3991|Chillingham Volcanics|38307|6|Mentioned|p523|||||||||
3991|Chillingham Volcanics|38837|6|Mentioned|p235|||Geological Province: New England Fold Belt||||||
3991|Chillingham Volcanics|39445|6|Mentioned|Table 9|||||||||
3991|Chillingham Volcanics|40245|6|Mentioned|p185|||Mention Fig.2||||||
3991|Chillingham Volcanics|40328|6|Mentioned|p195|||||||||
3991|Chillingham Volcanics|40479|6|Mentioned|p32|||||||||
3991|Chillingham Volcanics|40517|6|Mentioned|p358|||||||||
3991|Chillingham Volcanics|40623|5|Briefly described|p40|||||||||
3991|Chillingham Volcanics|40780|4|Described|p5|||||||||
3991|Chillingham Volcanics|40784|6|Mentioned|p982|||||||||
3991|Chillingham Volcanics|41591|5|Briefly described|p18|||||||||
3991|Chillingham Volcanics|41738|6|Mentioned|p168|||||||||
3991|Chillingham Volcanics|42041|6|Mentioned|Fig.5 P227|||||||||
3991|Chillingham Volcanics|42182|5|Briefly described|p302|||||||||
3991|Chillingham Volcanics|42317|5|Briefly described|p2|||||||||
3991|Chillingham Volcanics|43001|5|Briefly described|p121|||||||||
3991|Chillingham Volcanics|43003|6|Mentioned|Fig.21,p173|||||||||
3991|Chillingham Volcanics|43092|5|Briefly described|p31|||||||||
3991|Chillingham Volcanics|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
3991|Chillingham Volcanics|43161|5|Briefly described|14, 36||Triassic|||||||
3991|Chillingham Volcanics|43383|14|Not recorded|p24||Triassic|||||||
3991|Chillingham Volcanics|43384|14|Not recorded|Map Legend||Triassic|||||||
3991|Chillingham Volcanics|43479|14|Not recorded|p224,243||Early Triassic|||||||
3991|Chillingham Volcanics|43736|6|Mentioned|p3||Middle Triassic|||||||
3991|Chillingham Volcanics|43881|14|Not recorded|p6-7,10,13,29,34,49|||p51-52,58(anal.)66,80,143,168-9||||||
3991|Chillingham Volcanics|45003|14|Not recorded|p107|||QLD and NSW||||||
3991|Chillingham Volcanics|48917|6|Mentioned|p9|||Correlation||||||
3991|Chillingham Volcanics|60281|6|Mentioned|p25|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|60993|6|Mentioned|p8 Tb. 2|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|60996|6|Mentioned|p76|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|61002|5|Briefly described|p202|Middle Triassic|Middle Triassic|Felsic to basaltic rocks. Conformably overlain by Ipswich C.M. See also p199 Fig. 3.||||||
3991|Chillingham Volcanics|61006|6|Mentioned|p277|Middle Triassic|Middle Triassic|||||||
3991|Chillingham Volcanics|61310|5|Briefly described|p14 Fig. C5, p34|||Overlain by Ipswich Coal Measures. Geological Province: Clarence-Moreton Basin. Equivalent to Nymboida Coal Measures.||||||24-SEP-08
3991|Chillingham Volcanics|61772|6|Mentioned|p128, p129 Fig. 4||Middle Triassic|In New England Orogen.||||||24-SEP-08
3991|Chillingham Volcanics|61775|6|Mentioned|p182 Fig. 1|||||||||
3991|Chillingham Volcanics|64665|6|Mentioned|p53 Fig.2.|Late Triassic|Late Triassic|Ipswich Basin.||||||
3991|Chillingham Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
3991|Chillingham Volcanics|66855|5|Briefly described|pp955-956.|Late Triassic|Late Triassic|Andesitic rocks at Evans Head included (Scott 1982) with New England Fold Belt; basaltic rocks  were mapped as correlates of Tertiary Lismore Basalt. This study shows they are both part of a Late Triassic volcanic province extending 360 km to the north.|||||Rhyolitic pyroclastic rocks and lavas; associated volcanic rocks including basaltic andesites in southern Queensland.|
3991|Chillingham Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
3991|Chillingham Volcanics|67402|5|Briefly described|p222, p223|Carnian|Ladinian|Ipswich Basin.|||||Sub-aerial tuffaceous conglomerate and sandstone.|
3991|Chillingham Volcanics|68327|5|Briefly described|Map legend.|Triassic|Triassic||||||Rhyolite flows and tuff.|
3991|Chillingham Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
3991|Chillingham Volcanics|68679|5|Briefly described|p388, p392-394, p433-435|Late Triassic|Late Triassic|Base of the Ipswich Basin: Brisbane/Beenleigh/offshore. Previously thought equivalent to Nymboida Coal Measures, but contradicted by macrofloral and radiometric dating.|||||Early pyroclastic phase: rhyolitic ignimbrites (<1m to ~200m thick) with abundant felsic volcanic lithic fragments; less common air fall and surge deposits associated with epiclastic sediments; later effusive phase of flow-banded felsic lava flows.|
3991|Chillingham Volcanics|69594|6|Mentioned|p519, p543|||Ipswich Basin.||||Is overlain by Ipswich Coal Measures and locally by Raceview Formation.||
3991|Chillingham Volcanics|72297|5|Briefly described|p755, p758|Triassic|Triassic|Source of thunder eggs at Thunderbird Park at Mount Tamborine. At Back Creek, SE of Canungra, amethyst and quartz crystals occur with chalcedony and common opal in veins in this unit.|||||Spherulitic rhyolite.|
3991|Chillingham Volcanics|73306|5|Briefly described|p564-566, 568, 572 Fig.8|Late Triassic|Late Triassic|||||Probable equivalent to the Brisbane Tuff.|A thick sequence of rhyolite and tuff.|
3991|Chillingham Volcanics|73450|5|Briefly described|p38|||Gold Coast hinterland. Divided into a lower and upper package (Roach, 1993; 1996).|||||Felsic pyroclastic deposits including ignimbrites up to ca 200 m thick with abundant felsic volcanic lithic fragments, flow-banded felsic lava flows, less common airfall and surge deposits, and epiclastic sedimentary rocks.|
4013|Chinghee Conglomerate|30604|6|Mentioned|p66|||||||||
4013|Chinghee Conglomerate|30687|4|Described|p64|||See also P65. Miocene age.||||||
4013|Chinghee Conglomerate|31130|6|Mentioned|Fig. 2|||Lower Miocene||||||
4013|Chinghee Conglomerate|32491|6|Mentioned|p25|||Early Miocene||||||
4013|Chinghee Conglomerate|32924|6|Mentioned|p112|||Refers McTaggart (1962)||||||
4013|Chinghee Conglomerate|35296|4|Described|p13|||See also P12.||||||
4013|Chinghee Conglomerate|39445|5|Briefly described|Table 14|||||||||
4013|Chinghee Conglomerate|40623|5|Briefly described|p39|||||||||
4013|Chinghee Conglomerate|40780|5|Briefly described|p9|||||||||
4013|Chinghee Conglomerate|40896|4|Described|p47|||||||||
4013|Chinghee Conglomerate|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
4013|Chinghee Conglomerate|44813|14|Not recorded|p80,81,88||Tertiary|||||||
4013|Chinghee Conglomerate|44871|2|Defined|p139|Tertiary|Tertiary|of Lamington Group.||||||
4013|Chinghee Conglomerate|48917|6|Mentioned|p33|||Refers McTaggart. Stratigraphic relationships||||||
4013|Chinghee Conglomerate|69599|5|Briefly described|p595, p640|Miocene|Miocene|Up to 30m thick. Includes cobbles and boulders sourced from the Mount Barney Granophyre. Underlies Tweed volcano lavas. Contains sporadic dicotyledonous leaves.||Lamington Volcanics.||Overlies the Mount Gillies Rhyolite.|Sandstone with siltstone lenses, and coarse-boulder polymictic conglomerate.|
4013|Chinghee Conglomerate|73450|4|Described|p96, 98|||Associated with the Focal Peak volcano. Parts appear to fill deep gorges and paleovalleys. Include boulder-sized clasts of Mount Gillies Rhyolite, granophyre from the Mount Barny Central Complex, Mesozoic and Carboniferous sedimentary rocks, basalt and fluidal riebeckite-bearing comendite.||||Underlain by Mount Gillies Rhyolite. Overlain by Beechmont Basalt.|Fluvial conglomerate and coarse, feldspathic sandstones that are variably cemented; possibly includes lahar deposits.|
4041|Chowey Granite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
4041|Chowey Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
4041|Chowey Granite|39445|5|Briefly described|Table 12|||See also P101. Mid Permian.||||||14-AUG-08
4041|Chowey Granite|39505|6|Mentioned|p180|||||||||
4041|Chowey Granite|40475|6|Mentioned|p9|||||||||
4041|Chowey Granite|40919|6|Mentioned|Fig.2|||||||||
4041|Chowey Granite|41778|4|Described|p373|||||||||
4041|Chowey Granite|43008|5|Briefly described|map legend|||||||||
4041|Chowey Granite|45440|2|Defined|p.60,61||Triassic|Tb.1.||||||
4041|Chowey Granite|63821|5|Briefly described|p28|Late Permian|Early Permian|Age: 273+/-3Ma and 275+/-3Ma  (K-Ar biotite) and 266+/3Ma (K-Ar hornblende). Intrudes Good Night beds.Comprises hornblende-biotite granite.||||||07-FEB-11
4041|Chowey Granite|68679|5|Briefly described|p410, p420-421|Permian|Permian|Gayndah-Gladstone belt, southern part of the northern New England Orogen. Late Permian.|273 +/- 3 Ma (K-Ar: Dept. of Mines, 1982).|||Intrudes the Good Night beds and Shoalwater Formation. Is overlain by Toogoolawah Group and Aranbanga Volcanic Group.|Dominantly medium- to coarse-grained, hornblende-biotite granite with albite and perthitic orthoclase. Original descriptions suggested a syenitic margin grading into a granitic core. I-type.|
4056|Chudleigh Basalt|22744|5|Briefly described|P13, Table4, Fig2|Holocene|Pliocene|||||||
4056|Chudleigh Basalt|23220|6|Mentioned|p16|||||||||
4056|Chudleigh Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Age: Basalt flow in Einasleigh River is 0.26Ma; up to 8Ma in Clarke River Region. Geological Province: Georgetown Region.||||||08-JUL-15
4056|Chudleigh Basalt|23424|4|Described|Table 8.1|||Age: Mostly between 2.08 Ma and 0.25 Ma; but some as old as 8 Ma.||||||
4056|Chudleigh Basalt|23493|6|Mentioned|p16 Tb. 1|||On CLARKE RIVER Sheet.  Correlated with McBride Basalt.||||||
4056|Chudleigh Basalt|23494|5|Briefly described|p18 Tb. 1|Cenozoic|Cenozoic|Olivine basalt.  Max. thickness: <500ft.||||||19-NOV-08
4056|Chudleigh Basalt|23495|5|Briefly described|map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4056|Chudleigh Basalt|23498|5|Briefly described|p20 table 1||Cenozoic|||||||19-NOV-08
4056|Chudleigh Basalt|24013|5|Briefly described|p17 Tb. 1|Tertiary|Tertiary|Olivine basalt.  Correlated with the Nulla Basalt and McBride Basalt.  Max. thickness: ?100ft.  Geological Province: Great Artesian Basin.||||||
4056|Chudleigh Basalt|30587|6|Mentioned|Map legend|Holocene|Pliocene|Pliocene to Holocene||||||
4056|Chudleigh Basalt|31832|6|Mentioned|Table 6|||||||||
4056|Chudleigh Basalt|32553|4|Described|p34|||||||||
4056|Chudleigh Basalt|33638|5|Briefly described|Table 2|||||||||
4056|Chudleigh Basalt|33643|6|Mentioned|Map legend|Quaternary|Tertiary|Tertiary-Quaternary||||||
4056|Chudleigh Basalt|33958|6|Mentioned|p40|||See also p45.||||||21-MAY-15
4056|Chudleigh Basalt|34046|6|Mentioned|Table III|||Late Tert.||||||
4056|Chudleigh Basalt|34998|6|Mentioned|p347|||||||||
4056|Chudleigh Basalt|39027|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4056|Chudleigh Basalt|39445|5|Briefly described|Table 14|||Sapphires. See also P152||||||
4056|Chudleigh Basalt|39917|6|Mentioned|Map legend|Quaternary|Tertiary|Tertiary-Quaternary||||||
4056|Chudleigh Basalt|41680|6|Mentioned|p106|||||||||
4056|Chudleigh Basalt|43253|5|Briefly described|map legend|Quaternary||||||||
4056|Chudleigh Basalt|44048|14|Not recorded|Map Legend|Pleistocene|Pliocene|||||||
4056|Chudleigh Basalt|44049|14|Not recorded|Map Legend|Pleistocene|Pliocene|||||||
4056|Chudleigh Basalt|44542|14|Not recorded|p28|||||||||
4056|Chudleigh Basalt|44800|14|Not recorded|p22|||(early Mid Pleistocene, late Tertiary)||||||
4056|Chudleigh Basalt|45009|14|Not recorded|p75,91,92,100|||||||||
4056|Chudleigh Basalt|45014|14|Not recorded|Pl.38|||||||||
4056|Chudleigh Basalt|50200|5|Briefly described|Map Legend|Quaternary|Tertiary|Includes: Barkers Flow.||||||
4056|Chudleigh Basalt|50201|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4056|Chudleigh Basalt|60360|5|Briefly described|Map Legend|Quaternary|Quaternary|Olivine basalt. Grouped with Barkers Flow. Age: 0.26Ma.||||||19-AUG-04
4056|Chudleigh Basalt|64707|5|Briefly described|Map legend|Quaternary|Quaternary|Predominantly olivine basalt (volcanic cone or vent).||||||
4056|Chudleigh Basalt|68338|5|Briefly described|Map legend.|Neogene|Neogene|Chudleigh Province.|||||Olivine basalt, scoria, volcanic cone or vent.|
4056|Chudleigh Basalt|68346|5|Briefly described|Map legend.|Quaternary|Quaternary|Of Chudleigh Basalt Province.|||Includes Barkers Flow.||Olivine basalt.|
4056|Chudleigh Basalt|68410|5|Briefly described|Map Legend|Quaternary|Tertiary|Chudleigh Basalt Province.|||Includes Barkers Flow.||Olivine basalt, scoria (vent).|
4056|Chudleigh Basalt|68477|5|Briefly described|Map Legend|Quaternary|Quaternary||||Includes Barkers Flow.|||
4056|Chudleigh Basalt|68478|6|Mentioned|Map Legend|Quaternary|Quaternary|Chudleigh Province.|||||Olivine basalt.|
4056|Chudleigh Basalt|68479|6|Mentioned|Map Legend|Quaternary|Quaternary|Chudleigh Province.|||||Olivine basalt.|
4056|Chudleigh Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, McIvor River, McLean, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
4056|Chudleigh Basalt|68576|6|Mentioned|Q_11: p20 Fig.17|Pleistocene|Pliocene|Gives its name to the Chudleigh Basalt Province which also includes the Barkers Basalt.||||||
4056|Chudleigh Basalt|72297|5|Briefly described|p757|Cenozoic|Cenozoic|Gem quality anorthoclase occurs in a scoria vent at Moonstone Hill, between Hughenden and Mount Garnet.||||||
4064|Chumvale Breccia|22461|5|Briefly described|Fig 2 p466.|||of Overhang Jaspilite.||||||
4064|Chumvale Breccia|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4064|Chumvale Breccia|30531|1|Redefined|p18|Precambrian|Precambrian|Everywhere associated with the Overhang Jaspilite. Of Mary Kathleen Group.||||||
4064|Chumvale Breccia|33900|6|Mentioned|p17|||||||||
4064|Chumvale Breccia|35167|6|Mentioned|p154|||||||||
4064|Chumvale Breccia|38276|6|Mentioned|Fig.1|||||||||
4064|Chumvale Breccia|39445|6|Mentioned|p43|||See also Table 2||||||
4064|Chumvale Breccia|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
4064|Chumvale Breccia|41306|6|Mentioned|p12|||||||||
4064|Chumvale Breccia|41791|6|Mentioned|p249|||||||||
4064|Chumvale Breccia|41978|6|Mentioned|p491|||||||||
4064|Chumvale Breccia|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
4064|Chumvale Breccia|44271|14|Not recorded|p31|||||||||
4064|Chumvale Breccia|44275|14|Not recorded|Map Legend|||||||||
4064|Chumvale Breccia|44278|2|Defined|Tb.1,map||Paleoproterozoic|||||||07-NOV-08
4064|Chumvale Breccia|44989|2|Defined|p.95|||Tb.111. On many pages. (F54-2).||||||
4064|Chumvale Breccia|45161|6|Mentioned|p48|||||||||
4064|Chumvale Breccia|45166|5|Briefly described|p23|||||||||
4064|Chumvale Breccia|64250|5|Briefly described|p13 fig.5, p14-15|||Tommy Creek Block, Mount Isa Inlier. Appears as Chumvale Bx in Fig.5, for reasons of space.||Mary Kathleen Group.||Along with Overhang Jaspilite, correlated with Corella Formation.||19-MAR-18
4064|Chumvale Breccia|65396|6|Mentioned|p17, p180, p183|||Cover Sequence 3. Tommy Creek Block. Appears as Chumvale BX on p17.||Mary Kathleen Group||Assumed to correlate with Corella Formation.||
4064|Chumvale Breccia|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p16|Paleoproterozoic|Paleoproterozoic|Mitakoodi Domain, Leichhardt Superbasin. Described as "enigmatic" and of unknown origin.||Overhang Jaspilite.|||Quartzite breccia with jaspilite remnants|
4064|Chumvale Breccia|69056|5|Briefly described|p13, p53|||Geological Survey of Queensland (2011). Combined with other units to form the Mitakoodi Formation, a regionally discrete unit for modelling purposes.||||Overlies Mitakoodi Quartzite. Is overlain by Corella Formation.|Siliceous.|
4064|Chumvale Breccia|69591|5|Briefly described|p35, p57|||Mitakoodi Domain, Mount Isa Province. Part of Quilalar Supersequence. Described as "enigmatic, of unknown origin".||Overhang Jaspilite.|||Quartzite breccia.|
4064|Chumvale Breccia|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartzite breccia.|
4064|Chumvale Breccia|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartzite breccia.|
4064|Chumvale Breccia|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as younger and partly equivalent to the Malbon Group.||||Partially overlies and equivalent to Overhand Jaspilite, but is not a part of the Malbon Group.|Quartzite breccia.|
4064|Chumvale Breccia|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as younger and partly equivalent to the Malbon Group.||||Partially overlies and equivalent to Overhang Jaspilite, but is not a part of the Malbon Group.|Quartzite breccia.|
4077|Claddagh Granodiorite|22845|6|Mentioned|p35,51,58-63,78,9|||||||||
4077|Claddagh Granodiorite|22846|3|Fully described|p6-15,18,20,41,75|Early Permian|Westphalian|Possible lateral continuation of Gallangowan Granodiorite.||||||
4077|Claddagh Granodiorite|23251|6|Mentioned|p29||Late Carboniferous|Crouch & others (1995) Synkinematic S-type granitoid.||||||
4077|Claddagh Granodiorite|23440|5|Briefly described|p147|Carboniferous|Carboniferous|||||||
4077|Claddagh Granodiorite|23608|4|Described|p50 Fig 1, p51 Fig 3.||Carboniferous|307 Ma. Transitional S- to I-type granite.  Of Wratten Igneous Suite. North D'Aguilar Block.||||||
4077|Claddagh Granodiorite|23609|5|Briefly described|p7, 9|||North D'Aguilar Block.||||||
4077|Claddagh Granodiorite|23799|5|Briefly described|p23, p123|Early Permian|Late Carboniferous|Geological Province: North D'Aguilar Subprovince.||||||
4077|Claddagh Granodiorite|29968|6|Mentioned|p15|||Upper Carboniferous||||||
4077|Claddagh Granodiorite|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4077|Claddagh Granodiorite|31450|6|Mentioned|p47|||||||||
4077|Claddagh Granodiorite|35101|3|Fully described|p67|||||||||
4077|Claddagh Granodiorite|36528|6|Mentioned|p174|||||||||
4077|Claddagh Granodiorite|37252|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4077|Claddagh Granodiorite|37376|6|Mentioned|Table 1|||||||||
4077|Claddagh Granodiorite|39445|5|Briefly described|Table 12|||||||||
4077|Claddagh Granodiorite|40475|6|Mentioned|p9|||||||||
4077|Claddagh Granodiorite|40478|6|Mentioned|p24|||||||||
4077|Claddagh Granodiorite|41272|6|Mentioned|M 1of1 J15|||||||||
4077|Claddagh Granodiorite|41917|6|Mentioned|p522|||||||||
4077|Claddagh Granodiorite|42547|5|Briefly described|p56|||||||||
4077|Claddagh Granodiorite|42619|5|Briefly described|p29|||||||||
4077|Claddagh Granodiorite|42694|5|Briefly described|map legend|Carboniferous|Pre-Carboniferous|||||||
4077|Claddagh Granodiorite|43008|5|Briefly described|map legend|||||||||
4077|Claddagh Granodiorite|43092|4|Described|p22|||see also map enclosure||||||
4077|Claddagh Granodiorite|43588|6|Mentioned|p30||Late Carboniferous|||||||
4077|Claddagh Granodiorite|44923|5|Briefly described|Map Legend||Carboniferous|||||||
4077|Claddagh Granodiorite|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
4077|Claddagh Granodiorite|60077|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Coarse-grained leucocratic granodiorite.||||||19-JUL-04
4077|Claddagh Granodiorite|61782|5|Briefly described|p276|Late Carboniferous|Late Carboniferous|Nonconformity with Toogoolawah Group.||||||
4077|Claddagh Granodiorite|63821|5|Briefly described|p19|Late Carboniferous|Late Carboniferous|Geological Province: Esk Trough.||||||07-FEB-11
4077|Claddagh Granodiorite|65114|5|Briefly described|p397|Kasimovian||In the North D'Aguilar Block; 40Ar/39Ar plateau ages of 306.9 +/- 1.2 Ma and 306.5 +/- 0.6 Ma||||||
4077|Claddagh Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Capsize Creek Complex; the Coppermine Creek, Gallangowan, Karandah and Yabba Creek Granodiorites, are all mapped under the same symbol, Cgd.||||||
4077|Claddagh Granodiorite|68679|5|Briefly described|p320, p323, p325-326, p331-332, p403-405|Late Carboniferous|Late Carboniferous|See also p470. Kilkivan-Manumbar area, North D'Aguilar Subprovince. Syntectonic granitoids. Part of the Claddagh-Manumbar Assemblage. The Wide Bay Creek Gneiss is interpreted as an early marginal phase of this unit. Minimum age of 306.5 +/- 0.6 Ma (Little et al., 1993) is from a cross-cutting dyke. Cooling ages given.|>306 Ma.|Wratten Igneous Suite.|||Homogeneous, medium- to coarse-grained biotite granodiorite.|
4077|Claddagh Granodiorite|73197|6|Mentioned|p472 Tb.2|Artinskian|Artinskian|New England Orogen, northern.|289.0 +/- 1.1 Ma Ar-Ar (Kfs) age|Wratten Suite||||
4090|Claraville beds|23425|4|Described|p384, Table 9.7 p393.|||Geological Province Karumba Basin.||||||
4090|Claraville beds|23430|5|Briefly described|p526|||||||||
4090|Claraville beds|23496|5|Briefly described|Table 4, p61|Pleistocene|Pliocene|~70m thick.||||||
4090|Claraville beds|40659|6|Mentioned|p250|||Mention P254||||||
4090|Claraville beds|42637|6|Mentioned|p32|||||||||
4090|Claraville beds|43287|5|Briefly described|Map Legend|Quaternary|Neogene|||||||
4090|Claraville beds|61155|5|Briefly described|p16|Pleistocene|Late Pliocene|Together with Armraynald and Wondoola beds thickness is 70m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
4090|Claraville beds|67402|5|Briefly described|p177 tbl CRP/KRM1|Quaternary|Neogene|Karumba Basin. Deposited in a fluvial to paralic environment. Unsuitable reservoir for the storage of carbon dioxide. See also p181 tbl CRP/KRM2, p239.||||Unconformably overlies the Wyaaba beds.|Silt, clay, clayey quartzose sand and gravel.|
4090|Claraville beds|69599|5|Briefly described|p585, p603|Pleistocene|Pliocene|Claraville Plains, onshore Carpentaria region. Up to 70m thick.||||Correlated with Armraynald and Wondoola beds.|Clayey quartzose sand, sandy mud and minor gravel.|
4101|Claret Creek Ring Complex|23423|5|Briefly described|p309 Table 7.3|||Claret Creek Supersuite.||||||
4101|Claret Creek Ring Complex|23502|5|Briefly described|Map Legend||Late Carboniferous|of Claret Creek Supersuite.||||||
4101|Claret Creek Ring Complex|23616|6|Mentioned|Table 3 p55|||||||||
4101|Claret Creek Ring Complex|23624|6|Mentioned|p7|||||||||
4101|Claret Creek Ring Complex|36527|3|Fully described|p160|||||||||
4101|Claret Creek Ring Complex|43060|5|Briefly described|p100|||of Claret Creek Supersuite||||||
4101|Claret Creek Ring Complex|43259|6|Mentioned|Appendix 1,p9.||Carboniferous|||||||
4101|Claret Creek Ring Complex|45014|14|Not recorded|p10,45,68,78,85,98-9|||p136,Tb.1,Pl.25. Used as structural term.||||||
4101|Claret Creek Ring Complex|48976|6|Mentioned|p28|||Age||||||
4101|Claret Creek Ring Complex|60425|5|Briefly described|p40, p50 Tb. 3|||Structural term. One of several extensively eroded volcanic complexes in SW part of Cairns Region. Assoc'd with Claret Creek Volcanics which, together with other comagmatic intrusive rocks of the complex, are assigned to the Claret Creek Supersuite.||||||07-FEB-11
4101|Claret Creek Ring Complex|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Appears to be an alternative name for the Claret Creek Supersuite.|||Includes Claret Creek Volcanics, Munderra Granodiorite, Three Mile Microgranite, The Gorge Rhyolite and Ballast Creek Dacite.|||
4101|Claret Creek Ring Complex|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Appears to be an alternative name for the Claret Creek Supersuite.|||Includes Claret Creek Volcanics, Munderra Granodiorite, Three Mile Microgranite, The Gorge Rhyolite and Ballast Creek Dacite.|||
4105|Clarke Island Ignimbrite|32706|6|Mentioned|Table 1|||Refs. Jones & Jones.||||||07-OCT-08
4118|Clayhole Tuff Member|24613|5|Briefly described|p38|||Originally called "Clayhole Tuff Member" by Wyatt (1973) - his informal name for a 3m interval containing olive green, fine- to coarse-grained rhyolitic tuff - within Vanneck Formation; marker bed ( see p37)..||||||07-FEB-11
4118|Clayhole Tuff Member|37573|6|Mentioned|p210|||||||||
4118|Clayhole Tuff Member|38658|6|Mentioned|p152|||||||||
4118|Clayhole Tuff Member|39686|6|Mentioned|p78|||||||||
4118|Clayhole Tuff Member|62522|5|Briefly described|p23-24|Frasnian|Frasnian|Of Vanneck Fm. Useful marker bed in upper third of Vanneck Fm. Thickness: up to 3m. Fine- to coarse-gr.rhyolitic tuff (?ignimbrite) + pumice/ lithic fragments/glass shards in matrix. Geol.Prov: Burdekin Basin. See also Clay Hole Mbr - both names used||||||08-OCT-08
4118|Clayhole Tuff Member|68731|5|Briefly described|p186|Upper Devonian|Upper Devonian|Sandstones are from a mixed volcanic and basement source. Sporadic lycopod stem impressions are represented. See also Clayhole Tuff. Age constrained by the parent Vanneck Formation.||Of the Vanneck Formation.|||Comprises a thin dacitic ignimbrite.|
4137|Clematis Group|13516|5|Briefly described|p138, p159 fig 8, 160-162, p169|Middle Triassic|Middle Triassic|From Bowen Basin, Galilee Basin||||||
4137|Clematis Group|22857|6|Mentioned|p315 Fig. 22.8|||||||||
4137|Clematis Group|22865|6|Mentioned|Fig22.8p315|||||||||
4137|Clematis Group|22973|6|Mentioned|p12|||||||||
4137|Clematis Group|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
4137|Clematis Group|22976|5|Briefly described|p42 Fig.4|Triassic|Triassic|||||||
4137|Clematis Group|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
4137|Clematis Group|23052|5|Briefly described|Map Legend|Triassic|Triassic|||||||
4137|Clematis Group|23161|4|Described|p33 table4 fig11||Triassic|||||||
4137|Clematis Group|23430|5|Briefly described|p514-515|||Overlying Unit Moolayember Formation. Bowen Basin Province.||||||
4137|Clematis Group|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Age: 241-235Ma. Geological Province: Bowen Basin.||||||
4137|Clematis Group|24159|5|Briefly described|p147|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin.||||||
4137|Clematis Group|24615|5|Briefly described|CD|Triassic|Triassic|[Re]. Medium- to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.||||||
4137|Clematis Group|30692|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
4137|Clematis Group|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
4137|Clematis Group|31079|6|Mentioned|Fig. 6|||||||||
4137|Clematis Group|31401|6|Mentioned|Fig.1|||P30||||||
4137|Clematis Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
4137|Clematis Group|35901|6|Mentioned|Fig.1|||||||||
4137|Clematis Group|36121|6|Mentioned|p25|||||||||
4137|Clematis Group|36233|6|Mentioned|Table 1|||||||||
4137|Clematis Group|36472|6|Mentioned|Map legend|Triassic|Triassic|||||||
4137|Clematis Group|37565|6|Mentioned|p7|||||||||
4137|Clematis Group|37610|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|37612|6|Mentioned|Fig.1|||See also Fig.3 and P284.||||||
4137|Clematis Group|38518|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|39212|6|Mentioned|p14|||||||||
4137|Clematis Group|39269|6|Mentioned|Fig.1|||||||||
4137|Clematis Group|39445|5|Briefly described|p116|||Early-mid Trias Group status in Bowen B., Fm. status in Galilee B. See also Chart 7.||||||
4137|Clematis Group|39491|4|Described|p22|||||||||
4137|Clematis Group|39943|6|Mentioned|Table 5A|||See also Table 5B||||||
4137|Clematis Group|40120|4|Described|p428|||||||||
4137|Clematis Group|40245|6|Mentioned|Table 2|||||||||
4137|Clematis Group|40250|6|Mentioned|Table 6|||||||||
4137|Clematis Group|40539|6|Mentioned|Fig.2|||||||||
4137|Clematis Group|40574|6|Mentioned|p4|||||||||
4137|Clematis Group|40675|6|Mentioned|Table 5A|||||||||
4137|Clematis Group|40767|6|Mentioned|p14|||||||||
4137|Clematis Group|40999|6|Mentioned|p303|||||||||
4137|Clematis Group|41101|6|Mentioned|p295|||||||||
4137|Clematis Group|41191|6|Mentioned|p284|||||||||
4137|Clematis Group|41246|6|Mentioned|Map legend|Triassic||||||||
4137|Clematis Group|41266|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|41605|6|Mentioned|fig.2|||||||||
4137|Clematis Group|42259|6|Mentioned|p18|||||||||
4137|Clematis Group|42634|5|Briefly described|Table 2 P10|||||||||
4137|Clematis Group|42701|4|Described|p74|||||||||
4137|Clematis Group|42911|5|Briefly described|p11|||||||||
4137|Clematis Group|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
4137|Clematis Group|42999|5|Briefly described|Table 1,p90|Middle Triassic|Early Triassic|||||||
4137|Clematis Group|43000|5|Briefly described|p108|||see also Fig.5,p112||||||
4137|Clematis Group|43185|5|Briefly described|6||Triassic|||||||
4137|Clematis Group|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
4137|Clematis Group|44245|5|Briefly described|Map Legend||Triassic|||||||
4137|Clematis Group|45095|6|Mentioned|p3|||||||||
4137|Clematis Group|45110|3|Fully described|Table 17|||See also Fig.5.||||||
4137|Clematis Group|45151|5|Briefly described|Table 10|||See also Table 11 & p15. Contains former Carborough Sandstone.||||||05-SEP-18
4137|Clematis Group|46989|5|Briefly described|Table 1|||||||||
4137|Clematis Group|50602|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Sandstone, siltstone, mudstone, conglomerate.||||||
4137|Clematis Group|60659|5|Briefly described|p21, p89|Middle Triassic|Triassic|Medium- to coarse-grained quartzose to sublabile micaceous sandstone, siltstone, minor mudstone and granule to pebble conglomerate. Conformably overlies the Rewan Group. Geological Province: Bowen Basin.||||||07-FEB-11
4137|Clematis Group|61076|5|Briefly described|p188 Fig. 2|Triassic|Triassic|Age: >240Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
4137|Clematis Group|61612|6|Mentioned|p275, p270 Fig. 1|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||13-MAR-09
4137|Clematis Group|61782|5|Briefly described|p281|||Geological Province: Taroom Trough. Quartzose.||||||
4137|Clematis Group|62357|5|Briefly described|p524 Fig. 7|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
4137|Clematis Group|63713|5|Briefly described|p1507 Fig.2, p1512|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Rewan Group. Is overlain by Moolayember Formation and Warang Sandstone.||
4137|Clematis Group|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Is overlain by Moolayember Formation.||
4137|Clematis Group|64856|3|Fully described|p42, p69, p71-75, p77-78, p102|Middle Triassic|Early Triassic|Originally the Clematis Sandstone of Jensen (1926). Upgraded to Group status by Jensen (1975). Bowen Basin, Galilee Basin. Mainly quartzose sandstone. Contains the Glenidal Formation and Expedition Sandstone. Conformably to disconfomably overlies the Rewan Group; the nature of the contact is uncertain. Is overlain conformably by Snake Creek Mudstone Member (Moolayember Formation). Up to 460m thick. Age from palynoflora (units APT2-3).| | ||||28-NOV-17
4137|Clematis Group|64857|5|Briefly described|p113 Fig.3|||Denison Trough, Taroom Trough of Bowen Basin. Includes Showgrounds Sandstone.||||||
4137|Clematis Group|64858|6|Mentioned|p180 Fig.2, p181 Tb.1, p182 Fig.3, p183|Middle Triassic|Middle Triassic|Bowen Basin.||||||30-NOV-09
4137|Clematis Group|65003|5|Briefly described|p6|||Of Bowen Basin.||||Overlies the Rewan Formation.|Sandstone.|30-MAR-12
4137|Clematis Group|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Early Triassic|Unit in the Bowen Basin. Includes Showgrounds Sandstone. Underlies Moolayember Formation.||||||22-MAR-12
4137|Clematis Group|65113|5|Briefly described|p347, Fig 4 p340|Middle Triassic|Early Triassic|Overlies the Rewan Group, contains more quartz rich units than overlying and underlying units. Depositional environment was a braided river system.||||||
4137|Clematis Group|65114|5|Briefly described|p385 Fig.3|Middle Triassic|Early Triassic|||||||
4137|Clematis Group|65115|5|Briefly described|p425, Fig 2 p403, p421 Fig.14|Middle Triassic|Early Triassic|Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Includes Expedition Sandstone and Glenidal Formation.||||||
4137|Clematis Group|65116|5|Briefly described|p450, Fig 2 p436|Middle Triassic|Early Triassic|Includes Showgrounds Sandstone at top. Underlies the Moolayember Formation in the Bowen Basin.||||||
4137|Clematis Group|65118|5|Briefly described|p491, Fig 2 p479|Triassic|Triassic|Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Includes Showgrounds Sandstone?||||||06-MAR-12
4137|Clematis Group|65119|5|Briefly described|Fig 2 p503, Fig 7- 8, 11-12|Middle Triassic|Early Triassic|Bowen Basin. Sandstone and conglomeratic sandstone, minor siltstone. Max thickness 3220m.||||||
4137|Clematis Group|65388|6|Mentioned|p203|||?Overlies Rewan Group, but not in the area of this report.||||||
4137|Clematis Group|65706|4|Described|p12, p18 Tb.1|Middle Triassic|Early Triassic|Bowen Basin. Fluvial.||||Conformable on Rewan Group.|Medium to coarse-grained, cross-bedded, quartzose to sublabile and micaceous sandstone; siltstone, mudstone and granule to pebble conglomerate; some fine conglomerate and grey and red mudstone.|
4137|Clematis Group|66188|6|Mentioned|441, 450, Fig 3, TB1, Fig 16-17|Middle Triassic|Late Permian|||||||
4137|Clematis Group|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p6-8|||Denison and Southern Taroom Trough, Bowen Basin.||||||
4137|Clematis Group|67133|6|Mentioned|p20-21|||||||Overlies Rewan Group. Is overlain by Moolayember Formation.||
4137|Clematis Group|67402|4|Described|p19 fig WSD3, WSD4, p21|Anisian|Olenekian|Galilee Basin. Prospective unit for the storage of carbon dioxide, particularly the fluvial sandstone unit which has a porosity of 16.8%. Deposited in fluvial to fluvial-deltaic depositional environments. See also p45, p48 fig BWS1, p55, p57, p72, p80, p85 tbl BWN2, p124 fig GLL1, p165 tbl LPB1.||||Unconformably overlies the Rewan Group. Overlain by the Showgrounds Sandstone.|Quartzose to sublabile, micaceous sandstone, siltstone, mudstone and conglomerate.|
4137|Clematis Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.|||Includes Showgrounds Sandstone.|Overlies Rewan Group. Is overlain by Moolayember Formation.||
4137|Clematis Group|68279|5|Briefly described|p1-2,p4, p5 Tb.2, p7, p12-13,p15,p17-19|Anisian|Anisian|See also p16 Tb.4. Galilee Basin. A carbon geostorage target reservoir, sealed by Moolayember Formation. Deposited by a braided river system. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Overlies Rewan Group. Is overlain conformably by Moolayember Formation.|Predominantly quartzose. Includes very fine-grained, moderately sorted, angular sandstone consisting of quartz, minor feldspars and rock fragments; limited occurrence of 50cm intercalations of clayey siltstones.|
4137|Clematis Group|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably overlain by the Moolayember Formation. Conformably underlain by the Rewan Formation.|Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin.||||Conformably overlies Rewan Group. Is overalin conformably by Moolayember Formation.||
4137|Clematis Group|68576|5|Briefly described|Q_4: p1, p3, p5-7, p10, p12 Fig.14|Middle Triassic|Early Triassic|See also p14 Fig.17, p16, p21, p24. Bowen Basin. Sediments sourced from the craton to the W.|||Expedition Sandstone, Glenidal Formation.|Unconformably overlies Rewan Group. Is overlain by Snake Creek Mudstone Member (Moolayember Formation).|Sub-labile to quartzose sandstone, conglomeratic sandstone.|
4137|Clematis Group|68679|5|Briefly described|p353, p364, p376-377, p381, p397|Triassic|Triassic|Connors-Auburn Province. Quartzose sediment supply was mainly from the craton (in the W).||||Overlies the Rewan Group. Is overlain by the Moolayember Formation. In Roma area, upper part is equivalent to Showgrounds Sandstone.||
4137|Clematis Group|68731|5|Briefly described|p198, p200, p201, pp201-202 Fig 3.111|Middle Triassic|Early Triassic|Swarbrick and Wallin (1976). Bowen Basin. Has a comparable distribution to the Rewan Group. Possibly equivalent to the Clematis Sandstone.||||Unconformably to disconformably underlain by the Dunda beds.||03-JUL-14
4137|Clematis Group|68901|6|Mentioned|p2 Fig. i|Triassic|Triassic|||||||26-SEP-18
4137|Clematis Group|69681|6|Mentioned|p83 Fig.7|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
4137|Clematis Group|69952|6|Mentioned|p85|Triassic|Triassic|||||||
4137|Clematis Group|71710|4|Described|p370, 380, 381, 382, 383, 384, 385, 387|Middle Triassic|Early Triassic|Geological province: Galilee Basin.  ?Also Bowen Basin?(p387) Also known as Clematis Sandstone in northern Galilee Basin?. Provenance may be from Anakie Inlier as an intrusive high during Early Triassic, and other volcaniclastic input. Sequence 9.||sequence 9 + part 10.||Overlain by Moolayember Formation. Unconformably to disconformably underlain by Rewan Group. Possible lateral equivalent to Warang Sandstone and Dunda beds in upper and lower section respectively.|Moderately sorted, fine to coarse-grained quartzose sandstone with minor red siltstone and mudstone and rare conglomerate|22-MAY-19
4137|Clematis Group|72088|5|Briefly described|p8, p15, p17, p21-p23, p91|Anisian|Anisian|Southern and Eastern Galilee Basin and Bowen Basin. Deposited by braided rivers.||||Unconformably overlies the Dunda beds and Rewan Group. Conformably overlain by the Moolayember Formation.|Sandstone with a kaolonitic matrix and lesser amounts of siltstone and mudstone.|
4137|Clematis Group|72297|5|Briefly described|p744|||Bowen Basin. A significant regional hydrocarbon reservoir.|||Showgrounds Sandstone.|||
4137|Clematis Group|73036|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73037|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73038|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73040|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73113|6|Mentioned|p22-24, p36, p41, p46, p172, p191|||Bowen Basin. Regional aquifer. Written as equivalent to Showgrounds Sandstone [now a parent unit].||||||
4137|Clematis Group|73246|6|Mentioned|p190|Middle Triassic|Middle Triassic|Bowen Basin, northeast and northwest.||||Underlain by Rewan Group. Overlain by Moolyamber Formation.||
4137|Clematis Group|73304|6|Mentioned|p76|||||||||
4137|Clematis Group|73472|5|Briefly described|p115, p120, p129, p131, App.1|Anisian|Anisian|Bowen Basin. Not represented in the northeastern Galilee Basin. Previously thought to occur within Porcupine Gorge; however, these strata are younger and were formalized as the Porcupine Gorge Formation.||||Underlain by Rewan Group. Overlain by Moolayember Formation. Equivalent to Clematis Formation.||
4137|Clematis Group|73570|5|Briefly described|p914, p915 Fig.4, p916, p919 Fig.6|Middle Triassic|Middle Triassic|Bowen Basin.|||||Includes fluviatile, quartz-rich sandstones.|
4151|Cliffdale Volcanics|22457|6|Mentioned|Fig29 P30|||||||||
4151|Cliffdale Volcanics|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|22644|5|Briefly described|5|||Geol province: Mount Isa Basin.||||||04-AUG-06
4151|Cliffdale Volcanics|22673|6|Mentioned|64|||Geol province: Mount Isa Basin.||||||04-AUG-06
4151|Cliffdale Volcanics|22747|6|Mentioned|Table1,p7|||Correlates with Ewan Granite||||||
4151|Cliffdale Volcanics|22853|5|Briefly described|33|||Geol province Murphy Inlier.||||||04-AUG-06
4151|Cliffdale Volcanics|23065|6|Mentioned|11, 15, 17|Proterozoic|Proterozoic|Geol province: Murphy Province.||||||04-AUG-06
4151|Cliffdale Volcanics|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
4151|Cliffdale Volcanics|23363|5|Briefly described|344 Fig.3|Orosirian|Orosirian|Age: ~1851Ma.||||||04-AUG-06
4151|Cliffdale Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|23395|5|Briefly described|p389|||||||||
4151|Cliffdale Volcanics|23398|4|Described|p433|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|23405|6|Mentioned|p565|||||||||
4151|Cliffdale Volcanics|23406|5|Briefly described|p601 Fig.3|||||||||
4151|Cliffdale Volcanics|24197|5|Briefly described|p22, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Nicholson Suite. Includes the Billicumidji Rhyolite Member. Age: 1850Ma. Geological province: Murphy Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
4151|Cliffdale Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Nicholson Granite Complex. Geological Province: Murphy Province, Lawn Hill Subprovince (north).||||||07-NOV-08
4151|Cliffdale Volcanics|24442|5|Briefly described|p22 Fig. 1|||Geological Province: McArthur Basin.||||||
4151|Cliffdale Volcanics|26310|5|Briefly described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Lavas, tuff, agglomerate.||||||
4151|Cliffdale Volcanics|30318|6|Mentioned|p328|||||||||
4151|Cliffdale Volcanics|30536|6|Mentioned|p102|||Correlation ? with Tewinga Group||||||
4151|Cliffdale Volcanics|30912|6|Mentioned|p136|||Proterozoic||||||
4151|Cliffdale Volcanics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4151|Cliffdale Volcanics|31348|6|Mentioned|p344|||||||||
4151|Cliffdale Volcanics|31421|6|Mentioned|p507|||||||||
4151|Cliffdale Volcanics|31824|6|Mentioned|p28|||||||||
4151|Cliffdale Volcanics|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|32660|5|Briefly described|Table 2|||||||||
4151|Cliffdale Volcanics|35114|6|Mentioned|p200|||||||||
4151|Cliffdale Volcanics|35495|6|Mentioned|p344|||||||||
4151|Cliffdale Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|35950|6|Mentioned|p304|||||||||
4151|Cliffdale Volcanics|36012|3|Fully described|Table 1|||See also p8.||||||04-AUG-06
4151|Cliffdale Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36873|5|Briefly described|p27|||||||||
4151|Cliffdale Volcanics|37217|6|Mentioned|p650|||||||||
4151|Cliffdale Volcanics|37371|6|Mentioned|p368|||||||||
4151|Cliffdale Volcanics|37372|6|Mentioned|p2|||||||||
4151|Cliffdale Volcanics|37565|6|Mentioned|p11|||See also Fig.5||||||
4151|Cliffdale Volcanics|37568|6|Mentioned|Fig.5|||||||||
4151|Cliffdale Volcanics|38042|6|Mentioned|p167|||||||||
4151|Cliffdale Volcanics|38557|6|Mentioned|p293|||||||||
4151|Cliffdale Volcanics|38584|4|Described|p8|||||||||
4151|Cliffdale Volcanics|38902|6|Mentioned|p28|||||||||
4151|Cliffdale Volcanics|39123|6|Mentioned|p157|||||||||
4151|Cliffdale Volcanics|39445|5|Briefly described|Table 2|||Base of Carpentarian. Age p39. See also p35 and p38.||||||04-AUG-06
4151|Cliffdale Volcanics|39559|6|Mentioned|Table 1|||||||||
4151|Cliffdale Volcanics|39685|6|Mentioned|Fig.1|||||||||
4151|Cliffdale Volcanics|39925|6|Mentioned|Fig.9|||||||||
4151|Cliffdale Volcanics|40489|6|Mentioned|p88|||||||||
4151|Cliffdale Volcanics|40491|6|Mentioned|p79|||||||||
4151|Cliffdale Volcanics|40675|6|Mentioned|p306|||||||||
4151|Cliffdale Volcanics|40840|6|Mentioned|Map legend|||||||||
4151|Cliffdale Volcanics|41125|6|Mentioned|p35|||See also fig.22.||||||
4151|Cliffdale Volcanics|41319|6|Mentioned|p195|||||||||
4151|Cliffdale Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|41465|6|Mentioned|p9|||||||||
4151|Cliffdale Volcanics|41594|6|Mentioned|p50|||||||||
4151|Cliffdale Volcanics|41721|4|Described|p6|||Contains Billicumidji Rhyolite Member. Thickness: 4000m+. Alkali rhyolite lava, rhyolitic and alkali rhyolitic ignimbrite. Geological province: Murphy Inlier.||||||01-AUG-07
4151|Cliffdale Volcanics|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
4151|Cliffdale Volcanics|41757|5|Briefly described|p207|||||||||
4151|Cliffdale Volcanics|41961|6|Mentioned|Table 1 P39|||||||||
4151|Cliffdale Volcanics|42343|5|Briefly described|p28|||||||||
4151|Cliffdale Volcanics|42385|5|Briefly described|p3|||||||||
4151|Cliffdale Volcanics|42639|6|Mentioned|p6|||||||||
4151|Cliffdale Volcanics|42812|6|Mentioned|p60|||||||||
4151|Cliffdale Volcanics|43010|5|Briefly described|Fig.6||Paleoproterozoic|Of Early Proterozic age.||||||07-NOV-08
4151|Cliffdale Volcanics|43036|6|Mentioned|p26|||||||||
4151|Cliffdale Volcanics|43788|6|Mentioned|p13||Proterozoic|||||||
4151|Cliffdale Volcanics|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|44271|14|Not recorded|p38|||||||||
4151|Cliffdale Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
4151|Cliffdale Volcanics|44275|14|Not recorded|Map Legend|||||||||
4151|Cliffdale Volcanics|44280|14|Not recorded|Tb.1|||||||||
4151|Cliffdale Volcanics|44305|14|Not recorded|p.6,8,9,10,17||Paleoproterozoic|(E53-8). p18,19,20,opp.6,18. L.Prot.||||||07-NOV-08
4151|Cliffdale Volcanics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
4151|Cliffdale Volcanics|44482|14|Not recorded|p.6|||(E53-12).||||||
4151|Cliffdale Volcanics|44530|14|Not recorded|p.8|||Equiv.of Scrutton Volcanics. (D53-15).||||||
4151|Cliffdale Volcanics|44751|14|Not recorded|p302|||||||||
4151|Cliffdale Volcanics|44989|14|Not recorded|p.113|||Tb.II.||||||
4151|Cliffdale Volcanics|45086|5|Briefly described|p29|||Lithology and mineralization.||||||04-AUG-06
4151|Cliffdale Volcanics|45140|6|Mentioned|p12-13|||McArthur Basin region.|1770 +/- 20 Ma.|||||
4151|Cliffdale Volcanics|45162|6|Mentioned|p11|||||||||
4151|Cliffdale Volcanics|45166|4|Described|p13|||||||||
4151|Cliffdale Volcanics|45167|5|Briefly described|Fig.27|||||||||
4151|Cliffdale Volcanics|45287|14|Not recorded|p.226-7,229||Paleoproterozoic|Intruded by Nicholson Granite.  Mineralised U, Pb? Cu. Acid lavas. L. Proterozoic||||||07-NOV-08
4151|Cliffdale Volcanics|46804|6|Mentioned|p153|||Stratigraphy||||||
4151|Cliffdale Volcanics|46864|4|Described|p39|||||||||
4151|Cliffdale Volcanics|48901|14|Not recorded|Not recorded||Carpentarian|||||||
4151|Cliffdale Volcanics|49001|5|Briefly described|p1|||||||||
4151|Cliffdale Volcanics|49002|6|Mentioned|p1|||||||||
4151|Cliffdale Volcanics|50536|5|Briefly described|p1.4, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Nicholson Suite. Age: ~1850Ma (SHRIMP), 1732 +/- 20Ma (Rb-Sr). Thckness: 4000m.||||||26-MAR-18
4151|Cliffdale Volcanics|60558|5|Briefly described|p9 Fig. 7|||Age: 1850Ma (SHRIMP). Geological Province: Murphy Basin.||||||03-JUN-09
4151|Cliffdale Volcanics|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
4151|Cliffdale Volcanics|63109|6|Mentioned|p1109|||Age: ~1850Ma. Repersentation of the 'Barramundi' basement. Geological Province: Murphy Inlier.||||||30-SEP-08
4151|Cliffdale Volcanics|63112|5|Briefly described|p1190|||Part of basement to southern McArthur Basin.|c. 1850 Ma.|||||
4151|Cliffdale Volcanics|63116|6|Mentioned|p1299 Tb.1,|||Material properties detailed.||||||
4151|Cliffdale Volcanics|64250|6|Mentioned|p23|||Discussed as possible sediment source for Quilalar Formation.|1851 +/- 3 Ma|||||20-MAR-18
4151|Cliffdale Volcanics|65228|5|Briefly described|p20.|||SE McArthur Basin. 4,000 m+ thick. Felsic; geochemically similar to Scrutton Volcanics. May correlate with Leichhardt Volcanics.||||Unconformably overlies Murphy Metamorphic complex.||
4151|Cliffdale Volcanics|65232|5|Briefly described|p9, p8 Fig. 7, p66-68|||Unconform. over Murphy Metamorphics; unconform. under Westmoreland Conglomerate. Contact with Nicholson Granite. Felsic to intermediate ignimbrite and rhyolite. Age: 1851 Ma. Uranium mineralisation. Geol Prov: Murphy Inlier.||||||09-FEB-10
4151|Cliffdale Volcanics|65337|5|Briefly described|p5, p6 Fig.3, p8.||Paleoproterozoic|Murphy Inlier. Felsic volcanics, comagmatic with Nicholson Granite. Probably correlates with Connelly Volcanics.|c.1860-1845 Ma.|||||
4151|Cliffdale Volcanics|65340|6|Mentioned|p7, p83.|||Felsic. Emplaced with comagmatic Nicholson Granite into Murphy Metamorphics to form the regional basement, which is not exposed in this map area.|c.1860 - 1845 Ma.|||||
4151|Cliffdale Volcanics|65396|6|Mentioned|p196|Orosirian|Orosirian|Murphy Inlier.|1851 +/- 3 Ma |||||
4151|Cliffdale Volcanics|66529|5|Briefly described|p20-21  |Paleoproterozoic|Paleoproterozoic|Age of upper units.|~1840 Ma (M. Ahmad, NTGS, pers.comm.)|||Unconformably overlies the Murphy Metamorphics.|Alkali rhyolite lava and rhyolitic and alkali rhyolitic ignimbrite.|
4151|Cliffdale Volcanics|67323|4|Described|GIS attrib tbl, p9, p29, p39, p107|||See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Informally divided into 12 subunits.|~1845 Ma.|Tawallah Group.||Is intruded by Nicholson Granite Complex. Correlated with the Leichhardt Volcanics.|Rhyolitic to dacitic ignimbrite, rhyolitic lava, tuff, vent breccia; grey porphyritic andesite; pink medium, even granofels.|
4151|Cliffdale Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
4151|Cliffdale Volcanics|69417|5|Briefly described|p2:5, 9|Orosirian|Orosirian|Murphy Orogen.|c.1851 Ma.|||Unconformably overlies the Murphy Metamorphics.||12-JUL-16
4151|Cliffdale Volcanics|69418|5|Briefly described|p3:17, 19|||Murphy Province. Hosts the Eva Mine unconformity-related U deposit (described).||||Is overlain unconformably by Westmoreland Conglomerate.||12-JUL-16
4151|Cliffdale Volcanics|69423|4|Described|p8:1-4|Orosirian|Orosirian|Murphy Inlier, Murphy Province. Coeval and comagmatic with Connellys Volcanics and Nicholson Granite Complex. Over 4km thick. Complicated, apparently mutually intrusive relationship with Nicholson Granite Complex. SHRIMP U-Pb zircon age. Hosts copper occurrences including the Norris Copper Mine, and a number of uranium occurrences including the Eva (Pandanus Creek) Mine which also contains gold.|1851 +/- 3 Ma (Page et al., 2000).|||Unconformably overlies Murphy Metamorphics. Is overlain unconformably by Westmoreland Conglomerate.|Rhyolite, alkali rhyolite and dacitic lavas, ignimbrites and intrusions; minor andesite and sedimentary intervals.|12-JUL-16
4151|Cliffdale Volcanics|69429|5|Briefly described|p14:3|Paleoproterozoic|Paleoproterozoic|Murphy Province.|c.1850 Ma.|||Age-equivalent to Scrutton Volcanics (Scrutton Inlier).||12-JUL-16
4151|Cliffdale Volcanics|69430|5|Briefly described|p15:10, 49-50|||Underlies southern McArthur Basin succession. Hosts small U-Au deposits (eg Eva, described in some detail).||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).|Includes rhyolitic and alkali rhyolitic ignimbrite, and alkali rhyolite lava.|12-JUL-16
4151|Cliffdale Volcanics|69433|5|Briefly described|p18:2-3|||A probable source of 1847 +/- 13 Ma sediment (zircons) for Wire Creek Sandstone, and conglomerate clasts in the Fish River Formation.||||Is overlain unconformably by Wire Creek Sandstone.||12-JUL-16
4151|Cliffdale Volcanics|69434|5|Briefly described|p19:1, 4|||Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.|c.1850 Ma (Page et al., 2000).|||||12-JUL-16
4151|Cliffdale Volcanics|69591|5|Briefly described|p29-31, p58|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain. Co-magmatic with Nicholson Granite. Dated at 1851 +/- 3 Ma by Page, Jackson and Krassay (2000).|c.1865 - c.1845 Ma.|||Is intruded by Nicholson Granite Complex.|Rhyolitic to dacitic ignimbrite, rhyolitic lava, tuff.|
4151|Cliffdale Volcanics|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|69917|5|Briefly described|p199, 201|Orosirian|Orosirian|Co-magmatic with Nicholson Granite.||||Unconformably underlies Westmoreland Conglomerate.||
4151|Cliffdale Volcanics|70284|6|Mentioned|p1244, 1245|Orosirian|Orosirian||~1850 Ma|||||
4151|Cliffdale Volcanics|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.|||Billicumidji Rhyolite Member.|Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group). Is intruded by Nicholson Granite Complex.|Rhyolitic and alkali rhyolitic ignimbrite; rhyolitic lava, ashfall tuff.|
4151|Cliffdale Volcanics|71369|6|Mentioned|p47|||Basement rocks of the South Nicholson Basin.||||||
4151|Cliffdale Volcanics|71592|5|Briefly described|Appendix A.|||Murphy Region.|1851+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
4151|Cliffdale Volcanics|71606|5|Briefly described|p137|Orosirian|Orosirian|Murphy Tectonic Ridge.||||Correlable to Nicholson Granite. Underlain by Murphy Metamorphics.||
4151|Cliffdale Volcanics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Part of the early Basin volcanism and plutonism in the McArthur Basin.|||||Rhyolitic to dacitic volcanics, tuff.|
4151|Cliffdale Volcanics|71799|5|Briefly described|p150 fig 2||||||||Silicic volcanics, porphyry.|
4151|Cliffdale Volcanics|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|Shown as located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age.|1851 +/-3 Ma|Tawallah Group||Shown as overlying Murphy Metamorphics and partially underlying Nicholson Granite Complex.||
4151|Cliffdale Volcanics|72527|5|Briefly described|p5, p161, p184-185,|Orosirian|Orosirian|Murphy Province. The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds. Ref Ahmad et al. (2013).|1851 +/-3 Ma|||Unconformably overlies Murphy Metamorphics.||
4151|Cliffdale Volcanics|72912|5|Briefly described|p5 Fig.3, p19.|Orosirian|Orosirian|Located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1851+/-3 Ma|||Shown as overlying Murphy Metamorphics and underlies Nicholson Granite Complex and partially equivalent to Scrutton Volcanics.||15-MAR-21
4151|Cliffdale Volcanics|72919|4|Described|p1, p4-6, p11-14, p93|Orosirian|Orosirian|Murphy Province, North Australian Craton. Over 4000 m thick. Five members have been mapped, although only the uppermost member has been named (the Billicumidji Rhyolite Member). New U-Pb SHRIMP zircon magmatic crystallisation age of 1857 +/- 7 Ma. Broadly coeval with Connellys Volcanics, Nicholson Granite Complex, and Scrutton Volcanics.|1857 +/- 7 Ma U-Pb SHRIMP||Billicumidji Rhyolite|Unconformably underlain by Murphy Metamorphics.|Rhyolite (locally flow-banded) and dacitic lavas, tuffs and 'calc-alkaline ignimbrites'.|
4151|Cliffdale Volcanics|73042|6|Mentioned|p4|Orosirian|Orosirian|Southern McArthur Basin and South Nicholson Basin region. Geochronology is a U-Pb zircon igneous crystallisation age.|1851 +/- 3 Ma (see Fig.1.2)|||||
4151|Cliffdale Volcanics|73427|5|Briefly described|p1, p5, p12-13, App.A|Orosirian|Orosirian|North Australian Craton, Murphy Inlier/Murphy Province. Flat-lying. Co-magmatic with Nicholson Granite.|1855-1845 Ma||||Predominantly felsic lava and ignimbrite.|
4191|Clumber Teschenite|33290|4|Described|Table 1|||Analysis.||||||
4191|Clumber Teschenite|45087|5|Briefly described|p142|||See also p168. Chem. analyses||||||05-NOV-21
4192|Clump Point basalt|31452|6|Mentioned|p5|||||||||
4208|Coalstoun intrusives|34974|6|Mentioned|p952|||||||||
4208|Coalstoun intrusives|36217|6|Mentioned|p206|||Published by Ashley & others 1978.||||||
4212|Coane Range Granite Complex|23422|5|Briefly described|p181, p217 Table 6.11|Carboniferous|Carboniferous|Of Oweenee Supersuite.||||||
4212|Coane Range Granite Complex|23509|5|Briefly described|Map Legend||Carboniferous|||||||
4212|Coane Range Granite Complex|23617|4|Described|p18 Table 2|||Intrudes Paluma Rhyolite, Running River Metamorphics and Falls Creek Tonalite. Also see p23. Of Oweenee Supersuite of Kennedy Province.||||||
4212|Coane Range Granite Complex|23618|5|Briefly described|map legend||Carboniferous|||||||
4212|Coane Range Granite Complex|23893|5|Briefly described|p19|Carboniferous|Carboniferous|Structural term.  Geological Province: Oweenee Batholith.||||||
4212|Coane Range Granite Complex|24613|6|Mentioned|p113|||Age: 331+/-2Ma (Rb-Sr biotite-total rock).||||||07-FEB-11
4212|Coane Range Granite Complex|42689|5|Briefly described|map legend|Carboniferous||Reserved as Coane Range Granite.||||||
4212|Coane Range Granite Complex|42690|5|Briefly described|map legend|Carboniferous||||||||
4212|Coane Range Granite Complex|43095|3|Fully described|p51||Carboniferous|||||||
4212|Coane Range Granite Complex|43589|2|Defined|p22|Early Carboniferous|Early Carboniferous|Previously mapped as Oweenee Granite.  Intrudes Running River Metamorphics and Falls Creek Tonalite, Keelbottom Group and Paluma Volcanics.||||||26-JUN-15
4212|Coane Range Granite Complex|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink, grey, cream and orange, fine- to coarse-grained, equigranular, seriate and porphyritic biotite granite and common microgranite; local greisen.|
4212|Coane Range Granite Complex|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink, grey, cream and orange, fine- to coarse-grained, equigranular, seriate and porphyritic biotite granite and common microgranite; local greisen.|
4212|Coane Range Granite Complex|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Spinifex Creek Granite and Paluma Rhyolite.|Pink, grey, cream and orange, fine to coarse-grained, equigranular, seriate and porphyritic biotite granite and common microgranite; local greisen.|
4212|Coane Range Granite Complex|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Spinifex Creek Granite and Paluma Rhyolite.|Pink, grey, cream and orange, fine to coarse-grained, equigranular, seriate and porphyritic biotite granite and common microgranite; local greisen.|
4213|Coarsers Bridge Sandstone Member|42547|4|Described|p52|||||||||
4294|Coen Metamorphic Group|22533|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|In Georgetown Region||||||
4294|Coen Metamorphic Group|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||12-JAN-05
4294|Coen Metamorphic Group|22781|3|Fully described|p24|Proterozoic|Proterozoic|Savannah Province||||||
4294|Coen Metamorphic Group|22811|5|Briefly described|p597, Fig.2 p598|Mesoproterozoic|Mesoproterozoic|of Savannah Province||||||
4294|Coen Metamorphic Group|23420|4|Described|p 123|Mesoproterozoic|Mesoproterozoic|Also see p 142 table 4.4. Age: <1585+/-13Ma (detrital zircon). In the Savannah Province||||||12-JAN-05
4294|Coen Metamorphic Group|23430|4|Described|p454-455|||Savannah Province.||||||
4294|Coen Metamorphic Group|23431|6|Mentioned|p535|||Savannah Province.||||||
4294|Coen Metamorphic Group|24393|6|Mentioned|p149|||Geological Province: Savannah Province.||||||
4294|Coen Metamorphic Group|42610|6|Mentioned|p4|||Variation on Coen Metamorphics.||||||
4294|Coen Metamorphic Group|42640|5|Briefly described|p8|||Equivalent to Coen Metamorphics||||||
4294|Coen Metamorphic Group|42650|5|Briefly described|p13|||Supersedes Coen Metamorphics in Ebagoola 1:250 000 sheet area||||||
4294|Coen Metamorphic Group|43596|6|Mentioned|p6||Mesoproterozoic|Part of Savannah Province, together with Edward River and Staaten Metamorphic Groups and the Holroyd Group.||||||25-AUG-08
4294|Coen Metamorphic Group|43665|5|Briefly described|p10||Proterozoic|||||||
4294|Coen Metamorphic Group|43730|6|Mentioned|p13|||||||||
4294|Coen Metamorphic Group|43738|5|Briefly described|p5||Proterozoic|||||||
4294|Coen Metamorphic Group|43741|6|Mentioned|p14|||||||||
4294|Coen Metamorphic Group|63866|4|Described|p76, p81, p85|||Savannah Subprovince, Coen Region. Includes four metamorphic units with uncertain boundary relationships. Most of the group is structurally and metamorphically simpler than the Yambo and Newberry Metamorphic Group. A feldspathic gneiss from this group has zircon grains dated at 1554 +/- 4 Ma [although the meaning of this date isnt clear].|||||Mid- to upper-amphibolite facies schist, gneiss and lesser quartzite.|
4294|Coen Metamorphic Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||||The top part (at least) correlates with the Edward River and Holroyd Metamorphic Groups.||
4294|Coen Metamorphic Group|69591|4|Described|p74 Fig.2.71, p76-80|Mesoproterozoic|Mesoproterozoic|Coen Inlier, Etheridge Province. Redefined by Blewett et al. (1992) to include only the central N-S trending belt of metamorphic rocks in EBAGOOLA and southern COEN sheet areas. Age is uncertain.|<1585 +/- 13 Ma (maximum depositional age).||Goolha-Goolha Schist, Lochs Gneiss, Yarraden Schist, Mount Ryan Quartzite.||High-grade schist, paragneiss, quartzite and amphibolite.|
4294|Coen Metamorphic Group|69592|6|Mentioned|p289|||Possible protolith for at least the northern units of the Kintore Supersuite.||||||
4294|Coen Metamorphic Group|70207|6|Mentioned|p126|Paleoproterozoic|Paleoproterozoic|||||||
4294|Coen Metamorphic Group|71031|5|Briefly described|p14, p20, p26, p32|Proterozoic|Proterozoic|||||Intruded by the Lankelly Granite and the Flyspeck Granodiorite.||
4294|Coen Metamorphic Group|71592|5|Briefly described|Appendix A.|||Savannah Province. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|1614+/-15 Ma and 1554+/-4 Ma.||||Gneiss, feldspathic gneiss.|
4294|Coen Metamorphic Group|71792|3|Fully described|p3, p5-p8, p11-p13|Mesoproterozoic|Paleoproterozoic|Coen Inlier, Savannah Province. Named for the town of Coen in the central part of the inlier. Extends over a strike length of more than 180km through the centre of the Coen Inlier. Generally this group is recessive and commonly covered by Tertiary sediments. This term was introduced by Blewett et al. 1992. Forms a distinct band of high magnetic response with strong to moderate linear features trending nnw. The radiometric response is varied but generally subdued and dominated by relatively high potassium and uranium. Also referred to as the Coen Metamorphics on p30. MDA of 1648+/-4.5 Ma previously mapped in Sefton Metamorphics, now included in Coen Metamorphic Group on the basis of age. See also p15-p16, p27, p30-p31.|1648 +/- 4.5 Ma (Kositcin et al, 2015)||Includes the Choc-a-block Orthogneiss, Goolha Goolha Schist, Mount Ryan Quartzite, Yarraden Schist and the Lochs Gneiss.|Intruded by the Buthen Buthen Granite.|Biotite-muscovite-quartz schist, biotite-quartze-feldspar gneiss, garnet-amphibole-quartz-feldspar gneiss, amphibolite, quartzite, calc-silicate rocks and marble.|
4294|Coen Metamorphic Group|71849|4|Described|p8, p43, p46, p49, p57, p60, p79, p84|Mesoproterozoic|Paleoproterozoic|See also p86, p94, p98, p104, p108, p111, p114, p119, p124-126, p130, p176-177, p183, p195. Formerly Coen Metamorphics. Has significant Au occurrences in the vicinity of Coen. Most zircons from gneisses in this unit are aged between c.1700-1500 Ma.|||Goolha-Goolha Schist, Lochs Gneiss, Yarraden Schist.|Is intruded by Buthen Buthen, Tadpole, Twin Humps and McIlwraith Granites, Whites Creek and (inferred) Leo Creek Granodiorites.|High-grade metamorphic rocks.|
4294|Coen Metamorphic Group|71853|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||||Choc-A-Block Orthogneiss, Lochs Gneiss, Yarraden Schist.||Gneisses, schists.|
4294|Coen Metamorphic Group|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||||Choc-A-Block Orthogneiss; Goolha-Goolha and Yarraden Schists; Lochs Gneiss.|||
4294|Coen Metamorphic Group|72983|5|Briefly described|p4-6, p52-57, p83, p85, p91-106, p116|Mesoproterozoic|late Paleoproterozoic|Cut by an Au-mineralised rhyolitic dyke dated at 277.7 +/- 3 Ma.|||Choc-a-block Orthogneiss, Yarraden Schist, Lochs Gneiss|Intruded by Kintore Granite and Wigan Granite.|Includes marbles and skarns.|
4294|Coen Metamorphic Group|73083|6|Mentioned|p59-60, p64|||||||||
4294|Coen Metamorphic Group|73387|5|Briefly described|p1-2, p32-39|Statherian|Statherian|Savannah Province, northern. A new zircon U-Pb SHRIMP maximum depositional age of 1635 +/- 14 Ma was published herein along with metamorphic ages of 1421 +/- 28 Ma, 428.9 +/- 4.2 Ma, and 414 +/- 3.7 Ma. The youngest of these metamorphic events is associated with emplacement of the Kintore Granite.|1635 +/- 14 Ma U-Pb SHRIMP||Choc-a-block Orthogneiss, Lochs Gneiss|||
4337|Colleges Conglomerate|13516|6|Mentioned|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Kholo Subgroup||||
4337|Colleges Conglomerate|29386|6|Mentioned|p454|||Upper Triassic.||||||
4337|Colleges Conglomerate|30302|6|Mentioned|p415|||Refers to Allen(1959).||||||
4337|Colleges Conglomerate|30465|6|Mentioned|p3|||||||||
4337|Colleges Conglomerate|30466|6|Mentioned|p3|||Triassic age||||||
4337|Colleges Conglomerate|32136|6|Mentioned|p8|||Miospores||||||
4337|Colleges Conglomerate|32180|5|Briefly described|p4|||||||||
4337|Colleges Conglomerate|33381|4|Described|p109|||Triassic. See also PP113 & 117. Kholo Subgroup||||||
4337|Colleges Conglomerate|33769|5|Briefly described|p149|||U.Triassic||||||
4337|Colleges Conglomerate|34457|6|Mentioned|p484|||Mesozoic||||||
4337|Colleges Conglomerate|35866|6|Mentioned|p400|||||||||
4337|Colleges Conglomerate|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
4337|Colleges Conglomerate|36243|6|Mentioned|Table 10A|||||||||
4337|Colleges Conglomerate|36351|6|Mentioned|p373|||||||||
4337|Colleges Conglomerate|36354|3|Fully described|p366|||||||||
4337|Colleges Conglomerate|36779|6|Mentioned|p6|||||||||
4337|Colleges Conglomerate|37111|5|Briefly described|p292|||||||||
4337|Colleges Conglomerate|38074|5|Briefly described|Table 1|||||||||
4337|Colleges Conglomerate|38076|6|Mentioned|Table 3|||||||||
4337|Colleges Conglomerate|38307|4|Described|p519|||||||||
4337|Colleges Conglomerate|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
4337|Colleges Conglomerate|39445|5|Briefly described|Table 9 p121|Late Triassic||Of Kholo Subgroup, Ipswich Coal Measures.||||||28-SEP-05
4337|Colleges Conglomerate|39943|6|Mentioned|Table 12A|||||||||
4337|Colleges Conglomerate|40623|5|Briefly described|p35|||||||||
4337|Colleges Conglomerate|41906|3|Fully described|Table 2 P18|||max thickness: 240m||||||28-SEP-05
4337|Colleges Conglomerate|42336|5|Briefly described|Table 1 P5|||||||||
4337|Colleges Conglomerate|43076|5|Briefly described|p8|||||||||
4337|Colleges Conglomerate|43922|14|Not recorded|p324,325|||Formation of Kholo Subgroup of Ipswich Coal Measures.||||||
4337|Colleges Conglomerate|44384|14|Not recorded|p119|||||||||
4337|Colleges Conglomerate|44510|2|Defined|p252-253,Fig.35|||Overlies disconformably Mount Crosby and Blackwall Breccia and unconformably on Neranleigh-Fernvale Group.||||||
4337|Colleges Conglomerate|44542|2|Defined|p32,34||Middle Triassic|="Kholo Conglomerate". No fossils.||||||
4337|Colleges Conglomerate|44687|6|Mentioned|p227|||||||Disconformably overlain by Witty Gravel.||21-MAR-13
4337|Colleges Conglomerate|44703|14|Not recorded|Map|||||||||
4337|Colleges Conglomerate|44705|14|Not recorded|p15|||||||||
4337|Colleges Conglomerate|44708|14|Not recorded|p3,Sheet 2,section||Middle Triassic|||||||
4337|Colleges Conglomerate|44734|14|Not recorded|p5,7-9,13,15-19|||Pine Mountain area.||||||
4337|Colleges Conglomerate|44775|4|Described|p7,8,map 2||Triassic|(Kholo Sub-Group)||||||
4337|Colleges Conglomerate|44783|14|Not recorded|p16,18|||||||||
4337|Colleges Conglomerate|67402|5|Briefly described|p222, p223, p225|Carnian|Ladinian|Ipswich Basin.||Kholo Subgroup||Overlies the Mount Crosby Formation. Overlain by the Hector Tuff.|Pebble and granule conglomerates, sandstone with minor siltstone and mudstone.|
4337|Colleges Conglomerate|68679|4|Described|p393-394|Late Triassic|Late Triassic|Ipswich Basin. Up to 240m thick in the type section at Colleges Crossing; thins to the E and S; ~11m in drill hole IC 93.||Kholo Subgroup.||Conformably and disconformably overlies Mount Crosby Formation. Is overlain conformably by Hector Tuff.|Polymict pebble conglomerate dominated by basement clasts up to 30cm in diameter, and lithic labile sandstone with petrified wood.|
4338|Colless Volcanics|14019|6|Mentioned|p19|||Geochemically identical with Antrim Plateau Volcanics, Helen Springs Volcanics and Peaker Piker Volcanics in N.T.||||||
4338|Colless Volcanics|23328|5|Briefly described|1030|||||||||07-SEP-09
4338|Colless Volcanics|23393|5|Briefly described|p22|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|24303|6|Mentioned|p62 Appendix|||Geological Province: Georgina Basin. Possible correlative of Helen Springs Volcanics.||||||
4338|Colless Volcanics|26310|5|Briefly described|p4 Table 1|Cambrian|Proterozoic|Basalt. Maximum Thickness: 200 feet?||||||
4338|Colless Volcanics|30242|6|Mentioned|p10|||||||||
4338|Colless Volcanics|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
4338|Colless Volcanics|31396|6|Mentioned|Fig.3|||||||||
4338|Colless Volcanics|32659|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|33482|6|Mentioned|p9|||||||||
4338|Colless Volcanics|34162|6|Mentioned|p117|||Early Cambrian.||||||
4338|Colless Volcanics|35054|6|Mentioned|p245|||||||||
4338|Colless Volcanics|36003|6|Mentioned|Fig.8|||||||||
4338|Colless Volcanics|36644|6|Mentioned|p213|||||||||
4338|Colless Volcanics|37572|5|Briefly described|p155|||See also p151.||||||07-AUG-06
4338|Colless Volcanics|38444|6|Mentioned|p139|||||||||
4338|Colless Volcanics|38446|6|Mentioned|p143|||||||||
4338|Colless Volcanics|39445|5|Briefly described|Table 4|||See also p62.||||||07-AUG-06
4338|Colless Volcanics|39797|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|40852|6|Mentioned|p36|||||||||
4338|Colless Volcanics|40856|5|Briefly described|p315|||||||||
4338|Colless Volcanics|41240|6|Mentioned|p112|||||||||
4338|Colless Volcanics|44271|2|Defined|p38,40,42,57||Neoproterozoic|Appears to underlie Camooweal Dolomite.||||||
4338|Colless Volcanics|44274|2|Defined|Tb.2,p9,10,16,map|||Unconformably overlies Mullera Formation and Constance Sandstone. Unconformably overlain by Thorntonia Limestone.||||||24-MAR-16
4338|Colless Volcanics|44275|14|Not recorded|Map Legend|||||||||
4338|Colless Volcanics|44281|14|Not recorded|Map Legend|||Early Cambrian or Neoproterozoic.||||||
4338|Colless Volcanics|44290|2|Defined|p439|||Neoproterozoic or Early Cambrian.||||||
4338|Colless Volcanics|44482|14|Not recorded|p.11,15-16|||(E53-12). U.Prot. or L.Cam.||||||
4338|Colless Volcanics|44806|14|Not recorded|p298|||Petrographic descriptions.||||||
4338|Colless Volcanics|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
4338|Colless Volcanics|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Vesicular basalt; sandstone lenses.||||||01-JUL-04
4338|Colless Volcanics|44989|2|Defined|p.124|||Overlies Mullera Formation; underlies Camooweal Dolomite. (E54-9).||||||
4338|Colless Volcanics|45052|4|Described|p72|||Adelaidean or Cambrian.||||||12-NOV-08
4338|Colless Volcanics|45079|6|Mentioned|p8|||Petrography. Lower Cambrian age||||||
4338|Colless Volcanics|45287|14|Not recorded|p.223||Cambrian|||||||
4338|Colless Volcanics|60122|5|Briefly described|p15|Early Cambrian|Early Cambrian|Conformably overlain by Thorntonia Limestone.||||||
4338|Colless Volcanics|62557|5|Briefly described|p461, 462|Cambrian|Cambrian|Of the Kalkarindji continental flood basalt province.||||||24-NOV-09
4338|Colless Volcanics|64068|5|Briefly described|p81, p58, 225|Early Cambrian|Early Cambrian|Kalkarindji Flood Basalt Province, central and northwest Georgina Basin.|c.513-c.504 Ma.|||[Said to be] conformably and gradationally overlain by Thorntonia Limestone[but neither of the references given support this statement].||24-MAR-16
4338|Colless Volcanics|64589|5|Briefly described|chemistry file|||Geochemical analyses.||||||12-NOV-08
4338|Colless Volcanics|65337|6|Mentioned|p94.|||Probable minimum thickness of 60 m.||Unit in Kalkarindji Volcanic Group.||||
4338|Colless Volcanics|66526|5|Briefly described|p27.|Early Cambrian|Early Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.|||||
4338|Colless Volcanics|67323|5|Briefly described|p83, p107; GIS attrib tbl|Early Cambrian|Neoproterozoic|See also Solid Geology Map. Undilla Sub-basin, Centralian Superbasin.||||Is overlain unconformably by Thorntonia Limestone.|Amygdaloidal basalt, trachyte, arenite|
4338|Colless Volcanics|67352|6|Mentioned|p31 |||Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km.||||||
4338|Colless Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. ||||||
4338|Colless Volcanics|69443|6|Mentioned|p28:16|||Kalkarindji Province.||||Is overlain conformably and gradationally by Thorntonia Limestone (Narpa Group).||12-JUL-16
4338|Colless Volcanics|69445|3|Fully described|p30:1, 5, 16-17|Early Cambrian|Early Cambrian|Carter (1959), Carter and Opik (1961). Widespread small exposures of sub-aerial basaltic lavas on the margins of eastern Georgina Basin. Probable minimum thickness of 60m. Type section at about GDA94 54K 216029mE 7935918mN in western LAWN HILL map area.||Kalkarindji Suite.||Unconformably overlies Mullera Formation (South Nicholson Group). Is overlain by Thorntonia Limestone (unconformably) and Camooweal Dolostone.|Amygdaloidal basalt and other tholeiitic lavas.|12-JUL-16
4338|Colless Volcanics|69591|5|Briefly described|p29, p54, p87|Cambrian|Neoproterozoic|Camooweal-Murphy Domain. Georgina Basin.||Kalkarindji Volcanic Group.|||Amygdaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|71369|5|Briefly described|p45|Cambrian|Cambrian|Forms part of the southern margin of the South Nicholson Basin.|Middle Cambrian|Middle Cambrian||Correlative of Antrim Plateau Volcanics.||20-FEB-18
4338|Colless Volcanics|72408|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72414|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72415|4|Described|mapsheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72416|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|Shown with Helen Springs Volcanics.||||||
4338|Colless Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
4338|Colless Volcanics|73083|6|Mentioned|p3, p69|Cambrian|Cambrian|[Superseded by or a constituent of the Kalkarindji Suite]. These rocks comprise one of a series of widely separated exposures of Cambrian basalt attributed to the Kalkarindji Continental Flood Basalt Province (Glass et al, 2013). Correlation was based on matching magnetic signatures.|||||Basalt.|
4352|Collinsville Coal Measures|22675|4|Described|p86|Permian|Permian|Bowen Basin.||||||05-AUG-08
4352|Collinsville Coal Measures|22973|5|Briefly described|p9 Fig.2 (c)|Early Permian|Early Permian|||||||
4352|Collinsville Coal Measures|23008|6|Mentioned|p460|||||||||
4352|Collinsville Coal Measures|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
4352|Collinsville Coal Measures|23161|6|Mentioned|p30|||||||||
4352|Collinsville Coal Measures|23430|5|Briefly described|p515|||||||||
4352|Collinsville Coal Measures|29735|5|Briefly described|p5|||||||||
4352|Collinsville Coal Measures|30429|6|Mentioned|p113|||Quality of coal seam in||||||
4352|Collinsville Coal Measures|30450|6|Mentioned|p2|||||||||
4352|Collinsville Coal Measures|30545|6|Mentioned|Fig.2|||Lower Permian||||||
4352|Collinsville Coal Measures|30546|6|Mentioned|p107|||Lower Permian age. Correlation||||||
4352|Collinsville Coal Measures|31079|6|Mentioned|p5|||||||||
4352|Collinsville Coal Measures|31261|6|Mentioned|p518|||||||||
4352|Collinsville Coal Measures|31262|6|Mentioned|p2|||||||||
4352|Collinsville Coal Measures|31649|6|Mentioned|p57|||||||||
4352|Collinsville Coal Measures|31688|6|Mentioned|p408|||Refers correlation with Calen C.M.||||||
4352|Collinsville Coal Measures|31984|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
4352|Collinsville Coal Measures|32553|4|Described|p42|||See also P10||||||
4352|Collinsville Coal Measures|32554|6|Mentioned|Table 1|||||||||
4352|Collinsville Coal Measures|32556|4|Described|Table 3|||||||||
4352|Collinsville Coal Measures|32577|6|Mentioned|p23|||||||||
4352|Collinsville Coal Measures|32832|6|Mentioned|p7|||||||||
4352|Collinsville Coal Measures|32943|6|Mentioned|p87|||See also PP100,102||||||
4352|Collinsville Coal Measures|32945|6|Mentioned|p78|||See also P80 & Fig.2||||||
4352|Collinsville Coal Measures|32949|5|Briefly described|p441|||Depositional history.||||||
4352|Collinsville Coal Measures|33202|6|Mentioned|Table 2|||||||||
4352|Collinsville Coal Measures|33216|6|Mentioned|p8|||Permian||||||
4352|Collinsville Coal Measures|33686|6|Mentioned|p20|||||||||
4352|Collinsville Coal Measures|33701|6|Mentioned|Fig.1|||L.Perm.||||||
4352|Collinsville Coal Measures|33711|6|Mentioned|Table 3|||||||||
4352|Collinsville Coal Measures|34138|6|Mentioned|Cor.Chart|||Artinskian - Kungurian||||||
4352|Collinsville Coal Measures|34287|6|Mentioned|p136|||Permian||||||
4352|Collinsville Coal Measures|34314|5|Briefly described|Table 2|||L.- U.Permian. See P10||||||
4352|Collinsville Coal Measures|35150|6|Mentioned|p422|||||||||
4352|Collinsville Coal Measures|35467|6|Mentioned|p177|||Lithology described P184||||||
4352|Collinsville Coal Measures|35845|6|Mentioned|Fig.25|||||||||
4352|Collinsville Coal Measures|35873|6|Mentioned|p116|||See also Fig.25.||||||
4352|Collinsville Coal Measures|35937|6|Mentioned|p619|||||||||
4352|Collinsville Coal Measures|35940|6|Mentioned|Fig.2|||||||||
4352|Collinsville Coal Measures|36172|6|Mentioned|Appendix|||||||||
4352|Collinsville Coal Measures|36327|6|Mentioned|p3|||||||||
4352|Collinsville Coal Measures|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
4352|Collinsville Coal Measures|36739|6|Mentioned|p9|||See also P14.||||||
4352|Collinsville Coal Measures|37065|6|Mentioned|p29|||||||||
4352|Collinsville Coal Measures|37070|4|Described|p71|||||||||
4352|Collinsville Coal Measures|37071|4|Described|p83|||||||||
4352|Collinsville Coal Measures|37079|6|Mentioned|p137|||||||||
4352|Collinsville Coal Measures|37458|6|Mentioned|p438|||||||||
4352|Collinsville Coal Measures|37612|3|Fully described|p289|||See also P283.||||||
4352|Collinsville Coal Measures|38365|6|Mentioned|Fig.2|||||||||
4352|Collinsville Coal Measures|38958|5|Briefly described|p490|||||||||
4352|Collinsville Coal Measures|39212|5|Briefly described|p10|||||||||
4352|Collinsville Coal Measures|39252|5|Briefly described|p20|||||||||
4352|Collinsville Coal Measures|39264|6|Mentioned|p156|||||||||
4352|Collinsville Coal Measures|39267|6|Mentioned|p234|||||||||
4352|Collinsville Coal Measures|39268|6|Mentioned|p269|||||||||
4352|Collinsville Coal Measures|39423|6|Mentioned|p53|||||||||
4352|Collinsville Coal Measures|39445|5|Briefly described|Table 8|||||||||
4352|Collinsville Coal Measures|40093|6|Mentioned|p26|||||||||
4352|Collinsville Coal Measures|40321|6|Mentioned|p19|||||||||
4352|Collinsville Coal Measures|40539|6|Mentioned|p164|||||||||
4352|Collinsville Coal Measures|40571|6|Mentioned|p31|||||||||
4352|Collinsville Coal Measures|40574|6|Mentioned|p4|||||||||
4352|Collinsville Coal Measures|40685|5|Briefly described|p400|||||||||
4352|Collinsville Coal Measures|40968|4|Described|p276|||||||||
4352|Collinsville Coal Measures|41034|5|Briefly described|p366|||||||||
4352|Collinsville Coal Measures|41191|5|Briefly described|p284|||||||||
4352|Collinsville Coal Measures|41226|6|Mentioned|p26|||||||||
4352|Collinsville Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
4352|Collinsville Coal Measures|41597|6|Mentioned|p5|||||||||
4352|Collinsville Coal Measures|41689|6|Mentioned|Table 1|||||||||
4352|Collinsville Coal Measures|42187|6|Mentioned|p318|||See also Fig.3||||||
4352|Collinsville Coal Measures|42249|6|Mentioned|p22|||||||||
4352|Collinsville Coal Measures|42252|5|Briefly described|p49|||||||||
4352|Collinsville Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
4352|Collinsville Coal Measures|42257|5|Briefly described|Table 1 P263|||||||||
4352|Collinsville Coal Measures|42258|4|Described|p275|||||||||
4352|Collinsville Coal Measures|42648|6|Mentioned|p40|||||||||
4352|Collinsville Coal Measures|42932|6|Mentioned|p24|||||||||
4352|Collinsville Coal Measures|42994|6|Mentioned|p266|||Of Back Creek Group.||||||05-AUG-08
4352|Collinsville Coal Measures|43000|6|Mentioned|p111|||||||||
4352|Collinsville Coal Measures|43084|6|Mentioned|p15|||||||||
4352|Collinsville Coal Measures|43099|5|Briefly described|p7|||||||||
4352|Collinsville Coal Measures|43391|5|Briefly described|Map legend|Permian|Permian|Sandstone and conglomerate.||||||23-JUN-04
4352|Collinsville Coal Measures|43474|14|Not recorded|p69|||||||||
4352|Collinsville Coal Measures|43475|14|Not recorded|p553||Permian|||||||
4352|Collinsville Coal Measures|43706|5|Briefly described|p5||Early Permian|||||||
4352|Collinsville Coal Measures|43984|14|Not recorded|p132|||||||||
4352|Collinsville Coal Measures|43987|14|Not recorded|p267,270,273|||See also Lexicon.||||||
4352|Collinsville Coal Measures|43988|14|Not recorded|Map Legend||Permian|Of Back Creek Group.||||||
4352|Collinsville Coal Measures|43994|14|Not recorded|Map Legend|||||||||
4352|Collinsville Coal Measures|43995|14|Not recorded|p7|||||||||
4352|Collinsville Coal Measures|44000|14|Not recorded|Tb.1,2,p1,22,24-29,||Early Permian|Equivalent to upper part of Gebbie Formation. Contains Glendoo Sandstone Member, Unit of Middle Bowen Beds. p31-39,41,53,56-58,62-64,Pl.6||||||
4352|Collinsville Coal Measures|44001|14|Not recorded|Map Legend|||||||||
4352|Collinsville Coal Measures|44074|14|Not recorded|p185|||||||||
4352|Collinsville Coal Measures|44081|14|Not recorded|p205|||||||||
4352|Collinsville Coal Measures|44091|14|Not recorded|p44,Tb.3,p47||Permian|Basal Member of Middle Bowen Group.||||||
4352|Collinsville Coal Measures|44097|14|Not recorded|Fig.27,opp.p194|||||||||
4352|Collinsville Coal Measures|44127|14|Not recorded|p194|||||||||
4352|Collinsville Coal Measures|44219|14|Not recorded|p31||Artinskian|||||||
4352|Collinsville Coal Measures|44242|14|Not recorded|p14|||||||||
4352|Collinsville Coal Measures|44243|4|Described|p643-645,647-648||Early Permian|Coal seams.||||||
4352|Collinsville Coal Measures|44245|5|Briefly described|Map Legend||Permian|||||||
4352|Collinsville Coal Measures|44295|14|Not recorded|p6,43,map||Permian|||||||
4352|Collinsville Coal Measures|44311|2|Defined|p196-97|||Probably unconformably overlies Mount Devlin Volcanics.||||||
4352|Collinsville Coal Measures|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
4352|Collinsville Coal Measures|44347|14|Not recorded|p76-78,84|||||||||
4352|Collinsville Coal Measures|44348|14|Not recorded|p56|||||||||
4352|Collinsville Coal Measures|44372|6|Mentioned|p13|||||||||
4352|Collinsville Coal Measures|44424|14|Not recorded|p293-301|||Part of Gebbie Subgroup.||||||
4352|Collinsville Coal Measures|44489|14|Not recorded|p68,70|||||||||
4352|Collinsville Coal Measures|44542|14|Not recorded|p30|||||||||
4352|Collinsville Coal Measures|44630|14|Not recorded|p492,493||Early Permian|||||||
4352|Collinsville Coal Measures|44631|14|Not recorded|p205||Early Permian|||||||
4352|Collinsville Coal Measures|44635|14|Not recorded|p9|||Ref. to Reid 1929.||||||
4352|Collinsville Coal Measures|44722|14|Not recorded|p343,350,359||Early Permian|||||||
4352|Collinsville Coal Measures|44728|14|Not recorded|p222|||Equivalent to Calen Coal Measures.||||||
4352|Collinsville Coal Measures|45006|14|Not recorded|p38,39,126|||||||||
4352|Collinsville Coal Measures|45025|14|Not recorded|p62|||Mention to David 1932||||||
4352|Collinsville Coal Measures|45031|14|Not recorded|p9||Permian|||||||
4352|Collinsville Coal Measures|45071|3|Fully described|Table 8|||||||||
4352|Collinsville Coal Measures|45151|5|Briefly described|Table 10|||See also Table 7,11 and P15.||||||
4352|Collinsville Coal Measures|48626|14|Not recorded|p22|||||||||
4352|Collinsville Coal Measures|48841|14|Not recorded|p16,26,27|||Unconformably overlies Bulgonunna Volcanics.||||||
4352|Collinsville Coal Measures|48843|14|Not recorded|p.19-22,39,45|||(F55-11).||||||
4352|Collinsville Coal Measures|48847|14|Not recorded|p1-3,5,6,8,Pl.2|||Formerly thought to be at base of Middle Bowen Beds. Now equivalent to most of Unit B(middle).||||||
4352|Collinsville Coal Measures|48881|14|Not recorded|p6|||||||||
4352|Collinsville Coal Measures|48900|6|Mentioned|p84|||On table opposite.||||||
4352|Collinsville Coal Measures|48915|6|Mentioned|Table 1|||Permian. See also P3||||||
4352|Collinsville Coal Measures|48922|4|Described|p22|||L.-U.Perm.||||||
4352|Collinsville Coal Measures|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Early Permian|Geological Province: Bowen Basin.||||||04-FEB-08
4352|Collinsville Coal Measures|60386|6|Mentioned|p296|||Bowen/Sydney Basin. Non-marine, coal.||||||
4352|Collinsville Coal Measures|60659|5|Briefly described|p20|||Quartzose sandstone, conglomerate, siltstone, calcareous sublabile sandstone, coal seams and carbonaceous shale. Grade laterally into Gebbie Formation. Geological Province: Bowen Basin.||||||07-FEB-11
4352|Collinsville Coal Measures|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||13-MAR-09
4352|Collinsville Coal Measures|61772|6|Mentioned|p128 Fig. 2||Early Permian|In text, Coal Measures is C.M. Geological Province: Bowen Basin.||||||
4352|Collinsville Coal Measures|63172|6|Mentioned|p303|Early Permian|Early Permian|The Queensland equivalent of Mersey Coal Measures in Tasmania and Great Coal Measures in NSW.||||||07-FEB-11
4352|Collinsville Coal Measures|64665|6|Mentioned|p52, p53 Fig.2.|Middle Permian|Early Permian|Bowen Basin. Accumulated in a series of depositional environments, from fluvial to paralic.||||||
4352|Collinsville Coal Measures|65388|5|Briefly described|p187|||Northern Bowen Basin. Transitions into (lateral equivalent to) Gebbie Formation to the south, around the nominated Gebbie Formation type section in Gebbie Creek.  ||||||
4352|Collinsville Coal Measures|65706|6|Mentioned|p14 Tbl.1, p15 Tbl.1,|Late Permian|Early Permian|||Of Back Creek Group.||Unconformably overlies Bulgonunna Volcanic Group.||
4352|Collinsville Coal Measures|67402|4|Described|p21, p45, p80 tbl BWN1|Kungurian|Kungurian|Bowen Basin. Deposited in fluvial to near shore marine environments. See also  p84, p85 tbl BWN2, p165 tbl LPB1.||Back Creek Group||Overlies the Tiverton Formation. Unconformably overlain by the Moonlight Sandstone.|Quartzose sandstone, conglomerate, siltstone and coal.|
4352|Collinsville Coal Measures|67669|5|Briefly described|p11|Early Permian|Early Permian|Of Bowen Basin.||||Overlain by Blenheim Formation. Underlain by Tiverton Formation.||
4352|Collinsville Coal Measures|68679|4|Described|p378, p380-381, p383-384, p396|Permian|Permian|Webb and Crap (1960). N and NW Bowen Basin. 250m thick. Delta, delta plain deposits. Properties of the coal are described in some detail.||Blake Seam.|Glendoo Sandstone Member.|Unconformably overlies Lizzie Creek Volcanic Group. Passes laterally into Tiverton and Gebbie Formations. Correlated with Calen Coal Measures.|Quartzose sandstone, siltstone, mudstone, carbonaceous shale, conglomerate, coal.|
4352|Collinsville Coal Measures|70815|6|Mentioned|p3|||Bowen Basin.||||||
4352|Collinsville Coal Measures|71265|5|Briefly described|p589|Roadian|Kungurian|Bowen Basin.||||Overlies Lizzie Creek Volcanic Group. Is overlain unconformably by Blenheim Formation.||
4352|Collinsville Coal Measures|71701|5|Briefly described|p155, p170|Guadalupian|Cisuralian|Northern Area, Bowen Basin.||||Unconformably overlies the Lizzie Creek Volcanic Group. Unconformably overlain by the Blenheim Formation.||
4352|Collinsville Coal Measures|72297|5|Briefly described|p694, p703|Permian|Permian|SW of Moranbah, Bowen Basin. Includes coal of coking rank; indicative properties of export coking and thermal coals tabulated.||||||
4352|Collinsville Coal Measures|73246|6|Mentioned|p190|||Bowen Basin, northwest.||Back Creek Group||Overlain by Blenheim Subgroup. Equivalent to Gebbie Subgroup.||
4352|Collinsville Coal Measures|73495|6|Mentioned|p506|Kungurian|Artinskian|Bowen Basin.||||||
4381|Combarngo Volcanics|13516|5|Briefly described|p147 fig 5|Late Carboniferous|Late Carboniferous|From Roma Shelf, Bowen Basin. Also shown as "Kuttung" in brackets||||||
4381|Combarngo Volcanics|22863|6|Mentioned|p230|||||||||
4381|Combarngo Volcanics|22980|5|Briefly described|p248|||||||||
4381|Combarngo Volcanics|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
4381|Combarngo Volcanics|24069|5|Briefly described|p284|Carboniferous|Carboniferous|Geological Province: Surat Basin.||||||
4381|Combarngo Volcanics|24077|6|Mentioned|p407|||Geological Province: Bowen Basin.||||||
4381|Combarngo Volcanics|24263|5|Briefly described|p1389|Early Permian|Late Carboniferous|Geological Province: Bowen Basin||||||
4381|Combarngo Volcanics|29391|6|Mentioned|Table 4|||See P19.||||||
4381|Combarngo Volcanics|29721|6|Mentioned|p88|||||||||
4381|Combarngo Volcanics|30696|4|Described|Table 3|||Carboniferous-Lower Permian age. On P11||||||
4381|Combarngo Volcanics|32578|6|Mentioned|p347|||U.Carb. Strat. table||||||
4381|Combarngo Volcanics|33059|4|Described|Table 1|||L.Perm.-U.Carb.||||||
4381|Combarngo Volcanics|33530|6|Mentioned|Table 1|||Upper Carb.||||||
4381|Combarngo Volcanics|36045|6|Mentioned|p329|||||||||
4381|Combarngo Volcanics|36739|6|Mentioned|p22|||||||||
4381|Combarngo Volcanics|39252|6|Mentioned|p13|||||||||
4381|Combarngo Volcanics|39445|5|Briefly described|Table 7|||||||||
4381|Combarngo Volcanics|40787|4|Described|p356|||||||||
4381|Combarngo Volcanics|40960|6|Mentioned|p229|||||||||
4381|Combarngo Volcanics|41725|6|Mentioned|Fig.2|||||||||
4381|Combarngo Volcanics|42987|4|Described|p24|||||||||
4381|Combarngo Volcanics|43000|5|Briefly described|p106|||||||||
4381|Combarngo Volcanics|43008|5|Briefly described|map legend|||||||||
4381|Combarngo Volcanics|44787|14|Not recorded|Tb.p123,125,127,diag|||Equated to Carb.-L.Perm. Cracow Volcanics.||||||
4381|Combarngo Volcanics|45110|6|Mentioned|p66|||||||||
4381|Combarngo Volcanics|64855|5|Briefly described|p14-15, p16 Fig.2, p24|Early Permian|Late Carboniferous|Basal rocks in the Bowen Basin succession.||||||22-FEB-10
4381|Combarngo Volcanics|64856|3|Fully described|p42-44, p63, p102|Early Permian|Late Carboniferous|Traves (1966). Roma Shelf, Bowen Basin. Max thickness 145m. Correlated with Camboon Volcanics. Min age from overlying Reids Dome beds floras - APP1. Max age inferred from unconformably underlying Timbury Hills Formation. Basalt - rhyolite; felsic rocks widespread.| | ||||28-NOV-17
4381|Combarngo Volcanics|64857|5|Briefly described|p114, p113 Fig.3|||Bowen Basin. Unconformably overlain by Muggleton Formation. Text seems to imply an Early Permian age.||||||
4381|Combarngo Volcanics|64858|6|Mentioned|p180 Fig.2|Early Permian|Early Permian|||||||30-NOV-09
4381|Combarngo Volcanics|65115|5|Briefly described|p409|Early Permian|Late Carboniferous|Flows and pyroclastic rocks including olivine basalt, andesite and rhyolite. Considered by Murray (1994) to be equivalent to the Camboon Volcanics.||||||
4381|Combarngo Volcanics|65388|6|Mentioned|p21|||Roma Shelf. Intersected by petroleum wells. May be continuous with Camboon Volcanics.||||||
4381|Combarngo Volcanics|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
4381|Combarngo Volcanics|68679|5|Briefly described|p372 Fig.5.64, p375, p378-379, p381|Permian|Pennsylvanian|Traves (1966). Bowen Basin. >145m thick. Continental volcanics, with clastic detritus deposited in lakes: occurs west of the Meandarra Gravity Ridge. Age is uncertain.||||Is overlain by Reids Dome beds.|Mostly felsic volcanics: crystal and crystal-lithic tuff, some of which is probably ignimbrite; rhyolite; andesite and olivine basalt flows and clastics; andesitic conglomerates.|
4381|Combarngo Volcanics|68731|6|Mentioned|p164, p165 Fig 3.77, p166|Early Permian|Late Carboniferous|Fluvial to lacustrine sedimentary rocks are associated with this unit.|||Non-conformably underlain by the Roma granites.||Includes basalt, andesite, and rhyolitic tuffs, which are the most widespread component.|
4381|Combarngo Volcanics|70033|5|Briefly described|p2, p27, p29|Permian|Carboniferous|Age: late Carboniferous - earliest Permian (Murray 1994). Unit at base of Bowen Basin.|||||Volcanic succession.|
4381|Combarngo Volcanics|70673|4|Described|p3, p10, p62-65|Late Carboniferous|Late Carboniferous|Roma Shelf. A relatively thin, flat-lying succession of felsic and andesitic volcanic and volcaniclastic rocks with minor basalt. Sample from Bon Boggo Creek 3 core. 1973.28-2973.73m. This interval previously believed to be Timbury Hills Formation.|310.9 +/- 2.4 Ma (SHRIMP U-Pb zircon).|||Nonconformably overlies Roma Granites.|Includes rhyolitic ignimbrite.|23-APR-18
4381|Combarngo Volcanics|71592|5|Briefly described|Appendix A.|||Roma Shelf, Surat Basin.|311+/-2.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
4417|Condamine beds|22601|6|Mentioned|405|Permian|Permian|||||||
4417|Condamine beds|39071|6|Mentioned|p353|||||||||
4417|Condamine beds|43008|5|Briefly described|map legend|||||||||
4417|Condamine beds|63731|5|Briefly described|Map legend|Late Permian|Late Permian|Dark grey to black, slightly calcareous mudstone, with beds of coarse-grained pebbly arenite and conglomerate; some epiclastic sediments and rhyolitic crystal-lithic tuff beds; locally richly fossiliferous.||||||
4417|Condamine beds|63748|4|Described|p20, p21, p50|Late Permian|Late Permian|Faulted against Silverwood Group rocks; unconformably overlain by Marburg Subgroup sediments. Divided into 4 sequences (Olgers et al 1974) of arenites and mudstones, both fossiliferous and unfossiliferous. Geological province: Wandsworth Province.||||||07-FEB-11
4417|Condamine beds|68679|5|Briefly described|p446, p453|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Occurs 20km SE of Warwick as a 10 km2 outlier. Olgers et al. (1974) identified four subunits in the type area, each ~300m thick, briefly described in LITHOLOGY (DESCRIPTION). Abundant marine fauna includes the most diverse crinoid fauna in the State. Late Permian.||||Is faulted against the Silverwood Group. Is overlain unconformably by the Marburg Subgroup.|Mudstones, sandstones, conglomerate, rhyolitic crystal-lithic tuff.|
4417|Condamine beds|71628|5|Briefly described|p16:4|Permian|Permian|||||Is intruded by Cullendore Syenogranite.||
4448|Conjuboy Formation|23074|5|Briefly described|p737 (Fig 1)|Devonian|Devonian|||||||
4448|Conjuboy Formation|23291|4|Described|p37, p82 Tb. 3.6|Devonian|Devonian|First described and defined by Withnall (1889b) and Withnall (in Withnall and Lang 1993). Max. thickness: 150m. Geological Province: Georgetown Region.||||||08-JUL-15
4448|Conjuboy Formation|23430|4|Described|p505|||||||||
4448|Conjuboy Formation|23431|5|Briefly described|p532|||||||||
4448|Conjuboy Formation|23619|4|Described|p33 Table 1||Early Devonian|Underlying unit Einasleigh Metamorphics and Balcooma Metavolcanics - unconformable.||||||
4448|Conjuboy Formation|24611|5|Briefly described|p194|Emsian|Emsian|Geological Province: Georgetown Inlier.||||||11-MAY-17
4448|Conjuboy Formation|24613|6|Mentioned|p14, p131|||Geological province: Georgetown Province. Correlative of Mount Podge Limestone.||||||07-FEB-11
4448|Conjuboy Formation|41675|2|Defined|p67|Emsian||Reserved as Conjuboy||||||
4448|Conjuboy Formation|42031|5|Briefly described|Fig.3 P759|||||||||
4448|Conjuboy Formation|42054|6|Mentioned|p272|||||||||
4448|Conjuboy Formation|42279|4|Described|p22|||See also Fig.3||||||
4448|Conjuboy Formation|42933|4|Described|p220|||See also Fig.72||||||
4448|Conjuboy Formation|43113|4|Described|Table 1 p20||Emsian|||||||
4448|Conjuboy Formation|43253|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
4448|Conjuboy Formation|50202|5|Briefly described|Map legend|Early Devonian|Early Devonian|Quartzose to feldspathic sandstone, mudstone, and coralline limestone.||||||
4448|Conjuboy Formation|63154|5|Briefly described|p285 Fig. 5|Early Devonian|Early Devonian|Geological province: Georgetown Inlier. Mixed shallow marine sediments.||||||11-APR-07
4448|Conjuboy Formation|68344|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||||Quartzose to feldspathic sandstone, mudstone and coralline limestone.|
4448|Conjuboy Formation|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Broken River Province. This unit, as well as the Shield Creek Formation, Blue Rock Creek beds and Broken River Group, are all mapped under the symbol, Db.||||||
4448|Conjuboy Formation|68731|5|Briefly described|p187, p222, p223 Fig 3.126|Middle Devonian|Early Devonian|Type section occurs along Oaky Creek. Poorly exposed in its northern distribution. ~ 800 m thick. Richly fossiliferous with sporadic large heads of colonial rugose and tabulate corals.||||Nonconformably underlain by the Oasis Metamorphics. Correlative of the Chinaman Creek Limestone.|Comprises thick-bedded to very thick bedded, very coarse micaceous sandstone, commonly trough cross laminated.|03-JUL-14
4448|Conjuboy Formation|69592|6|Mentioned|p228|Middle Devonian|Early Devonian|Comprises remnants of minor basin successions as cover on parts of the North Australian Craton and Thompson Orogen.||||||
4448|Conjuboy Formation|70744|6|Mentioned|p947|Middle Devonian|Middle Devonian|Greenvale Province, NE extremity of Thomson Orogen. Is only slightly affected by tectonism.||||||
4452|Connolly Volcanics|22601|6|Mentioned|416|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
4452|Connolly Volcanics|31400|5|Briefly described|p165|||Mineralization discussed.||||||07-SEP-18
4452|Connolly Volcanics|32491|5|Briefly described|p7|||Sil.?-L.Devonian||||||
4452|Connolly Volcanics|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian? - Lower Devonian. Of Silverwood Group.||||||25-OCT-05
4452|Connolly Volcanics|32672|6|Mentioned|p673|||||||||
4452|Connolly Volcanics|33146|5|Briefly described|p2|||See also p3. ?Sil.-L.Dev.||||||07-SEP-18
4452|Connolly Volcanics|33326|6|Mentioned|p446|||Fauna.||||||
4452|Connolly Volcanics|33703|6|Mentioned|p207|||||||||
4452|Connolly Volcanics|35008|6|Mentioned|p175|||||||||
4452|Connolly Volcanics|35311|6|Mentioned|p207|||||||||
4452|Connolly Volcanics|35424|5|Briefly described|p8|||||||||
4452|Connolly Volcanics|35652|4|Described|p6|||||||||
4452|Connolly Volcanics|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
4452|Connolly Volcanics|39071|6|Mentioned|p345|||||||||
4452|Connolly Volcanics|39445|5|Briefly described|Table 5|||||||||
4452|Connolly Volcanics|42031|5|Briefly described|Fig.3 P759|||||||||
4452|Connolly Volcanics|48940|3|Fully described|p21|||||||||
4452|Connolly Volcanics|61392|4|Described|p163-165, p166|Emsian|Pridoli|Of Silverwood Group. Comprises lower extrusive lava flows, interbedded with sediments; upper unit deposited on a normal clastic or sand/mud-rich slope apron with sediments richer in primary volcaniclastic debris. Age: 422-389Ma. Max. thick: 2430m.||||||02-APR-13
4452|Connolly Volcanics|63731|5|Briefly described|Map legend|Devonian|Silurian|Of the Silverwood Group. Basaltic to locally dacitic volcaniclastic deposits, incl. volcanic breccia and crystal tuff, tog. with some flows; turbiditic volcaniclastic sediments; minor conglomerate lenses and limestone lenses; mod.-high magnetic response.||||||
4452|Connolly Volcanics|63748|4|Described|p6, p7 Fig. 3|Early Devonian|Middle Silurian|Of Silverwood Group. Conformable on Risdon Stud Formation; overlain by Bald Hill Formation. Max. thickness: ~2430m. In the Silverwood Province. Lower pyroclastics and lavas and upper thin bedded turbidites woth scattered coarse conglomeratic horizons||||||07-SEP-18
4452|Connolly Volcanics|68679|5|Briefly described|p445-446, p452-453|Early Devonian|Late Silurian|Olgers et al. (1974). Silverwood Province. 2430m thick. Lacks direct evidence of age. Some areas mapped as this unit were re-assigned to the Eight Mile Creek beds by Van Noord (1999).||Silverwood Group.||Overlies Risdon Stud Formation. Is overlain unconformably by Bald Hill Formation and Fitz Creek beds (or is faulted against the latter).|A lower succession of submarine volcaniclastics and lavas and associated intrusive dolerites: low-K tholeiitic basalt; overlain by mainly thin-bedded turbidites with scattered coarse conglomerate and limestone lenses, rich in volcaniclastic debris.|
4452|Connolly Volcanics|71628|5|Briefly described|p16:4|||||Silverwood Group.||Is intruded by Cullendore Syenogranite.||
4502|Cooktown Supersuite|23422|5|Briefly described|Plate 7.3|Late Permian|Late Permian|||||||
4502|Cooktown Supersuite|23423|4|Described|p310 table 7.4|Late Permian|Early Permian|S-type granite. Age: 275+/-5 Ma. See also p248-249. Units at the southern end were previously mapped as Mareeba Granite. Plutons farther north were mapped as Finlayson Granite and far north they were Alfanmoui Granite.||||||
4502|Cooktown Supersuite|23430|5|Briefly described|p475|||S-Type Granites - Daintree Subprovince. Kennedy Province.||||||
4502|Cooktown Supersuite|23431|5|Briefly described|p539|||S-type granite||||||
4502|Cooktown Supersuite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|||||||
4502|Cooktown Supersuite|23512|5|Briefly described|Map Legend||Late Permian|||||||
4502|Cooktown Supersuite|24086|5|Briefly described|p312 Fig. 1|Late Permian|Late Permian|||||||
4502|Cooktown Supersuite|24213|5|Briefly described|p777|||||||||
4502|Cooktown Supersuite|42658|6|Mentioned|p33|||Variation on Cooktown Granite?||||||
4502|Cooktown Supersuite|42968|5|Briefly described|p99|||||||||
4502|Cooktown Supersuite|43070|6|Mentioned|p13|||||||||
4502|Cooktown Supersuite|43111|6|Mentioned|p21|||||||||
4502|Cooktown Supersuite|43285|5|Briefly described|Map Legend|||age Early? to Late Permian.||||||
4502|Cooktown Supersuite|43625|4|Described|p56|||||||||
4502|Cooktown Supersuite|50587|5|Briefly described|Map Legend|Late Permian|Late Permian| Geological Province: Kennedy Province. Includes: Cooktown Granite, Charlotte Granite, Finch Bay Granite.||||||
4502|Cooktown Supersuite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|||||||
4502|Cooktown Supersuite|60425|4|Described|p36, p54 Tb. 4, p91|Late Permian|Late Permian|Contains 11 named Suites and their granites. Some units previously mapped as Mareeba and Finlayson Granites. Extensively deformed rocks of probably Early Permian age. S-type granites. Detailed lithology in Tb. 4 and p91,  p270-1 Appdx. 1.||||||07-FEB-11
4502|Cooktown Supersuite|62371|5|Briefly described|p472 Fig.3|Permian|Permian|S-type granite.||||||
4502|Cooktown Supersuite|63140|6|Mentioned|p572 fig 3|Early Permian|Early Permian||||||S-type.|
4502|Cooktown Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province. S-type granites.||||||
4502|Cooktown Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Brodies Camp, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
4502|Cooktown Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|275 +/- 5 Ma (SHRIMP).||||S-type granitoids.|
4502|Cooktown Supersuite|69593|4|Described|p478-482, p505, p506 Fig.6.26, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Comprises the eastern belt of magmatism in NE Hodkinson Province. Crops out over ~250 km2. Associated with lode (Collingwood) and alluvial (Kings Plain) tin deposits. Geochemistry described. Early- to late(?) Permian.|c.275 Ma.||Barrow Point, Big Tableland, Boolbun, Collingwood, Cooktown, Mount Hartley, Mount Poverty, Roaring Meg, Starcke, Waterfall Suites; Lizard Island, Mount Finnigan Granites; Mrs Watsons Bay Microgranite.||S-type. Highly-porphyritic to even-grained, (altered cordierite-tourmaline) biotite-muscovite and muscovite-biotite granite; rare garnet, topaz, sillimanite, andalusite; gneissic enclaves, miarolitic cavities.|
4502|Cooktown Supersuite|72983|6|Mentioned|p3, p28, p31|||Hodgkinson Province, eastern. Younger than the Whypalla Subersuite by 15-20 Myrs. Previously[?] described as the two-mica granites of the Cooktown-Rossville area.|||Collingwood Granite, Charlotte Granite||S-type igneous rocks.|
4502|Cooktown Supersuite|73197|6|Mentioned|p476 Fig.7|Middle Triassic|Lopingian||||||Intrusives.|
4512|Cooladdi Dolomite|22464|5|Briefly described|p9||Middle Devonian|Adavale Basin. Overlies Lissoy Sandstone, overlain by Etonvale Formation||||||
4512|Cooladdi Dolomite|22518|6|Mentioned|p 10|||Adavale Basin||||||
4512|Cooladdi Dolomite|22604|6|Mentioned|p442|||Of Log Creek Formation?, Emsian in age?||||||09-OCT-08
4512|Cooladdi Dolomite|29721|6|Mentioned|p38|||||||||
4512|Cooladdi Dolomite|33069|4|Described|p6|||Mid.Dev. Adavale Gp.||||||
4512|Cooladdi Dolomite|38226|6|Mentioned|p414|||||||||
4512|Cooladdi Dolomite|39478|6|Mentioned|Table 1|||||||||
4512|Cooladdi Dolomite|39482|6|Mentioned|p158|||||||||
4512|Cooladdi Dolomite|39494|6|Mentioned|Fig.3|||||||||
4512|Cooladdi Dolomite|40030|6|Mentioned|Fig.3|||||||||
4512|Cooladdi Dolomite|40322|6|Mentioned|Fig.3|||||||||
4512|Cooladdi Dolomite|40544|6|Mentioned|Fig.4|||||||||
4512|Cooladdi Dolomite|41097|6|Mentioned|Table 1|||||||||
4512|Cooladdi Dolomite|41167|6|Mentioned|p397|||||||||
4512|Cooladdi Dolomite|41198|6|Mentioned|p35|||See also Table 1||||||
4512|Cooladdi Dolomite|41208|6|Mentioned|Fig.1|||||||||
4512|Cooladdi Dolomite|41247|6|Mentioned|Fig.5|||||||||
4512|Cooladdi Dolomite|41289|6|Mentioned|p210|||||||||
4512|Cooladdi Dolomite|42031|5|Briefly described|Fig.8 P766|||||||||
4512|Cooladdi Dolomite|42999|5|Briefly described|Table1.p90|||||||||
4512|Cooladdi Dolomite|43004|5|Briefly described|Table 1,p179|||||||||
4512|Cooladdi Dolomite|43007|5|Briefly described|p256|||||||||
4512|Cooladdi Dolomite|43105|5|Briefly described|Fig.5,p10|||||||||
4512|Cooladdi Dolomite|62985|5|Briefly described|p16|Givetian|Givetian|Overlies Lissoy Sandstone and part of Bury Limestone. Its dolomitisation is postulated to have occurred with deposition of the halite-dominant Boree Salt in a restricted basin. Geol. prov: Adavale Basin.||||||09-OCT-08
4512|Cooladdi Dolomite|64783|3|Fully described|p95-98, 82, 84, 86, 87,93,99,100|Givetian|Givetian|Slanis and Netzel (1967) called it the Cooladdi Carbonate Member, replacing Etonvale D3 Member. Auchincloss (1976) included it in the Log Creek Formation. Paten (1977) gave it Formation status and Galloway (1970) defined the type section in PPC Etonvale-1 (2295.8 to 2335.4m).  A significant lithologic and seismic marker in the Adavale Basin and Warrabin Trough. Hosts minor hydrocarbons.||||Conformably overlies the Lissoy Sandstone and Bury Limestone. Lateral equivalent of upper Bury Limestone. Unconformably overlain by the Etonvale Formation; conformably overlain by the Boree Salt.|Maximum thickness is 84.9m. Consists mostly of dolomitic mudstone and siltstone; some lamination and interbedding with fine, sub-labile sandstone and minor limestone occurs.|15-NOV-17
4512|Cooladdi Dolomite|67402|4|Described|p167 fig ADV/WRR3, p168|Givetian|Givetian|Adavale Basin. Deposited in lagoonal, back reef, subtidal to intertidal and open marine environments. Up to 85m thick and forms a seal for hydrocarbons. See also p170, p171 fig ADV/WRR7, p172, p173, p175.||||Overlies the Bury Limestone and the Lissoy Sandstone. Overlain by the Boree Salt.|Dolomitic mudstone and siltstone interbedded with fine-grained sub-labile sandstone and minor limestone that is fossiliferous and alternatively wackestone or packstone.|
4512|Cooladdi Dolomite|68731|5|Briefly described|p177 Fig 3.91, p179, p180 Tb 3.3, p183|Late Devonian|Middle Devonian|Slanis and Netzel (1967). Subtidal-intertidal to open-marine and low- to high-energy environment. Includes minor corals, small brachiopods, annelids, gastropods, wood fragments, crinoids, corals, as well as algal ghosts and micro-organisms.|||||Comprises primarily dolomitic mudstone and siltstone; some lamination and interbedding with fine, sub-labile sandstone and minor limestone. Styolites and minor fossiliferous limestone (wackestone and packstone) are also present.|
4512|Cooladdi Dolomite|72297|5|Briefly described|p746|||Adavale Basin. Hydrocarbon cap rock (over the Lissoy Sandstone reservoir) in PPC Gilmore 1 in the Gilmore gasfield.||||||
4512|Cooladdi Dolomite|73179|6|Mentioned|p1135, p1152|Givetian|Eifelian|Adavale Basin. Dolomitic sandstone in Yongala-1 drillhole is not part of this unit.||||||
4543|Coolibah Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Limestone (micrite, grainstone, cryptalgal boundstone), marl, chert.||||||
4543|Coolibah Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Wackestones, grainstones, micrite, conglomerate.||||||
4543|Coolibah Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Early Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
4543|Coolibah Formation|13995|5|Briefly described|p67, p75, p77, p79, p89, p99, p101|Middle Ordovician|Early Ordovician|Georgina Basin. Bendigonian-Castlemanian. Rostroconch species listed. Gastropod species and biogeographic links. Nautiloid fauna (includes the first actinoceratid in Australia) have contemporaries in Horn Valley Siltstone and Stairway Sandstone (Amadeus Basin). Conodonts in this unit have links to those in N China and elsewhere in Asia and the Americas.||||||
4543|Coolibah Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
4543|Coolibah Formation|22954|6|Mentioned|Fig3p9|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 110m.||||||
4543|Coolibah Formation|24442|5|Briefly described|p49|Cambrian|Early Cambrian|Overlies the Kelly Creek Formation.  On TOBERMORY sheet.||||||
4543|Coolibah Formation|30983|4|Described|p70|||Arenigian||||||
4543|Coolibah Formation|33111|4|Described|p34|||Mention Fig.9||||||
4543|Coolibah Formation|33657|6|Mentioned|p1|||||||||
4543|Coolibah Formation|33738|6|Mentioned|p54|||||||||
4543|Coolibah Formation|34252|6|Mentioned|Po.2|||Fossils||||||
4543|Coolibah Formation|34454|5|Briefly described|Table 2|||M.Ordovician||||||
4543|Coolibah Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||07-AUG-06
4543|Coolibah Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|35139|4|Described|Table.2|||||||||
4543|Coolibah Formation|35146|6|Mentioned|p468|||||||||
4543|Coolibah Formation|36234|3|Fully described|p172|||See also Fig.1.||||||
4543|Coolibah Formation|36243|6|Mentioned|Table 1A|||||||||
4543|Coolibah Formation|36580|6|Mentioned|p469|||See also Fig.1||||||
4543|Coolibah Formation|37572|4|Described|p163|||See also Fig.8||||||
4543|Coolibah Formation|39445|5|Briefly described|Table 4|||See also p61 and Fig.5.||||||07-AUG-06
4543|Coolibah Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|39943|6|Mentioned|Table 2B|||||||||
4543|Coolibah Formation|40136|5|Briefly described|p22|||||||||
4543|Coolibah Formation|41524|6|Mentioned|Fig.3|||||||||
4543|Coolibah Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||07-AUG-06
4543|Coolibah Formation|42060|6|Mentioned|Fig.5 P140|||||||||
4543|Coolibah Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
4543|Coolibah Formation|43803|6|Mentioned|Fig.5,p71|||||||||
4543|Coolibah Formation|43808|5|Briefly described|p293||Early Ordovician|||||||
4543|Coolibah Formation|44308|14|Not recorded|p10,Tb.1||Early Ordovician|||||||
4543|Coolibah Formation|44309|2|Defined|Tb.1,p12,17|||Fauna closely related to Kelly Creek Formation.||||||
4543|Coolibah Formation|44312|14|Not recorded|Map Legend||Early Ordovician|||||||
4543|Coolibah Formation|44326|14|Not recorded|Map Legend||Early Ordovician|||||||
4543|Coolibah Formation|44358|6|Mentioned|p10,19|||||||||
4543|Coolibah Formation|44469|2|Defined|p.10,19,opp.p.6,Tb.I|||(F53-12). Unit of Toko Group. Overlies Kelly Creek Formation.; overlain by Nora Formation.||||||11-FEB-09
4543|Coolibah Formation|44470|5|Briefly described|map legend||Early Ordovician|Lower Ordovician.||||||02-DEC-04
4543|Coolibah Formation|44852|14|Not recorded|p71||Ordovician|Middle Ordovician||||||
4543|Coolibah Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Ordovician|Unit of Toko Group.||||||
4543|Coolibah Formation|45022|14|Not recorded|p.86|||Tb.12||||||
4543|Coolibah Formation|45052|2|Defined|p127|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|45115|6|Mentioned|p6|||||||||
4543|Coolibah Formation|45118|6|Mentioned|p3|||||||||
4543|Coolibah Formation|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
4543|Coolibah Formation|45155|6|Mentioned|Fig.8|||||||||
4543|Coolibah Formation|46841|6|Mentioned|p97|||||||||
4543|Coolibah Formation|46897|6|Mentioned|Fig.3|||||||||
4543|Coolibah Formation|46959|6|Mentioned|Table 1|||||||||
4543|Coolibah Formation|47024|6|Mentioned|p1|||||||||
4543|Coolibah Formation|47052|6|Mentioned|p262|||||||||
4543|Coolibah Formation|48901|14|Not recorded|Not recorded||Ordovician|M.Ordovician, Toko Gp.||||||
4543|Coolibah Formation|48938|6|Mentioned|p20|||Nomenclature table.||||||
4543|Coolibah Formation|48942|6|Mentioned|p59|||Refers Laing and Allen (1956).||||||07-AUG-06
4543|Coolibah Formation|48943|6|Mentioned|p62|||Refers Laing and Allen (1956).||||||07-AUG-06
4543|Coolibah Formation|49027|4|Described|p17|||||||||
4543|Coolibah Formation|60122|3|Fully described|p29-30, p10 Tb. 1|Early Ordovician|Early Ordovician|Of the Toko Group. Grey and white limestone, quartzic limestone, dolostone marl, siltstone, basal conglomerate; local chert lenses. Conformably overlies Kelly Cr Fm; conformably underlies Nora Fm. Max. thick: 110m. Geol.Prov: Georgina Basin. See also p4-5||||||
4543|Coolibah Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group.  Limestone, quartzic limestone, dolostone, marl, siltstone; basal limestone.  Overlies the Kelly Creek Formation; overlain by Nora Formation.||||||
4543|Coolibah Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Limestone, quartzic limestone, dolostone, marl, siltstone; basal sandstone. Geological Province: southern Georgina Basin.||||||12-OCT-05
4543|Coolibah Formation|62794|5|Briefly described|p298|Early Ordovician|Early Ordovician|Georgina Basin. Underlies Nora Formation. Stait & Druce (1993) correlated uppermost Coolibah Formation with lower Horn Valley Siltstone in the  Amadeus Basin, on the basis of conodont faunas.||||||05-DEC-12
4543|Coolibah Formation|63450|4|Described|p78 Fig. 5, p82|Arenig|Arenig|Conformably overlies Kelly Creek Formation; overlain by Nora Formation.Max. thickness: 110m. Geological province: Georgina Basin, West Toko Syncline. Comprises limestones, quartzic limestone, dolostone and marl.||||||07-FEB-11
4543|Coolibah Formation|64068|3|Fully described|p76, 75, p19|Middle Ordovician|Middle Ordovician|Variable thickness. Very diverse fauna. Correlations: Upper part of Kelly Creek Formation, Horn Valley Siltstone, possibly Djagamara Formation.||Of Toko Group.||Conformably to disconformably overlies Kelly Creek Formation. Is conformably overlain by Nora Formation.|Grey and white limestone, quartzic limestone, dolostone, marl, lenticular chert; basal sandstone, conglomerate or silicified microbial boundstone.|04-APR-12
4543|Coolibah Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
4543|Coolibah Formation|65237|5|Briefly described|p4 Fig. 7|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|65489|5|Briefly described|p123, p125-126|Ordovician|Ordovician|Georgina Basin. Contains bitumen. Gas show from Ethabuka 1 in the Toko Syncline.||||Overlies Kelly Creek Formation.||
4543|Coolibah Formation|67323|5|Briefly described|GIS attrib tbl, p83, p88, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also Solid Geology Map. Georgina Basin. A gas flow of c.6000 m3/day was recorded from this unit in AOD Ethabuka 1.||Toko Group.||Overlies Kelly Creek Formation. Is overlain by Nora Formation.|Limestone, calcilutite, dolomite, marl, chert|
4543|Coolibah Formation|67402|5|Briefly described|p25 tbl RRM3, p213 fig GRG3|Castlemanian|Chewtonian|Georgina Basin, West Toko Syncline. Maximum thickness of 110m. Potentially a conventional seal for carbon dioxide storage. Not likely to be a reservoir for carbon dioxide as it is believed to have inadequate injectivity. See also p213 fig GRG5, p215, p216, p217.||||Overlies the Kelly Creek Formation. Is laterally equivalent to or is conformably overlain by the Nora Formation.|Limestone, quartzitic limestone, dolostone and marl.|
4543|Coolibah Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as Kelly Creek Formation and the Toko Group, are all mapped under the symbol, Ot.||||||
4543|Coolibah Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Kelly Creek Formation. Is overlain by Nora Formation.||12-JUL-16
4543|Coolibah Formation|69443|3|Fully described|p28:7, 27-28|Early Ordovician|Early Ordovician|Casey in Smith (1965). Southern Georgina Basin. Poorly exposed. Upper and lower contacts are diachronous. Up to 110m thick; only 7.5m in the type area in southeast TOBERMOREY map area. Contains a varied fossil fauna (listed) indicating a mid- to late-Floian age. Intertidal to shallow-subtidal marine deposits with fluctuating energy conditions.||Toko Group.||Conformably to disconformably overlies Kelly Creek Formation. Is overlain by Nora Formation conformably.|Limestone, quartzose limestone, dolostone, marl and local lenticular chert; basal interval of sandstone, conglomerate or silicified microbial boundstone.|12-JUL-16
4543|Coolibah Formation|69591|5|Briefly described|p87, p94-95|Early Ordovician|Early Ordovician|West Toko Syncline, Georgina Basin. This unit is here removed from the otherwise clastic-dominated Toko Group and assigned to the carbonate-dominated Cockroach Group. Variable thickness up to 160m. Age from acritarchs and conodonts.||Cockroach Group.||Disconformably/conformably overlies Kelly Creek Formation. Is overlain by Nora Formation.|Includes limestone, sandy limestone, calcilutite, dolomite and marl with some lenses of chert.|
4543|Coolibah Formation|69673|4|Described|p118, p119 fig 94, p136, p140|Ordovician|Ordovician|up to 110m thick (in Queensland). Reasonable reservoir potential.||Toko Group||Conformably overlies Kelly Creek Formation, overlain by Nora Formation|Limestone, dolostone, marl and local lenticular chert with a basal interval of sandstone, conglomerate or silicified microbia boundstone.|
4543|Coolibah Formation|70380|6|Mentioned|p745|Dapingian|Floian|Southern Georgina Basin.||||||
4543|Coolibah Formation|70968|6|Mentioned|p115, p117|||Laing and Allen (1956), who included rocks subsequently named the Wondoan and Stubbs Formations.||||||
4543|Coolibah Formation|72500|6|Mentioned|p386, p393-394, p396-397, p399|Middle Ordovician|Early Ordovician|Georgina Basin. Said to be Arenig age.||||||28-AUG-20
4543|Coolibah Formation|72503|6|Mentioned|p33|||Georgina Basin. Contains typical shallow-water [conodont] forms (e.g., Aurilobodus leptosomatus and Tangshanodus sp.).||||||
4557|Cooloola dune sand|38302|6|Mentioned|Table 1|||Informal name||||||
4557|Cooloola dune sand|39495|6|Mentioned|p142|||||||||
4557|Cooloola dune sand|62102|5|Briefly described|p367 Tb. 1, p371|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast.  Age: >486Ka (est.).||||||
4610|Cooneana Sandstone Member|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Tivoli Formation||||
4610|Cooneana Sandstone Member|32180|5|Briefly described|p6|||||||||
4610|Cooneana Sandstone Member|38076|6|Mentioned|p26|||||||||
4610|Cooneana Sandstone Member|38307|6|Mentioned|p521|||||||||
4610|Cooneana Sandstone Member|41906|5|Briefly described|p22|||Of Tivoli Formation||||||28-SEP-05
4610|Cooneana Sandstone Member|68679|5|Briefly described|p394|||Ipswich Basin. ~40m thick. Bundamba Anticline axis.||Tivoli Formation.|||Coarse-grained sandstone.|
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.||
4727|Corella Formation|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Mary Kathleen Group.  Includes: Agate Downs Siltstone Member. Underlies Mount Birnie Beds, Roxmere Quartzite, Kuridala Formation. Overlies Marimo Slate, Answer Slate.||||||18-JAN-07
4727|Corella Formation|22460|5|Briefly described|p447|||Also see p460 Fig 19. Of the Mary Kathleen Group.||||||18-JAN-07
4727|Corella Formation|22461|4|Described|p473|||Also see Fig 1 p464 and Fig 2 p466.  Underlain by Marimo Slate.||||||18-JAN-07
4727|Corella Formation|22462|5|Briefly described|P6||Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|22483|4|Described|p414|||also fig 1 p415.||||||
4727|Corella Formation|22515|6|Mentioned|p401-2,404,407-8|||||||||
4727|Corella Formation|22623|6|Mentioned|p226|||||||||
4727|Corella Formation|22667|6|Mentioned|P235|||||||||
4727|Corella Formation|22720|5|Briefly described|Table 4 (p166)|||In the Mt Isa Block.||||||18-JAN-07
4727|Corella Formation|22722|6|Mentioned|p268-70,72,74,76,77||Statherian|||||||
4727|Corella Formation|22723|6|Mentioned|p262||Statherian|||||||
4727|Corella Formation|22734|5|Briefly described|p292,6,8||Statherian|Sag basin deposits hosting Revenue Granite.||||||18-JAN-07
4727|Corella Formation|22747|5|Briefly described|p6||Precambrian|See also Table1,p7. Unconformably overlies Eastern Creek Volcanics. Overlain by Myally Beds. 2000 m thick.||||||
4727|Corella Formation|23068|5|Briefly described|p784 (fig 1)|||||||||
4727|Corella Formation|23079|5|Briefly described|p701||Proterozoic|||||||
4727|Corella Formation|23324|5|Briefly described|p468 Fig.1, p470 Fig. 2|Statherian|Statherian|Age: 1780-1760Ma. Overlies Argylla Fm. Includes: calc-silicate, metasiltstone, marble, metaquartzite; banded garnet-pyroxene skarn; massive garnet skarn; metapelite, strongly sheared.||||||27-MAY-08
4727|Corella Formation|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1750+/-7Ma.||||||18-JAN-07
4727|Corella Formation|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
4727|Corella Formation|23395|6|Mentioned|p387|||||||||
4727|Corella Formation|23458|5|Briefly described|p115|||Intruded by Dipvale Granodiorite. Includes amphibolite-grade metasediments.||||||27-AUG-07
4727|Corella Formation|23518|4|Described|p10|Proterozoic|Proterozoic|Of Mary Kathleen Group. Geological Province: Eastern Fold Belt.||||||27-MAY-08
4727|Corella Formation|23519|5|Briefly described|p110 Table 1|Mesoproterozoic|Mesoproterozoic|Of Mary Kathleen Group. Geological Province: Tommy Creek Block.||||||
4727|Corella Formation|23901|5|Briefly described|p1685|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Geological Province: Mount Isa Inlier.||||||
4727|Corella Formation|23957|6|Mentioned|p1124|||Geological Province: Mary Kathleen Zone.||||||
4727|Corella Formation|23959|5|Briefly described|p1165|Precambrian|Precambrian|Intruded by the Burstall Granite and the Lunch Creek Gabbro.  Overlies Argylla Volcanics.  Geological Province: Cloncurry Basin.||||||18-JAN-07
4727|Corella Formation|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Of the Mary Kathleen Group.||||||
4727|Corella Formation|23971|5|Briefly described|p1406|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier||||||
4727|Corella Formation|23975|5|Briefly described|p1464|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Mary Kathleen Group.||||||
4727|Corella Formation|23986|5|Briefly described|p69|||||||||
4727|Corella Formation|24032|6|Mentioned|p27|||Calcareous outcrops.||||||
4727|Corella Formation|24197|6|Mentioned|p92|||Interbedded with felsic volcanics coeval with the intrusive Burstall Suite.||||||07-FEB-11
4727|Corella Formation|24253|5|Briefly described|p4, p6 Fig.2, p10 Fig.4|Proterozoic|Proterozoic|Age: 1760-1740Ma. Geological Province: Mount Isa Block.||||||
4727|Corella Formation|24254|5|Briefly described|p19 Fig.2|||Geological Province: Mount Isa Block.||||||
4727|Corella Formation|24255|5|Briefly described|p31, p32 Fig.2|||Geological Province: Eastern Succession, Mount Isa Block.||||||
4727|Corella Formation|24256|6|Mentioned|p52|||Geological Province: Mount Isa Block.||||||
4727|Corella Formation|24257|6|Mentioned|p66|||Geological Province: Eastern fold belt, Mount Isa Block. Formation is Fm. in text.||||||
4727|Corella Formation|24259|5|Briefly described|p106, p108|Statherian|Statherian|Geological Province: Mount Isa Block. Age: 1780 - 1740Ma.||||||
4727|Corella Formation|24432|4|Described|p562 Fig.2|Statherian|Statherian|Overlies Overhang Jaspilite. Age: 1742-1725 Ma. Carbonate. Geological Province: Eastern Fold Belt.||||||
4727|Corella Formation|24462|5|Briefly described|p296 Fig. 1|||||||||
4727|Corella Formation|29550|5|Briefly described|p44|||||||||
4727|Corella Formation|29960|6|Mentioned|p10|||||||||
4727|Corella Formation|29961|6|Mentioned|p6|||||||||
4727|Corella Formation|29965|6|Mentioned|p403|||||||||
4727|Corella Formation|29966|6|Mentioned|p396|||||||||
4727|Corella Formation|29969|5|Briefly described|p392|||||||||
4727|Corella Formation|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4727|Corella Formation|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4727|Corella Formation|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
4727|Corella Formation|30530|6|Mentioned|p516|||||||||
4727|Corella Formation|30531|1|Redefined|p20|Precambrian|Precambrian|||||||
4727|Corella Formation|30532|6|Mentioned|p113|||||||||
4727|Corella Formation|30558|6|Mentioned|p42|||||||||
4727|Corella Formation|30601|6|Mentioned|p419|||||||||
4727|Corella Formation|30912|6|Mentioned|p364|||Proterozoic age||||||
4727|Corella Formation|31043|4|Described|p53|||||||||
4727|Corella Formation|31257|6|Mentioned|p398|||||||||
4727|Corella Formation|31704|6|Mentioned|p4|||Copper associated with calcite.||||||
4727|Corella Formation|31824|6|Mentioned|p32|||L.Proterozoic||||||
4727|Corella Formation|32660|5|Briefly described|Table 5|||||||||
4727|Corella Formation|32770|6|Mentioned|p44|||Geological plan. Cordiorite P45||||||
4727|Corella Formation|32959|6|Mentioned|p31|||||||||
4727|Corella Formation|33111|6|Mentioned|p6|||||||||
4727|Corella Formation|33113|6|Mentioned|Fig.1|||U.Proterozoic||||||
4727|Corella Formation|33214|6|Mentioned|Fig.1|||||||||
4727|Corella Formation|33225|6|Mentioned|p25|||||||||
4727|Corella Formation|33561|6|Mentioned|p102|||||||||
4727|Corella Formation|33791|6|Mentioned|p373|||||||||
4727|Corella Formation|33900|5|Briefly described|p17|||||||||
4727|Corella Formation|34061|6|Mentioned|p54|||||||||
4727|Corella Formation|34998|6|Mentioned|p347|||||||||
4727|Corella Formation|35008|5|Briefly described|p180|||||||||
4727|Corella Formation|35074|6|Mentioned|Fig.2|||||||||
4727|Corella Formation|35139|6|Mentioned|p41|||||||||
4727|Corella Formation|35167|6|Mentioned|p151|||||||||
4727|Corella Formation|35286|6|Mentioned|p155|||||||||
4727|Corella Formation|35295|6|Mentioned|p601|||See aslo P602||||||
4727|Corella Formation|35309|6|Mentioned|p373|||||||||
4727|Corella Formation|35388|6|Mentioned|p89|||Also see Fig.10||||||
4727|Corella Formation|35470|6|Mentioned|22|||||||||
4727|Corella Formation|35495|6|Mentioned|p344|||||||||
4727|Corella Formation|35932|6|Mentioned|p452|||||||||
4727|Corella Formation|35939|5|Briefly described|p629|||||||||
4727|Corella Formation|36052|6|Mentioned|p419|||See also Fig.2.||||||
4727|Corella Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4727|Corella Formation|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
4727|Corella Formation|36963|6|Mentioned|p243|||||||||
4727|Corella Formation|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4727|Corella Formation|37462|6|Mentioned|p267|||||||||
4727|Corella Formation|37568|4|Described|p83|||||||||
4727|Corella Formation|37569|6|Mentioned|p92|||||||||
4727|Corella Formation|37645|5|Briefly described|Fig.3|||||||||
4727|Corella Formation|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4727|Corella Formation|37862|6|Mentioned|p581|||||||||
4727|Corella Formation|38234|4|Described|p103|||||||||
4727|Corella Formation|38235|3|Fully described|p113|||||||||
4727|Corella Formation|38238|6|Mentioned|p135|||||||||
4727|Corella Formation|38276|6|Mentioned|Fig.1|||||||||
4727|Corella Formation|38278|6|Mentioned|Fig.3|||||||||
4727|Corella Formation|38350|4|Described|p12|||||||||
4727|Corella Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4727|Corella Formation|38560|6|Mentioned|p115|||||||||
4727|Corella Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4727|Corella Formation|38618|6|Mentioned|p88|||||||||
4727|Corella Formation|38619|6|Mentioned|p127|||||||||
4727|Corella Formation|38833|6|Mentioned|p161|||||||||
4727|Corella Formation|38834|6|Mentioned|p162|||||||||
4727|Corella Formation|39049|6|Mentioned|p840|||||||||
4727|Corella Formation|39124|6|Mentioned|p160|||||||||
4727|Corella Formation|39202|5|Briefly described|p229|||||||||
4727|Corella Formation|39445|5|Briefly described|p36|||See also p42 and Table 2.||||||18-JAN-07
4727|Corella Formation|39492|6|Mentioned|p28|||||||||
4727|Corella Formation|39496|6|Mentioned|PP10|||||||||
4727|Corella Formation|39622|6|Mentioned|p27|||See also P28||||||
4727|Corella Formation|39798|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
4727|Corella Formation|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4727|Corella Formation|39937|4|Described|p81|||||||||
4727|Corella Formation|40593|6|Mentioned|p78|||||||||
4727|Corella Formation|40623|5|Briefly described|p95|||Briefly described p111.||||||18-JAN-07
4727|Corella Formation|40648|3|Fully described|p9|||||||||
4727|Corella Formation|40783|6|Mentioned|p1009|||||||||
4727|Corella Formation|40840|6|Mentioned|Map legend|||||||||
4727|Corella Formation|40984|5|Briefly described|p389|||||||||
4727|Corella Formation|41069|5|Briefly described|p452|||||||||
4727|Corella Formation|41150|5|Briefly described|p1806|||||||||
4727|Corella Formation|41272|5|Briefly described|M 1of1 D07|||See also M 1of 1 N06.||||||15-MAR-18
4727|Corella Formation|41306|6|Mentioned|p4|||||||||
4727|Corella Formation|41568|6|Mentioned|p10|||||||||
4727|Corella Formation|41614|6|Mentioned|p145|||||||||
4727|Corella Formation|41615|6|Mentioned|p147|||||||||
4727|Corella Formation|41744|5|Briefly described|p416|||||||||
4727|Corella Formation|41761|6|Mentioned|p284|||||||||
4727|Corella Formation|41791|6|Mentioned|p249|||||||||
4727|Corella Formation|41862|6|Mentioned|p474|||||||||
4727|Corella Formation|41979|6|Mentioned|p527|||||||||
4727|Corella Formation|42166|5|Briefly described|p108|||||||||
4727|Corella Formation|42173|6|Mentioned|p171|||||||||
4727|Corella Formation|42201|5|Briefly described|p292|||||||||
4727|Corella Formation|42234|5|Briefly described|p1055|||||||||
4727|Corella Formation|42365|5|Briefly described|Fig.3 P258|||Also BD Fig.15, p266, Fig.21.||||||18-JAN-07
4727|Corella Formation|42438|5|Briefly described|Fig.1 P276|||||||||
4727|Corella Formation|42556|6|Mentioned|p9|||of Mary Kathleen Group||||||
4727|Corella Formation|42565|4|Described|Table 1 P5, P2|||||||||
4727|Corella Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group.||||||09-FEB-09
4727|Corella Formation|42766|5|Briefly described|p1|||||||||
4727|Corella Formation|42781|4|Described|p427|||see also Fig.1 p426, Fig.3 p428.||||||07-AUG-06
4727|Corella Formation|42818|5|Briefly described|Fig.2 P205|||see also Table 1 p210.||||||18-JAN-07
4727|Corella Formation|42858|4|Described|p671|||||||||
4727|Corella Formation|42859|5|Briefly described|p675|||||||||
4727|Corella Formation|42879|6|Mentioned|p213|||||||||
4727|Corella Formation|43608|6|Mentioned|Fig.11,p11|||||||||
4727|Corella Formation|43614|6|Mentioned|p18|||||||||
4727|Corella Formation|43615|6|Mentioned|p15|||1740-1780 Ma||||||
4727|Corella Formation|43616|6|Mentioned|p2|||Pre-1740 Ma||||||
4727|Corella Formation|43619|6|Mentioned|p43||Proterozoic|||||||
4727|Corella Formation|43638|5|Briefly described|p59|||||||||
4727|Corella Formation|43643|5|Briefly described|p613|||||||||
4727|Corella Formation|43775|6|Mentioned|p26|||||||||
4727|Corella Formation|43928|6|Mentioned|24|||||||||
4727|Corella Formation|44091|14|Not recorded|p10||Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|44195|5|Briefly described|Fig.1,p344|||p345, Table 1. U-Pb ages given.||||||
4727|Corella Formation|44215|14|Not recorded|p353|||Coarse limestone and dolomite.||||||
4727|Corella Formation|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|44271|14|Not recorded|p30|||||||||
4727|Corella Formation|44274|14|Not recorded|p9|||Contemporaneous with Myally Beds.||||||
4727|Corella Formation|44275|14|Not recorded|Map Legend|||||||||
4727|Corella Formation|44276|2|Defined|p6,11,12,14,15,18,25|||Map,Tb.1||||||
4727|Corella Formation|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|44278|2|Defined|Tb.1,p5,6,77,9|||||||||
4727|Corella Formation|44279|2|Defined|p4,5,8,9,Tb.1|||||||||
4727|Corella Formation|44290|14|Not recorded|p438|||||||||
4727|Corella Formation|44521|14|Not recorded|p1,3,6-10,13,15,17-8||Paleoproterozoic|p37-42,44,45,map,Tb.p9||||||07-NOV-08
4727|Corella Formation|44552|14|Not recorded|p14,21|||||||||
4727|Corella Formation|44712|14|Not recorded|p256,257|||||||||
4727|Corella Formation|44713|14|Not recorded|p39,Fig.1||Paleoproterozoic|Host rock for Uranium.||||||07-NOV-08
4727|Corella Formation|44714|14|Not recorded|p46|||||||||
4727|Corella Formation|44751|14|Not recorded|p304|||||||||
4727|Corella Formation|44765|14|Not recorded|p15,16||Paleoproterozoic|||||||07-NOV-08
4727|Corella Formation|44766|14|Not recorded|p24|||||||||
4727|Corella Formation|44788|14|Not recorded|p10,18,29|||||||||
4727|Corella Formation|44806|14|Not recorded|p283-284,290-294|||Petrographic descriptions.||||||
4727|Corella Formation|44847|14|Not recorded|p652|||||||||
4727|Corella Formation|44854|14|Not recorded|p51|||Uranium ore.||||||
4727|Corella Formation|44989|2|Defined|p.80-6,96|||Tb.III, IV. On many pages.||||||
4727|Corella Formation|45136|3|Fully described|p29|||||||||
4727|Corella Formation|45161|4|Described|p24|||||||||
4727|Corella Formation|45166|4|Described|p20|||||||||
4727|Corella Formation|45287|14|Not recorded|p.225-9|||Mineralised. U, Cu, Pb, Zn, Ag, etc. p.230,232.||||||
4727|Corella Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
4727|Corella Formation|46843|6|Mentioned|Fig.2|||||||||
4727|Corella Formation|46872|6|Mentioned|p108|||||||||
4727|Corella Formation|46960|6|Mentioned|p216|||||||||
4727|Corella Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
4727|Corella Formation|46976|6|Mentioned|p97|||||||||
4727|Corella Formation|46995|5|Briefly described|p267|||||||||
4727|Corella Formation|46996|6|Mentioned|p273|||||||||
4727|Corella Formation|47083|5|Briefly described|p10|||Equivalent to Quilalar Formation.||||||
4727|Corella Formation|48894|6|Mentioned|p33|||1384my.||||||
4727|Corella Formation|48906|14|Not recorded|p11,25,27||Precambrian|||||||
4727|Corella Formation|49009|6|Mentioned|p10|||||||||
4727|Corella Formation|49041|6|Mentioned|p3|||||||||
4727|Corella Formation|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Intruded by granites of the Wonga and Burstall Suites, and Mount Philip Breccia.  Uranium occurrences.  Geological Province: Eastern Fold Belt and Kalkadoon-Ewen Provinces.  See also p55, p81.||||||18-JAN-07
4727|Corella Formation|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
4727|Corella Formation|50332|5|Briefly described|p16, p18-19, p50, p75, p77, 84|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Is intruded by Wonga and Burstall Suites.Geological Province: Kalkadoon-Ewen Province. Consists of scapolitic and calcareous rocks and has lower and upper parts dominated by pelites, seperated by a middle sandy unit.||||||07-FEB-11
4727|Corella Formation|50536|5|Briefly described|p1.1, 5.1, 6.2.|||Geological Province: Mount Isa Inlier. Intruded by Wonga Suite and Burstall Suite.||||||18-JAN-07
4727|Corella Formation|50547|5|Briefly described|p1228||Proterozoic|Of the Mary Kathleen Group. In Eastern Fold Belt,  Mount Isa Inlier.||||||18-JAN-07
4727|Corella Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Scapolitic and amphibolitic calc-silicate rocks, mafic and felsic metavolcanics, marble, schist, ironstone.||||||
4727|Corella Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block and Eastern Fold Belt.||||||03-JUN-09
4727|Corella Formation|60665|6|Mentioned|p1146, p1151-1157, p1161, p1163, p1171  |||A close association is noted between albitization and calcite and/or actinolite veining in this unit and equivalents.||Unit in Mary Kathleen Group.||||
4727|Corella Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1750Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
4727|Corella Formation|61736|5|Briefly described|p667 Tb. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1740Ma. Geological province: Mount Isa Inlier (eastern succession). Presented in Table as "Corella Formation".||||||
4727|Corella Formation|61830|5|Briefly described|p178|||Hosts Little Eva Cu-Au deposit on CLONCURRY SF 54-02 map sheet area. Geological Province: Mount Isa Block.||||||
4727|Corella Formation|61922|5|Briefly described|p8, p9 Fig. 3||| Geological Province: Mount Isa Inlier/Eastern Fold Belt. See also p12 Fig. 5, p15-16 Figs. 7 and 8.||||||
4727|Corella Formation|61925|5|Briefly described|p56 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Leichardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||07-NOV-08
4727|Corella Formation|61926|5|Briefly described|p70-71, 72|Paleoproterozoic|Paleoproterozoic|Intensely deformed amphibolite-facies calc-silicate rocks. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
4727|Corella Formation|61927|5|Briefly described|p92 Fig.1|||Geological Province: Mount Isa Inlier.||||||
4727|Corella Formation|61929|5|Briefly described|p127, p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Carbonate rocks. Age: ca1740Ma.||||||07-NOV-08
4727|Corella Formation|61933|5|Briefly described|p175, p177|||Characterised by widespread occurance of breccias.||||||
4727|Corella Formation|61936|5|Briefly described|p190 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: ca1725Ma. Geological Province: Eastern Fold Belt, Mount Isa Inlier. See also p195 Fig. 6. ||||||07-NOV-08
4727|Corella Formation|62047|5|Briefly described|p90 Fig.1 ||||c.1750+/-7 |||||
4727|Corella Formation|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Quilalar Supersequence spanning the interval ~1755-1740Ma (Mary Kathleen zone). Geological Province: Mount Isa Inlier.||||||07-NOV-08
4727|Corella Formation|63023|6|Mentioned|p1034, p1038|Paleoproterozoic|Paleoproterozoic|Age: 1755+/-3Ma. In the Mary Kathleen region of the Eastern Fold Belt.||||||07-NOV-08
4727|Corella Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Thickness >4000 m.|Between c.1840 and 1800 Ma.||||Banded calcareous and pelitic sedimentary rocks, sandstones and volcanics.|
4727|Corella Formation|63866|4|Described|p60-p61|Statherian|Statherian|Leichhardt Superbasin. A flow-banded porphyritic rhyolite within the formation provides an age of 1750 +/- 7 Ma (Page and Sun, 1998). This age is interpeted as either a maximum depositional age or the age of deposition of volcanic rocks. Additional ages include 1740 +/- 20 Ma from a tuffaceous sandstone (Page, OZCHRON), a crystallisation age of 1738 +/- 2 Ma and a metamorphic age of 1520 +/- 2 Ma.||||Overlies the Ballara Quartzite. Overlain by the Deighton Quartzite. Intruded by the Wonga Suite.|Fine-grained sandstone and siltstones grading up into pelitic schists and calcareous limestone, overlain by a regionally continuous quartzite unit.|
4727|Corella Formation|63884|5|Briefly described|p14|||Calc-silicate. Faulted contact with Toole Creek Volcanics.||||||
4727|Corella Formation|64248|5|Briefly described|p32, p33 Fig.1, p36-38, p40-41, p45|Statherian|Statherian|Deformed by Wonga event. Separated from the Doherty Formation|From <1750 +/- 7 Ma to 1738 +/- 2 Ma.|||Overlies Ballara Quartzite and Overhang Jaspilite. Correlates with Quilalar Formation.||11-DEC-17
4727|Corella Formation|64249|5|Briefly described|p83, p84 Fig. 2, p85, p86, p91, p103|Paleoproterozoic|Paleoproterozoic|Age range of deposition: 1762-1742Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
4727|Corella Formation|64250|5|Briefly described|p10-14, p18-19, p21-22, p23 fig 8, p26|||Some parts of this Formation may be much younger than others depending on how contacts with other units are interpreted (page 21). Possibly intruded by Mount Fort Constantine Volcanics. Correlates with Overhang Jaspilite and Chumvale Breccia.|1738 +/- 2 Ma.|Mary Kathleen Group||Overlies Ballara and Mitakoodi Quartzites. Overlain/thrust by Roxmere Quartzite. Lateral equivalent of Doherty Formation. Overlain by Deighton Quartzite and Knapdale Quartzite (conformably).|Calcareous (calc-silicate) metasediments.|
4727|Corella Formation|64251|5|Briefly described|p51 Fig. 1, p52, p55, p64|Paleoproterozoic|Paleoproterozoic|In contact with Soldiers Cap Group. Age: 1750-1742Ma. (Page and Sun 1998). Geological Province: Mount Isa Inlier.||||||22-APR-09
4727|Corella Formation|64253|5|Briefly described|p151, p152, p153, p154 Fig. 3, p154-155|Paleoproterozoic|Paleoproterozoic|Of Mary Kathleen Group. Geological Province: Mount Isa Block. Marbles, calc-silicate rocks, metasiltstones.||||||
4727|Corella Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
4727|Corella Formation|64744|5|Briefly described|p353 Fig.4, p357 Fig.7, p358.|Statherian|Statherian|Mount Isa Basin.|||||Metaquartzite; pelitic and calc-silicate metasediments.|
4727|Corella Formation|65387|6|Mentioned|p60, p82|||Supplied part of the detritus for Quamby Conglomerate.||||Is overlain by Quamby Conglomerate.||
4727|Corella Formation|65396|5|Briefly described|p4, p7, p12, p16-17, p23, p25, p27, p29|Statherian|Statherian|See also p32, p35-36, p43, p78, p82, p84-85, p105, p120, p143, p157, p171, p173, p175-180, p182-185, p187, p190-191, p194-196, p199, p201-202, p213, p217-218, p222, p226, p230, p234-241, p272, p274, p283-284, p292-293, p299-300, p311-312, p318, p321, p390-391, p396, p399, p439, p496. Leichhardt Superbasin. Eastern Succession. Cover Sequence 2. Proximity to this Formation and its contact with the Soldiers Cap Group is considered one of the most important predictors for economic mineralization in the region. Hosts numerous Cu+/- Au occurrences. Also mentioned as Corella+Doherty Formation. May be 20 m.y. older than Doherty Formation. Detrital zircon sources listed. Is correlated with Doherty Formation, Overhang Jaspilite, Chumvale Breccia. Is cut by Mount Fort Constantine Volcanics.|<1750 +/- 7 Ma, 1738 +/- 2 Ma|Mary Kathleen Group||Conformably overlies Ballara and Mitakoodi Quartzites, Overhang Jaspilite, Soldiers Cap Group, Marimo Slate. Unconformably overlain by Knapdale Quartzite, Deighton Quartzite, Quamby Conglomerate.|Calcareous sandstone, slate, schist, marl, calc-silicates and calc-silicate breccias, marbles, pelitic rocks and basaltic volcanics.|
4727|Corella Formation|65505|5|Briefly described|965-68, 974, 976, Fig 1-3,6|Proterozoic|Proterozoic|Intruded by 1740 Ma granites, overlies the Ballara Quartzite. Fine grained sandstone and carbonate. Age: 1776 +/- 3 Ma. Cut by felsic dyke associated with Burstall Granite.||||||
4727|Corella Formation|65755|5|Briefly described|p3, p3 Fig.1|||1750 - 1742 Ma||||||
4727|Corella Formation|66529|5|Briefly described|p61-62 |Statherian|Statherian|Hosts the Mary Kathleen U-REE deposit which is associated with garnet-pyroxene skarn related to Burstall Granite and associated dykes.|~1780-1760 Ma|||Intruded by the Burstall Granite.|Calc-silicate rocks, scapolitic metasediments and slates.|
4727|Corella Formation|66800|5|Briefly described|p933.|||With Doherty Formation, the oldest components of the Eastern Fold Belt, Mount Isa Inlier.|1750-1740 Ma (Page and Sun 1998).|||||
4727|Corella Formation|66913|5|Briefly described|p170 fig 1, p172||||1700-1725 Ma|||Correlated with Staveley Formation.|Carbonate-bearing.|
4727|Corella Formation|67127|5|Briefly described|p94, p96|||Hosts the Mary Kathleen deposits which were interpreted to be deposited during the formation of the Leichhardt Superbasin.|||||Metasedimentary rocks including metamorphosed calcareous pebble conglomerate, ophitic-textured monzonitic intrusion and minor banded calcareous sediments.|
4727|Corella Formation|67323|4|Described|p11, p15-18, p20, 24, p31-32, p39, 107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Post-rift sag phase of the Leichhardt Superbasin. Widespread unit in the Mount Isa Inlier. Metamorphosed and altered during the Isan Orogeny. Associated with very strong magnetic anomalies. Maximum depositional ages by Neumann et al. (2009); younger limit is constrained by age of Wonga (c.1738 Ma) and Burstall (c.1739 Ma) Suites. Previously correlated with Staveley Formation but is older than it. The upper part may consist of Mount Fort Constantine Volcanics. RELATED UNITS (continued): Folded or thrust against Overhang Jaspilite. May be thrust under Bulonga Volcanics. Equivalent to Quilalar Formation.|1776 +/- 3 Ma and 1770 +/- 6 Ma.|||Overlies Ballara Quartzite and Boomarra Metamorphics. Is overlain by Coocerina Formation and unconformably by Milo beds. Is intruded by Wonga Suite and Tommy Creek Microgranite. See COMMENTS for more|Calcareous siltstone, limestone, calcareous scapolitic granofels, quartzite, amphibolite, shale|
4727|Corella Formation|67498|5|Briefly described|p919, 920, 925, 929-931, p932 Fig.11|||Shown as part of 'cover sequence 3'.||||Intruded by the Mount Angelay Granite.|Bedded and brecciated calcsilicates.|07-MAY-12
4727|Corella Formation|67539|5|Briefly described|p7, p10, p13|||Correlative of the Argylla Formation / Ballara Formation? exposed in the Mary Kathleen Belt. Inclusions of the Burstall Granite occur in the Corella Formation belt.||||Overlain by the Mount Albert Group? Correlative of the Argylla Formation / Ballara Formation? Probably overlies Boomarra metamorphics.|Comprises a very narrow western belt of felsic meta-volcanics, quartzofeldspathic gneiss and quartzite.|12-JAN-15
4727|Corella Formation|68020|6|Mentioned|p127|||Hosts Uranium mineralisation.||Includes skarn-hosted  U mineralisation.|||U ore hosted by calcic exoskarn formed by replacement of  calcareous rocks.|
4727|Corella Formation|68021|5|Briefly described|p135 fig 4, p136|Statherian|Statherian|Eastern Succession.|1755-1740 Ma|||Overlies Ballara Quartzite, intruded by Wonga Granite?, Burstall Granite.  Lateral equivalent to Quilalar Supersequence.|Platform carbonates.|
4727|Corella Formation|68146|6|Mentioned|p127|Proterozoic|Proterozoic||~1760-1740 Ma.|||||
4727|Corella Formation|68542|5|Briefly described|p13, p14, p16 fig 4, p20 fig 6, p21|||||Mary Kathleen Group||Overlies Ballara Quartzite|Calcareous sediments, wollastonite and vesuvianite marble, quartztite, conglomerate, garnetised sediment and skarn.|
4727|Corella Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Ballara Quartzite under the symbol, -Pk.||||||
4727|Corella Formation|68575|5|Briefly described|p2, p6-7, p61, p63, p68, p70, p75, p126|||Maximum age from underlying unit. Is intruded by 1740 Ma granites.|c.1755-1740 Ma.|||Overlies the Ballara Quartzite.||
4727|Corella Formation|68576|5|Briefly described|Q_2: p13-14, p16, p20-21|||Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier. Hosts the Mary Kathleen uranium deposit.||Mary Kathleen Group.||Overlies Ballara Quartzite. Is intruded by Burstall Granite.|Calc-silicate and calcareous granofels, wollastonite, grossular and vesuvianite marbles; scapolite crystals abundant.|21-OCT-19
4727|Corella Formation|68732|5|Briefly described|p162, p165-166, p169, p171|Statherian|Statherian|Deposited during the highstand of the Quilalar Supersequence. Metamorphic grade varies from upper greenschist to amphibolite facies. Maximum sedimentary depositional age.|1750 +/- 7 Ma||||Includes carbonate-rich distal tempestites in lowermost part.|30-NOV-17
4727|Corella Formation|69056|4|Described|p2-6, p9-13, p18, p22-23, p28, p36-37|Statherian|Statherian|See also p53-56, Time-Space plot sheet, Reference images sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Ballara Quartzite. Widespread unit. Some rocks previously mapped as part of this unit are now assigned to the Staveley Formation. Shallow (locally evaporitic) carbonate shelf environment of deposition. Source of stratiform and stratabound bornite-chalcopyrite protore which was subsequently weathered and mapped as Mount Roseby Schist Cu mineralisation. Modelling values listed. Maximum depositional age of 1770 +/- 5 Ma. Is intruded by Dipvale Granodiorite; Tommy Creek Microgranite; Playboy, Burstall, Levian Granites. Equivalent of Quilalar Formation of the Mount Isa Western Succession.|~1752 Ma - 1740 Ma.|||Overlies Ballara Quartzite, Overhang Jaspilite, Bulonga Volcanics. Overlain by Mount Fort Constantine Volcanics.|Calcareous siltstone, limestone, calcareous scapolitic granofels, quartzite, amphibolite, shale and local metabasalt.|
4727|Corella Formation|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Eastern Fold Belt.||Mary Kathleen Group||Overlies Ballara Quartzite||09-FEB-18
4727|Corella Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Ovelies Overhang Jaspilite. Is intruded by Wonga Granite.||25-JAN-19
4727|Corella Formation|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia (subsurface)|
4727|Corella Formation|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia|
4727|Corella Formation|69591|4|Described|p29, p33-35, p40, p45, p49,p51,p57,p105|Paleoproterozoic|Paleoproterozoic|Mary Kathleen and Mitakoodi Domains, Leichhardt Superbasin, Mount Isa Province. Part of the Quilalar Supersequence. A widespread platform succession. Some rocks of this unit are assigned to the Mount Roseby Schist. Folding during the middle-Isan Orogeny becomes increasingly disharmonic. Contains widespread breccias possibly resulting from salt-tectonics mobilising carbonate successions.|1770 +/- 6 Ma (MDA: Neumann et al., 2009).|Mary Kathleen Group.|Lime Creek Metabasalt Member.|Overlies Ballara Quartzite and Boomarra Metamorphics. Equivalent to the Quilalar Formation. ?Intruded by Augustus Igneous Complex.|Carbonate-rich. Calcareous sandstone and siltstone and impure limestone, with some quartzose sandstone; metamorphosed and altered to calc-silicate rocks; local mafic lavas.|
4727|Corella Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Two minor facies are mapped separately.||Mary Kathleen Group.||Overlies Ballara Quartzite.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels (commonly scapolitic) and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Two minor facies are mapped separately.||Mary Kathleen Group.||Overlies Ballara Quartzite.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels (commonly scapolitic) and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Two sub-units are mapped separately: black slate and graphitic schist (subsurface and schematic diagram); and breccia of metasandstone, siltstone and locally limestone clasts in a calcareous sandy matrix grading into calc-silicate breccia.||Mary Kathleen Group.|||Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Two sub-units are mapped separately: black slate and graphitic schist (subsurface and schematic diagram); and breccia of metasandstone, siltstone and locally limestone clasts in a calcareous sandy matrix grading into calc-silicate breccia.||Mary Kathleen Group.|||Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|No fewer than 24 un-named sub-units are mapped separately.||Mary Kathleen Group.|Lime Creek Metabasalt Member.||Undivided: Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia (subsurface and Schematic Diagram).|
4727|Corella Formation|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|No fewer than 24 un-named sub-units are mapped separately.||Mary Kathleen Group.|Lime Creek Metabasalt Member.||Undivided: Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia (subsurface and Schematic Diagram).|
4727|Corella Formation|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Eleven facies are mapped separately.||Mary Kathleen Group.|Lime Creek Metabasalt Member.|Overlies Ballara Quartzite.|Calcareous siltstone, sandstone, limestone, shale, granofels, quartzite, amphibolite, metabasalt, breccia, marble, slate, schist.|
4727|Corella Formation|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes eight unnamed members: calcareous siltstone, sst, minor lst; breccia of metasandstone, siltstone; contact aureole rocks; laminated calc silicate granofels, mica schist; laminated calcareous siltstone, lst, metalimestone & marble; calcareous sst, slate, schist, quartzite; metasilstone, sst, lst, shale.||Mary Kathleen Group|Includes Lime Creek Metabasalt Member and eight unnamed members.|||
4727|Corella Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1660+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite.|
4727|Corella Formation|71799|4|Described|p150 fig 2, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca. 1750 Ma||Includes the Lime Creek Metabasalt Member.|Overlies the Overhang Jaspilite.|Dolomite, calc-silicate rocks.|03-OCT-18
4727|Corella Formation|72297|5|Briefly described|p710, p721|||Hosted the Tick Hill gold deposit in shear-hosted hydrothermal Au-quartz veins. Mined during 1992-1995.|||||Includes calc-silicate granofels containing cordierite with chlorite.|
4727|Corella Formation|72596|5|Briefly described|p1-27, p29, p34, p40, p46, p56, p59, p63|Statherian|Statherian|3 samples dated.  Geochronologic constraint includes magmatic emplacement ages (metarhyolites: 1739 +/- 5 Ma and 1740 +/- 5 Ma ) and a maximum depositional age (micaceous feldspathic quartzite: 1752 +/- 2 Ma ) using SHRIMP U-Pb dating. Metarhyolites are coeval with the Burstall Granite. Depositional age inferred to be in the 1770-1740 Ma range. One metarhyolite also yielded a metamorphic age of 1515 +/- 13 Ma from zircon rims. Authors propose there was only a short time interval between the cessation of deposition of the Corella Formation and the emplacement of at least part of the Mount Erle Igneous Complex. Metarhyolite sample BB590/2808846 was a recollection of a previous sample (Sample ID 95208069), which had yielded an anomalously young age from only five discordant analyses. Intruded by the Mount Erle Igneous Complex, Revenue Granite and Burstall Granite; however, metarhyolites of the Corella Formation are coeval with the Burstall Granite.|1739 +/- 5 Ma, 1740 +/- 5 Ma, 1752 +/- 2 Ma|||May include or be overlain by the Mount Fort Constantine Volcanics. Partly underlain conformably by Ballara Quartzite. Encloses the Mount Philp Breccia. See comments for cross-cutting relations.|Calcareous metasediments. Amphibolite grade in the Duchess region. Includes subunits dominated by foliated and recrystallised metarhyolite (incl. possible ignimbrites) and metadacite.|
4727|Corella Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|14 sub-units described with distinctive lithologies including a quartzite or meta-arenite marker bed, feldspathic granofels, porphyry, calc-silicate granofels, metabasalt, quartzite, para-amphibolite, banded ironstone, marble, granitic gneiss, breccia, black slate with phyllite and phyllonite.||Mary Kathleen Group||Overlies Ballara Quartzite.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|14 sub-units described with distinctive lithologies including a quartzite or meta-arenite marker bed, feldspathic granofels, porphyry, calc-silicate granofels, metabasalt, quartzite, para-amphibolite, banded ironstone, marble, granitic gneiss, breccia, black slate with phyllite and phyllonite.||Mary Kathleen Group||Overlies Ballara Quartzite.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
4727|Corella Formation|72799|6|Mentioned|p: 1, 4, 7, 26-27, 34-36, 46, 48, 52-53|||Mary Kathleen Domain. Hosts copper mineralisation possibly associated with the Overlander Granite.||||Intruded by Mount Godkin Granite, Myubee Igneous Complex, Overlander Granite, and Burstall Granite.|Includes metasedimentary rocks.|
4727|Corella Formation|72889|5|Briefly described|p6 Fig.i, p30-31.|Statherian|Statherian||c. 1750-1745 Ma.|||May correlate with Staveley Formation.|Calc-silicate dominated.|
4727|Corella Formation|72912|5|Briefly described|p12.|Statherian|Statherian|Of Leichhardt Superbasin? Regarded as a correlative unit to the Quilalar Formation.||Of Quilalar Supersequence?||||
4727|Corella Formation|73137|4|Described|p21-28, p55- 60 plus see coments.|Statherian|Statherian|Most extensive unit in the Mary Kathleen Domain; main unit in Mary Kathleen Group. Previous crystallisation ages from metadacite-metarhyolite intervals of 1740 Ma. Previous maximum depositional age of 1752 +/- 2 Ma from a feldspathic quartzite. A felsic metavolcanic from the northern tip of the Boomarra Horst yielded a crystallisation age of 1737 +/- 5 Ma, which supports inferences of widespread volcanism during this time. Metavolcanic rocks from drill holes were also dated and include a magmatic crystallisation age of 1737 +/- 6 Ma.  Various dates on zircon rims yielded metamorphic ages such as 1524 +/- 13 Ma and 1533 +/- 24 Ma. An area currently mapped as part of the Corella Formation in the southern part of the Mary Kathleen Domain is either intruded by ~1775-1780 Ma and significantly older (basement) granitic rocks [thus, it isn't part of the Corella Formation], or is tectonically interleaved with these rocks. Quartzite mapped as unnamed subunits of the formation were dated herein to investigate these relationships [interpretations were somewhat inconclusive; see article for details]. [See article for field description, petrographic description and detailed geochronology]. p: 1-2, 5-7, 9, 13, 16, 35, 38-40, 43, 51, 53, 68, 72, 95, 99.|~1740 Ma|Mary Kathleen Group||Conformably underlain by Ballara Quartzite. Coeval with Mount Fort Constantine Volcanics. Intruded by Mount Maggie Granite.|Includes felsic metavolcanic rocks and quartzite.|11-OCT-22
4727|Corella Formation|73413|5|Briefly described|p1-6, p8, p20-21, p23-24, App.1|Statherian|Statherian|Mount Isa Inlier. Covers large parts of the Mary Kathleen Domain. Included in Cover Sequence 2 of Foster and Austin (2008). Type locality is northwest of Mary Kathleen [historic township]. Interpreted as metamorphosed, shallow water, mixed siliciclastic-carbonate platform sequences intercalated with evaporite deposits. Previously thought to constitute dominant lithology in the Tick Hill area; however, new ages herein suggest otherwise. [Article includes a summary of previous geochonologic constraint for this unit].|1730-1760 Ma|||Intruded by Saint Mungo Granite, Tick Hill Complex, and Mount Erle Igneous Complex.|Scapolite-bearing calc-silicate and amphibolite, with lesser marble, metapelite, quartzite, and felsic metavolcanics.|
4727|Corella Formation|73481|5|Briefly described|p443-444, p449|||Mount Isa Inlier, Mary Kathleen Domain.|||||Calcsilicate rocks and meta-dolerite with calcite pods.|
4727|Corella Formation|73525|5|Briefly described|p2 Fig.1, p4, p19 Fig.13, p20|Statherian|Statherian|Kalkadoon-Leichhardt, Mary Kathleen, Mitakoodi-Tommy Creek Domains.|1776+/-3 Ma, 1738+/-2 Ma maximum depositional ages||||Carbonates, includes clastics, felsic extrusives, mafic extrusives, jaspilite, chert, siliciclastics.|
4727|Corella Formation|73529|4|Described|p4, p6 Fig.3, p7-11, p14|Statherian|Statherian|Shallow shelf carbonate platform environment.|1770+/-3 Ma, 1752+/-2 Ma detrital zircon|Mary Kathleen Group||Intruded by Revenue Granite, Overlander Granite, Myubee Igneous Complex, Myubee Granite|Mainly comprises calc-silicates, including metamorphosed calcareous siltstone, limestone, quartzite, basalt and shale protoliths.|09-MAR-23
4727|Corella Formation|73553|4|Described|p1-3, p5, p7-8, p10, p14, p18, p23, p27,|Statherian|Statherian|Most widespread unit in Mary Kathleen Domain. Range of maximum depositional ages provided, 1776+/-3 to 1740 +/-20 Ma. Metamorphic ages of 1525+/-30 to 1515+/-13 Ma. Interpreted as a shallow-water, near-shore, carbonate-shelf environment. Intruded by granitoids of the ~1740-1730 Ma Wonga Igneous Subprovince, and the ~1740-1720 Ma Burstall Igneous Subprovince. Contains numerous mafic intrusives. Encloses Mount Philp Breccia. Rocks mapped as Corella Formation enclosing The Monument Syenite are inferred to be older than ~1780 Ma, unlikely to be part of the same formation as rocks mapped further north in the same unit. Lenses of 'metarhyolite'  are delineated as subunit 'PLkc/a'. Also intruded by the Overlander, Mount Godkin, Revenue, Saint Mungo, Hillside Bore, and Burstall granites, Lunch Creek Gabbro, Mount Erle Igneous Complex, Myubee Igneous Complex, Mavis Granodiorite, Lakeview Dolerite. See also p29, p37, p47, p52, p54-55, p63, p74, p83, p95-96, p98, p103, p105, p108, p112-113, p117-120, p126-128, p132, p135, p137-139, p144, p149, p151, p154, p163, p169, p178, p180, p185, p187, p192, p199-203, p205, p211-212, p214-215, p221-225, p228, p230, p252-253, p257-258, p267.|1740+/-5 Ma U-Pb zircon SHRIMP, 1737+/-6 Ma|Mary Kathleen Group||Overlies Boomarra Metamorphics, Ballara Quartzite, unconformably overlies Argylla Formation, intruded by Tick Hill Complex, The Monument Syenite, Scheelite Granite, Dipvale Granodiorite|Mainly calc-silicate rocks, metamorphosed to middle-upper amphibolite grade and Na-(Ca)- metasomatised over wide areas. Metasedimentary rocks and felsic volcanics.|03-FEB-23
4730|Corinda Formation|29720|6|Mentioned|p79|||||||||
4730|Corinda Formation|31132|6|Mentioned|p150|||Refers Houston (1965)||||||
4730|Corinda Formation|31247|6|Mentioned|p160|||Fauna & flora. Refers Harris (1965)||||||
4730|Corinda Formation|31273|6|Mentioned|p13|||||||||
4730|Corinda Formation|33368|6|Mentioned|p49|||Correlation.||||||
4730|Corinda Formation|36237|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4730|Corinda Formation|36779|6|Mentioned|p8|||||||||
4730|Corinda Formation|38074|5|Briefly described|Table 1|||||||||
4730|Corinda Formation|38373|6|Mentioned|p624|||||||||
4730|Corinda Formation|38441|6|Mentioned|Map legend|Eocene|Eocene|||||||
4730|Corinda Formation|39445|5|Briefly described|p153|||See also Table 14||||||
4730|Corinda Formation|40623|5|Briefly described|p8|||||||||
4730|Corinda Formation|41906|3|Fully described|Table 4 P33|||||||||
4730|Corinda Formation|42417|5|Briefly described|p229|||Age Early Tertiary (Paleocene to Oligocene)||||||
4730|Corinda Formation|44030|14|Not recorded|p118,131|||Tertiary equivalent.||||||
4730|Corinda Formation|44677|14|Not recorded|p1|||||||||
4730|Corinda Formation|44687|2|Defined|p225-226||Oligocene|[Supersedes Corinda Beds]. Includes upper Eight Mile Plains Basalt Member and lower Archerfield Basalt Member. Age: ?Oligocene. Named from Corinda, suburb of Brisbane.||||Equivalent to Silkstone Formation of Staines (1960).|Basalt, minor pyroclastics, pyritic mudstone (calcareous in part), pyritic shale, minor sandstone, intraformational conglomerate and limestone|21-MAR-13
4730|Corinda Formation|44703|14|Not recorded|Map||Tertiary|||||||
4730|Corinda Formation|44704|14|Not recorded|p1|||||||||
4730|Corinda Formation|44708|14|Not recorded|p3,23,Sh.1-4,section||Tertiary|Unit of Oxley Group.||||||
4730|Corinda Formation|61155|5|Briefly described|p19|||Of the Oxley Group. Overlies the Darra Formation; underlies the Sunnybank Formation. Age: 55-46Ma.Thickness: ~278m.  In the Brisbane region.||||||03-MAR-10
4730|Corinda Formation|69599|4|Described|p586, p594-595, p645|Eocene|Paleocene|Houston (1965). Archerfield Basin, Brisbane area. Fossils include leaves, bivalves, reptiles and fishes. Capped by laterite and silcrete.|c.58 Ma to c.55 Ma.|Oxley Group.|Archerfield Basalt Member, Eight Mile Plains Basalt Member.|Disconformably overlies Darra Formation. Is overlain disconformably by Sunnybank Formation. Correlated with Silkstone Formation.|Basal basalt with intercalated mudstone (~60m), overlain by pyritic mudstone and shale, sandstone and minor limestone and intraformational conglomerate (up to 62m), overlain by basalt (43m).|
4733|Corkscrew Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Kungaree Volcanic Subgroup. Age: 323 Ma. Thickness: Up to 760m. Geological Province: Georgetown Region.||||||28-MAY-15
4733|Corkscrew Rhyolite|23430|5|Briefly described|Plate 14.7b|||||||||
4733|Corkscrew Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V18. I & A-Type.||||||
4733|Corkscrew Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4733|Corkscrew Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Kungaree Volcanic Subgroup.||||||
4733|Corkscrew Rhyolite|43740|4|Described|p9|||||||||
4733|Corkscrew Rhyolite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Kungaree Volcanic Subgroup (Newcastle Range Volcanic Group). Contains the Thornborough Andesite Member.||||||28-MAY-15
4733|Corkscrew Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Kungaree Volcanic Subgroup.|Includes Thornborough Andesite Member.||Brown to pink sparsely porphyritic rhyolite with very few quartz phenocrysts; probably includes intrusive equivalents.|
4733|Corkscrew Rhyolite|68576|6|Mentioned|Q_11: p22 Fig.20|Carboniferous|Carboniferous|||||||
4733|Corkscrew Rhyolite|70207|5|Briefly described|p82, p85|Permian|Permian|Northern part of the Newcastle Range.||Kungaree Volcanic Subgroup.|||A-type.|
4749|Corrie Member|22954|4|Described|Fig1p6,17,23-4|Warendan|Warendan|||||||
4749|Corrie Member|37572|4|Described|p162|||||||||
4749|Corrie Member|40136|5|Briefly described|p22|||||||||
4749|Corrie Member|40810|5|Briefly described|p14|||||||||
4749|Corrie Member|40852|6|Mentioned|Fig.3.7|||||||||
4749|Corrie Member|42354|6|Mentioned|p11|||Of Ninmaroo Formation.||||||07-AUG-06
4749|Corrie Member|46897|6|Mentioned|Fig.2|||||||||
4749|Corrie Member|46958|6|Mentioned|p195|||||||||
4749|Corrie Member|50244|6|Mentioned|p89 Fig. 1, p100 Fig. 7|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||22-APR-09
4749|Corrie Member|64068|4|Described|p74, 75|Early Ordovician|Early Ordovician|110 m thick in type section. Correlated with Kelly Creek Formation. [Said on p74 to be overlain by Jiggamore Member, but this makes no sense - probably a typo?]||Of Ninmaroo Formation.||Conformably overlies Mort Member. Is conformably overlain by Datson Member.|Bioclast (echinoderm), ooid, peloid and peloid-bioclast-intraclast grainstone, dolomitic sandstone, chert.|21-MAR-16
4749|Corrie Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin||Cockroach Group|||Limestone (pelmatozoan, peloid, clast and ooid grainstone), dolomitic sandstone, calcareous siltstone.|
4771|Cottenham Sandstone Member|23037|5|Briefly described|p66,9||Permian|Of Barfield Formation.||||||27-OCT-05
4771|Cottenham Sandstone Member|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pbrc].  Lithic and feldspathic sandstone, siltstone, mudstone, and minor conglomerate.||||||
4771|Cottenham Sandstone Member|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4771|Cottenham Sandstone Member|41666|6|Mentioned|p3|||||||||
4771|Cottenham Sandstone Member|42249|6|Mentioned|p22|||||||||
4771|Cottenham Sandstone Member|44640|14|Not recorded|p32|||Middle member of Barfield Formation.||||||
4771|Cottenham Sandstone Member|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Barfield Formation (Back Creek Group). Lithic and feldspathic sandstone, siltstone, mudstone and minor conglomerate.||||||18-JUN-09
4771|Cottenham Sandstone Member|65388|4|Described|p163 Fig. 63, p168, 169, 172|||Of Barfield Formation,  Bowen Basin. Redefined by Dear et al (1971) after Derrington & others (1959) formation. Exposed east of Banana. Type section along the Dawson Highway. Underlain by Four Mile Mudstone Member. Overlain by Station Mudstone Member. Well-bedded lithic sandstone and mudstone. Resembles Boomer Formation.||||||
4771|Cottenham Sandstone Member|68679|5|Briefly described|p380|||||Barfield Formation.||May correlate with the Boomer Formation.||
4771|Cottenham Sandstone Member|73570|5|Briefly described|p914, p915 Fig.4, p916, p919 Fig.6|Late Permian|Late Permian|Bowen Basin.||Barfield Formation||||
4838|Craigie Tonalite|23032|6|Mentioned|p39||Early Devonian|K/Ar Age: 406+/-3 Ma.||||||
4838|Craigie Tonalite|23422|5|Briefly described|p178, p215 Table 6.9|Early Devonian|Late Silurian|Of Craigie Supersuite.||||||
4838|Craigie Tonalite|42692|5|Briefly described|map legend|Early Devonian|Silurian|Variation on Craigie Granodiorite.||||||
4838|Craigie Tonalite|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
4838|Craigie Tonalite|42933|6|Mentioned|p227|||||||||
4838|Craigie Tonalite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
4838|Craigie Tonalite|43480|1|Redefined|7,25|Early Devonian|Late Silurian|K-Ar Hornblende age: 406+/-3Ma||||||21-JUN-13
4838|Craigie Tonalite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey, hornblende-biotite tonalite.|
4838|Craigie Tonalite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey, hornblende-biotite tonalite.|
4838|Craigie Tonalite|69592|5|Briefly described|p281, p285, p288 Fig.4.84|||Reedy Springs Batholith, Charters Towers Province. Geochemistry plots.|406 +/- 3 Ma (K-Ar hornblende).|Craigie Supersuite.|||Foliated hornblende-biotite and biotite-hornblende tonalite; accessory epidote, titanite, allanite, zircon. I-type.|
4859|Cravens Peak beds|8187|5|Briefly described|Map legend|Devonian|Devonian|Sandstone, conglomerate. Overlie Ethabuka Sandstone and Mithaka Formation.||||||05-SEP-14
4859|Cravens Peak beds|8217|5|Briefly described|Map Legend|Devonian|Devonian|Sandstone, conglomerate.||||||
4859|Cravens Peak beds|12951|5|Briefly described|p142, p143 fig 4, p145 fig 6, p152|Devonian|Devonian|Georgina Basin. Fan-delta sediments.||||Correlated with Dulcie Sandstone.||
4859|Cravens Peak beds|23858|5|Briefly described|p917|Middle Devonian|Middle Devonian|Geological Province: Georgina Basin.||||||
4859|Cravens Peak beds|24442|5|Briefly described|p49|Middle Devonian|Early Devonian|On TOBERMORY sheet||||||
4859|Cravens Peak beds|38593|6|Mentioned|p90|||Georgina Basin||||||
4859|Cravens Peak beds|38832|6|Mentioned|p157|||||||||
4859|Cravens Peak beds|42643|6|Mentioned|p32|||||||||
4859|Cravens Peak beds|45148|6|Mentioned|p20|||||||||
4859|Cravens Peak beds|45155|6|Mentioned|Fig.8|||||||||
4859|Cravens Peak beds|49027|4|Described|p20|||||||||
4859|Cravens Peak beds|60122|4|Described|p34|Devonian|Devonian|Originally included rocks now mapped as Ethabuka Sst, Cravens Peak beds proper and Poodyea Formation. Unconformably overlies Ethabuka Sandstone and Mithaka Formation. Max. thickness: 280m. Geological Province: Georgina Basin. See also p4-5, p10 Tb. 1||||||08-AUG-06
4859|Cravens Peak beds|60590|5|Briefly described|Map legend|Devonian|Devonian|Calcareous sandstone and siltstone, limestone, minor conglomerate; grades upward into quartz sandstone and conglomerate.||||||
4859|Cravens Peak beds|61404|5|Briefly described|Map legend|Devonian|Devonian|Calcareous sandstone and siltstone, limestone, minor conglomerate; grades upwards into quartz sandstone and conglomerate. Geological Province: southern Georgina Basin.||||||11-FEB-09
4859|Cravens Peak beds|62983|5|Briefly described|p11|Devonian|Devonian|Synorogenic sedimentation. Geological Province: Georgina Basin.||||||
4859|Cravens Peak beds|63450|5|Briefly described|p78 Fig. 5, p83|Middle Devonian|Early Devonian|Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
4859|Cravens Peak beds|64068|4|Described|p78-79, p77, p19, p ix|Eifelian|Pragian|Ungrouped. Formerly included in what are now Ethabuka Sandstone and Poodyea Formation (see Draper 1980). Diverse fauna, particularly fish. Thickness over 280 m. Correlations: Dulcie Sandstone, Mereenie Sandstone or Parke Siltstone.||||Unconformably overlies Ethabuka or Carlo Sandstones or Mithaka Formation.|Calcareous siltstone and sandstone, limestone; minor conglomerate; overlain by sandstone and conglomerate.|05-APR-12
4859|Cravens Peak beds|64778|6|Mentioned|p13|Devonian|Devonian|Toko Syncline, Southern Georgina Basin.||||||
4859|Cravens Peak beds|64812|5|Briefly described|p237 Fig. 2|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||07-FEB-11
4859|Cravens Peak beds|64813|5|Briefly described|p256 Fig. 3|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||11-FEB-09
4859|Cravens Peak beds|65237|5|Briefly described|p4 Fig. 7, p10|||Geological province: southern Georgina Basin. Also written as Craven Creek Beds.||||||07-FEB-11
4859|Cravens Peak beds|65489|5|Briefly described|p126|Middle Devonian|Early Devonian|See also Cravens Peak Beds (p125). Deposition of these sediments in the Toko Syncline to Dulcie Syncline was as a response to the Pertnjara-Brewer Movement. Thrusted and folded during Alice Springs Orogeny.|||||Fluvial and marginal marine siliciclastics.|
4859|Cravens Peak beds|66499|6|Mentioned|p61 Fig.5|||Georgina Basin. [Misspelt as Cravens Peak Beds in text]||||||
4859|Cravens Peak beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Devonian|Early Devonian|Georgina Basin. Age: Ordovician?|||||Conglomerate, sandstone, minor shale; limestone and calcareous siltstone at base.|
4859|Cravens Peak beds|67870|6|Mentioned|p43|Middle Devonian|Early Devonian|Georgina Basin.||||||
4859|Cravens Peak beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|||||||
4859|Cravens Peak beds|69443|4|Described|p28:5, 7, 27, 29-30, 32-33|Middle Devonian|Early Devonian|Reynolds in Smith (1965). Toko Syncline, Southern Georgina Basin. Synorogenic (Pertnjara-Brewer events of the Alice Springs Orogeny) foreland deposition of clastic sediments. Well-exposed as strike ridges or steep cuestas along the Toomba Range; elsewhere generally poorly exposed as low rubble-covered rises or dip slopes. Over 280m thick. Fossil assemblage contains ostracodes, fish, a plant and stromatolites. Pragian to early Eifelian age. Appears alliteratively, albeit incorrectly, as Craven Creek Beds in Figs.28.3 and 28.4.||||Unconformably overlies Carlo Sandstone and Mithaka Formation (Toko Group) or Ethabuka Sandstone. Correlative of Dulcie Sandstone.|A lower interval of calcareous siltstone, calcareous sandstone, limestone and minor conglomerate; an upper interval of cross-bedded, fine- to medium-grained quartz sandstone with clay pellets, and conglomerate.|12-JUL-16
4859|Cravens Peak beds|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
4859|Cravens Peak beds|69591|5|Briefly described|p94, p112|Devonian|Devonian|Toko Syncline. Occurs along the Toomba Range SW of Boulia. Deposition was initiated by the Alice Springs Orogeny. Originally included rocks now mapped as Ethabuka Sandstone and Poodyea Formation. Contains an extensively-studied, Emsian-Eifelian fossil fish assemblage.|||||Calcareous sandstone and siltstone, limestone, minor conglomerate grading upward into coarse sandstone and conglomerate.|
4859|Cravens Peak beds|69673|4|Described|p111, p118, p119 fig 94|Devonian|Devonian|Informal name. At least 280m thick. ||||Correlated with Dulcie Sandstone|Calcareous siltstone, calcareous sandstone, limestone and minor conglomerate, fine to medium grained quartz sandstone with clay pellets and conglomerate.|
4885|Cressbrook Creek Group|23440|6|Mentioned|p146|||||||||
4885|Cressbrook Creek Group|23799|3|Fully described|p30, p25|Permian|Permian|Formerly Cressbrook Creek "Series" (Swindon 1971), comprising Pinecliff Fm., Hampton Rd. Rhyolite, Biarraville and Box Gully Fms. and Buaraba Mudstone as defined by Cranfield et al(1976). Overlain unconformably by Woogaroo Subgroup. Max. thick: ~1500m.||||||
4885|Cressbrook Creek Group|23800|5|Briefly described|Map legend|Permian|Permian|||||||
4885|Cressbrook Creek Group|24560|5|Briefly described|Map legend|Permian|Permian|||||||
4885|Cressbrook Creek Group|30303|6|Mentioned|p322|||Intruded by Eskdale Granodiorite.||||||09-APR-08
4885|Cressbrook Creek Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
4885|Cressbrook Creek Group|31811|6|Mentioned|Fig. 1|||||||||
4885|Cressbrook Creek Group|32912|5|Briefly described|p157|||Refers Campbell (1952)||||||
4885|Cressbrook Creek Group|33381|4|Described|p108|||Perm. See also pp109 and 111. Constituent formations.||||||09-APR-08
4885|Cressbrook Creek Group|37252|6|Mentioned|Map legend|Permian|Permian|||||||
4885|Cressbrook Creek Group|38391|6|Mentioned|p6|||||||||
4885|Cressbrook Creek Group|39252|5|Briefly described|p22|||See also Fig.13.||||||09-APR-08
4885|Cressbrook Creek Group|39445|5|Briefly described|p106|||See also Table 8.||||||09-APR-08
4885|Cressbrook Creek Group|40623|5|Briefly described|p78|||||||||
4885|Cressbrook Creek Group|41591|5|Briefly described|p17|||||||||
4885|Cressbrook Creek Group|41917|6|Mentioned|Fig.3 P528|||||||||
4885|Cressbrook Creek Group|42525|5|Briefly described|Map legend|Early Permian?|Early Permian?|Includes Pinecliffe, Biarraville, Box Gully Formations, and Hampton Road Rhyolite, and Buaraba Mudstone.||||||15-JUL-04
4885|Cressbrook Creek Group|43001|6|Mentioned|Fig.3,p120|||||||||
4885|Cressbrook Creek Group|43002|5|Briefly described|Fig.2,p135|||||||||
4885|Cressbrook Creek Group|43017|6|Mentioned|p378|||||||||
4885|Cressbrook Creek Group|43092|5|Briefly described|Fig.1|||||||||
4885|Cressbrook Creek Group|43993|14|Not recorded|p94 (on map p.96)||Permian|Name attributed to Campbell K.S.W.,1952: The geology of the Cressbrook-Buaraba area. Marine Permain.||||||
4885|Cressbrook Creek Group|60993|5|Briefly described|p17|Permian|Permian|Unconformably overlain by Marburg Subgroup units. ||||||
4885|Cressbrook Creek Group|61002|5|Briefly described|p198 Fig 2|||Geological Province: basement beneath Esk Trough and Clarence-Moreton Basin. ||||||
4885|Cressbrook Creek Group|61781|6|Mentioned|p267|Permian|Permian|||||||
4885|Cressbrook Creek Group|61782|5|Briefly described|p275, p277, p278, p280|Permian|Permian|Includes; Biarraville Formation. Marine sediments and felsic volcanics, contains carbonates. Geol Prov: Esk Trough.||||||
4885|Cressbrook Creek Group|63821|5|Briefly described|p19|Middle Permian|Middle Permian|Geological Province: Esk Trough.||||||07-FEB-11
4885|Cressbrook Creek Group|64197|6|Mentioned|p630 Fig.7|Permian|Permian|Moreton Basin/Esk Trough.||||||
4885|Cressbrook Creek Group|67402|6|Mentioned|p205, p209 |||Approximately 100m thick.||||Overlain by the Bryden Formation.||
4885|Cressbrook Creek Group|68553|6|Mentioned|Map legend|Permian|Permian|||||||
4885|Cressbrook Creek Group|68679|5|Briefly described|p321, p323-324, p384-387, p389, p470|Guadalupian|Guadalupian|Cressbrook Basin, northern New England Orogen; previously included in the Esk Basin. Cover basin sediments. Shallow-marine unstable shelf or slope environment.|||Biarraville, Box Gully, Pinecliff Formations; Buaraba Mudstone; Hampton Road Rhyolite.|Is faulted against Sugarloaf Metamorphics. Is faulted against and unconformably overlain by Toogoolawah Group. Correlative with Northbrook beds.||
4893|Cribb Conglomerate|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Kholo Subgroup||||
4893|Cribb Conglomerate|30302|6|Mentioned|p415|||Refers to Allen(1959)||||||
4893|Cribb Conglomerate|30465|6|Mentioned|p3|||||||||
4893|Cribb Conglomerate|32180|5|Briefly described|p6|||||||||
4893|Cribb Conglomerate|33381|4|Described|p109|||Triassic. See also PP109 & 117. Kholo Subgroup||||||
4893|Cribb Conglomerate|36779|6|Mentioned|p7|||||||||
4893|Cribb Conglomerate|37111|5|Briefly described|p292|||||||||
4893|Cribb Conglomerate|38074|5|Briefly described|Table 1|||||||||
4893|Cribb Conglomerate|38076|6|Mentioned|Table 3|||||||||
4893|Cribb Conglomerate|38307|4|Described|p520|||||||||
4893|Cribb Conglomerate|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
4893|Cribb Conglomerate|39445|5|Briefly described|Table 9 p121|Late Triassic||Of Kholo Subgroup, Ipswich Coal Measures.||||||28-SEP-05
4893|Cribb Conglomerate|39943|6|Mentioned|Table 12A|||||||||
4893|Cribb Conglomerate|40623|6|Mentioned|Table 2|||||||||
4893|Cribb Conglomerate|41906|3|Fully described|Table 2 P18|||||||||
4893|Cribb Conglomerate|42336|5|Briefly described|Table 1 P5|||||||||
4893|Cribb Conglomerate|43922|14|Not recorded|p324,325|||Formation of Kholo Subgroup of Ipswich Coal Measures.||||||
4893|Cribb Conglomerate|44026|14|Not recorded|p123||Triassic|Equivalent of Esk Beds in Ipswich District.||||||
4893|Cribb Conglomerate|44510|2|Defined|p252,254,Fig.35|||Overlies unconformably on Hector Tuff.||||||
4893|Cribb Conglomerate|44542|2|Defined|p34,35|||=White Conglomerate. Underlies Tivoli Formation.||||||
4893|Cribb Conglomerate|44734|14|Not recorded|p5,7,9-10,16-19|||Pine Mountain area.||||||
4893|Cribb Conglomerate|44775|4|Described|p7,8,map 2||Middle Triassic|||||||
4893|Cribb Conglomerate|44783|14|Not recorded|p16,18|||||||||
4893|Cribb Conglomerate|67402|5|Briefly described|p222, p223, p225|Carnian|Ladinian|Ipswich Basin. Deposited in a piedmont-fluviatile environment. ||Kholo Subgroup||Overlies the Hector Tuff. Overlain by the Tivoli Formation.|Conglomerate with minor sandstone and mudstone.|
4893|Cribb Conglomerate|68679|5|Briefly described|p394-395|Late Triassic|Late Triassic|Ipswich Basin. A thin unit, 4.4m to 13.7m thick.||Kholo Subgroup.||Overlies Hector Tuff.|Dominated by medium-grained to very coarse-grained feldspathic sublabile sandstone; also includes polymict granule to cobble conglomerate.|
4911|Crocker Formation|22973|5|Briefly described|p11 Fig.2(e)|Late Permian|Late Permian|||||||
4911|Crocker Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
4911|Crocker Formation|22978|6|Mentioned|p148 Fig.1|||||||||
4911|Crocker Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
4911|Crocker Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: ~259Ma.  Geological Province: Bowen Basin.||||||
4911|Crocker Formation|30449|6|Mentioned|p4|||Brachiopods. See also P21||||||
4911|Crocker Formation|30450|6|Mentioned|Table 1|||Permian age||||||
4911|Crocker Formation|31079|6|Mentioned|Fig. 6|||||||||
4911|Crocker Formation|31690|6|Mentioned|p37|||||||||
4911|Crocker Formation|32577|4|Described|p23|||Upper Permian. See also p24,27-29,42.||||||13-OCT-08
4911|Crocker Formation|32689|1|Redefined|p436|Permian|Permian|Lower boundary differs from Derrington and Morgan's.||||||13-OCT-08
4911|Crocker Formation|32945|6|Mentioned|p90|||See also P91. Permian||||||
4911|Crocker Formation|33390|5|Briefly described|p5|||Correlation. Refers Prouza and Park (1973).||||||13-OCT-08
4911|Crocker Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
4911|Crocker Formation|37070|6|Mentioned|p72|||||||||
4911|Crocker Formation|37072|6|Mentioned|p91|||||||||
4911|Crocker Formation|37726|6|Mentioned|Fig.2|||||||||
4911|Crocker Formation|38518|6|Mentioned|Fig.3|||||||||
4911|Crocker Formation|39264|6|Mentioned|p165|||||||||
4911|Crocker Formation|39267|6|Mentioned|p236|||||||||
4911|Crocker Formation|39268|6|Mentioned|p270|||||||||
4911|Crocker Formation|39272|5|Briefly described|p295|||Correlation||||||
4911|Crocker Formation|39273|6|Mentioned|Fig.2|||||||||
4911|Crocker Formation|39445|5|Briefly described|Table 8|||||||||
4911|Crocker Formation|40539|6|Mentioned|Fig.2|||||||||
4911|Crocker Formation|41191|6|Mentioned|p284|||See also Fig.3||||||
4911|Crocker Formation|41246|6|Mentioned|Map legend|Permian||||||||
4911|Crocker Formation|41809|6|Mentioned|p64|||||||||
4911|Crocker Formation|42662|6|Mentioned|p85|||||||||
4911|Crocker Formation|42856|6|Mentioned|p645|||||||||
4911|Crocker Formation|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|||||||
4911|Crocker Formation|44514|2|Defined|p33,34||Late Permian|Conformably overlain by Taurus Formation and Maria Formation.||||||13-OCT-08
4911|Crocker Formation|44571|2|Defined|p207|||||||||
4911|Crocker Formation|44618|14|Not recorded|p511,513-518,520||Permian|||||||
4911|Crocker Formation|48847|14|Not recorded|p8,9|||Equivalent to beds near top of Middle Bowen Beds.||||||
4911|Crocker Formation|48915|6|Mentioned|Table 3|||Upper Permian. See also P12||||||
4911|Crocker Formation|67402|6|Mentioned|p71|||Forms part of a wave and fluvial dominated delta system with the Catherine Sandstone and German Creek Formation. ||||||
4911|Crocker Formation|68679|5|Briefly described|p378, p382|||Prouza and Park (1973). Bowen Basin. 55m thick. Shallow-marine delta deposits. A "poorly studied" unit, similar to Catherine Sandstone.||||Passes [presumably vertically] into Catherine Sandstone. Together they pass laterally into German Creek Formation.|Quartzose to sublabile sandstone, siltstone, mudstone.|
4921|Croftby Dolerite|33290|4|Described|Table 1|||Anal.||||||
4921|Croftby Dolerite|45087|5|Briefly described|p169|||Chem. analyses.||||||
4941|Crossdale Rhyolite|36440|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
4941|Crossdale Rhyolite|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
4941|Crossdale Rhyolite|39079|6|Mentioned|p8|||||||||
4941|Crossdale Rhyolite|44076|14|Not recorded|p273,274|||||||||
4941|Crossdale Rhyolite|44781|14|Not recorded|p367|||||||||
4958|Crows Nest Granite|23799|3|Fully described|p89, p12 Tb. 1|Triassic|Late Permian|Supersedes Crow's Nest Granite.  Informally subdivided into "Rocky Creek Granite", "Central Granite", "Vonhoff Granite", "WoodvilleGranite" "Paradise Granite" and Rangeview Aplite" by Holden (1991).  Geological Province: Yarraman Subprovince.||||||
4958|Crows Nest Granite|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
4958|Crows Nest Granite|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Biotite, granite, adamellite; microgranite.||||||
4958|Crows Nest Granite|30303|2|Defined|p322|Early Triassic|Late Permian|Late Permian or Early Triassic age.||||||02-APR-08
4958|Crows Nest Granite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
4958|Crows Nest Granite|32912|5|Briefly described|p157|||U.Perm. Kaolin deposit||||||
4958|Crows Nest Granite|35063|6|Mentioned|p79|||||||||
4958|Crows Nest Granite|36579|6|Mentioned|Table 1|||||||||
4958|Crows Nest Granite|36954|6|Mentioned|p114|||||||||
4958|Crows Nest Granite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
4958|Crows Nest Granite|39445|5|Briefly described|Table 12|||||||||
4958|Crows Nest Granite|39845|6|Mentioned|p20|||||||||
4958|Crows Nest Granite|43008|5|Briefly described|map legend|||||||||
4958|Crows Nest Granite|43009|5|Briefly described|Map Legend|||||||||
4958|Crows Nest Granite|50322|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Biotite granite, adamellite.||||||09-JUN-04
4958|Crows Nest Granite|61003|6|Mentioned|p224|||||||||
4958|Crows Nest Granite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
4958|Crows Nest Granite|68679|5|Briefly described|p323, p410-413, p415-416|||West of the Esk Basin, northern New England Orogen. Crops out in a NNW-trending belt; outcrop area ~100 km2. May represent (a) roof pendants in the ?intruding Eskdale Igneous Complex, or (b) a fractionated product of the latter unit. Has lower Na2O and K2O and higher CaO. Geochemical plot.|242-237 Ma (various ages and authors listed).|||Intrudes Sugarloaf Metamorphics.|Dominated by pink, coarse-grained biotite granite with local microgranite and pegmatite phases. Six geochemically similar, granitic to aplitic subunits and three phases of dykes have been identified (Holden, 1991).|
4958|Crows Nest Granite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Crows Nest.||||||
4968|Croydon Volcanic Group|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
4968|Croydon Volcanic Group|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
4968|Croydon Volcanic Group|22533|6|Mentioned|p54,p56|Calymmian|Calymmian|placed in Croydon Province||||||15-JUN-04
4968|Croydon Volcanic Group|22669|6|Mentioned|Fig1 P248||Mesoproterozoic|||||||
4968|Croydon Volcanic Group|22811|6|Mentioned|p605|Mesoproterozoic|Mesoproterozoic|of Georgetown Region, Age of unit 1550 Ma||||||
4968|Croydon Volcanic Group|23220|6|Mentioned|p8|||Sediments contributed to Gilberton Formation.||||||
4968|Croydon Volcanic Group|23291|3|Fully described|p26, p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Intruded by Esmeralda Supersuite granites. Age: ~1550Ma. Thickness: >5000m. Overlain by Inorunie Group. Geological Province: Georgetown Region.||||||08-JUL-15
4968|Croydon Volcanic Group|23430|4|Described|p455-456|||S-Type chemical character. Overlain by Inorunie Group unconformably. In the Croydon Province.||||||21-DEC-06
4968|Croydon Volcanic Group|23431|5|Briefly described|p531|||Croydon Province.||||||
4968|Croydon Volcanic Group|23453|5|Briefly described|p10 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
4968|Croydon Volcanic Group|23510|5|Briefly described|Map Legend||Mesoproterozoic|||||||
4968|Croydon Volcanic Group|24169|6|Mentioned|p674|||Geological Province: Georgetown Inlier.||||||04-JUN-15
4968|Croydon Volcanic Group|24197|5|Briefly described|p32, p76|Mesoproterozoic|Mesoproterozoic|Dominated by subaerial felsic ignimbrites. Overlain by Inorunie Group. Age: emplaced at~1550Ma. Geological Province: Georgetown Inlier (Croydon Province). Comagmatic with Esmeralda Supersuite.||||||07-FEB-11
4968|Croydon Volcanic Group|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4968|Croydon Volcanic Group|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||17-AUG-04
4968|Croydon Volcanic Group|40659|1|Redefined|p248|Mesoproterozoic|Mesoproterozoic|||||||
4968|Croydon Volcanic Group|40860|6|Mentioned|p109|||See also p110.||||||21-DEC-06
4968|Croydon Volcanic Group|41272|5|Briefly described|M 1of1 A04|||See also M1of1 K03 and M 1of1 M03||||||
4968|Croydon Volcanic Group|41975|3|Fully described|p438|||||||||
4968|Croydon Volcanic Group|43259|6|Mentioned|Appendix 1,p15.||Proterozoic|Middle Proterozoic age.||||||
4968|Croydon Volcanic Group|43595|5|Briefly described|p353|||Date (Rb-Sr) approx. 1400 Ma||||||
4968|Croydon Volcanic Group|43664|4|Described|p3-53,57|||Age: 1552+/-2 Ma.||||||21-DEC-06
4968|Croydon Volcanic Group|43729|5|Briefly described|p1||Mesoproterozoic|||||||
4968|Croydon Volcanic Group|43793|5|Briefly described|p332|||||||||
4968|Croydon Volcanic Group|50537|5|Briefly described|p1.1, 3.3|||Geological Province: Georgetown Inlier.||||||
4968|Croydon Volcanic Group|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes Wonnemarra, B Creek, Carron and Idalia Rhyolites.||||||
4968|Croydon Volcanic Group|61258|5|Briefly described|p386, p387 Fig. 1|Mesoproterozoic|Mesoproterozoic|Subaerial felsic ignimbrites. Overlies the Etheridge Group. Age: 1552+/-2Ma (Black et al 1979). Geological Province: Georgetown Inlier.||||||
4968|Croydon Volcanic Group|63866|4|Described|p78-p79|Calymmian|Calymmian|Croydon Province. Estimated to be at least 1100-1500m thick. Hosts tin deposits.|||Includes the Idalia Rhyolite.|Overlain by the Inorunie Group. Intruded by the Esmeralda Supersuite.|Rhyolitic ignimbrite and lesser porphyritic rhyolite with flow banding, dacitic ignimbrite, quartzo-feldspathic sandstones, siltstones and minor andesite.|
4968|Croydon Volcanic Group|65887|5|Briefly described|p40 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
4968|Croydon Volcanic Group|66529|5|Briefly described|p5 |||See also references to Croydon Volcanics (p41, p53-54).|~1552 Ma (Black and McCulloch, 1990).|||Unconformably overlies the Langlovale Group. Coeval with magmatic rocks of the Esmeralda and Forsayth Supersuites.|Felsic ignimbrites.|
4968|Croydon Volcanic Group|66800|5|Briefly described|pp925-926.|Proterozoic|Proterozoic||1552 +/- 2 Ma (Black & McCulloch 1990).|||Related to Esmeralda Supersuite. Overlies Etheridge Group.|Subaerial felsic ignimbrites.|
4968|Croydon Volcanic Group|67323|5|Briefly described|p21, p37|||See also Eastern Australia Time-Space Plot. Georgetown Inlier. Coeval with emplacement of the Esmeralda Supersuite. The rank [Group] is absent from the Time-Space Plot.|1548 +/- 18 Ma.|||Overlies Langlovale Group. Is intruded by Forsayth Supersuite.||
4968|Croydon Volcanic Group|67341|6|Mentioned|vi|||Croydon Subprovince, Etheridge Province.||||||
4968|Croydon Volcanic Group|67430|6|Mentioned|p25|||||||||
4968|Croydon Volcanic Group|68307|5|Briefly described|p78, p80-81, p85, p87-88, p97|Mesoproterozoic|Mesoproterozoic|Etheridge Province. North Australian Craton. With the granites of the Esmeralda Supersuite, shows as a very thin, nonreflective domain c.2.1km thick.||||||
4968|Croydon Volcanic Group|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province. Has high K, Th and U radiometric responses; is weakly- to non-magnetic.|||Includes Wallabadah Siltstone; B-Creek, Parrot Camp, Carron and Idalia Rhyolites.|||
4968|Croydon Volcanic Group|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province. Weakly to non-magnetic.|||Includes Wallabadah Siltstone; B-Creek, Parrot Camp, Carron and Idalia Rhyolites.|||
4968|Croydon Volcanic Group|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Wonnemarra, B-Creek, Carron and Idalia Rhyolites.||Ignimbrites and rhyolite.|
4968|Croydon Volcanic Group|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Wonnemarra, B-Creek, Carron and Idalia Rhyolites.||Ignimbrites and rhyolite.|
4968|Croydon Volcanic Group|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province. Generally weakly magnetic. |||Includes B-Creek, Carron and Idalia Rhyolites.||Ignimbrites and rhyolite.|
4968|Croydon Volcanic Group|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province. Generally weakly magnetic. |||Includes B-Creek, Carron and Idalia Rhyolites.||Ignimbrites and rhyolite.|
4968|Croydon Volcanic Group|68416|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Shown as younger than D2 ~ 1552 Ma.|< 1552 Ma||Includes Idalia Rhyolite.|||
4968|Croydon Volcanic Group|68417|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province.|||Includes Idalia Rhyolite.|||
4968|Croydon Volcanic Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||||||
4968|Croydon Volcanic Group|68576|6|Mentioned|Q_11: p2|||||||||
4968|Croydon Volcanic Group|69591|4|Described|p48, p61-62, p69-70, p73-75, p83|||See also p85 Fig.2.81, p103, p109-111. Branch (1966). Croydon Province, Georgetown Inlier. Coeval with emplacement of, and comagmatic with, the Esmeralda Supersuite. Neither base nor top are exposed; estimated thickness is at least 1100-1500m. Flat-lying (post-late Isan Orogeny). Geochemistry briefly described. LITHOLOGY continued: quartzose and quartzofeldspathic sandstones and siltstones, minor andesite, mostly near the base of the succession and/or in the north of the outcrop area. Graphite (mostly disseminated; also pellets to 1cm) is characteristic (up to 2% by volume), as are intense recrystallisation and moderate deuteric alteration.|1552 +/- 4 Ma.||Idalia, Carron, Parrot Camp, B-Creek, Wonnemarra Rhyolites; Goat Creek Andesite; Wallabadah Siltstone.|Unconformably overlies the Langlovale Group. Is overlain disconformably by Inorunie Group. Is faulted against Etheridge and Langlovale Groups. Is intruded by Esmeralda Supersuite.|Dominated by grey, massive, intensely welded rhyolitic ignimbrite, and lesser volumes of sparsely porphyritic rhyolite with contorted flow banding; local dacitic ignimbrite and unwelded dacitic fragmental rocks. S-type.  See COMMENTS for more.|
4968|Croydon Volcanic Group|70207|6|Mentioned|p14|Mesoproterozoic|Mesoproterozoic|Georgetown region.||||||
4968|Croydon Volcanic Group|73137|6|Mentioned|p84|||Georgetown Inlier. Emplaced between 1550 Ma and 1560 Ma[?].||||||
4968|Croydon Volcanic Group|73527|6|Mentioned|p2, p3 Fig.2|||See also Croydon Volcanics.||||||
4968|Croydon Volcanic Group|73642|5|Briefly described|p2 Fig.1, p5, p10 Fig.8|Calymmian|Calymmian|Co-magmatic with Esmeralda Granite. See also Croydon Volcanics.|1552+/-2 Ma, 1550+/-7 Ma, 1548+/-18 Ma|||Overlies Esmeralda Granite||
4968|Croydon Volcanic Group|75079|5|Briefly described|p2-3, 5-7, 9-14, 16-18|Mesoproterozoic|Mesoproterozoic|Western domain, Georgetown Inlier. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|1550 +/- 7 Ma.|Esmeralda Supersuite.||Unconformably overlies the Etheridge Group. Is intruded by the co-magmatic Esmeralda Supersuite.|Felsic extrusives, undeformed to weakly deformed. Includes rhyolite. Characterised by medium- to coarse-grained orthoclase phenocrysts.|
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||
4984|Culcraigie Granite|23037|4|Described|p93,4,5,6|Early Triassic|Late Permian|||||||
4984|Culcraigie Granite|33774|3|Fully described|p69|||||||||
4984|Culcraigie Granite|36333|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic.  Part of the Rawbelle batholith.||||||15-JUL-04
4984|Culcraigie Granite|36926|6|Mentioned|p176|||||||||
4984|Culcraigie Granite|39445|5|Briefly described|Table 12|||||||||
4984|Culcraigie Granite|41246|6|Mentioned|Map legend|Triassic|Permian|||||||
4984|Culcraigie Granite|43008|5|Briefly described|map legend|||||||||
4984|Culcraigie Granite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Pink, coarse grained, equigranular leucogranite with traces of bleached biotite.||||||
4984|Culcraigie Granite|65388|1|Redefined|p308-310, p205, 236, 301, 303, 304, 318|Early Triassic|Late Permian|Original definition modified. Smaller pluton now distinguished as Kildare Granodiorite. Of Tandora Suite. Western half of larger body now mapped as Tandora Granodiorite. Remaining area informally subdivided. Most contacts masked by cover. Overlain by Mount Eagle Volcanics. Intruded by Boolgal Granophyre, and probably Telemark Granodiorite. Age probable. Pink, coarse-grained, equigranular, leucocratic alkali granite, deeply weathered. Includes dyke swarms that may relate to Mount Eagle Volcanics or Telemark Granodiorite. See also p324, 331, 332, 340.||||||
4984|Culcraigie Granite|68679|5|Briefly described|p418-420|||Rawbelle Batholith. Separated from Tandora Granodiorite by radiometric interpretation and the latter's more diverse lithology. Geochemistry plot.||Tandora Suite.||Is overlain by Mount Eagle Volcanics. Is intruded by Boolgal Granophyre and Telemark Granodiorite.|Leucogranite.|
4999|Cultivation Gully Formation|23035|6|Mentioned|18|||||||||
4999|Cultivation Gully Formation|23422|5|Briefly described|p180, p206 Table 6.3|Middle Devonian|Middle Devonian|Of Fanning River Group.||||||
4999|Cultivation Gully Formation|23430|5|Briefly described|Plate 14.11 + p505||Devonian|Burdekin Basin Province.||||||
4999|Cultivation Gully Formation|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Fanning River Group.||||||14-NOV-07
4999|Cultivation Gully Formation|23522|5|Briefly described|p250 Fig 6|Givetian|Givetian|||||||
4999|Cultivation Gully Formation|23893|5|Briefly described|p16|Middle Devonian|Middle Devonian|Of Fanning River Group.  Geological Province:Burdekin Basin.||||||
4999|Cultivation Gully Formation|24577|4|Described|p753, p752 Fig. 1|Givetian|Eifelian|Of the Fanning River Group. Overlain by the Vanneck Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
4999|Cultivation Gully Formation|24610|5|Briefly described|p62|Middle Devonian|Middle Devonian|Of the Fanning River Group. Underlain by Burdekin Limestone. Maximum Thickness: 90m. Geological Province: Burdekin Basin. Dominated by shales, siltstones, and thin-bedded sandstones; locally rich brachiopod fauna.||||||14-NOV-07
4999|Cultivation Gully Formation|24611|5|Briefly described|p193|Givetian|Eifelian|Geological Province: Burdekin Basin.  See also p196 Fig. 2.||||||
4999|Cultivation Gully Formation|24612|4|Described|p10|Givetian|Eifelian|Of Fanning River Group. Overlain by Dotswood Group. Geological Province: Burdekin Basin. Consists of sandstone (calcareous in places), siltstone and shale, with rich coral fauna in lower section.||||||14-NOV-07
4999|Cultivation Gully Formation|24613|2|Defined|p9 Fig. 4, p17-18, Tb.1|Givetian|Givetian|Of Fanning Gp. Conformable on Burdekin Fm (transitional); disconformable below Vanneck Fm. Max.thickness: 90m. Geol.prov: Burdekin Basin. Lower mudst.+siltst.with some sst, minor l'st; upper feldspathic sst interbedded with siltst.- more detail included.||||||03-JUL-14
4999|Cultivation Gully Formation|24614|4|Described|p190, p194|Givetian|Givetian|Of the Fanning River Group. Consists of two informal members. Grades up out of Burdekin Limestone below. Thickness in type section: 90m; ~135m. Geological Province: Burdekin Basin. See also p191 Fig. 1, p193 Fig. 2.||||||07-FEB-11
4999|Cultivation Gully Formation|31285|4|Described|p82|||See also p85. Givetian. Unit of Fanning River Group.||||||14-NOV-07
4999|Cultivation Gully Formation|31999|5|Briefly described|p140|||Table 11||||||
4999|Cultivation Gully Formation|32619|6|Mentioned|p463|||Givetian. Fauna.||||||
4999|Cultivation Gully Formation|37573|4|Described|Table 1|||See also Fig.5 and p208.||||||14-NOV-07
4999|Cultivation Gully Formation|39445|5|Briefly described|Table 5|||||||||
4999|Cultivation Gully Formation|39686|5|Briefly described|Table 1|||||||||
4999|Cultivation Gully Formation|39731|6|Mentioned|p31|||||||||
4999|Cultivation Gully Formation|39732|6|Mentioned|p29|||||||||
4999|Cultivation Gully Formation|41774|6|Mentioned|p32|||||||||
4999|Cultivation Gully Formation|42031|6|Mentioned|p764|||||||||
4999|Cultivation Gully Formation|42295|5|Briefly described|p6|||||||||
4999|Cultivation Gully Formation|43461|14|Not recorded|table p618||Givetian|Part of Fanning River Group||||||
4999|Cultivation Gully Formation|43933|5|Briefly described|Map Legend||Middle Devonian|Of Fanning River Group.||||||14-NOV-07
4999|Cultivation Gully Formation|43935|5|Briefly described|Map Legend||Middle Devonian|Of Fanning River Group.||||||22-FEB-05
4999|Cultivation Gully Formation|44058|14|Not recorded|Tb.p104|||Part of Fanning River Group.||||||
4999|Cultivation Gully Formation|44061|14|Not recorded|p10|||Formation of Fanning River Group.||||||
4999|Cultivation Gully Formation|48904|2|Defined|p25|Givetian|Givetian|||||||
4999|Cultivation Gully Formation|62522|5|Briefly described|p23, p28|Givetian|Givetian|Parts overlain by Kukiandra Formation - which are now considered undifferentiated Dotswood Group. Most of the area originally mapped as C.G. Formation is now grouped with undifferentiated Dotswood Gp.  Parts underlie Vanneck Fm. Geol. prov: Burdekin Basin||||||
4999|Cultivation Gully Formation|65214|6|Mentioned|p279, p280|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
4999|Cultivation Gully Formation|65940|6|Mentioned|p201|Givetian|Givetian|Contains Endophyllum columna, ascribed mid-Givetian age (Zhen and Jell 1996).||||||
4999|Cultivation Gully Formation|67402|4|Described|p239, p247, p248|Givetian|Givetian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide.||Fanning River Group||Overlies the Burdekin Formation.|Varied calcaerous and siliciclastic rocks including fine to medium-grained feldspathic (arkosic) sandstone, siltstone, mudstone, lesser limestone and sandy limestone.|
4999|Cultivation Gully Formation|68731|5|Briefly described|p177 Fig 3.91, p184, p185 Tb 3.4, p186|Middle Devonian|Middle Devonian|Burdekin Basin. < 90 m thick. Fluviatile coastal floodplain with anastomosing channel networks interspersed with vegetated overbank tracts. Contemporary volcanism indicated by sandstone compositions.||Of the Fanning River Group.|||Comprises interbedded siltstone and fine- to medium-grained volcaniclastic sandstone lenses with common lycopod plant remains and horizons with pedigenic carbonate granules. Sporadic tuff beds and rare horizons with marine fossils also occur.|03-JUL-14
4999|Cultivation Gully Formation|69030|5|Briefly described|p6|Carboniferous|Devonian|Camel Creek Subprovince (Broken River Province).||Fanning River Group.||||
5003|Cumbana Rhyolite|23291|4|Described|p95 Tb. 3.10, p101 Tb. 3.13|Early Permian|Early Permian|Parent: Namarrong Volcanic Subgroup. Age of Brodies Gap Rhyolite, in same Subgroup:283+/-3Ma. Thickness: ~ 920m. Geological Province: Georgetown Region.||||||26-JUN-15
5003|Cumbana Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V16. Assumed to be I-Type.||||||
5003|Cumbana Rhyolite|23619|4|Described|p31 table 1||Carboniferous|Previously Cumbana Rhyolite Porphyry. Of the Nammarong Volcanic Subgroup, of the Newcastle Range Volcanic Group.||||||26-JUN-15
5003|Cumbana Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|Of Namarrong Volcanic Subgroup, Newcastle Range Volcanics.||||||04-NOV-04
5003|Cumbana Rhyolite|43113|4|Described|Table 1 p18||Carboniferous|of Nammarong Volcanic Subgroup.[or Namarrong Volcanic Subgroup?]||||||
5003|Cumbana Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Nammarong Volcanic Subgroup||||||
5003|Cumbana Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Namarrong Volcanic Subgroup.||||||
5003|Cumbana Rhyolite|43740|4|Described|p12|||||||||
5003|Cumbana Rhyolite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group.||||||
5003|Cumbana Rhyolite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Nammarong Volcanic Subgroup.||||||
5003|Cumbana Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Five facies are separately mapped.||Unit in Newcastle Range Volcanic Group.|||Rhyolitic ignimbrite with phenocrysts to 4 mm across; similar, but with phenocrysts to 2 mm across, minor volcanic rudite; volcanic breccia; greenish-grey aphyric andesite; brown crystal-rich rhyolitic volcanic lutite to very coarse volcanic rudite.|
5003|Cumbana Rhyolite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|The 5 facies are mapped separately. Kennedy Province.||Of the Nammarong Volcanic Subgroup.|||Grey to brown or purple (moderately) crystal-rich rhyolitic ignimbrite, locally abundant lithic clasts; rhyolitic ignimbrite with phenocrysts up to 4 mm; minor rhyolitic ignimbrite with phenocrysts up to 2 mm; andesite; rhyolitic lutite to rudite.|
5070|Currant Bush Limestone|22954|6|Mentioned|Fig3p9|Undillan|Middle Cambrian|||||||
5070|Currant Bush Limestone|23031|4|Described|28|||Geol province: Georgina Basin.||||||08-AUG-06
5070|Currant Bush Limestone|23393|5|Briefly described|p22|Paleozoic|Paleozoic|||||||07-NOV-08
5070|Currant Bush Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
5070|Currant Bush Limestone|26310|4|Described|Table 1|Middle Cambrian|Middle Cambrian|Maximum Thickness: 500 feet.  Limestone, some marl.||||||
5070|Currant Bush Limestone|30242|6|Mentioned|Fig.2|||||||||
5070|Currant Bush Limestone|30479|6|Mentioned|Fig.5|||See also Fig.6, Fig.7. Stratigraphic relationships||||||
5070|Currant Bush Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5070|Currant Bush Limestone|31396|6|Mentioned|Fig.3|||||||||
5070|Currant Bush Limestone|32948|4|Described|p111|||Re fossil locality.||||||08-AUG-06
5070|Currant Bush Limestone|33111|4|Described|p35|||By inference, the type locality is in the vicinity of Currant Bush Creek, 16 km SW of Thorntonia homestead. No type section has been specified.||||||24-NOV-22
5070|Currant Bush Limestone|33368|5|Briefly described|p5|||||||||
5070|Currant Bush Limestone|33482|6|Mentioned|Fig.2|||Middle Cambrian||||||
5070|Currant Bush Limestone|34287|6|Mentioned|Table.3?|||||||||
5070|Currant Bush Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|34659|6|Mentioned|p228|||||||||
5070|Currant Bush Limestone|35004|6|Mentioned|Fig.60|||||||||
5070|Currant Bush Limestone|35054|6|Mentioned|Table 23|||||||||
5070|Currant Bush Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|35139|4|Described|Table.2|||||||||
5070|Currant Bush Limestone|35553|6|Mentioned|p36|||See also Appendix 2, description of Agnostid localities.||||||
5070|Currant Bush Limestone|35843|6|Mentioned|p444|||Source of ostracods.||||||
5070|Currant Bush Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
5070|Currant Bush Limestone|36818|6|Mentioned|p203|||||||||
5070|Currant Bush Limestone|37275|6|Mentioned|p287|||||||||
5070|Currant Bush Limestone|37572|4|Described|p157|||See also p165 and Fig.7||||||08-AUG-06
5070|Currant Bush Limestone|38444|5|Briefly described|p105|||||||||
5070|Currant Bush Limestone|38445|6|Mentioned|p105|||||||||
5070|Currant Bush Limestone|38446|6|Mentioned|Table 23|||||||||
5070|Currant Bush Limestone|39422|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Thin-bedded grey limestone and lenses and interbeds of marl and sandy dolomite. Conformably overlies Border Waterhole Formation; conformably overlain and interfingered with Camooweal Dolomite.||||||11-JUN-08
5070|Currant Bush Limestone|39445|5|Briefly described|Table 4|||See also p62||||||08-AUG-06
5070|Currant Bush Limestone|39497|6|Mentioned|p16|||||||||
5070|Currant Bush Limestone|39690|6|Mentioned|Table 1|||||||||
5070|Currant Bush Limestone|39708|5|Briefly described|p477|||||||||
5070|Currant Bush Limestone|39942|6|Mentioned|p465|||||||||
5070|Currant Bush Limestone|40038|6|Mentioned|p248|||||||||
5070|Currant Bush Limestone|40686|5|Briefly described|p407|||||||||
5070|Currant Bush Limestone|40856|5|Briefly described|p315|||Mention Fig.23.6||||||
5070|Currant Bush Limestone|41018|6|Mentioned|p239|||||||||
5070|Currant Bush Limestone|41129|6|Mentioned|Fig.8|||||||||
5070|Currant Bush Limestone|41240|6|Mentioned|Fig.1|||||||||
5070|Currant Bush Limestone|41388|6|Mentioned|Fig.2|||||||||
5070|Currant Bush Limestone|42139|6|Mentioned|Fig.13 P80|||||||||
5070|Currant Bush Limestone|42477|5|Briefly described|p68|||||||||
5070|Currant Bush Limestone|44091|14|Not recorded|p16,Tb.1,18||Cambrian|||||||
5070|Currant Bush Limestone|44205|14|Not recorded|p89,155|||See also Lexicon.||||||
5070|Currant Bush Limestone|44210|2|Defined|map, Tb.2|||Overlies Inca Formation.||||||23-NOV-22
5070|Currant Bush Limestone|44211|4|Described|p97,100-103|||Contemporaneous with most of Age Creek Formation, Inca Formation, Quita Formation.||||||23-NOV-22
5070|Currant Bush Limestone|44213|14|Not recorded|Map Legend|||Not on white card.||||||
5070|Currant Bush Limestone|44274|2|Defined|Tb.1,p10,11,13,map||Middle Cambrian|See also Lexicon. Conformably overlies Border Waterhole Formation.||||||
5070|Currant Bush Limestone|44275|14|Not recorded|Map Legend|||||||||
5070|Currant Bush Limestone|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
5070|Currant Bush Limestone|44441|14|Not recorded|p.8||Middle Cambrian|O/lain by Camooweal Dolomite to North. Middle Cambrian. (E53-16).||||||
5070|Currant Bush Limestone|44482|14|Not recorded|p.11-12, opp.p.6,map|||(E53-12). See also p.15, for more details||||||
5070|Currant Bush Limestone|44483|5|Briefly described|map legend||Middle Cambrian|Middle Cambrian.||||||
5070|Currant Bush Limestone|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlies Border Waterhole Formation.||||||01-JUL-04
5070|Currant Bush Limestone|45032|14|Not recorded|p8,10||Middle Cambrian|Tb.1, Pl.1. (E53-12).||||||
5070|Currant Bush Limestone|45052|3|Fully described|p93|||M.Camb.||||||
5070|Currant Bush Limestone|45054|6|Mentioned|p6|||M.Cambrian. Fossil locality||||||
5070|Currant Bush Limestone|45079|5|Briefly described|p34|||Cambrian age||||||
5070|Currant Bush Limestone|45102|6|Mentioned|p43|||||||||
5070|Currant Bush Limestone|45119|6|Mentioned|p3,p5|||||||||
5070|Currant Bush Limestone|45166|5|Briefly described|Table 15|||||||||
5070|Currant Bush Limestone|47058|5|Briefly described|p132|||||||||
5070|Currant Bush Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin||||||11-MAY-05
5070|Currant Bush Limestone|60418|5|Briefly described|p140|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Partially dolomitised foetid argillaceous, quartzic and bioclast limestone; interbeds of ooid grainstone, dolostone, shale, siltstone and marl.||||||
5070|Currant Bush Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
5070|Currant Bush Limestone|64068|5|Briefly described|p63, 62, 64, p137|||Correlative with Arthur Creek Formation in NT. Sparked interest in oil shale potential of the Georgina Basin. Correlated with Blazan Shale, Inca Formation, Quita Formation, Roaring Siltstone, Devoncourt Limestone.||||Overlies and interdigitates with Inca Formation.|Contains thin oil shale, bituminous limestone and bituminous shale.|05-APR-12
5070|Currant Bush Limestone|64443|6|Mentioned|pg6 Tb.1, p14, p40.|||Correlative of Wonarah Formation, Ranken Limestone; conformably underlies the Camooweal Dolostone.||||||
5070|Currant Bush Limestone|65337|3|Fully described|p9 Fig.5, pp64-65.|Middle Cambrian|Middle Cambrian|Southeast MOUNT DRUMMOND area. 50 - 116 m thick. Occasional ellipsoidal concretions are characteristic.||Unit in Narpa Group.||Overlies Border Waterhole Formation. Is overlain by Camooweal Dolostone.|Grey and tan, partially dolomitised foetid argillaceous, quartzic and bioclastic limestone; interbeds of ooid grainstone, sandstone, shale, siltstone and marl.|
5070|Currant Bush Limestone|67323|5|Briefly described|Solid Geology Map; p72, p83|Middle Cambrian|Middle Cambrian|See also GIS attrib tbl. Undilla Sub-basin, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Overlies Inca Formation and (unconformably) Beetle Creek Formation. Is overlain by V-Creek Limestone. Partial lateral equivalent of Age Creek Formation.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
5070|Currant Bush Limestone|69437|5|Briefly described|p22:10|Series 3|Series 3|Eastern Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2.||||Is overlain by Camooweal Dolostone.||12-JUL-16
5070|Currant Bush Limestone|69443|4|Described|p28:16, 20, 22-24|Middle Cambrian|Middle Cambrian|Opik (1956, 1960). Undilla Sub-basin, Georgina Basin. Unclear stratigraphic relationships. Is overlain transitionally, and is partly equivalent to, Camooweal Dolostone. Correlated with Anthony Lagoon, Wonarah Formations and Ranken Limestone. Shallow-marine, carbonate ramp deposits. Contains a very diverse fossil assemblage; age determinations are discussed.||Narpa Group.||Overlies Border Waterhole Formation conformably or disconformably; Thorntonia Limestone unconformably; Gowers Formation disconformably. Overlies and interfingers with Age Creek and Inca Formations.|Mainly bedded, partially dolomitised foetid argillaceous, quartzose and bioclast limestone and dolomitic limestone, with interbeds of ooid grainstone, shale, siltstone, marl and chert, which occurs as discrete layers or irregular patches.|12-JUL-16
5070|Currant Bush Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
5070|Currant Bush Limestone|69591|5|Briefly described|p87-90, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Contains an extremely diverse fauna (listed).||Narpa Group.||Overlies and in part equivalent to Inca Formation; disconformably overlies Thorntonia Limestone and Age Creek Formation. Is overlain conformably by V Creek Limestone.|A bituminous, flaggy limestone with oolitic, shaly and marly interbeds up to 120m thick. Local beds up to 2m thick of rip-up conglomerates, and numerous algal-bound unbedded build-ups up to 10m diameter piercing the otherwise thin bedding.|
5070|Currant Bush Limestone|69673|4|Described|p116, p117|||116m thick.||Narpa Group|||Bedded, partially dolomitized foetid, argillaceous, quartzic and bioclast limestone, dolomitic limestone interbedded with ooid grainstone, shale, siltstone, marl and chert.|
5070|Currant Bush Limestone|70380|6|Mentioned|p745|Series 3|Series 3|Undilla Sub-basin, Georgina Basin.||||||
5070|Currant Bush Limestone|70723|4|Described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Deposited under anoxic conditions on a carbonate ramp. Contains a highly divese fossil assemblage. Karst features occur in the lower part of the unit. Oil-prone source rock. Kerogen type and biomarker compositions discussed in detail. Mis-spelt as Current Bush Limestone on p25.||Narpa Group||Overlies Beetle Creek and Inca Formations. Is overlain by Age Creek Formation.|Partially dolomitized argillaceous, fossiliferous, quartzic and bioclastic limestone with fine layers of shale; siltstone, marl and chert.|
5070|Currant Bush Limestone|72297|6|Mentioned|p752|Cambrian|Cambrian|Georgina Basin.||||||
5070|Currant Bush Limestone|72321|6|Mentioned|Fig 2|Drumian|Wulian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan. ||of Narpa Group.||||
5070|Currant Bush Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
5070|Currant Bush Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
5070|Currant Bush Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Gowers Formation, Beetle Creek Formation, Inca Formation, underlies V-Creek Limestone, Age Creek Formation|Limestone.|
5077|Currawinya Conglomerate|31694|6|Mentioned|p348|||||||||
5077|Currawinya Conglomerate|32086|2|Defined|p326|Late Carboniferous|Late Carboniferous|See also P325||||||
5077|Currawinya Conglomerate|36528|6|Mentioned|p171|||See also P182.||||||
5077|Currawinya Conglomerate|36936|6|Mentioned|p211|||||||||
5077|Currawinya Conglomerate|36961|6|Mentioned|p212|||||||||
5077|Currawinya Conglomerate|68679|6|Mentioned|p351|||North of Drake (NSW); similar acid igneous clasts to those in the Mount Barney beds across the QLD border near Mount Barney.||||||
5093|Curtis Island Group|9194|5|Briefly described|Map legend|Paleozoic|Paleozoic|Greywacke, siltstone, shale; minor andesite, spillite, chert.  Intruded by Miriam Vale Granodiorite; overlain by Agnes Water Volcanics.||||||23-DEC-09
5093|Curtis Island Group|23799|5|Briefly described|p18, p25|||Includes the Wandilla, Doonside and Shoalwater Formations.||||||
5093|Curtis Island Group|24279|5|Briefly described|p1799|Carboniferous|Carboniferous|Overlain by Aranbanga Volcanic Group. Includes metasediments, quartzite, phyillite and schist.||||||
5093|Curtis Island Group|24382|5|Briefly described|Map legend|Carboniferous|Carboniferous|Constituents include: Wandilla Formation, Shoalwater Formation and Karandah Granodiorite||||||
5093|Curtis Island Group|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Includes Doonside, Wandilla and Shoalwater Formations.||||||
5093|Curtis Island Group|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5093|Curtis Island Group|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5093|Curtis Island Group|30508|5|Briefly described|p89|||||||||
5093|Curtis Island Group|30655|3|Fully described|p5|||On Table 1.||||||18-AUG-08
5093|Curtis Island Group|30776|6|Mentioned|p104|||Contains oolitic arenite||||||
5093|Curtis Island Group|30777|4|Described|p417|||Discussed||||||
5093|Curtis Island Group|30811|5|Briefly described|p528|||||||||
5093|Curtis Island Group|30914|6|Mentioned|Map legend|Devonian|Devonian|Devonian - Carboniferous||||||
5093|Curtis Island Group|30915|6|Mentioned|p98|||||||||
5093|Curtis Island Group|30916|6|Mentioned|p96|||||||||
5093|Curtis Island Group|31365|6|Mentioned|p3|||||||||
5093|Curtis Island Group|31657|4|Described|p91|||See also p92, 99, 100. Ordovician and Silurian.||||||05-APR-07
5093|Curtis Island Group|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5093|Curtis Island Group|31659|2|Defined|p1, p11|Silurian|Ordovician|Thickness: >60,000ft. Characterised by quartz greywacke.||||||08-OCT-08
5093|Curtis Island Group|31999|4|Described|p133|||See also p146. Table 1.||||||05-APR-07
5093|Curtis Island Group|32357|3|Fully described|p7|||Table 1.||||||18-AUG-08
5093|Curtis Island Group|32358|3|Fully described|p6|||Table 1.||||||18-AUG-08
5093|Curtis Island Group|32359|5|Briefly described|p735|||||||||
5093|Curtis Island Group|32360|6|Mentioned|p748|||||||||
5093|Curtis Island Group|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5093|Curtis Island Group|32882|6|Mentioned|p380|||||||||
5093|Curtis Island Group|33696|6|Mentioned|p6|||Re oolitic arenite.||||||
5093|Curtis Island Group|33769|5|Briefly described|p150|||||||||
5093|Curtis Island Group|33774|6|Mentioned|p19|||Refers Kirkegaard et al. (1970)||||||
5093|Curtis Island Group|34974|6|Mentioned|Fig. 2|||||||||
5093|Curtis Island Group|35101|6|Mentioned|p1|||P19||||||
5093|Curtis Island Group|36211|6|Mentioned|p267|||||||||
5093|Curtis Island Group|36246|6|Mentioned|Fig.1|||||||||
5093|Curtis Island Group|36528|6|Mentioned|p170|||||||||
5093|Curtis Island Group|36716|6|Mentioned|p142|||||||||
5093|Curtis Island Group|37467|6|Mentioned|p4|||||||||
5093|Curtis Island Group|37565|6|Mentioned|Fig.8|||||||||
5093|Curtis Island Group|37676|6|Mentioned|p1|||||||||
5093|Curtis Island Group|38081|5|Briefly described|Table 1|||||||||
5093|Curtis Island Group|38087|6|Mentioned|p77|||||||||
5093|Curtis Island Group|38391|6|Mentioned|p6|||||||||
5093|Curtis Island Group|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
5093|Curtis Island Group|38805|6|Mentioned|p90|||||||||
5093|Curtis Island Group|39151|6|Mentioned|p248|||||||||
5093|Curtis Island Group|39445|6|Mentioned|p80|||Manganese ore. See also P83 & P84||||||
5093|Curtis Island Group|39493|6|Mentioned|Fig.2|||||||||
5093|Curtis Island Group|39505|6|Mentioned|p167|||||||||
5093|Curtis Island Group|39632|6|Mentioned|p209|||||||||
5093|Curtis Island Group|39973|6|Mentioned|p4|||||||||
5093|Curtis Island Group|40116|6|Mentioned|Fig.2|||||||||
5093|Curtis Island Group|40246|6|Mentioned|Fig.1|||||||||
5093|Curtis Island Group|40247|6|Mentioned|p207|||||||||
5093|Curtis Island Group|40435|6|Mentioned|p47|||||||||
5093|Curtis Island Group|40475|5|Briefly described|p2|||||||||
5093|Curtis Island Group|40623|5|Briefly described|p79|||||||||
5093|Curtis Island Group|40787|5|Briefly described|p346|||||||||
5093|Curtis Island Group|40919|6|Mentioned|Fig.2|||||||||
5093|Curtis Island Group|40960|6|Mentioned|p218|||||||||
5093|Curtis Island Group|41246|6|Mentioned|Map legend|Carboniferous|Devonian|||||||
5093|Curtis Island Group|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
5093|Curtis Island Group|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
5093|Curtis Island Group|41736|6|Mentioned|p115|||||||||
5093|Curtis Island Group|41738|6|Mentioned|p163|||||||||
5093|Curtis Island Group|41778|6|Mentioned|p372|||||||||
5093|Curtis Island Group|41790|6|Mentioned|p475|||||||||
5093|Curtis Island Group|41922|4|Described|Table 1, P11|||||||||
5093|Curtis Island Group|41925|6|Mentioned|p43|||||||||
5093|Curtis Island Group|41927|6|Mentioned|p61|||||||||
5093|Curtis Island Group|42547|4|Described|p53|||||||||
5093|Curtis Island Group|42660|6|Mentioned|App.3.1 P161|||||||||
5093|Curtis Island Group|42901|5|Briefly described|p403|||||||||
5093|Curtis Island Group|42929|6|Mentioned|Fig.3 P458|||||||||
5093|Curtis Island Group|43008|5|Briefly described|map legend|||||||||
5093|Curtis Island Group|44093|5|Briefly described|p134 Tb. 10.1|Carboniferous|Devonian|Geological Province: Beenleigh Block.||||||
5093|Curtis Island Group|45107|6|Mentioned|p6|||||||||
5093|Curtis Island Group|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes: Doonside Formation, Wandilla Formation, Shoalwater Formation.||||||17-MAY-04
5093|Curtis Island Group|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes Shoalwater, Wandilla and Doonside Formations, and Balnagowan Volcanic Member.||||||17-MAY-04
5093|Curtis Island Group|60557|5|Briefly described|p18 Fig. 5a, p23|Carboniferous|Late Devonian|Includes the Doonside, Wandilla and Shoalwater Formations.||||||09-JUN-05
5093|Curtis Island Group|61035|6|Mentioned|p16|Carboniferous|Devonian|Lower and upper greenschist facies metasedimentary rocks.||||||07-FEB-11
5093|Curtis Island Group|63821|4|Described|p15, p38|Carboniferous|Carboniferous|Comprises 3 sections: Wandilla, Shoalwater and an undivided Curtis Isalnd Group sequence. Lithological detail for the undivided section is given. Geological Province: Wandilla Province - Coastal Block.||||||07-FEB-11
5093|Curtis Island Group|64398|5|Briefly described|Map legend|Carboniferous|Late Devonian|Includes Doonside and Wandilla Formations and an unnamed upper unit if sedimentary rocks.||||||
5093|Curtis Island Group|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Includes Wandilla and Doonside Formations and unnamed sedimentary rocks.||||||18-AUG-08
5093|Curtis Island Group|64556|5|Briefly described|p18-23, p55-56|||Intruded by a microgranite dyke into the Shoalwater Formation.||||||07-FEB-11
5093|Curtis Island Group|65388|5|Briefly described|p153, 156|||Broome Head Metamorphics are considered high grade equivalents.||||||
5093|Curtis Island Group|68008|5|Briefly described|p4, p109-120, p294|||Wandilla Province. Interpreted as an accretionary wedge asemblage, known also as the Wandilla terrane or the Wandilla-Shoalwater accretionary wedge. Structurally complex; amphibolite facies metamorphosed.|||Doonside, Wandilla, Shoalwater Formations.|||
5093|Curtis Island Group|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince.||||||
5093|Curtis Island Group|68679|5|Briefly described|p309, p312-313, p317-321, p324, p347|Carboniferous|Devonian|Holcombe et al. (1997). The three Formations are described as "not strictly valid stratigraphic units", but are a useful means of describing the broad lithological changes across the accretionary wedge. Wandilla Province accretionary rocks. Assumed to consist of a stack of imbricate thrust slices.|||Doonside, Wandilla, Shoalwater, Townshend Formations.|Is faulted against Good Night beds. Equivalent to Broome Head Metamorphics.||
5093|Curtis Island Group|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
5093|Curtis Island Group|71592|5|Briefly described|Appendix A.|||New England Orogen.|270+/-2.9 Ma (metamorphism: U-Pb zircon SHRIMP)||||Pegmatite.|
5093|Curtis Island Group|73450|6|Mentioned|p18, p24|Carboniferous|late Devonian|Previously mapped to include part of the Grevillea Granite.||||Intruded by Hogback Granite.||
5124|Dadamarine Rhyolite|23799|6|Mentioned|p109|||Garnetiferous unit.||||||
5124|Dadamarine Rhyolite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Parent: Aranbanga Volcanic Group.||||||14-AUG-08
5124|Dadamarine Rhyolite|41738|2|Defined|p172|Late Triassic||Reserved as Dadamarine.||||||14-AUG-08
5124|Dadamarine Rhyolite|42054|6|Mentioned|p272|||||||||
5124|Dadamarine Rhyolite|63821|5|Briefly described|p21, p22|||Part of the Aranbanga Volcanic Group. Consists of rhyolitic block and ash flows, pyroclastic base surge deposits and garnet-bearing tuff.||||||07-FEB-11
5124|Dadamarine Rhyolite|68679|5|Briefly described|p437, p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. ~60m thick; in the Mungore Caldera. Quartz-free and garnet-bearing mineralogy, so unrelated to Johngboon Rhyolite; garnet-bearing unit similar to Ooramera Volcanics. Stratigraphic position unknown.||Aranbanga Volcanic Group.||Correlatd with Ooramera Volcanics.|Basal zone of laminated to thinly bedded volcanic sandstone/tuff (surge deposit); rhyolite breccia locally grading into bedded volcanic sandstone with abundant juvenile crystal fragments (feldspar, garnet), interbedded with minor welded ignimbrite.|
5124|Dadamarine Rhyolite|73450|5|Briefly described|p30, p34|||||||Equivalent to Aranbanga Volcanic Group.|Garnet-bearing breccia.|
5129|Dakiel Formation|30451|4|Described|p27|||||||||
5129|Dakiel Formation|31586|5|Briefly described|p6|||Fauna||||||
5129|Dakiel Formation|31587|6|Mentioned|p60|||Lithostrotion species distribution||||||
5129|Dakiel Formation|31659|6|Mentioned|p54|||Part of Caswell Ck. Gp.||||||
5129|Dakiel Formation|32866|6|Mentioned|p25|||Fossil content||||||
5129|Dakiel Formation|32867|6|Mentioned|p60|||||||||
5129|Dakiel Formation|32868|6|Mentioned|p208,Fig.7|||||||||
5129|Dakiel Formation|34155|6|Mentioned|p94||Early Carboniferous|Lower Carboniferous. Caswell Creek Group.||||||20-AUG-09
5129|Dakiel Formation|39445|5|Briefly described|Table 6|||||||||
5129|Dakiel Formation|42547|5|Briefly described|p51|||||||||
5129|Dakiel Formation|44360|2|Defined|p1-4,7,10-12,18,21,||Visean|p23-28,30-33,35,map.Unit of Caswell Creek Group.||||||
5129|Dakiel Formation|44379|14|Not recorded|p15|||Ref. to McKellar 1967.||||||
5129|Dakiel Formation|45097|6|Mentioned|Fig.|||Correlation Chart||||||
5129|Dakiel Formation|46803|6|Mentioned|Fig. 4|||||||||
5129|Dakiel Formation|50190|5|Briefly described|p39, 21, 59|Carboniferous|Carboniferous|Of the Casell Creek Group.||||||
5129|Dakiel Formation|68008|6|Mentioned|p596|||An area N of Cannindah Creek, previously mapped as this unit, has been assigned to Lorray Formation.||||||
5157|Dalrymple Sandstone|12575|5|Briefly described|p781, p784 Table 1.|Late Jurassic|Middle Jurassic|Basal unit of Laura Basin sequence. Apatite fission track analyses, vitrinite reflectance data are detailed. New vitrinite reflectance values of  0.75 and 0.79% indicate the Jurassic section has been considerably hotter after deposition.|178-157 Ma.|||Is overlain by Gilbert River Formation.|Fluvial and deltaic sandstone, mudstone, conglomerate and coal.|08-MAY-12
5157|Dalrymple Sandstone|22780|5|Briefly described|map|Middle Jurassic|Middle Jurassic|||||||
5157|Dalrymple Sandstone|22781|4|Described|p41|Middle Jurassic|Middle Jurassic|Laura Basin||||||
5157|Dalrymple Sandstone|23423|5|Briefly described|p304 table 7.3|||In the Laura Basin.  Underlying unit Normanby Formation (unconformable).||||||
5157|Dalrymple Sandstone|23425|5|Briefly described|Plate 10.2|||||||||
5157|Dalrymple Sandstone|23426|4|Described|p403 + Table 10.4 p407.||Jurassic|Evidence for age is bivalves and possible fish remains. Overlain by Gilbert River Formation - conformable contact. Laura Basin Province.  Max thickness 530 m.||||||17-APR-07
5157|Dalrymple Sandstone|23430|5|Briefly described|p522|||Previously Battle Camp Sandstone. Overlain by Gilbert River Formation - in the Laura Basin. Laura Basin Province.||||||17-APR-07
5157|Dalrymple Sandstone|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
5157|Dalrymple Sandstone|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
5157|Dalrymple Sandstone|24080|5|Briefly described|p445 Fig. 4|Jurassic|Jurassic|Quartzose sandstone and and conglomerate; minor siltstone, mudstone, coal (fluviatile).  Of the Laura Basin sequence.  Max. thickness: 600m.  Geological Province: Laura Basin.||||||
5157|Dalrymple Sandstone|24086|5|Briefly described|p312 Fig. 1|Cretaceous|Jurassic|||||||
5157|Dalrymple Sandstone|24213|5|Briefly described|p776 Fig. 1|Cretaceous|Jurassic|`||||||
5157|Dalrymple Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
5157|Dalrymple Sandstone|31832|6|Mentioned|Table 6|||||||||
5157|Dalrymple Sandstone|32633|5|Briefly described|p439|||||||||
5157|Dalrymple Sandstone|32705|5|Briefly described|p183|||||||||
5157|Dalrymple Sandstone|33529|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? - Late Jurassic||||||
5157|Dalrymple Sandstone|33772|4|Described|p13|||||||||
5157|Dalrymple Sandstone|33773|6|Mentioned|p17|||||||||
5157|Dalrymple Sandstone|34134|6|Mentioned|Cor.Chart|||Lower - Upper Jurassic||||||
5157|Dalrymple Sandstone|35204|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
5157|Dalrymple Sandstone|35220|4|Described|p16|||||||||
5157|Dalrymple Sandstone|35559|4|Described|Table 1|||||||||
5157|Dalrymple Sandstone|35811|6|Mentioned|Fig.3|||||||||
5157|Dalrymple Sandstone|36101|6|Mentioned|p168|||||||||
5157|Dalrymple Sandstone|36228|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
5157|Dalrymple Sandstone|37065|6|Mentioned|p39|||||||||
5157|Dalrymple Sandstone|37115|4|Described|p309|||||||||
5157|Dalrymple Sandstone|37603|6|Mentioned|p444|||||||||
5157|Dalrymple Sandstone|37608|3|Fully described|Table 2|||||||||
5157|Dalrymple Sandstone|39211|6|Mentioned|Fig.26|||||||||
5157|Dalrymple Sandstone|39445|5|Briefly described|Table 10|||||||||
5157|Dalrymple Sandstone|42187|6|Mentioned|Fig.5 P322|||||||||
5157|Dalrymple Sandstone|42256|6|Mentioned|Fig.2 P243|||||||||
5157|Dalrymple Sandstone|42369|4|Described|p56|Middle Jurassic||||||||
5157|Dalrymple Sandstone|42474|6|Mentioned|p28|||Laura Basin||||||
5157|Dalrymple Sandstone|42490|4|Described|p16|||Middle Jurassic||||||
5157|Dalrymple Sandstone|42632|6|Mentioned|p11|||||||||
5157|Dalrymple Sandstone|42637|4|Described|p21|||||||||
5157|Dalrymple Sandstone|42648|5|Briefly described|p42|||||||||
5157|Dalrymple Sandstone|42650|6|Mentioned|p17|||||||||
5157|Dalrymple Sandstone|43070|5|Briefly described|p7|||||||||
5157|Dalrymple Sandstone|43098|4|Described|p47|||||||||
5157|Dalrymple Sandstone|43596|5|Briefly described|p39 Tb. 4, p40|Middle Jurassic|Middle Jurassic|Geological province: Laura Basin. Quartzose sandstone, siltstone, shale. Max. thickness: 400m. Fluvial in origin.||||||27-JAN-09
5157|Dalrymple Sandstone|43738|6|Mentioned|p5|||||||||
5157|Dalrymple Sandstone|43820|5|Briefly described|Map Legend||Jurassic|||||||
5157|Dalrymple Sandstone|43896|14|Not recorded|Map Legend||Jurassic|||||||
5157|Dalrymple Sandstone|43898|14|Not recorded|Map Legend||Jurassic|||||||
5157|Dalrymple Sandstone|43899|14|Not recorded|p274||Jurassic|See also Lexicon.||||||
5157|Dalrymple Sandstone|43979|14|Not recorded|p65-68||Jurassic|||||||
5157|Dalrymple Sandstone|44084|14|Not recorded|p32 (Tb)|Late Jurassic|Early Jurassic|Laura Basin.||||||
5157|Dalrymple Sandstone|44267|14|Not recorded|Map Legend||Jurassic|||||||
5157|Dalrymple Sandstone|44292|2|Defined|p9,11,15,20,22,Tb.1|||Overlapped by Battle Camp Formation.||||||
5157|Dalrymple Sandstone|44293|14|Not recorded|Map Legend||Jurassic|||||||
5157|Dalrymple Sandstone|44294|2|Defined|p6,9,11,13-4,17,19,|||p22,25-27,Tb.2,map||||||
5157|Dalrymple Sandstone|44425|14|Not recorded|p19,opp.11,map|||See also Lexicon.||||||
5157|Dalrymple Sandstone|45025|3|Fully described|p96-97||Jurassic|||||||
5157|Dalrymple Sandstone|45168|6|Mentioned|p10|||||||||
5157|Dalrymple Sandstone|48850|14|Not recorded|Pl.9|||||||||
5157|Dalrymple Sandstone|50587|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Geological Province: Quincan Province, Laura Basin.  Pale grey to white, cross-bedded, quartzose, sublabile and labile sandstone.||||||07-JUL-04
5157|Dalrymple Sandstone|50596|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|Underlies: Gilbert River Formation.  Quartz sandstone, conglomerate, shale and mudstone.||||||
5157|Dalrymple Sandstone|60357|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Geological Province: Laura Basin. Sandstone, minor conglomerate and siltstone.||||||20-AUG-04
5157|Dalrymple Sandstone|60358|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Quartzose to sublabile sandstone; minor conglomeratic sandstone, pebble and cobble conglomerate, siltstone, shale. Geological Province: Laura Basin.||||||18-AUG-04
5157|Dalrymple Sandstone|60425|4|Described|p43 Tb.3, p199|||Unconformable over Normanby Formation. Max.thickness: 120m. Geol.prov: Laura Basin. Non-marine, fluvial sedimentary sequence of quartzose and quartzofeldspathic sandstone, siltstone, mudstone and coal. Hosts an Indicated Resource of 45Mt of coking coal||||||07-FEB-11
5157|Dalrymple Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Late Jurassic|Middle Jurassic|Laura Basin. Hosts coal seams up to 3 m thick in lower strata. High sulphur; coking properties. Resource estimates are poorly constrained; currently (2008) remains unexploited.||||Is overlain by Bathurst Range Coal Measures and Gilbert River Formation.||
5157|Dalrymple Sandstone|67402|5|Briefly described|p165 tbl LPB1, p226-p228, p230-p233|Tithonian|Aalenian|Laura Basin. Deposited in a fluvial or delta plain environment. More than 300m thick. ||||Equivalent to the Eulo Queen Group and the Westbourne Formation.|Quartz to lithic-feldspathic sandstone with subordinate claystone, siltstone, conglomerate and tuff.|
5157|Dalrymple Sandstone|68135|6|Mentioned|p52 fig 2b|Tithonian|Aaelenian|Carpentaria and Laura Basins. Contains plant macrofossils.||||Overlain by Gilbert River Formation|Cross bedded sandstone.|
5157|Dalrymple Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Laura Basin.||||||
5157|Dalrymple Sandstone|69079|6|Mentioned|p16|||Mesozoic gold placer deposits in this unit have been reworked and concentrated in the Palmer River goldfield.||||||
5157|Dalrymple Sandstone|69594|5|Briefly described|p539-540, p573|Middle Jurassic|Middle Jurassic|Laura Basin. Exposed along the E and S margins. Up to 540m thick. Fluvial to lacustrine deposits; contains some marine fossils. Palynomorphs indicate late Early to early Late Jurassic. A productive aquifer. Contains an as-yet uneconomic coking coal deposit, and auriferous deep lead deposits have been reported.||||Is overlain conformably by the Gilbert River Formation. Is equivalent to the Garraway Sandstone, Helby beds, Albany beds, Albany Pass beds, Eulo Queen Group of the Carpentaria Basin.|Basal conglomerate, fine to coarse, sporadically pebbly, quartzose to sublithic and feldspathic sandstone, with minor mudstone and siltstone; coal horizons.|
5157|Dalrymple Sandstone|70207|5|Briefly described|p74, p117|Middle Jurassic|Middle Jurassic|Basal unit of Laura Basin succession.||||Unconformably overlies Hodgkinson Formation.||
5157|Dalrymple Sandstone|70345|6|Mentioned|p3|Jurassic|Jurassic|||||||
5157|Dalrymple Sandstone|70673|6|Mentioned|p7, p100|Middle Jurassic|Middle Jurassic|||||||
5157|Dalrymple Sandstone|72297|5|Briefly described|p700, p748|Jurassic|Jurassic|Laura Basin. Favourable source rock: hydrocarbon indications (patchy oil staining and strong fluorescence) were observed in GSQ  Ebagoola 1, in the upper and lower parts of this unit. Also has potential reservoirs.|||||Contains coal seams up to 3m thick.|
5157|Dalrymple Sandstone|72983|6|Mentioned|p15, p35|Middle Jurassic|Middle Jurassic|Laura Basin.||||Underlain by Hope Vale Granite.||
5157|Dalrymple Sandstone|73083|6|Mentioned|p61|Jurassic|Jurassic|||||||
5228|Darra Formation|31132|6|Mentioned|p150|||Refers Hekel (1972)||||||
5228|Darra Formation|31247|6|Mentioned|p160|||Fauna & flora||||||
5228|Darra Formation|31273|6|Mentioned|p3|||||||||
5228|Darra Formation|31333|6|Mentioned|p14|||||||||
5228|Darra Formation|33368|6|Mentioned|p49|||Correlated with Petrie Fm.||||||
5228|Darra Formation|35053|6|Mentioned|p36|||||||||
5228|Darra Formation|36237|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5228|Darra Formation|36779|6|Mentioned|p8|||||||||
5228|Darra Formation|38074|5|Briefly described|Table 1|||||||||
5228|Darra Formation|38374|6|Mentioned|p607|||||||||
5228|Darra Formation|38441|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
5228|Darra Formation|39445|5|Briefly described|Table 14|||Clay deposits. See also P152||||||
5228|Darra Formation|40623|5|Briefly described|p8|||See also P109||||||
5228|Darra Formation|40982|6|Mentioned|p363|||||||||
5228|Darra Formation|41906|3|Fully described|Table 4 P33|||||||||
5228|Darra Formation|44030|14|Not recorded|p118,131|||Tertiary equivalent.||||||
5228|Darra Formation|44247|14|Not recorded|p9||Paleogene|Parastacid (crayfish) found.||||||07-NOV-08
5228|Darra Formation|44581|14|Not recorded|p348|||||||||
5228|Darra Formation|44677|14|Not recorded|p1|||||||||
5228|Darra Formation|44687|1|Redefined|p224-225|Oligocene|Eocene|Reduced in scope herein, to exclude basalts and sediments (now Corinda Formation) overlying a disconformity and underlying the Sunnybank Formation.||||Overlies Moorooka Formation disconformably, underlies Corinda Formation disconformably.||21-MAR-13
5228|Darra Formation|44703|14|Not recorded|Map|||||||||
5228|Darra Formation|44708|14|Not recorded|p3,12,Sh.1-2,section||Tertiary|Unit of Oxley Group.||||||
5228|Darra Formation|44783|14|Not recorded|p2,16||Eocene|Brisbane district.||||||
5228|Darra Formation|61155|5|Briefly described|p19|Early Eocene|Late Paleocene|Of the Oxley Group.Overlain by Corinda Formation. Age: ~58.5-55Ma. Thickness: ~60m. In the Brisbane region.||||||03-MAR-10
5228|Darra Formation|69599|5|Briefly described|p586, p594-595|Eocene|Eocene|McTaggart (1960); Houston (1965). Oxley Basin. Variable thickness (60-100m) due to pre-existing topography. Fluvial to lacustrine sediments. Contains sporadic plant fossils, vertebrates and bivalves.||Oxley Group.||Is overlain disconformably by Corinda Formation. Correlated with Redbank Plains Formation.|Poorly consolidated sandstone, pebbly conglomerate, siltstone, mudstone and shale.|
5263|Datson Member|22954|4|Described|Fig1p6,17,23-5||Warendan|||||||
5263|Datson Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
5263|Datson Member|37572|4|Described|p162|||||||||
5263|Datson Member|38532|4|Described|p245|||||||||
5263|Datson Member|40127|6|Mentioned|p8|||||||||
5263|Datson Member|40136|6|Mentioned|p23|||||||||
5263|Datson Member|40852|6|Mentioned|Fig.3.7|||||||||
5263|Datson Member|46897|6|Mentioned|Fig.2|||||||||
5263|Datson Member|46958|6|Mentioned|p195|||||||||
5263|Datson Member|50244|6|Mentioned|p89 Fig. 1|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||21-APR-09
5263|Datson Member|64068|4|Described|p74-75|Early Ordovician|Early Ordovician|210 m thick in type section. Fossiliferous. Correlated with Kelly Creek Formation.Conodonts indicate early Early Ordovician (late Warendian Chosonodina herfurthi-Cordylodus angulatus Assemblage Zone; Shergold and Nicoll 1992).||Of Ninmaroo Formation||Conformably overlies Corrie Member. Laterally grades into, and is gradationally overlain by, Swift Formation.|Bioclast (dolo)grainstone, (dolo)boundstone and chert.|21-MAR-16
5263|Datson Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin||Cockroach Group|||Thin-bedded limestone or dolomite with interbedded chert|
5288|Dayboro Tonalite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
5288|Dayboro Tonalite|32610|6|Mentioned|p15|||Refers Houston (1959) P42.||||||
5288|Dayboro Tonalite|33881|6|Mentioned|p95|||Possibility to be quarried||||||
5288|Dayboro Tonalite|35007|6|Mentioned|p74|||||||||
5288|Dayboro Tonalite|35430|6|Mentioned|Fig.2|||Geological map.||||||
5288|Dayboro Tonalite|35866|6|Mentioned|p400|||||||||
5288|Dayboro Tonalite|36238|6|Mentioned|Table 1|||||||||
5288|Dayboro Tonalite|36440|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
5288|Dayboro Tonalite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
5288|Dayboro Tonalite|38074|6|Mentioned|Table 2|||||||||
5288|Dayboro Tonalite|39079|6|Mentioned|p6|||||||||
5288|Dayboro Tonalite|39445|5|Briefly described|Table 12|||||||||
5288|Dayboro Tonalite|40623|5|Briefly described|p55|||||||||
5288|Dayboro Tonalite|42525|5|Briefly described|Map legend|Triassic|Permian|||||||
5288|Dayboro Tonalite|42970|5|Briefly described|Fig.2,p118|||||||||
5288|Dayboro Tonalite|43008|5|Briefly described|map legend|||||||||
5288|Dayboro Tonalite|44671|14|Not recorded|p247|||||||||
5288|Dayboro Tonalite|44911|14|Not recorded|p3-4|||Extends NE from Dayboro. Quartz diorite. Similar to Mount Samson Granodiorite.||||||
5288|Dayboro Tonalite|44912|14|Not recorded|E12-B-7|||||||||
5288|Dayboro Tonalite|68679|5|Briefly described|p409|Middle Triassic|Middle Triassic|Northern New England Orogen. Forms a NW-trending pluton ~35km NW of Brisbane.|237 +/- 7 Ma (Cranfield et al., 1976).||||Coarse-grained pyroxene-biotite tonalite and biotite granodiorite. NNW-trending quartz-feldspar porphyry dykes are late-stage differentiates of the tonalite; ellipsoidal xenoliths are possibly derived from greenstone and volcanic rocks.|
5338|Degilbo Granite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
5338|Degilbo Granite|40475|6|Mentioned|Table 2|||||||||
5338|Degilbo Granite|41778|6|Mentioned|p377|||||||||
5338|Degilbo Granite|41790|5|Briefly described|p471|||||||||
5338|Degilbo Granite|43008|5|Briefly described|map legend|||||||||
5338|Degilbo Granite|61809|4|Described|p455, p457, p463, p463 Fig. 9|Late Triassic|Late Triassic|Geological Province: New England Orogen. Intrudes Gympie Group and metamorphosed it. Medium-grained rock with hypidimorphic granular texture. Major minerals include; plagioclase, K-feldspar, hornblende and biotite.||||||
5338|Degilbo Granite|63821|4|Described|p33|Late Triassic|Late Triassic|Age: 220Ma (K-Ar biotite). Intrudes Good Night beds, undiv. Gympie Group and Mount Marcella Volcanics. Unconformably overlain by Barambah Basalt.||||||07-FEB-11
5338|Degilbo Granite|68679|5|Briefly described|p430|Late Triassic|Late Triassic|Just north of the Mungore Cauldron, northern New England Orogen.|220 Ma (K-Ar biotite: Webb and McDougall, 1967).||||Biotite granite, hornblende-biotite granite, granophyre and porphyritic granodiorite.|
5341|Deighton Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
5341|Deighton Quartzite|30531|6|Mentioned|p17|||Also mention p19 and p20.||||||02-APR-07
5341|Deighton Quartzite|30532|6|Mentioned|p113|||||||||
5341|Deighton Quartzite|30536|6|Mentioned|p100|||Stratigraphy||||||
5341|Deighton Quartzite|32660|4|Described|Table 5|||||||||
5341|Deighton Quartzite|32959|6|Mentioned|Fig.21|||||||||
5341|Deighton Quartzite|33900|5|Briefly described|p18|||Mention p15.||||||02-APR-07
5341|Deighton Quartzite|35074|6|Mentioned|Fig.2|||||||||
5341|Deighton Quartzite|35286|6|Mentioned|Fig.17|||||||||
5341|Deighton Quartzite|36052|6|Mentioned|Fig.2|||||||||
5341|Deighton Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5341|Deighton Quartzite|37568|5|Briefly described|p84|||Of Mount Albert Group.||||||
5341|Deighton Quartzite|38235|6|Mentioned|p115|||||||||
5341|Deighton Quartzite|39124|6|Mentioned|Fig.61|||||||||
5341|Deighton Quartzite|39445|5|Briefly described|Table 2|||See also p43.||||||02-APR-07
5341|Deighton Quartzite|39492|6|Mentioned|p30|||||||||
5341|Deighton Quartzite|39622|6|Mentioned|p26|||See also Fig.2||||||
5341|Deighton Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
5341|Deighton Quartzite|39937|6|Mentioned|Fig.1|||||||||
5341|Deighton Quartzite|40840|6|Mentioned|Map legend|||||||||
5341|Deighton Quartzite|40984|4|Described|p389|||||||||
5341|Deighton Quartzite|41614|6|Mentioned|p145|||||||||
5341|Deighton Quartzite|41615|6|Mentioned|p147|||||||||
5341|Deighton Quartzite|41744|5|Briefly described|p415|||||||||
5341|Deighton Quartzite|42565|6|Mentioned|p2|||||||||
5341|Deighton Quartzite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mount Albert Group.  Feldspathic sandstone.||||||18-JUL-13
5341|Deighton Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5341|Deighton Quartzite|44271|14|Not recorded|p32|||||||||
5341|Deighton Quartzite|44275|14|Not recorded|Map Legend|||||||||
5341|Deighton Quartzite|44276|2|Defined|p12,14,18,Tb.1,map|||||||||
5341|Deighton Quartzite|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5341|Deighton Quartzite|44278|2|Defined|Tb.2,p7,map|||||||||
5341|Deighton Quartzite|44279|14|Not recorded|p8|||||||||
5341|Deighton Quartzite|44788|14|Not recorded|p10|||||||||
5341|Deighton Quartzite|44989|2|Defined|p.96-7|||Tb. III. On many pages. Probably equivalent in age to Surprise Creek Beds. (F54-2,6).||||||
5341|Deighton Quartzite|45136|3|Fully described|p40|||||||||
5341|Deighton Quartzite|45161|6|Mentioned|p26|||||||||
5341|Deighton Quartzite|45166|4|Described|p32|||||||||
5341|Deighton Quartzite|45287|14|Not recorded|p.225-7,229||Paleoproterozoic|Unconformably overlies Corella Formation.||||||07-NOV-08
5341|Deighton Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
5341|Deighton Quartzite|46960|6|Mentioned|p218|||||||||
5341|Deighton Quartzite|46996|6|Mentioned|p273|||||||||
5341|Deighton Quartzite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
5341|Deighton Quartzite|50332|5|Briefly described|p16, p19|Paleoproterozoic|Paleoproterozoic|Overlain by the White Blow Formation. Age: 1755-1740Ma. Age equivalent to the upper Corella Formation. Outcrops in Quamby-Malbon Subprovince.||||||18-JUL-13
5341|Deighton Quartzite|63866|5|Briefly described|p61|||||||Overlies the Corella Formation. Possibly equivalent to the Fiery Creek Volcanics.|Quartzite interbedded with basaltic flows that feature vesicular tops and massive bases.|
5341|Deighton Quartzite|64248|6|Mentioned|p38 Fig.5|||||Unit in Mount Albert Group.||Is overlain by White Blow Formation.||
5341|Deighton Quartzite|64250|6|Mentioned|p13 fig 5, p11 fig 3, p18|||Kalkadoon-Leichhardt Belt, Mount Isa Inlier.||Mount Albert Group||Overlies Corella Formation. Is overlain conformably by White Blow Formation. Shown as equivalent to Knapdale Quartzite.|Feldspathic-, lithic-, and quartz-sandstone.|
5341|Deighton Quartzite|65396|5|Briefly described|p7, p16-17, p82, p84, p175, p182-184|Calymmian|Statherian|See also p190, p241. Kalkadoon-Leichhardt Belt. Has striking similarities with overlying White Blow Formation. Contacts beneath this unit are invariably tectonic, and may represent a thrust surface.||Mount Albert Group||Unconformably overlies Corella Formation. Overlain conformably (locally unconformably) by White Blow Formation. Correlated with Knapdale Quartzite.|Feldspathic-, lithic-, and quartz-sandstone and quartzite.|
5341|Deighton Quartzite|65505|5|Briefly described|966, Fig 2|Proterozoic|Proterozoic|Overlies the Corella Formation. Five sub units: quartz sandstone interbedded with basalt, conglomeratic sandstone, 2 units of medium to fine grained sandstone and an upper, mostly conglomerate unit.||||||
5341|Deighton Quartzite|67323|4|Described|p15, p25, GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Calvert Superbasin. Has been subdivided into five subunits; the (not definitive) maximum depositional ages of the lowest and highest are given (Neumann et al., 2009).|1748 +/- 4 Ma to 1715 +/- 11 Ma.|Mount Albert Group.||Unconformably overlies the Corella Formation. Overlies Fiery Creek Volcanics. Upper part correlated with Gun Supersequence.|Quartzite, feldspathic quartzite, pebble conglomerate.|
5341|Deighton Quartzite|67539|6|Mentioned|p10|||||Of the Mount Albert Group.||||
5341|Deighton Quartzite|68146|5|Briefly described|p3, p199-200|||Mary Kathleen and Marino-Stavely Domains. Contains the Gun Unconformity as shown by these maximum depositional ages for the lower and upper parts of the unit respectively, by Neumann et al. (2009).|1751 +/- 4 Ma to 1715 +/- 11 Ma.|Mount Albert Group.||Correlated with Roxmere and Knapdale Quartzites; also with Torpedo Creek and Warrina Park Quartzites (western succession).||
5341|Deighton Quartzite|68542|6|Mentioned|p13|||||||||
5341|Deighton Quartzite|68576|6|Mentioned|Q_2: p13|||||||||
5341|Deighton Quartzite|68732|5|Briefly described|p161, p165 Fig.3, p167, p168 Fig.5|Statherian|Statherian|Contains braided fluvial cross-stratified quartzites and pebbly quartzites in units 1, 2, and 5. Maximum sedimentary depositional ages. Correlated with the Prize and Big supersequences.|1715 +/- 11, 1749 +/- 5, 1747 +/- 4 Ma||||Includes cross-stratified quartzites and pebbly quartzites, and fine- to coarse-grained quartzites and arenites fining upwards into thinly bedded sandstones.|30-NOV-17
5341|Deighton Quartzite|69056|5|Briefly described|Time-Space plot sheet|Statherian|Statherian|Also appears as Deighton Formation on Time-Space plot sheet.||Lower Mount Albert Group.||||
5341|Deighton Quartzite|69591|4|Described|p38 Fig.2.22, p39, p45, p56|||Kalkadoon-Leichhardt (and ?Mary Kathleen) Domain, Calvert Superbasin. Presented as Lower Deighton Quartzite and Upper Deighton Quartzite in Fig.2.22, apparently separated by mid-Calvert inversion. Divided into 5 informal subunits (Wilson et al., 1977). Large shallow-marine sandstone bodies. Age of basal sandstone unit; the topmost unit has an MDA of 1715 +/- 11 Ma (given as 1690 +/- 32 Ma on p56) and is part of the Gun Supersequence (both ages by Neumann et al., 2009).|1747 +/- 4 Ma (maximum depositional age).|Mount Albert Group.||Correlates with Fiery Creek Volcanics and Prize Supersequence.|Quartzite, feldspathic quartzite, pebble conglomerate, interbedded with basalt.|
5341|Deighton Quartzite|71592|5|Briefly described|Appendix A.|||Mary Kathleen Domain, Mount Isa Orogen.|1715+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite, sandstone.|
5341|Deighton Quartzite|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP ages of 1751 +/- 4 Ma, 1748 +/- 3 Ma, and 1690 +/- 32 Ma reported by Neumann et al. (2009).|1751 +/- 4 Ma, 1748 +/- 3 Ma, 1690 +/- 32 Ma|||||
5341|Deighton Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Kalkadoon-Leichhardt Domain.|1715+/-11 Ma maximum depositional age||||Siliciclastics.|
5341|Deighton Quartzite|73529|5|Briefly described|p5|Statherian|Statherian|Calvert Superbasin, early. Shallow marine setting.|1715+/-11 Ma maximum depostional age|Mount Albert Group||||
5341|Deighton Quartzite|73553|5|Briefly described|p8 Fig.1.2.3, p187|Statherian|Statherian||1749+/-5 Ma, 1747+/-4 Ma, 1715+/-11 Ma MDA|Mount Albert Group||||
5344|Delaney Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Forsayth Supersuite. Geological Province: Georgetown Region.||||||27-MAY-15
5344|Delaney Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 820. S-Type.||||||
5344|Delaney Granite|34883|6|Mentioned|p85|||||||||
5344|Delaney Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
5344|Delaney Granite|36216|6|Mentioned|p208|||||||||
5344|Delaney Granite|37570|4|Described|p119|||||||||
5344|Delaney Granite|38366|6|Mentioned|p34|||||||||
5344|Delaney Granite|39687|6|Mentioned|p3|||||||||
5344|Delaney Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5344|Delaney Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
5344|Delaney Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
5344|Delaney Granite|50199|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
5344|Delaney Granite|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Part of the Forsayth Batholith.  Age: 1550-1560Ma.||||||17-MAY-04
5344|Delaney Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Porphyritic muscovite-biotite granite.||||||01-JUL-04
5344|Delaney Granite|63866|5|Briefly described|p77|||||Forsayth Supersuite||||
5344|Delaney Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Pale to dark grey, locally foliated, medium-grained, mostly porphyritic muscovite-biotite granite with 10-15 mm tabular K-feldspar phenocrysts.|
5344|Delaney Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Pale to dark grey, locally foliated, medium-grained, mostly porphyritic muscovite-biotite granite with 1-1.5 cm tabular K-feldspar phenocrysts.|
5344|Delaney Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Pale to dark grey, locally foliated, medium-grained, mostly porphyritic muscovite-biotite granite with 1-1.5 cm tabular K-feldspar phenocrysts.|
5344|Delaney Granite|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Forsayth Batholith. Of the Etheridge Province. Shown to occur during D2 (~ 1550-1560 Ma).|~ 1560-1550 Ma||||Pale to dark grey locally foliated medium-grained, mostly porphyritic muscovite-biotite granite with 1-1.5 cm tabular K-feldspar phenocrysts.|
5344|Delaney Granite|68576|5|Briefly described|Q_11: p24-25, p28|Mesoproterozoic|Mesoproterozoic|Georgetown area. Part of Forsayth Batholith.||||Intrudes Forsayth Granite.|Pale grey, medium-grained muscovite-biotite granite containing very small K-feldspar phenocrysts.|
5344|Delaney Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith.||Forsayth Supersuite.|||Irregular, equigranular to porphyritic granite plutons (as well as veins and dykes) with small phenocrysts.|
5344|Delaney Granite|73527|6|Mentioned|p2, p3 Fig.2, p8 Fig.6|||Georgetown Inlier, central domain.||Forsayth Supersuite||||
5344|Delaney Granite|75079|5|Briefly described|p3, 6, 9-13, 16, 18|Mesoproterozoic|Mesoproterozoic|Central domain, Georgetown Inlier. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|~1550 Ma.|Forsayth Supersuite.|||Foliated biotite-bearing granite with mafic xenoliths.|
5439|Devoncourt Limestone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, calcilutite, marl. Underlies Selwyn Range Limestone, O'Hara Shale. Overlies Roaring Siltstone.||||||30-JAN-07
5439|Devoncourt Limestone|22954|6|Mentioned|Fig3p9|||||||||
5439|Devoncourt Limestone|23182|6|Mentioned|p232|||||||||
5439|Devoncourt Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
5439|Devoncourt Limestone|30773|6|Mentioned|p266|||Middle Cambrian age||||||
5439|Devoncourt Limestone|30775|6|Mentioned|p1|||||||||
5439|Devoncourt Limestone|30778|6|Mentioned|p14,Fig.5|||||||||
5439|Devoncourt Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|31396|6|Mentioned|Fig.3|||||||||
5439|Devoncourt Limestone|32952|6|Mentioned|p1188|||See also p1189. M.-U. Cambrian||||||08-AUG-06
5439|Devoncourt Limestone|33111|4|Described|p35|||||||||
5439|Devoncourt Limestone|33113|6|Mentioned|Fig.1|||Middle Camb.||||||
5439|Devoncourt Limestone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
5439|Devoncourt Limestone|34287|6|Mentioned|Fig.3|||||||||
5439|Devoncourt Limestone|34903|6|Mentioned|p582|||||||||
5439|Devoncourt Limestone|35054|6|Mentioned|Table 23|||||||||
5439|Devoncourt Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5439|Devoncourt Limestone|35139|4|Described|Table.2|||||||||
5439|Devoncourt Limestone|35553|6|Mentioned|p18|||||||||
5439|Devoncourt Limestone|35939|6|Mentioned|p633|||||||||
5439|Devoncourt Limestone|37275|6|Mentioned|p290|||||||||
5439|Devoncourt Limestone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|37572|4|Described|p159|||See also Fig.8||||||
5439|Devoncourt Limestone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5439|Devoncourt Limestone|38444|6|Mentioned|p139|||||||||
5439|Devoncourt Limestone|38446|6|Mentioned|Table 23|||||||||
5439|Devoncourt Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||08-AUG-06
5439|Devoncourt Limestone|39690|6|Mentioned|Table 1|||See also Fig.2||||||
5439|Devoncourt Limestone|40856|5|Briefly described|p313|||||||||
5439|Devoncourt Limestone|41388|6|Mentioned|Fig.2|||||||||
5439|Devoncourt Limestone|41639|6|Mentioned|p3|||||||||
5439|Devoncourt Limestone|42139|6|Mentioned|Fig.18 P90|||||||||
5439|Devoncourt Limestone|42994|6|Mentioned|p3|||||||||
5439|Devoncourt Limestone|43807|6|Mentioned|Fig.2,p347|||||||||
5439|Devoncourt Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
5439|Devoncourt Limestone|44091|14|Not recorded|Tb.1,p1||Middle Cambrian|||||||
5439|Devoncourt Limestone|44205|2|Defined|p5,9-17,21-59,65-95,||Middle Cambrian|p107,134,141,161,170-184.||||||
5439|Devoncourt Limestone|44211|2|Defined|p96,100-104|||Overlies sharp but conformable contact on Roaring Siltstone. Overlain by Selwyn Range Limestone.||||||
5439|Devoncourt Limestone|44275|14|Not recorded|Map Legend|||||||||
5439|Devoncourt Limestone|44276|2|Defined|p20,21,Tb.2|||||||||
5439|Devoncourt Limestone|44882|14|Not recorded|p201||Cambrian|Selwyn Range. In French.||||||
5439|Devoncourt Limestone|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
5439|Devoncourt Limestone|45002|14|Not recorded|p16,21,24|||||||||
5439|Devoncourt Limestone|45012|14|Not recorded|p8,91,127||Middle Cambrian|||||||
5439|Devoncourt Limestone|45052|3|Fully described|p102|||M.Camb.||||||
5439|Devoncourt Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
5439|Devoncourt Limestone|45166|5|Briefly described|Table 15|||||||||
5439|Devoncourt Limestone|47058|6|Mentioned|p134|||||||||
5439|Devoncourt Limestone|48633|14|Not recorded|p96|||Ref. to Opik 1961.||||||
5439|Devoncourt Limestone|48906|14|Not recorded|Tb.1|||||||||
5439|Devoncourt Limestone|48971|6|Mentioned|p9|||See also P11, P30.||||||
5439|Devoncourt Limestone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Hard, flaggy, medium-bedded to laminated, and essentially detrital; trilobite fossils locally.  Conformably overlies the Roaring Siltstone; conformably overlain by Selwyn Range Limestone and O'Hara Shale. ||||||
5439|Devoncourt Limestone|50244|6|Mentioned|p88, p95, p99|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.||||||21-APR-09
5439|Devoncourt Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, marl, calcilutite.||||||
5439|Devoncourt Limestone|62790|6|Mentioned|p208, 216|Middle Cambrian|Middle Cambrian|Eastern Georgina Basin. Contains the comptalutid Aristaluta gutta Opik, 1961.||||||28-MAR-12
5439|Devoncourt Limestone|63450|5|Briefly described|p78 Fig. 5, p81|Middle Cambrian|Middle Cambrian|Overlies Inca Formation (with hiatus). Conformably overlain by Pomegranate Limestone. Geological province: Georgina Basin, Burke River Structural Belt. Max. thickness (est.): 210m. Bituminous, flaggy limestone.||||||07-FEB-11
5439|Devoncourt Limestone|64068|3|Fully described|p64, 62, 63, 67, 70|Middle Cambrian|Middle Cambrian|Diverse fossil fauna. Correlated with Georgina Limestone, upper Arthur Creek Formation, lower part with Blazan Shale, Quita Formation. Part correlated with Roaring Siltstone. Previously mapped as Thorntonia Limestone (Opik, 1963; Shergold and Druce, 1980).||Of Narpa Group.||Conformably overlies Inca Formation and Roaring Siltstone. Conformably and gradationally overlain by Selwyn Range Limestone and O'Hara Shale.|Interbedded  limestones: laminated, marly, foetid, and nodular; calcareous shale; minor intraformational breccia.|04-APR-12
5439|Devoncourt Limestone|64443|6|Mentioned|p41|||Correlative of Ranken Limestone, Camooweal Dolostone.||||||
5439|Devoncourt Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin. Appears as Devencourt Limestone on p83.||Narpa Group.||Overlies Roaring Siltstone conformably and Inca Formation unconformably. Is overlain by Pomegranate Limestone and Selwyn Range Limestone.|Impure limestone, calcilutite, bituminous limestone, marl.|
5439|Devoncourt Limestone|67870|5|Briefly described|p39, p43, p47, p50-53|||Burke River Structural Belt, Georgina Basin.||||Equivalent to the Arthur Creek Formation.||
5439|Devoncourt Limestone|69443|5|Briefly described|p28:16, 24-25|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Ranken Limestone and Camooweal Dolostone.||12-JUL-16
5439|Devoncourt Limestone|69573|6|Mentioned|p659, 661, 666, 668|||Georgina Basin. Intertidal to subtidal environment.||||Passes laterally and vertically (downwards) into Roaring Siltstone.||
5439|Devoncourt Limestone|69591|5|Briefly described|p87, p92-93, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Up to 215m thick. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Has a rich trilobite fauna of the Lejopyge laevigata Zone. Mis-spelt on p87 as Devencourt Limestone.||||Overlies Roaring Siltstone conformably (and passes laterally into it) and, unconformably, Inca Formation. Is overlain by Pomegranate Limestone and locally Selwyn Range Limestone.|Flaggy, thin-bedded limestones including sandy, bituminous and nodular types with the last leaving large thick ellipsoidal nodules up to 25cm in diameter upon weathering. Some fine cross-bedding and a few thin intraformational breccias occur.|
5439|Devoncourt Limestone|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Burke River Structural Belt, Georgina Basin.  Australian stages:  Undillan to Boomerangian.||of Narpa Group.||||
5439|Devoncourt Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation and the Steamboat Sandstone.||03-JUN-21
5439|Devoncourt Limestone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Roaring Siltstone and underlies Selwyn Limestone.|Impure limestone, calcilutite, bituminous limestone and marl.|
5439|Devoncourt Limestone|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Overlies Roaring Siltstone and underlies  Selwyn Range Limestone.|Impure limestone, calcilutite, bituminous limestone and marl.|
5439|Devoncourt Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Overlies Inca Formation, Roaring Siltstone, underlies Selwyn Range Limestone|Limestone.|
5458|Dicey Dolerite|41425|6|Mentioned|p67|||||||||
5458|Dicey Dolerite|41740|6|Mentioned|p222|||||||||
5473|Digby Peaks Breccia|22954|5|Briefly described|Fig1p6,24|Tertiary|Ordovician|||||||
5473|Digby Peaks Breccia|38532|4|Described|Fig.4|||||||||
5473|Digby Peaks Breccia|44362|4|Described|p11,Tb.1|||Post Early Ordovician.||||||
5473|Digby Peaks Breccia|46958|6|Mentioned|Fig.2|||||||||
5473|Digby Peaks Breccia|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|||Georgina Basin. Age: Ordovician?||Cravens Peak beds|||Silicified ferruginous chert and breccia|
5474|Digger Creek Granite|9539|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|White, grey and pink aplitic to pegmatitic muscovite leucogranite.||||||19-JUN-13
5474|Digger Creek Granite|9541|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Muscovite leucogranite pegmatite and aplite.  Intrudes Robertson River Metamorphics.||||||07-JUL-04
5474|Digger Creek Granite|22676|6|Mentioned|p302|||||||||
5474|Digger Creek Granite|23032|5|Briefly described|p12|Proterozoic|Proterozoic|||||||
5474|Digger Creek Granite|23220|5|Briefly described|Fig.2, p11||Mesoproterozoic|Intrudes the Roberston River Formation and Einasleigh Metamorphics and is intruded by the Robin Hood Granodiorite. Age: U-Pb Zircon SHRIMP 1554 +/- 10Ma.||||||
5474|Digger Creek Granite|23291|5|Briefly described|p31, p88 Tb. 3.7, plate 3.2f|Mesoproterozoic|Mesoproterozoic|Probably of Forsayth Supersuite. Geological Province: Georgetown Region.||||||27-MAY-15
5474|Digger Creek Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 817. S and I-Types.||||||15-JAN-07
5474|Digger Creek Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Parts of this granite are of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
5474|Digger Creek Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5474|Digger Creek Granite|32531|6|Mentioned|p477|||||||||
5474|Digger Creek Granite|33907|6|Mentioned|p5|||||||||
5474|Digger Creek Granite|33909|2|Defined|p229|Mesoproterozoic|Mesoproterozoic|||||||
5474|Digger Creek Granite|35214|6|Mentioned|p7|||||||||
5474|Digger Creek Granite|35920|6|Mentioned|p24|||||||||
5474|Digger Creek Granite|35948|6|Mentioned|Table 1|||Rb-Sr isotopic composition.||||||
5474|Digger Creek Granite|37570|4|Described|p121|||See also p119.||||||15-JAN-07
5474|Digger Creek Granite|37571|6|Mentioned|p133|||||||||
5474|Digger Creek Granite|37576|5|Briefly described|p8|||||||||
5474|Digger Creek Granite|39445|5|Briefly described|Table 2|||See also p45.||||||15-JAN-07
5474|Digger Creek Granite|39687|6|Mentioned|p3|||||||||
5474|Digger Creek Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5474|Digger Creek Granite|39981|6|Mentioned|p102|||||||||
5474|Digger Creek Granite|41272|5|Briefly described|M 1of1 B06|||||||||
5474|Digger Creek Granite|41680|6|Mentioned|p104|||||||||
5474|Digger Creek Granite|43259|4|Described|Appendix 1,p53.|Devonian|Silurian|Middle Proterozoic.||||||03-DEC-13
5474|Digger Creek Granite|43664|6|Mentioned|p67|||||||||
5474|Digger Creek Granite|43793|5|Briefly described|p333|||U-Pb age: 1554+/-10 Ma||||||
5474|Digger Creek Granite|45113|6|Mentioned|p7|||Also mentioned p33.||||||15-JAN-07
5474|Digger Creek Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
5474|Digger Creek Granite|50199|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5474|Digger Creek Granite|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1550-1560Ma.||||||17-MAY-04
5474|Digger Creek Granite|50211|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Medium- to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.  Age: 1550-1560 Ma.||||||19-JUN-13
5474|Digger Creek Granite|50537|5|Briefly described|p1.4, 2.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite. Age: 1554 +/- 10Ma (SHRIMP).||||||08-SEP-14
5474|Digger Creek Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Pegmatitic muscovite leucogranite.||||||01-JUL-04
5474|Digger Creek Granite|61258|6|Mentioned|p389|Mesoproterozoic|Mesoproterozoic|Age: 1554+/-10Ma (Black and Withnall 1993).||||||
5474|Digger Creek Granite|63866|4|Described|p77|Calymmian|Calymmian|Numeric age is a U-Pb zircon TIMS date.|1554 +/- 10 Ma (Black, OZCHRON)|Forsayth Supersuite|||Coarse pink garnetiferous muscovite granite.|
5474|Digger Creek Granite|66800|6|Mentioned|p926.||||1554 +/- 10 Ma (Black & Withnall 1993).|||||
5474|Digger Creek Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Medium- to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.|
5474|Digger Creek Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Medium- to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.|
5474|Digger Creek Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Medium- to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.|
5474|Digger Creek Granite|68357|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Medium- to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.|
5474|Digger Creek Granite|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Etheridge Province. Shown to occur during D2 (~ 1550-1560 Ma).|~ 1560-1550 Ma||||Medium-grained to coarse-grained or pegmatitic muscovite leucogranite and muscovite pegmatite.|
5474|Digger Creek Granite|69591|6|Mentioned|p83|||Georgetown Inlier. Probably part of the Forsayth Supersuite.||||||
5474|Digger Creek Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1554+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
5474|Digger Creek Granite|73527|6|Mentioned|p2|||Georgetown Inlier, central domain.||Forsayth Supersuite||||
5474|Digger Creek Granite|73642|5|Briefly described|p4 Tb.1, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier.|1554+/-20 Ma|Forsayth Supersuite||||
5474|Digger Creek Granite|75079|6|Mentioned|p3, 6, 9-12|Mesoproterozoic|Mesoproterozoic|Northeast Queensland. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|1550 Ma.|Forsayth Supersuite.||||
5514|Dinner Creek Conglomerate|23037|6|Mentioned|Fig 3||Late Permian|||||||
5514|Dinner Creek Conglomerate|24076|5|Briefly described|p397 Fig. 2|Late Permian|Late Permian|Max. thickness: 1100m.  Geological Province: Yarrol Basin.||||||
5514|Dinner Creek Conglomerate|24491|5|Briefly described|p14|Late Permian|Late Permian|||||||
5514|Dinner Creek Conglomerate|24615|5|Briefly described|CD|Permian|Permian|[Pd].  Conglomerate, lithic sandstone and carbonaceous mudstone.||||||
5514|Dinner Creek Conglomerate|30914|6|Mentioned|Map legend|Permian|Permian|||||||
5514|Dinner Creek Conglomerate|31657|4|Described|p95|||See also P101. Disconformable on Rookwood Volcs.||||||
5514|Dinner Creek Conglomerate|31658|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
5514|Dinner Creek Conglomerate|31659|4|Described|p68-69|Late Permian|Late Permian|Originally named Dinner Creek Beds by Dunstan (1901a). Max. thickness: 3500ft. Conglomerate, lithic sandstone, mudstone. See also Table 1.||||||09-JUN-09
5514|Dinner Creek Conglomerate|32141|6|Mentioned|p154|||Permian||||||
5514|Dinner Creek Conglomerate|32358|4|Described|Table 2|||P15||||||
5514|Dinner Creek Conglomerate|35069|6|Mentioned|Fig.1|||||||||
5514|Dinner Creek Conglomerate|37565|6|Mentioned|Fig.8|||||||||
5514|Dinner Creek Conglomerate|37860|6|Mentioned|Fig.2|||||||||
5514|Dinner Creek Conglomerate|38081|5|Briefly described|Table 1|||||||||
5514|Dinner Creek Conglomerate|38095|5|Briefly described|Table 5|||||||||
5514|Dinner Creek Conglomerate|38406|6|Mentioned|p12|||||||||
5514|Dinner Creek Conglomerate|39252|5|Briefly described|p27|||See also Fig.15||||||
5514|Dinner Creek Conglomerate|39445|5|Briefly described|Table 8|||See also Table 9||||||
5514|Dinner Creek Conglomerate|40623|5|Briefly described|p110|||||||||
5514|Dinner Creek Conglomerate|41246|6|Mentioned|Map legend|Permian||||||||
5514|Dinner Creek Conglomerate|41576|4|Described|p18|||See also Table 1||||||
5514|Dinner Creek Conglomerate|41577|6|Mentioned|Map legend|Late Permian||||||||
5514|Dinner Creek Conglomerate|41922|4|Described|Table 1, P9|||||||||
5514|Dinner Creek Conglomerate|42547|5|Briefly described|p49, p52|||||||||
5514|Dinner Creek Conglomerate|43017|6|Mentioned|p379|||||||||
5514|Dinner Creek Conglomerate|43992|14|Not recorded|p192|Early Permian|Late Carboniferous|Stanwell area.||||||
5514|Dinner Creek Conglomerate|44360|14|Not recorded|p30||Permian|||||||
5514|Dinner Creek Conglomerate|44379|14|Not recorded|p18|||||||||
5514|Dinner Creek Conglomerate|44388|2|Defined|p113,114||Permian|||||||
5514|Dinner Creek Conglomerate|50209|5|Briefly described|Map Legend|Permian|Permian|Overlies: Moah Creek beds.||||||
5514|Dinner Creek Conglomerate|50317|5|Briefly described|Map Legend|Permian|Permian|Conglomerate, lithic sandstone, mudstone.||||||09-JUN-04
5514|Dinner Creek Conglomerate|60557|5|Briefly described|p19 Fig. 5b, p26|Late Permian|Late Permian|Consists mainly of monomictic cobble conglomerate and minor interbeds of sandstone and mudstone.  Overlies the Moah Creek beds; unconformably overlain by Native Cat Andesite.  Geological Province: Bowen Basin.||||||09-JUN-05
5514|Dinner Creek Conglomerate|61782|6|Mentioned|p282|||Underlies Native Cat Conglomerate.||||||
5514|Dinner Creek Conglomerate|63832|6|Mentioned|p131 fig 2|Lopingian|Guadalupian|Of east Bowen Basin.||||||
5514|Dinner Creek Conglomerate|64631|6|Mentioned|p44 Fig.2.|Lopingian|Guadalupian|Eastern Bowen Basin or northern New England Fold Belt?||||Overlies Moah Creek Beds.||
5514|Dinner Creek Conglomerate|65388|6|Mentioned|p48 Fig. 18, p58,  174 Fig 65|Permian|Permian|Grantleigh Subprovince, Yarrol Province? Overlies Moah Creek beds.||||||
5514|Dinner Creek Conglomerate|68008|3|Fully described|p123, p132, p179-182, p190, p254, p257|Permian|Permian|See also p261, p483, p485. Fleming (1960, 1967) designated a type section along a line between the summits of Mount Lion and Native Cat. Name derived from Dinner Creek, a tributary of Lion Creek. Stanwell area. Alluvial fan deposits marginal to a freshwater lake. 1050m thick. Contains Glossopteris fossils: Late Permian. Is overlain unconformably by Native Cat Andesite, Dalma Basalt and Mount Salmon Volcanics.||||Overlies Moah Creek beds. Disconformably overlies Lorray Formation and Rockhampton Group, and Youlambie Conglomerate (or unconformably). See Comments.|Grey or brown, massive-bedded cobble conglomerate, with lenticular interbeds of lithic sandstone and carbonaceous mudstone.|
5514|Dinner Creek Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||||
5514|Dinner Creek Conglomerate|68679|5|Briefly described|p312-313, p338, p346|Permian|Permian|Dunstan (1901); Fleming (1967). Occurs on the flanks of Mount Candlelight Syncline, northern New England Orogen. High-energy alluvial deposits. Plant fossils indicate late Permian.||||Overlies Moah Creek beds.|Massive beds of conglomerate with mainly well-rounded, ellipsoidal, imbricated cobbles (almost wholly silicified sandstone) in a sandy matrix; lenticular interbeds of lithic sandstone and carbonaceous mudstone.|
5534|Dismal Creek Dacite|23291|4|Described|p42, 48, p91 Tb. 3.9|Carboniferous|Carboniferous|Included in the Cumberland Range Volcanic Group for ease of description. Thickness: 170m. Geological Province: Georgetown Region.||||||30-JUN-15
5534|Dismal Creek Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V9. Assumed to be I-Type.||||||
5534|Dismal Creek Dacite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
5534|Dismal Creek Dacite|40860|6|Mentioned|Fig.1|||||||||
5534|Dismal Creek Dacite|43259|4|Described|Appendix 1,p1.||Carboniferous|||||||
5534|Dismal Creek Dacite|43740|4|Described|p20|||||||||
5534|Dismal Creek Dacite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of the Cumberland Range Volcanic Group.||||||
5534|Dismal Creek Dacite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron.||Unit in Cumberland Range Volcanic Group.|Includes Huonfels Rhyolite Member.||Greyish-green, crystal-rich dacitic to rhyolitic ignimbrite; local rhyolite and altered rhyolitic breccia with minor interbedded sandstone and siltstone.|
5547|Djuan Tonalite|23799|3|Fully described|p90, p11 Tb. 1|Triassic|Permian|Grey to dark tonalite, common xenoliths, hornblendite.  Unconformably overlain by Tarong beds and Main Range Volcanics.  Intrudes Sugarloaf Metamorphics and Maronghi Creek Beds.  Geolological Province: Yarraman Subprovince.||||||
5547|Djuan Tonalite|23800|5|Briefly described|Map Legend|Triassic|Triassic|||||||
5547|Djuan Tonalite|24560|5|Briefly described|Map legend|Triassic|Triassic|Of Cressbrook Creek Group.   Grey to dark grey tonalite (common xenoliths); hornblendite.||||||
5547|Djuan Tonalite|30303|2|Defined|p323|Early Triassic|Early Triassic|K/Ar dating 230m.y.||||||
5547|Djuan Tonalite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
5547|Djuan Tonalite|35161|6|Mentioned|p591|||||||||
5547|Djuan Tonalite|36954|6|Mentioned|Fig.1|||||||||
5547|Djuan Tonalite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
5547|Djuan Tonalite|39445|5|Briefly described|Table 12|||||||||
5547|Djuan Tonalite|40245|6|Mentioned|p185|||||||||
5547|Djuan Tonalite|42525|5|Briefly described|Map legend|Triassic|Permian|||||||
5547|Djuan Tonalite|43008|5|Briefly described|map legend|||||||||
5547|Djuan Tonalite|61781|6|Mentioned|p271|||||||||
5547|Djuan Tonalite|68679|5|Briefly described|p323, p411-416|Triassic|Permian|West of the Esk Basin, northern New England Orogen. Just N of the Eskdale Igneous Complex. Two other, significantly older, ages given. Has lower Na2O and K2O and higher CaO. Geochemical plot.|234.8 +/- 8 Ma (K-Ar: Cranfield et al., 1976).|||Intrudes Sugarloaf Metamorphics. Is bounded to the N by Woolshed Mountain and Kenewah Granodiorites.|Xenolithic tonalite; prominent foliation.|
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||||
5619|Doomadgee Formation|22453|6|Mentioned|p 12|||In the McArthur Basin.||||||15-MAR-07
5619|Doomadgee Formation|22665|5|Briefly described|Table1, p229||Statherian|Age of unit is 1613+/-5 Ma U/Pb SHRIMP.||||||16-MAR-18
5619|Doomadgee Formation|22673|6|Mentioned|63,78|||Geol province: Mount Isa Basin.||||||09-AUG-06
5619|Doomadgee Formation|22680|6|Mentioned|84,85,87|||Geol province Mount Isa Basin. Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|23065|6|Mentioned|16|||Geol province: Lawn Hill Subprovince. Parent Fickling Group. Age: 1613 +/- 5 Ma.||||||09-AUG-06
5619|Doomadgee Formation|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
5619|Doomadgee Formation|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|23397|5|Briefly described|p466|Statherian|Statherian|Age: 1613+/-3Ma.||||||09-AUG-06
5619|Doomadgee Formation|23398|4|Described|p446|Statherian|Statherian|Age: 1619+/-5Ma U/Pb SHRIMP.||||||16-MAR-18
5619|Doomadgee Formation|23405|4|Described|p566|Statherian|Statherian|Of Fickling Group. Age: 1619+/-5Ma.||||||09-AUG-06
5619|Doomadgee Formation|23406|4|Described|p609 Fig. 9, p615|Statherian|Statherian|In Walford Creek area, consists mainly of dolarenite and and dolomitic sst grading up into laminated very fine-grained sandstone and siltstone; flaggy, micaceous, fine- to medium-gr. sst and pebble conglom. beds occasionally present. Age: 1619+/-5Ma.||||||16-JUN-09
5619|Doomadgee Formation|23407|5|Briefly described|p632|||||||||
5619|Doomadgee Formation|23409|5|Briefly described|p556|||Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
5619|Doomadgee Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: c.1613 Ma. Geological Province: Lawn Hill Platform.||||||
5619|Doomadgee Formation|24442|5|Briefly described|p22 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Fickling Group (upper part).  Geological Province: McArthur Basin.||||||
5619|Doomadgee Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|36012|3|Fully described|Table 3|||See also p16.||||||09-AUG-06
5619|Doomadgee Formation|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||09-AUG-06
5619|Doomadgee Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|38237|6|Mentioned|p130|||||||||
5619|Doomadgee Formation|38348|6|Mentioned|p18|||||||||
5619|Doomadgee Formation|38584|4|Described|p17|||||||||
5619|Doomadgee Formation|39445|5|Briefly described|Table 2|||See also p39.||||||09-AUG-06
5619|Doomadgee Formation|39497|6|Mentioned|Fig.4|||||||||
5619|Doomadgee Formation|39685|6|Mentioned|p407|||||||||
5619|Doomadgee Formation|39925|6|Mentioned|p333|||||||||
5619|Doomadgee Formation|41721|4|Described|p28|||||||||
5619|Doomadgee Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
5619|Doomadgee Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of Fickling Group. Of "Mid Proterozoic" age.||||||
5619|Doomadgee Formation|45162|6|Mentioned|p146|||||||||
5619|Doomadgee Formation|45166|5|Briefly described|p30|||||||||
5619|Doomadgee Formation|49001|2|Defined|p11|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Underlain by Mount Les Siltstone.||||||03-JUN-09
5619|Doomadgee Formation|61936|5|Briefly described|p194 Fig. 6|||Age: >1600Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||15-MAR-07
5619|Doomadgee Formation|62659|5|Briefly described|Map Legend|Calymmian|Statherian|Grey and green carbonaceous shale, flaggy reddish brown to maroon, dolomitic, micaceous, fine grained sandstone and siltstone; minor sandstone, dololutite, dolarenite, breccia.||||||
5619|Doomadgee Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of shale.||||||30-SEP-08
5619|Doomadgee Formation|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Seems to be part of Term, Lawn, Wide and Doom supersequences.||||Overlies Lawn Hill Formation. Is overlain by Widallion Sandstone.||
5619|Doomadgee Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
5619|Doomadgee Formation|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
5619|Doomadgee Formation|65228|5|Briefly described|pp35-36|Statherian|Statherian|Lower part of this unit constitutes Term Supersequence in the northern Lawn Hill Platform. It extends through the Lawn Supersequence (where it is dated 1613 +/- 5 Ma) into the Wide Supesequence. Shore-face and inner ramp facies.|1619 +/- 5 Ma (Page et al. 2000).|||||
5619|Doomadgee Formation|65337|4|Described|p9 Fig.5, p22 Table 4, pp31-32.|Mesoproterozoic|Paleoproterozoic|Northeast MOUNT DRUMMOND area. 200 - 250 m of marine shelf deposits. Time-equivalent to Lawn Hill Formation.|>1613 +/- 5 Ma to 1595 +/- 6 Ma.|Unit in Fickling Group.||Overlies Mount Les Siltstone. Is disconformably, locally unconformably, overlain by South Nicholson Group.|Coarsening-up shale, through flaggy maroon, dolomitic, micaceous, fine-grained sandstone and siltstone, to pale sublithic fine to coarse sandstones; dolostones, minor dolomitic sandstone and intraclast breccia; carbonaceous shale and siltstone.|
5619|Doomadgee Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin. Informally subdivided into 3 units. Shown as Lower and Upper Doomadgee Formation in both Time-Space Plots.|1613 +/- 5 Ma (maximum depositional age).|Fickling Group.|||Reddish fine to coarse sandstone; conglomerate beds at base. Dark grey fissile shale and siltstone with flaggy claystone interbeds. Grey and brown, laminated fine sandstone; dolomite, dolomitic sandstone and conglomerate.|
5619|Doomadgee Formation|68146|4|Described|p2, p6, p41-50, p196, p198, p211|||South Nicholson Region. This age is within error of two previous determinations from tuffs (c.1613 Ma and c.1619 Ma). Whole-rock Sm-Nd isotopic data tabulated.|1632 +/- 14 Ma maximum deposition age.|Uppermost Fickling Group.||Is overlain unconformably by South Nicholson Group.|Includes a 75-100mm thick bed of green tuffaceous metasediment, very fine-grained to glassy with interbedded thin sandy layers.|
5619|Doomadgee Formation|68575|5|Briefly described|p11|||||Fickling Group.||Is overlain unconformably by Hedleys Sandstone.||
5619|Doomadgee Formation|69433|4|Described|p18:2, 4-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Is c.400m thick in the type section in WESTMORELAND map area. SHRIMP detrital zircon maximum deposition age.|<1619 +/- 5 Ma (Page et al., 2000).|Fickling Group.||Disconformably, locally conformably, overlies Mount Les Siltstone. Is overlain unconformably by the South Nicholson Group.|Conglomerate, sandstone, siltstone, shale and dolostone; arranged in upward-coarsening cycles from shale to sandstone, punctuated by dolostone intervals. A variety of sedimentary structures is listed.|12-JUL-16
5619|Doomadgee Formation|69591|5|Briefly described|p43 Fig.2.31, p47, p55|||Camooweal-Murphy Domain, Isa Superbasin. Part of Lawn and Wide Supersequences. Is presented on p43 (in Fig.2.31) as Lower and Upper Doomadgee Formations.|1619 +/- 5 Ma (Page et al., 2000).|Fickling Group.||The lower part is equated with the Lawn Supersequence; the upper part with Wide and Doom Supersequences.|Brown and green shale, thin-bedded siltstone, fine sandstone.|
5619|Doomadgee Formation|69673|4|Described|p52 fig 42, p53 |Statherian|Statherian||1619 +/- 5 Ma||||Conglomerate, sandstone, siltstone, shale and dolostone.|
5619|Doomadgee Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Unconformably overlies Mount Les Siltstone. Is overlain unconformably by Constance Sandstone (South Nicholson Group).|Grey and brown or reddish, fine- to coarse-grained sandstone; dark grey fissile shale and siltstone with flaggy claystone interbeds; dolomite, dolomitic sandstone and conglomerate.|
5619|Doomadgee Formation|71369|5|Briefly described|p4, p9, p11|||Crops out as resistant benches (of sandstone).||Fickling Group.||Is overlain unconformably by Hedleys Sandstone.|Includes fine-grained sandstones, siltstone and shale.|20-FEB-18
5619|Doomadgee Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1632+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Ash tuff.|
5619|Doomadgee Formation|72526|4|Described|p1-2, p4, p7, p8, p20-32, p85, 87.|Statherian|Statherian|Lawn Hill Platform, Mount Isa Province. Shown as being located in the central and west of the South Nicholson Basin. This unit is c. 200-400m thick (Grimes and Sweet, 1979; Sweet et al., 1981; Ahmad and Munson, 2013a).  2 ages determined are maximum depositional ages (MDAs). Previous dating of tuff from lower Doomagee Formation, at 1619 +/- 5 Ma and 1613 +/- 5 Ma, is interpreted as depositional age (Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b).|1612+/-11 Ma, 1630+/-14 Ma max dep age.|Fickling Group||Disconormably overlies Mount Les Siltstone and shown as underlying South Nicholson Group.|Includes shale, micaceous, dolomitic fine-grained sandstone and siltstone, medium-to coarse-grained sandstone and pebble conglomerate, tuff and claystone.|
5619|Doomadgee Formation|72527|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Tuff bands within the middle of this unit yielded an age of 1613 +/- 5 Ma (Page and Sweet, 1998).|Middle of unit 1613 +/- 5 Ma.|Uppermost Fickling Group|||Includes tuff bands.|
5619|Doomadgee Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12, p45.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. Three U-Pb zircon sedimentary depositional ages [?] given for this unit on p5, two of them also shown on p33, suggesting that the 1613 date is from the upper part of the unit and the 1632 date from around the middle.|1632 +/- 14 Ma to 1613 +/- 5 Ma|Fickling Group||Unconformably overlies Mount Les Siltstone and partially equivalent to Lawn Hill Formation.|Includes dolomitic siltstone.|
5619|Doomadgee Formation|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p18, p21, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin. Identified in Amoco DDH 83-4 well in this study. Mineral composition boxplot shows majority quartz, microcline, muscovite and siderite.|1632 +/- 14, 1613 +/- 5 Ma|Fickling Group||Unconformably overlies Mount Les Siltstone.|Includes dolomitic siltstone.|
5619|Doomadgee Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||Fickling Group||||
5619|Doomadgee Formation|73042|5|Briefly described|p1, p4, p6, p14, p16-17||Statherian|Re-Os age overlaps with existing zircon depositional age constraints (generated from a number of sources) and is interpreted to record the timing of deposition for the unit. 4 other ages are given on p4 ranging from 1632+/-14Ma to 1613+/-5 Ma.  Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Maximum thickness: 400m. Broadly equivalent in age to Lawn Hill Formation.|1609 +/- 61 Ma Re-Os|Fickling Group||Disconformably underlain by Mount Les Siltstone. Partly overlain by Wangalinji Member of Playford Sandstone, unconformably.|Shale, micaceous dolomitic fine-grained sandstone and siltstone, medium-to coarse-grained sandstone and pebble conglomerate.|
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.|
5627|Doonmulla Member|13497|6|Mentioned|p112|||||Tinchoo Formation||||
5627|Doonmulla Member|13516|5|Briefly described|p171 fig 12|Middle Triassic|Middle Triassic|In Eromanga Basin.||Of Tinchoo Formation||||
5627|Doonmulla Member|23375|4|Described|Fig2 p265,280||Anisian|Of Tinchoo Formation, Cooper Basin.||||||30-JUN-08
5627|Doonmulla Member|42008|2|Defined|p273|Ladinian|Anisian|See also Fig.4 (p268). Of Tinchoo Formation.||||||16-APR-08
5627|Doonmulla Member|44133|5|Briefly described|p65 Fig. 8.3|Triassic|Triassic|Of the Tinchoo Formation. Geological Province: Cooper Basin.||||||
5627|Doonmulla Member|61613|5|Briefly described|p282 Fig. 2|Middle Triassic|Early Triassic|Of Tinchoo Formation. Overlain by Gilpeppee Member, Underlain by Wimma Sandstone Member. Geological Province: Cooper and Simpson Basins.||||||03-JUL-14
5627|Doonmulla Member|63978|2|Defined|p23-24, Fig. 3|Middle Triassic|Middle Triassic|Basal part of Tinchoo Fm. Unconformable on Arrabury Fm; conformably overlain by Gilpeppee Member. Max. thickness: 182m. In Cooper Basin. Detailed lithology for upper and lower sections given.||||||07-FEB-11
5627|Doonmulla Member|64048|5|Briefly described|p67|Middle Traissic|Middle Triassic|Basal unit of Tinchoo Formation. Unconformably overlies Arrabury Formation. Geological Province: Cooper Basin. Consists of fine- to medium-grained quartzose, fluvial sandstone.||||||07-FEB-11
5627|Doonmulla Member|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.||Lower unit in Tinchoo Formation.||Overlies Wimma Sandstone Member. Is overlain by Gilpeppee Member.||
5627|Doonmulla Member|65489|5|Briefly described|p96|||Cooper Basin.||Unit in Tinchoo Formation.||||
5627|Doonmulla Member|67402|5|Briefly described|P90 fig CPR4|||Deposited in a fluvial marine environment. May have some carbon dioxide storage potential. See also  p91 tbl CPR1, p90-p94, p99-p101, p101 tbl CPR2, p105.||Tinchoo Formation||Conformably overlain by the Gilpeppee Member. Unconformably overlies the Wimma Sandstone Member.|Interbedded fine to medium grained to granule conglomeratic sandstones that transition into siltstones and mudstones higher up.|
5627|Doonmulla Member|68731|5|Briefly described|p200 Fig 3.110, pp208-211|Middle Triassic|Middle Triassic|Cooper Basin. Powis (1989). ~ 50-180 m thick. Contains Anisian-early Ladinian (Gray and McKellar 2002) palynological units in its upper parts. Detailed palynology discussed.||Of the Tinchoo Formation.||Conformably overlain by the Gilpeppee Member.|Includes fine to medium, quartz-rich, planar cross-bedded and planar bedded sandstone, grading to granule conglomerate, with lesser interbedded silstone and mudstone; interbedded siltstone and mudstone, mostly horizontally laminated.|03-JUL-14
5627|Doonmulla Member|69946|5|Briefly described|p36|Early Triassic|Early Triassic|||Unit in Tinchoo Formation.||Conformably overlies Wimma Sandstone Member (Arrabury Formation). Is overlain conformably by Gilpeppee Member.||
5627|Doonmulla Member|70823|5|Briefly described|p76|||||Tinchoo Formation||Overlain by the Gilpepee Member.|Brown-grey siltstone and light grey sandstone.|
5627|Doonmulla Member|70824|6|Mentioned|p104|Middle Triassic|Middle Triassic|Cooper Basin.||Tinchoo Formation|||Interbedded brown-grey siltstone and light grey sandstone.|
5627|Doonmulla Member|71342|6|Mentioned|Ch5 p36|Ladinian|Anisian|Cooper Basin.  Palynological zone is given in fig 5.3 Ch5 p36.||Tinchoo Formation||||
5628|Doonside Formation|23799|6|Mentioned|p18|||Of Curtis Island Group.||||||
5628|Doonside Formation|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Curtis Island Group. Includes the Balnagowan Volcanic Member.||||||
5628|Doonside Formation|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
5628|Doonside Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
5628|Doonside Formation|24490|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group. Chert, mudstone, minor tuff and arenite.||||||04-SEP-08
5628|Doonside Formation|24615|5|Briefly described|CD|Carboniferous|Devonian|[DCcd].  Chert, jasper, mudstone, siltstone, lithic sandstone, tuff, limestone, and altered basalt.||||||
5628|Doonside Formation|30451|6|Mentioned|p8|||Lower ? Palaeozoic age||||||
5628|Doonside Formation|30777|4|Described|p417|||Discussed.||||||18-AUG-08
5628|Doonside Formation|31657|4|Described|p91|||See also P92. Ordovician - Silurian.||||||
5628|Doonside Formation|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5628|Doonside Formation|31659|2|Defined|p19|Early Paleozoic|Early Paleozoic|max. thickness: >9000ft. red, green and white chert, mudstone, limestone, acid tuff, tuffaceous arenite. See also Table 1.||||||07-NOV-08
5628|Doonside Formation|32357|4|Described|Table 1|||||||||
5628|Doonside Formation|32358|4|Described|Table 1|||||||||
5628|Doonside Formation|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5628|Doonside Formation|33769|5|Briefly described|p150|||||||||
5628|Doonside Formation|33774|3|Fully described|p6|||See also P7. ?Pre Devonian.||||||18-AUG-08
5628|Doonside Formation|34408|6|Mentioned|p185|||On table.||||||
5628|Doonside Formation|34947|6|Mentioned|p360|||||||||
5628|Doonside Formation|35008|6|Mentioned|p177|||||||||
5628|Doonside Formation|35266|6|Mentioned|p203|||||||||
5628|Doonside Formation|36211|6|Mentioned|p269|||||||||
5628|Doonside Formation|36333|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
5628|Doonside Formation|36488|6|Mentioned|p3|||||||||
5628|Doonside Formation|36528|6|Mentioned|p170|||||||||
5628|Doonside Formation|37453|5|Briefly described|p313|||||||||
5628|Doonside Formation|37676|6|Mentioned|p4|||||||||
5628|Doonside Formation|38081|5|Briefly described|Table 1|||||||||
5628|Doonside Formation|38391|6|Mentioned|p6|||||||||
5628|Doonside Formation|38406|5|Briefly described|p9|||||||||
5628|Doonside Formation|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
5628|Doonside Formation|39445|5|Briefly described|Table 6|||||||||
5628|Doonside Formation|39632|6|Mentioned|p208|||||||||
5628|Doonside Formation|39973|6|Mentioned|p4|||||||||
5628|Doonside Formation|39998|6|Mentioned|p189|||||||||
5628|Doonside Formation|40246|6|Mentioned|Fig.1|||||||||
5628|Doonside Formation|40475|6|Mentioned|p2|||||||||
5628|Doonside Formation|40960|6|Mentioned|p215|||||||||
5628|Doonside Formation|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
5628|Doonside Formation|41577|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|41922|4|Described|Table 1, P11|||||||||
5628|Doonside Formation|41927|6|Mentioned|p61|||||||||
5628|Doonside Formation|42143|6|Mentioned|p592|||||||||
5628|Doonside Formation|42547|4|Described|p53|||Age Devonian?||||||
5628|Doonside Formation|42660|4|Described|p23 p169|||||||||
5628|Doonside Formation|42901|5|Briefly described|p404|||see also Fig.12 P412.||||||18-AUG-08
5628|Doonside Formation|45107|6|Mentioned|p6|||||||||
5628|Doonside Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Curtis Island Group.  Contains the Balnagowan Volcanic Member.||||||17-MAY-04
5628|Doonside Formation|50208|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|50209|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||28-MAY-08
5628|Doonside Formation|60557|5|Briefly described|p19 Fig. 5b, p23|Early Carboniferous|Late Devonian|Contains the Balnagowan Volcanic Member.  Massive to ribbon-bedded chert and mudstone, with less abundant mafic volcanics, minor sandstone and rare small limestone lenses. See also p36.||||||18-AUG-08
5628|Doonside Formation|61035|5|Briefly described|p14|||Geological Province: Wandilla Province. Consists of chert-mudstone assemblage + some lithic sandstone, tuff, limestone, + altered basalt.||||||07-FEB-11
5628|Doonside Formation|64398|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of the Curtis Island Group. Chert, jasper, mudstone, siltstone, lithic sandstone, limestone and altered basalt.||||||
5628|Doonside Formation|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of Curtis Island Group. Comprises predominantly chert, jasper, mudstone, siltstone, lithic sandstone, limestone and altered basalt; with a subordinate unit of mudstone, siltstone, lithic sandstone, limestone and altered basalt.||||||
5628|Doonside Formation|64429|5|Briefly described|p20|Carboniferous|Devonian|Juxtaposed against Chalmers Formation||||||
5628|Doonside Formation|68008|3|Fully described|p50, p110-113, p119, p270, p273, p297|Early Carboniferous|Early Devonian|See also p426, p465, p480, p616. Kirkegaard et al. (1970), who defined it as the uppermost [sic] unit in the Group. Part of the Wandilla terrane. Usually forms prominent hills and strike ridges. Deep ocean-floor association. Repetition by faulting makes thickness determination impossible; certainly less than the 2100-3600m of Kirkegaard et al. (1970). Age from conodonts. Hosts Mn mineralisation. Geophysics modelling.||Basal Curtis Island Group.|Balnagowan Volcanic Member.|Is overlain by Alton Downs Basalt. Is faulted against Channer Creek beds. Is intruded by Targinie Quatrz Monzonite and Mount Hedlow Trachyte. Time equivalent of Mount Alma Formation.|Rhythmically interbedded radiolarian chert and jasper with argillite; minor greywacke, fine-grained volcaniclastic sandstone, and limestone.|
5628|Doonside Formation|68679|4|Described|p317-318, p338, p425|Mississippian|Devonian|Coastal Subprovince, Wandilla Province, New England Orogen. Forms a discontinuous belt immediately east of the Yarrol Fault, from Mundubbera to The Pointers. Includes a belt containing lenses of manganese mineralisation (psilomelane with some pyrolusite) from Mount Miller to Mount Beecher. Formed by slow deposition on abyssal sea-floor. Estimated thickness of 2100-3600m is almost certainly a gross overestimate from fault repetition. Brief mention of possible time-equivalence with Mount Alma Formation.||Curtis Island Group.|Balnagowan Volcanic Member.|Is faulted against, and locally overlain by, Wandilla Formation.|Ribbon chert and jasper, thin-bedded with slumps to very thick-bedded and massive; argillite and minor tuff and limestone; rhythmically interbedded radiolarian chert and mudstone dominate. Sporadic spilitic volcanics.|
5652|Double Mountain Volcanics|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
5652|Double Mountain Volcanics|31659|2|Defined|p70|Mesozoic|Mesozoic|Max. thickness: ~1500ft.  Dacitic crystal tuff, lithic, vitric and lapilli tuff, agglomerate, minor black siltstone. See also Table 1.||||||08-OCT-08
5652|Double Mountain Volcanics|32357|4|Described|Table 1|||||||||
5652|Double Mountain Volcanics|32361|6|Mentioned|Map legend|Cretaceous|Permian|Permian or Cretaceous||||||
5652|Double Mountain Volcanics|38143|6|Mentioned|p14|||||||||
5652|Double Mountain Volcanics|39445|5|Briefly described|Table 11|||||||||
5652|Double Mountain Volcanics|41246|6|Mentioned|Map legend|Cretaceous|Permian|||||||
5652|Double Mountain Volcanics|42660|4|Described|p23 p167|||||||||
5652|Double Mountain Volcanics|61035|5|Briefly described|p18|Mesozoic|Permian|Unconformably underlain by Shoalwater Formation. Consists of well-bedded, volcaniclastic siltstone, snadstone and breccia of dacitic composition and some rhyolitic ignimbrite. Geological Province: Coastal Block.||||||07-FEB-11
5652|Double Mountain Volcanics|68358|6|Mentioned|p7|||||||||
5652|Double Mountain Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with Berserker Group and Peninsula Range Volcanics, are all mapped under the symbol, Pk.||||||
5652|Double Mountain Volcanics|68679|5|Briefly described|p312-313, p347, p424, p426|Permian|Permian|Northern New England Orogen.||||Is intruded by Pyri Pyri Granite.||
5652|Double Mountain Volcanics|69952|5|Briefly described|p2 Tb.i, p5, p77, p79-83|Permian|Permian|In the Normanby and Polygon Ranges; New England Orogen. Resists erosion, and crops out as scattered rubble. This mid-Permian SHRIMP U-Pb zircon magmatic crystallisation age resolves uncertainty about possible Cretaceous age: Murray (1975) had suggested a possible correlation with the Early Cretaceous Whitsunday Volcanics. May be comagmatic with Mailmans Gap Granodiorite, as that unit's age of 269.3 +/- 1.7 Ma is indistinguishable.|270.6 + 4.6/ - 2.2 Ma (Cross et al., 2015).||||Includes dark grey, very fine-grained, porphyritic coherent dacite.|
5652|Double Mountain Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|271 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite.|
5652|Double Mountain Volcanics|73197|6|Mentioned|p474-475|Guadalupian|Guadalupian|New England Orogen, northern. Coeval with Owl Gully Volcanics, Rookwood Volcanics, Berserker Group, Peninsula Range Volcanics.|270 Ma U-Pb zircon.||||Lavas and pyroclastics.|
5661|Douglas Creek Limestone|22604|5|Briefly described|p442, Fig.1 p438||Emsian|||||||
5661|Douglas Creek Limestone|23161|6|Mentioned|p7||Early Devonian|||||||
5661|Douglas Creek Limestone|23430|5|Briefly described|p510|||||||||
5661|Douglas Creek Limestone|23522|5|Briefly described|p256|Middle Devonian|Early Devonian|||||||
5661|Douglas Creek Limestone|24611|5|Briefly described|p194, p220|Emsian|Emsian|Geological Province: Anakie Inlier.  See p196 Fig. 2.||||||
5661|Douglas Creek Limestone|30814|6|Mentioned|p71|||||||||
5661|Douglas Creek Limestone|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
5661|Douglas Creek Limestone|31502|5|Briefly described|p93|||See also P94-120. Age.||||||
5661|Douglas Creek Limestone|32493|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
5661|Douglas Creek Limestone|33326|6|Mentioned|p447|||Fauna||||||
5661|Douglas Creek Limestone|33329|6|Mentioned|p119|||Emsian or early Couvinian. Corals.||||||
5661|Douglas Creek Limestone|33434|6|Mentioned|p42|||||||||
5661|Douglas Creek Limestone|33641|6|Mentioned|p59|||M.Dev.||||||
5661|Douglas Creek Limestone|34389|4|Described|Table 1|||Middle Devonian.||||||
5661|Douglas Creek Limestone|39445|5|Briefly described|Table 5|||See also P73||||||
5661|Douglas Creek Limestone|41246|6|Mentioned|Map legend|Devonian||||||||
5661|Douglas Creek Limestone|42031|5|Briefly described|p764|||||||||
5661|Douglas Creek Limestone|42747|5|Briefly described|p36|||late Early Devonian||||||
5661|Douglas Creek Limestone|43204|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Anakie Inlier||||||23-DEC-11
5661|Douglas Creek Limestone|43213|3|Fully described|p9, p67-68, p149, p237|Early Devonian|Early Devonian|Veevers et al. (1964); Olgers (1969). Named after Douglas Creek Homestead. Type section described. Anakie Inlier; near Clermont. Contains corals, brachiopods and conodonts of late Emsian age.||||Inferred to overlie Bathampton Metamorphics unconformably. Correlated with Dunstable Volcanics, Glendarriwell and Ukalunda beds.|Calcirudite wackestone to packstone; brown, micaceous, thin-bedded and fossiliferous siltstone; quartzose, flat laminated, well sorted, fine- to very coarse-grained sandstone; matrix-supported conglomerate, quartz pebbles in a quartzose sandstone.|
5661|Douglas Creek Limestone|43461|14|Not recorded|table p618||Couvinian|||||||
5661|Douglas Creek Limestone|43530|14|Not recorded|p1035,1037|||||||||
5661|Douglas Creek Limestone|43994|14|Not recorded|Map Legend|||||||||
5661|Douglas Creek Limestone|44081|14|Not recorded|p28|||||||||
5661|Douglas Creek Limestone|44331|14|Not recorded|Map Legend||Middle Devonian|Lower Middle Devonian.||||||
5661|Douglas Creek Limestone|44337|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Lithology.||||||
5661|Douglas Creek Limestone|44432|14|Not recorded|p30||Middle Devonian|||||||
5661|Douglas Creek Limestone|45071|3|Fully described|p15|||||||||
5661|Douglas Creek Limestone|45073|4|Described|p14|||Refers Hill (1939)||||||
5661|Douglas Creek Limestone|48843|14|Not recorded|p.7-9,18,map||Middle Devonian|M.Devonian, probably Upper Couvinian (from corals).||||||
5661|Douglas Creek Limestone|48845|14|Not recorded|p10|||||||||
5661|Douglas Creek Limestone|48900|6|Mentioned|p9|||||||||
5661|Douglas Creek Limestone|65940|6|Mentioned|p203,209|Emsian|Emsian|Clermont, QLD. Contains A. clermontense (see Mawson and Talent, 2003), Thamnopora randsi (type area, mid-Emsian, perbonus to inversus Zones; Mawson and Talent, 2003).||||||
5661|Douglas Creek Limestone|68553|6|Mentioned|Map legend|Devonian|Devonian|This unit, as well as the Ukalunda and Sedgeford Formations, the Theresa Creek and Dunstable Volcanics, and unnamed Devonian sedimentary and volcanic units, are all mapped under the symbol, Da.||||||
5661|Douglas Creek Limestone|68731|5|Briefly described|p120, p171, p172, p173, p177 Fig 3.91|Early Devonian|Early Devonian|Veevers et al. (1964). Outcrops in the Douglas and Drummond Creek area ~8.5 km south of Clermont. Fossils include corals, conodonts, stromatoporoids, crinoidal debris, and less common brachiopods, gastropods and ostracods - indicating an Emsian age.|||||Comprises calcirudite wackestone limestone, brown micaceous thin-bedded siltstone, and quartzose sandstone and conglomerate.|03-JUL-14
5661|Douglas Creek Limestone|68900|6|Mentioned|p4, p31-p32|Devonian|Devonian|Drummond Basin. Possibly representative of a shallow marine platform.||||Equivalent to the Ukalunda Formation.||
5661|Douglas Creek Limestone|69541|6|Mentioned|p645 Fig.1(b), p654|Middle Devonian|Early Devonian|Thomson Orogen.||||||
5661|Douglas Creek Limestone|69592|6|Mentioned|p229|Devonian|Devonian|Scattered remnants in central QLD, developd on Thomson Orogen basement.||||||
5661|Douglas Creek Limestone|70740|5|Briefly described|p35|Emsian|Emsian|Age derived from fossils in the coeval Ukalunda Formation. ||||Equivalent to the Ukalunda Formation.||
5715|Dry Creek Andesitic Tuff Member|33381|5|Briefly described|p108|||Permian||||||
5726|Drynoch Granite|22847|3|Fully described|p 58|Early Permian|Carboniferous|||||||
5726|Drynoch Granite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
5726|Drynoch Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
5726|Drynoch Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 112. I-Type.||||||
5726|Drynoch Granite|42245|2|Defined|p41|Permian||Reserved as Drynoch Adamellite||||||
5726|Drynoch Granite|43093|4|Described|Appendix 1|Early Permian|Carboniferous|Middle Carboniferous to Early Permian||||||
5726|Drynoch Granite|43259|4|Described|Appendix 1,p23.|Permian|Carboniferous|||||||
5726|Drynoch Granite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
5726|Drynoch Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Suite.||||
5734|Duaringa Formation|24615|5|Briefly described|CD|Tertiary|Tertiary|[Tu].  Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt.||||||
5734|Duaringa Formation|38081|5|Briefly described|Table 1|||||||||
5734|Duaringa Formation|39445|5|Briefly described|Table 14|||Eocene. See also p150.||||||14-OCT-08
5734|Duaringa Formation|39943|6|Mentioned|Table 13A|||||||||
5734|Duaringa Formation|40434|6|Mentioned|p30|||||||||
5734|Duaringa Formation|40675|6|Mentioned|Table 12D|||||||||
5734|Duaringa Formation|41246|6|Mentioned|Map legend|Tertiary||||||||
5734|Duaringa Formation|41922|4|Described|Table 1, P8|||||||||
5734|Duaringa Formation|42975|5|Briefly described|p256|||||||||
5734|Duaringa Formation|43851|14|Not recorded|Tb p106||Tertiary|||||||
5734|Duaringa Formation|43998|14|Not recorded|Map||Tertiary|||||||
5734|Duaringa Formation|44170|14|Not recorded|p23||Tertiary|Ref. to QLD map 1953||||||
5734|Duaringa Formation|44581|14|Not recorded|p353-354|||See also Lexicon.||||||
5734|Duaringa Formation|50213|5|Briefly described|Map legend|Tertiary|Tertiary|Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt.||||||
5734|Duaringa Formation|50602|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt.  Overlies: Back Creek Group.||||||19-JUL-04
5734|Duaringa Formation|60475|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt.||||||
5734|Duaringa Formation|60480|5|Briefly described|Map Legend|Tertiary|Tertiary|Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt.||||||29-SEP-04
5734|Duaringa Formation|60557|5|Briefly described|p20 Fig. 5c, p28|Tertiary|Tertiary|||||||
5734|Duaringa Formation|61035|5|Briefly described|p20|Tertiary|Tertiary|Thickness: >1200m. Geological Province: Duaringa Basin. Consists of mudstone, siltstone and subordinate sandstone, ironstone and some oil shale.||||||07-FEB-11
5734|Duaringa Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Fitzroy region.||||||03-MAR-10
5734|Duaringa Formation|61906|5|Briefly described|p141|||Freshwater sandstones, siltstones and conglomerates. Contains fossilised trees at its base. Extensively ferruginised.||||||
5734|Duaringa Formation|65388|2|Defined|p225-226|Miocene.|Eocene|Duaringa Basin. Used by (Hill, 1953). Type section now designated in GSQ Duaringa 1-2R (Noon, 1982b), which intersected 1218.5m of mudstone, siltstone and subordinate sandstone, ironstone and some oil shale and lignite before  basalt  extending to 1303m. Overlies Permian. Age from palynology.||||||
5734|Duaringa Formation|67402|4|Described|p239, p256|Longfordian|Wangerripian|Duaringa Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a fluvial to lacustrine environment. 1300m thick. |||||Sandstone, claystone, siltstone, oil shale, lignite, diatomite and bituminous shale with interbedded basalt flows.|26-SEP-22
5734|Duaringa Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Emerald, Exevale, Floraville, Glendower, 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.||||||
5734|Duaringa Formation|68679|6|Mentioned|p312-313, p347|Paleogene|Paleogene|Northern New England Orogen.||||||
5734|Duaringa Formation|69599|5|Briefly described|p585, p591, p635, p651|Miocene|Eocene|Duaringa Basin. 1300m thick. Weathered capping of laterite. Forms low mesas and tablelands up to 100m high. Subsurface fossils include fish, insects and plant debris. Substantial oil (shale) resource not developed.||||Correlated with Biloela beds; Southern Cross, Exevale, Suttor, and Emerald Formations.|Sandstone, siltstone, lignite, oil shale and minor diatomite with interbedded basalt flows.|
5734|Duaringa Formation|72297|6|Mentioned|p726|Cenozoic|Cenozoic|Includes diatomite at Junee (QLD).||||||
5734|Duaringa Formation|73040|5|Briefly described|Map legend|Oligocene|Eocene||||||Mudstone, sandstone, conglomerate, siltstone, oil shale, lignite, basalt|
5734|Duaringa Formation|73246|6|Mentioned|p189|Cenozoic|Cenozoic|||||||
5734|Duaringa Formation|73450|6|Mentioned|p55|Quaternary|Tertiary|||||||
5734|Duaringa Formation|75060|6|Mentioned|p41, 43|||Completely fills the 1000m Duaringa Basin, in the central to eastern Bowen Basin.||||||
5739|Ducabrook Formation|22540|4|Described|p777|Visean|Visean|||||||
5739|Ducabrook Formation|23161|6|Mentioned|p13|||||||||
5739|Ducabrook Formation|23184|5|Briefly described|p177-8|Asbian|Holkerian|Max Age: ca. 335 Ma.||||||
5739|Ducabrook Formation|23430|5|Briefly described|p510|||Drummond Basin Province.||||||21-OCT-08
5739|Ducabrook Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Lithic and feldspathic sandstone, siltstone and mudstone;  minor tuff, algal and oolotic limestone.  Max. thickness: 2300m.  Geological Province: Drummond Basin.||||||
5739|Ducabrook Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
5739|Ducabrook Formation|30546|6|Mentioned|p107|||Lower Carboniferous age. Correlation||||||
5739|Ducabrook Formation|30691|4|Described|p13|||Lower Carboniferous age. See also p20,Table3.||||||02-NOV-22
5739|Ducabrook Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
5739|Ducabrook Formation|30915|6|Mentioned|p99|||||||||
5739|Ducabrook Formation|31120|4|Described|p148|||||||||
5739|Ducabrook Formation|31121|6|Mentioned|Table 1|||||||||
5739|Ducabrook Formation|32490|6|Mentioned|Table 2|||||||||
5739|Ducabrook Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
5739|Ducabrook Formation|32639|6|Mentioned|p75|||||||||
5739|Ducabrook Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
5739|Ducabrook Formation|33092|5|Briefly described|p7|||Strat. table||||||
5739|Ducabrook Formation|33096|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
5739|Ducabrook Formation|33645|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Drummond Gp.||||||
5739|Ducabrook Formation|33646|6|Mentioned|p18|||Construction materials||||||
5739|Ducabrook Formation|34174|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
5739|Ducabrook Formation|34389|4|Described|Table 1|||Lower Carboniferous.||||||
5739|Ducabrook Formation|34390|4|Described|Table 1|||Lower Carboniferous||||||
5739|Ducabrook Formation|34392|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
5739|Ducabrook Formation|34408|6|Mentioned|p185|||On table.||||||
5739|Ducabrook Formation|35560|6|Mentioned|Fig.4|||||||||
5739|Ducabrook Formation|35811|5|Briefly described|Table 4|||||||||
5739|Ducabrook Formation|35913|6|Mentioned|p35|||||||||
5739|Ducabrook Formation|36243|6|Mentioned|Table 2A|||||||||
5739|Ducabrook Formation|36739|6|Mentioned|p21|||||||||
5739|Ducabrook Formation|37451|6|Mentioned|Table 2|||||||||
5739|Ducabrook Formation|37610|6|Mentioned|Fig.4|||||||||
5739|Ducabrook Formation|38374|6|Mentioned|p601|||||||||
5739|Ducabrook Formation|39445|5|Briefly described|Table 6|||||||||
5739|Ducabrook Formation|39813|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|Late Middle Carboniferous.||||||
5739|Ducabrook Formation|39943|6|Mentioned|Table 3A|||||||||
5739|Ducabrook Formation|40623|5|Briefly described|p110|||||||||
5739|Ducabrook Formation|41120|5|Briefly described|p196|||||||||
5739|Ducabrook Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
5739|Ducabrook Formation|42486|5|Briefly described|p201|||||||||
5739|Ducabrook Formation|42547|5|Briefly described|Fig.17 P61|||||||||
5739|Ducabrook Formation|42564|6|Mentioned|p12|||Drummond Basin||||||
5739|Ducabrook Formation|42614|5|Briefly described|Table P5|||||||||
5739|Ducabrook Formation|42701|6|Mentioned|p25|||Emerald sheet area||||||
5739|Ducabrook Formation|43105|6|Mentioned|p12|||||||||
5739|Ducabrook Formation|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Anakie Inlier||||overlies Star of Hope Formation||23-DEC-11
5739|Ducabrook Formation|43213|3|Fully described|p92-94, p238|Early Carboniferous|Early Carboniferous|Of Hill (1957); previously named the Ducabrook Series by Shell (Queensland) Development Pty Ltd (1952). The lower part of Hill's unit was renamed the Star of Hope Formation by de Bretizel (1966). Occurs only in southern Drummond Basin. Thickness to 2100m. Fluviatile and lacustrine sediments from a coeval volcanic arc to the east. Contains fish and plant remains and the brachiopod Leaia. Geophysics described.||||Conformably overlies Star of Hope Formation. Is intruded by Hoy Basalt.|A well-bedded sequence of sandstone and mudstone with some conglomerate and limestone; includes persistent beds of volcaniclastic rock including tuff.|
5739|Ducabrook Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
5739|Ducabrook Formation|43990|14|Not recorded|Map Legend||Early Carboniferous|||||||
5739|Ducabrook Formation|43994|14|Not recorded|Map Legend|||||||||
5739|Ducabrook Formation|43998|4|Described|Not recorded|Carboniferous|Devonian|||||||
5739|Ducabrook Formation|43999|14|Not recorded|p96|||||||||
5739|Ducabrook Formation|44010|14|Not recorded|p68,69|||||||||
5739|Ducabrook Formation|44081|4|Described|p30-1,42-3,47-51,64,|||p66-8,70,73-4,78,81,86,90-1,Fig.8,p182,186,188,193,196-8,Pls.8,9. Described in French.||||||
5739|Ducabrook Formation|44085|2|Defined|Opp.p4-6,14,15|||||||||
5739|Ducabrook Formation|44091|14|Not recorded|p39,46,Tb.3||Early Carboniferous|||||||
5739|Ducabrook Formation|44102|14|Not recorded|p175-177,Fig.24|||Overlies Snake Range Group. Similar facies to Telemon Formation.||||||
5739|Ducabrook Formation|44103|14|Not recorded|p213,215|||||||||
5739|Ducabrook Formation|44247|14|Not recorded|p3||Early Carboniferous|See also Lexicon. Leaiid (crustacean) found.||||||
5739|Ducabrook Formation|44249|14|Not recorded|p65|||Palaeoniscoid fish? Elonichthys.||||||
5739|Ducabrook Formation|44331|14|Not recorded|Map Legend||Early Carboniferous|||||||
5739|Ducabrook Formation|44337|5|Briefly described|Map Legend||Early Carboniferous|Lithology.||||||
5739|Ducabrook Formation|44573|14|Not recorded|p98|||||||||
5739|Ducabrook Formation|44599|6|Mentioned|p10|||Intersected in Penjobe No.1||||||
5739|Ducabrook Formation|44697|14|Not recorded|p91|||See also Lexicon.||||||
5739|Ducabrook Formation|44852|14|Not recorded|p71||Early Carboniferous|||||||
5739|Ducabrook Formation|45071|3|Fully described|Table 1|||See also p17||||||02-NOV-22
5739|Ducabrook Formation|45073|3|Fully described|p40|||Refers Hill (1957)||||||
5739|Ducabrook Formation|45097|5|Briefly described|p22|||Refers to White (in Olgers, 1972). Correlation chart.||||||
5739|Ducabrook Formation|45155|6|Mentioned|p42|||||||||
5739|Ducabrook Formation|46849|6|Mentioned|Fig. 2|||||||||
5739|Ducabrook Formation|46881|6|Mentioned|Table 2|||||||||
5739|Ducabrook Formation|48630|14|Not recorded|p17|||||||||
5739|Ducabrook Formation|48843|14|Not recorded|p.8,14,16;map||Carboniferous|(F55-11).||||||
5739|Ducabrook Formation|48845|2|Defined|p7,10,13,15-20,23-27|||p51,map,Fig.10.||||||
5739|Ducabrook Formation|48900|3|Fully described|p18|||Lower Carboniferous. Fossils.||||||
5739|Ducabrook Formation|48908|6|Mentioned|p21||Early Carboniferous|||||||
5739|Ducabrook Formation|48915|6|Mentioned|Table 1|||Devonian - Carboniferous||||||
5739|Ducabrook Formation|48920|3|Fully described|p20|||Part of Drummond Group.||||||21-OCT-08
5739|Ducabrook Formation|48951|6|Mentioned|Table 1|||||||||
5739|Ducabrook Formation|48995|5|Briefly described|p83|||Age and thickness only.||||||
5739|Ducabrook Formation|61394|5|Briefly described|p963, p964 Fig. 1|Visean|Visean|New sp. of Gyracanthus discovered in this unit in Middle Paddock, Queensland. A tetrapod-bearing formation. Geological Province: southern Drummond Basin. See also p966, 968, 988, 993 Tb. 6.||||||21-OCT-08
5739|Ducabrook Formation|63713|6|Mentioned|p1526|Carboniferous|Carboniferous|||||Is locally overlain by Upper Aldebaran Sandstone.||
5739|Ducabrook Formation|63738|5|Briefly described|p1|Visean|Visean|Age is mid-Visean. Contains scales and bones of actinopterygians.||||||28-FEB-08
5739|Ducabrook Formation|64315|5|Briefly described|p509, p510 Tb. 1|Early Carboniferous|Early Carboniferous|Max.Thickness: 2100m. Geological province: southern Drummond Basin. Lithic arkose-feldspathic wacke, siltstone, mudstone, pebbly conglomerate, oolitic limestone; minor tuff, rhyolite; containsa tetrapod unit at Middle Paddock (Ducabrook cattle property).||||||21-OCT-08
5739|Ducabrook Formation|64855|5|Briefly described|p26, 27|Early Carboniferous|Early Carboniferous|A sedimentary sequence from PEC Warrong 1 is correlated with this Drummond Basin unit.||||||22-FEB-10
5739|Ducabrook Formation|65382|5|Briefly described|p713, 714|Visean|Visean|Drummond Basin. Age of 335 Ma given based on occurrence of the Anapiculatisporites largus Assemblage. Correlated with Mount Eclipse Sandstone, Ngalia Basin.||||||
5739|Ducabrook Formation|66085|5|Briefly described|Map legend|Carboniferous|Carboniferous|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.||||||
5739|Ducabrook Formation|66188|6|Mentioned|443, Fig 3|Early Carboniferous|Early Carboniferous|Of the Drummond Basin||||||
5739|Ducabrook Formation|66498|6|Mentioned|p47, 49-50|Carboniferous|Carboniferous|Drummond Basin, QLD. Contains the only tetrapod fauna in Australia between the Late Devonian and near-end Permian (c.100 m.y. gap). Species described.||||||
5739|Ducabrook Formation|67402|5|Briefly described|p165 tbl LPB1, p196 fig DRM2, p200, p201|Serpukhovian|Visean|Drummond Basin.||||Overlies the Star of Hope Formation.||
5739|Ducabrook Formation|68326|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|02-DEC-13
5739|Ducabrook Formation|68328|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Conformably overlies Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68411|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||Unconformably overlain by the Joe Joe Group. Conformably underlain by the Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68412|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68414|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin.||||Overlain by the Joe Joe Group. Conformably underlain by the Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68423|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|Drummond Basin. This unit is incorrectly colour-coded in the "Palaeozoic Units" inset on the sheet.||||Conformably overlies Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68482|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably underlain by the Star of Hope Formation.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Bulliwallah, Mount Rankin, Natal and Star of Hope Formations, are all mapped under the symbol, Cd3.||||||
5739|Ducabrook Formation|68679|5|Briefly described|p372|Mississippian|Late Devonian|Drummond Basin. Includes Lepidodendroid impressions.|||||Quartzofeldspathic sandstones and finer-grained, brown to red to green and grey rocks.|
5739|Ducabrook Formation|68731|5|Briefly described|p173 Fig 3.85, p191 Fig 3.102, p195|Mississippian|Mississippian|Restricted to the southwestern part of the Drummond Basin. < 2100 m thick. Fauna contained within this unit is discussed.||||Conformably underlain by the Star of Hope Formation.|Comprises thin- to thick-bedded, cross-laminated, fine- to medium-grained, quartzose to feldspatholithic sandstone interlayered with siltstones and mudstones, some with concretionary horizons.|03-JUL-14
5739|Ducabrook Formation|68900|2|Defined|p4, p37, p70, p74-p78|Early Carboniferous|Early Carboniferous|Drummond Basin. Originally named the Ducabrook Series (SQD, 1952) after the Ducabrook Pastoral Holding but was changed to Ducabrook Formation by Hill (1957). De Bretizel (1966) mapped the lower part of the formation as Star of Hope Formation and retained the name Ducabrook Formation for the upper part of the sequence. This unit is restricted to the southern part of the basin. No type area appears to have been specified. This unit has fairly prominent pink to dark red hues on composite radiometric images, indicating elevated potassium. Airborne magnetic images show only a very low magnetic response. Lithology is discussed in detail. Deposited within a fluvial and lacustrine environment. Thickness was calculated by Olgers (1972) at 2250m, but shallow dips and gentle folding preclude accurate estimates. Fossils including fish scales, brachiopods and plant fossils which suggest an early carboniferous age. This unit is considered a time equivalent of the Bulliwallah and Natal formations.||||Conformably overlies the Star of Hope Formation.|Very well-bedded sequence of interbedded sandstone, mudstone and some beds of tuff, reworked tuff, conglomerate and limestone.|
5739|Ducabrook Formation|69379|5|Briefly described|map legend|Early Carboniferous|Late Devonian||||||Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone|
5739|Ducabrook Formation|70856|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||Overlies Star of Hope Formation conformably.|Feldspatholithic sandstone, mudstone, siltstone (commonly tuffaceous), minor algal and oolitic limestone.|
5739|Ducabrook Formation|70857|5|Briefly described|Map Legend|Carboniferous|Devonian|||||Overlies Star of Hope Formation|Feldspatholithic sandstone, mudstone, siltstone, minor algal and oolitic limestone.|
5739|Ducabrook Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Early Carboniferous|Geological province: southern Drummond Basin.||||Unconformably overlain by Lake Galilee Sandstone of the Galilee Basin. Underlain by Star of Hope Formation. Equivalent to Natal and Bulliwallah formations in the northern Drummond Basin.||
5739|Ducabrook Formation|72297|5|Briefly described|p739|Early Carboniferous|Early Carboniferous|Drummond Basin. Associated with three significant zeolite deposits, only one of which is being mined (the Willows Zeolite mine, W of Emerald).|||||Includes waterlain ash-fall tuffs; locally altered to zeolite.|
5739|Ducabrook Formation|73198|4|Described|p499-500, p504-507, p510-511, p514-515|||Drummond Basin, south. Originally part of Cycle 3 of Olgers (1972); combined with Cycle 2 herein. Maximum thickness: 2100 m. Relatively consistent thickness. Compositionally indistinguishable from [previous] Cycle 2. Basement provenance. [See article for petrographic descriptions and data].||||Conformably underlain by Star of Hope Formation. Equivalent to Bulliwallah Formation and Natal Formation.|Includes quartz sandstone with horizontal bedding, parting liniation, planar cross-bedding, and bioturbation.|
5749|Duckinwilla Group|23251|5|Briefly described|Table 1 p6, p24|Early Jurassic|Late Triassic|Age based on ages of units. May be equivalent to either or both of Myrtle Creek Sandstone or Tiaro Coal Measures. Geological Province: Maryborough Basin.||||||14-AUG-08
5749|Duckinwilla Group|24382|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Includes Tiaro Coal Measures and the Myrtle Creek Sandstone.||||||
5749|Duckinwilla Group|41265|6|Mentioned|Map legend|Jurassic|Triassic|Reserved as Duckinwilla Creek.||||||14-AUG-08
5749|Duckinwilla Group|41736|6|Mentioned|Fig.1|||||||||
5749|Duckinwilla Group|41738|2|Defined|p173|Jurassic|Late Triassic|||||||
5749|Duckinwilla Group|41740|6|Mentioned|p222|||||||||
5749|Duckinwilla Group|42054|6|Mentioned|p976|||||||||
5749|Duckinwilla Group|42450|4|Described|p407|||||||||
5749|Duckinwilla Group|42616|4|Described|p6|||||||||
5749|Duckinwilla Group|42636|4|Described|p8|||||||||
5749|Duckinwilla Group|42894|4|Described|p21, Fig.1 p20|||see also Fig.2 P22||||||
5749|Duckinwilla Group|43008|5|Briefly described|map legend|||||||||
5749|Duckinwilla Group|43059|4|Described|Table 1|||see also p9.||||||
5749|Duckinwilla Group|43100|4|Described|p43|||||||||
5749|Duckinwilla Group|43123|5|Briefly described|p25|||||||||
5749|Duckinwilla Group|44928|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
5749|Duckinwilla Group|60281|5|Briefly described|p37, p40, Fig.30 App 1|Middle Jurassic|Late Triassic|Comprised of the Myrtle Creek Sandstone and Tiaro Coal Measures.  Geological Province: Maryborough Basin.||||||
5749|Duckinwilla Group|63821|4|Described|p23|Early Jurassic|Late Triassic|Comprises Myrtle Creek Sandstone, Tiaro C.M. and an undivided section (due to poor exposure). Undivided part of the Group has Booyal Surface developed on it in SE corner of MARYBOROUGH sheet. Geological Province: Nambour Basin. See also p11, p22, p37.||||||07-FEB-11
5749|Duckinwilla Group|67402|6|Mentioned|p234|Middle Jurassic|Late Triassic|Maryborough Basin.|||Includes the Tiaro Coal Measures and Myrtle Creek Sandstone.|||
5749|Duckinwilla Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Nambour Basin.||||||
5749|Duckinwilla Group|68679|6|Mentioned|p312-313|Jurassic|Late Triassic|Northern New England Orogen.||||||
5749|Duckinwilla Group|69582|6|Mentioned|p48|||Nambour Basin.|||Includes the Myrtle Creek Sandstone and the Tiaro Coal Measures.|||
5749|Duckinwilla Group|69594|6|Mentioned|p519, p546|||Cranfield (1989). Nambour Basin (previously included in the Maryborough Basin).|||Tiaro Coal Measures, Myrtle Creek Sandstone.|||
5776|Dugald River Shale Member|39492|2|Defined|p28|Proterozoic|Proterozoic|||||||
5776|Dugald River Shale Member|45166|5|Briefly described|p20|||||||||
5776|Dugald River Shale Member|67323|5|Briefly described|GIS attrib tbl, p15|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Isa Superbasin. Appears as Dugald River Shale on the Mount Isa Block Time-Space Plot, and on p15 where it is described as "part of the Mount Roseby Schist".|1686 +/- 7 Ma MDA (Carson et al., 2008).|Mount Albert Group.|||Dark grey, carbonaceous shale and siltstone and grey mica schist.|
5776|Dugald River Shale Member|69056|5|Briefly described|p55, Time-Space plot sheet|Statherian|Statherian|Mary Kathleen Domain. Hosts the Dugald River Ag-Pb-Zn deposit. Appears as Dugald River Shale in the Time-Space Plot. Maximum depositional age.|1686 +/- 7 Ma (Carson et al., 2011).|Mount Roseby Schist.||||
5776|Dugald River Shale Member|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Roseby Schist.|||Dark grey, carbonaceous shale and siltstone and grey mica schist. A sub-unit of dark grey silty dolomitic limestone and siltstone is mapped separately.|
5776|Dugald River Shale Member|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mount Roseby Schist|||Dark grey carbonaceous shale and siltstone and mica schist; dark grey silty, dolomitic limestone and siltstone.|
5776|Dugald River Shale Member|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP age of 1686 +/- 6 Ma reported by Carson et al. (2008).|1686 +/- 6 Ma|||||
5776|Dugald River Shale Member|73553|5|Briefly described|p8 Fig.1.2.3|Statherian|Statherian||1686+/-7 Ma MDA|Mount Albert Group||||
5784|Dulcie Sandstone|9694|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Georgina Basin. Overlies: Nora Formation. Arenite, rare conglomerate.||||||
5784|Dulcie Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Devonian|Early Devonian|Geological province: SW Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|12951|5|Briefly described|p142, 149, 152, p143 fig4, p145, 154|Devonian|Devonian|Georgina Basin. Fluvial deposits.||||Correlated with Cravens Peak beds.|Continental sandstone.|
5784|Dulcie Sandstone|22646|6|Mentioned|p 107|||informally divided into upper and lower Dulcie Sandstone p107.  Situated in the Georgina Basin.||||||28-FEB-13
5784|Dulcie Sandstone|22804|5|Briefly described|p454|||Geological Province: western Georgina Basin.||||||05-SEP-14
5784|Dulcie Sandstone|22954|6|Mentioned|Fig3p9|Emsian|Emsian|||||||
5784|Dulcie Sandstone|23732|5|Briefly described|p31|Late Devonian|Early Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|23818|5|Briefly described|p114|Late Devonian|Late Devonian|||||||
5784|Dulcie Sandstone|23858|5|Briefly described|p917|Early Devonian|Early Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|24065|4|Described|p235|Devonian|Silurian|Geological Province: Georgina Basin. Maximum thickness: ~646m.||||||
5784|Dulcie Sandstone|24066|5|Briefly described|p237|Devonian|Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|24613|6|Mentioned|p39|||Geological province: Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|30017|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
5784|Dulcie Sandstone|32865|4|Described|p482|||Frasnian||||||
5784|Dulcie Sandstone|33103|4|Described|Table 4|||||||||
5784|Dulcie Sandstone|33104|6|Mentioned|Map legend|Devonian|Devonian|||||||
5784|Dulcie Sandstone|33326|6|Mentioned|p449|||Fauna||||||
5784|Dulcie Sandstone|33625|6|Mentioned|p191|||||||||
5784|Dulcie Sandstone|34612|6|Mentioned|p114|||Upper Devonian||||||
5784|Dulcie Sandstone|34810|6|Mentioned|p9|||Re ages.||||||
5784|Dulcie Sandstone|36473|6|Mentioned|Map legend|Devonian|Devonian|||||||
5784|Dulcie Sandstone|37272|6|Mentioned|p237|||||||||
5784|Dulcie Sandstone|37727|4|Described|p56|||See also p23.||||||09-AUG-06
5784|Dulcie Sandstone|39978|6|Mentioned|p65|||||||||
5784|Dulcie Sandstone|40538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Quartz arenite, thin to thick bedded, cross-bedded, scarp-forming, brown to pale yellow brown. Geological Province: Georgina Basin.||||||15-NOV-05
5784|Dulcie Sandstone|40836|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
5784|Dulcie Sandstone|40906|4|Described|p29|||||||||
5784|Dulcie Sandstone|41018|6|Mentioned|p239|||||||||
5784|Dulcie Sandstone|41204|6|Mentioned|p14|||||||||
5784|Dulcie Sandstone|41276|6|Mentioned|p75|||||||||
5784|Dulcie Sandstone|41385|6|Mentioned|p363|||||||||
5784|Dulcie Sandstone|41524|3|Fully described|p21|||||||||
5784|Dulcie Sandstone|41525|5|Briefly described|Map legend|Devonian|Devonian|Quartz sandstone, whitish, crossbedded, medium to thick-bedded.||||||26-OCT-05
5784|Dulcie Sandstone|41820|6|Mentioned|p15|||||||||
5784|Dulcie Sandstone|41883|6|Mentioned|Fig.49|||||||||
5784|Dulcie Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
5784|Dulcie Sandstone|42504|6|Mentioned|p83|||Georgina Basin||||||
5784|Dulcie Sandstone|42643|3|Fully described|p32|Middle Devonian|Early Devonian|||||||
5784|Dulcie Sandstone|42644|5|Briefly described|Map Legend|Devonian|Devonian|Quartz arenite, medium-to-thick bedded, cross-bedded, white to brown. Geological Province: Georgina Basin.||||||15-NOV-05
5784|Dulcie Sandstone|44233|14|Not recorded|Fig.1||Late Devonian|||||||
5784|Dulcie Sandstone|44320|14|Not recorded|p.10||Late Devonian|U.Dev. Table 1.||||||
5784|Dulcie Sandstone|44321|14|Not recorded|map legend||Late Devonian|(F53-7). U.Dev.||||||
5784|Dulcie Sandstone|44322|5|Briefly described|map legend||Devonian|||||||22-DEC-09
5784|Dulcie Sandstone|44327|2|Defined|p.11,14,17||Late Devonian|(F53-11). Tb.I, map. Upper Devonian.||||||14-NOV-07
5784|Dulcie Sandstone|44328|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
5784|Dulcie Sandstone|44964|14|Not recorded|p.350||Ordovician|Of Harts Range Group. Ordovician?||||||
5784|Dulcie Sandstone|44998|14|Not recorded|p56||Late Devonian|||||||
5784|Dulcie Sandstone|45041|6|Mentioned|p89|||||||||
5784|Dulcie Sandstone|45052|2|Defined|p132|Devonian|Devonian|See also p39.||||||09-AUG-06
5784|Dulcie Sandstone|45064|4|Described|Table 1|||||||||
5784|Dulcie Sandstone|45148|6|Mentioned|Fig.5|||Of Milligan and others 1966; Milligan 1976; renamed Lake Surprise Sandstone.||||||09-AUG-06
5784|Dulcie Sandstone|45155|6|Mentioned|Fig.8|||||||||
5784|Dulcie Sandstone|45167|5|Briefly described|p54|||||||||
5784|Dulcie Sandstone|45168|6|Mentioned|p6|||||||||
5784|Dulcie Sandstone|47050|5|Briefly described|Fig.1|||||||||
5784|Dulcie Sandstone|48844|1|Redefined|p.51||Late Devonian|On many pages. p.16,47,51,53-56, F.26,65,68, Pl.8, U.Devn.ss.which caps the Dulcie Range.O/lies Nora Fm. & Tomahawk Beds. (F53-11).||||||
5784|Dulcie Sandstone|48901|14|Not recorded|Not recorded||Late Devonian|U.Devonian. "Revision of usage" - on Tech File F/53-11.||||||28-FEB-13
5784|Dulcie Sandstone|60122|6|Mentioned|p32, p57 Appendix|||Lower part synonymous with Tomahawk Formation (Joklik 1955), together with the major portion of the former Tomahawk Beds (Smith 1964), excluding  the uppermost section which is now referred to Kelly Creek Formation.||||||
5784|Dulcie Sandstone|61022|5|Briefly described|p15 Fig. 2|Middle Devonian|Middle Devonian|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.||||||09-AUG-06
5784|Dulcie Sandstone|61404|5|Briefly described|Map legend|Devonian|Devonian|Quartz arenite: fine to medium; rare conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
5784|Dulcie Sandstone|62376|5|Briefly described|p53|Mesozoic|Mid Devonian|Geological Province: Georgina Basin||||||09-FEB-10
5784|Dulcie Sandstone|62522|5|Briefly described|p23|||Geological Province: Georgina Basin.||||||14-NOV-07
5784|Dulcie Sandstone|62983|5|Briefly described|p11|Devonian|Devonian|Synorogenic sedimentation. Geological Province: Georgina Basin.||||||23-JAN-07
5784|Dulcie Sandstone|63562|4|Described|p338 fig 3, p345 fig 7, p347 fig 9.|Devonian|Devonian|See also p350-351, p352 Fig.10, p355. Dulcie Syncline, Georgina Basin. Syn-orogenic clastic sedimentary unit sourced from uplifted Alice Springs Orogen to the S. Divided into lower clay-cemented (Early Devonian) and upper silica-cemented (Frasnian) units. The upper unit has mixed zircon ages similar to Stairway Sandstone, suggesting derivation from reworked Cambro-Ordovician sedimentary rocks.|c.365 Ma (Frasnian) upper part.|||Correlated with Pertnjara Group.|Well-sorted, medium- to thickly-bedded non-marine quartz sandstone.|18-SEP-18
5784|Dulcie Sandstone|64068|3|Fully described|p78, p40, p71, p75,77,  p ix|Eifelian|Pragian|Ungrouped. Formerly (Joklik 1955) included rocks now in Tomahawk Formation, Kelly Creek Formation, Nora Formation. Synorogenic, continental aeolian and freshwater sedimentation in a siliciclastic foreland, accompanied by high heat flow. No overlying units. Correlations: Cravens Peak beds, Mereenie Sandstone or Parke Siltstone.||||Unconformably overlies Nora Formation or Kelly Creek Formation.|Crossbedded quartz arenite, silty calcareous sandstone, pebble conglomerate.|04-APR-12
5784|Dulcie Sandstone|64778|6|Mentioned|p13, 33|Devonian|Devonian|Dulcie Syncline, Southern Georgina Basin.||||||
5784|Dulcie Sandstone|64812|5|Briefly described|p237 Fig. 2|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|64813|5|Briefly described|p256 Fig. 3|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||11-FEB-09
5784|Dulcie Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Devonian|Devonian|Geological province: southern Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|65338|5|Briefly described|p iv, p67.|Devonian|Devonian|Georgina Basin.|||||Medium- to thickly-bedded, cross-bedded quartz arenite.|
5784|Dulcie Sandstone|65341|6|Mentioned|p2 Fig.2. |Devonian|Devonian|||||||
5784|Dulcie Sandstone|65342|6|Mentioned|p6.|||Georgina Basin. Max. thickness at least 216 m.||||||
5784|Dulcie Sandstone|66499|6|Mentioned|p59, p65 Fig.8|||Includes fish fossils||||||
5784|Dulcie Sandstone|66767|5|Briefly described|p59|Devonian|Devonian|Southern Georgina Basin. Synorogenic (Alice Springs Orogeny) sedimentation: over 650m thickness preserved.||||||
5784|Dulcie Sandstone|67164|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Georgina/Ngalia Basins.|||||Quartz arenite, medium- to thick-bedded, cross-bedded.|
5784|Dulcie Sandstone|67892|5|Briefly described|Map legend|Paleozoic|Paleozoic||||||Quartz arenite, medium- to thick-bedded, cross-bedded.|
5784|Dulcie Sandstone|68298|5|Briefly described|p234|||Georgina Basin. Placoderm association occurs in upper part of this unit (Young, 1988b).||||Includes similar fauna to Hervey Group, Khan Yunis Formation||
5784|Dulcie Sandstone|68518|5|Briefly described|p11, p14|Devonian|Devonian|Outcropping. A few small low mesas in the far west have been mapped as possible Dulcie Sandstone. Age: possible Devonian, however now regarded as Cambrian by NTGS (Stidolph, P.A., pers. comm., 1986).|||||Unfossiliferous fine-grained and medium-bedded sandstone with minor silty laminae.|30-MAY-16
5784|Dulcie Sandstone|69427|6|Mentioned|p12:48|Devonian|Devonian|Georgina Basin.||||||12-JUL-16
5784|Dulcie Sandstone|69443|4|Described|p28:3-5, 7, 28, 30, 32, 45|Middle Devonian|Early Devonian|K.G. Smith (1964) after Joklik (1955). Dulcie Syncline, Southern Georgina Basin. Synorogenic (Pertnjara-Brewer events of the Alice Springs Orogeny) foreland deposition of clastic sediments. Forms prominent cliff-forming caps and scarps. No overlying units. 450-650m thick. Contains Pragian to early Eifelian fish fauna. Continental aeolian and braided fluviatile deposits. Has been modelled for sediment-hosted uranium mineralisation.||||Unconformably overlies Nora or Kelly Creek Formations. Correlative of Cravens Peak beds.|Prominently cross-bedded, medium- to thickly-bedded quartz sandstone, with rare beds of silty calcareous sandstone and pebble conglomerate.|12-JUL-16
5784|Dulcie Sandstone|69447|6|Mentioned|p32:6|||Georgina Basin. Lithologically similar to Lake Surprise Sandstone (Wiso Basin).||||||12-JUL-16
5784|Dulcie Sandstone|69673|6|Mentioned|p111, p118, p119 fig 94|Devonian|Devonian|650m thick. Fossil assemblage of Devonian fish and rare ichnofossils.||||Correlated with Cravens Peak beds|Sandstone with rare beds of silty calcareous sandstone and pebble conglomerate.|
5784|Dulcie Sandstone|73591|6|Mentioned|p40, p42|||Georgina Basin.||||||
5808|Dunda beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
5808|Dunda beds|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
5808|Dunda beds|42447|6|Mentioned|Fig.3|||Variation of Dunda Beds.||||||
5808|Dunda beds|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. ||||||
5808|Dunda beds|67402|5|Briefly described|p135|||Incorporated into the Clematis Sandstone in this study. |||||Fluvial sandstones interbedded with siltstone and mudstones.|
5808|Dunda beds|68279|5|Briefly described|p2, p4, p5 Tb.2, p7, p12, p16 Tb.4|Olenekian|Olenekian|Galilee Basin. Considered a variant of the upper Rewan Group; has never been described in detail.|||||Light grey, quartzose (83-90% quartz) sandstones thickly interbedded with tan or grey micaceous (c.35% mica) clayey siltstones.|
5808|Dunda beds|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Galilee Basin.||||||
5808|Dunda beds|68731|5|Briefly described|p200, p201, p201 Fig 3.110|Middle Triassic|Early Triassic|Cine et al. (1965). Restricted to the central and southern Koburra Trough, although there is one record of this unit in the Springsure Shelf in the Denison Trough. Probably a facies variant of the Arcadia Formation.||||Conformably underlain by the Rewan Group. Unconformably to disconformably overlain by the Clematis Group.||
5808|Dunda beds|71265|5|Briefly described|p589-590|Olenekian|Olenekian|Eastern Galilee Basin.||||Overlies Rewan Formation.||
5808|Dunda beds|71710|5|Briefly described|p370, p380, p382, p383 Fig 19, p385|Early Triassic|Early Triassic|Geological province: northern Galilee Basin. A facies variant of the Rewan Group. Of limited extent. Sequence 8.||sequence 8.||Facies variant of the Rewan Group. Transitional unit between Rewan and Clematis groups.|Quartz-labile sandstone and interbedded lutite.|
5808|Dunda beds|72088|5|Briefly described|p8, p15, p21-p22, p91|Anisian|Anisian|Southern and Eastern Galilee Basin. True extent is unknown. This unit has been recorded in two drillholes: GSQ Tambo 4 and SPP Birkhead 1.||||Conformably overlies the Rewan Group. Unconformably overlain by the Clematis Group.|Poorly sorted sandstones with a kaolonitic matrix and siltstones containing up to 35% mica.|
5808|Dunda beds|72298|5|Briefly described|p801|Triassic|Permian|Eromanga Basin (SA,QLD).||||Overlies Rewan FZ. Is overlain by Clematis Sandstone.||
5808|Dunda beds|73472|6|Mentioned|p115|Olenekian|Olenekian|Galilee Basin.||||Underlain by and equivalent to Rewan Formation.||
5813|Dundas Dolerite|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Late to Middle Triassic||||||
5813|Dundas Dolerite|36937|6|Mentioned|p229|||||||||
5813|Dundas Dolerite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
5813|Dundas Dolerite|39079|6|Mentioned|p8|||||||||
5829|Dundee Rhyodacite|22490|6|Mentioned|4|Late Permian|Late Permian|Geol. province: New England Fold Belt. Of the Wandsworth Volcanic Group.||||||31-MAY-07
5829|Dundee Rhyodacite|22678|6|Mentioned|p724||Tertiary|||||||
5829|Dundee Rhyodacite|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Volcanic Group, part included in the Coombadhja Volcanic Complex within the same group. Ignimbritic rhyodacite; minor porphyritic dacite lava, bedded tuff and breccia. Max. thickness: 2km. Geological Province: New England Fold Belt.||||||
5829|Dundee Rhyodacite|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Of the Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||31-MAY-07
5829|Dundee Rhyodacite|23811|5|Briefly described|Map Legend|Permian|Early Permian|Of Wandsworth Volcanic Group. Comprises informally named geographically separated masses including "Dundee Adamellite Porphyrite" and "Blue Granite".||||||31-MAY-07
5829|Dundee Rhyodacite|23812|4|Described|p25, 30|Early Triassic|Early Triassic|Of the Wandsworth Group.  Age:246-249Ma (Rb-Sr).  Maximum thickness: 2000m. Intruded by the Stanthorpe Monzogranite.||||||08-NOV-05
5829|Dundee Rhyodacite|23859|5|Briefly described|p930 Fig 2|Late Permian|Late Permian|Age: 248.7-245.8 Ma (Radiometric dating). Of Wandsworth Volcanic Group. Underlain by Emmaville Volcanics. Geological Province: New England Fold Belt.||||||31-MAY-07
5829|Dundee Rhyodacite|24424|5|Briefly described|p538|Early Triassic|Early Triassic|Age: ~247 Ma. Palaeomagnetic poles given.||||||
5829|Dundee Rhyodacite|32513|6|Mentioned|p318|||||||||
5829|Dundee Rhyodacite|33476|6|Mentioned|p54|||As a footnote||||||
5829|Dundee Rhyodacite|35173|6|Mentioned|Fig.3|||||||||
5829|Dundee Rhyodacite|35803|6|Mentioned|p321|||||||||
5829|Dundee Rhyodacite|36290|6|Mentioned|p164|||||||||
5829|Dundee Rhyodacite|38823|5|Briefly described|p207|||||||||
5829|Dundee Rhyodacite|38824|4|Described|p215|||||||||
5829|Dundee Rhyodacite|38825|4|Described|p221|||||||||
5829|Dundee Rhyodacite|38842|6|Mentioned|p291|||||||||
5829|Dundee Rhyodacite|38915|4|Described|p337|||||||||
5829|Dundee Rhyodacite|39238|6|Mentioned|p123|||||||||
5829|Dundee Rhyodacite|39279|6|Mentioned|p370|||||||||
5829|Dundee Rhyodacite|39445|6|Mentioned|p148|||||||||
5829|Dundee Rhyodacite|40507|6|Mentioned|p75|||||||||
5829|Dundee Rhyodacite|40509|6|Mentioned|p47|||||||||
5829|Dundee Rhyodacite|40514|6|Mentioned|p7|||||||||
5829|Dundee Rhyodacite|40773|6|Mentioned|p458|||||||||
5829|Dundee Rhyodacite|41041|3|Fully described|p266|||||||||
5829|Dundee Rhyodacite|41413|6|Mentioned|Fig.1|||||||||
5829|Dundee Rhyodacite|41998|5|Briefly described|p481|||||||||
5829|Dundee Rhyodacite|42284|6|Mentioned|p108|||||||||
5829|Dundee Rhyodacite|42378|3|Fully described|p25|||Supersedes "Dundee Ignimbrite" and "Dundee Porphyritic Adamellite"||||||
5829|Dundee Rhyodacite|42559|4|Described|p11|||Variation on Dundee Rhyodacite, NSW.||||||
5829|Dundee Rhyodacite|43008|5|Briefly described|map legend|||||||||
5829|Dundee Rhyodacite|43017|5|Briefly described|Fig.1,p372|||||||||
5829|Dundee Rhyodacite|43161|4|Described|32|||||||||
5829|Dundee Rhyodacite|43705|6|Mentioned|p19||Triassic|||||||
5829|Dundee Rhyodacite|43755|6|Mentioned|Fig.9,p556|||||||||
5829|Dundee Rhyodacite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group, Coombadjha Volcanic Complex. Formerly Dundee "Adamellite Porphyrite", an "Blue Granite".||||||20-JUL-04
5829|Dundee Rhyodacite|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
5829|Dundee Rhyodacite|61793|5|Briefly described|p341, p344|||Geological Province: New England Fold Belt.||||||07-FEB-11
5829|Dundee Rhyodacite|62534|4|Described|p8, p11 (legend)|Early Triassic|Late Permian|Of the Wandsworth Volcanic Group. Enveloped by Tent Hill Volcanics. Strongly porphyritic rhyodacitic ignimbrite. Magnetics/radiometrics discussed.||||||07-FEB-11
5829|Dundee Rhyodacite|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Dacitic to rhyolitic ignimbrites -subdivided into Timbarra Mass, Tenterfield Mass, Sunnyside Mass and Tarban Mass.||||||13-DEC-07
5829|Dundee Rhyodacite|63748|4|Described|p20|Late Permian|Late Permian|Formerly Dundee Adamellite-Porphyrite (Shaw 1969). Of Wandsworth Group. Unconformable on Wallangarra Volcanics. Age: 257.6+/-0.5Ma (U-Pb zircon).  Distinct, widespread, highly fragmented rhyolitic ignimbrite with a distinctive microgranitic groundmass.||||||07-FEB-11
5829|Dundee Rhyodacite|65668|6|Mentioned|p32,p34|Permian|Permian|Stanthorpe area; New England Orogen. Overlies the Wallangarra Volcanics.||||||
5829|Dundee Rhyodacite|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Triassic|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|242-252 Ma magnetic age range|||||24-APR-12
5829|Dundee Rhyodacite|68111|5|Briefly described|p968 Tb.1, p970 Fig.2|Wuchiapingian|Capitanian|LA-ICP-MS U-Pb dating (Belousova et al. 2006). Also 254.34 +/- 0.34 Ma (TIMS U-Pb; Brownlow and Cross, 2010).|257.6 +/- 2.5 Ma|Of the Wandsworth Volcanic Group.||Overlies Emmaville Volcanics.||
5829|Dundee Rhyodacite|68679|4|Described|p453-456, p458|Permian|Permian|Previously the Dundee Adamellite-Porphyrite (Shaw, 1969). Very restricted extent in QLD but a distinctive (a useful regional marker) and widespread unit in NSW, where it forms several separate ignimbrite masses throughout the Tenterfield-Dundee-Coombadjha area. Another age, U-Pb (LA-ICP-MS) of 257.6 +/- 0.5 Ma by Belousova et al. (2006) contradicts stratigraphic relationships.|254.34 +/- 0.34 Ma (Brownlow and Cross, 2010).|Wandsworth Volcanic Group.||Unconformably overlies the Wallangarra Volcanics.|Very crystal-rich and contains abundant fragments of plagioclase, deformed biotite, hornblende, pyroxene and quartz phenocrysts in a groundmass of abundant, strongly welded glass shards.|
5829|Dundee Rhyodacite|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||26-SEP-18
5829|Dundee Rhyodacite|69188|5|Briefly described|p64|Permian|Permian|Age is interpreted as a magmatic crystallisation age.|254.1 +/- 2.2 Ma (Brownlow and Cross, 2010).|||Overlies Emmaville Volcanics (Wandsworth Volcanic Group).||16-APR-20
5829|Dundee Rhyodacite|69323|5|Briefly described|p1, p70|Lopingian|Lopingian|Geological province: New England Orogen.|254.1+\-2.2 Ma (Brownlow and Cross, 2010)|Unit of Wandsworth Volcanic Group.||||03-DEC-19
5829|Dundee Rhyodacite|69639|4|Described|p2, p21, p57, p62, p68, p87, p219, p222|Lopingian|Lopingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop.|254.1 +/- 2.2 Ma (Brownlow and Cross, 2010)|Wandsworth Volcanic Group||Intruded by the Dandahra Creek Leucogranite and (inferred) the Cottesbrook Monzogranite.||
5829|Dundee Rhyodacite|70876|5|Briefly described|p82|Late Permian|Late Permian|Additional ages are provided as follows: 254.1 +/- 2.2 Ma (SHRIMP, Brownlow et al, 2010), 254.34 +/- 0.34 Ma (TIMS U-Pb zircon, Brownlow et al, 2010), 257.6 +/- 2.5 Ma (LAICPMS, Belousova et al, 2006), c. 249-246 Ma (Rb-Sr biotite, Shaw and Flood, 1993), c. 242 Ma (K-Ar, Evernden and Richards, 1962).|250.9 +/- 1.9 Ma (Black, 2007)|Wandsworth Volcanic Group||Overlies the Emmaville Volcanics.||
5829|Dundee Rhyodacite|71628|5|Briefly described|p1:15; p8: 80, 87; p11: 8-11; p12: 5-6|||See also p13-3; p14: 7, 28; p15: 5, 9, 65, 106; p17: 4-5; p19: 18, 72, 111, 128, 130, 160. Now interpreted to include Postmans Creek Granodiorite (Blevin, pers. comm., 2013). Metamorphosed (by Mole Leucogranite) at 245 +/- 2 Ma (K-Ar biotite: Kleeman et al., 1997). RELATED UNITS (continued): Is also intruded by Black Snake Creek Granite; Sandy Flat and Bolivia Range Leucomonzogranites; Dandahra Creek and Tenterfield Creek Leucosyenogranites; Grasstree Quartz Monzodiorite. Is faulted against Surface Hill Leucomonzogranite. Is bounded by Moonta Gully Monzogranite.||Wandsworth Volcanic Group.||Conformably overlies Welcome Volcanic Member. Is intruded by Cottesbrook, Bungulla, Blacksmiths Creek, Mount Lindesay Monzogranites; Kingsgate Syenogranite; see COMMENTS for more.||
5829|Dundee Rhyodacite|71701|5|Briefly described|p170|Lopingian|Lopingian|Age is a SHRIMP date.|254.3 +/- 0.3 Ma (Brownlow and Cross, 2010)|||||
5829|Dundee Rhyodacite|72528|5|Briefly described|p2, p78, p109.|Lopingian|Lopingian||254.34+/-0.34 Ma ID-TIMS U-Pb|||Intruded by Black Snake Creek Granite.||
5835|Dundowran Basalt|24382|5|Briefly described|Map legend|Miocene|Miocene|||||||
5835|Dundowran Basalt|39445|5|Briefly described|Table 14|||||||||
5835|Dundowran Basalt|41265|6|Mentioned|Map legend|Miocene||||||||
5835|Dundowran Basalt|42617|6|Mentioned|p16|||||||||
5835|Dundowran Basalt|42895|5|Briefly described|p56|||||||||
5835|Dundowran Basalt|43059|4|Described|p16, Table 2|||||||||
5835|Dundowran Basalt|63821|5|Briefly described|p25|Miocene|Miocene|K-Ar age: 18.6Ma (Stevens 1961) and 12Ma (Barnbaum 1976). Comprises two olivine basalt flows.||||||07-FEB-11
5835|Dundowran Basalt|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Gin Gin and Mount Runsome Basalts; Main Range, Minerva Hills, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
5853|Dunstable Volcanics|22604|6|Mentioned|Fig.1 p438|||||||||
5853|Dunstable Volcanics|22800|6|Mentioned|p584|Early Devonian|Early Devonian|||||||
5853|Dunstable Volcanics|23522|5|Briefly described|p250 Fig 6|Middle Devonian|Early Devonian|||||||
5853|Dunstable Volcanics|24075|5|Briefly described|p394 Fig. 2|Middle Devonian|Early Devonian|Andesitic lavas and pyroclastics with coralline limestone lenses.  Geological Province: Drummond Basin.||||||
5853|Dunstable Volcanics|30814|6|Mentioned|p65|||Refs Mollan et.al.1969||||||
5853|Dunstable Volcanics|31999|6|Mentioned|p136|||Table 1||||||
5853|Dunstable Volcanics|32493|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
5853|Dunstable Volcanics|32619|6|Mentioned|p463|||Eifelian fauna||||||
5853|Dunstable Volcanics|33326|6|Mentioned|p447|||Fauna||||||
5853|Dunstable Volcanics|33641|6|Mentioned|p59|||M.Dev.||||||
5853|Dunstable Volcanics|34408|6|Mentioned|p185|||On table.||||||
5853|Dunstable Volcanics|37565|6|Mentioned|Fig.6|||||||||
5853|Dunstable Volcanics|42547|5|Briefly described|Fig.17 P61|||||||||
5853|Dunstable Volcanics|43213|5|Briefly described|p68-69|Middle Devonian|Early Devonian|Nogoa Anticline. Has lithological and stratigraphic similarities with Theresa Creek Volcanics.||||Correlated with Douglas Creek Limestone and Glendarriwell beds.||
5853|Dunstable Volcanics|43994|14|Not recorded|Map Legend|Middle Devonian|Silurian|||||||
5853|Dunstable Volcanics|43998|4|Described|p21|Carboniferous|Devonian|||||||
5853|Dunstable Volcanics|43999|14|Not recorded|p93,94,96||Middle Devonian|L.M.Devonian||||||
5853|Dunstable Volcanics|44337|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Lithology.||||||
5853|Dunstable Volcanics|45071|4|Described|p15|||||||||
5853|Dunstable Volcanics|45073|4|Described|p14|||Geol. history see also P46.||||||
5853|Dunstable Volcanics|48900|4|Described|p9|||||||||
5853|Dunstable Volcanics|64315|5|Briefly described|p510 Tb. 1|Middle Devonian|Early Devonian|Geological province: southern Drummond Basin. Andesitic lavas, pyroclastics, lenses of coralline limestone. ||||||
5853|Dunstable Volcanics|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Telemon. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
5853|Dunstable Volcanics|68414|5|Briefly described|Map Legend|Devonian|Devonian|||||Overlain by the Foyle Volcanics.|Andesite, dacite, tuff, shale, limestone.|
5853|Dunstable Volcanics|68553|6|Mentioned|Map legend|Devonian|Devonian|This unit, as well as the Ukalunda and Sedgeford Formations, the Douglas Creek Limestone, the Theresa Creek Volcanics, and unnamed Devonian sedimentary and volcanic units, are all mapped under the symbol, Da.||||||
5853|Dunstable Volcanics|68731|5|Briefly described|p171, p172, p173, p173 Fig 3.85|Middle Devonian|Middle Devonian|Subdivided by Mollan et al. (1969) from from the original definition of the Dunstable Formation of Hill (1957). Contains a rich early Middle Devonian fauna of corals, stromatoporoids and bryozoans and conodonts.||||Unconformably overlain by the Foyle Volcanics.|Comprises andesitic lavas and pyroclastics with lenses of coralline limestone.|03-JUL-14
5853|Dunstable Volcanics|68900|4|Described|p4, p32-p34, p54|Devonian|Devonian|Drummond Basin. Restricted to a relatively small area in the core of the Nogoa Anticline. Veever et al (1964) identified corals in the Dunstable beds. BMR and GSQ work (Malone et al, 1964; Mollan, 1967; Mollan et al, 1969; Olger, 1972) revised the stratigraphy and changed the Dunstable beds to the Dunstable Volcanics. Fordham (1976) continued to use the term Dunstable beds. Limestones contain fossils indicative of a shallow marine environment. Fordham (1976) recorded an approximate thickness of 1000m. Structure and biostratigraphy are discussed in some detailed. Probably related to other basement units of the Drummond Basin such as the Sedgeford Formation, Theresa Creek Volcanics, Douglas Creek Limestone and Ukalunda Formation.||||Unconformably overlain by the Foyle Volcanics.|Green, regularly jointed andesites including porphyritic andesite with associated dacites and pyroclastics.|
5853|Dunstable Volcanics|69592|6|Mentioned|p229|Devonian|Devonian|Scattered remnants in central QLD, developd on Thomson Orogen basement.||||||
5853|Dunstable Volcanics|70857|5|Briefly described|Map Legend|Devonian|Devonian|||||Overlain by Foyle Volcanics|Andesite, dacite, tuff, shale and limestone.|
5853|Dunstable Volcanics|73163|6|Mentioned|p468|Devonian|Devonian|Drummond Basin. May be one of the sediment sources for Joe Joe Group.||||||
5853|Dunstable Volcanics|73179|6|Mentioned|p1143|Late Devonian|Middle Devonian|Anakie Inlier.|||||Predominantly basaltic to andesitic.|
5886|Dynamite Creek Member|23518|5|Briefly described|p11|Proterozoic|Proterozoic|Of Eastern Creek Volcanics.  Geological Province: Western Fold Belt.||||||
5886|Dynamite Creek Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5886|Dynamite Creek Member|38560|2|Defined|p114|Jurassic|Jurassic|||||||
5886|Dynamite Creek Member|39495|6|Mentioned|p142|||||||||
5886|Dynamite Creek Member|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
5886|Dynamite Creek Member|39934|6|Mentioned|Fig.3|||||||||
5886|Dynamite Creek Member|41307|4|Described|p8|||||||||
5886|Dynamite Creek Member|45166|5|Briefly described|p15|||||||||
5886|Dynamite Creek Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin||Lower Haslingden Group|||Pink to buff, fine to coarse labile sandstone, conglomerate|
5886|Dynamite Creek Member|67539|5|Briefly described|p3, p4 Fig.3|||||Of the Eastern Creek Volcanics.|||Contains up to a 200m sequence of conglomerate and conglomerate lenses in sandstone with cobbles and boulders of granite and porphyry.|
5886|Dynamite Creek Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
5886|Dynamite Creek Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Is overlain by Cromwell Metabasalt Member.|Pink to buff, fine- to coarse-grained labile sandstone and conglomerate.|
5886|Dynamite Creek Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Is overlain by Cromwell Metabasalt Member.|Pink to buff, fine- to coarse-grained labile sandstone and conglomerate.|
5887|Dyraaba Member|23032|5|Briefly described|p33|||||||||
5887|Dyraaba Member|23424|5|Briefly described|Table 8.1|Early Carboniferous|Late Devonian|Of Teddy Mount Formation/Bundock Creek Group, Bundock Basin.||||||
5887|Dyraaba Member|41260|3|Fully described|p91|||Reserved as Dyraaba Formation.||||||23-MAR-15
5887|Dyraaba Member|41679|6|Mentioned|Fig.2|||||||||
5887|Dyraaba Member|41719|6|Mentioned|Fig.2|||||||||
5887|Dyraaba Member|41739|2|Defined|p304|early Tournaisian||||||||
5887|Dyraaba Member|41740|6|Mentioned|p222|||||||||
5887|Dyraaba Member|42054|6|Mentioned|p273|||||||||
5887|Dyraaba Member|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
5887|Dyraaba Member|42709|6|Mentioned|map legend|||||||||
5887|Dyraaba Member|42933|3|Fully described|p169|||Of Teddy Mount Formation.||||||25-MAR-08
5887|Dyraaba Member|68336|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Teddy Mount Formation.|||Fine- to medium-grained, micaceous, calcareous, feldspathic to lithofeldspathic sandstone, siltstone and mudstone; abundant plant fragments.|
5887|Dyraaba Member|68341|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Teddy Mount Formation.|||Fine- to medium-grained, micaceous, calcareous, feldspathic to lithofeldspathic sandstone, siltstone and mudstone; abundant plant fragments.|
5887|Dyraaba Member|69592|5|Briefly described|p274|Mississippian|Mississippian|Eastern Bundock Basin, Broken River Province. Paralic deposits.||Teddy Mount Formation.|||Sandstone. Contains abundant plant remains (calamitacean and lycopod affinities); internal moulds of logs are common.|
5891|Eagle Heights Member|40896|6|Mentioned|p5|||||||||
5891|Eagle Heights Member|41824|6|Mentioned|p201|||||||||
5891|Eagle Heights Member|43161|5|Briefly described|12|||||||||
5911|Eastern Creek Volcanics|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546||||||
5911|Eastern Creek Volcanics|22457|4|Described|p31|||Of the Haslingden Group.||||||13-APR-18
5911|Eastern Creek Volcanics|22498|6|Mentioned|Fig1 P234|||||||||
5911|Eastern Creek Volcanics|22514|6|Mentioned|p393|||||||||
5911|Eastern Creek Volcanics|22585|6|Mentioned|P746, Fig1 P736|||||||||
5911|Eastern Creek Volcanics|22644|5|Briefly described|3,5,12|||Geological province: Mount Isa Basin. Of the Haslingden Group. Max thickness 7000 m.||||||30-JAN-07
5911|Eastern Creek Volcanics|22667|6|Mentioned|P238|||||||||
5911|Eastern Creek Volcanics|22747|5|Briefly described|p6||Precambrian|See also Table1,p7. Unconformably overlies Argylla Formation. Unconformably overlain by Corella Formation. Thickness: 6000+m. Part of Soldiers Cap Formation||||||15-AUG-06
5911|Eastern Creek Volcanics|22836|6|Mentioned|Fig.10 p402|||||||||
5911|Eastern Creek Volcanics|23031|6|Mentioned|18|||Geol province Mount Isa Fold Belt. Overlying unit Myally Subgroup. See p 21||||||
5911|Eastern Creek Volcanics|23073|5|Briefly described|p744 (fig 2)|||||||||
5911|Eastern Creek Volcanics|23205|5|Briefly described|p44|||Age: 1700Ma. Of Haslingden Group, Mount Isa Inlier.||||||15-AUG-06
5911|Eastern Creek Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
5911|Eastern Creek Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
5911|Eastern Creek Volcanics|23395|6|Mentioned|p385|||||||||
5911|Eastern Creek Volcanics|23396|5|Briefly described|p407 Fig.2|||||||||
5911|Eastern Creek Volcanics|23399|5|Briefly described|p501|||||||||
5911|Eastern Creek Volcanics|23466|5|Briefly described|p265|||||||||
5911|Eastern Creek Volcanics|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.  Of the Haslingden Group.||||||
5911|Eastern Creek Volcanics|23554|6|Mentioned|pB35 Fig 1|||||||||
5911|Eastern Creek Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Leichhardt Superbasin. See also p1955.||||||
5911|Eastern Creek Volcanics|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
5911|Eastern Creek Volcanics|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
5911|Eastern Creek Volcanics|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
5911|Eastern Creek Volcanics|24033|5|Briefly described|p1, p5, p28|||Includes Lena Quartzite Member and Cromwell Basalt Member.||||||
5911|Eastern Creek Volcanics|24034|6|Mentioned|p9|||Geological Province: Mount Isa Inlier. Flood basalts.||||||
5911|Eastern Creek Volcanics|24168|6|Mentioned|p637|||||||||
5911|Eastern Creek Volcanics|24197|5|Briefly described|p132|||Continental tholeiite. Age: <1870Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
5911|Eastern Creek Volcanics|24253|6|Mentioned|p4|||Geological Province: Mount Isa Block.||||||
5911|Eastern Creek Volcanics|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|24419|5|Briefly described|p16, p12 Fig. 4, p13 Fig. 5|Proterozoic|Proterozoic|Of Haslingden Gp. Massive to strongly cleaved basalt lava flows, with interlayered quartz and feldspathic sandstone, conglomerate and other sedimentary rocks. Conformably underlies Myally Subgroup; conformably overlies Mount Guide Quartzite.||||||18-JAN-07
5911|Eastern Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Mount Guide Quartzite. Overlain by Myally Subgroup. Mafic.||||||
5911|Eastern Creek Volcanics|29961|6|Mentioned|p6|||||||||
5911|Eastern Creek Volcanics|29966|6|Mentioned|p396|||||||||
5911|Eastern Creek Volcanics|29969|6|Mentioned|p393|||||||||
5911|Eastern Creek Volcanics|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.  Underlies the Myally Subgroup.||||||25-AUG-04
5911|Eastern Creek Volcanics|30534|6|Mentioned|p300|||See also p305.||||||15-AUG-06
5911|Eastern Creek Volcanics|30535|6|Mentioned|p403|||||||||
5911|Eastern Creek Volcanics|30536|6|Mentioned|p100|||Stratigraphy||||||
5911|Eastern Creek Volcanics|30558|6|Mentioned|p43|||||||||
5911|Eastern Creek Volcanics|30721|6|Mentioned|p54|||Precambrian||||||
5911|Eastern Creek Volcanics|30723|5|Briefly described|p340|||See also p347,348. U-Th-Pb plot.||||||15-AUG-06
5911|Eastern Creek Volcanics|30725|5|Briefly described|p574|||Lower Proterozoic||||||
5911|Eastern Creek Volcanics|30912|6|Mentioned|p365|||||||||
5911|Eastern Creek Volcanics|31207|6|Mentioned|p1416|||||||||
5911|Eastern Creek Volcanics|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|31821|6|Mentioned|p1024|||||||||
5911|Eastern Creek Volcanics|31824|6|Mentioned|p32|||L.Proterozoic||||||
5911|Eastern Creek Volcanics|32041|4|Described|p358|||||||||
5911|Eastern Creek Volcanics|32042|5|Briefly described|p35|||||||||
5911|Eastern Creek Volcanics|32211|6|Mentioned|p12|||Stratigraphy||||||
5911|Eastern Creek Volcanics|32264|5|Briefly described|p383|||||||||
5911|Eastern Creek Volcanics|32287|6|Mentioned|p18|||||||||
5911|Eastern Creek Volcanics|32660|5|Briefly described|Table 5|||||||||
5911|Eastern Creek Volcanics|32951|6|Mentioned|Table 1|||||||||
5911|Eastern Creek Volcanics|32952|6|Mentioned|p1188|||Precambrian||||||
5911|Eastern Creek Volcanics|32959|6|Mentioned|Fig.21|||See also p31.||||||15-AUG-06
5911|Eastern Creek Volcanics|33214|5|Briefly described|p1277|||Age discussed||||||
5911|Eastern Creek Volcanics|33482|6|Mentioned|Fig.4|||||||||
5911|Eastern Creek Volcanics|33893|5|Briefly described|p22|||See also pp30-31.||||||15-AUG-06
5911|Eastern Creek Volcanics|33894|6|Mentioned|Table 2|||||||||
5911|Eastern Creek Volcanics|33896|5|Briefly described|p457|||||||||
5911|Eastern Creek Volcanics|33897|6|Mentioned|p1280|||||||||
5911|Eastern Creek Volcanics|33900|4|Described|p11|||Mention p10.||||||15-AUG-06
5911|Eastern Creek Volcanics|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|34499|6|Mentioned|Table 1|||||||||
5911|Eastern Creek Volcanics|34955|6|Mentioned|p227|||||||||
5911|Eastern Creek Volcanics|35074|6|Mentioned|Fig.2|||||||||
5911|Eastern Creek Volcanics|35115|6|Mentioned|Fig.1|||||||||
5911|Eastern Creek Volcanics|35116|6|Mentioned|p180|||||||||
5911|Eastern Creek Volcanics|35121|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|35139|4|Described|Table.2|||||||||
5911|Eastern Creek Volcanics|35146|6|Mentioned|p469|||||||||
5911|Eastern Creek Volcanics|35167|6|Mentioned|p151|||||||||
5911|Eastern Creek Volcanics|35286|6|Mentioned|Fig.17|||||||||
5911|Eastern Creek Volcanics|35295|6|Mentioned|p602|||||||||
5911|Eastern Creek Volcanics|35495|6|Mentioned|p341|||||||||
5911|Eastern Creek Volcanics|35892|6|Mentioned|p370|||||||||
5911|Eastern Creek Volcanics|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|36308|6|Mentioned|p209|||||||||
5911|Eastern Creek Volcanics|36548|6|Mentioned|p513|||||||||
5911|Eastern Creek Volcanics|36733|6|Mentioned|p12|||||||||
5911|Eastern Creek Volcanics|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|37459|6|Mentioned|p423|||||||||
5911|Eastern Creek Volcanics|37568|5|Briefly described|p81|||See also p84.||||||15-AUG-06
5911|Eastern Creek Volcanics|37572|6|Mentioned|Fig.8|||||||||
5911|Eastern Creek Volcanics|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|37862|6|Mentioned|p581|||See also P586.||||||
5911|Eastern Creek Volcanics|38232|6|Mentioned|p81|||||||||
5911|Eastern Creek Volcanics|38233|5|Briefly described|Table 1|||||||||
5911|Eastern Creek Volcanics|38234|4|Described|p103|||||||||
5911|Eastern Creek Volcanics|38236|6|Mentioned|p120|||||||||
5911|Eastern Creek Volcanics|38276|6|Mentioned|Fig.1|||||||||
5911|Eastern Creek Volcanics|38348|6|Mentioned|p6|||||||||
5911|Eastern Creek Volcanics|38350|4|Described|p9|||||||||
5911|Eastern Creek Volcanics|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Haslingden Group.  Overlies Mount Guide Quartzite.||||||25-AUG-04
5911|Eastern Creek Volcanics|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|38544|6|Mentioned|p295|||||||||
5911|Eastern Creek Volcanics|38557|5|Briefly described|p289|||||||||
5911|Eastern Creek Volcanics|38560|6|Mentioned|p112|||||||||
5911|Eastern Creek Volcanics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|38834|6|Mentioned|p162|||||||||
5911|Eastern Creek Volcanics|38900|6|Mentioned|p59|||||||||
5911|Eastern Creek Volcanics|38919|6|Mentioned|p493|||||||||
5911|Eastern Creek Volcanics|39125|6|Mentioned|p163|||||||||
5911|Eastern Creek Volcanics|39202|6|Mentioned|p242|||||||||
5911|Eastern Creek Volcanics|39362|6|Mentioned|p1468|||||||||
5911|Eastern Creek Volcanics|39445|5|Briefly described|p41|||See also p35 and Table 2.||||||15-AUG-06
5911|Eastern Creek Volcanics|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Pickwick Metabasalt and Lena Quartzite Members.  Underlies the Alsace Quartzite.||||||10-AUG-04
5911|Eastern Creek Volcanics|39602|6|Mentioned|p602|||||||||
5911|Eastern Creek Volcanics|39622|6|Mentioned|p19|||||||||
5911|Eastern Creek Volcanics|39798|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
5911|Eastern Creek Volcanics|39925|6|Mentioned|p334|||||||||
5911|Eastern Creek Volcanics|39934|4|Described|p317|||||||||
5911|Eastern Creek Volcanics|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|40202|6|Mentioned|p719|||||||||
5911|Eastern Creek Volcanics|40221|3|Fully described|p7|||||||||
5911|Eastern Creek Volcanics|40394|6|Mentioned|p284|||||||||
5911|Eastern Creek Volcanics|40598|6|Mentioned|p38|||||||||
5911|Eastern Creek Volcanics|40623|5|Briefly described|p95|||Briefly described p98.||||||15-AUG-06
5911|Eastern Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
5911|Eastern Creek Volcanics|41125|6|Mentioned|p10|||See also P45||||||
5911|Eastern Creek Volcanics|41248|5|Briefly described|p74|||||||||
5911|Eastern Creek Volcanics|41277|6|Mentioned|Fig.5|||||||||
5911|Eastern Creek Volcanics|41298|6|Mentioned|Map legend|Carpentarian||||||||
5911|Eastern Creek Volcanics|41307|4|Described|p8|||||||||
5911|Eastern Creek Volcanics|41465|5|Briefly described|p11|||||||||
5911|Eastern Creek Volcanics|41802|5|Briefly described|p530|||||||||
5911|Eastern Creek Volcanics|41978|6|Mentioned|p494|||||||||
5911|Eastern Creek Volcanics|41979|6|Mentioned|p537|||||||||
5911|Eastern Creek Volcanics|42072|4|Described|p1618|||||||||
5911|Eastern Creek Volcanics|42110|5|Briefly described|p131|||||||||
5911|Eastern Creek Volcanics|42166|6|Mentioned|p110|||||||||
5911|Eastern Creek Volcanics|42197|6|Mentioned|p238|||||||||
5911|Eastern Creek Volcanics|42367|5|Briefly described|p27|||Of the Haslingdon Group.||||||30-JAN-07
5911|Eastern Creek Volcanics|42503|6|Mentioned|p336|||||||||
5911|Eastern Creek Volcanics|42523|5|Briefly described|Fig.2 P373|||||||||
5911|Eastern Creek Volcanics|42565|5|Briefly described|Table 1 P5, P2|||||||||
5911|Eastern Creek Volcanics|42661|6|Mentioned|p96|||McArthur Basin||||||
5911|Eastern Creek Volcanics|42676|5|Briefly described|Fig.2 P41|||||||||
5911|Eastern Creek Volcanics|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Haslingden Group. Mafic lava: minor clastic sedimentary rocks.||||||09-FEB-09
5911|Eastern Creek Volcanics|42772|6|Mentioned|p17|||||||||
5911|Eastern Creek Volcanics|42782|5|Briefly described|p457|||see also Fig.1 p459.||||||30-JAN-07
5911|Eastern Creek Volcanics|42812|6|Mentioned|p65|||||||||
5911|Eastern Creek Volcanics|42818|4|Described|p206, Table 1 p207|||Of Haslingden Group.||||||15-AUG-06
5911|Eastern Creek Volcanics|43608|6|Mentioned|Fig.11,p11|||||||||
5911|Eastern Creek Volcanics|43616|6|Mentioned|p3|||||||||
5911|Eastern Creek Volcanics|43760|5|Briefly described|p431|||||||||
5911|Eastern Creek Volcanics|43788|6|Mentioned|p20|||||||||
5911|Eastern Creek Volcanics|43928|6|Mentioned|23|||||||||
5911|Eastern Creek Volcanics|43972|14|Not recorded|p7|||||||||
5911|Eastern Creek Volcanics|44162|14|Not recorded|p35,37||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44195|5|Briefly described|p358|||||||||
5911|Eastern Creek Volcanics|44210|2|Defined|map,Tb.1,p8-11,14-5|||||||||
5911|Eastern Creek Volcanics|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44271|14|Not recorded|p33|||||||||
5911|Eastern Creek Volcanics|44273|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
5911|Eastern Creek Volcanics|44276|2|Defined|p10,17,Tb.1,map|||||||||
5911|Eastern Creek Volcanics|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44278|2|Defined|Tb.1,2,p4,5,9,map|||||||||
5911|Eastern Creek Volcanics|44279|2|Defined|p4,5,9,map,Tb.1,2|||||||||
5911|Eastern Creek Volcanics|44309|2|Defined|Tb.1,opp.p7,map|||Intruded by Sybella Granite.||||||
5911|Eastern Creek Volcanics|44326|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44361|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44362|4|Described|p5,Tb.1||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44517|14|Not recorded|p234-236|||Overlies Mount Guide Formation.||||||
5911|Eastern Creek Volcanics|44521|14|Not recorded|p1,4,6-14,21-26,32-3||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44522|14|Not recorded|p1,3,4||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44552|14|Not recorded|p24|||||||||
5911|Eastern Creek Volcanics|44749|14|Not recorded|p26|||||||||
5911|Eastern Creek Volcanics|44751|14|Not recorded|p301|||||||||
5911|Eastern Creek Volcanics|44755|2|Defined|p89-93,||Mesoproterozoic|Includes Pickwick Beds, Paroo Beds, Cromwell Beds and Lena Quartzite.||||||
5911|Eastern Creek Volcanics|44765|14|Not recorded|p14-16||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44766|14|Not recorded|p23,25|||Intruded by Kalkadoon Granite.||||||
5911|Eastern Creek Volcanics|44767|14|Not recorded|p763|||Has " a number of quartz veins of supposed hydrothermal origin that contain disseminated crystals of sulfide."||||||
5911|Eastern Creek Volcanics|44769|14|Not recorded|p1284|||||||||
5911|Eastern Creek Volcanics|44788|14|Not recorded|p26|||||||||
5911|Eastern Creek Volcanics|44806|14|Not recorded|p288|||Petrographic descriptions.||||||
5911|Eastern Creek Volcanics|44812|14|Not recorded|p6|||Soils.||||||
5911|Eastern Creek Volcanics|44843|14|Not recorded|p175|||||||||
5911|Eastern Creek Volcanics|44847|14|Not recorded|p652,653|||Uranium||||||
5911|Eastern Creek Volcanics|44854|14|Not recorded|p51|||Mineralisation.||||||
5911|Eastern Creek Volcanics|44919|14|Not recorded|p596,600,Tb.||Carpentarian|||||||
5911|Eastern Creek Volcanics|44920|14|Not recorded|Map Legend,Sheet 2,4||Carpentarian|||||||
5911|Eastern Creek Volcanics|44989|2|Defined|p.73-6|||Tb.II-IV. On many pages. Pls.4,13,14. Tb.VI. (E54-13,14,F54-1,2,5,6,9.).||||||01-SEP-08
5911|Eastern Creek Volcanics|45052|4|Described|p72|||Carpentarian.||||||13-APR-18
5911|Eastern Creek Volcanics|45072|6|Mentioned|p10|||||||||
5911|Eastern Creek Volcanics|45087|5|Briefly described|p105|||Chem. analyses.||||||
5911|Eastern Creek Volcanics|45136|3|Fully described|p47|||||||||
5911|Eastern Creek Volcanics|45161|4|Described|p23|||||||||
5911|Eastern Creek Volcanics|45166|6|Mentioned|p13|||||||||
5911|Eastern Creek Volcanics|45287|14|Not recorded|p.225-230|||Uranium.||||||
5911|Eastern Creek Volcanics|46801|6|Mentioned|p115|||See also Fig. 14||||||
5911|Eastern Creek Volcanics|46859|4|Described|p313|||||||||
5911|Eastern Creek Volcanics|46919|6|Mentioned|p219|||||||||
5911|Eastern Creek Volcanics|46960|6|Mentioned|p219|||||||||
5911|Eastern Creek Volcanics|46962|4|Described|Table 1|||See also Fig.3.||||||
5911|Eastern Creek Volcanics|46995|6|Mentioned|p271|||||||||
5911|Eastern Creek Volcanics|47011|6|Mentioned|p331|||||||||
5911|Eastern Creek Volcanics|47083|4|Described|p5-6||Proterozoic|Consists of three formal members. Of Haslingden Group. Overlain by Myally Subgroup.||||||30-JAN-07
5911|Eastern Creek Volcanics|48906|14|Not recorded|p28|||||||||
5911|Eastern Creek Volcanics|49009|6|Mentioned|p39|||||||||
5911|Eastern Creek Volcanics|49041|6|Mentioned|p8|||||||||
5911|Eastern Creek Volcanics|50100|5|Briefly described|p16-17|Proterozoic|Proterozoic|Of the lower Haslingden Group.  Includes Cromwell Metabasalt, Lena Quartzite and Pickwick Metabasalt Members.  Conformably overlie Mount Guide and Leander Quartzites.  Unconformably overlie Leichhardt Volcanics.  Geological Province: Western Fold Belt.||||||20-JAN-05
5911|Eastern Creek Volcanics|50332|5|Briefly described|p17, p50, p70, p84|Proterozoic|Proterozoic|Includes; Cromwell Metabasalt Member, Lena Quatrzite Member + Pickwick Meatbasalt Member. Conformably overlain by Myally Subgroup, comformably underlain by Mount Guide and Leander Quartzites. Geological Province: Leichhardt River Subprovince.||||||07-FEB-11
5911|Eastern Creek Volcanics|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier.||||||
5911|Eastern Creek Volcanics|50550|4|Described|p1139 Fig.2, p1149||Statherian|Max. thickness: 6-8 km. Min. thickness: ~2 km. Includes continental tholeiitic basalts. Conformably overlain by Myally Subgroup. Geological Province: Western Fold Belt
.||||||20-JUN-22
5911|Eastern Creek Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|Of the Haslingden Group.||||||07-NOV-08
5911|Eastern Creek Volcanics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Haslingdon Group. Metabasalt, amphibolite, sedimentary lenses; minor gneiss, migmatite.||||||11-DEC-13
5911|Eastern Creek Volcanics|60513|6|Mentioned|p289, 290|||Basaltic.||||||
5911|Eastern Creek Volcanics|60558|5|Briefly described|p4 Fig. 3, p12|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
5911|Eastern Creek Volcanics|61204|4|Described|p538, p539, p540 Fig. 1|||Geological Province: Mount Isa Inlier. Of the Haslingden Group. Metabasalts and intercalated metasedimentary rocks.||||||31-MAY-07
5911|Eastern Creek Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
5911|Eastern Creek Volcanics|61922|5|Briefly described|p8, p9 Fig. 3, p20 Fig.12.|||Comprises: lower and upper basaltic units separated by a sandstone layer. Discordantly underlie the Myally Subgroup rocks. Max. thickness: >4km. Geological Province: Mount Isa Inlier/Western Fold Belt.||||||15-AUG-06
5911|Eastern Creek Volcanics|61923|5|Briefly described|p27, p34 Fig.6|||Of the Haslingden Group. Comprises: Cromwell Metabasalt, Lena Quartzite and Pickwick Metabasalt. Overlain by Mount Isa Group. Geological Province: Mount Isa Inlier. See also p29 Fig.2, p30 Fig.3, p32 Fig.4.||||||
5911|Eastern Creek Volcanics|61924|5|Briefly described|p44|||||||||
5911|Eastern Creek Volcanics|61929|5|Briefly described|p128 Fig. 2|||Includes Lena Quartzite and Cromwell Metabasalt.||||||
5911|Eastern Creek Volcanics|61936|5|Briefly described|p193|||Iron-rich continental flood basalt. Overlain by Myally Subgroup. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||
5911|Eastern Creek Volcanics|62084|6|Mentioned|p936 Fig.5, p951 Fig.15|||Leichhardt Superbasin. Shown as Eastern Ck Volcs.||||||
5911|Eastern Creek Volcanics|62287|5|Briefly described|p130, p131|||Metamorphosed basalts and sediments. Overlain by Urquhart Shale.  Geological Province: Mount Isa Inlier.||||||30-JAN-07
5911|Eastern Creek Volcanics|62288|5|Briefly described|p120, p121 Fig. 1, p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1785-1710Ma. Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
5911|Eastern Creek Volcanics|62373|6|Mentioned|p510, p516|||||||||
5911|Eastern Creek Volcanics|62873|4|Described|p691, p693, p707, p709|Paleoproterozoic|Paleoproterozoic|Of Haslingden Gp. Comprises 3 members. Series of copper-rich tholeiitic basalts adj. to giant sediment-hosted Mount Isa copper deposit; intercalated metabasalts and metasedimentary rocks. Age: 1710+/-25Ma and 1807+/-78Ma. Max. thickness: 7km.||||||07-NOV-08
5911|Eastern Creek Volcanics|63023|5|Briefly described|p1025 Fig. 2|||Of Haslingden Group. Overlain by Myally Subgroup (Haslingden Group); underlain by Mount Guide Quartzite (Haslingden Group). Geological Province: Leichardt Superbasin.||||||
5911|Eastern Creek Volcanics|63109|6|Mentioned|p1108, p1111|||Consists of mafic volcanics rocks. Geological Province: Leichhardt and Calvert Superbasin.||||||30-SEP-08
5911|Eastern Creek Volcanics|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Includes; Cromwell Metabasalt Member, Pickwick Metabasalt Member, Lena Quartzite Member. Overlain by Myally Subgroup, underlain by Mount Guide Quartzite.. Thickness: 7000m. Geological Province: Leichhardt Superbasin.||||||07-FEB-11
5911|Eastern Creek Volcanics|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Haslingden Group||Overlies Mount Guide Quartzite. Is overlain by Alsace Quartzite.||
5911|Eastern Creek Volcanics|63114|6|Mentioned|p1253 Fig.2, p1269-1270. |||||||Overlies Mount Guide Quartzite. Is overlain by Alsace Quartzite (Myally Subgroup).||
5911|Eastern Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1290. |||Leichhardt superbasin.||||||
5911|Eastern Creek Volcanics|63116|6|Mentioned|p1297 Fig.2, p1299-1305, p1310 |||Leichhardt superbasin. Material properties detailed. ||||||
5911|Eastern Creek Volcanics|63593|5|Briefly described|p284, p288 Fig.2, p291 Fig.3 and Tb.2 |||Western Fold Belt. The probable source of copper and associated metals ores in the Mount Isa mine. 7000 m thick.|||||Mafic lava, minor sandstone, siltstone and conglomerate.|
5911|Eastern Creek Volcanics|63866|5|Briefly described|p54, p56-p58|||Leichhardt Superbasin.||Myally Supersequence||Equivalent to the Seigal Volcanics and the Buddawadda Basalt. Overlies the Guide Supersequence.|Continental tholeiitic volcanics.|
5911|Eastern Creek Volcanics|63884|5|Briefly described|p14|||Metabasalts. Underlies Mt Isa Group.||||||
5911|Eastern Creek Volcanics|64250|5|Briefly described|p8, p16 fig 6, p19, p21-4|||Western Fold Belt, Mount Isa Inlier. Forms a single Supersequence with the Myally Subgroup.|<1779 +/- 4 Ma|Haslingden Group|Lena Quartzite|Overlies Mount Guide Quartzite. Is overlain by Myally Subgroup.|Mafic lavas.|12-MAY-14
5911|Eastern Creek Volcanics|64367|5|Briefly described|p553|Paleoproterozoic|Paleoproterozoic|Series of Cu-rich tholeiitic basalts,erupted into a continental rift .......Max.thickness: 7km - upper section is Pickwick Member, lower part is Cromwell Member, separated by Lena Quartzite. Age: 1.8Ga. Intruded by Sybella Batholith.||||||07-FEB-11
5911|Eastern Creek Volcanics|64575|6|Mentioned|p656|||||||||
5911|Eastern Creek Volcanics|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
5911|Eastern Creek Volcanics|64726|6|Mentioned|p83 Fig.2.|||||||||
5911|Eastern Creek Volcanics|64744|6|Mentioned|p353 Fig.4, p354, p356, |Statherian|Statherian|Mount Isa Basin. Basaltic volcanics.|1790 Ma.|||Is overlain by Myally Subgroup.||
5911|Eastern Creek Volcanics|64817|6|Mentioned|p373 |Statherian|Statherian|>5 km thick. Mount Isa Basin.|1780 Ma||||Flood basalt sequence.|
5911|Eastern Creek Volcanics|64832|5|Briefly described|p1153, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.Comprises Cromwell Metabasalt Mb (lower) + Pickwick Metabasalt Mmb (upper). Age: 1785-1775Ma. Intruded by Sybella Granite. Geol.Prov: Mt Isa Inlier. Thick series of intercalated metabasalts + metasedimentary rocks.Detailed chemistry.||||||07-FEB-11
5911|Eastern Creek Volcanics|64834|5|Briefly described|p11-16, p31, p33, p35-36|||Leichhardt Superbasin. Western Succession of Mount Isa Basin. Hosts Valhalla U deposit. Thickness: >6 km. Detailed lithology and mineralogy given.|1779¿4 Ma Neumann et al. 2006||Lena Quartzite, (lower part) Cromwell Metabasalt Member, (upper part) Pickwick Formation|Is unconformably overlain by Surprise Creek Formation. Unconformable upper contact.|Volcanics and interbedded conglomerate (with cobble bed) and sandstone; thick sequence of metabasalts that comprise varying amounts of epidote, actinolite, albite, calcite, sphene, chlorite and magnetite.|
5911|Eastern Creek Volcanics|65228|5|Briefly described|p23, Fig.09.|Statherian|Statherian|Leichhardt River Fault Trough.|c.1780 Ma.|||Is overlain unconformably by Surprise Creek Formation.||13-APR-18
5911|Eastern Creek Volcanics|65337|6|Mentioned|p11. |||Correlated with Mitchiebo Volcanics. ||||||
5911|Eastern Creek Volcanics|65387|6|Mentioned|p1, p55-56|Statherian|Statherian||c.1780 Ma (Neumann and Fraser, 2007).|||Equated with Jayah Creek Metabasalt.||04-APR-18
5911|Eastern Creek Volcanics|65396|4|Described|p16, p82, p173, p175, p187, p190, p192|Statherian|Statherian|See also p193-194, p197, p241. Leichhardt Superbasin. Widespread unit in Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough.|<1779 +/- 4 Ma|Haslingden Group|Includes Lena Quartzite|Overlies Mount Guide Quartzite; overlain by Myally Subgroup. Is correlated (possibly) with Kamarga Volcanics.|Mafic lavas.|03-APR-17
5911|Eastern Creek Volcanics|65505|5|Briefly described|979, 981, Fig 9|Proterozoic|Proterozoic.|Age equivalent with the Argylla Formation ~1780 Ma.||||||
5911|Eastern Creek Volcanics|65887|5|Briefly described|p52|Statherian|Statherian|Mount Isa Western Succession. Metatholeiites. ~1760 Ma.||||||
5911|Eastern Creek Volcanics|66302|6|Mentioned|p63|Statherian|Statherian|Has similar chemistry to the Tidnamurkuna and Myola Volcanics. |ca. 1790-1780 Ma (Wyborn et al, 1987)|||||
5911|Eastern Creek Volcanics|66529|5|Briefly described|p2, p32-37, p40, p41       |||Leichhardt Superbasin rift fill. Also appears as Eastern Creek Formation on p32, and Eastern Creek Basalt on p40. Has well-developed regional alteration assemblages; hosts most uranium deposits in the Mount Isa uranium field.|~1780 Ma|||Overlies Mount Guide Quartzite. Overlain by Myally Subgroup.|Continental tholeiite basalt; siliciclastic lenses.|
5911|Eastern Creek Volcanics|66824|6|Mentioned|p133, 135, 139|||||||Overlies Mount Guide Quartzite.||
5911|Eastern Creek Volcanics|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||Unit in Haslingden Group.||||
5911|Eastern Creek Volcanics|67057|5|Briefly described|p462.|Paleoproterozoic|Paleoproterozoic||1780 - 1760 Ma.|||||
5911|Eastern Creek Volcanics|67323|4|Described|p11-14, p16, p24-25, p39, p53|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Of Leichhardt River Domain, basement to Mount Oxide Domain, Mount Isa Inlier. Rocks previously included in this unit have been renamed in this report as the Alpha Centauri Metamorphics. Previously equated with Marraba Volcanics, but the latter are too young. Up to 8km thick.|~1775-1765 Ma.|(Lower) Haslingden Group.|Includes Cromwell Metabasalt Member, Lena Quartzite Member, Pickwick Metabasalt Member.|Is overlain unconformably by Surprise Creek Formation locally. Geophysics suggests this unit may underlie the Myally Subgroup in the far north of Mt Oxide Domain.|Voluminous continental tholeiitic basalt, metabasalt, amygdaloidal basalt, quartzite, tuff, pelitic schist.|
5911|Eastern Creek Volcanics|67497|5|Briefly described|p909||||Age range ~1790-1730 Ma||||Mafic volcanics.|07-MAY-12
5911|Eastern Creek Volcanics|67499|4|Described|pp938-941, pp944-947, p940 Fig.3|Statherian|Statherian|Intruded by the Sybella batholith around 1657 +/- 7 Ma, using SHRIMP zircon dating from samples of the Elizabeth Creek felsic pluton.|1830 Ma|Of the Haslingden Group.|Cromwell Metabasalt Member, Pickwick Metabasalt Member, Lena Quartzite.|Overlain by the Myally Subgroup.|Tholeiitic flood metabasalt and intercalated metasediments.|08-MAY-12
5911|Eastern Creek Volcanics|67539|5|Briefly described|p2, p3, p4 Fig.3, p8, p9 Fig.7|Statherian|Statherian|Recent geochronology indicates that rocks intruded by the Sybella Granite in the southern Ardmore 1:100k Sheet area are not the Eastern Creek Volcanics as previously believed. |~ 1780 Ma||Includes Dynamite Creek Member|Parts intruded by Ewen Granite and Leichhardt Metamorphics, parts appear to unconformably overlie Ewen Granite.||
5911|Eastern Creek Volcanics|67788|6|Mentioned|p22|||Mentioned in a list of units containing braided and low-sinuosity river deposits. Age is given as Precambrian.||||||
5911|Eastern Creek Volcanics|68020|5|Briefly described|p126, p127|||||||In faulted contact with Mount Isa Group, at the mine.|Metamorphosed basic volcanics and pelitic and psammitic metasediments.|
5911|Eastern Creek Volcanics|68021|5|Briefly described|p134, p135 fig 4, p135, 136, p138|Statherian|Statherian|Part of Myally Supersequence, Leichhardt Superbasin, Western Succession. Subaerial or shallow water.|1780 - 1775 Ma|||Overlies Mount Guide Quartzite, overlain by Myally Subgroup, inferred correlation with Marraba Volcanics, Argylla Formation, intruded by Sybella Granite.|Continental flood basalts and interbedded siliciclastic sediment.|
5911|Eastern Creek Volcanics|68542|6|Mentioned|p10|||||Haslingden Group|Includes Cromwell Member|||
5911|Eastern Creek Volcanics|68575|5|Briefly described|p97, p112-113|||Previous equating of this unit with the Oroopoo Metabasalt is called into question by detrital zircon population ages.||||Overlies Mount Guide Quartzite.||
5911|Eastern Creek Volcanics|68576|5|Briefly described|Q_2: p10, p12|Proterozoic|Proterozoic|||Haslingden Group.|||Basalts; fluvial sedimentary interbeds.|
5911|Eastern Creek Volcanics|68732|5|Briefly described|p165|||Associated with the c.1780 Ma Argylla Magmatic Event.||||Correlated with Cone Creek Volcanic Member. Interbedded with the Myally Supersequence.|Basaltic rocks.|30-NOV-17
5911|Eastern Creek Volcanics|69056|6|Mentioned|p52-53|||Western Mount Isa Inlier. Previously equated with Marraba Volcanics in the Mitakoodi Domain, but this latter unit is much younger.||||||
5911|Eastern Creek Volcanics|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|||Leichhardt River Fault Trough.|||Includes Lena Quartzite, Cromwell Metabasalt|Overlies Mount Guide Quartzite, overlain by Myally Subgroup|Voluminous continental tholeiites.|
5911|Eastern Creek Volcanics|69433|6|Mentioned|p18:6|||Mount Isa Inlier.||||Correlated with Mitchiebo Volcanics.||12-JUL-16
5911|Eastern Creek Volcanics|69542|5|Briefly described|p132, p133 Fig.2, p135|Mesoproterozoic|Paleoproterozoic|Western Fold Belt. Abbreviated in the text to ECV.||Haslingden Group|||Tholeiitic basalt and metabasalts.|09-FEB-18
5911|Eastern Creek Volcanics|69591|4|Described|p33-35, p38, p41, p45, p49, p57|||Wilson, Derrick and Perkins (1984). Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Up to 8km thick in basin depocentres. Eruption may have been synchronous with Argylla Formation. Correlation with Seigal Volcanics is speculative.|1779 +/- 4 Ma (MDA: Neumann et al., 2006).|Haslingden Group.||Is overlain by Myally Subgroup. Is equated with Buddawadda Basalt Member (Peters Creek Volcanics). Is faulted against Mount Isa Group.|Voluminous Fe-rich continental flood basalt: metabasalt, amygdaloidal basalt, quartzite, tuff, pelitic schist. Highly magnetic.|
5911|Eastern Creek Volcanics|70282|5|Briefly described|p544 Fig.1, p546, p551|||Cover sequence 2, Mount Isa. Up to 6km thick.|1790-1760 Ma (or 1720 Ma)|||Overlies Mount Guide Quartzite. Is overlain by Myally Subgroup. Overlain by Urquhart Shale|Basaltic; extensive.|13-FEB-18
5911|Eastern Creek Volcanics|70283|5|Briefly described|p24-26, p31-33|Paleoproterozoic|Paleoproterozoic|Biotite, muscovite ages discussed. Appears as Eastern Creek volcanics on p33.||Haslingden Group|||Metabasalt and interbedded sandstone.|14-FEB-18
5911|Eastern Creek Volcanics|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Dynamite Creek, Cromwell Metabasalt, Lena Quartzite, Pickwick Metabasalt, Members.|Is overlain by Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist.|
5911|Eastern Creek Volcanics|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Dynamite Creek, Cromwell Metabasalt, Lena Quartzite, Pickwick Metabasalt, Members.|Is overlain by Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist.|
5911|Eastern Creek Volcanics|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.|1780-1775 Ma.|||||
5911|Eastern Creek Volcanics|71348|6|Mentioned|p217|||Geological province: North Australian Craton. Formed in a back-arc setting consistent with mafic and bimodal magmatism.||||||
5911|Eastern Creek Volcanics|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform, Mount Isa Inlier.||||Overlain by Myally Subgroup. Underlain by Leichardt Volcanics and Kalkadoon Granite. Equivalent to Haslingden Group.||
5911|Eastern Creek Volcanics|71799|5|Briefly described|p150 fig 2, p151 fig 3|Statherian|Statherian|Lawn Hill. Ages are derived from underlying  Lena Quartzite and overlying Myally Supersequence. Geochemistry is discussed. See also p152, p153 tbl 1, p154, p156-p158, p162, p165.|ca 1775 Ma||Includes the Cromwell Metabasalt Member, Lena Quartzite Member and Pickwick Metabasalt Member.|Overlies the Mount Guide Formation.|Basalt, dolerite, gabbro or amphibolite.|
5911|Eastern Creek Volcanics|71960|5|Briefly described|p77, 78, 81, 82, 83, 85, 86, 95,103,105|Proterozoic|Proterozoic|~3km thick east of Hero Syncline.||Of Haslingden Group.|Includes Cromwell Metabasalt?|Unconformably overlain/truncated by lower Mount Isa Group in Hero Syncline.||
5911|Eastern Creek Volcanics|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Fluviolacustrine between basalt flows.||Of Haslingden Group|Includes Pickwick Metabasalt Member, Lena Quartzite Member, Cromwell Metabasalt Member, Native Bee Siltstone|Underlies Myally Subgroup.|metabasalt; fluviolacustrine sandstone between basalt flows.|
5911|Eastern Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||||Overlies Mount Guide Quartzite and underlies Alsace Quartzite.||
5911|Eastern Creek Volcanics|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Includes an epidotic quartzite and meta-arenite conglomerate marker bed and two other informal subdivisions.||Haslingden Group||Underlies Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist. Epidotic quartzite, meta-arenite conglomerate. Quartz sandstone, feldspathic quartzite, conglomerate, epidote quartzite; minor dolomitc sst. Schist, quartzite, amphibolite.|
5911|Eastern Creek Volcanics|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Includes an epidotic quartzite and meta-arenite conglomerate marker bed and two other informal subdivisions.||Haslingden Group||Underlies Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist. Epidotic quartzite, meta-arenite conglomerate. Quartz sandstone, feldspathic quartzite, conglomerate, epidote quartzite; minor dolomitc sst. Schist, quartzite, amphibolite.|
5911|Eastern Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Statherian|Part of the Leichhradt Superbasin. Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Guide Supersequence||Overlies Mount Guide Quartzite and partially overlies Bottletree Formation.|Includes continental flood basalts.|
5911|Eastern Creek Volcanics|72919|6|Mentioned|p63|||||Myally Supersequence||||
5911|Eastern Creek Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||||Partly underlain by Mount Guide Quartzite. Overlain by Alsace Quartzite (Myally Subgroup).||
5911|Eastern Creek Volcanics|73083|6|Mentioned|p74|||||||||
5911|Eastern Creek Volcanics|73525|5|Briefly described|p2 Fig.1, p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|<1779+/-4 Ma maximum depositional age||||Mafic extrusives, includes clastics, siliciclastics.|
5911|Eastern Creek Volcanics|73553|5|Briefly described|p125-126, p231-232|||Western Succession.|||Cromwell Metabasalt Member||Tholeiitic continental flood basalts.|
5953|Eddystone beds|13516|6|Mentioned|p159 fig 8, p169 fig 11|Late Triassic|Late Triassic|From Bowen Basin||||||
5953|Eddystone beds|23799|6|Mentioned|p48 Fig. 3|Late Triassic|Late Triassic|Geological Province: Surat Basin.||||||
5953|Eddystone beds|42493|5|Briefly described|p20, Fig.1 p18|||||||||
5953|Eddystone beds|60999|6|Mentioned|p176|||Geological Province: Surat Basin. May be equivalent to part of the Raceview Formation. ||||||
5953|Eddystone beds|63218|6|Mentioned|p211 Fig.2. |Late Triassic|Late Triassic|Surat Basin.||||||
5953|Eddystone beds|63979|6|Mentioned|p31|||Geological province: Surat Basin.||||||07-FEB-11
5953|Eddystone beds|64665|6|Mentioned|p53 Fig.2.|Late Triassic|Late Triassic|||||||
5953|Eddystone beds|64856|4|Described|p78-80|Rhaetian|Norian|Price et al. (1985). Informal name for latest Triassic strata in the Surat Basin. Included in overlying Precipice Sandstone in past. Sandstone, also mudstone and coal. Unconformably overlies the Rewan Group and Moolayember Formation. Contains palynoflora of APT5211 age.| | ||||28-NOV-17
5953|Eddystone beds|65112|6|Mentioned|Fig 11 p324|Late Triassic|Late Triassic|Underlies the Precipice Sandstone- relationship unknown.||||||14-SEP-09
5953|Eddystone beds|65113|5|Briefly described|Fig 4 p340|Late Triassic|Late Triassic|Denison Trough.||||||08-MAY-13
5953|Eddystone beds|65114|5|Briefly described|p385 Fig.3|Late Triassic||||||||
5953|Eddystone beds|65116|6|Mentioned|Fig 2 p437|Late Triassic|Late Triassic|Surat Basin.||||||
5953|Eddystone beds|66915|5|Briefly described|p6 Fig.3|Late Triassic|Late Triassic|Surat Basin.||||||
5953|Eddystone beds|68117|6|Mentioned|p346|Late Triassic|Late Triassic|Surat Basin.||||||
5953|Eddystone beds|68576|5|Briefly described|Q_4: p1, p3|Late Triassic|Late Triassic|Basal Surat Basin. Discontinuous, remnant pods.||||Is overlain unconformably by Precipice Sandstone.||
5953|Eddystone beds|68731|6|Mentioned|p201 Fig 3.110|Late Triassic|Late Triassic|||||||
5953|Eddystone beds|69594|5|Briefly described|p519, p524, p534-535, p545, p572|Rhaetian|Rhaetian|Price et al. (1985); first recognised by McKellar (1978). Basal (northern) Surat Basin. Up to 16m thick. Recognised only in bore holes.||||Unconformably overlies Rewan and Moolayember Formations. Is overlain unconformably by Precipice Sandstone. Equivalent to Raceview Formation and Aberdare Conglomerate.|Dominated by sandstone, with mudstone and coal in the upper parts.|
5953|Eddystone beds|69633|5|Briefly described|p3, p11|Late Triassic|Late Triassic|Surat Basin.||||Is overlain unconformably by Precipice Sandstone.||
5953|Eddystone beds|69681|6|Mentioned|p74 Fig.3|Rhaetian|Rhaetian|||||||
5953|Eddystone beds|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Northern Surat Basin.||||||
5953|Eddystone beds|70374|6|Mentioned|p809 figure 1|Hettanginian|Hettanginian|||||||
5985|Edkins Formation|22731|6|Mentioned|p536||Tertiary|||||||
5985|Edkins Formation|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5985|Edkins Formation|37607|4|Described|p333|||See also Fig.4.||||||
5985|Edkins Formation|39445|5|Briefly described|Table 14|||||||||
5985|Edkins Formation|44222|14|Not recorded|p121||Tertiary|?Tertiary, Unconformably on Winton Formation.||||||
5985|Edkins Formation|44406|14|Not recorded|p6,12,opp.p6||Tertiary|Fluviatile (current deposition) fossil tributary of Diamantina R||||||
5985|Edkins Formation|44413|14|Not recorded|p470,474||Tertiary|||||||
5985|Edkins Formation|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Geological region: Diamantina.||||||03-MAR-10
5985|Edkins Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Fluviatile white and red interlaminated quartzose sandstone and siltstone, thin pebble bands and conglomerate; duricrusted.|
5985|Edkins Formation|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit and the Werite beds are mapped under the symbol Ts: mostly unnamed sedimentary rocks.||||||
5985|Edkins Formation|69599|5|Briefly described|p580, p584, p600|Eocene|Paleocene|Vine (1964). Caps a line of small hills for 30km WNW of Kynuna. Up to 7m thick. Fluviatile. No known fossils. Capped by the Canaway profile.||||Unconformably overlies (weathered) Winton Formation. Correlated (at least partly) with Eyre, Glendower, Moonie, Springvale, Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.|Coarse sandstone, conglomerate and siltstone. Weathered and silcretised.|
5994|Edward River Metamorphic Group|22533|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|in Coen Region||||||
5994|Edward River Metamorphic Group|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||12-JAN-05
5994|Edward River Metamorphic Group|22781|3|Fully described|p16|Proterozoic|Proterozoic|Savannah Province||||||
5994|Edward River Metamorphic Group|22811|5|Briefly described|p597, Fig.2 p598|Mesoproterozoic|Mesoproterozoic|of Savannah Province||||||
5994|Edward River Metamorphic Group|23420|4|Described|p 123|Mesoproterozoic|Mesoproterozoic|Also see p 142 table 4.4. Older than 1563Ma, younger than 407Ma. Correlates with the lower part of the Holroyd Group. Previously included in the Holroyd Metamorphics. Savannah Province. Thickness >3200 m.||||||12-JAN-05
5994|Edward River Metamorphic Group|23425|5|Briefly described|p370.|||||||||
5994|Edward River Metamorphic Group|23430|5|Briefly described|p454|||Savannah Province.||||||
5994|Edward River Metamorphic Group|23431|6|Mentioned|p535|||Savannah Province.||||||
5994|Edward River Metamorphic Group|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|||||||
5994|Edward River Metamorphic Group|42610|6|Mentioned|p4|||Not var on Edward Albert Group, NT or use of reserved name "Edwards".||||||
5994|Edward River Metamorphic Group|43287|6|Mentioned|Map Legend||Paleozoic|||||||07-NOV-08
5994|Edward River Metamorphic Group|43596|4|Described|p6 Fig. 6, p15, p20 Tb. 1||Mesoproterozoic|Part of Savannah Province, tog. with Coen + Staaten Metamorphic Groups, + Holroyd Group. Thickness: 3200m.  Geol.prov: western edge of Coen Inlier. Has fault contact with Holroyd Group in west. Was previously included in the Holroyd Metamorphics of Willmott et al. (1973).||||||07-APR-15
5994|Edward River Metamorphic Group|43665|4|Described|p8||Proterozoic|||||||
5994|Edward River Metamorphic Group|43738|6|Mentioned|p5||Proterozoic|||||||
5994|Edward River Metamorphic Group|43820|5|Briefly described|Map Legend||Mesoproterozoic|||||||
5994|Edward River Metamorphic Group|63866|5|Briefly described|p79, p81|||Savannah Subprovince, Coen Region. Referred to as the Edward River Metamorphics on p79. Crops out along the western edge of the Coen Inlier and adjoins the Holroyd Group along the Cattle Swamp Shear Zone. No geochronological constraints on the age of this group exist but they are interpreted to be equivalent to the Holroyd Group.|||||Fine-grained clastic sediments.|
5994|Edward River Metamorphic Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||||Correlates with Holroyd and (at least the upper part of) Coen Metamorphic Groups.||
5994|Edward River Metamorphic Group|69591|5|Briefly described|p74 Fig.2.71, p76-79|Mesoproterozoic|Mesoproterozoic|Elongate N-S belt (>170 km2) along W margin of Coen Inlier, Etheridge Province. The rocks were previously included in the Holroyd Metamorphics (Willmott et al., 1973). At least 3200m thick. Extends under the Carpentaria and Karumba Basins. There are five defined units (Blewett et al., 1992; Blewett et al., 1995) and three unnamed concealed units. May be equivalent to the Holroyd Group. Possible shallow-marine intracontinental deposits.|||Potallah, Olkolo, Drovers Lagoon, O'Lane and Crosbie Formations.||Mostly low-grade slate and quartzite, some schist and mafic rock.|
5994|Edward River Metamorphic Group|71792|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Savannah Province.||||||
5997|Eerwah Vale Tonalite|23190|6|Mentioned|p11,Fig10p16,39||Triassic|||||||
5997|Eerwah Vale Tonalite|23251|5|Briefly described|Table 5 p32||Late Triassic|Intrudes Carol Creek Rhyolite, Kin Kin beds and other units of North Arm Volcanics.||||||21-JUN-06
5997|Eerwah Vale Tonalite|35101|3|Fully described|p77|||Variation of Eerwahvale?||||||
5997|Eerwah Vale Tonalite|39445|5|Briefly described|Table 12|||||||||
5997|Eerwah Vale Tonalite|40051|4|Described|p9|||||||||
5997|Eerwah Vale Tonalite|42695|5|Briefly described|Fig.2|Triassic||||||||
5997|Eerwah Vale Tonalite|42764|4|Described|p28|||||||||
5997|Eerwah Vale Tonalite|42801|6|Mentioned|Fig.2 P82|||||||||
5997|Eerwah Vale Tonalite|42902|5|Briefly described|Fig.1 P416|||||||||
5997|Eerwah Vale Tonalite|43077|5|Briefly described|p5|||||||||
5997|Eerwah Vale Tonalite|43100|3|Fully described|p59||Late Triassic|Implied Late Triassic or younger age.||||||
5997|Eerwah Vale Tonalite|44925|5|Briefly described|Map Legend||Late Triassic|||||||
5997|Eerwah Vale Tonalite|44928|5|Briefly described|Map Legend||Late Triassic|||||||
5997|Eerwah Vale Tonalite|68679|5|Briefly described|p429|Late Triassic|Late Triassic|Sunshine Coast hinterland, northern New England Orogen. A small, elongate body.||||Intrudes North Arm Volcanic Group.|Tonalite and diorite.|
5997|Eerwah Vale Tonalite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
6010|Eight Mile Plains Basalt Member|29720|6|Mentioned|p79|||||||||
6010|Eight Mile Plains Basalt Member|31132|6|Mentioned|p150|||||||||
6010|Eight Mile Plains Basalt Member|38074|6|Mentioned|p14|||||||||
6010|Eight Mile Plains Basalt Member|38441|6|Mentioned|Map legend|Eocene|Eocene|||||||
6010|Eight Mile Plains Basalt Member|41906|3|Fully described|Table 4 P33|||||||||
6010|Eight Mile Plains Basalt Member|42417|5|Briefly described|p229|||45.7 Ma K/Ar||||||
6010|Eight Mile Plains Basalt Member|44687|2|Defined|p225,226|Oligocene|Oligocene|Upper member of Corinda Formation. [Replaces Eight Mile Plains Basalt]. Age: ?Oligocene.||||||21-MAR-13
6010|Eight Mile Plains Basalt Member|44703|14|Not recorded|Map|||||||||
6010|Eight Mile Plains Basalt Member|44704|14|Not recorded|p1,4,7,8|||||||||
6010|Eight Mile Plains Basalt Member|44708|14|Not recorded|Unknown (183pp)|||Not listed on white card.||||||
6010|Eight Mile Plains Basalt Member|45087|6|Mentioned|p171|||Chem. analyses.||||||
6010|Eight Mile Plains Basalt Member|69599|5|Briefly described|p595|Eocene|Paleocene|Oxley Basin. Up to 43m thick.|46.9 +/- 1.0 Ma (Green and Stevens, 1975).|Corinda Formation.||||
6018|Einasleigh Metamorphics|9539|5|Briefly described|Map legend|Proterozoic|Proterozoic|Age: Mid-Proterozoic?||||||07-JUL-04
6018|Einasleigh Metamorphics|9541|5|Briefly described|Map legend|Proterozoic|Proterozoic|Biotite gneiss, calc-silicate gneiss.  Age: Early or Middle Proterozoic.||||||07-JUL-04
6018|Einasleigh Metamorphics|22533|6|Mentioned|p55|||In Georgetown Region||||||
6018|Einasleigh Metamorphics|22611|6|Mentioned|P189||Mesoproterozoic|||||||
6018|Einasleigh Metamorphics|22630|5|Briefly described|p27|||||||||
6018|Einasleigh Metamorphics|22669|6|Mentioned|P251||Proterozoic|||||||
6018|Einasleigh Metamorphics|22744|5|Briefly described|P6, Table1 P8||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|22844|5|Briefly described|p27,28|||||||||
6018|Einasleigh Metamorphics|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Glen Idol Schist and lower sequence of the Willyama Supergroup.||||||07-NOV-08
6018|Einasleigh Metamorphics|23032|4|Described|p8,9,49|Paleoproterozoic|Paleoproterozoic|Deformed 1550-1560 Ma.||||||07-NOV-08
6018|Einasleigh Metamorphics|23074|5|Briefly described|p739||Proterozoic|||||||
6018|Einasleigh Metamorphics|23158|5|Briefly described|p811|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|23220|5|Briefly described|Fig.1,2 p8||Proterozoic|Age: ~1700Ma +/- 100Ma. Correlate of Juntala Metamorphics and Corbett Formation. Of the Etheridge Group.||||||15-JAN-07
6018|Einasleigh Metamorphics|23291|4|Described|p86 Tb. 3.6, p22|Paleoproterozoic|Paleoproterozoic|Stratigraphic equivalent to Bernecker Creek Formation. Of the Etheridge Group. Geological Province: Georgetown Region.||||||08-JUL-15
6018|Einasleigh Metamorphics|23422|6|Mentioned|p167|||||||||
6018|Einasleigh Metamorphics|23429|5|Briefly described|p441|||Also see p438.||||||
6018|Einasleigh Metamorphics|23430|5|Briefly described|p450|||Of Etheridge Group. Etheridge Province.||||||
6018|Einasleigh Metamorphics|23431|5|Briefly described|p530|||Of Etheridge Group. Etheridge Province.||||||15-JAN-07
6018|Einasleigh Metamorphics|23432|5|Briefly described|p547|||Of Forsayth Subprovince.||||||15-JAN-07
6018|Einasleigh Metamorphics|23453|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|23493|5|Briefly described|p7, p19 Tb. 1|Archean|Archean|Gneiss, banded granulite, migmatite garnetiferous quartzite, amphibolite.||||||07-NOV-08
6018|Einasleigh Metamorphics|23494|4|Described|p7, p25 Tb. 1|Precambrian|Precambrian|Migmatite, banded granulite, schist, amphibolite.  Intruded by Cobbold Dolerite, Dumbano Granite.  Geological Province: Georgetown Inlier.||||||
6018|Einasleigh Metamorphics|23495|5|Briefly described|map legend||Archean|Age shown as Archaean?||||||07-NOV-08
6018|Einasleigh Metamorphics|23498|5|Briefly described|p25 table 1||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|23510|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|23616|5|Briefly described|Table 1C p16, p28||Proterozoic|Age: Proterozoic; recent SHRIMP age dating from the Georgetown region suggests an age of ~1690 Ma. Unconformably overlain by Cainozoic Undara Basalt. Dargalong Province.||||||
6018|Einasleigh Metamorphics|23619|4|Described|p37 Table 1||Proterozoic|Older than 1570 Ma. Divided into 4 unnamed members. Georgetown Province.||||||
6018|Einasleigh Metamorphics|23713|5|Briefly described|p8 Table 1||Mesoproterozoic|Georgetown Province.||||||
6018|Einasleigh Metamorphics|23846|5|Briefly described|p4 Fig.2, p5|Proterozoic|Proterozoic|High-grade metamorphics: granulaite, gneiss, migmatite, amphilbolite, schist and quartzite. Free gold occurs in quartz reefs associated with minor galena, pyrite and chalcopyrite.||||||
6018|Einasleigh Metamorphics|24013|5|Briefly described|p19 Tb. 1|Archean|Archean|Gneiss, granulite, migmatite, garnetiferous quartzites, schist.  Correlated with Hall's Reward Metamorphics.||||||07-NOV-08
6018|Einasleigh Metamorphics|24485|5|Briefly described|p1, 25|Neoproterozoic|Neoproterozoic|Age: ~1690-1670Ma (U-Pb SHRIMP zircon).||||||15-JAN-07
6018|Einasleigh Metamorphics|30508|6|Mentioned|p94|||Interrelationships||||||
6018|Einasleigh Metamorphics|30587|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6018|Einasleigh Metamorphics|31832|6|Mentioned|Table 6|||||||||
6018|Einasleigh Metamorphics|31999|6|Mentioned|p127|||Table 111||||||
6018|Einasleigh Metamorphics|32518|4|Described|p765|||||||||
6018|Einasleigh Metamorphics|32528|5|Briefly described|Table 1|||||||||
6018|Einasleigh Metamorphics|32531|6|Mentioned|p476|||||||||
6018|Einasleigh Metamorphics|32553|4|Described|p54|||||||||
6018|Einasleigh Metamorphics|33179|4|Described|Table 1|||||||||
6018|Einasleigh Metamorphics|33180|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6018|Einasleigh Metamorphics|33638|6|Mentioned|p7|||||||||
6018|Einasleigh Metamorphics|33648|6|Mentioned|p7|||Correlation.||||||
6018|Einasleigh Metamorphics|33669|6|Mentioned|p517|||||||||
6018|Einasleigh Metamorphics|33907|5|Briefly described|p4|||||||||
6018|Einasleigh Metamorphics|33909|6|Mentioned|p229|||||||||
6018|Einasleigh Metamorphics|33910|6|Mentioned|p9|||||||||
6018|Einasleigh Metamorphics|34284|6|Mentioned|Table 1|||Archaean.||||||
6018|Einasleigh Metamorphics|34703|6|Mentioned|p23|||||||||
6018|Einasleigh Metamorphics|34955|6|Mentioned|p228|||||||||
6018|Einasleigh Metamorphics|35009|6|Mentioned|p371|||||||||
6018|Einasleigh Metamorphics|35214|6|Mentioned|p4|||||||||
6018|Einasleigh Metamorphics|35429|4|Described|p126|||Granulite facies studied.||||||15-JAN-07
6018|Einasleigh Metamorphics|35920|6|Mentioned|p24|||||||||
6018|Einasleigh Metamorphics|35921|5|Briefly described|p31|||Defined by White 1959.||||||
6018|Einasleigh Metamorphics|35930|6|Mentioned|Fig.1|||||||||
6018|Einasleigh Metamorphics|35948|4|Described|p106|||Deformation and metamorphism p107.||||||15-JAN-07
6018|Einasleigh Metamorphics|36153|6|Mentioned|Fig.10|||||||||
6018|Einasleigh Metamorphics|36555|6|Mentioned|p78|||||||||
6018|Einasleigh Metamorphics|36780|6|Mentioned|Fig.10|||||||||
6018|Einasleigh Metamorphics|37570|4|Described|p113|||See also p109.||||||15-JAN-07
6018|Einasleigh Metamorphics|37571|4|Described|p135|||||||||
6018|Einasleigh Metamorphics|37573|6|Mentioned|Fig.12|||||||||
6018|Einasleigh Metamorphics|37576|5|Briefly described|p8|||||||||
6018|Einasleigh Metamorphics|37768|4|Described|p31|||||||||
6018|Einasleigh Metamorphics|38063|6|Mentioned|p28|||||||||
6018|Einasleigh Metamorphics|38714|6|Mentioned|p182|||||||||
6018|Einasleigh Metamorphics|38715|6|Mentioned|p191|||||||||
6018|Einasleigh Metamorphics|38791|4|Described|p175|||||||||
6018|Einasleigh Metamorphics|38947|5|Briefly described|p22|||||||||
6018|Einasleigh Metamorphics|39027|6|Mentioned|Map legend|Archean|Archean|Prob. Archaean||||||07-NOV-08
6018|Einasleigh Metamorphics|39172|6|Mentioned|p272|||||||||
6018|Einasleigh Metamorphics|39337|6|Mentioned|p339|||||||||
6018|Einasleigh Metamorphics|39445|5|Briefly described|p45|||Correlation. See also Table 2||||||
6018|Einasleigh Metamorphics|39566|6|Mentioned|p51|||||||||
6018|Einasleigh Metamorphics|39687|6|Mentioned|p1|||||||||
6018|Einasleigh Metamorphics|39689|6|Mentioned|Fig.2|||||||||
6018|Einasleigh Metamorphics|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
6018|Einasleigh Metamorphics|39924|4|Described|p341|||||||||
6018|Einasleigh Metamorphics|39981|6|Mentioned|p102|||||||||
6018|Einasleigh Metamorphics|40623|5|Briefly described|p92|||||||||
6018|Einasleigh Metamorphics|40798|5|Briefly described|p236|||||||||
6018|Einasleigh Metamorphics|40961|6|Mentioned|p239|||||||||
6018|Einasleigh Metamorphics|41092|6|Mentioned|Table 1|||||||||
6018|Einasleigh Metamorphics|41260|6|Mentioned|p111|||||||||
6018|Einasleigh Metamorphics|41272|5|Briefly described|p27|||See also M 1of1 I05||||||
6018|Einasleigh Metamorphics|41431|5|Briefly described|p1|||||||||
6018|Einasleigh Metamorphics|41465|6|Mentioned|p14|||||||||
6018|Einasleigh Metamorphics|41574|6|Mentioned|p405|||||||||
6018|Einasleigh Metamorphics|41675|3|Fully described|p7|||||||||
6018|Einasleigh Metamorphics|41680|3|Fully described|p107|||||||||
6018|Einasleigh Metamorphics|41807|5|Briefly described|p62|||||||||
6018|Einasleigh Metamorphics|41916|6|Mentioned|p26|||||||||
6018|Einasleigh Metamorphics|41975|3|Fully described|p435|||||||||
6018|Einasleigh Metamorphics|42199|5|Briefly described|Table 1 P280|||||||||
6018|Einasleigh Metamorphics|42216|5|Briefly described|Fig.1, P425|||||||||
6018|Einasleigh Metamorphics|42279|5|Briefly described|p22|||See also Fig.3||||||
6018|Einasleigh Metamorphics|42344|5|Briefly described|p58||Proterozoic|||||||
6018|Einasleigh Metamorphics|42407|6|Mentioned|p12|||||||||
6018|Einasleigh Metamorphics|42691|5|Briefly described|map legend|Precambrian||||||||
6018|Einasleigh Metamorphics|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|42765|5|Briefly described|p18|||see also p21, of Etheridge Group.||||||15-JAN-07
6018|Einasleigh Metamorphics|42933|5|Briefly described|Fig.72|||||||||
6018|Einasleigh Metamorphics|43060|3|Fully described|p36,Table 1c||Proterozoic|||||||
6018|Einasleigh Metamorphics|43083|6|Mentioned|p17 Tb 1|||Of Etheridge Group. Probably Early Proterozoic.||||||17-JUN-09
6018|Einasleigh Metamorphics|43103|6|Mentioned|p16|||||||||
6018|Einasleigh Metamorphics|43110|4|Described|Table 1.|||?Proterozoic age||||||
6018|Einasleigh Metamorphics|43113|4|Described|Table 1 p23||Paleoproterozoic|Older than 1570 Ma (Black & others,1979)||||||07-NOV-08
6018|Einasleigh Metamorphics|43120|6|Mentioned|p365|||||||||
6018|Einasleigh Metamorphics|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age. Of Etheridge Group.||||||
6018|Einasleigh Metamorphics|43286|5|Briefly described|Map Legend||Proterozoic|Of Etheridge Group.||||||15-JAN-07
6018|Einasleigh Metamorphics|43480|3|Fully described|1-41|||Age: 1700-1650 Ma SHRIMP.||||||15-JAN-07
6018|Einasleigh Metamorphics|43603|5|Briefly described|p6||Proterozoic|||||||
6018|Einasleigh Metamorphics|43625|6|Mentioned|p14,Table 1|||Age: pre-1690 Ma||||||
6018|Einasleigh Metamorphics|43664|3|Fully described|p14-20|||[No type section or locality discussed]||||||20-MAR-18
6018|Einasleigh Metamorphics|43716|6|Mentioned|p21|||||||||
6018|Einasleigh Metamorphics|43772|6|Mentioned|Fig.1,p787||Precambrian|||||||
6018|Einasleigh Metamorphics|44043|14|Not recorded|p63|||||||||
6018|Einasleigh Metamorphics|44047|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|44048|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|44049|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|44059|2|Defined|p442,443,445||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|44091|14|Not recorded|p11||Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|44195|6|Mentioned|p357|||Georgetown region.||||||
6018|Einasleigh Metamorphics|44246|5|Briefly described|Map Legend||Proterozoic|||||||
6018|Einasleigh Metamorphics|44258|14|Not recorded|p7,10,21,27-30||Archean|||||||07-NOV-08
6018|Einasleigh Metamorphics|44516|14|Not recorded|p34,36|||||||||
6018|Einasleigh Metamorphics|44542|14|Not recorded|p26-28|||||||||
6018|Einasleigh Metamorphics|44723|14|Not recorded|p562,563|||||||||
6018|Einasleigh Metamorphics|44883|14|Not recorded|p229|||||||||
6018|Einasleigh Metamorphics|44926|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|45009|2|Defined|p19,21,23-5,27,29,32||Archean|p35,102,111,115,118-9,Tb.2,13,Pl.13. Intruded by Cobbold Dolerite. [No type section or locality discussed]||||||20-MAR-18
6018|Einasleigh Metamorphics|45087|5|Briefly described|p116|||See also p230. Chem. analyses.||||||15-JAN-07
6018|Einasleigh Metamorphics|45113|6|Mentioned|p7|||||||||
6018|Einasleigh Metamorphics|45272|14|Not recorded|p.76||Precambrian|||||||
6018|Einasleigh Metamorphics|48894|6|Mentioned|p50|||Age: 432my, 415my.||||||15-JAN-07
6018|Einasleigh Metamorphics|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
6018|Einasleigh Metamorphics|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
6018|Einasleigh Metamorphics|50200|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|50201|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6018|Einasleigh Metamorphics|50211|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Etheridge Group.||||||07-NOV-08
6018|Einasleigh Metamorphics|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||30-JUL-04
6018|Einasleigh Metamorphics|60081|5|Briefly described|Map legend|Proterozoic|Proterozoic|Gneiss, migmatite, schist, amphibolite.||||||
6018|Einasleigh Metamorphics|60360|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
6018|Einasleigh Metamorphics|61258|5|Briefly described|p386, p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Geological Province: Georgetown Inlier. See also p388 Fig. 2. ||||||07-NOV-08
6018|Einasleigh Metamorphics|63866|4|Described|p75-p77, p79, p85-p87|||Forsayth Subprovince, Etheridge Province. Hosts base metal deposits.|1675 +/- 3 Ma (U-Pb zircon, Black et al., 1998)|Etheridge Group||||
6018|Einasleigh Metamorphics|64250|6|Mentioned|p26|||Hosts the Mount Misery and Railway Flat Pb-Zn-Ag deposits in the Georgetown Block. The precise age of the host rocks is not well defined, although it is likely to be between ca. 1700 and 1675 Ma (Black et al., 1998).||||||19-MAR-18
6018|Einasleigh Metamorphics|64707|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Calc-silicate (hornblende-diopside) gneiss with abundant magnetite, and leucogneiss; biotite gniess, sillimanite-biotite schist and micaceous quartzite grading locally into migmatite; subordinate calc-silicate gneiss and ortho-amphibolite.||||||
6018|Einasleigh Metamorphics|64722|5|Briefly described|p12|Statherian|Statherian|Georgetown-Coen region. Interpreted as metamorphosed epiclastic sediments. Maximum depositional age from detrital zircons. Minimum age from granite intrusion.|1703 +/- 14 Ma to 1695.8 +/- 1.5 Ma.|Lowermost unit of Etheridge Group.||||11-APR-12
6018|Einasleigh Metamorphics|65396|6|Mentioned|p201|||Georgetown Inlier. Hosts the Mount  Misery and Railway Flat Pb-Zn-Ag deposits.|c.1700-1675 Ma.|||||
6018|Einasleigh Metamorphics|65887|5|Briefly described|p40 Fig.1, p41, p44, p47|Statherian|Paleoproterozoic|Calcareous mica-schist, calc-silicate and biotite granofels and quartzite. Intruded by 1675+/-3 Ma amphibolite (Black et al., 1998). Unit in Etheridge Group.||||||
6018|Einasleigh Metamorphics|66529|5|Briefly described|p5, p16, p46   |Proterozoic|Proterozoic|Eastern Etheridge Province. Metamorphosed c.1675 Ma. Much higher metamorphic grade (amphibolite and granulite facies) than rocks in the western part of the Province (greenschist and sub-greenschist). Has elevated U concentrations and is a probable local source. Hosts Cu-Ag-Au deposits with Fe.|Deposition began 1710 Ma.||||Calc-silicate gneisses.|
6018|Einasleigh Metamorphics|66800|4|Described|pp925-929, pp932-933.|Proterozoic|Proterozoic|Eastern subdivision of Etheridge Group. Medium- to high-grade. Mafic rocks in this unit have been correlated with Cobbold Metadolerite on basis of similar chemical composition, and may be related.||Unit in Etheridge Group.|||Biotite-, hornblende-, and hornblende-diopside gneisses, mica schist and quartzite; minor leucocratic quartzo-feldspathic gneiss and amphibolite.|
6018|Einasleigh Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Georgetown-Coen-Yambo Inliers.|Protoliths deposited ~1720-1690 Ma.|Lower Etheridge Group.||||
6018|Einasleigh Metamorphics|67341|5|Briefly described|vi, p32-45|Calymmian|Calymmian|Forsayth Subprovince, Etheridge Province. SHRIMP U-Pb zircon ages of recrystallisation (metamorphism) from three samples.|1559 +/- 3 Ma and 1568 +/- 4 Ma (twice).|||Is overlain by Juntala Metamorphics.|Includes psammitic biotite+quartz gneiss, migmatite, quartz+feldspar+sillimanite+garnet gneiss, leucocratic quartzo-feldspathic gneiss, hornblende-diopside calc-silicate rock.|
6018|Einasleigh Metamorphics|67430|6|Mentioned|p25|||||||||
6018|Einasleigh Metamorphics|67455|4|Described|p574, p577. |Early Mesoproterozoic|Paleoproterozoic|Georgetown Inlier. West of Lynd Mylonite Zone. Part of the Paleoproterozoic to Early Mesoproterozoic craton. Weak foliation trends easterly at a high angle to the Lynd Mylonite Zone.|1700 - 1550 Ma (SHRIMP zircon: Black et al 2005).||||Dominantly biotite gneiss and calc-silicate gneiss; minor leucocratic gneiss.|
6018|Einasleigh Metamorphics|68307|6|Mentioned|p88-89|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Etheridge Group.||||
6018|Einasleigh Metamorphics|68330|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Etheridge Province.|||||Nebulitic to agmatitic migmatite grading into garnetiferous, schlieren-rich, gneissic biotite granite or orthogneiss; subordinate biotite gneiss, sillimanite-biotite schist, quartzite and amphibolite.|
6018|Einasleigh Metamorphics|68338|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||||Gneiss, schist and quartzite grading into migmatite; calc-silicate gneiss often with abundant magnetite; common leucogranite and pegmatite.|
6018|Einasleigh Metamorphics|68344|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||||Calc-silicate gneiss and leucogneiss, biotite gneiss, quartzite, schist, local amphibolite, abundant leucogranite and pegmatite dykes and veins, sillimanite-biotite schist and micaceous quartzite grading locally into migmatite.|
6018|Einasleigh Metamorphics|68346|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Eight facies/associations are mapped separately.|||||Calc-silicate (hornblende-diopside) gneiss, biotite gneiss, schist, quartzite, ortho-amphibolite, mafic granulite, leucogranite and pegmatite dykes and veins.|
6018|Einasleigh Metamorphics|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Ten facies associations are mapped separately.||Unit in Etheridge Group.|||Gneiss, schist, quartzite, leucogranite and pegmatite dykes and veins, amphibolite, migmatite.|
6018|Einasleigh Metamorphics|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Five facies associations are mapped separately.||Unit in Etheridge Group.|||Gneiss, schist, quartzite, leucogranite and pegmatite, amphibolite +/- relict pillow structures, migmatite, local mafic granulite.|
6018|Einasleigh Metamorphics|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Nine facies associations are mapped separately.||Unit in Etheridge Group.|||Gneiss, schist, quartzite, leucogranite and pegmatite dykes and veins, amphibolite, migmatite.|
6018|Einasleigh Metamorphics|68405|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Etheridge Province. ||||Overlain by Lyndbrook Complex. Older than Fig Tree Hill Granite Complex.|Nebulitic to agmatitic migmatite grading into garnetiferous, schlieren-rich, gneissic biotite granite or orthogneiss; subordinate biotite gneiss, sillimanite-biotite schist, quartzite and amphibolite.|
6018|Einasleigh Metamorphics|68410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Contains 9 unnamed subunits.|||||Variety of lithologies including calc-silicate gneisses, often with magnetite; biotite gneiss; mica schist; ortho-amphibolite and mafic granulite; leucogranite and pegmatite dykes and veins.|
6018|Einasleigh Metamorphics|68477|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|The 7 facies are mapped separately. Etheridge Province.||Of the Etheridge Group.|||Ortho-amphibolite, mafic granulite; biotite gneiss, schist and quartzite; migmatite grading into granite or orthogneiss; white quartzite; biotite gneiss and schist with quartzite grading into migmatite and granitoid.|
6018|Einasleigh Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.||Interfingers with Bernecker Creek Formation. Is overlain conformably by Robertson River Subgroup.||
6018|Einasleigh Metamorphics|68576|4|Described|Q_11: p21,p22 Fig.20,p23-25,p27,p29-32|Paleoproterozoic|Paleoproterozoic|Type locality is in the bed of the Einasleigh River below the Einasleigh mine. Is in contact with White Springs Granodiorite at O'Brien's Creek, but the nature of the contact is not specified. East of the Newcastle Range, this unit grades into nebulitic migmatites that resemble the Mistletoe Granite. Hosts numerous small base metal occurrences; thought to be stratabound (briefly described). Peak metamorphism (upper amphibolite to granulite facies) at ~1560 Ma. Includes rocks W of the Lynd Mylonite Zone (=Tasman Line) with ~1700 Ma detrital zircons (cf. Oasis Metamorphics).|||||Includes well-layered, multiply deformed mica schist, quartzite, biotite gneiss and migmatite that passes into nebulitic granite. Amphibolite (~1675 Ma) and metagabbro sills and stocks are also present.|
6018|Einasleigh Metamorphics|68731|5|Briefly described|p115, p153 Fig 3.52, p153 Fig 3.53, p189|Mesoproterozoic|Mesoproterozoic|Georgetown Inlier. Suggested that the Oasis Metamorphics and Lynwater Complex are not part of the Einasleigh Metamorphics as originally thought by Withnall (1989) and Withnall et al. (1997).||||||13-MAY-16
6018|Einasleigh Metamorphics|69591|4|Described|p61-63, p65, p67, p69, p82-84, p107|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. In the Lyndbrook area, some migmatites of this unit have been mapped as the Lyndbrook Complex. Possibly equivalent to Bernecker Creek and Daniel Creek Formations. Grades E and S into the Juntala Metamorphics. Several age determinations given.|~1705 Ma - 1675 +/- 3 Ma.|Etheridge Group.||Is faulted against Juntala Metamorphics. Equivalent to older parts of Forsayth Supersuite.|Characterised by biotite gneiss and calc-silicate gneiss; well-layered; amphibolite common throughout; migmatite common. Pegmatitic and leucocratic granitoid dykes, veins and pods are ubiquitous.|
6018|Einasleigh Metamorphics|69952|5|Briefly described|p5, p61-62, p69-70|Paleoproterozoic|Paleoproterozoic|Withnall (1989); Withnall et al. (1997). Etheridge Province. Probably deposited c.1700 Ma; multiply deformed with a major tectonothermal event at c.1560 Ma. Originally included rocks which were later separated as Oasis Metamorphics (Withnall et al., 2002). These latest age determinations show that the Oasis Metamorphics may in fact correlate with similar rocks in the Einasleigh Metamorphics.||||||
6018|Einasleigh Metamorphics|70207|6|Mentioned|p14|Paleoproterozoic|Paleoproterozoic|Georgetown region.||||||
6018|Einasleigh Metamorphics|70744|5|Briefly described|p937|Mesoproterozoic|Paleoproterozoic|Lynd Mylonite Zone.||||Thrust under Oasis Metamorphics.||
6018|Einasleigh Metamorphics|71592|5|Briefly described|Appendix A.|||Etheridge Province. About 24 age determinations are given, for crystallisation, inheritance, metamorphism, intrusions, recrystallisation and "significance unknown".|1703+/-14 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss, amphiboliote, schist, dacite, granitic gneiss, trondhjemite gneiss, psammite, calc-silicate rock.|
6018|Einasleigh Metamorphics|71799|6|Mentioned|p155 fig 4|||Georgetown Province.||||||
6018|Einasleigh Metamorphics|72297|5|Briefly described|p716|||Etheridge Province. Hosts Ag-Pb-Zn deposits near Georgetown.|||||Epidote- to diopside-bearing quartzite, quartzofeldspathic granofels and gneiss; associated with stratabound concentrations of iron and base metal sulfides.|
6018|Einasleigh Metamorphics|73147|6|Mentioned|p131|||||||||
6018|Einasleigh Metamorphics|73425|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier.||||||
6018|Einasleigh Metamorphics|73527|6|Mentioned|p3 Fig.2|||[Abbreviated as Einasleigh p4 Fig.3, p6, S-type?]||||||
6018|Einasleigh Metamorphics|73642|5|Briefly described|p3 Fig.2, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier. See also Einasleigh Metamorphic Complex p11.|1554+/-10, 1568+/-4 Ma|||||
6018|Einasleigh Metamorphics|75079|5|Briefly described|p2-3, 9-12, 14, 16-18|Paleoproterozoic|Paleoproterozoic|Eastern Georgetown Inlier. The lower Etheridge Group is regarded as the protolith of this unit. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|||||High-grade migmatite.|
6098|Ellinthorpe Clay|42593|5|Briefly described|p300|||||||||
6098|Ellinthorpe Clay|69600|6|Mentioned|p661|Pleistocene|Pleistocene|Sobbe (1990). A unit in limited stratigraphies of sections along creeks in the eastern Darling Downs. Not considered to be a valid stratigraphic unit.||||||
6106|Elliott Formation|23251|5|Briefly described|Table 1 p6|Tertiary|Tertiary|Overlies Tiaro Coal Measures. Geological Province: Elliott Basin province.||||||21-JUN-06
6106|Elliott Formation|23841|4|Described|p440 Fig. 2|Tertiary|Tertiary|Geological Province: Maryborough Basin.  Maximum thickness: ~52m.||||||
6106|Elliott Formation|24382|5|Briefly described|Map legend|Oligocene|Eocene|||||||
6106|Elliott Formation|29420|6|Mentioned|p99|||||||||
6106|Elliott Formation|32774|5|Briefly described|Table 2|||||||||
6106|Elliott Formation|34950|5|Briefly described|p40|||||||||
6106|Elliott Formation|35053|5|Briefly described|p37|||||||||
6106|Elliott Formation|35134|6|Mentioned|p579|||||||||
6106|Elliott Formation|35727|6|Mentioned|p364|||||||||
6106|Elliott Formation|35900|6|Mentioned|p448|||||||||
6106|Elliott Formation|36101|6|Mentioned|p171|||||||||
6106|Elliott Formation|36243|6|Mentioned|Table 9A|||||||||
6106|Elliott Formation|36581|6|Mentioned|Fig.1|||||||||
6106|Elliott Formation|36772|6|Mentioned|p131|||See also P134, 135||||||
6106|Elliott Formation|36926|6|Mentioned|p165|||||||||
6106|Elliott Formation|37120|6|Mentioned|p321|||||||||
6106|Elliott Formation|37618|4|Described|p27|||||||||
6106|Elliott Formation|37861|6|Mentioned|p591|||||||||
6106|Elliott Formation|38308|6|Mentioned|p234|||||||||
6106|Elliott Formation|38309|6|Mentioned|p229|||||||||
6106|Elliott Formation|38391|6|Mentioned|p11|||||||||
6106|Elliott Formation|38397|6|Mentioned|p51|||||||||
6106|Elliott Formation|39315|6|Mentioned|Fig.5|||||||||
6106|Elliott Formation|39445|5|Briefly described|Table 14|||||||||
6106|Elliott Formation|39505|6|Mentioned|p167|||||||||
6106|Elliott Formation|39943|6|Mentioned|Table 11A|||||||||
6106|Elliott Formation|39968|6|Mentioned|p75|||||||||
6106|Elliott Formation|41265|6|Mentioned|Map legend|Tertiary||||||||
6106|Elliott Formation|42617|5|Briefly described|p16|||||||||
6106|Elliott Formation|42636|5|Briefly described|p10|||||||||
6106|Elliott Formation|42895|6|Mentioned|p53|||||||||
6106|Elliott Formation|43059|4|Described|p11,Table 2|||||||||
6106|Elliott Formation|43100|5|Briefly described|p48|||||||||
6106|Elliott Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
6106|Elliott Formation|43995|14|Not recorded|Tb.p10,36|||||||||
6106|Elliott Formation|44068|14|Not recorded|p15|||||||||
6106|Elliott Formation|44117|14|Not recorded|p23|||||||||
6106|Elliott Formation|44167|14|Not recorded|p12,15,map,p22||Tertiary|||||||
6106|Elliott Formation|44239|14|Not recorded|p278|||||||||
6106|Elliott Formation|44240|14|Not recorded|p339|||||||||
6106|Elliott Formation|44243|14|Not recorded|p8-14, Tb.8||Tertiary|Unconformity on Burrum Coal Measures. (Early Tertiary)||||||
6106|Elliott Formation|44581|14|Not recorded|p351,352|||Overlies Gin Gin Basalt, overlain by basalt.||||||
6106|Elliott Formation|44587|14|Not recorded|p383|||Affected by laterisation.||||||
6106|Elliott Formation|44616|14|Not recorded|p32-35|Miocene|Oligocene|Hard, course, feldspathic sandstone with red and grey clayey shales.||||||
6106|Elliott Formation|44752|14|Not recorded|Fig.43,p300||Tertiary|Unconformably overlies Maryborough Formation.||||||
6106|Elliott Formation|44753|14|Not recorded|p48,52,54|Tertiary|Tertiary|(Early Tertiary-Middle Tertiary)||||||
6106|Elliott Formation|44783|14|Not recorded|p2|||||||||
6106|Elliott Formation|44810|14|Not recorded|p167 (Tb.)||Oligocene|||||||
6106|Elliott Formation|44821|14|Not recorded|p34||Tertiary|||||||
6106|Elliott Formation|45168|6|Mentioned|p10|||||||||
6106|Elliott Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|Thickness, together with Takura beds: 50m. In the Bundaberg-Maryborough region.||||||03-MAR-10
6106|Elliott Formation|61611|6|Mentioned|p265 Fig. 3|Tertiary|Tertiary|Geological Province: Maryborough Basin. Sandstone.||||||13-MAR-09
6106|Elliott Formation|63821|4|Described|p25|Early Miocene|Late Oligocene|Overlain by Elliott Surface. Comprises sandstone, siltstone, minor mudstone, conglomerate and shale. See also p10, p11.||||||07-FEB-11
6106|Elliott Formation|64714|5|Briefly described|p3-4 Fig. 1|Early Miocene|Early Miocene|Overlies Burrum Coal Measures. Quartzose to sublabile sandstone, conglomerate, siltstone, mudstone, shale. ||||||
6106|Elliott Formation|68319|5|Briefly described|Map Legend|Miocene|Miocene|Early Miocene age.||||Unconformably underlain by the Maryborough Formation.|Quartzose to sublabile sandstone, conglomerate, silstone, mudstone, shale.|
6106|Elliott Formation|68332|5|Briefly described|Map legend.|Miocene|Miocene|||||Conformably overlies Gooburrum Clay.|Quartzose to sublabile sandstone, conglomerate, siltstone, mudstone, shale.|
6106|Elliott Formation|68421|5|Briefly described|Map Legend|Early Miocene|Early Miocene||||||Quartzose to sublabile sandstone, conglomerate, siltstone, mudstone, shale.|
6106|Elliott Formation|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Mueller and Poodyea Formations; Austral Downs, Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
6106|Elliott Formation|68679|6|Mentioned|p312|Neogene|Paleogene|Northern New England Orogen.||||||
6106|Elliott Formation|68811|5|Briefly described|p50, p51, p125 tbl 12|Tertiary|Tertiary|Inconsistent spelling. Elliot Fm in text p50, 51, p125. Elliott Fm in fig 25 p51, p162. Overlain by Quaternary sediments. Hosts an aquifer system in unconsolidated alluvial sediments. See also p152 App 1, p162 tbl 25.||||Unconformably overlies the Burrum Coal Measures and overlies the Gooburrum Clay.|Alluvial sediments of quartzose sandstone, conglomerate, siltstone, mudstone and shale.|
6106|Elliott Formation|69599|5|Briefly described|p586-587, p651|Oligocene|Eocene|Rands (1886); Ridley (1957) and others. Onshore Capricorn Basin. Up to 34m thick. Fluvio-deltaic sediments. Deeply lateritised. Has been divided into two subunits. Age discussed. Appears as Elliot Formation on p651. RELATED UNITS (continued): Also correlated with Lowmead and Petrie Formations, and (at least partly) with Beaudesert, Pomona, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds.||||Overlies Fairymead beds conformably and Burrum Coal Measures unconformably. Is overlain unconformably by Hummock Basalt. Correlated  with Flinders Dolomite; Oakdale Sandstone; see COMMENTS for more.|Includes conglomerate, sandstone, siltstone, silty mudstone and shale.|
6106|Elliott Formation|72298|5|Briefly described|p796-797|||Unconsolidated sediments contain semiconfined, unconsolidated aquifers in the Woongarra area.||||Overlies Fairymead beds and Burrum Coal Measures.|Unconsolidated to semiconsolidated sands and gravels that can be overlain by thick clay layers.|
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.||
6127|Emerald Formation|39445|5|Briefly described|Table 14|||Eocene. See also P150||||||
6127|Emerald Formation|44581|14|Not recorded|p354|||||||||
6127|Emerald Formation|48841|14|Not recorded|p36|||Similar to Exevale Formation. Overlain by Basalt flows.||||||
6127|Emerald Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|Relationship with the Oligocene Emerald Volcanics, also of the Fitzroy region, is unclear.||||||03-MAR-10
6127|Emerald Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Exevale, Floraville, Glendower, 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.||||||
6127|Emerald Formation|69599|5|Briefly described|p585, p592|Eocene|Paleocene|Zillman (1979); Wallin (1979). Emerald Basin. Up to 171m thick. Economic oil shale not found.||||Correlated with Biloela beds; Southern Cross, Exevale, Suttor and Duarings Formations.|A variable succession of siltstone, claystone, sandstone and subordinate oil shale.|
6127|Emerald Formation|70856|5|Briefly described|Map Legend|Tertiary|Tertiary||||||Fluviatile and lacustrine claystone and siltstone, quartzose sandstone, pebbly sandstone, gravel, lignite, oil shale and interbedded basalt.|02-FEB-17
6164|Emu Park Sands|42143|6|Mentioned|p397|||||||||
6188|Engow Member|23422|5|Briefly described|p183|Early Permian|Late Carboniferous|Of Marshs Creek Formation.||||||
6188|Engow Member|23430|5|Briefly described|p520|||||||||
6188|Engow Member|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|of Marshs Creek Formation, Sybil Group.||||||30-JUN-15
6188|Engow Member|23893|5|Briefly described|p19|Early Permian|Late Carboniferous|Of Marshs Creek Formation.||||||
6188|Engow Member|42692|5|Briefly described|map legend|Permian|Late Carboniferous|of Marshs Creek Formation. Reserved as Engow Formation.||||||
6188|Engow Member|43095|3|Fully described|p71|||of Marshs Creek Formation.||||||
6188|Engow Member|68350|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Marshs Creek Formation.||Conformably overlies Malairo Rhyolite Member (Hells Gate Rhyolite).|Fine-grained, laminated, tuffaceous sandstone, siltstone and mudstone.|
6188|Engow Member|68351|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Marshs Creek Formation.||Conformably overlies Malairo Rhyolite Member (Hells Gate Rhyolite).|Fine-grained, laminated, tuffaceous sandstone, siltstone and mudstone.|
6188|Engow Member|68731|5|Briefly described|p203|||||Of the Marshes Creek Formation.|||Comprises fine-grained volcaniclastic sandstone, siltstone, mudstone, chert and minor polymict conglomerate.|
6188|Engow Member|69592|5|Briefly described|p275|Pennsylvanian|Pennsylvanian|Sybil Graben.||Marshs Creek Formation.|||Fine-grained, volcaniclastic sandstone, mudstone, chert and minor polymict conglomerate.|
6196|Enoggera Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
6196|Enoggera Granite|31133|6|Mentioned|p160|||Triassic||||||
6196|Enoggera Granite|31271|6|Mentioned|Fig. 2|||||||||
6196|Enoggera Granite|31370|6|Mentioned|Fig. 1|||||||||
6196|Enoggera Granite|32610|5|Briefly described|p42|||Refers Bryan (1914,1923) & P42 age Evernden & Richards (1962)||||||
6196|Enoggera Granite|33289|6|Mentioned|p166|||||||||
6196|Enoggera Granite|33881|6|Mentioned|p95|||Possibility to be quarried||||||
6196|Enoggera Granite|35007|6|Mentioned|p74|||||||||
6196|Enoggera Granite|35063|6|Mentioned|p79|||||||||
6196|Enoggera Granite|35812|6|Mentioned|Fig.2|||||||||
6196|Enoggera Granite|35866|6|Mentioned|p400|||||||||
6196|Enoggera Granite|36045|6|Mentioned|p335|||||||||
6196|Enoggera Granite|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early Triassic||||||09-NOV-15
6196|Enoggera Granite|36779|6|Mentioned|p6|||||||||
6196|Enoggera Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
6196|Enoggera Granite|38074|6|Mentioned|Table 2|||||||||
6196|Enoggera Granite|39079|6|Mentioned|p6|||||||||
6196|Enoggera Granite|39445|5|Briefly described|Table 12|||||||||
6196|Enoggera Granite|40623|5|Briefly described|p9|||||||||
6196|Enoggera Granite|41906|5|Briefly described|p38|||||||||
6196|Enoggera Granite|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
6196|Enoggera Granite|43008|5|Briefly described|map legend|||||||||
6196|Enoggera Granite|43009|5|Briefly described|Map Legend|||||||||
6196|Enoggera Granite|43076|5|Briefly described|p6|||||||||
6196|Enoggera Granite|44671|14|Not recorded|p247|||||||||
6196|Enoggera Granite|44703|14|Not recorded|Map||Early Triassic|||||||
6196|Enoggera Granite|44708|14|Not recorded|p3,4,20,23,24,Sh.4||Early Triassic|||||||
6196|Enoggera Granite|44783|14|Not recorded|p7,48,50|||||||||
6196|Enoggera Granite|45003|14|Not recorded|p42,82|||||||||
6196|Enoggera Granite|48894|6|Mentioned|p40|||219my.||||||
6196|Enoggera Granite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
6196|Enoggera Granite|68576|5|Briefly described|QLD_D1: p2-4, p14, p16-17|||Appears as Enoggera (or Blackbutt) Granite. Used for the base, stairs and some portals of the Old Bank of New South Wales (Queen Street); base course and plinth in the Old Administration Building; steps and base of the Queen Victoria statue in Queens Park; base of Old Government Printery Buildings; the Wall of Epiphytes in Roma Street Parklands. Map location.|||||Light grey to pink (biotite) granite.|
6196|Enoggera Granite|68679|5|Briefly described|p334, p427-428, p472|Late Triassic|Late Triassic|In and around Brisbane. An age of 232.2 +/- 1.4 Ma (SHRIMP U-Pb zircon) has been determined by Cross (unpub.).|223.6 Ma (K-Ar: Evernden and Richards, 1962).|||Intrudes Neranleigh-Fernvale beds and Bunya Phyllite.|Biotite granite and biotite-hornblende granodiorite.|
6196|Enoggera Granite|69952|5|Briefly described|p2 Tb.i, p38-42, p45|Late Triassic|Late Triassic|Exposed in the Brisbane suburb of Keperra. Not comagmatic with Brisbane Tuff; possibly unroofed prior to the latter's eruption. SHRIMP U-Pb zircon magmatic crystallisation age. A variety of K-Ar ages from 1962 to 1975 is given.|232.2 +/- 1.5 Ma (Cross et al., 2015).|||Intrudes Neranleigh-Fernvale beds and Bunya Phyllite.|Medium-grey, medium- to coarse-grained, slightly porphyritic biotite granite. Microdiorite xenoliths (2-3cm) are common. Some large crystals and aggregates of sulfide (probably pyrite).|09-NOV-15
6196|Enoggera Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|232+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
6196|Enoggera Granite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Enoggera.||||||
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.||
6244|Erringibba formation|40443|6|Mentioned|p116|||||||||
6244|Erringibba formation|40954|6|Mentioned|p133|||||||||
6265|Esk Formation|13516|5|Briefly described|p159 fig 8, p163, 164|Middle Triassic|Middle Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
6265|Esk Formation|22845|6|Mentioned|p82|Triassic|Permian|||||||
6265|Esk Formation|23440|4|Described|p140|||Of Toogoolawah Group.||||||18-AUG-08
6265|Esk Formation|23799|3|Fully described|p38, p12 Tb. 1, p37 Tb. 3|Middle Triassic|Early Triassic|Formerly "Esk Shales", "Esk Beds" and "Esk Formation".  Unconformably overlain by Tarong beds, Main Range Volcs, Oakdale Sst; unconformably overlies Maronghi Creek beds.  Intruded by phases of Tarameo Tonalite.  Max.thick: ~3000m.  Geol. Prov: Esk Trough.||||||
6265|Esk Formation|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||
6265|Esk Formation|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 3000m.||||||
6265|Esk Formation|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Polymictic pebble to boulder conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||
6265|Esk Formation|30302|6|Mentioned|p414|||Lower to Middle Triassic||||||
6265|Esk Formation|30471|6|Mentioned|Fig.2|||See also P130. Correlation of drillhole sections||||||
6265|Esk Formation|30473|6|Mentioned|p377|||Refers Cranfield and Schwarzbock(1972). Part of Toogoolawah Group||||||
6265|Esk Formation|30475|6|Mentioned|p159|||||||||
6265|Esk Formation|30508|6|Mentioned|p88|||Triassic age. Esk Sewerage Scheme||||||
6265|Esk Formation|30565|6|Mentioned|p133|||||||||
6265|Esk Formation|31300|6|Mentioned|Pl. 9|||See also Pl. 10||||||
6265|Esk Formation|31450|6|Mentioned|p47|||||||||
6265|Esk Formation|31811|6|Mentioned|Fig. 1|||||||||
6265|Esk Formation|32022|6|Mentioned|p24|||||||||
6265|Esk Formation|32136|6|Mentioned|p6|||Miospores||||||
6265|Esk Formation|32838|6|Mentioned|p320|||||||||
6265|Esk Formation|35101|3|Fully described|p41|||||||||
6265|Esk Formation|35161|6|Mentioned|p591|||||||||
6265|Esk Formation|35427|6|Mentioned|p121|||||||||
6265|Esk Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
6265|Esk Formation|35647|6|Mentioned|p58|||||||||
6265|Esk Formation|35648|6|Mentioned|p13|||||||||
6265|Esk Formation|35901|6|Mentioned|p17|||||||||
6265|Esk Formation|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early Triassic||||||
6265|Esk Formation|36825|6|Mentioned|p12|||||||||
6265|Esk Formation|36899|6|Mentioned|p1085|||||||||
6265|Esk Formation|36954|6|Mentioned|p114|||||||||
6265|Esk Formation|37065|6|Mentioned|p36|||Formerly Esk Shales||||||
6265|Esk Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
6265|Esk Formation|37376|6|Mentioned|p491|||||||||
6265|Esk Formation|37755|6|Mentioned|p79|||||||||
6265|Esk Formation|37812|6|Mentioned|p657|||||||||
6265|Esk Formation|38304|6|Mentioned|p83|||||||||
6265|Esk Formation|38306|6|Mentioned|p509|||||||||
6265|Esk Formation|38358|6|Mentioned|p14|||||||||
6265|Esk Formation|39079|5|Briefly described|p9|||||||||
6265|Esk Formation|39218|6|Mentioned|p47|||Flora||||||
6265|Esk Formation|39445|5|Briefly described|Table 9|||||||||
6265|Esk Formation|40051|6|Mentioned|p8|||||||||
6265|Esk Formation|40245|6|Mentioned|p182|||||||||
6265|Esk Formation|40475|5|Briefly described|p8|||||||||
6265|Esk Formation|40484|6|Mentioned|p63|||||||||
6265|Esk Formation|40623|5|Briefly described|p65|||||||||
6265|Esk Formation|40634|6|Mentioned|Fig.3|||||||||
6265|Esk Formation|41059|6|Mentioned|p168|||||||||
6265|Esk Formation|41738|6|Mentioned|p168|||||||||
6265|Esk Formation|41906|6|Mentioned|p14|||||||||
6265|Esk Formation|42336|6|Mentioned|p2|||||||||
6265|Esk Formation|42492|5|Briefly described|Table 2 P14|||||||||
6265|Esk Formation|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
6265|Esk Formation|42893|6|Mentioned|p6|||of Toogoolawah Group||||||
6265|Esk Formation|43008|5|Briefly described|map legend|||||||||
6265|Esk Formation|43009|5|Briefly described|Map Legend|||||||||
6265|Esk Formation|43072|6|Mentioned|p80|||||||||
6265|Esk Formation|43150|6|Mentioned|Map Legend||Triassic|Name used only in context of equivalents.||||||12-APR-05
6265|Esk Formation|44115|14|Not recorded|p17|||||||||
6265|Esk Formation|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
6265|Esk Formation|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group. Geological Province: Esk Trough (Wandilla Province)||||||28-MAY-04
6265|Esk Formation|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Shale, sandstone, conglomerate, acid tuff.||||||
6265|Esk Formation|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Polymictic pebble to boulder conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||
6265|Esk Formation|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group. Geological Province: Esk Trough. Polymictic pebble to cobble conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||03-SEP-04
6265|Esk Formation|60726|6|Mentioned|p5.|Middle Triassic|Middle Triassic|Wivenhoe/Bellevue area. Contains some fossil insects.||||||
6265|Esk Formation|60993|6|Mentioned|p8 Tb. 2|||See also Esk beds.||||||
6265|Esk Formation|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Ipswich C.M. ||||||
6265|Esk Formation|61781|6|Mentioned|p267, p270|||Geological Province: Esk Trough.||||||
6265|Esk Formation|61782|5|Briefly described|p275, p277, p277 Fig. 3|||Geol Prov: Esk Trough.||||||
6265|Esk Formation|63821|6|Mentioned|p20|||||||||07-FEB-11
6265|Esk Formation|67402|5|Briefly described|p204, p205 tbl ESK/ABR1|Ladinian|Anisian|Esk Trough. Is only present in the western portion of this basin. Deposited in a fluvial environment. Time equivalent of the Neara Volcanics and Bryden Formation.  See also p206 fig ESK/ABR6, p208-p210.||Toogoolawah Group|||Sandstone, shale, conglomerate and tuff.|
6265|Esk Formation|68679|4|Described|p322, p324, p326,p389-391,p397,p427,p471|Middle Triassic|Middle Triassic|McDonnell (1956) and others (listed). Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Crops out along the entire W margin of the Basin. Has a basal conglomerate at the type section, west of Moore, where the Formation is ~3000m thick; it thins southward to 300m near Esk. Differing stratigraphic interpretations discussed. Rich in plant macrofossils and miospores.||Toogoolawah Group.||Is faulted against the Bjelke-Petersen and ?Maronghi Creek beds. Is intruded by Brisbane Valley Porphyrite.|Interbedded sandstone, shale, conglomerate, minor andesite and tuff.|
6265|Esk Formation|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.||Toogoolawah Group.||||
6279|Esmeralda Granite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Very coarse to medium-grained (muscovite-) biotite granite, porphyritic in part.  Overlain by Nonda Granite.||||||15-JAN-07
6279|Esmeralda Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite granite.||||||02-JUL-04
6279|Esmeralda Granite|22669|6|Mentioned|P249|||||||||
6279|Esmeralda Granite|22744|6|Mentioned|P7|||||||||
6279|Esmeralda Granite|23220|6|Mentioned|Fig.1|||In the Georgetown Inlier.||||||15-JAN-07
6279|Esmeralda Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Geological Province: Georgetown Region.||||||12-MAY-15
6279|Esmeralda Granite|23429|5|Briefly described|p446|||||||||
6279|Esmeralda Granite|23430|5|Briefly described|p456|||Age: 1558 +/- 4 Ma.||||||15-JAN-07
6279|Esmeralda Granite|23493|5|Briefly described|p9, p16 Tb. 1|Late Paleozoic|Late Paleozoic|Grey massive even-grained granite.  Intrudes Croydon Felsite along its margins, and Etheridge and Langdon River Formations.||||||07-NOV-08
6279|Esmeralda Granite|23498|6|Mentioned|p20 table 1|||||||||
6279|Esmeralda Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 808. S-Type.||||||
6279|Esmeralda Granite|24197|5|Briefly described|p32, p77|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province). See also p79 Tb. 9.1.||||||07-FEB-11
6279|Esmeralda Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1550Ma. Geological Province: Georgetown Inlier. Name written as Esmeralda only under heading for GRANITE.||||||09-MAY-05
6279|Esmeralda Granite|30584|4|Described|Table 1|||||||||
6279|Esmeralda Granite|30585|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6279|Esmeralda Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6279|Esmeralda Granite|31164|6|Mentioned|Fig. 1|||Refers to Riverean (1966)||||||
6279|Esmeralda Granite|31435|6|Mentioned|p19|||||||||
6279|Esmeralda Granite|32528|5|Briefly described|Table 1|||||||||
6279|Esmeralda Granite|33179|6|Mentioned|Table 1|||||||||
6279|Esmeralda Granite|33669|6|Mentioned|p517|||||||||
6279|Esmeralda Granite|33908|6|Mentioned|p585|||||||||
6279|Esmeralda Granite|35921|6|Mentioned|p40|||||||||
6279|Esmeralda Granite|35950|6|Mentioned|p307|||||||||
6279|Esmeralda Granite|36153|6|Mentioned|Fig.10|||||||||
6279|Esmeralda Granite|36216|6|Mentioned|p208|||||||||
6279|Esmeralda Granite|36780|6|Mentioned|Fig.11|||||||||
6279|Esmeralda Granite|37462|6|Mentioned|p274|||||||||
6279|Esmeralda Granite|37570|4|Described|p122|||See also Fig.3.||||||
6279|Esmeralda Granite|37571|6|Mentioned|p133|||||||||
6279|Esmeralda Granite|38716|4|Described|p193|||||||||
6279|Esmeralda Granite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
6279|Esmeralda Granite|39445|5|Briefly described|Table 2|||See also p37 and p45. Post tectonic. Age: 1444 Ma.||||||15-JAN-07
6279|Esmeralda Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6279|Esmeralda Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6279|Esmeralda Granite|40659|6|Mentioned|p250|||||||||
6279|Esmeralda Granite|40860|6|Mentioned|p109|||||||||
6279|Esmeralda Granite|41272|5|Briefly described|M 1of1 A04|||See also M 1of1 M03||||||
6279|Esmeralda Granite|41465|6|Mentioned|p14|||||||||
6279|Esmeralda Granite|41975|5|Briefly described|p438|||||||||
6279|Esmeralda Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic. U-Pb zircon age is 1558+/-4 Ma.||||||03-DEC-13
6279|Esmeralda Granite|43664|6|Mentioned|p57|||Part of Emeralda Supersuite?||||||15-JAN-07
6279|Esmeralda Granite|43793|5|Briefly described|p332|||||||||
6279|Esmeralda Granite|44047|14|Not recorded|Map Legend||Permian|||||||
6279|Esmeralda Granite|44053|2|Defined|p239,240|Permian|Late Carboniferous|Probably Late Carboniferous or Permian||||||
6279|Esmeralda Granite|44057|14|Not recorded|p606-607|Early Permian|Early Carboniferous|Grey adamellite. (Middle Carboniferous-Early Permian)||||||
6279|Esmeralda Granite|44059|14|Not recorded|p442(Tb.),444|Permian|Carboniferous|||||||
6279|Esmeralda Granite|44258|14|Not recorded|p6,7,9,10,18,30,37|||||||||
6279|Esmeralda Granite|44516|2|Defined|p35|Late Paleozoic|Early Paleozoic|Intrudes Stockyard Creek Siltstone and Etheridge Formation. (Middle Palaeozoic-Late Palaeozoic)||||||07-NOV-08
6279|Esmeralda Granite|45003|14|Not recorded|p16,44|||||||||
6279|Esmeralda Granite|45009|14|Not recorded|p21,75,111,Tb.13,||Permian|Pl.13. Intrudes Croydon Volcanics.||||||
6279|Esmeralda Granite|45014|2|Defined|p38-39,93-98,Pl.23||Carboniferous|Pls.24,36-38,41. (Probably Carboniferous)||||||
6279|Esmeralda Granite|45086|6|Mentioned|p45|||Age. Mineralization.||||||
6279|Esmeralda Granite|45087|5|Briefly described|p30|||Chemical analyses.||||||
6279|Esmeralda Granite|45113|3|Fully described|p2|||Emphasis on petrography. Geochemistry p29.||||||15-JAN-07
6279|Esmeralda Granite|48894|6|Mentioned|p50|||Ages: 602my, 701my, 515my.||||||15-JAN-07
6279|Esmeralda Granite|48976|6|Mentioned|p6|||See also p7||||||15-JAN-07
6279|Esmeralda Granite|50537|5|Briefly described|p1.1, 1.5, 3.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite. Age: 1558 +/- 4Ma (U-Pb).||||||
6279|Esmeralda Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Very coarse to medium-grained, (muscovite)-biotite granite; porphyritic in part.||||||
6279|Esmeralda Granite|60081|5|Briefly described|Map legend|Proterozoic|Proterozoic|Grey biotite adamellite, granodiorite.||||||
6279|Esmeralda Granite|61258|6|Mentioned|p386|Mesoproterozoic|Mesoproterozoic|Age: 1558+/-4Ma (Black and McCulloch 1990) and 1556+/-4Ma. ||||||
6279|Esmeralda Granite|66529|5|Briefly described|p77 |Mesoproterozoic|Mesoproterozoic|Underlies Carpentaria and Eromanga Basins; 4751 km2 in (subterranean) extent. A high heat-producing basement unit.||||||
6279|Esmeralda Granite|66800|6|Mentioned|p926.||||1558 +/- 4 Ma (Black & McCulloch 1990).|||||
6279|Esmeralda Granite|67323|5|Briefly described|solid geol.|||||Esmeralda Supersuite|||Very coarse to medium-grained (muscovite) biotite granite, porphyritic in part|
6279|Esmeralda Granite|68307|6|Mentioned|p88, p97|||Very thin, with relatively flat base.||||||
6279|Esmeralda Granite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to medium-grained (muscovite-) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68416|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province. Shown as younger than D2 ~ 1552 Ma.|< 1552 Ma|Of the Esmeralda Supersuite.|||Very coarse to medium-grained (muscovite) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|68417|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province.||Of the Esmeralda Supersuite.|||Very coarse to medium-grained (muscovite) biotite granite, porphyritic in part.|
6279|Esmeralda Granite|69591|4|Described|p75, p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier. Underwent alteration at 353 +/- 7 Ma and 293 +/- 3 Ma.|1558 +/- 4 Ma (Black and McCulloch, 1990).|Esmeralda Supersuite.||Intrudes Croydon Volcanic Group.|Coarse biotite granite. Contains enclaves and graphite concentrated into narrow, tabular zones subparallel to contact with the volcanic rocks it intrudes.|
6279|Esmeralda Granite|73527|6|Mentioned|p2, p3 Fig.2, p5, p8 Fig.6|||Georgetown Inlier, western domain.||Esmeralda Supersuite, western part||||
6279|Esmeralda Granite|73642|5|Briefly described|p3 Fig.2, p4-5, p6 Fig.4, p8-11, p13|Calymmian|Calymmian|Georgetown Inlier. S-type. Also referred to as Esmeralda granite p8.|1558+/-8 Ma U-Pb zircon, 1561+/-8 Ma|Esmeralda Supersuite||||
6279|Esmeralda Granite|75079|5|Briefly described|p5-6, 9-13, 16-18|Mesoproterozoic|Mesoproterozoic|Western domain, Georgetown Inlier. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|~1550 Ma.|Esmeralda Supersuite.||||
6282|Esperanza Formation|22438|4|Described|p539, Fig.3 p537|||See also Fig.10a p546.||||||18-SEP-06
6282|Esperanza Formation|22453|5|Briefly described|p 11  Fig 10|||||||||
6282|Esperanza Formation|22585|6|Mentioned|P739, Fig1, Fig2|||||||||
6282|Esperanza Formation|22665|6|Mentioned|P221, Table1|||||||||
6282|Esperanza Formation|22680|6|Mentioned|84 fig 2,85|||Geol province Mount Isa Basin. Parent McNamara Group. Formation as 'Fm' in text||||||
6282|Esperanza Formation|22681|6|Mentioned|91|||Overlying unit Lady Loretta Formation||||||
6282|Esperanza Formation|23031|5|Briefly described|26|||Geol. province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Lady Lorretta Formation; underlain by Paradise Creek Formation||||||18-SEP-06
6282|Esperanza Formation|23072|5|Briefly described|p754|||||||||
6282|Esperanza Formation|23073|5|Briefly described|p744 (fig 2), p745|||||||||
6282|Esperanza Formation|23362|5|Briefly described|339|||||||||
6282|Esperanza Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
6282|Esperanza Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group. Overlain by Lady Loretta Formation.||||||07-NOV-08
6282|Esperanza Formation|23396|4|Described|p421, 407|Statherian|Statherian|Of McNamara Group. Age: 1657+/-3Ma U/Pb zircon analyses, [presumably detrital zircon, on SHRIMP].||||||16-MAR-18
6282|Esperanza Formation|23397|5|Briefly described|p469|||||||||
6282|Esperanza Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group.||||||
6282|Esperanza Formation|23399|5|Briefly described|p493 Fig.3|||Of McNamara Group.||||||18-SEP-06
6282|Esperanza Formation|23408|4|Described|p512, p513 Fig. 2, p521|||Of McNamara Group. Upper section includes accretions of deeper water 'organ pipe' digitate stromatolite bioherms and biostromes.||||||15-JUN-09
6282|Esperanza Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group||||||18-SEP-06
6282|Esperanza Formation|23466|5|Briefly described|p269|||||||||
6282|Esperanza Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3||||||
6282|Esperanza Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
6282|Esperanza Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thickness: 250m.||||||21-NOV-16
6282|Esperanza Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
6282|Esperanza Formation|23986|5|Briefly described|p65|||Of McNamara Group.||||||
6282|Esperanza Formation|24033|6|Mentioned|p25, p26 Fig. 10|||||||||
6282|Esperanza Formation|24308|5|Briefly described|p995 Fig. 8|||||||||
6282|Esperanza Formation|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Paradise Creek Formation. Age: c.1657 Ma. Carbonate. Geological Province: Lawn Hill Platform.||||||
6282|Esperanza Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|36937|6|Mentioned|p229|||||||||
6282|Esperanza Formation|37459|1|Redefined|p429|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||18-SEP-06
6282|Esperanza Formation|37568|6|Mentioned|p84|||||||||
6282|Esperanza Formation|38237|4|Described|p129|||||||||
6282|Esperanza Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|38348|4|Described|p11|||||||||
6282|Esperanza Formation|38584|6|Mentioned|p22|||||||||
6282|Esperanza Formation|39445|5|Briefly described|Table 2|||||||||
6282|Esperanza Formation|39497|6|Mentioned|Fig.4|||||||||
6282|Esperanza Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Stromatolitic chert and dolomite, siliceous and dolomitic siltstone.||||||15-JUN-06
6282|Esperanza Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|39925|6|Mentioned|Fig.9|||||||||
6282|Esperanza Formation|39944|6|Mentioned|Fig.1|||||||||
6282|Esperanza Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|40221|3|Fully described|p17|||||||||
6282|Esperanza Formation|40394|6|Mentioned|p286|||||||||
6282|Esperanza Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
6282|Esperanza Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||27-MAY-08
6282|Esperanza Formation|45166|5|Briefly described|p30|||||||||
6282|Esperanza Formation|47083|3|Fully described|p16-17||Proterozoic|Previously part of Paradise Crk Fm by Carter and others (1961). Of McNamara Gp. Overlain by Lady Loretta Fm; underlain by Paradise Crk Fm. Max. thickness: 350 m.||||||18-SEP-06
6282|Esperanza Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1647 Ma, <1657 Ma. Conformably overlies Paradise Creek Formation. Conformably overlain by Lady Loretta Formation. Geological Province: Western Fold Belt.||||||17-DEC-07
6282|Esperanza Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Stromatolitic chert, dolomitic sandstone, siltstone, oolitic dolomite. Overlies Paradise Creek Formation; overlain by Lady Loretta Formation.||||||21-NOV-16
6282|Esperanza Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Lady Loretta Formation, underlain by Paradise Creek Formation.||||||
6282|Esperanza Formation|61732|5|Briefly described|p25|||Superseded Paradise Creek Formation. Well preserved microfossils in stromatolites. In the Mount Isa region.||||||07-FEB-11
6282|Esperanza Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
6282|Esperanza Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Esperanza Fm.||McNamara Group|||Platform carbonates.|
6282|Esperanza Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1657 +/- 3 Ma.|McNamara Group.||||
6282|Esperanza Formation|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: ca 1660-1655Ma. Of the Gun Supersequence.||||||07-NOV-08
6282|Esperanza Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
6282|Esperanza Formation|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
6282|Esperanza Formation|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Gun supersequence. Appears in Fig.2 only as Esp.|c.1657 Ma.|Of the McNamara Group||||
6282|Esperanza Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa Superbasin.||Of the Gun supersequence||||05-APR-17
6282|Esperanza Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
6282|Esperanza Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
6282|Esperanza Formation|63866|5|Briefly described|p58|||Isa Superbasin.||Gun Supersequence||||
6282|Esperanza Formation|63884|5|Briefly described|p14|||Dolomitic.||||||
6282|Esperanza Formation|64250|6|Mentioned|p11 fig 3|||||Unit in McNamara Group.||||
6282|Esperanza Formation|65228|6|Mentioned|p24, Fig.04.|||Southern Lawn Hill Platform. Part of Gun Supersequence.||Unit in McNamara Group.||||
6282|Esperanza Formation|65337|5|Briefly described|p30.|||Equivalent to lower Brumby Formation.||||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation.|Includes carbonate-chert-conglomerate facies.|
6282|Esperanza Formation|65396|5|Briefly described|p82, p175, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1657 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation; overlain by Lady Loretta Formation.||03-APR-17
6282|Esperanza Formation|66844|4|Described|p243-244,251,253, 254,270-273|Statherian|Statherian|Lawn Hill Platform. Age from SHRIMP dating. Comprises Gun 2.1 to 2.5 sequences. Shale-dominated MFS in lower part associated with Gun 2.2. Stromatolites are dominantly digitate columnar, indicative of silicification by late-stage diagenetic processes. Upper part received locally sourced, nearshore siliciclastic accummulations in the Kamarga Dome and Gregory River regions associated with basinward shift in facies.|1657+\-3 Ma SHRIMP|Of lower McNamara Group; Gun Supersequence (2.1-2.5).|Informally subdivided into upper and lower parts p267, 268.|Overlain unconformably by Lady Loretta Formation.|Includes ooid grainstones; digitage stromatolite and dolomudstone.|
6282|Esperanza Formation|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|~1660-1650 Ma.|McNamara Group.|||Stromatolitic chert and dolomite, siliceous and dolomitic sandstone.|
6282|Esperanza Formation|68542|5|Briefly described|p6|||||Lower McNamara Group||Overlain by Lady Loretta Formation, overlies Paradise Creek Formation|Stromatolitic chert and dolomitic siltstone.|
6282|Esperanza Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation.|Stromatolitic chert and dolomitic siltstone.|
6282|Esperanza Formation|68732|5|Briefly described|p162, p163, p168 Fig.5, p169|Statherian|Statherian|Geochronology based on a "pinkite": tuffaceous rock or peperite in the lower part of this formation.|1657 +/- 3 Ma|Of the McNamara Group.|||Includes stromatolitic bioherms and biostromes.|30-NOV-17
6282|Esperanza Formation|69591|5|Briefly described|p42-43, p44 Fig.2.36, p54|||Isa Superbasin. Deposition on a carbonate platform: tempestites/peritidal deposits. Part of Gun Supersequence.||McNamara Group.||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation. Equated with the Urquhart Shale.|Stromatolitic dolomite and chert, siliceous and dolomitic sandstone.|
6282|Esperanza Formation|70864|5|Briefly described|p75, 74 Fig 2, p78, p80, 81, 84, p100|Mesoproterozoic||Host to sulphide mineralization in siliceous and calcareous rocks.||McNamara Group|||Stromatolitic chert, dolomitic siltstone, calcareous and siliceous siltstone, carbonaceous black shale, dolostones and sandstones.|21-NOV-16
6282|Esperanza Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1657 +/-3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.||
6282|Esperanza Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the The Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Four U-Pb zircon sedimentary depositional ages [?] given for this unit on p33 are shown for the underlying Paradise Creek Formation on p5. The date listed is common to both figures.|1657 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.|Includes dolostone.|
6282|Esperanza Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.|1653 +/- 7 Ma to 1658 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.|Includes dolostone.|
6282|Esperanza Formation|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1657 +/- 3 Ma (see Fig.1.2)|McNamara Group||Underlain by Paradise Creek Formation. Overlain by Lady Loretta Formation.||
6282|Esperanza Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Gun Supersequence. Partial aquifer.||McNamara Group||Underlain by Paradise Creek Formation. Overlain by Lady Loretta Formation.||
6282|Esperanza Formation|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Carbonates.|
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||
6300|Etheridge Group|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Langdon River Mudstone.||||||
6300|Etheridge Group|22533|6|Mentioned|p54|Statherian|Statherian|Placed in Forsyth subprovince.||||||15-JAN-07
6300|Etheridge Group|22630|6|Mentioned|p 3|Proterozoic|Proterozoic|||||||
6300|Etheridge Group|22669|6|Mentioned|P248, Fig1||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|22811|5|Briefly described|p604|||Of Forsayth Subprovince. Age of unit 1700 Ma||||||15-JAN-07
6300|Etheridge Group|22844|5|Briefly described|p31,37||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|22963|6|Mentioned|p67||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|23085|5|Briefly described|p670|||||||||
6300|Etheridge Group|23220|5|Briefly described|Fig.1 p8|||Of Forsayth Subprovince.||||||15-JAN-07
6300|Etheridge Group|23291|3|Fully described|p22, p46, p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Indruded by Yataga Granodiorite with thermal metamorphic aureole. Geological Province: Georgetown Region.||||||08-JUL-15
6300|Etheridge Group|23420|6|Mentioned|p 125|||||||||
6300|Etheridge Group|23425|5|Briefly described|p371|||Etheridge Province.||||||
6300|Etheridge Group|23430|4|Described|p450 p453||Paleoproterozoic|Forsayth Subprovince. SHRIMP U-Pb ~1650 Ma. Overlain by Langlovale Group - unconformable contact. Etheridge Province.||||||07-NOV-08
6300|Etheridge Group|23431|5|Briefly described|p530|||Etheridge Province.||||||
6300|Etheridge Group|23502|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|23510|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|23616|5|Briefly described|p27||Paleoproterozoic|SHRIMP U-Pb ~1650 Ma.||||||07-NOV-08
6300|Etheridge Group|23619|4|Described|p36 Table 1||Proterozoic|Intruded by Mullindie Granite. Also see p18. The original age is not known but the rocks are certainly older than 1570 Ma. Georgetown Province.||||||
6300|Etheridge Group|23624|3|Fully described|p4|||Precambrian age assumed.||||||05-JAN-05
6300|Etheridge Group|23713|6|Mentioned|p8 Table 1|||Georgetown Province.||||||
6300|Etheridge Group|24197|5|Briefly described|p76|Paleoproterozoic|Paleoproterozoic|Includes Candlow and Lane Creek Formations. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
6300|Etheridge Group|24485|5|Briefly described|p1, 21|Proterozoic|Proterozoic|Age: ~1700Ma. Geological Province: Forsayth Subprovince.||||||15-JAN-07
6300|Etheridge Group|35921|1|Redefined|p29|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
6300|Etheridge Group|36153|5|Briefly described|p54|||||||||
6300|Etheridge Group|36216|6|Mentioned|p208|||||||||
6300|Etheridge Group|36780|5|Briefly described|p1|||||||||
6300|Etheridge Group|37462|5|Briefly described|p273|||||||||
6300|Etheridge Group|37565|6|Mentioned|Fig.5|||||||||
6300|Etheridge Group|37570|4|Described|p113|||See also Fig.2||||||
6300|Etheridge Group|38714|6|Mentioned|p182|||||||||
6300|Etheridge Group|38715|6|Mentioned|p191|||||||||
6300|Etheridge Group|38716|6|Mentioned|p193|||||||||
6300|Etheridge Group|38752|5|Briefly described|p43|||||||||
6300|Etheridge Group|39445|5|Briefly described|p45|||See also Table 2||||||
6300|Etheridge Group|39566|6|Mentioned|p51|||||||||
6300|Etheridge Group|39687|6|Mentioned|p1|||||||||
6300|Etheridge Group|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
6300|Etheridge Group|39924|6|Mentioned|p339|||||||||
6300|Etheridge Group|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6300|Etheridge Group|40659|6|Mentioned|p248|||||||||
6300|Etheridge Group|40798|5|Briefly described|p236|||||||||
6300|Etheridge Group|40860|6|Mentioned|p112|||||||||
6300|Etheridge Group|41125|6|Mentioned|p53|||||||||
6300|Etheridge Group|41272|6|Mentioned|p29|||||||||
6300|Etheridge Group|41431|6|Mentioned|p1|||||||||
6300|Etheridge Group|41675|6|Mentioned|p7|||||||||
6300|Etheridge Group|41680|6|Mentioned|p107|||||||||
6300|Etheridge Group|41975|3|Fully described|p431|||||||||
6300|Etheridge Group|42199|5|Briefly described|Table 1 P280|||||||||
6300|Etheridge Group|42279|5|Briefly described|p23|||||||||
6300|Etheridge Group|42407|6|Mentioned|p33|||||||||
6300|Etheridge Group|42747|6|Mentioned|p35|||||||||
6300|Etheridge Group|42765|6|Mentioned|p18|||||||||
6300|Etheridge Group|43060|6|Mentioned|p30|||||||||
6300|Etheridge Group|43083|5|Briefly described|p17 tb. 1, p27|||Contains the Robertson River Subgroup, Einasleigh Metamorphics. Older than 1570+/-20 Ma. Geological province: Georgetown Province.||||||17-JUN-09
6300|Etheridge Group|43110|6|Mentioned|p8|||||||||
6300|Etheridge Group|43113|4|Described|Table 1 p23||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|43213|5|Briefly described|p62|Mesoproterozoic|Mesoproterozoic|Withnall et al. (1980, 1988); Withnall (1984, 1985). Central Georgetown Province. Deformed c. 1570 Ma (Black et al., 1979). Possible correlative of Anakie Metamorphic Group, although style and age of deformation are different. Coarse-grained quartzose metapsammites are virtually absent.|||||A psammopelitic succession that includes tholeiitic basalts and dolerites.|
6300|Etheridge Group|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
6300|Etheridge Group|43286|5|Briefly described|Map Legend||Proterozoic|||||||
6300|Etheridge Group|43287|6|Mentioned|Map Legend||Paleozoic|||||||07-NOV-08
6300|Etheridge Group|43480|6|Mentioned|10-47|||||||||
6300|Etheridge Group|43595|5|Briefly described|p353|||Deposited 2400-1570 Ma.||||||15-JAN-07
6300|Etheridge Group|43664|3|Fully described|p14||Neoproterozoic|||||||
6300|Etheridge Group|43665|4|Described|p13||Proterozoic|||||||
6300|Etheridge Group|43729|5|Briefly described|p1||Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|43793|5|Briefly described|p331|||||||||
6300|Etheridge Group|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Consists of the Robertson River Subgroup and the Einasleigh Metamorphics.||||||07-NOV-08
6300|Etheridge Group|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Consists of: Einasleigh Metamorphics (Robertson River Subgroup).||||||07-NOV-08
6300|Etheridge Group|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Robertson River Subgroup, Cobbold Metadolerite, Townley Formation, Heliman Formation, Candlow Formation, Langdon River Mudstone.||||||07-NOV-08
6300|Etheridge Group|50211|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6300|Etheridge Group|50537|5|Briefly described|p1.1, 2.4, 2.5|||Geological Province: Georgetown Inlier. Intruded by Forest Home Supersuite.||||||
6300|Etheridge Group|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Includes: Robertson River Subgroup.||||||07-NOV-08
6300|Etheridge Group|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Heliman and Candlow Formations, and Langdon River Mudstone.||||||
6300|Etheridge Group|60360|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Einasleigh Metamorphics, Cassidy Creek Metamorphics.||||||07-NOV-08
6300|Etheridge Group|61258|5|Briefly described|p386, p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Overlain by Croydon Volcanic Group. Max. thickness: 11km (est.). Geological Province: Georgetown Inlier.||||||07-NOV-08
6300|Etheridge Group|61924|5|Briefly described|p49 Fig.6, p50|Paleoproterozoic|Paleoproterozoic|Geological Province: Mary Kathleen Belt.||||||07-NOV-08
6300|Etheridge Group|63866|4|Described|p75-p76, p79, p85-p86|||Forsayth Subprovince, Etheridge Province. Interpreted to be at least 13km thick. Metamorphic grade increases eastward. Informally seperated into upper and lower halfs. Hosts base metal deposits. Also includes Dead Horse Metabasalt, Corbett Formation, Lane Creek Formation, Townley Formation and the Langdon River Mudstone.|||Includes the Bernecker Creek Formation, Einasleigh Metamorphics, Daniel Creek Formation.|Unconformably overlain by the Langlovale Group. Intruded by the Esmeralda Supersuite.||
6300|Etheridge Group|64250|6|Mentioned|p25 fig 10|||Georgetown Block.|||Includes Dead Horse Metabasalt.|||
6300|Etheridge Group|64722|5|Briefly described|p12|Statherian|Statherian|Of Georgetown-Coen region. Detrital zircons give maximum depositional age. Intruded by 1695.8 +/- 1.5 to 1684.2 +/- 2.1 Ma granites giving minimum age.|Maximum 1703 +/- 14 Ma.||Includes lowermost unit, Einasleigh Metamorphics.|||11-APR-12
6300|Etheridge Group|64726|6|Mentioned|p89.|||Deeper water sedimentation along the eastern margin of the Australian continent after c.1670 Ma.||||||
6300|Etheridge Group|65887|4|Described|p39-53|Statherian|Paleoproterozoic|In Georgetown region. Includes Bernecker Creek Formation and Robertson River Subgroup. 6-11km thick. Multiply deformed and metamorphosed supracrustal rocks. Minimum depositional age ~1660-1670 Ma. Includes Einasleigh Metamorphics.||||||
6300|Etheridge Group|66529|5|Briefly described|p5|||Western Etheridge Province. Much lower metamorphic grade (greenschist and sub-greenschist facies) than rocks in the eastern part of the Province (amphibolite and granulite facies).|||Includes Robertson River Subgroup.|Unconformably overlain by the Langlovale Group. Correlated with Soldiers Cap Group.||
6300|Etheridge Group|66800|3|Fully described|pp925-935.|Paleoproterozoic|Paleoproterozoic|Pre-dates the earliest recognised deformation and metamorphism. Thickness to c.13 km; base not exposed. Grouped (Laing 1990) with Etheridge and Willyama Groups into Diamantina Orogen on basis of broadly similar sedimentation, orogeny and cratonisation.|>1548 +/- 18 Ma.||Includes Bernecker Creek and Daniel Creek Formations and Einasleigh Metamorphics.|Is overlain by Croydon Volcanic Group.|Shallow-water, clastic, metasedimentary rocks; minor tholeiitic basaltic lavas and related dolerite intrusions.|
6300|Etheridge Group|67323|5|Briefly described|p21-22, p35|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier and possibly Claraville Domain to the west. This age is for the deposition of the upper part of the unit.|~1650-1620 Ma.|||Is overlain unconformably by Langlovale Group.||
6300|Etheridge Group|67341|6|Mentioned|v-vi|||Etheridge Province. At least 6km, possibly 13km, thick.||||||
6300|Etheridge Group|68307|5|Briefly described|p78, p85, p87-88, p97|Paleoproterozoic|Paleoproterozoic|Etheridge Province, North Australian Craton. Metamorphic grade increases towards the E. Seismic interpretation puts this at the surface east of Croydon Volcanic Group and Langlovale Group, immediately above the highly reflective Numil Seismic Province in the middle crust, and below the Carpentaria Basin. A major change in the provenance between the lower and upper parts of the Group is reflected [!] in seismic reflectivity.|||Einasleigh Metamorphics.|||
6300|Etheridge Group|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?|||Includes Robertson River Subgroup; Heliman and Candlow Formations; and Langdon River Mudstone.||Mainly mudstone.|12-MAY-15
6300|Etheridge Group|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?|||Includes Robertson River Subgroup; Heliman and Candlow Formations; and Langdon River Mudstone.||Mainly mudstone.|12-MAY-15
6300|Etheridge Group|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Min Age: Mesoproterozoic?|||Includes Robertson River Subgroup; Cobbold Metadolerite; Townley, Heliman, Candlow Formations; and Langdon River Mudstone.||Mica schist, quartzite, calc-silicate rocks, metagabbro, metadolerite, orthoamphibolite, mudstone, siltstone and mudclast sandstone.|18-MAY-15
6300|Etheridge Group|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||Includes Einasleigh Metamorphics, Bernecker Creek Formation and Robertson River Subgroup.|||
6300|Etheridge Group|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||Includes Einasleigh Metamorphics and Robertson River Subgroup.|||
6300|Etheridge Group|68355|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?|||Includes Candlow Formation and Langdon River Mudstone.||Mainly mudstone.|04-JUN-15
6300|Etheridge Group|68356|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min Mesoproterozoic?|||Includes Langdon River Mudstone.||Mainly mudstone.|04-JUN-15
6300|Etheridge Group|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||Includes Einasleigh Metamorphics, Juntana Metamorphics and Robertson River Subgroup.|||
6300|Etheridge Group|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Deposited prior to D1 (1560 Ma < D1 < 1590? Ma).|<1590? Ma||Includes Robertson River Subgroup; Cobbold Metadolerite; Townley, Heliman and Candlow Formations; Langdon River Mudstone.|||
6300|Etheridge Group|68477|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Etheridge Province.  |||Includes Cassidy Creek Metamorphics and Einasleigh Metamorphics.|||
6300|Etheridge Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||Includes Einasleigh, Cassidy Creek, Juntala and McDevitt Metamorphics, Bernecker Creek Formation, Upper Etheridge Group and Robertson River Subgroup.|||
6300|Etheridge Group|68576|6|Mentioned|Q_11: p27|Paleoproterozoic|Paleoproterozoic||||Lane Creek Formation.|||
6300|Etheridge Group|69582|5|Briefly described|p76|||Etheridge Province. Outcrops over approximately half of the Etheridge Province in the central and southern parts of the Georgetown Inlier. Withnall (1996; 1997) suggested that the group was deposited on a shelf or in an epicontinental sea. Multiply deformed with deformation intensity and complexity increasing towards the east.|||Includes the Robertston River Subgroup.|Intruded by the Forsayth Supersuite.|Metabasalts and metadolerite sills.|
6300|Etheridge Group|69591|5|Briefly described|p61-70, p75, p80-83, p103-104, p108-109|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier, Forsayth Subprovince, Etheridge Province. Base not exposed; lowermost known part is the Bernecker Creek Formation. Multiply deformed (described in some detail); intensity increases towards the east. Detrital zircon spectra.|~1710 Ma.||Robertson River Subgroup; Bernecker Creek, Townley, Heliman, Candlow Formations; Langdon River Mudstone; Einasleigh, Cassidy Creek, Juntala Metamorphics.|Is faulted against Croydon Volcanic Group. Is intruded by Esmeralda Supersuite, Cobbold Metadolerite and the Forest Home and Talbot Creek Trondhjemites. Is overlain unconformably by Langlovale Group.||
6300|Etheridge Group|69592|5|Briefly described|p290|Proterozoic|Proterozoic|The presence of Archean zircons suggests possible Archean crustal component in the Georgetown Inlier.|||||Metasedimentary rocks.|
6300|Etheridge Group|73387|6|Mentioned|p9, p15, p36|Statherian|Statherian|Maximum depositional age of 1695 +/- 13 Ma from Neumann and Kositcin (2011).|1695 +/- 13 Ma||Daniel Creek Formation|||
6300|Etheridge Group|73529|6|Mentioned|p16 Fig.12|||||||||
6300|Etheridge Group|73642|5|Briefly described|p3-4, p10 Fig.8, p12|||Deformed and metamorphosed at ca. 1600 Ma and ca. 1550 Ma. Upper part has a different zircon provenance to the lower Etheridge Group and more radiogenic eNd values. Lower part intruded by dolerite dykes and sills at ca. 1660 Ma. Intruded by orthogneiss with a zircon U-Pb crystallisation age of ca. 1694 Ma. Misspelt Ethridge Group p4. Age range shown as ~1720-1600 Ma.|||||Sedimentary and mafic rocks in lower part, regionally deformed and variably metamorphosed, locally to granulite facies. Fine-grained sedimentary rocks in upper part.|
6300|Etheridge Group|75079|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Regarded as the protolith of Einasleigh Metamorphics.|1700-1650 Ma.|||Is overlain unconformably by the Croydon Volcanic Group. Is intruded by Deadhorse Metabasalt and Cobbold Metadolerite.|Deformed metasedimentary sequence: low-grade shales and sandstones in the west, to high-grade metapelites and psammites in the east. Is interlayered with c.1665 Ma mafic lava flows, and intruded by similarly-aged dykes and sills.|
6314|Etna Formation|31659|6|Mentioned|p28|||Now included in Mt. Holly Beds||||||
6314|Etna Formation|38081|5|Briefly described|Table 1|||||||||
6314|Etna Formation|38390|6|Mentioned|p7|||||||||
6314|Etna Formation|41922|4|Described|Table 1, P11|||||||||
6314|Etna Formation|43998|4|Described|p21,map|Carboniferous|Devonian|See also Lexicon.||||||
6319|Etonvale Formation|22464|5|Briefly described|p9|Late Devonian|Middle Devonian|Adavale Basin. Overlies Cooladdi Dolomite||||||
6319|Etonvale Formation|22518|5|Briefly described|p 10, Fig 3|||Adavale Basin||||||
6319|Etonvale Formation|22604|5|Briefly described|p442||Devonian|Possibly Eifelian in age.||||||18-SEP-06
6319|Etonvale Formation|23834|4|Described|p314|Early Devonian|Early Devonian|Geological Province: Adavale Basin.||||||
6319|Etonvale Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6319|Etonvale Formation|29387|6|Mentioned|Table 1|||||||||
6319|Etonvale Formation|29391|6|Mentioned|Table 2|||See P14.||||||
6319|Etonvale Formation|29393|6|Mentioned|Table 1|||Middle Devonian.||||||
6319|Etonvale Formation|29721|6|Mentioned|p38|||||||||
6319|Etonvale Formation|29753|4|Described|Table 2|||||||||
6319|Etonvale Formation|30103|5|Briefly described|p5|||Part of Adavale Group. Table 2 on p5. See also p6.||||||18-SEP-06
6319|Etonvale Formation|30104|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|30544|6|Mentioned|p52|||||||||
6319|Etonvale Formation|30691|4|Described|p7|||See also p20,Table 6.||||||18-SEP-06
6319|Etonvale Formation|30853|1|Redefined|p24|Middle Devonian|Middle Devonian|See also Table 2.||||||18-SEP-06
6319|Etonvale Formation|30854|4|Described|Table 2|||Middle Devonian||||||
6319|Etonvale Formation|30855|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|31150|6|Mentioned|p98|||Refers de Jersey (1966)||||||
6319|Etonvale Formation|31250|6|Mentioned|p10|||||||||
6319|Etonvale Formation|31431|5|Briefly described|Table 2|||Mid.Dev.-L.Carboniferous||||||
6319|Etonvale Formation|31436|6|Mentioned|Map legend|Early Carboniferous|Middle Devonian|Middle Devonian to Lower Carboniferous||||||
6319|Etonvale Formation|31438|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|31999|5|Briefly described|p135|||Table 1||||||
6319|Etonvale Formation|32619|6|Mentioned|p463|||Fauna. Givetian.||||||
6319|Etonvale Formation|32640|6|Mentioned|p241|||||||||
6319|Etonvale Formation|32865|6|Mentioned|p483|||Fauna. Givetian||||||
6319|Etonvale Formation|33069|4|Described|p6|||Mid. Dev.||||||
6319|Etonvale Formation|33078|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|33079|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|33087|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|33088|4|Described|Table 2|||Of the Adavale Gp.||||||18-SEP-06
6319|Etonvale Formation|33092|5|Briefly described|p5|||Strat. table||||||
6319|Etonvale Formation|33192|6|Mentioned|p19|||||||||
6319|Etonvale Formation|33641|6|Mentioned|p59|||M.Dev.||||||
6319|Etonvale Formation|33732|6|Mentioned|p103|||||||||
6319|Etonvale Formation|34065|4|Described|p7|||Middle Devonian.||||||18-SEP-06
6319|Etonvale Formation|34217|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6319|Etonvale Formation|34218|5|Briefly described|Table 1|||See also Tables 2,3. Middle Devonian.||||||
6319|Etonvale Formation|35030|6|Mentioned|p335|||||||||
6319|Etonvale Formation|37565|6|Mentioned|Fig.6|||||||||
6319|Etonvale Formation|38226|5|Briefly described|p414|||||||||
6319|Etonvale Formation|39445|5|Briefly described|Table 5|||See also p73.||||||18-SEP-06
6319|Etonvale Formation|39478|6|Mentioned|Table 1|||||||||
6319|Etonvale Formation|39482|6|Mentioned|Fig.5|||||||||
6319|Etonvale Formation|39494|6|Mentioned|Fig.3|||||||||
6319|Etonvale Formation|39998|6|Mentioned|p192|||||||||
6319|Etonvale Formation|40030|6|Mentioned|Fig.3|||||||||
6319|Etonvale Formation|40322|6|Mentioned|Fig.3|||||||||
6319|Etonvale Formation|40544|6|Mentioned|Fig.4|||||||||
6319|Etonvale Formation|41097|6|Mentioned|p163|||See also Table 1||||||
6319|Etonvale Formation|41167|6|Mentioned|p398|||||||||
6319|Etonvale Formation|41198|6|Mentioned|p35|||See also Table 1||||||
6319|Etonvale Formation|41208|6|Mentioned|Fig.1|||||||||
6319|Etonvale Formation|41247|6|Mentioned|Fig.5|||||||||
6319|Etonvale Formation|41289|5|Briefly described|p211|||||||||
6319|Etonvale Formation|41492|6|Mentioned|p154|||||||||
6319|Etonvale Formation|42351|6|Mentioned|p46|||Adavale Basin||||||
6319|Etonvale Formation|42564|6|Mentioned|p12|||Adavale Basin.||||||
6319|Etonvale Formation|42999|5|Briefly described|p89,Table1,p90|||||||||
6319|Etonvale Formation|43004|5|Briefly described|Table 1,p179|||||||||
6319|Etonvale Formation|43105|5|Briefly described|Fig.5,p10|||||||||
6319|Etonvale Formation|43461|14|Not recorded|p617,table p618|||M.Dev.overlaps on Gilmore Formation (Gilmore Formation was renamed Log Creek Formation)||||||
6319|Etonvale Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
6319|Etonvale Formation|43914|14|Not recorded|p1,3,5-9,11-14,16,19|||p24-26,Fig.2,3||||||
6319|Etonvale Formation|43975|14|Not recorded|p1,2|||||||||
6319|Etonvale Formation|44091|14|Not recorded|p33||Middle Devonian|||||||
6319|Etonvale Formation|44419|14|Not recorded|p279|||||||||
6319|Etonvale Formation|44701|14|Not recorded|p9||Middle Devonian|||||||
6319|Etonvale Formation|44770|14|Not recorded|p111-116|||Unconformable on Gilmore Formation. Part of Adavale Group.||||||
6319|Etonvale Formation|44839|14|Not recorded|p20|||||||||
6319|Etonvale Formation|44841|14|Not recorded|p27|||||||||
6319|Etonvale Formation|44842|14|Not recorded|p20||Devonian|||||||
6319|Etonvale Formation|44851|4|Described|p172|Devonian|Late Silurian|(Late Silurian - Early and Middle Devonian)||||||
6319|Etonvale Formation|44852|14|Not recorded|p73|Devonian|Silurian|Uppermost Silurian-Middle Devonian.||||||
6319|Etonvale Formation|44875|14|Not recorded|p11,15|||||||||
6319|Etonvale Formation|44888|14|Not recorded|p32|||||||||
6319|Etonvale Formation|44889|14|Not recorded|p160|Devonian|Late Silurian|Late Silurian - Middle-Upper? Devonian||||||
6319|Etonvale Formation|44895|14|Not recorded|p2|||||||||
6319|Etonvale Formation|44896|14|Not recorded|p18|||||||||
6319|Etonvale Formation|44899|14|Not recorded|p24|||||||||
6319|Etonvale Formation|45073|6|Mentioned|p46|||Geological history||||||
6319|Etonvale Formation|46881|6|Mentioned|Table.2|||||||||
6319|Etonvale Formation|48920|6|Mentioned|p85|||Refers Heikkila (1965)||||||
6319|Etonvale Formation|48995|5|Briefly described|p3|||||||||
6319|Etonvale Formation|62985|5|Briefly described|p16|Frasnian|Givetian|Unconformably overlies Lissoy Sandstone, Boree Salt and Bury Limestone. Geol. prov: Adavale Basin. Quartzose sandstone, mudstone, shale and minor limestone.||||||
6319|Etonvale Formation|64783|1|Redefined|p100-102, 82, 84,87-90, 93-94,96-99,104|Frasnian|Givetian|Name first used by Phillips Petroleum Company (1963) and the type section was designated in 1964 within PPC Etonvale-1 at 1910.2-3057.1 m depth. It included the later Log Creek, Etonvale and Buckabie Formations. Galloway (1970) redefined the type section to 2011.7-2335.4m to exclude the Log Creek and Buckabie Formations, but still included the Cooladdi Dolomite Member and the Boree Salt Member. These were excluded by Auchincloss (1976) and Boreham and De Boer (1998) respectively, so the type section is here taken to be the 2011.7-2298 m interval in PPC Etonvale-1.  Age is latest Givetian to early Frasnian.||||Unconformably overlies the Gumbardo Formation, Cooladdi Dolomite, Boree Salt, Bury Limestone and Lissoy Sandstone. Is overlain conformably by Buckabie Formation.|Up to 762m thick. Quartzose sandstone, mudstone, shale and minor limestone. Minor anhydrite and sparite also occur, and shale rip-up clasts are present in some cores. Grey to red and green calcareous to dolomitic cements are common.|15-NOV-17
6319|Etonvale Formation|66127|5|Briefly described|p441.|Frasnian|Givetian|Adavale Basin. Palynoflora correlate this unit with Gneudna Formation of Carnarvon Basin and Canning Basin reef complexes, WA.||||||
6319|Etonvale Formation|67402|4|Described|p167 fig ADV/WRR3|Frasnian|Frasnian|Adavale Basin. Deposited in a shallow marine to restricted marginal-marine and arid fluvial environments. See also p168-p170, p172, p173, p175.||||Overlain by the Buckabie Formation.|Quartzose sandstone, shale and mudstone with minor anhydrite and sparite.|
6319|Etonvale Formation|68731|5|Briefly described|p178, p179, p180 Tb 3.3, p223 Fig 3.126|Late Devonian|Middle Devonian|Adavale Basin. Deposited in a fluvial to marginal marine environment under arid conditions. Between 40.4-762 m thick. Absent in the far north and northwest of the Adavale Basin.||||Overlain by the Buckabie Formation.|Comprises quartz sandstone, mudstone and shale. Minor anhydrite and sparite occur, and shale rip-up clasts are present in some cores. Generally contains calcareous to dolomitic cements and are grey to red and green.|10-MAY-16
6319|Etonvale Formation|72297|5|Briefly described|p724|||Along the western edge of the Adavale Basin.|||Boree Salt Member.|||
6319|Etonvale Formation|73179|5|Briefly described|p1135 Fig.2, p1136, p1137 Fig.4|Frasnian|Frasnian|Adavale Basin.||||Unconformably underlain by Boree Salt Member. Overlain by Buckabie Formation.|Shallow marine shale, sandstone and carbonate. Includes fine- to medium-grained sandstone and pelitic sandstone.|26-SEP-22
6356|Eulo Queen Group|9541|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Includes Loth Formation and Hampstead Sandstone.||||||
6356|Eulo Queen Group|22744|5|Briefly described|P12, Table3 P10||Jurassic|||||||
6356|Eulo Queen Group|22747|5|Briefly described|p9||Mesozoic|Eromanga Basin||||||
6356|Eulo Queen Group|23032|5|Briefly described|p47|Late Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|23291|4|Described|p81 Tb 3.6|Late Jurassic|Middle Jurassic|Geological Province: Georgetown Region.||||||08-JUL-15
6356|Eulo Queen Group|23425|4|Described|Plate 9.3 p379.|||Comprises the Hampstead Sandstone and Loth Formation. Also see Table 9.7 p395. Overlain by Gilbert River Formation. Carpentaria Basin Province.||||||08-DEC-08
6356|Eulo Queen Group|23426|5|Briefly described|p403|||Carpentaria Basin Province.||||||
6356|Eulo Queen Group|23430|5|Briefly described|p455.|||Eromanga Basin Province||||||
6356|Eulo Queen Group|23453|5|Briefly described|p20|Cretaceous|Cretaceous|||||||
6356|Eulo Queen Group|23846|5|Briefly described|p5|Jurassic|Jurassic|Includes Hampstead Sandstone and Loth Formation. Quartzose sandstone, conglomerate, silstone, and shale. Underlies Gilbert River Formation. Geological province: Eronmanga Basin.||||||18-SEP-06
6356|Eulo Queen Group|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|24073|5|Briefly described|p378 Table 2|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|30020|6|Mentioned|p29|||||||||
6356|Eulo Queen Group|30587|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|31164|5|Briefly described|p9|||Water supplies||||||
6356|Eulo Queen Group|31422|5|Briefly described|Map legend|Jurassic|Jurassic|Quartzose sandstone and siltstone, shale, conglomerate.||||||02-DEC-04
6356|Eulo Queen Group|31433|5|Briefly described|p8|||Correlation. Jurassic||||||
6356|Eulo Queen Group|31434|6|Mentioned|p8|||Refer Smart et al.(1971)||||||
6356|Eulo Queen Group|32531|6|Mentioned|Fig.2|||On p474.||||||18-SEP-06
6356|Eulo Queen Group|32705|6|Mentioned|p179|||See also p183.||||||18-SEP-06
6356|Eulo Queen Group|32706|6|Mentioned|p10|||||||||
6356|Eulo Queen Group|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
6356|Eulo Queen Group|33176|4|Described|p171|||||||||
6356|Eulo Queen Group|33177|6|Mentioned|p10|||||||||
6356|Eulo Queen Group|33178|6|Mentioned|p11|||||||||
6356|Eulo Queen Group|33182|6|Mentioned|p190|||||||||
6356|Eulo Queen Group|33183|2|Defined|p230|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|33644|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
6356|Eulo Queen Group|33648|4|Described|p19|||||||||
6356|Eulo Queen Group|33882|6|Mentioned|p19|||||||||
6356|Eulo Queen Group|33907|6|Mentioned|p5|||||||||
6356|Eulo Queen Group|35220|6|Mentioned|p16|||||||||
6356|Eulo Queen Group|35811|5|Briefly described|Table 3|||||||||
6356|Eulo Queen Group|35814|6|Mentioned|p582|||||||||
6356|Eulo Queen Group|35920|6|Mentioned|p26|||||||||
6356|Eulo Queen Group|35921|6|Mentioned|p31|||||||||
6356|Eulo Queen Group|36228|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|36229|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
6356|Eulo Queen Group|37576|6|Mentioned|p34|||||||||
6356|Eulo Queen Group|37603|6|Mentioned|p444|||||||||
6356|Eulo Queen Group|37608|3|Fully described|Table 1|||See also Table 2.||||||
6356|Eulo Queen Group|38199|6|Mentioned|Fig.1|||||||||
6356|Eulo Queen Group|39211|6|Mentioned|p36|||Fig.26||||||
6356|Eulo Queen Group|39337|6|Mentioned|Fig.1|||||||||
6356|Eulo Queen Group|39445|5|Briefly described|p128|||Sedimentation cycles. See also Table 10||||||
6356|Eulo Queen Group|39797|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
6356|Eulo Queen Group|39917|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|40218|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Late Jurassic||||||
6356|Eulo Queen Group|40659|6|Mentioned|p250|||||||||
6356|Eulo Queen Group|41064|6|Mentioned|p60|||||||||
6356|Eulo Queen Group|41125|6|Mentioned|p42|||||||||
6356|Eulo Queen Group|41266|6|Mentioned|Fig.3|||||||||
6356|Eulo Queen Group|42061|4|Described|p155|||See also Fig.11||||||
6356|Eulo Queen Group|42637|5|Briefly described|p9|||||||||
6356|Eulo Queen Group|43286|5|Briefly described|Map Legend||Jurassic|||||||
6356|Eulo Queen Group|43603|5|Briefly described|p9|Late Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
6356|Eulo Queen Group|45145|3|Fully described|Table 5|||||||||
6356|Eulo Queen Group|46791|6|Mentioned|Table 2|||||||||
6356|Eulo Queen Group|46937|6|Mentioned|Fig.10|||||||||
6356|Eulo Queen Group|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
6356|Eulo Queen Group|49011|6|Mentioned|Fig.3|||Carpentaria Basin||||||
6356|Eulo Queen Group|50199|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Loth Formation, Hampstead Sandstone.||||||
6356|Eulo Queen Group|50200|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Loth Formation, Hampstead Sandstone.||||||
6356|Eulo Queen Group|50201|5|Briefly described|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|50210|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Hampstead Sandstone, Loth Formation.  Underlies: Gilbert River Formation.||||||
6356|Eulo Queen Group|50211|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes the Loth Formation and Hampstead Sandstone.||||||17-MAY-04
6356|Eulo Queen Group|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Includes: Hampstead Sandstone, Loth Formation.||||||
6356|Eulo Queen Group|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Includes the Hampstead Sandstone, and Loth  and Gilbert River Formations.||||||06-JUL-04
6356|Eulo Queen Group|60081|5|Briefly described|Map legend|Late Jurassic|Jurassic|Includes the Loth and Hamspstead Sandstone.  Quartzose sandstone, siltstone, minor shale and conglomerate.||||||22-JUL-04
6356|Eulo Queen Group|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Hettangian|Age: 205-180 Ma. Geological Province: Burketown Depression.||||||01-MAR-10
6356|Eulo Queen Group|64707|5|Briefly described|Map legend|Jurassic|Jurassic|Includes Loth Formation and Hampstead Sandstone.||||||
6356|Eulo Queen Group|66529|6|Mentioned|p12 Fig.5 |||Presented as Eulo Qn Gp in figure, and does not appear elsewhere in article. Carpentaria Basin.|||Includes Hampstead Sandstone and Loth Formation.|||
6356|Eulo Queen Group|67323|5|Briefly described|p86, p96, p106|Jurassic|Jurassic|Carpentaria Basin. Appears as Eulo Queen beds on p86. A regional aquifer.||||||
6356|Eulo Queen Group|67402|5|Briefly described|p165 tbl LPB1, p176|Kimmeridgian|Oxfordian|Carpentaria Basin, Staaten Sub-basin. Contains aquifers. Generally 100m thick. See also p177, p180, p181 tbl CRP/KRM2, p226, p231.|||Includes the Loth Formation and Hampstead Sandstone.|Unconformably overlain by the Garraway Sandstone.||
6356|Eulo Queen Group|68349|5|Briefly described|Map legend.|Late Jurassic|Middle Jurassic|Carpentaria Basin.|||Includes Hampstead Sandstone and Loth Formation.|Is overlain conformably by Gilbert River Formation.||
6356|Eulo Queen Group|68417|6|Mentioned|Map Legend|Late Jurassic|Middle Jurassic|Of the Carpentaria Basin.|||Includes Loth Formation, Hampstead Sandstone.|Conformably overlain by the Gilbert River Formation.|Sandstone, siltstone, mudstone, conglomerate.|
6356|Eulo Queen Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Eromanga and Carpentaria Basins. This unit is mapped with the Blantyre Sandstone under the symbol, Ju.||||||
6356|Eulo Queen Group|69297|6|Mentioned|p274 fig 4.3|Late Jurassic|Middle Jurassic |||||||
6356|Eulo Queen Group|69455|5|Briefly described|p39:15|||Southern Carpentaria Basin. Areally restricted.||||Is overlain by the Gilbert River Formation.|Includes quartzic sandstone.|12-JUL-16
6356|Eulo Queen Group|69591|5|Briefly described|p100|Jurassic|Jurassic|Fill in the Burketown Depression, overlying probably Permian tilloids.|||||Quartzose sandstones.|
6356|Eulo Queen Group|69594|5|Briefly described|p518, p521, p527-528, p540, p573|Late Jurassic|Middle Jurassic|Southern Staaten Sub-basin, Carpentaria Basin; extends into the northern Eromanga Basin. Deposited in palaeotopographic depressions. The two constituents are not differentiated in the Eromanga Basin.|||Hampstead Sandstone, Loth Formation.|Is overlain disconformably/unconformably by the Gilbert River Formation. Part-equivalent to Dalrymple Sandstone (Laura Basin).||
6356|Eulo Queen Group|70207|6|Mentioned|p14|Jurassic|Jurassic|Georgetown region.||||||
6356|Eulo Queen Group|72297|5|Briefly described|p746|||Carpentaria Basin. Excellent hydrocarbon reservoir potential because it contains aquifers.|||Garraway Sandstone.|||
6356|Eulo Queen Group|72298|5|Briefly described|p801|Jurassic|Jurassic|Carpentaria Basin.|||Hampstead Sandstone, Loth FZ.|Is overlain by Gilbert River FZ.||
6356|Eulo Queen Group|73144|6|Mentioned|p8|Jurassic|Jurassic|Carpentaria Basin. Aquifer. Basal and upper unconformity.||||||
6356|Eulo Queen Group|73147|5|Briefly described|p126-130|Late Jurassic|Middle Jurassic|Gregory Range area.|||Hampstead Sandstone, Loth Formation.|Is overlain by Yappar Member (Gilbert River Formation).||
6357|Eulogie Park Gabbro|24491|5|Briefly described|p25|||||||||
6357|Eulogie Park Gabbro|24571|6|Mentioned|p6, 27|||||||||
6357|Eulogie Park Gabbro|24615|5|Briefly described|CD|Triassic|Triassic|[Rgep].  Layered olivine gabbro, augite troctolite, ferrigabbro, leucogabbro, magnetic bands.||||||
6357|Eulogie Park Gabbro|29455|6|Mentioned|p23|||||||||
6357|Eulogie Park Gabbro|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
6357|Eulogie Park Gabbro|31658|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6357|Eulogie Park Gabbro|31659|4|Described|p90|||Post Lower Carb.||||||
6357|Eulogie Park Gabbro|32358|4|Described|p17|||Table 4||||||
6357|Eulogie Park Gabbro|38081|5|Briefly described|Table 2|||||||||
6357|Eulogie Park Gabbro|38406|6|Mentioned|p13|||||||||
6357|Eulogie Park Gabbro|39252|6|Mentioned|p28|||||||||
6357|Eulogie Park Gabbro|39445|5|Briefly described|Table 12|||||||||
6357|Eulogie Park Gabbro|41246|6|Mentioned|Map legend|Permian||||||||
6357|Eulogie Park Gabbro|41922|4|Described|Table 2, P13|||||||||
6357|Eulogie Park Gabbro|43775|6|Mentioned|p28|||||||||
6357|Eulogie Park Gabbro|44820|14|Not recorded|p139,141-150,152-157|||Probably early Triassic or Permian||||||
6357|Eulogie Park Gabbro|45087|5|Briefly described|p76|||Chemical analyses.||||||
6357|Eulogie Park Gabbro|50190|6|Mentioned|p36|||On the MOUNT MORGAN 1:100k sheet.||||||
6357|Eulogie Park Gabbro|50317|5|Briefly described|Map Legend|Triassic|Triassic|Layered olive gabbro, augite troctolite, ferrigrabbro, leucogabbro, magnetite bands.||||||09-JUN-04
6357|Eulogie Park Gabbro|60282|6|Mentioned|p39|||On the MOUNT MORGAN map sheet.||||||
6357|Eulogie Park Gabbro|65388|5|Briefly described|p322, 323|Triassic|Permian|Mount Morgan sheet area. One of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton. Displays 'diorite intruding gabbro' relationship. Compared with Kariboe Layered Gabbro.||||||
6357|Eulogie Park Gabbro|68008|3|Fully described|p50,p61,p368,p429-432,p435,p486,p624-625|Early Triassic||Wilson and Mathison (1968). Variation in mineral composition from base to top studied by Bourke (1995). 25km S of Mount Morgan. Comprises several outcrops separated by intrusions and faulting. Named after Eulogie Park homestead. The type section trends NE across the widest part of the largest remnant, at right angles to layering. Forms semicircular ridges. Geophysics detailed and modelled; lies along the Marlborough Gravity Ridge. Comprises about 65 saucer-shaped layers dipping SW at c.30 degrees; at least 1350m thick. Geochemistry described. No dated; a diorite 2km NW of Eulogie Park homestead gave a K-Ar age of 241.6 +/- 3 Ma. Possible source of ilmenite.||||Intrudes Balaclava and Mount Hoopbound Formations.|Layered gabbro. Repetitions of six main rock types: olivine gabbro, ferrigabbro, troctolite, leucogabbro, gabbro and magnetite-rich rocks. Also a later relatively uniform, medium-grained diorite.|
6357|Eulogie Park Gabbro|68679|5|Briefly described|p423-425|||Yarrol belt. A tilted, funnel-shaped lopolith with c.65 saucer-shaped, laterally continuous layers. Up to ~900m thick. Includes a western mass of layered gabbroic rocks ~450m thick.||||Intrudes Balaclava Formation.|Layered olivine gabbro, augite troctolite, ferrigabbro, leucogabbro, magnetite bands. Tholeiitic to transitional.|
6357|Eulogie Park Gabbro|72297|5|Briefly described|p728||||||||Contains cumulate bands with ilmenite, titanomagnetite, feldspar, vanadium oxide and minor apatite.|
6371|Eungella Granodiorite|23052|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
6371|Eungella Granodiorite|23161|5|Briefly described|p44 table6||Early Cretaceous|Rb/Sr Ages: 127+/-2Ma, 127Ma & 128Ma.||||||
6371|Eungella Granodiorite|42701|2|Defined|p98|Early Cretaceous||Age 127 +/- 2Ma, Rb/Sr, K/Ar. Variation on Eungella Complex.||||||
6371|Eungella Granodiorite|44245|5|Briefly described|Map Legend||Cretaceous|||||||
6371|Eungella Granodiorite|69594|6|Mentioned|p570|||Geochemistry plots and discussion.||||||
6371|Eungella Granodiorite|73037|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Fine to medium-grained hornblende, biotite granodiorite.|
6386|Eurombah Formation|12597|5|Briefly described|p492 Tb.1, p496|Callovian|Callovian|N Surat Basin. Up to 100m thick.||Unit in Injune Creek Group.|||Interbedded lithic sandstone and minor polymictic conglomerate, siltstone and mudstone.|
6386|Eurombah Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Middle Jurassic|Middle Jurassic|In Surat Basin, Eromanga Basin.||||||
6386|Eurombah Formation|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig. 22.8|Bathonian|Bajocian|Of the Injune Creek Group. Geological Province: Surat Basin.||||||
6386|Eurombah Formation|22865|5|Briefly described|Table22.1p296-7||Bajocian|||||||
6386|Eurombah Formation|23056|6|Mentioned|10|||Geol province Eromanga Basin||||||
6386|Eurombah Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
6386|Eurombah Formation|24068|4|Described|p270 Table 2|Middle Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 95m.||||||
6386|Eurombah Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
6386|Eurombah Formation|30699|6|Mentioned|p53|||Middle Jurassic age||||||
6386|Eurombah Formation|33367|3|Fully described|p16|||||||||
6386|Eurombah Formation|33371|2|Defined|p57|Jurassic|Jurassic|See also p58.?mid Jurassic.||||||
6386|Eurombah Formation|33672|5|Briefly described|p44|||||||||
6386|Eurombah Formation|33774|6|Mentioned|p55|||Refers Swarbrick et al. (1973)||||||
6386|Eurombah Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
6386|Eurombah Formation|35937|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|36243|6|Mentioned|Table 6A|||||||||
6386|Eurombah Formation|36570|6|Mentioned|p66|||||||||
6386|Eurombah Formation|37117|5|Briefly described|p313|||||||||
6386|Eurombah Formation|37463|6|Mentioned|p479|||||||||
6386|Eurombah Formation|37993|6|Mentioned|Fig.2|||||||||
6386|Eurombah Formation|37995|4|Described|p64|||||||||
6386|Eurombah Formation|39212|5|Briefly described|p16|||||||||
6386|Eurombah Formation|39445|5|Briefly described|Table 10|||||||||
6386|Eurombah Formation|39494|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|39943|6|Mentioned|Table 9A|||||||||
6386|Eurombah Formation|40030|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|40245|6|Mentioned|Table 2|||||||||
6386|Eurombah Formation|40249|6|Mentioned|p38|||Mention P41||||||
6386|Eurombah Formation|40250|6|Mentioned|Fig.7|||||||||
6386|Eurombah Formation|40541|6|Mentioned|p114|||||||||
6386|Eurombah Formation|40544|6|Mentioned|Fig.6|||||||||
6386|Eurombah Formation|41187|5|Briefly described|p225|||||||||
6386|Eurombah Formation|41247|6|Mentioned|Fig.7|||||||||
6386|Eurombah Formation|41266|6|Mentioned|Fig.3|||||||||
6386|Eurombah Formation|41992|4|Described|Fig.2 P183|||||||||
6386|Eurombah Formation|42007|5|Briefly described|Fig.2 P182|||||||||
6386|Eurombah Formation|42248|6|Mentioned|p410|||||||||
6386|Eurombah Formation|42493|5|Briefly described|Fig. 1 P18|||||||||
6386|Eurombah Formation|42911|5|Briefly described|p13, p37|||||||||
6386|Eurombah Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
6386|Eurombah Formation|43002|5|Briefly described|Fig.2,p135|||||||||
6386|Eurombah Formation|45110|2|Defined|p93|Middle Jurassic|Middle Jurassic|See also p24. Formerly Eurombah Beds, Exon (1971).||||||
6386|Eurombah Formation|46937|6|Mentioned|Fig.10|||||||||
6386|Eurombah Formation|46984|6|Mentioned|Table 1|||||||||
6386|Eurombah Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
6386|Eurombah Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
6386|Eurombah Formation|60995|6|Mentioned|p66|||Geological Province: Surat Basin. ||||||
6386|Eurombah Formation|60999|5|Briefly described|p177, p178 Fig. 10|||Partly equivalent to Walloon Coal Measures.  Geological Province: Surat Basin.||||||
6386|Eurombah Formation|61000|5|Briefly described|p183|Bajocian|Bajocian|Geological Province: Surat Basin.||||||
6386|Eurombah Formation|61377|5|Briefly described|p148 Tb. SU1|Early Jurassic|Early Jurassic|Labile sandstone, polymictic conglomerate, siltstone, mudstone. Geological Province: Surat Basin.||||||07-FEB-11
6386|Eurombah Formation|63218|6|Mentioned|p211 Fig.2, p212 Fig.3. |Middle Jurassic|Middle Jurassic|Surat Basin.||Basal unit in Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Durabilla Formation.||
6386|Eurombah Formation|64197|6|Mentioned|p630 Fig.7|Middle Jurassic|Middle Jurassic|||||Underlies the Walloon Coal Measures, overlies the Hutton Sandstone.||
6386|Eurombah Formation|64665|5|Briefly described|p60.|Middle Jurassic|Middle Jurassic|Surat Basin. With the Hutton Sandstone and Walloon Subgroup, forms the second of six cyclothems.||||Overlies Hutton Sandstone. Is overlain by Walloon Subgroup.||
6386|Eurombah Formation|64856|4|Described|p86-87|Middle Jurassic|Middle Jurassic|Swarbrick et al. (1973). Formerly Eurombah beds of Exon et al. (1967). Type section set as the interval 27-120m in stratigraphic bore DRD 22. Surat Basin. Conformably overlies Hutton Sandstone. Thickly cross-bedded, fine to coarse-grained sandstones and interbedded siltstones and mudstones. Included in the Walloon Coal Measures in this article (and therefore of Middle Jurassic age).| | ||||28-NOV-17
6386|Eurombah Formation|64857|5|Briefly described|p132-133, p113 Fig.3|||Surat Basin. Sublabile to labile sandstones. Relationship with overlying unit not clear: Text states it underlies Walloon Coal Measures, however figures suggest Hutton Sandstone underlies Walloon Coal Measures.||||||
6386|Eurombah Formation|65003|6|Mentioned|p32|||||||||
6386|Eurombah Formation|65096|5|Briefly described|p368, p370 Fig.2|Middle Jurassic|Middle Jurassic|Previously Eurombah Beds of Exon (1971). Later defined as Formation (Swarbrick et al., 1973). ~100 m thick. Distinguishable from underlying Hutton Sandstone by higher gamma response, lower resistivity, flat SP response and much lower water production. Not readily distinguishable from overlying units - lithologically or on wireline logs.||Of the Walloon Coal Measures/Walloon Subgroup.||Gradationally overlies the Hutton Sandstone.|Variably a sandstone or shale and is largely devoid of coal.|
6386|Eurombah Formation|65117|5|Briefly described|p469, 470, Fig 4 p465|Bathonian|Middle Jurassic|Conformably overlies Hutton Sandstone and conformably underlies and interfingers with Walloon Coal Measures. Not laterally extensive. Lithic conglomeratic sandstone with mudstone and siltstone beds. Up to 100m thick. Seismic resolution does not allow identification of base of unit.||||||
6386|Eurombah Formation|65388|5|Briefly described|p214, 215|||Basal Injune Creek Group in SW Bungaban map sheet area. Defined by Swarbrick & others (1973), but cannot  be consistently differentiated from Walloon Coal Measures (Green & others, 1997). Poor outcrop. Overlies Hutton Sandstone.||||||
6386|Eurombah Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|68117|4|Described|p345-349|Middle Jurassic|Middle Jurassic|Swarbrick, Gray and Exon (1973) in their redefinition of the Injune Creek Group of Exon (1966). Recognised throughout the eastern Surat Basin. 80m thick, thinning to zero eastwards. Recognisable in resistivity and spontaneous potential logs.||Basal Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Durabilla Formation (Walloon Subgroup).|Porous sandstones.|
6386|Eurombah Formation|68139|5|Briefly described|p25 Fig.4|Middle Jurassic|Middle Jurassic|"Surat Basin. Appears as ""Durabilla Formation""/Eurombah Formation. Scott et al. (2004) had this Formation underlying the Durabilla Formation which was their basal unit in the Walloon Subgroup."||Basal Walloon Subgroup.||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
6386|Eurombah Formation|69574|6|Mentioned|p24|||"Surat Basin. Presented on p24 as ""Durabilla Formation""/Eurombah Formation."||||||
6386|Eurombah Formation|69582|5|Briefly described|p38|||Surat Basin.|||||Sandstone, mudstone and coal.|
6386|Eurombah Formation|69594|5|Briefly described|p536|||Exon et al. (1967); Swarbrick et al. (1973). Surat Basin. Has been included in basal Injune Creek Group (Exon, 1971), and Walloon Coal Measures (Green et al., 1997). Fluviatile deposits. In this study, it is regarded as a Member of the Walloon Coal Measures only in the NE Surat Basin.||||Conformably overlies the Hutton Sandstone.|Sublabile sandstone with minor interbedded conglomerate and carbonaceous mudstone. Contains a significant volcanic detrital component, unlike the underlying Hutton Sandstone.|
6386|Eurombah Formation|69790|5|Briefly described|p1066|||Early nomenclatural work restricted this unit to W side of the Mimosa Syncline. Its continued recognition is under debate: in this article it is included in Durabilla Formation.||||Overlies Hutton Sandstone. Is overlain by Walloon Subgroup.||
6386|Eurombah Formation|70374|5|Briefly described|p808, p809, figure 1,p813|Callovian|Callovian|Previously considered Bathonian - Callovian age. New dating within overlying Walloon Coal Measures, Surat Basin, suggest this unit now wholly Callovian. Amalgamated with Durabilla Formation in areas where the wireline log responses cannot be distinguished. ||Included in Walloon Subgroup by some, but not in Walloon Coal Measures by others.||Overlies Hutton Sandstone. Underlies Walloon Coal Measures conformably. Underlies Taroom Coal Measures.||28-SEP-16
6386|Eurombah Formation|70628|5|Briefly described|p952,953|Jurassic|Jurassic|Age inferred from stratigraphic description.||||Grades up into Walloon Subgroup (Taroom Coal Measures), overlies Hutton Sandstone conformably.|Heterolithic succession of isolated channel sandstones encased in overbank and flood-basin siltstones and mudstones, fines upward.|
6386|Eurombah Formation|70725|6|Mentioned|p13|Middle Jurassic|Middle Jurassic|Surat Basin. Is presented as Durabilla/Eurombah Formation.||||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
6386|Eurombah Formation|70821|5|Briefly described|p80|||Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|72297|5|Briefly described|p699 Fig.10.11|Jurassic|Jurassic|Surat Basin.||||Is overlain ?conformably by Walloon Coal Measures or Walloon Subgroup.||
6386|Eurombah Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|72921|4|Described|p13, p15 Fig.2, p16, p20, p40-42,46|Middle Jurassic|Middle Jurassic|Shown as located in the Surat Basin in Queensland.  Acts an aquitard between the Walloon Coal Measures and the Hutton Sandstone.||||Overlies and is equivalent to Hutton Sandstone and is underlying Walloon Coal Measures.||
6386|Eurombah Formation|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
6386|Eurombah Formation|73393|6|Mentioned|p20-22|Callovian|Bathonian|Surat Basin.||Injune Creek Group||Underlain by Hutton Sandstone. Overlain by Walloon Coal Measures. Equivalent to Birkhead Formation.||
6400|Eva Creek Microgranite|9539|5|Briefly described|Map legend|Permian|Carboniferous|||||||
6400|Eva Creek Microgranite|22669|6|Mentioned|P259||Visean|Age of unit is 320+/-4 Ma||||||
6400|Eva Creek Microgranite|23291|5|Briefly described|p97 Tb. 3.11|Namurian|Namurian|Of the Newcastle Range I-types. Age: 320-317Ma. Geological Province: Georgetown Region.||||||29-MAY-15
6400|Eva Creek Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 26. I-Type.||||||
6400|Eva Creek Microgranite|33909|2|Defined|p231|Late Paleozoic|Late Paleozoic|Prob.Late Palaeozoic||||||07-NOV-08
6400|Eva Creek Microgranite|35214|6|Mentioned|p8|||||||||
6400|Eva Creek Microgranite|37571|5|Briefly described|p141|||||||||
6400|Eva Creek Microgranite|39445|5|Briefly described|Table 12|||Georgetown Inlier. See also P90||||||
6400|Eva Creek Microgranite|39687|6|Mentioned|Fig.2|||||||||
6400|Eva Creek Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
6400|Eva Creek Microgranite|41272|6|Mentioned|M 1of1 K04|||||||||
6400|Eva Creek Microgranite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
6400|Eva Creek Microgranite|43664|6|Mentioned|p96|||||||||
6400|Eva Creek Microgranite|43740|4|Described|p17|||||||||
6400|Eva Creek Microgranite|46845|6|Mentioned|Table 1|||||||||
6400|Eva Creek Microgranite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||||||
6400|Eva Creek Microgranite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Biotite microgranite and fine-grained leucogranite.||||||
6400|Eva Creek Microgranite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. High K, Th and U radiometric responses.|||||Grey to green or brown, abundantly porphyritic biotite microgranite to fine-grained leucogranite.|30-JUN-15
6400|Eva Creek Microgranite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Grey to green or brown abundantly porphyritic biotite microgranite to fine-grained leucogranite.|
6400|Eva Creek Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Newcastle Range Volcanic Group.|||||I-type: biotite microgranite and granite.|
6414|Everetts Creek Volcanics|23032|4|Described|p16,17||Late Ordovician|||||||
6414|Everetts Creek Volcanics|23423|6|Mentioned|p263|||Broken River Province.||||||
6414|Everetts Creek Volcanics|23424|4|Described|Table 8.1 Fig 8.2/8.3 p331.||Ordovician|Age: Ordovician; relationship to Carriers Well Fm. Possibly underlying or faulted against Carriers Well Formation. Camel Creek Subprovince.||||||
6414|Everetts Creek Volcanics|23430|5|Briefly described|p476, 478|||Broken River Province.||||||
6414|Everetts Creek Volcanics|23431|5|Briefly described|p541|||||||||
6414|Everetts Creek Volcanics|23619|5|Briefly described|p19|||Camel Creek Subprovince.||||||
6414|Everetts Creek Volcanics|24577|4|Described|p754 Fig. 2|Ordovician|Ordovician|Overlain by the Carriers Well Formation. Overlies the Wairuna Formation. Geological Province: Broken River Region, Lachlan Fold Belt. See also Everett's Creek Volcanics.||||||
6414|Everetts Creek Volcanics|31999|6|Mentioned|p157|||||||||
6414|Everetts Creek Volcanics|37727|6|Mentioned|p21|||||||||
6414|Everetts Creek Volcanics|37768|5|Briefly described|p40|||||||||
6414|Everetts Creek Volcanics|40136|5|Briefly described|p20|||See also p24||||||08-MAY-15
6414|Everetts Creek Volcanics|40746|6|Mentioned|p360|||||||||
6414|Everetts Creek Volcanics|40961|3|Fully described|p243|||||||||
6414|Everetts Creek Volcanics|41260|4|Described|p12|||See also p144||||||08-MAY-15
6414|Everetts Creek Volcanics|41675|6|Mentioned|p52|||||||||
6414|Everetts Creek Volcanics|41679|6|Mentioned|Fig.1|||||||||
6414|Everetts Creek Volcanics|41719|6|Mentioned|Fig.1|||||||||
6414|Everetts Creek Volcanics|41739|6|Mentioned|Fig.1|||||||||
6414|Everetts Creek Volcanics|42279|5|Briefly described|p27|||||||||
6414|Everetts Creek Volcanics|42692|5|Briefly described|map legend|Ordovician||||||||
6414|Everetts Creek Volcanics|42693|5|Briefly described|map legend|Ordovician||||||||
6414|Everetts Creek Volcanics|42752|5|Briefly described|p45|||see also Fig.2 p46, Fig.3 p47.||||||08-MAY-15
6414|Everetts Creek Volcanics|42933|3|Fully described|p19|||||||||
6414|Everetts Creek Volcanics|43083|6|Mentioned|p39|||Geological province: Broken River Province.||||||17-JUN-09
6414|Everetts Creek Volcanics|43113|6|Mentioned|p32|||||||||
6414|Everetts Creek Volcanics|43213|5|Briefly described|p65-66|||Precise age is unknown.||||Is overlain by Carriers Well Formation.|A sequence of basaltic (both calc-alkaline and MORB affinities) to rhyolitic lavas and volcaniclastics.|
6414|Everetts Creek Volcanics|43259|4|Described|Appendix 1,p1.||Ordovician|||||||
6414|Everetts Creek Volcanics|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|Overlain by and grades into Carriers Well Formation.||||||
6414|Everetts Creek Volcanics|44515|14|Not recorded|p32|||||||||
6414|Everetts Creek Volcanics|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Broken River Province/Camel Creek Subprovince.||||||
6414|Everetts Creek Volcanics|65756|5|Briefly described|p26|Late Ordovician|Late Ordovician|Camel Creek Subprovince. Part of island arc sequence.||||||
6414|Everetts Creek Volcanics|67455|5|Briefly described|p593.|Late Ordovician|Late Ordovician|Western margin of Camel Creek Subprovince. Accreted in Early Silurian contractional deformation.|||||Subduction-related, calc-alkaline island arc volcanics.|
6414|Everetts Creek Volcanics|67848|5|Briefly described|p1, p2, pp4-6, pp8-15.|Late Ordovician|Late Ordovician|Western edge of Camel Creek Subprovince. Part of an arc assemblage in collisional accretion. Melange development is characteristic. Geochemistry, and web address for geochemical data, are given.||||Has a transitional contact with Carriers Well Formation.|Massive, mafic to intermediate, aphyric and feldspar-phyric, volcanic and hypabyssal rocks; intrusives and pillowed; minor volcanic breccia, sandstone, chert.|
6414|Everetts Creek Volcanics|68336|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician|Camel Creek Subprovince, Broken River Province.|||||Andesitic and basaltic lava (locally pillowed) and volcanic breccia.|
6414|Everetts Creek Volcanics|68339|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician|Camel Creek Subprovince.|||||Andesitic and basaltic lava (locally pillowed) and volcanic breccia.|
6414|Everetts Creek Volcanics|68340|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician|Camel Creek Subprovince.|||||Andesitic and basaltic lava (locally pillowed) and volcanic breccia.|
6414|Everetts Creek Volcanics|68341|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician|Camel Creek Subprovince, Broken River Province.|||||Andesitic and basaltic lava (locally pillowed) and volcanic breccia.|
6414|Everetts Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Silurian|Ordovician|Broken River Province. This unit, as well as Pelican Range, Wairuna and Carriers Well Formations and Tribute Hills Arenite, are all mapped under the symbol, OSb.||||||
6414|Everetts Creek Volcanics|68576|5|Briefly described|Q_11: p34-35, p38|||W margin of the Camel Creek Subprovince, S of Greenvale. Henderson et al. (2011) suggest that this unit was part of a Late Ordovician island arc that may have been accreted in the Early Silurian.|||||Calc-alkaline volcanic rocks. Includes aphyric, green to purple, spilitised basalt, with pillows and calcite-filled amygdales locally; minor feldspar-phyric basalt or andesite, and cobble to boulder-sized fragmental mafic rocks.|
6414|Everetts Creek Volcanics|68731|6|Mentioned|p221|||||||||
6414|Everetts Creek Volcanics|68822|5|Briefly described|p335, p336 Fig.11|Upper Ordovician|Upper Ordovician||||||Calcalkaline and tholeiitic basaltic to dacitic volcanics.|
6414|Everetts Creek Volcanics|69030|6|Mentioned|p6|Ordovician|Ordovician|Camel Creek Subprovince (Broken River Province).||||||
6414|Everetts Creek Volcanics|69079|6|Mentioned|p5|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.||||||
6414|Everetts Creek Volcanics|69592|5|Briefly described|p251 Fig.4.35, p252, p255-257|Late Ordovician|Late Ordovician|Western edge of Camel Creek Subprovince, Broken River Province. Part of the Lucky Springs Assemblage. Includes a fault-bounded area of volcanic rocks previously mapped as Wairuna Formation (Henderson et al., 2011). Seen as a facies variant of Carriers Well Formation. Geochemical plots and discussion. Island arc deposits close to a continental margin.||||Is overlain gradationally by Carriers Well Formation.|Largely massive, basaltic to andesitic, aphyric and feldspar-phyric, volcanic and hypabyssal rocks. Minor sedimentary beds of volcanic breccia, sandstone and chert. Amygdaloidal or vesicular fabrics, veins of epidote, quartz and calcite, are common.|
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.|
6432|Ewen Granite|22747|6|Mentioned|p8||Statherian|Age: 1770 Ma.||||||18-SEP-06
6432|Ewen Granite|23518|5|Briefly described|p9 Fig.3|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province.||||||
6432|Ewen Granite|24197|5|Briefly described|p21, p93|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Geological province: Mount Isa Inlier. See also p94 Tb. 12.1 (Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
6432|Ewen Granite|29969|6|Mentioned|p394|||||||||
6432|Ewen Granite|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|30534|6|Mentioned|p302|||See also P305||||||
6432|Ewen Granite|30536|6|Mentioned|p102|||||||||
6432|Ewen Granite|30723|6|Mentioned|p341|||Geological map||||||
6432|Ewen Granite|30725|5|Briefly described|p574|||||||||
6432|Ewen Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|31821|6|Mentioned|p1024|||||||||
6432|Ewen Granite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6432|Ewen Granite|32660|5|Briefly described|Table 5|||||||||
6432|Ewen Granite|32951|5|Briefly described|p1276|||||||||
6432|Ewen Granite|32959|6|Mentioned|Fig.21|||||||||
6432|Ewen Granite|33214|5|Briefly described|p1279|||||||||
6432|Ewen Granite|33897|6|Mentioned|p1280|||||||||
6432|Ewen Granite|33900|4|Described|p8|||Mention p7.||||||18-SEP-06
6432|Ewen Granite|35074|6|Mentioned|Fig.2|||||||||
6432|Ewen Granite|35295|6|Mentioned|p603|||||||||
6432|Ewen Granite|37462|5|Briefly described|Table4.VII|||||||||
6432|Ewen Granite|37568|6|Mentioned|p85|||||||||
6432|Ewen Granite|38232|6|Mentioned|p82|||||||||
6432|Ewen Granite|38276|6|Mentioned|Fig.1|||||||||
6432|Ewen Granite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6432|Ewen Granite|38560|6|Mentioned|p113|||||||||
6432|Ewen Granite|38833|6|Mentioned|p161|||||||||
6432|Ewen Granite|39202|6|Mentioned|p234|||||||||
6432|Ewen Granite|39445|5|Briefly described|Table 2|||See also p35 and p39.||||||18-SEP-06
6432|Ewen Granite|39556|5|Briefly described|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
6432|Ewen Granite|39798|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|39934|6|Mentioned|Fig.3|||||||||
6432|Ewen Granite|40648|6|Mentioned|p6|||||||||
6432|Ewen Granite|40840|6|Mentioned|Map legend|||||||||
6432|Ewen Granite|41307|4|Described|p20|||||||||
6432|Ewen Granite|41465|5|Briefly described|p7|||||||||
6432|Ewen Granite|41961|6|Mentioned|Table 1 P39|||||||||
6432|Ewen Granite|41979|6|Mentioned|Table 1 P510|||||||||
6432|Ewen Granite|42754|6|Mentioned|p3|||||||||
6432|Ewen Granite|44068|14|Not recorded|p4|||||||||
6432|Ewen Granite|44091|14|Not recorded|p10||Paleoproterozoic|||||||07-NOV-08
6432|Ewen Granite|44210|14|Not recorded|p8|||||||||
6432|Ewen Granite|44257|14|Not recorded|p19,21,22|||1760-1800 Ma. Rb-Sr.||||||
6432|Ewen Granite|44271|14|Not recorded|p37,38,45|||Intrudes Argylla Formation. Overlain by Eastern Creek Volcanics.||||||
6432|Ewen Granite|44275|14|Not recorded|Map Legend|||||||||
6432|Ewen Granite|44276|14|Not recorded|p17|||||||||
6432|Ewen Granite|44279|14|Not recorded|p5,map|||||||||
6432|Ewen Granite|44749|14|Not recorded|p25,26|||||||||
6432|Ewen Granite|44751|14|Not recorded|p300||Precambrian|||||||
6432|Ewen Granite|44765|14|Not recorded|p15||Paleoproterozoic|||||||07-NOV-08
6432|Ewen Granite|44766|14|Not recorded|p23,25|||Age: 1760Ma. Suggests equivalent to older phase of Kalkadoon Granite.||||||
6432|Ewen Granite|44849|14|Not recorded|p69,74-5,87|||1780 Ma = approx age of Sybella Granite.||||||18-JUL-13
6432|Ewen Granite|44918|14|Not recorded|p75,77,88|||Emplaced in Argylla Formation at 1780+/- 20 Ma. (see NT author card)||||||18-JUL-13
6432|Ewen Granite|44989|2|Defined|p145-7|||Tb.IV. On many pages. Intrudes Argylla Formation. Underlies Eastern Creek Volcanics. (E54-14).||||||18-SEP-06
6432|Ewen Granite|45052|6|Mentioned|p73|||Rb/Sr age.||||||
6432|Ewen Granite|45087|5|Briefly described|p21|||Chemical analyses.||||||
6432|Ewen Granite|45166|6|Mentioned|p13|||||||||
6432|Ewen Granite|45287|14|Not recorded|p.227,228|||Related to Argylla Formation?||||||
6432|Ewen Granite|46801|6|Mentioned|p117|||See also Fig. 14||||||
6432|Ewen Granite|46919|6|Mentioned|p221|||||||||
6432|Ewen Granite|46962|4|Described|Fig.3|||||||||
6432|Ewen Granite|48906|14|Not recorded|p4|||||||||
6432|Ewen Granite|49041|5|Briefly described|Table 2|||||||||
6432|Ewen Granite|50100|5|Briefly described|p13 Fig.4|Orosirian|Orosirian|Geological Province: Western Fold Belt Province.||||||
6432|Ewen Granite|50536|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite. Age: ~1820Ma (U-Pb).||||||07-NOV-08
6432|Ewen Granite|63866|5|Briefly described|p60|Orosirian|Orosirian|Kalkadoon-Leichhardt Belt.|c. 1820 Ma (Wyborn and Page, 1983)|||||
6432|Ewen Granite|65505|6|Mentioned|969, 978, 981, Fig1,4|Proterozoic|Proterozoic|Kalkadoon-Leichhardt Block basement. Age: 1856 +/-3 Ma (zircon).||||||
6432|Ewen Granite|66529|6|Mentioned|p67, p94|Paleoproterozoic|Paleoproterozoic|High potential along its eastern margin for magmatic-hydrothermal U mineralisation.||Unit in Kalkadoon Supersuite.||||
6432|Ewen Granite|67323|4|Described|GIS attrib tbl, Solid Geology Map, p14|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block. Age:1840 +/-20 Ma (Wyborn & Page 1983), 1859+/-3.3 Ma (Magee et al, in prep) from close to boundary with Eastern Creek Volcanics. May be two plutons of distinctly different age.|1856 +/- 3.3 Ma.|Kalkadoon Suite or Supersuite||Intrudes Leichhardt Volcanics. Boundary with Eastern Creek Volcanics appears to be intrusive.|Medium pink leucogranite, pink to grey coarse porphyritic granite and granodiorite microgranite, pegmatite, schist, mylonite; some phases possibly coeval with Kalkadoon Granite.|
6432|Ewen Granite|67539|5|Briefly described|p2, p3, p3 Fig.2, p4 Fig.3|||Boundary relationships reviewed. May be two distinct phases and ages. Description of outcrops has been modified significantly to include more metabasalt enclaves and less dolerite dykes. Outcrop is commonly as much as  ~ 15% enclaves of metabasalt. ||||Intrudes Myally Subgroup, parts of the Eastern Creek Volcanics, but in other places unconformably overlain by Dynamite Creek Member, Eastern Creek Volcanics.||
6432|Ewen Granite|68146|6|Mentioned|p193|||Age determinations by several authors (listed) are similar to the age determined in this study for the Kalkadoon Granodiorite and Plum Mountain Gneiss.||||||
6432|Ewen Granite|68575|5|Briefly described|p1, p6-7, p112-117, p124, p134|||Kalkadoon-Leichhardt Domain, Mount Isa Province. Whole rock Sm-Nd isotopic data and age (1859 Ma).|1859 +/- 3 Ma.||||Altered, coarse-grained granite characterised by euhedral plagioclase (typically replaced by fine-grained sericite) and interstitial microcline.|
6432|Ewen Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province. Also dated as 1840 +/- 20 Ma (Wyborn and Page, 1983).|1859 +/- 3.3 Ma (Magee et al. in press).|Kalkadoon Suite.|||Medium pink leucogranite, pink to grey coarse porphyritic granite and granodiorite, microgranite, pegmatite, schist, mylonite; some phases possibly coeval with Kalkadoon Granodiorite.|
6432|Ewen Granite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink medium-grained leucogranite, pink to grey coarse-grained porphyritic granite and granodiorite, microgranite, pegmatite, schist and mylonite. Coarse-grained granodiorite and tonalite (mapped separately).|
6432|Ewen Granite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink medium-grained leucogranite, pink to grey coarse-grained porphyritic granite and granodiorite, microgranite, pegmatite, schist and mylonite. Coarse-grained granodiorite and tonalite (mapped separately).|
6432|Ewen Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1859+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
6432|Ewen Granite|72889|5|Briefly described|p1, p3, p7, p9-12, p17-18.|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain. Magmatic crystallisation age of main phase  well established by zircon U-Pb SHRIMP dating. This Record reports magmatic crystallisation age of a quartz-poor phase that might be a younger intrusion, but the age obtained,1853.5+/-3.6 Ma, is within uncertainty of the main phases. The coarse grained granodiorite has a U-Pb age of 1855.9 +/- 2.4 Ma (Neumann et al., 2009). Refer to 1:250 000 sheet DOBBYN (SE5414). Located in Mount Isa Orogen. Part of the Ewen Batholith, a 72km x 15km body of granite rocks. Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results.|1859 +/- 3 Ma. (Magee et al., 2012)|Kalkadoon Suite||Coeval with Kalkadoon Granodiorite.|Includes medium-grained, leucogranite, coarse porphyritic granite and granodiorite phases and smaller outcrops of coarse-grained granodiorite and tonalite phases.|25-NOV-20
6432|Ewen Granite|72919|6|Mentioned|p7|Orosirian|Orosirian|Mount Isa Province. Ages of 1856 +/- 3 Ma and 1859 +/- 3 Ma were reported by Neumann et al. (2009) and Magee et al. (2012), respectively.|1856 +/- 3 Ma, 1859 +/- 3 Ma|||||
6432|Ewen Granite|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Orosirian|Orosirian|Leichhardt River and Kalkadoon-Leichhardt Domains.|1856+/-3 Ma crystallisation age||||Felsic intrusive.|
6432|Ewen Granite|73553|6|Mentioned|p6|||Kalkadoon-Leichhardt Domain.||Kalkadoon Suite||||
6440|Exevale Formation|23052|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
6440|Exevale Formation|23161|4|Described|p5,7,34 table1|Tertiary|Tertiary|||||||
6440|Exevale Formation|23422|6|Mentioned|p187|||||||||
6440|Exevale Formation|23430|5|Briefly described|p504 Table 14.5|||||||||
6440|Exevale Formation|32553|4|Described|p38|||||||||
6440|Exevale Formation|33353|6|Mentioned|p457|||||||||
6440|Exevale Formation|34314|5|Briefly described|table 3|||See also PP10,14. Tertiary||||||
6440|Exevale Formation|37073|6|Mentioned|p99|||||||||
6440|Exevale Formation|37607|6|Mentioned|Fig.7|||||||||
6440|Exevale Formation|39445|5|Briefly described|Table 14|||||||||
6440|Exevale Formation|42701|4|Described|p74|||||||||
6440|Exevale Formation|43988|14|Not recorded|Map Legend||Tertiary|||||||
6440|Exevale Formation|44001|14|Not recorded|Map Legend||Tertiary|||||||
6440|Exevale Formation|44245|5|Briefly described|Map Legend||Tertiary|||||||
6440|Exevale Formation|45145|6|Mentioned|Table 7|||||||||
6440|Exevale Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6440|Exevale Formation|48841|2|Defined|p34-37,41,48,Tb.I||Tertiary|Fresh water lake deposit. Overlain by basalt flows. Similar to Emerald Formation.||||||
6440|Exevale Formation|48843|14|Not recorded|p.47|||(Not defined).||||||
6440|Exevale Formation|48915|6|Mentioned|Table 1|||Tertiary||||||
6440|Exevale Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Fitzroy region.||||||03-MAR-10
6440|Exevale Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Floraville, Glendower, 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.||||||
6440|Exevale Formation|69599|5|Briefly described|p580, p585, p593|Oligocene|Eocene|Malone et al. (1969). Remapping by Hutton et al. (1991) restricted Malone et al. (1969)'s distribution. Crops out in the east of MOUNT COOLON 250k sheet area. Up to 120m thick. Fluvial to lacustrine sediments. Locally faulted and weakly folded. Silcrete and ferricrete development (Featherby Surface) occurred in late Eocene-Oligocene.||||Correlated with Biloela beds; Southern Cross, Emerald, Suttor and Duarings Formations.|Fine-grained quartz sandstone, mudstone, medium- to coarse-grained sandstone and conglomerate. Sandstones are thin-bedded to massive and rarely cross-bedded. Silicified and overlain by (Oligocene) basalt flows.|
6440|Exevale Formation|73037|5|Briefly described|Map legend|Eocene|Paleocene||||||Fluviatile sediments.|
6440|Exevale Formation|75060|6|Mentioned|p41|||NW Bowen Basin.|||||Overlain by weathered  basalt flows.|
6442|Exley Microgranite|22847|3|Fully described|p 40|||||||||
6442|Exley Microgranite|23422|5|Briefly described|p173, p210 Table 6.6|||Of Brittany Supersuite.  Probably Ordovician.||||||
6442|Exley Microgranite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 106.  Assumed to be I-Type.||||||
6442|Exley Microgranite|42245|2|Defined|p32|Ordovician||Reserved as Exley Microadamellite||||||
6442|Exley Microgranite|42633|6|Mentioned|Table 1 P8|||||||||
6442|Exley Microgranite|43093|4|Described|Appendix 1||Ordovician|||||||
6442|Exley Microgranite|43259|4|Described|Appendix 1,p23.||Ordovician|||||||
6442|Exley Microgranite|43933|5|Briefly described|Map Legend||Ordovician|||||||
6442|Exley Microgranite|43935|5|Briefly described|Map Legend||Ordovician|||||||
6447|Expedition Sandstone|23161|6|Mentioned|p33|||||||||
6447|Expedition Sandstone|23430|5|Briefly described|p515|||Of Clematis Group||||||
6447|Expedition Sandstone|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Of the Clematis Group.  Age: 241-235Ma.  Geological Province: Bowen Basin.||||||
6447|Expedition Sandstone|35467|6|Mentioned|p180|||||||||
6447|Expedition Sandstone|37612|6|Mentioned|Fig.3|||||||||
6447|Expedition Sandstone|37804|6|Mentioned|p63|||||||||
6447|Expedition Sandstone|38518|6|Mentioned|Fig.3|||||||||
6447|Expedition Sandstone|39212|4|Described|p15|||See also P24||||||
6447|Expedition Sandstone|39445|5|Briefly described|Table 9|||||||||
6447|Expedition Sandstone|39491|4|Described|p18|||||||||
6447|Expedition Sandstone|39943|6|Mentioned|Table 6A|||||||||
6447|Expedition Sandstone|40120|6|Mentioned|p424|||||||||
6447|Expedition Sandstone|41191|6|Mentioned|Fig.3|||||||||
6447|Expedition Sandstone|42911|5|Briefly described|p11|||of Clematis Group||||||
6447|Expedition Sandstone|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
6447|Expedition Sandstone|43185|6|Mentioned|11||Triassic|||||||
6447|Expedition Sandstone|43714|6|Mentioned|p33|||||||||
6447|Expedition Sandstone|45095|2|Defined|p29|Triassic|Triassic|||||||
6447|Expedition Sandstone|64856|3|Fully described|p71-75, p102|Middle Triassic|Early Triassic|Jensen (1975). Of Clematis Group in Taroom Trough, Bowen Basin. Medium to very coarse grained sandstone, conglomeratic in part, interbedded with lesser fine grained sandstone, siltstone, mudstone. Overlies Glenidal Formation. Contains palynofloras of APT2 and lower APT3 age (251-230 Ma).| | ||||28-NOV-17
6447|Expedition Sandstone|64857|5|Briefly described|p126-127|Triassic|Triassic|Correlative of the Showgrounds Sandstone. Contained in the Clematis Group. Quartzose sandstones with sublabile sandstones, siltstones and mudstones.||||||
6447|Expedition Sandstone|65115|5|Briefly described|p426, 427, Fig 14 p406|Middle Triassic|Middle Triassic|braided fluvial. Of the Clematis Group, Denison Trough. Overlies the Glenidal Formation. Part of Supersequence I.||||||
6447|Expedition Sandstone|68576|5|Briefly described|Q_4: p7, p16-17, p21, p24|Middle Triassic|Middle Triassic|Bowen Basin. Braided stream deposits.||Clematis Group.||Overlies Glenidal Formation.|Pale grey to white, medium- to very coarse-grained, quartzose to sub-labile sandstone with conglomerate, interbedded with lesser fine-grained sandstone, siltstone and mudstone. Pebble bands and cross-bedding are diagnostic for this unit.|
6447|Expedition Sandstone|68679|5|Briefly described|p377, p383|||Jensen (1975). Bowen Basin. 250m thick. Braided fluvial deposits.||||Laterally equivalent to Showgrounds Sandstone.|Medium- to coarse-grained, sublabile to quartzose sandstone, pebbly in part; siltstone and mudstone in lower part.|
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.|
6469|Fair Hill Formation|13516|6|Mentioned|p145 fig 3, p146 fig 4|Late Permian|Late Permian|From Comet Ridge, Bowen Basin. Age: APP5004 - APP5005||||||
6469|Fair Hill Formation|22601|5|Briefly described|418|Permian|Permian|Geol province Bowen Basin||||||
6469|Fair Hill Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
6469|Fair Hill Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
6469|Fair Hill Formation|29409|6|Mentioned|Table 1|||Correlation||||||
6469|Fair Hill Formation|29412|6|Mentioned|p209|||See Table.||||||
6469|Fair Hill Formation|30088|6|Mentioned|p22|||||||||
6469|Fair Hill Formation|30850|6|Mentioned|p343|||||||||
6469|Fair Hill Formation|30852|6|Mentioned|Fig.2|||||||||
6469|Fair Hill Formation|30915|6|Mentioned|p92|||To be redefined as Moranbah Coal Measures in North Central Bowen Basin||||||
6469|Fair Hill Formation|31079|6|Mentioned|p5|||||||||
6469|Fair Hill Formation|31401|6|Mentioned|p30|||||||||
6469|Fair Hill Formation|31649|6|Mentioned|p57|||||||||
6469|Fair Hill Formation|31656|4|Described|Table 1|||U.Permian||||||
6469|Fair Hill Formation|31687|6|Mentioned|p285|||Correlation N.Bowen Basin||||||
6469|Fair Hill Formation|31689|6|Mentioned|p245|||Economic coal seams||||||
6469|Fair Hill Formation|31690|6|Mentioned|p36|||||||||
6469|Fair Hill Formation|31691|4|Described|p427|||U.Permian. Basal unit of Blackwater Gp.||||||
6469|Fair Hill Formation|32177|6|Mentioned|p146|||||||||
6469|Fair Hill Formation|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6469|Fair Hill Formation|32689|1|Redefined|p433|Permian|Permian|||||||
6469|Fair Hill Formation|32729|6|Mentioned|p36|||See also P37. Coal seams in drill holes||||||
6469|Fair Hill Formation|32730|6|Mentioned|p47|||||||||
6469|Fair Hill Formation|32834|6|Mentioned|p26|||||||||
6469|Fair Hill Formation|33202|6|Mentioned|Table 2|||||||||
6469|Fair Hill Formation|33250|5|Briefly described|p140|||||||||
6469|Fair Hill Formation|33390|5|Briefly described|p5|||||||||
6469|Fair Hill Formation|33981|6|Mentioned|Fig.2|||||||||
6469|Fair Hill Formation|34276|6|Mentioned|p42|||Permian||||||
6469|Fair Hill Formation|34390|4|Described|Table 2|||Permian||||||
6469|Fair Hill Formation|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6469|Fair Hill Formation|35433|5|Briefly described|p27|||||||||
6469|Fair Hill Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
6469|Fair Hill Formation|35822|6|Mentioned|Fig.3|||||||||
6469|Fair Hill Formation|36739|6|Mentioned|p24|||||||||
6469|Fair Hill Formation|37065|6|Mentioned|p32|||||||||
6469|Fair Hill Formation|37069|6|Mentioned|p66|||||||||
6469|Fair Hill Formation|37070|6|Mentioned|p73|||||||||
6469|Fair Hill Formation|37072|5|Briefly described|p92|||||||||
6469|Fair Hill Formation|37073|3|Fully described|p99|||||||||
6469|Fair Hill Formation|37076|4|Described|p120|||||||||
6469|Fair Hill Formation|37138|6|Mentioned|p92|||||||||
6469|Fair Hill Formation|37612|6|Mentioned|Fig.3|||See also P284||||||
6469|Fair Hill Formation|37726|3|Fully described|p150|||||||||
6469|Fair Hill Formation|38518|6|Mentioned|Fig.3|||||||||
6469|Fair Hill Formation|38958|5|Briefly described|p493|||||||||
6469|Fair Hill Formation|39212|5|Briefly described|p12|||||||||
6469|Fair Hill Formation|39218|6|Mentioned|p48|||||||||
6469|Fair Hill Formation|39261|6|Mentioned|Fig.6|||||||||
6469|Fair Hill Formation|39273|6|Mentioned|Fig. 2|||||||||
6469|Fair Hill Formation|39445|5|Briefly described|Table 8|||See also Table 9||||||
6469|Fair Hill Formation|39943|6|Mentioned|Table 5A|||||||||
6469|Fair Hill Formation|40321|6|Mentioned|Fig.3|||||||||
6469|Fair Hill Formation|40675|6|Mentioned|Table 5A|||||||||
6469|Fair Hill Formation|41191|6|Mentioned|Fig.3|||||||||
6469|Fair Hill Formation|41246|6|Mentioned|Map legend|Permian||||||||
6469|Fair Hill Formation|42091|6|Mentioned|Text fig.2 P284|||||||||
6469|Fair Hill Formation|42249|6|Mentioned|Table 1 P22|||||||||
6469|Fair Hill Formation|42250|6|Mentioned|Fig.4 P31|||||||||
6469|Fair Hill Formation|42254|6|Mentioned|Fig.2 P223|||||||||
6469|Fair Hill Formation|42614|5|Briefly described|p13|||Bowen Basin, Blackwater Group.||||||
6469|Fair Hill Formation|42641|6|Mentioned|p112|||||||||
6469|Fair Hill Formation|42648|5|Briefly described|p40|||||||||
6469|Fair Hill Formation|42856|6|Mentioned|Fig.11 P646|||||||||
6469|Fair Hill Formation|43580|6|Mentioned|Fig.1,p360|||||||||
6469|Fair Hill Formation|43994|14|Not recorded|Map Legend||Late Permian|Part of Blackwater Group.||||||
6469|Fair Hill Formation|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
6469|Fair Hill Formation|45071|3|Fully described|Table 12|||||||||
6469|Fair Hill Formation|45095|3|Fully described|p8|||||||||
6469|Fair Hill Formation|48898|2|Defined|p50|Late Permian|Late Permian|See also pp38,43 etc||||||20-JUN-19
6469|Fair Hill Formation|48947|5|Briefly described|p8|||||||||
6469|Fair Hill Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
6469|Fair Hill Formation|64665|6|Mentioned|p52.|Permian|Permian|Bowen Basin.||||||
6469|Fair Hill Formation|65388|6|Mentioned|p198|||Rocks previously included in lower part of Fair Hill Formation, now assigned to Moranbah Coal Measures.||||||
6469|Fair Hill Formation|67402|6|Mentioned|p21, p45, p85 tbl BWN2|Capitanian|Capitanian|Bowen Basin. ||||Overlies the German Creek Formation. Overlain by the Rangal Coal Measures.||
6469|Fair Hill Formation|68679|5|Briefly described|p377, p381-382, p384|Permian|Permian|Prouza and Park (1973). Bowen Basin. 140m thick. Delta plain, alluvial plain deposits. Appears as Fairhill Formation on p381. Properties of the coal are described in some detail.||||Overlies Macmillan Formation. Is overlain by Burngrove Formation. Laterally equivalent to the upper Peawaddy Formation.|Labile and sublabile sandstone, siltstone, mudstone, carbonaceous mudstone, coal, tuff.|
6469|Fair Hill Formation|70861|4|Described|p36-40, 41,42-45|Late Permian|Late Permian|Of Bowen Basin. Aggradational package with increasing faunal bioturbation upward. Contains more frequent, but thinner tuffaceous layers than Burngrove Formation. Sedimentary and coal analysis from Foxleigh 4 well. Comprises alternating sequence of mire and channel sandstone facies; represents channel abandonment and reoccupation in a proximal fluvial environment. As base sea-level rises, channels avulse, become distal distributaries, and eventually flooded by a marine trangression. Does not contains bright coals due to high mineral matter but are vitrinite-rich; accumulated peat was preserved and buried rapidly due to high sediment input and volcanic ash fall.||Unit of Fort Cooper Coal Measures.|Includes Fair Hill, Lepus, Canis, Hercules, Pegasus/Phoenix seams.|Lowermost unit of Fort Cooper Coal Measures. Overlain by Black Alley Shale or Middle Main Seams.|Thick, amalgamated channel sandstones separated by finger-grained heterolithic sequences and coals.|29-AUG-19
6469|Fair Hill Formation|70940|5|Briefly described|p843-845, p848, p850-853, p855|Permian|Permian|Northern Taroom Trough, central Bowen Basin. Decompacted thickness of 415m deposited in 0.46 Ma. Contains a tuff bed.||Blackwater Group.||Overlies MacMillan Formation. Is overlain by Burngrove Formation.||
6469|Fair Hill Formation|71265|5|Briefly described|p589-590, p592, p598-601, p603-607|Changhsingian|Changhsingian|Eastern Galilee Basin. Identified as a separate unit by Phillips et al. (2017). References to "Fair Hill Formations equivalent". Facies discussed. Sedimentary logs of CRD Montani 1 and OEC Glue Pot Creek 1.||||Overlies Colinlea Sandstone. Is overlain by and lateral equivalent of Black Alley Shale. With Burngrove Formation, is equivalent to Fort Cooper Coal Measures.|Includes highly tuffaceous coals.|
6469|Fair Hill Formation|71276|5|Briefly described|p295-297|Lopingian|Lopingian|Prouza and Park (1973). Bowen Basin. The authors appear to assign the Fair Hill Formation to the basal section of Fort Cooper Coal Measures [?].||||Is overlain by Black Alley Shale. Correlates with the upper part of the Peawaddy Formation.|Highly tuffaceous and coal-bearing.|
6469|Fair Hill Formation|71701|4|Described|p153, p155-p156, p167-p171|Lopingian|Lopingian|Eastern Area; Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin.  An equivalent Lopingian tuff is the source of the dates provided.|254.32 +/- 0.10 Ma (CA-IDTIMS)|||Overlies the Colinlea Sandstone, MacMillan Formation. Overlain by the Black Alley Shale, Burngrove Fm. Part equivalent to the Betts Creek Group of NE Galilee Basin.||29-AUG-19
6469|Fair Hill Formation|71710|6|Mentioned|p367|||Bowen Basin. Dates of Betts Creek beds equivalents correlated with radiometric ages of this formation.||||||22-MAY-19
6469|Fair Hill Formation|72297|5|Briefly described|p694, p695 Fig.10.9|Permian|Permian|Bowen Basin. The coal in this unit is less economic due to high ash (tuff).|||Lepus, Canis, Hercules Seams.|Overlies Macmillan Formation. Is overlain by Burngrove Formation. Correlated with Black Alley Shale and Kaloola Member.|Contains coal seams and tuffs.|
6469|Fair Hill Formation|73246|6|Mentioned|p190-191|Upper Permian|Upper Permian|Bowen Basin, central.||Blackwater Group||Underlain by Blenheim Subgroup (Back Creek Group). Overlain by Burngrove Formation. Equivalent to Fort Cooper Coal and Moranbah coal measures.||
6469|Fair Hill Formation|73305|4|Described|p547-548, p550-553, p554-555, p561|Late Permian|Late Permian|Northern Bowen Basin. Represents a regressive succession. Merged coal seams on the Collinsville Shelf split and thin to the NE and SE at morphotectonic zone boundaries.  Thickness varies from 35.1 to 268.7 m, increases with seam splitting and increased interburden in trough areas, greatest thickness is in the northern Taroom Trough. Named coal seams include the Fair Hill Seam, Upper Fair Hill Seam, Lower Fair Hill Seam, FH1, FH2, Scorpio, Pegasus, Phoenix, Hercules, Canis, Lepus seams and the Fair Hill seams. See also p550 Fig.3, p555 Fig.7, p556 Tb.3.||Fort Cooper Coal Measures|Fair Hill Seam|Overlies the MacMillan Formation. Equivalent to the Tinowon Formation, Gyranda Formation and upper part of the Peawaddy Formation. Underlies the Middle Main Seams, Burngrove Formation.|Comprises coal seams interbedded with tuffs and coarse-grained sediments.|12-FEB-23
6500|Fairview Gravel|23426|4|Described|p403 + Table 10.4 p407 7   7.|||Probably equivalent to Bulimba Formation of the Karumba Basin. Underlying Unit: Rolling Downs Group - unconformable contact. Geological Province Kalpowar Basin.||||||
6500|Fairview Gravel|23430|5|Briefly described|p527|||Kalpowar Basin Province.||||||
6500|Fairview Gravel|23511|5|Briefly described|Map Legend||Tertiary|||||||
6500|Fairview Gravel|32705|5|Briefly described|p185|||||||||
6500|Fairview Gravel|36228|6|Mentioned|Map legend|Eocene|Eocene|||||||
6500|Fairview Gravel|37605|5|Briefly described|p387|||||||||
6500|Fairview Gravel|37607|6|Mentioned|Fig.6|||||||||
6500|Fairview Gravel|39445|5|Briefly described|Table 14|||||||||
6500|Fairview Gravel|42637|6|Mentioned|p29|||||||||
6500|Fairview Gravel|44294|14|Not recorded|p15,17,26|||||||||
6500|Fairview Gravel|45025|6|Mentioned|p100|||Disconformably overlies Wolena Claystone.||||||
6500|Fairview Gravel|45145|5|Briefly described|p33|||||||||
6500|Fairview Gravel|60358|5|Briefly described|Map Legend|Early Oligocene|Early Eocene|Clayey quartz gravel and sand, muddy sand. Geological Province: Kalpower Basin.||||||18-AUG-04
6500|Fairview Gravel|61155|5|Briefly described|p20|Middle Eocene|Late Paleocene|Thickness: 6m. In eastern Cape York.||||||03-MAR-10
6500|Fairview Gravel|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
6500|Fairview Gravel|69599|5|Briefly described|p585, p605, p616, p650|Eocene|Paleocene|Grimes (1980). Kalpowar Basin, Carpentaria region. Poorly exposed near Kalpowar Station. 30-40m thick in drill holes. Fluvial deposits. Age unknown. Capped by laterite and silcrete of the Aurukun Surface.||||Correlated with Floraville, Louisa and Bulimba Formations.|Conglomerate and clay-cemented sandstone.|
6509|Falloch beds|23420|6|Mentioned|p 131|||||||||
6509|Falloch beds|42637|6|Mentioned|p31|||Variation on Falloch Beds.||||||
6509|Falloch beds|42640|5|Briefly described|p12|||Variation on Falloch Beds.||||||
6509|Falloch beds|42650|4|Described|p18|||Belong to the Wyaaba Cycle||||||
6509|Falloch beds|49769|6|Mentioned|p4|||||||||
6509|Falloch beds|61155|5|Briefly described|p16|?Late Miocene|?Middle Miocene|Together with Wyaaba beds overlie Carl Creek and Gregory Downs Limestones. Together with Wyaaba beds thickness is 140m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
6509|Falloch beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as the Lilyvale, Wyaaba and Yam Creek beds, are all mapped under the symbol, Tu.||||||
6509|Falloch beds|69599|5|Briefly described|p580, p585, p602|Miocene|Miocene|Karumba Basin, Carpentaria region; crops out poorly near Coen. Up to 55m thick. Fluvial deposits. Appears as Faloch beds on p585. Capped by laterite of the Kendall Surface.||||Correlated with Yam Creek, Lilyvale and Wyaaba beds and ?Campaspe Formation.|Clayey quartzose sand, gravel and interbedded sandy clay.|
6509|Falloch beds|71792|5|Briefly described|p2, p59-p62|Pliocene|Miocene|Appears as Falloch Creek beds on p2 and p 59.|||||Fluviatile clayey quartz sand, gravel, interbedded sandy clay; mildly lateritised.|
6509|Falloch beds|71849|5|Briefly described|p8, p49, p64, p79, p94, p102, p105|Quaternary|Tertiary|See also p107-108, p114, p195. Extensively weathered; forms flat-lying country.||||Nonconformably overlies Meldrum, Emu Yard, Lankelly and McIlwraith Granites.||
6509|Falloch beds|71853|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartz sands, gravel, interbedded sandy clay; fluviatile deposits, mildly lateritised.|
6509|Falloch beds|71854|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartz sand, gravel, interbedded sandy clay; fluviatile deposits; mildly lateritised.|
6511|Falls Creek Tonalite|23422|4|Described|p174|||Ordovician?  Intrudes Running River Metamorphics.  See also p209 Table 6.5.||||||
6511|Falls Creek Tonalite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
6511|Falls Creek Tonalite|23513|5|Briefly described|Map legend|Devonian|Proterozoic|Palaeozoic Intrusive No.162. I-Type.||||||23-APR-08
6511|Falls Creek Tonalite|23617|4|Described|p7|||Intrudes Running River Metamorphics. Also see Table 2 p18 and Table 3 p52. Macrossan Province.||||||
6511|Falls Creek Tonalite|23618|5|Briefly described|map legend|Devonian|Ordovician|||||||
6511|Falls Creek Tonalite|23893|6|Mentioned|p27|||||||||
6511|Falls Creek Tonalite|42407|3|Fully described|p37|||NOT variation of Falls Creek Granodiorite, Vic.  Age uncertain, mid-Proterozoic to Carboniferous.||||||
6511|Falls Creek Tonalite|42474|5|Briefly described|p28|||||||||
6511|Falls Creek Tonalite|42689|5|Briefly described|map legend|Proterozoic|Paleoproterozoic|||||||07-NOV-08
6511|Falls Creek Tonalite|42690|5|Briefly described|map legend|Early Paleozoic|Paleoproterozoic|Early to Middle Proterozoic and/or Early Palaeozoic||||||07-NOV-08
6511|Falls Creek Tonalite|42692|5|Briefly described|map legend|Proterozoic||||||||
6511|Falls Creek Tonalite|43095|5|Briefly described|Plate 2.|||||||||
6511|Falls Creek Tonalite|43259|4|Described|Appendix 1,p26.|Devonian|Proterozoic|Proterozoic to Devonian?.||||||
6511|Falls Creek Tonalite|43589|6|Mentioned|p23|||Age: 331+/-2 Ma (Rb-Sr). Intruded by Kallanda Granite and Coane Range Granite Complex.||||||23-APR-08
6511|Falls Creek Tonalite|68350|5|Briefly described|Map legend.|Early Devonian?|Ordovician|Macrossan Province.|||||Grey, medium-grained, equigranular biotite tonalite (hornfelsed).|
6511|Falls Creek Tonalite|68351|5|Briefly described|Map legend.|Early Devonian?|Ordovician|Macrossan Province.|||||Grey, medium-grained, equigranular biotite tonalite (hornfelsed).|
6511|Falls Creek Tonalite|68419|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained, equigranular biotite tonalite (hornfelsed).|
6511|Falls Creek Tonalite|68420|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained, equigranular biotite tonalite (hornfelsed).|
6511|Falls Creek Tonalite|73425|5|Briefly described|p1, 3-5, 10, 14, 16-18|Ordovician|Ordovician|Continental arc setting. Linked to migmatites in Running River Metamorphics.|457 +/- 1 Ma.|||Intrudes Running River Metamorphics.|I-type granitoid; calc-alkaline. Occurs mainly as a series of deformed, medium- to coarse-grained intrusions, from biotite tonalite to granodiorite. Rafts/enclaves of gneiss, amphibolite and quartzite are very common.|
6516|Fanning River Group|22800|6|Mentioned|p591||Givetian|||||||
6516|Fanning River Group|22847|6|Mentioned|p 7|||||||||
6516|Fanning River Group|23422|4|Described|p180, p206 Table 6.3|Middle Devonian|Middle Devonian|Overlain by Dotswood Group. Maximum thickness: 690m. Geological Province: Burdekin Basin:||||||14-NOV-07
6516|Fanning River Group|23424|6|Mentioned|p346|||Burdekin Basin Province.||||||
6516|Fanning River Group|23430|5|Briefly described|p505|||||||||
6516|Fanning River Group|23431|5|Briefly described|p538|||||||||
6516|Fanning River Group|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|||||||
6516|Fanning River Group|23522|5|Briefly described|p258|Middle Devonian|Early Devonian|||||||
6516|Fanning River Group|23893|5|Briefly described|p16|Tournaisian|Emsian|Geological Province: Burdekin Province||||||
6516|Fanning River Group|24074|5|Briefly described|p389 Table 1|Givetian|Givetian|Maximum thickness: 360m.||||||
6516|Fanning River Group|24577|5|Briefly described|p752 Fig. 1|Givetian|Eifelian|Overlain by the Vanneck Formation. Group is Gp in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
6516|Fanning River Group|24610|5|Briefly described|p62|Middle Devonian|Middle Devonian|Overlying Unit: Dotswood Group (u). Geological Province: Burdekin Basin. Maximum Thickness: >670m. Overlain dis/unconform. by Myrtlevale Fm. (basal part of Keelbottom Group) where Dotswood Gp. is missing.||||||
6516|Fanning River Group|24611|6|Mentioned|p193|Devonian|Devonian|||||||
6516|Fanning River Group|24612|4|Described|p7|Middle Devonian|Early Devonian|Geological Province: Burdekin Basin. First studied by Hill (1942) - major revision in 1987 by GSQ. Now includes 5 lithostratigraphic units instead of the original 3 - with 10 coral associations recognised. Overlain by Dotswood Group or Myrtlevale Fm.||||||04-JUL-14
6516|Fanning River Group|24613|2|Defined|p3, p6 Fig. 6, p10-12, p18-19|Givetian|Givetian|Formerly Fanning Group (Wyatt 1961, 1963, unpub). Comprises Laroona Fm, Mount Podge Limestone, Big Bend Arkose, Cultivation + Burdekin Formations. Unconformable below Dotswood Group. Thickness: 690m. Geol.prov: Burdekin Basin. Type section included.||||||14-MAY-15
6516|Fanning River Group|24614|4|Described|p191 Fig. 1, p192|||Formerly contained the Laroona Arkose and Mount Podge Limestone (Wilkie Group). Includes Cultivation Gully Formation and Burdekin Limestone (or Formation) and Big Bend Arkose. Geological Province: Burdekin Basin. See also P193 Fig. 2.||||||07-FEB-11
6516|Fanning River Group|29960|5|Briefly described|p10|||||||||
6516|Fanning River Group|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
6516|Fanning River Group|31285|4|Described|p82|||See also P85, 86. Couvinian - See also P85, 86. Couvinian -||||||
6516|Fanning River Group|31999|5|Briefly described|p140|||Table 11||||||
6516|Fanning River Group|32140|6|Mentioned|p4|||See also P5||||||
6516|Fanning River Group|32169|6|Mentioned|Table 2|||M.Devonian||||||
6516|Fanning River Group|32553|4|Described|p50|||||||||
6516|Fanning River Group|32619|6|Mentioned|p463|||Fauna. Givetian.||||||
6516|Fanning River Group|35008|6|Mentioned|p179|||||||||
6516|Fanning River Group|36472|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6516|Fanning River Group|37565|6|Mentioned|Fig.6|||||||||
6516|Fanning River Group|37573|3|Fully described|p207|||See also Figs.2,4 and Table 1.||||||
6516|Fanning River Group|39445|6|Mentioned|p73|||See also Table 5||||||
6516|Fanning River Group|39686|4|Described|p75|||||||||
6516|Fanning River Group|39689|6|Mentioned|p57|||||||||
6516|Fanning River Group|39731|4|Described|p31|||||||||
6516|Fanning River Group|39732|4|Described|p29|||||||||
6516|Fanning River Group|39735|6|Mentioned|p18|||||||||
6516|Fanning River Group|39987|6|Mentioned|p66|||||||||
6516|Fanning River Group|40623|5|Briefly described|p88|||||||||
6516|Fanning River Group|40787|6|Mentioned|p339|||||||||
6516|Fanning River Group|41735|6|Mentioned|p284|||||||||
6516|Fanning River Group|41774|6|Mentioned|p31|||||||||
6516|Fanning River Group|41916|4|Described|p28|||||||||
6516|Fanning River Group|42031|6|Mentioned|p764|||||||||
6516|Fanning River Group|42295|5|Briefly described|p4|||||||||
6516|Fanning River Group|42407|6|Mentioned|p22, p42|||||||||
6516|Fanning River Group|42689|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
6516|Fanning River Group|42690|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
6516|Fanning River Group|42692|5|Briefly described|map legend|Devonian||||||||
6516|Fanning River Group|42750|6|Mentioned|p36, p46|||||||||
6516|Fanning River Group|42933|5|Briefly described|Fig. 73|||||||||
6516|Fanning River Group|43095|5|Briefly described|Plate 2|||||||||
6516|Fanning River Group|43775|6|Mentioned|p27|||||||||
6516|Fanning River Group|43933|5|Briefly described|Map Legend||Middle Devonian|||||||
6516|Fanning River Group|43935|5|Briefly described|Map Legend||Middle Devonian|||||||
6516|Fanning River Group|44058|14|Not recorded|p99,103,Tb.p104|||||||||
6516|Fanning River Group|44060|14|Not recorded|Map Legend||Middle Devonian|||||||
6516|Fanning River Group|44061|4|Described|Table 2||Devonian|||||||
6516|Fanning River Group|44091|14|Not recorded|p31||Middle Devonian|||||||
6516|Fanning River Group|45151|5|Briefly described|Table 6|||See also P8.||||||
6516|Fanning River Group|48904|4|Described|p22|||New name||||||
6516|Fanning River Group|48914|6|Mentioned|p30|||M. Middle Dev.||||||
6516|Fanning River Group|62522|5|Briefly described|p20|Middle Devonian|Middle Devonian|Unconformably overlain by Dotswood Group.  Geological Province: Burdekin Basin. Limestones and associated siliciclastic rocks.||||||
6516|Fanning River Group|63154|5|Briefly described|p285 Fig. 5|Devonian|Devonian|Geological province: Charters Towers Province.||||||
6516|Fanning River Group|67402|5|Briefly described|p246|Givetian|Givetian|Burdekin Basin. |||Includes the Big Bend Formation, Burdekin Formation and Cultivation Gully Formation.|Overlain by the Dotswood Group.||
6516|Fanning River Group|68350|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Burdekin Basin.|||Includes Burdekin Formation.|Is overlain conformably by Dotswood Group.|Undivided calcareous, fossiliferous, feldspathic sandstone, pebbly sandstone and conglomerate and fossiliferous limestone.|
6516|Fanning River Group|68351|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Burdekin Basin.|||Includes Burdekin Formation.|Is overlain conformably by Dotswood Group.|Undivided calcareous, fossiliferous, feldspathic sandstone, pebbly sandstone and conglomerate and fossiliferous limestone.|
6516|Fanning River Group|68419|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Of the Burdekin Basin. Includes three facies of which the top and bottom units are unnamed.|||Includes Burdekin Formation.|Conformably overlain by the Dotswood Group.|Calcareous, fossiliferous, feldspathic sandstone, pebbly sandstone and conglomerate, and fossiliferous limestone.|
6516|Fanning River Group|68420|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Of the Burdekin Basin. Includes three facies of which the top and bottom units are unnamed.|||Includes Burdekin Formation.|Conformably overlain by the Dotswood Group.|Calcareous, fossiliferous, feldspathic sandstone, pebbly sandstone and conglomerate, and fossiliferous limestone.|
6516|Fanning River Group|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Burdekin Basin.||||||
6516|Fanning River Group|68731|5|Briefly described|p177 Fig 3.91, p183, p185 Tb 3.4, p187|Middle Devonian|Middle Devonian|Burdekin Basin. Represents a transgressive-regressive succession.|||Includes Cultivation Gully Formation, Burdekin Formation, and Big Bend Formation.|Equivalent to the Collopy Formation.|Comprises predominantly shallow-marine carbonates.|
6516|Fanning River Group|69030|5|Briefly described|p6|Carboniferous|Devonian|Camel Creek Subprovince (Broken River Province).|||Big Bend, Burdekin, Cultivation Gully Formations.|||
6516|Fanning River Group|71031|5|Briefly described|p56-p57|Middle Devonian|Middle Devonian|Burdekin Basin. |||Includes the Big Bend Formation.|Overlies the Millchester Supersuite.||
6516|Fanning River Group|73143|6|Mentioned|p17|Givetian|Givetian|Burdekin Basin. Contains rugose coral Nardophyllum proliferum (Zhen, 1994).||||||
6565|Featherbed Volcanic Group|22675|5|Briefly described|p124|Early Permian|Early Permian|||||||
6565|Featherbed Volcanic Group|23291|5|Briefly described|p37|||Geological Province: Georgetown Region.||||||08-JUL-15
6565|Featherbed Volcanic Group|23420|5|Briefly described|p 131||Early Permian|||||||
6565|Featherbed Volcanic Group|23423|3|Fully described|p305 Table 7.3|Early Permian|Late Carboniferous|Contained within the Featherbed Cauldron Complex. Also see p236. Kennedy Igneous Province.||||||
6565|Featherbed Volcanic Group|23430|5|Briefly described|p475|||||||||
6565|Featherbed Volcanic Group|23497|6|Mentioned|p32||Permian|||||||
6565|Featherbed Volcanic Group|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Kennedy Province.||||||03-JUN-09
6565|Featherbed Volcanic Group|23501|5|Briefly described|map legend|Early Permian|Early Permian|||||||
6565|Featherbed Volcanic Group|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
6565|Featherbed Volcanic Group|23506|5|Briefly described|Map Legend||Late Carboniferous|||||||
6565|Featherbed Volcanic Group|23616|5|Briefly described|p5, Table 3 p46.|||Hodgkinson Province.||||||
6565|Featherbed Volcanic Group|23624|5|Briefly described|p23|||||||||
6565|Featherbed Volcanic Group|23713|3|Fully described|p21-24|Early Permian|Late Carboniferous|Parallel to the Palmerville Fault. A-type volcanics.||||||
6565|Featherbed Volcanic Group|24086|5|Briefly described|p312 Fig. 1|Early Permian|Early Permian|See also Featherbed Volcanics.||||||
6565|Featherbed Volcanic Group|24213|5|Briefly described|p776 Fig. 1|Permian|Early Permian|||||||
6565|Featherbed Volcanic Group|24485|5|Briefly described|p2, 40|Early Permian|Late Carboniferous|||||||
6565|Featherbed Volcanic Group|24486|5|Briefly described|Map legend|Early Permian|Early Permian|Contains the Wakara Volcanics Subgroup.  Geological Province: Kennedy Province.||||||
6565|Featherbed Volcanic Group|41569|6|Mentioned|p71|||||||||
6565|Featherbed Volcanic Group|41775|6|Mentioned|p71|||||||||
6565|Featherbed Volcanic Group|42681|4|Described|p18|||||||||
6565|Featherbed Volcanic Group|43060|5|Briefly described|p67|||see also Table 5.||||||
6565|Featherbed Volcanic Group|43083|4|Described|p79, p90|Early Permian|Late Carboniferous|Part of the Wakara Caldera sequence.||||||17-JUN-09
6565|Featherbed Volcanic Group|43087|5|Briefly described|Fig.3|||||||||
6565|Featherbed Volcanic Group|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Includes the Wakara, Djungan, Yongala, Tennyson, Timber Top and Boonmoo Volcanic Subgroups.||||||15-JUN-06
6565|Featherbed Volcanic Group|43254|5|Briefly described|map legend||Early Permian|||||||
6565|Featherbed Volcanic Group|43259|6|Mentioned|Appendix 1,p9.||Late Carboniferous|||||||
6565|Featherbed Volcanic Group|43285|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
6565|Featherbed Volcanic Group|43625|3|Fully described|p35,68|Early Permian|Late Carboniferous|||||||
6565|Featherbed Volcanic Group|43626|3|Fully described|p10,16||Late Carboniferous|313-301 Ma||||||
6565|Featherbed Volcanic Group|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||31-MAY-04
6565|Featherbed Volcanic Group|60425|5|Briefly described|p63-64, p14 Tb. 1, p46 Tb.3, p52|Early Permian|Late Carboniferous|Includes 6 named volcanic subgroups - Boonmoo, Tennyson, Timber Top, Yongala, Djungan and Wakara + named but ungrouped units. Includes interpretation of origin, age and granite-type (p63-64). About 10% of group is welded. I-types.||||||07-FEB-11
6565|Featherbed Volcanic Group|61035|6|Mentioned|p6|||||||||07-FEB-11
6565|Featherbed Volcanic Group|62523|4|Described|p2, p3-4 (map/legend)|Early Permian|Late Carboniferous|Previously "Featherbed Volcanics". Succession of overlapping subsidence structures, each a distinct volcanic rocks assemblage (subgroups) which together form Featherbed Cauldron Complex -- Timber Top, Yongala and Djungan Volcanic Subgroups.||||||07-FEB-11
6565|Featherbed Volcanic Group|65114|5|Briefly described|p383 Tb.1, p398|Cisuralian|Upper Carboniferous|300-280 Ma (?start at 313 Ma); Tectonic unit: Kennedy Igneous Province; volcanism in this group began at about 313 Ma with major pulses at about 300, 290 and 280 Ma||||||
6565|Featherbed Volcanic Group|65388|6|Mentioned|p85|||Example of QLD practice of retaining original names as Group names even though dating has shown considerable time spans and probable breaks. ||||||
6565|Featherbed Volcanic Group|66529|6|Mentioned|p60|Permian|Late Carboniferous|Minimum age is Early Permian. Has high prospectivity for orthomagmatic U mineralisation.||||||
6565|Featherbed Volcanic Group|68307|5|Briefly described|p78, p81, p83, p92|Permian|Late Carboniferous|Mossman Orogen. Shows a synclinal form to a depth of ~2.5 km.||||||
6565|Featherbed Volcanic Group|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Boonmoo, Tennyson, Yongala, Djungan and Wakara Volcanic Subgroups; Boxwood Volcanics; Patrick, Beapeo, Doolan Creek and Jamtin Rhyolites.|||
6565|Featherbed Volcanic Group|68553|6|Mentioned|Map legend|Permian|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk. Also mapped in part under symbol CPvk||||||26-APR-13
6565|Featherbed Volcanic Group|68576|5|Briefly described|Q_11: p11, p14|Permian|Late Carboniferous|Dimbulah area. Forms hilly terrain. Emplaced within the Featherbed Cauldron Complex.|||Includes Boonmoo Volcanic Subgroup.||Mostly (85%) welded rhyolitic ignimbrite; 10% is dacitic to andesitic ignimbrite; 5% is dacitic to andesitic lavas, rhyolitic lava flows and domes, rare unwelded pyroclastic rocks including tuffs, and very rare reworked (sedimentary) volcaniclastics.|23-OCT-19
6565|Featherbed Volcanic Group|68679|6|Mentioned|p355|||Mackenzie (1993). Cited as an example (as with the Connors Volcanics/Volcanic Group) of the practice whereby a succession mapped as a single unit is subdivided, with the original name retained as a Group.||||||
6565|Featherbed Volcanic Group|69030|5|Briefly described|p6, p9|Permian|Carboniferous|Chillagoe Subprovince, Hodgkinson Province.|308 +/- 3 Ma; 288 +/- 17 Ma.|||||
6565|Featherbed Volcanic Group|69079|6|Mentioned|p42|||Mentioned as a possible source of gold  mineralisation in the Hodgkinson Goldfield.||||||
6565|Featherbed Volcanic Group|69592|5|Briefly described|p243-244, p249, p300 Fig.4.93|Permian|Pennsylvanian|SW margin of Palmer-Barron Subprovince. Essentially undeformed. Source of rhyolite clasts in lower Pepper Pot Sandstone conglomerates.||||||
6565|Featherbed Volcanic Group|69593|4|Described|p484-487, p488 Fig.6.11, p503-504, p513|Permian|Late Carboniferous|Herberton and Tate Subprovinces. These A-type extrusive rocks are included in the Lags Supersuite. Also includes Nightflower Dacite. Andesitic or dacitic rocks comprise <15 % of the Group. Geochemistry described. Sm-Nd isotope data tabulated.|~312-280 Ma.||Djungan, Wakara, Yongara Subgroups; Timbertop, Tennyson, Boonmoo, Volcanic Subgroups; Boxwood Volcanics; Bluewater, Jamtin, Fisherman, Arringunna, Ticklehim, Combella, Lumma Rhyolites. See COMMENTS.||A-type. Rhyolitic-dacitic ignimbrite, lava and tuff; minor to rare basalt and andesite.|
6565|Featherbed Volcanic Group|70207|6|Mentioned|p82|||Chillagoe area.|||||A-type.|
6565|Featherbed Volcanic Group|72297|5|Briefly described|p697, p726|||Basement to the unconformably-overlying, coal-bearing Ngarrabullgan Basin. Minor rhyolitic ignimbrite has been quarried near Emuford for dimension stone.||||||
6565|Featherbed Volcanic Group|72983|6|Mentioned|p19|Kungurian|Kungurian|Suspected coeval with Collins Weir Rhyolite, Tinaroo Granite, Hope Vale Granite and Nychum Volcanics.|278 +/- 3 Ma|||||
6568|Featherby Surface|23424|5|Briefly described|p340|Tertiary|Tertiary|||||||
6568|Featherby Surface|37607|5|Briefly described|Fig.3|||See also Fig.4 and p332,333.||||||03-MAR-22
6568|Featherby Surface|69599|5|Briefly described|p584-586, p593-594, p650|Oligocene|Eocene|Grimes (1980). Emerald-Biloela area. Two phases of duricrust development. Age also given as middle-late Miocene.|||||Silcrete and laterite.|
6568|Featherby Surface|70352|5|Briefly described|Map legend|Neogene|Neogene||||||Deeply weathered: ferricrete and minor silcrete.|
6568|Featherby Surface|70570|5|Briefly described|Map legend.|Neogene|Paleogene|Deeply weathered.|||||Ferricrete and minor silcrete.|
6631|Fickling Group|7071|5|Briefly described|p1|Mesoproterozoic|Paleoproterozoic|Geological Province: northern Mount Isa Inlier.||||||07-NOV-08
6631|Fickling Group|22457|6|Mentioned|Fig29 P30|||||||||
6631|Fickling Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
6631|Fickling Group|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Underlain by Peters Creek Volcanics.||||||18-SEP-06
6631|Fickling Group|22665|6|Mentioned|P219, P229|||||||||
6631|Fickling Group|22673|6|Mentioned|63,64,65|||Geol province Mount Isa Basin. Overlying unit South Nicholson Group Volcanics, underlying unit Peters Creek Volcanics.||||||23-DEC-08
6631|Fickling Group|22680|5|Briefly described|83-87|Mesoproterozoic|Paleoproterozoic|Geological province: Mount Isa Basin.||||||07-NOV-08
6631|Fickling Group|23031|6|Mentioned|27|||||||||
6631|Fickling Group|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geol province Lawn Hill Subprovince||||||
6631|Fickling Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
6631|Fickling Group|23362|6|Mentioned|337|||||||||
6631|Fickling Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6631|Fickling Group|23395|6|Mentioned|p383|||||||||
6631|Fickling Group|23396|5|Briefly described|p407 Fig.2|||||||||
6631|Fickling Group|23397|5|Briefly described|p463|||||||||
6631|Fickling Group|23398|4|Described|p445|||||||||
6631|Fickling Group|23405|4|Described|p566|||||||||
6631|Fickling Group|23406|4|Described|p606, p609 Fig. 9|Paleoproterozoic|Paleoproterozoic|Includes Fish River Formation, Walford Dolomite, Mount Les Siltstone and Doomadgee Formation. Overlain by South Nicholson Group. Age: 1700-1585Ma. In the Murphy Inlier.||||||17-JUN-09
6631|Fickling Group|23409|5|Briefly described|p533|||||||||
6631|Fickling Group|23958|6|Mentioned|p1132|||||||||
6631|Fickling Group|24308|5|Briefly described|p987 Fig. 2|Mesoproterozoic|Paleoproterozoic|Geological Province:  Mount Isa Superbasin||||||07-NOV-08
6631|Fickling Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
6631|Fickling Group|24432|6|Mentioned|p566 Fig.5|Statherian|Statherian|||||||25-FEB-05
6631|Fickling Group|24442|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic|Revised as a new unit and probably belongs to the South Nicholson Group.  Formerly mapped in the Bauhinia Dome. Age: 1670-1600Ma.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||
6631|Fickling Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6631|Fickling Group|31421|6|Mentioned|p509|||||||||
6631|Fickling Group|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|36012|3|Fully described|Table 3|||See also p16.||||||09-AUG-06
6631|Fickling Group|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|37462|4|Described|Table4.VII|||||||||
6631|Fickling Group|37565|6|Mentioned|Fig.5|||||||||
6631|Fickling Group|37568|6|Mentioned|Fig.5|||||||||
6631|Fickling Group|38584|4|Described|p17|||||||||
6631|Fickling Group|39445|6|Mentioned|p36|||See also p39 & Table 2. Correlated with McArthur, McNamara & Mt Isa Group.||||||02-FEB-22
6631|Fickling Group|39497|6|Mentioned|Fig.4|||||||||
6631|Fickling Group|39685|6|Mentioned|Fig.1|||||||||
6631|Fickling Group|39925|6|Mentioned|p333|||||||||
6631|Fickling Group|40840|6|Mentioned|Map legend|||||||||
6631|Fickling Group|41319|6|Mentioned|Fig.1|||||||||
6631|Fickling Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
6631|Fickling Group|41721|6|Mentioned|p28|||Includes detailed descriptions of components Fish River Formation, Walford Dolomite, Mount Les Siltstone and Doomadgee Formation.||||||01-AUG-07
6631|Fickling Group|41722|6|Mentioned|Map legend|||||||||
6631|Fickling Group|42385|5|Briefly described|Fig.4 p7|||||||||02-FEB-22
6631|Fickling Group|42386|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6631|Fickling Group|42638|6|Mentioned|Map legend|||Appears on Regional Setting map.|||||Dolostone, dolomitic siltstone, sandstone, shale.|07-NOV-11
6631|Fickling Group|42639|5|Briefly described|Fig.4 P7|||||||||
6631|Fickling Group|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic" age.||||||18-SEP-06
6631|Fickling Group|43235|6|Mentioned|p8|||Proterozoic||||||
6631|Fickling Group|43486|5|Briefly described|21|||||||||
6631|Fickling Group|43615|6|Mentioned|p13|||||||||
6631|Fickling Group|45162|6|Mentioned|p147|||||||||
6631|Fickling Group|45166|5|Briefly described|p27|||||||||
6631|Fickling Group|46804|6|Mentioned|p154|||||||||
6631|Fickling Group|49001|2|Defined|p13|Carpentarian|Carpentarian|||||||
6631|Fickling Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: Calvert Superbasin.||||||07-FEB-11
6631|Fickling Group|60558|5|Briefly described|p3, p5 Fig. 4|||Includes; Fish River and Doomadgee Formations, Mount Les Siltstone and Walford Dolomite.||||||29-JUN-09
6631|Fickling Group|61736|5|Briefly described|p674|Paleoproterozoic|Paleoproterozoic|Age: 1640+/-7Ma (the Walford deposit).||||||
6631|Fickling Group|62473|5|Briefly described|p75||Paleoproterozoic|Age: ca. 1640Ma. Contains the Walford deposit.||||||17-JUN-09
6631|Fickling Group|62535|5|Briefly described|p674|||Hosts the Walford Pb-Zn-Ag deposit.|1640 +/- 7 Ma.|||||
6631|Fickling Group|62659|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
6631|Fickling Group|63115|6|Mentioned|p1280-1281. ||||||Includes Mount Les Siltstone.|||
6631|Fickling Group|64575|6|Mentioned|p657|||Geological Province: Murphy Inlier.||||||
6631|Fickling Group|64724|5|Briefly described|p45 Fig.5, p46|Proterozoic|Proterozoic|South Nicholson Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
6631|Fickling Group|64815|6|Mentioned|p3|||||||||
6631|Fickling Group|65228|6|Mentioned|p9|||||||||
6631|Fickling Group|65337|5|Briefly described|p6 Fig.3, p30, p36.|Mesoproterozoic|Paleoproterozoic|Carbonate sediments; probably contiguous with McNamara Group to the south in the Carrara Range.|c.1670-1590 Ma.||Includes Walford Dolomite.|||
6631|Fickling Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107||||||Includes Doom Supersequence, Doomagee Formation, Fish River Formation, Mount Les Siltstone, Walford Dolomite|||
6631|Fickling Group|68146|5|Briefly described|p2, p196, p198||||||Doomadgee Formation.|Is overlain unconformably by South Nicholson Group.||
6631|Fickling Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
6631|Fickling Group|68575|6|Mentioned|p11|||||`|Doomadgee Formation.|Overlies Peters Creek Volcanics.||
6631|Fickling Group|69417|6|Mentioned|p2:5-6|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
6631|Fickling Group|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
6631|Fickling Group|69433|4|Described|p18:1-4, 10|Statherian|Statherian|Formerly the Fickling beds (Carter, 1959). Northern succession, Lawn Hill Platform. Hosts the large low-grade pyrite-rich Walford Creek and Bluebush stratiform Pb-Zn deposits in Qld.|||Fish River, Doomadgee Formations; Walford Dolostone; Mount Les Siltstone.|Unconformably overlies Peters Creek Volcanics. Correlated with McArthur and McNamara Groups.|A succession of sandstone, dolostone, siltstone and shale.|12-JUL-16
6631|Fickling Group|69434|5|Briefly described|p19:1, 6|||Lawn Hill Platform. Mapping by Smith and Roberts (1963) included rocks later distinguished as a separate unit (the Caulfield beds) by Rawlings et al. (2008).||||Is overlain disconformably or unconformably by Accident Subgroup (South Nicholson Group).||12-JUL-16
6631|Fickling Group|69591|5|Briefly described|p29, p55|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Mount Isa Province.|||Doomadgee, Fish River Formations; Mount Les Siltstone; Walford Dolomite.|||
6631|Fickling Group|69673|5|Briefly described|p3 fig 2, p51, p52 fig 42|Mesoproterozoic|Paleoproterozoic||||Includes Fish River Formation|Unconformably overlies Wire Creek Sandstone, Peters Creek Volcanics, Correlated with McNamara Group, McArthur Group|Sandstone, dolostone, siltstone and shale.|
6631|Fickling Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.|||Fish River, Doomadgee Formations; Walford Dolostone; Mount Les Siltstone.|Unconformably overlies Peters Creek Volcanics (Tawallah Group equivalent). Is overlain unconformably by Constance Sandstone (South Nicholson Group).||
6631|Fickling Group|70897|5|Briefly described|p39, p45|||Mixed carbonate-clastic lithofacies.||||All units are overlain with an angular unconformity by South Nicholson Group.||
6631|Fickling Group|71369|5|Briefly described|p4, p10-11|||Underwent moderate folding but little metamorphism during the 1585-1500 Ma Mount Isa Orogeny. Basement for South Nicholson Group.|||Doomadgee Formation.|Is overlain unconformably by the Hedleys Sandstone and the South Nicholson Group.||20-FEB-18
6631|Fickling Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain unconformably by South Nicholson Group. Underlain unconformably by Peters Creek Volcanics. Equivalent to McNamara Group.||
6631|Fickling Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||||Dolostone, dolomitic siltstone, sandstone, shale (+/- carbonaceous).|
6631|Fickling Group|72526|5|Briefly described|p1, p4, p6, p8, p20, 27, 33, 40, 46, 85|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin, p8. Said to be of theLawn Hill Platform, Mount Isa Province, p20 etc. Depositional ages from Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b.|c. 1649 Ma to 1613 Ma||Includes Doomadgee Formation, Mount Les Siltstone, Walford Dolomite, Fish River Formation.|Shown as partially overlying Weberra Granite and Nicholson Granite Complex.||
6631|Fickling Group|72527|6|Mentioned|p5, p10, p161, p185.|Statherian|Statherian||1613 +/- 5 Ma||Includes Doomadgee Formation|||
6631|Fickling Group|72912|4|Described|p5 Fig.3, p13, p32, p33, p35, p45-46.|Statherian|Statherian|Northwestern Mount Isa Province. Known to be potential sources of hydrocarbons. See also p35 Fig.13.|||Doomadgee Formation, Mount Les Siltstone, Walford Dolomite and Fish River Formation.|Unconformably underlies South Nicholson Group. Laterally equivalent to McNamara Group.|Includes shallow marine carbonates, dolomitic siltstone, organic rich siltstone and shales, and dolostone.|15-MAR-21
6631|Fickling Group|72913|5|Briefly described|p7, p9 Tb.1.|Paleoproterozoic|Paleoproterozoic|Shown as being in the west of the Isa Superbasin.|||Includes Doomadgee Formation, Mount Les Siltstone, Walford Dolostone/Dolomite and Fish River Formation||Includes dolomitic siltstone and dolostone.|
6631|Fickling Group|72919|6|Mentioned|p3, p98|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.||||||
6631|Fickling Group|72967|6|Mentioned|p2, p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||Doomadgee Formation, Mount Les Siltstone, Walford Dolostone|||
6631|Fickling Group|73042|6|Mentioned|p1, p3-4, p6, p14, p16-17|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.|||Doomadgee Formation, Fish River Formation, Mount Les Siltstone, Walford Dolomite.|||
6639|Fiery Creek Volcanics|22438|3|Fully described|p537, Fig.3 p537|Paleoproterozoic|Paleoproterozoic|Bimodal volcanics (intercalated with sedimentary rocks of Bigie Formation). See also Fig.10a p546.||||||23-DEC-08
6639|Fiery Creek Volcanics|22457|4|Described|P29, Fig29, Fig30|||Equivalent to part of Peters Creek Volcanics?||||||
6639|Fiery Creek Volcanics|22585|5|Briefly described|Fig1 P736, Fig3|||||||||
6639|Fiery Creek Volcanics|22644|5|Briefly described|5 fig 2|||Geol. province: Mount Isa Basin. Underlain by Quilalar Formation. Volcanics as 'V' in text.||||||18-JAN-07
6639|Fiery Creek Volcanics|22665|5|Briefly described|P219, Table1||Statherian|Age of unit is 1709+/-3 Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|22680|6|Mentioned|83|||||||||
6639|Fiery Creek Volcanics|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Fold Belt. Underlain by Bigie Formation, Myally Subgroup, Quilalar Formation.||||||07-NOV-08
6639|Fiery Creek Volcanics|23205|6|Mentioned|p44|||Of Mount Isa Inlier.||||||23-DEC-08
6639|Fiery Creek Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: ~1709+/-3Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23393|5|Briefly described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Age: 1709+/-3Ma.  Geological Province: Lawn Hill Sub-province.  See also p17 Fig.5.||||||07-NOV-08
6639|Fiery Creek Volcanics|23395|6|Mentioned|p385|||||||||
6639|Fiery Creek Volcanics|23396|4|Described|p418|Statherian|Statherian|||||||
6639|Fiery Creek Volcanics|23397|5|Briefly described|p463|||||||||
6639|Fiery Creek Volcanics|23398|5|Briefly described|p433 Fig.2|Statherian|Statherian|Age: 1709+/-3Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23399|6|Mentioned|p489|||||||||
6639|Fiery Creek Volcanics|23406|5|Briefly described|p603, p607 Fig. 8|||Stated to be of a basal "rift" package. Geological province: Lawn Hill Platform.||||||16-JUN-09
6639|Fiery Creek Volcanics|23408|5|Briefly described|p511, p513 Fig. 2|||Unconformable below the McNamara Group. This unit was added by Hutton et al (1981) to the McNamara and Mount Isa Groups.||||||15-JUN-09
6639|Fiery Creek Volcanics|23466|5|Briefly described|p267|Statherian|Statherian|Age:1708+/-2Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
6639|Fiery Creek Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1955.||||||
6639|Fiery Creek Volcanics|23965|5|Briefly described|p1297|Paleoproterozoic|Paleoproterozoic|Age: 1709 +/- 3Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
6639|Fiery Creek Volcanics|24197|5|Briefly described|p28, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1710Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
6639|Fiery Creek Volcanics|24307|5|Briefly described|p978|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
6639|Fiery Creek Volcanics|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6639|Fiery Creek Volcanics|24309|5|Briefly described|p1017|||||||||
6639|Fiery Creek Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
6639|Fiery Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1709 Ma.||||||
6639|Fiery Creek Volcanics|36548|6|Mentioned|p513|||||||||
6639|Fiery Creek Volcanics|37459|2|Defined|p426|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||23-DEC-08
6639|Fiery Creek Volcanics|37462|4|Described|Table4.VII|||See also p244.||||||18-SEP-06
6639|Fiery Creek Volcanics|37565|6|Mentioned|p11|||||||||
6639|Fiery Creek Volcanics|37568|6|Mentioned|p85|||||||||
6639|Fiery Creek Volcanics|38232|6|Mentioned|p82|||||||||
6639|Fiery Creek Volcanics|38237|5|Briefly described|p126|||||||||
6639|Fiery Creek Volcanics|38276|6|Mentioned|Fig.1|||||||||
6639|Fiery Creek Volcanics|38310|6|Mentioned|p237|||||||||
6639|Fiery Creek Volcanics|38348|6|Mentioned|p6|||||||||
6639|Fiery Creek Volcanics|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|38560|6|Mentioned|p113|||||||||
6639|Fiery Creek Volcanics|38584|6|Mentioned|p22|||||||||
6639|Fiery Creek Volcanics|38833|6|Mentioned|p161|||||||||
6639|Fiery Creek Volcanics|38835|6|Mentioned|p164|||||||||
6639|Fiery Creek Volcanics|38919|6|Mentioned|p497|||||||||
6639|Fiery Creek Volcanics|39445|5|Briefly described|p40|||See also p36 and Table 2.||||||18-JAN-07
6639|Fiery Creek Volcanics|39497|6|Mentioned|p8|||||||||
6639|Fiery Creek Volcanics|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
6639|Fiery Creek Volcanics|39622|6|Mentioned|Fig.2|||||||||
6639|Fiery Creek Volcanics|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|39925|6|Mentioned|p329|||||||||
6639|Fiery Creek Volcanics|39934|6|Mentioned|Fig.3|||||||||
6639|Fiery Creek Volcanics|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|40105|6|Mentioned|p310|||||||||
6639|Fiery Creek Volcanics|40221|3|Fully described|p12|||||||||
6639|Fiery Creek Volcanics|40691|5|Briefly described|p11|||||||||
6639|Fiery Creek Volcanics|40811|6|Mentioned|p318|||||||||
6639|Fiery Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
6639|Fiery Creek Volcanics|40984|6|Mentioned|p400|||||||||
6639|Fiery Creek Volcanics|41307|4|Described|p13|||||||||
6639|Fiery Creek Volcanics|41978|6|Mentioned|p502|||||||||
6639|Fiery Creek Volcanics|41979|6|Mentioned|p522|||||||||
6639|Fiery Creek Volcanics|42565|5|Briefly described|Table 1 P5, P4|||||||||
6639|Fiery Creek Volcanics|43595|5|Briefly described|p440-1|||U-Pb Zircon age: 1678+/-3 Ma||||||
6639|Fiery Creek Volcanics|43616|6|Mentioned|p4|||Age 1680 Ma.||||||23-DEC-08
6639|Fiery Creek Volcanics|45166|5|Briefly described|p26|||||||||
6639|Fiery Creek Volcanics|46960|6|Mentioned|p215|||||||||
6639|Fiery Creek Volcanics|47083|4|Described|p11||Proterozoic|Comagmatic with Weberra Volcanics. Unconformably overlain by Surprise Crk Fm, Mt Isa and McNamara Groups. Unconformably overlies Haslingden Gp and Quilalar Fm. Max thick: 250 m.||||||18-SEP-06
6639|Fiery Creek Volcanics|49041|5|Briefly described|Table 1|||||||||
6639|Fiery Creek Volcanics|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
6639|Fiery Creek Volcanics|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Suite. Age: 1709 +/-3Ma (Shrimp).||||||07-NOV-08
6639|Fiery Creek Volcanics|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1708 Ma. Conformably overlies Bigie Formation. Overlain by Surprise Creek Formation at a syn-rift unconformity. Geological Province: Western Fold Belt.||||||24-JAN-22
6639|Fiery Creek Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
6639|Fiery Creek Volcanics|60558|5|Briefly described|p4 Fig. 3, p12|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
6639|Fiery Creek Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
6639|Fiery Creek Volcanics|61924|5|Briefly described|p44|||||||||
6639|Fiery Creek Volcanics|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1708+/-2Ma. ||||||07-NOV-08
6639|Fiery Creek Volcanics|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Intercalated with the Bigie Formation. Age: 1709+/-3Ma. Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
6639|Fiery Creek Volcanics|62535|5|Briefly described|p672|Statherian|Statherian||1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Age: 1709+/-3Ma. (Page and Sweet 1998). Geological Province: Calvert Superbasin (Mount Isa Inlier).||||||07-NOV-08
6639|Fiery Creek Volcanics|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ca 1710Ma. Geological Province: Calvert Superbasin. See also p1034.||||||07-NOV-08
6639|Fiery Creek Volcanics|63109|6|Mentioned|p1108, p1108 Fig. 3, p1111|||Overlain by Surprise Creek Formation, underlain by Bigie Formation. Consists of mafic volcanics rocks. Geological Province: Leichhardt and Calvert Superbasin.||||||
6639|Fiery Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
6639|Fiery Creek Volcanics|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Surprise Creek Formation, underlain by Bigie Formation. Age: ~1709Ma (U/Pb zircon ages). Geological Province: Calvert Superbasin. Consists of volcanic rocks.||||||07-FEB-11
6639|Fiery Creek Volcanics|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Big supersequence||Overlies Bigie Formation. Is overlain by Surprise Creek Formation.||
6639|Fiery Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1281, p1290, |||Calvert superbasin. High-permeability aquifer.||||||
6639|Fiery Creek Volcanics|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Calvert superbasin. Material properties detailed.||||||
6639|Fiery Creek Volcanics|63866|5|Briefly described|p57-p58, p61|Statherian|Statherian|Calvert Superbasin.|1709 +/- 3 Ma (Page and Sweet, 1998)|||(Possibly) coeval with the Bigie Formation. Possibly equivalent to the Deighton Quartzite.||
6639|Fiery Creek Volcanics|64250|6|Mentioned|p19, p25 fig 10, p11 fig 3, p21, p24|||Western Fold Belt, Mount Isa Inlier. Co-magmatic with Weberra Granite.|1709 +/- 3 Ma||||Bimodal volcanics.|
6639|Fiery Creek Volcanics|64575|6|Mentioned|p656, p664|||||||||
6639|Fiery Creek Volcanics|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
6639|Fiery Creek Volcanics|64726|6|Mentioned|p83 Fig.2.|||||||||
6639|Fiery Creek Volcanics|64744|6|Mentioned|p353 Fig.4, p354. |Statherian|Statherian|Mount Isa Basin. Bimodal volcanics.|1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
6639|Fiery Creek Volcanics|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin. Shown as Fiery Ck. Volcs.|||||Volcanics.|
6639|Fiery Creek Volcanics|65228|5|Briefly described|Figs.04, 10.|Statherian|Statherian|Mount Isa area. Part of the Big Supersequence.|1709 +/- 3 Ma (Page et al. 2000).|||||
6639|Fiery Creek Volcanics|65337|6|Mentioned|p5. |||Calvert Superbasin. Correlative of Carrara Range Group.||||||
6639|Fiery Creek Volcanics|65396|5|Briefly described|p16, p82, p175, p187, p190, p193|Statherian|Statherian|See also p195-197, p241. Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt. Co-magmatic with Weberra Granite. Formations with detrital zircons from this unit are listed.|1709 +/- 3 Ma|||Overlies Bigie Formation.|Felsic and mafic volcanics.|
6639|Fiery Creek Volcanics|65887|5|Briefly described|p52|Statherian|Statherian|Mount Isa Western Succession. Metatholeiites. ~1710 Ma.||||||09-JUN-15
6639|Fiery Creek Volcanics|66529|6|Mentioned|p3|||Calvert Superbasin.|~1709 Ma|||||
6639|Fiery Creek Volcanics|66824|6|Mentioned|p148|||||||Overlies Bigie Formation. Is overlain unconformably by Surprise Creek Formation. With Bigie Formation, equivalent to Carter's Bore Rhyolite.||
6639|Fiery Creek Volcanics|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1709 +/- 2 Ma (Page et al. 2000).|||||24-APR-12
6639|Fiery Creek Volcanics|67323|4|Described|p9-11, p13, p24-25, p33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Bimodal volcanism associated with extension of the Calvert Superbasin. Mount Oxide Domain, Mount Isa Inlier. Age significantly younger than Peters Creek Volcanics. Shown as two parts, mafic ~10 my older than felsic, on both Time-Space Plots.|1709 +/- 3 Ma (felsic: Page & Sweet 1998).|Of Big Supersequence.||Coeval with Weberra Granite. Unconformably overlain by Surprise Creek Formation. Overlies Bigie Formation.|Reddish brown, grey and black vesicular volcanics, grey porphyritic volcanics, purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|68021|5|Briefly described|p135 fig 4, p136, 138|Statherian|Statherian|Part of Big Supersequence, Calvert Superbasin, Western Succession.|1710 Ma|||Overlies Bigie Formation?, Quilalar Formation, overlain by Surprise Creek Formation.|?Bimodal volcanics.|
6639|Fiery Creek Volcanics|68146|5|Briefly described|p6, p188-193|||Informal name. Mount isa Region. Sample did not yield results; zircons are interpreted as either xenocrysts and/or geological sampling contamination.||||Is overlain by Surprise Creek Formation or Torpedo Creek Quartzite.|(Weathered) brick-red rhyolite or rhyodacite, containing a very fine-grained matrix with prominent glassy quartz "eyes"; local flow layering.|
6639|Fiery Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Bigie Formation under the symbol, -Pf.||||||
6639|Fiery Creek Volcanics|68575|6|Mentioned|p40|||||||Upper part may be equivalent to the Bularnu Formation.||
6639|Fiery Creek Volcanics|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Of the Big Supersequence. Igneous crystallisation age.|1709 +/- 3 Ma|||||
6639|Fiery Creek Volcanics|69056|5|Briefly described|p2, p54|||Mount Isa Western Succession; Calvert Superbasin. Mapped as one unit with Bigie Formation Volcanics.|||||Local bimodal volcanism.|
6639|Fiery Creek Volcanics|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the Mount Isa Rift Event.|1708 +/- 2 Ma (Page and Sweet, 1998).|||Overlies Quilalar Formation, overlain by Carters Bore Rhyolite|Felsic volcanic rocks.|
6639|Fiery Creek Volcanics|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intertongues with Bigie Formation.||25-JAN-19
6639|Fiery Creek Volcanics|69591|5|Briefly described|p29, p37-39, p56, p106|Paleoproterozoic|Paleoproterozoic|Jackson, Scott and Rawlings (2000). Mount Oxide, Leichhardt River Domains, Calvert Superbasin. Part of the Big Supersequence. Bimodal felsic and highly altered mafic volcanics. Coeval with the ~1710 Ma Weberra Granite. May be the source of ~1712 Ma detrital zircons in Roxmere Quartzite. Jackson et al. (2005) dated this unit at 1701 +/- 23 Ma.|1709 +/- 3 Ma (Page and Sweet, 1998).|||Correlated with basal Deighton Quartzite.|Reddish-brown, grey and black vesicular volcanics, grey porphyritic volcanics, purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70282|5|Briefly described|p544 table 1|||Cover sequence 3, Mount Isa.|1710-1709 Ma|||Overlies Bigie Formation|Bimodal volcanics.|13-FEB-18
6639|Fiery Creek Volcanics|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Reddish-brown, grey and black vesicular metabasalt and trachybasalt, locally porphyritic; purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Reddish-brown, grey and black vesicular metabasalt and trachybasalt, locally porphyritic; purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.|1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1709+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
6639|Fiery Creek Volcanics|71799|5|Briefly described|p150 fig 2, p153 tbl 1|Statherian|Statherian|Lawn Hill. Age is derived from SHRIMP U-Pb magmatic ages (not provided) derived from Page et al, 2000 and from Page, 1983. Geochemistry is discussed. See also p154, p156, p157 fig 5, p158.|1710-1705 Ma|||Overlies the Bigie Formation. Overlain by the Prize Supersequence.|Basalt, dolerite, gabbro or amphibolite.|
6639|Fiery Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown with Bigie Formation, as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Unclear whether this unit or Bigie Fm was dated. Age given as U-Pb zircon igneous crystallisation age.|1709 +/-3 Ma|||Shown as overlying Carrara Range Group and shown as unconformably underlying Surprise Creek Formation.||
6639|Fiery Creek Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
6639|Fiery Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Shown with Bigie Formation. Lateral equivalents? Located in the  Leichhardt River Fault Trough, the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1709 +/- 3 Ma|||Shown as unconformably overlying Quilalar Formation, Carrara Range Group and unconformably underlies Surprise Creek Formation.|Bimodal volcanics.|
6639|Fiery Creek Volcanics|73042|6|Mentioned|p4|Statherian|Statherian|Written as Fiery Creek Vol/Bigie Fm on chronostratigraphic diagram (Fig.1.2). South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age (although it is unclear whether this age is from the Fiery Creek Volcanics or Bigie Formation(?), or if these two units can be distinguished from one another).|1709 +/- 3 Ma (see comments and Fig.1.2)|||Unconformably overlain(?) by Surprise Creek Formation. Equivalent to Bigie Formation(?).||
6639|Fiery Creek Volcanics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
6639|Fiery Creek Volcanics|73144|6|Mentioned|p9-10|||Calvert Superbasin. Part of the Big Supersequence.||||Partly interbedded with Bigie Formation.|Includes banded rhyolite flows.|
6639|Fiery Creek Volcanics|73412|6|Mentioned|p20|||Western Succession of the Mount Isa Inlier. Contains potassic alteration assemblages, interpreted as regional fluid flow associated with Zn-Pb-Ag metallogenesis.||||||
6639|Fiery Creek Volcanics|73525|5|Briefly described|p4, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1709+/-3 Ma crystallisation age||||Mafic extrusives with clastics, and felsic extrusives.|
6665|Finlayson Granite|23423|5|Briefly described|p249|||||||||
6665|Finlayson Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
6665|Finlayson Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
6665|Finlayson Granite|31435|6|Mentioned|p17|||||||||
6665|Finlayson Granite|31500|5|Briefly described|p57|||||||||
6665|Finlayson Granite|31832|6|Mentioned|Table 6|||||||||
6665|Finlayson Granite|36527|6|Mentioned|p164|||||||||
6665|Finlayson Granite|37614|6|Mentioned|p240|||||||||
6665|Finlayson Granite|37633|6|Mentioned|Table 38|||||||||
6665|Finlayson Granite|39252|6|Mentioned|p26|||See also P28||||||
6665|Finlayson Granite|39445|5|Briefly described|Table 12|||||||||
6665|Finlayson Granite|39845|6|Mentioned|p24|||||||||
6665|Finlayson Granite|42490|5|Briefly described|p14|||||||||
6665|Finlayson Granite|42658|6|Mentioned|p27|||||||||
6665|Finlayson Granite|43070|2|Defined|p46|Late Permian||of Cooktown Supersuite||||||
6665|Finlayson Granite|43111|6|Mentioned|p1|||||||||
6665|Finlayson Granite|43896|14|Not recorded|Map Legend||Permian|||||||
6665|Finlayson Granite|43979|14|Not recorded|p66(map),67,68||Permian|||||||
6665|Finlayson Granite|44258|14|Not recorded|p1,5,11,12,15,32||Late Permian|247+/-6 Ma.||||||
6665|Finlayson Granite|44259|14|Not recorded|p109|||247+/-6 Ma||||||
6665|Finlayson Granite|44267|14|Not recorded|Map Legend||Permian|||||||
6665|Finlayson Granite|44292|2|Defined|Tb.opp.p8,map||Permian|Correlated with Mareeba Granite. Intrudes Hodgkinson Formation.||||||
6665|Finlayson Granite|44293|14|Not recorded|Map Legend||Permian|||||||
6665|Finlayson Granite|44294|2|Defined|Tb.2,opp.p10,p11,map|||Adamellite.||||||
6665|Finlayson Granite|45025|4|Described|p78,anal.p85||Permian|||||||
6665|Finlayson Granite|45087|5|Briefly described|p13|||Chemical analyses.||||||
6665|Finlayson Granite|45113|3|Fully described|p22|||Emphasis on petrography.||||||
6665|Finlayson Granite|48894|6|Mentioned|p59|||246my||||||
6665|Finlayson Granite|48976|6|Mentioned|p77|||||||||
6665|Finlayson Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic, cordierite(altered)-biotite granite.||||||06-JUL-04
6665|Finlayson Granite|60425|4|Described|p91, p270-1 Appdx. 1|Late Permian|Late Permian|Of Mount Poverty Suite (Cooktown Supersuite). White, med.-gr., seriate to mod'ly porphyritic (altered cordierite?)-tourmaline-biotite granite; accessory muscovite; extensively altered; S-type. Formerly contained granites of Yates and Cooktown Supersuites||||||07-FEB-11
6665|Finlayson Granite|69592|6|Mentioned|p249 Fig.4.34|Permian|Permian|Time-space diagram of Kennedy Igneous Association granitoids relative to Permian deformation in the Palmer-Barron Subprovince.||||||
6665|Finlayson Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Poverty Suite.|||S-type granitoids.|
6674|First Branch Creek Sandstone|24076|5|Briefly described|p397 Fig. 2|Middle Devonian|Middle Devonian|Max. thickness: 800m.  Geological Province: Yarrol Basin.||||||
6674|First Branch Creek Sandstone|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
6674|First Branch Creek Sandstone|33774|3|Fully described|p12|||||||||
6674|First Branch Creek Sandstone|33905|6|Mentioned|p265|||||||||
6674|First Branch Creek Sandstone|36333|6|Mentioned|Map legend|Middle Devonian|Early Devonian|||||||15-JUL-04
6674|First Branch Creek Sandstone|39445|5|Briefly described|Table 5|||||||||
6674|First Branch Creek Sandstone|42031|5|Briefly described|Fig.3 P759|||||||||
6674|First Branch Creek Sandstone|42868|5|Briefly described|p28|||||||||
6674|First Branch Creek Sandstone|43008|5|Briefly described|map legend|||||||||
6674|First Branch Creek Sandstone|61761|6|Mentioned|p4|||Consists of lithic and feldspathic sandstone.||||||07-FEB-11
6674|First Branch Creek Sandstone|68679|5|Briefly described|p317|Middle Devonian|Middle Devonian|Driscoll (1960). Northern Philpott Subprovince.|||||Mainly basaltic and andesitic volcaniclastics with some possible lava and lesser lithic sandstone, mudstone and limestone.|
6682|Fish River Formation|22673|6|Mentioned|66 fig 3|||||||||
6682|Fish River Formation|22680|5|Briefly described|84 fig 2, 85,86|||Geol province Mount Isa Basin. Of theFickling Group.||||||18-SEP-06
6682|Fish River Formation|23065|6|Mentioned|16|||Geol province Lawn Hill Subprovince. Parent Fickling Group. Overlying unit Walford Dolomite.||||||
6682|Fish River Formation|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||18-SEP-06
6682|Fish River Formation|23397|5|Briefly described|p463|||Of Fickling Group.||||||18-SEP-06
6682|Fish River Formation|23398|4|Described|p445|Statherian|Statherian|Age: ~1770Ma||||||18-SEP-06
6682|Fish River Formation|23406|4|Described|p608, p609 Fig. 9|||Of Fickling Group. Parts in both Gun and Prize Supersequences. Lithological details included in Fig. 9.||||||16-JUN-09
6682|Fish River Formation|31421|6|Mentioned|p509|||||||||
6682|Fish River Formation|32660|5|Briefly described|Table 5|||||||||
6682|Fish River Formation|35114|6|Mentioned|p202|||||||||
6682|Fish River Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|36012|3|Fully described|Table 3|||See also p16.||||||18-SEP-06
6682|Fish River Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|37568|6|Mentioned|Fig.5|||||||||
6682|Fish River Formation|38237|6|Mentioned|p126|||||||||
6682|Fish River Formation|38584|4|Described|p17|||||||||
6682|Fish River Formation|39445|5|Briefly described|Table 2|||See also p36 and p39.||||||18-SEP-06
6682|Fish River Formation|39497|6|Mentioned|Fig.4|||||||||
6682|Fish River Formation|39685|6|Mentioned|p407|||||||||
6682|Fish River Formation|39944|6|Mentioned|Fig.5|||||||||
6682|Fish River Formation|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
6682|Fish River Formation|41721|4|Described|p28|||||||||
6682|Fish River Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
6682|Fish River Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Fickling Group. Of "Mid Proterozoic" age.||||||18-SEP-06
6682|Fish River Formation|44305|14|Not recorded|p.13|||(E53-8). opp.6,18.||||||
6682|Fish River Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
6682|Fish River Formation|44482|14|Not recorded|p.8|||(E53-12).||||||
6682|Fish River Formation|45162|6|Mentioned|p147|||||||||
6682|Fish River Formation|45166|5|Briefly described|p30|||||||||
6682|Fish River Formation|46804|6|Mentioned|p154|||||||||
6682|Fish River Formation|49001|2|Defined|p8|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Overlian by Walford Dolomite, underlain by Peters Creek Volcanics.||||||
6682|Fish River Formation|63111|5|Briefly described|p1162, p1164 Tb. 1|Statherian|Statherian|Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
6682|Fish River Formation|63866|5|Briefly described|p56|||Calvert and Isa Superbasins.||||Equivalent to the Prize Supersequence.||
6682|Fish River Formation|65337|6|Mentioned|p30.|||||Basal unit in Fickling Group.||||
6682|Fish River Formation|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map,Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Isa Superbasin. Listed as unit within the McNamara Group on p26 and p34. Shown as Lower and Upper Fish River Formation on both Time-Space Plots. MDA of 1715 +/- 11 Ma.|~1660-1650 Ma.|Fickling Group.|||Medium orthoquartzite|
6682|Fish River Formation|69433|4|Described|p18:2-4|Statherian|Statherian|Northern succession, Lawn Hill Platform. 10m to over 200m thick; c.250m in the type section in WESTMORELAND map area. Fluvial to shallow-marine tidal flat deposits. Age from detrital zircons (Page et al., 2000).|<1770 Ma (maximum deposition age).|Basal Fickling Group.||Unconformably overlies Peters Creek Volcanics. Is overlain conformably by Walford Dolostone.|Mainly sandstone: medium-grained, quartz-rich, with ripple marks, mudcracks and herringbone cross-strata; siltstone; and conglomerate lenses, with clasts derived from Wire Creek Sandstone, Peters Creek Volcanics and (?)Cliffdfale Volcanics.|12-JUL-16
6682|Fish River Formation|69591|5|Briefly described|p40, p42-43, p55|||Camooweal-Murphy Domain. S of Murphy Tectonic Ridge. Lower part was deposited during late Calvert time, with the upper part during Isa Superbasin time. Part of Loretta Supersequence. Fluvial/coastal deposits.|||||Medium orthoquartzite.|
6682|Fish River Formation|69673|5|Briefly described|p52 fig 42, p53 |||Maximum thickness of 200m. Deposited in shallow marine to tidal flat environment.||Fickling Group|||Sandstone with conglomerate lenses.|
6682|Fish River Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Unconformably overlies Peters Creek Volcanics (Tawallah Group equivalent). Is overlain by Walford Dolostone.|Sandstone, fine- to coarse-grained, flaggy to massive; minor conglomerate and siltstone.|
6682|Fish River Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1771+/-24 Ma (MDA: U-Pb zircon SHRIMP)||||Tuffite.|
6682|Fish River Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin.||Fickling Group||Shown as partially overlying Weberra Granite and Nicholson Granite Complex and underlies Walford Dolomite.||
6682|Fish River Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin.||Fickling Group||Underlies Walford Dolomite and is partially equivalent to Drummond Formation, Brumby Formation and Bullrush Conglomerate.|Includes dolostone.|
6682|Fish River Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin.||Fickling Group||Underlies Walford Dolomite.|Includes dolostone.|
6682|Fish River Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||Fickling Group||Overlain by Walford Dolomite.||
6684|Fish Seale Marker Bed|38446|6|Mentioned|p171|||||||||
6684|Fish Seale Marker Bed|39495|6|Mentioned|p142|||||||||
6731|Flat Top Formation|13516|6|Mentioned|p145 fig 3|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5004||||||
6731|Flat Top Formation|22439|5|Briefly described|p15, Fig.2|Late Permian|Late Permian|Taroom Trough, Bowen Basin.||||||
6731|Flat Top Formation|22973|5|Briefly described|p11 Fig.2(f)|Late Permian|Late Permian|||||||
6731|Flat Top Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
6731|Flat Top Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
6731|Flat Top Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
6731|Flat Top Formation|23037|6|Mentioned|p65,9||Permian|Part of the Back Creek Group.||||||
6731|Flat Top Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
6731|Flat Top Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbf].  Siltstone, sandstone, mudstone, conglomerate, tuff.||||||
6731|Flat Top Formation|29437|6|Mentioned|p136|||Permian||||||
6731|Flat Top Formation|29440|6|Mentioned|p37|||||||||
6731|Flat Top Formation|30141|5|Briefly described|p134|||||||||
6731|Flat Top Formation|30449|6|Mentioned|p2|||Brachiopods. See also P4,6,8,13,19||||||
6731|Flat Top Formation|30450|6|Mentioned|Table 1|||Permian age. Southeast Bowen Basin||||||
6731|Flat Top Formation|30451|3|Fully described|p57|||||||||
6731|Flat Top Formation|30546|6|Mentioned|p107|||Correlation. Upper Permian age. See also P116||||||
6731|Flat Top Formation|30743|6|Mentioned|p24|||Geological map||||||
6731|Flat Top Formation|30916|6|Mentioned|p98|||||||||
6731|Flat Top Formation|31079|6|Mentioned|Fig. 6|||||||||
6731|Flat Top Formation|31396|6|Mentioned|p1185|||||||||
6731|Flat Top Formation|31659|6|Mentioned|p68|||U.Permian||||||
6731|Flat Top Formation|32141|6|Mentioned|p154|||||||||
6731|Flat Top Formation|32577|6|Mentioned|p23|||Blenheim Sub Gp.||||||
6731|Flat Top Formation|32944|6|Mentioned|p710|||See also Fig.3 Permian||||||
6731|Flat Top Formation|32945|6|Mentioned|p90|||See also P91||||||
6731|Flat Top Formation|33436|6|Mentioned|p2371|||Fauna.||||||
6731|Flat Top Formation|33711|6|Mentioned|Table 3|||||||||
6731|Flat Top Formation|33774|3|Fully described|p37|||||||||
6731|Flat Top Formation|34132|6|Mentioned|p2|||Upper Permian||||||
6731|Flat Top Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
6731|Flat Top Formation|34475|6|Mentioned|p255|||See also P262||||||
6731|Flat Top Formation|35284|6|Mentioned|Fig.1|||||||||
6731|Flat Top Formation|35426|3|Fully described|p658|||||||||
6731|Flat Top Formation|35845|6|Mentioned|Fig.25|||||||||
6731|Flat Top Formation|35873|6|Mentioned|p125|||||||||
6731|Flat Top Formation|36243|6|Mentioned|Table 4A|||||||||
6731|Flat Top Formation|36333|6|Mentioned|Map legend|Late Permian|Late Permian|Of the Back Creek Group.||||||15-JUL-04
6731|Flat Top Formation|36739|6|Mentioned|Fig.2|||||||||
6731|Flat Top Formation|36740|6|Mentioned|p4|||||||||
6731|Flat Top Formation|36794|6|Mentioned|p388|||||||||
6731|Flat Top Formation|36925|6|Mentioned|p179|||||||||
6731|Flat Top Formation|37075|5|Briefly described|Table 1|||||||||
6731|Flat Top Formation|37858|6|Mentioned|p82|||||||||
6731|Flat Top Formation|38204|4|Described|p76|||||||||
6731|Flat Top Formation|38444|6|Mentioned|p302|||||||||
6731|Flat Top Formation|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6731|Flat Top Formation|38917|6|Mentioned|p167|||||||||
6731|Flat Top Formation|39212|5|Briefly described|p12|||||||||
6731|Flat Top Formation|39252|5|Briefly described|p20|||See also Fig.13||||||
6731|Flat Top Formation|39261|6|Mentioned|p112|||See also Fig.6||||||
6731|Flat Top Formation|39267|6|Mentioned|p238|||See also P240||||||
6731|Flat Top Formation|39268|6|Mentioned|p270|||||||||
6731|Flat Top Formation|39445|5|Briefly described|Table 8|||||||||
6731|Flat Top Formation|39943|6|Mentioned|Table 6A|||||||||
6731|Flat Top Formation|40093|4|Described|p33|||||||||
6731|Flat Top Formation|40539|6|Mentioned|Fig.2|||||||||
6731|Flat Top Formation|41246|6|Mentioned|Map legend|Permian||||||||
6731|Flat Top Formation|41639|6|Mentioned|p7|||||||||
6731|Flat Top Formation|41666|6|Mentioned|p1|||||||||
6731|Flat Top Formation|41736|6|Mentioned|p119|||||||||
6731|Flat Top Formation|41809|6|Mentioned|p64|||||||||
6731|Flat Top Formation|42249|6|Mentioned|p22|||||||||
6731|Flat Top Formation|42250|6|Mentioned|Fig.4 P31|||||||||
6731|Flat Top Formation|42641|6|Mentioned|Fig.3 P110|||||||||
6731|Flat Top Formation|42865|5|Briefly described|p18|||||||||
6731|Flat Top Formation|42994|6|Mentioned|p273|||||||||
6731|Flat Top Formation|43000|5|Briefly described|p113|||see also Fig.5,p112||||||
6731|Flat Top Formation|43017|5|Briefly described|Fig.3,p375|||||||||
6731|Flat Top Formation|43050|5|Briefly described|p4|||||||||
6731|Flat Top Formation|43185|6|Mentioned|6,9||Late Permian|||||||
6731|Flat Top Formation|43471|14|Not recorded|p247-249,252|||Megadesmus, Astartila||||||
6731|Flat Top Formation|43474|14|Not recorded|p7,10,52,66,73-4,104||Kazanian|p108||||||
6731|Flat Top Formation|43475|14|Not recorded|p553,555||Permian|||||||
6731|Flat Top Formation|43483|6|Mentioned|14||Permian|||||||
6731|Flat Top Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
6731|Flat Top Formation|43894|14|Not recorded|p791|||||||||
6731|Flat Top Formation|43987|14|Not recorded|p267,269,270|||||||||
6731|Flat Top Formation|43994|14|Not recorded|Map Legend|||||||||
6731|Flat Top Formation|44079|14|Not recorded|p50|||||||||
6731|Flat Top Formation|44118|14|Not recorded|Map Legend||Late Permian|||||||
6731|Flat Top Formation|44169|2|Defined|Tb.1,p8,map|||||||||
6731|Flat Top Formation|44170|4|Described|p6,8-11,13,Tb.1,map||Late Permian|||||||
6731|Flat Top Formation|44218|14|Not recorded|p19||Kazanian|||||||
6731|Flat Top Formation|44243|14|Not recorded|p649,map||Late Permian|||||||
6731|Flat Top Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
6731|Flat Top Formation|44347|14|Not recorded|p77|||||||||
6731|Flat Top Formation|44348|14|Not recorded|p56|||||||||
6731|Flat Top Formation|44350|14|Not recorded|p52|||||||||
6731|Flat Top Formation|44381|14|Not recorded|p6|||||||||
6731|Flat Top Formation|44424|14|Not recorded|p293-301|||||||||
6731|Flat Top Formation|44426|14|Not recorded|p11|||||||||
6731|Flat Top Formation|44427|14|Not recorded|p159,160,163-165|||Theodore-Banana area.||||||
6731|Flat Top Formation|44489|14|Not recorded|p72|||||||||
6731|Flat Top Formation|44490|14|Not recorded|p46-48|||Fossils.||||||
6731|Flat Top Formation|44514|2|Defined|p27,30,33||Permian|Overlies Barfield Formation and Station Mudstone N of Fault.(Middle Permian).||||||27-OCT-08
6731|Flat Top Formation|44571|2|Defined|p205,206,Fig.28|||||||||
6731|Flat Top Formation|44573|14|Not recorded|p98|||To include part of Banana Formation.||||||
6731|Flat Top Formation|44640|14|Not recorded|p31|||||||||
6731|Flat Top Formation|45006|14|Not recorded|Tb.1,p6,97,101,103|||p106,120||||||
6731|Flat Top Formation|45031|14|Not recorded|p9,Fig.3||Permian|||||||
6731|Flat Top Formation|45071|3|Fully described|Table 10|||||||||
6731|Flat Top Formation|46949|6|Mentioned|Fig.3|||||||||
6731|Flat Top Formation|48600|14|Not recorded|p32|||||||||
6731|Flat Top Formation|48898|6|Mentioned|p25|||||||||
6731|Flat Top Formation|48900|6|Mentioned|p84|||Table opposite||||||
6731|Flat Top Formation|48919|4|Described|p26|||See also p27. Upper Permian.||||||06-FEB-08
6731|Flat Top Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Back Creek Group. Siltstone, lithic sandstone, mudstone, conglomerate and minor coquinitic sandy limestone and tuff.||||||18-JUN-09
6731|Flat Top Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Back Creek Group. Siltstone, lithic sandstone, mudstone, conglomerate and minor coquinitic sandy limestone and tuff.||||||
6731|Flat Top Formation|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Back Creek Group.  Buff to bluish-grey mudstone, buff siltstone, lithofeldspathic sandy siltstone and sandstone.||||||09-JUN-04
6731|Flat Top Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
6731|Flat Top Formation|60282|5|Briefly described|p7|||Uppermost part of the Back Creek Group. Lithic sandstone and mudstone.  Overlies the Barfield Formation; overlain by Gyranda Formation, the lowermost part of the Backwater Group.  Geological Province: Bowen Basin.||||||
6731|Flat Top Formation|60330|5|Briefly described|p259|Late Permian|Late Permian|Includes grey-brown fossiliferous calcarenites; grey fossiliferous, limy mudstones. Contains foraminferida. Geological Province: Bowen Basin.||||||27-OCT-08
6731|Flat Top Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
6731|Flat Top Formation|61778|5|Briefly described|p239||Late Permian|Geological Province: Bowen Basin.||||||07-FEB-11
6731|Flat Top Formation|61782|5|Briefly described|p280|||Of Blenheim Subgroup. Contains carbonates as well as tuffs and andesite.||||||
6731|Flat Top Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
6731|Flat Top Formation|64856|3|Fully described|p42, p49, p53-55, p57 Fig.8|Late Permian|Late Permian|Derrington et al. (1959). Bowen Basin. Informally subdivided into 3 unnamed parts. Conformably overlies the Barfield Formation. Age from palynoflora (unit APP5). Max thickness 494m. Predominantly siltstone with lesser sandstone, shale, conglomerate, tuff and coal.| | ||||28-NOV-17
6731|Flat Top Formation|64857|4|Described|p118-119, p113 Fig.3, p115|Late Permian|Late Permian|Taroom Trough, Bowen Basin. Sandstone dominated unit overlying Barfield Formation.||||||
6731|Flat Top Formation|64858|5|Briefly described|p181, p180 Fig.2, p183 Fig. 4, p191|Late Permian|Late Permian|Bowen Basin. Includes coals.||||||30-NOV-09
6731|Flat Top Formation|64859|6|Mentioned|p196, 225|Permian|Permian|Gas source rocks.||||||
6731|Flat Top Formation|65112|6|Mentioned|p316; Fig 4 p314|Triassic|Late Permian|Post-extension stratigraphic sequences of the Taroom Trough. Overlies Barfield Formation, underlies Banana Formation.||||||22-MAR-12
6731|Flat Top Formation|65113|5|Briefly described|p349, Fig 4 p340|Late Permian|Late Permian.|In the Taroom Trough, Overlies the Barfield Formation, underlies the Banana Formation.||||||
6731|Flat Top Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
6731|Flat Top Formation|65115|5|Briefly described|p414, 415, 416, Fig 2 p403|Kazanian|Ufimian|Coarse grained siltstone, fine grained sandstone and conglomerate. Underlies the Banana Formation and overlies the Barfield Formation in the Taroom Trough, Bowen Basin. Part of Supersequence D.||||||
6731|Flat Top Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|?Underlies the Banana Formation and ?overlies the Barfield Formation in the Taroom Trough, Bowen Basin.||||||
6731|Flat Top Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|?Underlies the Banana Formation, ?overlies the Barfield Formation in the Taroom Trough, Bowen Basin.||||||
6731|Flat Top Formation|65119|6|Mentioned|p504 Table 1, Fig 4-6, Fig 9-10|Late Permian|Late Permian|Age: 252-253 Ma. Present in the Cockatoo Creek 1, Burunga 1 Wells.||||||07-MAR-12
6731|Flat Top Formation|65388|4|Described|p170-172, p161 Fig. 62, p163, 194, 437|Late Permian|Roadian|Of Back Creek Group, Bowen Basin. Succession of feldspatholithic sandstone, mudstone and minor limestone overlying the Station Mudstone Member north-east of the Banana Fault and the Barfield Formation conformably. Overlain by Banana Formation, Gyranda Formation? 400-610m. Fossils indicate late Permian (Kazanian) age to APP5 (Tatarian)||||||
6731|Flat Top Formation|66615|6|Mentioned|p2 Fig.1, p9|||Southern Taroom Trough, Bowen Basin.||||||
6731|Flat Top Formation|67402|6|Mentioned|p21, p45|Capitanian|Capitanian|Bowen Basin. ||||Overlain by the Burunga Formation. Overlies the Oxtrack Formation.||
6731|Flat Top Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Gyranda Formation. Underlain by Barfield Formation.||
6731|Flat Top Formation|68679|5|Briefly described|p350, p353, p377, p380-382|Permian|Permian|Derrington et al. (1959). Taroom Trough, Bowen Basin. 660m thick. Fan delta, shallow-marine deposits. Mentioned as having the same fossil species as, and thus establishing the age of, the Warminster Formation (Yarrol Province).||||Overlies Barfield Formation. Is overlain by Banana Formation. May correlate with the Boomer Formation.|Siltstone, sandstone, shale, conglomerate and coal with minor tuff; marine fossils.|
6731|Flat Top Formation|70940|5|Briefly described|p844|Permian|Permian|Burunga Anticline, southern Bowen Basin.|c.259-256 Ma.|Blackwater Group.||Is overlain by Gyranda Formation.||
6731|Flat Top Formation|71276|5|Briefly described|p294, p296-297|Permian|Permian|Olgers et al. (1966). Bowen Basin. Marine deposits. The authors state that this unit, with the German Creek Formation, "become the lower part of the Moranbah Coal Measures (Koppe, 1978) in the northern Bowen Basin"[?].||||Passes laterally into Catherine Sandstone.||
6731|Flat Top Formation|72297|6|Mentioned|p744-745|||Bowen Basin. The best hydrocarbon reservoir in the northern Taroom Trough.||||||
6731|Flat Top Formation|73305|6|Mentioned|p548 Fig.1|Late Permian|Late Permian|Bowen Basin. Taroom Trough, northeast.||||||
6731|Flat Top Formation|73450|6|Mentioned|p55|||Bowen Basin.||||||
6731|Flat Top Formation|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Taroom Trough, Eastern Bowen Basin.||||Overlies Barfield Formation. Is overlain by Baralaba Coal Measures.||
6753|Flinders Dolomite|32913|4|Described|p397|||||||||
6753|Flinders Dolomite|35032|6|Mentioned|p117|||||||||
6753|Flinders Dolomite|36779|6|Mentioned|p8|||||||||
6753|Flinders Dolomite|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6753|Flinders Dolomite|39445|5|Briefly described|Table 14|||||||||
6753|Flinders Dolomite|41906|3|Fully described|p29|||||||||
6753|Flinders Dolomite|42525|5|Briefly described|Map legend|Miocene|Paleocene|||||||
6753|Flinders Dolomite|61155|5|Briefly described|p19|Middle Eocene|Middle Eocene|Age: 46-42Ma. Thickness: 60m. In the Brisbane region.||||||03-MAR-10
6753|Flinders Dolomite|69599|5|Briefly described|p580, p586, p595|Eocene|Eocene|Crops out over a small area on Limestone Ridge, near Peak Crossing. Up to 60m thick. An important local agricultural lime source. Capped by silcrete and laterite.|||||Magnesian limestone.|
6767|Floraville Formation|22747|6|Mentioned|p6||Precambrian|||||||
6767|Floraville Formation|23065|5|Briefly described|18|||Geol province Karumba Basin||||||
6767|Floraville Formation|23393|5|Briefly described|p24|Eocene|Paleocene|||||||
6767|Floraville Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6767|Floraville Formation|24073|5|Briefly described|p378 Table 2|Cenozoic|Cenozoic|Formerly part of Lynd Formation?  Maximum thickness: 40m.  Geological Province: Carpentaria Basin.||||||19-NOV-08
6767|Floraville Formation|30095|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Upper Cretaceous - Tertiary||||||
6767|Floraville Formation|30582|6|Mentioned|p7|||||||||
6767|Floraville Formation|31433|4|Described|p6|||Upper Cretaceous-Tertiary||||||
6767|Floraville Formation|31434|3|Fully described|Table 1|||See also p9. U.Cretaceous-Tertiary||||||18-SEP-06
6767|Floraville Formation|31437|6|Mentioned|Map legend|Tertiary|Late Cretaceous|U.Cretaceous-Tertiary||||||
6767|Floraville Formation|33150|5|Briefly described|p13|||Possible equiv. Bulimba and Glendower Fms.||||||18-SEP-06
6767|Floraville Formation|33182|6|Mentioned|Fig.1|||Upper Cretaceous or Tertiary||||||
6767|Floraville Formation|33183|2|Defined|p227|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|34811|6|Mentioned|p5|||||||||
6767|Floraville Formation|35253|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|35640|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|36012|3|Fully described|Table 6|||See also p20.||||||18-SEP-06
6767|Floraville Formation|36228|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
6767|Floraville Formation|36439|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|36442|6|Mentioned|Map legend|early Tertiary|early Tertiary|||||||
6767|Floraville Formation|37607|5|Briefly described|p334|||See also Fig.5.||||||
6767|Floraville Formation|38584|4|Described|p21|||||||||
6767|Floraville Formation|39445|5|Briefly described|Table 14|||Early Tertiary. See also p150.||||||18-SEP-06
6767|Floraville Formation|39556|5|Briefly described|Map legend|Oligocene|Paleocene|Palaeocene to Oligocene||||||
6767|Floraville Formation|39797|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|40648|6|Mentioned|p12|||||||||
6767|Floraville Formation|41307|4|Described|p18|||||||||
6767|Floraville Formation|42637|6|Mentioned|p29|||||||||
6767|Floraville Formation|45145|5|Briefly described|p33|||See also Table 7.||||||
6767|Floraville Formation|46802|6|Mentioned|p135|||||||||
6767|Floraville Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6767|Floraville Formation|61155|5|Briefly described|p16|Eocene||Together with Louisa and Bulimba Formations thickness is 140m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
6767|Floraville Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleogene|Paleogene|Age: Early Tertiary?|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone.|
6767|Floraville Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Glendower, 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.||||||
6767|Floraville Formation|69599|5|Briefly described|p580, p585, p602|Eocene|Paleocene|Carpentaria region. Capped by laterite and silcrete of the Tennant Creek Surface.||||Correlated with Fairview Gravel, Louisa and Bulimba Formations.||
6767|Floraville Formation|72421|4|Described|mapsheet|Paleogene|Paleogene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet. Subsurface unit, appears on schematic diagram only.|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone|10-DEC-19
6767|Floraville Formation|72422|4|Described|mapsheet|Eocene|Paleocene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone|
6786|Flyspeck Granodiorite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
6786|Flyspeck Granodiorite|22781|4|Described|p27|Paleozoic|Paleozoic|Flyspeck Supersuite||||||07-NOV-08
6786|Flyspeck Granodiorite|23420|4|Described|p 148 table 4.7|Early Devonian|Late Silurian|In the Flyspeck Supersuite. Intruded by Glen Garland Granodiorite, Two Rail Monzogranite and Ebagoola Granite.||||||10-DEC-19
6786|Flyspeck Granodiorite|30257|6|Mentioned|p286|||Dating P296||||||
6786|Flyspeck Granodiorite|32528|5|Briefly described|Table 2|||||||||
6786|Flyspeck Granodiorite|32563|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
6786|Flyspeck Granodiorite|33529|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian - Early Devonian||||||
6786|Flyspeck Granodiorite|33772|4|Described|Table 1|||||||||
6786|Flyspeck Granodiorite|33773|4|Described|Table 1|||||||||
6786|Flyspeck Granodiorite|33880|6|Mentioned|Map legend|Middle Paleozoic|Middle Paleozoic|||||||07-NOV-08
6786|Flyspeck Granodiorite|34581|6|Mentioned|p130|||See also PP135,140. Devonian||||||
6786|Flyspeck Granodiorite|35204|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
6786|Flyspeck Granodiorite|35220|4|Described|Table 1|||||||||
6786|Flyspeck Granodiorite|37614|4|Described|p238|||||||||
6786|Flyspeck Granodiorite|39445|5|Briefly described|Table 12|||||||||
6786|Flyspeck Granodiorite|42464|6|Mentioned|p8|||||||||
6786|Flyspeck Granodiorite|42610|1|Redefined|p20|Early Devonian|Early Devonian|Age approx 400Ma.RDEF of B135 usage.||||||
6786|Flyspeck Granodiorite|42640|5|Briefly described|p10|||Called Flyspeck Supersuite on Ebagoola 1:250 000 sheet||||||
6786|Flyspeck Granodiorite|42650|5|Briefly described|p15|||Renamed as Flyspeck Supersuite in Ebagoola 1:250 000 sheet area||||||
6786|Flyspeck Granodiorite|43124|6|Mentioned|p28|||||||||
6786|Flyspeck Granodiorite|43708|4|Described|p8,14-17|||||||||
6786|Flyspeck Granodiorite|43725|5|Briefly described|p13-15|||U-Pb age: 406+/-10 Ma, 398+/-10 Ma||||||
6786|Flyspeck Granodiorite|43738|6|Mentioned|p51|||||||||
6786|Flyspeck Granodiorite|43811|6|Mentioned|Fig.1,p192,193|||||||||
6786|Flyspeck Granodiorite|44025|2|Defined|p349,351,353||Late Devonian|||||||
6786|Flyspeck Granodiorite|45076|3|Fully described|p89|||Anal.  p30.||||||10-DEC-19
6786|Flyspeck Granodiorite|49769|6|Mentioned|p4|||||||||
6786|Flyspeck Granodiorite|69592|5|Briefly described|p282, p288 Fig.4.84|||Cape York Peninsula Batholith. REE diagram.||Flyspeck Supersuite.|||I-type.|
6786|Flyspeck Granodiorite|71031|4|Described|p2, p26, p29, p32-p33|Early Devonian|Early Devonian|Intruded by a rhyolite plug dated at 281.6 +/- 3.9 Ma and a rhyolitic dyke dated at 394.3 +/- 3.1 (maximum intrusive age). Also possibly intruded by the Two Rail Monzogranite and the Barwon Granite. Intruded by unnamed dykes of rhyolitic, dacitic, andesitic and dioritic to doleritic composition.|406 +/- 10 Ma (SHRIMP, Black et al, 1992a,b)|||Intrudes the Coen Metamorphic Group. Intruded by the Ebagoola Granite and (probably) the Glen Garland Granodiorite.|fine- to coarse-grained strongly porphyritic hornblende-biotite granodiorite, grading into biotite monzogranite and biotite granite.|
6786|Flyspeck Granodiorite|71592|5|Briefly described|Appendix A.|||Palma Igneous Province.|406+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
6786|Flyspeck Granodiorite|71792|6|Mentioned|p50|||Rocks formerly mapped as belonging to this unit have in this volumed been included in the Wigan Granite on the basis of geophysical evidence.||||||
6786|Flyspeck Granodiorite|71849|6|Mentioned|p65, p115, p147, p170|||Trail et al. (1969), Whitaker and Gibson (1977). Part of this unit has been renamed the Rokeby Quartz Monzodiorite.||||||
6786|Flyspeck Granodiorite|72983|6|Mentioned|p46|Early Devonian|Early Devonian|||||Intruded by[?] Spion Kop rhyolite.||
6786|Flyspeck Granodiorite|73179|6|Mentioned|p1154|||||||||
6788|Focal Diorite Complex|40896|5|Briefly described|p53|||||||||
6788|Focal Diorite Complex|44778|14|Not recorded|p128,131-133|||(Post Triassic - pre Eocene-Oligocene)||||||
6788|Focal Diorite Complex|44781|14|Not recorded|p362|||||||||
6821|Fork Lagoons beds|22557|5|Briefly described|p568||Late Ordovician|||||||
6821|Fork Lagoons beds|23424|5|Briefly described|p345|||Probably correlate with Everetts Ck Volcanics and Carriers Well Fm. Anakie Province.||||||
6821|Fork Lagoons beds|23854|5|Briefly described|p858 Fig 1|Ordovician|Ordovician|Informal name.||||||
6821|Fork Lagoons beds|41246|6|Mentioned|Map legend|Ordovician||||||||
6821|Fork Lagoons beds|42611|6|Mentioned|p9|||Ordovician.||||||
6821|Fork Lagoons beds|42614|4|Described|p8|||||||||
6821|Fork Lagoons beds|42747|4|Described|p35, Fig.5|||||||||
6821|Fork Lagoons beds|42987|4|Described|p20|||||||||
6821|Fork Lagoons beds|43029|5|Briefly described|Fig.1,p13|||||||||
6821|Fork Lagoons beds|43204|5|Briefly described|Map Legend||Late Ordovician|Anakie Inlier||||||23-DEC-11
6821|Fork Lagoons beds|43213|2|Defined|p9, p11, p17, p19, p20, p22, p34, p46-51|Late Ordovician|Late Ordovician|See also p53-60, p65-66, p143-149, p184, p207, p237, p240, p245. Anderson and Palmieri (1977); Palmieri (1978). Type area described. Foliation is steeply dipping to vertical. Mylonite zones, locally containing foliated granite, mylonitised gabbro and serpentinite, may represent both thrust and strike slip faults. Contact with Anakie Metamorphic Group is a 1 km-wide zone of phyllonite, with slices of deformed granite and serpentinite. Includes rocks previously mapped as Anakie Metamorphics. Geochemistry, chemical analyses, deformation structures and lithology described in considerable detail. Correlated on conodont data with Carriers Well Formation (Broken River Province) and Mountain Creek Conglomerate (W Hodgkinson Province). Associated with gold deposits in Mount Clifford area. Appears as Fork Lagoon Beds on p237 and p240.||||Intruded by Taroborah Granodiorite. Probably thrust against Anakie Metamorphic Group. Overlain unconformably by Silver Hills Volcanics, Aldebaran Sandstone, Reids Dome beds, Red Mountain Formation.|Phacoidal quartzose arenite, and mudstone with a single slaty cleavage; locally contact metamorphosed to coarse micaceous rocks; minor aphyric basalt, mafic to felsic volcaniclastic rocks, and local limestone or marble.|
6821|Fork Lagoons beds|43625|6|Mentioned|p21|||||||||
6821|Fork Lagoons beds|43861|5|Briefly described|24,25; Fig2 p27; 28||Late Ordovician|||||||
6821|Fork Lagoons beds|64855|5|Briefly described|p20|Late Ordovician|Late Ordovician|Include sandstones with volcanic quartz.||||||22-FEB-10
6821|Fork Lagoons beds|66851|6|Mentioned|p916 Fig.1.|||||||||
6821|Fork Lagoons beds|67848|5|Briefly described|p16.|||Central Queensland, 475 km south of Townsville. Comparable to the arc assemblage and Wairuna Formation of Broken River Province. Mainly terrigenous sediments. Its limestone correlated with Carriers Well Formation.||||Is faulted against the Anakie Metamorphic Group.|Volcaniclastic and quartzose arenites, mafic volcanic rocks, limestone/marble and serpentinite.|
6821|Fork Lagoons beds|68553|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
6821|Fork Lagoons beds|68731|5|Briefly described|pp128-130, p132, p135, p215, p221|Silurian|Late Ordovician|Anakie Province. Defined by Anderson and Palmieri (1977) in several isolated inliers, but shown by Withnall et al. (1995) to extend from Fork Lagoons to 10 km west of Anakie. Palmieri (1978) identified five conodont faunas of Gisbornian-Bolindian age.|||||Comprises predominantly slate, phyllite and interbedded, thin to thick, brown to grey, quartzose sandstone and mudstone.|
6821|Fork Lagoons beds|68823|5|Briefly described|p372 Fig.1.|Late Ordovician|Late Ordovician|Faulted against metamorphic rocks in SE Anakie Inlier. Intruded by Devonian granite.||||Faulted against Anakie Metamorphic Group.|Includes minor limestone and basalt.|
6821|Fork Lagoons beds|68900|6|Mentioned|p4, p18|Ordovician|Ordovician|Drummond Basin.||||||
6821|Fork Lagoons beds|69541|5|Briefly described|p645 Fig.1(b), p654|Late Ordovician|Late Ordovician|Thomson Orogen. Appears as Forks Lagoons beds in Fig.1(b). Occupies a belt 35 km long and 10 km wide.|||||Turbiditic interbedded slate, siltstone and fine- to medium-grained sandstone; scattered small lenses of limestone, some interbedded with basalt; local volcanolithic sandstone and felsic volcaniclastic rocks.|
6821|Fork Lagoons beds|69599|5|Briefly described|p593|Late Ordovician|Late Ordovician|||||Is overlain unconformably by Red Mountain Formation.||
6821|Fork Lagoons beds|69952|6|Mentioned|p115|Ordovician|Ordovician|||||||
6821|Fork Lagoons beds|70499|6|Mentioned|p4|Late Ordovician|Late Ordovician|Geological province: Thomson Orogen. Suite of sedimentary rocks and volcanic rocks adjacent to, and immediately SW of Ruby Creek mylonite zone.||||||
6821|Fork Lagoons beds|70744|5|Briefly described|p939, p947|Late Ordovician|Late Ordovician|Southern Anakie Province. Age from fossils by Withnall et al. (1995). Detrital zircon ages and provenance discussed. Strongly shortened by the Benambran Orogeny.|c.460-450 Ma (estimated from Fig.7).||||A varied unit of slate, quartz-rich turbidites, shallow-marine limestone, mafic volcanic rocks, rare serpentinite and silicic volcaniclastic rocks.|
6821|Fork Lagoons beds|73425|6|Mentioned|p16|Late Ordovician|Late Ordovician|Anakie Province, northeast Thomson Orogen.||||||
6827|Forsayth Granite|9539|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Grey foliated coarse porphyritic biotite leuco- and melagranite.||||||
6827|Forsayth Granite|22744|5|Briefly described|P6, Table1 P8||Proterozoic|||||||
6827|Forsayth Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Geological Province: Georgetown Region.||||||15-JAN-07
6827|Forsayth Granite|23453|5|Briefly described|p16|Proterozoic|Proterozoic|||||||
6827|Forsayth Granite|23493|5|Briefly described|p8, p18 Tb. 1|Precambrian|Precambrian|Grey, coarse-grained massive to porphyritic biotite granite. Intruded by Dumbano Granite; intrudes Cobbold Dolerite.||||||27-MAY-15
6827|Forsayth Granite|23494|4|Described|p10, p24 Tb. 1|Precambrian|Precambrian|Unconformably overlain by Newcastle Range Volcanics. Intrudes Einasleigh Metamorphics and Cobbold Dolerite; intruded by Dumbano Granite, Butlers Igneous Complex and Lochaber Granite.||||||27-MAY-15
6827|Forsayth Granite|23495|5|Briefly described|map legend||Proterozoic|Age shown as Proterozoic?||||||
6827|Forsayth Granite|23498|5|Briefly described|p24 table1||Proterozoic|Intruded Einasleigh Metasmorphics. Intruded by Bagstowe Igneous Complex||||||
6827|Forsayth Granite|23510|5|Briefly described|Map Legend||Mesoproterozoic|Of Forsayth Supersuite.||||||15-JAN-07
6827|Forsayth Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 819. S-Type.||||||
6827|Forsayth Granite|23616|5|Briefly described|p64|||SHRIMP U-Pb 1550+/-7 Ma. Of Forsayth Supersuite. Dargalong Province.||||||
6827|Forsayth Granite|24013|5|Briefly described|p18 Tb. 1|Proterozoic|Proterozoic|Grey, coarse-grained massive to porphyritic biotite granite. Correlated with Robin Hood and Dumbano Granites.  Intruded by Agate Creek Volcanics; intrudes the Etheridge Formation.||||||27-MAY-15
6827|Forsayth Granite|24197|5|Briefly described|p17, p77|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Metasedimentary xenoliths common. Age: 1544+/7Ma. Geological province: Georgetown Inlier. See also p79 Tb. 9.1.||||||07-FEB-11
6827|Forsayth Granite|24485|5|Briefly described|p59|Mesoproterozoic|Mesoproterozoic|Age: 1550 +/- 7Ma (U-Pb SHRIMP zircon). Of the Forsayth Supersuite.||||||15-JAN-07
6827|Forsayth Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1550Ma. Geological Province: Georgetown Inlier. Name written as Forsayth only under heading for GRANITE.||||||09-MAY-05
6827|Forsayth Granite|29795|6|Mentioned|Fig.1|||||||||
6827|Forsayth Granite|29796|6|Mentioned|Fig.1|||||||||
6827|Forsayth Granite|30508|6|Mentioned|p94|||Not possible to map separate phases||||||
6827|Forsayth Granite|30587|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6827|Forsayth Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6827|Forsayth Granite|31822|6|Mentioned|p66|||Proterozoic||||||
6827|Forsayth Granite|31832|6|Mentioned|Table 6|||||||||
6827|Forsayth Granite|32527|6|Mentioned|p403|||||||||
6827|Forsayth Granite|32528|5|Briefly described|Table 1|||||||||
6827|Forsayth Granite|32553|4|Described|p62|||||||||
6827|Forsayth Granite|33179|4|Described|Table 1|||||||||
6827|Forsayth Granite|33180|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Prob.Upper Proterozoic||||||
6827|Forsayth Granite|33669|6|Mentioned|p516|||||||||
6827|Forsayth Granite|33907|6|Mentioned|p4|||||||||
6827|Forsayth Granite|33909|6|Mentioned|p229|||Refers White (1959).||||||
6827|Forsayth Granite|34284|6|Mentioned|Table 1|||Prot.||||||
6827|Forsayth Granite|34883|6|Mentioned|p85|||||||||
6827|Forsayth Granite|34955|6|Mentioned|p228|||||||||
6827|Forsayth Granite|35214|6|Mentioned|p7|||||||||
6827|Forsayth Granite|35921|6|Mentioned|p31|||||||||
6827|Forsayth Granite|35930|6|Mentioned|Fig.1|||||||||
6827|Forsayth Granite|35948|6|Mentioned|Table 2|||40Ar-39Ar data.||||||
6827|Forsayth Granite|36216|6|Mentioned|p208|||||||||
6827|Forsayth Granite|37570|4|Described|p119|||||||||
6827|Forsayth Granite|38029|6|Mentioned|PB47|||||||||
6827|Forsayth Granite|38366|6|Mentioned|p34|||||||||
6827|Forsayth Granite|39027|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
6827|Forsayth Granite|39445|5|Briefly described|Table 2|||Age: 1238 and 1468 Ma? See also p45.||||||15-JAN-07
6827|Forsayth Granite|39687|6|Mentioned|p3|||||||||
6827|Forsayth Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6827|Forsayth Granite|39981|6|Mentioned|p102|||||||||
6827|Forsayth Granite|41272|5|Briefly described|M 1of1 B05|||||||||
6827|Forsayth Granite|41680|6|Mentioned|p119|||||||||
6827|Forsayth Granite|43060|5|Briefly described|p78|||Age of 1550+/-7 Ma.Of Forsayth Supersuite||||||
6827|Forsayth Granite|43083|5|Briefly described|p114, p117|||U-Pb age of 1550+/-7 Ma. S-type. Appears to have been superseded by Nundah Grandiorite (p117).||||||17-JUN-09
6827|Forsayth Granite|43087|5|Briefly described|p8|||U-Pb zircon age of 1550 +/-7 Ma.||||||
6827|Forsayth Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic. U-Pb zircon age is 1544+/-7 Ma.||||||03-DEC-13
6827|Forsayth Granite|43664|6|Mentioned|p58|Calymmian|Calymmian|Age: 1550+7-2 U-Pb zircon||||||
6827|Forsayth Granite|43716|6|Mentioned|p35|||||||||
6827|Forsayth Granite|43896|14|Not recorded|Map Legend||Proterozoic|||||||
6827|Forsayth Granite|43978|14|Not recorded|p145,147-150|||||||||
6827|Forsayth Granite|44043|14|Not recorded|Tb.1,p63-4,68,70,72||Late Precambrian|p74. Intrudes Einasleigh Metamorphics, Etheridge Formation and Robertson River Metamorphics.||||||
6827|Forsayth Granite|44047|14|Not recorded|Map Legend||Proterozoic|||||||
6827|Forsayth Granite|44048|14|Not recorded|Map Legend||Proterozoic|||||||
6827|Forsayth Granite|44049|14|Not recorded|Map Legend||Proterozoic|||||||
6827|Forsayth Granite|44053|14|Not recorded|p238|||||||||
6827|Forsayth Granite|44059|14|Not recorded|p442-447|||Neoproterozoic or Early Palaeozoic.||||||
6827|Forsayth Granite|44091|14|Not recorded|p12||Neoproterozoic|||||||
6827|Forsayth Granite|44258|14|Not recorded|p1,7-10,12,18,27,28||Precambrian|1200 Ma minimum age.||||||
6827|Forsayth Granite|44259|14|Not recorded|p107|||1200 Ma.||||||
6827|Forsayth Granite|44296|14|Not recorded|Map Legend||Proterozoic|||||||
6827|Forsayth Granite|44516|14|Not recorded|p36||Proterozoic|||||||
6827|Forsayth Granite|44542|14|Not recorded|p27|||||||||
6827|Forsayth Granite|44723|14|Not recorded|p562|||||||||
6827|Forsayth Granite|45003|14|Not recorded|p29,35,38|||||||||
6827|Forsayth Granite|45009|2|Defined|p21,30,34-5,75,101-3|||p107,118-9,121-3,127-9,Pl.13,Tb.15. Intruded by Dumbano Granite.||||||
6827|Forsayth Granite|45014|14|Not recorded|p21,58,59,109||Proterozoic|||||||
6827|Forsayth Granite|45025|4|Described|p24||Precambrian|||||||
6827|Forsayth Granite|45076|6|Mentioned|p35|||Refers Best (1962).||||||
6827|Forsayth Granite|45086|4|Described|p44|||See also p45. Age. Mineralization.||||||15-JAN-07
6827|Forsayth Granite|45087|6|Mentioned|p25|||Chemical analyses||||||
6827|Forsayth Granite|45113|3|Fully described|p5|||Emphasis on petrography.Geochemistry P32.||||||
6827|Forsayth Granite|45686|14|Not recorded|p.352|||||||||
6827|Forsayth Granite|45806|14|Not recorded|252|||Orange card not found.||||||
6827|Forsayth Granite|48894|6|Mentioned|p48|||Age. See also PP49,50.||||||
6827|Forsayth Granite|48976|5|Briefly described|Table 21|||Isotopic data||||||
6827|Forsayth Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
6827|Forsayth Granite|50199|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
6827|Forsayth Granite|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Part of the Forsayth Batholith. Age: 1550-1560Ma.||||||27-MAY-15
6827|Forsayth Granite|50537|5|Briefly described|p1.2, 2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite. Age: 1544-1550 +/- 7Ma (U-Pb).||||||
6827|Forsayth Granite|50542|6|Mentioned|p96|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
6827|Forsayth Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Biotite granites.||||||05-JUL-04
6827|Forsayth Granite|60081|5|Briefly described|Map legend|Proterozoic|Proterozoic|Grey porphyritic biotite granite.||||||
6827|Forsayth Granite|61258|6|Mentioned|p386|Mesoproterozoic|Mesoproterozoic|Age: 1550+/-6Ma (Black and McCulloch 1990).||||||
6827|Forsayth Granite|63866|5|Briefly described|p77|Calymmian|Calymmian||1550 +/- 6 Ma (U-Pb zircon, TIMS)|Forsayth Supersuite||||
6827|Forsayth Granite|66800|6|Mentioned|p926.||||1550 +/- 6 Ma (Black & McCulloch 1990).|||||
6827|Forsayth Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province. Grey, dark-coloured, and potassically-altered variants are each mapped separately.|||||Grey to pink, medium- to coarse-grained, generally strongly porphyritic biotite granite, commonly foliated, with tabular K-feldspar megacrysts to 5 cm.|
6827|Forsayth Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province. A dark grey to locally dark pink variant is mapped separately.|||||Grey, medium- to coarse-grained, generally strongly porphyritic biotite granite, commonly foliated, with tabular K-feldspar phenocrysts to 5 cm.|
6827|Forsayth Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province. A dark grey to locally dark pink variant is mapped separately.|||||Grey, medium- to coarse-grained, generally strongly porphyritic biotite granite, commonly foliated, with tabular K-feldspar phenocrysts to 5 cm.|
6827|Forsayth Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Grey to pink, medium- to coarse-grained, generally strongly porphyritic biotite granite, commonly foliated, with tabular K-feldspar megacrysts to 5 cm.|
6827|Forsayth Granite|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Forsayth Batholith. Etheridge Province. Shown to occur during D2 (~ 1550-1560 Ma).|~ 1560-1550 Ma||||Dark grey to locally dark pink, medium to coarse-grained, generally strongly porphyritic biotite granite, commonly foliated with tabular K-feldspar megacrysts to 5 cm.|
6827|Forsayth Granite|68576|5|Briefly described|Q_11: p24-25, p28|Mesoproterozoic|Mesoproterozoic|Georgetown area. Part of Forsayth Batholith.||||Is intruded by Delaney Granite.|Dark grey, porphyritic, medium- to coarse-grained biotite granite with abundant grey, tabular K-feldspar megacrysts to 2cm. Local irregular dykes and veins of pale grey, medium, K-feldspar-phyric muscovite-biotite granite (?Delaney Granite).|
6827|Forsayth Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith. Large elliptical plutons (mostly 20-75 km2).||Forsayth Supersuite.|||Megacrystic granite.|
6827|Forsayth Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province. Age determination by U-Pb zircon (unspecified).|1550+/-6 Ma (crystallisation).||||Granite.|
6827|Forsayth Granite|72983|5|Briefly described|p78|Calymmian|Calymmian|Previous K-Ar dating yielded younger ages of ~380 Ma for this unit, which have been attributed to a complete loss of argon from the analysed biotites due to a possible thermal event during the Devonian (Richards et al., 1966).|1560-1550 Ma|Forsayth Supersuite||Intruded by Lineament Prospect dyke.||
6827|Forsayth Granite|73527|6|Mentioned|p2, p3 Fig.2, p8 Fig.6|||Georgetown Inlier, central domain. Forsayth Batholith also used p5.||Forsayth Supersuite||||
6827|Forsayth Granite|73642|5|Briefly described|p3 Fig.2, p4, p5 Fig.3, p8, p10-11, p13|Calymmian|Calymmian|Georgetown Inlier. S-type. See also p6 Fig.4, p9 Tb.3.|1565+/-10 Ma, 1550+/-7 Ma|Forsayth Supersuite|||Includes grey, weakly foliated, medium to coarse-grained, generally porphyritic granite with magmatic biotite and prismatic K-feldspar megacrysts.|
6827|Forsayth Granite|75079|5|Briefly described|p3, 5-6, 9-13, 16, 18|Mesoproterozoic|Mesoproterozoic|Central domain, Georgetown Inlier. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|~1550 Ma.|Forsayth Supersuite.|||Foliated K-feldspar megacrystic granite.|
6874|Four Mile Mudstone Member|23037|6|Mentioned|p66||Permian|Of Barfield Formation.||||||
6874|Four Mile Mudstone Member|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbrm].  Siltstone, mudstone.||||||
6874|Four Mile Mudstone Member|30451|6|Mentioned|Fig.9|||See also p54,56.||||||12-NOV-08
6874|Four Mile Mudstone Member|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6874|Four Mile Mudstone Member|43050|6|Mentioned|p52|||Of Barfield Formation||||||12-NOV-08
6874|Four Mile Mudstone Member|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Barfield Formation (Back Creek Group). Siltstone and mudstone.||||||18-JUN-09
6874|Four Mile Mudstone Member|65388|4|Described|p163 Fig. 63, p168, 169|||Of Barfield Formation,  Bowen Basin. Redefined by Dear et al (1971) after Derrington & others (1959) formation. Type section along the Dawson Highway is incomplete. Overlain by Cottenham Sandstone Member.||||||
7012|Gargoogie Oolite Member|34155|6|Mentioned|p91|||See also p93. Lower Visean. Rockhampton Group.||||||12-NOV-08
7031|Garraway Sandstone|23425|4|Described|p376-378/Table 9.7 p395.|||Lithostratigraphic and biostratigraphic correlative of the Eulo Queen Group in the Staaten Sub-basin. Overlying unit Gilbert River Formation - conformable. Geological Province Carpentaria Basin. Max thickness 100 m.||||||
7031|Garraway Sandstone|23430|5|Briefly described|p522|||||||||
7031|Garraway Sandstone|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Contains the Wenlock, Bromley and Wreath Members.||||||
7031|Garraway Sandstone|42061|4|Described|p156|||See also Fig.4||||||
7031|Garraway Sandstone|42550|5|Briefly described|p9|||||||||
7031|Garraway Sandstone|42637|5|Briefly described|Fig.4 P14, P46|||Typo For Garraway beds?||||||21-JUN-05
7031|Garraway Sandstone|62837|5|Briefly described|Stratigraphic columns|Kimmeridgian|Bathonian|Includes Wenlock, Bromley, Wreath Members. Age: 170-140Ma. Geological Province: Northern Cape York.||||||01-MAR-10
7031|Garraway Sandstone|66915|5|Briefly described|p6 Fig.3|Jurassic|Jurassic|Carpentaria Basin. Also presented as misspelt Garraway Beds in this paper.||||Is overlain ?unconformably by Gilbert River Formation.||12-JAN-17
7031|Garraway Sandstone|67323|6|Mentioned|p96|||Carpentaria Basin. A regional aquifer.||||||
7031|Garraway Sandstone|67402|4|Described|p165 tbl LPB1, p176|Tithonian|Kimmeridgian|Carpentaria Basin, Weipa Sub-basin. Contains aquifers. Is generally 90m thick but may be up to 130m thick in the Weipa Sub-Basin. See also p177, p180, p181, p231.||||Unconformably overlies the Eulo Queen Group. Unconformably overlain by the Gilbert River Formation.|Coarse to fine-grained quartz sandstone.|
7031|Garraway Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Carpentaria Basin.||||||
7031|Garraway Sandstone|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Jurassic|Middle Jurassic|Carpentaria Basin. Deposited in a fluvio-lacustrine environment. This unit is a good potential hydrocarbon reservoir. |||||Quartzose sandstone and thin coal seams.|
7031|Garraway Sandstone|69455|6|Mentioned|p39:4 Fig.39.3; 39:14-15|Jurassic|Jurassic|Carpentaria Basin. Possible source rock.||||||12-JUL-16
7031|Garraway Sandstone|69594|5|Briefly described|p518, p520-522, p540, p573|Late Jurassic|Late Jurassic|Southern Weipa and northern Staaten Sub-basins, Carpentaria Basin. 38-90m thick. Meandering to braided fluvial deposits. One of the main aquifers in the Basin.||||Is overlain conformably by Gilbert River Formation. Part-equivalent to Dalrymple Sandstone (Laura Basin).|Succession of quartzose sandstone, conglomerate, siltstone and claystone.|
7031|Garraway Sandstone|69673|6|Mentioned|p202 fig 165|||||||Overlain by Gilbert River Formation||
7031|Garraway Sandstone|71792|4|Described|p39, p46, p57-p58|Jurassic|Jurassic|Carpentaria Basin. Appears to directly overlie the Glennie Creek Granite.||||Overlies the Janet Ranges Volcanics.|Clayey micaceous quartzose sandstone and granule to pebble conglomerate; carbonaceous in part.|
7031|Garraway Sandstone|71853|5|Briefly described|Map legend.|Late Jurassic|Late Jurassic||||||Clayey micaceous quartzose sandstone and granule to pebble conglomerate; carbonaceous in part.|
7031|Garraway Sandstone|72297|5|Briefly described|p746|||Carpentaria Basin. Excellent hydrocarbon reservoir potential because it contains aquifers.||Eulo Queen Group.||||
7050|Gatton Sandstone|12597|5|Briefly described|p492 Tb.1|Toarcian|Pliensbachian|Clarence-Moreton Basin. 500m thick. The coal is of no economic significance.||Unit in Marburg Subgroup.||Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.|Medium- to very coarse-grained, quartz-feldspathic-lithic sandstone including beds of pebbly sandstone with calcareous cement; minor beds of conglomerate and siltstone-shale, and fossil wood; thin coal seams.|
7050|Gatton Sandstone|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Of Marburg Subgroup||||
7050|Gatton Sandstone|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Quartz-lithic arenite, conglomerate, minor fossil wood. Contains the Calamia Member. Max. thickness: 600m. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|22865|6|Mentioned|Fig.22.10ap318|||||||||
7050|Gatton Sandstone|23799|5|Briefly described|p48, p10 Tb. 1|Jurassic|Jurassic|Of Marburg Group.  Lithic labile and feldspathic labile sandstone.  Overlain by Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Marburg Subgroup.||||||
7050|Gatton Sandstone|23811|5|Briefly described|Map Legend|Toarcian|Pliensbachian|Of Marburg Subgroup.  Thin- to thick-bedded, coarse- to medium-grained, feldspathic to lithic feldspathic sandstone with clay matrix; subordinate intervals of granule, pebble and minor cobble polymictic conglomeGeological Province: Clarence-Moreton Basin.||||||20-DEC-04
7050|Gatton Sandstone|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Maximum thickness: 600m. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Marburg Subgroup (Bundamba Group).  Lithic labile and feldspathic labile sandstone (Clarence-Moreton Basin).||||||
7050|Gatton Sandstone|29591|6|Mentioned|p83|||||||||
7050|Gatton Sandstone|31118|4|Described|Table 3|||Lithology||||||
7050|Gatton Sandstone|41631|4|Described|p17|||See also Fig.2||||||
7050|Gatton Sandstone|42248|2|Defined|App.1 p412|Early Jurassic||||||||15-MAY-19
7050|Gatton Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
7050|Gatton Sandstone|42869|5|Briefly described|Table 1, P33|||Of Marburg Group.||||||27-AUG-08
7050|Gatton Sandstone|42951|5|Briefly described|Fig.11|||Of Marburg Subgroup.||||||27-AUG-08
7050|Gatton Sandstone|43001|6|Mentioned|Fig.6,p123|||||||||
7050|Gatton Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Of the Marburg Subgroup.  Geological Province: Clarence-Moreton Basin.||||||12-APR-05
7050|Gatton Sandstone|43736|5|Briefly described|Table 1,p4|||||||||
7050|Gatton Sandstone|44026|14|Not recorded|p123||Jurassic|||||||
7050|Gatton Sandstone|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Marburg Subgroup.  Overlies: Woogaroo Subgroup.  Underlies: Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
7050|Gatton Sandstone|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Formation.||||||
7050|Gatton Sandstone|60281|5|Briefly described|p24, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group).  Sandstone, conglomerate, minor fossil wood.  Overlain by Koukandowie Formation; overlies the Ripley Road Sandstone.  Max. thickness: 800m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
7050|Gatton Sandstone|60993|3|Fully described|p21, p18|||Supersedes the Gatton Sst Mbr. Includes the conglomeratic beds of the former Tenthill Conglomerate Mbr or Winwill Conglomerate Mbr. Overlies: Woogaroo Subgp. Max. thickness: >100m. Geol. Prov: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60995|4|Described|p62, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Marburg Subgp. Formerly informally known as "Peak Fm"; and partly equivalent to "Olive Gap Fm". Overlies Laytons Range Conglom.  Max. thick: ~500m. Geol. Prov: Clarence-Moreton Basin. Equivalent to Blaxland Fossil Wood Conglom. mbr.||||||
7050|Gatton Sandstone|60996|5|Briefly described|p72, p93||| Unconformably overlies the Laytons Range and Aberdare Conglomerates, or Raceview Fm; and also overlaps Ripley Road Sst onto basement at the basin edges.  Max. thickness: 1100m. Geol. Prov: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60997|5|Briefly described|p138|Toarcian|Sinemurian|Formerly the "Blaxland Fossil Wood Conglomerate Member" (McElroy 1963). Conformably overlain by Koukandowie Formation. Geological Province: Clarence-Moreton Basin. ||||||
7050|Gatton Sandstone|60998|5|Briefly described|p146 Fig. 2|||Characterised by medium to coarse-grained quartz-lithic sandstone with mainly upward-fining cycles. Overlain by Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60999|5|Briefly described|p164, p173|Early Jurassic|Early Jurassic|Of the Marburg Subgroup. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p176. Broadly correlated in time with uppermost Precipice Sandstone and lowermost Evergreen Formation, both in the Surat Basin. ||||||
7050|Gatton Sandstone|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61002|6|Mentioned|p202|||Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
7050|Gatton Sandstone|61006|5|Briefly described|p277|Jurassic|Jurassic|Includes the Calamia Member. Labile sandstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
7050|Gatton Sandstone|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Of the Marburg Subgroup. Includes the Koreelah Conglomerate Member. Thick-bedded, medium- to coarse-grained, quartz-lithic amd feldspathic sandstone.||||||12-DEC-07
7050|Gatton Sandstone|63748|5|Briefly described|p21-22|Early Jurassic|Early Jurassic|Of Marburg Subgp. Includes Koreelah Conglomerate Member at base. Unconformable on Texas beds and Silverwood Group; conformable below Koukandowie Fm. Geol.province: Clarence-Moreton Basin. Quartz-lithic and feldspathic sandstone in a calcareous cement.||||||07-FEB-11
7050|Gatton Sandstone|64289|5|Briefly described|p6 Fig. 2, p17|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Overlain by Koukandowie Formation. Max. thickness: 500m. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
7050|Gatton Sandstone|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with the middle part of Landsborough Sandstone (Southern Nambour Basin).||Basal unit in Marburg Subgroup.||Overlies Ripley Road Sandstone.Is overlain by Ma Ma Creek Member (of Koukandowie Formation).||
7050|Gatton Sandstone|67402|5|Briefly described|p165 tbl LPB1|Sinemurian|Sinemurian|Clarence-Moreton Basin. Deposited in a braided stream to floodplain environment. Sandstones are often of reservoir quality. Greater than 150m thick. See also p187, p188, p190, p192, p193, p307.||Marburg Subgroup|Includes the Calamia Member.|Overlies the Ripley Road Sandstone. Overlain by the Ma Ma Creek Member,  Koukandowie Formation.|Medium to very coarse grained, quartz-feldspathic-lithic sandstone.|
7050|Gatton Sandstone|68135|5|Briefly described|p52 fig 2b, p64|Pleinsbachian||Clarence-Moreton Basin. Includes plant macrofossils and invertebrate fossils, including the oldest Australian leech cocoons.||||Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.|Cross-bedded sandstone.|14-SEP-17
7050|Gatton Sandstone|69297|5|Briefly described|p487 fig 5.38, p488|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 200-600m thick. Appears as Gatton Formation on p488. Potential hydrocarbon reservoir rock. ||Mauburg Subgroup|Includes the Koreelah Conglomerate and the Calamia Member.||Sandstone, conglomerate and minor fossilised wood.|
7050|Gatton Sandstone|69594|4|Described|p519, p544-547, p572|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||Marburg Subgroup.|Calamia Member, Koreelah Conglomerate Member.|Overlies Ripley Road Sandstone. Is overlain by Ma Ma Creek Member (Koukandowie Formation). Correlated with upper Precipice Sandstone and lower Evergreen Formation.|Predominantly thick-bedded, medium- and coarse-grained, quartz-lithic and feldspathic sandstone, blue-grey (fresh) commonly with calcareous cement; large-scale trough cross-bedding, carbonised wood fragments and pebble beds generally characteristic.|
7050|Gatton Sandstone|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Marburg Subgroup.||||
7050|Gatton Sandstone|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
7050|Gatton Sandstone|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Aquifer: generally artesian.||Marburg Subgroup.|Koreelah Conglomerate Member.|Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.||
7050|Gatton Sandstone|71628|6|Mentioned|p9: 5, 32|||||||Overlies Bruxner Granodiorite and (locally) Jenny Lind Tonalite.||
7050|Gatton Sandstone|71805|5|Briefly described|p76|Pleinsbachian|Sinemurian|Clarence-Moreton Basin.||Marburg Subgroup||Overlies the Ripley Road Sandstone. Overlain by the Ma Ma Creek Member.||
7050|Gatton Sandstone|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Early Jurassic|Shown as located within the Clarence-Moreton Basin.||||Overlies Ripley Road Sandstone and underlies Koukandowie Formation|Includes fossiliferous sandstone.|
7050|Gatton Sandstone|73570|5|Briefly described|p912 Fig.2, p913-914, p915 Fig.4|Early Jurassic|Early Jurassic|Clarence-Morton Basin.|187+/-1 Ma|Marburg Subgroup||||
7065|Gayndah Formation|23799|3|Fully described|p36, p12 Tb. 1|Middle Triassic|Early Triassic|Upgraded from "Gayndah beds".  Conformably overlain by Neara Volcanics; unconformably overlain also by units of Aranbanga Volcanic Group.  Max. thickness: <200m.  Geological Province: Esk Trough.  See also p37 Tb. 3.||||||
7065|Gayndah Formation|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||
7065|Gayndah Formation|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|Parent: Toogoolawah Group.||||||14-AUG-08
7065|Gayndah Formation|41738|1|Redefined|p165|Middle Triassic||Originally Gayndah Beds.||||||14-AUG-08
7065|Gayndah Formation|41778|6|Mentioned|Table 1|||||||||
7065|Gayndah Formation|41790|5|Briefly described|p473|||||||||
7065|Gayndah Formation|42054|6|Mentioned|p273|||||||||
7065|Gayndah Formation|43008|5|Briefly described|map legend|||||||||
7065|Gayndah Formation|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
7065|Gayndah Formation|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||09-JUN-04
7065|Gayndah Formation|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group. Geological Province: Esk Trough. Polymictic pebble to cobble conglomerate; lithic labile, sublabile and quartzose sandstone, siltstone, shale.||||||02-SEP-04
7065|Gayndah Formation|60726|6|Mentioned|p5, throughout text. |?Middle Triassic|?Middle Triassic|Gayndah area. Contains fossil insects.||||||
7065|Gayndah Formation|61782|5|Briefly described|p275|||Of Toogoolawah Group. Geol Prov: Esk Trough.||||||
7065|Gayndah Formation|63821|5|Briefly described|p20|Middle Triassic|Middle Traissic|Of Toogoolwah Gp. Overlies/interfingers with Kinella Basalt; underlies Mount Marcella Volcanics. Polymictic conglomerate, sandstone, mudstone, siltstone, minor volcanics and thin coal beds; fluviatile; Middle Triassic miospores. Geol.Province: Esk Trough.||||||07-FEB-11
7065|Gayndah Formation|68679|3|Fully described|p326, p391|Middle Triassic|Middle Triassic|Northern Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Crops out around and NW of Gayndah. The type section is in GSQ Maryborough 1 and comprises fining-up successions with 30-40% matrix and framework supported conglomerates, 30% sandstone and the remainder siltstone and shale. Thickness ranges from ~173m in the type section to ~40m N of Gayndah. ||Toogoolawah Group.||Disconformably overlies Kinellan Basalt. With Kinellan Basalt, is equivalent to the Bryden and Esk Formations.|Sandstones, thick-bedded conglomerate, siltstone (locally carbonaceous with poorly preserved plant remains and fossil wood), mudstone, carbonaceous shale, minor andesite flows and thin coal seams.|
7078|Gebbie Formation|22593|6|Mentioned|Table 1|||divided into informal Members||||||
7078|Gebbie Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
7078|Gebbie Formation|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
7078|Gebbie Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
7078|Gebbie Formation|23161|4|Described|p28 table4|Early Permian|Early Permian|||||||
7078|Gebbie Formation|23430|5|Briefly described|p515|||||||||
7078|Gebbie Formation|29437|6|Mentioned|p136|||||||||
7078|Gebbie Formation|31690|6|Mentioned|p36|||||||||
7078|Gebbie Formation|32945|6|Mentioned|p78|||See also PP79,80,81 & Fig.2||||||
7078|Gebbie Formation|32949|4|Described|p441|||||||||
7078|Gebbie Formation|33711|6|Mentioned|Table 3|||||||||
7078|Gebbie Formation|34132|6|Mentioned|p5|||Lower Permian||||||
7078|Gebbie Formation|35160|6|Mentioned|p1|||||||||
7078|Gebbie Formation|35284|6|Mentioned|Fig.1|||||||||
7078|Gebbie Formation|35467|6|Mentioned|p177|||||||||
7078|Gebbie Formation|36739|6|Mentioned|Fig.2|||||||||
7078|Gebbie Formation|37612|6|Mentioned|p282|||||||||
7078|Gebbie Formation|38917|6|Mentioned|p156|||||||||
7078|Gebbie Formation|39220|6|Mentioned|p43|||Fauna III||||||
7078|Gebbie Formation|39261|6|Mentioned|Fig.6|||||||||
7078|Gebbie Formation|39262|6|Mentioned|p121|||||||||
7078|Gebbie Formation|39267|4|Described|p234|||||||||
7078|Gebbie Formation|39304|6|Mentioned|Photo 19.1|||||||||
7078|Gebbie Formation|39423|6|Mentioned|p53|||||||||
7078|Gebbie Formation|40093|6|Mentioned|p26|||||||||
7078|Gebbie Formation|40571|5|Briefly described|p31|||||||||
7078|Gebbie Formation|41034|5|Briefly described|p367|||||||||
7078|Gebbie Formation|41191|6|Mentioned|Fig.3|||||||||
7078|Gebbie Formation|41246|6|Mentioned|Map legend|Permian||||||||
7078|Gebbie Formation|41689|6|Mentioned|Table 1|||||||||
7078|Gebbie Formation|42249|6|Mentioned|Table 1 P22|||||||||
7078|Gebbie Formation|42250|6|Mentioned|Fig.4 P31|||||||||
7078|Gebbie Formation|42257|5|Briefly described|Table 1 P263|||||||||
7078|Gebbie Formation|42258|4|Described|p275|||||||||
7078|Gebbie Formation|42701|4|Described|p63|||||||||
7078|Gebbie Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
7078|Gebbie Formation|43000|6|Mentioned|p111|||||||||
7078|Gebbie Formation|43018|5|Briefly described|Table 1,p386|||||||||
7078|Gebbie Formation|43213|6|Mentioned|p158|||||||||
7078|Gebbie Formation|43475|14|Not recorded|p552,553||Permian|||||||
7078|Gebbie Formation|43882|14|Not recorded|p87-90,94,95,97|||Bowen Basin. Ammonoids.||||||
7078|Gebbie Formation|43893|14|Not recorded|p202||Permian|||||||
7078|Gebbie Formation|44000|2|Defined|Tb.1,2,p1,22,26,29,||Early Permian|Overlies Tiverton Formation & Lower Bowen Volcanics; underlies Blenheim Formation. Unit of Middle Bowen Beds. Lower Permian marine fossils.p.31-39,63-4,Pl.6||||||
7078|Gebbie Formation|44245|5|Briefly described|Map Legend||Permian|||||||
7078|Gebbie Formation|44409|14|Not recorded|Map Legend||Permian|||||||
7078|Gebbie Formation|44424|14|Not recorded|p293-301|||Now Gebbie Subgroup.||||||
7078|Gebbie Formation|44489|14|Not recorded|p69|||=Unit B.||||||
7078|Gebbie Formation|44635|4|Described|p11,Tb.1,map||Late Permian|||||||
7078|Gebbie Formation|45031|14|Not recorded|p6|||Part of Back Creek Group.||||||
7078|Gebbie Formation|48881|2|Defined|p1,12,20-24,36,45,||Early Permian|Tb.1.||||||
7078|Gebbie Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Early Permian|Geological Province: northern Bowen Basin.||||||04-FEB-08
7078|Gebbie Formation|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Quartzose to lithic sandstone, sandy siltstone, siltstone, carbonaceous shale, calcareous sandstone, coquinite.||||||
7078|Gebbie Formation|60659|5|Briefly described|p20||Early Permian|Of the Back Creek Group. Grades laterally into Collinsville Coal Measures. Conformably overlies Tiverton Formation. Geological Province: Bowen Basin.||||||07-FEB-11
7078|Gebbie Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||13-MAR-09
7078|Gebbie Formation|61917|5|Briefly described|Map legend|Late Permian|Early Permian|Of the Back Creek Group. Quartzose to lithic sandstone, sandy siltstone, siltstone, carbonaceous shale, calcareous sandstone, coquinite; fossiliferous.||||||16-MAR-06
7078|Gebbie Formation|65388|3|Fully described|p187-189, 159, 167, 186|Wordian|Artinskian|Of Back Creek Group in northern Bowen Basin. Defined by Malone & others (1966). Includes Wall Sandstone Member and Moonlight Sandstone Member, although these subdivisions appear not to be in current use. The name has  reverted to Gebbie Formation (from Subgroup) and is restricted to the area in which it was first defined (Staines and Koppe, 1979; McClung, (1981). Overlies Tiverton Formation conformably or disconformably or  Lizzie Creek Volcanic Group disconformably. Boundary with overlying Blenheim Fm is controversial. Type section  in Gebbie Creek, is 435m thick. Probably deposited in a shallow marine environment. Correlated with Oxtrack Formation. Collinsville Coal Measures are lateral equivalent. Grey, micaceous, fine to granule-grained quartzose to lithic labile sandstone, siltstone, carbonaceous shale and coquinite lenses. Thin conglomerate lags, dropstones and ferruginous and calcareous concretions occur throughout.||||||05-SEP-14
7078|Gebbie Formation|65706|6|Mentioned|p15 Tb.1, p16 Tb.1|Late Permian|Early Permian|Possibly unconformably overlies Lizzie Creek Volcanic Group. ||Of Back Creek Group.||||
7078|Gebbie Formation|67402|4|Described|p21, p45, p80 tbl BWN1|Kungurian|Kungurian|Bowen Basin. See also  p84, p85 tbl BWN2, p165 tbl LPB1.||Back Creek Group||Overlies the Tiverton Formation. Unconformably overlain by the Moonlight Sandstone.|Quartzose sandstone, lithic labile sandstone, sandy siltstone, siltstone, carbonaceous shale, calcareous sandstone and coquinite.|
7078|Gebbie Formation|68679|4|Described|p353, p378, p380-381|Permian|Permian|Malone et al. (1966). Connors-Auburn Province. Bowen Basin. 600m thick. Barrier, strand plain deposits.||Back Creek Group.||Gradationally overlies Tiverton Formation. Passes laterally into the Collinsville Coal Measures.|Quartzose to lithic sandstone, siltstone, carbonaceous shale, calcareous sandstone, coquinite; scattered marine fossils.|
7078|Gebbie Formation|73036|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Quartzose to lithic sandstone, sandy siltstone, siltstone, carbonaceous shale, calcareous sandstone, coquinite; fossiliferous.|
7078|Gebbie Formation|73037|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Quartzose to lithic sandstone, sandy siltstone, siltstone, carbonaceous shale, calcareous sandstone, coquinite; fossiliferous.|
7100|Gelaro Granite|23291|5|Briefly described|p45, p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Ootann Supersuite. Intrudes Saucebottle, Mount Cardwell, Junevale Granites; intruded by Rices Creek Granite. Geological Province: Georgetown Region.||||||08-JUL-15
7100|Gelaro Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
7100|Gelaro Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 355. I-Type.||||||
7100|Gelaro Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
7100|Gelaro Granite|23624|4|Described|p15|Permian|Carboniferous|Parent: Ootann Supersuite.||||||30-JUN-15
7100|Gelaro Granite|42691|5|Briefly described|map legend|Precambrian||||||||
7100|Gelaro Granite|43087|6|Mentioned|p42|||||||||
7100|Gelaro Granite|43110|5|Briefly described|p47|||||||||
7100|Gelaro Granite|43259|4|Described|Appendix 1,p41.||Carboniferous|||||||
7100|Gelaro Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
7100|Gelaro Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Mapped separately is a geophysical subdivision of this unit, described as a probable variant of its lithology.||Unit in Ootann Supersuite.|||Pink to red, medium- to coarse-grained, even-grained biotite monzogranite; commonly altered.|
7100|Gelaro Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Mapped separately is a geophysical subdivision of this unit, described as a probable variant of its lithology.||Unit in Ootann Supersuite.|||Pink to red, medium- to coarse-grained, even-grained biotite monzogranite; commonly altered.|
7100|Gelaro Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Late Carboniferous age. Informal subunits contain a geological subdivision. ||Of the Ootann Supersuite.|Informally subdivided into two units, based on geophysics.||Pink to red, medium to coarse-grained, even-grained biotite granite (commonly altered); rock type uncertain: possible variant of pink to red, medium to coarse-grained, even-grained, biotite monzogranite (commonly altered).|
7116|Gemini Coal|42642|6|Mentioned|p170|||Bowen Basin. Variation on Gemini Seam.||||||
7137|Georgina Limestone|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Sandy and laminated micrite, intraformational conglomerate, two-toned limestone, algal boundstones, minor oolitic grainstones and silicification.  Overlies Thorntonia Limestone; underlies Ninmaroo Formation.||||||21-JUN-04
7137|Georgina Limestone|10116|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Sandy and laminated micrite, conglomerate, limestone, grainstones.||||||
7137|Georgina Limestone|22954|6|Mentioned|Fig3p9|Idamean|Undillan|||||||
7137|Georgina Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 30m.||||||
7137|Georgina Limestone|30479|6|Mentioned|Fig.6|||Stratigraphic relations||||||
7137|Georgina Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7137|Georgina Limestone|31287|3|Fully described|p424|||See also p425-432. Lithostratigraphy.||||||19-SEP-06
7137|Georgina Limestone|31288|6|Mentioned|p325|||||||||
7137|Georgina Limestone|31572|6|Mentioned|p4|||Refers Opik (1963, 1967)||||||
7137|Georgina Limestone|33111|4|Described|p36|||Mention p17,18||||||19-SEP-06
7137|Georgina Limestone|34454|5|Briefly described|Table 2|||U.Cambrian||||||
7137|Georgina Limestone|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||19-SEP-06
7137|Georgina Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7137|Georgina Limestone|35139|4|Described|Table.2|||||||||
7137|Georgina Limestone|36234|3|Fully described|p168|||See also Fig.1.||||||
7137|Georgina Limestone|36243|6|Mentioned|Table 1A|||||||||
7137|Georgina Limestone|37155|6|Mentioned|p265|||||||||
7137|Georgina Limestone|37572|4|Described|p161|||See also p165 and Fig.8.||||||19-SEP-06
7137|Georgina Limestone|38532|4|Described|p243|||See also Fig.1.||||||
7137|Georgina Limestone|39445|5|Briefly described|Table 4|||Was Ninmaroo Formation on map. See also p61, p64 and Fig.5.||||||19-SEP-06
7137|Georgina Limestone|39690|6|Mentioned|p88|||||||||
7137|Georgina Limestone|39921|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
7137|Georgina Limestone|39943|6|Mentioned|Table 2A|||||||||
7137|Georgina Limestone|40038|6|Mentioned|p248|||||||||
7137|Georgina Limestone|40136|6|Mentioned|p29|||||||||
7137|Georgina Limestone|41587|6|Mentioned|p923|||||||||
7137|Georgina Limestone|41810|6|Mentioned|p112|||||||||
7137|Georgina Limestone|42060|6|Mentioned|Fig.5 P140|||||||||
7137|Georgina Limestone|42139|6|Mentioned|Fig.10 P74|||||||||
7137|Georgina Limestone|42956|5|Briefly described|p31 Fig.4|||||||||
7137|Georgina Limestone|43105|5|Briefly described|Fig.4,p9.|||||||||
7137|Georgina Limestone|43807|6|Mentioned|p352|||||||||
7137|Georgina Limestone|44091|14|Not recorded|p17,Tb.1,p18|Idamean|Mindyallan|||||||
7137|Georgina Limestone|44205|14|Not recorded|p8|||||||||
7137|Georgina Limestone|44211|2|Defined|p91,95,96,100-104|||Overlain disconformably by Ninmaroo Formation, rests on Mungerebar Limestone.||||||
7137|Georgina Limestone|44212|2|Defined|p110|||||||||
7137|Georgina Limestone|44285|14|Not recorded|p.4|||Ref. to Whitehouse. Qld,N.T. border.||||||
7137|Georgina Limestone|44308|14|Not recorded|p3,5,14,Tb.1||Late Cambrian|||||||
7137|Georgina Limestone|44309|2|Defined|Tb.1,p7,9,10,map|||||||||
7137|Georgina Limestone|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
7137|Georgina Limestone|44312|14|Not recorded|Map Legend||Late Cambrian|||||||
7137|Georgina Limestone|44326|14|Not recorded|Map Legend||Late Cambrian|||||||
7137|Georgina Limestone|44362|6|Mentioned|p11|||||||||
7137|Georgina Limestone|44441|14|Not recorded|p.4|||Ref.to Whitehouse, 1931,1936. (E53-16).||||||
7137|Georgina Limestone|44457|14|Not recorded|p.3|||||||||
7137|Georgina Limestone|44543|14|Not recorded|p32|||Similar lithology to Mungerebar Limestone.||||||
7137|Georgina Limestone|44920|14|Not recorded|Map Legend,Sheet 4||Late Cambrian|||||||
7137|Georgina Limestone|45002|14|Not recorded|p14-122|||Late Cambrian fossils described. See also lexicon.||||||
7137|Georgina Limestone|45012|14|Not recorded|p101-154,162-167,|||p202-288,320-3. Late Cambrian fauna.||||||
7137|Georgina Limestone|45051|6|Mentioned|p5|||Cambrian age||||||
7137|Georgina Limestone|45052|3|Fully described|p115|||U.Camb.||||||
7137|Georgina Limestone|45053|6|Mentioned|p12|||||||||
7137|Georgina Limestone|45115|6|Mentioned|p6|||||||||
7137|Georgina Limestone|45130|6|Mentioned|p23|||||||||
7137|Georgina Limestone|46956|6|Mentioned|p160|||||||||
7137|Georgina Limestone|46958|6|Mentioned|Fig.2|||||||||
7137|Georgina Limestone|46959|6|Mentioned|Table 1|||||||||
7137|Georgina Limestone|47024|6|Mentioned|p1|||||||||
7137|Georgina Limestone|47058|6|Mentioned|p136|||||||||
7137|Georgina Limestone|48906|14|Not recorded|Tb.1,App.D|||||||||
7137|Georgina Limestone|48971|6|Mentioned|p10|||See aslo P27.||||||
7137|Georgina Limestone|49027|5|Briefly described|p8|||||||||
7137|Georgina Limestone|60122|6|Mentioned|p19|||||||||
7137|Georgina Limestone|60990|6|Mentioned|p85, |||||||||
7137|Georgina Limestone|63450|4|Described|p78 Fig. 5, p81|Late Cambrian|Middle Cambrian|Overlies Blazan Shale. Thickness at Mt Whelan: 406m. Geological province: Georgina Basin, East Toko Syncline. Dominated by fine-grained limestone with lesser calcarenite and intraformational conglomerate. See also p81.||||||21-MAR-16
7137|Georgina Limestone|64068|3|Fully described|p67-69, p64, 65, 73, 75|Late Cambrian|Middle Cambrian|Diverse fossil fauna. Lower part correlated with Devoncourt Limestone, Steamboat Sandstone. Correlated with Chabalowe Formation, Arrinthrunga Formation, Mungerebar Limestone, Devoncourt Limestone, Selwyn Range Limestone, O'Hara Shale, Pomegranate Limestone.||Of Narpa Group.||Conformably overlies Blazan Shale. Is overlain disconformably by Ninmaroo Formation.|Limestone, sandstone, interbedded mudstone and grainstone; overlain by grainstone and quartzic and silty limestone with breccia interbeds.|04-APR-12
7137|Georgina Limestone|64443|6|Mentioned|p3|Ordovician|Middle Cambrian|Of Ogilvie (1931) for fossiliferous carbonate rocks near the Georgina River. Mapped by Whitehouse (1936). Now defunct term embracing Middle Cambrian to Cambro-Ordovician rocks that straddle the NT-QLD border. Included by Noakes and Traves (1954) in their Barkly Group. Appears as Georgina Limestones on p3.||||Interdigitates with Arrinthrunga Formation.|Fossiliferous carbonate rocks.|14-MAY-14
7137|Georgina Limestone|65489|5|Briefly described|p125|Cambrian|Cambrian|Georgina Basin.||||Is overlain unconformably by Ninmaroo Formation.||
7137|Georgina Limestone|67323|5|Briefly described|GIS attrib tbl, p83,p88,p90,p92 Fig.12.2|Late Cambrian|Late Cambrian|See also Solid Geology Map. East Toko Syncline, Georgina Basin. Petroleum exploration target.||Narpa Group.||Unconformably overlies Thorntonia Limestone. Is overlain unconformably by Ninmaroo Formation.|Flaggy calcilutite and sandy calcilutite with chert, sandstone.|
7137|Georgina Limestone|67402|4|Described|p25 tbl RRM3|Iverian|Undillian|Georgina Basin, East Toko Syncline. Maximum thickness of 406m. Gas has been observed in fractures from this unit. Deposited in an open marine shelf environment. See also  p213 fig GRG3, p213 fig GRG5, p214, p215, p217.   ||||Overlies the Marqua beds. Unconformably overlies the Thorntonia Limestone or Hay River Formation. Overlain by the Arrinthrunga Formation.|Massive carbonate, dolomite, dolomitic limestone with minor argillaceous and sandy interbeds.|
7137|Georgina Limestone|67870|6|Mentioned|p43|Late Cambrian|Middle Cambrian|Georgina Basin.||||||
7137|Georgina Limestone|69443|5|Briefly described|p28:7, 16, 19, 26-28|Late Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.||Interdigitates with Arrinthrunga Formation. Is overlain disconformably by Ninmaroo Formation and unconformably by Kelly Creek Formation (Toko Group).||12-JUL-16
7137|Georgina Limestone|69573|6|Mentioned|p659, 661|||Georgina Basin.||||||
7137|Georgina Limestone|69591|4|Described|p87, p93-94|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. 30m thick. Crops out S of Glenormiston homestead around Tysons Bore and Pollys Lookout. Disputed relationship with Sun Hill Arkose is described. Low-energy intertidal or shallow subtidal environment with periodic episodes of higher energy. Contact not exposed. Time-equivalent to Pomegranate, Selwyn Range Limestones and O'Hara Shale. Contains a rich trilobite fauna.||Narpa Group.||Is overlain disconformably by Ninmaroo Formation.|Flaggy, grey, sandy limestone and pale aphanitic limestone (lower); cross-stratified, ripple-marked and ooid limestones.|
7137|Georgina Limestone|69673|6|Mentioned|p127|||||||||
7137|Georgina Limestone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Mungerebar Limestone|Limestone.|
7137|Georgina Limestone|71283|6|Mentioned|p479|Late Cambrian|Late Cambrian|Glenormiston, western Queensland. Contains the type species of Eugonocare tessellatum Whitehouse (1939).||||||
7137|Georgina Limestone|72321|6|Mentioned|Fig 2|Jiangshanian|Pabian|Toko Syncline, Georgina Basin. Australian stages: Idamean to Iverian.||of Narpa Group.||||
7137|Georgina Limestone|72358|5|Briefly described|p117. p125|||Of Georgina Basin. Equivalent to Goyder Formation in the Amadeus Basin. G. reticulatus Zone is recorded in petroleum well Netting Fence 1 (Green & Balfe, 1980) at the base of the Georgina Limestone (195 m), and extended to occur throughout the Georgina Limestone (Laurie 2012). Also includes G. stolidotus zone.||||Underlain by Mungerebar Limestone.||10-JAN-20
7137|Georgina Limestone|72516|6|Mentioned|p92 - p94|||Southeastern Georgina Basin.||||Lower part equivalent to the Steamboat Sandstone, also generally equivalent to the Arrinthrunga Formation and the Eurowie Sandstone Member.||07-JUN-21
7142|German Creek Formation|22973|5|Briefly described|p11 Fig.2(e)|Late Permian|Late Permian|||||||
7142|German Creek Formation|22974|6|Mentioned|p17|||||||||
7142|German Creek Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
7142|German Creek Formation|22978|6|Mentioned|p148 Fig.1|||||||||
7142|German Creek Formation|22979|5|Briefly described|p217|Late Permian|Late Permian|||||||
7142|German Creek Formation|22986|5|Briefly described|p291|||||||||
7142|German Creek Formation|22987|5|Briefly described|p299|||||||||
7142|German Creek Formation|22988|5|Briefly described|p304|||||||||
7142|German Creek Formation|22997|5|Briefly described|p369|Permian|Permian|||||||
7142|German Creek Formation|22998|5|Briefly described|p377|||||||||
7142|German Creek Formation|23000|5|Briefly described|p296|||||||||
7142|German Creek Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
7142|German Creek Formation|23444|6|Mentioned|p184|||||||||
7142|German Creek Formation|29730|6|Mentioned|p181|||||||||
7142|German Creek Formation|30508|6|Mentioned|p85|||Small inferred reserves of non-coking coal||||||
7142|German Creek Formation|30850|6|Mentioned|p343|||||||||
7142|German Creek Formation|30852|4|Described|p171|||Re:coal resources.||||||13-OCT-08
7142|German Creek Formation|30916|6|Mentioned|p91|||||||||
7142|German Creek Formation|31079|6|Mentioned|p5|||See also Fig. 6||||||
7142|German Creek Formation|31690|4|Described|p41|||See also p35.||||||13-OCT-08
7142|German Creek Formation|32689|1|Redefined|p435|Permian|Permian|Replaces German Creek Coal Measures.||||||13-OCT-08
7142|German Creek Formation|32730|6|Mentioned|p48|||||||||
7142|German Creek Formation|33390|4|Described|p3|||||||||
7142|German Creek Formation|33981|5|Briefly described|p574|||||||||
7142|German Creek Formation|35266|6|Mentioned|p190|||||||||
7142|German Creek Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin. Lithology described P184.||||||
7142|German Creek Formation|35822|5|Briefly described|p40|||||||||
7142|German Creek Formation|35922|6|Mentioned|p49|||||||||
7142|German Creek Formation|35937|6|Mentioned|p619|||||||||
7142|German Creek Formation|36739|6|Mentioned|p5|||See also P24,25.||||||
7142|German Creek Formation|37070|4|Described|p72|||||||||
7142|German Creek Formation|37072|4|Described|p91|||||||||
7142|German Creek Formation|37612|3|Fully described|p290|||See also Fig.3. and p283.||||||13-OCT-08
7142|German Creek Formation|37726|6|Mentioned|Fig.2|||||||||
7142|German Creek Formation|37859|6|Mentioned|p69|||||||||
7142|German Creek Formation|38518|6|Mentioned|Fig.3|||||||||
7142|German Creek Formation|38958|5|Briefly described|p493|||||||||
7142|German Creek Formation|39212|6|Mentioned|p13|||||||||
7142|German Creek Formation|39252|5|Briefly described|p20|||||||||
7142|German Creek Formation|39259|6|Mentioned|p90|||||||||
7142|German Creek Formation|39261|6|Mentioned|Fig.6|||||||||
7142|German Creek Formation|39269|5|Briefly described|p275|||Sedimentary environment||||||
7142|German Creek Formation|39272|5|Briefly described|p295|||Correlation||||||
7142|German Creek Formation|39273|6|Mentioned|Fig. 2|||||||||
7142|German Creek Formation|39445|5|Briefly described|Table 8|||||||||
7142|German Creek Formation|40321|6|Mentioned|p17|||See also Fig.3||||||
7142|German Creek Formation|40539|6|Mentioned|p164|||||||||
7142|German Creek Formation|40675|6|Mentioned|Table 5A|||||||||
7142|German Creek Formation|41191|5|Briefly described|p284|||||||||
7142|German Creek Formation|41226|6|Mentioned|Fig.8|||||||||
7142|German Creek Formation|41246|6|Mentioned|Map legend|Permian||||||||
7142|German Creek Formation|41689|6|Mentioned|Table 1|||||||||
7142|German Creek Formation|42091|6|Mentioned|p289|||||||||
7142|German Creek Formation|42120|6|Mentioned|Fig.5 P413|||||||||
7142|German Creek Formation|42187|6|Mentioned|p318|||||||||
7142|German Creek Formation|42249|6|Mentioned|p22|||||||||
7142|German Creek Formation|42250|6|Mentioned|Fig.4 P31|||||||||
7142|German Creek Formation|42251|4|Described|p36|||||||||
7142|German Creek Formation|42252|5|Briefly described|p50|||||||||
7142|German Creek Formation|42256|6|Mentioned|Fig.1 P243|||||||||
7142|German Creek Formation|42648|5|Briefly described|p40|||||||||
7142|German Creek Formation|42662|4|Described|p85|||||||||
7142|German Creek Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
7142|German Creek Formation|42974|5|Briefly described|p195|||||||||
7142|German Creek Formation|43000|6|Mentioned|p111|||||||||
7142|German Creek Formation|43050|6|Mentioned|p55|||||||||
7142|German Creek Formation|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin and Comet Ridge.||||||04-FEB-08
7142|German Creek Formation|60286|4|Described|p277|Late Permian|Late Permian|Conformably overlies Ingelara Formation. Equivalent to Catherine Sandstone. Overlain by Peawaddy Formation. Coastal and deltaic. Contains coal. Geological Province: Bowen Basin.||||||
7142|German Creek Formation|60731|5|Briefly described|p64|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
7142|German Creek Formation|61612|6|Mentioned|p272, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
7142|German Creek Formation|64665|5|Briefly described|p52, p53 Fig.2.|Middle Permian|Middle Permian|Bowen Basin. Deposited in a deltaic environment during the early stages of foreland basin development. An important coking coal-bearing unit.||||Overlies Ingelara Formation. Is overlain by Moranbah Coal Measures.||
7142|German Creek Formation|67402|6|Mentioned|p21, p45, p71|Capitanian|Capitanian|Bowen Basin. Deposited in a wave and fluvial-dominated delta system with the Crocker Formation and the Catherine Sandstone. See also  p85 tbl BWN2, p165 tbl LPB1.||||Overlain by the Burngrove, Fair Hill and Mac Millan Formations. Overlies the Maria Formation.||
7142|German Creek Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Moranbah Coal Measures. Underlain by Aldebaran Silststone or Bleinheim Formation.||
7142|German Creek Formation|67788|6|Mentioned|p22|Permian|Permian|Crossplot of channel belt width against thickness for channel sandstones.||||||
7142|German Creek Formation|68679|5|Briefly described|p377, p381-382, p384|Permian|Permian|Prouza and Park (1973). Bowen Basin. 240m thick. Mixed influence delta complex sediments. Properties of the coal are described in some detail.||||Overlies Maria Formation. Is overlain by Macmillan Formation. Passes laterally into Catherine Sandstone and Crocker Formation. To the north, merges with Exmoor Formation and Moranbah Coal Measures.|A lower quartzose to sublabile sandstone, siltstone succession without coal seams; and an upper succession of coal-bearing quartzose sandstone, siltstone and mudstone; marine fossils.|
7142|German Creek Formation|70815|6|Mentioned|p3-6, 9|||Bowen Basin. Vitrinite reflectance values mapped.|||||Produces high-quality coking coal.|
7142|German Creek Formation|70861|5|Briefly described|p37|Late Permian|Late Permian|Of Bowen Basin. ||Unit of Blackwater Group.||Overlain by MacMillan Formation. Correlable with Moranbah Coal Measures, Lower Peawaddy Formation.||
7142|German Creek Formation|70940|5|Briefly described|p844|Permian|Permian|Comet Ridge and northern Taroom Trough, southeast Bowen Basin.|257 - 256 Ma.|Blackwater Group.||Is overlain by MacMillan Formation.||
7142|German Creek Formation|71276|5|Briefly described|p294, p296-297|Permian|Permian|Prouza and Park (1973). Bowen Basin. The authors state that this unit, with the Flat Top Formation, "become the lower part of the Moranbah Coal Measures (Koppe, 1978) in the northern Bowen Basin"[?].||||Passes laterally into Catherine Sandstone.|Coal-bearing.|
7142|German Creek Formation|72297|5|Briefly described|p694-695, p703, p705|Permian|Permian|Central Bowen Basin. Excellent high-grade, vitrinite-rich, hard coking coal seams. Fluvial floodplain deposits. Coal seam correlation diagram, in which it appears as German Creek Coal Measures. Indicative properties of export coking and thermal coals tabulated.|||Liskeard, German Creek, Corvus, Tieri, Aquila, Pleiades Seams.|Is overlain by Macmillan Formation, Moranbah Coal Measures, Rangal Coal Measures.||
7142|German Creek Formation|73246|6|Mentioned|p190|Permian|Permian|Bowen Basin, northwest.||Blenheim Subgroup, Back Creek Group||Overlain by Moranbah Coal Measures (Blackwater Group).||
7142|German Creek Formation|73305|6|Mentioned|p548 Fig.1|Late Permian|Late Permian|Bowen Basin. Comet Ridge and northern Taroom Trough||||||
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|||
7190|Gidyea Bore mudstone|30778|6|Mentioned|p14|||||||||
7193|Gigoomgan Limestone|24078|5|Briefly described|p425 Tb. 1|Early Permian|Early Permian|Bio-terriginous to greywacke 'Atomodesma' prisms; some terriginous material; bio fragments. Max. thickness: 540m.  Geological Province: Gympie Basin.||||||
7193|Gigoomgan Limestone|24382|5|Briefly described|Map legend|Permian|Permian|Parent: Gympie Group||||||
7193|Gigoomgan Limestone|39252|6|Mentioned|p22|||||||||
7193|Gigoomgan Limestone|41736|2|Defined|p119|Late Permian|Middle Permian|||||||
7193|Gigoomgan Limestone|42054|6|Mentioned|p273|||||||||
7193|Gigoomgan Limestone|43017|5|Briefly described|Fig.3,p375|||||||||
7193|Gigoomgan Limestone|43050|5|Briefly described|p32|||||||||
7193|Gigoomgan Limestone|45440|14|Not recorded|p.13|||||||||
7193|Gigoomgan Limestone|60330|5|Briefly described|p261|||Of the Tamaree Formation. Dark grey, very fossiliferous limestone. Contains abundant bivalves and some fish fossils, and foraminiferida. See also Gigoomgan Limestone Formation.||||||
7193|Gigoomgan Limestone|63821|4|Described|p17, p40|Late Permian|Late Permian|Of the Gympie Group. Geological Province: Gympie Province. Comprises basal and upper bioclastic grainstones and a middle unit of calcareous sandstone and siltstone; shallow marine to neritic lagoonal depositional environment.||||||07-FEB-11
7193|Gigoomgan Limestone|68679|5|Briefly described|p370|Kungurian|Kungurian|Northern Gympie Province. Crops out from Sandy Creek to 15km N of Gigoomgan homestead. 195m thick. Marine, lagoonal.||||Correlated with South Curra Limestone.|Silty, sandy and muddy limestone, minor sparry limestone. Distinctive widespread sandstone marker within 20m of the top of the limestone with lithic grains and abundant shell fragments.|
7193|Gigoomgan Limestone|73303|4|Described|p61 Fig.2, p62-64, p66 Fig.6, p67-70|Lopingian|Cisuralian|New England Orogen. Gympie Terrane, northern. ca 263 Ma detrital zircon maximum depositional age. Brachiopod fauna assemblage equivalent to South Curra Limestone, assumed by Runnegar (1969) to be northern continuation of the South Curra Limestone. Fossil-rich horizons contain crinoids, bryozoa and brachiopods. Upper part contains Ingelarella ingelarensis brachiopod, constrains minimum age from type locality in Bowen Basin (Nicoll et al., 2015). Shallow marine depositional environment, likely carbonate shoal. Maximum depositional age from volcanogenic pebble conglomerate at the top of the unit.|277-257 Ma, ca 263 Ma detrital zircon|||Overlies Kolbar Formation, conformably underlies Teebar Formation.|Dominated by thick beds of coarse-grained calc-arenite limestone with some calcareous mudstone interbeds. Contains fossil-rich horizons and a single 0.5m-thick volcanogenic pebble conglomerate horizon. More siliceous calc-arenite in upper parts.|
7197|Gilbert River Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes two members: Coffin Hill and Yappar Members.  Fine to coarse clayey quartzose and lithic quartz sandstone, siltstone and shale.||||||
7197|Gilbert River Formation|9531|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Coffin Hill Member, Yappar Member.||||||02-JUL-04
7197|Gilbert River Formation|9541|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, minor conglomerate, siltstone and shale.||||||
7197|Gilbert River Formation|12575|5|Briefly described|p781, p784 Table 1.|Albian|Late Jurassic|Laura Basin. Apatite fission track analyses, vitrinite reflectance data are detailed.|157-131 Ma.|||Overlies Dalrymple Sandstone.|Predominantly marine glauconitic sandstone.|
7197|Gilbert River Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
7197|Gilbert River Formation|22747|5|Briefly described|p9||Mesozoic|||||||
7197|Gilbert River Formation|22780|5|Briefly described|map|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|22781|4|Described|p41|Early Carboniferous|Late Jurassic|In the Laura Basin.||||||19-SEP-06
7197|Gilbert River Formation|23031|5|Briefly described|31|||Geol province Carpentaria Basin||||||
7197|Gilbert River Formation|23032|5|Briefly described|p47|Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23065|5|Briefly described|18|||Geol province Carpentaria Basin||||||
7197|Gilbert River Formation|23071|6|Mentioned|p761|||||||||
7197|Gilbert River Formation|23220|6|Mentioned|p16||Mesozoic|||||||
7197|Gilbert River Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Eulo Queen Group. Thickness: 10-12m. in Gilberton Plateau. Geological Province: Georgetown Region.||||||08-JUL-15
7197|Gilbert River Formation|23393|4|Described|p22|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23420|6|Mentioned|p 131|||||||||
7197|Gilbert River Formation|23423|5|Briefly described|p259|Early Cretaceous|Late Jurassic|Carpentaria Basin.||||||
7197|Gilbert River Formation|23424|4|Described|Table 8.1 Fig 8.3 p340|Early Cretaceous|Late Jurassic|Age: Late Jurassic to Early Cretaceous? Maximum thickness ~10 m.||||||
7197|Gilbert River Formation|23425|4|Described|Table 9.7 p395|||Also see p378. Overlain by Wallumbilla Formation, conformably. Underlain by Garraway Sandstone, conformably. Geological Province Carpentaria Basin and Laura Basin. Max thickness 100 m.||||||30-JAN-07
7197|Gilbert River Formation|23426|4|Described|p403, Table 10.4 p407||Jurassic|Previously Battle Camp Sandstone. Overlain by Rolling Downs Group - conformable contact. Underlain by Dalrymple Sandstone - conformable contact. Geological Province: Laura Basin. Max. thickness 280 m.||||||30-JAN-07
7197|Gilbert River Formation|23428|6|Mentioned|p422|||||||||
7197|Gilbert River Formation|23430|4|Described|p455 & p520.|||Also found in Laura Basin, and Carpentaria Basin. Previously Battle Camp Sandstone in the Laura Basin. Underlain by Dalrymple Sandstone - in the Laura Basin. Eromanga Basin Province.||||||30-JAN-07
7197|Gilbert River Formation|23453|5|Briefly described|p19|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|23493|4|Described|p7|Early Cretaceous|Early Cretaceous|Sandstone, conglomerate and shale.  Unconformably overlain by Lynd Formation; unconformably underlain by Inoruni Sandstone.  Of the Carpentaria and Great Artesian Basins.||||||30-JAN-07
7197|Gilbert River Formation|23495|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|23496|5|Briefly described|Table 4, p59|Early Cretaceous|Late Jurassic|Thickness: ~107m.||||||19-SEP-06
7197|Gilbert River Formation|23498|5|Briefly described|p20 table 1||Cretaceous|Correlates with Blythesdale Sandstone.||||||
7197|Gilbert River Formation|23499|5|Briefly described|map legend|Early Cretaceous|Jurassic|Eromanga Basin||||||
7197|Gilbert River Formation|23500|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins. Age shown as Late Jurassic? - Early Cretaceous.||||||
7197|Gilbert River Formation|23501|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|Late Jurassic? - Early Cretaceous, Carpentaria Basin.||||||
7197|Gilbert River Formation|23510|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
7197|Gilbert River Formation|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
7197|Gilbert River Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|23616|5|Briefly described|Table 1C p12 p39|Early Cretaceous|Late Jurassic|Overlies Proterozoic rocks of the Dargalong Inlier. Carpentaria Basin.||||||
7197|Gilbert River Formation|23713|5|Briefly described|p8 Table 1|Early Cretaceous|Late Jurassic|See also p6.||||||19-SEP-06
7197|Gilbert River Formation|23846|5|Briefly described|p5|Early Cretaceous|Early Cretaceous|Overlies the Eulo Queen Group. Quartzose sandstone and conglomerate with some thin marine sediment beds. Geological Province: Eromanga Basin.||||||
7197|Gilbert River Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24013|5|Briefly described|p17 Tb. 1|Early Cretaceous|Early Cretaceous|Conglomerate, sandstone, arkose, siltstone.  Unconformably overlies Croydon Felsite.  Max. thickness: 250ft.  Geological Province: Great Artesian Basin.||||||
7197|Gilbert River Formation|24032|5|Briefly described|p5, p12, p23 Fig. 10, p29, p31 Fig. 11|Early Cretaceous|Late Jurassic|Max thickness: 3-40m. Consists of basal conglomerate overlain by cross bedded quartzose sandstone, and mudstone.||||||
7197|Gilbert River Formation|24048|6|Mentioned|p76|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24073|5|Briefly described|p378 Table 2|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24086|5|Briefly described|p312 Fig. 1|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|24089|5|Briefly described|Student Activites|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24213|5|Briefly described|p776 Fig. 1|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Contains the Batavia, Glennie and Briscoe Members.||||||
7197|Gilbert River Formation|24419|5|Briefly described|p19|Early Cretaceous|Late Jurassic|Of the Carpentaria and Eromanga Basin Sequences.||||||08-MAR-05
7197|Gilbert River Formation|24485|3|Fully described|p2, p38 Tb.6|Early Cretaceous|Late Jurassic|Max Thickness: ~107m. Basal unit of the Carpentaria Basin. Geological Province: Carpentaria Basin.||||||29-OCT-15
7197|Gilbert River Formation|24486|5|Briefly described|Map legend|Cretaceous|Late Jurassic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|29591|6|Mentioned|Table 72|||||||||
7197|Gilbert River Formation|30020|4|Described|p29|||||||||
7197|Gilbert River Formation|30021|6|Mentioned|p87|||||||||
7197|Gilbert River Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
7197|Gilbert River Formation|30102|4|Described|p27|||See also p31-34. Correlation with Jurassic-Cretaceous units.||||||19-SEP-06
7197|Gilbert River Formation|30582|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|30584|4|Described|Table 1|||Also mention p6.||||||19-SEP-06
7197|Gilbert River Formation|30585|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
7197|Gilbert River Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
7197|Gilbert River Formation|30916|6|Mentioned|p98|||Table on P98.||||||
7197|Gilbert River Formation|31121|4|Described|p390|||||||||
7197|Gilbert River Formation|31163|6|Mentioned|p247|||Jurassic - Cretaceous||||||
7197|Gilbert River Formation|31164|5|Briefly described|p9|||Neocomian ? - Abtian||||||
7197|Gilbert River Formation|31165|5|Briefly described|Table 1|||||||||
7197|Gilbert River Formation|31166|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|31168|4|Described|p10|||||||||
7197|Gilbert River Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone and conglomerate; siltstone.||||||02-DEC-04
7197|Gilbert River Formation|31433|4|Described|p7|||Jurassic-Cretaceous||||||
7197|Gilbert River Formation|31434|3|Fully described|Table 1|||U.Jurassic - L.Cretaceous. See also p8.||||||19-SEP-06
7197|Gilbert River Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
7197|Gilbert River Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|31832|6|Mentioned|Table 6|||||||||
7197|Gilbert River Formation|32314|6|Mentioned|Fig. 4|||||||||
7197|Gilbert River Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
7197|Gilbert River Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
7197|Gilbert River Formation|32518|5|Briefly described|p765|||||||||
7197|Gilbert River Formation|32531|6|Mentioned|Fig.2|||On P474||||||
7197|Gilbert River Formation|32553|4|Described|p38|||||||||
7197|Gilbert River Formation|32563|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|32705|5|Briefly described|p179|||||||||
7197|Gilbert River Formation|32706|6|Mentioned|p10|||||||||
7197|Gilbert River Formation|33075|6|Mentioned|p451|||||||||
7197|Gilbert River Formation|33086|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|33150|4|Described|p9|||||||||
7197|Gilbert River Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
7197|Gilbert River Formation|33176|5|Briefly described|p171|||||||||
7197|Gilbert River Formation|33177|5|Briefly described|Table 1|||||||||15-JUL-04
7197|Gilbert River Formation|33178|5|Briefly described|p11|||||||||
7197|Gilbert River Formation|33179|4|Described|Table 2|||||||||
7197|Gilbert River Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|33182|1|Redefined|p190|Early Cretaceous|Late Jurassic|Replaces Wrotham Park Sandstone. U.Jur.- L.Cret.||||||19-SEP-06
7197|Gilbert River Formation|33183|3|Fully described|p230|||Description includes history of nomenclature.||||||19-SEP-06
7197|Gilbert River Formation|33184|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33185|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|33226|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|33368|6|Mentioned|p25|||Strat.table.||||||
7197|Gilbert River Formation|33528|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33529|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33561|6|Mentioned|p102|||||||||
7197|Gilbert River Formation|33638|5|Briefly described|Table 1|||||||||
7197|Gilbert River Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|33648|5|Briefly described|p19|||||||||
7197|Gilbert River Formation|33772|4|Described|p13|||||||||
7197|Gilbert River Formation|33773|4|Described|Table 1|||||||||
7197|Gilbert River Formation|33882|4|Described|p14|||Mention p8.||||||19-SEP-06
7197|Gilbert River Formation|33900|6|Mentioned|p21|||||||||
7197|Gilbert River Formation|33907|6|Mentioned|p5|||||||||
7197|Gilbert River Formation|33908|6|Mentioned|p595|||||||||
7197|Gilbert River Formation|34356|6|Mentioned|p2|||Upper Jurassic - Lower Cretaceous. See also pp10,11,12 etc.||||||19-SEP-06
7197|Gilbert River Formation|34811|4|Described|Table 1|||||||||
7197|Gilbert River Formation|35204|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
7197|Gilbert River Formation|35214|6|Mentioned|p8|||||||||
7197|Gilbert River Formation|35220|4|Described|p16|||||||||
7197|Gilbert River Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|35434|6|Mentioned|p37|||||||||
7197|Gilbert River Formation|35559|4|Described|Table 1|||||||||
7197|Gilbert River Formation|35560|4|Described|p290|||||||||
7197|Gilbert River Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|35648|6|Mentioned|p18|||||||||
7197|Gilbert River Formation|35793|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|35811|5|Briefly described|Table 3|||||||||
7197|Gilbert River Formation|35814|6|Mentioned|p582|||||||||
7197|Gilbert River Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
7197|Gilbert River Formation|35920|6|Mentioned|p26|||||||||
7197|Gilbert River Formation|35921|6|Mentioned|p31|||||||||
7197|Gilbert River Formation|36012|3|Fully described|Table 5|||See also p18.||||||19-SEP-06
7197|Gilbert River Formation|36216|6|Mentioned|p211|||||||||
7197|Gilbert River Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|36243|6|Mentioned|Table 6A|||||||||
7197|Gilbert River Formation|36552|6|Mentioned|p59|||||||||
7197|Gilbert River Formation|36571|6|Mentioned|Table 4|||||||||
7197|Gilbert River Formation|37603|6|Mentioned|p444|||||||||
7197|Gilbert River Formation|37608|3|Fully described|Table 2|||||||||
7197|Gilbert River Formation|38199|5|Briefly described|p423|||Palynology||||||
7197|Gilbert River Formation|38291|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late and/or Early Cretaceous||||||
7197|Gilbert River Formation|38348|6|Mentioned|p25|||||||||
7197|Gilbert River Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
7197|Gilbert River Formation|39027|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||25-AUG-04
7197|Gilbert River Formation|39211|5|Briefly described|p34|||Fossils in strat. holes. See also Fig.11||||||
7197|Gilbert River Formation|39315|6|Mentioned|Fig.6|||||||||
7197|Gilbert River Formation|39425|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39445|5|Briefly described|Table 10|||||||||
7197|Gilbert River Formation|39496|6|Mentioned|p7|||See also p16.||||||19-SEP-06
7197|Gilbert River Formation|39556|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39562|5|Briefly described|Map legend|Cretaceous|Jurassic|Pebbly quartz sandstone. Part of the Trans-Australian Platform Cover.||||||15-JUN-06
7197|Gilbert River Formation|39687|6|Mentioned|Fig.5|||||||||
7197|Gilbert River Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39899|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Early Cretaceous||||||
7197|Gilbert River Formation|39943|6|Mentioned|Table 8A|||||||||
7197|Gilbert River Formation|40218|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|40221|6|Mentioned|p20|||||||||
7197|Gilbert River Formation|40648|3|Fully described|p12|||||||||
7197|Gilbert River Formation|40659|6|Mentioned|p250|||Mention p254.||||||19-SEP-06
7197|Gilbert River Formation|40924|6|Mentioned|p7|||||||||
7197|Gilbert River Formation|41125|6|Mentioned|p42|||||||||
7197|Gilbert River Formation|41204|6|Mentioned|p14|||||||||
7197|Gilbert River Formation|41266|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|41306|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|41307|4|Described|p17|||||||||
7197|Gilbert River Formation|41310|5|Briefly described|p14|||||||||
7197|Gilbert River Formation|41361|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|41675|6|Mentioned|p71|||||||||
7197|Gilbert River Formation|42061|4|Described|p155|||See also Fig.11||||||
7197|Gilbert River Formation|42369|3|Fully described|p57|||Supersedes Battle Camp Formation.||||||19-SEP-06
7197|Gilbert River Formation|42464|6|Mentioned|p8|||||||||
7197|Gilbert River Formation|42474|6|Mentioned|p28|||formerly Battle Camp Formation||||||
7197|Gilbert River Formation|42490|4|Described|p17||Cretaceous|Equivalent to the Battle Camp Formation (used 1965)||||||
7197|Gilbert River Formation|42500|5|Briefly described|p12|||Jurassic?||||||
7197|Gilbert River Formation|42556|5|Briefly described|p13|||||||||
7197|Gilbert River Formation|42632|6|Mentioned|p11|||||||||
7197|Gilbert River Formation|42637|4|Described|p10, 22|||||||||
7197|Gilbert River Formation|42640|5|Briefly described|p11|||||||||
7197|Gilbert River Formation|42650|4|Described|p16|||||||||
7197|Gilbert River Formation|42691|5|Briefly described|map legend|Mesozoic||||||||
7197|Gilbert River Formation|42693|5|Briefly described|map legend|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|42804|5|Briefly described|p115|||||||||
7197|Gilbert River Formation|42933|4|Described|p236|||||||||
7197|Gilbert River Formation|43060|4|Described|p58,Table 1c|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43083|5|Briefly described|p185|Cretaceous|Late Jurassic|Includes quartzose sand, gravel and minor clay desposits.||||||17-JUN-09
7197|Gilbert River Formation|43087|6|Mentioned|p12|||||||||
7197|Gilbert River Formation|43098|4|Described|p47|||||||||
7197|Gilbert River Formation|43105|5|Briefly described|p16|||||||||
7197|Gilbert River Formation|43110|4|Described|p53|||In the Laura Basin.||||||19-SEP-06
7197|Gilbert River Formation|43124|5|Briefly described|p31|||||||||
7197|Gilbert River Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43286|5|Briefly described|Map Legend|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|43287|5|Briefly described|Map Legend||Mesozoic|Late Jurassic? to Early Cretaceous.||||||
7197|Gilbert River Formation|43487|5|Briefly described|20|||||||||
7197|Gilbert River Formation|43564|6|Mentioned|p463|||||||||
7197|Gilbert River Formation|43596|4|Described|p40, p39 Tb. 4|Early Cretaceous|Late Jurassic|Overlies Dalrymple Sandstone. Geological province: Laura and Carpentaria Basins. Max. thickness: 283m. Mostly clayey quartzose sandstone; some coarser rocks towards base, lenses of coarser material including quartz gravels, throughout; top locally silicified.||||||07-APR-15
7197|Gilbert River Formation|43603|5|Briefly described|p9|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43625|6|Mentioned|p9|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43630|6|Mentioned|p16,69|||||||||
7197|Gilbert River Formation|43665|6|Mentioned|p24|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43730|5|Briefly described|p9,29||Mesozoic|||||||
7197|Gilbert River Formation|43738|5|Briefly described|p5|||||||||
7197|Gilbert River Formation|43740|5|Briefly described|Fig.2,p11|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43820|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
7197|Gilbert River Formation|43995|14|Not recorded|Tb.p9||Cretaceous|||||||
7197|Gilbert River Formation|44031|14|Not recorded|p3,Tb.1,p4|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|44047|14|Not recorded|Map Legend|||||||||
7197|Gilbert River Formation|44049|14|Not recorded|Map Legend||Early Cretaceous|||||||
7197|Gilbert River Formation|44050|14|Not recorded|p154,163,Pl.8|||||||||
7197|Gilbert River Formation|44082|6|Mentioned|p6,Tb.p34|Aptian|Neocomian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
7197|Gilbert River Formation|44112|6|Mentioned|p82|||||||||
7197|Gilbert River Formation|44246|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|44251|14|Not recorded|p2|||Correlated with Wrotham Park Sandstone.||||||
7197|Gilbert River Formation|44346|14|Not recorded|opp.p5|||||||||
7197|Gilbert River Formation|44373|14|Not recorded|p20|||Map only.||||||
7197|Gilbert River Formation|44376|14|Not recorded|p4,5|||||||||
7197|Gilbert River Formation|44414|14|Not recorded|p111,114||Cretaceous|||||||
7197|Gilbert River Formation|44417|14|Not recorded|p417|||Overlain by Rolling Downs Group.||||||
7197|Gilbert River Formation|44514|2|Defined|p35,36||Aptian|(Lower Aptian) Fossils.||||||
7197|Gilbert River Formation|44656|2|Defined|p325,327,Fig.49,T.10|||Unconformably overlies Croydon Felsite, Inoruni Sandstone and Croydon Granite.||||||19-SEP-06
7197|Gilbert River Formation|44727|14|Not recorded|p302-303|||Unconformably overlies Inoruni Sandstone. (Gulf of Carpentaria)||||||
7197|Gilbert River Formation|44926|5|Briefly described|Map Legend|||Late Jurassic? - Early Cretaceous||||||
7197|Gilbert River Formation|45004|2|Defined|p.8,14,15|||Tb.2||||||
7197|Gilbert River Formation|45009|2|Defined|p21,35,62-69,71,110,||Early Cretaceous|p134,Pls.5,10,13,14. Overlain by Lynd Formation. Name "Gilbert River Formation" preferred to "Blythesdale Group" as sediments equivalent only to upper beds of Blythesdale Group fossils.||||||30-JAN-07
7197|Gilbert River Formation|45014|14|Not recorded|p57,63,Pl.39,41,42||Cretaceous|||||||
7197|Gilbert River Formation|45025|6|Mentioned|p95|||Ref. to Laing and Power 1960.||||||19-SEP-06
7197|Gilbert River Formation|45145|3|Fully described|p18 Table 5|||||||||14-JUN-13
7197|Gilbert River Formation|45161|6|Mentioned|p67|||||||||
7197|Gilbert River Formation|45167|5|Briefly described|p54|||||||||
7197|Gilbert River Formation|45168|6|Mentioned|p6|||||||||
7197|Gilbert River Formation|46791|5|Briefly described|p42|||||||||
7197|Gilbert River Formation|46881|6|Mentioned|Table 2|||||||||
7197|Gilbert River Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7197|Gilbert River Formation|47083|4|Described|p19-20|Aptian|Neocomian|In the Carpentaria Basin.||||||22-FEB-07
7197|Gilbert River Formation|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
7197|Gilbert River Formation|48995|5|Briefly described|p72|||Age and thickness only described.||||||
7197|Gilbert River Formation|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
7197|Gilbert River Formation|49011|6|Mentioned|p28|||See also Fig.3.||||||
7197|Gilbert River Formation|49769|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|50100|5|Briefly described|p23|Early Cretaceous|Late Jurassic|Partly fluvial and partly shallow-marine clastic unit.  Overlain by Rolling Downs Group.  Geological Province: Carpentaria Basin / Eromanga Basin.||||||
7197|Gilbert River Formation|50198|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Consists of: Coffin Hill Member, Yappar Member.||||||
7197|Gilbert River Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Yappar Member, Coffin Hill Member.||||||
7197|Gilbert River Formation|50210|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Overlies: Eulo Queen Group.  Includes: Yappar Member, Coffin Hill Member.||||||
7197|Gilbert River Formation|50211|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Conformably overlies Loth Formation||||||
7197|Gilbert River Formation|50332|6|Mentioned|p77|Mesozoic|Mesozoic|Sedimentary rocks host a minor uranium mineralisation of the roll-front type.||||||07-FEB-11
7197|Gilbert River Formation|50587|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Geological Province: Quincan Province, Laura Basin. Fine to coarse-grained, clayey quartzose sandstone.||||||28-JUN-04
7197|Gilbert River Formation|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Includes: Coffin Hill Member, Yappar Member.||||||
7197|Gilbert River Formation|50596|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|Overlies: Dalrymple Sandstone.  Quartz sandstone, conglomerate, mudstone.||||||
7197|Gilbert River Formation|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group. Fine to coarse clayey quartzose and lithic-quartz sandstone; siltstone and shale.  Overlies Loth Formation.||||||06-JUL-04
7197|Gilbert River Formation|50630|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, minor conglomerate, siltstone, shale.||||||
7197|Gilbert River Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes the Yappar and Coffin Hll Members.  Quartzose sandstone, with minor conglomerate, siltstone, shale.||||||22-JUL-04
7197|Gilbert River Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes the Coffin Hill and Yappar Members.  Quartzose sandstone, shale, siltstone, minor conglomerate.||||||
7197|Gilbert River Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Coffin Hill Member, Yappar Member. Underlies: Wallumbilla Formation. Geological Province: Carpentaria Basin.||||||20-AUG-04
7197|Gilbert River Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Clayey quartzose sandstone, conglomeritic sandstone, pebble and cobble conglomerate; muddy sandstone, glauconitic sandstone, mudstone and siltstone. Geological Province: Laura Basin.||||||18-AUG-04
7197|Gilbert River Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone, grit, conglomerate, claystone.||||||
7197|Gilbert River Formation|60425|5|Briefly described|p70, p110|Early Cretaceous|Late Jurassic|Overlies Nychum Volcanics in the west. Geological province: Carpentaria Basin.||||||07-FEB-11
7197|Gilbert River Formation|62837|5|Briefly described|Stratigraphic columns|Barremian|Kimmeridgian|Includes Batavia, Glennie and Briscol Members, and Coffin Hill and Yappar Members.  Age: 140-~114Ma.  Geological Province: Northern Cape York, Southern Cape York and Burketown Depression.||||||01-MAR-10
7197|Gilbert River Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Bathurst Range Coal Measures and Dalrymple Sandstone. Is overlain by Rolling Downs Group.||
7197|Gilbert River Formation|64707|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Clayey quartz sandstone.||||||
7197|Gilbert River Formation|64820|5|Briefly described|pS6 Fig. 4|Neocomian|Neocomian|Of the Rolling Downs Group. Coarse-medium-grained quartz sandstone with minor siltstone and claystone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
7197|Gilbert River Formation|64822|5|Briefly described|pS89|Early Cretaceous|Early Cretaceous|Geological province: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
7197|Gilbert River Formation|65755|5|Briefly described|p7 Fig.4||Jurassic|Conglomerate, sandstone, siltstone, claystone.||||||
7197|Gilbert River Formation|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||||Is overlain by Rolling Downs Group.||
7197|Gilbert River Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Carpentaria Basin. See also misspelt Gilbert River Group in this paper.||||Is overlain by Wallumbilla Formation in Carpentaria and Laura Basins, at C-horizon boundary.||
7197|Gilbert River Formation|67323|5|Briefly described|p84-87, p94 Fig.12.4, p96, p106|Early Cretaceous|Late Jurassic|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Fluvial and lacustrine sediments. A regional aquifer.||||Is overlain by Wallumbilla Formation.|Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|67402|4|Described|p165 tbl LPB1, p176|Aptian|Tithonian|Carpentaria and Laura Basins. Deposited in a lagoonal to marginal marine setting. Forms an aquifer with generally good water quality across the Carpentaria Basin. Generally 300m thick. Formerly the Battle Camp Sandstone. See also p177, p179 fig CRP/KRM5, p180, p181, p226, p228-p233.|||Includes the Yappar Member and the Coffin Hill Member.|Unconformably overlies the Garraway Sandstone. Overlain by the Wallumbilla Formation and the Rolling Downs Group.|Very fine to coarse-grained quartz to sublabile sandstone with minor silstone and claystone.|
7197|Gilbert River Formation|67498|6|Mentioned|p925, p926 Fig.5, p929, 930, p932 Fig.10|Early Cretaceous|Late Jurassic|Also shown informally as 'Jurassic mesa'.|||||Includes sandstones.|08-MAY-12
7197|Gilbert River Formation|67784|5|Briefly described|p25, p26, p31, p33|Aptian|Neocomian|Northern Eromanga Basin. Littoral deposits.||Wilgunya Subgroup.||Overlain by Wallumbilla Formation|Sandstone|08-FEB-18
7197|Gilbert River Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Potential hydrocarbon reservoir.|||||Sandstone (quartzite), conglomerate, organic-rich siltstone, shale.|
7197|Gilbert River Formation|68135|5|Briefly described|p52 fig 2b, p65|Early Cretaceous|Tithonian|Carpentaria and Laura Basins. Contains plant and invertebrate fossils. Lagoonal to marginal marine deposits.||||Overlies Dalrymple Sandstone, Garraway beds, Helby beds|Interbedded sandstone and siltstone.|14-SEP-17
7197|Gilbert River Formation|68337|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic?|Carpentaria Basin.|||||Reddish brown, medium- to coarse-grained, clayey, quartzose sandstone, pebbly sandstone; minor quartz pebble conglomerate, siltstone, fine-grained quartzose sandstone; ferruginised in places.|
7197|Gilbert River Formation|68341|5|Briefly described|Map legend.|Early Cretaceous|Middle Jurassic||||||Clayey quartz sandstone.|
7197|Gilbert River Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.|Is overlain conformably by Wallumbilla Formation.|Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.|Conformably overlies Eulo Queen Group. Is overlain conformably by Wallumbilla Formation.|Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.||Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor feruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68405|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins.|||Includes Coffin Hill and Yappar Members.|Unconformably overlain by Bulimba Formation.|Medium to coarse-grained, clayey quartzose sandstone and pebbly sandstone (commonly cross-bedded); minor quartz pebble conglomerate, siltstone, mudstone.|24-AUG-15
7197|Gilbert River Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.  |||Includes Coffin Hill Member, Yappar Member.|Conformably overlain by the Wallumbilla Formation. Conformably underlain by the Loth Formation, Eulo Queen Group.|(Undifferentiated):clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Eromanga, Carpentaria and Laura Basins. ||||||
7197|Gilbert River Formation|68821|6|Mentioned|p292 Fig.1|Cretaceous|Cretaceous|Lower Cretaceous age.||||||
7197|Gilbert River Formation|69056|5|Briefly described|p57, Reference images sheet.|Early Cretaceous|Late Jurassic|Carpentaria Basin. Shown on the simplified surface geology map of the Quamby Project area. Unconformably overlies the ~3km-thick Millungera Basin sequence.||||||
7197|Gilbert River Formation|69079|6|Mentioned|p16|||Mesozoic gold placer deposits in this unit have been reworked and concentrated in the Palmer River goldfield.||||||
7197|Gilbert River Formation|69297|5|Briefly described|p273, p274 fig 4. 3|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. This unit is a good potential hydrocarbon reservoir. ||||Overlain by the Wallumbilla Formation. Overlies the Garraway Sandstone.|Quartzose sandstone and quartzose glauconitic sandstone.|
7197|Gilbert River Formation|69377|5|Briefly described|map legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated|
7197|Gilbert River Formation|69455|5|Briefly described|p39:2; 39:4 Fig.39.3; 39:14-15|||Offshore Western Gulf Sub-basin, Carpentaria Basin. Contains sandstones with good reservoir potential, sealed by Wallumbilla Formation equivalent shales. Also is a possible source rock.||||Overlies Eulo Queen Group.|Includes fluvial quartzic sandstones.|12-JUL-16
7197|Gilbert River Formation|69591|5|Briefly described|p99, p101|Early Cretaceous|Late Jurassic|Carpentaria Basin.||||Is overlain by Wallumbilla Formation.||
7197|Gilbert River Formation|69594|4|Described|p518, p520-522, p526-528, p540, p573|Barremian|Tithonian|Carpentaria, Laura and northern Eromanga Basins. Diachronous: deposition progressed southwards. 30-123m thick; 58-280m in the Laura Basin. Fluvial to marine deposition. One of the main aquifers in the Basin. RELATED UNITS (continued): Equivalent to Yappar and Coffin Hill Members; Helby beds (and interfingers with it); and (lower sandstone part of) Battle Camp Formation.|||Yappar and Coffin Hill Members.|Overlies Garraway and Dalrymple Sandstones conformably and Eulo Queen Group disconformably/unconformably. Is overlain conformably by Wallumbilla Formation (Rolling Downs Group). See COMMENTS.|Dominated by clayey quartzose sandstones, fining upwards into siltstone and glauconitic sandstone. In Laura Basin: fine to coarse, quartzose to sublabile sandstone, minor mudstone, siltstone and conglomerate.|
7197|Gilbert River Formation|69673|6|Mentioned|p202 fig 165|||||||Overlies Garraway Sandstone||
7197|Gilbert River Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Late Jurassic|Georgetown region.||||||
7197|Gilbert River Formation|70345|6|Mentioned|p3|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|70354|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|70356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|70570|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|05-MAY-16
7197|Gilbert River Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|20-JAN-22
7197|Gilbert River Formation|70673|6|Mentioned|p7, p100|Early Cretaceous|Late Jurassic|Lakeland Downs-Maytown region.||||||
7197|Gilbert River Formation|71409|5|Briefly described|p1058-1059, p1061|Jurassic|Jurassic|Carpentaria Basin. Likely distal source rocks for heavy minerals in central-eastern Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.|||||Sandstones.|23-APR-18
7197|Gilbert River Formation|71792|4|Described|p57-p58|Early Cretaceous|Late Jurassic|Carpentaria Basin. |||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|71849|5|Briefly described|p8, p43, p49, p119, p133, p144, p195|Early Cretaceous|Late Jurassic|Forms the base of the Carpentaria Basin sequence.||||Nonconformably overlies Morris, Wolverton and Meldrum Granites and Rokeby Quartz Monzodiorite.|Sandstone.|
7197|Gilbert River Formation|71853|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|The two facies are mapped separately.|||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated. Another facies has identical lithologies but deeply weathered.|
7197|Gilbert River Formation|71854|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|The two facies are mapped separately.|||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated. Another facies has identical lithologies but is deeply weathered.|
7197|Gilbert River Formation|71863|5|Briefly described|p5|Aptian|Berriasian|Carpentaria Basin.||||Overlain by the Wallumbilla Formation.||
7197|Gilbert River Formation|72088|6|Mentioned|p25|||Forms part of The Pyramid rock formation.||||Overlies the Blantyre Sandstone.||
7197|Gilbert River Formation|72297|5|Briefly described|p746, p748, p761|||Carpentaria, Laura Basins. Potential source rocks: minor hydrocarbons reported in AAO Karumba 8 (oil staining and fluorescence). Excellent hydrocarbon reservoir potential because it contains aquifers. Temperatures in its aquifers highlight a broad heat anomaly through the Carpentaria and Eromanga Basins; potential for geothermal energy.||||Overlies Eulo Queen Group.|Includes interbedded fine carbonaceous sedimentary rocks (mudstones).|
7197|Gilbert River Formation|72298|5|Briefly described|p801|Cretaceous|Jurassic|Carpentaria Basin. Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Loth FZ (Eulo Queen Group) and Garraway beds. Is overlain by Wallumbilla FZ (Rolling Downs Group).||
7197|Gilbert River Formation|72526|6|Mentioned|p6 Fig.1.2.|Jurassic|Jurassic|||||||
7197|Gilbert River Formation|72683|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|?Eromanga Basin or Carpentaria Basin?||||Unconformably overlies Wimberu Granite, Narpa Group, Mount Albert Group, Kuridala Group, Malbon Group.|Clayey quartz sandstone, some sublabile and glauconitic sand stone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|72889|6|Mentioned|p8.||||||||Includes calc-silicate dominated rocks.|
7197|Gilbert River Formation|72913|6|Mentioned|p8.|||Four wells intersected this cover unit.||||||
7197|Gilbert River Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
7197|Gilbert River Formation|72983|6|Mentioned|p15|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|73083|6|Mentioned|p57, p60-62, p77|Cretaceous|Jurassic||||||Includes fossiliferous sandstone and conglomerate.|
7197|Gilbert River Formation|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquifer with potential tight gas/oil. Basal unconformity.||||Overlain by Wallumbilla Formation (Rolling Downs Group).||14-OCT-22
7197|Gilbert River Formation|73147|5|Briefly described|p126-127, 129-131, 138, 141, 143-144|Aptian|Aptian|Gregory Range area, SE Carpentaria Basin.|||Yappar Member|Overlies Eulo Queen Group.||
7197|Gilbert River Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
7225|Gilgurry Mudstone|22601|6|Mentioned|416|Permian|Permian|||||||
7225|Gilgurry Mudstone|22857|4|Described|p536 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wandsworth Volcanic Group. Grey siltstone, feldspathic sandstone, quartzite, carbonaceous mudstone; minor tuff. Max. thickness: 573m. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|23103|5|Briefly described|p551, Fig.1|Permian|Permian|||||||
7225|Gilgurry Mudstone|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Parent: Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|23812|6|Mentioned|p30|||||||||
7225|Gilgurry Mudstone|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|29441|6|Mentioned|p113|||||||||
7225|Gilgurry Mudstone|30911|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|32086|6|Mentioned|p325|||Marine mudstones||||||
7225|Gilgurry Mudstone|32484|6|Mentioned|Fig.1|||||||||
7225|Gilgurry Mudstone|32491|5|Briefly described|p13|||Permian||||||
7225|Gilgurry Mudstone|32492|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7225|Gilgurry Mudstone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|32944|6|Mentioned|p709|||||||||
7225|Gilgurry Mudstone|32945|6|Mentioned|p90|||||||||
7225|Gilgurry Mudstone|33436|3|Fully described|Fig.1|||Upper Permian.||||||13-NOV-08
7225|Gilgurry Mudstone|33476|2|Defined|p45|Permian|Permian|||||||
7225|Gilgurry Mudstone|33766|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
7225|Gilgurry Mudstone|34340|6|Mentioned|Table 6.1|||Permian||||||
7225|Gilgurry Mudstone|34350|6|Mentioned|p17|||Permian||||||
7225|Gilgurry Mudstone|34556|5|Briefly described|p268|||||||||
7225|Gilgurry Mudstone|35257|6|Mentioned|Fig.18|||||||||
7225|Gilgurry Mudstone|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
7225|Gilgurry Mudstone|36961|6|Mentioned|Fig.5|||||||||
7225|Gilgurry Mudstone|37252|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|38837|6|Mentioned|p234|||||||||
7225|Gilgurry Mudstone|39279|4|Described|p367|||||||||
7225|Gilgurry Mudstone|40504|6|Mentioned|p97|||||||||
7225|Gilgurry Mudstone|40505|5|Briefly described|p81|||||||||
7225|Gilgurry Mudstone|40773|3|Fully described|p450|||Mention p458.||||||13-NOV-08
7225|Gilgurry Mudstone|41413|6|Mentioned|p327|||||||||
7225|Gilgurry Mudstone|42378|5|Briefly described|Table 1 P10, Fig.1 5|||Redefined Offenberg 1968 (P21)||||||
7225|Gilgurry Mudstone|42963|5|Briefly described|Fig.2|||||||||
7225|Gilgurry Mudstone|43008|5|Briefly described|map legend|||||||||
7225|Gilgurry Mudstone|43017|5|Briefly described|Fig.2,p374|||||||||
7225|Gilgurry Mudstone|43385|14|Not recorded|p179,180||Kungurian|||||||
7225|Gilgurry Mudstone|43745|6|Mentioned|p16||Late Permian|||||||
7225|Gilgurry Mudstone|43881|14|Not recorded|p6-7,9||Permian|Lower formation of Boorook Group.||||||
7225|Gilgurry Mudstone|43894|14|Not recorded|p787||Permian|Part of Boorook Group. Late Kungurian or Early Kazanian.||||||
7225|Gilgurry Mudstone|44093|5|Briefly described|p233 App. 1|Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|48940|3|Fully described|p48|||Refers Voisey (1957).||||||14-APR-08
7225|Gilgurry Mudstone|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
7225|Gilgurry Mudstone|60937|5|Briefly described|p426, p437|Late Permian|Late Permian|See also Gilgurry mudstones. Geological Province: texas Block. See also p434.||||||14-APR-08
7225|Gilgurry Mudstone|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
7225|Gilgurry Mudstone|67908|6|Mentioned|p285|Permian.|Permian.|Late Permian. Not affected by the deformation producing the Texas Orocline.||||||
7225|Gilgurry Mudstone|69793|6|Mentioned|p1113 Fig.3|Permian|Permian|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
7225|Gilgurry Mudstone|71628|6|Mentioned|p11: 26, 29; p15: 33, 57; p16: 2, 4|||||||Is intruded by Cullendore Supersuite, Rocky River Monzogranite, and Mount Lindesay Monzogranite (Stanthorpe Complex).||
7245|Gin Creek Granite|22515|6|Mentioned|p397|Statherian||||||||
7245|Gin Creek Granite|22667|6|Mentioned|Fig1 P234, P240||Statherian|Age of unit is 1741+/-7 Ma||||||
7245|Gin Creek Granite|23064|6|Mentioned|136|||||||||
7245|Gin Creek Granite|23069|5|Briefly described|p775 (fig 1)|||||||||
7245|Gin Creek Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|1741+/-7Ma||||||
7245|Gin Creek Granite|23396|5|Briefly described|p426|Statherian|Statherian|~1741Ma||||||
7245|Gin Creek Granite|23519|5|Briefly described|p128|Proterozoic|Proterozoic|Age: 1741+/-7 Ma. See also page 106 Fig 1. Geological Province: Williams Batholith.||||||
7245|Gin Creek Granite|23967|6|Mentioned|p1331|||Geological Province: Williams batholith.||||||
7245|Gin Creek Granite|23973|5|Briefly described|p1436 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: 1740Ma.||||||
7245|Gin Creek Granite|23974|5|Briefly described|p1451|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: 1741 +/- 7Ma.||||||
7245|Gin Creek Granite|24197|5|Briefly described|p17, p96 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1740Ma. Muscovite-tourmaline phase. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
7245|Gin Creek Granite|24254|5|Briefly described|p17 Fig.1, p23|Proterozoic|Proterozoic|Age: 1741 +/- 7 Ma (SHRIMP U/Pb). Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
7245|Gin Creek Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
7245|Gin Creek Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
7245|Gin Creek Granite|37862|4|Described|p588|||||||||
7245|Gin Creek Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7245|Gin Creek Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
7245|Gin Creek Granite|39043|6|Mentioned|p9|||||||||
7245|Gin Creek Granite|39445|6|Mentioned|Table 2|||||||||
7245|Gin Creek Granite|40840|6|Mentioned|Map legend|||||||||
7245|Gin Creek Granite|41306|6|Mentioned|p4|||||||||
7245|Gin Creek Granite|41978|4|Described|p493|||||||||
7245|Gin Creek Granite|43490|6|Mentioned|8|||older granites 1740Ma. Of Narraku Batholith||||||
7245|Gin Creek Granite|44195|5|Briefly described|p345 Table 1,354|||U-Pb ages given 1741+/-7 Ma.||||||
7245|Gin Creek Granite|45161|5|Briefly described|p52|||See also P41||||||
7245|Gin Creek Granite|45166|5|Briefly described|p38|||||||||
7245|Gin Creek Granite|49009|2|Defined|p15|Proterozoic|Proterozoic|Previously mapped as Kalkadoon Granite(Carter & Opik,1963)||||||
7245|Gin Creek Granite|49041|5|Briefly described|Table 3|||||||||
7245|Gin Creek Granite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Deformed biotite-muscovite pluton body.  Intrudes Answer Slate.  Geological Province: Eastern Fold Belt Province.  See also p49.||||||
7245|Gin Creek Granite|50536|5|Briefly described|p1.5, 11.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Gin Creek Suite.   Age: 1741 +/- 7Ma.||||||07-NOV-08
7245|Gin Creek Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
7245|Gin Creek Granite|60658|6|Mentioned|p61|||Granite Pluton. Geological Province: Eastern Fold Belt / Mount Isa Inlier||||||
7245|Gin Creek Granite|61933|5|Briefly described|p169 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1740 Ma.||||||07-NOV-08
7245|Gin Creek Granite|61936|5|Briefly described|p195 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: ~1745-1740Ma. Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
7245|Gin Creek Granite|63866|5|Briefly described|p62||||1741 +/- 7 Ma|||||
7245|Gin Creek Granite|64248|6|Mentioned|p33 Fig.1, p36, p38 Fig.5|Statherian|Statherian||1741 +/- 7 Ma.|||||
7245|Gin Creek Granite|64250|5|Briefly described|p10 fig 2, p12, p14-15, p27|||Cloncurry Fold Belt, Mount Isa Inlier. Inferred by Beardsmore et al.(1988) to have been tectonically emplaced; contradicted by this study.|1741 +/- 7 Ma|||||12-MAY-14
7245|Gin Creek Granite|65396|5|Briefly described|p7, p40, p53, p82, p84, p90, p172-173|Statherian|Statherian|See also p175-176, p180, p182, p202, p218, p241, p361, p438-440, p444-446, p454-491. Eastern succession, Cover Sequence 2. Cloncurry Fold Belt. Stress partitioning and fluid flow models detailed.|1741 +/- 7 Ma (Page and Sun, 1998).|||Intrudes Double Crossing Metamorphics. Is conformably overlain by Answer Slate, Staveley Formation.||03-APR-17
7245|Gin Creek Granite|65505|6|Mentioned|980|Proterozoic|Proterozoic|Age: 1741 +/- 7 Ma, intrudes the Mt Isa Inlier.||||||
7245|Gin Creek Granite|66913|5|Briefly described|p171 fig 2|Statharian|Statherian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2.||||||
7245|Gin Creek Granite|67323|4|Described|GIS attrib tbl, p15, p18-20, p24|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Marimo-Staveley Domain, Mount Isa Inlier. Gneissic domes: probably metamorphic core complexes. Could have formed during the Wonga Event. A probable source of sediment for Staveley Formation. Relatively weak magnetic response.|1741 +/- 7 Ma.|Wonga Suite, Burstall Suite.||Is surrounded by Double Crossing Metamorphics.|Foliated and non-foliated biotite granite, tourmaline-muscovite granite; minor pegmatite, aplite; schistose and gneissic inclusions common. Unique in  Mount Isa Inlier by being weakly to strongly peralkaline; S-type.|
7245|Gin Creek Granite|67498|5|Briefly described|p918 Fig.1, p919, p927, p928, p934|Statherian|Statherian|Defined by Blake (1987). Old name for Wonga Granite? Replaces Wonga Granite? Or of Wonga Suite? Emplaced during Wongan Event|1750 - 1730 Ma.|Of the Wonga Suite? Shown as part of Williams Granite Suite Fig 7|||Peraluminous muscovite-bearing granite. Consists mainly of non-foliated, partly porphyritic biotite granites and weakly foliated tourmaline-muscovite leucogranites.|07-MAY-12
7245|Gin Creek Granite|67539|5|Briefly described|p11, p14|Statherian|Statherian|Dated from 1740 Ma primary zircons.|ca. 1740 Ma|||Intrudes and contact metamorphoses the Double Crossing Metamorphics.||
7245|Gin Creek Granite|68146|5|Briefly described|p76|||Eastern Fold Belt, Mount Isa Inlier.|C.1740 Ma (Page and Sun, 1998).|||Intrudes Double Crossing Metamorphics.||
7245|Gin Creek Granite|68542|5|Briefly described|p1, p16 fig 4, p17 fig 5, p18||||||||Granite.|
7245|Gin Creek Granite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, the Burstall Suite and Wonga Suite are all mapped under the same symbol, -Pgw.||||||
7245|Gin Creek Granite|68575|5|Briefly described|p2-3, p45, p47, p63-64, p125-126||||1741 +/- 7 Ma (Page and Sun, 1998).|||Intrudes Double Crossing Metamorphics.||
7245|Gin Creek Granite|68576|5|Briefly described|Q_2: p1, p16-18|Paleoproterozoic|Paleoproterozoic|Mount Isa area. Appears as Gin Creek 'Granite' on p16, and as Wonga Granite (Gin Creek Granite) on p18.|1740 Ma.|||||
7245|Gin Creek Granite|68732|6|Mentioned|p158 Fig.1, p165 Fig.3|Statherian|Statherian|Mount Isa Inlier. Igneous crystallisation age.|1741 +/- 7 Ma|||||
7245|Gin Creek Granite|69056|5|Briefly described|p5, p54, Time-Space plot sheet|Statherian|Statherian|Marimo-Staveley Domain. Metamorphosed and intruded during the ~1740 Ma Wonga Event.|1741 +/- 7 Ma (Page and Sun, 1998).|||Is enveloped by Double Crossing Metamorphics.||
7245|Gin Creek Granite|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Foliated and non-foliated biotite granite, tourmaline-muscovite granite; minor pegmatite, aplite; schistose and gneissic inclusions common|
7245|Gin Creek Granite|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Foliated and non-foliated biotite granite, tourmaline-muscovite granite; minor pegmatite, aplite; schistose and gneissic inclusions common|
7245|Gin Creek Granite|69591|5|Briefly described|p28, p33, p35, p37, p60|Paleoproterozoic|Paleoproterozoic|Marimo-Staveley Domain, Leichhardt Superbasin, Mount Isa Province. This age is identical to that of a migmatitic leucosome in the Double Crossing Metamorphics, both related to the Wonga Extension Event. Separated from the overlying Staveley Formation by an inferred folded decollement.|1741 +/- 7 Ma (Page and Sun, 1998).|||Is surrounded by (?intrudes) Double Crossing Metamorphics.|Foliated and non-foliated biotite granite, tourmaline-muscovite granite; minor pegmatite, aplite; schistose and gneissic inclusions common.|
7245|Gin Creek Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1741+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)|||||
7245|Gin Creek Granite|72297|6|Mentioned|p758|||At Amethyst Castle, 100km S of Cloncurry, amethyst occurs in banded, laminated and comb-textured veins.||||||
7245|Gin Creek Granite|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1725 +/- 3 Ma|||||
7245|Gin Creek Granite|72889|4|Described|p2-3, p5, p6, p8, p27-28, p30-31.|Statherian|Statherian|This dated sample: weathered, coarse-grained, leucocratic granite. Age determined in this sample (1758 +/- 47 Ma) is imprecise and uncertain due to the low zircon yield, but in broad agreement with 1741+/-7 Ma crystallisation age reported by Page and Sun (1998). Refer to 1:250 000 sheet DUCHESS (SF5406). Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results.|1741+/-7 Ma magmatic crystallisation age.|||Intrudes Double Crossing Metamorphics and possibly Staveley Formation, but may underlie Staveley.|Variably deformed porphyritic to equigranular biotite granite and tourmaline-bearing leucogranite.|
7245|Gin Creek Granite|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
7245|Gin Creek Granite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Kuridala-Selwyn-Marimo-Doherty Domain.|1743+/-9 Ma, 1741+/-7 Ma crystallisation age||||Felsic intrusive.|
7245|Gin Creek Granite|73529|5|Briefly described|p15 Fig.1, p17|Statherian|Statherian||~1740 Ma|||Intrudes Double Crossing Metamorphics||
7257|Gingerella Volcanics|23291|4|Described|p38, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Of the Sundown Volcanic Group. Geological Province: Georgetown Region.||||||13-NOV-08
7257|Gingerella Volcanics|23502|5|Briefly described|Map Legend||Late Carboniferous|Part of the Gingerella Cauldron Complex, Sundown Volcanic Group.||||||13-NOV-08
7257|Gingerella Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. 89.  Assumed to be I-Type.||||||
7257|Gingerella Volcanics|23616|5|Briefly described|Table 3 p54||Late Carboniferous|Of Sundown Volcanic Group. Conformably underlain by Double Barrel Andesite. Dargalong Province. Max thickness ~75 m.||||||13-NOV-08
7257|Gingerella Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7257|Gingerella Volcanics|37613|6|Mentioned|p257|||See also Fig.1.||||||
7257|Gingerella Volcanics|39445|5|Briefly described|Table 7|||||||||
7257|Gingerella Volcanics|42547|5|Briefly described|p74|||||||||
7257|Gingerella Volcanics|42691|5|Briefly described|map legend|Paleozoic||||||||07-NOV-08
7257|Gingerella Volcanics|43110|6|Mentioned|p7|||||||||
7257|Gingerella Volcanics|43259|4|Described|Appendix 1,p9.||Late Carboniferous|||||||
7257|Gingerella Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
7257|Gingerella Volcanics|44926|5|Briefly described|Map Legend|||||||||
7257|Gingerella Volcanics|45014|2|Defined|p54-56,Tb.1,Pl.38|Late Carboniferous|Early Carboniferous|(Middle Carboniferous-Late Carboniferous)||||||
7257|Gingerella Volcanics|45025|6|Mentioned|fig.9, p69|||Ref. to Brance 1966||||||
7257|Gingerella Volcanics|46845|6|Mentioned|Table 1|||||||||
7257|Gingerella Volcanics|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Two un-named facies associations within this unit are mapped separately: crystal-rich, rhyolitic ignimbrite and flow-banded rhyolitic lava, minor andesitic to rhyodacitic tuff, dacite, volcanic breccia; and massive lithics-rich, crystal-rich welded, rhyolitic to rhyodacitic ignimbrite.||Unit in Gingerella Cauldron Complex.|||Rhyolitic-rhyodacitic ignimbrite, lava and high-level intrusive rocks; minor tuff, rhyodacite, dacite, volcanic breccia with blocks of flow-banded rhyolite and granite up to 2 m across.|
7257|Gingerella Volcanics|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Two un-named facies associations within this unit are mapped separately: crystal-rich, rhyolitic ignimbrite and flow-banded rhyolitic lava, minor andesitic to rhyodacitic tuff, dacite, volcanic breccia; and massive lithics-rich, crystal-rich welded, rhyolitic to rhyodacitic ignimbrite.||Unit in Gingerella Cauldron Complex.|||Rhyolitic-rhyodacitic ignimbrite, lava and high-level intrusive rocks; minor tuff, rhyodacite, dacite, volcanic breccia with blocks of flow-banded rhyolite and granite up to 2 m across.|
7257|Gingerella Volcanics|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Sundown Volcanic Group.||Unconformably underlain by the Blackman Gap Complex.|Welded, dacitic? to rhyolitic ignimbrite; minor tuff, dacite lava, volcanic breccia.|
7313|Glandore Granodiorite|23037|6|Mentioned|p35,71||Late Carboniferous|Subdivided and reclassified as the Glandore Quartz Monzonite.||||||
7313|Glandore Granodiorite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Cggd].  Grey to pinkish, medium-grained, biotite-hronblende granite, granodiorite or monzonite.||||||
7313|Glandore Granodiorite|29964|6|Mentioned|p5|||Upper Carboniferous||||||
7313|Glandore Granodiorite|30451|3|Fully described|p80|||Upper Carboniferous age||||||
7313|Glandore Granodiorite|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7313|Glandore Granodiorite|33728|6|Mentioned|Fig.1|||||||||
7313|Glandore Granodiorite|33774|3|Fully described|p60|||Late Carb. 284-312my||||||
7313|Glandore Granodiorite|36333|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
7313|Glandore Granodiorite|36528|6|Mentioned|p170|||||||||
7313|Glandore Granodiorite|38153|6|Mentioned|p373|||||||||
7313|Glandore Granodiorite|38447|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
7313|Glandore Granodiorite|39445|5|Briefly described|Table 12|||||||||
7313|Glandore Granodiorite|40246|6|Mentioned|p172|||||||||
7313|Glandore Granodiorite|41246|6|Mentioned|Map legend|Carboniferous||||||||
7313|Glandore Granodiorite|42547|5|Briefly described|p56|||||||||
7313|Glandore Granodiorite|43008|5|Briefly described|map legend|||||||||
7313|Glandore Granodiorite|50214|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
7313|Glandore Granodiorite|50273|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
7313|Glandore Granodiorite|60282|6|Mentioned|p6, p38|Late Carboniferous|Late Carboniferous|Age: 324+/-4Ma.  See also Glandore Granodiorite Complex.||||||13-APR-05
7313|Glandore Granodiorite|65388|4|Described|p251-253, 236, 237, 238, 247,259,277,315|Late Carboniferous|Late Carboniferous|Auburn Arch. Similar lithology to Hainault Granodiorite and  Hildura Quartz Monzodiorite. Intrudes Torsdale Volcanics. Relationship with surrounding granites unclear. SHRIMP U-Pb date: 323+/-4 Ma. K-Ar dates 300-306 (Webb & McDougall, 1968). Two K-Ar ages reported by Green (1975) and Whitaker & others (1974), interpreted to belong to the "Glandore Granodiorite" are now considered to be from Crystal Vale Monzogranite.  Biotite age: 246Ma, hornblende age: 319Ma.||||||
7313|Glandore Granodiorite|68008|5|Briefly described|p123|Carboniferous|Carboniferous|Possible source of detritus for Lorray Formation.|323.4 +/- 3.9 Ma (Withnall et al., 2009).|||||
7313|Glandore Granodiorite|68679|5|Briefly described|p353, p404, p407-408|Carboniferous|Carboniferous|Auburn Subprovince, New England Orogen. Three K-Ar ages around 305 Ma by Webb and McDougall (1968) are also given.|323 +/- 4 Ma (SHRIMP U-Pb: Fanning et al., 2009).|||May intrude or be intruded by Tindarra Granite.|Grey to pink, medium-grained, hornblende-biotite quartz monzonite, granodiorite and possibly granite, locally with large poikilitic alkali feldspar megacrysts.|
7313|Glandore Granodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|323+/-3.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
7340|Glen Gordon Volcanics|23423|4|Described|p308 Table 7.3|Early Permian|Late Carboniferous|Underlain by Hodgkinson Formation + Silver Valley Conglomerate. In the Kennedy Igneous Province.||||||06-AUG-08
7340|Glen Gordon Volcanics|23430|5|Briefly described|p517|||Underlain by Silver Valley Conglomerate.||||||06-AUG-08
7340|Glen Gordon Volcanics|23497|5|Briefly described|Table 1|Early Permian|Late Carboniferous|Of Kennedy Province. Intruded by Tully Granite Complex, unconformably overlain by Atherton Basalt, uncertain relationship with Ingham Granite Complex. Thickness: 600m.||||||06-AUG-08
7340|Glen Gordon Volcanics|23503|5|Briefly described|Map Legend||Late Carboniferous|||||||
7340|Glen Gordon Volcanics|23506|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
7340|Glen Gordon Volcanics|23507|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
7340|Glen Gordon Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V82.||||||
7340|Glen Gordon Volcanics|23616|5|Briefly described|Table 3 p45|Early Permian|Late Carboniferous|Age: L. Carbon. plant fossls in siltstone. Unit includes the Sunday Creek Volcanics of Best (1962) as well as volcanics in the Silver Valley previously mapped as Nanyeta Volcanics. Of Koolmoon Volc Gp. Hodgkinson Province. Thickness >300 m.||||||06-AUG-08
7340|Glen Gordon Volcanics|23617|4|Described|p14-15|||Also see Table 1 p12. Kennedy Province.||||||
7340|Glen Gordon Volcanics|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
7340|Glen Gordon Volcanics|23619|4|Described|p30 table 1||Carboniferous|Also see p9.  In the Georgetown Province||||||
7340|Glen Gordon Volcanics|29794|6|Mentioned|Fig.4|||||||||
7340|Glen Gordon Volcanics|29820|6|Mentioned|p450|||||||||
7340|Glen Gordon Volcanics|30505|4|Described|p4|||See also p5-7,14. Carboniferous to Permian.||||||06-SEP-18
7340|Glen Gordon Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7340|Glen Gordon Volcanics|31832|6|Mentioned|Table 6|||||||||
7340|Glen Gordon Volcanics|32553|4|Described|p46|||||||||
7340|Glen Gordon Volcanics|32836|6|Mentioned|p8|||||||||
7340|Glen Gordon Volcanics|33205|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7340|Glen Gordon Volcanics|33963|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7340|Glen Gordon Volcanics|36419|6|Mentioned|p392|||See also p396.||||||06-SEP-18
7340|Glen Gordon Volcanics|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
7340|Glen Gordon Volcanics|36563|6|Mentioned|Table 1|||||||||
7340|Glen Gordon Volcanics|37606|6|Mentioned|p353|||||||||
7340|Glen Gordon Volcanics|37613|6|Mentioned|p249|||See also Figs.1 and 3.||||||
7340|Glen Gordon Volcanics|39252|6|Mentioned|Fig.11|||||||||
7340|Glen Gordon Volcanics|39445|5|Briefly described|Table 7|||See also p90.||||||06-SEP-18
7340|Glen Gordon Volcanics|39689|6|Mentioned|p63|||||||||
7340|Glen Gordon Volcanics|39735|6|Mentioned|p18|||||||||
7340|Glen Gordon Volcanics|40049|6|Mentioned|Fig.2|||||||||
7340|Glen Gordon Volcanics|40623|5|Briefly described|p88|||||||||
7340|Glen Gordon Volcanics|40743|6|Mentioned|Fig.1|||||||||
7340|Glen Gordon Volcanics|42459|5|Briefly described|p72|||||||||
7340|Glen Gordon Volcanics|42547|5|Briefly described|p73|||||||||
7340|Glen Gordon Volcanics|43060|5|Briefly described|p73|||||||||
7340|Glen Gordon Volcanics|43113|4|Described|Table 1||Carboniferous|||||||
7340|Glen Gordon Volcanics|43253|5|Briefly described|map legend||Carboniferous|||||||
7340|Glen Gordon Volcanics|43259|4|Described|Appendix 1,p8.||Carboniferous|||||||
7340|Glen Gordon Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
7340|Glen Gordon Volcanics|43903|14|Not recorded|Map Legend||Early Permian|Early Permian to Middle (?) Carboniferous||||||
7340|Glen Gordon Volcanics|43926|2|Defined|Tb.2,opp.10,map,16-7|||||||||
7340|Glen Gordon Volcanics|43927|14|Not recorded|p6-19|||||||||
7340|Glen Gordon Volcanics|44246|5|Briefly described|Map Legend|Early Permian|Early Carboniferous|(Middle Carboniferous - Early Permian)||||||
7340|Glen Gordon Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
7340|Glen Gordon Volcanics|44359|14|Not recorded|Map Legend||Late Carboniferous|||||||
7340|Glen Gordon Volcanics|45014|2|Defined|p45,48-52,Pl.13,15,|Late Carboniferous|Early Carboniferous|Tb.1,Pl.35,38. (Middle Carboniferous-Late Carboniferous).||||||02-JUN-09
7340|Glen Gordon Volcanics|45025|4|Described|p68|Permian|Carboniferous|||||||
7340|Glen Gordon Volcanics|45065|6|Mentioned|Fig.4|||||||||
7340|Glen Gordon Volcanics|45113|3|Fully described|p27|||Emphasis on petrography.||||||
7340|Glen Gordon Volcanics|46845|6|Mentioned|Table 1|||||||||
7340|Glen Gordon Volcanics|48976|6|Mentioned|p65|||||||||
7340|Glen Gordon Volcanics|60425|3|Fully described|p15 Tb. 1, p50 Tb.3, p53|Permian|Carboniferous|Name applies only to sequence exposed in Ravenshoe area; includes type area + Sunday Creek Volcanics of Best (1962), Branch (1966).Overlies Silver Valley Conglom., possibly conformably. Two facies: rhyolite lava, volc.breccia+ tuff; rhyolitic ignimbrite.||||||07-FEB-11
7340|Glen Gordon Volcanics|66529|5|Briefly described|p60|Late Carboniferous|Late Carboniferous|Has high prospectivity for orthomagmatic U mineralisation.||Of the Koolmoon Volcanic Group.||||
7340|Glen Gordon Volcanics|69593|5|Briefly described|p496|Permian|Late Carboniferous|Herberton and Tate Subprovinces.||||Correlated with Wallaman Falls Volcanics.||
7377|Glendarriwell Limestone|22604|6|Mentioned|Fig.1 p438|||||||||
7377|Glendarriwell Limestone|42031|5|Briefly described|Fig.3 P759|||||||||
7377|Glendarriwell Limestone|42614|5|Briefly described|p8|||||||||
7377|Glendarriwell Limestone|43213|5|Briefly described|p9, p68, p237|||See also Glendarriwell beds (p67-69). W of Emerald. Mapped by Veevers et al. (1964) and Darcy (1987). Named by Jell (1988). The informal name Glendarriwell beds is used in this Report because of the poor exposure which precludes a type area, and because a variety of other rocks are known from the area. Appears as Glendariwell Limestone on p9.|||||Poorly exposed limestone with rhyolite, shale, pebbly quartz sandstone, and siltstone.|
7383|Glendoo Sandstone Member|22593|6|Mentioned|p92|||||||||
7383|Glendoo Sandstone Member|22983|6|Mentioned|p272 Fig.1|||||||||
7383|Glendoo Sandstone Member|29735|6|Mentioned|p5|||||||||
7383|Glendoo Sandstone Member|30450|6|Mentioned|p9|||Northern Bowen Basin||||||
7383|Glendoo Sandstone Member|32943|6|Mentioned|p87|||See also PP87,100,102||||||
7383|Glendoo Sandstone Member|32945|6|Mentioned|p78|||See also PP79,80 & Fig.2. Collinsville C.M.||||||
7383|Glendoo Sandstone Member|32949|6|Mentioned|p441|||||||||
7383|Glendoo Sandstone Member|35150|6|Mentioned|p422|||||||||
7383|Glendoo Sandstone Member|35467|6|Mentioned|p183|||Lithology briefly described P184||||||
7383|Glendoo Sandstone Member|36739|6|Mentioned|p14|||||||||
7383|Glendoo Sandstone Member|37071|4|Described|p84|||||||||
7383|Glendoo Sandstone Member|37612|6|Mentioned|p289|||||||||
7383|Glendoo Sandstone Member|38204|6|Mentioned|p79|||||||||
7383|Glendoo Sandstone Member|39212|6|Mentioned|p28|||||||||
7383|Glendoo Sandstone Member|39267|6|Mentioned|p234|||||||||
7383|Glendoo Sandstone Member|39423|6|Mentioned|p53|||||||||
7383|Glendoo Sandstone Member|40571|5|Briefly described|p34|||||||||
7383|Glendoo Sandstone Member|41034|4|Described|p374|||||||||
7383|Glendoo Sandstone Member|41191|5|Briefly described|p284|||||||||
7383|Glendoo Sandstone Member|42257|5|Briefly described|Table 1 P263|||||||||
7383|Glendoo Sandstone Member|42258|6|Mentioned|p275|||||||||
7383|Glendoo Sandstone Member|43475|14|Not recorded|p553||Permian|||||||
7383|Glendoo Sandstone Member|43987|14|Not recorded|p267|||Member of Collinsville Coal Measures.||||||
7383|Glendoo Sandstone Member|44000|2|Defined|Tb.1,p34-37,Pl.6||Early Permian|Middle unit of Collinsville Coal Measures.||||||
7383|Glendoo Sandstone Member|44243|14|Not recorded|p645,647||Early Permian|||||||
7383|Glendoo Sandstone Member|44311|14|Not recorded|p197|||||||||
7383|Glendoo Sandstone Member|44489|14|Not recorded|p70|||||||||
7383|Glendoo Sandstone Member|44542|2|Defined|p30|||Middle Bowen and Upper Collinsville Coal Measures.||||||
7383|Glendoo Sandstone Member|45006|14|Not recorded|p38,39|||||||||
7383|Glendoo Sandstone Member|48915|6|Mentioned|Table 1|||Permian||||||
7383|Glendoo Sandstone Member|68679|5|Briefly described|p380|Permian|Permian|N and NW Bowen Basin. Separates the lower and upper parts of the Coal Measures. Contains marine fossils.||Collinsville Coal Measures.||||
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.|
7433|Glenlyon beds|42559|4|Described|p9|Early Permian||Stated to be an informal name.||||||
7433|Glenlyon beds|68679|6|Mentioned|p451|Permian|Permian|Denaro and Burrows (1992). Refers to the Queensland part of the Bondonga beds [q.v. p449 Fig.5.113, p451-452] which occupies a linear, NW-trending fault-bounded basin remnant, from Mole valley (NSW) to N of Glen Lyon (QLD).||||||
7441|Glenrock Group|22800|5|Briefly described|Fig.14 p592||Visean|||||||
7441|Glenrock Group|22847|5|Briefly described|p 22||Early Carboniferous|||||||
7441|Glenrock Group|23422|4|Described|p180, p205 Table 6.3|Visean|Visean|Underlain by Keelbottom Group. Maximum thickness: 1900m. Geological Province: Burdekin Basin.||||||14-NOV-07
7441|Glenrock Group|23430|4|Described|p506|||Underlain by Keelbottom Group - unconformable. Burdekin Basin Province.||||||21-APR-08
7441|Glenrock Group|23431|5|Briefly described|p538|||Burdekin Basin Province.||||||
7441|Glenrock Group|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
7441|Glenrock Group|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V51. I-Type.||||||
7441|Glenrock Group|23893|5|Briefly described|p17|Visean|Visean|Geological Province: Kennedy Province.||||||
7441|Glenrock Group|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin.||||||20-DEC-04
7441|Glenrock Group|24613|2|Defined|p6 Fig. 3, p92-94|Early Carboniferous|Early Carboniferous|Comprises Horse Pocket, Percy Creek, Tareela and St James Volcanics, Mount Douglas and Ewan Formation. Unconformably overlies Keelbottom Group. Combined thickness of units = 3400m. Uppermost unit in the Burdekin Basin.||||||07-FEB-11
7441|Glenrock Group|24614|5|Briefly described|p196 Fig. 5, p204|Namurian|Visean|Alluvial/lacustrine and volcanic deposits. Unconformably overlies the Keelbottom Group. Geological Province: Burdekin Basin.||||||07-FEB-11
7441|Glenrock Group|37565|6|Mentioned|Fig.8|||||||||
7441|Glenrock Group|37573|6|Mentioned|Fig.2|||||||||
7441|Glenrock Group|38658|6|Mentioned|p152|||||||||
7441|Glenrock Group|39445|5|Briefly described|p90|||||||||
7441|Glenrock Group|41774|6|Mentioned|p31|||||||||
7441|Glenrock Group|42295|5|Briefly described|Fig.2 P5|||||||||
7441|Glenrock Group|42547|4|Described|p76|||||||||
7441|Glenrock Group|42689|5|Briefly described|map legend|Carboniferous||||||||
7441|Glenrock Group|42933|5|Briefly described|Fig.94 p258|||||||||
7441|Glenrock Group|43095|5|Briefly described|Plate 1|||||||||
7441|Glenrock Group|43259|4|Described|Appendix 1,p5.||Carboniferous|||||||
7441|Glenrock Group|43589|5|Briefly described|p18|||Includes Percy Creek and Saint James Voclanics and Ewan Formation. Formerly included the Taralee Volcanics. On TOWNSVILLE  1:25K sheet area||||||23-APR-08
7441|Glenrock Group|43933|5|Briefly described|Map Legend||Carboniferous|||||||
7441|Glenrock Group|43935|5|Briefly described|Map Legend||Carboniferous|||||||
7441|Glenrock Group|60705|5|Briefly described|p649|||Geological Province: Burdekin Basin||||||
7441|Glenrock Group|62522|6|Mentioned|p20|||Geological Province: Burdekin Basin.||||||
7441|Glenrock Group|63154|5|Briefly described|p285 Fig. 5|Early Carboniferous|Early Carboniferous|Geological Province: Charters Towers Province.||||||04-FEB-08
7441|Glenrock Group|66529|5|Briefly described|p24, p30|||||||Includes the Saint James Volcanics.|Includes Fe-rich volcanics.|
7441|Glenrock Group|67402|6|Mentioned|p246|||Previously a part of the Burdekin Basin, this group has since been reassigned [though the author does not state where to].||||||
7441|Glenrock Group|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Burdekin Basin.|||Includes Ewan Formation.||Basalt, andesite, mafic tuff and breccia, rare rhyolitic ignimbrite; pebbly lithic arenite and conglomerate; siltstone, volcanolithic arenite, dacitic tuff (including ignimbrite), pebbly lithic (basement-derived) arenite and conglomerate.|
7441|Glenrock Group|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Burdekin Basin.|||Includes Ewan Formation.||Basalt, andesite, mafic tuff and breccia, rare rhyolitic ignimbrite; pebbly lithic arenite and conglomerate; siltstone, volcanolithic arenite, dacitic tuff (including ignimbrite), pebbly lithic (basement-derived) arenite and conglomerate.|
7441|Glenrock Group|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.|||Includes Tareela Volcanics and Saint James Volcanics.|Shown as younger than the Keelbottom Group.|Mafic and felsic lavas and volcaniclastic rocks.|
7441|Glenrock Group|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.|||Includes Tareela Volcanics and Saint James Volcanics.|Shown as younger than the Keelbottom Group.||
7441|Glenrock Group|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Burdekin Basin.||||||
7441|Glenrock Group|68731|5|Briefly described|p177 Fig 3.91, p183, p223 Fig 3.126|Mississippian|Mississippian|Hutton et al. (1990). Burdekin Basin. Fossils include lepidodendroid plant remains, consistent with a Carboniferous age, and no radiometeric age constraints are available.||||Unconformably underlain by the Keelbottom Group.|Comprises largely mafic to silicic volcanics with subordinate volcaniclastic intervals.|
7441|Glenrock Group|69592|6|Mentioned|p274 Fig.4.65, p276|Mississippian|Late Devonian|Burdekin Basin. Contains volcanics similar to those in the Bundock Basin.||||||
7441|Glenrock Group|69593|5|Briefly described|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province; Burdekin Basin. Deposition in several NW-trending grabens.|||Ewan Formation; Tareela, Saint James Volcanics.||Volcanics include calc-alkaline basaltic and andesitic lava, rhyolitic ignimbrite, tuff and pyroclastic rocks.|
7441|Glenrock Group|70207|6|Mentioned|p20|Carboniferous|Carboniferous|Clarke River and/or Cairns region.||||||
7464|Go Sam Granite|23446|4|Described|p447|||||||||
7464|Go Sam Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
7464|Go Sam Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: ~315Ma Rb-Sr.||||||
7464|Go Sam Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 259. I-Type.||||||
7464|Go Sam Granite|23616|6|Mentioned|Fig 14 p74|||Of O'Briens Creek Supersuite.||||||
7464|Go Sam Granite|40743|6|Mentioned|Fig.2|||||||||
7464|Go Sam Granite|41740|6|Mentioned|p222|||||||||
7464|Go Sam Granite|41824|6|Mentioned|p201|||||||||
7464|Go Sam Granite|42200|6|Mentioned|p325|||||||||
7464|Go Sam Granite|43060|5|Briefly described|Table 6|||of O'Briens Creek Supersuite||||||
7464|Go Sam Granite|43259|4|Described|Appendix 1,p34.||Carboniferous|||||||
7464|Go Sam Granite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Pink to yellow, medium-grained, porphyritic biotite granite; with associated Sn mineralisation. I-type. Includes Parker Microgranite on most recent maps.||||||07-FEB-11
7486|Gold Creek Volcanics|22432|5|Briefly described|p21,22, Fig.23|||McArthur Basin.||||||20-SEP-06
7486|Gold Creek Volcanics|22538|6|Mentioned|App1 P722|||||||||
7486|Gold Creek Volcanics|22644|5|Briefly described|5 fig 2|||Geol province McArthur Basin. Overlain by McArthur Group; underlain by Wollogorang Formation. Creek as 'Ck' in text||||||20-SEP-06
7486|Gold Creek Volcanics|22670|6|Mentioned|53|||Geol province McArthur Basin||||||
7486|Gold Creek Volcanics|22853|3|Fully described|13|Proterozoic|Proterozoic|Geol province: McArthur Basin. Of Tawallah Group. Underain by Wollogorang Formation.||||||20-SEP-06
7486|Gold Creek Volcanics|23216|6|Mentioned|p24|||||||||
7486|Gold Creek Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
7486|Gold Creek Volcanics|23395|5|Briefly described|p389|||||||||
7486|Gold Creek Volcanics|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||20-SEP-06
7486|Gold Creek Volcanics|23397|6|Mentioned|p480|||||||||
7486|Gold Creek Volcanics|23398|6|Mentioned|p437|||||||||
7486|Gold Creek Volcanics|23733|5|Briefly described|p32 Fig. 19|||||||||
7486|Gold Creek Volcanics|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
7486|Gold Creek Volcanics|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with Diamond Creek Volcanics (Katherine River Group).  Geological Province: McArthur Basin.||||||
7486|Gold Creek Volcanics|23961|6|Mentioned|p1193 Fig. 4|||Geological Province: Mt Isa Inlier.||||||
7486|Gold Creek Volcanics|23963|4|Described|p1237, 1240|||Geological Province: McArthur Basin. Overlies the Settlement Creek Volcanics. Max. Thickness: 180m.||||||22-FEB-08
7486|Gold Creek Volcanics|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
7486|Gold Creek Volcanics|24050|6|Mentioned|p27|||||||||
7486|Gold Creek Volcanics|24179|5|Briefly described|p84 Fig. 2|||Overlies the Wollogorang Formation.  Overlain by the Tanumbirini Rhyolite.  Geological Province:  McArthur Basin.||||||
7486|Gold Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Upper Tawallah Group. Geological Province: Southern McArthur Basin.||||||
7486|Gold Creek Volcanics|26310|4|Described|p8, Table 1|Proterozoic|Proterozoic|Porphyritic acidic to intermediate lavas, interbedded sediments. Maximum Thickness: 300 feet. Overlies: Constance Sandstone.||||||
7486|Gold Creek Volcanics|32519|4|Described|Table 1|||||||||
7486|Gold Creek Volcanics|32904|6|Mentioned|p89|||||||||
7486|Gold Creek Volcanics|36012|6|Mentioned|Table 2|||||||||
7486|Gold Creek Volcanics|37670|6|Mentioned|p71|||||||||
7486|Gold Creek Volcanics|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7486|Gold Creek Volcanics|40109|6|Mentioned|Fig.2|||||||||
7486|Gold Creek Volcanics|40259|6|Mentioned|Table 1|||||||||
7486|Gold Creek Volcanics|40489|6|Mentioned|p89|||||||||
7486|Gold Creek Volcanics|40691|5|Briefly described|p11|||Briefly described p19.||||||20-SEP-06
7486|Gold Creek Volcanics|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7486|Gold Creek Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|41721|3|Fully described|p24|||Of the Tawallah Group. Conformably overlain by Hobblechain Rhyolite. Thickness: 180m. Trachyte, latite, tuff and sandstone. Geological province: McArthur Basin.||||||01-AUG-07
7486|Gold Creek Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|42385|4|Described|p13, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Conformable on Wollogorang Formation.Thickness: <180m. Amydaloidal vesicular basaltic lavas, basaltic-dolerite sills and dykes, very fine- to medium-grained. Parts now mapped in with Settlement Creek Volcanics.||||||18-SEP-07
7486|Gold Creek Volcanics|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||Not shown in schematic sections.|Basaltic lavas; basaltic-doleritic sills and dykes; feldspathic-micaceous sandstone; hyaloclastic breccia (peperite); rhyolitic lavas. Detailed lithology given.|09-NOV-11
7486|Gold Creek Volcanics|42639|4|Described|p15|||||||||
7486|Gold Creek Volcanics|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Amygdaloidal basalt lava; dolerite dykes and sills; minor intercalated medium grained sandstone; hyaloclastic breccia with basalt blocks in sandy matrix.||||||19-OCT-05
7486|Gold Creek Volcanics|42812|3|Fully described|p24, Table 3|||Of Tawallah Group.||||||20-SEP-06
7486|Gold Creek Volcanics|42873|4|Described|p109|||see also Fig.1, P110||||||
7486|Gold Creek Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||20-SEP-06
7486|Gold Creek Volcanics|43036|5|Briefly described|p33|||||||||
7486|Gold Creek Volcanics|43715|6|Mentioned|p27|||||||||
7486|Gold Creek Volcanics|43788|6|Mentioned|p14|||||||||
7486|Gold Creek Volcanics|44271|14|Not recorded|p44|||||||||
7486|Gold Creek Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
7486|Gold Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
7486|Gold Creek Volcanics|44280|14|Not recorded|p6,7,Tb.1,map|||||||||
7486|Gold Creek Volcanics|44287|14|Not recorded|p.8|||(E53-3).||||||
7486|Gold Creek Volcanics|44436|5|Briefly described|p.12|||(E53-4).||||||02-DEC-04
7486|Gold Creek Volcanics|44989|14|Not recorded|Tb.II||Neoproterozoic|Tb.II. Overlies Mullera Formation. Upper Proterozoic.||||||
7486|Gold Creek Volcanics|45162|3|Fully described|p41|||||||||22-FEB-18
7486|Gold Creek Volcanics|45287|14|Not recorded|p.223,226||Neoproterozoic|||||||
7486|Gold Creek Volcanics|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
7486|Gold Creek Volcanics|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Warramana Sandstone and Masterton Sandstone, underlain by Wollogorang Formation.||||||
7486|Gold Creek Volcanics|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Interbedded with and overlies the Wollogorang Formation. Overlain by the Pungalina Member. Intruded by the Packsaddle Microgranite. Grey to red, vesicular to massive basalt; dolomitic sandstone, mudstone and peperite||||||07-NOV-08
7486|Gold Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Of Tawallah Group. Shows extensive orthoclase-hematite alteration and base metal depletion. Geological Province: Calvert Superbasin.||||||11-JUN-08
7486|Gold Creek Volcanics|63112|6|Mentioned|p1189, p1192-1198, p1201, p1203-1206|||Calvert Superbasin. Framework grain dissolution after burial produced secondary porosity, allowing movement of basinal brines similar to those reported from Pb-Zn and U deposits of southern McArthur Basin. Age approximated from Fig.2. 15-230 m thick. |c.1725 Ma.|Unit in Big Supersequence.||Overlies Wollogorang Formation.|Seven 10- to 35m-thick vesicular basalt and fine-grained dolerite sheets divided by sandstone interbeds (proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained).|
7486|Gold Creek Volcanics|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin.||Unit in Tawallah Group.||||
7486|Gold Creek Volcanics|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p16  |||Appears as GCV in Fig.2. Often missing in stratigraphic successions.||Of the Tawallah Group.||||
7486|Gold Creek Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2, p370 |||||Of the Tawallah Group.|||Basalt flows.|
7486|Gold Creek Volcanics|65228|5|Briefly described|p22, p25, Figs.02, 05, 06, 07, 10, 12.|Statherian|Statherian|Southern McArthur Basin. Felsic.|1723 +/- 4 Ma (Page et al. 2000).|Unit in Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Warramana Sandstone, Pungalina Member (Echo Sandstone) and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|65337|6|Mentioned|p13.|||Southern McArthur Basin.||||||
7486|Gold Creek Volcanics|65340|3|Fully described|p12 Fig.6, pp25-38, pp68-78, p93. |||Wearyan Shelf. The upper flow unit in this formation is an interpreted extrusive correlative of the Settlement Creek Dolerite. Lithologies, conditions of deposition/emplacement, correlation are discussed in detail. Intertidal to supratidal hypersaline lake or restricted marine depositional environment; sequential emplacement of shallow basalt-peperite sills and flows into wet sediments; local fluidisation. Correlated with Diamond Creek Volcanics to the north, and Peters Creek Volcanics on the Lawn Hill Platform, and temporally with Settlement Creek Dolerite. Produces a high-frequency magnetic response beneath Mesozoic and Cenozoic cover. Hosts a number of Cu(-Co-Ni) stratabound and breccia pipe deposits, eg at Running Creek.||Unit in Tawallah Group.||Overlies Wollogorang Formation. Is intruded by Packsaddle Microgranite. Is overlain by Lower Pungalina Member and Hobblechain Rhyolite.|Grey to red, vesicular to massive, aphyric and locally porphyritic basalt; dolomitic to quartzose sandstone; mudstone; peperite breccia; local auotobreccia and massive sand bodies; local chlorite-bitumen alteration and sulfides.|
7486|Gold Creek Volcanics|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive. ||Unit in Tawallah Group.||Overlies Wollogorang Formation.|Amygdaloidal vesicular basaltic lavas; dolerite sills and dykes; hyaloclastic breccia with basalt blocks in fine sandy matrix; very fine- to medium-grained feldspathic-micaceous sandstone; autoclastic flow-banded rhyolitic lavas.|
7486|Gold Creek Volcanics|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p34|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Calvert Superbasin.|Erupted ~1730-1720 Ma.|Of Tawallah Group.|||Trachyte and latite flows, basalt; tuff; tuffaceous and lithic siltstone; siltstone.|
7486|Gold Creek Volcanics|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 225 m thick. Subaerial extrusive (quiet to explosive), shallow sills; terrestrial sediments.||Tawallah Group||Overlies Wollogorang Formation conformably. Intruded by Packsaddle Microgranite. Is overlain unconformably by Masterton Sandstone.|Basic to intermediate lavas, volcanic interbeds: trachyte or trachyandesite lava: vesicular, amygdaloidal, saussuritic, uralitic; agglomerate, tuff, dolerite, microsyenite, rhyolite; tuffaceous and lithic sandstone and siltstone.|
7486|Gold Creek Volcanics|69418|5|Briefly described|p3:11, 15, 29|||McArthur Basin. Hosts breccia pipe Cu(-Co-Ni) deposits, eg Redbank field (described).||||Overlies Wollogorang Formation.||12-JUL-16
7486|Gold Creek Volcanics|69430|4|Described|p15:3, 10-12, 44-48|Paleoproterozoic|Paleoproterozoic|Batten Fault Zone and SE McArthur Basin. 15-230m thick. Intertidal to supratidal hypersaline lake, or restricted marine, deposits. Hosts numerous Cu-bearing breccia pipes in the Redbank area (described in detail). Is intruded by Packsaddle Microgranite.||Tawallah Group.||Conformably overlies Wollogorang Formation. Is overlain by Pungalina Member (Warramana Sandstone) conformably to disconformably, and by Hobblechain Rhyolite and Echo Sandstone disconformably.|Porphyritic basalt; dolomitic to quartzic sandstone, mudstone, peperite breccia, local autobreccia, local stratiform polymict breccia and massive sandstone bodies, local chlorite-bitumen alteration and sulfides.|12-JUL-16
7486|Gold Creek Volcanics|69591|5|Briefly described|p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of Tawallah Supersequence. Subaerial, local fluvial deposits.||Tawallah Group.|||Trachyte and latite flows, basalt; tuff, tuffaceous and lithic siltstone; siltstone.|
7486|Gold Creek Volcanics|69673|6|Mentioned|p16 fig 13, p17 fig 14|||||Tawallah Group||Overlain by Warramana Sandstone, Pungalina Member, Hobblechain Rhyolite, conformably overlies Wollogorang Formation|Basalt.|
7486|Gold Creek Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Hobblechain Rhyolite.|Trachyte and latite flows, tuff, tuffaceous and lithic sandstone, siltstone.|
7486|Gold Creek Volcanics|71374|6|Mentioned|p6|||McArthur Basin.||Tawallah Group||Unconformably overlain by the Masterton Sandstone.||
7486|Gold Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown to be located in the Batten Fault Zone and the Southeastern McArthur Basin of the Southern McArthur Basin.||Tawallah Group||Partially overlies Wollogorang Formation and underlies Warramana Sandstone, Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by Wollogorang Foramtion. Partly overlain by and equivalent to Warramana Sandstone. Partly overlain by Pungalina Member, Hobblechain Rhyolite, Packsaddle Microgranite.||
7486|Gold Creek Volcanics|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone and the Southeastern McArthur Basin of the Southern McArthur Basin.||Tawallah Group||Overlies Wollogorang Formation and is partially equivalent to and underlies Warramana Sandstone. Underlies Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Underlain by Wollogorang Formation. Partly overlain by Warramana Sandstone, Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|73083|6|Mentioned|p40|||Speckled magnetic appearance.|||||Mafic volcanics.|
7486|Gold Creek Volcanics|73412|5|Briefly described|p2, 4, 8-9, 12, 14-15, 20|||Southern McArthur Basin. Higher conductivity and magnetic responses than most of the Group.||Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Warramana Sandstone. Eruptive equivalent to Settlement Creek Volcanics sills.||
7524|Gomaren Basalt|23799|5|Briefly described|p54|||Of Main Range Volcanics.  Overlain by Cooby Trachyte Member.  Geological Province: Main Range-Lamington Volcanic Province.||||||
7524|Gomaren Basalt|34507|4|Described|p88|||||||||
7524|Gomaren Basalt|45087|5|Briefly described|p149|||Chemical analyses||||||
7524|Gomaren Basalt|73450|6|Mentioned|p90|||Can be difficult to distinguish from the Cooby Trachyte Member (Main Range Volcanics).|||||Dark, fine grained basalt.|
7645|Goyan Andesite|24382|5|Briefly described|Map legend|Triassic|Triassic|||||||
7645|Goyan Andesite|41736|6|Mentioned|Fig.1|||||||||
7645|Goyan Andesite|41738|2|Defined|p168|Middle Triassic|Early Triassic|Reserved as Goyan.||||||14-AUG-08
7645|Goyan Andesite|41778|6|Mentioned|Fig.1|||||||||
7645|Goyan Andesite|42054|6|Mentioned|p272|||||||||
7645|Goyan Andesite|63821|5|Briefly described|p21|Triassic|Triassic|Comprises a sequence of shallow-dipping altered andesitic flows and pyroclastics. Unconformably overlies undivided Curtis Island Group. Intruded by Hogback Granite.||||||07-FEB-11
7645|Goyan Andesite|68679|5|Briefly described|p433-434, p440-441|Late Triassic|Late Triassic|Northern Gayndah region. Thickness estimates from 60m to ~150m. Previously considered Early-Middle Triassic (by correlation with Neara Volcanics). Now Late Triassic by correlation of lithology and relationships with surrounding intrusives.|||||Includes fine-grained, porphyritic pyroxene andesite lava flows with lesser pyroclastic deposits. Has no epiclastic deposits.|
7645|Goyan Andesite|73450|6|Mentioned|p24|early Triassic|early Triassic|||||Intruded by Hogback Granite.||
7661|Grafton Formation|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p494|Early Cretaceous|Tithonian|S Clarence-Moreton Basin.|||||Lithic quartz sandstones containing beds of montmorillonitic mudstone; contains plant fragments, reed impressions and traces of coal.|
7661|Grafton Formation|22857|4|Described|p318-9, p548 App. 1 Tb.A1.12|Early Cretaceous|Late Jurassic|Sandstone, clayey siltstone; minor claystone, coal. Max. thickness: 276m. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|22865|6|Mentioned|p318,Fig22.9p317|Cretaceous|Late Jurassic|||||||
7661|Grafton Formation|22892|5|Briefly described|p7 fig6|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|23811|5|Briefly described|Map Legend|Tithonian|Oxfordian|Interbedded sandstone (lithic to quartz arenites ans wackes), clayey siltstone, claystone and local coal; bedding thin to thick; commonly with ferruginous lateritic weathering profile.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
7661|Grafton Formation|23812|5|Briefly described|p34 Tb.4, p31|Late Jurassic|Late Jurassic|Maximum thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|23843|5|Briefly described|p456 Table 1|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 440m.||||||
7661|Grafton Formation|23888|6|Mentioned|p262|||||||||
7661|Grafton Formation|24237|5|Briefly described|p6 Fig.2|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|29591|5|Briefly described|p85|||||||||
7661|Grafton Formation|29988|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|29995|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|30785|6|Mentioned|p397|||||||||
7661|Grafton Formation|30911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|32491|5|Briefly described|p18|||U.Jurassic||||||
7661|Grafton Formation|32492|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|32916|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|33476|6|Mentioned|Fig.10|||||||||
7661|Grafton Formation|33709|6|Mentioned|p104|||||||||
7661|Grafton Formation|34340|3|Fully described|p472|||||||||
7661|Grafton Formation|34400|5|Briefly described|p14|||||||||
7661|Grafton Formation|35065|6|Mentioned|p45|||||||||
7661|Grafton Formation|36354|6|Mentioned|Fig.1|||||||||
7661|Grafton Formation|37122|5|Briefly described|Table 1|||||||||
7661|Grafton Formation|37252|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
7661|Grafton Formation|38064|5|Briefly described|p41|||||||||
7661|Grafton Formation|41631|4|Described|p20|||See also Fig.2||||||
7661|Grafton Formation|42463|6|Mentioned|Fig.3 P170|||||||||
7661|Grafton Formation|42869|5|Briefly described|Table 1, P33|||||||||
7661|Grafton Formation|43001|5|Briefly described|p131|||||||||
7661|Grafton Formation|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
7661|Grafton Formation|43344|14|Not recorded|p102|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43383|14|Not recorded|p28|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43384|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43468|14|Not recorded|Map Legend||Cretaceous|Provisional Edition||||||
7661|Grafton Formation|43479|14|Not recorded|p251,262||Tithonian|||||||
7661|Grafton Formation|43736|5|Briefly described|Table 1,p4|||||||||
7661|Grafton Formation|43881|14|Not recorded|p5-7,11-14,44-8,64,|Cretaceous|Late Jurassic|Replaces Grafton Beds. p73,76,79-80,115,153,156.||||||
7661|Grafton Formation|44028|14|Not recorded|Fig.2|Cretaceous|Jurassic|See Strat Table.||||||
7661|Grafton Formation|48917|3|Fully described|p30|||See also P47. Water.||||||
7661|Grafton Formation|60079|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Interbedded sandstone, clayey siltstone, claystone and minor coal.||||||
7661|Grafton Formation|60281|5|Briefly described|p27, Fig.20 App.1|Cretaceous|Late Jurassic|Overlies the Kangaroo Creek Sandstone.  Sandstone, clayey siltstone, minor claystone, coal.  Max. thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
7661|Grafton Formation|60993|3|Fully described|p4, p36|Tithonian|Callovian|Initially termed the "Grafton Beds" and the "Grafton Stage". Sandstone, siltstone and claystone; coal. Conformably/gradationally overlies Kangaroo Creek Sst. Thickness in grafton 2 bore: 267m. Geol. Prov: Clarence-Moreton Basin. ||||||
7661|Grafton Formation|60995|4|Described|p69, p51 Fig. 3|Late Jurassic|Late Jurassic|Thin and thick-bedded, silty quartz sandstone,lithic sandstone,clayey siltstone, minor claystone, and coal. Overlies Kangaroo Creek Sandstone. Max. thickness: 250m. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|60997|5|Briefly described|p139|Berriasian|Tithonian|Composed of lithic-labile sandstone. Conformably overlies Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1.||||||29-JAN-08
7661|Grafton Formation|60999|5|Briefly described|p164|||Overlies Walloon C. M. in places.||||||
7661|Grafton Formation|61000|5|Briefly described|p181, p183|Late Jurassic|Middle Jurassic|Siltstone and mudstone are common. Geological Province: Clarence-Moreton Basin. See also p186.||||||
7661|Grafton Formation|61002|5|Briefly described|p213|Late Jurassic|Late Jurassic|Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|||||||
7661|Grafton Formation|61005|6|Mentioned|p248, p252|||An eroded unit. ||||||
7661|Grafton Formation|61006|5|Briefly described|p278 Fig. 2||Jurassic|Mudstone, labile sandstone. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|61310|5|Briefly described|p14 Fig. C5|Early Cretaceous|Early Cretaceous|Comprises clayey siltstone and soft sadstone with minor claystone and coal. Overlies Kangaroo Creek Sandstone. Max. thickness: 276m. Geological Province: Clarence -Moreton Basin. See also p24.||||||
7661|Grafton Formation|61377|6|Mentioned|p159|||||||||07-FEB-11
7661|Grafton Formation|64289|5|Briefly described|p6 Fig. 2|Late Jurassic|Late Jurassic|Geological province: Clarence-Moreton Basin.||||||07-FEB-11
7661|Grafton Formation|67402|5|Briefly described|p187, p193|Berriasian|Oxfordian|Clarence-Moreton Basin. ||||Overlies the Kangaroo Creek Formation.||
7661|Grafton Formation|68135|5|Briefly described|p52 fig 2b |Early Cretaceous|Late Jurassic|Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone|Interbedded siltstone and sandstone.|14-SEP-17
7661|Grafton Formation|69297|5|Briefly described|p487 fig 5.38|Cretaceous|Upper Jurassic|Clarence-Moreton Basin. Between 150-250m thick. Deposited in a low-energy, mixed load meandering fluvial environment. ||||Overlies the Kangaroo Creek Sandstone.|Sandstone, clayey siltstone, minor claystone and coal.|
7661|Grafton Formation|69594|5|Briefly described|p544-545|||Clarence-Moreton Basin (NSW only). In QLD it is known as the (upper part of) Woodenbong beds. 250+ m thick. Fluvial to lacustrine sediments, derived from Texas Subprovince.||||Overlies Kangaroo Creek Sandstone.|Sublabile to labile, tough, sandstone, siltstone and shale; conglomerates up to 2.5m thick. Sandstones cross-bedded in places; plant fossils common. Abundant andesitic fragments suggest contemporaneous volcanism.|
7661|Grafton Formation|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurrasic|Shown as located within the Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone|May includes siltstone.|
7661|Grafton Formation|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone.||
7661|Grafton Formation|73570|6|Mentioned|p913-915, p917 Fig.5, p921, p923|Early Cretaceous|Late Jurassic|Clarence-Morton Basin.|134 Ma|||||
7690|Grant Bluff Formation|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Sandstone(thin bedded), siltstone, shale. Overlies: Gnallan-a-gea Arkose.||||||28-OCT-04
7690|Grant Bluff Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Sandstone, shale. Underlies: Elkera Formation. Overlies: Elyuah Formation.||||||01-NOV-04
7690|Grant Bluff Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Elkera Formation. Overlies: Elyuah Formation. Fine thin-bedded sandstone.||||||
7690|Grant Bluff Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Georgina Basin.  Age - Ediacarian in text.||||||
7690|Grant Bluff Formation|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
7690|Grant Bluff Formation|23844|5|Briefly described|p37|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin||||||
7690|Grant Bluff Formation|24442|6|Mentioned|p49|||Geological Province: Georgina Basin.||||||
7690|Grant Bluff Formation|33103|4|Described|Table 4|||||||||
7690|Grant Bluff Formation|33104|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
7690|Grant Bluff Formation|33111|6|Mentioned|p38|||||||||
7690|Grant Bluff Formation|34557|6|Mentioned|p351|||Cambrian||||||
7690|Grant Bluff Formation|34724|6|Mentioned|p343|||||||||
7690|Grant Bluff Formation|35005|5|Briefly described|p145|||||||||
7690|Grant Bluff Formation|35121|6|Mentioned|Map legend|Early Cambrian|Adelaidean|||||||
7690|Grant Bluff Formation|35139|4|Described|Table.2|||See also p10.||||||21-SEP-06
7690|Grant Bluff Formation|35221|6|Mentioned|p14|||||||||
7690|Grant Bluff Formation|35798|4|Described|p307|||Proterozoic rather than Cambrian.||||||
7690|Grant Bluff Formation|35863|6|Mentioned|Table 1|||||||||
7690|Grant Bluff Formation|37572|5|Briefly described|p154|||See also p164 and Fig.8.||||||21-SEP-06
7690|Grant Bluff Formation|37928|6|Mentioned|Fig.4|||||||||
7690|Grant Bluff Formation|38157|6|Mentioned|Table IX|||||||||
7690|Grant Bluff Formation|39210|4|Described|p51|||||||||
7690|Grant Bluff Formation|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7690|Grant Bluff Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Quartz arenite to quartz wacke, fine grained, fissile and undulose laminated. Geological Province: Georgina Basin.||||||15-NOV-05
7690|Grant Bluff Formation|40906|4|Described|p21|||||||||
7690|Grant Bluff Formation|41005|6|Mentioned|p217|||||||||
7690|Grant Bluff Formation|41388|6|Mentioned|p552|||||||||
7690|Grant Bluff Formation|41429|6|Mentioned|p247|||||||||
7690|Grant Bluff Formation|41801|5|Briefly described|p215|||||||||
7690|Grant Bluff Formation|42059|6|Mentioned|Fig.2 P131|||||||||
7690|Grant Bluff Formation|42225|6|Mentioned|p219|||||||||
7690|Grant Bluff Formation|42504|5|Briefly described|Table 4 P73|||||||||
7690|Grant Bluff Formation|42643|5|Briefly described|p29|||||||||
7690|Grant Bluff Formation|44327|2|Defined|Tb.I,p.8,9,11,18|||(F53-11). Underlies conformably Mount.Baldwin Formation. Of the Mopunga Group.||||||29-SEP-11
7690|Grant Bluff Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
7690|Grant Bluff Formation|44334|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
7690|Grant Bluff Formation|44358|4|Described|p8,Tb.1|Early Cambrian|Neoproterozoic|||||||
7690|Grant Bluff Formation|44469|2|Defined|p.7,opp.p.6, Tb.I|||(F53-12). See also p.16.||||||
7690|Grant Bluff Formation|44470|5|Briefly described|map legend|||Upper Proterozoic to Lower Cambrian.||||||02-DEC-04
7690|Grant Bluff Formation|45052|4|Described|p64|||See also Fig.9 and Table 8||||||21-SEP-06
7690|Grant Bluff Formation|45102|6|Mentioned|p43|||See also p44,45.||||||21-SEP-06
7690|Grant Bluff Formation|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
7690|Grant Bluff Formation|46865|5|Briefly described|p48|||||||||
7690|Grant Bluff Formation|46903|6|Mentioned|p53|||||||||
7690|Grant Bluff Formation|47035|6|Mentioned|Fig.1|||||||||
7690|Grant Bluff Formation|48844|2|Defined|p.20-31|||On many pages. p.1,16,17,20-31,33,34,36,39, F.26,58,59,67, Pl.8. (new name).Overlies Elyuah Formation. Good marker bed. (F53-11).||||||21-SEP-06
7690|Grant Bluff Formation|48901|14|Not recorded|Not recorded||Adelaidean|Part of Mopunga Group.||||||21-SEP-06
7690|Grant Bluff Formation|48990|1|Redefined|p12|Adelaidean|Adelaidean|See also p10.||||||21-SEP-06
7690|Grant Bluff Formation|49027|5|Briefly described|p5|||||||||
7690|Grant Bluff Formation|60122|4|Described|p4-5, p13-14|Neoproterozoic|Neoproterozoic|Of the Mopunga Group.  Revised by Walter (1980) to exclude the Elkera Formation.  Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone. Conformable on Gnallan-a-Gea Arkose and Elyuah Fm. Max. thickness: 1170m in HAY RIVER. See also p11Tb. 1||||||21-SEP-06
7690|Grant Bluff Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin.  Underlies: Elkera Formation. Overlies: Elyuah Formation. Thin bedded fine sandstone, shale.||||||17-NOV-04
7690|Grant Bluff Formation|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Mopunga Group.  Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone.  Overlies the Elyuah Formation and the Gnallan-a-Gea Arkose.||||||
7690|Grant Bluff Formation|60668|5|Briefly described|Fig. 23a|||Shale, silty sandstone and pebble conglomerate.   Geological Province: Georgina Basin. ||||||
7690|Grant Bluff 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
7690|Grant Bluff Formation|61208|5|Briefly described|p208|||Unconformably overlies the Utopia Quartzite. Geological Province: Georgina Basin.||||||12-JAN-06
7690|Grant Bluff Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Fine-grained, thin bedded, flaggy white, brown and reddish sandstone; local coarse to pebbly sandstone; interbedded mudstone. Geological Province: Georgina Basin.||||||
7690|Grant Bluff Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
7690|Grant Bluff Formation|61732|3|Fully described|p5 Tb. 1, p109|Ediacaran|Ediacaran|Of Mopunga Group. Transitionally overlies Eluyah Fm; underlies (probably unconconformably) Elkera Fm. Geol. Prov: Georgina Basin. See also p106, p108 Fig. 40.||||||07-FEB-11
7690|Grant Bluff Formation|62376|5|Briefly described|p53|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
7690|Grant Bluff Formation|62595|6|Mentioned|p28 Fig.4.|Late Neoproterozoic|Late Neoproterozoic|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
7690|Grant Bluff Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Mopunga Group. Geological Province: Georgina/Ngalia Basin. Sandstone, micaceous-quartzofeldspathic, with abundant ripple marks, low angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.||||||21-SEP-06
7690|Grant Bluff Formation|62984|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlies the Eyuah Formation; overlain by Elkera Formation. Geological Province: Georgina Basin. Sandy deposits.||||||23-JAN-07
7690|Grant Bluff Formation|63450|5|Briefly described|p78 Fig. 5, p79|Neoproterozoic|Neoproterozoic|Overlies Gnallan-A-Gea Arkose. Geological province: Georgina Basin, West Toko Syncline. Contains quartzose sandstone and numerous sedimentary structures including trace fossils, glauconitic sandstone and mudstone; marine in origin.||||||07-FEB-11
7690|Grant Bluff Formation|63562|4|Described|p338 fig 3, p344-345, p347 fig 9|Ediacaran|Ediacaran|See also p351, p352 fig 10. Of Georgina Basin. Forms escarpments in the Elua Range. Zircons are similar to, but more concordant than, those in Cyclops Member; source probably Arunta Inlier.||Mopunga Group||Overlies Elyuah Formation. Has been correlated with Cyclops Member (Pertatataka Formation). Is overlain by Elkera Formation.|Coarse-grained sandstone, with interbeds of fine-grained, thinly-bedded, recessive sandstone units. Contains ichnofossils, syneresis cracks and fine disseminated pyrite.|
7690|Grant Bluff Formation|64068|3|Fully described|p50-51, p44, 49, 52, 54, 57, 162|Ediacaran|Ediacaran|Now includes rocks formerly assigned to the Forster Member of the Central Mount Stuart Formation.||Of Mopunga Group.||Conformably, gradationally, overlies Elyuah Formation, Gnallan-a-Gea Arkose. Conformably and gradationally overlain by Elkera Formation, Central Mount Stuart Formation.|Orange-brown, white and purple quartz sandstone, quartzite and quartz greywacke, arkose, siltstone, shale, minor dolostone.|04-APR-12
7690|Grant Bluff Formation|65237|5|Briefly described|p5|||Of the Mopunga Group. Overlain by Elkera Formation; conformable/gradation on Elyuah Formation. Geological province: southern Georgina Basin.||||||07-FEB-11
7690|Grant Bluff Formation|65338|4|Described|p iv, p60, pp64-65.|Ediacaran|Ediacaran|Georgina Basin. Deltaic clastic rocks. Now recognised to be more widespread than previously mapped. Correlated with middle to upper Pertatataka Formation of Amadeus Basin. Cross-bedding and ripples are common. Shallow marine.||Unit in Mopunga Group.||Faulted against Amesbury Quartzite. Overlies Elyuah Formation and Gnallan-a-gea Arkose. Is overlain by Elkera and Central Mount Stuart Formations.|Laminated to thinly bedded, fine-grained quartz arenite and sublitharenite with micaceous partings; bounded by a lowermost and uppermost interval of well-sorted and well-rounded, medium- to coarse-grained, thinly to thickly bedded quartz arenite.|
7690|Grant Bluff Formation|65341|5|Briefly described|p2 Fig.2, p5, p15. |||Includes some outcrops previously (Shaw and Warren 1975) mapped as 'Central Mount Stuart beds'. Outcrops over basement near the northern map area are continuous with the mapped Forster Member of the Central Mount Stuart Formation; thus this Member is here abandoned. ||Unit in Mopunga Group.||Conformably overlies Elyuah Formation.|White, brown and reddish, thinly bedded, tabular, fine sandstone; local coarse to pebbly sandstone; interbedded mudstone.|
7690|Grant Bluff Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Mopunga Group.||Overlies Elyuah Formation. Is overlain by Central Mount Stuart Formation.|Micaceous quartzofeldspathic sandstone with abundant ripple marks, low-angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.|
7690|Grant Bluff Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Mopunga Group.||Overlies Elyuah Formation. Is overlain by Central Mount Stuart Formation.|Sandstone, micaceous, quartzofeldspathic, with abundant ripple marks, low-angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.|
7690|Grant Bluff Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Mopunga Group.||Overlies Elyuah Formation and Gnallan-a-Gea Arkose. Is overlain by Elkera Formation.||12-JUL-16
7690|Grant Bluff Formation|69443|4|Described|p28:7, 10-11, 15-16, 35|Ediacaran|Ediacaran|K.G. Smith (1964); modified by Walter (1980). Southern Georgina Basin. Forms widespread prominent strike ridges. Thickness varies considerably, from 20m to 1170m. Deposited as a transgressive sand sheet in a shallow- to marginal-marine environment. Is also overlain disconformably by Thorntonia Limestone or Adam Shale, or unconformably by Red Heart Dolostone.||Mopunga Group.||Gradationally overlies Elyuah Formation and Gnallan-a-Gea Arkose. Is overlain conformably and gradationally by Elkera and Central Mount Stuart Formations, and Andagera Formation.|Mainly laminated to medium undulose-bedded, medium to coarse quartz sandstone and quartzite with micaceous partings; also quartz greywacke, arkose, siltstone, shale, minor dolostone and local basal polymict conglomerate have been reported.|12-JUL-16
7690|Grant Bluff Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |||Mopunga Group||Overlies Elyuah Formation, Gnallan-a-gea Arkose, overlain by Elkera Formation, Central Mount Stuart Formation|Sandstone and quartzite.|
7690|Grant Bluff Formation|71621|5|Briefly described|p30|||Georgina Basin. Said to have an unconformable and in part faulted contact with the Xanten Granodioritie [although the exact nature of this contact isnt provided].||||||02-FEB-19
7690|Grant Bluff Formation|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Georgina Basin.||||Overlies the Elyuah Formation. Overlain by the Ellkera Formation.|Medium sandstone.|
7690|Grant Bluff Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains ichnofossils, microbial mat fragments.||Mopunga Group||Overlain by the Elkera Formation. Overlies the Elyuah Formation.|Quartz sandstone, quartzwacke; laminated to medium undulose-bedded, trough cross-bedded; syneresis cracks; ripple marks; minor arkose, locally glauconitic; minor siltstone, shale, dolostone; local basal conglomerate.|
7690|Grant Bluff Formation|72516|2|Defined|p15-16, 21, 46, 47, 85, 86, 88-90|Ediacaran|Ediacaran|Georgina Basin.Widespread unit forming prominent strike ridges and hills. Type section is defined 15km southeast of Grant Bluff in Elua Range in JINKA. In JERVOIS RANGE SPECIAL it forms ridges nof the Jervois Range and Johansen Range. Rocks previously assigned to this unit in the Charlotte Fault Zone are now assigned to Elkera Formation. Contains Ediacaran ichnofossils, indeterminate filaments, mat fragments, vendotaeniid fragments, leiospheres, acritarchs and microbial mat fragments. Deposited in a shallow to marginal-marine trangressive sheet sand environment. 66-90m thick in the map sheet area, 20-1170m thick elsewhere. Equivalent to the Cyclops Member and the Badens Camp Quartzite. See also p12, 13, p186, p189,198, 201, 218. Also misspelt as Grand Bluff Formation p186, p189, 198, 201, 218.|ca 818 Ma (max dep age)|Mopunga Group||Conformably to gradationally overlain by the Elkera Formation. Conformably overlies the Elyuah Formation, Unconformably overlies the Bonya Metamorphics,Tarlton Granite and the Jericho Granite.|Quartz sandstone, quartzwacke; laminated to medium-undulose-bedded, trough cross bedded; syneresis cracks; ripple marks; minor arkose, locally glauconitic; minor siltstone, shale, dolostone; local basal conglomerate.|16-JUN-21
7690|Grant Bluff Formation|73086|6|Mentioned|p122|||Georgina Basin, south-eastern.||||Correlates to Pertatataka Formation.||
7724|Gray Creek Complex|23032|4|Described|p12|Mesoproterozoic|Mesoproterozoic|Ar/Ar Ages: 1111+/-30 Ma and 1316+/- 40 Ma.||||||
7724|Gray Creek Complex|23291|3|Fully described|p30, p20 Fig. 3.2, p83 Tb. 3.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Cape River Province.||||||27-MAY-09
7724|Gray Creek Complex|23424|5|Briefly described|Table 8.1 p327 p330||Mesoproterozoic|Faulted against Judea Formation. Of Green (1958) & White (1965). Structurally identical to the Boiler Gully Complex. Age: Hornblende 1111+/-30 Ma and 1316+/-40 Ma. (Forsayth Subprovince/Etheridge Province)?? - from p327?. p330 says Cape River Province??||||||
7724|Gray Creek Complex|23430|5|Briefly described|p450|||Etheridge Province.||||||
7724|Gray Creek Complex|23431|5|Briefly described|p531, 540|||Etheridge Province.||||||03-AUG-20
7724|Gray Creek Complex|23494|5|Briefly described|p10, p21 Tb. 1|Devonian|Devonian|Ultrabasic and basic rocks.||||||
7724|Gray Creek Complex|23498|5|Briefly described|p21 table 1||Devonian|||||||
7724|Gray Creek Complex|23619|5|Briefly described|p43 Table 2 + p7|||Georgetown Province||||||
7724|Gray Creek Complex|24577|6|Mentioned|p755 Fig. 2|Early Paleozoic|Proterozoic|||||||07-NOV-08
7724|Gray Creek Complex|24613|5|Briefly described|p6 Fig. 3|Early Devonian|Precambrian|Geological province: Burdekin Basin.||||||07-FEB-11
7724|Gray Creek Complex|29445|6|Mentioned|p73|||||||||
7724|Gray Creek Complex|29446|4|Described|p123|||See also P120||||||
7724|Gray Creek Complex|30334|6|Mentioned|p120|||||||||
7724|Gray Creek Complex|30780|6|Mentioned|p996|||||||||
7724|Gray Creek Complex|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7724|Gray Creek Complex|31999|6|Mentioned|p139|||||||||
7724|Gray Creek Complex|32553|4|Described|p66|||||||||
7724|Gray Creek Complex|32959|6|Mentioned|Fig.30|||||||||
7724|Gray Creek Complex|35948|6|Mentioned|Table 3|||||||||
7724|Gray Creek Complex|37507|6|Mentioned|p501|||||||||
7724|Gray Creek Complex|37570|6|Mentioned|p112|||||||||
7724|Gray Creek Complex|37571|6|Mentioned|p129|||||||||
7724|Gray Creek Complex|37575|4|Described|p182|||See also P184 and Fig.3||||||
7724|Gray Creek Complex|37609|6|Mentioned|p309|||||||||
7724|Gray Creek Complex|37768|6|Mentioned|p34|||||||||
7724|Gray Creek Complex|37769|4|Described|p47|||||||||
7724|Gray Creek Complex|37770|6|Mentioned|Fig.12|||||||||
7724|Gray Creek Complex|39027|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
7724|Gray Creek Complex|39445|6|Mentioned|p56|||See also Table 3 & Fig.6||||||
7724|Gray Creek Complex|39689|6|Mentioned|p49|||||||||
7724|Gray Creek Complex|40961|6|Mentioned|p244|||||||||
7724|Gray Creek Complex|41260|3|Fully described|p24|||Described P140||||||
7724|Gray Creek Complex|41594|5|Briefly described|p74|||||||||
7724|Gray Creek Complex|41675|6|Mentioned|p14|||||||||
7724|Gray Creek Complex|41679|6|Mentioned|Fig.1|||||||||
7724|Gray Creek Complex|41719|6|Mentioned|p215|||||||||
7724|Gray Creek Complex|41739|6|Mentioned|Fig.1|||||||||
7724|Gray Creek Complex|41975|5|Briefly described|p439|||||||||
7724|Gray Creek Complex|42031|5|Briefly described|Fig.4 P761|||||||||
7724|Gray Creek Complex|42279|6|Mentioned|Fig.2 P18|||||||||
7724|Gray Creek Complex|42407|6|Mentioned|p33|||||||||
7724|Gray Creek Complex|42692|5|Briefly described|map legend|Proterozoic||||||||
7724|Gray Creek Complex|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
7724|Gray Creek Complex|42747|6|Mentioned|p36|||||||||
7724|Gray Creek Complex|42752|5|Briefly described|p49, Fig.3 p47|||||||||
7724|Gray Creek Complex|42933|2|Defined|p46|Precambrian||||||||
7724|Gray Creek Complex|43113|4|Described|Table 2 p28||Proterozoic|||||||
7724|Gray Creek Complex|43213|6|Mentioned|p9|||Near Greenvale, Broken River Province.||||Faulted against Carriers Well Formation.||
7724|Gray Creek Complex|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
7724|Gray Creek Complex|43286|5|Briefly described|Map Legend||Proterozoic|||||||
7724|Gray Creek Complex|43480|6|Mentioned|13|||||||||
7724|Gray Creek Complex|43664|6|Mentioned|Fig.3,p15|||||||||
7724|Gray Creek Complex|44043|14|Not recorded|p69|||||||||
7724|Gray Creek Complex|44044|14|Not recorded|p125,126||Early Devonian|||||||
7724|Gray Creek Complex|44046|14|Not recorded|p150-3||Early Devonian|Intrudes Graveyard Creek Formation. Probably early Early Devonian.||||||
7724|Gray Creek Complex|44048|14|Not recorded|Map Legend||Devonian|||||||
7724|Gray Creek Complex|44049|14|Not recorded|Map Legend||Devonian|||||||
7724|Gray Creek Complex|44059|14|Not recorded|p442(Tb)||Early Devonian|||||||
7724|Gray Creek Complex|44093|5|Briefly described|p91|Proterozoic|Proterozoic|Ultramafic/mafic rocks. Geological Province: Tasman Fold Belt.||||||
7724|Gray Creek Complex|44258|14|Not recorded|p4||Middle Devonian|(pre Middle Devonian)||||||
7724|Gray Creek Complex|44515|2|Defined|p32,36|Late Devonian|Early Devonian|Gabbro-peridodite suite. Overlain by Broken River Formation.||||||
7724|Gray Creek Complex|44516|14|Not recorded|p32,35|||||||||
7724|Gray Creek Complex|45009|2|Defined|p21,41,44,48,50,75,|||p79,81,83-90,111-2,125,Pl.13,15. Intrudes Wairuna Formation. Ultrabasic of Bushveld type.||||||
7724|Gray Creek Complex|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|Serpentinite.||||||07-NOV-08
7724|Gray Creek Complex|61211|5|Briefly described|p274|Late Cambrian|Middle Cambrian|Includes ultramafic to mafic rocks; intensely deformed in lower levels but decreases upwards towards the overlying Judea Formation. Geological Province: Broken River Province.||||||13-JAN-06
7724|Gray Creek Complex|61258|5|Briefly described|p387 Fig. 1|Paleoproterozoic|Neoproterozoic|Geological Province: Georgetown Inlier.||||||07-NOV-08
7724|Gray Creek Complex|65887|5|Briefly described|p40 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
7724|Gray Creek Complex|67455|5|Briefly described|p576, p587, p588 Fig.11.|||Mafic/ultramafic basement to Graveyard Creek Subprovince, Broken River Province.||||Is overlain by Judea Formation.|Strongly deformed ultramafic and mafic rocks.|
7724|Gray Creek Complex|67848|5|Briefly described|p1, p4, p5 Fig.3, p12, pp14-15.|||Broken River Province. Basement of mafic-ultramafic rocks; multiply-deformed oceanic crust with sedimentary cover (Judea Formation). Amphibolite facies. Age is uncertain.||||Is intruded by Saddington Tonalite. Is overlain by Judea Formation.|Pyroxenite, serpentinised peridotite, meta-gabbro, amphibolite.|
7724|Gray Creek Complex|68336|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||||Undivided: metagabbro, amphibolite, clinopyroxenite and serpentinite. Separately mapped facies associations are serpentinite; clinopyroxenite, metagabbro and serpentinite; and amphibolite, locally mylonitised.|
7724|Gray Creek Complex|68341|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||||Undivided: metagabbro, amphibolite, clinopyroxenite and serpentinite. Separately mapped facies associations are serpentinite; clinopyroxenite, metagabbro and serpentinite; and amphibolite, locally mylonitised.|
7724|Gray Creek Complex|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Cape River Province.|||||Serpentinite.|
7724|Gray Creek Complex|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Greenvale Province. This unit, the Boiler Gully Complex, and unnamed mafic and ultramafic intrusive units are all mapped under the same symbol, -P-Cx.||||||
7724|Gray Creek Complex|68576|5|Briefly described|Q_11: p34-37|||Greenvale area. Mylonitised in the Gray Creek Fault Zone.||||Is faulted against Judea Formation and Carriers Well Formation.|Includes serpentinite, clinopyroxenite, amphibolite.|
7724|Gray Creek Complex|68731|6|Mentioned|p151 Fig 3.51, p221|||||||||
7724|Gray Creek Complex|69030|6|Mentioned|p6|Cambrian|Cambrian|Graveyard Creek Subprovince (Broken River Province).||||||
7724|Gray Creek Complex|69079|5|Briefly described|p65|||Hosts auriferous quartz stringers which are the source of the small alluvial Gold Hill gold occurrence.|||||Serpentinite and silicified serpentinite.|
7724|Gray Creek Complex|69592|5|Briefly described|p250-253, p255, p258, p263, p267, p277|Ordovician|Cambrian|Green (1958), White (1965) et al. Broken River Province. Tectonised, pre-Benambran basement to the Graveyard Creek Subprovince. Straddles the Gray Creek Fault. Mafic and ultramafic rocks suggesting an ophiolitic protolith: supra-subduction rather than MORB. Lithologies discussed; geochemical plots.||||Is overlain by Donaldsons Well Volcanic Member (Judea Formation). Is intruded by Saddington Tonalite.|Serpentinite, clinopyroxenite, amphibolite, metagabbro, metadolerite and rare plagiogranite and felsic dykes. Represents a  layered assemblage now largely serpentinised.|
7724|Gray Creek Complex|72297|5|Briefly described|p702|||Part of a narrow belt extending SW from Greenvale.|||||Serpentinised ultrabasics; contains chromite prospects.|
7724|Gray Creek Complex|73201|6|Mentioned|p609|||Part of a (?)Cambrian ophiolite assemblage.|||||Ultramafic rocks.|
7777|Greenvale Formation|23032|4|Described|p17,18|Early Silurian|Late Ordovician|||||||
7777|Greenvale Formation|23423|5|Briefly described|Plate 8.2a|||||||||
7777|Greenvale Formation|23424|4|Described|Table 8.1 Fig 8.2 p332.|Early Silurian|Late Ordovician|Probably faulted against Wairuna & Pelican Range Fms. Age: unfossiliferous but probably late Ordovician or early Silurian. Similar facies in Perry Ck & Kangaroo Hills Fms. Overlying Unit Clarke River Gp (u). Camel Ck Subprovince.||||||
7777|Greenvale Formation|23430|5|Briefly described|p476|||Broken River Province.||||||
7777|Greenvale Formation|23431|5|Briefly described|p541|||||||||
7777|Greenvale Formation|23494|4|Described|p9, p23 Tb. 1|Silurian|Silurian|Unconformably overlain by Kangaroo Hills Formation.  Quartz siltstone, shale, greywacke sequence.  Intruded by Herbert River Granite.  Max. thickness: 30,000ft?||||||
7777|Greenvale Formation|23498|5|Briefly described|p 23 table 1||Silurian|Unconformably overlain by Graveyard Creek Formation||||||
7777|Greenvale Formation|23509|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Broken River Province.||||||
7777|Greenvale Formation|23617|5|Briefly described|p13|||Now assigned to Kangaroo Hills Formation. Camel Creek Subprovince of Broken River Province.||||||
7777|Greenvale Formation|23619|4|Described|p34 Table 1|Early Silurian|Late Ordovician|Faulted against Wairuna and Pelican Range Formation. Unfossiliferous. Also see p8. Camel Creek Subprovince.||||||
7777|Greenvale Formation|23893|5|Briefly described|p14|Early Silurian|Late Ordovician|Geological Province: Camel Creek Subprovince.||||||
7777|Greenvale Formation|24074|5|Briefly described|p389 Table 1|Silurian|Late Ordovician|Maximum thickness: ?9000m.||||||
7777|Greenvale Formation|24577|4|Described|p752 Fig. 1|Silurian|Ordovician|Overlain by the Perry Creek Formation. Overlies the Tribute Hills Formation. Formation is Fm in text. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
7777|Greenvale Formation|29445|6|Mentioned|p73|||||||||
7777|Greenvale Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Ordovician - Devonian||||||
7777|Greenvale Formation|31832|6|Mentioned|Table 6|||||||||
7777|Greenvale Formation|31999|6|Mentioned|p137|||Fig.3, Table 11||||||
7777|Greenvale Formation|32169|6|Mentioned|Table 2|||Sil.-L.Dev.||||||
7777|Greenvale Formation|32553|4|Described|p52|||||||||
7777|Greenvale Formation|34284|6|Mentioned|Table 1|||Palaeozoic||||||
7777|Greenvale Formation|36472|6|Mentioned|Map legend|Late Silurian|Early Silurian|Late to Early Silurian||||||
7777|Greenvale Formation|37575|4|Described|p181|||See also Fig.3||||||
7777|Greenvale Formation|37727|4|Described|p61|||||||||
7777|Greenvale Formation|39027|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
7777|Greenvale Formation|39445|5|Briefly described|Table 5|||See also P74 & Fig.6||||||
7777|Greenvale Formation|39686|6|Mentioned|Fig.1|||||||||
7777|Greenvale Formation|39689|6|Mentioned|p52|||||||||
7777|Greenvale Formation|39735|6|Mentioned|p16|||||||||
7777|Greenvale Formation|41260|3|Fully described|p14|||Described p137.||||||19-APR-18
7777|Greenvale Formation|41735|6|Mentioned|p284|||See also P285||||||
7777|Greenvale Formation|42031|6|Mentioned|Fig.6 P763|||||||||
7777|Greenvale Formation|42690|5|Briefly described|map legend|Early Devonian|Ordovician?|||||||
7777|Greenvale Formation|42692|5|Briefly described|map legend|Silurian|Ordovician|||||||
7777|Greenvale Formation|42752|5|Briefly described|p45|||see also Fig.2 P46||||||
7777|Greenvale Formation|42933|2|Defined|p20|Early Silurian|Late Ordovician|||||||
7777|Greenvale Formation|43095|5|Briefly described|Plate 2|||||||||
7777|Greenvale Formation|43113|4|Described|Table 1 p21|||Ordivician to Early Silurian||||||
7777|Greenvale Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
7777|Greenvale Formation|43259|6|Mentioned|Appendix 1,p4.|Silurian|Late Ordovician|||||||
7777|Greenvale Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
7777|Greenvale Formation|43716|6|Mentioned|p14|||||||||
7777|Greenvale Formation|43926|2|Defined|Tb.2,opp.p10,map,11|||||||||
7777|Greenvale Formation|44044|2|Defined|p124-5,127-8|||Late Middle Silurian.||||||
7777|Greenvale Formation|44046|14|Not recorded|p153-4|||||||||
7777|Greenvale Formation|44048|14|Not recorded|Map Legend||Silurian|||||||
7777|Greenvale Formation|44049|14|Not recorded|Map Legend||Silurian|||||||
7777|Greenvale Formation|44059|14|Not recorded|p442(Tb)||Early Silurian|(Middle Silurian)||||||
7777|Greenvale Formation|44060|14|Not recorded|Map Legend|Early Devonian|Silurian|||||||
7777|Greenvale Formation|44061|4|Described|Table 1|Early Devonian|Silurian|||||||
7777|Greenvale Formation|44258|14|Not recorded|p32|||Intruded by Herbert River Granite||||||
7777|Greenvale Formation|44359|14|Not recorded|Map Legend||Silurian|(Middle Silurian)||||||
7777|Greenvale Formation|44515|2|Defined|p32,33||Silurian|Intruded by Herbert River Granite. (Silurian, possibly Middle Silurian)||||||
7777|Greenvale Formation|45009|2|Defined|p21,40-46,52,Pl.7,13||Early Silurian|Tb.6. Unconformably overlain by Kangaroo Hills Formation.||||||
7777|Greenvale Formation|45151|6|Mentioned|p8|||See also Table 3.||||||
7777|Greenvale Formation|48904|4|Described|p15|||See Table 1||||||
7777|Greenvale Formation|61727|5|Briefly described|p942 Fig.1|Ordovician|Ordovician|Geological Province: Broken River Province/Camel Creek Subprovince.||||||
7777|Greenvale Formation|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Broken River Province/Camel Creek Subprovince.||||||
7777|Greenvale Formation|67848|5|Briefly described|p3 Fig.2, p8.|||Part of the accretionary wedge in the arc-trench gap succession involved in collisional accretion. Similar to the Wairuna Formation's volcaniclastic rocks.|||||Dominantly lithic sandstone.|
7777|Greenvale Formation|68339|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician?|Camel Creek Subprovince.|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate, local melange; jasper and chert; altered aphyric basalt with local pillows and hyaloclastic breccia in Pelican Range and Greenvale Formations.|
7777|Greenvale Formation|68340|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician?|Camel Creek Subprovince.|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate, local melange; jasper and chert; altered aphyric basalt with local pillows and hyaloclastic breccia in Pelican Range and Greenvale Formations.|
7777|Greenvale Formation|68350|5|Briefly described|Map legend.|||Camel Creek Subprovince, Broken River Province. Age max: Late Ordovician? Age min: Early Devonian?|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate, local melange; altered aphyric basalt with local pillows and hyaloclastic breccia is mapped separately.|30-JUN-15
7777|Greenvale Formation|68351|5|Briefly described|Map legend.|||Camel Creek Subprovince, Broken River Province. Age max: Late Ordovician? Age min: Early Devonian?|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate, local melange; altered aphyric basalt with local pillows and hyaloclastic breccia is mapped separately.|30-JUN-15
7777|Greenvale Formation|68480|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. Late Ordovician? to Early Silurian? in age.|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate; local melange.|
7777|Greenvale Formation|68481|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. Late Ordovician? to Early Silurian? in age.|||||Lithofeldspathic arenite, mudstone and minor polymictic conglomerate; local melange.|
7777|Greenvale Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Broken River Province. This unit, as well as Perry Creek and Kangaroo Hills Formations, are all mapped under the symbol, SDb.||||||
7777|Greenvale Formation|68576|5|Briefly described|Q_11: p38-40|||Camel Creek Subprovince. Forms relatively subdued topography. Unfossiliferous: ages poorly known.|||||A package of lithofeldspathic turbidites: from very thick amalgamated massive sandstone beds, to alternating thin to medium sandstone and mudstone with classic Bouma structures.|
7777|Greenvale Formation|69030|5|Briefly described|p6|Silurian|Silurian|Camel Creek Subprovince (Broken River Province). Both ages are maximum detrital ages, but from near the base and towards the top of the formation.|433.3 +/- 4.2 Ma - 420.7 +/- 5.6 Ma. U/Pb SHRIMP|||||19-APR-18
7777|Greenvale Formation|69079|6|Mentioned|p5, p65|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province. Hosts small gold prospects in NNE-striking faults in the Mount Picklebottle area.||||||
7777|Greenvale Formation|69592|5|Briefly described|p251 Fig.4.35, p268-270, p278-279, p297|Devonian|Late Silurian|See also p303. Camel Creek Subprovince, Broken River Province. Undated. Generally fault-bounded; dislocated into discrete tracts in the NW. May be stratigraphically overlain by Pelican Range Formation. No fossils known.||||Adjacent to Wairuna and Pelican Range Formations.|Lithic sandstone, mudstone and subordinate polymict conglomerate and mafic volcanics, locally hyaloclastic. Sandstone-dominated packages are up to 500m thick and generally massive. Interlayered mudstone/sandstone melange common.|
7777|Greenvale Formation|70207|6|Mentioned|p20|Early Devonian|Silurian|Clarke River and/or Cairns region.||||||
7777|Greenvale Formation|73201|4|Described|p607, p610-618, p620|Middle Devonian|Silurian|Mossman Orogen, Broken River Province. Geochron are U-Pb LA-ICP-MS detrital zircon maximum depositional ages. Detrital zircon provenance is linked to igneous rocks of the Macrossan and Pama Igneous associations. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Interleaved with the Pelican Range Formation and Wairuna Formation. Age given as late Silurian to Middle Devonian.|414 +/- 3.8 Ma, 418 +/- 5.8 Ma||||Lithofeldspathic greywacke with widespread melange and pre-slaty cleavage folding, common mafic volcanic bodies and chert lenses, and uncommon polymict conglomerate horizons.|16-NOV-22
7781|Gregory Downs Limestone|23393|5|Briefly described|p24|Miocene|Oligocene|||||||
7781|Gregory Downs Limestone|23425|4|Described|p383, Table 9.7 p393.|||Geological Province Karumba Basin.||||||
7781|Gregory Downs Limestone|36217|6|Mentioned|p206|||Published by Grimes 1979. Definition approved by Qld SNC.||||||
7781|Gregory Downs Limestone|36228|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
7781|Gregory Downs Limestone|37607|6|Mentioned|Fig.5|||See also P334||||||
7781|Gregory Downs Limestone|38291|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7781|Gregory Downs Limestone|38348|5|Briefly described|p25|||See also P24||||||
7781|Gregory Downs Limestone|39445|5|Briefly described|Table 14|||||||||
7781|Gregory Downs Limestone|39797|6|Mentioned|Map legend|Miocene|Miocene|||||||
7781|Gregory Downs Limestone|42637|6|Mentioned|p29|||||||||
7781|Gregory Downs Limestone|45145|5|Briefly described|p37|||||||||
7781|Gregory Downs Limestone|46902|6|Mentioned|p39|||||||||
7781|Gregory Downs Limestone|61155|5|Briefly described|p16|Miocene|Miocene|?Overlain by Wyaaba and Falloch beds. Age: Together with Carl Creek Limestone thickness is 12m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
7781|Gregory Downs Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Massive, fine to coarsely crystalline limestone.|
7781|Gregory Downs Limestone|67402|5|Briefly described|p177 tbl CRP/KRM1||Longfordian|Karumba Basin. Deposited in a lacustrine environment. Unsuitable reservoir for the storage of carbon dioxide. See also p181 tbl CRP/KRM2, p239.||||Overlies the Bulimba Formation. Unconformably overlain by the Wyaaba beds.|Micritic arenaceous limestone, claystone, chert and conglomerate.|
7781|Gregory Downs Limestone|69599|5|Briefly described|p585|Miocene|Oligocene|Carpentaria region.||||Correlated with Gregory Downs Limestone.||
7788|Gregory Sandstone Member|42894|6|Mentioned|p36|||Of Maryborough Formation.||||||13-MAR-09
7788|Gregory Sandstone Member|60281|5|Briefly described|p37, p40, Fig.33 App 1|Cretaceous|Cretaceous|Basal unit of the Maryborough Formation.  Overlain by the Cherwell Mudstone Member.  Geological Province: Maryborough Basin.||||||
7788|Gregory Sandstone Member|61611|5|Briefly described|p264, p266, p267|Cretaceous|Cretaceous|Basal unit of Maryborough Formation. Underlain by Cherwell Mudstone Member. Geological Province: Maryborough Basin. Consists of sandstones, siltstones and shales with minor conglomerates, deposited in margial marine to esturine environments.||||||
7788|Gregory Sandstone Member|69582|5|Briefly described|p53|||Maryborough Basin. Shallow marine rocks. Thermal conductivity is provided. Intersected in GSQ Maryborough 16. This unit is interpreted as the basal 500m of the Maryborough Formation.||Maryborough Formation.|||Sandstone.|
7819|Greymare Granodiorite|32491|5|Briefly described|p16|||Upper Permian or Triassic.||||||19-NOV-07
7819|Greymare Granodiorite|32492|6|Mentioned|Map legend|Triassic|Late Permian|Upper Permian or Triassic||||||
7819|Greymare Granodiorite|32876|6|Mentioned|Map legend|Early Triassic|Late Permian|Upper Permian-Lower Triassic||||||
7819|Greymare Granodiorite|32880|4|Described|p3|||See also p11. Upper Permian or Lower Triassic.||||||19-NOV-07
7819|Greymare Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
7819|Greymare Granodiorite|38905|6|Mentioned|p303|||||||||
7819|Greymare Granodiorite|39071|6|Mentioned|p346|||||||||
7819|Greymare Granodiorite|39445|5|Briefly described|Table 12|||||||||
7819|Greymare Granodiorite|43008|5|Briefly described|map legend|||||||||
7819|Greymare Granodiorite|48940|4|Described|p65|||||||||
7819|Greymare Granodiorite|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Grey, medium-grained, uneven-grained to slightly porphyritic, quartz-rich, biotite tonalite to granodiorite; moderate to high magnetic response.||||||
7819|Greymare Granodiorite|63748|4|Described|p16, p26, p28-30|Early Triassic|Permian|Of Greymare Suite. Age:279.6+/-2.6Ma (SHRIMP). Intrudes Texas beds. I-type; grey, fine- to med.-grained, slightly porphyritic to uneven-grained, quartz-rich tonalite to granodiorite? Possibly should be termed a 'tonalite'. Further lith.details included.||||||07-FEB-11
7819|Greymare Granodiorite|65668|6|Mentioned|p1, p16|Permian|Permian|Age: c.280 Ma. Undeformed; intrudes accretionary wedge sediments.||||||
7819|Greymare Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Jibbinbar, Mount Bullaganang, Mount You You and Palgrave Granites, and Boxwell Granodiorite, are all mapped under the symbol, Pgn.||||||
7819|Greymare Granodiorite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
7819|Greymare Granodiorite|68679|4|Described|p455-457, p464-466|Permian|Permian|Northern New England Batholith (NNEB). Originally assigned to the Greymare Supersuite by Donchak et al. (2007). ~45 km2. Compositionally distinct from all other granitoids in the NNEB. Cut by a dyke swarm extending from Braeside to Greymare. Geochemistry described in some detail; geochemical plots. Has adakitic affinities; may be prospective for Cu and Cu-Au.|279.6 +/- 2.6 Ma (SHRIMP: PRISE, ANU).|Greymare Suite.||Intrudes Texas beds.|Grey, fine- to medium-grained, porphyritic to uneven-grained tonalite to granodiorite?; slightly altered; slightly to moderately deformed. Widespread ~2cm biotite phenocrysts and rare hornblende, are characteristic. Unevolved, low-medium-K, I-type.|
7819|Greymare Granodiorite|68901|5|Briefly described|p8, p6|Early Permian|Early Permian|New England Region. SHRIMP age derived from Donchak et al, 2007.|279.6 +/- 2.6 Ma (SHRIMP U-Pb)|||||26-SEP-18
7819|Greymare Granodiorite|70373|6|Mentioned|p790|Early Permian|Early Permian|Probable variation on Greymare Granite, p800.||||||
7819|Greymare Granodiorite|70876|5|Briefly described|p77|Early Permian|Early Permian|New England Orogen. SHRIMP date is derived from Donchak et al, 2013.|279.6 +/- 2.6 Ma (SHRIMP U-Pb)|Clarence River Supersuite||||
7819|Greymare Granodiorite|71628|6|Mentioned|p18: 10|||Robertson (1970). Now Greymare Tonalite.||||||
7819|Greymare Granodiorite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Warwick.||||||
7819|Greymare Granodiorite|73197|6|Mentioned|p475 Fig.6, p477-478|Cisuralian|Cisuralian|New England Orogen, southern. Depleted in K, Th and U.|279 Ma||||Granitic intrusive.|
7826|Griman Creek Formation|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3, p498|Albian|Albian|N Surat Basin. Up to 48m thick.|||||Labile glauconitic and commonly calcareous sandstone, with siltstone and minor mudstone; intraformational conglomerates and thin coal lenses in upper part; molluscan coquinites in lower part.|
7826|Griman Creek Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Albian|Albian|In Surat Basin, Eromanga Basin.||||||
7826|Griman Creek Formation|22757|5|Briefly described|Table6,p11||Early Cretaceous|200 m thick. Surat Basin||||||
7826|Griman Creek Formation|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Cenomanian|Albian|Of the Rolling Downs Group. Lithic arenite, siltstone, minor conglomerate. Contains the Coocoran Claystone Member. Max. thickness: 30m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5..||||||
7826|Griman Creek Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
7826|Griman Creek Formation|23053|6|Mentioned|p86|||||||||
7826|Griman Creek Formation|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 345m.||||||
7826|Griman Creek Formation|24085|5|Briefly described|p42 Tb.2|Early Cretaceous|Early Cretaceous|Freshwater deposit.||||||
7826|Griman Creek Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|29387|6|Mentioned|Table 5|||||||||
7826|Griman Creek Formation|29721|6|Mentioned|Table 246|||||||||
7826|Griman Creek Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7826|Griman Creek Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
7826|Griman Creek Formation|31116|4|Described|p45|||See also P1. L.Cretaceous||||||
7826|Griman Creek Formation|31208|6|Mentioned|Table 1|||See also Fig. 7||||||
7826|Griman Creek Formation|31376|6|Mentioned|p4|||||||||
7826|Griman Creek Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|32314|6|Mentioned|Fig. 4|||||||||
7826|Griman Creek Formation|32796|2|Defined|p30|middle Albian|early Albian|Lower to Middle Albian.||||||17-NOV-15
7826|Griman Creek Formation|33070|4|Described|Table 2|||L.Cret.||||||
7826|Griman Creek Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33090|4|Described|Table 4|||L.Cret.||||||
7826|Griman Creek Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
7826|Griman Creek Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
7826|Griman Creek Formation|33448|6|Mentioned|p7|||||||||
7826|Griman Creek Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33642|6|Mentioned|p144|||Refers Jenkins (1960).||||||
7826|Griman Creek Formation|34613|6|Mentioned|Table 4|||||||||
7826|Griman Creek Formation|34948|6|Mentioned|Fig. 70|||||||||
7826|Griman Creek Formation|35793|6|Mentioned|Fig.3|||||||||
7826|Griman Creek Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
7826|Griman Creek Formation|35937|6|Mentioned|Fig.5|||||||||
7826|Griman Creek Formation|36243|6|Mentioned|Table 7A|||||||||
7826|Griman Creek Formation|36356|6|Mentioned|p66|||||||||
7826|Griman Creek Formation|36581|6|Mentioned|p464|||||||||
7826|Griman Creek Formation|36749|6|Mentioned|p144|||||||||
7826|Griman Creek Formation|37117|5|Briefly described|p313|||||||||
7826|Griman Creek Formation|37995|4|Described|p66|||||||||
7826|Griman Creek Formation|38199|6|Mentioned|p431|||||||||
7826|Griman Creek Formation|39211|5|Briefly described|p33|||||||||
7826|Griman Creek Formation|39212|5|Briefly described|p18|||||||||
7826|Griman Creek Formation|39216|6|Mentioned|p56|||||||||
7826|Griman Creek Formation|39445|5|Briefly described|Table 11|||||||||
7826|Griman Creek Formation|39943|6|Mentioned|Table 9A|||||||||
7826|Griman Creek Formation|40245|6|Mentioned|Table 2|||||||||
7826|Griman Creek Formation|40249|6|Mentioned|p38|||Mention Fig.1||||||
7826|Griman Creek Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
7826|Griman Creek Formation|41064|6|Mentioned|p62|||||||||
7826|Griman Creek Formation|41187|6|Mentioned|Fig.2|||||||||
7826|Griman Creek Formation|41216|6|Mentioned|Fig.18|||||||||
7826|Griman Creek Formation|41266|6|Mentioned|Fig.3|||||||||
7826|Griman Creek Formation|41628|6|Mentioned|p86|||||||||
7826|Griman Creek Formation|41992|4|Described|Fig.2 P183|||||||||
7826|Griman Creek Formation|42007|5|Briefly described|p182|||||||||
7826|Griman Creek Formation|42071|6|Mentioned|p117|||||||||
7826|Griman Creek Formation|42429|5|Briefly described|p156|||||||||
7826|Griman Creek Formation|42494|5|Briefly described|Table 1 P24|||||||||
7826|Griman Creek Formation|42673|5|Briefly described|Fig.2, P184|||||||||
7826|Griman Creek Formation|43000|5|Briefly described|Fig.5,p112|||Of Rolling Downs Group.||||||13-MAR-09
7826|Griman Creek Formation|43002|5|Briefly described|Fig.2,p135|||||||||
7826|Griman Creek Formation|43085|5|Briefly described|Fig.4|||0f Rolling Downs Group||||||
7826|Griman Creek Formation|43196|6|Mentioned|p418|||||||||
7826|Griman Creek Formation|43459|14|Not recorded|p316-7|||||||||
7826|Griman Creek Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Rolling Downs Group||||||
7826|Griman Creek Formation|43995|14|Not recorded|Tb.p9||Cretaceous|Equivalent to Blythesdale Group.||||||
7826|Griman Creek Formation|45110|2|Defined|p121|late Albian|late Albian|See also p24 & Table 18. Formerly Griman Ck.Gp. (Jenkins,59).||||||17-NOV-15
7826|Griman Creek Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
7826|Griman Creek Formation|46791|4|Described|p48|||||||||
7826|Griman Creek Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7826|Griman Creek Formation|46984|6|Mentioned|Table 1|||||||||
7826|Griman Creek Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
7826|Griman Creek Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
7826|Griman Creek Formation|60524|5|Briefly described|p485, p486 Fig. 1|Aptian|Aptian|Coastal brackish/estuarine to freshwater fluviatile-lacustrine unit; contains viviparids, thiarids and other non-marine gastropod taxa.  Geological Province: Surat Basin.  See also p488.||||||21-OCT-04
7826|Griman Creek Formation|61198|5|Briefly described|p5, p6 Tb. 1, p18-20, p43|Cretaceous|Cretaceous|Where exposed, rock is weathered and silicified; unweathered rock is bluish-grey (due to finely disseminated pyrite) and greenish-grey glauconitic rocks; dominantly siltstone and very fine sst in which sedimentary structures have been preserved. p29-30.||||||25-JAN-06
7826|Griman Creek Formation|61199|5|Briefly described|p1, p4|Cretaceous|Cretaceous|Meta-sediments. Mentioned also in terms of equivalent rocks. See also pages, 7,9,11 etc. - Figures 4, 5, and 7 etc.||||||25-JAN-06
7826|Griman Creek Formation|61200|5|Briefly described|p1, p7 Tb. 2|Cretaceous|Cretaceous|Deltaic to marine deposits at base, and fluviatile deposits in upper part of unit - characterised by labile sandstone, siltstone, minor mudstone; variably kaolinised, silicified and ferruginised.||||||
7826|Griman Creek Formation|61221|4|Described|p1-2, p5, p13|Cretaceous|Cretaceous|Geological Province: Surat Basin. Weathered and mottled sandstone in outcrop. Fresher rock consists of red coloured, commonly medium grained, well sorted arkosic sandstone frequently interbedded with shale beds.||||||
7826|Griman Creek Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Labile sandstone, siltstone, minor conglomerate. Geological Province: Surat Basin.||||||07-FEB-11
7826|Griman Creek Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
7826|Griman Creek Formation|63218|6|Mentioned|p211. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|64061|4|Described|p66, p67|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Geol. prov: Surat Basin. Mostly non-marine: comprises interbedded fine-grained sandstones, mudstones + siltstones (sporadically with intraformational conglomerate, coal+glauconitic pellets reworked from underlying marine strata.||||||17-APR-08
7826|Griman Creek Formation|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|Surat Basin||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|64856|3|Fully described|p79, p100-102|Albian|Albian|Reiser (1970) after Jenkins (1960). Originally the Griman Creek Group (Jenkins, 1959), which also included a weathered upper unit which he named the Telgazli Formation. Superseded by Griman Creek Formation (Jenkins, 1960). This was expanded by Thomas and Reiser (1968) to include the Telgazli Formation, in their informal Griman Creek beds. This last was redefined by Reiser (1970) as the Griman Creek Formation, with a reference section 8-346m in GSQ Surat 3. Surat Basin. Thinly bedded fine to medium grained labile sandstone, siltstone, mudstone, with thick sandstone beds and minor muddy siltstone, intraformational conglomerate and coal. Conformably overlies Surat Siltstone. Age from palynoflora (unit APK5).| | ||||29-NOV-17
7826|Griman Creek Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Surat Siltstone, Surat Basin.||||||
7826|Griman Creek Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
7826|Griman Creek Formation|65112|6|Mentioned|p329, Fig 11 p324; Fig 16 p328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|135-101 Ma.|||Overlies Surat Siltstone.||22-MAR-12
7826|Griman Creek Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Surat Siltstone.||||||
7826|Griman Creek Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
7826|Griman Creek Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Overlies the Surat Siltstone, Surat Basin||||||
7826|Griman Creek Formation|65119|5|Briefly described|Table 1 p504, fig 2,7- 8, 14, 16-19|Aptian|Aptian|Surat Basin. Lithic glauconitic, sandstone, siltstone and mudstone, up to 480 m thick. Age: ?-107Ma. Fission Track age: 103+/-9 Ma.||||||07-MAR-12
7826|Griman Creek Formation|65386|5|Briefly described| S141, S142, S146 Fig.7, S147|Cretaceous|Cretaceous|Marginal marine and freshwater sediments. Slightly deformed and extensively weathered. Western margin of Surat Basin.||||||
7826|Griman Creek Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|66623|6|Mentioned|p265.|||Surat Basin. Equivalent in part to Allaru Mudstone, Koonenberry Belt.||||||
7826|Griman Creek Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
7826|Griman Creek Formation|67402|4|Described|p146 fig SRT3, p148, p156|Albian|Albian|Surat Basin. Deposited in nearshore marine to deltaic environments. Approximately 346m thick.||||Overlies the Surat Siltstone.|Sandstone, minor muddy siltstone, intraformational conglomerate and coal.|
7826|Griman Creek Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|68069|4|Described|Map legend, p2.|Early Cretaceous|Early Cretaceous|Surat Basin. Terrestrial (possibly estuarine) environment. Forms subdued outcrop and is only exposed on the margins of slope systems where preserved by Tertiary silcrete. Zone to 30 m is host for opal mineralisation.||Topmost unit in Rolling Downs Group.|Includes Coocoran Claystone Member and the Wallangulla Sandstone Member.|Overlies Surat Siltstone conformably.|Interbedded fine- to medium-grained sandstone with rhyolite detritus, siltstone and claystone, minor coal; grey when unweathered, surface exposures are kaolinised and locally silicified; plant fossils common; opalised plant and animal fossils.|12-JUN-14
7826|Griman Creek Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
7826|Griman Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat Basin. ||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation.||
7826|Griman Creek Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|68593|3|Fully described|p4-8, p11, p23, p44, p47, p84-86|Albian|Albian|Said to be redefined, but most information only refers to Angledool. Defined by Reiser (1970): his type section was the interval between 25' and 1135' (7.6m and 346m) in GSQ drillhole Surat 3. Named after Griman Creek near Surat (Qld). 196.5m thick in borehole (Bourke, 1973); up to 400m thick in Surat Inlier. New type section [actually new Reference section]: eastern walls in Lunatic Hill open cut (GR 593940mE 6740354mN). Felsic volcanic origin. Relatively abundant and highly diverse fossils (listed in Appendix 6). Middle to possibly late Albian. Depositional environment changed from beach or near-shore marine at the base, to flood-plain in upper parts.||Rolling Downs Group.|Wallangulla Sandstone, Coocoran Claystone, Members.|Conformably overlies Surat Siltstone. Is overlain unconformably by Cumborah Gravel.|Grey, weathering to white, fine- to medium-grained sandstone, laminated to massive siltstone, and mudstone; kaolinised. Intraformational conglomerate and coal present in upper part.|11-DEC-15
7826|Griman Creek Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Albian|Albian|Surat Basin. Fluvial floodplain to paralic.||Of the Rolling Downs Group.|Includes Coocoran Claystone, Wallangulla Sandstone, Finch Claystone, and Lower Griman Creek Formation.|||16-JAN-17
7826|Griman Creek Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, pp298-301, p307|Cretaceous|Cretaceous|Lower Cretaceous age. Contains ubiquitous disseminated pyrite. Fluvial to fluvial-lacustrine depositional environment (brackish).||Of the Rolling Downs Group.||Underlain by the Surat Siltstone.|Comprises fluvial sandstone and siltstone.|
7826|Griman Creek Formation|69582|5|Briefly described|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Surat Siltstone.||
7826|Griman Creek Formation|69594|5|Briefly described|p519, p538-539, p550, p574|Albian|Albian|Jenkins (1959, 1960); Reiser (1970). The uppermost unit of the Surat Basin. Refers to most of the Cretaceous rocks S and E of Surat, including its weathered equivalent, the Telgazli Formation (Jenkins, 1959) as synonymised by Thomas and Reisler (1968). Up to 400m thick. Initially shallow-marine or shoreline deposits, followed by paralic to deltaic grading to floodplain conditions in the upper part. Diverse fossils (in NSW).||||Conformably overlies Surat Siltstone. Correlated with Styx Coal Measures.|Labile sandstones, siltstones and mudstones, with intraformational conglomerate and minor coal, mostly in the upper parts. Shelly coquinas occur low in the Formation.|
7826|Griman Creek Formation|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|70836|5|Briefly described|p473-475|Albian|Albian|Surat Basin; Lightning Ridge area. Contains fragmentary remains of a new, unnamed megaraptorid: systematic paleontology. Regressive beach or nearshore marine deposits, followed by paralic to deltaic and finally fluvial floodplain conditions. Diverse vertebrate fauna (listed). Limited age determinations discussed.|~107 Ma to c.99 Ma (fission-track).|Rolling Downs Group.||Overlies Surat Siltstone. Coeval with Toolebuc and Allaru Formations.|Primarily non-marine, thinly-bedded and interlaminated fine- to medium-grained sandstone and mudstone. Freshwater and brackish molluscs in lower part; coal seams and freshwater molluscs in upper part.|
7826|Griman Creek Formation|71092|6|Mentioned|p237|Early Cretaceous|Early Cretaceous|Lightning Ridge. Contains the turtle fossil Spoochelys ormondea.||||||
7826|Griman Creek Formation|71601|5|Briefly described|p120, p121-122, 123|Albian|Albian|Geological province: Surat Basin. Near Lightning Ridge, NSW. A succession of regressive beach or nearshore marine to paralic/deltaic, and finally fluvial floodplain deposits. Includes diverse dinosaurian fauna, e.g. plesiosaurs. Evidence of ankylosaurians described.||Unit of Rolling Downs Group.|Wallangulla Sandstone Member, Finch clay facies.||Includes some coal seams near top.|
7826|Griman Creek Formation|72297|6|Mentioned|p758|Cretaceous|Cretaceous|An extension of this unit in the Hebel-Dirranbandi area hosts opal.||||||
7826|Griman Creek Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|73113|6|Mentioned|p22|Late Cretaceous|Late Cretaceous|Partial aquifer.||||||
7826|Griman Creek Formation|73153|6|Mentioned|p285|Cenomanian|Cenomanian|Holotype material[?] (NHMUK R3718) for Rapator ornitholestoides (a megaraptoran) was recovered from this unit in New South Wales, as well as a fragmentary cervical vertebra (LRF 3050.AR) classified within Noasauridae.||||||
7826|Griman Creek Formation|73203|6|Mentioned|p648|Cretaceous|Cretaceous|Hosts opal at Lightning Ridge.|||Finch Clay Facies|||
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.||
7852|Guilder Formation|41277|6|Mentioned|p83|||||||||
7852|Guilder Formation|41740|6|Mentioned|p222|||||||||
7864|Gum Gully member|36906|5|Briefly described|p28|||Informal name mentioned P26.||||||
7864|Gum Gully member|37675|6|Mentioned|p3|||||||||
7864|Gum Gully member|38310|6|Mentioned|p237|||||||||
7866|Gum Ridge Formation|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia|Ordian-Early Templetonia|||||||
7866|Gum Ridge Formation|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
7866|Gum Ridge Formation|23410|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Chertified bioclast, onkoid and cryptomicrobial limestone, marly calcimudstone, minor siliciclastic mudstone; carbonate and evaporite nodules; basal sandstone and siliciclastic mudstone; fossiliferous. Geol. Prov: Georgina Basin.||||||02-NOV-05
7866|Gum Ridge Formation|23981|6|Mentioned|p65|||Geological Province: western Georgina Basin in NT.||||||
7866|Gum Ridge Formation|24172|4|Described|p55|Cambrian|Cambrian|Unconformably overlies Helen Springs Volcanics . Max. Thickness: 14m.||||||21-SEP-06
7866|Gum Ridge Formation|24297|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral equivalent of Montejinni Limestone. Geological Province: Georgina Basin.||||||
7866|Gum Ridge Formation|24303|2|Defined|p36, p63 Appendix|Ordian-Early Templetonian|Ordian-Early Templetonian|Overlain by the Anthony Lagoon beds. Overlies the Helen Springs Volcanics. Geological Province: Barkly Sub-basin, Georgina basin. Max. Thickness: 150.5m. Equivalent to Montejinni Limestone, Tindall Limestone, Linekar Limestone, Panton Fm. & Top Springs Ls||||||24-MAR-16
7866|Gum Ridge Formation|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Limestone: fine-grained sandstone and siliciclastic mudstone; bioclast, oncoid, styololitic and cryptomicrobial limestone, marly limestone; fossiliferous, nodular chert; carbonate and evaporite pseudomorphs; silicified, recessive.||||||17-OCT-05
7866|Gum Ridge Formation|29940|6|Mentioned|p169|||||||||
7866|Gum Ridge Formation|30017|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7866|Gum Ridge Formation|30320|6|Mentioned|p422|||||||||
7866|Gum Ridge Formation|30479|6|Mentioned|p19|||||||||
7866|Gum Ridge Formation|32174|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Early Middle Cambrian||||||
7866|Gum Ridge Formation|32959|6|Mentioned|Fig.12|||||||||
7866|Gum Ridge Formation|33307|6|Mentioned|Fig.8|||||||||
7866|Gum Ridge Formation|33516|6|Mentioned|p99|||||||||
7866|Gum Ridge Formation|34053|6|Mentioned|p8|||M.Camb.  See also P11||||||
7866|Gum Ridge Formation|34149|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|34151|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|34439|6|Mentioned|p9|||See also P11. Middle Cambrian||||||
7866|Gum Ridge Formation|34440|5|Briefly described|Table 1|||M.Camb. PP8,10||||||
7866|Gum Ridge Formation|34441|4|Described|Table 1|Middle Cambrian||M.Camb. See also pp11,12,14 etc.||||||14-NOV-06
7866|Gum Ridge Formation|35224|6|Mentioned|p5|||||||||
7866|Gum Ridge Formation|35231|6|Mentioned|p8|||||||||
7866|Gum Ridge Formation|35771|4|Described|Table 1|||||||||
7866|Gum Ridge Formation|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
7866|Gum Ridge Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
7866|Gum Ridge Formation|37572|4|Described|p156|||See also p165.||||||21-SEP-06
7866|Gum Ridge Formation|39213|6|Mentioned|Fig.8|||||||||
7866|Gum Ridge Formation|39624|4|Described|p43|||||||||
7866|Gum Ridge Formation|39900|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian||||||
7866|Gum Ridge Formation|40580|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|40852|6|Mentioned|p37|||See also Fig.3.9||||||
7866|Gum Ridge Formation|40856|5|Briefly described|p315|||||||||
7866|Gum Ridge Formation|41128|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Chert, ferruginised, laminated and concentrically banded; siltstone, laminated and fossiliferous, coquinite, ferruginised and silicified; minor sandstone; rare dolostone. Geological Province: Georgina Basin.||||||16-NOV-05
7866|Gum Ridge Formation|41129|3|Fully described|p15|||||||||
7866|Gum Ridge Formation|41204|4|Described|p13|||Mention p4.||||||21-SEP-06
7866|Gum Ridge Formation|41205|5|Briefly described|Map legend|Cambrian|Cambrian|Siltstone, chert, sandstone. Geological Province: Georgina Basin.||||||16-NOV-05
7866|Gum Ridge Formation|41308|4|Described|p13|||||||||
7866|Gum Ridge Formation|41310|5|Briefly described|p14|||||||||
7866|Gum Ridge Formation|41524|6|Mentioned|p6|||||||||
7866|Gum Ridge Formation|42643|6|Mentioned|p26|||||||||
7866|Gum Ridge Formation|42956|5|Briefly described|p31 Fig.4|||||||||
7866|Gum Ridge Formation|43223|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
7866|Gum Ridge Formation|43224|5|Briefly described|Map legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
7866|Gum Ridge Formation|43652|6|Mentioned|p386|||||||||
7866|Gum Ridge Formation|44201|6|Mentioned|p.10|||||||||
7866|Gum Ridge Formation|44205|14|Not recorded|p49|||||||||
7866|Gum Ridge Formation|44283|14|Not recorded|p.8|||Outcrops to west of Alroy sheet.||||||
7866|Gum Ridge Formation|44285|14|Not recorded|Tb.opp.p.6||Middle Cambrian|May be continuous with Wonarah Beds. M.Cambrian.||||||
7866|Gum Ridge Formation|44322|5|Briefly described|map legend||Cambrian|||||||22-DEC-09
7866|Gum Ridge Formation|44441|14|Not recorded|opp.p.6, Tb.1||Middle Cambrian|May be continuous with Wonarah Beds. Mid.Cambrian. (E53-16).||||||
7866|Gum Ridge Formation|44960|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|44965|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|45032|14|Not recorded|p8||Middle Cambrian|||||||
7866|Gum Ridge Formation|45045|6|Mentioned|p7|||||||||
7866|Gum Ridge Formation|45052|2|Defined|p75|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|45055|6|Mentioned|p7|||See also P8,10,11,22,23||||||
7866|Gum Ridge Formation|45062|6|Mentioned|p11|||||||||
7866|Gum Ridge Formation|45064|3|Fully described|Table 1|||See also p19.||||||21-SEP-06
7866|Gum Ridge Formation|45148|6|Mentioned|p11|||||||||
7866|Gum Ridge Formation|45167|5|Briefly described|p53|||||||||
7866|Gum Ridge Formation|45373|14|Not recorded|p.177,178|||||||||
7866|Gum Ridge Formation|47058|6|Mentioned|Fig.3 P123|||||||||
7866|Gum Ridge Formation|48831|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|48835|14|Not recorded|p.16,Pl.1|||||||||
7866|Gum Ridge Formation|48860|4|Described|p.17||Cambrian|On many pages. p.1,4,7,17,70, Pl.6. Lower Middle Cambrian. (E53-14/Tennant Creek). See base card under Helen Springs Volcs.||||||
7866|Gum Ridge Formation|48891|14|Not recorded|p.22||Cambrian|Tb.1. L-M Cambrian.||||||
7866|Gum Ridge Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin.  Contains fauna of Ordian age.||||||
7866|Gum Ridge Formation|60637|5|Briefly described|Map legend|||Fossiliferous siltstone and chert; silicified limestone; some sandstone and leached calcareous sandstone; silicified limestone.||||||
7866|Gum Ridge Formation|60684|4|Described|p14||Ordian-Early Templetonia|Chert, chert breccia, limestone. Most common lithotype: red-brown to yellow-grey tabular chertified rocks, with occasional trilobites and lingulate brachiopods.  Overlies Helen Springs Volcanics. Max. thickness: 145m (clay, dolostone, chert on FREW RIVER)||||||14-DEC-05
7866|Gum Ridge Formation|60685|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral correlative of Montejinni Limestone. Geological Province: Georgina Basin.||||||
7866|Gum Ridge Formation|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Georgina Basin. Faunal links with Antarctica.||||||
7866|Gum Ridge Formation|61567|5|Briefly described|p632|Cambrian|Cambrian|In the Amelia impact structure this unit is composed of chert and cherty breccias up to 10m thick.  See also p633 Tb. 1.||||||27-APR-06
7866|Gum Ridge Formation|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Georgina Basin (NT).||||||07-FEB-11
7866|Gum Ridge Formation|63569|6|Mentioned|p123|Cambrian|Cambrian|Georgina Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
7866|Gum Ridge Formation|64068|6|Mentioned|p53, 59|Cambrian|Cambrian|Western Georgina Basin. Correlated with Thorntonia Limestone.||||Transitionally or disconformably overlies Andagera Formation.||05-APR-12
7866|Gum Ridge Formation|64443|6|Mentioned|p10, p31, p40|Middle Cambrian|Ordian-Early Templetonian|Fossiliferous. Barkly Sub-basin.||Of Barkly Group.||||14-MAY-14
7866|Gum Ridge Formation|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
7866|Gum Ridge Formation|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Barkly Sub-basin, central Georgina Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
7866|Gum Ridge Formation|65344|4|Described|p3, 5, 6, 7, 8, 9, 12, 20-24, Figs.,Tbls|Middle Cambrian|Middle Cambrian|Of the Barkly Sub-basin, Georgina Basin. See well logs and thin section descriptions for detail. Thickness: up to 148.8m in NTGS02/1||||Overlies the South Nicholson Group and the Helen Springs Volcanics. Underlies the Anthony Lagoon beds and the Wonarah Formation.|Dolostone.|03-MAY-12
7866|Gum Ridge Formation|65345|5|Briefly described|pp3-4, p6 Fig.5, p11 Fig.11. |Cambrian|Cambrian|Western Georgina Basin.Contains two intervals with anomalous phosphate.  Equivalent to the Tindall Limestone of the Daly Basin, and to the Montejinni Limestone/Hooker Creek Formation/Lothari Hill Sandstone sequence in the Wiso Basin.||||Is unconformably overlain by Anthony Lagoon beds.|Cherty limestone, mudstone, siltstone and sandstone.|
7866|Gum Ridge Formation|67148|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|||Unit in Barkly Group.||Is unconformably overlain by Wonarah Formation.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, ribbon limestone, minor oncoid rudstone; minor maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate.|
7866|Gum Ridge Formation|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Unit in Barkly Group.||Overlies Helen Springs Volcanics. Is overlain by Anthony Lagoon and Wonarah Formations.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, mudstone interbeds; minor oncoid rudstone, maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate.|
7866|Gum Ridge Formation|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Unit in Barkly Group.||Unconformably overlies Helen Springs Volcanics and South Nicholson Group. Is unconformably overlain by Anthony Lagoon Formation.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, mudstone interbeds; minor oncoid rudstone, maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate (cross-section only).|
7866|Gum Ridge Formation|67352|6|Mentioned|v, pages17-21,23,40,44-45,47,49,50-52,69|Middle Cambrian|Middle Cambrian|Full description on pp 19-21. Simplified lithology quoted here. Contains a widespread (NT-SA-Antarctica) fossil fauna.||Barkly Group||Correlative of Top Springs Limestone. Is conformably overlain by Anthony Lagoon or Wonarah Formations. Overlies (disconformably) Helen Springs Volcanics or Renner Group or South Nicholson Group.|Two successive marine limestone units, each underlain by thin (8-10 m thick) peritidal siliciclastic intervals.|
7866|Gum Ridge Formation|68518|6|Mentioned|p14|||Sandover beds are probable correlatives in Hatches Creek Region (Blake and other, 1986)||||||30-JUN-14
7866|Gum Ridge Formation|69437|5|Briefly described|p22:9-10|Series 2|Series 2|Barkly Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 1. Restricted marine and peritidal deposits.||||Overlies Helen Springs Volcanics. Is overlain by Anthony Lagoon Formation. Is equivalent to Top Springs Limestone.|Limestone and minor siliciclastic mudstone.|12-JUL-16
7866|Gum Ridge Formation|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Georgina Basin. Correlation based on a distinct positive excursion in stable carbon and oxygen isotopes.||||Time-equivalent to Giles Creek Dolostone (Amadeus Basin).||12-JUL-16
7866|Gum Ridge Formation|69443|4|Described|p28:12, 16, 21-22, 42|Middle Cambrian|Middle Cambrian|Opik in Ivanac (1954). Central and western Georgina Basin. Crops out discontinuously as low, rubble-covered plateaux and rises. Commonly pervasively ferruginised and/or silicified to chert. Is correlated with Narpa Group, Tindall and Montejinni Limestones. Is lateral equivalent of, and likely to be continuous under cover with, Top Springs Limestone. Numerous sedimentary structures listed. Thickness consistently 141-151m, thinning locally to 51m. Diverse fossil assemblage. Restricted marine shelf deposits, subject to episodic peritidal influence. Hosts an ore-grade (>15% P2O5) phosphorite horizon in the Wonarah area.||Barkly Group.||Disconformably overlies Helen Springs Volcanics, Renner or South Nicholson Groups, Andagera Formation (?transitionally). Conformably underlies Anthony Lagoon or (disconformably?) Wonarah Formations.|Commonly partially dolomitised, massive, ribbon, bioclast, lithoclast and minor oncoid limestone, and minor cryptomicrobial dololaminite and siliciclastic mudstone. Local thin basal siltstone or basal conglomerate.|12-JUL-16
7866|Gum Ridge Formation|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Central Georgina Basin.||||Unconformably overlies Helen Springs Volcanics (Kalkarindji Suite).||12-JUL-16
7866|Gum Ridge Formation|69446|5|Briefly described|p31:3-4|Middle Cambrian|Middle Cambrian|Georgina Basin. Broadly age-equivalent to Daly River Group (Daly Basin).||||Is overlain by Anthony Lagoon Formation.|Carbonate-dominated.|12-JUL-16
7866|Gum Ridge Formation|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
7866|Gum Ridge Formation|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
7866|Gum Ridge Formation|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
7866|Gum Ridge Formation|69673|5|Briefly described|p117, p142|||151m thick.||Barkly Group|||Dolomitised limestone, siliciclastic mudstone.|
7866|Gum Ridge Formation|70380|5|Briefly described|p745, p759|Stage 5|Stage 4|Barkly Sub-basin, Georgina Basin.||||Correlated with Tindall Limestone (Daly Basin).||
7866|Gum Ridge Formation|70752|5|Briefly described|p125, p127, p131, p137, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains at least two linguliform brachiopod species also found in Giles Creek Dolostone. Ordian age from the age-diagnostic trilobite Redlichia gumridgensis. Systematic palaeontological descriptions.||||||
7866|Gum Ridge Formation|70968|5|Briefly described|p112|Middle Cambrian|Middle Cambrian|Georgina Basin. The Lake Woods beds were originally mapped as part of this unit in HELEN SPRINGS (Randal et al., 1966) and BEETALOO (Brown and Randal, 1969) .||||||
7866|Gum Ridge Formation|72321|5|Briefly described|Fig 2|Stage 4|Stage 4|Western Georgina Basin.   Age Cambrian Series 2, Stage 4, Australian Stage: Ordian.||of Narpa Group.||Correlated with Hay River Formation,  Top Springs Limestone.||
7866|Gum Ridge Formation|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
7866|Gum Ridge Formation|73083|6|Mentioned|p7, p22, p25|Cambrian|Cambrian|Contains macrofossils of trilobites and brachiopods.||||||
7931|Gurrumba Ring Complex|23423|4|Described|p314 Table 7.4|Early Permian|Late Carboniferous|I-Type. Intrudes Hodgkinson Formation, Emuford and Opah Granite. Also see p255.||||||
7931|Gurrumba Ring Complex|23446|6|Mentioned|p448 Fig.1|||||||||
7931|Gurrumba Ring Complex|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
7931|Gurrumba Ring Complex|23503|5|Briefly described|Map Legend||Late Carboniferous|||||||
7931|Gurrumba Ring Complex|23616|6|Mentioned|Table 3 p56|||Referred to as the Gurrumba Volcanic Neck.||||||
7931|Gurrumba Ring Complex|23624|4|Described|p24|Permian|Permian|Formerly Gurrumba Volcanic Neck.||||||09-SEP-04
7931|Gurrumba Ring Complex|39564|6|Mentioned|p14|||||||||
7931|Gurrumba Ring Complex|41297|6|Mentioned|Fig.1|||||||||
7931|Gurrumba Ring Complex|43259|4|Described|Appendix 1,p44.||Carboniferous|||||||
7931|Gurrumba Ring Complex|45113|3|Fully described|p23|||Emphasis on petrography.||||||
7931|Gurrumba Ring Complex|46845|6|Mentioned|Table 1|||||||||
7931|Gurrumba Ring Complex|46976|6|Mentioned|Fig.1|||||||||
7931|Gurrumba Ring Complex|48976|4|Described|p52|||Isotopic data Table 14||||||
7931|Gurrumba Ring Complex|60425|4|Described|p51 Tb. 3, p60 Tb. 4, p77|Late Carboniferous|Late Carboniferous|Complex of olivine gabbro, quartz diorite/diorite, granite and granophyric granite - inferred to cut into Gurrumba Volcanics. Comprises 3 informal subunits . Age: ~303Ma (Rb-Sr). Intruded Hodgkinson Formation and Emuford Granite. I-type.||||||17-DEC-13
7931|Gurrumba Ring Complex|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes un-named intrusions from the Ootann and Almaden Supersuites, and an unassigned gabbro; these three are mapped separately.|||Includes Gurrumba Volcanics.|||
7931|Gurrumba Ring Complex|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes un-named intrusions from the Ootann and Almaden Supersuites, and an unassigned gabbro; these three are mapped separately.|||Includes Gurrumba Volcanics.|||
7932|Gurrumba Volcanics|23423|4|Described|p309 Table 7.3||Late Carboniferous|Also see p236-237. Faulted against Hodgkinson Formation. Age: 314 Ma, 303 Ma (Rb-Sr). Unconformably underlain by Hodgkinson Formation. Kennedy Igneous Province.||||||20-NOV-08
7932|Gurrumba Volcanics|23502|5|Briefly described|Map Legend||Late Carboniferous|Part of Gurrumba Ring Complex.||||||20-NOV-08
7932|Gurrumba Volcanics|23503|5|Briefly described|Map Legend||Late Carboniferous|Part of Gurrumba Ring Complex.||||||20-NOV-08
7932|Gurrumba Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V93. I-Type.||||||
7932|Gurrumba Volcanics|23616|5|Briefly described|Table 3 p56||Late Carboniferous|Age: Late Carboniferous? Unconformable on Hodgkinson Fm. Cut by Gurrumba Ring Complex - referred to as Gurrumba Volcanic Neck and Gurrumba Cauldron. Of Sundown Volcanic Gp. Hodgkinson Province. Max thick: ~150 m.||||||
7932|Gurrumba Volcanics|23624|5|Briefly described|p24|||Part of the Gurrumba Ring Complex.||||||20-NOV-08
7932|Gurrumba Volcanics|33963|6|Mentioned|Map legend|Permian|Permian|Probably  Permian.||||||20-NOV-08
7932|Gurrumba Volcanics|37613|6|Mentioned|p252|||See also Fig.1.||||||
7932|Gurrumba Volcanics|43259|4|Described|Appendix 1,p9.||Carboniferous|Age Late? Carboniferous.||||||
7932|Gurrumba Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
7932|Gurrumba Volcanics|45065|4|Described|Table 4|||||||||
7932|Gurrumba Volcanics|45113|4|Described|p23|||||||||
7932|Gurrumba Volcanics|46845|6|Mentioned|Table 1|||||||||
7932|Gurrumba Volcanics|60425|4|Described|p40, p50 Tb. 3, p77|Late Carboniferous|Late Carboniferous|Of Blake (1972). Central outcrop in Gurrumba Ring Complex. Unconformable on Hodgkinson Fm. Age:314Ma (Rb-Sr).Thickness: ~150m.Pale grey, autobrecciated + flow-banded, slightly porphyritic rhyolitic lava; extensivley altered; sericite + pyrite common||||||07-FEB-11
7932|Gurrumba Volcanics|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gurrumba Ring Complex.|||Pale grey, flow-banded and auto-brecciated, porphyritic, rhyolitic? lava.|
7932|Gurrumba Volcanics|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gurrumba Ring Complex.|||Pale grey, flow-banded and auto-brecciated, porphyritic, rhyolitic? lava.|
7932|Gurrumba Volcanics|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Chillagoe Subprovince, Hodgkinson Province.||||||
7932|Gurrumba Volcanics|69593|6|Mentioned|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
7945|Gympie Group|22845|6|Mentioned|p42,46,82||Permian|||||||
7945|Gympie Group|22846|6|Mentioned|Plate 1||Permian|||||||
7945|Gympie Group|23251|6|Mentioned|Table 1 p17, p18|||||||||30-NOV-05
7945|Gympie Group|23542|4|Described|Fig 1 p378|||Also see p380, 391, Fig 1 p378.  In the Gympie Province.||||||14-AUG-08
7945|Gympie Group|23608|5|Briefly described|p50 Fig 1.||Permian|||||||
7945|Gympie Group|23799|6|Mentioned|p125|Early Permian|Early Permian|Geological Province: Kin Kin Subprovince (Gympie Province).||||||
7945|Gympie Group|24382|5|Briefly described|Map legend|Permian|Permian|Constituents include: Mant Basalt, Kolbar Formation, Gigoomgan Limestone and Teebar Formation||||||
7945|Gympie Group|30508|6|Mentioned|p93|||Stratigraphy||||||
7945|Gympie Group|30655|6|Mentioned|p7|||||||||
7945|Gympie Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
7945|Gympie Group|31703|6|Mentioned|p3|||||||||
7945|Gympie Group|32943|6|Mentioned|p106|||||||||
7945|Gympie Group|34474|6|Mentioned|Fig.1|||Permian||||||
7945|Gympie Group|35101|3|Fully described|p30|||||||||
7945|Gympie Group|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
7945|Gympie Group|36045|6|Mentioned|p332|||||||||
7945|Gympie Group|36926|6|Mentioned|p162|||||||||
7945|Gympie Group|36961|6|Mentioned|Table 1|||||||||
7945|Gympie Group|37252|6|Mentioned|Map legend|Permian|Permian|||||||
7945|Gympie Group|37618|6|Mentioned|Fig.1|||||||||
7945|Gympie Group|38391|6|Mentioned|p9|||||||||
7945|Gympie Group|38805|6|Mentioned|p82|||||||||
7945|Gympie Group|39252|5|Briefly described|p16|||See also p28.||||||13-SEP-21
7945|Gympie Group|39284|4|Described|p431|||||||||
7945|Gympie Group|39445|6|Mentioned|Table 8|||See also P107 & Fig.7||||||
7945|Gympie Group|39505|6|Mentioned|p167|||||||||
7945|Gympie Group|39943|6|Mentioned|Table 12A|||||||||
7945|Gympie Group|40051|4|Described|p6|||||||||
7945|Gympie Group|40245|6|Mentioned|Table 2|||||||||
7945|Gympie Group|40475|5|Briefly described|p7|||||||||
7945|Gympie Group|40478|6|Mentioned|p22|||||||||
7945|Gympie Group|40480|6|Mentioned|p40|||||||||
7945|Gympie Group|40623|5|Briefly described|p53|||||||||
7945|Gympie Group|41157|5|Briefly described|p81|||||||||
7945|Gympie Group|41272|6|Mentioned|M 1of1 C16|||||||||
7945|Gympie Group|41736|3|Fully described|p117|||||||||
7945|Gympie Group|41738|6|Mentioned|p168|||||||||
7945|Gympie Group|41790|5|Briefly described|p469|||||||||
7945|Gympie Group|41917|6|Mentioned|p521|||||||||
7945|Gympie Group|42450|4|Described|p403|||||||||
7945|Gympie Group|42695|5|Briefly described|Fig.2|Permian||||||||
7945|Gympie Group|42751|4|Described|p24|||||||||
7945|Gympie Group|42894|6|Mentioned|p23|||||||||
7945|Gympie Group|42895|6|Mentioned|p53|||||||||
7945|Gympie Group|43006|5|Briefly described|Fig.1,p238|||||||||
7945|Gympie Group|43017|6|Mentioned|p379|||||||||
7945|Gympie Group|43077|5|Briefly described|p4|||||||||
7945|Gympie Group|43092|5|Briefly described|Fig.1|||||||||
7945|Gympie Group|43100|4|Described|p17|||||||||
7945|Gympie Group|43883|14|Not recorded|p18 Fig.4-3|||See also Lexicon||||||
7945|Gympie Group|43995|14|Not recorded|Tb.p10||Permian|||||||
7945|Gympie Group|44068|14|Not recorded|p15|||||||||
7945|Gympie Group|44239|14|Not recorded|p278|||||||||
7945|Gympie Group|44241|14|Not recorded|p4,Tb.4|Permian|Carboniferous|||||||
7945|Gympie Group|44387|14|Not recorded|p17|||||||||
7945|Gympie Group|44528|14|Not recorded|p394|||See also Lexicon.||||||
7945|Gympie Group|44616|14|Not recorded|p30|||Equivalent in part to Lower Permian.||||||
7945|Gympie Group|44752|14|Not recorded|Fig.43,p300||Permian|||||||
7945|Gympie Group|44753|14|Not recorded|p47,49-54|Permian|Carboniferous|||||||
7945|Gympie Group|44762|14|Not recorded|opp.p34||Paleozoic|Section.||||||07-NOV-08
7945|Gympie Group|44783|14|Not recorded|p47|||||||||
7945|Gympie Group|44925|5|Briefly described|Map Legend||Permian|||||||
7945|Gympie Group|44928|5|Briefly described|Map Legend||Permian|||||||
7945|Gympie Group|60077|5|Briefly described|Map legend|Permian|Permian|Andesite, agglomerate, rhyolite, shale, siltstone, conglomerate, limestone, greywacke.||||||
7945|Gympie Group|61780|5|Briefly described|p255||Early Permian|Includes; Highbury Volcanics. Overlain by Kin Kin beds. Shallow marine association.||||||
7945|Gympie Group|61809|4|Described|p445, p457, p462, p463, p463 Fig. 9|Early Permian|Early Permian|Overlian by Mount Marcella Volcanics. Geological Province: New England Orogen. Comprises interbedded basaltic/andesitic flows, tuffaceous and fragmental rocks of sedimentary/volcanic affinity, siltstone, chert and limestone.||||||
7945|Gympie Group|63821|5|Briefly described|p14 Fig. 4,  p16-17, p18|Permian|Permian|Comprises: Mant Basalt, Kolbar Fm, Gigoomgan Limestone and Teebar Fm. Max. thickness: >2000m. Geol.Prov: Gympie Province. Shallow marine deposits. Lithology of Gympie Group volcanics and undivided Gympie Group limestones also discussed in detail (p17-18).||||||07-FEB-11
7945|Gympie Group|65380|5|Briefly described|p657, 671|Permian|Permian|Gympie Terrane.|||Includes Tamaree Formation at top.|Overlain by Keefton Formation|Basal mafic to intermediate volcanics and volcaniclastics overlain by limestone and clastics (Keefton Formation).|26-MAR-12
7945|Gympie Group|65452|6|Mentioned|p5-6|Permian|Permian|||||Is overlain by, or faulted against, Agnes Water Volcanics.||
7945|Gympie Group|65668|6|Mentioned|p11|Permian|Permian|Unconformably overlain by Agnes Water Volcanics.||||||
7945|Gympie Group|68319|5|Briefly described|Map Legend|Permian|Permian|Gympie Province. Informally subdivided into two unnamed lithological units.||||Unconformably overlain by Brooweena Formation and Agnes Water Volcanics.|Fine grained siltstone, mudstone, slate, shale; conglomerate and coarse-grained sandstone.|
7945|Gympie Group|68332|5|Briefly described|Map legend.|Permian|Permian|Gympie Province. Weak- to non-magnetic response.|||||Fine-grained siltstone, mudstone, slate, shale.|
7945|Gympie Group|68421|5|Briefly described|Map Legend|Permian|Permian|Gympie Province. Includes three unnamed units, separately mapped.|||||Undivided: fine-grained siltstone, mudstone, slate and shale. Separately mapped are: basalt, andesite, dacite and minor fine-grained sediments; limestone; conglomerate and coarse-grained sandstone.|
7945|Gympie Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Gympie Province.||||||
7945|Gympie Group|68679|5|Briefly described|p312-313, p320, p331, p369-371, p430|Triassic|Permian|Runnegar and Ferguson (1969). Northern New England Orogen. Includes some rocks formerly included in the Biggenden beds (Ellis, 1968). Some rocks of this Group have been reassigned to the Amamoor beds.|||Highbury Volcanics; South Curra Limestone; Rammutt, Tamaree, Keefton, Traveston Formations; Kin Kin Phyllite.|Overlies (?thrust over) Good Night beds. Separated from Amamoor beds by a zone of tectonic melange. Is intruded by Musket Flat Granodiorite, Broomfield Granite, and Tawah Granodiorite (=Granite).||
7945|Gympie Group|69582|5|Briefly described|p48|Permian|Early Permian|Gympie Province. Deposited in a shallow to deep marine environment. Strata strikes north-northwest to northeasterly, with moderate to steep deeps.||||Overlain by the Brooweena Formation.|Basaltic to andesitic and epiclastic flows, limestones and turbiditic sequences.|
7945|Gympie Group|70913|4|Described|p14-60, p1, 2,6, 7, 8, 65, 76|Late Permian|Late Carboniferous|Gympie Province. Hosts the Gympie Goldfield. Previously included Triassic Kin Kin beds and Keefton Formation, but restriced to Permian strata in 1999. Previously referred to as Gympie Formation (Dunstan 1911), Gympie beds (Rands 1889), see p6.|||Includes from base, Highbury Basalt, Dawn Formation, Mary Formation, Rammutt Formation, South Curra Limestone and the Tamaree Formation.|||18-SEP-17
7945|Gympie Group|73197|5|Briefly described|p470, p472, p474-475, p477-478, p483|Lopingian|Late Carboniferous|New England Orogen, northern. Gympie Province. New England Orogen provenance of detrital zircons in units including and above the Rammutt Formation (Li et al., 2015). Age ranges provided in text include 300-290 Ma, 280-265 Ma, 275-255 Ma, and is coeval with Berserker Group.|ca 300-290 Ma, 280-265 Ma, 275-255 Ma||Highbury Volcanics, Rammutt Formation||Volcanics. Includes sequence of basalt and associated marine sedimentary rocks in lower part, overlying andesitic and minor dacitic volcanics include volcaniclastic granule conglomerate and sandstone.|
7945|Gympie Group|73303|6|Mentioned|p60 Fig.1, p63|Permian|Permian|New England Orogen, Gympie Terrane.||||||
7945|Gympie Group|73450|6|Mentioned|p29|Paleozoic|Paleozoic||||Intruded by Mount Walsh Granite.|||
7965|Haddon Silcrete|36217|6|Mentioned|p206|||Published by Senior 1979.||||||
7965|Haddon Silcrete|37484|6|Mentioned|p412|||||||||
7965|Haddon Silcrete|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
7965|Haddon Silcrete|66623|5|Briefly described|p269, p277.|||Equivalent to Cordillo Silcrete. This sub-surface silcrete formed by infiltration of silica-charged surface water into aquifers.||Sub-surface part of the informal Canaway profile of surface weathering with silcrete cap.||||
7985|Halliday Bay Granite|40577|3|Fully described|p51|||||||||
7985|Halliday Bay Granite|40954|6|Mentioned|p133|||||||||
7985|Halliday Bay Granite|69594|5|Briefly described|p569-570, p571 Fig.7.47|Early Cretaceous|Early Cretaceous|Ball Bay, Bowen region. Plots in A-type field on some classification diagrams. Geochemistry plots and discussion.|<125 Ma.||||Leucogranite; abundant mafic enclaves.|
7985|Halliday Bay Granite|73450|4|Described|p45-48|Albian|Aptian|[Also written as 'Halliday Bay Granite' to indicate specific usage, and Halliday Bay granite]. Formal name used by Stephenson (1985); otherwise mapped as an unnamed granite labelled Kg. Crops out in hilly terrain between Cape Hillsborough and Seaforth. Contains strongly pleochroic sodic amphibole. A-type with high REE concentrations relative to other Cretaceous granites in the region (Bultitude et al., 2013). Yielded K-Ar hornblende ages of 112 +/- 2 Ma and 117 +/- 2 Ma (Webb and McDougall, 1968; recalculated based on Steiger and Jager, 1977).|112 +/- 2 Ma, 117 +/- 2 Ma K-Ar||||Hypersolvus medium-grained peralkaline granite/alkali feldspar granite and some syenoogranite with cavities, abundant mafic enclaves up to 60 cm in diameter, and thin aplitic veins.|
8019|Hammonds Creek Granodiorite|23423|5|Briefly described|p314 Table 7.4|Early Permian|Late Carboniferous|Formerly assigned to Almaden Supersuite. Intrudes the Chillagoe Formation. Also see p240, p280. Kennedy Igneous Province.||||||
8019|Hammonds Creek Granodiorite|23503|5|Briefly described|Map Legend||Late Carboniferous|||||||
8019|Hammonds Creek Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 288. I-Type.||||||
8019|Hammonds Creek Granodiorite|23616|5|Briefly described|p99 Appendix 2||Permian|Of Almaden Supersuite.||||||
8019|Hammonds Creek Granodiorite|29820|6|Mentioned|p450|||||||||
8019|Hammonds Creek Granodiorite|33777|4|Described|p32|||||||||
8019|Hammonds Creek Granodiorite|33963|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
8019|Hammonds Creek Granodiorite|36527|6|Mentioned|p162|||||||||
8019|Hammonds Creek Granodiorite|39445|6|Mentioned|p90|||Blake(1972)||||||
8019|Hammonds Creek Granodiorite|42547|5|Briefly described|p75|||||||||
8019|Hammonds Creek Granodiorite|43060|6|Mentioned|p95|||||||||
8019|Hammonds Creek Granodiorite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
8019|Hammonds Creek Granodiorite|45065|4|Described|Table 4|||||||||
8019|Hammonds Creek Granodiorite|45113|3|Fully described|p14|||Emphasis on petrography.||||||
8019|Hammonds Creek Granodiorite|46845|6|Mentioned|Table 1|||||||||
8019|Hammonds Creek Granodiorite|46879|6|Mentioned|Fig.1|||||||||
8019|Hammonds Creek Granodiorite|48976|4|Described|p50|||||||||
8019|Hammonds Creek Granodiorite|60425|4|Described|p77, p282-3 Appdx.|Early Permian|Early Permian|Formerly mapped into Almaden Supersuite. May be composite unit? Part assigned to Claret Creek Supersuite (age ~293Ma (Rb-Sr)). Even-gr., to slightly porph'c hornblende-biotite and biotite-hornblende granodiorite; I-type - more lithology included||||||07-FEB-11
8019|Hammonds Creek Granodiorite|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|~293 Ma (Rb/Sr isochron age).||||I-type granitoids.|
8019|Hammonds Creek Granodiorite|69593|5|Briefly described|p484, p510|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|~293 Ma.|Claret Creek Supersuite.|||I-type.|
8019|Hammonds Creek Granodiorite|72297|5|Briefly described|p718|Late Carboniferous|Late Carboniferous|Formed the Gillian Prospect near Mount Garnet; the largest tin skarn deposit in QLD.||||Intrudes the Chillagoe Formation.||
8025|Hampstead Sandstone|9541|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group.  Quartzose sandstone commonly pebbly and cross-bedded, and conglomerate.  Overlain by Loth Formation.||||||07-JUL-04
8025|Hampstead Sandstone|22744|5|Briefly described|Fig1, P12, Table3||Jurassic|||||||
8025|Hampstead Sandstone|23032|5|Briefly described|p47||Middle Jurassic|Lowermost formation of Eulo Queen Group.||||||
8025|Hampstead Sandstone|23220|6|Mentioned|p16|Cretaceous|Jurassic|||||||
8025|Hampstead Sandstone|23291|4|Described|p81 Tb. 3.6|Late Jurassic|Middle Jurassic|Parent: Eulo Queen Group. Thickness: 30-60m. Geological Province: Georgetown Region.||||||08-JUL-15
8025|Hampstead Sandstone|23425|4|Described|p379.|Late Jurassic|Middle Jurassic|Of Eulo Queen Group. Geological Province: Carpentaria Basin.||||||
8025|Hampstead Sandstone|23846|5|Briefly described|p5|Jurassic|Jurassic|Of the Eulo Queen Group. Geological Province: Eromanga Basin.||||||
8025|Hampstead Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
8025|Hampstead Sandstone|24073|5|Briefly described|p378 Table 2|||Of Eulo Queen Group.  Maximum thickness: 50m.  Geological Province: Carpentaria Basin.||||||
8025|Hampstead Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
8025|Hampstead Sandstone|30587|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8025|Hampstead Sandstone|31121|6|Mentioned|p390|||||||||
8025|Hampstead Sandstone|32531|6|Mentioned|p477|||||||||
8025|Hampstead Sandstone|32553|4|Described|p38|||||||||
8025|Hampstead Sandstone|33086|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8025|Hampstead Sandstone|33176|6|Mentioned|p171|||||||||
8025|Hampstead Sandstone|33182|6|Mentioned|Table 2|||Jurassic||||||
8025|Hampstead Sandstone|33183|2|Defined|p230|Jurassic|Jurassic|||||||
8025|Hampstead Sandstone|33644|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
8025|Hampstead Sandstone|33648|4|Described|p19|||||||||
8025|Hampstead Sandstone|35082|6|Mentioned|Fig.2|||||||||
8025|Hampstead Sandstone|35560|6|Mentioned|p290|||||||||
8025|Hampstead Sandstone|35811|5|Briefly described|Table 3|||||||||
8025|Hampstead Sandstone|36216|6|Mentioned|Fig.1|||||||||
8025|Hampstead Sandstone|37576|5|Briefly described|p9|||||||||
8025|Hampstead Sandstone|37608|3|Fully described|Table 1|||||||||
8025|Hampstead Sandstone|38199|6|Mentioned|p421|||See also P428||||||
8025|Hampstead Sandstone|38714|6|Mentioned|p188|||||||||
8025|Hampstead Sandstone|38715|6|Mentioned|p192|||||||||
8025|Hampstead Sandstone|38752|5|Briefly described|p43|||||||||
8025|Hampstead Sandstone|39445|5|Briefly described|Table 10|||||||||
8025|Hampstead Sandstone|39687|6|Mentioned|Fig.5|||||||||
8025|Hampstead Sandstone|39917|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8025|Hampstead Sandstone|40218|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Late Jurassic||||||
8025|Hampstead Sandstone|41266|6|Mentioned|Fig.3|||||||||
8025|Hampstead Sandstone|42061|4|Described|p153|||See also Fig.4||||||
8025|Hampstead Sandstone|43286|5|Briefly described|Map Legend||Jurassic|of Eulo Group.||||||
8025|Hampstead Sandstone|43603|5|Briefly described|p9|||||||||
8025|Hampstead Sandstone|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
8025|Hampstead Sandstone|45145|3|Fully described|Table 5|||||||||
8025|Hampstead Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
8025|Hampstead Sandstone|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
8025|Hampstead Sandstone|49011|6|Mentioned|Fig.3|||Carpentaria Basin||||||
8025|Hampstead Sandstone|50199|5|Briefly described|Map Legend|Jurassic|Jurassic|Of the Eulo Queen Group.||||||
8025|Hampstead Sandstone|50200|5|Briefly described|Map Legend|Jurassic|Jurassic|Of the Eulo Queen Group.||||||
8025|Hampstead Sandstone|50201|5|Briefly described|Map Legend|Jurassic|Jurassic|Of the Eulo Queen Group.||||||
8025|Hampstead Sandstone|50210|5|Briefly described|Map Legend|Jurassic|Jurassic|Underlies: Loth Formation.  Of the Eulo Queen Group.||||||
8025|Hampstead Sandstone|50211|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Eulo Queen Group. Overlain by Loth Formation. Clayey, commonly pebbly, quartzose sandstone and conglomerate.||||||17-MAY-04
8025|Hampstead Sandstone|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Of the Eulo Queen Group. Underlies: Loth Formation.||||||01-JUL-04
8025|Hampstead Sandstone|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group.  Coarse to very coarse white clayey quartz sandstone, commonly pebbly.  Underlies Loth Formation.||||||06-JUL-04
8025|Hampstead Sandstone|60081|5|Briefly described|Map legend|Late Jurassic|Jurassic|Of the Eulo Queen Group.  Quartzose sandstone , commonly pebbly, some conglomerate.||||||
8025|Hampstead Sandstone|64707|5|Briefly described|Map legend|Jurassic|Jurassic|Of Eulo Queen Group. Clayey, commonly pebbly, quartzose sandstone and conglomerate.||||||
8025|Hampstead Sandstone|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||Unit in Eulo Q Group.||||
8025|Hampstead Sandstone|67402|5|Briefly described|p177 tbl CRP/KRM1|Kimmeridgian|Oxfordian|Carpentaria/Karumba Basins. Deposited in low-sinuosity fluvial systems. ||Eulo Queen Group|||Quartz, planar and trough cross bedded sandstone with reverse graded conglomerates at the base.|
8025|Hampstead Sandstone|68135|5|Briefly described|p52 fig 2b|Tithonian||Carpentaria Basin.||||Overlain by Helby beds, Garraway beds and Lees Sandstone|Cross-bedded sandstone.|14-SEP-17
8025|Hampstead Sandstone|68349|5|Briefly described|Map legend.|Late Jurassic|Middle Jurassic|Carpentaria Basin.||Unit in Eulo Queen Group.||Is overlain conformably by Loth Formation.|Clayey, commonly pebbly, quartzose sandstone and conglomerate.|
8025|Hampstead Sandstone|68417|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Of the Carpentaria Basin.||Of the Eulo Queen Group.||Conformably overlain by the Loth Formation.|Clayey, commonly pebbly, quartzose sandstone and conglomerate.|
8025|Hampstead Sandstone|69594|4|Described|p521-522, p527|Middle Jurassic|Middle Jurassic|Southern Staaten Sub-basin, Carpentaria Basin. 30-60m thick. Low-sinuosity fluvial deposits. One of the main aquifers in the Basin. Not differentiated from the Loth Formation in the Eromanga Basin.||Eulo Queen Group.||Is overlain by Loth Formation.|Quartzose sandstone and conglomerate.|
8025|Hampstead Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Carpentaria Basin.||Eulo Queen Group.||Is overlain by Loth FZ and Garraway beds.||
8025|Hampstead Sandstone|73147|5|Briefly described|p128-131, 138-144|Middle Jurassic|Middle Jurassic|Smart et al. (1971). Gregory Range area. 30 - 45m thick. High-energy fluvial deposits. An MDA for the top of the Formation is 162.5 +/- 1.7 Ma. Age spectra summary diagrams. Based on this, sediment provenance from the Lachlan Orogen (>1,000 km to the S) is proposed.|168.5 +/- 7.2 Ma (MDA: U-Pb detrital zircon).|Eulo Queen Group (lower part).||Is overlain conformably by Loth Formation.|Fining-upward, cross-stratified quartzose sandstone unit; typically medium to thickly bedded and medium- to very coarse-grained.|
8033|Hampton Road Rhyolite|23799|3|Fully described|p32, p14 Tb. 1|Early Permian|Early Permian|Of Cressbrook Creek Group.  Overlain by Biarraville Formation; underlain by Pinecliff Formation.  Max. thickness: 1500m.  Age : based on similarities with Rammut Formation. Geological Province: Cressbrook Creek Subprovince.||||||
8033|Hampton Road Rhyolite|23800|5|Briefly described|Map legend|Permian|Permian|Of the Cressbrook Creek Group.||||||
8033|Hampton Road Rhyolite|24560|5|Briefly described|Map legend|Permian|Permian|Of Cressbrook Creek Group.  Acid volcanics (silicic alteration).||||||
8033|Hampton Road Rhyolite|32912|6|Mentioned|p157|||Lower Permian.||||||
8033|Hampton Road Rhyolite|33381|4|Described|p108|||Permian. See also P111. Cressbrook Creek Group.||||||
8033|Hampton Road Rhyolite|39252|6|Mentioned|Fig.13|||||||||
8033|Hampton Road Rhyolite|39445|5|Briefly described|Table 8|||||||||
8033|Hampton Road Rhyolite|42525|5|Briefly described|Map legend|Early Permian?|Early Permian?|Of the Cressbrook Creek Group.||||||15-JUL-04
8033|Hampton Road Rhyolite|44555|2|Defined|p224|Permian|Permian|See also Lexicon.||||||09-APR-08
8033|Hampton Road Rhyolite|44786|14|Not recorded|p193-202||Permian|Middle-?Early Permian.||||||
8033|Hampton Road Rhyolite|68679|5|Briefly described|p386|Guadalupian|Guadalupian|Cranfield et al. (2001). Cressbrook Basin. Partly subaerial. 1500m thick; thins to <30m in the north.||Cressbrook Creek Group.||Unconformably overlies Pinecliff Formation. Is faulted against the Toogoolawah Group.|Thick, glassy, spherulitic, fluidal (flow-banded) rhyolite lava flows and pyroclastic deposits with minor interbedded sandstone, conglomerate and chert with minor andesite.|
8085|Hardway Granite|24197|5|Briefly described|p21, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Age: 1860Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
8085|Hardway Granite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
8085|Hardway Granite|30531|6|Mentioned|p20|||Also mention P22||||||
8085|Hardway Granite|33900|5|Briefly described|p23|||Mention P15||||||
8085|Hardway Granite|35074|6|Mentioned|Fig.2|||||||||
8085|Hardway Granite|35167|2|Defined|p153|Middle Precambrian|Middle Precambrian|||||||
8085|Hardway Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
8085|Hardway Granite|36052|6|Mentioned|Fig.1|||||||||
8085|Hardway Granite|38235|6|Mentioned|p115|||||||||
8085|Hardway Granite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
8085|Hardway Granite|40840|6|Mentioned|Map legend|||||||||
8085|Hardway Granite|45136|3|Fully described|p59|||Also mention P29.||||||
8085|Hardway Granite|45166|5|Briefly described|p19|||||||||
8085|Hardway Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
8085|Hardway Granite|49041|5|Briefly described|Table 2|||||||||
8085|Hardway Granite|50536|5|Briefly described|p1.4 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
8085|Hardway Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event.||Kalkadoon Supersuite|||Coarse to medium-grained biotite granite, leucogranite, aplite, minor granodiorite.|
8085|Hardway Granite|69591|5|Briefly described|p60|||Kalkadoon Batholith.|||||Medium- to coarse-grained, biotite granite, leucogranite, aplite, minor granodiorite.|
8085|Hardway Granite|72596|5|Briefly described|p1-p3, p56-61|Orosirian|Orosirian|Mary Kathleen Domain. Geochronologic constraint is a magmatic crystallisation age . Forms 3 main bodies with a total area of ca. 19 km2. Outcrops of Hardway Granite had been included in the ca. 1860 Ma Kalkadoon Granodiorite by Carter et al. (1961; their Kalkadoon Granite), but were subsequently delineated as a discrete unit by Derrick et al. (1977) who vaguely alluded to an age of 1681+/- 68 Ma and the unit was described as intruding the Corella Formation. The new geochronology does not support this interpretation, but is consistent with that of Budd et al. (2001) who included the unit in the Kalkadoon-Leichhardt Suite.|1862 +/- 3 Ma SHRIMP U-Pb||||Includes monzogranite.|
8085|Hardway Granite|73413|6|Mentioned|App.1|Orosirian|Orosirian|U-Pb age of 1862 +/- 3 Ma reported by Kositcin et al. (2019).|1862 +/- 3 Ma|||||
8085|Hardway Granite|73553|5|Briefly described|p1, p6, p8 Fig.1.2.3, p10-13, p28|Orosirian|Orosirian|Included in Kalkadoon-Leichhardt Igneous Province based on geochronology. Crops out in three main bodies as a basement inlier in the Mary Kathleen Domain. Mapped by Carter et al., (1961) as Kalkadoon Granite (now Kalkadoon Granodiorite) and delineated by Derrick et al., (1977a) as Hardway Granite; these authors refer to an age of 1681+/-68 Ma and an Rb-Sr age of 1645+/-67 Ma, described unit as intruding the Corella Formation [at odds with more recent isotopic dating]. Included in Kalkadoon Supersuite (1860 Ma) by Budd et al., (2001) on the basis of geochemistry. Appears as distinct magnetic lows in airborne TMI images, parts are slightly magnetic. Yellowish to slightly greenish tones in radiometric images. Intruded by a mafic intrusive phase or phases which have irregular but sharp contacts with the granite.|1862+/-3 Ma zircon U-Pb SHRIMP||||Heterogeneous in composition and fabric; dominated by mildly deformed, medium- to coarse-grained, equigranular biotite-amphibolite monzogranite to syenogranite. Locally contains leucogranite, aplite, pegmatite.|03-FEB-23
8130|Haslingden Group|22457|5|Briefly described|p31, Fig30 p31|||Shown as Upper and Lower Haslingden Group in Fig29 p30.||||||04-APR-18
8130|Haslingden Group|22483|6|Mentioned|Table 2 p416.|||||||||
8130|Haslingden Group|22644|5|Briefly described|3,4,12|||Geol. province: McArthur Basin. Max thickness 17,000 m.||||||18-JAN-07
8130|Haslingden Group|22665|6|Mentioned|P220||Statherian|||||||
8130|Haslingden Group|23031|6|Mentioned|18|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|23073|6|Mentioned|p744|||||||||
8130|Haslingden Group|23393|5|Briefly described|p18, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
8130|Haslingden Group|23395|4|Described|p384 Fig.2|||||||||
8130|Haslingden Group|23396|5|Briefly described|p407 Fig.2|||||||||
8130|Haslingden Group|23408|6|Mentioned|p512|||Mentioned only in the context of "......geological evolution of post-Haslingden group sedimentary rocks on the Lawn Hill Platform" (Hutton and Sweet 1982)..||||||15-JUN-09
8130|Haslingden Group|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
8130|Haslingden Group|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier.||||||
8130|Haslingden Group|24034|5|Briefly described|p9|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Feldspar sandstones, tuff, siltstone, quartzite and meta-basalt.||||||
8130|Haslingden Group|24419|5|Briefly described|p16, p14, p15 Fig. 6|Paleoproterozoic|Paleoproterozoic|Includes Myally Subgroup, Eastern Creek Volcanics, Jayah Creek and Oroopa Metabasalts, Mount Guide and Leander Quartzites and May Downs Gneiss Member.  See also misspelt Hasllngden Group (p13 Fig.5). Geol.Prov: Leichardt Superbasin. See also p13 Fig. 5.||||||07-NOV-08
8130|Haslingden Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Myally Subgroup, Eastern Creek Volcanics and Mount Guide Quartzite.||||||25-AUG-04
8130|Haslingden Group|30530|6|Mentioned|p516|||||||||
8130|Haslingden Group|30531|6|Mentioned|p15|||||||||
8130|Haslingden Group|30534|2|Defined|p305|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|30535|6|Mentioned|p403|||||||||
8130|Haslingden Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|32660|4|Described|Table 5|||||||||
8130|Haslingden Group|33111|6|Mentioned|p5|||||||||
8130|Haslingden Group|33900|4|Described|p10|||Mention p4.||||||25-SEP-06
8130|Haslingden Group|35074|6|Mentioned|Fig.2|||||||||
8130|Haslingden Group|35286|6|Mentioned|p145|||||||||
8130|Haslingden Group|35295|6|Mentioned|p601|||Also mentioned p603.||||||15-MAR-18
8130|Haslingden Group|35369|6|Mentioned|PB5|||||||||
8130|Haslingden Group|35495|6|Mentioned|p341|||||||||
8130|Haslingden Group|35950|6|Mentioned|p305|||||||||
8130|Haslingden Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|36733|6|Mentioned|p21|||||||||
8130|Haslingden Group|37217|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|37459|6|Mentioned|p423|||||||||
8130|Haslingden Group|37462|4|Described|Table4.VII|||||||||
8130|Haslingden Group|37565|5|Briefly described|p2|||See also Fig.5||||||
8130|Haslingden Group|37568|4|Described|p81|||See also p85.||||||25-SEP-06
8130|Haslingden Group|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8130|Haslingden Group|37862|6|Mentioned|p581|||||||||
8130|Haslingden Group|38232|6|Mentioned|p81|||||||||
8130|Haslingden Group|38233|6|Mentioned|p93|||||||||
8130|Haslingden Group|38235|6|Mentioned|p113|||||||||
8130|Haslingden Group|38237|6|Mentioned|p125|||||||||
8130|Haslingden Group|38276|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|38278|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|38350|4|Described|p9|||||||||
8130|Haslingden Group|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Eastern Creek Volcanics and Mount Guide Quartzite.||||||25-AUG-04
8130|Haslingden Group|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|38560|6|Mentioned|p114|||||||||
8130|Haslingden Group|38598|6|Mentioned|p197|||||||||
8130|Haslingden Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|38833|6|Mentioned|p161|||||||||
8130|Haslingden Group|38835|6|Mentioned|p163|||||||||
8130|Haslingden Group|38836|6|Mentioned|p165|||||||||
8130|Haslingden Group|38900|6|Mentioned|p55|||||||||
8130|Haslingden Group|38919|6|Mentioned|p493|||||||||
8130|Haslingden Group|39202|6|Mentioned|Fig.2|||||||||
8130|Haslingden Group|39362|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|39445|5|Briefly described|p40|||See also p39 and Table 2.||||||25-SEP-06
8130|Haslingden Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
8130|Haslingden Group|39622|6|Mentioned|p19|||See also Fig.2||||||
8130|Haslingden Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
8130|Haslingden Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|40105|6|Mentioned|p310|||||||||
8130|Haslingden Group|40202|6|Mentioned|p719|||||||||
8130|Haslingden Group|40221|3|Fully described|p6|||||||||
8130|Haslingden Group|40598|6|Mentioned|p31|||||||||
8130|Haslingden Group|40840|6|Mentioned|Map legend|||||||||
8130|Haslingden Group|41248|5|Briefly described|p69|||||||||
8130|Haslingden Group|41277|6|Mentioned|p83|||||||||
8130|Haslingden Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
8130|Haslingden Group|41307|4|Described|p8|||||||||
8130|Haslingden Group|41381|6|Mentioned|p323|||||||||
8130|Haslingden Group|41465|6|Mentioned|p11|||||||||
8130|Haslingden Group|41744|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|41791|6|Mentioned|p266|||||||||
8130|Haslingden Group|41978|6|Mentioned|p490|||||||||
8130|Haslingden Group|41979|6|Mentioned|p523|||||||||
8130|Haslingden Group|42234|5|Briefly described|p1055|||||||||
8130|Haslingden Group|42342|6|Mentioned|p23|||||||||
8130|Haslingden Group|42367|5|Briefly described|p17, p18||Proterozoic|||||||
8130|Haslingden Group|42503|5|Briefly described|p336|||||||||
8130|Haslingden Group|42523|5|Briefly described|p372|||||||||
8130|Haslingden Group|42565|4|Described|Table 1 P5, P2|||||||||
8130|Haslingden Group|42676|5|Briefly described|Fig.2 p41|||||||||04-APR-18
8130|Haslingden Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes May Downs Gneiss, Mount Guide Quartzite, Eastern Creek Volcanics and the Myally Subgroup.||||||09-FEB-09
8130|Haslingden Group|42782|6|Mentioned|p457|||||||||
8130|Haslingden Group|42812|6|Mentioned|p65|||||||||
8130|Haslingden Group|42818|4|Described|p206, Fig.2 p205|||||||||
8130|Haslingden Group|43561|6|Mentioned|p1438|||||||||
8130|Haslingden Group|43595|5|Briefly described|p439|||||||||
8130|Haslingden Group|43760|5|Briefly described|p431|||||||||
8130|Haslingden Group|43788|6|Mentioned|p20|||||||||
8130|Haslingden Group|44195|6|Mentioned|p356 Fig.9|||||||||
8130|Haslingden Group|45136|4|Described|Table 1|||Also mention p2.||||||25-SEP-06
8130|Haslingden Group|45161|4|Described|p22|||See also p11.||||||25-SEP-06
8130|Haslingden Group|45162|6|Mentioned|p11|||||||||
8130|Haslingden Group|45166|4|Described|p14|||||||||
8130|Haslingden Group|46801|6|Mentioned|p115|||See also Table 1 and Fig.14.||||||
8130|Haslingden Group|46859|6|Mentioned|p313|||||||||
8130|Haslingden Group|46919|6|Mentioned|p213|||||||||
8130|Haslingden Group|46960|6|Mentioned|p218|||||||||
8130|Haslingden Group|46962|4|Described|Table 1|||See also Fig.3.||||||
8130|Haslingden Group|46995|5|Briefly described|p267|||||||||
8130|Haslingden Group|46996|6|Mentioned|p273|||||||||
8130|Haslingden Group|47083|4|Described|p5-10||Proterozoic|Includes Myally Subgroup. Overain by Quilalar Formation.||||||25-SEP-06
8130|Haslingden Group|49041|5|Briefly described|Table 1|||||||||
8130|Haslingden Group|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Contains the Myally Subgroup.  Unconformably overlies the Bottletree Formation. Geological Province: Western Fold Belt Province.||||||11-FEB-09
8130|Haslingden Group|50332|6|Mentioned|p16|Paleoproterozoic|Paleoproterozoic|Age: 1800-1755Ma.||||||07-FEB-11
8130|Haslingden Group|50624|4|Described|p234 Fig.2||Paleoproterozoic|Overlain by Mount Isa Group.||||||07-NOV-08
8130|Haslingden Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Eastern Creek Volcanics, Mount Guide Quartzite, Judenan Beds.||||||
8130|Haslingden Group|61204|5|Briefly described|p537-538|Statherian|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1710 +/- 25 Ma. Includes Mount Guide Quartzite and Eastern Creek Volcanics.||||||07-NOV-08
8130|Haslingden Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
8130|Haslingden Group|61735|5|Briefly described|p658|||Includes the Argylla Formation. Geological province: Mount Isa Inlier.||||||30-JUN-09
8130|Haslingden Group|61736|5|Briefly described|p673, p674|Paleoproterozoic|Paleoproterozoic|Age: </-1790Ma. Sediments.||||||
8130|Haslingden Group|61923|5|Briefly described|p28 Fig.1|||Includes the Eastern Creek Volcanics. Intruded by Sybella Granite. Geological Province: Mount Isa Inlier.||||||
8130|Haslingden Group|62535|5|Briefly described|p673-674||||c.1790 Ma.|||||
8130|Haslingden Group|62536|6|Mentioned|p658|||Mount Isa Inlier.|||Argylla Formation.|||
8130|Haslingden Group|62873|5|Briefly described|p692|Paleoproterozoic|Paleoproterozoic|Mafic igneous rocks. Comprises Mount Guide Quartzite and Eastern Creek Volcanics. Intruded by the Sybella Batholith. Geological Province: Mount Isa Inlier.||||||07-NOV-08
8130|Haslingden Group|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|||Comprises Eastern Creek Volcanics, Mount Guide Quartzite and the Myally Subgroup. Geological Province: Leichhardt Superbasin.||||||30-APR-13
8130|Haslingden Group|63113|5|Briefly described|p1214 Fig.2.|||Leichhardt Superbasin.|||Includes the Bottle Tree Formation, Mount Guide Quartzite, Eastern Creek Volcanics, Alsace Quartzite and Bortala Formation.|||
8130|Haslingden Group|64250|5|Briefly described|p11 fig 3, p19, p22, p23|||Age 1773 +/- 2 Ma from Myally Subgroup in upper part of Group.|c.1790 - c.1770 Ma.||Mount Guide Quartzite, Eastern Creek Volcanics, Myally Subgroup|||15-MAR-18
8130|Haslingden Group|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Comprises Mount Guide Quartzite, Eastern Creek Volcanics and Quilalar Formation at the top. Age range: ca.1785Ma to 1763+/-8Ma.||||||07-FEB-11
8130|Haslingden Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
8130|Haslingden Group|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Comprises Eastern Creek Volcanics, Mount Guide Quartzite and Myally Subgroup. Age ranges from ca.1785Ma to ca.1775Ma. Geological Province: Mt Isa Inlier.||||||07-FEB-11
8130|Haslingden Group|65337|5|Briefly described|p5, p11. |||Leichhardt Superbasin; Leichhardt River Fault Trough.|||Includes Myally Subgroup.|Overlies Bottletree Formation.||
8130|Haslingden Group|65387|6|Mentioned|p60|||Deposition of this unit is suggested to represent the unconformity between Argylla suite and Ballara Quartzite to the east.||||||
8130|Haslingden Group|65396|5|Briefly described|p82, p173, p175, p187, p193, p196, p241|||Cover Sequence 2, Western Fold Belt, Mount Isa Inlier.|c.1790-1770 Ma.||Includes Eastern Creek Volcanics, Mount Guide Quartzite, Myally Subgroup|Overlain by Quilalar Formation.||03-APR-17
8130|Haslingden Group|66824|6|Mentioned|p133|Paleoproterozoic|Paleoproterozoic|||||Is intruded by Sybella Granite.|Metavolcanic and metasedimentary units.|
8130|Haslingden Group|67026|6|Mentioned|p336 Fig. 2 & 3.|Proterozoic|Proterozoic||||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup.|||
8130|Haslingden Group|67323|5|Briefly described|Solid Geology Map, p11, p39, p107|||See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Oxide Domain, Mount Isa Inlier. Small positive magnetic anomalies may indicate lower Haslingden Group beneath cover. See also references to Lower Haslingden Group (GIS attrib tbl, sol geol.; p107).|||Myally Subgroup, Eastern Creek Volcanics, Jayah Creek Metabasalt, Leander Quartzite, Mount Guide Quartzite.||Quartz, sandstone, feldspathic sandstone, metabasalt.|
8130|Haslingden Group|67499|6|Mentioned|p937, p938|||Western Fold Belt|||Eastern Creek Volcanics, Myally Subgroup, Mount Guide Quartzite.|||
8130|Haslingden Group|68542|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic||||Includes Eastern Creek Volcanics|||
8130|Haslingden Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||Conformably overlies Bottletree Formation.||
8130|Haslingden Group|68576|5|Briefly described|Q_2: p10, p13|Proterozoic|Proterozoic|Leichhardt River Fault Trough. Deposited over 25 to 30 m.y.|||Eastern Creek Volcanics.|||
8130|Haslingden Group|68732|6|Mentioned|p159, p160, p164||||||Mount Guide, Alsace, Whitworth Quartzites; Bortala, Bottletree, Lochness Formations.|||30-NOV-17
8130|Haslingden Group|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.|||Includes Mount Guide Quartzite and Myally Subgroup.|||25-JAN-19
8130|Haslingden Group|69430|6|Mentioned|p15:9|||Isa Superbasin.||||May be contiguous with Tawallah Group (McArthur Basin).||12-JUL-16
8130|Haslingden Group|69542|5|Briefly described|p132, p134-135, p142|Mesoproterozoic|Paleoproterozoic|Blake and Stewart (1988). Western Fold Belt.|||Includes Eastern Creek Volcanics.||Sandstone and tholeiitic basalt interbedded with pelitic, psammopelitic and psammitic rocks.|09-FEB-18
8130|Haslingden Group|69591|5|Briefly described|p29, p41, p57|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Part of Myally and Guide Supersequences.|||Myally Subgroup; Eastern Creek Volcanics, Jayah Creek Metabasalt, Leander Quartzite, Mount Guide Quartzite.|||
8130|Haslingden Group|70283|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Leichhardt River fault trough, Western fold belt, Mount Isa Inlier. Is intruded by the 1660-1655 Ma Sybella batholith.|||Includes Eastern Creek Volcanics|Overlies Bottletree Formation; overlain by Mount Isa Group.|Sandstones, amphibolite, metasediments and chlorite schist.|14-FEB-18
8130|Haslingden Group|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Myally Subgroup, Eastern Creek Volcanics.|||
8130|Haslingden Group|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Myally Subgroup, Eastern Creek Volcanics.|||
8130|Haslingden Group|70864|6|Mentioned|p74 Fig 2|||Shown as Lower Haslingden Group.|||?Includes Myall Subgroup?|||
8130|Haslingden Group|70897|6|Mentioned|p41|||Mount Isa Inlier. Matches the age of some 1780-1770 Ma zircons extracted from Mullera Formation.||||||
8130|Haslingden Group|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier. Age from Blake and Stewart, 1992.|1790-1760 Ma|||Overlain by Myally Subgroup. Underlain by Leichardt Volcanics and Kalkadoon Granite. Equivalent to Eastern Creek Volcanics.||
8130|Haslingden Group|71960|5|Briefly described|p77, 86, 87|Proterozoic|Proterozoic|Provenence of basal part shown to be from east.|||Includes Leander Quartzite, Eastern Creek Volcanics, Myally Subgroup.|Unconformably overlain/truncated by Mount Isa Group.||
8130|Haslingden Group|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic||||Includes Leander Quartzite, Eastern Creek Volcanics, Myally Subgroup.|Unconformably underlies Mount Isa Group.|Quartzite, metabasalt, sandstone, basalt, arkose, sandstone, siltstone.|03-APR-19
8130|Haslingden Group|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.|||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup|Shown as older than Quilalar Formation.|Includes variably feldspathic and lithic sandstone, siltstone and minor conglomerate and metavolcanic rocks. Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist epidotic quartzite, sericitic, feldspathic and quartzose rocks.|
8130|Haslingden Group|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.|||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup|Shown as older than Quilalar Formation.|Includes variably feldspathic and lithic sandstone, siltstone and minor conglomerate and metavolcanic rocks. Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist epidotic quartzite, sericitic, feldspathic and quartzose rocks.|
8130|Haslingden Group|72889|6|Mentioned|p6 Fig.i.|||||||||
8130|Haslingden Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
8130|Haslingden Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt.||||||
8130|Haslingden Group|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13, p20|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Mafic extrusives.|
8130|Haslingden Group|73553|6|Mentioned|p177 Tb.5.9.1|||Contains mafic intrusive rocks.||||||
8195|Hay River Formation|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone and chert overlying black pyritic shale, shelly dolomite at base.||||||
8195|Hay River Formation|12951|6|Mentioned|p143|||Probably obsolete name for rocks now included in part in the Thorntonia Limestone (lower part) and Arthur Creek Formation (upper part), Georgina Basin.||||||
8195|Hay River Formation|35798|2|Defined|p312|Middle Cambrian|Middle Cambrian|||||||
8195|Hay River Formation|39921|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8195|Hay River Formation|40810|6|Mentioned|p5|||||||||
8195|Hay River Formation|40856|5|Briefly described|p316|||||||||
8195|Hay River Formation|41388|6|Mentioned|p557|||||||||
8195|Hay River Formation|41524|6|Mentioned|p17|||||||||
8195|Hay River Formation|41532|6|Mentioned|p301|||||||||
8195|Hay River Formation|41594|6|Mentioned|p49|||||||||
8195|Hay River Formation|42956|5|Briefly described|p31 Fig.4|||||||||
8195|Hay River Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
8195|Hay River Formation|45155|6|Mentioned|Fig.8|||||||||
8195|Hay River Formation|47035|6|Mentioned|p85|||||||||
8195|Hay River Formation|49027|4|Described|p7|||||||||
8195|Hay River Formation|60122|5|Briefly described|p15|Middle Cambrian|Middle Cambrian|Name abandoned. Formerly divided into 3 discrete packages - the "Lower H. R. Formation", the "Upper H. R. Formation Member 1" and the "Upper H. R. Formation Member 2". Now assigned to Thorntonia Limestone and Arthur Creek Formation.||||||17-MAY-05
8195|Hay River Formation|63450|4|Described|p78 Fig. 5, p80|Middle Cambrian|Middle Cambrian|Subdivided into lower, middle and upper Hay River Formation. Unconformably overlies Red Heart Dolomite; conformably overlain by Marqua Formation. Max. thickness: 100m. Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
8195|Hay River Formation|64068|5|Briefly described|p57, 59, p18, p44, p151-152, 225|||Lower Hay River Formation and Upper Hay River Formation, Member 1, of Shergold in Walter et al (1979), replaced by Thorntonia Limestone.  Upper Hay River Formation, Member 2 replaced  by Arthur Creek Formation. Ground SIROTEM surveys identified conductors in the basal part of this unit, but subsequent drilling did not support the interpretation.||||||
8195|Hay River Formation|65489|6|Mentioned|p124|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
8195|Hay River Formation|67402|6|Mentioned|p213 fig GRG3|Templetonian|Ordian|Georgina Basin. ||||Unconformably overlies the Red Heart Dolomite. Unconformably overlain by the Arrinthrunga Formation, Georgina Limestone or the Marqua beds.||
8195|Hay River Formation|69206|6|Mentioned|p1-2|||Georgina Basin. A hydrocarbon source and reservoir.||||||
8195|Hay River Formation|69673|6|Mentioned|p122|||Previously abandoned name, reinstated the name to refer to the calcareous deposits at the base of the Narpa group.||||||
8195|Hay River Formation|70723|6|Mentioned|p22, p29, p31|||Name superseded by Thorntonia Limestone.||||||
8195|Hay River Formation|70752|6|Mentioned|p129, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Ordian. Brachiopod systematic palaeontological descriptions.||||||
8195|Hay River Formation|72321|4|Described|Fig 2, p4, 6, 7|Stage 4|Stage 4|Of Walter et al., 1979. Name reinstated here. Elkedra Shelf/Dulcie Syncline, Toko Syncline, Burke River Structural Belt, Georgina Basin.  Previously included in Thorntonia Limestone, but separated here, across southern portion of the basin, due to older age. Age Cambrian Series 2, Stage 4, Australian Stage: Ordian.||of Narpa Group.||Unconformably overlain by Arthur Creek Formation. Correlated with Top Springs Limestone, Gum Ridge Formation.||
8195|Hay River Formation|73418|5|Briefly described|p4 Fig.3|Cambrian Series 2|Cambrian Series 2|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Underlies Thorntonia Limestone|Limestone.|
8240|Hector Tuff|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Kholo Subgroup||||
8240|Hector Tuff|29386|6|Mentioned|p454|||Upper Triassic.||||||
8240|Hector Tuff|30302|6|Mentioned|p415|||Refers to Allen(1959)||||||
8240|Hector Tuff|30465|5|Briefly described|p3|||||||||
8240|Hector Tuff|32180|5|Briefly described|p6|||||||||
8240|Hector Tuff|33381|4|Described|p109|||See also PP113,117. Triassic. Kholo Sub Gp.||||||
8240|Hector Tuff|36354|6|Mentioned|p368|||||||||
8240|Hector Tuff|36779|6|Mentioned|p7|||See also Plate 2.||||||
8240|Hector Tuff|37111|5|Briefly described|p292|||||||||
8240|Hector Tuff|38074|5|Briefly described|Table 1|||||||||
8240|Hector Tuff|38076|6|Mentioned|Table 3|||||||||
8240|Hector Tuff|38307|4|Described|p519|||||||||
8240|Hector Tuff|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
8240|Hector Tuff|39445|5|Briefly described|Table 9|||||||||
8240|Hector Tuff|39943|6|Mentioned|Table 12A|||||||||
8240|Hector Tuff|40623|5|Briefly described|p30|||Also Mention Table 2||||||
8240|Hector Tuff|41906|3|Fully described|Table 2 P18|||||||||
8240|Hector Tuff|42336|5|Briefly described|Table 1 P5|||||||||
8240|Hector Tuff|43922|14|Not recorded|p324,325|||Formation of Kholo Subgroup of Ipswich Coal Measures.||||||
8240|Hector Tuff|44026|14|Not recorded|p123|||Equivalent of Esk Beds in Ipswich District.||||||
8240|Hector Tuff|44510|2|Defined|p252-254,Fig.35|||||||||
8240|Hector Tuff|44542|14|Not recorded|p32,34||Middle Triassic|Conformable between Colleges Conglomerate below and Cribb Conglomerate above.||||||
8240|Hector Tuff|44734|14|Not recorded|p5,7,9,16-18|||Pine Mountain area.||||||
8240|Hector Tuff|44775|4|Described|p7,8,map 2||Middle Triassic|||||||
8240|Hector Tuff|44783|14|Not recorded|p16,18|||||||||
8240|Hector Tuff|67402|5|Briefly described|p222, p223, p225|Carnian|Ladinian|Ipswich Basin. Deposited in a fluvial to lacustrine environment. ||Kholo Subgroup||Overlies the Colleges Conglomerate. Overlain by the Cribb Conglomerate.|Tuff beds with fine to very fine grained sandstones, carbonaceous mudstone that is thinly interbedded with claystone and coal.|
8240|Hector Tuff|68679|5|Briefly described|p393-395, p434-435|Late Triassic|Late Triassic|Ipswich Basin. Up to ~60m thick; 22m in the type section in drill hole IC 93; thins to the E. Detritus is dominantly explosive volcanic; mostly lacustrine deposits.||Kholo Subgroup.||Conformably overlies Colleges Conglomerate. Is overlain by Cribb Conglomerate.|Thin air-fall deposits, non-welded ignimbrite, reworked tuff in mudstone, sandstone and conglomerate, and minor shale and coal.|
8240|Hector Tuff|73450|6|Mentioned|p38||||||||Includes felsic volcanics.|
8248|Heifer Creek Sandstone Member|13516|5|Briefly described|p159 fig 8|Middle Jurassic|Middle Jurassic|From Clarence-Moreton Basin.||of Koukandowie Formation||||
8248|Heifer Creek Sandstone Member|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Coarse quartz arenite, granule conglomerate. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
8248|Heifer Creek Sandstone Member|23799|5|Briefly described|p47|Middle Jurassic|Middle Jurassic|See also Heifer Creek Sandstone. Of the Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.  See also p34 Fig. 3.||||||
8248|Heifer Creek Sandstone Member|23812|5|Briefly described|p34 Tb.4|Middle Jurassic|Early Jurassic|Of Koukandowie Formation.  Geological Province:Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|30058|6|Mentioned|p4|||Refers to McTaggart(1963)||||||
8248|Heifer Creek Sandstone Member|31118|6|Mentioned|p320|||||||||
8248|Heifer Creek Sandstone Member|33381|4|Described|p117|||See also P118. L.-M. Jur. Marburg Fm.||||||
8248|Heifer Creek Sandstone Member|33476|6|Mentioned|Table 6 P100|||Refers Swindon 1971||||||
8248|Heifer Creek Sandstone Member|37375|6|Mentioned|p472|||||||||
8248|Heifer Creek Sandstone Member|37436|6|Mentioned|p540|||||||||
8248|Heifer Creek Sandstone Member|37463|6|Mentioned|p483|||||||||
8248|Heifer Creek Sandstone Member|38205|6|Mentioned|p84|||Member of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|38441|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8248|Heifer Creek Sandstone Member|39907|5|Briefly described|p9|||||||||
8248|Heifer Creek Sandstone Member|40623|5|Briefly described|p107|||||||||
8248|Heifer Creek Sandstone Member|41631|4|Described|p19|||See also Fig.2||||||
8248|Heifer Creek Sandstone Member|41906|3|Fully described|Table 2 P15|||See also P32||||||
8248|Heifer Creek Sandstone Member|42248|1|Redefined|App.1 P411|Early Jurassic||||||||
8248|Heifer Creek Sandstone Member|42463|6|Mentioned|Fig.3 P170|||||||||
8248|Heifer Creek Sandstone Member|42869|5|Briefly described|Table 1, P33|||of Koukandowie formation||||||
8248|Heifer Creek Sandstone Member|42951|5|Briefly described|Fig.11|||of Koukandowie Formation||||||
8248|Heifer Creek Sandstone Member|43993|2|Defined|p93,97,100||Triassic|Unit of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|44026|14|Not recorded|p123||Jurassic|Ref. to McTaggart 1963||||||
8248|Heifer Creek Sandstone Member|44028|14|Not recorded|Fig.2,p509||Jurassic|Of Marburg Formation. See Strat Table.||||||
8248|Heifer Creek Sandstone Member|44032|14|Not recorded|p462,464,465|||Part of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||20-JUL-04
8248|Heifer Creek Sandstone Member|60281|5|Briefly described|p30, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation. Coarse quartz sandstone, granite conglomerate.  Max. thickness: 50m.  Geological Province: Clarence-Moreton Basin.  See also the misspelt Heffer Creek Sandstone Member.||||||20-JAN-05
8248|Heifer Creek Sandstone Member|60993|4|Described|p6 Fig. 2, p27|||First named by Gray (1975 as part of Marburg Fm), and retained in current use as member of Koukandowie Fm (Marburg Subgrp). Tough, quartzose sst, cross-bedded. Geol. Prov: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60995|4|Described|p66, p51 Fig. 3|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Coarse quartz sandstone, granite conglomerate. Overlies Ma Ma Creek Member. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. ||||||
8248|Heifer Creek Sandstone Member|60996|5|Briefly described|p72|||Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60997|5|Briefly described|p140 Fig. 2|||Superseded by Heifer Creek Member. Formerly part of McTaggart's Marburg Formation (1963).||||||
8248|Heifer Creek Sandstone Member|60998|5|Briefly described|p146 Fig. 2|||Consists of fluvial stacked channel sand. Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60999|6|Mentioned|p174|||Probably should be Heifer Creek Member - names used interchangeably.||||||
8248|Heifer Creek Sandstone Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|61006|5|Briefly described|p278|||Of the Koukandowie Formation. Quartzose sandstone unit (sheet-like braided-stream deposits) with potential as reservoir rocks. See also Heifer Creek Member - names used interchangeably. See also p279 Tb. 1, p285.||||||
8248|Heifer Creek Sandstone Member|64665|5|Briefly described|p53 Fig.2.|Middle Jurassic|Middle Jurassic|Clarence-Moreton Basin. Correlates with Hutton Sandstone (Eromanga and Surat basins).||Upper unit in Koukandowie Formation.||Overlies Ma Ma Creek Member. Is overlain by Walloon Coal Measures.||
8248|Heifer Creek Sandstone Member|67402|4|Described|p187, p190 fig CLM6, p193|Aalenian|Pliensbachian|Clarence-Moreton Basin. Represents a change in depositional environment from floodplain back to braided stream deposition. ||Koukandowie Formation||Overlies the Ma Ma Creek Member. Overlain by the Walloon Subgroup.|Thick to very thickly bedded, coarse to very coarse-grained, white to grey, quartzose and minor quartz lithic sandstone and granule conglomerate.|
8248|Heifer Creek Sandstone Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. 10-50m thick. Deposited as channel fill deposits in a meandering fluvial system. Good reservoir potential in coarse sandstone and granule conglomerates. ||Koukandowie Formation||Overlies the Ma Ma Creek Member.|Coarse quartz sandstone and granite conglomerate.|
8248|Heifer Creek Sandstone Member|69594|5|Briefly described|p519, p544, p573|Middle Jurassic|Middle Jurassic|Clarence-Moreton Basin. Diachronous. Forms prominent topographic features. Appears as Heifer Creek Sandstone on p544.||Koukandowie Formation.||Overlies Ma Ma Creek Member. Is overlain by Walloon Coal Measures.|Coarse-grained, cross-bedded, quartzose sandstone.|
8248|Heifer Creek Sandstone Member|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Middle Jurassic|Northern Clarence-Moreton Basin area.||Unit in Koukandowie Formation.||||
8248|Heifer Creek Sandstone Member|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
8248|Heifer Creek Sandstone Member|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Koukandowie Formation.||Overlies Ma Ma Creek Member.||
8248|Heifer Creek Sandstone Member|71805|5|Briefly described|p76|Bajocian|Aalenian|Clarence-Moreton Basin.||Koukandowie Formation||Overlies the Ma Ma Creek Sandstone Mmeber.||
8248|Heifer Creek Sandstone Member|72297|5|Briefly described|p746|||Clarence-Moreton Basin. Hydrocarbon reservoir potential.||Marburg Subgroup.||||
8255|Helby beds|23425|5|Briefly described|p381.|||Also see Plate 9.2. Geological Province Carpentaria Basin.||||||
8255|Helby beds|23430|5|Briefly described|p522|||||||||
8255|Helby beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
8255|Helby beds|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
8255|Helby beds|42637|4|Described|p9|||Variation on Helby Beds.||||||
8255|Helby beds|43105|5|Briefly described|p16|||||||||
8255|Helby beds|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||||||
8255|Helby beds|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Middle Jurassic|Carpentaria Basin.||||||
8255|Helby beds|68135|5|Briefly described|p52 fig 2b, p65|Early Cretaceous|Kimmeridgian|Carpentaria Basin. Described as "poorly understood". Contains plant and invertebrate fossils. Marine deposits.
||||Overlies Hampstead Sandstone; overlain by Gilbert River Formation|Cross-bedded sandstone.|14-SEP-17
8255|Helby beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Albany Pass beds under the symbol, JKh.||||||
8255|Helby beds|69594|5|Briefly described|p518, p520-522, p540-541, p573|Hauterivian|Middle Jurassic|Powell et al. (1976). Western Gulf Sub-basin (Cape York Peninsula), Carpentaria Basin. >330m (possibly up to 600m) thick. Bioturbation and microflora indicate paralic to marine deposition. One of the main aquifers in the Basin. In the Peninsula Basin, the onshore succession was mapped as Helby beds. RELATED UNITS (continued): Equivalent to Gilbert River Formation (and interfingers with it); Albany Pass beds; and Dalrymple Sandstone (partly).||||Is overlain by Wallumbilla Formation. Intercalates with, transgresses and is equivalent to the Garraway Sandstone. See COMMENTS for more.|Quartzose sandstones and minor siltstone. Peninsula Basin: quartzose sandstones, granule conglomerates, micaceous calcareous siltstones with minor glauconite and pyrite, tuff and tuffaceous sandstones in the lower part.|
8255|Helby beds|71409|5|Briefly described|p1058-1059, p1061|Jurassic|Jurassic|Carpentaria Basin. Likely source rocks for heavy minerals in northern Cape York Peninsula. Appears as Helby Beds on p1058.|||||Sandstones.|
8255|Helby beds|71863|5|Briefly described|p5|Barremian|Berriasian|Northern Carpentaria Basin.||||Overlain by the Wallumbilla Formation.||01-MAY-19
8255|Helby beds|72298|5|Briefly described|p801|Cretaceous|Jurassic|Carpentaria Basin. Main confined aquifers, generally producing flowing artesian water bores.||||Is overlain by Albany Pass beds and Wallumbilla FZ.||
8255|Helby beds|73083|6|Mentioned|p68, p73|Mesozoic|Mesozoic|||||||
8256|Helen Springs Volcanics|12891|5|Briefly described|p731|||Equivalent of Antrim Plateau Volcanics.||||||07-FEB-11
8256|Helen Springs Volcanics|14019|6|Mentioned|p19|||Geochemically identical with Antrim Plateau Volcanics, Peaker Piker Volcanics in the N.T. and  Colless Volcanics in Qld.||||Geochemically identical with Antrim Plateau Volcanics, Peaker Piker Volcanics in the N.T. and  Colless Volcanics in Qld.||24-NOV-09
8256|Helen Springs Volcanics|22954|6|Mentioned|Fig3p9|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|23328|5|Briefly described|1030 Fig.1|||K-Ar age 508+/-12 Ma||||||07-SEP-09
8256|Helen Springs Volcanics|23410|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Weathered vesicular basalt; minor felsic volcanic and volcaniclastic rocks; pebble conglomerate and lithic arenite.||||||02-NOV-05
8256|Helen Springs Volcanics|24172|4|Described|p29|Cambrian|Cambrian|Unconformably overlies Warramunga Fm (Tennant Creek) and Flynn Subgroup. Part of this unit may belong to Whittington Range Member as suggested by Mendum and Tonkin (1976); conversely, Whittington Range Member rocks are possibly Helen Springs Volcanics.||||||26-SEP-06
8256|Helen Springs Volcanics|24303|2|Defined|p34, p62 Appendix|Early Cambrian|Early Cambrian|Max. Thickness: 36 m excluding Muckaty Sandstone Member. Disconformably overlain by the Gum Ridge Formation and Montejinni Limestone. Correlates with the Antrim Plateau Volcanics, Nutwood Downs Volcanics and possibly Peaker Piker and Colless Volcanics.||||||
8256|Helen Springs Volcanics|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Includes basalt (tholeiitic, massive, aphanitic to coarse-grained), calcite or smoky quartz amydales; sandstone, quartz arenite; and, undifferentiated basalt, sandstone, pebble to cobble bearing sandstone and breccia.||||||17-OCT-05
8256|Helen Springs Volcanics|30320|6|Mentioned|p422|||||||||
8256|Helen Springs Volcanics|31637|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|32174|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|32959|6|Mentioned|Fig.12|||||||||
8256|Helen Springs Volcanics|33307|6|Mentioned|Fig.8|||||||||
8256|Helen Springs Volcanics|33516|6|Mentioned|p99|||||||||
8256|Helen Springs Volcanics|34051|6|Mentioned|p6|||L.Camb.||||||
8256|Helen Springs Volcanics|34053|6|Mentioned|p7|||L.Camb.||||||
8256|Helen Springs Volcanics|34149|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|34151|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|34162|6|Mentioned|p117|||Early Cambrian.||||||
8256|Helen Springs Volcanics|34440|5|Briefly described|Table 1|||L.Camb.||||||
8256|Helen Springs Volcanics|34441|4|Described|Table 1|||L.Camb. See also pp11,12 etc.||||||26-SEP-06
8256|Helen Springs Volcanics|35054|6|Mentioned|p245|||||||||
8256|Helen Springs Volcanics|35229|4|Described|Table.1|||||||||
8256|Helen Springs Volcanics|35771|4|Described|Table 1|||||||||
8256|Helen Springs Volcanics|36335|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|37572|5|Briefly described|p155|||See also p151,165.||||||26-SEP-06
8256|Helen Springs Volcanics|38446|6|Mentioned|p143|||||||||
8256|Helen Springs Volcanics|39213|6|Mentioned|Fig.8|||||||||
8256|Helen Springs Volcanics|40852|6|Mentioned|p36|||||||||
8256|Helen Springs Volcanics|41129|6|Mentioned|p15|||||||||
8256|Helen Springs Volcanics|41524|6|Mentioned|Fig.3|||||||||
8256|Helen Springs Volcanics|42504|5|Briefly described|Table 4 P73|||||||||
8256|Helen Springs Volcanics|42956|5|Briefly described|p31 Fig.4|||||||||
8256|Helen Springs Volcanics|43223|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
8256|Helen Springs Volcanics|43224|5|Briefly described|Map legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
8256|Helen Springs Volcanics|44482|14|Not recorded|p.11|||(E53-12).||||||
8256|Helen Springs Volcanics|44960|14|Not recorded|Not recorded|||||||||
8256|Helen Springs Volcanics|45052|4|Described|p64|||See also p69.||||||26-SEP-06
8256|Helen Springs Volcanics|45064|3|Fully described|Table 1|||See also p18.||||||26-SEP-06
8256|Helen Springs Volcanics|45079|6|Mentioned|p8|||Lower Cambrian age||||||
8256|Helen Springs Volcanics|45087|6|Mentioned|p152|||Chemical analyses||||||
8256|Helen Springs Volcanics|45140|6|Mentioned|p13|||Tennant Creek region.||||||
8256|Helen Springs Volcanics|45148|5|Briefly described|p9|||||||||
8256|Helen Springs Volcanics|45373|14|Not recorded|p.177-179|||||||||
8256|Helen Springs Volcanics|46842|6|Mentioned|p115|||||||||
8256|Helen Springs Volcanics|47058|6|Mentioned|Fig.3 p123|||||||||08-JUL-20
8256|Helen Springs Volcanics|48835|14|Not recorded|p.9|||||||||
8256|Helen Springs Volcanics|48860|14|Not recorded|map legend|||may legend of Tennant Creek, 1 mile. (SE 53-14).||||||
8256|Helen Springs Volcanics|48891|14|Not recorded|p.22||Early Cambrian|Tb.1. Lower Cambrian.||||||
8256|Helen Springs Volcanics|60637|5|Briefly described|Map legend|||Basalt; basalt sandstone and breccia.||||||02-DEC-04
8256|Helen Springs Volcanics|60684|4|Described|p14|Early Cambrian|Early Cambrian|Basic to intermediate volcanic rocks - largely composed of amygdaloidal or vesicular tholeiitic basalt. Unconformably overlie folded Warramunga Formation; parts unconformably overlie Rising Sun Conglomerate. Also underlies Gum Ridge Formation.||||||
8256|Helen Springs Volcanics|62557|5|Briefly described|p461-463|Middle Cambrian|Middle Cambrian|Of the Kalkarindji continental flood basalt province. Ar/Ar age 508+/-2 Ma.||||||24-NOV-09
8256|Helen Springs Volcanics|64068|5|Briefly described|p81|Early Cambrian|Early Cambrian|Kalkarindji Flood Basalt Province, central and northwest Georgina Basin. c.513-c.504 Ma. ||||||
8256|Helen Springs Volcanics|64443|4|Described|iii, p4, p6-8, Tb.1, p40.|Early Cambrian|Early Cambrian|Combined with Peaker Piker Volcanics (of Smith & Roberts, 1963) by Kruse (2003). Max 34m thick. Dated at 508 +/- 2 Ma (Glass and Phillips 2002).||||Unconformably underlies Wonarah Formation (Barkly Group); unconformably overlies Mittiebah Sandstone, Mullera Formation or undivided South Nicholson Group.|Basalt, trachyte, microdolerite; minor dolerite; basal pebbly mudstone, sandstone and conglomerate. Shows alteration and amygdales.|01-MAY-15
8256|Helen Springs Volcanics|64589|4|Described|dated_samples, chemistry files||Cambrian|Coarse grained basaltic rock. K-Ar whole rock crystallization age of basalt 500+/-12 Ma. Geochemical analyses from Helen Springs NT.||||||12-NOV-08
8256|Helen Springs Volcanics|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|65209|6|Mentioned|p38|||||||Correlated with Rising Sun Conglomerate.||05-JAN-17
8256|Helen Springs Volcanics|65336|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Kalkarindji Volcanic Group. Unconformably overlies South Nicholson Group; unconformably underlies Thorntonia Limestone of Narpa Group and Wonorah Formation, Barkly Group. Consists of basalt, trachyte, microdolerite, minor dolerite, basal mudstone, pebbly sandstone, conglomerate.||||||29-SEP-11
8256|Helen Springs Volcanics|65337|3|Fully described|p v, p6 Fig.3, pp61-63.|Early Cambrian|Early Cambrian|Part of cratonic-scale flood basalt event in northern Australia; represents basal Georgina Basin deposits in southern and western MOUNT DRUMMOND area. Has a distinctive aeromagnetic signature. Outcrops as sporadic corestones in red-brown pisolitic soils.|508+/-2 Ma (Glass and Phillips 2002).|Unit in Kalkarindji Volcanic Group.|Includes Muckaty Sandstone Member.|Unconformably overlies South Nicholson Group. Is unconformably overlain by Wonarah Formation.|Basal pebbly sandstone and conglomerate; basalt, trachyte, dolerite, variably altered and amygdaloidal.|
8256|Helen Springs Volcanics|65344|4|Described|p3, 6, 7, 9, 12, 13, 17-20, Figs., Tbls|Early Cambrian|Early Cambrian|Of the Barkly Sub-basin and Alexandria-Wonarah Basement High, Georgina Basin. See well logs and thin section descriptions for detail. Thickness: up to 155.9m in AY06DD0||||Overlies the Renner Group and the South Nicholson Group. Underlies Gum Ridge Formation and Wonarah Formation.|Metavolcanics.|03-MAY-12
8256|Helen Springs Volcanics|65345|6|Mentioned|p11 Fig.11. |||||||||
8256|Helen Springs Volcanics|67149|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|||||Overlies South Nicholson Group. Is overlain by Gum Ridge Formation.|Variably altered, locally amygdaloidal basalt and microdolerite; thin basal pebbly sandstone and conglomerate (cross-section only).|
8256|Helen Springs Volcanics|67150|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|||||Unconformably overlies South Nicholson Group. Is unconformably overlain by Gum Ridge Formation.|Basalt, dolerite; basal and interbedded mudstone, pebbly sandstone, conglomerate, breccia (cross-section only).|
8256|Helen Springs Volcanics|67352|4|Described|v, p6,16-17,19-21,31-32,42,45-49,51,54|Early Cambrian|Early Cambrian|Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km. Widespread in subsurface of central Georgina Basin. Not exposed in these map areas.|505 +/- 2 Ma (40Ar/39Ar, Glass and Phillips 2006)||Muckety Sandstone Member.|Overlies South Nicholson, Hatches Creek, Renner and McArthur Groups. Overlain by Gum Ridge Formation, Top Springs Limestone. Synonymous with Peaker Piker Volcanics.|Variably altered and locally amygdaloidal tholeiitic basalt, trachyte, microdolerite and minor dolerite, together with subordinate basal and intraformational sandstone, mudstone and conglomerate.|
8256|Helen Springs Volcanics|69424|5|Briefly described|p9:26-27|Early Cambrian|Early Cambrian|Kalkarindji Province.|||Muckaty Sandstone Member.||Tuffaceous siltstone and sandstone.|12-JUL-16
8256|Helen Springs Volcanics|69431|6|Mentioned|p16:18-19|||Kalkarindji Province.|||Muckaty Sandstone Member.|||12-JUL-16
8256|Helen Springs Volcanics|69434|5|Briefly described|p19:4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Unconformably overlies South Nicholson Group.||12-JUL-16
8256|Helen Springs Volcanics|69437|5|Briefly described|p22:10|Series 2|Series 2|Kalkarindji Large Igneous Province.||||Is overlain by Gum Ridge Formation and Thorntonia Limestone.||12-JUL-16
8256|Helen Springs Volcanics|69443|5|Briefly described|p28:5, 12, 21-22, 42|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Unconformably overlies Bukalara Sandstone. Is overlain dis/unconformably by Wonarah Formation (Barkly Group).|Volcanic and minor sedimentary rocks.|12-JUL-16
8256|Helen Springs Volcanics|69445|3|Fully described|p30:1-2, 5-6, 8-9, 16-17|Early Cambrian|Early Cambrian|Noakes and Traves (1954). Georgina Basin (subsurface) and east of the Tennant Region (exposed). Synonymous with the former Peaker Piker Volcanics. Up to 156m thick; 36m thick in the type section in HELEN SPRINGS map area (9m in cored drillhole NTGS 96/1 at 18o24'55"S, 134o14'40"E). Other age determinations include Ar40/Ar39 plagioclase separates: 508 +/- 2 Ma and 505 +/- 2 Ma (average 507 +/- 2 Ma) by Glass and Phillips (2006).|511 +/- 12 Ma (K-Ar; Bultitude, 1972).|Kalkarindji Suite.|Muckaty Sandstone Member.|Unconformably overlies South Nicholson Group. Is overlain disconformably by Gum Ridge, Wonarah Formations and Top Springs Limestone.|Widespread sub-aerial basaltic lavas.|12-JUL-16
8256|Helen Springs Volcanics|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Thorntonia Limestone||
8256|Helen Springs Volcanics|69673|6|Mentioned|p39, p40, p58, p112, p136|||||Kalkarindji Suite|Includes Muckaty Sandstone Member|Unconformably overlies Bukalara Sandstone||
8256|Helen Springs Volcanics|70380|5|Briefly described|p745|Early Cambrian|Early Cambrian|Kalkarindji Large Igneous Province. Forms basement to central and northern Georgina Basin.||||||
8256|Helen Springs Volcanics|70968|5|Briefly described|p93, p100-101, p105, p108, p115|||Has a high-frequency magnetic expression.||Kalkarindji Suite.|Muckaty Sandstone Member.|Unconformably overlies Baralandji, Powell, Wiernty Formations (Renner Group).||
8256|Helen Springs Volcanics|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|Shown with Colless Volcanics.||||||
8256|Helen Springs Volcanics|72527|6|Mentioned|p5 Fig.1.2.|Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|72919|6|Mentioned|p77|Cambrian|Cambrian|Georgina Basin. 101 m intersected in drillhole CRDD001.|||Overlain by Barkly Group.|||
8256|Helen Springs Volcanics|72967|6|Mentioned|p5|||Georgina Basin.||||||
8256|Helen Springs Volcanics|73083|6|Mentioned|p3, p47|Cambrian|Cambrian|[Superseded by or a constituent of the Kalkarindji Suite]. These rocks comprise one of a series of widely separated exposures of Cambrian basalt attributed to the Kalkarindji Continental Flood Basalt Province (Glass et al, 2013). Correlation was based on matching magnetic signatures.|||||Basalt.|
8264|Heliman Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Toole Creek Volcanics and Willyama Supergroup Bijerkerno Metasediments.||||||07-NOV-08
8264|Heliman Formation|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon).Thickness: 800-2500m. Geological Province: Georgetown Region.||||||08-JUL-15
8264|Heliman Formation|23430|5|Briefly described|p456.|||||||||
8264|Heliman Formation|35082|6|Mentioned|p209|||||||||
8264|Heliman Formation|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
8264|Heliman Formation|35921|2|Defined|p38|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
8264|Heliman Formation|36153|6|Mentioned|Fig.10|||||||||
8264|Heliman Formation|36216|6|Mentioned|p208|||||||||
8264|Heliman Formation|36780|6|Mentioned|Fig.10|||||||||
8264|Heliman Formation|37570|4|Described|p116|||See also Fig.2||||||
8264|Heliman Formation|38714|6|Mentioned|p182|||||||||
8264|Heliman Formation|39445|5|Briefly described|Table 2|||||||||
8264|Heliman Formation|39687|6|Mentioned|p1|||||||||
8264|Heliman Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
8264|Heliman Formation|39924|6|Mentioned|Fig.3|||||||||
8264|Heliman Formation|39943|6|Mentioned|Table 1A|||||||||
8264|Heliman Formation|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8264|Heliman Formation|41975|6|Mentioned|Fig.3 P433|||||||||
8264|Heliman Formation|42199|5|Briefly described|Table 1 P280|||||||||
8264|Heliman Formation|43664|4|Described|p29-31|||||||||
8264|Heliman Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Overlies: Townley Formation. Underlies: Candlow Formation.||||||30-JUN-15
8264|Heliman Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||30-JUL-04
8264|Heliman Formation|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Etheridge Group. Overlies: Townley Formation. Underlies: Candlow Formation.||||||30-JUN-15
8264|Heliman Formation|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Etheridge Group. Sandstone, sandy siltstone and mudstone.||||||
8264|Heliman Formation|66800|6|Mentioned|p926 Table 1.|||||||Overlies Townley Formation. Is overlain by Candlow Formation.||
8264|Heliman Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.|1625 +/- 15 Ma (40Ar/39Ar mica).|Upper Etheridge Group.||||
8264|Heliman Formation|67341|5|Briefly described|vi, p18-21|||Forsayth Subprovince, Etheridge Province. Maximum depositional age.|1656 +/- 4 Ma (SHRIMP U-Pb zircon).|||Overlies Townley Formation. Is overlain by Candlow Formation.|Includes fine-grained sandstone with mud clasts.|
8264|Heliman Formation|67430|6|Mentioned|p25|||||||||
8264|Heliman Formation|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min Mesoproterozoic?||Unit in Etheridge Group.||Is overlain conformably by Candlow Formation.|Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|12-MAY-15
8264|Heliman Formation|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.||Is overlain conformably by Candlow Formation.|Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|12-MAY-15
8264|Heliman Formation|68352|5|Briefly described|Map legend.|Mesoproterozoic?|Paleoproterozoic|Etheridge Province. Moderately magnetic. Min Age: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Townley Formation. Is overlain conformably by Candlow Formation.|Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|18-MAY-15
8264|Heliman Formation|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Includes a separately mapped facies variant. Shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Etheridge Group.||Conformably overlain by the Candlow Formation. Conformably underlain by the Townley Formation.|Mudstone, siltstone and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|
8264|Heliman Formation|69582|5|Briefly described|p76, p80|||Etheridge Province. Intersected in GSQ Georgetown 8-9R.||||Overlies the Townley Formation.|Sericitic siltstone and lithic quartz sandstone with prominent beds of very dark-grey siliceous 'flinty' siltstone and quartzose sandstone.|
8264|Heliman Formation|69591|5|Briefly described|p61-62, p65, p67-68|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Similar lithologies, but differing proportions, to Candlow Formation. Their combined thickness is 2000-6000m. Contains significant population of ~1655-1650 Ma zircons (Neumann and Kositcin, 2011). |~1655 Ma.|Etheridge Group.|||Siltstone, carbonaceous mudstone, siliceous siltstone, fine sandstone (characterised by high proportion of sand-sized carbonaceous mudstone clasts); rare thin limestones.|
8264|Heliman Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1656+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
8269|Hells Gate Rhyolite|23422|4|Described|p183|Late Carboniferous|Late Carboniferous|Of Sybil Group.||||||
8269|Hells Gate Rhyolite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|of Sybil Group.||||||
8269|Hells Gate Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V57. Assumed to be I-Type.||||||
8269|Hells Gate Rhyolite|23893|5|Briefly described|p9 Fig. 4|Late Carboniferous|Late Carboniferous|Of Sybil Group.||||||
8269|Hells Gate Rhyolite|24612|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|Geological Province: Burdekin Basin.||||||
8269|Hells Gate Rhyolite|24613|5|Briefly described|p6 Fig. 3, p113|Early Devonian|Precambrian|Geological province: Burdekin Basin.||||||07-FEB-11
8269|Hells Gate Rhyolite|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
8269|Hells Gate Rhyolite|32169|6|Mentioned|Table 2|||U.Carboniferous||||||
8269|Hells Gate Rhyolite|32553|4|Described|p46|||||||||
8269|Hells Gate Rhyolite|34408|6|Mentioned|p185|||On Table||||||
8269|Hells Gate Rhyolite|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
8269|Hells Gate Rhyolite|37573|6|Mentioned|p226|||||||||
8269|Hells Gate Rhyolite|37613|5|Briefly described|p249|||See also Fig.3||||||
8269|Hells Gate Rhyolite|39445|5|Briefly described|Table 7|||See also Fig.6||||||
8269|Hells Gate Rhyolite|39686|6|Mentioned|p73|||||||||
8269|Hells Gate Rhyolite|39735|6|Mentioned|p18|||||||||
8269|Hells Gate Rhyolite|42295|5|Briefly described|Fig.2 P5|||||||||
8269|Hells Gate Rhyolite|42547|5|Briefly described|p76|||||||||
8269|Hells Gate Rhyolite|42690|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
8269|Hells Gate Rhyolite|42692|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
8269|Hells Gate Rhyolite|42933|5|Briefly described|p214|||||||||
8269|Hells Gate Rhyolite|43095|1|Redefined|p67|Late Carboniferous||of Sybil Group||||||
8269|Hells Gate Rhyolite|43259|4|Described|Appendix 1,p5.||Late Carboniferous|of Sybil Group. Age Late Carboniferous?||||||
8269|Hells Gate Rhyolite|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
8269|Hells Gate Rhyolite|44061|4|Described|Table 3||Late Carboniferous|||||||
8269|Hells Gate Rhyolite|44091|14|Not recorded|p40|Late Carboniferous|Early Carboniferous|(Middle Carb - Late Carb)||||||
8269|Hells Gate Rhyolite|45151|5|Briefly described|Table 7|||||||||
8269|Hells Gate Rhyolite|46845|6|Mentioned|Table 1|||||||||
8269|Hells Gate Rhyolite|48904|2|Defined|p39|Late Carboniferous|Late Carboniferous|||||||
8269|Hells Gate Rhyolite|68350|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Sybil Group.|Includes Malairo Rhyolite Member.|Is overlain conformably by Engow Member (Marshs Creek Formation).|Rhyolitic to dacitic volcaniclastic rocks (including ignimbrite) and lava; minor andesite or basalt and polymictic conglomerate and sandstone.|
8269|Hells Gate Rhyolite|68351|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Sybil Group.|Includes Malairo Rhyolite Member.|Is overlain conformably by Engow Member (Marshs Creek Formation).|Rhyolitic to dacitic volcaniclastic rocks (including ignimbrite) and lava; minor andesite or basalt and polymictic conglomerate and sandstone.|
8269|Hells Gate Rhyolite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
8269|Hells Gate Rhyolite|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
8269|Hells Gate Rhyolite|68731|5|Briefly described|p203||||||Includes the Malairo Rhyolite Member.|Unconformably underlain by the Ruxton Formation.|Comprises, in its lower part, volcaniclastics and tuff including ignimbrite, dominantly or rhyolitic composition, with very minor contribution of mafic volcanic rocks. Its upper parts consists of rhyolite flows.|
8269|Hells Gate Rhyolite|69592|4|Described|p274 Fig.4.65, p275|Permian|Pennsylvanian|Sybil Graben; extends beyond the Graben boundaries to the S. Up to 900m thick.||Sybil Group.|Malairo Rhyolite Member.|Is overlain by Marshs Creek Formation.|Lower part is largely volcaniclastic, rhyolitic strata including massive, crystal-rich ignimbrite; upper part is predominantly rhyolite flows.|
8269|Hells Gate Rhyolite|69593|5|Briefly described|p496-497|||Wyatt et al. (1970). NW-trending Sybil Graben, Townsville hinterland. Up to 900m thick.||Sybil Group.|||Dominated by rhyolitic ignimbrite.|
8283|Herbert River Granite|22744|6|Mentioned|P12|||||||||
8283|Herbert River Granite|23291|5|Briefly described|p99 Tb. 3.11|Carboniferous|Carboniferous|Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||14-APR-15
8283|Herbert River Granite|23494|4|Described|p10, p20 Tb. 1|Permian|Carboniferous|Intrudes Sunday Creek Volcanics, Mount Garnet Formation, Wairuna, Greenvale and Pelican Range Formations; intruded by Elizabeth Creek Granite and Tiger Hill Microgranite.||||||
8283|Herbert River Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 407. I-Type.||||||
8283|Herbert River Granite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p33. Kennedy Province.||||||
8283|Herbert River Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
8283|Herbert River Granite|23619|4|Described|p38 Table 2|Permian|Carboniferous|In contact with Princess Hills and Minnamoolka Granites but exact relationship not known. Also see p10. Herbert River Batholith.||||||
8283|Herbert River Granite|23624|6|Mentioned|p23|||Superseded by Rudd Granite.||||||
8283|Herbert River Granite|24013|5|Briefly described|p17 Tb. 1|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
8283|Herbert River Granite|29605|6|Mentioned|p1|||||||||
8283|Herbert River Granite|29793|6|Mentioned|Fig.1|||||||||
8283|Herbert River Granite|29794|6|Mentioned|Fig.1|||||||||
8283|Herbert River Granite|29795|6|Mentioned|p273|||||||||
8283|Herbert River Granite|29796|6|Mentioned|Fig.1|||||||||
8283|Herbert River Granite|30505|5|Briefly described|p5|||Permian. See also P6,7. Divided into a number of units||||||
8283|Herbert River Granite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
8283|Herbert River Granite|31453|6|Mentioned|p617|||||||||
8283|Herbert River Granite|31812|6|Mentioned|p481|||Host to fluorspar.||||||
8283|Herbert River Granite|31822|6|Mentioned|p67|||||||||
8283|Herbert River Granite|31832|6|Mentioned|Table 6|||||||||
8283|Herbert River Granite|32360|6|Mentioned|p741|||||||||
8283|Herbert River Granite|32528|5|Briefly described|Table 1|||||||||
8283|Herbert River Granite|32553|4|Described|p58|||||||||
8283|Herbert River Granite|32818|6|Mentioned|p21|||||||||
8283|Herbert River Granite|35000|6|Mentioned|p137|||||||||
8283|Herbert River Granite|36527|6|Mentioned|p163|||||||||
8283|Herbert River Granite|36563|6|Mentioned|Table 1|||||||||
8283|Herbert River Granite|38225|6|Mentioned|Fig.2|||||||||
8283|Herbert River Granite|38688|6|Mentioned|p47|||||||||
8283|Herbert River Granite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
8283|Herbert River Granite|39445|5|Briefly described|Table 12|||6 units (Blake 1972). See also P90||||||
8283|Herbert River Granite|39689|6|Mentioned|p58|||||||||
8283|Herbert River Granite|40743|5|Briefly described|p311|||||||||
8283|Herbert River Granite|41235|6|Mentioned|p40|||||||||
8283|Herbert River Granite|42200|6|Mentioned|Fig.1 P325|||||||||
8283|Herbert River Granite|42459|5|Briefly described|p70|||||||||
8283|Herbert River Granite|42547|4|Described|p75|||||||||
8283|Herbert River Granite|43087|6|Mentioned|p19|||||||||
8283|Herbert River Granite|43113|4|Described|Table 2 p24|Permian|Carboniferous|||||||
8283|Herbert River Granite|43253|5|Briefly described|map legend|Permian|Carboniferous|||||||
8283|Herbert River Granite|43259|4|Described|Appendix 1,p45.|Permian|Carboniferous|||||||
8283|Herbert River Granite|43716|6|Mentioned|p17|||||||||
8283|Herbert River Granite|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
8283|Herbert River Granite|43901|14|Not recorded|Map Legend||Late Permian|(Early Triassic) - Late Permian||||||
8283|Herbert River Granite|43903|14|Not recorded|Map Legend||Early Permian|Early Permian to Middle (?) Carboniferous||||||
8283|Herbert River Granite|43904|14|Not recorded|Map Legend||Neoproterozoic|||||||
8283|Herbert River Granite|43926|14|Not recorded|p17,Tb.2,opp.p10|||||||||
8283|Herbert River Granite|43927|14|Not recorded|p11,opp.p8|||||||||
8283|Herbert River Granite|43978|14|Not recorded|p150|||||||||
8283|Herbert River Granite|44044|14|Not recorded|p125,Fig.18|||||||||
8283|Herbert River Granite|44046|14|Not recorded|p153|||Intrudes Wairuna Formation.||||||
8283|Herbert River Granite|44048|14|Not recorded|Map Legend||Permian|(Triassic?)||||||
8283|Herbert River Granite|44052|14|Not recorded|p128|||||||||
8283|Herbert River Granite|44053|2|Defined|p240-3||Carboniferous|||||||
8283|Herbert River Granite|44057|14|Not recorded|p606-607|Permian|Carboniferous|Anatectic magma||||||
8283|Herbert River Granite|44059|14|Not recorded|p442(Tb)||Late Devonian|||||||
8283|Herbert River Granite|44068|14|Not recorded|p8|||||||||
8283|Herbert River Granite|44258|14|Not recorded|p1,5,7,12,14,18,31,||Late Paleozoic|p34-36||||||07-NOV-08
8283|Herbert River Granite|44259|14|Not recorded|p107|||286+/-8 Ma.||||||
8283|Herbert River Granite|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
8283|Herbert River Granite|44515|2|Defined|p32,33||Mesoproterozoic|||||||
8283|Herbert River Granite|44516|2|Defined|p32,33||Early Paleozoic|(Middle Palaeozoic)||||||07-NOV-08
8283|Herbert River Granite|44557|14|Not recorded|p121|||Contains lode (copper)||||||
8283|Herbert River Granite|44573|14|Not recorded|p98|||||||||
8283|Herbert River Granite|44843|14|Not recorded|p179|||||||||
8283|Herbert River Granite|45003|14|Not recorded|p34|||||||||
8283|Herbert River Granite|45008|14|Not recorded|p12,16,39-43,51,95,|||p109,maps||||||
8283|Herbert River Granite|45009|2|Defined|p75,104-5,110-1,114,||Permian|p119-20,131-3,136,Pl.13,Tb.13,p41,45,46.||||||
8283|Herbert River Granite|45014|2|Defined|40,48-50,102-107,157|Permian|Early Carboniferous|Pl.29,38,40,Tb.A, Tb.1.||||||
8283|Herbert River Granite|45025|4|Described|p75, anal.p81|Permian|Carboniferous|||||||
8283|Herbert River Granite|45065|6|Mentioned|p35|||||||||
8283|Herbert River Granite|45087|5|Briefly described|p9|||Chemical analyses||||||
8283|Herbert River Granite|45113|3|Fully described|p16|||Emphasis on petrography.||||||
8283|Herbert River Granite|46845|6|Mentioned|Table 1|||||||||
8283|Herbert River Granite|46879|6|Mentioned|Fig.1|||||||||
8283|Herbert River Granite|48894|6|Mentioned|p51|||See also P52. 285my.||||||
8283|Herbert River Granite|48976|4|Described|p24|||Isotopic data Table 4||||||
8283|Herbert River Granite|70207|6|Mentioned|p25|||||||||
8297|Herring Gully Limestone Member|30451|6|Mentioned|p22|||||||||
8297|Herring Gully Limestone Member|31659|6|Mentioned|p55|||Mb. of Bancroft Fm.||||||
8297|Herring Gully Limestone Member|42002|5|Briefly described|p92|||||||||
8297|Herring Gully Limestone Member|42547|5|Briefly described|p50|||of the Bancroft Formation.||||||
8297|Herring Gully Limestone Member|44360|2|Defined|p1,4-6,26,30,map||Tournaisian|Member of Bancroft Formation.||||||
8297|Herring Gully Limestone Member|44379|14|Not recorded|p15|||Ref. to McKellar 1967.||||||
8297|Herring Gully Limestone Member|68008|5|Briefly described|p90|Early Carboniferous|Early Carboniferous|||Basal Caswell Creek Group.||Correlated with the Gudman Oolite.||
8297|Herring Gully Limestone Member|68679|5|Briefly described|p340|||Yarrol Syncline.||||Correlated with Gudman Oolite.||
8388|Hobblechain Rhyolite|22432|5|Briefly described|p22|Statherian|Statherian|Age 1725+/- 2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|22538|6|Mentioned|App1 P722||Statherian|||||||
8388|Hobblechain Rhyolite|22665|5|Briefly described|Table1 P222, P225||Statherian|Age of unit is 1725+/-2 Ma||||||
8388|Hobblechain Rhyolite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawalla Group.||||||07-NOV-08
8388|Hobblechain Rhyolite|23395|5|Briefly described|p389|||||||||
8388|Hobblechain Rhyolite|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of Tawallah Group.  Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23398|5|Briefly described|p436|Statherian|Statherian|Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23776|5|Briefly described|p705 Fig 2.|Statherian|Statherian|Age: 1725+/-2 Ma. Of Tawallah Group.||||||26-SEP-06
8388|Hobblechain Rhyolite|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
8388|Hobblechain Rhyolite|24050|6|Mentioned|p27|||||||||
8388|Hobblechain Rhyolite|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Rocks of lava domes and flows. Coarse porphyritic quartz-feldspar rhyolite.||||||07-FEB-11
8388|Hobblechain Rhyolite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
8388|Hobblechain Rhyolite|24432|6|Mentioned|p570 Fig.10|||||||||
8388|Hobblechain Rhyolite|32519|6|Mentioned|p341|||||||||
8388|Hobblechain Rhyolite|32904|6|Mentioned|p95|||||||||
8388|Hobblechain Rhyolite|35114|6|Mentioned|Fig.5|||||||||
8388|Hobblechain Rhyolite|36012|6|Mentioned|p16|||||||||
8388|Hobblechain Rhyolite|37371|6|Mentioned|p368|||||||||
8388|Hobblechain Rhyolite|38042|6|Mentioned|p167|||||||||
8388|Hobblechain Rhyolite|40105|6|Mentioned|Fig.7|||||||||
8388|Hobblechain Rhyolite|40691|5|Briefly described|p11|||Mention Fig.4||||||
8388|Hobblechain Rhyolite|41721|3|Fully described|p25|||Of the Tawallah Group. Conformably overlies Gold Creek Volcanics; overlain by McArthur Group. Porphyrytic rhyolite. Geological province: McArthur Basin.||||||18-FEB-08
8388|Hobblechain Rhyolite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
8388|Hobblechain Rhyolite|41957|6|Mentioned|p68|||||||||
8388|Hobblechain Rhyolite|42385|5|Briefly described|p14|||||||||
8388|Hobblechain Rhyolite|42639|6|Mentioned|p17|||Calvert Hills, Robinson River||||||
8388|Hobblechain Rhyolite|42812|5|Briefly described|p27, Fig.5|||||||||
8388|Hobblechain Rhyolite|42873|5|Briefly described|Fig.1, P110|||||||||
8388|Hobblechain Rhyolite|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
8388|Hobblechain Rhyolite|43036|6|Mentioned|Fig.5|||||||||
8388|Hobblechain Rhyolite|43715|6|Mentioned|p27|||||||||
8388|Hobblechain Rhyolite|44112|6|Mentioned|p43|||||||||
8388|Hobblechain Rhyolite|44436|5|Briefly described|p.10|||(E53-4).||||||02-DEC-04
8388|Hobblechain Rhyolite|45162|2|Defined|p43|||||||||
8388|Hobblechain Rhyolite|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin. Age: 1725 +/- 2Ma (Shrimp).||||||07-NOV-08
8388|Hobblechain Rhyolite|60483|5|Briefly described|p7 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1725+/-2Ma. Geological Province: McArthur Basin.||||||07-NOV-08
8388|Hobblechain Rhyolite|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Underlain by Gold Creek Volcanics.||||||03-JUN-09
8388|Hobblechain Rhyolite|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Intrudes the Pungalina Member.||||||07-NOV-08
8388|Hobblechain Rhyolite|63112|6|Mentioned|p1192 Tb.1|||Calvert Superbasin. May have been fed by a fissure feeder of Packsaddle Microgranite. <100 m thick.|1725 +/- 2 Ma.||||Porphyritic rhyolite with quartz phenocrysts and micropoikilitic texture.|
8388|Hobblechain Rhyolite|63866|5|Briefly described|p54|||||Prize Supersequence||||
8388|Hobblechain Rhyolite|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1725 +/- 2 Ma.|||||
8388|Hobblechain Rhyolite|64817|6|Mentioned|p353 Fig.4, p355 Fig.5|Statherian|Statherian||1725 +/- 2 Ma.|Of the Tawallah Group.||||
8388|Hobblechain Rhyolite|65228|5|Briefly described|p22, p25, Figs.02, 06, 07, 10.|Statherian|Statherian|McArthur Basin. Felsic.|1725 +/- 2 Ma.|Unit in Tawallah Group.||Overlies Gold Creek Volcanics. Is overlain by Pungalina Member.||
8388|Hobblechain Rhyolite|65337|6|Mentioned|p15, p17.|||Southeastern McArthur Basin.|c.1725 Ma.|||||
8388|Hobblechain Rhyolite|65340|4|Described|p11, p.13 Table 4, pp39-46, p52, p69.|||Named by Yates (1963); included adjacent epiclastic deposits which are now considered part of Pungalina Member of Echo Sandstone. Consistent 70 - 100 m thickness. Mineralogy, microstructure, fabric and contact relationships are described in detail. Hosts Cu mineralisation in chlorite-altered rhyolite breccia at Camel Creek.|1725 +/- 2 Ma (Page and Sweet 1998).|Unit in Tawallah Group.||Disconformably overlies Gold Creek Volcanics. Contiguous and co-magmatic with Packsaddle Microgranite. Is overlain by Upper Pungalina Member.|Pink, porphyritic (K-feldspar-quartz), massive to flow-banded, spherulitic to microgranophyric rhyolite with local lithophysae, autobreccia, peperite and chlorite alteration.|
8388|Hobblechain Rhyolite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.||Tawallah Group|||Rhyolite, reddish brown, porphyritic.|
8388|Hobblechain Rhyolite|67352|6|Mentioned|p14  Tb.2|||||||Is overlain unconformably by Masterton Sandstone.||
8388|Hobblechain Rhyolite|69430|4|Described|p15:3, 9-10, 12, 48|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin. 70-100m thick. Lava flow with talus-lined margin. Comagmatic with Packsaddle Microgranite. A typographical error in 15:10 has the age at 1752 +/- 2 Ma.|1725 +/- 2 Ma (Page and Sweet, 1998).|Tawallah Group.||Disconformably overlies Gold Creek Volcanics. Is overlain conformably by Pungalina Member (Warramana Sandstone).|Pink, porphyritic (K-feldspar-quartz), massive to flow-banded, spherulitic to microgranophyric rhyolite.|12-JUL-16
8388|Hobblechain Rhyolite|69591|5|Briefly described|p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of Tawallah Supersequence. Subaerial (?) deposits.||Tawallah Group.|||Reddish-brown, porphyritic rhyolite.|
8388|Hobblechain Rhyolite|69673|5|Briefly described|p16 fig 13, p17 fig 14||||1725 Ma|Tawallah Group||Overlain by Pungalina Member, Warramana Sandstone, overlies Gold Creek Volcanics|Rhyolite.|
8388|Hobblechain Rhyolite|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Gold Creek Volcanics. Is overlain by Masterton Sandstone (McArthur Group).|Reddish-brown, porphyritic rhyolite.|
8388|Hobblechain Rhyolite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1725+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
8388|Hobblechain Rhyolite|71606|5|Briefly described|p135,137|||McArthur Basin. SHRIMP data givers 1710-1700 Ma age, associated with Fagan Phase magmatism of Rawlings 1994.||Unit of Tawallah Group.||Hosted in the uppermost Tawallah Group.||
8388|Hobblechain Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age.|1725 +/-2 Ma|Tawallah Group||Overlies Gold Creek Volcanics and is partially laterally equivalent to Pungalina Member and Warramana Sandstone.||
8388|Hobblechain Rhyolite|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin.|1725 +/- [?] Ma|Tawallah Group||Underlaing by Gold Creek Volcanics. Partly overlain by Warramana Sandstone[?] and Pungalina Member. Equivalent to Packsaddle Microgranite.||
8388|Hobblechain Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age given.|1725 +/- 2 Ma|Tawallah Group||Overlies Gold Creek Volcanics and is laterally equivalent to Pungalina Member.||
8388|Hobblechain Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1725 +/- 2 Ma (see Fig.1.2)|Tawallah Group||Underlain by Gold Creek Volcanics. Overlain by Echo Sandstone.||
8388|Hobblechain Rhyolite|73083|6|Mentioned|p40|||||||||
8395|Hobwee Basalt|22773|5|Briefly described|p345|||||||||
8395|Hobwee Basalt|22857|5|Briefly described|p345|Cenozoic|Cenozoic|Included in the central-volcano provinces of NSW. Max. thickness: 600m. ||||||19-NOV-08
8395|Hobwee Basalt|30604|6|Mentioned|p66|||||||||
8395|Hobwee Basalt|30687|4|Described|p65|||See also P67,68,76. Tertiary age||||||
8395|Hobwee Basalt|30689|5|Briefly described|p76|||Also mention P73||||||
8395|Hobwee Basalt|31130|6|Mentioned|Fig. 2|||L. Miocene||||||
8395|Hobwee Basalt|32924|4|Described|p112|||Tholeiitic. Thickest N. of Mt. Warning||||||
8395|Hobwee Basalt|33290|4|Described|p38|||Anal. P39||||||
8395|Hobwee Basalt|35296|5|Briefly described|p14|||See also P12.||||||
8395|Hobwee Basalt|36806|6|Mentioned|p131|||||||||
8395|Hobwee Basalt|39445|5|Briefly described|Table 14|||||||||
8395|Hobwee Basalt|40623|5|Briefly described|p39|||||||||
8395|Hobwee Basalt|40896|4|Described|p9|||||||||
8395|Hobwee Basalt|43161|4|Described|13, 14|||Dated: 20.5 to 23.5 Ma||||||
8395|Hobwee Basalt|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
8395|Hobwee Basalt|44813|14|Not recorded|p80||Tertiary|||||||
8395|Hobwee Basalt|44818|6|Mentioned|p275|||||||||
8395|Hobwee Basalt|44871|2|Defined|p141,map|||||||||
8395|Hobwee Basalt|48917|6|Mentioned|p38|||One map symbol for all units of Lamington Volcanics||||||
8395|Hobwee Basalt|69599|5|Briefly described|p640|||Northern side of the Tweed volcano, centred on Mount Warning.|23.6 +/- 0.4 Ma (Knesel et al., 2008)..|||Approximate equivalent of Blue Knob Basalt in NSW.||
8395|Hobwee Basalt|73450|6|Mentioned|p99-100|||Associated with the Tweed Volcano. Up to 600 m thick.|||||Basaltic lavas.|
8395|Hobwee Basalt|73581|5|Briefly described|p6|||Tweed Volcano. Overlies Springbrook Rhyolite to the north/Nimbin Rhyolite to the south.||Lamington Volcanics, top|||Olivine-bearing basalt.|
8404|Hodgkinson Formation|12575|5|Briefly described|p780, p784 Table 1.|Late Devonian|Emsian|Hodgkinson Province. Strongly folded, faulted and intruded by granites in late Devonian, with widespread rhyolitic ignimbritic cauldron volcanism in Late Carboniferous to Permian. Apatite fission track analyses are detailed.|420-363 Ma.||||Thick succession of deep-water turbiditic sandstone and mudstone.|
8404|Hodgkinson Formation|22497|4|Described|p108|||||||||
8404|Hodgkinson Formation|22811|6|Mentioned|p606|||of Hodgkinson Province, Age of unit ~400 Ma||||||
8404|Hodgkinson Formation|23076|5|Briefly described|p724|Devonian|Devonian|||||||
8404|Hodgkinson Formation|23086|5|Briefly described|p664|Devonian|Devonian|||||||
8404|Hodgkinson Formation|23422|5|Briefly described|p168|||||||||
8404|Hodgkinson Formation|23423|4|Described|p301 Table 7.2|Late Devonian|Late Silurian|Intruded by Cannibal Creek Granite.  Underlying unit Chillagoe Formation - unconformable.  Hodgkinson Province.||||||
8404|Hodgkinson Formation|23424|5|Briefly described|p346|||Hodgkinson Province.||||||
8404|Hodgkinson Formation|23426|5|Briefly described|p400|||Hodgkinson Province.||||||
8404|Hodgkinson Formation|23427|6|Mentioned|p411|||||||||
8404|Hodgkinson Formation|23430|4|Described|p471-473|||Intruded by late Palaeozoic granite plutons. Hodgkinson Province.||||||
8404|Hodgkinson Formation|23431|5|Briefly described|p539|||||||||
8404|Hodgkinson Formation|23446|6|Mentioned|p447|||||||||
8404|Hodgkinson Formation|23497|5|Briefly described|Table 1||Devonian|of Hodgkinson Province. Faulted against Barnard Metamorphics and Mission Beach Granite Complex.||||||
8404|Hodgkinson Formation|23500|6|Mentioned|Map legend|Early Devonian||Age: Late Silurian? - Early Devonian. Hodgkinson Province.||||||
8404|Hodgkinson Formation|23501|5|Briefly described|map legend|Devonian||Age: Late Silurian? - Devonian.||||||
8404|Hodgkinson Formation|23502|5|Briefly described|Map Legend|Devonian|Late Silurian|Age: Late Silurian? - Devonian.||||||
8404|Hodgkinson Formation|23503|5|Briefly described|Map Legend|Devonian|Late Silurian|||||||
8404|Hodgkinson Formation|23506|5|Briefly described|Map Legend||Devonian|||||||
8404|Hodgkinson Formation|23507|5|Briefly described|Map Legend|Late Devonian|Late Silurian|||||||
8404|Hodgkinson Formation|23511|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
8404|Hodgkinson Formation|23512|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
8404|Hodgkinson Formation|23522|5|Briefly described|p250 Fig 6|Early Carboniferous|Pragian|||||||
8404|Hodgkinson Formation|23616|4|Described|Table 1C p13, p32-36|Late Devonian|Early Devonian|Age: late Early Devonian to Late Devonian; lower age limit determined by conodont age dating of the underlying Chillagoe Fm. Upper age limit constrained by intrusion of Carboniferous granitoids. Hodgkinson Province.||||||
8404|Hodgkinson Formation|23617|6|Mentioned|p26|||||||||
8404|Hodgkinson Formation|23624|3|Fully described|p7, p24|Early Devonian|Early Devonian|Previously included in the Mount Garnet Formation on the Atherton 1:250 000 geological map (1st. ed.). Geological Province: Gurrumba Ring Complex.||||||31-MAR-15
8404|Hodgkinson Formation|23713|4|Described|p14-15|Early Carboniferous|Early Devonian|Consists of Kitoba Member and OK Member. Hodgkinson Province.||||||
8404|Hodgkinson Formation|24080|5|Briefly described|p445 Fig. 4|Carboniferous|Devonian|Greywacke, slate, shale, volcanics.  Geological Province: Laura Basin.||||||
8404|Hodgkinson Formation|24086|5|Briefly described|p314|Early Devonian|Late Silurian| Geological Province: Hodgkinson Basin.||||||
8404|Hodgkinson Formation|24213|5|Briefly described|p777|Devonian|Silurian|Intruded by the Whypalla Supersuite.  Geological Province: Hodgkinson Province||||||
8404|Hodgkinson Formation|24393|5|Briefly described|p147, p148 Fig. 4|Late Devonian|Late Silurian|||||||
8404|Hodgkinson Formation|24485|5|Briefly described|p26|||Geological Province: Hodgkinson Province||||||
8404|Hodgkinson Formation|24486|5|Briefly described|Map legend|Devonian|Late Silurian|Contains the Kitoba Member.  Geological Province: Hodgkinson Province.||||||
8404|Hodgkinson Formation|24612|5|Briefly described|p12|Early Devonian|Early Devonian|Contains Carlinastraea fauna.||||||20-DEC-04
8404|Hodgkinson Formation|29605|6|Mentioned|Table 1|||||||||
8404|Hodgkinson Formation|29795|6|Mentioned|p271|||||||||
8404|Hodgkinson Formation|29803|6|Mentioned|p557|||||||||
8404|Hodgkinson Formation|29815|6|Mentioned|p993|||||||||
8404|Hodgkinson Formation|29820|6|Mentioned|p449|||||||||
8404|Hodgkinson Formation|30505|4|Described|p3|||Silurian-Devonian age. See also p4,6,7,15.||||||23-APR-18
8404|Hodgkinson Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
8404|Hodgkinson Formation|31184|6|Mentioned|p127|||||||||
8404|Hodgkinson Formation|31435|6|Mentioned|p13|||||||||
8404|Hodgkinson Formation|31676|6|Mentioned|p3|||||||||
8404|Hodgkinson Formation|31822|6|Mentioned|p68|||||||||
8404|Hodgkinson Formation|31832|6|Mentioned|p29|||See also Table 6||||||
8404|Hodgkinson Formation|31999|5|Briefly described|p44|||Table 11||||||
8404|Hodgkinson Formation|32359|5|Briefly described|p731|||||||||
8404|Hodgkinson Formation|32360|6|Mentioned|p740|||||||||
8404|Hodgkinson Formation|32619|6|Mentioned|p464|||Einsian - Eifelian||||||
8404|Hodgkinson Formation|32633|5|Briefly described|p439|||||||||
8404|Hodgkinson Formation|32634|6|Mentioned|p29|||Dev. - Carb.||||||
8404|Hodgkinson Formation|32654|6|Mentioned|p95|||Mid. - U.Dev.||||||
8404|Hodgkinson Formation|32655|6|Mentioned|p760|||||||||
8404|Hodgkinson Formation|32665|5|Briefly described|p763|||||||||
8404|Hodgkinson Formation|32865|6|Mentioned|p477|||Late Dev. or early Carb.||||||
8404|Hodgkinson Formation|33205|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
8404|Hodgkinson Formation|33303|6|Mentioned|PB28|||||||||
8404|Hodgkinson Formation|33326|6|Mentioned|p449|||Fauna.||||||
8404|Hodgkinson Formation|33777|4|Described|p31|||See also Fig.1||||||
8404|Hodgkinson Formation|33880|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Middle - Upper Devonian||||||
8404|Hodgkinson Formation|33963|6|Mentioned|Map legend|Devonian|Silurian|Sil. - Dev.||||||
8404|Hodgkinson Formation|34046|6|Mentioned|Table 1|||Middle Dev.||||||
8404|Hodgkinson Formation|34826|6|Mentioned|p29|||Location of Mount Carbine Wolframite Mine.||||||
8404|Hodgkinson Formation|35000|6|Mentioned|p138|||||||||
8404|Hodgkinson Formation|35006|6|Mentioned|p278|||||||||
8404|Hodgkinson Formation|35008|5|Briefly described|p180|||||||||
8404|Hodgkinson Formation|35946|6|Mentioned|p28|||||||||
8404|Hodgkinson Formation|36353|6|Mentioned|p355|||||||||
8404|Hodgkinson Formation|36527|6|Mentioned|p157|||||||||
8404|Hodgkinson Formation|36563|6|Mentioned|Table 1|||||||||
8404|Hodgkinson Formation|37098|6|Mentioned|p253|||||||||
8404|Hodgkinson Formation|37565|6|Mentioned|Fig.6|||||||||
8404|Hodgkinson Formation|37574|6|Mentioned|Fig.6|||||||||
8404|Hodgkinson Formation|37575|3|Fully described|p177|||See also p183 and Fig.2||||||23-APR-18
8404|Hodgkinson Formation|37609|6|Mentioned|p309|||||||||
8404|Hodgkinson Formation|37721|6|Mentioned|p1|||||||||
8404|Hodgkinson Formation|37727|4|Described|p63|||See also p22 and p34.||||||23-APR-18
8404|Hodgkinson Formation|39278|6|Mentioned|p359|||||||||
8404|Hodgkinson Formation|39445|5|Briefly described|p74|||Mid-Late Devonian. 4 generations of folding. See also P84 & Tables 5 & 6||||||
8404|Hodgkinson Formation|39564|6|Mentioned|p9|||||||||
8404|Hodgkinson Formation|39650|6|Mentioned|p37|||||||||
8404|Hodgkinson Formation|39689|6|Mentioned|p54|||See also p63.||||||
8404|Hodgkinson Formation|39845|6|Mentioned|p24|||||||||
8404|Hodgkinson Formation|39998|6|Mentioned|p188|||||||||
8404|Hodgkinson Formation|40049|6|Mentioned|Fig.2|||||||||
8404|Hodgkinson Formation|40076|6|Mentioned|p42|||||||||
8404|Hodgkinson Formation|40277|6|Mentioned|p293|||||||||
8404|Hodgkinson Formation|40278|6|Mentioned|p645|||||||||
8404|Hodgkinson Formation|40623|5|Briefly described|p87|||||||||
8404|Hodgkinson Formation|40743|5|Briefly described|p310|||||||||
8404|Hodgkinson Formation|40787|5|Briefly described|p330|||||||||
8404|Hodgkinson Formation|40892|6|Mentioned|p74|||||||||
8404|Hodgkinson Formation|40918|5|Briefly described|p101|||||||||
8404|Hodgkinson Formation|40944|6|Mentioned|p187|||||||||
8404|Hodgkinson Formation|41272|4|Described|M 1of1 G02|||||||||
8404|Hodgkinson Formation|41297|6|Mentioned|Fig.1|||||||||
8404|Hodgkinson Formation|41425|4|Described|p19|||||||||
8404|Hodgkinson Formation|41470|5|Briefly described|p1171|||||||||
8404|Hodgkinson Formation|41569|6|Mentioned|p71|||||||||
8404|Hodgkinson Formation|41639|6|Mentioned|p8|||||||||
8404|Hodgkinson Formation|41772|4|Described|p435|||||||||
8404|Hodgkinson Formation|41775|6|Mentioned|p71|||||||||
8404|Hodgkinson Formation|41981|4|Described|p1855|||||||||
8404|Hodgkinson Formation|42031|4|Described|p576|||||||||
8404|Hodgkinson Formation|42063|5|Briefly described|p313|||See also Fig.2||||||
8404|Hodgkinson Formation|42304|2|Defined|p6|Late Devonian|Devonian|||||||
8404|Hodgkinson Formation|42369|4|Described|p19-39|||||||||
8404|Hodgkinson Formation|42474|5|Briefly described|p27|||Cooktown 1:100 000 sheet||||||
8404|Hodgkinson Formation|42490|3|Fully described|p11|||||||||
8404|Hodgkinson Formation|42500|5|Briefly described|p12|||||||||
8404|Hodgkinson Formation|42532|5|Briefly described|p303|||||||||
8404|Hodgkinson Formation|42620|2|Defined|p80|Late Devonian|Early Devonian|||||||
8404|Hodgkinson Formation|42625|5|Briefly described|Map legend|Devonian|Silurian|||||||
8404|Hodgkinson Formation|42632|6|Mentioned|p9|||||||||
8404|Hodgkinson Formation|42658|3|Fully described|p17|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|42670|5|Briefly described|Figure 1 P26|||||||||
8404|Hodgkinson Formation|42681|3|Fully described|p14|||||||||
8404|Hodgkinson Formation|42810|3|Fully described|Table 1 P17|Late Devonian|Late Silurian|see also p11.||||||23-APR-18
8404|Hodgkinson Formation|42874|6|Mentioned|Fig.1, P116|||||||||
8404|Hodgkinson Formation|43060|3|Fully described|p44,Table 1c|Early Carboniferous|Early Devonian|||||||
8404|Hodgkinson Formation|43070|5|Briefly described|p7|||see also Fig.1||||||
8404|Hodgkinson Formation|43083|3|Fully described|p51, p53 Tb. 5|Early Carboniferous|Late Silurian|Comprises Larramore Metabasalt, OK and Kitoba Members. Geological province: Hodgkinson Province.||||||17-JUN-09
8404|Hodgkinson Formation|43087|5|Briefly described|Fig.3|||||||||
8404|Hodgkinson Formation|43098|1|Redefined|p12|Early Carboniferous|Late Silurian|||||||
8404|Hodgkinson Formation|43111|5|Briefly described|p29|||||||||
8404|Hodgkinson Formation|43124|6|Mentioned|p28|||||||||
8404|Hodgkinson Formation|43151|5|Briefly described|Map legend|||Includes the Kitoba Member.  Early Devonian - Late Silurian? in age.||||||15-JUN-06
8404|Hodgkinson Formation|43254|5|Briefly described|map legend|Late Devonian|Late Silurian|Hodgkinson Province.||||||
8404|Hodgkinson Formation|43285|5|Briefly described|Map Legend|||age Late Silurian? to Late Devonian?||||||
8404|Hodgkinson Formation|43461|14|Not recorded|p615,table p618||Couvinian|(Devonian)||||||
8404|Hodgkinson Formation|43625|3|Fully described|p19,25||Devonian|||||||
8404|Hodgkinson Formation|43626|6|Mentioned|p10|||||||||
8404|Hodgkinson Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
8404|Hodgkinson Formation|43896|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|43897|14|Not recorded|p91-2,97-8|Late Devonian|Middle Devonian|Flysch deposits.||||||
8404|Hodgkinson Formation|43898|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|43901|14|Not recorded|Map Legend|Middle Devonian||Early Carboniferous? - Middle Devonian||||||
8404|Hodgkinson Formation|43902|14|Not recorded|p119|Carboniferous|Devonian|||||||
8404|Hodgkinson Formation|43904|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|43927|14|Not recorded|p5,10,16|||||||||
8404|Hodgkinson Formation|43967|14|Not recorded|p73,75|||Quartz keratophyre sills present.||||||
8404|Hodgkinson Formation|43979|14|Not recorded|p65-68|Early Carboniferous|Middle Devonian|M.Dev-?E.Carb.||||||
8404|Hodgkinson Formation|44024|14|Not recorded|p73,75|||||||||
8404|Hodgkinson Formation|44068|2|Defined|p7|||||||||
8404|Hodgkinson Formation|44091|14|Not recorded|p31,40|Late Devonian|Middle Devonian|Carb?||||||
8404|Hodgkinson Formation|44207|14|Not recorded|p115|||||||||
8404|Hodgkinson Formation|44246|5|Briefly described|Map Legend||Devonian|||||||
8404|Hodgkinson Formation|44258|14|Not recorded|p4,32-34|Early Carboniferous|Late Devonian|||||||
8404|Hodgkinson Formation|44267|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|44292|2|Defined|p7-9,13-15,18-9,map|||Tb.1||||||
8404|Hodgkinson Formation|44293|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|44294|2|Defined|Tb.2,p10-2,15,17-18,|||p22,26,map||||||
8404|Hodgkinson Formation|44296|14|Not recorded|Map Legend|Early Carboniferous|Middle Devonian|||||||
8404|Hodgkinson Formation|44329|14|Not recorded|p5,9|||See also Lexicon.||||||
8404|Hodgkinson Formation|44425|14|Not recorded|p7-28,map|||Now includes Barron River Metamorphics.||||||
8404|Hodgkinson Formation|44520|14|Not recorded|p130|||||||||
8404|Hodgkinson Formation|44560|14|Not recorded|p359|||||||||
8404|Hodgkinson Formation|44880|14|Not recorded|unknown (p195-208)|||||||||
8404|Hodgkinson Formation|44883|14|Not recorded|p111,131|||||||||
8404|Hodgkinson Formation|45008|14|Not recorded|p11,25-28,46,50,113,|Late Devonian|Middle Devonian|Plant fossils,corals. Maps.||||||
8404|Hodgkinson Formation|45025|2|Defined|p38,43-46||Paleozoic|Chemical analysis, palaeontology and age.||||||07-NOV-08
8404|Hodgkinson Formation|45065|4|Described|Table 4|||||||||
8404|Hodgkinson Formation|45087|5|Briefly described|p188|||Chemical analyses||||||
8404|Hodgkinson Formation|45113|6|Mentioned|p11|||||||||
8404|Hodgkinson Formation|46845|6|Mentioned|p143|||||||||
8404|Hodgkinson Formation|46879|6|Mentioned|p173|||||||||
8404|Hodgkinson Formation|48764|6|Mentioned|p112|||||||||
8404|Hodgkinson Formation|48850|14|Not recorded|Pls.9-12|||||||||
8404|Hodgkinson Formation|48976|4|Described|p2|||See also p75.||||||23-APR-18
8404|Hodgkinson Formation|50316|5|Briefly described|Map Legend|Devonian|Late Silurian|Geological Province: Hodgkinson Province.||||||
8404|Hodgkinson Formation|50335|5|Briefly described|Map Lagend|Late Devonian|Late Silurian|Geological Province: Hodgkinson Province||||||11-JUN-04
8404|Hodgkinson Formation|50387|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Hodgkinson Province||||||
8404|Hodgkinson Formation|50587|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Hodgkinson Province. Arenite, siltstone, mudstone, chert, shale, melange.||||||28-JUN-04
8404|Hodgkinson Formation|50596|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Greywacke, mudstone, limestone, chert, siltstone, metabasalt.||||||
8404|Hodgkinson Formation|50630|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Mount Walker Member.||||||
8404|Hodgkinson Formation|60087|5|Briefly described|Map legend|Early Carboniferous|Middle Devonian|Greywacke, sandstone, silty mudstone, limestone, chert lenses.||||||
8404|Hodgkinson Formation|60357|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Geological Province: Hodgkinson Province. Includes: Larramore Metabasalt Member, OK Member, Kitoba Member.||||||
8404|Hodgkinson Formation|60358|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Includes Larramore Metabasalt Member. Meta arenite, arenite, phyllitic mudstone, mudstone, minor chert, metabasalt, conglomerate, metasiltstone. Geological Province: Hodgkinson Province.||||||18-AUG-04
8404|Hodgkinson Formation|60425|3|Fully described|p6, p16 tb. 1, p24-25|Late Devonian|Early Devonian|Includes Kitoba, OK and Larramore Metabasalt Members. Several thousand metres thick. Geol.prov: Hodgkinson Province. Deep water marine siliciclastic/turbidity-currents deposits for which a detailed lithology is included. Sparsely fossiliferous.||||||07-FEB-11
8404|Hodgkinson Formation|61527|5|Briefly described|p789, p790|||Thick, monotonous succession of turbiditic greywacke-siltstone-shale, slate, minor volcanics, conglomerate, chert and rare limestone of deep-marine origin. Geological Province: Hodgkinson Province.||||||
8404|Hodgkinson Formation|61763|5|Briefly described|p28|Devonian|Devonian|Includes shallow water limestone and basic volcanics. Geological Province: New England Orogen.||||||
8404|Hodgkinson Formation|62371|5|Briefly described|p470 Fig.1|Devonian|Devonian|Includes lower greenschist facies metasedimentary rocks. Hosts the Hodgkinson Goldfield. Geological Province: Hodgkinson Province. See also p472 Fig.3||||||
8404|Hodgkinson Formation|62523|6|Mentioned|p7, p8|||Refers to arenite deposits within the Hodgkinson Formation.||||||07-FEB-11
8404|Hodgkinson Formation|63140|4|Described|p569-583.|Carboniferous|Devonian|The mafic units are mostly part of structurally disrupted thrust packages; almost exclusively occur as fault-bounded units. Some host massive sulphide deposits, eg King Vol. Major, trace and REE geochemistry are detailed. Asthenosphere-sourced basalts.|c.555 Ma.||Includes Larramore Metabasalt Member.||Basalt and basaltic andesite, metamorphosed, fine-grained, occasionally pillowed and brecciated; interspersed with mature deep-marine flysch-type sedimentary rocks.|
8404|Hodgkinson Formation|63154|5|Briefly described|p281 Fig. 3|Devonian|Devonian|Geological province: Hodgkinson Province. Mainly deep marine sediments.||||||11-APR-07
8404|Hodgkinson Formation|64665|6|Mentioned|p56. |Devonian|Devonian|Part of the basement to the Ngarrabullan Basin.||||||
8404|Hodgkinson Formation|65214|6|Mentioned|p279, p283|Devonian|Devonian|QLD, Hodgkinson. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
8404|Hodgkinson Formation|66180|5|Briefly described|pp279-282, p287|Early Devonian|Late Silurian|Intruded by Carboniferous to Devonian granitoids.||||Underlies the Walsh Bluff Volcanics.|Weakly metamorphosed turbidite sequences with minor occurrences of mafic volcanics.|10-MAY-12
8404|Hodgkinson Formation|66852|5|Briefly described|pp937-939.|Devonian|Silurian|Shows a prominent meridional structural grain. Cut by swarms of WNW-ESE faults marked by resistant subvertical zones of milky quartz, or swarms of quartz veins. Total wrench displacement was not large; very small across individual faults.|||Includes Larramore Metabasalt Member.|||
8404|Hodgkinson Formation|68330|5|Briefly described|Map legend.|Devonian|Late Silurian|Hodgkinson Province. Three facies associations are mapped separately.|||||Grey to brown, fine to medium-grained labile and feldspathic arenite, siltstone, mudstone, minor chert, conglomerate, arenite and calc-silicate rocks; hornfelsed/metasomatised arenite and mudstone; interbedded sandstone and siltstone/mudstone.|
8404|Hodgkinson Formation|68331|5|Briefly described|Map legend.|Devonian|Late Silurian|Hodgkinson Province. Three facies associations are mapped separately.|||||Grey to brown, fine to medium-grained labile and feldspathic arenite, siltstone, mudstone, minor chert, conglomerate, arenite and calc-silicate rocks; hornfelsed/metasomatised arenite and mudstone; interbedded sandstone and siltstone/mudstone.|
8404|Hodgkinson Formation|68337|5|Briefly described|Map legend|Devonian|Late Silurian?|Three facies associations are mapped separately.|||||Rhythmically interbedded labile arenite and medium-bedded siltstone; labile arenite with subordinate mudstone and siltstone; dark grey, thick-bedded pebble to boulder conglomerate, conglomeratic arenite.|
8404|Hodgkinson Formation|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Hodgkinson Province.||||||
8404|Hodgkinson Formation|68576|4|Described|Q_11: p2-9, p12-13|Late Devonian|Late Silurian|Very extensive distribution: 150 km E-W and over 300 km N-S. Bedrock in the Cairns region and forms Macalister Range, N of Cairns; also several large ridges, buttressed by swarms of felsic dykes, on the road to Dimbulah. Deposited by gravity flows building deep-sea fans. Fossils rare, hence poorly dated. Poly-deformed (melange) by shortening in the Carboniferous and Permian. Lithologies and deformation/structures described in detail. Hosts the Hodgkinson gold field (Tyrconnel mine) in gold-quartz and gold-stibnite veins.||||Is intruded by Mount Formartine Granite.|Folded and cleaved metasedimentary rocks: sandstone and mudstone in subequal but variable proportions (commonly as Bouma sequences), with minor redeposited conglomerate, basalt and chert and rare limestone lenses.|
8404|Hodgkinson Formation|68731|5|Briefly described|p115, p159, p162, p163, p163 Fig 3.76||Late Devonian|Hodgkinson Province. Age poorly constrained; however, unpublished U-Pb detrital zircon (LA-ICP-MS) data indicate maximum depositional ages of [Wenlock (Silurian, ~ 430 Ma) and] Mississippian (~360 Ma).|< 360 Ma, U-Pb detrital zircon (LA-ICP-MS)|||||10-MAY-16
8404|Hodgkinson Formation|68822|5|Briefly described|p320 Fig.3, p349|Late Devonian|Middle Devonian|Hodgkinson Province.|||||Siltstone.|27-JUL-15
8404|Hodgkinson Formation|69030|5|Briefly described|p2-3, p6, p11, p14, p17|Late Devonian|Late Silurian|Hodgkinson Province. Gravity modelling briefly discussed. Hosts significant gold mineralisation.|||Kitoba, OK Members.||Deep-marine sedimentary rocks (commonly turbidites).|
8404|Hodgkinson Formation|69079|5|Briefly described|p3-4, p6, p8, p12, p20, p24-27, p40, p42|||See also p48-50, p52, p55-57, p59. Hodgkinson Province. Hosts gold-antimony mineralisation in quartz veins. Numerous deposits described in some detail.|||||Metasedimentary rocks including coarse- to medium-grained arenite or greywacke and carbonaceous slaty mudstone, with interspersed lenses of chert and melange zones.|
8404|Hodgkinson Formation|69582|5|Briefly described|p70, p73|Devonian|Devonian|Hodgkinson Province. Metasediments of this unit have high thermal conductivity and are thus unlikely to retain heat generated by the intruding Whypalla Supersuite. Rocks of this formation are steeply dipping. Intersected in GSQ Mossman 2-3R.||||Overlies the Chillagoe Formation. Intruded by the Whypalla Supersuite.|Metasedimentary rocks including metasandstone, siltstone and mudstone.|
8404|Hodgkinson Formation|69592|4|Described|p230, p231 Fig.4.4, p232-233, p235-243|Devonian|Silurian|See also p245-249 Figs.4.22-33, p297, p302-303. Mossman Orogen, Palmer-Barron Subprovince, Hodgkinson Province. Remarkably uniform over its 40,000 km2 outcrop area. Turbidite sediments deposited in deep-sea fans. Lithologies described in some detail. Sparsely fossiliferous. Geochemical plots. Complex internal structure; steeply-dipping strata young to the W; photographs and diagrams of deformation. Backarc depositional model discussed in detail. Poor age control (discussed); intruded c.357 Ma. Detrital zircon provenances treated in great detail.|||Kitoba, OK, Larramore Metabasalt, Members.|Is overlain unconformably by Silver Valley Conglomerate. Is intruded by Mount Formartine Supersuite.|Sandstone (quartz-intermediate greywacke), siltstone and mudstone interlayers locally >100m are characteristic; subordinate stratiform chert, massive mafic volcanic flows and conglomerate layers; rare limestone, one small ultramafic body.|
8404|Hodgkinson Formation|69599|6|Mentioned|p610|Devonian|Devonian|Correlated with deformed metasediments in basement of the western Queensland Plateau.||||||
8404|Hodgkinson Formation|70033|4|Described|p5, p51, p52 Fig 8.1, p56, p60-61|Early Carboniferous||Hodgkinson Province. Min age: Kositcin et al. in prep. Age shown in map legend (Fig 8.1) as Late Silurian? - Early Carboniferous.||||Is intruded by Mount Formartine Granite; is in faulted contact to the east with Barnard Metamorphics.||
8404|Hodgkinson Formation|70207|5|Briefly described|p3-5, p11, p45, p49, p59, p74, p94, p96|Early Carboniferous||See particularly p101-124. Eastern Hodgkinson Province, Mossman Orogen. Tectonic models discussed. Three sandstone maximum depositional age determinations and spectra discussed (Kositcin et al., 2015). Maximum age given as Late Silurian?.|373.7+/-4.0 Ma; 345.3+/-2.6 Ma; 342.4+/-6.2 Ma .|||Is overlain unconformably by Dalrymple Sandstone. Is intruded by Emerald Creek Microgranite and Mount Formartine Granite.|Includes phyllitic to schistose metasedimentary rocks including thick-bedded sandstones and scarce very thin beds of black carbonaceous mudstone.|
8404|Hodgkinson Formation|70345|4|Described|p1, p3-7, p13-18, p22-26, p30|Carboniferous|Silurian|Mossman Orogen. The sole component of the Palmer-Barron Subprovince of the Hodgkinson Province. Dominated by turbidity current deposits and is the most extensive unit in the Hodgkinson province forming a belt at least 400km long and up to 150 km wide. Ages provided are SHRIMP U-Pb maximum depositional ages. Exposed in the eastern bank of Limestone Creek. Petrography, zircon morphology, SHRIMP analyses and results are discussed. Additional SHRIMP ages include 396 +/- 8 Ma (max dep age); 377 +/- 5 Ma (max dep); 370 +/- 3 Ma; 374 +/- 7 Ma. See also , p32-35, p37-43, p45-50, p52-56, p58, p60-64.|374 +/- 7 Ma; 405 +/- 6 Ma (max dep age)||Includes the Kitoba Member and the OK Member.|Faulted against the Chillagoe Formation.|Thick, dark-grey sandstone with scattered grains of detrital muscovite.|
8404|Hodgkinson Formation|70673|4|Described|p4, p6-7, p10, p83-115|Early Carboniferous|Late Silurian?|Mossman Orogen, Hodgkinson Province. Mainly turbidity current deposits. Various detrital zircon ages and provenance possibilities discussed.|412.0 +/- 3.3 Ma; 378 +7/-4 Ma; 366 +/- 16 Ma|||Is intruded by Mount Formartine Granite.|Sandstone, conglomerate, lesser mudstone.|
8404|Hodgkinson Formation|71031|5|Briefly described|p70-p71, p73|Early Carboniferous|Late Silurian|Included in the Mossman Orogen by Henderson and Donchak (2013).|||Includes the Kitoba Member.||Quartzofeldspathic sandstone.|
8404|Hodgkinson Formation|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen. Over 30 age determinations (provenance clusters and maximum depositional ages) are given within this range; (all U-Pb zircon SHRIMP).|2587+/-10 Ma to 366+/-16 Ma.||||Sandstone.|
8404|Hodgkinson Formation|72297|5|Briefly described|p697, p718, p726, p728, p757, p759|Devonian|Devonian|Basement to the unconformably-overlying, coal-bearing Ngarrabullgan Basin. Hosts the significant Watershed tungsten skarn deposit: disseminated scheelite in quartz vein swarms in stratabound replacement lenses in calc-silicate rocks, and in dyke-like intrusions of albitised granite. Minor sandstone and slate for pavers is produced at the River of Gold Slate mine in far north Queensland. Poor gem quality garnets occur in quartz veins and weathered metasediments 2km SW of Mount Garnet.||||Is intruded by Mount Gibson Microgranite.||
8404|Hodgkinson Formation|72298|5|Briefly described|p792|||Six bores drilled into this unit augment the Cooktown water supply.|||||Metasediments.|
8404|Hodgkinson Formation|72983|6|Mentioned|p15, p35|early Carboniferous|Devonian|Hodgkinson Province. Mossman Orogen.||||Intruded by Hope Vale Granite.||
8404|Hodgkinson Formation|73083|6|Mentioned|p61, p71||||||Larrimore Metabasalt Member||Includes mudstone.|
8404|Hodgkinson Formation|73387|5|Briefly described|p2-3, p43-44, p46-48|Early Carboniferous|Wenlock|Hodgkinson Province. New zircon U-Pb SHRIMP maximum depositional age of 427.2 +/- 4.4 Ma published herein. Matches maximum depositional ages of 426 +/- 5 Ma, 433 +/- 6 Ma from Adams et al. (2013). Inferred to have been tectonically interleaved with the Barnard Metamorphics near Innisfail. Described as mainly Devonian-aged.|427.2 +/- 4.4 Ma U-Pb SHRIMP, c. 342 Ma MDA|||||20-DEC-22
8404|Hodgkinson Formation|73595|5|Briefly described|p1132, 1134-1135, 1142-1143|Devonian|Devonian|Hodgkinson Province, Mossman Orogen. Either a backarc or forearc environment.||||Is faulted against Barnard Metamorphics in the SE.|Turbidite sequences and tectonic melange, with minor volcanic intercalations and pelagic sediments. Greenschist facies metamorphism.|
8418|Hogsflesh Creek Granodiorite|22847|3|Fully described|p 39|Ordovician|Early Ordovician|||||||
8418|Hogsflesh Creek Granodiorite|23062|6|Mentioned|260|||||||||
8418|Hogsflesh Creek Granodiorite|23422|5|Briefly described|p173, p209 Table 6.6|Middle Ordovician|Early Ordovician|Of Hogsflesh Supersuite.||||||
8418|Hogsflesh Creek Granodiorite|23423|5|Briefly described|p228||Ordovician|In the Ravenswood Batholith.||||||
8418|Hogsflesh Creek Granodiorite|23429|5|Briefly described|Fig 13.25(a) p446|||||||||
8418|Hogsflesh Creek Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 463. I-Type.||||||
8418|Hogsflesh Creek Granodiorite|41659|5|Briefly described|p366|||Reserved as Hogsflesh (Creek) Granodiorite||||||
8418|Hogsflesh Creek Granodiorite|41668|3|Fully described|p30|||See also Fig.3.5||||||
8418|Hogsflesh Creek Granodiorite|42054|6|Mentioned|p272|||||||||
8418|Hogsflesh Creek Granodiorite|42633|5|Briefly described|Table 1 P11|||||||||
8418|Hogsflesh Creek Granodiorite|42750|2|Defined|p36|Middle Ordovician|Early Ordovician|||||||
8418|Hogsflesh Creek Granodiorite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Probable Early to Middle Ordivician||||||
8418|Hogsflesh Creek Granodiorite|43259|4|Described|Appendix 1,p49.||Ordovician|||||||
8418|Hogsflesh Creek Granodiorite|43934|5|Briefly described|Map Legend||Ordovician|||||||
8418|Hogsflesh Creek Granodiorite|50552|6|Mentioned|p1048 Fig.2|Late Ordovician|Early Ordovician|In Lolworth-Ravenswood Terrane.||||||
8418|Hogsflesh Creek Granodiorite|60425|5|Briefly described|p11|Ordovician|Ordovician|Part of Ravenswood Batholith in Charters Towers region. I-type granite.||||||07-FEB-11
8418|Hogsflesh Creek Granodiorite|62075|6|Mentioned|p11 Fig.3|Middle Ordovician|Early Ordovician|Appears as Hogsflesh Creek granodiorite.||||||
8418|Hogsflesh Creek Granodiorite|62521|5|Briefly described|p8, p26|Middle Ordovician|Late Cambrian|Of the Hogsflesh Creek Suite and Supersuite. Geological Province: Ravenswood Batholith. Medium-grained grey, hornblende-biotite granodiorite.||||||14-JAN-08
8421|Holborn Granodiorite|23422|5|Briefly described|p173, p210 Table 6.6|Middle Ordovician|Middle Ordovician|Probably part of the Columbia Creek Supersuite.||||||
8421|Holborn Granodiorite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
8421|Holborn Granodiorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 175. ?S-Type.||||||
8421|Holborn Granodiorite|42407|2|Defined|p40|Early Devonian|Ordovician|Reserved as Holborn Granite.||||||
8421|Holborn Granodiorite|42474|5|Briefly described|p28|||||||||
8421|Holborn Granodiorite|42689|5|Briefly described|map legend|Early Paleozoic||||||||07-NOV-08
8421|Holborn Granodiorite|43095|5|Briefly described|Plate 1|||||||||
8421|Holborn Granodiorite|43259|4|Described|Appendix 1,p27.|Devonian|Ordovician|Ordovician to Devonian?.||||||
8421|Holborn Granodiorite|43589|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Intruded by Clemant Microgranite.||||||07-NOV-08
8421|Holborn Granodiorite|68419|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained, muscovite-biotite granodiorite to tonalite.|
8421|Holborn Granodiorite|68420|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained, muscovite-biotite granodiorite to tonalite.|
8421|Holborn Granodiorite|70207|6|Mentioned|p20|Early Silurian|Ordovician|Clarke River and/or Cairns region.||||||
8467|Hook beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
8467|Hook beach sand|39495|6|Mentioned|p142|||||||||
8467|Hook beach sand|62102|5|Briefly described|p367 Tb. 1|||Informal name for morphostratigraphic unit on southeast Queensland coast.||||||
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||
8499|Horse Creek Limestone|37607|6|Mentioned|Fig.4|||||||||
8499|Horse Creek Limestone|39445|5|Briefly described|Table 14|||||||||
8499|Horse Creek Limestone|60703|6|Mentioned|p714, p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
8499|Horse Creek Limestone|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Austral Downs and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
8499|Horse Creek Limestone|69599|5|Briefly described|p584|Miocene|Miocene|Has Pliocene silcrete. See also Horse Creek Formation p599.||||Correlated with Doonbara, Whitula and Poodyea Formations; Noranside and Austral Downs Limestones; and Mount Coley Sinter.||03-MAY-22
8584|Hummock Basalt|33754|6|Mentioned|p59|||||||||
8584|Hummock Basalt|35688|3|Fully described|p357|||No type section.||||||
8584|Hummock Basalt|36581|6|Mentioned|Fig.1|||||||||
8584|Hummock Basalt|39445|5|Briefly described|Table 14|||||||||
8584|Hummock Basalt|39505|6|Mentioned|p171|||||||||
8584|Hummock Basalt|39968|4|Described|p84|||||||||
8584|Hummock Basalt|42895|3|Fully described|p76|||middle Pleistocene age||||||
8584|Hummock Basalt|43883|14|Not recorded|p18 Fig.4-3|||||||||
8584|Hummock Basalt|44581|14|Not recorded|p352|||||||||
8584|Hummock Basalt|44754|14|Not recorded|Map||Quaternary|||||||
8584|Hummock Basalt|44786|14|Not recorded|p193-202||Pleistocene|||||||
8584|Hummock Basalt|44810|14|Not recorded|p167 (Tb.)||Pliocene|||||||
8584|Hummock Basalt|61155|5|Briefly described|p20|Pleistocene|Pleistocene|Together with Berrembea and Barambah Basalts, overlies the Tarraran and Maroondan Melanephelinites. In the Bundaberg-Maryborough region. ||||||
8584|Hummock Basalt|64714|5|Briefly described|p3-4 Fig. 1, p11, p20|Pleistocene|Pleistocene|Age: 0.93+/-0.05Ma, and 1.09+/-0.06Ma. Olivine basalt flows, minor scoria, agglomerate. See also p68 Appendix 3. ||||||
8584|Hummock Basalt|68332|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Bundaberg Volcanic Province.|1.09 +/- 0.06 - 0.93 +/- 0.05 Ma K/Ar.||||Olivine basalt flows, minor scoria, agglomerate.|26-MAR-15
8584|Hummock Basalt|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Barambah and Berrembea Basalts, are all mapped under the symbol, Qbs.||||||
8584|Hummock Basalt|69599|5|Briefly described|p586|Pleistocene|Pleistocene|Capricorn Basin.||||Unconformably overlies the Elliott Formation.||
8584|Hummock Basalt|69600|5|Briefly described|p669|Pleistocene|Pleistocene|Capricorn Basin. Bundaberg area. Up to 55m thick; crops out over 215 km2. Extruded from a vent at Sloping Hummock.|1.1-0.9 Ma (K-Ar; Wellman, 1978).||||Vesicular olivine basalt flows.|
8589|Hungerford Granite|34469|6|Mentioned|p108|||Devonian||||||
8589|Hungerford Granite|42467|5|Briefly described|Map Legend|||||||||
8589|Hungerford Granite|43386|14|Not recorded|Map Legend||Devonian|||||||
8589|Hungerford Granite|43411|14|Not recorded|Map Legend||Late Devonian|361 million years||||||
8589|Hungerford Granite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
8589|Hungerford Granite|68731|5|Briefly described|p166 Fig 3.78, p167 Tb 3.2|Early Devonian|Silurian|Includes sparse inclusions of biotite schist (to ~10 cm). See also Eulo Ridge Granite.|419.1 +/- 2.5 Ma||||Pale grey, medium-grained, moderately porphyritic; muscovite-biotite monzogranite; scattered phenocrysts of white K-feldspar (to ~ 5 cm); gneiss (to ~30 cm); reduced; cut by sparse, thin quartz veins; deformed; very poorly exposed.|
8589|Hungerford Granite|68823|5|Briefly described|p378 Fig.4, p393|Lochkovian|Ludlow|Geochronology by Bultitude and Cross (2012).|419.1 +/- 2.5 Ma, SHRIMP-IIe|||||
8589|Hungerford Granite|68901|5|Briefly described|p7 Fig. ii|Late Silurian|Late Silurian|Eulo Ridge, Thomson Region.
|||||Grey, porphyritic muscovite-biotite monzogranite.|26-SEP-18
8589|Hungerford Granite|69002|5|Briefly described|p10, p13, Map 1b|Famennian|Givetian|Exposed in scattered outcrops between Hungerford on the NSW-QLD border and  Eulo 100km north in QLD. K-Ar dating by Evernden and Richards (1962) and SHRIMP-IIe dating by Geoscience Australia.|c.361 Ma, K-Ar; 385 Ma, SHRIMP-IIe|||||
8589|Hungerford Granite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen. ?Low-magnetic intensity||||||
8589|Hungerford Granite|69043|6|Mentioned|p11|||Thomson Orogen.||||||
8589|Hungerford Granite|69541|6|Mentioned|p644 Fig.1(a)|Early Devonian|Late Silurian|Thomson Orogen.||||||
8589|Hungerford Granite|69952|5|Briefly described|p1, p2 Tb.i, p16, p30-33, p123|Late Silurian|Late Silurian|Southern part of the Eulo Ridge, Thomson Orogen. Deeply weathered; poor exposures of sparse low boulders and bouldery rubble. SHRIMP U-Pb zircon age of emplacement.|419.1 +/- 2.5 Ma (Cross et al., 2015).||||Grey, porphyritic muscovite-biotite monzogranite.|
8589|Hungerford Granite|70033|6|Mentioned|p1, p18|Silurian|Silurian|Age: late Silurian.|419.1 +/- 2.5 Ma, Cross et al. 1995|||||16-JUL-15
8589|Hungerford Granite|70720|6|Mentioned|p2|||Eulo Ridge, southern Thomson Orogen.||||||
8589|Hungerford Granite|70744|5|Briefly described|p939|||Thomson Orogen (NW NSW). Age by Bultitude and Cross (2013).|c.419 Ma (estimated from Fig.7).|||||
8589|Hungerford Granite|70749|5|Briefly described|p43|Devonian|Devonian|Southern Thomson and Koonenberry area.|419.1 +/- 2.5 Ma.|||||
8589|Hungerford Granite|70821|5|Briefly described|p9-10, p12, p13 Tb.2.1, p89|Early Devonian|Late Silurian||419.1 +/- 2.5 Ma (Bultitude and Cross, 2013).||||Includes monzogranite.|01-DEC-16
8589|Hungerford Granite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|419+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
8589|Hungerford Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|419.1 +/- 2.5 Ma (Bultitude et al. 2012)||||Monzogranite.|
8589|Hungerford Granite|71965|5|Briefly described|p897,901-904,906,910,913|Lochkovian|Pridoli|Geological province: Thomson Orogen. Outcropping S-type granite in the southern Thomson Orogen. Dated at 419.5+\-2.5 Ma (Cross et al., 2015).|419.5+\-2.5 Ma||||Deeply weathered, medium-grained, moderately porphyritic muscovite-biotite monzogranite with metasedimentary inclusions.|
8589|Hungerford Granite|71966|5|Briefly described|p988-993,995,1000-1002,1004-1005|Early Devonian|Late Silurian|Geological province: Thomson Orogen. S-type granitic intrusion associated with c. 430-395 Ma magmatism in the southern Thomson Orogen. Crops out along the Eulo Ridge basement high; part of a batholithic scale belt of intrusions termed the Ella belt (Purdy et al., 2018). Outcrop sample collected and analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 2122055 yielded an age of 419.1+\-2.5 Ma, which is interpreted as the crystallisation age of this rock. Age equivalent to Tibooburra Suite. Hf and O isotopic analysis confirms S-type affinity, with less evolved Hf isotopic signatures than the Ordovician granites, indicating different source components between Silurian and Ordovician granites.|419.1+\-2.5 Ma (crystallisation)|||||25-OCT-19
8589|Hungerford Granite|72522|5|Briefly described|p49|Lochkovian|Pridoli|Along Eulo Ridge, south of Granite Springs Granite.|419.1+/-2.5 Ma|||||
8589|Hungerford Granite|72914|6|Mentioned|p16|Lochkovian|Silurian|S-type affinity. Similar U-Pb age, geochemistry and petrological characteristics as Brewarrina Granite. These two units potentially represent intrusions with a close spatial affinity but were separated by extension related to the Paka Tank Trough (~400 Ma).|419.1 +/- 2.5 Ma|Tibooburra Suite?||||
8589|Hungerford Granite|72915|6|Mentioned|p5, p17|||May be intrinsically related to the metamorphic basement rock from the Congararra 1 borehole [tentatively interpreted as the Twin Tanks Metamorphics]. Map symbol suggests Silurian age.||||||
8589|Hungerford Granite|72951|6|Mentioned|p1026, 1028|Lochkovian|Pridoli|Thomson Orogen, southern.|419.1 +/- 2.5 Ma|||||
8589|Hungerford Granite|73179|6|Mentioned|p1133, p1134 Fig.1, p1153-1154|late Silurian|late Silurian|||||||20-SEP-22
8599|Hurleys Metamorphics|22557|6|Mentioned|p567,569|||||||||
8599|Hurleys Metamorphics|22982|5|Briefly described|p269 Fig.4|||||||||
8599|Hurleys Metamorphics|23078|5|Briefly described|p708|||||||||
8599|Hurleys Metamorphics|42747|5|Briefly described|p33, Fig.3|||of Anakie Metamorphic Group. Reserved as Hurleys Meta-arenite.||||||
8599|Hurleys Metamorphics|43204|5|Briefly described|Map Legend||Neoproterozoic|Neoproterozoic or Early Cambrian.  Anakie Inlier||||||23-DEC-11
8599|Hurleys Metamorphics|43213|3|Fully described|p8, p20-22, p33, p41-42, p130-140, p237|||See also p240, p245. Named after Hurleys Diggings (old alluvial gold workings). Type area and geophysical properties briefly described. Deformation structures detailed. Possibly equivalent to Monteagle Quartzite. Forms a series of alternating belts with Scurvy Creek Meta-arenite, due to folding or thrust repetition.||Unit in Anakie Metamorphic Group.||Is overlain structurally by Scurvy Creek Meta-arenite and unconformably by Blair Athol Coal Measures.|White, medium- to very thick-bedded, generally fine- to medium-grained quartzite, locally calcite-rich; interlayered with grey to greenish-grey phyllite or fine-grained mica schist and slate.|
8599|Hurleys Metamorphics|43861|2|Defined|25, 30, 31|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group. Overlies Scurvy Creek Meta-arenite, underlies Blair Athol Coal Measures||||||
8599|Hurleys Metamorphics|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.||Conformably overlies Rolfe Creek Schist. Is conformably overlain by Scurvy Creek Meta-arenite.|White, fine-to coarse-grained, strongly foliated quartzite and fine-grained quartz-mica schist grading to phyllite.|23-JUN-15
8599|Hurleys Metamorphics|68731|5|Briefly described|p120 Fig 3.6, p122, p126, p133|Early Cambrian|Neoproterozoic|The meta-arenite is pale green, mainly fine- to medium-grained consisting of quartz, minor feldspar and ubiquitous detrital muscovite flakes in a matrix of muscovite, chlorite, biotite, and finer quartz. Age constrained by the Anakie Metamorphic Group.||Of the Anakie Metamorphic Group.||Overlain by the Scurvy Creek Meta-arenite.|Comprises quartzite (locally calcareous), phyllite, fine mica schist and slate. Rare sedimentary features, including relict load clasts and soft sediment deformation features, are preserved.|
8599|Hurleys Metamorphics|68900|5|Briefly described|p6|||Drummond Basin. Potentially correlated with the Monteagle Quartzite.|||||Quartzite-rich metamorphics.|
8599|Hurleys Metamorphics|70749|6|Mentioned|p43|Cambrian|Neoproterozoic|Anakie Province.||Anakie Metamorphic Group.||||
8599|Hurleys Metamorphics|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Anakie Province, Thomson Orogen.||||||
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.||
8675|Inca Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|23031|6|Mentioned|17|||Geol Province Georgina Basin||||||
8675|Inca Formation|23393|5|Briefly described|p22, p23 Fig. 6|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|24034|6|Mentioned|p48|||Clay-rich litology.||||||06-MAY-09
8675|Inca Formation|30239|5|Briefly described|p1193|||||||||
8675|Inca Formation|30242|6|Mentioned|Fig.2|||||||||
8675|Inca Formation|30479|6|Mentioned|Fig.5|||See also Fig.6,Fig.7. stratigraphic relationships||||||
8675|Inca Formation|30775|6|Mentioned|p1|||||||||
8675|Inca Formation|30778|6|Mentioned|p1,Fig.5|||||||||
8675|Inca Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|31289|6|Mentioned|Fig. 1|||Middle Cambrian||||||
8675|Inca Formation|31342|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8675|Inca Formation|31396|6|Mentioned|Fig.3|||||||||
8675|Inca Formation|31465|6|Mentioned|p418|||Trilobite content||||||
8675|Inca Formation|32576|5|Briefly described|p49|||||||||
8675|Inca Formation|32948|6|Mentioned|p111|||||||||
8675|Inca Formation|32952|4|Described|p1188|||M.-U.Cambrian. See also pp1189-1194,1203-1213.||||||27-SEP-06
8675|Inca Formation|33111|4|Described|p36|||Mention Fig.4||||||
8675|Inca Formation|33368|6|Mentioned|p5|||Bituminous limestone||||||
8675|Inca Formation|33482|6|Mentioned|Fig.2|||Cambrian||||||
8675|Inca Formation|34287|6|Mentioned|Fig.3|||||||||
8675|Inca Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|34543|6|Mentioned|p98|||||||||
8675|Inca Formation|34754|6|Mentioned|p42|||||||||
8675|Inca Formation|34903|6|Mentioned|p582|||||||||
8675|Inca Formation|35001|6|Mentioned|Fig.45|||||||||
8675|Inca Formation|35004|6|Mentioned|Fig.60|||||||||
8675|Inca Formation|35054|6|Mentioned|Table 23|||||||||
8675|Inca Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|35139|4|Described|Table.2|||||||||
8675|Inca Formation|35553|6|Mentioned|p10|||See also Appendix 2, description of Agnostid localities.||||||
8675|Inca Formation|35556|6|Mentioned|Plate 4|||||||||
8675|Inca Formation|35939|6|Mentioned|p633|||||||||
8675|Inca Formation|36234|3|Fully described|p168|||||||||
8675|Inca Formation|36243|6|Mentioned|Table 1A|||||||||
8675|Inca Formation|36645|5|Briefly described|p314|||Fig.2.||||||
8675|Inca Formation|36818|6|Mentioned|p203|||||||||
8675|Inca Formation|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|37572|4|Described|p158|||See also Fig.7||||||
8675|Inca Formation|38444|5|Briefly described|p105|||||||||
8675|Inca Formation|38446|6|Mentioned|Table 23|||||||||
8675|Inca Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|39445|5|Briefly described|Table 4|||See also p62.||||||27-SEP-06
8675|Inca Formation|39690|6|Mentioned|Table 1|||||||||
8675|Inca Formation|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|39943|6|Mentioned|Table 2C|||||||||
8675|Inca Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|40221|4|Described|p20|||||||||
8675|Inca Formation|40386|6|Mentioned|p440|||||||||
8675|Inca Formation|40686|5|Briefly described|p407|||||||||
8675|Inca Formation|40852|6|Mentioned|p37|||||||||
8675|Inca Formation|40855|6|Mentioned|p345|||||||||
8675|Inca Formation|40856|5|Briefly described|p315|||||||||
8675|Inca Formation|40857|5|Briefly described|p268|||||||||
8675|Inca Formation|40858|5|Briefly described|p132|||||||||
8675|Inca Formation|41129|6|Mentioned|Fig.8|||||||||
8675|Inca Formation|41240|6|Mentioned|Fig.1|||||||||
8675|Inca Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
8675|Inca Formation|41388|6|Mentioned|p552|||||||||
8675|Inca Formation|41639|6|Mentioned|p3|||||||||
8675|Inca Formation|42139|6|Mentioned|Fig.12 P78|||||||||
8675|Inca Formation|42575|5|Briefly described|Fig.2 P335|||||||||
8675|Inca Formation|43105|6|Mentioned|p16|||||||||
8675|Inca Formation|43807|6|Mentioned|Fig.2,p347|||||||||
8675|Inca Formation|44091|14|Not recorded|p16,Tb.1,18||Middle Cambrian|||||||
8675|Inca Formation|44205|14|Not recorded|p69,78,89|||||||||
8675|Inca Formation|44210|2|Defined|map,p6,13,Tb.2|||Overlies Beetle Creek Formation or Pilpah Sandstone.||||||
8675|Inca Formation|44211|14|Not recorded|p95-98,100-103|||||||||
8675|Inca Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
8675|Inca Formation|44275|14|Not recorded|Map Legend|||||||||
8675|Inca Formation|44276|14|Not recorded|p20,22,Tb.2,map|||||||||
8675|Inca Formation|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
8675|Inca Formation|44757|14|Not recorded|p155||Middle Cambrian|Divided into Upper Limestone, and Lower Shale members.||||||
8675|Inca Formation|44788|14|Not recorded|p27|||||||||
8675|Inca Formation|44882|14|Not recorded|p177||Cambrian|In French||||||
8675|Inca Formation|44989|14|Not recorded|p.122|||||||||
8675|Inca Formation|45052|3|Fully described|p92|||M.Camb. See also p32.||||||27-SEP-06
8675|Inca Formation|45054|6|Mentioned|p6|||Fossil locality||||||
8675|Inca Formation|45062|6|Mentioned|p7|||||||||
8675|Inca Formation|45079|4|Described|p30|||Cambrian age||||||
8675|Inca Formation|45119|6|Mentioned|p4|||||||||
8675|Inca Formation|45166|5|Briefly described|Table 15|||||||||
8675|Inca Formation|47024|6|Mentioned|Table 1|||||||||
8675|Inca Formation|47058|5|Briefly described|p125|||||||||
8675|Inca Formation|49027|6|Mentioned|p7|||||||||
8675|Inca Formation|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks.  Overlies the Beetle Creek Formation.; passes laterally into Roaring Siltstone.  ||||||
8675|Inca Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of the arthur Creek Formation. Geological Province: eastern Georgina Basin and Burke River Structural Belt.||||||
8675|Inca Formation|60264|5|Briefly described|p575 Fig. 1|Middle Cambrian|Middle Cambrian|See also Inca Shale.||||||
8675|Inca Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, shale, sandstone, chert, limestone.||||||
8675|Inca Formation|63450|4|Described|p81|Middle Cambrian|Middle Cambrian|Contains a shale member ~100m thick - probably the Inca Shale mentioned in Fig. 5 (p78). Overlain by Devoncourt Limestone but with hiatus between.||||||07-FEB-11
8675|Inca Formation|64068|4|Described|p63, p59, 62, p114|Middle Cambrian|Middle Cambrian|Potential oil source. Contains diverse fauna. Correlated with Arthur Creek Formation, Blazan Shale, Currant Bush Limestone, Age Creek Formation.||Of Narpa Group.||Disconformably overlies Beetle Creek Formation or Thorntonia Limestone. Conformably overlain by Currant Bush Limestone, V Creek Limestone, Roaring Silstone, Devoncourt Limestone.|Laminated pyritic siliceous shale and siltstone, chert, dark foetid limestone.|05-APR-12
8675|Inca Formation|64443|6|Mentioned|p40.|||Correlative of Wonarah Formation.||||||
8675|Inca Formation|67127|6|Mentioned|p78|||Primary host for phosphorite REE deposits.||||||
8675|Inca Formation|67323|5|Briefly described|GIS attrib tbl; p83, p92 Fig.12.2|Cambrian|Cambrian|Georgina Basin.||Narpa Group.||Overlies Beetle Creek Formation, locally unconformably. Is overlain by Currant Bush Limestone and (unconformably) by Roaring Siltstone and Devencourt Limestone.|Siliceous shale and chert with limestone interbeds.|
8675|Inca Formation|67352|6|Mentioned|p69|||||||||
8675|Inca Formation|67402|6|Mentioned|p215, p217|||||||Overlies the Thorntonia Limestone||
8675|Inca Formation|69443|5|Briefly described|p28:16, 20, 2223|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Disconformably overlies Thorntonia Limestone. Is overlain by and partially interfingers with Currant Bush Limestone. Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
8675|Inca Formation|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
8675|Inca Formation|69591|4|Described|p87-89, p91-92, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Exposed in low rolling hills, mesas, cliffs and creek banks along the Basin margin. Up to 150m thick. Contains a rich agnostoid trilobite fauna. Is in part laterally equivalent to Currant Bush Limestone and Gowers Formation. Is lithologically identical to Blazan Shale. Is also lithologically identical to Roaring Siltstone, which is considered to be its northern younging extension; they are distinguished by fossil fauna (named).||Narpa Group.||Conformably overlies Beetle Creek Formation and Thorntonia Limestone. Is overlain by Currant Bush Limestone, and unconformably by Roaring Siltstone and Devoncourt Limestone.|Laminated siliceous shale and siltstone (bituminous when fresh) with bands of chert and large lenses of impure flaggy and ellipsoidal limestone varying from 3 to 150m thick and pinching out to the N.|
8675|Inca Formation|70723|5|Briefly described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Deposited in a marine environment under anoxic conditions. Oil-prone source rock. Kerogen type and biomarker compositions discussed in detail.||Narpa Group||Overlies Beetle Creek Formation, overlain by Currant Bush Limestone|Laminated pyritic and calcareous shale and siltstone, interbedded with limestone that contains abundant organic matter.|
8675|Inca Formation|70864|6|Mentioned|p74 Fig 2||Paleozoic|Shown as a combined unit with Beetle Creek Formation.||||||
8675|Inca Formation|72297|5|Briefly described|p747, p752|Cambrian|Cambrian|Georgina Basin. TOC value of 2.82% reported.|||||Contains thin oil shale beds.|
8675|Inca Formation|72321|6|Mentioned|Fig 2|Drumian|Wulian|Burke River Structural Belt, Georgina Basin. Australian stages:  Floran to Undillan. Undilla Sub-basin, Georgina Basin.  Australian Stages: Templetonian to Undillan. ||of Narpa Group.||||
8675|Inca Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
8675|Inca Formation|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Overlies Beetle Creek Formation, underlies Currant Bush Limestone, lateral equivalent of Blazan Shale and Roaring Siltstone.|Shale/siltstone/chert sequence.|
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.||
8736|Innisplain member|48917|6|Mentioned|p17|||Refers Pearde (1964)||||||
8762|Ipswich Coal Measures|12597|6|Mentioned|p493 Fig.2, p494|||||||||
8762|Ipswich Coal Measures|13516|5|Briefly described|p159 fig 8, p163, p164|Late Triassic|Late Triassic|From Clarence-Moreton Basin.|||Includes Kholo and Brassal Subgroups|||
8762|Ipswich Coal Measures|22857|5|Briefly described|p277, p318-9 Figs. 22.10A,B|Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|22860|6|Mentioned|p277||Late Triassic|||||||
8762|Ipswich Coal Measures|22861|6|Mentioned|p284|||||||||
8762|Ipswich Coal Measures|22865|5|Briefly described|p295,Fig22.9p317||Late Triassic|||||||
8762|Ipswich Coal Measures|23056|6|Mentioned|6|||Geol province Eromanga Basin||||||
8762|Ipswich Coal Measures|23440|6|Mentioned|p146|||||||||
8762|Ipswich Coal Measures|23799|5|Briefly described|p46|Norian|Carnian|Supersedes the Ipswich Beds.  Lower coal measures of the Bundamba Group.  Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|23811|6|Mentioned|Map Legend|||Mentioned as equivalent to Red Cliff Measures.||||||20-DEC-04
8762|Ipswich Coal Measures|23812|5|Briefly described|p31, p33 Fig.6|||Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|23843|5|Briefly described|p456 Table 1|Triassic|Triassic|Geological Province: Ipswich Basin.  Maximum thickness: 1220m.||||||
8762|Ipswich Coal Measures|24081|6|Mentioned|p451|||||||||
8762|Ipswich Coal Measures|24082|5|Briefly described|p453|Late Triassic|Late Triassic|Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|24237|5|Briefly described|p5 Fig.1|||Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|24551|6|Mentioned|p241|||||||||
8762|Ipswich Coal Measures|29385|6|Mentioned|p81|||Also P82. Triassic.||||||
8762|Ipswich Coal Measures|29591|6|Mentioned|p83|||||||||
8762|Ipswich Coal Measures|29720|6|Mentioned|Fig.1|||||||||
8762|Ipswich Coal Measures|29869|6|Mentioned|p37|||See also P33||||||
8762|Ipswich Coal Measures|29995|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|30086|5|Briefly described|p4|||Triassic||||||
8762|Ipswich Coal Measures|30087|4|Described|p3|||Consists of Blackstone, Cooneana and Tivoli Formations.||||||
8762|Ipswich Coal Measures|30131|5|Briefly described|p9|||See also P8||||||
8762|Ipswich Coal Measures|30302|5|Briefly described|p414|||Upper Triassic age||||||
8762|Ipswich Coal Measures|30455|6|Mentioned|p5|||See also P12,18. Triassic age||||||
8762|Ipswich Coal Measures|30458|6|Mentioned|p1|||||||||
8762|Ipswich Coal Measures|30459|6|Mentioned|p309|||||||||
8762|Ipswich Coal Measures|30460|6|Mentioned|p5|||See also P12-14,16,22,26. Triassic age||||||
8762|Ipswich Coal Measures|30463|6|Mentioned|p464|||Triassic age||||||
8762|Ipswich Coal Measures|30464|6|Mentioned|Fig.1|||Triassic||||||
8762|Ipswich Coal Measures|30465|5|Briefly described|p1|||See also P2-22. Late Triassic age||||||
8762|Ipswich Coal Measures|30466|6|Mentioned|p1|||Triassic age||||||
8762|Ipswich Coal Measures|30467|6|Mentioned|p412|||Triassic age||||||
8762|Ipswich Coal Measures|30470|6|Mentioned|p457|||||||||
8762|Ipswich Coal Measures|30471|6|Mentioned|p132|||||||||
8762|Ipswich Coal Measures|30472|6|Mentioned|p134|||Pollen distribution.||||||
8762|Ipswich Coal Measures|30474|6|Mentioned|p249|||Microflora||||||
8762|Ipswich Coal Measures|30475|5|Briefly described|p164|||Refer palynology||||||
8762|Ipswich Coal Measures|30477|6|Mentioned|p461|||||||||
8762|Ipswich Coal Measures|30478|6|Mentioned|p272|||||||||
8762|Ipswich Coal Measures|30517|6|Mentioned|p436|||||||||
8762|Ipswich Coal Measures|30565|6|Mentioned|p132|||||||||
8762|Ipswich Coal Measures|30654|6|Mentioned|p48|||||||||
8762|Ipswich Coal Measures|30687|6|Mentioned|p65|||Triassic age||||||
8762|Ipswich Coal Measures|30784|6|Mentioned|p70|||Correlated with Red Cliff & Nymboiden Coal Measures (McElroy,1963,1969)||||||
8762|Ipswich Coal Measures|30785|6|Mentioned|p397|||Correlated with Red Cliff Coal Measures||||||
8762|Ipswich Coal Measures|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|30915|6|Mentioned|p98|||||||||
8762|Ipswich Coal Measures|31086|6|Mentioned|p33|||Triassic. Refers Jones & de Jersey (1947)||||||
8762|Ipswich Coal Measures|31118|6|Mentioned|p311|||||||||
8762|Ipswich Coal Measures|31272|6|Mentioned|p47|||||||||
8762|Ipswich Coal Measures|31276|6|Mentioned|p151|||Palynology||||||
8762|Ipswich Coal Measures|31300|6|Mentioned|p79|||Triassic plants.||||||
8762|Ipswich Coal Measures|31450|6|Mentioned|p47|||||||||
8762|Ipswich Coal Measures|31649|6|Mentioned|p63|||||||||
8762|Ipswich Coal Measures|31739|6|Mentioned|p85|||Stratigraphy||||||
8762|Ipswich Coal Measures|32136|6|Mentioned|p5|||Miospores||||||
8762|Ipswich Coal Measures|32176|6|Mentioned|p2|||Triassic||||||
8762|Ipswich Coal Measures|32178|6|Mentioned|p2|||||||||
8762|Ipswich Coal Measures|32179|6|Mentioned|p3|||Trias.||||||
8762|Ipswich Coal Measures|32180|6|Mentioned|Table 1|||||||||
8762|Ipswich Coal Measures|32491|5|Briefly described|p20|||M.-U. Triassic||||||
8762|Ipswich Coal Measures|32492|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Mid.-U.TriassicM - U||||||
8762|Ipswich Coal Measures|32801|6|Mentioned|Fig.9|||||||||
8762|Ipswich Coal Measures|32803|6|Mentioned|p83|||||||||
8762|Ipswich Coal Measures|32838|6|Mentioned|p320|||||||||
8762|Ipswich Coal Measures|32920|6|Mentioned|p89|||||||||
8762|Ipswich Coal Measures|33128|5|Briefly described|p50|||Geochemistry. See also Fig. 5.||||||
8762|Ipswich Coal Measures|33381|4|Described|p109|||Triassic. See also PP110-116,122.||||||
8762|Ipswich Coal Measures|33769|6|Mentioned|p149|||U.Triassic||||||
8762|Ipswich Coal Measures|33881|5|Briefly described|p96|||||||||
8762|Ipswich Coal Measures|34010|6|Mentioned|Cor. chart|||||||||
8762|Ipswich Coal Measures|34070|6|Mentioned|p2|||Triassic.  See also P3||||||
8762|Ipswich Coal Measures|34148|6|Mentioned|p18|||See also PP20,21. Upper Triassic.||||||
8762|Ipswich Coal Measures|34172|5|Briefly described|p50|||Palynological subdivision and correlations.||||||
8762|Ipswich Coal Measures|34340|6|Mentioned|p457|||Coal measures in Kyogle No.1 Well||||||
8762|Ipswich Coal Measures|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
8762|Ipswich Coal Measures|34457|6|Mentioned|p484|||||||||
8762|Ipswich Coal Measures|34505|6|Mentioned|p1|||Middle Triassic. See also P3.||||||
8762|Ipswich Coal Measures|34755|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|35007|6|Mentioned|p75|||||||||
8762|Ipswich Coal Measures|35095|6|Mentioned|p115|||||||||
8762|Ipswich Coal Measures|35126|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|35156|4|Described|p6|||See also Table.2||||||
8762|Ipswich Coal Measures|35161|6|Mentioned|p591|||||||||
8762|Ipswich Coal Measures|35280|6|Mentioned|p143|||||||||
8762|Ipswich Coal Measures|35428|6|Mentioned|p125|||Biostratigraphy||||||
8762|Ipswich Coal Measures|35435|6|Mentioned|p44|||||||||
8762|Ipswich Coal Measures|35648|6|Mentioned|p13|||||||||
8762|Ipswich Coal Measures|35812|6|Mentioned|p568|||||||||
8762|Ipswich Coal Measures|35866|6|Mentioned|p403|||||||||
8762|Ipswich Coal Measures|35901|6|Mentioned|p5|||||||||
8762|Ipswich Coal Measures|35937|6|Mentioned|Fig.4|||||||||
8762|Ipswich Coal Measures|36045|6|Mentioned|p335|||||||||
8762|Ipswich Coal Measures|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
8762|Ipswich Coal Measures|36243|6|Mentioned|p74|||||||||
8762|Ipswich Coal Measures|36351|6|Mentioned|p373|||||||||
8762|Ipswich Coal Measures|36354|6|Mentioned|p366|||||||||
8762|Ipswich Coal Measures|36440|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
8762|Ipswich Coal Measures|36779|4|Described|p6|||||||||
8762|Ipswich Coal Measures|36825|6|Mentioned|p4|||||||||
8762|Ipswich Coal Measures|36899|6|Mentioned|p1085|||||||||
8762|Ipswich Coal Measures|36941|6|Mentioned|p162|||||||||
8762|Ipswich Coal Measures|36954|6|Mentioned|p114|||||||||
8762|Ipswich Coal Measures|36961|6|Mentioned|Table 1|||||||||
8762|Ipswich Coal Measures|37065|6|Mentioned|p36|||||||||
8762|Ipswich Coal Measures|37109|6|Mentioned|p283|||||||||
8762|Ipswich Coal Measures|37111|5|Briefly described|p291|||||||||
8762|Ipswich Coal Measures|37112|6|Mentioned|p298|||||||||
8762|Ipswich Coal Measures|37122|5|Briefly described|Table 1|||||||||
8762|Ipswich Coal Measures|37135|6|Mentioned|p300|||||||||
8762|Ipswich Coal Measures|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|37375|6|Mentioned|Fig.1|||||||||
8762|Ipswich Coal Measures|37405|6|Mentioned|p30|||||||||
8762|Ipswich Coal Measures|37755|6|Mentioned|p79|||||||||
8762|Ipswich Coal Measures|37757|6|Mentioned|p17|||||||||
8762|Ipswich Coal Measures|37812|6|Mentioned|p657|||||||||
8762|Ipswich Coal Measures|38074|5|Briefly described|Table 1|||||||||
8762|Ipswich Coal Measures|38076|6|Mentioned|Table 3|||||||||
8762|Ipswich Coal Measures|38077|5|Briefly described|p30|||||||||
8762|Ipswich Coal Measures|38079|6|Mentioned|p46|||||||||
8762|Ipswich Coal Measures|38306|6|Mentioned|p509|||||||||
8762|Ipswich Coal Measures|38307|6|Mentioned|p519|||||||||
8762|Ipswich Coal Measures|38358|6|Mentioned|p3|||||||||
8762|Ipswich Coal Measures|38391|6|Mentioned|p10|||||||||
8762|Ipswich Coal Measures|38441|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|39079|5|Briefly described|p10|||||||||
8762|Ipswich Coal Measures|39218|6|Mentioned|p47|||Flora||||||
8762|Ipswich Coal Measures|39306|6|Mentioned|p425|||||||||
8762|Ipswich Coal Measures|39445|6|Mentioned|Table 9|||||||||
8762|Ipswich Coal Measures|39907|4|Described|p10|||Sedimentology||||||
8762|Ipswich Coal Measures|40245|6|Mentioned|p185|||||||||
8762|Ipswich Coal Measures|40434|6|Mentioned|p25|||||||||
8762|Ipswich Coal Measures|40479|6|Mentioned|p32|||||||||
8762|Ipswich Coal Measures|40579|6|Mentioned|Map legend|late Carnian|late Carnian|||||||
8762|Ipswich Coal Measures|40623|5|Briefly described|p7|||||||||
8762|Ipswich Coal Measures|40634|6|Mentioned|p33|||||||||
8762|Ipswich Coal Measures|40780|5|Briefly described|p6|||||||||
8762|Ipswich Coal Measures|41058|6|Mentioned|p51|||||||||
8762|Ipswich Coal Measures|41059|6|Mentioned|p168|||||||||
8762|Ipswich Coal Measures|41063|6|Mentioned|p45|||||||||
8762|Ipswich Coal Measures|41475|6|Mentioned|p72|||||||||
8762|Ipswich Coal Measures|41550|6|Mentioned|p491|||||||||
8762|Ipswich Coal Measures|41591|6|Mentioned|p15|||||||||
8762|Ipswich Coal Measures|41631|6|Mentioned|p4|||||||||
8762|Ipswich Coal Measures|41738|6|Mentioned|p168|||||||||
8762|Ipswich Coal Measures|41906|6|Mentioned|p44|||||||||
8762|Ipswich Coal Measures|42187|6|Mentioned|p319|||||||||
8762|Ipswich Coal Measures|42248|5|Briefly described|p397|||||||||
8762|Ipswich Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
8762|Ipswich Coal Measures|42316|6|Mentioned|p5|||||||||
8762|Ipswich Coal Measures|42336|4|Described|p4|||||||||
8762|Ipswich Coal Measures|42370|6|Mentioned|p329|||||||||
8762|Ipswich Coal Measures|42405|6|Mentioned|Table 3 P.7|||||||||
8762|Ipswich Coal Measures|42463|6|Mentioned|Fig.3 P170|||||||||
8762|Ipswich Coal Measures|42474|6|Mentioned|p30|||Bundamba||||||
8762|Ipswich Coal Measures|42492|5|Briefly described|Table 2 P14|||||||||
8762|Ipswich Coal Measures|42525|5|Briefly described|Map legend|Late Triassic|Late Triassic|Includes the Kholo and Brassall Sub-Groups.||||||15-JUL-04
8762|Ipswich Coal Measures|42539|6|Mentioned|p183|||||||||
8762|Ipswich Coal Measures|42541|6|Mentioned|p203|||||||||
8762|Ipswich Coal Measures|42648|5|Briefly described|Fig.7 P43|||||||||
8762|Ipswich Coal Measures|42725|6|Mentioned|p24|||||||||
8762|Ipswich Coal Measures|42869|5|Briefly described|p33|||see also Fig.2 P32||||||
8762|Ipswich Coal Measures|42893|5|Briefly described|Fig.2 P7|||||||||
8762|Ipswich Coal Measures|43001|5|Briefly described|p121|||||||||
8762|Ipswich Coal Measures|43009|5|Briefly described|Map Legend|||||||||
8762|Ipswich Coal Measures|43072|6|Mentioned|p80|||||||||
8762|Ipswich Coal Measures|43076|5|Briefly described|p8|||||||||
8762|Ipswich Coal Measures|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
8762|Ipswich Coal Measures|43736|6|Mentioned|p9||Triassic|||||||
8762|Ipswich Coal Measures|43881|14|Not recorded|p13,25,28,74,79,80,|||p85(prox.anal.),99-102,134,146. Comparison with equivalent Nymboida Coal Measures in NSW.||||||
8762|Ipswich Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
8762|Ipswich Coal Measures|43895|4|Described|p114,115|||Important source for ceramics.||||||
8762|Ipswich Coal Measures|43905|14|Not recorded|p87||Triassic|Flora||||||
8762|Ipswich Coal Measures|43908|14|Not recorded|p6|||||||||
8762|Ipswich Coal Measures|43910|14|Not recorded|p2,4-5,7-8,10-13,|||p18-19, Fig.2||||||
8762|Ipswich Coal Measures|43911|14|Not recorded|p17,18|||||||||
8762|Ipswich Coal Measures|43914|14|Not recorded|p14|||||||||
8762|Ipswich Coal Measures|43918|14|Not recorded|p54,63,64|||||||||
8762|Ipswich Coal Measures|43919|14|Not recorded|p39|||||||||
8762|Ipswich Coal Measures|43920|14|Not recorded|p74|||||||||
8762|Ipswich Coal Measures|43921|14|Not recorded|p315,323|||Now "the entire Triassic sequence in the Brisbane area is correlated with the Ipswich Coal Measures."||||||
8762|Ipswich Coal Measures|43922|14|Not recorded|p324,325|||Middle or late Upper Triassic.||||||
8762|Ipswich Coal Measures|43923|6|Mentioned|p1|||||||||
8762|Ipswich Coal Measures|43924|14|Not recorded|p3|||||||||
8762|Ipswich Coal Measures|43984|14|Not recorded|p129,139|||||||||
8762|Ipswich Coal Measures|43993|14|Not recorded|p93-95,97,102|||||||||
8762|Ipswich Coal Measures|43995|14|Not recorded|p8,Tb.p10,26,28,29,||Middle Triassic|p38,42,43,54,57,60,Fig.16.||||||
8762|Ipswich Coal Measures|43997|14|Not recorded|p113|||||||||
8762|Ipswich Coal Measures|44026|14|Not recorded|p122,123||Triassic|||||||
8762|Ipswich Coal Measures|44029|14|Not recorded|p157,167|||||||||
8762|Ipswich Coal Measures|44030|14|Not recorded|p117,122,125,130|Late Triassic|Middle Triassic|||||||
8762|Ipswich Coal Measures|44075|14|Not recorded|p251|||||||||
8762|Ipswich Coal Measures|44076|14|Not recorded|p269,271|||||||||
8762|Ipswich Coal Measures|44091|14|Not recorded|p51,52||Triassic|||||||
8762|Ipswich Coal Measures|44093|5|Briefly described|p72|Late Triassic|Late Triassic|Geological Province: Ipswich Basin.||||||11-MAR-05
8762|Ipswich Coal Measures|44128|14|Not recorded|Tb.1,p426,430|||||||||
8762|Ipswich Coal Measures|44164|14|Not recorded|p26|||||||||
8762|Ipswich Coal Measures|44239|14|Not recorded|p278|||||||||
8762|Ipswich Coal Measures|44247|14|Not recorded|p3|||Chonchostracan (crustacean) found.||||||
8762|Ipswich Coal Measures|44250|14|Not recorded|p90|||See also Lexicon.||||||
8762|Ipswich Coal Measures|44382|14|Not recorded|p113|||||||||
8762|Ipswich Coal Measures|44384|14|Not recorded|p119|||||||||
8762|Ipswich Coal Measures|44387|14|Not recorded|p17|||||||||
8762|Ipswich Coal Measures|44428|14|Not recorded|p277|||||||||
8762|Ipswich Coal Measures|44430|14|Not recorded|p263,266-268|||Unconformably overlies Brisbane Metamorphics.||||||
8762|Ipswich Coal Measures|44510|2|Defined|p252-256,260-262,|||Figs.35,36. Overlain unconformably by Bundamba Group and Aberdare Conglomerate.||||||
8762|Ipswich Coal Measures|44542|2|Defined|p32||Middle Triassic|||||||
8762|Ipswich Coal Measures|44543|14|Not recorded|p27|||||||||
8762|Ipswich Coal Measures|44554|14|Not recorded|p295|||||||||
8762|Ipswich Coal Measures|44570|14|Not recorded|p677|||||||||
8762|Ipswich Coal Measures|44581|14|Not recorded|p346|||||||||
8762|Ipswich Coal Measures|44607|14|Not recorded|p36|||||||||
8762|Ipswich Coal Measures|44633|14|Not recorded|p2|||Includes Blackstone and Cooneana Formations.||||||
8762|Ipswich Coal Measures|44668|14|Not recorded|p60|||||||||
8762|Ipswich Coal Measures|44678|14|Not recorded|Fig.1|||||||||
8762|Ipswich Coal Measures|44687|5|Briefly described|p221|Triassic|Triassic|Described by Bryan & Jones (1960) as sandstone, shale and conglomerate with minor coal seams, unconformably overlying the Neranleigh-Fernvale "Group".||||||21-MAR-13
8762|Ipswich Coal Measures|44703|14|Not recorded|Map|||||||||
8762|Ipswich Coal Measures|44705|14|Not recorded|p1,15|||||||||
8762|Ipswich Coal Measures|44706|14|Not recorded|p413-415|||||||||
8762|Ipswich Coal Measures|44707|14|Not recorded|p1,3,5|||||||||
8762|Ipswich Coal Measures|44708|14|Not recorded|p19,Sheet 2,section||Middle Triassic|||||||
8762|Ipswich Coal Measures|44716|14|Not recorded|p74,75,105|||||||||
8762|Ipswich Coal Measures|44734|14|Not recorded|p7-11|||||||||
8762|Ipswich Coal Measures|44771|14|Not recorded|p1,3|||||||||
8762|Ipswich Coal Measures|44772|14|Not recorded|p3|||||||||
8762|Ipswich Coal Measures|44774|6|Mentioned|p30||Middle Triassic|||||||
8762|Ipswich Coal Measures|44775|4|Described|p7,9,map 2||Triassic|||||||
8762|Ipswich Coal Measures|44776|14|Not recorded|p1,3||Middle Triassic|||||||
8762|Ipswich Coal Measures|44777|14|Not recorded|p55|||||||||
8762|Ipswich Coal Measures|44783|14|Not recorded|p2-6,9-12,16-20|||Brisbane District.||||||
8762|Ipswich Coal Measures|44786|14|Not recorded|p193-202||Permian|||||||
8762|Ipswich Coal Measures|44789|14|Not recorded|p18,19||Triassic|Unconformably overlies Bunya Phyllites||||||
8762|Ipswich Coal Measures|44801|14|Not recorded|p25|||||||||
8762|Ipswich Coal Measures|44814|14|Not recorded|p485||Middle Triassic|De Jersey: Middle-Late Triassic.||||||
8762|Ipswich Coal Measures|44828|14|Not recorded|p14|||||||||
8762|Ipswich Coal Measures|44884|14|Not recorded|p2|||||||||
8762|Ipswich Coal Measures|44913|14|Not recorded|p57,Fig.3,68|||||||||
8762|Ipswich Coal Measures|45110|6|Mentioned|p80|||||||||
8762|Ipswich Coal Measures|48917|4|Described|p9|||See also correlation P7||||||
8762|Ipswich Coal Measures|48920|6|Mentioned|p90|||||||||
8762|Ipswich Coal Measures|48928|6|Mentioned|p2|||See also P10||||||
8762|Ipswich Coal Measures|60079|5|Briefly described|Map Legend|||Equivalent to Evans Head and Red Cliff Coal Measures.||||||
8762|Ipswich Coal Measures|60281|5|Briefly described|p28, Fig.18 App1|Late Triassic|Early Triassic|Overlie the Nymboida Coal Measures; underlie the Raceview Formation.  Geological Province: Ipswich Basin.||||||20-JAN-05
8762|Ipswich Coal Measures|60726|5|Briefly described|p1-4, throughout text.|Late Triassic|Late Triassic||||Mount Crosby, Blackstone Formations.|||
8762|Ipswich Coal Measures|60991|6|Mentioned|p46|||||||||
8762|Ipswich Coal Measures|60993|5|Briefly described|p5, p6 Fig. 2|Carnian (Late Triassic)|Carnian (Late Triassic)|Unconformably overlain by the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. Equivalent to Evans Head Coal Measures. ||||||
8762|Ipswich Coal Measures|60995|5|Briefly described|p52 Tb. 1|Late Triassic|Late Triassic|Includes Redcliff and Evans head Coal Measures. Geological Province: Clarence-Moreton Basin. Coal Measures is written as C.M. in text.  See also p51 Fig. 3 (equivalents mentioned). ||||||
8762|Ipswich Coal Measures|60996|5|Briefly described|p73|||Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|60997|5|Briefly described|p140 Fig. 2|||Overlain by the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|61002|5|Briefly described|p198, p202|Late Triassic|Late Triassic|Conformably overlie Chillingham Volcanics. Age is Carnian. Geological Province: Ipswich Basin.See also p199 Fig. 3. ||||||
8762|Ipswich Coal Measures|61004|5|Briefly described|p230, p232 Fig. 2|Triassic|Triassic|Contains minor component inertinite.   Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|61005|5|Briefly described|p239, p242|Late Triassic|Late triassic|Geological Province: Ipswich Basin.  See also p248.||||||
8762|Ipswich Coal Measures|61006|5|Briefly described|p278 Fig. 2|Triassic|Triassic|Contain coal and carbonaceous shale. Underlie the Clarence-Moreton Basin. ||||||
8762|Ipswich Coal Measures|61310|4|Described|p16, p11 Fig. C2|Late Triassic|Late Triassic|Considered to have both hydrocarbon source and reservoir potential. Overlie Nymboida Coal Measures and Chillingham Volcanics. Geological Province: Clarence-Moreton Basin. Equivalents are Red Cliff and Evans Head Coal Measures.||||||
8762|Ipswich Coal Measures|61772|6|Mentioned|p129, p130 Fig. 5||Late Triassic|Contains tuffs.||||||24-SEP-08
8762|Ipswich Coal Measures|63117|6|Mentioned|p158, p162|||Contains Ginkgoites fossils.||||||
8762|Ipswich Coal Measures|63979|6|Mentioned|p31|||In south eastern Queensland.||||||07-FEB-11
8762|Ipswich Coal Measures|64298|6|Mentioned|p122|||||||||
8762|Ipswich Coal Measures|64665|5|Briefly described|p53 Fig.2, p57.|Late Triassic|Late Triassic|Ipswich Basin. First coal mined in Queensland. Up to 1200 m thick. Dominantly bright coal with some interbanded bright and dull coal; ash content generally high; rank is high volatile bituminous; predominantly thermal, some local coking coal in the north.|||Includes Kholo and Brassall Subgroups.|Is unconformably overlain by Bundamba Group.||
8762|Ipswich Coal Measures|65003|5|Briefly described|p7|||Of Clarence-Moreton Basin.||||Unconformably overlain by the Bundamba Group.|Shale, conglomerate, sandstone, coal, siltstone, basalt and tuff.|30-MAR-12
8762|Ipswich Coal Measures|67402|4|Described|p186, p205, p209, p222-p225|Late Triassic|Late Triassic|Clarence-Moreton Basin. Maximum thickness of 1200m.  |||Includes the Kholo and Brassall Subgroups.|Overlies the Neara Volcanics.|Conglomerates, sandstones, shales, coals and minor volcanics.|
8762|Ipswich Coal Measures|68008|6|Mentioned|p220, p261|Late Triassic|Late Triassic|||||Correlated with Callide Coal Measures.||
8762|Ipswich Coal Measures|68327|5|Briefly described|Map legend.|Triassic|Triassic||||||Conglomerate, sandstone, shale, tuff, coal seams.|
8762|Ipswich Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Ipswich Basin.||||||
8762|Ipswich Coal Measures|68579|6|Mentioned|p221, 222|||||||Overlain unconformably by Redbank Plains Formation.||26-APR-13
8762|Ipswich Coal Measures|68679|5|Briefly described|p321, p388, p391-395, p398-399, p435|Late Triassic|Late Triassic|Ipswich Basin, northern New England Orogen. Appears as Ipswich Basin Coal Measures on p321. Represents a thermal relaxation phase. ~1200m thick. Previously considered equivalent to Nymboida Coal Measures, but contradicted by macrofloral and radiometric dating. Carnian-Norian age.|||Kholo and Brassall Subgroups.|Unconformably overlies Neranleigh-Fernvale beds. Is overlain unconformably by the Woogaroo Subgroup (Bundamba Group). Equivalent to the Evans Head and Red Cliff, Coal Measures.||
8762|Ipswich Coal Measures|69297|6|Mentioned|p370, p386, p487 fig 5.38, p488|Lower Jurassic|Middle Triassic|Clarence-Moreton Basin. Gas prone source rocks are present. |||||Coal and mudstones.|
8762|Ipswich Coal Measures|69594|5|Briefly described|p519, p543, p545-546|Late Triassic|Late Triassic|Ipswich Basin.||||Overlies Chillingham Volcanics and Brisbane Tuff. Is overlain unconformably by Bundamba Group.||
8762|Ipswich Coal Measures|69599|5|Briefly described|p610|||Offshore Ipswich Basin. A 277m succession of carbonaceous sediments with several igneous intervals, intersected in APS Matjara 1 drilled 15km off Moreton Island, is interpreted as this unit. The igneous rocks compared with the Brisbane Tuff.||||||
8762|Ipswich Coal Measures|72297|5|Briefly described|p698, p700|Triassic|Triassic|Ipswich Basin. Mining ceased in 2003 after 160 years of continuous mining.|||Tivoli Formation.||High-volatile, low-sulfur bituminous coals.|
8762|Ipswich Coal Measures|73294|6|Mentioned|p1014, p1006|late Triassic|late Triassic|Late Triassic Craterisporites rotundus spore-pollen zone age. Correlated with the Brisbane Tuff. Misspelt as Ipswich Coal measures p1006.||||||
8762|Ipswich Coal Measures|73570|6|Mentioned|p912 Fig.2|||||||Underlies Laytons Range Conglomerate||
8773|Iron Hut Quartz Monzonite|42747|5|Briefly described|p40, Fig.9|||see also Table 1||||||
8773|Iron Hut Quartz Monzonite|43029|2|Defined|p15||Devonian|see also Fig.2,p16||||||
8773|Iron Hut Quartz Monzonite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
8773|Iron Hut Quartz Monzonite|43213|3|Fully described|p88,p96-97, p102-103, p116-121, p174-175|Devonian|Devonian|See also p178, p208, p214-215, p231, p240, p243. Northern end of Retreat Batholith; centred on Theresa Creek Dam. Forms tors and boulders. Very strongly magnetic. Type locality described. The Silver Hills Volcanics separate this unit from the Sunny Park Granodiorite. Geochemistry, modal analyses and geophysics detailed.||||Intrudes Theresa Creek Volcanics. Is overlain unconformably by Silver Hills Volcanics. Is intruded by Hoy Basalt.|Grey, fine- to medium-grained, equigranular to porphyritic hornblende-biotite quartz monzonite; includes pink to grey, fine- to medium-grained porphyritic micromonzonite.|
8773|Iron Hut Quartz Monzonite|69952|5|Briefly described|p115, p118|||Inferred Devonian age (Withnall et al., 1995) based on similarities with Stevenson Quartz Monzodiorite.||||Intrudes Theresa Creek Volcanics.||
8804|Isla Formation|35873|6|Mentioned|Fig.9|||||||||
8804|Isla Formation|43991|4|Described|p44,46|||Conformably overlies Kia-Ora Formation.||||||
8804|Isla Formation|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|Part of Theodore Group.||||||
8804|Isla Formation|44514|2|Defined|p27,32|Triassic|Late Permian|Conformable between Clematis Sandstone above Kia-Ora below.||||||
8804|Isla Formation|44571|2|Defined|p205|||Overlies Kia-Ora Formation.||||||
8804|Isla Formation|45095|5|Briefly described|p55|||Refers Derrington & Morgan (1960)||||||
8804|Isla Formation|48919|4|Described|Table 3|||||||||
8815|Ixe Microgranodiorite|23291|5|Briefly described|p101 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Ixe Suite. Intrudes Fulford Creek granite. Age: ~320 Ma. Geological Province: Georgetown Region.||||||08-JUL-15
8815|Ixe Microgranodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 336. I-Type.||||||
8815|Ixe Microgranodiorite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
8815|Ixe Microgranodiorite|39445|5|Briefly described|Table 12|||||||||
8815|Ixe Microgranodiorite|42547|5|Briefly described|p75|||||||||
8815|Ixe Microgranodiorite|43259|4|Described|Appendix 1,p39.||Carboniferous|||||||
8815|Ixe Microgranodiorite|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
8815|Ixe Microgranodiorite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
8815|Ixe Microgranodiorite|45014|2|Defined|p24,102-106,Pl.38||Neoproterozoic|Tb.1||||||
8815|Ixe Microgranodiorite|45025|4|Described|p74-75|Permian|Carboniferous|||||||
8815|Ixe Microgranodiorite|45113|3|Fully described|p17|||Emphasis on petrography.||||||
8815|Ixe Microgranodiorite|48976|5|Briefly described|p32|||Isotopic data Table 6||||||
8815|Ixe Microgranodiorite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Fine-grained, porphyritic biotite granodiorite to granite.|
8817|Jabiru Formation|29387|6|Mentioned|Table 3|||Lower Permian.||||||
8855|Jamieson Member|23032|5|Briefly described|p31|||||||||
8855|Jamieson Member|23424|5|Briefly described|Table 8.1 p336.|Famennian|Frasnian|Upper part of Bulgeri Formation. Age: Famennian; marine fossils. Of Bulgeri Formation/Bundock Creek Group, Bundock Basin.||||||
8855|Jamieson Member|24613|5|Briefly described|p77|Late Devonian|Late Devonian|Of the Bulgeri Formation. Age is probably Famennian.||||||07-FEB-11
8855|Jamieson Member|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|Not a variation on Jamieson Formation, NT & WA, or Jamieson Member WA.||||||21-JUN-13
8855|Jamieson Member|42933|4|Described|p130|||Of  Bulgeri Formation.||||||27-MAY-09
8855|Jamieson Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bulgeri Formation.||||||
8855|Jamieson Member|68336|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.|||Medium- to very coarse-grained sandstone, cobbly-pebbly conglomerate, fine-grained redbeds, grey siltstone and reworked tuff, rare marine fossils.|
8855|Jamieson Member|68341|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.|||Medium- to very coarse-grained sandstone, cobbly-pebbly conglomerate, fine-grained redbeds, grey siltstone and reworked tuff, rare marine fossils.|
8855|Jamieson Member|68478|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin. Occurs locally at the top of the Bulgeri Formation. The 5 facies are mapped separately.||Of the Bulgeri Formation.||Conformably overlain by the Turrets Formation.|Medium to very coarse-grained sandstone, cobbly-pebbly conglomerate, fine-grained redbeds, grey siltstone and reworked tuff, rare marine fossils.|
8855|Jamieson Member|68479|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin. Occurs locally at the top of the Bulgeri Formation. The 5 facies are mapped separately.||Of the Bulgeri Formation.||Conformably overlain by the Turrets Formation. Shown as younger than the Stopem Blockem Conglomerate Member.|Medium to very coarse-grained sandstone, conglomerate and minor calcirudite.|
8855|Jamieson Member|69592|4|Described|p259, p273|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. Up to 670m thick. A marine-fossiliferous mudstone or calcareous sandstone interval occurs in the middle section.||Topmost Bulgeri Formation.||Overlies Stopem Blockem Conglomerate Member. Is overlain by Turrets Formation.|Medium- to coarse-grained, locally pebbly, feldspathic to volcaniclastic sandstone with fine sandstone or siltstone interbeds; pebble conglomerate horizons are characteristic of its lower part.|
8869|Janet Ranges Volcanics|22811|5|Briefly described|p603|Permian|Permian|of Kennedy Province||||||
8869|Janet Ranges Volcanics|23420|5|Briefly described|p 146 table 4.5|Early Permian|Late Carboniferous|Also see p 129.Variation on Janet Ranges Volcanic Group. I-type characteristics. Intruded by Weymouth Granite.||||||30-APR-13
8869|Janet Ranges Volcanics|23425|5|Briefly described|p372|||||||||
8869|Janet Ranges Volcanics|23431|6|Mentioned|p535|||||||||
8869|Janet Ranges Volcanics|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
8869|Janet Ranges Volcanics|32528|5|Briefly described|Table 2|||||||||
8869|Janet Ranges Volcanics|32563|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
8869|Janet Ranges Volcanics|33226|6|Mentioned|Map legend|Early Permian|Carboniferous|Carboniferous to Early Permian||||||
8869|Janet Ranges Volcanics|33773|4|Described|Table 1|||||||||
8869|Janet Ranges Volcanics|33880|6|Mentioned|Map legend|Early Permian|Early Carboniferous|Lower Carboniferous to Lower Permian||||||
8869|Janet Ranges Volcanics|33882|4|Described|Table 1|||P12||||||
8869|Janet Ranges Volcanics|34581|2|Defined|p140|Permian|Carboniferous|Carboniferous - Permian||||||
8869|Janet Ranges Volcanics|37613|6|Mentioned|p247|||See also Fig.2||||||
8869|Janet Ranges Volcanics|39252|6|Mentioned|Fig.11|||||||||
8869|Janet Ranges Volcanics|39445|5|Briefly described|Table 7|||||||||
8869|Janet Ranges Volcanics|42327|6|Mentioned|Fig. 22 P15|||||||||
8869|Janet Ranges Volcanics|42547|5|Briefly described|p73, p74|||||||||
8869|Janet Ranges Volcanics|43567|5|Briefly described|p402|Permian|Carboniferous|||||||
8869|Janet Ranges Volcanics|43708|6|Mentioned|Fig.1b,p3||Proterozoic|||||||
8869|Janet Ranges Volcanics|43741|6|Mentioned|p16|Permian|Carboniferous|||||||
8869|Janet Ranges Volcanics|45076|3|Fully described|p108|||Late Pal. See P17.||||||
8869|Janet Ranges Volcanics|49769|6|Mentioned|p4|||||||||
8869|Janet Ranges Volcanics|63154|5|Briefly described|p285 Fig. 5|Early Permian|Late Carboniferous|Geological province: Coen Inlier.||||||
8869|Janet Ranges Volcanics|69591|5|Briefly described|p101-102|Permian|Permian|Trail et al. (1969). Believed to postdate the rocks filling the Pascoe River Basin. Undated; assumed to be early Permian.||||Overlies Pascoe River beds.|Rhyolite flows, volcanic breccias, welded tuff and rhyolite.|
8869|Janet Ranges Volcanics|70207|6|Mentioned|p126|Permian|Late Carboniferous|||||||
8869|Janet Ranges Volcanics|71792|5|Briefly described|p2, p22-p23, p33-p39|Early Permian|Early Permian|Northern Coen Inlier. Outcrops extensively on the Cape Weymouth Map Sheet area. No mineralisation is known in this unit, however, prospectivity for epithermal minerals is considered high. Distribution, outcrop characteristics and geophysical characteristics are discussed. In previous extensive mapping this unit was divided into three informal subunits. Intruded by the Weymouth Granite. Equivalent to the Kangaroo River Volcanics. |284.7 +/- 1.7 Ma (Cross et al, in prep)|Janet Ranges Volcanic Group||Unconformably overlies the Choc-a-block Orthogneiss and the Pascoe River Beds. Overlain by the Garraway Sandstone and/or the Yam Creek Beds.|Rhyolitic ignimbrite and breccia, rhyolite lava and autobreccia, volcaniclastic conglomerate and sandstone.|
8869|Janet Ranges Volcanics|71849|5|Briefly described|p6, p11, p144||||284.7 +/- 1.7 Ma (SHRIMP; Cross et al. in prep).||||Includes rhyolitic ignimbrite.|
8869|Janet Ranges Volcanics|71853|5|Briefly described|Map legend.|Permian|Permian|The two facies are mapped separately.||Janet Ranges Volcanic Group.|||Rhyolitic welded tuff, rhyolite, welded pumice-flow breccia; minor volcanic breccia and hornfels. Coherent and autoclastic rhyolite lavas, domes or cryptodomes; high radiometric response.|
8869|Janet Ranges Volcanics|73083|6|Mentioned|p56-57|Carboniferous|Carboniferous||||||Felsic volcanic rocks.|
8952|Jiggamore Member|22954|4|Described|Fig1p6,17,21-2||Datsonian|||||||
8952|Jiggamore Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
8952|Jiggamore Member|37572|4|Described|p162|||||||||
8952|Jiggamore Member|38532|4|Described|p242|||||||||
8952|Jiggamore Member|40136|5|Briefly described|p28|||||||||
8952|Jiggamore Member|42354|6|Mentioned|p11|||Of Ninmaroo Formation||||||
8952|Jiggamore Member|46897|6|Mentioned|p351|||||||||
8952|Jiggamore Member|46958|6|Mentioned|p195|||||||||
8952|Jiggamore Member|64068|4|Described|p74|Late Cambrian|Late Cambrian|186 m thick in type section.||Of Ninmaroo Formation.||Overlies Unbunmaroo Member. Is overlain by Mort Member.|Ribbon limestone, ooid, peloid, and peloid-intraclast grainstone, calcimudstone, dolostone, dolomitic breccia.|05-APR-12
8952|Jiggamore Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin||Cockroach Group|||Thin to thick-bedded limestone (peloid and intraclast grainstone, micrite, two-toned limestone), calcareous siltstone|
8952|Jiggamore Member|69377|5|Briefly described|map legend|Early Ordovician|Late Cambrian|||Ninmaroo Formation|||Thin- to thick-bedded limestone (peloid and intraclast grainstone, micrite, two-toned limestone) and calcareous limestone|
8989|Jinker Creek Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Wirra Volcanic Subgroup. Age: 329+/-9Ma (Black & Holmes, unpub.ms.). Thickness: Up to 550m. Geological Province: Georgetown Region.||||||26-MAY-15
8989|Jinker Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V23. I-Type.||||||
8989|Jinker Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
8989|Jinker Creek Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Wirra Volcanic Subgroup.||||||
8989|Jinker Creek Rhyolite|43740|4|Described|p8|||||||||
8989|Jinker Creek Rhyolite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Wirra Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
8989|Jinker Creek Rhyolite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Wirra Volcanic Subgroup.|||Grey to brown, crystal-rich rhyolitic ignimbrite (50-70% quartz and feldspar, sparse to rare hornblende and biotite crystals).|
8989|Jinker Creek Rhyolite|69593|5|Briefly described|p512|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|330 Ma.|Newcastle Range Volcaniuc Group.|||I-type.|
8991|Jochmus Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Galilee Basin||||||
8991|Jochmus Formation|22464|5|Briefly described|p9|Early Permian|Silesian|Cooper Basin||||||
8991|Jochmus Formation|23430|4|Described|p519 Table 14.6|||Maximum thickness <750 m.||||||
8991|Jochmus Formation|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
8991|Jochmus Formation|31120|6|Mentioned|p155|||||||||
8991|Jochmus Formation|31121|6|Mentioned|p385|||||||||
8991|Jochmus Formation|31122|2|Defined|p350|Early Permian|Early Permian|||||||
8991|Jochmus Formation|31258|4|Described|p101|||re petroleum prospects||||||
8991|Jochmus Formation|31860|6|Mentioned|p277|||See also P280||||||
8991|Jochmus Formation|32138|6|Mentioned|p397|||||||||
8991|Jochmus Formation|33372|5|Briefly described|p16|||See also P22. From wells.||||||
8991|Jochmus Formation|33674|4|Described|p439|||Lithology.||||||
8991|Jochmus Formation|35457|6|Mentioned|p627|||Also Fig.4 biostratigraphic relationships.||||||
8991|Jochmus Formation|35845|6|Mentioned|Fig.25|||||||||
8991|Jochmus Formation|36243|6|Mentioned|Table 5A|||||||||
8991|Jochmus Formation|36562|6|Mentioned|p547|||||||||
8991|Jochmus Formation|36921|4|Described|p183|||See also Table 1.||||||
8991|Jochmus Formation|37451|6|Mentioned|Table 2|||||||||
8991|Jochmus Formation|37610|3|Fully described|p301|||See also Fig.3.||||||
8991|Jochmus Formation|39252|6|Mentioned|p13|||||||||
8991|Jochmus Formation|39261|6|Mentioned|Fig. 9|||||||||
8991|Jochmus Formation|39264|6|Mentioned|Fig. 13|||||||||
8991|Jochmus Formation|39265|6|Mentioned|Fig. 3|||||||||
8991|Jochmus Formation|39445|5|Briefly described|Table 7|||||||||
8991|Jochmus Formation|39478|6|Mentioned|Table 1|||||||||
8991|Jochmus Formation|39943|6|Mentioned|Table 7A|||||||||
8991|Jochmus Formation|39989|6|Mentioned|p426|||||||||
8991|Jochmus Formation|39991|6|Mentioned|p428|||||||||
8991|Jochmus Formation|40123|6|Mentioned|p465|||||||||
8991|Jochmus Formation|41116|5|Briefly described|p431|||||||||
8991|Jochmus Formation|41198|6|Mentioned|Table 1|||||||||
8991|Jochmus Formation|41707|6|Mentioned|Fig.6|||||||||
8991|Jochmus Formation|41710|6|Mentioned|Fig.2|||||||||
8991|Jochmus Formation|42446|3|Fully described|p7|||||||||
8991|Jochmus Formation|42447|6|Mentioned|Fig. 2|||||||||
8991|Jochmus Formation|42474|6|Mentioned|p25|||||||||
8991|Jochmus Formation|42491|6|Mentioned|p5|||||||||
8991|Jochmus Formation|42547|4|Described|p80|||||||||
8991|Jochmus Formation|42999|5|Briefly described|p95,Table1,p90|||||||||
8991|Jochmus Formation|43105|5|Briefly described|p13|||||||||
8991|Jochmus Formation|43114|4|Described|p6|||||||||
8991|Jochmus Formation|43812|6|Mentioned|Fig.3,p145|||||||||
8991|Jochmus Formation|46849|6|Mentioned|Fig. 7|||||||||
8991|Jochmus Formation|63713|5|Briefly described|p1505, p1507 Fig.2, p1508|Cisuralian|Cisuralian|Lovelle depression, Galilee Basin. Early Permian.||Unit in Joe Joe Group.||Overlies Jericho Formation. Is overlain by Reids Dome Beds.||
8991|Jochmus Formation|64288|5|Briefly described|p532 Fig.1|Sakmarian|Moscovian|||Unit in Joe Joe Group.||Overlies Jericho Formation. Is overlain by Aramac Coal Measures.||
8991|Jochmus Formation|65489|5|Briefly described|p143, p144 Fig.53|Asselian|Late Carboniferous|Lovelle Depression, Galilee Basin.|||Includes Eddie Tuff Member.|Is overlain by Aramac Coal Measures.||
8991|Jochmus Formation|66188|6|Mentioned|439, 443, Fig 3, TB1, Fig 16-17|Early Permian|Late Carboniferous|||||||
8991|Jochmus Formation|67323|5|Briefly described|p84, p88, p93 Fig.12.3|Permian|Carboniferous|Lovelle Depression, eastern Galilee Basin. Glacial and fluvial deposits. Hydrocarbon source potential.||||Is overlain by Aramac Coal Measures.||
8991|Jochmus Formation|67402|5|Briefly described|p124 fig GLL1, p125 tbl GLL1|Artinskian|Sakmarian|Galilee Basin. Best potential reservoir for storage of carbon dioxide in the Galilee Basin. See also p127 fig GLL5, p129 fig GLL9, p131 fig GLL12, p132, p135-p138.|||Includes the Eddie Tuff Member|Overlain by the Aramac Coal Measures, unconformably overlain by the Colinlea Sandstone. Overlies the Jericho Formation.|Carbonaceous siltstone, tuffaceous-carbonaceous mudstone and volcano-lithic labile sandstone that is locally conglomeratic with numerous tuff horizons.|
8991|Jochmus Formation|67561|6|Mentioned|p53 Fig.3|||||||||
8991|Jochmus Formation|68279|6|Mentioned|p4|Sakmarian|Kasimovian|Galilee Basin.||Unit in Joe Joe Group.||Overlies Jericho Formation.||
8991|Jochmus Formation|68413|5|Briefly described|Map Legend|Early Permian|Early Permian|Galilee Basin? Early Permian age.||||Conformably underlain by the Jericho Formation.|Sandstone, siltstone, mudstone, conglomerate, tuff.|
8991|Jochmus Formation|68731|6|Mentioned|p198, p200 Fig 3.110, p201 Fig 3.110|Cisuralian|Cisuralian|A facies variant, in its upper part, of the Aramac Coal Measures.||Of the Joe Joe Group.||||
8991|Jochmus Formation|69582|6|Mentioned|p65-p66|Cisuralian|Late Carboniferous|Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Jericho Formation. Overlain by the Aramac Coal Measures.||
8991|Jochmus Formation|70837|5|Briefly described|p246|Cisuralian|Cisuralian|Of Galilee Basin.|||Includes Edie Tuff.|||
8991|Jochmus Formation|71265|5|Briefly described|p589|Artinskian|Kasimovian|Galilee Basin.||Joe Joe Group.|Edie Tuff Member.|Overlies Jericho Formation. Is overlain by Aramac Coal Measures or Colinlea Sandstone.||
8991|Jochmus Formation|71701|4|Described|p155-p158, p167, p169|Artinskian|Kasimovian|Central Western Area, Eastern Area, Galilee Basin.||Joe Joe Group|Includes the Edie Tuff Member.|Overlies the Jericho Formation. Overlain by the Aramac Coal Measures.||
8991|Jochmus Formation|71710|5|Briefly described|p378-381, p385, p386|||Galilee Basin. See also: Upper Jochmus Formation and Lower Jochmus Formation. Deposited as part of basin overfill during thermal subsidence, characterised by slow rate of subsidence. Known only from drill core?||Uppermost unit of the Joe Joe Group. |Informally subdivided into lower and upper parts, with Edie Tuff Member between.|Overlies Jericho Formation, at sequence boundary. Basin wide hiatus between 295-290 Ma between Jochmus Formation and overlying Betts Creek beds in Galilee Basin.|Interbedded labile sandstone, siltstone and mudstone. Sandstone - fine- to med-grained, moderately/well sorted, locally conglomeratic. Siltstone - argillaceous to sandy + carbonaceous. Mudstone - micaceous, carbonaceous + in places tuffaceous.|
8991|Jochmus Formation|72088|4|Described|p8, p17-p18, p91|Cisuralian|Pennsylvanian|Lovelle Depression and Koburra Trough, Galileee Basin. Deposited in a fluvio-lacustrine environment under glacial influence. ||Joe Joe Group|Includes the Edie Tuff Member.|Conformably overlain by the Aramac Coal Measures. Unconformably overlain by the Betts Creek Beds. Overlies the Jericho Formation.|Sandstone, siltstone and varved mudstone.|
8991|Jochmus Formation|73163|5|Briefly described|p467, p470-471|Asselian|Asselian|Galilee Basin.||Joe Joe Group|Edie Tuff Member|Overlies the Jericho Formation. Underlies the Aramac Coal Measures.|Mostly fine- to medium-grained sandstone with siltstone, mudstone, and tuff near top.|02-FEB-22
8991|Jochmus Formation|73472|6|Mentioned|p115-116|Sakmarian|Kasimovian|Galilee Basin.||Joe Joe Group|Edie Tuff Member|Overlain by Aramac Coal Measures. Underlain by Jericho Formation. Equivalent to Boonderoo beds.||
8991|Jochmus Formation|73495|6|Mentioned|p500||||||Edie Tuff Member|||
9007|Johngboon Rhyolite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Parent: Aranbanga Volcanic Group.||||||14-AUG-08
9007|Johngboon Rhyolite|41738|2|Defined|p171|Late Triassic||Reserved as Johngboon.||||||14-AUG-08
9007|Johngboon Rhyolite|41790|6|Mentioned|p474|||||||||
9007|Johngboon Rhyolite|42054|6|Mentioned|p272|||||||||
9007|Johngboon Rhyolite|63821|5|Briefly described|p21, p22|||Part of the Aranbanga Volcanic Group. Contains the Cambalanga Tuff Member. Crystal-poor, welded tuff to ignimbrite.||||||07-FEB-11
9007|Johngboon Rhyolite|67874|5|Briefly described|p2-3, p7, p40-43, p51|Late Triassic|Middle Triassic|Mungore Cauldron. An intra-caldera ignimbrite. Co-genetic with Mungore Granite. SHRIMP U-Pb zircon magmatic crystallisation age.|227.9 +/- 1.4 Ma (Cross et al., 2012).|Aranbanga Volcanic Group.||Is intruded by Mungore Granite.|Includes pink, lithic- and crystal-rich ignimbrite.|
9007|Johngboon Rhyolite|68679|4|Described|p437, p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. Maximum thickness 300-400m. Intracaldera fill of Mungore Caldera; ignimbrite has same mineralogy and chemistry as ring dyke.|229.7 +/- 1.4 Ma (SHRIMP: Cross et al., 2012).|Aranbanga Volcanic Group.|Cambalanga Tuff Member.||Two basal deposits: a fine boundary layer with rare charcoal, then a bedded tuff, overlain by rhyolite breccia (0-50m thick) that grades upwards into rhyolitic ignimbrite: massive, welded, crystal to lithic-rich and forms a single cooling unit.|
9007|Johngboon Rhyolite|71592|5|Briefly described|Appendix A.|||New England Orogen.|228+/-1.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
9007|Johngboon Rhyolite|73450|5|Briefly described|p30, p34-35|Norian|Carnian|Up to 400 m thick. U-Pb SHRIMP zircon age of 227.9 +/- 1.4 Ma (Cross et al., 2012).|227.9 +/- 1.4 Ma U-Pb SHRIMP||||Massive, welded, crystal-rich (quartz) rhyolitic ignimbrite.|
9016|Jollys Lookout Andesite|33289|5|Briefly described|p163|||See also PP164,166. Perm.||||||
9016|Jollys Lookout Andesite|35007|6|Mentioned|p75|||||||||
9016|Jollys Lookout Andesite|35812|6|Mentioned|p568|||See also Fig.2||||||
9016|Jollys Lookout Andesite|36440|6|Mentioned|Map legend|Early Triassic|Late Permian|Early Triassic to Late Permian||||||
9016|Jollys Lookout Andesite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
9016|Jollys Lookout Andesite|38074|5|Briefly described|Table 1|||||||||
9016|Jollys Lookout Andesite|39079|6|Mentioned|p8|||||||||
9016|Jollys Lookout Andesite|39252|6|Mentioned|p27|||||||||
9016|Jollys Lookout Andesite|40623|5|Briefly described|p20|||||||||
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.||
9059|Jukes Granite|23042|5|Briefly described|p105|||||||||
9059|Jukes Granite|40577|3|Fully described|p56|||||||||
9059|Jukes Granite|40954|6|Mentioned|p133|||||||||
9059|Jukes Granite|61917|5|Briefly described|Map legend|Tertiary|Tertiary|Hypersolvus granite containing minor clinopyroxene and biotite.||||||
9059|Jukes Granite|65388|4|Described|p420-421 ,422, p403 Fig. 135|Oligocene|Oligocene|Of Mount Jukes Intrusive Complex. Younger than Blackwood Quartz Syenite, probably older than Seaforth Microgranite. Hypersolvus syenogranite, within the centre of (intrudes?) the Neilson Leucogabbro. Also shown as Mount Jukes Granite p421.||||||08-SEP-14
9059|Jukes Granite|69599|5|Briefly described|p634|||1-2 km2. Forms steep-sided, flat-topped Mount Jukes.||Mount Jukes Intrusive Complex.||Intrudes the Neilson Leucogabbro.|Hypersolvus granite, with microperthitic alkali feldspar. Radial and concentric microgranite dykes with a variety of textures occur around the unit.|
9059|Jukes Granite|73450|4|Described|p45, p71-74|Rupelian|Priabonian|Forms a distinctive flat-topped and steep sided mountain surrounded by an extensive talus apron. Surrounded by radial and concentric dykes probably emplaced prior to the granite (Stephenson, 1985). Ar-Ar age of 33.6 +/- 0.5 Ma (Cohen, 2007).|33.6 +/- 0.5 Ma Ar-Ar|Mount Jukes Intrusive Complex|||Hypersolvus granite with miarolitic cavities.|
9065|Julia Formation|23422|5|Briefly described|p180, p206 Table 6.3|Late Devonian|Late Devonian|Of Dotswood Group.||||||
9065|Julia Formation|23424|6|Mentioned|p346|||Underlying unit Vanneck Formation. Burdekin Basin Province.||||||
9065|Julia Formation|23430|5|Briefly described|Plate 14.11 + p505||Devonian|Of Dotswood Group. Underlying Unit Stud Formation. Burdekin Basin Province.||||||
9065|Julia Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Dotswood Group.||||||
9065|Julia Formation|23522|5|Briefly described|p250 Fig 6|Famennian|Givetian|||||||
9065|Julia Formation|23893|5|Briefly described|p16|Late Devonian|Late Devonian|Of Dotswood Group. Geological Province: Burdekin Basin.||||||04-FEB-08
9065|Julia Formation|24577|4|Described|p752 Fig. 1, p755 Fig. 2|Famennian|Frasnian|Of the Dotswood Group. Overlain by the Myrtlevale Formation. Overlies the Stud Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
9065|Julia Formation|24613|2|Defined|p9 Fig. 4, p42-43|Frasnian|Frasnian|Supersedes Julia's Creek Fm. Conformable on Stud Fm; conformably overlain by Myrtlevale Fm. Max. thickness: ~800m. Geol.prov: Burdekin Basin. Two subunits; lower sandstone-rich section + upper pebbly sandstone to conglomeratic subunit. Details included.||||||07-FEB-11
9065|Julia Formation|24614|5|Briefly described|p191 Fig. 1|Famennian|Famennian|Of the Dotswood Group. Geological Province: Burdekin Basin. See also p196 Fig. 5.||||||07-FEB-11
9065|Julia Formation|37573|4|Described|p210|||See also Figs.7 and 8.||||||13-NOV-07
9065|Julia Formation|39445|5|Briefly described|Table 6|||||||||
9065|Julia Formation|39686|4|Described|p80|||||||||
9065|Julia Formation|40852|6|Mentioned|Fig.3.2|||Originally entered as NT unit.||||||
9065|Julia Formation|41774|6|Mentioned|p32|||||||||
9065|Julia Formation|42689|5|Briefly described|map legend|Late Devonian||||||||
9065|Julia Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
9065|Julia Formation|42933|5|Briefly described|p257|||||||||
9065|Julia Formation|43095|5|Briefly described|Plate 2|||of Dotswood Group||||||
9065|Julia Formation|43589|6|Mentioned|p24|Late Devonian|Late Devonian|Represented as a belt of hornfelsed sedimentary rocks surrounded largely by Speed Creek Granite.||||||23-APR-08
9065|Julia Formation|43933|5|Briefly described|Map Legend||Late Devonian|Of Dotswood Group.||||||
9065|Julia Formation|62522|2|Defined|p26|Famennian|Frasnian|Of Dotswood Group. Conformably overlies Stud Fm; overlain by Myrtle Fm. Max. thickness: 2000m. Geological Province: Burdekin Basin. Comprises 2 subunits: lower sandstone-rich and upper pebbly sandstone-conglomerate, medium to very thick bedded.||||||
9065|Julia Formation|65214|6|Mentioned|p279, p280, p283|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
9065|Julia Formation|67402|4|Described|p239, p246, p247, p248|Famennian|Frasnian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under upper alluvial plain and alluvial fan conditions. ||||Overlies the Stud Formation.|Medium to coarse-grained sandstones and pebbly sandstones.|
9065|Julia Formation|68350|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Stud Formation. Is overlain conformably by Myrtlevale Formation (Keelbottom Group).|Medium- to coarse-grained feldspathic to quartzose sandstone, polymictic conglomerate, red calcareous mudstone and siltstone.|
9065|Julia Formation|68351|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Stud Formation. Is overlain conformably by Myrtlevale Formation (Keelbottom Group).|Medium- to coarse-grained feldspathic to quartzose sandstone, polymictic conglomerate, red calcareous mudstone and siltstone.|14-JUL-14
9065|Julia Formation|68419|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin.||Of the Dotswood Group.||Conformably overlain by the Myrtlevale Formation (Keelbottom Group). Conformably underlain by the Stud Formation.|Medium to coarse-grained feldspathic to quartzose sandstone, polymictic conglomerate and red calcareous mudstone and siltstone.|
9065|Julia Formation|68420|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin.||Of the Dotswood Group.||Conformably overlain by the Myrtlevale Formation (Keelbottom Group). Conformably underlain by the Stud Formation.|Medium to coarse-grained feldspathic to quartzose sandstone, polymictic conglomerate and red calcareous mudstone and siltstone.|
9065|Julia Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4,  p186|Late Devonian|Late Devonian|Burdekin Basin. Upper alluvial plain to distal alluvial fan. Limestone conglomerate clasts identify the Burdekin Formation as a sediment source (paleocurrent vectors suggest to the south). < 200 m thick.||Of the Dotswood Group.||Likely coeval with the Kukiandra Formation.|Comprises medium-grained to very coarse-grained lithofeldspathic quartzose and volcanolithic pebbly sandstone, granule to cobble conglomerate with mostly quartz, but subordinate volcanic and limestone, clasts. Minor fine sandstone and siltstone.|14-JUL-14
9076|Junction Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
9076|Junction Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 290. I-Type.||||||
9076|Junction Microgranite|41297|6|Mentioned|Fig.1|||||||||
9076|Junction Microgranite|41740|6|Mentioned|p222|||||||||
9076|Junction Microgranite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
9076|Junction Microgranite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Topaz-bearing microgranite; with associated Sn mineralisation. I-type.||||||07-FEB-11
9108|Kajabbi Formation|35939|2|Defined|p632|Middle Cambrian|Middle Cambrian|||||||
9108|Kajabbi Formation|36937|6|Mentioned|p229|||||||||
9108|Kajabbi Formation|39445|5|Briefly described|Table 4|||||||||
9108|Kajabbi Formation|39492|6|Mentioned|p31|||||||||
9108|Kajabbi Formation|39799|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
9108|Kajabbi Formation|40648|6|Mentioned|p10|||||||||
9108|Kajabbi Formation|50332|5|Briefly described|p22|Cambrian|Cambrian|Unconformably underlain by Quamby Conglomerate and Corella Formation. Comprises flaggy limestone and sandstone.||||||07-FEB-11
9108|Kajabbi Formation|64068|6|Mentioned|p225|||Of Narpa Group. Eastern Georgina Basin?||||||
9108|Kajabbi Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin||Narpa Group|||Calcareous siltstone, limestone, sandstone, quartzite, chert|
9108|Kajabbi Formation|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
9108|Kajabbi Formation|69573|6|Mentioned|p659, 661|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites.||||||
9108|Kajabbi Formation|69591|5|Briefly described|p92|Cambrian|Cambrian|Wilson, Gunn and Smit (1979). Forms an isolated belt in a graben near Kajabbi, N of Cloncurry. Has similar lithology and fauna to Devoncourt Limestone.||||||
9108|Kajabbi Formation|70574|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian||||||Calcareous siltstone, limestone, quartzose to lithofeldspathic sandstone and chert.|
9108|Kajabbi Formation|71592|5|Briefly described|Appendix A.|||Millungera Basin.|700+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
9108|Kajabbi Formation|73553|6|Mentioned|p9|Cambrian|Cambrian||||||Sedimentary.|
9136|Kalkadoon Granodiorite|23430|5|Briefly described|p451|||||||||
9136|Kalkadoon Granodiorite|23518|5|Briefly described|p9 Fig.3, p10|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province.||||||
9136|Kalkadoon Granodiorite|23545|5|Briefly described|p605.|||also see Table 1 p606.||||||
9136|Kalkadoon Granodiorite|24197|5|Briefly described|p21, p93|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Age: 1860Ma. Geological province: Mount Isa Inlier. See also p94 Tb. 12.1 (Table numbered incorrectly as Tb. 1.1).||||||07-FEB-11
9136|Kalkadoon Granodiorite|33897|6|Mentioned|p1280|||||||||
9136|Kalkadoon Granodiorite|38900|1|Redefined|p68|Paleoproterozoic|Paleoproterozoic|See also P55||||||07-NOV-08
9136|Kalkadoon Granodiorite|39622|6|Mentioned|Appendix|||||||||
9136|Kalkadoon Granodiorite|41961|6|Mentioned|p38|||||||||
9136|Kalkadoon Granodiorite|41979|6|Mentioned|Table 1 P510|||||||||
9136|Kalkadoon Granodiorite|42830|6|Mentioned|Fig.4 P159|||||||||
9136|Kalkadoon Granodiorite|43608|6|Mentioned|Fig.11,p11|||||||||
9136|Kalkadoon Granodiorite|44751|14|Not recorded|p305,307|||||||||
9136|Kalkadoon Granodiorite|44989|14|Not recorded|p.135,136,150,157-60|||On many pages.||||||
9136|Kalkadoon Granodiorite|45166|5|Briefly described|p73|||||||||
9136|Kalkadoon Granodiorite|48894|6|Mentioned|p31|||1364my. See also PP33,39.||||||
9136|Kalkadoon Granodiorite|50100|5|Briefly described|p11, p13 Fig. 4|Orosirian|Orosirian|Of the Kalkadoon Batholith.  Age: 1862Ma (Page, 1978) and 1856Ma (Wyborn and Page, 1983).  Intrudes the Leichhardt Volcanics. Geological Province: Western Fold Belt and Kalkadoon-Ewen Provinces.||||||06-FEB-07
9136|Kalkadoon Granodiorite|50332|5|Briefly described|p10, p16, p20, p84|Proterozoic|Proterozoic|Overlain by Surprise Creek Formation. Intrudes Leichhardt Volcanics, Candover Metamorphics and Kurbayia Migmatite.||||||07-FEB-11
9136|Kalkadoon Granodiorite|50536|5|Briefly described|p1.2, 1.4, 2.1, 5.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite. Age: 1862-1856 +/- 32Ma (U-Pb). Intruded by Wonga Suite.||||||07-NOV-08
9136|Kalkadoon Granodiorite|66529|6|Mentioned|p67, p94 |Paleoproterozoic|Paleoproterozoic|Western margin has moderate prospectivity for magmatic-hydrothermal U mineralisation.||Unit in Kalkadoon Supersuite.||||
9136|Kalkadoon Granodiorite|67323|5|Briefly described|GIS attrib tbl, p15, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River and Kalkadoon-Leichhardt Domains, Mount Isa Inlier. Kalkadoon Igneous Event.|1847 +/- 3 Ma.|Kalkadoon Supersuite.|||Medium-grained, biotite granite to granodiorite; generally with pink K-feldspar megacrysts to 2cm long; biotite generally chloritised; commonly partly chloritised ; massive to strongly foliated cut by mafic dykes; minor aplite.|
9136|Kalkadoon Granodiorite|68146|5|Briefly described|p1, p6, p57-62, p193|||Part of the crystalline basement of the Kalkadoon-Leichhardt Domain. Forms extensive pavements and rocky hills and tors. Previously mapped as undivided Tewinga Group.|1855 +/- 4 Ma protolith emplacement.||||Gneissic granite: pink, strongly to moderately deformed and foliated, megacrystic biotite granite.|
9136|Kalkadoon Granodiorite|68307|5|Briefly described|p78, p94|Paleoproterozoic|Paleoproterozoic|North Australian Craton. Part of the basement of the Mount Isa Province. Has strong magmatic arc-like geochemical signature. Grouped with the Leichhardt Volcanics as a "magmatic suite".|c.1875-1850 Ma.|||||
9136|Kalkadoon Granodiorite|69056|5|Briefly described|p52, Time-Space plot sheet;|Orosirian|Orosirian|Broadly coeval with Leichhardt Volcanics. Geochronology by Wyborn and Page (1983), Magee et al. (2012).|1862-1856 Ma.|||Intrudes Leichhardt Volcanics.|Granitoids of varying compositions.|
9136|Kalkadoon Granodiorite|69591|4|Described|p30-32, p34, p60|||Kalkadoon Batholith. Basement rocks. Mount Isa Province. Moderately to tightly folded by Barramundi Orogeny. Coeval with Nicholson Granite Complex. Ages by Magee et al. (in press) and Wyborn and Page (1983).|1857 +/- 3 Ma (Neumann et al., 2009).|Kalkadoon Suite.||Intrudes Leichhardt Volcanics.|Grey biotite (+/- rare hornblende) granodiorite and tonalite, pink biotite granite (commonly foliated, porphyritic and xenolithic); minor leucogranite, muscovite granite, microgranite, porphyritic granophyre, monzonite, diorite and aplite.|
9136|Kalkadoon Granodiorite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The porphyritic rocks are mapped separately.|||||Massive to strongly foliated, medium-grained, biotite granite to granodiorite; generally with pink K-feldspar megacrysts to 2cm; commonly partly chloritised; minor aplite; cut by mafic dykes. Coarsely porphyritic microgranite and microgranodiorite.|
9136|Kalkadoon Granodiorite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The porphyritic rocks are mapped separately.|||||Massive to strongly foliated, medium-grained, biotite granite to granodiorite; generally with pink K-feldspar megacrysts to 2cm; commonly partly chloritised; minor aplite; cut by mafic dykes. Coarsely porphyritic microgranite and microgranodiorite.|
9136|Kalkadoon Granodiorite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1855+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
9136|Kalkadoon Granodiorite|72596|6|Mentioned|p1, p54|Orosirian|Orosirian|Previouly called Kalkadoon Granite. Kalkadoon-Leichhardt Domain. Along with Leichhardt Volcanics, considered the oldest units in the domain. Included what is now Hardway Granite until 1977.|ca. 1860 Ma|||||19-JAN-22
9136|Kalkadoon Granodiorite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Leichhardt River Domain and Kalkadoon-Leichhardt Domain. Five informal subdivisions shown.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Age equivalent to Woonigan Granite, Mayfield Gneiss, Plum Mountain Gneiss.|Massive to strongly foliated, med-grained, biotite granite to granodiorite, some xenolithic; K-feldspar megacrysts common;part chloritised;minor aplite;cut by mafic dykes. Parts deeply weathered.Also diorite,migmatitic gneiss,pegmatite,leucogranite.|
9136|Kalkadoon Granodiorite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Leichhardt River Domain and Kalkadoon-Leichhardt Domain. Five informal subdivisions shown.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Age equivalent to Woonigan Granite, Mayfield Gneiss, Plum Mountain Gneiss.|Massive to strongly foliated, med-grained, biotite granite to granodiorite, some xenolithic; K-feldspar megacrysts common;part chloritised;minor aplite;cut by mafic dykes. Parts deeply weathered.Also diorite,migmatitic gneiss,pegmatite,leucogranite.|
9136|Kalkadoon Granodiorite|72889|5|Briefly described|p9, p14, p17, p18 Tb.1.2.|Orosirian|Orosirian|Previous age determinations: 1857.4+/-2.6 Ma, 1855+/-4 Ma, 1858+/-4 Ma (See Neumann et al., 2009; Carson et al., 2011; Magee et al., 2012). Intruded by dolerite dated as 1853+/- 2.9 Ma.|c. 1860-1855 Ma.|Kalkadoon Suite||Coeval with Ewen Granite. Intruded by dolerite.||25-NOV-20
9136|Kalkadoon Granodiorite|72919|6|Mentioned|p7|Orosirian|Orosirian|Mount Isa Province. Ages between ca. 1855-1860 Ma were reported previously.|ca. 1855-1860 Ma|||||
9136|Kalkadoon Granodiorite|73083|6|Mentioned|p53, p74|||||||||
9136|Kalkadoon Granodiorite|73413|6|Mentioned|p21|||||||Intrudes Leichardt Volcanics.||
9136|Kalkadoon Granodiorite|73525|5|Briefly described|p2 Fig.1, p4-5 Fig.2, p17, p19 Fig.13|Orosirian|Orosirian|Leichhardt River and Kalkadoon-Leichhardt Domains.|1857+/-3 Ma, 1849+/-4 Ma crystallisation age.||||Intermediate intrusive.|
9136|Kalkadoon Granodiorite|73553|5|Briefly described|p6, p8 Fig.1.2.3, p10, p205, p246|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain. Previously Kalkadoon Granite. Reported to be intruded by Birds Well Granite.|1855+/-4 to 1862+/-24 Ma|Kalkadoon Suite||||
9150|Kaloola Member|13516|6|Mentioned|p156|Late Permian|Late Permian|Said to be of Rangal Coal Measures, but shown as part of Baralaba Coal Measures and Bandanna Formation too, p145.||Rangal Coal Measures [?]||||
9150|Kaloola Member|23003|5|Briefly described|p423 Table 1|Permian|Permian|Part of Blackwater Group.||||||04-DEC-08
9150|Kaloola Member|23004|5|Briefly described|p431 Table 1|Permian|Permian|Part of Blackwater Group.||||||04-DEC-08
9150|Kaloola Member|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pwbk].  Blue-grey to white, silicified mudstone, siltstone, feldspathic and lithic sandstone, tuff and conglomerate; minor coal; locally abundant Glossopteris beds.||||||
9150|Kaloola Member|29723|6|Mentioned|p17|||||||||
9150|Kaloola Member|29727|6|Mentioned|p455|||||||||
9150|Kaloola Member|30141|5|Briefly described|p131|||See also p135.||||||04-DEC-08
9150|Kaloola Member|30451|4|Described|p63|||Member of Baralaba Coal Measures.||||||04-DEC-08
9150|Kaloola Member|30743|3|Fully described|p22|||See also p23. Correlation||||||04-DEC-08
9150|Kaloola Member|30916|6|Mentioned|p98|||||||||
9150|Kaloola Member|31079|6|Mentioned|p5|||See also Fig. 6||||||
9150|Kaloola Member|31531|6|Mentioned|Table 11|||U. Permian||||||
9150|Kaloola Member|31647|6|Mentioned|p354|||||||||
9150|Kaloola Member|32834|6|Mentioned|p26|||||||||
9150|Kaloola Member|32835|4|Described|p1|||Flora. See also pp2-12.||||||04-DEC-08
9150|Kaloola Member|33363|6|Mentioned|p115|||U.Perm.||||||
9150|Kaloola Member|34095|6|Mentioned|p26||Late Permian|||||||
9150|Kaloola Member|34235|6|Mentioned|p93|||||||||
9150|Kaloola Member|35426|5|Briefly described|p659|||||||||
9150|Kaloola Member|35873|6|Mentioned|Fig.9|||See also P125.||||||
9150|Kaloola Member|37070|4|Described|p73|||||||||
9150|Kaloola Member|37075|5|Briefly described|Table 1|||||||||
9150|Kaloola Member|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
9150|Kaloola Member|38958|5|Briefly described|p493|||||||||
9150|Kaloola Member|39212|6|Mentioned|p13|||||||||
9150|Kaloola Member|39260|6|Mentioned|Fig.2|||||||||
9150|Kaloola Member|39270|5|Briefly described|p282|||||||||
9150|Kaloola Member|40539|6|Mentioned|Fig.2|||||||||
9150|Kaloola Member|41666|6|Mentioned|Fig.1|||||||||
9150|Kaloola Member|42641|6|Mentioned|p121|||Baralaba Coal Measures||||||
9150|Kaloola Member|43017|6|Mentioned|p378|||||||||
9150|Kaloola Member|44630|14|Not recorded|p494|||||||||
9150|Kaloola Member|44639|14|Not recorded|p56-58,65|||Part of Baralaba Coal Measures.||||||
9150|Kaloola Member|45095|4|Described|p9|||Represents Burngrove Fm. in the SE.||||||
9150|Kaloola Member|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Baralaba Coal Measures. Blue-green to white, silicified mudstone, siltstone, feldspathic and lithic sandstone, tuff and conglomerate; minor coal; locally abundant Glossopteris beds.||||||18-JUN-09
9150|Kaloola Member|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Baralaba Coal Measures (Blackwater Group). Blue-grey to white, silicified mudstone, siltstone, feldspathic and lithic sandstone, tuff and conglomerate; minor coal; locally abundant Glossopteris beds.||||||18-MAY-04
9150|Kaloola Member|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Barabala [Baralaba] Coal Measures (Blackwater Group).||||||22-DEC-05
9150|Kaloola Member|60282|5|Briefly described|p7|||Basal tuffaceous unit of Baralaba Coal Measures.||||||
9150|Kaloola Member|64856|4|Described|p61-62, p102|Late Permian|Late Permian|Basal Member of Baralaba Coal Measures. Mudstones, siltstone, sandstone, tuff and conglomerate. Glossopteris sp. leaves common. Implied to be Late Permian.| | ||||29-NOV-17
9150|Kaloola Member|65388|4|Described|p163, 194, 197|||Of Dear & others (1971) as forming the lowermost part of Baralaba Coal Measures. Bowen Basin. Type section  in a tributary of Kianga Creek. This unit is probably represented by the interval 79-214m in GSQ Mundubbera 5. Siltstone, feldspathic and lithic sandstone, tuff and conglomerate. Includes hard, white and brown cherty tuff containing well-preserved leaf impressions.||||||
9150|Kaloola Member|70861|6|Mentioned|p37,45|Late Permian|Late Permian|Of Bowen Basin. ||||Time-equivalent to Fort Cooper Coal Measures.||
9150|Kaloola Member|70878|5|Briefly described|p717, p720, p726|Permian|Permian|Bowen Basin. Calibration of palynological ages.|254.1+/-0.09 Ma - 252.54+/-0.04 Ma.|Bandanna Formation.||||
9150|Kaloola Member|70940|5|Briefly described|p843-844, p853, p855|Permian|Permian|Roma Shelf and Burunga Anticline, southern Bowen Basin. Correlated with Yarrabee Tuff.|252.52 +/- 0.04 Ma (Metcalfe et al., 2015).|Blackwater Group.||Overlies Gyranda Formation or Black Alley Shale. Is overlain by Yarrabee Tuff.||
9150|Kaloola Member|71592|5|Briefly described|Appendix A.|||Bowen Basin.|254+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Sedimentary rock.|
9150|Kaloola Member|72297|5|Briefly described|p695|Permian|Permian|Near Moura, SE Bowen Basin.||||Correlated with Fair Hill and Burngrove Formations.||
9150|Kaloola Member|73304|5|Briefly described|p65, p72|||Dating by U-Pb CA-TIMS from near the top and base of unit. Three other intermediate dates also shown.|252.54+/-0.04 Ma, 254.10+/-0.05 Ma|Shown as Bandanna Formation||||
9150|Kaloola Member|73305|5|Briefly described|p548, p553, p556 Fig.8, p560|Late Permian|Late Permian|Bowen Basin. Taroom Trough, northeast. Equivalent of the Burngrove Formation, preserves the Yarrabee Tuff and 3-4 coal seams correlated as stratigraphically equivalent to the Virgo and Libra seams.||||Interbedded with/equivalent to the Burngrove Formation. Overlies the Gyranda Formation in northeast Taroom Trough.|Dark grey shale, includes coal seams.|
9150|Kaloola Member|73625|5|Briefly described|p5 Fig.3, p20-21|Permian|Permian|Eastern Bowen Basin. Freshwater and estuarine deposits.||Basal Baralaba Coal Measures.||Overlies Black Alley Shale.|A tuff-rich interval.|
9156|Kamarga Volcanics|22438|5|Briefly described|p545-547, Fig.12|||Possibly equivalent to Eastern Creek Volcanics||||||
9156|Kamarga Volcanics|22457|6|Mentioned|Fig29 P30|||Shown as Kamarga Volcs.||||||
9156|Kamarga Volcanics|22680|6|Mentioned|85|||||||||
9156|Kamarga Volcanics|23031|6|Mentioned|28|||||||||
9156|Kamarga Volcanics|23198|6|Mentioned|p873, 875|||||||||
9156|Kamarga Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
9156|Kamarga Volcanics|23393|5|Briefly described|p18, p16 Fig.4|Proterozoic|Proterozoic|Intruded by Yeldham Granite.  Geological Province: Lawn Hill Sub-province.||||||
9156|Kamarga Volcanics|23406|5|Briefly described|p601 Fig.3|||||||||
9156|Kamarga Volcanics|23408|6|Mentioned|p515, p516 Fig. 5|||Onlapped by Torpedo Creek Quartzite. Includes igneous rocks.||||||15-JUN-09
9156|Kamarga Volcanics|23409|5|Briefly described|p535 Fig.2|||||||||
9156|Kamarga Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin.||||||
9156|Kamarga Volcanics|23958|5|Briefly described|p1133|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|23964|5|Briefly described|p1265|||Geological Province: Mount Isa Inlier.||||||
9156|Kamarga Volcanics|24308|5|Briefly described|p999, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|24309|6|Mentioned|p1012 Fig. 1|||||||||
9156|Kamarga Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Lawn Hill Subprovince.||||||07-NOV-08
9156|Kamarga Volcanics|24432|6|Mentioned|p565 Fig.4|||||||||
9156|Kamarga Volcanics|36548|2|Defined|p513|Precambrian|Precambrian|||||||
9156|Kamarga Volcanics|37459|6|Mentioned|p427|||||||||
9156|Kamarga Volcanics|38237|6|Mentioned|Fig.3|||||||||
9156|Kamarga Volcanics|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9156|Kamarga Volcanics|38310|6|Mentioned|p237|||||||||
9156|Kamarga Volcanics|38348|4|Described|p4|||||||||
9156|Kamarga Volcanics|38584|6|Mentioned|p22|||||||||
9156|Kamarga Volcanics|39445|5|Briefly described|Table 2|||See also p35 and p40.||||||04-OCT-06
9156|Kamarga Volcanics|39497|6|Mentioned|Fig.4|||||||||
9156|Kamarga Volcanics|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9156|Kamarga Volcanics|39925|6|Mentioned|p334|||||||||
9156|Kamarga Volcanics|39944|6|Mentioned|p229|||||||||
9156|Kamarga Volcanics|40840|6|Mentioned|Map legend|||||||||
9156|Kamarga Volcanics|41979|5|Briefly described|p518|||||||||
9156|Kamarga Volcanics|42565|5|Briefly described|Table 1 P6, P2|||||||||
9156|Kamarga Volcanics|45166|4|Described|p17|||||||||
9156|Kamarga Volcanics|49041|5|Briefly described|Table 1|||||||||
9156|Kamarga Volcanics|50536|6|Mentioned|p4.1|||Geological Province: Mount Isa Inlier.||||||
9156|Kamarga Volcanics|50550|5|Briefly described|p1146 Fig.9, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
9156|Kamarga Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|60558|5|Briefly described|p5 Fig. 4, p9 Fig. 7|||Age: ~1740 - 1730Ma.||||||03-JUN-09
9156|Kamarga Volcanics|63109|6|Mentioned|p1112|||||||||
9156|Kamarga Volcanics|63866|5|Briefly described|p57||||||||Lower greenschist-facies basalts and feldspathic sandstones of unknown age.|
9156|Kamarga Volcanics|64250|6|Mentioned|p23|||||||||
9156|Kamarga Volcanics|64575|6|Mentioned|p656|||Correlated with Eastern Creek Volcanics.||||||
9156|Kamarga Volcanics|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Lawn Hill Platform.||||||
9156|Kamarga Volcanics|65396|6|Mentioned|p196|||Kamarga Dome, NW Mount Isa Inlier.||||Correlated (possibly) with Eastern Creek Volcanics.||
9156|Kamarga Volcanics|67323|5|Briefly described|GIS attrib tbl, p10, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Post-Barramundi basement to Century Domain, Mount Isa Inlier. Is directly overlain by the Isa Superbasin sequence.|Pre-1810 Ma.|||Intruded by Yeldham Granite.|Vesicular, amygdaloidal and massive basalt; flow top breccias common; interbeds of feldspathic and conglomeratic sandstone|
9156|Kamarga Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
9156|Kamarga Volcanics|69591|5|Briefly described|p29-30, p32, p58|Paleoproterozoic|Paleoproterozoic|Century Domain, Mount Isa Province. Crops out in the Kamarga Dome, E of Century Mine. Subaerial, local fluvial environment.||||Is intruded by Yeldham Granite.|Vesicular, massive and amygdaloidal basalt; flow-top breccias common; interbeds of feldspathic and conglomeratic sandstone.|
9156|Kamarga Volcanics|72526|5|Briefly described|p6 Fig.1.2,|Paleoproterozoic|Paleoproterozoic|||||||
9156|Kamarga Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
9156|Kamarga Volcanics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
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|||||||||
9211|Kangaroo Creek Sandstone|12597|5|Briefly described|p491, p492 Tb.1, p493 Fig.2|Tithonian|Oxfordian|S Clarence-Moreton Basin. Forms characteristic escarpments up to 90m high.||||Is overlain by Grafton Formation.|Coarse-grained, cross-bedded quartz sandstone.|
9211|Kangaroo Creek Sandstone|22857|4|Described|p318-9, p548 App. 1 Tb.A1.12|Early Cretaceous|Late Jurassic|Quartzose crossbedded sandstone. Unconformably overlies Walloon Coal Measures. Max. thickness: ~500m. Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|22865|6|Mentioned|p318,Fig22.9p317|Cretaceous|Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
9211|Kangaroo Creek Sandstone|23720|5|Briefly described|Map Legend|||Quartz arenite, quartz and lithic conglomerate.||||||15-DEC-04
9211|Kangaroo Creek Sandstone|23811|5|Briefly described|Map Legend|Oxfordian|Callovian|Quartz arenite, minor quartz and lithic conglomerate; thick to very thin-bedded, high-angle crossbedding.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
9211|Kangaroo Creek Sandstone|23812|4|Described|p31, p34 Tb.4|Middle Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|23843|5|Briefly described|p456 Table 1|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 290m.||||||
9211|Kangaroo Creek Sandstone|23888|6|Mentioned|p262|||||||||
9211|Kangaroo Creek Sandstone|24127|5|Briefly described|p5|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|24129|5|Briefly described|p4|||Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|24299|5|Briefly described|p4|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|29591|6|Mentioned|p85|||||||||
9211|Kangaroo Creek Sandstone|29698|6|Mentioned|p65|||||||||
9211|Kangaroo Creek Sandstone|29988|6|Mentioned|Map legend|Cretaceous|Jurassic|Cretaceous-Jurassic||||||
9211|Kangaroo Creek Sandstone|29995|6|Mentioned|Map legend|Jurassic|Jurassic|Cretaeous||||||
9211|Kangaroo Creek Sandstone|30785|6|Mentioned|p397|||||||||
9211|Kangaroo Creek Sandstone|30911|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
9211|Kangaroo Creek Sandstone|31806|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
9211|Kangaroo Creek Sandstone|32491|5|Briefly described|p18|||U.Jurassic||||||
9211|Kangaroo Creek Sandstone|32492|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|32671|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
9211|Kangaroo Creek Sandstone|32916|6|Mentioned|Map legend|Cretaceous|Jurassic|Cretaceous-Jurassic||||||
9211|Kangaroo Creek Sandstone|33476|6|Mentioned|Fig.10|||||||||
9211|Kangaroo Creek Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
9211|Kangaroo Creek Sandstone|34254|6|Mentioned|p490|||||||||
9211|Kangaroo Creek Sandstone|34340|3|Fully described|p471|||||||||
9211|Kangaroo Creek Sandstone|34400|5|Briefly described|p13|||||||||
9211|Kangaroo Creek Sandstone|34755|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|36354|6|Mentioned|Fig.1|||||||||
9211|Kangaroo Creek Sandstone|37122|5|Briefly described|Table 1|||||||||
9211|Kangaroo Creek Sandstone|37252|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
9211|Kangaroo Creek Sandstone|38064|5|Briefly described|p41|||||||||
9211|Kangaroo Creek Sandstone|39907|6|Mentioned|Fig.6|||||||||
9211|Kangaroo Creek Sandstone|39969|6|Mentioned|p11|||||||||
9211|Kangaroo Creek Sandstone|41631|4|Described|p20|||See also Fig.2, Fig.5 and P 19||||||
9211|Kangaroo Creek Sandstone|42248|6|Mentioned|Fig.8 P403|||||||||
9211|Kangaroo Creek Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
9211|Kangaroo Creek Sandstone|42869|5|Briefly described|Table 1, p33|||||||||12-SEP-21
9211|Kangaroo Creek Sandstone|43008|5|Briefly described|map legend|||||||||
9211|Kangaroo Creek Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
9211|Kangaroo Creek Sandstone|43344|14|Not recorded|p14,102|||||||||
9211|Kangaroo Creek Sandstone|43383|14|Not recorded|p25,28|Cretaceous|Jurassic|Above Walloon Coal Measures?||||||
9211|Kangaroo Creek Sandstone|43384|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|43468|14|Not recorded|Map Legend|Cretaceous|Jurassic|Provisional Edition||||||
9211|Kangaroo Creek Sandstone|43479|14|Not recorded|p251,252||Early Cretaceous|||||||
9211|Kangaroo Creek Sandstone|44028|14|Not recorded|p509,512,Fig.2||Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|44450|4|Described|p28 Table 7|Late Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin||||||
9211|Kangaroo Creek Sandstone|48917|3|Fully described|p30|||||||||
9211|Kangaroo Creek Sandstone|60079|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Quartz arenite, conglomerate.||||||
9211|Kangaroo Creek Sandstone|60281|5|Briefly described|p27, p31|Cretaceous|Late Jurassic|Interconnected quartzose cross-bedded sandstone deposited by braided streams. Overlain by Grafton Formation; overlies the Walloon Coal Measures.  Max. thickness: ?500m.||||||27-APR-05
9211|Kangaroo Creek Sandstone|60993|3|Fully described|p35, p19 Fig. 16|Late Jurassic|Middle Jurassic|First termed Kangaroo Creek "Series" and Kangaroo Creek "Stage". Overlies Walloon Coal Measures; grades into the Woodenbong beds. Conformably underlies Grafton Fm.  Max. thickness: >870m. Geol. Prov: Clarence-Moreton Basin.||||||04-DEC-08
9211|Kangaroo Creek Sandstone|60995|4|Described|p69, p51 Fig. 3|Late Jurassic|Late Jurassic|Massive, coarse-grained, cross-bedded, white saccharoidal, quartz sandstone.Overlies Walloon C.M.  Max. thickness: ~500m. Geological Province: Clarence-Moreton Basin. See also p52.||||||
9211|Kangaroo Creek Sandstone|60997|5|Briefly described|p139|Tithonian|Kimmeridgian|Highly quartzose sandstone.  Overlies the Walloon Coal Measures; conformably overlain by Grafton Formation. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1.||||||
9211|Kangaroo Creek Sandstone|60999|5|Briefly described|p164|||Overlies Walloon C. M. in places.||||||
9211|Kangaroo Creek Sandstone|61000|5|Briefly described|p181, p183|Middle Jurassic|Middle Jurassic|Clean and cross-bedded sandstones are common. Overlies Walloon C.M. Probably Bajocian in age. Geological Province: Clarence-Moreton Basin. See also p186.||||||
9211|Kangaroo Creek Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|||||||
9211|Kangaroo Creek Sandstone|61006|5|Briefly described|p278 Fig. 2|Jurassic|Jurassic|Quartzose sandstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285, p289.||||||
9211|Kangaroo Creek Sandstone|61310|4|Described|p14 Fig. C5|Early Cretaceous|Late Jurassic|Distinctive medium- to coarse-grained, white to cream, saccharoidal sst., with minor siltstone, shale and quartz pebble sst. Unconformably overlies Walloon Coal Measures; overlain by Grafton Fm. Max. thickness: ?500m. Geol. Prov: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|64289|5|Briefly described|p6 Fig. 2|Late Jurassic|Middle Jurassic|Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9211|Kangaroo Creek Sandstone|67402|4|Described|p187, p192, p193|Oxfordian|Bathonian|Clarence-Moreton Basin. Deposited in a fluvial environment. Sandstones are often of reservoir quality.  ||||Overlain by the Grafton Formation. Overlies the Walloon Coal Measures.|Fine feldspathic, sub-labile to coarse-grained quartzose sandstone.|
9211|Kangaroo Creek Sandstone|68135|5|Briefly described|p52 fig 2b|Oxfordian|Oxfordian|Clarence-Moreton Basin.||||Unconformably overlies Walloon Coal Measures. Overlain by Grafton Formation|Sandstone.|14-SEP-17
9211|Kangaroo Creek Sandstone|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Jurassic|Upper Jurassic|Clarence-Moreton Basin. Between 200-500m thick. Deposited in a braided fluvial environment. Potential reservoir rock.||||Overlies the Maclean Sandstone Member and Walloon Coal Measures. Overlain by the Grafton Formation.|Cross-bedded, quartzose sandstone.|
9211|Kangaroo Creek Sandstone|69594|5|Briefly described|p544-545|||Clarence-Moreton Basin (NSW only). In QLD it is known as the (lower part of) Woodenbong beds. Cliff-forming unit. Sediment derived from the Texas Subprovince.||||Overlies Walloon Coal Measures conformably or disconformably (in part unconformably). Is overlain by Grafton Formation.|White quartzose sandstone.|
9211|Kangaroo Creek Sandstone|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Late Jurassic|Shown as located within the Clarence-Moreton Basin.||||Shown as unconformably overlying Walloon Coal Measures and underlies Grafton Formation.||
9211|Kangaroo Creek Sandstone|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Walloon Coal Measures. Is overlain by Grafton Formation.||
9211|Kangaroo Creek Sandstone|73570|6|Mentioned|p911, p912 Fig.2, p914, p915 Fig.4, p920|Late Jurassic|Late Jurassic|Clarence-Morton Basin. Paleocurrent directions predominantly to the east and southeast. Grades laterally into Woodenbong beds. Misspelt as Kangaroo Formation p913.|||||Quartz-rich sandstones.|
9215|Kangaroo Hills Formation|23032|4|Described|p19,20|Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|23291|5|Briefly described|p51|Devonian|Devonian|Geological Province: Georgetown Region.||||||08-JUL-15
9215|Kangaroo Hills Formation|23423|5|Briefly described|Plate 8.2e|||||||||
9215|Kangaroo Hills Formation|23424|4|Described|Table 8.1 Fig 8.2 p333.|Early Devonian|Silurian|Age:?Silurian to Early Devonian; Lochkovian conodonts in allochthonous lmst. Faulted against Pelican Range Fm & Perry Ck Fm. Intruded by granite plutons & Princess Hills Granite. O'lain by Clarke Rvr Gp (u) & Tertiary seds & basalt. Camel Ck Subprovince.||||||
9215|Kangaroo Hills Formation|23430|5|Briefly described|p476, Plate 14.11|Devonian|Silurian|Broken River Province.||||||
9215|Kangaroo Hills Formation|23431|6|Mentioned|p541|||Camel Creek Subprovince.||||||
9215|Kangaroo Hills Formation|23494|4|Described|p9, p22 Tb. 1|Early Devonian|Late Silurian|Sequence of rhythmically alternating beds of siltstone, sandstone, graded greywacke and lenses of greywacke conglomerate.  Conformably overlain by Perry Creek Formation; unconformably overlies Greenvale Formation.   Max. thickness: 40,000ft.||||||
9215|Kangaroo Hills Formation|23498|5|Briefly described|p 23 table 1|Early Devonian|Late Silurian|||||||
9215|Kangaroo Hills Formation|23509|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Broken River Province.||||||
9215|Kangaroo Hills Formation|23617|3|Fully described|p12-14|Early Devonian|Late Silurian|Also see Table 1 p12. Overlain by Clarke River Group. Camel Creek Subprovince of Broken River Province.||||||23-APR-08
9215|Kangaroo Hills Formation|23618|5|Briefly described|map legend|Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|23619|4|Described|p33 Table 1|Early Devonian|Silurian|Also see p8. Divided into 2 unnamed units. The lowermost was previously mapped as part of Greenvale Formation. Overlying unit Clarke River Group. Camel Creek Subprovince.||||||
9215|Kangaroo Hills Formation|23893|5|Briefly described|p15|Early Devonian|Late Silurian|Geological Province: Camel Creek Subprovince.||||||
9215|Kangaroo Hills Formation|24074|5|Briefly described|p389 Table 1|Late Silurian|Late Silurian|Maximum thickness: 12,000m.||||||
9215|Kangaroo Hills Formation|24577|4|Described|p752 Fig. 1|Devonian|Silurian|Overlies the Perry Creek Formation. Formation is Fm in text. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
9215|Kangaroo Hills Formation|29445|6|Mentioned|p73|||||||||
9215|Kangaroo Hills Formation|30914|6|Mentioned|Map legend|Devonian|Ordovician|Ordovician - Devonian||||||
9215|Kangaroo Hills Formation|31832|6|Mentioned|p31|||Table 6||||||
9215|Kangaroo Hills Formation|31999|6|Mentioned|Fig.3|||See also Table 11||||||
9215|Kangaroo Hills Formation|32169|6|Mentioned|Table 2|||Sil.-L.Dev.||||||
9215|Kangaroo Hills Formation|32553|4|Described|p52|||||||||
9215|Kangaroo Hills Formation|33326|6|Mentioned|p448|||Fauna.||||||
9215|Kangaroo Hills Formation|34046|6|Mentioned|Table 1|||||||||
9215|Kangaroo Hills Formation|36472|6|Mentioned|Map legend|Early Devonian|Late Silurian|Early Devonian to Late Silurian||||||
9215|Kangaroo Hills Formation|37573|4|Described|p202|||See also Fig.2||||||
9215|Kangaroo Hills Formation|37575|4|Described|p181|||See also Fig.3||||||
9215|Kangaroo Hills Formation|37727|4|Described|p66|||See also P22.||||||
9215|Kangaroo Hills Formation|39027|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
9215|Kangaroo Hills Formation|39445|5|Briefly described|Table 4|||See also P74, Table 5 & Fig.6||||||
9215|Kangaroo Hills Formation|39686|6|Mentioned|Fig.1|||||||||
9215|Kangaroo Hills Formation|39689|6|Mentioned|p52|||||||||
9215|Kangaroo Hills Formation|39735|6|Mentioned|p18|||||||||
9215|Kangaroo Hills Formation|40623|5|Briefly described|p92|||||||||
9215|Kangaroo Hills Formation|40943|6|Mentioned|p50|||||||||
9215|Kangaroo Hills Formation|41260|3|Fully described|p15|||Described (p116).||||||23-APR-08
9215|Kangaroo Hills Formation|41735|6|Mentioned|p284|||||||||
9215|Kangaroo Hills Formation|41916|6|Mentioned|p25|||||||||
9215|Kangaroo Hills Formation|42031|4|Described|p762|||||||||
9215|Kangaroo Hills Formation|42690|5|Briefly described|map legend|Early Devonian|Ordovician?|||||||
9215|Kangaroo Hills Formation|42692|5|Briefly described|map legend|Early Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|42752|5|Briefly described|p45|||see also Fig.2 P46||||||
9215|Kangaroo Hills Formation|42933|3|Fully described|p28|||||||||
9215|Kangaroo Hills Formation|43095|5|Briefly described|Plate 2|||||||||
9215|Kangaroo Hills Formation|43113|4|Described|Table 1 p20|Early Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
9215|Kangaroo Hills Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
9215|Kangaroo Hills Formation|43461|14|Not recorded|table p618|Siegenian|Gedinnian|||||||
9215|Kangaroo Hills Formation|43589|6|Mentioned|p23|Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|43716|6|Mentioned|p14|||||||||
9215|Kangaroo Hills Formation|43902|2|Defined|p124-125|||||||||
9215|Kangaroo Hills Formation|43926|2|Defined|Tb.2 opp.p.10,map,7|||p11,19,20,22.||||||23-APR-08
9215|Kangaroo Hills Formation|44044|2|Defined|p124-128|||Conformably overlain by Perry Creek Formation.||||||
9215|Kangaroo Hills Formation|44046|14|Not recorded|p153-4|||||||||
9215|Kangaroo Hills Formation|44048|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
9215|Kangaroo Hills Formation|44049|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
9215|Kangaroo Hills Formation|44050|14|Not recorded|p153,154,156|||||||||
9215|Kangaroo Hills Formation|44051|14|Not recorded|p178,180|||Unconformably overlain by Clarke River Formation.||||||
9215|Kangaroo Hills Formation|44052|14|Not recorded|p128|||Unconformably overlain by Star Group.||||||
9215|Kangaroo Hills Formation|44059|14|Not recorded|p442(Tb)||Late Silurian|||||||
9215|Kangaroo Hills Formation|44060|14|Not recorded|Map Legend|Early Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|44061|4|Described|Table 2|Early Devonian|Silurian|||||||
9215|Kangaroo Hills Formation|44359|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
9215|Kangaroo Hills Formation|44515|2|Defined|p33-35|Early Devonian|Late Silurian|||||||
9215|Kangaroo Hills Formation|44516|14|Not recorded|p35|||||||||
9215|Kangaroo Hills Formation|45009|2|Defined|p7,41,45-8,50-2,61-2|||p131,132,Pls.9,12,13,Tbs.5,6. Unconformably overlies Greenvale Formation. Conformably overlain by Perry Creek Formation. Intruded by Herbert River Granite.||||||
9215|Kangaroo Hills Formation|45151|6|Mentioned|Table 3|||||||||
9215|Kangaroo Hills Formation|48904|4|Described|p15|||See Table 1||||||
9215|Kangaroo Hills Formation|60425|5|Briefly described|p115|Early Devonian|Silurian|Geological province: Broken River Province.||||||07-FEB-11
9215|Kangaroo Hills Formation|61727|5|Briefly described|p942 Fig.1|Devonian|Silurian|Includes open to tightly folded lower greenschist facies metasedimentary rocks. Overlain by Clarke River Group basal units. Geological Province: Broken River Province/Camel Creek Subprovince. See also p943 Fig.2.||||||
9215|Kangaroo Hills Formation|63154|5|Briefly described|p281 Fig. 3|Middle Devonian|Early Devonian|Geological province: Broken River Province/Camel Creek Subprovince.||||||
9215|Kangaroo Hills Formation|67848|5|Briefly described|p3, p8.|||Most easterly, and youngest, fossils in Camel Creek Subprovince. Part of the accretionary wedge in the arc-trench gap succession involved in collisional accretion. Has conglomerates with early Devonian limestone clasts.||||||
9215|Kangaroo Hills Formation|68339|5|Briefly described|Map legend.|Early Devonian|Late Silurian?|Camel Creek Subprovince.|||||Quartzose to feldspathic sublabile arenite and mudstone; feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate with limestone clasts, allochthonous limestone blocks.|
9215|Kangaroo Hills Formation|68340|5|Briefly described|Map legend.|Early Devonian|Late Silurian?|Camel Creek Subprovince.|||||Quartzose to feldspathic sublabile arenite and mudstone; feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate with limestone clasts, allochthonous limestone blocks.|
9215|Kangaroo Hills Formation|68350|5|Briefly described|Map legend.|Early Devonian?|Late Ordovician?|Camel Creek Subprovince, Broken River Province.|||||Feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate|
9215|Kangaroo Hills Formation|68351|5|Briefly described|Map legend.|Early Devonian?|Late Ordovician?|Camel Creek Subprovince, Broken River Province.|||||Feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate|
9215|Kangaroo Hills Formation|68480|5|Briefly described|Map Legend|Early Devonian|Late Silurian|The 4 facies are mapped separately. Camel Creek Subprovince. Late Silurian? Maximum age.|||||Feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate with limestone clasts, allochthonous limestone blocks; quartzose to feldspathic sublabile arenite and mudstone; mudstone and lithofeldspathic arenite; altered basalt?|
9215|Kangaroo Hills Formation|68481|5|Briefly described|Map Legend|Early Devonian|Late Silurian|The 4 facies are mapped separately. Camel Creek Subprovince. Late Silurian? maximum age.||||Is intruded by Ingham Granite Complex and Bewilder Granite.|Feldspathic to lithofeldspathic arenite and mudstone, local polymictic conglomerate with limestone clasts, allochthonous limestone blocks; quartzose to feldspathic sublabile arenite and mudstone; mudstone and lithofeldspathic arenite; altered basalt?|
9215|Kangaroo Hills Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Broken River Province. This unit, as well as Perry Creek and Greenvale Formations, are all mapped under the symbol, SDb.||||||
9215|Kangaroo Hills Formation|68576|5|Briefly described|Q_11: p38-40|Early Devonian|Late Silurian|Camel Creek Subprovince. Forms relatively subdued topography. Facies variations are common; interpreted as alternating proximal and distal turbidites. Source of clasts for an unnamed conglomerate in the basal Clarke River Group.|||||Typical turbidites: thin to medium-bedded, fine- to medium-grained labile sandstone (with BC Bouma structures) interbedded with grey mudstone (with weak slaty cleavage); conglomerate with limestone clasts.|
9215|Kangaroo Hills Formation|69030|5|Briefly described|p6, p15, p40|Silurian|Silurian|Camel Creek Subprovince (Broken River Province). Hosts significant gold mineralisation.|||||Turbidites.|
9215|Kangaroo Hills Formation|69079|5|Briefly described|p5-6, p62|Early Devonian|Late Silurian|Camel Creek Subprovince, Broken River Province. Hosts gold-antimony mineralisation in quartz veins.|||||Strongly folded sediments with local shear zones (possibly melanges).|
9215|Kangaroo Hills Formation|69592|5|Briefly described|p251 Fig.4.35, p268, p271-272, p277-279|Early Devonian|Late Silurian|See also p297, p303. Easternmost Camel Creek Subprovince, Broken River Province. Crops out over 3000 km2. Submarine fan accumulations. Age from conodonts and corals. Deformation discussed; photographs of various structures.||||Is overlain unconformably by Clarke River Group. Is faulted against Perry Creek Formation.|Interlayered thick-bedded sandstone and sparse mudstone interbeds, and intervals of alternating thin- to medium-bedded sandstone and mudstone; minor conglomerate.|
9215|Kangaroo Hills Formation|70207|6|Mentioned|p20, p25|Early Devonian|Silurian|Clarke River and/or Cairns region.||||||
9215|Kangaroo Hills Formation|73201|4|Described|p607, p610-618, p620|Middle Devonian|Silurian|Broken River Province. Geochron are three of four U-Pb LA-ICP-MS detrital zircon maximum depositional ages (the fourth: 381 +/- 10 Ma). Based on these results, deposition spanned from late Silurian to Middle Devonian, which is consistent with biostratigraphic control from limestone clasts in conglomerates. Detrital zircon provenance is linked to igneous rocks of the Macrossan and Pama Igneous associations. The scarcity of Proterozoic zircons indicates that basement rocks were not a source. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Age given as late Silurian to Middle Devonian.|427.6 +/- 8.1 Ma, 400.6 +/- 3.8 Ma, 424.3 +/- 4 Ma||||Lithofeldspathic greywacke with widespread melange and pre-slaty cleavage folding, common polymict conglomerate horizons (clasts: quartz, chert, sandstone, limestone, igneous rocks), uncommon limestone olistoliths, rare mafic volcanic bodies.|
9227|Kangaroo River Volcanics|22811|5|Briefly described|Fig.2 p598|Carboniferous|Carboniferous|of Kennedy Province||||||
9227|Kangaroo River Volcanics|23420|5|Briefly described|p 146 table 4.5, p 129|Early Permian|Late Carboniferous|In the Janet Ranges Volcanic Group. I-type characteristics. Intruded by Weymouth Granite.||||||
9227|Kangaroo River Volcanics|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
9227|Kangaroo River Volcanics|32528|5|Briefly described|Table 2|||||||||
9227|Kangaroo River Volcanics|33226|6|Mentioned|Map legend|Early Permian|Carboniferous|Carboniferous to Early Permian||||||
9227|Kangaroo River Volcanics|33880|6|Mentioned|Map legend|Early Permian|Early Carboniferous|Lower Carboniferous - Lower Permian||||||
9227|Kangaroo River Volcanics|33882|4|Described|Table 1|||P12||||||
9227|Kangaroo River Volcanics|34581|2|Defined|p137|Permian|Carboniferous|Carboniferous - Permian. See also PP130,140||||||
9227|Kangaroo River Volcanics|37613|6|Mentioned|p247|||See also Fig.2||||||
9227|Kangaroo River Volcanics|39252|6|Mentioned|Fig.11|||||||||
9227|Kangaroo River Volcanics|39445|5|Briefly described|Table 7|||||||||
9227|Kangaroo River Volcanics|42547|5|Briefly described|p74|||||||||
9227|Kangaroo River Volcanics|42550|4|Described|p8|||||||||
9227|Kangaroo River Volcanics|45076|3|Fully described|p111|||Late Pal. P17.||||||
9227|Kangaroo River Volcanics|49769|6|Mentioned|p4|||||||||
9227|Kangaroo River Volcanics|71792|5|Briefly described|p33, p37, p40-p42, p44|Early Permian|Early Permian|Northern Coen Inlier. Early mapping work subdivided this unit into two informal units; a lower unit of andesite, rhyodacite and dacite and an upper rhyolite tuff and breccia unit. Distribution, outcrop and geophysical characteristics are discussed. As its considered equivalent to the Janet Ranges Volcanics it is interpreted to be of the same age (284.7 +/- 1.7 Ma).||Janet Ranges Volcanic Group||Equivalent to the Janet Ranges Volcanics. Overlies the Sefton Metamorphics. Intruded(?) By the Kennedy Hill Granite.|Rhyolitic welded tuff and breccia, andesite, dacite(?); minor rhyolite lava.|
9227|Kangaroo River Volcanics|71853|5|Briefly described|Map legend.|Permian|Permian|The three facies are mapped separately.||Janet Ranges Volcanic Group.|||Rhyolitic welded tuff and breccia, andesite, dacite(?); minor rhyolite lava. Basaltic to andesitic volcanic rocks; with dark tones on radiometric images. Coherent and autoclastic rhyolite lavas, dome or cryptodomes; high radiometric response.|
9227|Kangaroo River Volcanics|73083|6|Mentioned|p56-57|||||||||
9284|Karin Granite|42747|5|Briefly described|p37|||||||||
9284|Karin Granite|43029|2|Defined|p23|Carboniferous|Devonian|see also Fig.1,p13||||||
9284|Karin Granite|43204|5|Briefly described|Map Legend|Early Carboniferous|Middle Devonian|||||||23-DEC-11
9284|Karin Granite|43213|3|Fully described|p17, p95, p113-114, p117, p121-124, p184|||See also p215. Karin-Retro area, SE of Clermont. Its presence was postulated by Darby (1969) from a large gravity low, and confirmed by the authors of this Report. Includes granite previously mapped by Veevers et al. (1964) as Retreat Granite near Capella. Type locality described. Geochemistry detailed. Tentative Devonian to Carboniferous age. Hosts a group of gold prospects W of Capella.|||||Pink, fine- to medium-grained, equigranular biotite granite and microgranite. Felsic I-type.|
9284|Karin Granite|48915|6|Mentioned|p22, plate 6|||See also Plate 6||||||
9284|Karin Granite|68553|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|||||||
9284|Karin Granite|68731|6|Mentioned|p132|||Biotite-bearing and is only exposed approximately 2km west of Capella.||||||
9284|Karin Granite|68900|6|Mentioned|p4|Early Carboniferous|Late Devonian|Drummond Basin.||||||
9362|Keefton Formation|23251|5|Briefly described|Table 1 p10, p20||Early Triassic|Plant fossils of Early Triassic Age. Kin Kin Subprovince, Gympie Province.||||||30-NOV-05
9362|Keefton Formation|24078|5|Briefly described|p425 Tb. 1|Early Triassic|Early Triassic|Predominantly coarse lithic sandstone, pebbly sandstone with interbedded sheared granule and pebble conglomerate.  Max. thickness: 320m.  Geological Province: Gympie Basin.||||||
9362|Keefton Formation|30547|6|Mentioned|p426|||Correlation||||||
9362|Keefton Formation|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
9362|Keefton Formation|34474|6|Mentioned|Fig.1|||Lower Triassic||||||
9362|Keefton Formation|34475|2|Defined|p247|Triassic|Triassic|See also PP257,258||||||
9362|Keefton Formation|35101|3|Fully described|p32|||||||||
9362|Keefton Formation|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
9362|Keefton Formation|36045|6|Mentioned|p334|||||||||
9362|Keefton Formation|36926|6|Mentioned|p175|||||||||
9362|Keefton Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
9362|Keefton Formation|38391|6|Mentioned|p9|||||||||
9362|Keefton Formation|39252|6|Mentioned|p28|||||||||
9362|Keefton Formation|39261|6|Mentioned|Fig. 10|||||||||
9362|Keefton Formation|39284|5|Briefly described|p431|||||||||
9362|Keefton Formation|39445|5|Briefly described|Table 9|||See also Fig.7||||||
9362|Keefton Formation|40051|4|Described|p8|||||||||
9362|Keefton Formation|40623|5|Briefly described|p53|||||||||
9362|Keefton Formation|41157|6|Mentioned|Fig.1|||||||||
9362|Keefton Formation|41272|6|Mentioned|M 1of1 C16|||||||||
9362|Keefton Formation|41917|6|Mentioned|p522|||||||||
9362|Keefton Formation|42450|3|Fully described|p404, p405|||||||||
9362|Keefton Formation|42695|5|Briefly described|Fig.2|Triassic||||||||
9362|Keefton Formation|42751|4|Described|p25|||||||||
9362|Keefton Formation|43008|5|Briefly described|map legend|||||||||
9362|Keefton Formation|43017|6|Mentioned|p380|||||||||
9362|Keefton Formation|43077|5|Briefly described|p4|||||||||
9362|Keefton Formation|43100|4|Described|p31||Early Triassic|||||||
9362|Keefton Formation|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
9362|Keefton Formation|44928|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
9362|Keefton Formation|60077|5|Briefly described|Map legend|Early Triassic|Early Triassic|Conglomerate, lithic arenite.||||||
9362|Keefton Formation|65380|5|Briefly described|p660 Table 1, p670, 671, p672 Table 3|Induan|Late Permian|Gympie Terrane. Maximum depositional age from detrital zircon: 252 +/-2 Ma. Includes Triassic plants.||||Overlies Gympie Group (Tamaree Formation). Is overlain by Traveston Formation.|Volcaniclastic conglomerate and coarse sandstone.|27-MAR-12
9362|Keefton Formation|68111|5|Briefly described|p979|Induan|Induan|Gympie Terrane? Zircon ages have multiple peaks: 252 +/- 2 Ma, 318 +/- 3 Ma, 351 +/- 4 Ma (Korsch et al. 2009).||||||21-OCT-14
9362|Keefton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Gympie Province. This unit, as well as the Brooweena and Traveston Formations, and the Kin Kin beds, are all mapped under the symbol, Rb.||||||
9362|Keefton Formation|68679|5|Briefly described|p312-313, p369-370|Middle Triassic|Early Triassic|Runnegar and Ferguson (1969). Southern Gympie Province, northern New England Orogen. 320m thick. Contains non-marine plant fossils and redbeds.||||Unconformably overlies Tamaree Formation. Is overlain by Kin Kin beds. With Kin Kin beds, is correlated with Brooweena Formation.|Pebble conglomerate, sandstone, siltstone, minor hematitic siltstone, limestone, shale.|
9362|Keefton Formation|70913|5|Briefly described|p6, p7, p12 fig 4, p16, p67 fig 9, App1|Late Triassic|Early Triassic|Kin Kin Subprovince of the Gympie Province. Previously included in Upper Gympie Formation of Dunstan (1911), Gympie Group. See also Appendix 1 maps.|||Conformable overlies Tamaree Formation.||Conglomerates.|18-SEP-17
9362|Keefton Formation|72037|4|Described|p859,861-867,869|Middle Triassic|Early Triassic|Geological province: New England Orogen, Gympie Terrane. Depositional environment: fluvial terrestial. Zircon age spectrum with Carboniferous detrital peak, interpreted to have been sourced from New England Orogen during accretion of Gympie Terrane onto the Australian margin (Korsch et al., 2009a). LA-ICP-MS peak detrital zircon U-Th-Pb ages include 251, 268, 295, 328, 378, and 424 Ma. Maximum depositional age at 251 Ma, consistent with Induan age (252.17-251.2 Ma) based on plant fossils (Cohen et al., 2013; Runnegar and Ferguson, 1969). Late Permian to Triassic detrital zircons likely sourced from a middle Permian to Triassic continental arc system to the west, which was built on the former accretionary complex of the New England Orogen Gust et al., 1993; Bryant et al., 1997; Holcombe et al., 1997b; Li et al., 2012b). Carboniferous-age zircons correspond to detritus eroded from a Carboniferous magmatic arc of the New England Orogen, or recycled through the Carboniferous fore-arc and accretionary complex rocks. Cambrian to Devonian zircons likely originated from the Tabberabberan (~382-397 Ma), Benambran (~430-450 Ma), and Delamerian (~490-516 Ma) orogenies (Korsch et al., 2009a).||||Fault contact with Kin Kin beds.|Pebble conglomerate, sandstone, siltstone, limestone, and mudstone.|
9362|Keefton Formation|73303|4|Described|p60 Fig.1, p61 Fig.2, p62, p69|Early Triassic|Early Triassic|New England Orogen. Gympie Terrane, southern. Inferred depositional environment of distal alluvial fan, terrestrial with sediment derived from the New England Orogen. See also  p68 Fig.9.|251 Ma detrital zircon maximum depositional age|||Overlies Tamaree Formation, underlies Kin-Kin beds. Correlated with lower Brooweena Formation.|Terrestrial conglomerate.|
9362|Keefton Formation|73570|6|Mentioned|p914, p915 Fig.4, p916, p918, p919 Fig.6|Induan|Induan|Gympie Province.||||||
9375|Keepera Group|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Includes: Oorabra Arkose.||||||
9375|Keepera Group|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Oorabra Arkose. Geological Province: Georgina Basin.||||||
9375|Keepera Group|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
9375|Keepera Group|37462|4|Described|Table 4.IX|||||||||
9375|Keepera Group|37928|6|Mentioned|Fig.5|||||||||
9375|Keepera Group|37929|5|Briefly described|p526|||||||||
9375|Keepera Group|38157|6|Mentioned|Table IX|||||||||
9375|Keepera Group|39445|6|Mentioned|p56|||||||||
9375|Keepera Group|40538|6|Mentioned|Map legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin.||||||15-NOV-05
9375|Keepera Group|40906|4|Described|p18|||||||||
9375|Keepera Group|42504|5|Briefly described|Table 4 P73|||||||||
9375|Keepera Group|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
9375|Keepera Group|45155|6|Mentioned|Fig.7|||||||||
9375|Keepera Group|48990|2|Defined|p17|Adelaidean|Adelaidean|||||||
9375|Keepera Group|60122|5|Briefly described|p5, p11|Neoproterozoic|Neoproterozoic|Includes the Black Stump Arkose and Wonnadinna Dolostone.  Gological Province: Georgina Basin.||||||17-MAY-05
9375|Keepera Group|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Oorabra Arkose. Geological province: Georgina Basin.||||||
9375|Keepera Group|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes Black Stump Arkose and Wonnadinna Dolostone.||||||
9375|Keepera Group|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes: Boko Formation, Ooraba Arkose, Wonnadinna Dolostone, and Black Stump Arkose.  Geological Province: southern Georgina Basin.||||||13-OCT-05
9375|Keepera Group|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin.||||||
9375|Keepera Group|64068|3|Fully described|p223-224 App 1, pp45-48, p7, 35, p viii|Ediacaran|Cryogenian|Intended as redefinition. Disconformably overlies Aroota Group after c.650 Ma uplift.|||Now includes Sun Hill, Black Stump and Oorabra Arkoses, Little Burke Tillite, Boko Formation (correlated with Marinoan glaciation) and Wonnadinna Dolostone.|Disconformably overlies Aroota Group.||04-APR-12
9375|Keepera Group|65338|6|Mentioned|pp60-63.|||Named by Walter (1980); redefined by Kruse in Dunster et al. (2007). |||Includes Black Stump, Oorabra and Sun Hill Arkoses, Wonnadinna Dolostone, Little Burke Tillite and Boko Formation.|||
9375|Keepera Group|65341|6|Mentioned|p4, pp12-15. |Cryogenian|Cryogenian||||Includes Boko Formation and Oorabra Arkose.|||
9375|Keepera Group|66767|5|Briefly described|p58|Neoproterozoic|Neoproterozoic|Georgina Basin. Over 450m thick. Glacial units are tentatively attributed to the Marinoan glaciation.|||||Glacial sedimentary rocks and intertidal to deeper marine dolostone.|
9375|Keepera Group|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.|||Includes Boko Formation.|||
9375|Keepera Group|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
9375|Keepera Group|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Boko Formation.|||
9375|Keepera Group|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.|||Black Stump, Sun Hill, Oorabra Arkoses; Boko Formation; Little Burke Tillite.|Is overlain by Wonnadinna Dolostone.|Glacial outwash deposits.|12-JUL-16
9375|Keepera Group|69443|5|Briefly described|p28:2-3, 7-10, 31|Ediacaran|Cryogenian|Walter (1980); redefined by Kruse in Dunster et al. (2007). Southern Georgina Basin. Deposition followed uplift associated with the Rinkabeena Movement. Glacigene and post-glacial deposits. Equivalent to Olympic Formation, Pioneer Sandstone, middle to upper Inindia beds, Boord Formation and Mount Doreen Formation.|||Boko Formation; Oorabra, Black Stump, Sun Hill Arkoses; Little Burke Tillite; Wonnadinna Dolostone.|Disconformably overlies Aroota Group; overlain unconformably or disconformably by Shadow Group.||12-JUL-16
9375|Keepera Group|69673|6|Mentioned|p111, p114 fig 92, p115|Neoproterozoic|Neoproterozoic||||Includes Black Stump Arkose, Oorabra Arkose, Boko Formation, Wonnadinna Dolostone|||
9375|Keepera Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Oorabra Arkose.|Disconformably overlain by the Mopunga Group. Disconformably overlies the Aroota Group.||20-APR-22
9375|Keepera Group|72516|5|Briefly described|p13, p21, p85-87, p135, p171, p176|Ediacaran|Ediacaran|Georgina Basin.|||Includes the Oorabra Arkose.|Disconformably overlain by the Mopunga Group.||20-APR-22
9375|Keepera Group|72711|6|Mentioned|p3 Fig.2.|||Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
9383|Keilambete Tonalite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37. Reserved as Keilambete Granodiorite.||||||
9383|Keilambete Tonalite|43029|2|Defined|p22||Devonian|see also Fig.2,p16||||||
9383|Keilambete Tonalite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
9383|Keilambete Tonalite|43213|4|Described|p98,p110,p116-121, p174-175, p178, p233|Devonian|Devonian|See also p241-242. See also [superseded] Keilambete Granodiorite (p96-97, p208, p217). Type locality described. Part of the Retreat Batholith. Geochemistry and geophysics detailed.||||Intrudes Bathampton Metamorphics and Gem Park Granite.|Dark grey to grey, locally foliated, fine- to coarse-grained, subequigranular to porphyritic biotite-hornblende tonalite.|
9394|Kelly Creek Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone, siltstone.||||||
9394|Kelly Creek Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Quartzose sandstone and dolomite.||||||
9394|Kelly Creek Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
9394|Kelly Creek Formation|12951|5|Briefly described|p143 fig 4, p145 fig 6, p151|Early Ordovician|Early Ordovician|Georgina Basin.||||||
9394|Kelly Creek Formation|13995|6|Mentioned|p99|||Georgina Basin.||||||
9394|Kelly Creek Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
9394|Kelly Creek Formation|22954|6|Mentioned|Fig3p9|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: ~170m.||||||
9394|Kelly Creek Formation|24442|5|Briefly described|p49|Early Cambrian|Early Cambrian|Overlain by Coolibah Formation.  On TOBERMORY sheet.||||||
9394|Kelly Creek Formation|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9394|Kelly Creek Formation|30983|6|Mentioned|p70|||||||||
9394|Kelly Creek Formation|31572|6|Mentioned|p21|||Correlation chart||||||
9394|Kelly Creek Formation|33111|4|Described|p37|||Mention Fig.9||||||
9394|Kelly Creek Formation|33738|6|Mentioned|p49|||||||||
9394|Kelly Creek Formation|34454|5|Briefly described|Table 2|||p16.||||||04-OCT-06
9394|Kelly Creek Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||04-OCT-06
9394|Kelly Creek Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|35139|4|Described|Table.2|||||||||
9394|Kelly Creek Formation|36234|3|Fully described|p170|||||||||
9394|Kelly Creek Formation|36243|6|Mentioned|Table 1A|||||||||
9394|Kelly Creek Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
9394|Kelly Creek Formation|36580|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|37572|4|Described|p162|||See also Fig.8||||||
9394|Kelly Creek Formation|38532|4|Described|Fig.1|||||||||
9394|Kelly Creek Formation|38832|6|Mentioned|p157|||||||||
9394|Kelly Creek Formation|39445|5|Briefly described|Table 4|||Disconformity within. See also p64 and Fig.5.||||||04-OCT-06
9394|Kelly Creek Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|39943|6|Mentioned|Table 2B|||||||||
9394|Kelly Creek Formation|40136|5|Briefly described|p29|||||||||
9394|Kelly Creek Formation|40906|6|Mentioned|Fig.11|||||||||
9394|Kelly Creek Formation|41524|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|42059|6|Mentioned|Fig.2 P131|||||||||
9394|Kelly Creek Formation|42060|6|Mentioned|Fig.5 P140|||||||||
9394|Kelly Creek Formation|42643|6|Mentioned|p32|||||||||
9394|Kelly Creek Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
9394|Kelly Creek Formation|43803|6|Mentioned|Fig.5,p71|||||||||
9394|Kelly Creek Formation|43808|5|Briefly described|p294|||||||||
9394|Kelly Creek Formation|44233|14|Not recorded|Fig.1||Early Ordovician|||||||
9394|Kelly Creek Formation|44308|14|Not recorded|p10,11,Tb.1||Early Ordovician|||||||
9394|Kelly Creek Formation|44309|2|Defined|Tb.1,p11,12,17,map||Ordovician|||||||
9394|Kelly Creek Formation|44312|14|Not recorded|Map Legend||Early Ordovician|||||||
9394|Kelly Creek Formation|44326|14|Not recorded|Map Legend||Early Ordovician|||||||
9394|Kelly Creek Formation|44358|5|Briefly described|p10,19|||similar lithologically and stratigraphically to Swift Formation.||||||
9394|Kelly Creek Formation|44469|2|Defined|p.9,19,Tb.I|||(F53-12). See also p.13-16,Tb.II. Conformably overlies Ninmaroo Fm.;Overlain by Coolibah Fm. Laterally equiv.to lower part of Tomahawk Beds. Similar lithology to Swift Fm.Fossils Good aquifer.||||||04-OCT-06
9394|Kelly Creek Formation|44470|5|Briefly described|map legend|||Upper Proterozoic to Lower Cambrian.||||||02-DEC-04
9394|Kelly Creek Formation|44848|14|Not recorded|p111|||||||||
9394|Kelly Creek Formation|44852|14|Not recorded|p71||Early Ordovician|||||||
9394|Kelly Creek Formation|44920|14|Not recorded|Map Legend,Sheet 4||Early Ordovician|||||||
9394|Kelly Creek Formation|45052|2|Defined|p124|Early Ordovician|Early Ordovician|See also p37.||||||04-OCT-06
9394|Kelly Creek Formation|45155|6|Mentioned|Fig.8|||||||||
9394|Kelly Creek Formation|46887|6|Mentioned|p251|||||||||
9394|Kelly Creek Formation|46897|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|46956|6|Mentioned|p160|||||||||
9394|Kelly Creek Formation|46958|6|Mentioned|p195|||See also Fig.2.||||||
9394|Kelly Creek Formation|46959|6|Mentioned|p213|||||||||
9394|Kelly Creek Formation|47024|6|Mentioned|p2|||||||||
9394|Kelly Creek Formation|48901|14|Not recorded|Not recorded|Early Ordovician|Late Cambrian|U.Camb-L.Ord.||||||
9394|Kelly Creek Formation|49027|4|Described|p16|||||||||
9394|Kelly Creek Formation|60122|3|Fully described|p27, p4, p10 Tb. 1, p28 Fig. 33|Early Ordovician|Early Ordovician|Conformable on Tomahawk and Ninmaroo Fms; disconformable on Ninmaroo Fm and Georgina Lst; unconformable beneath Nora Fm, conformable below Coolibah Fm; also unconformably overlain by Austral Downs Lst. . Max. thickness: 290m. Geol. Prov: Georgina Basin.||||||17-MAY-05
9394|Kelly Creek Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Quartzose and dolomitic quartz sandstone, siltstone, dolostone, partially dolomitised limestone, minor conglomerate.  Overlies the Arrinthrunga and Ninmaroo Formations.||||||
9394|Kelly Creek Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Quartzose and dolomitic quartz sandstone, siltstone, dolostone, partially dolomitised limestone, minor conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
9394|Kelly Creek Formation|63450|5|Briefly described|p76, p78 Fig. 5|Arenig|Arenig|Overlies Ninmaroo Formation; overlain by conformably by Coolibah Formation. Max. thickness: 290m. Geological province: Georgina Basin, West Toko Syncline. Lower section predominantly sandstone; upper part is dolostone and dolomitised limestone.||||||07-FEB-11
9394|Kelly Creek Formation|63562|6|Mentioned|p338 fig 3, p352 Fig.10|Early Ordovician|Early Ordovician|Of Georgina Basin.||||Overlies Tomahawk Formation. Is overlain by Nora Formation.||
9394|Kelly Creek Formation|64068|3|Fully described|p75-76, p71,73,78, 82, 226|Early Ordovician|Late Cambrian|Established by Casey in Smith (1965).Parts formerly included in Dulcie Sandstone (Joklik 1955), Ninmaroo Formation (Prichard 1960), Tomahawk Formation (Smith 1964), Tarlton Formation (Smith 1965).||Of Toko Group.||Conformably overlies Tomahawk Formation and conformably to disconformably overlies Ninmaroo Formation. Conformably overlain by Coolibah Formation or Nora Formation.|Sandstones, dolostone, siltstone, minor conglomerate and coquinite; overlain by dolostone, sandstone, dolomudstone, dolomitic limestone, minor conglomerate. Contains surficial manganocrete.|04-APR-12
9394|Kelly Creek Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Dulcie Syncline, Southern Georgina Basin.||||||
9394|Kelly Creek Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
9394|Kelly Creek Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
9394|Kelly Creek Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician||Conformably overlies Tomahawk beds; disconformably overlain by Dulcie Sandstone. Geological province: southern Georgina Basin/Dulcie Syncline. Comprises fresh water/aeolian clastic rocks.||||||07-FEB-11
9394|Kelly Creek Formation|65341|6|Mentioned|p2 Fig.2. |Ordovician|Ordovician|||||||
9394|Kelly Creek Formation|65342|5|Briefly described|p6.|||Georgina Basin. |||||Quartzose and glauconitic sandstone; minor dolostone, mudstone, and conglomerate; upper part dominantly limestone with lesser interbedded sandstone, marl at top.|
9394|Kelly Creek Formation|65489|5|Briefly described|p125-128|Ordovician|Early Ordovician|Georgina Basin. A thick and relatively homogeneous dolostone reservoir exists in this unit. Hosts the Ethabuka 1 gas discovery.||||Overlies Ninmaroo Formation. Is overlain by Coolibah Formation.||
9394|Kelly Creek Formation|66767|5|Briefly described|p59|Ordovician|Ordovician|Southern Georgina Basin.||Toko Group.|||Dolomitic quartz sandstone and dolostone.|
9394|Kelly Creek Formation|67323|5|Briefly described|p81, p83, p88, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. Toko Syncline, Georgina Basin. Age: Ordovician? A petroleum target in the underexplored Georgina Basin. An aquifer supplying water bores.||Toko Group.||Overlies Ninmaroo Formation. Is overlain by Nora Formation unconformably and Coolibah Formation conformably.|Sandstone, dolomite, siltstone, coquinite|
9394|Kelly Creek Formation|67402|6|Mentioned|p25, p25 tbl RRM3|Chewtonian|Bendigonian|Georgina Basin, West Toko Syncline. Maximum thickness of 290m. Potential reservoir for carbon dioxide storage. Sealed by the Nora Formation. See also p165 tbl LPB1, p213 fig GRG3, p214, p215, p217.  ||||Overlies the Ninmaroo Formation. Overlain by the Coolibah or Nora Formations.|Predominantly sandstone overlain by dolostone and dolomitised limestone.|
9394|Kelly Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as the Toko Group and Coolibah Formation, are all mapped under the symbol, Ot.||||||
9394|Kelly Creek Formation|69437|5|Briefly described|p22:10, 15|Ordovician|Ordovician|Southern Georgina Basin. Hosts surficial manganocrete and pisolitic manganiferous lag.||||Overlies Tomahawk, Ninmaroo Formations. Is overlain by Coolibah Formation.||12-JUL-16
9394|Kelly Creek Formation|69443|4|Described|p28:7, 26-28, 30, 44, 46|Early Ordovician|Early Ordovician|Casey in Smith (1965). Southern Georgina Basin. Forms prominent hills, scarps and dissected plateaux. Contains a varety of sedimentary structures (listed). 92-290m thick. Sparse fossil assemblage. Peritidal to unrestricted open-marine deposits. Hosts uneconomic manganese deposits at the Halfway Dam prospect. Potential petroleum reservoir. Flowed gas from Ethabuka-1 in Qld.||Toko Group.||Overlies Tomahawk and Ninmaroo Formations, conformably to locally disconformably. Is overlain conformably by Coolibah or Nora Formations, or unconformably by Dulcie Sandstone.|Lower interval of calcareous and dolomitic sandstones, dolostone, siltstone, minor conglomerate and coquinite, overlain by an upper interval of dolostone, dolomitic quartz sandstone, dolomudstone, quartzose dolomitic limestone and minor conglomerate.|12-JUL-16
9394|Kelly Creek Formation|69591|5|Briefly described|p87, p93-95, p97|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. This unit is here removed from the otherwise clastic-dominated Toko Group and assigned to the carbonate-dominated Cockroach Group. Up to 168m thick. Contains a diverse and abundant fauna (listed).||Cockroach Group.||Conformably/disconformably overlies Ninmaroo Formation. Is overlain disconformably by Coolibah Formation and Nora Formation.|Includes quartz and calcareous sandstones, siltstone, dolomite, calcarenite and silicified coquinite with lenses of white chert.|
9394|Kelly Creek Formation|69673|4|Described|p118, p120, p127, p129, p135, p137, p140|Ordovician|Ordovician|92m thick. Potential source rocks present.||Toko Group||Conformably overlain by Coolibah Formation, conformably overlies Tomahawk Formation, Ninmaroo Formation|Calcareous and dolomitic sandstone, dolostone, siltstone, dolomudstone, limestone and minor conglomerate and coquinite.|
9394|Kelly Creek Formation|70380|6|Mentioned|p745|Floian|Tremadocian|Southern Georgina Basin.||||||
9394|Kelly Creek Formation|71800|6|Mentioned|p26 fig 3|Early Ordovician|Early Ordovician|Georgina Basin.||||Overlies the Tomahawk Formation. Overlain by the Nora Formation.||
9394|Kelly Creek Formation|72516|6|Mentioned|p11, p94|||Georgina Basin.||||Conformably overlies the Tomahawk Formation.||
9394|Kelly Creek Formation|73591|6|Mentioned|p40|||Georgina Basin.||||||
9437|Kennedy Siltstone|22836|6|Mentioned|Fig.10 p402|||||||||
9437|Kennedy Siltstone|23031|6|Mentioned|27|||Geol province Leichardt River Subprovince. Parent Mount Isa Group.||||||
9437|Kennedy Siltstone|23362|5|Briefly described|339|||||||||
9437|Kennedy Siltstone|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group.||||||07-NOV-08
9437|Kennedy Siltstone|23397|5|Briefly described|p469|||||||||
9437|Kennedy Siltstone|23398|6|Mentioned|p442|||||||||
9437|Kennedy Siltstone|23399|4|Described|p498|||Of Mount Isa Group.||||||01-OCT-08
9437|Kennedy Siltstone|23408|4|Described|p512|||Of Mount Isa Group. Contains stromatolites, halite pseudomorphs, flat pebble conglomerates and x-bedded channel deposits.||||||15-JUN-09
9437|Kennedy Siltstone|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
9437|Kennedy Siltstone|23961|6|Mentioned|p1192 Fig. 3|||Geological Province: Mt Isa Inlier.||||||
9437|Kennedy Siltstone|23969|6|Mentioned|p1379 Fig.6|||Geological Province: Mount Isa Inlier.||||||02-MAR-05
9437|Kennedy Siltstone|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: Mount Isa Group.||||||07-NOV-08
9437|Kennedy Siltstone|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group. Overlies Spear Siltstone.||||||01-OCT-08
9437|Kennedy Siltstone|30535|6|Mentioned|p403|||Refers Bennett(1965). See also P405||||||
9437|Kennedy Siltstone|31207|6|Mentioned|Table 1|||||||||
9437|Kennedy Siltstone|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9437|Kennedy Siltstone|32041|4|Described|p356|||||||||
9437|Kennedy Siltstone|32042|4|Described|p44|||||||||
9437|Kennedy Siltstone|32660|5|Briefly described|Table 5|||||||||
9437|Kennedy Siltstone|32959|6|Mentioned|Fig.21|||||||||
9437|Kennedy Siltstone|33900|5|Briefly described|p14|||||||||
9437|Kennedy Siltstone|34499|6|Mentioned|Table 1|||||||||
9437|Kennedy Siltstone|34754|6|Mentioned|p42|||||||||
9437|Kennedy Siltstone|35074|6|Mentioned|Fig.2|||||||||
9437|Kennedy Siltstone|35116|6|Mentioned|Table.4|||||||||
9437|Kennedy Siltstone|39445|5|Briefly described|Table 2|||||||||
9437|Kennedy Siltstone|40623|5|Briefly described|p101|||||||||
9437|Kennedy Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
9437|Kennedy Siltstone|42072|6|Mentioned|Fig.1 P1615|||||||||
9437|Kennedy Siltstone|42350|6|Mentioned|Fig.1 P543|||||||||
9437|Kennedy Siltstone|42782|6|Mentioned|p458|||of Mount Isa Group||||||
9437|Kennedy Siltstone|43760|6|Mentioned|p441|||||||||
9437|Kennedy Siltstone|44517|2|Defined|p234-236,244,map||Paleoproterozoic|Unit of Mount Isa Group.||||||07-NOV-08
9437|Kennedy Siltstone|44843|14|Not recorded|p175|||||||||
9437|Kennedy Siltstone|45072|4|Described|p35|||Group 2 shales. Chem. anal. Table 9||||||
9437|Kennedy Siltstone|45136|5|Briefly described|p50|||||||||
9437|Kennedy Siltstone|45166|5|Briefly described|p28|||||||||
9437|Kennedy Siltstone|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
9437|Kennedy Siltstone|50624|5|Briefly described|p237 Fig.4||Statherian|Parent: Mount Isa Group.||||||24-NOV-04
9437|Kennedy Siltstone|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Overlain by Magazine Shale, underlain by Spear Siltstone. Geological Province: Western Fold Belt.||||||
9437|Kennedy Siltstone|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Mount Isa. Shown as Kennedy Slst.||Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
9437|Kennedy Siltstone|62535|5|Briefly described|p672, p674|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.||Mount Isa Group.||||
9437|Kennedy Siltstone|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
9437|Kennedy Siltstone|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Kennedy.||Of the Loretta supersequence||||
9437|Kennedy Siltstone|63866|5|Briefly described|p59|||Isa Superbasin.||Gun Supersequence||Equivalent to the overlying Loretta Supersequence.||
9437|Kennedy Siltstone|65228|6|Mentioned|p26, Fig.04.|||Part of Loretta Supersequence at Mount Isa.||||||
9437|Kennedy Siltstone|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
9437|Kennedy Siltstone|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Isa Superbasin.|~1660-1650 Ma.|Mount Isa Group.|||Dolomitic siltstone, dolomitic quartzite|
9437|Kennedy Siltstone|67499|6|Mentioned|p946||||||||Albitic|
9437|Kennedy Siltstone|68542|6|Mentioned|p6|||||||Overlies Spear Siltstone, overlain by Magazine Shale||
9437|Kennedy Siltstone|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Spear Siltstone. Is overlain by Magazine Shale.||
9437|Kennedy Siltstone|68732|6|Mentioned|p160, p165 Fig.3|||Presented as Magazine Kennedy Siltstone [?Magazine and Kennedy Siltstones].|1647 +/- 4 Ma|||||30-NOV-17
9437|Kennedy Siltstone|69591|5|Briefly described|p43 Fig.2.31, p45, p55|||Leichhardt River Domain, Isa Superbasin. Part of Gun Superseqeunce. Deposited below storm base.||Mount Isa Group.|||Dolomitic siltstone, dolomitic quartzite.|
9437|Kennedy Siltstone|70282|6|Mentioned|p544 Fig.1, p546|||Presented as Kennedy-Spear Siltstone.||||Overlies Urquhart Shale,||13-FEB-18
9437|Kennedy Siltstone|73525|6|Mentioned|p4-5 Fig.2|||Leichhardt River Domain. Misspelt as Silstone.|||||Carbonates.|
9451|Keppel Sands|41576|6|Mentioned|p24|||||||||
9451|Keppel Sands|42054|6|Mentioned|p272|||||||||
9451|Keppel Sands|42143|6|Mentioned|p597|||||||||
9521|Kianga Formation|22757|6|Mentioned|Table3,p9|Late Permian|Late Permian|Bowen Basin||||||
9521|Kianga Formation|24159|5|Briefly described|p148 Fig. 2, p147|Late Permian|Late Permian|Geological Province: Bowen Basin. Overlies the Back Creek Group. Unconformably overlain by the Showgrounds Sandstone.||||||
9521|Kianga Formation|24241|5|Briefly described|p19 Fig.4|Late Permian|Late Permian|||||||
9521|Kianga Formation|29490|6|Mentioned|p21|||||||||
9521|Kianga Formation|29721|6|Mentioned|Table 65|||||||||
9521|Kianga Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
9521|Kianga Formation|30743|6|Mentioned|p21|||Refers Mack (1963)||||||
9521|Kianga Formation|32712|6|Mentioned|Table 1|||||||||
9521|Kianga Formation|36100|6|Mentioned|p178|||||||||
9521|Kianga Formation|39494|6|Mentioned|Fig.5|||||||||
9521|Kianga Formation|40030|6|Mentioned|Fig.5|||||||||
9521|Kianga Formation|40249|6|Mentioned|p41|||||||||
9521|Kianga Formation|40544|6|Mentioned|p161|||See also Fig.6||||||
9521|Kianga Formation|41159|4|Described|p340|||||||||
9521|Kianga Formation|41210|5|Briefly described|p165|||||||||
9521|Kianga Formation|41247|6|Mentioned|p128|||See also Fig.7||||||
9521|Kianga Formation|41725|6|Mentioned|p403|||||||||
9521|Kianga Formation|42463|6|Mentioned|Fig.5 P172|||||||||
9521|Kianga Formation|42634|6|Mentioned|Fig.10 P30|||||||||
9521|Kianga Formation|43883|14|Not recorded|p18 Fig.4-3,19|||||||||
9521|Kianga Formation|43912|14|Not recorded|2,7|||(Cabawin No.1)||||||
9521|Kianga Formation|43916|14|Not recorded|p2481||Permian|||||||
9521|Kianga Formation|44163|4|Described|p1,2,10-13,17-20,|Early Triassic|Late Permian|Pl.1,4||||||
9521|Kianga Formation|44164|4|Described|p1,13,16-18,20,27-8,|||Oil Producing. p30, Fig.4,Pl.1.||||||
9521|Kianga Formation|44165|4|Described|p1,8,9,11,16-18,|||Fig.4,Pl.1. Oil Producing.||||||
9521|Kianga Formation|44166|14|Not recorded|p1,9,10,Pl.2|||||||||
9521|Kianga Formation|44566|4|Described|p13,15-17,Pls.2,3|||||||||
9521|Kianga Formation|44567|14|Not recorded|p11,13-15|||||||||
9521|Kianga Formation|44568|4|Described|p1,4,6,7,Pls.1,3|||||||||
9521|Kianga Formation|44585|14|Not recorded|p45-Fig.2|||||||||
9521|Kianga Formation|44610|14|Not recorded|p49,Tb.1|||||||||
9521|Kianga Formation|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
9521|Kianga Formation|44627|14|Not recorded|p139-141||Permian|||||||
9521|Kianga Formation|44844|14|Not recorded|p154||Permian|Cabawin No.1.||||||
9521|Kianga Formation|44853|14|Not recorded|p299,301||Permian|||||||
9521|Kianga Formation|44855|14|Not recorded|p27||Permian|Tuffaceous sandstone.||||||
9521|Kianga Formation|45110|6|Mentioned|Table 13|||||||||
9521|Kianga Formation|47122|14|Not recorded|?|||||||||
9521|Kianga Formation|48600|2|Defined|p7-23|||Formation of Bowen Group.||||||
9521|Kianga Formation|48603|14|Not recorded|?|||||||||
9521|Kianga Formation|61377|5|Briefly described|p150, p157|Late Permian|Late Permian|Of Blackwater Gp. Volcanogenically derived terrestrial conglom., sst and sltst sequence. Conformable on Back Creek Group; unconformable beneath Rewan Group. Only present in northern part of Surat Basin. Equivalent of lower Digby Fm (Gunnedah Basin).||||||07-FEB-11
9521|Kianga Formation|64099|5|Briefly described|p374 Fig 5|Permian|Permian|Underlies Sagittarius Sandstone. Geol Prov: Bowen Basin.||||||
9521|Kianga Formation|64856|6|Mentioned|p61, p78|||Permian coal measures.| | ||||31-JAN-13
9521|Kianga Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Cabawin Formation. Underlain by Back Creek Formation.||
9521|Kianga Formation|68004|5|Briefly described|p142.|Late Permian|Late Permian|Far NE of the Brigalow Belt South Bioregion. Equivalent to Black Jack Group. Contains coal but at depths >600 m.||||||
9521|Kianga Formation|68202|6|Mentioned|p176|Permian|Permian|Bowen Basin.||||||
9557|Killala Creek Limestone|31586|6|Mentioned|p6|||Correlation of Visean coral horizons.||||||
9557|Killala Creek Limestone|31587|6|Mentioned|p59|||Geological map||||||
9557|Killala Creek Limestone|32388|6|Mentioned|Fig.1|||||||||
9557|Killala Creek Limestone|33774|6|Mentioned|p21|||Faunal zones||||||
9557|Killala Creek Limestone|36528|6|Mentioned|p173|||||||||
9557|Killala Creek Limestone|39239|5|Briefly described|p119|||||||||
9557|Killala Creek Limestone|42002|5|Briefly described|p92|||||||||
9557|Killala Creek Limestone|42547|4|Described|p52|||||||||
9557|Killala Creek Limestone|44360|14|Not recorded|p16,30,32||Early Carboniferous|Equivalent of Baywulla Formation.||||||
9563|Kilmarnock Granodiorite|42614|6|Mentioned|Table 2 P12|||Reserved as Kilmarnock Quartz Monzonite.||||||
9563|Kilmarnock Granodiorite|42747|5|Briefly described|p37, Fig.9|||||||||
9563|Kilmarnock Granodiorite|43029|2|Defined|p18||Middle Devonian|Rb-Sr date of 375 Ma,See also Fig.2,p16||||||
9563|Kilmarnock Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
9563|Kilmarnock Granodiorite|43213|3|Fully described|p33,p35,p95-97, p106, p116-121, p174-175|Devonian|Devonian|See also p178, p208, p210-211, p217-219, p232, p240, p243. Extensive unit in the Retreat Batholith. Type area described. Several ages are given, from 352 Ma (K-Ar biotite: Webb et al., 1963) to 375 +/- 3 Ma (Rb-Sr biotite-whole rock pair: Carr, pers. comm., 1993). Geochemistry, modal analyses and geophysics detailed.|352 - 375 Ma.|||Intrudes Bathampton Metamorphics and Rolfe Creek Schist. Is intruded by Hoy Basalt. Is faulted against Karmoo Quartz Diorite, Mount Observatory Granite and Mount Newsome Granodiorite.|Grey, fine- to coarse-grained, equigranular to porphyritic, hornblende-biotite granodiorite. Metasedimentary xenoliths common in the W, decreasing eastwards.|
9563|Kilmarnock Granodiorite|43861|5|Briefly described|28,29||Devonian|Intrudes Bathampton Metamorphics and Rolfe Creek Schist||||||
9563|Kilmarnock Granodiorite|68482|5|Briefly described|Map Legend|Famennian|Frasnian|Another site provided ages of 370 +/- 7 Ma, K-Ar (biotite); 361 +/- 7 Ma, K-Ar (hornblende).|375 +/- 3 Ma, Rb-Sr (biotite).||||Grey, fine to coarse-grained, equigranular to porphyritic hornblende-biotite granodiorite.|
9563|Kilmarnock Granodiorite|68731|6|Mentioned|p132|||||||||
9563|Kilmarnock Granodiorite|69599|5|Briefly described|p593|Devonian|Devonian|||||Is overlain unconformably by Red Mountain Formation.||
9570|Kimbala Granodiorite|22846|4|Described|p6,24-6,41,46,76|Early Triassic|Late Permian|||||||
9570|Kimbala Granodiorite|23609|4|Described|p13-15|||I-Type. Metaluminous.Also see p7 and 10 and Fig 1 p6. North d'Aguilar Block.||||||
9570|Kimbala Granodiorite|23799|5|Briefly described|p115 Fig. 10|Triassic|Permian|Geological Province: D'Aguilar Subprovince.||||||
9570|Kimbala Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
9570|Kimbala Granodiorite|35101|3|Fully described|p70|||||||||
9570|Kimbala Granodiorite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
9570|Kimbala Granodiorite|39445|5|Briefly described|Table 12|||||||||
9570|Kimbala Granodiorite|41917|6|Mentioned|p522|||||||||
9570|Kimbala Granodiorite|43008|5|Briefly described|map legend|||||||||
9570|Kimbala Granodiorite|43588|6|Mentioned|p31|Early Triassic|Late Permian|||||||
9570|Kimbala Granodiorite|60077|5|Briefly described|Map legend|Triassic|Permian|Medium-grained, grey granodiorite.||||||
9570|Kimbala Granodiorite|60370|5|Briefly described|Map Legend|Triassic|Permian|Biotite-hornblende granodiorite||||||
9570|Kimbala Granodiorite|68679|5|Briefly described|p409, p411|Middle Triassic|Late Permian|Northern New England Orogen. Similar to Kingaham Creek Granodiorite; may be related in source and emplacement time.||||Intrudes Marumba beds.|Biotite-hornblende granodiorite.|21-NOV-21
9581|Kin Kin beds|23251|5|Briefly described|Table 1 p10, p20.|Middle Triassic|Early Triassic|The fossil content is similar to Brooweena Formation. Kin Kin Subprovince, Gympie Province.||||||28-NOV-05
9581|Kin Kin beds|23542|5|Briefly described|Fig 1 p378|||Also see p379. In the Gympie Province.||||||25-NOV-05
9581|Kin Kin beds|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|||||||
9581|Kin Kin beds|37618|6|Mentioned|Fig.1|||||||||
9581|Kin Kin beds|39284|5|Briefly described|p431|||||||||
9581|Kin Kin beds|40051|4|Described|p8|||||||||
9581|Kin Kin beds|40475|6|Mentioned|p7|||||||||
9581|Kin Kin beds|40623|5|Briefly described|p53|||||||||
9581|Kin Kin beds|41917|6|Mentioned|p521|||||||||
9581|Kin Kin beds|42450|4|Described|p405|||||||||
9581|Kin Kin beds|42492|6|Mentioned|p12|||||||||
9581|Kin Kin beds|42695|5|Briefly described|Fig.2|Triassic||||||||
9581|Kin Kin beds|42751|4|Described|p25|||||||||
9581|Kin Kin beds|42764|4|Described|p21|||||||||
9581|Kin Kin beds|43006|4|Described|Table 1, p239|||||||||
9581|Kin Kin beds|43077|5|Briefly described|p4|||||||||
9581|Kin Kin beds|43100|4|Described|p33|||Contains fossils of Early Triassic age.||||||
9581|Kin Kin beds|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
9581|Kin Kin beds|44928|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
9581|Kin Kin beds|60281|5|Briefly described|Fig. 30 App 1|Early Triassic|Early Triassic|Equivalent to the Brooweena Formation.  Geological Province: Maryborough Basin.||||||28-NOV-05
9581|Kin Kin beds|61772|6|Mentioned|p129 Fig. 4||Middle Triassic|In New England Orogen.||||||14-AUG-08
9581|Kin Kin beds|61780|4|Described|p255|Early Triassic|Triassic|Underlain by Gympie Group. Thickness: >300m. Arenite, argillite, phyllite, claystone. Forearc setting.||||||
9581|Kin Kin beds|63821|5|Briefly described|p16, p18, p36|Middle Triassic|Early Triassic|Geological Province: Gympie Province. Fine-grained turbidite deposits with slaty and crenulation cleavages; contains Triassic marine fossils, including crinoid stems.||||||07-FEB-11
9581|Kin Kin beds|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Gympie Province. This unit, as well as the Brooweena, Keefton and Traveston Formations, are all mapped under the symbol, Rb.||||||
9581|Kin Kin beds|68679|5|Briefly described|p312-313, p369-370, p437, p469, p471|Middle Triassic|Early Triassic|Southern Gympie Province, Northern New England Orogen. Murphy et al. (1976) combined the Traveston Formation and the Kin Kin Phyllite, both by Runnegar and Ferguson (1969) and which were not possible on field relationships to map separately, as the Kin Kin beds. Over 500m thick. Contains Olenekian marine fossils. Appears as Kin Kin Fm. on p469.||||Is overlain unconformably by Kullangor Member. With Keefton Formation, is equivalent to the Brooweena Formation.|Metasiltstone, metashale, phyllite, fine-grained marine turbidite with slaty crenulation cleavage.|
9581|Kin Kin beds|69599|5|Briefly described|p595, p637|||Noosa hinterland, Gympie Province.||||Is overlain by Pomona beds.||
9581|Kin Kin beds|70913|5|Briefly described|p6, p7, p76|Late Triassic|Early Triassic|Kin Kin Subprovince of the Gympie Province. Previously included in Upper Gympie Formation of Dunstan (1911), Gympie Group. Shown as Kin Kin Beds p12. Strong cleavage.|||||Shales.|18-SEP-17
9581|Kin Kin beds|72037|4|Described|p859,861-865,867|Middle Triassic|Early Triassic|Geological province: New England Orogen, Gympie Terrane. Depositional environment: marine. LA-ICP-MS peak detrital zircon U-Th-Pb ages include 240, 256, 296, 318, and 394 Ma. Maximum depositional age at 240 Ma, which is younger than Early Triassic ammanoid fauna within the Kin Kin beds described by Runnegar and Ferguson, 1969. Late Permian to Triassic detrital zircons likely sourced from a middle Permian to Triassic continental arc system to the west, which was built on the former accretionary complex of the New England Orogen Gust et al., 1993; Bryant et al., 1997; Holcombe et al., 1997b; Li et al., 2012b). Carboniferous-age zircons correspond to detritus eroded from a Carboniferous magmatic arc of the New England Orogen, or recycled through the Carboniferous fore-arc and accretionary complex rocks. Cambrian to Devonian zircons likely originated from the Tabberabberan (~382-397 Ma), Benambran (~430-450 Ma), and Delamerian (~490-516 Ma) orogenies (Korsch et al., 2009a).||||Fault contact with Keefton Formation.|Relatively homogenous sequence of phyllites and slate.|
9581|Kin Kin beds|72297|6|Mentioned|p728|Triassic|Triassic|Quarried at Anderleigh for coloured slate and decorative stone.||||||
9581|Kin Kin beds|73306|5|Briefly described|p564, 573, 575|Middle Triassic|Early Triassic|Gympie Terrane. Evidence of contractional deformation.|c.240 Ma (MDA: Li et al., 2015).|||Is overlain unconformably by North Arm Volcanics.|Strongly deformed phyllites and slates.|
9581|Kin Kin beds|73450|6|Mentioned|p86|Triassic|Triassic|||||Intruded by Allandale Granite.||
9588|Kinellan Basalt|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|Parent: Toogoolawah Group.||||||14-AUG-08
9588|Kinellan Basalt|41738|2|Defined|p165|Middle Triassic|Early Triassic|Reserved as Kinellan.||||||14-AUG-08
9588|Kinellan Basalt|41790|5|Briefly described|p473|||||||||
9588|Kinellan Basalt|61782|5|Briefly described|p275|||Of Toogoolawah Group, basaltic basal unit. Geol Prov: Esk Trough.||||||
9588|Kinellan Basalt|63821|5|Briefly described|p20|||Basal unit of Toogoolwah Group. Overlain by, and interfingers with, Gayndah Formation. Max. thickness: 300m. Geological Province: Esk Trough. Purple to grey, low-K tholeiitic basalt - amygdaloidal olivine basalt.||||||07-FEB-11
9588|Kinellan Basalt|68679|4|Described|p391, p437, p439|Late Triassic|Late Triassic|Northern Esk Basin. Occurs as small scattered outcrops. ~140-300m thick.  Has distinctive OIB-like trace element geochemistry.||Toogoolawah Group.||Is overlain disconformably by Gayndah Formation. With Gayndah Formation, is equivalent to the Bryden and Esk Formations. Possibly equivalent to (part of) the Abernethy Basalt.|Olivine basalt flows; amygdaloidal flow tops; separated by weathered zones; lower parts contain basement-derived oolitic limestone fragments. Chemically transitional between tholeiitic and alkali basalts; plots as "within-plate".|
9606|Kingaham Creek Granodiorite|22845|6|Mentioned|p46,69,82|Triassic|Permian|||||||
9606|Kingaham Creek Granodiorite|22846|2|Defined|p6-9,12,3,22-4,39-41|Triassic|Triassic|||||||
9606|Kingaham Creek Granodiorite|23609|4|Described|p6, 9, 7, 10.|||Also see Fig 1 p6. I-Type granite. North D'Aguilar Block.||||||
9606|Kingaham Creek Granodiorite|23799|5|Briefly described|p42,  p115 Fig. 10|Triassic|Permian|Creek is Ck. in text of figure.  Intrudes the Neara Volcanics.  Geological Province: Esk Trough.||||||
9606|Kingaham Creek Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
9606|Kingaham Creek Granodiorite|35101|3|Fully described|p72|||||||||
9606|Kingaham Creek Granodiorite|35161|6|Mentioned|p592|||||||||
9606|Kingaham Creek Granodiorite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
9606|Kingaham Creek Granodiorite|36954|6|Mentioned|p114|||||||||
9606|Kingaham Creek Granodiorite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
9606|Kingaham Creek Granodiorite|37376|6|Mentioned|Table 1|||||||||
9606|Kingaham Creek Granodiorite|39445|5|Briefly described|Table 12|||||||||
9606|Kingaham Creek Granodiorite|41917|6|Mentioned|p522|||||||||
9606|Kingaham Creek Granodiorite|43008|5|Briefly described|map legend|||||||||
9606|Kingaham Creek Granodiorite|43588|6|Mentioned|p31|Late Triassic|Early Triassic|||||||
9606|Kingaham Creek Granodiorite|44923|5|Briefly described|Map Legend||Triassic|||||||
9606|Kingaham Creek Granodiorite|50320|5|Briefly described|Map Legend|Triassic|Triassic|||||||
9606|Kingaham Creek Granodiorite|60077|5|Briefly described|Map legend|Triassic|Permian|Coarse-grained, grey granodiorite.||||||
9606|Kingaham Creek Granodiorite|60370|5|Briefly described|Map Legend|Triassic|Triassic|Hornblende-biotite granodiorite; quartz diorite to diorite; porphyritic microdiorite.||||||
9606|Kingaham Creek Granodiorite|68679|5|Briefly described|p331, p409, p411|Triassic|Permian|Northern New England Orogen. Other age determinations given.|238.9 +/- 7 Ma (K-Ar: Green, 1975).|||Intrudes Amamoor and Marumba beds. Is overlain by Neara Volcanics.|Hornblende-biotite granodiorite; quartz diorite to diorite; porphyritic microdiorite.|
9629|Kintore Supersuite|22780|5|Briefly described|map|Early Devonian|Late Silurian|||||||12-JAN-05
9629|Kintore Supersuite|22781|4|Described|p30|Paleozoic|Paleozoic|||||||07-NOV-08
9629|Kintore Supersuite|22811|6|Mentioned|p603|||of Pama Province||||||
9629|Kintore Supersuite|23420|4|Described|p 147 table 4.6|Early Devonian|Late Silurian|Also see table 4.8. Age: 407Ma. S-type granite.||||||12-JAN-05
9629|Kintore Supersuite|23430|5|Briefly described|p485|||S-Type granite. 1977-2200 Ma. Pama Province.||||||
9629|Kintore Supersuite|23496|5|Briefly described|p37|Devonian|Silurian|of Mackenzie and Knutson (1992).||||||
9629|Kintore Supersuite|42610|4|Described|p5, p6|||Contains Ebagoola Suite, Lankelly Suite. Igneous equivalent to Supergroup?||||||
9629|Kintore Supersuite|42640|5|Briefly described|p9|||Ebagoola 1:250000 sheet Equivalent to Kintore Adamellite?||||||
9629|Kintore Supersuite|42650|6|Mentioned|p14|||||||||
9629|Kintore Supersuite|42769|5|Briefly described|Fig.11|||||||||
9629|Kintore Supersuite|43596|4|Described|p24, p25-29, p26-27 Tb. 2|Early Devonian|Late Silurian|Contains Lukinville, Aralba, Ebagoola, Wipella, and Lankelly Suites. Major S-type component of the Siluro-Devonian Cape York Peninsula Batholith.||||||15-JAN-09
9629|Kintore Supersuite|43665|5|Briefly described|p14|||||||||
9629|Kintore Supersuite|43738|6|Mentioned|p5|Devonian|Silurian|||||||
9629|Kintore Supersuite|43741|4|Described|p7,21|Devonian|Silurian|||||||
9629|Kintore Supersuite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
9629|Kintore Supersuite|63154|5|Briefly described|p285 Fig. 5|Early Devonian|Early Devonian|Geological province: Coen Inlier.||||||
9629|Kintore Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|This unit, as well as the Flyspeck and Blue Mountains Supersuites, are all mapped under the same symbol, Dg.||||||
9629|Kintore Supersuite|69592|5|Briefly described|p282, p286-289, p297|||Cape York Peninsula Batholith. Geochemistry described in some detail. Characterised by widespread prominent flakes and small books of muscovite and pale pink-violet garnet. CONSTITUENTS continued: Heneage, Imooya, Ingleby, Kingvale, Kendle River, King Junction, Kintore, Kokomini, Kopo, Laia, Lankelly, Lindalong, Leconsfield, Lilyponds, McIlwraith, Mena, Morehead, Pelican Creek, Pine Tree Creek, Rocky King, Rosser Creek, Strathleven, Tadpole, Terrible Creek, The Falls, Top Pinnacle, Turtle Swamp, Ukin, Warner, Wongu Granites.|||Lukinville, Wipella Granodiorites; Aralba, Artella, Barwon, Bunira, Bums, Burton Lagoon, Buthen Buthen, Chevy Creek, Culpin, Dixie, Ebagoola, Fernhill, Fish Creek, Goanna Granites. More in COMMENTS.||S-type. Even-grained, variably porphyritic muscovite-biotite granite and granodiorite; biotite granite and granodiorite; (biotite-)muscovite leucogranite; pegmatite, aplite. Granophyric textures common.|
9629|Kintore Supersuite|70207|5|Briefly described|p72-73, p77|||Cape York Peninsula Batholith. Unit in Pama Igneous Association.|~415-375 Ma.||Aralba Granite, Lukinville Suite.||S-type.|
9629|Kintore Supersuite|71792|5|Briefly described|p13, p26, p29-p31|Devonian|Devonian|Coen Inlier. S-type supersuite; this is the most widespread supersuite in the Cape York Peninsula Batholith. Includes the informal units Dgk/9 and Dgk/10. |||Includes the Buthen Buthen Suite, Kintore Granite and the Little Round Back Granite.|Intrudes the Choc-a-Block Orthogneiss.||
9629|Kintore Supersuite|71849|4|Described|p2, p8, p13-18, p46, p50-51, p56-57, p60|Devonian|Devonian|See also p65, p67, p71, p81, p84-86, p89, p94, p104, p107-108, p110, p114, p122, p125, p147-163, p166, p173-177, p183-184, p195. The most widespread Supersuite in the Cape York Peninsula Batholith; extends the length of the Coen Inlier. Geochemistry detailed.|||Kintore, Lankelly, Buthen Buthen Suites.||Highly-reduced, S-type granitoids.|
9629|Kintore Supersuite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Buthen Buthen, Ebagoola Suites; Little Round Back Granite.|||
9629|Kintore Supersuite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Buthen Buthen, Ebagoola, Lankelly Suites.|||
9629|Kintore Supersuite|73387|6|Mentioned|p1, p29, p36|Early Devonian|Early Devonian|S-type. Dominates Devonian granitoids of the Cape York Peninsula Batholith by volume; northernmost exposed representatives of the Pama Igneous Association. Emplacement is associated with metamorphism in the Coen Metamorphic Group.|c. 409-405 Ma||Keane Granite||Granitoids.|
9631|Kipper Creek Andesite Member|23799|5|Briefly described|p31|||Of Pinecliff Formation.  Geological Province:  Gympie Province.  See also Kipper Creek Andesites.||||||
9631|Kipper Creek Andesite Member|33381|4|Described|p108|||Permian. Pinecliff Fm.||||||
9649|Kitoba Member|23086|6|Mentioned|p668|||Hodgkinson Formation.||||||
9649|Kitoba Member|23423|5|Briefly described|p232|||Faulted against Chillagoe Formation. Parent: Hodgkinson Formation. Hodgkinson Province.||||||
9649|Kitoba Member|23500|5|Briefly described|Map legend|Early Devonian||Age: Late Silurian? - Early Devonian. Of Hodgkinson Formation, Hodgkinson Province.||||||
9649|Kitoba Member|23616|4|Described|Table 1C p14; p33|||Kitoba Member interpreted to form basal part of Hodgkinson Formation sequence, conformably overlying Chillagoe Formation. Of Hodgkinson Formation, Hodgkinson Province.||||||
9649|Kitoba Member|23713|4|Described|p73 Appendix 2, p14|||Includes most of the rocks formerly mapped as Mount Garnet Formation. One of the oldest parts of the Hodgkinson Formation, but age unknown. Of Hodgkinson Formation, Hodgkinson Province.||||||
9649|Kitoba Member|24485|3|Fully described|p26, p34 Tb.4|Devonian|Early Devonian|Faulted against the Chillagoe Formation. Parent: Hodgkinson Formation. Geological Province: Hodgkinson Province||||||
9649|Kitoba Member|24486|5|Briefly described|Map legend|Devonian|Late Silurian|Of the Hodgkinson Formation.  Geological Province: Hodgkinson Province.||||||
9649|Kitoba Member|42500|6|Mentioned|p27|||of Hodgkinson Formation. Supersedes Mount Garnet Formation.||||||
9649|Kitoba Member|42620|4|Described|p107|||of What Formation? Hodgkinson?||||||
9649|Kitoba Member|43083|3|Fully described|p52 Tb 5, p62|||Of Hodgkinson Formation. Previously mapped as Mount Garnet Formation. Unconformably overlain by Nychum Volcanics and Featherbed Volcanic group. Geological province: Hodgkinson Province.||||||17-JUN-09
9649|Kitoba Member|43151|5|Briefly described|Map legend|||Of the Hodgkinson Formation. Feldspathic quartz arenite; rare graded bedding and ripple lamination. Early Devonian - Late Silurian? in age.||||||15-JUN-06
9649|Kitoba Member|43254|5|Briefly described|map legend|Late Devonian|Late Silurian|of Hodgkinson Formation.||||||
9649|Kitoba Member|43285|5|Briefly described|Map Legend|||age Late Silurian? to Late Devonian?Of Hodgkinson Formation.||||||
9649|Kitoba Member|43625|3|Fully described|p19,26,30|||||||||
9649|Kitoba Member|43626|6|Mentioned|p68|||||||||
9649|Kitoba Member|44246|5|Briefly described|Map Legend||Devonian|||||||
9649|Kitoba Member|60357|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Geological Province: Hodgkinson Province. Of the Hodgkinson Formation.||||||
9649|Kitoba Member|60425|3|Fully described|p26|||Of Hodgkinson Fm. Formerly mapped as most of Mount Garnet Fm. Fault against Chillagoe Fm. In Hodgkinson Prov. Distinctive sequences of mainly arenite beds with subordinate mudstone, pebbly arenite and conglomerate, and minor siltstone, chert + metabasalt||||||07-FEB-11
9649|Kitoba Member|69030|5|Briefly described|p6|Devonian|Devonian|Chillagoe Subprovince, Hodgkinson Province.||Hodgkinson Formation.||||
9649|Kitoba Member|69592|5|Briefly described|p231 Fig.4.4, p232, p237, p238 Fig.4.17|Devonian|Silurian|Mossman Orogen, Palmer-Barron Subprovince, Hodgkinson Province. Regarded more as sedimentary and volcanic rock assemblages rather than stratigraphic units which imply superpositional relationships. Up to 25km wide, along the Walsh Fault.||Hodgkinson Formation.||Abuts (is faulted against) Chillagoe Formation.|Apart from the usual Hodgkinson Formation lithologies, this unit is characterised by prominent thick, amalgamated sandstone intervals of coarser grain size.|
9649|Kitoba Member|70345|4|Described|p4, p13-18, p22, p24, p34|Lochkovian|Lochkovian|Sample locality, zircon morphology, SHRIMP analyses and results are discussed. Forms a prominent outcrop at the western side of the Burke Developmental Road. Sandstone there is massive with no obvious bedding, and forms large rounded boulders and massive outcrops. Interpreted to be slightly younger than and possibly even contemporaneous with the Chillagoe Formation.|417 +/- 10 Ma (SHRIMP U-Pb)|Hodgkinson Formation||Faulted against the Chillagoe Formation and the OK Member.|Gray, thick, amalgamated and coarse-grained sandstones.|
9649|Kitoba Member|71031|5|Briefly described|p71|Early Carboniferous|Late Silurian|||Hodgkinson Formation|||Mainly thick bedded-massive, quartzofeldspathic sandstone, chert and metabasalt.|
9649|Kitoba Member|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen.|417+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
9656|Knapdale Quartzite|23959|6|Mentioned|p1165|||Geological Province: Cloncurry Basin.||||||
9656|Knapdale Quartzite|30192|6|Mentioned|Fig.4|||||||||
9656|Knapdale Quartzite|30532|3|Fully described|p115|||||||||
9656|Knapdale Quartzite|33791|4|Described|p373|||||||||
9656|Knapdale Quartzite|33900|6|Mentioned|p15|||||||||
9656|Knapdale Quartzite|35074|6|Mentioned|Fig.2|||||||||
9656|Knapdale Quartzite|35309|4|Described|p373|||||||||
9656|Knapdale Quartzite|35470|6|Mentioned|p22|||||||||
9656|Knapdale Quartzite|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
9656|Knapdale Quartzite|37568|5|Briefly described|p84|||Of Mount Albert Group.||||||
9656|Knapdale Quartzite|38235|6|Mentioned|p115|||||||||
9656|Knapdale Quartzite|38278|6|Mentioned|Fig.3|||||||||
9656|Knapdale Quartzite|38619|6|Mentioned|p127|||||||||
9656|Knapdale Quartzite|38833|6|Mentioned|p161|||||||||
9656|Knapdale Quartzite|38834|6|Mentioned|p163|||||||||
9656|Knapdale Quartzite|39445|6|Mentioned|p43|||See also Table 2||||||
9656|Knapdale Quartzite|39492|6|Mentioned|p28|||||||||
9656|Knapdale Quartzite|39622|6|Mentioned|Fig.2|||||||||
9656|Knapdale Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
9656|Knapdale Quartzite|40648|6|Mentioned|p11|||||||||
9656|Knapdale Quartzite|40840|6|Mentioned|Map legend|||||||||
9656|Knapdale Quartzite|42173|6|Mentioned|p171|||See also Fig.1||||||
9656|Knapdale Quartzite|43638|5|Briefly described|p59|||||||||
9656|Knapdale Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
9656|Knapdale Quartzite|44271|14|Not recorded|21-62|||Not listed on white card.||||||
9656|Knapdale Quartzite|44275|14|Not recorded|Map Legend|||||||||
9656|Knapdale Quartzite|44276|14|Not recorded|Tb.1|||||||||
9656|Knapdale Quartzite|44278|2|Defined|p7,Tb.1,map||Paleoproterozoic|||||||07-NOV-08
9656|Knapdale Quartzite|44733|14|Not recorded|p697-699,732|||||||||
9656|Knapdale Quartzite|44846|14|Not recorded|p1430||Paleoproterozoic|Dugald River area.||||||07-NOV-08
9656|Knapdale Quartzite|44989|2|Defined|p.94-5|||Tb.III. On many pages. (F54-2).||||||
9656|Knapdale Quartzite|45166|4|Described|p32|||||||||
9656|Knapdale Quartzite|45287|14|Not recorded|p.226,227|||Contemp.with Roxmere Quartzite. Probably conformably overlies Corella Formation.||||||
9656|Knapdale Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
9656|Knapdale Quartzite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
9656|Knapdale Quartzite|50332|5|Briefly described|p16, p20, p81|Paleoproterozoic|Paleoproterozoic|Age correlative of the Surprise Creek Formation. Outcrops in the Wonga Subprovince. Consists of feldspathic, quartzose, calcareous and micaceous sandstone and quartzite, with minor siltstone and conglomerate.||||||07-FEB-11
9656|Knapdale Quartzite|61830|5|Briefly described|p178|||||||||
9656|Knapdale Quartzite|64248|6|Mentioned|p38 Fig.5|||||Unit in Mount Albert Group.||||
9656|Knapdale Quartzite|64250|6|Mentioned|p11 fig 3, p13 fig 5, p18|||||Unit in Mount Albert Group.||Is overlain conformably by Coocerina Formation. Shown as equivalent to Deighton Quartzite.|Feldspathic, quartzose, calcareous and micaceous sandstone and quartzite.|
9656|Knapdale Quartzite|65387|4|Described|p1, p3 Tb.1, p34-42, p82-84|Statherian|Statherian|Mount Isa region; eastern succession. Outcrops as well-exposed, prominent N-S oriented strike ridges. Maximum depositional age from detrital zircons. Appears as 1730 +/- 5 Ma in Tb.1. Youngest individual analysis is 1692 +/- 54 Ma. Younger zircons were probably derived from Wonga and Burstall Suites granites.|1728 +/- 5 Ma SHRIMP zircon (Carson et al. 2008)|Basal unit in Mount Albert Group.||Is overlain by Coocerina Formation.|Pink-orange, silicified quartzo-feldspathic sandstone, massive poorly-defined bedding.|
9656|Knapdale Quartzite|65396|5|Briefly described|p7, p16-17, p82, p84, p175, p182-184|Calymmian|Statherian|See also p186, p190, p241. Dugald River area, Mary Kathleen Fold Belt.||Mount Albert Group||Conformably overlain by Coocerina Formation. Overlies Corella Formation unconformably (locally conformably). Is correlated with Deighton Quartzite and possibly with Quamby Conglomerate.|Feldspathic, quartzose, calcareous and micaceous sandstone and quartzite.|
9656|Knapdale Quartzite|67323|5|Briefly described|GIS attrib tbl, p15, p25|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier. Calvert Superbasin.|1728 +/- 5 Ma MDA (Carson et al., 2008). |Mount Albert Group.||Unconformably overlies the Corella Formation. Equated with the Prize Supersequence.|Pink, fine-grained, feldspathic to quartzose, locally micaceous sandstone|
9656|Knapdale Quartzite|67539|6|Mentioned|p10|||||Of the Mount Albert Group.||||
9656|Knapdale Quartzite|68146|5|Briefly described|p3, p199-200|||Mary Kathleen and Marino-Stavely Domains. Geochronology by Carson et al. (2008).|1728 +/- 5 Ma maximum depositional age.|Basal Mount Albert Group.||Correlated with Roxmere and Deighton Quartzites.||
9656|Knapdale Quartzite|68732|5|Briefly described|p165 Fig.3, p167|Statherian|Statherian|Of the Prize Supersequence. Maximum sedimentary depositional age.|1728 +/- 5 Ma|||||30-NOV-17
9656|Knapdale Quartzite|69056|5|Briefly described|p54-55, Time-Space plot sheet|Statherian|Statherian|Mary Kathleen Domain. Time-equivalent to the Staveley-Roxmere sequence.|1728 +/- 5 Ma (Carson et al., 2008).|Lower Mount Albert Group.||Is overlain by Coocerina Formation. Equivalent to the Prize Supersequence.|Pink feldspathic and micaceous sandstone and quartzite.|
9656|Knapdale Quartzite|69591|4|Described|p38 Fig.2.22, p39, p45, p56|||Mary Kathleen Domain, Calvert Superbasin. Part of the Prize and Gun Supersequences. Shallow-marine deposits.|1730 +/- 5 Ma; 1728 +/- 5 Ma (MDA).|Mount Albert Group.||Is overlain by Coocerina Formation and Lady Clayre Formation.|Pink, fine-grained, feldspathic to quartzose, locally micaceous sandstone, with thin interbedded mudstone layer showing dessication cracks.|
9656|Knapdale Quartzite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Pink, fine-grained, feldspathic to quartzose, locally micaceous sandstone. Separately mapped: white fine-grained quartz sandstone; pink feldspathic-micaceous siltstone, minor pebble conglomerate; calcareous feldspathic medium sandstone, siltstone.|
9656|Knapdale Quartzite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes three unnamed members: white fine grained quartzose sandstone; pink feldspathic and micaceous siltstone with minor pebble conglomerate; calcareous feldspathic sandstone, quartzite and siltstone.||Mount Albert Group|Includes three unnamed members.||Pink fine grained, feldspathic to quartzose, locally micaceous sandstone.|
9656|Knapdale Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1728+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
9656|Knapdale Quartzite|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP age of 1728 +/- 5 Ma reported by Carson et al. (2008).|1728 +/- 5 Ma|||||
9656|Knapdale Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mary Kathleen Domain.|1730+/-5 Ma, 1728+/-5 Ma max. depositional ages||||Siliciclastics.|
9656|Knapdale Quartzite|73529|5|Briefly described|p5|Statherian|Statherian|Calvert Superbasin, early. Shallow marine setting.|1728+/-5 Ma maximum depositional age|Mount Albert Group||||
9656|Knapdale Quartzite|73553|5|Briefly described|p8 Fig.1.2.3|Statherian|Statherian||1728+/-5 Ma MDA|Mount Albert Group||||
9727|Kolonga Creek Limestone Member|30451|6|Mentioned|p26|||See also p29.||||||09-DEC-08
9727|Kolonga Creek Limestone Member|31586|6|Mentioned|p4|||Aphrophyllid corals||||||
9727|Kolonga Creek Limestone Member|31587|6|Mentioned|p60|||Distribution of Lithostrotion||||||
9727|Kolonga Creek Limestone Member|42547|5|Briefly described|p50|||||||||
9727|Kolonga Creek Limestone Member|44360|2|Defined|p1,7,8,10,24,30||Visean|Unit of Splinter Creek Formation.||||||
9727|Kolonga Creek Limestone Member|44487|14|Not recorded|p199|||Ref. to McKellar 1967.||||||
9727|Kolonga Creek Limestone Member|45097|6|Mentioned|p23|||Fossils. Correlation chart.||||||
9727|Kolonga Creek Limestone Member|70050|6|Mentioned|p341, p366|||Monto area. Contains Cionodendron coral fossils.||Splinter Creek Formation.||||
9750|Kondaparinga Formation|23423|5|Briefly described|p259||Middle Triassic|Underlying unit Pepper Pot Sandstone.||||||
9750|Kondaparinga Formation|42681|5|Briefly described|p22|||Unlikely to be misspelling of Kondoparinga Sandy Loam, SA.||||||
9750|Kondaparinga Formation|50316|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Geological Province: Ngarrabullgan Basin. Brown to white, or grey, fine to medium-grained sandstone, conglomeratic sandstone, claystone, mudstone, siltstone; minor granule to pebble conglomerate; finer grained rocks carbonaceous or ferruginous in part.||||||31-MAY-04
9750|Kondaparinga Formation|60425|3|Fully described|p14 Tb. 1, p109|Middle Triassic|Middle Triassic|Conformable on Pepper Pot Sandstone. Max. thickness: >200m. Fluvial deposits: mainly buff, brown or white interlayered claystone, mudstone, siltstone, sandstone; minor granule conglomerate.||||||07-FEB-11
9750|Kondaparinga Formation|69592|5|Briefly described|p244|Middle Triassic|Middle Triassic|Bultitude (1997). Over 200m of sediments in the upper part of a hole drilled on top on Mount Mulligan. Age from palynomorphs.||||Overlies Pepper Pot Sandstone.|Interlayered claystone, mudstone, siltstone, sandstone and minor granule conglomerate.|
9802|Kooralbyn member|48917|6|Mentioned|p17|||Refers Pearce (1964)||||||
9839|Koukandowie Formation|12597|5|Briefly described|p491, p492 Tb.1|Bathonian|Toarcian|Clarence-Moreton Basin. 250m thick. Generally fluviatile. Basal claystones include (shallow lacustrine?) chamositic oolite beds containing acritarch-bearing horizons.||Unit in Marburg Subgroup.|||Predominantly arenaceous: fine- to coarse-grained quartzose to quartz-lithic sandstone, with a variable sandstone/siltstone/shale sequence at the base.|
9839|Koukandowie Formation|13516|5|Briefly described|p159 fig 8|Jurassic|Jurassic|From Clarence-Moreton Basin.||Of Marburg Subgroup|Includes Ma Ma Creek Member, Heifer Creek Sandstone Member|||
9839|Koukandowie Formation|22857|5|Briefly described|p318-9 Figs. 22.10 A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Interbedded sandstone, siltstone, claystone, coal. Contains the Heifer Creek Sandstone, Ma Ma Creek and Towallum Members. Max. thickness: 400m. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|22865|6|Mentioned|Fig.22.10ap318|||||||||
9839|Koukandowie Formation|23799|4|Described|p48, p10 Tb. 1|Middle Jurassic|Early Jurassic|Upper unit of Marburg Subgroup (Bundamba Group).  Includes Ma Ma Creek and Heifer Creek Sandstone Members.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Marburg Subgroup.||||||
9839|Koukandowie Formation|23811|5|Briefly described|Map Legend|Bajocian|Aalenian|Of Marburg Subgroup.  Fine- to coarse-grained, quartz to quartz-lithic sandstone in fining-up sequences.  Crossbedded and rippled; thin pebble conglomerates at base of sand channels; shale and siltstone.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
9839|Koukandowie Formation|23812|5|Briefly described|p34 Tb.4|Middle Jurassic|Early Jurassic|Of Bundamba Group.  Maximum thickness: 400m. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Marburg Subgroup (Bundamba Group).||||||
9839|Koukandowie Formation|41631|4|Described|p18|||See also Fig.2||||||
9839|Koukandowie Formation|42248|2|Defined|App.1 p410|Bajocian|Toarcian|Age: late Toarcian to early Bajocian.||||||21-NOV-21
9839|Koukandowie Formation|42463|6|Mentioned|Fig.3 P170|||||||||
9839|Koukandowie Formation|42869|5|Briefly described|Table 1, P33|||of Marburg Subgroup||||||
9839|Koukandowie Formation|42893|6|Mentioned|p11|||||||||
9839|Koukandowie Formation|42951|5|Briefly described|Fig.11|||Of Marburg Subgroup.||||||27-AUG-08
9839|Koukandowie Formation|43150|5|Briefly described|Map Legend||Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
9839|Koukandowie Formation|43736|5|Briefly described|Table 1,p4|||||||||
9839|Koukandowie Formation|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Marburg Subgroup.  Overlies: Gatton Sandstone.  Underlies: Walloon Coal Measures, Main Range Volcanics.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
9839|Koukandowie Formation|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
9839|Koukandowie Formation|60281|5|Briefly described|p22, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group).  Contains the Heifer Creek Sandstone and Ma Ma Creek Members, and Towallum Basalt. Overlies the Gatton Sandstone; underlies the Walloon C.M.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60993|3|Fully described|p6 Fig. 2, p27|||Supersedes Koukandowie Sst Mbr. Mixed sandstone, siltstone and shale unit. Conformably overlain by Walloon Coal Measures; conformably overlies Gatton Sst. Max. thickness: ~345m. Geol. Prov: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60995|4|Described|p65-66, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Marburg Subgroup. Originally called "Marburg Formation" in NSW.  Interbedded sandstone, siltstone, claystone, coal; detailed lithology presented (p66).  Max. thickness: 400m. Geological Province: Clarence-Moreton Basin. ||||||
9839|Koukandowie Formation|60996|5|Briefly described|p72, p113|||Of the Marburg Subgroup (Bundamba Group). Contains the Ma Ma Creek Member and heifer Creek Sandstone Member. Conformably overlies Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60997|5|Briefly described|p138|Callovian|Toarcian|Conformably overlies Gatton Sandstone; conformably overlain by Walloon C.M. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2.||||||
9839|Koukandowie Formation|60998|5|Briefly described|p146 Fig. 2|||Of the Marburg Subgroup. Overlies the Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60999|5|Briefly described|p164, p174|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p176-177.||||||
9839|Koukandowie Formation|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61002|6|Mentioned|p202|||Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61004|5|Briefly described|p230, p232 Fig. 2|Jurassic|Jurassic|Of the Marburg Subgroup (Bundamba Group). Oil mature unit in the western and central parts of NSW.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
9839|Koukandowie Formation|61006|5|Briefly described|p277, p289|Jurassic|Jurassic|Includes the Ma Ma Creek and Heifer Creek Members. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
9839|Koukandowie Formation|63748|5|Briefly described|p21|||Top part of Marburg Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9839|Koukandowie Formation|64289|5|Briefly described|p6 Fig. 2|Middle Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Includes the Ma Ma Creek and Heifer Creek Members. Overlies Gatton Sandstone. Max. thickness: 250m. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9839|Koukandowie Formation|64665|5|Briefly described|p53 Fig.2, p59.|Middle Jurassic|Early Jurassic|Clarence-Moreton Basin.||Upper unit in Marburg Subgroup.|Includes Ma Ma Creek Member and Heifer Creek Sandstone Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.||
9839|Koukandowie Formation|67402|5|Briefly described|p165 tbl LPB1|Aalenian|Sinemurian|Clarence-Moreton Basin. Deposited in fresh water lakes or lagoon environments. In excess of 150m thick. See also p188, p190, p190 fig CLM6, p193.||Marburg Subgroup|Includes the Ma Ma Creek Member and the Heifer Creek Sandstone Member.|Overlies the Gatton Sandstone. Overlain by the Walloon Subgroup.|Sandstone, siltstone and shale.|
9839|Koukandowie Formation|68135|5|Briefly described|p52 fig 2b|Bajocian|Pleinsbachian|Clarence-Moreton Basin. Includes plant macrofossils and invertebrate fossils. ||||Overlies Gatton Sandstone, overlain by Walloon Coal Measures|Silty sandstone with oolitic ironstone beds.|14-SEP-17
9839|Koukandowie Formation|69297|5|Briefly described|p487 fig 5.38, p488, p489, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 50-400m thick. Deposited as overbank or flood plain deposits as part of a meandering fluvial system. Good potential as a hydrocarbon source rock.  ||Mauburg Subgroup|Includes the Heifer Creek Sandstone Member, Ma Ma Creek Member and the Towallum Basalt.|||
9839|Koukandowie Formation|69594|4|Described|p519, p536 Fig.7.17, p544-547, p572|Toarcian|Toarcian|Clarence-Moreton Basin. Weakly sinuous river deposits with linguoid bars. Appears as Koukandouie Formation in Fig.7.17.||Marburg Subgroup.|Heifer Creek Sandstone Member, Ma Ma Creek Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.|Mixed sandstone, siltstone and shale; near the base in the head of the Lockyer Valley is a 25m unnamed member of stacked quartz-lithic channel-sandstones with planar and trough cross-bed sets interpreted as dunes, transverse bars and sand waves.|
9839|Koukandowie Formation|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Marburg Subgroup.|Includes Ma Ma Creek, and Heifer Creek Sandstone, Members.|||
9839|Koukandowie Formation|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
9839|Koukandowie Formation|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Marburg Subgroup.|Ma Ma Creek Member, Heifer Creek Sandstone Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.||
9839|Koukandowie Formation|71805|5|Briefly described|p76|Bajocian|Pleinsbachian|Clarence-Moreton Basin.||Marburg Subgroup|Includes the Ma Ma Creek Member and the Heifer Creek Sandstone Member.|||
9839|Koukandowie Formation|72921|5|Briefly described|p15 Fig.2.|Middle Jurassic|Early Jurassic|Shown as located within the Clarence-Moreton Basin. Along with Evergreen Formaiton, shown as including the Westgrove Ironstone Member in Fig.2.||||Overlies Gatton Sandstone and underlies Walloon Coal Measures||10-JUN-22
9839|Koukandowie Formation|73570|6|Mentioned|p912 Fig.2, p913-914, p915 Fig.4|Middle Jurassic|Middle Jurassic|Clarence-Morton Basin.||||||
9866|Kukiandra Formation|23422|5|Briefly described|p180, p206 Table 6.3|Late Devonian|Late Devonian|Of Dotswood Group.||||||
9866|Kukiandra Formation|23430|5|Briefly described|p505|||||||||
9866|Kukiandra Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Dotswood Group.||||||
9866|Kukiandra Formation|23893|5|Briefly described|p16|Late Devonian|Late Devonian|Of Dotswood Group. Geological Province: Burdekin Basin.||||||04-FEB-08
9866|Kukiandra Formation|24613|2|Defined|p9 Fig. 4, p34, p43|Frasnian|Frasnian|Formerly the informal "Kukiandra Conglomerate". Conformable below undiff'd Keelbottom Gp; over Cultivation Gully Fm in places.Thickness: ~250m in type section. Geol.prov: Burdekin Basin. Lith.details for this sublabile feldspathic to lithic sst included||||||07-FEB-11
9866|Kukiandra Formation|24614|5|Briefly described|p196 Fig. 5|Famennian|Famennian|Alluvial fan deposits.||||||07-FEB-11
9866|Kukiandra Formation|42295|6|Mentioned|p6|||||||||
9866|Kukiandra Formation|43935|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Dotswood Group||||||22-FEB-05
9866|Kukiandra Formation|62522|2|Defined|p27-28|Late Devonian|Late Devonian|Of the Dotswood Group. Formerly Kukiandra Conglomerate. Calcareous pebbly to cobbly polymictic conglomerate + reworked limestone clasts, feldspathic-lithic sst, +greyish red siltst.+fine-gr.sst. Thickness: ~250m in type section. Geol.prov: Burdekin Basin||||||
9866|Kukiandra Formation|67402|5|Briefly described|p246|Famennian|Frasnian|Burdekin Basin. ||Dotswood Group||Overlies the Stud Formation.|Conglomerates.|
9866|Kukiandra Formation|68731|5|Briefly described|p185 Tb 3.4|Upper Devonian|Upper Devonian|Exhibits a restricted distribution in the south on MINGELA and is characterised by limestone pebbles derived from the Burdekin Formation. > 250 m thick.||Of the Dotswood Group.||Likely coeval with the Julia Formation.|Comprises massive, poorly sorted, pebble to cobble polymict conglomerate with reworked limestone clasts. Fine to very coarse feldspathic to lithic sandstone. Siltstone, in part red, with sporadic mudcracks.|
9872|Kulangoor Formation|42316|6|Mentioned|p5|||||||||
9872|Kulangoor Formation|42893|5|Briefly described|p6|||||||||
9904|Kumbarilla beds|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p494, p495 Fig.3|Early Cretaceous|Late Jurassic|See also p497. N Clarence-Moreton Basin.||||Interfingers with Pilliga Sandstone.|Fine- to medium-grained lithic to quartzose sandstones with siltstone, mudstone and minor thin pebble conglomerates.|
9904|Kumbarilla beds|22857|6|Mentioned|p315 Fig. 22.8|||Geological Province: Surat Basin.||||||
9904|Kumbarilla beds|22865|6|Mentioned|Fig22.8p315|||||||||
9904|Kumbarilla beds|23799|5|Briefly described|p138|Early Cretaceous|Jurassic|||||||
9904|Kumbarilla beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
9904|Kumbarilla beds|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
9904|Kumbarilla beds|39413|6|Mentioned|p53|||||||||
9904|Kumbarilla beds|40623|5|Briefly described|p109|||||||||
9904|Kumbarilla beds|43150|5|Briefly described|Map Legend|Cretaceous|Jurassic|Geological Province: Surat Basin.||||||12-APR-05
9904|Kumbarilla beds|60281|6|Mentioned|p27|||Probably replaces Kumbarilla Beds?  Lithic clastics.  Geological Province: Clarence-Moreton Basin.||||||23-MAR-05
9904|Kumbarilla beds|60993|5|Briefly described|p34|Late Cretaceous|Middle Jurassic|Sandstone, siltstone, mudstone and conglomerate. Overlies the Walloon Coal Measures in the Cecil Plains Sub-basin western margin region.||||||28-AUG-12
9904|Kumbarilla beds|61377|5|Briefly described|p149 Fig. SU8|||||||||07-FEB-11
9904|Kumbarilla beds|63729|5|Briefly described|Map legend|Cretaceous|Jurassic|Interfingers with Walloon Coal Measures and upper part of Marburg Subgroup. Thickly bedded, medium- to coarse-grained quartzose sandstone and conglomerate.||||||11-DEC-07
9904|Kumbarilla beds|63748|5|Briefly described|p21, p23|Cretaceous|Jurassic|Overlie Marburg Subgroup and Walloon Coal Measures. Max. thickness: ~800m. Geological province: Surat Basin. Mostly thick beds of cross-bedded, medium- to coarse-grained quartzose sandstone and pebble conglomerate.||||||07-FEB-11
9904|Kumbarilla beds|64856|5|Briefly described|p90, p94, p96-98|||Lowermost part is easterly equivalent of Springbok Sandstone. Middle part equivalent to Gubberamunda Sandstone. Upper part equivalent to Orallo Formation, Mooga Sandstone. Uppermost part equivalent to Bungil Formation.| |||||29-NOV-17
9904|Kumbarilla beds|65003|6|Mentioned|p29|||||||Overlies the Juandah Coal Measures.||30-MAR-12
9904|Kumbarilla beds|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||||
9904|Kumbarilla beds|68003|6|Mentioned|p57 Fig.3-n.|||Bowen Basin.||||||
9904|Kumbarilla beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, are all mapped under the symbol, JKb.||||||
9904|Kumbarilla beds|68679|6|Mentioned|p455|Early Cretaceous|Early Jurassic|||||||
9904|Kumbarilla beds|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic |||||||26-SEP-18
9904|Kumbarilla beds|69594|5|Briefly described|p537-538|||Mentioned as having elements that correlate with the Gubberamunda Sandstone and Orallo Formation.||||Laterally grades into the Mooga Sandstone. Part-equivalent to Bungil Formation.||
9904|Kumbarilla beds|70821|5|Briefly described|p80|||Surat, Clarence-Moreton Basins.||||Overlies Pilliga Sandstone or Walloon Coal Measures. Is overlain by Wallumbilla Formation.||
9904|Kumbarilla beds|72297|6|Mentioned|p758|Mesozoic|Mesozoic|In the Chinchilla area, hosts petrified wood in unconsolidated gravels capping low ridges.||||||
9904|Kumbarilla beds|72298|5|Briefly described|p801|Cretaceous|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Pilliga Sandstone and Walloon Coal Measures. Is overlain by Doncaster Member (Wallumbilla FZ).||
9919|Kuridala Group|42556|6|Mentioned|p5|||Variation on Kuridala Formation.||||||
9919|Kuridala Group|67323|4|Described|p18-21, p25, p34, p39, p107|||See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot. Kuridala-Selwyn Domain, Mount Isa Inlier. Informally subdivided to distinguish mafic intrusives. Low magnetic response; linear belts of metadolerite sills produce higher response. Turbidite succession deposited on a continental slope. Tightly folded and metamorphosed (lower amphibolite facies) during the Isan Orogeny. Future studies may consider dropping the dual nomenclature with Soldiers Cap Group.|Deposition started ~1690-1670 Ma.||Includes Hampden Slate, Kuridala Formation, New Hope Sandstone, Starcross Formation|Correlated with Soldiers Cap Group. Is intruded by Williams Supersuite (Mount Dore and Yellow Waterhole Granites). Is thrust under Mount Dore Granite.|Includes metadolerite, metabasalt and amphibolite; mainly sills, intruding units of the Kuridala Group|
9919|Kuridala Group|67539|6|Mentioned|p13, p14|||Previously Kuridala Formation. Formations are all time and lithological equivalents of Soldiers Cap Group units.|||Includes basal Starcross Formation, middle New Hope Sandstone, and upper Answer Slate.|Equivalent to Soldiers Cap Group.||
9919|Kuridala Group|68146|5|Briefly described|p3-4, p113-114, p201|||Formerly Kuridala Formation, until this latter unit had part excised as the Starcross Formation. Dating suggests the three components of this Group cannot be correlated directly with those of the Soldiers Cap Group; may only be equivalent to the upper part of the latter.|||Starcross Formation.|||
9919|Kuridala Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
9919|Kuridala Group|69056|5|Briefly described|p2, p13, p18, p23, p28, p55|Statherian|Statherian|See also Time-Space plot sheet. Kuridala-Selwyn Domain. Modelling values listed.|||Starcross Formation, New Hope Sandstone, Hampden Slate.|Time-equivalent of Soldiers Cap Group.||
9919|Kuridala Group|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Hampden Slate, New Hope Sandstone|||
9919|Kuridala Group|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Hampden Slate, New Hope Sandstone|||
9919|Kuridala Group|69591|5|Briefly described|p29, p41, p43, p46, p55|Paleoproterozoic|Paleoproterozoic|The dominant unit in the Kuridala-Selwyn Domain, Calvert Superbasin. A turbidite succession deposited on a continental slope. Geographically separated from the Soldiers Cap Group by a belt of Staveley Formation and Squirrel Hills Granite. |||Answer Slate, Starcross Formation, New Hope Sandstone, Hampden Slate.|Is adjacent to the Soldiers Cap Group subsurface.||
9919|Kuridala Group|69952|5|Briefly described|p4, p51, p53-54|||Kuridala-Selwyn Domain, North Australian Craton. This latest age determination of the Hampden Slate conflicts with previous age determinations of the bottom-most unit; the authors suggest that the stratigraphy of the Kuridala Group needs reassessing. It also appears to refute the previous (eg Hutton and Withnall, 2013) correlation with the Toole Creek Volcanics.|||Includes Hampden and Answer Slates and Starcross Formation.|||
9919|Kuridala Group|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.|||Hampden Slate, New Hope Sandstone, Starcross Formation|Overlies Mount Albert Group. Is equivalent to Soldiers Cap Group.|Psammitic and pelitic schist; quartzose to feldspathic metasandstone and mica schist; carbonaceous slate and metasiltstone, minor schist, calcareous and banded calc-silicate rocks. Intruded by metadolerite, metabasalt and amphibolite sills.|05-MAY-16
9919|Kuridala Group|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala- Selwyn Domain. |||Includes Hampden Slate, New Hope Sandstone, Starcross Formation.|||
9919|Kuridala Group|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.|||Includes Hampden Slate, New Hope Sandstone, Starcross Formation.|||20-JAN-22
9919|Kuridala Group|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.|||Includes Hampden Slate, New Hope Sandstone, Starcross Formation.|||
9919|Kuridala Group|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1674+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
9919|Kuridala Group|71799|6|Mentioned|p154, p160|||Eastern Fold Belt, Mt Isa.||||||
9919|Kuridala Group|72297|5|Briefly described|p758|||Amethyst occurs in veins, 65km S of Cloncurry.|||||Includes pegmatite and muscovite schist.|
9919|Kuridala Group|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kuridala-Selwyn Domain.|||Includes Hampden Slate and New Hope Sandstone.|||
9919|Kuridala Group|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kuridala-Selwyn Domain.|||Includes Hampden Slate and New Hope Sandstone.|||
9919|Kuridala Group|72889|5|Briefly described|p2, p4,5,6, p8, p33, p54.||||||Includes Starcross Formation, Hampden Slate.|Laterally equaivalent to the Soldiers Cap Group.|Metamorphosed sedimentary succession with basal micaceous psammopelitic beds interbedded with coarse-grained, quartzose and locally feldspathic sandstone packages.|
9919|Kuridala Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
9919|Kuridala Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
9951|Kuttung Formation|22757|4|Described|Table4,p10|Carboniferous|Late Devonian|Conformable on Texas Beds. Unconformably underlies Back Creek Group.||||||
9951|Kuttung Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
9951|Kuttung Formation|29721|6|Mentioned|p267|||||||||
9951|Kuttung Formation|30692|6|Mentioned|Map legend|Late Carboniferous|Early Carboniferous|Lower to Upper Carboniferous||||||
9951|Kuttung Formation|30699|6|Mentioned|p55|||||||||
9951|Kuttung Formation|30701|6|Mentioned|Map legend|Carboniferous|Late Devonian|Upper Devonian to Upper Carboniferous||||||
9951|Kuttung Formation|31118|6|Mentioned|Fig. 4|||||||||
9951|Kuttung Formation|32276|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|Upper Devonian? to Upper? Carboniferous. Prob.Upper Carboniferous||||||
9951|Kuttung Formation|33091|5|Briefly described|p6|||Stratigraphy||||||
9951|Kuttung Formation|33451|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9951|Kuttung Formation|34613|6|Mentioned|Table 3|||||||||
9951|Kuttung Formation|39907|6|Mentioned|Fig.3|||||||||
9951|Kuttung Formation|42634|5|Briefly described|p8|||||||||
9951|Kuttung Formation|43000|5|Briefly described|p106|||||||||
9951|Kuttung Formation|43003|5|Briefly described|p168|||||||||
9951|Kuttung Formation|43008|5|Briefly described|map legend|||||||||
9951|Kuttung Formation|43925|14|Not recorded|p30,32,Fig.3|||||||||
9951|Kuttung Formation|44163|14|Not recorded|p11|||||||||
9951|Kuttung Formation|44166|14|Not recorded|p1,10,15,Pl.1||Carboniferous|K-Ar: 300+/- 10 Ma.||||||
9951|Kuttung Formation|44567|14|Not recorded|p10-17|||Not shown on white card.||||||
9951|Kuttung Formation|44585|14|Not recorded|p45-Fig.2|||||||||
9951|Kuttung Formation|44627|14|Not recorded|p139-143|Early Permian|Devonian|Unit of Horton Gruop.||||||
9951|Kuttung Formation|48600|14|Not recorded|p3-7,24|Early Permian|Carboniferous|Formation of Horton Group.||||||
9951|Kuttung Formation|61377|5|Briefly described|p150|Early Permian|Late Carboniferous|Sequence of marine to non-marine andesitic volcanics and volcaniclastics. Limited reservoir potential. Unconformably overlain by the Back Creek Group. Geological Province: Surat, Gunnedah and Bowen Basins.||||||07-FEB-11
9951|Kuttung Formation|67669|5|Briefly described|p11-12,22-23|Late Carboniferous|Late Carboniferous|Of Bowen Basin. Part of the basement assemblage to the Bowen Basin. Also known as Cracow Formation. Intersected in inglestone-1 borehole at 3.8 km depth, as modelled on Line 270.||||Overlain by, and laterally grades into Timbury Hills Formation. Also overlain by Camboon and Connors volcanics.||
9996|Lacon Creek Chert Member|42547|4|Described|p52|||See also Lacon Creek Member.||||||09-DEC-08
